Findings Of Fact The Hearing Officer finds that if this request was approved, and pumpage reduced at the old wells to 1.5 MGD that together with the 1 MGD well New Port Richey would have permits totaling 6.5 MGD. Considering a service area population of 20,000 people, this would be 300 gallons of water per person per day in the service area, or over two (2) time1s the generally accepted per capita usage. While the Hearing Officer recognizes the desirability of shifting the water sources for the coastal area further inland and the desirability for the City to have emergency water pumping capacity, the per capita quantities involved in New Port Richey total water resource program are out of line and are unjustifiable in light of current and even projected needs within the 3.5 year period of this permit. Many solutions exist to emergency pumping, not the least of which is installation of gas or diesel anxillary pumps at least one of the Starkey wells. The Hearing Officer would note that salt water intrusion is an important basis for approval of the Starkey Well Field applications, and that pumping 1.5 MGD from the old wells will not allow the full benefit to the coastal water supply to be achieved. Continued salt water intrusion will work a hardship on all well owners in the New Port Richey area. The Hearing Officer is also aware, having heard the case, of the application of the 1 MGD well at Starkey Well Field. Part of the justification for approval of that application was that it would be used to meet peak demands when this instant application was approved. (See Hearing Officer's Recommended Order dated August 5, 1976.) Together with the old wells, this would provide 2.5 MGD for peak usage, or an amount equal to the daily per capita needs for 20,000 people, over and above the 4 MGD requested in this application. The Hearing Officer further notes that an objection to this current application was filed in behalf of an adjacent landowner. There is no indication within the file provided the Hearing Officer that this landowner received notice of the instant hearing by letter or publication.
Recommendation The Hearing Officer having considered the law and the evidence recommends the denial of this application, and further, in the absence of any proof of notice to the objecting adjacent landowner, the Hearing Officer recommends that the Board permit him to present any evidence which he feels is relevant at its consideration of this application. DONE and ORDERED this 27th day of February, 1976. STEPHEN F. DEAN, Hearing Officer Division of Administrative Hearings Room 101, Collins Building Tallahassee, Florida 32301 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Counsel for SWFWMD Jack B. McPherson Esquire Counsel for City of New Port Richey
The Issue Whether a consumptive use permit for the quantities of water applied for should be granted.
Findings Of Fact Applicant Phillips Petroleum Company submitted application Number 7500103 for a consumptive use permit for an average daily withdrawal of 9,000,000 gallons of water a day to be withdrawn from the Florida Aquifer in DeSoto County, Florida. The application is for a new use and the withdrawal is for industrial use from four withdrawal points. The center of withdrawals will be located at Latitude 27 degrees, 14 minutes, 40 seconds north. Longitude 82 degrees, 2 minutes, 48 seconds west, in DeSoto County. Notice of the September 3, 1975 public hearing was published in a newspaper of general circulation, to wit: The Arcadian on August 14 and 21, 1975, pursuant to Section 373.146, Florida Statutes. Notice of the continuation of the hearing held at 10:30 a.m., December 11, 1974 were duly noticed. Sarasota County was granted leave to intervene as a party to the proceeding. Evidence was received and testimony was heard by all parties at the September 3, 1975 hearing and evidence was received and testimony was heard by she Applicant and Intervenor at the December 11, 1975 hearing, and although the attorneys for the Southwest Florida Water Management District took no further part in the December 11, 1975 hearing on the merits, depositions of the Southwest Florida Water Management District staff members, James Mann and Barbara Boatwright, were received. Phillips Petroleum Company owns approximately 15,200 acres of land in DeSoto County and Manatee County and proposes to commence a phosphate mining operation on that property using a total of 15 million gallons of water per day, 9,000,000 gallons per day (MGD) from DeSoto County and 6 million gallons per day (MGD) from Manatee County. This application for a permit is for the 9 million gallons of water to be withdrawn from an 8,700 acre parcel owned by the Applicant in DeSoto County, Florida. As such it presumptively seeks withdrawal and consumptive use of no more than the average annual water crop for this parcel. Pursuant to the water crop theory, the water crop for the 8,700 acres contro led by the Applicant in the Southwest Florida Water Management District is 8.7 million gallons of water per day. However, as shown by correspondence of a hydrologist from Southwest Florida Water Management District, a phosphate mining operation is only 90 percent consumptive and therefore the actual consumptive use is 7.8 million gallons per day and falls within the water crop theory assumption set forth in Rule 16J-2.11(3), F.A.C., infra. The statutory criteria for granting a consumptive use permit is found in Section 373.223, Florida Statutes, which states: "(1) To obtain a permit pursuant to the provisions of this chapter, the applicant must establish that the proposed use of water: Is a reasonable-beneficial use as defined in 474.019(5); and Will not interfere with any presently existing use of water; and Is consistent with the public interest. (2) The governing board of the department may authorize the holder of a use permit to transport and use ground or surface water beyond overlying land or outside the watershed from which it is taken if the governing board or department determines that such transport and use is consistent with the public interest." This statute has been supplemented by rules adopted by the Southwest Florida Water Management District and is found in Rule 16J-2.11, F.A.C.: "16J-2.11 Conditions for a Consumptive Use Permit. The intended consumptive use: Must be a reasonable, beneficial use. Must be consistent with the public interest. Will not interfere with any legal use of water existing at the time of the application. Issuance of a permit will be denied if the withdrawal of water: Will cause the rate of flow of a stream or other watercourse to be lowered below the minimum rate of flow established by the Board. Will cause the level of the potentiometric surface to be lowered below the regulatory level established by the Board. Will cause the level of the surface of water to be lowered below the minimum level established by the Board. Will significantly induce salt water encroachment. Will cause the water table to be lowered so that the lake stages or vegetation will be adversely and significantly affected on lands other than those owned, leased or otherwise controlled by the applicant. Issuance of a permit will be denied if the amount of water consumptively used will exceed the water crop of lands owned, leased, or otherwise controlled by the applicant. (Except where determined otherwise, the water crop [precipitation less evapotranspiration] throughout the District will be three hundred sixty-five thousand (365,000) gallons per year per acre.") The United States Geological Survey and the Florida Department of Environmental Relation have received data supplied to Southwest Florida Water Management District with the application for a consumptive use permit. Throughout the course of the hearing testimony was heard and evidence was received as to the "leakance value" of the parcel of land in question. "Leakance value" was defined as the moving of water from the surface down into the deeper aquifer. A geologist, Mr. Donald S. Kell, with the Department of Environmental Regulation, and who testified at the request of the Intervenor, Sarasota County, was of the opinion that insufficient data to determine leakance value in connection with the mining operation had been submitted and therefore further tests were needed. Mr. Jack Hickey of the United States Geological Survey was of the opinion that leakance value had not been obtained. The technical staff members of the Southwest Florida Water Management District were uncertain as to whether reliable leakance value had been obtained. It was the position of the Intervenor, Sarasota County, that due to the geological conditions of the proposed mining operation, this leakance value or surface recharge into the aquifer was insufficient and was not in conformity with Southwest Florida Water Management District's water crop theory assumption of 1,000 gallons per acre per day. Although evidence was presented on this point, it is the finding of this Hearing Officer that such evidence was insufficient to establish the basis of, any finding of fact or to rebut the assumption contained in the above referenced rule. The validity of this rule was not challenged and the presumption is that the rule is valid. The water used in the flotation process of applicants mining and benefication process would be recycled and reused in other areas of the phosphate operation. A letter of objection by Donald T. Yeats was examined and considered in this Order. The Applicant presented evidence that the construction of the facility would be in excess of $94 million expended over a period of 3 years, 61 percent of which would be spent in the region. 350 people would be employed at full production. Additional support jobs would employe from 200-400 people. Evidence was presented by the Applicant and was not rebutted by the Intervenor or by the Southwest Florida Water Management District as to each of the applicable conditions for a consumptive use permit in Chapter 16J-2.11, Rules of the Southwest Florida Water Management District, effectuating the provisions of Chapter 378, Florida Statutes.
Recommendation That the Southwest Florida Water Management District approve Phillips Petroleum Company's application for a consumptive use permit as requested, subject to the following terms and conditions: Prior to commencing withdrawals, Phillips Petroleum shall notify the District of said commencement; All production wells will be equipped with appropriate flow deters or other measuring devices; Phillips shall submit periodic reports of withdrawal to the District; and Phillips shall install appropriate observation wells or other monitoring facilities. DONE and ORDERED this 12th day of January, 1976. DELPHENE C. STRICKLAND Hearing Officer Division of Administrative Hearings Room 101, Collins Building Tallahassee, Florida 32301 (904) 488-9675 COPIES FURNISHED: Jacob D. Varn, Esquire Carlton, Fields, Ward, Emmanuel, Smith & Cutler 2000 Exchange Bank Building Tampa, Florida Jay T. Ahern, Esquire Southwest Florida Water Management District Post Office Box 457 Brooksville, Florida Richard E. Nelson, Esquire Richard L. Smith, Esquire Nelson, Payne, Hesse and Cyril 2070 Ringling Boulevard Sarasota, Florida
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 in this case is whether the Department of Environmental Protection (DEP) should issue a permit to Out of Bounds, Inc. (Out of Bounds, or applicant), to construct, operate, and close a construction and demolition debris disposal facility (C&D facility) in Hernando County.
Findings Of Fact On September 8, 2008, Out of Bounds applied to DEP for a permit to construct, operate, and close an unlined C&D facility on 26 acres located at 29251 Wildlife Lane, Brooksville, Hernando County, Florida, to be known as the Croom C&D Debris Landfill and Recycling Facility. There were four requests by DEP for additional information, which was provided, and the application was complete on September 3, 2009. In 1994, a previous owner of the property was issued a permit to construct, operate, and close an unlined C&D facility on the property. That owner did not proceed with construction, and the permit expired in 1999. The Out of Bounds application was for a new permit, not for the renewal of an existing permit. Robert McCune owns property adjacent to the proposed C&D facility. He and his wife reside on the property, keep horses in stables on the property, and use the property for horseback riding business, which includes hosting public horseback riding events. Hernando SSK was formed by David Belcher and one or more others to continue the business being operated by Paige Cool when she died during this proceeding. The business is conducted on ten acres of property Cool owned approximately one mile west of the proposed C&D facility. Belcher is one of two co-personal representatives of Cool’s estate. Belcher and his wife hold a mortgage on the property. When the estate is finalized, the Belchers plan to assign their mortgage to Hernando SSK. It is not clear who will own the property after the estate is finalized, or how Hernando SSK will be authorized to continue the business on the property. Western pleasure and trail-riding horses are boarded on the Cool property, which is known as At Home Acres. The business also has access to 20 adjoining acres to the east, which are used for grazing. Access to the horseback riding trails in the Withlacoochee State Forest is conveniently located just across Wildlife Lane from the property, to the north. A manager resides in a double-wide trailer on the property, and another trailer and a barn to the east of it are leased out. There is a potable water well on the property, which is the source of drinking water for the manager and lessees. Well Setback In the application process, Out of Bounds disclosed two potable water wells within 500 feet of the proposed landfill disposal area. The application provided that those wells would be converted to non-potable use. Out of Bounds did not disclose the existence of a third potable water well, on property owned by Daniel Knox, which is within 500 feet of the proposed landfill disposal area. When the Knox well was brought to the attention of DEP, Out of Bounds admitted that the well was permitted for potable use but took the position that it was not for potable use because it was not in use, was not connected to a source of electricity, and appeared to be abandoned. Daniel Knox and his brother, Robert Knox, had the Knox well dug and permitted in 1979 in anticipation of using it as the source of potable water for a residence to be built on the property for their parents and sister. The Knoxes have not yet built a residence on the property, but it still is their intention to do so and to use the well as the source of potable water. Since its construction, the well had been maintained and operated periodically using a gasoline-powered generator so that it will be ready for use when needed. During the application process, Out of Bounds also did not disclose the existence of a fourth potable water well within 500 feet of the proposed landfill disposal area on property once owned by Larry Fannin and now owned by his daughter and son-in- law, Robert McCune. The McCune well was permitted and installed in mid-2005 while the sale of the land from Fannin to the McCunes was pending. The intended purpose of the well was to provide potable water for the use of the McCunes when they started to reside on the property. Despite this intent, and unbeknownst to the McCunes, Fannin had the well permitted as an irrigation well. In mid-2008, the McCunes began to reside on their property. At first, they resided in a mobile home. They ran pipes from the well to the mobile home to provide drinking water. Eventually, later in 2008, they began construction of a residence on the property and ran pipes from the well to the house to provide drinking water to the house. The well was being used for drinking water before the Out of Bounds application was complete. (They also use water from the well from time to time for irrigation purposes--i.e., when they host horseback-riding events on weekends, they truck water from the well to their horseback-riding arena to apply to the ground to control dust.) Groundwater flows from the disposal area of the proposed landfill to the west and southwest. The Knox and McCune wells are down-gradient of the groundwater flow from the proposed disposal area. Out of Bounds represented at the hearing that it would accept a permit condition that no C&D debris, but only clean debris, would be disposed within 500 feet of the Knox and McCune wells. See Fla. Admin. Code R. 62-701.200(15)-(16) and (24). However, there was no evidence of new designs, plans, or operations that would be used to meet such a permit condition. Liner and Leachate Collection Existing unlined C&D facilities in the Southwest District report various parameters that exceed groundwater quality standards and criteria. These include arsenic, benzene, iron, aluminum, nitrate, ammonia, vinyl chloride, methylene chloride, 3- and 4-methyl phenols, sulfate, and total dissolved solids (TDS). Arsenic and benzene are primary (health-based) groundwater quality standards. The others are secondary standards that relate to taste, odor, and aesthetics. The likely source of the reported arsenic violations in the Southwest District is wood treated with chromate copper arsenate (CCA). See Fla. Admin. Code R. 62-701.200(11). Out of Bounds proposes to not accept CCA-treated wood and to use a trained “spotter” to exclude CCA-treated wood from the landfill. This is an appropriate measure to prevent arsenic violations, and is now required for C&D facilities. See Fla. Admin. Code R. 62-701.730(7)(d), (8), and (20). It was not clear from the evidence whether the C&D facilities in the Southwest District with arsenic violations accepted CCA-treated wood. Even if they did, the operational plan proposed by Out of Bounds to exclude CCA-treated wood and to use a trained spotter is not a guarantee that no CCA-treated wood will enter the landfill. A C&D facility would not be expected to dispose of material that would result in benzene contamination. The reported benzene violations suggest that unauthorized material contaminated with benzene nonetheless makes its way into C&D facilities in the Southwest District. The evidence was not clear whether a trained spotter was used at those facilities. Whether or not a spotter was used at those facilities, having a trained spotter would not guarantee that no benzene-contaminated material will enter the landfill proposed by Out of Bounds. Out of Bounds suggested that ammonia violations result from C&D facilities accepting yard trash. However, there was no evidence of a connection between acceptance of yard trash and ammonia violations. The operational plan proposed by Out of Bounds to “cover as you go” is the accepted best practice to control hydrogen sulfide odor, which comes from wet drywall. Out of Bounds suggested that its cover plan would prevent any sulfate violations, but there was no evidence to prove it. There was no evidence as to whether the C&D facility proposed by Out of Bounds would be substantially different from the other existing C&D facilities in DEP’s Southwest District. Absent such evidence, Out of Bounds did not provide reasonable assurances that its proposed facility would not cause groundwater quality violations. The site for the C&D facility proposed by Out of Bounds is internally drained. There are no surface waters onsite or within a mile of the site. There was no evidence of a surficial aquifer above the Floridan aquifer. Rainfall entering the Out of Bounds property migrates downward into the Floridan aquifer. Once in the aquifer, there is a horizontal component of groundwater water flow in a generally southwest direction, towards the Knox and McCune wells. Contaminated leachate from the proposed C&D facility would migrate with the groundwater. Out of Bounds suggests that a thick clay layer under the site of its proposed facility would prevent the downward migration of groundwater into the Floridan aquifer. There are several reasons why the clay layer does not provide the reasonable assurance of a liner that contamination from the proposed landfill would not reach the Floridan aquifer. Clay is much more permeable than a geomembrane meeting DEP’s specifications for use as a liner. The clay on the proposed site is on the order of at least a thousand times more permeable. (Out of Bounds appeared to confuse the permeability of such a geomembrane with the allowable permeability of the geosynthetic clay layer or compacted clay layer underlying the geomembrane. Cf. Fla. Admin. Code R. 62-701.730(4)(f).) In the application process, Out of Bounds relied on the clay layer for purposes of sinkhole prevention and mitigation, not for reasonable assurance that no liner was needed. The limestone formation underlying the site is highly variable, with numerous pinnacles; for that reason, the thickness of the clay layer also is highly variable, making it difficult to excavate the proposed landfill with complete assurance that the clay layer would not be penetrated. To provide reasonable assurance for purposes of sinkhole prevention and mitigation, Out of Bounds proposed to leave or create a clay layer at least six feet thick underlying the bottom of the proposed landfill. Because the site is in an area of high recharge to the Floridan aquifer and drains entirely internally, the clay layer alone does not provide reasonable assurance that there will be no downward migration of contaminated groundwater to the Floridan aquifer. Reasonable assurance requires a liner and leachate collection system.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that DEP deny the application for a C&D facility made by Out of Bounds. DONE AND ENTERED this 8th day of December, 2011, in Tallahassee, Leon County, Florida. S J. LAWRENCE JOHNSTON 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 8th day of December, 2011. COPIES FURNISHED: Ronda L. Moore, Esquire Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Stop 35 Tallahassee, Florida 32399-3000 John R. Thomas, Esquire Law Office of John R. Thomas, P.A. 233 Third Street North, Suite 101 St. Petersburg, Florida 33701-3818 Timothy W. Weber, Esquire Battaglia, Ross, Dicus & Wein, P.A. Post Office Box 41100 St. Petersburg, Florida 33743-1100 Herschel T. Vinyard, Jr., Secretary Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Stop 35 Tallahassee, Florida 32399-3000 Thomas Beason, General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Stop 35 Tallahassee, Florida 32399-3000 Lea Crandall, Agency Clerk Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Stop 35 Tallahassee, Florida 32399-3000
The Issue The issue to be determined in this case is whether Florida Power & Light Company (“FPL”), is entitled to a water use permit issued by the South Florida Water Management District (“District”) to withdraw water for use at FPL’s Turkey Point Power Plant in Miami-Dade County.
Findings Of Fact The Parties Tropical Audubon is a Florida not-for-profit corporation incorporated more than one year prior to the date FPL filed its permit application. Tropical Audubon was formed for the purpose of protecting the environment, fish and wildlife resources, and air and water quality. Its mission is to “conserve and restore South Florida’s ecosystems, focusing on birds, other wildlife and their habitats for the benefit of humanity and the earth’s biological diversity.” Tropical Audubon has approximately 465 members. More than 25 reside in Miami-Dade County. A substantial number of Tropical Audubon’s members use the area near Turkey Point for recreational activities, including wildlife observation. The District is a multi-purpose water management district with powers and duties set forth in chapter 373, Florida Statutes, and Florida Administrative Code Chapters 40E and 62- 40.410, including powers and duties related to the regulation of consumptive uses of water. Its principal office is located at 3301 Gun Club Road, West Palm Beach, Florida. FPL is a regulated public utility which provides electric service to its customers in 35 Florida counties. FPL owns and operates the Turkey Point Power Plant, an electric power generating facility located in unincorporated southeastern Miami- Dade County and within the boundaries of the District. Background FPL’s Turkey Point property is located 25 miles south of Miami and is situated on the coastline adjacent to Biscayne Bay. The property covers about 9,400 acres. The Turkey Point Power Plant consists of five electric generating units. Units 1 and 2 are gas and oil-fired boilers. Unit 2 has been decommissioned. Units 3 and 4 are nuclear units. Unit 5 is a combined cycle gas turbine unit. Construction of Units 1, 2, 3, and 4, as well as the Turkey Point Cooling Canal System (“CCS”), predated the enactment of the PPSA. However, Units 3 and 4 were certified under the PPSA in 2008 when they were uprated to increase their steam- electric generating capacity. Unit 5 was certified under the PPSA in 2005. Units 1 and 2 originally used once-through cooling, which involved taking water from Biscayne Bay and discharging it back into the Bay. In 1971, following a lawsuit brought by the U.S. Department of Justice, FPL signed a Consent Decree that required FPL to construct the CCS, a closed-loop cooling canal system, to eliminate heated, surface water discharges to Biscayne Bay and Card Sound. The CCS is a 5,900-acre network of canals which dissipate heat from the water used in the operation of Units 3 and 4, as well as Unit 1 when in operation. The CCS functions like a large radiator, which uses evaporation, convective heat transfer, and radiated heat loss to lower the water temperature. Circulating water pumps provide for counter-clockwise flow of water from the discharge canal, down through the western side of the CCS, and then back up the eastern side of the CCS to the power plant. The full circuit from discharge to intake takes about 48 hours. The CCS does not directly discharge to surface water, but water can enter or leave the CCS by groundwater seepage because the canals are not lined. Additions of water into the CCS include plant process water, rainfall, stormwater runoff, and groundwater seepage. In addition to the Consent Decree, FPL entered into an agreement with the District’s predecessor agency in 1972 to address the operation of the CCS. The agreement has been updated, with the most recent version being the Fifth Supplemental Agreement, executed in 2009. Pursuant to the Fifth Supplemental Agreement, FPL implemented an extensive surface water and groundwater monitoring program in and around the CCS. Since 2010, FPL has collected monitoring data for water levels, fluid density, salt concentrations, and conductivity from 42 groundwater monitoring wells. FPL also collects water level data at seven locations within the CCS on an hourly basis. In 2013 and 2014, monitoring data showed water quality decreased in the CCS, with increased salinity, algae blooms, and suspended solids in the water. Decreased water quality reduced heat dissipation, so water temperatures increased. FPL was authorized by the Nuclear Regulatory Commission (NRC) to operate the CCS with water temperatures as high as 100 degrees Fahrenheit (F). In 2014, water temperatures exceeding 100 degrees caused plant shutdowns. As a result, FPL requested and the NRC allowed the maximum operating temperature of CCS water to be raised to 104 degrees. Higher water temperatures cause more evaporation and because the evaporation of water leaves its salt content behind, the salinity of the water in the CCS increased. Water in the CCS became “hypersaline,” having chloride concentrations greater than 35 Practical Salinity Units (PSU), which is the average salinity of seawater. Because hypersaline water is denser and heavier than the naturally occurring groundwater, it sinks down through the CCS canals into the Biscayne Aquifer and down through the aquifer to a confining layer that separates the Biscayne Aquifer from the Floridan Aquifer, about 80 feet below the CCS. When the hypersaline water reaches the bottom of the Biscayne Aquifer, it moves laterally in all directions. However, the primary focus of the District and the DEP has been on the western movement of the hypersaline water because of the potential harm to existing legal uses of water and offsite land uses to the west. The hypersaline “plume” has migrated two to three miles west of the CCS. In August 2014, FPL requested and the District issued an emergency order to withdraw water from the L-31E Canal and discharge it to the CCS to reduce salinity and temperature. FPL withdrew water over a 21-day period in September and October, an average of 43 mgd, and observed reductions in salinity, algae blooms, and temperatures within the CCS. With the combination of rainfall and water from the L-31E Canal, CCS salinity levels were reduced by about 20 practical salinity units (PSU). When the proposed permit that is the subject of this case was challenged, FPL sought and obtained another emergency order to use water from the L-31E Canal during the 2015 rainy season (June 1 to November 30). Use of water from the L-31E Canal in 2015 reduced temperature and salinity levels in the CCS. Salinity declined from 95 PSU to 60 PSU. On December 23, 2014, the DEP issued an Administrative Order (“AO”) which, among other things, directs FPL to submit a Salinity Management Plan with the primary goal of “reduc[ing] the hypersalinity of the CCS to abate westward movement of CCS groundwater into class G-II groundwaters of the State.” The Proposed Permit FPL applied for the water use permit at issue in this case so it could continue to use water from the L-31E Canal for reducing temperature and salinity in the CCS. The proposed water use permit would authorize FPL to pump up to 100 million gallons per day during the period June 1 through November 30 in 2015 and 2016.1/ The permit prohibits withdrawals during the June through November period if they would interfere with the water reservation for Nearshore Central Biscayne Bay, which was established by Florida Administrative Code Rule 40E-10.061. The proposed project involves installation of three pumps and pipes to transfer water from the L-31E North Canal to the L-31E Canal where it would flow south to a point where two pumps would withdraw the water and discharge it through two pipes into the CCS. The permit would allow FPL to withdraw up to 100 million gallons per day (“mgd”). The proposed permit does not identify temperature or salinity objectives, but FPL would be required to submit weekly water temperature and salinity data to demonstrate that the water use is reducing the temperature and salinity of the water within the CCS. Tropical Audubon contends the proposed project is not entitled to a permit because it would harm the natural resources of Biscayne Bay, would increase saltwater intrusion, is not limited to the amount of water needed, and is inconsistent with the 2008 Certification Order and the 2014 AO. Biscayne Bay Biscayne Bay was a tidal estuary before human changes, as described above, reduced freshwater inflows to the Bay. Now the Bay has salinity levels characteristic of a marine lagoon. Salinity levels historically varied across Biscayne Bay, but now the salinity levels are higher. The species richness of Biscayne Bay has been reduced by the reduction of freshwater inflows; that is, the observed numbers of some animals and the areal extent of some plants have been reduced. The reservation of water for Nearshore Central Biscayne Bay is for a geographic area which generally follows the shoreline along Biscayne Bay and extends 500 meters from the shoreline. It is a small fraction of the total area of the Bay. Tropical Audubon stipulated that FPL’s proposed water use would not interfere with the water reservation for Nearshore Central Biscayne Bay, but it contends the reservation does not account for all of the freshwater needs of the Bay. Tropical Audubon’s expert, Dr. Lodge, suggested that the areal extent of “lower salinity grass beds” would increase with fresh water inputs exceeding the water reservation, which would benefit the species that use these grass beds. Neither the reservation rule nor the evidence presented by Tropical Audubon indicates what amount of freshwater is needed for all of Biscayne Bay. Tropical Audubon’s position is simply that more freshwater flow into Biscayne Bay is better than less and FPL’s proposed water withdrawal from the L-31E Canal will result in less freshwater reaching Biscayne Bay. Respondents stipulated that a substantial number of Tropical Audubon’s members have substantial interests in recreational uses in and near Biscayne Bay, but Respondents did not stipulate that the proposed project affected those interests. Tropical Audubon presented little evidence to demonstrate the proposed water use could affect its members’ substantial interests. Instead, it devoted almost all of its efforts at the final hearing and in its proposed recommended order to addressing matters that would not affect Tropical Audubon’s members, such as saltwater intrusion or inconsistency with the Certification Order. Tropical Audubon’s three-part proposition for harm to the substantial interests of its members is that (1) taking fresh water out of the L-31E Canal will deprive Biscayne Bay of fresh water that would otherwise flow to the Bay; (2) there will be a resulting reduction in the biological health of the Bay; and (3) the reduction in biological health will be noticed by Tropical Audubon’s members and will materially diminish their recreational enjoyment of the Bay. However, Dr. Lodge, was unable to say what effect FPL’s proposed water use (in two wet seasons) would have on the Bay. The effect could be de minimis. It could be undiscernible to a member of Tropical Audubon who is recreating on or near the Bay. Tropical Audubon failed to prove the proposed water use would have more than a de minimis effect on the environmental resources of Biscayne Bay. Therefore, it failed to prove non- compliance with any District permit requirement applicable to protection of Biscayne Bay and its natural resources. Saline Water Intrusion Section 3.4 of the Applicant’s Handbook requires that a water withdrawal must not cause harmful saline water intrusion. The saline water interface is generally where groundwater with greater than 10,000 milligrams per liter total dissolved solids (“mg/L TDS”) meets groundwater with less than 10,000 mg/L TDS. Because DEP classifies groundwater with less than 10,000 mg/L TDS as G-II groundwater and groundwater with greater than 10,000 mg/L TDS as G-III groundwater, the saline water interface can also be described as the interface between G-II and G-III groundwater. The location of the saltwater interface is affected by many factors, such as rainfall. “Saltwater intrusion” usually describes the human-induced landward movement of the saline water interface that has resulted from drainage structures, fresh water withdrawals, and other activities that have reduced the volume and, therefore, reduced the “push” of fresh groundwater toward the coast. Saltwater intrusion is considered harmful to water resources in large part because of its effect on land uses. Saltwater intrusion prevents or makes significantly more difficult future land uses that typically require withdraw and use of fresh groundwater, such as agriculture. For existing land uses that rely on withdraw of fresh groundwater, saltwater intrusion “contaminates” the water supply and can make the land uses no longer practicable. The hypersaline plume extends two or three miles west of the CCS and continues to move westward. It is pushing the saline water interface, which is now four or five miles west of the CCS, futher west. The saline water interface is moving westward at the rate of 400 to 600 feet per year. The CCS is causing harmful saline water intrusion. The factual dispute in this proceeding is whether the proposed use of water from the L-31E Canal increases the current intrusion problem. The parties also have a legal dispute about the scope of the District’s review regarding saline water intrusion: whether the District’s review is confined to the impacts of the withdrawal, itself, or whether the District must also consider the impacts of the use of the water after the withdrawal (discharging it into the CCS). The criteria in the Applicant’s Handbook focus the District’s review on the effects of a proposed withdrawal. With regard to saline water intrusion, the District evaluates whether the withdrawal will cause lateral or vertical migration of saline water. The District determined that FPL’s withdrawal from the L- 31E Canal would not cause the migration of saline water. That determination was not disputed by Tropical Audubon. Tropical Audubon contends the District must also determine whether FPL’s use of the water--discharging it into the CCS--would cause harmful saline water intrusion by pushing the saline water interface more landward. The District permit reviewer testified that, in determining whether FPL’s proposed project was consistent with the public interest, he considered the expected benefits of lowering salinity and temperature in the CCS, as well as reducing the hypersaline plume and its impacts on saline water intrusion.2/ As explained in the Conclusions of Law, this analyses is required to determine whether FPL’s proposed water use is consistent with the public interest. FPL used a water/salt budget model for the CCS to quantify the volume of water and mass of salt entering and exiting the CCS over time. The water/salt budget model was run for dry and average weather conditions and multiple withdrawal rates. In each scenario, the model results showed that the greater the volume of water pumped into the CCS, the greater the reduction of salinity in the CCS. The District performed groundwater modeling which showed that freshening of the groundwater would occur rapidly in the upper portion of the Biscayne aquifer near the CCS. The model showed no adverse impacts and some slight improvements in water quality in all areas except for one temporary effect at one monitor well. Based on modeling results and monitoring well data, it was the opinion of the District’s principal scientist, Mr. Giddings, that the addition of water from the L-31E Canal would not increase the western movement of the saline interface. FPL’s expert hydrologist, Mr. Burns, agreed. Tropical Audubon’s expert hydrogeologist, Mr. Martin, opined that the addition of L-31E water into the CCS would increase the westward migration of the hypersaline water in the Biscayne Aquifer and the saline water interface. It was his opinion that the addition of freshwater into the CCS would increase the water levels and the “driving head” within the CCS and thereby increase the downward push against the hypersaline plume, pushing it westward at a greater rate. Mr. Martin did not know what the increase in the rate of western movement would be. Mr. Martin conducted no modeling or other analysis to substantiate his opinion about the increase in driving head, and it appeared he did not take into account how the driving head would be affected by reducing the density of the water in the CCS. Reducing the density of the water would offset the effects of raising the water level. Mr. Martin’s opinion that adding water from the L-31E Canal would push the saline water interface westward was also based on his assumption that the fresher water moving downward from the CCS would not mix with the hypersaline water. However, this opinion was not supported by modeling as was the contrary opinions of Mr. Giddings and Mr. Burns. Monitoring data collected during the period in which FPL has added fresher water to the CCS indicates that mixing is occurring and that head differences in the CCS do not appear to affect chloride levels at distance. FPL provided reasonable assurance that the proposed water use would not increase the rate of saline water intrusion. Existing Legal Uses, Offsite Land Uses, and Pollution Tropical Audubon does not contend the withdrawal of water from the L-31E Canal would interfere with existing legal uses of water, adversely affect off-site land uses, or cause pollution. However, similar to its claim regarding harmful saline water intrusion, Tropical Audubon claims the proposed discharge of the water into the CCS would interfere with existing legal uses of water, harm offsite land uses, and cause pollution. These claims are derived from Tropical Audubon’s belief that discharging freshwater into the CCS would increase the rate of saline water intrusion. Because Tropical Audubon failed to prove the proposed water would increase saline water intrusion, there is no need to address the derivative claims. Conflict with the Conditions of Certification Tropical Audubon asserts that the proposed water use is inconsistent with the DEP National Pollution Discharge Elimination System (“NPDES”) permit for the Turkey Point Plant and with the Fifth Supplemental Agreement between FPL and the District. As explained in the Conclusions of Law, it is normally beyond the scope of a permit proceeding to claim the conditions of another permit would be violated. However, because the NPDES permit and the Fifth Supplemental Agreement are incorporated into or addressed in the 2008 Certification Order for Turkey Point, and the PPSA preempts all other environmental permitting associated with an electric power plant, it is relevant in this proceeding to determine whether the proposed water use would conflict with the conditions of certification for the Turkey Point Power Plant. It is also explained in the Conclusions of Law that the Administrative Law Judge’s consideration of potential conflict must be based on a conflict ascertainable from the plain meaning of the Certification Order, NPDES permit, and Fifth Supplemental Agreement. There has been no determination of conflict by the Siting Board or DEP. In fact, DEP has determined there is no conflict between the proposed water use permit and the NPDES permit. The fact that the NPDES permit describes the CCS as a closed-loop system does not create an irreconcilable conflict. The requirement for a closed-loop system was to terminate a system that had surface discharges of heated water to Biscayne Bay and replace it with a system that circulates water through the power plant with no surface discharges to the Bay. The CCS would still be a closed-loop system with the additions of water from the L-31E Canal because it would still have no surface discharges to Biscayne Bay. The fact that the NPDES permit does not mention the discharge of water from the L-31E Canal into the CCS does not create an irreconcilable conflict. The NPDES permit also does not address rainfall inputs to the CCS. The NPDES permit addresses industrial waste inputs. Water from the L-31E Canal, like rainwater, is not a waste input. The fact that the CCS will operate differently with the addition of L-31E water does not create an irreconcilable conflict. The manner in which water from the L-31E Canal would change the operation of the CCS is not different from the way variable rainfall constantly changes the operation of the CCS. The NPDES permit does not specifically prohibit the introduction of other water into the CCS. DEP determined that the addition of L-31E water would not require a modification of the NPDES permit because it would not change the effluent limits or monitoring requirements of the permit. Tropical Audubon asserts that the proposed permit is inconsistent with the Fifth Supplemental Agreement between the District and FPL. It points to a requirement in the agreement to “operate the interceptor ditch system to restrict movement of the water from the cooling water system westward of Levee 31 E adjacent to the cooling water system to those amounts which would occur without the existence of the cooling canal system.” The interceptor ditch is a ditch running along the western border of CCS, which was intended to intercept hypersaline groundwater and prevent it from moving further westward. It has failed to prevent the western movement of hypersaline water. Tropical Audubon did not show the proposed water use would affect the operation of the interceptor ditch. Therefore, Tropical Audubon failed to prove there is an irreconcilable conflict between the proposed water use permit and the Fifth Supplemental Agreement. Conflict with the DEP Administrative Order Tropical Audubon asserts that the proposed permit is inconsistent with an AO issued by DEP in December 2014 to address CCS salinity issues. However, the AO is not yet in effect and is not a part of the 2008 Certification Order. As explained in the Conclusions of Law, FPL’s compliance with the AO cannot be made a condition of compliance with the proposed water use permit. Furthermore, Tropical Audubon failed to demonstrate there is a conflict between the AO and the proposed water use. Summary In summary, FPL provided reasonable assurance that the proposed water use would comply with all applicable permit criteria. Tropical Audubon did not meet its burden to prove otherwise.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law it is RECOMMENDED that South Florida Water Management District issue a final order that grants the proposed Individual Water Use Permit (No. 13-05856-W) to Florida Power & Light Company. DONE AND ENTERED this 31st day of December, 2015, 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 December, 2015.
Findings Of Fact By application filed on September 9, 1980, Respondent/Applicant, John H. Land Builders, Inc., sought a permit from Respondent, Department of Environmental Regulation (DER), to conduct dredge and fill activities in an approximate one acre area located in the southeast corner of a proposed housing development in Section 10, Township 29 South, Range 19 East, in Hillsborough County, Florida. A copy of this permit application may be found as DER Composite Exhibit B. Specifically, Land sought to excavate 4,100 cubic yards of material (muck) and to backfill the area with 14,400 cubic yards of granular material from adjacent uplands to allow for development of a street and building lots in an unnamed wetland. A permit from DER is required because the project involves a wetland that is contiguous with a ditch that connects to the Palm River, all of which constitute waters of the State that are subject to dredge and fill permitting requirements. The plans have been reviewed by other state and local authorities in the Hillsborough County area, and no adverse comments have been received. After the installation is completed, the elevation of the land will be raised, and will permit five homesites to be built on the land as well as the construction of an access road to the property from an adjacent street. The installation in question is but a small part of a larger proposed housing development known as Timberlake Subdivision that will ultimately involve more than 300 homesites. However, no further dredge and fill activities under DER jurisdiction will be undertaken. The proposal of Respondent/Applicant was received by the Department and certain timely additional requests were made from the Department to the Applicant to provide information necessary to evaluate the request for permit. Applicant subsequently furnished the required information, and it may be found in DER Exhibit C. The Department performed a field inspection and review of the dredge and fill site, including the surrounding areas, to assess the impact of water quality caused by proposed dredging and filling activities in wetlands areas. It concluded that the Applicant had affirmatively provided reasonable assurance to the Department that the short-term and long-term effects of the activity would not result in violations of the water quality criteria, standards, requirements and provisions of Chapter 17-3, Florida Administrative Code. A copy of the permit application appraisal may be found in DER Exhibit A. On January 21, 1981, DER issued its Intent to Issue a dredge and fill/water quality certification with certain conditions therein, including the requirement that future development be dependent upon separate stormwater review by the Department (DER Exhibit D). On October 20, 1980, Applicant filed a Notice of Stormwater Discharge with the Department's Southwest District Office in Tampa (DER Composite Exhibits B & F). Thereafter, the Department conducted a field inspection and review of the proposed housing development and surrounding areas to determine whether the proposed stormwater discharge would have a significant impact on water quality. Based upon the results of that inspection, which concluded that the proposed discharge would not have a significant impact on the waters of this State, the Department issued Applicant a stormwater exemption on November 7, 1980. The project site is located in an unnamed wetlands area. It is weedy and has a dense cover of primrose willow (Ludwigia peruviana), willow (Salix caroliniana), cattail (Typha sp.), red maple (Ace rubrum) and is overgrown with grapes vines (Vitus rotendifolia). It lies just to the north of a series of fish farms owned by Petitioner, Penisular Fisheries, Inc. Other commercial industries and single family dwellings are found south of the proposed activities. To the west and northwest lie marshlands, two old borrow pits, and Interstate Highway 4. Water runoff from the dredge and fill area will flow to the storm drainage system in the proposed street, and from there to a designated retention pond. Because there will be minor contaminants in the runoff, the water will be retained for treatment for a period of five days, which exceeds the 100 hour retention period required by DER. After treatment, the runoff will flow into a well-defined county drainage ditch west of 58th Street, travel down the ditch which lies adjacent to the fish ponds, and then meander into the existing marshland. Water runoff from the remainder of the project (excluding the dredge and fill area) will drain into the two existing borrow pit lakes which lie close to Interstate Highway 4. The designated retention pond will be located west of the project and has a controlled spill-off elevation. It will provide sufficient treatment to and cleaning of the water to insure that no violation of water quality standards will occur. A stormwater system to be constructed by Applicant will actually reduce the volume of water runoff now occurring. Reasonable assurances have been given that the short-term and long-term effects of the proposed activity will not result in violations of the water quality criteria, standards, requirements and provisions of the Florida Administrative Code. Based upon Use location of the point of discharge of Land's proposed stormwater discharge, the volume and frequency of discharge for which the proposed facilities are designed, and the anticipated constituents of discharge, the proposal will not have a significant impact on the water quality of the waters of this State. Accordingly, the exemption from stormwater licensing requirements was properly issued by the Department. Water quality violations which were alleged to have existed in a ditch on property adjoining the properties of Land and Petitioners were the subject of a notice of violation issued to the owners of that property. However, no notice of violation was ever issued to Land. Further, the ditch is not a part of the installation proposed by Applicant for issuance of the dredge and fill permit. Petitioners' concern is that Applicant has not given reasonable assurance that water quality standards would not be violated by the stormwater discharge and that downstream waters might be contaminated by urban runoff from the project. In reaching that conclusion, Petitioners' expert relied on a review of certain materials submitted to him by Petitioner's counsel. He did not visit the project site, nor had he reviewed drainage plans or construction drawings for drainage improvements contemplated by the notice of stormwater discharge filed by Land.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that Respondent Department of Environmental Regulation grant the requested dredge and fill permit/water quality certification to Respondent/Applicant John H. Land Builders, Inc. It is further RECOMMENDED that the Respondent Department of Environmental Regulation enter a final order confirming the stormwater exemption issued by the Department to Respondent/Applicant on November 7, 1980. DONE and ENTERED this 27th day of April, 1981, in Tallahassee, Florida. DONALD R. ALEXANDER 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 27th day of April, 1981.
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
Findings Of Fact At all times pertinent to the issues herein, the Southwest Florida Water Management District had permitting authority for the issuance of consumptive use permits in the area in which Respondent, El Jobean, proposes to sink its irrigation well. On December 12, 1988, El Jobean submitted a consumptive use permit application to sink a new well for the purpose of irrigation of a golf course to be developed on the property it owns in Sarasota County. The well is to be located in the NE 1/4 of the NE 1/4 of Section 32, Township 365, Range 20R, in Sarasota County, Florida near the southern boundary of an irregularly shaped piece of property consisting of approximately 855 acres, owned by the applicant, which extends over Sections 28, 29, 32 and 33, Township 365, Range 20E. Respondent proposed to sink a 10 inch diameter well to a total depth of approximately 900 feet with casing in the well now to extend down to 300 feet, with a pump capacity of 1,000 GPM. The golf course to be irrigated is to encompass approximately 190 acres. The applicant requested authority to withdraw an average of 600,000 GPD with a limitation of a maximum of 1,440,000 GPD. The application was properly staffed by the District. In the staff report on the application, the average daily use limitation was expanded to 707,000 GPD; consumptive use was raised from 0 to 139,000 GPD; and maximum daily consumption was reduced from 1,440,000 GPD to 1,240,000 GPD. These changes were due to correction of arithmetic errors in the application and were accepted by the applicant. The ultimate recommendation of the staff was for approval of a 6 year permit, subject to certain conditions outlined in subparagraph I of the staff report. These special conditions require the provision and use of flow measuring devices to maintain an accurate record of the water withdrawn; the maintenance of flow records and the providing of periodic reports to the District; the collection and analyzing of water quality of samples taken from the well to measure the appropriate parameters for chlorides, sulfates, and total dissolved solids; the reporting of the results of these samplings and a description of the sampling and analytical methodologies employed; and a requirement that the permittee investigate the feasibility of supplementing and/or substituting drawn water with treated sewage affluent. After the staff report was submitted, proper notice of the District's intent to issue the permit was published. Based on that notice, protests were filed both by Miakka and Mr. Bishop. The area in question is located within the Manasota Basin which, itself, is located within the Southern West-Central Florida Ground Water Basin, (SWCFGWB), which encompasses all of Pasco, Hillsborough, Manatee, Sarasota, Polk, Hardee, and DeSoto Counties, and parts of Lee, Glades, Charlotte and Highlands Counties. The SWCFGWB sits atop several aquifers which include the Floridian Aquifer, two Intermediate aquifers, and the Surficial Aquifer. The Floridian Aquifer is the deepest and the Surficial Aquifer is on the top. The Miakka Community Club is a Florida corporation made up of residents of the pertinent area whose primary function is to preserve and conserve the rural nature and spirit of the Northeast section of Sarasota County. The club performs this function through educational programs, community activities, and participation in the legislative process. Miakka urges denial of the permit sought by El Jobean based on its membership's belief that the property owners whose property is in the immediate vicinity of the proposed well will be adversely affected if El Jobean is permitted to sink its well and withdraw water from it. The club membership believes that approval of El Jobean's well will result in contamination of existing personal water wells due to excessive use by El Jobean; potential contamination of Sarasota County's future drinking water sources which include the capital Ringling,/MacArthur tract and the Myakka River; reduction of property values; and destruction of personal resources. Petitioner also urges that since the proposed golf course will be a part of a private club for the use of members only, in which membership will be limited, there is no public benefit derived from the approval of and sinking of the well in question. Petitioner also contends that during the periods of severe water shortage as are being currently experienced, permission to sink a well of this size to draw water in of the magnitude expressed in the application, would be counterproductive and detrimental to the interests of the other property owners in the area. In support of its claim, Petitioner presented the testimony of two homeowners from the area, Mr. Richardson and Ms. Mustico. Mr. Richardson, whose well is 183 feet deep, has had several problems with his well even without the instant drilling. In 1974, and subsequent thereto, he has had to go deeper with a suction pipe because the water has dropped below the level of the tail pipe. Ms. Mustico's 160 foot deep well, with 80 feet of casing, is used to supply water for the home. She also has other wells for watering her lawn and for livestock, one of which goes down 500 feet. She is concerned that the well proposed by El Jobean will adversely impact her ability to draw water from her wells because, she believes, the water level from which her water is drawn will drop. In the past, her primary well has gone dry and the wells of several neighbors have gone dry as well. Through maps and other documentation taken from the Ground Water Resource Availability Inventory for Sarasota County, Florida, prepared by the District in March 1988, Petitioner has established that areas of significant groundwater withdrawal within the SWCFGWB occur in Hillsborough, Manatee, Polk, Hardee, DeSoto and Highlands Counties. With the exception of an extremely small portion of Sarasota County located contiguous to Manatee County, there appear to be no areas of major ground water withdrawal currently existing in Sarasota County. The majority of the major municipal well fields within the pertinent basin that are located within Sarasota County, extend down to the Intermediate and Surficial Aquifers with only 3 extending through the lower Intermediate into the Floridan Aquifer. These include the Verna well field located in the northeast corner of Sarasota County where it abuts Manatee County; the Sarasota County well field located in northwest Sarasota County near the Manatee County line; and the Sorrento Utility, Inc., well field which is located near the Gulf Coast, approximately two-fifths of the way down between the Manatee and Charlotte County lines. With the exception of the Verna well field, all the municipal well fields in Sarasota County appear to be reverse osmosis systems and as of 1987, there were 28 reverse osmosis systems located within Sarasota County. Most are relatively small in their output measured in millions of gallons per day. With the exception of 3 public supply wells, 2 of which are permitted an average annual pumpage greater than 100,000 GPD and 1 of which is permitted less, all of the permitted public supply well fields in Sarasota County are located west and south of 1-75 as it extends from the Manatee County line in the north to the Charlotte County line in the south. The El Jobean well would be located east of the line, in that area occupied by the 3 public supply wells. Generalized recharge areas for the upper Floridan Aquifer in the groundwater basin in issue here have been categorized from "high", with a rate of more than 10 inches per year, to "Generally none", with a recharge rate at 0. In 1980, the high recharge rates existed in the north-central part of Pasco, the eastern part of Polk County, and the northeastern part of Highlands County. Sarasota County is in an area wherein the recharge rate was either very low or generally none. In September 1986, the high recharge rate was found in a very small area of northeastern Pasco County, and small areas in both Polk and Highlands Counties. Sarasota County, for the most part, was classified as having no recharge. In May 1987, the high recharge rates were, again, a small area in eastern Pasco County, a small area in northeastern Hillsborough County, a small area in southeastern Polk and northwestern Highlands Counties, and a minuscule area in central Pinellas County. Again, Sarasota County had a recharge rate of 0. Generalized estimated, calibrated, model-derived recharge and discharge values for the upper Floridan Aquifer in the ground water basin in issue here, as they pertain to Sarasota County, reflect positive 2 recharge to negative 1 discharge inches per year. Historically, however, the northeast portion of Sarasota County, where the El Jobean well in question would be located, evaluated by various individuals or agencies periodically from 1980 through 1988, reflects a recharge of anywhere from 0 to 2 inches per year. None of this documentation was supplemented, however, by direct testimony by an individual knowledgeable in this area, and Petitioner's main thrust appears to be an unsubstantiated fear that the sinking of El Jobean's well will have a negative impact on its membership's wells. Admittedly, the residents in the area in question all rely on private wells for the majority of their water supply, other than through the catchment of rainwater, which is insignificant. It was also established that the area has been undergoing a severe water shortage and that conservation measures have been mandated. On the other hand, El Jobean presented the testimony of a hydrogeologist, Mr. Moresi, who has extensive experience with the modeling process used to determine water consumption and recharge in southwest Florida and Sarasota County. The aquifer system in Florida is made up of water bearing limestone layers below the surficial sand base. This aquifer system underlays the various zones throughout the state and reflects a surficial aquifer extending from ground level down approximately 70 feet to a confining bed which separates it from the lower strata. This top confining bed is approximately 20 feet thick, and below it is the Tamiami-Upper Hawthorn Aquifer, which is between 100 and 200 feet deep and which rests on another confining bed somewhat thicker than the upper one. Below the second confining bed is the Lower Hawthorn-Upper Tampa Aquifer which extends approximately from the 250 foot to the 450 foot level at the Manatee County line, and between the 320 foot and the 710 foot level at the Charlotte County line. Another confining bed lays between this aquifer and the Floridan Aquifer which starts at the 500 foot level and goes down well below the 900 foot level in the north and extends from the 730 foot level down in the south. The confining bed below the surficial aquifer is made up of a clay material which retards the movement of water from one aquifer to another. The surficial aquifer is porous and saturated with water from the water table down. Since the confining beds are far less porous than the aquifers they separate, water moves much more slowly through them. The lower aquifers are made up of limestone and are also porous and contain water. The Tamiami-Upper Hawthorn formation consists of limestone and clay, but is water bearing. The Lower Hawthorn-Upper Tampa formation is similar and both make up the intermediate aquifer below which is the lower confining bed followed by the Floridan aquifer. Respondent's well would be cased in steel down to an area approximately 100 feet into the Floridan Aquifer, through the Lower Hawthorn- Upper Tampa Aquifer and through the lower confining bed. Since the well would be cased to well below the lower confining bed, water existing in the upper aquifers, would be prevented from being drawn down by operation, of the Respondent's well either directly or by settling down to replace the water drawn out. Generally, the deeper a well is drilled, the worse the quality of the water, and it becomes less potable. The Floridan Aquifer produces far more copious quantities of water than do the intermediate aquifers. However, since it is cheaper to drill to the intermediate zones as the wells need not be so deep, and since the water there is better, most domestic wells go no deeper than these aquifers. They go down approximately 150 to 180 feet. The pressure in each level is separate from and different from that in the other aquifers. The upper intermediate system generally has a lower pressure than the lower intermediate system. As a result, water from the lower intermediate system tends to leak upward toward the upper intermediate aquifer, rather than the reverse. In addition, a recent survey tends to show that the Floridan aquifer also tends to leak upward into the lower intermediate level. It also shows that leakage through the confining beds amounts to .002 GPD per cubic foot of aquifer. Petitioner claims that since the lower water is of lesser quality, and since withdrawal of water from the upper layers would promote leakage upward, thereby adding lower grade water to the better grade upper water, there could be a diminishment in upper level water quality as a result of water being drawn from the upper levels. However, according to Mr. Moresi, the .002 figure is so small it would result in an infinitesimally small drawdown of water level from the upper intermediate level aquifer and the potential for compromise of the water quality therein is remote. Clearly, this is not the result of drawing water from the Floridan Aquifer as the well in question would do but more the result of the residential wells extending into the upper levels. The District ran a model for the proposed El Jobean well (a Jacob- Hantush model) which showed that drawdown at the wellhead would be just over 2 feet. This means that use of the Respondent's well would reduce the water level in the Floridan Aquifer at the well head by 2 feet. However, this drawdown is shown to decrease rapidly out to where, at distance, it is almost immeasurable. In fact, drawdown of the Floridan Aquifer at 24,000 feet from the well head (approximately 4.5 miles) would be .1 feet, slightly or 1 inch. The .1 foot drawdown relates to the lowest (Floridan) aquifer and the resultant drawdown in the upper intermediate aquifer, into which the majority of residential wells are sunk, would be relatively undetectable. Since the Petitioner's wells, at their deepest, go only into the upper intermediate level, and would be separated by 2 confining beds from the Floridan Aquifer, the impact on the domestic wells at 2 miles from the El Jobean wellhead would be immeasurable. Even at 1 mile, there would be minimal drawdown in the Floridan Aquifer and almost none in the upper intermediate aquifer. The potentiometric surface of the intermediate layer would not be adversely affected, nor would that of the surface water. Recognizing the potential for saltwater intrusion which occurs all along the coast, based on his studies, Mr. Moresi concluded that the well in question here would not induce significant saltwater intrusion. He concluded as well that the permit is consistent with the requirements of the District rule; that the amount permitted for the use of irrigation of the golf course is reasonable, assuming a golf course is a reasonable and appropriate use of water; that the withdrawal by the well in issue would not have an adverse impact on users outside the property on which the well was located; that it would not impact existing users; that there is no other water available for the purpose intended; that the water taken from the Floridan Aquifer under this permit may be potable but is of poor quality; and that the applicant met rule standards. Mr. Moresi also discussed the possible cumulative impact of the proposed well when operated along with the currently existing wells. If there are other drawdowns from the same cone into which El Jobean's well would be sunk, the withdrawals would be cumulative. However, as best he can determine, the only other significant drawdown from the cone pertinent here is that of the Verna well field. In his opinion, that well field's drawdown, which is from the northeast, would not be significant even when considered with the El Jobean well. Mr. Moresi was also satisfied that while the confining bed separating the surficial aquifer from the next lower level might be disturbed, the deeper one goes, the less likely there is to be mixing of aquifers. The only instance where water could move from one level to another as a result of the well is where there is no casing on the bore hole. In the instant case, plans call for, and permit conditions require, the well to be cased to below the lowest confining bed. Consequently, there should be no upward or downward flow of water as a result of the bore. Mr. Tyson, who worked on the evaluation of El Jobean's application for permit, was of the opinion that the amount of water requested by El Jobean in its application was appropriate for a golf course. This does not mean that a golf course is an appropriate use of the property. The special conditions imposed on the granting of the permit by the District are designed to reduce any impact possibly caused by the permitted activity. The Jacob-Hantush model used in analysis of the instant application is considered to be a conservative tool and showed minimal drawdown at all property boundaries. The use of other models in this case was considered neither necessary nor appropriate. Mr. Tyson considers the proposed permit a reasonable beneficial use as defined in the Florida Administrative Code and statutes because it proposes use of reasonable amounts of water and the models indicate no unfavorable impact. Based on the past practice of permitting golf courses with subdivisions, he feels the proposed use is reasonable. He concludes, therefore, that it is in the public interest to grant this permit. In his opinion, the permit will not interfere with legal existing uses and meets all statute and rule requirements. Considering the evidence as a whole, it is found that petitioner has presented insufficient evidence to support its claim that approval and operation of El Jobean's well as proposed would have an adverse impact on the property owners. It's concerns are no doubt sincere, but these concerns are not sufficiently confirmed by evidence of record. At the hearing, the parties stipulated that if the permit were granted, it would be modified by the addition of two conditions: The proposed well shall be constructed with a minimum of 600 feet of casing so as to prevent the unauthorized interchange of water between water bearing zones in order to prevent the deterioration of water quality in the shallower zones. If the well cannot be properly completed to prevent such an unauthorized interchange of water, the well shall be abandoned and plugged in accordance with Rule 17-21.10(2)(c), F.A.C.. Upon completion of the well, a copy of the well construction completion report shall be sent to the District. The permittee shall line the bottom of the pond that will be used as the irrigation source, with clay to a thickness equal to 1.5 feet.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that the Southwest Florida Water Management District enter a Final Order issuing Consumptive Use Permit Number 209458, as modified by the conditions stipulated to at the hearing held herein on June 7, 1989, and outlined in Finding of Fact Number 27 herein, to El Jobean Philharmonic Group, Inc. RECOMMENDED this 9th day of August, 1989 at Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of Division of Administrative Hearings this 9th day of August, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 88-1176 The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. For the Petitioner: Not a Finding of Fact but a statement of the ultimate issue of fact. Accepted and incorporated herein. 3-6. Accepted and incorporated herein. 7-12. Accepted and incorporated herein. Accepted as indicating original conditions. The parties stipulated to additional conditions at the hearing. Accepted. 15 & 16. Accepted and incorporated herein. 17-33. Accepted and incorporated herein as pertinent. 34 & 35. Accepted. 36 & 37. Accepted. 38 & 39. Redundant. 40-43. Accepted. 44. Accepted. 45-51. Accepted. 52 & 53. Accepted. 54-56. Accepted. 57 & 58. Accepted and incorporated herein. 59-66. Accepted. 67-75. Accepted and incorporated herein. 76 & 77. Accepted and incorporated herein. 78. Accepted. 79-84. Accepted. Accepted and incorporated herein. Rejected. 87 & 88. Accepted. 89-93. Accepted and incorporated herein. Accepted. Accepted in the natural source sense suggested by Petitioner. 96-99. Accepted and incorporated herein. 100 & 101. Accepted and incorporated herein. 102-105. Accepted and incorporated herein. 106. Accepted. 107 & 108. Accepted. 109 & 110. Accepted. For the Respondents: 1 & 2. Stipulation between the parties accepted and incorporated herein. 3-6. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence except for the second sentence which is incorporated herein as a Finding of Fact. Not a Finding of Fact but a comment on the evidence. 9-11. Accepted and incorporated herein. 12. Accepted. 13-16. Accepted and incorporated herein. 17. Accepted and incorporated herein. 18 & 19. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. 22-26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29. Accepted. 30-32. Accepted and incorporated herein. 33-40. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Not a Finding of Fact but a Conclusion of Law. COPIES FURNISHED: Becky Ayech Personal Representative Miakka Community Club 421 Verna Rd. Sarasota, Florida 34240 Douglas Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Edward B. Helvenston, Esquire Assistant General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609 6899
The Issue The issue 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.
