The Issue The issue for determination in this case is whether Florida Administrative Code Rule 62-302.300(6) is an invalid exercise of delegated legislative authority because the rule is vague, fails to establish adequate standards for agency decisions, or vests unbridled discretion in the agency.
Findings Of Fact The Parties The Department is the state agency authorized under Chapter 403, Florida Statutes, to regulate discharges of industrial wastewater to waters of the state. Under a delegation from the United States Environmental Protection Agency, the Department administers the National Pollution Discharge Elimination (NPDES) permitting program in Florida. The Department promulgated the rules in Florida Administrative Code Title 62 that are applicable to the permitting of wastewater discharges. FOPB is a non-profit Alabama corporation established in 1988 whose members are interested in protecting the water quality and natural resources of Perdido Bay. FOPB has approximately 450 members. About 90 percent of the members own property adjacent to Perdido Bay. James Lane is the president of FOPB. Jacqueline Lane and James Lane live on property adjacent to Perdido Bay. IP owns and operates a paper mill in Cantonment, Escambia County, Florida. IP is the applicant for the Department authorizations that are the subject of DOAH Case Nos. 08-3922 and 08-3923. Background When this rule challenge was filed, DOAH Cases Nos. 08-3922 and 08-3923 (the permit cases) involved challenges by these same Petitioners to four Department authorizations for IP: an NPDES permit, a Consent Order, an approved exemption for the experimental use of wetlands pursuant to Florida Administrative Code Rule 62-660.300, and a waiver related to the experimental use of wetlands. IP later withdrew its request for the experimental use of wetlands exemption and the related waiver. Petitioners were ordered to show cause why their claim regarding the invalidity of Florida Administrative Code Rule 62- 660.300 was not rendered moot by IP’s withdrawal of its request for the exemption. Subsequently, the challenge to the validity of Florida Administrative Code Rule 62-660.300 was dismissed as moot. At the commencement of the final hearing on June 22, 2009, FOPB and James Lane announced that they were withdrawing their rule challenges except with respect to Florida Administrative Code Rule 62-302.300(6), and that the only legal ground being asserted for the invalidity of the rule is that it is vague and vests unbridled authority in the Department. Petitioners’Standing Jacqueline Lane, James Lane and a substantial number of the members of FOPB swim, boat, and make other uses of Perdido Bay. Perdido Bay would be affected by IP's wastewater effluent. The challenged rule was applied by the Department to determine that IP's proposed industrial wastewater discharge was in the public interest. The Challenged Rule Florida Administrative Code Rule 62-302.300, is entitled "Findings, Intent, and Antidegradation Policy for Surface Water Quality." Subsection (6) of the rule states: Public interest shall not be construed to mean only those activities conducted solely to provide facilities or benefits to the general public. Private activities conducted for private purposes may also be in the public interest. Most of the permits that are issued by the Department are issued to private entities whose primary purposes are personal uses or the production of private incomes and profits, rather than solely to provide facilities or benefits to the general public.
The Issue Whether the applicants own the property in question? Whether the project would comply with the criteria of the South Florida Water Management District contained in Basis of Review for Surface Water Management Systems, specifically Sections 3.1.3 and 3.2? Whether flood protection would be inadequate or septic tanks unsuitable or whether the public health and safety would be compromised or the ultimate purchasers be deprived of usage of the property due to inundation in violation of Chapter 373, Florida Statutes (1981), or Rule 40E-4.301(1), Florida Administrative Code?
Findings Of Fact Ms. Williamson and Messrs. Leggett and Collins hold in fee simple a triangular 117.24-acre parcel in Okeechobee County as tenants in common under a warranty deed executed in their favor by one W. C. Sherman. They propose to develop the property as a trailer park (complete with airstrip) large enough to accommodate 109 trailers. To this end, soil would be dug up from the center of the property and used to raise the elevation of the surrounding land above the 100-year floodplain. (T. 47) The applicants have a dredging permit from the Department of Environmental Regulation authorizing them to excavate 629,889 cubic yards. They are proposing to dig to a depth of 76 feet below ground. This would create an 18-acre body of water ("Poe's Lake") which would overflow a V-notched weir into a county canal. The county canal would take the water to C- 38, one of the large canals to which the Kissimmee River has been relegated, at a point about 18 miles upstream from Lake Okeechobee. Runoff would wash over residential lots and roadways; the site would be graded to assure drainage into Poe's Lake. The minimum road crest elevation would be 30 feet NGVD ("[a]round twenty-nine feet" T.52), as compared to the control elevation for surface waters of 28.5 feet NGVD. WATER QUALITY The developers plan septic tanks for wastewater treatment. At the close of all the evidence, counsel for the applicants stated that sanitary sewers could be installed instead. Respondents' Proposed Recommended Order, p. With all the housing units in use, at least 10,900 gallons of effluent would seep into the ground from the tanks daily. There would be some evapotranspiration, but all the chemicals dissolved in the effluent would eventually end up in the groundwater. During the dry season, septic tank effluent would cause mounding of the groundwater and some groundwater movement toward, and eventual seepage into, Poe's Lake. The eventual result would be eutrophication and the growth of algae or macrophytes on the surface of Poe's Lake. This would cause dissolved oxygen violations in Poe's Lake. Discharges from the lake would inevitably occur, aggravating the situation in C-38, which already experiences dissolved oxygen levels below 5.0 milligrams per liter in the rainy summer months. Some fraction of the nutrients in the effluent from the septic tanks would ultimately reach Lake Okeechobee itself. The sheer depth of the excavation would create another water quality problem. Under the anaerobic conditions that would obtain at the bottom of Poe's Lake, bacteria acting on naturally occurring sulfates would produce hydrogen sulfide, ammonia and various other reduced organic nitrogen compounds. These substances are toxic to human beings and would, in some indeterminate quantity, enter the groundwater from Poe's Lake. This would affect the taste and perhaps the potability of water from any well nearby. It would be "possible to design a better system where there would be nutrient removal and a greatly reduced probability of violation of the dissolved oxygen criterion and obviation of the potential for ground water contamination." (T. 200) Installation of a baffle on the weir would serve to prevent buoyant debris from entering surface waters of the state. BASIS OF REVIEW Official recognition was taken of the "Basis of Review for Surface Water Management Permit Applications Within the South Florid Water Management District," parts of which all parties agree pertain in the present proceedings. Among the criteria stated in this document are: 3.1.3 Waste and Wastewater Service - Potable water and wastewater facilities must be identified. The Applicant for a Surface Water Management Permit must provide information on how these services are to be provided. If wastewater disposal is accomplished on-site, additional information will normally be requested regarding separation of waste and storm systems. 3.2.1.4 Flood protection - Building floors shall be above the 100 year flood elevations, as determined from the most appropriate information, including Federal Flood Insurance Rate Maps. Both tidal flooding and the 100 year, 3 day storm event shall be considered in determining elevations. b. Commercial and industrial projects to be subdivided for sale are required to have installed by the permittee, as a minimum, the required water quality system for one inch of runoff detention or one half inch of runoff retention from the total developed site. State standards - Projects shall be designed so that discharges will meet State water quality standards, as set forth in Chapter 17-3, Retention/detention criteria - Retention and/or detention in the overall system, including swales, lakes, canals, greenways, etc., shall be provided for one of the three following criteria or equivalent combinations thereof . . . Wet detention volume shall be provided for the first inch of runoff from the developed project, or the total runoff from a 3-year, 1-hour rainfall event, whichever is greater. Dry detention volume shall be provided equal to 75 percent of the above amounts computed for wet detention. Retention volume shall be provided equal to 50 percent of the above amounts computed for wet detention. 3.2.4.1 Discharge structures should include gratings for safety and maintenance purposes. The use of trash collection screens is desirable. Discharge structures shall include a "baffle" system to encourage discharge from the center of the water column rather than the top or bottom. 3.2.4.4.2 b. Control elevations should be no higher than 2 feet below the minimum road centerline elevation in the area served by the control device in order to protect the road subgrade. Simply detaining runoff before discharging it offsite will not insure that the water quality standards set forth in Chapter 17-3 will be met. Whether the standards are met depends on, among other things, the composition of the runoff. FWF'S INTEREST Among the purposes of the FWF, as stated in its charter, Shall be to further advance the cause of conservation in environmental protection, to perpetuate and conserve fish and wildlife, oil, water, clean air, other resources of the State and so manage the use of all natural resources, that this generation and posterity will receive the maximum benefit from the same. (T. 248-9) Four or five thousand Floridians belong to FWF. FWF members "make use" (T. 250) of the waters of Lake Okeechobee, the Kissimmee River and specifically of the waters in C-38. PROPOSED FINDINGS CONSIDERED The applicants and FWF filed post hearing memoranda and proposed recommended orders including proposed findings of fact which have been considered in preparation of the foregoing findings of fact. They have been adopted, in substance, for the most part. To the extent they have been rejected, they have been deemed unsupported by the weight of the evidence, immaterial, cumulative or subordinate.
Recommendation Upon consideration of the foregoing, it is RECOMMENDED: That SFWMD deny the pending application for surface water management permit. DONE and ENTERED this 29th day of November, 1983, in Tallahassee, Florida. ROBERT T. BENTON II, 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 November, 1983. COPIES FURNISHED: Dennis J. Powers, Esquire Gunster, Yoakley, Criser & Stewart 400 South County Road Palm Beach 33480 Terrell K. Arline, Esquire 325-C Clematis Street West Palm Beach, Florida 33401 Irene Kennedy Quincey, Esquire 3301 Gun Club Road West Palm Beach, Florida 33406 Charles P. Houston, Esquire 324 Datura Street, Suite 106 West Palm Beach, Florida 33401
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.
Findings Of Fact Petitioner seeks to irrigate 450 acres of pasture land. In preparing its application Petitioner consulted the soil conservation office to obtain the amount of water required under extreme drought conditions. Petitioner's maximum pumping capacity is 2,500 gallons per minute, 108 million gallons per month, or 5.56 gallons per acre per minute. The longest period in which applicant recalls running its pumps continuously was 3 weeks. This occurred during a drought period and after the pumps had been out of operation for an extended period. During normal drought conditions Petitioner would expect to run its pumps 18 days per month. At the pumping capacity available to Petitioner this would amount to 64.8 million gallons of water per month. The maximum monthly allocation recommended by Respondent was 66 million gallons. The source of water from which an allocation is sought is the Florida aquifer and none of the water removed therefrom by this Petitioner will return. The Florida aquifer for which the water herein requested will be obtained is presently being mined, i.e. more water is being withdrawn therefrom than is going back into the aquifer. In evaluating the application the C&SFCD engineer took the 30 to 40 years annual rainfall, the consumptive water use for the crops to be grown and the difference between these figures as the annual supplemental irrigation required. Correcting these figures for evapotranspiration rates and allowing for drought conditions occurring 2 out of 10 years the figures of 66.5 million gallons, or 263 acre feet per month maximum usage was reached. Respondent proposed two special conditions upon the Petitioner. One, that Petitioner submit a water quality analysis from the pump discharge in May and October of each year. The second condition was that a measuring device be installed upon the pump to measure the amount of water pumped. The water quality analysis will cost Petitioner approximately $70 per year for the test alone. An hours of operation clock on the pump will suffice for the water measuring device.
The Issue The issue for consideration in this case is whether the Respondent, Hi Hat Cattle and Grove, should be issued water use permit 204387.03, to withdraw groundwater from the wells on its property, and if so, in what amount and under what conditions.
Findings Of Fact At all times pertinent to the issues herein, the Respondent, District, was the state agency responsible for the permitting of consumptive water use within its area of geographical jurisdiction. The Respondent, Hi Hat, is a family owned farming and ranching operation in eastern Sarasota County with water wells on its property. The Intervenor, City of Sarasota, is a municipality in Sarasota County which operates wells in the general area of those operated by Hi Hat, and which has an agreement with Hi Hat for the latter's use of treated wastewater pumped from the city's treatment plant to Hi Hat Ranch. The Petitioner, Wyatt S. Bishop, Jr., is a property owner and resident of Sarasota County whose property is located near the Hi Hat Ranch, and whose potable water is drawn from a well on his property which utilizes both the surficial and intermediate aquifers which are penetrated by the wells on Hi Hat Ranch. Hi Hat Ranch consists of 11,000 acres owned by Hi Hat Cattle and Grove, the family owned business which operates it, and an additional 3,227 acres leased from the City of Sarasota. Agricultural operations, including citrus farming, truck farming, sod farming, and grazing have been conducted on the ranch since the mid 1940's. In February, 1990, Hi Hat applied to the District for a permit to withdraw and use water from some 14 wells located on its property. It requested an annual average of 6,267,000 gallons per day, (gpd), and a peak monthly rate of 32, 668,000 gpd. Upon receipt by the District, the application was assigned a number, (204387.03), and was submitted for evaluation by the District staff for conformity with applicable District rules and policies. When the staff evaluation was completed, the District issued a staff report and proposed staff agency action in which it indicated its intention to issue a permit authorizing water to be drawn from the wells at a rate of 6,570,000 gpd, average annual, a peak monthly rate of 14,300,000 gpd, and a maximum daily rate of 5,210,000 gpd. In conducting its evaluation, the District staff relied upon the District's Basis of Review For Water Use Permit Applications which contains within it the provision for use of a "water use model" in assessing the need and appropriateness of water withdrawal amounts. This model, known as the Blaney- Criddle Model considers numerous factors in the evaluation, including rainfall, soil characteristics, irrigation methods used, and proposed crop types, all in an effort to determine a reasonable estimate of the applicant's supplemental water needs. Hi Hat's application was evaluated primarily by Marie Jackson, a Hydrologist III employed by the District, and an expert in hydrology, who has, over the years, reviewed between 350 and 400 permit applications, of which approximately 90 percent have been for agriculture. She is, therefore, quite familiar with the specifics of agricultural water use needs. Her evaluation of Hi Hat's application was done in the same manner as the others she has done and utilized the same tests, measurements and factors for consideration in arriving at her conclusion. In its application, a renewal with modification sought to increase average annual quantities due to a change in crop plans, Hi Hat indicated that its criteria for water use was based on certain agricultural uses and application rates. These included: low volume under tree spray irrigation of 778 acres of citrus at an application rate of 17.2 inches/year plus one inch/year for frost and freeze protection. open ditch irrigation of 135 acres of sod at an application rate of 30 inches/year. open ditch irrigation of 1,367 acres of improved pasture at an average application rate of 26.6 inches/year. overhead spray irrigation of 1,200 acres of improved pasture at an application rate of 20.3 inches/year. open ditch irrigation of 110 acres of spring peppers at an application rate of 30.0 inches/crop, and open ditch irrigation of 110 acres of fall peppers at an application rate of 45.2 inches/crop. Applicant also stipulated that the peak monthly quantities that it requested would be utilized for pasture, sod and citrus irrigation during the month of May. The proposed maximum quantities were for frost and freeze protection of citrus only. In January, 1989, Hi Hat entered into a contract with the City of Sarasota under which the City was obligated to deliver reclaimed water from its wastewater treatment plant to a "header" located on the ranch which thereafter distributes the water through pipes to "turnouts" located at various high points on the property. From these, the water is then discharged into a system of ridges and furrows for distribution of the water across the needed area. The reclaimed water is used to irrigate approximately 5,403 acres of ranchland. The Contract provides for minimum and maximum amounts of water to be delivered as well as for water quality standards which must be met. In periods of adequate rainfall, when irrigation is not required, any treated wastewater which is not needed is stored in a 185 million gallon holding pond on City property located adjacent to the ranch. When needed, water can be fed into the wastewater distribution system described above from the holding pond. This reclaimed water, whether from the pond or direct from the header, can also be utilized to irrigate citrus crops, but this requires a filter system which has not yet been able to operate properly. Therefore, no reclaimed water has yet to be utilized for citrus irrigation on the ranch. At an average annual flow of 6.2 million gallons per day, the pond has the capacity to hold enough treated water for almost 30 days. Not all wells on Hi Hat Ranch are active wells. Several of the wells are classified as standby wells which are intended to be used only to back up the reclaimed water delivery system and are located, normally, beside the "turnouts." In the event the reclaimed water is not available from the city, the standby wells can be utilized to provide water to the ridge and furrow system used to irrigate pasture land. The standby wells are numbers 1, 6, 7, 11, 13, 14, and 15. Well number 5, also identified as a standby well in the staff report and in the draft permit was mistakenly so identified. The draft permit contains several special conditions which impact on the drawing of water under the terms of the permit. Significant among these is Special Condition 33 which prohibits the withdrawal of water from any of the standby wells unless the reclaimed water supply from the city is interrupted. Special Condition 27 requires the installation of a flow meter on any standby well that becomes active as a result of permanent discontinuance of the reclaimed water supply. With regard to flow meters, Special Condition 22 requires flow meters on all of Hi Hat's wells. Ms. Jackson, however, indicated this was in error and has recommended that the standby wells be deleted from that Special Condition. When that is done, only those wells actively producing water on a regular basis would require the installation of flow meters. In its analysis of the application for permit, the District staff considered several factors pertinent to the impact the well would have on the water supply in the area and its effect on other users. These factors include hydrologic impacts, well condition, the history of water use at the ranch, the reliability of the reclaimed water system and its ability to provide a uniform source, and the city's water reuse policy. Addressing each individually, and starting with the hydrologic impact of the withdrawal of the requested amounts, the District considered the nature of the existing wells and how they are constructed and maintained. The District assumed, because the data regarding the construction of the existing wells was incomplete and insufficient to properly disclose the status of casing on each well, that they were shallow cased. As a result, the calculations incorporating this assumption indicate a situation that would occur in its most aggravated form. The parties agreed that Hi Hat's wells are shallow cased and probably go no deeper than 90 feet. To determine, as much as possible, the projected drawdowns in the surficial and intermediate aquifers that might be expected if Hi Hat withdrew the amounts of water proposed, the District utilized the "MODFLOW" computer model which factors in simultaneous peak withdrawals from all 14 of the wells along with a 90 day no rainfall drought condition. This, too, contributes to a worst case scenario, and the resultant figures are considered to be conservative estimates of the hydrologic impact of the water withdrawal. Notwithstanding, the application of this computer model resulted in the indication that, as to the surficial aquifer, the drawdown at Mr. Bishop's property located approximately one half mile from the ranch border, would be no more than .055 feet. Since normal fluctuations in the surficial aquifer during the course of the year can be as much as 6 feet, the projected drawdown as a result of Hi Hat's withdrawals was considered insignificant. Applying the same assumptions and utilizing the same computer model as it relates to the intermediate aquifer resulted in an indication of a drawdown of no more than 2.3 feet at Mr. Bishop's property. Since annual fluctuation in the intermediate aquifer can range from 15 to 20 feet normally, the District considers that any reduction of less than five feet in the intermediate aquifer is insignificant. The permit held by Hi hat currently allows for the withdrawal of more water than would be withdrawn under the proposed permit as conditioned and is consistent with the proposed reduction in allowable withdrawals. Considering that factor, as well as the prohibition against withdrawals from standby wells as long as reclaimed water is available, the actual impact of the water withdrawals consistent with the proposed permit would be substantially less than the computed prediction which includes production from all wells. Drawdown contours are defined across the entire effected area. One of the levels is a 4 foot contour, and when a computer simulation indicates that the 4 foot contour includes a withdrawal previously or otherwise permitted, the District will generally conduct a cumulative impact analysis. In this case, however, since there was only one golf course well within the area circumscribed by the 4 foot contour line, and since this withdrawal was too small to have effected an evaluation, it was not done. The condition of the wells on the Hi Hat Ranch has some bearing on whether or not the application for additional withdrawal of water should be granted. These wells are almost 30 years old, having been drilled in the 1960's. As a result, there is little information available regarding their construction detail. This is not necessarily unusual for agricultural wells, and there is evidence that there are many similar wells in use within the District. The reason for this is that at the time the wells were drilled, information regarding their depth, casing and other matters were not required to be kept or reported. However, there is no indication the wells are in any way violative of well construction criteria and their use has been authorized continuously since 1977. When he prepared Hi Hat's application, Mr. Turner included much the same information regarding the wells as pertains as to depth and diameter which he had previously submitted in earlier applications and which had been accepted. In each case, casing depths had been reported as unknown. Notwithstanding the information contained in some old well logs relative to only a few of Hi Hat's wells, this information is in no way definitive and it is difficult to describe anything specific with the majority of these wells. Nonetheless, as already found, it is stipulated that most are approximately 90 feet deep. It is reasonable to assume that the existing wells, however, are cased only to a shallow depth, and that in many cases, the existing casings have corroded away, either totally or in part. This can cause an intermixing of water from the separate aquifers, but whether this is in fact happening depends upon factors specific to that particular well. Petitioner did not present any evidence to show that as a result of the condition of Hi Hat's wells, any degradation is occurring in the more potable, surficial aquifer as a result of intermixing with water from the intermediate aquifer on or around the Hi Hat Ranch. In Ms. Jackson's opinion, and there appears to be no evidence to contradict it, the amount of drawdown which would occur as a result of maximum pumping at Hi Hat Ranch would not be sufficient to cause poorer quality water from the Floridan aquifer to percolate upward (upcone) into the better quality water of the two upper aquifers even during drought conditions. By the same token, there is no evidence that drawdown would encourage or permit salt water intrusion. Petitioner attempted to show by the records kept on the various Hi Hat wells that many of them have been abandoned and are no longer operative and should not be allowed to fall within the parameters of this permit. He testified clearly that over the years, the level of water in his potable water well has lowered and presumed that this was the result of increased water usage by other entities which draw from the aquifer into which his well is sunk. Water level, however, depends upon numerous factors, of which usage is only one. Others include recharging of the aquifer and the amount of rainfall and other recharge sources not only in the immediate area but across the large area which feeds the aquifer. Mr. Bishop did not present any evidence showing a causal connection between the lowering of the water in his well, or the degradation in water quality he claims to have experienced, and either the drawdown caused by Hi Hat's operation or by aquifer intermixing. He indicated, and it is not disputed, that within the past year, he has had to take measures to improve the water quality in his potable well, but, again, he has not presented any evidence to show this was caused by Hi Hat's ground water withdrawals. In its long range planning, the District intends to implement a program to rehabilitate old wells, and when that program is implemented, almost every agricultural well within the District may require recasing or redrilling. This program will not be implemented for several years, however. In an effort, however, to insure that all reasonable precautions are taken to see that approval of any petition for withdrawal does not have an unacceptable adverse impact on the water needs of the surrounding community, in its analysis of this application, and in all cases, the District makes certain assumptions when adequate empirical data is not available. In this case, pertaining to the unavailability of information regarding Hi Hat's wells, the District assumed that all wells were shallow cased, and this placed the application in the worst possible light. Shallow cased wells allow more upconing and aquifer intermixing. Nonetheless, the amount of water permitted to Hi Hat, even if not used, could impact on Mr. Bishop and other adjoining owner's use of additional water as a result of a possible change to their permitted quantities. However, to compensate for this, the District has also included a special condition, (#26), which requires Hi Hat to log all 14 of its wells within the term of the permit, (7 years), which will require at least 2 wells be done each year. The cost of that action will be between $800 and $2500 per well. Another condition, (#31), requires Hi Hat to look into any complaint from adjacent property owners regarding adverse impacts due to water withdrawal, to report the results of its inquiry to the District, and to mitigate, as much as possible, all adverse impacts due to its withdrawal. Mr. Bishop claimed, and introduced evidence purporting to demonstrate, that many of the wells on the Hi Hat Ranch, which are covered by the permit applied for here, are no longer in use and have been abandoned. In response, Mr. Turner, who has been actively engaged in the ranch's operations for at least the past four years, indicates from his personal knowledge, that all 14 wells included in the permit applied for have been operated within the past two years, and all are capable of producing water. It is so found. Not all wells, however, have been operated at all times. Crop rotation and a varying need for groundwater has resulted in some wells not being used at some times. This is, of course, commonplace in agriculture and to be expected as a result of crop planning programs. Admittedly, an accurate figure for the amount of water which has been withdrawn from the 14 wells cannot be established because these wells do not have, and were not required to have, flow meters. Two of the wells were fitted with hour meters in January, 1989, but because the capacity of the pumps on those wells is variable, a precise estimate of volume pumped cannot be determined. The meters measured only the number of hours the pumps were in operation and not the amount of water passed through the pumps. Evidence was presented, however, to show that wells have been utilized at the ranch since the 1960's, and in 1977, some 14 years ago, following District implementation of a consumptive water use permit program, the ranch first applied for water withdrawal permits. These permits have been renewed as required and all water usage since the implementation of the program has been permitted. Turning to the reclaimed water supply, the delivery system, incorporating a program to pump reclaimed water from the treatment plant all the way back out to the ranch site, is subject to material failure and operator error, and either one can occur at any number of places along the system route. Each could result in interruption of the delivery of the reclaimed water to the ranch. The system is far more complex than would be the use of on-site wells for delivery of ground water. One two week shutdown in the system was occasioned by a major pipe failure as a result of pressure building up in the pipes. Were it not for the fact that a contractor was already at the ranch with replacement parts on hand to effect expeditious repair of the system, the shutdown could have lasted considerably longer than it did. This is not the only interruption, however. Several main line leaks and valve problems have caused the system to be shut down on several occasions for short periods of time. The filter system required for the water destined for the citrus area is problematical, and so far this area of the ranch has not received any reclaimed water in the 10 months the system has been in operation. Mr. Bishop argues that the wet weather holding pond is a solution to the reliability problems with the pipe line, but the pond has had problems of its own. Sand in the water, which comes from the holding pond, has been the primary difficulty in the filter system for the citrus area, and algae growth in that pond has the potential to create other filter problems. Delivery of the water from the pond is not accomplished by a gravity system, but instead, requires the use of pumps powered by an electric motor. In the event of a power failure, this source would be unavailable. Discounting all of the above, however, and assuming, arguendo, that all systems were in top operating condition, the fact remains that the delivery system from the pond to the distribution system is not adequate to supply the amount of water that would be necessary to have an effective freeze protection program. In any case, the reclaimed water supply is not the panacea for all water shortage problems experienced at Hi Hat Ranch. In the first place, the quality of the reclaimed water is generally lower than that of the groundwater which would come from wells on the ranch. Also, the City's treatment process does not remove from the water all the pollutants that are of concern to the farm operators. For one thing, total dissolved solids in the reclaimed water are considerably higher than in the ground water, and high dissolved solid levels can be harmful to citrus crops. In fact, the Institute of Food and Agricultural Sciences recommends that citrus irrigation water not exceed total dissolved solid ranges of from 1000 to 1500 milligrams per liter, (mpl). Testing done on the reclaimed water delivered to Hi Hat Ranch showed it averaged between 1200 and 1500 mpl. Though within recommended parameters, it was toward the high end. Further, reclaimed water is not totally interchangeable with ground water for all agricultural purposes. It cannot, by law, be applied to certain types of ground crops such as melons, nor can it be used for overhead citrus irrigation. There is also a restriction on the use of reclaimed water for pastures on which dairy cattle will be grazed. This all results in a restriction on the options available to the farmer who chooses to use reclaimed water in his irrigation plan. As a result, many farmers try not to use reclaimed water if they have access to adequate amounts of groundwater from on- site wells. Notwithstanding all the above, the parties agree that the use of reclaimed water for irrigation purposed is in the public interest. The District encourages it but nonetheless concedes that even with the availability of reclaimed water, a farmer should have access to wells on his property, in a standby capacity, as an alternative source of water to support his farming activities. Not only that, the agreement between the City and Hi Hat provides for Hi Hat to maintain its water use permit even while receiving reclaimed water from the City. Hi Hat is not the only farm operation with whom the City has negotiated in a effort to expand its wastewater distribution program. It has found in those negotiations, that most farm producers are not willing to rely totally on reclaimed water for all their irrigation needs, and it has concluded that were it mandatory that a farmer give up his on-site ground water withdrawals in order to utilize reclaimed water for a part of his needs, most would be reluctant to use it at all. This would seriously interfere with the City's ability to dispose of its surplus reclaimed water consistent with its policy. Even though Hi Hat's property lies within the Eastern Tampa Bay Water Use Cautionary Area, the rule pertaining thereto is inapplicable to Hi Hat because Hi Hat filed its application for permit, which was deemed complete, prior to the adoption of the rule. Nonetheless, water use officials agree that the proposed permit is consistent with the rule emphasis on the use and reuse of reclaimed water, and the District does not object to backup wells being permitted as supportive of the District's desire to keep ground water within the ground.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that Hi Hat Cattle and Grove be issued water use permit No. 204387.03, within the limits of the authorized quantities as indicated in the intent to issue, subject to conditions contained therein; except that the permit be amended to show well No. 5 as a non-standby well, and to delete standby wells from the terms and requirements of Special Condition 22. RECOMMENDED this 17th day of May, 1991, in Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 17th day of May, 1991. APPENDIX TO RECOMMENDED ORDER The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONER: Accepted Accepted and incorporated herein. Accepted and incorporated herein. - 6. Accepted and incorporated herein. 7. - 11. Accepted. - 15. Accepted and incorporated herein. Accepted. Accepted. & 19. Accepted and incorporated herein. - 22. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. - 28. Accepted and incorporated herein. Accepted and incorporated herein. Rejected. She testified that Condition 28 of the permit provides this. Accepted. Accepted. Accepted and incorporated herein. Accepted. & 36. Accepted. Rejected as not supported by the evidence except that the method permitted was the method being used. - 40. Accepted. Ms. Jackson indicated she "assumed" some wells were drilled into the Florida aquifer. Rejected. Accepted as qualified by the comment, "depending on the respective potentiometric heads." - 47. Accepted. Accepted but incomplete. This is because they did not feel it was necessary under the circumstances. - 51. Accepted. Accepted. Accepted. Accepted. Accepted. Accepted and incorporated herein. Accepted. Redundant. - 61. Accepted. - 66. Accepted and incorporated herein. Accepted. More a restatement of testimony than a Finding of Fact Accepted and incorporated herein. & 71. Accepted and incorporated herein. - 74. Accepted. Accepted. First sentence accepted. Second portion rejected since cited case involves active wells versus standby, as here. The comparison made is accepted. The conclusion drawn as to validity is rejected. & 79. Accepted. FOR THE RESPONDENTS AND INTERVENOR: & 2. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. & 6. Accepted and incorporated herein. 7. - 10. Accepted and incorporated herein. 11. - 13. Accepted and incorporated herein. - 17. Accepted and incorporated herein. Accepted. Accepted. Accepted and incorporated herein. Accepted and incorporated herein. & 23. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence. 27. Accepted. 28. & 29. Accepted and incorporated herein. 30. - 33. Accepted and incorporated herein. 34. - 37. Accepted and incorporated herein. 38. Accepted. 39. Accepted. 40. - 42. Accepted and incorporated herein. Accepted and incorporated herein, & 45. Accepted. 46. & 47. Accepted and incorporated herein. COPIES FURNISHED: Wyatt S. Bishop 5153 Tucumcari Trail Sarasota, Florida 34241 Bram D.E. Canter, Esquire Haben, Culpepper, Dunbar & French, P.A. 306 N. Monroe Street Tallahassee, Florida 32301 Edward B. Helvenston, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Barbara B. Levin, Esquire de la Parte & Gilbert 705 East Kennedy Blvd. Tampa, Florida 33602 Peter G. Hubbell Executive Director SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
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.
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.
The Issue Whether General Water Use Permit (WUP) Number 20012185.000 (Permit) meets the conditions for issuance as established in Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, and should be issued to Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc.
Findings Of Fact The Parties DCAP is not-for-profit corporation incorporated in the State of Florida. Behrens is the President of DCAP. See also Findings of Fact 63-77. Farmland Hydro is a Delaware Limited Partnership authorized to transact business in Florida, and is the owner of the property leased by Basso/Redland, which is the subject of this WUP. Frank T. Basso, Jr., is a third generation farmer, who operates as Redland Growers Exchange, and seeks a General WUP to authorize groundwater withdrawals for crop irrigation. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries pursuant to Chapter 373, Florida Statutes, and the rules promulgated thereunder as Chapter 40D, Florida Administrative Code. The Proposed Water Use An Application for a General WUP was submitted by Farmland Hydro and Basso, as co-applicants, and received by the District on April 11, 2001. After receipt of additional information, the Application was deemed complete on October 22, 2001. The Applicants seek a General WUP to authorize a new water use for the irrigation of 140 acres for the production of both Spring and Fall row crops, using a seepage-with-mulch irrigation system.1 Basso plans to grow tomatoes and/or peppers in the Spring, and squash and/or cucumbers in the Fall. Crop planting for both seasons will be phased-in over a one-month period. Water allocation quantities are calculated on a weekly phase-in basis of approximately 35 acres for each planting date. The total time that the parcel will be in use for farming, to include planting and harvesting for each crop, is approximately six months per year. The subject parcel is part of a 250-acre tract known as the Brushy Creek Tract and is located in Hardee County approximately two miles south of the town of Ona; approximately two miles south of the intersection of U.S. Highway 64 and County Road 663; and is within the Southern Water Use Caution Area (SWUCA). The subject parcel currently does not contain a water well. The Brushy Creek Tract is a larger parcel of approximately 1,230 acres leased from Farmland Hydro by Redland and also by Parker Farms for cattle grazing, farming, and hunting. The subject parcel is used for cattle grazing and is surrounded by land owned by Farmland Hydro and used for either cattle grazing or agricultural row crops. Farmland Hydro also operates an additional approximately 1,941 acres of property near the subject parcel, which is used for citrus groves. Farmland Hydro has consumptive WUPs for this property. The closest existing legal user to the proposed Basso well site is another well on the Farmland Hydro property. As is generally done with vegetable crop production in Florida, vegetable crops grown on the Farmland Hydro property are grown in rotation with pasture, and have been rotated in this manner for many years. Typically, farmers have farmed a piece of land for one, two or three years and then, to avoid the buildup of insects and diseases, have allowed the land to revert to pasture and have moved on to another field for crop production. The subject parcel for which the WUP is being sought will be similarly treated. Crop rotation is an important agricultural best management practice that is used to address pest management, soil conservation, and maximizing nutrients for obtaining favorable crop production. Soil conservation is important to Basso, notwithstanding that there is a response in the Application that no approved Soil Conservation Service plan exists for the operation included in the Application. If the WUP is issued and the subject parcel is placed into crop production, another parcel of land will be taken out of crop production by Basso, resulting in the discontinuation of another permitted well. As a result, the issuance of this WUP will not result in a "water use change." Determination of Reasonable Demand/Allocated Quantities In determining whether a proposed water use is reasonable-beneficial and in the public interest, the District calculates the appropriate permit quantities for the particular water use, which is a function of demonstrated need, or demand for water; efficiency of the water treatment and distribution systems; whether water is sold or transferred to other entities; whether acceptable water can be acquired from lower quality sources; and whether conservation practices are employed. District Basis of Review (BOR), page B3-1. The reasonable need for agricultural water use is generally composed of one or more demand components, depending upon the specific agricultural use. "Typically, the reasonable need for irrigation water uses is equal to the supplemental crop requirement divided by the system efficiency or the system design capacity, whichever is less." "The supplemental crop requirement is the amount of water needed for a particular crop beyond the amount of water provided by effective rainfall." The supplemental crop requirement is generally determined by using the Agricultural Water Use Calculation Program (AGMOD) Version 2.1, which is based on the modified Blaney-Criddle method. This program takes into account site specific information such as crop type, growing period, evapotranspiration rate, soil type, rainfall, irrigation method and number of irrigated areas. "In most cases, the supplemental irrigation requirement is determined for a 2 in 10-year drought condition." The AGMOD program determines an inch-application rate which, when applied to the number of acres to be irrigated, results in a calculation of total annual average and peak monthly quantities for the proposed water use. District BOR, pages B3-4 and 3-5. See also District Water Use Design Aids, pages C4-1 through C4-7. In determining the allocated quantities, or reasonable demand for water, the District seeks to avoid both over- allocating water and under-allocating water for the specific crop intended, to ensure that the permitted amount is sufficient for the "2 in 10-year drought condition." Consequently, the allocated quantities arrived at by District staff through use of the AGMOD methodology may be different from the quantities indicated on an applicant's initial application, which are generally estimated without benefit of an agricultural water use calculation program. The AGMOD program was used to calculate water use quantities for the proposed water use. The allocated quantities for Basso's proposed use are 454,000 gallons per day (gpd) on an annual average basis and 1,241,000 gpd, as a peak month quantity. No quantities were requested or allocated for crop protection. See Finding of Fact 52. Modeling for Simulated Impacts As part of the application review process, the District evaluates potential impacts to existing legal uses of water, the water resources and environmental features that may result from the proposed groundwater withdrawals. To assist in the review process, analytical and numerical models, which incorporate best available hydrogeologic parameters for the area being considered for a permit, are used to simulate drawdowns for the withdrawal of the proposed quantities. The results of these simulations are used in the evaluation of potential impacts to assess whether the application meets the conditions for issuance. The District undertook simulation modeling of the potential effects of the proposed water withdrawals to be authorized by the permit. The allocated quantities were entered into the MODFLOW 387 groundwater flow model, which is a three- layer model developed by the U.S. Geological Survey and is the generally accepted model for this purpose. Model layers were set up to represent the surficial, intermediate, and Upper Floridan aquifers. (The Applicants seek to pump water solely from the Upper Floridan Aquifer.) There are limitations to the model in that the model assumes a homogeneous isotropic aquifer, with no preferred flow direction. In actuality, there is variability in the geology of the area. Modeling is intended to serve as a screening tool for assessing localized impacts anticipated from a proposed water use and is based upon the best available information. As distance from the proposed withdrawal site increases, the reliability of the modeling decreases, due to the variability in the geology and other parameters or boundary conditions that can affect the model. Use of the MODFLOW groundwater model allows the District to look at potential impacts at the site, and in the proximity of the site, and assists the District in assessing possible cumulative impacts associated with a proposed use. To assist in assessing potential impacts from the proposed use, a Peak Month modeling simulation was undertaken by the District, which simulates the effect of pumping the proposed Peak Month withdrawal rate of 1,241,000 gpd for 90 consecutive days, with no recharge to the aquifer systems. The model essentially presents a worst case scenario that is a more severe prediction than what is actually likely to occur from the permitted use under normal conditions. Simulating the period of greatest demand on the hydrologic system is likely to provide maximum protection to existing legal water users and the water resources. The Peak Month simulation undertaken by the District predicts drawdowns in the potentiometric surface of the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site; less than 1.4 feet at the nearest property boundary (approximately 1,250 feet from the proposed withdrawal site); and less than 1.2 feet at the nearest existing legal user (a Farmland Hydro well approximately 3,500 feet from the proposed withdrawal site). These numbers did not raise a concern for District staff. ("Potentiometric surface" is "a surface defined by the level to which water rises in an open pipe that is constructed into or all the way through an artesian aquifer. This is measured in feet relative to NGVD or sea level. The level to which water rises inside this open pipe is a function of the pressures on the water in the artesian aquifer." District BOR, page B-xii.) The Peak Month simulation predicts drawdowns in the intermediate aquifer of approximately 0.9 feet at the proposed withdrawal site, and less than 0.9 feet at the property boundary, and at the nearest existing legal user. The Peak Month simulation predicts drawdowns in the water level of the surficial aquifer (water table) of approximately 0.01 feet or less at the proposed withdrawal site, property boundary and nearest existing legal user. Based upon the Peak Month simulations, the District reasonably determined that further cumulative impact modeling was not necessary in order to assess localized cumulative impacts resulting from the proposed use. To assess regional cumulative impacts, the District evaluated Regional Observation Monitoring Program (ROMP) data and found no significant trends in withdrawals in recent years, other than a slight decline attributed to the recent drought. Conditions of Issuance of the Proposed Permit In order to obtain a water use permit, an applicant must establish that the proposed use of water is a reasonable- beneficial use, will not interfere with any existing legal use of water, and is consistent with the public interest, by providing reasonable assurance, on both an individual and cumulative basis, that the water use meets the conditions for issuance as specified in Section 373.223(1), Florida Statutes, and Rule 40D-2.301, Florida Administrative Code. A permit must be obtained from the District prior to withdrawing water, where the withdrawal is from a well having an outside diameter of six inches or more at land surface, where the annual average withdrawal from all sources is 100,000 gpd or greater, or where the total combined withdrawal capacity from all sources is greater than or equal to 1 mgd. The proposed water use falls within these parameters. Rule 40D-2.041(1)(b) and (c), Florida Administrative Code. The quantities allocated for the proposed use have been determined by the District to be necessary to fulfill a certain reasonable demand, for the reasons specified herein. To assist in assessing impacts, the District utilizes a network of ROMP wells to obtain basic groundwater monitoring data over time and to help characterize the lithology, stratigraphy, aquifer depths, water levels and, in some cases, water quality for the various water resources. Data obtained from the ROMP and other wells is compiled to ascertain aquifer characteristics within the District and is also integrated into the District's modeling efforts pertaining to proposed water uses. ROMP well No. 31 is located just off the northeast corner of the Basso site. Having a ROMP well adjacent to the Basso site increases confidence in the specific geological information being used in the groundwater model to assess potential impacts from the proposed uses. ROMP well No. 17 is located approximately 1/2 mile from DCAP member Behren's well. Data from both wells were considered in assessing potential impacts from the proposed water use. Based on available information, the possible sources of groundwater for the proposed use at the Basso site are the surficial aquifer, intermediate aquifer, and the Upper Floridan Aquifer systems. To ensure sufficient quantities of water for the proposed use and to avoid potential impacts to environmental features, such as wetlands and surface waters, the District will require the proposed use to limit withdrawals to solely the Upper Floridan Aquifer. By examining stratigraphic cross sectional information generated from the ROMP wells, particularly ROMP No. 31 well, which is in close proximity to the Basso site, District staff were able to determine, with reasonable certainty, the approximate depths of the aquifers at the Basso well site. To ensure that the well will be open solely to the Upper Floridan Aquifer, the permit requires the Basso well to have a minimum of 400 feet of casing, with an estimated well depth of 1,000 feet. Based upon available information concerning the construction of other wells in the vicinity of the proposed Basso well, the District is reasonably assured that a well cased for a minimum of 400 feet will draw water only from the Upper Floridan Aquifer and will minimize the potential for water to move between the aquifers through the well. The well construction requirements imposed for Basso's well are in line with the best available stratigraphic information and with known construction of wells in the area. By casing the well to a depth of 400 feet and due to the extremely low leakage of the intermediate confining unit, the intermediate and surficial aquifers will be buffered from impacts associated with the proposed use. The District will deny a water use permit application if the proposed withdrawal of water, together with other withdrawals, would cause an unmitigated adverse impact on a legal water withdrawal existing at the time of the application. The District considers an adverse impact "to occur when the requested withdrawal would impair the withdrawal capacity of an existing legal withdrawal to a degree that the existing withdrawal would require modification or replacement to obtain the water it was originally designed to obtain." District BOR, page B4-14. Based upon an assessment of individual and cumulative regional information, there are no existing legal uses of water that will be adversely impacted as a result of the proposed withdrawals. Based upon an assessment of individual and cumulative regional information, no quantity or quality changes that adversely impact the water resources, including both surface and groundwaters, are anticipated from the proposed withdrawals. The District requires that consideration be given to the lowest water quality available, which is acceptable for the proposed use. Lower quality water includes reclaimed water, collected stormwater, recovered agricultural tailwater, saline water or other sources. District BOR, page B4-12. For the proposed water use, there is no viable lower quality water source and no reclaimed water available near the site to use as an alternative to groundwater pumping. The Applicants are proposing to use the lowest quality water that is available. There are no known concerns regarding the quality of water in the Upper Floridan Aquifer at this location in Hardee County. Restricting the proposed water use to the Upper Floridan Aquifer will not cause water quality concerns or result in pollution to any of the aquifers. Simulated drawdowns to the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site, less than 1.4 feet at the nearest property boundary, and less than 1.2 feet at the nearest permitted well, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the intermediate aquifer of 0.9 feet at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the surficial aquifer of 0.01 feet or less at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, constitute a nearly undetectable impact to the surficial aquifer, which is not an adverse impact. The modeling simulations demonstrate that the proposed withdrawals will have no significant effect on the surficial aquifer and, therefore, will not cause adverse impacts to environmental features such as wetlands, lakes, streams, fish and wildlife, or other natural resources. None of the simulated drawdowns are considered to be predictions of adverse impacts, not even in the localized vicinity of the well site. Mr. Jackson explained that because the localized modeling simulations were small or insignificant and showed no adverse impacts, cumulative modeling is not considered necessary. Reasonable assurance on a cumulative basis is determined by assessing the potential localized impacts in conjunction with existing cumulative data for the region, such as the available ROMP data and hydrographs, which depict the existing regional condition, taking into account, on a cumulative basis, all existing uses as well as rainfall conditions and climate. Based on an assessment of the cumulative data and the modeling for individualized impacts, and applying professional judgment, District staff reasonably concluded that the proposed water use presents no concerns that it will cause, on either an individual or a cumulative basis, adverse impacts to the water resource or existing legal uses. Minimum flows and levels have not been established by the District for the area where the proposed use is located. (The parties stipulated that the District has not established minimum flows and levels pursuant to Section 373.042, Florida Statutes, for the Southern Water Use Caution Area (SWUCA)). Therefore, Rule 40D-2.301(1)(d), Florida Administrative Code, (requirements for minimum flows and levels), is not applicable to the proposed permit. The proposed use presents no concerns for saline water intrusion. The proposed use raises no concerns regarding causing pollution to the aquifer. There are no offsite land uses that will be adversely impacted as a result of this permit. Basso currently uses best management practices for water conservation in his ongoing farming operations, and intends to use such practices with the new farming operation authorized under the permit. In keeping with such practices, irrigation is stopped when the water reaches the end of the watering ditch. Basso uses seepage irrigation and tries to regulate the ditches so that there is a minimum, if no, runoff. Also, a watering cycle generally lasts from three to seven days before irrigation has to be resumed. Any runoff goes into "filtering ponds, before reaching ditches or creeks" in its raw content. Basso does not intend to farm during months of likely frost so no separate allocation for frost/freeze protection was requested or needed. Given these irrigation practices, water is not reasonably expected to be wasted. All necessary and feasible agricultural water conservation activities will be implemented upon issuance of the WUP. In addition, Specific Condition No. 3 of the proposed WUP requires the incorporation of best water management practices in all irrigation practices. The proposed use presents no concerns that it will otherwise be harmful to the water resource. The Applicants have met all the requirements for issuance of a WUP. Southern Water Use Caution Area The proposed water use site is located within the SWUCA. The District established the SWUCA as a means of addressing on a regional scale concerns about long-term impacts to the water resource. Water use caution areas were created in recognition of regional water concerns. There have been drought conditions in the area which have caused reduced aquifer levels. The proposed water use site is not within the "Most Impacted Area" (MIA), which is located approximately 18 miles to the west of the site in Manatee County, nor within the "East Tampa Bay Water Use Cautionary Area" (ETB WUCA), which is approximately six miles to the west of the proposed site, also in Manatee County. (The SWUCA includes the MIA and ETB WUCA.) Pending final adoption of rules for the SWUCA, the District will continue to issue WUPs for proposed water uses that meet the conditions for issuance. The District cannot treat new uses and existing renewal uses any differently when considering the issuance of a permit. Once SWUCA rules and minimum flows and levels are established, the District expects to rely on a more regional approach to address long-term cumulative impacts over the entire use caution area, instead of relying on a permit-by-permit basis to address regional concerns. Standard Condition No. 9 of the proposed WUP requires the permittee to cease or reduce withdrawals as directed by the District, if water levels in the aquifers fall below the minimum levels established by the District Governing Board. The proposed withdrawal will use a seepage with mulch irrigation method, which has a 50 percent efficiency level. See footnote 1. This is the minimum efficiency level currently required for agricultural WUPs within the SWUCA, which approve the use of this irrigation method. As SWUCA rules come into effect, a higher percentage efficiency level probably will be required, as is now required in the Eastern Tampa Bay Water Use Caution Area and also in the Highlands Ridge Water Use Caution Area. Consequently, Standard Condition No. 11 of the proposed WUP requires that, when SWUCA rules are implemented, the permittee must comply with any higher efficiency level or other special regulation that may be required for the SWUCA area. DCAP's Challenge to the Proposed WUP DCAP does not keep official membership records. It does not maintain any list of current members. According to Behrens, there are five members of the board of directors. DCAP does not hold corporate meetings, annual meetings or maintain corporate records. Members do not meet. There are no means to document the existence of members for this organization. Behrens is a member of DCAP. He has owned five acres adjoining the west side of Horse Creek (in DeSoto County) since 1985. Behrens complains that the District does not look at the cumulative effect on his well and other people he knows, such as George Chase. Behrens is concerned with any lowering of the water level in the area, including Horse Creek. He believes that approval of wells in the area, including the proposed well, is the straw that is breaking the camel's back. Mr. Chase shares this view. Behrens relies on an artesian free-flowing, two-inch diameter well, for domestic water use, located in the intermediate aquifer, approximately 150 feet deep. (Behrens' well is approximately 18-20 miles from the proposed Basso well.) For most of the time he has lived there, the well had an electric pump for obtaining water. Approximately one year ago, the pump went bad, and a replacement system has not been installed. Currently, Behrens has no pump on the well, and in dry periods, has to obtain water for domestic uses from nearby Horse Creek, which is low during the dry season. (Behrens depends on Horse Creek to pursue his recreation, wildlife, and aesthetic values.) Having a flowing artesian well will enable him to obtain water from the well without having to install an electrical pump, a situation which is desired by Behrens, in part, because the property is in a flood plain and experiences frequent flooding and electrical outages. Not all artesian wells flow. Artesian wells are completed into confined aquifers in which the water in a tightly cased well, will rise to a level above the formation being measured. Water would have to rise above the land surface to be a flowing well. For a well to be artesian, the well must be under confined pressure. For a well drawing water from a confined aquifer, such as the intermediate or the Upper Floridan Aquifer systems, the measured water level in the well is a reflection of the amount of potentiometric pressure in the well. This level can be affected just as much by the amount of recharge as it can by the amount of water withdrawals. There is no evidence that the proposed water use will adversely impact the flowing nature of either Behrens' or Chase's well. The evidence demonstrates that the proposed water use will not adversely impact Behrens' well. George Chase is a member of DCAP. Mr. Chase lives in Arcadia, DeSoto County, Florida. His property is adjacent to the Peace River. Mr. Chase's well is a two-inch diameter well, believed to be about 150 feet deep and equipped with a 12-volt DC solar-powered pump. Mr. Chase has in the past relied on artesian pressure within the confined intermediate aquifer to supply water to his solar-powered home. The solar-powered pump assists in supplying water to the home. In recent years, Mr. Chase has experienced low water pressure in his well. In Spring 2000, Mr. Chase contacted the District to complain that when an adjacent citrus grove was irrigating the groves, it appeared to affect the water level in his well such that the well's ability to flow was impacted. (According to Mr. Chase, his neighbors have had problems obtaining sufficient water from their wells and reaching water with standard pumps.) This citrus grove is an existing legal user of water that pre-existed Mr. Chase's well. In recent years, numerous domestic wells have been constructed in the vicinity of the Chase home that are large diameter wells utilizing submersible pumps with 110-volt AC power. These wells are more efficient at producing water than the type of well and pump being used by Mr. Chase, are located within a few hundred feet of Mr. Chase's well, and are open to the intermediate aquifer as is the Chase well. Based upon the District's experience in other areas, where there is a cluster of domestic wells drawing from the same intermediate aquifer, such adjacent wells have a much greater impact on each other than do other more distant wells, such as the previously discussed citrus irrigation wells, that are open solely to the confined Upper Floridan Aquifer System. This conclusion is based upon monitoring of the ROMP sites in the affected areas. Mr. Chase's well is approximately ten miles from the proposed withdrawal site. There is no basis to conclude that the proposed water use will cause any adverse impacts to Mr. Chase's well. DCAP members' interests are not affected any differently by the proposed use than are the interests of the general public. DCAP has produced no evidence to support its assertion that the issuance of this permit will result in lowered water levels in the Horse Creek and Peace River or other surface waters. DCAP has produced no evidence to support its assertion that the permit will cause adverse impacts to surface water flows or surface waters or to environmental features such as vegetation, fish, and wildlife. DCAP has produced no evidence that its substantial interests are affected by the proposed agency action.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that Southwest Florida Water Management District enter a final order: Determining that Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc., have satisfied the requirements of Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, regarding conditions for issuance of WUPs;3 Issuing proposed General Water Use Permit No. 20012185.000, as set forth in District Exhibit No. 4; and Finding that DCAP lacks standing to challenge the issuance of the permit. DONE AND ENTERED this 3rd day of June, 2002, in Tallahassee, Leon County, Florida. CHARLES A. STAMPELOS Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 3rd day of June, 2002.
The Issue Respondent Jacksonville Shipyards, Inc. (JSI) filed a permit application with the State of Florida, Department of Environmental Regulation, (DER), for permission to conduct maintenance dredging in a basin associated with its shipyard operation. This permit application was made in accordance with Chapter 403, Florida Statutes, and Chapter 17, Florida Administrative Code. In the face of DER's statement of intent to grant this permit, George H. Hodges, Jr., (Petitioner), has petitioned in protest. Therefore, the issues to be considered in this dispute concern the entitlement of JSI to the grant of an environmental permit for maintenance dredging of its shipyard basin.
Findings Of Fact DER is an agency of the State of Florida charged with the environmental protection of waters within Florida. Its authority includes regulatory powers announced in Chapter 403, Florida Statutes, and Chapter 17, Florida Administrative Code. Certain activities involving state waters require permission from DER before they be lawfully undertaken. Among those activities are dredge projects such as contemplated by JSI in its pending request to be allowed to maintenance dredge as much as 66,000 cubic yards of material per year from its shipyard basin located in Jacksonville, Duval County, Florida. This is an undertaking which is envisioned by Chapter 403, Florida Statutes, related to the permit responsibility of DER. It is specifically addressed by Rule 17-4.28, Florida Administrative Code, in which is found the statement of permit requirements for dredge and fill activities. JSI, the applicant, operates a facility known as Bellinger Shipyard, which is engaged in the repair and maintenance of commercial and naval vessels. This enterprise includes the drydocking of vessels upon which repairs are effected, through the use of several drydock chambers in shipyard basin. In the course of the maintenance, a technique known as "gritblasting" is employed. The purpose of this "gritblasting" is to clean the ships in anticipation of repainting. On occasion the "gritblasting" would remove all coats of paint down to the metal finish of the ship. The paints being removed contain antifouling and anticorrosive materials. Those materials have, among other properties, the ability to repel marine organisms, causing their mortality. The "gritblasting" process utilizes a material known as "black beauty." This is a waste product from firing power plant boilers and it contains iron, silica, aluminum, titanium, magnesium, lime, penta oxide (P2O5), sodium oxide, sulfur trioxide and potassium oxide. The "black beauty" is applied through the use of a pressurized system which forces the material onto the treated surface under pressure of 70 to 85 pounds per square inch. After the preparation is made, vessels under repair are repainted, and similar paint with antifouling and anticorrosive properties is reapplied. During the "gritblasting" process, dust is generated and a portion of that material finds its way into the water within the basin. Other particles being removed drop to the deck surface of the drydock. When paint is reapplied to the surface of a vessel undergoing repair, it is given the opportunity to dry and the vessel is then refloated and removed from the drydock. To do this, the drydock itself is submerged. When the vessel has exited the drydock facility, the drydock resurfaces and is allowed to dry out. The material which has been removed from the surface of the repaired vessel is then shoveled into containers and transported to an offsite sanitary landfill for disposal. This material removed includes the "gritblasting" compound and paint which has been stripped from the surface of the vessel. When the drydock is submerged following vessel servicing, the inference can be drawn that a certain amount of the materials on the drydock deck surface will be introduced into the water within the basic before the drydock is resurfaced. The arrangement for refloating the vessel is the reverse of the technique employed in lifting the vessel out of the water for maintenance. When the vessel is brought in for service, it is guided into a submerged drydock. Water is then pumped out of the hollow drydock walls and deck to raise the vessel out of the water, allowing access to the vessel, which is completely above the water surface, as is the drydock work deck. The basin in which the business activities of JSI take place is located on the western shore of the Intercoastal Waterway. The Waterway and basin are part of an estuarine system, as these water bodies are tidally influenced. The basin and the Intercoastal Waterway constitute Class III waters of Florida. The configuration of the basin is as found in JSI Exhibit 16, an aerial photograph of the site. Moving from east to west within the basin, it is approximately one thousand feet from the Intercoastal Waterway to the back of the basin in its western-most extremity. In the back area of the basin the north- south axis is 250 feet. The interface between the basin and the Intercoastal Waterway on the eastern reach north-south axis is approximately 625 feet. There are no obstructions to the confluence of the Intercoastal Waterway and the eastern side of the repair basin. The southern-most reach of the basin is approximately 350 feet in length running east to west. On the eastern side of the basin there is a pier area which is roughly 360 feet north-south by 60 feet east-west. As described before, the pier is not a solid structure extending to the bottom of the water. Thus, water can be exchanged between the basin and the Intercoastal Waterway beneath the pier. JSI had acquired the Bellinger Shipyard in 1974. At that time environmental permits had been issued allowing for the maintenance dredging of the basin. These permits were valid through 1975. In 1975, JSI obtained a dredge and fill permit from the Florida Board of Trustees of the Internal Improvement Trust Fund, as well as a dredge and fill permit from the United States Corps of Engineers. These permits were for a ten-year period. They allowed maintenance dredging in the amount of 66,000 cubic yards per annum and for the disposal of the dredged material in an EPA-approved offshore site. In 1980 DER confirmed the dredge and fill permit that had been obtained from the Florida Board of Trustees. This permit by DER required JSI to conduct monitoring of turbidity during dredging, but did not require employment of turbidity screens. In 1979 the Army Corps had required JSI to conduct bioassay analysis in furtherance of the federal dredge and fill permit. In the face of the results obtained in that bioassay analysis, the Army Corps continued the dredge and fill permit to JSI dating from August 14, 1980. A subsequent extension of the federal permit was given through August 14, 1986. Contemporaneous with the present permit application before DER, JSI has requested further permission from the Army Corps related to the ability to excavate as much as 66,000 cubic yards of material on an annual basis. JSI has not been cited by any regulatory agency related to water quality violations associated with its dredging activity. The present DER permit application is for renewal of the 1980 Permit No. 16-21380 and is being processed under the DER File No. 161071139. This application for permit renewal was submitted on July 16, 1985. The application requests permission to maintenance dredge for a period of ten years. If granted, it is the intention of the applicant to use a closed clam shell bucket to excavate the material in the basin. This choice is in furtherance of the suggestion of DER and is a departure from the applicant's initial intention to use an open bucket to excavate. JSI also intends to employ turbidity curtains during the dredge activities. The applicant intends to transport the dredged material to the aforementioned EPA disposal site which is at sea. In doing so, a hopper barge is propelled by a towing vessel. Both the barge and towing vessel are inspected and certified by the United States Coast Guard. The crews involved in the transport of the material are qualified and licensed. In the past, transport of the material has been done under fair weather and smooth sea conditions, and it is intended that the transportation be done in that same setting if the permit is granted. The barge would not be loaded fully, thereby minimizing spillage. This was the arrangement in the past. The United States Coast Guard will be apprised of the departure time of the voyage in transport of the material, certain activities within that transport and upon return. The hopper barge has a bottom dump which is closed during transport and is opened at the bottom in disposing the dredge material. After satisfying DER about its proposal, JSI was informed that DER intended to grant the dredge permit requested. When Petitioner, George H. Hodges, Jr., the owner of real property adjacent to the site of the project, learned of the stated intention to grant the maintenance dredging permit, he offered a timely petition in opposition to the proposed agency action. This property of Petitioner is in Jacksonville, Duval County, Florida. It is located north of the JSI property at issue. Petitioner's real property is connected to the Intercoastal Waterway. Petitioner has filed this action in opposition to the grant of the permit upon the expressed belief that the dredging activity will cause pollution at his property. In particular, it is JSI's intention at various times in the calendar year to do maintenance dredging in the entire basin. In addition to using a closed clam shell bucket, a system of turbidity barriers or curtains will be employed in segmented dredge areas. Those several locations within the basin which are cordoned off with the turbidity curtains are as depicted in JSI's Exhibit 9 admitted into evidence. The design maintenance depths for the dredging project are set forth in JSI's Exhibit 4 admitted into evidence. They vary from -17 to -37.5 feet, with the greatest depth being contemplated under drydock number 1 in the northwestern corner of the basin. Near the Intercoastal Waterways the depth sought is -17 feet, transitioning to -21.5 feet moving toward the back of the basin at the western extreme and outside of the area dredged beneath drydock number 1. The depths sought under drydock numbers 2 and 3 are -26.5 feet and -20 feet respectively. These desired elevations correspond to conditions at mean low water. The tidal range in the Intercoastal Waterway adjacent to the basin, which would promote an influence in the basin proper, is in the neighborhood of 4-foot intervals, with two tidal cycles a day. This would mean, as example, that at the high tide range, the shallowest design depths for dredging of -17 feet become -21 feet in the transition from mean low water to mean high water. Those 4-foot variations would pertain to the other design depths contemplated in the dredging as described in the preceding paragraph as well. The turbidity barriers contemplated for use will extend from the surface through the water column to depths near the bottom. See JSI Exhibits 4 and 9. It is desirable, according to Dr. Gregory Powell, witness for JSI, a reliable expert in describing the effectiveness and use of turbidity curtains, to have those curtains extend to an area just above the bottom. Dr. Powell's education includes a Masters Degree in coastal and oceanographic engineering and a Ph.D. Degree in engineering mechanics, with emphasis on coastal and oceanographic engineering. In consideration of his remarks, under the influence of high tide there could be as much as a 4 foot gap between the curtain and the bottom. Powell and other experts who offered testimony agreed that turbidity screens can have effectiveness in areas of low current velocity, assuming the proper installation, maintenance and extension to a location near the bottom of the water body. If mismanaged, turbidity screens are not effective in controlling turbidity. Moreover, they are less effective in areas where significant current velocities are experienced. This would include the circumstance in which a foot and a half or more per second of flow was being experienced, according to Dr. Powell, whose opinion is accepted on this point. He also indicated that the quiescent areas in the basin, toward the back of the basin or western dimension of the basin, would show a flow regime in a rate of one centimeter per second. This expression is credited. Although, as described by Dr. Powell, the currents in the Intercoastal Waterway are moving at a rate approximating nine feet per second on ebb time at the bridge located on the Intercoastal Waterway to the south of the project site, these current velocities are not expected in the area where the dredging is occurring. Dr. Powell is correct in this assessment. As he describes, and in acceptance of that testimony, eddies from the current from the Intercoastal Waterway at peak flood tide could come into the basin and temporarily show velocities of one foot per second; however, these velocities are within the acceptable range of performance of the turbidity barrier. Dr. Powell's conclusion that wind would have no significant effect on the current velocity, given the depth of this basin, is also accepted. The remaining flow regime in the basin is not found to be a detriment to the function of the turbidity barriers. The use of turbidity curtains in this project is not found to be a "placebo" to placate DER as suggested by Erik J. Olson, engineering expert who testified in behalf of the Petitioner The monitoring that is intended in the course of the dredging activities would call for examination of background turbidity levels at three sites in the Intercoastal Waterway prior to commencing of dredging and twice daily at each of these sites during dredging. Should a violation of state water quality standards for turbidity be detected, dredging will cease until the problem with turbidity can be rectified. To provide ongoing assurances of compliance with water quality standards, JSI will analyze the sediment in the basin for the parameters of cadmium, copper, aluminum, lead, mercury, oil and grease every two years. Dr. Powell, expert in engineering and recognized as an expert in the matter of transport of the resuspended sediment associated with the dredging, as well as David Bickner, the project review specialist for DER, believe that the use of the closed clam shell bucket technique and employment of siltation screens or barriers, together with turbidity monitoring, will effectively protect against turbidity violations in the Intercoastal Waterway adjacent to the basin. This opinion is accepted. Bickner brings to his employment a Bachelor of Science degree in biology and a Master of Science degree in ecology. Bickner identified the principal concern of DER related to this project as the possibility of release of resuspended sediments into the Intercoastal Waterway. With the advent of the techniques described in the previous paragraph, only minimal changes in background conditions related to turbidity are expected. Although there would be turbidity violations within the confines of the areas where the dredging occurs, the principal influence of that turbidity will be confined in those regions. This speaks to dredge areas I, 2 and 3. According to Bickner, whose opinion is accepted, the turbidity changes within the dredge areas in relationship to background conditions do not require a mixing zone permit, nor do they constitute a basis for denial of the permit. As alluded to before, and as described by Dr. Powell, the basic nature of the basin in question is one of quiescent conditions with low current velocity. He points out that the layout of the basin is such that it is a sediment trap allowing the deposit of silt, in particular in the deeper sections of the basin near the western side. The greatest influence by resuspension of sediment in the dredging activities can be expected in the back portions of the basin and it is in this area that the silt barrier can be expected to be most efficient, based upon Powell's remarks. Dr. Powell indicated that there is the expectation of increased efficiency in turbidity control when a closed clam shell bucket is used, as opposed to the open style of clam shell bucket. Those efficiencies range from 30 to 70 per cent. There is some risk of increased turbidity near the bottom of the water column in the use of a closed clam shell bucket, and for that reason the applicant should monitor the activities of the operator of the excavation machinery to guard against inordinate disturbance of the area being excavated. On balance, the closed clam shell bucket is a superior technique to the open style of clam shell bucket excavation when those alternatives are compared. As Dr. Powell explained, the segmentation of the dredge area allows the resuspended sediment to be confined in more discrete circumstances and to be controlled. The location of the silt barriers behind the pier structure guard against the effects of eddying. The silt barriers can be properly anchored and will not be unduly influenced by current velocity. Dr. Powell believes that the use of silt barriers, taking into account a low velocity of current in the basin, and the proper deployment of the siltation screen could bring about a reduction of the resuspended solids by 80 to 90 per cent on the outside of the barrier. To calculate the influence or the environmental significance of that remaining 10 to 20 per cent of resuspended solids at the Intercoastal Waterway, Dr. Powell testified that the suspended load behind the silt curtain resulting from the dredging is expected to average from 100 milligrams per liter to a peak amount of 500 milligrams per liter. He believes that, depending on which methods of calculation is used, the dilution factor in the Intercoastal Waterway ranges from 330:1 to 600:1. In using an environmentally conservative assessment, that is 80 per cent effectiveness of the silt curtain with a 330:1 ratio, Powell calculated that the release of resuspended materials into the Intercoastal Waterway would be approximately .3 to 1.5 milligrams per liter. This translates to less than 1 NTU against background conditions. This result would not exceed the 29 NTU limit against background that is described as the standard for turbidity control. Dr. Powell's opinion of turbidity results based upon the dredge activity is accepted. There is exchange of water between the basin and the Intercoastal Waterway and to accommodate this influence, the turbidity curtains would be placed in such a fashion that they would not compete with the ebb and flow of the tide. Dr. Powell's assessment of the circumstance in describing the effectiveness of turbidity barriers takes into account the tidal conditions and the inappropriateness of trying to have the silt curtains prohibit the flow conditions during these tidal changes. In order to promote maximum effectiveness of the turbidity barriers during the entire course of excavation of materials, the length of, the silt screen must be adjusted as desired elevations are approached. Erik J. Olson is an expert in civil engineering with an emphasis on hydraulics and the holder of a Masters Degree in coastal and oceanographic engineering. As alluded to before, he questions the validity of the use of siltation barriers as an effective protection against the implications of turbidity. He properly points out that the curtains will not extend to the region of the interface of the basin and the water column at all times. He describes the exchange of water between the basin and the Intercoastal Waterway, to include the unrestricted sediment transport beneath the turbidity curtain. He believes that wind can cause changes in current velocity as great as .2 foot per second, activities within the basin an additional .3 foot per second, and eddying .3 foot per second. All of these taken together do not exceed the range of effective response of the turbidity barriers. On balance, Olson's criticism of the benefit of turbidity curtains is unconvincing. Arlynn Quinton White, Jr., who holds a Bachelor of Science Degree, a Master of Science Degree in biology and a Ph.D. in matters related to marine biology, offered his testimony in support of Petitioner. He believes that as much as 2 to 3 per cent of the resuspended sediment related to the dredging activities would reach the Intercoastal Waterway under the best of conditions. It is difficult to translate that testimony into a measurement of changes in turbidity levels against ambient conditions in the Intercoastal Waterway. In any event, as already indicated, the changes in turbidity levels are not expected to exceed 29 NTU against background. It is evident that the turbidity curtains are necessary and their proper use must be assured to protect against problems associated with turbidity and the implications of the constituents of the resuspended particulate matter related to possible toxicity. Therefore, the close monitoring suggested in the statement of intent to grant the dredge permit is viable. Another matter associated with the implications of turbidity pertains to the fact that when the dredge material has been resuspended, as much as two days could pass before the basin returns to background conditions, given the high content of silt with its attached metals. This becomes significant given the uncertainty of the location of the dredge equipment during the course of excavation, i.e., inside the barrier or outside the barrier. Final choice about the placement of the dredge equipment will have to be made at the time of the excavation. Should the dredge equipment be inside of the cordoned area while excavation is occurring, it would be necessary to allow turbidity conditions to achieve background levels before opening up the barrier for the exit of the hopper barge which contains the excavated material. Otherwise, the estimates as to the influence of the dredging activities in the Intercoastal Waterway are unduly optimistic. Likewise, if the excavation platform is placed outside of the work site, that is to say, on the outside of the siltation curtain, extreme caution must be used to avoid spillage of the excavated material when being loaded onto the hopper barge. The occasions in which the excavation is being made from this side of the barrier should be minimized. These safeguards are important because any changes in sediment loading within the Intercoastal Waterway promote an influence in the area immediately adjacent to the basin and other sites within the Intercoastal Waterway as well. The subject of the use of a hydraulic dredge as an alternative to excavation by use of a closed clam shell bucket was examined in remarks by the witnesses appearing at hearing. Olson believes that there are hydraulic dredges which can achieve the design depth contemplated by the project and which equipment could fit inside the basin area. This is contrary to the opinion of witnesses for the applicant and DER who do not believe that the hydraulic dredging equipment which would be necessary to achieve the design depths would fit into the basin area. On balance, the record does not establish that such equipment with the appropriate capability and size does exist. More importantly, the proposed method of excavation is environmentally acceptable when examined in the context of the permit sought in this case. Finally, it was not essential for the applicant to make a detailed investigation of availability of hydraulic dredging equipment and it is not determined that failure to make this investigation warrants the denial of the requested permit. Although an hydraulic dredge is more desirable from the standpoint that it causes less turbidity through resuspension of sediments, it is not the only plausible method of excavation in this instance. Raymond D. Schulze testified in behalf of JSI. He holds a Bachelor of Science Degree and a Master of Science Degree in environmental engineering sciences. In particular, he established the fact that the amount of resuspended solids that would be introduced into the Intercoastal Waterway associated with the dredging activity would not result in the smothering of organisms or to clogging of gills of fish. In addition to the possible problems with turbidity, there is the additional issue of violation of water quality standards in the several parameters associated with concentrations of metals in the water column within the basin and in the sediments or related parameters such as dissolved oxygen and biological integrity. Having considered the testimony, the facts do not point to water quality violations for any parameters occurring in the Intercoastal Waterway as a result of the dredging. To arrive at this factual impression, the testimony of Dr. Pollman and Schulze is relied upon. Water quality sampling done by JSI in locations within the basin and in the Intercoastal Waterway, that by Dr. Pollman and Schulze, supports their impression of the acceptability of the dredge activities. This water quality data was admitted as JSI's Exhibit 18. Additionally, the field conditions existing at the time of testing, to include water temperature, weather conditions, tidal cycle, ph and dissolved oxygen were also made known. This water quality data and other information examined by these witnesses points to the fact that no increases in concentrations of metals are occurring within the Intercoastal Waterway as a result of the business activities of the applicant, nor are they to be expected while dredging operations are under way. Dr. Pollman correctly identifies the fact that there will not be significant degradation of water quality, above DER's minimum standards, related to the Intercoastal Waterway based upon the dredging activities within the basin, dealing with the water quality parameters of mercury, zinc, cadmium, chromium, lead, aluminum, iron and copper, substances which are within the basin. Dr. Pollman also examined sediment data collected by DER, and that data tended to confirm his assessment of the influences of the dredging activity related to these parameters. Dr. Pollman does not believe that metal concentrations contained in the sediment of the basin are leaching into the water column in quantities sufficient to cause violation of water quality standards. His opinion is accepted. Pollman had collected water quality samples in the two locations where the greatest siltation rate was expected and as a consequence the greatest concentration of metals would be expected. The water quality samples were taken at several depths to reach an opinion as to the matter of leaching of metals into the water column and the possibility of those metals dissolving in the water column. If leaching had been occurring, a concentration of metals expressed as a gradient would be expected. The greatest concentration in this instance would be near the sediment interface with the water column. No such gradation was detected and the idea of leaching was ruled out. Bickner's testimony established that testing for the exact amount of iron present at the dredge site was not required, given the nature of the iron source being introduced into the water within the basin. Bickner did not find that type of iron to be toxic. As stated before, Pollman agrees that no violation of state water quality standards as a result of the presence of iron associated with the maintenance dredging should be expected. There is some data which shows water quality violation for mercury in the basin and the Intercoastal Waterway. Subsequent water samples collected by Schulze in the westerly portion of the basis did not show detectable levels of mercury. Moreover, data taken by Pollman and Schulze and compared with the DER sediment data shows that the concentration levels of mercury are greater in the Intercoastal Waterway than in the basin, thereby suggesting that there is no concentration gradient for mercury which would lead to the belief that the basin contributes to the amount of mercury found in the Intercoastal Waterway, nor is the mercury believed to be leaching into the water column in the basin. The explanation of the differences in measurements of the amount of mercury in the basin, depending upon the point in time at which analysis was made, may be attributable to a natural phenomenon, given numerous sources of mercury within the environment. Whatever the explanation of these changes, Dr. Pollman does not believe that the release of mercury associated with the resuspended sediments that may find their way into the Intercoastal Waterway would show a violation of the state water quality standard for mercury in that water body and his opinion is credited. Data collected by Pollman and Schulze did not show water quality violations for aluminum and the DER test data described before indicated aluminum levels lower in the basin than in the Intercoastal Waterway. Some data collected by Technical Services, Inc., an environmental consulting firm in Jacksonville, Florida, which was reviewed by Pollman, Schulze, and Bickner showed a substantial violation of the water quality standard related to aluminum in sediment sampling that was done. The origin of that amount of aluminum found on that occasion was not clear. It is possible, as described by Bickner, Pollman and Schulze, that the level detected In the Technical Service report could have occurred based upon natural phenomena such as storm water runoff from uplands. Bickner also questioned the findings of Technical Service and felt like the determination might be influenced by some intervening circumstance which would promote the need for re-analyzing that parameter. Whatever the explanation of the findings in the Technical Service report, it does not point to any water quality violation of the standard related to aluminum based upon the dredging activities, given the limited amount of total suspended solids that would be introduced into the Intercoastal Waterway. Schulze, in his assessment of the implications of metal concentrations in the sediment transported to the Intercoastal Waterway, did not find them to cause concern about toxicity to marine life in the Intercoastal Waterway. This point of view is accepted. In trying to understand the implications of metal concentrations, Schulze believed that the biologically available fractions of those metals in the sediment is not very high, and when the dilution of the sediments which occurs in these circumstances is examined, no toxicity is expected. Moreover, as Dr. Pollman described related to the parameter aluminum, it is not a toxic material at the ph levels found in the basin, and the resuspension during dredging will not cause it to gain toxicity. This opinion of Dr. Pollman is supported by Bickner and Schulze. The opinion of Dr. White that the amount of aluminum, copper and zinc within the sediment found in the basin would eventuate in the violation of water quality standards for those parameters when introduced into the Intercoastal Waterway is rejected. The information available to Pollman, Schulze and Bickner which describes their opinion about water quality standards was sufficient to reach an opinion, the position of Petitioner's witness Sanford Young, holder of a Bachelor of Science Degree in civil engineering and a Master of Science Degree in zoology notwithstanding. As Bickner indicated in his testimony, it is essential that an applicant give reasonable assurances of compliance with all parameters listed in Chapter 17-3, Florida Administrative Code, dealing with water quality. However, this does not mean that testing must be done for each parameter set forth in that chapter. Reasonable assurance has been given that water quality parameters as identified in that chapter will not be violated. Bickner indicates the biological integrity standard is not one of concern in that given the nature of business operations within the basin, there is no expectation of a stable benthic community which might be disturbed by dredging. From the remarks of Schulze, there is no prospect of danger to benthic communities within the Intercoastal Waterway. These impressions by Bickner and Schulze are accepted. Under the facts of the case, the failure of the DER permit appraisers to discover benthic organisms in the sample grabbed at the site is not unexpected. There is also some question about whether that sample is representative of the circumstance at the site, given the limited sampling. On the topic of normalization of the DER data which was described in the course of the hearing and is identified by Dr. Pollman, the value of that information is seen as establishing the relative quantities of certain metals within the basin as compared with other sites throughout the Intercoastal Waterway. Twenty-one different locations were involved in this analysis. Concentration ratios using aluminum to normalize the data are as reflected in JSI's Exhibit 17 admitted into evidence. The significance of this information as it grossly describes whether the basin routinely contributes to increases in the amounts of these metals within the Intercoastal Waterway. Overall, basin activities are not shown to have promoted such an outcome. This normalization comparison does not address the issue of site specific water quality violations; however, no such violations are expected associated with the dredging activities within the basin as it relates to violations in the adjacent Intercoastal Waterway. Schulze had made sampling related to dissolved oxygen within the basin and the Intercoastal Waterway. As Schulze describes, the levels of dissolved oxygen seem to be at their lowest point just prior to the dawn hours. Sampling which he did was done at 5:00 a.m. in order to obtain the lowest dissolved oxygen readings. Three sites were sampled within the basin and an additional site was sampled in the Intercoastal Waterway. Readings were taken at varying depths at each site to gain an impression of the overall water column. The mean reading for the circumstance was in excess of the required range for state water quality, that is 4.0 per million. Having considered the evidence, no problems with dissolved oxygen are expected in that deficit contribution is in the range of .1 milligram per liter, per Pollman. In addition, Dr. Powell, through modeling, examined the implications of long-term dredging activities on the topic of dissolved oxygen. He employed field data gathered by Schulze in this assessment. This modeling established that decreases in dissolved oxygen levels would range from .1 to .15 milligrams per liter. Given the average of 4.5 parts per million oxygen in the basin at present, the incremental decreases in dissolved oxygen levels related to the dredging would not pose a problems with state water quality standards for dissolved oxygen other than short-term effects in the immediate vicinity of the dredge area, which is an acceptable deviation. As the Petitioner urges in its fact proposal, a 1983 report of Technical Services, Inc., JSI Exhibit 4, and a 1985 report of that firm, JSI Exhibit 7, were made available as part of the application. Officials within Technical Services, Inc. did not appear at the hearing and offer testimony related to the specific findings found in those reports. This information was used by the experts who did testify on behalf of the applicant, in particular Dr. Pollman, as data to question, his assumptions made about the implications of the project in terms of water quality concerns. Pollman also utilized DER data taken from a source known as Storette, and this pertains to the 21 sampling stations involved in the preparation of JSI Exhibit 17, the graphing document related to concentrations of various metals. Again, this was in furtherance of the basic underlying opinion which Pollman had about the project. The Storette data as such was not offered into evidence. Witnesses for the Petitioner, namely Olson and White, were aware of the two reports of Technical Services, Inc. and the use of the DER Storette data and offered their criticism of the project taking into account this information. Petitioner points out that there is no indication as to how far below the sediment/water interface the Technical Services, Inc., and DER sediment samples related to reports of the consultant and the Storette information of DER were extracted. Therefore, it only reflected one portion of the sediment at a depth of extraction. A more complete understanding of the sediment characteristics would have been shown through a core sample, especially in the area to be dredged, but that understanding was not essential. The suggestion by the Petitioner that it was inappropriate to normalize data for purposes of describing the relative concentrations of the metals parameters is not accepted. The preparation of JSI's Exhibit 17 does not point to abnormally high amounts of aluminum, such that the use of aluminum as a known commodity in carrying out the normalization would be contraindicated. As identified by the petitioner in its proposal, sediment sizes within the strata found in the basin depicts higher percentage of silt and clay-size sediments in the back end of the basin with lesser amounts of the silt- and clay-size sediments in the southern reach of the basin and at the intersection of the basin with the Intercoastal Waterway. The smaller the particles, such as silt and clay, will remain suspended for a longer period of time and have a tendency to promote bonding with heavy metal. Nonetheless, this information does not change the impression that the turbidity barriers will be effective. The 1983 Technical Services, Inc., information related to the settling of resuspended sediment and similar information imparted in the 1985 report by that organization tend to confirm that approximately two days should be necessary to allow the area of excavation to return to background conditions related to turbidity. This is in corroboration of remarks by Dr. Powell. These time projections are not found to be inadequate when taking into account other factors such as tidal changes, boat traffic, other activities within the basin, wind and weather events. As White described, the antifouling properties of the paint involved in the business activity of the applicant can be expected to adversely impact any larval forms of marine organisms when introduced into the basin. Nonetheless, this toxicity is not expected to pose a danger to marine organisms in the Intercoastal Waterway given the percentage of resuspended sediment that will escape capture by the sediment barriers and the dilution factor before introduction of those resuspended sediments into the Intercoastal Waterway. Petitioner questions the acceptability of evidence of the findings set forth by E G & G Bionomics, a firm which performed an examination to determine existing diversity of benthic macroinvertebrates. Those results are reported in Petitioner's Exhibit 13, a 1980 report. They were not accepted as evidence of the specific findings within that report in that they were not the subject of discussion by persons who authored that report. The use was limited to corroboration of the opinion by Dr. Pollman and Schulze as to water quality considerations and they were not Crucial to their opinions. Moreover, it was not necessary for the applicant to perform a more recent bioassay in order to give reasonable assurance to DER concerning water quality matters or to establish the implications of the influence of contaminants within the sediment found in the basin related to benthic macroinvertebrates. The biological integrity of the basin area was at risk prior to the proposal for maintenance dredging. The relevant inquiry is the influence of the dredging activities on the biological integrity in the Intercoastal Waterway and those activities do not place organisms within the Intercoastal Waterway in peril. Any synergistic aspects of metals which act as toxins, for example, the increase in the aggregate value of the toxicity of zinc and cadmium, compared to their individual implications as toxins, will not present problems with water quality in the Intercoastal Waterway. Petitioner takes issue with the proposed disposition of the dredge material at an ocean site. While an appropriate upland disposal site would be preferred, it is not mandated. The approved EPA disposal site within federal jurisdiction is acceptable. Petitioner in its fact proposals found at paragraphs 36-39 (incorporated by this reference) points out violations of water quality standards for cadmium, mercury, and aluminum, and other possible violations of the standard for mercury. This information does not cause a change of opinion about the acceptability of the project in terms of reasonable assurances. There is no indication that oils and greases will present a problem related to water quality standards. The project is not contrary to public interest in that: (a) the project will not adversely affect the public health, safety, welfare or the property of others; (b) the project will not adversely affect the conservation of fish and wildlife, including endangered or threatened species, or their habitat; (c) the project will not adversely affect navigation or the flow of water or cause harmful erosion of shoaling; (d) the project will not adversely affect the fishing or recreational values or marine productivity in the vicinity of the project; (e) the project will be of a temporary nature; (f) the project will not adversely affect significant historical and archaeological resources under the provisions of s. 267.061; (g) the project is in no other way contrary to the public interest. The purpose of this fact finding does not include the issue of whether there are ongoing violations of state water quality standards associated with the business activity of the applicant, that not being the subject of the hearing. In any event, the testimony of Dr. Pollman established that the operations of JSI are not causing water quality problems associated with the parameters of cadmium, copper, aluminum, mercury, lead, chromium, tin, zinc or iron related to the Intercoastal Waterway. The influences of the business activities associated with those parameters within the basin are not understood when the evidence presented is examined but are not found to be essential to the resolution of this dispute.
Recommendation Having considered the facts, and the conclusions of law, it is, RECOMMENDED: That DER issue a final order which grants the requested maintenance dredging permit in keeping with the safeguards described in the fact finding of this recommended order. DONE AND ORDERED this 16th day of October 1986 at Tallahassee, Florida. CHARLES C. ADAMS, Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 16th day of October 1986. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 86-0365 Having examined the proposed facts submitted by the parties, those proposals have been found as fact with the exception of the following which are distinguished: Petitioner's facts Paragraph 1: Subordinate to fact finding. Paragraph 2: The first sentence in this paragraph is rejected because the fact is not found within the indicated exhibits, nor can that fact be fairly inferred. Paragraphs 9, 10, 11, 14, and 15: Except for the last sentence in that latter paragraph are subordinate to facts found. Paragraph 15: The last sentence: Contrary to facts found. Paragraph 18: The last sentence: Subordinate to fact finding. Paragraphs 21, 22, 23, 24, 25 and 26: Subordinate to fact finding. Paragraph 27: Contrary to facts found. Paragraphs 28, 29, 30 and 31: Subordinate to fact finding. Paragraph 32: Not necessary to dispute resolution. Paragraphs 33 and 34: Subordinate to fact finding. Paragraph 35: Contrary to facts found. Paragraphs 40, 41 and 42: Subordinate to fact finding. Paragraphs 44, 45: Not necessary to dispute resolution. Paragraph 47: The first two sentences are information that is not sufficiently credible to allow application to the issues of the present case. Paragraphs 48, 49, 50 and 51: Not necessary to dispute resolution. Paragraph 52: Reject as fact. Paragraph 54: Contrary to facts found. Paragraph 55: Not necessary to dispute resolution. JSI and DER facts Paragraph 2: Pertaining to sentence 8 and the last phrase within sentence 11; Not necessary to dispute resolution. Paragraph 3: As to the first sentence, fourth sentence and seventh sentence; Not necessary to fact resolution. Paragraphs 4, 5 and 6 to the colon in paragraph 6: Not necessary to dispute resolution. The remaining portions of paragraph 6 are subordinate to fact finding. Paragraph 10: as to the last two sentences; Not necessary to dispute resolution. Paragraph 13: As to the next to the last sentence; Not necessary to dispute resolution. Paragraph 14: As to the fourth sentence and the last sentence; Not necessary to dispute resolution. Paragraphs 16, 17, 18 and 20: Subordinate to fact finding. Paragraph 21: Sentence 3 is subordinate to fact finding sentence 4 is not necessary to dispute resolution; sentences 5 and 6 are subordinate to fact finding. Paragraph 22: Next to the last sentence; Not necessary to dispute resolution. Paragraphs 24, 25, 26, 27, 28, 29, 30, 31, 32, 33, 34, 35, 36, 38 and 41: Subordinate to fact finding, except the comments in the last sentence of paragraph 41 related to the operations of JSI causing or contributing elevated concentrations of parameters within the basin which is not found as fact. Paragraphs 42, 43 and 44: Subordinate to fact finding. COPIES FURNISHED: Kenneth G. Oertel, Esquire Chris Bryant, Esquire OERTEL AND HOFFMAN, P.A. Post Office Box 6507 Tallahassee, Florida 32314-6507 Thomas M. Baumer, Esquire Deborah Barton, Esq. GALLAGHER, BAUMER, MIKALS, BRADFORD, CANNON AND WALTER, P.A. 252-5 Independent Square Jacksonville, Florida 32202 Bradford L. Thomas, Esquire Assistant General Counsel Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 Victoria Tschinkel, Secretary Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32301
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.
