The Issue As reflected in the parties' prehearing stipulation filed on August 28, 1991, the issue in this case is whether the St. Johns River Water Management District (SJRWMD) should approve South Brevard Water Authority's (SBWA) consumptive use permit (CUP) application. The SBWA is seeking permission to withdraw an annual average daily rate of 18.8 million gallons (mgd) and a maximum daily rate of 21.4 mgd. The District proposes to grant the permit with specified conditions. Petitioners challenge the issuance of the permit, alleging that applicable requirements of Chapter 373, F.S. and Chapter 40C-2, F.A.C. and other applicable law are not met. The standing of Petitioners, other than Osceola County, is at issue. Also at issue is whether the relevant criteria include consideration of the adequacy of existing sources of water, and the consideration of costs of utilizing existing sources versus the cost of the proposed new source of water.
Findings Of Fact The Parties The applicant, South Brevard Water Authority (SBWA) was created by special act of the legislature, Chapter 83-375, Laws of Florida. Its principal office is located in Melbourne, Brevard County, Florida. Its general mission is described in Section 1, of Chapter 83-375, Laws of Florida, as amended by Chapter 87-481, Laws of Florida: Section 1. It is hereby declared and determined by the Legislature that a regional water authority is the most responsive, efficient, and effective local government entity to secure, operate, and maintain an adequate, dependable, and safe water supply for the district and customers of the district. It is the intent of the Legislature that such regional water authority possess the full power and authority to implement, finance, and operate a single coordinated program of water supply transmission and distribution to meet the future quantity and quality needs of the district and for customers of the district. There is a paramount public need to develop a safe, reliable, and energy-efficient source of public water for the district residents and to contruct the wellfields, transmission lines, and other facilities necessary to supply such water. The St. Johns River Water Management District (SJRWMD or District) is an agency created pursuant to Chapter 373, F.S. in charge of regulating consumptive uses of water in a 19-county area of the State of Florida, including all of Brevard and part of Osceola County. The geographical boundaries of the District are described in Section 373.069(2)(c), F.S. Osceola County is a political subdivision of the state, west of, and contiguous to, south Brevard County. The Corporation of the President of the Church of Jesus Christ of Latter Day Saints (Deseret) is a Utah corporation authorized to conduct business in the State of Florida. Deseret owns real property in Osceola County to the north and east of the proposed wellfield. Deseret possesses a valid consumptive use permit authorizing the withdrawal of water for this property. East Central Florida Services (ECFS) does not own land or possess a consumptive use permit (CUP). Its purpose is to take over the water management program for the Deseret property. It has applied to the Public Service Commission for certification. Notwithstanding the parties' stipulation that "Triple E Corporation" and "Triple N Corporation" own real property in Osceola County near the proposed wellfield (prehearing stipulation, filed 8/28/91, p. 5), no such corporations are registered in the State of Florida. The lands identified as Triple E and Triple N are owned by multiple parties through trusts, primarily managed by Maury L. Carter, one of the owners. Neither Triple E nor Triple N properties have CUP's. The properties are used for agricultural purposes and the Triple N property has a well and recreational camp. The Site of the Proposed Use The proposed wellfield is located on property owned by the SJRWMD, the Bull Creek Wildlife Management Area (BCWMA), located entirely in eastern Osceola County. The BCWMA is comprised of 22,206 acres within the drainage area of the St. Johns River. The northern third of the management area is drained by Crabgrass Creek, and the southern two-thirds is drained by Bull Creek. The easternmost boundary is located approximately one mile from the Brevard County boundary. Currently all 22,206 acres of the BCWMA are under lease to the Florida Game and Fresh Water Fish Commission, which agency manages the area as a public recreation facility for hunting, fishing, hiking, horseback riding, camping and archeological studies. The sparsely populated area has historically been used for logging and cattle grazing. It was acquired for a detention area and it currently provides nonstructural flood protection. Its surface topography is relatively flat, with uplands and wetlands separated by only inches in vertical elevation. Upland communities include pine flatwoods, saw palmetto prairies, pine savannahs and sand oaks. Wetland communities include cypress domes, mixed shallow marshes, sawgrass marsh, wet prairies and transitional prairies. The BCWMA is classified as a "conservation area" in the District's current adopted Five Year Land Plan which summarizes the agency's land acquisition and management policies. A "conservation area" is defined as "...an area acquired for water resource conservation and protection in an environmentally-acceptable manner". The term includes water supply areas, including areas for public wellfield location. (Osceola Co. exhibit #33, p. 15) Facilities Associated with the Proposed Consumptive Use Although the precise siting of the wells has not been established, the wellfield will be located at the northern end of the BCWMA, east-west into a "panhandle" area, and extending south, for an inverted "L" shape. The wellfield will consist of 12 production wells in 2000 ft. intervals. Wells 1-9 will lie along an east-west axis adjacent to Crabgrass Creek, while wells 10-12 will lie along a north-south axis below well 9, the eastern-most well. The capacity of each well is designed at 3,000 gallons per minute or approximately 4.30 million gallons a day (mgd). Each well consists of 20" diameter casing pipe extending 700' below the ground surface. From there, an open hole for production will extend another 250 feet in depth. A small, 20 ft. by 30 ft., concrete building will enclose the motor and other equipment associated with each well, in order to eliminate vandalism and to baffle the noise. The wells will be sited to avoid jurisdictional wetlands. In addition to the production wells, monitoring wells will be constructed to comply with permit conditions. Because the water drawn from the proposed wellfield will exceed potable standards, reverse osmosis (RO) desalinization treatment is required. A below ground header pipeline will carry raw water from the wellfield to an RO treatment facility in Brevard County. The RO treatment facility will process 75 percent of water coming from the wellfield, 85 percent of which is recovered as finished water, and 15 percent of which is disposed of as brine by deep well injection. The 25 percent of raw water which bypasses the treatment process will be blended with the finished water to yield water which meets drinking water standards for chloride levels. The yield is anticipated to be 16.67 mgd on an average day and 18.9 mgd on a maximum day. However, the finished water yield could be higher if raw water quality permits greater blending and less reject water. On the finished water side, the water will need to be treated again to assure that it will be compatible with water from the City of Melbourne plant. Failure to balance the blended waters chemically could result in corrosion of pipes, leaching of pipes, discoloration, rusty water, and odorous water. A proper process, therefore, is essential and is highly sophisticated. From the treatment facility the water will travel in underground pipes, beneath the St. Johns River, beneath I-95 and east to the Melbourne distribution system. From there some water is anticipated to travel south to connect to the General Development Utilities (GDU) system. Hydrogeologic Characteristics of the Site For modelling purposes, the aquifer system in the region is represented by sequential layers of differing characteristics in the flow and movement of water. The SBWA model contains 6 layers; the Osceola model contains 7 layers. In both models, layer 1 corresponds to the surficial (water table) aquifer; layer 2 corresponds to the Hawthorn formation (the upper confirming layer); layer 3 is the Upper Floridan aquifer; layer 4 describes the 200 ft. thick portion of the Upper Floridan called the "production zone"; layer 5 in the SBWA model is approximately 450 ft. thick and is called a confining unit; Osceola's consultants consider this layer less permeable or semi-confirming; layer 6 is the lower Floridan; and layer 7 in the Osceola model is the bottom reaches of the lower Floridan. The surficial aquifer consists of sand and shell deposits and extends to a depth of approximately 100 feet below land surface. The surficial aquifer is capable of producing small to moderate amounts of water for domestic uses. The Hawthorn is an interbedded formation consisting of clay, limestone and phosphate. Due to its extremely low permeability, this layer restricts both the vertical and horizontal movement of water. The Hawthorn is thicker in Central Florida than in other portions of the state. At the BCWMA the thickness of the Hawthorn ranges from 240 feet in the area northwest of the management area to 80 feet in the southeastern portion of the management area. The upper Floridan Aquifer at the BCWMA, as characterized by the SBWA's consultant and based on site specific data, extends from the base of the Hawthorn to a depth of approximately 900 feet below land surface. That portion of the upper Floridan Aquifer between the bottom of the Hawthorn and 700 feet below land surface consists of fine grained limestone with relatively low permeability. This zone corresponds with layer 3 in the groundwater modeling done by the SBWA. The portion of the upper Floridan between the bottom of the Hawthorn and 700 feet below land surface is less capable of producing water than the portions below this level. That portion of the upper Floridan Aquifer between 700 feet and 900 feet of depth consists of hard dolomites. Dolomitic zones are the most productive zones of water within the Floridan in this part of the state because these formations contain solution fractures and cavities. This zone corresponds with layer 4 in the groundwater modeling done by the SBWA. Several researchers and modelers have suggested the existence of a zone, variously referred to as a semi-confining unit, a zone of lower permeability or a middle semi-confining unit, located between the upper and lower Floridan Aquifer. This area between 900 feet and 1350 feet below land surface consists largely of hard dolomites similar in nature to those in the zone immediately above it. This zone corresponds to layer 5 in the groundwater modeling done by SBWA. Previous regional modeling efforts have utilized model derived values to describe the middle semi-confining unit rather than site specific information showing the location, thickness or hydrogeological characteristics of the zone. Site specific data tends to confirm the lower permeability of this zone relative to the layers above and below it. Site specific data consists of a core sample, mineral content observed during the drilling of the test monitor well, and a Neumann-Witherspoon ratio analysis conducted during the aquifer performance test. The area between 1350 feet and 1450 feet below land surface also consists of dolomites but with greater permeability and greater transmissivity (the measure of an aquifer's ability to transmit water in a horizontal direction). This area corresponds to layer 6 in the groundwater modeling done by the SBWA. No site specific data exists beneath 1483 feet, representing the total depth of test well TM. Regional data does exist which characterizes the areas from 1500 feet below land surface to the bottom of the lower Floridan Aquifer as consisting of zones of varying lithology, and varying permeabilities. This zone which corresponds to layer 7 in the groundwater modeling done by Osceola County is not homogeneous or uniform over its entire thickness according to available regional data, consisting of geologic reports of deep wells in the east-central Florida area. All parties agree that in the area of the proposed wellfield, horizontal movement of water in the Floridan aquifer is from west, where the greatest recharge occurs along the Lake Wales Ridge, to east, where there is little or no recharge. Water quality in the upper Floridan as measured by chloride concentrations deteriorates as one moves from west to east. The Floridan aquifer beneath the BCWMA represents a transition zone between the recharge area to the west and high saline formation waters in the east. The dominant geochemical components in water beneath the BCWMA are biocarbonates. Water quality, as measured by chloride concentrations, also deteriorates with depth. Chloride concentrations, based on data derived from the drilling of well TM at the BCWMA, increase gradually from 306 milligrams per liter (mgl) at 410 feet, to 658 mgl at 1473 feet below land surface. Chloride concentrations increase abruptly to 1980 mgl in well TM at 1483 feet of depth. Evidence is inconclusive as to whether all of the proposed production wells will draw water exceeding 250 mgl in chloride concentrations. It is undisputed that most will, but chloride contours initially provided by SBWA's consultant indicate that the southernmost wells may produce water between 150 and 250 mgl. A comprehensive aquifer performance test (APT) was conducted at the BCWMA by the SBWA's consultant, Post, Buckley Schuh, and Jernigan, Inc. (PBSJ). The test was designed by the staff of the SJRWMD in consultation with the U.S. Geological Survey (USGS). This test yielded data which enabled PBSJ to calculate several aquifer characteristics for use in the groundwater modeling which was later done by SBWA's modeling consultant, Environmental Science and Engineering, Inc. (ESE). Eight wells were utilized in connection with the APT conducted at the BCWMA in January and February 1990. Three of the wells were dual zone monitoring wells capable of monitoring events in two different geologic units simultaneously. Three wells, including the test production well (TP) were open to the interval between 700 and 900 feet below land surface which was identified by the SBWA as the production zone. Typically APT's are run for 12 to 72 hours in Florida. Well TP was pumped for approximately 10 days at a rate equivalent to that expected during actual production while observations were made of water levels in all wells, including three off-site wells (the Holopaw test well, the Kempfer well and the Bruner well). All of the information the SBWA needed from the APT was obtained in the first hours of the test. Water levels in the area monitored during the APT ceased dropping due to pumpage within 1 hour after the pumping started. Three different analytical models were used to calculate a transmissivity value for the production zone, utilizing data derived during the APT. The result showed transmissivity in this zone to be approximately 2 million gallons per foot per day. This is a very high transmissivity value indicating a comparatively prolific aquifer, capable of producing the volumes of water requested in the application. As transmissivity increases, the cone of depression associated with pumpage tends to flatten out and be less steep. The cone of depression extends further out, creating a wider area of drawdown. Hydraulic conductivity is the measure of an aquifer's resistance to flow either in a vertical (KV) or horizontal (KH) direction. Two methods were used to calculate the hydraulic conductivity of the Hawthon Formation by PBSJ: laboratory analysis of a core sample taken from this unit, and a bail test (measuring an increase in water level over time) conducted on a well on site by the SJRWMD. Two different methods were used by PBSJ to calculate the hydraulic conductivity of layer 5: laboratory analysis of a core sample taken from that zone, and the Neuman-Witherspoon ratio analysis method. Porosity is the void space in porous media through which transport of particles, such as chlorides, can occur. Effective porosity has an impact on the ability of saline or dense water to move upward from depth toward a pumping well. The lower the effective porosity within an aquifer, the greater the potential for upconing of saline water within that aquifer. Effective porosity for layers 4 and 5 was calculated using two different methods, those being laboratory analysis of core samples taken from these zones, and analysis of acoustic logs generated during the APT. Each of these methods is accepted in the field of hydrogeology. Anticipated Impacts to Groundwater Levels and Flows as a Result of the Proposed Consumptive Use A numeric groundwater flow model is a computer code representing the groundwater flow process. Both SBWA and Osceola used numeric groundwater flow models developed by their consultants to predict and simulate the impacts associated with withdrawals proposed in the application. The SBWA used a finite difference model called INTERSAT for its simulations. INTERSAT is a widely used and accepted groundwater flow model. The model was run by ESE for the SBWA in the impact or drawdown mode. Drawdown or impact models simulate changes in water levels in response to a stress such as a pumping well. Drawdown models are an accepted and frequently used method to evaluate wellfield stress, particularly in association with a CUP application. ESE and PBSJ utilized several analytical models to first determine and later to verify the area to which the boundaries of their model would extend. The radius of influence of a well or wellfield is the distance from the center of pumpage extending out to where drawdowns caused by that pumpage reach zero. The boundary for a numeric groundwater model should be set at, or beyond, the radius of influence of the pumpage being simulated by the model. Based on the analytical models run by ESE and PBSJ the radius of influence of the wellfield proposed in the application is 43,000 to 45,000 feet. The approximate distances of the boundaries set in INTERSAT model from well TP were 50,000 feet to the east, 40,000 feet to the west, 40,000 feet to the north and 50,000 feet to the south. The INTERSAT model covers a total area of 320 square miles. This size falls somewhere between a regional model and a local model, and is adequate in size to address the impacts associated with the proposed withdrawals. The vertical boundary of SBWA's model extends to 1450 feet below land surface and, as stated above, is divided into 6 layers. The 1450 feet depth generally coincides with the limits of site specific data generated during the APT. The six layers in the SBWA flow model coincide with the six distinct geologic units identified by PBSJ in their APT report. The site specific data generated by the APT was utilized, along with other regional modeling studies, to arrive at a set of "conservative" aquifer parameters to be utilized in the INTERSAT model. "Conservative" parameters for purposes of this application are those which would tend to overpredict drawdown in the surficial aquifer and the production zone, while allowing for more upconing of dense water from the bottom of the model. The selection of "conservative" aquifer parameters by SBWA involved taking site specific values, comparing them with the ranges of values reported in the other available regional models and selecting values which, while still within the range of reported values used in other studies, would tend to show greater impacts for the areas of primary concern than the site specific values. Every aquifer parameter utilized in SBWA's groundwater flow model falls within the range of values reported in at least one of the groundwater modeling studies previously done in this region. The size of the grids utilized in the SBWA model were 500 feet by 500 feet within the vicinity of the wellfield. Grid sizes expand as one moves toward the outer boundaries of the model. The fineness of the grids used by ESE, particularly in the wellfield area, allows for accurate representation and resolution of surface water features, impacts in the production zone and for evaluating the effects of saltwater upcoming in the transport model also done by ESE. Within the radius of influence of the proposed wellfield, there are no existing wells in layers 5 or 6. The ESE model simulations for 18.8 mgd pumpage predict a maximum drawdown in the surficial aquifer (layer 1) of 0.14 feet centered primarily within the BCWMA. At a distance of 1 mile from the wellfield the impact drops to 0.12 feet. None of the existing legal users of water in layer 1 within the radius of influence of the proposed wellfield will suffer a ten percent or greater reduction in withdrawal capacity from their wells solely as a result of the proposed withdrawals, since 10 percent reduction would require at least 3 feet of drawdown. The ESE model simulations predict a maximum drawdown caused by the proposed pumpage of 4.5 feet in layer 3 centered along the alignment of wells and primarily within the BCWMA. At a distance of 2 miles, the drawdown drops to 2 feet. At the Brevard-Osceola County line the drawdown in layer 3 is approximately .5 feet. Petitioner Deseret's flowing wells are drilled in layer 3 and are located within the area where a drawdown of 1 foot is predicted in layer 3 by the ESE model. Deseret uses its property for a cow/calf ranching operation and has approximately 32,000 head of cows. Deseret uses 39 flowing wells east of state road 192 to irrigate pasture, water cattle and supply drinking water. Deseret possesses a valid CUP for a portion of the total flow capacity from those wells. Seasonally, the wells flow at different rates, but they are most relied upon in dry conditions when the natural flow would be decreased. It is unlikely that the proposed SBWA withdrawals will stop the flow of any of Deseret's wells; and it is unlikely that the flow will be reduced by more than 10 percent. Deseret and Osceola's consultants do predict a greater drawdown and opine that approximately 12 of Deseret's wells will cease flowing as a result of the SBWA withdraw As addressed below, the modelling by Petitioner's consultants, upon which those predictions are based, is less reliable than that of SBWA's consultants. If the effects are greater than predicted, mitigation in the form of installation of pumps is possible, albeit inconvenient and expensive. Mitigation would have to be provided by the applicant, SBWA. The drawdowns predicted by the ESE model for layer 4 are not significantly different from those for layer 3. It is anticipated that no legal user of water within the radius of influence of the proposed wellfield will suffer a 10 percent or greater reduction in withdrawal capacity for its wells, as a result of SBWA's proposed withdrawals. Petitioners' consultants, Hartman and Associates, (Hartman) modeled a significantly larger (4900 square miles) and deeper (3000 feet) area than did SBWA. The model makes its predictions based on one data point for every 49 square miles within the modeled area. Petitioners utilized much larger model grids in the wellfield area (2000 feet by 2000 feet) than did the SBWA. Grid of this size lacks the resolution necessary to evaluate wellfield impacts. Petitioners selected their aquifer parameters from another regional modeling study done in 1985 rather than using site specific data. Those parameters were then adjusted or calibrated until a match was obtained to a computer created potentiometric surface which was supposed to reflect the potentiometric surface for May 1990, an uncharacteristically dry period. The created potentiometric surface to which Hartman calibrated its model varies greatly from the potentiometric surface as reflected in the actual data points from which USGS derives its potentiometric surface maps. While no model is perfect, and actual data is preferable, in the absence of all the actual data that is needed, the ESE model is a more credible predictor of drawdowns. Anticipated Impacts to Groundwater Quality as a Result of the Proposed Consumptive Use Solute transport models are computer models designed to simulate the movement of mass, in this case -- chlorides -- through a groundwater flow system. These models are linked to, and are dependent on flow fields generated by groundwater flow models. In order to predict changes in water quality anticipated to occur as a result of its proposed withdrawals, SBWA's consultants used a solute transport model called HST3D. Developed by the USGS, this model is widely used and accepted. For simulations using the HST3D model, SBWA used the flow field and a portion of the grid generated by its INTERSAT groundwater flow model. The HST3D simulations run by ESE utilized a cross section of the INTERSAT model grid extending through row 26 of that grid, which is the row containing the line of 9 proposed wells running on an east-west axis. Use of a cross sectional grid is an appropriate method by which to examine salt water intrusion. Upconing, to the extent that it will occur as a result of the proposed pumpage, would be greatest within the cross section containing the 9 wells. The cross section extends two miles through the wellfield to the west. As chloride concentrations in water increase, the density of the water increases. Density can retard the degree of upconing when chloride concentrations are as low as 1000-2000 parts per million and becomes significant at 3000-5000 parts per million. Failure of a model to consider density effects, when appropriate, would tend to overstate upconing. HST3D does consider density effects. SBWA's consultant ran several simulations with the HST3D model to predict changes that would occur as a result of the proposed pumpage in chloride concentrations over 7, 14 and 30 year time periods. These simulations utilized the same aquifer parameters as the INTERSAT model together with the effective porosity values derived from site specific data. Assuming a starting chloride concentration of 1000 mgl at the bottom of layer 5, the measured concentration at that level in well TM on the BCWMA site, after 30 years of pumpage at 18.8 mgd, the chloride concentrations in layer 4 would increase by only 100 mgl. The simulations for 7 years of pumpage which is the duration of the proposed permit, show that the predicted increase in chloride levels would be substantially less than 100 mgl. Other HST3D simulations were run by SBWA for a pumpage rate of 35 mgd utilizing beginning chloride concentrations of 5,000 mgl and 10,000 mgl, respectively at the bottom of layers. The results did not show any significant changes in chloride concentrations in layer 4 over and above those shown when a lower starting chloride concentration was assumed. In a circumstance where, as here, the chloride concentrations in the zone from which water is proposed to be withdrawn exceeds secondary drinking water standards (250 mgl), the SJRWMD evaluates the existing legal water uses within the area that would be impacted by the proposed use. If it is determined that the increase in chloride concentrations caused by a proposed use would detrimentally affect other existing legal users or the applicant, only then is the increase deemed to be "significant". Within the layers of the aquifer which would experience increases in chloride concentrations as a result of the proposed withdrawal, layers 4, 5 and 6, no existing users of water would be detrimentally affected. Petitioner Deseret's closest wells to the proposed wellfield are in layer 3 where chloride levels will not be affected by the proposed wellfield within the 7 year duration of the proposed permit or even beyond that period. Further, the use Deseret makes of the water from the wells in closest proximity to the proposed wellfield, pasture irrigation, can tolerate significantly higher chloride concentrations than will exist even directly beneath the wellfield in level 4 after 30 years of pumping. Use of water for public supply purposes is considered by SJRWMD to be in the public interest. Utilization of the water beneath BCWMA for public supply purposes, even with some increase in chloride concentrations in the source of the water over the life of the permit, does not on balance detrimentally affect the public interest. Two different solute transport models were done by Petitioners' consultants, one a numeric model and the other an analytical model. The numeric model done by Hartman, RANDOMWALK, does not predict changes in chloride concentrations within an aquifer, but rather tracks movement of particles. RANDOMWALK does not account for density effects. The analytical model done by Prickett for the Petitioners relies on assumptions, many of which are not met in the aquifer system at BCWMA. Those assumptions relate to uniformity of the system, for example: porosity and permeabilities, and lack of regional gradients. The solute transport models utilized by the Petitioners are less reliable for predicting water quality changes resulting from the proposed pumpage than the model utilized by the SBWA. Salt water intrusion is a dramatic increase of chloride levels in an aquifer layer. The saline water encroachment which occurs from the wellfield stress will be in the lower confining unit. There will be limited degradation in the lower part of the production zone. The wellfield will not induce significant lateral intrusion from the east. There will not be any dramatic changes in chlorides. The movement of the chlorides is confined to the locality of the wellfield. Most of the movement is vertical and is of limited increase. The proposed Bull Creek withdrawals will not aggravate any currently existing salt water intrusion problems. The reject brine water from the RO treatment plant will be disposed of in deep injection wells in Brevard County. These injection wells would deposit the brine into a receiving body of water in the Oldsmar geologic formation. The brine reject will have a total dissolved solids (TDS) concentration of approximately 7,000 mgl. The receiving water into which the brine will be injected approximates sea water, with TDS concentrations in the range of 36,000 mgl. The receiving body will obviously not be further degraded. Environmental Impacts of the Proposed Consumptive Use District staff, SBWA consultants and Osceola's consultants independently conducted onsite field investigations of the BCWMA to evaluate the vegetative communities and land uses which exist on site. Each consultant prepared a habitat map identifying the various vegetative communities found at the site. While relatively pristine, the BCWMA has been logged and grazed by cattle in the past. The impacts of man's activities have been remediated by ceasing the activity. There are few permanent incursions, such as roads, canals and buildings. The area is a very diverse landscape, with a mosaic of different types of plant communities. There are various upland and wetland habitats. The variety of wetlands are forested and non-forested, deep and shallow, open and closed. These wetlands perform important functions, including water storage and purification, aquifer recharge, flood control, and provision of food sources and habitat for wildlife, and they are "factories" for producing the materials needed by many higher organisms. The wetlands on site are structurally complex and are good habitat for macro- invertebrates and the fish and higher organisms that feed on them. A number of these wetlands are shallow, isolated wetlands. During periods of inundation, when the wetlands fill up with water and interconnect with the Bull Creek drainage system, the system exports various organisms to the wetlands. Fish that are live bearers move into isolated wetlands during periods of inundation, and they and their offspring become a source of food for birds. Fish species that lay eggs can withstand desiccation (total drying out) can survive the temporary drying of wetlands, but live bearers must repopulate during periods of inundation. The mixed wetland hardwoods on site contain a diversity of bugs, crawfish, mayflies, damsel flies, midges, and snails. Some of these are important food sources for higher organisms. The apple snail, for example, is an important food source for such birds as the limpkin and the endangered snail kite, and its eggs are food for crawfish and other organisms. The biological communities that exist in the wetlands and uplands at the site are determined by a number of factors, including the depth and duration of the hydroperiod, soils, climate, temperature, and availability of sunlight. These communities and their habitats will react to changes in light, water, temperature, and many other subtle effects, causing changes in plant diversity and structure, the areal extent of certain types of habitats and wetlands, and utilization by wildlife. Natural fluctuations in the hydroperiod also cause these changes, generally from the exterior edges of a wetland to the interior. The wetlands in the BCWMA have been able to withstand the natural drought and flood periods, or they wouldn't be there today. Periodic burning is essential to the health of ecosystems such as in the Bull Creek area. Fires reduce the prevalence of species less tolerant to fire, allow other species to strengthen their presence, return organic material to the soil, and reduce the fuel available for wild fires. Originally occurring naturally as a result of lightening strikes, prescribed burns are now undertaken by agencies such as the Division of Forestry and the Game and Fresh Water Fish Commission to replicate the beneficial functions of natural periodic burning. Fire management is used as a land management technique at BCWMA and continued fire management at the BCWMA will maintain a natural ecological setting typical of Florida. Slight variations in elevation which mark the difference between wetlands and uplands can result in utilization of the areas by different animal communities. Where different types of plant communities meet, an "ecotone" is created. Where an ecotone exists, the "edge effect" of the competition between the two communities occurs. The result of the edge effect is higher plant and animal species diversity, which is extremely important to the natural community. Some animals make specific use of the ecotone for habitat and food resources. Many amphibians, frogs in particular, live in the ecotone. Some birds will not roost in the upland forests but will roost in the edge of the forest adjacent to wetlands. Wetlands in the BCWMA are connected to the remainder of the Bull Creek system through groundwater resources. Their biological and ecological communities are also connected as the same organisms move throughout the system. Isolated wetlands also exhibit a "moving edge" effect, where changes in the surface water and water table levels cause different plants, or plants at different levels of maturity, to exist in the wetland and its perimeter. This increases the productivity of the wetland by making it attractive to a wider variety of plant and animal species. If the expansion and contraction of isolated wetlands is reduced by lowered water levels, the smaller wetlands would exhibit a reduced edge effect, and the cumulative effect of this reduction over time would disrupt the functioning of the wetland-upland system. Isolated wetland systems are more sensitive to drawdowns in the surficial aquifer than connected wetland systems because the drainage area contributing water to the wetland system is smaller. Isolated herbaceous wetland communities are the most sensitive of the vegetative communities on BCWMA to drawdowns in the surficial aquifer. The surficial aquifer fluctuates naturally as much as five feet annually. Rainfall is the primary source of water for the surficial aquifer. Water levels in the surficial aquifer respond very quickly to rainfall events. Hydroperiods of the wetland systems in the BCWMA respond to rainfall and surficial aquifer levels. The wetland hydroperiods vary from year to year, and wetland ecosystems have adopted to those annual changes. But a groundwater withdrawal from the surficial aquifer in the Bull Creek area would cause a corresponding lowering of the surface water level, since the wetlands are not "perched", or separated from the aquifer by a confining layer. A drawdown would lower water levels throughout the hydroperiod, under both high water and low water conditions, with a more pronounced effect during the dry season and drought periods. Some of the over twenty threatened and endangered plant species present at Bull Creek grow in shallow, marginally wet areas. Changes in even a few inches of groundwater would cause these plant species to be retarded in growth, and their abundance would decrease or they would die out at the site. Many of the wetlands are shallow, broad, sloping areas, and groundwater elevation changes of just a few inches will cause changes in the areal extent of these wetlands. Even the .14 foot drawdown predicted by SBWA's modeling would affect shallow inundated or saturated systems by changing the moisture level at the surface, particularly by affecting the lowest water levels. Changes in the vegetative composition of wetlands will affect the macro-invertebrate characteristics of a site. For example, as water levels change, the density of the vegetation (in terms of number of plant stems per acre) can decrease, leaving fewer places for the macro-invertebrates to hide, and the populations of macro-invertebrates will decrease through predation. As food sources, habitat and breeding grounds decrease, those animal species that can relocate will attempt to do so. Relocation can adversely affect the survival of the species; for example, a wood stork unable to find a particular food upon which it is dependent at a particular interval in its life cycle may abandon its nest and its young. Animals that attempt to relocate may find that there is not a suitable similar habitat available, making their attempt to adjust to the change in their environment unsuccessful. The proposed use will not significantly affect the stages or vegetation of the upland communities at the BCWMA because they are not as dependent on saturation or inundation as a wetland community. Forested wetland systems, be they isolated or connected, will not be influenced by a drawdown of the magnitude predicted by SBWA for the surficial aquifer. Forested systems have deep root zones and the canopy provides shading to the strata below. Forested systems are able to tolerate natural changes in hydrology. The SBWA assessment does not offer any detailed cataloguing of the plant and animal communities on site, or a description of how the systems operate or interface with each other. It does not provide sufficient information to be able to assess the impacts of the proposed wellfield on these systems. There was insufficient information presented by the applicant to conclude that the environmental harm to be caused by operation of a wellfield at the BCWMA has been reduced to an acceptable level. The applicant relied on the fact that drawdowns in the surficial aquifer will be minimal, without fully considering the impact of those minimal drawdowns on a fragile wetland ecosystem during a dry period. Water Demand The SBWA was created by special act in 1983 as a dependent special district for the purpose of developing regional water supplies and transmission of water to water distribution systems. In its existence so far, its labors have been in the former, and none in the latter category. Efforts to develop a regional water supply have been frustrated by litigation, by reluctance of local public systems to give up their authority and by delays in pursuing and processing CUP applications, two of which are still pending, in addition to the instant application. The City of Melbourne's public water system provides water to Melbourne, Palm Bay and West Melbourne, and to some unincorporated areas surrounding Melbourne. It also supplies water to the area called south beaches, comprised of the Brevard County area south of Patrick Air Force Base, including Satellite Beach, Melbourne Beach, Indiatlantic and Indian Harbor Beach. The current water supply is Lake Washington, which is part of the chain of lakes on the St. Johns River. The city of Melbourne was granted a CUP on January 15, 1991, for withdrawals from Lake Washington, ranging from 27.15 million gallons maximum daily withdrawals in 1991 to 21.7 million gallons maximum daily withdrawals in 1998. In addition, Melbourne has planned a new facility and has the CUP to withdraw 8.13 million gallons a day from the Floridan Aquifer commencing in 1993. After reverse osmosis treatment, the groundwater withdrawal will yield 6.5 million gallons a day finished water, making up the difference from reduced withdrawals from Lake Washington. Approximately 56 potable water systems have been identified by SBWA in South Brevard, south of the Pineda Causeway. Almost all are small private systems. Besides Melbourne, the other major water supplier in the area is General Development Utilities (GDU), serving the City of Palm Bay. GDU's CUP expires in 1993 with an average daily withdrawal of 6.5 mgd and maximum daily withdrawal of 8.5 mgd. It has ample capacity until 1996, and beyond to the year 2000, if an additional Department of Environmental Regulation capacity rating is obtained. The total capacity of the two major existing facilities is approximately 30 mgd and total existing consumptive use quantities (including existing CUPs with expiration dates varying from 1993 to 1998) approach 40 mgd. The current SBWA water master plan assumes that existing sources need replacing. More specifically, SBWA, if this CUP is granted, seeks to replace Lake Washington as the primary source of water in the area with the groundwater obtained from the BCWMA wellfield. An agreement between the City of Melbourne and SBWA provides that the City will initially purchase 8 mgd, plus all future needs of water from the SBWA. This 8 mgd would be used by Melbourne prior to using its 6.5 mgd finished water from the RO facility, and the RO water would be used prior to withdrawals from Lake Washington. The agreement, dated January 9, 1991, acknowledges the need for, and specifically authorizes improvements to Melbourne's Lake Washington Water Treatment Plant, including the conversion of the existing high service pumping station to a low service pumping station with average daily capacity of 20 mgd and maximum capacity of 25 mgd. (SBWA Ex. 49) GDU is a private utility and currently is outside the jurisdiction of the SBWA. General Development Corporation is in receivership and the City of Palm Bay is negotiating for purchase of the utility. If the purchase is successful, the supply will become publicly owned and subject to the jurisdiction of the SBWA. The City of Palm Bay is not bound to purchase GDU at any price, and the requirement that it would shut down its newly purchased facility to receive water from SBWA is a disincentive to the acquisition. In the meantime, GDU has no incentive to reduce CUP capacity and devalue its facility. GDU's service has been uninterrupted and reliable. Contamination to the surface aquifer utilized by GDU has been successfully treated. Although septic tanks proliferate in Palm Bay, their location, as well as the presence of confining layers in the surficial aquifer, reduce the susceptibility of GDU wells to contamination from septic tanks. The applicant's concerns about unreliability and safety of Lake Washington as a continued water source are unsubstantiated by the weight of evidence in this proceeding. Surface water facilities have been used in Florida since before the turn of the century and no major facility has ever been off-line one day due to raw water contamination. Nor has any major Florida surface water plant ever been sabotaged. There is a greater chance in Florida of problems with pipeline failures, and the miles of pipes planned to transmit ground water from Bull Creek east to SBWA consumers increase the chances of those problems. Recently, the SJRWMD Upper Basin Project has significantly improved the water quality and quantity in Lake Washington through restoration of marshlands in the upper basin and capping flowing wells. Restored marsh areas will allow for additional removal of nutrients and provide an additional storage to the Lake Washington/Upper Basin system, significantly improving safe yield quantities. Comparisons of concentrations of raw water chlorides and total dissolved solids for the drought years of 1989 and 1990, show significant reductions for the latter time frame. Recent evaluations indicate that Lake Washington would be acceptable in terms of chlorides and TDS concentrations for a 35 mgd withdrawal, even during 50 and 100 year droughts. Water quality improvements to Lake Washington can be directly related to the Upper Basin project. Trihalomethanes are regulated by the Safe Drinking Water Act. They are produced by the disinfection process of treating raw water with chlorines, and they are carcinogenic. A previously experienced problem at the Melbourne plant has been corrected with operational changes. As recently as 1988, an internal staff report by SJRWMD staff provided: Lake Washington has been a reliable source of public water supply since 1960 and can remain so in the future with the continuation of sound basin planning and watershed management by the St. John's river Water Management District. The quality of the raw water from Lake Washington is subject to annual and seasonal variations that make the treatment process more difficult, and the quality of the delivered water less consistent, than would be the case with a groundwater supply. A supplemental water source near Lake Washington would improve the quality of the water delivered to the users, would increase the total volume that could be taken from the lake in times of stress, and would provide a reliable alternative in case of emergency. The upper zone of the Floridan Aquifer within south Brevard County has the potential to supply a significant portion of the area's future water needs with existing low-pressure, reverse osmosis technology at a cost that is comparable to current supplies.
Recommendation Based on the foregoing, it is hereby, recommended that the SBWA application for CUP be denied. RECOMMENDED this 12th day of March, 1992, in Tallahassee, Leon County, Florida. MARY CLARK 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 12th day of March, 1992. APPENDIX TO RECOMMENDED ORDER, CASE NOS. 91-1779, 91-1780, & 91-1781 The following constitute disposition of the findings of fact proposed by each party. Petitioner, Osceola County These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-5, 7-8, 14, 21-22, 24-25, 27-28, 30, 32, 35, 62-65, 73, 104, 113, 116-125, 127, 129-130, 132-138, 140, 154, 157-158, 164, 167-168, 183, 186, 189, 191-195, 197-200, 202-204, 209, 212. These findings are rejected as contrary to or unsupported by the weight of evidence: 37-38, 48, 51, 53, 56, 66, 79-81, 84-90, 92-94, 102-103, 105-107, 110-112, 115, 128, 171-172, 212(d), (f) and (g), 213-214. These findings are rejected as cumulative, unnecessary or irrelevant: 6, 9- 13, 15-20, 23, 26, 29, 31, 33-34, 36, 39-47, 49-50, 52, 54-55, 57-61, 67-72, 74- 78, 82-83, 91, 95-101, 108-109, 114, 126, 131, 139, 141-153, 155-156, 159-163, 165-166, 169-170, 173-182, 184-185, 190, 196, 201, 205-208, 210-211, 212(e), 215. Petitioners, Triple E, Triple N, East Central Florida Services, Inc., and Deseret These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-6, 8-9, 16-20, 22-25, 27-28, 30-31, 50- 56, 59-60. These findings are rejected as contrary to or unsupported by the weight of evidence: 7, 12, 32, 34-37, 40, 42, 44, 48, 49, 58. These findings are rejected as cumulative, unnecessary or irrelevant: 10- 11, 13-15, 21, 26, 29, 33, 38-39, 41, 43, 45-47, 57, 61-63. Respondent, South Brevard Water Authority These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-6, 9-11, 13, 16-24, 28, 30-34, 36, 38, 46-48, 61, 64, 70, 72-74, 90-91, 94-98, 105-108, 110-111, 113, 115-116, 121, 126-129, 133, 149, 152, 157, 169, 179, 181-190, 192-194. These findings are rejected as contrary to or unsupported by the weight of evidence: 41, 130-132, 156, 158, 167, 174, 177. These findings are rejected as cumulative, unnecessary or irrelevant: 7-8, 12, 14-15, 25-27, 29, 35, 37, 39-40, 42-45, 49-60, 62-63, 65-69, 71, 75-89, 92- 93, 100-104, 109, 112, 114, 117-120, 122-125, 134-148, 150-151, 153-155, 159- 166, 168, 170-173, 175-176, 178, 180, 191. Respondent, St. Johns River Water Management District These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-8, 10-22, 24-36, 38-44, 47-62, 64-88, 90, 92-116, 118-122, 124-130, 132-142, 144-151, 159-160, 164, 166-167, 169, 171, 174-175, 177, 193-196, 198, 202, 206. These findings are rejected as contrary to or unsupported by the weight of evidence: 131 (the conclusion), 153-154, 156-157, 161-162, 197, 204, 207. These findings are rejected as cumulative, unnecessary or irrelevant: 9, 23, 37, 45-46, 63, 89, 91, 117, 123, 143, 150, 152, 155, 158, 163, 165, 168, 170, 172-173, 176, 178-192, 199-201, 203, 208-210. COPIES FURNISHED: Segundo J. Fernandez, Esquire Scott Shirley, Esquire OERTEL, HOFFMAN, FERNANDEZ & COLE, P.A. Post Office Box 6507 Tallahassee, FL 32314-6507 Douglas P. Manson, Esquire BLAIN & CONE, P.A. 202 Madison Street Tampa, FL 33602 Clifton A. McClelland, Esquire POTTER, McCLELLAND, MARKS & HEALY, P.A. Post Office Box 2523 Melbourne, FL 32902-2523 Wayne Flowers, Esquire Nancy B. Barnard, Esquire St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429 Neal D. Bowen, County Attorney Osceola County Room 117 17 South Vernon Avenue Kissimmee, FL 32741 Carol Browner, Secretary Dept. of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Daniel H. Thompson, General Counsel Dept. of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400
Findings Of Fact At all times pertinent to the issues herein, the Southwest Florida Water Management District had permitting authority for the issuance of consumptive use permits in the area in which Respondent, El Jobean, proposes to sink its irrigation well. On December 12, 1988, El Jobean submitted a consumptive use permit application to sink a new well for the purpose of irrigation of a golf course to be developed on the property it owns in Sarasota County. The well is to be located in the NE 1/4 of the NE 1/4 of Section 32, Township 365, Range 20R, in Sarasota County, Florida near the southern boundary of an irregularly shaped piece of property consisting of approximately 855 acres, owned by the applicant, which extends over Sections 28, 29, 32 and 33, Township 365, Range 20E. Respondent proposed to sink a 10 inch diameter well to a total depth of approximately 900 feet with casing in the well now to extend down to 300 feet, with a pump capacity of 1,000 GPM. The golf course to be irrigated is to encompass approximately 190 acres. The applicant requested authority to withdraw an average of 600,000 GPD with a limitation of a maximum of 1,440,000 GPD. The application was properly staffed by the District. In the staff report on the application, the average daily use limitation was expanded to 707,000 GPD; consumptive use was raised from 0 to 139,000 GPD; and maximum daily consumption was reduced from 1,440,000 GPD to 1,240,000 GPD. These changes were due to correction of arithmetic errors in the application and were accepted by the applicant. The ultimate recommendation of the staff was for approval of a 6 year permit, subject to certain conditions outlined in subparagraph I of the staff report. These special conditions require the provision and use of flow measuring devices to maintain an accurate record of the water withdrawn; the maintenance of flow records and the providing of periodic reports to the District; the collection and analyzing of water quality of samples taken from the well to measure the appropriate parameters for chlorides, sulfates, and total dissolved solids; the reporting of the results of these samplings and a description of the sampling and analytical methodologies employed; and a requirement that the permittee investigate the feasibility of supplementing and/or substituting drawn water with treated sewage affluent. After the staff report was submitted, proper notice of the District's intent to issue the permit was published. Based on that notice, protests were filed both by Miakka and Mr. Bishop. The area in question is located within the Manasota Basin which, itself, is located within the Southern West-Central Florida Ground Water Basin, (SWCFGWB), which encompasses all of Pasco, Hillsborough, Manatee, Sarasota, Polk, Hardee, and DeSoto Counties, and parts of Lee, Glades, Charlotte and Highlands Counties. The SWCFGWB sits atop several aquifers which include the Floridian Aquifer, two Intermediate aquifers, and the Surficial Aquifer. The Floridian Aquifer is the deepest and the Surficial Aquifer is on the top. The Miakka Community Club is a Florida corporation made up of residents of the pertinent area whose primary function is to preserve and conserve the rural nature and spirit of the Northeast section of Sarasota County. The club performs this function through educational programs, community activities, and participation in the legislative process. Miakka urges denial of the permit sought by El Jobean based on its membership's belief that the property owners whose property is in the immediate vicinity of the proposed well will be adversely affected if El Jobean is permitted to sink its well and withdraw water from it. The club membership believes that approval of El Jobean's well will result in contamination of existing personal water wells due to excessive use by El Jobean; potential contamination of Sarasota County's future drinking water sources which include the capital Ringling,/MacArthur tract and the Myakka River; reduction of property values; and destruction of personal resources. Petitioner also urges that since the proposed golf course will be a part of a private club for the use of members only, in which membership will be limited, there is no public benefit derived from the approval of and sinking of the well in question. Petitioner also contends that during the periods of severe water shortage as are being currently experienced, permission to sink a well of this size to draw water in of the magnitude expressed in the application, would be counterproductive and detrimental to the interests of the other property owners in the area. In support of its claim, Petitioner presented the testimony of two homeowners from the area, Mr. Richardson and Ms. Mustico. Mr. Richardson, whose well is 183 feet deep, has had several problems with his well even without the instant drilling. In 1974, and subsequent thereto, he has had to go deeper with a suction pipe because the water has dropped below the level of the tail pipe. Ms. Mustico's 160 foot deep well, with 80 feet of casing, is used to supply water for the home. She also has other wells for watering her lawn and for livestock, one of which goes down 500 feet. She is concerned that the well proposed by El Jobean will adversely impact her ability to draw water from her wells because, she believes, the water level from which her water is drawn will drop. In the past, her primary well has gone dry and the wells of several neighbors have gone dry as well. Through maps and other documentation taken from the Ground Water Resource Availability Inventory for Sarasota County, Florida, prepared by the District in March 1988, Petitioner has established that areas of significant groundwater withdrawal within the SWCFGWB occur in Hillsborough, Manatee, Polk, Hardee, DeSoto and Highlands Counties. With the exception of an extremely small portion of Sarasota County located contiguous to Manatee County, there appear to be no areas of major ground water withdrawal currently existing in Sarasota County. The majority of the major municipal well fields within the pertinent basin that are located within Sarasota County, extend down to the Intermediate and Surficial Aquifers with only 3 extending through the lower Intermediate into the Floridan Aquifer. These include the Verna well field located in the northeast corner of Sarasota County where it abuts Manatee County; the Sarasota County well field located in northwest Sarasota County near the Manatee County line; and the Sorrento Utility, Inc., well field which is located near the Gulf Coast, approximately two-fifths of the way down between the Manatee and Charlotte County lines. With the exception of the Verna well field, all the municipal well fields in Sarasota County appear to be reverse osmosis systems and as of 1987, there were 28 reverse osmosis systems located within Sarasota County. Most are relatively small in their output measured in millions of gallons per day. With the exception of 3 public supply wells, 2 of which are permitted an average annual pumpage greater than 100,000 GPD and 1 of which is permitted less, all of the permitted public supply well fields in Sarasota County are located west and south of 1-75 as it extends from the Manatee County line in the north to the Charlotte County line in the south. The El Jobean well would be located east of the line, in that area occupied by the 3 public supply wells. Generalized recharge areas for the upper Floridan Aquifer in the groundwater basin in issue here have been categorized from "high", with a rate of more than 10 inches per year, to "Generally none", with a recharge rate at 0. In 1980, the high recharge rates existed in the north-central part of Pasco, the eastern part of Polk County, and the northeastern part of Highlands County. Sarasota County is in an area wherein the recharge rate was either very low or generally none. In September 1986, the high recharge rate was found in a very small area of northeastern Pasco County, and small areas in both Polk and Highlands Counties. Sarasota County, for the most part, was classified as having no recharge. In May 1987, the high recharge rates were, again, a small area in eastern Pasco County, a small area in northeastern Hillsborough County, a small area in southeastern Polk and northwestern Highlands Counties, and a minuscule area in central Pinellas County. Again, Sarasota County had a recharge rate of 0. Generalized estimated, calibrated, model-derived recharge and discharge values for the upper Floridan Aquifer in the ground water basin in issue here, as they pertain to Sarasota County, reflect positive 2 recharge to negative 1 discharge inches per year. Historically, however, the northeast portion of Sarasota County, where the El Jobean well in question would be located, evaluated by various individuals or agencies periodically from 1980 through 1988, reflects a recharge of anywhere from 0 to 2 inches per year. None of this documentation was supplemented, however, by direct testimony by an individual knowledgeable in this area, and Petitioner's main thrust appears to be an unsubstantiated fear that the sinking of El Jobean's well will have a negative impact on its membership's wells. Admittedly, the residents in the area in question all rely on private wells for the majority of their water supply, other than through the catchment of rainwater, which is insignificant. It was also established that the area has been undergoing a severe water shortage and that conservation measures have been mandated. On the other hand, El Jobean presented the testimony of a hydrogeologist, Mr. Moresi, who has extensive experience with the modeling process used to determine water consumption and recharge in southwest Florida and Sarasota County. The aquifer system in Florida is made up of water bearing limestone layers below the surficial sand base. This aquifer system underlays the various zones throughout the state and reflects a surficial aquifer extending from ground level down approximately 70 feet to a confining bed which separates it from the lower strata. This top confining bed is approximately 20 feet thick, and below it is the Tamiami-Upper Hawthorn Aquifer, which is between 100 and 200 feet deep and which rests on another confining bed somewhat thicker than the upper one. Below the second confining bed is the Lower Hawthorn-Upper Tampa Aquifer which extends approximately from the 250 foot to the 450 foot level at the Manatee County line, and between the 320 foot and the 710 foot level at the Charlotte County line. Another confining bed lays between this aquifer and the Floridan Aquifer which starts at the 500 foot level and goes down well below the 900 foot level in the north and extends from the 730 foot level down in the south. The confining bed below the surficial aquifer is made up of a clay material which retards the movement of water from one aquifer to another. The surficial aquifer is porous and saturated with water from the water table down. Since the confining beds are far less porous than the aquifers they separate, water moves much more slowly through them. The lower aquifers are made up of limestone and are also porous and contain water. The Tamiami-Upper Hawthorn formation consists of limestone and clay, but is water bearing. The Lower Hawthorn-Upper Tampa formation is similar and both make up the intermediate aquifer below which is the lower confining bed followed by the Floridan aquifer. Respondent's well would be cased in steel down to an area approximately 100 feet into the Floridan Aquifer, through the Lower Hawthorn- Upper Tampa Aquifer and through the lower confining bed. Since the well would be cased to well below the lower confining bed, water existing in the upper aquifers, would be prevented from being drawn down by operation, of the Respondent's well either directly or by settling down to replace the water drawn out. Generally, the deeper a well is drilled, the worse the quality of the water, and it becomes less potable. The Floridan Aquifer produces far more copious quantities of water than do the intermediate aquifers. However, since it is cheaper to drill to the intermediate zones as the wells need not be so deep, and since the water there is better, most domestic wells go no deeper than these aquifers. They go down approximately 150 to 180 feet. The pressure in each level is separate from and different from that in the other aquifers. The upper intermediate system generally has a lower pressure than the lower intermediate system. As a result, water from the lower intermediate system tends to leak upward toward the upper intermediate aquifer, rather than the reverse. In addition, a recent survey tends to show that the Floridan aquifer also tends to leak upward into the lower intermediate level. It also shows that leakage through the confining beds amounts to .002 GPD per cubic foot of aquifer. Petitioner claims that since the lower water is of lesser quality, and since withdrawal of water from the upper layers would promote leakage upward, thereby adding lower grade water to the better grade upper water, there could be a diminishment in upper level water quality as a result of water being drawn from the upper levels. However, according to Mr. Moresi, the .002 figure is so small it would result in an infinitesimally small drawdown of water level from the upper intermediate level aquifer and the potential for compromise of the water quality therein is remote. Clearly, this is not the result of drawing water from the Floridan Aquifer as the well in question would do but more the result of the residential wells extending into the upper levels. The District ran a model for the proposed El Jobean well (a Jacob- Hantush model) which showed that drawdown at the wellhead would be just over 2 feet. This means that use of the Respondent's well would reduce the water level in the Floridan Aquifer at the well head by 2 feet. However, this drawdown is shown to decrease rapidly out to where, at distance, it is almost immeasurable. In fact, drawdown of the Floridan Aquifer at 24,000 feet from the well head (approximately 4.5 miles) would be .1 feet, slightly or 1 inch. The .1 foot drawdown relates to the lowest (Floridan) aquifer and the resultant drawdown in the upper intermediate aquifer, into which the majority of residential wells are sunk, would be relatively undetectable. Since the Petitioner's wells, at their deepest, go only into the upper intermediate level, and would be separated by 2 confining beds from the Floridan Aquifer, the impact on the domestic wells at 2 miles from the El Jobean wellhead would be immeasurable. Even at 1 mile, there would be minimal drawdown in the Floridan Aquifer and almost none in the upper intermediate aquifer. The potentiometric surface of the intermediate layer would not be adversely affected, nor would that of the surface water. Recognizing the potential for saltwater intrusion which occurs all along the coast, based on his studies, Mr. Moresi concluded that the well in question here would not induce significant saltwater intrusion. He concluded as well that the permit is consistent with the requirements of the District rule; that the amount permitted for the use of irrigation of the golf course is reasonable, assuming a golf course is a reasonable and appropriate use of water; that the withdrawal by the well in issue would not have an adverse impact on users outside the property on which the well was located; that it would not impact existing users; that there is no other water available for the purpose intended; that the water taken from the Floridan Aquifer under this permit may be potable but is of poor quality; and that the applicant met rule standards. Mr. Moresi also discussed the possible cumulative impact of the proposed well when operated along with the currently existing wells. If there are other drawdowns from the same cone into which El Jobean's well would be sunk, the withdrawals would be cumulative. However, as best he can determine, the only other significant drawdown from the cone pertinent here is that of the Verna well field. In his opinion, that well field's drawdown, which is from the northeast, would not be significant even when considered with the El Jobean well. Mr. Moresi was also satisfied that while the confining bed separating the surficial aquifer from the next lower level might be disturbed, the deeper one goes, the less likely there is to be mixing of aquifers. The only instance where water could move from one level to another as a result of the well is where there is no casing on the bore hole. In the instant case, plans call for, and permit conditions require, the well to be cased to below the lowest confining bed. Consequently, there should be no upward or downward flow of water as a result of the bore. Mr. Tyson, who worked on the evaluation of El Jobean's application for permit, was of the opinion that the amount of water requested by El Jobean in its application was appropriate for a golf course. This does not mean that a golf course is an appropriate use of the property. The special conditions imposed on the granting of the permit by the District are designed to reduce any impact possibly caused by the permitted activity. The Jacob-Hantush model used in analysis of the instant application is considered to be a conservative tool and showed minimal drawdown at all property boundaries. The use of other models in this case was considered neither necessary nor appropriate. Mr. Tyson considers the proposed permit a reasonable beneficial use as defined in the Florida Administrative Code and statutes because it proposes use of reasonable amounts of water and the models indicate no unfavorable impact. Based on the past practice of permitting golf courses with subdivisions, he feels the proposed use is reasonable. He concludes, therefore, that it is in the public interest to grant this permit. In his opinion, the permit will not interfere with legal existing uses and meets all statute and rule requirements. Considering the evidence as a whole, it is found that petitioner has presented insufficient evidence to support its claim that approval and operation of El Jobean's well as proposed would have an adverse impact on the property owners. It's concerns are no doubt sincere, but these concerns are not sufficiently confirmed by evidence of record. At the hearing, the parties stipulated that if the permit were granted, it would be modified by the addition of two conditions: The proposed well shall be constructed with a minimum of 600 feet of casing so as to prevent the unauthorized interchange of water between water bearing zones in order to prevent the deterioration of water quality in the shallower zones. If the well cannot be properly completed to prevent such an unauthorized interchange of water, the well shall be abandoned and plugged in accordance with Rule 17-21.10(2)(c), F.A.C.. Upon completion of the well, a copy of the well construction completion report shall be sent to the District. The permittee shall line the bottom of the pond that will be used as the irrigation source, with clay to a thickness equal to 1.5 feet.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that the Southwest Florida Water Management District enter a Final Order issuing Consumptive Use Permit Number 209458, as modified by the conditions stipulated to at the hearing held herein on June 7, 1989, and outlined in Finding of Fact Number 27 herein, to El Jobean Philharmonic Group, Inc. RECOMMENDED this 9th day of August, 1989 at Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of Division of Administrative Hearings this 9th day of August, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 88-1176 The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. For the Petitioner: Not a Finding of Fact but a statement of the ultimate issue of fact. Accepted and incorporated herein. 3-6. Accepted and incorporated herein. 7-12. Accepted and incorporated herein. Accepted as indicating original conditions. The parties stipulated to additional conditions at the hearing. Accepted. 15 & 16. Accepted and incorporated herein. 17-33. Accepted and incorporated herein as pertinent. 34 & 35. Accepted. 36 & 37. Accepted. 38 & 39. Redundant. 40-43. Accepted. 44. Accepted. 45-51. Accepted. 52 & 53. Accepted. 54-56. Accepted. 57 & 58. Accepted and incorporated herein. 59-66. Accepted. 67-75. Accepted and incorporated herein. 76 & 77. Accepted and incorporated herein. 78. Accepted. 79-84. Accepted. Accepted and incorporated herein. Rejected. 87 & 88. Accepted. 89-93. Accepted and incorporated herein. Accepted. Accepted in the natural source sense suggested by Petitioner. 96-99. Accepted and incorporated herein. 100 & 101. Accepted and incorporated herein. 102-105. Accepted and incorporated herein. 106. Accepted. 107 & 108. Accepted. 109 & 110. Accepted. For the Respondents: 1 & 2. Stipulation between the parties accepted and incorporated herein. 3-6. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence except for the second sentence which is incorporated herein as a Finding of Fact. Not a Finding of Fact but a comment on the evidence. 9-11. Accepted and incorporated herein. 12. Accepted. 13-16. Accepted and incorporated herein. 17. Accepted and incorporated herein. 18 & 19. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. 22-26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29. Accepted. 30-32. Accepted and incorporated herein. 33-40. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Not a Finding of Fact but a Conclusion of Law. COPIES FURNISHED: Becky Ayech Personal Representative Miakka Community Club 421 Verna Rd. Sarasota, Florida 34240 Douglas Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Edward B. Helvenston, Esquire Assistant General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609 6899
The Issue The issue in this case is whether the South Florida Water Management District (SFWMD) should modify Surface Water Management (SWM) Permit No. 50-00548-S, held by the ACME Improvement District (Acme) to authorize alternate SWM facilities within Acme Basin B primarily by: eliminating the water quality function originally provided by a 79-acre retention area known as Peacock Pond pursuant to a 1979 permit; replacing it with adequate alternate methods of water quality treatment; and authorizing an alternative pump operation schedule for the remainder of Acme Basin B. The permit should be modified only if Acme has provided reasonable assurances that the proposed modifications comply with the relevant portions of SFWMD's Environmental Resource Permit (ERP) regulations set forth in: Part IV of Chapter 373, Florida Statutes; Chapter 40E-4, Florida Administrative Code; and the Basis of Review for ERP Applications (BOR) (collectively referred to as ERP criteria).
Findings Of Fact General SFWMD is a public corporation existing by virtue of Chapter 25270, Laws of Florida, 1949, and operating pursuant to Chapter 373, Florida Statutes, and Title 40E, Florida Administrative Code, as a multipurpose water management district with its principal office in West Palm Beach, Florida. Acme is a dependent special district of the Village of Wellington, a municipality of the State of Florida. Polo is a Florida corporation and a developer in the Village of Wellington, Palm Beach County, Florida, including a 79-acre parcel of real property known as Peacock Pond, and other undeveloped property that are part of the subject of this permitting proceeding. Wellington Country Place Property Owners Association, Inc. (POA) is the property owners association for WCPPUD. Permit History 1978 Permit In 1978, SFWMD issued to Acme the original backbone SWM permit for approximately 18,000 acres, including primary drainage Basins A (to the north) and B (to the south). Pierson Road, which runs east/west, is the boundary between the two basins. (The backbone C-23 canal parallels Pierson Road to its immediate north.) Acme Basin A discharges to the C-51 canal, which flows east to the Atlantic Ocean. Acme Basin B, which consists of approximately 8,680 acres, discharges to the Loxahatchee National Wildlife Refuge (Refuge) through two Acme pump stations. The Refuge is part of what is now designated the Everglades Protection Area. The 1978 backbone permit, which modified a still earlier permit, established lower water control elevations in Basin A, which was being developed for urban use, than in Basin B, which was planned to remain largely in agricultural use. Under the 1978 permit, the maintained (regulation) stage in Basin A was set at 11' above mean sea level (msl) with discharge beginning at 12' msl during the wet season and 12' msl with discharge beginning at 13' msl during the dry season. The maintained stage in Basin B remained at 13' msl in both the wet and dry season. Under the 1978 permit, it was anticipated that routing surface water runoff in Basin A through canals and retention lakes would provide the water quality treatment required under the criteria in effect at the time (including a requirement to provide half an inch of detention over the entire Basin A for water quality treatment purposes.) At the time, planned residential development in the extreme southwest corner of Basin B was anticipated to generate only limited quantities of runoff due to the nature of typical development in 5-acre parcels; quality of runoff was expected to be better than from previous agricultural use. Presumably because there would be no change under the 1978 permit, water quality treatment in the remainder of Basin B was not addressed. 1979 Permit By 1979, Acme requested a permit modification for development of the Wellington WCPPUD, which is located entirely within Acme Basin B. The PUD's northern boundary is Pierson Road; the western boundary is the backbone C-2 canal; and the eastern boundary is the backbone C-6 canal. The north/south backbone C-4 canal divides the western third of the PUD from its eastern two-thirds; it also forms the western boundary of the area known as Peacock Pond. The southern boundary of the PUD generally follows the east/west backbone C-24 canal.2 The 1979 permit modification authorized construction and operation of water management facilities in portions of WCPPUD, including a 79-acre pumped retention area (which was to become known as Peacock Pond), pump station, and control structure. Under the 1979 permit, the maintenance stage (water control) elevation within WCPPUD only was set at 12' National Geodetic Vertical Datum (NGVD) (essentially, the same as msl) in the wet season and 13' NGVD in the dry season. The minimum road and finish floor elevations were established at elevation 16' and 17' NGVD, respectively. Without regard to seasonality, the retention area pump station was to begin operation when a stage of 13' NGVD was reached in the adjacent C-4 canal and was to discontinue operation when the system was drawn down to elevation 12' NGVD. The 1979 permit used the 79-acre area known as Peacock Pond as its central water quality feature. Runoff from WCPPUD was to be collected in roadside swales within road right-of-ways and routed by storm sewer inlets and pipe to either a proposed 12-acre lake or one of the collector swales or canals connected to the Peacock Pond site. The 1979 permit contemplated use of the Peacock Pond site as a "retention-type" surface water management facility. Generally, such a facility detains the water, allows the pollutants to settle, then slowly lets the water out. In the 1979 permit, Acme was required to construct a berm or dike around the 79-acre area to create an above-ground impoundment to serve as the retention area. A pump was required to be installed at the northwest corner of Peacock Pond to pump water from the adjacent C-4 canal into the retention area. The berm or dike was to detain water on the site until it reached the level of a gravity flashboard riser outfall structure at the southwest corner of the site, which would be set at 15' NGVD and would return the water to Acme's C-4 canal just downstream of a broad-crested weir, which would be set at 14' NGVD. Additional discharge from the system would be provided by two 72-inch gravity-flow flashboard risers with crest elevation 14' NGVD-- one to the C-4 canal and the other to the C-6 canal. Water discharged from the system would flow south and west through Acme's system of Basin B canals, eventually discharging to the Refuge through the two pump stations to the south and southwest. During a rise in stage in the C-4 from 13' to 14' NGVD, the pump station in the northwest corner of Peacock Pond would continue filling the retention area. Considering pumped inflow of 4000 gallons per minute (gpm), the retention area would take 3.3 days to reach a peak stage of 16'. At that stage, 58 acre-feet of water would be stored within the retention area. SFWMD calculated that Peacock Pond would treat approximately 200 million gallons of water a year in this way. SFWMD and Acme have taken the position in this case that the sole purpose of Peacock Pond in the 1979 permit was to serve as a water quality treatment area for the Wellington WCPPUD. It is true that the 1979 permit contemplated that flood protection for Basin B would be provided through use of the two pumps discharging into the Refuge (Pump #1 capable of pumping at the rate of 100,000 gpm, and Pump #2 capable of pumping at 120,000 gpm). But, as subsequent events showed, the Peacock Pond retention area was part of an overall SWM system for WCPPUD that maintained water stage elevations there at a lower level than in the rest of Basin B. In other words, while designed primarily to provide water quality treatment, and not designated a flood control facility, it had some residual flood control benefit within WCPPUD. Actual Operation After 1979 Permit Although Peacock Pond was critical to the functioning of the SWM system for WCPPUD and Basin B, SFWMD never obtained from the owner the legal right to use it for SWM purposes. From 1979 to 1986, SFWMD was advised that the Peacock Pond facility was in substantial conformance with the permitted conditions. But some time after property, including Peacock Pond, was transferred to Landmark Land Company of Florida, Inc., the pumps in the northwest corner of Peacock Pond stopped being used regularly.3 Instead, Acme water control structure 115 (a 48-inch culvert and 72-inch flashboard riser which replaced the broad- crested weir in the C-4 canal through a 1982 permit modification) and structure 117 (discharging to the C-6 canal) were opened so that water levels in Wellington Country Place equalized with the surrounding Acme Basin B, which was controlled by the two pump stations discharging to the Refuge to the south and southwest. The evidence indicates, for at least the last ten years, the Basin B pumps have been operated to maintain water elevations of 12' NGVD in the wet season and 13' NGVD in the dry season--the same as for the County Place PUD under the 1979 permit. Under this water elevation control regime, flooding within WCPPUD was not a problem, but the water quality treatment from the Peacock Pond facility required under the 1979 permit was not being realized. The pump operation schedule under the 1979 permit did not specify a "bleed-down" mechanism. As a result, when internal stages exceeded the specified control elevation threshold, both Basin B pumps would be operated at a combined rate of 220,000 gpm until the seasonal water control elevation was again established. This operation did not take full advantage of the nutrient removal capacity of the existing system. 1989 Equestrian Estates Permit Modification In 1989, construction and operation authorization was issued for the Equestrian Estates development located within WCPPUD west of the C-4 canal. Among other things, this modification to SWM Permit No. 50-00548-S included the construction of lakes for use as wet detention ponds and a control structure allowing discharge from Lake No. 5 (as designated in Exhibit 2 of the Staff Report, SFWMD Exhibit 5) to the C-4 Canal. However, this control structure and its associated culvert were never constructed. Peacock Pond Enforcement Proceedings Around 1997, SFWMD was informed that the Peacock Pond pump was not being operated and initially brought enforcement proceedings against Polo, which had become the owner of the property in 1993, to resume pumping into Peacock Pond. At the time, SFWMD was involved in enforcement proceedings against Polo, as owner, for unauthorized dredging and filling in Peacock Pond, and SFWMD made an incorrect assumption that Polo was the operator of the Peacock Pond facility under the 1979 permit. SFWMD subsequently realized that Acme, not Polo, was the permit holder. When Acme attempted to turn the pumps on again, Polo refused to allow Acme to do so without compensation. SFWMD then brought an enforcement action against Acme for not operating Peacock Pond in accordance with its permit. SFWMD and Acme entered into a Consent Order requiring Acme to operate Peacock Pond and the rest of the SWM system as required by the 1979 permit. Acme subsequently brought eminent domain proceedings against Polo to acquire Peacock Pond and obtained a final judgment, but the compensation required under the final judgment was prohibitive. SFWMD and the Village of Wellington then entered into a Joint Cooperation Agreement, which (among other things) required the Village of Wellington to submit an "application to modify the Peacock Pond Permit and Consent Agreement to either eliminate or substantially reduce the size of Peacock Pond [which] must provide reasonable assurances that demonstrate that the water quality treatment, water quantity and environmental benefits associated with the Peacock Pond Permit are maintained through the modified facility or by other equivalent measures." In the meantime, SFWMD ordered Acme to set control structures 115 in the C-4 canal and 117 in the C-6 canal at 14' NGVD as required by the original 1979 permit. When this was done without operation of the Peacock Pond retention area as also contemplated and required by the 1979 Permit, the water levels caused septic tank problems to some residents in WCPPUD, leading SFWMD to issue emergency authorizations to lower the crest-settings of structures 115 and 117 to 12.5' NGVD. At those settings, water levels in WCPPUD stayed between 12' and 13' NGVD, and there have been no septic tank problems in the last two years. Specifically, measured water levels in the C-4 canal north of control structure 115 generally ranged between elevation 12' NGVD and 13' NGVD from November 2001 through October 2003, with occasional variances above or below due to drought or rain periods. Proposed Modification to Eliminate Use of Peacock Pond On May 12, 2000, Acme filed an application to modify its permit. The primary purpose of this modification was to authorize alternate SWM facilities within Basin B (primarily within WCPPUD) to maintain the water quality treatment function that was assumed would be realized by Peacock Pond in the WCPPUD permit issued in 1979. Additional components of the permit modification are: installation of a 7.8 acre flow through littoral zone within the C-2 Canal for additional cleansing of Acme Basin B water; modification of the pump operation schedule for Basin B; revision of surface water management design requirements for future development within Country Place to include additional lake acreage and littoral zones; elimination of a previously permitted (but not constructed) control structure allowing discharge from Lake No. 5 to the C- 4 Canal so that water from Lake 5 continues to drain through established canals and lakes into the C-4 Canal; modification of existing flashboard riser water control structures 115 and 117 within the C-4 and C-6 Canals to crest elevations of 12’ and 13’ NGVD, respectively, so that water will be detained upstream but water from both the eastern and western ends of the Wellington WCPPUD drain toward and into the C-4 canal during low flow; and an analysis of nutrient (and phosphorus) loading, removal and export from the Country Place system During the application process, Acme submitted detailed water quality calculations analyzing and comparing the 1979 permit, based on the land uses at that time and the anticipated phosphorous loading that would be discharged from the system, and the proposed modification with current land uses and phosphorous loading now anticipated. To support its modification application, Acme recalculated the water quality treatment currently provided by existing lakes--many of which were not planned in 1979--and other water quality treatment features in WCPPUD. Acme's calculations assumed that all land owners of undeveloped tracts in Basin B, including land owners in WCPPUD, wishing to develop their properties in the future will have to provide for adequate water quality treatment or other acceptable alternatives, as required by SFWMD regulations in place at the time the future permit applications are filed. In order to meet those requirements, future developers can either create lakes on their properties, treat their water off-site on properties such as Peacock Pond, or use other equivalent alternatives. In conformance with current SFWMD criteria, Acme’s application only considered and counted as water quality treatment features water bodies with an average width of at least 100' and a size of at least 0.5 acres. SFWMD spent an enormous amount of time reviewing the data and analyses that were submitted. SFWMD then issued numerous lengthy requests for additional administrative and technical information, requiring Acme among other things to provide water level information and perform management calculations. Acme provided necessary calculations to demonstrate that flood levels within WCPPUD would not be affected by the elimination of Peacock Pond as a water quality feature. Acme's calculations demonstrated that the water quality treatment functions currently provided by existing lakes meeting SFWMD's dimensional criteria and by on-site swales, together with the 7.8-acre off-site littoral shelf to be constructed in canal C-2, would be sufficient to replace the water quality treatment functions assumed to be provided by Peacock Pond under the 1979 permit. SFWMD issued a Staff Report on April 29, 2003, recommending approval of the application to modify the SWM permit. SFWMD found that Acme had provided reasonable assurances by Acme that the applicable permit criteria would be met. On May 15, 2003, the SFWMD Governing Board approved the Staff Report to issue a modification to SWM Permit No. 50-00548- S, Application No. 000512-12. Control Elevations and Pump Operation Schedules The proposed permit modification states that there will be a change in the permitted water control elevations and pump operation schedule within Basin B. However, as set out in Finding 17, supra, in actual practice, water elevations throughout Basin B have been maintained at the levels permitted for WCPPUD under the 1979 permit for at least the last ten years, which include the time period after the Peacock Pond pumped retention area stopped being operated as required under the 1979 permit. The proposed modifications essentially would continue the historical operation of the Acme Basin B system during this time period. In essence, the changes in Basin B outside WCPPUD will simply conform the permit conditions to actual conditions for at least the last ten years. For that reason, SFWMD and Acme has referred to modification as being only "on paper." As reflected in Finding 23(e), supra, water control structures 115 and 117 would be modified in association with this permit modification so that structure 115 (located in the C-4 canal adjacent to Peacock Pond) will have a weir crest elevation of 12' NGVD and structure 117 (located adjacent to the C-6 canal) will have a weir crest elevation of 13' NGVD. As a result, when the water level in WCPPUD exceeds 12' NGVD, it would begin to "bleed down" out of structure 115 in the C-4 canal. If the water level in WCPPUD continued to rise and reached 13' NGVD, it would begin to "bleed down" out of the 117 structure in the C-6 canal as well. Under the proposed permit modification, the pump operation schedule would be revised so that no pumping would occur until Basin B stages reached 13' NGVD. Then, the pump rate will average 30,000 gpm, which equates to a "bleed down" discharge of 20 percent of the one-inch detention above 12' NGVD per day. When the stage has been brought down to 12' NGVD, all pumping would cease. During significant storm events, when the internal stages exceed 13' NGVD, the previously permitted peak discharge rate of 220,000 gpm will be maintained. If the pumps are operated as proposed in this modification, the system will be able to take full advantage of its nutrient removal capacity. At the same time, water levels will be maintained within the ranges of historical operation over at least the last ten years. The only difference is that, except for major storm events, water levels will be allowed to "bleed down" at a slower rate. Notwithstanding these facts, Petitioners believe that control elevations in WCPPUD have always been higher than in Basin B, and are concerned that the proposed "on paper" modification is in the nature of a "smoke and mirrors" trick. Petitioners are concerned the proposed modifications will cause additional water to be detained in WCPPUD to the detriment of the equine industry there. But the evidence indicated that the their concerns are not well-taken. Under the proposed modification, there will be one inch of detention over the entire Basin B water management system between the elevations of 12' NGVD and 13' NGVD. This is the same range of elevations established for WCPPUD in the 1979 SWM permit. The calculated detention volume accounts for the volume of water which is physically accommodated in the system between 12' NGVD and 13' NGVD. There is no additional detention created in the WCPPUD system through the proposed changes. The proposed Basin B pump schedule will result in the same range of water table fluctuation as required in the 1979 SWM permit. As Petitioners' witness, Mr. Straub, testified, the system has worked well as operated for the last three years. No significant changes are to be expected as a result of the proposed pump operation schedule changes designed to achieve greater water quality treatment benefits. In combination, the modification of the pump operation schedule for Basin B and the revisions to the WCPPUD system are expected to result in an improvement in flood control with lower flood stages within WCPPUD through a more efficient water management system. Acme has demonstrated that the proposed modifications will not result in a change in actual water control elevations on Petitioners' properties; will not cause water to back up and cause flooding or septic tank problems within WCPPUD; and will comply with Florida Administrative Code Rule 40E-4.301(1)(a), (b), and (c.) The undisputed expert testimony was that Acme gave reasonable assurances that the proposed permit modification will not "lower existing water table elevations." (Emphasis added.) Fla. Admin. Code R. 40E-41.363(4). Equivalent Water Quality Treatment Provided Acme provided calculations comparing the treatment which was assumed to take place within the originally permitted surface water management system of WCPPUD (which included Peacock Pond), the treatment which is currently being provided by the existing system, and the treatment that will be provided under various assumed future scenarios. Acme demonstrated that there will be an equivalent amount of water quality treatment even though the use of Peacock Pond as a water quality retention area is being eliminated. Petitioner did not provide any contrary evidence to show that the removal of Peacock Pond reduced water quality treatment in the system. As a result, reasonable assurances were given that there will be no adverse effect on the quality of receiving waters as a result of this proposed modification. Additional Wet Detention Areas Now Exist Although the 1979 permit required only 12 acres of wet retention ponds, analysis of aerial photographs and existing permits issued after 1979 indicates that 54.4 acres of wet detention lakes meeting current regulatory criteria now exist in WCPPUD. Another 33 acres of existing wet retention areas (including canals) are present but do not meet the minimum width criteria required for wet detention ponds. Approximately another 4 acres meet the dimensional requirements but are not legally encumbered for use by Acme for water quality purposes. For example, Lakes 6 and 8 meet the dimensional criteria but are not platted as water management areas or encumbered by suitable drainage easement. A similar situation exists with Lake 9, which has been assumed to provide wet detention treatment over only 15.41 acres since the northern 2.25 acres of the 17.66-acre lake are outside the platted water management area's footprint. If all lakes, ponds, and canals within WCPPUD were counted for water quality purposes, Acme calculated that there would be enough capacity to treat approximately one inch of runoff from WCPPUD. Not counting the water bodies not meeting dimensional requirements or not legally encumbered, but assuming that future development within WCPPUD will have 13% water bodies qualifying for use as wet detention areas under current criteria, Acme calculated that there would be capacity to treat one inch runoff from current and future development within WCPPUD. (Instead of 13 percent qualifying wet detention areas, alternative equivalent water quality treatment also could be used to meet applicable water quality treatment criteria.) Planted Filter Marsh Located in C-2 Canal Provides Additional Water Quality Treatment Phosphorus loading can be described as the pounds of phosphorus which are being discharged to a water body through storm water runoff. In WCPPUD today, phosphorous loading is higher than originally anticipated and calculated when the 1979 Permit was issued due to differences in the way the land has been developed over the last 20 years. The main difference is more equestrian activity and its higher phosphorus loading than anticipated in 1979. Acme submitted detailed phosphorus loading information which is included in Exhibits 7A through 7E to the Staff Report (SFWMD Exhibit 5), comparing what the original permit anticipated to what is happening today, and what would happen with the modified system. The detailed information is summarized on Exhibit 8 to the Staff Report. To address phosphorus loading, the proposed project includes construction of a 7.8-acre filter marsh within a portion of the Acme C-2 Canal right-of-way located within Basin B about a half mile west of WCPPUD. The project will extend from the intersection of the C-2 and C-23A canals southwards approximately 6,800'. The filter marsh will treat water flowing south through the C-2 canal prior to reaching the Acme pump stations discharging into the Refuge. The existing Acme C-2 canal will be expanded to a width of approximately 80' to 130' and will incorporate a meandering 40' to 60' wide constructed and planted littoral shelf at elevation 10.0' NGVD. Adjacent to the proposed littoral zone, a 25' wide section of the canal will be excavated to an elevation of approximately 6.0' NGVD. This deeper section is proposed to prevent any reduction in hydraulic capacity of the existing C-2 Canal. The 7.8-acre area will be planted with native wetland vegetation on three centers. It is anticipated that the planted vegetation will meet or exceed the eighty percent coverage requirement within two years; however, additional plants will be installed if the area fails to meet such expectations. Monitoring will occur on a monthly basis until the filter marsh achieves a 50 percent areal coverage of desirable planted and recruited wetland vegetation. Upon attainment of the 50 percent coverage criterion, the monitoring frequency will be reduced to four times per year for a period of three years. Subsequent maintenance and monitoring events will occur semi- annually. Should exotic infestation occur, herbicide and/or hand clearing will be utilized to bring the filter marsh into compliance with desired plant specie densities. Special Condition No. 12 of the Staff Report (SFWMD Exhibit 5) requires that the Acme adhere to the filter marsh maintenance plan. The proposed littoral zone construction is expected to be initiated within six months of permit issuance and completed within six months of commencement. The pollutant loading/removal spreadsheets provide an estimate that the marsh will result in the annual removal of 33 pounds of total phosphorus. At the same time, the proposed filter marsh will add the equivalent of one-half inch of water quality treatment benefits within the entirety of Basin B. As a result, with the proposed filter marsh, Acme gave reasonable assurances that the proposed permit modification would provide "an additional fifty (50) percent retention/detention water quality treatment addition to the water quality treatment volumes required in section 5.2.1. of the Basis of Review [for projects within a Water Protection Area or Area Basin]." Fla. Admin. Code R. 40E-41.363(5). Approximately half of the proposed filter marsh will extend north of the east/west C-24 Canal, and half will extend south of it. The northern half will treat water from an area of relatively intense equestrian use just west of WCPPUD; the southern half will continue to treat water flowing through the northern half of the filter marsh. However, the southern half also will treat some water from the C-4 and C-6 canals in WCPPUD, which flows south to the C-24 and then west to the C-2. Exhibit 9B of the Staff Report (SFWMD Exhibit 5) delineates the assumed contributing area of 960 acres. BMPs Provide Improvements in Water Quality Best Management practices (BMPs) are water quality treatment operational practices to prevent pollutants from ultimately entering the receiving water body. BMPs are also often referred to as source controls. Examples of BMPs include street-sweeping and cleaning out storm gutters to control pollutants at their source. BMPs are commonly considered in ERP permitting. The Village of Wellington has mandated a BMP program in Basin B, including: an ordinance dealing with phosphorus and water quality improvement; an ordinance regulating the application of fertilizer, requiring no more than two percent phosphorus content; and an equestrian BMP requiring equestrian residuals, commonly known as manure, be collected and contained in concrete covered bins. Historically, horse manure was stockpiled in the open and exposed to rainfall. Stormwater runoff from the stockpiled manure often flowed directly into the Acme canals. Stormwater runoff from equestrian residuals has been a major contributing factor to the amount of phosphorus being discharged to the Everglades from Basin B. The Village of Wellington also is implementing BMPs for its own canal maintenance and for cleaning phosphorous-laden sediments from its canals. The calculations provided to SFWMD by Acme concerning BMPs do not assume an initial 100-percent compliance. Initially, a 20-percent compliance was assumed because the ordinances are fairly new. These BMPs were not in place when the 1979 permit was issued. Under the current application, it is expected that the BMPs throughout Basin B will significantly reduce the amount of phosphorus ultimately discharged through the two Acme pump stations to the Refuge. Although there is an increase in phosphorus loading from that anticipated in 1979, the BMPs, filter marsh, amendment to the pump operation schedule, comprehensive water quality monitoring plan, and other items in the modification offset the increase. (The modifications in the proposed permit are not designed to address the overall Basin B phosphorus problems.) Comprehensive Water Quality Monitoring Program SFWMD and the Village of Wellington have implemented a comprehensive water quality monitoring program with Basin B. This program includes existing and proposed sampling points within WCPPUD shown on Exhibits 2 and 9B of the Staff Report (SFWMD Exhibit 5). This permit modification requires that Acme continue this monitoring program as specified in Special Condition No. 11 to the Staff Report. Elimination of Existing Control Structure As stated in Finding 19, supra, a 1989 modification to the 1979 authorized construction and operation of a control structure allowing discharge from Lake No. 5 (as designated in Exhibit 2 of the Staff Report, SFWMD Exhibit 5) to the C-4 Canal, which was never built. Instead, as shown on Exhibit 2 of the Staff Report, the existing SWM system for Equestrian Estates discharges to the C-4 Canal well to the north of the authorized control structure via a 100' wide canal. The proposed permit modification will eliminate the authorization for the Equestrian Estates control structure which was never constructed. This revision is necessary to ensure that discharge from the development will continue to occur upstream of Structure 115, as it does today, and that the on- site detention facilities within Equestrian Estates will function as modeled in the water quality analysis. Polo's Pending Application for Peacock Pond Polo has pending a separate application to SFWMD (Application No. 020215-10) requesting authorization for development of Peacock Pond as a polo field. Polo’s proposed water quality feature for its Peacock Pond polo fields development includes a lake on the north end of Peacock Pond. It appears that the lake would utilize lakes/canals 12 and 13, which are currently located at the north end and northeast corner of Peacock Pond, essentially enlarging those lakes/canals to the south and west into Peacock Pond. Polo's application is currently incomplete and fails to address a number of significant water resource issues. SFWMD mailed an initial Request for Additional Information (RAI) to Polo on March 15, 2002. Responses were due within thirty days. As of the date of the final hearing in this case, no response to the initial RAI had been submitted. Notwithstanding its pending application, Polo professes to believe that its undeveloped properties in WCPPUD are "vested," so that Polo should not be required to provide water quality treatment when developing its properties in the future. But the 1979 permit stated that it only permitted construction in certain parts of WCPPUD and that individual permit modifications would be required for the future development of additional phases. (SFWMD Exhibit 2 at p. 1; special conditions.) All "grand fathered" development already has taken place. No evidence or convincing legal argument was presented by Petitioners for the proposition that land owners seeking to develop their properties in Wellington WCPPUD now or in the future should be "vested" and thus subject to different water management regulations than other land owners seeking to develop their properties in Acme Basin B. SFWMD's Proposed Corrections to Staff Report At the Final Hearing, SFWMD suggested that two corrections be made to the Staff Report. The first would add "Section No. 20" on page 1 of the Staff Report (SFWMD Exhibit 5) to clarify the property is actually located in sections 20 and This type of change would be made administratively even without this proceeding. The other correction is proposed on page 4 of the Staff Report (SFWMD Exhibit 5), pertaining to the description of the water elevation within Basin B and Country Place, as follows: The water elevation within Basin B and Country Place was originally permitted with a wet season control elevation of 12.0' and a dry season control of 13.0' NGVD. The minimum road and finish floor elevations were established at elevation 16.0' and 17.0 NGVD, respectively. The water elevation within Basin B was permitted in 1978 with a schedule stage of 13' NGVD in the wet season and 13' NGVD in the dry season; however, the system has historically been operated with a control elevation of 12' NGVD in the wet season and 13' in the dry season. WCPPUD was originally permitted with a wet season control elevation of 12' NGVD and a dry season control elevation of 13' NGVD. The Country Place pump station discharging into Peacock Pond was to begin operation when water elevations reached 13' NGVD and discontinue when the system was drawn down to elevation 12' NGVD. The operational elevations authorized in this staff report are consistent with those authorized in 1979 for Country Place. The 1978 permit also established a minimum road grade elevation of 16' NGVD and a finished floor elevation of 17' NGVD for Basin B. The 1979 permit for Country Place established the same minimum road grade and finished floor elevations. This correction accurately describes the 1978 permit for Basin B; it is not a substantive change. These and other possible changes to the Staff Report were drafted shortly before the final hearing in the form of an "Addendum to Staff Report." Petitioners contended that this denied them due process. However, this Addendum (which was not introduced into evidence) was presented to propose corrections to minor errors in the original Staff Report and to suggest appropriate ways to address issues raised by Petitioners during prehearing procedures in this case in order to help clarify the intention of the Staff Report for Petitioners' benefit. SFWMD offered to withdraw the latter Addendum proposals if Petitioners so wished; Petitioners declined to request that these proposals be withdrawn, but none are considered to be necessary. Other Contentions Raised By Petitioners Alleged Elimination of Petitioners' Water Treatment Facilities Petitioners contended in their Second Amended Petition that the modification will cause "33 acres of previously permitted and constructed water management facilities to no longer be considered toward meeting water quality treatment." But the 33 acres referenced by the Petitioners were never counted for water quality treatment in the previous permits. Additionally, as discussed above, they do not meet the minimal dimensional criteria or have not been encumbered for water quality purposes. See Finding 41, supra. The only surface water management facility which has a change in its permitted status for water quality treatment is Peacock Pond. Future Development is Not Precluded from Proposing Alternative Water Quality Treatment Petitioners expressed a concern that the proposed permit modification would bind future development to the Acme's design assumptions--specifically, the assumption that, in order to meet SFWMD's criteria for new development, future development projects would include 13 percent lakes. This concern seems to spring primarily from the following statement on page 3 of 21 of the Staff Report (SFWMD Exhibit 5): "This permit modification requires that applicants adhere to the stated surface water management system assumptions for all future development." Reading the Staff Report as a whole, it was reasonably clear that Acme's assumption was made only for purposes of its permit modification application and would not bind future developers in WCPPUD. Rather, future applicants may propose any alternative methods that comply with Chapter 40E-4, Florida Administrative Code, and the BOR to demonstrate compliance with water quality requirements. For example, the Staff Report states on page 13: Future Country Place applicants are not precluded from proposing alternative means of treatment which can be demonstrated to provide an equivalent level of treatment. Further, the assumptions do not preclude the SFWMD from requiring additional treatment measures as necessary from an applicant to provide reasonable assurance that future projects will not cause or contribute to existing water quality problems in Basin B. The testimony of SFWMD witnesses confirmed this reading of the Staff Report. There is no need to further modify the Staff Report to allay Petitioners' expressed concern. Canals/Lakes 12 and/or 13 Not Affected Petitioners' Second Amended Petition questioned whether Acme's canals/lakes 12 and 13, which border Peacock Pond on the north and in the northeast corner, are properly located within Acme's easements. But Acme's application proposes no modifications to those canals/lakes. Not only are canals/lakes 12 and 13 not the subject of this permit modification, Petitioners introduced no competent, substantial evidence demonstrating improper placement of those conveyance features. In an abundance of caution, SFWMD suggested adding the following Special Condition Number 14 to address this issue: If a final determination is made by a court of competent jurisdiction that Acme does not own, have an easement or otherwise have the right to utilize the area where canal/lake Number 12 and/or canal/lake Number 13 is located, then within 30 days of such determination, Acme shall file an application with the SFWMD to move the canal/lake Number 12 and or canal/lake Number 13 to an area which is determined to be owned by Acme or over which Acme has an easement, or modify the surface water management system to discontinue use of canal/lake Number 12 and or canal/lake Number 13. Inclusion of this language would confirm that, if a court makes a final determination that Acme does not have the right or access to utilize Canals/Lakes Number 12 and/or 13, Acme would be required to modify the permit. While adding the suggested language to the Staff Report is appropriate, it is not necessary; reasonable assurances have been provided without any additional language that the permit criteria have been satisfied. If canal/lakes 12 and 13 should ever become unusable, thus preventing a discharge of the eastern half of WCPPUD into the C-4 canal, the drainage system could be split so that the western half discharges into the C-4 canal and the eastern half into the C-6 canal. In that case, a minor modification would be required to lower the weir at structure 117 to 12’ NGVD and the permit is modified. Mr. Higgins performed calculations to demonstrate that such a minor modification would be permittable under applicable criteria.4 Wetlands in Pod F Not Adversely Affected The Staff Report includes reference to wetlands located in the southeast corner of Pod F of WCPPUD. (Pod F itself is in the southeast corner of Section 20.) Petitioners seemed to take issue with the Staff Report's description of these wetlands. They also disputed whether Acme provided reasonable assurance that these wetlands would not be adversely affected by the proposed modifications. Specifically, Polo expressed concern that the proposed modifications would undermine a plan it has to restore wetlands in Pod F for use as mitigation for an after-the-fact permit to be issued to resolve a SFWMD cease and desist order imposed on Polo for activities in an adjacent polo field, and perhaps also as mitigation for wetland impacts by Polo and other future developers in the area. In taking these positions, Petitioners criticized SFWMD for not presenting expert testimony from a biologist. The Staff Report states that "the 3.74-acres of cypress wetland contained within Pod F" are the only other wetlands in WCPPUD besides Peacock Pond. These wetlands were described as being "in poor biological condition." Petitioners argued that the testimony of their expert supported a finding that the wetlands in Pod F actually are approximately 25 acres in size. However, her actual testimony was that her proposed wetlands restoration project was 25 acres in size. Part of her proposed restoration project includes the "vertical relocation" of higher ground now infested with melaleuca and other nuisance and exotic species. In addition, she admitted that she had not delineated wetlands in Pod F using the methodology adopted for that purpose by the State of Florida; instead, she used methodology adopted by the United States Army Corps of Engineers was used. Not only are the two methodologies different, the Army Corps methodology includes wetlands not included under the State of Florida methodology. Finally, Petitioners' expert admitted that less than 4 acres of the 25 acres included in her project area consisted of "cypress heads." Taken as a whole, the evidence did not demonstrate a need to revise the Staff Report's description of the size of the wetlands in Pod F. As for the Staff Report's description of the Pod F wetlands' "poor biological condition," this is consistent with the testimony of Petitioners' expert. She testified that the wetlands' hydrology was deficient, especially on the northern half of the restoration project area, and that the tract is "highly infested with exotic vegetation," leading to the need for restoration. The hydrology is better on the southern half of the restoration project area, where the cypress trees are healthy; but the cypress trees on the northern half of the tract are under stress, with lots of old world climbing vines on them and other infestation of exotic vegetation, including melaleuca. On site visits, the expert saw "wading birds, snakes, signs of raccoon [and n]umerous bird species." No endangered or threatened species were said to be using the tract at this time. One purpose of the restoration project would be to create better wildlife habitat. Petitioners' expert testified that if water levels were lowered in the proposed restoration project area, there could be an adverse impact on existing and planned wetlands. However, Petitioners' expert did not have evidence or information indicating historic or current water levels. Petitioners' expert also did not know whether the permit modification will lower or have any affect on the water levels in that area. Petitioners introduced neither competent evidence of current groundwater levels under the proposed wetlands mitigation project, nor competent evidence as to how the permit modification might change those groundwater levels. Acme and SFWMD presented evidence that the water levels in the C-4 and C-23 canals, directly adjacent to Pod F, will not be changed significantly as a result of the permit modification; that the proposed permit modification will have no effect on the groundwater levels in this wetland area; and that, as a result, no wetland impacts will occur from the permit modifications. Petitioners did not rebut the Respondents' evidence. As a result, Acme has demonstrated that not only groundwater and surface water flows and levels but also the value of wetland functions in Pod F will not be adversely impacted, as required by Rule 40E-4.301(d) and (g), Florida Administrative Code. The evidence was that SFWMD biologists visited the Pod F wetlands and prepared a report which formed the basis of statements in the Staff Report about the absence of wetland impacts. Given the finding that groundwater levels in the Pod F will not change, the testimony of expert biologists was not necessary. Assumed Commercial Acreage Through the testimony of Michael Nelson, Petitioners questioned a purported statement in the Staff Report that there are 24.4 acres of commercial acreage in WCPPUD. According to Mr. Nelson, there actually are only five acres of commercially zoned property in the PUD. Mr. Nelson stated that this, along with other alleged errors, undermine his confidence in SFWMD's entire evaluation of the proposed permit modification. In fact, the Staff Report, at page 8, states that "the original permit application (in 1979) included only two land uses: 935.6 acres of single family use . . . and 24.4 acres of commercial area." There was no statement that 24.4 acres is zoned commercial today. Past Violations Petitioners also assert that the proposed permit modification should be denied because Acme has not strictly abided by applicable permits. But Acme's most significant past violation was the failure to operate Peacock Pond as required by the 1979 Permit. As reflected in Findings 21 and 23, supra, the primary purpose of this proposed modification is to resolve the enforcement proceedings that arose out of the Peacock Pond violation. Acme also has been one of thousands of SFWMD permit holders who have not certified construction of their systems in conformance with the applicable permits, which is required to transfer the permit into operational status. For many years, SFWMD did not monitor permits for certification and did not enforce failure to certify permits. When monitoring and enforcement was initiated in 1995, it was found that over 12,000 permits were in violation for failure to submit the required certifications. SFWMD prioritized the missing certifications and began methodical follow-up. When SFWMD raised the issue with Acme, Acme responded, and the outstanding violations are being resolved. SFWMD saw no need to initiate formal enforcement proceedings and has been treating the outstanding violations as a "non-compliance" issue since it is a paperwork problem, not an environmental resource problem. At this time, the modifications to structures 115 and 117 in accordance with the several emergency authorizations to address septic tank problems have been certified. However, as indicated, the 1979 Permit itself cannot be certified so long as the Peacock Pond pumped retention area is not in place and operational. It is found that Acme has sufficient financial, legal, and administrative capabilities to ensure that water management modifications will be undertaken in accordance with the terms and conditions of the modified permit. (Since Acme is now a dependent special district of the Village of Wellington, the Village of Wellington actually will be responsible for installation, operation, and maintenance of these structures.) Notwithstanding the past violations, reasonable assurances have been given that Acme will comply with the terms of its proposed permit modification. Propriety of Petitioners’ Purpose Acme has raised the issue whether Petitioners participated in this proceeding for an "improper purpose," i.e., "primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of licensing or securing the approval of an activity." § 120.595(1)(e)1, Fla. Stat. (2003). But it is found that, under the totality of circumstances, Petitioners' participation in this proceeding was not for an improper purpose, as defined by statute. Petitioners' participation in this proceeding has indeed needlessly increased Acme's cost of obtaining SFWMD's permit approval; but the evidence did not prove that this was Petitioners' primary purpose. It also is clear that Petitioners attempted to delay this proceeding through repeated requests for continuances (and other procedural and evidentiary objections) and that, while they usually based their requests for continuances in part on the alleged need for more time for more discovery, they failed to pick up voluminous copies of requested discovery documents and complained about how much money they had already spent on discovery. Nonetheless, it is found that Acme did not prove that Petitioners' primary purpose for participating in this proceeding was to delay the proceeding. It seems reasonably clear that, had Petitioners retained a competent expert engineer to evaluate its case, the expert probably would have advised Petitioners that they would not be able to successfully challenge SFWMD's proposed agency action. For that and other reasons, a reasonable person would not have raised and pursued some of the issues raised by Petitioners in this proceeding. But it cannot be found that all of the issues they raised were frivolous or that their participation in this proceeding was for an improper purpose.
Findings Of Fact As planned, Phase I of Foxwood Lake Estates will consist of 300 mobile homes, which would require treatment of up to 45,000 gallons of sewage per day. The proposed sewage treatment plant would have a capacity of 46,000 gallons per day and would be capable of expansion. It would discharge treated, chlorinated water into a completely clay-lined polishing pond that has been designed for the whole of Foxwood Lake Estates at build-out; capacity of the polishing pond would be three times the capacity necessary for Phase I by itself. From the polishing pond, water is to flow into one or both of two evaporation-percolation ponds, either of which would be big enough for all the sewage expected from Phase I. The sides of these ponds would be lined with clay and a clay plug would constitute the core of the dike on the downslope side of each pond. According to the uncontroverted evidence, effluent leaving the treatment plant for the polishing pond would have been effectively treated by the latest technology and would already have been sufficiently purified to meet the applicable DER water quality requirements. The applicant proposes to dig the triangular polishing pond in the northwest corner of the Foxwood Lake Estates property, some 400 feet east of the western property line. The evaporation-percolation ponds would lie adjacent to the polishing pond along an axis running northwest to southeast. Their bottoms would be at an elevation of 164.5 feet above mean sea level and they are designed to be three feet deep. The evaporation-percolation ponds would lie some 300 feet east of the western property line at their northerly end and some 400 feet east of the western property line at their southerly end. A berm eight feet wide along the northern edge of the northern evaporation-percolation pond would be 50 feet from the northern boundary of the applicant's property. Forrest Sawyer owns the property directly north of the site proposed for the evaporation-percolation ponds. He has a house within 210 feet of the proposed sewage treatment complex, a well by his house, and another well some 300 feet away next to a barn. Two or three acres in the southwest corner of the Sawyer property are downhill from the site proposed for the ponds. This low area, which extends onto the applicant's property, is extremely wet in times of normal rainfall. Together with his brother and his sister, Charles C. Krug owns 40 acres abutting the applicant's property to the west; their father acquired the property in 1926. They have a shallow well some 100 feet from the applicant's western property boundary, and farm part of the hill that slopes downward southwesterly from high ground on the applicant's property. Sweetgum and bayhead trees in the area are also a money crop. Charles C. Krug, whose chief source of income is from his work as an employee of the telephone company, remembers water emerging from this sloping ground in wet weather. Borings were done in two places near the site proposed for the ponds. An augur boring to a depth of six feet did not hit water. The other soil boring revealed that the water table was 8.8 feet below the ground at that point. The topsoil in the vicinity is a fine, dark gray sand about six inches deep. Below the topsoil lies a layer of fine, yellow-tan sand about 30 inches thick. A layer of coarser sand about a foot thick lies underneath the yellow-tan sand. Beginning four or five feet below the surface, the coarser sand becomes clayey and is mixed with traces of cemented sand. Clayey sand with traces of cemented sand is permeable but water percolates more slowly through this mixture than through the soils above it. The applicant caused a percolation test to be performed in the area proposed for the ponds. A PVC pipe six feet long and eight inches in diameter was driven into the ground to the depth proposed for the evaporation-percolation ponds and 50 gallons of water were poured down the pipe. This procedure was repeated on 14 consecutive days except that, after a few days, the pipe took only 36 gallons, which completely drained into the soil overnight. There was some rain during this 14-day period. Extrapolating from the area of the pipe's cross-section, Vincent Pickett, an engineer retained by the applicant, testified that the percolation rate of the soils was on the order of 103 gallons per square foot per day, as compared to the design assumption for the ponds of 1.83 or 1.87 gallons per square foot per day. Water percolating down through the bottoms of the evaporation- percolation ponds would travel in a southwesterly direction until it mixed with the groundwater under the applicant's property. It is unlikely that the ponds would overflow their berms even under hurricane conditions. Under wet conditions, however, the groundwater table may rise so that water crops out of the hillside higher up than normal. The proposed placement of the ponds makes such outcropping more likely, but it is impossible to quantify this enhanced likelihood in the absence of more precise information about, among other things, the configuration of the groundwater table.
Recommendation Upon consideration of the foregoing, it is RECOMMENDED: That DER grant the application on the conditions specified in its notice of intent to issue the same. Respectfully submitted and entered this 17th day of December, 1980, in Tallahassee, Florida. ROBERT T. BENTON, II Hearing Officer Division of Administrative Hearings Room 101, Carlton Building Tallahassee, Florida 32301 Telephone: 904/488-9675 FILED with the Clerk of the Division of Administrative Hearings this 17th day of December, 1980. COPIES FURNISHED: Andrew R. Reilly, Esquire Post Office Box 2039 Haines City, Florida 33844 Walter R. Mattson, Esquire 1240 East Lime Street Lakeland, Florida 33801 David M. Levin, Esquire Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32301
The Issue The issue is whether Respondent Department of Environmental Protection may issue to Respondent Tampa Bay Water a variance from the requirements, in Rules 62-555.520(4)(c) and (d), Florida Administrative Code, that an application for a permit to construct and operate a drinking water system contain drawings of the project with sufficient detail to describe clearly the work to be undertaken and complete specifications of the project to supplement the drawings.
Findings Of Fact Inception of Tampa Bay Water, Consolidated Permit, and Other Documentation for the Production of Drinking Water Respondent Tampa Bay Water (TBW) is a wholesale public water supply utility. TBW is governed by a nine-member board of directors with one member each from the municipalities of Tampa, St. Petersburg, and New Port Richey and two members each from the counties of Hillsborough, Pinellas, and Pasco. The purpose of TBW is to use group resources to find regional solutions to the problems of water supply in the region. Over two million persons in the three-county area rely on TBW for their drinking water. The predecessor of TBW was the West Coast Regional Water Supply Authority (WCRWSA), which was created in 1974. The West Coast Regional Water Supply Authority was also a wholesale public water supply authority. However, the authority operated as a cooperative entity, and TBW operates as a regulatory entity. In 1996, WCRWSA sought to renew its permit from Intervenor Southwest Florida Water Management District (SWFWMD) to allow continued withdrawals from four of its eleven major wellfields. Concerned with the environmental impacts, such as drawdowns of the water levels of wetlands, streams, and lakes, from the environmental, if not regulatory, overpumping of the wellfields, SWFWMD denied the application for the quantities requested. An Administrative Law Judge at the Division of Administrative Hearings conducted a hearing and issued a recommended order finding adverse environmental effects from overpumping, but recommending that SWFWMD issue the requested permits subject to certain conditions. Subsequent negotiations resulted in the parties' entering into a series of agreements covering withdrawals from the four wellfields that had been the subject of the administrative hearing and seven more wellfields that were approaching repermitting (11 Wellfields), as well as a series of other matters. On May 20, 1998, WCRWSA, the three member counties, the three member municipalities, and SWFWMD entered into the Northern Tampa Bay New Water Supply and Ground Water Withdrawal Reduction Agreement (Partnership Agreement). The Partnership Agreement requires WCRWSA to bring one or more projects online, by December 31, 2002, to produce at least 38 million gallons per day (MGD) and, by December 31, 2007, to produce at least 85 MGD of new water supply. The Partnership Agreement requires SWFWMD to provide WCRWSA with $183 million toward eligible water supply projects. The Partnership Agreement notes that the then-current Master Water Plan of WCRWSA recognizes that "an aggressive conservation and demand management program is an integral component of a sustainable water supply." (Joint Exhibit 3, p. 31.) The Partnership Agreement notes that the then-current Master Water Plan states that the conservation program was expected to reduce use by 10 MGD per day by 2000 and 17 MGD by 2005. From the effective date of the agreement through December 31, 2002, the Partnership Agreement requires a reduction in pumping of the 11 Wellfields to 158 MGD, based on a rolling 36-month average. For the next five years, the Partnership Agreement requires a reduction in pumping of the 11 Wellfields to 121 MGD, based on an annual average. After that, effective December 31, 2007, the Partnership Agreement requires a reduction in pumping of the 11 Wellfields to 90 MGD, also based on an annual average. Three weeks after the execution of the Partnership Agreement, WCRWSA was reorganized into TBW in June 1998 through the execution of two documents: an Amended and Restated Interlocal Agreement dated June 10, 1998 (Interlocal Agreement), and a Master Water Supply Contract dated June 10, 1998. TBW assumed WCRWSA's rights and responsibilities under the Partnership Agreement. The Interlocal Agreement empowers TBW to produce and supply drinking water "in such manner as will give priority to reducing adverse environmental effects of excessive or improper withdrawals of Water from concentrated areas." (Joint Exhibit 1, pp. 20-21.) The Interlocal Agreement incorporates the phased-in reductions in withdrawals from the 11 Wellfields that are set forth in the Partnership Agreement. The Interlocal Agreement notes that, if the Partnership Agreement provides for extensions of the deadlines, the deadlines contained in the Interlocal Agreement shall likewise be subject to extension. Applying to the 11 Wellfields, SWFWMD issued TBW a Consolidated Permit, which was issued on December 15, 1998, and became effective on January 1, 1999. Complementing the Partnership Agreement, which reflects SWFWMD's resource- development role, is the Consolidated Permit, which reflects SWFWMD's regulatory role. The Consolidated Permit incorporates the phased-in reductions of withdrawals, as set forth above, for the 11 Wellfields. Although the deadlines for phased-in reductions are conditioned on the funding to be provided by SWFWMD, pursuant to the Partnership Agreement, these deadlines are otherwise unconditional and firm. The Consolidated Permit expressly provides for extensions of deadlines, except the deadlines set for the phased-in reductions of withdrawals from the 11 Wellfields. The Consolidated Permit imposes upon TBW extensive responsibilities regarding environmental monitoring, reporting, and mitigation. These responsibilities extend to groundwater, wetlands, and surface waters, as TBW must, among other things, monitor and report levels in the surficial and Floridan aquifers and potentiometric surfaces in the Floridan aquifer in the vicinity of the 11 Wellfields, as well as in the vicinity of selected wetlands and surface waters. The Consolidated Permit sets specific "regulatory levels" for these resources. Present and Future Tampa Bay Water Facilities, Including the Surface Water Treatment Plant A majority of TBW's production facilities consists of the 11 Wellfields. In an effort to supplement these production sources so as to comply with the phased-in reduction deadlines set forth in the Consolidated Permit and other documents, TBW annually adopts a New Water Plan, which describes capital planning for drinking water production facilities. The June 2000 New Water Plan summarizes the requirements of the Partnership Agreement. The June 2000 New Water Plan notes that TBW reaffirmed its Master Water Plan and New Water Plan projects in April 2000. These projects include the Enhanced Surface Water System, which includes the Tampa Bay Regional Surface Water Treatment Plant (SWTP), Tampa Bay Reservoir Project (Reservoir), and projects obtaining water from the Alafia River, Hillsborough River, and Tampa Bypass Canal. Other projects, besides the Enhanced Surface Water System, include Seawater Desalination (Desal Plant). The June 2000 New Water Plan states that the Enhanced Surface Water System is eligible for a maximum of $120 million from SWFWMD, pursuant to its funding obligation under the Partnership Agreement. This case involves the means by which the SWTP will be permitted, and, in consideration of the manner of permitting, this case involves the means by which the SWTP will be designed and constructed. The June 2000 New Water Plan notes that TBW and USFilter Operating Services, Inc. (USFilter) have entered into a contract for the latter to design, build, and operate (DBO) the SWTP (DBO Contract). The June 2000 New Water Plan reports that USFilter is currently constructing an access road to the site. Among current issues, the June 2000 New Water Plan describes this case, noting that TBW obtained a variance from Respondent Department of Environmental Protection (DEP) allowing a design, build (DB) approach to permitting the SWTP. The June 2000 Water Plan states that the present challenge "has the potential to delay the completion of the [SWTP] by an estimated 8 months, subsequently delaying delivery of the initial 22 mgd (dry weather conditions) of new surface water to the regional system until May 2003 and more likely final acceptance of the [SWTP] to September 2003." (Joint Exhibit 5, p. 4.) (The accuracy of this statement is open to debate because SWFWMD granted an environmental resource permit for the SWTP project only on June 27, 2000--before which no significant alteration of the land could have taken place.) In the meantime, the June 2000 New Water Plan predicts a water supply shortfall of 100,000 to 2 million gallons per day in the South-Central service area of Hillsborough County. Addressing the SWTP, the June 2000 New Water Plan states that TBW purchased the site in October 1999 and released a Request for Proposals on July 19, 1999. Four pre-qualified DBO teams responded on October 18, 1999. The June 2000 New Water Plan erroneously states that TBW applied for a public drinking water facility construction permit (Water Treatment Permit) in October 1999. Actually, in September or October, TBW prefiled with the Hillsborough County Health Department (Health Department) its application for a Water Treatment Permit and paid the $7500 filing fee. The purpose of this courtesy filing or prefiling was to allow Health Department representatives to examine the application, including drawings and specifications for the SWTP, and perhaps expedite the approval process, once TBW filed a formal application. The June 2000 New Water Plan reports that the SWTP will have a peak day, surface water treatment capacity of 60 MGD and will be located on a 433-acre site near U.S. Route 301 and Broadway Avenue in central Hillsborough County. The June 2000 New Water Plan states that the SWTP project schedule calls for completion of construction by March 2003 with plant startup and testing in May 2003 and final acceptance testing in September 2003. The June 2000 New Water Plan estimates that detailed design, site permitting, and construction of the SWTP will cost $84.3 million, and the annual operation and maintenance expenses will be $7.9 million. As for the Desal Plant, the June 2000 New Water Plan reports that TBW will pursue a design, build, own, operate, and transfer (DBOOT) approach to acquire a plant to produce, initially, 25 MGD and capable of expansion by an additional 10 MGD. The June 2000 New Water Plan states that this plant will cost a total of about $96 million in capital expenses and about $19 million annually to operate. Procurement of the Surface Water Treatment Plant Design, Build, Operate Contract and Basis of Design TBW issued a Request for Proposals (RFP) that invited base and alternative proposals for the SWTP. TBW hired Parsons Engineering Sciences to prepare a preliminary design of the SWTP, so as to assist in the preparation of the proposals; although offerors could use alternative designs to the Parsons base design, all proposals had to meet the performance standards specified in the RFP. After publishing the RFP in papers and technical journals and on the Internet, TBW was able to prequalify five teams of offerors. Four of the five prequalified offerors submitted proposals. TBW received a total of nine proposals because each offeror submitted a base proposal and one alternative proposal, and one offeror submitted a second alternative proposal. At its January board meeting, TBW selected the USFilter proposal. No party filed a bid protest to the specifications of the RFP or the selection of USFilter and its team. After the selection of USFilter, TBW entered into negotiations with USFilter. During this process, USFilter agreed, at its expense, to add sand to the granulated activated carbon filters to remove fine particles more efficiently, even though it cannot recover the resulting cost of $1.5 million before or after the commencement of operations. TBW and USFilter entered into the DBO Contract on April 10, 2000 (DBO Contract). The DBO Contract identifies "Design Requirements" that "are intended to include the basic design principles, concepts and requirements for the [c]onstruction . . but do not include the detailed design or indicate or describe each and every item required for full performance of the physical [c]onstruction . . .." (Joint Exhibit 23, Section 1.2.6.) The "Design Requirements" are Schedule 6 to the DBO Contract. Schedule 6 contains all of the individual, technical specifications for the SWTP. Schedule 6 occupies two of the four volumes of large, three-ringed binders forming the DBO Contract. The DBO Contract identifies USFilter, Clark, and Camp Dresser & McKee, Inc. (Camp Dresser) as the DBO team for the SWTP project. Camp Dresser is providing design services, Clark is performing the construction, and USFilter is providing the operation and maintenance services for at least 15 years, as well as the financial guarantee, through its corporate parent. The DBO Contract provides TBW with a fixed construction cost, fixed operating costs, and guaranteed finished water quality. Schedule 8 assures that finished water quality will meet all applicable state and federal drinking water quality standards. Two witnesses at the hearing testified that TBW exacted from USFilter assurances of water quality that, as to certain parameters, will exceed applicable state and federal drinking water quality standards. The DBO Contract provides TBW with a firm completion date, subject to design modifications requested by TBW and uncontrollable circumstances, such as acts of God, raw water whose quality exceeds the maximum limits, or the delay caused by this case. A key document in this case is the Basis of Design Report (Basis of Design), which was prepared by the DBO team in April 2000. Acknowledging the phased-in withdrawal limitations and potential for fines for not meeting the deadlines set forth in the Consolidated Permit, the Basis of Design describes the purpose of the DBO process as follows: By utilizing the [DBO] approach for the [SWTP], [TBW] expects to secure substantial benefits . . .[,] includ[ing] costs savings, innovative design, reduced risk of schedule and cost excesses, long-term contracted facility operations, and maintenance efficiencies and guaranties. (Joint Exhibit 8, pp. 1-2.) The Basis of Design reports that the SWTP will be located on a 100-acre parcel within a 435-acre tract that will also accommodate facilities for groundwater treatment and storage of the treated groundwater, treated surface water from the SWTP, and treated saline water from the Desal Plant. The Basis of Design identifies the sources of raw water for the SWTF as the Tampa Bypass Canal, Hillsborough River, and Alafia River. Once online, the reservoir will help normalize quantities of available raw water throughout the dry season. The Basis of Design describes the main treatment process as pretreatment, including pH adjustment with sulfuric acid or caustic soda, powdered activated car feed, and ferric sulfate coagulant addition; coagulation, flocculation, and sedimentation using a high-rate ballasted sedimentation process known by its tradename as ACTIFLO; ozonoation for primary disinfection, taste and odor control, and partial conversion of dissolved organic carbon to an assimilable or biodegradable form; biologically active filtration for turbidity reduction, taste and odor control; reduction of biodegradable organic carbon; and post-treatment, including secondary disinfection using chloramines. The finished water will then be pumped into tanks for storage and blending before release into the distribution facilities. Distinguishing the DB process from the typical design, bid, build (DBB) process, the Basis of Design states: a very significant amount of process studies and pre-engineering was performed by the Project Team in support of its [DBO p]roposal. This work included a set of drawings covering all disciplines and developed to the 25 to 30 percent completion stage at a minimum with some drawings developed to a greater degree. This stage of drawing development is significantly beyond the sketches and diagrams usually provided in Basis of Design or Preliminary Design Reports. For this [Basis of Design,] the referenced drawings are attached and should be examined when reviewing this [Basis of Design]. As such, a relatively small number of figures are contained within this [Basis of Design]. (Joint Exhibit 8, pp. 1-4.) The Basis of Design notes that the Project Team conducted "pilot-scale" studies of the chosen treatment processes using Lake Manatee raw water. The purpose of these studies was to validate the selected treatment processes, provide water quality data, and establish appropriate operating criteria, such as coagulant dosages. The Basis of Design addresses raw water quality issues. One table sets out values for 30 different water quality parameters for each of the three raw water sources. The Basis of Design discloses expected water quality data for 11 water quality parameters. Of particular interest are total nitrogen and total phosphorus because, as noted in the Basis of Design, the algal life-cycle increases dissolved organic carbon and nutrient concentrations in reservoir water, and the "severity of this problem is impossible to predict." (Joint Exhibit 8, pp. 2-4.) The expected water quality values for total nitrogen and total phosphorus, respectively, are, on average, 0.8 and 0.55 mg/L and, at maximum, 1.6 and 2.1 mg/L. Each of the three surface waters approaches the average values, but none approaches the maximum values, for total nitrogen. The same is true for total phosphorus for the Tampa Bypass Canal and Hillsborough River. However, for the Alafia River, total phosphorus is 2.09 mg/L, so the raw water from the Alafia River may present a substantial treatment challenge, as it exceeds even the maximum expected value for total phosphorus. An error in Table 2-4 in reporting the maximum and average values of manganese (either the maximum value should be 0.02 mg/L or the average value should be 0.001 mg/L) and the omission of a turbidity parameter expressed in NTUs precludes analysis of these water quality parameters. However, the other expected parameters appear to reflect the actual water quality of these three surface waters. Section 4 of the Basis of Design describes the facilities and design criteria for the SWTP. This section begins with site grading, roadways, yardpiping, and stormwater management and extends to detailed discussions of the pretreatment and treatment processes, including the ACTIFLO, ozone contactor, and biologically active filtration. Urgency of New Means of Producing Drinking Water The SWTP is the hub of a network of production, storage, transmission, and distribution facilities that TBW plans to bring online in order to meet the requirements and deadlines set forth in the Consolidated Permit and other documents. The urgency for bringing this component of these new facilities online as soon as possible is due to environmental reasons, as well as the financial and legal reasons set forth above. Overpumping of existing wellfields has drawn down water levels in surface waters and wetlands, to the detriment of the overall level of biodiversity supported by these natural resources. Some lakes have been down 10 years, and a few have been down 40 or 50 years. During the recent drought, the City of Tampa, which obtains water from the Hillsborough River, lacked adequate volumes of surface water from which to produce sufficient finished water to meet the demand of its customers. Not surprisingly, these supply problems are accompanied by record withdrawals from the 11 Wellfields. Withdrawals in May and June of this year were the highest monthly withdrawals on record--208 MGD and 175 MGD, respectively. If the drought continues and TBW continues to meet the demands of its customers, TBW's withdrawals from the 11 Wellfields will exceed the permitted 158 MGD, on a rolling 36-month average, by April 2001. Wellfield overpumping has stressed the groundwaters. Although surface waters respond to substantial rains in as little as a day or two, groundwater takes significantly longer to respond. The surficial water table is as much as 20 feet below ground level, and the Floridan Aquifer is even deeper. The surficial aquifer does not begin to respond to substantial rains for one week, and the Floridan Aquifer begins to respond in two to four weeks. The condition of the surficial and Floridan aquifers affects the Hillsborough River and Tampa Bypass Canal, which are significantly recharged by the surficial and, sometimes, the Floridan Aquifer. The Floridan Aquifer is especially important to the Tampa Bypass Canal, whose rock bed has been breached. During dry periods, the two aquifers are the primary sources of recharge for these two surface waters. The Alafia River is more confined, but gets water from the Floridan Aquifer through two springs at the head of the river. TBW has already made substantial gains through conservation and has met the goal of nearly 10 MGD for 2000. Over the next 20 years, maximum potential gains are expected to be no more than 74-94 MGD. Conservation will continue to play an important role in securing adequate drinking water supplies in the Tampa Bay area, but conservation, even in conjunction with reclaimed water, will not suffice, especially when future population growth in the area is considered. TBW also manages wellfield production efficiently. Under its Optimized Regulatory Operations Plan, TBW collects and analyzes wellfield data to determine which wellfield to tap, notwithstanding specific limits set by wellfield, in order to minimize environmental damage. The consumptive use permits issued to TBW for the surface waters that will provide raw water to the SWTP restrict the amounts and timing of the removals. Additionally, a hydrobiological monitoring program requires the collection and analysis of data to safeguard against adverse effects in the rivers and, downstream, in the estuary. The contractual deadline for delivery of the SWTP is September 30, 2002. The timeframe for bringing online the SWTP necessarily relies on acceptance testing in the wet season, during which 60-65 percent of the annual rain occurs. The wet season extends from mid June to the end of September. Acceptance testing of the SWTP is imperative toward the end of this period because this is when the water quality of the surface waters bears the highest levels of the contaminants. Thus, if delays postpone beyond the wet season the point at which acceptance testing can take place, the postponement will effectively be until the next wet season and, possibly, the end of the next wet season. Permitting the Design, Build Process for the Surface Water Treatment Plant General The DB process envisioned by TBW would essentially break into phases the process by which TBW would obtain the necessary Public Drinking Water Treatment Construction Permit (Permit). The Permit initially would be based on "30 percent plans," which reflect about a 30 percent level of effort toward the overall design work or 30 percent completion of all of the design work (30 Percent Plans). Generally, 30 Percent Plans mark the end of the preliminary design phase. Plans reflecting 30, 60 and 90 percent levels of effort are customary in DBB processes, as these are the stages at which owners typically review design work. In 30 Percent Plans, some items are designed to 100 percent and other items are not designed at all. However, 30 Percent Plans provide reasonable assurance that the designed system is constructable. In essence, the Permit initially would be a conceptual permit for the entire SWTP coupled with a construction permit for those components for which the design is already complete on the 30 Percent Plans. Construction of each remaining component of the SWTP would await subsequent permit modifications authorizing construction of that component. As noted above, the May 18, 2000, cover letter anticipates another interim permit, or permit modification, covering specific components, and then the final permit, or permit modification, covering the entire SWTP. The DEP district office in Orlando has substantial experience with permitting DB water treatment projects. From 1996-98, the DEP Orlando office has permitted four such projects for the Orlando Utilities Commission and one such project for the City of Kissimmee. One of the Orlando Utilities Commission projects was to construct a completely new water treatment plant. Based on the experience of the DEP Orlando office, DB permitting, when based initially on 30 Percent Plans, shortens and simplifies the permitting process. DB permitting eliminates, or at least postpones, the presentation of elements, such as electrical and HVAC, that are irrelevant to the permitting process; the elimination of elements irrelevant to permitting from the initial designs helps the regulator find the elements that are relevant to the permitting process. Also, the experience of the DEP Orlando office is that the DB process results in no more permit modifications for change orders than are typical of a conventional DBB process. The DB-approval process used by the DEP Orlando office is modeled after the DEP-permitting process for wastewater treatment plants. DEP rules allow DB permitting of these plants, which are similar in construction to water treatment plants. In fact, DEP is preparing to adopt rules to allow DB permitting of water treatment plants. Because the DEP Orlando office did not issue variances from the rules that arguably preclude DB construction of water treatment plants, there is no precedent for the issuance of the variance sought in this case. However, the experience of the DEP Orlando office is that applicants do not present basic design changes after the initial submission, and DB permitting does not mean that regulatory objectives are sacrificed to the expediency sought by the applicant. The Present Case On April 11, 2000, Camp Dresser, on behalf of TBW, filed with the Health Department an Application for a Public Drinking Water Facility Construction Permit. The April 2000 drawings that accompanied the April 11, 2000, application are described above. The cover letter to the Health Department notes that, "upon conceptual approval of the project, individual components will be permitted through permit modifications based on submittals of complete drawings and specifications for each component." In this case, the availability of the Basis of Design meant that the 30 Percent Plans reflected more than a 30 percent level of effort or completion of the five-stage process of pretreatment, pH adjustment, ozone contactors, filtration, and storage in tanks. The engineer had already sized the facilities and defined all of the processes and elements of the SWTP. The April 2000 drawings, as supplemented by the Basis of Design, therefore presented a relatively detailed description of the scope, elements, and processes of the project. On May 18, 2000, Camp Dresser submitted to the Health Department more advanced drawings, which are dated May 18, 2000. The cover letter explains that the drawings are a complete set of Phase I drawings and specifications. The letter states that Camp Dresser intends to file complete drawings and specifications in three phases. Phase I, which is completed with the May 2000 drawings, consists of sitework, high rate flocculation and sedimentation, and ozone contact tanks. Phase II consists of biologically active granulated active carbon filters, clearwell, and gravity thickeners. Phase III consists of the remainder of the project. As of July 3, 2000, prior to the final hearing, the design for the SWTP had reached the 60 percent level of effort or completion. Although the SWTP described in the DBO Contract, Basis of Design, and May drawings is a relatively large, complex facility, it does not employ unproven technology. The standardization of design and regulatory review is facilitated by the use of the so-called Ten States' Standards, which are standards commonly used by the permitting authorities of numerous states, including Florida, to determine the capabilities of specified treatment processes in achieving specific water quality levels. Although the ACTIFLO technology is relatively new, it has been in use for at least five years. A pretreatment sedimentation barrier that reduces treatment time and thus tankage volume requirements, ACTIFLO is in use in a water treatment plant with a capacity of 60 MGD in Canada, which TBW's selection team members visited. ACTIFLO presently is being incorporated into a surface water treatment plant in Melbourne, Florida, where it must treat the nutrient-rich water of Lake Washington and the St. Johns River. The City of Tampa is adding ACTIFLO basins to its facilities. Also significant is the fact that ACTIFLO easily passed the pilot test on Lake Manatee. At present, 25 facilities using ACTIFLO are under design or construction in North America. As is consistent with the theory, the DBO process for designing, building, and operating the SWTP has demanded greater cooperation among the three entities that operate relatively independently in the DBB process. Pursuant to their obligations under the DBO Contract, Camp Dresser, Clark, and USFilter have coordinated, and likely will continue to coordinate, their efforts closely from design and construction, up to operation, to save time and money from the traditional DBB process, in which the design phase, construction phase, and operation phase are relatively independent of each other. The Variance In general, DEP has the authority to issue public drinking water treatment construction permits. The successful applicant obtains one permit--for construction and operation. There are no conceptual permits or separate operating permits. In Hillsborough County, as well as 10 other counties, DEP has delegated its responsibilities for issuing public drinking water treatment construction permits. In Hillsborough County, DEP has delegated this responsibility by an interagency agreement to the Health Department. Applying DEP rules to determine whether to issue a public drinking water construction permit, the Health Department defers to DEP for the issuance of variances from DEP rules. In typical permitting cases, the Health Department uses its own staff in processing the application and reaching a permitting decision. In a large case, such as this, the Health Department's lone professional engineer, who was hired in September 1999, can obtain considerable assistance from professional engineers within the Tampa Bay area and professional engineers employed by DEP. Perceiving a possible incompatibility between the DB process and the rules from which the variance is sought in this case, TBW initially filed a request for a variance with the Health Department. However, the Health Department declined to issue a variance to DEP rules and informed TBW that it had to file its request with DEP. Thus, on January 10, 2000, TBW filed a petition for a variance with DEP. On March 28, 2000, DEP issued a final order, pursuant to Section 120.542, Florida Statutes, granting the requested variance from Rule 62-555.520(4)(c) and (d), Florida Administrative Code (Variance). The Variance finds that the purpose of the underlying statutes would be met "because no component of the project would be permitted or constructed without review by the permitting authority of the complete plans and specifications for that portion of the project." The Variance finds that the DB approach will protect the public health, safety, and welfare in providing safe drinking water without exacerbating possible negative environmental impacts from the overuse of groundwater. The Variance relieves TBW of the necessity of complying with two subsections of the rule governing the contents of applications for a public drinking water construction permit. Rule 62-555.520(4)(c) and (d), Florida Administrative Code, provides: The permit application form sets forth the minimum information which is to be supplied to the Department or the Approved County Health Department. Additional information may be required by the Department to clarify information submitted in the permit application or to demonstrate that the proposed level of treatment will effectively treat the contaminants present in the raw water. The information required by the application is as follows: * * * Prints of drawings of the work project which contain sufficient detail to clearly apprise the Department of the work to be undertaken. All prints shall be minimum of 18 x 24 inches and a maximum size of 36 x 42 inches. The scale of details contained shall be satisfactory for microfilm reproduction. (Reduced size photographic reproduction of drawings for submission may be authorized.) Complete specifications of the project necessary to supplement the prints submitted. The issuance of the Variance by DEP has met with approval, albeit cautious approval, by the Health Department. One Health Department witness was an Engineer III, who is 19-year employee of the Health Department and supervisor of four Environmental Specialists charged with reviewing construction plans for drinking water plants. He testified that he agreed with DEP's final order granting the Variance. The Engineer III and the other Health Department witness, its professional engineer, testified that the issuance of the initial permit would not influence the Health Department in deciding whether to issue permit modifications, except to ensure compatibility. Allowing TBW not to comply with Rule 62-555.520(4)(c) and (d), Florida Administrative Code, the Variance provides that the initial permit shall not authorize the construction of any component of the SWTP; each component may be constructed only after the submission of complete plans and specifications for that component and the issuance of a permit modification based on those complete plans and specifications. The Variance also provides that the permitting authority shall publish a notice of intent to issue a permit modification "if the permitting authority believes that the modifications are of a controversial nature, or that there is heightened public awareness of the project." Save Our Bays and Canals, Inc. The Verified Amended Petition On May 1, 2000, Petitioner filed a petition challenging the Variance. On June 29, 2000, Petitioner filed an amended petition challenging the Variance, and the Administrative Law Judge granted Petitioner leave to file an amended petition on July 3, 2000. At the start of the hearing, on July 7, 2000, Petitioner filed a verified amended petition, which was identical to the amended petition, except that, on July 6, 2000, Petitioner's president had verified the pleading "to the best of [his] knowledge, information and belief." The verified amended petition states that Petitioner has over 400 members. The verified amended petition alleges that a substantial number of Petitioner's members will consume the finished water produced by the SWTP and will use the surface waters supplying the SWTP for recreation. The verified amended petition states that the purpose of Petitioner is to save the bays, canals, and waterways of the Tampa Bay area and to ensure safe drinking water for its members and residents of the Tampa Bay area. The verified amended petition states that the Variance affects Petitioner because it would allow the issuance of the Permit and construction of initial phases of the SWTP prior to submittal, review, and approval of complete plans for the next and subsequent phases. The verified amended petition alleges that Petitioner incorporated to pool its resources to review applications, so as to ensure safe drinking water. The verified amended petition states that submittal and review of a complete set of drawings and specifications is necessary prior to construction of the SWTP to ensure the ability of the facility to comply with state drinking water standards. The verified amended petition states that review of all individual components of the SWTP is necessary to assure the protection of the public health, safety, and welfare and the compliance with all applicable state and federal laws. Addressing specifically the 30 Percent Plans, the verified amended petition objects to the absence of a list of items to be included in the 30 Percent Plans. The verified amended petition alleges that this piecemeal approach to permitting will require Petitioner to request administrative hearings on each phase of permitting. The verified amended petition states that the Variance may have adverse environmental and safety impacts that cannot be evaluated fully without a submittal and review of the complete drawings and specifications. The verified amended petition states that the DBO approach is "self-created." The verified amended petition objects to the failure of TBW to obtain the Variance before issuing the RFP and instead using the DBO Contract as a basis for claiming hardship so as to qualify for the Variance. The verified amended petition states that the number of variances issued for similar 30 Percent Plans threatens to create a situation in which the variance subsumes the rule requiring complete drawings and specifications. The verified amended petition objects to this form of unwritten policy that has not been published as a rule. The verified amended petition states that the phased permitting of the SWTP may create permitting momentum that discourages a rigorous application of the rules at a later stage. The verified amended petition states that the request for a variance is improper because it is for a variance from statutes, not rules. The verified amended petition states that Section 403.861(10), Florida Statutes, requires DEP or Health Department approval of "complete plans and specifications prior to the installation, operation, alteration, or extension of any public water system." The verified amended petition states that "installation" means construction. The verified amended petition states that Section 403.861(5), Florida Statutes, prohibits the issuance of a public drinking water treatment construction permit "until the water system has been determined to have the required capabilities . . .." The verified amended petition states that the assurances of USFilter are insufficient to satisfy this requirement. The verified amended petition states that Section 120.542, Florida Statutes, which authorizes the variance procedure used in this case, does not authorize variances for compliance with federal law. The verified amended petition states that TBW must obtain a federal variance in order to obtain the Variance. The verified amended petition states that the 30 Percent Plans omit information required for permitting, such as the listing of a certified operator, monitoring and recordkeeping programs, and various financial elements, such as the posting of a bond and creation of reserves to demonstrate financial soundness. The verified amended petition states that TBW's substantial hardship is based on contract deadlines that are entirely self-created and, thus, insufficient to warrant a variance. The verified amended petition notes that the environmental damage cited as a basis for granting the Variance "was caused by years of overpumping by . . . TBW . . .." Also, the verified amended petition states that member governments of TBW continue to approve new development, which increases the demand for drinking water, because TBW and its member governments have failed to exploit fully the potential for conservation and reclaimed water. Similarly, the verified amended petition states that SWFWMD helped create the hardship by renewing the permits for additional withdrawals from the 11 Wellfields. The verified amended petition states that the DBO process will not necessarily save time and money and is not a recognized exception to the general requirement that an applicant must submit complete drawings and specifications prior to permitting. The verified amended petition states that 30 Percent Plans do not provide sufficient detail to know what the contractor is promising to build, and it would be faster to correct any mistakes prior to the start of construction, rather than after the start of construction. Standing Petitioner was an unincorporated association from its formation in early October 1999 through February 3, 2000, when it was incorporated as a Florida not-for-profit corporation. Originally named Save Our Bays and Canals Association, the unincorporated association was formed by members of the Apollo Beach Civic Association who were concerned about the environmental impact upon their bays and canals of intensive utility and industrial land uses in close proximity to their homes. Apollo Beach is an unincorporated area along the southeast shore of Tampa Bay, just south of the mouth of the Alafia River. The land uses with which the unincorporated association has been concerned in its brief existence include a sulfur plant, the TECO Big Bend plant, a proposed National Gypsum plant, a proposed concrete plant, the proposed Desal Plant, and, now the proposed SWTP. The Apollo Beach area is very close to the proposed site of the Desal Plant, but is about 17 miles south southeast from the proposed site of the SWTP. Petitioner and its members are primarily concerned with the Desal Plant, not the SWTP. However, Petitioner and its members express concern with the SWTP. The concerns are that DB permitting of the SWTP will jeopardize the production of safe drinking water and will result in greater costs to TBW customers, who will eventually bear the financial burden of costly reworking of a hastily designed and constructed project. Standing analysis is simplified by the elimination of the issue of whether the verification of the amended petition confers standing. The claims of Petitioner in this case do not rise to the level of an attempt to prevent an activity, conduct, or product to be permitted from impairing, polluting, or otherwise injuring the air, water, or other natural resources of the State. First, finished drinking water is not a natural resource of the State. Although a resource, finished drinking water is not natural. Although of lower water quality, raw water is a natural resource. The potable water leaving the SWTP is a manufactured resource. Second, even if finished drinking water were a natural resource, the issuance of the Variance does not have the effect of impairing, polluting, or otherwise injuring a natural resource. The Variance excuses compliance with two rules requiring complete drawings and specifications. Even assuming that the SWTP would impair, pollute, or otherwise injure natural resources, the Variance would not have such an effect because the act of granting the Variance is distinct from the act of granting the Permit itself. Thus, facts regarding the circumstances under which Petitioner's president verified the amended petition are irrelevant for the purpose of determining standing. Petitioner's standing is a function of the characteristics of the corporation and its members. At the corporate level, the articles of incorporation state that the "specific and primary purposes for which this corporation is formed are to operate for the public education and advancement of the water quality of Tampa Bay, its tributaries, its estuaries and its canals and for other charitable purposes, by the distribution of its funds for such purposes." There is some indication in the record of an attempt, after filing the petition commencing this proceeding, to amend the articles of incorporation to state, among Petitioner's purposes, the protection of drinking water. The record does not contain the written articles of incorporation, as amended, or amended articles of incorporation after February 3, 2000. However, for the purpose of this recommended order, the Administrative Law Judge shall assume that such an amendment was made at some point after the filing of the petition and before the final hearing. At the membership level, the water to be produced by the SWTP will be distributed primarily to customers in Pasco and Pinellas counties, St. Petersburg, and the Northwest Service Area of Hillsborough County, not to Apollo Beach, which is in southern Hillsborough County. Nearly all of Petitioner's members reside in Apollo Beach or other nearby communities, which also will not be served by the SWTP. Although an insubstantial number of Petitioner's members will consume finished water from the SWTP in their homes, a substantial number will consume finished water from the SWTP at their places of work or schools and where they shop or dine out. Drinking water is ubiquitous, and the mixture of functional land uses in Apollo Beach is not, so it is highly probable that members of Petitioner will travel the three-county area in connection with their employment, education, and recreation. Close analysis of the characteristics of Petitioner and its members reveals no basis for finding standing to challenge the Variance. Nothing in the record suggests that Petitioner or any of its members have devoted themselves to the arcane task of resisting a perceived trend of state and local agencies to issue series of permits in response to DB proposals--or, more colorfully, to engage in "piecemeal permitting." About the only interest that Petitioner can legitimately claim in DB permitting is that multiple points of entry, at each permit and permit modification, will result in additional expense. If Petitioner has standing to contest even the permitting of the SWTP, Petitioner must petition each time for an administrative hearing, conduct discovery, and participate in the final hearing. However, this seems, at most, like a tenuous interest, which suffers also from the speculation that later stages of the DB permitting process will continue to present new issues not raised in the challenge of the Permit initially approved. Turning to the members themselves, their consumption of drinking water produced by the SWTP is no basis for standing either because the attenuated relationship between the Variance, which excuses compliance with two rules concerning the contents of applications, and the safety of drinking water or the additional costs that could arise from hasty designing, constructing, or permitting. Although it is conceivable that a record could have been made that the DB permitting proposed in this case would likely result in incomplete, incompetent permitting review, so as to jeopardize the public health if the permit were to issue, the record in this case does not support such a contention. To the contrary, the record establishes that the DB permitting is at least as likely as DBB permitting to provide the regulatory oversight necessary to assure the design and construction of a successful public drinking water treatment plant Lacking a substantial nexus in the record between the DB permitting authorized by the Variance and the quality of the drinking water that, if the Health Department issues the Permit, would likely be produced by the SWTP and likelihood of success of the overall construction project, the members of Petitioner likewise lack standing to challenge the Variance. Ultimate Findings of Fact Petitioner and its members lack standing to challenge the Variance. TBW faces a substantial hardship if not given the Variance. The legal and financial consequences of a failure to meet the phased-in withdrawal reductions are real and substantial. The environmental damage caused by overpumping the 11 Wellfields underscores the urgency of developing alternative sources of raw water for production into finished drinking water. The rule from which TBW seeks the Variance is derived from the statute discussed in the Conclusions of Law. The underlying purpose of this statute is the protection of the public health, safety, and welfare. The Variance serves the underlying purposes in two respects. First, the 30 Percent Plans contain sufficient detail to allow permitting to proceed without jeopardizing the objective of the rules to ensure that the USFilter team designs and constructs a water treatment plant that is in full compliance with all federal and state law. Second, the Variance provides that the USFilter team shall construct no component of the SWTP until it has been permitted, either initially or by a permit modification. Petitioner's Liability for Attorneys' Fees and Costs Petitioner has a Technical Committee on which Petitioner relies for examination of technical aspects of matters that are of general concern to Petitioner. This committee obtained a copy of the Variance and, after examination and discussion, developed a position in opposition to DEP's stated intent to grant the Variance. The Chair of Petitioner's Technical Committee, who has a bachelor of science degree in chemistry and is an industrial hygienist, drafted a letter reflecting the opinion of the committee in opposition to the Variance. Petitioner's attorney then converted this letter into the petition that commenced this proceeding. At all times, the Board of Directors of Petitioner approved the actions of the Technical Committee and Petitioner's attorney, including the filing of the petition. When Petitioner's president verified the amended petition, he reasonably relied on the advice of counsel concerning the substance of the assertions, and the advice of counsel was based on the work of the Technical Committee. Petitioner's president also reasonably relied on the work of the Technical Committee when he verified the amended petition. Although DB permitting has been available for the design and construction of wastewater treatment plants for an undetermined period of time, DB permitting for the design and construction of public drinking water plants is a new concept. The concept is so new that the DEP Orlando office mistakenly issued at least 2 DB permits for public drinking water plants without requiring the applicant to obtain a variance from the two rules that prevent DB permitting for such facilities. The concept is so new that the key Health Department employees have expressed concern over personnel demands from this new means of permitting, although they have also expressed at least lukewarm support for the Variance. The record portrays the employees of the Health Department as hard-working and competent, but over-burdened. The DB permitting obviously places significant responsibilities upon the Health Department, especially as it familiarizes itself with DP permitting. Although the availability of professional support from other sources, including DEP, ultimately resolves this issue, the situation of the Health Department also is relevant in assessing Petitioner's liability for attorneys' fees and costs. Two or three aspects of the drawings were deficient, according to Petitioner's professional engineer, whose testimony has been admitted despite the unreasonably restricted opportunity presented for cross-examination by his contractually driven refusal to identify past clients or jobs. Although none of these items seems likely to jeopardize a successful construction project, these were design points on which well-informed professionals could reasonably differ. Although the issue of "improper purpose" presents a closer question than the substantive issues discussed above, there is inadequate subjective or objective evidence in the record supporting TBW's claim for attorneys' fees and costs on this ground. Ultimately, the novelty of DB permitting of drinking water treatment plants precludes a finding of improper purpose. All available facts drive this determination, and, at this point in time, the relative uniqueness of DB permitting of drinking water treatment plants to DEP, the Health Department, and Petitioner and its members provides the necessary margin to preclude a finding of improper purpose.
Recommendation It is RECOMMENDED that the Department of Environmental Protection enter a final order granting the Variance and denying the request of Tampa Bay Water for attorneys' fees and costs. DONE AND ENTERED this 24th day of July, 2000, in Tallahassee, Leon County, Florida. ROBERT E. MEALE Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 24th day of July, 2000. COPIES FURNISHED: Kathy C. Carter, Agency Clerk Office of General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000 Teri L. Donaldson, General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000 Ralf G. Brookes, Attorney 1217 East Cape Coral Parkway Suite 107 Cape Coral, Florida 33904 Donald D. Conn, General Counsel Tampa Bay Water 2535 Landmark Drive, Suite 211 Clearwater, Florida 33761 J. Frazier Carraway Thomas A. Lash Salem, Saxon & Nielson, P.A. 101 East Kennedy Boulevard Suite 3200 Tampa, Florida 33601 Cynthia K. Christen Senior Assistant General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000 William S. Bilenky General Counsel Jack R. Pepper, Jr. Associate General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899
The Issue The issue to be determined in this case is whether the Administrative Order issued by DEP on December 23, 2014, is a reasonable exercise of its enforcement authority.
Findings Of Fact Parties FPL is a subsidiary of NextEra Energy. It is a regulated Florida Utility providing electric service to 4.7 million customers in 35 counties. FPL owns and operates the Turkey Point Power Plant, which includes a cooling canal system (“CCS”) that is the subject of the AO at issue in this proceeding. DEP is the state agency charged with administering the Florida Electric Power Plant Siting Act (“PPSA”), chapter 403, Part II, Florida Statutes. DEP has the power and the duty to control and prohibit pollution of air and water in accordance with the law and rules adopted and promulgated by it. § 403.061, Fla. Stat. (2015). ACI is a Florida corporation and the owner of 2,598 acres of land in southeast Miami-Dade County approximately four miles west of the Turkey Point CCS. ACI is engaged in agriculture and limerock mining on the land. ACI withdraws and uses water from the Biscayne Aquifer pursuant to two SFWMD water use permits. ACI also has a Life- of-the-Mine Environmental Resource Permit issued by DEP for its mining activities. The Life-of-the-Mine permit requires that mining be terminated if monitoring data indicate the occurrence of chloride concentrations greater than 250 milligrams per liter (“mg/L”) in the mine pit. The City of Miami is a municipal corporation located about 25-miles north of Turkey Point. The City purchases water from Miami-Dade County, which withdraws the water from the Biscayne Aquifer. Turkey Point FPL’s Turkey Point property covers approximately 9,400 acres in unincorporated Miami-Dade County, along the coastline adjacent to Biscayne Bay. Five electrical generating units were built at Turkey Point. Units 1 and 2 were built in the 1960s. Unit 2 ceased operating in 2010. Units 3 and 4 are Florida’s first nuclear generating units, which FPL constructed in the 1970s. Unit 5 is a natural gas combined cycle generating unit brought into service in 2007. Units 1 through 4 pre-date the PPSA and were not certified when they were built. However, Units 3 and 4 were certified pursuant to the PPSA in 2008 when FPL applied to increase their power output, referred to as an “uprate.” Unit 5 was built after the PPSA and was certified under the Act. The CCS The Turkey Point CCS is a 5,900-acre network of canals, which provides a heat removal function for Units 1, 3, and 4, and receives cooling tower blowdown from Unit 5. FPL constructed the CCS pursuant to satisfy a 1971 consent judgment with the U.S. Department of Justice which required FPL to terminate its direct discharges of heated water into Biscayne Bay. The CCS is not a certified facility under the PPSA, but it is an “associated facility,” which means it directly supports the operation of the power plant. The CCS functions like a radiator, using evaporation, convective heat transfer, and radiated heat loss to lower the water temperature. When cooling water enters the plant, heat is transferred to the water by flow-through heat exchangers and then discharged to the “top” or northeast corner of the CCS. Circulating water pumps provide counter-clockwise flow of water from the discharge point, down (south) through the 32 westernmost canals, across the southern end of the CCS, and then back up the seven easternmost canals to the power plant intake. The full circuit through the CCS from discharge to intake takes about 48 hours and results in a reduction in water temperature of about 10 to 15 degrees Fahrenheit. The CCS canals are unlined, so they have a direct connection to the groundwater. Makeup water for the CCS to replace water lost by evaporation and seepage comes from process water, rainfall, stormwater runoff, and groundwater infiltration. When the CCS was first constructed, FPL and SFWMD’s predecessor, the Central and Southern Florida Flood Control District, entered into an agreement to address the operation and management of the CCS. The agreement has been updated from time to time. The original agreement and updates called for monitoring the potential impacts of the CCS. Operation of the CCS is also subject to a combined state industrial wastewater permit and National Pollution Discharge Elimination System (“NPDES”) permit administered by DEP. The industrial wastewater/NPDES permit is incorporated into the Conditions of Certification. Hypersaline Conditions The original salinity levels in the CCS were probably the same as Biscayne Bay. However, because the salt in saltwater is left behind when the water evaporates, and higher water temperature causes more evaporation, the water in the CCS becomes saltier. Salinity levels in the CCS are also affected by rainfall, air temperature, the volume of flow from the power plant, and the rate of water circulation. In 2008, when FPL applied for certification of the uprate of Units 3 and 4, it reported average salinity to be 50 to 60 Practical Salinity Units (“PSU”). This is a “hypersaline” condition, which means the salinity level is higher than is typical for seawater, which is about 35 PSU. Higher salinity makes water denser, so the hypersaline water in the CCS sinks beneath the canals and to the bottom of the Biscayne Aquifer, which is about 90 feet beneath the CCS. At this depth, there is a confining layer that separates the Biscayne Aquifer from the deeper Upper Floridan Aquifer. The confining layer stops the downward movement of the hypersaline “plume” and it spreads out in all directions. FPL estimated that the average daily loading of salt moving from the CCS into the Biscayne Aquifer is 600,000 pounds per day. In late 2013, salinity levels in the CCS began to spike, reaching a high of 92 PSU in the summer of 2014. FPL believes the salinity spikes in recent years are attributable in part to lower than normal rainfall and to higher turbidity in the CCS caused by algal blooms. Reductions in flow and circulation during this period associated with the retirement of Unit 2 and the uprate of Units 3 and 4 could also have contributed to increased temperatures in the CCS, more evaporation, and higher salinity. ACI presented evidence suggesting that the uprate of Units 3 and 4 could be the primary cause of recent, higher water temperatures and higher salinity. The analyses that have been conducted to date are not comprehensive or meticulous enough to eliminate reasonable disagreement about the relative influence of the factors that affect salinity in the CCS. FPL has taken action to reduce salinity within the CCS by adding stormwater from the L-31E Canal (pursuant to emergency orders), adding water from shallow saline water wells, and removing sediment build-up in the canals to improve flow. These actions, combined with more normal rainfall, have decreased salinity levels in the CCS to about 45 PSU at the time of the final hearing. Saltwater Intrusion Historical data show that when the CCS was constructed in the 1970s, saltwater had already intruded inland along the coast due to water withdrawals, drainage and flood control structures, and other human activities. The “front” or westernmost line of saltwater intrusion is referred to as the saline water interface. More specifically, the saline water interface is where groundwater with total dissolved solids (“TDS”) of 10,000 mg/L or greater meets groundwater with a lower chloride concentration. DEP classifies groundwater with a TDS concentration less than 10,000 mg/L as G-II groundwater, and groundwater with a TDS concentration equal to or greater than 10,000 mg/L as G-III groundwater, so the saline water interface can be described as the interface between Class G-II groundwater and Class G-III groundwater. In the 1980s, the saline water interface was just west of the interceptor ditch, which runs generally along the western boundary of the CCS. The interceptor ditch was installed when the CCS was first constructed as a means to prevent saline waters from the CCS from moving west of the ditch. Now, the saline water interface is four or five miles west of the CCS, and it is still moving west. The groundwater that comes from the CCS can be identified by its tritium content because tritium occurs in greater concentrations in CCS process water than occurs naturally in groundwater. CCS water has been detected four miles west of the CCS. Saline waters from the CCS have been detected northwest of the CCS, moving in the direction of Miami-Dade County’s public water supply wellfields. The hypersaline plume from the CCS is pushing the saline water interface further west. Respondents identified factors that contributed to the saltwater intrusion that occurred before the CCS was constructed. However, while saltwater intrusion has stabilized in other parts of Miami-Dade County, it continues to worsen in the area west of the CCS. Respondents made no effort to show how any factor other than the CCS is currently contributing to the continuing westward movement of the saline water interface in this area of the County. The preponderance of the record evidence indicates the CCS is the major contributing cause of the continuing westward movement of the saline water interface. Fresh groundwater in the Biscayne Aquifer in southeast Miami-Dade County is an important natural resource that supports marsh wetland communities and is utilized by numerous existing legal water uses including irrigation, domestic self-supply, and public water supply. The Biscayne Aquifer is the main source of potable water in Miami-Dade County and is designated by the federal government as a sole source aquifer under the Safe Drinking Water Act. Saltwater intrusion into the area west of the CCS is reducing the amount of fresh groundwater in the Biscayne Aquifer available for natural resources and water uses. Water Quality Violations At the final hearing, a DEP administrator testified that DEP was unable to identify a specific violation of state groundwater or surface water quality standards attributable to the CCS, but DEP’s position cannot be reconciled with the undisputed evidence that the CCS has a groundwater discharge of hypersaline water that is contributing to saltwater intrusion. Florida Administrative Code Rule 62-520.400, entitled “Minimum Criteria for Ground Water,” prohibits a discharge in concentrations that “impair the reasonable and beneficial use of adjacent waters.” Saltwater intrusion into the area west of the CCS is impairing the reasonable and beneficial use of adjacent G-II groundwater and, therefore, is a violation of the minimum criteria for groundwater in rule 62-520.400. In addition, sodium levels detected in monitoring wells west of the CCS and beyond FPL’s zone of discharge are many times greater than the applicable G-II groundwater standard for sodium. The preponderance of the evidence shows that the CCS is contributing to a violation of the sodium standard. Agency Response The 2008 Conditions of Certification included a Section X, entitled “Surface Water, Ground Water, Ecological Monitoring,” which, among other things, required FPL and SFWMD to execute a Fifth Supplemental Agreement regarding the operation and management of the CCS. New monitoring was required and FPL was to “detect changes in the quantity and quality of surface and ground water over time due to the cooling canal system.” Section X.D. of the Conditions of Certification provides in pertinent part: If the DEP in consultation with SFWMD and [Miami-Dade County Department of Environmental Resources Management] determines that the pre- and post-Uprate monitoring data: is insufficient to evaluate changes as a result of this project; indicates harm or potential harm to the waters of the State including ecological resources; exceeds State or County water quality standards; or is inconsistent with the goals and objectives of the CERP Biscayne Bay Coastal Wetlands Project, then additional measures, including enhanced monitoring and/or modeling, shall be required to evaluate or to abate such impacts. Additional measures include but are not limited to: * * * 3. operational changes in the cooling canal system to reduce any such impacts; DEP determined that the monitoring data indicates harm to waters of the State because of the contribution of CCS waters to westward movement of the saline water interface. Under the procedures established in the Conditions of Certification, this determination triggered the requirement for “additional measures” to require FPL to “evaluate or abate” the impacts. Pursuant to the Conditions of Certification, a Fifth Supplemental Agreement was executed by FPL and SFWMD, which, among other things, requires FPL to operate the interceptor ditch to restrict movement of saline water from the CCS westward of Levee 31E “to those amounts which would occur without the existence of the cooling canal system.” The agreement provides that if the District determines that the interceptor ditch is ineffective, FPL and the District shall consult to identify measures to “mitigate, abate or remediate” impacts from the CCS and to promptly implement those approved measures. SFWMD determined that the interceptor ditch is ineffective in preventing saline waters from the CCS in deeper zones of the Biscayne Aquifer from moving west of the ditch, which triggered the requirement of the Fifth Supplemental Agreement for FPL to mitigate, abate, or remediate the impacts. Following consultation between DEP and SFWMD, the agencies decided that, rather than both agencies responding to address the harm caused by the CCS, DEP would take action. DEP then issued the AO for that purpose. The AO The AO begins with 36 Findings of Fact, many of which are undisputed background facts about the history of Turkey Point and the CCS. Also undisputed is the statement in Finding of Fact 25 that “the CCS is one of the contributing factors in the western migration of CCS saline Water” and “the western migration of the saline water must be abated to prevent further harm to the waters of the state.” Findings of Fact 16-19 and 25 indicate there is insufficient information to identify the causes and relative contributions of factors affecting saltwater intrusion in the area west of the CCS. However, as found above, the preponderance of the record evidence indicates the CCS is the major contributing cause of the continuing westward movement of the saltwater interface. In the “Ordered” section of the AO, FPL is required to submit to DEP for approval a detailed CCS Salinity Management Plan. The AO explains that “[t]he primary goal of the Management Plan shall be to reduce the hypersalinity of the CCS to abate westward movement of CCS groundwater into class G-II (<10,000 mg/L TDS) groundwaters of the State.” The goal of reducing hypersalinity of the CCS to abate westward movement of CCS groundwater into class G-II groundwaters is to be demonstrated by two success criteria: (1) reducing and maintaining the average annual salinity of the CCS at a practical salinity of 34 within 4 years of the effective date of the Salinity Management Plan; and (2) decreasing salinity trends in four monitoring wells located near the CCS. Although the AO states that FPL’s proposal to withdraw 14 mgd from the Upper Florida Aquifer and discharge it into the CCS might accomplish the goal of the AO, the AO does not require implementation of this particular proposal. It is just one of the options that could be proposed by FPL in its Salinity Management Plan.1/ If the success criteria in the AO are achieved, hypersaline water will no longer sink beneath the CCS, the rate of saltwater intrusion will be slowed, and the existing hypersaline plume would begin to “freshen.” Petitioners’ Objections ACI and the City object to the AO because the success criteria do not prevent further harm to water resources. Maintaining salinity in the CCS to 34 PSU will not halt the western movement of the saline water interface. They also contend the AO is vague, forecloses salinity management options that could be effective, and authorizes FPL’s continued violation of water quality standards. For ACI, it doesn’t matter when the saline water interface will reach its property because, advancing in front of the saltwater interface (10,000 mg/L TDS) is a line of less salty water that is still “too salty” for ACI’s mining operations. Years before the saline water interface reaches ACI’s property, ACI’s mining operations will be disrupted by the arrival of groundwater with a chloride concentration at or above 250 mg/L.2/
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law it is RECOMMENDED that the Department of Environmental Protection rescind the AO or amend it as described above. DONE AND ENTERED this 15th day of February, 2016, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 15th day of February, 2016.
Findings Of Fact The parties stipulated, and it is so found, that Petitioner, DER, has jurisdiction over both the issues and the Respondents Dey and KWC. KWC owns and operates a water system which supplies water to both residential and commercial customers in the City of Keystone Heights, Florida. Virginia Key is the President of KWC, a member of the Board of Directors of the corporation, and one of the five stockholders. The other stockholders are her sisters. The five sisters are the daughters of the late G. E Wiggins, and inherited the company from him at his death in 1969. Mr. Wiggins developed the water company in the 1920's and operated it until his death. KWC came under the jurisdiction of the Florida Public Service Commission (PSC) just prior to Mr. Wiggins' death. At that time, pursuant to a PSC requirement, it was assessed and valued at a sum in excess of $250,000.00 by a consultant firm hired for the purpose. As of late November, 1984, KWC served approximately 752 residential customers which, when multiplied by an average 2.5 persons per family factor, results in a total of approximately 1,880 residential inhabitants served by the water system. In addition, the system serves 105 commercial customers. It is impossible to estimate with any reasonable degree of accuracy the number of individuals involved in the commercial service. The system consists of three wells drilled in 1940, 1946, and 1960 to a depth of 350, 450, and 492 feet respectively. Total yield from the three wells is normally 1,350 gallons per minute. The wells are generally well protected against surface water infusion, are normally not subject to inundation, and have had no salt water infiltration problems in the past. At the present time, well number 2, drilled in 1946, with a 350 gpm yield is out of service. The water, when pumped from the ground, is stored in two tanks-one with a 60,000 gallon capacity and the other with a capacity of 800 gallons. Both tanks are steel. Chlorine is added to the water in each storage situation by a hyper-chlori- nation system before the water is sent to the storage tank. The distribution system is made up of 6" and 2" diameter pipe. In March, 1984, two different inspections of the water system, done by, in one case, an environmental specialist and in the other, an Engineer I with DER, revealed several deficiencies in the maintenance and operation of the system all of which constitute violations of DER rules. Specifically, these include (1) failure to provide an auxiliary power source in the event the main pumping capability of the system is lost, (Rule 17-22.106 (3)(a); (2) failure to utilize for the system an operator certi- fied by the state with a Class C license, (Rule 17-22.107(3)(b); (3) failure to maintain a free chlorine residual in the water of at least 0.2 ppm in the system, (Rule 17-22.106(3)(c); (4) failure to maintain a minimum pressure of 20 ppi in the distribution system, (Rule 17-22.106(3)(f); (5) failure to have a gas chlorination facility, (Rule 17-22.106(3)(d); and (6) failure to obtain proper permits to expand the distribution system, (Rule 17-22.108 (1)(b) Rule 17-22, F.A.C., sets up requirements for safe drinking water and was designed to establish guidelines and standards for facilities and water and to bring water into compliance with the Federal Act. Twenty ppi of pressure in the system was adopted as a standard minimum for residual pressure to protect against outside contaminants getting into the water system. Such contaminants could come from ground water, leaks, and water in storage tanks attached to the system such as toilet tanks, being aspirated into the system. Also a certain amount of pressure is required to operate appliances. Normally minimum pressure is found in areas at the edge of the system and in those areas where inadequate chlorination is located. They interact and both pressure and chlorinization are required. Chlorine can be injected into the system generally in two ways: the first is through gas chlori- nation and the second, through hyper-chlorinization as is used in the instant system. The effectiveness of hyper-chlorinization is limited, however, by the size of the system. Basically, hyper- chlorinization is effective when the demand in the system for pressure is no more than 10 ppi. Above this, gas chlorinization is necessary. As late as January 4, 1985, Mr. Dykes went to Keystone Heights to test the system. His tests showed that 11.9 ppi is the average daily flow per 24 hours for the last 12 months. Since this figure is above 10 ppi, in his opinion, a gas chlorinization system would be needed. Chlorine is used to purify water because it has been shown, through long use, to prevent disease. The requirement for a residual chlorine level in water, therefore, is consistent with that concept to insure chlorine is always in the water in sufficient quantity to prevent disease. Respondent's plant has less than the 0.2 residual that is required under the rule. This insufficiency is caused by the inadequate chlorinization system which has insufficient capacity to provide the appropriate amount of chlorine. At the current level, it is providing only approximately 60 percent of the needed chlorine. To correct this deficiency Mr. Dykes recommends installation of a gas chlorinization system. In addition, the pneumatic tank storing the water from the number 3 well does not give sufficient detention time to allow for appropriate reaction of the chlorine contained in the water before the water is released into the distribution system. Another factor relating to the lack of adequate pressure in the system is the fact that, in Mr. Dykes' opinion, too much of the system is made up of 2" diameter water line. A line of this small diameter prevents the maintenance of adequate pressure especially in light of the fact that there are numerous old lines in the system some with corrosion and scale in them which tends to reduce pressure. This latter factor would be prevalent even in the 6" lines. The current plant manager, Mr. Cross, who has been with Respondent for approximately 4 years is, with the exception of one part time employee, the only operations individual associated with the plant. As such, he repairs the meters and the lines, checks the pumps, the chlorinator, and checks and refills the chlorine reservoir on a seven day a week basis. Be learned the operation of the plant from his precedessor, Mr. Johnson, an unlicensed operator who was with the company for 10 years. Mr. Cross has a "D" license which he secured last year after being notified by DER that a license was required. It was necessary for him to get the "D" license before getting the required "C" license. At the present time, he is enrolled to take courses leading toward the "C" license. At the present time, however, he is not, nor is anyone else associated with KWC, holding a license as required. The rule regarding auxiliary power provides that all community systems serving 350 or more persons shall have standby pumping capability or auxiliary power to allow operation of the water treatment unit and pumping capability of approximately one-half the maximum daily system demand. Respondent has admitted that the system is not equipped with an auxiliary power source and it has already been established that more than 350 persons are served by the system. Respondent also admits that subsequent to November 9, 1977, it constructed main water lines for the system which required the obtaining of a permit from either the Petitioner or the county health unit. Respondent admits that it did not obtain or possess a permit to do the additional construction referenced above from either DER or the Clay County Health Department prior to the construction of the water lines referenced. The inspections referenced above, which identified the problems discussed herein, were accomplished by employees of Petitioner, DER, at a stipulated cost of $898.10. Respondent contends, and there is no evidence to the contrary, that there have been no complaints of contaminated water and that the monthly water samples which Mr. Cross forwards to the Clay County Health Department have been satisfactory. Mr. Cross also indicates that a September, 1983 DER analysis of water samples taken from the system was satisfactory. However, bacteriological analysis reports on water collected from Respondent's system on July 11 and 27, 1983, reflect unsatisfactory levels of either coliform or non-coliform bacteria in the water requiring resubmission of test samples. Respondent also contends that no one has ever gotten sick or died from the water furnished by the system and there is, in fact, no evidence to show this is not true. Even though so far as is known, no one has ever been made sick from the water in the system, in Mr. Dykes' opinion, the risk is there. As a result of the defects identified in this system, insufficient chlorine is going into the system to meet reasonable health standards. Though this does not mean that the water is now bad, it does mean that at any time, given a leak or the infusion of some contaminant, the water could become bad quickly, and the standard established by rule is preventive, designed to insure that even in the case of contamination, the water will remain safe and potable. Respondent does not deny that it is and has been in violation of the rules as set out by the Petitioner. It claims, however, that it does not have sufficient funds available to comply with the rules as promulgated by DER. Respondent has recently filed a request for variance under Section 403.854, Florida Statutes, setting forth as the basis for its request that it does not have the present financial ability to comply with any of the suggested or recommended corrective actions to bring its operation into compliance with the rules. Mr. Protheroe, the consulting engineer who testified for Respondent has not evaluated the system personally. His familiarity with it is a result of his perusal of the records of the company and the Petitioner. Based on his limited familiarity with the system, he cannot say with any certainty if it can be brought into compliance with, for example, the 20 ppi requirement. There are too many unknowns. If, however, the central system was found to be in, reasonably good shape, in his opinion, it would take in excess of $100,000.00 to bring it within pressure standards. To do so would require replacement of the 2" lines, looping the lines, and cleaning and replacing some central system lines as well. In his opinion, it would take three months to do a complete and competent analysis of the system's repair needs. Once that was done, he feels it would take an additional three months to bring the plant into compliance with DER requirements. Other repairs, such as those to the lines outside the plant, would take longer because some are located in the downtown area and have interfaced with other utilities. This could take from three to four months if the money were available to start immediately. Here, however, it has been shown that it is not. Consequently, to do the study and then, if possible, procure the funds required, could take well in excess of six months or so. Mr. Protheroe contends, and there is little if any evidence to indicate to the contrary, that to replace the current system with a new one entirely as it is currently constituted would cost at least $250,000.00. However, in his opinion, no one would ever put in a new system similar to the one currently there. He cannot say how much it would cost to buy the system and make the necessary corrections to it to rectify the deficiencies. His familiarity with the system is not sufficiently complete to do this. He cannot say exactly how much the system is worth in its current state, but he is satisfied that it is worth more than $65,000.00. In that regard, Mrs. Dey indicated that in her opinion, the fair market value of the system is currently at $250,000.00. At the present time, there are current outstanding loans in excess of $9,000.00 at 16 percent interest. This current loan basis has been reduced from a higher figure. In 1977, the company borrowed $15,000.00 at 9 percent. In 1981, it borrowed $5,000.00 more at 18 percent. In 1982, the loans were consolidated at an increased rate of 16 percent and the officers have been advised by their current creditors that they cannot borrow any more money for the system in its current state. They would sell the system if a reasonable price could be realized. However, any inquiries on prospective purchases have been chilled by a low rate base assigned by the PSC. In that regard, the City of Keystone Heights offered to purchase the system for $59,000.00. This offer was declined as being unreasonable. Nonetheless, in light of the low rate base assigned by the PSC in its order issued on December 21, 1981 of slightly over $53,000.00 the offer by the city of $59,000.00 is not completely out of line. A certified public accountant, in KWC's December 31, 1983 financial report assigned a valuation of approximately $62,000.00, again a figure only slightly higher than that offered by the city, but substantially less than the $175,000.00 price asked of the city by Respondent Dey and her sisters. Mrs. Dey indicated that to the best of her knowledge the PSC denied rate increases for the purposes of improvements. In the presentation before the commission, respondents relied exclusively on the services of their attorney and accountant. Evidence from Mr. Lowe, of the PSC, however, indicates that KWC has never requested a rate increase to finance any of the improvements called for here. In the PSC order referred to above, Respondent was awarded a 12.25 percent rate of return on its rate base. This figure was an amalgam of a more than 13 percent rate on equity and a lesser figure for cost of doing business, including debt. At the time of that hearing, however, the debt cost was based on a 9 percent interest figure. The 16 percent interest figure came afterwards and no hearing has been requested based on the higher interest rate and it is so found.
Recommendation Based on the foregoing findings of fact and conclusion of law, it is, therefore: RECOMMENDED that Respondents Virginia W. Day and the Keystone Water Company be ordered to comply with the Orders for Corrective Action previously filed herein to bring the water system in question in compliance with the Florida Safe Water Drinking Act without delay or suffer the penalties for non- compliance called for by statute and, in addition, pay costs of investigation in the amount of $898.16. RECOMMENDED in Tallahassee, Florida this 19th day of February, 1985. ARNOLD H. POLLOCK Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 19th day of February, 1987. COPIES FURNISHED: Debra A. Swim, Esquire Assistant General Counsel Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32301 John E Norris, Esquire 10 North Columbia Street Lake City, Florida 32055 Victoria Tschinkel, Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301
Findings Of Fact Petitioner's application for a Class B waste water treatment plant operator was received by Respondent on September 20, 1991. Ms. Setchfield who is in charge of reviewing and approving and/or denying all applications, reviewed Petitioner's application. Based on the documentary evidence submitted by Petitioner, he was given constructive credit for 58 months and actual credits received was 27.6 months for a total credit time of 85.6 months. To receive credit for educational experience, an applicant must demonstrate that his major area of study is in science or biology. Alternatively, an applicant may receive credit provided he furnish Respondent a transcript which would delineate the areas of his studies he successfully completed and the credits received. However, in such instances, an applicant only receives partial credit. Petitioner has been advised (by Respondent) that if he furnish a copy of his transcript, it will be reviewed and if it demonstrates that he is entitled to credit for courses he successfully completed, he would be awarded such credit. Petitioner steadfastly refuses to provide a transcript to Respondent. To be eligible for certification as a Class B waste water treatment plant operator, an applicant must demonstrate, at minimum, that he/she has the required minimum of 96 months total creditable time.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that: Respondent enter a Final Order denying Petitioner's application for certification as a Class B waste water treatment plant operator, as he has failed to satisfy the minimum total time requirement for such certification. 1/ DONE and ENTERED this 29th Tallahassee, Leon County, Florida. day of May, 1992, in JAMES E. BRADWELL 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 29th day of May, 1992.
Findings Of Fact Background In 1983, Concerned Citizens of Citrus County, Inc. (Concerned Citizens), an intervenor in this case, filed a petition toe initiate rulemaking for single source reclassification of groundwater under the existing provisions of Rule 17-3.403, Florida Administrative Code (F.A.C.). In this manner, Concerned Citizens sought to have existent potable waters in Pinellas, Hillsborough, Pasco, Hernando, and Citrus Counties classified Class G-I groundwater, and to thereby provide them the most stringent water quality protection accorded groundwaters of the state. At a public meeting in February 1985, the Environmental Regulation Commission (ERC) deferred action on the petition of Concerned Citizens, and directed the Department of Environmental Regulation (Department) to review the existing G-I rule, prepare proposed revisions, and present its recommendations to the ERC. Following the ERC directive, the Department held numerous public meetings and workshops to explore different approaches to groundwater protection. As a consequence, it prepared the proposed revisions to Rules 17-3.021, 17-3.403, 17-3.404, and 17- 4.245, F.A.C., at issue in these proceedings. On October 31, 1986, the Department duly noticed the proposed rules in volume 12, number 44, of the Florida Administrative Weekly. The notice interested parties that a public hearing would be held on December 16, 1986, before the ERC. 1/ On December 16-17, 1986, the ERC held a public hearing at which time it considered the rules recommended by the Department. During the course of this meeting, the ERC approved and adopted the rules with certain changes. These changes were duly noticed in volume 13, number 3, of the Florida Administrative Weekly on January 16, 1987. Petitioners and Intervenors Petitioners, Adam Smith Enterprises, Inc., and Alliance for Rational Groundwater Rules (Case No. 86-4492RP), and Petitioners Aloha Utilities, Inc.; Interphase, Inc.; Phase 1 Homes, Inc.; A.C. & R., Inc.; Tahitian Development, Inc.; Great Cypress Mobile Village, Inc.; and Barrington, Ltd. (Case No. 86- 4705R), filed timely petitions to challenge the validity of the proposed rules, which petitions were consolidated for hearing. Petitions for leave to intervene were granted on behalf of Florida Electric Power Coordinating Group, Inc.; Florida Land Council, Inc.; and Pasco County. These Intervenors' interests were aligned with those of petitioners. Petitions for leave to intervene were a1so granted on behalf of West Coast Regional Water Supply Authority and Concerned Citizens of Citrus County, Inc. These Intervenors' interests were aligned with those of the Department and the ERC. Petitioner, Adam Smith Enterprises, Inc. (Adam Smith), is the owner/developer of a 3,800-acre development of regional impact (DRI) to be known as Trinity Communities. This development, which has been in the acquisition and planning stages for almost 5 years, is currently undergoing DRI review and Adam Smith anticipates that it will receive its development order by September 1987. The Trinity Communities development is located predominately in Pasco County, with just over 250 acres of its lands located in Pinellas County. These properties are predominately open pasture land, and are bordered on the north, east and west by roads and on the south by Hillsborough and Pinellas Counties. As proposed, the Trinity Communities development will include 1100 acres of parks, golf courses, and other open areas. The remaining lands will be developed to accommodate 9500 dwelling units, as well as industrial and commercial uses to service the community, over a 20-year period. At today's market value, the property represents an investment of approximately 28 million dollars. Abutting the Trinity Communities development is the Eldridge-Wilde Well Field. This well field is covered by consumptive use permits issued by the Southwest Florida Water Management District (SWFWMD), and contains major public community drinking water supply wells as defined by the rules at issue in this proceeding. Of these wells, 5 are located within 9.63 feet and 181.5 feet of the proposed development's property line, and 5 are located with 204.72 fee and 297.5 feet of its property line. Petitioner, Alliance for Rational Groundwater Rules (Alliance), is an association of landowners who united to educate themselves about the proposed rules. The proof failed, however, to establish whether Alliance had ever elected any officers or directors, or the magnitude of its membership. Consequently, the proof failed to establish that a substantial number of its members, although not necessarily a majority, were substantially affected by the proposed rules, and that the relief requested by it was of a type appropriate for it to receive on behalf of its members. Petitioner, Aloha Utilities, Inc. (Aloha Utilities), is a utility certified by the Florida Public Service Commission to provide water and sewer service to two separate service areas in southern Pasco County. Currently, Aloha Utilities operates an 850,000 gallon per day (gpd) sewage treatment facility (Aloha Gardens) and a 1.2 million gpd sewage treatment plant (Seven Springs). It also operates 10-11 producing wells, at least 7 of which are permitted by SWFWMD to withdraw at least 100,000 gpd. One of these wells is located approximately 1/4-1/2 mile from an Aloha Utility sewage treatment plant. At least 3 of Aloha Utilities' wells which are permitted to withdraw 100,000 gpd or more, will service or are servicing the Riverside projects and Aloha Gardens Unit Number 12 project discussed infra. Consequently, the proof establishes that Aloha Utilities operates a major public community drinking water supply system as defined by the subject rules. The Aloha Gardens facility is under a Department order to expand its effluent disposal capacity. To satisfy the Department's order and the need for increased disposal capacity, Aloha Utilities commenced condemnation proceedings 8-12 months ago to secure the needed property. While the condemnation proceeding is not yet completed, Aloha Utilities has already expended considerable sums for engineering studies and attorney's fees in its efforts to acquire the property. That property is located approximately 1/2 mile from an existing well that is permitted for an average daily flow of at least 100,000 gpd. The effluent disposal capacity of the Seven Springs facility is also being expanded to meet existing and future demand. In April 1987, Aloha Utilities acquired a 27-28 acre parcel of land immediately adjacent to its existing facility. Upon these lands, Aloha Utilities proposes to construct percolation ponds, a rapid rate land application effluent disposal process. As sited, these ponds would be located 1/2 to 3/4 of a mile from a well permitted for an average daily flow of 100,000 gallons or more. 2/ Petitioners, Interphase, Inc., Phase 1 Homes, Inc., and Tahitian Development, Inc., are corporations with common management which are developing three separate but geographically proximate projects in Pasco County. These projects will be, or are, serviced by Aloha Utilities. Interphase, Inc., is the owner/developer of a 100- acre tract known as Riverside Village Unit Number Four. This property is currently being developed to include 57 acres dedicated to single family use and 43 acres dedicated to multifamily use, and will require the installation of stormwater facilities and underground sewage transportation facilities. Two wells of Aloha Utilities that are permitted for an average daily flow of 100,000 gallons or more are located 1/2 mile and 1/3 mile, respectively, from this development. Interphase, Inc., is also the owner of a 17-acre parcel of vacant land in Pasco County that is zoned commercial. This property is located within 400 feet of Aloha Utilities' Seven Springs sewer treatment plant, and its development will require the installation of underground sewage transportation facilities. Phase 1 Homes, Inc., is the owner/developer of a project known as Riverside Village Townhouses. This project is fully developed and is currently serviced by Aloha Utilities. Located within 1/2 mile of the development are two wells of Aloha Utilities that are permitted for an average daily flow of 100,000 gallons or more. Tahitian Development, Inc., is the owner/developer of a 40-acre tract known as Riverside Villas. Twenty of these acres have been developed and some of the units sold. The remaining 20 acres are currently under development. In developing its remaining 20 acres, Tahitian Development would be required to install stormwater drainage systems and sewage transportation lines to connect with Aloha Utilities. Located within 1/2 mile of the development are wells of Aloha Utilities that are permitted for an average daily flow of 100,000 gallons or more. Tahitian Development also owns a 40-acre parcel in Orange County which it plans to develop for light industrial uses such as an industrial park or an office complex. Such development would result in at least a 40 percent impervious surface, including building tops, within that 40-acre parcel, and require the installation of a sewage transportation system and a stormwater drainage system. Petitioner, A.C. & R., Inc., is the owner/developer of a project in Pasco County known as Aloha Gardens Unit Number 12. The project, which currently is represented by 40-50 developed lots, is located just north of the Aloha Gardens sewage treatment facility, and is serviced by Aloha Utilities. Located within 1/2 mile of the development that is permitted for an average daily flow of 100,000 gallons or more. Petitioner, Great Cypress Mobile Village, Inc., is the owner/developer of a 149 unit mobile home park in Pasco County. Twenty of these units are completed and ready for occupancy. Completion of the project will require the installation of additional sewer lines. Located at the interior of the property is a sewage treatment plant owned by Northern Utilities which services the project, and within 600 feet of the project's boundary there is a well which services that utility. The capacity of that well was not, however, demonstrated in these proceedings, nor was it shown whether such well was part of a community water system. Petitioner, Barrington, Ltd. is a party of unknown capacity, origin, or interest. No evidence was presented on its behalf to demonstrate that its substantial interests would be affected by the proposed rules. Intervenor, Florida Electric Power Coordinating Group, Inc. (FCG), a Florida corporation, is an association of Florida's electric utilities, and is composed of 37 members. The FCG has, as part of its internal organization, an environmental committee whose purpose is to participate in regulatory development and provide mutual member assistance with regard to water related matters. This committee was authorized by the FCG executive committee to participate in the development of the rules at issue in these proceedings, as well as Intervene in these proceedings, to represent and protect the interests of FCG members. The FCG participated in the development of the subject rules by the Department, and was granted full party status by the ERC during that rulemaking process. The members of FCG are owners and operators of electric power generating facilities. These facilities“ include the power plant and ancillary facilities such as substations. Incident to the operation of these facilities are wastewater discharges associated with the production of electricity and stormwater discharges. One of these facilities, Gainesville Regional Utilities' Deer Haven generating station is located across Highway 441 from a major community drinking water supply well. Intervenor, Florida Land Council, Inc., a Florid corporation, is composed of 12 primary members who own large tracts of land in interior Florida, and who are engaged primarily in agribusiness. The Land Council's purpose is to protect the asset value of its members property and, because of that purpose, it is concerned with environmental regulations, growth management regulations, land use regulations, and comprehensive planning. To protect its interests, the Land Council sought leave to intervene in these proceedings. There was, however, no proof that any lands owned by any member of the Land Council were proximate to any major public community drinking water well. Intervenor, Pasco County, is the owner/operator of 25 wastewater treatment plants with capacities In excess of 100,000 gallons per day, and has under construction, or in the design stage, additional facilities with capacities in excess of 100,000 gallons per day. The construction of these new facilities will require the installation of new lines for the collection of wastewater. Pasco County's current, as well as its planned, wastewater treatment facilities will utilities a rapid rate land application effluent disposal process. Within a mile of any wastewater treatment plan operated by Pasco County can be found a major public community drinking water well as defined by the rules at issue in these proceedings. Pasco County also owns and operates wells within the county with permitted withdrawal rates exceeding 100,000 gpd, and participates in the ownership and management of their wells with permitted withdrawal rates exceeding 100,000 gpd through West Coast Regional Water Supply Authority. Pasco County currently has plans to add new production wells in the county with an average daily pumpage in excess of 100,000 gallons per day. Intervenor, West Coast Regional Water Supply Authority (West Coast), is an interlocal government body created in 1974 to develop, store, and supply water to its member governments so that all citizens within the areas served by the authority may be assured an adequate supply of water. Member governments served by WCRWSA are Hillsborough County, Pasco County, and the cities of St. Petersburg and Tampa. Wellfields operated by West Coast are the Starkey Wellfield located in west central Pasco County, which serves the citizens of New Port Richey and Pasco County; the South-Central Hillsborough Regional Wellfield located in south-central Hillsborough County, which serves the citizens of Hillsborough, County; the crossbar Ranch Wellfield located in north-central Pasco County, which principally serves the citizens of Pinellas, County; the Cypress Creek Wellfild located in south-central Pasco County, which serves the citizens of Hillsborough, Pinellas, and western Pasco Counties and the City of St. Petersburg; the Northwest Hillsborough Wellfield located in northwest Hillsborough County, which serves the citizens of Hillsborough County; the Section 21 Wellfield located in northwest Hillsborough County, which serves the citizens of the City of St. Petersburg; and, the Come-Odessa Wellfield located in northwest Hillsborough County, which serves the citizens of the City of St. Petersburg. 3/ Each of the wellfields operated by West Coast are public community water systems, and contain wells permitted to withdraw in excess of 100,000 gallons per day. Collectively, these wellfields serve a total population of 800,000 persons. Intervenor, Concerned Citizens of Citrus County, Inc. (Concerned Citizens), is a not-for-profit corporation, was chartered in 1981, and has 350 members who obtain their drinking water from operational community water supply wells permitted for over 100,000 gallons per day in Inverness, Crystal River, Floral City, Sugar Mill Woods, Beverly Hills, and Rolling Oaks, Citrus County, Florida. The purpose of Concerned Citizens is to protect the natural resources of Citrus County through planning and zoning regulations, and local and state legislation and regulations. It was granted party status by the ERC. General aspects of the proposed rules The proposed rules establish new eligibility criteria for designation of an aquifer segment as Class G-I groundwater. Under the existing rule, the ERC could reclassify an aquifer or portion of an aquifer as G-I within specified boundaries upon a finding that: The aquifer or portion of the aquifer is the only reasonably available source of potable water to a significant segment of the population; and The designated use is attainable, upon consideration of environmental, techological, water quality, institutional, and social and economic factors. Under the proposed revisions, an aquifer segment could be classified by the ERC as G-I provided it was: ...within the zones of protection of a major public community drinking water supply well(s) or wellfield(s) withdrawing water from unconfined aquifers or from leaky confined aquifer... and, upon consideration of: ...environmental, technologial, water quality, institutional (including local land use comprehensive plans), public health, public interest, social and economic factors. As with thee existing rule, the proposed rules require that rulemaking procedures be followed to actually designate a G-I aquifer or aquifer segment at any particular location. The scheme envisioned by the proposed rules is to provide protection to "major community drinking water supply wells", community water systems that are permitted by consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater, by preventing contaminants from entering the groundwater within a circumscribed radius of the wells. To accomplish this purpose, the proposed rules establish a methodology whereby two zones of protection would be established around such wells if they were withdrawing waters from unconfined aquifers (an aquifer exposed to the atmosphere) or leaky confined aquifers (an aquifer in which groundwater moves vertically from the water table to the top of the aquifer in five years or less). The first zone (the inner zone) would be based on a fixed radius of 200 feet. The second zone (the outer zone) would be based on a radius, calculated under the rule's methodology, of 5 years groundwater travel time. Within the inner zone, discharges would be prohibited. Within the outer zone, certain developments which discharge to groundwater would be prohibited or restricted. A major emphasis of the proposed rules is to restrict discharges to groundwater within the zones of protection. For example, the rules eliminate the zone of discharge within the zones of protection, and require that new discharges to groundwater of treated domestic effluent meet the groundwater criteria specified in rule 17-3.404, F.A.C., prior to discharge. 4/ Additionally, such wastewater treatment facilities would be required to pre-treat industrial wastewater, provide daily monitoring to insure proper treatment plant process control, and provide 24 hour a day attendance of a wastewater operator under the general supervision of a Class A certified wastewater operator. New underground lines for the transport of domestic raw wastewater would be required to be constructed so that no more than 50 gallons per inch of pipe diameter per mile per day could leak into the ground. Within the 5 year zone of protection, there are no restrictions on stormwater discharges for residential developments. However, discharges from new stormwater facilities serving an area forty acres or larger with a forty percent impervious surface, excluding building tops, are required to monitor the discharge. Construction and operation of new sanitary landfills would be prohibited. As previously noted, to be eligible for reclassification as a G-I aquifer, the aquifer or aquifer segment under consideration must be leaky confined or unconfined. Whether the aquifer is leaky confined or not will be determined through application of the "Vv" and "Tv" formulae contained in the proposed rules, and the zones of protection will be established by reference to the "r" formula contained in the proposed rule. To date, neither the Department nor any party has applied the "Vv" and "Tv" formulae to identify wells hat are withdrawing from unconfined or leaky confined aquifers, nor has anyone delineated any zones of protection by application of the "r" formula. The Department has, however, identified those areas of the state at which it is likely that major community drinking water supply wells are withdrawing from such aquifers. Based on this identification, the Department has contracted with the U.S. Geological Survey (USGS) to "map" the Middle-Gulf region (Pinellas, Hillsborough, Pasco, Hernando, and Citrus Counties) by applying the "Vv" and "Tv" formulas to each well permitted to withdraw 100,000 gpd or more to determine if it is withdrawing from such aquifers and, if so, to delineate proposed zones of protection around such wells or wellfields through application of the "r" formula. The USGS is currently mapping the Middle-Gulf region. Pertinent to this case, the Department has identified all of Pasco and Pinellas Counties, the northern half of Hillsborough County, and most of Orange County including Orlando, as areas within which wells are most probably withdrawing from unconfined or leaky confined aquifers, and for which aquifers the Department will seek G-I reclassification. Under the circumstances, the parties have established, except as heretofore noted, that there is a reasonable likelihood that the proposed rules will substantially affect their interests. The rule challenge The gravamen of the protestant's challenge is that certain definitions and formulae continued within the proposed rule are vague, ambiguous, or not supported by fact or logic. The Protestants' also challenge the adequacy of the economic impact statement. The Protestants concerns are addressed below. Definitions Rule 17-3.021, as amended, would define "Confined Aquifer", "Leaky Confined Aquifer", and "Unconfined Aquifer", as follows: (7) "Confined Aquifer" shall mean an aquifer bounded above and below by impermeable beds or by beds of distinctly lower permeability than that of the aquifer itself. For the purpose of G-I, it shall mean an aquifer confined from above by a formation(s) which restricts the movement of groundwater vertically from the water table to the top of the confined aquifer for a period of more than five years * * * (16) "Leaky Confined Aquifer" shall mean, for the purposes of G-I, an aquifer confined from above by a formation(s) which allows groundwater to move vertically from the water table to the top of the leaky confined aquifer in five years or less. * * * (34) "Unconfined Aquifer" shall mean an aquifer other than a confined aquifer. For the purpose of G-I it shall mean an aquifer other than a confined or leaky confined aquifer. 5/ Protestants contend that the definition of "confined aquifer" and "leaky confined aquifer" are vague and meaningless because they are "defined by use of the phrase being defined". Accordingly, they conclude that proposed rule 17-3.021(7) and (16) must fall because they are without thought and reason, irrational and vague. Protestants further contend that since the definitions of "confined aquifer" and "leaky confined aquifer" are flawed, proposed rule 17-3.021(34), which defines unconfined aquifer, must also fall. The Protestants' contentions are not persuasive. If one were restricted to the definition of "confined", "leaky confined" and "unconfined" aquifer to glean their meaning, the rules might be considered vague. However, these definitions are, as they specifically provide, "for the purpose of G-I" and they must be read in context with the balance of the rule. When so read, it is apparent that "top of the confined aquifer" or "top of the leaky confined aquifer" is the top of the aquifer that has been calculated as confined or leaky through manipulation of the "Vv" and "Tv" formulae. Under the circumstances, the subject definitions are not vague, arbitrary or capricious. Proposed rule 17-3.021(20) provides: "New Discharge" shall mean, for the purpose of G-I, a discharge from a new installation; or a discharge from an existing permitted installation that has been altered, after the effective date of G-I reclassification, either chemically, biologically, or physically or that has a 211 22 different point of discharge, and which causes a significantly different impact on groundwater. Protestants contend that the definition of "new discharge" is vague, arbitrary and capricious because existing installations would be classified as new dischargers, and subject to the more stringent requirements of the proposed rules, whether the alteration of their discharge significantly improved or adversely affected groundwater. As proposed, the rule would so define new discharge, and it is not vague or ambiguous. The proof demonstrated, however, that the Department only proposed to define, as new dischargers, those existing installations whose altered discharge caused a significantly different negative impact on groundwater. The Department conceded this point, and offered no proof to demonstrate the reasonableness of classifying existing installations that improve their discharge as new discharges. Under the circumstances, proposed rule 17-3.021(20) is arbitrary and capricious. Proposed rule 17-3.021(35) defines "underground storage facility or underground transportation facility as follows: "Underground storage facility" or "underground transportation facility" shall mean that 10 percent or more of the facility is buried below the ground surface. This proposed rule is, however, only pertinent to proposed rule 17-4.245, which addresses the permitting and monitoring requirements for installations discharging to groundwater. Pertinent to this case, proposed rules 17-4.245(3)(c) and (d) establish construction requirements for the following facilities within the five year zone of protection: Underground storage facilities. An underground storage facility includes any enclosed structure, container, tank or other enclosed stationary devices used for storage or containment of pollutants as defined in Section 376.301(12), F.S. or any contaminant as defined in Sect ion 403.031(1), F.S. Nothing in this paragraph is intended to include septic tanks, enclosed transformers or other similarly enclosed underground facilities.... Underground facilities for transportation of wastewater or pollutants as defined in Section 376.301(12), F.S. or any contaminant as defined in Section 403.031(1), F.S. excluding natural and liquified petroleum gas. Underground facilities for transportation of waste effluent or pollutants or contaminants include piping, sewer lines, and ducts or other conveyances to transport pollutants as defined in Section 376.301(12), F.S., and contaminants as defined in Section 403.031(1), F.S.... Protestants contend that the proposed rules are contained in two separate chapters of the Florida Administrative Code with no bridge between them. Under such circumstances, they contend the rules fail to adequately define either facility in either chapter, and that the rules are therefore vague, arbitrary and capricious. Protestants' contention is not persuasive. Proposed rule 17-3.021(35) defines "underground storage facility" or "underground transportation facility" as meaning that 10 percent or more of the facility is buried below the ground surface. Proposed rules 17-4.245(3)(c) and (d) address what type of facility is included within the terms "underground storage facility" and "underground transportation facility." Notably, Rule 17-4.021, F.A.C., provides: Definitions contained in other chapters of the Department's rules may be utilized to clarify the meaning of terms used herein unless such terms are defined in Section 17-4.020, F.A.C., or transfer of such definition would defeat the purpose or alter the intended effect of the provisions of this chapter. Under the circumstances of this case, the rules are appropriately read together. So read, the construction requirements for "underground storage facilities" and "underground transportation facilities", as required by proposed rule 17-4.245(3)(c) and (d), are applicable if 10 percent or more of the containment device used for the storage or transport of pollutants is buried below the ground surface, and the proposed rules are not vague, arbitrary or capricious. Proposed rule 17-3.021(39) defines "Zones of Protection" as follows: "Zones of Protection" shall mean two concentric areas around a major public community drinking water supply well(s) or wellfield(s) drawing from a G-I aquifer whose boundaries are determined based on radii from the well or wellfields of 200 feet and five years groundwater travel time respectively. Protestants contend that the definition of "Zones of Protection" is vague, arbitrary and capricious because nowhere within the proposed rules is "G-I aquifer" defined. protestants' contention is not persuasive. Proposed rules 17-3.403(1) and (7) adequately explain what is meant by "G-I aquifer", and proposed rule 17-3.403(8) sets forth the metodology for calculating the zones of protection. The definition of "Zones of Protection", set forth in proposed rule 17-3.02(39) is not vague, arbitrary or capricious, because of any failure to define "G-I aquifer." Mapping Priorities When considering whether to reclassify an aquifer or aquifer segment as G-I, proposed rule 17-3.403(5)(e)2 requires that the aquifer or aquifer segment: Be specifically mapped and delineated by the Department on a detailed map of a scale which would clearly depict the applicable zones of protection. Maps will be grouped and submitted for reclassification generally on a regional basis. Mapping priorities shall follow the Commission directive of February 27, 1985. The remaining areas of the state will be mapped by the Department as time and resources allow. The mapping priority directive referred to in purposed Rule 17-3.403(5)(e)2a, was an oral directive of the ERC that Pinellas, Hillsborough, Pasco, Hernando, and Citrus Counties, referred to as the Middle-Gulf region, be mapped first. That directive has not been reduced to writing and, consequently, a copy thereof has never been available for inspection. Categories of G-I Aquifers and determination of zones and protection Proposed rules 17-3.403(7) and (8), respectively, set forth the eligibility criteria for reclassification as G-I aquifers and the methodology whereby the boundaries of the zones of protection are established. To this end, proposed rule 17- 3.403 (7) provides: Categories of G-I aquifers. For aquifers or aquifer segments to be eligible for potential reclassification as G-I aquifers one of the following criteria must be met: That the aquifer or aquifer segment under consideration be within the zones of protection of a major public community drinking water supply well(s) or wellfield(s) withdrawing water from unconfined aquifers or from leaky confined aquifers.... (b)(. reserved.) Proposed rule 17-3.403(8) provides: Determination of the boundaries of the zones of protection. (a) The boundaries of the zones of protection shall be based on radii from the wellhead or wellfield (if closely clustered, so that the five year zones of protection are overlapping) measured in 200 feet for the inner zone and five years for the outer zone. The radius of the outer zone shall be determined using the following formula: percent.x4n where Q = permitted average daily flow from the well (measured in cubic feet per day); T = five years (1825 days); 3.14 = mathematical constant pi; r = radius (feet); h distance from the top of the producing aquifer to the bottom of the hole (feet); n effective porosity. Protestants contend that the foregoing provisions of the proposed rules are vague, arbitrary and capricious because the wells that would be subject to and around which a zone of protection would be established cannot be identified or, if identifiable, do not comport with the Department's intent or interpretation. Protestant's concerns are not without merit. To be eligible for consideration as a G-I aquifer, proposed rule 17-3.403(7) requires that the aquifer segment be within the zones of protection of a "major public community drinking water supply well(s) or wellfield(s). Proposed rule 17- 3.021(17) provides that "major public community drinking water supply" shall mean: those community water systems as defined in Section 17-22.103(5), F.A.C., that are permitted by consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater. Community water system" is defined by Section 17-22.103(5) as: a public water system which serves at least IS service connections used by year- round residents or regularly serves at least 25 year-round residents. Facially then, the proposed G-I rules are applicable to "community water system" that hold a consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater", and which are withdrawing from unconfined or leaky confined aquifers. Notably, the rule does not ascribe the 100,000 gpd permitted rate of withdrawal to each well, but to a permit held by a community water system. Accordingly, under the literal reading of the proposed rules, each well covered by the consumptive use permit would be subject to a zone of protection regardless of its individually permitted rate, so long as it was withdrawing from an unconfined or leaky confined aquifer. While there may be legitimate reasons to designate zones of protection around wells, regardless of their individual permitted rate when the community water system holds a consumptive use permit to withdraw groundwater at a 100,000 gpd average, the Department advanced none. To the contrary, the Department contended that zones of protection were only to be established around a well that was permitted to withdraw an average daily amount of 100,000 gallons or greater. Under the circumstances, the provisions of proposed rules 17-3.403(7) and (8) are arbitrary and capricious. 6/ The "Vv" and "Tv" formulae Proposed rule 17-3.403(7)(a) prescribes the methodology where by vertical travel time will be calculated, and therefore whether a particular aquifer will be classified as confined or leaky confined. To this end, the proposed rule provides: ... Determination of vertical travel time for leaky confinement will be by application of the following formulae: Vv= Kv h/nl where: Vv= vertical velocity (feet/day). Kv= vertical hydraulic conductivities of the surficial aquifer and underlying confining bed materials (feet/day). h= head difference between water table in the surficial aquifer and the potentiometric surface of the producing aquifer (feet). n = effective porosities of the surficial aquifer and underlying confining bed materials. 1 = distance from the water table to the top of the producing aquifer (feet). Tv= 1/Vv 365 where: Tv= vertical travel time (years). 1 = same as above. Vv= same as above. The "Vv" formula and the "Tv" formula are valid formulae, and are commonly used by hydrogeologists to calculate the vertical velocity and vertical travel time of groundwater. As proposed, the formulae present a reasonable methodology for computing the vertical velocity and vertical travel time of groundwater if the well is producing from one aquifer. The formulae cannot, however, as hereafter discussed, be reasonably applied if tee well is producing from multiple aquifers or if another aquifer intervenes between the surf aquifer and the producing aquifer. While not the most prevalent occurrence in the state wells in the Middle-Gulf regions often do penetrate more than one aquifer and do produce water from more than one aquifer. The rule defines the "Kv" element of the "Vv" formula as the "vertical hydraulic conductivities of the surficial aquifer and underlying confining bed materials (feet/day)." This is a reasonable definition and will produce a scientifically valid result provided the well does not penetrate multiple aquifers. Should the well penetrate multiple aquifers, the values derived for vertical velocity ("Vv") and vertical travel time ("Tv") will not be accurate since the hydraulic conductivities of the intervening aquifers are not, by the rule definition, factored into the calculation of "Kv". Under such circumstances, whether an aquifer was classified as confined or leaky confined would not be determined by a valid "Kv" but, rather, by chance. Protestants also contend that the rule is vague, arbitrary and capricious because it does not specify the methodology by which "Kv" is to be calculated. There are, however, methodologies commonly accepted by hydrogeologists to derive a scientifically valid "Kv", whether the well penetrates one or more than one aquifer. The infirmity of the rule is not its failure to specify a methodology, but its to include data necessary to produce a meaningful result. The rule defines the "n" element of the Vv formula as "effective porosities of the surficial aquifer and underlying confining bed materials." This is a reasonable definition and will, though the application of commonly accepted methodologies, produce a scientifically valid result. 7/ The rule defines the element "Delta h" in the Vv formula as the "head difference between the water table in the surficial aquifer and the potentiometric surface of the producing aquifer (feet)", and defines the element "1" as the "distance from the water table to the top of the producing aquifer (feet)." These elements are utilized in the formula to calculate a gradient, and must be measured using the same points of reference to yield a meaningful result. To this end, the proof demonstrates that the definitions are reasonable since they utilize the same points of reference, and that when applied in accordance with accepted hydrogeologic practice will produce a scientifically valid gradient. (See Department exhibit 7). Protestants contend, however, that the definitions of "Delta h" and "1" are vague, arbitrary and capricious because they do not specify when the measurements should be made, do not define "producing aquifer", and do not define "top" of the producing aquifer. For the reasons that follow, Protestants' contentions are found to be without merit. While a water table is a dynamic surface subject to frequent, if not daily fluctuation, resulting from variations in rainfall and the demands of man, and while a potentiometric surface is likewise a dynamic elevation that changes with time and season, protestants failed to demonstrate that there was any particular date or dates that would be most appropriate to make such calculations. Rather, protestants contended that unless such measurements were taken contemporaneously, any derivation of "Delta h" and "1" would not be reliable. While such might be the case, the rule does not mandate a divergence from the accepted hydrogeologic practice of taking such measurements contemporaneously. While the rule does not define "producing aquifer," it is an accepted hydrogeologic term and not subject to confusion. The only confusion in this case was the introduction of the issue of multiple producing aquifers and protestants' contentions that this rendered the Vv formula vague, arbitrary and capricious since it did not factor in such a consideration. Protestants' contention does not, however render the term "producing aquifer" vague. The sole purpose of the Vv and Tv formulas are to determine whether the aquifer from which water is being produced is leaky confined. To establish this, the formulae are applied to calculate whether the vertical travel time is five years or less. If a well is withdrawing water from more than one aquifer it may be necessary to calculate Vv and Tv for each aquifer to discern which of those aquifers are within the 5 year vertical travel time threshold, and therefore subject to G-I reclassification. To this end the rule is not vague, and would adequately address the multiple producing aquifer scenario. While the rule doe not define "top" of the producing aquifer, this term is an accepted hydrogeologic term and is not subject to confusion. In application there may, however, be disagreements among hydrogeologists as to where this line should be established because geologic boundaries are fine gradations, and not sharp lines which would lend themselves to the designation of precise points of reference. This is not, however, a failure of the rule, but a peculiarity of nature, and is subject to scientific proof. Notably, protestants did not demonstrate that "top" of the producing aquifer could be defined with reference to a fixed point. Under the circumstances, "top" of the producing aquifer is a reasonable reference point. Zones of Protection Proposed rule 17-3.408 provides: Determination of the boundaries of the zones of protection shall be based on radii from the wellhead or wellfield (if closely clustered, so that the five year zones of protection are overlapping), measured in 200 feet for the inner zone and five years for the outer zone. The radius of the outer zone shall be determined using the following formula: QT 2 3.14 hn where Q = permitted average daily flow from the well (measured in cubic feet per day); T = five years (1825 days); 3.14 = mathematical constant pi; r = radius (feet); h distance from the top of the producing aquifer to the bottom of the hole (feet); n effective porosity. For the purpose of this calculation the following effective porosities for representative Florida aquifers will be used: Floridan .05 Sand and Gravel .2 Biscayne .15 Surficial .2 The Department shall use more site-specific values for "Q", "n", or "h" when available for designation of the zones of protection by the Commission. Proposed rule 17-3.403(8)(a) provides that the inner zone of protection shall be based on a radius from the wellhead or wellfilled, as appropriate, of 200 feet. While denoted as an arbitrary radius, the 200 foot radius was not derived without fact or reason. Rather, it was a result reached at the workshops after consideration of existing regulations that establish buffer zones of 200-500 feet between a public water supply and a pollution source. Conceptually, the 200 foot zone was adopted because it is so small and so close to the well that it essentially constituted a zone of protection of the well head by preventing contaminants from moving into the well opening directly or the annular space around the well casing. Accordingly, the 200 foot zone has a reasonable basis. Its actual delineation is, however, as flawed as that of the five year zone discussed infra. The "r" formula defines the outer zone of protection, and calculates it as a radius equal to the distance groundwater would flow in five years toward the well. The basis for the "r" formula is the formula used to calculate the volume of a cylinder. That formula, V = pi r2 h, yields a simple volumetric measurement without any consideration of velocity. By the introduction of the element "n" (effective porosity), the "r" formula introduces a velocity component which would, properly applied, produce a radius equal to the distance groundwater would flow in 5 years. 8/ As proposed, however, the rule would establish a meaningless line around a well. Under the proposed rule, the Department would calculate "r" based on specified effective porosities ("n") for the Floridan, Biscayne, sand and gravel, and surficial aquifers absent site specific data. The Department is, however, under no requirement to generate site specific data, and currently is mapping the Middle-Gulf region based on the values established by the rule. Absent chance, the areas mapped will bear no relationship to groundwater travel time. The lithology of an aquifer and the surrounding layers is varied and diverse, and directly affects the direction and velocity of groundwater flow. By assuming "n", the "r" formula ignores the varied lithology, and produces a radius that would seldom, if ever, represent the actual rate at which groundwater moved toward any well. 9/ The zone thus circumscribed is an illusion since the groundwaters and contaminants within it may move at a rate significantly greater than or less than 5 years travel time. Notably, the Department has conducted no study or test to validate its proposed methodology. The element "Q" in the "r" formula is defined as the "permitted average daily flow from the well (measured in cubic feet per day)." Protestants contend that such definition is vague, arbitrary and capricious because the Department proposes to rely on consumptive use permits issued by the various water management districts to derive "Q", and such permits would not necessarily provide the requisite data. While the proof demonstrates that "Q" cannot always be derived by reference to a consumptive use permit, this does not render the definition of "Q" vague, arbitrary, or capricious. Rather, "Q" is a factual matter, and subject to a factual derivation through reference to consumptive use permits and other site specific data. The element "T" in the "r" formula is defined as "five years (1825) days." By its inclusion, the Department proposes to circumscribe the outer zone of protection at five years groundwater travel time. The concept of a zone of protection is premised on the theory that restrictions should be placed on discharges to groundwater within an area proximate to a public water supply for public health and safety concerns. The five year standard, which is found throughout the rules, was based on the theory that if a contaminant was introduced to groundwater a period of time should be allowed to discover the contamination and remove it or make provision for an alternate water supply before the contaminant reached the public water supply. The five years proposed by the rule was not, however, founded on fact or reason. During the workshops that under scored the proposed rule, the time factor was the subject of considerable discussion and ranged from less than two years to greater than ten years. Based on its own in-house search, the Department initially proposed a 10-year standard. That search revealed that it took 10 to 15 years between the time a contaminant was discovered and cleanup could commence, and between seven and eight years between the time a contaminant was introduced into groundwater and it discovery. Notwithstanding the results of its own in-house search, the Department, in the face of debate, elected to "compromise" and propose a five-year standard. Such standard was not the result of any study to assess its validity, and no data, reports or other research were utilized to derive it. In sum, the five- year standard was simply a "compromise", and was not supported by fact or reason. As previously noted, the lithology of an aquifer and the surrounding layers is varied and diverse, and directly affects the direction and velocity of groundwater flow. The effective porosity of those materials in the Floridan aquifer canvary from to .4 at various places. The rule proposes, however, to use an effective porosity for the Floridan aquifer of .05 to establish "r." The value ascribed to "n" is a critical value, as previously discussed in paragraph 65. It also has a profound impact on the aeral extent of the zone of protection. For example, assuming "Q" equals 3 million gallons and "h" equals 600 feet, an "n" of .02 would result in a radius of 4,406 feet or 1,400 acres, an "n" of .03 would result in a radius of 3,578 fee or 934 acres, an "n" of .05 would result in a radius of 2,787 feet or 560 acres, and an "n" of .2 would result in a radius of 1,393 feet or 140 acres. While an effective porosity of 05 for the Floridan aquifer may be a reasonable value at a particular site, it is not a value that can be reasonably ascribed to the Floridan in general. For this reason, and the reasons heretofore set forth, the rule's specification of an effective porosity of .05 for the Floridan aquifer is unreasonable. Proposed rule 17-3.403(8)(a), sets forth the manner in which the zones of protection will be drawn around a well or wellfield. That proposed rule provides: For well fields whose individual zones of protection overlap due to clustering, a single zone of protection will be calculated in the following manner: Using the permitted average daily withdrawal rate of the wells with overlapping zones of protection, the area on the surface overlying the aquifer equal to the sum of the areas of the five year zones of protection of the individual wells, shall be used to define the area which encircles the perimeter of the wellfield. In cases where a zone of protection of a single well protrudues beyond the calculated perimeter or when the configuration of the wellfield is irregular, the perimeter will be shaped to accommodate the configuration. The surface are encircling the perimeter of the wellfield shall not exceed the total surface area of the overlapping zones of protection for individual wells. In the case of unclustered wells within a wellfield, individual zones of protection around each well will be calculated. As previously discussed, the proposed G-I rules are facially applicable to "community water systems" that hold a " consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater," and which are withdrawing from unconfined or leaky confined aquifers. Under proposed rule 1773.403(8)(a), the five-year zone of protection would be drawn around each of these wells. If the wells are located so close to each other that the five year zones of protection are overlapping (clustered), those wells would be deemed a wellfield by rule definition and a five year zone of protection would be established around it. The proposed rule's description at how to determine and configure a zone of protection around a wellfield is however, vague and ambiguous. While the rule provides that when the configuration of the wellfield is "irregular", the perimeter will be shaped to accommodate the configuration", it sets forth no standard by which the perimeter will be established. Effectively, the rule vests unbridled discretion in the Department to establish the configuration of a wellfield. The Economic Impact Statements Pursuant to the mandate of Section 120.54(2), Florida Statutes, the Department prepared economic impact statements for the proposed revisions to Chapters 17-3 and 17-4, Florida Administrative Code. The economic impact statements were prepared by Dr. Elizabeth Field, the Department's chief economist, an expert in economics. Dr. Field developed the economic impact statements by examining the proposed rules and discussing their potential impact with Department staff. Additionally, Dr. Field attended the public workshops that were held concerning the proposed rules, and solicited input from those participants. The Florida Home Builders Association and the Florida Petroleum Council submitted data for her consideration, but none of the petitioners, although some were represented at such workshops, responded to her requests for information. The economic impact statements prepared by Dr. Field to address the proposed rules conclude that, apart from the cost to the Department for mapping, there are no direct costs or economic benefits occasioned by the rules. Dr. Field's conclusion was premised on the fact that the proposed rules only establish the eligibility criteria for reclassification of an aquifer to G-I and the standards for discharge to that aquifer. Under the proposed rules, further rulemaking would be required to actually designate a specific aquifer as G-I, and delineate a zone of protection. 10/ Pertinent to this case, proposed rule 17-3.403, provides: The intent of establishing G-I eligibility criteria is to determine which aquifer or aquifer segments qualify for potential reclassification to G-I aquifers. Adoption of these criteria does not imply nor does it designate aquifer or aquifer segments as G-I. Such designation can only be achieved through reclassification by the Commission after eligible segments have been mapped by the Department. (6)... the following procedure shall be used to designate Class G-I aquifers: Rulemaking procedures pursuant to Chapter 17-102, F.A.C., shall be followed; Fact-finding workshops shall be held in the affected area; All local, county, or municipal governments, water management districts, state legislators, regional water supply authorities, and regional planning councils whose districts or jurisdictions include all or part of a proposed G-I aquifer shall be notified in writing by the Department at least 60 days prior to the workshop; A prominent public notice shall be placed in an appropriate newspaper(s) of general circulation in the area of the proposed G-I aquifer at least 60 days prior to the workshop. The notice shall contain a geographic location map indicating the area of the zones of protection and a general description of the impact of reclassification on present and future discharges to groundwater. A notice of a G-I workshop shall be published in the Florida Administrative Weekly prior to the workshop(s). At least 180 days prior to the Commission meeting during which a particular zone of protection will be considered for reclassification, the Department will provide notice in the Florida Administrative Weekly and appropriate newspaper(s) of the intended date of the Commission meeting. The Commission may reclassify an aquifer or aquifer segment as a G-I aquifer within specified boundaries upon consideration of environmental, technological, water quality, institutional (including local land use comprehensive plans), public health, public interest, social and economic factors. When considering a reclassification an aquifer or aquifer segment shall: ....(Be within the zones of protection of a major public community drinking water supply well(s) or wellfield(s) withdrawing water from unconfined or from leaky confined aquifers.).... Be specifically mapped and delineated by the Department on a detailed map of a scale which would clearly depict the applicable zones or protection. Maps will be grouped and submitted for reclassification generally on a regional basis. Mapping priorities shall follow the Commission directive of February 27, 1985. The remaining areas of the state will be mapped by the Department as time and resources allow. (Emphasis added). While, if and when applied, the proposed rules would certainly have a direct economic impact as a consequence of a reclassification of an aquifer to G-I and the designation of a zone of protection, as well as the standards for discharge to that aquifer, such costs at this stage are not direct or are not quantifiable. When mapped and the zones of protection identified, a reasonable assessment of the economic cost or benefit of the proposal can be addressed. This is specifically reserved by the Commission whereby its decision to reclassify an aquifer as G-I will, pursuant to proposed rule 17-3.403(6) follow rule making procedures and be based on consideration of economic factors. This result obtains whether the affected party is a small business or some other entity. In reaching the conclusion that the economic costs or benefits of the proposed rules, apart from the cost of mapping, do not at this stage have a direct or quantifiable impact, I have not overlooked the "announcement effect" that is occasioned by the announcement of a governmental agency to regulate an activity. Such announcement certainly has a chilling effect on the community that may reasonably be impacted. The economic impact is, however, speculative or not quantifiable in the instant case. Further, the proof does not demonstrate any incorrectness or unfairness in the proposed adoption of the rules occasioned by the EIS prepared in this case.
The Issue The issue is whether Respondent HBJ Investments, Inc. is entitled to an environmental resource permit to facilitate the construction of the Betty Jones Spa on property adjacent to property owned by Petitioner.
Findings Of Fact On November 17, 1998, Respondent HBJ Investments, Inc. (Applicant) filed an application (Application) with the South Florida Water Management District (District) for an environmental resource permit (ERP). The Application is for a Standard General (minor systems) ERP. The Application states that the proposed surface water management system is to serve a 11,564 square foot health spa with associated infrastructure improvements, such as parking, utilities, landscaping, and a stormwater detention facility. Section H of the Application responds to form questions that are intended to determine whether an application meets the requirements of a standard general ERP for a minor surface water system. Among the threshold requirements is that the proposed discharges from the site "will meet State water quality standards, and the surface water management system will meet the applicable technical criteria for stormwater management in the Basis of Review." Another threshold requirement is that the proposed activities will not cause significant adverse impacts individually or cumulatively. The Application states that the water quality treatment system will be on-line detention with effluent filtration. The Application and related documents describe the system in greater detail. The system consists of drains, inlets, a swale, an underground vault to provide effluent filtration through a sand filter and perforated pipe, an internal oil and grease skimmer, a control box, and a 15-inch diameter reinforced concrete pipe providing outfall from the vault. By Notice of Final Agency Action for Approval dated February 4, 1999, the District proposed the issuance of a "Standard General for Minor Surface Water Management Systems" ERP for the construction, operation, and maintenance of the proposed system (Permit). Permit Specific Condition 2 requires: "The discharges from this system shall meet state water quality standards as set forth in Chapter 62-302 and Rule 62-4.242, F.A.C., for class waters equivalent to the receiving waters." Permit Specific Condition 8 requires, for vault systems, that the system become dry within 72 hours after a rainfall event. Permit Specific Condition 9 requires the operation and maintenance entity to submit inspection reports for inspections to be performed every 18 months. Permit Specific Condition 10 requires a water quality monitoring program for systems, such as the proposed system, using an internal oil and grease skimmer. This condition obligates HBJ to take three samples during each of the first two annual rainy seasons following the commencement of operation of the system. The monitoring must take place immediately after rainfall events of sufficient magnitude to cause a discharge from the outfall structure. If the discharged water does not meet water quality standards for oil and grease, as established by Rule 62.302.510(3)(k), Florida Administrative Code, then the permittee must alter the system to attain compliance for this water quality parameter. The subject parcel is bounded by Fourth Avenue South on the north, First Street South on the east, Second Street South on the west, and an unnamed alley on the south. This site is just south of Al Lang Field. In its present state, the parcel is nearly entirely pervious surface. Some of the stormwater flowing onto the parcel percolates into the soils, and the remainder flows into City of Saint Petersburg stormwater sewers, from which it is carried about two city blocks to Tampa Bay, where it is discharged. The parcel was formerly used for single-family residential housing, but is now mostly cleared. The runoff from the site presently carries mostly sediments. After the proposed construction, 79 percent of the parcel would consist of impervious surface. Although small areas of the developed parcel might remain vegetated, and thus add nutrients into the runoff, the primary change in the runoff will consist of the addition of automobile-related contaminants, including, but not limited to, oil and grease. HBJ's engineer designed the proposed surface water management system to treat the first one-half inch of stormwater runoff. The engineer's report notes, in a letter dated November 13, 1998, that siltation in the vault reduces storage volume, so it is "required that cleaning be done every six (6) months." The report suggests the removal of grass clippings from the parking area, so that they are not transported to the retention vault. The report suggests that the underdrain system should be backflushed periodically, and the control structure should be checked monthly and all debris cleared. In general, the system would collect runoff from the roof downspouts and parking area. The system would provide treatment of the first 1/2 inch of runoff by capturing it in the vault, where it would filter through a layer of several cubic feet of sand before entering a perforated pipe leading to the City stormwater sewer. Runoff from rainfall in excess of the first 1/2 inch would receive little, if any, treatment. It is implicit that the first 1/2 inch of rainfall contains the first flush of contaminants from impervious surfaces. Nothing in the record specifies the efficacy of treatment provided by this standard, although it obviously is less than 100 percent efficient because of the higher standard imposed upon systems discharging into Outstanding Florida Waters (OFW). However, a pre- and post-development analysis of the runoff from the subject parcel would reveal an unknown additional volume of runoff from the developed site, due to the replacement of pervious surface with impervious surface. It is unclear whether the developed site would generate a reduced volume of sediments in this increased volume of runoff. Although little vegetated surface would exist post-development, the record does not reveal the extent to which the pre-development pervious area fails to capture the sediments prior to their entering the City stormwater system. More problematic are the automobile-related contaminants, such as oil and grease, that will be introduced into the runoff by the developed site. Presumably, the runoff from the undeveloped site contains few, if any, such contaminants. Thus, any automobile-related contaminants discharged from the surface water management system would likely be an increase from the amount of such contaminants presently discharged from the site. The runoff from the developed site would enter the City of Saint Petersburg stormwater sewer system and would be released in the nearby Tampa Bay. The record does not disclose the stormwater sewer line transporting the discharge, nor the outfall of the line into Tampa Bay. By stipulation, the parties agreed that Tampa Bay is an OFW and that discharge from the developed site would enter the City of Saint Petersburg stormwater sewer system. Tampa Bay is classified as Class II waters, which are approved for shellfish harvesting. The record does not disclose the point of discharge of the City stormwater line that would receive discharge from the developed site. However, the proximity of the site to Tampa Bay strongly suggests that the outfall would be in Tampa Bay, and it is only slightly less probable that the outfall would be at a point in the bay in the immediate vicinity of the site. The record suggests that the waters of Tampa Bay likely to receive the discharge from the site are impaired. For example, water quality conditions mandated the closing of "Lower Tampa Bay" to shellfish harvesting, for an unstated period of time, effective at sunset on July 5, 1999. Also, the Department of Environmental Protection listed two bayous in the immediate vicinity of the site as noncompliant with federal water quality standards due to excessive coliform bacteria counts and nutrients and insufficient levels of dissolved oxygen. The Basis of Review (BOR) is a document adopted by the District. It contains specific "criteria" for permitting. However, as BOR Section 1.3 explains, the goal of these criteria is to meet District water resource objectives, and the criteria are "flexible." Alternative methods of meeting "overall objectives" may be acceptable, depending upon the "magnitude of specific or cumulative impacts." The criteria, which are flexible, are the means by which the District assures that it meets its objectives, which are not flexible. BOR Section 3.1.0 recognizes that "a wide array of biological, physical and chemical factors affect the functioning of any wetland or other surface water community. Maintenance of water quality standards in applicable wetlands and other surface waters is critical to their ability to provide many of these functions." BOR Section 3.1.0 elaborates: "It is the intent of the Governing Board [of the District] that the criteria in subsections 3.2 through 3.2.8 be implemented in a manner which achieves a programmatic goal and a project permitting goal of no net loss of wetlands or other surface water functions." BOR Section 3.1.1 requires that an applicant provide "reasonable assurance" of several things. BOR Section 3.1.1(a) requires that "a regulated activity will not adversely impact the value of functions provided to fish, wildlife and listed species, including aquatic and wetland dependent species, by wetlands and other surface waters and other water related resources of the District. (paragraph 40D-4.301(1)(d), F.A.C.) (see subsection 3.2.2)." BOR Section 3.1.1(c) provides that: a regulated activity will not adversely affect the quality of receiving waters such that the water quality standards set forth in Chapters 62-3, 62-4, 62-302, 62-520, 62-522 and 62-550, F.A.C., including any antidegradation provisions of Sections 62-4.242(1)(a) and (b), 62-4.242(2) and (3), and 62-302.300 and any special standards for Outstanding Florida Waters . . . set forth in sections 62-4.242(2) and (3), F.A.C., will be violated (paragraph 40D-4.301(1)(e), F.A.C.). BOR Section 3.1.1(d) provides that "a regulated activity . . . located in close proximity to Class II waters . . . will comply with the additional criteria in subsection 3.2.5 (paragraph 40D-4.302(1)(c), F.A.C.)." BOR Section 3.1.l(f) provides that "a regulated activity will not cause adverse secondary impacts to the water resources (paragraph 40D-4.301(1)(f), F.A.C.) (see subsection 3.2.7)." BOR Section 3.1.1(g) provides that "a regulated activity will not cause adverse cumulative impacts upon wetlands and other surface waters . . . (paragraph 40D-4.302(1)(b), F.A.C.) (see subsection 3.2.8)." BOR Section 3.2.4 provides that an applicant must provide "reasonable assurance that the regulated activity will not violate water quality standards in areas where water quality standards apply. . . . The following requirements are in addition to the water quality requirements found in Chapter 5." BOR Section 3.2.4.2(c) provides that the applicant must address the long-term water quality impacts of a proposed system, including "prevention of any discharge or release of pollutants from the system that will cause water quality standards to be violated." BOR Section 3.2.5 provides: The special value and importance of shellfish harvesting waters to Florida's economy as existing or potential sites of commercial and recreational shellfish harvesting and as a nursery area for fish and shell fish is recognized by the District. In accordance with section 3.1.1.(d), the District shall: (b) deny a permit for a regulated activity in any class of waters where the location of the system is adjacent or in close proximity to Class II waters, unless the applicant submits a plan or proposes a procedure which demonstrates that the regulated activity will not have a negative effect on the Class II waters and will not result in violations of water quality standards in the Class II waters. BOR Section 3.2.7 provides that an applicant must provide "reasonable assurance" that "a regulated activity will not cause adverse secondary impacts to the water resource" as described in this section. However, this section explicitly disregards negligible or remotely related secondary impacts. BOR Section 3.2.8 provides that an applicant must provide "reasonable assurance" that "a regulated activity will not cause unacceptable cumulative impacts upon wetlands and other surface waters " BOR Section 4.2 limits off-site discharge "to amounts which will not cause adverse off-site impacts." For a proposed activity within an open drainage basin, as is the subject proposed activity, the allowable discharge is (presumably the greatest of) any amount determined in previous District permits, the legally allowable discharge at the time of the permit application, or historic discharge. Historic discharge is the peak rate at which runoff leaves a parcel of land by gravity under existing site conditions. BOR Section 5.1 requires that proposed discharges meet applicable state water quality standards. This chapter of the BOR requires that proposed systems satisfy certain quantitative criteria, depending on the type of water treatment system. However, BOR Section 5.1 warns: in certain instances a design meeting those standards may not result in compliance with the state water quality standards referenced above. Unless an applicant has provided reasonable assurance that a design will not cause or contribute to a violation of state water quality standards, the District may apply more stringent design and performance standards than are otherwise required by this chapter. Projects designed to the criteria found in this section shall be presumed to provide reasonable assurance of compliance with the state water quality standards referenced above. . . . BOR Section 5.2 sets quantitative criteria for various types of surface water management systems. The subject system is a detention, on-line treatment system. BOR Section 1.7.5 defines "detention" as the "delay of storm runoff prior to discharge into receiving waters." BOR Section 1.7.28 defines "on-line treatment system" as a "dual purpose system that collects project runoff for both water quality and water quantity requirements. Water quality volumes are recovered through percolation and evaporation while water quantity volumes are recovered through a combination of percolation, evaporation, and surface discharge." BOR Section 5.2.b applies to "[d]etention with effluent filtration system (manmade underdrains)." BOR Section 5.2.b.1 provides that proposed activities draining less than 100 acres "shall treat the runoff from . . . the first one-half inch runoff." BOR Section 5.2.b.6 adds: "Maintenance of filter includes proper disposal of spent filter material." BOR Section 5.2.c applies to "on-line treatment system[s]." This section also requires the treatment of the first one-half inch of runoff. However, BOR Section 5.2.e provides: Projects discharging directly into Outstanding Florida Waters (OFW) shall be required to provide treatment for a volume 50 percent more than required for the selected treatment system . . .. Applicant has provided reasonable assurance that the proposed surface water management system would not cause adverse water quantity impacts to receiving waters and adjacent lands and would not cause flooding. In terms of water quantity, the proposed system is designed to meet the requirements of the ten-year storm. The subject site is a short distance from Tampa Bay, and, as already noted, it is very likely that the runoff discharges into Tampa Bay at a location not far from the subject site. Thus, water quantity and flooding are irrelevant to this case. However, Applicant has not provided reasonable assurance that the proposed surface water management system would not cause adverse impacts to the value of functions provided to fish and wildlife by nonwetland surface waters and would not adversely affect the quality of receiving waters. The receiving waters of the discharge from the subject site are Class II waters that are OFW. However, these waters are also impaired sufficiently as to be in violation of certain federal water quality standards and to require the closure, at least at times, of shellfish harvesting. There are three deficiencies in the proposed permit. First, it does not specify, in clear and enforceable language, an inspection and maintenance program, which includes the undertaking by the Applicant to backwash the system at specified intervals, to replace the sand filtration medium at specified intervals, to dispose of the sand filtration medium so that the captured contaminants do not reenter waters of the state, to monitor the water discharged from the oil and grease skimmer at specified intervals following the first two years' monitoring, and generally to take any necessary action to correct deficiencies uncovered from inspections. Second, the treatment of the first 1/2 inch of runoff is insufficient for the system, which is discharging directly into an OFW. BOR Section 5.2.e raises this standard to 3/4 inch. Direct discharges requires the identification of the first receiving waters. Receiving waters are waters of the state that are classifiable as Class I-V waters. Receiving waters thus do not include waters in a stormwater sewer pipe, which are not waters of the state nor are they classifiable. Water quality determinations often require comparison of the quality of the discharged water with quality of the receiving waters. The off-site piping of the discharged water does not preclude such comparison. In such case, the analysis extends to the first receiving waters into which the pipe empties. The District's argument to the contrary invites circumvention of those provisions enacted and promulgated for the protection of OFWs. For example, several owners of land abutting an OFW could establish a jointly owned stormwater sewer line so that the point of comparison for their discharge would be the waters in the pipe rather than the OFW. Third, Applicant failed to submit a plan or propose a procedure demonstrating that the proposed activity would not have a negative effect on the Class II waters of Tampa Bay and would not result in violations of water quality standards in these Class II waters. The District failed to determine the outfall of the discharge from the subject site, so it failed to enforce the requirement of the plan required by BOR 3.2.5 for the protection of the special value of Class II waters. Although required to account for cumulative impacts, the plan will necessarily reflect the characteristics of the site--e.g., 1.6 acres contributing largely automobile-based contaminants and not nutrients--and the characteristics of the receiving waters--e.g., Tampa Bay is vast and relatively impaired, though, in the vicinity of the subject site, more likely due to excessive nutrients.
Recommendation It is RECOMMENDED that the Southwest Florida Water Management District enter a final order denying the ERP application of HBJ Investments, Inc. DONE AND ENTERED this 23rd day of December, 1999, in Tallahassee, Leon County, Florida. ROBERT E. MEALE Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 23rd day of December, 1999. COPIES FURNISHED: E. D. "Sonny" Vergara, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 John R. Thomas Wyckoff & Thomas, P.A. 233 Third Street North, Suite 102 Saint Petersburg, Florida 33701 Michael Jacobs Director, Legal Affairs 25 Second Street North, Suite 160 Saint Petersburg, Florida 33701 Anthony J. Mutchler Assistant General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899
