The Issue The primary issue in this case is whether the St. Johns River Water Management District (District, or SJRWMD) should issue consumptive use permit (CUP) 95581 to Seminole County (Seminole) authorizing the withdrawal and use of 2,007.5 million gallons a year (mgy) or 5.5 million gallons a day (mgd) of surface water from the St. Johns River for public supply and reclaimed water supply augmentation.
Findings Of Fact Parties Seminole County (Seminole) is north of Orlando, Florida, and contiguous with the St. Johns River. It is located entirely within the District, and the Central Florida Coordination Area (“CFCA”). Seminole owns and operates water, wastewater, and reclaimed water utilities. These include a wastewater treatment facility at Yankee Lake near the St. Johns River just downstream from Lake Monroe, where Seminole proposes to construct surface water withdrawal and related facilities. The District is the regulatory agency charged with issuing permits for the consumptive use of water within a sixteen county area located in East-Central Florida. The City of Jacksonville (Jacksonville) is a Florida municipality located about 140 miles downstream of the proposed Yankee Lake facility. Jacksonville’s standing is based on the filing of a verified pleading pursuant to Section 403.412(5), Florida Statutes.2 St. Johns County (St. Johns) is a Florida political subdivision located approximately 100 miles downstream of the proposed Yankee Lake facility. St. Johns County’s standing also is based on the filing of a verified pleading pursuant to Section 403.412(5), Florida Statutes. St. Johns Riverkeeper, Inc. (Riverkeeper), is a Florida not-for-profit corporation. It alleges Seminole’s proposed withdrawal of water will adversely affect the use and enjoyment of the St. Johns River by a substantial number of its members. At the end of its evidentiary presentation at the final hearing, Riverkeeper requested leave to amend its petition to also allege standing under Section 403.412(6), Florida Statutes. Seminole's Water Utility Systems Seminole serves customers in its Northwest, Northeast, Southwest, and Southeast Potable Water Service Areas, and holds separate groundwater CUPs for each service area. The existing CUPs authorize a total allocation of 21.7 mgd. Seminole has four main wastewater water service areas roughly contiguous with its water service areas. Seminole treats wastewater from the Southeast Service Area at the Iron Bridge Regional Water Reclamation Facility,3 and treats wastewater from the Northwest and Northeast Service Areas at its Yankee Lake Wastewater Treatment Plant (WWTP) and Greenwood Lakes WWTP. Seminole has two reclaimed water service areas, the Northwest-Northeast Service Area, which utilizes treated wastewater supplied by the Yankee Lake and Greenwood Lakes WWTPs, and the Southeast Service Area, which utilizes treated wastewater from the Iron Bridge WWTP. Seminole plans to expand reclaimed water use in the Northwest-Northeast Service Area by installing an $80 million, 5-phase residential reclaimed retrofit program. Seminole has developed an Integrated Water Supply Plan (Seminole's Plan) to address existing and future potable and reclaimed water needs in compliance with the CFCA rules, which limit groundwater withdrawals to the quantity required to meet each user’s 2013 demand and encourage development of AWS sources to meet excess demands.4 Seminole's Plan includes traditional and AWS sources and a conservation program that has been approved by the District. Seminole's traditional water source is groundwater, and Seminole has a pending application to consolidate its existing groundwater CUPs (Consolidated Groundwater CUP). With current allocations of 21.7 mgd expired or soon to expire, the Consolidated Groundwater CUP requests an allocation of 25.6 mgd to meet 2013 demands. The current plan is for surface water withdrawals from St. Johns River at Yankee Lake be Seminole's non-traditional water source. Yankee Lake Project CUP On February 12, 2008, the District issued its Technical Staff Report (“TSR”) for CUP 95581. The TSR recommended a 20-year CUP with a surface water allocation of 0.70 mgd starting in 2009, increasing to 5.5 mgd in 2025-2028. Between 2009 and 2013, the surface water allocation identified in the TSR would be used for reclaimed water augmentation. Starting in 2014, the TSR recommends an allocation of 5.35 mgd, which coincides with the completion of Seminole’s surface water treatment facility and the use of surface water as a potable water source. Condition 6 of the TSR limits the maximum daily withdrawal to 11.59 mgd. The intake structure for the Yankee Lake surface water facility will be located on a manmade canal connected to the St. Johns River, in or just outside the Wekiva River Aquatic Preserve and in Seminole's Yankee Lake Black Bear Wilderness Area. The capacity of the intake structure is 10 mgd, and it has been sized for expansion to 50 mgd to meet potential future demands over the useful life of the facility. The intake structure is designed with an intake velocity much less than 0.5 feet per second, which is the industry standard. The intake structure includes a sheet pile wall, an 8-inch bar screen manatee barrier at the mouth of the canal, a second screen which removes aquatic debris and serves as a second barrier to aquatic life, and a 4-millimeter intake pump screen. Raw water pipelines from the intake structure will run through previously disturbed wetlands within the Wekiva River Aquatic Preserve and the Seminole Black Bear Wilderness Area to new treatment facilities, all of which will be located on land owned by Seminole. The pipelines consist of two 42-inch lines with a total capacity of 50 mgd, which is intended to meet possible future demands during the 50-year useful life of the facilities. It is common to design utility infrastructure to accept larger quantities of water than immediately needed to accommodate possible future expansion. Seminole Water Demand and Need The reasonableness of Seminole's proposed CUP depends in large part on potable water and reclaimed water demand. Potable Water In 2005, Seminole provided water service to a residential population of 101,585. For the most recent five- year period, from 2003-2007, Seminole’s average residential per capita potable water use rate was 153.7 gallons per capita per day (gpcd). The historic per capita use rates in Seminole’s four service areas are below 150 gpcd, with the exception of the Northwest Service Area. The served population in the Northwest Service Area increased from 12,655 in 2001 to 20,745 in 2005, and per capita usage declined from 285 gpcd in 2001 to 213.5 gpcd in 2005. The higher per capita rate in the Northwest Service area is attributable to larger residential lots and lawns and more irrigation than in the other service areas. Additionally, the residents are more affluent and are not as responsive to Seminole’s water conservation rate structure. Seminole is implementing an $80 million reclaimed water retrofit program in order to reduce per capita potable water use in the Northwest Service Area. In order to project future water demands for the life of the proposed CUP, Seminole’s consultant, Dr. Terrence McCue, used the population projections published by the University of Florida Bureau of Economic and Business Research (“BEBR”).5 He used the BEBR 2008 medium population projections, which were the most recent projections available at the time of hearing. Since BEBR data are published on a county-wide basis, Dr. McCue disaggregated the data to Seminole’s service areas by using traffic analysis zones and water utility billing data. This is a recognized methodology used to calculate service area population for the purpose of determining water demand. Using this methodology, Dr. McCue estimated Seminole’s service area population to be 110,860 in 2008 and projected that it would increase to 126,531 in 2013 and to 161,971 in 2027. The District asked its consultant, Richard Doty, to perform an independent water demand projection as a check on Dr. McCue’s work product. Mr. Doty also relied on BEBR projections, but disaggregated the county-wide population projections differently, using a sophisticated GIS model to calculate build-out densities. Mr. Doty estimated Seminole’s service area population to be 109,202 in 2007 and projected that it would increase to 126,075 in 2013 and to 155,368 in 2027. Although Mr. Doty’s population projections were somewhat lower than Dr. McCue's, they were close enough to essentially corroborate the validity of Dr. McCue's projections. Mr. Doty testified that, while he prefers his projection, Dr. McCue’s population projections are plausible. Jacksonville's expert witness, Nolton Johnson, who did not himself project service area population, could not say that Mr. Doty’s population projections are superior because Dr. McCue used actual water billing data that was more specific to Seminole’s service area. For these reasons, it is reasonable to base projected water demand on either Dr. McCue's or Mr. Doty's population projections. To project service area demand, projected population is multiplied by a use rate. Here, Mr. Doty used the simple method specified in A.H. Section 12.2.2. He basically averaged the historical gross per capita daily (gpcd) water use in each service area for the most recent five-year period (2003-2007). Using the average use rate for those years, he calculated a total potable water demand (for all sources and all kinds of uses) of 24.87 mgd for 2013, 30.67 mgd for 2027, and 30.76 mgd for 2028. In contrast, Dr. McCue averaged the historical per capita residential use rate for 2001 through 2005, instead of 2003 through 2007. Then, he made several adjustments not used by Mr. Doty and not included in A.H. Section 12.2.2. Some of these adjustments had the effect of increasing demand while others decreased demand. First, Dr. McCue's demand estimates included an 8% "unaccounted-for flow factor." There was evidence that this is an accepted industry standard and consistent with other utilities in Central Florida. However, it seems high for Seminole, which may actually over-account for flow. (Seminole is currently attempting to ascertain the accuracy of its flow meters.) Mr. Doty did not incorporate an "unaccounted-for flow factor" in his demand projections because any discrepancy, whether Seminole's flow meters are over-accounting or under- accounting for actual flow, should already be incorporated into the historical use rate Mr. Doty calculated. Second, Dr. McCue multiplied the historical average by a 6% "drought correction factor." Dr. McCue's rationale for the drought correction factor was that it accounted for the increased demand that would occur during drought years (although the historical average already accounted for use rate changes due to the fluctuations in rainfall that occurred during 2001- 2005). Dr. McCue also made adjustments to the historical use rate to reduce projected potable water demand as a result of Seminole's Water Conservation Plan, which meets all District requirements and CUP permitting criteria and has been approved by the District. Seminole's Water Conservation Plan includes Seminole’s ongoing residential irrigation audit program, which from 2007 through 2013 is projected to conserve 0.082 mgd per year, with a total savings of 0.622 mgd. Seminole has had a water conservation rate structure in place since 1985, which discourages high water use by increasing customer billing rates as usage increases. Seminole also has implemented a block billing structure for its reclaimed water customers to conserve that water. Seminole's Water Conservation Plan also includes an augmentation minimization plan, conservation gardens, and a public education program. The total cost of implementing Seminole’s conservation plan will exceed $125 million. The plan is focused on the Northwest Service Area, where per capita water use has declined 25% from 2001 to 2007. If Seminole's objectives are achieved, projected water use within the Northwest Service Area will decline an additional 25%, for a 50% reduction in potable water use within the Northwest Service Area from 2001-2028. Dr. McCue applied a 9% reduction in potable water demand due to implementation of the reclaimed water retrofit program and a 4% reduction to account for other planned conservation measures. Based on Dr. McCue’s projections, Seminole’s residential per capita use rate will fall below 150 gpcd in 2012, and will continue to decline to 134.5 gpcd in 2027 as a result of the proposed conservation, with corresponding reductions in potable water demand. Petitioners contend that Dr. McCue's conservation adjustments were "negotiated" between Seminole and the District, and are too low. The "negotiation" process itself does not negate the reasonableness of the resulting agreed conservation adjustments since it is impossible to predict the results of Seminole's Water Conservation Plan with certainty. The conservation adjustments used by Dr. McCue were reasonable. Riverkeeper expert witness, Dr. John Woolschlager, testified that Seminole could achieve greater reductions (15%) in water use through conservation. He based his opinion on reductions achieved by other utilities, including the City of Tampa and Miami-Dade County. Dr. Woolschlager relied on an EPA report on the City of Tampa, which indicated that Tampa experienced a 26% decline in per capita use from 1989 to 2001. However, he was not aware of how lot sizes, land use patterns, persons per household, or other demographic information for Tampa compare to Seminole, and he did not have enough data to say that Seminole could achieve similar savings from 2008 to 2028. Dr. Woolschlager also did not know whether Seminole had already implemented any of the conservation measures utilized by Tampa from 1989 to 2001. Dr. Woolschlager also relied on a study involving Miami-Dade County. However, he admitted that Miami-Dade County is not similar to Seminole demographically. Dr. Woolschlager also was not aware of Miami-Dade’s total water use during the study period, but was only aware that Miami-Dade had reduced its water consumption by 19.8 mgd. Without knowing Miami-Dade’s total use, it was impossible to calculate the percentage savings that was achieved by Miami-Dade in order to compare it to Seminole. Jacksonville expert witness, Nolton Johnson, opined that greater conservation savings could be achieved through the mandatory implementation of the Florida Water Star Program, a voluntary certification process for builders. While promoted by the District, the Florida Water Star Program is not part of the District’s conservation requirements. It is not appropriate to include a CUP requirement that Seminole make the program mandatory. It is not reasonable from an engineering perspective, or appropriate, to assume savings from 100% compliance with the Florida Water Star Program by new development in Seminole, as Mr. Johnson did for his opinion. In addition, Mr. Johnson based his assumptions regarding the amount of water savings achievable through mandatory implementation of the Florida Water Star Program on a District brochure. However, the brochure assumed an extremely high starting per capita water rate prior to implementation of the program--much higher than Seminole’s existing per capita water use rate, even in the Northwest Service Area. For that reason, Mr. Johnson's assumptions were not applicable to Seminole. In part as a result of his conservation adjustments, Dr. McCue assumed that Seminole would be allocated only 23.71 mgd of groundwater from 2013 on, instead of the 25.6 mgd of groundwater requested in the pending Consolidated Groundwater CUP. While on the one hand criticizing Dr. McCue's assumed conservation savings for being too low, Riverkeeper in particular also criticized Dr. McCue for applying any conservation adjustments to reduce the assumed groundwater allocation in the pending Consolidated Groundwater CUP. Riverkeeper argued essentially: that Seminole was entitled to the groundwater necessary to supply its 2013 projected demand, without any conservation reduction, as requested in the pending Consolidated Groundwater CUP; that Seminole essentially is being unfair to itself by not asserting in this case its entitlement to the full 25.6 mgd of groundwater requested for 2013 in the pending Consolidated Groundwater CUP (which would have the effect of reducing or eliminating its need for any water from the river); and that allowing Seminole to decline to take the maximum groundwater would somehow discourage other applicants from implementing conservation programs. These criticisms are rejected. First, there is no guarantee that the Consolidated Groundwater CUP will authorize the full requested amount, as the District has expressed concern about potential environmental impacts to wetlands and lake MFLs. Second, there is no guarantee that the District will approve the Consolidated Groundwater CUP in time to meet Seminole’s needs. At the time of the final hearing, it was projected that Seminole could begin to face a water deficit in some of its service areas as early as the end of 2008 if the Consolidated Groundwater CUP was not approved soon. Finally, there is no requirement that Seminole use groundwater up to the 2013 demand limit in the CFCA rules. If Seminole is allocated surface water from the St. Johns River in this case because it applied conservation adjustments to its demand calculations, the appropriate amount of groundwater Seminole needs for reasonable-beneficial use will be determined in the pending Consolidated Groundwater CUP application, which also will determine how much "redundancy" is appropriate, if any. Condition 4 of the TSR specifically provides that the combined allocations of surface water under CUP 95581 and groundwater resulting from pending Consolidated Groundwater CUP application may not exceed the total projected demand for all four service areas in any year. With his adjustments, Dr. McCue projected a total potable water demand (for all sources and all kinds of uses) of 23.19 mgd for 2013 and 28.1 mgd for 2027. Based on those assumptions, Dr. McCue projected a requirement for 0.46 mgd of AWS in 2012, none in 2013 and 2014, 0.18 mgd in 2015, with increasing AWS requirements each succeeding year, up to 4.39 mgd in 2027. Seminole also is requesting a maximum day allocation of 11.59 million gallons. Of this amount, 7.59 million gallons are attributable to potable water needs. This maximum day demand for potable water supply use was calculated using a peaking factor of 1.7 based on existing potable water use rates, which is consistent with the District’s applicable rules. See A.H. § 12.2.4. (ii) Reclaimed Water Seminole has undertaken the expansion of its reclaimed water system to existing potable water customers in the Northwest-Northeast Service Area, which receives reclaimed water from the Yankee Lake and the Greenwood Lakes WWTPs. In 2005, about 4 mgd of reclaimed water was produced at these facilities; by 2025, 8.16 mgd will be available for reclaimed use. Upon implementation of the reclaimed water retrofit program, roughly 75% of the reclaimed water produced by these facilities will be reused to meet annual average demand, and about 100% will be used to meet maximum day demands. This complies with the requirement that CUP applicants meet non-potable water demands through the use of lower quality sources, such as reclaimed water, when feasible. See A.H. § 10.3(g). The reclaimed retrofit program is being implemented in 5 phases. Phase I has been completed and was put on-line in 2008. Phase II will be completed in 2010. Phases III, IV, and V are scheduled to be completed in 2015. The reclaimed retrofit program cannot be accelerated, because Seminole must produce sufficient wastewater to meet reclaimed water demands in those areas. Otherwise, greater reclaimed water augmentation than requested in the pending CUP application would be required to meet reclaimed water demand. There was no genuine dispute as to Seminole's need for an mgd on an annual average basis and a four-million gallon maximum daily allocation to augment its reclaimed water system as a result of the reclaimed retrofit program. The relevant issue raised by the objectors is whether there are lower acceptable quality sources of water than the St. Johns River available to augment Seminole's reclaimed water system. See A.H. § 10.3(g). Seminole’s Consideration of AWS Options Before filing the application for the CUP at issue in this case, Seminole evaluated a number of AWS options, including brackish groundwater, seawater desalination, and the St. Johns River. Brackish Groundwater Seminole considered and actually identified brackish groundwater withdrawn from Lower Floridan Aquifer wells as a potential AWS source and applied for a CUP in 2004 to use brackish groundwater wells near its Greenwood Lakes WWTP as a source of water to augment its reclaimed water system. Preliminary modeling of withdrawals of 6.25 mgd from wells near the Greenwood Lakes WWTP and 1 mgd from wells near the Yankee Lake WWTP indicated that there would be adverse impacts to wetlands and other surface waters, including the minimum level established at Lake Sylvan. The Greenwood Lakes WWTP is approximately five miles from Lake Sylvan. The Yankee Lakes WWTP is approximately a mile from Lake Sylvan. The modeled impacts on Lake Sylvan probably were significantly larger than the impacts of smaller brackish groundwater withdrawals, especially if withdrawn only from Greenwood Lakes wells. No pump tests were conducted. Even with limited knowledge, Seminole and the District concluded that the Lower Floridan Aquifer would not be a long- term, stable water supply source in Seminole and that use of brackish groundwater would require Seminole to design and construct a water treatment facility with a short useful life, making brackish groundwater an infeasible AWS option for Seminole. This conclusion was reached because there is little freshwater recharge to the Lower Floridan Aquifer in the area, and withdrawn brackish groundwater likely would be replenished by saltier water from the deeper aquifer, resulting in a degraded water supply. No expert testimony refuted that evaluation. Seawater Desalination The most probable location of a desalination facility to supply Seminole would be near the Atlantic Ocean in Volusia County. This option would require the construction of an extensive pipeline to transport desalinated water to Seminole, and reverse osmosis concentrate would have to be disposed of through an ocean outfall or deep injection well. Seawater desalination would require a complicated, expensive, and energy-intensive treatment process. The capital cost to supply 4.5 mgd to Seminole would be about $183 million, and operation costs would be twice those of the proposed Yankee Lake project, making the desalination option economically infeasible. RIBs Petitioners contended that Seminole should obtain supplemental water for its reclaimed system from its rapid infiltration basins (“RIBs”). RIBs are basins with highly- permeable soil that allow water to percolate into the surficial aquifer for disposal and beneficial recharge. Seminole uses RIBs to dispose of excess reclaimed water during wet weather conditions, when it is not needed to meet reclaimed water demands. When needed to meet reclaimed water demands, reclaimed water will be supplied to reclaimed water customers and will not be discharged to RIBs. Thus, reclaimed water will not be available from the RIBs during those times when augmentation water is needed. For RIBs to be used for reclaimed water augmentation, they would have to be combined with a large reservoir. The evidence was that a 400-acre, 450 million gallon reservoir would have to be constructed to store enough reclaimed water to meet Seminole’s augmentation needs. In addition, a treatment facility would be required to treat the reclaimed water stored in a reservoir prior to distribution to customers. Construction of the reservoir and treatment system would cost $110 million, which is far more than the $41 million required for construction of the reclaimed water augmentation component of the Yankee Lake Project. It would not be economically or technically feasible for Seminole to implement this reclaimed water storage and re- treatment system. Stormwater Petitioners also contend that Seminole could use stormwater to meet its reclaimed water augmentation needs, something that is almost unheard of in Florida. For this idea to work, stormwater would have to be captured and stored in order. This would require construction of a stormwater collection and transmission system extending throughout the Northwest Service Area. It also would require construction of a 450-million gallon reservoir and a treatment facility. The capital cost of a stormwater augmentation option would be $171 million, making it technically and economically infeasible. Tri-Party Agreement In December 1996, Seminole and the Cities of Sanford and Lake Mary entered into a contract known as the Tri-Party Agreement for the potential development of a regional reuse system. On its face, the agreement allows Seminole to obtain up to 2.75 mgd of reclaimed water from Sanford. However, in reality, the Tri-Party Agreement is not a feasible source of reclaimed water. First, the Tri-Party Agreement does not guarantee a specific quantity of reclaimed water that will always be available to Seminole. Second, Sanford's effluent is not required to meet the more stringent water quality standards, in particular for nitrogen, established for the Wekiva River Protection Zone, which Seminole’s Northwest-Northeast Service Area is in. Sanford only has to meet a 12 mg/l standard for nitrogen, while 10 mg/l is required for the Wekiva River Protection Zone. There is no indication that Sanford would be willing to guarantee 10 mg/l, and meeting the Wekiva River Protection Zone standards through blending would be problematic because blending would have to occur before introduction into Seminole's distribution system. Finally, Sanford’s reclaimed water transmission system does not operate at a high enough pressure to provide the required flow to Seminole’s system. For these reasons, despite the fact the Agreement has been in effect for over a decade, Sanford has been unable to provide any reclaimed water to Seminole. Iron Bridge WWTP The Iron Bridge WWTP is owned by the City of Orlando (Orlando). Under a contract with Orlando, Seminole sends wastewater from its Southeast Service Area to the facility and is entitled to receive a like amount of reclaimed water from the facility for reuse, up to a limit of 8.5 mgd. As a result, Seminole does not need augmentation for its reclaimed water reuse system for the Southeast Service Area. In addition to itself using reclaimed water under this contract, Seminole also sends some to the City of Oviedo (Oviedo) and to the University of Central Florida (UCF) under a contract for reuse by them. Riverkeeper in particular contends that Seminole should be required to use reclaimed water from the Iron Bridge WWTP to meet its needs for augmentation of its reclaimed water reuse system in the Northwest Service Area. But this would require the construction of multiple conveyance systems and large storage capacity to move sufficient quantities of reclaimed water from the Iron Bridge WWTP to the Northwest Service Area. In addition, it would create an augmentation deficit in the Southeast Service Area or eliminate amounts of reclaimed water being sent to Oviedo and UCF for reuse. The evidence was that this is not a feasible option for Seminole. St. Johns River Seminole’s ultimate selection of the St. Johns River as an AWS source was the culmination of more than a decade of planning and study. The 1994 District Water Supply Needs and Source Assessment found groundwater resources to be limited in Central Florida. The District engaged in the Water 2020 process to identify AWS sources to meet future demands in the region. The Water 2020 evaluation led to the development of the 2000 Surface Water Treatability Study at Lake Monroe on the St. Johns River, near the Yankee Lake site, which found the St. Johns River to be a cost-effective public supply source. In 1999-2000, the District developed the 2000 District Water Supply Plan, which identified the St. Johns River as a potential AWS source for Central Florida. The 2000 District Water Supply Plan was updated in 2004 to specifically identify the St. Johns River near Lake Monroe as a potential water source. The 2005 District Water Supply Plan re-confirmed the St. Johns River near Lake Monroe as a specific AWS project. Updates to the 2005 District Water Supply Plan also identified the Yankee Lake Site as the proposed location of the St. Johns River near the Lake Monroe Project. Starting in 2006, the District began implementation of an action plan for development of AWS sources consistent with the CFCA rules. The CFCA planning process also resulted in the identification of the proposed Yankee Lake Facility as an appropriate AWS source to meet Seminole’s post-2013 demands. In evaluating the St. Johns River as an AWS source, Seminole considered existing withdrawals from the St. Johns River. The Cities of Melbourne and Cocoa have used the St. Johns River for potable supply for several decades, and both are permitted to withdraw quantities greater than the 4.5 mgd requested by Seminole for potable use. In addition, the Cities of Deland, Winter Springs, and Sanford each have been permitted to use the St. Johns River as a reclaimed water augmentation source. These existing permitted uses have proved to be safe and reliable and created a reasonable expectation the river can be used for potable supply and reclaimed water augmentation. In addition to the planning and regulatory efforts described above, the District also established MFLs at various locations along the St. Johns River. In particular, the District established MFLs at State Road (SR) 44, which is 10 miles downstream of the Yankee Lake Site. In developing this MFL, the District determined that 155 mgd could be withdrawn from the St. Johns River upstream of SR 44. Since the requested 5.5 mgd is less than 4% of this quantity, the MFL determinations provide assurance that the river is a reliable AWS source. The capital costs of a 4.5 mgd surface water facility at Yankee Lake on the St. Johns River would be $78 million. The operation cost for a surface water facility at Yankee Lake would be much less than a seawater desalination facility, which would require twice as much energy as the surface water source. Capability and Environmental Concerns General The St. Johns River runs from south to north, starting at its headwaters in Indian River, Osceola, and Okeechobee Counties and emptying into the Atlantic Ocean in Duval County. The District has adopted 6 MFLs along the St. Johns River, and there are numerous United States Geologic Survey gauging stations which provide a long-term record of stage and flow. The St. Johns River Watershed is about 8,900 square miles. The St. Johns has a very gradual elevation decline from its headwater to its mouth. Rainfall, surface runoff, springs, seepage from the aquifer, and ocean tides affect the flow of the River. These characteristics result in relatively slow flow, slow reaction to rainfall, and reverse flows from the tidal influences. Seminole evaluated the historic relationships between rainfall and stage and flow in the St. Johns River over time. Because rainfall is the primary source of water for the St. Johns River, there is a close relationship between rainfall and river flow and stage. The stage and flow of the St. Johns River has fluctuated over time. These fluctuations are attributable to the Atlantic Multidecadal Oscillation, which is a long-term natural rainfall frequency cycle. Increases and decreases in flow and stage of the St. Johns River are explained by changes in rainfall. The evidence does not demonstrate manmade impacts to river stage or flow. The major tributaries of the St. Johns River are the Wekiva and Ocklawaha Rivers. The evidence does not indicate detectable impacts to the flow in the main stem of the St. Johns River due to changes in flow in these major tributaries. MFLs MFLs are defined as limits beyond which further withdrawals would be significantly harmful to the water resources or ecology of the area. MFLs are established based on: the collection of ecological data to identify the most constraining water resource features; the development of hydrologic models to simulate the effects of water withdrawals; the preparation of reports; scientific peer review; and the adoption of standards by the District through formal rulemaking. See § 373.042, Fla. Stat. MFLs are used by the District to assess cumulative impacts on a water body. The MFLs determinations at SR 44 near Deland measure from withdrawals in existence prior to 1999. Existing permitted withdrawals on the St. Johns River upstream of the SR 44 MFL, plus Seminole’s proposed 5.5 mgd withdrawal, total 37.9 mgd. Of this total, 22 mgd was not being withdrawn from the St. Johns River prior to 1999. Seminole used a conservative 25 mgd of new withdrawals to evaluate potential cumulative impacts. A total of 57 mgd of withdrawals from the entire St. Johns River was used to evaluate cumulative impacts associated with Seminole’s proposed withdrawals. This amount reflects the total permitted quantity of water which was not being withdrawn prior to 1999. The District is required to establish recovery strategies when an MFL has been violated and prevention strategies when an MFL will be violated within the next 20 years. None of the MFLs on the St. Johns River require recovery or prevention strategies. Impact of Yankee Lake Withdrawal Flow and Stage The historic flow records do not indicate that the existing withdrawals have had a detectable impact on flow or stage. Since these withdrawals are significantly greater than Seminole’s proposed withdrawal, it is reasonable to conclude that Seminole’s proposed withdrawal also would have an undetectable impact on the St. Johns River. The historic relationship between rainfall and flow can also be used to evaluate whether historic withdrawals have had any impact on flow in the St. Johns River. A double-mass analysis of rainfall and flow on the St. Johns River does not indicate any change in the relationship between rainfall and flow over time, even as the quantity of withdrawals has increased. The evidence was that the proposed withdrawal of 5.5 mgd would not cause a measurable change in either the flow or stage of the St. Johns River on an individual basis or cumulatively with other withdrawals from the River. Salinity Seminole and the District used sophisticated hydrodynamic models to predict the impact of the proposed withdrawal, individually and cumulatively with other withdrawals on the St. Johns. The models were well-calibrated to observed data, including water level, velocity, salinity, and discharge. Pointing to differences between observed and modeled salinities, primarily at the Dames Point Bridge (relatively near the mouth of the river), Riverkeeper's modeling expert, Dr. Mark Luther, expressed concern that the models did not properly account for estuarine or overturning circulation and therefore did not accurately predict salinity changes. Dr. Peter Sucsy, who developed the models, recognized the importance of estuarine overturning circulation. However, with the exception of the Dames Point station, statistical analysis showed a very good fit between simulated and observed data. At the Dames Point Station, the differences between simulated and observed salinities are larger (1.6 parts per thousand). But that location is close enough to the mouth of the river that it often measures marine water and a narrow range in salinities. Taking this into consideration, the model matches the observed data reasonably well. Dr. Sucsy's models are sufficiently accurate to provide reasonable assurance with respect to harm to the estuary system from water withdrawals. Dr. Luther also testified that it would have been more appropriate to examine salinity changes for each layer of the hydrodynamic models, rather than using vertically-averaged salinity values. But Seminole's expert, Mr. Ivan Chou, determined that there was no perceptible difference in the salinity impacts derived from vertically-averaged salinity versus salinity values at specific model layers for the proposed 5.5 mgd and cumulative 57 mgd withdrawals. As a result, it was proper to use vertically-averaged salinities when evaluating the impact of Seminole’s proposed withdrawal. Using the hydrodynamic models, Mr. Chou compared salinity values at 60 points along the St. Johns River from the mouth of the river to Buffalo Bluff, which is 90 river miles upstream, for a pre-1999 baseline scenario, a 5.5 mgd individual withdrawal scenario, a cumulative withdrawal scenario of 25 mgd, a cumulative withdrawal scenario of 57 mgd, and the minimum flow scenario of 155 mgd. The baseline modeling scenario reflects the natural fluctuations in salinity that occur as a result of tidal influence and seasonal changes in rainfall. The natural fluctuation in salinity on a daily basis can be 7 to 8 parts per thousand (ppt), while the seasonal change can be as high as 20 ppt. When the simulated 5.5 mgd, 25 mgd, and 57 mgd withdrawals are plotted against the baseline salinity levels, whether for maximum or minimum daily or 5-year salinities, the differences are undetectable. (For the 155 mgd withdrawal scenario, there is a slightly increased salinity level, but the change is still a fraction of a ppt.) The same results occur when examining average salinities or dry season salinities (May and June). In the 57 mgd withdrawal scenario, the largest increase in average salinity under annual conditions is only 0.135 ppt, and under dry season conditions is only 0.170 ppt. Even in the 155 mgd scenario, the largest predicted increase in average salinity at any point on the St. Johns River is just 0.365 ppt. The withdrawal scenarios have minimal impact on the location of isohalines--a line representing a specific salinity level in the river. Under natural conditions, there are large daily and seasonal changes in the location of a particular isohaline due to tidal effects. For example, the 15 ppt isohaline moves 8.1 miles on the average day. In comparison, the withdrawal of 5.5 mgd would cause the 15 ppt isohaline to move by just 0.02 miles, a withdrawal of 25 mgd would cause the 15 ppt isohaline to move 0.07 miles, and a withdrawal of 57 mgd would cause the 15 ppt isohaline to move 0.59 miles during the dry season. The salinity modeling demonstrates that the impact of Seminole’s proposed 5.5 mgd withdrawal is so small as to be indiscernible with the field instruments used to measure salinity in the St. Johns River. The cumulative withdrawal scenarios of 25 mgd and 57 mgd are similarly minimal and would not be measurable using conventional instrumentation. Nutrients The most prominent manifestation of nutrient imbalance in the St. Johns River is the increase in algal biomass, which can result in algal blooms. In the St. Johns River, algal biomass begins to accumulate in April, and the potential for algal blooms continues through September. Seminole will not make any nutrient discharges to the St. Johns River as part of its proposed use of water. Instead, the proposed withdrawals will remove nutrients from the River. It was determined there would not be a significant hydrodynamic impact from any of the three withdrawal scenarios. A 5.5 mgd withdrawal results in just a 0.17% decrease in flow, a 25 mgd withdrawal results in a 0.8% decrease in flow, and a 57 mgd withdrawal results in a 1.8% decrease in flow. From 1995-2007, the average total nitrogen level in the vicinity of the Yankee Lake site was 1.51 mg/l, while the average total phosphorus concentration was 0.09 mg/l. For 2003- 2007, the average total nitrogen concentration was 1.29 mg/l, while the average total phosphorus concentration was 0.09 mg/l. For the 5.5 mgd withdrawal scenario, the quantity of water removed would result in a 0.13% reduction in nitrogen loading and 0.14% reduction in phosphorus loading compared to the 1995- 2007 levels, and a 0.11% reduction in nitrogen loading and 0.14% reduction in phosphorus loading compared to 2003-2007 levels. A comparison of flow and load reduction for the 5.5 mgd withdrawal shows no impact on water quality. The same relationship holds true for cumulative withdrawals of 25 mgd or 57 mgd. Withdrawals of water from the River can increase residence time, which in turn has the potential to increase biomass in the water body. Seminole and the District used another version of Dr. Sucsy's hydrodynamic model to simulate water age and evaluate the effect of 5.5 mgd and 55.4 mgd withdrawals on residence time in the Lower St. Johns River. Compared to the baseline condition of 1996-2005, a withdrawal of 5.5 mgd is projected to cause a slight increase in the duration of algal blooms at Racy Point and Lake George. Under baseline conditions, an algal bloom with a duration of 60 days is expected to occur once every other year, an algal bloom with a duration of 71 days is expected to occur once every three years, and an algal bloom with a duration of 115 days is expected to occur once every 20 years. When Seminole’s proposed 5.5 mgd withdrawal is applied to these baseline values, the duration of an algal bloom increases by less than one hour once every other year up to 3.2 hours once every 20 years. When the cumulative 55.4 mgd scenario is applied, the duration of an algal bloom increases by 22.6 hours once every other year up to 71 hours once every 20 years. It is possible to offset the elevated algal biomass resulting from the slight increase in residence time from surface water withdrawals by further reducing nutrient loading to the river. Seminole and the District propose to achieve this nutrient reduction through reductions in discharges from the Iron Bridge WWTP. The Iron Bridge facility currently discharges treated wastewater to the Little Econlockhatchee River (the Little Econ), a tributary of the St. Johns River. However, Seminole and the other Iron Bridge participants plan to eliminate the discharge of wastewater to the Little Econ through increased reclaimed water use. The cessation of discharges to the Little Econ from the Iron Bridge facility will more than offset the impacts of increased retention time caused by the Yankee Lake withdrawal. The load reduction achieved through elimination of the Little Econ discharges is 3.3 times greater than the load reduction that would have to be achieved in order to offset the increased residence time. Even at 11.59 mgd, the maximum permitted daily withdrawal from the Yankee Lake intake facility, the Iron Bridge offset would still be 1.7 times greater than the amount needed to offset increased residence time. The District and Seminole have agreed to an additional permit condition that would prohibit Seminole from withdrawing water from the St. Johns River on any day following a day when discharges have occurred to the Little Econ from April 1 to September 15. This additional condition provides reasonable assurance that the proposed CUP will not cause or contribute to an increase in nutrients in the River. It is not uncommon for the District to require permittees to work with other entities to make reclaimed water changes a condition for CUP issuance. Such a permit condition appears in a recent CUP issued to the Orlando Utilities Commission. Riverkeeper in particular contends that these permit conditions are not enforceable without the agreement of the other entities involved in Iron Bridge, namely those who would relinquish a right to discharge to the Little Econ. But the condition clearly is enforceable against Seminole. Ecological Evaluation The evidence provided reasonable assurance that there will be no discernable changes to key ecological parameters as a result of the Yankee Lake withdrawal, individually or cumulatively with other surface water withdrawals from the River system. Ongoing withdrawals on the Peace and Alafia Rivers having a much greater impact on the flow of water in those rivers than the proposed Yankee Lake withdrawal, individually or cumulatively, have not caused significant changes in vegetation, benthic invertebrates, fish population, phytoplankton population, or other indicators. The evidence was that there was no appreciable change in population of the American shad, a common species in the St. Johns River, between the 1970s and 2000s. No appreciable change in the biodiversity of fish species is expected as a result of the proposed Yankee Lake withdrawal, individually or cumulatively. Submerged aquatic vegetation (SAV) provides a static habitat and a food source for aquatic species. The most common SAV in the St. Johns River is Vallisneria americana, or tape grass, which occurs in freshwater and oligohaline habitats. Its ideal salinity level is 1 ppt or less, but it can tolerate salinities up to 8 or 9 ppt. Between 1999 and 2001, an extended drought resulted in a fairly sizable decline in Vallisneria in the Lower St. Johns River due to higher salinities. Data from 2003-2004 indicate that Vallisneria had expanded and re-colonized areas with salinities up to 5 ppt. Since changes in salinity as a result of Seminole’s proposed withdrawal, on an individual or cumulative basis, will be small, it is not expected that there will be a significant impact on Vallisneria, or the aquatic life that depends on it. Riverkeeper witness Robin Lewis testified that existing withdrawals have reduced flows in the St. Johns River, which has impacted the ability of SAV to recover from higher salinities that occur during droughts. However, the graph he relied on to show a declining trend in flows in the St. Johns River only reflected data recorded through 2002; the most recent flow data indicates there has been an increase in flows, with the highest flow on record at SR 44 occurring in August 2008. The evidence provided reasonable assurance that there will be no impact to macroinvertebrates as a result of Seminole’s proposed withdrawal. Macroinvertebrates tolerate wide salinity ranges, and there would be no meaningful change in the distribution of macroinvertebrates due to Seminole’s proposed withdrawal. Impingement and Entrainment The intake structure for the proposed Yankee Lake facility is designed to prevent impingement and entrainment by minimizing the velocity of water entering the structure and by using a series of screens to prevent entry into the structure. The intake structure is in an area where the intake velocity would be equal to or less than the velocity of the river, making the intake structure area an unattractive place for fish to spawn. While fish and other mobile aquatic life would not be expected to be impinged or entrained, it is expected that some immobile aquatic life forms, such as certain fish eggs, will become entrained. Jacksonville’s consultant Terry Cheek estimated that 35,000 American shad eggs could be entrained by Seminole’s proposed withdrawal each year. However, an American shad female typically carries about 470,000 eggs and spawns repeatedly during a season, meaning a single female can produce more than a million eggs in a season. Meanwhile, the average number of female shad removed from the St. Johns River due to recreational fishing is about 1,130 individuals, meaning that fishing removes about 530 million eggs from the St. Johns River every year. Even if the egg density were two orders of magnitude greater than Mr. Cheek assumed, entrainment would remove far fewer eggs from the St. Johns River than recreational fishing. Public Interest The evidence provided reasonable assurance that the issuance of Seminole’s CUP is in the public interest. It will provide a source of needed potable water other than stressed fresh groundwater. It will allow Seminole to maximize reuse of reclaimed water, which will also reduce its need for fresh groundwater. There is reasonable assurance that environmental harm from the issuance of Seminole’s CUP will not be significant and has been reduced to an acceptable amount. St. Johns County in particular contends that, despite all the evidence of reasonable assurance provided, not enough consideration has been given to the impact of Seminole’s CUP project on the Wekiva River Aquatic Preserve and Seminole's Black Bear Wilderness Area. However, additional consideration of those kinds of impacts will be considered in further required permitting for the project. The evidence in this case provided reasonable assurance that the proposed water withdrawal will not significantly harm those natural resources and that harm to those resources has been reduced to an acceptable amount. The Petitioners contend that issuance of Seminole’s CUP should be delayed until after the District completes its two-year AWS Study of the entire St. Johns River basin, including the Oklawaha. The greater weight of evidence indicates that such a delay is unwarranted and would impose additional unnecessary costs on Seminole. Starting in 2006, Seminole implemented an increased rate structure to finance a $156 million bond issue for its water and wastewater capital improvement program, including the Yankee Lake Project. Seminole has also received a $7.5 million grant from the District to finance the project. Seminole has already incurred approximately $4.3 million in engineering design services. If the project were delayed one year, it would incur about $4.5 million of additional costs. If the Yankee Lake Project were delayed more than a year, Seminole would incur additional cost of $15.4 million, including the expenditures to date and the loss of the $7.5 million in grant money. Given the extra costs that would be incurred by Seminole and its residents as a result of any delay in implementation of the Yankee Lake Project, deferring Seminole’s CUP until after completion of the larger AWS study would not be in the public interest. Petitioners' Standing Riverkeeper bases its standing in part on allegations that Seminole’s proposed use will impact the use and enjoyment of the St. Johns River by a substantial number of Riverkeeper’s members. A substantial number of Riverkeeper's members use and enjoy the River for recreation, boating, fishing, watching wildlife, and similar activities. However, it was not proven that Seminole's proposed CUP will affect their use or enjoyment of air, water, or natural resources of the River. Riverkeeper also bases its standing in part on Section 403.412(6), Florida Statutes, which allows not-for- profit corporations to establish standing if they have 25 members residing in the county where the proposed activity is to take place. Riverkeeper introduced evidence that, by the time of the final hearing, it had more than 25 members residing in Seminole County. Some of these Seminole residents did not join Riverkeeper until shortly before the final hearing. Seminole did not object to testimony regarding the new Seminole members of Riverkeeper, and it was given an opportunity to depose the witness during the hearing but declined to do so. (Seminole's objection to admission of an updated membership list into evidence was overruled.) At the conclusion of Riverkeeper's case on the second-to-last day of the final hearing, Riverkeeper made an ore tenus motion to amend its petition to allege standing based on Section 403.412(6), Florida Statutes, and ruling was reserved. See Conclusion of Law 141, infra, for the ruling. Jacksonville and St. Johns County base their standing on Section 403.412(5), Florida Statutes, which allows local governments to establish standing by filing a verified pleading alleging that the permitted activity will have the effect of impairing, polluting, or otherwise injuring the air, water, or other natural resources of the state. Jacksonville and St. Johns County filed the verified petitions required by Section 403.412(5), Florida Statutes. In addition, the evidence proved that Seminole’s proposed CUP will impair, pollute, or otherwise injure the air, water, or other natural resources of the state to some extent, even if not enough to require denial of the CUP application, especially before the agreement between the District and Seminole to add a condition to the CUP.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the District enter a final order granting Seminole's pending CUP 95581 with the conditions specified in the TSR and the additional condition proposed by the District and Seminole regarding nutrient impacts. Jurisdiction is retained for up to 30 days after the District's entry of its final order to rule on Seminole's motions for attorney's fees and costs under Sections 57.105(4) and 120.595(1), Florida Statutes, by a separate final order if Seminole invokes the exercise of that jurisdiction within the 30-day time period. DONE AND ENTERED this 12th day of January, 2009, in Tallahassee, Leon County, Florida. S J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 12th day of January, 2009.
The Issue The issues in this case essentially are whether the Respondent, the Department of Environmental Regulation (DER), should reimburse Anthony F. Kopp, Owner, La Casa Del Sol, for the difference between the cost to him of the DER's remedy for the EDB contamination of the drinking water supply at La Casa Del Sol and the remedy that is least costly to the Petitioner, together with the cost of a new irrigation system, engineering and attorney fees, and other incidental costs to the Petitioner.
Findings Of Fact The Petitioner, Anthony F. Kopp, is the owner of La Casa Del Sol (La Casa), a 40-acre development at 1255 U.S. Highway 27 North, Davenport, Florida. La Casa is divided into 309 mobile home lots, a clubhouse and five acres of common green space. In January, 1987, the Petitioner received a permit for construction of a water supply system for both drinking water and irrigation needs at La Casa. The construction permit was granted with the proviso that, when La Casa's population reached 350, a second backup drinking water well, six inches in diameter at 410 feet, with a casing to 366 feet, and an auxiliary power source would have to be installed. It would cost La Casa approximately $65,000 to install the backup well and auxiliary power source. La Casa did not reach a population of 350 until January, 1991. The St. Johns River Water Management District permitted the construction of the backup well, but the well never was constructed, and the construction permit now has expired. The auxiliary power source also was not installed. The main water supply system for La Casa was installed during the summer of 1987. It included a well and a system of lines for carrying water to each of the 309 lots. It also included hose bibs (faucets) at each lot so that the water also could be used for irrigation at each lot. The system also supplied water for irrigation of the common green space. Although all of the lots at La Casa were connected to the water supply system in the manner described, not all the lots had homes on them. During the summer of 1989, only about 175 of the lots had homes on them; by January, 1991, 198 lots had homes on them. Although not all of the lots were occupied, the entire water supply system was permitted, and no additional permits were required to provide water to the lots. However, when La Casa's population reached 350, the backup well and auxiliary power source would have to be installed under the permit conditions. In about May, 1988, DER tests showed that the La Casa water supply system was contaminated with ethylene dibromide (EDB) at levels in excess of the maximum allowable for drinking water. In October, 1988, the Petitioner completed and filed a Grant Application for EDB Clean-Up Funds. As part of the application, the Petitioner agreed that DER could: arrange for the purchase and installation of appropriate filters and inhibitors; provide a new well; or arrange for the connection of [the Petitioner's] well to an existing public supply system, whichever is more cost-effective as determined by the Department of Environmental Regulation. DER contracted with Continental Water Systems to provide a temporary carbon filter system for La Casa's water supply system to remove the EDB and supply uncontaminated drinking water to the development, pending a permanent solution to the EDB contamination. The temporary filter system was designed to provide 100 gallons per minute of water, which should have been adequate for drinking water needs at La Casa. However, water pressure problems arose due to algal growth and the use of the system for irrigation purposes in addition to the drinking water purposes for which it was designed. DER is a member of the Ground Water Task Force, which met biweekly or monthly to discuss, among other things, potable wells contaminated with EDB. Other member agencies are the Department of Heath and Rehabilitative Services, the Department of Agriculture and Consumer Services, the Department of Transportation and the Department of Community Affairs. The Task Force discussed the La Casa contamination problem and agreed that the possibility of having La Casa connected to an existing water supply should be explored. DER began negotiating both with Polk County and with Haines City for a water line connection. Connection with the Polk County line would have been more expensive, and Polk County was not particularly interested in extending its line. Negotiations continued with Haines City. Negotiations with Haines City progressed to the point that DER was able to present for consideration by the Task Force cost figures for a permanent filter system at La Casa, with ten years of projected cost of operation and maintenance, as compared to the cost of extending the Haines City line. The Task Force agreed with DER that extending the Haines City line north to La Casa and connecting La Casa to it was the most cost-effective use of state funds to remedy the EDB problem at La Casa, particularly in view of other EDB-related drinking water supply problems in the area and anticipated future drinking water supply problems in the area. The Petitioner was not invited to participate in the negotiations with Polk County and Haines City and did not participate in them. Nor was the Petitioner invited to participate in either the DER or the Task Force decision- making process, and the Petitioner did not participate in those processes, either. However, the Petitioner, through his engineering consultant, was made aware in early 1989 that DER was exploring options to have La Casa connected to an existing water supply. DER paid approximately $400,000 for the Haines City water line extension and La Casa connection. This included $90,000 for Haines City impact fees to cover the 175 then existing mobile homes at La Casa (DER actually paid $450 per unit for 200 units), as well as the plumbing contractor fees for connecting La Casa to the extended city water line. It also includes the cost of installing a water meter at La Casa. The ten-year cost to the DER to solve just the La Casa drinking water problem using an EDB filter system would have been less than the cost to the DER of extending the Haines City line and connecting La Casa to it. But the evidence is clear that, in the long run, and taking into consideration other EDB-related drinking water supply problems in the area, and anticipated future drinking water supply problems in the area, the most cost-effective use of state funds to remedy the problem was to extend the Haines City line and connect La Casa to it. (Even the Petitioner's expert witness agreed that the Haines City extension and connection was the most cost-effective use of state funds to remedy the area's EDB problem.) DER advised the Petitioner of its agreement with Haines City in approximately May or June, 1989. By letter dated July 27, 1989, DER explained to the Petitioner the details of the agreement, specifically what DER would pay and what DER would not pay. By the fall of 1989, the Petitioner knew that work was beginning. At the time, the extension of the Haines City line and connection to La Casa was projected for completion in January, 1990, but there were delays, and the city water supply was not ready to be connected to La Casa until August, 1990. By this time, a dispute had arisen between the Petitioner and DER as to the cost to the Petitioner of connecting to the city water, and actual connection was further delayed. Finally, by letter dated October 11, 1990, DER gave the Petitioner an ultimatum: either be connected to the city water supply; or forfeit any state contribution to the cost of remedying the EDB contamination of the Petitioner's water supply. Faced with the prospect of having to open the winter peak season without any drinking water, the Petitioner agreed, under protest, to be connected to the city water supply, and initiated formal administrative proceedings to challenge DER's intended decision to limit the extent to which the DER would cover the Petitioner's costs. There was evidence that the plumbing contractor hired by DER may have caused damage to the landscaping and one mobile home that has not yet been repaired. However, DER acknowledged its responsibility for the damage and intends to have the plumbing contractor repair the damage. There also was evidence that the Petitioner received a bill from Haines City for the installation of a water meter at La Casa. But the evidence also was that DER may already have paid the bill. In any event, DER acknowledges its responsibility for the cost of the water meter as part of the cost of connecting La Casa to the extended city water line. Although DER had the Haines City water line extended in response to the Petitioner's Grant Application for EDB Clean-Up Funds, two commercial properties south of La Casa were connected because of EDB contamination, and the line also was extended north of La Casa in preparation to address anticipated future EDB contamination problems. Under the DER's response to the Petitioner's Grant Application, each additional mobile home unit over 200 connected to the city water supply will require the payment of a $450 impact fee. In addition, Haines City will charge monthly water fees of $1.80 1/ per 1000 gallons for the use of water at La Casa, with a $1,000 minimum charge per month. 2/ Based on current occupancy of 200 lots, the Petitioner estimates water fees of $42,000 per year, figured at approximately $5,000 per month for six peak months (based on a recent peak season monthly bill) and $2,000 per month for six off-peak months. However, it is not clear whether some of that estimated usage includes irrigation. If, in order to save gallonage fees, the Petitioner puts in a separate irrigation system supplied by its well, it will have to put in a separate distribution system since the current system is being used to bring city water to the lots. This would cost approximately $90,000. The Petitioner has paid approximately $2,100 in engineering fees to assess the problem with the temporary filter and to propose solutions, to estimate the cost of installing a separate irrigation system, and to estimate the cost to the Petitioner of connecting to the Haines City water supply. There was no evidence as to the reasonableness of those fees. The Petitioner also has paid approximately $4,500 in attorney fees to negotiate with the DER for payment of a larger portion of the Petitioner's cost of connecting to the Haines City water supply. There was no evidence as to the reasonableness of the attorney fees.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is recommended that the Department enter a final order dismissing the Amended Petition for Formal Hearing in this case. RECOMMENDED this 14th day of March, 1991, in Tallahassee, Florida. J. LAWRENCE JOHNSTON 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 14th day of March, 1991.
The Issue The issues to be determined in this proceeding are: whether the challengers have standing; and (2) whether Proposed Rule 40E-8.221(2) is an invalid exercise of delegated legislative authority.
Findings Of Fact Based on the parties' stipulations and the evidence adduced at the final hearing, the following findings of fact are made: The Parties The District is a government entity existing and operating pursuant to chapter 373, Florida Statutes, as a multi- purpose water management district. The District has the power and duty to adopt MFLs consistent with the provisions of part I of chapter 373. Sanibel is a barrier island sanctuary in Lee County and a duly-formed municipality with a population of more than 6,000. Sanibel is situated at the mouth of the Caloosahatchee River, within the Caloosahatchee's greater estuarine area. Sanibel is known primarily for its natural beauty, including clear blue waters, shell beaches, world-class sport fisheries, and wildlife refuges. That is why tourists come from around the globe to visit Sanibel, and why Sanibel's residents move and remain there. Sanibel actively participated in the rulemaking process for the Proposed Rule from its inception. Sanibel submitted two technical comment letters to the District during the development of the Proposed Rule. Sanibel's natural resources director, James Evans, attended numerous public and technical meetings associated with the development of the Proposed Rule, speaking on the record at each of the public meetings prior to the adoption hearing by the District's governing board. The Town, located on Estero Island in Lee County, is also a barrier island community and duly-formed municipality with a population of more than 6,000. The Town is situated just south of the mouth of the Caloosahatchee River and on the southeastern edge of the Caloosahatchee River's greater estuarine area. The Town is known primarily for its natural beauty, including clear blue waters, shell beaches, world-class sport fisheries, and wildlife refuges. Cape Coral is a duly-formed municipality in Lee County and is the largest city between Tampa and Miami, with a population in excess of 150,000. Cape Coral is bordered on the south by the Caloosahatchee River and has over 400 miles of navigable canals and waterways, all of which are within the Caloosahatchee River's greater estuarine area. In addition, Cape Coral has an assigned load reduction allocation under the Basin Management Action Plan (BMAP) for the Caloosahatchee River Estuary (CRE) due to it being designated as impaired for dissolved oxygen and nutrients. Maintaining sufficient flow in the Caloosahatchee River would have a direct impact on Cape Coral's ability to meet its assigned load reduction allocation. In addition to living on or near the water, a substantial number of the residents of Sanibel, Cape Coral, and the Town engage in water-based recreational activities such as swimming, fishing, boating, kayaking, paddle boarding, bird watching, and nature observation in and around the Caloosahatchee River's greater estuarine area. Fort Myers is a duly-formed municipality in Lee County and has a population of approximately 80,000. Fort Myers is bordered by the CRE throughout its entire jurisdictional boundary. Fort Myers owns and maintains a yacht basin (Ft. Myers Yacht Basin), which includes a mooring field and an anchorage field in the Caloosahatchee River. Fort Myers presented testimony that commercial crabbing and recreational fishing have declined and that it has suffered economic harm due to water quality issues. Fort Myers owns the submerged land in the Caloosahatchee River from Marker 39 to Marker 58, and islands in the river. One such island will be used as a park for recreational activities such as canoeing, kayaking, and hiking for visitors to enjoy the Caloosahatchee River. Fort Myers also owns and operates piers and a public boat ramp within the Caloosahatchee River. Fort Myers' dock master has observed declines in seagrasses in the Caloosahatchee River during his 19-year career working at the Ft. Myers Yacht Basin. Fort Myers has adopted a Harbor Management Plan for the management of its mooring and anchorage fields in the Caloosahatchee River. Fort Myers has also been assigned a load reduction allocation under the BMAP for the CRE, and is responsible for a certain amount of pollution reduction over time. Bonita Springs is a municipality of more than 50,000 in Lee County. The borders of Bonita Springs include portions of Estero Bay, which, along with San Carlos Bay and the Caloosahatchee River, is part of the greater Lower Charlotte Harbor Estuary. Bonita Springs includes wildlife refuges, such as the Estero Bay Aquatic Preserve and Lovers Key State Park and Recreation Area. While Bonita Springs' strategic priorities include environmental protection and water quality, it does not have environmental staff or test water quality. Bonita Springs participates in Estero Bay Management and the Charlotte Harbor National Estuary Program (CHNEP). Bonita Springs provides financial assistance to the Caloosahatchee Citizen Sea Grass Gardening Project. Concerns regarding harm to the CRE and tape grasses are shared by a significant number of residents in Bonita Springs and Estero, including injury to the quality of life and recreational uses such as swimming, boating, and kayaking in the waterways. Estero is a municipality of more than 30,000 in Lee County. Estero borders the eastern portion of Estero Bay. Estero includes wildlife refuges, such as Estero Bay Aquatic Preserve and Koreshan State Park. While Estero has environmental policies, it does not have environmental staff or test water quality. Estero makes financial contributions to CHNEP. Estero is concerned that the Proposed Rule will affect its water quality, which could affect its residents' quality of life. Estero believes it could be harmed by poor water quality because its residents are portable retirees who can move away, or tourists who can choose not to visit. Captiva Island is situated at the mouth of the Caloosahatchee River, within the Caloosahatchee's greater estuarine area. CCP is a Florida not-for-profit corporation representing property owners, businesses, and the community of Captiva Island. Captiva Island is part of unincorporated Lee County and is located north of Sanibel. CCP has 200 financial contributors comprised of property owners, businesses, and residents on Captiva Island. CCP's mission includes protection of clean off-shore water, diverse and healthy marine life, and robust native vegetation along with the protection of mangrove fringe and water quality. CCP works with Lee County on provisions of the County's comprehensive plan, which include the quality of adjacent waters. CCP relied on the expertise of James Evans, the director of natural resources for Sanibel, and on the Sanibel- Captiva Conservation Foundation (SCCF). CCP was advised that the Proposed Rule was not sufficient to protect the environment and Vallisneria americana (Vallisneria) or tape grass during the dry season. Caloosahatchee River and Estuary The watershed of the Caloosahatchee River covers approximately 861,058 acres. The watershed consists of four sub-watersheds, three of which are upstream of the S-79 structure. The Tidal Caloosahatchee Basin sub-watershed (estuarine system) is downstream of the S-79 structure. The S-79 structure captures all the upstream discharges of fresh water that go into the estuarine system through the S-79 structure. Major tidal tributaries of the Tidal Caloosahatchee Basin are the Orange River and Telegraph Creek, which drain into the upper estuary downstream of the S-79 structure. Fresh water inflows from these and other tributaries also contribute fresh water into the estuarine system. The Caloosahatchee River was originally a natural watercourse running from its origin at Lake Flirt to San Carlos Bay. It is currently defined as the "surface waters that flow through the S-79 structure, combined with tributary contributions below S-79 that collectively flow southwest to San Carlos Bay." Fla. Admin. Code. R. 40E-8.021(2). Man-made alterations to the Caloosahatchee River began as early as 1884, but major alterations began in the 1930s with the authorization and construction of the C-43 Canal. The C-43 Canal runs 41.6 miles from Lake Okeechobee at Moore Haven, i.e., from the S-77 structure, to Olga, i.e., the S-79 structure. The C-43 Canal serves as a conveyance feature to drain water from the three sub-watersheds located upstream of the S-79 structure and convey regulatory discharges of water from Lake Okeechobee. In 1957, the United States Army Corps of Engineers (USACOE) prepared a report focused on drainage, flood control, and navigation needs of the Caloosahatchee River Basin, and one recommendation was construction of the S-79 structure. The key objectives of the S-79 structure were to eliminate undesirable salinity in the lower Caloosahatchee River, prevent the rapid depletion of water supplies, and raise the prevailing dry weather water table levels. The S-79 structure was constructed in 1965. It is a lock and dam structure that is also known as the Franklin Lock and Dam. The S-79 structure captures all upstream fresh water discharges that go into the CRE. The S-79 structure demarcates the head of the CRE, which extends 26 miles downstream to Shell Point, where it empties into San Carlos Bay in the southern portion of the greater Lower Charlotte Harbor Estuary. Most of this surface water flow takes a southerly route, flowing to the Gulf of Mexico under the Sanibel Causeway that crosses San Carlos Bay. When fresh water inflows are high, tidal action pushes some of this water back up into Matlacha Pass and Pine Island Sound. Additionally, some water exits to the south and flows into Estero Bay through Matanzas Pass. Salinity exhibits a strong gradient in the CRE. Changes in the watershed upstream of the S-79 structure have profoundly influenced the delivery of fresh water to the CRE. Runoff is now more variable with higher wet season flows and lower dry season discharges. Large volumes of fresh water during the wet season can flush salt water from the tidally-influenced sections of the water body, resulting in low salinity conditions throughout most of the CRE. In contrast, fresh water inflow at the S-79 structure can stop entirely during the dry season, especially during significant drought events. This results in saline intrusion that can extend upstream to the S-79 structure. Fluctuations of this magnitude at the head and mouth of the system cause mortality of organisms at both ends of the salinity gradient. Downstream of the S-79 structure, the CRE was significantly altered by multiple dredging activities, including the removal of extensive shoals and oyster bars. Seven automobile bridges, a railroad trestle, and the Sanibel Causeway were built between the 1880s and 1960s. A large canal network was built along the northern shoreline of the CRE in Cape Coral. To provide navigational access from the canal network to deeper water, multiple access channels were dredged within the CRE. Alterations to the delivery of fresh water combined with structural changes to the tidally-influenced sections of the water body have had lasting ecological consequences. These include the loss of extensive shoals and oyster bars, loss of a flourishing bay scallop fishery, and significant decline in seagrass cover in deeper areas. MFLs An MFL is the limit at which further withdrawals would be significantly harmful to the water resources or ecology of the area. The District's rules define significant harm as the "temporary loss of water resource functions, which results from a change in surface or ground water hydrology, that takes more than two years to recover, but which is considered less severe than serious harm." Fla. Admin. Code R. 40E-8.021(31). The rule further specifies that a water body's specific water resource functions addressed by an MFL are defined in the MFL technical support document. Id. MFLs are calculated using the best information available. The regulatory agency is required to consider changes and structural alterations to watersheds, and the constraints such changes or alterations placed on the hydrology of an affected watershed. Certain waterbodies may not serve their historical hydrologic functions and recovery of these waterbodies to historical hydrologic conditions may not be economically or technically feasible. Accordingly, the regulatory agencies may determine that setting an MFL for such a water body based on its historical condition is not appropriate. Caloosahatchee MFL For the CRE, MFL criteria were designed to protect the estuary from significant harm due to insufficient fresh water inflows and were not guidelines for restoration of estuarine functions to conditions that existed in the past. The MFL criteria consider three aspects of the flow in terms of potential significant harm to the estuary: (1) the magnitude of the flow or the volume of fresh water entering the estuary; (2) the duration of time that flows can be below the recommended level before causing significant harm; and (3) the return frequency, or the number of times the MFL can be violated over a number of years before it results in significant harm, recognizing that natural climatic variability will be expected to cause fresh water inflows to fall below recommended levels at some natural frequency. The CRE MFL initially adopted in 2001 was primarily based on the salinity tolerance of one valued ecosystem component (VEC). The VEC was Vallisneria americana or tape grass, a fresh water aquatic plant that tolerates low levels of salinity. A major assumption of this approach was that flow and salinity conditions that protect Vallisneria would also protect other key organisms in the estuary. The 2001 CRE MFL was based on a regression model for estimating the relationship between surface salinity measured at the Ft. Myers monitoring station located in the Ft. Myers Yacht Basin and discharge at the S-79 structure. Although the District monitors surface and bottom salinity at multiple stations in the CRE, the Ft. Myers monitoring station is located centrally in the CRE and at the historical downstream extent of the Vallisneria habitat. The Ft. Myers monitoring station also has the most comprehensive period of record of monitoring data available. The fixed data sondes that monitor surface and bottom salinity are located at 20 percent and 80 percent of total river depth measured at mean low water. The data sondes continuously measure temperature and specific conductivity and, depending on the manufacturer, contains programs that calculate salinity. Those calculations are based on standards recognized and used worldwide by estuarine, marine, and oceanographic scientists.1/ The regression model only implicitly included inflows from the Tidal Caloosahatchee Basin sub-watershed downstream of the S-79 structure. To address this, during the 2003 re-evaluation, a linear reservoir model of Tidal Caloosahatchee Basin inflows was developed. The regression model results showed that a total inflow from S-79 plus the Tidal Caloosahatchee Basin of about 500 cubic feet per second (cfs) was required to produce a salinity of 10 at the Ft. Myers monitoring station. Thus, the 2001 CRE MFL of 300 cfs measured at the S-79 structure would produce a salinity of 10 at the Ft. Myers monitoring station only with additional inflow from the downstream Tidal Caloosahatchee Basin sub- watershed. However, that additional inflow estimate was highly uncertain. The conclusion was that actual flow measurements over a period of time were needed in order to perform more robust calibrations for the new models that were being developed. The Re-evaluation The District's re-evaluation effort began in 2010 after the Conservancy of Southwest Florida filed a petition requesting review of the Caloosahatchee MFL. At the time, the governing board denied the petition but directed staff to undertake additional research and monitoring to ensure a future revision would be supported by the best information available. The first step was to review the September 2000 Final Peer Review Report (PRR) for the initial adoption. The 2000 PRR identified several items the District should consider, including a hydrodynamic salinity model, a numerical population model for Vallisneria, quantification of habitat value for Vallisneria, and documentation of the effects of minimum flows on downstream estuarine biota. The 2000 PRR documented concerns that the current MFL was based solely on the salinity tolerance of Vallisneria and recommended using multiple indicator species. To address those recommendations, the District conducted studies to evaluate multiple ecological indicators, such as zooplankton, aquatic vegetation, oysters, benthic communities, and blue crabs, in the Caloosahatchee from the S-79 structure to beyond Shell Point. In addition, the District collected flow data from the Tidal Caloosahatchee Basin sub-watershed for at least five years to develop watershed, flow, and hydrodynamic models that could properly simulate inflows and salinity responses. When the initial research was complete in 2016, the District published the Draft Science Document containing 11 component studies. In September 2016, the District held a two- day Science Symposium to present the 11 component studies and gather public comment. In response to public comment, the District performed additional evaluations, modeling, and updated the component studies to produce a Draft Technical Document. A Peer Review Panel reviewed the Draft Technical Document, which included the Draft Science Document. The Peer Review Panel has over 150 years of combined relevant scientific experience. The Peer Review Panel toured the CRE by air and water. The District also held a Peer Review Session to engage the public and obtain feedback. The Peer Review Panel's 2017 report (PRP report) stated that the District had "crafted a well-executed and well- documented set of field and laboratory studies and modeling effort" to re-evaluate the CRE MFL. The PRP report supported the 11 component studies, the modeling, the evaluations, and the initial proposed rule language. The Final Technical Document published in January 2018 incorporated five different models and additional science, examining the entire watershed and the criteria itself. The Final Science Document was Appendix A to the Final Technical Document and contained the scientific research and analysis that was done for the 11 component studies, the modeling, and the additional scientific analyses performed in response to public and stakeholder input. The District initiated rule development in December 2017. Rule development workshops were held in February and June 2018 and a stakeholder technical meeting was held in May 2018. The District validated the comments after each workshop and meeting, and revised the proposed rule language. The District published its Notice of Proposed Rule on July 23, 2018.2/ At its September 13, 2018, meeting, the District's governing board held a public hearing on the Proposed Rule. The mayors of Sanibel, Cape Coral, and the Town publicly commented at the hearing. After considering public comments, the governing board adopted the Proposed Rule. The District documented and responded to each public comment, memorializing the information in the Final Technical Document. Later, after the rule workshops and May 2018 technical meeting, the District prepared and presented all of the updated information, including public comment, at the September 2018 adoption hearing. Thus, the District's re-evaluation process was open and transparent. The Re-evaluated Caloosahatchee MFL The science supporting the re-evaluation involved a comprehensive assessment of the effects of diminished dry season fresh water inflows on the CRE. The dry season was chosen for two reasons. First, because it is well-established that the upstream migration of salt combined with reduced fresh water inflow alters the health and productivity of estuarine habitats. Second, because the dry seasons are the times when the current MFL criteria are likely to be exceeded or violated. The 11 component studies targeted specific concerns regarding physical and ecological characteristics. Together they offered a holistic understanding of the negative effects of diminished fresh water inflow on estuarine ecology. The re-evaluated MFL criteria were developed using a resource-based approach. The approach combined the VEC approach and the habitat overlap concept. The habitat overlap approach is based on the idea that estuaries serve a nursery function and salinity determines the distribution of species within an estuary, including distribution during different life stages. The combined approach studied the minimum flow requirements of the various indicator species in terms of magnitude, duration, and return frequency, resulting in the following three aspects of the flow: (1) for magnitude, a 30-day moving average flow of 400 cfs measured at the S-79 structure; for duration, an MFL exceedance occurs during a 365-day period when the 30-day moving average flow at S-79 is below 400 cfs and the 30-day moving average salinity exceeds 10 at the Ft. Myers salinity monitoring station; and (3) for return frequency, an MFL violation occurs when an exceedance occurs more than once in a five-year period. The magnitude component is based on the salinity requirements of Vallisneria, along with results from the 11 studies modeling salinity and considering the salinity requirements of the other VECs. The duration component is based mainly on the estimates of rate of loss of Vallisneria shoots when salinity rises above 10 and the recovery rate of the shoots when salinities fall back below 10. Return frequency was determined based on long-term rainfall records rather than flow measurements from the S-79 structure, which the PRP report felt was well justified. In addition to the component studies, the re-evaluated MFL criteria and existing recovery strategy were evaluated using a suite of hydrologic and ecological models simulating long-term fresh water inflow to the CRE associated with varying management options, the resulting salinity in the CRE, and the ecological response of indicator species that are sensitive to low fresh water inflows. Five models were utilized. Three models simulated fresh water inflows to the CRE: two for S-79 flows; and one for Tidal Caloosahatchee Basin sub-watershed flows. The other two models were a three-dimensional hydrodynamic salinity model and a Vallisneria model. Tidal Caloosahatchee Basin sub-watershed has a number of tributaries that drain fresh water into the CRE. The flow at several of the tributaries was monitored for a five-year period. The measured flow was used to calibrate a watershed model and conduct a long-term simulation. The results showed an average fresh water inflow for all seasons of approximately 430 cfs. The average fresh water inflow during the dry season was 245 cfs while the wet season average fresh water inflow was 613 cfs. Fresh water inflow from the Tidal Caloosahatchee Basin sub- watershed was approximately 20 percent of total fresh water inflow to the CRE while 80 percent was released through the S-79 structure. Petitioners' and Intervenors' Objections 400 cfs Is Too Low Sanibel relied on a memorandum prepared by Dr. David Tomasko (Tomasko report) concerning his company's review of the January 2018 Final Technical Document supporting the Proposed Rule. The Tomasko report, dated October 23, 2018, was in the form of a "technical memorandum" outlining "preliminary findings." The Tomasko report was admitted as a joint exhibit; however, Dr. Tomasko did not testify at the final hearing. The Tomasko report is hearsay that was not used to supplement or explain competent direct evidence. Although hearsay is admissible in this proceeding, it cannot be the sole basis for a finding of fact.3/ See § 120.57(1)(c), Fla. Stat. The District's expert witnesses, who testified at the final hearing, explained that ten of the 11 component studies identified average indicator flows at S-79 ranging from 237 to 545 cfs with standard deviations ranging from plus or minus 57 to plus or minus 774 cfs.4/ The District's experts performed three different evaluations of those flow results. They identified the mean of all the means, calculated the median of the means, and performed a probability density function. The flow results for each of the three evaluations were 381 cfs, 400 cfs, and 365 cfs, with standard deviations that ranged from plus or minus 277 cfs to plus or minus 706 cfs. The District's experts testified that the three flow results are indistinguishable from a statistical point of view. The District chose 400 cfs because it was the highest flow result, and, therefore, the most protective of the three. The Petitioners and Intervenors failed to present evidence that showed any deficiencies in the District's component studies, hydrologic, hydrodynamic, or statistical modeling, or analysis of compliance data. The preponderance of the evidence established that the District used the best available science to calculate the MFL criteria. The District did not act arbitrarily or capriciously when it chose 400 cfs as the magnitude component of the MFL criteria. Inclusion of Salinity in the MFL Criteria The preponderance of the evidence also established that Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE. It supports essential ecological goods and services, is sensitive to salinity fluctuations at the ecosystem scale, and has value to a variety of stakeholders. The location of Vallisneria habitat in the upper CRE and its negative response to increased salinity made it an excellent candidate as an ecological indicator for fresh water inflow. A combination of field monitoring, mesocosm studies, and modeling results allowed the application of Vallisneria responses as a platform to quantify the effects of high salinity duration in the upper CRE. Component Study Eight reviewed the development and initial application of a simulation model for Vallisneria in the CRE. The Vallisneria model was used to evaluate the salinity conditions that led to net annual mortality, or, in other words, the duration of high salinity exposure that led to decreased Vallisneria shoots versus the duration of low salinity conditions required for recovery. Component Study Seven included an analysis of the relationship between the number of consecutive days where salinity at the Ft. Myers monitoring station was greater than 10 and the percentage of initial Vallisneria shoots remaining at the end of each high salinity period. To further evaluate the duration element associated with the MFL criteria, the field monitoring data contained in Component Study Seven was evaluated with the mesocosm and modeling results. All three sources were analyzed similarly to derive a combined curve showing high salinity exposure duration that is significantly harmful to Vallisneria. The model also provided information that was used to quantify the duration of low salinity conditions required for Vallisneria to recover a relative fraction of shoots after high salinity exposure. Merging the exposure and recovery evaluations facilitated a determination of the unfavorable salinity duration that could significantly harm Vallisneria habitat. With significant harm defined as the environmental harm from which two years are required to recover, the determination was that Vallisneria should experience no more than 55 consecutive days of salinity greater than 10. However, stakeholders expressed concerns regarding the percentage loss of Vallisneria habitat after 55 days of high salinity exposure. In response, the District conducted further analysis of modeling results and revised the duration component to accept the stakeholder recommendation, now expressed in the Proposed Rule, of a 30-day moving average salinity greater than 10. The Petitioners and Intervenors argued that by expressing the MFL as a "flow plus salinity component" the Proposed Rule enlarges, modifies, or contravenes the specific provisions of law implemented. However, the duration component is part of compliance and represents the duration of time that flows can be below the recommended level before causing significant harm to the indicator species Vallisneria. The MFL in the Proposed Rule is a 30-day moving average flow of 400 cfs measured at the S-79 structure. Flow is both measured and operationally controlled at the S-79 structure. However, as previously found, there are other sources of fresh water entering the CRE downstream of the S-79 structure. The District does not control and cannot control these downstream sources, which modeling reveals contribute approximately 20 percent of total fresh water inflow to the CRE. By including salinity, the District can account for fresh water inflows coming from the tidal basin when there are low or no flows at S-79 since the significant harm threshold in the CRE is directly related to salinity tolerance of the indicator species Vallisneria. The District's experts also testified that salinity can be used as a flow component because it is not affected by chemical or biological processes and is an indicator of how much fresh water is entering the system.5/ Salinity is included in the duration component of the MFL criteria and is an exceedance criterion because the science established that the salinity gradient is crucial to the overall health of the CRE. Including salinity in the duration component of the MFL criteria achieves the purpose of the statutory mandate to set MFLs that are designed to avoid significant harm to the water resources and ecology of the area. No Unit of Measurement for Salinity The Petitioners and Intervenors argued that the Proposed Rule is vague because the language does not contain any units for salinity. The UNESCO calculation is the standard equation used by the estuarine and marine science community to convert specific conductivity and temperature data to salinity. The District's experts testified that the UNESCO calculation reports salinity as a ratio, which is a dimensionless number and has no units. The District uses the UNESCO calculation and performs the conversion in a spreadsheet that it maintains. In some instances, certain brands of data sondes are programmed to perform the calculation and provide the salinity number. The preponderance of the evidence established that use of the practical salinity unit (PSU) is not technically correct. PSU is a misnomer, a pseudo-unit equivalent to a unitless salinity number. The Petitioners' and Intervenors' expert witness, Dr. Anthony Janicki, conceded there is no difference between reporting salinity as unitless or as PSU. And although technically incorrect, he suggested that placing the word "practical" or putting "PSU" in the Proposed Rule would reduce confusion and vagueness. However, since the preponderance of the evidence established that use of PSU is not technically correct, the use of a pseudo-unit would actually cause confusion instead of reduce confusion. The Petitioners and Intervenors also argued that the Proposed Rule is vague because the language does not state that the method of measuring salinity is specific conductivity, or that the equation used to convert specific conductivity and temperature data to salinity is the standard developed by UNESCO. The Petitioners and Intervenors essentially argued that members of the public and those who may be regulated by the Proposed Rule are left to guess about the method or methods used to measure salinity. Because the Proposed Rule identifies and locates by latitude and longitude coordinates the Ft. Myers salinity monitoring station as the location where salinity would be measured for compliance, the Proposed Rule language is not vague. The Proposed Rule is not vague because it does not describe the data sondes, what parameters are measured by the data sondes, and how those parameters are converted to a salinity number. Salinity Monitoring Location and Mean Low Water The Petitioners and Intervenors argued that the Proposed Rule is vague for failing to define the phrase "20% of the total river depth at mean low water," and is arbitrary or capricious for failing to include more than one salinity monitoring station. Total river depth or the water column depth is a standardized measurement that is made from the surface down to the bottom of the river bed. Mean low water is commonly understood in the oceanographic and coastal sciences community as the average of all low tides over the time period defined as the national tidal datum epic. The District's expert witness, Dr. Cassondra Armstrong, testified that mean low water can be determined by using two documents prepared by the National Oceanographic and Atmospheric Administration (NOAA), i.e., the NOAA tide charts and glossary. The District's expert witnesses testified that "20% of the total river depth at mean low water" is the location of the data sonde at the Ft. Myers monitoring station that measures surface salinity. This is also the depth at which Vallisneria is located in the CRE. Since, the Proposed Rule language simply identifies the location of the existing data sonde at the Ft. Myers salinity monitoring station, the language is not vague. The preponderance of the evidence established that the Ft. Myers salinity monitoring station has two salinity data sondes, the one at 20 percent of the total river depth and the other at 80 percent. The data sonde at 20 percent of the total river depth was identified in the Proposed Rule for the following reasons. First, this is the depth where Vallisneria grows and is representative of the salinity exposure for Vallisneria. Second, it guarantees the data sonde is always submerged and able to record data. Third, it has the most comprehensive period of record of monitoring data available. As previously found, Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE. The location of Vallisneria habitat in the upper CRE and its negative response to increased salinity made it an excellent candidate as an ecological indicator for fresh water inflow. Because the preponderance of the evidence established that Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE, the choice of the Ft. Myers monitoring station is not arbitrary or capricious. Water Resource Functions vs. Environmental Values The District's MFL rule specifies that a water body's specific water resource functions addressed by an MFL are defined in the MFL technical support document. See Fla. Admin. Code R. 40E-8.021(31). The Final Technical Document identified the relevant water resource functions of the CRE as fish and wildlife habitats, estuarine resources, water supply, recreation, navigation, and flood control. The Petitioners and Intervenors argued that the environmental values listed in Florida Administrative Code Chapter 62-40, also known as the Water Resource Implementation Rule, were not adequately addressed in the Final Technical Document. A proposed rule challenge is not the proper forum to determine whether a proposed rule is consistent with the Water Resource Implementation Rule. Such a determination is within the exclusive jurisdiction of the Department of Environmental Protection under section 373.114(2), Florida Statutes. Consistency of the District's Proposed Rule with the Water Resource Implementation Rule of the Department of Environmental Protection is not a basis in this proceeding for a finding that the Proposed Rule is an invalid exercise of delegated legislative authority. Other Issues The Petitioners and Intervenors raised other issues during the hearing, although not specifically argued in their proposed final order. Since those issues were identified as disputed issues in the Joint Pre-hearing Stipulation, they are addressed below. 1. Elimination of Single-day Exceedance Criterion During the rulemaking process, Sanibel and SCCF sent the District a letter requesting justification for eliminating the single-day exceedance salinity criterion in the current rule. The District staff evaluated the available Caloosahatchee River MFL compliance record, dating back to when the MFL was adopted in September 2001. The District maintains a historical record of MFL monitoring data and reviewed it to determine if the single-day exceedance salinity criterion was exceeded before the 30-day moving average criterion. The compliance record showed five exceedance events of the single-day salinity criterion have occurred. However, the compliance record also showed that the 30- day moving average salinity criterion had already been exceeded before the five events occurred. In other words, the single-day criterion was never exceeded before the 30-day moving average criterion. Based on this evaluation, the District eliminated the single-day exceedance salinity criterion because it did not provide any additional resource protection. The District's decision was not arbitrary or capricious. 2. Not Using the Latest Model Evaluation of recommended MFL criteria and a recovery strategy for the CRE were greatly aided by integration of a suite of hydrologic and ecological models simulating (1) long-term fresh water inflow associated with varying management options, (2) the resulting salinity in the estuary, and (3) ecological response of indicator species that are sensitive to low fresh water inflows. Five models were specifically utilized, including three models for simulations of fresh water inflows to the CRE, a three-dimensional hydrodynamic salinity model, and a Vallisneria model. The three models simulating fresh water inflows included (1) the South Florida Water Management Model (SFWMM) to simulate fresh water discharges at S-79, which includes regional operations of Lake Okeechobee and incorporates Caloosahatchee River irrigation demands; (2) the C-43 Reservoir Model, which uses the SFWMM-simulated daily S-79 flow as input and simulates the management benefit of the C-43 Reservoir; and (3) the Watershed (WaSh) Model to simulate tidal tributary inflow from the Tidal Caloosahatchee Basin sub-watershed. The Caloosahatchee Hydrodynamic/Salinity Model was based on the Curvilinear Hydrodynamic Three-dimensional Model (CH3D) modeling framework with the functionality of simulating the spatial salinity structure across the entire estuary. The Vallisneria Model took the CH3D modeled salinity as input to simulate Vallisneria growth at critical locations in the estuary. The District did review the more recent Environmental Fluid Dynamic Code (EFDC) model developed for the Caloosahatchee Total Maximum Daily Load (TMDL) and being used by the Department of Environmental Protection. The District's expert witness, Dr. Detong Sun, testified that until 2014, the hydrodynamic part of the EFDC model was not working well. He testified that in 2016, the District still had concerns and suggested the use of the District's continuous monitoring data from seven locations across the CRE rather than grab samples for model calibration. Dr. Sun's opinion was that the EFDC model has improved in recent years, but was still behind the CH3D model in terms of performance. The District's expert witness, Dr. Amanda Kahn, testified that the water quality component of the EFDC model was not appropriate for this re-evaluation because the MFL is about water quantity, not water quality. The water quality component of the EFDC model addresses nutrient loadings, not minimum flows. Dr. Kahn also testified that in setting MFL criteria for the CRE, salinity was not a water quality component. Salinity was used as a water quantity component because it does not change with biological processes and can be a measure of how much fresh water is coming into the system. Based on a preponderance of the evidence, the District's decision not to use the EFDC model was not arbitrary or capricious. 3. Seasonality The Petitioners and Intervenors argued that the District is required to set an MFL that varies by season. For the CRE, the District set MFL criteria that protect the system from low flow that would occur in either the wet or dry season. As previously found, the re-evaluation studies focused on the dry season for two reasons: first, because it is well-established that the upstream migration of salt combined with reduced fresh water inflow alters the health and productivity of estuarine habitats; and second, because the dry seasons are the times when the current MFL criteria are likely to be exceeded or violated. The MFL statute states that "when appropriate, [MFLs] may be calculated to reflect seasonal variations." § 373.042(1)(b), Fla. Stat. The preponderance of the evidence showed that for the CRE, it was not necessary to set an MFL that varied by season. Improper Purpose The Petitioners, Sanibel, Cape Coral, and the Town, did not participate in this proceeding primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of litigation. The Petitioners did not participate in this proceeding for an improper purpose. The Intervenors, Fort Myers, Estero, Bonita Springs, and CCP, did not participate in this proceeding primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of litigation. The Intervenors did not participate in this proceeding for an improper purpose.
The Issue The issue in this case is whether Bocilla Utilities, Inc. is entitled to a public drinking water construction permit for the expansion of an existing reverse-osmosis water plant located on Don Pedro Island.
Findings Of Fact Bocilla Utilities, Inc. (Applicant) was incorporated in the mid-1980s for the purpose of supplying water to a residential development being developed by some or all of the principals of the water utility. The residential development is on a bridgeless barrier island in Charlotte County. Applicant initially proposed locating the plant on the mainland with submerged pipes to the island. This proposal was approved by the Army Corps of Engineers and Department of Environmental Regulation, but the Trustees of the Internal Improvement Trust Fund denied Applicant's request for an easement across submerged state lands. After failing to obtain a submerged land easement, Applicant obtained the permits to build a reverse-osmosis (RO) water plant at its present location on the barrier island. Included among the permits was a permit from the Department of Natural Resources dated September 11, 1985, allowing Applicant to construct the water treatment plant, two underground concrete water storage tanks, and a tennis court on top of the tanks up to 100 feet seaward of the coastal construction control line. Applicant is a certificated utility that, since September 1994, has been regulated by the Public Service Commission. It was previously regulated by Charlotte County. By Application for a Public Drinking Water Facility Construction Permit filed January 26, 1995 (Application), Applicant requested a permit to expand the treatment capacity of its water plant from 30,000 gallons per day (gpd) to 120,000 gpd. By installing the new treatment equipment in two stages, the plant would have an immediate capacity of 60,000 gpd. Applicant proposes no material changes to the existing water storage tanks, distribution system, or the size or location of the building that houses the existing and proposed water treatment equipment. The Application form asks Applicant to identify any well construction permits obtained from the water management district and to provide a map showing any sanitary hazards within 500 feet of each proposed well. The Application form requires Applicant's professional engineer to attest that the project complies with Chapter 62-555, Florida Administrative Code. The Engineering Report attached to the completed Application supplies the requested information, but explains that Applicant's hydrogeologist had not, as of the date of the report, obtained the well-construction permits from the water management district. By Intent to Issue dated February 27, 1995, the Department of Environmental Protection (DEP) gave notice of its intent to issue the requested permit. Noting that it has permitting jurisdiction under Section 403.861(9), Florida Statutes, and that the project is not exempt, DEP determined that a public drinking water construction permit is required for the proposed work. The Intent to Issue is based on DEP's belief that reasonable assurances have been provided to indicate that the proposed project will not adversely impact water quality and the proposed project will comply with the appropriate provisions of Florida Administrative Code Rules 62-4, 62-550, 62- 555 and 62-699. Petitioners timely objected to the issuance of the proposed permit. Petitioners reside in Applicant's certificated area on the barrier island. They presently obtain their water from private wells or cisterns, rather than Applicant. If the permit were granted so as to expand Applicant's production capacity, Petitioners would be more likely required to obtain water from Applicant due to Charlotte County's mandatory hookup ordinance. About a week before filing the Application, Applicant applied on January 20, 1995, to the Southwest Florida Water Management District (SWFWMD) for permits for the construction of the two wells included in the draft permit. SWFWMD granted these permits on February 8, 1995, about three weeks after receiving the applications. Consistent with its normal practice in granting well-construction permits, SWFWMD did not provide interested persons with a point of entry to challenge the permits. The SWFWMD permits provide in part: Compliance with state and local county health regulations as per Chapter 17-555, Florida Administrative Code (F.A.C.), is required via the Drinking Water System Permit. Compliance with Chapters 17-532 and 17- 555, F.A.C., on construction standards and grouting procedures for Public Supply Wells shall be followed. * * * This well site has been judged as satisfactory based on the location and information provided to [SWFWMD] at the time of the well site inspection. . . . * * * Public Supply Wells must meet certain setback requirements from all potential sources of contamination. To obtain and retain your Drinking Water System Permit, please coordinate any future development of the surrounding property within 200' of your well site with the Charlotte County Health Department. * * * By letter dated February 14, 1995, from a SWFWMD representative to Applicant's hydrogeological consultant, SWFWMD acknowledged that it granted Applicant a setback variance of 100 feet from nearby septic systems in permitting the two new wells. The letter states that the "variance is based upon the known geohydrology of the area and the proposed construction of the wells," as well as an understanding that the "existing public system is working out with no problems." A month later, a letter from a DEP engineer identifies various types of sanitary hazards and implicitly ratifies the setback variance granted by SWFWMD. By letter dated March 14, 1995, Gary Maier identified sanitary hazards as septic tank systems, sewer lines, swimming pools and associated chemicals, pet excretions, and residential chemicals such as pesticides, fertilizers, paints, oils, and solvents. Mr. Maier's letter acknowledges that SWFWMD had granted a variance from 200 feet to 100 feet "due to geologic and treatment conditions," but cautions that "any further decrease in setbacks for sanitary hazards would be imprudent." Applicant's water plant is located on Don Pedro Island, which is part of an island chain consisting, from north to south, of Knight Island, Don Pedro Island, and, usually, Little Gasparilla Island. The low-lying island chain fronts the Gulf of Mexico on the west. The northern end of the island chain abuts Lemon Bay on the east. Over the years, storms have opened and closed passes at various points along the island chain. The island chain is vulnerable to flooding, and some areas are more vulnerable than others. One of the historic passes is Bocilla Pass. The plant site area is about a half mile south of this now-closed pass. The Gulf beaches on either side of the point at which the Bocilla Pass emptied into the Gulf have suffered considerable erosion in recent years, to the point that recently built homes have been inundated by water and had to be removed or razed. The plant site area includes the building housing the water treatment and other equipment, two 50,000-gallon storage tanks immediately to the west of the building, the existing water supply well located just east of the building, and the two proposed water supply wells located a short distance east and south of the building. The existing storage tanks, which mark the westernmost extent of the plant site area, are about 235 feet east of a pronounced erosion line along the Gulf shore and are separated from the Gulf by South Gulf Boulevard. Immediately adjacent to the tanks is the building housing the water treatment equipment. The two proposed wells would be located about 200 and 450 feet south of the tanks. The plant site area is much closer to water on the east. The southerly proposed well is about 12 feet west of the mean high water line of Bocilla Lagoon, and the northerly proposed well is about 16 feet west of the mean high water line of Bocilla Lagoon. The building housing the water treatment equipment is further away from the water, but still less than 50 feet. Bocilla Lagoon is a long and narrow waterway that was dredged in a north-south direction parallel to the Gulf shoreline. Bocilla Lagoon is closed off by land less than a quarter of a mile south of the plant site area. The lagoon runs to the north to connect to what remains of Bocilla Pass, which then runs easterly a short distance to a dredged extension of Lemon Bay. The building housing the water treatment equipment and the storage tanks are not located in the vulnerable FEMA V[elocity] zone. However, the record does not establish the location of the proposed wells relative to the V- zone. Testimony concerning the location of the V-zone relative to the water plant establishes only that the building, not the two proposed wells, are safely outside the V-zone. Nothing in the record establishes contour lines on the barrier island in the vicinity of the plant site area or the elevation of the land at the site of the two proposed wells. Applicant has recently upgraded the security of the storage tanks through the addition of locks to the manholes. The installation of fences is impractical and unnecessary because the tanks are topped by a six-inch, reinforced slab of concrete that also serves as tennis courts. The proposed wells would be well constructed. They would extend 167 feet into a confined artesian aquifer. The concrete pressurized grouting coupled with a potentiometric surface of seven feet make it unlikely that the wells would be vulnerable to contaminants. During severe-storm conditions, pumping would cease, leaving the system in its naturally pressurized state, so that surface water could not easily flow down into the well. Additionally, the RO filtration technology is one of the most effective at eliminating contaminants from drinking water. However, failing to have shown that the two proposed wells are outside the V-zone, Applicant has also failed to provide reasonable assurances that the two proposed wells would be protected from damage from the velocity wave action associated with the V-zone. Applicant has constructed and operated the water plant in an exemplary fashion. Applicant has at all times met or exceeded applicable standards for water quality, safety, and operations. Original construction exceeded minimum requirements and added to the durability of the fixtures. The building housing the water treatment equipment and hydropneumatic tank has been issued a floodproofing certificate by a registered engineer. The certificate states that, with human intervention in the form of bolting predrilled plywood boards over openings, the plant is waterproofed to an elevation of 14 feet NGVD, which is one foot higher than the FEMA-supplied base flood elevation of 13 feet NGVD. Applicant employs an operations manager with a Class A license rather than one with merely a Class C license, even though only a Class C operator is required for a water plant of this size. Also, Applicant maintains a low-level chlorine indicator, even though not required to do so due to the small size of the utility. The relevant sewage flows from the quantity of water that would be drawn by each proposed well would be greater than 2000 gpd. Near the proposed wells are single- and multi-family residences served by on-site sewage disposal systems, the above- described road, a swimming pool on the other side of the road, an injection well, and the treatment plant at which Applicant stores anti-scaling agents, ammonia, chlorine, and acid. However, Applicant has shown that none of these items is within 100 feet of the proposed wells. Bocilla Lagoon is not a sanitary hazard at this time. The two deficiencies in Applicant's proof relate solely to the susceptibility of the proposed wells to a significant risk of damage from flooding and other disasters and the location of the proposed wells relative to areas least subject to localized flooding. In all other respects, such as fire flow and security, Applicant has provided reasonable assurances that the applicable criteria would be satisfied or that the proposed work would have no bearing on the issue raised by Petitioners.
Recommendation It is RECOMMENDED that the Department of Professional Regulation enter a final order denying the application of Bocilla Utilities, Inc. for a public water supply construction permit. ENTERED on August 25, 1995, in Tallahassee, Florida. ROBERT E. MEALE 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 on August 25, 1995. APPENDIX Rulings on Respondents' Proposed Findings 1-4: adopted or adopted in substance. 5: rejected as irrelevant and repetitious. 6-7 (except last sentence): adopted or adopted in substance. (last sentence): rejected as unsupported by the appropriate weight of the evidence and legal argument. (except last sentence): rejected as subordinate, recitation of testimony, and irrelevant. 8 (last sentence): adopted or adopted in substance. 9: rejected as irrelevant. 10: adopted or adopted in substance, except to extent of legal argument as to effect of action of SWFWMD in granting variance. 11-12: rejected as irrelevant. 13 (except last sentence): adopted or adopted in substance. 13 (last sentence): rejected as irrelevant. 14-17 (except last sentence): adopted or adopted in substance. 17 (last sentence): rejected as legal argument. 18-21: adopted or adopted in substance. 22: rejected as unnecessary. 23: adopted or adopted in substance as to protection from only sanitary hazards. 24-26: adopted or adopted in substance as to description of aquifer, proposed well construction, and efficiency of RO filtration process, but not as reasons in support of Paragraph 23. 27 (first sentence): adopted or adopted in substance. 27 (remainder): rejected as unnecessary. 28: adopted or adopted in substance. 29: rejected as unnecessary. 30-31: adopted or adopted in substance. 32: rejected as irrelevant. 33-40: rejected as unsupported by the appropriate weight of the evidence. COPIES FURNISHED: Virginia B. Wetherell, Secretary Department of Environmental Protection Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Kenneth Plante, General Counsel Department of Environmental Protection Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Robert Starr P.O. Box 5337 Grove City, FL 34224 Betty Brenneman P.O. Box 67 Placida, FL 33946 Jim Duff P.O. Box 41 Placida, FL 33946 M. Christopher Bryant Oertel Hoffman P.O. Box 6507 Tallahassee, FL 32314-6507 Thomas I. Mayton, Jr. Assistant General Counsel Department of Environmental Protection 2600 Blair Stone Road Tallahassee, FL 32399-2440
The Issue The issues to be determined in this case are whether proposed Florida Administrative Code Rules 62-42.100, 62-42.200, 62-42.300, and a document incorporated by reference (“the Proposed Rules”) are invalid exercises of delegated legislative authority; whether the Department of Environmental Protection (“DEP”) complied with statutory requirements regarding preparation of a statement of estimated regulatory costs (“SERC”) for the Proposed Rules; and whether the approval by the Governing Board of the Suwannee River Water Management District (“SRWMD”) of a document entitled “Recovery Strategy: Lower Santa Fe River Basin” (“Recovery Strategy”) is invalid because it required rulemaking.
Findings Of Fact The Parties The Alliance is a Florida not-for-profit corporation with its principal place of business at 203 Northeast First Street, Gainesville, Florida. Its mission is to ensure the restoration, preservation, and protection for future generations of the ecosystems along the Ichetucknee River, including its associated springs. The Alliance has approximately 40 members. Seventeen members appeared at the final hearing and testified that they regularly use the Ichetucknee River and its associated priority springs for recreation, wildlife observation, and other purposes. Seventeen members is a substantial number of the total membership of the Alliance. Petitioner Still is a natural person who owns 117 acres of land in Bradford County. He uses the land primarily for timber production. He does not have a consumptive (water) use permit. He has used the Lower Santa Fe River and associated springs for recreation since 1979 and continues to visit the river and springs for this purpose. Petitioner FWF is a Florida not-for-profit corporation with its principal place of business at 2545 Blairstone Drive, Tallahassee, Florida. The mission of FWF includes the preservation, management, and improvement of Florida’s water resources and wildlife habitat. In the parties’ Pre-Hearing Stipulation, FWF identified Manley Fuller, its President, as its witness for organizational standing. It also listed “standing witnesses as needed,” but did not name them. At his deposition, Mr. Fuller stated that he did not know how many FWF members use the MFL water bodies. At the beginning of the final hearing, FWF made an oral proffer that it was prepared to call “10 members who are using the water bodies.” Later, FWF stated that some members were unwilling or unable to come to Tallahassee, but suggested that 10 or 15 might (now) be talked into coming to the final hearing or testifying by video. FWF also proffered a membership list, showing the number of members by county. It shows that FWF has a total of 11,788 members. In the six counties in the vicinity of the MFL water bodies (Alachua, Bradford, Columbia, Gilchrist, Suwannee, and Union) there are 457 FWF members. Ten, 15, or 20 members is not a substantial number of FWF’s 11,788 total members, nor is it a substantial number of its 457 members who live in the vicinity of the MFL waterbodies. Respondent DEP is a state agency with powers and duties under chapter 373, Florida Statutes, including the power and duty under section 373.042(1), which it shares with the water management districts, to establish minimum flows for surface watercourses and minimum levels for groundwater (“MFLs”) and recovery strategies when MFLs will not be achieved. Respondent/Intervenor SRWMD is a regional water management district with powers and duties under chapter 373, including powers and duties related to MFLs. The MFL waterbodies are located within SRWMD. Intervenor SJRWMD is the water management district adjacent to SRWMD. A portion of SJRWMD is included within the planning area created for the MFL waterbodies. Intervenor NFUCG is a regional trade organization representing interests of public water supply utilities in North Florida that hold consumptive use permits and are subject to the Proposed Rules. Intervenors CCUA and JEA are two members of NFUCG. Intervenors Alachua County, Gilchrist County, Suwannee County, Bradford County, and Columbia County are political subdivisions of the State in geographic proximity to the MFL water bodies. These Counties have the duty to plan for and protect the MFL water bodies as part of their local government comprehensive planning responsibilities under chapter 163, Florida Statutes. Minimum Flows and Recovery Strategies The water management districts and the DEP are required to establish minimum flows for surface water courses. § 373.042(1), Fla. Stat. Minimum flows are “the limit at which further withdrawals would be significantly harmful to the water resources or ecology of the area.” § 373.042(1)(a), Fla. Stat. If the existing flow in a water body is below its established minimum flow, DEP or the district is required to develop a “recovery strategy” designed to “[a]chieve recovery to the established minimum flow or level as soon as practicable.” § 373.0421(2), Fla. Stat. MFLs and recovery strategies are required to be included in a water management district’s regional water supply plan. § 373.709(2)(c) and (g), Fla. Stat. Water management districts must develop regional water supply plans in regions where they determine existing sources of water are not adequate to supply water for all existing and future users and to sustain water resources and related natural systems. § 373.709(1), Fla. Stat. SRWMD does not have a regional water supply plan. It is working on a draft plan that is expected to be completed in late 2015. The MFL Water Bodies The Lower Santa Fe River runs for approximately 30 miles from Santa Fe River Rise Spring to its confluence with the Suwannee River. The Lower Santa Fe is fed primarily by groundwater discharge from the Upper Floridan aquifer including the baseflow provided by several major springs. The Lower Santa Fe River system, including its tributary, the Ichetucknee River (below State Road 27), is classified as an Outstanding Florida Water, a designation conferred on waters “with exceptional recreational or ecological significance.” See Fla. Admin. Code R. 62-302.700(3). The Ichetucknee River runs for six miles from the Head Spring to its confluence with the Lower Santa Fe. Its flow is derived almost entirely from springflow. The ecological, recreational, and economic values of the Santa Fe and Ichetucknee Rivers are widely recognized. Both rivers flow through lands preserved for public use as part of the State Park System. SRWMD published a Water Supply Assessment in 2010 to determine whether water demands could be met for the 2010-2030 planning period without adversely affecting natural resources. The North Florida Groundwater Flow Model was used to evaluate groundwater withdrawals and their effect on aquifer levels and the flows in springs and rivers. The 2010 assessment concluded that groundwater levels of the Upper Floridan Aquifer in the eastern and northeastern portions of the District were in decline. The District’s analysis of river and streamflows also found declining trends. It was concluded that existing water sources would not be able to meet projected water demands over the planning period. As a result, the Lower Santa Fe River Basin (including the Ichetucknee River) was designated as a water supply planning region and SRWMD began to develop minimum flows for these water bodies. Because groundwater withdrawals within the adjacent SJRWMD were also affecting the MFL waterbodies1/, DEP, SRWMD, and SJRWMD entered into an interagency agreement in 2011 to work together on water supply issues and the development of a joint regional groundwater model. Development of the Minimum Flows The procedural difficulties faced in establishing minimum flows affected by water uses in two water management districts eventually lead to the Legislature’s creation of section 373.042(4) in 2013, which authorizes DEP to adopt relevant rules which can be applied by the water management districts without the need for their own rulemaking. In June 2013, SRWMD requested that DEP adopt minimum flows for the MFL waterbodies pursuant to the new law. A gage2/ for the Lower Santa Fe River near Fort White, and a gage for the Ichetucknee River on US 27 were selected for establishment of the respective minimum flows. The minimum flows were determined by first establishing a hydrologic baseline condition at the two gages. Then, SRWMD determined a departure from the baseline that would cause significant harm to the water resources and ecology of the area. The minimum flows are expressed as stage duration curves rather than a single number, in order to account for the changes in flow that occur naturally due to seasonal, climatic, and other factors affecting rainfall. Once the minimum flows were determined, SRWMD evaluated whether they are being met. It concluded that the minimum flows are not being met. Therefore, in accordance with section 373.0421(2), a recovery strategy had to be prepared and implemented. The Recovery Strategy A recovery strategy is a plan for achieving a return to adopted MFLs and will generally include plans for developing new water supplies and implementing conservation and efficiency measures. See § 373.0421(2), Fla. Stat. The practice of the water management districts has been to also adopt regulatory measures that are used in the review of consumptive use permits as part of a recovery strategy. See, e.g., Fla. Admin. Code R. 40D-80.074. That practice was followed for the MFL water bodies. The Recovery Strategy includes planning, water conservation, water supply development, and water resource development components. These components comprise the non-regulatory portion of the Recovery Strategy. Section 6.0 of the Recovery Strategy, entitled “Supplemental Regulatory Measures,” is the regulatory portion and is incorporated by reference in proposed rule 62-42.300(1)(d). The Recovery Strategy is to be implemented in two phases and the objectives of each phase are described in Table 4-1 of the Recovery Strategy. Phase I includes adoption of supplemental regulatory measures, work with user groups to implement water conservation measures, completion of an improved regional groundwater model, and identification and investigation of water supply projects. In Phase II of the Recovery Strategy, DEP plans to use the new regional model to develop long-term regulatory measures to address regional impacts to the MFLs water bodies. In addition, SRWMD and SJRWMD would develop and implement additional water resource and supply projects. The Proposed Rules The Proposed Rules would create three sections in a new chapter 62-42 of the Florida Administrative Code. Rules 62- and 62-42.200 set forth the scope and definitions: 62-42.100 Scope The purpose of this chapter is to set forth Department-adopted minimum flows and levels (MFLS) and the regulatory provisions of any required recovery or prevention strategy as provided in Section 373.042(4), F.S. The Department recognizes that recovery and prevention strategies may contain both regulatory and non-regulatory provisions. The non-regulatory provisions are not included in this rule, and will be included in the applicable regional water supply plans approved by the appropriate districts pursuant to Section 373.0421(2) and Section 373.709, F.S. [Rulemaking authority and law implemented omitted.] 62-42.200 Definitions When used in this chapter, the following words shall have the indicated meanings unless the rule indicates otherwise: Flow Duration Curve means a plot of magnitude of flow versus percent of time the magnitude of flow is equaled or exceeded. Flow Duration Frequency means the percentage of time that a given flow is equaled or exceeded. [Rulemaking authority and law implemented omitted.] Rule 62-42.300 is where the proposed minimum flows are set forth. The minimum flows for the Lower Santa Fe River are established in rule 62-42.300(1)(a); the minimum flows for the Ichetucknee River are established in rule 62-42.300(1)(b); and the minimum flows for 16 priority springs are established in rule 62-42.300(1)(c). The minimum flows for the Santa Fe and Ichetucknee Rivers are expressed as water flow in cubic feet per second (“cfs”) at various points on a flow duration curve. The minimum flows for ten named springs associated with the Santa Fe River and six named springs associated with the Ichetucknee River are set forth as a “percent reduction from the median baseline flow contribution of the spring to the flow” at a particular river gage. This approach, which ties spring flow to river flow, was used by DEP because there is minimal flow data for the springs. Rule 62-42.300(1)(d) adopts by reference “Supplemental Regulatory Measures,” which is Section 6.0 of the Recovery Strategy. Rule 62-42.300(1)(e) states that DEP, in coordination with SRWMD and SJRWMD, shall reevaluate these minimum flows after completion of the North Florida Southeast Georgia Regional Groundwater Flow Model, which is currently under development. The rule also states that DEP will “strike” rules 62-42.300(1)(a) through (d) and adopt new rules no later than three years after completion of the final peer review report regarding the new groundwater model, or by December 31, 2019, whichever date is earlier. The Supplemental Regulatory Measures adopted by reference in rule 62-42.300(1)(d) are intended to provide additional criteria for review of consumptive use permit applications during Phase I. These measures would be applied to water uses within the North Florida Regional Water Supply Planning Area. For the purposes of the issues raised in these consolidated cases, it is necessary to discuss three categories of permit applications and how they would be treated under the Supplemental Regulatory Measures in Phase I: (1) A new permit application that shows a “potential impact” to the MFL water bodies must eliminate or offset the potential impact; (2) An application to renew a permit, which does not seek to increase the amount of water used, would be renewed for five years no matter what impact it is having on the MFL water bodies; however, if the impact is eliminated or offset, the renewal would not be limited to five years; and (3) An application to renew a permit which seeks an increased quantity of water would have to eliminate or offset the potential impact to the MFL water bodies associated only with the increase. This category of permits is limited to a five-year renewal unless the existing impacts are also eliminated or offset. See § 6.5(a)-(d) of the Recovery Strategy. Section 6.5(e) states that existing permits that do not expire during Phase I are considered consistent with the Recovery Strategy and are not subject to modification during the term of their permits. Many permits are issued for a 20-year period, so Phase I would not capture all existing permits because they would not all expire during Phase I.3/ DEP stated that existing permits may be affected by the regulatory measures DEP plans to adopt for Phase II. Section 6.5(f) of the Supplemental Regulatory Measures states that permittees are not responsible for impacts to the MFL water bodies caused by water users in Georgia, or for more than the permittee’s “proportionate share of impacts.” The record evidence established that the effect of Georgia water users on the MFL water bodies is small. Section 6.6(b) requires permits for agricultural use in the counties surrounding the MFL water bodies to include a condition requiring participation in the Mobile Irrigation Lab (MIL) program. The purpose of SRWMD’s MIL program is to improve the efficiency of irrigation systems. SRWMD provides cost- sharing in this program. Whether DEP Must Adopt the Entire Recovery Strategy by Rule Petitioners contend that proposed rules 62-42.100(1) and (2) enlarge, modify, or contravene sections 373.042(4) and 373.0421(2) because these statutes require DEP to adopt all of a recovery strategy by rule, not just the regulatory portion of a recovery strategy. Respondents contend that it was consistent with the law for DEP to adopt only the regulatory portion of the Recovery Strategy by rule and have SRWMD approve the non- regulatory portion and implement it through a regional water supply plan. It has been the practice of the water management districts to adopt by rule only the regulatory portion of a recovery strategy and to implement the non-regulatory portion as a component of their regional water supply plans. This is primarily a legal issue and is addressed in the Conclusions of Law where it is concluded that DEP is not required to adopt the entire Recovery Strategy by rule. Whether SRWMD Must Adopt the Recovery Strategy By Rule Petitioner Still challenged SRWMD’s approval of the Recovery Strategy as violating the rulemaking requirements of section 120.54. However, Petitioner Still presented no evidence in support of his claim that the Recovery Strategy contains statements that meet the definition of a rule, but were not adopted as rules. Whether the Non-Regulatory Portion of the Recovery Strategy Will Prevent Recovery The Alliance claims that there are flaws in the non- regulatory portion of the Recovery Strategy that was approved by SRWMD, primarily related to the estimate of flow deficits in the MFL water bodies and the corresponding amount of water that must be returned to the system to achieve the minimum flows. There is unrefuted record evidence indicating that SRWMD did not account for consumptive use permits issued in the last three or four years. Therefore, the Recovery Strategy probably underestimates the flow deficits in the Lower Santa Fe and Ichetucknee Rivers and the amount of water needed to achieve the minimum flows.4/ However, as explained in the Conclusions of Law, the Alliance cannot challenge the non-regulatory portion of the Recovery Strategy in this proceeding. The Recovery Strategy, including the non-regulatory portion approved by SRWMD, is in Phase I. SRWMD can revise the Recovery Strategy at any time, and in Phase II can do so with the improved analysis made possible with the new regional model. As explained in the Conclusions of Law, the non-regulatory portion does not have to achieve recovery in Phase I. Whether the Minimum Flows are Based on the Best Information Available Petitioner Still contends that the minimum flows are not based on the best information available as required by section 373.042(1)(b). He claims that the wrong method was used to estimate streamflow, the modeling was based on a false assumption about the relationship between groundwater levels and river flows, the relationship between withdrawals and flows was not properly accounted for, withdrawals and other anthropogenic impacts were not properly distinguished, tailwater effects were not properly accounted for, and the wrong period of record was used. Petitioner Still’s arguments in this respect are based largely on his own opinions about the quality and significance of the technical data that was used and how it affects the modeling results used in establishing the minimum flows. Petitioner Still does not have the requisite expertise to express these opinions and he did not get expert witnesses at the final hearing to agree with his claims. Petitioner Still does not have an expertise in modeling to express an opinion about the ability of the model to use particular data or how the model accounts for various surface and groundwater phenomena. Petitioner Still failed to prove that the minimum flows are not based on the best available information. Whether the Proposed Rules Are Vague Petitioner Still contends the Proposed Rules are invalid because they use terms that are vague. Some of the terms which Petitioner Still objects to are the same or similar to terms commonly used in other environmental regulations, such as “best available information,” “impact,” “offset,” and “eliminate.” The term “potential impact” is not materially different than the term “impact.” The term “best available modeling tools” is not vague. It reflects the recognition that, like best available information, hydrologic models and technical information are continually being created and updated. Petitioner Still contends that the definitions of “Flow Duration Curve” and “Flow Duration Frequency” in proposed rules 62-42.200(1) and (2), respectively, are vague because they do not state whether “synthetic” data may be used in the production of the flow duration curve, or that they are based on a specific period of record. Synthetic data are numeric inputs used to account for missing data and are created by extrapolating from existing data. As an example, they can be used to satisfy a model’s need to have a water flow entry for every month in a multi-year period being analyzed when there is no actual data available for some of the months. The use of synthetic data is a regular and accepted practice in modeling and does not have to be mentioned in the rule. Flow duration curves and flow duration frequencies are calculated from data covering specific periods of record. Although the definitions of these two terms in proposed rule 62-42.200 could contain more information than is provided, the proposed definitions are not inaccurate. They are not vague. Petitioner Still contends that proposed rule 62-42.300(1)(a) is vague because it establishes the minimum flows for the Santa Fe River at a location without precisely identifying the location. The record shows that the reference in proposed rule 62-42.300(1)(a) to “the Santa Fe River near Ft. White, FL” is the actual name of the United States Geological Survey flow gage that has been in use for many years. Furthermore, proposed rule 62-42.300(1)(c), which establishes the minimum flows for the priority springs, refers to “the respective river gages listed in paragraphs 62-42.300(1)(a) and (b).” Therefore, it is made clear that the reference to “the Santa Fe River near Ft. White, FL” in proposed rule 62-42.300(1)(a) is a reference to a river gage. The rule is not vague. Petitioner Still asserts that the minimum flows in proposed 62-42.300(1) are vague because they do not identify the period of record that was used in deriving the flow duration curves which are used in the rule. He compared the wording in the proposed rule to SRWMD’s existing rule 40B-8.061(1), which identifies the technical report from which the flow duration curve in that rule was derived. A general description of flow duration curves is found in “Minimum Flows and Levels for the Lower Santa Fe and Ichetucknee River and Priority Springs” dated November 22, 2013 (“MFL Technical Document”), at page 3-6: They show the percent of time specified discharges were equaled or exceeded for a continuous record in a given period. For example, during the period 1932 to 2010, the daily mean flow of the Santa Fe River near Fort White (Figure 3-2) was at least 767 cfs, 90 percent of the time. The curves are influenced by the period of record used in their creation, but for comparison purposes between different scenarios over a fixed time period they are extremely useful. [Emphasis added.] However, proposed rule 62-42.300(1) does not give the period of record for the flow duration curves that will be used to determine compliance with the minimum flows for the Lower Santa Fe and Ichetucknee Rivers. Respondents argued that identifying the period of record is unnecessary because anyone interested in knowing the period of record or anything else pertaining to how the flow duration curves were produced could refer to the MFL Technical Document. This is not a situation where a specific number and unit, such as 100 cfs, has been established as a criterion based on technical analyses that can be found in documents. In such a case, the technical documents are not needed to determine compliance with the criterion; they simply explain why the criterion was selected. In the case of a flow duration curve, however, the period of record for the data to be used must be known to determine compliance. For example, proposed rule 62-42.300(1)(a)1. would establish the following criterion: “3,101 cubic feet per second (cfs) for a flow duration frequency of five percent.” Five percent of what? Five percent of what data set? Data from what time period? Must the same synthetic data be used? The rule does not inform persons subject to the rule what data SRWMD will use to determine compliance. They would not know how to calculate flow duration frequencies without reviewing the MFL Technical Document. Because the minimum flows are not completely identified in the rule, they are vague. Whether a Minimum Flow Should be Established for Each Priority Spring Petitioner Still contends that the Proposed Rules are invalid because minimum flows are not established for each priority spring, which causes them to be unprotected. He claims that each spring needs its own minimum flow “that takes into account the surface and ground water inputs to its flow.” DEP and SRWMD presented evidence that establishing minimum flows for each spring was impracticable because there were insufficient data for the springs. Petitioner Still did not refute this evidence. Whether the Proposed Rules Allow Further Degradation of the MFL Water Bodies The Alliance contends that the Proposed Rules must reduce permitted withdrawals in Phase I and must require monitoring of water use by agricultural water users, but it did not present evidence that these alternative regulatory measures are practicable in SRWMD in Phase I. The Alliance did not show there are permitting mechanisms that have been used by other water management districts as part of the first phase of a recovery strategy that are practicable for use in SRWMD and would be more effective. The only evidence presented on the subject of what regulatory measures other water management districts have adopted as part of a recovery strategy pertained to the Southwest Florida Water Management District (“SWFWMD”). That evidence showed that SWFWMD took a similar approach of allowing existing permitted uses to continue their water withdrawals while new water supplies and conservation mechanisms were developed. The Alliance contends that the Supplemental Regulatory Measures do not prevent further degradation because there are projected to be numerous, new agricultural water uses in Phase I. However, under section 6.5(b), new water uses will not be allowed to adversely impact the MFL water bodies. The Alliance makes a similar argument regarding existing agricultural water users who will request an increase in water. Under section 6.5(c), increases in water use will not be allowed to adversely impact the MFL water bodies. Whether the SERC and Revised SERC are Good Faith Estimates and Whether the Proposed Rules Impose the Lowest Cost Regulatory Alternatives Petitioner Still failed to meet his burden under section 120.56(2) of going forward with evidence to support his allegations that DEP’s original SERC or the revised SERC were not good faith estimates of regulatory costs associated with the Proposed Rules. The record evidence shows they are good faith estimates. He also failed to meet his burden under section 120.56(2) of going forward with evidence to support his allegations that the objectives of the law being implemented could be substantially accomplished by a less costly regulatory alternative.
Findings Of Fact Upon a consideration of the oral and documentary evidence adduced at the hearing in this cause, the following pertinent facts are found: 1/ By application number 25793, the applicant seeks a permit to construct and operate a proposed surface water management system to serve a 2,541 acre project within the St. Johns River Basin in Indian River County. The proposed system will consist of a perimeter dike, a central canal with interior laterals and four discharge pumps. The applicant will be discharging into the St. Johns Marsh and seeks a discharge capacity of 139,000 GPM. Three of the discharge pumps are to be located at the southeast corner of the property and a two-way 25,000 GPM pump is to be located at the intersection of the central canal and the western boundary of the property. By application number 25794, the applicant seeks a permit for the use of surface and artesian water for the irrigation of the same 2,541 acres of pasture and truck crops. The applicant requests to withdraw surface water from the St. Johns Marsh by means of a two-way 25,000 GPM pump located at the intersection of the central canal and the western property boundary and to withdraw water from the Floridan aquifer by means of eight eight-inch artesian wells. The amount requested is 5,294 acre-feet per year with a maximum monthly pumpage of 1.47 billion gallons. A staff report of the Central and Southern Florida Flood Control District (FCD) concluded that the major problem with the permit applications is the impact on water quality of the receiving bodies of water and that nutrients and other pollutants will be introduced into runoff waters discharged into the St. Johns Marsh, which is the source of the public water supply for South Brevard County. The staff therefore recommended that the applicant institute a water quality and quantity monitoring program to monitor discharges to the Marsh. The staff further recommended that the applicant not be allowed to discharge from the western property boundary nor irrigate from the ditch on the western property boundary. It was recommended that the two-way 25,000 GPM pump be installed adjacent to the other pumps located at the southeast corner of the property. More specifically, the staff found that if a permit were to be issued pursuant to application number 25793, it should be subject to the conditions that: the allowable discharge capacity to be 104,000 GPM, with discharges to be east to the St. Johns Marsh by means of one 44,000 GPM pump, one 35,000 GPM pump and one 25,000 PM two-way pump to be located at the southeast corner of the property; the applicant notify the FCD prior to any excavation of materials from land lying east of the east property boundary and, if such excavation is done, a discontinuous borrow ditch be created by either leaving 25 foot portions of undisturbed marsh or by placing 25 foot earthen plugs at approximately 500 foot intervals (this was later modified at the hearing to 1,000 foot intervals); and the applicant submit monthly reports of total daily discharges and water quality, the samples to be taken at the southeast corner of the property. With regard to application number 25794, the staff recommended that if such permit were to be issued, it be subject to the following conditions: for the use of surface water, an annual allocation of 2329.3 acre- feet per year and for the use of artesian water, an annual allocation of 2518.5 acre-feet per year, with a maximum monthly pumpage from all sources of 355.3 million gallons; no withdrawal of surface water from the St. Johns Marsh when the water level in Blue Cypress Lake drops to 22.0' msl.; surface water to be withdrawn by means of a 25,000 GPM two-way pump located at the property's southeast corner; artesian waters to be withdrawn by eight eight-inch wells with effective and operative controls placed thereon and analyses of water samples from the water discharge of each the submission of monthly reports of total monthly pumpages and total monthly flows; and permit for the withdrawal of surface and artesian water to expire on January 15, 1979. At the hearing, the applicant agreed to the recommended conditions placed upon the permits by the staff report with the exception of: the amount of the allowable discharge (staff recommending 104,000 GPM as opposed to a desired 139,000 GPM); the location of the 25,000 GPM two-way pump (staff recommending southeast corner as opposed to a proposed site on the western boundary of the property); the expiration date of January 15, 1979. The Environmental Protection Bureau of the Florida Game and Fresh Water Commission requested the FCD to delay issuance of permits for all projects in the Upper St. Johns River basin until a comprehensive water management plan for the area is formulated. Read into the record was a resolution adopted by the Commission on May 16, 1975, recommending that "the further destruction of the marsh be curtailed and a plan be formulated for the return of the diverted waters as a management tool for restoration of fish and wildlife resources." On behalf of the Florida Audubon Society, Mr. Charles Lee contended that, because of this resolution and request of the Game and Fresh Water Fish Commission and that agency's constitutional status, the FCD is precluded from issuing the subject permits. Intervenors and members of the general public who were opposed to the issuance of the instant permits expressed the following concerns: the low water quality and quantity of the St. Johns River and its marshes; the decline in hunting and fishing because of agricultural activities in the St. Johns River valley; the loss of marsh land due to agricultural activity; the lack of a basic water management program for the area; the lack of remedial measures should degradation of the water occur; and the lack of an expiration date for the surface water management system permit.
Recommendation Based upon the findings of fact and conclusions of law recited above, it is the recommendation of the hearing officer that application numbers 25793 and 25794 be granted, subject to those special conditions set forth in the Staff Report as modified by the following: In paragraph number 3 on page 14 of the Staff Report, substitute the words "1,000 foot intervals" for "500 foot intervals;" Add as paragraphs 6 on page 15, paragraph 6 on page 16 and paragraph 7 on page 18 the following: "Should the data in the monthly reports submitted by the applicant indicate the occurrence of a degradation of the waters utilized, the applicant will be required to remedy the situation causing the de- gradation." Add as paragraph 7 on page 15 the following: "7. This permit shall expire on January 15, 1979." Respectfully submitted and entered this 25th of March, 1976, in Tallahassee, Florida. DIANE D. TREMOR Hearing Officer Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304
Findings Of Fact Ed Smith is the President of Riverside Village Mobile Home Park, Inc., which in turn is the owner of the mobile home park in question in this case. The mobile home park is located in Ruskin, Hillsborough County, Florida. Petitioner was served with an Administrative Complaint alleging that the chlorine residual in the park water supply distribution system was inadequate and that this constituted a violation of Chapter 513 and Section 386.041(1)(f), Florida Statutes, as well as Rule 10D-26.67(1), Florida Administrative Code. Specifically, the Administrative Complaint alleges violations occurring between July 16, 1986 and July 29, 1986, and seeks the imposition of a civil penalty in the amount of $500 per day which "shall be calculated when this complaint is received by the (Petitioner), and will run until the violation has been corrected." Petitioner requested a hearing to contest these allegations, and his request was filed with Respondent's Clerk on October 8, 1986. It was not established by competent substantial evidence when Petitioner "received" the Administrative Complaint which is the subject of this action. The only evidence of any violation occurring between July 16 and July 29, 1986 was the testimony of Harry Messick who signed an Official Notice and Notice of Intended Action which were both dated July 16, 1986, and which alleged that "chlorine reading found at time of inspection (was) between 0.1 ppm and (a) trace." However, Messick did not perform any test to either produce or confirm this result. He testified that someone else performed the field test, but there was no testimony from anyone else who may have actually conducted a test on Petitioner's water supply system on July 16, 1986. Therefore, it has not been established by competent substantial evidence that Petitioner's water supply system on July 16, 1986, was in violation of the requirement that .2 mg/1 of free chlorine residual be maintained. Testimony from Respondent's other witnesses, Norman Vik and Neil R. Schobert, indicates Vik was not even at Petitioner's mobile home park between July 16 and 29, 1986, and the only test conducted by Schobert found that Petitioner's water supply system was in compliance on July 24, 1986. Design modifications in Petitioner's water supply distribution system were approved by the Hillsborough County Health Department on July 9, 1986.
Recommendation Based on the foregoing, it is recommended that Respondent enter a Final Order DISMISSING the Administrative Complaint filed against Petitioner. DONE AND ENTERED this 19th day of February 1987 in Tallahassee, Florida. DONALD D. CONN Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 19th day of February 1987. APPENDIX (DOAH Case No. 86-4094) Rulings on Respondent's Proposed Findings of Fact: 1. Adopted in Finding of Fact 1. 2-3. Rejected in Findings of Fact 4, 5. COPIES FURNISHED: James A. Sheehan, Esquire Florida Federal Building One Fourth Street North Suite 800 St. Petersburg, Florida 33701 Carol M. Dittmar, Esquire 4000 West Buffalo Avenue Suite 520 Tampa, Florida 33614 Gregory L. Coler Secretary Department of Health and Rehabilitative Services 1323 Winewood Blvd. Tallahassee, Florida 32301 John Miller, Esquire General Counsel Department of Health and Rehabilitative Services 1323 Winewood Blvd. Tallahassee, Florida 32301 =================================================================
Findings Of Fact At all times pertinent to the issues herein, the Southwest Florida Water Management District had permitting authority for the issuance of consumptive use permits in the area in which Respondent, El Jobean, proposes to sink its irrigation well. On December 12, 1988, El Jobean submitted a consumptive use permit application to sink a new well for the purpose of irrigation of a golf course to be developed on the property it owns in Sarasota County. The well is to be located in the NE 1/4 of the NE 1/4 of Section 32, Township 365, Range 20R, in Sarasota County, Florida near the southern boundary of an irregularly shaped piece of property consisting of approximately 855 acres, owned by the applicant, which extends over Sections 28, 29, 32 and 33, Township 365, Range 20E. Respondent proposed to sink a 10 inch diameter well to a total depth of approximately 900 feet with casing in the well now to extend down to 300 feet, with a pump capacity of 1,000 GPM. The golf course to be irrigated is to encompass approximately 190 acres. The applicant requested authority to withdraw an average of 600,000 GPD with a limitation of a maximum of 1,440,000 GPD. The application was properly staffed by the District. In the staff report on the application, the average daily use limitation was expanded to 707,000 GPD; consumptive use was raised from 0 to 139,000 GPD; and maximum daily consumption was reduced from 1,440,000 GPD to 1,240,000 GPD. These changes were due to correction of arithmetic errors in the application and were accepted by the applicant. The ultimate recommendation of the staff was for approval of a 6 year permit, subject to certain conditions outlined in subparagraph I of the staff report. These special conditions require the provision and use of flow measuring devices to maintain an accurate record of the water withdrawn; the maintenance of flow records and the providing of periodic reports to the District; the collection and analyzing of water quality of samples taken from the well to measure the appropriate parameters for chlorides, sulfates, and total dissolved solids; the reporting of the results of these samplings and a description of the sampling and analytical methodologies employed; and a requirement that the permittee investigate the feasibility of supplementing and/or substituting drawn water with treated sewage affluent. After the staff report was submitted, proper notice of the District's intent to issue the permit was published. Based on that notice, protests were filed both by Miakka and Mr. Bishop. The area in question is located within the Manasota Basin which, itself, is located within the Southern West-Central Florida Ground Water Basin, (SWCFGWB), which encompasses all of Pasco, Hillsborough, Manatee, Sarasota, Polk, Hardee, and DeSoto Counties, and parts of Lee, Glades, Charlotte and Highlands Counties. The SWCFGWB sits atop several aquifers which include the Floridian Aquifer, two Intermediate aquifers, and the Surficial Aquifer. The Floridian Aquifer is the deepest and the Surficial Aquifer is on the top. The Miakka Community Club is a Florida corporation made up of residents of the pertinent area whose primary function is to preserve and conserve the rural nature and spirit of the Northeast section of Sarasota County. The club performs this function through educational programs, community activities, and participation in the legislative process. Miakka urges denial of the permit sought by El Jobean based on its membership's belief that the property owners whose property is in the immediate vicinity of the proposed well will be adversely affected if El Jobean is permitted to sink its well and withdraw water from it. The club membership believes that approval of El Jobean's well will result in contamination of existing personal water wells due to excessive use by El Jobean; potential contamination of Sarasota County's future drinking water sources which include the capital Ringling,/MacArthur tract and the Myakka River; reduction of property values; and destruction of personal resources. Petitioner also urges that since the proposed golf course will be a part of a private club for the use of members only, in which membership will be limited, there is no public benefit derived from the approval of and sinking of the well in question. Petitioner also contends that during the periods of severe water shortage as are being currently experienced, permission to sink a well of this size to draw water in of the magnitude expressed in the application, would be counterproductive and detrimental to the interests of the other property owners in the area. In support of its claim, Petitioner presented the testimony of two homeowners from the area, Mr. Richardson and Ms. Mustico. Mr. Richardson, whose well is 183 feet deep, has had several problems with his well even without the instant drilling. In 1974, and subsequent thereto, he has had to go deeper with a suction pipe because the water has dropped below the level of the tail pipe. Ms. Mustico's 160 foot deep well, with 80 feet of casing, is used to supply water for the home. She also has other wells for watering her lawn and for livestock, one of which goes down 500 feet. She is concerned that the well proposed by El Jobean will adversely impact her ability to draw water from her wells because, she believes, the water level from which her water is drawn will drop. In the past, her primary well has gone dry and the wells of several neighbors have gone dry as well. Through maps and other documentation taken from the Ground Water Resource Availability Inventory for Sarasota County, Florida, prepared by the District in March 1988, Petitioner has established that areas of significant groundwater withdrawal within the SWCFGWB occur in Hillsborough, Manatee, Polk, Hardee, DeSoto and Highlands Counties. With the exception of an extremely small portion of Sarasota County located contiguous to Manatee County, there appear to be no areas of major ground water withdrawal currently existing in Sarasota County. The majority of the major municipal well fields within the pertinent basin that are located within Sarasota County, extend down to the Intermediate and Surficial Aquifers with only 3 extending through the lower Intermediate into the Floridan Aquifer. These include the Verna well field located in the northeast corner of Sarasota County where it abuts Manatee County; the Sarasota County well field located in northwest Sarasota County near the Manatee County line; and the Sorrento Utility, Inc., well field which is located near the Gulf Coast, approximately two-fifths of the way down between the Manatee and Charlotte County lines. With the exception of the Verna well field, all the municipal well fields in Sarasota County appear to be reverse osmosis systems and as of 1987, there were 28 reverse osmosis systems located within Sarasota County. Most are relatively small in their output measured in millions of gallons per day. With the exception of 3 public supply wells, 2 of which are permitted an average annual pumpage greater than 100,000 GPD and 1 of which is permitted less, all of the permitted public supply well fields in Sarasota County are located west and south of 1-75 as it extends from the Manatee County line in the north to the Charlotte County line in the south. The El Jobean well would be located east of the line, in that area occupied by the 3 public supply wells. Generalized recharge areas for the upper Floridan Aquifer in the groundwater basin in issue here have been categorized from "high", with a rate of more than 10 inches per year, to "Generally none", with a recharge rate at 0. In 1980, the high recharge rates existed in the north-central part of Pasco, the eastern part of Polk County, and the northeastern part of Highlands County. Sarasota County is in an area wherein the recharge rate was either very low or generally none. In September 1986, the high recharge rate was found in a very small area of northeastern Pasco County, and small areas in both Polk and Highlands Counties. Sarasota County, for the most part, was classified as having no recharge. In May 1987, the high recharge rates were, again, a small area in eastern Pasco County, a small area in northeastern Hillsborough County, a small area in southeastern Polk and northwestern Highlands Counties, and a minuscule area in central Pinellas County. Again, Sarasota County had a recharge rate of 0. Generalized estimated, calibrated, model-derived recharge and discharge values for the upper Floridan Aquifer in the ground water basin in issue here, as they pertain to Sarasota County, reflect positive 2 recharge to negative 1 discharge inches per year. Historically, however, the northeast portion of Sarasota County, where the El Jobean well in question would be located, evaluated by various individuals or agencies periodically from 1980 through 1988, reflects a recharge of anywhere from 0 to 2 inches per year. None of this documentation was supplemented, however, by direct testimony by an individual knowledgeable in this area, and Petitioner's main thrust appears to be an unsubstantiated fear that the sinking of El Jobean's well will have a negative impact on its membership's wells. Admittedly, the residents in the area in question all rely on private wells for the majority of their water supply, other than through the catchment of rainwater, which is insignificant. It was also established that the area has been undergoing a severe water shortage and that conservation measures have been mandated. On the other hand, El Jobean presented the testimony of a hydrogeologist, Mr. Moresi, who has extensive experience with the modeling process used to determine water consumption and recharge in southwest Florida and Sarasota County. The aquifer system in Florida is made up of water bearing limestone layers below the surficial sand base. This aquifer system underlays the various zones throughout the state and reflects a surficial aquifer extending from ground level down approximately 70 feet to a confining bed which separates it from the lower strata. This top confining bed is approximately 20 feet thick, and below it is the Tamiami-Upper Hawthorn Aquifer, which is between 100 and 200 feet deep and which rests on another confining bed somewhat thicker than the upper one. Below the second confining bed is the Lower Hawthorn-Upper Tampa Aquifer which extends approximately from the 250 foot to the 450 foot level at the Manatee County line, and between the 320 foot and the 710 foot level at the Charlotte County line. Another confining bed lays between this aquifer and the Floridan Aquifer which starts at the 500 foot level and goes down well below the 900 foot level in the north and extends from the 730 foot level down in the south. The confining bed below the surficial aquifer is made up of a clay material which retards the movement of water from one aquifer to another. The surficial aquifer is porous and saturated with water from the water table down. Since the confining beds are far less porous than the aquifers they separate, water moves much more slowly through them. The lower aquifers are made up of limestone and are also porous and contain water. The Tamiami-Upper Hawthorn formation consists of limestone and clay, but is water bearing. The Lower Hawthorn-Upper Tampa formation is similar and both make up the intermediate aquifer below which is the lower confining bed followed by the Floridan aquifer. Respondent's well would be cased in steel down to an area approximately 100 feet into the Floridan Aquifer, through the Lower Hawthorn- Upper Tampa Aquifer and through the lower confining bed. Since the well would be cased to well below the lower confining bed, water existing in the upper aquifers, would be prevented from being drawn down by operation, of the Respondent's well either directly or by settling down to replace the water drawn out. Generally, the deeper a well is drilled, the worse the quality of the water, and it becomes less potable. The Floridan Aquifer produces far more copious quantities of water than do the intermediate aquifers. However, since it is cheaper to drill to the intermediate zones as the wells need not be so deep, and since the water there is better, most domestic wells go no deeper than these aquifers. They go down approximately 150 to 180 feet. The pressure in each level is separate from and different from that in the other aquifers. The upper intermediate system generally has a lower pressure than the lower intermediate system. As a result, water from the lower intermediate system tends to leak upward toward the upper intermediate aquifer, rather than the reverse. In addition, a recent survey tends to show that the Floridan aquifer also tends to leak upward into the lower intermediate level. It also shows that leakage through the confining beds amounts to .002 GPD per cubic foot of aquifer. Petitioner claims that since the lower water is of lesser quality, and since withdrawal of water from the upper layers would promote leakage upward, thereby adding lower grade water to the better grade upper water, there could be a diminishment in upper level water quality as a result of water being drawn from the upper levels. However, according to Mr. Moresi, the .002 figure is so small it would result in an infinitesimally small drawdown of water level from the upper intermediate level aquifer and the potential for compromise of the water quality therein is remote. Clearly, this is not the result of drawing water from the Floridan Aquifer as the well in question would do but more the result of the residential wells extending into the upper levels. The District ran a model for the proposed El Jobean well (a Jacob- Hantush model) which showed that drawdown at the wellhead would be just over 2 feet. This means that use of the Respondent's well would reduce the water level in the Floridan Aquifer at the well head by 2 feet. However, this drawdown is shown to decrease rapidly out to where, at distance, it is almost immeasurable. In fact, drawdown of the Floridan Aquifer at 24,000 feet from the well head (approximately 4.5 miles) would be .1 feet, slightly or 1 inch. The .1 foot drawdown relates to the lowest (Floridan) aquifer and the resultant drawdown in the upper intermediate aquifer, into which the majority of residential wells are sunk, would be relatively undetectable. Since the Petitioner's wells, at their deepest, go only into the upper intermediate level, and would be separated by 2 confining beds from the Floridan Aquifer, the impact on the domestic wells at 2 miles from the El Jobean wellhead would be immeasurable. Even at 1 mile, there would be minimal drawdown in the Floridan Aquifer and almost none in the upper intermediate aquifer. The potentiometric surface of the intermediate layer would not be adversely affected, nor would that of the surface water. Recognizing the potential for saltwater intrusion which occurs all along the coast, based on his studies, Mr. Moresi concluded that the well in question here would not induce significant saltwater intrusion. He concluded as well that the permit is consistent with the requirements of the District rule; that the amount permitted for the use of irrigation of the golf course is reasonable, assuming a golf course is a reasonable and appropriate use of water; that the withdrawal by the well in issue would not have an adverse impact on users outside the property on which the well was located; that it would not impact existing users; that there is no other water available for the purpose intended; that the water taken from the Floridan Aquifer under this permit may be potable but is of poor quality; and that the applicant met rule standards. Mr. Moresi also discussed the possible cumulative impact of the proposed well when operated along with the currently existing wells. If there are other drawdowns from the same cone into which El Jobean's well would be sunk, the withdrawals would be cumulative. However, as best he can determine, the only other significant drawdown from the cone pertinent here is that of the Verna well field. In his opinion, that well field's drawdown, which is from the northeast, would not be significant even when considered with the El Jobean well. Mr. Moresi was also satisfied that while the confining bed separating the surficial aquifer from the next lower level might be disturbed, the deeper one goes, the less likely there is to be mixing of aquifers. The only instance where water could move from one level to another as a result of the well is where there is no casing on the bore hole. In the instant case, plans call for, and permit conditions require, the well to be cased to below the lowest confining bed. Consequently, there should be no upward or downward flow of water as a result of the bore. Mr. Tyson, who worked on the evaluation of El Jobean's application for permit, was of the opinion that the amount of water requested by El Jobean in its application was appropriate for a golf course. This does not mean that a golf course is an appropriate use of the property. The special conditions imposed on the granting of the permit by the District are designed to reduce any impact possibly caused by the permitted activity. The Jacob-Hantush model used in analysis of the instant application is considered to be a conservative tool and showed minimal drawdown at all property boundaries. The use of other models in this case was considered neither necessary nor appropriate. Mr. Tyson considers the proposed permit a reasonable beneficial use as defined in the Florida Administrative Code and statutes because it proposes use of reasonable amounts of water and the models indicate no unfavorable impact. Based on the past practice of permitting golf courses with subdivisions, he feels the proposed use is reasonable. He concludes, therefore, that it is in the public interest to grant this permit. In his opinion, the permit will not interfere with legal existing uses and meets all statute and rule requirements. Considering the evidence as a whole, it is found that petitioner has presented insufficient evidence to support its claim that approval and operation of El Jobean's well as proposed would have an adverse impact on the property owners. It's concerns are no doubt sincere, but these concerns are not sufficiently confirmed by evidence of record. At the hearing, the parties stipulated that if the permit were granted, it would be modified by the addition of two conditions: The proposed well shall be constructed with a minimum of 600 feet of casing so as to prevent the unauthorized interchange of water between water bearing zones in order to prevent the deterioration of water quality in the shallower zones. If the well cannot be properly completed to prevent such an unauthorized interchange of water, the well shall be abandoned and plugged in accordance with Rule 17-21.10(2)(c), F.A.C.. Upon completion of the well, a copy of the well construction completion report shall be sent to the District. The permittee shall line the bottom of the pond that will be used as the irrigation source, with clay to a thickness equal to 1.5 feet.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that the Southwest Florida Water Management District enter a Final Order issuing Consumptive Use Permit Number 209458, as modified by the conditions stipulated to at the hearing held herein on June 7, 1989, and outlined in Finding of Fact Number 27 herein, to El Jobean Philharmonic Group, Inc. RECOMMENDED this 9th day of August, 1989 at Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of Division of Administrative Hearings this 9th day of August, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 88-1176 The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. For the Petitioner: Not a Finding of Fact but a statement of the ultimate issue of fact. Accepted and incorporated herein. 3-6. Accepted and incorporated herein. 7-12. Accepted and incorporated herein. Accepted as indicating original conditions. The parties stipulated to additional conditions at the hearing. Accepted. 15 & 16. Accepted and incorporated herein. 17-33. Accepted and incorporated herein as pertinent. 34 & 35. Accepted. 36 & 37. Accepted. 38 & 39. Redundant. 40-43. Accepted. 44. Accepted. 45-51. Accepted. 52 & 53. Accepted. 54-56. Accepted. 57 & 58. Accepted and incorporated herein. 59-66. Accepted. 67-75. Accepted and incorporated herein. 76 & 77. Accepted and incorporated herein. 78. Accepted. 79-84. Accepted. Accepted and incorporated herein. Rejected. 87 & 88. Accepted. 89-93. Accepted and incorporated herein. Accepted. Accepted in the natural source sense suggested by Petitioner. 96-99. Accepted and incorporated herein. 100 & 101. Accepted and incorporated herein. 102-105. Accepted and incorporated herein. 106. Accepted. 107 & 108. Accepted. 109 & 110. Accepted. For the Respondents: 1 & 2. Stipulation between the parties accepted and incorporated herein. 3-6. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence except for the second sentence which is incorporated herein as a Finding of Fact. Not a Finding of Fact but a comment on the evidence. 9-11. Accepted and incorporated herein. 12. Accepted. 13-16. Accepted and incorporated herein. 17. Accepted and incorporated herein. 18 & 19. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. 22-26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29. Accepted. 30-32. Accepted and incorporated herein. 33-40. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Not a Finding of Fact but a Conclusion of Law. COPIES FURNISHED: Becky Ayech Personal Representative Miakka Community Club 421 Verna Rd. Sarasota, Florida 34240 Douglas Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Edward B. Helvenston, Esquire Assistant General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609 6899
Findings Of Fact Application No. 75-00196 is a request by the Standard Sand and Silica Company, for a consumptive water use permit. This application is for an existing use involving withdrawal from one well. The application seeks an average daily withdrawal of 1.6925 million gallons per day and a maximum daily withdrawal of 2.16 million gallons per day. The sought-for withdrawal will not exceed the water crop as defined by the district, with the withdrawal consumptively using only 35 percent of the water crop. The water will be used on site for the washing of sand. Mr. Clifton W. Golden is an adjacent landowner who testified that he was afraid of salt water intrusion and that a sink hole might develop because of the vast quantities of water taken from the aquifer by the applicant. He does not feel that the issuance of a permit would be consistent with the public interest. He presented no hydrological data showing that issuance of the permit would adversely affect his property. Mary Fausteen Thompson is a property owner adjacent to the site from which the water will be taken. She has had problems in the past with Standard Sand and Silica Company apparently discharging excess water on to her property. She thinks those problems may be occurring again, causing some of her property to be flooded. The sought-for consumptive use will not significantly induce salt water intrusion. Except as otherwise noted in the findings of fact, none of the conditions set forth in Subsection 16J-2.11(2), (3) or (4), F.A.C., will be violated. Several letters of objections have been received in addition to the objectors noted above. The Southwest Florida Water Management District's staff recommends issuance of the subject permit in the amounts requested with the following conditions: That no off-site runoff be permitted by the applicant. That flowmeters be placed on the well and quarterly reports made to the district.
Recommendation It is hereby RECOMMENDED that Application No. 75-00196 be granted with the conditions set forth in paragraph 7 above. ENTERED this 28th day of May, 1976, in Tallahassee, Florida. CHRIS H. BENTLEY, Hearing Officer 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 P.O. Box 457 Brooksville, Florida 33512 Eugene W. Harris Standard Sand and Silica Co. P.O. Box 35 Davenport, Florida 33837 Mrs. Mary Fausteen Thompson Box 82-C, Evans Road Polk City, Florida Mr. Clifton W. Golden 800 Oriole Drive Virginia Beach, Florida 23451 Mr. John C. Jones Executive Director Florida Wildlife Federation 4080 North Haverhill Road West Palm Beach, Florida 33407
