Findings Of Fact This application is a request for a consumptive use permit for two wells located in Pasco County, Florida, within the Pithlachascotee Basin. The subject wells are also located in that area wherein the Board of Governors of the Southwest Florida Water Management District declared a water shortage in Order No. 76-3D, Southwest Florida Water Management District. The application seeks an average daily withdrawal of 95,000 gallons with a maximum daily withdrawal of 360,000 gallons. The use of this water is for public supply involving effluent disposal by on-site percolation and ponding. This-use was existing prior to January 1, 1975 with am average daily withdrawal for 1974 of 74,000 gallons. The testimony presented by staff members of the Southwest Florida Water Management District establishes that the consumptive use for which a permit is sought will not violate any of the criteria set forth in Subsections 163- 2.11(2)(3) or (4), Florida Administrative Code, except that the use may significantly induce salt water encroachment. No evidence was presented showing that the sought for consumptive use will, in fact, significantly induce salt water encroachment. In the twelve month period ending October, 1975, applicant's highest average daily withdrawal was 81,000 gallons. This time frame corresponds to that time frame referred to in paragraph 1 of Water Shortage Order No. 76-3D, Southwest Florida Water Management District. In view of Water Shortage Order No. 76-3D, Southwest Florida Water Management District, the staff recommends granting of the permit for an average daily withdrawal of 81,000 gallons and a maximum daily withdrawal of four times that figure or 234,000 gallons. The staff further recommends imposition of the following conditions: That the permittee shall install totalizer flow meters of the propeller driven type on all withdrawal points covered by the permit with the exception of those wells which are currently ganged together using a single meter. That the permittee shall submit to the District a record of his pumpage for each meter, said pumpage to be read on a monthly basis and submitted quarterly to the District on April 15, July 15, October 15, and January 15 for each preceding calendar quarter. That all individual connections to the system be metered. That the permittee have water samples from all wells permitted analyzed for chloride on a monthly basis and results submitted to the District by April 15, July 15, October 15, and January 15 for each preceding calendar year.
The Issue The issue to be determined in this case is whether the Respondents, Florida Department of Transportation (“FDOT”) and Palm Beach County (also referred to as “the Applicants”), are entitled to the issuance of an Environmental Resource Permit (“ERP”) to construct an extension of State Road 7 (“SR 7”) and its associated surface water management system in Palm Beach County.
Findings Of Fact The Parties The City is a municipality incorporated under Florida law. The District is a regional agency with the authority to regulate the construction, operation, and maintenance of any surface water management system pursuant to chapter 373, Part IV, Florida Statutes, and Florida Administrative Code Titles 40E and 62. FDOT is an agency of the state of Florida charged with the establishment, maintenance, and regulation of public transportation. It is a co-applicant for the ERP permit. Palm Beach County is a political subdivision of the State of Florida, and is a co-applicant for the ERP permit. Background State Road 7 Extension The ERP was issued by the District for an 8.5-mile extension of SR 7 between Okeechobee Boulevard and Northlake Boulevard in Palm Beach County. The purpose of the proposed roadway is to relieve traffic now moving through rural residential areas and two large residential developments known as The Acreage and Jupiter Farms. The proposed roadway would also improve hurricane evacuation by providing additional capacity and connectivity, and reduce emergency response time in the rural residential areas. The proposed roadway alignment was selected by FDOT after a multiyear corridor study under a National Environmental Protection Policy Act process. Four corridors were considered using federal selection criteria that addressed social, environmental, property, physical, and financial impacts. There are two segments of the proposed roadway covered by the ERP. The southern segment would add two more lanes to the existing two-lanes of SR 7 from Okeechobee Boulevard North to 60th Street North, just south of the M-Canal. This segment is 4.4 miles long. The southern segment is not at issue in this case. The northern segment would extend four lanes of SR 7 east from 60th Street North about one mile, and then north 3.1 miles to Northlake Boulevard. This is the roadway segment challenged by Petitioner. Hereafter, all references to “the Project” are to the northern segment. The Project includes a raised roadway, median, sidewalks, bike lanes, and stormwater swales. It also includes a bridge over the M-Canal and a bridge over a water control outfall. The Project would be constructed in an existing right- of-way (“ROW”). FDOT owns a ROW that is approximately 200 feet wide. The County owns an adjacent 120-foot-wide ROW, so that the total width of the Project ROW is 320 feet. Running north/south within the ROW is a dirt service road, a ditch, and a fence. Much of the vegetation in the ROW is dominated by invasive and exotic plant species, including Melaleuca, Carolina Willow, Brazilian Pepper, and Australian Pine. The Ibis Development West of the Project ROW is the 1,958-acre Ibis Golf and Country Club residential development (“Ibis”). In 1989, an ERP was issued for Ibis’ surface water management system (“the Ibis system”). The Ibis system includes almost 300 acres of interconnected lakes that provide water management and water quality treatment for Ibis. The 1989 permit required the Ibis system to be sized to receive and treat runoff from a segment of Northlake Boulevard and from an existing two-lane road off of Northlake Boulevard that serves the commercial area of Ibis, which is directly north of the Ibis residential area. The Ibis system was also required to receive and provide water treatment and storage for the stormwater runoff from 46.8 acres of the ROW for SR 7. The parties introduced evidence about modifications to the 1989 permit, which the City contends reduced the treatment capabilities of the system. It is found from the preponderance of the evidence that the original system and its modifications continued to meet design requirements to store and treat future runoff from 46.8 acres of the SR 7 ROW.1/ When the water in the Ibis lakes reaches elevation 17.5 feet NGVD (National Geodetic Vertical Datum), pumps at two pump stations at the south end of Ibis begin pumping water over a berm into Ibis Preserve, a 366-acre natural area directly south of Ibis. Water is retained in Ibis Preserve unles it exceeds an elevation of 18.5 feet, when it then passes over an outfall structure into the Grassy Waters Everglades Preserve (“Grassy Waters”) to the east. Ibis Preserve provides additional water quality treatment for the water pumped from Ibis, but this additional treatment was not part of the calculation of water quality management for Ibis. The Ibis system was required to meet District permitting criteria before discharge to Ibis Preserve. The North Palm Beach County Improvement District (“Improvement District”) owns and has operational and maintenance responsibility for the Ibis system. It also owned and managed Ibis Preserve, but transferred ownership and management of Ibis Preserve to the City in 2004. Grassy Waters/Water Catchment Area To the east of the Project is the City-owned “Water Catchment Area,” which covers about 14,700 acres or 23 square miles. The Water Catchment Area is owned by the City and is part of its public drinking water supply system. Water in the Water Catchment Area flows to Lake Mangonia where it is withdrawn, treated, and then delivered to residents and businesses in the City, the Town of Palm Beach, and the Town of South Palm Beach. There is a statement in the Project application that Grassy Waters refers only to the open water marsh within the Water Catchment Area. The Water Catchment Area includes other habitat types besides open marsh. Most of the information in the record indicates that Grassy Waters and the Water Catchment Area have the same boundaries. Therefore, in this Recommended Order, Grassy Waters and the Water Catchment Area are treated as being two names for the same area. Grassy Waters was once connected to the Everglades and large portions of it have the same characteristics, being an open water marsh with an extended hydroperiod. It is oligotrophic, meaning it is low in nutrients and has an ecosystem adapted to low nutrient conditions. It was undisputed that most areas of Grassy Waters are of high or even pristine environmental quality. Grassy Waters has periphyton, an assemblage of algae that only survive in phosphorous levels of less than 10 parts per billion (“ppb”). Periphyton is the base of the food chain in the open water marsh area of Grassy Waters and is consumed by apple snails and many invertebrates and fish. Grassy Waters has a visitor and nature center and provides recreational opportunities, such as canoeing, hiking, and bird watching. There appeared to be disagreement about whether the Project ROW is located in Grassy Waters or adjacent to it. The ROW is not within Grassy Waters, it is adjacent. However, the wetlands and other surface waters within the ROW are hydrologically connected to Grassy Waters. In the western part of Grassy Waters, which ends at the Project ROW, there are hammock islands and hydric pine flatwoods. The City contends these areas and the rest of the ROW were historically open water marsh, but were changed by human activities. The more persuasive evidence is that this western area was not all open marsh, historically. It was an area of natural transition from open water marsh to other habitat types. Ibis Impacts to Grassy Waters The parties disputed whether the Ibis system is a “failed system.” This is not a technical or defined term. The relevant issue is whether the Ibis system is operating in conformance with the requirements of its permit. The City contends the Ibis lakes are eutrophic and that sediment accumulation in the lakes is releasing phosphorus back into the water, which ends up in Grassy Waters. However, the City’s expert witness, Dr. Harper, admitted that the phosphorus concentration being discharged from the Ibis system, about 40 ppb, is typical for surface water management systems serving large residential developments, although that concentration is at the high end of the range. The phosphorus concentration is closer to 30 ppb in discharges from Ibis Preserve into Grassy Waters, showing that Ibis Preserve provides additional treatment to the waters coming out of Ibis. The characterization of the nutrient loading from the Ibis system as “typical” did not address the additional nutrients in the drainage that the Ibis system is required to accept from the SR 7 ROW. The record does not show that the nutrient concentrations from the Ibis system would still be typical if all of the ROW drainage were added without pre-treatment, as was contemplated by the 1989 Ibis permit. Because Grassy Waters is an oligotrophic ecosystem, it can be adversely affected by phosphorus levels above 10 ppb. When phosphorus is introduced into an oligotrophic system in concentrations over 10 ppb, the system begins to change to denser wetland vegetation, which can include invasive and nuisance species, such as cattail. There is denser vegetation and cattails in Grassy Waters near the Ibis Preserve outfall. There is also more phosphorus in sediments near the outfall. These effects decrease with distance from the outfall, but some effects were detected as far as a half mile from the outfall. The City’s expert witness, Dr. Gaiser, testified that periphyton is dissolved by high nutrient levels and replaced by weedy algae. She found adverse effects on periphyton near the outfall. Dr. Gaiser also found microcystis near the outfall. Microcystis is a toxic algae caused by high elevations of phosphorous. Microcystis comprised over 10 percent of the cell density of the algal community near the outfall. The District’s witness, Mr. Waterhouse, conceded that there is a problem with nuisance vegetation at the discharge point into Grassy Waters. He said the District was not aware of the problem before information was developed for this case. No evidence was presented about what consideration the District gave in 1989, when Ibis was permitted, to the potential adverse impacts of discharging phosphorus into the oligotrophic ecosystem of Grassy Waters. Based on the evidence that a phosphorus concentration of 30 ppb is expected for this kind of surface water management system, it must be concluded that the Ibis system was not designed to prevent harm to oligotrophic receiving waters. Respondents presented evidence to show that phosphorus loadings from the M-Canal could be the cause of the adverse impacts found near the Ibis Preserve outfall. The M-Canal was constructed by the City for the primary purpose of delivering water from Lake Okeechobee, via connection to the L-8 Canal, to the Water Catchment Area for public water supply. For most of its length, the M-Canal runs through Grassy Waters. The City generally maintains the water level in the M-Canal below the elevation of Grassy Waters so water in the canal will not flow into Grassy Waters. However, on some occasions, water flows from the M-Canal into Grassy Waters. High phosphorus concentrations have been recorded in the M-Canal; as high as 300 ppb. Nuisance vegetation is growing in the area where the M-Canal connects to the Water Catchment Area. The preponderance of the evidence establishes that the adverse impacts described by the City’s experts in the area of the Ibis Preserve outfall are caused primarily by discharges from Ibis Preserve. There are three other developments adjacent to Grassy Waters that occasionally discharge to Grassy Waters. These discharges are likely to contain some nutrients, but the amount of nutrients and their effects, if any, on Grassy Waters were not described in the record. The Water Catchment Area is a Class I waterbody because it is used for public water supply. The water quality standard for phosphorus and other nutrients in a Class I waterbody is set forth in Florida Administrative Code Rule 62-302.530(48)(b): In no case shall nutrient concentrations of a body of water be altered so as to cause an imbalance in natural populations of aquatic flora or fauna. Grassy Waters was designated by the Department of Environmental Protection (“DEP”) as a stream. Rule 62-302.531(2)(c) states that the narrative criterion “shall be interpreted as being achieved in a stream segment where information on chlorophyll a levels, algal mats or blooms, nuisance macrophyte growth, and changes in algal species composition indicates there are no imbalances in flora or fauna.” The City presented some evidence regarding nuisance macrophyte growth and changes in algal species composition in Grassy Waters near the Ibis Preserve outfall. Little evidence was presented regarding the practice of DEP or the District in the application of the narrative nutrient standard, but the preponderance of the evidence indicates the agency practice is to consider a stream segment as a whole to determine whether it exhibits an imbalance in natural populations of aquatic flora and fauna.2/ During the course of this proceeding, the District issued administrative complaints against the Improvement District and the City, which include Orders for Corrective Action. The complaints were issued pursuant to section 373.119, Florida Statutes, which authorizes such action when a water management district believes that a violation of any provision of chapter 373 or district rule has occurred. However, at the final hearing, the District was reluctant to say the Improvement District had violated any law or permit condition. The Improvement District did not challenge the enforcement action against it and, therefore, the District’s enforcement order became final. The Improvement District is required to address the accumulation of sediment in the Ibis Lakes, develop a nutrient source control plan, eliminate and reduce the use of herbicides containing copper sulfate, and reassess pumping schedules. There is no target nutrient limit specified in the District’s Orders for Corrective Action. The District’s enforcement action against the City seeks to require the City to increase secondary treatment and retention in Ibis Preserve, provide a plan to remove the exotic/invasive vegetation at the outfall, provide a vegetation monitoring plan, and develop source control measures for residential developments that discharge into Grassy Waters. The City challenged the enforcement action and it remains pending. Snail Kites The Everglades snail kite gets its name from its primary food, the apple snail. In the Everglades, snail kites also feed on an exotic island snail, which occurs there in about equal numbers as apple snails. There was no evidence presented that there are exotic island snails in Grassy Waters. Snail kite habitat is dependent on conditions conducive to apple snails, which are the open marsh and oligotrophic conditions where periphyton flourish. If a sufficient number of apple snails are present, snail kites will find suitable nesting nearby. Dense wetland vegetation is not good forage for snail kites because, even if apple snails are present, the apple snails will be difficult or impossible for the snail kites to see. Dr. Welch, who was the state snail kite conservation coordinator at the Florida Fish and Wildlife Conservation Commission and wrote the snail kite management plan for Florida, testified for the District, where he is now employed as a senior scientist. He said field surveys of snail kite nests in Grassy Waters indicate their numbers are relatively low compared to other areas where snail kites are found. There were only ten successful nests (eggs laid) observed from 2000 to 2016. The City’s Everglades expert, Dr. Lodge, speculated that the low nest counts could be due to difficulty in seeing the nests, but he was not familiar with the survey techniques used and, therefore, his opinion that the numbers could be materially underestimated is not credited. Snail kites nest throughout the Water Catchment Area, but primarily in the open marsh areas of the central and eastern portions of the Water Catchment Area. Over 90 percent of snail kite nests are more than a mile from the Project ROW. Dr. Lodge said there are four snail kite nests within 800 feet of the Project, but he was not more specific about their locations. Most nests are closer to Northlake Boulevard, State Road 710, and the Florida Turnpike. The major factor that adversely affects successful nesting by snail kites and production of offspring is predation, usually by raccoons and rat snakes. “Cold snaps” and drought are also factors. Impacts of The Proposed Project Water Quantity Impacts Water storage for the Project, which was going to be handled in the Ibis system under the 1989 Ibis permit, would be provided in the roadside swales. The Project is designed to retain water volumes greater than typically required for roadways. Stormwater would not flow out of the Project into the Ibis system except in unusually large storm events, in excess of six inches of rainfall. The City did not dispute the Project’s compliance with the applicable water quantity criteria in the District rules. Water Quality Impacts To address the City’s concerns about adverse impacts caused by the Ibis system, the Applicants expanded the roadside swales by ten feet and raised the outfall elevation by 0.05 feet. With these modifications, the Project would provide water quality treatment for its stormwater and no longer rely on the Ibis system for treatment. The swales would provide treatment in excess of the treatment required by District rules. Respondents contend that, when the treatment provided by the Ibis system is added, the total treatment provided for the Project stormwater is more than twice as much as required by District rules. The City, on the other hand, claims that no additional water quality treatment can be provided by the Ibis system because the Ibis Lakes are eutrophic. The preponderance of the evidence supports a finding that Project runoff to the Ibis system would receive additional water quality treatment in the Ibis system and in Ibis Preserve before flowing to Grassy Waters. The effect of the Project’s on-site treatment of its stormwater is that the amount of nutrients that would otherwise flow into the Ibis system from SR 7 would be reduced. Therefore, the effect of the Project is to reduce the nutrient load that the Improvement District was permitted to discharge to Ibis Preserve and Grassy Waters. The City did not dispute the Applicants’ evidence that the Project exceeds the District’s design criteria for water quality. The City focused instead on its contention that, despite its compliance with water quality design criteria, the Project would result in additional nutrient loading to Grassy Waters, which would cause additional adverse impacts to its flora and fauna. The Applicants and the City performed nutrient loading analyses even though such analyses are only required by the District when the receiving waters have been designated by the Department as “impaired” by nutrients or in the case of certain other specially designated waters. Grassy Waters does not have any of these special designations. The Applicants’ nutrient loading analysis concluded that the post-development loading of phosphorus and nitrogen from the Ibis system would be less than the pre-development condition, so there would be a net decrease in nutrients discharged into Grassy Waters. Petitioner’s expert witness, Dr. Harper, believes the Project would increase nutrient loading to Grassy Waters, even if stormwater from the Project did not carry additional nutrients, because the increased volume of water moving through the Ibis system would entrain more nutrients from sediments in the Ibis lakes. Dr. Harper believes the Project would also cause nutrient loading via groundwater seepage through the roadway swales into Grassy Waters. The preponderance of the evidence does not support his opinion that groundwater seepage would cause additional nutrient loading.3/ Dr. Harper believes another source of nutrient loading from the Project would be from surface flow down the roadway embankments. On the eastern embankment, this flow would enter the mitigation area 150 feet from Grassy Waters. Dr. Harper’s estimated total loading from all sources is not persuasive. The estimate gives a false sense of precision. It is based on a number of variable assumptions, some of which are not widely known or in use by experts in the field. In addition, Dr. Harper’s opinion did not appear to appropriately account for the modifications to the Project’s storage capacity. Dr. Harper’s estimated loading was not translated into physical effects in Grassy Waters. The Applicants’ estimate of total nutrient loading also gives a false sense of precision, but it is based on a well-known and widely used methodology. The City failed to prove that the Project would result in more nutrient loading to Grassy Waters than is currently contributed by the ROW. Because the Project would not rely on the Ibis system for stormwater treatment, the Project would reduce the loading that the Improvement District was permitted to discharge to Grassy Waters. To address potential vehicular spills into Grassy Waters, FDOT produced a Spill Response Plan. The swales would capture and contain any material spilled on the roadway or swale. The curb and gutter, a guardrail, gravity wall, and fence also provide protection against spills. The bridge over the M-Canal would use a 54-inch traffic barrier, which is higher than FDOT specifications for the design speed for the bridge. The City did not present evidence to show that the protective measures proposed by the Applicants are less than what is usually considered adequate under similar circumstances, or fails to meet a relevant safety standard. Wetland Impacts Direct Impacts The Project would directly impact 52.37 acres of wetlands and 7.86 acres of surface waters. The impacted wetlands are fresh water marsh, mixed shrubs, and hydric pine flatwoods. The surface waters affected consist of vegetated ditches and un- vegetated channels or canals. The impacted wetlands include 11.77 acres of freshwater marsh. The impacted surface waters are ditches. Most of these wetlands are disturbed and their functional values have been reduced. Secondary Impacts District rules require an applicant to account for the secondary impacts caused by a project that could adversely affect the functions of adjacent wetlands or other surface waters. The Applicant’s Handbook defines secondary impacts to include impacts on wetland functions, water quality, and endangered species, including impacts on areas needed by endangered species for foraging. Part of the Applicants’ assessment of secondary impacts of the Project was made by reviewing the effects of the Acreage Reliever Road on Pond Cypress Preserve, a 1,737-acre conservation area managed by the County that is immediately south of the proposed Project. The County has been monitoring the effect of the Acreage Reliever Road on hydrology, vegetation, and species compensation ever since the road was built. The County found no adverse secondary impacts caused by the road. The species that use the wetlands near the road, including wading birds, appear to be unaffected by the road. The scoring of secondary impacts for the Projects, using the Uniform Mitigation Assessment Methodology (“UMAM”), was conservative, meaning that assumptions were made at the high side of the potential range of impacts. This resulted in more mitigation being required. The Applicants claim the Project would “maintain a 300-foot buffer between the project’s construction boundary and [Grassy Waters].” This appears to be a misstatement. The Applicants’ combined ROW is only 320 feet wide. Going east from the limits of construction, it is 160 feet to Grassy Waters. The Project’s buffer is 160 feet wide. The District accounted for secondary impacts to wetland dependent species, including snail kites, from noise and lights that might discourage use of the area. The Project would provide a tree buffer that will reduce noise and light impacts to Grassy Waters. The roadway lighting plan is also intended to reduce light penetration into Grassy Waters. Most of the threatened and endangered bird species are tolerant of roadways for foraging and roosting, but not for nesting. Section 10.2.7 requires the Applicants to provide reasonable assurances that any future phase of a project or project-related activities will not result in adverse impacts to the functions of wetlands or water quality violations. The Applicants satisfied this requirement by releasing of FDOT ROW north and south of the Project. Cumulative Impacts An applicant must provide reasonable assurance that a regulated activity will not cause unacceptable cumulative impacts upon wetlands and other surface waters within the same drainage basin as the regulated activity for which a permit is sought. Some of the proposed mitigation for the Project is out- of-basin. If an applicant proposes to mitigate impacts in another drainage basin, District rules require consideration of factors such as “connectivity of waters, hydrology, habitat range of affected species, and water quality” to determine whether there are unacceptable cumulative impacts. The Project is located in the eastern Palm Beach County Basin, which has approximately 21,000 acres of wetlands. About 89 percent of the wetlands in the basin are publicly-owned conservation lands, which means their wetland functions will continue into the future. The cumulative impact analysis was conservative, meaning that the actual impacts are likely to be fewer. Petitioner contends that Respondents’ cumulative impact analysis did not account for the unique nature of the Grassy Waters ecosystem as the only remaining low nutrient oligotrophic wetland in the region. The preponderance of the evidence shows that the historical wetland types in the Project area were not all like the open marsh found in the central and eastern portion of Grassy Waters. Respondents accounted for the loss of open water marsh that would be caused by the Project. On-Site Mitigation There would be 52.4 acres of on-site mitigation within a 160-foot-wide strip of land along the eastern limits of proposed construction. This area of the ROW would be managed by removing or treating the exotic vegetation, such as Brazilian Pepper and Maleleuca. Removing the exotic vegetation seed source would prevent further spread of these nuisance species into Grassy Waters. Where native habitats have been altered with ditches and berms, the land would be graded to create a slope from the limits of construction eastward to the edge of the ROW. The eastern elevation would be similar to the adjacent marsh or hydric pine areas of Grassy Waters. Then, native vegetation would be planted. The habitats enhanced, restored, or created would include freshwater marsh, hydric pine flatwoods and mixed forested wetlands, including cypress. The planting of mixed, forested species would provide sound and light buffering for snail kites and other species in Grassy Waters. Two wildlife passages would be created underneath the Project with fencing designed to direct wildlife to use the wildlife passages. Slats would be placed in the roadway fencing to prevent small animals from going through the fence and onto the roadway. The on-site mitigation was scored using UMAM and determined to result in functional gain. The UMAM analysis was conservative, meaning that the actual functional gain is likely to be greater. The City did not contest the UMAM scoring. Off-site Mitigation FDOT is applying mitigation credits from 210 acres at the Pine Glades Natural Area (“Pine Glades”) to offset impacts to 15.7 acres of herbaceous marsh and 26.78 acres of forested wetland impacts. Pine Glades is a regional off-site mitigation area located in the Loxahatchee River Basin and is owned and operated by Palm Beach County. Pine Glades consists of a mix of wet prairie, depression marshes, hydric pine flatwoods, and mesic flatwoods. The restoration work in Pine Glades has already been completed. Pines Glades implements a detailed management plan that provides regional ecological value. Robbins testified that Pine Glades has similar habitats to Grassy Waters. Pine Glades has periphyton, apple snails, snail kites, wood storks, and sand hill cranes. Pine Glades has some areas with oligotrophic conditions. Additional off-site mitigation to offset 52 acres of wetland impacts caused by the Project would be provided at the DuPuis Reserve (“DuPuis”). DuPuis is a regional off-site mitigation area located between the L-8 Canal and the C-44 Canal in western Palm Beach and Martin Counties, and is owned and operated by the District. DuPuis would provide mitigation with 34.71 acres of herbaceous wetlands and 43.8 acres of forested wetlands. DuPuis is appropriate to offset the impacts associated with the Project because it provides similar habitats with similar values of functions for similar wildlife. DuPuis implements a detailed management plan that provides regional ecological value. The City argues that there is little similarity between the Grassy Waters ecosystem and Pine Glades or DuPuis, so the mitigation there cannot offset the unique assemblage of plants and animals that would be lost in Grassy Waters. It is unnecessary for Pine Glades and DuPuis to be dominated by open water marshes like Grassy Waters. It is only necessary that they have some of these areas to offset Project impacts to open water marsh. Proposed snail kite mitigation would provide 52.5 more acres of snail kite habitat than would be directly impacted by the Project. The mitigation for snail kites will be located in FDOT ROW adjacent to the Project, south of the M-Canal, and north of Northlake Blvd. Erwin expressed concern about fragmentation of the ecosystems that would be caused by the Project. The areas that would be affected by the Project have already been fragmented by berms, ditches, and fences. Grassy Waters is surrounded by berms, a canal, and highways. The Project would cause fragmentation, like all roads. However, the fragmentation was reduced where practicable, and the City did not show that the roadway would cause the loss of any significant “greenway” now used by wildlife. Snail Kite Impacts Section 10.2.2(a) requires an applicant to provide reasonable assurances that a proposed activity would not impact wetlands and other surface waters so as to reduce the abundance and diversity of listed species. Snail kites, wood storks, sandhill cranes, white ibises, and little blue herons are listed species that have been observed within the Project corridor. As explained in the Conclusions of Law, the UMAM process is designed to mitigate for wetland functional losses, not snail kite functional losses. However, the potential impact to any listed species warrants close attention to the issue of whether function-for-function wetland mitigation would be provided. There will be 11.5 acres of direct impacts to snail kite habitat within the footprint of the Project area. Dr. Welch believes secondary impacts to wetland functions associated with snail kites could extend 800 feet east of the ROW. Mitigation for snail kites would be located in the Rangeline corridor south of the M-Canal and north of Northlake Boulevard. Dr. Welch estimated there were about 64 acres of snail kite habitat in the Rangeline corridor similar to the 11.5 acres of habitat located in the Project footprint. Dr. Welch conceded that he has no evidence that snail kites currently use the Rangeline, but he believes the habitat is suitable and is appropriate mitigation. Petitioner claims there are studies of “similar birds” indicating that snail kites avoid highways due to noise. However, the studies were not of similar birds. More weight is given to Dr. Welch’s testimony that snail kites are not particularly sensitive to roadway noise. Dr. Welch stated that Pine Glades would likely have value for snail kites because it is near the Hungryland Wildlife Management Area, which has the same number of successful snail kite nests as Grassy Waters. The City contends that Pine Glades is too far away from Grassy Waters to mitigate Project impacts to snail kites. However, snail kites range long distances to forage; several hundred miles in a few days. Satellite telemetry of snail kites shows snail kites from Grassy Waters are using Pine Glades for feeding. Dr. Welch reviewed snail kite nesting data to determine whether roads deterred nesting and found that snail kites frequently nested within 500 feet of major roadways. Dr. Welch refuted the idea that Grassy Waters provided snail kite refuge during drought conditions, because Grassy Waters is also subject to drought conditions that adversely affect snail kites. There are conditions in the permit to limit potential impacts to snail kites during construction of the Project. If snail kite nesting is observed within 1,640 feet of construction, all Project construction must cease. Thereafter, monitoring of the nest and notification of the U.S. Fish and Wildlife Service is required. Construction cannot resume until that nest has been considered finished. FDOT would place a conservation easement over 82.6 acres in the FDOT ROW between Okeechobee Boulevard and the M-Canal, south of the Project area that is the subject of this proceeding. The conservation easement would maintain connectivity between the Pond Cypress Natural Area and Grassy Waters and ensure that no future southern extension of the roadway will be constructed. A conservation easement would be placed on the FDOT ROW between Northlake Boulevard and SR 710, an area of approximately 43.5 acres. Preserving this area protects a hydrologic connection between Loxahatchee Slough Natural Area and Grassy Waters. It also ensures no future northern extension of the roadway. A conservation easement would be placed on a portion of the FDOT ROW between SR 710 and Jupiter Farms, an area of 44.5 acres. This section of ROW is in the Loxahatchee Slough and the release of the ROW would be a direct benefit to Loxahatchee Slough. The preservation of these areas would benefit fishing and recreational values in the Pond Cypress Natural Area, Grassy Waters, and the Loxahatchee Slough Natural Area. These conservation areas did not receive UMAM credits to reduce the wetland acreage needed to offset wetland functional losses, but they were included in the mitigation credit for benefits to snail kites and other wildlife. Summary The preponderance of the evidence established that the proposed mitigation offsets the impacts to wetlands and other surface waters that would be caused by the Project and exceeds the requirements of District rules. Practicable Design Modifications District rules require an applicant to consider alternatives that would avoid or reduce wetland impacts. The City claims the Applicants failed to comply with this rule because FDOT selected a roadway corridor that was expected to have greater environmental impacts than some of the other three corridors that were being considered. As explained in the Conclusions of Law, this argument is misplaced. The District’s review of the Applicants’ measures to avoid or minimize wetland impacts was appropriately confined to Corridor 3, the corridor selected by FDOT where the Project is proposed. The Applicants reduced and eliminated impacts of the Project in several ways. For example, the footprint of the road was narrowed from six lanes to four lanes, wildlife underpasses were provided, retaining walls were used to narrow stormwater features, the median was reduced in size, and the design speed limit was reduced for the bridge at the M-Canal crossing. Under two circumstances, District rules allow an applicant to avoid the requirement to implement practicable design modifications to reduce or eliminate wetland impacts, which are referred to as the “opt-out” provisions. Section 10.2.1.2, Volume I, of the Applicant’s Handbook (“A.H.”) provides: The ecological value of the functions provided by the area of wetland or other surface water to be adversely affected is low, based on a site specific analysis using the factors in section 10.2.2.3, below, and the proposed mitigation will provide greater long term ecological value than the area of wetland or other surface water to be adversely affected, or The applicant proposes mitigation that implements all or part of a plan that provides regional ecological value and that provides greater long term ecological value than the area of wetland or other surface water to be adversely affected. The District determined that the Applicants meet both tests. The preponderance of the evidence supports the District’s determination. The ecological value of the functions provided by the affected wetlands and surface is low and the proposed mitigation would provide greater long-term ecological value than the area being impacted. Pine Glades and DuPuis are part of a plan to restore the ecological value of Northern Palm Beach County and create an “ocean to lake” system of preserves and natural areas.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the South Florida Water Management District enter a final order approving Permit Number 50-05422-P on the terms and conditions set forth in the amended Staff Report, and the complete application for the Permit. DONE AND ENTERED this 31st day of March, 2017, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 31st day of March, 2017.
Findings Of Fact The subject application requests a water use permit from the Central and Southern Florida Flood Control District (FCD) for the supplemental irrigation of 145 acres of citrus lands located in Orange County. Received into evidence at the hearing were the public notice of hearing appearing in the Sentinel Star, permit application number 21424 with an attached report and the Staff Report of the FCD, prepared by Nagendra Khanal. The applicant requested an annual allocation of water in the amount of 120.15 acre-feet or 9.94 inches per year, for a period of twenty (20) years. The Staff Report recommends the issuance of a permit for said amount, with maximum monthly pumpages not to exceed 49.8 acre-feet or 4.13 inches, the permit to expire on January 15, 1978. Several further special provisions were recommended on pages 4 & 5 of the Staff Report, which report is attached hereto. There is no dispute between the applicant and the FCD over the technical aspects of the Staff Report. The protests of the applicant center around the length of the permit and some of the special provisions recommended in the Staff Report, which the applicant feels are vague and ambiguous. Mr. James A. Hinson, the applicant's corporate secretary, felt that the FCD had sufficient data and statistics as to the water resources and agricultural usage within the area to sustain the granting of a twenty year permit. It was further felt that the issuance of a two-year permit for the purpose of gathering information as to the quantity of use would tend to prompt higher usage and even lead to falsification of pumpage records on the part of agricultural users so as to assure the issuance of future permits. The applicant was also concerned with the costs of applying for another permit in two years. Mr. Nagendra Khanal, a hydrologist with the FCD, explained that the purpose of the two-year permit was to obtain information from agricultural users in the area as to the amount of water used and the effect of such usage on the Florida aquifer system. Since the outset of regulatory provisions, the FCD has set the same termination date for each permit for agricultural use within each of the basins. At that expiration time, the pumpage records for all users in the area will be established and present experimental estimates can then be compared with actual usage. Little is known by the FCD about how the Florida aquifer system operates and the data presently in use are experimental. Since all permits within each basin will expire on the same date, the entire basin can then be evaluated at one point in time. It was felt that if falsification of pumpage records were to occur, it could probably be detected by data currently available to the FCD. It was further opined by Mr. Khanal that at, the expiration date of all permits issued in each basin, an automatic conversion into new permits would occur at little or no cost to the applicant. With regard to the special provisions recommended in the Staff Report, Mr. Hinson expressed concern over the manner of compliance. Specifically, he desired more information on the type of equipment or devises required by the FCD when it calls for "minimum head pressures", and "a measuring device on each of the three wells." He also desired information as to the times of year the water quality analyses were to be performed. Mr. Khanal explained that no regulatory criteria had been established by the FCD with regard to pumpage and that the minimum type of measuring device, such as a time clock, on each of the wells would suffice. Further specifications will be supplied to the applicant upon request. It was explained by Khanal that the water quality analyses should be performed once before the rainy season (at the end of May) and once after the rainy season (at the end of October). There was some confusion over the inclusion of the parameter of "specific conductivity" within the definition of a standard complete water quality analysis. Finally, Mr. Khanal listed two amendments to be made in the Staff Report. On page 2, under "B. Existing Facilities", "3,500 gpm" should read "3,600 gpm." The last item on the chart on page 3 of the Staff Report should read "2 in 10 Year Drought" in lieu of "1 in 10 Year Drought."
Recommendation Based upon the findings of fact and conclusions of law recited above, it is recommended that Application No. 21424 be granted and that a permit be issued in accordance with the recommendations and provisions set forth in the Staff Report, as amended. Due to the apparent confusion over the inclusion of "specific conductivity" as a parameter to be included within the definition of a standard complete analysis, it is further recommended that the Staff make further inquiry into its necessity. If the Staff then concludes that "specific conductivity" is necessary to obtain a complete water quality analysis, it is recommended that it remain on the list of parameters. Respectfully submitted this 5th day of March, 1976, in Tallahassee, Florida. DIANE D. TREMOR Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 5th day of March, 1976 COPIES FURNISHED: Thomas C. Garwood, Jr., Esquire Akerman, Senterfitt, Eidson and Wharton 17th Floor CNA Building Orlando, Florida Stephen A. Walker, Esquire Post Office Box V West Palm Beach, Florida 33402
Findings Of Fact Upon consideration of the oral and documentary evidence adduced at the hearing, as well as the stipulation of facts contained in the Prehearing Stipulation, the following relevant facts are found: The Gardinier Applications. l. The East Tampa Chemical Plant (plant) operated by Gardinier is located on approximately 3,500 acres of land owned by it at the mouth of the Alafia River and the Hillsborough Bay. The facilities have been there since 1924, and the withdrawal of water utilized to operate the plane predates the consumptive use permitting process. The plant manufactures various fertilizer products, including sulphuric acid, phosphoric acid, diammonium phosphate, granular triple superphosphate, run of pile triple superphosphate, byproducts of phosphoric acid, as well as fluosilic acid and sodium silicofluoride. The phosphoric acid products are used by farmers to grow corn, soy beans, and wheat, and fluosilic acid and sodium silicofluoride are used by municipalities to fluorinate drinking water. When the plant is fully operating, Gardinier employs 950 people with a payroll of $22 million a year. The company pays annual property and other taxes of $1.5 million a year and annually purchases approximately $25 million in materials and equipment in Hillsborough County. Garciinier was recently purchased by Cargill, Inc. after a bankruptcy proceeding. In order to manufacture its products and operate the plant, Gardinier uses both salt water and fresh water. The salt water comes from salt water wells located on the plant's property, and has been used since 1924 for cooling purposes. It is used for once-through, non-contact cooling of sulphuric acid and is then discharged into the Alafia River at the Hillsborough Bay. Due to the naturally occurring radium in this discharged salt water, Gardinier intends to discontinue using its salt water wells and utilize fresh water for all its cooling requirements. This will require the construction of a fresh water cooling tower, for which a permit is currently being sought and which will take about two years to complete. Gardinier's existing CUP No. 7601530 for its salt water wells permits an average annual withdrawal of 56,260,000 gallons of water per day (gpd) and a maximum daily withdrawal of 64,890,000 gpd. Despite expansions in its plant over the years, the amounts of salt water and fresh water required has decreased. Gardinier's present renewal application for its salt water withdrawals proposes a reduction to an average annual rate and maximum daily rate of 31,968,000 gpd . Fresh water is used at Gardinier's plant as boiler feed water, for manufacturing of product or process water, cooling and potable needs. This water is obtained from Buckhorn Springs and Lithia Sprlngs, both wholly owned by Gardinier. Gardinier purchased 148 acres at Buckhorn Springs in 1947, and 160 acres at Lithia Springs in 1967, including the spring pools, and has been withdrawing water from those springs since those times. Lithia Springs is leased to Hillsborough County for recreational purposes. Gardinier's withdrawals from the springs have been gradually reduced since 1977. The original CUP No. 7601532 issued in 1977 for Buckhorn Springs authorized an annual average withdrawal of 2,176,000 gpd with a maximum daily withdrawal not to exceed 2,370,800 gpd. Gardinier requested a reduced withdrawal s renewal application, with an annual average and a maximum daily rate of 1,440,000 gpd. Gardinier's original CUP No. 7601533 for Lithia Springs issued in 1977 was for 5,840,700 gpd average annual withdrawal and 5,894.000 gpd as a maximum daily withdrawal. Gardinier's renewal is for a reduced average withdrawal rate of 5,822,000 gpd and a maximum daily withdrawal of 5,904,000 gpd. The increased maximum quantity is for the well used for the concession stand at the park. Withdrawals from Gardinier's salt water wells consists of comingled waters from the intermediate aquifer, the Floridan aquifer and Hillsborough Bay. The water is salty, high in chloride and its constituents are very similar to bay water. The evidence is inconclusive as to whether Gardinier's operation of its salt water wells for a period of over 60 years has caused or contributed to salt water intrusion in thc area of the plant. There is some evidence that the pumping may have been beneficial in reducing salt water encroachment along the coast due to the release of pressure on the deeper Floridan aquifer which allows fresh water to move into the system. In any event, if there has been an adverse effect from more than 60 years of pumping, the effect would be reduced by the reduction in withdrawals which Gardinier now seeks in its permit renewals. While Gardinier is the largest use of water in the plant area, there are domestic wells in the vicinity of the plant. Computer modeling demonstrates that present withdrawals from the salt water wells will affect the potentiometric surface at the plant's boundary by less than five feet and create less than a one-foot drawdown in the water table. The greater portion of the water pumped is recharge water from the bay. Any reduction in the amount of pumping would have a positive impact on the potentiometric surface, will decrease any impact on nearby domestic wells and will allow the quality of the water in domestic wells to either remain stable or improve. Since the potentiometric surface in the plant's vicinity is already at sea level, it is SWFWMD's policy not to take into account the regulatory criterion relating to the lowering of the potentiometric surface below sea level. SWFWMD has not established regulatory levels for the rate of flow of streams or watercourses, the potentiometric surface or surface waters in the vicinity of the plant. Salt water marshes, estuarine systems and uplands exist to the north, south and east of the plant. Any adverse ecological impact suffered by these systems are more attributable to cultural impacts than to a less than one foot lowering of the water table. Since Gardinier's withdrawals have been occurring for over 60 years, it is likely that biological communities in the area have adapted, and the proposed reduction in pumping have no additional adverse effect. In order to satisfy its requirements for fresh water of reliable quantity and quality, Gardinier has been withdrawing water from Buckhorn Springs for almost 40 years and Lithia Springs for almost 20 years. The boilers and cooling towers at the plant are designed to utilize water of that quality and temperature. But for Gardinier's withdrawals, these spring waters would flow into the Alafia River and eventually into the bay. The spring water from Lithia is pumped through a pipeline to Buckhorn Springs, comingles with the Buckhorn spring water and is pumped some 1< miles through a pipeline to the chemical plant for use as boiler feed water, process water, cooling water and sanitary and drinking water. During full production periods, Gardinier uses all the water withdrawn from Lithia and Buckhorn Springs. Because of cutbacks in production in 1983, Gardinier installed a pressure relief valve to alleviate pressure problems in the plant during times of reduced production. This allowed water to be discharged into the Alafia River from the Lithia pipeline without passing through the plant. Over the past two years, approximately .5 to 1.2 million gallons of water per day has passed through the pressure relief valve and discharged in the Alafia River at a point downstream from where it would have entered the river naturally. Gardinier is presently in the process of developing an alternative pressure control system which would permit it to take from Lithia and Buckhorn Springs only the amounts actually required at the plant. Lithia Springs and Buckhorn Springs are typical karst artisian sink springs. The geology and hydrogeology of the area of both springs demonstrates a series of fault features, where solid rock has fractured and the fractures extend into the Floridan aquifer. Solutioning occurs and a sinkhole system is created. The springs are discharge points of the Floridan aquifer. These aquifer waters discharge into the springs from artisian pressure. An examination of various well logs and literature on Florida geology leads to the conclusion that the water in Lithia Springs and Buckhorn Springs withdrawn by Gardinier are supplied primarily by the Floridan aquifer with very minimal contribution from the intermediate or surficial aquifers. The withdrawals at both springs constitute ground water, as opposed to surface water, withdrawals. As noted above, Gardinier owns 148 acres at Buckhorn Springs and 160 acres at Lithia Springs. There are 350 feet from the edge of Buckhorn Springs to the nearest property line and 400 feet from the edge of Lithia Springs to the nearest property line. Pump tests designed to determine the lateral and vertical extent of the impact from the stress of pumping in amounts far greater than usual demonstrate that the impacts from withdrawals do not extend beyond 300 feet from the edge of either spring. After stabilizing the springs and pumping at a greater rate than normal, the pump tests revealed only a 1.25 foot decline in the spring boil, a 1.06 foot decline in the spring pool and no appreciable change in the water table or surface water at Buckhorn Springs. The impacts from pumping at Lithia Springs were even more minimal -- a two inch decline in the water level of the spring boil and a decline in the pool level of less than one inch. These results lead to the conclusion that the artisian systems are not adversely affected by Cardinier's pumping at Buckhorn or Lithia Springs. Chemical analyses reveals that the quality of the waters at Buckhorn and Lithia Springs has not been adversely affected by Cardinler's pumping or withdrawals. The proposed withdrawals will have no adverse effect upon vegetation in the areas of Lithla or Buckhorn Springs. There will be no inducement of salt water encroachment as a result of Gardinier's withdrawals from Lithia or Buckhorn Springs. SWFWMD has set no regulatory levels pertaining to the rate of flow of streams or watercourses, the level of the potentiometric surface or the level of surface waters in the areas of Buckhorn or Lithia Springs. It is the policy of the SWFWMD not to require extensive testing or monitoring when an applicant is applying for a renewal of a presently existing legal use, particularly when the renewal is for a permit with reduced quantities. In order to determine the future adequacy of the water supply available from Lithia and Buckhorn Springs, as well as to determine the effect of a diminuition of the outflow by outside sources, it would be beneficial to place continuous recording gases on spring flow, spring height and pumpage at those spring sites. Many industries are capable of and do now utilize reclaimed, recovered or recycled water in their plant operations. Dependent upon the plant's equipment and ;he quantity and quality of the reuse or recycled water, such water can be utilized in chemical plant operations for such nonpotable uses as cooling water, boiler feed and process water. A source of reuse water is treated effluent from advanced wastewater treatment facilities. Several new County wastewater treatment plants are presently in the planning stage, but none are currently on line nor are there pipelines in existence which could supply reuse water to Gardinier's East Tampa Chemical Plant. Use of the existing pipeline for reclaimed or reuse water would contaminate Gardinier's existing fresh water supply from the springs. Considering the quantity and quality of its present source of fresh water, reuse water has no technical or economic advantage to Gardinier. Its plant equipment would have to be retrofitted, a new distribution system both within and outside the plant would be required and experience by other industrial users has demonstrated problems with scaling, increased temperature and the consistency of water quality. When weighing the potential for reuse water in plant operations, a large factor to be considered is the economic feasibility, including the cost of treatment, maintenance costs, the cost of the current supply, availability, etc. While the reuse of water should be encouraged as a conservation measure, the economic feasibility of such use must be considered. Gardinier has studied and has agreed to continue to study the feasibility, both technical and economical, of reuse water for some of the plant operations. The Authority's and County's Application. The Authority is a five member governmental entity consisting of Pasco County, Pinellas County, Hillsborough County, the City of Tampa, and the City of St. Petersburg. Its obligations are to provide an adequate and dependable source of supply for all citizens within the tri-county area and to do so without concentrating withdrawals to the point where they would have an adverse environmental or hydrological impact. The Authority first began operating public supply wellfields in 1978. Currently, the Authority operates the Cypress Creek Wellfield, the Cross Bar Ranch Wellfield, the Starkey Wellfield, the Section 21 Wellfield, the Cosme-Odessa Wellfield, and the Northwest Hillsborough Wellfield. The permitted average annual withdrawal rate and maximum daily withdrawal of these wellfields are 30 million gallons per day (mgd)/30 mod for Cypress Creek, 30 mgdt45 mgd for Cross Bar, 8 mgd/15 mgd for Starkey, 13 mgd/22 mgd for Section 21 and Cosme-Odessa and 8.8 mgd/18.q mgd for the Northwest Hillsborough Wellfield. In addition, the Authority has a consumptive use permit to withdraw water from the Tampa Bypass Canal at a rate of 20 mgd average annual withdrawal and 40 mgd maximum daily withdrawal. The south central Hillsborough County region and service area has been described in this proceeding as an area bounded by Interstate ~ on the north, by Valrico on the east, by the Little Manatee River on the south and by Tampa Bay on the west. The area is largely a rural area, but has several population centers, including Brandon, Ruskin, Apollo Beach, Sun City and Riverview. The County's current public water supply facilities in the south central region comprise some 75 dispersed wells permitted under 8 different CUPs. The evidence is conflicting and inconclusive as to the actual number of existing wells and the quantities presently permitted. Some of the presently permitted wells have been converted to monitoring wells and others have been plugged. The Authority and the County have concluded that it is no longer possible to continue to use the County's existing public water supply facilities in the south central area. Consequently, they have applied for a CUP which would renew and consolidate their existing 8 CUPs and add 17 new wells to be located at a regional wellfield. It is the intent of the Authority and the County to continue using the existing wells during construction of the planned wellfield and then to discontinue their use and serve the entire area from a centralized wellfield. The amended application requests total average annual combined permit withdrawals of 24,100,000 gpd and total maximum daily withdrawals of 44,600,000 gpd. The current, existing Brandon water supply system is comprised of some 30 dispersed wells capable of producing from 7 to 10 mgd of good quality water. However, there are problems in this system, as well as the smaller systems serving Sun City, Apollo Beach, Ruskin and Riverview. The Brandon wells have individual chlorinators and, on occasion, suffer pressure problems. Because of their dispersed locations, the County's operators can only visit each well site once a day. If a problem occurs after the operator's visit, it will not be discovered until the following day and recipients of the water may use water that has not been disinfected. It is difficult to monitor and sample the well waters due to their dispersed locations. The existing system relies totally on local wells for local distribution as there is a complete lack of transmission facilities. The systems are hydraulically isolated and there is no transmission capacity within the Brandon system at all. While there is one intertie with the City of Tampa's water system, this is not used primarily because the City has its own supply problems and also because the City's water treatment is different than and incompatible with the County's water treatment. Some of the existing wells located south of the Alafia Rlver are old, in poor repair and violate Florida's drinking water standards for total dissolved solids, sulfates, fecal coliform and occasionally odor. Many of the existing well sites are not secured and their locations are such as to constrain access to the larger repair equipment. The existing system has inadequate storage capacity. On the basis of present demand for water within the system, there should be at least 10 million gallons of available storage. The current storage capacity is slightly more than 4 million gallons and not all of this storage is available. A storage tank is generally kept at least half full to provide for local fire demand and, therefore, the effective storage capacity of the existing system is about 2 to 3 million gallons. The existing water supply system lacks the capacity for both adequate fire protection and adequate emergency pumping. Retrofitting or refurbishing the existing system with newer or more dispersed wells would simply perpetuate the existing inadequacies in the system. For these reasons, the Authority and the County have determined that the only feasible alternative to solve the inadequacies and to meet the current and future demand is to provide a centralized system of transmission lines, centralized master pumping facilities and a centralized source of water supply. As the wellfield production wells, pump station and transmission lines are constructed and become operational, the existing wells will be either taken out of service or will be utilized as monitor wells. It is estimated that the construction of the proposed wellfield will take from 18 to 24 months. In reaching a determination as to the location and design of the proposed south central wellfield, the Authority and the County analyzed various alternatives. Studies and testing were done regarding the placement of a regional wellfield in the Brandon area. However, testing demonstrated that the potential yield would be very low in that area and could cause the upconing of highly mineralized water. Tests conducted further to the east, in the Medard area, demonstrated a productive aquifer with good water quality. However, because large amounts of water are withdrawn from that area by strawberry farmers, particularly during freezing weather, that site was found unsuitable for a regional wellfield. The Authority also investigated the feasibility of creating a surface water supply and constructing reverse osmosis plants. These alternatives were rejected due to concerns regarding economics, adverse environmental impacts and the production of sufficient yield. Testing performed at the Lithia site resulted in findings that the aquifer was productive and had a good quality of water. To confirm these findings, further testing was done to the east of the Lithia site at Alderman's Ford Park. This testing resulted in a finding of a high yield of water that met drinking water standards. While traces of a volatile organic compound were revealed, these were determined to have resulted from the laboratory cleaning process. Thus, the Alafia River corridor was determined to be the appropriate location for a regional wellfield because it would not compete with the agricultural irrigation to the north, would avoid the poorer water quality to the south and would produce an adequate yield. The Authority and the County have completed the preliminary design of the proposed wellfield. It is to consist of 17 production wells and a pump station. Wells 1 and 2 are to be used as standby wells and pumpage is to be rotated among wells 3 through 17 so that withdrawals are evenly distributed among those wells. The standby wells are only to be used if there is a failure at another well within the wellfield. Well 1 is already constructed and is located about 1 1/2 miles from Lithia Springs on 80 acres of land purchased by the County for the master pump station. Well 1 is located about 100 feet from the nearest property boundary to the south. The remaining wells would be placed on one-acre well sites to be purchased by the applicant and located somewhere within the 40 acre quarter-quarter sections which the authority submitted to the SWFWMD as proposed well locations. The total additional land area to be acquired for the well sites is 14 acres. Two of the wells will be located on land already owned by the County. Some of the wells are concentrated, with three in one section. The Authority has attempted to locate the wells adjacent to road right-of-ways which could be used for transmission pipelines. The Authority has not yet developed a management plan or a monitoring plan for the proposed wellfield. Each of the wells within the regional wellfield is designed to pump at an average annual withdrawal rate of 3 mgd and a maximum withdrawal rate of 4 mgd. If only one well were turned on in the system and no other wells were running, the well would produce 4 mgd. However, with all of the other wells running, a single well would only produce 3 mgd due to friction loss and the energy required to pump a large mass of water through the pipe under greater pressure. Thus, while the wellfield would be able mechanically to pump 60 mgd, the optimum production capacity will be 45 mgd. On an average day, pumping will be rotated among a small number of wells to produce a total of 24.1 mgd. On a peak day, all 15 wells would be producing approximately 3 mgd each for a total combined withdrawal rate of 44.6 mgd. Based upon a per capita consumption of 189 gpd, it is estimated that the total water supply requirements for the south central service area in the year 1990 to meet average day and maximum day demands is approximately 24 mgd and 44 mgd, respectively. The proposed wellfield is located along the north and south prongs of the Alafia River. That area is characterized by rural and light agricultural land uses, residential areas and recreational sites. Land uses in the area have been dependent upon private, individual water wells, many of which are shallow and draw water from an intermediate aquifer. One proposed well site has 31 property owners within 1/2 mile of the well. One hundred property owners live within 1/2 mile of proposed well 17. These domestic well users will not be served by the proposed system. The Authority has issued revenue bonds to finance the construction of the regional wellfield and transmission lines. The regional wellfield will cost approximately $14,000,000 and the transmission lines will cost approximately S19.000,000. An additional S2,000,000 will be needed to complete construct on and these funds will be raised through the rate structure. In order to determine the proposed wellfield's impacts upon the potentiometric surface, water table and lake stages, the parties in this proceeding utilized information gathered from literature, pump tests, computer modeling and hand-calculated modeling to predict the drawdowns expected during periods of average and maximum pumping. While the actual numerical drawdown 1evels anticipated vary greatly among the expert witnesses presented, it is clear that the wellfield withdrawals, after pumping for 30 days at 24 mgd, will lower the potentiometric surface by more than 5 feet at the boundary of a one-acre well site and that the 5-foot drawdown contour will extend at least 2 1/2 miles radially around the center of the wellfield . The water table level will not be lowered more than three feet at the boundaries of the one-acre tracts, surface waters of lakes and impoundments will not be lowered more than one foot, and the potentiometric surface will not be lowered below sea level. Withdrawals from the wellfield will not induce salt water encroachment. When utilizing computer modeling to predict the impacts from withdrawals, it is essential to understand the site-specific geology and aquifer characteristics of the area. After studying the literature on the area of the wellfield, examining well logs and geophysical logs and conducting a well inventory in a 5-mile area across the wellfield, Gardinier's hydrogeologlsts found the area to be nonisotroptc and calibrated their modeling to account for the changes in geology throughout the area. The area of 'he proposed wellfield was fond to contain a thick clay confining layer which allows less water to permeate it. Inasmuch as less water moves through the layers to recharge the aquifer, the cone depression created by withdrawals from the wellfield extends over a larger and deeper area. Utilizing a value for leakance (defined as the vertical permeability through which water flows from the upper aquifer through a confining layer into the lower aquifer) of 1 x 104. Gardinier's experts predict that the potentiometric surface drawdown at Lithla Springs when the wellfield is pumping 24 mgd for 30 days will be about one foot under normal conditions. During a drought, the drawdown in the Floridan aquifer at Lithia Springs could be as much as 18.9 feet. The effects would, of course, be greater during pumpage rates of 45 mgd. During drought conditions, and possibly also when the wellfield is operating at maximum withdrawal rates, Gardinier may well have difficulty pumping water from Lithia Springs in the amounts for which it is seeking a permit. Various methodologies demonstrate that the potentiometric surface drawdown in the center of the proposed wellfield will be from 20 to 6G feet, depending upon the pumpage amounts and seasonal conditions. Such drawdown levels can interfere with existing wells in the area. Also, a lowering of the potentiometric surface could potentially lead to catastrophic collapse or subsidence in the area of the wellfield. The area is karstic in nature, with solution features such as sin);holes and springs present. Rapid ground collapses can occur in such areas due to a loss in the bearing strength of the unconsolidated material that fills the solution features. Such collapses have been associated with large withdrawals of water from pumping, thus creating extensive drawdowns, followed by a heavy rain. because of the particular geologic and aquifer characteristics of the wellfield area and the potential for interference with existing users, there should be a controlled maximum amount of water development in this area, along with observation wells and extensive monitoring of the various aquifer systems. In order to justify an exception to the District's rule that withdrawals not lower the level of the potentiometric surface more than five feet, the Authority proposes a mitigation program which it utilizes in other wellfields operated by it. This after-the-fact mitigation program consists of receiving complaints, sending a field representative to conduct an on-site investigation to determine the nature and cause of the problem, and sending a letter to the complainant and to SWFWMD documenting the results of the investigation. If the .authority determines that its wellfield operation caused the problem, if it takes mitigative action, such as reimbursing the complainant, hiring a contractor to solve the problem, or refurbishing or replacing the complainant's well or pumping equipment. The Authority also proposes various alternative mitigative actions if the wellfield affects Gardinier's ability to withdraw a sufficient quantity of water from Lithia Springs. These include the construction of new wells at Lithia Springs or along Gardinier's transmission pipeline, lowering the intake system at the springs and supplying Gardinier with water from the wellfield on an emergency basis. These suggested alternatives have not been fully investigated with regard to the effect upon the springs and fail to take into account the economic repercussions to Gardinier should it be unable to supply fresh water for the plant's operation while the Authority is investigating the problem and/or implementing the solution. The SWFWMD has proposed a before-the-fact mitigation plan for landowners living within one-half mile of each well site. This preventative mitigation plan would require the Authority to conduct a detailed water well inventory of all property owners located within one-half mile of the withdrawal point of each production well when the sites are finally selected. The Authority is to review each well's depth, casing size and depth, pump type and depth and the static water level, and then determine whether each well will be adversely affected with regard to its intended use. If so, the Authority is to commence its mitigative actions prior to or during construction of its production well. If an adverse effect is determined during testing of any production well, the Authority is to commence mitigative action prior to withdrawing water for public supply. The mitigative actions for impacted wells are to include well deepening, lowering or replacement of pumping facilities or whatever action is required to maintain an adequate water supply. The five-foot potentiometric surface drawdown contour extends beyond one-half mile during certain scenarios of pumping or seasonal conditions. The .Authority has been operating Well 1 as a test well under a temporary CUP, and has received six complaints from private well owners in the vicinity regarding water levels. No corrective action has been taken with regard to these complaints. With the exception of some phosphate mining cuts and small farm ponds, there are no significant lakes or other impoundments in the area of the proposed wellfield. It is anticipated that such water bodies will be affected by less than one foot by withdrawals from the wellfield. The greatest water table drawdown predicted is 2.8 feet at the center of the wellfield, where there are no open bodies of water. The area is culturally impacted now and is not ecologically sensitive. Vegetative species in the area are able to adapt to a wide range of soil moisture situations, and a less than one-foot reduction in the water table should not adversely or significantly affect vegetation in the area. Operation of the proposed wellfield at the requested rates of withdrawal will have no effect upon Buckhorn Springs or the East Tampa Chemical Plant. Intervenor Hebbard's private well is located between Well l in the proposed wellfield and Lithia Springs. He is concerned that the proposed wellfield will adversely affect land values in the area and the quantity and quality of his water withdrawals. He is also concerned with the potential for terrorist activity in a centralized water supply source and feels that the location of the proposed wellfield will not benefit existing Florida residents. The Lithia-Pinecrest Civic Association is not incorporated and has no membership list or bylaws. Its 47 years, uses the Alafia River for fishing and boating and is that the proposed wellfield will adversely affect his well and pumping facilities without adequate or timely mitigation and that the wellfield will remove the very resource for which the area is zoned: to wit: agicultural. Intervenor A. H. Varnum resides in the area of the proposed wellfield and also operates his business, Central Maintenance and Welding, Inc, in that area. He is concerned that the wellfield will adversely affect his water supply without sufficient mitigation. He is further concerned about the social impact of permitting a wellfield in this area when the water withdrawn will not benefit the persons who reside there. Intervenor I. A. Albritton was in attendance throughout the hearing. He was born in the area and now resides near Wel1 He has noticed odors, ground vibrations and decreasing water levels when Well 1 is pumping. He is concerned with dropping water table levels and the general condition of the land in the area.
Recommendation Based upon the findings of fact and conclusions of law recited herein, it is RECOMMENDED that: CUP Number 7C01530 be ISSUED to Cardinier for its salt water wells at the East Tampa Chemical Plant for a period of two years an average annual and maximum daily withdrawal rates of 31,968,000 gallons per day: CUP Number 7601532 be ISSUED to Gardinier for spring withdrawals from Buckhorn Springs for a period of six years at average annual and maximum daily withdrawal rates of 1,.40,000 gallons per day, with the condition that total discharge from the spring pool be recorded on a daily basis and reported to the SWFWMD on a monthly basis, and that continuous recording gages be placed to monitor spring flow, spring height and pumpage. CUP Number 7601533 be ISSUED to Gardinier for spring and groundwater withdrawals from Lithia Springs for a period of six years at an average annual withdrawal rate of 5,822,000 gallons per day and a maximum combined withdrawal rate not to exceed 5,904,000 gallons during a single day, with the following conditions: that Gardinier cease utilizing its existing pressure relief system and develop an alternate system for withdrawing sprirlg water only in the amounts actually required, and that total discharge from the spring pool be recorded on a daily basis and reported to the SWFWMD on a monthly basis, and that continuous recording gages be placed to monitor spring flow, spring height and pumpage; and CUP Number 204352 be ISSUED to the West Coast Regional water Supply Authority and Hillsborough County for a period of six years, such permit to consolidate prior permits for approximately 75 existing wells used for public water supply and to construct and operate a regional wellfield containing 17 production wells, with total combined average withdrawal rates of 24 ,100, 000 gallons per day and a total maximum combined withdrawal rate not to exceed 44,600,000 gallons during a single day, with the following conditions, as amplified in the above conclusions of law: that pre-development hydrologic conditions at the wellfield, particularly at each well site, continue to be monitored by the Authority; that a report be submitted to the SWFWMD summarizing the planned schedule for retiring each of the existing wells and the schedule for the phased production of water from each wellfield well; that a written mitigation policy be submitted to the SWFWMD and incorporated as a condition of the permit, said policy to contain adequate measures to eliminate interference without interruption of presently existing legal uses, as suggested by the SWFWMD and including those users who will be affected by a potentiometric surface level drawdown exceeding five feet and Galdinier's withdrawals from Lithia Springs; and that, once production at the wellfield reaches a level of 15,000,000 gallons per day, the Authority will notify the SWFWMD staff and engage in a joint review of the hydrologic monitoring results of pumpage at that .ate and a joint determination of the future pumping scenario. The conditions recommended herein are intended to be inclusive only, and not exclusive of other customary permit terms and conditions nor of those conditions suggested by the SWFWMD in its proposed CUPs Numbers 201530, 201532, 201533 and 204352. Respectfully submitted and entered this 11th day of July, 1986, in Tallahassee, Florida. DIANE D. TREMOR Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904 ) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 11th day of July, 1986. COPIES FURNISHED: Edward P. de la Parte, Jr., Esquire Edward M. Chew, Esquire de la Parte, Gilbert & Gramovot, P.A. 705 E. Kennedy Boulevard Tampa, Florida 3360- Roger W. Sims, Esquire Julia Sullivan Waters, Esquire Holland & Knight P. O. Drawer BW Lakeland, Florida 33802 and 600 N. Florida Avenue Tampa, Florida 33602 J. Edward Curren, Esqulre Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 33512-9712 L. M. Blain, Esquire Charles G. Stephen Esquire Anita C. Brannon, Esquire Blain & Cone, P.A. 202 East Madison Street Tampa, Florida 33602 George M. Hebbard, Jr. Route 3, Box 430 Lithla, Florida 33547 Gary W. Kuhl, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 33512-9712
The Issue The issue to be determined in this case is whether Respondents, United States Sugar Corporation (“USSC”), Sugar Farms Co-op (“SFC”), and Sugar Cane Growers Cooperative of Florida (“SCGC”) (collectively “the Applicants”) are entitled to the Everglades Works of the District permits (“WOD Permits”), issued to them by the South Florida Water Management District (“District”).
Findings Of Fact The Parties Audubon is a not-for-profit organization dedicated to restoring and conserving natural ecosystems, focusing on birds and their habitats. Audubon has a substantial interest in the protection of the Everglades and other ecosystems in the area. Audubon’s interest is affected by the proposed agency action because the WOD Permits authorize agricultural discharges that affect these ecosystems. The District is a Florida public corporation with the authority and duty to administer regulatory programs in chapter 373, and Florida Administrative Code Title 40E, including a program for regulating discharges from the Everglades Agricultural Area (“EAA”) into works of the District. The EAA is located south of Lake Okeechobee and comprises about 570,000 acres. The majority of EAA agriculture is sugarcane, with some row crops, such as radishes, leafy vegetables, and corn, and turf sod. During fallow periods, rice is also grown. The Applicants are owners and lessees of agricultural lands in the EAA. Background Some essential background for this case is set forth in rule 40E-63.011: The Everglades is a unique national resource. It has a high diversity of species, and provides habitat for large populations of wading birds and several threatened and endangered species, including wood storks, snail kites, bald eagles, Florida panthers, and American crocodiles. Large portions of the northern and eastern Everglades have been drained and converted to agricultural or urban land uses. Only 50% of the original Everglades ecosystem remains today. The remainder is the largest and most important freshwater sub-tropical peatland in North America. The remaining components of the historic Everglades are located in the Water Conservation Areas (WCAs) and Everglades National Park (ENP). ENP and Loxahatchee National Wildlife Refuge (WCA 1) are Outstanding Florida Waters, a designation which requires special protection for the resource. Large portions of the Everglades ecosystem have evolved in response to low ambient concentrations of nutrients and seasonal fluctuations of water levels. Prior to creation of the Everglades Agricultural Area (EAA), nitrogen and phosphorus were mainly supplied to large areas only in rainfall. Phosphorus is the primary limiting nutrient throughout the remaining Everglades. Sawgrass has lower phosphorus requirements than other species of Everglades vegetation. A substantial portion of EAA nutrients is transported to the remaining Everglades either in dissolved or in particulate form in surface waters. The introduction of phosphorus from EAA drainage water has resulted in ecological changes in substantial areas of Everglades marsh. These changes are cultural eutrophication, which is an increase in the supply of nutrients available in the marsh. The increased supply of phosphorus in Everglades marshes has resulted in documented impacts in several trophic levels, including microbial, periphyton, and macrophyte. The areal extent of these impacts is increasing. In 1988, the United States sued the District and the Florida Department of Environmental Regulation, now the Department of Environmental Protection (“DEP”), in federal court, alleging that the agencies failed to enforce Florida’s water quality standard for nutrients in waters of Loxahatchee Wildlife Refuge and Everglades National Park. The principal pollutant of concern was phosphorus. Audubon, USSC, and certain members of SCGC and SFC intervened in the federal case. In February 1992, the parties resolved their dispute through a settlement agreement approved by the federal court (“the Consent Decree”). The Consent Decree required the District and DEP to take action to meet water quality standards by December 31, 2002. At that time, the nutrient water quality standard was a narrative standard, prohibiting the discharge of nutrients so as to cause “an imbalance in natural populations of aquatic flora and fauna.” The Consent Decree directed the District to construct 34,700 acres of stormwater treatment areas (“STAs”) so that nutrient-laden surface water discharged from the EAA could be treated before discharge to the Everglades Protection Area (“EvPA”), which includes Loxahatchee Wildlife Refuge, Everglades National Park, and the Water Conservation Areas. STAs are large freshwater wetlands which remove phosphorus from the water column through physical, chemical, and biological processes such as sedimentation, precipitation, plant growth, and microbial activity. The first STAs were constructed and in operation in 1993. The Applicants operate in the S-5A Basin within the EAA. Their surface water is conveyed to STA-1W for treatment before being discharged to the EvPA. The Consent Decree required the District to initiate a regulatory program by 1992 to require permits for discharges from internal drainage systems (farms) in the EAA. The regulatory program was to be based on agricultural best management practices (“BMPs”). The goal of the program, as stated in the Consent Decree, was to reduce phosphorus loads from the EAA by 25 percent over the base period (1979-1988). In 1992, the District promulgated rule chapter 40E-63, which required EAA farmers to obtain WOD permits and to implement agricultural BMP plans. The BMP plans address fertilizer use and water management. Permittees must also implement a water quality monitoring plan. The rules require reduction of the total phosphorus loads discharged from the EAA Basin, as a whole, by 25 percent from historic levels. See Fla. Admin. Code R. 40E-63.101. If the EAA, as a whole, is in compliance, individual permittees are not required to make changes to their operations. See Fla. Admin. Code R. 40E-63.145(3)(d). If the 25 percent reduction requirement is not met, the rule contemplates that individual permittees in the EAA would have to reduce nutrient loads in their discharges. See Fla. Admin. Code R. 40E-63.145(3)(e).1/ The Consent Decree also required the District to obtain permits from the Department for discharges from the STAs to the EvPA and to conduct research and adopt rules to “numerically interpret” the narrative standard. In 1994, the Florida Legislature enacted the Everglades Forever Act (“the Act”), chapter 94-115, Laws of Florida, which is codified in section 373.4592. The Legislature authorized the district to proceed expeditiously with implementation of the Everglades Program. See § 373.4592(1)(b), Fla. Stat. The “Everglades Program” means the program of projects, regulations, and research described in the Act, including the Everglades Construction Project. The Everglades Construction Project involved the construction of 40,452 acres of STAs, which is 5,350 acres more than was required by the federal Consent Decree. The Act acknowledged the BMP regulatory program for the EAA that the District had established in rule chapter 40E-63, and stated: Prior to the expiration of existing permits, and during each 5-year term of subsequent permits as provided for in this section, those rules shall be amended to implement a comprehensive program of research, testing, and implementation of BMPs that will address all water quality standards within the EAA and Everglades protection Area. See § 373.4592(4)(f)2., Fla. Stat. The Act required DEP to issue permits to the District to construct, operate, and maintain the STAs. See § 373.4592(9)(e), Fla. Stat. The Act required development of a numeric water quality phosphorus standard for the EvPA by 2003. See § 373.4592(4)(e), Fla. Stat. The Act set the goal of achieving the phosphorus standard in all parts of the EvPA by December 31, 2006. In June 1995, modifications were made to the Consent Decree. The deadline for achieving water quality standards in the EvPA was changed from December 31, 2002, to December 31, 2006. The STAs were increased from 34,700 acres to 40,452 acres. The chronological developments outlined above indicate the intent of the Legislature and the parties to the Consent Decree to conform state law and the Consent Decree to each other. In 2001, DEP initiated rulemaking that lead to its adoption of the Phosphorus Rule, rule 62-302.540, in 2003. The rule set a numeric phosphorus criterion for the EvPA of 10 parts per billion (“ppb”), applied through a four-part test in which attainment is determined separately for “unimpacted” and “impacted areas” of the EvPA. See Fla. Admin Code R. 62- 302.540(4). In conjunction with this rulemaking, the DEP and District developed the Everglades Protection Area Tributary Basins Long Term Plan for Achieving Water Quality Goals (“Long- Term Plan”) in March 2003. The Long-Term Plan provided remedial measures and strategies divided into pre-2006 projects and post- 2006 projects. The pre-2006 projects included structural and operational modifications to the existing STAs, implementation of agricultural and urban BMPs in areas outside the EAA or C-139 basins, and construction of several restoration projects congressionally mandated by the Comprehensive Everglades Restoration Plan. Modeling of treatment capabilities of the STAs after implementation of the pre-2006 projects predicted that the 10 ppb standard for phosphorus could be achieved, but not consistently. Therefore, the Long-Term Plan required the District to identify and evaluate methods to improve phosphorus reductions, and if the phosphorus criterion was not achieved by December 31, 2006, to implement post-2006 modifications and improvements. The post- 2006 strategies include projects to expand and improve the STAs. They do not include changes to the BMP program. In 2003, the Legislature substantially amended the Act. It incorporated the Long-Term Plan into the Act, finding that it “provides the best available phosphorus reduction technology based on a combination of the BMPs and STAs.” § 373.4592(3)(b), Fla. Stat. The Long-Term Plan contemplates maintenance of the BMP program in the EAA, with refinements derived from BMP research. Recent Conditions and Events As previously stated, chapter 40E-63 requires the total phosphorus load from the EAA to be reduced by not less than 25 percent from historic levels. Since full implementation of the BMP regulatory program, annual phosphorus loads have been reduced by approximately 50 percent. Despite the efforts and projects undertaken, the phosphorus standard was not being achieved as of December 31, 2006, in all parts of the EvPA. In 2007, the DEP issued a permit to the District for discharges from the STAs to the EvPA (referred to as the “Everglades Forever Act” or “EFA permit”). The permit required the District to design and construct several regional water management projects, including structural enhancements to STA-1W, and the construction of 6,800 acres of additional STAs. The permit and its compliance schedules provided interim relief through 2016 from the water quality based effluent limitation (WQBEL) necessary to achieve the 10 ppb phosphorus standard. The 2007 EFA permit was not challenged by Audubon or any other entity. The District, DEP, and the United States Environmental Protection Agency began working together in 2010 to develop new strategies for achieving compliance with the phosphorus standard in the EvPA. The agencies determined that compliance could be achieved by expanding the STAs by 7,300 acres (6,500 acres would be added to STA-1W) and constructing flow equalization basins to store up to 110,000 acre feet of stormwater runoff. These basins are designed to attenuate peak flows into the STAs in order to improve the processes that remove phosphorus. In September 2012, DEP issued the District a new EFA permit, which authorized continued operation of the District’s S-5A pump station, STA-1W, and the related conveyance systems by which stormwater runoff from the S-5A Basin is ultimately discharged to the EvPA. The permit was issued with a Consent Order, requiring the District to expand STA-1W by 6,500 acres of effective treatment area in accordance with a timeline and the District’s Restoration Strategies. The 2012 EFA Permit and Consent Order were not challenged by Audubon or any other entity. In 2013, the Legislature amended the Act again. The Act’s reference to the Long-Term Plan was revised to include the District’s Restoration Strategies Regional Water Quality Plan, which called for expanding the STAs and constructing flow equalization basins. See § 373.4592(2)(j), Fla. Stat. The Legislature added a finding that “implementation of BMPs, funded by the owners and users of land in the EAA, effectively reduces nutrients in waters flowing into the Everglades Protection Area.” See § 373.4592(1)(g), Fla. Stat. The 2013 amendments indicated the Legislature’s intent to codify into law the strategies developed by the District and other regulatory agencies to achieve water quality standards in the EvPA. Those strategies do not materially change the BMP program in the EAA. The Act and the rules of the District create programs for achieving restoration of the EvPA that rely heavily on the STAs. Over the years, the STAs have repeatedly been enlarged and enhanced. In contrast, the requirement for farmers in the EAA to reduce their phosphorus loading by 25 percent has not changed in 21 years. It is beyond the scope of this proceeding to question the wisdom of the programs that have been established by statute and rule. Whether Additional Water Quality Measures Are Required A principal dispute in this case is whether the WOD Permits must include additional water quality measures to be implemented by the Applicants. Section 373.4592(4)(f)4. provides that, as of December 31, 2006, all EAA permits shall include “additional water quality measures, taking into account the water quality treatment actually provided by the STAs and the effectiveness of the BMPs.” Audubon asserts that the requirement for additional water quality measures has been triggered. The District does not interpret the statute as requiring additional water quality measures under current circumstances. The interpretation of the statute is primarily a disputed issue of law and is addressed in the Conclusions of Law. There, it is concluded that additional water quality measures are not required. Whether the BMP Plans are Adequate Audubon contends that the WOD Permits should be denied because the Applicant’s existing BMP plans are not “tailored” to particular soils, crops, and other conditions. This contention is based on section 373.4592(4)(f)2.c., which states in relevant part: BMPs as required for varying crops and soil types shall be included in permit conditions in the 5-year permits issued pursuant to this section. Audubon showed that the Applicants have similar BMP plans for the thousands of acres covered in the three WOD Permits, and contends that this similarity proves that BMPs are not being tailored to specific farm conditions. However, soils and crops are similar throughout the EAA. The soils of the EAA are almost entirely muck soils and the primary crop is sugarcane with some corn or other vegetable rotated in. The Applicants use many of the same BMPs because they have similar soils and grow similar crops. There are three main categories of BMPs implemented in the EAA: nutrient and sediment control BMPs, particulate matter and sediment control BMPs, and water management BMPs. See Fla. Admin. Code R. 40E-63.136, Appendix A2. The BMPs proposed by the Applicants are based on research in the EAA and recommendations specifically for EAA soils and the crops grown there. The Applications do not identify the specific BMPs that will be implemented, but only the number of BMPs that will be selected from each of the BMP categories (i.e., sediment control). The Applicants must use BMPs on the District’s list of approved BMPs unless an alternative BMP is requested and approved. The lack of greater detail was explained as necessitated by the need for flexibility during the life of the permit to adapt BMPs to varied crops and conditions. Audubon does not believe the BMP plans are tailored enough, but there is no rule criterion for determining how tailored BMP plans must be, except they must achieve the overall goal of reducing phosphorus loading in discharges from the EAA by at least 25 percent. This goal is being achieved.2/ Audubon did not show that any particular BMP being used by an Applicant was the wrong BMP for a particular soil and crop, or identify the BMP that Audubon believes should be used. Audubon failed to prove that the Applicants’ BMP plans do not meet applicable requirements. Whether the Applications Are Complete Audubon contends that the WOD Permits must be denied because the Applications are incomplete. Many of Audubon’s completeness issues deal with minor discrepancies of a type that are more appropriately resolved between the District and applicants, not violations of criteria that are likely to affect a third party’s interest in environmental protection. Rule 40E-63.130 lists the requirements for a permit application for activities in the EAA Basin. An Application Guidebook is incorporated into chapter 40E-63, which contains instructions for completing the application. For applications to renew a permit, the practice of the District is to not require the resubmittal of information that was previously submitted to the District and which has not changed. The Application Guidebook explains this practice. The Applicants supplemented their applications at the final hearing to provide information that Audubon claimed was omitted from the Applications.3/ Audubon contends that the Applications are incomplete because some application forms are not dated and other forms are not signed by appropriate entities. The District explained its rule interpretation and practices associated with the forms. Additional signatures and dates were submitted at the final hearing. Audubon failed to demonstrate that the Applications are incomplete based on the identity of the persons who signed application forms or the lack of dates. Audubon contends the Applications are incomplete because copies of contracts or agreements are not included as required by rule 40E-63.132(3). Audubon failed to prove that contracts and agreements exist that were not included. Audubon contends the Applications are incomplete because they do not contain a completed Form 0779, entitled “Application For A Works Of The District Permit,” as required by rule 40E-63.132(5). In some cases, the information for Form 0779 had been previously submitted and was unchanged, so the District did not require it to be resubmitted for the permit renewal. Additional information was provided at the final hearing. Audubon failed to prove that the Applications are incomplete based on missing information on Form 0779. Audubon contends that the Applications are incomplete because documentation regarding leased parcels was missing. Pursuant to rule 40E-63.130(1)(a), individual permit applications must be submitted by the owner of the land on which a structure is located and any entity responsible for operating the structure, and the permit application must include the owners of all parcels which discharge water tributary to the structure. Applications may be submitted by a lessee if the lessee has the legal and financial capability of implementing the BMP Plan and other permit conditions. The District explained that when applications are submitted by a lessee who will be the permittee or co-permittee, the District requires the lessee to be a responsible party for the entire term of the permit, which is five years. If the lessee is a not a co-permittee, the District does not require information about the lease and does not require the lessee’s signature. If the lessee is a co-permittee, but the lease expires during the term of the permit, the District requires the applicant to modify the permit when the lease expires. Audubon failed to prove that the Applications are incomplete based on lease information Audubon contends that the Applications are incomplete because they fail to show that the Applicants participated in an education and training program as required by rule 40E- 63.136(1)(g). The preponderance of the evidence shows that the Applicants participated in education and training programs. Audubon failed to prove that the Applications are incomplete for any of the reasons raised in its petition for hearing or advanced at the final hearing. Water Quality Standards in the EAA Audubon presented some evidence of algal accumulations in ditches and canals, but the evidence was insufficient to prove the Applicants are violating water quality standards applicable in the EAA. Summary Audubon failed to carry its burden to prove that the Applicants are not entitled to the WOD Permits.
Recommendation Based on the foregoing Findings of Facts and Conclusions of Law, it is RECOMMENDED that South Florida Water Management District issue Permit Nos. 50-00031-E, 50-00018-E, and 50-00047-E. DONE AND ENTERED this 10th day of February, 2014, 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 10th day of February, 2014.
Findings Of Fact Application No. 76-00254 seeks a consumptive use water permit for 1.08 million gallons per day average daily withdrawal and 2.16 million gallons per day maximum daily withdrawal from one well. This is a new use. The purpose of the consumptive use is a semi-enclosed irrigation system for the irrigation of tomatoes in south Hillsborough County. The water is to be taken from the Floridan Aquifer with some discharge off site. According to Barbara Boatwright, hydrologist for the district, there is some possibility that salt water intrusion may occur, but the district has never documented it in the subject area. The consumptive use will exceed the water crop as defined by the district because 25 percent of the water used will run off site and thus be lost. Except as otherwise stated above, none of the conditions set forth in Subsection 16J-2.11(2),(3) or (4), F.A.C., will be violated. The Southwest Florida Water Management District's staff recommends issuance of the subject permit in the amounts requested with the following conditions: By January 1, 1978, applicant shall reduce runoff to 8.6 percent of the amount pumped, which reduction will bring the amount pumped within the water crop as defined by the district. That the applicant analyze the quality of the water at the beginning and end of each production season and that these analyses be submitted to the district. That the district be allowed to install flowmeters on any discharge canal and on the pump with proper notification of applicant and to enter on property to read the meters.
Recommendation Noting that, with the conditions requested by the Southwest Florida Water Management District's staff, issuance of the sought for permit appears consistent with the public interest, it is RECOMMENDED that a consumptive use permit be issued pursuant to Application No. 75-00254 with the conditions set forth in paragraph 4. CHRIS H. BENTLEY Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Terry Elsberry Staff Attorney Elsberry Brothers, Inc. Southwest Florida Water Route 2, Box 70 Management District Ruskin, Florida 33570 Post Office Box 457 Brooksville, Florida 33512
The Issue The issue for consideration at the hearing was whether the Respondent, Roger Harloff, should be issued a consumptive use permit to withdraw and use ground water from the wells on his property, and if so, in what amount and under what conditions.
Findings Of Fact Respondent, Roger Harloff, owns several farms in southeastern Manatee County, Florida which, taken together, make up an irregular 8,500 acre tract located approximately 2 1/2 miles north of the City of Sarasota's Verna Wellfield. Mr. Harloff grows vegetables on much of this tract, of which approximately 1,500 acres is devoted to tomatoes. This tomato crop is the prime crop produced by Mr. Harloff, and provides the raw material for the Harloff packing plant which is dependent upon the tomato crop in order to stay in business. Mr. Harloff also operates a plant nursery at which he produces many if not most of the seedling plants utilized in his vegetable growing operations. In order to be economically feasible and remain operative, Mr. Harloff must farm approximately 3,800 acres during the Spring growing season and approximately 3,000 acres during the Fall. These acres are made up of tomatoes and other vegetables. The packing plant and the plant nursery are dependent upon the farm operation and without adequate water, the farm operation cannot be successfully carried on. In September 1988, Mr. Harloff applied to the District for a consumptive use permit to withdraw water from twelve wells located on his property, requesting an annual average rate of 12,995,606 gpd, and a maximum daily rate of 47,520,000 gpd. The consumptive use permit application filed by Mr. Harloff was assigned District Number 204467.04. After evaluation of the application in conjunction with its needs and policies, the District issued a staff report and proposed agency action on the application which recommended issuance of the permit authorizing water to be drawn from the 12 wells at a rate approximating that requested in the application. Thereafter, the City of Sarasota, which operates the nearby Verna Wellfield, considering that the proposed withdrawal would have a substantial adverse impact on its wellfield operations, filed a Petition for Formal Administrative Hearing objecting to the issuance of the permit to Mr. Harloff. Though Mr. Harloff has owned much of the property which make up the 8,500 acre tract in question here, at the time of his application, he did not own, but had under contract, a substantial portion. He closed on the purchase of that remainder after he received notice of the District's intention to issue the permit in question but prior to the City's filing its Petition For Formal Hearing. The purchase price of the property in question was $9,000,000.00 which carries an interest payment on the financed portion of $52,000.00 per month. The wells pertinent to the issues in this proceeding are as follows: # Cons. Depth Cas. Lin. Diam. Cap. Loc. 1 1978 1185' 200' 220-490' 12" 2000 gpm SE 2. 1988 1320' 210' 210-480' 16" 3000 gpm SE 9. 1974 1130' 390' 16" 3000 gpm C 10. 1976 1232' 231' 283-400' 16" 3000 gpm NW 11. 1979 1120' 210' 260-480' 12" 2000 gpm NW 12. 1976 1180' 480' 12" 2000 gpm SW 3. 1989 1434' 460' 16" 3000 gpm SE 5. 1989 1374' 610' 16" 3000 gpm W 8. 1989 1292' 548' 16" 3000 gpm NW 13. 1989 1310' 635' 16" 2000 gpm NE Well No. 8 was used as the pump test well for the constant rate discharge test and Well No. 13 was the deep observation well for that test. Wells 1, 2, 9, 10, 11, and 12 have all been previously permitted by the District and No's 1, 2, 9 and 10 are currently permitted under two other permits, while 11 and 12 were permitted under a different permit. Wells No. 3, 5, 8 and 13 have been authorized for construction but not, as yet, to produce water. Wells 4, 6 and 7 have not yet been constructed. The intention is to drill them to a depth of 1,300 feet and case them to 600 feet. Each will have a pump capacity of 3,000 gpm. Number 4 will be in the southeast portion of the tract, number 6 in the central portion, and number 7 will be located just north of number 6. Wells 1, 2, 9, and 10 currently have a combined permitted maximum daily rate of 13,680,000 gallons under permits number 204467.03 for 1 and 2, and 204630 for 9 and 10. The former was issued on December 29, 1987 and will expire on December 29, 1993, and the latter, issued on October 7, 1981, will expire on that same day in 1991. The permit previously issued for wells 11 and 12 authorized withdrawal at a maximum daily rate of 2,160,000 gallons. That permit, number 204374, expired on September 9, 1986 and was not renewed. After the City filed its Petition challenging Mr. Harloff's proposed permit, Mr. Harloff, on June 26, 1989, filed an amended application to withdraw water at an average annual rate of 10.99 mgd and a maximum daily rate of 48.96 million gallons. This amended application refers to an additional proposed well, Number 13. The District, however, had previously approved wells 3 - 8 and 13, and pursuant to this authorization, wells 3, 5, 8, and 13 were built. Mr. Harloff submitted additional amendments to his application on August 7 and 9, 1989. The former requests a seasonal average daily rate of 25.34 mgd and a seasonal maximum daily rate of 32.79 mgd. The latter requests a seasonal average rate of 26.18 mgd, an annual average rate of 15.18 mgd, and a seasonal maximum rate of 31.56 mgd. In that regard, a seasonal rate is the same as an annual rate, (average or maximum) when applied to a growing season as opposed to a year. The additional amendments to the application were evaluated by District staff who, on August 18, 1989, issued a revised staff report and a proposal to issue to Mr. Harloff a consumptive use permit authorizing an average annual withdrawal of 11.1. mgd, an average seasonal withdrawal of 15.6 mgd, and a seasonal maximum withdrawal of 20.1 mgd. The proposed permit also contains terms and conditions which, the District contends, will, inter alia, permit Mr. Harloff to withdraw more water than he is currently authorized without additional adverse impact on the City's Verna Wellfield. It is to some of these terms and conditions that Mr. Harloff objects. Since the issuance of the revised staff report and intent to issue, the parties have negotiated on the various terms and conditions in question and have agreed to some and the amendment of others. Mr. Harloff has no objection to conditions number 1, 2, 3, 7 - 14, 23, 24, 26, 28 - 30, 32, and 34 & 35. The parties agree that other conditions, as indicated herein, should be amended as follows: Condition 19, on the third line, should be changed to read, " up to 20 inches tapering to 12 inches." Condition 22, on the second line, should be changed from "30 days" to "10 days". Condition 25, on the first line, should be changed from "within 60 days" to within 120 days". Condition 31, on the third line, starting with "following month" should be changed to "following months: January, April, July and October". Also, under Sampling Frequency, "Monthly" should be changed to "Quarterly". Condition 33, on the ninth line, insert the work "economically" before the word "feasible" in the phrase "specific operation and irrigation improvements are feasible". Mr. Harloff objects to conditions 4, 5, 15 - 17, 20 & 27. He does not object to the proposed new standards for new wells. Taken together, the parties then disagree only on the requirement for abandonment or refurbishment of existing wells and the quantities of water Mr. Harloff will be allowed to draw. The City supports the District's position on both issues. The City of Sarasota owns and operates a public water system to serve between 50 to 75 thousand people located in Sarasota County. The primary source of water for this system is the Verna Well field which is also owned by the City and which accounts for approximately 60 percent of the City's water needs. The City also operates a reverse osmosis, (R.O.) water desalinization facility, and has back-up wells at St. Armond Key and at the Bobby Jones Wellfield. The Verna Wellfield is located about 17 miles east of the Sarasota city limits on approximately 2,000 acres of land in northeastern Sarasota County. It consists of two tracts of land: Part "A", which is approximately 1/2 mile wide by 4 miles long; and Part "B", which is approximately 1 mile square located about 500 feet southeast of Part "A". The Verna Wellfield's permitted allocation is based on whether the R.O. facility is producing at capacity. If it is, the Verna daily allocation is 7 mgd, and if not, 9.5 mgd. The R.O. facility's capacity is 4.5 mgd and the backup wells have a capacity of 1.7 mgd. The wellfield contains 39 permitted production wells, 30 of which are in Part "A" and 9 of which are in Part "B." One of them, well 30, is currently inactive. The wellfield has been in operation as a part of the City's public water system since September 1966. When the Verna Wellfield was constructed in 1965-1966, its original design specified casing on most wells down to 140 feet with pump bowl settings at 125 feet. Each pump was to have a total dynamic head, (TDH) of 200 feet. Over the years, the City has decreased the TDH of the pumps at Verna from 200 feet to 175 feet. This has resulted in a reduction of the pumps' ability to produce water with sufficient pressure to carry it to the discharge point. This decline has been caused by an increase in withdrawal of water regionally, and not solely because of withdrawals from the Verna Well field. Verna is impacted by the use of water outside the boundaries of the wellfield. The City has an ongoing program calling for the refurbishment of 2 to 3 wells per year at the Verna Wellfield. It is the City's intent to convert the pumps to 200 feet TDH on all well refurbishments in the future. In August 1977, a program requiring permits for the consumptive use of water was implemented in both Sarasota and Manatee Counties. At that time, the Verna Wellfield had a production rate of 6.9 mgd annual average daily rate. On January 6, 1978, the City applied for a permit for Verna and on April 3, 1979, the District issued permit number 27804318 to allow the City to draw water from the Verna Wellfield. The City applied for a renewal of that permit in October 1983 and thereafter, in January 1985, the District authorized the continued withdrawal of water from Verna by the issuance of permit 204318 which, at Condition 18, placed limitations on the City's use of water from the wellfield. Specifically, the permit limited withdrawals from Verna to: ...6,000,000 gallons per day average and 7,000,000 gallons per day maximum, except during those times when ... [the R.O. process is reduced or to facilitate maintenance or repairs]. At such times, ... [withdrawals) may be increased to provide additional supplies not to exceed 8,000,000 gallons per day average annual and 9,500,000 gallons per day maximum. This condition clearly provides for additional supplies to be drawn to increase the Verna Well field production to a total of 8,000,000 and 9,500,000 mgd, respectively, not in addition to the regular permitted amount, by those quantities. The City's permit has been neither suspended nor revoked nor is any violation enforcement action currently under way. The current permit expires January 9, 1991. The water pumped from the Verna wells is held in a 1,000,000 gallon reservoir at the wellfield. This reservoir, which is topped at approximately 22 to 23 feet, electronically controls the pumping activity at the well field by turning on and shutting off pumps, in series, as the water level in the reservoir rises and falls. The water, when needed, is transmitted to another reservoir near the City's treatment plant in downtown Sarasota by gravity flow through a 30" diameter, 92,000 foot long pipe. The flow rate is approximately 5,000 gpm normally. When the treatment plant needs more water, a pump at the well field forces the flow at a rate of between 7,200 to 8,200 gpm, depending upon the level of water in the receiving reservoir. A flow of 8,200 gpm would draw 11.8 mgd from the wellfield. The operating capacity of the Verna Wellfield, in August 1988, was 17.9 mgd. Harloff's experts assert, and there is no concrete evidence to rebut it, that if all wells at Verna were pumping during a 24 hour period in May 1989, the reservoir could have been maintained at full level. However, though there is a manual override of the automatic reservoir/pump control system, it is unrealistic and unwise to expect full production on a 24 hour basis for any lengthy time period. Water under both Mr. Harloff's property and the Verna Well field is found at various levels known by different names. These include, in order of descent, the Surficial Aquifer, the Intermediate Aquifer, the Upper Floridan Aquifer, and the Lower Floridan Aquifer. The Surficial Aquifer extends from the surface down to between 20 and 60 feet below the surface. A 20 foot thick bed of clay separates the water in this aquifer from that in the aquifer immediately below it, the Intermediate Aquifer, which extends from approximately 80 feet down to approximately 420 feet below the surface. In the lower part of the Intermediate Aquifer, permeability decreases until a confining unit separating the bottom of the Intermediate Aquifer from the top of the Upper Floridan Aquifer is formed. There is such a confining unit between 420 and 500 feet. There is no well-defined confining unit between the Upper and Lower Floridan Aquifers. There is, however, a substantial difference in the transmissivity in each zone. "Transmissivity" is defined as the amount of water that will exist through a section of the aquifer that is the same width from the top to the bottom. The lower the transmissivity rate, the deeper the cone and the narrower the radius of effect. The higher the rate, the shallower the cone and the broader the radius. The Lower Floridan Aquifer has an extremely high transmissivity. Its top is found at a range of from 1,050 to 1,200 feet below the surface on Mr. Harloff's property. The water from the Upper Floridan Aquifer is of higher quality than that in the Lower. It is more readily usable for drinking than that in the Lower, but the Lower water is quite acceptable for agricultural purposes. What confining layer exists between the Upper and Lower Floridan Aquifers is made up of relatively impermeable anhydrides and gypsum. Because of this, there is little likelihood of the highly mineralized water from the Lower Floridan Aquifer rising into the better quality water in the Upper. If, therefore, water for agricultural purposes is drawn from the Lower Floridan Aquifer, with its high transmissivity and narrower cone radius, and if the wells utilized to procure this water are cased down to within the Lower aquifer, there is little chance of a negative impact on the better quality water, used for drinking by the City, within the Upper Floridan and Intermediate Aquifers. Mr. Hardin, an expert geologist and hydrogeologist testifying for Mr. Harloff, concluded, utilizing certain commonly accepted computer models, that Mr. Harloff's requested additional withdrawals would not have a significant effect on the Verna Wellfield's ability to produce water sufficient for the City's needs. This conclusion was based on 1989 seasonal use figures including an average rate of 21.95 mgd, a maximum rate of 27.04 mgd, and a maximum rate of 29 mgd under a "run time" calculation and the fact that during that period, the City was able to pump at least its permitted quantity from its wells at Verna. The City and the District do not accept this conclusion as reasonable, however, because, they claim, the withdrawal figures cited are not meter readouts but estimates based on the number of acres farmed and the number of pump operating hours during the period in question. The City's experts contend the data used by Hardin and Prochaska in their opinions is not that which other experts in the field would reasonably rely upon. They do not appear to be unrealistic, however, and, therefore, Mr. Hardin's opinion is accepted as but one factor to be considered. On the other hand, Mr. Anderson, also a Harloff expert hydrogeologist, claims the requested withdrawals would result in only an additional 1.7 foot drawdown in the Upper Floridan Aquifer underlying the Northeast corner of the Verna Well field. To be sure, this is only one small portion of the wellfield in issue. There has, however, been a continuing history of declining groundwater levels in this area over the past several years. After the 1975 drought, the City started to experience declining water levels at Verna which, because of the reduction in ability to produce water, required a lowering of the pump elements in some wells, and also caused the City to develop an R.O. facility in an effort to reduce dependence on well water. This drop in capability occurred again during the 1985 drought and this time the City modified the pump motors to shut off prior to cavitation and initiated a schedule of operating times for wells, so that water is drawn from different and geographically separated areas in a sequence designed to allow periodic regeneration of an area's supply. Nevertheless, water supply remains a concern at Verna, and the problems previously experienced continue to occur during periods of drought. In May 1989, the Verna Wellfield was periodically "unable" to meet it's short term peak demands at times even though all operating wells were pumping. This means that at the times in question, more water was being drawn from the Verna reservoir than could be replaced by pumping activities. It does not mean that the reservoir ran dry and water could not be furnished to the treatment plant. However, this condition is serious and indicative of a more serious shortage in the future unless appropriate safeguards are instituted. Mr. Balleau, the City's expert in hydrology and hydrogeology, and the District's experts all believe the Verna Wellfield is in trouble. It is operating well beyond its design range and the imposition of additional demands on it would seriously and adversely affect its ability to produce water. This position is supported by the facts and found to be accurate. There appear to be several options open to the City to contend with the Verna problem potential. These include: drill deeper wells at Verna to tap the Lower Floridan Aquifer. (This will produce the lower quality water found there and require additional treatment facilities. construct a linear wellfield along the pipeline from Verna to the treatment facility. (This will require additional permitting to draw the water, high construction and operating costs, and still result in low quality water requiring treatment. redevelop the downtown wells currently supplying the R.O. facility. (This will require satisfaction of regulatory issues, adversely impact on the users of the upper aquifers, possibly result in poor water quality and in contamination from nearby landfills.) develop a new well field southeast of Verna. (This will experience regulatory issues and high construction costs, with an unknown water quality result.) buy water from Manatee County. (This is expensive, may result in transmission and compatibility problems, and would be only a short term solution. lower pump assemblies; replace existing pumps and modify the pump circuits. (These are all unreliable, short term solutions of minimal benefit.) Mr. Harloff and the City/District disagree on the appropriate amount of water needed for the successful growing of the crops produced by his operations. Both agree, however, that the heaviest demands for water come in the spring growing season including April and May. Tomatoes require the most water. Peppers require nearly as much. This is because the short root systems require a higher water table in the soil to supply needed moisture. In its analysis of Mr. Harloff's application, the District, referring to tables developed for the purpose of allocation and relating to Harloff's watering history during the period from August 15, 1988 to June 7, 1989, subtracted the fall season recorded application of 20.7 acre-inches from the total 10 month figure of 50.92 acre-inches and concluded he would need 30.22 acre-inches for peppers during the spring, 1989 season. Unless shown to be totally unreasonable, however, (not the case here), the applicant's water need figures should be accepted. Mr. Harloff's operation constitutes an important part of Manatee County's agricultural economy, and agriculture utilizes 68.9 percent of the land in the county. Agricultural products sold in Manatee County in 1987 were valued at $145,655,000.00, which ranked Manatee County third among all Florida counties in vegetable production. Agriculture is the fourth largest employer in Manatee County, employing an average of 4,692 people per month. Through his farm operation alone, Harloff employes as many as 1,050 people, with 200 employed on a full-time basis. Experts estimate that the loss of the Harloff operation would cause a reduction of between 16 and 18 million dollars in agricultural sales in the county with an additional loss in jobs and income to his suppliers. This estimate is not at all unreasonable. Florida produces approximately 95 percent of all tomatoes grown in this country for the fresh tomato market during the winter growing season. Tomatoes are the single largest vegetable crop grown in the state and accounted for 39.7 percent of the total value of vegetables produced in Florida during the 1987-1988 growing season. Mr. Harloff produced 4.8 percent of the total shipment of tomatoes from this state during that period. Water, primarily through irrigation, is an indispensable portion of the farming operation for this crop. Mr. Harloff currently irrigates the majority of his non-citrus crops by use of a "semi-closed ditch irrigation system", as opposed to a "drip system." The drip system is considerably more efficient than the semi-closed system having an efficiency rating, (amount of water actually used by the plants) of between 80 to 90 percent, as opposed to 40 to 60 percent for the other. While Mr. Harloff could reduce his water needs considerably and achieve substantial savings on pump fuel by conversion to a drip system for all or a part of his crops, such an undertaking would be quite costly. One of the conditions proposed by the District for the approval of Harloff's permit, as amended, is the refurbishment of several of the existing wells utilized by Mr. Harloff to make them more efficient and to promote the withdrawal of water from the Lower Floridan Aquifer, in which there appears to be adequate water and from which the Verna Well field does not draw. Currently, Mr. Harloff has seven wells which do not meet the standards of this proposed condition. They are not drilled to 1,300 feet below mean sea level and are not cased to 600 feet. To bring these wells into compliance, they would have to be drilled to the 1,300 foot level, or to a level which has a specific capacity of 400 gpm, and the casings in each would have to be extended to 600 feet. Extending the casings would be a complicated procedure and Harloff's experts in the area cannot guarantee the procedure would successfully achieve the desired end. Assuming the retrofit was successful, the cost of the entire process would be approximately $15,000.00 to $16,000.00 per well. In addition, the process would, perforce, require reducing the diameter of the well from 10 to 8 inches, thereby necessitating increasing the pump capacity to produce sufficient water. The cost of this is substantial with an appropriate new pump costing somewhere between $10,000.00 and $15,000.00 each. Consequently, the anticipated cost of bringing the existing wells up to condition standards would be between $25,000.00 to $31,000.00 per well, while the cost of constructing a new well is between $40,000.00 and $50,000.00 per well. Mr. Harloff feels it would be more prudent for him to replace the existing wells rather than to retrofit them. This may be correct. Harloff experts also claim that extending the casings on the existing wells down to 600 feet would not provide a significant benefit to the aquifer nor cause any significant reduction in drawdown impact at Verna. The District and City experts disagree and, taken on balance, caution and the interests of the public indicate that a conservative approach is more appropriate. While Mr. Harloff proposes to convert the areas served by wells 1, 9, 11, and 12 to the growing of citrus which requires much less water than tomatoes, this would not be sufficient mitigation to offset the need for some modification if large amounts of water will still be drawn. The entire area under the District's jurisdiction has been experiencing a water shortage due to a lack of rainfall. As a result, in June 1989, the District adopted a resolution identifying an area, including the area in question here, as a "water use caution area." This was done because the Floridan Aquifer has been subjected to large seasonable drawdowns of the potientiometric surface, the level to which water in a confined aquifer can rise in a well which penetrates that acquifer. This drawdown is directly related to increased water use in the area, much of which is for agricultural purposes. As a result of the District's action, special conditions on well construction for consumptive use applicants have been imposed on a permit by permit basis to insure, as much as possible, that the applicant uses the lowest quality water appropriate for his intended purpose. These conditions are not unreasonable. While accepting the District's and City's conclusion that his wells, if permitted, would have some impact on the Verna Wellfield, Mr. Harloff does not concede that the impact is significant. Specifically, the difference in impact resulting from an increase from his currently permitted use of 13.68 mgd seasonal maximum and his requested use of 31.56 mgd seasonal maximum for wells 1, 2, 9, and 10 would be a maximum increased drawdown of 1.1 feet at the Intermediate aquifer and 1.8 feet at the Upper Floridan Aquifer. Both figures relate to that portion of the wellfield found in the northeast corner of Part A. If the anticipated usage for crops predicted by Mr. Harloff's experts for the spring of 1989 is accurate, the drawdown would be 0.2 feet for the intermediate aquifer and 0.4 feet for the Upper Floridan Aquifer measured at the northeast corner of Part B of the Verna We1lfield. Harloff's experts contend that additional impacts for the spring of 1989 included, the increased usage will not have a significant effect on Verna's ability to produce its permitted daily maximum withdrawal of 9.5 mgd. While this is an educated speculation, it should be noted that during May 1989, the Verna field was able to produce up to 8.3 mgd without using all wells during any 24 hour period. This does not consider, however, the problems encountered by the City as indicated by the wellfield personnel, and the fact that some of the City wells are not pumping water.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that Roger Harloff be issued a consumptive use permit, No. 204467.04, as modified, to reflect authorization to draw 15.18 mgd annual average, not to exceed 31.56 mgd seasonal maximum, conditioned upon compliance with the conditions found in the conditions portion of the permit, as modified to conform to the quantities as stated herein, and to include those requirements as to acre-inch and crop-acre limitations, well usage and abandonment schedules, well modification standards, and record keeping, as are contained therein. RECOMMENDED this 5th day of December, 1989, in Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 5th day of December, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE No. 89-0574 The following constitutes my specific rulings pursuant to s. 120.59(2), Florida Statutes, on all of the proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONER: City of Sarasota, joined by the District 1 & 2. Accepted and incorporated herein. 3. Accepted and incorporated herein. 8-12. Accepted and incorporated herein. 13. Accepted and incorporated herein. 14-22. Accepted and incorporated herein. 23-25. Accepted and incorporated herein. 26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29-33. Accepted and incorporated herein. Not a Finding of Fact but a statement of party position. & 36. Accepted. 37. & 38. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not a Finding of Fact but a comment on opponent's satisfaction of its burden of proof. 42-44. Accepted and incorporated herein. Accepted and incorporated herein. Rejected as a misstatement of fact. Water service was never interrupted. The deficiency was in the City's inability to keep its wellfield reservoir filled. 47-54. Accepted and incorporated herein. Accepted and incorporated herein. Rejected for the reasons outlined in 41. 57-62. Accepted and incorporated herein. 63. Rejected for the reasons outlined in 41. 64-66. Accepted and incorporated herein. Rejected for the reasons outlined in 41. Rejected. & 70. Accepted and incorporated herein. 71. & 72. Accepted and incorporated herein. 73. Accepted and incorporated herein. 74 & 75. Accepted and incorporated herein. Accepted. Not a Finding of Fact but a statement of party position. Rejected. Accepted. Irrelevant. 81-84. Rejected. 85. & 86. Accepted and incorporated herein. 87 & 88. Accepted and incorporated herein. 89. Accepted and incorporated herein. 90 & 91. Accepted and incorporated herein. 92. & 93. Accepted and incorporated herein. FOR THE RESPONDENT: Roger Harloff 1-9. Accepted and incorporated herein. 10-13. Accepted and incorporated herein. 14 & 15. Accepted and incorporated herein. 16-25. Accepted and incorporated herein. 26-28. Accepted and incorporated herein. 29 & 30. Accepted. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not proven. 35 & 36. Accepted and incorporated herein. 37 & 38. Accepted and incorporated herein. 39-41. Accepted and incorporated herein. 42 & 43. Accepted and incorporated herein. 44. Accepted. 45 & 46. Accepted and incorporated herein. 47 & 48. Accepted and incorporated herein. 49. Accepted. 50 & 51. Accepted and incorporated herein. Accepted. Accepted. Accepted. & 56. Accepted and incorporated herein. 57. Accepted. 58-60. Accepted and incorporated herein. 61 & 62. Accepted and incorporated herein. Rejected as unproven. Accepted. Accepted and incorporated herein. Accepted. 67-68. Accepted. Not a Finding of Fact but an interpretation of party po Accepted. Rejected. 72 & 73. Accepted. COPIES FURNISHED: Edward P. de la Parte, Jr., Esquire de la Parte, Gilbert and Gramovot, P.A. 705 East Kennedy- Blvd. Tampa, Florida 33602 Edward B. Helvenston, Esquire SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899 Douglas P. Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Peter G. Hubbell Executive Director SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
The Issue Whether Bay County has demonstrated its entitlement to the Permit?
Findings Of Fact The Ecologically Diverse Florida Panhandle With its high diversity of species and richness in endemic plants, the Florida Panhandle has been identified as one of six continental "biodiversity hot spots" north of Mexico. It has more species of frogs and snakes, for example, than any other equivalently-sized area in the United States and Canada and has botanical species that do not exist anywhere else in the Coastal Plain, one of the three floristic provinces of the North Atlantic American Region. The biodiversity stems from a number of factors. The Panhandle was not glaciated during the Pleistocene Period. Several major river systems that originate in the southern Appalachian Mountains terminate on the Panhandle's Gulf Coast. Its temperate climate includes relatively high rainfall. These factors promote or produce plentiful sources of surface and groundwater that encourage botanical and zoological life and, in turn, a diverse ecology. When compared to the rest of Florida, the Panhandle is relatively free from man-made impacts to its water resources. Until recently, the population growth rate lagged behind much of the state. Despite a rapid increase in the population in the late 1990s into the early part of the twenty-first century, it remains much less densely populated than areas in the I-4 Corridor and coastal peninsular Florida to the south. The Panhandle can be divided into physiographic areas of geological variation that are highly endemic; a substantial number of plant and animal species found in these areas are found nowhere else in the world. One of these areas is of central concern to this case. Located in southern Washington County and northern Bay County, it is known as the Sand Hill Lakes Area. The Sand Hill Lakes Area The Sand Hill Lakes Area (the "Area") is characterized by unusual geology that produces extraordinary ecological value. With few exceptions (see findings related to Dr. Keppner's flora and fauna inventories on the NTC/Knight Property below), the Area has not been extensively studied. The data on biological communities and water levels that exist, sparse as it is, has been obtained from historic aerials dating to 1941. The aerials are of some use in analyzing lakes and surface waters whose source is the Surficial Aquifer, but they are of limited value otherwise. They are not of use in determining the level in the Surficial Aquifer. Nor are they of assistance in determining river height when the banks of the river are covered by hardwood forest canopy. The resolution of the aerials is insufficient to show details of the various ecosystems. They do not show pitcher plants, for example, that exist at the site of hillside seepage bogs common in the Area. An aspect of the Area that the aerials do reveal is its many karst features on the surface of the land. Karst lakes and sinkholes dominate the Area and are a component of its highly unusual geology which is part of a larger system: the Dougherty Karst Plain. The Dougherty Karst Plain is characterized by numerous karst features: springs, caverns, sinkhole lakes, and sinkholes. Sinkholes In Florida, there are three types of sinkholes: cover subsidence, cover collapse, and "rock" or "cavern" collapse. Of the three, cover subsidence sinkholes are the most common in the state. Cover subsidence sinkholes form as the result of processes that occur on the surface. A cover subsidence sinkhole is usually a shallow pan typically not more than a few feet deep. Found throughout Central and South Florida, they are the most common type of sinkholes in most of peninsular Florida. In contrast, the other two major types of sinkholes (cover collapse and cavern collapse) occur as the result of processes below the surface that cause collapse of surface materials into the substrata. Both types of "collapse" sinkholes are found in the Area, but cover collapse is the more common. Cavern collapse sinkholes are relatively rare. Typical of the Area, cover subsidence sinkholes are not found on the NTC/Knight Property. The NTC/Knight Property The majority of the NTC/Knight Property is in Washington County, but the property straddles the county line so that a smaller part of it is in northern Bay County. All of the NTC/Knight Property is within the Area. The District recognizes that the NTC/Knight Property contains natural resources of extraordinary quality as does the Area generally. Over the three years that preceded the hearing, Dr. Keppner, an NTC/Knight expert, conducted extensive inventories of the flora and fauna on NTC/Knight Property. Dr. Keppner's inventory showed the NTC/Knight Property supports more than 500 species of vascular plants (flora with a system of tubes within the stem, phloem, and the xylem that exchange materials between the roots and leaves) and 300 species of animals. Among them are at least 28 vascular plants and six animals listed as imperiled (threatened or endangered) by state or federal agencies. At least 22 of the imperiled species of vascular plants and eight of the imperiled species of animals are located within an area expected to be affected by the Wellfield for which Bay County seeks the permit modification. For example, at Big Blue Lake alone where impacts were predicted by NTC/Knight experts to take place, the following imperiled plant species are found: Smoothbark, St. John's Wort, Kral's Yelloweyed Grass, Quilwort Yelloweyed Grass, Threadleaf Sundew, Panhandle Meadowbeauty, and Crystal Lake Nailwort. In addition to the Keppner inventory, NTC/Knight commissioned other studies to determine the nature of the sinkholes and whether they are connected to the Floridan Aquifer. NTC/Knight's experts determined that the property contains cover collapse and a few cavern collapse sinkholes that connect to the Floridan Aquifer. Despite evidence to the contrary submitted by the District and Bay County, the NTC/Knight determinations are accepted as facts for a number of reasons, including the lineup of the sinkholes and sinkhole lakes along identified photo-lineaments and the distribution of them in patterns that are not random. A District study using a dye test, moreover, confirmed conduit flow exists in the Area just east of the NTC/Knight Property. With regard to the distribution of the sinkholes and sinkhole lakes on the NTC/Knight Property, Dr. Sam Upchurch used the term "String of Pearls" to describe multiple sinkholes that exist along the edges of several lakes on the property. When sinkholes closer to the center of a lake are clogged or plugged with sediment and debris, the lakes continue to leak around the plugs which causes new sinkholes to form along the edge of the plugs. Examples of the "String of Pearls" formation on the edges of existing lakes are found at White Western and Big Blue Lakes on the NTC/Knight Property and at Crystal Lake nearby in Washington County. The multiple sinkholes bordering the edge of Big Blue Lake are examples of cover collapse sinkholes that, in geological terms, are relatively young as evidenced by their steep sides. In a karst area such as the Area, there is preferential flow in the conduits because of the difference of efficiency of transmission of water flowing through a porous medium of rock compared to that flowing though a conduit. Absent pumping in the Wellfield, the underlying aquifers are relatively stable. If the requested pumping does not take place, it is likely the stability will remain for a substantial period of time. It is not known with precision what will happen in the long term to the karst environment should pumping occur at the Wellfield at the rate the District proposes. When pumping occurs, however, water in the Area affected by the Wellfield will move toward the Wellfield. "[A]s it does[,] you may get some turbulent flow or vorticity in the water." Tr. 1391, (emphasis supplied). At some point, a change in the potentiometric surface and loss of buoyancy will most likely occur. This leads to concerns for Dr. Upchurch from two perspectives: One . . . is that if there is a[n affected] sinkhole lake [on the surface,] it may induce downward flow . . . the other . . . is that if it breaks the plug it may either create a new sinkhole or create a substantial drop in the level of water in the lake . . . which drains periodically, not necessarily because of a wellfield, but because that plug breaks. Id. In the first instance, lake levels could be reduced significantly. In the second, a new sinkhole could be created or the water level could drop dramatically as occurred at Lake Jackson in Tallahassee. Sand Hill Lakes Wetlands The Area contains a number of wetland communities. These include hillside seepage bogs, steepheads, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and creeks and streams in forested wetlands. A number of these wetlands occur on the NTC/Knight Property within the zone of influence in the Surficial Aquifer predicted by NTC/Knight's experts employing a model known as the "HGL Model." The wetland systems on the NTC/Knight Property are diverse, by type, plant species composition, and richness. This remarkable diversity led the District to recognize that the NTC/Knight Property contains lakes of nearly pristine quality, interconnected karst features, and endemic steephead ravines, all of which are regionally significant resources of extraordinary quality. The Area's wetlands also include many streams, among them Pine Log Creek, the majority of which is located on the NTC/Knight Property. Significant recharge to the Floridan Aquifer occurs on NTC/Knight Property. To the west, north, and east of the NTC/Knight Property are major concentrations of Floridan Aquifer springs that are crucial to the quality and character of regional surface water systems, including the Choctawhatchee River, Holmes Creek, and Econfina Creek systems. All of these surficial systems are dependent on the groundwater resources of the Area. The Area's Hillside Seepage Bogs Hillside seepage bogs are marsh-like wetland usually located on gentle slopes of the sides of valleys. They form when the Surficial Aquifer intercepts the sloping landscape allowing water to seep onto the sloped surface. The plant communities in the bogs are dominated by a great number and variety of herbaceous plants that prefer full sun. Among them are carnivorous plants. These unusual plants include the Trumpet and White-Topped pitcher plants as well as other varieties of pitcher plants. Inundation or saturation for extended periods of time is necessary for pitcher plants and most of the rest of the plant communities found in the bogs to thrive and to fend off invasion by undesirable species. Hillside seepage bogs are valued because they are among the most species-rich communities in the world. A reduction in water levels in the bogs below the root zone of associated plants will kill the plant communities that live in them and pose a threat to the continued existence of the bogs. Hillside seepage bogs were once abundant in pre- settlement Florida, but their expanse has been greatly reduced. They are now estimated to only occupy between one and five percent of their original range. On NTC/Knight Property, they have been spared to a significant degree. Numerous hillside seepage bogs continue to exist on the NTC/Knight Property primarily along the margin of Botheration Creek and its tributaries. The Area's Steepheads Steepheads are unique wetland systems. Found around the globe, they are usually regarded as a rarity. More than 50 percent of the steepheads that exist in the world are in a narrow latitudinal band that extends from Santa Rosa County in the west to Leon County in the east, a major section of the Florida Panhandle. Steepheads occur in deep sandy soils where water originating in the Surficial Aquifer carries away sand and cuts into sandy soils. The seepage emerges as a "headwater" to create a stream that conveys the water from the steephead into a river, or in some rare circumstances, into a karst lake. Over time, flow of the seepage waters results in deep, amphitheater- shaped ravines with steep valley side walls. Steepheads are important to the ecologies of the areas in which they occur. They provide habitat for a number of Florida endemic animals and plants believed to be relics of once-abundant species. Water that emerges from a steephead is perennial. Because the steep slopes of the steephead have not been disturbed over a long period of time, the water remains at a relatively constant temperature, no matter the season. Sampling of aquatic invertebrates at the Russ Pond and Tiller Mill Steepheads on the NTC/Knight Property found 41 and 33 distinct taxa, respectively, to inhabit the steepheads. Among them were a number of long-lived taxa. Their presence is consistent with the hallmark of a steephead: perennial flow of water at a relatively constant temperature. Most of the known steepheads flow into streams or rivers. Between six and ten within the Area, however, flow into Sand Hill Lakes. They have no direct connection to any surface drainage basin, thereby adding to their uniqueness. The level in the Surficial Aquifer has a direct impact on where and to what extent seepage flows from the sidewalls of a steephead. The Area's Sphagnum Bogs Sphagnum moss grows in many locations within the landscape and requires moisture. Where there is a large amount of sphagnum moss, it can form a unique community known as a sphagnum bog that is capable of supporting unique plant and animal populations. In the Area, these sphagnum bogs form along the valley sidewalls of steephead ravines and are fed by Surficial Aquifer seepage from the sidewall of the ravine. These sphagnum bogs support unique plant and animal communities, including a salamander discovered by Dr. Means that is new to science and so far only known to exist in sphagnum bogs in the Florida Panhandle. The Area's Sinkhole Lakes and their Littoral Seepage Slopes Sand Hill Lakes are nutrient poor, or "oligotrophic," receiving most of their nutrient inputs through exchange with the plant and animal communities on the adjacent littoral shelves during periods of high water levels. Fluctuating water levels in the Sand Hill Lakes allow a littoral zone with many different micro-habitats. Areas closest to the lakes are inundated regularly, but higher areas of the littoral zone are generally dry and inundated only every ten or 20 years -- just often enough to prevent encroachment of trees. In a few instances, portions of the littoral zones are inundated by seepage from the Surficial Aquifer. Above the normal low water of the Sand Hill Lakes, the littoral shelf occurs along a low gradient. As the littoral shelf transitions into the lake bottom and toward the deeper parts of the lake, there is an inflection point, where the gradient of the lake bottom becomes much steeper than the littoral shelf. If lake water levels fall below that natural inflection point, gully erosion will occur. The flow of water will be changed along the littoral shelf from seepage sheet flow over a wide expanse to water flowing down gullies in a concentrated stream. This change in flow will result in a loss of area needed by certain seepage dependent plants and animals as well as increased sedimentation from erosion. Big Blue Lake is unique because it boasts the largest known littoral zone seepage area of any Sand Hill Lake. The seepage zone along Big Blue Lake supports a number of rare plant species, including the Thread-Leaf Sundew, Smoothed Barked St. Johns Wort, and Crystal Lake Nailwort. The Area's Temporary Ponds Temporary ponds are small isolated water bodies that generally have no surface water inlet or outlet. Typically very shallow, they are sometimes wet and sometimes dry. Temporary ponds can range from basins that have continuous water for three to five years, to basins that have standing water for a month or two, every two to four years. These conditions limit their occupation by fish and, therefore, provide ideal conditions for amphibian reproduction which only occurs when water levels are maintained long enough to complete a reproductive cycle. In the Area, temporary ponds are a direct expression of the Surficial Aquifer and contain no known restrictive layer that might cause water to be "perched" above the Surficial Aquifer. Temporary ponds are critical to the viability of amphibian populations and support high amphibian biodiversity. A given pond can contain between five and eight species of salamander, and between 12 and 15 species of frogs. There has been a decline recently in the population of frogs and other amphibians that depend upon temporary ponds. The decline is due in part to ditching and other anthropogenic activities that have altered the hydrology of temporary ponds. Temporary ponds have a higher likelihood of being harmed by a drawdown than larger, connected wetlands systems. Lowered Surficial Aquifer water levels would lower water levels in temporary ponds and, thereby, threaten amphibian reproduction. Creeks/Streams in Forested Wetlands Streams are classified on the basis of the consistency of flowing water, including perennial (always flowing), intermittent (flowing part of the year), and ephemeral (flowing only occasionally during rain events). The type of stream flow is important because movement of water is essential to support aquatic systems in stream habitats. The NTC/Knight Property includes a number of stream systems, including Botheration Creek and Pine Log Creek. Botheration Creek is fed by groundwater discharge and originates, in large part, on the NTC/Knight Property. Botheration Creek flows from east to west until it intersects Pine Log Creek on the southwest part of the NTC/Knight Property. Botheration Creek provides Pine Log Creek with approximately 89 percent of Pine Log Creek's flow. From the confluence, Pine Log Creek flows south and west into the Pine Log State Forest and eventually joins the Choctawhatchee River. Botheration Creek contains high quality water and a diverse mix of aquatic invertebrates and fish. Sampling at a stage recorder located approximately two miles west of the eastern boundary of the NTC/Knight Property ("BCS-01") identified 46 taxa of macroinvertebrates, including six long- lived taxa, and mussels. The water level in Botheration Creek at BCS-01 was measured to be between 0.1 and 0.32 feet by four measurements taken from October 2010 to July 2011. Nonetheless, the presence of long-lived taxa and mussels indicates that, at BCS-01, Botheration Creek is a perennial stream. Carbon export from streams provides nutrients that feed the stream system. Headwater streams like Botheration Creek and its tributaries are essential to carbon export. For carbon export to occur, a stream must have out-of-bank flood events regularly to promote nutrient exchange with the flood plain. Bay County and its Water Supply Prior to 1961, the County obtained its public water supply from wellfields located near downtown Panama City. The wellfields drew from the Floridan Aquifer. An assessment of the pre-1961 groundwater pumping appears in a District Water Supply Assessment released in June 1998. In summary, it found that near Panama City, the potentiometric surface was substantially depressed by the pumping. Due to the threat of saltwater intrusion, the Deer Point Lake Reservoir (the "Reservoir") was constructed as an alternate water supply. A local paper mill, the city of Panama City, and Tyndall Air Force Base, all began to obtain public supply water from the Reservoir. Six years after the construction of the Reservoir, the Floridan Aquifer's water levels had rebounded to pre-pumping levels. See NTC/Knight Ex. 93 at 69. The authorization for the Reservoir began in the 1950's when the Florida Legislature passed a series of laws that granted Bay County authority to create a saltwater barrier dam in North Bay, an arm of the St. Andrews Bay saltwater estuary. The laws also allowed Panama City to develop and operate a surface freshwater reservoir to supply water for public use. The Deer Point Lake Dam (the "Dam") was built in 1961 from metal sheet piling installed across a portion of North Bay. The Dam created the Reservoir. The watershed of the Reservoir includes portions of Jackson, Calhoun, Washington, and Bay Counties and covers approximately 438 square miles. The Reservoir receives freshwater inflow from several tributaries, including Econfina Creek, Big Cedar Creek, Bear Creek/Little Bear Creek, and Bayou George Creek, totaling about 900 cubic feet per second ("cfs") or approximately 582 MGD. The volume of inflow would increase substantially, at least two-fold, during a 100-year storm event. The Dam is made of concrete and steel. Above it is a bridge and two-lane county road roughly 11.5 feet above sea level. The bridge is tied to the Dam by pylons. The top of the Dam is 4.5 feet above sea level, leaving a distance between the Dam and the bridge bottom of about seven feet. There is an additional structure above the Dam that contains gates, which swing open from the force of water on the Reservoir's side of the Dam. Capable of releasing approximately 550 MGD of freshwater into the saltwater bay, the gates keep the level of the Reservoir at about five feet above sea level. The height of the Dam and the gate structure leaves a gap between the bottom of the bridge deck and the top of the structure of "somewhere between 12 and 14 inches, a little better than a foot." Tr. 140. If storm surge from the Gulf of Mexico and St. Andrew's Bay were to top the Dam and the gate structure, the gap would allow saltwater to enter the Reservoir. The gates and the Dam structure are not designed to address storm surge. The Dam is approximately four feet thick and roughly 1,450 feet long. The 12-to-14 inch gap extends across the length of the Dam. With normal reservoir levels, the volume of water it contains is approximately 32,000-acre-feet or roughly 10.4 billion gallons. Bay County needs to drawdown the lake level for fish and wildlife purposes, the control of aquatic growth, and weed control. In winter, FWS prescribes a 45-day period of time to draw down the lake to expose the banks to kill vegetation. The last time the lake was drawn down by the County, the water level dropped approximately three feet, from five feet above sea level to two feet above sea level. This process took approximately six days and 16 hours, or approximately 53 hours/foot. Repair of the Dam and its Maintenance The Dam has been repaired three times. The last repair was following Hurricane Opal which hit the Florida Panhandle in the fall of 1995. During Hurricane Opal, "saltwater . . . entered . . . the [R]eservoir . . . [t]hat took 20-some days to flush out . . . ." Tr. 135. No evidence was presented regarding the Dam's vulnerability from the perspective of structural integrity during normal or emergency conditions. Other than the inference drawn from Mr. Lackemacher's testimony that Hurricane Opal damaged the Dam in 1995, no evidence was presented to suggest that the Dam's structure is vulnerable to damage caused by a storm surge, wave effect or other conditions caused by a storm of any magnitude. After the last of the three repairs, Bay County implemented a detailed maintenance program. Based upon the latest inspection reports, the Dam is in good condition and structurally sound. No work other than routine inspection and maintenance is currently planned. The 1991 Agreement and the WTP Bay County's current withdrawal of water from the Reservoir is based on a 1991 agreement between Bay County and the District (the "1991 Agreement"). See Joint Ex. Vol. II, Tab K. The 1991 Agreement allows Bay County after the year 2010 to withdraw 98 MGD (annual average) with a maximum daily withdrawal of 107 MGD. The 1991 Agreement, still in effect, authorizes Bay County to withdraw enough water from the Reservoir to meet its needs through 2040. Water for public supply is withdrawn from the Reservoir by a water utility pump station (the "Pump Station") located a short distance from the Dam in Williams Bayou. The water is piped to the water utility's treatment plant (the "Water Treatment Plant") five miles away. The Water Treatment Plant treats 60 MGD. Following treatment, the water is distributed to Bay County's wholesale and retail customers. The Reservoir water available to Bay County utilities is more than adequate to fulfill the water consumption demands of Bay County's system through a 20-year permit horizon. The transmission line between the Pump Station and the Water Treatment Plant has fittings that were designed to allow transmission of groundwater withdrawn from groundwater wells to be located along the transmission line to the Water Treatment Plant to provide a backup supply for the Reservoir. Bay County's Current Use of Potable Water The amount of water consumed by Bay County utility customers has declined over the last five years. Bay County's current use of water, based upon the average of the 13 months prior to the hearing, was 24.5 MGD, an amount that is only 25 percent of the water allocation authorized by the 1991 Agreement. There are approximately 560,000 linear feet of main transmission lines in Bay County with small service lines accounting for another several hundred thousand linear feet. Bay County furnishes water directly to approximately 6,000 retail customers in areas known as North Bay, Bay County, and the former Cedar Grove area, which is now part of Bay County. Wholesale customers include Panama City Beach, Panama City, Mexico Beach, Callaway, Parker, Springfield, and parts of Lynn Haven. The County also furnishes potable water to Tyndall Air Force Base. Lynn Haven does have some water supply wells; however, Bay County still supplements this water supply by approximately 30 percent. No other cities serviced by Bay County produce their own water. Bay County has a population of approximately 165,000- 170,000 permanent residents, which includes residents of the cities. The Bay County area experiences seasonal tourism. From spring break to July 4th, the population can grow to more than 300,000. The users of Bay County's drinking water supplies include hospitals, Tyndall Air Force Base, and the Naval Support Activity of Panama City ("NSA"). The County has 178 doctor's offices, 56 dental offices, 29 schools, 21 fire departments, 12 walk-in-clinics, six nursing and rehabilitation homes, six major employers, three colleges and universities, and two major hospitals, all which are provided drinking water by Bay County. Panama City Beach is the community which has the highest water use. Panama City Beach's average daily use is approximately 12 MGD. The peak day of usage for all of Bay County's customers over the 13 months prior to the hearing was 40 MGD. Bay County sells water to community water utility systems referred to as a "consecutive system." They include Panama City Beach, Panama City, and Mexico Beach. Bay County's request for 30 MGD contemplates provision of water for all essential and non-essential water uses occurring within the consecutive system. Bay County and the consecutive systems are subject to the District's regulations regarding emergency water use restrictions which typically restrict the non-essential use of water during water shortage emergencies. Hurricanes, Train Wrecks, and Post-9/11 America At the District's recommendation, Bay County has been considering a backup potable water source since the mid-1980's. Bay County's main concern is that it has inadequate alternatives to the Reservoir should it be contaminated. Contamination to date has been minimal. In the period of time after the 1961 creation of the Reservoir to the present, the Dam and the Reservoir have suffered no major damage or impacts from a tropical storm. No tropical storm since 1961 has disrupted Bay County's ability to provide potable water. Even Hurricane Opal in 1995 did not disrupt the water supply. Recent hurricane activity in the Gulf of Mexico, however, has aroused the County's fears. Should a storm of sufficient magnitude make landfall in proximity to the Dam, there is potential for saltwater contamination of the Reservoir from storm surge or loss of impounded freshwater due to damage to the Dam. Mr. Lackemacher, assistant director of the Bay County Utility Department and manager of the water and wastewater divisions of the department, has experience with other hurricanes in Palm Beach, Florida, and Hurricane Hugo in Myrtle Beach, South Carolina, during which water utilities suffered disruption of their distribution systems. The experience bolsters his concern about the damage a storm could cause Bay County's source of public water supply. Bay County's intake structure at Williams Bayou is approximately one mile away from the Dam. The location of the Pump Station puts it at risk for damage from a strong storm or hurricane. There is a rail line near the Reservoir. It runs along Highway 231 and over creeks that flow into the Reservoir, including the Econfina Creek. The rail line is known as "Bayline." Bayline's most frequent customers are the paper mill and the Port of Panama City. Not a passenger line, Bayline is used for the transport of industrial and chemical supplies. In 1978, a train derailment occurred on tracks adjacent to creeks that feed the Reservoir. The derailment led to a chlorine gas leak into the atmosphere. There was no proof offered at hearing of contamination of the Reservoir. There has never been a spill that resulted in a hazardous chemical or pollutant being introduced into the Reservoir. Bay County has not imposed restrictions on the type of vehicles that are allowed to use, or the material that may pass over, the county road on the bridge above the Dam. Nonetheless, in addition to saltwater contamination, Bay County also bases the need for an alternative water source on the possibility of a discharge into the Reservoir of toxic substances from a future train derailment. Bay County is also concerned about contamination of the Reservoir from a terrorist attack. In short, Bay County is concerned about "anything that could affect the water quality and water in Deer Point Lake." Tr. 184. The concerns led Bay County to file its application for the Wellfield on lands currently owned by the St. Joe Company. Consisting of ten wells spaced over an area of approximately ten square miles, the Wellfield would have a capacity of 30 MGD. Bay County's application was preceded by the development of the District's Region III Regional Water Supply Plan and efforts to acquire funding. Funding for the Wellfield and the Region III Regional Water Supply Plan Shortly after the commencement of the planning for the Wellfield, the District, in May 2007, authorized the use of funds from the State's Water Protection and Sustainability Trust Fund ("WPSTF"). The WPSTF is intended for development of alternative water supplies. In cooperation with the District, Bay County began drilling a test well followed by analyses to evaluate the water for potable suitability. In October of the same year, the District passed a resolution to request the Department of Environmental Protection to release $500,000 from the WPSTF to the District for local utilities in Bay and Escambia Counties for "Water Resource Development." NTC/Knight Ex. 195, p. 2. The amount was to be used "to provide funding for implementation of alternative water supply development and water resource developments projects pursuant to sections 403.890 and 373.1961, F.S." Id., p. 1. In February 2008, the District began a process to develop a regional water supply plan for Bay County. If the Wellfield were designated in the applicable regional water supply plan as "nontraditional for a water supply planning region," then it would meet the definition of "alternative water supplies" found in section 373.019(1), Florida Statutes. "In evaluating an application for consumptive use of water which proposes the use of an alternative water supply project as described in the regional water supply plan," the District is mandated "to presume that the alternative water supply is consistent with the public interest " § 373.223(5). Whether the Wellfield is to be presumed to be in the public interest depends on whether the application proposes the use of an alternative water supply project as described in the District's Region III Water (Bay County) Water Supply Plan adopted in 2008. The 2008 RWSP Pursuant to the process commenced in February, the District in August 2008 produced the Region III (Bay County) Regional Water Supply Plan (the "2008 RWSP"). In a section entitled "Identification of Alternative Water Supply Development Projects," the 2008 RWSP provides the following: "All of the water supply development projects identified in Table 4 are interrelated and considered alternative, nontraditional water supply development projects." NTC/Knight Ex. 187 at 14. Table 4 of the 2008 RWSP does not specifically identify the Wellfield. It identifies three projects in general terms. The first of the three (the only one that arguably covers the Wellfield) shows "Bay County Utilities" as the sole entity under the heading "Responsible Entities." Id. at 13. The project is: "Inland Ground Water Source Development and Water Supply Source Protection." Id. Under the heading, "Purpose/Objective," the Table states for the first project, "Develop inland alternative water supply sources to meet future demands and abate risks of salt water intrusion and extreme drought." Id. The Table shows "Estimated Quantity (MGD)" to be "10.0." Id. (In July 2008, the District's executive director informed Bay County that the Wellfield could produce 10 MGD.) The "Time Frame" is listed as 2008-12, and the "Estimated Funding" is "$5,200,000 WPSPTF" and "$7,800,000 Local, NWFWMD." Id. While not specifically identified in the 2008 RWSP, Table 4's project description supports a finding that the Wellfield is, in fact, one of the inland alternative water supply sources. The 2008 RWSP, therefore, designates the Wellfield as a "nontraditional" water supply source for Region III.4/ (The Wellfield also, therefore, meets the definition of "[a]lternative water supplies" in section 373.019(1). The demonstration of a prima facie case by Bay County and the District, however, make the applicability of the presumption a moot point. See Conclusions of Law, below.) Water Supply Assessments and Re-evaluations Development of a regional water supply plan by the governing board of each water management district is mandated "where [the governing board] determines that existing and reasonably anticipated sources of water are not adequate to supply water for all existing and future reasonable-beneficial uses and to sustain the water resources and related natural systems for the planning period." § 373.709(1), Fla. Stat. (the "Regional Water Supply Planning Statute"). The District determined in its 1998 District Water Supply Assessment ("WSA") for Region III (Bay County) that the existing and reasonably anticipated water sources are adequate to meet the requirements of existing legal users and reasonably anticipated future water supply needs of the region through the year 2020, while sustaining the water resource and related natural systems. See NTC/Knight 93 at 79. In 2003, Ron Bartel, the director of the District's Resource Management Division, issued a memorandum to the Governing Board (the "2003 Re-evaluation Memorandum"), the subject of which is "Regional Water Supply Planning Re- evaluation." NTC/Knight 95 (page stamped 42). The 2003 Re-evaluation Memorandum sets out the following with regard to when a "water supply plan" is needed: The primary test we have used for making a determination that a water supply plan was "not needed" for each region is that projected consumptive use demands for water from major water users do not exceed water available from traditional sources without having adverse impacts on water resources and related natural systems. Similarly, regional water supply planning is initiated "where it is determined that sources of water are not adequate for the planning period (20) years to supply water for all existing and reasonable-beneficial uses and to sustain the water resources and related natural systems." Id. With regard to the need for a Water Supply Plan for Bay County the 2003 Re-evaluation Memorandum states: [I]n Bay County (Region III), sufficient quantities have been allocated for surface water withdrawal from Deer Point Lake Reservoir through the District's consumptive use permitting program extending through the year 2040. In this area, the District is also scheduled to complete a minimum flow and level determination for the lake by the year 2006. This determination will be useful for deciding if additional water supply planning is needed before the permit expires in 2040. Id. (page stamped 43). The 2008 RWSP's designation of the Wellfield is justified in the minutes of the Governing Board meeting at which the 2008 RWSP's approval took place: While the reservoir has largely replaced the use of coastal public supply wells historically impacted by saltwater intrusion, there remain challenges within the region that make development and implementation of a Regional Water Supply Plan (RWSP) appropriate. Development of alternative water supplies would diversify public supply sources and help drought-proof the region through establishment of facility interconnections. Development of alternative supplies would also minimize vulnerability associated with salt water potentially flowing into the reservoir during major hurricane events. Id., p. 3 of 4. The adoption of the 2008 RWSP was followed in December 2008 by the District's 2008 Water Supply Assessment Update. The update is consistent with the earlier determinations of the adequacy of the Reservoir as a water supply source for the foreseeable future (in the case of the update, through 2030). The update also voices the concern about water quality impacts from storm surge. The update concludes with the following: In Region III, the existing and reasonably anticipated surface water resources are adequate to meet the requirements of existing and reasonably anticipated future average demands and demands for a 1-in-10 year drought through 2030, while sustaining water resources and related natural systems. However, the major concern for potential water quality impacts is that resulting from hurricane storm surge. A Regional Water Supply Plan (NWFWMD 2008) has recently been prepared for Region III to address concerns associated with existing surface water systems. NTC/Knight Ex. 101, p. 3-41. The Parties Washington County is a political subdivision of the State of Florida. Washington County is located directly north of Bay County and the Wellfield and within one mile of some of the proposed wells. Washington County includes thousands of wetlands and open water systems. Because of the hydro-geologic system in the area of the Wellfield, if there are wetland, Surficial Aquifer, and surface water impacts from the withdrawal under the Permit, it is likely that impacts will occur in Washington County. Washington County has a substantial interest in protection, preservation, and conservation of its natural resources, including lakes, springs, and wetlands, and the flora and fauna that depend on these water resources, especially endangered flora and fauna. Washington County has a substantial interest in the protection of all water resources in Washington County because of the close relationship between surface waters, groundwater, and the potable water supply used by Washington County residents. NTC/Knight is the owner of approximately 55,000 acres of land located in northern Bay County and southern Washington County. The NTC/Knight Property includes thousands of acres of wetlands and open waters, including Sand Hill Lakes, steepheads, hillside seepage bogs, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and forested wetlands. A large portion of the NTC/Knight Property is directly adjacent to the Wellfield and within the HGL Model projected drawdown contour. Based on the projected amount of drawdown from pumping at the proposed average rate of 5 MGD, the 0.5 projected drawdown contour predicted by the HGL Modeling Report (see Finding of Fact 121, below) extends over thousands of acres of the property. NTC/Knight has a substantial interest in the protection of the surface and groundwater directly on, under, and adjacent to its property. The water supports the numerous ecosystems of extraordinary value located on the property. James Murfee and Lee Lapensohn are individuals, who reside in Bay County on property fronting on and beneath Tank Pond approximately five miles from the Wellfield. Petitioners Murfee and Lapensohn have a well which extends into the Intermediate Aquifer. The Murfee and Lapensohn properties are within the HGL Model projected drawdown contour. Petitioners Murfee and Lapensohn have a substantial interest in the protection of their drinking water supply well and the surface waters directly on and adjacent to their properties. Bay County, the applicant, is a political subdivision of the State of Florida. The District is a water management district created by section 373.069(1). It has the responsibility to conserve, protect, manage, and control the water resources within its geographic boundaries. See § 373.069(2)(a), Fla. Stat. Section 120.569(2)(p), Florida Statutes Section 120.569(2)(p), in pertinent part, provides: For any proceeding arising under chapter 373, chapter 378, or chapter 403, if a nonapplicant petitions as a third party to challenge an agency’s issuance of a license, permit, or conceptual approval, the order of presentation in the proceeding is for the permit applicant to present a prima facie case demonstrating entitlement to the license, permit, or conceptual approval, followed by the agency. This demonstration may be made by entering into evidence the application and relevant material submitted to the agency in support of the application, and the agency’s staff report or notice of intent to approve the permit, license, or conceptual approval. Subsequent to the presentation of the applicant’s prima facie case and any direct evidence submitted by the agency, the petitioner initiating the action challenging the issuance of the license, permit, or conceptual approval has the burden of ultimate persuasion and has the burden of going forward to prove the case in opposition to the license, permit, or conceptual approval through the presentation of competent and substantial evidence. The permit applicant and agency may on rebuttal present any evidence relevant to demonstrating that the application meets the conditions for issuance. Paragraph (p) was added to section 120.569(2) in the 2011 Session of the Florida Legislature. Accordingly, the final hearing commenced with the Bay County and the District's presentation of its prima facie case by submitting the application, supporting documentation, and the District's approval of the application. Respondents also presented the testimony of four witnesses in the hearing's first phase. Phase I of the Final Hearing: Bay County's Application, Supporting Documents, the District's Approval and Supporting Testimony The Application File At the final hearing, Bay County and the District offered the "application file," marked as Joint Exhibit Binder Volumes I-IV (the "Application File") in the hearing's first phase. It was admitted into evidence. A document entitled "Alternate Water Supply Report - Bay County Water Division" dated May 20, 2008 (the "Hatch Mott MacDonald Report") is contained in the Application File. See Joint Ex. Vol. I, Tab B. The Hatch Mott MacDonald Report is a preliminary evaluation of a wellfield with 22 wells, an "initial phase . . . [of] five (5) wells producing 5 MGD and the final phase . . . [of] 17 wells, producing 25 MGD." Id. at 1. The evaluation includes the gathering of information, a recommendation for the best method of treatment, an analysis of whether individual well sites or a centralized site would be superior, a hydraulic model and analysis, and the potential construction and operation costs. The report concludes in its Executive Summary: HMM's preliminary results, based upon water analysis of Well No. 1, indicate that only disinfection will be required for potable water treatment. Additionally, the hydraulic analysis indicated that the wells are capable of providing the initial 5 MGD and future 25 MGD to the proposed connection point along Highway 388 without re-pumping. Adequate storage for fire protection should be considered at current and future service areas. The use of chlorine gas at each well site during the initial phase had the lowest present worth of $16,770,270; that is, the smallest amount of funds needed today to build, operate, and maintain the system. The use of chlorine gas at each well in the final phase had a present worth of $41,245,118, only slightly more than the present worth of $40,834,245 for on-site Id. generation of disinfectant at three (3) central facilities. The Application File contains a response to a District request for additional information (the "2009 RAI Response") submitted by the Bay County Services Utility Director and received by the District in September 2009. See Joint Ex. Vol. II, Tab K. The 2009 RAI Response contains the 1991 Agreement and numerous other documents. Among them is a report prepared by HydroGeoLogic, Inc. ("HGL") entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" dated September 2009 (the "2009 HGL Modeling Report"). The report predicts impacts that would be created to the surrounding aquifers as a result of the Wellfield pumping, but recommends that additional data be obtained. The Application File contains the District's Notice dated March 25, 2010. See Joint Ex. Vol. III, Tab B. Attached to the Notice is a draft of the Permit and a staff report from the District recommending approval with conditions. Condition 11 of the Permit's standard conditions obligates Bay County to mitigate any significant adverse impacts caused by withdrawals and reserves the right to the District to curtail permitted withdrawal rates "if the withdrawal causes significant adverse impact on the resource and legal uses of water, or adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. III, Tab B, p. 3 of 17. Attachment A to the Permit requires conditions in addition to the standard conditions contained in the body of the Permit. Paragraph 12 of Attachment A, for example, requires that Bay County implement and maintain a water and conservation efficiency program with a number of goals. Attachment B to the Permit requires a monitoring and evaluation program and wetland monitoring of adjacent properties to determine if the pumping causes adverse impacts to wetland areas, including habitat and species utilization. The Application File contains a revised modeling report also entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" (the "2011 Revised HGL Modeling Report" or the "HGL Model Report"). See Joint Ex. Vol. III, Tab P. The 2011 Revised HGL Modeling Report predicts impacts of the pumping of the Wellfield on the Upper Floridan Aquifer and the Surficial Aquifer. The HGL Model is based on an adaptation of an original model first developed by the U.S. Geological Survey (USGS) and then further adapted by HGL. The adapted model is known as MODFLOW-SURFACT. The MODFLOW-SURFACT Model has been used in excess of 600 applications and is used worldwide. The HGL Model predicted impact from pumping when wellfield pumping achieves a "steady state." Steady state impact is achieved after 10-12 years of constant pumping. The impact and the area of impact is depicted on Figure 5.1b(1) of the 2011 Revised HGL Modeling Report. The predicted drawdown of the Surficial Aquifer is predicted to be six inches (0.5 ft) within the areas indicated. The Application File shows that the permit was revised twice. Ultimately, a Second Revised Notice of Proposed Agency Action dated July 22, 2011, was issued by the District. Attached to the Second Revised NOPAA is the District's Permit. See Joint Ex. Vol. IV, Tab U. A revised Staff Report from the District dated July 18, 2011, is also included in Volume IV of the joint exhibits. See id., Tab Q. The Permit as supported by the staff report allows an average daily withdrawal of 5 MGD, a maximum daily withdrawal of 30 MGD for no more than 60 days per year (with a maximum of 52 consecutive days), and a maximum monthly amount of 775 million gallons. See Joint Ex. Vol. IV, Tab U. The Permit also includes the LTEMP jointly prepared by the Applicant and the District. See id., Attachment B. The Permit requires Bay County to "mitigate any significant adverse impact caused by withdrawals . . . on the resource and legal water withdrawals and uses, and on adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. IV, Tab R, p. 3 of 11. If the District receives notice of an impact from the existing legal user, it contacts the utility. "Within 72 hours [the utility has] a well contractor out there and they have determined what the problem is." Tr. 615. There are no time requirements for the resolution of the impact or any other resolution procedures in the Permit. Definitions of Emergency and Maintenance Amounts The Permit does not include a definition of when the Reservoir may be considered to be unavailable as a public water supply. That determination is left to Bay County. The Permit does not set a withdrawal limit lower than the limits detailed above for maintenance of the Wellfield. There is one set of withdrawal limits. They apply irrespective of the purpose of the withdrawals, that is, whether for backup in an emergency, maintenance, or some other purpose that falls under Public Supply or Industrial Use. Conditions and Monitoring Requirements Bay County is required to mitigate any significant adverse impacts on resources and legal water withdrawals and uses caused by the County's withdrawal from the Wellfield. In addition, the District reserves the right to curtail permitted withdrawal rates if Bay County's withdrawal causes adverse impacts on local resources and legal uses of water in existence at the time of the permit application. In the event of a declared water shortage, the Permit requires Bay County to make water withdrawal reductions ordered by the District. In addition, the District may alter, modify, or deactivate all or parts of the Permit. Attachment A to the Permit, states: The Permittee shall not exceed total, combined groundwater and surface water (authorized in Individual Water Use Permit No. 19910142) withdrawals of an average daily withdrawal of 98,000,000 gallons, a maximum daily withdrawal of 107,000,000 gallons and a maximum monthly withdrawal of 2,487,750,000 gallons. Joint Ex. Vol. IV, Tab U, p. 4 of 11. The inclusion of "surface water" in the condition covers withdrawals from the Reservoir. The combination of actual withdrawals from the Wellfield and actual withdrawals from the Reservoir, therefore, means that Bay County may not exceed the limitations of the withdrawals authorized by the 1991 Agreement. Attachment A to the Permit further explains how Bay County must mitigate harm caused by groundwater withdrawals. The Permittee, within seven days of determination or notification by the District that the authorized groundwater withdrawal is causing harm to the resources, shall cease or reduce, as directed by the District, its pumping activity. The Permittee shall retain the services of a qualified, licensed professional to investigate allegations of interference with an existing, legal groundwater use. The Permittee shall ensure their chosen contractor investigates the alleged interference within 72 hours of the allegation being made. If it is determined that the use of a well has been impaired as a result of the Permittee's operation, the Permittee shall undertake the required mitigation or some other arrangement mutually agreeable to the Permittee and the affected party. The Permittee shall be responsible for the payment of services rendered by the licensed water well contractor and/or professional geologist. The Permittee, within 30 days of any allegation of interference, shall submit a report to the District including the date of the allegation, the name and contact information of the party making the allegation, the result of the investigation made and any mitigation action undertaken. Joint Ex. Vol. IV, Tab U, Attachment A, p. 4 of 11. Bay County is also required, within two years from the Permit's issuance, to submit to the District for review and approval a contingency plan to mitigate potential impacts. The County must wait one full year prior to commencing withdrawal of groundwater for production purposes. During the one-year period, the County must complete groundwater, surface water, and wetland monitoring. The requirements of the mandatory monitoring are found in Attachment B of the Permit, LTEMP. See Joint Ex. Vol. IV, Tab U, Attachment B. The LTEMP "is designed to track trends in ecological and hydrological conditions caused by naturally occurring fluctuations in rainfall, which may affect ground and surface water hydrologic conditions; and to identify potential effects caused by wellfield pumping." Joint Ex. Vol. IV, Tab U, Attachment B at 1. If a substantive deviation occurs from predictions made by the HGL Modeling, or if any other hydrologic or ecologic changes due to the withdrawals are observed at monitoring sites, the District is required to review and, in consultation with Bay County, appropriately revise the LTEMP as necessary with the aim that the monitoring will assure that the conditions for issuance of the Permit are being met. Testimony in Support of the Application In addition to the documentary evidence offered in the first phase of the proceeding, Bay County and the District presented the testimony of several witnesses. These witnesses testified as to background and the 2008 RWSP, the vulnerability of the Reservoir to saltwater contamination from storm surge, and the basis for the District's decision. Vulnerability to Storm Surge There is a one percent chance every year of a 100- year storm event. Flood Insurance Rates Maps ("FIRMS") show that the 100-year water level (the level of storm surge in a 100-year storm event) at the Dam will reach 11 feet NAVD, two feet above the top of the gate structure above the Dam. The Federal Emergency Management Agency ("FEMA") and the National Weather Service ("NWS") have developed the Sea, Lake, and Overland Surge from Hurricanes ("SLOSH") model, which estimates storm surge depths resulting from historical, hypothetical, or predicted hurricanes. A Florida Department of Emergency Management's SLOSH model of the Panama City area shows maximum surge levels for Storm Categories 1, 2, 3, 4, and 5, in NAVD feet as 3.3, 5.8, 10.8, 14.1, and 18.1, respectively. The SLOSH model, in all likelihood, is a low estimation. It is reasonable to expect surge levels in a Category 3 hurricane that passes directly over the Dam, for example, to be higher than 10.8 feet NAVD predicted by the SLOSH model at the Dam. According to the National Oceanic and Atmospheric Administration's ("NOAA") database, 43 tropical storms and hurricanes have passed within 200 miles of the Reservoir between 1970 and 2010 and 20 have come within 100 miles. None have made landfall closer than 40 miles away from the Dam. Of the 20 storms passing within 100 miles of the Reservoir, four have reached Category 3 strength or higher: Eloise, Elena, Opal, and Dennis. In 2004, Hurricane Ivan made landfall over 100 miles to the west of the Dam and raised water levels near the Dam to nearly five feet NAVD. The following year, Hurricane Dennis made landfall 76 miles to the west of the Dam. Dennis produced a surge level of nearly four feet NAVD near the Dam. "Hurricane Eloise (1975) made landfall 40 miles west of Panama City and produced water levels 15 ft above normal at Panama City ([citation omitted]). However, the storm passed through the area quickly and does not appear to have significantly affected the dam." Bay County Ex. 1, p. 3 of 9. Hurricane Opal made landfall 86 miles west of Panama City Beach and produced water levels of about 8.3 feet NAVD near the Dam. The storm surge did not overtop the gate structure above the Dam, but the gates were jammed by debris. "[C]hloride levels rose above 50 ppm at the intake pumps and two to three times above normal background levels of 8 to 10 ppm 'almost one mile up-reservoir.'" Id. The levels of chloride were "still well within drinking water limits," tr. 434, of 250 parts-per- million (ppm). Hurricane Katrina made landfall in 2005 more than 200 miles west of the Reservoir with storm surges higher than 20 feet. Katrina produced surge levels of five feet above normal tide levels in Bay County. The rate and amount of saltwater that would enter the Reservoir depends on the height of the storm surge above the Dam. The 100-year surge levels could remain above the top of the Dam for three or more hours. Such an event would introduce approximately 56,200,000 cubic feet or 1,290 acre-feet of saltwater into the Reservoir, even if the Dam were to remain intact (undamaged) and the tide gates remain closed. The salinity levels bay-side of the dam are generally 23,000 to 33,000 ppm. It is reasonable to expect that in the event of a 100-year storm event, much of the storm surge would come directly from the Gulf of Mexico, which has higher salinity levels. With the Dam intact, the introduction of 1,290 acre- feet of saltwater at 33,000 ppm would raise the average chloride concentration in the Reservoir to at least 800 ppm, more than three times the maximum drinking water chloride level of 250 ppm. Assuming the Dam remained intact during a 100-year storm event, freshwater added over time to the lake from the streams and aquifer will dilute the elevated lake chloride level and restore the lake water to a level fit for human consumption. The USGS has measured stream flow at Deer Point Lake and estimated the lake receives an average of 600 million gallons of freshwater per day or 900 cfs. Post-Opal rates were estimated at 1,500 cfs by the District. Given the estimated volume of saltwater introduced to the lake, at an inflow rate equal to the estimated post- hurricane freshwater inflow rate, Bay County's expert, Dr. Miller, estimated it would take at least two weeks to reduce salinity in the lake to drinkable levels. The inflow rate, however, is not certain. Dr. Miller estimated it is reasonable to expect that it could take anywhere from two weeks to two months for the lake to recover from the saltwater intrusion depending on the variation in the inflow rate. Nonetheless, Dr. Miller assumed that the saltwater from storm surge entering the Reservoir would mix in a uniform matter. There would be "quite a bit of mixing in a storm," tr. 485, of saltwater topping the Dam and freshwater in the Dam. But there would also be stratification due to the sinking of denser saltwater and the rising in the water column of freshwater. The above estimations assume the bridge and Dam remain intact during a major storm. The Dam and tide gates act as a solid barrier, protecting the lake from saltwater in the bay. If rainfall rises in the lake prior to a surge, the tide gates would open to release water, becoming vulnerable to damage or jamming by debris as occurred during Hurricane Opal. In the event of storm surge bringing saltwater into the Reservoir, the opening of the tide gates will assist the Reservoir in reaching chloride levels below 250 ppm provided the tide gates operate properly. Dr. Janicki, an NTC/Knight expert, used the Environmental Fluid Dynamics Code hydrodynamic model ("EFDC Model") to simulate the effects of control structures and water withdrawals on the Reservoir. Taking into consideration the factors Dr. Janicki considered relevant, he predicted that chloride levels, in the event of storm surge from a Category 3 hurricane overtopping the Dam, would only exceed 250 ppm, the drinking water standard, for approximately 3.4 days. Dr. Janicki's prediction, however, was flawed. He added too little saltwater to the lake in the event of contamination from storm surge. He assumed that saltwater would be flushed too soon from the Reservoir following contamination. He did not account for the effects of waves in his model. His model was not in accord with data for Hurricane Opal and the chloride levels near the Dam taken by Bay County after Opal. If the bridge and Dam were severely damaged, more saltwater could enter the lake. With severe damage to the Dam, the Reservoir would be exposed to normal tides. Restoration would not begin until the Dam and bridge had been fully repaired. If an event were catastrophic, the Reservoir could be offline for a lengthy period of time. The Basis for the District's Decision Bay County's reliance on the Reservoir for water for the majority of the population led the District in the mid-1980s to encourage the County to obtain a backup supply. After the District turned down several requests for withdrawals of up to 30 MGD for every day of the year, the District ultimately approved what is reflected in the Permit. The justification for the permitted withdrawal is as a backup supply in the event the Reservoir becomes unavailable and for maintenance of the system and recoupment of its cost. With regard to maintenance, the District attempted to obtain information from Bay County as to appropriate withdrawal limitations. The attempts were abandoned. Despite repeated requests by the District, Bay County did not provide the amount of water needed to be withdrawn for maintenance since it did not have "infrastructure specifics," tr. 552, needed to provide the District with a numeric limit. In contrast to the amount needed for maintenance, the District found Bay County to have demonstrated that it needs 30 MGD when the Reservoir is offline and that it is reasonable for the County to need 30 MGD up to 60 days per year. The District determined that the Bay County's application met the requirements for the issuance of a consumptive use permit found in section 373.221(1)(a)-(c). In determining whether approval of the application is in the public interest, the District did not presume that it is in the public interest on the basis of the designation in the 2008 RWSP of an inland groundwater source as an alternative water supply. The District determined that it is in the public's interest for Bay County to have a reliable and safe water supply source as a backup to the Reservoir irrespective of the statutory presumption. Nonetheless, the District maintains in this proceeding that the presumption applies. The District also applied the 18 criteria test for finding a reasonable-beneficial use found in Florida Administrative Code Rule 62-40.410(a)-(r) and determined that the application should be approved. Petitioners' Case in Opposition Washington County (Petitioner in Case No. 10-2983), NTC/Knight (Petitioner in Case No. 10-2984), and Messrs. Murfee and Lapensohn (Petitioners in Case No. 10-10100) filed individual petitions for formal administrative hearing. Although not identical, the petitions share the similarity that, in essence, each alleges that Bay County failed to establish that the proposed use of water meets the statutory and rule criteria for obtaining a permit for the consumptive use of water. For example, among the many issues listed under the heading "Disputed Issues of Material Fact and Law" in Washington County's Petition for Formal Administrative Hearing is "[w]hether Bay County has provided reasonable assurance that its proposed use of water is a reasonable-beneficial use as defined in section 373.019, Florida Statutes." See p. 5 of the Washington County petition. In like fashion, the Washington County petition and the other two petitions allege that the issues are whether Bay County provided reasonable assurance that it meets the other statutory criteria in section 373.223, and the applicable rule criteria that must be met by an applicant in order for the District to issue a permit for the consumptive use of water. The Petitioners' cases focused on five topics: 1) the limitations of the HGL Model; 2) the likelihood of impacts to wetlands and the failure of the monitoring plan to provide reasonable assurance that the District's monitoring under the plan will succeed in detecting harm to wetlands caused by the withdrawals; 3) the reasonable-beneficial nature of the proposed use of the permit, including the vulnerability of the Reservoir; 4) interference with presently existing legal users; and 5) the feasibility of alternative sources. Bay County and the District offered evidence on rebuttal to meet the Petitioners' cases. Surrebuttal was conducted by Petitioners. Modeling Groundwater models "represent what is happening in very complex physical systems." Tr. 1495. Typically, the data used by models is not sufficient to obtain a completely accurate representation. The models depend on specific data points such as information from boreholes or water level measurements that do not reveal everything that is occurring in the complex system and, therefore, are not enough to support completely accurate model predictions. As explained by Dr. Guvanasen, Bay County and the District's expert, in order to reach a representation of the entire system when the data available from boreholes and measurements is insufficient, which is typically the case, the modeler must "extrapolate a lot of information and use other knowledge of other events." Id. The "knowledge of other events" that the HGL Model used included Dr. Scott's knowledge of the karst environment in the Panhandle of Florida, the mapping of Bay and Washington County geology by the Florida Geological Society, and Dr. Upchurch's knowledge of karst topography. The HGL results of the available data and the extrapolations were placed into a mathematical model (the HGL Model) that considered the withdrawals at issue to determine the response of the system to the additional stress of the withdrawals. Mathematical models like the HGL Model lead to "non- unique solutions" in which "no model . . . is exactly 100 percent correct . . . ." Tr. 1635. Modeling results, therefore, are subject to changes as additional data is collected that demand a better representation than the model provided prior to the data's collection and analysis. HGL Modeling for this case provides examples of non- unique solutions. HGL "built a model twice . . . and got two different sets of answers." Tr. 1633. Besides the recommendation that more data be obtained after the first HGL Model results, the model was not satisfactorily calibrated and the model was recalibrated for the Revised HGL Modeling results. Mr. Davis, NTC/Knight's expert, conducted additional modeling work (the "Davis Modeling"). Using the HGL Model and additional data concerning the NTC/Knight Property, Mr. Davis found drawdowns would occur over a similar but greater area than shown in the 2011 Revised HGL Modeling Report. (Compare NTC/Knight Ex. 31 at 2 to Joint Ex. Vol. III, Tab P, Figure 51b(1).) The Davis Modeling drawdowns, moreover, ranged up to 0.8 feet, 60 percent more than the 0.5 feet determined by the second HGL Modeling results. In the area of Big Blue Lake, for example, the drawdown contours produced by the Davis Model were either 0.6 feet or 0.7 feet, 20 to 40 percent more than the 0.5 feet produced by the second HGL Modeling results. See NTC/Knight Ex. 31 at 2. Asked to rank the modeling results between the first HGL Model run, the second HGL Model run, and his own results, Mr. Davis was unable to say which was better because of the sparseness of the data. Mr. Davis opined that he could conduct another "dozen more model runs," but without additional data he would be "hard pressed" to be able to say which run was more accurate. Tr. 1633. In Mr. Davis' opinion there remain significant uncertainties that cannot be resolved without more data. Inadequate data "precludes . . . reasonable assurance as to exactly where the impacts will travel and exactly what the magnitude of those impacts will be . . . ." Tr. 1637. Ecological Impacts Bruce A. Pruitt, Ph.D., was accepted as an expert in hydrology, soil science, fluvial geomorphology, and wetland sciences. Dr. Pruitt mapped the soil types on the NTC/Knight Property using the Natural Resource Conservation Service ("NRCS") Web Soil Survey and tested soil types by hand-auguring in wetland areas. He characterized the various soil-types on the property by drainage class (relative wetness of the soil under natural conditions) and hydraulic conductivity (permeability). Dr. Pruitt ranked the vulnerability of wetlands within the zone of drawdown predicted by the HGL Model as "very high," "high," or "moderate." The categories were based on the presence of threatened and endangered species, Florida Natural Area Inventor ("FNAI") habitat designation, and the hydrology of the wetland. He assumed that if the water level in the Surficial Aquifer were to be drawn down by 0.3 feet or 0.4 feet then the water level in the seepage bogs at Botheration Creek would be drawn down by the same amount. Wetlands with a vulnerability classification of "very high" will suffer an adverse impact at a drawdown level of 0.2 feet; those at "high" at 0.3 feet and those at "moderate" at 0.5 feet in times of drought. Dr. Pruitt calculated wetland acreage by type using the Florida Cover Classification System. He assigned vulnerability rating for the wetlands within the Surficial Aquifer drawdown contours generated by the HGL Model. Based on Dr. Pruitt's calculations, a total of approximately 4,200 acres of wetlands are likely to be harmed by the predicted drawdown. A majority of these wetlands are located in Washington County. Based on Dr. Pruitt's analysis, it is likely that the NTC/Knight Property contains 1,981 acres of "very highly" vulnerable wetlands; 1,895 acres of "highly" vulnerable wetlands; and 390 acres of "moderately" vulnerable wetlands, which are likely to be harmed by the drawdown in times of drought. In reaching his opinion about the quantification of acres of wetlands likely to be harmed, Dr. Pruitt applied the Florida Uniform Mitigation Assessment Method ("UMAM"). UMAM was designed to address compensatory mitigation in dredge and fill cases. It was not designed for consumptive water use cases. In contrast and damaging to its case of reasonable assurance that natural systems will not be significantly affected, the District did not conduct an analysis to determine loss of wetland function resulting from operation under the Permit. Nor did it determine how much drawdown the affected wetlands could tolerate before they were harmed. Rather than conducting such an analysis, the District chose to rely on implementation of the LTEMP to cure any harm that might be down by drawdown to the Surficial Aquifer. The District and Bay County's wetland scientists opined that there might be a less permeable restrictive layer maintaining water levels above the Surficial Aquifer on the NTC/Knight Property. Dr. Pruitt acknowledged that the NTC/Knight Property had scattered clay layers beneath the surface. It is possible, therefore, that some of the wetland areas he identified as subject to harm have restrictive features under them which would hold water and resist dehydration. In his hand-auguring, however, Dr. Pruitt found no evidence of a less permeable layer. The auguring only went to a depth of three feet and would have to go to a depth of two meters to be definitive. Furthermore, Dr. Pruitt found no evidence of a less permeable layer from well drillings. The District and Bay County did not prove that there is, in fact, such a restrictive layer. NTC/Knight collected water-level data from shallow hand-augured wells and stage recorders at the Botheration Creek Hillside Seepage Bog. The data demonstrate that the water level in the shallow, hand-augured wells at the Botheration Creek Bog is a direct reflection of the level of the Surficial Aquifer. The Surficial Aquifer at the Botheration Creek Bog was approximately 95.5 feet NAVD, over 35 feet higher than at Big Blue Lake and the highest measured level south of Big Blue Lake. The Botheration Creek Hillside Seepage Bog is located between the 0.3 and 0.4 foot Surficial Aquifer drawdown contours predicted by the HGL Model. Based on the HGL Model, the District and Bay County's experts estimated the Surficial Aquifer drawdown at this bog would be 0.39 feet. During the approximately one year of NTC/Knight's water-level recording, a drawdown of 0.39 feet would have reduced the frequency and duration of inundation at this bog significantly. For example, an analysis of the approximately one year of data collected by NTC/Knight shows that at the intermediate water-level recorder location in the bog, one 29-day period of inundation would have been reduced to just nine days and that further down gradient in the bog, none of the five instances when the bog was inundated would have occurred. This is consistent with Dr. Pruitt's vulnerability assessment, which finds that the vulnerability of the hillside seepage bogs to drawdown is "very high," that is, these systems are likely to be harmed in times of drought at drawdown levels in the Surficial Aquifer of 0.2 feet or greater. A drawdown of 0.3-0.4 feet in the Surficial Aquifer at the hillside seepage bog along Botheration Creek increases the likelihood that the hillside seepage bogs along Botheration Creek will be lost in times of drought. The littoral shelves of Sand Hill Lakes typically occur along a low gradient above the normal low water level of the lakes. The existence of the shelf promotes seepage sheet flow along a wide expanse. The drawdown will change the flow from seepage sheet flow to concentrated stream flow within gullies. The erosion and increased sedimentation produced by the greater force of the water in the gullies will cause a loss of area needed by certain seepage dependent plants and animals. If Big Blue Lake were to be drawn down by the 0.71 feet predicted by Mr. Davis, the location of the seepage would move down 0.71 feet vertically and an estimated 24.5 feet horizontally. The result would be a reduction in the littoral shelf conducive to seepage-dependent plant communities by approximately nine acres. The impact would likely be significant since the seepage zone is in an area of "very high" vulnerability according to Dr. Pruitt. Between October 2010 and July 2011, NTC/Knight took four measurements of water level at "BCS-01," a stage recorder in Botheration Creek. The measurements showed the water level in the creek at that point to be 0.1 to 0.32 feet. NTC/Knight also sampled for taxa of macroinvertebrates in the reach of the creek. NTC/Knight identified 46 taxa, including mussels and six long-lived taxa. The presence of the long-lived taxa and mussels indicate that the reach of the creek in the vicinity of the stage recorder should be considered to be a perennial stream. Botheration Creek is high-quality water and, as shown by NTC/Knight's sampling, it contains a diverse mix of aquatic invertebrates and fish. A drop in the level of Botheration Creek of 0.2 feet predicted by the HGL Model would have caused the creek to go dry at BCA-01 during three of the four dates on which the water level was measured. Such a drop would convert the reach of the creek in the vicinity of the stage recorder from a perennial to an intermittent stream and would eliminate the reach's viability for long-lived taxa. Similarly, upstream reaches that are intermittent would become ephemeral (streams that flow only during periods of high rainfall). If the Wellfield becomes fully operational as allowed by the Permit, there will be a reduction in the Surficial Aquifer at Botheration Creek of between 0.2 and 0.3 feet. The reduction in the aquifer will reduce flow in Botheration Creek, reduce the volume downstream, including in Pine Log Creek, and reduce out-of-bank flood frequency and duration. The result will be a reduction in nutrients delivered downstream and to the floodplain to the detriment of plants and animal life that depend on them. Additionally, other reaches of the creek that have perennial flow will be converted to intermittent streams and reaches that are intermittent will become ephemeral. The result will be the elimination of plant and animal species currently living in these portions of the creek. The impact of the HGL Model predicted drawdown to steepheads depends on the individual steephead and the drawdown contour at its location and the amount of rainfall. Four steepheads on the NTC/Knight Property could suffer impacts similar to the impact at Russ Steephead to which Dr. Pruitt assigned a high probability of impact. Russ Steephead is located on the NTC/Knight Property above Russ Pond. NTC/Knight installed Surficial Aquifer wells at Russ Steephead between the HGL Model's predicted 0.5 and 0.6 foot Surficial Aquifer drawdown contours. NTC/Knight also installed a stage recorder just downstream from the steephead. During drought, NTC/Knight observed a loss of flow from the sidewall seepage areas and in the Russ Steephead Stream. If the Surficial Aquifer at Russ Pond were to be drawn down by 0.5-0.6 feet, the sidewalls of the Russ Steephead Stream and the stream itself would lose flow in times of drought. The loss of flow would lead to oxidation and loss of organic materials in the stream channel and flood plain, resulting in soil subsidence. If the water level at the terminus of the Russ Steephead Stream were drawn down, headward down cutting in the stream channel would be induced. In such a case, in the words of Dr. Pruitt, "there is a high probability that if drawdown occurs and . . . over a long period of time," the process will make the steephead "look more like a gully . . . ." Tr. 2120. The drawdown will also reduce the frequency and duration of inundation of the sphagnum bogs in the four steepheads likely to be affected by the drawdown. The bogs and the associated animals that depend upon them would be lost. Dr. Means identified a number of temporary ponds within HGL's predicted drawdown of the Surficial Aquifer. Nine were between the 0.3 and 0.6 foot drawdown contour, and two were between the 0.6 and 0.7 foot drawdown contours. These ponds and plant and animal communities dependent upon them would likely be harmed by the drawdowns. Mr. Cantrell offered testimony to rebut the Petitioners' case on wetland impacts. His testimony was based on an evaluation of aerial photography, site visits to the Wellfield, and a one-day trip to the NTC/Knight Property. It is Mr. Cantrell's opinion that if the NTC/Knight Property were to drain, it would be because of a surface water drainage system, such as ditching, not because of drawdown in the Surficial Aquifer caused by operation of the Wellfield. Mr. Cantrell's opinion is that because the Area has been subjected to a wide range of fluctuations in water levels and the wetland systems have survived, operation of the Wellfield will not have significant impacts. Mr. Cantrell's opinion, however, overlooks the effect of constant drawdown during times of severe drought. That wetlands have survived severe drought in the past does not mean they will survive severe drought conditions exacerbated by drawdown caused by operation of the Wellfield. Monitoring Special condition 19 of the Permit requires Bay County to implement the LTEMP after the Permit is issued. The LTEMP requires Bay County to establish a monitoring network, but does not provide the location of any particular monitoring site. Sites identified in the LTEMP are recommended, but the ability to use a particular site is dependent on field verification of suitability and authorization by the landowner. Over half the area designated in the LTEMP from the HGL Model's projected 0.5 foot drawdown in the Surficial Aquifer is located on the NTC/Knight Property. It will be necessary, therefore, to include sites on the NTC/Knight Property in the ultimate environmental monitoring network. The LTEMP's recommended sites do not include monitoring of some of the most susceptible wetland systems: temporary ponds, the Botheration Creek hillside seepage bogs, and the perennial headwaters of Botheration Creek. Without this monitoring, the LTEMP will be unable to detect whether these systems are harmed by withdrawals. The Permit and LTEMP require no more than one-year of baseline data to be collected prior to initiation of water withdrawals. The proposed monitoring time is inadequate to create a sufficient record for use in determining whether a reduction in water levels is attributable to water withdrawals or natural phenomena, such as drought. Baseline monitoring should be conducted for a sufficient duration to ensure that a full range of wet and dry years is captured. The LTEMP describes the types of data that are to be collected. A missing component is sampling for frogs, salamanders, and other amphibians that are sensitive to changes in hydrologic regimes and which depend upon infrequent periods of inundation in order to breed. This type of faunal sampling is particularly important in the temporary ponds and seepage environments. Without sampling for the presence of these species, the LTEMP will be unable to determine whether these populations have been harmed by withdrawals. The LTEMP includes a number of "triggers," that if tripped, require the preparation of an auxiliary report. A number of these triggers make reference to changes in water levels at the level of "significant deviation," an undefined term. More importantly, the LTEMP fails to require any statistical analysis. Without it, the LTEMP will be inadequate to establish whether a reduction in water levels is caused by water withdrawals or another cause. Similarly, other triggers lack sufficient detail to determine when they are tripped, such as those that refer to downward movement of plants. Finally, even if one of these triggers is tripped and an auxiliary report is prepared, nothing in the Permit or LTEMP sets forth the circumstances under which withdrawals would need to be curtailed and by what amount. The purpose of the LTEMP is to determine whether withdrawals are causing harm to the wetlands within the vicinity of the Wellfield. The LTEMP fails to provide reasonable assurance that it will succeed in achieving its purpose. Reasonable-Beneficial Use Use if the Reservoir is Unavailable In the event of Reservoir unavailability, Bay County is likely to need much less than 30 MGD. The need is likely to fall between 7.42 MGD and 9.71 MGD for the current population. In 2013, the need is likely to fall between 9.40 MGD and 12.29 MGD. See NTC/Knight Ex. 5, p. 4 of 4. The Permit, however, does not limit Bay County to emergency or backup use. While Bay County might voluntarily limit withdrawals to emergency use or backup supply, it has unfettered discretion to determine what constitutes an emergency or the necessity for a backup supply. The Permit is also not restricted to essential uses. Authorization of 30 MGD provides more than Bay County's current average daily demand for potable water. If the Permit restricted the use to essential uses, the authorization would be far less than 30 MDG. The District commissioned King Engineering to assist in development of a "Coastal Water Systems Interconnect Project" (the "Interconnect Project"). On average, the utilities subject to the Interconnect Project estimated that 42 percent of the average daily demand is dedicated to essential uses with the remaining 58 percent going to non-essential uses. Consistent with the estimate, the Project set a target of 50 percent of average daily demand to be allowed for use in an emergency. None of the information from the Interconnect Project, however, was used by the District in setting the limits of withdrawal in the Permit. b. Daily Use Bay County claims the 5 MGD annual average allocation under the Permit is needed for several reasons, principally the maintenance of pumps. Bay County's justification for 5 MGD is found in testimony from Mr. Lackemacher and a document he authored entitled, "Confidential Draft for Internal Use Only 5 MGD Pumping Rate" (the "Lackemacher Confidential Draft"), admitted as Bay County Ex. 24. Mr. Lackemacher's testimony follows: A. The fact is that there are no absolute knowns when we're talking about what needs to be. Q. What do you mean? A. Well, here we have a document [Bay County Ex. 24] where I talk about rationalization for 5 million gallons a day, why we would need it, mechanical reasons, financial reasons, regulatory reasons. I always felt that it was very difficult to justify a number. I don't know. We haven't designed the system. We haven't got all of the wells in. We don't know what their specific yields are. There's unknowns here. So do we need 2 million gallons a day or 5 million gallons a day? I don't know. I don't know that. But here is the rationalization for 5 million if that's in fact what we need. We may very well find out that we don't need 5 million gallons a day. Q. Is that because you don't know the precise locations of the well and how they're going to be piped and distributed? A. That's absolutely true. Q. Well, did you in this report, Exhibit 24, did you make some reasonable assumptions? A. I based it on some of the values as you discussed or as I pointed out earlier from Hatch Mott MacDonald's preliminary design. * * * Q. And do you feel confident that your analysis supported that in the area of 5 million gallons a day is what would be needed to operate the wellfield? A. Yes. And that's why the paper was generated that [is] a justification for 5 million gallons a day, here's what we think we would need. Tr. 209-10. The Lackemacher Confidential Draft is a one-page, written justification for the 5 MGD. Based on the Hatch Mott McDonald Report, see tr. 210, it considers regulatory, mechanical and financial factors. It is not supported, however, by engineering analysis. Any financial analysis found in the Hatch Mott McDonald Report, moreover, is far from complete. The factors taken into consideration are recited in the most general of terms. For example, of four such factors, the document lists the second as: "All water pumps are designed to run - turning pumps on and off is not the best situation for the overall electrical efficiency or the mechanicals of a pump." Bay County Ex. 24. Consistent with Mr. Lackemacher's testimony, the document concludes that the amount of water needed to run each well is unknown. The financial justification is based on costs shown in the Hatch Mott MacDonald Report for construction and operation of 22 wells, ten more wells than are contained in the Wellfield and without any analysis of revenue to recoup the costs. The financial justification is a bare conclusion on the part of Mr. Lackemacher: We cannot afford to operate a well field at a financial loss, based on this fact alone we would have to pump a minimum of 4.49 MGD. Combined with the fact that we don't know what volumes of water have to be turned over to ensure water quality 5 MGD seems quite reasonable. Bay County Ex. 24. The Lackemacher Confidential Draft is dated May 17, 2011. It was not part of Bay County's Application nor was it submitted to the District prior to the decision to issue the Permit. Although the District attempted to obtain information from Bay County about what was needed for maintenance, Bay County did not provide it. As Mr. Gowans testified, "[t]hen I finally told staff, [s]top asking, we're not going to get the numbers . . . ." Tr. 552. The District performed no analysis to determine the minimum amount of water needed to maintain the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Phillip Waller, an engineer accepted as an expert in the design and construction of potable water systems, including groundwater wells, surface water, and transmission and distribution of drinking water. Mr. Waller testified that if the wells were connected to a central treatment system, there would not be the need to flush the pipeline for disinfection prior to use of the well in an emergency. Only 2.4 million gallons per year or 6,500 gallons per day would be needed to maintain optimum operating conditions, an amount far less than 5 MGD. Mr. Waller's experience when groundwater is used as a backup, moreover, is that they are operated periodically. While prudent to periodically operate backup wells especially in advance of hurricane season, vertical pumps in wells, unlike horizontal pumps, do not have a need for frequent operation because of even force distribution. They certainly do not need to be continuously operated. "In fact, wells routinely are idle for months at a time." Tr. 1123. Interference with Existing Legal Users In its Revised Staff Report dated July 18, 2011, the District wrote: Nearby Users: Under the most intensive pumping activity, drawdown in the Upper Floridan Aquifer is predicted to be approximately 15 feet in the vicinity of the nearest private wells. Water level declines of this magnitude may cause water levels to fall below the level of the pump intake in some privately-owned wells. Joint Ex. Vol. IV, Tab Q, p. 4. The District's high estimate of the number of wells used by existing legal users that might suffer impacts approaches 900. The exact number or whether any existing legal users would be likely to suffer impacts was not proven. Alternatives Groundwater wells, if installed and attached to the fitting in the existing transmission line that delivers water from the Pump Station to the Water Treatment Plant, could serve as backup to the Reservoir. Bay County did not conduct a study of whether groundwater in the area of the transmission line was adequate to serve as an alternative. Mr. Waller, on behalf of NTC/Knight and Washington County, on the other hand, testified that the transmission line could support ten wells with a capacity of 10 MGD and could be constructed at a cost of $12 million, far less than the Wellfield. The area of the transmission line is in an area identified by the District as acceptable for the creation of potable water wells. The area does not present a significant risk of saltwater intrusion if not used continuously. The water meets the drinking water requirements for the Department of Environmental Protection and the Department of Health. The existing transmission line alternative is located near the existing raw water supply line which minimizes the need for additional piping. There is sufficient length along the existing raw water pipeline to accommodate ten wells. The existing transmission line alternative, therefore, has significant potential to succeed as a water supply backup to the Reservoir. NTC/Knight and Washington County, through Mr. Waller, also proposed another alternative: an intake at Bayou George. Near Highway 231, the main pipeline from the intake would run along public right-of-way. North of the existing intake in Williams Bayou and three miles north of the Dam, the proposed intake would be less susceptible to contamination from storm surge. Neither Bay County nor the District presented a thorough analysis of any alternative to the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Mr. Waller that there are two alternatives that could be constructed at much less cost than the Wellfield and that have significant potential of providing backup supply.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Northwest Florida Water Management District enter a final order that denies the application of Bay County for the individual water use permit at issue in this proceeding. DONE AND ENTERED this 26th day of July, 2012, in Tallahassee, Leon County, Florida. S DAVID M. MALONEY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 26th day of July, 2012.
