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ALAN R. BEHRENS vs CONSOLIDATED MINERALS, INC., AND SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 92-000953 (1992)
Division of Administrative Hearings, Florida Filed:Arcadia, Florida Feb. 12, 1992 Number: 92-000953 Latest Update: Dec. 07, 1994

Findings Of Fact THE PARTIES CMI is a Florida corporation authorized to do business in Florida. CMI owns a mine site as is depicted in the permit application, which mine site is known as "Pine Level". Alan R. Behrens owns residential property approximately two miles from Pine Level, which abuts Horse Creek. He maintains an individual well for domestic and other purposes, and is a substantially affected person under the statute. Charlotte County is a government entity and a political subdivision of the State of Florida, and is a substantially affected person under the statute. The City of North Port is an incorporated municipality of the State of Florida, and is a substantially affected person under the statute. The Environmental Confederation (ECOSWF), a citizens group, is a substantially affected person under the statute. The District is the agency with the responsibility for reviewing and ruling upon CMI's water use permit application. APPLICATION AND PROCESS CMI proposes to operate a phosphate mine facility at "Pine Level" ("site"). The site is located approximately seven miles west of Arcadia, DeSoto County, Florida. The mine reserves at the site are approximately 17,700 acres. 9,000 to 10,000 acres are projected for mining. In 1978, Consumptive Use Permit No. 200103, was issued and in 1986, the current owners purchased the corporation which held the permit, and changed the name of the corporation to CMI. The Industrial Water Use Permit has not been used since it was issued to a prior owner of the site, and provided for average daily withdrawals of 13.6 mgd from wells. In 1984, this permit was renewed and modified to provide for average daily withdrawals of 12.8 mgd from deep wells. The groundwater withdrawals currently sought by CMI is 6.9 million gallons per day ("mgd") average daily withdrawal, which totals include 5.1 mgd from deep wells for use in the amine flotation process and 1.7 mgd for sealing the matrix slurry pumps. This reduction to 6.9 mgd in permitted withdrawals is a significant reduction. In addition, the proposed permit allows 3.7 mgd to be withdrawn from the surficial aquifer by dewatering mine cuts. In November, 1990, CMI submitted an application for renewal. In November 1991, CMI submitted to the District a revised Water Use Application No. 200103.02 ("application") to renew and modify the existing water use permit. The District requested more information, and CMI provided additional information and supplemental responses to aid in the review and evaluation of the application. The District prepared and submitted a Notice of Intent to Issue Permit and the District staff has prepared a "draft" Permit No. 200103.02 authorizing the withdrawal of the quantities requested in the application with certain conditions. In addition to renewal and modification of the water use permit, which is the subject of this proceeding, CMI will be required to participate in numerous regulatory reviews and permitting procedures (i.e. a development of regional impact evaluation, a federal environmental impact statement, federal approvals under the Clean Water Act [including a national pollutant discharge elimination system ("NPDES") permit], and a conceptual reclamation plan review) before CMI may commence mining, and consequently, begin any withdrawal of water. The mining process will utilize large walking draglines to excavate over burden and stack it beside the active mining area for land reclamation. The ore material called "matrix" will be dug up by the draglines, placed into an earthen pit where it will be slurried with a high pressure water jet. A pump will pick up this slurried matrix material, pump it back to the processing plant where it will first go through various separation devices, including screens and cyclones. The course material termed "pebble" will be separated and parts of that will be directly saleable as a product. The bulk of the phosphate product is contained in intermediate-sized material called concentrate feed. The concentrate feed consists of ore and sand. The ore is separated from the sand in a process called "flotation". The flotation process is a two stage process that ends up separating the tailings sand, which can then go back to the sand-clay flocculation and mixing units, and be pumped out ultimately for land reclamation back in the mine-out areas. The phosphate product which is called "wet rock", is placed in storage bins where it can drain, and be loaded onto rail cars for shipment. The "amine flotation process" is the second stage of flotation where sand and phosphates are separated. This process requires clean water for the amine flotation phase, because any amount of contaminants, including organic reagents, will adversely affect the process. Any mineral particles must be removed so that the amine may attach itself to the phosphate. Any contaminants will destroy or significantly and adversely affect not only the phosphate recovery, but the entire flotation process. Deep well water is requested for use in the amine flotation process because it is clean. All phosphate mines in Florida currently rely on deep well water. 5.2 mgd is the minimum amount of "clean" water needed to assure efficient processing of the amine flotation process of the mine beneficiation plant. Deep well withdrawals are also commonly used for the purpose of sealing or protecting the packing of pumps at various points in the mine system in order to avoid damage to the equipment. These wells are often referred to as "sealing water wells". The Pine Level mine will require 1.7 mgd for this purpose. Water for the sealing water wells must be clean and clear in order to effectively seal pumps for leaks. The Pine Level project will provide 400-500 construction jobs during the construction period. It will provide approximately 200 full-time jobs with an annual payroll of about five million dollars once it is in operation. It will result in about one thousand additional jobs providing services to the development. It will pay in excess of one million dollars a year to DeSoto County in ad valorem taxes. TECHNICAL CRITERIA The water use is a reasonable and beneficial use. 5.2 mgd groundwater withdrawal is "necessary to fill a certain reasonable demand." The technical criteria relating to water level or rates of flow impacts set forth in Rule 40D-2.301(1)(d), Florida Administrative Code, are not applicable in this proceeding because the District has not established any regulatory levels or rates of flow for the area encompassed by the application. In addition, this presumption only addresses surface water withdrawals. Phosphate mining is a beneficial activity and is consistent with the public interest. There is no significant risk of salt water intrusion. The water use withdrawal will not degrade the water quality in the aquifer by causing any contamination plume to spread. There have been no contaminant plumes identified on site. GROUNDWATER IMPACTS There is sufficient ground water at the site of a suitable quality and quantity to support the proposed phosphate mining and beneficiation activities. The local hydrogeology at the site consists of an upper layer known as the surficial aquifer. Rain penetrates the surficial aquifer to flow vertically to the water table. The water that is not consumed by vegetation at this layer will flow either to a nearby stream channel or will leak down through a semi- confining layer. The water continues to seep vertically into the lower underlying limestone aquifers. There are three limestone water-bearing layers: the intermediate, the Suwannee or Upper Floridan, and the Avon Park or Lower Floridan aquifers, respectively. The intermediate and the underlying Suwannee aquifer are separated by another semi-confining layer. Likewise, the Avon Park aquifer and the Suwannee aquifer are separated by another semi-confining layer. At the site, wells in the intermediate aquifer will draw water to seal the bearings on the matrix slurry pumps. There will be one deep well in the Suwannee and one deep well in the Avon Park to draw for the beneficiation plant. The groundwater modeling performed by CMI simulated the four aquifers, that is, the surficial aquifer and each of the three limestone aquifers. An Aquifer Performance Test ("APT") was performed at the site. The data generated from the APT was used to calculate various aquifer parameters, for example, transmissivity, storage coefficient, and leakiness. This information was then used in setting up the groundwater flow model that ultimately was incorporated into the application. During the District staff's review of the application, the deep well withdrawal quantities requested by CMI were compared with approximately 6 other phosphate mines of comparable size, acreage, and type of operation. As a result of this comparison, the staff found CMI's requested use to be less than the other six phosphate mines. The use of recycled water in the amine flotation process in place of deep well water in the past by CMI has proven unsuccessful because a constant temperature and a constant ph level could not be maintained with recycled water, and recycled water contains traces of fatty acids and oils, which also negatively affect the amine flotation process. C.F. Industries, Inc., has been operating a phosphate mine in Hardee County, Florida, since 1978. C.F. Industries, Inc., has since 1983 at the Hardee County mine, successfully substituted recirculation water for deep well water for operation of the amine flotation circuit on a routine basis. C.F. Industries, Inc., presently plans to employ substitution of some recirculation water for deep well water in a new yet-to-be permitted mine. C.F. Industries, Inc., at its existing Hardee County mine requires use of deep well water for start-up purposes to "charge" the system. C.F. Industries, Inc., at its existing mine, uses deep well water to respond to abnormal operational conditions, including excessive rainfall events, when the quality of the normal recirculation water is not suitable for substitution of deep well water. Neither CMI, nor District staff was aware prior to hearing, that the C.F. mine was successfully substituting recycled water for deep well water in the amine flotation process. At the time of making the representations to the District about necessary water quality requirements of the flotation process, CMI had a study, entitled, Amine Water Evaluation, Pine Level Project, July 27, 1984, ("Pilot Plant Study"), which concluded that deep well pumping and discharge could be reduced by use of water drawn from mine cuts. The Pilot Plant study was site specific to CMI's proposed phosphate mine. The Pilot Plant study bench tests were verified in the same pilot plant facility CMI uses to verify the grade of ore on the Pine Level Site. The Pilot Plant study or its results were known to CMI officials or experts involved in the permit application at issue in this case. CMI did not inform District staff of the existence or conclusions of the Pilot Plant study. The Pilot Plant study indicates that CMI could reduce its water usage by substituting water from mine cuts for deep well water. CMI did no studies to determine if the substitution of mine cut water for deep well water, as suggested by the Pilot Plant Study, was feasible to implement. SURFACE WATER IMPACTS The phosphate ore (matrix), is extracted by an excavation machine called a "dragline", which opens mining cuts of approximately 32 to 35 feet in depth, 330 feet wide, and up to 4,000 feet long. Seepage occurs into the mine cuts from the water table, and must be pumped out in order to see and extract the matrix. This dewatering is also necessary to protect the draglines against slope stability problems. Water pumped out of the mining cuts is introduced into the mine water recirculation system which is operated for purposes of collecting and recycling water within the mine complex. The matrix that is extracted from the mining cut is placed in a shallow excavation near the cut, and is converted to a slurry and, thereafter, transported hydraulically to the mine processing (or "beneficiation") plant. The beneficiation plant uses considerable quantities of water, utilizing supplies from within the mine system (i.e. surface water) and water from deep wells. Sand tailings and sand and clay mixture are by-products of the mining process. Recycled water is used to transport waste clay and sand from the plant to the disposal and reclamation areas. Reclamation takes 1-2 years for areas reclaimed with sand tailings and 5-6 years for areas reclaimed with a sand-clay mixture. Groundwater that is used in the processing plant is recycled. Water within the mine is recycled a number of times, and CMI's proposal calls for 90 percent of the total mine demand to be satisfied by this recirculation system and approximately 96 percent of the water used is recyclable water. DEWATERING AND WATER BALANCE CMI's mine pit dewatering activities result in the withdrawal of water from the surficial aquifer. A "water balance" demonstrates that requested quantities relate to reasonable mining, processing, and dewatering needs. The "water balance" for the mining operation evidences a balance between sources and uses/losses. The sources of water in the CMI water balance that input to the mining operation include groundwater from wells (6.9 mgd), mine cut dewatering or water table drainage (3.7 mgd), and collected rainfall (3.1 mgd). Uses and losses associated with the mining operation include water retained in clays (6.7 mgd), water shipped with final product (.7 mgd), evapotranspiration and evaporation (3.0 mgd), water used for agricultural irrigation (5.0 mgd), and water seeping from the Mine Water Surge Area ("MWSA") (1.2 mgd). The water balance matrix moisture component of 2.9 mgd is not a withdrawal of water for water use permitting purposes. The District's modeling of the impacts resulting from mine cut dewatering resulted in a finding of 2.34 MGD as opposed to the 3.7 mgd derived by CMI. For calculation purposes, rainfall is collected at the rate of 3,974 gallons per acre per day. CMI calculates that it will collect 3.1 mgd of rainfall, and use it in its recirculation system. The 3.1 mgd calculation is based on the amount of rain that will fall on 600 acres of mine water surge area, 80 acres of plant site, and two 50 acre mine cuts. CMI plans to mine 450 acres each year at the Pine Level Site over a period of 22 years. Runoff over disturbed areas on the CMI mine site must be captured, and will become part of the recirculation system. Assuming only one year of disturbed area during the permit term, CMI has failed to account for nearly 1.8 mgd in its water balance (450 acres x 3,974 gallons/acre/day). CMI plans to pump any rainfall collected from all disturbed areas to the mine water surge area (MWSA). CMI has not included any acres of disturbed area in its calculations of the amount of rainfall it will collect for the current permit. CMI has not submitted a mine plan. Without a mine plan, the number of disturbed acres cannot be determined. Because CMI's water balance does not include rainfall collected over disturbed areas, the water balance is incorrect. The rainfall collected from the disturbed areas will increase the amount of water that CMI will need to discharge or use for agricultural purposes. Excavation of the Mine Water Surge Area will cause dewatering of the surficial aquifer. No analysis was done of how much dewatering of the surficial aquifer will occur as a result of the excavation of the MWSA, or of the potential impacts to wetlands as a result of the dewatering activities. The District's one foot draw down presumption applies to dewatering as well as to groundwater pumping. The proposed dewatering setback from wetlands was set at 660 feet. The 660 foot setback distance is in lieu of mitigation if CMI wishes to mine within the setback distance, it will be required to implement mitigation procedures. Dewatering draw downs in the surficial aquifer as great as six and one-half to seven feet could occur on the CMI site at 660 feet from a mine cut under dry weather conditions. At 660 feet, the predicted draw down is nearly one and one-half feet using a mine pit depth of 26 feet, based on a three foot water table and a 29 foot average mine cut depth for the area expected to be mined during the term of the permit. Actual mine cut depths during the term of the permit would be as deep as thirty-seven feet which result in a draw down in the aquifer that is greater than one and on-half feet. Combining the dewatering calculations with the surficial aquifer draw downs resulting from CMI's planned well pumping from the intermediate and Floridian aquifers result in greater than predicted draw downs. CMI's water balance did not account for changes in water needs due to variability of the ore body. WATER QUALITY CMI has not demonstrated that the water quantities requested for the operation of the phosphate mine and beneficiation plant, and land reclamation and water handling will utilize the lowest water quality to the greatest extent practicable. Nevertheless, the Pine Level mine is innovative in comparison to other operating mines. It proposes to reduce its groundwater requirement by increasing the amount of recycled water used in the amine flotation process; employ an innovative sand/clay mixing technique for land reclamation, thus eliminating the need for conventional large, above-ground day settling areas or slime ponds; and use surplus water for irrigation of agricultural crops or pasture. CMI plans to mine the Pine Level Site for a period of 22 years. For phosphate mines, neither DNR, nor SWFWMD analyze impacts with respect to surface water during the mining process. For phosphate mines, no state agency looks at off-site surface water impacts from the standpoint of draw downs, with the possible exception of cities and counties. The District has not required CMI to submit an application for the management and storage of surface waters permit, since the District staff believes that phosphate mines are exempt from obtaining any MSSW permit from the District. A gap exists in the regulatory scheme for phosphate mines with respect to the reduction of surface water flows during the mining process if SWFWMD exempts phosphate mines from obtaining an MSSW permit. INTERFERENCE WITH EXISTING LEGAL USERS The City of North Port is an existing legal user of water. The City of North Port has a public water supply facility which draws its water from the Big Slough. The Big Slough normally gets a portion of its flow from high quality water in the surficial aquifer. CMI's proposed Pine Level phosphate mine is located in the watersheds which feed the Big Slough and the Peace River. In the initial years of the mine, virtually all of the collected rainfall will be diverted from the Big Slough watershed. No analysis has been done to see how dewatering might affect the City of North Port. Any significant reduction in flow to the City of North Port's facility during the low flow season will interfere with North Ports existing legal use of water. Diversion of 3.1 mgd of rainfall from the Big Slough will have an adverse impact on the City of North Port's water facility. The City of North Port is currently under a consent agreement with the Florida Department of Environmental Regulation because the water supplied by its facility violates drinking water quality standards for sulfates and total dissolved solids ("TDS") regularly during periods of low flow in the Big Slough. The MWSA, the plant area and the initial mining areas are primarily within the Big Slough drainage area. Seepage of 1.2 mgd from the MWSA will flow into the Big Slough. The only analysis done of the quality of the seepage from the MWSA was a rough analysis which showed that sulfates will likely be around 550 grams per liter. The legal standard for sulfates in drinking water is 250 grams per liter. Seepage from the MWSA will be high in total dissolved solids ("TDS") since a good portion of it was pumped from deep wells which have very high levels of TDS. No analysis was done of the potential of this seepage water to interfere with North Port's facility. Charlotte County is an existing legal user of water whose water supply is drawn from the Peace River downstream from the proposed CMI phosphate mine at Pine Level. Discharge of 5.0 mgd from the Pine Level mine could adversely affect Charlotte County's drinking water facility located on the Peace River. AGRICULTURAL USE CMI proposes to use 5.0 MGD of surplus water for irrigation of pasture grasses for cattle. CMI has not conducted any specific tests to determine the feasibility of using the discharge or the quality of the water that they plan to use for agricultural irrigation. The water for irrigation will be drawn out of the mine water surge area. The determination of whether the 5.0 mgd discharge can be used for agricultural irrigation has been postponed. The staff's position is that the proposed special conditions provide reasonable assurances that the discharge will comply with the requirements of the Basis for Review. WETLANDS Isolated wetlands occur throughout the CMI mine site. The isolated wetlands on the CMI property provide habitat for endangered and threatened species. Sandhill Cranes and Wood Storks, both threatened or endangered species, were sighted on the CMI property by wetlands experts during their site visit prior to the hearing. Small isolated wetlands on CMI property would be adversely affected by less than a one foot draw down. Wetland peat soils oxidize if exposed to the air. Oxidation results in subsidence of the wetland soils, which adversely impacts wetlands. Too much water as well as too little water can adversely impact wetlands. The combined effects of aquifer pumping and dewatering planned at the CMI site will adversely affect wetlands. No analysis was completed of the impacts to wetlands as a result of the combined effects of dewatering and pumping from the aquifer. No information regarding the normal range of wetland hydroperiods for preserved wetlands or other onsite unmined wetlands was introduced. No information was provided regarding the habitat functions provided by the wetlands on the CMI site either for threatened or endangered species or otherwise. ENVIRONMENTAL IMPACT The Applicant did not provide reasonable assurance that the water use will not cause unacceptable adverse impacts to environmental features on or off- site. The Applicant did not provide reasonable assurances that the water use will not have an adverse impact to surface water bodies such as lakes, ponds, impoundments, springs, streams, canals, estuaries or other water courses. The Applicant did not provide reasonable assurances that there will be no adverse environmental impact to wetlands, lakes, streams, estuaries, fish, and wildlife or other natural resources. The Applicant did not provide reasonable assurances that there will be no adverse impacts to the surface water system or vegetation as a result of groundwater withdrawal. The Applicant did not provide reasonable assurances that the water use will not have an adverse impact by altering or impairing the habitat of threatened or endangered species. The Applicant did not provide reasonable assurances that the projected draw downs will not result in any adverse impact to any protected or non-protected plant or animal species. The Applicant did not provide reasonable assurances that the water use will not have an adverse environmental impact to wetlands.

Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Governing Board of Southwest Florida Water Management District enter a Final Order DENYING the issuance of a Water Use Permit to the Applicant, CMI. DONE and ENTERED this 20th day of April, 1993, in Tallahassee, Florida. DANIEL M. KILBRIDE Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 20th day of April, 1993. APPENDIX The following constitutes my specific rulings, in accordance with section 120.59, Florida Statutes, on proposed findings of fact submitted by the parties. Proposed findings of fact submitted by Petitioner. Accepted in substance: paragraphs - 13, 14, 15, 21, 24, 31, 35, 38, 70, 71, 73, 75, 91, 97, 100, 104, 105, 114, 115, 116, 125, 126, 127, 128, and 129. Rejected as subsumed or irrelevant and immaterial: paragraphs - 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 16, 17, 19, 20, 22, 23, 25, 27, 28, 29, 30, 33, 34, 36, 37, 37A, 39 40, 43, 44, 45, 48, 49, 50, 51, 52, 53, 54, 55, 56, 57, 58, 59, 60, 61, 62, 63, 64, 65, 66, 67, 68, 72, 74, 76, 77, 78, 79, 80, 81, 82, 83, 84, 85, 86,87, 92, 93, 94, 95, 96, 98, 99, 101, 102, 103, 106A, 106, 107, 108, 109, 110, 111, 112, 113, 117, 120, 121, 122, 123, 124, 130, 131, 132, 133, and 134. Rejected as against the greater weight of the evidence: paragraphs - 18, 26, 32, 41, 42, 46 (omitted), 47 (omitted), 69, 88 (omitted), 89 (omitted), 90 (omitted), 118 (omitted), 119 (omitted), and 135 (omitted). Proposed findings of fact submitted by Petitioner, Charlotte County. Accepted in substance: paragraphs - 1, 2, 7, 18, 19, 20, 22, 25, 28, 29, 36, 40, 41, 51, 59, and 62. Rejected as argument, subsumed or irrelevant and immaterial: paragraphs - 3, 4, 5, 6, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 21, 23, 24, 26, 27, 30, 31, 32, 33, 34, 35, 37, 38, 39, 42, 45, 46, 47, 48, 49, 50, 52, 53, 54, 55, 56, 57, 58, 60, and 61. Rejected as hearsay: paragraphs - 43 and 44. Proposed findings of fact submitted by Petitioner, City of North Port. Accepted in substance: paragraphs - 1, 2, 3, 5, 6, 7, 9, 19, 20, 21, 22, 24(in part), 25, 26, 27, 28, 29, 30, 31, 32, 34, 35, 36, 37, 38, 39, 40, 41, 42, 45, 47, 48, 49(in part), 50, 51, 52, 53, 54, 56, 57(in part), 58, 59, 60, 61, 63(in part), 65, 66, 67, 68, 69, 70, 71, 72, 73, 74, 75, 78, 79, 80, 83, 84, 85, 86(in part), 87, 92, 93, 95, 96, 99, 104, 107, 108(in part), 109(in part), 112, 113, 114, 115, 116, 120, 122, 123, 126, 138, 139, 140, 141, 142, 143(in part), 144, 150, 153, 154, 155, 156, 159, 167, 168, 170, 171, 172, 173, 176, 177, 179, 180, 187, 193, 194, 195, 197, 198, 199, 200, 201, 202, 204, 205. Rejected as argument, subsumed or irrelevant and immaterial: paragraphs - 4(contained in Preliminary Statement), 8, 10, 11, 12, 13, 14, 15, 16, 17, 18, 23, 24(in part), 33, 43, 44, 46, 49(in part), 55, 57(in part), 62, 63(in part), 64, 76, 77, 81, 82, 86(in part), 88, 89, 90, 91, 94, 97, 98, 100, 101, 102, 103, 105, 106, 108(in part), 109 (in part), 110, 111, 117, 118, 119, 121, 124, 125, 127, 128, 129, 130, 131, 132, 133, 134, 135, 136, 137, 143(in part), 145, 146, 147, 148, 149, 151, 152, 157, 158, 160, 161, 162, 163, 164, 165, 166, 169, 174, 175, 178, 181, 182, 183, 184, 185, 186, 188, 189, 190, 191, 192, 196, 203, 206, 207, 208, 209, 210, 211, 212, 213, 214, 215, 216, 217. Proposed findings of fact submitted by Respondent/Petitioner Consolidated Minerals, Inc. and Southwest Florida Water Management District. Accepted in Substance: paragraphs - 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 14, 17, 18, 19, 20, 21, 22(in part), 23, 24, 25(in part), 26, 27(in part), 28, 29(in part), 32, 33(in part), 39, 40, 41, 42, 43, 44, 45, 46, 47, 49, 50, 52(in part), 53, 54, 55, 56, 57(in part), 58, 62, 71, 82, 85, 87, 88, 91, 92(in part), 93, 94(in part), 95(in part), 96(in part), 97(in part), 100(in part), 101, 115, 119, 120, 123, 124(in part), 125(in part), 126(in part), 127(in part), 130(in part), 133(in part), 137, 138(in part), 139, 145. Rejected as argument, subsumed, or irrelevant and immaterial: paragraphs - 12, 13, 15, 16, 31, 36, 37, 38, 48, 51, 52(in part), 57(in part), 59, 60, 63, 80, 81, 83, 84, 86, 90, 94(in part), 105, 106, 107, 108, 109, 110, 111, 112, 113, 114, 116, 117, 118, 124(in part), 126(in part), 127(in part), 130(in part), 134, 135, 136, 138(in part), 140, 141, 142, 143. Rejected as against the greater weight of evidence: paragrahs - 22(in part), 25(in part), 27(in part), 29(in part), 30, 33(in part), 34, 35, 61, 64, 65, 66, 67, 68, 69, 70, 72, 73, 74, 75, 76, 77, 78, 79, 89, 92(in part), 95(in part), 96(in part), 97(in part), 98, 99, 100(in part), 102, 103, 121, 122, 125(in part), 128, 129, 131, 132, 133(in part), 144. Proposed findings of fact submitted by Petitoner, Environmental Confederation of Southwest Florida, Inc. Accepted in substance: paragraphs - 1, 2, 3, 4 6, 7, 17, 22, 26, 27, 28, 29, 30, 33(in part), 34, 35, 39(in part) 41, 42, 43, 45, 48, 53, 56, 57, 59, 60, 61, 62, 71, 73, 80, 81, 82, 85, 86, 87, 92(in part), 106, 107, 110, 112, 113, 114, 115, 116, 117, 121, 122, 123, 124, 125, 126, 127, 128, 129, 130, 131, 132, 133, 134, 135, 136, 137, 138, 139(in part), 140, 141, 142, 143, 144, 145, 148, 149, 150, 151, 152, 154, 155, 157, 158, 162, 163, 164, 165. Rejected as argument, subsumed, or irrelevant and immaterial: paragraphs - 5, 8, 9, 10, 11, 12, 13, 14, 15, 16, 18, 19, 20, 21, 23, 24, 25, 31, 32 33(in part), 36, 37, 38, 39(in part), 46, 47, 49, 50, 51, 52, 55, 58, 63, 64, 65, 66, 67, 68, 70, 72, 74, 75, 76, 77, 78, 79, 83, 84, 88, 89, 90, 91, 92(in part), 93, 94, 95, 96, 97, 98, 99, 100, 101, 102, 103, 104, 105, 108, 109, 111, 118, 119, 120, 146, 147, 153, 156, 159, 160, 161, 166, 167, 168. Rejected as against the greater weight of evidence: paragraphs - 44, 54, 69, 139(in part). COPIES FURNISHED: Rory C. Ryan, Esquire Roger W. Sims, Esquire HOLLAND & KNIGHT Suite 2600 200 S. Orange Avenue P. O. Box 1526 Orlando, Florida 32802 Vivian Arenas, Esquire Assistant General Counsel Southwest Florida Water Management District 2379 Broad St. Brooksville, Florida 34609 Mr. Alan R. Behrens Route 2, Box 725-A-32 Arcadia, Florida 33821 Matthew G. Minter, Esquire County Attorney 18500 Murdock Cr. Port Charlotte, Florida 33948-1094 David M. Levin, Esquire ICARD, MERRILL, CULLIS, TIMM, FUREN & GINSBURG PO Box 4195 Sarasota, Florida 34237 Kenneth B. Wright, Esquire Sierra Club Legal Defense Fund PO Box 1329 Tallahassee, Florida 32302 Peter G. Hubbell Executive Director 2379 Broad Street Brooksville, Florida 34609-6899

USC (1) 50 CFR 17.12 Florida Laws (7) 120.5717.12373.019373.219373.223373.406373.414 Florida Administrative Code (4) 40D-2.09140D-2.10140D-2.30140D-2.381
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CARL F. ZINN vs ST. JOHNS RIVER WATER MANAGEMENT DISTRICT, 91-003862 (1991)
Division of Administrative Hearings, Florida Filed:Deland, Florida Jun. 24, 1991 Number: 91-003862 Latest Update: Jun. 10, 1992

The Issue The issue concerns the entitlement of GJPS Lukas, Inc. to be granted a consumptive use of water permit from the St. Johns River Water Management District. See Chapter 373, Florida Statutes, and Chapter 40C-2, Florida Administrative Code.

Findings Of Fact On December 7, 1990, the Applicant applied for a consumptive use of water permit under application no. 2-127-0808AN as submitted to St. Johns. The Applicant asked that it be allowed to withdraw water from the Floridian aquifer to irrigate a 240 acre sod farm by the use of four wells and a pipeline ditch irrigation system. This was a new use. On January 9, 1991, St. Johns prepared a technical staff report recommending approval of the application. Petitioner was provided notice of this pending disposition on January 15, 1991 leading to his protest to the grant of the permit. Petitioner's property is adjacent to the Applicant's property. Petitioner has a well which he uses for domestic water needs which is in the vicinity of the proposed project. He also has a commercial fish operation with a number of fish ponds including fresh water ponds. Both these uses may potentially be affected by the proposed consumptive water use contemplated by the Applicant. St. Johns calculated that the irrigation of 240 acres of sod, by calculation using the modified Blaney-Criddle formula pertaining to evapotranspiration, calls for a maximum extraction of 169.4 million gallons a year. In any one month the amount withdrawn should not exceed 37.4 million gallons. The Floridian aquifer at the place where the Applicant proposes to draw water is capable of the production of 169.4 million gallons of water per year and 37.4 million gallons per month without promoting environmental or economic harm. Extraction of this water for purposes of irrigation is an acceptable arrangement in that no wastewater treatment plants are within a five mile radius of the site of the proposed use. Therefore it would not be economically, technically or environmentally feasible for the Applicant to use reclaimed wastewater as a source for its irrigation needs. The aquifer in that area is stable. There was no showing in the hearing by competent evidence that saline water intrusion problems now exist in the area of the proposed site of withdrawal. There was no showing that the withdrawal of as much as 169.4 million gallons per year would cause a saline water intrusion problem. The fields where the Applicant intends to apply the extracted water for irrigation purposes are surrounded by a system of ditches and water control structures to confine the water as applied to the sod and any mixing of that water with any surface or subsurface waters that are contributed by rain events. The ditches and control structures keep the water on the property and prevent flooding downgradient of the subject property. As a consequence flood damage on adjacent properties is not to be expected. On a related issue, the ditches and control structures will prevent water from discharging into receiving bodies of water and thereby degrading water in those receiving bodies such as the fish ponds operated by the Petitioner. The water quality of the Floridian aquifer will not be harmed by the activities of the Applicant in withdrawing this water. In the worse circumstances the well used by the Petitioner will be affected by the Applicant extracting the water from the aquifer to the extent of .25 to .4 drawdown in feet in the well the Petitioner uses. This is not a substantial impediment to the Petitioner's ability to withdraw needed water from the well he uses. The Floridian aquifer in the area in question is semi-confined. The four wells that would be used in withdrawing water for the Applicant's purposes will extract the water at 110 feet below the surface. Between that level and the surface are three confining areas of clay totaling approximately 40 feet in thickness. Those confining units of clay would protect the water at the surface when the Applicant withdraws water and induces a gradient. In particular, the nature of the stratification in the soils in the area in question and the topography are such that the Petitioner's fish ponds, when taking into account the distance between the Applicant's operation and those fish ponds, the clay confining units and the gradient between the Applicant's property and the Petitioner's fish ponds, would not lead to a reduction in the water levels of the Petitioner's fish ponds when the water was extracted by the Applicant. The proposed use by the Applicant would not require invading another use reserved by a permit issued from St. Johns. St. Johns has not established minimum levels or rates of flow for the surface water in the area where the Applicant proposes to extract the water. Nor has St. Johns established a minimum level for a water table aquifer or a minimum potentiometric surface water for an aquifer in the area where the Applicant proposes to extract the water. The surficial aquifer water table beneath the property where the Applicant intends to apply the extracted water should not be raised inordinately should the Applicant follow the best management practice as recommended as special condition No. 9 to the Consumptive Use Technical Staff Report pertaining to this project. Nonetheless if the water table beneath the Applicant's property were to be raised to a level which is too high or if the activities by the Applicant would result in excessive surface water runoff the ditches and water control structures that isolate the Applicant's property would prevent the water level in the Petitioner's fish pond from being increased by the Applicant's proposed activities. The application of the extracted water and the expected flow pattern of water applied to the surface and control of that water is set out in St. Johns' Exhibit No. 5 and described in the testimony of Jack Caldwell Lawrence, Jr., employee of St. Johns and an expert in geology and hydrology. See pages 61 and 62 of the transcript. Concerning water quality in the Petitioner's fish pond, it will not be affected by the Applicant's proposed activities in extracting the water. The gradients and distances between the Petitioner's fish pond and the Applicant's fields do not allow surface water or water in the surficial aquifer, which is groundwater above the confining clay unit, to flow from the Applicant's fields into the Petitioner's fish ponds. Again the ditches and control structures related to the project offer additional protection against a compromise to the water quality in the Petitioner's fish ponds. The Technical Staff Report on this project is an apt description of the project and the necessary conditions to granting a permit which would protect the public and environment. One modification has been made to that report and that modification is appropriate. It changes the intended disposition from one of allowing surface water from the onsite management system to be used as the primary irrigation supply with the Floridian aquifer serving as a supplementary source to one in which the Applicant would not use the onsite management system as a water supply source but would use the onsite management system simply as a discharge holding area.

Recommendation Based upon the facts found and the conclusions of law reached, it is, RECOMMENDED: That a Final Order be entered which approves the application for consumptive use of water subject to the conditions set forth in the Technical Staff Report, excepting the need to have the Applicant utilize water from the onsite management system as the primary source of irrigation of its sod. DONE and ENTERED this 4th day of November, 1991, in Tallahassee, Florida. CHARLES C. ADAMS, Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 4th day of November, 1991. APPENDIX TO RECOMMENDED ORDER The following discussion is made of the suggested facts set forth in the proposed recommended orders. Petitioner's Facts Paragraphs 1-6 are subordinate to facts found. Concerning Paragraph 7, Petitioner does not have standing to take issue with the quality of notice provided to other adjacent landowners. As to Paragraph 8, the witness had sufficient understanding of the location and nature of the surficial or sand aquifer and the clay confining units to have his testimony credited. As to Paragraph 9 the fact that the witness is unaware of the exact depth of the Petitioner's fish pond does not cause his testimony to be disregarded in deciding that the fish ponds would not be negatively impacted by the activities contemplated in this permit application. As to Paragraph 10, this proposed fact is inconsequential given the de novo nature of this proceeding. As to Paragraph 11, see discussion of Paragraph 7. As to Paragraph 12, it is rejected. As to Paragraph 13, that knowledge was not necessary in determining the outcome here. As to Paragraph 14, it is accepted in hypothetical terms, however, no showing was made that chlorides would increase in this instance and adversely affect the Petitioner's fish based upon the evidence adduced at hearing. As to Paragraph 15, the soil samples from Petitioner's property are inclusive and less reliable that the description of soil in the general area as set forth by the witness for St. Johns. COPIES FURNISHED: Clayton D. Simmons, Esquire Stenstrom, Mackintosh, Julian, Colbert, Whigham and Simmons, P.A. 200 West First Street, Suite 22 Sanford, FL 32772-4848 Michael D. Jones, Esquire 996 Westwood Square, Suite 04 Oviedo, FL 32765 Michael D. Jones, Esquire Post Office Box 3567 Winter Springs, FL 32708 Eric T. Olsen, Esquire St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429 Henry Dean, Executive Director St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429

Florida Laws (3) 120.57373.019373.223 Florida Administrative Code (1) 40C-2.101
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DESOTO CITIZENS AGAINST POLLUTION, INC. vs FARMLAND HYDRO LIMITED PARTNERSHIP, REDLAND GROWERS EXCHANGE, INC., AND SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 02-000232 (2002)
Division of Administrative Hearings, Florida Filed:Bartow, Florida Jan. 16, 2002 Number: 02-000232 Latest Update: Jun. 18, 2004

The Issue Whether General Water Use Permit (WUP) Number 20012185.000 (Permit) meets the conditions for issuance as established in Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, and should be issued to Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc.

Findings Of Fact The Parties DCAP is not-for-profit corporation incorporated in the State of Florida. Behrens is the President of DCAP. See also Findings of Fact 63-77. Farmland Hydro is a Delaware Limited Partnership authorized to transact business in Florida, and is the owner of the property leased by Basso/Redland, which is the subject of this WUP. Frank T. Basso, Jr., is a third generation farmer, who operates as Redland Growers Exchange, and seeks a General WUP to authorize groundwater withdrawals for crop irrigation. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries pursuant to Chapter 373, Florida Statutes, and the rules promulgated thereunder as Chapter 40D, Florida Administrative Code. The Proposed Water Use An Application for a General WUP was submitted by Farmland Hydro and Basso, as co-applicants, and received by the District on April 11, 2001. After receipt of additional information, the Application was deemed complete on October 22, 2001. The Applicants seek a General WUP to authorize a new water use for the irrigation of 140 acres for the production of both Spring and Fall row crops, using a seepage-with-mulch irrigation system.1 Basso plans to grow tomatoes and/or peppers in the Spring, and squash and/or cucumbers in the Fall. Crop planting for both seasons will be phased-in over a one-month period. Water allocation quantities are calculated on a weekly phase-in basis of approximately 35 acres for each planting date. The total time that the parcel will be in use for farming, to include planting and harvesting for each crop, is approximately six months per year. The subject parcel is part of a 250-acre tract known as the Brushy Creek Tract and is located in Hardee County approximately two miles south of the town of Ona; approximately two miles south of the intersection of U.S. Highway 64 and County Road 663; and is within the Southern Water Use Caution Area (SWUCA). The subject parcel currently does not contain a water well. The Brushy Creek Tract is a larger parcel of approximately 1,230 acres leased from Farmland Hydro by Redland and also by Parker Farms for cattle grazing, farming, and hunting. The subject parcel is used for cattle grazing and is surrounded by land owned by Farmland Hydro and used for either cattle grazing or agricultural row crops. Farmland Hydro also operates an additional approximately 1,941 acres of property near the subject parcel, which is used for citrus groves. Farmland Hydro has consumptive WUPs for this property. The closest existing legal user to the proposed Basso well site is another well on the Farmland Hydro property. As is generally done with vegetable crop production in Florida, vegetable crops grown on the Farmland Hydro property are grown in rotation with pasture, and have been rotated in this manner for many years. Typically, farmers have farmed a piece of land for one, two or three years and then, to avoid the buildup of insects and diseases, have allowed the land to revert to pasture and have moved on to another field for crop production. The subject parcel for which the WUP is being sought will be similarly treated. Crop rotation is an important agricultural best management practice that is used to address pest management, soil conservation, and maximizing nutrients for obtaining favorable crop production. Soil conservation is important to Basso, notwithstanding that there is a response in the Application that no approved Soil Conservation Service plan exists for the operation included in the Application. If the WUP is issued and the subject parcel is placed into crop production, another parcel of land will be taken out of crop production by Basso, resulting in the discontinuation of another permitted well. As a result, the issuance of this WUP will not result in a "water use change." Determination of Reasonable Demand/Allocated Quantities In determining whether a proposed water use is reasonable-beneficial and in the public interest, the District calculates the appropriate permit quantities for the particular water use, which is a function of demonstrated need, or demand for water; efficiency of the water treatment and distribution systems; whether water is sold or transferred to other entities; whether acceptable water can be acquired from lower quality sources; and whether conservation practices are employed. District Basis of Review (BOR), page B3-1. The reasonable need for agricultural water use is generally composed of one or more demand components, depending upon the specific agricultural use. "Typically, the reasonable need for irrigation water uses is equal to the supplemental crop requirement divided by the system efficiency or the system design capacity, whichever is less." "The supplemental crop requirement is the amount of water needed for a particular crop beyond the amount of water provided by effective rainfall." The supplemental crop requirement is generally determined by using the Agricultural Water Use Calculation Program (AGMOD) Version 2.1, which is based on the modified Blaney-Criddle method. This program takes into account site specific information such as crop type, growing period, evapotranspiration rate, soil type, rainfall, irrigation method and number of irrigated areas. "In most cases, the supplemental irrigation requirement is determined for a 2 in 10-year drought condition." The AGMOD program determines an inch-application rate which, when applied to the number of acres to be irrigated, results in a calculation of total annual average and peak monthly quantities for the proposed water use. District BOR, pages B3-4 and 3-5. See also District Water Use Design Aids, pages C4-1 through C4-7. In determining the allocated quantities, or reasonable demand for water, the District seeks to avoid both over- allocating water and under-allocating water for the specific crop intended, to ensure that the permitted amount is sufficient for the "2 in 10-year drought condition." Consequently, the allocated quantities arrived at by District staff through use of the AGMOD methodology may be different from the quantities indicated on an applicant's initial application, which are generally estimated without benefit of an agricultural water use calculation program. The AGMOD program was used to calculate water use quantities for the proposed water use. The allocated quantities for Basso's proposed use are 454,000 gallons per day (gpd) on an annual average basis and 1,241,000 gpd, as a peak month quantity. No quantities were requested or allocated for crop protection. See Finding of Fact 52. Modeling for Simulated Impacts As part of the application review process, the District evaluates potential impacts to existing legal uses of water, the water resources and environmental features that may result from the proposed groundwater withdrawals. To assist in the review process, analytical and numerical models, which incorporate best available hydrogeologic parameters for the area being considered for a permit, are used to simulate drawdowns for the withdrawal of the proposed quantities. The results of these simulations are used in the evaluation of potential impacts to assess whether the application meets the conditions for issuance. The District undertook simulation modeling of the potential effects of the proposed water withdrawals to be authorized by the permit. The allocated quantities were entered into the MODFLOW 387 groundwater flow model, which is a three- layer model developed by the U.S. Geological Survey and is the generally accepted model for this purpose. Model layers were set up to represent the surficial, intermediate, and Upper Floridan aquifers. (The Applicants seek to pump water solely from the Upper Floridan Aquifer.) There are limitations to the model in that the model assumes a homogeneous isotropic aquifer, with no preferred flow direction. In actuality, there is variability in the geology of the area. Modeling is intended to serve as a screening tool for assessing localized impacts anticipated from a proposed water use and is based upon the best available information. As distance from the proposed withdrawal site increases, the reliability of the modeling decreases, due to the variability in the geology and other parameters or boundary conditions that can affect the model. Use of the MODFLOW groundwater model allows the District to look at potential impacts at the site, and in the proximity of the site, and assists the District in assessing possible cumulative impacts associated with a proposed use. To assist in assessing potential impacts from the proposed use, a Peak Month modeling simulation was undertaken by the District, which simulates the effect of pumping the proposed Peak Month withdrawal rate of 1,241,000 gpd for 90 consecutive days, with no recharge to the aquifer systems. The model essentially presents a worst case scenario that is a more severe prediction than what is actually likely to occur from the permitted use under normal conditions. Simulating the period of greatest demand on the hydrologic system is likely to provide maximum protection to existing legal water users and the water resources. The Peak Month simulation undertaken by the District predicts drawdowns in the potentiometric surface of the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site; less than 1.4 feet at the nearest property boundary (approximately 1,250 feet from the proposed withdrawal site); and less than 1.2 feet at the nearest existing legal user (a Farmland Hydro well approximately 3,500 feet from the proposed withdrawal site). These numbers did not raise a concern for District staff. ("Potentiometric surface" is "a surface defined by the level to which water rises in an open pipe that is constructed into or all the way through an artesian aquifer. This is measured in feet relative to NGVD or sea level. The level to which water rises inside this open pipe is a function of the pressures on the water in the artesian aquifer." District BOR, page B-xii.) The Peak Month simulation predicts drawdowns in the intermediate aquifer of approximately 0.9 feet at the proposed withdrawal site, and less than 0.9 feet at the property boundary, and at the nearest existing legal user. The Peak Month simulation predicts drawdowns in the water level of the surficial aquifer (water table) of approximately 0.01 feet or less at the proposed withdrawal site, property boundary and nearest existing legal user. Based upon the Peak Month simulations, the District reasonably determined that further cumulative impact modeling was not necessary in order to assess localized cumulative impacts resulting from the proposed use. To assess regional cumulative impacts, the District evaluated Regional Observation Monitoring Program (ROMP) data and found no significant trends in withdrawals in recent years, other than a slight decline attributed to the recent drought. Conditions of Issuance of the Proposed Permit In order to obtain a water use permit, an applicant must establish that the proposed use of water is a reasonable- beneficial use, will not interfere with any existing legal use of water, and is consistent with the public interest, by providing reasonable assurance, on both an individual and cumulative basis, that the water use meets the conditions for issuance as specified in Section 373.223(1), Florida Statutes, and Rule 40D-2.301, Florida Administrative Code. A permit must be obtained from the District prior to withdrawing water, where the withdrawal is from a well having an outside diameter of six inches or more at land surface, where the annual average withdrawal from all sources is 100,000 gpd or greater, or where the total combined withdrawal capacity from all sources is greater than or equal to 1 mgd. The proposed water use falls within these parameters. Rule 40D-2.041(1)(b) and (c), Florida Administrative Code. The quantities allocated for the proposed use have been determined by the District to be necessary to fulfill a certain reasonable demand, for the reasons specified herein. To assist in assessing impacts, the District utilizes a network of ROMP wells to obtain basic groundwater monitoring data over time and to help characterize the lithology, stratigraphy, aquifer depths, water levels and, in some cases, water quality for the various water resources. Data obtained from the ROMP and other wells is compiled to ascertain aquifer characteristics within the District and is also integrated into the District's modeling efforts pertaining to proposed water uses. ROMP well No. 31 is located just off the northeast corner of the Basso site. Having a ROMP well adjacent to the Basso site increases confidence in the specific geological information being used in the groundwater model to assess potential impacts from the proposed uses. ROMP well No. 17 is located approximately 1/2 mile from DCAP member Behren's well. Data from both wells were considered in assessing potential impacts from the proposed water use. Based on available information, the possible sources of groundwater for the proposed use at the Basso site are the surficial aquifer, intermediate aquifer, and the Upper Floridan Aquifer systems. To ensure sufficient quantities of water for the proposed use and to avoid potential impacts to environmental features, such as wetlands and surface waters, the District will require the proposed use to limit withdrawals to solely the Upper Floridan Aquifer. By examining stratigraphic cross sectional information generated from the ROMP wells, particularly ROMP No. 31 well, which is in close proximity to the Basso site, District staff were able to determine, with reasonable certainty, the approximate depths of the aquifers at the Basso well site. To ensure that the well will be open solely to the Upper Floridan Aquifer, the permit requires the Basso well to have a minimum of 400 feet of casing, with an estimated well depth of 1,000 feet. Based upon available information concerning the construction of other wells in the vicinity of the proposed Basso well, the District is reasonably assured that a well cased for a minimum of 400 feet will draw water only from the Upper Floridan Aquifer and will minimize the potential for water to move between the aquifers through the well. The well construction requirements imposed for Basso's well are in line with the best available stratigraphic information and with known construction of wells in the area. By casing the well to a depth of 400 feet and due to the extremely low leakage of the intermediate confining unit, the intermediate and surficial aquifers will be buffered from impacts associated with the proposed use. The District will deny a water use permit application if the proposed withdrawal of water, together with other withdrawals, would cause an unmitigated adverse impact on a legal water withdrawal existing at the time of the application. The District considers an adverse impact "to occur when the requested withdrawal would impair the withdrawal capacity of an existing legal withdrawal to a degree that the existing withdrawal would require modification or replacement to obtain the water it was originally designed to obtain." District BOR, page B4-14. Based upon an assessment of individual and cumulative regional information, there are no existing legal uses of water that will be adversely impacted as a result of the proposed withdrawals. Based upon an assessment of individual and cumulative regional information, no quantity or quality changes that adversely impact the water resources, including both surface and groundwaters, are anticipated from the proposed withdrawals. The District requires that consideration be given to the lowest water quality available, which is acceptable for the proposed use. Lower quality water includes reclaimed water, collected stormwater, recovered agricultural tailwater, saline water or other sources. District BOR, page B4-12. For the proposed water use, there is no viable lower quality water source and no reclaimed water available near the site to use as an alternative to groundwater pumping. The Applicants are proposing to use the lowest quality water that is available. There are no known concerns regarding the quality of water in the Upper Floridan Aquifer at this location in Hardee County. Restricting the proposed water use to the Upper Floridan Aquifer will not cause water quality concerns or result in pollution to any of the aquifers. Simulated drawdowns to the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site, less than 1.4 feet at the nearest property boundary, and less than 1.2 feet at the nearest permitted well, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the intermediate aquifer of 0.9 feet at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the surficial aquifer of 0.01 feet or less at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, constitute a nearly undetectable impact to the surficial aquifer, which is not an adverse impact. The modeling simulations demonstrate that the proposed withdrawals will have no significant effect on the surficial aquifer and, therefore, will not cause adverse impacts to environmental features such as wetlands, lakes, streams, fish and wildlife, or other natural resources. None of the simulated drawdowns are considered to be predictions of adverse impacts, not even in the localized vicinity of the well site. Mr. Jackson explained that because the localized modeling simulations were small or insignificant and showed no adverse impacts, cumulative modeling is not considered necessary. Reasonable assurance on a cumulative basis is determined by assessing the potential localized impacts in conjunction with existing cumulative data for the region, such as the available ROMP data and hydrographs, which depict the existing regional condition, taking into account, on a cumulative basis, all existing uses as well as rainfall conditions and climate. Based on an assessment of the cumulative data and the modeling for individualized impacts, and applying professional judgment, District staff reasonably concluded that the proposed water use presents no concerns that it will cause, on either an individual or a cumulative basis, adverse impacts to the water resource or existing legal uses. Minimum flows and levels have not been established by the District for the area where the proposed use is located. (The parties stipulated that the District has not established minimum flows and levels pursuant to Section 373.042, Florida Statutes, for the Southern Water Use Caution Area (SWUCA)). Therefore, Rule 40D-2.301(1)(d), Florida Administrative Code, (requirements for minimum flows and levels), is not applicable to the proposed permit. The proposed use presents no concerns for saline water intrusion. The proposed use raises no concerns regarding causing pollution to the aquifer. There are no offsite land uses that will be adversely impacted as a result of this permit. Basso currently uses best management practices for water conservation in his ongoing farming operations, and intends to use such practices with the new farming operation authorized under the permit. In keeping with such practices, irrigation is stopped when the water reaches the end of the watering ditch. Basso uses seepage irrigation and tries to regulate the ditches so that there is a minimum, if no, runoff. Also, a watering cycle generally lasts from three to seven days before irrigation has to be resumed. Any runoff goes into "filtering ponds, before reaching ditches or creeks" in its raw content. Basso does not intend to farm during months of likely frost so no separate allocation for frost/freeze protection was requested or needed. Given these irrigation practices, water is not reasonably expected to be wasted. All necessary and feasible agricultural water conservation activities will be implemented upon issuance of the WUP. In addition, Specific Condition No. 3 of the proposed WUP requires the incorporation of best water management practices in all irrigation practices. The proposed use presents no concerns that it will otherwise be harmful to the water resource. The Applicants have met all the requirements for issuance of a WUP. Southern Water Use Caution Area The proposed water use site is located within the SWUCA. The District established the SWUCA as a means of addressing on a regional scale concerns about long-term impacts to the water resource. Water use caution areas were created in recognition of regional water concerns. There have been drought conditions in the area which have caused reduced aquifer levels. The proposed water use site is not within the "Most Impacted Area" (MIA), which is located approximately 18 miles to the west of the site in Manatee County, nor within the "East Tampa Bay Water Use Cautionary Area" (ETB WUCA), which is approximately six miles to the west of the proposed site, also in Manatee County. (The SWUCA includes the MIA and ETB WUCA.) Pending final adoption of rules for the SWUCA, the District will continue to issue WUPs for proposed water uses that meet the conditions for issuance. The District cannot treat new uses and existing renewal uses any differently when considering the issuance of a permit. Once SWUCA rules and minimum flows and levels are established, the District expects to rely on a more regional approach to address long-term cumulative impacts over the entire use caution area, instead of relying on a permit-by-permit basis to address regional concerns. Standard Condition No. 9 of the proposed WUP requires the permittee to cease or reduce withdrawals as directed by the District, if water levels in the aquifers fall below the minimum levels established by the District Governing Board. The proposed withdrawal will use a seepage with mulch irrigation method, which has a 50 percent efficiency level. See footnote 1. This is the minimum efficiency level currently required for agricultural WUPs within the SWUCA, which approve the use of this irrigation method. As SWUCA rules come into effect, a higher percentage efficiency level probably will be required, as is now required in the Eastern Tampa Bay Water Use Caution Area and also in the Highlands Ridge Water Use Caution Area. Consequently, Standard Condition No. 11 of the proposed WUP requires that, when SWUCA rules are implemented, the permittee must comply with any higher efficiency level or other special regulation that may be required for the SWUCA area. DCAP's Challenge to the Proposed WUP DCAP does not keep official membership records. It does not maintain any list of current members. According to Behrens, there are five members of the board of directors. DCAP does not hold corporate meetings, annual meetings or maintain corporate records. Members do not meet. There are no means to document the existence of members for this organization. Behrens is a member of DCAP. He has owned five acres adjoining the west side of Horse Creek (in DeSoto County) since 1985. Behrens complains that the District does not look at the cumulative effect on his well and other people he knows, such as George Chase. Behrens is concerned with any lowering of the water level in the area, including Horse Creek. He believes that approval of wells in the area, including the proposed well, is the straw that is breaking the camel's back. Mr. Chase shares this view. Behrens relies on an artesian free-flowing, two-inch diameter well, for domestic water use, located in the intermediate aquifer, approximately 150 feet deep. (Behrens' well is approximately 18-20 miles from the proposed Basso well.) For most of the time he has lived there, the well had an electric pump for obtaining water. Approximately one year ago, the pump went bad, and a replacement system has not been installed. Currently, Behrens has no pump on the well, and in dry periods, has to obtain water for domestic uses from nearby Horse Creek, which is low during the dry season. (Behrens depends on Horse Creek to pursue his recreation, wildlife, and aesthetic values.) Having a flowing artesian well will enable him to obtain water from the well without having to install an electrical pump, a situation which is desired by Behrens, in part, because the property is in a flood plain and experiences frequent flooding and electrical outages. Not all artesian wells flow. Artesian wells are completed into confined aquifers in which the water in a tightly cased well, will rise to a level above the formation being measured. Water would have to rise above the land surface to be a flowing well. For a well to be artesian, the well must be under confined pressure. For a well drawing water from a confined aquifer, such as the intermediate or the Upper Floridan Aquifer systems, the measured water level in the well is a reflection of the amount of potentiometric pressure in the well. This level can be affected just as much by the amount of recharge as it can by the amount of water withdrawals. There is no evidence that the proposed water use will adversely impact the flowing nature of either Behrens' or Chase's well. The evidence demonstrates that the proposed water use will not adversely impact Behrens' well. George Chase is a member of DCAP. Mr. Chase lives in Arcadia, DeSoto County, Florida. His property is adjacent to the Peace River. Mr. Chase's well is a two-inch diameter well, believed to be about 150 feet deep and equipped with a 12-volt DC solar-powered pump. Mr. Chase has in the past relied on artesian pressure within the confined intermediate aquifer to supply water to his solar-powered home. The solar-powered pump assists in supplying water to the home. In recent years, Mr. Chase has experienced low water pressure in his well. In Spring 2000, Mr. Chase contacted the District to complain that when an adjacent citrus grove was irrigating the groves, it appeared to affect the water level in his well such that the well's ability to flow was impacted. (According to Mr. Chase, his neighbors have had problems obtaining sufficient water from their wells and reaching water with standard pumps.) This citrus grove is an existing legal user of water that pre-existed Mr. Chase's well. In recent years, numerous domestic wells have been constructed in the vicinity of the Chase home that are large diameter wells utilizing submersible pumps with 110-volt AC power. These wells are more efficient at producing water than the type of well and pump being used by Mr. Chase, are located within a few hundred feet of Mr. Chase's well, and are open to the intermediate aquifer as is the Chase well. Based upon the District's experience in other areas, where there is a cluster of domestic wells drawing from the same intermediate aquifer, such adjacent wells have a much greater impact on each other than do other more distant wells, such as the previously discussed citrus irrigation wells, that are open solely to the confined Upper Floridan Aquifer System. This conclusion is based upon monitoring of the ROMP sites in the affected areas. Mr. Chase's well is approximately ten miles from the proposed withdrawal site. There is no basis to conclude that the proposed water use will cause any adverse impacts to Mr. Chase's well. DCAP members' interests are not affected any differently by the proposed use than are the interests of the general public. DCAP has produced no evidence to support its assertion that the issuance of this permit will result in lowered water levels in the Horse Creek and Peace River or other surface waters. DCAP has produced no evidence to support its assertion that the permit will cause adverse impacts to surface water flows or surface waters or to environmental features such as vegetation, fish, and wildlife. DCAP has produced no evidence that its substantial interests are affected by the proposed agency action.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that Southwest Florida Water Management District enter a final order: Determining that Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc., have satisfied the requirements of Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, regarding conditions for issuance of WUPs;3 Issuing proposed General Water Use Permit No. 20012185.000, as set forth in District Exhibit No. 4; and Finding that DCAP lacks standing to challenge the issuance of the permit. DONE AND ENTERED this 3rd day of June, 2002, in Tallahassee, Leon County, Florida. CHARLES A. STAMPELOS Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 3rd day of June, 2002.

Florida Laws (6) 120.569120.57373.019373.042373.223403.412
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SEACOAST UTILITY AUTHORITY vs PGA NATIONAL GOLF CLUB AND SPORTS CENTER, LTD., AND SOUTH FLORIDA WATER MANAGEMENT DISTRICT, 94-002903 (1994)
Division of Administrative Hearings, Florida Filed:West Palm Beach, Florida May 24, 1994 Number: 94-002903 Latest Update: Apr. 24, 1995

The Issue The issue in this case is whether Seacoast Utility Authority's challenge to the South Florida Water Management District's proposed issuance of a water use permit to PGA National Golf Club and Sports Center, Ltd. in a critical water supply area should be upheld. As discussed below, the parties have stipulated that, in deciding to issue the permit, the South Florida Water Management District has not evaluated or considered whether the use of reclaimed water was either economically, environmentally or technically infeasible.

Findings Of Fact Based upon the evidence adduced at the hearing and the entire record in this proceeding, the following findings of fact are made: Seacoast is a publicly owned water and sewer utility which operates a wastewater treatment facility in Palm Beach County, Florida. Seacoast's service area is bounded on the south by Riviera Beach and on the north by the Town of Jupiter. Seacoast operates four treatment plants: two water plants and two wastewater plants. Seacoast's regional wastewater facility currently generates approximately six (6) million gallons per day ("MGD") of reclaimed water and is permitted by the Florida Department of Environmental Protection ("DEP") as an eight (8) MGD wastewater treatment plant. As discussed in more detail in the Conclusions of Law below, the Florida Legislature and DEP have sought to encourage the reuse of reclaimed water. This policy is one of the many sometimes competing goals that are supposed to be taken into account in the water use permitting process. Until a few years ago, the treated effluent from one of Seacoast's wastewater plants was directly discharged to nearby surfacewater. During the last four years, Seacoast installed a pumping station and five miles worth of transmission lines to deliver all of its treated effluent to its regional wastewater facility. Seacoast claims that these efforts were prompted by its interpretation of changing regulations and a perceived regulatory preference for reuse of water.1 Although Seacoast claims that there has been a change in regulatory emphasis in favor of reuse of reclaimed water, Seacoast is not under a mandate from any court or agency to sell or utilize any specific amount of reclaimed water. It does appear that a deep injection well used by Seacoast for disposal of wastewater is not or was not operating as designed. Seacoast was apparently obligated to construct reclaimed water facilities at its wastewater treatment plant as part of its permit from DEP for the injection well. There was no requirement that the reclaimed water be sold or otherwise utilized. The intended primary disposal for Seacoast's reclaimed water is reuse.2 Seacoast's wastewater treatment plant provides irrigation quality reclaimed water. Seacoast tries to sell the reclaimed water for irrigation use in an effort to recoup the costs incurred in constructing the facilities necessary to reclaim the water. Backup disposal is achieved through injection down a 3300 feet deep injection well into the boulder zone. Once the reclaimed water is injected down the well, it is unavailable for reuse. The evidence suggests that there are other possible utilizations available for Seacoast's reclaimed water including sale to another utility and/or backup recharge to preserve wetlands during periods of high pumpage. For example, Seacoast is apparently in the process of applying for the necessary permits to utilize a portion of its reclaimed water to prevent harm to wetlands adjacent to its Hood Road Well Field by constructing an hydraulic barrier. At all times pertinent to this proceeding, only approximately 1.2 MGD of the reclaimed water generated by Seacoast was being reused. The remaining approximately 5 MGD was disposed of through the injection well. PGA owns and operates three (3) golf courses in Palm Beach County within Seacoast's service area. PGA's golf courses are located within an area that has been designated by the District as a Critical Water Supply Problem Area. Critical Water Supply Problems Areas are geographical regions where the available water supply due to the potential for saltwater intrusion, wetland impacts, or impacts to existing legal uses, is predicted not to meet water demands that are projected during the next 20 years. See, Chapter 40E-23, Florida Administrative Code. The use of reclaimed water is not mandated in such areas. However, the District's Rules seek to insure the optimal utilization of alternative sources of water in such areas to minimize the potential harm to water resources. It is not clear from the evidence presented in this case when PGA first obtained the Permit from the District for golf course irrigation. The Permit allows PGA to use the groundwater table as the source of water for its irrigation. Before its expiration, PGA timely sought renewal of the Permit. On April 12, 1994, the District staff recommended renewal of PGA's Permit. The staff recommendation would allow PGA to continue using the groundwater table as the source of its water. The recommendation did not contain a requirement for PGA to use any reclaimed water as part of its golf course irrigation system. Seacoast became aware of PGA's application to renew its Permit through a routine review of all water use permit applications made to the District by "potential reclaimed water users in [its] service area." Seacoast filed a Petition for Formal Administrative Hearing challenging the District staff's recommendation to renew PGA's Permit. In its Petition, Seacoast alleged that its substantial interests would be affected by the renewal of the Permit because Seacoast's ability to achieve the State of Florida's goals of conservation and environmental protection depends upon PGA, and other similar country clubs, being required to consume reclaimed water. Seacoast contends that the staff recommendation immediately eliminates a major potential consumer of Seacoast's reclaimed water which purportedly impairs Seacoast's ability to meet state objectives for reuse of reclaimed water and results in the undesirable continued disposal of reclaimed water via deep well injection. In connection with its challenge to the proposed renewal of PGA's Permit, Seacoast has stipulated that PGA's proposed withdrawals from the groundwater table would not cause harm to the water resources of the District. Seacoast also admits that it has never evaluated whether it would be environmentally injured by PGA's withdrawals from the groundwater table and/or whether the proposed use by PGA is wasteful. The District does not currently have any goals for the utilization of reclaimed water on a regional basis. Instead, the District oversight of the utilization of reclaimed water is done on a permit by permit basis. As a general policy, the District will not accept a water use permit application in an area of critical water shortage unless a reuse feasibility determination is included. The District's rules do not currently contain any guidelines as to how the determination of feasibility is to be made, nor are there any criteria for reviewing an applicant's determination of feasibility. As discussed below, the District does not even consider the applicant's reuse feasibility determination unless the proposed withdrawal is projected to result in harm to the resources of the District. Even when harm to a resource is projected, the District accepts an applicant's feasibility determination regarding the use of reclaimed water without question or analysis. For the other consumptive use criteria set forth in Rule 40E-2.301, the District independently evaluates the applicant's conclusions to confirm that they are reasonable. In other words, the District treats reclaimed water as an alternative source of water in the event that an applicant's proposed water use is projected to cause harm to the water resources of the District. If no harm is expected to occur to water resources as a result of a proposed use, the District does not review the applicant's determination of whether or not to use reclaimed water. If harm is projected, the applicant is required to look at alternatives like water conservation or utilization of water sources other than those proposed (such as reclaimed water). The applicant is free to select any alternative that mitigates the harm. Thus, even in a Critical Water Supply Area, an applicant can mitigate concerns about harm to the resource without utilizing reclaimed water. In sum, under the District's current procedures, the use of reclaimed water is never required. It is simply one alternative an applicant can utilize to offset or mitigate projected harm to water resources (such as saltwater intrusion, contamination, wetland drawdowns or existing legal use impacts) from a proposed withdrawal. Even when the District staff concludes that an applicant's proposed use will result in harm to water resources, the staff does not critically review the applicant's determination of whether the use of reclaimed water is economically, environmentally, or technically infeasible. With respect to PGA's Permit, the District staff concluded that no harm to the resource was predicted as a result of PGA's proposed use. Thus, PGA's determination not to use reclaimed water was not evaluated or even considered. The District explains that its implementation of the permitting program is based upon its interpretation that its primary responsibility is to prevent harm to water resources. The District points out that there are a number of factors to be considered in utilizing reclaimed water. These factors include, but are not limited to, the cost of the reclaimed water, the cost of retrofitting an irrigation system, the long-term availability of the reclaimed supply and the availability of a back-up supply.

Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the South Florida Water Management District enter a Final Order dismissing the Petition filed by Seacoast challenging the renewal of Permit Number 50-00617-W to PGA for golf course irrigation. DONE AND ENTERED in Tallahassee, Leon County, Florida, this 6th day of February 1995. J. STEPHEN MENTON Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 6th day of February 1995.

Florida Laws (6) 120.57373.019373.219373.223373.250403.064 Florida Administrative Code (1) 40E-2.301
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CITY OF LAKELAND vs SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT, 07-000564 (2007)
Division of Administrative Hearings, Florida Filed:Lakeland, Florida Feb. 01, 2007 Number: 07-000564 Latest Update: Apr. 07, 2008

The Issue The issue is whether the Southwest Florida Water Management District (District) should issue water use permit (WUP) No. 2004912.006 to the City of Lakeland (City), and if so, how much water should be allocated under the permit and what conditions should be imposed on the allocation, particularly in regard to withdrawals from the City's Northeast Wellfield (NEWF).

Findings Of Fact Introduction This is an unusual case in that the District gave notice of its intent to issue a permit that the City does not want and that the District staff testified that the City is not even entitled to based upon the information submitted prior to and at the final hearing. That said, there is no disagreement between the parties that a permit should be issued to the City. Indeed, despite the District Staff's testimony that the City failed to provide “reasonable assurances” prior to or at the final hearing on a variety of issues, the District takes the position in its PRO that a permit should be issued to the City, subject to various conditions and limitations. There is also no disagreement between the parties that the permit should include an allocation of 28.03 mgd from the City’s Northwest Wellfield (NWWF). The main areas of disagreement between the District and the City are the duration of the permit; the total allocation of water under the permit; and, perhaps most significant, the total allocation from the NEWF. Parties The City is an incorporated municipality located in Polk County. The City is within the boundaries of the District and is within the Southern Water Use Caution Area (SWUCA) designated by the District. The City is the applicant for the WUP at issue in this case, No. 20004912.006. The City operates a public water utility that provides potable water and wastewater services to customers in and around the City. The utility’s water service area extends beyond the City limits into surrounding unincorporated areas of Polk County. The District is the administrative agency responsible for conservation, protection, management and control of the water resources within its geographic boundaries pursuant to Chapter 373, Florida Statutes, and Florida Administrative Code Rule Chapter 40D. The District is responsible for reviewing and taking final agency action on the WUP at issue in this case. Stipulated Facts The parties stipulated that the City’s substantial interests have been adversely affected by the District’s intent to issue the proposed permit, and that the proposed permit is different from the permit that the City applied for. The parties also stipulated that there is reasonable assurance that the City’s proposed water use will not interfere with a reservation of water as set forth in Florida Administrative Code Rule 40D-2.302; that the proposed use will not significantly induce saline water intrusion; that the proposed use will incorporate the use of alternative water supplies to the greatest extent practicable; and that the proposed use will not cause water to go to waste. The City’s Wellfields Overview The City obtains the water that its water utility provides to its customers from two wellfields, the NWWF and the NEWF. The NWWF is located north of Lake Parker in close proximity to Interstate 4 and Kathleen Road. It provides water to the Williams Water Treatment Plant, from which the water is distributed throughout the City water utility’s service area. The NWWF is located on the Lakeland Ridge, which is a geographic feature that is approximately 250 to 260 feet above sea level. The Lakeland Ridge has a thick clay intermediate confining unit that isolates the surficial aquifer from the underlying aquifers. The NEWF is located to the north of Interstate 4, adjacent to Old Polk City Road. It provides water to the Combee Water Treatment Plant (Combee), from which the water is distributed throughout the City water utility’s service area. The NEWF is located at an elevation of approximately 135 feet above sea level. The surficial aquifer at the NEWF is relatively thin, and the intermediate confining unit at the NEWF is not as thick as it is at the NWWF. The Upper Floridan Aquifer (UFA) begins at approximately 65 below land surface at the NEWF. The City’s water treatment plants are traditional lime softening plants and are not able to treat brackish groundwater or surface water to the extent necessary for human consumption. It would be cost-prohibitive to implement a process to treat brackish water at the plants. Relevant Permitting History The City’s water utility has been in operation for more than 100 years, and the NWWF has been in operation since at least the early 1980’s. The earliest permit for the NWWF contained in the record is permit No. 204912, which was issued by the District in January 1987. The permit authorized average annual withdrawals of 28.3 mgd, and had an expiration date of January 1993. The NEWF was first permitted by the District in December 1989. The permit, No. 209795.00, authorized the City to pump an average of 9.0 mgd from the NEWF. The permit had a six-year duration, with a December 1995 expiration date. The permits for the NWWF and the NEWF were combined into a single permit in October 1993. The permit, No. 204912.03, authorized the City to pump a total of 28.1 mgd, with 9.0 mgd from the NEWF. The permit had a 10-year duration, with an October 2003 expiration date. In December 2002, the City's WUP was administratively modified pursuant to the District’s SWUCA rules. The modified permit, No. 20004912.004, did not change the permitted quantities at the NEWF or the 2003 expiration date, but the total allocation was reduced to 28.03 mgd. In October 2003, prior to the expiration of the existing permit, the City submitted an application to renew and modify its WUP permit. The application requested a 20-year permit with a total allocation of 32.8 mgd, with up to 16.0 mgd from the NEWF. During the permit review process, the City amended its application to increase the requested total allocation by 4.0 mgd (from 32.8 mgd to 36.8 mgd) and to decrease the requested duration of the permit by five years (from 2023 to 2018). The 36.8 mgd requested by the City was to be allocated between the NWWF (28.03 mgd) and the NEWF (8.77 mgd). The City supplemented its application during the permit review process in response to multiple requests for additional information and clarification from the District. The information provided by the City in support of the application is extensive; the “permit file” received into evidence consisted of approximately 2,500 pages, and the entire file is approximately twice that size.2 The review process culminated in what the District staff considered to be a “negotiated permit”3 that would initially authorize pumping of 33.03 mgd, with 28.03 from the NWWF, 1.5 mgd from the NEWF, and 3.5 mgd from a production well to be constructed at Combee. The proposed permit includes a phasing schedule that would allow for increased withdrawals -- up to 35.03 mgd total and 4.0 mgd from the NEWF4 -- if the City is able to demonstrate to the District’s satisfaction that the increased pumping will not cause adverse environmental impacts. The District gave notice of its intent to issue the proposed permit on December 29, 2006, and the permit was placed on the “consent agenda” for the District Governing Board’s meeting on January 30, 2007. On January 23, 2007, before the proposed permit was considered by the Governing Board,5 the City timely filed a petition challenging the proposed permit. The petition alleges that the proposed permit does not allocate sufficient water to meet the City's projected population demands in 2018 and that it does not allocate water quantities from the NEWF and the NWWF in the manner requested by the City. The NEWF The NEWF is approximately 880 acres in size. Wetlands comprise approximately half of the site. The NEWF is located within the boundaries of the Green Swamp, which is an area of critical state concern (ACSC) designated under Chapter 380, Florida Statutes. The Green Swamp is a hydrologically and environmentally important feature of central Florida encompassing thousands of acres of cypress wetlands, marshes, and forests. In 1992, a task force recommended that public water supply wellfields “of capacity greater than 1.8 mgd (average 3.6 mgd maximum)” from the UFA be discouraged in the Green Swamp ACSC in favor of wells from the Lower Floridan Aquifer in order to “mitigate drawdown impacts to the surficial aquifer system and resulting dehydration of wetlands . . . .” There is no evidence of that recommendation being formally adopted by the District or any other governmental agency, and the District does not have more stringent permitting criteria for WUP applications in the Green Swamp, except that it considers potential adverse impacts to all isolated wetlands and not just those larger than one-half acre in size.6 The City installed five 16-inch production wells at the NEWF, along with a number of associated monitoring wells. The production wells, which are cased to approximately 120 feet with a total depth of approximately 750 feet, pump water from the UFA. Pumping at the NEWF started in October 2005. The City has been pumping 4.0 mgd from the NEWF since that time. The City has spent over $34 million to bring the NEWF into service. The costs directly related to the acquisition of the NEWF site and the installation of the wells at the site account for approximately $7.6 million of that amount; the remainder of the costs are for associated infrastructure, such as the installation of water lines from the NEWF site and the construction of Combee. The wetlands on the NEWF site are predominantly isolated cypress wetlands, although there are some connected systems. Isolated wetlands are more susceptible to impacts from water deprivation than are connected wetland systems. The uplands on the NEWF site consist primarily of open pasture and fields and areas of planted pines. Extensive drainage improvements were constructed on the NEWF site between 1941 and 1980 when the site was being used as improved pastureland for cattle grazing and managed woodland for logging and silviculture. The improvements included the construction of a network of drainage ditches, culverts, roads, a grass landing strip, and a gas pipeline. The intent and effect of the drainage improvements was to remove surface water from the onsite wetlands. Historical aerial photographs show that these efforts were successful. The wetlands on the NEWF were adversely impacted by the drainage improvements, but for the most part, they are still functioning, albeit low-quality wetlands. The extensive ditching on the NEWF site continues to have an adverse impact on the wetlands even though the ditches have not been maintained and do not function as efficiently as they once did. The planted pine trees on the NEWF site may also be adversely affecting the wetlands through increased evapotranspiration from the surficial aquifer. However, the evidence was not persuasive regarding the extent of the impact from evapotranspiration. The present condition of the wetlands at the NEWF is not the result of recent activity. The biological indicators in the wetlands (e.g., adventitious roots on cypress trunks, large oak trees in the wetlands, red maple trees in areas that had at one time been dominated by cypress trees) show that the degraded condition of the wetlands dates back decades. The progressive draining and degradation of the wetlands caused by the ditching and other drainage improvements constructed on the NEWF site is apparent in the historic aerial photographs of the site. The size of the wetlands and the “hydrologic signatures” (e.g., standing water around the rims of wetlands and across the site, extensive cypress canopies, etc.) visible on earlier aerial photographs are less visible or non- existent in more recent aerial photographs. The wetlands on the NEWF site have shown no biological indicators of impacts from the pumping at the NEWF that started in October 2005. This does not necessarily mean that the pumping is not impacting the wetlands because the parties' experts agree that it can take many years for such biological indicators to appear. The more persuasive evidence establishes that the historical drainage improvements on the NEWF site were the primary cause of the degraded condition of the wetlands.7 The more persuasive evidence also establishes that unless altered, the drainage improvements on the NEWF site will continue to have an adverse effect on the wetlands. The City proposed a conceptual Wetland Improvement Plan (WIP) that is designed to restore and enhance the wetlands on the NEWF. A central component of the WIP is the reengineering and alteration of the drainage features by installing “ditch blocks” in some areas and culverts in other areas. The WIP also includes not replanting the pine trees on the NEWF site once the existing planted pines are harvested. The ditch blocks and other modifications to the drainage features are intended to hold water on the NEWF site and redirect it to the wetlands. This will help to hydrate the wetlands, increase soil moisture levels, and allow more water to percolate into the surficial aquifer following rain events. The District staff expressed some concerns with the City’s WIP at the final hearing, but acknowledged that the plan’s “conception . . . has a lot of merit.” Indeed, in its PRO, the District recommends the “installation of ditch blocks and similar measures at the [NEWF] site.” The WIP, if properly implemented, has the potential to enhance the wetlands by returning them to a more natural condition. The City will likely need an Environmental Resource Permit (ERP) from the District before any system of ditch blocks can be installed. The details of the WIP can be worked out during the ERP permitting process.8 A good monitoring plan is part of providing reasonable assurances. The parties agree that a monitoring plan should be included as a permit condition, and the EMMPs attached to the parties’ respective PROs appear to be materially the same. The City has monitored the wetlands at the NEWF since 1994, pursuant to a specific condition in the 1993 WUP permit. The methodology used by the City to monitor the wetlands was approved by the District, and despite the fact that the City has submitted biannual monitoring reports to the District for almost 14 years, the District expressed no concerns regarding the methodology or results of the monitoring until recently. The District commenced its own wetland assessment procedure at the NEWF in May 2007, which included setting “normal pools” in several of the wetlands. “Normal pool” describes the level at which water stands in a wetland in most years for long enough during the wet season to create biological indicators of the presence of water. The establishment of normal pools was part of the District’s efforts to establish the “existing natural system” against which any post-withdrawal adverse impacts at the NEWF would be measured in accordance with Section 4.2 of the Basis of Review for Water Use Permit Applications (BOR).9 Normal pools could not be established in several of the wetlands because there was no measurable standing water above the surface in the wetland. District staff observed similar conditions –- i.e., no standing water in the wetlands –- on at least one occasion following a significant rain event prior to the start of pumping at the NEWF. The District does not have a rule governing the setting of normal pools, but the City’s experts did not take issue with the normal pools set by the District or the methodology used by the District to set the normal pools. The EMMP proposed by the City is an extensive monitoring plan that incorporates a series of onsite monitoring wells, wetland monitoring stations for vegetation and hydrogeology, monitoring of pumping rates and pumping data, and monitoring of rainfall data. The EMMP will make use of the extensive data that has been collected on the NEWF site since the 1990’s as well as the normal pools set by the District, and if properly implemented, the EMMP will detect any potential adverse impacts as they occur to allow for remedial mitigation. The District staff acknowledged at the final hearing that the EMMP proposed by the City “with some minor modifications” is an appropriate plan to monitor changes in the wetlands at the NEWF. The necessary "minor modifications" were not explained at the final hearing, and as noted above, there does not appear to be any material difference in the EMMPs attached to the parties’ respective PROs. The Green Swamp is generally viewed as a “leaky” area, with little or no confinement between the surficial aquifer and the Floridan aquifer. Regional data, including studies by the United States Geologic Survey (USGS) and the District, reflect that the NEWF is located in a “transitional area” between areas of little or no confinement to the north, northwest, and east of the NEWF and areas of thicker confinement to the south. However, at least one study (published in 1977 USGS report) shows the NEWF in an area designated as "poor" for its relative potential for downward leakage. Regional data may be used to gain knowledge about the aquifer properties at a potential well site, but such data is not a valid substitute site-specific data. Indeed, the location of the NEWF in a “transitional area” makes site-specific data even more important. The City used geologic cross-sections (e.g., soil borings and core samples) at the NEWF to determine the site’s lithologic characteristics. By contrast, the District relied primarily on USGS reports and other regional data to postulate as to the lithologic characteristics of the NEWF. As a result, the City’s position regarding the lithologic characteristics of the NEWF was more persuasive than the District’s position. The lithology of the NEWF site consists of a shallow, sandy surficial aquifer, which extends to a depth of 3 to 5 feet, proceeding downward to sandy clay and clay sand semi- confining layers, alternating with impermeable clay units, interspersed with an intermediate aquifer composed of sandy clays and clay sands that contain water, proceeding downward to the limestone of the UFA. The presence of clay layers between the intermediate aquifer and the UFA, together with clay layers between the intermediate aquifer and the surficial aquifer, provide two layers of protection between the pumped aquifer and the surficial aquifer and wetlands, and serve to ameliorate any impacts to the surficial aquifer caused by withdrawals from the UFA. “Leakance” is a measure of vertical conductivity that describes the rate at which water flows through a confining unit. As a result, leakance is one of the most important factors to consider when modeling surficial aquifer impacts and potential wetland impacts from groundwater pumping. Generally, a higher leakance value is an indication of a “leakier” system with less confinement between the surficial aquifer and the UFA. The “leakier” the system, the greater the impacts of pumping on the surficial aquifer will be. The District contends that the confining unit underlying the NEWF is “leaky” and that the pumping at the NEWF is likely to directly and adversely affect the onsite wetlands. However, the more persuasive evidence establishes that the lower leakance value derived by the City based upon the site-specific lithology of the NEWF and the data from the aquifer performance tests (APTs) conducted at the NEWF is more accurate than the higher leakance value urged by the District. The purpose of an APT is to determine the hydrologic parameters of an aquifer. In particular, an APT is used to determine the transmissivity, leakance, and storage values of the aquifer. Transmissivity is a measure of how easily water flows through the ground, and storage is a measure of the amount of water in the porous spaces of the aquifer. Generally, a higher transmissivity value and a lower storage value indicate better confinement. There have been three APTs conducted at the NEWF. The first APT (APT-1) was conducted in 1989 as part of the initial permitting of the NEWF. A high transmissivity value and a low storage value were calculated in APT-1. A leakance value was not calculated. The results of APT-1 were presented to the District to justify the City’s request to pump 9.0 mgd from the NEWF, which the District approved. The 1993 permit combining the NWWF and the NEWF required the City to conduct a long-term APT in order to “determine the leakance parameter between the surficial and intermediate aquifers and the leakance parameter between the intermediate and Upper Floridan aquifers.” The permit stated that if the hydrologic parameters obtained in the APT were different from those used in the model submitted in support of the initial WUP, the City would have to revise the model and, if necessary, modify the WUP to reduce withdrawals. This second APT (APT-2) was a seven-day test conducted by the City in January 2001 in accordance with a methodology approved by the District. An “exceedingly low” leakance value of 4.5 x 10-4 gallons per day per cubic foot was calculated in APT-2. The transmissivity and storage values calculated in APT- 2 were essentially the same as the values calculated in APT-1. The District expressed concerns with the results of APT-2, and in December 2001, the District advised the City that it should “proceed with caution during the planning of infrastructure (pipelines) for the [NEWF]” because the “wellfield may not be able to produce the volume of water the City has stated that would like from the wellfield, without causing adverse impacts.”10 Based upon these concerns, the District conducted an APT (APT-3) at the NEWF in April and May 2003. The parties’ experts agree that data from APT-3 is reliable, but the experts disagree in their interpretation of the data, particularly in regards to the leakance value. The City’s experts calculated a leakance value of 1.4 x 10-4 feet per day per foot, which is a low leakance value. The expert presented by the District, Dann Yobbi, calculated a higher leakance value of 3.4 x 10-3 feet per day per foot, which suggests relatively “leaky” aquifer. The leakance value calculated by the City’s experts is more persuasive than the value calculated by Mr. Yobbi because Mr. Yobbi did not “de-trend” the data from APT-3 based upon the general declines in water levels occurring at the time of APT-3. Indeed, Mr. Yobbi testified that he is in the process of revising his report on APT-3 to address this issue and he acknowledged that the surficial aquifer showed only a “slight response” to the pumping during APT-3. The leakance value calculated by the City’s experts in APT-3 is consistent with the leakance value calculated in APT-2. The transmissivity and storage values calculated in APT-3 are also consistent with the values calculated in APT-1 and APT-2. The reliability of the leakance values and other aquifer parameters calculated by the City’s experts for the NEWF is confirmed by water level data compiled by the City pursuant to the monitoring requirements in the existing WUP. The water level data was collected from monitoring wells at the NEWF in the surficial aquifer, the intermediate aquifer, and the UFA. The City began collecting this data in 1994 and it continues to collect and report the data to the District as required by the existing WUP. The water level monitoring data reflects that the surficial aquifer at the NEWF responds almost immediately to rain events. By contrast, the intermediate aquifer and UFA show a more subdued response to rainfall events, which is indicative of good confinement, especially between the UFA and the surficial aquifer. The water level monitoring data shows that rainfall or lack of rainfall is the major controlling factor relative to the rate of surficial aquifer recharge at the NEWF. The water level monitoring data since pumping began at the NEWF shows that the pumping at 4.0 mgd is having a minimal impact on the surficial aquifer at the NEWF. Indeed, the more persuasive evidence establishes that the general decline in water levels that has been observed in the monitoring wells at the NEWF over the past several years is more likely than not attributable to the severe drought in the area and the onsite drainage features, and not the pumping at the NEWF.11 Moreover, the more persuasive evidence shows that following the start of pumping at the NEWF in October 2005, the water levels in the surficial, intermediate, and Floridan aquifers returned to the historic patterns of up and down response to rainfall events shown throughout the thirteen-year period of record: the surficial aquifer fills quickly (as it receives the rainwater directly) and empties quickly (through a combination of surface drainage, evapotranspiration, evaporation, and leakage), while the UFA responds with more gradual rising and falling (as water enters the aquifer through recharge areas and slowly percolates into the aquifer through more confined areas). The analysis of the water level data collected during APT-3 showed a similar trend in the rates of decline in the surficial aquifer as were reflected in the hydrographic record of the monitoring well data collected by the City since 1994. The natural, post-rainfall rate of decline under non-pumping conditions was consistent with the rate of decline observed during pumping conditions in APT-3. In sum, the interpretation of the water level data by the City’s experts was more persuasive than the interpretation by the District’s experts. Modeling of Predicted Drawdowns and Impacts The City utilized two different models to predict drawdowns from the proposed pumping at the NWWF and NEWF: the USGS “Mega Model” and the District’s District-Wide Regulation Model (DWRM). The models incorporated regional data published by the USGS and the District as well as site-specific data from the NEWF, including the lithologic information collected through soil borings and the hydrologic parameters of the aquifers calculated in APT-3. The models were calibrated and de-trended to remove “background conditions” (e.g., regional water level declines) so that the models would only show the predicted effects of the pumping. Once the calibration was complete, the models were run to simulate the effect of the pumping on the groundwater flows in the area. The models produced contour maps that showed the predicted drawdowns in the surficial aquifer as a result of the pumping. The USGS Mega Model predicted that pumping the NEWF at 8.77 mgd would result in drawdowns of approximately 0.5 foot in the surficial aquifer in and around the NEWF. The DWRM model predicted a 0.18 foot drawdown in the surficial aquifer in and around the NEWF when pumping the NEWF at 4.0 mgd, and a drawdown of 0.4 foot when pumping at 8.77 mgd. The same models were used to predict the “cumulative” drawdowns by taking into account pumping by existing legal users as well as the pumping at the NWWF. The cumulative models assumed pumping of 36.8 mgd from the City’s wellfields. The USGS Mega Model predicted that cumulative drawdowns in the surficial aquifer in and around the NEWF would be an additional 0.3 feet, with 8.77 mgd of pumping at the NEWF. The DWRM model predicted that the cumulative drawdowns in the surficial aquifer in and around the NEWF would be 0.4 foot with 4.0 mgd of pumping at the NEWF, and 0.6 foot at 8.77 mgd of pumping at the NEWF. The City utilized the 1995 data set of existing legal users in its cumulative DWRM modeling because that was the data set provided by the District. The difference between the 1995 data set and the more current 2002 data set is on the order of 20 mgd, which is inconsequential in comparison to the 1.1 billion gallons per day of withdrawals included in the model that are spread over the geographic extent of the District. The predicted drawdowns in the surficial aquifers in and around the NEWF would be considerably greater if the hydrologic parameters calculated by Mr. Yobbi were used in the DWRM model. For example, the District’s modeling predicted drawdowns between 1.0 and 1.2 feet in the surficial aquifer in and around the NEWF when pumping 1.5 mgd from the NEWF, 3.5 mgd from Combee, and 28.03 mgd from the NWWF. The wetlands experts presented by the parties agreed that the level of drawdown predicted by the City at the NEWF has the potential to adversely impact the wetlands on the site. The experts also agreed that there is no bright line as to the amount of drawdown that will adversely impact the wetlands. The City’s expert, Dr. Michael Dennis, testified that drawdowns in the surficial aquifer between 0.18 foot and 0.5 foot “probably” would not affect the wetlands at all, or at least “not measurably.” He also testified that drawdowns between 0.5 foot and one foot “are the drawdowns that you need to be concerned about.” The District’s expert, John Emery, testified that a drawdown in the surficial aquifer of 0.4 foot “could” adversely affect the wetlands if no mitigation is provided, but that a drawdown of 0.2 to 0.3 foot might not.12 The WIP is expected to increase the amount of water that gets to the wetlands on the NEWF site. However, the extent to which the WIP will increase the water levels in the wetlands and offset the predicted drawdowns in the surficial aquifer is unknown at this point. Limiting pumping at the NEWF to 4.0 mgd is reasonable and prudent based upon the uncertainty regarding the effectiveness of the WIP and the experts’ testimony regarding the level of drawdowns that likely would, and would not, adversely affect the wetlands at the NEWF. In sum, the more persuasive evidence establishes that the drawdown predicted at 4.0 mgd of pumping –- 0.18 foot (individually) and 0.4 feet (cumulatively) –- is not likely to adversely impact the already significantly degraded wetlands at the NEWF, particularly if the WIP is properly implemented. Demand Projections The City did not use the full 28 mgd allocated under its existing WUP. It pumped only 21 mgd in the 12 months preceding October 2003, when the permit was scheduled to expire; it pumped only 26 mgd in 2006; and the pumping for 2007 was expected to be approximately 1 mgd lower than the pumping in 2006. The City's WUP application contained population and demand projections for different years in the future. For 2014 (the permit expiration date proposed by the District), the “functional population”13 of the service area was projected to be 183,264 and the average demand was projected to be 29.5 mgd; for 2023 (the original permit expiration date requested by the City), the projections were 203,721 people and 32.8 mgd; and for 2018 (the permit expiration date now requested by the City), the projections were 192,176 people and 30.9 mgd. The projections in the WUP application were prepared in 2003, and City's primary consultant, Charles Drake, testified that the data was “accurate” and “reliable.” However, more recent data shows that the population projections in the WUP application were slightly understated. The more recent data is contained in the “Water Services Territory Population Estimates and Projections” reports prepared by the City's utility department in March 2006 and March 2007. The reports include estimates of the functional population for prior years, and projections of the functional population for future years. The estimates reflect the “actual” population for a given year in the past, whereas the projections reflect the “expected” population for future years. The estimates and projections in these reports, like the projections in the WUP application, were prepared in accordance with the methodology contained in the BOR. The District did not take issue with the projections in the reports or the WUP application. The estimated functional population of the service area in 2003, 2004, 2005, and 2006 exceeded the population projected for those years in the WUP application. On average, the projected populations for each year understated the “actual” populations by approximately 3,500 persons.14 Likewise, the population projections for future years in the March 2007 report are higher than the population projections for the same years in the WUP application. For example, the report projects that the functional population of the service area in 2014 will be 191,208 (as compared to 183,264 in the WUP application), and that population in 2018 will be 203,247 (as compared to 192,176 in the WUP application). The City presented “revised” population projections at the final hearing in City Exhibit 140. The revised projections were based on the projections in the March 2006 report, but also included data from the “water allocation waiting list” that is part of the City’s concurrency management system that was created by the City in response to legislation passed in 2005 requiring local governments to allocate and approve requests for water for new development. The population projections in City Exhibit 140 are 234,959 in 2014; 247,390 in 2018; and 264,556 in 2023. These projections include an additional 43,471 persons related to new development in the concurrency management system, as well as the additional 2,600 to 3,000 persons projected per year in the WUP application and the March 2006 report. The City failed to establish the reasonableness of the revised population projections. Indeed, among other things, the evidence was not persuasive that the additional population attributed to the new development in the concurrency management system is not already taken into account, at least in part, in the annual population increases projected in the March 2006 report.15 The most reasonable population projections for the service area of the City's utility are those in the March 2007 report.16 The record does not contain demand projections directly related to the population projections in the March 2007 report. However, demand projections for those population projections can be inferred from the WUP application (City Exhibit 1(a)(2), at 0036) and City Exhibit 140 (at page 0015). The 2014 projected population of 191,208 in the March 2007 report roughly corresponds to the projected population for 2018 in the WUP application (192,176) for which the projected demand was 30.9 mgd; and it also roughly corresponds to the projected population for 2008 in City Exhibit 140 (193,001), for which the projected demand was 28.7. Thus, in 2014, it is reasonable to expect that demand will be between 28.7 and 30.9 mgd. The 2018 projected population of 203,247 in the March 2007 report roughly corresponds to the projected population for 2023 in the WUP application (203,721) for which the projected demand was 32.8 mgd; and it also roughly corresponds to the projected population for 2009 in City Exhibit 140 (201,983), for which the projected demand was 30.2 mgd. Thus, in 2018, it is reasonable to expect that demand will be between 30.2 and 32.8 mgd. The demand projections in the WUP for 2014 (29.5 mgd) and 2018 (30.9 mgd) fall within the range inferred for the populations in the March 2007 report. Thus, even though the population projections in the WUP application for 2014 and 2018 are understated, the demand projections for those years in the WUP are still reasonable. The demand projections in City Exhibit 140 –- 35.3 mgd in 2014 and 36.6 mgd in 2018 –- are overstated as a result of unreliable population projections upon which they are based. Other Issues Duration of Permit The 1987 permit for the NWWF had a six-year duration, as did the original 1989 permit for the NEWF. The 1993 permit had a 10-year duration, but that permit did not increase the amount of authorized withdrawals; it simply combined the authorizations for the NWWF and the NEWF into a single permit. In this case, the City is requesting a permit that expires in 2018, which was a 15-year duration at the time the application was filed, but now is a 10-year duration. The District is proposing a permit with a six-year duration, expiring in 2014. The District is authorized to approve a WUP with a duration of up to 50 years. The District’s rules provide that the duration of the permit is to be determined based upon “the degree and likelihood of potential adverse impacts to the water resource or existing users.” The District’s rules require that in order for the District to approve a permit with a duration of more than 10 years, the applicant is required to present sufficient facts to demonstrate that such a permit is “appropriate.” Section 1.9 of the BOR provides “guidelines” regarding the duration of permits. The guidelines in the BOR are not binding on the District, but the nearly identical language in Florida Administrative Code Rule 40D-2.321 is binding on the District. The BOR provides that a six-year permit is to be issued for renewal permits “with modification to increase the quantity withdrawn by more than or equal to 100,000 gpd or 10% or more of the existing permitted quantities, whichever is greater.” The BOR and Florida Administrative Code Rule 40D- 2.321(2)(b) also provide that a six-year permit is to be issued “where the potential for significant adverse impacts are predicted.” The renewal permit that the City is seeking requests an increase of 8.7 mgd (from 28.1 mgd to 36.8 mgd) over the existing permitted quantities, which exceeds the 10 percent threshold in Section 1.9 of the BOR. Moreover, there is a potential for significant adverse impact from the renewal permit that the City is seeking. Accordingly, a six-year permit is appropriate under the District’s rules and the guidelines in the BOR. The City failed to demonstrate why a longer permit duration is appropriate under the circumstances of this case. District staff testified at the final hearing that the permit term should be calculated from the date the permit is issued, which will be some point in 2008. Therefore, the permit should have an expiration date of 2014. Offsite Impacts The City used the modeling described above to predict the drawdown in the UFA from the proposed pumping in order to determine whether there will be any adverse impacts on existing legal users. The predicted drawdown in the UFA in the vicinity of the NEWF ranges from 1.6 feet to 2.4 feet with 4.0 mgd of pumping at the NEWF, and between 3.4 feet and 5 feet with pumping at 8.77 mgd. The predicted drawdown in the UFA in the vicinity of the NWWF ranges from 10.0 to 14.0 feet, with 28.03 mgd of pumping at the NWWF.17 These predicted drawdowns are not expected to have any adverse impacts on existing legal users that have wells in the UFA. Most permitted wells in the UFA use vertical turbine pumps, which can easily accommodate fluctuations in water levels of five feet or more. The City has not received any complaints from existing users since it began pumping 4.0 mgd at the NEWF in October 2005. The pumping at the NWWF, which has been ongoing for more than 20 years, has not caused any adverse impacts to existing legal users. The City is required under the existing WUP to respond to any adverse impact complaints from existing legal users, and it is required to implement mitigation, as needed. In short, City is required to do whatever is necessary (e.g., relocating or increasing capacity of pump, lowering pipes) to return any well impacted by the pumping to its prior function. The City did not evaluate the potential impacts of its proposed pumping on unpermitted wells because the District does not maintain a database of unpermitted wells. However, the City acknowledges that if its pumping impacts an unpermitted well, it will be obligated to mitigate those impacts in the same manner that it is required to mitigate impacts to existing permitted users. The predicted drawdowns for water bodies in the vicinity of the NWWF and the NEWF that have designated Minimum Flows and Levels (MFLs) -- Lake Bonny, Lake Bonnett, and the Cone Ranch wetlands -- are minimal, on the order of 0.1 foot. The City evaluated the impacts of pumping on contaminated sites listed by the Department of Environmental Protection (DEP) in the vicinity of the NWWF and NEWF. Based upon the results of the modeling conducted by the City, there is no reason to expect that pumping at the NWWF and/or NEWF will have any measurable impact on those sites or lead to pollution of the aquifer. Potential Impacts of NWWF Pumping The only concern expressed by the District with respect to the pumping at the NWWF relates to the potential environmental impacts of the pumping on Lake Bonny and Lake Bonnett. The City agreed to include those lakes in its EMMP. Combee Combee is located approximately four miles south of the NEWF. There is a relatively thick clay confining unit at Combee, which, according to the District, makes it a better location for water withdrawals than the NEWF. The District conducted an APT at Combee in 2006. The hydrologic parameters derived from the APT, and the “preliminary modeling” performed by the District show that the City may be able to withdraw at least 3.0 mgd from wells at Combee. The proposed permit authorized pumping of 3.5 mgd from Combee. The proposed permit also included a phasing schedule pursuant to which pumping at Combee would be decreased to 3.0 mgd if pumping at the NEWF reached 4.0 mgd. The City expressed an interest in obtaining water from Combee throughout the permitting process. However, the City represented at the outset of the final hearing that the Combee well is “off the table because the City wishes to maximize the withdrawal allocation from [the NEWF].” The City stated in its PRO that it is “willing to consider permitting a production well at [Combee] as a potential mitigation resource, should unexpected adverse impacts require the City to divert production to a back-up resource.” The District stated in its PRO that the Combee well is “available for mitigation purposes," and that the City “should be encouraged to apply for a WUP for withdrawals from Combee up to 3.0 mgd to provide additional mitigation for pumping from the [NEWF].” Pump rotation Rotation of pumping between the wells in a wellfield is a standard practice, and it can be an effective mitigation technique. The City utilizes well rotation programs at the NWWF and the NEWF in order to minimize the stress on the production aquifers. Rotating pumping between the production wells at the NEWF is particularly appropriate because several of the wells are located in very close proximity to wetlands. Rotating the pumping will help to minimize the potential for adverse impacts to the wetlands. The actual rotation schedule is an operational decision that is made based upon observed conditions at the wellfield site, rather than something that is typically included in the WUP. Conservation and Reuse The City has a four-tiered conservation rate structure, modeled after the District’s graduated water-rates prototype. The rate structure imposes higher unit costs as individual consumption increases, thereby discouraging wasteful uses of water. The City has a comprehensive leak detection program aimed at preventing the loss of water within the City’s water distribution system. This program has helped to reduce the per- capita per-day consumption rate for the City by reducing the volume of water that is wasted before it is delivered to the consumer. The City has implemented irrigation restrictions aimed at reducing the quantities of water used by domestic customers for lawn and garden watering. The per capita rate of water consumption is a measure of the effectiveness of a water conservation program; the lower the figure, the better. The City’s per capita rate has increased in recent years, but its adjusted gross per capita rate has decreased. The adjusted gross per capita rate takes into account “significant users,” which are defined as non-residential customers other than golf courses that use more than 25,000 gallons per day or that represent more than five percent of the utility’s annual water use.18 The City’s per capita rate in 2005 was 145.69 gallons per day, and its adjusted gross per capita rate in that year was 132.01 gallons per day. The adjusted gross per capita rate may not exceed 150 gallons per day within the SWUCA. Thus, the City will be required to continue its conservation programs (and implement additional programs, if necessary) to ensure that its adjusted gross per capita rate does not exceed 150 gallons per day over the life of the permit. A portion of the City’s treated wastewater is reused for cooling at the City’s McIntosh Power Plant pursuant to a permit from DEP under Chapter 403, Florida Statutes. The DEP permit, No. FL0039772 (Major), states in pertinent part: Industrial Reuse: Effluent is reused . . . as a non-contact cooling water at the City of Lakeland McIntosh Power Generating Plant. The volume of water used on a daily basis fluctuates on an as needed basis. There are no restrictions on the volume that can be routed to the reuse system. The power plant evaporates water in the cooling process or returns cooling water into the Glendale WWTP for final treatment in the manmade wetlands treatment system. The reuse in the power plant is not required as effluent disposal. . . . . The remainder of the City’s treated wastewater is “blended” with the water used at the power plant in order to meet the conductivity standards in the DEP permit and the conditions of certification for the power plant and/or directly discharged into an artificial wetland system that ultimately discharges to the Alafia River. Section 3.1 of the BOR (at page B3-2) provides that “Water Use Permittees within the SWUCA who generate treated domestic wastewater are encouraged to demonstrate that . . . 50% of the total annual effluent flows is beneficially reused.” (Emphasis supplied). The BOR lists a number of uses of treated wastewater that are considered to be beneficial reuse. The list includes “industrial uses for cooling water, process water and wash waters” and “environmental enhancement, including discharges to surface water to replace withdrawals.” The City’s use of treated wastewater for cooling at the McIntosh Power Plant is a beneficial reuse under the BOR. The treated wastewater directly discharged by the City into the artificial wetland system is not a beneficial reuse under the BOR because it is not replacing surface water withdrawals. The BOR requires all users within the SWUCA to investigate the feasibility of reuse, and requires the implementation of reuse “where economically, environmentally and technically feasible.” The City has not recently undertaken a study or otherwise evaluated the feasibility of increasing its reuse. The draft permit attached to the District's PRO includes a specific condition requiring the City to "provide a comprehensive study of reuse opportunities encompassing the [City's] water, wastewater, and electrical utilities systems" by January 1, 2009.

Recommendation Based upon the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the District issue WUP No. 2004912.006 with the terms and conditions contained in the draft permit attached to the District’s PRO, except that: The 2014 population referenced in the permit shall be 191,208; The adjusted gross per capita rate shall not exceed 150 gallons per day; Special Condition No. 2 shall be amended to authorize withdrawals from the NEWF at 4.0 mgd annual average and 4.8 mgd peak month, and the quantities listed in the Withdrawal Point Table for the NEWF wells shall be adjusted accordingly; Special Condition No. 4 shall be replaced with a reference to the EMMP and the conceptual WIP attached to the City’s PRO, and the list of monitoring stations in the EMMP shall be amended to include Lake Bonny and Lake Bonnet; and An additional specific condition shall be added encouraging the City to pursue a WUP for the Combee site for future water needs and/or for additional mitigation of the impacts of pumping at the NEWF. DONE AND ENTERED this 4th day of January, 2008, in Tallahassee, Leon County, Florida. S T. KENT WETHERELL, II Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 4th day of January, 2008.

Florida Laws (7) 120.569120.57132.0128.0335.03373.019373.223 Florida Administrative Code (5) 40D-2.09140D-2.30140D-2.30240D-2.32140D-2.381
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SUMTER CITIZENS AGAINST IRRESPONSIBLE DEVELOPMENT, INC.; KENNETH ROOP; AUBREY VARNUM; AND T. DANIEL FARNSWORTH vs SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT AND VILLAGES OF LAKE-SUMTER, INC., 02-001123 (2002)
Division of Administrative Hearings, Florida Filed:Bushnell, Florida Mar. 20, 2002 Number: 02-001123 Latest Update: Aug. 12, 2002

The Issue Whether proposed Water Use Permits Nos. 20012236.000 (the Potable Water Permit) and 20012239.000 (the Irrigation Permit) and proposed Environmental Resource Permit No. 43020198.001 (the ERP) should be issued by the Respondent, Southwest Florida Water Management District (the District).

Findings Of Fact The Parties The individual Petitioners, Farnsworth, Roop, and Varnum are all Florida citizens and residents of Sumter County. None of the individual Petitioners offered any evidence relating to direct impacts that the ERP would have on their property. With respect to the Potable Water and Irrigation Permits, anecdotal testimony was presented by Petitioners and Wing and Weir relating to well failures and sinkholes in the area. Two Petitioners, Roop and Varnum, live in close proximity to the property encompassed by the three permits. Petitioner Farnsworth’s property is approximately three and a half miles from the project boundary. Wing and Weir live approximately four and a half to five and 18 miles from the project site, respectively. SCAID is a Florida not-for-profit corporation that has approximately 130 members. Farnsworth, the president of SCAID, identified only Roop and Varnum as members who will be directly affected by the activities to be authorized by the permits. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries. The Utility and the Authority are limited liability companies, of which the Villages Inc. is the managing partner. The Villages Inc. is a Florida corporation. The Utility, which will serve as a provider of potable water, is regulated by the Public Service Commission, while the Authority which will provide irrigation water, is not. The Villages Inc., Development The Villages Inc. is a phased, mixed use, retirement community, which is located at the intersecting borders of Lake, Marion, and Sumter Counties. Development has been on going since at least 1983, with a current planning horizon of the year 2019. Currently, there are 15,362 constructed dwelling units in the built-out portion of the Villages Inc. that are located in Lake County and the extreme northeast corner of Sumter County. The portion located in Marion County is 60 percent complete, with 750 homes completed and another 600 under construction. Approximately another 22,000 residences are planned for development in Sumter County by the year 2012, with an additional 10,200 by the year 2019. However, the Potable Water and Irrigation Permits are only for a six-year duration, and the ERP has a duration of only six years. None of the permits authorize development activities beyond that time frame. Generally speaking, the three permits at issue include an area owned by the Villages Inc. that lies in northeast Sumter County South of County Road 466 and North of County Road 466A. However, it is not projected that this entire area will be built-out during the terms of three proposed permits. Area Hydrology and Topography In the area of the Villages Inc., there is a layer of approximately five to ten feet of sand at the land surface, which is underlain by ten to 70 feet of a clayey sand. Both of these constitute the surficial aquifer and are extremely leaky, allowing water to percolate easily through to a lower layer. Except in the vicinity of Lake Miona, there is no water in the surficial aquifer except after rainfall events. The clayey sand layer is underlain by the Upper Floridan, a limestone unit. The top of this limestone layer ("the top of the rock") occurs at fluctuating depths of between 30 and 70 feet. At approximately 350 to 400 feet below the land surface, there begins a transition to a denser unit that serves as a confining layer between the Upper Floridan production zone and the Lower Floridan production zone. This confining layer, which was confirmed by drilling at three locations in the Villages Inc. is approximately 150 feet thick in the area of the Villages Inc. Another transition, this time to a less dense formation, begins at approximately 550 to 600 feet, which is considered the top of the Lower Floridan production zone. While testing conducted on the project site indicated almost no leakage between the Upper and Lower Floridan production zones, it is generally known by experts that there is some exchange of water between the two layers. Both the Upper and the Lower Floridan contain water that meets potable water standards and both are considered water production zones. The water quality of the two zones is not significantly different. The project area is prone to karst activity, that is, the formation of sinkholes. Sinkholes are formed as a result of the collapse of the overburden above subsurface cavities which have been formed through a very gradual dissolution of limestone, thus resulting in a "sink" at the land surface. Surface water bodies in the area include Lake Miona, Black Lake, Cherry Lake, and Dry Prairie, as well as several other small wetlands. The Potable Water and Irrigation Permits The potable water permit is for the withdrawal from the Upper Floridan Aquifer of 1.164 million gallons of water per day (MGD), on an annual average, for potable use in residences and both commercial and recreational establishments. It also limits the maximum withdrawal during peak months to 2.909 MGD. The Irrigation Permit is for the withdrawal from the Lower Floridan Aquifer of 2.850 MGD, on an annual average, for use in irrigation. The peak month usage rate permissible under the proposed permit would be 9.090 MGD. Water withdrawal under the Irrigation Permit will be used for the irrigation of residential lawns, common areas, commercial landscaping, and golf courses. Modeling of Drawdowns In assessing the impacts of proposed water withdrawals from an aquifer, District personnel considered effects on the aquifers and on-surface water features in the area. Computer- generated models of the predicted effects of the Potable Water and Irrigation Permits withdrawals provided one of the principal bases for this assessment. The primary geologist assigned to review the permit applications reviewed two of the models submitted by the Utility and the Authority (jointly the WUP Applicants) and ran one personal model of her own in order to predict the effects of the proposed withdrawals on the aquifers, as well as on any wetlands and other surface water bodies. In particular, the models predict both the vertical and horizontal extent to which the withdrawals may lower the level of water within the aquifers and in-surface waters under various conditions. One of the models submitted by the WUP Applicants predicted drawdowns during a 90-day period of no rainfall while the other predicted the impacts of the withdrawals over the life of the permits, considered cumulatively with the effects of withdrawals from the already-existing Villages' development in Sumter, Marion, and Lake Counties. The District’s geologist modeled the impacts of the withdrawals over the life of the permits and included the cumulative effects of all of the current Villages' withdrawals in Sumter County. All of these models included the combined effects of both the proposed Potable Water and the Irrigation Permits. Based upon these models, it is concluded that there will be no significant drawdowns as a result of the withdrawals authorized by the proposed water use permits. Specifically, the only predicted drawdown in the surficial aquifer (0.25 feet of drawdown) is in an area where there are no natural surface water features. Drawdown in the Upper Floridan is predicted at between 0.1 and 0.2 feet, while the drawdown in the Lower Floridan is predicted at a maximum of 1.5 feet. These minor drawdowns are not expected to cause any adverse impacts. Transmissivity is the rate at which water moves horizontally through the aquifer. In areas with high transmissivity, the results of water withdrawals from an aquifer will generally be low in magnitude, but broad in lateral extent. Water withdrawals from areas of low transmissivity will result in cones of depression that are more limited in lateral extent, but steeper vertically. The use of too high a transmissivity rate in a model, would overpredict the horizontal distance of the drawdowns caused by withdrawals, but would underpredict the vertical drawdown in the immediate vicinity of the withdrawal. Conversely, use of too low a transmissivity would over-predict the effects in the immediate vicinity of the withdrawal but underpredict the lateral extent of the drawdown. The WUP Applicants’ models used a transmissivity value for the Lower Floridan Aquifer of 100,000 feet squared per day ("ft.2/d'). The WUP Applicants’ consultant derived the transmissivity values from a regional model prepared by the University of Florida. The regional model uses a transmissivity value for the entire region of 200,000 ft.2/d for the Lower Floridan. While that transmissivity is appropriate for assessing large-scale impacts, on a more localized level, the transmissivity of the aquifer may be lower. Therefore, the WUP Applicants’ consultant met with District representatives and agreed to use a value half that used in the University of Florida model. A similar approach was used for the transmissivity value used in modeling effects in the Upper Floridan. Notably, specific transmissivity values recorded in four wells in the Villages Inc. area were not used because two of these wells were only cased to a depth of just over 250 feet, with an open hole below that to a depth of 590 feet. Thus, the transmissivity measured in these wells reflect conditions in the confining layer at the immediate location of the wells - not the transmissivity of the Lower Floridan production zone. Further, site-specific information on transmissivity, measured during pump tests at individual wells, does not correlate well to the transmissivity of the aquifer, even at short distances from the well. Transmissivities measured at individual wells are used to determine the depth at which the pump should be set in the well, not to determine the transmissivity of the aquifer. Thus, the use of transmissivities derived from the regional model, but adjusted to be conservative, is entirely appropriate. Moreover, using a transmissivity in her modeling of the project impacts of 27,000 ft.2/d for the Lower Floridan Aquifer, the district geologist’s model predicted no adverse impacts. Leakance is the measure of the resistance of movement vertically through confining units of the aquifer. The leakance value used by the District for the confining layer between the Upper and Lower Floridan was taken from the University of Florida model. Tests conducted on the site actually measured even lower leakance values. Thus, the evidence establishes that the leakance value used in the WUP Applicants’ and the District’s modeling for the Floridan confining layer was reasonable and appropriate. Competent, substantial evidence also establishes that the leakance value used for Lake Miona was reasonable. The WUP Applicants submitted to the District substantial data, gathered over several years, reflecting the balance of water flowing into Lake Miona and the lake’s levels in relation to the potentiometric surface. This documentation verified the leakance value used for Lake Miona in the modeling. Finally, the District modeling used appropriate boundary condition parameters. The District modeling used what is known as the "constant head" boundary and assumes the existence of water generated off-site at the boundaries. Such a boundary simulates the discharge of the aquifer at a certain level. The use of constant head boundaries is an accepted practice. The modeling conducted on behalf of the District and the Applicants provides a reasonable assurances that the Potable Water and Irrigation Permits will not cause adverse water quality or quantity changes to surface or groundwater resources, will not cause adverse environmental impacts to natural resources, and will not cause pollution of the aquifer. Furthermore, because the predicted drawdowns are so insignificant, reasonable assurances have been provided that the withdrawals will not adversely impact existing off-site land uses or existing legal withdrawals. The modeling also provides reasonable assurances that the withdrawals will not be harmful to the water resources of the District. Moreover, monitoring requirements included in the proposed Potable Water and Irrigation Permits provide additional reasonable assurance that – should the withdrawal effects exceed those predicted by the modeling – such effects are identified and necessary steps are taken to mitigate for any potential impacts. The District has reserved the right to modify or revoke all or portions of the water use permits under certain circumstances. Specifically, the proposed Potable Water Permit requires a monitoring plan that includes the following pertinent provisions: There shall be no less than three control wetland and ten onsite wetland monitoring sites; A baseline monitoring report, outlining the current wetland conditions; * * * A statement indicating that an analysis of the water level records for area lakes, including Miona Lake, Black Lake, Cherry Lake, Lake Deaton and Lake Griffin, will be included in the annual report; A statement indicating that an analysis of the spring flow records for Gum Spring, Silver Spring, and Fenney Spring, will be included in the annual report; * * * Wildlife analyses for potentially impacted wetlands, lakes, and adjacent property owner uses or wells, including methods to determine success of the mitigation; A mitigation plan for potentially impacted wetlands, lakes, and adjacent property owner uses or wells, including methods and thresholds to determine success of the mitigation; An annual report of an analysis of the monitoring data . . . . Similar provisions are included in the proposed irrigation permit. The WUP Applicants, in conjunction with the District, have developed sites and methodologies for this monitoring. Reasonable Demand The water to be withdrawn under the proposed Potable Water Permit will serve 10,783 people. This total results from the simple multiplication of the number of residences to be built during the next six years (5,675) by the average number of residents per household (1.9). Those numbers are based upon historical absorption rates within the Villages Inc. development since 1983, an absorption rate that doubles approximately every five years. The Utility proposed a per capita use rate of 108 gallons per day for potable use only. District personnel independently verified that per capita rate, based upon current usage in the existing portions of the Villages Inc. and determined that the rate was reasonable. Based upon the population projections and the per capita rate, the District determined that there is a reasonable demand for the withdrawal of the amount of water, for potable purposes, that is reflected in the Potable Water Permit. The Utility has provided reasonable assurance regarding the Utility’s satisfaction of this permitting criterion. As to the irrigation permit, the Villages Inc. plans, within the next six years, to complete the construction of 1,911 acres of property that will require irrigation. The amount of water originally requested by the Authority for irrigation withdrawals was reduced during the course of the application process at the request of the District. The District determined the reasonable amount of irrigation water needed through the application of AGMOD, a computer model that predicts the irrigation needs of various vegetative covers. Since the Authority intends to utilize treated wastewater effluent as another source of irrigation water, the District reduced the amount of water that it would permit to be withdrawn from the Lower Floridan for irrigation. The District, thus, determined that the Authority would need 1.59 MGD annual average for recreational and aesthetic area irrigation and 1.26 MGD annual average for residential lawn irrigation, for a total of 2.85 MGD. The Villages Inc. also plans to accumulate stormwater in lined ponds for irrigation use. However, unlike its treatment of wastewater effluent, the District did not deduct accumulated stormwater from the amount of water deemed necessary for irrigation. This approach was adopted due to the inability to predict short-term rainfall amounts. The uncontroverted evidence of record establishes reasonable assurances that there is a reasonable demand for the amount of water to be withdrawn under the proposed irrigation permit. Conservation and Reuse Measures Both the Utility and the Authority applications included proposed measures for the conservation and reuse of water. The conservation plan submitted in conjunction with the irrigation permit application provides for control valves to regulate both the pressure and timing of irrigation by residential users; contractual restrictions on water use by commercial users; xeriscaping; and an irrigation control system for golf course irrigation that is designed to maximize the efficient use of water. In addition, in the proposed permits, the District requires the Utility and the Authority to expand upon these conservation measures through such measures as educational efforts, inclined block rate structures, and annual reporting to assess the success of conservation measures. The Authority also committed to reduce its dependence on groundwater withdrawals through the reuse of wastewater effluent, both from the on-site wastewater treatment facility and through contract with the City of Wildwood. Reasonable assurances have been provided that conservation measures have been incorporated and that, to the maximum extent practicable, reuse measures have been incorporated. Use of Lowest Available Quality of Water In addition to the reuse of treated wastewater effluent, the Authority intends to minimize its dependence on groundwater withdrawals for irrigation use through the reuse of stormwater accumulated in lined ponds. Thirty-one of the lined stormwater retention ponds to be constructed by the Villages Inc. are designed as a component of the irrigation system on-site. Ponds will be grouped with the individual ponds within each group linked through underground piping. There will be an electronically controlled valve in the stormwater pond at the end of the pipe that will be used to draw out water for irrigation purposes. These lined stormwater ponds serve several purposes. However, the design feature that is pertinent to the reuse of stormwater for irrigation is the inclusion of additional storage capacity below the top of the pond liner. No groundwater will be withdrawn for irrigation purposes unless the level of stormwater in these lined ponds drops below a designed minimum irrigation level. Groundwater pumped into these ponds will then be pumped out for irrigation. Thus, the use of groundwater for irrigation is minimized. The Authority has met its burden of proving that it will use the lowest quality of water available. With respect to the potable permit, the evidence establishes that there are only minor differences between the water quality in the Upper Floridan and Lower Floridan in this area. The Upper Floridan is a reasonable source for potable supply in this area. Thus, reasonable assurances have been provided by the Utility that it will utilize the lowest water quality that it has the ability to use for potable purposes. Waste of Water In regard to concerns that the design of the Villages Inc.'s stormwater/irrigation system will result in wasteful losses of water due to evaporation from the surface of the lined ponds, it must be noted that there are no artesian wells relating to this project and nothing in the record to suggest that the groundwater withdrawals by either the Utility or the Authority will cause excess water to run into the surface water system. Additionally, the evidence establishes that, to the extent groundwater will be withdrawn from the Lower Floridan and pumped into lined stormwater ponds, such augmentation is not for an aesthetic purpose. Instead, the groundwater added to those ponds will be utilized as an integral part of the irrigation system and will be limited in quantity to the amount necessary for immediate irrigation needs. Finally, the water to be withdrawn will be put to beneficial potable and irrigation uses, rather than wasteful purposes. Under current regulation, water lost from lined stormwater ponds through evaporation is not considered as waste. Thus, the Authority and the Utility have provided reasonable assurances that their withdrawals of groundwater will not result in waste. The ERP The stormwater management system proposed by the Villages Inc. will eventually serve 5,016 acres on which residential, commercial, golf course, and other recreational development will ultimately be constructed. However, the proposed permit currently at issue is preliminary in nature and will only authorize the construction of stormwater ponds, earthworks relating to the construction of compensating flood storage, and wetland mitigation. Water Quality Impacts The stormwater management system will include eight shallow treatment ponds that will be adjacent to Lake Miona and Black Lake and 45 lined retention ponds. Thirty-one of these lined ponds will serve as part of the irrigation system for a portion of the Villages Inc.'s development. All of these ponds provide water quality treatment. The unlined ponds will retain the first one inch of stormwater and then overflow into the lakes. The ponds provide water quality treatment of such water before it is discharged into the lakes. The water quality treatment provided by these ponds provides reasonable assurances that the project will not adversely impact the water quality of receiving waters. While they do not discharge directly to surface receiving waters, the lined retention ponds do provide protection against adverse water quality impacts on groundwater. There will be some percolation from these ponds, from the sides at heights above the top of the liner. However, the liners will prevent the discharge of pollutants through the highly permeable surface strata into the groundwater. The Villages Inc. designed the system in this manner in response to concerns voiced by the Department of Environmental Protection during the DRI process regarding potential pollutant loading of the aquifer at the retention pond sites. Furthermore, by distributing the accumulated stormwater - through the irrigation system - over a wider expanse of vegetated land surface, a greater degree of water quality treatment will be achieved than if the stormwater were simply permitted to percolate directly through the pond bottom. There is no reasonable expectation that pollutants will be discharged into the aquifer from the lined ponds. If dry ponds were used, there would be an accumulation of pollutants in the pond bottom. These measures provide reasonable assurances that there will be no adverse impact on the quality of receiving waters. Water Quantity Impacts With regard to the use of lined retention ponds, as part of the Villages Inc.’s stormwater system and the impact of such ponds on water quantity, the evaporative losses from lined ponds as opposed to unlined ponds is a differential of approximately one (1) inch of net recharge. The acreage of the lined ponds - even measured at the very top of the pond banks - is only 445 acres. That differential, in terms of a gross water balance, is not significant, in view of the other benefits provided by the lined ponds. As part of the project, wetlands will be created and expanded and other water bodies will be created. After rainfalls, these unlined ponds will be filled with water and will lose as much water through evaporation as would any other water body. The design proposed by the Villages Inc., however, will distribute the accumulated stormwater across the project site through the irrigation of vegetated areas. The documentation submitted by the Villages Inc. establishes that the ERP will not cause adverse water quantity impacts. The Villages Inc. has carried its burden as to this permitting criterion. Flooding, Surface Water Conveyance, and Storage Impacts Parts of the project are located in areas designated by the Federal Emergency Management Administration (FEMA) as 100-year flood zones. Specifically, these areas are located along Lake Miona, Black Lake, between Black Lake and Cherry Lake, and at some locations south of Black Lake. Under the District’s rules, compensation must be provided for any loss of flood zone in filled areas by the excavation of other areas. The District has determined, based upon the documentation provided with the Villages Inc.’s application, work on the site will encroach on 871.37 acre feet of the FEMA 100-year flood zone. However, 1,051.70 acre feet of compensating flood zone is being created. The Villages Inc. proposes to mitigate for the loss of flood zone primarily in the areas of Dry Prairie and Cherry Lake. At present, Cherry Lake is the location of a peat mining operation authorized by DEP permit. Mining has occurred at that site since the early 1980s. The flood zone mitigation proposed by the Villages Inc. provides reasonable assurance that it will sufficiently compensate for any loss of flood basin storage. The Villages Inc.'s project provides reasonable assurance that it will neither adversely affect surface water storage or conveyance capabilities, surface or groundwater levels or surface water flows nor cause adverse flooding. Each of the 45 retention ponds to be constructed on-site will include sufficient capacity, above the top of the pond liner, to hold a 100-year/24-hour storm event. This includes stormwater drainage from off-site. In addition, these ponds are designed to have an extra one foot of freeboard above that needed for the 100-year/24-hour storm, thus providing approximately an additional 100 acres of flood storage beyond that which will be lost through construction on-site. Furthermore, the Villages Inc. has proposed an emergency flood plan. In the event of a severe flood event, excess water will be pumped from Dry Prairie, Cherry Lake, and Lake Miona and delivered to the retention ponds and to certain golf course fairways located such that habitable living spaces would not be endangered. Environmental Impacts and Mitigation There are 601 acres of wetlands and surface waters of various kinds in the Villages Inc.’s project area. Forty-one acres of wetlands will be impacted by the work that is authorized under the ERP. Each of these impacted wetlands, along with the extent of the impact, is listed in the ERP. The impacts include both fill and excavation and all will be permanent. When assessing wetland impacts and proposed mitigation for those impacts, the District seeks to ensure that the activities proposed will not result in a net loss of wetland functionality. The object is to ensure that the end result will function at least as well as did the wetlands in their pre-impact condition. Functional value is judged, at least in part, by the long term viability of the wetland. While small, isolated wetlands are not completely without value, large wetland ecosystems – which are less susceptible to surrounding development – generally have greater long-term habitat value. The District’s policy is that an applicant need not provide any mitigation for the loss of habitat in wetlands of less than 0.5 acre, except under certain limited circumstances, including where the wetland is utilized by threatened or endangered species. Some wetlands that will be impacted by the Villages Inc.’s project are of high functional value and some are not as good. The Villages Inc. proposes a variety of types of mitigation for the wetlands impacts that will result from its project, all of which are summarized in the ERP. In all, 331.55 acres of mitigation are proposed by the Villages Inc. First, the District proposes to create new wetlands. Approximately 11 acres of this new wetland will consist of a marsh, which is to be created east of Cherry Lake. Second, it proposes to undertake substantial enhancement of Dry Prairie, a 126-acre wetland. Currently – and since at least the early nineties – Dry Prairie received discharge water from the peat mining operation at Cherry Lake. Without intervention, when the mining operations stop, Dry Prairie would naturally become drier than it has been for several years and would lose some of the habitat function that it has been providing. The Villages Inc.’s proposed enhancement is designed to match the current hydroperiods of Dry Prairie, thus ensuring its continued habitat value. Third, the Villages Inc. has proposed to enhance upland buffers around wetlands and surface waters by planting natural vegetation, thus providing a natural barrier. Placement of these buffers in conservation easements does not provide the Villages Inc. with mitigation credit, since a 25-foot buffer is required anyway. However, the District determined that the enhancement of these areas provided functional value to the wetlands and surface waters that would not be served by the easements alone. Fourth, the Villages Inc. will place a conservation easement over certain areas, including a 1500-foot radius preserve required by the Fish and Wildlife Conservation Commission (FWCC) around an identified eagles’ nest. These areas will also be used for the relocation of gopher tortoises and, if any are subsequently located, of gopher frogs. While the Villages Inc. is also performing some enhancement of this area, it will receive no mitigation credit for such enhancement – which was required to meet FWCC requirements. However, since the conservation easement will remain in effect in perpetuity, regardless of whether the eagles continue to use the nest, the easement ensures the continued, viability of the area’s wetlands and provides threatened and endangered species habitat. In order to provide additional assurances that these mitigation efforts will be successful, the District has included a condition in the proposed permit establishing wetland mitigation success criteria for the various types of proposed mitigation. If these success criteria are not achieved, additional mitigation must be provided. With the above described mitigation, the activities authorized under the ERP will not adversely impact the functional value of wetlands and other surface waters to fish or wildlife. The Villages Inc. has met its burden of providing reasonable assurances relating to this permit criterion. Capability of Performing Effectively The Villages Inc. has also provided reasonable assurances that the stormwater management system proposed is capable of functioning as designed. The retention ponds proposed are generally of a standard-type design and will not require complicated maintenance procedures. In its assessment of the functional capability of the system, the District did not concern itself with the amount of stormwater that the system might contribute for irrigation purposes. Rather, it focused its consideration on the stormwater management functions of the system. The question of the effectiveness of the system for irrigation purposes is not relevant to the determination of whether the Villages Inc. has met the criteria for permit issuance. Consequently, the record establishes that the documentation provided by the Villages Inc. contains reasonable assurances that the stormwater system will function effectively and as proposed. Operation Entity The Villages Inc. has created Community Development District No. 5 (CDD No. 5), which will serve as the entity responsible for the construction and maintenance of the stormwater system. CDD No. 5 will finance the construction through special revenue assessment bonds and will finance maintenance through the annual assessments. Similar community development districts were established to be responsible for earlier phases of the Villages Inc. The ERP includes a specific condition that, prior to any wetlands impacts, the Villages Inc. will either have to provide the District with documentation of the creation of a community development district or present the District with a performance bond in the amount of $1,698,696.00. Since the undisputed testimony at hearing was that CDD No. 5 has, in fact, now been created, there are reasonable assurances of financial responsibility. Secondary and Cumulative Impacts The Villages Inc.’s application also provides accurate and reliable information sufficient to establish that there are reasonable assurances that the proposed stormwater system will not cause unacceptable cumulative impacts upon wetlands or other surface waters or adverse secondary impacts to water resources. The system is designed in a manner that will meet water treatment criteria and there will be no secondary water quality impacts. Further, the use of buffers will prevent secondary impacts to wetlands and wetland habitats and there will be no secondary impacts to archeological or historical resources. In this instance, the stormwater system proposed by the Villages Inc. will function in a manner that replaces any water quantity or water quality functions lost by construction of the system. In its assessment of the possible cumulative impacts of the system, the District considered areas beyond the bounds of the current project, including the area to the south that is currently being reviewed under the DRI process as a substantial deviation. The District’s environmental scientist, Leonard Bartos, also reviewed that portion of the substantial deviation north of County Road 466A, in order to determine the types of wetlands present there. Furthermore, the District is one of the review agencies that comments on DRI and substantial deviation applications. When such an application is received by the District’s planning division, it is routed to the regulatory division for review. The District includes its knowledge of the DRIs in its determination that there are no cumulative impacts. Reasonable assurances have been provided as to these permitting criteria. Public Interest Balancing Test Because the proposed stormwater system will be located in, on, and over certain wetlands, the Villages Inc. must provide reasonable assurances that the system will not be contrary to the public interest. This assessment of this permitting criteria requires that the District balance seven factors. While the effects of the proposed activity will be permanent, the Villages Inc. has provided reasonable assurances that it will not have an adverse impact on the public health, safety, or welfare; on fishing or recreational values; on the flow of water; on environmental resources, including fish and wildlife and surface water resources; or on off-site properties. Furthermore, the District has carefully assessed the current functions being provided by the affected wetland areas. With respect to historical or archeological resources, the Villages Inc. has received letters from the Florida Department of State, Division of Historical Resources, stating that there are no significant historical or archeological resources on the project site that is the subject of this permit proceeding. Thus, the evidence establishes reasonable assurances that the Villages Inc.'s stormwater system will not be contrary to the public interest. Additionally, the District and Applicant presented uncontroverted evidence that the proposed project will not adversely impact a work of the District, and that there are no applicable special basin or geographic area criteria.

Recommendation Based on the foregoing findings of fact and conclusions of law, it is: RECOMMENDED that a final order be entered issuing Water Use Permit Nos. 20012236.000 and 20012239.000 and Environmental Resource Permit No. 43020198.001, in accordance with the District’s proposed agency action. DONE AND ENTERED this 24th day of June, 2002, in Tallahassee, Leon County, Florida. DON W. DAVIS Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 24th day of June, 2002.

Florida Laws (5) 120.569120.57373.203380.06403.412
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ELSBERRY AND ELSBERRY vs. SOUTHWEST FLORIDA REGIONAL PLANNING COUNCIL, 75-002095 (1975)
Division of Administrative Hearings, Florida Number: 75-002095 Latest Update: Mar. 21, 1977

Findings Of Fact Application 7500165 requested average withdrawal of water of 1,804,750 gallons per day from 4 wells located about a mile east of Highway 41 and a mile north of Apollo Beach. The four wells would be for irrigation of tomato crops on total acreage of 4 acres located in Hillsborough County (Exhibit 1, Testimony of Elsberry and Boatwright). Notice of hearing as to the application was published in a newspaper of general circulation in accordance with statute and rule (Exhibit 3). A letter of objection from Joseph S. Benham, Apollo Beach, Florida, dated November 19, 1975 was submitted to the Water Management District, wherein he expressed concern regarding water shortages and, although he does not seek to totally deny the application, is of the belief that the district must insure sufficient controls and management of irrigation activities so that resources are not wasted, water runoff to drainage ditches is eliminated and renewed justification is given each year for the withdrawal (Exhibit 2). A representative of the District staff established that there would be no violation of statutory or regulatory requirement for issuance of a consumptive water use permit in this case except as to the fact that potentiometric level of the applicant's property would be lowered below sea level as a result of withdrawal. It was agreed at the hearing that a period of thirty days should be granted both parties to formulate a stipulation as to control of runoff. An unsigned stipulation was received from the Water Management District by the hearing officer on March 1, 1976, which provided that the permit would be granted with the following stipulations: Runoff from the property will be limited to 25 percent of the quantity pumped and by December 31, 1980 shall be reduced to 16.5 percent of the quantity pumped. The District may at its own expense install metering devices for the purpose of monitoring runoff. The permittee will be notified in advance of such action. The Permit will expire on December 31, 1980. (Testimony of Boatwright, Exhibit 4).

Recommendation That application 8500165 submitted by Elsberry and Elsberry, Inc. Route 2, Box 70 Ruskin, Florida, for a consumptive water use permit be granted with the conditions as follow: Runoff from the property will be limited to 25 percent of the quantity pumped and by December 31, 1980 shall be reduced to 16.5 percent of the quantity pumped. The District may at its own expenseinstall metering devices for the purpose of monitoring runoff. The permittee will be notified in advance of such action. The Permit will expire on December 31, 1980. That the Board grant an exception to the provision of Rule 16J- 2.11(4)(e), F.A.C., for good cause shown. DONE and ENTERED this 15th day of March, 1976, in Tallahassee, Florida. THOMAS C. OLDHAM Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Southwest Florida Water Management District Post Office Box 457 Brooksville, Florida 33512 Elsberry & Elsberry, Inc. Route 2, Box 70 Ruskin, Florida

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OSCEOLA FISH FARMERS ASSOCIATION, INC. vs SOUTH FLORIDA WATER MANAGEMENT DISTRICT, 01-002900RP (2001)
Division of Administrative Hearings, Florida Filed:West Palm Beach, Florida Jul. 20, 2001 Number: 01-002900RP Latest Update: Mar. 20, 2003

The Issue The issues are whether the proposed amendment to Rule 40E- 2.041(1), Florida Administrative Code, exceeds the agency's grant of rulemaking authority; enlarges, modifies, or contravenes the specific law implemented; or is vague, fails to establish adequate standards for agency discretion, and vests unbridled discretion in the agency.

Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Petitioner, Osceola Fish Farmers Association, Inc. (OFFA), is a non-profit corporation whose members consist of tropical fish farmers in Osceola County, Florida. The parties have stipulated that OFFA has standing to bring this action. Respondent, South Florida Water Management District (District or Respondent), is a public corporation operating pursuant to Chapter 373, Florida Statutes, with its principal office in West Palm Beach, Florida. Among other things, the District has the authority to regulate the uses of water within its geographic boundaries, including Osceola County. On an undisclosed date, the District began test drawdowns (a lowering of the elevation of the water through control structures) in the Alligator Chain of Lakes just east of St. Cloud in Osceola County, where OFFA's members are engaged in tropical fish farming. The drawdowns were undertaken for the purpose of allowing the Florida Fish and Wildlife Conservation Commission (FFWCC) to conduct demucking activities in the lakes to enhance aquatic habitat. Prior to beginning work, the FFWCC obtained an Environmental Resource Permit from the Department of Environmental Protection (DEP). However, the District did not require either itself or the FFWCC to obtain a consumptive use permit on the theory that a lake drawdown for demucking activities was not a consumptive use and therefore did not require a permit. In an effort to halt future scheduled drawdowns, OFFA participated in a United States Army Corps of Engineers proceeding which culminated in the preparation of an Economic Impact Statement for FFWCC's drawdowns; filed a complaint with DEP under Section 373.219(2), Florida Statutes, alleging that an unlawful consumptive use (without a permit) was taking place (which complaint was found to be insufficient); filed an action for injunctive relief in circuit court under Section 403.412, Florida Statutes (which was dismissed or dropped for undisclosed reasons); and finally initiated a proceeding against the District under Section 120.56(4), Florida Statutes, alleging that the District had adopted "an incipient non-rule policy of exempting lake 'drawdowns' from water use permitting requirements" (DOAH Case No. 00-3615RU). To avoid the consequences of an adverse ruling in the latter action, the District began rulemaking proceedings to adopt an amendment to Rule 40E-2.041(1), Florida Administrative Code, to codify its policy relative to lake drawdowns. As amended, the rule reads as follows: Unless expressly exempt by law or District rule, a water use permit must be obtained from the District prior to any use or withdrawal of water. The drawdown of lakes for environmental, recreational, or flood control purposes is not regulated by Chapter 40E-2 or 40E-20, F.A.C. (Underscored language represents amended language). Petitioner has challenged only the amendment, and not the existing rule. The effect of the rule is obvious - a lake drawdown for one of the three stated purposes in the rule will not require a permit, while all other lake drawdowns will. As specific authority for the proposed amendment, the District cites Sections 373.044 and 373.113, Florida Statutes. The former statute authorizes the District to "adopt rules pursuant to [Chapter 120] to implement the provisions of this chapter," while the latter statute authorizes it to "adopt rules pursuant to [Chapter 120] to implement the provisions of law conferring powers or duties upon it." The District has cited Sections 373.103(1), 373.219, and 373.244, Florida Statutes, as the specific laws being implemented. The first statute provides that if specifically authorized by DEP, the District has the authority to "administer and enforce all provisions of this chapter, including the permit systems established in parts II, III, and IV of [Chapter 373], consistent with the water implementation rule"; the second statute provides in relevant part that the District may "require such permits for consumptive use of water and may impose such reasonable conditions as are necessary to assure that such use is consistent with the overall objectives of the district or department and is not harmful to the water resources of the area"; and the third statute provides for the issuance of temporary permits while a permit application is pending. In regulating the uses of water within its boundaries, the District administers a comprehensive consumptive water use permit program under Part II, Chapter 373, Florida Statutes. Both parties agree that under Section 373.219(1), Florida Statutes (2000), all "consumptive uses" of water require a permit, except for the "domestic consumption of water by individual users," which use is specifically exempted by the same statute. The global requirement for permits is also found in Rule 40E-2.041 (the rule being amended), as well as Rule 40E- 1.602(1), which provides in relevant part that unless expressly exempted by statute or rule, "[a] water use individual or general permit pursuant to Chapters 40E-2 or 40E-20, F.A.C., must be obtained prior to use or withdrawal of water " The term "consumptive uses" is not defined by statute, but the District has promulgated a rule defining that term. By Rule 40E-2.091, Florida Administrative Code, the District has adopted by reference a document known as the "Basis for Review for Water Use Permit Applications with the South Florida Water Management District." Section 1.8 of that document contains definitions of various terms used in the permitting program, including "consumptive use," which is defined as "[a]ny use of water which reduces the supply from which it is withdrawn or diverted." The District's policy for lake drawdowns, as proposed in the rule amendment, is inconsistent with this definition. On this disputed issue, Petitioner's evidence is accepted as being the most persuasive, and it is found that a lake drawdown for any purpose is a consumptive use of water. Section 373.219(1), cited as a specific law being implemented, provides that the District "may require such permits for consumptive use of water and may impose such reasonable conditions as are necessary to assure such use is consistent with the overall objectives of the district and department and is not harmful to the water resources of the area." The District construes this language as authorizing it to decide which uses of water are a "consumptive use," and which are not, and to implement a rule which codifies those decisions relative to lake drawdowns. Not surprisingly, Petitioner views the statute in a different manner and argues that the statute simply allows the District to create a permit program that is consistent with Chapter 373; that under the law a permit is required for all consumptive uses, including lake drawdowns; and that the District has no authority to carve out an exception for a lake drawdown from the permitting process, no matter what the purpose. As noted above, the District has identified three instances (for environmental, recreational, and flood control purposes) when a lake drawdown does not require a consumptive use permit. These terms are not so vague that a person of common intelligence would have difficulty understanding them. However, the proposed rule contains no prescribed standards to guide the District in its administration of the rule.

Florida Laws (12) 120.52120.536120.56120.682.04373.044373.103373.113373.219373.223373.244403.412
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SUWANNEE RIVER WATER MANAGEMENT DISTRICT vs FLORIDA CONFERENCE OF THE ASSOCIATION OF SEVENTH-DAY ADVENTISTS, INC., 03-000955 (2003)
Division of Administrative Hearings, Florida Filed:Live Oak, Florida Mar. 20, 2003 Number: 03-000955 Latest Update: Aug. 13, 2004

The Issue The issue is whether Respondent's water use permit should be revoked for nonuse of the permit for a period of two years or more.

Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Background The District is a state agency charged with the responsibility of issuing water use permits under Chapter 373, Florida Statutes, and Florida Administrative Code Chapter 40B- 2 for the geographic area under its statutory jurisdiction. Alachua County is within that geographic jurisdiction. Respondent is a Florida corporation with offices at 700 Northwest Cheeota Avenue, High Springs, in northern Alachua County. It owns approximately 700 acres in High Springs (west of Interstate Highway 75) on which it operates a church retreat and summer camping and recreational facility known as Camp Kulaqua. The property surrounds, and is contiguous to, Hornsby Spring, a first-order magnitude spring (having a flow rate of 100 CFS or greater) which, under normal conditions, discharges into the nearby Santa Fe River. Hornsby Spring is one of 296 documented springs within the District's jurisdiction. After receiving an overture from a representative of a private water bottling company, on September 28, 1999, Respondent filed an application for a General Water Use Permit in Township 7 South, Range 17 East, Section 26, in High Springs. In its application, Respondent represented that it desired a daily allocation of 2,000,000 gallons; that it intended to install two 12-inch wells, each having a capacity of 1,400 gallons per minute, just east of, and upgradient from, Hornsby Spring; and that all water withdrawals would be used in conjunction with a privately-owned commercial spring water bottling facility to be located on its property. The application also represented that the facility would employ 36 persons and operate 168 hours per week. The application was reviewed by a former District hydrogeologist, William H. Kirk. During the review process, and in response to Mr. Kirk's request for more information, Respondent provided a comparison of the requested allocation with the overall flow of Hornsby Spring. This was because Mr. Kirk was concerned that the requested allocation was "a bit high," and he wanted to ensure that the issuance of the permit would not cause harm to, or adversely affect, the water resources. Under a professional guideline that Mr. Kirk used, if the applicant could show that the cumulative amount being withdrawn was to be less than ten percent of what the available data showed to be the mean spring flow, the District would consider it to be "an acceptable impact." Notwithstanding Mr. Kirk's use of this guideline, the District points out that there is no District rule or policy sanctioning the ten percent rule, and at hearing it denied that this standard is used by the District in assessing water use applications. Further, the Permit itself does not refer to a relationship between spring flow and the size of the allocation. Even so, this analysis was considered by Mr. Kirk in determining whether Respondent had given reasonable assurance that the spring would not be impacted. In its response to the request for additional information, Respondent reduced its requested allocation to 750,000 gallons per day and indicated that if a bottling plant were to be constructed on its property, approximately 700,000 gallons of the total allocation would be consumed in "bulk transfer and bottling," with the remainder for camp use. More specifically, Respondent indicated that it would allocate 490,000 gallons per day for bulk transport, 210,000 gallons per day for spring bottling water, and 50,000 gallons per day for incidental uses at its property. By reducing the allocation from 2,000,000 gallons per day to 750,000 gallons per day, Respondent's requested average daily allocation represented only 0.4 percent of the average daily spring flow as measured over the last 28 years. The reduced allocation satisfied Mr. Kirk's concern that Respondent demonstrate a reasonable demand and a reasonable need for that allocation, and he recommended approval of the application.2 On February 25, 2000, the District approved the application and issued Water Use Permit No. 2-99-00130 (Permit).3 The Permit authorizes an average daily withdrawal of 0.7500 million gallons per day (750,000 gallons per day) or a maximum daily withdrawal and use of 0.7500 million gallons per day with an annual allocation not to exceed 273.750 million gallons (273,750,000 gallons) per calendar year in conjunction with the operation of a privately-owned water bottling plant. The Permit expires on February 25, 2020. After the Permit was issued, under the regulatory process in place, Respondent was required first to obtain a permit for a temporary test well which would be used to collect information concerning the site of the proposed activity, and to then file an application for permits authorizing the construction and operation of the two 12-inch production wells. The Permit contains a number of conditions, two of which require a brief comment. First, Condition No. 2 provides that "[t]his permit is classified as unconfined [F]loridan aquifer for privately owned bottled water plant." This means that all water withdrawals must be made from the unconfined Floridan aquifer, as opposed to the spring head of Hornsby Spring. (Respondent's proposed siting of its two production wells 660 yards east of the spring is consistent with this provision.) Second, Condition No. 4 provides that "[t]he permittee shall submit daily pumpage records on a monthly basis to the [District]." Pumpage reports are filed by permittees so that the District can determine whether the permit is actually being used, and if so, to ensure that the amount of water being withdrawn under the permit does not exceed the authorized allocation. As it turned out, pumpage reports were never filed by Respondent. (However, the record shows that the District has never strictly enforced this requirement for any permittee.) In late 2002, the District staff undertook a review of the nine water bottling permit holders within its jurisdiction, including Respondent. That category of permit holders was selected for review because of the small number of permits and the limited resources of the District staff. (In all, the District has probably issued several thousand permits to other types of users.) On February 4, 2003, the District served its Complaint under the authority of Sections 120.60 and 373.243, Florida Statutes, and Florida Administrative Code Rule 40B-2.341. As grounds for revoking the permit, the District alleged that there was "non-use of the water supply allowed by the permit for a period of two (2) years or more." Although Respondent contends that it should have been given an opportunity to correct the nonuse allegation before the Complaint was issued, nothing in the Administrative Procedure Act or District rules requires that this be done. Until the issuance of the Complaint against Respondent in early 2003, and similar Complaints against eight other permit holders at the same time, the District had never invoked this statutory provision.4 There is no evidence to support Respondent's contention that the Complaints were issued for "purely political reasons." On March 4, 2003, Respondent requested a formal hearing challenging the District's proposed action. In the parties' Pre-Hearing Stipulation, the issues have been broadly described as follows: whether Section 373.243(4), Florida Statutes, is to be strictly or liberally construed; whether Respondent's nonuse is based upon extreme hardship for reasons beyond its control; and whether the District is equitably estopped from permit revocation. (According to the District, even if the Permit is revoked, such revocation is without prejudice to Respondent reapplying for, and receiving, another permit so long as it meets all applicable requirements.) Equitable Estoppel Respondent first contends that the District is estopped from revoking its Permit on the theory that, under the circumstances here, the doctrine of equitable estoppel applies. For that doctrine to apply, however, Respondent must show that the District made a representation as to a material fact that is contrary to a later asserted position; that Respondent relied upon that representation; and that the District then changed its position in a manner that was detrimental to Respondent. See, e.g., Salz v. Dep't of Admin., Div. of Retirement, 432 So. 2d 1376, 1378 (Fla. 3d DCA 1983). The District issued Respondent's Permit on the condition that Respondent operate in conformity with all pertinent statutes and regulations. This finding is consistent with language on the face of the Permit, which states that the Permit "may be permanently or temporarily revoked, in whole or in part, for the violation of the conditions of the permit or for the violation of any provision of the Water Resources Act and regulations thereunder." Respondent relied on the District's representation that it could use the Permit so long as it complied with all statutes and regulations. In reliance on that representation, in addition to staff time, after its Permit was issued, Respondent expended "somewhere around" $70,000.00 to $74,000.00 for conducting water quality testing; sending cave divers underground to ascertain the correct location of the portion of the aquifer on which to place its production wells; drilling a 6-inch test well in August 2000; obtaining the City of High Springs' approval in March 2000 for industrial zoning on a 10-acre tract of land on which to site a "water plant"; and engaging the services of a professional who assisted Respondent in "seeking out businesses and getting the right qualifications of the spring water to make sure that it was a marketable water." The District has never asserted anything different from its original position: that if Petitioner complied with all statutes and rules, it could continue to lawfully make water withdrawals under its Permit. The issuance of the Complaint did not represent a change in the District's position. Because a change in position in a manner that was detrimental to Respondent did not occur, the necessary elements to invoke the doctrine of equitable estoppel are not present. Was the Permit Used? A preliminary review by District staff indicated that Respondent had never filed the daily pumpage reports on a monthly basis and had never requested permits authorizing the construction of the two 12-inch production wells. These preliminary observations were confirmed at final hearing, along with the fact that Respondent has never entered into an agreement with a water bottling company (although draft agreements were once prepared); that Respondent has never constructed a water bottling facility; and that no operations were ever conducted under the Permit. Therefore, the evidence supports a finding that Respondent did not use its Permit for the two-year period after it was issued, as alleged in the Complaint. Respondent's contention that the evidence fails to support this finding belies the evidence of record. In an effort to show that it actually used the Permit, Respondent points out that in August 2000 it applied for, and received a permit to construct, an unmetered 6-inch test well in association with its General Water Use Permit. (Respondent sometimes erroneously refers to the test well as a test production well. This is incorrect as the well is a test well, and not a production well.) After the test well was installed, at some point Respondent says it began withdrawing approximately 50,000 gallons per day of water from that well for incidental uses associated with the operation of Camp Kulaqua.5 These withdrawals were made on the assumption that the test well permit fell under the broad umbrella of the General Water Use Permit. (Respondent also has a permitted 6- inch diameter well and an unregulated 4-inch well on its premises, both of which are used for water supply needs at Camp Kulaqua.) It is true, as Respondent asserts, that its Permit authorized incidental withdrawals of up to 50,000 gallons per day for unspecified uses at Camp Kulaqua. However, these withdrawals are authorized under the General Water Use Permit and not the test well permit. The two permits are separate and distinct. On the one hand, a test well is intended to be temporary in nature and used only for the purpose of test well development and collecting information regarding the height of the aquifer and water quality at the site of the proposed activity. Conversely, withdrawals for any other purpose, even incidental, must be made from the production wells, which are only authorized by the General Water Use Permit. Before a test well can be used for normal consumptive purposes, the permit holder must seek a modification of the permit to include it as a part of its general water use permit. Here, no such modification was sought by Respondent, and no authorization was given by the District. Therefore, Respondent's incidental water uses associated with its test well cannot be counted as "uses" for the purpose of complying with the use requirement in Section 373.243(4), Florida Statutes. In light of the District's credible assertion to the contrary, Respondent's contention that it is common practice to lawfully withdraw water from a test well for incidental consumptive purposes has been rejected. (It is noted, however, that the District has not charged Respondent with violating the terms of its test well permit.) Extreme Hardship Under Section 373.243, Florida Statutes (which was enacted in 1972), the District is authorized to revoke a water use permit "for nonuse of the water supply allowed by the permit for a period of 2 years." However, if the user "can prove that his or her nonuse was due to extreme hardship caused by factors beyond the user's control," revocation of the permit is not warranted. The phrase "extreme hardship caused by factors beyond the user's control" is not defined by statute or rule. In the context of this case, however, the District considers an extreme hardship to occur under two scenarios. First, if the aquifer level has dropped so low due to drought conditions that a permit holder cannot access the water through its well, its nonuse is excusable. Alternatively, if an emergency order has been issued by the District directing permit holders (including Respondent) to stop pumping due to certain conditions, an extreme hardship has occurred. (Presumably, a severe water shortage would precipitate such an order.) In this case, the District issued a water shortage advisory, but not an emergency order, due to a "severe drought," indicating that users could still pump water, but were encouraged to voluntarily reduce their usage. This advisory remained in effect from the summer of 1998 until the spring of 2003, when a severe drought ended. However, no emergency order was ever issued by the District. Respondent contends that its nonuse was due to an extreme hardship caused by factors beyond its control. More specifically, it argues that a severe drought occurred in Alachua County during the years 1998-2003, and that under these conditions, federal regulations prevented it from withdrawing water for bottling purposes, which was the primary purpose for securing a permit. Further, even if it had withdrawn water during these drought conditions, such withdrawals could have adversely impacted Hornsby Spring and constituted a violation of a District requirement that water resources not be adversely impacted. Because an investment of several hundred thousand dollars was required to drill and install the two production wells, Respondent contends it was not financially prudent to make that type of investment and begin operations until normal spring conditions returned. These contentions are discussed in greater detail below. Around September 7, 1999, a representative of a water bottling company first approached Respondent about the possibility of the two jointly operating a water bottling plant and/or transporting water in bulk from Respondent's property. Prompted by this interest, less than three weeks later Respondent filed its application for a water use permit (although at that time it did not mention on the application that off-site bulk transfers would occur), and a permit was eventually issued in February 2000. Later, and through a professional firm it employed, Respondent had discussions with representatives of several bottling companies, including Great Springs Waters of America (Great Springs) and Perrier Group of America. Apparently, these more serious discussions with a potential suitor did not take place until either late 2000 or the spring of 2001. Periodic measurements taken by District staff at Hornsby Spring reflected natural drought conditions from April 2000 to April 2003. As noted earlier, this was the product of a "severe drought" which took place between the summer of 1998 and the spring of 2003; the drought was one of a magnitude that occurs only once in every 50 to 100 years. During the years 2000 through 2002, the spring had zero flow or was barely flowing much of the time.6 Had Respondent pumped water during 20 out of the 24 months after the Permit was issued, it could have potentially violated the requirement that it not harm Hornsby Spring. This fact is acknowleged by a District witness who agreed that if the "spring is not flowing, . . . [pumping] would have an [adverse] impact." Even as late as October 2003, the spring had tannic discoloration caused by the lengthy drought conditions. The parties agree, however, that there is no water shortage in the District at the present time. To illustrate the difficulty that it experienced in obtaining a joint venture partner for water bottling purposes, Respondent established that in the spring of 2001, a Great Springs representative visited the site when the spring was "barely flowing." For obvious reasons, Respondent could not "bring a party there who would want to enter into a business [agreement]" under those conditions. These same conditions remained in effect during most of the two year period. The District points out, however, that even though the spring was low or barely flowing, so long as the aquifer itself was not too low, Respondent could still withdraw water from the aquifer, since Condition 2 of the Permit authorizes withdrawals from the aquifer, and not the spring. The reason for this apparent anomaly is that when a spring ceases to flow, the aquifer has simply dropped below the level of the spring vent; even under these circumstances, however, there may still be a substantial quantity of water in the aquifer available for pumping. Assuming that it could still lawfully pump water when the spring was dry or barely flowing without causing adverse impacts to the spring, Respondent was still subject to federal regulations which govern the bottling of spring water. See Title 21, Part 165, C.F.R. For spring water to be marketed as bottled "spring water," 21 C.F.R. § 165.119(2)(vi) requires that the water "be collected only at the spring or through a bore hole tapping the underground formation feeding the spring." This means that the bore hole had to be physically connected with the cave system feeding Hornsby Spring or produce water of the same quality as that discharging from the spring. The regulation goes on to provide that "[i]f spring water is collected with the use of an external force [such as by a pump], water must continue to flow naturally to the surface of the earth through the spring's natural orifice." While this regulation obviously does not prohibit Respondent from pumping water, since that authority lies within the District's exclusive jurisdiction, it does provide that in order to use spring water for bottling purposes, the water must continue to flow naturally from the aquifer to the spring. If it does not, the water cannot be used for this purpose. Because Hornsby Spring had zero flow for parts of 2001 and 2002, and severely reduced flows during most of the other time during the two-year period ending February 2002, Respondent was effectively prevented by the foregoing regulation from using the water for bottling purposes. Therefore, Respondent's nonuse was due to extreme hardship caused by factors beyond its control -- a severe drought lasting throughout the two-year period after the Permit was issued, and federal regulations which prevented it from using water for the purpose for which the Permit was issued. Thus, the nonuse is excusable.

CFR (2) 21 CFR 165.11021 CFR 165.119(2)(vi) Florida Laws (4) 120.569120.57120.60373.243
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