Findings Of Fact Application No. 76-00451 seeks a consumptive water use permit for an existing use involving 14 withdrawal points. The application seeks a total average annual withdrawal of 20.2584 million gallons per day and a maximum daily withdrawal of 45.8539 million gallons per day. The water will be used for citrus processing. The Southwest Florida Water Management District's staff recommends issuance of the permit with the following conditions: That the applicant shall install totalizing flow meters of the propeller-driven type on all withdrawal points covered by this permit. That the applicant shall record the pumpage from the above-referenced meters on a weekly basis and submit a record of that pumpage to the district quarterly, beginning on January 15, 1977. That the permit shall expire on December 31, 1980.
Recommendation It is hereby Recommended that a consumptive use permit in the amounts and from the points set forth in the application be granted subject to the conditions set forth in paragraph 2 above. ENTERED this 13th day of October, 1976, in Tallahassee, Florida. CHRIS H. BENTLEY Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Southwest Florida Water Management District Post Office Box 457 Brooksville, Florida 33512 Lykes Pasco Packing Company Post Office Box 97 Dade City, Florida
Findings Of Fact The CLDD was established pursuant to Chapter 298, Florida Statutes, on August 4, 1967. Its purpose was to "reclaim" or render the land within its boundaries usable for agricultural purposes. The land comprising the CLDD consists of approximately 3,500 acres in Lee County, mostly planted in citrus trees. Pursuant to the requirements of Chapter 298, Florida Statutes, a "Plan of Reclamation" was prepared by consulting engineers for the CLDD's Board of Supervisors in August, 1967. That plan contains provisions for reclaiming lands within the CLDD's boundaries and for managing and controlling surface water within CLDD. The method of water control outlined in the 1967 reclamation plan included a dike and ditch system around the boundaries of CLDD with a series of interior canals to carry excess water away from the citrus trees. The land in the north part of he CLDD is higher than the south and water generally, naturally flows from north to south. The interior canals were designed to carry water in accordance with existing contours of the land and eventually discharge excess surface water to the rim ditches on the north and east sides of Spoil Area "M," which is south of the CLDD and which was then owned by the C&SFFCD, the predecessor agency to SFWMD. The system of drainage delineated in that 1967 plan, inaugurated pursuant to Chapter 298, Florida Statutes, was put into effect substantially as described therein. CLDD's 1967 plan was altered somewhat because of an agreement entered into on September 30, 1971, between the CLDD and neighboring landowner Kenneth Daniels. Pursuant to that agreement, the two parties agreed to extend the dike on the west side of the CLDD property and construct a ditch from a point 50 feet north of the northwest corner of the Petitioner Mellor's property, which new ditch was to run southwest across the Daniels' property and connect with Spanish Creek. That ditch or canal would thus connect the western rim ditch of the SFWMD's Spoil Area "M" with Spanish Creek and have the result that surface waters could be discharged from CLDD lands through the western rim ditch of Spoil Area "M" thence through the "Daniels' Ditch" finally discharging into the lower reaches of Spanish Creek. (see Exhibits 1 and 11) Because the western side or western rim canal of the SFWMD's Spoil Area "M" had not been used under the original plan of reclamation approved by the C&SFFCD, CLDD sought permission from C&SFFCD to use this western rim canal for the purpose stated pursuant to the agreement with Daniels. Thus, CLDD's proposed use of the rim canal of Spoil Area "M" would be confined to the western, northern and eastern perimeter canals and not the southern boundary canal. All affected landowners, Kenneth Daniels as well a Jake and Lilly Lee, agreed to those proposed installations and uses. The resulting agreement between CLDD and C&SFFCD was entered into on October 12, 1972, and describes the flood control District land to be used by CLDD as a 100 foot wide strip running along the west, north and east sides of Spoil Area "M," also know as "Aspic." This 100 foot wide strip of land running thusly is co-extensive with the rim ditch of Spoil Area "M." The CLDD was mandated by this agreement to install 72- inch pipes in the rim ditch at the southwest corner of the spoil area, just north of the Mellor property, giving a point of discharge from the western rim ditch into the Daniels' Ditch with similar pipes connecting that Daniels' Ditch with Spanish Creek, such that the canal between these two points could carry water from the west rim ditch to Spanish Creek. The easement incorporated in this agreement was to last for five years with an option for a five-year renewal, which option was exercised. At the end of this 10-year period, SFWMD, successor to C&SFFCD, notified CLDD that because its statutory authority had since changed, the easement could not be renewed and that CLDD would have to seek the subject permit so as to be authorized to use works and lands of the District. The requirements to be met by an applicant for a right-of-way permit such as this one are set out in Rule 40E-6.301, Florida Administrative Code, and SFWMD's permitting information manual, Vol. V, Criteria Manual for Use of Works of the District, July, 1981, which is incorporated by reference in that rule. In that connection, the permit at issue, if granted, would not cause an interference with the "works" of the District, that is dikes, ditches, flood control structures arid drainage structures because it would merely renew the pre-existing authorized use. The permit will not be inconsistent with an comprehensive water use plan developed by the District. Further, the permit applicant owns or leases the land adjacent to the portion of the "works of the District" involved herein that is the east, north and west rim ditches of Spoil Area "M," the Daniels' Ditch and the pipes at either end of it coupled with the water control structures at the southeast corner and southwest corners of Spoil Area "M," which control water entering the south rim ditch. CLDD has a surface water management permit, issued in August, 1980, which is a prerequisite to the granting of the subject right-of-way permit. It remains in full force and effect. That surface water management permit authorizes "operation of a water management system serving 3,642 acres of agricultural lands by a network of canals and control structures, with a perimeter dike and canal discharging into Cypress Creek." The "surface permit" authorized the system of drainage and discharge in existence at the time of its issuance, May 8, 1980. The system of drainage, at the day of the hearing, consisted of the same basic water flow and discharge pattern that existed for approximately 10 years, and this permit would allow that to be continued, thus, there will not be any additional effect on environmentally sensitive lands occasioned by an issuance of the subject right-of-way permit. The surface water management permit, by its terms, refers initially to the operation of a water management system" . . . discharging into Cypress Creek." The reference to "Cypress Creek" was an administrative error. The express language on the face of the permit authorization incorporates by reference the application, including all plans and specifications attached thereto, as addressed by the staff report, and those materials, including the staff report, are a part of the permit. The complete permit, including all those documents incorporated by reference, makes it clear that the authorization of the surface water management permit was that the system of drainage in existence at the time of permit issuance (1980) was that which was being approved, and that included discharge to Spanish Creek and not Cypress Creek. Discharge of water to Cypress Creek as an alternative was never recommended or authorized by that surface water management permit. This is clearly the intent expressed in the permit in view of the language contained in a special condition of that surface water management permit imposed by the SFWMD as a condition for issuance which stated as follows: Within 45 days of the issuance of this permit the permittee shall submit for staff approval a proposal and schedule for the elimination of the adverse impacts being created by the operation of the permittee's water management system, which can be legally and physically accomplished by the permittee. Adverse impacts are considered herein to be reduced flows to Spanish Creek and increased flows to Cypress Creek. Thus, it is obvious that the authorization of the surface water management permit was designed to provide for discharge into Spanish Creek and to enhance the flows to Spanish Creek pursuant to a required proposal which the permittee submitted to SFWMD. Thus, the right-of-way permit applied for herein is consistent with the valid surface water management permit held by the permit applicant in this proceeding. Petitioners William H. and Patricia H. Mellor are co-owners of parcels of property lying some distance south of Spoil Area "4" in the vicinity of the Caloosahatchee River. This property does not abut the spoil area at any point. Spanish Creek does cross their property several thousand feet south of the south boundary of the spoil area. In the past, particularly in 1982, water flowing from the south rim ditch of the spoil area through a break in the dike of that south rim ditch, has flowed through a ditch known as Dry Creek in a generally southerly direction under S.R. 78 and has washed out an access road constructed by William Mellor which leads from Highway 78 to his property. He had this washout repaired at his own expense in 1982. The washout was caused by water from CLDD flowing into the south rim canal of Spoil Area "M," that is, the ditch that traverses (and defines) the southerly boundary of the spoil area. Mr. Mellor admitted, however, that SFWMD had at least partially plugged the opening in the south rim ditch which had allowed flow down the Dry Creek ditch and wash out his road. If closed water control structures are maintained at the southwest and southeast corners of the spoil area ditches, then no water could flow into the south rim canal and no such injury could again be caused. Petitioner's Jim English and Patricia Mellor are co-owners of a 45- acre parcel of land located in the southwest corner of Spoil Area "M." The five acres forming the extreme southwest corner of the spoil area do not belong to these Petitioners, but are owned by one Lynwood Brown, who is not a party to this proceeding. The English/Mellor property forms a part of the spoil area, but does not adjoin or constitute any part of the spoil area which is sought to be used by CLDD through the proposed right-of-way use permit (as clarified by CLDD's stipulation). The south rim ditch, either part of, or adjoined by their property, has been used for water storage in the past (they maintain illegally) 1/ Mr. Tom Pancoast has observed Spanish Creek frequently over a nine- year period starting in approximately 1973. He has often used those waters during that period for fishing. During the early years of his use and observation of Spanish Creek, the water flowed out of Spanish Creek into the Caloosahatchee River. Beginning in about 1976, the water appeared to be flowing in the opposite direction, from the river into Spanish Creek. Contemporaneous with this hydrologic change, the creek has become increasingly characterized by siltation and hyacinth growth. Mr. William Mellor owns property along the course of Spanish Creek. He has used the stream for recreational purposes, picnicking where the stream traverses his property. In recent years there has occurred a marked increase in the growth or profusion of aquatic plants of unidentified types in the creek, reduced clarity and reduced flows or volumes of water in the creek. Witness English has made a similar observation. Witness James English has a substantial degree of training by formal education and experience in water management and drainage practices and methods, particularly as they relate to citrus grove development and management in southwest Florida. Mr. English has observed Spanish Creek regularly for most of his life, including the region of its headwaters in the "Cow Prairie Cypress," a remnant wetland cypress strand lying within the CLDD immediately north of Soil Area "M." The chief adverse impact of the CLDD water management system is reduced flow to Spanish Creek, especially its upper reaches since the advent of the "Daniels' Ditch" as a drainage route and discharge point into lower Spanish Creek. However, the only special condition on the issuance of the surface water management permit approving CLDD's extant water management system was the requirement that CLDD should submit a plan for eliminating that adverse effect, which it did (as Petitioner English admits). Beyond the submission of such a plan, no concrete action designed to restore historic flows to Spanish Creek has yet begun, however. The restoration of historic flows, adequate in volume and quality, to the entire creek system would require discharging water from CLDD's system to the Cow Prairie Cypress area at the headwaters of the creek rather than substantially further downstream at the present Daniels' Ditch site. The Petitioners' complaints (aside from the issue of adequacy of flows in Spanish Creek), although meritorious, are, because of stipulations asserted by CLDD during the course of this proceeding, now rendered moot. CLDD stipulated that it only seeks a permit to use the west, north and eastern spoil area ditches. It does not seek and stipulated that it will not use, at any time, the south rim ditch and will maintain water control structures so to block water from entering that ditch. This will alleviate the problem of potential storage of water on Petitioners English and Patricia Mellor's property and the erosion problem on Petitioners William and Patricia Mellor's property south of the spoil area. It was thus established that the issuance of the right-of-way permit will not cause the injuries these Petitioners have suffered in the past because of use of the south rim ditch for water drainage and storage.
Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence in the record and the candor and demeanor of the witnesses, it is, therefore RECOMMENDED: That the South Florida Water Management District grant the County Line Drainage District's application for a permit for utilization of works and lands of the District. Subject to the following special condition: Issuance of this right-of-way permit does not relieve the Respondent CLDD from the responsibility of complying with special condition number 1 of the surface water management permit number 36-00184-S. Respondent CLDD shall, within 30 days of date of permitting, submit a design to the satisfaction of the SFWMD staff which will prevent the ability of CLDD to discharge to the southern rim ditch, described above. DONE and ENTERED this 29th day of September, 1983, in Tallahassee, Florida. P. MICHAEL RUFF Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 29th day of September, 1983.
Findings Of Fact Application No. 75-00196 is a request by the Standard Sand and Silica Company, for a consumptive water use permit. This application is for an existing use involving withdrawal from one well. The application seeks an average daily withdrawal of 1.6925 million gallons per day and a maximum daily withdrawal of 2.16 million gallons per day. The sought-for withdrawal will not exceed the water crop as defined by the district, with the withdrawal consumptively using only 35 percent of the water crop. The water will be used on site for the washing of sand. Mr. Clifton W. Golden is an adjacent landowner who testified that he was afraid of salt water intrusion and that a sink hole might develop because of the vast quantities of water taken from the aquifer by the applicant. He does not feel that the issuance of a permit would be consistent with the public interest. He presented no hydrological data showing that issuance of the permit would adversely affect his property. Mary Fausteen Thompson is a property owner adjacent to the site from which the water will be taken. She has had problems in the past with Standard Sand and Silica Company apparently discharging excess water on to her property. She thinks those problems may be occurring again, causing some of her property to be flooded. The sought-for consumptive use will not significantly induce salt water intrusion. Except as otherwise noted in the findings of fact, none of the conditions set forth in Subsection 16J-2.11(2), (3) or (4), F.A.C., will be violated. Several letters of objections have been received in addition to the objectors noted above. The Southwest Florida Water Management District's staff recommends issuance of the subject permit in the amounts requested with the following conditions: That no off-site runoff be permitted by the applicant. That flowmeters be placed on the well and quarterly reports made to the district.
Recommendation It is hereby RECOMMENDED that Application No. 75-00196 be granted with the conditions set forth in paragraph 7 above. ENTERED this 28th day of May, 1976, in Tallahassee, Florida. CHRIS H. BENTLEY, Hearing Officer Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Southwest Florida Water Management District P.O. Box 457 Brooksville, Florida 33512 Eugene W. Harris Standard Sand and Silica Co. P.O. Box 35 Davenport, Florida 33837 Mrs. Mary Fausteen Thompson Box 82-C, Evans Road Polk City, Florida Mr. Clifton W. Golden 800 Oriole Drive Virginia Beach, Florida 23451 Mr. John C. Jones Executive Director Florida Wildlife Federation 4080 North Haverhill Road West Palm Beach, Florida 33407
The Issue The issues to be determined in these consolidated cases are whether All Aboard Florida – Operations, LLC (“the Applicant”), and Florida East Coast Railway, LLC (“FECR”), are entitled to an Environmental Resource Permit Modification authorizing the construction of a stormwater management system and related activities to serve railway facilities, and a verification of exemption for work to be done at 23 roadway crossings (collectively referred to as “the project”).
Findings Of Fact The Parties Petitioners Martin County and St. Lucie County are political subdivisions of the State of Florida. Petitioners have substantial interests that could be affected by the District’s proposed authorizations. Intervenor Town of St. Lucie Village is a political subdivision of the State of Florida. Intervenor has substantial interests that could be affected by the District’s proposed authorizations. The Applicant, All Aboard Florida – Operations, LLC, is a Delaware limited liability company based in Miami. All Aboard Florida is part of a group of corporate entities formed for the principal purpose of developing and operating express passenger train service in Florida. Co-applicant Florida East Coast Railway, LLC, is a Florida limited liability company based in Jacksonville. FECR owns the existing railway corridor the passenger train service will use between Miami and Cocoa. South Florida Water Management District is a regional agency granted powers and assigned duties under chapter 373, part IV, Florida Statutes, including powers and duties related to the regulation of construction activities in wetlands. The proposed activities are within the boundaries of the District. Background The objective of the All Aboard Florida Project is to establish express passenger train service connecting four large urban areas: Miami, Fort Lauderdale, West Palm Beach, and Orlando. Most of the passenger service route, including the portion which will pass through Martin County and St. Lucie County, will use an existing railroad right-of-way used since the late 1800s. The FECR rail corridor runs along Florida’s east coast from Miami to Jacksonville. It supported passenger and freight operations on shared double mainline tracks from 1895 to 1968. The passenger service was terminated in 1968 and portions of the double track and certain bridge structures were removed. The freight service continued and remains in operation today. The passenger service will use the FECR right-of-way from Miami to Cocoa and then turn west on a new segment to be constructed from Cocoa to Orlando. The railway corridor will be operated as a joint facility, with passenger and freight trains sharing the double mainline tracks. The Applicant is upgrading the portion of the corridor between Miami and Cocoa by, among other things, replacing existing railroad ties and tracks, reinstalling double mainline tracks, and improving grade crossings. The Applicant is also installing Positive Train Control systems which provide integrated command and control of passenger and freight train movements and allow the trains to be directed and stopped remotely or automatically in the event of operator error or disability, or an obstruction on the track. The All Aboard Florida Project is being developed in two phases, Phase I extends from Miami to West Palm Beach, and Phase II from West Palm Beach to Orlando. This proceeding involves a segment within Phase II, known as Segment D09, which runs from just north of West Palm Beach to the northern boundary of St. Lucie County. The railway corridor in Segment D09 passes through Jonathan Dickinson State Park in Martin County and the Savannas Preserve State Park, parts of which are in both Martin County and St. Lucie County. Surface waters within these state parks are Outstanding Florida Waters (“OFWs”). The railway in Segment D09 also passes over the St. Lucie River using a bridge that can be opened to allow boats to pass. The Applicant plans to run 16 round trips per day between Miami and Orlando, which is about one train an hour in each direction, starting early in the morning and continuing to mid-evening. In 2013, the District issued the Applicant an exemption under section 373.406(6), which exempts activities having only minimal or insignificant adverse impacts on water resources. The 2013 exemption covers proposed work in approximately 48 of the 65 miles which make up Segment D09, and includes replacement of existing tracks and re-establishment of a second set of mainline tracks where they were historically located. The 2013 exemption covers all but 24 of the roadway crossings within Segment D09 where work is to be done in connection with the All Aboard Florida Project. In 2015, the District issued the Applicant a general permit under rule 62-330.401, which authorizes activities that are expected to cause minimal adverse impacts to water resources, for the installation of fiber optic cable along the rail bed within Segment D09. The 2013 exemption and 2015 general permit were not challenged and became final agency action. The Proposed Agency Actions The ERP Modification covers work to be done in approximately 17 of the 65 miles which make up Segment D09. The work will consist primarily of replacing existing tracks, installing new tracks, making curve modifications in some locations to accommodate faster trains, culvert modifications, and work on some fixed bridge crossings over non-navigable waters. The 2017 Exemption at issue in this proceeding covers improvements to 23 of the 24 roadway crossings that were not covered by the 2013 exemption. Proposed improvements at Southeast Florida Street in Stuart will be permitted separately. The improvements covered by the 2017 Exemption include upgrading existing safety gates and signals; installing curbs, guardrails, and sidewalks; resurfacing some existing paved surfaces; and adding some new paving. Petitioners argue that, because the District’s staff report for the ERP Modification states that the ERP does not cover work at roadway crossings, track work at roadway crossings has not been authorized. However, the staff report was referring to the roadway improvements that are described in the 2017 Exemption. The proposed track work at the roadway crossings was described in the ERP application and was reviewed and authorized by the District in the ERP Modification. “Segmentation” Petitioners claim it was improper for the District to separately review and authorize the proposed activities covered by the 2013 exemption, the 2015 general permit, the ERP Modification, and the 2017 Exemption. Petitioners contend that, as a consequence of this “segmentation” of the project, the District approved “roads to nowhere,” by which Petitioners mean that these activities do not have independent functionality. Petitioners’ argument is based on section 1.5.2 of the Applicant’s Handbook, Volume 1,1/ which states that applications to construct phases of a project can only be considered when each phase can be constructed, operated, and maintained totally independent of future phases. However, the activities authorized by the four agency actions are not phases of a project. They are all parts of Phase II of the All Aboard Florida Project, which is the passenger railway from West Palm Beach to Orlando. Section 1.5.2 is not interpreted or applied by the District as a prohibition against separate review and approval of related activities when they qualify under the District’s rules for exemptions, general permits, and ERPs. Much of Phase II is outside the District’s geographic boundaries and, therefore, beyond its regulatory jurisdiction. The District can only review and regulate a portion of Phase II. The District is unable to review this portion as a stand-alone railway project that can function independently from other project parts. The Proposed Stormwater Management System Where the Applicant is replacing existing tracks or re- establishing a second set of tracks, it will be laying new ties, ballast, and rail on previously-compacted earth. In those areas, no stormwater management modifications were required by the District. The Applicant’s new proposed stormwater management system will be located in a five-mile area of the corridor where an existing siding will be shifted outward and used as a third track. In this area, swales with hardened weir discharge structures and skimmers will be installed to provide stormwater treatment beyond what currently exists. The weir discharge structures will serve to prevent erosion at discharge points. The skimmers will serve to capture any floating oils or refuse. Because the FECR right-of-way is not wide enough in some three-track areas to also accommodate swales, the proposed stormwater management system was oversized in other locations to provide compensating volume. The District determined that this solution was an accepted engineering practice for linear systems such as railroads. Petitioners argue that the Applicant’s proposed stormwater management system is deficient because some of the proposed swales do not meet the definition of “swale” in section 403.803(14) as having side slopes equal to or greater than three feet horizontal to one foot vertical (3:1). The statute first defines a swale to include a manmade trench which has “a top width-to-depth ratio of the cross-section equal to or greater than 6:1.” The swales used in the proposed stormwater management system meet this description. Petitioners showed that the plans for one of the 46 proposed swales included some construction outside the FECR right-of-way. In response, the Applicant submitted revised plan sheets to remove the swale at issue. The Emergency Access Way The ERP application includes proposed modifications to portions of an existing unpaved emergency access way which runs along the tracks in some areas. The access way is a private dirt road for railroad-related vehicles and is sometimes used for maintenance activities. At the final hearing, Petitioners identified an inconsistency between an application document which summarizes the extent of proposed new access way construction and the individual plan sheets that depict the construction. The Applicant resolved the inconsistency by correcting the construction summary document. Petitioners also identified an individual plan sheet showing proposed access way modifications to occur outside of the FECR right-of-way. This second issue was resolved by eliminating any proposed work outside the right-of-way. Petitioners believe the proposed work on the access way was not fully described and reviewed because Petitioners believe the access way will be made continuous. However, the access way is not continuous currently and the Applicant is not proposing to make it continuous. No District rule requires the access way segments to be connected as a condition for approval of the ERP. Water Quantity Impacts An applicant for an ERP must provide reasonable assurance that the construction, operation, and maintenance of a proposed project will not cause adverse water quantity impacts to receiving waters and adjacent lands, adverse flooding to on-site or off-site property, or adverse impacts to existing surface water storage and conveyance capabilities. The District’s design criterion to meet this requirement for water quantity management is a demonstration that the proposed stormwater system will capture the additional runoff caused during a 25-year/3-day storm event. The Applicant’s proposed stormwater system meets or exceeds this requirement. Petitioners argue that the Applicant failed to provide reasonable assurance because the ERP application materials did not include a calculation of the discharge rates and velocities for water discharging from the swales during the design storm. The ERP application contains the information required to calculate the discharge rates and velocities and the Applicant’s stormwater expert, Bruce McArthur, performed the calculations and testified at the final hearing that in the areas where there will be discharges, the discharge rates and velocities would be “minor” and would not cause adverse impacts. The District’s stormwater expert, Jesse Markle, shared this opinion. Petitioners argue that this information should have been provided to the District in the permit application, but this is a de novo proceeding where new evidence to establish reasonable assurances can be presented. Petitioners did not show that Mr. McArthur is wrong. Petitioners failed to prove that the proposed project will cause adverse water quantity impacts, flooding, or adverse impacts to surface water storage and conveyance capabilities. Water Quality Impacts To obtain an ERP, an applicant must provide reasonable assurance that the construction, operation, and maintenance of a regulated project will not adversely affect the quality of receiving waters, such that state water quality standards would be violated. The District’s design criteria for water quality required the Applicant to show that its proposed stormwater system will capture at least 0.5 inches of runoff over the developed area. To be conservative, the Applicant designed its proposed system to capture 1.0 inch of runoff in most areas. Under District rules, if a stormwater system will directly discharge to impaired waters or OFWs, an additional 50 percent of water quality treatment volume is required. The proposed stormwater system will not directly discharge to either impaired waters or OFWs. In some locations, there is the potential for stormwater discharged from the proposed stormwater system to reach OFWs by overland flow, after the stormwater has been treated for water quality purposes. The Applicant designed its proposed stormwater system to provide at least an additional 50 percent of water quality treatment volume in areas where this potential exists. To ensure that the proposed construction activities do not degrade adjacent wetlands, other surface waters, or off-site areas due to erosion and sedimentation, the Applicant prepared an Erosion and Sediment Control Plan. Temporary silt fences and turbidity barriers will be installed and maintained around the limits of the construction. The District’s design criteria for water quality do not require an analysis of individual contaminants that can be contained in stormwater, except in circumstances that do not apply to this project. Compliance with the design criteria creates a presumption that water quality standards for all potential contaminants are met. See Applicant’s Handbook, V. II, § 4.1.1. Although not required, the Applicant provided a loading analysis for the proposed swales which could potentially discharge overland to impaired waters or OFWs. The analysis compared pre- and post-development conditions and showed there would be a net reduction in pollutant loading. Petitioners believe the pollutant loading analysis was inadequate because it did not specifically test for arsenic and petroleum hydrocarbons. However, the analysis was not required and adequate treatment is presumed. Petitioners did not conduct their own analysis to show that water quality standards would be violated. Petitioners’ expert, Patrick Dayan, believes the compaction of previously undisturbed soils in the emergency access way would increase stormwater runoff. However, he did not calculate the difference between pre- and post-construction infiltration rates at any particular location. His opinion on this point was not persuasive. Petitioners failed to prove that the proposed project will generate stormwater that will adversely affect the quality of receiving waters such that state water quality standards would be violated. The preponderance of the evidence shows the project complies with District design criteria and will not cause water quality violations. Soil and Sediment Contamination Petitioners argue that the ERP Modification does not account for the disturbance of existing contaminants in soils and sediments that could be carried outside of the right-of-way and into OFWs. Petitioners’ argument is based on investigations by their geologist, Janet Peterson, who collected soil, sediment, and surface water samples at 13 sites along the FECR rail corridor in the vicinity of OFWs, or surface waters that eventually flow into OFWs. During her sampling visits, Ms. Peterson saw no visual evidence of an oil spill, fluid leak, or other release of hazardous materials. Ms. Peterson compared her soil sample results to the Residential Direct Exposure Soil Cleanup Target Levels (“SCTLs”) established in rule 62-777. The SCTLs are the levels at which toxicity becomes a human health concern and the residential SCTLs assume soil ingestion of 200 mg/day for children, and 100 mg/day for adults, 350 days a year, for 30 years. Some of the soil sampling results showed exceedances of SCTLs, but the SCTLs are not applicable here because none of the sample sites are locations where children or adults would be expected to ingest soil at such levels for such lengths of time. Petitioners did not show that the contaminants are likely to migrate to locations where such exposure would occur. Ms. Peterson compared her soil sample results to the Marine Surface Water Leachability SCTLs, but she did not develop site-specific leachability-based SCTLs using DEP’s approved methodology. Nor did she show that the proposed project will cause the soils to leach the contaminants. Ms. Peterson collected sediment samples from shorelines, but not where construction activities are proposed. She compared her sediment sample results to the Florida Department of Environmental Protection’s (“DEP”) Sediment Quality Assessment Guidelines (“SQAGs”). These guidelines are not water quality standards. Any exceedance of these guidelines requires further analysis to determine potential water quality impacts. Ms. Peterson did not conduct the analysis. Ms. Peterson acknowledged that there are numerous sources for these pollutants at or near her sample sites, such as high-traffic roads, vehicular bridges, commercial and industrial facilities, boatyards, and golf courses. She did not establish baselines or controls. Ms. Peterson collected surface water samples at seven sites, some of which were located outside the FECR right-of-way. The results showed levels of phosphorous and nitrogen above the criteria for nutrients at some locations. Phosphorous, nitrogen, and the other nutrients are prevalent in the waters of Martin County and St. Lucie County and come from many sources. Petitioners’ evidence focused on existing conditions and not expected impacts of the proposed project. The evidence was insufficient to prove the proposed project will cause or contribute to water quality violations. Functions Provided by Wetlands and Other Surface Waters An applicant for an ERP must provide reasonable assurance that a proposed project will not adversely impact the value of functions provided to fish and wildlife and listed species by wetlands and other surface waters. Petitioners claim the Applicant and District should not have relied on Florida Land Use Cover and Forms Classification System (“FLUCCS”) maps to identify and characterize wetlands and other habitat areas because the maps are too general and inaccurate. However, the FLUCCS maps were not used by the Applicant or District to evaluate impacts to wetlands or other habitats. The Applicant began its evaluation of impacts to wetlands and other habitat areas by field-flagging and surveying the wetland and surface water boundaries in the project area using a GPS device with sub-meter accuracy. It then digitized the GPS delineations and overlaid them with the limits of construction to evaluate anticipated direct impacts to wetlands and other surface waters. The District then verified the delineations and assessments in the field. The Applicant and District determined that there are a total of 4.71 acres of wetlands within the FECR right-of-way, including tidal mangroves, freshwater marsh, and wet prairie. They also determined the proposed project will directly impact 0.35 acres of wetlands, consisting of 0.09 acres of freshwater marsh and 0.26 acres of mangroves. Petitioners contend that the Applicant failed to account for all of the project’s wetland impacts, based on the wetland delineations made by their wetland expert, Andrew Woodruff. Most of the impacts that Mr. Woodruff believes were not accounted for are small, between 0.01 and 0.05 acres. The largest one is acres. The Applicant’s delineations are more reliable than Mr. Woodruff’s because the methodology employed by the Applicant had greater precision. It is more likely to be accurate. Petitioners argue that the 2013 exemption and the 2015 general permit did not authorize work in wetlands and, therefore, the impacts they cause must be evaluated in this ERP Modification. However, Petitioners did not prove that there are unaccounted-for wetland impacts associated with those authorizations. Any impacts associated with best management practices for erosion control, such as the installation of silt fences, would be temporary. The District does not include such temporary minor impacts in its direct, secondary, or cumulative impacts analyses. Most of the wetlands that would be directly impacted by the ERP Modification are degraded due to past hydrologic alterations and soil disturbances from the original construction and historical use of the FECR railway corridor, and infestation by exotic plant species. Most of these wetlands are also adjacent to disturbed uplands within or near the rail corridor. The functional values of most of the wetlands that would be affected have been reduced by these disturbances. The Applicant provided reasonable assurance that the project will not adversely impact the value of functions provided to fish and wildlife and listed species by wetlands and other surface waters. Secondary Impacts Section 10.2.7 of the Applicant’s Handbook requires an applicant to provide reasonable assurance that the secondary impacts from construction, alteration, and intended or reasonably expected uses of a proposed activity (a) will not cause or contribute to violations of water quality standards or adverse impacts to the functions of wetlands or other surface waters; (b) will not adversely impact the ecological value of uplands for bald eagles, and aquatic or wetland-dependent listed animal species for nesting or denning by these species; (c) will not cause impacts to significant historical or archaeological resources; and (d) additional phases for which plans have been submitted, and closely linked projects regulated under chapter 373, part IV, will not cause water quality violations or adverse impacts to the functions of wetlands or other surface waters. The proposed work will be entirely within the limits of the existing railway corridor where secondary impacts to wetlands and other surface waters caused by noise, vibration, fragmentation of habitats, and barriers to wildlife have existed for decades. The preponderance of the evidence shows that any increase in these kinds of impacts would be insignificant and would not reduce the current functions being provided. Because the affected wetlands are not preferred habitat for wetland-dependent, endangered, or threatened wildlife species, or species of special concern, and no such species were observed in the area, no adverse impacts to these species are expected to occur. Petitioners contend that adverse impacts will occur to the gopher tortoise, scrub jay, and prickly apple cactus. These are not aquatic or wetland-dependent species. However, the preponderance of the evidence shows any increase in impacts to these species would be insignificant. When the train bridges are closed, boats with masts or other components that make them too tall to pass under the train bridges must wait for the bridge to open before continuing. Petitioners contend that the current “stacking” of boats waiting for the bridges to open would worsen and would adversely impact seagrass beds and the West Indian Manatee. However, it was not shown that seagrass beds are in the areas where the boats are stacking. The available manatee mortality data does not show a link between boat stacking and boat collisions with manatees. Mr. Woodruff’s opinion about increased injuries to manatees caused by increased boat stacking was speculative and unpersuasive. The preponderance of the evidence shows that the adverse effects on both listed and non-listed wildlife species, caused by faster and more numerous trains would be insignificant. The activities associated with the 2013 exemption and the 2015 general permit for fiber optic cable were based on determinations that the activities would have minimal or insignificant adverse impacts on water resources. These determinations are not subject to challenge in this proceeding. The Applicant provided reasonable assurance that the secondary impacts of the project will not cause or contribute to violations of water quality standards, adversely impact the functions of wetlands or other surface waters, adversely impact the ecological value of uplands for use by listed animal species, or cause impacts to significant historical or archaeological resources. Elimination and Reduction of Impacts Under section 10.2.1.1 of the Applicant’s Handbook, if a proposed activity will result in adverse impacts to wetlands and other surface waters, the applicant for an ERP must implement practicable design modifications to eliminate or reduce the impacts, subject to certain exceptions that will be discussed below. Petitioners argue that this rule requires the Applicant and District to evaluate the practicability of alternative routes through the region, routes other than the existing railway corridor in Segment D09. As explained in the Conclusions of Law, that argument is rejected. The evaluation of project modifications to avoid impacts was appropriately confined to the railway corridor in Segment D09. The Applicant implemented practicable design modifications in the project area to reduce or eliminate impacts to wetlands and other surface waters. Those modifications included the shifting of track alignments, the elimination of certain third-track segments, and the elimination of some proposed access way modifications. However, the project qualified under both “opt out” criteria in section 10.2.1.2 of the Applicant’s Handbook so that design modifications to reduce or eliminate impacts were not required: (1) The ecological value of the functions provided by the area of wetland or surface water to be adversely affected is low, and the proposed mitigation will provide greater long-term ecological value; and (2) the applicant proposes mitigation that implements all or part of a plan that provides regional ecological value and provides greater long-term ecological value. Mitigation The Applicant proposes to mitigate for impacts to wetlands by purchasing mitigation credits from four District- approved mitigation banks: the Bluefield Ranch, Bear Point, Loxahatchee, and F.P.L. Everglades Mitigation Banks. Each is a regional off-site mitigation area which implements a detailed management plan and provides regional long-term ecological value. The number of mitigation credits needed to offset loss of function from impacts to wetlands was calculated using the Modified Wetland Rapid Assessment Procedure (“MWRAP”) or Wetland Assessment Technique for Environmental Review (“WATER”), as prescribed in the state permit for each mitigation bank. Applying these methods, the Applicant is required to purchase mitigation credits. The Applicant proposed to mitigate the adverse impacts to freshwater marsh wetlands by purchasing 0.01 freshwater herbaceous credits from the Bluefield Ranch Mitigation Bank, and 0.06 freshwater herbaceous credits from the Loxahatchee Mitigation Bank. The adverse impacts to tidal mangrove wetlands would be mitigated by purchasing 0.12 saltwater credits from the Bear Point Mitigation Bank, and 0.02 saltwater credits from the F.P.L. Everglades Mitigation Bank. The Applicant committed to purchase an additional 0.29 freshwater herbaceous credits from the Bluefield Ranch Mitigation Bank, for a total of 0.50 mitigation credits. The proposed mitigation implements a plan that will provide greater long-term ecological value than is provided by the wetlands that will be impacted. The Applicant proved by a preponderance of the evidence that the project complies with the District’s mitigation requirements. Cumulative Impacts To obtain an ERP, an applicant must provide reasonable assurance that a regulated activity will not result in unacceptable cumulative impacts to water resources. This assurance can be provided by proposing to fully mitigate the impacts within the same basin. However, when an applicant proposes mitigation in another drainage basin, the applicant must demonstrate that the regulated activity will not cause unacceptable cumulative impacts. The proposed project will adversely impact 0.02 acres of freshwater marsh wetlands and 0.21 acres of tidal mangrove wetlands in the St. Lucie River basin. The impacts to the freshwater marshes must be mitigated out-of-basin because there are no mitigation banks in the basin which offer freshwater herbaceous mitigation credits. The proposed project will adversely impact 0.07 acres of the freshwater marshes and 0.05 acres of the mangrove wetlands in the Loxahatchee River basin. Those impacts must also be mitigated out-of-basin because there are no mitigation banks in the Loxahatchee River basin. Because some of the Applicant’s proposed mitigation must be provided out-of-basin, the ERP application included a cumulative impact analysis. The analysis evaluated whether the proposed project, when considered in conjunction with other possible development within the St. Lucie River and Loxahatchee River drainage basins, would result in unacceptable cumulative impacts considering each basin as a whole. There are approximately 10,068 acres of freshwater marshes within the St. Lucie basin, of which an estimated 4,929 acres are not preserved and would be at risk of potential future development. The proposed project will adversely impact 0.02 of those acres, which is only 0.0004 percent of the total at-risk acreage. There are about 34,000 acres of freshwater marshes within the Loxahatchee River basin, of which an estimated 7,463 acres are at risk of future development, and approximately 564 acres of tidal mangrove wetlands, of which an estimated 75 acres are at risk of future development. The project will adversely impact 0.07 acres of the freshwater marshes (0.0009 percent), and 0.05 acres of the tidal mangrove wetlands (0.0667 percent). Petitioners contend the Applicant’s analysis did not account for impacts from proposed activities authorized in the 2013 and 2015 general permit. However, Petitioners failed to prove there are unaccounted-for wetland impacts. The preponderance of the evidence supports the District’s determination that the proposed project will not cause unacceptable cumulative impacts to wetlands and other surface waters. Public Interest When an applicant seeks authorization for a regulated activity in, on, or over wetlands or surface waters, it must provide reasonable assurance that the activity will not be contrary to the public interest, or if the activity is within or significantly degrades an OFW, is clearly in the public interest, as determined by balancing the following criteria set forth in section 373.414(1)(a): Whether the activities will adversely affect the public health, safety, or welfare or the property of others; Whether the activities will adversely affect the conservation of fish and wildlife, including endangered or threatened species, or their habitats; Whether the activities will adversely affect navigation or the flow of water or cause harmful erosion or shoaling; Whether the activities will adversely affect the fishing or recreational values or marine productivity in the vicinity of the activity; Whether the activities will be of a temporary or permanent nature; Whether the activities will adversely affect or will enhance significant historical and archaeological resources; and The current condition and relative value of functions being performed by areas affected by the proposed activities. The proposed work is not within an OFW, but entirely within the FECR corridor. The potential for overland flow and indirect impacts to OFWs is addressed by additional treatment of the stormwater prior to discharge. The proposed project would not significantly degrade an OFW. Therefore, the applicable inquiry is whether the project is contrary to the public interest. Factor 1: Public Safety, Safety, and Welfare Petitioners contend that the proposed project will adversely affect public health, safety, and welfare by impacting water quantity, water quality, and certain non-environmental matters such as emergency response times, traffic congestion, and potential train collisions with pedestrians and vehicles. Potential environmental impacts have been addressed above and, by a preponderance of the evidence, the District and the Applicant showed that such impacts would be insignificant or would be mitigated. As to the potential for non-environmental impacts associated with train operations, it is explained in the Conclusions of Law that the public interest test does not include consideration of non-environmental factors other than those expressly articulated in the statute, such as navigation and preservation of historical or archaeological resources. However, because evidence of non-environmental impacts was admitted at the final hearing, the issues raised by Petitioners will be briefly addressed below. The regulatory agency with specific responsibility for railroad safety is the Federal Railroad Administration (“FRA”). The FRA reviewed the safety features associated with the proposed passenger train operations, and approved them. Public safety will be enhanced at roadway crossings because of the proposed improvements and the use of modern technology in monitoring and managing the movement of trains. Petitioners contend that the addition of the passenger rail service will impede emergency response times in Martin County and St. Lucie County due to more frequent roadway closures. However, freight trains currently impede emergency response times due to their length and slow speed. The passenger trains will be much shorter in length and faster so that roadway crossing closures for passing passenger trains will be much shorter than for freight trains. The ERP Modification and 2017 Exemption do not affect freight train operations. The preponderance of the evidence shows that passenger rail service is unlikely to cause a material increase in the occurrence of circumstances where an emergency responder is impeded by a train. The current problem must be addressed through changes in freight train operations. Petitioners also contend that the passenger rail service will interfere with hurricane evacuation. The persuasive evidence does not support that contention. Train service would cease when a hurricane is approaching. Petitioners contend the trains will have to be “staged” on either side of the two moveable bridges while other trains cross, thereby blocking road intersections. However, this was a matter of speculation. The Applicant does not propose or want to stage trains at the bridges. Petitioners contend that the project will cause hazards to boaters on the St. Lucie River because there will be more times when the train bridge will be closed to allow the passage of passenger trains. Although there were many statistics presented about the number of boats affected, the evidence was largely anecdotal with respect to the current hazard associated with boaters waiting for the passage of freight trains and speculative as to the expected increase in the hazard if shorter and faster passenger trains are added. Factor 2: Conservation of Fish and Wildlife As previously found, the proposed activities will not adversely affect the conservation of fish and wildlife, including threatened or endangered species. The preponderance of the evidence shows the project will have only insignificant adverse impacts on water resources and wildlife. Factor 3: Navigation of the Flow of Water Petitioners claim the project will hinder navigation on the St. Lucie and Loxahatchee Rivers because of the increase in bridge closures if passenger trains are added. The U.S. Coast Guard is the agency with clear authority to regulate the opening and closing of moveable train bridges over navigable waters in the interests of navigation. Petitioners’ insistence that the District address the bridge openings is novel. No instance was identified by the parties where this District, any other water management district, or DEP has attempted through an ERP to dictate how frequently a railroad bridge must open to accommodate boat traffic. The Coast Guard is currently reviewing the project’s potential impacts on navigation and will make a determination about the operation of the moveable bridges. It has already made such a determination for the moveable bridge which crosses the New River in Ft. Lauderdale. Petitioners point to section 10.2.3.3 of the Applicant’s Handbook, which states that the District can consider an applicant’s Coast Guard permit, and suggest that this shows the District is not limited to what the Coast Guard has required. However, Section 10.2.3.3 explains the navigation criterion in terms of preventing encroachments into channels and improving channel markings, neither of which encompasses the regulation of train bridges. The preponderance of the evidence shows the project would not cause harmful erosion or shoaling or adversely affect the flow of water. Factor 4: Fishing, Recreational Values, and Marine Productivity The preponderance of the evidence shows that there would be no adverse impacts or only insignificant impacts to fishing or recreational values and marine productivity. Factor 5: Permanent Impact The proposed project will have both temporary and permanent impacts. The temporary impacts include the installation of silt fences and turbidity barriers designed to reduce water quality impacts and impacts to functions provided by wetlands and surface waters. The impacts due to track installation, construction and rehabilitation of the non-moveable bridges, at-grade crossing improvements, and stormwater system improvements are permanent in nature. The permanent impacts have been minimized and mitigated. Factor 6: Historical or Archaeological Resources Petitioners do not contend that the project will adversely affect significant historical or archaeological resources. Factor 7: Wetland Functions in Areas Affected Because the proposed work is within the limits of an existing railway corridor where impacts have been occurring for decades, and the majority of the wetlands to be affected are of a low to moderate quality, there would be only a small loss of functional values and that loss would be fully mitigated. Public Interest Summary When the seven public interest factors are considered and balanced, the proposed project is not contrary to the public interest. Even if Petitioners’ non-environmental issues are included, the project is not contrary to the public interest. Compliance With Other Permit Conditions The project is capable, based on accepted engineering and scientific principles, of performing and functioning as proposed. The Applicant demonstrated sufficient real property interests over the lands upon which project activities will be conducted. It obtained the required consent for proposed activities relating to bridge crossings over state-owned submerged lands. The Applicant provided reasonable assurance of compliance with all other applicable permit criteria. Exemption Verification for Roadway Crossings The Applicant’s ERP application included a mixture of activities which required an individual permit, as well as activities in roadway crossings which the Applicant claimed were exempt from permitting. Pursuant to section 5.5.3.4 of the Applicant’s Handbook, the Applicant requested a verification of exemption as to certain work to be done within 23 of those 24 roadway crossings. The District determined that the improvements for which an exemption was sought were exempt from permitting under rule 62-330.051(4)(c) for minor roadway safety construction, rule 62-330.051(4)(d) resurfacing of paved roads, and rule 62-330.051(10) for “construction, alteration, maintenance, removal or abandonment of recreational paths for pedestrians, bicycles, and golf carts.” The preponderance of the evidence shows the proposed work qualifies for exemption under these rules.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the South Florida Water Management District enter a final order that: approves Environmental Resource Permit Modification No. 13-05321-P on the terms and conditions set forth in the District’s Corrected Proposed Amended Staff Report of May 11, 2017; and approves the Verification of Exemption dated March 31, 2017. DONE AND ENTERED this 29th day of September, 2017, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER 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 29th day of September, 2017.
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.
Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: This controversy began on July 9, 1990, when petitioners, David and Victoria Page, filed an application with the district office of respondent, Department of Environmental Regulation (DER), seeking the issuance of a permit authorizing certain construction activities (including the erection of a seawall) on their residential lot located at 3108 Gulfwinds Circle, Hernando Beach, Florida. The property faces west on the Gulf of Mexico, a water body designated as a Class III water in the State. The application was eventually deemed to be complete on October 24, 1990. After conducting a review of the application and an on-site inspection of the property, on January 18, 1991, DER issued its notice of permit denial. The notice identified the reasons for the denial as being petitioners' failure to give reasonable assurances that water quality standards would not be violated and that the project would be in the public interest. Also, DER cited expected adverse cumulative impacts if the application was granted. The notice provided further that if petitioners agreed to locate their seawall landward of the jurisdictional line, the project would be approved. In July 1991, petitioners amended their application to propose that the seawall be constructed even further seaward of the jurisdictional line. When efforts to resolve the case were unsuccessful, petitioners requested a formal hearing on January 17, 1992, to contest the agency's decision. Petitioners purchased their property in 1989. It lies within Unit 2 of Gulf Coast Retreats, a residential subdivision in Hernando Beach, Florida. The property is identified as lot 20 on Gulfwinds Circle and fronts the Little Pine Island Bay (Bay), which is a part of the Gulf of Mexico. Access to the Gulf is provided by a channel (six feet in depth) in the Bay in front of lot 20 and which eventually runs into the Gulf several miles south of petitioners' lot. It is undisputed that in 1985 Hurricane Elena passed offshore causing erosion to lot 20 and other adjacent lots. Consequently, the upland portion of the lot is now smaller than before the hurricane. However, petitioners purchased their property in that state of condition. Lots 19 and 21 are on the south and north sides of petitioners' property and are owned by the Steins and Budricks, respectively. Both neighbors have constructed vertical concrete seawalls in front of their homes. Budrick was issued a permit to construct a seawall on December 28, 1989, while Stein constructed his without a permit. However, Stein has subsequently filed an after-the-fact permit application and was recently advised by DER that the application was complete. At hearing, a DER representative expressed the view that the Stein application will probably be approved since his wall is landward of the DER jurisdictional line. It is noted that the Stein and Budrick seawalls sit back from the original property lines because of the erosion suffered during the 1985 hurricane and correspond to the jurisdictional line established by DER on their property. Another application for a permit to construct a seawall was filed by the owner of lot 18 in March 1992. Like Stein and Budrick, that owner proposed to construct his wall on the landward side of the jurisdictional line. Petitioners, who live in Kansas, desire to construct a home on their lot. They have proposed to place one hundred cubic yards of fill (limerock) on 1,065 square feet of intertidal wetlands on the western end of their lot and construct a 110-foot vertical seawall up to thirty feet seaward of the jurisdictional line. Thus, there will be dredge and filling activities in the Gulf of Mexico, a class III water of the state, thereby invoking the jurisdiction of DER. By law, DER is required to establish a jurisdictional line to show the landward extent of waters of this state, including the Gulf of Mexico. Such extent is normally defined by species of plants or soils which are characteristic of those areas subject to regular and periodic inundation by the waters of the state. As a general practice, using a prescribed plant or species indicator list, DER makes an on-site inspection of the property to determine what vegetation, if any, is found on the property and is subject to regular and periodic inundation by the waters. In this case, the dominant vegetation found on lot 20 was paspalum distichum, a plant on the species list subject to regular and periodic inundation by the Gulf waters. Accordingly, DER observed where the vegetation ended and used that point for the placement of the jurisdictional line. As a cross check, DER also noted the rack line, which is indicative of the landward extent to which the high tides rise, and found it to correspond to the vegetation line. It should be noted that the jurisdictional line established on petitioners' property corresponds with the line drawn on lots 18, 19 and 21, and if that line is used to construct the seawall on lot 20, the seawalls on all four lots would run in a straight line. Although petitioners objected to the jurisdictional line as established by DER, they offered no credible evidence to show that it was improper or should have been placed at a different location. On January 9 and 15, 1991, Richard W. Pugh, a DER field environmental specialist, conducted an on-site inspection of the property and adjacent waters. He also was responsible for establishing the jurisdictional line. Finding numerous adverse environmental effects that would occur if the permit was granted as proposed, Pugh recommended that the application be denied. This recommendation was accepted by the deputy assistant secretary for DER's Southwest District Office and a notice of permit denial was accordingly issued. The bases for the denial were that (a) reasonable assurances had not been given by petitioners that water quality standards would be satisfied; (b) a cumulative adverse impact on the area would occur if the permit was approved, and (c) petitioners had failed to give reasonable assurances that the project was in the public interest. In order to prove entitlement to a permit, petitioners must give reasonable assurance that water quality standards will not be violated and that the project is in the public interest. In this respect, they offered no evidence to provide these assurances. This in itself supports a finding that no entitlement to a permit has been shown. Even so, the agency elected to present evidence on these issues after petitioners' case-in-chief was concluded. Findings of fact drawn from that evidence are set forth below. On April 6, 1992, a DER marine biologist, Dr. George H. Farrell, visited the site and conducted a biological evaluation of the composition of the benthic community in the intertidal and subtidal wetlands which would be impacted by the project. Based on his tests and observations, Dr. Farrell concluded that the project as proposed would have an adverse impact on marine and wildlife resources in the area. This is because the area has very good water quality, contains a high species diversity, performs an integral part in the food web, and serves a valuable nursery function for estuarine dependent juvenile fish species and a corridor function for migrating estuarine dependent fish species. This testimony was not challenged by petitioners and is hereby accepted. 1/ In granting or denying a water resource permit, DER is also required to consider certain statutory criteria found in Subsection 403.918(2), Florida Statutes, to determine whether a project is in the public interest. Although petitioners did not address these criteria, and thus failed to give any assurances that the project is in the public interest as required by law, testimony adduced by DER established that under petitioners' proposal, there will be a permanent loss of 1,065 square feet of intertidal wetlands due to filling activities. These wetlands are now used by fish and wildlife habitat and will no longer be available for use. In addition, the same area is used as a nursery area by a variety of fish species. As such, the project will adversely affect the conservation of fish and wildlife and their habitats and will adversely affect the fishing values and marine productivity in the vicinity. Second, because petitioners' proposed seawall will jut out from their neighbors' walls by as much as thirty feet, and the corners of the seawall in that configuration will result in erosion or shoaling depending on whether the waters are moving north or south, the project will cause harmful erosion or shoaling. Third, because the wall is being constructed of concrete and steel and is not temporary, the project will be of a permanent nature and thus have a permanent adverse impact. Finally, the ecological functions being performed in the immediate vicinity of the project are extremely important and the elimination of this zone will significantly impair those functions. Collectively, these considerations support a finding that the project is not in the public interest. DER has a policy of not granting a permit if adverse cumulative impacts may be expected as a result of granting that permit. This policy is derived from a statute (s. 403.919, F.S.) requiring such impacts to be considered in the permitting process. In the case at bar, DER reasonably predicts that if it granted petitioners' application and authorized them to construct a seawall which jutted out up to thirty feet beyond their neighbors' walls, it would be obligated to grant similar permits to property owners on adjacent lots. Because petitioners' application will have an adverse impact on the water quality and is contrary to the public interest, the granting of additional permits would exacerbate those impacts. When an applicant proposes to fill (destroy) wetlands, and the applicant is unable to meet the public interest criteria set forth in subsection 403.918(2), DER shall consider measures proposed by or acceptable to the applicant to mitigate the adverse effects caused by the project. In this case, no mitigative measures were proposed by petitioners. At hearing, petitioners' representative asserted that in June 1991, the Cabinet (presumably sitting as the Board of Trustees of the Internal Improvement Trust Fund) implemented a new "policy" which allows property owners to "recover and bulkhead" land previously lost due to avulsion and erosion. He further represented that such requests were to be filed within five years after the event (hurricane). Although petitioners were not the property owners when the event occurred, and more than five years has elapsed, in July 1991 petitioners filed a request with the Department of Natural Resources (DNR) to reclaim and bulkhead their property and that request remained pending as of the date of hearing. A copy of the policy itself (or rule, if any, implementing the policy) was not made a part of this record. Even so, there was no evidence to establish that the granting of that application would require DER to grant a water resource permit, and DER takes the position that the request has no bearing on the issue of whether a water resource permit should be issued to petitioners.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that a final order be entered denying petitioners' application for a water resource permit. DONE and ENTERED this 27th day of April, 1992, in Tallahassee, Florida. DONALD R. ALEXANDER Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 27th day of April, 1992.
The Issue The issue in this case is whether Water Use Permit (WUP) Application Number 20009478.005 meets the conditions for issuance as established in Section 373.223, Florida Statutes (2001), Florida Administrative Code Rule 40D-2.301 (April 2001), and the District’s Basis of Review for Water Use Permit Applications.
Findings Of Fact The Parties Petitioner, Alan Behrens, owns real property and a house trailer located at 4070 Southwest Armadillo Trail, in Arcadia, Florida. Behrens uses a two-inch well as the primary source of running water for his trailer. Boran and his family operate a ranch and sod farm in Arcadia, Florida, under the limited partnership of Boran Ranch and Sod, Ltd. Boran uses several different on-site wells to irrigate the farm. See Findings 12-17, infra. 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 Florida Administrative Code Rule Chapter 40D. Permit History Boran’s property is a little over 1,000 acres in size, on which he has raised cattle and grown sod for approximately the past four years. Before Boran owned the property, its prior occupants used the land for growing fall and spring row crops (primarily tomatoes). Boran's cattle and sod farm uses less water than was used by previous owners and occupants. In 1989, the original permit holders could make annual average daily withdrawals of 309,000 gallons but also were allowed a maximum daily withdrawal of 6,480,000 gallons. In 1992, the permitted withdrawals increased to an annual average daily quantity of 2,210,000 gallons, with a peak monthly limit of 3,596,000 gallons per day. On December 14, 1999, Boran received an agricultural water use permit (WUP No. 20009478.004) from the District. This current existing permit expires on December 14, 2009. The current permit grants Boran the right to withdraw groundwater for his agricultural use in the annual average daily quantity of 1,313,000 gallons, and with a peak month daily quantity of 3,177,000 gallons. On September 11, 2000, Boran filed an application to modify his existing water use permit. Modification of Boran's existing permit does not lengthen the term of the permit, and the scope of the District's review was limited to those features or changes that are proposed by the modification. The proposed modification would allow Boran to increase his annual average daily quantity by 175,000 gallons, and increase the peak month daily quantity by 423,900 gallons, for the irrigation of an additional 129 acres of sod. With the proposed increase, the new annual average daily quantity will be 1,488,000 gallons, and the new peak month daily quantity will be 3,600,900 gallons. The proposed modification also provides for the construction of an additional well (DID #6) on the southeastern portion of property, which will withdraw groundwater from the upper Floridan aquifer. The proposed agency action also entails a revision of the irrigation efficiency rating for the entirety of Boran Ranch. Irrigation efficiency refers to the ability to direct water to its intended target, which in this case means the root zone of the sod, without losing water to evaporation and downward seepage. Under the proposed permit modification, Boran will increase the entire farm’s water efficiency from 65 percent to 75 percent. As discussed further in the Conditions for Issuance section infra, the District's AGMOD modeling program uses this efficiency rating as part of its determination of the appropriate quantities for withdrawals. The higher the efficiency rating, the less water received under a permit. Because the efficiency rating increased, the application rate for water decreased from 42" per year to 36.4" per year for the entire Boran Ranch. Boran's Wells There are six well sites (labeled according to District identification numbers, e.g., DID #3) existing or proposed on Boran’s property. DID #1 is an eight-inch well located in the northeastern portion of the property. DID #1 provides water solely from the intermediate aquifer. DID #2 is an eight-inch well located in the middle of the property. DID #2 withdraws water from both the intermediate and upper Floridan aquifers. Both DID #1 and DID #2 were installed in 1968, and predate both the first water use permit application for the farm and the District's water use regulatory system. DID #4 is a twelve-inch well located in the north- central part of the property and solely taps from the upper Floridan aquifer. DID #4 had already been permitted and constructed as of the date of the proposed modification application at issue in this case. DID #3 and DID #5 are twelve-inch wells which have already been permitted for the southern and northern portions of the property, respectively, but have not yet been constructed. Both wells will withdraw water only from the upper Floridan aquifer. DID #6 is a proposed twelve-inch well to be located on the southeastern portion of the property and to irrigate an additional area of sod. DID #3, #5, and #6 will all be cased to a depth of approximately 540 feet, and only open to the upper Floridan aquifer to a depth of approximately 940 feet. By casing the well with pipe surrounded by cement, these wells will be sealed off to all aquifers above 540 feet, including the intermediate aquifer. All the wells on the property are used to irrigate sod. The wells have artesian flow, but utilize diesel pumps to provide consistent flow pressure year-round throughout the fields (some of which can be a mile and a half from a well). Since running the pumps costs money, there is an economic incentive not to over-irrigate. In addition, over-irrigation can lead to infestations of fungi and insects, and eventually cause the grass to rot and die. As a result, the fields receive irrigation only when dry areas in the fields appear and the grass begins to wilt. Boran Ranch Operations and Management Practices Boran Ranch primarily grows three kinds of grasses: St. Augustine Floratam; St. Augustine Palmetto; and Bahia. (Boran also is experimenting on a smaller scale with common paspalum and common Bermuda.) The Bahia grass, which is what also grows in the ranch's cattle pasture, does not require irrigation; the St. Augustine grasses are less drought- resistant and require irrigation at times. The majority of the sod sold to residential installers (who ordinarily work for landscape companies) is a St. Augustine grass. Commercial or governmental roadside installations favor Bahia. Currently, Boran sells more Bahia than St. Augustine. But market demand determines which types of grass are produced on the farm. As residential use and demand for St. Augustine in southwest Florida increases, so would the proportion of the farm used for growing St. Augustine grass. Boran grows sod year-round because of a large demand for the product in Ft. Myers and Cape Coral, and to a lesser extent in Punta Gorda and Port Charlotte. Sod helps control erosion and is considered to have aesthetic value. There also was some evidence that sod lowers the ambient temperatures, as compared to bare dirt; but the evidence was not clear how sod would compare to other ground cover in lowering temperatures. When subsurface seepage irrigation is being used, a sod field must be disked and "laser-leveled" to the proper elevation, with a slight slope created in the field to help ensure proper irrigation and drainage, before it can be used for sod production. The fields are laser-leveled before the irrigation system is installed and the crop is planted. The perforated irrigation supply lines of Boran Ranch’s subsurface irrigation system, also known as the "tile," run the opposite direction of the slope of the field and perpendicular to the main irrigation line. Once the subsurface irrigation system is installed, the field receives sprigs of sod, which are then watered and "rolled" to pack them into the ground. Approximately three months after a field has been rolled, the new sod is then periodically fertilized, sprayed and mowed. Sod takes approximately one year to grow before it may be harvested. The sod at Boran Ranch is harvested via tractor with a "cutter" on its side, which cuts underneath the grass, lifts it up onto a conveyor belt, and then onto a pallet for shipping. There are four different types of irrigation systems used for growing sod in Florida: (1) pivot systems which rely on sprinklers attached to overhead lines that rotate around a fixed point; (2) overhead rain guns which utilize motorized hydraulic pressure to spray a field; (3) above-ground seepage; and (4) subsurface irrigation systems (which can also be used to drain excess water from fields during large rain events). The most efficient irrigation system used for sod in Florida is the subsurface irrigation system. Boran Ranch first started the subsurface irrigation system approximately four years ago. Since that time, Boran Ranch has converted almost all its fields to the subsurface irrigation system, at a cost of approximately $1150 to $1350 per acre. As a result of this conversion process, Boran Ranch now uses less water per acre of sod. The subsurface irrigation system delivers water from a well to a water control structure (also known as the "box") via the imperforated main irrigation line. The perforated lines of the "tile" are connected to this main irrigation line at a 90-degree angle. The largest portion of the "box" sits underground. Once the water in the main irrigation line reaches the "box," water builds up behind removable boards contained in the box, creating the backpressure which forces water out into the tile. Water flows out from the tile to maintain the water table level at or near the root zone of the sod. Subsurface irrigation systems only function on property that has a hardpan layer beneath the soil. The hardpan layer acts as a confining unit to minimize the downward seepage of water, thereby allowing the subsurface irrigation system to work efficiently. Behrens questioned whether Boran Ranch has the necessary hardpan based on Todd Boran's reliance on hydrogeologists for this information. But the expert testimony of Boran's hydrogeology consultant and the District's hydrogeologist confirmed Todd Boran's understanding. Typically, the highest board in the box has the same height as the top of the field. Once the water level inside the box surpasses the height of the last board, water will spill over that board into the remainder of the box and then out another main irrigation line to the next box and set of tiles. By removing some of the boards in the box, Boran can bypass irrigating certain sections of his fields in favor of other areas. Excess water from the fields flows into field ditches which lead to wetlands on the property. If water leaves the wetlands during episodes of heavy rains, it flows downstream to the Peace River. Conditions for Issuance Boran Ranch is located in southwestern DeSoto County, in an area designated by the District as the Southern Water Use Caution Area (SWUCA). The District created the SWUCA, which covers 5,000 square miles, after first determining that the groundwater resources of eastern Tampa Bay and Highlands Ridge regions were stressed and creating the Eastern Tampa Bay Water Use Caution Area (ETBWUCA) and Highlands Ridge Water Caution Area (HRWUCA). Both the ETBWUCA and the HRWUCA are contained within the larger boundaries of the SWUCA. Within the ETBWUCA is an area along the coasts of portions of Hillsborough, Manatee, and Sarasota counties known as the Most Impacted Area (MIA). Special permitting rules exist for new projects located within the ETBWUCA, HRWUCA, and MIA, but not within the remainder of the "undifferentiated" SWUCA. Boran Ranch is located in this "undifferentiated" area of the SWUCA. Behrens took the position that Boran should not be permitted any additional water use until special permitting rules are promulgated for the "undifferentiated" SWUCA. But Behrens could cite no authority for such a moratorium. Meanwhile, the more persuasive evidence was that no such moratorium would be reasonable or appropriate. The evidence proved that the quantities authorized by the proposed modification are necessary to fulfill a certain reasonable demand, as required by Rule 40D- 2.301(1)(a). Boran sought additional water quantities through the permit modification application in order to irrigate an additional 129 acres of its sod farm. The application reflects a need for additional water, associated with additional acreage added to the farm. Boran used the District's AGMOD spreadsheet model, which is based on a mathematical methodology known as the modified Blainey-Criddle method, to determine the reasonable quantities for Boran's specific agricultural use. AGMOD inputs into its computations the following variables: (1) geographic location of the proposed use; (2) type of crop grown; (3) irrigation (efficiency); (4) pump capacity; (5) soil type; and (6) number of acres to be irrigated. AGMOD is a generally accepted tool used for determining the allocation of water quantities for agricultural use. In the instant case, the AGMOD calculations incorporated 87 years of rainfall data and its results reflect the quantities necessary in the event of a two-in-ten-year drought. Similarly, the AGMOD calculations in the instant case take into account the change in irrigation efficiency from 65 percent to 75 percent. Behrens suggested that Boran should not be allowed to use any more water until minimum flows and levels are established for the intermediate aquifer in the vicinity. However, Behrens could cite no authority for imposing such a moratorium. Meanwhile, the more persuasive evidence was that no such moratorium would be reasonable or appropriate. See Finding 49 and Conclusion 86, infra. Behrens also suggested that inputs to AGMOD should assume more Bahia and less St. Augustine grass so as to reduce the resulting amount of reasonable demand. He also suggested that Boran's reasonable demand should not take into account possible future increases in St. Augustine grass production based on possible future market demand increases. But it does not appear that the District requires an applicant to differentiate among various types of grasses when inputting the crop type variable into the AGMOD model for purposes of determining reasonable demand. See Water Use Permit Information Manual, Part C, Design Aids (District Exhibit 2C), Table D-1, p. C4-9. The evidence proved that Boran demonstrated that the proposed use will not cause quantity or quality changes that adversely impact the water resources, on either an individual or cumulative basis, including both surface and ground waters, as required by Rule 40D-2.301(1)(b). Data from water quality monitoring reports indicate that water quality at Boran Ranch and in the region has remained fairly consistent. There were no statistically significant declining trend in water levels in the region. Behrens admitted that water quality in his well has been consistently good. One apparent increase in total dissolved solids and chlorides in DID #1 was explained as being a reporting error. Boran inadvertently reported some findings from DID #2 as coming from DID #1. Until the error was corrected, this made it appear that water quality from DID #1 had decreased because, while DID #1 is open only to the intermediate aquifer, DID #2 is open to both the intermediate aquifer and the upper Florida aquifer, which has poorer water quality. Both Boran and the District used the MODFLOW model, a generally accepted tool in the field of hydrogeology, to analyze withdrawal impacts. The purpose of modeling is to evaluate impacts of a proposed use on the aquifer tapped for withdrawals, and any overlying aquifers including surficial aquifers connected to lakes and wetlands. MODFLOW uses mathematics to simulate the different aquifer parameters for each production unit determined from aquifer performance testing. During the permit application process, both Boran and the District conducted groundwater modeling by simply adding the proposed new quantities to models developed for Boran's permit application in 1999. The models were comparable but not identical; the District's model was somewhat more detailed in that it separated predicted drawdowns into more aquifer producing units. Both models satisfied the District that the proposed modification would have no adverse impact on water resources. After the challenge to the Proposed Agency Action, the District created a new model to assess the impact of only the additional quantities requested by the modification. This new model added some aquifer parameters obtained from Regional Observation Monitoring Program (ROMP) well 9.5, which was constructed very close to the Boran Ranch in 1999. (Information from ROMP 9.5 was not available at the time of the earlier models.) The new model allowed the District to limit the scope of its review to those changes proposed by the modification. The results of this model show that impacts are localized and that most are within the confines of Boran’s property. The greatest impacts resulting from the proposed modification would occur in the Suwannee Limestone producing unit (the upper-most portion of the upper Floridan aquifer), the unit to be tapped by DID #6. The confining unit above the upper Floridan aquifer in this region of DeSoto County is approximately 300-400 feet thick, and impacts on the intermediate aquifer, which is above this confining unit, are much less. When the District's new model was run for peak monthly withdrawals (423,900 gpd for 90 days), the model's 1.0 foot drawdown contour was contained within the confines of Boran’s property, and the 0.1 foot drawdown contour extended only approximately two miles out from the well node of DID #6. Atmospheric barometric changes can cause fluctuations in aquifer levels that exceed a tenth of a foot. As minimal as these modeled impacts appear to be, they are larger than would be expected in reality. This is because, for several reasons, MODFLOW is a conservative model- -i.e., impacts modeled are greater than impacts that would be likely in actuality. First, MODFLOW is a mathematical, asyntopic model. This means it models very gradually decreasing drawdowns continuing over long distances as predicted drawdowns approach zero. This tends to over-predict impacts at greater distances from the withdrawal. In reality, the heterogeneity or discontinuity of confining units cuts down on drawdown effects. The steepest drawdowns occur at a well node and then decline relatively rapidly with distance. Second, several model inputs are conservative. The annual average quantities for water use generated under the AGMOD methodology is based on a two-in-ten-year drought year. The peak month quantity applies to the three driest months within the two-in-ten-year drought period. The MODFLOW model applies this 90-day peak usage continuous pumping under AGMOD and conservatively assumes no rainfall or recharge to the aquifers during this period. Both of these are extremely conservative assumptions for this region of Florida. The District's determination of reasonable assurances "on both an individual and a cumulative basis" in water use permit cases only considers the sum of the impact of the applicant's proposal, together with all other existing impacts (and perhaps also the impacts of contemporaneous applicants). The impacts of future applicants are not considered. This differs from the cumulative impact review under Part IV of Chapter 373 (environmental resource permitting). See Conclusions 80-84, infra. Modeling is a component of the District’s assessment of impacts on a cumulative basis. In addition, the District reviewed and assessed hydrographs of the potentiometric surface from nearby ROMP wells, water quality data, permit history of the Boran site, and regional hydrologic conditions. The hydrographs represent the accumulation of all impacts from pumpage in the area and show stable groundwater levels in the region. Water quality also is stable, with no declining trends. The permit history indicates that permitted withdrawals on the Boran site have declined. For all of these reasons, the evidence was that Boran's proposed withdrawals would create no adverse impacts on water resources on a cumulative basis. The evidence proved that the proposed agency action will not cause adverse environmental impacts to wetlands, lakes, streams, estuaries, fish and wildlife, or other natural resources, as required by Rule 40D-2.301(1)(c). Due to the significant confinement between the source aquifers and the surficial aquifer and surface water bodies, the modeling results show no adverse impact to the surficial aquifer, and no adverse impact to wetlands, streams, estuaries, fish and wildlife, or other natural resources. The evidence was that there are no minimum flows or levels set for the area in question. Furthermore, Standard Condition 9 of the Proposed Agency Action requires Boran to cease or reduce withdrawals as directed by the District if water levels should fall below any minimum level later established by the District. The more persuasive evidence was that the requirements of section 4.3 of the District's Basis of Review have been met. (A moratorium on water use permits until establishment of minimum flows and levels would be neither reasonable nor appropriate.) The evidence proved that the proposed use will utilize the lowest water quality he has the ability to use, as required by Rule 40D-2.301(1)(e), because the new withdrawals are exclusively from the upper Floridan aquifer, which has poorer quality than the intermediate aquifer. Deeper aquifers cannot be used because the water quality is poorer than the upper Floridan aquifer, and it is technically and economically infeasible to use it for agricultural purposes. Behrens suggests that Boran should be required to discontinue all withdrawals of higher quality water from the intermediate aquifer as part of the proposed modification. While an offer to do so might be welcomed (as was Boran's offer to install subsurface seepage irrigation and apply the higher efficiency percentage to the entire Boran Ranch), Behrens could cite no authority for imposing such a condition; and the more persuasive evidence was that imposition of such a condition would be neither reasonable nor appropriate under the circumstances of this case. The evidence proved that the proposed use will not significantly induce saline water intrusion, as required by Rule 40D-2.301(1)(f), because the model results show that the drawdown contours do not approach anywhere near the ETBWUCA or MIA areas. Boran's Ranch is located approximately 21 miles from the MIA boundary and 10.8 miles from ETBWUCA boundary. Further, Boran must monitor the water quality in DID #1 and DID #4 and document any changes in water quality as a result of the withdrawals. The parties have stipulated that the proposed use meets the requirements of Rule 40D-2.301(1)(g) and will not cause pollution of the aquifer. The evidence proved that the proposed use will not adversely impact offsite land uses existing at the time of the application, as required by Rule 40D-2.301(1)(h), because the modeling showed no impact to the surficial aquifer or land use outside Boran Ranch. The confinement between the point of withdrawal and the surface is too great to impact offsite land uses in the instant case. The evidence proved that the proposed use will not adversely impact any existing legal withdrawal, as required by Rule 40D-2.301(1)(i), based on the ROMP hydrographs and modeling showing minimal drawdowns outside the boundaries of Boran Ranch. Behrens claims that Boran's proposed modification will adversely impact his well, which is approximately 3.5 miles northeast of the northeast corner of the Boran property and over four miles away from DID #6. But the greater weight of the evidence was to the contrary. (The wells of other DCAP members were even further away, making impacts even less likely.) Behrens has no independent knowledge of the depth of his two-inch well but believes it is approximately 150 feet deep, which would place it within the intermediate aquifer. In view of the consistent quality of Behrens' well water, and the nature of his well construction, it is most likely that Behrens' well does not penetrate the confining layer between the intermediate aquifer and the upper Floridan aquifer. If 150 feet deep, Behrens' well would not extend into the deepest producing unit of the intermediate aquifer (PZ-3); rather, it would appear to extend into the next deepest producing unit of the intermediate aquifer (PZ-2). But it is possible that Behrens' well cross-connects the PZ-2 and the shallowest producing unit of the intermediate aquifer (PZ-1). (The evidence did not even rule out the possibility that Behrens' well also is open to the surficial aquifer.) Assuming that Behrens' well is open to the PZ-2 only, conservative MODFLOW modeling predicts no impact at all from the proposed modification. (Behrens' well would be outside the zero drawdown contour.) Meanwhile, hydrographs of PZ-2 from nearby ROMP wells show marked fluctuations (five-foot oscillations) of the potentiometric surfaces in producing units of the intermediate aquifer. These fluctuations appear to coincide with increased pumping out of the intermediate aquifer. These fluctuations in the potentiometric surface are not being transmitted up from the upper Floridan aquifer or down from the surficial aquifer. The potentiometric surface in those aquifers do not exhibit matching fluctuations. It appears that the intermediate aquifer is being impacted almost exclusively by pumping out of that aquifer. (This evidence also confirms the integrity of the relatively thick confining layer between the intermediate and the upper Floridan aquifers, which serves to largely insulate Behrens' well from the influence of pumping out of the upper Floridan.) Behrens seems to contend that, in order to determine adverse impacts on a cumulative basis, the impact of Boran's entire withdrawal, existing and proposed, which is modeled conservatively at approximately 0.3 feet, must be considered. But the District considers an adverse impact to an existing legal withdrawal to consist of an impact large enough to necessitate modification to the producing well in order for it to continue to function as intended. The greater weight of the evidence was that the well on Behrens' property was not designed to be a free-flowing well but was designed to use a pump to operate as intended. At the time Behrens purchased his property, there was a well and a non-functioning pump on the property. Even at the beginning of his ownership, he did not always have running water without a functioning pump. In approximately 1986 or 1987, Behrens installed a new electric pump because it allowed the well to produce more water. After installation of the pump, Behrens raised his trailer an additional five feet (to guard against flooding) which caused it to be approximately ten feet high, meaning the water had to travel that much farther against gravity to reach Behrens' faucets. For most of the time that he has owned the property, Behrens has used a pump on the well. Behrens installed a check valve to allow him to turn off the pump. Sometimes during storm or flood conditions, electric power failed or was cut off, and Behrens was forced to rely solely on artesian flow, which was sometimes adequate in flood conditions during the rainy season. At other times when artesian flow was adequate, Behrens would turn off the pump and rely solely on artesian flow. But it also was sometimes necessary for Behrens to use the pump to get adequate water flow. During the summer of 2001, Behrens' pump failed, and he had to rely solely on artesian flow. As in prior years, artesian flow was sometimes inadequate. In order to be able to get at least some artesian flow for the maximum amount of time, Behrens lowered the spigot on his well by about two feet. Although Behrens is aware that the iron casing of his well could corrode over time, he has never called a licensed well driller or other contractor to inspect his well. Behrens did not test his own well for possible blockage that would result in a lower yield. Furthermore, Behrens admits that his whole outdoor water system needs to be completely replaced. The evidence proved that the proposed use will incorporate water conservation measures, as required by Rule 40D-2.301(1)(k), based on the water conservation plan submitted to the District, installation of a state-of-the-art irrigation system, increase in efficient use of the water, and decrease in the application rate. (Behrens' arguments that Boran has been allowed to use too much water and his question as to the existence of hardpan underlying Boran's fields already has been addressed. See Findings 27 and 35, supra.) The parties have stipulated that Boran has demonstrated that the proposed use will incorporate reuse measures to the greatest extent practicable, as required by Rule 40D-2.301(1)(l). The evidence proved that the proposed use will not cause water to go to waste, as required by Rule 40D-2.301(m), because the irrigation method is the most efficient system that is economically and technically feasible available for sod. (Behrens' question as to the existence of hardpan underlying Boran's fields already has been addressed. See Finding 27, supra.) The evidence proved that the proposed use will not otherwise be harmful to the water resources of the District, as required by Rule 40D-2.301(1)(n), based on the review of all other permit criteria. Propriety of Behrens' Purpose Behrens did not review the District's permit file on Boran's application before he filed his petition. The evidence suggested that he traveled to the District's Sarasota office for that purpose but found on his arrival that the complete permit file was not available for inspection there. Because of the filing deadline, he did not find time to make another attempt to review the permit file of record before he filed his petition. Behrens also did not contact Boran, the District or anyone else with any questions about the proposed agency action before filing his petition. He also did not visit Boran’s property, and made no inquiry as to the irrigation system employed by Boran. Behrens also did not do any additional legal research (beyond what he had done in connection with other water use permit proceedings) before filing his petition. Behrens believed he had all the information he needed to file his petition. Behrens has previously filed at least one unsuccessful petition challenging the District’s issuance of a water use permit. See Behrens v. Southwest Fla. Water Management Dist., DOAH Case No. 00-4801 (DOAH Jan. 29, 2001). DCAP, with Behrens acting as its president, has previously filed at least three unsuccessful petitions challenging the District’s issuance of a water use permit. See, e.g., DeSoto Citizens Against Pollution, Inc. v. Farmland Hydro Limited Partnership, DOAH Case No. 02-232 (Southwest Fla. Water Man. Dist. June 25, 2002); DeSoto Citizens Against Pollution, Inc. v. Southwest Fla. Water Management Dist., DOAH Case No. 01- 3056 (DOAH Aug. 22, 2001); DeSoto Citizens Against Pollution, Inc. v. Southwest Fla. Water Management Dist., DOAH Case No. 01-2917 (DOAH Sept. 24, 2001). However, none of those proceedings involved a project at the Boran site. It is found that, under the totality of circumstances, Behrens' and DCAP's participation in this proceeding was not for an improper purpose--i.e., not primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of Boran's permit modification. While a reasonable person would not have raised and pursued some of the issues raised by Behrens and DCAP in this proceeding, it cannot be found that all of the issues they raised were frivolous or that their participation in this proceeding was for an improper purpose. It appears that Behrens based his standing in part on the requirement in Rule 40D-2.301(1)(i) that Boran provide reasonable assurances that the proposed use will not adversely impact an existing legal withdrawal to be provided "on both an individual and a cumulative basis.” (Emphasis added.) Not unreasonably, Behrens argued that this requirement allowed him to base his standing on alleged injuries from all of Boran's withdrawals, existing and proposed, which would create a 0.3- foot drawdown on his well. While his argument is rejected, it cannot be found to be frivolous or made for improper purpose. Behrens' argument that Boran did not meet Rule 40D- 2.301(1)(i) was based on the 0.3-foot drawdown and his position that his well was designed to be artesian free- flowing. While Behrens' proposed finding was rejected, the position he took is not found to be frivolous or taken for improper purpose. Several other arguments made and positions taken by Behrens have been rejected. See Findings 27, 34, 35, and 51, supra, and Conclusions 86-87, infra. But they cannot all be found to have been frivolous or made and taken for improper purpose.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the District enter an order granting Boran’s water use permit application number 20009478.005; and denying the motions for attorney's fees and costs under Section 120.595(1), Florida Statutes. Jurisdiction is reserved to enter a final order on the part of the motions for sanctions under Section 120.569(2)(e). DONE AND ENTERED this 29th day of July, 2002, in Tallahassee, Leon County, Florida. Hearings Hearings ___________________________________ J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative 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 29th day of July, 2002. COPIES FURNISHED: Alan R. Behrens, President DeSoto Citizens Against Pollution, Inc. 4070 Southwest Armadillo Trail Arcadia, Florida 34266 Mary Beth Russell, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Douglas P. Manson, Esquire Carey, O'Malley, Whitaker & Manson, P.A. 712 South Oregon Avenue Tampa, Florida 33606 E.D. "Sonny" Vergara, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899
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.
The Issue The issues presented in this matter concern the request by the Petitioner to be granted a management and storage of surface waters permit by Respondent. Respondent proposes to deny the permit based upon the perception that the activities contemplated by Petitioner: (1) are not consistent with the public interest as envisioned by Section 373.016, Florida Statutes, and 40C- 4.301(1)(b), Florida Administrative Code, (2) are not a reasonable and beneficial activity, per Section 40C-4.301(1)(a), Florida Administrative Code, alter the peak discharge rate of runoff from the proposed activity or the downstream peak stage or duration for the 1 in 10 year design storm, per Section 40C-4.301(3)(a), Florida Administrative Code, (4) cause an increase in velocity or flood stage on lands other than those owned, leased, or otherwise controlled by the applicant for the design storm, per Section 40C-4.301(3)(b), Florida Administrative Code, (5) cause an increase in flow or stage such that it would adversely affect lands other than those owned, leased, or otherwise controlled by the applicant, per Section 40C-4.301(3)(c), Florida Administrative Code. 1/
Findings Of Fact A predecessor applicant had requested permission to construct and operate the water management system which is the subject of this controversy. The approximate acreage involved was 197 acres in Lake County, Florida. This acreage and requested activity was subject to the regulatory requirements of St. Johns River Water Management District. Clay Island Farms, Inc., hereinafter referred to as CIF, was substituted for the initial applicant and this matter has been litigated before the Division of Administrative Hearings on the continuing application of the Petitioner. The permit application number is 4- 8089. This application was considered with application number 4-8088, pertaining to property owned by A. Duda and Sons, Inc. Subsequently, the latter application shall be referred to as the Duda request for permit. Certain additional information was sought by Respondent from the applicants, CIF and Duda, in the permit review, by correspondence dated October 2, 1981. A copy of that correspondence may be found as Petitioner's Exhibit No. 16 admitted into evidence. In particular, CIF was requested to prepare pre and post-development runoff rates in the 1 in 10, 1 in 25,and 1 in 100-year storms, to include stage-storage and stage-discharge rates for any and all retention facilities within the project design. Petitioner's Composite Exhibit No. 1 admitted into evidence contains a copy of the engineering report by CIF which are CIF's responses to the request for information. The date of the engineering report is July 12, 1982. The CIF application, as originally envisioned, called for the construction of exterior and interior ditches to be placed around a dike of 71 feet MSL elevation. The dike would enclose a proposed farm operation of approximately 197 acres, should the permit be granted. Within that 197 acre plot, would be found numerous drainage ditches to include major ditches and minor arterial ditches. The purpose of those ditches found in the 197 acres would be to serve as a conveyance for rainfall runoff. The system of conveyance would be connected to an existing conveyance system already in place and related to farm operations of A. Duda and Sons. The runoff would be eventually placed in a retention pond and at times discharged from that retention pond or basin into Lake Apopka by means of gravity flow. The particulars of the development of the 197 acre plot and its service dike, canals, and ditches are more completely described in Petitioner's Exhibit No. 1, which is the engineering report for the surface water management permit application. The CIF application was reviewed by the staff of the Respondent. Recommendation was made to deny the permit. Details of that denial may be found in Respondent's Exhibit No. 1. In the face of the denial, CIF requested an administrative hearing. This request was made on August 27, 1982, by petition for formal Subsection 120.57(1), Florida Statutes, hearing to determine Petitioner's entitlement to the requested permit. St. Johns River Water Management District, in the person of its governing board, determined to refer this matter to the Division of Administrative Hearings to conduct the formal proceeding and the request for the assignment of a hearing officer was received by the Division on September 13, 1982, leading to the final hearing in this cause. During the course of the final hearing, the CIF permit application was modified in a fashion which reduced the amount of acreage sought for cultivation. Now, approximately 122 acres would be farmed per the amended proposal. A general depiction of the design of the project in its amended form may be found in the engineer's sheet, which is Petitioner's Exhibit No. 20 admitted into evidence. When contrasted with the engineering drawings set out in Petitioner's Composite Exhibit No. 1, the new design is essentially the same as contemplated in the original permit application, on a lesser scale. Other than dimensions, the basic concepts of the CIF operation would remain the same under the amended proposal. At present, Petitioner proposes to remove the vegetation which covers the subject 122 acre plot and to conduct a muck farming operation. That vegetation is mostly mixed hardwood with the primary species being red maple. The soil in this area is constituted of monteverde muck, which is conducive to the production of corn and carrots, the crops which Petitioner would plant, to prepare the land for the operation, the system of ditches dikes and canals described would be installed following the cleaning, draining, and leveling of the 122 acres. Petitioner's Exhibit No. 10 admitted into evidence depicts land which has been cultivated and the subject 122 acres in its undisturbed state. Petitioner's Exhibit No. 4 admitted into evidence shows the overall CIF area is outlined in red, except for its southerly extent, which carries a red and yellow line on the exhibit. This exhibit depicts Wolfshead Lake which is a small interior lake in the southeastern corner of the overall CIF property. The yellow line in the middle of the CIF property represents, the location of a former north-south canal. The westernmost north-south reach, which is shown with a red line, depicts a canal which runs north from Wolfshead Lake into the existing Duda system of canals and ditches. The Duda operation has attempted to plug that north-south canal on the western fringe to stop the flow from the area of Wolfshead Lake, but has been unsuccessful and the water still enters the Duda farm ditches and canals. In the 1940's and early 1950's, the CIF property had been partially developed for a cattle operation and truck farming. Those canals, as described before, were installed, together with the diagonal yellow line on Petitioner's Exhibit 4, which represents a canal that was built with an axis running northeast and southwest. In addition, there was a centrally placed east-west canal and a slough running from Wolfshead Lake in a southeasterly direction. The slough is still there, although water that might be diverted from the Wolfshead Lake area into the slough is flowing north in the westerly north-south canal at present. If the project were allowed, most of the water flowing in and around the Wolfshead Lake would be introduced into the slough and from there exit to Lake Apopka. The center north-south canal and the interior east-west canal, together with the diagonal canal, are not in operation at present. The center north-south-canal would become the approximate eastern boundary of the 122 acres with the western north-south canal representing the approximate western boundary of the 122 acre plot. The northern boundary of the CIF property is constituted of an east-west canal which is part of the present Duda system. This is the only one of the canals associated with the former farming operation on the CIF property which is part of any maintained system of conveyances presently in existence. Approximately 1,000 acres are being farmed by Duda and Sons in property north of the proposed project. The Duda permit application, 4-8088 as granted, is described in Petitioner's Exhibit No. 13 which is a copy of the permit. This acreage is generally found to the northwest of the CIF plot, and would allow an additional 300 acres to be farmed in that muck area, on land which has been cleared for the most part and/or which has an elevation predominantly above 68.5 feet MSL. Eighty acres of the proposed Duda permit application was denied based upon the fact that it had not been cleared prior to the Duda permit application and in consideration of the amount of the 80 acre segment which lies below 68.5 feet MSL. The elevation 68.5 feet MSL represents the flood plain for the 1 in 10 year rainfall event for Lake Apopka. The area of the Duda permit is depicted on Petitioner's Exhibit No. 4 and outlined on that exhibit with lines of green and yellow at the southern end, green and yellow and red and yellow on its western flanks, red at the north end and by red on the east side, together with a Duda drainage ditch, which runs north from the terminus of the north-south drainage ditch coming from Wolfshead Lake and the east-west drainage ditch at the northern extent of the CIF property. Exhibit No. 4 was made prior to clearing operations depicted in Petitioner's Exhibit No. 10 and that letter exhibit is a more correct indication of the appearance of the new Duda permit property today. A green diagonal line running northwest and southeast intersecting with a line running east-west and a line running north-south depicts the approximate part of the 80 acres, which lies below 68.5 feet MSL, as shown in Petitioner's Exhibit No. 4. Farm operations, in keeping with the authority of Permit No. 4-8088, have not commenced. If the CIF permit application is successful, the original 1,000 acres, approximately 300 acre area of the Duda permit and the 122 acres of CIF, would be tied in by a system of conveyance ditches or canals allowing the interchange and transport of water through and around the three farm areas. The existing retention pond would be expanded to accommodate the additional farm acreage. The Petitioner is willing to increase the present retention pond to a design capacity which would equal one acre of basin for each ten acres of farm land, at the place in time when all three elements of the muck farm operation were under way. This again pertains to the existing 1,000 acres, the approximately 300 acre recent Duda permit, and the 122 acres related to the CIF application. With the addition of the CIF acreage, when water in the ditches reached 67.1 feet MSL, this would cause the engagement of a 40,000 GPM pump allowing the ditch water influent into the retention pond. The pump automatically would shut off at any time the water level in the access ditches to the pond dropped below 61 feet MSL. The primary purpose of the retention pond is to make water available for irrigation of crops, in its present state, and as contemplated with the addition of the CIF project. The pond does and would detain farm water for a period of about a day allowing the settling out of certain nutrients which are in particulate form. The existing pond and in its expanded form does not and would not filter nutrients which have been dissolved and have become a part of the water column. At times of high incidence of rainfall, when the crops are inundated with water for a 48-hour period of time, the retention pond is now designed and as contemplated by the addition of the CIF farm land, would allow for the discharge of effluent into Lake Apopka through two discharge culverts. The discharge is by means of gravity through an adjustable riser system. The retention pond as presently designed and as contemplated in its expansion has established the height at which water would be released from the retention pond into Lake Apopka through the riser at 68 feet MSL. The occasion of high incidence of rainfall occurs during the normal rainy season in a given year. Discharge could also be expected in the 1 in 10 year, 24hour storm event. During that storm event or design, Lake Apopka would rise to a level of 68.54 feet MSL, a level which would correspond to the 10year flood plain. Whether in the pre or post-development phase of the 122 acres, waters from that acreage would be discharged during the course of the storm through culverts leading from the retention pond into Lake Apopka. This process would continue until the gravity flow stopped at the moment where the water level in the pond and the water level in Lake Apopka adjacent to the discharge culverts achieved equilibrium of elevation. At that point in time, the gravity flow or discharge from the retention basin would cease, there no longer being a positive gradient from the detention pond to Lake Apopka. There will be some amount of discharge in the 24-hour storm event through the culverts at the retention pond either in the pre or post-development phases of the project, because, at present, the western most north-south ditch, which is found at the western boundary of the CIF property, allows water to flow north into the present Duda ditch system, water which has fallen on the 122 acres in question. From the ditch system, that water finds its way into the retention pond and thus into the lake. The contemplated system to be installed with the 122 acres at build-out would also allow water from the 122 acres to go through a system of conveyances and to the retention pond and from there into Lake Apopka. Although considerable testimony was presented by both parties on the subject of comparing pre-development and post-development peak discharge rates of runoff from the proposed activity, in the 1 in 10 year, 24-hour storm design or event, neither party has satisfactorily proven the dimensions of the pre-development and post-development peak discharge rates of runoff from the proposed activity. This determination is made having reviewed the testimony and the exhibits in support of that testimony. Notwithstanding a lack of proof of this differential with exactitude, it has been shown by the testimony and exhibits that the post- development peak discharge rate of runoff in the 1 in 10 year, 24-hour design storm or event can be expected to exceed that of the pre-development rate. On the associated topic of the ability of the post-development design to accommodate the differential in peak discharge rate of runoff between pre- development and post-development, Petitioner has failed to establish this proof. The modeling that was done by the Petitioner, in an effort to depict the differential as 10 acre feet with an available capacity of attenuation approximating 26 acre feet within the system of ditches, is not convincing. Nor has petitioner shown that there is sufficient storage in the retention pond, in the course of the storm event. The data offered in support of Petitioner's position does not sufficiently address accommodation of the drainage from areas surrounding the 122 acres in question, which are not part of the Duda system; the amounts of water already found in the system of ditches and canals at the onset of the storm event; the amount of water located on the crops at the onset of the storm event, which would have to be removed; and the amount of water already found in the retention pond at the time of the storm event. During the 1 in 10 year 24-hour storm, the CIF 122 acres will be protected by the 71-foot MSL dike, in that the expected elevation of Lake Apopka would not exceed 68.54 feet MSL. The dike would also protect the 122 acres in the 25, 50, and 100-year, 24-hour storm events whose elevations are anticipated to be 68.98, 69.28, and 69.56 feet MSL, respectively. As a consequence, an increase in flood stage would occur on lands other than those controlled by CIF. The amount of increase in flood stage would be approximately .046 inches during the 1 in 10 year storm, and an increasingly greater amount for the larger storms. It was not established where the amount of water which could not be staged on the 122 acres would be brought to bear through the surface flow on the 31,000 acres of water which constitute Lake Apopka. Nonetheless, that water could be expected to increase the flood stage on lands other than those of the Applicant. Possibly the dikes protecting the muck farms on the northern side of Lake Apopka could be influenced by the .046 inches in elevation due to the forces associated with the 1 in 10 year storm event, such as winds and movement of the water in the lake. This is true, notwithstanding the fact that the design goal of the dikes in the area is 71 feet MSL. The dikes are constituted of muck and are susceptible to overtopping, erosion, or blowout. By history, there have bean dike failures in the northern end of Lake Apopka, and associated increases in stage or flood stage. This incremental increase in water level in the 1 in 10 year storm event, due to the CIF development, when considered in the context with the other influences of that storm event, could possibly be the determining incident leading to dike failure in the northern perimeter of Lake Apopka. However, given the history of dike failures, prior to this potential loss of the storage area on the applicant's property, it has not been shown that the proximate cause of dike failure in the 1 in 10 year storm could be expected to be the contribution of an additional .046 inches of water on the lake surface. Those failures existed prior to the potential for the addition of water and were the result of inadequate maintenance of a structure which demanded a better quality of attention. Nonetheless, the additional amount of water could be expected to exacerbate the extent of a dike breach in any 1 in 10 year storm event that occurred subsequent to the development of the CIF 122 acres. In summary, the likelihood that the increase in elevation of water caused by the loss of storage on the subject property will be the critical event that causes a dike failure is not accepted. A dike could breach because of the influence of the storm even itself, without regard for the incremental increases in water elevation due to loss of water storage on the CIF property. The poor condition of some dikes due to less than adequate design or maintenance, would promote that dike failure and be exacerbated to the extent of more water being introduced on that property through the incremental amount of increase due to loss of storage on the CIF property. The dike failure circumstance in and of itself would not be sufficient to deny the permit application; however, the applicant had the burden of addressing the possible problem of increases in stage or flood stage on other properties, not its own, which are not protected by dikes. This showing was not made by the applicant, notwithstanding the fact that an increase in stage or flood stage could be expected to occur on property fronting Lake Apopka, which property is not protected by any form of artificial barrier. The installation of the protective dike aground the 122 areas of the CIF property in the 1 in 10 year design storm and potentially at times of lesser rainfall events, could be expected to increase the stage or flood stage on lands unprotected by dikes and thereby adversely affect lands other than those controlled by the applicant. Most of the 122 acres and the property to the east of that development and a portion of the undeveloped 80 acres in the recent Duda permit would be inundated in the 1 in 10 year storm event, prior to development. This is true because the elevation of much of that property is approximately 67.5 foot MSL. During the 1 in 10 year storm event, it would store approximately one foot of water, as presently constituted. It could also be expected to be inundated on an average of approximately once in two years. Lake Apopka is a part of a controlled system of lakes known as the Oklawaha River chain of lakes. Respondent regulates the water level in that chain of lakes by operation of a lock on the Apopka-Beauclair canal. The maximum desirable elevation of 67.5 feet MSL for Lake Apopka is a part of the regulation schedule found in Respondent's Exhibit No. 2 admitted into evidence. In the 1 in 10 year or better storm event, the Apopka-Beauclair system could not draw down the surface water at a rate faster than 27 days per foot, even assuming the lock was fully open to flow. Consequently, those properties that were suffering an, increase in flood stage on their surface could not expect to gain prompt relief through the regulation of waters in the Oklawaha River chain of lakes. Lake Apopka is an hyper-eutrophic lake. Although it is classified as Class III water body (ambient water quality) within the meaning of Section 17- 3.161, Florida Administrative Code, it fails to match that classification in terms of its actual water quality. This is as a consequence of its highly eutrophic state, brought about by the age of the lake and the contributions of man. Some of the contributors to the eutrophication have been removed from the lake area and water quality has improved. Those facilities removed were sewage treatment and citrus processing plants around the Lake Apopka rim. The muck farms remain and the quality of the water in the retention basins or ponds when compared to the receiving waters of Lake Apopka is similar in nature. Consequently, the receiving waters are not enhanced in their water quality when the retention ponds discharge water into Lake Apopka. As stated before, the retention ponds do not have as their primary purpose the treatment of water. Any water quality improvement is a secondary function of the retention pond. The retention ponds do improve the water somewhat, as described, and are adequately sized to fulfill that partial cleansing. Whether the water quality in Lake Apopka would ever improve sufficiently to allow Lake Apopka to become a more diversified habitat for fish and wildlife is not certain, even if all contributing discharges of pollutants were curtailed, to include the discharge of water from the muck farms with its high nutrient loads. Nonetheless, Lake Apopka cannot accomplish the recovery if the effluent from the muck farms continues to be introduced into the lake with the present constituents found in the water. Out of concern for the water quality in Lake Apopka, officials of the University of Florida have conducted experiments on nutrient removal which they hoped would approximate the quality of removal accomplished by transitional vegetation and swamp. (The 122 acres at issue and the western and eastern adjoining property are constituted of these water treatment zones.) This experiment of nutrient removal through use of retention ponds calls for the retention of the muck farm water for a period of six days allowing settlement of particulates and for the vegetation within those experimental retention basins to uptake dissolved nutrients. Several types of vegetation are used to gain a better quality of nutrient uptake add the vegetation is harvested every six to eight weeks to improve that performance. The experiment has shown that the quality of water discharged from the ponds utilized by the University of Florida was comparable in its quality to the natural wetlands system water discharge. The natural wetlands discharge is of a better quality than the receiving waters. Unlike the university experiment, the pond contemplated by CIF primarily emphasizes detention for a shorter period of time than was used in the experiment and allows highly eutrophic water to be mixed with that quality of water already found in Lake Apopka. The only exception to that comment is that water flowing from Wolfshead Lake, which is south of the proposed 122 acres, is a high quality of water, and through the project as contemplated, this water would be directly introduced into Lake Apopka through a flow over a natural wetlands system. This is in opposition to the present situation where the water from Wolfshead Lake flows primarily to the north through an existing canal and is mixed with water from the muck farm and is, therefore, of the eutrophic character as opposed to the high quality character. The Duda permit, which was issued, would allow the introduction of water which is similar in character to the water of Lake Apopka, through the system of ditch conveyances, placement in the retention pond, and at times, flow to the lake. In its effect, the nutrient loading which occurs by introduction of waters from that new farm, would be similar to that proposed in the CIF project. The fact of this similarity does not prohibit the district from evaluating water quality matters on the occasion of the CIF permit decision. Should the 122 acres be converted from natural vegetation to a muck farm, wildlife and fish habitat would be adversely impacted. The habitat provided by the plot is in scarce supply and is essential to the maintenance of a diversified fish population. The hardwood swamp, which is part of and adjacent to the 122 acres of the CIF application, supports benthic invertebrates, which are a food source for game fish. The type of vegetation found in the lake, due to its eutrophic state, is plankton and one of the by- products of the reproduction of that plant through the process and respiration is the destruction of the fish population. This occurs in the summer months. The plankton has replaced the emergent and submergent vegetation which once covered as much as two-thirds of Lake Apopka and now represents .05 percent of the lake. As a consequence, game fish have diminished over a period of years with plankton feeding fish predominating. Consequently, the fish population is less diverse and the removal of the vegetation becomes a significant contributor to the imbalance in fish population.
The Issue The issue is whether Respondent's water use permit should be revoked for nonuse of the permit for a period of two years or more.
Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Background The District is a state agency charged with the responsibility of issuing water use permits under Chapter 373, Florida Statutes, and Florida Administrative Code Chapter 40B- 2 for the geographic area under its statutory jurisdiction. Alachua County is within that geographic jurisdiction. Respondent is a Florida corporation with offices at 700 Northwest Cheeota Avenue, High Springs, in northern Alachua County. It owns approximately 700 acres in High Springs (west of Interstate Highway 75) on which it operates a church retreat and summer camping and recreational facility known as Camp Kulaqua. The property surrounds, and is contiguous to, Hornsby Spring, a first-order magnitude spring (having a flow rate of 100 CFS or greater) which, under normal conditions, discharges into the nearby Santa Fe River. Hornsby Spring is one of 296 documented springs within the District's jurisdiction. After receiving an overture from a representative of a private water bottling company, on September 28, 1999, Respondent filed an application for a General Water Use Permit in Township 7 South, Range 17 East, Section 26, in High Springs. In its application, Respondent represented that it desired a daily allocation of 2,000,000 gallons; that it intended to install two 12-inch wells, each having a capacity of 1,400 gallons per minute, just east of, and upgradient from, Hornsby Spring; and that all water withdrawals would be used in conjunction with a privately-owned commercial spring water bottling facility to be located on its property. The application also represented that the facility would employ 36 persons and operate 168 hours per week. The application was reviewed by a former District hydrogeologist, William H. Kirk. During the review process, and in response to Mr. Kirk's request for more information, Respondent provided a comparison of the requested allocation with the overall flow of Hornsby Spring. This was because Mr. Kirk was concerned that the requested allocation was "a bit high," and he wanted to ensure that the issuance of the permit would not cause harm to, or adversely affect, the water resources. Under a professional guideline that Mr. Kirk used, if the applicant could show that the cumulative amount being withdrawn was to be less than ten percent of what the available data showed to be the mean spring flow, the District would consider it to be "an acceptable impact." Notwithstanding Mr. Kirk's use of this guideline, the District points out that there is no District rule or policy sanctioning the ten percent rule, and at hearing it denied that this standard is used by the District in assessing water use applications. Further, the Permit itself does not refer to a relationship between spring flow and the size of the allocation. Even so, this analysis was considered by Mr. Kirk in determining whether Respondent had given reasonable assurance that the spring would not be impacted. In its response to the request for additional information, Respondent reduced its requested allocation to 750,000 gallons per day and indicated that if a bottling plant were to be constructed on its property, approximately 700,000 gallons of the total allocation would be consumed in "bulk transfer and bottling," with the remainder for camp use. More specifically, Respondent indicated that it would allocate 490,000 gallons per day for bulk transport, 210,000 gallons per day for spring bottling water, and 50,000 gallons per day for incidental uses at its property. By reducing the allocation from 2,000,000 gallons per day to 750,000 gallons per day, Respondent's requested average daily allocation represented only 0.4 percent of the average daily spring flow as measured over the last 28 years. The reduced allocation satisfied Mr. Kirk's concern that Respondent demonstrate a reasonable demand and a reasonable need for that allocation, and he recommended approval of the application.2 On February 25, 2000, the District approved the application and issued Water Use Permit No. 2-99-00130 (Permit).3 The Permit authorizes an average daily withdrawal of 0.7500 million gallons per day (750,000 gallons per day) or a maximum daily withdrawal and use of 0.7500 million gallons per day with an annual allocation not to exceed 273.750 million gallons (273,750,000 gallons) per calendar year in conjunction with the operation of a privately-owned water bottling plant. The Permit expires on February 25, 2020. After the Permit was issued, under the regulatory process in place, Respondent was required first to obtain a permit for a temporary test well which would be used to collect information concerning the site of the proposed activity, and to then file an application for permits authorizing the construction and operation of the two 12-inch production wells. The Permit contains a number of conditions, two of which require a brief comment. First, Condition No. 2 provides that "[t]his permit is classified as unconfined [F]loridan aquifer for privately owned bottled water plant." This means that all water withdrawals must be made from the unconfined Floridan aquifer, as opposed to the spring head of Hornsby Spring. (Respondent's proposed siting of its two production wells 660 yards east of the spring is consistent with this provision.) Second, Condition No. 4 provides that "[t]he permittee shall submit daily pumpage records on a monthly basis to the [District]." Pumpage reports are filed by permittees so that the District can determine whether the permit is actually being used, and if so, to ensure that the amount of water being withdrawn under the permit does not exceed the authorized allocation. As it turned out, pumpage reports were never filed by Respondent. (However, the record shows that the District has never strictly enforced this requirement for any permittee.) In late 2002, the District staff undertook a review of the nine water bottling permit holders within its jurisdiction, including Respondent. That category of permit holders was selected for review because of the small number of permits and the limited resources of the District staff. (In all, the District has probably issued several thousand permits to other types of users.) On February 4, 2003, the District served its Complaint under the authority of Sections 120.60 and 373.243, Florida Statutes, and Florida Administrative Code Rule 40B-2.341. As grounds for revoking the permit, the District alleged that there was "non-use of the water supply allowed by the permit for a period of two (2) years or more." Although Respondent contends that it should have been given an opportunity to correct the nonuse allegation before the Complaint was issued, nothing in the Administrative Procedure Act or District rules requires that this be done. Until the issuance of the Complaint against Respondent in early 2003, and similar Complaints against eight other permit holders at the same time, the District had never invoked this statutory provision.4 There is no evidence to support Respondent's contention that the Complaints were issued for "purely political reasons." On March 4, 2003, Respondent requested a formal hearing challenging the District's proposed action. In the parties' Pre-Hearing Stipulation, the issues have been broadly described as follows: whether Section 373.243(4), Florida Statutes, is to be strictly or liberally construed; whether Respondent's nonuse is based upon extreme hardship for reasons beyond its control; and whether the District is equitably estopped from permit revocation. (According to the District, even if the Permit is revoked, such revocation is without prejudice to Respondent reapplying for, and receiving, another permit so long as it meets all applicable requirements.) Equitable Estoppel Respondent first contends that the District is estopped from revoking its Permit on the theory that, under the circumstances here, the doctrine of equitable estoppel applies. For that doctrine to apply, however, Respondent must show that the District made a representation as to a material fact that is contrary to a later asserted position; that Respondent relied upon that representation; and that the District then changed its position in a manner that was detrimental to Respondent. See, e.g., Salz v. Dep't of Admin., Div. of Retirement, 432 So. 2d 1376, 1378 (Fla. 3d DCA 1983). The District issued Respondent's Permit on the condition that Respondent operate in conformity with all pertinent statutes and regulations. This finding is consistent with language on the face of the Permit, which states that the Permit "may be permanently or temporarily revoked, in whole or in part, for the violation of the conditions of the permit or for the violation of any provision of the Water Resources Act and regulations thereunder." Respondent relied on the District's representation that it could use the Permit so long as it complied with all statutes and regulations. In reliance on that representation, in addition to staff time, after its Permit was issued, Respondent expended "somewhere around" $70,000.00 to $74,000.00 for conducting water quality testing; sending cave divers underground to ascertain the correct location of the portion of the aquifer on which to place its production wells; drilling a 6-inch test well in August 2000; obtaining the City of High Springs' approval in March 2000 for industrial zoning on a 10-acre tract of land on which to site a "water plant"; and engaging the services of a professional who assisted Respondent in "seeking out businesses and getting the right qualifications of the spring water to make sure that it was a marketable water." The District has never asserted anything different from its original position: that if Petitioner complied with all statutes and rules, it could continue to lawfully make water withdrawals under its Permit. The issuance of the Complaint did not represent a change in the District's position. Because a change in position in a manner that was detrimental to Respondent did not occur, the necessary elements to invoke the doctrine of equitable estoppel are not present. Was the Permit Used? A preliminary review by District staff indicated that Respondent had never filed the daily pumpage reports on a monthly basis and had never requested permits authorizing the construction of the two 12-inch production wells. These preliminary observations were confirmed at final hearing, along with the fact that Respondent has never entered into an agreement with a water bottling company (although draft agreements were once prepared); that Respondent has never constructed a water bottling facility; and that no operations were ever conducted under the Permit. Therefore, the evidence supports a finding that Respondent did not use its Permit for the two-year period after it was issued, as alleged in the Complaint. Respondent's contention that the evidence fails to support this finding belies the evidence of record. In an effort to show that it actually used the Permit, Respondent points out that in August 2000 it applied for, and received a permit to construct, an unmetered 6-inch test well in association with its General Water Use Permit. (Respondent sometimes erroneously refers to the test well as a test production well. This is incorrect as the well is a test well, and not a production well.) After the test well was installed, at some point Respondent says it began withdrawing approximately 50,000 gallons per day of water from that well for incidental uses associated with the operation of Camp Kulaqua.5 These withdrawals were made on the assumption that the test well permit fell under the broad umbrella of the General Water Use Permit. (Respondent also has a permitted 6- inch diameter well and an unregulated 4-inch well on its premises, both of which are used for water supply needs at Camp Kulaqua.) It is true, as Respondent asserts, that its Permit authorized incidental withdrawals of up to 50,000 gallons per day for unspecified uses at Camp Kulaqua. However, these withdrawals are authorized under the General Water Use Permit and not the test well permit. The two permits are separate and distinct. On the one hand, a test well is intended to be temporary in nature and used only for the purpose of test well development and collecting information regarding the height of the aquifer and water quality at the site of the proposed activity. Conversely, withdrawals for any other purpose, even incidental, must be made from the production wells, which are only authorized by the General Water Use Permit. Before a test well can be used for normal consumptive purposes, the permit holder must seek a modification of the permit to include it as a part of its general water use permit. Here, no such modification was sought by Respondent, and no authorization was given by the District. Therefore, Respondent's incidental water uses associated with its test well cannot be counted as "uses" for the purpose of complying with the use requirement in Section 373.243(4), Florida Statutes. In light of the District's credible assertion to the contrary, Respondent's contention that it is common practice to lawfully withdraw water from a test well for incidental consumptive purposes has been rejected. (It is noted, however, that the District has not charged Respondent with violating the terms of its test well permit.) Extreme Hardship Under Section 373.243, Florida Statutes (which was enacted in 1972), the District is authorized to revoke a water use permit "for nonuse of the water supply allowed by the permit for a period of 2 years." However, if the user "can prove that his or her nonuse was due to extreme hardship caused by factors beyond the user's control," revocation of the permit is not warranted. The phrase "extreme hardship caused by factors beyond the user's control" is not defined by statute or rule. In the context of this case, however, the District considers an extreme hardship to occur under two scenarios. First, if the aquifer level has dropped so low due to drought conditions that a permit holder cannot access the water through its well, its nonuse is excusable. Alternatively, if an emergency order has been issued by the District directing permit holders (including Respondent) to stop pumping due to certain conditions, an extreme hardship has occurred. (Presumably, a severe water shortage would precipitate such an order.) In this case, the District issued a water shortage advisory, but not an emergency order, due to a "severe drought," indicating that users could still pump water, but were encouraged to voluntarily reduce their usage. This advisory remained in effect from the summer of 1998 until the spring of 2003, when a severe drought ended. However, no emergency order was ever issued by the District. Respondent contends that its nonuse was due to an extreme hardship caused by factors beyond its control. More specifically, it argues that a severe drought occurred in Alachua County during the years 1998-2003, and that under these conditions, federal regulations prevented it from withdrawing water for bottling purposes, which was the primary purpose for securing a permit. Further, even if it had withdrawn water during these drought conditions, such withdrawals could have adversely impacted Hornsby Spring and constituted a violation of a District requirement that water resources not be adversely impacted. Because an investment of several hundred thousand dollars was required to drill and install the two production wells, Respondent contends it was not financially prudent to make that type of investment and begin operations until normal spring conditions returned. These contentions are discussed in greater detail below. Around September 7, 1999, a representative of a water bottling company first approached Respondent about the possibility of the two jointly operating a water bottling plant and/or transporting water in bulk from Respondent's property. Prompted by this interest, less than three weeks later Respondent filed its application for a water use permit (although at that time it did not mention on the application that off-site bulk transfers would occur), and a permit was eventually issued in February 2000. Later, and through a professional firm it employed, Respondent had discussions with representatives of several bottling companies, including Great Springs Waters of America (Great Springs) and Perrier Group of America. Apparently, these more serious discussions with a potential suitor did not take place until either late 2000 or the spring of 2001. Periodic measurements taken by District staff at Hornsby Spring reflected natural drought conditions from April 2000 to April 2003. As noted earlier, this was the product of a "severe drought" which took place between the summer of 1998 and the spring of 2003; the drought was one of a magnitude that occurs only once in every 50 to 100 years. During the years 2000 through 2002, the spring had zero flow or was barely flowing much of the time.6 Had Respondent pumped water during 20 out of the 24 months after the Permit was issued, it could have potentially violated the requirement that it not harm Hornsby Spring. This fact is acknowleged by a District witness who agreed that if the "spring is not flowing, . . . [pumping] would have an [adverse] impact." Even as late as October 2003, the spring had tannic discoloration caused by the lengthy drought conditions. The parties agree, however, that there is no water shortage in the District at the present time. To illustrate the difficulty that it experienced in obtaining a joint venture partner for water bottling purposes, Respondent established that in the spring of 2001, a Great Springs representative visited the site when the spring was "barely flowing." For obvious reasons, Respondent could not "bring a party there who would want to enter into a business [agreement]" under those conditions. These same conditions remained in effect during most of the two year period. The District points out, however, that even though the spring was low or barely flowing, so long as the aquifer itself was not too low, Respondent could still withdraw water from the aquifer, since Condition 2 of the Permit authorizes withdrawals from the aquifer, and not the spring. The reason for this apparent anomaly is that when a spring ceases to flow, the aquifer has simply dropped below the level of the spring vent; even under these circumstances, however, there may still be a substantial quantity of water in the aquifer available for pumping. Assuming that it could still lawfully pump water when the spring was dry or barely flowing without causing adverse impacts to the spring, Respondent was still subject to federal regulations which govern the bottling of spring water. See Title 21, Part 165, C.F.R. For spring water to be marketed as bottled "spring water," 21 C.F.R. § 165.119(2)(vi) requires that the water "be collected only at the spring or through a bore hole tapping the underground formation feeding the spring." This means that the bore hole had to be physically connected with the cave system feeding Hornsby Spring or produce water of the same quality as that discharging from the spring. The regulation goes on to provide that "[i]f spring water is collected with the use of an external force [such as by a pump], water must continue to flow naturally to the surface of the earth through the spring's natural orifice." While this regulation obviously does not prohibit Respondent from pumping water, since that authority lies within the District's exclusive jurisdiction, it does provide that in order to use spring water for bottling purposes, the water must continue to flow naturally from the aquifer to the spring. If it does not, the water cannot be used for this purpose. Because Hornsby Spring had zero flow for parts of 2001 and 2002, and severely reduced flows during most of the other time during the two-year period ending February 2002, Respondent was effectively prevented by the foregoing regulation from using the water for bottling purposes. Therefore, Respondent's nonuse was due to extreme hardship caused by factors beyond its control -- a severe drought lasting throughout the two-year period after the Permit was issued, and federal regulations which prevented it from using water for the purpose for which the Permit was issued. Thus, the nonuse is excusable.
