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SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT vs GOODSON FARMS, INC., 02-001117 (2002)
Division of Administrative Hearings, Florida Filed:Tampa, Florida Mar. 19, 2002 Number: 02-001117 Latest Update: Dec. 16, 2002

The Issue The issue is whether Respondents should be subject to civil penalties and required to submit a Compliance Plan for the reasons stated in the Administrative Complaint and Order filed on January 8, 2002.

Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Background In this enforcement action, Petitioner, Southwest Florida Water Management District (District), proposes to assess civil penalties against, and require a compliance plan from, Respondents, Balm Associates, Inc. (Balm) and Goodson Farms, Inc. (Goodson), on the grounds that from March 1999 through July 2001 they made water withdrawals from certain property in Hillsborough County, Florida, without a water use permit, and after a permit was obtained in August 2001, they continued to exceed the annual average daily withdrawals authorized under the permit through the month of November 2001, or just prior to the preparation and issuance of the Administrative Complaint and Order (Complaint).1 While not denying that excessive pumpages may have occurred, and that a permit was not obtained until August 2001, Balm points out that it is the owner-lessor of the property and not the consumptive user of the water, and contends that the District has no authority to enforce its rules against, and recover civil penalties from, the non-user of the water. In its request for a hearing, Goodson did not specifically dispute the allegation that it consumed water without a permit, or exceeded the withdrawal limits under the new permit, but contended instead that the limits were unrealistic and should be modified. At the final hearing, however, Goodson disputed the accuracy of the water consumption figures used in the Complaint. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries and to administer and enforce Chapter 373, Florida Statutes. Balm is a corporation registered to do business in the State of Florida. Its mailing address is 2101 Huntington Avenue, Sarasota, Florida 34232. It owns approximately 220 acres of land in Section 28, Township 31 South, Range 21 East, in Hillsborough County, Florida, which is the site of the alleged wrongdoing. Goodson is a corporation registered to do business in the State of Florida. Its mailing address is Post Office Box 246, Balm, Florida 33503. Goodson is in the farming business and operates a total of 13 farms, including the farm at issue in this proceeding. Permit Requirements Under Rule 40D-2.041(1), Florida Administrative Code, a water use permit is required whenever total withdrawal capacity from any source or combined sources is greater than or equal to 1,000,000 gallons per day (gpd); annual average withdrawal from any source or combined sources is greater than or equal to 100,000 gpd; or withdrawal is from a well having an outside diameter of 6 inches or more at the surface. Rule 40D-2.351(1), Florida Administrative Code, provides that a permittee must notify the District within 30 days of the sale or conveyance of permitted water withdrawal facilities or the land on which the facilities are located. The same rule also provides that where a permit has been issued to a party whose ownership or legal control of the permitted water withdrawal facilities subsequently ends, the party who assumes control over the facilities may apply to transfer the permit to himself or herself up to the renewal date of the transferor's permit. Finally, Rule 40D-2.351(2), Florida Administrative Code, provides that until a permit is transferred or a new permit is obtained, the party subsequently controlling the permitted water withdrawal facilities will be in violation of District rules for making withdrawals without the required permit. History of Permits on the Property On September 29, 1989, the District issued Water Use Permit No. 207135.001 (the .001 permit) to James Brown (Brown) and B & T Growers Partnership (B & T) for water withdrawals from one well for agricultural purposes on Balm's property. The .001 permit authorized annual average withdrawals of 102,000 gpd of groundwater for agricultural irrigation. On August 29, 1990, the District adopted new rules applicable to District permits within the Eastern Tampa Bay Water Use Caution Area (ETBWUCA). The .001 permit was within the ETBWUCA, and Brown and B & T were provided with a Notice of Permit Modification and new Permit Conditions. The new conditions became effective November 15, 1990. New Condition No. 5 provided that By July 31, 1995, all permitted withdrawal points shall be equipped with totalizing flow meters or other measuring devices as approved in writing by the Director, Resource Regulation Department. Such devices shall have and maintain accuracy within five percent of the actual flow installed. On December 14, 1992, the District approved the transfer of the .001 permit from Brown and B & T to B. Kenda Produce. The Unpermitted Water Withdrawals On June 30, 1997, Goodson entered into a two-year agricultural lease with Balm to use a portion of the property, including acreage previously used by B. Kendra Produce. At the time the lease was entered into, neither Respondent applied to the District to have the .001 permit transferred from B. Kendra Produce. It can be reasonably inferred from the evidence that after the first lease expired, the parties continued to execute new lease agreements at least through the time of the hearing. The portion of the property which Goodson leased and farmed is referred to as the "Sweat Loop Farm" and consists of approximately 100 acres. There is one well with an outside diameter of 10 inches at the surface located on the Sweat Loop Farm. The well's total withdrawal capacity is approximately 1,500 gallons per minute (gpm), which is over 1,000,000 gpd. Thus, withdrawals from the well required a water use permit. As noted earlier, Goodson operates a total of 13 farms on approximately 2,500 acres of land. There are approximately 15 wells on all 13 farms, including the Sweat Loop Farm. Michael E. Hare, an irrigation supervisor who is responsible for the irrigation of all 13 of Goodson's farms, installed a total of approximately 8 meters on the farms, including the meter on the Sweat Loop Farm. A totalizing flow meter, which was made by MiCrometer, was installed at the Sweat Loop Farm in June 1997. Mr. Hare acknowledged that he was familiar with MiCrometer meters and would be aware if the MiCrometer flow meter on the Sweat Loop Farm was not functioning properly. Whenever metering devices on the various Goodson farms have malfunctioned in the past, Mr. Hare has taken the malfunctioning meter to a metering company to be fixed. Goodson began irrigating the Sweat Loop Farm in June 1997. Since that time, Goodson has been the sole water user of the well on the farm. In March 1999, Goodson began submitting to the District monthly pumpage reports for the groundwater withdrawals on the Sweat Loop Farm. Although some unmeasured withdrawals presumably occurred prior to March 1999, the Complaint does not identify these as being a violation. Mr. Hare and other supervisors are responsible for collecting the meter readings which go on the monthly pumpage reports and providing them to the District. The information on the reports includes the permit number; the last month's meter reading; the current month's meter reading; the total gallons of water pumped for the current month; the meter total; and the meter factor. To determine the average daily withdrawal on the Sweat Loop Farm, the District relied upon the calculations provided by Goodson as to the total gallons of water pumped for the month and divided this number by 30 days. From March 1999 through July 2001, these quantities were as follows: MONTH/YEAR AVERAGE DAILY PUMPAGE March 1999 April 1999 531,487 No data available May 1999 364,930 June 1999 0 July 1999 0 August 1999 57,410 September 1999 49,563 October 1999 222,667 November 1999 250,667 December 1999 755,003 January 2000 689,433 February 2000 695,073 March 2000 544,427 April 2000 305,153 May 2000 597,720 June 2000 0 July 2000 62,120 August 2000 86,370 September 2000 123,233 October 2000 602,020 November 2000 409,550 December 2000 145,823 January 2001 957,690 February 2001 890,213 March 2001 391,280 April 2001 467,640 May 2001 617,177 June 2001 0 July 2001 0 Under Rule 40D-2.041(1)(a)-(c), Florida Administrative Code, a water use permit was required for Goodson's withdrawals since the well's total withdrawal capacity is approximately 1,500 gpm, which is greater than 1,000,000 gpd; the annual average withdrawals exceeded 100,000 gpd; and the well has an outside diameter of 10 inches at the surface. The withdrawals on the Sweat Loop Farm were not authorized by the .001 permit since neither Goodson or Balm was a permittee under the permit. Even if Goodson could rely on the permit, which it cannot, pumpage data provided by Goodson reflects that the water withdrawals (except for nine months) were in excess of that authorized by the permit. On June 16, 2000, the District mailed a Notice of Non-Compliance for excessive water withdrawals to Goodson. The Notice indicated that if the pumpage values submitted by Goodson were incorrect, Goodson was to explain the error and provide corrected quantities. On June 26, 2000, the District received a written response to the Notice of Non-Compliance from the superintendent of the Sweat Loop Farm who indicated that the pumpage values were correct, and that the excess usage was due to a "serious drought condition" which had caused a "significant financial hardship on [the] farm." The response also indicated that Goodson would contact Mr. Haftel, owner of Balm, to request that he "revise the water use permit for spring crops." On November 22, 2000, the District mailed Goodson a Notice of Violation indicating that the quantities authorized by the .001 permit were still being exceeded and that the District might seek monetary penalties if Goodson failed to come into compliance within 30 days. Despite the foregoing Notice, Goodson continued to make withdrawals without a permit and in excess of the quantities formerly authorized under the .001 permit until August 2001 when a new permit was finally obtained. Issuance of a New Water Use Permit On January 2, 2001, the District received an application for a General Water Use Permit seeking to modify the .001 permit to increase the withdrawal quantities and to transfer the permit from B. Kendra Produce to Balm. "Seymour Haftel/ Balm Associates, Inc." was listed as the applicant, and "Donn Goodson" from " Goodson Farms" was listed as the contact or consultant. Mr. Haftel signed the application on behalf of Balm. Goodson assisted Balm in securing the permit for the Sweat Loop Farm because Goodson wanted more water for irrigation purposes. Section 2.1 of the Basis of Review for Water Use Permit Application, adopted and incorporated by reference by Rule 40D-2.091, Florida Administrative Code, provides that "[a]pplications for leased property, except property leased from the District, must be either a joint application in the name of the lessee and the property owner(s) or be only in the name of the property owner(s)." In a Request for Additional Information mailed to Balm on January 29, 2001, the District asked whether Goodson should be listed as co-applicant on the application. On April 27, 2001, Balm submitted a response which indicated that Goodson should not be listed as co-applicant. On August 6, 2001, the District issued Water Use Permit No. 200007135.002 (the .002 permit) to Seymour Haftel/Balm Associates, Inc. authorizing an increase in the annual average withdrawals to 224,300 gpd. The permit had an expiration date of September 29, 2009. The permit contained a number of special conditions, none of which were challenged by Balm. Unauthorized Withdrawals Under the .002 Permit Special Condition No. 2 of the .002 permit requires in part that the permittee: continue to maintain and operate the existing non-resettable, totalizing flow meter(s), or other flow measuring device(s) as approved by the Regulation Department Director, Resource Regulation, for District ID No(s), Permittee ID No(s)[,] G-1. Such device(s) shall maintain an accuracy within five percent of the actual flow as installed. Total withdrawal and meter readings from each metered withdrawal shall be recorded on a monthly basis and reported to the Permit Data Section, Records and Data Department, (using District forms) on or before the tenth day of the following month. In the event a permittee chooses not to use a totalizing flow meter, as required by Special Condition No. 2, the District will review information provided by the measuring device's manufacturer to determine if the measuring device would maintain a five percent accuracy as required by the Condition. The meters have to be monitored and calibrated periodically for accuracy. It is the permittee's responsibility to comply with the conditions of the permit, including Special Condition No. 2, which requires the submittal of accurate pumpage reports. Goodson submitted the meter readings on behalf of Balm beginning in September 2001, which covered the withdrawals for the month of August 2001. The District relied on the meter readings submitted by Goodson to determine the annual average daily pumpage calculation for the .002 permit. The calculation is a running 12-month average, whereby each month the annual average daily quantity is recalculated based on the previous 12-month pumpage. The running annual average daily pumpage and percentage of pumpage which exceeded the .002 permit from August 2001 through May 2002 are as follows: MONTH/YEAR ANNUAL AVERAGE DAILY PUMPAGE PERCENTAGE OVERPUMPED August 2001 378,462 69 percent September 2001 382,622 71 percent October 2001 376,687 68 percent November 2001 383,008 71 percent December 2001 379,212 69 percent January 2002 327,343 46 percent February 2002 321,530 43 percent March 2002 350,701 56 percent April 2002 356,013 59 percent May 2002 338,131 51 percent As the foregoing data reflects, the withdrawals from the Sweat Loop Farm were in excess of that authorized by the .002 permit from August 2001 through May 2002.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Southwest Florida Water Management District enter a final order determining that Respondents are guilty of the charges in its Administrative Complaint and Order except as concluded in paragraph 48 above and endnote 2 below; that Respondents be required to submit an acceptable written plan (Compliance Plan) to the District for its consideration and approval within fourteen days after entry of the final order; that the Compliance Plan describe how Respondents shall achieve full compliance with the .002 permit; that the Compliance Plan include reductions in withdrawals, water conservation measures, and development and utilization of alternative resources; that the Compliance Plan establish deadlines for implementation and completion of corrective actions; that full compliance be achieved within 120 days after entry of the final order; and that any failure of Respondents to comply with any provision of the Compliance Plan shall constitute a violation of the final order. DONE AND ENTERED this 30th day of July, 2002, in Tallahassee, Leon County, Florida. ___________________________________ DONALD R. ALEXANDER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 30th day of July, 2002.

Florida Laws (5) 120.56120.569120.57373.119373.219
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SAVE OUR BAYS AND CANALS ASSOCIATION vs TAMPA BAY WATER AND DEPARTMENT OF ENVIRONMENTAL PROTECTION, 00-002010 (2000)
Division of Administrative Hearings, Florida Filed:Tampa, Florida May 11, 2000 Number: 00-002010 Latest Update: Aug. 18, 2000

The Issue The issue is whether Respondent Department of Environmental Protection may issue to Respondent Tampa Bay Water a variance from the requirements, in Rules 62-555.520(4)(c) and (d), Florida Administrative Code, that an application for a permit to construct and operate a drinking water system contain drawings of the project with sufficient detail to describe clearly the work to be undertaken and complete specifications of the project to supplement the drawings.

Findings Of Fact Inception of Tampa Bay Water, Consolidated Permit, and Other Documentation for the Production of Drinking Water Respondent Tampa Bay Water (TBW) is a wholesale public water supply utility. TBW is governed by a nine-member board of directors with one member each from the municipalities of Tampa, St. Petersburg, and New Port Richey and two members each from the counties of Hillsborough, Pinellas, and Pasco. The purpose of TBW is to use group resources to find regional solutions to the problems of water supply in the region. Over two million persons in the three-county area rely on TBW for their drinking water. The predecessor of TBW was the West Coast Regional Water Supply Authority (WCRWSA), which was created in 1974. The West Coast Regional Water Supply Authority was also a wholesale public water supply authority. However, the authority operated as a cooperative entity, and TBW operates as a regulatory entity. In 1996, WCRWSA sought to renew its permit from Intervenor Southwest Florida Water Management District (SWFWMD) to allow continued withdrawals from four of its eleven major wellfields. Concerned with the environmental impacts, such as drawdowns of the water levels of wetlands, streams, and lakes, from the environmental, if not regulatory, overpumping of the wellfields, SWFWMD denied the application for the quantities requested. An Administrative Law Judge at the Division of Administrative Hearings conducted a hearing and issued a recommended order finding adverse environmental effects from overpumping, but recommending that SWFWMD issue the requested permits subject to certain conditions. Subsequent negotiations resulted in the parties' entering into a series of agreements covering withdrawals from the four wellfields that had been the subject of the administrative hearing and seven more wellfields that were approaching repermitting (11 Wellfields), as well as a series of other matters. On May 20, 1998, WCRWSA, the three member counties, the three member municipalities, and SWFWMD entered into the Northern Tampa Bay New Water Supply and Ground Water Withdrawal Reduction Agreement (Partnership Agreement). The Partnership Agreement requires WCRWSA to bring one or more projects online, by December 31, 2002, to produce at least 38 million gallons per day (MGD) and, by December 31, 2007, to produce at least 85 MGD of new water supply. The Partnership Agreement requires SWFWMD to provide WCRWSA with $183 million toward eligible water supply projects. The Partnership Agreement notes that the then-current Master Water Plan of WCRWSA recognizes that "an aggressive conservation and demand management program is an integral component of a sustainable water supply." (Joint Exhibit 3, p. 31.) The Partnership Agreement notes that the then-current Master Water Plan states that the conservation program was expected to reduce use by 10 MGD per day by 2000 and 17 MGD by 2005. From the effective date of the agreement through December 31, 2002, the Partnership Agreement requires a reduction in pumping of the 11 Wellfields to 158 MGD, based on a rolling 36-month average. For the next five years, the Partnership Agreement requires a reduction in pumping of the 11 Wellfields to 121 MGD, based on an annual average. After that, effective December 31, 2007, the Partnership Agreement requires a reduction in pumping of the 11 Wellfields to 90 MGD, also based on an annual average. Three weeks after the execution of the Partnership Agreement, WCRWSA was reorganized into TBW in June 1998 through the execution of two documents: an Amended and Restated Interlocal Agreement dated June 10, 1998 (Interlocal Agreement), and a Master Water Supply Contract dated June 10, 1998. TBW assumed WCRWSA's rights and responsibilities under the Partnership Agreement. The Interlocal Agreement empowers TBW to produce and supply drinking water "in such manner as will give priority to reducing adverse environmental effects of excessive or improper withdrawals of Water from concentrated areas." (Joint Exhibit 1, pp. 20-21.) The Interlocal Agreement incorporates the phased-in reductions in withdrawals from the 11 Wellfields that are set forth in the Partnership Agreement. The Interlocal Agreement notes that, if the Partnership Agreement provides for extensions of the deadlines, the deadlines contained in the Interlocal Agreement shall likewise be subject to extension. Applying to the 11 Wellfields, SWFWMD issued TBW a Consolidated Permit, which was issued on December 15, 1998, and became effective on January 1, 1999. Complementing the Partnership Agreement, which reflects SWFWMD's resource- development role, is the Consolidated Permit, which reflects SWFWMD's regulatory role. The Consolidated Permit incorporates the phased-in reductions of withdrawals, as set forth above, for the 11 Wellfields. Although the deadlines for phased-in reductions are conditioned on the funding to be provided by SWFWMD, pursuant to the Partnership Agreement, these deadlines are otherwise unconditional and firm. The Consolidated Permit expressly provides for extensions of deadlines, except the deadlines set for the phased-in reductions of withdrawals from the 11 Wellfields. The Consolidated Permit imposes upon TBW extensive responsibilities regarding environmental monitoring, reporting, and mitigation. These responsibilities extend to groundwater, wetlands, and surface waters, as TBW must, among other things, monitor and report levels in the surficial and Floridan aquifers and potentiometric surfaces in the Floridan aquifer in the vicinity of the 11 Wellfields, as well as in the vicinity of selected wetlands and surface waters. The Consolidated Permit sets specific "regulatory levels" for these resources. Present and Future Tampa Bay Water Facilities, Including the Surface Water Treatment Plant A majority of TBW's production facilities consists of the 11 Wellfields. In an effort to supplement these production sources so as to comply with the phased-in reduction deadlines set forth in the Consolidated Permit and other documents, TBW annually adopts a New Water Plan, which describes capital planning for drinking water production facilities. The June 2000 New Water Plan summarizes the requirements of the Partnership Agreement. The June 2000 New Water Plan notes that TBW reaffirmed its Master Water Plan and New Water Plan projects in April 2000. These projects include the Enhanced Surface Water System, which includes the Tampa Bay Regional Surface Water Treatment Plant (SWTP), Tampa Bay Reservoir Project (Reservoir), and projects obtaining water from the Alafia River, Hillsborough River, and Tampa Bypass Canal. Other projects, besides the Enhanced Surface Water System, include Seawater Desalination (Desal Plant). The June 2000 New Water Plan states that the Enhanced Surface Water System is eligible for a maximum of $120 million from SWFWMD, pursuant to its funding obligation under the Partnership Agreement. This case involves the means by which the SWTP will be permitted, and, in consideration of the manner of permitting, this case involves the means by which the SWTP will be designed and constructed. The June 2000 New Water Plan notes that TBW and USFilter Operating Services, Inc. (USFilter) have entered into a contract for the latter to design, build, and operate (DBO) the SWTP (DBO Contract). The June 2000 New Water Plan reports that USFilter is currently constructing an access road to the site. Among current issues, the June 2000 New Water Plan describes this case, noting that TBW obtained a variance from Respondent Department of Environmental Protection (DEP) allowing a design, build (DB) approach to permitting the SWTP. The June 2000 Water Plan states that the present challenge "has the potential to delay the completion of the [SWTP] by an estimated 8 months, subsequently delaying delivery of the initial 22 mgd (dry weather conditions) of new surface water to the regional system until May 2003 and more likely final acceptance of the [SWTP] to September 2003." (Joint Exhibit 5, p. 4.) (The accuracy of this statement is open to debate because SWFWMD granted an environmental resource permit for the SWTP project only on June 27, 2000--before which no significant alteration of the land could have taken place.) In the meantime, the June 2000 New Water Plan predicts a water supply shortfall of 100,000 to 2 million gallons per day in the South-Central service area of Hillsborough County. Addressing the SWTP, the June 2000 New Water Plan states that TBW purchased the site in October 1999 and released a Request for Proposals on July 19, 1999. Four pre-qualified DBO teams responded on October 18, 1999. The June 2000 New Water Plan erroneously states that TBW applied for a public drinking water facility construction permit (Water Treatment Permit) in October 1999. Actually, in September or October, TBW prefiled with the Hillsborough County Health Department (Health Department) its application for a Water Treatment Permit and paid the $7500 filing fee. The purpose of this courtesy filing or prefiling was to allow Health Department representatives to examine the application, including drawings and specifications for the SWTP, and perhaps expedite the approval process, once TBW filed a formal application. The June 2000 New Water Plan reports that the SWTP will have a peak day, surface water treatment capacity of 60 MGD and will be located on a 433-acre site near U.S. Route 301 and Broadway Avenue in central Hillsborough County. The June 2000 New Water Plan states that the SWTP project schedule calls for completion of construction by March 2003 with plant startup and testing in May 2003 and final acceptance testing in September 2003. The June 2000 New Water Plan estimates that detailed design, site permitting, and construction of the SWTP will cost $84.3 million, and the annual operation and maintenance expenses will be $7.9 million. As for the Desal Plant, the June 2000 New Water Plan reports that TBW will pursue a design, build, own, operate, and transfer (DBOOT) approach to acquire a plant to produce, initially, 25 MGD and capable of expansion by an additional 10 MGD. The June 2000 New Water Plan states that this plant will cost a total of about $96 million in capital expenses and about $19 million annually to operate. Procurement of the Surface Water Treatment Plant Design, Build, Operate Contract and Basis of Design TBW issued a Request for Proposals (RFP) that invited base and alternative proposals for the SWTP. TBW hired Parsons Engineering Sciences to prepare a preliminary design of the SWTP, so as to assist in the preparation of the proposals; although offerors could use alternative designs to the Parsons base design, all proposals had to meet the performance standards specified in the RFP. After publishing the RFP in papers and technical journals and on the Internet, TBW was able to prequalify five teams of offerors. Four of the five prequalified offerors submitted proposals. TBW received a total of nine proposals because each offeror submitted a base proposal and one alternative proposal, and one offeror submitted a second alternative proposal. At its January board meeting, TBW selected the USFilter proposal. No party filed a bid protest to the specifications of the RFP or the selection of USFilter and its team. After the selection of USFilter, TBW entered into negotiations with USFilter. During this process, USFilter agreed, at its expense, to add sand to the granulated activated carbon filters to remove fine particles more efficiently, even though it cannot recover the resulting cost of $1.5 million before or after the commencement of operations. TBW and USFilter entered into the DBO Contract on April 10, 2000 (DBO Contract). The DBO Contract identifies "Design Requirements" that "are intended to include the basic design principles, concepts and requirements for the [c]onstruction . . but do not include the detailed design or indicate or describe each and every item required for full performance of the physical [c]onstruction . . .." (Joint Exhibit 23, Section 1.2.6.) The "Design Requirements" are Schedule 6 to the DBO Contract. Schedule 6 contains all of the individual, technical specifications for the SWTP. Schedule 6 occupies two of the four volumes of large, three-ringed binders forming the DBO Contract. The DBO Contract identifies USFilter, Clark, and Camp Dresser & McKee, Inc. (Camp Dresser) as the DBO team for the SWTP project. Camp Dresser is providing design services, Clark is performing the construction, and USFilter is providing the operation and maintenance services for at least 15 years, as well as the financial guarantee, through its corporate parent. The DBO Contract provides TBW with a fixed construction cost, fixed operating costs, and guaranteed finished water quality. Schedule 8 assures that finished water quality will meet all applicable state and federal drinking water quality standards. Two witnesses at the hearing testified that TBW exacted from USFilter assurances of water quality that, as to certain parameters, will exceed applicable state and federal drinking water quality standards. The DBO Contract provides TBW with a firm completion date, subject to design modifications requested by TBW and uncontrollable circumstances, such as acts of God, raw water whose quality exceeds the maximum limits, or the delay caused by this case. A key document in this case is the Basis of Design Report (Basis of Design), which was prepared by the DBO team in April 2000. Acknowledging the phased-in withdrawal limitations and potential for fines for not meeting the deadlines set forth in the Consolidated Permit, the Basis of Design describes the purpose of the DBO process as follows: By utilizing the [DBO] approach for the [SWTP], [TBW] expects to secure substantial benefits . . .[,] includ[ing] costs savings, innovative design, reduced risk of schedule and cost excesses, long-term contracted facility operations, and maintenance efficiencies and guaranties. (Joint Exhibit 8, pp. 1-2.) The Basis of Design reports that the SWTP will be located on a 100-acre parcel within a 435-acre tract that will also accommodate facilities for groundwater treatment and storage of the treated groundwater, treated surface water from the SWTP, and treated saline water from the Desal Plant. The Basis of Design identifies the sources of raw water for the SWTF as the Tampa Bypass Canal, Hillsborough River, and Alafia River. Once online, the reservoir will help normalize quantities of available raw water throughout the dry season. The Basis of Design describes the main treatment process as pretreatment, including pH adjustment with sulfuric acid or caustic soda, powdered activated car feed, and ferric sulfate coagulant addition; coagulation, flocculation, and sedimentation using a high-rate ballasted sedimentation process known by its tradename as ACTIFLO; ozonoation for primary disinfection, taste and odor control, and partial conversion of dissolved organic carbon to an assimilable or biodegradable form; biologically active filtration for turbidity reduction, taste and odor control; reduction of biodegradable organic carbon; and post-treatment, including secondary disinfection using chloramines. The finished water will then be pumped into tanks for storage and blending before release into the distribution facilities. Distinguishing the DB process from the typical design, bid, build (DBB) process, the Basis of Design states: a very significant amount of process studies and pre-engineering was performed by the Project Team in support of its [DBO p]roposal. This work included a set of drawings covering all disciplines and developed to the 25 to 30 percent completion stage at a minimum with some drawings developed to a greater degree. This stage of drawing development is significantly beyond the sketches and diagrams usually provided in Basis of Design or Preliminary Design Reports. For this [Basis of Design,] the referenced drawings are attached and should be examined when reviewing this [Basis of Design]. As such, a relatively small number of figures are contained within this [Basis of Design]. (Joint Exhibit 8, pp. 1-4.) The Basis of Design notes that the Project Team conducted "pilot-scale" studies of the chosen treatment processes using Lake Manatee raw water. The purpose of these studies was to validate the selected treatment processes, provide water quality data, and establish appropriate operating criteria, such as coagulant dosages. The Basis of Design addresses raw water quality issues. One table sets out values for 30 different water quality parameters for each of the three raw water sources. The Basis of Design discloses expected water quality data for 11 water quality parameters. Of particular interest are total nitrogen and total phosphorus because, as noted in the Basis of Design, the algal life-cycle increases dissolved organic carbon and nutrient concentrations in reservoir water, and the "severity of this problem is impossible to predict." (Joint Exhibit 8, pp. 2-4.) The expected water quality values for total nitrogen and total phosphorus, respectively, are, on average, 0.8 and 0.55 mg/L and, at maximum, 1.6 and 2.1 mg/L. Each of the three surface waters approaches the average values, but none approaches the maximum values, for total nitrogen. The same is true for total phosphorus for the Tampa Bypass Canal and Hillsborough River. However, for the Alafia River, total phosphorus is 2.09 mg/L, so the raw water from the Alafia River may present a substantial treatment challenge, as it exceeds even the maximum expected value for total phosphorus. An error in Table 2-4 in reporting the maximum and average values of manganese (either the maximum value should be 0.02 mg/L or the average value should be 0.001 mg/L) and the omission of a turbidity parameter expressed in NTUs precludes analysis of these water quality parameters. However, the other expected parameters appear to reflect the actual water quality of these three surface waters. Section 4 of the Basis of Design describes the facilities and design criteria for the SWTP. This section begins with site grading, roadways, yardpiping, and stormwater management and extends to detailed discussions of the pretreatment and treatment processes, including the ACTIFLO, ozone contactor, and biologically active filtration. Urgency of New Means of Producing Drinking Water The SWTP is the hub of a network of production, storage, transmission, and distribution facilities that TBW plans to bring online in order to meet the requirements and deadlines set forth in the Consolidated Permit and other documents. The urgency for bringing this component of these new facilities online as soon as possible is due to environmental reasons, as well as the financial and legal reasons set forth above. Overpumping of existing wellfields has drawn down water levels in surface waters and wetlands, to the detriment of the overall level of biodiversity supported by these natural resources. Some lakes have been down 10 years, and a few have been down 40 or 50 years. During the recent drought, the City of Tampa, which obtains water from the Hillsborough River, lacked adequate volumes of surface water from which to produce sufficient finished water to meet the demand of its customers. Not surprisingly, these supply problems are accompanied by record withdrawals from the 11 Wellfields. Withdrawals in May and June of this year were the highest monthly withdrawals on record--208 MGD and 175 MGD, respectively. If the drought continues and TBW continues to meet the demands of its customers, TBW's withdrawals from the 11 Wellfields will exceed the permitted 158 MGD, on a rolling 36-month average, by April 2001. Wellfield overpumping has stressed the groundwaters. Although surface waters respond to substantial rains in as little as a day or two, groundwater takes significantly longer to respond. The surficial water table is as much as 20 feet below ground level, and the Floridan Aquifer is even deeper. The surficial aquifer does not begin to respond to substantial rains for one week, and the Floridan Aquifer begins to respond in two to four weeks. The condition of the surficial and Floridan aquifers affects the Hillsborough River and Tampa Bypass Canal, which are significantly recharged by the surficial and, sometimes, the Floridan Aquifer. The Floridan Aquifer is especially important to the Tampa Bypass Canal, whose rock bed has been breached. During dry periods, the two aquifers are the primary sources of recharge for these two surface waters. The Alafia River is more confined, but gets water from the Floridan Aquifer through two springs at the head of the river. TBW has already made substantial gains through conservation and has met the goal of nearly 10 MGD for 2000. Over the next 20 years, maximum potential gains are expected to be no more than 74-94 MGD. Conservation will continue to play an important role in securing adequate drinking water supplies in the Tampa Bay area, but conservation, even in conjunction with reclaimed water, will not suffice, especially when future population growth in the area is considered. TBW also manages wellfield production efficiently. Under its Optimized Regulatory Operations Plan, TBW collects and analyzes wellfield data to determine which wellfield to tap, notwithstanding specific limits set by wellfield, in order to minimize environmental damage. The consumptive use permits issued to TBW for the surface waters that will provide raw water to the SWTP restrict the amounts and timing of the removals. Additionally, a hydrobiological monitoring program requires the collection and analysis of data to safeguard against adverse effects in the rivers and, downstream, in the estuary. The contractual deadline for delivery of the SWTP is September 30, 2002. The timeframe for bringing online the SWTP necessarily relies on acceptance testing in the wet season, during which 60-65 percent of the annual rain occurs. The wet season extends from mid June to the end of September. Acceptance testing of the SWTP is imperative toward the end of this period because this is when the water quality of the surface waters bears the highest levels of the contaminants. Thus, if delays postpone beyond the wet season the point at which acceptance testing can take place, the postponement will effectively be until the next wet season and, possibly, the end of the next wet season. Permitting the Design, Build Process for the Surface Water Treatment Plant General The DB process envisioned by TBW would essentially break into phases the process by which TBW would obtain the necessary Public Drinking Water Treatment Construction Permit (Permit). The Permit initially would be based on "30 percent plans," which reflect about a 30 percent level of effort toward the overall design work or 30 percent completion of all of the design work (30 Percent Plans). Generally, 30 Percent Plans mark the end of the preliminary design phase. Plans reflecting 30, 60 and 90 percent levels of effort are customary in DBB processes, as these are the stages at which owners typically review design work. In 30 Percent Plans, some items are designed to 100 percent and other items are not designed at all. However, 30 Percent Plans provide reasonable assurance that the designed system is constructable. In essence, the Permit initially would be a conceptual permit for the entire SWTP coupled with a construction permit for those components for which the design is already complete on the 30 Percent Plans. Construction of each remaining component of the SWTP would await subsequent permit modifications authorizing construction of that component. As noted above, the May 18, 2000, cover letter anticipates another interim permit, or permit modification, covering specific components, and then the final permit, or permit modification, covering the entire SWTP. The DEP district office in Orlando has substantial experience with permitting DB water treatment projects. From 1996-98, the DEP Orlando office has permitted four such projects for the Orlando Utilities Commission and one such project for the City of Kissimmee. One of the Orlando Utilities Commission projects was to construct a completely new water treatment plant. Based on the experience of the DEP Orlando office, DB permitting, when based initially on 30 Percent Plans, shortens and simplifies the permitting process. DB permitting eliminates, or at least postpones, the presentation of elements, such as electrical and HVAC, that are irrelevant to the permitting process; the elimination of elements irrelevant to permitting from the initial designs helps the regulator find the elements that are relevant to the permitting process. Also, the experience of the DEP Orlando office is that the DB process results in no more permit modifications for change orders than are typical of a conventional DBB process. The DB-approval process used by the DEP Orlando office is modeled after the DEP-permitting process for wastewater treatment plants. DEP rules allow DB permitting of these plants, which are similar in construction to water treatment plants. In fact, DEP is preparing to adopt rules to allow DB permitting of water treatment plants. Because the DEP Orlando office did not issue variances from the rules that arguably preclude DB construction of water treatment plants, there is no precedent for the issuance of the variance sought in this case. However, the experience of the DEP Orlando office is that applicants do not present basic design changes after the initial submission, and DB permitting does not mean that regulatory objectives are sacrificed to the expediency sought by the applicant. The Present Case On April 11, 2000, Camp Dresser, on behalf of TBW, filed with the Health Department an Application for a Public Drinking Water Facility Construction Permit. The April 2000 drawings that accompanied the April 11, 2000, application are described above. The cover letter to the Health Department notes that, "upon conceptual approval of the project, individual components will be permitted through permit modifications based on submittals of complete drawings and specifications for each component." In this case, the availability of the Basis of Design meant that the 30 Percent Plans reflected more than a 30 percent level of effort or completion of the five-stage process of pretreatment, pH adjustment, ozone contactors, filtration, and storage in tanks. The engineer had already sized the facilities and defined all of the processes and elements of the SWTP. The April 2000 drawings, as supplemented by the Basis of Design, therefore presented a relatively detailed description of the scope, elements, and processes of the project. On May 18, 2000, Camp Dresser submitted to the Health Department more advanced drawings, which are dated May 18, 2000. The cover letter explains that the drawings are a complete set of Phase I drawings and specifications. The letter states that Camp Dresser intends to file complete drawings and specifications in three phases. Phase I, which is completed with the May 2000 drawings, consists of sitework, high rate flocculation and sedimentation, and ozone contact tanks. Phase II consists of biologically active granulated active carbon filters, clearwell, and gravity thickeners. Phase III consists of the remainder of the project. As of July 3, 2000, prior to the final hearing, the design for the SWTP had reached the 60 percent level of effort or completion. Although the SWTP described in the DBO Contract, Basis of Design, and May drawings is a relatively large, complex facility, it does not employ unproven technology. The standardization of design and regulatory review is facilitated by the use of the so-called Ten States' Standards, which are standards commonly used by the permitting authorities of numerous states, including Florida, to determine the capabilities of specified treatment processes in achieving specific water quality levels. Although the ACTIFLO technology is relatively new, it has been in use for at least five years. A pretreatment sedimentation barrier that reduces treatment time and thus tankage volume requirements, ACTIFLO is in use in a water treatment plant with a capacity of 60 MGD in Canada, which TBW's selection team members visited. ACTIFLO presently is being incorporated into a surface water treatment plant in Melbourne, Florida, where it must treat the nutrient-rich water of Lake Washington and the St. Johns River. The City of Tampa is adding ACTIFLO basins to its facilities. Also significant is the fact that ACTIFLO easily passed the pilot test on Lake Manatee. At present, 25 facilities using ACTIFLO are under design or construction in North America. As is consistent with the theory, the DBO process for designing, building, and operating the SWTP has demanded greater cooperation among the three entities that operate relatively independently in the DBB process. Pursuant to their obligations under the DBO Contract, Camp Dresser, Clark, and USFilter have coordinated, and likely will continue to coordinate, their efforts closely from design and construction, up to operation, to save time and money from the traditional DBB process, in which the design phase, construction phase, and operation phase are relatively independent of each other. The Variance In general, DEP has the authority to issue public drinking water treatment construction permits. The successful applicant obtains one permit--for construction and operation. There are no conceptual permits or separate operating permits. In Hillsborough County, as well as 10 other counties, DEP has delegated its responsibilities for issuing public drinking water treatment construction permits. In Hillsborough County, DEP has delegated this responsibility by an interagency agreement to the Health Department. Applying DEP rules to determine whether to issue a public drinking water construction permit, the Health Department defers to DEP for the issuance of variances from DEP rules. In typical permitting cases, the Health Department uses its own staff in processing the application and reaching a permitting decision. In a large case, such as this, the Health Department's lone professional engineer, who was hired in September 1999, can obtain considerable assistance from professional engineers within the Tampa Bay area and professional engineers employed by DEP. Perceiving a possible incompatibility between the DB process and the rules from which the variance is sought in this case, TBW initially filed a request for a variance with the Health Department. However, the Health Department declined to issue a variance to DEP rules and informed TBW that it had to file its request with DEP. Thus, on January 10, 2000, TBW filed a petition for a variance with DEP. On March 28, 2000, DEP issued a final order, pursuant to Section 120.542, Florida Statutes, granting the requested variance from Rule 62-555.520(4)(c) and (d), Florida Administrative Code (Variance). The Variance finds that the purpose of the underlying statutes would be met "because no component of the project would be permitted or constructed without review by the permitting authority of the complete plans and specifications for that portion of the project." The Variance finds that the DB approach will protect the public health, safety, and welfare in providing safe drinking water without exacerbating possible negative environmental impacts from the overuse of groundwater. The Variance relieves TBW of the necessity of complying with two subsections of the rule governing the contents of applications for a public drinking water construction permit. Rule 62-555.520(4)(c) and (d), Florida Administrative Code, provides: The permit application form sets forth the minimum information which is to be supplied to the Department or the Approved County Health Department. Additional information may be required by the Department to clarify information submitted in the permit application or to demonstrate that the proposed level of treatment will effectively treat the contaminants present in the raw water. The information required by the application is as follows: * * * Prints of drawings of the work project which contain sufficient detail to clearly apprise the Department of the work to be undertaken. All prints shall be minimum of 18 x 24 inches and a maximum size of 36 x 42 inches. The scale of details contained shall be satisfactory for microfilm reproduction. (Reduced size photographic reproduction of drawings for submission may be authorized.) Complete specifications of the project necessary to supplement the prints submitted. The issuance of the Variance by DEP has met with approval, albeit cautious approval, by the Health Department. One Health Department witness was an Engineer III, who is 19-year employee of the Health Department and supervisor of four Environmental Specialists charged with reviewing construction plans for drinking water plants. He testified that he agreed with DEP's final order granting the Variance. The Engineer III and the other Health Department witness, its professional engineer, testified that the issuance of the initial permit would not influence the Health Department in deciding whether to issue permit modifications, except to ensure compatibility. Allowing TBW not to comply with Rule 62-555.520(4)(c) and (d), Florida Administrative Code, the Variance provides that the initial permit shall not authorize the construction of any component of the SWTP; each component may be constructed only after the submission of complete plans and specifications for that component and the issuance of a permit modification based on those complete plans and specifications. The Variance also provides that the permitting authority shall publish a notice of intent to issue a permit modification "if the permitting authority believes that the modifications are of a controversial nature, or that there is heightened public awareness of the project." Save Our Bays and Canals, Inc. The Verified Amended Petition On May 1, 2000, Petitioner filed a petition challenging the Variance. On June 29, 2000, Petitioner filed an amended petition challenging the Variance, and the Administrative Law Judge granted Petitioner leave to file an amended petition on July 3, 2000. At the start of the hearing, on July 7, 2000, Petitioner filed a verified amended petition, which was identical to the amended petition, except that, on July 6, 2000, Petitioner's president had verified the pleading "to the best of [his] knowledge, information and belief." The verified amended petition states that Petitioner has over 400 members. The verified amended petition alleges that a substantial number of Petitioner's members will consume the finished water produced by the SWTP and will use the surface waters supplying the SWTP for recreation. The verified amended petition states that the purpose of Petitioner is to save the bays, canals, and waterways of the Tampa Bay area and to ensure safe drinking water for its members and residents of the Tampa Bay area. The verified amended petition states that the Variance affects Petitioner because it would allow the issuance of the Permit and construction of initial phases of the SWTP prior to submittal, review, and approval of complete plans for the next and subsequent phases. The verified amended petition alleges that Petitioner incorporated to pool its resources to review applications, so as to ensure safe drinking water. The verified amended petition states that submittal and review of a complete set of drawings and specifications is necessary prior to construction of the SWTP to ensure the ability of the facility to comply with state drinking water standards. The verified amended petition states that review of all individual components of the SWTP is necessary to assure the protection of the public health, safety, and welfare and the compliance with all applicable state and federal laws. Addressing specifically the 30 Percent Plans, the verified amended petition objects to the absence of a list of items to be included in the 30 Percent Plans. The verified amended petition alleges that this piecemeal approach to permitting will require Petitioner to request administrative hearings on each phase of permitting. The verified amended petition states that the Variance may have adverse environmental and safety impacts that cannot be evaluated fully without a submittal and review of the complete drawings and specifications. The verified amended petition states that the DBO approach is "self-created." The verified amended petition objects to the failure of TBW to obtain the Variance before issuing the RFP and instead using the DBO Contract as a basis for claiming hardship so as to qualify for the Variance. The verified amended petition states that the number of variances issued for similar 30 Percent Plans threatens to create a situation in which the variance subsumes the rule requiring complete drawings and specifications. The verified amended petition objects to this form of unwritten policy that has not been published as a rule. The verified amended petition states that the phased permitting of the SWTP may create permitting momentum that discourages a rigorous application of the rules at a later stage. The verified amended petition states that the request for a variance is improper because it is for a variance from statutes, not rules. The verified amended petition states that Section 403.861(10), Florida Statutes, requires DEP or Health Department approval of "complete plans and specifications prior to the installation, operation, alteration, or extension of any public water system." The verified amended petition states that "installation" means construction. The verified amended petition states that Section 403.861(5), Florida Statutes, prohibits the issuance of a public drinking water treatment construction permit "until the water system has been determined to have the required capabilities . . .." The verified amended petition states that the assurances of USFilter are insufficient to satisfy this requirement. The verified amended petition states that Section 120.542, Florida Statutes, which authorizes the variance procedure used in this case, does not authorize variances for compliance with federal law. The verified amended petition states that TBW must obtain a federal variance in order to obtain the Variance. The verified amended petition states that the 30 Percent Plans omit information required for permitting, such as the listing of a certified operator, monitoring and recordkeeping programs, and various financial elements, such as the posting of a bond and creation of reserves to demonstrate financial soundness. The verified amended petition states that TBW's substantial hardship is based on contract deadlines that are entirely self-created and, thus, insufficient to warrant a variance. The verified amended petition notes that the environmental damage cited as a basis for granting the Variance "was caused by years of overpumping by . . . TBW . . .." Also, the verified amended petition states that member governments of TBW continue to approve new development, which increases the demand for drinking water, because TBW and its member governments have failed to exploit fully the potential for conservation and reclaimed water. Similarly, the verified amended petition states that SWFWMD helped create the hardship by renewing the permits for additional withdrawals from the 11 Wellfields. The verified amended petition states that the DBO process will not necessarily save time and money and is not a recognized exception to the general requirement that an applicant must submit complete drawings and specifications prior to permitting. The verified amended petition states that 30 Percent Plans do not provide sufficient detail to know what the contractor is promising to build, and it would be faster to correct any mistakes prior to the start of construction, rather than after the start of construction. Standing Petitioner was an unincorporated association from its formation in early October 1999 through February 3, 2000, when it was incorporated as a Florida not-for-profit corporation. Originally named Save Our Bays and Canals Association, the unincorporated association was formed by members of the Apollo Beach Civic Association who were concerned about the environmental impact upon their bays and canals of intensive utility and industrial land uses in close proximity to their homes. Apollo Beach is an unincorporated area along the southeast shore of Tampa Bay, just south of the mouth of the Alafia River. The land uses with which the unincorporated association has been concerned in its brief existence include a sulfur plant, the TECO Big Bend plant, a proposed National Gypsum plant, a proposed concrete plant, the proposed Desal Plant, and, now the proposed SWTP. The Apollo Beach area is very close to the proposed site of the Desal Plant, but is about 17 miles south southeast from the proposed site of the SWTP. Petitioner and its members are primarily concerned with the Desal Plant, not the SWTP. However, Petitioner and its members express concern with the SWTP. The concerns are that DB permitting of the SWTP will jeopardize the production of safe drinking water and will result in greater costs to TBW customers, who will eventually bear the financial burden of costly reworking of a hastily designed and constructed project. Standing analysis is simplified by the elimination of the issue of whether the verification of the amended petition confers standing. The claims of Petitioner in this case do not rise to the level of an attempt to prevent an activity, conduct, or product to be permitted from impairing, polluting, or otherwise injuring the air, water, or other natural resources of the State. First, finished drinking water is not a natural resource of the State. Although a resource, finished drinking water is not natural. Although of lower water quality, raw water is a natural resource. The potable water leaving the SWTP is a manufactured resource. Second, even if finished drinking water were a natural resource, the issuance of the Variance does not have the effect of impairing, polluting, or otherwise injuring a natural resource. The Variance excuses compliance with two rules requiring complete drawings and specifications. Even assuming that the SWTP would impair, pollute, or otherwise injure natural resources, the Variance would not have such an effect because the act of granting the Variance is distinct from the act of granting the Permit itself. Thus, facts regarding the circumstances under which Petitioner's president verified the amended petition are irrelevant for the purpose of determining standing. Petitioner's standing is a function of the characteristics of the corporation and its members. At the corporate level, the articles of incorporation state that the "specific and primary purposes for which this corporation is formed are to operate for the public education and advancement of the water quality of Tampa Bay, its tributaries, its estuaries and its canals and for other charitable purposes, by the distribution of its funds for such purposes." There is some indication in the record of an attempt, after filing the petition commencing this proceeding, to amend the articles of incorporation to state, among Petitioner's purposes, the protection of drinking water. The record does not contain the written articles of incorporation, as amended, or amended articles of incorporation after February 3, 2000. However, for the purpose of this recommended order, the Administrative Law Judge shall assume that such an amendment was made at some point after the filing of the petition and before the final hearing. At the membership level, the water to be produced by the SWTP will be distributed primarily to customers in Pasco and Pinellas counties, St. Petersburg, and the Northwest Service Area of Hillsborough County, not to Apollo Beach, which is in southern Hillsborough County. Nearly all of Petitioner's members reside in Apollo Beach or other nearby communities, which also will not be served by the SWTP. Although an insubstantial number of Petitioner's members will consume finished water from the SWTP in their homes, a substantial number will consume finished water from the SWTP at their places of work or schools and where they shop or dine out. Drinking water is ubiquitous, and the mixture of functional land uses in Apollo Beach is not, so it is highly probable that members of Petitioner will travel the three-county area in connection with their employment, education, and recreation. Close analysis of the characteristics of Petitioner and its members reveals no basis for finding standing to challenge the Variance. Nothing in the record suggests that Petitioner or any of its members have devoted themselves to the arcane task of resisting a perceived trend of state and local agencies to issue series of permits in response to DB proposals--or, more colorfully, to engage in "piecemeal permitting." About the only interest that Petitioner can legitimately claim in DB permitting is that multiple points of entry, at each permit and permit modification, will result in additional expense. If Petitioner has standing to contest even the permitting of the SWTP, Petitioner must petition each time for an administrative hearing, conduct discovery, and participate in the final hearing. However, this seems, at most, like a tenuous interest, which suffers also from the speculation that later stages of the DB permitting process will continue to present new issues not raised in the challenge of the Permit initially approved. Turning to the members themselves, their consumption of drinking water produced by the SWTP is no basis for standing either because the attenuated relationship between the Variance, which excuses compliance with two rules concerning the contents of applications, and the safety of drinking water or the additional costs that could arise from hasty designing, constructing, or permitting. Although it is conceivable that a record could have been made that the DB permitting proposed in this case would likely result in incomplete, incompetent permitting review, so as to jeopardize the public health if the permit were to issue, the record in this case does not support such a contention. To the contrary, the record establishes that the DB permitting is at least as likely as DBB permitting to provide the regulatory oversight necessary to assure the design and construction of a successful public drinking water treatment plant Lacking a substantial nexus in the record between the DB permitting authorized by the Variance and the quality of the drinking water that, if the Health Department issues the Permit, would likely be produced by the SWTP and likelihood of success of the overall construction project, the members of Petitioner likewise lack standing to challenge the Variance. Ultimate Findings of Fact Petitioner and its members lack standing to challenge the Variance. TBW faces a substantial hardship if not given the Variance. The legal and financial consequences of a failure to meet the phased-in withdrawal reductions are real and substantial. The environmental damage caused by overpumping the 11 Wellfields underscores the urgency of developing alternative sources of raw water for production into finished drinking water. The rule from which TBW seeks the Variance is derived from the statute discussed in the Conclusions of Law. The underlying purpose of this statute is the protection of the public health, safety, and welfare. The Variance serves the underlying purposes in two respects. First, the 30 Percent Plans contain sufficient detail to allow permitting to proceed without jeopardizing the objective of the rules to ensure that the USFilter team designs and constructs a water treatment plant that is in full compliance with all federal and state law. Second, the Variance provides that the USFilter team shall construct no component of the SWTP until it has been permitted, either initially or by a permit modification. Petitioner's Liability for Attorneys' Fees and Costs Petitioner has a Technical Committee on which Petitioner relies for examination of technical aspects of matters that are of general concern to Petitioner. This committee obtained a copy of the Variance and, after examination and discussion, developed a position in opposition to DEP's stated intent to grant the Variance. The Chair of Petitioner's Technical Committee, who has a bachelor of science degree in chemistry and is an industrial hygienist, drafted a letter reflecting the opinion of the committee in opposition to the Variance. Petitioner's attorney then converted this letter into the petition that commenced this proceeding. At all times, the Board of Directors of Petitioner approved the actions of the Technical Committee and Petitioner's attorney, including the filing of the petition. When Petitioner's president verified the amended petition, he reasonably relied on the advice of counsel concerning the substance of the assertions, and the advice of counsel was based on the work of the Technical Committee. Petitioner's president also reasonably relied on the work of the Technical Committee when he verified the amended petition. Although DB permitting has been available for the design and construction of wastewater treatment plants for an undetermined period of time, DB permitting for the design and construction of public drinking water plants is a new concept. The concept is so new that the DEP Orlando office mistakenly issued at least 2 DB permits for public drinking water plants without requiring the applicant to obtain a variance from the two rules that prevent DB permitting for such facilities. The concept is so new that the key Health Department employees have expressed concern over personnel demands from this new means of permitting, although they have also expressed at least lukewarm support for the Variance. The record portrays the employees of the Health Department as hard-working and competent, but over-burdened. The DB permitting obviously places significant responsibilities upon the Health Department, especially as it familiarizes itself with DP permitting. Although the availability of professional support from other sources, including DEP, ultimately resolves this issue, the situation of the Health Department also is relevant in assessing Petitioner's liability for attorneys' fees and costs. Two or three aspects of the drawings were deficient, according to Petitioner's professional engineer, whose testimony has been admitted despite the unreasonably restricted opportunity presented for cross-examination by his contractually driven refusal to identify past clients or jobs. Although none of these items seems likely to jeopardize a successful construction project, these were design points on which well-informed professionals could reasonably differ. Although the issue of "improper purpose" presents a closer question than the substantive issues discussed above, there is inadequate subjective or objective evidence in the record supporting TBW's claim for attorneys' fees and costs on this ground. Ultimately, the novelty of DB permitting of drinking water treatment plants precludes a finding of improper purpose. All available facts drive this determination, and, at this point in time, the relative uniqueness of DB permitting of drinking water treatment plants to DEP, the Health Department, and Petitioner and its members provides the necessary margin to preclude a finding of improper purpose.

Recommendation It is RECOMMENDED that the Department of Environmental Protection enter a final order granting the Variance and denying the request of Tampa Bay Water for attorneys' fees and costs. DONE AND ENTERED this 24th day of July, 2000, in Tallahassee, Leon County, Florida. ROBERT E. MEALE Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 24th day of July, 2000. COPIES FURNISHED: Kathy C. Carter, Agency Clerk Office of General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000 Teri L. Donaldson, General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000 Ralf G. Brookes, Attorney 1217 East Cape Coral Parkway Suite 107 Cape Coral, Florida 33904 Donald D. Conn, General Counsel Tampa Bay Water 2535 Landmark Drive, Suite 211 Clearwater, Florida 33761 J. Frazier Carraway Thomas A. Lash Salem, Saxon & Nielson, P.A. 101 East Kennedy Boulevard Suite 3200 Tampa, Florida 33601 Cynthia K. Christen Senior Assistant General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000 William S. Bilenky General Counsel Jack R. Pepper, Jr. Associate General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899

Florida Laws (6) 120.542120.569120.57120.595403.412403.861 Florida Administrative Code (2) 62 -555.52062-555.520
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WYATT S. BISHOP, JR. vs HI HAT CATTLE AND GROVES AND SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 90-007734 (1990)
Division of Administrative Hearings, Florida Filed:Sarasota, Florida Dec. 06, 1990 Number: 90-007734 Latest Update: May 17, 1991

The Issue The issue for consideration in this case is whether the Respondent, Hi Hat Cattle and Grove, should be issued water use permit 204387.03, to withdraw groundwater from the wells on its property, and if so, in what amount and under what conditions.

Findings Of Fact At all times pertinent to the issues herein, the Respondent, District, was the state agency responsible for the permitting of consumptive water use within its area of geographical jurisdiction. The Respondent, Hi Hat, is a family owned farming and ranching operation in eastern Sarasota County with water wells on its property. The Intervenor, City of Sarasota, is a municipality in Sarasota County which operates wells in the general area of those operated by Hi Hat, and which has an agreement with Hi Hat for the latter's use of treated wastewater pumped from the city's treatment plant to Hi Hat Ranch. The Petitioner, Wyatt S. Bishop, Jr., is a property owner and resident of Sarasota County whose property is located near the Hi Hat Ranch, and whose potable water is drawn from a well on his property which utilizes both the surficial and intermediate aquifers which are penetrated by the wells on Hi Hat Ranch. Hi Hat Ranch consists of 11,000 acres owned by Hi Hat Cattle and Grove, the family owned business which operates it, and an additional 3,227 acres leased from the City of Sarasota. Agricultural operations, including citrus farming, truck farming, sod farming, and grazing have been conducted on the ranch since the mid 1940's. In February, 1990, Hi Hat applied to the District for a permit to withdraw and use water from some 14 wells located on its property. It requested an annual average of 6,267,000 gallons per day, (gpd), and a peak monthly rate of 32, 668,000 gpd. Upon receipt by the District, the application was assigned a number, (204387.03), and was submitted for evaluation by the District staff for conformity with applicable District rules and policies. When the staff evaluation was completed, the District issued a staff report and proposed staff agency action in which it indicated its intention to issue a permit authorizing water to be drawn from the wells at a rate of 6,570,000 gpd, average annual, a peak monthly rate of 14,300,000 gpd, and a maximum daily rate of 5,210,000 gpd. In conducting its evaluation, the District staff relied upon the District's Basis of Review For Water Use Permit Applications which contains within it the provision for use of a "water use model" in assessing the need and appropriateness of water withdrawal amounts. This model, known as the Blaney- Criddle Model considers numerous factors in the evaluation, including rainfall, soil characteristics, irrigation methods used, and proposed crop types, all in an effort to determine a reasonable estimate of the applicant's supplemental water needs. Hi Hat's application was evaluated primarily by Marie Jackson, a Hydrologist III employed by the District, and an expert in hydrology, who has, over the years, reviewed between 350 and 400 permit applications, of which approximately 90 percent have been for agriculture. She is, therefore, quite familiar with the specifics of agricultural water use needs. Her evaluation of Hi Hat's application was done in the same manner as the others she has done and utilized the same tests, measurements and factors for consideration in arriving at her conclusion. In its application, a renewal with modification sought to increase average annual quantities due to a change in crop plans, Hi Hat indicated that its criteria for water use was based on certain agricultural uses and application rates. These included: low volume under tree spray irrigation of 778 acres of citrus at an application rate of 17.2 inches/year plus one inch/year for frost and freeze protection. open ditch irrigation of 135 acres of sod at an application rate of 30 inches/year. open ditch irrigation of 1,367 acres of improved pasture at an average application rate of 26.6 inches/year. overhead spray irrigation of 1,200 acres of improved pasture at an application rate of 20.3 inches/year. open ditch irrigation of 110 acres of spring peppers at an application rate of 30.0 inches/crop, and open ditch irrigation of 110 acres of fall peppers at an application rate of 45.2 inches/crop. Applicant also stipulated that the peak monthly quantities that it requested would be utilized for pasture, sod and citrus irrigation during the month of May. The proposed maximum quantities were for frost and freeze protection of citrus only. In January, 1989, Hi Hat entered into a contract with the City of Sarasota under which the City was obligated to deliver reclaimed water from its wastewater treatment plant to a "header" located on the ranch which thereafter distributes the water through pipes to "turnouts" located at various high points on the property. From these, the water is then discharged into a system of ridges and furrows for distribution of the water across the needed area. The reclaimed water is used to irrigate approximately 5,403 acres of ranchland. The Contract provides for minimum and maximum amounts of water to be delivered as well as for water quality standards which must be met. In periods of adequate rainfall, when irrigation is not required, any treated wastewater which is not needed is stored in a 185 million gallon holding pond on City property located adjacent to the ranch. When needed, water can be fed into the wastewater distribution system described above from the holding pond. This reclaimed water, whether from the pond or direct from the header, can also be utilized to irrigate citrus crops, but this requires a filter system which has not yet been able to operate properly. Therefore, no reclaimed water has yet to be utilized for citrus irrigation on the ranch. At an average annual flow of 6.2 million gallons per day, the pond has the capacity to hold enough treated water for almost 30 days. Not all wells on Hi Hat Ranch are active wells. Several of the wells are classified as standby wells which are intended to be used only to back up the reclaimed water delivery system and are located, normally, beside the "turnouts." In the event the reclaimed water is not available from the city, the standby wells can be utilized to provide water to the ridge and furrow system used to irrigate pasture land. The standby wells are numbers 1, 6, 7, 11, 13, 14, and 15. Well number 5, also identified as a standby well in the staff report and in the draft permit was mistakenly so identified. The draft permit contains several special conditions which impact on the drawing of water under the terms of the permit. Significant among these is Special Condition 33 which prohibits the withdrawal of water from any of the standby wells unless the reclaimed water supply from the city is interrupted. Special Condition 27 requires the installation of a flow meter on any standby well that becomes active as a result of permanent discontinuance of the reclaimed water supply. With regard to flow meters, Special Condition 22 requires flow meters on all of Hi Hat's wells. Ms. Jackson, however, indicated this was in error and has recommended that the standby wells be deleted from that Special Condition. When that is done, only those wells actively producing water on a regular basis would require the installation of flow meters. In its analysis of the application for permit, the District staff considered several factors pertinent to the impact the well would have on the water supply in the area and its effect on other users. These factors include hydrologic impacts, well condition, the history of water use at the ranch, the reliability of the reclaimed water system and its ability to provide a uniform source, and the city's water reuse policy. Addressing each individually, and starting with the hydrologic impact of the withdrawal of the requested amounts, the District considered the nature of the existing wells and how they are constructed and maintained. The District assumed, because the data regarding the construction of the existing wells was incomplete and insufficient to properly disclose the status of casing on each well, that they were shallow cased. As a result, the calculations incorporating this assumption indicate a situation that would occur in its most aggravated form. The parties agreed that Hi Hat's wells are shallow cased and probably go no deeper than 90 feet. To determine, as much as possible, the projected drawdowns in the surficial and intermediate aquifers that might be expected if Hi Hat withdrew the amounts of water proposed, the District utilized the "MODFLOW" computer model which factors in simultaneous peak withdrawals from all 14 of the wells along with a 90 day no rainfall drought condition. This, too, contributes to a worst case scenario, and the resultant figures are considered to be conservative estimates of the hydrologic impact of the water withdrawal. Notwithstanding, the application of this computer model resulted in the indication that, as to the surficial aquifer, the drawdown at Mr. Bishop's property located approximately one half mile from the ranch border, would be no more than .055 feet. Since normal fluctuations in the surficial aquifer during the course of the year can be as much as 6 feet, the projected drawdown as a result of Hi Hat's withdrawals was considered insignificant. Applying the same assumptions and utilizing the same computer model as it relates to the intermediate aquifer resulted in an indication of a drawdown of no more than 2.3 feet at Mr. Bishop's property. Since annual fluctuation in the intermediate aquifer can range from 15 to 20 feet normally, the District considers that any reduction of less than five feet in the intermediate aquifer is insignificant. The permit held by Hi hat currently allows for the withdrawal of more water than would be withdrawn under the proposed permit as conditioned and is consistent with the proposed reduction in allowable withdrawals. Considering that factor, as well as the prohibition against withdrawals from standby wells as long as reclaimed water is available, the actual impact of the water withdrawals consistent with the proposed permit would be substantially less than the computed prediction which includes production from all wells. Drawdown contours are defined across the entire effected area. One of the levels is a 4 foot contour, and when a computer simulation indicates that the 4 foot contour includes a withdrawal previously or otherwise permitted, the District will generally conduct a cumulative impact analysis. In this case, however, since there was only one golf course well within the area circumscribed by the 4 foot contour line, and since this withdrawal was too small to have effected an evaluation, it was not done. The condition of the wells on the Hi Hat Ranch has some bearing on whether or not the application for additional withdrawal of water should be granted. These wells are almost 30 years old, having been drilled in the 1960's. As a result, there is little information available regarding their construction detail. This is not necessarily unusual for agricultural wells, and there is evidence that there are many similar wells in use within the District. The reason for this is that at the time the wells were drilled, information regarding their depth, casing and other matters were not required to be kept or reported. However, there is no indication the wells are in any way violative of well construction criteria and their use has been authorized continuously since 1977. When he prepared Hi Hat's application, Mr. Turner included much the same information regarding the wells as pertains as to depth and diameter which he had previously submitted in earlier applications and which had been accepted. In each case, casing depths had been reported as unknown. Notwithstanding the information contained in some old well logs relative to only a few of Hi Hat's wells, this information is in no way definitive and it is difficult to describe anything specific with the majority of these wells. Nonetheless, as already found, it is stipulated that most are approximately 90 feet deep. It is reasonable to assume that the existing wells, however, are cased only to a shallow depth, and that in many cases, the existing casings have corroded away, either totally or in part. This can cause an intermixing of water from the separate aquifers, but whether this is in fact happening depends upon factors specific to that particular well. Petitioner did not present any evidence to show that as a result of the condition of Hi Hat's wells, any degradation is occurring in the more potable, surficial aquifer as a result of intermixing with water from the intermediate aquifer on or around the Hi Hat Ranch. In Ms. Jackson's opinion, and there appears to be no evidence to contradict it, the amount of drawdown which would occur as a result of maximum pumping at Hi Hat Ranch would not be sufficient to cause poorer quality water from the Floridan aquifer to percolate upward (upcone) into the better quality water of the two upper aquifers even during drought conditions. By the same token, there is no evidence that drawdown would encourage or permit salt water intrusion. Petitioner attempted to show by the records kept on the various Hi Hat wells that many of them have been abandoned and are no longer operative and should not be allowed to fall within the parameters of this permit. He testified clearly that over the years, the level of water in his potable water well has lowered and presumed that this was the result of increased water usage by other entities which draw from the aquifer into which his well is sunk. Water level, however, depends upon numerous factors, of which usage is only one. Others include recharging of the aquifer and the amount of rainfall and other recharge sources not only in the immediate area but across the large area which feeds the aquifer. Mr. Bishop did not present any evidence showing a causal connection between the lowering of the water in his well, or the degradation in water quality he claims to have experienced, and either the drawdown caused by Hi Hat's operation or by aquifer intermixing. He indicated, and it is not disputed, that within the past year, he has had to take measures to improve the water quality in his potable well, but, again, he has not presented any evidence to show this was caused by Hi Hat's ground water withdrawals. In its long range planning, the District intends to implement a program to rehabilitate old wells, and when that program is implemented, almost every agricultural well within the District may require recasing or redrilling. This program will not be implemented for several years, however. In an effort, however, to insure that all reasonable precautions are taken to see that approval of any petition for withdrawal does not have an unacceptable adverse impact on the water needs of the surrounding community, in its analysis of this application, and in all cases, the District makes certain assumptions when adequate empirical data is not available. In this case, pertaining to the unavailability of information regarding Hi Hat's wells, the District assumed that all wells were shallow cased, and this placed the application in the worst possible light. Shallow cased wells allow more upconing and aquifer intermixing. Nonetheless, the amount of water permitted to Hi Hat, even if not used, could impact on Mr. Bishop and other adjoining owner's use of additional water as a result of a possible change to their permitted quantities. However, to compensate for this, the District has also included a special condition, (#26), which requires Hi Hat to log all 14 of its wells within the term of the permit, (7 years), which will require at least 2 wells be done each year. The cost of that action will be between $800 and $2500 per well. Another condition, (#31), requires Hi Hat to look into any complaint from adjacent property owners regarding adverse impacts due to water withdrawal, to report the results of its inquiry to the District, and to mitigate, as much as possible, all adverse impacts due to its withdrawal. Mr. Bishop claimed, and introduced evidence purporting to demonstrate, that many of the wells on the Hi Hat Ranch, which are covered by the permit applied for here, are no longer in use and have been abandoned. In response, Mr. Turner, who has been actively engaged in the ranch's operations for at least the past four years, indicates from his personal knowledge, that all 14 wells included in the permit applied for have been operated within the past two years, and all are capable of producing water. It is so found. Not all wells, however, have been operated at all times. Crop rotation and a varying need for groundwater has resulted in some wells not being used at some times. This is, of course, commonplace in agriculture and to be expected as a result of crop planning programs. Admittedly, an accurate figure for the amount of water which has been withdrawn from the 14 wells cannot be established because these wells do not have, and were not required to have, flow meters. Two of the wells were fitted with hour meters in January, 1989, but because the capacity of the pumps on those wells is variable, a precise estimate of volume pumped cannot be determined. The meters measured only the number of hours the pumps were in operation and not the amount of water passed through the pumps. Evidence was presented, however, to show that wells have been utilized at the ranch since the 1960's, and in 1977, some 14 years ago, following District implementation of a consumptive water use permit program, the ranch first applied for water withdrawal permits. These permits have been renewed as required and all water usage since the implementation of the program has been permitted. Turning to the reclaimed water supply, the delivery system, incorporating a program to pump reclaimed water from the treatment plant all the way back out to the ranch site, is subject to material failure and operator error, and either one can occur at any number of places along the system route. Each could result in interruption of the delivery of the reclaimed water to the ranch. The system is far more complex than would be the use of on-site wells for delivery of ground water. One two week shutdown in the system was occasioned by a major pipe failure as a result of pressure building up in the pipes. Were it not for the fact that a contractor was already at the ranch with replacement parts on hand to effect expeditious repair of the system, the shutdown could have lasted considerably longer than it did. This is not the only interruption, however. Several main line leaks and valve problems have caused the system to be shut down on several occasions for short periods of time. The filter system required for the water destined for the citrus area is problematical, and so far this area of the ranch has not received any reclaimed water in the 10 months the system has been in operation. Mr. Bishop argues that the wet weather holding pond is a solution to the reliability problems with the pipe line, but the pond has had problems of its own. Sand in the water, which comes from the holding pond, has been the primary difficulty in the filter system for the citrus area, and algae growth in that pond has the potential to create other filter problems. Delivery of the water from the pond is not accomplished by a gravity system, but instead, requires the use of pumps powered by an electric motor. In the event of a power failure, this source would be unavailable. Discounting all of the above, however, and assuming, arguendo, that all systems were in top operating condition, the fact remains that the delivery system from the pond to the distribution system is not adequate to supply the amount of water that would be necessary to have an effective freeze protection program. In any case, the reclaimed water supply is not the panacea for all water shortage problems experienced at Hi Hat Ranch. In the first place, the quality of the reclaimed water is generally lower than that of the groundwater which would come from wells on the ranch. Also, the City's treatment process does not remove from the water all the pollutants that are of concern to the farm operators. For one thing, total dissolved solids in the reclaimed water are considerably higher than in the ground water, and high dissolved solid levels can be harmful to citrus crops. In fact, the Institute of Food and Agricultural Sciences recommends that citrus irrigation water not exceed total dissolved solid ranges of from 1000 to 1500 milligrams per liter, (mpl). Testing done on the reclaimed water delivered to Hi Hat Ranch showed it averaged between 1200 and 1500 mpl. Though within recommended parameters, it was toward the high end. Further, reclaimed water is not totally interchangeable with ground water for all agricultural purposes. It cannot, by law, be applied to certain types of ground crops such as melons, nor can it be used for overhead citrus irrigation. There is also a restriction on the use of reclaimed water for pastures on which dairy cattle will be grazed. This all results in a restriction on the options available to the farmer who chooses to use reclaimed water in his irrigation plan. As a result, many farmers try not to use reclaimed water if they have access to adequate amounts of groundwater from on- site wells. Notwithstanding all the above, the parties agree that the use of reclaimed water for irrigation purposed is in the public interest. The District encourages it but nonetheless concedes that even with the availability of reclaimed water, a farmer should have access to wells on his property, in a standby capacity, as an alternative source of water to support his farming activities. Not only that, the agreement between the City and Hi Hat provides for Hi Hat to maintain its water use permit even while receiving reclaimed water from the City. Hi Hat is not the only farm operation with whom the City has negotiated in a effort to expand its wastewater distribution program. It has found in those negotiations, that most farm producers are not willing to rely totally on reclaimed water for all their irrigation needs, and it has concluded that were it mandatory that a farmer give up his on-site ground water withdrawals in order to utilize reclaimed water for a part of his needs, most would be reluctant to use it at all. This would seriously interfere with the City's ability to dispose of its surplus reclaimed water consistent with its policy. Even though Hi Hat's property lies within the Eastern Tampa Bay Water Use Cautionary Area, the rule pertaining thereto is inapplicable to Hi Hat because Hi Hat filed its application for permit, which was deemed complete, prior to the adoption of the rule. Nonetheless, water use officials agree that the proposed permit is consistent with the rule emphasis on the use and reuse of reclaimed water, and the District does not object to backup wells being permitted as supportive of the District's desire to keep ground water within the ground.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that Hi Hat Cattle and Grove be issued water use permit No. 204387.03, within the limits of the authorized quantities as indicated in the intent to issue, subject to conditions contained therein; except that the permit be amended to show well No. 5 as a non-standby well, and to delete standby wells from the terms and requirements of Special Condition 22. RECOMMENDED this 17th day of May, 1991, in Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 17th day of May, 1991. APPENDIX TO RECOMMENDED ORDER The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONER: Accepted Accepted and incorporated herein. Accepted and incorporated herein. - 6. Accepted and incorporated herein. 7. - 11. Accepted. - 15. Accepted and incorporated herein. Accepted. Accepted. & 19. Accepted and incorporated herein. - 22. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. - 28. Accepted and incorporated herein. Accepted and incorporated herein. Rejected. She testified that Condition 28 of the permit provides this. Accepted. Accepted. Accepted and incorporated herein. Accepted. & 36. Accepted. Rejected as not supported by the evidence except that the method permitted was the method being used. - 40. Accepted. Ms. Jackson indicated she "assumed" some wells were drilled into the Florida aquifer. Rejected. Accepted as qualified by the comment, "depending on the respective potentiometric heads." - 47. Accepted. Accepted but incomplete. This is because they did not feel it was necessary under the circumstances. - 51. Accepted. Accepted. Accepted. Accepted. Accepted. Accepted and incorporated herein. Accepted. Redundant. - 61. Accepted. - 66. Accepted and incorporated herein. Accepted. More a restatement of testimony than a Finding of Fact Accepted and incorporated herein. & 71. Accepted and incorporated herein. - 74. Accepted. Accepted. First sentence accepted. Second portion rejected since cited case involves active wells versus standby, as here. The comparison made is accepted. The conclusion drawn as to validity is rejected. & 79. Accepted. FOR THE RESPONDENTS AND INTERVENOR: & 2. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. & 6. Accepted and incorporated herein. 7. - 10. Accepted and incorporated herein. 11. - 13. Accepted and incorporated herein. - 17. Accepted and incorporated herein. Accepted. Accepted. Accepted and incorporated herein. Accepted and incorporated herein. & 23. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence. 27. Accepted. 28. & 29. Accepted and incorporated herein. 30. - 33. Accepted and incorporated herein. 34. - 37. Accepted and incorporated herein. 38. Accepted. 39. Accepted. 40. - 42. Accepted and incorporated herein. Accepted and incorporated herein, & 45. Accepted. 46. & 47. Accepted and incorporated herein. COPIES FURNISHED: Wyatt S. Bishop 5153 Tucumcari Trail Sarasota, Florida 34241 Bram D.E. Canter, Esquire Haben, Culpepper, Dunbar & French, P.A. 306 N. Monroe Street Tallahassee, Florida 32301 Edward B. Helvenston, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Barbara B. Levin, Esquire de la Parte & Gilbert 705 East Kennedy Blvd. Tampa, Florida 33602 Peter G. Hubbell Executive Director SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899

Florida Laws (2) 120.57373.303 Florida Administrative Code (3) 40D-2.04140D-2.09140D-2.301
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JAMES G. MURFEE AND LEE LAPENSOHN vs NORTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 10-010100 (2010)
Division of Administrative Hearings, Florida Filed:Tallahassee, Florida Nov. 08, 2010 Number: 10-010100 Latest Update: Jan. 22, 2013

The Issue Whether Bay County has demonstrated its entitlement to the Permit?

Findings Of Fact The Ecologically Diverse Florida Panhandle With its high diversity of species and richness in endemic plants, the Florida Panhandle has been identified as one of six continental "biodiversity hot spots" north of Mexico. It has more species of frogs and snakes, for example, than any other equivalently-sized area in the United States and Canada and has botanical species that do not exist anywhere else in the Coastal Plain, one of the three floristic provinces of the North Atlantic American Region. The biodiversity stems from a number of factors. The Panhandle was not glaciated during the Pleistocene Period. Several major river systems that originate in the southern Appalachian Mountains terminate on the Panhandle's Gulf Coast. Its temperate climate includes relatively high rainfall. These factors promote or produce plentiful sources of surface and groundwater that encourage botanical and zoological life and, in turn, a diverse ecology. When compared to the rest of Florida, the Panhandle is relatively free from man-made impacts to its water resources. Until recently, the population growth rate lagged behind much of the state. Despite a rapid increase in the population in the late 1990s into the early part of the twenty-first century, it remains much less densely populated than areas in the I-4 Corridor and coastal peninsular Florida to the south. The Panhandle can be divided into physiographic areas of geological variation that are highly endemic; a substantial number of plant and animal species found in these areas are found nowhere else in the world. One of these areas is of central concern to this case. Located in southern Washington County and northern Bay County, it is known as the Sand Hill Lakes Area. The Sand Hill Lakes Area The Sand Hill Lakes Area (the "Area") is characterized by unusual geology that produces extraordinary ecological value. With few exceptions (see findings related to Dr. Keppner's flora and fauna inventories on the NTC/Knight Property below), the Area has not been extensively studied. The data on biological communities and water levels that exist, sparse as it is, has been obtained from historic aerials dating to 1941. The aerials are of some use in analyzing lakes and surface waters whose source is the Surficial Aquifer, but they are of limited value otherwise. They are not of use in determining the level in the Surficial Aquifer. Nor are they of assistance in determining river height when the banks of the river are covered by hardwood forest canopy. The resolution of the aerials is insufficient to show details of the various ecosystems. They do not show pitcher plants, for example, that exist at the site of hillside seepage bogs common in the Area. An aspect of the Area that the aerials do reveal is its many karst features on the surface of the land. Karst lakes and sinkholes dominate the Area and are a component of its highly unusual geology which is part of a larger system: the Dougherty Karst Plain. The Dougherty Karst Plain is characterized by numerous karst features: springs, caverns, sinkhole lakes, and sinkholes. Sinkholes In Florida, there are three types of sinkholes: cover subsidence, cover collapse, and "rock" or "cavern" collapse. Of the three, cover subsidence sinkholes are the most common in the state. Cover subsidence sinkholes form as the result of processes that occur on the surface. A cover subsidence sinkhole is usually a shallow pan typically not more than a few feet deep. Found throughout Central and South Florida, they are the most common type of sinkholes in most of peninsular Florida. In contrast, the other two major types of sinkholes (cover collapse and cavern collapse) occur as the result of processes below the surface that cause collapse of surface materials into the substrata. Both types of "collapse" sinkholes are found in the Area, but cover collapse is the more common. Cavern collapse sinkholes are relatively rare. Typical of the Area, cover subsidence sinkholes are not found on the NTC/Knight Property. The NTC/Knight Property The majority of the NTC/Knight Property is in Washington County, but the property straddles the county line so that a smaller part of it is in northern Bay County. All of the NTC/Knight Property is within the Area. The District recognizes that the NTC/Knight Property contains natural resources of extraordinary quality as does the Area generally. Over the three years that preceded the hearing, Dr. Keppner, an NTC/Knight expert, conducted extensive inventories of the flora and fauna on NTC/Knight Property. Dr. Keppner's inventory showed the NTC/Knight Property supports more than 500 species of vascular plants (flora with a system of tubes within the stem, phloem, and the xylem that exchange materials between the roots and leaves) and 300 species of animals. Among them are at least 28 vascular plants and six animals listed as imperiled (threatened or endangered) by state or federal agencies. At least 22 of the imperiled species of vascular plants and eight of the imperiled species of animals are located within an area expected to be affected by the Wellfield for which Bay County seeks the permit modification. For example, at Big Blue Lake alone where impacts were predicted by NTC/Knight experts to take place, the following imperiled plant species are found: Smoothbark, St. John's Wort, Kral's Yelloweyed Grass, Quilwort Yelloweyed Grass, Threadleaf Sundew, Panhandle Meadowbeauty, and Crystal Lake Nailwort. In addition to the Keppner inventory, NTC/Knight commissioned other studies to determine the nature of the sinkholes and whether they are connected to the Floridan Aquifer. NTC/Knight's experts determined that the property contains cover collapse and a few cavern collapse sinkholes that connect to the Floridan Aquifer. Despite evidence to the contrary submitted by the District and Bay County, the NTC/Knight determinations are accepted as facts for a number of reasons, including the lineup of the sinkholes and sinkhole lakes along identified photo-lineaments and the distribution of them in patterns that are not random. A District study using a dye test, moreover, confirmed conduit flow exists in the Area just east of the NTC/Knight Property. With regard to the distribution of the sinkholes and sinkhole lakes on the NTC/Knight Property, Dr. Sam Upchurch used the term "String of Pearls" to describe multiple sinkholes that exist along the edges of several lakes on the property. When sinkholes closer to the center of a lake are clogged or plugged with sediment and debris, the lakes continue to leak around the plugs which causes new sinkholes to form along the edge of the plugs. Examples of the "String of Pearls" formation on the edges of existing lakes are found at White Western and Big Blue Lakes on the NTC/Knight Property and at Crystal Lake nearby in Washington County. The multiple sinkholes bordering the edge of Big Blue Lake are examples of cover collapse sinkholes that, in geological terms, are relatively young as evidenced by their steep sides. In a karst area such as the Area, there is preferential flow in the conduits because of the difference of efficiency of transmission of water flowing through a porous medium of rock compared to that flowing though a conduit. Absent pumping in the Wellfield, the underlying aquifers are relatively stable. If the requested pumping does not take place, it is likely the stability will remain for a substantial period of time. It is not known with precision what will happen in the long term to the karst environment should pumping occur at the Wellfield at the rate the District proposes. When pumping occurs, however, water in the Area affected by the Wellfield will move toward the Wellfield. "[A]s it does[,] you may get some turbulent flow or vorticity in the water." Tr. 1391, (emphasis supplied). At some point, a change in the potentiometric surface and loss of buoyancy will most likely occur. This leads to concerns for Dr. Upchurch from two perspectives: One . . . is that if there is a[n affected] sinkhole lake [on the surface,] it may induce downward flow . . . the other . . . is that if it breaks the plug it may either create a new sinkhole or create a substantial drop in the level of water in the lake . . . which drains periodically, not necessarily because of a wellfield, but because that plug breaks. Id. In the first instance, lake levels could be reduced significantly. In the second, a new sinkhole could be created or the water level could drop dramatically as occurred at Lake Jackson in Tallahassee. Sand Hill Lakes Wetlands The Area contains a number of wetland communities. These include hillside seepage bogs, steepheads, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and creeks and streams in forested wetlands. A number of these wetlands occur on the NTC/Knight Property within the zone of influence in the Surficial Aquifer predicted by NTC/Knight's experts employing a model known as the "HGL Model." The wetland systems on the NTC/Knight Property are diverse, by type, plant species composition, and richness. This remarkable diversity led the District to recognize that the NTC/Knight Property contains lakes of nearly pristine quality, interconnected karst features, and endemic steephead ravines, all of which are regionally significant resources of extraordinary quality. The Area's wetlands also include many streams, among them Pine Log Creek, the majority of which is located on the NTC/Knight Property. Significant recharge to the Floridan Aquifer occurs on NTC/Knight Property. To the west, north, and east of the NTC/Knight Property are major concentrations of Floridan Aquifer springs that are crucial to the quality and character of regional surface water systems, including the Choctawhatchee River, Holmes Creek, and Econfina Creek systems. All of these surficial systems are dependent on the groundwater resources of the Area. The Area's Hillside Seepage Bogs Hillside seepage bogs are marsh-like wetland usually located on gentle slopes of the sides of valleys. They form when the Surficial Aquifer intercepts the sloping landscape allowing water to seep onto the sloped surface. The plant communities in the bogs are dominated by a great number and variety of herbaceous plants that prefer full sun. Among them are carnivorous plants. These unusual plants include the Trumpet and White-Topped pitcher plants as well as other varieties of pitcher plants. Inundation or saturation for extended periods of time is necessary for pitcher plants and most of the rest of the plant communities found in the bogs to thrive and to fend off invasion by undesirable species. Hillside seepage bogs are valued because they are among the most species-rich communities in the world. A reduction in water levels in the bogs below the root zone of associated plants will kill the plant communities that live in them and pose a threat to the continued existence of the bogs. Hillside seepage bogs were once abundant in pre- settlement Florida, but their expanse has been greatly reduced. They are now estimated to only occupy between one and five percent of their original range. On NTC/Knight Property, they have been spared to a significant degree. Numerous hillside seepage bogs continue to exist on the NTC/Knight Property primarily along the margin of Botheration Creek and its tributaries. The Area's Steepheads Steepheads are unique wetland systems. Found around the globe, they are usually regarded as a rarity. More than 50 percent of the steepheads that exist in the world are in a narrow latitudinal band that extends from Santa Rosa County in the west to Leon County in the east, a major section of the Florida Panhandle. Steepheads occur in deep sandy soils where water originating in the Surficial Aquifer carries away sand and cuts into sandy soils. The seepage emerges as a "headwater" to create a stream that conveys the water from the steephead into a river, or in some rare circumstances, into a karst lake. Over time, flow of the seepage waters results in deep, amphitheater- shaped ravines with steep valley side walls. Steepheads are important to the ecologies of the areas in which they occur. They provide habitat for a number of Florida endemic animals and plants believed to be relics of once-abundant species. Water that emerges from a steephead is perennial. Because the steep slopes of the steephead have not been disturbed over a long period of time, the water remains at a relatively constant temperature, no matter the season. Sampling of aquatic invertebrates at the Russ Pond and Tiller Mill Steepheads on the NTC/Knight Property found 41 and 33 distinct taxa, respectively, to inhabit the steepheads. Among them were a number of long-lived taxa. Their presence is consistent with the hallmark of a steephead: perennial flow of water at a relatively constant temperature. Most of the known steepheads flow into streams or rivers. Between six and ten within the Area, however, flow into Sand Hill Lakes. They have no direct connection to any surface drainage basin, thereby adding to their uniqueness. The level in the Surficial Aquifer has a direct impact on where and to what extent seepage flows from the sidewalls of a steephead. The Area's Sphagnum Bogs Sphagnum moss grows in many locations within the landscape and requires moisture. Where there is a large amount of sphagnum moss, it can form a unique community known as a sphagnum bog that is capable of supporting unique plant and animal populations. In the Area, these sphagnum bogs form along the valley sidewalls of steephead ravines and are fed by Surficial Aquifer seepage from the sidewall of the ravine. These sphagnum bogs support unique plant and animal communities, including a salamander discovered by Dr. Means that is new to science and so far only known to exist in sphagnum bogs in the Florida Panhandle. The Area's Sinkhole Lakes and their Littoral Seepage Slopes Sand Hill Lakes are nutrient poor, or "oligotrophic," receiving most of their nutrient inputs through exchange with the plant and animal communities on the adjacent littoral shelves during periods of high water levels. Fluctuating water levels in the Sand Hill Lakes allow a littoral zone with many different micro-habitats. Areas closest to the lakes are inundated regularly, but higher areas of the littoral zone are generally dry and inundated only every ten or 20 years -- just often enough to prevent encroachment of trees. In a few instances, portions of the littoral zones are inundated by seepage from the Surficial Aquifer. Above the normal low water of the Sand Hill Lakes, the littoral shelf occurs along a low gradient. As the littoral shelf transitions into the lake bottom and toward the deeper parts of the lake, there is an inflection point, where the gradient of the lake bottom becomes much steeper than the littoral shelf. If lake water levels fall below that natural inflection point, gully erosion will occur. The flow of water will be changed along the littoral shelf from seepage sheet flow over a wide expanse to water flowing down gullies in a concentrated stream. This change in flow will result in a loss of area needed by certain seepage dependent plants and animals as well as increased sedimentation from erosion. Big Blue Lake is unique because it boasts the largest known littoral zone seepage area of any Sand Hill Lake. The seepage zone along Big Blue Lake supports a number of rare plant species, including the Thread-Leaf Sundew, Smoothed Barked St. Johns Wort, and Crystal Lake Nailwort. The Area's Temporary Ponds Temporary ponds are small isolated water bodies that generally have no surface water inlet or outlet. Typically very shallow, they are sometimes wet and sometimes dry. Temporary ponds can range from basins that have continuous water for three to five years, to basins that have standing water for a month or two, every two to four years. These conditions limit their occupation by fish and, therefore, provide ideal conditions for amphibian reproduction which only occurs when water levels are maintained long enough to complete a reproductive cycle. In the Area, temporary ponds are a direct expression of the Surficial Aquifer and contain no known restrictive layer that might cause water to be "perched" above the Surficial Aquifer. Temporary ponds are critical to the viability of amphibian populations and support high amphibian biodiversity. A given pond can contain between five and eight species of salamander, and between 12 and 15 species of frogs. There has been a decline recently in the population of frogs and other amphibians that depend upon temporary ponds. The decline is due in part to ditching and other anthropogenic activities that have altered the hydrology of temporary ponds. Temporary ponds have a higher likelihood of being harmed by a drawdown than larger, connected wetlands systems. Lowered Surficial Aquifer water levels would lower water levels in temporary ponds and, thereby, threaten amphibian reproduction. Creeks/Streams in Forested Wetlands Streams are classified on the basis of the consistency of flowing water, including perennial (always flowing), intermittent (flowing part of the year), and ephemeral (flowing only occasionally during rain events). The type of stream flow is important because movement of water is essential to support aquatic systems in stream habitats. The NTC/Knight Property includes a number of stream systems, including Botheration Creek and Pine Log Creek. Botheration Creek is fed by groundwater discharge and originates, in large part, on the NTC/Knight Property. Botheration Creek flows from east to west until it intersects Pine Log Creek on the southwest part of the NTC/Knight Property. Botheration Creek provides Pine Log Creek with approximately 89 percent of Pine Log Creek's flow. From the confluence, Pine Log Creek flows south and west into the Pine Log State Forest and eventually joins the Choctawhatchee River. Botheration Creek contains high quality water and a diverse mix of aquatic invertebrates and fish. Sampling at a stage recorder located approximately two miles west of the eastern boundary of the NTC/Knight Property ("BCS-01") identified 46 taxa of macroinvertebrates, including six long- lived taxa, and mussels. The water level in Botheration Creek at BCS-01 was measured to be between 0.1 and 0.32 feet by four measurements taken from October 2010 to July 2011. Nonetheless, the presence of long-lived taxa and mussels indicates that, at BCS-01, Botheration Creek is a perennial stream. Carbon export from streams provides nutrients that feed the stream system. Headwater streams like Botheration Creek and its tributaries are essential to carbon export. For carbon export to occur, a stream must have out-of-bank flood events regularly to promote nutrient exchange with the flood plain. Bay County and its Water Supply Prior to 1961, the County obtained its public water supply from wellfields located near downtown Panama City. The wellfields drew from the Floridan Aquifer. An assessment of the pre-1961 groundwater pumping appears in a District Water Supply Assessment released in June 1998. In summary, it found that near Panama City, the potentiometric surface was substantially depressed by the pumping. Due to the threat of saltwater intrusion, the Deer Point Lake Reservoir (the "Reservoir") was constructed as an alternate water supply. A local paper mill, the city of Panama City, and Tyndall Air Force Base, all began to obtain public supply water from the Reservoir. Six years after the construction of the Reservoir, the Floridan Aquifer's water levels had rebounded to pre-pumping levels. See NTC/Knight Ex. 93 at 69. The authorization for the Reservoir began in the 1950's when the Florida Legislature passed a series of laws that granted Bay County authority to create a saltwater barrier dam in North Bay, an arm of the St. Andrews Bay saltwater estuary. The laws also allowed Panama City to develop and operate a surface freshwater reservoir to supply water for public use. The Deer Point Lake Dam (the "Dam") was built in 1961 from metal sheet piling installed across a portion of North Bay. The Dam created the Reservoir. The watershed of the Reservoir includes portions of Jackson, Calhoun, Washington, and Bay Counties and covers approximately 438 square miles. The Reservoir receives freshwater inflow from several tributaries, including Econfina Creek, Big Cedar Creek, Bear Creek/Little Bear Creek, and Bayou George Creek, totaling about 900 cubic feet per second ("cfs") or approximately 582 MGD. The volume of inflow would increase substantially, at least two-fold, during a 100-year storm event. The Dam is made of concrete and steel. Above it is a bridge and two-lane county road roughly 11.5 feet above sea level. The bridge is tied to the Dam by pylons. The top of the Dam is 4.5 feet above sea level, leaving a distance between the Dam and the bridge bottom of about seven feet. There is an additional structure above the Dam that contains gates, which swing open from the force of water on the Reservoir's side of the Dam. Capable of releasing approximately 550 MGD of freshwater into the saltwater bay, the gates keep the level of the Reservoir at about five feet above sea level. The height of the Dam and the gate structure leaves a gap between the bottom of the bridge deck and the top of the structure of "somewhere between 12 and 14 inches, a little better than a foot." Tr. 140. If storm surge from the Gulf of Mexico and St. Andrew's Bay were to top the Dam and the gate structure, the gap would allow saltwater to enter the Reservoir. The gates and the Dam structure are not designed to address storm surge. The Dam is approximately four feet thick and roughly 1,450 feet long. The 12-to-14 inch gap extends across the length of the Dam. With normal reservoir levels, the volume of water it contains is approximately 32,000-acre-feet or roughly 10.4 billion gallons. Bay County needs to drawdown the lake level for fish and wildlife purposes, the control of aquatic growth, and weed control. In winter, FWS prescribes a 45-day period of time to draw down the lake to expose the banks to kill vegetation. The last time the lake was drawn down by the County, the water level dropped approximately three feet, from five feet above sea level to two feet above sea level. This process took approximately six days and 16 hours, or approximately 53 hours/foot. Repair of the Dam and its Maintenance The Dam has been repaired three times. The last repair was following Hurricane Opal which hit the Florida Panhandle in the fall of 1995. During Hurricane Opal, "saltwater . . . entered . . . the [R]eservoir . . . [t]hat took 20-some days to flush out . . . ." Tr. 135. No evidence was presented regarding the Dam's vulnerability from the perspective of structural integrity during normal or emergency conditions. Other than the inference drawn from Mr. Lackemacher's testimony that Hurricane Opal damaged the Dam in 1995, no evidence was presented to suggest that the Dam's structure is vulnerable to damage caused by a storm surge, wave effect or other conditions caused by a storm of any magnitude. After the last of the three repairs, Bay County implemented a detailed maintenance program. Based upon the latest inspection reports, the Dam is in good condition and structurally sound. No work other than routine inspection and maintenance is currently planned. The 1991 Agreement and the WTP Bay County's current withdrawal of water from the Reservoir is based on a 1991 agreement between Bay County and the District (the "1991 Agreement"). See Joint Ex. Vol. II, Tab K. The 1991 Agreement allows Bay County after the year 2010 to withdraw 98 MGD (annual average) with a maximum daily withdrawal of 107 MGD. The 1991 Agreement, still in effect, authorizes Bay County to withdraw enough water from the Reservoir to meet its needs through 2040. Water for public supply is withdrawn from the Reservoir by a water utility pump station (the "Pump Station") located a short distance from the Dam in Williams Bayou. The water is piped to the water utility's treatment plant (the "Water Treatment Plant") five miles away. The Water Treatment Plant treats 60 MGD. Following treatment, the water is distributed to Bay County's wholesale and retail customers. The Reservoir water available to Bay County utilities is more than adequate to fulfill the water consumption demands of Bay County's system through a 20-year permit horizon. The transmission line between the Pump Station and the Water Treatment Plant has fittings that were designed to allow transmission of groundwater withdrawn from groundwater wells to be located along the transmission line to the Water Treatment Plant to provide a backup supply for the Reservoir. Bay County's Current Use of Potable Water The amount of water consumed by Bay County utility customers has declined over the last five years. Bay County's current use of water, based upon the average of the 13 months prior to the hearing, was 24.5 MGD, an amount that is only 25 percent of the water allocation authorized by the 1991 Agreement. There are approximately 560,000 linear feet of main transmission lines in Bay County with small service lines accounting for another several hundred thousand linear feet. Bay County furnishes water directly to approximately 6,000 retail customers in areas known as North Bay, Bay County, and the former Cedar Grove area, which is now part of Bay County. Wholesale customers include Panama City Beach, Panama City, Mexico Beach, Callaway, Parker, Springfield, and parts of Lynn Haven. The County also furnishes potable water to Tyndall Air Force Base. Lynn Haven does have some water supply wells; however, Bay County still supplements this water supply by approximately 30 percent. No other cities serviced by Bay County produce their own water. Bay County has a population of approximately 165,000- 170,000 permanent residents, which includes residents of the cities. The Bay County area experiences seasonal tourism. From spring break to July 4th, the population can grow to more than 300,000. The users of Bay County's drinking water supplies include hospitals, Tyndall Air Force Base, and the Naval Support Activity of Panama City ("NSA"). The County has 178 doctor's offices, 56 dental offices, 29 schools, 21 fire departments, 12 walk-in-clinics, six nursing and rehabilitation homes, six major employers, three colleges and universities, and two major hospitals, all which are provided drinking water by Bay County. Panama City Beach is the community which has the highest water use. Panama City Beach's average daily use is approximately 12 MGD. The peak day of usage for all of Bay County's customers over the 13 months prior to the hearing was 40 MGD. Bay County sells water to community water utility systems referred to as a "consecutive system." They include Panama City Beach, Panama City, and Mexico Beach. Bay County's request for 30 MGD contemplates provision of water for all essential and non-essential water uses occurring within the consecutive system. Bay County and the consecutive systems are subject to the District's regulations regarding emergency water use restrictions which typically restrict the non-essential use of water during water shortage emergencies. Hurricanes, Train Wrecks, and Post-9/11 America At the District's recommendation, Bay County has been considering a backup potable water source since the mid-1980's. Bay County's main concern is that it has inadequate alternatives to the Reservoir should it be contaminated. Contamination to date has been minimal. In the period of time after the 1961 creation of the Reservoir to the present, the Dam and the Reservoir have suffered no major damage or impacts from a tropical storm. No tropical storm since 1961 has disrupted Bay County's ability to provide potable water. Even Hurricane Opal in 1995 did not disrupt the water supply. Recent hurricane activity in the Gulf of Mexico, however, has aroused the County's fears. Should a storm of sufficient magnitude make landfall in proximity to the Dam, there is potential for saltwater contamination of the Reservoir from storm surge or loss of impounded freshwater due to damage to the Dam. Mr. Lackemacher, assistant director of the Bay County Utility Department and manager of the water and wastewater divisions of the department, has experience with other hurricanes in Palm Beach, Florida, and Hurricane Hugo in Myrtle Beach, South Carolina, during which water utilities suffered disruption of their distribution systems. The experience bolsters his concern about the damage a storm could cause Bay County's source of public water supply. Bay County's intake structure at Williams Bayou is approximately one mile away from the Dam. The location of the Pump Station puts it at risk for damage from a strong storm or hurricane. There is a rail line near the Reservoir. It runs along Highway 231 and over creeks that flow into the Reservoir, including the Econfina Creek. The rail line is known as "Bayline." Bayline's most frequent customers are the paper mill and the Port of Panama City. Not a passenger line, Bayline is used for the transport of industrial and chemical supplies. In 1978, a train derailment occurred on tracks adjacent to creeks that feed the Reservoir. The derailment led to a chlorine gas leak into the atmosphere. There was no proof offered at hearing of contamination of the Reservoir. There has never been a spill that resulted in a hazardous chemical or pollutant being introduced into the Reservoir. Bay County has not imposed restrictions on the type of vehicles that are allowed to use, or the material that may pass over, the county road on the bridge above the Dam. Nonetheless, in addition to saltwater contamination, Bay County also bases the need for an alternative water source on the possibility of a discharge into the Reservoir of toxic substances from a future train derailment. Bay County is also concerned about contamination of the Reservoir from a terrorist attack. In short, Bay County is concerned about "anything that could affect the water quality and water in Deer Point Lake." Tr. 184. The concerns led Bay County to file its application for the Wellfield on lands currently owned by the St. Joe Company. Consisting of ten wells spaced over an area of approximately ten square miles, the Wellfield would have a capacity of 30 MGD. Bay County's application was preceded by the development of the District's Region III Regional Water Supply Plan and efforts to acquire funding. Funding for the Wellfield and the Region III Regional Water Supply Plan Shortly after the commencement of the planning for the Wellfield, the District, in May 2007, authorized the use of funds from the State's Water Protection and Sustainability Trust Fund ("WPSTF"). The WPSTF is intended for development of alternative water supplies. In cooperation with the District, Bay County began drilling a test well followed by analyses to evaluate the water for potable suitability. In October of the same year, the District passed a resolution to request the Department of Environmental Protection to release $500,000 from the WPSTF to the District for local utilities in Bay and Escambia Counties for "Water Resource Development." NTC/Knight Ex. 195, p. 2. The amount was to be used "to provide funding for implementation of alternative water supply development and water resource developments projects pursuant to sections 403.890 and 373.1961, F.S." Id., p. 1. In February 2008, the District began a process to develop a regional water supply plan for Bay County. If the Wellfield were designated in the applicable regional water supply plan as "nontraditional for a water supply planning region," then it would meet the definition of "alternative water supplies" found in section 373.019(1), Florida Statutes. "In evaluating an application for consumptive use of water which proposes the use of an alternative water supply project as described in the regional water supply plan," the District is mandated "to presume that the alternative water supply is consistent with the public interest " § 373.223(5). Whether the Wellfield is to be presumed to be in the public interest depends on whether the application proposes the use of an alternative water supply project as described in the District's Region III Water (Bay County) Water Supply Plan adopted in 2008. The 2008 RWSP Pursuant to the process commenced in February, the District in August 2008 produced the Region III (Bay County) Regional Water Supply Plan (the "2008 RWSP"). In a section entitled "Identification of Alternative Water Supply Development Projects," the 2008 RWSP provides the following: "All of the water supply development projects identified in Table 4 are interrelated and considered alternative, nontraditional water supply development projects." NTC/Knight Ex. 187 at 14. Table 4 of the 2008 RWSP does not specifically identify the Wellfield. It identifies three projects in general terms. The first of the three (the only one that arguably covers the Wellfield) shows "Bay County Utilities" as the sole entity under the heading "Responsible Entities." Id. at 13. The project is: "Inland Ground Water Source Development and Water Supply Source Protection." Id. Under the heading, "Purpose/Objective," the Table states for the first project, "Develop inland alternative water supply sources to meet future demands and abate risks of salt water intrusion and extreme drought." Id. The Table shows "Estimated Quantity (MGD)" to be "10.0." Id. (In July 2008, the District's executive director informed Bay County that the Wellfield could produce 10 MGD.) The "Time Frame" is listed as 2008-12, and the "Estimated Funding" is "$5,200,000 WPSPTF" and "$7,800,000 Local, NWFWMD." Id. While not specifically identified in the 2008 RWSP, Table 4's project description supports a finding that the Wellfield is, in fact, one of the inland alternative water supply sources. The 2008 RWSP, therefore, designates the Wellfield as a "nontraditional" water supply source for Region III.4/ (The Wellfield also, therefore, meets the definition of "[a]lternative water supplies" in section 373.019(1). The demonstration of a prima facie case by Bay County and the District, however, make the applicability of the presumption a moot point. See Conclusions of Law, below.) Water Supply Assessments and Re-evaluations Development of a regional water supply plan by the governing board of each water management district is mandated "where [the governing board] determines that existing and reasonably anticipated sources of water are not adequate to supply water for all existing and future reasonable-beneficial uses and to sustain the water resources and related natural systems for the planning period." § 373.709(1), Fla. Stat. (the "Regional Water Supply Planning Statute"). The District determined in its 1998 District Water Supply Assessment ("WSA") for Region III (Bay County) that the existing and reasonably anticipated water sources are adequate to meet the requirements of existing legal users and reasonably anticipated future water supply needs of the region through the year 2020, while sustaining the water resource and related natural systems. See NTC/Knight 93 at 79. In 2003, Ron Bartel, the director of the District's Resource Management Division, issued a memorandum to the Governing Board (the "2003 Re-evaluation Memorandum"), the subject of which is "Regional Water Supply Planning Re- evaluation." NTC/Knight 95 (page stamped 42). The 2003 Re-evaluation Memorandum sets out the following with regard to when a "water supply plan" is needed: The primary test we have used for making a determination that a water supply plan was "not needed" for each region is that projected consumptive use demands for water from major water users do not exceed water available from traditional sources without having adverse impacts on water resources and related natural systems. Similarly, regional water supply planning is initiated "where it is determined that sources of water are not adequate for the planning period (20) years to supply water for all existing and reasonable-beneficial uses and to sustain the water resources and related natural systems." Id. With regard to the need for a Water Supply Plan for Bay County the 2003 Re-evaluation Memorandum states: [I]n Bay County (Region III), sufficient quantities have been allocated for surface water withdrawal from Deer Point Lake Reservoir through the District's consumptive use permitting program extending through the year 2040. In this area, the District is also scheduled to complete a minimum flow and level determination for the lake by the year 2006. This determination will be useful for deciding if additional water supply planning is needed before the permit expires in 2040. Id. (page stamped 43). The 2008 RWSP's designation of the Wellfield is justified in the minutes of the Governing Board meeting at which the 2008 RWSP's approval took place: While the reservoir has largely replaced the use of coastal public supply wells historically impacted by saltwater intrusion, there remain challenges within the region that make development and implementation of a Regional Water Supply Plan (RWSP) appropriate. Development of alternative water supplies would diversify public supply sources and help drought-proof the region through establishment of facility interconnections. Development of alternative supplies would also minimize vulnerability associated with salt water potentially flowing into the reservoir during major hurricane events. Id., p. 3 of 4. The adoption of the 2008 RWSP was followed in December 2008 by the District's 2008 Water Supply Assessment Update. The update is consistent with the earlier determinations of the adequacy of the Reservoir as a water supply source for the foreseeable future (in the case of the update, through 2030). The update also voices the concern about water quality impacts from storm surge. The update concludes with the following: In Region III, the existing and reasonably anticipated surface water resources are adequate to meet the requirements of existing and reasonably anticipated future average demands and demands for a 1-in-10 year drought through 2030, while sustaining water resources and related natural systems. However, the major concern for potential water quality impacts is that resulting from hurricane storm surge. A Regional Water Supply Plan (NWFWMD 2008) has recently been prepared for Region III to address concerns associated with existing surface water systems. NTC/Knight Ex. 101, p. 3-41. The Parties Washington County is a political subdivision of the State of Florida. Washington County is located directly north of Bay County and the Wellfield and within one mile of some of the proposed wells. Washington County includes thousands of wetlands and open water systems. Because of the hydro-geologic system in the area of the Wellfield, if there are wetland, Surficial Aquifer, and surface water impacts from the withdrawal under the Permit, it is likely that impacts will occur in Washington County. Washington County has a substantial interest in protection, preservation, and conservation of its natural resources, including lakes, springs, and wetlands, and the flora and fauna that depend on these water resources, especially endangered flora and fauna. Washington County has a substantial interest in the protection of all water resources in Washington County because of the close relationship between surface waters, groundwater, and the potable water supply used by Washington County residents. NTC/Knight is the owner of approximately 55,000 acres of land located in northern Bay County and southern Washington County. The NTC/Knight Property includes thousands of acres of wetlands and open waters, including Sand Hill Lakes, steepheads, hillside seepage bogs, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and forested wetlands. A large portion of the NTC/Knight Property is directly adjacent to the Wellfield and within the HGL Model projected drawdown contour. Based on the projected amount of drawdown from pumping at the proposed average rate of 5 MGD, the 0.5 projected drawdown contour predicted by the HGL Modeling Report (see Finding of Fact 121, below) extends over thousands of acres of the property. NTC/Knight has a substantial interest in the protection of the surface and groundwater directly on, under, and adjacent to its property. The water supports the numerous ecosystems of extraordinary value located on the property. James Murfee and Lee Lapensohn are individuals, who reside in Bay County on property fronting on and beneath Tank Pond approximately five miles from the Wellfield. Petitioners Murfee and Lapensohn have a well which extends into the Intermediate Aquifer. The Murfee and Lapensohn properties are within the HGL Model projected drawdown contour. Petitioners Murfee and Lapensohn have a substantial interest in the protection of their drinking water supply well and the surface waters directly on and adjacent to their properties. Bay County, the applicant, is a political subdivision of the State of Florida. The District is a water management district created by section 373.069(1). It has the responsibility to conserve, protect, manage, and control the water resources within its geographic boundaries. See § 373.069(2)(a), Fla. Stat. Section 120.569(2)(p), Florida Statutes Section 120.569(2)(p), in pertinent part, provides: For any proceeding arising under chapter 373, chapter 378, or chapter 403, if a nonapplicant petitions as a third party to challenge an agency’s issuance of a license, permit, or conceptual approval, the order of presentation in the proceeding is for the permit applicant to present a prima facie case demonstrating entitlement to the license, permit, or conceptual approval, followed by the agency. This demonstration may be made by entering into evidence the application and relevant material submitted to the agency in support of the application, and the agency’s staff report or notice of intent to approve the permit, license, or conceptual approval. Subsequent to the presentation of the applicant’s prima facie case and any direct evidence submitted by the agency, the petitioner initiating the action challenging the issuance of the license, permit, or conceptual approval has the burden of ultimate persuasion and has the burden of going forward to prove the case in opposition to the license, permit, or conceptual approval through the presentation of competent and substantial evidence. The permit applicant and agency may on rebuttal present any evidence relevant to demonstrating that the application meets the conditions for issuance. Paragraph (p) was added to section 120.569(2) in the 2011 Session of the Florida Legislature. Accordingly, the final hearing commenced with the Bay County and the District's presentation of its prima facie case by submitting the application, supporting documentation, and the District's approval of the application. Respondents also presented the testimony of four witnesses in the hearing's first phase. Phase I of the Final Hearing: Bay County's Application, Supporting Documents, the District's Approval and Supporting Testimony The Application File At the final hearing, Bay County and the District offered the "application file," marked as Joint Exhibit Binder Volumes I-IV (the "Application File") in the hearing's first phase. It was admitted into evidence. A document entitled "Alternate Water Supply Report - Bay County Water Division" dated May 20, 2008 (the "Hatch Mott MacDonald Report") is contained in the Application File. See Joint Ex. Vol. I, Tab B. The Hatch Mott MacDonald Report is a preliminary evaluation of a wellfield with 22 wells, an "initial phase . . . [of] five (5) wells producing 5 MGD and the final phase . . . [of] 17 wells, producing 25 MGD." Id. at 1. The evaluation includes the gathering of information, a recommendation for the best method of treatment, an analysis of whether individual well sites or a centralized site would be superior, a hydraulic model and analysis, and the potential construction and operation costs. The report concludes in its Executive Summary: HMM's preliminary results, based upon water analysis of Well No. 1, indicate that only disinfection will be required for potable water treatment. Additionally, the hydraulic analysis indicated that the wells are capable of providing the initial 5 MGD and future 25 MGD to the proposed connection point along Highway 388 without re-pumping. Adequate storage for fire protection should be considered at current and future service areas. The use of chlorine gas at each well site during the initial phase had the lowest present worth of $16,770,270; that is, the smallest amount of funds needed today to build, operate, and maintain the system. The use of chlorine gas at each well in the final phase had a present worth of $41,245,118, only slightly more than the present worth of $40,834,245 for on-site Id. generation of disinfectant at three (3) central facilities. The Application File contains a response to a District request for additional information (the "2009 RAI Response") submitted by the Bay County Services Utility Director and received by the District in September 2009. See Joint Ex. Vol. II, Tab K. The 2009 RAI Response contains the 1991 Agreement and numerous other documents. Among them is a report prepared by HydroGeoLogic, Inc. ("HGL") entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" dated September 2009 (the "2009 HGL Modeling Report"). The report predicts impacts that would be created to the surrounding aquifers as a result of the Wellfield pumping, but recommends that additional data be obtained. The Application File contains the District's Notice dated March 25, 2010. See Joint Ex. Vol. III, Tab B. Attached to the Notice is a draft of the Permit and a staff report from the District recommending approval with conditions. Condition 11 of the Permit's standard conditions obligates Bay County to mitigate any significant adverse impacts caused by withdrawals and reserves the right to the District to curtail permitted withdrawal rates "if the withdrawal causes significant adverse impact on the resource and legal uses of water, or adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. III, Tab B, p. 3 of 17. Attachment A to the Permit requires conditions in addition to the standard conditions contained in the body of the Permit. Paragraph 12 of Attachment A, for example, requires that Bay County implement and maintain a water and conservation efficiency program with a number of goals. Attachment B to the Permit requires a monitoring and evaluation program and wetland monitoring of adjacent properties to determine if the pumping causes adverse impacts to wetland areas, including habitat and species utilization. The Application File contains a revised modeling report also entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" (the "2011 Revised HGL Modeling Report" or the "HGL Model Report"). See Joint Ex. Vol. III, Tab P. The 2011 Revised HGL Modeling Report predicts impacts of the pumping of the Wellfield on the Upper Floridan Aquifer and the Surficial Aquifer. The HGL Model is based on an adaptation of an original model first developed by the U.S. Geological Survey (USGS) and then further adapted by HGL. The adapted model is known as MODFLOW-SURFACT. The MODFLOW-SURFACT Model has been used in excess of 600 applications and is used worldwide. The HGL Model predicted impact from pumping when wellfield pumping achieves a "steady state." Steady state impact is achieved after 10-12 years of constant pumping. The impact and the area of impact is depicted on Figure 5.1b(1) of the 2011 Revised HGL Modeling Report. The predicted drawdown of the Surficial Aquifer is predicted to be six inches (0.5 ft) within the areas indicated. The Application File shows that the permit was revised twice. Ultimately, a Second Revised Notice of Proposed Agency Action dated July 22, 2011, was issued by the District. Attached to the Second Revised NOPAA is the District's Permit. See Joint Ex. Vol. IV, Tab U. A revised Staff Report from the District dated July 18, 2011, is also included in Volume IV of the joint exhibits. See id., Tab Q. The Permit as supported by the staff report allows an average daily withdrawal of 5 MGD, a maximum daily withdrawal of 30 MGD for no more than 60 days per year (with a maximum of 52 consecutive days), and a maximum monthly amount of 775 million gallons. See Joint Ex. Vol. IV, Tab U. The Permit also includes the LTEMP jointly prepared by the Applicant and the District. See id., Attachment B. The Permit requires Bay County to "mitigate any significant adverse impact caused by withdrawals . . . on the resource and legal water withdrawals and uses, and on adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. IV, Tab R, p. 3 of 11. If the District receives notice of an impact from the existing legal user, it contacts the utility. "Within 72 hours [the utility has] a well contractor out there and they have determined what the problem is." Tr. 615. There are no time requirements for the resolution of the impact or any other resolution procedures in the Permit. Definitions of Emergency and Maintenance Amounts The Permit does not include a definition of when the Reservoir may be considered to be unavailable as a public water supply. That determination is left to Bay County. The Permit does not set a withdrawal limit lower than the limits detailed above for maintenance of the Wellfield. There is one set of withdrawal limits. They apply irrespective of the purpose of the withdrawals, that is, whether for backup in an emergency, maintenance, or some other purpose that falls under Public Supply or Industrial Use. Conditions and Monitoring Requirements Bay County is required to mitigate any significant adverse impacts on resources and legal water withdrawals and uses caused by the County's withdrawal from the Wellfield. In addition, the District reserves the right to curtail permitted withdrawal rates if Bay County's withdrawal causes adverse impacts on local resources and legal uses of water in existence at the time of the permit application. In the event of a declared water shortage, the Permit requires Bay County to make water withdrawal reductions ordered by the District. In addition, the District may alter, modify, or deactivate all or parts of the Permit. Attachment A to the Permit, states: The Permittee shall not exceed total, combined groundwater and surface water (authorized in Individual Water Use Permit No. 19910142) withdrawals of an average daily withdrawal of 98,000,000 gallons, a maximum daily withdrawal of 107,000,000 gallons and a maximum monthly withdrawal of 2,487,750,000 gallons. Joint Ex. Vol. IV, Tab U, p. 4 of 11. The inclusion of "surface water" in the condition covers withdrawals from the Reservoir. The combination of actual withdrawals from the Wellfield and actual withdrawals from the Reservoir, therefore, means that Bay County may not exceed the limitations of the withdrawals authorized by the 1991 Agreement. Attachment A to the Permit further explains how Bay County must mitigate harm caused by groundwater withdrawals. The Permittee, within seven days of determination or notification by the District that the authorized groundwater withdrawal is causing harm to the resources, shall cease or reduce, as directed by the District, its pumping activity. The Permittee shall retain the services of a qualified, licensed professional to investigate allegations of interference with an existing, legal groundwater use. The Permittee shall ensure their chosen contractor investigates the alleged interference within 72 hours of the allegation being made. If it is determined that the use of a well has been impaired as a result of the Permittee's operation, the Permittee shall undertake the required mitigation or some other arrangement mutually agreeable to the Permittee and the affected party. The Permittee shall be responsible for the payment of services rendered by the licensed water well contractor and/or professional geologist. The Permittee, within 30 days of any allegation of interference, shall submit a report to the District including the date of the allegation, the name and contact information of the party making the allegation, the result of the investigation made and any mitigation action undertaken. Joint Ex. Vol. IV, Tab U, Attachment A, p. 4 of 11. Bay County is also required, within two years from the Permit's issuance, to submit to the District for review and approval a contingency plan to mitigate potential impacts. The County must wait one full year prior to commencing withdrawal of groundwater for production purposes. During the one-year period, the County must complete groundwater, surface water, and wetland monitoring. The requirements of the mandatory monitoring are found in Attachment B of the Permit, LTEMP. See Joint Ex. Vol. IV, Tab U, Attachment B. The LTEMP "is designed to track trends in ecological and hydrological conditions caused by naturally occurring fluctuations in rainfall, which may affect ground and surface water hydrologic conditions; and to identify potential effects caused by wellfield pumping." Joint Ex. Vol. IV, Tab U, Attachment B at 1. If a substantive deviation occurs from predictions made by the HGL Modeling, or if any other hydrologic or ecologic changes due to the withdrawals are observed at monitoring sites, the District is required to review and, in consultation with Bay County, appropriately revise the LTEMP as necessary with the aim that the monitoring will assure that the conditions for issuance of the Permit are being met. Testimony in Support of the Application In addition to the documentary evidence offered in the first phase of the proceeding, Bay County and the District presented the testimony of several witnesses. These witnesses testified as to background and the 2008 RWSP, the vulnerability of the Reservoir to saltwater contamination from storm surge, and the basis for the District's decision. Vulnerability to Storm Surge There is a one percent chance every year of a 100- year storm event. Flood Insurance Rates Maps ("FIRMS") show that the 100-year water level (the level of storm surge in a 100-year storm event) at the Dam will reach 11 feet NAVD, two feet above the top of the gate structure above the Dam. The Federal Emergency Management Agency ("FEMA") and the National Weather Service ("NWS") have developed the Sea, Lake, and Overland Surge from Hurricanes ("SLOSH") model, which estimates storm surge depths resulting from historical, hypothetical, or predicted hurricanes. A Florida Department of Emergency Management's SLOSH model of the Panama City area shows maximum surge levels for Storm Categories 1, 2, 3, 4, and 5, in NAVD feet as 3.3, 5.8, 10.8, 14.1, and 18.1, respectively. The SLOSH model, in all likelihood, is a low estimation. It is reasonable to expect surge levels in a Category 3 hurricane that passes directly over the Dam, for example, to be higher than 10.8 feet NAVD predicted by the SLOSH model at the Dam. According to the National Oceanic and Atmospheric Administration's ("NOAA") database, 43 tropical storms and hurricanes have passed within 200 miles of the Reservoir between 1970 and 2010 and 20 have come within 100 miles. None have made landfall closer than 40 miles away from the Dam. Of the 20 storms passing within 100 miles of the Reservoir, four have reached Category 3 strength or higher: Eloise, Elena, Opal, and Dennis. In 2004, Hurricane Ivan made landfall over 100 miles to the west of the Dam and raised water levels near the Dam to nearly five feet NAVD. The following year, Hurricane Dennis made landfall 76 miles to the west of the Dam. Dennis produced a surge level of nearly four feet NAVD near the Dam. "Hurricane Eloise (1975) made landfall 40 miles west of Panama City and produced water levels 15 ft above normal at Panama City ([citation omitted]). However, the storm passed through the area quickly and does not appear to have significantly affected the dam." Bay County Ex. 1, p. 3 of 9. Hurricane Opal made landfall 86 miles west of Panama City Beach and produced water levels of about 8.3 feet NAVD near the Dam. The storm surge did not overtop the gate structure above the Dam, but the gates were jammed by debris. "[C]hloride levels rose above 50 ppm at the intake pumps and two to three times above normal background levels of 8 to 10 ppm 'almost one mile up-reservoir.'" Id. The levels of chloride were "still well within drinking water limits," tr. 434, of 250 parts-per- million (ppm). Hurricane Katrina made landfall in 2005 more than 200 miles west of the Reservoir with storm surges higher than 20 feet. Katrina produced surge levels of five feet above normal tide levels in Bay County. The rate and amount of saltwater that would enter the Reservoir depends on the height of the storm surge above the Dam. The 100-year surge levels could remain above the top of the Dam for three or more hours. Such an event would introduce approximately 56,200,000 cubic feet or 1,290 acre-feet of saltwater into the Reservoir, even if the Dam were to remain intact (undamaged) and the tide gates remain closed. The salinity levels bay-side of the dam are generally 23,000 to 33,000 ppm. It is reasonable to expect that in the event of a 100-year storm event, much of the storm surge would come directly from the Gulf of Mexico, which has higher salinity levels. With the Dam intact, the introduction of 1,290 acre- feet of saltwater at 33,000 ppm would raise the average chloride concentration in the Reservoir to at least 800 ppm, more than three times the maximum drinking water chloride level of 250 ppm. Assuming the Dam remained intact during a 100-year storm event, freshwater added over time to the lake from the streams and aquifer will dilute the elevated lake chloride level and restore the lake water to a level fit for human consumption. The USGS has measured stream flow at Deer Point Lake and estimated the lake receives an average of 600 million gallons of freshwater per day or 900 cfs. Post-Opal rates were estimated at 1,500 cfs by the District. Given the estimated volume of saltwater introduced to the lake, at an inflow rate equal to the estimated post- hurricane freshwater inflow rate, Bay County's expert, Dr. Miller, estimated it would take at least two weeks to reduce salinity in the lake to drinkable levels. The inflow rate, however, is not certain. Dr. Miller estimated it is reasonable to expect that it could take anywhere from two weeks to two months for the lake to recover from the saltwater intrusion depending on the variation in the inflow rate. Nonetheless, Dr. Miller assumed that the saltwater from storm surge entering the Reservoir would mix in a uniform matter. There would be "quite a bit of mixing in a storm," tr. 485, of saltwater topping the Dam and freshwater in the Dam. But there would also be stratification due to the sinking of denser saltwater and the rising in the water column of freshwater. The above estimations assume the bridge and Dam remain intact during a major storm. The Dam and tide gates act as a solid barrier, protecting the lake from saltwater in the bay. If rainfall rises in the lake prior to a surge, the tide gates would open to release water, becoming vulnerable to damage or jamming by debris as occurred during Hurricane Opal. In the event of storm surge bringing saltwater into the Reservoir, the opening of the tide gates will assist the Reservoir in reaching chloride levels below 250 ppm provided the tide gates operate properly. Dr. Janicki, an NTC/Knight expert, used the Environmental Fluid Dynamics Code hydrodynamic model ("EFDC Model") to simulate the effects of control structures and water withdrawals on the Reservoir. Taking into consideration the factors Dr. Janicki considered relevant, he predicted that chloride levels, in the event of storm surge from a Category 3 hurricane overtopping the Dam, would only exceed 250 ppm, the drinking water standard, for approximately 3.4 days. Dr. Janicki's prediction, however, was flawed. He added too little saltwater to the lake in the event of contamination from storm surge. He assumed that saltwater would be flushed too soon from the Reservoir following contamination. He did not account for the effects of waves in his model. His model was not in accord with data for Hurricane Opal and the chloride levels near the Dam taken by Bay County after Opal. If the bridge and Dam were severely damaged, more saltwater could enter the lake. With severe damage to the Dam, the Reservoir would be exposed to normal tides. Restoration would not begin until the Dam and bridge had been fully repaired. If an event were catastrophic, the Reservoir could be offline for a lengthy period of time. The Basis for the District's Decision Bay County's reliance on the Reservoir for water for the majority of the population led the District in the mid-1980s to encourage the County to obtain a backup supply. After the District turned down several requests for withdrawals of up to 30 MGD for every day of the year, the District ultimately approved what is reflected in the Permit. The justification for the permitted withdrawal is as a backup supply in the event the Reservoir becomes unavailable and for maintenance of the system and recoupment of its cost. With regard to maintenance, the District attempted to obtain information from Bay County as to appropriate withdrawal limitations. The attempts were abandoned. Despite repeated requests by the District, Bay County did not provide the amount of water needed to be withdrawn for maintenance since it did not have "infrastructure specifics," tr. 552, needed to provide the District with a numeric limit. In contrast to the amount needed for maintenance, the District found Bay County to have demonstrated that it needs 30 MGD when the Reservoir is offline and that it is reasonable for the County to need 30 MGD up to 60 days per year. The District determined that the Bay County's application met the requirements for the issuance of a consumptive use permit found in section 373.221(1)(a)-(c). In determining whether approval of the application is in the public interest, the District did not presume that it is in the public interest on the basis of the designation in the 2008 RWSP of an inland groundwater source as an alternative water supply. The District determined that it is in the public's interest for Bay County to have a reliable and safe water supply source as a backup to the Reservoir irrespective of the statutory presumption. Nonetheless, the District maintains in this proceeding that the presumption applies. The District also applied the 18 criteria test for finding a reasonable-beneficial use found in Florida Administrative Code Rule 62-40.410(a)-(r) and determined that the application should be approved. Petitioners' Case in Opposition Washington County (Petitioner in Case No. 10-2983), NTC/Knight (Petitioner in Case No. 10-2984), and Messrs. Murfee and Lapensohn (Petitioners in Case No. 10-10100) filed individual petitions for formal administrative hearing. Although not identical, the petitions share the similarity that, in essence, each alleges that Bay County failed to establish that the proposed use of water meets the statutory and rule criteria for obtaining a permit for the consumptive use of water. For example, among the many issues listed under the heading "Disputed Issues of Material Fact and Law" in Washington County's Petition for Formal Administrative Hearing is "[w]hether Bay County has provided reasonable assurance that its proposed use of water is a reasonable-beneficial use as defined in section 373.019, Florida Statutes." See p. 5 of the Washington County petition. In like fashion, the Washington County petition and the other two petitions allege that the issues are whether Bay County provided reasonable assurance that it meets the other statutory criteria in section 373.223, and the applicable rule criteria that must be met by an applicant in order for the District to issue a permit for the consumptive use of water. The Petitioners' cases focused on five topics: 1) the limitations of the HGL Model; 2) the likelihood of impacts to wetlands and the failure of the monitoring plan to provide reasonable assurance that the District's monitoring under the plan will succeed in detecting harm to wetlands caused by the withdrawals; 3) the reasonable-beneficial nature of the proposed use of the permit, including the vulnerability of the Reservoir; 4) interference with presently existing legal users; and 5) the feasibility of alternative sources. Bay County and the District offered evidence on rebuttal to meet the Petitioners' cases. Surrebuttal was conducted by Petitioners. Modeling Groundwater models "represent what is happening in very complex physical systems." Tr. 1495. Typically, the data used by models is not sufficient to obtain a completely accurate representation. The models depend on specific data points such as information from boreholes or water level measurements that do not reveal everything that is occurring in the complex system and, therefore, are not enough to support completely accurate model predictions. As explained by Dr. Guvanasen, Bay County and the District's expert, in order to reach a representation of the entire system when the data available from boreholes and measurements is insufficient, which is typically the case, the modeler must "extrapolate a lot of information and use other knowledge of other events." Id. The "knowledge of other events" that the HGL Model used included Dr. Scott's knowledge of the karst environment in the Panhandle of Florida, the mapping of Bay and Washington County geology by the Florida Geological Society, and Dr. Upchurch's knowledge of karst topography. The HGL results of the available data and the extrapolations were placed into a mathematical model (the HGL Model) that considered the withdrawals at issue to determine the response of the system to the additional stress of the withdrawals. Mathematical models like the HGL Model lead to "non- unique solutions" in which "no model . . . is exactly 100 percent correct . . . ." Tr. 1635. Modeling results, therefore, are subject to changes as additional data is collected that demand a better representation than the model provided prior to the data's collection and analysis. HGL Modeling for this case provides examples of non- unique solutions. HGL "built a model twice . . . and got two different sets of answers." Tr. 1633. Besides the recommendation that more data be obtained after the first HGL Model results, the model was not satisfactorily calibrated and the model was recalibrated for the Revised HGL Modeling results. Mr. Davis, NTC/Knight's expert, conducted additional modeling work (the "Davis Modeling"). Using the HGL Model and additional data concerning the NTC/Knight Property, Mr. Davis found drawdowns would occur over a similar but greater area than shown in the 2011 Revised HGL Modeling Report. (Compare NTC/Knight Ex. 31 at 2 to Joint Ex. Vol. III, Tab P, Figure 51b(1).) The Davis Modeling drawdowns, moreover, ranged up to 0.8 feet, 60 percent more than the 0.5 feet determined by the second HGL Modeling results. In the area of Big Blue Lake, for example, the drawdown contours produced by the Davis Model were either 0.6 feet or 0.7 feet, 20 to 40 percent more than the 0.5 feet produced by the second HGL Modeling results. See NTC/Knight Ex. 31 at 2. Asked to rank the modeling results between the first HGL Model run, the second HGL Model run, and his own results, Mr. Davis was unable to say which was better because of the sparseness of the data. Mr. Davis opined that he could conduct another "dozen more model runs," but without additional data he would be "hard pressed" to be able to say which run was more accurate. Tr. 1633. In Mr. Davis' opinion there remain significant uncertainties that cannot be resolved without more data. Inadequate data "precludes . . . reasonable assurance as to exactly where the impacts will travel and exactly what the magnitude of those impacts will be . . . ." Tr. 1637. Ecological Impacts Bruce A. Pruitt, Ph.D., was accepted as an expert in hydrology, soil science, fluvial geomorphology, and wetland sciences. Dr. Pruitt mapped the soil types on the NTC/Knight Property using the Natural Resource Conservation Service ("NRCS") Web Soil Survey and tested soil types by hand-auguring in wetland areas. He characterized the various soil-types on the property by drainage class (relative wetness of the soil under natural conditions) and hydraulic conductivity (permeability). Dr. Pruitt ranked the vulnerability of wetlands within the zone of drawdown predicted by the HGL Model as "very high," "high," or "moderate." The categories were based on the presence of threatened and endangered species, Florida Natural Area Inventor ("FNAI") habitat designation, and the hydrology of the wetland. He assumed that if the water level in the Surficial Aquifer were to be drawn down by 0.3 feet or 0.4 feet then the water level in the seepage bogs at Botheration Creek would be drawn down by the same amount. Wetlands with a vulnerability classification of "very high" will suffer an adverse impact at a drawdown level of 0.2 feet; those at "high" at 0.3 feet and those at "moderate" at 0.5 feet in times of drought. Dr. Pruitt calculated wetland acreage by type using the Florida Cover Classification System. He assigned vulnerability rating for the wetlands within the Surficial Aquifer drawdown contours generated by the HGL Model. Based on Dr. Pruitt's calculations, a total of approximately 4,200 acres of wetlands are likely to be harmed by the predicted drawdown. A majority of these wetlands are located in Washington County. Based on Dr. Pruitt's analysis, it is likely that the NTC/Knight Property contains 1,981 acres of "very highly" vulnerable wetlands; 1,895 acres of "highly" vulnerable wetlands; and 390 acres of "moderately" vulnerable wetlands, which are likely to be harmed by the drawdown in times of drought. In reaching his opinion about the quantification of acres of wetlands likely to be harmed, Dr. Pruitt applied the Florida Uniform Mitigation Assessment Method ("UMAM"). UMAM was designed to address compensatory mitigation in dredge and fill cases. It was not designed for consumptive water use cases. In contrast and damaging to its case of reasonable assurance that natural systems will not be significantly affected, the District did not conduct an analysis to determine loss of wetland function resulting from operation under the Permit. Nor did it determine how much drawdown the affected wetlands could tolerate before they were harmed. Rather than conducting such an analysis, the District chose to rely on implementation of the LTEMP to cure any harm that might be down by drawdown to the Surficial Aquifer. The District and Bay County's wetland scientists opined that there might be a less permeable restrictive layer maintaining water levels above the Surficial Aquifer on the NTC/Knight Property. Dr. Pruitt acknowledged that the NTC/Knight Property had scattered clay layers beneath the surface. It is possible, therefore, that some of the wetland areas he identified as subject to harm have restrictive features under them which would hold water and resist dehydration. In his hand-auguring, however, Dr. Pruitt found no evidence of a less permeable layer. The auguring only went to a depth of three feet and would have to go to a depth of two meters to be definitive. Furthermore, Dr. Pruitt found no evidence of a less permeable layer from well drillings. The District and Bay County did not prove that there is, in fact, such a restrictive layer. NTC/Knight collected water-level data from shallow hand-augured wells and stage recorders at the Botheration Creek Hillside Seepage Bog. The data demonstrate that the water level in the shallow, hand-augured wells at the Botheration Creek Bog is a direct reflection of the level of the Surficial Aquifer. The Surficial Aquifer at the Botheration Creek Bog was approximately 95.5 feet NAVD, over 35 feet higher than at Big Blue Lake and the highest measured level south of Big Blue Lake. The Botheration Creek Hillside Seepage Bog is located between the 0.3 and 0.4 foot Surficial Aquifer drawdown contours predicted by the HGL Model. Based on the HGL Model, the District and Bay County's experts estimated the Surficial Aquifer drawdown at this bog would be 0.39 feet. During the approximately one year of NTC/Knight's water-level recording, a drawdown of 0.39 feet would have reduced the frequency and duration of inundation at this bog significantly. For example, an analysis of the approximately one year of data collected by NTC/Knight shows that at the intermediate water-level recorder location in the bog, one 29-day period of inundation would have been reduced to just nine days and that further down gradient in the bog, none of the five instances when the bog was inundated would have occurred. This is consistent with Dr. Pruitt's vulnerability assessment, which finds that the vulnerability of the hillside seepage bogs to drawdown is "very high," that is, these systems are likely to be harmed in times of drought at drawdown levels in the Surficial Aquifer of 0.2 feet or greater. A drawdown of 0.3-0.4 feet in the Surficial Aquifer at the hillside seepage bog along Botheration Creek increases the likelihood that the hillside seepage bogs along Botheration Creek will be lost in times of drought. The littoral shelves of Sand Hill Lakes typically occur along a low gradient above the normal low water level of the lakes. The existence of the shelf promotes seepage sheet flow along a wide expanse. The drawdown will change the flow from seepage sheet flow to concentrated stream flow within gullies. The erosion and increased sedimentation produced by the greater force of the water in the gullies will cause a loss of area needed by certain seepage dependent plants and animals. If Big Blue Lake were to be drawn down by the 0.71 feet predicted by Mr. Davis, the location of the seepage would move down 0.71 feet vertically and an estimated 24.5 feet horizontally. The result would be a reduction in the littoral shelf conducive to seepage-dependent plant communities by approximately nine acres. The impact would likely be significant since the seepage zone is in an area of "very high" vulnerability according to Dr. Pruitt. Between October 2010 and July 2011, NTC/Knight took four measurements of water level at "BCS-01," a stage recorder in Botheration Creek. The measurements showed the water level in the creek at that point to be 0.1 to 0.32 feet. NTC/Knight also sampled for taxa of macroinvertebrates in the reach of the creek. NTC/Knight identified 46 taxa, including mussels and six long-lived taxa. The presence of the long-lived taxa and mussels indicate that the reach of the creek in the vicinity of the stage recorder should be considered to be a perennial stream. Botheration Creek is high-quality water and, as shown by NTC/Knight's sampling, it contains a diverse mix of aquatic invertebrates and fish. A drop in the level of Botheration Creek of 0.2 feet predicted by the HGL Model would have caused the creek to go dry at BCA-01 during three of the four dates on which the water level was measured. Such a drop would convert the reach of the creek in the vicinity of the stage recorder from a perennial to an intermittent stream and would eliminate the reach's viability for long-lived taxa. Similarly, upstream reaches that are intermittent would become ephemeral (streams that flow only during periods of high rainfall). If the Wellfield becomes fully operational as allowed by the Permit, there will be a reduction in the Surficial Aquifer at Botheration Creek of between 0.2 and 0.3 feet. The reduction in the aquifer will reduce flow in Botheration Creek, reduce the volume downstream, including in Pine Log Creek, and reduce out-of-bank flood frequency and duration. The result will be a reduction in nutrients delivered downstream and to the floodplain to the detriment of plants and animal life that depend on them. Additionally, other reaches of the creek that have perennial flow will be converted to intermittent streams and reaches that are intermittent will become ephemeral. The result will be the elimination of plant and animal species currently living in these portions of the creek. The impact of the HGL Model predicted drawdown to steepheads depends on the individual steephead and the drawdown contour at its location and the amount of rainfall. Four steepheads on the NTC/Knight Property could suffer impacts similar to the impact at Russ Steephead to which Dr. Pruitt assigned a high probability of impact. Russ Steephead is located on the NTC/Knight Property above Russ Pond. NTC/Knight installed Surficial Aquifer wells at Russ Steephead between the HGL Model's predicted 0.5 and 0.6 foot Surficial Aquifer drawdown contours. NTC/Knight also installed a stage recorder just downstream from the steephead. During drought, NTC/Knight observed a loss of flow from the sidewall seepage areas and in the Russ Steephead Stream. If the Surficial Aquifer at Russ Pond were to be drawn down by 0.5-0.6 feet, the sidewalls of the Russ Steephead Stream and the stream itself would lose flow in times of drought. The loss of flow would lead to oxidation and loss of organic materials in the stream channel and flood plain, resulting in soil subsidence. If the water level at the terminus of the Russ Steephead Stream were drawn down, headward down cutting in the stream channel would be induced. In such a case, in the words of Dr. Pruitt, "there is a high probability that if drawdown occurs and . . . over a long period of time," the process will make the steephead "look more like a gully . . . ." Tr. 2120. The drawdown will also reduce the frequency and duration of inundation of the sphagnum bogs in the four steepheads likely to be affected by the drawdown. The bogs and the associated animals that depend upon them would be lost. Dr. Means identified a number of temporary ponds within HGL's predicted drawdown of the Surficial Aquifer. Nine were between the 0.3 and 0.6 foot drawdown contour, and two were between the 0.6 and 0.7 foot drawdown contours. These ponds and plant and animal communities dependent upon them would likely be harmed by the drawdowns. Mr. Cantrell offered testimony to rebut the Petitioners' case on wetland impacts. His testimony was based on an evaluation of aerial photography, site visits to the Wellfield, and a one-day trip to the NTC/Knight Property. It is Mr. Cantrell's opinion that if the NTC/Knight Property were to drain, it would be because of a surface water drainage system, such as ditching, not because of drawdown in the Surficial Aquifer caused by operation of the Wellfield. Mr. Cantrell's opinion is that because the Area has been subjected to a wide range of fluctuations in water levels and the wetland systems have survived, operation of the Wellfield will not have significant impacts. Mr. Cantrell's opinion, however, overlooks the effect of constant drawdown during times of severe drought. That wetlands have survived severe drought in the past does not mean they will survive severe drought conditions exacerbated by drawdown caused by operation of the Wellfield. Monitoring Special condition 19 of the Permit requires Bay County to implement the LTEMP after the Permit is issued. The LTEMP requires Bay County to establish a monitoring network, but does not provide the location of any particular monitoring site. Sites identified in the LTEMP are recommended, but the ability to use a particular site is dependent on field verification of suitability and authorization by the landowner. Over half the area designated in the LTEMP from the HGL Model's projected 0.5 foot drawdown in the Surficial Aquifer is located on the NTC/Knight Property. It will be necessary, therefore, to include sites on the NTC/Knight Property in the ultimate environmental monitoring network. The LTEMP's recommended sites do not include monitoring of some of the most susceptible wetland systems: temporary ponds, the Botheration Creek hillside seepage bogs, and the perennial headwaters of Botheration Creek. Without this monitoring, the LTEMP will be unable to detect whether these systems are harmed by withdrawals. The Permit and LTEMP require no more than one-year of baseline data to be collected prior to initiation of water withdrawals. The proposed monitoring time is inadequate to create a sufficient record for use in determining whether a reduction in water levels is attributable to water withdrawals or natural phenomena, such as drought. Baseline monitoring should be conducted for a sufficient duration to ensure that a full range of wet and dry years is captured. The LTEMP describes the types of data that are to be collected. A missing component is sampling for frogs, salamanders, and other amphibians that are sensitive to changes in hydrologic regimes and which depend upon infrequent periods of inundation in order to breed. This type of faunal sampling is particularly important in the temporary ponds and seepage environments. Without sampling for the presence of these species, the LTEMP will be unable to determine whether these populations have been harmed by withdrawals. The LTEMP includes a number of "triggers," that if tripped, require the preparation of an auxiliary report. A number of these triggers make reference to changes in water levels at the level of "significant deviation," an undefined term. More importantly, the LTEMP fails to require any statistical analysis. Without it, the LTEMP will be inadequate to establish whether a reduction in water levels is caused by water withdrawals or another cause. Similarly, other triggers lack sufficient detail to determine when they are tripped, such as those that refer to downward movement of plants. Finally, even if one of these triggers is tripped and an auxiliary report is prepared, nothing in the Permit or LTEMP sets forth the circumstances under which withdrawals would need to be curtailed and by what amount. The purpose of the LTEMP is to determine whether withdrawals are causing harm to the wetlands within the vicinity of the Wellfield. The LTEMP fails to provide reasonable assurance that it will succeed in achieving its purpose. Reasonable-Beneficial Use Use if the Reservoir is Unavailable In the event of Reservoir unavailability, Bay County is likely to need much less than 30 MGD. The need is likely to fall between 7.42 MGD and 9.71 MGD for the current population. In 2013, the need is likely to fall between 9.40 MGD and 12.29 MGD. See NTC/Knight Ex. 5, p. 4 of 4. The Permit, however, does not limit Bay County to emergency or backup use. While Bay County might voluntarily limit withdrawals to emergency use or backup supply, it has unfettered discretion to determine what constitutes an emergency or the necessity for a backup supply. The Permit is also not restricted to essential uses. Authorization of 30 MGD provides more than Bay County's current average daily demand for potable water. If the Permit restricted the use to essential uses, the authorization would be far less than 30 MDG. The District commissioned King Engineering to assist in development of a "Coastal Water Systems Interconnect Project" (the "Interconnect Project"). On average, the utilities subject to the Interconnect Project estimated that 42 percent of the average daily demand is dedicated to essential uses with the remaining 58 percent going to non-essential uses. Consistent with the estimate, the Project set a target of 50 percent of average daily demand to be allowed for use in an emergency. None of the information from the Interconnect Project, however, was used by the District in setting the limits of withdrawal in the Permit. b. Daily Use Bay County claims the 5 MGD annual average allocation under the Permit is needed for several reasons, principally the maintenance of pumps. Bay County's justification for 5 MGD is found in testimony from Mr. Lackemacher and a document he authored entitled, "Confidential Draft for Internal Use Only 5 MGD Pumping Rate" (the "Lackemacher Confidential Draft"), admitted as Bay County Ex. 24. Mr. Lackemacher's testimony follows: A. The fact is that there are no absolute knowns when we're talking about what needs to be. Q. What do you mean? A. Well, here we have a document [Bay County Ex. 24] where I talk about rationalization for 5 million gallons a day, why we would need it, mechanical reasons, financial reasons, regulatory reasons. I always felt that it was very difficult to justify a number. I don't know. We haven't designed the system. We haven't got all of the wells in. We don't know what their specific yields are. There's unknowns here. So do we need 2 million gallons a day or 5 million gallons a day? I don't know. I don't know that. But here is the rationalization for 5 million if that's in fact what we need. We may very well find out that we don't need 5 million gallons a day. Q. Is that because you don't know the precise locations of the well and how they're going to be piped and distributed? A. That's absolutely true. Q. Well, did you in this report, Exhibit 24, did you make some reasonable assumptions? A. I based it on some of the values as you discussed or as I pointed out earlier from Hatch Mott MacDonald's preliminary design. * * * Q. And do you feel confident that your analysis supported that in the area of 5 million gallons a day is what would be needed to operate the wellfield? A. Yes. And that's why the paper was generated that [is] a justification for 5 million gallons a day, here's what we think we would need. Tr. 209-10. The Lackemacher Confidential Draft is a one-page, written justification for the 5 MGD. Based on the Hatch Mott McDonald Report, see tr. 210, it considers regulatory, mechanical and financial factors. It is not supported, however, by engineering analysis. Any financial analysis found in the Hatch Mott McDonald Report, moreover, is far from complete. The factors taken into consideration are recited in the most general of terms. For example, of four such factors, the document lists the second as: "All water pumps are designed to run - turning pumps on and off is not the best situation for the overall electrical efficiency or the mechanicals of a pump." Bay County Ex. 24. Consistent with Mr. Lackemacher's testimony, the document concludes that the amount of water needed to run each well is unknown. The financial justification is based on costs shown in the Hatch Mott MacDonald Report for construction and operation of 22 wells, ten more wells than are contained in the Wellfield and without any analysis of revenue to recoup the costs. The financial justification is a bare conclusion on the part of Mr. Lackemacher: We cannot afford to operate a well field at a financial loss, based on this fact alone we would have to pump a minimum of 4.49 MGD. Combined with the fact that we don't know what volumes of water have to be turned over to ensure water quality 5 MGD seems quite reasonable. Bay County Ex. 24. The Lackemacher Confidential Draft is dated May 17, 2011. It was not part of Bay County's Application nor was it submitted to the District prior to the decision to issue the Permit. Although the District attempted to obtain information from Bay County about what was needed for maintenance, Bay County did not provide it. As Mr. Gowans testified, "[t]hen I finally told staff, [s]top asking, we're not going to get the numbers . . . ." Tr. 552. The District performed no analysis to determine the minimum amount of water needed to maintain the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Phillip Waller, an engineer accepted as an expert in the design and construction of potable water systems, including groundwater wells, surface water, and transmission and distribution of drinking water. Mr. Waller testified that if the wells were connected to a central treatment system, there would not be the need to flush the pipeline for disinfection prior to use of the well in an emergency. Only 2.4 million gallons per year or 6,500 gallons per day would be needed to maintain optimum operating conditions, an amount far less than 5 MGD. Mr. Waller's experience when groundwater is used as a backup, moreover, is that they are operated periodically. While prudent to periodically operate backup wells especially in advance of hurricane season, vertical pumps in wells, unlike horizontal pumps, do not have a need for frequent operation because of even force distribution. They certainly do not need to be continuously operated. "In fact, wells routinely are idle for months at a time." Tr. 1123. Interference with Existing Legal Users In its Revised Staff Report dated July 18, 2011, the District wrote: Nearby Users: Under the most intensive pumping activity, drawdown in the Upper Floridan Aquifer is predicted to be approximately 15 feet in the vicinity of the nearest private wells. Water level declines of this magnitude may cause water levels to fall below the level of the pump intake in some privately-owned wells. Joint Ex. Vol. IV, Tab Q, p. 4. The District's high estimate of the number of wells used by existing legal users that might suffer impacts approaches 900. The exact number or whether any existing legal users would be likely to suffer impacts was not proven. Alternatives Groundwater wells, if installed and attached to the fitting in the existing transmission line that delivers water from the Pump Station to the Water Treatment Plant, could serve as backup to the Reservoir. Bay County did not conduct a study of whether groundwater in the area of the transmission line was adequate to serve as an alternative. Mr. Waller, on behalf of NTC/Knight and Washington County, on the other hand, testified that the transmission line could support ten wells with a capacity of 10 MGD and could be constructed at a cost of $12 million, far less than the Wellfield. The area of the transmission line is in an area identified by the District as acceptable for the creation of potable water wells. The area does not present a significant risk of saltwater intrusion if not used continuously. The water meets the drinking water requirements for the Department of Environmental Protection and the Department of Health. The existing transmission line alternative is located near the existing raw water supply line which minimizes the need for additional piping. There is sufficient length along the existing raw water pipeline to accommodate ten wells. The existing transmission line alternative, therefore, has significant potential to succeed as a water supply backup to the Reservoir. NTC/Knight and Washington County, through Mr. Waller, also proposed another alternative: an intake at Bayou George. Near Highway 231, the main pipeline from the intake would run along public right-of-way. North of the existing intake in Williams Bayou and three miles north of the Dam, the proposed intake would be less susceptible to contamination from storm surge. Neither Bay County nor the District presented a thorough analysis of any alternative to the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Mr. Waller that there are two alternatives that could be constructed at much less cost than the Wellfield and that have significant potential of providing backup supply.

Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Northwest Florida Water Management District enter a final order that denies the application of Bay County for the individual water use permit at issue in this proceeding. DONE AND ENTERED this 26th day of July, 2012, in Tallahassee, Leon County, Florida. S DAVID M. MALONEY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 26th day of July, 2012.

Florida Laws (9) 120.569120.57120.574373.019373.069373.223373.709403.8907.42 Florida Administrative Code (1) 62-40.410
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SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT vs BALM ASSOCIATES, INC., 02-001116 (2002)
Division of Administrative Hearings, Florida Filed:Tampa, Florida Mar. 19, 2002 Number: 02-001116 Latest Update: Dec. 16, 2002

The Issue The issue is whether Respondents should be subject to civil penalties and required to submit a Compliance Plan for the reasons stated in the Administrative Complaint and Order filed on January 8, 2002.

Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Background In this enforcement action, Petitioner, Southwest Florida Water Management District (District), proposes to assess civil penalties against, and require a compliance plan from, Respondents, Balm Associates, Inc. (Balm) and Goodson Farms, Inc. (Goodson), on the grounds that from March 1999 through July 2001 they made water withdrawals from certain property in Hillsborough County, Florida, without a water use permit, and after a permit was obtained in August 2001, they continued to exceed the annual average daily withdrawals authorized under the permit through the month of November 2001, or just prior to the preparation and issuance of the Administrative Complaint and Order (Complaint).1 While not denying that excessive pumpages may have occurred, and that a permit was not obtained until August 2001, Balm points out that it is the owner-lessor of the property and not the consumptive user of the water, and contends that the District has no authority to enforce its rules against, and recover civil penalties from, the non-user of the water. In its request for a hearing, Goodson did not specifically dispute the allegation that it consumed water without a permit, or exceeded the withdrawal limits under the new permit, but contended instead that the limits were unrealistic and should be modified. At the final hearing, however, Goodson disputed the accuracy of the water consumption figures used in the Complaint. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries and to administer and enforce Chapter 373, Florida Statutes. Balm is a corporation registered to do business in the State of Florida. Its mailing address is 2101 Huntington Avenue, Sarasota, Florida 34232. It owns approximately 220 acres of land in Section 28, Township 31 South, Range 21 East, in Hillsborough County, Florida, which is the site of the alleged wrongdoing. Goodson is a corporation registered to do business in the State of Florida. Its mailing address is Post Office Box 246, Balm, Florida 33503. Goodson is in the farming business and operates a total of 13 farms, including the farm at issue in this proceeding. Permit Requirements Under Rule 40D-2.041(1), Florida Administrative Code, a water use permit is required whenever total withdrawal capacity from any source or combined sources is greater than or equal to 1,000,000 gallons per day (gpd); annual average withdrawal from any source or combined sources is greater than or equal to 100,000 gpd; or withdrawal is from a well having an outside diameter of 6 inches or more at the surface. Rule 40D-2.351(1), Florida Administrative Code, provides that a permittee must notify the District within 30 days of the sale or conveyance of permitted water withdrawal facilities or the land on which the facilities are located. The same rule also provides that where a permit has been issued to a party whose ownership or legal control of the permitted water withdrawal facilities subsequently ends, the party who assumes control over the facilities may apply to transfer the permit to himself or herself up to the renewal date of the transferor's permit. Finally, Rule 40D-2.351(2), Florida Administrative Code, provides that until a permit is transferred or a new permit is obtained, the party subsequently controlling the permitted water withdrawal facilities will be in violation of District rules for making withdrawals without the required permit. History of Permits on the Property On September 29, 1989, the District issued Water Use Permit No. 207135.001 (the .001 permit) to James Brown (Brown) and B & T Growers Partnership (B & T) for water withdrawals from one well for agricultural purposes on Balm's property. The .001 permit authorized annual average withdrawals of 102,000 gpd of groundwater for agricultural irrigation. On August 29, 1990, the District adopted new rules applicable to District permits within the Eastern Tampa Bay Water Use Caution Area (ETBWUCA). The .001 permit was within the ETBWUCA, and Brown and B & T were provided with a Notice of Permit Modification and new Permit Conditions. The new conditions became effective November 15, 1990. New Condition No. 5 provided that By July 31, 1995, all permitted withdrawal points shall be equipped with totalizing flow meters or other measuring devices as approved in writing by the Director, Resource Regulation Department. Such devices shall have and maintain accuracy within five percent of the actual flow installed. On December 14, 1992, the District approved the transfer of the .001 permit from Brown and B & T to B. Kenda Produce. The Unpermitted Water Withdrawals On June 30, 1997, Goodson entered into a two-year agricultural lease with Balm to use a portion of the property, including acreage previously used by B. Kendra Produce. At the time the lease was entered into, neither Respondent applied to the District to have the .001 permit transferred from B. Kendra Produce. It can be reasonably inferred from the evidence that after the first lease expired, the parties continued to execute new lease agreements at least through the time of the hearing. The portion of the property which Goodson leased and farmed is referred to as the "Sweat Loop Farm" and consists of approximately 100 acres. There is one well with an outside diameter of 10 inches at the surface located on the Sweat Loop Farm. The well's total withdrawal capacity is approximately 1,500 gallons per minute (gpm), which is over 1,000,000 gpd. Thus, withdrawals from the well required a water use permit. As noted earlier, Goodson operates a total of 13 farms on approximately 2,500 acres of land. There are approximately 15 wells on all 13 farms, including the Sweat Loop Farm. Michael E. Hare, an irrigation supervisor who is responsible for the irrigation of all 13 of Goodson's farms, installed a total of approximately 8 meters on the farms, including the meter on the Sweat Loop Farm. A totalizing flow meter, which was made by MiCrometer, was installed at the Sweat Loop Farm in June 1997. Mr. Hare acknowledged that he was familiar with MiCrometer meters and would be aware if the MiCrometer flow meter on the Sweat Loop Farm was not functioning properly. Whenever metering devices on the various Goodson farms have malfunctioned in the past, Mr. Hare has taken the malfunctioning meter to a metering company to be fixed. Goodson began irrigating the Sweat Loop Farm in June 1997. Since that time, Goodson has been the sole water user of the well on the farm. In March 1999, Goodson began submitting to the District monthly pumpage reports for the groundwater withdrawals on the Sweat Loop Farm. Although some unmeasured withdrawals presumably occurred prior to March 1999, the Complaint does not identify these as being a violation. Mr. Hare and other supervisors are responsible for collecting the meter readings which go on the monthly pumpage reports and providing them to the District. The information on the reports includes the permit number; the last month's meter reading; the current month's meter reading; the total gallons of water pumped for the current month; the meter total; and the meter factor. To determine the average daily withdrawal on the Sweat Loop Farm, the District relied upon the calculations provided by Goodson as to the total gallons of water pumped for the month and divided this number by 30 days. From March 1999 through July 2001, these quantities were as follows: MONTH/YEAR AVERAGE DAILY PUMPAGE March 1999 April 1999 531,487 No data available May 1999 364,930 June 1999 0 July 1999 0 August 1999 57,410 September 1999 49,563 October 1999 222,667 November 1999 250,667 December 1999 755,003 January 2000 689,433 February 2000 695,073 March 2000 544,427 April 2000 305,153 May 2000 597,720 June 2000 0 July 2000 62,120 August 2000 86,370 September 2000 123,233 October 2000 602,020 November 2000 409,550 December 2000 145,823 January 2001 957,690 February 2001 890,213 March 2001 391,280 April 2001 467,640 May 2001 617,177 June 2001 0 July 2001 0 Under Rule 40D-2.041(1)(a)-(c), Florida Administrative Code, a water use permit was required for Goodson's withdrawals since the well's total withdrawal capacity is approximately 1,500 gpm, which is greater than 1,000,000 gpd; the annual average withdrawals exceeded 100,000 gpd; and the well has an outside diameter of 10 inches at the surface. The withdrawals on the Sweat Loop Farm were not authorized by the .001 permit since neither Goodson or Balm was a permittee under the permit. Even if Goodson could rely on the permit, which it cannot, pumpage data provided by Goodson reflects that the water withdrawals (except for nine months) were in excess of that authorized by the permit. On June 16, 2000, the District mailed a Notice of Non-Compliance for excessive water withdrawals to Goodson. The Notice indicated that if the pumpage values submitted by Goodson were incorrect, Goodson was to explain the error and provide corrected quantities. On June 26, 2000, the District received a written response to the Notice of Non-Compliance from the superintendent of the Sweat Loop Farm who indicated that the pumpage values were correct, and that the excess usage was due to a "serious drought condition" which had caused a "significant financial hardship on [the] farm." The response also indicated that Goodson would contact Mr. Haftel, owner of Balm, to request that he "revise the water use permit for spring crops." On November 22, 2000, the District mailed Goodson a Notice of Violation indicating that the quantities authorized by the .001 permit were still being exceeded and that the District might seek monetary penalties if Goodson failed to come into compliance within 30 days. Despite the foregoing Notice, Goodson continued to make withdrawals without a permit and in excess of the quantities formerly authorized under the .001 permit until August 2001 when a new permit was finally obtained. Issuance of a New Water Use Permit On January 2, 2001, the District received an application for a General Water Use Permit seeking to modify the .001 permit to increase the withdrawal quantities and to transfer the permit from B. Kendra Produce to Balm. "Seymour Haftel/ Balm Associates, Inc." was listed as the applicant, and "Donn Goodson" from " Goodson Farms" was listed as the contact or consultant. Mr. Haftel signed the application on behalf of Balm. Goodson assisted Balm in securing the permit for the Sweat Loop Farm because Goodson wanted more water for irrigation purposes. Section 2.1 of the Basis of Review for Water Use Permit Application, adopted and incorporated by reference by Rule 40D-2.091, Florida Administrative Code, provides that "[a]pplications for leased property, except property leased from the District, must be either a joint application in the name of the lessee and the property owner(s) or be only in the name of the property owner(s)." In a Request for Additional Information mailed to Balm on January 29, 2001, the District asked whether Goodson should be listed as co-applicant on the application. On April 27, 2001, Balm submitted a response which indicated that Goodson should not be listed as co-applicant. On August 6, 2001, the District issued Water Use Permit No. 200007135.002 (the .002 permit) to Seymour Haftel/Balm Associates, Inc. authorizing an increase in the annual average withdrawals to 224,300 gpd. The permit had an expiration date of September 29, 2009. The permit contained a number of special conditions, none of which were challenged by Balm. Unauthorized Withdrawals Under the .002 Permit Special Condition No. 2 of the .002 permit requires in part that the permittee: continue to maintain and operate the existing non-resettable, totalizing flow meter(s), or other flow measuring device(s) as approved by the Regulation Department Director, Resource Regulation, for District ID No(s), Permittee ID No(s)[,] G-1. Such device(s) shall maintain an accuracy within five percent of the actual flow as installed. Total withdrawal and meter readings from each metered withdrawal shall be recorded on a monthly basis and reported to the Permit Data Section, Records and Data Department, (using District forms) on or before the tenth day of the following month. In the event a permittee chooses not to use a totalizing flow meter, as required by Special Condition No. 2, the District will review information provided by the measuring device's manufacturer to determine if the measuring device would maintain a five percent accuracy as required by the Condition. The meters have to be monitored and calibrated periodically for accuracy. It is the permittee's responsibility to comply with the conditions of the permit, including Special Condition No. 2, which requires the submittal of accurate pumpage reports. Goodson submitted the meter readings on behalf of Balm beginning in September 2001, which covered the withdrawals for the month of August 2001. The District relied on the meter readings submitted by Goodson to determine the annual average daily pumpage calculation for the .002 permit. The calculation is a running 12-month average, whereby each month the annual average daily quantity is recalculated based on the previous 12-month pumpage. The running annual average daily pumpage and percentage of pumpage which exceeded the .002 permit from August 2001 through May 2002 are as follows: MONTH/YEAR ANNUAL AVERAGE DAILY PUMPAGE PERCENTAGE OVERPUMPED August 2001 378,462 69 percent September 2001 382,622 71 percent October 2001 376,687 68 percent November 2001 383,008 71 percent December 2001 379,212 69 percent January 2002 327,343 46 percent February 2002 321,530 43 percent March 2002 350,701 56 percent April 2002 356,013 59 percent May 2002 338,131 51 percent As the foregoing data reflects, the withdrawals from the Sweat Loop Farm were in excess of that authorized by the .002 permit from August 2001 through May 2002.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Southwest Florida Water Management District enter a final order determining that Respondents are guilty of the charges in its Administrative Complaint and Order except as concluded in paragraph 48 above and endnote 2 below; that Respondents be required to submit an acceptable written plan (Compliance Plan) to the District for its consideration and approval within fourteen days after entry of the final order; that the Compliance Plan describe how Respondents shall achieve full compliance with the .002 permit; that the Compliance Plan include reductions in withdrawals, water conservation measures, and development and utilization of alternative resources; that the Compliance Plan establish deadlines for implementation and completion of corrective actions; that full compliance be achieved within 120 days after entry of the final order; and that any failure of Respondents to comply with any provision of the Compliance Plan shall constitute a violation of the final order. DONE AND ENTERED this 30th day of July, 2002, in Tallahassee, Leon County, Florida. ___________________________________ DONALD R. ALEXANDER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 30th day of July, 2002.

Florida Laws (5) 120.56120.569120.57373.119373.219
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DESOTO CITIZENS AGAINST POLLUTION, INC. vs FARMLAND HYDRO LIMITED PARTNERSHIP, REDLAND GROWERS EXCHANGE, INC., AND SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 02-000232 (2002)
Division of Administrative Hearings, Florida Filed:Bartow, Florida Jan. 16, 2002 Number: 02-000232 Latest Update: Jun. 18, 2004

The Issue Whether General Water Use Permit (WUP) Number 20012185.000 (Permit) meets the conditions for issuance as established in Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, and should be issued to Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc.

Findings Of Fact The Parties DCAP is not-for-profit corporation incorporated in the State of Florida. Behrens is the President of DCAP. See also Findings of Fact 63-77. Farmland Hydro is a Delaware Limited Partnership authorized to transact business in Florida, and is the owner of the property leased by Basso/Redland, which is the subject of this WUP. Frank T. Basso, Jr., is a third generation farmer, who operates as Redland Growers Exchange, and seeks a General WUP to authorize groundwater withdrawals for crop irrigation. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries pursuant to Chapter 373, Florida Statutes, and the rules promulgated thereunder as Chapter 40D, Florida Administrative Code. The Proposed Water Use An Application for a General WUP was submitted by Farmland Hydro and Basso, as co-applicants, and received by the District on April 11, 2001. After receipt of additional information, the Application was deemed complete on October 22, 2001. The Applicants seek a General WUP to authorize a new water use for the irrigation of 140 acres for the production of both Spring and Fall row crops, using a seepage-with-mulch irrigation system.1 Basso plans to grow tomatoes and/or peppers in the Spring, and squash and/or cucumbers in the Fall. Crop planting for both seasons will be phased-in over a one-month period. Water allocation quantities are calculated on a weekly phase-in basis of approximately 35 acres for each planting date. The total time that the parcel will be in use for farming, to include planting and harvesting for each crop, is approximately six months per year. The subject parcel is part of a 250-acre tract known as the Brushy Creek Tract and is located in Hardee County approximately two miles south of the town of Ona; approximately two miles south of the intersection of U.S. Highway 64 and County Road 663; and is within the Southern Water Use Caution Area (SWUCA). The subject parcel currently does not contain a water well. The Brushy Creek Tract is a larger parcel of approximately 1,230 acres leased from Farmland Hydro by Redland and also by Parker Farms for cattle grazing, farming, and hunting. The subject parcel is used for cattle grazing and is surrounded by land owned by Farmland Hydro and used for either cattle grazing or agricultural row crops. Farmland Hydro also operates an additional approximately 1,941 acres of property near the subject parcel, which is used for citrus groves. Farmland Hydro has consumptive WUPs for this property. The closest existing legal user to the proposed Basso well site is another well on the Farmland Hydro property. As is generally done with vegetable crop production in Florida, vegetable crops grown on the Farmland Hydro property are grown in rotation with pasture, and have been rotated in this manner for many years. Typically, farmers have farmed a piece of land for one, two or three years and then, to avoid the buildup of insects and diseases, have allowed the land to revert to pasture and have moved on to another field for crop production. The subject parcel for which the WUP is being sought will be similarly treated. Crop rotation is an important agricultural best management practice that is used to address pest management, soil conservation, and maximizing nutrients for obtaining favorable crop production. Soil conservation is important to Basso, notwithstanding that there is a response in the Application that no approved Soil Conservation Service plan exists for the operation included in the Application. If the WUP is issued and the subject parcel is placed into crop production, another parcel of land will be taken out of crop production by Basso, resulting in the discontinuation of another permitted well. As a result, the issuance of this WUP will not result in a "water use change." Determination of Reasonable Demand/Allocated Quantities In determining whether a proposed water use is reasonable-beneficial and in the public interest, the District calculates the appropriate permit quantities for the particular water use, which is a function of demonstrated need, or demand for water; efficiency of the water treatment and distribution systems; whether water is sold or transferred to other entities; whether acceptable water can be acquired from lower quality sources; and whether conservation practices are employed. District Basis of Review (BOR), page B3-1. The reasonable need for agricultural water use is generally composed of one or more demand components, depending upon the specific agricultural use. "Typically, the reasonable need for irrigation water uses is equal to the supplemental crop requirement divided by the system efficiency or the system design capacity, whichever is less." "The supplemental crop requirement is the amount of water needed for a particular crop beyond the amount of water provided by effective rainfall." The supplemental crop requirement is generally determined by using the Agricultural Water Use Calculation Program (AGMOD) Version 2.1, which is based on the modified Blaney-Criddle method. This program takes into account site specific information such as crop type, growing period, evapotranspiration rate, soil type, rainfall, irrigation method and number of irrigated areas. "In most cases, the supplemental irrigation requirement is determined for a 2 in 10-year drought condition." The AGMOD program determines an inch-application rate which, when applied to the number of acres to be irrigated, results in a calculation of total annual average and peak monthly quantities for the proposed water use. District BOR, pages B3-4 and 3-5. See also District Water Use Design Aids, pages C4-1 through C4-7. In determining the allocated quantities, or reasonable demand for water, the District seeks to avoid both over- allocating water and under-allocating water for the specific crop intended, to ensure that the permitted amount is sufficient for the "2 in 10-year drought condition." Consequently, the allocated quantities arrived at by District staff through use of the AGMOD methodology may be different from the quantities indicated on an applicant's initial application, which are generally estimated without benefit of an agricultural water use calculation program. The AGMOD program was used to calculate water use quantities for the proposed water use. The allocated quantities for Basso's proposed use are 454,000 gallons per day (gpd) on an annual average basis and 1,241,000 gpd, as a peak month quantity. No quantities were requested or allocated for crop protection. See Finding of Fact 52. Modeling for Simulated Impacts As part of the application review process, the District evaluates potential impacts to existing legal uses of water, the water resources and environmental features that may result from the proposed groundwater withdrawals. To assist in the review process, analytical and numerical models, which incorporate best available hydrogeologic parameters for the area being considered for a permit, are used to simulate drawdowns for the withdrawal of the proposed quantities. The results of these simulations are used in the evaluation of potential impacts to assess whether the application meets the conditions for issuance. The District undertook simulation modeling of the potential effects of the proposed water withdrawals to be authorized by the permit. The allocated quantities were entered into the MODFLOW 387 groundwater flow model, which is a three- layer model developed by the U.S. Geological Survey and is the generally accepted model for this purpose. Model layers were set up to represent the surficial, intermediate, and Upper Floridan aquifers. (The Applicants seek to pump water solely from the Upper Floridan Aquifer.) There are limitations to the model in that the model assumes a homogeneous isotropic aquifer, with no preferred flow direction. In actuality, there is variability in the geology of the area. Modeling is intended to serve as a screening tool for assessing localized impacts anticipated from a proposed water use and is based upon the best available information. As distance from the proposed withdrawal site increases, the reliability of the modeling decreases, due to the variability in the geology and other parameters or boundary conditions that can affect the model. Use of the MODFLOW groundwater model allows the District to look at potential impacts at the site, and in the proximity of the site, and assists the District in assessing possible cumulative impacts associated with a proposed use. To assist in assessing potential impacts from the proposed use, a Peak Month modeling simulation was undertaken by the District, which simulates the effect of pumping the proposed Peak Month withdrawal rate of 1,241,000 gpd for 90 consecutive days, with no recharge to the aquifer systems. The model essentially presents a worst case scenario that is a more severe prediction than what is actually likely to occur from the permitted use under normal conditions. Simulating the period of greatest demand on the hydrologic system is likely to provide maximum protection to existing legal water users and the water resources. The Peak Month simulation undertaken by the District predicts drawdowns in the potentiometric surface of the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site; less than 1.4 feet at the nearest property boundary (approximately 1,250 feet from the proposed withdrawal site); and less than 1.2 feet at the nearest existing legal user (a Farmland Hydro well approximately 3,500 feet from the proposed withdrawal site). These numbers did not raise a concern for District staff. ("Potentiometric surface" is "a surface defined by the level to which water rises in an open pipe that is constructed into or all the way through an artesian aquifer. This is measured in feet relative to NGVD or sea level. The level to which water rises inside this open pipe is a function of the pressures on the water in the artesian aquifer." District BOR, page B-xii.) The Peak Month simulation predicts drawdowns in the intermediate aquifer of approximately 0.9 feet at the proposed withdrawal site, and less than 0.9 feet at the property boundary, and at the nearest existing legal user. The Peak Month simulation predicts drawdowns in the water level of the surficial aquifer (water table) of approximately 0.01 feet or less at the proposed withdrawal site, property boundary and nearest existing legal user. Based upon the Peak Month simulations, the District reasonably determined that further cumulative impact modeling was not necessary in order to assess localized cumulative impacts resulting from the proposed use. To assess regional cumulative impacts, the District evaluated Regional Observation Monitoring Program (ROMP) data and found no significant trends in withdrawals in recent years, other than a slight decline attributed to the recent drought. Conditions of Issuance of the Proposed Permit In order to obtain a water use permit, an applicant must establish that the proposed use of water is a reasonable- beneficial use, will not interfere with any existing legal use of water, and is consistent with the public interest, by providing reasonable assurance, on both an individual and cumulative basis, that the water use meets the conditions for issuance as specified in Section 373.223(1), Florida Statutes, and Rule 40D-2.301, Florida Administrative Code. A permit must be obtained from the District prior to withdrawing water, where the withdrawal is from a well having an outside diameter of six inches or more at land surface, where the annual average withdrawal from all sources is 100,000 gpd or greater, or where the total combined withdrawal capacity from all sources is greater than or equal to 1 mgd. The proposed water use falls within these parameters. Rule 40D-2.041(1)(b) and (c), Florida Administrative Code. The quantities allocated for the proposed use have been determined by the District to be necessary to fulfill a certain reasonable demand, for the reasons specified herein. To assist in assessing impacts, the District utilizes a network of ROMP wells to obtain basic groundwater monitoring data over time and to help characterize the lithology, stratigraphy, aquifer depths, water levels and, in some cases, water quality for the various water resources. Data obtained from the ROMP and other wells is compiled to ascertain aquifer characteristics within the District and is also integrated into the District's modeling efforts pertaining to proposed water uses. ROMP well No. 31 is located just off the northeast corner of the Basso site. Having a ROMP well adjacent to the Basso site increases confidence in the specific geological information being used in the groundwater model to assess potential impacts from the proposed uses. ROMP well No. 17 is located approximately 1/2 mile from DCAP member Behren's well. Data from both wells were considered in assessing potential impacts from the proposed water use. Based on available information, the possible sources of groundwater for the proposed use at the Basso site are the surficial aquifer, intermediate aquifer, and the Upper Floridan Aquifer systems. To ensure sufficient quantities of water for the proposed use and to avoid potential impacts to environmental features, such as wetlands and surface waters, the District will require the proposed use to limit withdrawals to solely the Upper Floridan Aquifer. By examining stratigraphic cross sectional information generated from the ROMP wells, particularly ROMP No. 31 well, which is in close proximity to the Basso site, District staff were able to determine, with reasonable certainty, the approximate depths of the aquifers at the Basso well site. To ensure that the well will be open solely to the Upper Floridan Aquifer, the permit requires the Basso well to have a minimum of 400 feet of casing, with an estimated well depth of 1,000 feet. Based upon available information concerning the construction of other wells in the vicinity of the proposed Basso well, the District is reasonably assured that a well cased for a minimum of 400 feet will draw water only from the Upper Floridan Aquifer and will minimize the potential for water to move between the aquifers through the well. The well construction requirements imposed for Basso's well are in line with the best available stratigraphic information and with known construction of wells in the area. By casing the well to a depth of 400 feet and due to the extremely low leakage of the intermediate confining unit, the intermediate and surficial aquifers will be buffered from impacts associated with the proposed use. The District will deny a water use permit application if the proposed withdrawal of water, together with other withdrawals, would cause an unmitigated adverse impact on a legal water withdrawal existing at the time of the application. The District considers an adverse impact "to occur when the requested withdrawal would impair the withdrawal capacity of an existing legal withdrawal to a degree that the existing withdrawal would require modification or replacement to obtain the water it was originally designed to obtain." District BOR, page B4-14. Based upon an assessment of individual and cumulative regional information, there are no existing legal uses of water that will be adversely impacted as a result of the proposed withdrawals. Based upon an assessment of individual and cumulative regional information, no quantity or quality changes that adversely impact the water resources, including both surface and groundwaters, are anticipated from the proposed withdrawals. The District requires that consideration be given to the lowest water quality available, which is acceptable for the proposed use. Lower quality water includes reclaimed water, collected stormwater, recovered agricultural tailwater, saline water or other sources. District BOR, page B4-12. For the proposed water use, there is no viable lower quality water source and no reclaimed water available near the site to use as an alternative to groundwater pumping. The Applicants are proposing to use the lowest quality water that is available. There are no known concerns regarding the quality of water in the Upper Floridan Aquifer at this location in Hardee County. Restricting the proposed water use to the Upper Floridan Aquifer will not cause water quality concerns or result in pollution to any of the aquifers. Simulated drawdowns to the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site, less than 1.4 feet at the nearest property boundary, and less than 1.2 feet at the nearest permitted well, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the intermediate aquifer of 0.9 feet at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the surficial aquifer of 0.01 feet or less at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, constitute a nearly undetectable impact to the surficial aquifer, which is not an adverse impact. The modeling simulations demonstrate that the proposed withdrawals will have no significant effect on the surficial aquifer and, therefore, will not cause adverse impacts to environmental features such as wetlands, lakes, streams, fish and wildlife, or other natural resources. None of the simulated drawdowns are considered to be predictions of adverse impacts, not even in the localized vicinity of the well site. Mr. Jackson explained that because the localized modeling simulations were small or insignificant and showed no adverse impacts, cumulative modeling is not considered necessary. Reasonable assurance on a cumulative basis is determined by assessing the potential localized impacts in conjunction with existing cumulative data for the region, such as the available ROMP data and hydrographs, which depict the existing regional condition, taking into account, on a cumulative basis, all existing uses as well as rainfall conditions and climate. Based on an assessment of the cumulative data and the modeling for individualized impacts, and applying professional judgment, District staff reasonably concluded that the proposed water use presents no concerns that it will cause, on either an individual or a cumulative basis, adverse impacts to the water resource or existing legal uses. Minimum flows and levels have not been established by the District for the area where the proposed use is located. (The parties stipulated that the District has not established minimum flows and levels pursuant to Section 373.042, Florida Statutes, for the Southern Water Use Caution Area (SWUCA)). Therefore, Rule 40D-2.301(1)(d), Florida Administrative Code, (requirements for minimum flows and levels), is not applicable to the proposed permit. The proposed use presents no concerns for saline water intrusion. The proposed use raises no concerns regarding causing pollution to the aquifer. There are no offsite land uses that will be adversely impacted as a result of this permit. Basso currently uses best management practices for water conservation in his ongoing farming operations, and intends to use such practices with the new farming operation authorized under the permit. In keeping with such practices, irrigation is stopped when the water reaches the end of the watering ditch. Basso uses seepage irrigation and tries to regulate the ditches so that there is a minimum, if no, runoff. Also, a watering cycle generally lasts from three to seven days before irrigation has to be resumed. Any runoff goes into "filtering ponds, before reaching ditches or creeks" in its raw content. Basso does not intend to farm during months of likely frost so no separate allocation for frost/freeze protection was requested or needed. Given these irrigation practices, water is not reasonably expected to be wasted. All necessary and feasible agricultural water conservation activities will be implemented upon issuance of the WUP. In addition, Specific Condition No. 3 of the proposed WUP requires the incorporation of best water management practices in all irrigation practices. The proposed use presents no concerns that it will otherwise be harmful to the water resource. The Applicants have met all the requirements for issuance of a WUP. Southern Water Use Caution Area The proposed water use site is located within the SWUCA. The District established the SWUCA as a means of addressing on a regional scale concerns about long-term impacts to the water resource. Water use caution areas were created in recognition of regional water concerns. There have been drought conditions in the area which have caused reduced aquifer levels. The proposed water use site is not within the "Most Impacted Area" (MIA), which is located approximately 18 miles to the west of the site in Manatee County, nor within the "East Tampa Bay Water Use Cautionary Area" (ETB WUCA), which is approximately six miles to the west of the proposed site, also in Manatee County. (The SWUCA includes the MIA and ETB WUCA.) Pending final adoption of rules for the SWUCA, the District will continue to issue WUPs for proposed water uses that meet the conditions for issuance. The District cannot treat new uses and existing renewal uses any differently when considering the issuance of a permit. Once SWUCA rules and minimum flows and levels are established, the District expects to rely on a more regional approach to address long-term cumulative impacts over the entire use caution area, instead of relying on a permit-by-permit basis to address regional concerns. Standard Condition No. 9 of the proposed WUP requires the permittee to cease or reduce withdrawals as directed by the District, if water levels in the aquifers fall below the minimum levels established by the District Governing Board. The proposed withdrawal will use a seepage with mulch irrigation method, which has a 50 percent efficiency level. See footnote 1. This is the minimum efficiency level currently required for agricultural WUPs within the SWUCA, which approve the use of this irrigation method. As SWUCA rules come into effect, a higher percentage efficiency level probably will be required, as is now required in the Eastern Tampa Bay Water Use Caution Area and also in the Highlands Ridge Water Use Caution Area. Consequently, Standard Condition No. 11 of the proposed WUP requires that, when SWUCA rules are implemented, the permittee must comply with any higher efficiency level or other special regulation that may be required for the SWUCA area. DCAP's Challenge to the Proposed WUP DCAP does not keep official membership records. It does not maintain any list of current members. According to Behrens, there are five members of the board of directors. DCAP does not hold corporate meetings, annual meetings or maintain corporate records. Members do not meet. There are no means to document the existence of members for this organization. Behrens is a member of DCAP. He has owned five acres adjoining the west side of Horse Creek (in DeSoto County) since 1985. Behrens complains that the District does not look at the cumulative effect on his well and other people he knows, such as George Chase. Behrens is concerned with any lowering of the water level in the area, including Horse Creek. He believes that approval of wells in the area, including the proposed well, is the straw that is breaking the camel's back. Mr. Chase shares this view. Behrens relies on an artesian free-flowing, two-inch diameter well, for domestic water use, located in the intermediate aquifer, approximately 150 feet deep. (Behrens' well is approximately 18-20 miles from the proposed Basso well.) For most of the time he has lived there, the well had an electric pump for obtaining water. Approximately one year ago, the pump went bad, and a replacement system has not been installed. Currently, Behrens has no pump on the well, and in dry periods, has to obtain water for domestic uses from nearby Horse Creek, which is low during the dry season. (Behrens depends on Horse Creek to pursue his recreation, wildlife, and aesthetic values.) Having a flowing artesian well will enable him to obtain water from the well without having to install an electrical pump, a situation which is desired by Behrens, in part, because the property is in a flood plain and experiences frequent flooding and electrical outages. Not all artesian wells flow. Artesian wells are completed into confined aquifers in which the water in a tightly cased well, will rise to a level above the formation being measured. Water would have to rise above the land surface to be a flowing well. For a well to be artesian, the well must be under confined pressure. For a well drawing water from a confined aquifer, such as the intermediate or the Upper Floridan Aquifer systems, the measured water level in the well is a reflection of the amount of potentiometric pressure in the well. This level can be affected just as much by the amount of recharge as it can by the amount of water withdrawals. There is no evidence that the proposed water use will adversely impact the flowing nature of either Behrens' or Chase's well. The evidence demonstrates that the proposed water use will not adversely impact Behrens' well. George Chase is a member of DCAP. Mr. Chase lives in Arcadia, DeSoto County, Florida. His property is adjacent to the Peace River. Mr. Chase's well is a two-inch diameter well, believed to be about 150 feet deep and equipped with a 12-volt DC solar-powered pump. Mr. Chase has in the past relied on artesian pressure within the confined intermediate aquifer to supply water to his solar-powered home. The solar-powered pump assists in supplying water to the home. In recent years, Mr. Chase has experienced low water pressure in his well. In Spring 2000, Mr. Chase contacted the District to complain that when an adjacent citrus grove was irrigating the groves, it appeared to affect the water level in his well such that the well's ability to flow was impacted. (According to Mr. Chase, his neighbors have had problems obtaining sufficient water from their wells and reaching water with standard pumps.) This citrus grove is an existing legal user of water that pre-existed Mr. Chase's well. In recent years, numerous domestic wells have been constructed in the vicinity of the Chase home that are large diameter wells utilizing submersible pumps with 110-volt AC power. These wells are more efficient at producing water than the type of well and pump being used by Mr. Chase, are located within a few hundred feet of Mr. Chase's well, and are open to the intermediate aquifer as is the Chase well. Based upon the District's experience in other areas, where there is a cluster of domestic wells drawing from the same intermediate aquifer, such adjacent wells have a much greater impact on each other than do other more distant wells, such as the previously discussed citrus irrigation wells, that are open solely to the confined Upper Floridan Aquifer System. This conclusion is based upon monitoring of the ROMP sites in the affected areas. Mr. Chase's well is approximately ten miles from the proposed withdrawal site. There is no basis to conclude that the proposed water use will cause any adverse impacts to Mr. Chase's well. DCAP members' interests are not affected any differently by the proposed use than are the interests of the general public. DCAP has produced no evidence to support its assertion that the issuance of this permit will result in lowered water levels in the Horse Creek and Peace River or other surface waters. DCAP has produced no evidence to support its assertion that the permit will cause adverse impacts to surface water flows or surface waters or to environmental features such as vegetation, fish, and wildlife. DCAP has produced no evidence that its substantial interests are affected by the proposed agency action.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that Southwest Florida Water Management District enter a final order: Determining that Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc., have satisfied the requirements of Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, regarding conditions for issuance of WUPs;3 Issuing proposed General Water Use Permit No. 20012185.000, as set forth in District Exhibit No. 4; and Finding that DCAP lacks standing to challenge the issuance of the permit. DONE AND ENTERED this 3rd day of June, 2002, in Tallahassee, Leon County, Florida. CHARLES A. STAMPELOS Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 3rd day of June, 2002.

Florida Laws (6) 120.569120.57373.019373.042373.223403.412
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BECKY AYECH vs SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 01-002294 (2001)
Division of Administrative Hearings, Florida Filed:Sarasota, Florida Jun. 07, 2001 Number: 01-002294 Latest Update: Dec. 24, 2001

The Issue The issue presented for decision in this case is whether Respondent, the Southwest Florida Water Management District (the "District"), should issue Water Use Permit ("WUP") No. 20005687.003 to Dr. Thomas E. Kelly, pursuant to the terms of the proposed permit issued on April 11, 2001.

Findings Of Fact Based on the oral and documentary evidence adduced at the final hearing and the entire record in this proceeding, the following findings of fact are made: PARTIES Petitioner Becky Ayech is a resident of Sarasota County and a citizen of the State of Florida. The District is a water management district in the State of Florida created pursuant to Section 373.069(1)(d) and (2)(d), Florida Statutes. The District is the governmental agency charged with the responsibility and authority to review and act upon water use permit applications, pursuant to Chapter 373, Part II, Florida Statutes, and Chapters 40D-1 and 40D-2, Florida Administrative Code. Dr. Thomas E. Kelly is the owner of the real property in Sarasota County on which Pop's Golf and Batting Center is located, and as such is recognized as the applicant for and holder of any WUP issued for the property. Pursuant to a 50- year lease with Dr. Kelly, Ralph Perna owns and operates Pop's Golf and Batting Center and is the person who would be responsible for day-to-day compliance with the terms of the WUP at issue. Neither Dr. Kelly nor Mr. Perna formally intervened in this proceeding. THE PROPOSED PERMIT The proposed permit is for irrigation and sanitary uses at a golf driving range and batting cage facility called Pop's Golf and Batting Center, on Fruitville Road in Sarasota County. The site leased by Mr. Perna comprises approximately 30 acres, of which the westward 15 acres is taken up by the Pop's facility. The eastern 15 acres is heavily wooded, overgrown with brush, and contains a five-acre lake. The majority of the 15 acres used by Pop's is taken up by the landing area for the driving range. Near the front of the facility are a tee box and putting green sown with Bermuda grass. This grassy area, about six-tenths of an acre, is the only part of the 30-acre property requiring irrigation, aside from some landscape plants in front of the business office. The landing area is not watered and is not even set up for irrigation. The Pop's facility is in a low-lying area historically prone to flooding. For this reason, the tee box, putting green, and business office are elevated about two and one-half feet higher than the landing area. This elevation also serves the esthetic purpose of allowing golfers to follow the flight of their drives and watch the balls land. The proposed WUP is a renewal of an existing permit. The existing permit is premised on the property's prior use for agriculture, and permits withdrawals of 34,000 gpd on an average annual basis and 99,000 gpd on a peak monthly basis. The renewal would authorize withdrawals of 1,700 gpd on an average annual basis and 4,400 gpd on a peak monthly basis, reductions of 95 percent and 96 percent, respectively. "Average annual" quantity is the total amount of water withdrawn over the course of one year. This quantity is divided by 365 to arrive at the allowable gallons per day. "Peak monthly" quantity is the amount of water allowed to be withdrawn during the driest month of the year. This quantity is divided by 30 to arrive at the allowable gallons per day. Pop's draws water from two wells on the property. A six-inch diameter well, designated District Identification No. 1 ("DID 1"), is used for irrigation of the tee box and putting green. A four-inch diameter well, designated District Identification No. 3 ("DID 3"), is used to supply water to the two restrooms at the facility. THE PERMIT CONDITIONS The proposed WUP includes the following basic information: the permittee's name and address; the permit number; the date the permit application was filed; the date the permit was issued; the expiration date of the proposed permit; the property location; the quantity of water to be permitted; the withdrawal locations; and the water use classification proposed pursuant to the District's permit application. The District's permit application provides the applicant with the following five choices regarding proposed water use: Public Supply; Industrial or Commercial; Recreation or Aesthetic; Mining or Dewatering; and Agriculture. The proposed permit in this case has been classified as Recreation or Aesthetic. The proposed WUP would allow the permittee to withdraw from DID 1 an average of 1,600 gpd, with a peak monthly withdrawal of 4,200 gpd, and to withdraw from DID 3 an average of 100 gpd, with a peak monthly withdrawal of 200 gpd. The proposed WUP contains four Special Conditions. Relevant to the issues raised in this proceeding, Special Condition No. 3 requires the permittee to incorporate best water management practices, to limit daytime irrigation to the greatest extent practicable, to implement a leak detection and repair program, to conduct a system-wide inspection of the irrigation system at least once per year, and to evaluate the feasibility of improving the efficiency of the current irrigation system. Special Condition No. 4 requires the permittee to submit a conservation plan no later than April 30, 2006. The plan must address potential on-site reuse of water and external sources of reuse water. The proposed WUP also contains 16 Standard Conditions. Standard Condition No. 2 reserves the District's right to modify or revoke the WUP following notice and a hearing, should the District determine that the permittee's use of the water is no longer reasonable and beneficial, consistent with the public interest, or if the water use interferes with an existing legal use of water. Standard Condition No. 3 provides that the permittee may not deviate from the terms of the WUP without the District's written approval. Standard Condition No. 4 provides that, if the District declares a water shortage pursuant to Chapter 40D-21, Florida Administrative Code, the District may alter, modify, or declare inactive all or any part of the proposed WUP as necessary to address the water shortage. Standard Condition No. 5 provides that the District will collect water samples from DIDs 1 and 3, or require the permittee to submit water samples to the District, if the District determines there is a potential for adverse impacts to water quality. Standard Condition No. 9 provides that the District may require the permittee to cease or reduce its withdrawals if water levels in aquifers fall below minimum levels established by the District. Standard Condition No. 11 provides that the District may establish special regulations for Water Use Caution Areas ("WUCAs"), and that the permit will be subject to such regulations upon notice and a reasonable period to come into compliance. Standard Condition No. 12 requires the permittee to install flow metering or other measuring devices to record withdrawal quantities, when the District deems it necessary to analyze impacts to the water resource or existing users. CONDITIONS FOR ISSUANCE OF PERMIT Generally, the miniscule withdrawals proposed by Pop's would not fall within the District's permitting authority, which mostly confines itself to withdrawals of 100,000 gpd or more. However, Rule 40D-2.041(1)(c), Florida Administrative Code, requires a permit for any withdrawal from a well having an outside diameter of six inches or more at the surface. DID 1 has an outside diameter of six inches. An applicant for a WUP must demonstrate that the proposed use of water is reasonable and beneficial, is in the public interest, and will not interfere with any existing legal use of water, by providing reasonable assurances on both an individual and a cumulative basis that the proposed use of water satisfies the 14 specific conditions set forth in Rule 40D-2.301(1)(a)-(n), Florida Administrative Code, identified in the subheadings below. Necessary to Fulfill a Certain Reasonable Demand Pop's is open for business twelve hours per day. During the summer months, it averages 100 customers per day. The tee box and putting green at Pop's are heavily used. When golfers hit balls from the tee box, they make small gouges, or divots, in the Bermuda grass. These divots are later filled with sand, and the grass naturally grows over them. Irrigation is essential to the health of the Bermuda grass, allowing the application of fertilizer and chemicals to treat for pests and fungus. The tee box and putting green are watered as little as possible, because over-watering can itself lead to fungus problems with the Bermuda grass. The District uses an irrigation allocation computer program called AGMOD to determine reasonable average annual and peak monthly quantities for irrigation in an objective and consistent manner. Data on the pump capacity, soil type, the area to be irrigated, and its geographic location are input, and AGMOD allocates a quantity of water sufficient to irrigate for the driest 20 percent of the time, based on 75 years of historic rainfall data. The AGMOD program allows quantities for irrigation of the fairways of a typical golf course; however, Pop's does not have fairways and thus the proposed permit does not authorize any water for such irrigation. The District's expert, David Brown, credibly testified that the amounts allocated under this permit are conservative because the area to be irrigated is a high traffic area, because the irrigation methodology employed by Pop's ensures that 75 percent of the water withdrawn from DID 1 will get to the grass, because of the fertilizers and chemicals necessary to maintain and repair the grass, and because of the elevation of the area to be watered. Mr. Brown testified that the AGMOD model uses native soil types, not the fill used to elevate the tee box and putting green, and therefore the soil for the elevated areas will likely require more water and drain more quickly than AGMOD indicated. The quantities allocated for withdrawals from DID 3 on an average annual and peak monthly basis are necessary to fulfill the demand associated with the use of the two restrooms by Pop's employees and customers. In summary, the amounts of water authorized for withdrawal under the proposed permit are no more than necessary to fulfill a certain reasonable demand. Quantity/Quality Changes Adversely Impacting Resources The evidence at the hearing established that the operation of DIDs 1 and 3 pursuant to the terms of the proposed WUP will cause no quality or quantity changes adversely impacting the water resources. The proposed withdrawal amounts constitute a decrease of 95 percent on an average annual basis and of 96 percent on a peak monthly basis from the existing permit. The District reasonably presumes that decreases in permitted withdrawal amounts will not cause quantity or quality changes that will adversely impact the water resources. Nonetheless, Mr. Brown performed groundwater modeling to confirm that the District's presumption was correct in this case. The first step in model development is to study the geology at the site being studied. Mr. Brown looked at detailed information from surrounding WUPs and geographic logs to arrive at a "vertical" view of the stratigraphic column in place at Pop's, giving him an idea of which zones below Pop's produce water and which zones confine water and impede its movement between the producing units. Mr. Brown then looked to site-specific aquifer test information from other permits to give him an idea of the "horizontal" continuity of the system across the area under study. The hydrogeologic profile at Pop's contains five different aquifer production zones separated by confining units of clay or dense limestone. Moving downward from the surface, the production zones are the surficial aquifer, zones called Production Zone 2 ("PZ-2") and Production Zone 3 ("PZ- 3") within the intermediate aquifer, and the Suwannee limestone and Avon Park limestone layers within the Upper Floridan aquifer system. DID 3 has approximately 96 feet of casing and a total depth of approximately 195 feet. It draws water from PZ-2, the upper production zone of the intermediate aquifer. DID 1 was built before the District assumed regulation of well construction and consumptive water use; therefore, the District does not possess specific information as to its construction. Mr. Brown reviewed historical documents, including a 1930s report by the United States Geological Survey ("U.S.G.S.") about irrigation wells drilled in the location now occupied by Pop's. Mr. Brown's review led him to a reasonable conclusion that DID 1 has approximately 75 to 100 feet of casing and is drilled to a total depth of 600 to 700 feet below land surface. The District's water level measurements confirmed Mr. Brown's judgment, indicating that the well penetrates only through the Suwannee limestone formation in the Upper Floridan aquifer. His hydrogeological findings in place, Mr. Brown proceeded to perform a number of analyses using a five-layer groundwater model based on the "Mod-Flow EM" program developed by the U.S.G.S. to determine whether the withdrawals authorized by the proposed WUP would have any adverse impacts on water resources. The model's five layers simulated the five aquifer zones found in the area of Pop's. Mr. Brown performed simulations to predict the effect of the combined pumping of DID 1 and DID 3 at 1,700 gpd on a steady state basis and at 4,400 gpd for a period of 90 days. A "steady state" model assumes continuous pumping at the stated quantity forever. The scenario for pumping 4,400 gpd for 90 days is called a "transient" model, and simulates the effect of continuous pumping at the peak month quantity, without replenishment of the water source, for the stated period. Both the steady state and transient models used by Mr. Brown were conservative, in that it is unlikely that their scenarios would actually occur at Pop's. The modeling predicted that Pop's withdrawals would have no effect on the surficial aquifer or on the deep Avon Park limestone formation. Because DID 1 is likely to open to the PZ-2, PZ-3, and Suwannee limestone production zones, Mr. Brown analyzed the steady state and transient conditions for each zone. The greatest effect predicted by any of the modeling runs was a drawdown in water levels of approximately two-hundredths of a foot in the PZ-3 and Suwannee limestone zones. This drawdown would extend no farther than the boundary of Pop's property. All of the predicted drawdowns were smaller than the natural fluctuations in water levels caused by changes in barometric pressure. Thus, any possible effects of withdrawals at the quantities proposed in the WUP would be lost in the background noise of the natural water level fluctuations that occur in all confined aquifers. The water level or pressure within subterranean production zones is referred to as the "head." For water to move from one zone to another, there must be a difference in head between the zones. The evidence established that groundwater quality declines with depth at the Pop's site, but that the heads in the PZ-2, PZ-3, and Suwannee limestone production zones are essentially the same in that area. The similarity in heads means that there is no driving force to move water between the zones and thus no potential for adverse water quality changes caused by DID 1's being open to multiple production zones. In summary, the amounts of water authorized for withdrawal under the proposed permit will not cause quantity or quality changes which adversely impact the water resources, including both surface and ground waters. Adverse Environmental Impacts to Wetlands, Lakes, Streams, Estuaries, Fish and Wildlife, or Other Natural Resources Mr. Brown's model indicated there would be no drawdown from the surficial aquifer, where there would be the potential for damage to water related environmental features and/or the fish and wildlife using those features as habitat. Petitioner offered no evidence indicating that the proposed water use will cause adverse environmental impacts. Deviation from Water Levels or Rates of Flow The District has not established minimum flows or levels for the area including Pop's. Therefore, Rule 40D- 2.301(1)(d), Florida Administrative Code, is not applicable to this WUP. Utilization of Lowest Quality of Water Ninety percent of the water withdrawn from DID 1 will come from the Suwannee limestone formation and is highly mineralized and of lower quality than the water in PZ-2 or PZ- 3. DID 3 draws its water from PZ-2. As noted above, DID 3 provides water to the two restrooms on the premises of Pop's. Because its water is used in the public restrooms, DID 3 is considered a limited public supply well, the water from which must meet potable standards. Mr. Brown testified that, though PZ-2 provides water of higher quality than do the zones beneath it, that water only barely meets potable standards. Lower quality water than that obtained from PZ-2 would require extensive treatment to meet potable standards. Reuse or reclaimed water is unavailable to Pop's under any rational cost-benefit analysis. There is a reclaimed water transmission network in Sarasota County, but the nearest point of connection is more than one mile away from Pop's. The wetland lake on Pop's site is unsuitable because extensive land clearing, pipeline construction, and intensive filtration would be required to use its water. Such a project would not be technically or economically feasible for the small amount of water in question. The evidence establishes that Pop's will utilize the lowest quality water available. Saline Water Intrusion The evidence demonstrated that the proposed use will not significantly induce saline water intrusion. Saline water intrusion occurs in the Avon Park limestone formation. Withdrawals must cause a drawdown in the Avon Park formation to further induce saline water intrusion. DID 1 does not penetrate into the Avon Park formation. Mr. Brown's modeling indicated that the withdrawals allowed under the proposed WUP will not cause any drawdown in the Avon Park formation. Pollution of the Aquifer The proposed use will not cause pollution of the aquifer. As noted above, absent a difference in head or some driving force, there is no potential for water to be exchanged between the confined producing zones. Any small quantity that might be exchanged due to the pumping of the well would be removed by the same pumping. There is no potential for pollution of the aquifer by storm water moving through DID 1 or DID 3 because there is no head differential or driving force to move storm water down into the wells. The District's historic water level measurements indicated that during the rainy season, when the site is most likely to be inundated, water levels in the wells are 0.15 feet above land surface. The well structures extend at least one foot above ground level and are sealed with plates and gaskets. Adverse Impacts to Existing Off-site Land Uses The proposed use will not adversely impact off-site land uses. The District's reasonable practice, when authorizing renewal of the permit for an existing well, is to consider off-site impacts only where the applicant seeks to increase withdrawal amounts. In this case, the applicant is requesting a substantial decrease in the amount of withdrawals allowed under the renewed WUP. Adverse Impacts to Existing Legal Withdrawals The proposed use will not adversely affect any existing legal withdrawals of water. The District's reasonable practice, when authorizing renewal of the permit for an existing well, is to consider adverse impacts to existing legal withdrawals only where the applicant seeks to increase withdrawal amounts. In this case, the applicant is requesting a substantial decrease in the amount of withdrawals allowed under the renewed WUP. As noted above, Mr. Brown's modeling indicated that any drawdowns caused by these withdrawals are so small as to be lost within the natural fluctuations of water levels in the aquifer, even at the edge of Pop's 30-acre site. Petitioner's well is more than ten miles away from the wells at Pop's. Utilization of Local Resources to Greatest Extent Practicable The proposed use of water will use local resources to the greatest extent practicable, because the water withdrawn pursuant to the permit will be used on the property where the withdrawal occurs. Water Conservation Measures The proposed use of water incorporates water conservation measures. Pop's uses a commercial irrigation system with low volume misters, spray tips and sprinkler heads, and a rain gauge that automatically shuts down the system if one-eighth to one-quarter inch of rain falls. Mr. Perna testified that the automatic shutdown system rarely has the opportunity to work, because he manually shuts down the system if the weather forecast calls for rain. Mr. Perna testified that the typical golf range irrigates from 30 to 45 minutes per sprinkler head. Pop's irrigates roughly eight minutes per head. Overwatering can cause fungus on the Bermuda grass, giving Pop's a practical incentive to minimize irrigation. Pop's irrigates only the high traffic areas of the tee box and putting green, not the landing area. In its Basis of Review, the District has adopted a water conservation plan for golf courses located in the Eastern Tampa Bay Water Use Caution Area ("WUCA"). Basis of Review 7.2, subsection 3.2. Pop's is located in the Eastern Tampa Bay WUCA, and has implemented the items that golf courses are required to address in their conservation plans. Reuse Measures Given the small total irrigated area and the efficiency of the irrigation methods employed by Pop's, there is no realistic opportunity to capture and reuse water on the site. There is no reuse water realistically available from other sources. Thus, Pop's incorporates reuse measures to the greatest extent practicable. Waste Given the reduction in permitted quantities and the limited scope of the irrigation, the proposed use will not cause waste. Otherwise Harmful to District Resources No evidence was presented that the use of this water by Pop's will otherwise harm the water resources of the District. PETITIONER'S EVIDENCE Petitioner testified on her own behalf and presented the testimony of Ellen Richardson. Ms. Richardson testified that she had once seen a sprinkler running at Pop's during a rainfall, though she conceded that it had just begun to rain when she saw it. Ms. Richardson also testified that she had more than once seen sprinklers running at Pop's during daylight hours. However, Mr. Brown testified that some daytime irrigation is permissible under the District's watering restrictions, where heat stress and applications of fertilizers and chemicals make daytime watering necessary. These conditions applied to Pop's. Petitioner's chief concern was with her own well. Since the late 1980s, she has experienced intermittent water outages. The District has repeatedly worked with Petitioner on her well problems, and Petitioner feels frustrated at the District's inability to solve them. However, the District's evidence established that Petitioner's problems with water levels in her own well could not possibly be caused or exacerbated by the withdrawals at Pop's, ten miles away. To the extent that the renewal of this WUP will result in drastic decreases in permitted withdrawals, Petitioner's position would be improved even accepting her theory that these withdrawals have some impact on her well. In her petition, Petitioner alleged that there were disputed issues of material fact as to eight of the fourteen permitting criteria discussed above. While she engaged in spirited cross-examination of the District's witnesses, Petitioner offered no affirmative evidence showing that the any of the conditions for issuance of permits were not met. Petitioner's chief attack was that Rule 40D- 2.301(1), Florida Administrative Code, requires "reasonable assurances" that the permittee will fulfill the listed conditions, and that the applicant here could not supply "reasonable assurances" because of his long history of failure to comply with the conditions of prior permits. As evidence, Petitioner offered the District's historic record of this permit, which indeed was replete with correspondence from the District requesting records related to pumpage and water quality, and apparent silence from Dr. Kelly in reply. However, the record also explains that the failure to provide data was not the result of obduracy, but because farming had ceased on the property. When the less water intensive use of the driving range commenced approximately nine years ago, the owner ceased monitoring activities. The District, under the impression that farming was still taking place on the property, continued to request pumpage and water quality data for several years after the conversion. It appears from the record that Dr. Kelly, an absentee landlord, simply did not bother to respond. Dr. Kelly's past discourtesy does not rise to the level of calling into question the reasonable assurances provided in this permit renewal application, particularly where the lessee, Mr. Perna, has every reason to ensure that the conditions of the WUP are fulfilled. The evidence did not prove that Petitioner participated in this proceeding for an improper purpose--i.e., primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of licensing or securing the approval of the permit renewal application. To the contrary, the evidence was that Petitioner participated in this proceeding in an attempt to raise justifiable issues as to why the permit renewal application should not be granted. In particular, Petitioner raised an important policy issue as to whether an applicant's history of failure to comply with permit conditions should be considered by the District in assessing the reasonableness of the applicant's assurances of future compliance. The District contended that the applicant's compliance history is irrelevant. While the District ultimately prevailed on the substantive issue, its procedural claim of irrelevance was rejected, and Petitioner was allowed to attempt to prove her contention as to Dr. Kelly's noncompliance. It is not found that Petitioner's litigation of this claim was frivolous.

Recommendation Upon the foregoing Findings of Fact and Conclusions of Law, it is recommended that the Southwest Florida Water Management District enter a final order determining that Dr. Thomas E. Kelly has satisfied the requirements of Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, regarding conditions for issuance of water use permits, and that the District issue Water Use Permit No. 20005687.003 to Dr. Thomas E. Kelly. DONE AND ENTERED this 27th day of November, 2001, in Tallahassee, Leon County, Florida. ___________________________________ LAWRENCE P. STEVENSON Administrative Law Judge Division of Administrative Hearings Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative this 27th day of November, 2001. COPIES FURNISHED: Becky Ayech 421 Verna Road Sarasota, Florida 34240 Jack R. Pepper, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34604 E. D. "Sonny" Vergara, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899

Florida Laws (6) 120.569120.57120.595373.019373.069373.223
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OSCEOLA FISH FARMERS ASSOCIATION, INC. vs SOUTH FLORIDA WATER MANAGEMENT DISTRICT, 01-002900RP (2001)
Division of Administrative Hearings, Florida Filed:West Palm Beach, Florida Jul. 20, 2001 Number: 01-002900RP Latest Update: Mar. 20, 2003

The Issue The issues are whether the proposed amendment to Rule 40E- 2.041(1), Florida Administrative Code, exceeds the agency's grant of rulemaking authority; enlarges, modifies, or contravenes the specific law implemented; or is vague, fails to establish adequate standards for agency discretion, and vests unbridled discretion in the agency.

Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Petitioner, Osceola Fish Farmers Association, Inc. (OFFA), is a non-profit corporation whose members consist of tropical fish farmers in Osceola County, Florida. The parties have stipulated that OFFA has standing to bring this action. Respondent, South Florida Water Management District (District or Respondent), is a public corporation operating pursuant to Chapter 373, Florida Statutes, with its principal office in West Palm Beach, Florida. Among other things, the District has the authority to regulate the uses of water within its geographic boundaries, including Osceola County. On an undisclosed date, the District began test drawdowns (a lowering of the elevation of the water through control structures) in the Alligator Chain of Lakes just east of St. Cloud in Osceola County, where OFFA's members are engaged in tropical fish farming. The drawdowns were undertaken for the purpose of allowing the Florida Fish and Wildlife Conservation Commission (FFWCC) to conduct demucking activities in the lakes to enhance aquatic habitat. Prior to beginning work, the FFWCC obtained an Environmental Resource Permit from the Department of Environmental Protection (DEP). However, the District did not require either itself or the FFWCC to obtain a consumptive use permit on the theory that a lake drawdown for demucking activities was not a consumptive use and therefore did not require a permit. In an effort to halt future scheduled drawdowns, OFFA participated in a United States Army Corps of Engineers proceeding which culminated in the preparation of an Economic Impact Statement for FFWCC's drawdowns; filed a complaint with DEP under Section 373.219(2), Florida Statutes, alleging that an unlawful consumptive use (without a permit) was taking place (which complaint was found to be insufficient); filed an action for injunctive relief in circuit court under Section 403.412, Florida Statutes (which was dismissed or dropped for undisclosed reasons); and finally initiated a proceeding against the District under Section 120.56(4), Florida Statutes, alleging that the District had adopted "an incipient non-rule policy of exempting lake 'drawdowns' from water use permitting requirements" (DOAH Case No. 00-3615RU). To avoid the consequences of an adverse ruling in the latter action, the District began rulemaking proceedings to adopt an amendment to Rule 40E-2.041(1), Florida Administrative Code, to codify its policy relative to lake drawdowns. As amended, the rule reads as follows: Unless expressly exempt by law or District rule, a water use permit must be obtained from the District prior to any use or withdrawal of water. The drawdown of lakes for environmental, recreational, or flood control purposes is not regulated by Chapter 40E-2 or 40E-20, F.A.C. (Underscored language represents amended language). Petitioner has challenged only the amendment, and not the existing rule. The effect of the rule is obvious - a lake drawdown for one of the three stated purposes in the rule will not require a permit, while all other lake drawdowns will. As specific authority for the proposed amendment, the District cites Sections 373.044 and 373.113, Florida Statutes. The former statute authorizes the District to "adopt rules pursuant to [Chapter 120] to implement the provisions of this chapter," while the latter statute authorizes it to "adopt rules pursuant to [Chapter 120] to implement the provisions of law conferring powers or duties upon it." The District has cited Sections 373.103(1), 373.219, and 373.244, Florida Statutes, as the specific laws being implemented. The first statute provides that if specifically authorized by DEP, the District has the authority to "administer and enforce all provisions of this chapter, including the permit systems established in parts II, III, and IV of [Chapter 373], consistent with the water implementation rule"; the second statute provides in relevant part that the District may "require such permits for consumptive use of water and may impose such reasonable conditions as are necessary to assure that such use is consistent with the overall objectives of the district or department and is not harmful to the water resources of the area"; and the third statute provides for the issuance of temporary permits while a permit application is pending. In regulating the uses of water within its boundaries, the District administers a comprehensive consumptive water use permit program under Part II, Chapter 373, Florida Statutes. Both parties agree that under Section 373.219(1), Florida Statutes (2000), all "consumptive uses" of water require a permit, except for the "domestic consumption of water by individual users," which use is specifically exempted by the same statute. The global requirement for permits is also found in Rule 40E-2.041 (the rule being amended), as well as Rule 40E- 1.602(1), which provides in relevant part that unless expressly exempted by statute or rule, "[a] water use individual or general permit pursuant to Chapters 40E-2 or 40E-20, F.A.C., must be obtained prior to use or withdrawal of water " The term "consumptive uses" is not defined by statute, but the District has promulgated a rule defining that term. By Rule 40E-2.091, Florida Administrative Code, the District has adopted by reference a document known as the "Basis for Review for Water Use Permit Applications with the South Florida Water Management District." Section 1.8 of that document contains definitions of various terms used in the permitting program, including "consumptive use," which is defined as "[a]ny use of water which reduces the supply from which it is withdrawn or diverted." The District's policy for lake drawdowns, as proposed in the rule amendment, is inconsistent with this definition. On this disputed issue, Petitioner's evidence is accepted as being the most persuasive, and it is found that a lake drawdown for any purpose is a consumptive use of water. Section 373.219(1), cited as a specific law being implemented, provides that the District "may require such permits for consumptive use of water and may impose such reasonable conditions as are necessary to assure such use is consistent with the overall objectives of the district and department and is not harmful to the water resources of the area." The District construes this language as authorizing it to decide which uses of water are a "consumptive use," and which are not, and to implement a rule which codifies those decisions relative to lake drawdowns. Not surprisingly, Petitioner views the statute in a different manner and argues that the statute simply allows the District to create a permit program that is consistent with Chapter 373; that under the law a permit is required for all consumptive uses, including lake drawdowns; and that the District has no authority to carve out an exception for a lake drawdown from the permitting process, no matter what the purpose. As noted above, the District has identified three instances (for environmental, recreational, and flood control purposes) when a lake drawdown does not require a consumptive use permit. These terms are not so vague that a person of common intelligence would have difficulty understanding them. However, the proposed rule contains no prescribed standards to guide the District in its administration of the rule.

Florida Laws (12) 120.52120.536120.56120.682.04373.044373.103373.113373.219373.223373.244403.412
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DR. GEORGES BLAHA, ET AL. vs. AQUARINA DEVELOPMENTS, INC., 81-002259 (1981)
Division of Administrative Hearings, Florida Number: 81-002259 Latest Update: Sep. 09, 1982

Findings Of Fact By application No. 2-7738 filed on June 29, 1981, Aquarina has requested a withdrawal for consumptive use of ground water in Brevard County in the amount of 468,000 gallons per day (850,000 gallons per day maximum) of raw water (before processing). The purpose of the proposed consumptive water use is a proposed development of 196+- acres in Brevard County located between Mullet Creek, a tributary of the Indian River and the Atlantic Ocean in South Brevard County. It is located on the barrier islands separated from the mainland by the Indian River, and is 13 miles south of Melbourne and 5 miles north of Indian River County. Aquarina proposes to develop a condominium community with a projected population of 3,500 persons consisting of 1,600 residences, a commercial area, and 500 hotel rooms. An on-site well field is proposed as well as reverse osmosis water treatment and wastewater treatment plants which are to be constructed near the southern boundary of the development. Two wells with a capacity of approximately 500 gallons per minute are proposed to be constructed and both will withdraw water from the Floridian Aquifer for conversion by reverse osmosis treatment into potable water. 3/ In addition to potable water supply requirements for the development, although part of the requirement will be met by wastewater, there is a requirement for irrigation water for landscaping. The Aquarina site has been zoned Planned Unit Development (PUD) since 1973 and the proposed densities are in accordance with those established in the Brevard County Comprehensive Plan and Zoning Ordinance. As a result of an earlier application of Aquarina for consumptive use, a temporary water use permit was granted by the District to allow Aquarina to drill test wells for aquifer testing before the present application for water use would be considered by the District. This earlier application is not now at issue. Pursuant to this temporary permit, Aquarina conducted an aquifer test program. During the first test, well #1 (the northernmost well) was utilized as a monitor or observation well for the test conducted on well #2, and an existing mosquito control well was also used as an observation well. A two-step pump test was run for 24 hours, with drawdown readings recorded at all three wells. The pump test analysis showed that the Floridian Aquifer transmissivity (the measure of the ability of the aquifer to transmit water) ranged from 173,000 gallons per day per foot at the observation wells to 87,000 gallons per day per foot at the discharge well. The total depth of these two wells was #1 -- 425 feet and #2 -- 412 feet. Following submission of the results of the first aquifer test and the application for consumptive use filed on June 29, 1981, the District staff prepared a Technical Staff Report (TSR) for the benefit of the District Governing Board based upon the two wells drilled pursuant to the temporary permit. However, because the proposed withdrawals would be from the Sebastian Inlet fresh water lens which is a finite potable source of water rapidly being depleted by existing domestic uses and mosquito control wells, the TSR recommended, among other things, that the two wells be deepened to a depth below the Sebastian Inlet fresh water lens and cased to the depth of 450 feet to insure that withdrawals occur from expected saltier water below the lens. Also, the District staff recommended that three mosquito control wells on the Aquarina property be properly plugged to eliminate fresh water loss from the lens due to the following wells. The three flowing mosquito control wells on the site were estimated to have been flowing at 432,000 gallons per day. The Sebastian Inlet fresh water lens from which Aquarina initially intended to withdraw its water appears as two underground bubbles or lenses of water fresher than the surrounding connate or saltier water. The lenses apparently are a result of stratigraphic entrapment of fresh water due to geological formations and are not being recharged with fresh water. When withdrawals are made from these lenses, salty or connate-water fills the void left by the fresher water following withdrawal. The two lenses were substantially larger during recent times but, because of many domestic uses as well as mosquito control wells which have been flowing freely, the reservoirs have shrunk significantly. Based upon present usage, the north portion of the lens will last until approximately the year 2000 at current rates of consumption and the south portion of the lens will last until approximately the year 2030 at current rates of consumption. Because of the impact on the Sebastian Inlet lens, the staff of the District could not recommend approval of Aquarina's application unless Aquarina agreed to three main conditions: The Applicant would case its production wells to 450 feet below the surface, to avoid interference with the freshwater reservoir. (Because of the combined factors of upward artesian pressure in the aquifer, the greater density of salt or connate water in relation to fresh- water, and the known range of transmis- sivity and storage factors for that portion of the aquifer [an underground waterbearing stratum or group of strata] in that geographical area, connate water would flow upward and from the sides into the area of the Applicant's withdrawal of water from beneath the lens, and the lighter, fresh water of the lens above would remain there, free from interfer- ence by the withdrawal.) The Applicant would have to plug all the preexisting mosquito control wells on the development site. The Applicant would have to undergo early monitoring of the chemical quality of this water and the water within the fresh water reservoir. As a result of Aquarina's agreement to meet these three conditions, the Technical Staff Report (TSR) issued by the District on August 20, 1981, recommended approval of the application with the addition of the above conditions. During the course of (1) deepening of well #2 to a depth of 650 feet and backplugging to 595 feet; (2) casing it to a depth of 450 feet; (3) performing a second aquifer test on the deeper well; and (4) evaluating the proposed withdrawals, Aquarina's consultants came to the following conclusions which were unrebutted by other evidence submitted at the final hearing: During the process of deepening well #2 to 650 feet, later backplugged to 595 feet, the consultants discovered an aquitard or confining layer made up of small clay-sized particles which retard the vertical flow of water at a depth of 440 to 450 feet. This well was cased to a depth of 450 feet or to the top of the aquitard. Before reaching this layer, the quality of water was generally declining with increasing depths. Below this layer, the quality of water improved to a depth of approximately 550 feet and the transmissivity was greater below the aquitard than above. Further, that same aquitard was also discovered in a mosquito control well on site when it was logged. Sufficient quantities of treatable water are available from the deepened well to supply the needs of the Aquarina project. That in both the June, 1991, and the subsequent aquifer test, there appeared to be interferences from other sources which impact the potentiometric pressure levels of the wells on the Aquarina site. These were identified as the South Brevard Utilities Corporation (SBUC) and nearby domestic well users. That the results of the June, 1981, test and computer modeling were that the impact of the proposed Aquarina with- drawls on existing nearby wells drilled to the shallower level was between a one to two foot decline in the potentiometric pressure. The average potentiometric pressure in the local aquifer is 27 feet above National Vertical Geodetic Datum (NVGD) or Mean Sea Level (MSL). These existing nearby wells were identified to be the SBUC well approximately 2,400 feet away from Aquarina and those wells of nearby homeowners in the same vicinity as the SBUC well. That flownet analysis (EPA computer model) of the results of the second aquifer test program revealed that approximately 6% of the water obtained from the deepened well would come from the layers above the aquitard, i.e. connate water and the Sebastian Inlet fresh water lens. Based on this model, the effect on water quality for existing users of the proposed withdrawals was concluded to be insignificant and known existing users would not be harmed by the proposed withdrawals. The aquitard was observed in the Aquarina deepened well and the observation mosquito control well which was logged. It was impossible to state definitely that the observed aquitard in the area was a continuous geologic feature. Partly due to the proximity of the aquitard and the depth of the wells in relation to the Sebastian Inlet fresh water lens, the conclusion was reached that effect on water quality of the Aquarina withdrawals would be insignificant. There is no fresh water recharge into the Sebastian Inlet fresh water lens, but there is a continuous pressure con- nection throughout the Florida aquifer in the area. Any replacement of water discharged from the Sebastian Inlet fresh water lens or the lower zones will be of saltier, less potable connate water. It is not understood how long the part of the aquifer below the aquitard (lower zone) will continue to be a significant source of fresh water due to insufficient data. The three mosquito control wells on the Aquarina site are flowing when uncapped or unplugged an estimated 432,000 gallons per day while the wells in the northern sector of the Sebastian Inlet fresh water lens (below where Aquarina is located) flowed at an approximate rate of 2.6 MGD. These withdrawals by the mosquito control wells are primarily from the Sebastian Inlet fresh water lens and are the major cause of premature depletion of the lens. The testimony and the data presented at the hearing demonstrated that the Applicant has met its burden to show by a preponderance of the evidence that the proposed withdrawals by Aquarina will not significantly affect either the quality or quantity of water available to neighboring water users. This appears to be the case regardless of whether the aquitard testified to be about ten feet thick exists and whether the leakance value of less that 6% exists in the aquifer between the point of the Aquarina withdrawals and neighboring users. Data which may be generated subsequently may lead to a different conclusion, but this finding is based on the data presented to the Hearing Officer by the parties at the hearing. 4/ Aquarina has agreed to the following permit condition: (b) The applicant would have to plug all the preexisting mosquito control wells on the development site. The proper plugging of the mosquito control wells on the Aquarina site will save approximately 432.000 GPD of water from the finite Sebastian Inlet lens. This condition was agreed to independently of the contribution by Aquarina of $25,000 to the well plugging program with the District and Brevard County which has as its goal, the plugging of all mosquito control wells in the area. Without the plugging of the mosquito control wells, it is estimated that the northern reservoir of the lens would be depleted by the year 2000, and the southern reservoir by the year 2030. It was also estimated that the plugging of the mosquito control wells would prolong the life of the fresh water reservoirs by over 100 years. Furthermore, by plugging all the mosquito control wells, approximately 6,700,000 gallons per day will be saved from the entire lens area. The basin in which Aquarina is located is in an overdraft condition with more water withdrawn than is presently being recharged. However, the Aquarina project will bring about a net improvement in the situation due to the mosquito control well plugging program imposed as a condition of the permit. Under the sites current PUD zoning, a density of 12 dwelling units per acre is permitted. The current classification of the property in the Brevard County Comprehensive Plan is "urbanizing." Under that classification, the Applicant could seek a rezoning of the property from PUD to single family attached residential. Such a reclassification would avoid the requirements of Chapter 373, Florida Statutes, by allowing each of the 196+- dwelling units to have its own well with a per unit consumptive use below the quantity required to activate Chapter 373, Florida Statutes. Nothing would prevent any of the residential wells from tapping the fresh water lens presently used by the Petitioners in a total amount exceeding that sought in the instant application. Given the designated land use of the Aquarina site, the controlled withdrawal from one or two points within the development is a preferable alternative to the unregulated development and water use which in all probability would follow from the denial of this permit. In large measure, the District's options regarding this site and its attendant consequences have been predetermined by land use decisions made by local officials. Under these circumstances, the District has been required to choose among a set of options which do not include an option for controlled and limited growth directly tied to availability of fresh water resources envisioned by the Petitioner. The choice which the District made in this case, although obviously not ideal, is the best among the presently available alternatives.

Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED: That the Respondent St. Johns River Water Management District grant the requested consumptive water use permit to the Applicant Aquarina Developments, Inc., subject to the conditions contained in the staff's TSR, as corrected and amended on March 25, 1982, which include, but are not limited to: The maximum daily withdrawal shall not exceed 9.765 million gallons per day for five years. The maximum annual withdrawal shall not exceed 171 million gallons for five years. The existing ten inch public supply wells shall be lined or cased to a depth of 450 feet below land surface to insure with- drawals from below this depth. The construction standards used to perform these well modifications shall be accomplished through all appropriate permitting regulations and conform to existing construc- tion standards as stated in Chapter 373, Florida Statutes (F.S.) and Chapter 40C-3, Florida Administrative Code (F.A.C.). That any subsequent Public Supply well or wells constructed for this project be cased to an equal depth. That all mosquito control wells (3) within the property boundaries of the permittee be plugged with neat cement grout from bottom to top as specified in Chapter 40C-3, F.A.C. Chloride concentrations and dissolved solids in water samples from each water supply well shall be measured monthly, and results shall be submitted within 60 days of measure- ment to the St. Johns River Water Management District. A complete water quality analysis including Ca, Mg, Na, K, Cl, S04, HC03, pH and Co3 shall be performed on samples collected in May of each year. The permittee shall maintain withdrawal records showing daily withdrawals of raw (pre-treatment) water for each year ending May 31. These records shall be submitted on a quarterly basis on District Form En-3. Nothing in this permit shall be construed to limit the authority of the St. Johns River Water management District to declare a water shortage and issue orders pursuant to Section 373.175, Florida Statutes, or formulate a plan for implementation during periods of water shortage pursuant to Section 373.246, Florida Statutes. District representatives may visit the site to insure compliance with conditions of this permit following advance notifica- tion of the permittee of the time of visit. The water conserving techniques and methods as outlined in the July 30, 1981 letter to the District from Ed Fleis, P.E., to Thomas K. Ziegler, TSR Exhibit 10, shall be implemented and included throughout all phases of this project. Further, should the replace- ment of any fixtures or appliances be required during the life of this permit, water conserving fixtures equivalent to those originally specified shall be installed. DONE AND ORDERED this 6th day of August, 1982, in Tallahassee, Florida. SHARYN L. SMITH Hearing Officer Division of Administrative Hearings Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 6th day of August, 1982.

Florida Laws (5) 120.57373.019373.175373.223373.246
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WASHINGTON COUNTY vs BAY COUNTY AND NORTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 10-002983 (2010)
Division of Administrative Hearings, Florida Filed:Tallahassee, Florida May 28, 2010 Number: 10-002983 Latest Update: Jan. 22, 2013

The Issue Whether Bay County has demonstrated its entitlement to the Permit?

Findings Of Fact The Ecologically Diverse Florida Panhandle With its high diversity of species and richness in endemic plants, the Florida Panhandle has been identified as one of six continental "biodiversity hot spots" north of Mexico. It has more species of frogs and snakes, for example, than any other equivalently-sized area in the United States and Canada and has botanical species that do not exist anywhere else in the Coastal Plain, one of the three floristic provinces of the North Atlantic American Region. The biodiversity stems from a number of factors. The Panhandle was not glaciated during the Pleistocene Period. Several major river systems that originate in the southern Appalachian Mountains terminate on the Panhandle's Gulf Coast. Its temperate climate includes relatively high rainfall. These factors promote or produce plentiful sources of surface and groundwater that encourage botanical and zoological life and, in turn, a diverse ecology. When compared to the rest of Florida, the Panhandle is relatively free from man-made impacts to its water resources. Until recently, the population growth rate lagged behind much of the state. Despite a rapid increase in the population in the late 1990s into the early part of the twenty-first century, it remains much less densely populated than areas in the I-4 Corridor and coastal peninsular Florida to the south. The Panhandle can be divided into physiographic areas of geological variation that are highly endemic; a substantial number of plant and animal species found in these areas are found nowhere else in the world. One of these areas is of central concern to this case. Located in southern Washington County and northern Bay County, it is known as the Sand Hill Lakes Area. The Sand Hill Lakes Area The Sand Hill Lakes Area (the "Area") is characterized by unusual geology that produces extraordinary ecological value. With few exceptions (see findings related to Dr. Keppner's flora and fauna inventories on the NTC/Knight Property below), the Area has not been extensively studied. The data on biological communities and water levels that exist, sparse as it is, has been obtained from historic aerials dating to 1941. The aerials are of some use in analyzing lakes and surface waters whose source is the Surficial Aquifer, but they are of limited value otherwise. They are not of use in determining the level in the Surficial Aquifer. Nor are they of assistance in determining river height when the banks of the river are covered by hardwood forest canopy. The resolution of the aerials is insufficient to show details of the various ecosystems. They do not show pitcher plants, for example, that exist at the site of hillside seepage bogs common in the Area. An aspect of the Area that the aerials do reveal is its many karst features on the surface of the land. Karst lakes and sinkholes dominate the Area and are a component of its highly unusual geology which is part of a larger system: the Dougherty Karst Plain. The Dougherty Karst Plain is characterized by numerous karst features: springs, caverns, sinkhole lakes, and sinkholes. Sinkholes In Florida, there are three types of sinkholes: cover subsidence, cover collapse, and "rock" or "cavern" collapse. Of the three, cover subsidence sinkholes are the most common in the state. Cover subsidence sinkholes form as the result of processes that occur on the surface. A cover subsidence sinkhole is usually a shallow pan typically not more than a few feet deep. Found throughout Central and South Florida, they are the most common type of sinkholes in most of peninsular Florida. In contrast, the other two major types of sinkholes (cover collapse and cavern collapse) occur as the result of processes below the surface that cause collapse of surface materials into the substrata. Both types of "collapse" sinkholes are found in the Area, but cover collapse is the more common. Cavern collapse sinkholes are relatively rare. Typical of the Area, cover subsidence sinkholes are not found on the NTC/Knight Property. The NTC/Knight Property The majority of the NTC/Knight Property is in Washington County, but the property straddles the county line so that a smaller part of it is in northern Bay County. All of the NTC/Knight Property is within the Area. The District recognizes that the NTC/Knight Property contains natural resources of extraordinary quality as does the Area generally. Over the three years that preceded the hearing, Dr. Keppner, an NTC/Knight expert, conducted extensive inventories of the flora and fauna on NTC/Knight Property. Dr. Keppner's inventory showed the NTC/Knight Property supports more than 500 species of vascular plants (flora with a system of tubes within the stem, phloem, and the xylem that exchange materials between the roots and leaves) and 300 species of animals. Among them are at least 28 vascular plants and six animals listed as imperiled (threatened or endangered) by state or federal agencies. At least 22 of the imperiled species of vascular plants and eight of the imperiled species of animals are located within an area expected to be affected by the Wellfield for which Bay County seeks the permit modification. For example, at Big Blue Lake alone where impacts were predicted by NTC/Knight experts to take place, the following imperiled plant species are found: Smoothbark, St. John's Wort, Kral's Yelloweyed Grass, Quilwort Yelloweyed Grass, Threadleaf Sundew, Panhandle Meadowbeauty, and Crystal Lake Nailwort. In addition to the Keppner inventory, NTC/Knight commissioned other studies to determine the nature of the sinkholes and whether they are connected to the Floridan Aquifer. NTC/Knight's experts determined that the property contains cover collapse and a few cavern collapse sinkholes that connect to the Floridan Aquifer. Despite evidence to the contrary submitted by the District and Bay County, the NTC/Knight determinations are accepted as facts for a number of reasons, including the lineup of the sinkholes and sinkhole lakes along identified photo-lineaments and the distribution of them in patterns that are not random. A District study using a dye test, moreover, confirmed conduit flow exists in the Area just east of the NTC/Knight Property. With regard to the distribution of the sinkholes and sinkhole lakes on the NTC/Knight Property, Dr. Sam Upchurch used the term "String of Pearls" to describe multiple sinkholes that exist along the edges of several lakes on the property. When sinkholes closer to the center of a lake are clogged or plugged with sediment and debris, the lakes continue to leak around the plugs which causes new sinkholes to form along the edge of the plugs. Examples of the "String of Pearls" formation on the edges of existing lakes are found at White Western and Big Blue Lakes on the NTC/Knight Property and at Crystal Lake nearby in Washington County. The multiple sinkholes bordering the edge of Big Blue Lake are examples of cover collapse sinkholes that, in geological terms, are relatively young as evidenced by their steep sides. In a karst area such as the Area, there is preferential flow in the conduits because of the difference of efficiency of transmission of water flowing through a porous medium of rock compared to that flowing though a conduit. Absent pumping in the Wellfield, the underlying aquifers are relatively stable. If the requested pumping does not take place, it is likely the stability will remain for a substantial period of time. It is not known with precision what will happen in the long term to the karst environment should pumping occur at the Wellfield at the rate the District proposes. When pumping occurs, however, water in the Area affected by the Wellfield will move toward the Wellfield. "[A]s it does[,] you may get some turbulent flow or vorticity in the water." Tr. 1391, (emphasis supplied). At some point, a change in the potentiometric surface and loss of buoyancy will most likely occur. This leads to concerns for Dr. Upchurch from two perspectives: One . . . is that if there is a[n affected] sinkhole lake [on the surface,] it may induce downward flow . . . the other . . . is that if it breaks the plug it may either create a new sinkhole or create a substantial drop in the level of water in the lake . . . which drains periodically, not necessarily because of a wellfield, but because that plug breaks. Id. In the first instance, lake levels could be reduced significantly. In the second, a new sinkhole could be created or the water level could drop dramatically as occurred at Lake Jackson in Tallahassee. Sand Hill Lakes Wetlands The Area contains a number of wetland communities. These include hillside seepage bogs, steepheads, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and creeks and streams in forested wetlands. A number of these wetlands occur on the NTC/Knight Property within the zone of influence in the Surficial Aquifer predicted by NTC/Knight's experts employing a model known as the "HGL Model." The wetland systems on the NTC/Knight Property are diverse, by type, plant species composition, and richness. This remarkable diversity led the District to recognize that the NTC/Knight Property contains lakes of nearly pristine quality, interconnected karst features, and endemic steephead ravines, all of which are regionally significant resources of extraordinary quality. The Area's wetlands also include many streams, among them Pine Log Creek, the majority of which is located on the NTC/Knight Property. Significant recharge to the Floridan Aquifer occurs on NTC/Knight Property. To the west, north, and east of the NTC/Knight Property are major concentrations of Floridan Aquifer springs that are crucial to the quality and character of regional surface water systems, including the Choctawhatchee River, Holmes Creek, and Econfina Creek systems. All of these surficial systems are dependent on the groundwater resources of the Area. The Area's Hillside Seepage Bogs Hillside seepage bogs are marsh-like wetland usually located on gentle slopes of the sides of valleys. They form when the Surficial Aquifer intercepts the sloping landscape allowing water to seep onto the sloped surface. The plant communities in the bogs are dominated by a great number and variety of herbaceous plants that prefer full sun. Among them are carnivorous plants. These unusual plants include the Trumpet and White-Topped pitcher plants as well as other varieties of pitcher plants. Inundation or saturation for extended periods of time is necessary for pitcher plants and most of the rest of the plant communities found in the bogs to thrive and to fend off invasion by undesirable species. Hillside seepage bogs are valued because they are among the most species-rich communities in the world. A reduction in water levels in the bogs below the root zone of associated plants will kill the plant communities that live in them and pose a threat to the continued existence of the bogs. Hillside seepage bogs were once abundant in pre- settlement Florida, but their expanse has been greatly reduced. They are now estimated to only occupy between one and five percent of their original range. On NTC/Knight Property, they have been spared to a significant degree. Numerous hillside seepage bogs continue to exist on the NTC/Knight Property primarily along the margin of Botheration Creek and its tributaries. The Area's Steepheads Steepheads are unique wetland systems. Found around the globe, they are usually regarded as a rarity. More than 50 percent of the steepheads that exist in the world are in a narrow latitudinal band that extends from Santa Rosa County in the west to Leon County in the east, a major section of the Florida Panhandle. Steepheads occur in deep sandy soils where water originating in the Surficial Aquifer carries away sand and cuts into sandy soils. The seepage emerges as a "headwater" to create a stream that conveys the water from the steephead into a river, or in some rare circumstances, into a karst lake. Over time, flow of the seepage waters results in deep, amphitheater- shaped ravines with steep valley side walls. Steepheads are important to the ecologies of the areas in which they occur. They provide habitat for a number of Florida endemic animals and plants believed to be relics of once-abundant species. Water that emerges from a steephead is perennial. Because the steep slopes of the steephead have not been disturbed over a long period of time, the water remains at a relatively constant temperature, no matter the season. Sampling of aquatic invertebrates at the Russ Pond and Tiller Mill Steepheads on the NTC/Knight Property found 41 and 33 distinct taxa, respectively, to inhabit the steepheads. Among them were a number of long-lived taxa. Their presence is consistent with the hallmark of a steephead: perennial flow of water at a relatively constant temperature. Most of the known steepheads flow into streams or rivers. Between six and ten within the Area, however, flow into Sand Hill Lakes. They have no direct connection to any surface drainage basin, thereby adding to their uniqueness. The level in the Surficial Aquifer has a direct impact on where and to what extent seepage flows from the sidewalls of a steephead. The Area's Sphagnum Bogs Sphagnum moss grows in many locations within the landscape and requires moisture. Where there is a large amount of sphagnum moss, it can form a unique community known as a sphagnum bog that is capable of supporting unique plant and animal populations. In the Area, these sphagnum bogs form along the valley sidewalls of steephead ravines and are fed by Surficial Aquifer seepage from the sidewall of the ravine. These sphagnum bogs support unique plant and animal communities, including a salamander discovered by Dr. Means that is new to science and so far only known to exist in sphagnum bogs in the Florida Panhandle. The Area's Sinkhole Lakes and their Littoral Seepage Slopes Sand Hill Lakes are nutrient poor, or "oligotrophic," receiving most of their nutrient inputs through exchange with the plant and animal communities on the adjacent littoral shelves during periods of high water levels. Fluctuating water levels in the Sand Hill Lakes allow a littoral zone with many different micro-habitats. Areas closest to the lakes are inundated regularly, but higher areas of the littoral zone are generally dry and inundated only every ten or 20 years -- just often enough to prevent encroachment of trees. In a few instances, portions of the littoral zones are inundated by seepage from the Surficial Aquifer. Above the normal low water of the Sand Hill Lakes, the littoral shelf occurs along a low gradient. As the littoral shelf transitions into the lake bottom and toward the deeper parts of the lake, there is an inflection point, where the gradient of the lake bottom becomes much steeper than the littoral shelf. If lake water levels fall below that natural inflection point, gully erosion will occur. The flow of water will be changed along the littoral shelf from seepage sheet flow over a wide expanse to water flowing down gullies in a concentrated stream. This change in flow will result in a loss of area needed by certain seepage dependent plants and animals as well as increased sedimentation from erosion. Big Blue Lake is unique because it boasts the largest known littoral zone seepage area of any Sand Hill Lake. The seepage zone along Big Blue Lake supports a number of rare plant species, including the Thread-Leaf Sundew, Smoothed Barked St. Johns Wort, and Crystal Lake Nailwort. The Area's Temporary Ponds Temporary ponds are small isolated water bodies that generally have no surface water inlet or outlet. Typically very shallow, they are sometimes wet and sometimes dry. Temporary ponds can range from basins that have continuous water for three to five years, to basins that have standing water for a month or two, every two to four years. These conditions limit their occupation by fish and, therefore, provide ideal conditions for amphibian reproduction which only occurs when water levels are maintained long enough to complete a reproductive cycle. In the Area, temporary ponds are a direct expression of the Surficial Aquifer and contain no known restrictive layer that might cause water to be "perched" above the Surficial Aquifer. Temporary ponds are critical to the viability of amphibian populations and support high amphibian biodiversity. A given pond can contain between five and eight species of salamander, and between 12 and 15 species of frogs. There has been a decline recently in the population of frogs and other amphibians that depend upon temporary ponds. The decline is due in part to ditching and other anthropogenic activities that have altered the hydrology of temporary ponds. Temporary ponds have a higher likelihood of being harmed by a drawdown than larger, connected wetlands systems. Lowered Surficial Aquifer water levels would lower water levels in temporary ponds and, thereby, threaten amphibian reproduction. Creeks/Streams in Forested Wetlands Streams are classified on the basis of the consistency of flowing water, including perennial (always flowing), intermittent (flowing part of the year), and ephemeral (flowing only occasionally during rain events). The type of stream flow is important because movement of water is essential to support aquatic systems in stream habitats. The NTC/Knight Property includes a number of stream systems, including Botheration Creek and Pine Log Creek. Botheration Creek is fed by groundwater discharge and originates, in large part, on the NTC/Knight Property. Botheration Creek flows from east to west until it intersects Pine Log Creek on the southwest part of the NTC/Knight Property. Botheration Creek provides Pine Log Creek with approximately 89 percent of Pine Log Creek's flow. From the confluence, Pine Log Creek flows south and west into the Pine Log State Forest and eventually joins the Choctawhatchee River. Botheration Creek contains high quality water and a diverse mix of aquatic invertebrates and fish. Sampling at a stage recorder located approximately two miles west of the eastern boundary of the NTC/Knight Property ("BCS-01") identified 46 taxa of macroinvertebrates, including six long- lived taxa, and mussels. The water level in Botheration Creek at BCS-01 was measured to be between 0.1 and 0.32 feet by four measurements taken from October 2010 to July 2011. Nonetheless, the presence of long-lived taxa and mussels indicates that, at BCS-01, Botheration Creek is a perennial stream. Carbon export from streams provides nutrients that feed the stream system. Headwater streams like Botheration Creek and its tributaries are essential to carbon export. For carbon export to occur, a stream must have out-of-bank flood events regularly to promote nutrient exchange with the flood plain. Bay County and its Water Supply Prior to 1961, the County obtained its public water supply from wellfields located near downtown Panama City. The wellfields drew from the Floridan Aquifer. An assessment of the pre-1961 groundwater pumping appears in a District Water Supply Assessment released in June 1998. In summary, it found that near Panama City, the potentiometric surface was substantially depressed by the pumping. Due to the threat of saltwater intrusion, the Deer Point Lake Reservoir (the "Reservoir") was constructed as an alternate water supply. A local paper mill, the city of Panama City, and Tyndall Air Force Base, all began to obtain public supply water from the Reservoir. Six years after the construction of the Reservoir, the Floridan Aquifer's water levels had rebounded to pre-pumping levels. See NTC/Knight Ex. 93 at 69. The authorization for the Reservoir began in the 1950's when the Florida Legislature passed a series of laws that granted Bay County authority to create a saltwater barrier dam in North Bay, an arm of the St. Andrews Bay saltwater estuary. The laws also allowed Panama City to develop and operate a surface freshwater reservoir to supply water for public use. The Deer Point Lake Dam (the "Dam") was built in 1961 from metal sheet piling installed across a portion of North Bay. The Dam created the Reservoir. The watershed of the Reservoir includes portions of Jackson, Calhoun, Washington, and Bay Counties and covers approximately 438 square miles. The Reservoir receives freshwater inflow from several tributaries, including Econfina Creek, Big Cedar Creek, Bear Creek/Little Bear Creek, and Bayou George Creek, totaling about 900 cubic feet per second ("cfs") or approximately 582 MGD. The volume of inflow would increase substantially, at least two-fold, during a 100-year storm event. The Dam is made of concrete and steel. Above it is a bridge and two-lane county road roughly 11.5 feet above sea level. The bridge is tied to the Dam by pylons. The top of the Dam is 4.5 feet above sea level, leaving a distance between the Dam and the bridge bottom of about seven feet. There is an additional structure above the Dam that contains gates, which swing open from the force of water on the Reservoir's side of the Dam. Capable of releasing approximately 550 MGD of freshwater into the saltwater bay, the gates keep the level of the Reservoir at about five feet above sea level. The height of the Dam and the gate structure leaves a gap between the bottom of the bridge deck and the top of the structure of "somewhere between 12 and 14 inches, a little better than a foot." Tr. 140. If storm surge from the Gulf of Mexico and St. Andrew's Bay were to top the Dam and the gate structure, the gap would allow saltwater to enter the Reservoir. The gates and the Dam structure are not designed to address storm surge. The Dam is approximately four feet thick and roughly 1,450 feet long. The 12-to-14 inch gap extends across the length of the Dam. With normal reservoir levels, the volume of water it contains is approximately 32,000-acre-feet or roughly 10.4 billion gallons. Bay County needs to drawdown the lake level for fish and wildlife purposes, the control of aquatic growth, and weed control. In winter, FWS prescribes a 45-day period of time to draw down the lake to expose the banks to kill vegetation. The last time the lake was drawn down by the County, the water level dropped approximately three feet, from five feet above sea level to two feet above sea level. This process took approximately six days and 16 hours, or approximately 53 hours/foot. Repair of the Dam and its Maintenance The Dam has been repaired three times. The last repair was following Hurricane Opal which hit the Florida Panhandle in the fall of 1995. During Hurricane Opal, "saltwater . . . entered . . . the [R]eservoir . . . [t]hat took 20-some days to flush out . . . ." Tr. 135. No evidence was presented regarding the Dam's vulnerability from the perspective of structural integrity during normal or emergency conditions. Other than the inference drawn from Mr. Lackemacher's testimony that Hurricane Opal damaged the Dam in 1995, no evidence was presented to suggest that the Dam's structure is vulnerable to damage caused by a storm surge, wave effect or other conditions caused by a storm of any magnitude. After the last of the three repairs, Bay County implemented a detailed maintenance program. Based upon the latest inspection reports, the Dam is in good condition and structurally sound. No work other than routine inspection and maintenance is currently planned. The 1991 Agreement and the WTP Bay County's current withdrawal of water from the Reservoir is based on a 1991 agreement between Bay County and the District (the "1991 Agreement"). See Joint Ex. Vol. II, Tab K. The 1991 Agreement allows Bay County after the year 2010 to withdraw 98 MGD (annual average) with a maximum daily withdrawal of 107 MGD. The 1991 Agreement, still in effect, authorizes Bay County to withdraw enough water from the Reservoir to meet its needs through 2040. Water for public supply is withdrawn from the Reservoir by a water utility pump station (the "Pump Station") located a short distance from the Dam in Williams Bayou. The water is piped to the water utility's treatment plant (the "Water Treatment Plant") five miles away. The Water Treatment Plant treats 60 MGD. Following treatment, the water is distributed to Bay County's wholesale and retail customers. The Reservoir water available to Bay County utilities is more than adequate to fulfill the water consumption demands of Bay County's system through a 20-year permit horizon. The transmission line between the Pump Station and the Water Treatment Plant has fittings that were designed to allow transmission of groundwater withdrawn from groundwater wells to be located along the transmission line to the Water Treatment Plant to provide a backup supply for the Reservoir. Bay County's Current Use of Potable Water The amount of water consumed by Bay County utility customers has declined over the last five years. Bay County's current use of water, based upon the average of the 13 months prior to the hearing, was 24.5 MGD, an amount that is only 25 percent of the water allocation authorized by the 1991 Agreement. There are approximately 560,000 linear feet of main transmission lines in Bay County with small service lines accounting for another several hundred thousand linear feet. Bay County furnishes water directly to approximately 6,000 retail customers in areas known as North Bay, Bay County, and the former Cedar Grove area, which is now part of Bay County. Wholesale customers include Panama City Beach, Panama City, Mexico Beach, Callaway, Parker, Springfield, and parts of Lynn Haven. The County also furnishes potable water to Tyndall Air Force Base. Lynn Haven does have some water supply wells; however, Bay County still supplements this water supply by approximately 30 percent. No other cities serviced by Bay County produce their own water. Bay County has a population of approximately 165,000- 170,000 permanent residents, which includes residents of the cities. The Bay County area experiences seasonal tourism. From spring break to July 4th, the population can grow to more than 300,000. The users of Bay County's drinking water supplies include hospitals, Tyndall Air Force Base, and the Naval Support Activity of Panama City ("NSA"). The County has 178 doctor's offices, 56 dental offices, 29 schools, 21 fire departments, 12 walk-in-clinics, six nursing and rehabilitation homes, six major employers, three colleges and universities, and two major hospitals, all which are provided drinking water by Bay County. Panama City Beach is the community which has the highest water use. Panama City Beach's average daily use is approximately 12 MGD. The peak day of usage for all of Bay County's customers over the 13 months prior to the hearing was 40 MGD. Bay County sells water to community water utility systems referred to as a "consecutive system." They include Panama City Beach, Panama City, and Mexico Beach. Bay County's request for 30 MGD contemplates provision of water for all essential and non-essential water uses occurring within the consecutive system. Bay County and the consecutive systems are subject to the District's regulations regarding emergency water use restrictions which typically restrict the non-essential use of water during water shortage emergencies. Hurricanes, Train Wrecks, and Post-9/11 America At the District's recommendation, Bay County has been considering a backup potable water source since the mid-1980's. Bay County's main concern is that it has inadequate alternatives to the Reservoir should it be contaminated. Contamination to date has been minimal. In the period of time after the 1961 creation of the Reservoir to the present, the Dam and the Reservoir have suffered no major damage or impacts from a tropical storm. No tropical storm since 1961 has disrupted Bay County's ability to provide potable water. Even Hurricane Opal in 1995 did not disrupt the water supply. Recent hurricane activity in the Gulf of Mexico, however, has aroused the County's fears. Should a storm of sufficient magnitude make landfall in proximity to the Dam, there is potential for saltwater contamination of the Reservoir from storm surge or loss of impounded freshwater due to damage to the Dam. Mr. Lackemacher, assistant director of the Bay County Utility Department and manager of the water and wastewater divisions of the department, has experience with other hurricanes in Palm Beach, Florida, and Hurricane Hugo in Myrtle Beach, South Carolina, during which water utilities suffered disruption of their distribution systems. The experience bolsters his concern about the damage a storm could cause Bay County's source of public water supply. Bay County's intake structure at Williams Bayou is approximately one mile away from the Dam. The location of the Pump Station puts it at risk for damage from a strong storm or hurricane. There is a rail line near the Reservoir. It runs along Highway 231 and over creeks that flow into the Reservoir, including the Econfina Creek. The rail line is known as "Bayline." Bayline's most frequent customers are the paper mill and the Port of Panama City. Not a passenger line, Bayline is used for the transport of industrial and chemical supplies. In 1978, a train derailment occurred on tracks adjacent to creeks that feed the Reservoir. The derailment led to a chlorine gas leak into the atmosphere. There was no proof offered at hearing of contamination of the Reservoir. There has never been a spill that resulted in a hazardous chemical or pollutant being introduced into the Reservoir. Bay County has not imposed restrictions on the type of vehicles that are allowed to use, or the material that may pass over, the county road on the bridge above the Dam. Nonetheless, in addition to saltwater contamination, Bay County also bases the need for an alternative water source on the possibility of a discharge into the Reservoir of toxic substances from a future train derailment. Bay County is also concerned about contamination of the Reservoir from a terrorist attack. In short, Bay County is concerned about "anything that could affect the water quality and water in Deer Point Lake." Tr. 184. The concerns led Bay County to file its application for the Wellfield on lands currently owned by the St. Joe Company. Consisting of ten wells spaced over an area of approximately ten square miles, the Wellfield would have a capacity of 30 MGD. Bay County's application was preceded by the development of the District's Region III Regional Water Supply Plan and efforts to acquire funding. Funding for the Wellfield and the Region III Regional Water Supply Plan Shortly after the commencement of the planning for the Wellfield, the District, in May 2007, authorized the use of funds from the State's Water Protection and Sustainability Trust Fund ("WPSTF"). The WPSTF is intended for development of alternative water supplies. In cooperation with the District, Bay County began drilling a test well followed by analyses to evaluate the water for potable suitability. In October of the same year, the District passed a resolution to request the Department of Environmental Protection to release $500,000 from the WPSTF to the District for local utilities in Bay and Escambia Counties for "Water Resource Development." NTC/Knight Ex. 195, p. 2. The amount was to be used "to provide funding for implementation of alternative water supply development and water resource developments projects pursuant to sections 403.890 and 373.1961, F.S." Id., p. 1. In February 2008, the District began a process to develop a regional water supply plan for Bay County. If the Wellfield were designated in the applicable regional water supply plan as "nontraditional for a water supply planning region," then it would meet the definition of "alternative water supplies" found in section 373.019(1), Florida Statutes. "In evaluating an application for consumptive use of water which proposes the use of an alternative water supply project as described in the regional water supply plan," the District is mandated "to presume that the alternative water supply is consistent with the public interest " § 373.223(5). Whether the Wellfield is to be presumed to be in the public interest depends on whether the application proposes the use of an alternative water supply project as described in the District's Region III Water (Bay County) Water Supply Plan adopted in 2008. The 2008 RWSP Pursuant to the process commenced in February, the District in August 2008 produced the Region III (Bay County) Regional Water Supply Plan (the "2008 RWSP"). In a section entitled "Identification of Alternative Water Supply Development Projects," the 2008 RWSP provides the following: "All of the water supply development projects identified in Table 4 are interrelated and considered alternative, nontraditional water supply development projects." NTC/Knight Ex. 187 at 14. Table 4 of the 2008 RWSP does not specifically identify the Wellfield. It identifies three projects in general terms. The first of the three (the only one that arguably covers the Wellfield) shows "Bay County Utilities" as the sole entity under the heading "Responsible Entities." Id. at 13. The project is: "Inland Ground Water Source Development and Water Supply Source Protection." Id. Under the heading, "Purpose/Objective," the Table states for the first project, "Develop inland alternative water supply sources to meet future demands and abate risks of salt water intrusion and extreme drought." Id. The Table shows "Estimated Quantity (MGD)" to be "10.0." Id. (In July 2008, the District's executive director informed Bay County that the Wellfield could produce 10 MGD.) The "Time Frame" is listed as 2008-12, and the "Estimated Funding" is "$5,200,000 WPSPTF" and "$7,800,000 Local, NWFWMD." Id. While not specifically identified in the 2008 RWSP, Table 4's project description supports a finding that the Wellfield is, in fact, one of the inland alternative water supply sources. The 2008 RWSP, therefore, designates the Wellfield as a "nontraditional" water supply source for Region III.4/ (The Wellfield also, therefore, meets the definition of "[a]lternative water supplies" in section 373.019(1). The demonstration of a prima facie case by Bay County and the District, however, make the applicability of the presumption a moot point. See Conclusions of Law, below.) Water Supply Assessments and Re-evaluations Development of a regional water supply plan by the governing board of each water management district is mandated "where [the governing board] determines that existing and reasonably anticipated sources of water are not adequate to supply water for all existing and future reasonable-beneficial uses and to sustain the water resources and related natural systems for the planning period." § 373.709(1), Fla. Stat. (the "Regional Water Supply Planning Statute"). The District determined in its 1998 District Water Supply Assessment ("WSA") for Region III (Bay County) that the existing and reasonably anticipated water sources are adequate to meet the requirements of existing legal users and reasonably anticipated future water supply needs of the region through the year 2020, while sustaining the water resource and related natural systems. See NTC/Knight 93 at 79. In 2003, Ron Bartel, the director of the District's Resource Management Division, issued a memorandum to the Governing Board (the "2003 Re-evaluation Memorandum"), the subject of which is "Regional Water Supply Planning Re- evaluation." NTC/Knight 95 (page stamped 42). The 2003 Re-evaluation Memorandum sets out the following with regard to when a "water supply plan" is needed: The primary test we have used for making a determination that a water supply plan was "not needed" for each region is that projected consumptive use demands for water from major water users do not exceed water available from traditional sources without having adverse impacts on water resources and related natural systems. Similarly, regional water supply planning is initiated "where it is determined that sources of water are not adequate for the planning period (20) years to supply water for all existing and reasonable-beneficial uses and to sustain the water resources and related natural systems." Id. With regard to the need for a Water Supply Plan for Bay County the 2003 Re-evaluation Memorandum states: [I]n Bay County (Region III), sufficient quantities have been allocated for surface water withdrawal from Deer Point Lake Reservoir through the District's consumptive use permitting program extending through the year 2040. In this area, the District is also scheduled to complete a minimum flow and level determination for the lake by the year 2006. This determination will be useful for deciding if additional water supply planning is needed before the permit expires in 2040. Id. (page stamped 43). The 2008 RWSP's designation of the Wellfield is justified in the minutes of the Governing Board meeting at which the 2008 RWSP's approval took place: While the reservoir has largely replaced the use of coastal public supply wells historically impacted by saltwater intrusion, there remain challenges within the region that make development and implementation of a Regional Water Supply Plan (RWSP) appropriate. Development of alternative water supplies would diversify public supply sources and help drought-proof the region through establishment of facility interconnections. Development of alternative supplies would also minimize vulnerability associated with salt water potentially flowing into the reservoir during major hurricane events. Id., p. 3 of 4. The adoption of the 2008 RWSP was followed in December 2008 by the District's 2008 Water Supply Assessment Update. The update is consistent with the earlier determinations of the adequacy of the Reservoir as a water supply source for the foreseeable future (in the case of the update, through 2030). The update also voices the concern about water quality impacts from storm surge. The update concludes with the following: In Region III, the existing and reasonably anticipated surface water resources are adequate to meet the requirements of existing and reasonably anticipated future average demands and demands for a 1-in-10 year drought through 2030, while sustaining water resources and related natural systems. However, the major concern for potential water quality impacts is that resulting from hurricane storm surge. A Regional Water Supply Plan (NWFWMD 2008) has recently been prepared for Region III to address concerns associated with existing surface water systems. NTC/Knight Ex. 101, p. 3-41. The Parties Washington County is a political subdivision of the State of Florida. Washington County is located directly north of Bay County and the Wellfield and within one mile of some of the proposed wells. Washington County includes thousands of wetlands and open water systems. Because of the hydro-geologic system in the area of the Wellfield, if there are wetland, Surficial Aquifer, and surface water impacts from the withdrawal under the Permit, it is likely that impacts will occur in Washington County. Washington County has a substantial interest in protection, preservation, and conservation of its natural resources, including lakes, springs, and wetlands, and the flora and fauna that depend on these water resources, especially endangered flora and fauna. Washington County has a substantial interest in the protection of all water resources in Washington County because of the close relationship between surface waters, groundwater, and the potable water supply used by Washington County residents. NTC/Knight is the owner of approximately 55,000 acres of land located in northern Bay County and southern Washington County. The NTC/Knight Property includes thousands of acres of wetlands and open waters, including Sand Hill Lakes, steepheads, hillside seepage bogs, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and forested wetlands. A large portion of the NTC/Knight Property is directly adjacent to the Wellfield and within the HGL Model projected drawdown contour. Based on the projected amount of drawdown from pumping at the proposed average rate of 5 MGD, the 0.5 projected drawdown contour predicted by the HGL Modeling Report (see Finding of Fact 121, below) extends over thousands of acres of the property. NTC/Knight has a substantial interest in the protection of the surface and groundwater directly on, under, and adjacent to its property. The water supports the numerous ecosystems of extraordinary value located on the property. James Murfee and Lee Lapensohn are individuals, who reside in Bay County on property fronting on and beneath Tank Pond approximately five miles from the Wellfield. Petitioners Murfee and Lapensohn have a well which extends into the Intermediate Aquifer. The Murfee and Lapensohn properties are within the HGL Model projected drawdown contour. Petitioners Murfee and Lapensohn have a substantial interest in the protection of their drinking water supply well and the surface waters directly on and adjacent to their properties. Bay County, the applicant, is a political subdivision of the State of Florida. The District is a water management district created by section 373.069(1). It has the responsibility to conserve, protect, manage, and control the water resources within its geographic boundaries. See § 373.069(2)(a), Fla. Stat. Section 120.569(2)(p), Florida Statutes Section 120.569(2)(p), in pertinent part, provides: For any proceeding arising under chapter 373, chapter 378, or chapter 403, if a nonapplicant petitions as a third party to challenge an agency’s issuance of a license, permit, or conceptual approval, the order of presentation in the proceeding is for the permit applicant to present a prima facie case demonstrating entitlement to the license, permit, or conceptual approval, followed by the agency. This demonstration may be made by entering into evidence the application and relevant material submitted to the agency in support of the application, and the agency’s staff report or notice of intent to approve the permit, license, or conceptual approval. Subsequent to the presentation of the applicant’s prima facie case and any direct evidence submitted by the agency, the petitioner initiating the action challenging the issuance of the license, permit, or conceptual approval has the burden of ultimate persuasion and has the burden of going forward to prove the case in opposition to the license, permit, or conceptual approval through the presentation of competent and substantial evidence. The permit applicant and agency may on rebuttal present any evidence relevant to demonstrating that the application meets the conditions for issuance. Paragraph (p) was added to section 120.569(2) in the 2011 Session of the Florida Legislature. Accordingly, the final hearing commenced with the Bay County and the District's presentation of its prima facie case by submitting the application, supporting documentation, and the District's approval of the application. Respondents also presented the testimony of four witnesses in the hearing's first phase. Phase I of the Final Hearing: Bay County's Application, Supporting Documents, the District's Approval and Supporting Testimony The Application File At the final hearing, Bay County and the District offered the "application file," marked as Joint Exhibit Binder Volumes I-IV (the "Application File") in the hearing's first phase. It was admitted into evidence. A document entitled "Alternate Water Supply Report - Bay County Water Division" dated May 20, 2008 (the "Hatch Mott MacDonald Report") is contained in the Application File. See Joint Ex. Vol. I, Tab B. The Hatch Mott MacDonald Report is a preliminary evaluation of a wellfield with 22 wells, an "initial phase . . . [of] five (5) wells producing 5 MGD and the final phase . . . [of] 17 wells, producing 25 MGD." Id. at 1. The evaluation includes the gathering of information, a recommendation for the best method of treatment, an analysis of whether individual well sites or a centralized site would be superior, a hydraulic model and analysis, and the potential construction and operation costs. The report concludes in its Executive Summary: HMM's preliminary results, based upon water analysis of Well No. 1, indicate that only disinfection will be required for potable water treatment. Additionally, the hydraulic analysis indicated that the wells are capable of providing the initial 5 MGD and future 25 MGD to the proposed connection point along Highway 388 without re-pumping. Adequate storage for fire protection should be considered at current and future service areas. The use of chlorine gas at each well site during the initial phase had the lowest present worth of $16,770,270; that is, the smallest amount of funds needed today to build, operate, and maintain the system. The use of chlorine gas at each well in the final phase had a present worth of $41,245,118, only slightly more than the present worth of $40,834,245 for on-site Id. generation of disinfectant at three (3) central facilities. The Application File contains a response to a District request for additional information (the "2009 RAI Response") submitted by the Bay County Services Utility Director and received by the District in September 2009. See Joint Ex. Vol. II, Tab K. The 2009 RAI Response contains the 1991 Agreement and numerous other documents. Among them is a report prepared by HydroGeoLogic, Inc. ("HGL") entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" dated September 2009 (the "2009 HGL Modeling Report"). The report predicts impacts that would be created to the surrounding aquifers as a result of the Wellfield pumping, but recommends that additional data be obtained. The Application File contains the District's Notice dated March 25, 2010. See Joint Ex. Vol. III, Tab B. Attached to the Notice is a draft of the Permit and a staff report from the District recommending approval with conditions. Condition 11 of the Permit's standard conditions obligates Bay County to mitigate any significant adverse impacts caused by withdrawals and reserves the right to the District to curtail permitted withdrawal rates "if the withdrawal causes significant adverse impact on the resource and legal uses of water, or adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. III, Tab B, p. 3 of 17. Attachment A to the Permit requires conditions in addition to the standard conditions contained in the body of the Permit. Paragraph 12 of Attachment A, for example, requires that Bay County implement and maintain a water and conservation efficiency program with a number of goals. Attachment B to the Permit requires a monitoring and evaluation program and wetland monitoring of adjacent properties to determine if the pumping causes adverse impacts to wetland areas, including habitat and species utilization. The Application File contains a revised modeling report also entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" (the "2011 Revised HGL Modeling Report" or the "HGL Model Report"). See Joint Ex. Vol. III, Tab P. The 2011 Revised HGL Modeling Report predicts impacts of the pumping of the Wellfield on the Upper Floridan Aquifer and the Surficial Aquifer. The HGL Model is based on an adaptation of an original model first developed by the U.S. Geological Survey (USGS) and then further adapted by HGL. The adapted model is known as MODFLOW-SURFACT. The MODFLOW-SURFACT Model has been used in excess of 600 applications and is used worldwide. The HGL Model predicted impact from pumping when wellfield pumping achieves a "steady state." Steady state impact is achieved after 10-12 years of constant pumping. The impact and the area of impact is depicted on Figure 5.1b(1) of the 2011 Revised HGL Modeling Report. The predicted drawdown of the Surficial Aquifer is predicted to be six inches (0.5 ft) within the areas indicated. The Application File shows that the permit was revised twice. Ultimately, a Second Revised Notice of Proposed Agency Action dated July 22, 2011, was issued by the District. Attached to the Second Revised NOPAA is the District's Permit. See Joint Ex. Vol. IV, Tab U. A revised Staff Report from the District dated July 18, 2011, is also included in Volume IV of the joint exhibits. See id., Tab Q. The Permit as supported by the staff report allows an average daily withdrawal of 5 MGD, a maximum daily withdrawal of 30 MGD for no more than 60 days per year (with a maximum of 52 consecutive days), and a maximum monthly amount of 775 million gallons. See Joint Ex. Vol. IV, Tab U. The Permit also includes the LTEMP jointly prepared by the Applicant and the District. See id., Attachment B. The Permit requires Bay County to "mitigate any significant adverse impact caused by withdrawals . . . on the resource and legal water withdrawals and uses, and on adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. IV, Tab R, p. 3 of 11. If the District receives notice of an impact from the existing legal user, it contacts the utility. "Within 72 hours [the utility has] a well contractor out there and they have determined what the problem is." Tr. 615. There are no time requirements for the resolution of the impact or any other resolution procedures in the Permit. Definitions of Emergency and Maintenance Amounts The Permit does not include a definition of when the Reservoir may be considered to be unavailable as a public water supply. That determination is left to Bay County. The Permit does not set a withdrawal limit lower than the limits detailed above for maintenance of the Wellfield. There is one set of withdrawal limits. They apply irrespective of the purpose of the withdrawals, that is, whether for backup in an emergency, maintenance, or some other purpose that falls under Public Supply or Industrial Use. Conditions and Monitoring Requirements Bay County is required to mitigate any significant adverse impacts on resources and legal water withdrawals and uses caused by the County's withdrawal from the Wellfield. In addition, the District reserves the right to curtail permitted withdrawal rates if Bay County's withdrawal causes adverse impacts on local resources and legal uses of water in existence at the time of the permit application. In the event of a declared water shortage, the Permit requires Bay County to make water withdrawal reductions ordered by the District. In addition, the District may alter, modify, or deactivate all or parts of the Permit. Attachment A to the Permit, states: The Permittee shall not exceed total, combined groundwater and surface water (authorized in Individual Water Use Permit No. 19910142) withdrawals of an average daily withdrawal of 98,000,000 gallons, a maximum daily withdrawal of 107,000,000 gallons and a maximum monthly withdrawal of 2,487,750,000 gallons. Joint Ex. Vol. IV, Tab U, p. 4 of 11. The inclusion of "surface water" in the condition covers withdrawals from the Reservoir. The combination of actual withdrawals from the Wellfield and actual withdrawals from the Reservoir, therefore, means that Bay County may not exceed the limitations of the withdrawals authorized by the 1991 Agreement. Attachment A to the Permit further explains how Bay County must mitigate harm caused by groundwater withdrawals. The Permittee, within seven days of determination or notification by the District that the authorized groundwater withdrawal is causing harm to the resources, shall cease or reduce, as directed by the District, its pumping activity. The Permittee shall retain the services of a qualified, licensed professional to investigate allegations of interference with an existing, legal groundwater use. The Permittee shall ensure their chosen contractor investigates the alleged interference within 72 hours of the allegation being made. If it is determined that the use of a well has been impaired as a result of the Permittee's operation, the Permittee shall undertake the required mitigation or some other arrangement mutually agreeable to the Permittee and the affected party. The Permittee shall be responsible for the payment of services rendered by the licensed water well contractor and/or professional geologist. The Permittee, within 30 days of any allegation of interference, shall submit a report to the District including the date of the allegation, the name and contact information of the party making the allegation, the result of the investigation made and any mitigation action undertaken. Joint Ex. Vol. IV, Tab U, Attachment A, p. 4 of 11. Bay County is also required, within two years from the Permit's issuance, to submit to the District for review and approval a contingency plan to mitigate potential impacts. The County must wait one full year prior to commencing withdrawal of groundwater for production purposes. During the one-year period, the County must complete groundwater, surface water, and wetland monitoring. The requirements of the mandatory monitoring are found in Attachment B of the Permit, LTEMP. See Joint Ex. Vol. IV, Tab U, Attachment B. The LTEMP "is designed to track trends in ecological and hydrological conditions caused by naturally occurring fluctuations in rainfall, which may affect ground and surface water hydrologic conditions; and to identify potential effects caused by wellfield pumping." Joint Ex. Vol. IV, Tab U, Attachment B at 1. If a substantive deviation occurs from predictions made by the HGL Modeling, or if any other hydrologic or ecologic changes due to the withdrawals are observed at monitoring sites, the District is required to review and, in consultation with Bay County, appropriately revise the LTEMP as necessary with the aim that the monitoring will assure that the conditions for issuance of the Permit are being met. Testimony in Support of the Application In addition to the documentary evidence offered in the first phase of the proceeding, Bay County and the District presented the testimony of several witnesses. These witnesses testified as to background and the 2008 RWSP, the vulnerability of the Reservoir to saltwater contamination from storm surge, and the basis for the District's decision. Vulnerability to Storm Surge There is a one percent chance every year of a 100- year storm event. Flood Insurance Rates Maps ("FIRMS") show that the 100-year water level (the level of storm surge in a 100-year storm event) at the Dam will reach 11 feet NAVD, two feet above the top of the gate structure above the Dam. The Federal Emergency Management Agency ("FEMA") and the National Weather Service ("NWS") have developed the Sea, Lake, and Overland Surge from Hurricanes ("SLOSH") model, which estimates storm surge depths resulting from historical, hypothetical, or predicted hurricanes. A Florida Department of Emergency Management's SLOSH model of the Panama City area shows maximum surge levels for Storm Categories 1, 2, 3, 4, and 5, in NAVD feet as 3.3, 5.8, 10.8, 14.1, and 18.1, respectively. The SLOSH model, in all likelihood, is a low estimation. It is reasonable to expect surge levels in a Category 3 hurricane that passes directly over the Dam, for example, to be higher than 10.8 feet NAVD predicted by the SLOSH model at the Dam. According to the National Oceanic and Atmospheric Administration's ("NOAA") database, 43 tropical storms and hurricanes have passed within 200 miles of the Reservoir between 1970 and 2010 and 20 have come within 100 miles. None have made landfall closer than 40 miles away from the Dam. Of the 20 storms passing within 100 miles of the Reservoir, four have reached Category 3 strength or higher: Eloise, Elena, Opal, and Dennis. In 2004, Hurricane Ivan made landfall over 100 miles to the west of the Dam and raised water levels near the Dam to nearly five feet NAVD. The following year, Hurricane Dennis made landfall 76 miles to the west of the Dam. Dennis produced a surge level of nearly four feet NAVD near the Dam. "Hurricane Eloise (1975) made landfall 40 miles west of Panama City and produced water levels 15 ft above normal at Panama City ([citation omitted]). However, the storm passed through the area quickly and does not appear to have significantly affected the dam." Bay County Ex. 1, p. 3 of 9. Hurricane Opal made landfall 86 miles west of Panama City Beach and produced water levels of about 8.3 feet NAVD near the Dam. The storm surge did not overtop the gate structure above the Dam, but the gates were jammed by debris. "[C]hloride levels rose above 50 ppm at the intake pumps and two to three times above normal background levels of 8 to 10 ppm 'almost one mile up-reservoir.'" Id. The levels of chloride were "still well within drinking water limits," tr. 434, of 250 parts-per- million (ppm). Hurricane Katrina made landfall in 2005 more than 200 miles west of the Reservoir with storm surges higher than 20 feet. Katrina produced surge levels of five feet above normal tide levels in Bay County. The rate and amount of saltwater that would enter the Reservoir depends on the height of the storm surge above the Dam. The 100-year surge levels could remain above the top of the Dam for three or more hours. Such an event would introduce approximately 56,200,000 cubic feet or 1,290 acre-feet of saltwater into the Reservoir, even if the Dam were to remain intact (undamaged) and the tide gates remain closed. The salinity levels bay-side of the dam are generally 23,000 to 33,000 ppm. It is reasonable to expect that in the event of a 100-year storm event, much of the storm surge would come directly from the Gulf of Mexico, which has higher salinity levels. With the Dam intact, the introduction of 1,290 acre- feet of saltwater at 33,000 ppm would raise the average chloride concentration in the Reservoir to at least 800 ppm, more than three times the maximum drinking water chloride level of 250 ppm. Assuming the Dam remained intact during a 100-year storm event, freshwater added over time to the lake from the streams and aquifer will dilute the elevated lake chloride level and restore the lake water to a level fit for human consumption. The USGS has measured stream flow at Deer Point Lake and estimated the lake receives an average of 600 million gallons of freshwater per day or 900 cfs. Post-Opal rates were estimated at 1,500 cfs by the District. Given the estimated volume of saltwater introduced to the lake, at an inflow rate equal to the estimated post- hurricane freshwater inflow rate, Bay County's expert, Dr. Miller, estimated it would take at least two weeks to reduce salinity in the lake to drinkable levels. The inflow rate, however, is not certain. Dr. Miller estimated it is reasonable to expect that it could take anywhere from two weeks to two months for the lake to recover from the saltwater intrusion depending on the variation in the inflow rate. Nonetheless, Dr. Miller assumed that the saltwater from storm surge entering the Reservoir would mix in a uniform matter. There would be "quite a bit of mixing in a storm," tr. 485, of saltwater topping the Dam and freshwater in the Dam. But there would also be stratification due to the sinking of denser saltwater and the rising in the water column of freshwater. The above estimations assume the bridge and Dam remain intact during a major storm. The Dam and tide gates act as a solid barrier, protecting the lake from saltwater in the bay. If rainfall rises in the lake prior to a surge, the tide gates would open to release water, becoming vulnerable to damage or jamming by debris as occurred during Hurricane Opal. In the event of storm surge bringing saltwater into the Reservoir, the opening of the tide gates will assist the Reservoir in reaching chloride levels below 250 ppm provided the tide gates operate properly. Dr. Janicki, an NTC/Knight expert, used the Environmental Fluid Dynamics Code hydrodynamic model ("EFDC Model") to simulate the effects of control structures and water withdrawals on the Reservoir. Taking into consideration the factors Dr. Janicki considered relevant, he predicted that chloride levels, in the event of storm surge from a Category 3 hurricane overtopping the Dam, would only exceed 250 ppm, the drinking water standard, for approximately 3.4 days. Dr. Janicki's prediction, however, was flawed. He added too little saltwater to the lake in the event of contamination from storm surge. He assumed that saltwater would be flushed too soon from the Reservoir following contamination. He did not account for the effects of waves in his model. His model was not in accord with data for Hurricane Opal and the chloride levels near the Dam taken by Bay County after Opal. If the bridge and Dam were severely damaged, more saltwater could enter the lake. With severe damage to the Dam, the Reservoir would be exposed to normal tides. Restoration would not begin until the Dam and bridge had been fully repaired. If an event were catastrophic, the Reservoir could be offline for a lengthy period of time. The Basis for the District's Decision Bay County's reliance on the Reservoir for water for the majority of the population led the District in the mid-1980s to encourage the County to obtain a backup supply. After the District turned down several requests for withdrawals of up to 30 MGD for every day of the year, the District ultimately approved what is reflected in the Permit. The justification for the permitted withdrawal is as a backup supply in the event the Reservoir becomes unavailable and for maintenance of the system and recoupment of its cost. With regard to maintenance, the District attempted to obtain information from Bay County as to appropriate withdrawal limitations. The attempts were abandoned. Despite repeated requests by the District, Bay County did not provide the amount of water needed to be withdrawn for maintenance since it did not have "infrastructure specifics," tr. 552, needed to provide the District with a numeric limit. In contrast to the amount needed for maintenance, the District found Bay County to have demonstrated that it needs 30 MGD when the Reservoir is offline and that it is reasonable for the County to need 30 MGD up to 60 days per year. The District determined that the Bay County's application met the requirements for the issuance of a consumptive use permit found in section 373.221(1)(a)-(c). In determining whether approval of the application is in the public interest, the District did not presume that it is in the public interest on the basis of the designation in the 2008 RWSP of an inland groundwater source as an alternative water supply. The District determined that it is in the public's interest for Bay County to have a reliable and safe water supply source as a backup to the Reservoir irrespective of the statutory presumption. Nonetheless, the District maintains in this proceeding that the presumption applies. The District also applied the 18 criteria test for finding a reasonable-beneficial use found in Florida Administrative Code Rule 62-40.410(a)-(r) and determined that the application should be approved. Petitioners' Case in Opposition Washington County (Petitioner in Case No. 10-2983), NTC/Knight (Petitioner in Case No. 10-2984), and Messrs. Murfee and Lapensohn (Petitioners in Case No. 10-10100) filed individual petitions for formal administrative hearing. Although not identical, the petitions share the similarity that, in essence, each alleges that Bay County failed to establish that the proposed use of water meets the statutory and rule criteria for obtaining a permit for the consumptive use of water. For example, among the many issues listed under the heading "Disputed Issues of Material Fact and Law" in Washington County's Petition for Formal Administrative Hearing is "[w]hether Bay County has provided reasonable assurance that its proposed use of water is a reasonable-beneficial use as defined in section 373.019, Florida Statutes." See p. 5 of the Washington County petition. In like fashion, the Washington County petition and the other two petitions allege that the issues are whether Bay County provided reasonable assurance that it meets the other statutory criteria in section 373.223, and the applicable rule criteria that must be met by an applicant in order for the District to issue a permit for the consumptive use of water. The Petitioners' cases focused on five topics: 1) the limitations of the HGL Model; 2) the likelihood of impacts to wetlands and the failure of the monitoring plan to provide reasonable assurance that the District's monitoring under the plan will succeed in detecting harm to wetlands caused by the withdrawals; 3) the reasonable-beneficial nature of the proposed use of the permit, including the vulnerability of the Reservoir; 4) interference with presently existing legal users; and 5) the feasibility of alternative sources. Bay County and the District offered evidence on rebuttal to meet the Petitioners' cases. Surrebuttal was conducted by Petitioners. Modeling Groundwater models "represent what is happening in very complex physical systems." Tr. 1495. Typically, the data used by models is not sufficient to obtain a completely accurate representation. The models depend on specific data points such as information from boreholes or water level measurements that do not reveal everything that is occurring in the complex system and, therefore, are not enough to support completely accurate model predictions. As explained by Dr. Guvanasen, Bay County and the District's expert, in order to reach a representation of the entire system when the data available from boreholes and measurements is insufficient, which is typically the case, the modeler must "extrapolate a lot of information and use other knowledge of other events." Id. The "knowledge of other events" that the HGL Model used included Dr. Scott's knowledge of the karst environment in the Panhandle of Florida, the mapping of Bay and Washington County geology by the Florida Geological Society, and Dr. Upchurch's knowledge of karst topography. The HGL results of the available data and the extrapolations were placed into a mathematical model (the HGL Model) that considered the withdrawals at issue to determine the response of the system to the additional stress of the withdrawals. Mathematical models like the HGL Model lead to "non- unique solutions" in which "no model . . . is exactly 100 percent correct . . . ." Tr. 1635. Modeling results, therefore, are subject to changes as additional data is collected that demand a better representation than the model provided prior to the data's collection and analysis. HGL Modeling for this case provides examples of non- unique solutions. HGL "built a model twice . . . and got two different sets of answers." Tr. 1633. Besides the recommendation that more data be obtained after the first HGL Model results, the model was not satisfactorily calibrated and the model was recalibrated for the Revised HGL Modeling results. Mr. Davis, NTC/Knight's expert, conducted additional modeling work (the "Davis Modeling"). Using the HGL Model and additional data concerning the NTC/Knight Property, Mr. Davis found drawdowns would occur over a similar but greater area than shown in the 2011 Revised HGL Modeling Report. (Compare NTC/Knight Ex. 31 at 2 to Joint Ex. Vol. III, Tab P, Figure 51b(1).) The Davis Modeling drawdowns, moreover, ranged up to 0.8 feet, 60 percent more than the 0.5 feet determined by the second HGL Modeling results. In the area of Big Blue Lake, for example, the drawdown contours produced by the Davis Model were either 0.6 feet or 0.7 feet, 20 to 40 percent more than the 0.5 feet produced by the second HGL Modeling results. See NTC/Knight Ex. 31 at 2. Asked to rank the modeling results between the first HGL Model run, the second HGL Model run, and his own results, Mr. Davis was unable to say which was better because of the sparseness of the data. Mr. Davis opined that he could conduct another "dozen more model runs," but without additional data he would be "hard pressed" to be able to say which run was more accurate. Tr. 1633. In Mr. Davis' opinion there remain significant uncertainties that cannot be resolved without more data. Inadequate data "precludes . . . reasonable assurance as to exactly where the impacts will travel and exactly what the magnitude of those impacts will be . . . ." Tr. 1637. Ecological Impacts Bruce A. Pruitt, Ph.D., was accepted as an expert in hydrology, soil science, fluvial geomorphology, and wetland sciences. Dr. Pruitt mapped the soil types on the NTC/Knight Property using the Natural Resource Conservation Service ("NRCS") Web Soil Survey and tested soil types by hand-auguring in wetland areas. He characterized the various soil-types on the property by drainage class (relative wetness of the soil under natural conditions) and hydraulic conductivity (permeability). Dr. Pruitt ranked the vulnerability of wetlands within the zone of drawdown predicted by the HGL Model as "very high," "high," or "moderate." The categories were based on the presence of threatened and endangered species, Florida Natural Area Inventor ("FNAI") habitat designation, and the hydrology of the wetland. He assumed that if the water level in the Surficial Aquifer were to be drawn down by 0.3 feet or 0.4 feet then the water level in the seepage bogs at Botheration Creek would be drawn down by the same amount. Wetlands with a vulnerability classification of "very high" will suffer an adverse impact at a drawdown level of 0.2 feet; those at "high" at 0.3 feet and those at "moderate" at 0.5 feet in times of drought. Dr. Pruitt calculated wetland acreage by type using the Florida Cover Classification System. He assigned vulnerability rating for the wetlands within the Surficial Aquifer drawdown contours generated by the HGL Model. Based on Dr. Pruitt's calculations, a total of approximately 4,200 acres of wetlands are likely to be harmed by the predicted drawdown. A majority of these wetlands are located in Washington County. Based on Dr. Pruitt's analysis, it is likely that the NTC/Knight Property contains 1,981 acres of "very highly" vulnerable wetlands; 1,895 acres of "highly" vulnerable wetlands; and 390 acres of "moderately" vulnerable wetlands, which are likely to be harmed by the drawdown in times of drought. In reaching his opinion about the quantification of acres of wetlands likely to be harmed, Dr. Pruitt applied the Florida Uniform Mitigation Assessment Method ("UMAM"). UMAM was designed to address compensatory mitigation in dredge and fill cases. It was not designed for consumptive water use cases. In contrast and damaging to its case of reasonable assurance that natural systems will not be significantly affected, the District did not conduct an analysis to determine loss of wetland function resulting from operation under the Permit. Nor did it determine how much drawdown the affected wetlands could tolerate before they were harmed. Rather than conducting such an analysis, the District chose to rely on implementation of the LTEMP to cure any harm that might be down by drawdown to the Surficial Aquifer. The District and Bay County's wetland scientists opined that there might be a less permeable restrictive layer maintaining water levels above the Surficial Aquifer on the NTC/Knight Property. Dr. Pruitt acknowledged that the NTC/Knight Property had scattered clay layers beneath the surface. It is possible, therefore, that some of the wetland areas he identified as subject to harm have restrictive features under them which would hold water and resist dehydration. In his hand-auguring, however, Dr. Pruitt found no evidence of a less permeable layer. The auguring only went to a depth of three feet and would have to go to a depth of two meters to be definitive. Furthermore, Dr. Pruitt found no evidence of a less permeable layer from well drillings. The District and Bay County did not prove that there is, in fact, such a restrictive layer. NTC/Knight collected water-level data from shallow hand-augured wells and stage recorders at the Botheration Creek Hillside Seepage Bog. The data demonstrate that the water level in the shallow, hand-augured wells at the Botheration Creek Bog is a direct reflection of the level of the Surficial Aquifer. The Surficial Aquifer at the Botheration Creek Bog was approximately 95.5 feet NAVD, over 35 feet higher than at Big Blue Lake and the highest measured level south of Big Blue Lake. The Botheration Creek Hillside Seepage Bog is located between the 0.3 and 0.4 foot Surficial Aquifer drawdown contours predicted by the HGL Model. Based on the HGL Model, the District and Bay County's experts estimated the Surficial Aquifer drawdown at this bog would be 0.39 feet. During the approximately one year of NTC/Knight's water-level recording, a drawdown of 0.39 feet would have reduced the frequency and duration of inundation at this bog significantly. For example, an analysis of the approximately one year of data collected by NTC/Knight shows that at the intermediate water-level recorder location in the bog, one 29-day period of inundation would have been reduced to just nine days and that further down gradient in the bog, none of the five instances when the bog was inundated would have occurred. This is consistent with Dr. Pruitt's vulnerability assessment, which finds that the vulnerability of the hillside seepage bogs to drawdown is "very high," that is, these systems are likely to be harmed in times of drought at drawdown levels in the Surficial Aquifer of 0.2 feet or greater. A drawdown of 0.3-0.4 feet in the Surficial Aquifer at the hillside seepage bog along Botheration Creek increases the likelihood that the hillside seepage bogs along Botheration Creek will be lost in times of drought. The littoral shelves of Sand Hill Lakes typically occur along a low gradient above the normal low water level of the lakes. The existence of the shelf promotes seepage sheet flow along a wide expanse. The drawdown will change the flow from seepage sheet flow to concentrated stream flow within gullies. The erosion and increased sedimentation produced by the greater force of the water in the gullies will cause a loss of area needed by certain seepage dependent plants and animals. If Big Blue Lake were to be drawn down by the 0.71 feet predicted by Mr. Davis, the location of the seepage would move down 0.71 feet vertically and an estimated 24.5 feet horizontally. The result would be a reduction in the littoral shelf conducive to seepage-dependent plant communities by approximately nine acres. The impact would likely be significant since the seepage zone is in an area of "very high" vulnerability according to Dr. Pruitt. Between October 2010 and July 2011, NTC/Knight took four measurements of water level at "BCS-01," a stage recorder in Botheration Creek. The measurements showed the water level in the creek at that point to be 0.1 to 0.32 feet. NTC/Knight also sampled for taxa of macroinvertebrates in the reach of the creek. NTC/Knight identified 46 taxa, including mussels and six long-lived taxa. The presence of the long-lived taxa and mussels indicate that the reach of the creek in the vicinity of the stage recorder should be considered to be a perennial stream. Botheration Creek is high-quality water and, as shown by NTC/Knight's sampling, it contains a diverse mix of aquatic invertebrates and fish. A drop in the level of Botheration Creek of 0.2 feet predicted by the HGL Model would have caused the creek to go dry at BCA-01 during three of the four dates on which the water level was measured. Such a drop would convert the reach of the creek in the vicinity of the stage recorder from a perennial to an intermittent stream and would eliminate the reach's viability for long-lived taxa. Similarly, upstream reaches that are intermittent would become ephemeral (streams that flow only during periods of high rainfall). If the Wellfield becomes fully operational as allowed by the Permit, there will be a reduction in the Surficial Aquifer at Botheration Creek of between 0.2 and 0.3 feet. The reduction in the aquifer will reduce flow in Botheration Creek, reduce the volume downstream, including in Pine Log Creek, and reduce out-of-bank flood frequency and duration. The result will be a reduction in nutrients delivered downstream and to the floodplain to the detriment of plants and animal life that depend on them. Additionally, other reaches of the creek that have perennial flow will be converted to intermittent streams and reaches that are intermittent will become ephemeral. The result will be the elimination of plant and animal species currently living in these portions of the creek. The impact of the HGL Model predicted drawdown to steepheads depends on the individual steephead and the drawdown contour at its location and the amount of rainfall. Four steepheads on the NTC/Knight Property could suffer impacts similar to the impact at Russ Steephead to which Dr. Pruitt assigned a high probability of impact. Russ Steephead is located on the NTC/Knight Property above Russ Pond. NTC/Knight installed Surficial Aquifer wells at Russ Steephead between the HGL Model's predicted 0.5 and 0.6 foot Surficial Aquifer drawdown contours. NTC/Knight also installed a stage recorder just downstream from the steephead. During drought, NTC/Knight observed a loss of flow from the sidewall seepage areas and in the Russ Steephead Stream. If the Surficial Aquifer at Russ Pond were to be drawn down by 0.5-0.6 feet, the sidewalls of the Russ Steephead Stream and the stream itself would lose flow in times of drought. The loss of flow would lead to oxidation and loss of organic materials in the stream channel and flood plain, resulting in soil subsidence. If the water level at the terminus of the Russ Steephead Stream were drawn down, headward down cutting in the stream channel would be induced. In such a case, in the words of Dr. Pruitt, "there is a high probability that if drawdown occurs and . . . over a long period of time," the process will make the steephead "look more like a gully . . . ." Tr. 2120. The drawdown will also reduce the frequency and duration of inundation of the sphagnum bogs in the four steepheads likely to be affected by the drawdown. The bogs and the associated animals that depend upon them would be lost. Dr. Means identified a number of temporary ponds within HGL's predicted drawdown of the Surficial Aquifer. Nine were between the 0.3 and 0.6 foot drawdown contour, and two were between the 0.6 and 0.7 foot drawdown contours. These ponds and plant and animal communities dependent upon them would likely be harmed by the drawdowns. Mr. Cantrell offered testimony to rebut the Petitioners' case on wetland impacts. His testimony was based on an evaluation of aerial photography, site visits to the Wellfield, and a one-day trip to the NTC/Knight Property. It is Mr. Cantrell's opinion that if the NTC/Knight Property were to drain, it would be because of a surface water drainage system, such as ditching, not because of drawdown in the Surficial Aquifer caused by operation of the Wellfield. Mr. Cantrell's opinion is that because the Area has been subjected to a wide range of fluctuations in water levels and the wetland systems have survived, operation of the Wellfield will not have significant impacts. Mr. Cantrell's opinion, however, overlooks the effect of constant drawdown during times of severe drought. That wetlands have survived severe drought in the past does not mean they will survive severe drought conditions exacerbated by drawdown caused by operation of the Wellfield. Monitoring Special condition 19 of the Permit requires Bay County to implement the LTEMP after the Permit is issued. The LTEMP requires Bay County to establish a monitoring network, but does not provide the location of any particular monitoring site. Sites identified in the LTEMP are recommended, but the ability to use a particular site is dependent on field verification of suitability and authorization by the landowner. Over half the area designated in the LTEMP from the HGL Model's projected 0.5 foot drawdown in the Surficial Aquifer is located on the NTC/Knight Property. It will be necessary, therefore, to include sites on the NTC/Knight Property in the ultimate environmental monitoring network. The LTEMP's recommended sites do not include monitoring of some of the most susceptible wetland systems: temporary ponds, the Botheration Creek hillside seepage bogs, and the perennial headwaters of Botheration Creek. Without this monitoring, the LTEMP will be unable to detect whether these systems are harmed by withdrawals. The Permit and LTEMP require no more than one-year of baseline data to be collected prior to initiation of water withdrawals. The proposed monitoring time is inadequate to create a sufficient record for use in determining whether a reduction in water levels is attributable to water withdrawals or natural phenomena, such as drought. Baseline monitoring should be conducted for a sufficient duration to ensure that a full range of wet and dry years is captured. The LTEMP describes the types of data that are to be collected. A missing component is sampling for frogs, salamanders, and other amphibians that are sensitive to changes in hydrologic regimes and which depend upon infrequent periods of inundation in order to breed. This type of faunal sampling is particularly important in the temporary ponds and seepage environments. Without sampling for the presence of these species, the LTEMP will be unable to determine whether these populations have been harmed by withdrawals. The LTEMP includes a number of "triggers," that if tripped, require the preparation of an auxiliary report. A number of these triggers make reference to changes in water levels at the level of "significant deviation," an undefined term. More importantly, the LTEMP fails to require any statistical analysis. Without it, the LTEMP will be inadequate to establish whether a reduction in water levels is caused by water withdrawals or another cause. Similarly, other triggers lack sufficient detail to determine when they are tripped, such as those that refer to downward movement of plants. Finally, even if one of these triggers is tripped and an auxiliary report is prepared, nothing in the Permit or LTEMP sets forth the circumstances under which withdrawals would need to be curtailed and by what amount. The purpose of the LTEMP is to determine whether withdrawals are causing harm to the wetlands within the vicinity of the Wellfield. The LTEMP fails to provide reasonable assurance that it will succeed in achieving its purpose. Reasonable-Beneficial Use Use if the Reservoir is Unavailable In the event of Reservoir unavailability, Bay County is likely to need much less than 30 MGD. The need is likely to fall between 7.42 MGD and 9.71 MGD for the current population. In 2013, the need is likely to fall between 9.40 MGD and 12.29 MGD. See NTC/Knight Ex. 5, p. 4 of 4. The Permit, however, does not limit Bay County to emergency or backup use. While Bay County might voluntarily limit withdrawals to emergency use or backup supply, it has unfettered discretion to determine what constitutes an emergency or the necessity for a backup supply. The Permit is also not restricted to essential uses. Authorization of 30 MGD provides more than Bay County's current average daily demand for potable water. If the Permit restricted the use to essential uses, the authorization would be far less than 30 MDG. The District commissioned King Engineering to assist in development of a "Coastal Water Systems Interconnect Project" (the "Interconnect Project"). On average, the utilities subject to the Interconnect Project estimated that 42 percent of the average daily demand is dedicated to essential uses with the remaining 58 percent going to non-essential uses. Consistent with the estimate, the Project set a target of 50 percent of average daily demand to be allowed for use in an emergency. None of the information from the Interconnect Project, however, was used by the District in setting the limits of withdrawal in the Permit. b. Daily Use Bay County claims the 5 MGD annual average allocation under the Permit is needed for several reasons, principally the maintenance of pumps. Bay County's justification for 5 MGD is found in testimony from Mr. Lackemacher and a document he authored entitled, "Confidential Draft for Internal Use Only 5 MGD Pumping Rate" (the "Lackemacher Confidential Draft"), admitted as Bay County Ex. 24. Mr. Lackemacher's testimony follows: A. The fact is that there are no absolute knowns when we're talking about what needs to be. Q. What do you mean? A. Well, here we have a document [Bay County Ex. 24] where I talk about rationalization for 5 million gallons a day, why we would need it, mechanical reasons, financial reasons, regulatory reasons. I always felt that it was very difficult to justify a number. I don't know. We haven't designed the system. We haven't got all of the wells in. We don't know what their specific yields are. There's unknowns here. So do we need 2 million gallons a day or 5 million gallons a day? I don't know. I don't know that. But here is the rationalization for 5 million if that's in fact what we need. We may very well find out that we don't need 5 million gallons a day. Q. Is that because you don't know the precise locations of the well and how they're going to be piped and distributed? A. That's absolutely true. Q. Well, did you in this report, Exhibit 24, did you make some reasonable assumptions? A. I based it on some of the values as you discussed or as I pointed out earlier from Hatch Mott MacDonald's preliminary design. * * * Q. And do you feel confident that your analysis supported that in the area of 5 million gallons a day is what would be needed to operate the wellfield? A. Yes. And that's why the paper was generated that [is] a justification for 5 million gallons a day, here's what we think we would need. Tr. 209-10. The Lackemacher Confidential Draft is a one-page, written justification for the 5 MGD. Based on the Hatch Mott McDonald Report, see tr. 210, it considers regulatory, mechanical and financial factors. It is not supported, however, by engineering analysis. Any financial analysis found in the Hatch Mott McDonald Report, moreover, is far from complete. The factors taken into consideration are recited in the most general of terms. For example, of four such factors, the document lists the second as: "All water pumps are designed to run - turning pumps on and off is not the best situation for the overall electrical efficiency or the mechanicals of a pump." Bay County Ex. 24. Consistent with Mr. Lackemacher's testimony, the document concludes that the amount of water needed to run each well is unknown. The financial justification is based on costs shown in the Hatch Mott MacDonald Report for construction and operation of 22 wells, ten more wells than are contained in the Wellfield and without any analysis of revenue to recoup the costs. The financial justification is a bare conclusion on the part of Mr. Lackemacher: We cannot afford to operate a well field at a financial loss, based on this fact alone we would have to pump a minimum of 4.49 MGD. Combined with the fact that we don't know what volumes of water have to be turned over to ensure water quality 5 MGD seems quite reasonable. Bay County Ex. 24. The Lackemacher Confidential Draft is dated May 17, 2011. It was not part of Bay County's Application nor was it submitted to the District prior to the decision to issue the Permit. Although the District attempted to obtain information from Bay County about what was needed for maintenance, Bay County did not provide it. As Mr. Gowans testified, "[t]hen I finally told staff, [s]top asking, we're not going to get the numbers . . . ." Tr. 552. The District performed no analysis to determine the minimum amount of water needed to maintain the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Phillip Waller, an engineer accepted as an expert in the design and construction of potable water systems, including groundwater wells, surface water, and transmission and distribution of drinking water. Mr. Waller testified that if the wells were connected to a central treatment system, there would not be the need to flush the pipeline for disinfection prior to use of the well in an emergency. Only 2.4 million gallons per year or 6,500 gallons per day would be needed to maintain optimum operating conditions, an amount far less than 5 MGD. Mr. Waller's experience when groundwater is used as a backup, moreover, is that they are operated periodically. While prudent to periodically operate backup wells especially in advance of hurricane season, vertical pumps in wells, unlike horizontal pumps, do not have a need for frequent operation because of even force distribution. They certainly do not need to be continuously operated. "In fact, wells routinely are idle for months at a time." Tr. 1123. Interference with Existing Legal Users In its Revised Staff Report dated July 18, 2011, the District wrote: Nearby Users: Under the most intensive pumping activity, drawdown in the Upper Floridan Aquifer is predicted to be approximately 15 feet in the vicinity of the nearest private wells. Water level declines of this magnitude may cause water levels to fall below the level of the pump intake in some privately-owned wells. Joint Ex. Vol. IV, Tab Q, p. 4. The District's high estimate of the number of wells used by existing legal users that might suffer impacts approaches 900. The exact number or whether any existing legal users would be likely to suffer impacts was not proven. Alternatives Groundwater wells, if installed and attached to the fitting in the existing transmission line that delivers water from the Pump Station to the Water Treatment Plant, could serve as backup to the Reservoir. Bay County did not conduct a study of whether groundwater in the area of the transmission line was adequate to serve as an alternative. Mr. Waller, on behalf of NTC/Knight and Washington County, on the other hand, testified that the transmission line could support ten wells with a capacity of 10 MGD and could be constructed at a cost of $12 million, far less than the Wellfield. The area of the transmission line is in an area identified by the District as acceptable for the creation of potable water wells. The area does not present a significant risk of saltwater intrusion if not used continuously. The water meets the drinking water requirements for the Department of Environmental Protection and the Department of Health. The existing transmission line alternative is located near the existing raw water supply line which minimizes the need for additional piping. There is sufficient length along the existing raw water pipeline to accommodate ten wells. The existing transmission line alternative, therefore, has significant potential to succeed as a water supply backup to the Reservoir. NTC/Knight and Washington County, through Mr. Waller, also proposed another alternative: an intake at Bayou George. Near Highway 231, the main pipeline from the intake would run along public right-of-way. North of the existing intake in Williams Bayou and three miles north of the Dam, the proposed intake would be less susceptible to contamination from storm surge. Neither Bay County nor the District presented a thorough analysis of any alternative to the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Mr. Waller that there are two alternatives that could be constructed at much less cost than the Wellfield and that have significant potential of providing backup supply.

Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Northwest Florida Water Management District enter a final order that denies the application of Bay County for the individual water use permit at issue in this proceeding. DONE AND ENTERED this 26th day of July, 2012, in Tallahassee, Leon County, Florida. S DAVID M. MALONEY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 26th day of July, 2012.

Florida Laws (9) 120.569120.57120.574373.019373.069373.223373.709403.8907.42 Florida Administrative Code (1) 62-40.410
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