Findings Of Fact Upon a consideration of the oral and documentary evidence adduced at the hearing in this cause, the following pertinent facts are found: 1/ By application number 25793, the applicant seeks a permit to construct and operate a proposed surface water management system to serve a 2,541 acre project within the St. Johns River Basin in Indian River County. The proposed system will consist of a perimeter dike, a central canal with interior laterals and four discharge pumps. The applicant will be discharging into the St. Johns Marsh and seeks a discharge capacity of 139,000 GPM. Three of the discharge pumps are to be located at the southeast corner of the property and a two-way 25,000 GPM pump is to be located at the intersection of the central canal and the western boundary of the property. By application number 25794, the applicant seeks a permit for the use of surface and artesian water for the irrigation of the same 2,541 acres of pasture and truck crops. The applicant requests to withdraw surface water from the St. Johns Marsh by means of a two-way 25,000 GPM pump located at the intersection of the central canal and the western property boundary and to withdraw water from the Floridan aquifer by means of eight eight-inch artesian wells. The amount requested is 5,294 acre-feet per year with a maximum monthly pumpage of 1.47 billion gallons. A staff report of the Central and Southern Florida Flood Control District (FCD) concluded that the major problem with the permit applications is the impact on water quality of the receiving bodies of water and that nutrients and other pollutants will be introduced into runoff waters discharged into the St. Johns Marsh, which is the source of the public water supply for South Brevard County. The staff therefore recommended that the applicant institute a water quality and quantity monitoring program to monitor discharges to the Marsh. The staff further recommended that the applicant not be allowed to discharge from the western property boundary nor irrigate from the ditch on the western property boundary. It was recommended that the two-way 25,000 GPM pump be installed adjacent to the other pumps located at the southeast corner of the property. More specifically, the staff found that if a permit were to be issued pursuant to application number 25793, it should be subject to the conditions that: the allowable discharge capacity to be 104,000 GPM, with discharges to be east to the St. Johns Marsh by means of one 44,000 GPM pump, one 35,000 GPM pump and one 25,000 PM two-way pump to be located at the southeast corner of the property; the applicant notify the FCD prior to any excavation of materials from land lying east of the east property boundary and, if such excavation is done, a discontinuous borrow ditch be created by either leaving 25 foot portions of undisturbed marsh or by placing 25 foot earthen plugs at approximately 500 foot intervals (this was later modified at the hearing to 1,000 foot intervals); and the applicant submit monthly reports of total daily discharges and water quality, the samples to be taken at the southeast corner of the property. With regard to application number 25794, the staff recommended that if such permit were to be issued, it be subject to the following conditions: for the use of surface water, an annual allocation of 2329.3 acre- feet per year and for the use of artesian water, an annual allocation of 2518.5 acre-feet per year, with a maximum monthly pumpage from all sources of 355.3 million gallons; no withdrawal of surface water from the St. Johns Marsh when the water level in Blue Cypress Lake drops to 22.0' msl.; surface water to be withdrawn by means of a 25,000 GPM two-way pump located at the property's southeast corner; artesian waters to be withdrawn by eight eight-inch wells with effective and operative controls placed thereon and analyses of water samples from the water discharge of each the submission of monthly reports of total monthly pumpages and total monthly flows; and permit for the withdrawal of surface and artesian water to expire on January 15, 1979. At the hearing, the applicant agreed to the recommended conditions placed upon the permits by the staff report with the exception of: the amount of the allowable discharge (staff recommending 104,000 GPM as opposed to a desired 139,000 GPM); the location of the 25,000 GPM two-way pump (staff recommending southeast corner as opposed to a proposed site on the western boundary of the property); the expiration date of January 15, 1979. The Environmental Protection Bureau of the Florida Game and Fresh Water Commission requested the FCD to delay issuance of permits for all projects in the Upper St. Johns River basin until a comprehensive water management plan for the area is formulated. Read into the record was a resolution adopted by the Commission on May 16, 1975, recommending that "the further destruction of the marsh be curtailed and a plan be formulated for the return of the diverted waters as a management tool for restoration of fish and wildlife resources." On behalf of the Florida Audubon Society, Mr. Charles Lee contended that, because of this resolution and request of the Game and Fresh Water Fish Commission and that agency's constitutional status, the FCD is precluded from issuing the subject permits. Intervenors and members of the general public who were opposed to the issuance of the instant permits expressed the following concerns: the low water quality and quantity of the St. Johns River and its marshes; the decline in hunting and fishing because of agricultural activities in the St. Johns River valley; the loss of marsh land due to agricultural activity; the lack of a basic water management program for the area; the lack of remedial measures should degradation of the water occur; and the lack of an expiration date for the surface water management system permit.
Recommendation Based upon the findings of fact and conclusions of law recited above, it is the recommendation of the hearing officer that application numbers 25793 and 25794 be granted, subject to those special conditions set forth in the Staff Report as modified by the following: In paragraph number 3 on page 14 of the Staff Report, substitute the words "1,000 foot intervals" for "500 foot intervals;" Add as paragraphs 6 on page 15, paragraph 6 on page 16 and paragraph 7 on page 18 the following: "Should the data in the monthly reports submitted by the applicant indicate the occurrence of a degradation of the waters utilized, the applicant will be required to remedy the situation causing the de- gradation." Add as paragraph 7 on page 15 the following: "7. This permit shall expire on January 15, 1979." Respectfully submitted and entered this 25th of March, 1976, in Tallahassee, Florida. DIANE D. TREMOR Hearing Officer Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304
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 This case presents two questions for consideration. The first question concerns the Petitioners' contention that the grant of the permit at issue must be considered contemporaneously with the matters of file in the application made by the Respondent, The Deltona Corporation, with the Respondent, State of Florida, Department of Environmental Regulation, File No. 64-24208, pending before the Department. From the point of view of the Petitioners, should this contemporaneous review process be afforded, then the current permit would not be granted due to the alleged deficiencies associated with the application, File No. 64-24208. The second question to be answered in this case concerns the dispute between the Respondents on the issue of water quality monitoring as a condition to granting the permit sought herein. The Respondent Department would have the applicant monitor in six lakes in the area of the project and the applicant would restrict its monitoring activity to three lakes in the project area. The Petitioners support the Department in its position on the monitoring question. 1/
Findings Of Fact The Respondent, The Deltona Corporation, has made application with the Respondent, State of Florida, Department of Environmental Regulation, to effect drainage system improvements to a land locked conveyance network which consists of the enlargement and regrading 990 lineal feet of existing channel cross- section and the installation of additional culverts and control structures at road crossings. The project also involves repairs and replacement of a damaged culvert. The work would be accomplished by land based equipment transported to the work site by existing overland routes. The excavated sand fill would be placed on upland property owned by The Deltona Corporation. The details of the project and data related to the geographical area may be found in the Joint Exhibit I admitted into evidence. The date of the application for permit is December 12, 1979. On January 25, 1980, the Department of Environmental Regulation sent out a notice of the pending review by the Department of the permit application. After receipt of that notice, attorney for the Petitioners, on February 12, 1980, wrote to the Department expressing the objection to the project made by property owners in the area of the project site, together with a list of those owners found in an attached Petition of owners' names and addresses. A copy of this letter and attached Petition may be found as Joint Exhibit No. VII admitted into evidence. Subsequent to the receipt of the statement of objections, the Department issued a construction permit dated April 30, 1980, subject to conditions. A copy of this permit may be found as Joint Exhibit No. VIII admitted into evidence. The Petitioners, through their counsel, then filed a formal petition dated May 6, 1980, which was the vehicle utilized in establishing the details of this dispute and was the basis for the Department Secretary forwarding the case to the Division of Administrative Hearings for consideration by a hearing officer in keeping with the provisions of Section 120.57, Florida Statutes. The hearing was conducted on October 16, 1980, and the Petitioners' position was more specifically defined in the course of that hearing and the claim as described in the issue statement of this order constitutes the substance of the Petitioners' position. 2/ Joint Exhibit No. I; petitioners' Exhibit No. 1 and Respondent Deltona's Exhibits 1, 2 and 4 constitute sketches and aerial photographs of the general project area. Joint Exhibit No. 1 identifies the work area with more particularity. Respondent's Exhibit No. 2 indicates the desired flow pattern of the water through the various lake systems and indicates whether the flow is by gravity flow or pump flow. This drawing depicts the proposed channels and structural improvements that would be involved. The Department has indicated that all the regulatory concerns which it has about the project associated with Permit No. 64-26478-4E, the permit in question, have been adequately addressed, subject to the conditions set forth in the permit document. Joint Exhibit Nos. V and VI; Respondent Deltona's Exhibit Nos. 5, 6 and 7; and the Petitioners Exhibit No. 2 are exhibits pertaining to water quality concerns, to include sample results. The testing and other information provided indicates that the project as contemplaced, would meat the regulatory parameters set forth in Chapter 403, Florida Statutes, and Chapters 17-3 and 17-4, Florida Administrative Code. The Department in expressing its concern that continued water quality monitoring be conducted has indicated that it feels that future periodic monitoring should be done in Jenkins Pond, Lake Big, Lake Diana, McGarity Lake, Sidney Lake and Lake Mitnik. The Respondent Deltona would only conduct this monitoring in the first three lakes named. By looking at the Respondent Deltona's Exhibit No. 2, it could be seen that all of the aforementioned lakes would be in the same basic flow pattern. Of the system of lakes, the area around McGarity Lake is the most highly developed and and has the greatest potential for causing unacceptable pollution. That pollution could be carried through the other lakes within the system as described in view of the potential of the system, if the project is built, to convey a greater volume of water at a higher rate of flow. A more expansive water quality monitoring system within six lakes as opposed to three lakes would increase the opportunity to discover potential hazards from pollutant at an earlier data. This is particularly so by using lakes such as McGarity Lake where there is a higher level of developmental build-out.
Findings Of Fact During approximately 1961, the Board of County Commissioners of Orange County adopted the Orange County Conservation and Water Control Act. This act included a comprehensive drainage plan. Orange County is divided into several natural drainage basins. The Petitioner is presently actively seeking to implement the comprehensive drainage plan in what is known as the Upper Howell Branch drainage basin. The proposed Lateral H-15 forms a part of the drainage plan in the Upper Howell Branch drainage basin. The proposed Lateral H-l5 would begin at the outfall of Park Lake, and would extend approximately 1900 feet to Lake Maitland. Lateral H-l5 would allow the controlled lowering of Park Lake, with excess water flowing into Lake Maitland. Lateral H-15 as proposed would be a structure with a concrete paved bottom. It would be 18 feet wide, and would have vertical side walls constructed of aluminum siding. A weir would be constructed at the Park Lake outfall, and a new crossover would be constructed at the point where Highway 17-92 crosses over the project. The depth of the structure would be 5 feet. At peak flows water would flow at four foot depths leaving a one foot free area. The structure has been designed to allow passage of peak flows of water using as little land area as possible. Vertical side walls have been proposed in order to limit the amount of property which the Petitioner would need to obtain in order to construct the project. The Petitioner's comprehensive drainage plan is designed to ultimately prevent flooding which would result from a "25 year storm". The term "25 year storm" means that there is a 4 percent chance that such a storm would occur in any given year. The Petitioner's comprehensive plan for the Upper Howell Branch basin is depicted in an aerial photograph which was received into evidence as Petitioner's Exhibit 1. Generally, waters within the basin will flow from Lake Killarney through Lateral H-22, which is nearly completed, and from Lake Bell through the Lake Bell Lateral, which has been completed, into Park Lake. The Lake Bell Lateral and Lateral H-22 permit the controlled lowering of the water in Lake Bell and Lake Killarney into Park Lake. Lateral H-15 would permit the controlled lowering of the waters of Park Lake into Lake Maitland. Waters from Lake Maitland would then flow out of the drainage basin through Howell Creek which is now extremely swampy. Petitioner proposes ultimately to clear Howell Creek so that it can accept peak water loads from Lake Maitland. The proposed Lateral H-15 would follow the channel presently followed by a naturally occurring creek bed known as the Maitland Branch. Maitland Branch is a dried up waterway during dry weather periods. When waters in Park Lake rise during rainy seasons, overflow goes through the Maitland Branch into Lake Maitland. In addition storm runoff from areas surrounding the Maitland Branch drain into Maitland Branch and then into Lake Maitland. At its most Westward point, adjacent to Park Lake, the Maitland Brunch is approximately 40- 50 feet wide. A railroad crosses the branch near to the Park Lake outfall and the pipe and culvert under the railroad control the water level in the branch. The branch then extends under Highway 17-92, and into Lake Maitland. From the railroad, into Lake Maitland, Maitland Branch is confined to a narrow channel. The Maitland Branch is not a navigable water body. Lake Maitland is a navigable water body. Petitioner's proposed dredging activities would extend approximately 55 yards into Lake Maitland in order to permit the free flow of waters through the proposed Lateral H-15 into Lake Maitland. Maitland Branch is dominated by a variety of emergent and aquatic vegetation. Maitland Branch presently serves a significant function in preserving the waters of Lake Maitland. The water quality of Lake Maitland is presently good. Tests taken within the lake do not reveal violations of the Respondent's water quality rules and regulations. The lake is, however, dominated by hydrilla, and does not support a diverse aquatic plant population. The water quality in Lake Park is inferior to that of Lake Maitland. Lake Park is dominated by algal growths. During periods of high water, the waters of Park Lake flow through Maitland Branch. The aquatic vegetation in Maitland Branch serves to filter the waters and to assimilate nutrients contained in the water before the water enters Lake Maitland. Approximately 27 acres of impervious surfaces adjacent to the Maitland Branch drain directly into the branch. Storm water runs across the surfaces into Maitland Branch generally without the benefit of any filtration mechanism at all. Without the aquatic vegetation present in Maitland Branch, this storm water runoff would enter Lake Maitland without being filtered, and without nutrients being assimilated by vegetation. Aquatic vegetation in Maitland Branch does serve the filtration and assimilative functions outlined above. The degree of filtration and assimilation that is occurring is not subject to any finite measurement. No scientific means exists for accomplishing such a measurement. The very fact that the vegetation is flourishing, provides scientific evidence that the assimilation of nutrients is occurring. Furthermore, the large amounts of toxic substances which enter the Maitland Branch would cause a very rapid and provocative deterioration of the waters of Lake Maitland unless the runoff were filtered. The fact that the water of Lake Maitland is of fairly good quality evidences the fact that filtration and assimilation functions are occurring in Maitland Brunch. The Petitioner sought to demonstrate that the aquatic, vegetation in the Maitland Branch does not serve to filter the waters, or to assimilate nutrients. Petitioner's testimony tends to show that the water quality of waters at the Park Lake outfall and at the western extremes, of the Maitland Branch are of higher quality than waters at the end of Maitland Branch closest to Lake Maitland. This evidence is not creditable. In the first place the sampling techniques used by the Petitioner's agents were inadequate. Too few samples were taken to permit the drawing of any proper scientific conclusions. The samples were not taken simultaneously and in some cases samples taken at the Park Lake outfall were taken several days prior to the taking of samples at sampling stations closer to Lake Maitland. Furthermore, samples were taken at times when vegetation in the Maitland Branch was most sparse. One group of samples was taken just subsequent to a freeze which killed all of the vegetation. Another group of samples was taken shortly after the Petitioner had removed vegetation from the Maitland Branch in accordance with a temporary permit that had been issued by the Respondent (see discussion in paragraph 9 infra) Even if the Petitioner's samples had been taken in such a way that the conclusion could be drawn that the water quality in Maitland Branch is worse close to Lake Maitland that it is at the Park Lake outfall, it would still be clear that the aquatic vegetation in the branch is performing its important environmental function. Runoff from adjacent impervious surfaces into Lake Maitland constitutes water of the poorest possible quality. It is thus to be expected that the water quality of the branch would be worse at the points farthest from the Park Lake outfall where more runoff water can accumulate. This does not however permit the conclusion that no filtration and assimilation is occurring, but rather amplifies the necessity for such functions if the water quality of Lake Maitland is to be preserved. Petitioner's proposed Lateral H-15 would constitute a source of pollution for the waters of Lake Maitland. The concrete bottom of Lateral H-15 would reduce the PH level of water the branch and could result in violations of PH standards set out in the Respondent's rules and regulations. Emergent and attached aquatic vegetation could not exist in Lateral H-15. There would be no place for such vegetation to take root. The only sort of vegetation that could take hold would be water hyacinths. During peak water flows these hyacinths would be flushed out of the branch into Lake Maitland. While water hyacinths do serve to filter water that flows through them and to assimilate nutrients from the water, they are not attached, and do not serve that function as well as attached aquatic vegetation. Since water hyacinths would be washed out of the branch during periods of heavy storm runoff, when filtration and assimilation are most essential, they would not be likely to serve to maintain the water quality of Lake Maitland to the extent that the present vegetation in Maitland Branch serves this function. Lateral H-15, with the reduced ability to preserve water quality would permit water of inferior quality from Park Lake to enter Lake Maitland, and would permit storm runoff with high levels of pollutants to enter Lake Maitland. The amount of injury to water quality in Lake Maitland that would result from replacing Maitland Branch with Lateral H-15 cannot be measured finitely. It is, however, clear from the evidence that injury is certain. The frequency of water quality violations, the degree of degradation of the water, and the amount of consequent harm to fish and wildlife in Lake Maitland that will result from Petitioner's proposed project are matters for speculation. It does appear that violations will occur, that the water will be degraded, and that fish and wildlife will be harmed. The testimony will clearly not support a finding that Petitioner has given reasonable assurance that water quality violations will not occur, that the quality of water will not be degraded, and that fish and wildlife will not be harmed. The Respondent within recent months had issued a permit allowing the Petitioner to remove aquatic vegetation from the Maitland Branch between the railroad which crosses the branch near to the Park Lake outfall , and Highway 17-92 which crosses the branch approximately halfway between Park Lake and Lake Maitland. Issuance of this permit does not demonstrate that the Respondent sees no value in the aquatic vegetation of Maitland Branch. Aquatic vegetation will rapidly reestablish itself in the area, and it will be missing for only a temporary period. In addition, the Petitioner was permitted to remove vegetation from less than half of the length of Maitland Branch.
Findings Of Fact The Petitioner is a political subdivision of the State of Florida. Respondent, State of Florida, Department of Environmental Regulation, is an agency of the State of Florida charged with carrying out the mandates of Chapter 403, Florida Statutes, and the rules contained in the Florida Administrative Code promulgated thereunder. Respondent, MRT, is a real estate investment trust organized under the laws of the State of Maryland and authorized to do business in Florida. Royal Oaks Development Corporation is a Florida corporation, a wholly-owned subsidiary of Maryland Realty Trust. MRT is developing a parcel of land in Sections 33 and 34, T-2-N, R-1-E, Leon County, Florida, and Section 4, T-1-N, R-1-E, Leon County, Florida, of which approximately 60 acres has already been developed as Royal Oaks Unit No. 1, a recorded subdivision pursuant to Chapter 177, Florida Statutes. The balance of the 120 acres is yet to be developed, and is the subject of this proceeding. The specific activity for which the application for dredge and fill permit was submitted consists of improvements to a drainage-way running from the south boundary of the MRT property to a pond designated in the application as "Pond II", together with a drawndown structure, referred to as "S-15". Following submittal of the permit application, DER notified MRT of the receipt of the application and advised that both a permit under Chapter 403, Florida Statutes and a license for stormwater discharge under Rule 17-4.248, Florida Administrative Code, would be required. Following review by the Department, during which MRT was notified that the application in its original form would not be received favorably, MRT, on August 21, 1980, revised its application and based on such revisions, the Department, on October 10, 1980, notified MRT of its intent to issue the permit and license sought. As indicated in the Intent to Issue, DER has asserted jurisdiction over the dredge and fill activities in question contending that they are contemplated to either be in or connected to "waters of the State". Specifically, the Department's Intent to Issue states as follows: The Department has permitting jurisdiction under Chapter 403, Florida Statutes, Section 17-4.28, Florida Administrative Code, and Public Law 92-500 over dredge and fill activities conducted in or connected to certain waters of the State. The specific pond in question and the pond to which it is connected constitute waters of the State over which the Department has dredge and fill permitting jurisdiction as defined in Section 17-4.28, Florida Administrative Code. The project is not exempt from permitting procedures. Pond II is approximately four acres in size and consists of a western lobe of approximately one acre. Pond II is connected to the north to a waterbody known as Pond III/Foxcroft Lake". The vegetation in the south portion of Pond III is typical of fresh water vegetation that grows in submerged or wet areas. The vegetation in an existing well-defined channel between Pond II and the proposed location of structure S-15 is also comprised of water-tolerant species. Sagittaria subulata was observed in the channel in the area proposed for location of S-15. This plant species cannot tolerate dry conditions, indicating that water is present in the channel under most conditions. Further, no upland or pioneer species were observed in the channel, which also is indicative of the fact that the channel usually contains water. Water flows from Pond II to Pond III approximately 90 percent of the time. The base flow in the channel is approximately 2 cubic feet per second. Based on the storage capacity of Pond II, it is probable that flow occurs out of Pond II into Pond III under most conditions. Although 88.0 feet mean seal level is the design normal pond elevation expected after construction of S-15, the present observable elevation of Pond II appears to be between 89.94 and 90.09 mean sea level. Observations of the types of vegetation surrounding Pond II supports the conclusion that the existing normal level of Pond II is approximately 90.0 mean sea level. Pond III is a waterbody of approximately four acres in size and is a portion of the continuation of a larger 10 acre body of water referred to in this proceeding as "Foxcroft Lake". Pond III was the subject of a prior Department dredge and fill permit in which it was determined that Pond III constituted waters of the State subject to the dredge and fill jurisdiction of the Department. Pond III/Foxcroft Lake is a lake owned by more than one person, of approximately 14 acres of surface area and a maximum average depth of approximately 3 feet. Pond III/Foxcroft Lake discharges to and is connected directly to a waterbody known as Long Pond. Long Pond in turn is eventually connected to and discharges into Lake Lafayette. Without any mechanisms designed to treat the pollutants expected to be generated by the proposed project, the development by MRT of its 120 acres of property could reasonably be expected to have a significant adverse impact on the waters of Pond II, Pond III and Foxcroft Lake. Scientific studies demonstrate that potential pollutants generated from developments - single family, multi-family and commercial - have a significant impact on receiving waters if not treated before discharged. The project as presently designed will correct an existing source of pollution by removing sediment which is entering Pond II from the south from Shannon Forest Subdivision. This sediment has been deposited in the drainage- way between Shannon Forest and Pond II and is damaging and severely stressing biota in the drainage-way. This sediment has filled a portion of Pond II and could be expected to eventually discharge into Pond III/Foxcroft Lake. The pre-development rate of flow off the project site as it presently exists is approximately 600 cubic ft. per second. The project as proposed will reduce the rate of flow by 50 percent, to approximately 300 cfs. The project incorporates five mechanisms or abatement controls to treat contaminants customarily contained in stormwater: a grassed conveyance system; retention of natural vegetated areas; energy dissipators; sediment traps; and added storage. Grassed conveyance systems treat stormwater by the assimulation by plant communities of dissolved pollutants, such as nutrients, and the deposition of suspended pollutants that have absorbed to the sediment particles. Approximately 50 percent of the conveyance system in the Phase II development will be grassed swales and re-vegetated ditches. As many swales as possible will be used to convey the stormwater from the discharge at the street outfalls to the ponds. The main drainage ditch through the property will also be grassed. Natural vegetated areas to be left around the existing ponds will treat stormwater by assimilation and filtration in the same manner as the grassed swales and ditches. A one-acre parcel of wetlands is to be left between the southern most portion of the drainage-way and Pond II as described in MRT Exhibit No. 8 and in the revised permit application of August 21, 1980. The vegetation downstream of Pond II between the pond and control structure S-15 will also be left intact. Virtually all the vegetation bordering Pond II and Pond III will be left in place. Five energy dissipaters are to be constructed upstream of Pond II. These structures are designed to reduce the existing sedimentation and erosion problems by reducing the energy gradient and allowing the deposition of sediment, upon which absorbed pollutants have attached, into the accompanying sediment traps. Sediment traps are also to be constructed upstream of Pond II. Sediment traps treat stormwater by reducing the velocity gradient. Sediment and the pollutants absorbed to the sediment will drop out due to insufficient velocity. Storage will be increased in Pond II by the construction of control structure S-15 and by the planned excavation of Pond II. Added storage has a beneficial effect on water quality in that it allows additional sediment particles to settle out, allows additional time for the vegetation on the edge of the ponds to assimilate dissolved pollutants such as nutrients, and reduces the peak discharge velocity. The project is in the public interest in that it will alleviate an existing stormwater problem. In terms of probable efficiency, physical needs and costs, the project represents the best available treatment alternative. Based on existing technology, the system designed for this project is the most effective system within reasonable costs. The effectiveness of the stormwater treatment system depends on the presence of vegetation and will require less maintenance and attendant costs. There does not presently appear to be any local government effort to implement stormwater controls to address this problem or source. Petitioner submitted no evidence of such local government efforts. The system proposed by MRT will mitigate not only the effects of the discharge generated by the proposed development of the 120 acres of property owned by MRT, but will also mitigate the effects of an existing source of stormwater pollution. The system, as designed, is sufficient to afford the Department reasonable assurance that stormwater quality standards will not be violated. The parties stipulated that, should the requested permit and license be issued, they should incorporate the following additional condition: Roads and drainage facilities are to be owned and maintained by Leon County. All paving and drainage shall be done in accordance with the County's standards, details and specifications. In addition, MRT has instituted civil litigation against Leon County concerning the property involved in this proceeding. One of the allegations of MRT's complaint is that Leon County has, through the action amounting to inverse condemnation, acquired a drainage easement over the property for which MRT is now seeking the dredge and fill and stormwater permits. The plans submitted to DER by MRT with its application contain the following: When the construction plans for Phase III of the Royal Oaks development are prepared, these plans shall be submitted to the Department for evaluation for compliance with the original stormwater review.
Findings Of Fact Background Petitioner, David E. Musselman, is the owner of Lot 23, Block 22, Cudjoe Gardens Eighth Addition, Cudjoe Key, Monroe County, Florida. The lot measures 127 feet along its front and rear property line, 135 feet along its side property lines and, similar to adjacent lots, its rear property line abuts an artificially created waterway. Currently, most of petitioner's lot enjoys an elevation of six feet; however, from the edge of the waterway landward a distance of approximately 20 feet [to what has been referred to as the "toe of the existing slope" in these proceedings] the surface consists of exposed caprock at an elevation of approximately four inches above mean high water. It is petitioner's desire to construct a single family residence upon such lot and, incident to such construction, to erect a seawall along the edge of the waterway such that the elevation at the waterway will be increased by two feet, and to backfill from the seawall to his home. Such backfilling would require the deposition of approximately 3,540 square feet of fill within the Department's jurisdiction, which was shown to extend from the edge of the waterway to the toe of the existing slope, and would raise the elevation in such area two feet above existing grade. On December 16, 1991, petitioner filed an application with respondent, Department of Environmental Regulation (Department), for an exemption from the Department's wetland permitting requirements. If approved, such exemption would allow petitioner to construct the vertical seawall along the waterway, and backfill from the seawall to his proposed home. By notice of agency action dated February 14, 1992, the Department proposed to deny petitioner's application predicated on its conclusion that his proposal did not meet the exemption criteria established by Rule 17- 312.050(1)(g), Florida Administrative Code. Petitioner filed a timely protest to contest the Department's conclusion. The exemption Pertinent to this case, Rule 17-312.050(1)(g), Florida Administrative Code, exempts from permitting the following activities: (g) Construction of seawalls or riprap, including only that backfilling needed to level the land behind the seawalls or riprap, in artificially created waterways where such construction will not violate existing water quality standards, impede navigation or adversely affect flood control. An artificially created waterway shall be defined as a body of water that has been totally dredged or excavated and which does not overlap natural surface waters of the state. For the purpose of this exemption, artificially created waterways shall also include existing residential canal systems . . . . At hearing, the parties stipulated that the waterway which abuts the rear property line of petitioner's lot is an artificially created waterway, as well as an existing residential canal, and that the proposed project will not violate existing water quality standards, impede navigation, or adversely affect flood control. Notwithstanding, the Department contends that petitioner's application should be denied because no need has been demonstrated that would support the construction of the seawall along the edge of the waterway, as opposed to locating it further inland, and therefore the amount of backfill, with its attendant loss of wetlands, is excessive. For the reasons set forth in the conclusions of law, the Department's position is untenable as a matter of law. 1/
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Department enter a final order approving petitioner's application for an exemption to construct a seawall, and to backfill from such seawall to his proposed home, as applied for. DONE AND ENTERED in Tallahassee, Leon County, Florida, this 4th day of June 1992. WILLIAM J. KENDRICK 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 4th day of June 1992.
Findings Of Fact On November 1, 1982, Respondent Janson filed a Joint Application for a dredge and fill permit from Respondent, Department of Environmental Regulation, and from the Department of the Army Corps of Engineers. The project described in that application involved the construction of an approximately 1,000-square- foot, pile-supported residence, landward of the mean high water line but within the landward extent of Robinson Creek in St. Johns County, Florida. The proposed project also involved the placement of approximately 35 cubic yards of fill and a 30-foot culvert within a small (approximately 4-foot), tidally- influenced roadside ditch for driveway access and parking. The original application sought permission to place part of a concrete driveway and tool shed within the landward extent of Robinson Creek. The project is to be constructed on Lot 47, J.A. Lew Subdivision. Respondent Janson owns Lot 47, as well as Lots 45 and 46, which lots are north of and adjoining Lot 47 and also adjoining Robinson Creek. The next adjoining property owner to the north is the City of St. Augustine, Florida, which presumably owns the street. The adjoining property owner to the south of Lot 47 is Virginia P. Melichar. Neither Melichar nor the City objected to the Department's approval of the dredge and fill permit application. In support of his application, Janson retained the services of a registered surveyor and civil engineer, who performed a survey on Lot 47 to determine the location of the mean high water line with reference to the proposed project. That expert determined the location of the mean high water line to be at elevation 2.4 feet. Accordingly, all work contemplated by the dredge and fill permit is upland from the mean high water line. T.J. Deuerling, an environmental specialist for Respondent, Department of Environmental Regulation, visited the project site on December 13, 1982 and on December 30, 1982 in order to prepare the Department's Biological and Water Quality Assessment. As a result of those site visits, Deuerling recommended to Respondent Janson that he modify his permit application by moving the concrete slab and tool shed from the marsh area onto the uplands. Janson did so revise his application. In spite of the name of the permit being sought by Respondent Janson, the project involves no dredging. However, the culvert and its attendant fill would be placed in the man-made roadside ditch. That ditch constitutes a very weak transitional marsh. Although the culvert will eliminate some vegetation within that ditch, the effect of the elimination will be insignificant on water quality. The pilings for the pile-supported residence will also eliminate a small area of marsh. The anticipated shading caused by the pile-supported residence may impact somewhat on the vegetation in a small area below the residence; however, due to the fact that the floor of the house will be eight feet above the ground, light will still be able to penetrate. Therefore, the vegetation below the pile-supported residence will continue to act as a filter for pollutants. Janson has mitigated the small loss in wetlands by modifying his project so as to remove the concrete slab and tool shed from the marsh area to the uplands. Due to the project's small size, no storm water impact can be expected. Additionally, no evidence was introduced to show a violation of any water quality standard as a result of the proposed project. On March 16, 1983, Respondent, Department of Environmental Regulation, executed its Intent to Issue the dredge and fill permit in accordance with the revised application and subject to the conditions that: (1) turbidity curtains be employed in the ditch during the placement of fill over the culvert to contain any turbidity generated, and (2) construction on the uplands be confined to periods of normal water level conditions. On July 5, 1983, the Department of the Army Corps of Engineers issued its Permit and Notice of Authorization. The essence of the testimony presented by the Petitioners, including that of the employees of the St. Johns River Water Management District, who testified in opposition to the proposed project, is that even though Janson's proposed project would not impact water quality in a way that was either significant or measurable (although no one even suggested any specific water quality standard that might be violated), approval of Janson's permit might set a precedent for other projects which might then have a cumulative impact in some unspecified way at some unspecified location. No evidence was offered to show that Respondent, Department of Environmental Regulation's review of permit applications is other than site specific. Further, no evidence was introduced to show any proposed project anywhere having any impact with which Janson's project could be cumulative. Petitioners Sandquist and Shuler live in the neighborhood of the proposed project, perhaps as close as two blocks away.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that a Final Order be entered dismissing with prejudice the petition filed herein as to each individual Petitioner and issuing a dredge and fill permit to Respondent Janson in accordance with his revised application. DONE and RECOMMENDED this 13th day of January, 1984, in Tallahassee, Leon County, Florida. LINDA M. RIGOT, 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 13th day of January, 1984. COPIES FURNISHED: Stormy Sandquist 3 Aviles Street St. Augustine, FL 32084 Marion C. Snider Volla F. Snider 79 Fullerwood Drive St. Augustine, FL 32084 Carmen Ashton 51 East Park Avenue St. Augustine, FL 32084 Reuben D. Sitton Gail P.Sitton 35 Seminole Drive St. Augustine, FL 32084 Sandra N. Shuler 22 East Park Avenue St. Augustine, FL 32084 Patty Severt Greg Severt 1 Fern Street St. Augustine, FL 32084 Nancy Moore Paul Moore, Jr. 6 Fern Street St. Augustine, FL 32084 John D. Bailey, Jr., Esq. P.O. Box 170 St. Augustine, FL 32085-0170 Charles G. Stephens, Esq. Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, FL 32301 Victoria Tschinkel, Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, FL 32301
The Issue The issues to be determined in this proceeding are: whether the challengers have standing; and (2) whether Proposed Rule 40E-8.221(2) is an invalid exercise of delegated legislative authority.
Findings Of Fact Based on the parties' stipulations and the evidence adduced at the final hearing, the following findings of fact are made: The Parties The District is a government entity existing and operating pursuant to chapter 373, Florida Statutes, as a multi- purpose water management district. The District has the power and duty to adopt MFLs consistent with the provisions of part I of chapter 373. Sanibel is a barrier island sanctuary in Lee County and a duly-formed municipality with a population of more than 6,000. Sanibel is situated at the mouth of the Caloosahatchee River, within the Caloosahatchee's greater estuarine area. Sanibel is known primarily for its natural beauty, including clear blue waters, shell beaches, world-class sport fisheries, and wildlife refuges. That is why tourists come from around the globe to visit Sanibel, and why Sanibel's residents move and remain there. Sanibel actively participated in the rulemaking process for the Proposed Rule from its inception. Sanibel submitted two technical comment letters to the District during the development of the Proposed Rule. Sanibel's natural resources director, James Evans, attended numerous public and technical meetings associated with the development of the Proposed Rule, speaking on the record at each of the public meetings prior to the adoption hearing by the District's governing board. The Town, located on Estero Island in Lee County, is also a barrier island community and duly-formed municipality with a population of more than 6,000. The Town is situated just south of the mouth of the Caloosahatchee River and on the southeastern edge of the Caloosahatchee River's greater estuarine area. The Town is known primarily for its natural beauty, including clear blue waters, shell beaches, world-class sport fisheries, and wildlife refuges. Cape Coral is a duly-formed municipality in Lee County and is the largest city between Tampa and Miami, with a population in excess of 150,000. Cape Coral is bordered on the south by the Caloosahatchee River and has over 400 miles of navigable canals and waterways, all of which are within the Caloosahatchee River's greater estuarine area. In addition, Cape Coral has an assigned load reduction allocation under the Basin Management Action Plan (BMAP) for the Caloosahatchee River Estuary (CRE) due to it being designated as impaired for dissolved oxygen and nutrients. Maintaining sufficient flow in the Caloosahatchee River would have a direct impact on Cape Coral's ability to meet its assigned load reduction allocation. In addition to living on or near the water, a substantial number of the residents of Sanibel, Cape Coral, and the Town engage in water-based recreational activities such as swimming, fishing, boating, kayaking, paddle boarding, bird watching, and nature observation in and around the Caloosahatchee River's greater estuarine area. Fort Myers is a duly-formed municipality in Lee County and has a population of approximately 80,000. Fort Myers is bordered by the CRE throughout its entire jurisdictional boundary. Fort Myers owns and maintains a yacht basin (Ft. Myers Yacht Basin), which includes a mooring field and an anchorage field in the Caloosahatchee River. Fort Myers presented testimony that commercial crabbing and recreational fishing have declined and that it has suffered economic harm due to water quality issues. Fort Myers owns the submerged land in the Caloosahatchee River from Marker 39 to Marker 58, and islands in the river. One such island will be used as a park for recreational activities such as canoeing, kayaking, and hiking for visitors to enjoy the Caloosahatchee River. Fort Myers also owns and operates piers and a public boat ramp within the Caloosahatchee River. Fort Myers' dock master has observed declines in seagrasses in the Caloosahatchee River during his 19-year career working at the Ft. Myers Yacht Basin. Fort Myers has adopted a Harbor Management Plan for the management of its mooring and anchorage fields in the Caloosahatchee River. Fort Myers has also been assigned a load reduction allocation under the BMAP for the CRE, and is responsible for a certain amount of pollution reduction over time. Bonita Springs is a municipality of more than 50,000 in Lee County. The borders of Bonita Springs include portions of Estero Bay, which, along with San Carlos Bay and the Caloosahatchee River, is part of the greater Lower Charlotte Harbor Estuary. Bonita Springs includes wildlife refuges, such as the Estero Bay Aquatic Preserve and Lovers Key State Park and Recreation Area. While Bonita Springs' strategic priorities include environmental protection and water quality, it does not have environmental staff or test water quality. Bonita Springs participates in Estero Bay Management and the Charlotte Harbor National Estuary Program (CHNEP). Bonita Springs provides financial assistance to the Caloosahatchee Citizen Sea Grass Gardening Project. Concerns regarding harm to the CRE and tape grasses are shared by a significant number of residents in Bonita Springs and Estero, including injury to the quality of life and recreational uses such as swimming, boating, and kayaking in the waterways. Estero is a municipality of more than 30,000 in Lee County. Estero borders the eastern portion of Estero Bay. Estero includes wildlife refuges, such as Estero Bay Aquatic Preserve and Koreshan State Park. While Estero has environmental policies, it does not have environmental staff or test water quality. Estero makes financial contributions to CHNEP. Estero is concerned that the Proposed Rule will affect its water quality, which could affect its residents' quality of life. Estero believes it could be harmed by poor water quality because its residents are portable retirees who can move away, or tourists who can choose not to visit. Captiva Island is situated at the mouth of the Caloosahatchee River, within the Caloosahatchee's greater estuarine area. CCP is a Florida not-for-profit corporation representing property owners, businesses, and the community of Captiva Island. Captiva Island is part of unincorporated Lee County and is located north of Sanibel. CCP has 200 financial contributors comprised of property owners, businesses, and residents on Captiva Island. CCP's mission includes protection of clean off-shore water, diverse and healthy marine life, and robust native vegetation along with the protection of mangrove fringe and water quality. CCP works with Lee County on provisions of the County's comprehensive plan, which include the quality of adjacent waters. CCP relied on the expertise of James Evans, the director of natural resources for Sanibel, and on the Sanibel- Captiva Conservation Foundation (SCCF). CCP was advised that the Proposed Rule was not sufficient to protect the environment and Vallisneria americana (Vallisneria) or tape grass during the dry season. Caloosahatchee River and Estuary The watershed of the Caloosahatchee River covers approximately 861,058 acres. The watershed consists of four sub-watersheds, three of which are upstream of the S-79 structure. The Tidal Caloosahatchee Basin sub-watershed (estuarine system) is downstream of the S-79 structure. The S-79 structure captures all the upstream discharges of fresh water that go into the estuarine system through the S-79 structure. Major tidal tributaries of the Tidal Caloosahatchee Basin are the Orange River and Telegraph Creek, which drain into the upper estuary downstream of the S-79 structure. Fresh water inflows from these and other tributaries also contribute fresh water into the estuarine system. The Caloosahatchee River was originally a natural watercourse running from its origin at Lake Flirt to San Carlos Bay. It is currently defined as the "surface waters that flow through the S-79 structure, combined with tributary contributions below S-79 that collectively flow southwest to San Carlos Bay." Fla. Admin. Code. R. 40E-8.021(2). Man-made alterations to the Caloosahatchee River began as early as 1884, but major alterations began in the 1930s with the authorization and construction of the C-43 Canal. The C-43 Canal runs 41.6 miles from Lake Okeechobee at Moore Haven, i.e., from the S-77 structure, to Olga, i.e., the S-79 structure. The C-43 Canal serves as a conveyance feature to drain water from the three sub-watersheds located upstream of the S-79 structure and convey regulatory discharges of water from Lake Okeechobee. In 1957, the United States Army Corps of Engineers (USACOE) prepared a report focused on drainage, flood control, and navigation needs of the Caloosahatchee River Basin, and one recommendation was construction of the S-79 structure. The key objectives of the S-79 structure were to eliminate undesirable salinity in the lower Caloosahatchee River, prevent the rapid depletion of water supplies, and raise the prevailing dry weather water table levels. The S-79 structure was constructed in 1965. It is a lock and dam structure that is also known as the Franklin Lock and Dam. The S-79 structure captures all upstream fresh water discharges that go into the CRE. The S-79 structure demarcates the head of the CRE, which extends 26 miles downstream to Shell Point, where it empties into San Carlos Bay in the southern portion of the greater Lower Charlotte Harbor Estuary. Most of this surface water flow takes a southerly route, flowing to the Gulf of Mexico under the Sanibel Causeway that crosses San Carlos Bay. When fresh water inflows are high, tidal action pushes some of this water back up into Matlacha Pass and Pine Island Sound. Additionally, some water exits to the south and flows into Estero Bay through Matanzas Pass. Salinity exhibits a strong gradient in the CRE. Changes in the watershed upstream of the S-79 structure have profoundly influenced the delivery of fresh water to the CRE. Runoff is now more variable with higher wet season flows and lower dry season discharges. Large volumes of fresh water during the wet season can flush salt water from the tidally-influenced sections of the water body, resulting in low salinity conditions throughout most of the CRE. In contrast, fresh water inflow at the S-79 structure can stop entirely during the dry season, especially during significant drought events. This results in saline intrusion that can extend upstream to the S-79 structure. Fluctuations of this magnitude at the head and mouth of the system cause mortality of organisms at both ends of the salinity gradient. Downstream of the S-79 structure, the CRE was significantly altered by multiple dredging activities, including the removal of extensive shoals and oyster bars. Seven automobile bridges, a railroad trestle, and the Sanibel Causeway were built between the 1880s and 1960s. A large canal network was built along the northern shoreline of the CRE in Cape Coral. To provide navigational access from the canal network to deeper water, multiple access channels were dredged within the CRE. Alterations to the delivery of fresh water combined with structural changes to the tidally-influenced sections of the water body have had lasting ecological consequences. These include the loss of extensive shoals and oyster bars, loss of a flourishing bay scallop fishery, and significant decline in seagrass cover in deeper areas. MFLs An MFL is the limit at which further withdrawals would be significantly harmful to the water resources or ecology of the area. The District's rules define significant harm as the "temporary loss of water resource functions, which results from a change in surface or ground water hydrology, that takes more than two years to recover, but which is considered less severe than serious harm." Fla. Admin. Code R. 40E-8.021(31). The rule further specifies that a water body's specific water resource functions addressed by an MFL are defined in the MFL technical support document. Id. MFLs are calculated using the best information available. The regulatory agency is required to consider changes and structural alterations to watersheds, and the constraints such changes or alterations placed on the hydrology of an affected watershed. Certain waterbodies may not serve their historical hydrologic functions and recovery of these waterbodies to historical hydrologic conditions may not be economically or technically feasible. Accordingly, the regulatory agencies may determine that setting an MFL for such a water body based on its historical condition is not appropriate. Caloosahatchee MFL For the CRE, MFL criteria were designed to protect the estuary from significant harm due to insufficient fresh water inflows and were not guidelines for restoration of estuarine functions to conditions that existed in the past. The MFL criteria consider three aspects of the flow in terms of potential significant harm to the estuary: (1) the magnitude of the flow or the volume of fresh water entering the estuary; (2) the duration of time that flows can be below the recommended level before causing significant harm; and (3) the return frequency, or the number of times the MFL can be violated over a number of years before it results in significant harm, recognizing that natural climatic variability will be expected to cause fresh water inflows to fall below recommended levels at some natural frequency. The CRE MFL initially adopted in 2001 was primarily based on the salinity tolerance of one valued ecosystem component (VEC). The VEC was Vallisneria americana or tape grass, a fresh water aquatic plant that tolerates low levels of salinity. A major assumption of this approach was that flow and salinity conditions that protect Vallisneria would also protect other key organisms in the estuary. The 2001 CRE MFL was based on a regression model for estimating the relationship between surface salinity measured at the Ft. Myers monitoring station located in the Ft. Myers Yacht Basin and discharge at the S-79 structure. Although the District monitors surface and bottom salinity at multiple stations in the CRE, the Ft. Myers monitoring station is located centrally in the CRE and at the historical downstream extent of the Vallisneria habitat. The Ft. Myers monitoring station also has the most comprehensive period of record of monitoring data available. The fixed data sondes that monitor surface and bottom salinity are located at 20 percent and 80 percent of total river depth measured at mean low water. The data sondes continuously measure temperature and specific conductivity and, depending on the manufacturer, contains programs that calculate salinity. Those calculations are based on standards recognized and used worldwide by estuarine, marine, and oceanographic scientists.1/ The regression model only implicitly included inflows from the Tidal Caloosahatchee Basin sub-watershed downstream of the S-79 structure. To address this, during the 2003 re-evaluation, a linear reservoir model of Tidal Caloosahatchee Basin inflows was developed. The regression model results showed that a total inflow from S-79 plus the Tidal Caloosahatchee Basin of about 500 cubic feet per second (cfs) was required to produce a salinity of 10 at the Ft. Myers monitoring station. Thus, the 2001 CRE MFL of 300 cfs measured at the S-79 structure would produce a salinity of 10 at the Ft. Myers monitoring station only with additional inflow from the downstream Tidal Caloosahatchee Basin sub- watershed. However, that additional inflow estimate was highly uncertain. The conclusion was that actual flow measurements over a period of time were needed in order to perform more robust calibrations for the new models that were being developed. The Re-evaluation The District's re-evaluation effort began in 2010 after the Conservancy of Southwest Florida filed a petition requesting review of the Caloosahatchee MFL. At the time, the governing board denied the petition but directed staff to undertake additional research and monitoring to ensure a future revision would be supported by the best information available. The first step was to review the September 2000 Final Peer Review Report (PRR) for the initial adoption. The 2000 PRR identified several items the District should consider, including a hydrodynamic salinity model, a numerical population model for Vallisneria, quantification of habitat value for Vallisneria, and documentation of the effects of minimum flows on downstream estuarine biota. The 2000 PRR documented concerns that the current MFL was based solely on the salinity tolerance of Vallisneria and recommended using multiple indicator species. To address those recommendations, the District conducted studies to evaluate multiple ecological indicators, such as zooplankton, aquatic vegetation, oysters, benthic communities, and blue crabs, in the Caloosahatchee from the S-79 structure to beyond Shell Point. In addition, the District collected flow data from the Tidal Caloosahatchee Basin sub-watershed for at least five years to develop watershed, flow, and hydrodynamic models that could properly simulate inflows and salinity responses. When the initial research was complete in 2016, the District published the Draft Science Document containing 11 component studies. In September 2016, the District held a two- day Science Symposium to present the 11 component studies and gather public comment. In response to public comment, the District performed additional evaluations, modeling, and updated the component studies to produce a Draft Technical Document. A Peer Review Panel reviewed the Draft Technical Document, which included the Draft Science Document. The Peer Review Panel has over 150 years of combined relevant scientific experience. The Peer Review Panel toured the CRE by air and water. The District also held a Peer Review Session to engage the public and obtain feedback. The Peer Review Panel's 2017 report (PRP report) stated that the District had "crafted a well-executed and well- documented set of field and laboratory studies and modeling effort" to re-evaluate the CRE MFL. The PRP report supported the 11 component studies, the modeling, the evaluations, and the initial proposed rule language. The Final Technical Document published in January 2018 incorporated five different models and additional science, examining the entire watershed and the criteria itself. The Final Science Document was Appendix A to the Final Technical Document and contained the scientific research and analysis that was done for the 11 component studies, the modeling, and the additional scientific analyses performed in response to public and stakeholder input. The District initiated rule development in December 2017. Rule development workshops were held in February and June 2018 and a stakeholder technical meeting was held in May 2018. The District validated the comments after each workshop and meeting, and revised the proposed rule language. The District published its Notice of Proposed Rule on July 23, 2018.2/ At its September 13, 2018, meeting, the District's governing board held a public hearing on the Proposed Rule. The mayors of Sanibel, Cape Coral, and the Town publicly commented at the hearing. After considering public comments, the governing board adopted the Proposed Rule. The District documented and responded to each public comment, memorializing the information in the Final Technical Document. Later, after the rule workshops and May 2018 technical meeting, the District prepared and presented all of the updated information, including public comment, at the September 2018 adoption hearing. Thus, the District's re-evaluation process was open and transparent. The Re-evaluated Caloosahatchee MFL The science supporting the re-evaluation involved a comprehensive assessment of the effects of diminished dry season fresh water inflows on the CRE. The dry season was chosen for two reasons. First, because it is well-established that the upstream migration of salt combined with reduced fresh water inflow alters the health and productivity of estuarine habitats. Second, because the dry seasons are the times when the current MFL criteria are likely to be exceeded or violated. The 11 component studies targeted specific concerns regarding physical and ecological characteristics. Together they offered a holistic understanding of the negative effects of diminished fresh water inflow on estuarine ecology. The re-evaluated MFL criteria were developed using a resource-based approach. The approach combined the VEC approach and the habitat overlap concept. The habitat overlap approach is based on the idea that estuaries serve a nursery function and salinity determines the distribution of species within an estuary, including distribution during different life stages. The combined approach studied the minimum flow requirements of the various indicator species in terms of magnitude, duration, and return frequency, resulting in the following three aspects of the flow: (1) for magnitude, a 30-day moving average flow of 400 cfs measured at the S-79 structure; for duration, an MFL exceedance occurs during a 365-day period when the 30-day moving average flow at S-79 is below 400 cfs and the 30-day moving average salinity exceeds 10 at the Ft. Myers salinity monitoring station; and (3) for return frequency, an MFL violation occurs when an exceedance occurs more than once in a five-year period. The magnitude component is based on the salinity requirements of Vallisneria, along with results from the 11 studies modeling salinity and considering the salinity requirements of the other VECs. The duration component is based mainly on the estimates of rate of loss of Vallisneria shoots when salinity rises above 10 and the recovery rate of the shoots when salinities fall back below 10. Return frequency was determined based on long-term rainfall records rather than flow measurements from the S-79 structure, which the PRP report felt was well justified. In addition to the component studies, the re-evaluated MFL criteria and existing recovery strategy were evaluated using a suite of hydrologic and ecological models simulating long-term fresh water inflow to the CRE associated with varying management options, the resulting salinity in the CRE, and the ecological response of indicator species that are sensitive to low fresh water inflows. Five models were utilized. Three models simulated fresh water inflows to the CRE: two for S-79 flows; and one for Tidal Caloosahatchee Basin sub-watershed flows. The other two models were a three-dimensional hydrodynamic salinity model and a Vallisneria model. Tidal Caloosahatchee Basin sub-watershed has a number of tributaries that drain fresh water into the CRE. The flow at several of the tributaries was monitored for a five-year period. The measured flow was used to calibrate a watershed model and conduct a long-term simulation. The results showed an average fresh water inflow for all seasons of approximately 430 cfs. The average fresh water inflow during the dry season was 245 cfs while the wet season average fresh water inflow was 613 cfs. Fresh water inflow from the Tidal Caloosahatchee Basin sub- watershed was approximately 20 percent of total fresh water inflow to the CRE while 80 percent was released through the S-79 structure. Petitioners' and Intervenors' Objections 400 cfs Is Too Low Sanibel relied on a memorandum prepared by Dr. David Tomasko (Tomasko report) concerning his company's review of the January 2018 Final Technical Document supporting the Proposed Rule. The Tomasko report, dated October 23, 2018, was in the form of a "technical memorandum" outlining "preliminary findings." The Tomasko report was admitted as a joint exhibit; however, Dr. Tomasko did not testify at the final hearing. The Tomasko report is hearsay that was not used to supplement or explain competent direct evidence. Although hearsay is admissible in this proceeding, it cannot be the sole basis for a finding of fact.3/ See § 120.57(1)(c), Fla. Stat. The District's expert witnesses, who testified at the final hearing, explained that ten of the 11 component studies identified average indicator flows at S-79 ranging from 237 to 545 cfs with standard deviations ranging from plus or minus 57 to plus or minus 774 cfs.4/ The District's experts performed three different evaluations of those flow results. They identified the mean of all the means, calculated the median of the means, and performed a probability density function. The flow results for each of the three evaluations were 381 cfs, 400 cfs, and 365 cfs, with standard deviations that ranged from plus or minus 277 cfs to plus or minus 706 cfs. The District's experts testified that the three flow results are indistinguishable from a statistical point of view. The District chose 400 cfs because it was the highest flow result, and, therefore, the most protective of the three. The Petitioners and Intervenors failed to present evidence that showed any deficiencies in the District's component studies, hydrologic, hydrodynamic, or statistical modeling, or analysis of compliance data. The preponderance of the evidence established that the District used the best available science to calculate the MFL criteria. The District did not act arbitrarily or capriciously when it chose 400 cfs as the magnitude component of the MFL criteria. Inclusion of Salinity in the MFL Criteria The preponderance of the evidence also established that Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE. It supports essential ecological goods and services, is sensitive to salinity fluctuations at the ecosystem scale, and has value to a variety of stakeholders. The location of Vallisneria habitat in the upper CRE and its negative response to increased salinity made it an excellent candidate as an ecological indicator for fresh water inflow. A combination of field monitoring, mesocosm studies, and modeling results allowed the application of Vallisneria responses as a platform to quantify the effects of high salinity duration in the upper CRE. Component Study Eight reviewed the development and initial application of a simulation model for Vallisneria in the CRE. The Vallisneria model was used to evaluate the salinity conditions that led to net annual mortality, or, in other words, the duration of high salinity exposure that led to decreased Vallisneria shoots versus the duration of low salinity conditions required for recovery. Component Study Seven included an analysis of the relationship between the number of consecutive days where salinity at the Ft. Myers monitoring station was greater than 10 and the percentage of initial Vallisneria shoots remaining at the end of each high salinity period. To further evaluate the duration element associated with the MFL criteria, the field monitoring data contained in Component Study Seven was evaluated with the mesocosm and modeling results. All three sources were analyzed similarly to derive a combined curve showing high salinity exposure duration that is significantly harmful to Vallisneria. The model also provided information that was used to quantify the duration of low salinity conditions required for Vallisneria to recover a relative fraction of shoots after high salinity exposure. Merging the exposure and recovery evaluations facilitated a determination of the unfavorable salinity duration that could significantly harm Vallisneria habitat. With significant harm defined as the environmental harm from which two years are required to recover, the determination was that Vallisneria should experience no more than 55 consecutive days of salinity greater than 10. However, stakeholders expressed concerns regarding the percentage loss of Vallisneria habitat after 55 days of high salinity exposure. In response, the District conducted further analysis of modeling results and revised the duration component to accept the stakeholder recommendation, now expressed in the Proposed Rule, of a 30-day moving average salinity greater than 10. The Petitioners and Intervenors argued that by expressing the MFL as a "flow plus salinity component" the Proposed Rule enlarges, modifies, or contravenes the specific provisions of law implemented. However, the duration component is part of compliance and represents the duration of time that flows can be below the recommended level before causing significant harm to the indicator species Vallisneria. The MFL in the Proposed Rule is a 30-day moving average flow of 400 cfs measured at the S-79 structure. Flow is both measured and operationally controlled at the S-79 structure. However, as previously found, there are other sources of fresh water entering the CRE downstream of the S-79 structure. The District does not control and cannot control these downstream sources, which modeling reveals contribute approximately 20 percent of total fresh water inflow to the CRE. By including salinity, the District can account for fresh water inflows coming from the tidal basin when there are low or no flows at S-79 since the significant harm threshold in the CRE is directly related to salinity tolerance of the indicator species Vallisneria. The District's experts also testified that salinity can be used as a flow component because it is not affected by chemical or biological processes and is an indicator of how much fresh water is entering the system.5/ Salinity is included in the duration component of the MFL criteria and is an exceedance criterion because the science established that the salinity gradient is crucial to the overall health of the CRE. Including salinity in the duration component of the MFL criteria achieves the purpose of the statutory mandate to set MFLs that are designed to avoid significant harm to the water resources and ecology of the area. No Unit of Measurement for Salinity The Petitioners and Intervenors argued that the Proposed Rule is vague because the language does not contain any units for salinity. The UNESCO calculation is the standard equation used by the estuarine and marine science community to convert specific conductivity and temperature data to salinity. The District's experts testified that the UNESCO calculation reports salinity as a ratio, which is a dimensionless number and has no units. The District uses the UNESCO calculation and performs the conversion in a spreadsheet that it maintains. In some instances, certain brands of data sondes are programmed to perform the calculation and provide the salinity number. The preponderance of the evidence established that use of the practical salinity unit (PSU) is not technically correct. PSU is a misnomer, a pseudo-unit equivalent to a unitless salinity number. The Petitioners' and Intervenors' expert witness, Dr. Anthony Janicki, conceded there is no difference between reporting salinity as unitless or as PSU. And although technically incorrect, he suggested that placing the word "practical" or putting "PSU" in the Proposed Rule would reduce confusion and vagueness. However, since the preponderance of the evidence established that use of PSU is not technically correct, the use of a pseudo-unit would actually cause confusion instead of reduce confusion. The Petitioners and Intervenors also argued that the Proposed Rule is vague because the language does not state that the method of measuring salinity is specific conductivity, or that the equation used to convert specific conductivity and temperature data to salinity is the standard developed by UNESCO. The Petitioners and Intervenors essentially argued that members of the public and those who may be regulated by the Proposed Rule are left to guess about the method or methods used to measure salinity. Because the Proposed Rule identifies and locates by latitude and longitude coordinates the Ft. Myers salinity monitoring station as the location where salinity would be measured for compliance, the Proposed Rule language is not vague. The Proposed Rule is not vague because it does not describe the data sondes, what parameters are measured by the data sondes, and how those parameters are converted to a salinity number. Salinity Monitoring Location and Mean Low Water The Petitioners and Intervenors argued that the Proposed Rule is vague for failing to define the phrase "20% of the total river depth at mean low water," and is arbitrary or capricious for failing to include more than one salinity monitoring station. Total river depth or the water column depth is a standardized measurement that is made from the surface down to the bottom of the river bed. Mean low water is commonly understood in the oceanographic and coastal sciences community as the average of all low tides over the time period defined as the national tidal datum epic. The District's expert witness, Dr. Cassondra Armstrong, testified that mean low water can be determined by using two documents prepared by the National Oceanographic and Atmospheric Administration (NOAA), i.e., the NOAA tide charts and glossary. The District's expert witnesses testified that "20% of the total river depth at mean low water" is the location of the data sonde at the Ft. Myers monitoring station that measures surface salinity. This is also the depth at which Vallisneria is located in the CRE. Since, the Proposed Rule language simply identifies the location of the existing data sonde at the Ft. Myers salinity monitoring station, the language is not vague. The preponderance of the evidence established that the Ft. Myers salinity monitoring station has two salinity data sondes, the one at 20 percent of the total river depth and the other at 80 percent. The data sonde at 20 percent of the total river depth was identified in the Proposed Rule for the following reasons. First, this is the depth where Vallisneria grows and is representative of the salinity exposure for Vallisneria. Second, it guarantees the data sonde is always submerged and able to record data. Third, it has the most comprehensive period of record of monitoring data available. As previously found, Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE. The location of Vallisneria habitat in the upper CRE and its negative response to increased salinity made it an excellent candidate as an ecological indicator for fresh water inflow. Because the preponderance of the evidence established that Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE, the choice of the Ft. Myers monitoring station is not arbitrary or capricious. Water Resource Functions vs. Environmental Values The District's MFL rule specifies that a water body's specific water resource functions addressed by an MFL are defined in the MFL technical support document. See Fla. Admin. Code R. 40E-8.021(31). The Final Technical Document identified the relevant water resource functions of the CRE as fish and wildlife habitats, estuarine resources, water supply, recreation, navigation, and flood control. The Petitioners and Intervenors argued that the environmental values listed in Florida Administrative Code Chapter 62-40, also known as the Water Resource Implementation Rule, were not adequately addressed in the Final Technical Document. A proposed rule challenge is not the proper forum to determine whether a proposed rule is consistent with the Water Resource Implementation Rule. Such a determination is within the exclusive jurisdiction of the Department of Environmental Protection under section 373.114(2), Florida Statutes. Consistency of the District's Proposed Rule with the Water Resource Implementation Rule of the Department of Environmental Protection is not a basis in this proceeding for a finding that the Proposed Rule is an invalid exercise of delegated legislative authority. Other Issues The Petitioners and Intervenors raised other issues during the hearing, although not specifically argued in their proposed final order. Since those issues were identified as disputed issues in the Joint Pre-hearing Stipulation, they are addressed below. 1. Elimination of Single-day Exceedance Criterion During the rulemaking process, Sanibel and SCCF sent the District a letter requesting justification for eliminating the single-day exceedance salinity criterion in the current rule. The District staff evaluated the available Caloosahatchee River MFL compliance record, dating back to when the MFL was adopted in September 2001. The District maintains a historical record of MFL monitoring data and reviewed it to determine if the single-day exceedance salinity criterion was exceeded before the 30-day moving average criterion. The compliance record showed five exceedance events of the single-day salinity criterion have occurred. However, the compliance record also showed that the 30- day moving average salinity criterion had already been exceeded before the five events occurred. In other words, the single-day criterion was never exceeded before the 30-day moving average criterion. Based on this evaluation, the District eliminated the single-day exceedance salinity criterion because it did not provide any additional resource protection. The District's decision was not arbitrary or capricious. 2. Not Using the Latest Model Evaluation of recommended MFL criteria and a recovery strategy for the CRE were greatly aided by integration of a suite of hydrologic and ecological models simulating (1) long-term fresh water inflow associated with varying management options, (2) the resulting salinity in the estuary, and (3) ecological response of indicator species that are sensitive to low fresh water inflows. Five models were specifically utilized, including three models for simulations of fresh water inflows to the CRE, a three-dimensional hydrodynamic salinity model, and a Vallisneria model. The three models simulating fresh water inflows included (1) the South Florida Water Management Model (SFWMM) to simulate fresh water discharges at S-79, which includes regional operations of Lake Okeechobee and incorporates Caloosahatchee River irrigation demands; (2) the C-43 Reservoir Model, which uses the SFWMM-simulated daily S-79 flow as input and simulates the management benefit of the C-43 Reservoir; and (3) the Watershed (WaSh) Model to simulate tidal tributary inflow from the Tidal Caloosahatchee Basin sub-watershed. The Caloosahatchee Hydrodynamic/Salinity Model was based on the Curvilinear Hydrodynamic Three-dimensional Model (CH3D) modeling framework with the functionality of simulating the spatial salinity structure across the entire estuary. The Vallisneria Model took the CH3D modeled salinity as input to simulate Vallisneria growth at critical locations in the estuary. The District did review the more recent Environmental Fluid Dynamic Code (EFDC) model developed for the Caloosahatchee Total Maximum Daily Load (TMDL) and being used by the Department of Environmental Protection. The District's expert witness, Dr. Detong Sun, testified that until 2014, the hydrodynamic part of the EFDC model was not working well. He testified that in 2016, the District still had concerns and suggested the use of the District's continuous monitoring data from seven locations across the CRE rather than grab samples for model calibration. Dr. Sun's opinion was that the EFDC model has improved in recent years, but was still behind the CH3D model in terms of performance. The District's expert witness, Dr. Amanda Kahn, testified that the water quality component of the EFDC model was not appropriate for this re-evaluation because the MFL is about water quantity, not water quality. The water quality component of the EFDC model addresses nutrient loadings, not minimum flows. Dr. Kahn also testified that in setting MFL criteria for the CRE, salinity was not a water quality component. Salinity was used as a water quantity component because it does not change with biological processes and can be a measure of how much fresh water is coming into the system. Based on a preponderance of the evidence, the District's decision not to use the EFDC model was not arbitrary or capricious. 3. Seasonality The Petitioners and Intervenors argued that the District is required to set an MFL that varies by season. For the CRE, the District set MFL criteria that protect the system from low flow that would occur in either the wet or dry season. As previously found, the re-evaluation studies focused on the dry season for two reasons: first, because it is well-established that the upstream migration of salt combined with reduced fresh water inflow alters the health and productivity of estuarine habitats; and second, because the dry seasons are the times when the current MFL criteria are likely to be exceeded or violated. The MFL statute states that "when appropriate, [MFLs] may be calculated to reflect seasonal variations." § 373.042(1)(b), Fla. Stat. The preponderance of the evidence showed that for the CRE, it was not necessary to set an MFL that varied by season. Improper Purpose The Petitioners, Sanibel, Cape Coral, and the Town, did not participate in this proceeding primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of litigation. The Petitioners did not participate in this proceeding for an improper purpose. The Intervenors, Fort Myers, Estero, Bonita Springs, and CCP, did not participate in this proceeding primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of litigation. The Intervenors did not participate in this proceeding for an improper purpose.
The Issue The central issue in this case is whether the application for a surface water management permit (permit no. 4-009-0077AM) filed by the Respondent, David A. Smith (Applicant), should be approved.
Findings Of Fact Based upon the prehearing stipulations of the parties, the testimony of the witnesses, and the documentary evidence received at the hearing, the following findings of fact are made: The Applicant is the owner of the subject property. The Applicant filed an application for a permit to construct a stormwater management system which was proposed to serve a residential and golf course development to be known as Sabal Hammocks. The site of the proposed project is approximately 720 acres in size and is located in township 24 south, sections 28, 29, 30, 32, 33, and 34, range 35 east, Brevard County, Florida. The entire project site for the Sabal Hammocks development is located within the boundaries of the St. Johns River Water Management District. To the west of the project site is an 140 acre public park that treats its own stormwater and releases pre-treated stormwater during some storm events into the canals on the Sabal Hammocks site. The Applicant's site is located adjacent to Lake Poinsett and prior uses of the land have included cattle grazing and the cultivation of rye and oats. The Applicant filed his application for the stormwater management permit (permit NO. 4-009-0077AM) on December 22, 1989. That application was deemed complete by the District on June 19, 1990. The District issued a notice of its intended action to approve the permit application on June 28, 1990. Save timely filed a petition challenging the proposed action. By law the District is the appropriate agency charged with the responsibility of reviewing applications for stormwater management permits within the subject area. Save is an association of individual persons and representatives from groups who utilize the waters of Lake Poinsett and its surrounding areas for recreational and business purposes. The receiving waters for stormwater discharge from the proposed Sabal Hammocks development will be Lake Poinsett. That water body is classified as Class III waters. Currently, a dike system exists along the southern boundary of the subject property. That dike system separates the internal grazing lands of the parcel from the lower marsh and flooded areas external to the dike. A series of ditches cross the parcel to drain the interior areas. Two agricultural discharge pumps are currently in use at the site. The operation of those pumps has been authorized pursuant to a consent order approved by the District's governing board on December 13, 1990. The dike system on the subject site has been in place since the 1970s. The original construction specifications of the dike are unknown. Sometime in the 1980s, several openings or breaches were cut in the dike system. Those breaches were opened pursuant to permits issued by the District and the Department of Environmental Regulation (DER) . The breaches were cut to a sufficient width and depth to allow boats to navigate through to interior areas of the subject property during those times when the water levels outside the dike would allow such entrance. The breaches were not cut to ground level and the original dike remained intact and uncompromised by the breaches. That is, the dike has not failed to impede water movement and the integrity of the dike was not weakened by the breaches. The original outline, dimension of the dike, remained visible despite the breaches. In 1986, the Applicant requested permission from the District staff in order to close or restore the dike breaches. At that time, the District staff advised David Smith that a permit would not be required to restore the dike since such improvements would be considered a maintenance exemption. Subsequently, and in reliance upon the representations made by the District's director,, the Applicant closed the breaches and restored the continuity of the dike system of the subject property. The Applicant's work to close the breaches was performed in an open manner, would have been visible to persons using the adjacent marsh or water areas for recreational purposes, and was completed at least one year prior to the application being filed in this case. Neither the District nor DER has asserted that the work to complete the original dike in the 1970s, nor the breaches completed in the 1980s, nor the restoration of the breaches in 1986 was performed in violation of law. Further, the District had knowledge of the subject activities. Save contends that the restoration of the dike system was contrary to law and that it was not afforded a point of entry to contest the closure of the breaches. Additionally, Save infers that the original construction of the dike system in the early 1970s was without authorization from authorities. Save's contention is that the prior condition of the property, ie. the parcel with breached openings, must be considered the correct pre- development condition of the land. The District, however, considered the pre- development condition of the parcel to be that of a diked impoundment separated from Lake Poinsett. The same assumption was made regarding the pumping of water from the area enclosed by the dike via an existing 36 inch pump which discharges to Bass Lake (and then to Lake Poinsett) and an existing 12 inch pump that discharges into the marsh areas adjacent to the property (between it and Lake Poinsett). The District's consideration of the site and the application at issue was based upon the actual condition of the land as it existed at the time this application was filed. The pre-development peak rate and volume of discharge from the site was calculated based upon the maximum discharge capacity of the two existing pumps (described above). Accordingly, the maximum pre-development rate of discharge from the two existing pumps is in the range of 90-107 cubic feet per second. The pre-development volume of discharge, based upon actual pump records, was calculated as 710 acre-feet for a 25 year, 96 hour storm event. The total areas encompassed by the Applicant's proposal are the 720 acre site where the golf course and residential homes will be located together with 140 acres from an adjacent public park. The runoff entering the stormwater system from that public park will have already been treated in its own stormwater management system. The Applicant's proposed stormwater system will consist of a series of lakes and interconnected swales. This wet detention system will capture the runoff and direct its flow through the series of swales and lakes via culverts. The waters will move laterally from the northwestern portion of the parcel to she southeastern end of the site. From the final collecting pond, she waters will be pumped to Bass Lake and ultimately flow to Lake Poinsett. Wet detention systems generally provide greater pollutant treatment efficiencies than other types of stormwater treatment systems. The maintenance associated with these systems is also considered less intensive than other types of treatment systems. The wet detention system proposed for Sabal Hammocks accomplishes three objectives related to the flow of stormwater. The first objective, the collection of the. stormwater, requires the creation of several lakes or pools into which water is directed and accumulates. The size and dimension of the lakes will allow the volume of accumulated water to be sufficient to allow stormwater treatment. The capacity of the lakes will also provide for a sufficient volume to give adequate flood protection during rainfall events and storms. The second objective, the treatment of the stormwater, requires the creation of a littoral zone within the system. The littoral zone, an area of rooted aquatic plants within the lakes or ponds, provide for the natural removal of nutrients flowing into the system. The plants serve as a filtering system whereby some nutrients are processed. The proposed littoral zone in this project constitutes approximately 37 percent of the detention system surface area and therefore exceeds District size requirements. The depth of the treatment volume for the proposed system will not exceed 18 inches. A third objective accomplished by the creation of the series of lakes is the provision for an area where pollutants flowing into the detention system may settle and through sedimentation be removed from the water moving through the system. The average residence time estimated for runoff entering the Sabal Hammocks detention system is 48 days. The permanent pool volume will, therefore, be sufficient to assure the proposed project exceeds the District's requirements related to residence time. The design and volume of the Sabal Hammocks system will also exceed the District's requirements related to the dynamic pool volumes. In this case the Sabal Hammocks system will provide for approximately 65 acre-feet of runoff. Thus, the proposed system will adequately control and detain the first 1 inch of runoff from the site. The length to width ratio for the proposed lakes, 18:1, exceeds the District's minimum criteria (2:1). The final lake or pond into which the stormwater will flow will be 17 acres and will have 15 acres of planted wetland vegetation. Before waters will be released into Bass Lake, the site's runoff will pass through 3100 linear feet of this final lake before being discharged. The proposed project will eliminate the two agricultural pumps and replace them with one pump station. That station will contain four pumps with a total pumping capacity of 96 cubic feet per second. Under anticipated peak times, the rate of discharge from the proposed single station is estimated to be less than the calculated peak pre-development rate of discharge (90-107 c.f.s.). The estimated peak volume of discharge will also be lower than the pre-development discharge volumes for the comparable storm events. The proposed pump station is designed to be operated on electrical power but will have a backup diesel generator to serve in the event of the interruption of electrical service. Additionally, the pumps within the station will be controlled by a switching device that will activate the pump(s) only at designated times. It is unlikely that all four pumps will activate during normal rainfall events. The Applicant intends to relinquish maintenance responsibilities for the stormwater system including the pump station to Brevard County, Florida. Finished floor elevations for all residential structures to be built within the Sabal Hammocks development will be at a minimum of 18.2 mean sea level. This level is above that for a 100 year flood. The floor elevations will be at least one foot above the 100 year flood elevation even in the event of the dike or pump failure or both. Finished road elevations for the project will be set at 17.5 feet mean sea level. This elevation meets or exceeds the County's requirements regarding the construction of roadways. It is estimated that the Sabal Hammocks system will retain at least 26 percent of all storm events on site. If the lake system is utilized to irrigate the golf course the proposed system could retain 45 percent of all storm events on site. Of the 31.27 acres of wetlands within the proposed site, only 4.73 acres of wetlands will be disturbed by the construction of this project. Some of the wetlands are isolated and presently provide minimal benefits to off-site aquatic and wetland dependent species. No threatened or endangered species are currently utilizing the isolated wetlands. The areas of wetlands which are productive and which will be disturbed by the development will be replaced by new wetlands to be created adjacent to their current location at a lower elevation. The new wetlands should provide improved wetland function since those areas will be planted with a greater diversity of wetland plant species. Additionally, other wetland areas will be enhanced by the removal of invader species and increased hydroperiod in the area. The integrated pesticide management plan for the proposed project will be sufficient with the additional condition chat use of Orthene, Subdue, and Tersan LSR will be authorized when approved insecticides or fungicides have not been effective. In this case, the estimates regarding the water quality for the proposed project were based upon data from studies of multifamily residential projects. Data from single family/ golf course developments was not available. Therefore, based upon the data used, the projected runoff concentrations for this project should over estimate pollutants and are more challenging to the treatment system than what is reasonably expected to occur. In this regard, the overall treatment efficiencies are estimated to be good for all of the parameters of concern with the exception of nitrogen. The projected increase in nitrogen, however, will not adversely impact the receiving water body. The projected average concentration for each constituent which may be discharged is less than the state standard with the exceptions of cadmium and zinc. In this regard, the District's proposed conditions (set forth in the District's exhibits 4 and 9) adequately offset the potential for a violation of state water quality standards. More specifically, the use of copper-based algaecides in the stormwater management system should be prohibited; the use of galvanized metal culverts in the stormwater management system, or as driveway culverts, should be prohibited; and the use of organic fertilizers or soil amendments derived from municipal sludge on the golf course should be prohibited. Additionally, a water quality monitoring plan should be implemented by the Applicant. The monitoring plan mandates the collection of water samples from areas in order to adequately monitor the overall effectiveness of the treatment facility. The source of cadmium is not be expected to be as great as projected since the most common source for such discharge is automobiles. It is unlikely that the golf course use will generate the volume of discharge associated with automobile use that the multifamily data presumed. The projected quality of the discharges from this project should be similar to the ambient water quality in Lake Poinsett. In fact, the post- development pollutant loading rates should be better than the pre-development pollutant loading rates. The discharge from the proposed Sabal Hammocks project will not cause or contribute to a violation of state water quality standards in Lake Poinsett nor will the groundwater discharges violate applicable state groundwater quality standards. The floodways and floodplains, and the levels of flood flows or velocities of adjacent water courses will not be altered by the proposed project so as to adversely impact the off- site storage and conveyance capabilities of the water resource. The proposed project will not result in the flow of adjacent water courses to be decreased to cause adverse impacts. The proposed project will not cause hydrologically-related environmental functions to be adversely impacted The proposed project will not endanger life, health, or property. The proposed project will not adversely affect natural resources, fish and wildlife. The proposed project is consistent with the overall objectives of the District.
Recommendation Based upon the foregoing, it is RECOMMENDED: That the governing board of the St. Johns River Water Management District enter a final order approving the application for permit number 4-009-0077AM with the conditions outlined within the District's exhibits numbered 4, 8, and 9 and as previously stated in the notice of intent. DONE and ENTERED this 2 day of July, 1991, in Tallahassee, Leon County, Florida. Joyous D. Parrish Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32301 (904)488-9675 Filed with the Clerk of the Division of Administrative Hearings this 2 day of July, 1991. APPENDIX TO CASE NO. 90-5247 RULINGS ON THE PROPOSED FINDINGS OF FACT SUBMITTED BY THE APPLICANT: Paragraphs 1 through 3 are accepted. Paragraph 4 is rejected as irrelevant. Paragraphs 5 and 6 are accepted. The first sentence of paragraph 7 is accepted the remainder is rejected as irrelevant. Paragraph 8 is accepted. Paragraphs 9 through 11 are accepted. Paragraph 12 is rejected as irrelevant. 8 Paragraphs 13 through 21 are accepted. Paragraph 22 is rejected as irrelevant. Paragraphs 23 through 25 are accepted. The last two sentences of paragraph 26 are accepted, the remainder is rejected as irrelevant. Paragraph 27 is accepted. Paragraph 28 is rejected as comment, irrelevant, or unnecessary to the resolution of the issues of this case. Paragraph 29 is accepted. Paragraph 30 is rejected as irrelevant. Paragraph 31 is rejected as argumentative. Paragraphs 32 and 33 are accepted. With regard to paragraph 34 it is accepted that compensating storage was not required. Otherwise, unnecessary, irrelevant, or comment. With regard to paragraph 35, it is accepted the proposed system meets the first 1 inch of runoff requirement otherwise, unnecessary or irrelevant or comment. Paragraph 36 is accepted. Paragraphs 37 through 41 are rejected as irrelevant, argumentative or comment. Paragraphs 42 and 43 are accepted. With the deletion of the last sentence which is irrelevant, paragraph 44 is accepted. Paragraphs 44 through 49 are accepted. The second sentence of paragraph 50 is accepted, the remainder of the paragraph is rejected as irrelevant or contrary to the weight of the evidence. The first sentence of paragraph 51 is accepted, the remainder is rejected as irrelevant or contrary to the weight of the evidence. Paragraphs 52 through 56 are rejected as irrelevant, comment, or recitation of testimony. Paragraph 57 is accepted. Paragraph 58 is accepted. Paragraphs 59 and 60 are rejected as irrelevant, comment, or argumentative. Paragraphs 61 and 62 are accepted. The first sentence of Paragraph 63 is accepted. The remainder of the Paragraph is rejected as contrary to the weight of the evidence. The proposed project will benefit the wetland areas in an unquanitifiable measure due to the enhancements to prior wetlands and the creation of new wetlands. The first sentence of paragraph 64 is accepted. The remainder is rejected as contrary to the weight of the evidence. Paragraph 65 is accepted. Paragraph 66 is rejected as argument or irrelevant. Paragraph 67 is accepted. Paragraphs 68 and 69 are accepted. Paragraph 70 is rejected as irrelevant or contrary to the weight of the evidence. Paragraphs 71 through 73 are accepted. Paragraph 74 is rejected as irrelevant or unnecessary. Paragraphs 75 through 78 are rejected as argument, irrelevant, or unnecessary to the resolution of the issues of this case. Paragraphs 79 through 82 are accepted. Paragraph 83 is rejected as irrelevant. Paragraphs 84 and 85 are rejected as argument or comment. It is accepted that the Corp and DER are aware of the restoration of the dike and that neither has asserted such work was performed contrary to law. Paragraph 86 is rejected as comment on the evidence or irrelevant. It is accepted that the District advised Applicant that he could restore the dike system and that the District was apprised of the completion of that work. With regard to paragraph 87, it is accepted that the restoration of the dike entailed filling the breaches to conform to the dike's original design; otherwise, rejected as irrelevant. Paragraphs 88 and 89 and the first sentence of Paragraph 90 are accepted. The remainder of paragraph 90 and Paragraphs 91 through 93 are rejected as irrelevant, argument, or comment. Paragraph 94 is accepted. RULINGS ON THE PROPOSED FINDINGS OF FACT SUBMITTED BY THE DISTRICT: Paragraphs 1 through 78 is accepted. Paragraph 79 is rejected as argumentative. Paragraph 80 is accepted. RULINGS ON THE PROPOSED FINDINGS OF FACT SUBMITTED BY SAVE: None submitted. COPIES FURNISHED: Mary D. Hansen 1600 S. Clyde Morris Boulevard Suite 300 Daytona Beach, Florida 32119 Brain D.E. Canter HABEN, CULPEPPER, DUNBAR & FRENCH, P.A. 306 North Monroe Street Tallahassee, Florida 32301 Wayne Flowers Jennifer Burdick St. Johns River Water Management District Post Office Box 1429 Palatka, Florida 32178
The Issue The issue for consideration at the hearing was whether the Respondent, Roger Harloff, should be issued a consumptive use permit to withdraw and use ground water from the wells on his property, and if so, in what amount and under what conditions.
Findings Of Fact Respondent, Roger Harloff, owns several farms in southeastern Manatee County, Florida which, taken together, make up an irregular 8,500 acre tract located approximately 2 1/2 miles north of the City of Sarasota's Verna Wellfield. Mr. Harloff grows vegetables on much of this tract, of which approximately 1,500 acres is devoted to tomatoes. This tomato crop is the prime crop produced by Mr. Harloff, and provides the raw material for the Harloff packing plant which is dependent upon the tomato crop in order to stay in business. Mr. Harloff also operates a plant nursery at which he produces many if not most of the seedling plants utilized in his vegetable growing operations. In order to be economically feasible and remain operative, Mr. Harloff must farm approximately 3,800 acres during the Spring growing season and approximately 3,000 acres during the Fall. These acres are made up of tomatoes and other vegetables. The packing plant and the plant nursery are dependent upon the farm operation and without adequate water, the farm operation cannot be successfully carried on. In September 1988, Mr. Harloff applied to the District for a consumptive use permit to withdraw water from twelve wells located on his property, requesting an annual average rate of 12,995,606 gpd, and a maximum daily rate of 47,520,000 gpd. The consumptive use permit application filed by Mr. Harloff was assigned District Number 204467.04. After evaluation of the application in conjunction with its needs and policies, the District issued a staff report and proposed agency action on the application which recommended issuance of the permit authorizing water to be drawn from the 12 wells at a rate approximating that requested in the application. Thereafter, the City of Sarasota, which operates the nearby Verna Wellfield, considering that the proposed withdrawal would have a substantial adverse impact on its wellfield operations, filed a Petition for Formal Administrative Hearing objecting to the issuance of the permit to Mr. Harloff. Though Mr. Harloff has owned much of the property which make up the 8,500 acre tract in question here, at the time of his application, he did not own, but had under contract, a substantial portion. He closed on the purchase of that remainder after he received notice of the District's intention to issue the permit in question but prior to the City's filing its Petition For Formal Hearing. The purchase price of the property in question was $9,000,000.00 which carries an interest payment on the financed portion of $52,000.00 per month. The wells pertinent to the issues in this proceeding are as follows: # Cons. Depth Cas. Lin. Diam. Cap. Loc. 1 1978 1185' 200' 220-490' 12" 2000 gpm SE 2. 1988 1320' 210' 210-480' 16" 3000 gpm SE 9. 1974 1130' 390' 16" 3000 gpm C 10. 1976 1232' 231' 283-400' 16" 3000 gpm NW 11. 1979 1120' 210' 260-480' 12" 2000 gpm NW 12. 1976 1180' 480' 12" 2000 gpm SW 3. 1989 1434' 460' 16" 3000 gpm SE 5. 1989 1374' 610' 16" 3000 gpm W 8. 1989 1292' 548' 16" 3000 gpm NW 13. 1989 1310' 635' 16" 2000 gpm NE Well No. 8 was used as the pump test well for the constant rate discharge test and Well No. 13 was the deep observation well for that test. Wells 1, 2, 9, 10, 11, and 12 have all been previously permitted by the District and No's 1, 2, 9 and 10 are currently permitted under two other permits, while 11 and 12 were permitted under a different permit. Wells No. 3, 5, 8 and 13 have been authorized for construction but not, as yet, to produce water. Wells 4, 6 and 7 have not yet been constructed. The intention is to drill them to a depth of 1,300 feet and case them to 600 feet. Each will have a pump capacity of 3,000 gpm. Number 4 will be in the southeast portion of the tract, number 6 in the central portion, and number 7 will be located just north of number 6. Wells 1, 2, 9, and 10 currently have a combined permitted maximum daily rate of 13,680,000 gallons under permits number 204467.03 for 1 and 2, and 204630 for 9 and 10. The former was issued on December 29, 1987 and will expire on December 29, 1993, and the latter, issued on October 7, 1981, will expire on that same day in 1991. The permit previously issued for wells 11 and 12 authorized withdrawal at a maximum daily rate of 2,160,000 gallons. That permit, number 204374, expired on September 9, 1986 and was not renewed. After the City filed its Petition challenging Mr. Harloff's proposed permit, Mr. Harloff, on June 26, 1989, filed an amended application to withdraw water at an average annual rate of 10.99 mgd and a maximum daily rate of 48.96 million gallons. This amended application refers to an additional proposed well, Number 13. The District, however, had previously approved wells 3 - 8 and 13, and pursuant to this authorization, wells 3, 5, 8, and 13 were built. Mr. Harloff submitted additional amendments to his application on August 7 and 9, 1989. The former requests a seasonal average daily rate of 25.34 mgd and a seasonal maximum daily rate of 32.79 mgd. The latter requests a seasonal average rate of 26.18 mgd, an annual average rate of 15.18 mgd, and a seasonal maximum rate of 31.56 mgd. In that regard, a seasonal rate is the same as an annual rate, (average or maximum) when applied to a growing season as opposed to a year. The additional amendments to the application were evaluated by District staff who, on August 18, 1989, issued a revised staff report and a proposal to issue to Mr. Harloff a consumptive use permit authorizing an average annual withdrawal of 11.1. mgd, an average seasonal withdrawal of 15.6 mgd, and a seasonal maximum withdrawal of 20.1 mgd. The proposed permit also contains terms and conditions which, the District contends, will, inter alia, permit Mr. Harloff to withdraw more water than he is currently authorized without additional adverse impact on the City's Verna Wellfield. It is to some of these terms and conditions that Mr. Harloff objects. Since the issuance of the revised staff report and intent to issue, the parties have negotiated on the various terms and conditions in question and have agreed to some and the amendment of others. Mr. Harloff has no objection to conditions number 1, 2, 3, 7 - 14, 23, 24, 26, 28 - 30, 32, and 34 & 35. The parties agree that other conditions, as indicated herein, should be amended as follows: Condition 19, on the third line, should be changed to read, " up to 20 inches tapering to 12 inches." Condition 22, on the second line, should be changed from "30 days" to "10 days". Condition 25, on the first line, should be changed from "within 60 days" to within 120 days". Condition 31, on the third line, starting with "following month" should be changed to "following months: January, April, July and October". Also, under Sampling Frequency, "Monthly" should be changed to "Quarterly". Condition 33, on the ninth line, insert the work "economically" before the word "feasible" in the phrase "specific operation and irrigation improvements are feasible". Mr. Harloff objects to conditions 4, 5, 15 - 17, 20 & 27. He does not object to the proposed new standards for new wells. Taken together, the parties then disagree only on the requirement for abandonment or refurbishment of existing wells and the quantities of water Mr. Harloff will be allowed to draw. The City supports the District's position on both issues. The City of Sarasota owns and operates a public water system to serve between 50 to 75 thousand people located in Sarasota County. The primary source of water for this system is the Verna Well field which is also owned by the City and which accounts for approximately 60 percent of the City's water needs. The City also operates a reverse osmosis, (R.O.) water desalinization facility, and has back-up wells at St. Armond Key and at the Bobby Jones Wellfield. The Verna Wellfield is located about 17 miles east of the Sarasota city limits on approximately 2,000 acres of land in northeastern Sarasota County. It consists of two tracts of land: Part "A", which is approximately 1/2 mile wide by 4 miles long; and Part "B", which is approximately 1 mile square located about 500 feet southeast of Part "A". The Verna Wellfield's permitted allocation is based on whether the R.O. facility is producing at capacity. If it is, the Verna daily allocation is 7 mgd, and if not, 9.5 mgd. The R.O. facility's capacity is 4.5 mgd and the backup wells have a capacity of 1.7 mgd. The wellfield contains 39 permitted production wells, 30 of which are in Part "A" and 9 of which are in Part "B." One of them, well 30, is currently inactive. The wellfield has been in operation as a part of the City's public water system since September 1966. When the Verna Wellfield was constructed in 1965-1966, its original design specified casing on most wells down to 140 feet with pump bowl settings at 125 feet. Each pump was to have a total dynamic head, (TDH) of 200 feet. Over the years, the City has decreased the TDH of the pumps at Verna from 200 feet to 175 feet. This has resulted in a reduction of the pumps' ability to produce water with sufficient pressure to carry it to the discharge point. This decline has been caused by an increase in withdrawal of water regionally, and not solely because of withdrawals from the Verna Well field. Verna is impacted by the use of water outside the boundaries of the wellfield. The City has an ongoing program calling for the refurbishment of 2 to 3 wells per year at the Verna Wellfield. It is the City's intent to convert the pumps to 200 feet TDH on all well refurbishments in the future. In August 1977, a program requiring permits for the consumptive use of water was implemented in both Sarasota and Manatee Counties. At that time, the Verna Wellfield had a production rate of 6.9 mgd annual average daily rate. On January 6, 1978, the City applied for a permit for Verna and on April 3, 1979, the District issued permit number 27804318 to allow the City to draw water from the Verna Wellfield. The City applied for a renewal of that permit in October 1983 and thereafter, in January 1985, the District authorized the continued withdrawal of water from Verna by the issuance of permit 204318 which, at Condition 18, placed limitations on the City's use of water from the wellfield. Specifically, the permit limited withdrawals from Verna to: ...6,000,000 gallons per day average and 7,000,000 gallons per day maximum, except during those times when ... [the R.O. process is reduced or to facilitate maintenance or repairs]. At such times, ... [withdrawals) may be increased to provide additional supplies not to exceed 8,000,000 gallons per day average annual and 9,500,000 gallons per day maximum. This condition clearly provides for additional supplies to be drawn to increase the Verna Well field production to a total of 8,000,000 and 9,500,000 mgd, respectively, not in addition to the regular permitted amount, by those quantities. The City's permit has been neither suspended nor revoked nor is any violation enforcement action currently under way. The current permit expires January 9, 1991. The water pumped from the Verna wells is held in a 1,000,000 gallon reservoir at the wellfield. This reservoir, which is topped at approximately 22 to 23 feet, electronically controls the pumping activity at the well field by turning on and shutting off pumps, in series, as the water level in the reservoir rises and falls. The water, when needed, is transmitted to another reservoir near the City's treatment plant in downtown Sarasota by gravity flow through a 30" diameter, 92,000 foot long pipe. The flow rate is approximately 5,000 gpm normally. When the treatment plant needs more water, a pump at the well field forces the flow at a rate of between 7,200 to 8,200 gpm, depending upon the level of water in the receiving reservoir. A flow of 8,200 gpm would draw 11.8 mgd from the wellfield. The operating capacity of the Verna Wellfield, in August 1988, was 17.9 mgd. Harloff's experts assert, and there is no concrete evidence to rebut it, that if all wells at Verna were pumping during a 24 hour period in May 1989, the reservoir could have been maintained at full level. However, though there is a manual override of the automatic reservoir/pump control system, it is unrealistic and unwise to expect full production on a 24 hour basis for any lengthy time period. Water under both Mr. Harloff's property and the Verna Well field is found at various levels known by different names. These include, in order of descent, the Surficial Aquifer, the Intermediate Aquifer, the Upper Floridan Aquifer, and the Lower Floridan Aquifer. The Surficial Aquifer extends from the surface down to between 20 and 60 feet below the surface. A 20 foot thick bed of clay separates the water in this aquifer from that in the aquifer immediately below it, the Intermediate Aquifer, which extends from approximately 80 feet down to approximately 420 feet below the surface. In the lower part of the Intermediate Aquifer, permeability decreases until a confining unit separating the bottom of the Intermediate Aquifer from the top of the Upper Floridan Aquifer is formed. There is such a confining unit between 420 and 500 feet. There is no well-defined confining unit between the Upper and Lower Floridan Aquifers. There is, however, a substantial difference in the transmissivity in each zone. "Transmissivity" is defined as the amount of water that will exist through a section of the aquifer that is the same width from the top to the bottom. The lower the transmissivity rate, the deeper the cone and the narrower the radius of effect. The higher the rate, the shallower the cone and the broader the radius. The Lower Floridan Aquifer has an extremely high transmissivity. Its top is found at a range of from 1,050 to 1,200 feet below the surface on Mr. Harloff's property. The water from the Upper Floridan Aquifer is of higher quality than that in the Lower. It is more readily usable for drinking than that in the Lower, but the Lower water is quite acceptable for agricultural purposes. What confining layer exists between the Upper and Lower Floridan Aquifers is made up of relatively impermeable anhydrides and gypsum. Because of this, there is little likelihood of the highly mineralized water from the Lower Floridan Aquifer rising into the better quality water in the Upper. If, therefore, water for agricultural purposes is drawn from the Lower Floridan Aquifer, with its high transmissivity and narrower cone radius, and if the wells utilized to procure this water are cased down to within the Lower aquifer, there is little chance of a negative impact on the better quality water, used for drinking by the City, within the Upper Floridan and Intermediate Aquifers. Mr. Hardin, an expert geologist and hydrogeologist testifying for Mr. Harloff, concluded, utilizing certain commonly accepted computer models, that Mr. Harloff's requested additional withdrawals would not have a significant effect on the Verna Wellfield's ability to produce water sufficient for the City's needs. This conclusion was based on 1989 seasonal use figures including an average rate of 21.95 mgd, a maximum rate of 27.04 mgd, and a maximum rate of 29 mgd under a "run time" calculation and the fact that during that period, the City was able to pump at least its permitted quantity from its wells at Verna. The City and the District do not accept this conclusion as reasonable, however, because, they claim, the withdrawal figures cited are not meter readouts but estimates based on the number of acres farmed and the number of pump operating hours during the period in question. The City's experts contend the data used by Hardin and Prochaska in their opinions is not that which other experts in the field would reasonably rely upon. They do not appear to be unrealistic, however, and, therefore, Mr. Hardin's opinion is accepted as but one factor to be considered. On the other hand, Mr. Anderson, also a Harloff expert hydrogeologist, claims the requested withdrawals would result in only an additional 1.7 foot drawdown in the Upper Floridan Aquifer underlying the Northeast corner of the Verna Well field. To be sure, this is only one small portion of the wellfield in issue. There has, however, been a continuing history of declining groundwater levels in this area over the past several years. After the 1975 drought, the City started to experience declining water levels at Verna which, because of the reduction in ability to produce water, required a lowering of the pump elements in some wells, and also caused the City to develop an R.O. facility in an effort to reduce dependence on well water. This drop in capability occurred again during the 1985 drought and this time the City modified the pump motors to shut off prior to cavitation and initiated a schedule of operating times for wells, so that water is drawn from different and geographically separated areas in a sequence designed to allow periodic regeneration of an area's supply. Nevertheless, water supply remains a concern at Verna, and the problems previously experienced continue to occur during periods of drought. In May 1989, the Verna Wellfield was periodically "unable" to meet it's short term peak demands at times even though all operating wells were pumping. This means that at the times in question, more water was being drawn from the Verna reservoir than could be replaced by pumping activities. It does not mean that the reservoir ran dry and water could not be furnished to the treatment plant. However, this condition is serious and indicative of a more serious shortage in the future unless appropriate safeguards are instituted. Mr. Balleau, the City's expert in hydrology and hydrogeology, and the District's experts all believe the Verna Wellfield is in trouble. It is operating well beyond its design range and the imposition of additional demands on it would seriously and adversely affect its ability to produce water. This position is supported by the facts and found to be accurate. There appear to be several options open to the City to contend with the Verna problem potential. These include: drill deeper wells at Verna to tap the Lower Floridan Aquifer. (This will produce the lower quality water found there and require additional treatment facilities. construct a linear wellfield along the pipeline from Verna to the treatment facility. (This will require additional permitting to draw the water, high construction and operating costs, and still result in low quality water requiring treatment. redevelop the downtown wells currently supplying the R.O. facility. (This will require satisfaction of regulatory issues, adversely impact on the users of the upper aquifers, possibly result in poor water quality and in contamination from nearby landfills.) develop a new well field southeast of Verna. (This will experience regulatory issues and high construction costs, with an unknown water quality result.) buy water from Manatee County. (This is expensive, may result in transmission and compatibility problems, and would be only a short term solution. lower pump assemblies; replace existing pumps and modify the pump circuits. (These are all unreliable, short term solutions of minimal benefit.) Mr. Harloff and the City/District disagree on the appropriate amount of water needed for the successful growing of the crops produced by his operations. Both agree, however, that the heaviest demands for water come in the spring growing season including April and May. Tomatoes require the most water. Peppers require nearly as much. This is because the short root systems require a higher water table in the soil to supply needed moisture. In its analysis of Mr. Harloff's application, the District, referring to tables developed for the purpose of allocation and relating to Harloff's watering history during the period from August 15, 1988 to June 7, 1989, subtracted the fall season recorded application of 20.7 acre-inches from the total 10 month figure of 50.92 acre-inches and concluded he would need 30.22 acre-inches for peppers during the spring, 1989 season. Unless shown to be totally unreasonable, however, (not the case here), the applicant's water need figures should be accepted. Mr. Harloff's operation constitutes an important part of Manatee County's agricultural economy, and agriculture utilizes 68.9 percent of the land in the county. Agricultural products sold in Manatee County in 1987 were valued at $145,655,000.00, which ranked Manatee County third among all Florida counties in vegetable production. Agriculture is the fourth largest employer in Manatee County, employing an average of 4,692 people per month. Through his farm operation alone, Harloff employes as many as 1,050 people, with 200 employed on a full-time basis. Experts estimate that the loss of the Harloff operation would cause a reduction of between 16 and 18 million dollars in agricultural sales in the county with an additional loss in jobs and income to his suppliers. This estimate is not at all unreasonable. Florida produces approximately 95 percent of all tomatoes grown in this country for the fresh tomato market during the winter growing season. Tomatoes are the single largest vegetable crop grown in the state and accounted for 39.7 percent of the total value of vegetables produced in Florida during the 1987-1988 growing season. Mr. Harloff produced 4.8 percent of the total shipment of tomatoes from this state during that period. Water, primarily through irrigation, is an indispensable portion of the farming operation for this crop. Mr. Harloff currently irrigates the majority of his non-citrus crops by use of a "semi-closed ditch irrigation system", as opposed to a "drip system." The drip system is considerably more efficient than the semi-closed system having an efficiency rating, (amount of water actually used by the plants) of between 80 to 90 percent, as opposed to 40 to 60 percent for the other. While Mr. Harloff could reduce his water needs considerably and achieve substantial savings on pump fuel by conversion to a drip system for all or a part of his crops, such an undertaking would be quite costly. One of the conditions proposed by the District for the approval of Harloff's permit, as amended, is the refurbishment of several of the existing wells utilized by Mr. Harloff to make them more efficient and to promote the withdrawal of water from the Lower Floridan Aquifer, in which there appears to be adequate water and from which the Verna Well field does not draw. Currently, Mr. Harloff has seven wells which do not meet the standards of this proposed condition. They are not drilled to 1,300 feet below mean sea level and are not cased to 600 feet. To bring these wells into compliance, they would have to be drilled to the 1,300 foot level, or to a level which has a specific capacity of 400 gpm, and the casings in each would have to be extended to 600 feet. Extending the casings would be a complicated procedure and Harloff's experts in the area cannot guarantee the procedure would successfully achieve the desired end. Assuming the retrofit was successful, the cost of the entire process would be approximately $15,000.00 to $16,000.00 per well. In addition, the process would, perforce, require reducing the diameter of the well from 10 to 8 inches, thereby necessitating increasing the pump capacity to produce sufficient water. The cost of this is substantial with an appropriate new pump costing somewhere between $10,000.00 and $15,000.00 each. Consequently, the anticipated cost of bringing the existing wells up to condition standards would be between $25,000.00 to $31,000.00 per well, while the cost of constructing a new well is between $40,000.00 and $50,000.00 per well. Mr. Harloff feels it would be more prudent for him to replace the existing wells rather than to retrofit them. This may be correct. Harloff experts also claim that extending the casings on the existing wells down to 600 feet would not provide a significant benefit to the aquifer nor cause any significant reduction in drawdown impact at Verna. The District and City experts disagree and, taken on balance, caution and the interests of the public indicate that a conservative approach is more appropriate. While Mr. Harloff proposes to convert the areas served by wells 1, 9, 11, and 12 to the growing of citrus which requires much less water than tomatoes, this would not be sufficient mitigation to offset the need for some modification if large amounts of water will still be drawn. The entire area under the District's jurisdiction has been experiencing a water shortage due to a lack of rainfall. As a result, in June 1989, the District adopted a resolution identifying an area, including the area in question here, as a "water use caution area." This was done because the Floridan Aquifer has been subjected to large seasonable drawdowns of the potientiometric surface, the level to which water in a confined aquifer can rise in a well which penetrates that acquifer. This drawdown is directly related to increased water use in the area, much of which is for agricultural purposes. As a result of the District's action, special conditions on well construction for consumptive use applicants have been imposed on a permit by permit basis to insure, as much as possible, that the applicant uses the lowest quality water appropriate for his intended purpose. These conditions are not unreasonable. While accepting the District's and City's conclusion that his wells, if permitted, would have some impact on the Verna Wellfield, Mr. Harloff does not concede that the impact is significant. Specifically, the difference in impact resulting from an increase from his currently permitted use of 13.68 mgd seasonal maximum and his requested use of 31.56 mgd seasonal maximum for wells 1, 2, 9, and 10 would be a maximum increased drawdown of 1.1 feet at the Intermediate aquifer and 1.8 feet at the Upper Floridan Aquifer. Both figures relate to that portion of the wellfield found in the northeast corner of Part A. If the anticipated usage for crops predicted by Mr. Harloff's experts for the spring of 1989 is accurate, the drawdown would be 0.2 feet for the intermediate aquifer and 0.4 feet for the Upper Floridan Aquifer measured at the northeast corner of Part B of the Verna We1lfield. Harloff's experts contend that additional impacts for the spring of 1989 included, the increased usage will not have a significant effect on Verna's ability to produce its permitted daily maximum withdrawal of 9.5 mgd. While this is an educated speculation, it should be noted that during May 1989, the Verna field was able to produce up to 8.3 mgd without using all wells during any 24 hour period. This does not consider, however, the problems encountered by the City as indicated by the wellfield personnel, and the fact that some of the City wells are not pumping water.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that Roger Harloff be issued a consumptive use permit, No. 204467.04, as modified, to reflect authorization to draw 15.18 mgd annual average, not to exceed 31.56 mgd seasonal maximum, conditioned upon compliance with the conditions found in the conditions portion of the permit, as modified to conform to the quantities as stated herein, and to include those requirements as to acre-inch and crop-acre limitations, well usage and abandonment schedules, well modification standards, and record keeping, as are contained therein. RECOMMENDED this 5th day of December, 1989, 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 5th day of December, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE No. 89-0574 The following constitutes my specific rulings pursuant to s. 120.59(2), Florida Statutes, on all of the proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONER: City of Sarasota, joined by the District 1 & 2. Accepted and incorporated herein. 3. Accepted and incorporated herein. 8-12. Accepted and incorporated herein. 13. Accepted and incorporated herein. 14-22. Accepted and incorporated herein. 23-25. Accepted and incorporated herein. 26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29-33. Accepted and incorporated herein. Not a Finding of Fact but a statement of party position. & 36. Accepted. 37. & 38. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not a Finding of Fact but a comment on opponent's satisfaction of its burden of proof. 42-44. Accepted and incorporated herein. Accepted and incorporated herein. Rejected as a misstatement of fact. Water service was never interrupted. The deficiency was in the City's inability to keep its wellfield reservoir filled. 47-54. Accepted and incorporated herein. Accepted and incorporated herein. Rejected for the reasons outlined in 41. 57-62. Accepted and incorporated herein. 63. Rejected for the reasons outlined in 41. 64-66. Accepted and incorporated herein. Rejected for the reasons outlined in 41. Rejected. & 70. Accepted and incorporated herein. 71. & 72. Accepted and incorporated herein. 73. Accepted and incorporated herein. 74 & 75. Accepted and incorporated herein. Accepted. Not a Finding of Fact but a statement of party position. Rejected. Accepted. Irrelevant. 81-84. Rejected. 85. & 86. Accepted and incorporated herein. 87 & 88. Accepted and incorporated herein. 89. Accepted and incorporated herein. 90 & 91. Accepted and incorporated herein. 92. & 93. Accepted and incorporated herein. FOR THE RESPONDENT: Roger Harloff 1-9. Accepted and incorporated herein. 10-13. Accepted and incorporated herein. 14 & 15. Accepted and incorporated herein. 16-25. Accepted and incorporated herein. 26-28. Accepted and incorporated herein. 29 & 30. Accepted. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not proven. 35 & 36. Accepted and incorporated herein. 37 & 38. Accepted and incorporated herein. 39-41. Accepted and incorporated herein. 42 & 43. Accepted and incorporated herein. 44. Accepted. 45 & 46. Accepted and incorporated herein. 47 & 48. Accepted and incorporated herein. 49. Accepted. 50 & 51. Accepted and incorporated herein. Accepted. Accepted. Accepted. & 56. Accepted and incorporated herein. 57. Accepted. 58-60. Accepted and incorporated herein. 61 & 62. Accepted and incorporated herein. Rejected as unproven. Accepted. Accepted and incorporated herein. Accepted. 67-68. Accepted. Not a Finding of Fact but an interpretation of party po Accepted. Rejected. 72 & 73. Accepted. COPIES FURNISHED: Edward P. de la Parte, Jr., Esquire de la Parte, Gilbert and Gramovot, P.A. 705 East Kennedy- Blvd. Tampa, Florida 33602 Edward B. Helvenston, Esquire SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899 Douglas P. Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Peter G. Hubbell Executive Director SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
