The Issue Whether Bay County has demonstrated its entitlement to the Permit?
Findings Of Fact The Ecologically Diverse Florida Panhandle With its high diversity of species and richness in endemic plants, the Florida Panhandle has been identified as one of six continental "biodiversity hot spots" north of Mexico. It has more species of frogs and snakes, for example, than any other equivalently-sized area in the United States and Canada and has botanical species that do not exist anywhere else in the Coastal Plain, one of the three floristic provinces of the North Atlantic American Region. The biodiversity stems from a number of factors. The Panhandle was not glaciated during the Pleistocene Period. Several major river systems that originate in the southern Appalachian Mountains terminate on the Panhandle's Gulf Coast. Its temperate climate includes relatively high rainfall. These factors promote or produce plentiful sources of surface and groundwater that encourage botanical and zoological life and, in turn, a diverse ecology. When compared to the rest of Florida, the Panhandle is relatively free from man-made impacts to its water resources. Until recently, the population growth rate lagged behind much of the state. Despite a rapid increase in the population in the late 1990s into the early part of the twenty-first century, it remains much less densely populated than areas in the I-4 Corridor and coastal peninsular Florida to the south. The Panhandle can be divided into physiographic areas of geological variation that are highly endemic; a substantial number of plant and animal species found in these areas are found nowhere else in the world. One of these areas is of central concern to this case. Located in southern Washington County and northern Bay County, it is known as the Sand Hill Lakes Area. The Sand Hill Lakes Area The Sand Hill Lakes Area (the "Area") is characterized by unusual geology that produces extraordinary ecological value. With few exceptions (see findings related to Dr. Keppner's flora and fauna inventories on the NTC/Knight Property below), the Area has not been extensively studied. The data on biological communities and water levels that exist, sparse as it is, has been obtained from historic aerials dating to 1941. The aerials are of some use in analyzing lakes and surface waters whose source is the Surficial Aquifer, but they are of limited value otherwise. They are not of use in determining the level in the Surficial Aquifer. Nor are they of assistance in determining river height when the banks of the river are covered by hardwood forest canopy. The resolution of the aerials is insufficient to show details of the various ecosystems. They do not show pitcher plants, for example, that exist at the site of hillside seepage bogs common in the Area. An aspect of the Area that the aerials do reveal is its many karst features on the surface of the land. Karst lakes and sinkholes dominate the Area and are a component of its highly unusual geology which is part of a larger system: the Dougherty Karst Plain. The Dougherty Karst Plain is characterized by numerous karst features: springs, caverns, sinkhole lakes, and sinkholes. Sinkholes In Florida, there are three types of sinkholes: cover subsidence, cover collapse, and "rock" or "cavern" collapse. Of the three, cover subsidence sinkholes are the most common in the state. Cover subsidence sinkholes form as the result of processes that occur on the surface. A cover subsidence sinkhole is usually a shallow pan typically not more than a few feet deep. Found throughout Central and South Florida, they are the most common type of sinkholes in most of peninsular Florida. In contrast, the other two major types of sinkholes (cover collapse and cavern collapse) occur as the result of processes below the surface that cause collapse of surface materials into the substrata. Both types of "collapse" sinkholes are found in the Area, but cover collapse is the more common. Cavern collapse sinkholes are relatively rare. Typical of the Area, cover subsidence sinkholes are not found on the NTC/Knight Property. The NTC/Knight Property The majority of the NTC/Knight Property is in Washington County, but the property straddles the county line so that a smaller part of it is in northern Bay County. All of the NTC/Knight Property is within the Area. The District recognizes that the NTC/Knight Property contains natural resources of extraordinary quality as does the Area generally. Over the three years that preceded the hearing, Dr. Keppner, an NTC/Knight expert, conducted extensive inventories of the flora and fauna on NTC/Knight Property. Dr. Keppner's inventory showed the NTC/Knight Property supports more than 500 species of vascular plants (flora with a system of tubes within the stem, phloem, and the xylem that exchange materials between the roots and leaves) and 300 species of animals. Among them are at least 28 vascular plants and six animals listed as imperiled (threatened or endangered) by state or federal agencies. At least 22 of the imperiled species of vascular plants and eight of the imperiled species of animals are located within an area expected to be affected by the Wellfield for which Bay County seeks the permit modification. For example, at Big Blue Lake alone where impacts were predicted by NTC/Knight experts to take place, the following imperiled plant species are found: Smoothbark, St. John's Wort, Kral's Yelloweyed Grass, Quilwort Yelloweyed Grass, Threadleaf Sundew, Panhandle Meadowbeauty, and Crystal Lake Nailwort. In addition to the Keppner inventory, NTC/Knight commissioned other studies to determine the nature of the sinkholes and whether they are connected to the Floridan Aquifer. NTC/Knight's experts determined that the property contains cover collapse and a few cavern collapse sinkholes that connect to the Floridan Aquifer. Despite evidence to the contrary submitted by the District and Bay County, the NTC/Knight determinations are accepted as facts for a number of reasons, including the lineup of the sinkholes and sinkhole lakes along identified photo-lineaments and the distribution of them in patterns that are not random. A District study using a dye test, moreover, confirmed conduit flow exists in the Area just east of the NTC/Knight Property. With regard to the distribution of the sinkholes and sinkhole lakes on the NTC/Knight Property, Dr. Sam Upchurch used the term "String of Pearls" to describe multiple sinkholes that exist along the edges of several lakes on the property. When sinkholes closer to the center of a lake are clogged or plugged with sediment and debris, the lakes continue to leak around the plugs which causes new sinkholes to form along the edge of the plugs. Examples of the "String of Pearls" formation on the edges of existing lakes are found at White Western and Big Blue Lakes on the NTC/Knight Property and at Crystal Lake nearby in Washington County. The multiple sinkholes bordering the edge of Big Blue Lake are examples of cover collapse sinkholes that, in geological terms, are relatively young as evidenced by their steep sides. In a karst area such as the Area, there is preferential flow in the conduits because of the difference of efficiency of transmission of water flowing through a porous medium of rock compared to that flowing though a conduit. Absent pumping in the Wellfield, the underlying aquifers are relatively stable. If the requested pumping does not take place, it is likely the stability will remain for a substantial period of time. It is not known with precision what will happen in the long term to the karst environment should pumping occur at the Wellfield at the rate the District proposes. When pumping occurs, however, water in the Area affected by the Wellfield will move toward the Wellfield. "[A]s it does[,] you may get some turbulent flow or vorticity in the water." Tr. 1391, (emphasis supplied). At some point, a change in the potentiometric surface and loss of buoyancy will most likely occur. This leads to concerns for Dr. Upchurch from two perspectives: One . . . is that if there is a[n affected] sinkhole lake [on the surface,] it may induce downward flow . . . the other . . . is that if it breaks the plug it may either create a new sinkhole or create a substantial drop in the level of water in the lake . . . which drains periodically, not necessarily because of a wellfield, but because that plug breaks. Id. In the first instance, lake levels could be reduced significantly. In the second, a new sinkhole could be created or the water level could drop dramatically as occurred at Lake Jackson in Tallahassee. Sand Hill Lakes Wetlands The Area contains a number of wetland communities. These include hillside seepage bogs, steepheads, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and creeks and streams in forested wetlands. A number of these wetlands occur on the NTC/Knight Property within the zone of influence in the Surficial Aquifer predicted by NTC/Knight's experts employing a model known as the "HGL Model." The wetland systems on the NTC/Knight Property are diverse, by type, plant species composition, and richness. This remarkable diversity led the District to recognize that the NTC/Knight Property contains lakes of nearly pristine quality, interconnected karst features, and endemic steephead ravines, all of which are regionally significant resources of extraordinary quality. The Area's wetlands also include many streams, among them Pine Log Creek, the majority of which is located on the NTC/Knight Property. Significant recharge to the Floridan Aquifer occurs on NTC/Knight Property. To the west, north, and east of the NTC/Knight Property are major concentrations of Floridan Aquifer springs that are crucial to the quality and character of regional surface water systems, including the Choctawhatchee River, Holmes Creek, and Econfina Creek systems. All of these surficial systems are dependent on the groundwater resources of the Area. The Area's Hillside Seepage Bogs Hillside seepage bogs are marsh-like wetland usually located on gentle slopes of the sides of valleys. They form when the Surficial Aquifer intercepts the sloping landscape allowing water to seep onto the sloped surface. The plant communities in the bogs are dominated by a great number and variety of herbaceous plants that prefer full sun. Among them are carnivorous plants. These unusual plants include the Trumpet and White-Topped pitcher plants as well as other varieties of pitcher plants. Inundation or saturation for extended periods of time is necessary for pitcher plants and most of the rest of the plant communities found in the bogs to thrive and to fend off invasion by undesirable species. Hillside seepage bogs are valued because they are among the most species-rich communities in the world. A reduction in water levels in the bogs below the root zone of associated plants will kill the plant communities that live in them and pose a threat to the continued existence of the bogs. Hillside seepage bogs were once abundant in pre- settlement Florida, but their expanse has been greatly reduced. They are now estimated to only occupy between one and five percent of their original range. On NTC/Knight Property, they have been spared to a significant degree. Numerous hillside seepage bogs continue to exist on the NTC/Knight Property primarily along the margin of Botheration Creek and its tributaries. The Area's Steepheads Steepheads are unique wetland systems. Found around the globe, they are usually regarded as a rarity. More than 50 percent of the steepheads that exist in the world are in a narrow latitudinal band that extends from Santa Rosa County in the west to Leon County in the east, a major section of the Florida Panhandle. Steepheads occur in deep sandy soils where water originating in the Surficial Aquifer carries away sand and cuts into sandy soils. The seepage emerges as a "headwater" to create a stream that conveys the water from the steephead into a river, or in some rare circumstances, into a karst lake. Over time, flow of the seepage waters results in deep, amphitheater- shaped ravines with steep valley side walls. Steepheads are important to the ecologies of the areas in which they occur. They provide habitat for a number of Florida endemic animals and plants believed to be relics of once-abundant species. Water that emerges from a steephead is perennial. Because the steep slopes of the steephead have not been disturbed over a long period of time, the water remains at a relatively constant temperature, no matter the season. Sampling of aquatic invertebrates at the Russ Pond and Tiller Mill Steepheads on the NTC/Knight Property found 41 and 33 distinct taxa, respectively, to inhabit the steepheads. Among them were a number of long-lived taxa. Their presence is consistent with the hallmark of a steephead: perennial flow of water at a relatively constant temperature. Most of the known steepheads flow into streams or rivers. Between six and ten within the Area, however, flow into Sand Hill Lakes. They have no direct connection to any surface drainage basin, thereby adding to their uniqueness. The level in the Surficial Aquifer has a direct impact on where and to what extent seepage flows from the sidewalls of a steephead. The Area's Sphagnum Bogs Sphagnum moss grows in many locations within the landscape and requires moisture. Where there is a large amount of sphagnum moss, it can form a unique community known as a sphagnum bog that is capable of supporting unique plant and animal populations. In the Area, these sphagnum bogs form along the valley sidewalls of steephead ravines and are fed by Surficial Aquifer seepage from the sidewall of the ravine. These sphagnum bogs support unique plant and animal communities, including a salamander discovered by Dr. Means that is new to science and so far only known to exist in sphagnum bogs in the Florida Panhandle. The Area's Sinkhole Lakes and their Littoral Seepage Slopes Sand Hill Lakes are nutrient poor, or "oligotrophic," receiving most of their nutrient inputs through exchange with the plant and animal communities on the adjacent littoral shelves during periods of high water levels. Fluctuating water levels in the Sand Hill Lakes allow a littoral zone with many different micro-habitats. Areas closest to the lakes are inundated regularly, but higher areas of the littoral zone are generally dry and inundated only every ten or 20 years -- just often enough to prevent encroachment of trees. In a few instances, portions of the littoral zones are inundated by seepage from the Surficial Aquifer. Above the normal low water of the Sand Hill Lakes, the littoral shelf occurs along a low gradient. As the littoral shelf transitions into the lake bottom and toward the deeper parts of the lake, there is an inflection point, where the gradient of the lake bottom becomes much steeper than the littoral shelf. If lake water levels fall below that natural inflection point, gully erosion will occur. The flow of water will be changed along the littoral shelf from seepage sheet flow over a wide expanse to water flowing down gullies in a concentrated stream. This change in flow will result in a loss of area needed by certain seepage dependent plants and animals as well as increased sedimentation from erosion. Big Blue Lake is unique because it boasts the largest known littoral zone seepage area of any Sand Hill Lake. The seepage zone along Big Blue Lake supports a number of rare plant species, including the Thread-Leaf Sundew, Smoothed Barked St. Johns Wort, and Crystal Lake Nailwort. The Area's Temporary Ponds Temporary ponds are small isolated water bodies that generally have no surface water inlet or outlet. Typically very shallow, they are sometimes wet and sometimes dry. Temporary ponds can range from basins that have continuous water for three to five years, to basins that have standing water for a month or two, every two to four years. These conditions limit their occupation by fish and, therefore, provide ideal conditions for amphibian reproduction which only occurs when water levels are maintained long enough to complete a reproductive cycle. In the Area, temporary ponds are a direct expression of the Surficial Aquifer and contain no known restrictive layer that might cause water to be "perched" above the Surficial Aquifer. Temporary ponds are critical to the viability of amphibian populations and support high amphibian biodiversity. A given pond can contain between five and eight species of salamander, and between 12 and 15 species of frogs. There has been a decline recently in the population of frogs and other amphibians that depend upon temporary ponds. The decline is due in part to ditching and other anthropogenic activities that have altered the hydrology of temporary ponds. Temporary ponds have a higher likelihood of being harmed by a drawdown than larger, connected wetlands systems. Lowered Surficial Aquifer water levels would lower water levels in temporary ponds and, thereby, threaten amphibian reproduction. Creeks/Streams in Forested Wetlands Streams are classified on the basis of the consistency of flowing water, including perennial (always flowing), intermittent (flowing part of the year), and ephemeral (flowing only occasionally during rain events). The type of stream flow is important because movement of water is essential to support aquatic systems in stream habitats. The NTC/Knight Property includes a number of stream systems, including Botheration Creek and Pine Log Creek. Botheration Creek is fed by groundwater discharge and originates, in large part, on the NTC/Knight Property. Botheration Creek flows from east to west until it intersects Pine Log Creek on the southwest part of the NTC/Knight Property. Botheration Creek provides Pine Log Creek with approximately 89 percent of Pine Log Creek's flow. From the confluence, Pine Log Creek flows south and west into the Pine Log State Forest and eventually joins the Choctawhatchee River. Botheration Creek contains high quality water and a diverse mix of aquatic invertebrates and fish. Sampling at a stage recorder located approximately two miles west of the eastern boundary of the NTC/Knight Property ("BCS-01") identified 46 taxa of macroinvertebrates, including six long- lived taxa, and mussels. The water level in Botheration Creek at BCS-01 was measured to be between 0.1 and 0.32 feet by four measurements taken from October 2010 to July 2011. Nonetheless, the presence of long-lived taxa and mussels indicates that, at BCS-01, Botheration Creek is a perennial stream. Carbon export from streams provides nutrients that feed the stream system. Headwater streams like Botheration Creek and its tributaries are essential to carbon export. For carbon export to occur, a stream must have out-of-bank flood events regularly to promote nutrient exchange with the flood plain. Bay County and its Water Supply Prior to 1961, the County obtained its public water supply from wellfields located near downtown Panama City. The wellfields drew from the Floridan Aquifer. An assessment of the pre-1961 groundwater pumping appears in a District Water Supply Assessment released in June 1998. In summary, it found that near Panama City, the potentiometric surface was substantially depressed by the pumping. Due to the threat of saltwater intrusion, the Deer Point Lake Reservoir (the "Reservoir") was constructed as an alternate water supply. A local paper mill, the city of Panama City, and Tyndall Air Force Base, all began to obtain public supply water from the Reservoir. Six years after the construction of the Reservoir, the Floridan Aquifer's water levels had rebounded to pre-pumping levels. See NTC/Knight Ex. 93 at 69. The authorization for the Reservoir began in the 1950's when the Florida Legislature passed a series of laws that granted Bay County authority to create a saltwater barrier dam in North Bay, an arm of the St. Andrews Bay saltwater estuary. The laws also allowed Panama City to develop and operate a surface freshwater reservoir to supply water for public use. The Deer Point Lake Dam (the "Dam") was built in 1961 from metal sheet piling installed across a portion of North Bay. The Dam created the Reservoir. The watershed of the Reservoir includes portions of Jackson, Calhoun, Washington, and Bay Counties and covers approximately 438 square miles. The Reservoir receives freshwater inflow from several tributaries, including Econfina Creek, Big Cedar Creek, Bear Creek/Little Bear Creek, and Bayou George Creek, totaling about 900 cubic feet per second ("cfs") or approximately 582 MGD. The volume of inflow would increase substantially, at least two-fold, during a 100-year storm event. The Dam is made of concrete and steel. Above it is a bridge and two-lane county road roughly 11.5 feet above sea level. The bridge is tied to the Dam by pylons. The top of the Dam is 4.5 feet above sea level, leaving a distance between the Dam and the bridge bottom of about seven feet. There is an additional structure above the Dam that contains gates, which swing open from the force of water on the Reservoir's side of the Dam. Capable of releasing approximately 550 MGD of freshwater into the saltwater bay, the gates keep the level of the Reservoir at about five feet above sea level. The height of the Dam and the gate structure leaves a gap between the bottom of the bridge deck and the top of the structure of "somewhere between 12 and 14 inches, a little better than a foot." Tr. 140. If storm surge from the Gulf of Mexico and St. Andrew's Bay were to top the Dam and the gate structure, the gap would allow saltwater to enter the Reservoir. The gates and the Dam structure are not designed to address storm surge. The Dam is approximately four feet thick and roughly 1,450 feet long. The 12-to-14 inch gap extends across the length of the Dam. With normal reservoir levels, the volume of water it contains is approximately 32,000-acre-feet or roughly 10.4 billion gallons. Bay County needs to drawdown the lake level for fish and wildlife purposes, the control of aquatic growth, and weed control. In winter, FWS prescribes a 45-day period of time to draw down the lake to expose the banks to kill vegetation. The last time the lake was drawn down by the County, the water level dropped approximately three feet, from five feet above sea level to two feet above sea level. This process took approximately six days and 16 hours, or approximately 53 hours/foot. Repair of the Dam and its Maintenance The Dam has been repaired three times. The last repair was following Hurricane Opal which hit the Florida Panhandle in the fall of 1995. During Hurricane Opal, "saltwater . . . entered . . . the [R]eservoir . . . [t]hat took 20-some days to flush out . . . ." Tr. 135. No evidence was presented regarding the Dam's vulnerability from the perspective of structural integrity during normal or emergency conditions. Other than the inference drawn from Mr. Lackemacher's testimony that Hurricane Opal damaged the Dam in 1995, no evidence was presented to suggest that the Dam's structure is vulnerable to damage caused by a storm surge, wave effect or other conditions caused by a storm of any magnitude. After the last of the three repairs, Bay County implemented a detailed maintenance program. Based upon the latest inspection reports, the Dam is in good condition and structurally sound. No work other than routine inspection and maintenance is currently planned. The 1991 Agreement and the WTP Bay County's current withdrawal of water from the Reservoir is based on a 1991 agreement between Bay County and the District (the "1991 Agreement"). See Joint Ex. Vol. II, Tab K. The 1991 Agreement allows Bay County after the year 2010 to withdraw 98 MGD (annual average) with a maximum daily withdrawal of 107 MGD. The 1991 Agreement, still in effect, authorizes Bay County to withdraw enough water from the Reservoir to meet its needs through 2040. Water for public supply is withdrawn from the Reservoir by a water utility pump station (the "Pump Station") located a short distance from the Dam in Williams Bayou. The water is piped to the water utility's treatment plant (the "Water Treatment Plant") five miles away. The Water Treatment Plant treats 60 MGD. Following treatment, the water is distributed to Bay County's wholesale and retail customers. The Reservoir water available to Bay County utilities is more than adequate to fulfill the water consumption demands of Bay County's system through a 20-year permit horizon. The transmission line between the Pump Station and the Water Treatment Plant has fittings that were designed to allow transmission of groundwater withdrawn from groundwater wells to be located along the transmission line to the Water Treatment Plant to provide a backup supply for the Reservoir. Bay County's Current Use of Potable Water The amount of water consumed by Bay County utility customers has declined over the last five years. Bay County's current use of water, based upon the average of the 13 months prior to the hearing, was 24.5 MGD, an amount that is only 25 percent of the water allocation authorized by the 1991 Agreement. There are approximately 560,000 linear feet of main transmission lines in Bay County with small service lines accounting for another several hundred thousand linear feet. Bay County furnishes water directly to approximately 6,000 retail customers in areas known as North Bay, Bay County, and the former Cedar Grove area, which is now part of Bay County. Wholesale customers include Panama City Beach, Panama City, Mexico Beach, Callaway, Parker, Springfield, and parts of Lynn Haven. The County also furnishes potable water to Tyndall Air Force Base. Lynn Haven does have some water supply wells; however, Bay County still supplements this water supply by approximately 30 percent. No other cities serviced by Bay County produce their own water. Bay County has a population of approximately 165,000- 170,000 permanent residents, which includes residents of the cities. The Bay County area experiences seasonal tourism. From spring break to July 4th, the population can grow to more than 300,000. The users of Bay County's drinking water supplies include hospitals, Tyndall Air Force Base, and the Naval Support Activity of Panama City ("NSA"). The County has 178 doctor's offices, 56 dental offices, 29 schools, 21 fire departments, 12 walk-in-clinics, six nursing and rehabilitation homes, six major employers, three colleges and universities, and two major hospitals, all which are provided drinking water by Bay County. Panama City Beach is the community which has the highest water use. Panama City Beach's average daily use is approximately 12 MGD. The peak day of usage for all of Bay County's customers over the 13 months prior to the hearing was 40 MGD. Bay County sells water to community water utility systems referred to as a "consecutive system." They include Panama City Beach, Panama City, and Mexico Beach. Bay County's request for 30 MGD contemplates provision of water for all essential and non-essential water uses occurring within the consecutive system. Bay County and the consecutive systems are subject to the District's regulations regarding emergency water use restrictions which typically restrict the non-essential use of water during water shortage emergencies. Hurricanes, Train Wrecks, and Post-9/11 America At the District's recommendation, Bay County has been considering a backup potable water source since the mid-1980's. Bay County's main concern is that it has inadequate alternatives to the Reservoir should it be contaminated. Contamination to date has been minimal. In the period of time after the 1961 creation of the Reservoir to the present, the Dam and the Reservoir have suffered no major damage or impacts from a tropical storm. No tropical storm since 1961 has disrupted Bay County's ability to provide potable water. Even Hurricane Opal in 1995 did not disrupt the water supply. Recent hurricane activity in the Gulf of Mexico, however, has aroused the County's fears. Should a storm of sufficient magnitude make landfall in proximity to the Dam, there is potential for saltwater contamination of the Reservoir from storm surge or loss of impounded freshwater due to damage to the Dam. Mr. Lackemacher, assistant director of the Bay County Utility Department and manager of the water and wastewater divisions of the department, has experience with other hurricanes in Palm Beach, Florida, and Hurricane Hugo in Myrtle Beach, South Carolina, during which water utilities suffered disruption of their distribution systems. The experience bolsters his concern about the damage a storm could cause Bay County's source of public water supply. Bay County's intake structure at Williams Bayou is approximately one mile away from the Dam. The location of the Pump Station puts it at risk for damage from a strong storm or hurricane. There is a rail line near the Reservoir. It runs along Highway 231 and over creeks that flow into the Reservoir, including the Econfina Creek. The rail line is known as "Bayline." Bayline's most frequent customers are the paper mill and the Port of Panama City. Not a passenger line, Bayline is used for the transport of industrial and chemical supplies. In 1978, a train derailment occurred on tracks adjacent to creeks that feed the Reservoir. The derailment led to a chlorine gas leak into the atmosphere. There was no proof offered at hearing of contamination of the Reservoir. There has never been a spill that resulted in a hazardous chemical or pollutant being introduced into the Reservoir. Bay County has not imposed restrictions on the type of vehicles that are allowed to use, or the material that may pass over, the county road on the bridge above the Dam. Nonetheless, in addition to saltwater contamination, Bay County also bases the need for an alternative water source on the possibility of a discharge into the Reservoir of toxic substances from a future train derailment. Bay County is also concerned about contamination of the Reservoir from a terrorist attack. In short, Bay County is concerned about "anything that could affect the water quality and water in Deer Point Lake." Tr. 184. The concerns led Bay County to file its application for the Wellfield on lands currently owned by the St. Joe Company. Consisting of ten wells spaced over an area of approximately ten square miles, the Wellfield would have a capacity of 30 MGD. Bay County's application was preceded by the development of the District's Region III Regional Water Supply Plan and efforts to acquire funding. Funding for the Wellfield and the Region III Regional Water Supply Plan Shortly after the commencement of the planning for the Wellfield, the District, in May 2007, authorized the use of funds from the State's Water Protection and Sustainability Trust Fund ("WPSTF"). The WPSTF is intended for development of alternative water supplies. In cooperation with the District, Bay County began drilling a test well followed by analyses to evaluate the water for potable suitability. In October of the same year, the District passed a resolution to request the Department of Environmental Protection to release $500,000 from the WPSTF to the District for local utilities in Bay and Escambia Counties for "Water Resource Development." NTC/Knight Ex. 195, p. 2. The amount was to be used "to provide funding for implementation of alternative water supply development and water resource developments projects pursuant to sections 403.890 and 373.1961, F.S." Id., p. 1. In February 2008, the District began a process to develop a regional water supply plan for Bay County. If the Wellfield were designated in the applicable regional water supply plan as "nontraditional for a water supply planning region," then it would meet the definition of "alternative water supplies" found in section 373.019(1), Florida Statutes. "In evaluating an application for consumptive use of water which proposes the use of an alternative water supply project as described in the regional water supply plan," the District is mandated "to presume that the alternative water supply is consistent with the public interest " § 373.223(5). Whether the Wellfield is to be presumed to be in the public interest depends on whether the application proposes the use of an alternative water supply project as described in the District's Region III Water (Bay County) Water Supply Plan adopted in 2008. The 2008 RWSP Pursuant to the process commenced in February, the District in August 2008 produced the Region III (Bay County) Regional Water Supply Plan (the "2008 RWSP"). In a section entitled "Identification of Alternative Water Supply Development Projects," the 2008 RWSP provides the following: "All of the water supply development projects identified in Table 4 are interrelated and considered alternative, nontraditional water supply development projects." NTC/Knight Ex. 187 at 14. Table 4 of the 2008 RWSP does not specifically identify the Wellfield. It identifies three projects in general terms. The first of the three (the only one that arguably covers the Wellfield) shows "Bay County Utilities" as the sole entity under the heading "Responsible Entities." Id. at 13. The project is: "Inland Ground Water Source Development and Water Supply Source Protection." Id. Under the heading, "Purpose/Objective," the Table states for the first project, "Develop inland alternative water supply sources to meet future demands and abate risks of salt water intrusion and extreme drought." Id. The Table shows "Estimated Quantity (MGD)" to be "10.0." Id. (In July 2008, the District's executive director informed Bay County that the Wellfield could produce 10 MGD.) The "Time Frame" is listed as 2008-12, and the "Estimated Funding" is "$5,200,000 WPSPTF" and "$7,800,000 Local, NWFWMD." Id. While not specifically identified in the 2008 RWSP, Table 4's project description supports a finding that the Wellfield is, in fact, one of the inland alternative water supply sources. The 2008 RWSP, therefore, designates the Wellfield as a "nontraditional" water supply source for Region III.4/ (The Wellfield also, therefore, meets the definition of "[a]lternative water supplies" in section 373.019(1). The demonstration of a prima facie case by Bay County and the District, however, make the applicability of the presumption a moot point. See Conclusions of Law, below.) Water Supply Assessments and Re-evaluations Development of a regional water supply plan by the governing board of each water management district is mandated "where [the governing board] determines that existing and reasonably anticipated sources of water are not adequate to supply water for all existing and future reasonable-beneficial uses and to sustain the water resources and related natural systems for the planning period." § 373.709(1), Fla. Stat. (the "Regional Water Supply Planning Statute"). The District determined in its 1998 District Water Supply Assessment ("WSA") for Region III (Bay County) that the existing and reasonably anticipated water sources are adequate to meet the requirements of existing legal users and reasonably anticipated future water supply needs of the region through the year 2020, while sustaining the water resource and related natural systems. See NTC/Knight 93 at 79. In 2003, Ron Bartel, the director of the District's Resource Management Division, issued a memorandum to the Governing Board (the "2003 Re-evaluation Memorandum"), the subject of which is "Regional Water Supply Planning Re- evaluation." NTC/Knight 95 (page stamped 42). The 2003 Re-evaluation Memorandum sets out the following with regard to when a "water supply plan" is needed: The primary test we have used for making a determination that a water supply plan was "not needed" for each region is that projected consumptive use demands for water from major water users do not exceed water available from traditional sources without having adverse impacts on water resources and related natural systems. Similarly, regional water supply planning is initiated "where it is determined that sources of water are not adequate for the planning period (20) years to supply water for all existing and reasonable-beneficial uses and to sustain the water resources and related natural systems." Id. With regard to the need for a Water Supply Plan for Bay County the 2003 Re-evaluation Memorandum states: [I]n Bay County (Region III), sufficient quantities have been allocated for surface water withdrawal from Deer Point Lake Reservoir through the District's consumptive use permitting program extending through the year 2040. In this area, the District is also scheduled to complete a minimum flow and level determination for the lake by the year 2006. This determination will be useful for deciding if additional water supply planning is needed before the permit expires in 2040. Id. (page stamped 43). The 2008 RWSP's designation of the Wellfield is justified in the minutes of the Governing Board meeting at which the 2008 RWSP's approval took place: While the reservoir has largely replaced the use of coastal public supply wells historically impacted by saltwater intrusion, there remain challenges within the region that make development and implementation of a Regional Water Supply Plan (RWSP) appropriate. Development of alternative water supplies would diversify public supply sources and help drought-proof the region through establishment of facility interconnections. Development of alternative supplies would also minimize vulnerability associated with salt water potentially flowing into the reservoir during major hurricane events. Id., p. 3 of 4. The adoption of the 2008 RWSP was followed in December 2008 by the District's 2008 Water Supply Assessment Update. The update is consistent with the earlier determinations of the adequacy of the Reservoir as a water supply source for the foreseeable future (in the case of the update, through 2030). The update also voices the concern about water quality impacts from storm surge. The update concludes with the following: In Region III, the existing and reasonably anticipated surface water resources are adequate to meet the requirements of existing and reasonably anticipated future average demands and demands for a 1-in-10 year drought through 2030, while sustaining water resources and related natural systems. However, the major concern for potential water quality impacts is that resulting from hurricane storm surge. A Regional Water Supply Plan (NWFWMD 2008) has recently been prepared for Region III to address concerns associated with existing surface water systems. NTC/Knight Ex. 101, p. 3-41. The Parties Washington County is a political subdivision of the State of Florida. Washington County is located directly north of Bay County and the Wellfield and within one mile of some of the proposed wells. Washington County includes thousands of wetlands and open water systems. Because of the hydro-geologic system in the area of the Wellfield, if there are wetland, Surficial Aquifer, and surface water impacts from the withdrawal under the Permit, it is likely that impacts will occur in Washington County. Washington County has a substantial interest in protection, preservation, and conservation of its natural resources, including lakes, springs, and wetlands, and the flora and fauna that depend on these water resources, especially endangered flora and fauna. Washington County has a substantial interest in the protection of all water resources in Washington County because of the close relationship between surface waters, groundwater, and the potable water supply used by Washington County residents. NTC/Knight is the owner of approximately 55,000 acres of land located in northern Bay County and southern Washington County. The NTC/Knight Property includes thousands of acres of wetlands and open waters, including Sand Hill Lakes, steepheads, hillside seepage bogs, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and forested wetlands. A large portion of the NTC/Knight Property is directly adjacent to the Wellfield and within the HGL Model projected drawdown contour. Based on the projected amount of drawdown from pumping at the proposed average rate of 5 MGD, the 0.5 projected drawdown contour predicted by the HGL Modeling Report (see Finding of Fact 121, below) extends over thousands of acres of the property. NTC/Knight has a substantial interest in the protection of the surface and groundwater directly on, under, and adjacent to its property. The water supports the numerous ecosystems of extraordinary value located on the property. James Murfee and Lee Lapensohn are individuals, who reside in Bay County on property fronting on and beneath Tank Pond approximately five miles from the Wellfield. Petitioners Murfee and Lapensohn have a well which extends into the Intermediate Aquifer. The Murfee and Lapensohn properties are within the HGL Model projected drawdown contour. Petitioners Murfee and Lapensohn have a substantial interest in the protection of their drinking water supply well and the surface waters directly on and adjacent to their properties. Bay County, the applicant, is a political subdivision of the State of Florida. The District is a water management district created by section 373.069(1). It has the responsibility to conserve, protect, manage, and control the water resources within its geographic boundaries. See § 373.069(2)(a), Fla. Stat. Section 120.569(2)(p), Florida Statutes Section 120.569(2)(p), in pertinent part, provides: For any proceeding arising under chapter 373, chapter 378, or chapter 403, if a nonapplicant petitions as a third party to challenge an agency’s issuance of a license, permit, or conceptual approval, the order of presentation in the proceeding is for the permit applicant to present a prima facie case demonstrating entitlement to the license, permit, or conceptual approval, followed by the agency. This demonstration may be made by entering into evidence the application and relevant material submitted to the agency in support of the application, and the agency’s staff report or notice of intent to approve the permit, license, or conceptual approval. Subsequent to the presentation of the applicant’s prima facie case and any direct evidence submitted by the agency, the petitioner initiating the action challenging the issuance of the license, permit, or conceptual approval has the burden of ultimate persuasion and has the burden of going forward to prove the case in opposition to the license, permit, or conceptual approval through the presentation of competent and substantial evidence. The permit applicant and agency may on rebuttal present any evidence relevant to demonstrating that the application meets the conditions for issuance. Paragraph (p) was added to section 120.569(2) in the 2011 Session of the Florida Legislature. Accordingly, the final hearing commenced with the Bay County and the District's presentation of its prima facie case by submitting the application, supporting documentation, and the District's approval of the application. Respondents also presented the testimony of four witnesses in the hearing's first phase. Phase I of the Final Hearing: Bay County's Application, Supporting Documents, the District's Approval and Supporting Testimony The Application File At the final hearing, Bay County and the District offered the "application file," marked as Joint Exhibit Binder Volumes I-IV (the "Application File") in the hearing's first phase. It was admitted into evidence. A document entitled "Alternate Water Supply Report - Bay County Water Division" dated May 20, 2008 (the "Hatch Mott MacDonald Report") is contained in the Application File. See Joint Ex. Vol. I, Tab B. The Hatch Mott MacDonald Report is a preliminary evaluation of a wellfield with 22 wells, an "initial phase . . . [of] five (5) wells producing 5 MGD and the final phase . . . [of] 17 wells, producing 25 MGD." Id. at 1. The evaluation includes the gathering of information, a recommendation for the best method of treatment, an analysis of whether individual well sites or a centralized site would be superior, a hydraulic model and analysis, and the potential construction and operation costs. The report concludes in its Executive Summary: HMM's preliminary results, based upon water analysis of Well No. 1, indicate that only disinfection will be required for potable water treatment. Additionally, the hydraulic analysis indicated that the wells are capable of providing the initial 5 MGD and future 25 MGD to the proposed connection point along Highway 388 without re-pumping. Adequate storage for fire protection should be considered at current and future service areas. The use of chlorine gas at each well site during the initial phase had the lowest present worth of $16,770,270; that is, the smallest amount of funds needed today to build, operate, and maintain the system. The use of chlorine gas at each well in the final phase had a present worth of $41,245,118, only slightly more than the present worth of $40,834,245 for on-site Id. generation of disinfectant at three (3) central facilities. The Application File contains a response to a District request for additional information (the "2009 RAI Response") submitted by the Bay County Services Utility Director and received by the District in September 2009. See Joint Ex. Vol. II, Tab K. The 2009 RAI Response contains the 1991 Agreement and numerous other documents. Among them is a report prepared by HydroGeoLogic, Inc. ("HGL") entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" dated September 2009 (the "2009 HGL Modeling Report"). The report predicts impacts that would be created to the surrounding aquifers as a result of the Wellfield pumping, but recommends that additional data be obtained. The Application File contains the District's Notice dated March 25, 2010. See Joint Ex. Vol. III, Tab B. Attached to the Notice is a draft of the Permit and a staff report from the District recommending approval with conditions. Condition 11 of the Permit's standard conditions obligates Bay County to mitigate any significant adverse impacts caused by withdrawals and reserves the right to the District to curtail permitted withdrawal rates "if the withdrawal causes significant adverse impact on the resource and legal uses of water, or adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. III, Tab B, p. 3 of 17. Attachment A to the Permit requires conditions in addition to the standard conditions contained in the body of the Permit. Paragraph 12 of Attachment A, for example, requires that Bay County implement and maintain a water and conservation efficiency program with a number of goals. Attachment B to the Permit requires a monitoring and evaluation program and wetland monitoring of adjacent properties to determine if the pumping causes adverse impacts to wetland areas, including habitat and species utilization. The Application File contains a revised modeling report also entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" (the "2011 Revised HGL Modeling Report" or the "HGL Model Report"). See Joint Ex. Vol. III, Tab P. The 2011 Revised HGL Modeling Report predicts impacts of the pumping of the Wellfield on the Upper Floridan Aquifer and the Surficial Aquifer. The HGL Model is based on an adaptation of an original model first developed by the U.S. Geological Survey (USGS) and then further adapted by HGL. The adapted model is known as MODFLOW-SURFACT. The MODFLOW-SURFACT Model has been used in excess of 600 applications and is used worldwide. The HGL Model predicted impact from pumping when wellfield pumping achieves a "steady state." Steady state impact is achieved after 10-12 years of constant pumping. The impact and the area of impact is depicted on Figure 5.1b(1) of the 2011 Revised HGL Modeling Report. The predicted drawdown of the Surficial Aquifer is predicted to be six inches (0.5 ft) within the areas indicated. The Application File shows that the permit was revised twice. Ultimately, a Second Revised Notice of Proposed Agency Action dated July 22, 2011, was issued by the District. Attached to the Second Revised NOPAA is the District's Permit. See Joint Ex. Vol. IV, Tab U. A revised Staff Report from the District dated July 18, 2011, is also included in Volume IV of the joint exhibits. See id., Tab Q. The Permit as supported by the staff report allows an average daily withdrawal of 5 MGD, a maximum daily withdrawal of 30 MGD for no more than 60 days per year (with a maximum of 52 consecutive days), and a maximum monthly amount of 775 million gallons. See Joint Ex. Vol. IV, Tab U. The Permit also includes the LTEMP jointly prepared by the Applicant and the District. See id., Attachment B. The Permit requires Bay County to "mitigate any significant adverse impact caused by withdrawals . . . on the resource and legal water withdrawals and uses, and on adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. IV, Tab R, p. 3 of 11. If the District receives notice of an impact from the existing legal user, it contacts the utility. "Within 72 hours [the utility has] a well contractor out there and they have determined what the problem is." Tr. 615. There are no time requirements for the resolution of the impact or any other resolution procedures in the Permit. Definitions of Emergency and Maintenance Amounts The Permit does not include a definition of when the Reservoir may be considered to be unavailable as a public water supply. That determination is left to Bay County. The Permit does not set a withdrawal limit lower than the limits detailed above for maintenance of the Wellfield. There is one set of withdrawal limits. They apply irrespective of the purpose of the withdrawals, that is, whether for backup in an emergency, maintenance, or some other purpose that falls under Public Supply or Industrial Use. Conditions and Monitoring Requirements Bay County is required to mitigate any significant adverse impacts on resources and legal water withdrawals and uses caused by the County's withdrawal from the Wellfield. In addition, the District reserves the right to curtail permitted withdrawal rates if Bay County's withdrawal causes adverse impacts on local resources and legal uses of water in existence at the time of the permit application. In the event of a declared water shortage, the Permit requires Bay County to make water withdrawal reductions ordered by the District. In addition, the District may alter, modify, or deactivate all or parts of the Permit. Attachment A to the Permit, states: The Permittee shall not exceed total, combined groundwater and surface water (authorized in Individual Water Use Permit No. 19910142) withdrawals of an average daily withdrawal of 98,000,000 gallons, a maximum daily withdrawal of 107,000,000 gallons and a maximum monthly withdrawal of 2,487,750,000 gallons. Joint Ex. Vol. IV, Tab U, p. 4 of 11. The inclusion of "surface water" in the condition covers withdrawals from the Reservoir. The combination of actual withdrawals from the Wellfield and actual withdrawals from the Reservoir, therefore, means that Bay County may not exceed the limitations of the withdrawals authorized by the 1991 Agreement. Attachment A to the Permit further explains how Bay County must mitigate harm caused by groundwater withdrawals. The Permittee, within seven days of determination or notification by the District that the authorized groundwater withdrawal is causing harm to the resources, shall cease or reduce, as directed by the District, its pumping activity. The Permittee shall retain the services of a qualified, licensed professional to investigate allegations of interference with an existing, legal groundwater use. The Permittee shall ensure their chosen contractor investigates the alleged interference within 72 hours of the allegation being made. If it is determined that the use of a well has been impaired as a result of the Permittee's operation, the Permittee shall undertake the required mitigation or some other arrangement mutually agreeable to the Permittee and the affected party. The Permittee shall be responsible for the payment of services rendered by the licensed water well contractor and/or professional geologist. The Permittee, within 30 days of any allegation of interference, shall submit a report to the District including the date of the allegation, the name and contact information of the party making the allegation, the result of the investigation made and any mitigation action undertaken. Joint Ex. Vol. IV, Tab U, Attachment A, p. 4 of 11. Bay County is also required, within two years from the Permit's issuance, to submit to the District for review and approval a contingency plan to mitigate potential impacts. The County must wait one full year prior to commencing withdrawal of groundwater for production purposes. During the one-year period, the County must complete groundwater, surface water, and wetland monitoring. The requirements of the mandatory monitoring are found in Attachment B of the Permit, LTEMP. See Joint Ex. Vol. IV, Tab U, Attachment B. The LTEMP "is designed to track trends in ecological and hydrological conditions caused by naturally occurring fluctuations in rainfall, which may affect ground and surface water hydrologic conditions; and to identify potential effects caused by wellfield pumping." Joint Ex. Vol. IV, Tab U, Attachment B at 1. If a substantive deviation occurs from predictions made by the HGL Modeling, or if any other hydrologic or ecologic changes due to the withdrawals are observed at monitoring sites, the District is required to review and, in consultation with Bay County, appropriately revise the LTEMP as necessary with the aim that the monitoring will assure that the conditions for issuance of the Permit are being met. Testimony in Support of the Application In addition to the documentary evidence offered in the first phase of the proceeding, Bay County and the District presented the testimony of several witnesses. These witnesses testified as to background and the 2008 RWSP, the vulnerability of the Reservoir to saltwater contamination from storm surge, and the basis for the District's decision. Vulnerability to Storm Surge There is a one percent chance every year of a 100- year storm event. Flood Insurance Rates Maps ("FIRMS") show that the 100-year water level (the level of storm surge in a 100-year storm event) at the Dam will reach 11 feet NAVD, two feet above the top of the gate structure above the Dam. The Federal Emergency Management Agency ("FEMA") and the National Weather Service ("NWS") have developed the Sea, Lake, and Overland Surge from Hurricanes ("SLOSH") model, which estimates storm surge depths resulting from historical, hypothetical, or predicted hurricanes. A Florida Department of Emergency Management's SLOSH model of the Panama City area shows maximum surge levels for Storm Categories 1, 2, 3, 4, and 5, in NAVD feet as 3.3, 5.8, 10.8, 14.1, and 18.1, respectively. The SLOSH model, in all likelihood, is a low estimation. It is reasonable to expect surge levels in a Category 3 hurricane that passes directly over the Dam, for example, to be higher than 10.8 feet NAVD predicted by the SLOSH model at the Dam. According to the National Oceanic and Atmospheric Administration's ("NOAA") database, 43 tropical storms and hurricanes have passed within 200 miles of the Reservoir between 1970 and 2010 and 20 have come within 100 miles. None have made landfall closer than 40 miles away from the Dam. Of the 20 storms passing within 100 miles of the Reservoir, four have reached Category 3 strength or higher: Eloise, Elena, Opal, and Dennis. In 2004, Hurricane Ivan made landfall over 100 miles to the west of the Dam and raised water levels near the Dam to nearly five feet NAVD. The following year, Hurricane Dennis made landfall 76 miles to the west of the Dam. Dennis produced a surge level of nearly four feet NAVD near the Dam. "Hurricane Eloise (1975) made landfall 40 miles west of Panama City and produced water levels 15 ft above normal at Panama City ([citation omitted]). However, the storm passed through the area quickly and does not appear to have significantly affected the dam." Bay County Ex. 1, p. 3 of 9. Hurricane Opal made landfall 86 miles west of Panama City Beach and produced water levels of about 8.3 feet NAVD near the Dam. The storm surge did not overtop the gate structure above the Dam, but the gates were jammed by debris. "[C]hloride levels rose above 50 ppm at the intake pumps and two to three times above normal background levels of 8 to 10 ppm 'almost one mile up-reservoir.'" Id. The levels of chloride were "still well within drinking water limits," tr. 434, of 250 parts-per- million (ppm). Hurricane Katrina made landfall in 2005 more than 200 miles west of the Reservoir with storm surges higher than 20 feet. Katrina produced surge levels of five feet above normal tide levels in Bay County. The rate and amount of saltwater that would enter the Reservoir depends on the height of the storm surge above the Dam. The 100-year surge levels could remain above the top of the Dam for three or more hours. Such an event would introduce approximately 56,200,000 cubic feet or 1,290 acre-feet of saltwater into the Reservoir, even if the Dam were to remain intact (undamaged) and the tide gates remain closed. The salinity levels bay-side of the dam are generally 23,000 to 33,000 ppm. It is reasonable to expect that in the event of a 100-year storm event, much of the storm surge would come directly from the Gulf of Mexico, which has higher salinity levels. With the Dam intact, the introduction of 1,290 acre- feet of saltwater at 33,000 ppm would raise the average chloride concentration in the Reservoir to at least 800 ppm, more than three times the maximum drinking water chloride level of 250 ppm. Assuming the Dam remained intact during a 100-year storm event, freshwater added over time to the lake from the streams and aquifer will dilute the elevated lake chloride level and restore the lake water to a level fit for human consumption. The USGS has measured stream flow at Deer Point Lake and estimated the lake receives an average of 600 million gallons of freshwater per day or 900 cfs. Post-Opal rates were estimated at 1,500 cfs by the District. Given the estimated volume of saltwater introduced to the lake, at an inflow rate equal to the estimated post- hurricane freshwater inflow rate, Bay County's expert, Dr. Miller, estimated it would take at least two weeks to reduce salinity in the lake to drinkable levels. The inflow rate, however, is not certain. Dr. Miller estimated it is reasonable to expect that it could take anywhere from two weeks to two months for the lake to recover from the saltwater intrusion depending on the variation in the inflow rate. Nonetheless, Dr. Miller assumed that the saltwater from storm surge entering the Reservoir would mix in a uniform matter. There would be "quite a bit of mixing in a storm," tr. 485, of saltwater topping the Dam and freshwater in the Dam. But there would also be stratification due to the sinking of denser saltwater and the rising in the water column of freshwater. The above estimations assume the bridge and Dam remain intact during a major storm. The Dam and tide gates act as a solid barrier, protecting the lake from saltwater in the bay. If rainfall rises in the lake prior to a surge, the tide gates would open to release water, becoming vulnerable to damage or jamming by debris as occurred during Hurricane Opal. In the event of storm surge bringing saltwater into the Reservoir, the opening of the tide gates will assist the Reservoir in reaching chloride levels below 250 ppm provided the tide gates operate properly. Dr. Janicki, an NTC/Knight expert, used the Environmental Fluid Dynamics Code hydrodynamic model ("EFDC Model") to simulate the effects of control structures and water withdrawals on the Reservoir. Taking into consideration the factors Dr. Janicki considered relevant, he predicted that chloride levels, in the event of storm surge from a Category 3 hurricane overtopping the Dam, would only exceed 250 ppm, the drinking water standard, for approximately 3.4 days. Dr. Janicki's prediction, however, was flawed. He added too little saltwater to the lake in the event of contamination from storm surge. He assumed that saltwater would be flushed too soon from the Reservoir following contamination. He did not account for the effects of waves in his model. His model was not in accord with data for Hurricane Opal and the chloride levels near the Dam taken by Bay County after Opal. If the bridge and Dam were severely damaged, more saltwater could enter the lake. With severe damage to the Dam, the Reservoir would be exposed to normal tides. Restoration would not begin until the Dam and bridge had been fully repaired. If an event were catastrophic, the Reservoir could be offline for a lengthy period of time. The Basis for the District's Decision Bay County's reliance on the Reservoir for water for the majority of the population led the District in the mid-1980s to encourage the County to obtain a backup supply. After the District turned down several requests for withdrawals of up to 30 MGD for every day of the year, the District ultimately approved what is reflected in the Permit. The justification for the permitted withdrawal is as a backup supply in the event the Reservoir becomes unavailable and for maintenance of the system and recoupment of its cost. With regard to maintenance, the District attempted to obtain information from Bay County as to appropriate withdrawal limitations. The attempts were abandoned. Despite repeated requests by the District, Bay County did not provide the amount of water needed to be withdrawn for maintenance since it did not have "infrastructure specifics," tr. 552, needed to provide the District with a numeric limit. In contrast to the amount needed for maintenance, the District found Bay County to have demonstrated that it needs 30 MGD when the Reservoir is offline and that it is reasonable for the County to need 30 MGD up to 60 days per year. The District determined that the Bay County's application met the requirements for the issuance of a consumptive use permit found in section 373.221(1)(a)-(c). In determining whether approval of the application is in the public interest, the District did not presume that it is in the public interest on the basis of the designation in the 2008 RWSP of an inland groundwater source as an alternative water supply. The District determined that it is in the public's interest for Bay County to have a reliable and safe water supply source as a backup to the Reservoir irrespective of the statutory presumption. Nonetheless, the District maintains in this proceeding that the presumption applies. The District also applied the 18 criteria test for finding a reasonable-beneficial use found in Florida Administrative Code Rule 62-40.410(a)-(r) and determined that the application should be approved. Petitioners' Case in Opposition Washington County (Petitioner in Case No. 10-2983), NTC/Knight (Petitioner in Case No. 10-2984), and Messrs. Murfee and Lapensohn (Petitioners in Case No. 10-10100) filed individual petitions for formal administrative hearing. Although not identical, the petitions share the similarity that, in essence, each alleges that Bay County failed to establish that the proposed use of water meets the statutory and rule criteria for obtaining a permit for the consumptive use of water. For example, among the many issues listed under the heading "Disputed Issues of Material Fact and Law" in Washington County's Petition for Formal Administrative Hearing is "[w]hether Bay County has provided reasonable assurance that its proposed use of water is a reasonable-beneficial use as defined in section 373.019, Florida Statutes." See p. 5 of the Washington County petition. In like fashion, the Washington County petition and the other two petitions allege that the issues are whether Bay County provided reasonable assurance that it meets the other statutory criteria in section 373.223, and the applicable rule criteria that must be met by an applicant in order for the District to issue a permit for the consumptive use of water. The Petitioners' cases focused on five topics: 1) the limitations of the HGL Model; 2) the likelihood of impacts to wetlands and the failure of the monitoring plan to provide reasonable assurance that the District's monitoring under the plan will succeed in detecting harm to wetlands caused by the withdrawals; 3) the reasonable-beneficial nature of the proposed use of the permit, including the vulnerability of the Reservoir; 4) interference with presently existing legal users; and 5) the feasibility of alternative sources. Bay County and the District offered evidence on rebuttal to meet the Petitioners' cases. Surrebuttal was conducted by Petitioners. Modeling Groundwater models "represent what is happening in very complex physical systems." Tr. 1495. Typically, the data used by models is not sufficient to obtain a completely accurate representation. The models depend on specific data points such as information from boreholes or water level measurements that do not reveal everything that is occurring in the complex system and, therefore, are not enough to support completely accurate model predictions. As explained by Dr. Guvanasen, Bay County and the District's expert, in order to reach a representation of the entire system when the data available from boreholes and measurements is insufficient, which is typically the case, the modeler must "extrapolate a lot of information and use other knowledge of other events." Id. The "knowledge of other events" that the HGL Model used included Dr. Scott's knowledge of the karst environment in the Panhandle of Florida, the mapping of Bay and Washington County geology by the Florida Geological Society, and Dr. Upchurch's knowledge of karst topography. The HGL results of the available data and the extrapolations were placed into a mathematical model (the HGL Model) that considered the withdrawals at issue to determine the response of the system to the additional stress of the withdrawals. Mathematical models like the HGL Model lead to "non- unique solutions" in which "no model . . . is exactly 100 percent correct . . . ." Tr. 1635. Modeling results, therefore, are subject to changes as additional data is collected that demand a better representation than the model provided prior to the data's collection and analysis. HGL Modeling for this case provides examples of non- unique solutions. HGL "built a model twice . . . and got two different sets of answers." Tr. 1633. Besides the recommendation that more data be obtained after the first HGL Model results, the model was not satisfactorily calibrated and the model was recalibrated for the Revised HGL Modeling results. Mr. Davis, NTC/Knight's expert, conducted additional modeling work (the "Davis Modeling"). Using the HGL Model and additional data concerning the NTC/Knight Property, Mr. Davis found drawdowns would occur over a similar but greater area than shown in the 2011 Revised HGL Modeling Report. (Compare NTC/Knight Ex. 31 at 2 to Joint Ex. Vol. III, Tab P, Figure 51b(1).) The Davis Modeling drawdowns, moreover, ranged up to 0.8 feet, 60 percent more than the 0.5 feet determined by the second HGL Modeling results. In the area of Big Blue Lake, for example, the drawdown contours produced by the Davis Model were either 0.6 feet or 0.7 feet, 20 to 40 percent more than the 0.5 feet produced by the second HGL Modeling results. See NTC/Knight Ex. 31 at 2. Asked to rank the modeling results between the first HGL Model run, the second HGL Model run, and his own results, Mr. Davis was unable to say which was better because of the sparseness of the data. Mr. Davis opined that he could conduct another "dozen more model runs," but without additional data he would be "hard pressed" to be able to say which run was more accurate. Tr. 1633. In Mr. Davis' opinion there remain significant uncertainties that cannot be resolved without more data. Inadequate data "precludes . . . reasonable assurance as to exactly where the impacts will travel and exactly what the magnitude of those impacts will be . . . ." Tr. 1637. Ecological Impacts Bruce A. Pruitt, Ph.D., was accepted as an expert in hydrology, soil science, fluvial geomorphology, and wetland sciences. Dr. Pruitt mapped the soil types on the NTC/Knight Property using the Natural Resource Conservation Service ("NRCS") Web Soil Survey and tested soil types by hand-auguring in wetland areas. He characterized the various soil-types on the property by drainage class (relative wetness of the soil under natural conditions) and hydraulic conductivity (permeability). Dr. Pruitt ranked the vulnerability of wetlands within the zone of drawdown predicted by the HGL Model as "very high," "high," or "moderate." The categories were based on the presence of threatened and endangered species, Florida Natural Area Inventor ("FNAI") habitat designation, and the hydrology of the wetland. He assumed that if the water level in the Surficial Aquifer were to be drawn down by 0.3 feet or 0.4 feet then the water level in the seepage bogs at Botheration Creek would be drawn down by the same amount. Wetlands with a vulnerability classification of "very high" will suffer an adverse impact at a drawdown level of 0.2 feet; those at "high" at 0.3 feet and those at "moderate" at 0.5 feet in times of drought. Dr. Pruitt calculated wetland acreage by type using the Florida Cover Classification System. He assigned vulnerability rating for the wetlands within the Surficial Aquifer drawdown contours generated by the HGL Model. Based on Dr. Pruitt's calculations, a total of approximately 4,200 acres of wetlands are likely to be harmed by the predicted drawdown. A majority of these wetlands are located in Washington County. Based on Dr. Pruitt's analysis, it is likely that the NTC/Knight Property contains 1,981 acres of "very highly" vulnerable wetlands; 1,895 acres of "highly" vulnerable wetlands; and 390 acres of "moderately" vulnerable wetlands, which are likely to be harmed by the drawdown in times of drought. In reaching his opinion about the quantification of acres of wetlands likely to be harmed, Dr. Pruitt applied the Florida Uniform Mitigation Assessment Method ("UMAM"). UMAM was designed to address compensatory mitigation in dredge and fill cases. It was not designed for consumptive water use cases. In contrast and damaging to its case of reasonable assurance that natural systems will not be significantly affected, the District did not conduct an analysis to determine loss of wetland function resulting from operation under the Permit. Nor did it determine how much drawdown the affected wetlands could tolerate before they were harmed. Rather than conducting such an analysis, the District chose to rely on implementation of the LTEMP to cure any harm that might be down by drawdown to the Surficial Aquifer. The District and Bay County's wetland scientists opined that there might be a less permeable restrictive layer maintaining water levels above the Surficial Aquifer on the NTC/Knight Property. Dr. Pruitt acknowledged that the NTC/Knight Property had scattered clay layers beneath the surface. It is possible, therefore, that some of the wetland areas he identified as subject to harm have restrictive features under them which would hold water and resist dehydration. In his hand-auguring, however, Dr. Pruitt found no evidence of a less permeable layer. The auguring only went to a depth of three feet and would have to go to a depth of two meters to be definitive. Furthermore, Dr. Pruitt found no evidence of a less permeable layer from well drillings. The District and Bay County did not prove that there is, in fact, such a restrictive layer. NTC/Knight collected water-level data from shallow hand-augured wells and stage recorders at the Botheration Creek Hillside Seepage Bog. The data demonstrate that the water level in the shallow, hand-augured wells at the Botheration Creek Bog is a direct reflection of the level of the Surficial Aquifer. The Surficial Aquifer at the Botheration Creek Bog was approximately 95.5 feet NAVD, over 35 feet higher than at Big Blue Lake and the highest measured level south of Big Blue Lake. The Botheration Creek Hillside Seepage Bog is located between the 0.3 and 0.4 foot Surficial Aquifer drawdown contours predicted by the HGL Model. Based on the HGL Model, the District and Bay County's experts estimated the Surficial Aquifer drawdown at this bog would be 0.39 feet. During the approximately one year of NTC/Knight's water-level recording, a drawdown of 0.39 feet would have reduced the frequency and duration of inundation at this bog significantly. For example, an analysis of the approximately one year of data collected by NTC/Knight shows that at the intermediate water-level recorder location in the bog, one 29-day period of inundation would have been reduced to just nine days and that further down gradient in the bog, none of the five instances when the bog was inundated would have occurred. This is consistent with Dr. Pruitt's vulnerability assessment, which finds that the vulnerability of the hillside seepage bogs to drawdown is "very high," that is, these systems are likely to be harmed in times of drought at drawdown levels in the Surficial Aquifer of 0.2 feet or greater. A drawdown of 0.3-0.4 feet in the Surficial Aquifer at the hillside seepage bog along Botheration Creek increases the likelihood that the hillside seepage bogs along Botheration Creek will be lost in times of drought. The littoral shelves of Sand Hill Lakes typically occur along a low gradient above the normal low water level of the lakes. The existence of the shelf promotes seepage sheet flow along a wide expanse. The drawdown will change the flow from seepage sheet flow to concentrated stream flow within gullies. The erosion and increased sedimentation produced by the greater force of the water in the gullies will cause a loss of area needed by certain seepage dependent plants and animals. If Big Blue Lake were to be drawn down by the 0.71 feet predicted by Mr. Davis, the location of the seepage would move down 0.71 feet vertically and an estimated 24.5 feet horizontally. The result would be a reduction in the littoral shelf conducive to seepage-dependent plant communities by approximately nine acres. The impact would likely be significant since the seepage zone is in an area of "very high" vulnerability according to Dr. Pruitt. Between October 2010 and July 2011, NTC/Knight took four measurements of water level at "BCS-01," a stage recorder in Botheration Creek. The measurements showed the water level in the creek at that point to be 0.1 to 0.32 feet. NTC/Knight also sampled for taxa of macroinvertebrates in the reach of the creek. NTC/Knight identified 46 taxa, including mussels and six long-lived taxa. The presence of the long-lived taxa and mussels indicate that the reach of the creek in the vicinity of the stage recorder should be considered to be a perennial stream. Botheration Creek is high-quality water and, as shown by NTC/Knight's sampling, it contains a diverse mix of aquatic invertebrates and fish. A drop in the level of Botheration Creek of 0.2 feet predicted by the HGL Model would have caused the creek to go dry at BCA-01 during three of the four dates on which the water level was measured. Such a drop would convert the reach of the creek in the vicinity of the stage recorder from a perennial to an intermittent stream and would eliminate the reach's viability for long-lived taxa. Similarly, upstream reaches that are intermittent would become ephemeral (streams that flow only during periods of high rainfall). If the Wellfield becomes fully operational as allowed by the Permit, there will be a reduction in the Surficial Aquifer at Botheration Creek of between 0.2 and 0.3 feet. The reduction in the aquifer will reduce flow in Botheration Creek, reduce the volume downstream, including in Pine Log Creek, and reduce out-of-bank flood frequency and duration. The result will be a reduction in nutrients delivered downstream and to the floodplain to the detriment of plants and animal life that depend on them. Additionally, other reaches of the creek that have perennial flow will be converted to intermittent streams and reaches that are intermittent will become ephemeral. The result will be the elimination of plant and animal species currently living in these portions of the creek. The impact of the HGL Model predicted drawdown to steepheads depends on the individual steephead and the drawdown contour at its location and the amount of rainfall. Four steepheads on the NTC/Knight Property could suffer impacts similar to the impact at Russ Steephead to which Dr. Pruitt assigned a high probability of impact. Russ Steephead is located on the NTC/Knight Property above Russ Pond. NTC/Knight installed Surficial Aquifer wells at Russ Steephead between the HGL Model's predicted 0.5 and 0.6 foot Surficial Aquifer drawdown contours. NTC/Knight also installed a stage recorder just downstream from the steephead. During drought, NTC/Knight observed a loss of flow from the sidewall seepage areas and in the Russ Steephead Stream. If the Surficial Aquifer at Russ Pond were to be drawn down by 0.5-0.6 feet, the sidewalls of the Russ Steephead Stream and the stream itself would lose flow in times of drought. The loss of flow would lead to oxidation and loss of organic materials in the stream channel and flood plain, resulting in soil subsidence. If the water level at the terminus of the Russ Steephead Stream were drawn down, headward down cutting in the stream channel would be induced. In such a case, in the words of Dr. Pruitt, "there is a high probability that if drawdown occurs and . . . over a long period of time," the process will make the steephead "look more like a gully . . . ." Tr. 2120. The drawdown will also reduce the frequency and duration of inundation of the sphagnum bogs in the four steepheads likely to be affected by the drawdown. The bogs and the associated animals that depend upon them would be lost. Dr. Means identified a number of temporary ponds within HGL's predicted drawdown of the Surficial Aquifer. Nine were between the 0.3 and 0.6 foot drawdown contour, and two were between the 0.6 and 0.7 foot drawdown contours. These ponds and plant and animal communities dependent upon them would likely be harmed by the drawdowns. Mr. Cantrell offered testimony to rebut the Petitioners' case on wetland impacts. His testimony was based on an evaluation of aerial photography, site visits to the Wellfield, and a one-day trip to the NTC/Knight Property. It is Mr. Cantrell's opinion that if the NTC/Knight Property were to drain, it would be because of a surface water drainage system, such as ditching, not because of drawdown in the Surficial Aquifer caused by operation of the Wellfield. Mr. Cantrell's opinion is that because the Area has been subjected to a wide range of fluctuations in water levels and the wetland systems have survived, operation of the Wellfield will not have significant impacts. Mr. Cantrell's opinion, however, overlooks the effect of constant drawdown during times of severe drought. That wetlands have survived severe drought in the past does not mean they will survive severe drought conditions exacerbated by drawdown caused by operation of the Wellfield. Monitoring Special condition 19 of the Permit requires Bay County to implement the LTEMP after the Permit is issued. The LTEMP requires Bay County to establish a monitoring network, but does not provide the location of any particular monitoring site. Sites identified in the LTEMP are recommended, but the ability to use a particular site is dependent on field verification of suitability and authorization by the landowner. Over half the area designated in the LTEMP from the HGL Model's projected 0.5 foot drawdown in the Surficial Aquifer is located on the NTC/Knight Property. It will be necessary, therefore, to include sites on the NTC/Knight Property in the ultimate environmental monitoring network. The LTEMP's recommended sites do not include monitoring of some of the most susceptible wetland systems: temporary ponds, the Botheration Creek hillside seepage bogs, and the perennial headwaters of Botheration Creek. Without this monitoring, the LTEMP will be unable to detect whether these systems are harmed by withdrawals. The Permit and LTEMP require no more than one-year of baseline data to be collected prior to initiation of water withdrawals. The proposed monitoring time is inadequate to create a sufficient record for use in determining whether a reduction in water levels is attributable to water withdrawals or natural phenomena, such as drought. Baseline monitoring should be conducted for a sufficient duration to ensure that a full range of wet and dry years is captured. The LTEMP describes the types of data that are to be collected. A missing component is sampling for frogs, salamanders, and other amphibians that are sensitive to changes in hydrologic regimes and which depend upon infrequent periods of inundation in order to breed. This type of faunal sampling is particularly important in the temporary ponds and seepage environments. Without sampling for the presence of these species, the LTEMP will be unable to determine whether these populations have been harmed by withdrawals. The LTEMP includes a number of "triggers," that if tripped, require the preparation of an auxiliary report. A number of these triggers make reference to changes in water levels at the level of "significant deviation," an undefined term. More importantly, the LTEMP fails to require any statistical analysis. Without it, the LTEMP will be inadequate to establish whether a reduction in water levels is caused by water withdrawals or another cause. Similarly, other triggers lack sufficient detail to determine when they are tripped, such as those that refer to downward movement of plants. Finally, even if one of these triggers is tripped and an auxiliary report is prepared, nothing in the Permit or LTEMP sets forth the circumstances under which withdrawals would need to be curtailed and by what amount. The purpose of the LTEMP is to determine whether withdrawals are causing harm to the wetlands within the vicinity of the Wellfield. The LTEMP fails to provide reasonable assurance that it will succeed in achieving its purpose. Reasonable-Beneficial Use Use if the Reservoir is Unavailable In the event of Reservoir unavailability, Bay County is likely to need much less than 30 MGD. The need is likely to fall between 7.42 MGD and 9.71 MGD for the current population. In 2013, the need is likely to fall between 9.40 MGD and 12.29 MGD. See NTC/Knight Ex. 5, p. 4 of 4. The Permit, however, does not limit Bay County to emergency or backup use. While Bay County might voluntarily limit withdrawals to emergency use or backup supply, it has unfettered discretion to determine what constitutes an emergency or the necessity for a backup supply. The Permit is also not restricted to essential uses. Authorization of 30 MGD provides more than Bay County's current average daily demand for potable water. If the Permit restricted the use to essential uses, the authorization would be far less than 30 MDG. The District commissioned King Engineering to assist in development of a "Coastal Water Systems Interconnect Project" (the "Interconnect Project"). On average, the utilities subject to the Interconnect Project estimated that 42 percent of the average daily demand is dedicated to essential uses with the remaining 58 percent going to non-essential uses. Consistent with the estimate, the Project set a target of 50 percent of average daily demand to be allowed for use in an emergency. None of the information from the Interconnect Project, however, was used by the District in setting the limits of withdrawal in the Permit. b. Daily Use Bay County claims the 5 MGD annual average allocation under the Permit is needed for several reasons, principally the maintenance of pumps. Bay County's justification for 5 MGD is found in testimony from Mr. Lackemacher and a document he authored entitled, "Confidential Draft for Internal Use Only 5 MGD Pumping Rate" (the "Lackemacher Confidential Draft"), admitted as Bay County Ex. 24. Mr. Lackemacher's testimony follows: A. The fact is that there are no absolute knowns when we're talking about what needs to be. Q. What do you mean? A. Well, here we have a document [Bay County Ex. 24] where I talk about rationalization for 5 million gallons a day, why we would need it, mechanical reasons, financial reasons, regulatory reasons. I always felt that it was very difficult to justify a number. I don't know. We haven't designed the system. We haven't got all of the wells in. We don't know what their specific yields are. There's unknowns here. So do we need 2 million gallons a day or 5 million gallons a day? I don't know. I don't know that. But here is the rationalization for 5 million if that's in fact what we need. We may very well find out that we don't need 5 million gallons a day. Q. Is that because you don't know the precise locations of the well and how they're going to be piped and distributed? A. That's absolutely true. Q. Well, did you in this report, Exhibit 24, did you make some reasonable assumptions? A. I based it on some of the values as you discussed or as I pointed out earlier from Hatch Mott MacDonald's preliminary design. * * * Q. And do you feel confident that your analysis supported that in the area of 5 million gallons a day is what would be needed to operate the wellfield? A. Yes. And that's why the paper was generated that [is] a justification for 5 million gallons a day, here's what we think we would need. Tr. 209-10. The Lackemacher Confidential Draft is a one-page, written justification for the 5 MGD. Based on the Hatch Mott McDonald Report, see tr. 210, it considers regulatory, mechanical and financial factors. It is not supported, however, by engineering analysis. Any financial analysis found in the Hatch Mott McDonald Report, moreover, is far from complete. The factors taken into consideration are recited in the most general of terms. For example, of four such factors, the document lists the second as: "All water pumps are designed to run - turning pumps on and off is not the best situation for the overall electrical efficiency or the mechanicals of a pump." Bay County Ex. 24. Consistent with Mr. Lackemacher's testimony, the document concludes that the amount of water needed to run each well is unknown. The financial justification is based on costs shown in the Hatch Mott MacDonald Report for construction and operation of 22 wells, ten more wells than are contained in the Wellfield and without any analysis of revenue to recoup the costs. The financial justification is a bare conclusion on the part of Mr. Lackemacher: We cannot afford to operate a well field at a financial loss, based on this fact alone we would have to pump a minimum of 4.49 MGD. Combined with the fact that we don't know what volumes of water have to be turned over to ensure water quality 5 MGD seems quite reasonable. Bay County Ex. 24. The Lackemacher Confidential Draft is dated May 17, 2011. It was not part of Bay County's Application nor was it submitted to the District prior to the decision to issue the Permit. Although the District attempted to obtain information from Bay County about what was needed for maintenance, Bay County did not provide it. As Mr. Gowans testified, "[t]hen I finally told staff, [s]top asking, we're not going to get the numbers . . . ." Tr. 552. The District performed no analysis to determine the minimum amount of water needed to maintain the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Phillip Waller, an engineer accepted as an expert in the design and construction of potable water systems, including groundwater wells, surface water, and transmission and distribution of drinking water. Mr. Waller testified that if the wells were connected to a central treatment system, there would not be the need to flush the pipeline for disinfection prior to use of the well in an emergency. Only 2.4 million gallons per year or 6,500 gallons per day would be needed to maintain optimum operating conditions, an amount far less than 5 MGD. Mr. Waller's experience when groundwater is used as a backup, moreover, is that they are operated periodically. While prudent to periodically operate backup wells especially in advance of hurricane season, vertical pumps in wells, unlike horizontal pumps, do not have a need for frequent operation because of even force distribution. They certainly do not need to be continuously operated. "In fact, wells routinely are idle for months at a time." Tr. 1123. Interference with Existing Legal Users In its Revised Staff Report dated July 18, 2011, the District wrote: Nearby Users: Under the most intensive pumping activity, drawdown in the Upper Floridan Aquifer is predicted to be approximately 15 feet in the vicinity of the nearest private wells. Water level declines of this magnitude may cause water levels to fall below the level of the pump intake in some privately-owned wells. Joint Ex. Vol. IV, Tab Q, p. 4. The District's high estimate of the number of wells used by existing legal users that might suffer impacts approaches 900. The exact number or whether any existing legal users would be likely to suffer impacts was not proven. Alternatives Groundwater wells, if installed and attached to the fitting in the existing transmission line that delivers water from the Pump Station to the Water Treatment Plant, could serve as backup to the Reservoir. Bay County did not conduct a study of whether groundwater in the area of the transmission line was adequate to serve as an alternative. Mr. Waller, on behalf of NTC/Knight and Washington County, on the other hand, testified that the transmission line could support ten wells with a capacity of 10 MGD and could be constructed at a cost of $12 million, far less than the Wellfield. The area of the transmission line is in an area identified by the District as acceptable for the creation of potable water wells. The area does not present a significant risk of saltwater intrusion if not used continuously. The water meets the drinking water requirements for the Department of Environmental Protection and the Department of Health. The existing transmission line alternative is located near the existing raw water supply line which minimizes the need for additional piping. There is sufficient length along the existing raw water pipeline to accommodate ten wells. The existing transmission line alternative, therefore, has significant potential to succeed as a water supply backup to the Reservoir. NTC/Knight and Washington County, through Mr. Waller, also proposed another alternative: an intake at Bayou George. Near Highway 231, the main pipeline from the intake would run along public right-of-way. North of the existing intake in Williams Bayou and three miles north of the Dam, the proposed intake would be less susceptible to contamination from storm surge. Neither Bay County nor the District presented a thorough analysis of any alternative to the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Mr. Waller that there are two alternatives that could be constructed at much less cost than the Wellfield and that have significant potential of providing backup supply.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Northwest Florida Water Management District enter a final order that denies the application of Bay County for the individual water use permit at issue in this proceeding. DONE AND ENTERED this 26th day of July, 2012, in Tallahassee, Leon County, Florida. S DAVID M. MALONEY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 26th day of July, 2012.
Findings Of Fact Application 7500165 requested average withdrawal of water of 1,804,750 gallons per day from 4 wells located about a mile east of Highway 41 and a mile north of Apollo Beach. The four wells would be for irrigation of tomato crops on total acreage of 4 acres located in Hillsborough County (Exhibit 1, Testimony of Elsberry and Boatwright). Notice of hearing as to the application was published in a newspaper of general circulation in accordance with statute and rule (Exhibit 3). A letter of objection from Joseph S. Benham, Apollo Beach, Florida, dated November 19, 1975 was submitted to the Water Management District, wherein he expressed concern regarding water shortages and, although he does not seek to totally deny the application, is of the belief that the district must insure sufficient controls and management of irrigation activities so that resources are not wasted, water runoff to drainage ditches is eliminated and renewed justification is given each year for the withdrawal (Exhibit 2). A representative of the District staff established that there would be no violation of statutory or regulatory requirement for issuance of a consumptive water use permit in this case except as to the fact that potentiometric level of the applicant's property would be lowered below sea level as a result of withdrawal. It was agreed at the hearing that a period of thirty days should be granted both parties to formulate a stipulation as to control of runoff. An unsigned stipulation was received from the Water Management District by the hearing officer on March 1, 1976, which provided that the permit would be granted with the following stipulations: Runoff from the property will be limited to 25 percent of the quantity pumped and by December 31, 1980 shall be reduced to 16.5 percent of the quantity pumped. The District may at its own expense install metering devices for the purpose of monitoring runoff. The permittee will be notified in advance of such action. The Permit will expire on December 31, 1980. (Testimony of Boatwright, Exhibit 4).
Recommendation That application 8500165 submitted by Elsberry and Elsberry, Inc. Route 2, Box 70 Ruskin, Florida, for a consumptive water use permit be granted with the conditions as follow: Runoff from the property will be limited to 25 percent of the quantity pumped and by December 31, 1980 shall be reduced to 16.5 percent of the quantity pumped. The District may at its own expenseinstall metering devices for the purpose of monitoring runoff. The permittee will be notified in advance of such action. The Permit will expire on December 31, 1980. That the Board grant an exception to the provision of Rule 16J- 2.11(4)(e), F.A.C., for good cause shown. DONE and ENTERED this 15th day of March, 1976, in Tallahassee, Florida. THOMAS C. OLDHAM Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Southwest Florida Water Management District Post Office Box 457 Brooksville, Florida 33512 Elsberry & Elsberry, Inc. Route 2, Box 70 Ruskin, Florida
The Issue The matter to be resolved by this Recommended Order concerns the Petitioner's Notice of Violation and Order of Corrective Action filed against the Respondent on the subject of alleged violations by the Respondent of the "Florida Safe Drinking Water Act", Sections 403.850 through 403.864, Florida Statutes. Within this complaint document there are six counts constituted of the following allegations: Count I. The Respondent does not continually apply effective disinfection measures to the water distributed to the service connections of the Respondent's water system. Respondent's water system has chlorination equipment installed but a chlorine residual is not continually maintained. This condition has existed since at least February, 1979. These facts show a violation of Rule 17- 22.106(3)(c), Florida Administrative Code. Count II. The Department has not received reports from the Respondent which contain information about the operation and maintenance of the water system. This condition has existed since at least April, 1978. These facts show a violation of Rule 17-22.111(2), Florida Administrative Code. Count III. The Respondent's water system has a daily flow of more than 2,500 gallons per day but less than 0.1 million gallons per day. The operation, maintenance and supervision, if any, of the water system is not performed by a person who has passed an examination that entitled such person to be a certified operator. This condition has existed since at least April, 1978. These facts show a violation of Rule 17-22.107(3)(b), Florida Administrative Code. Count IV. The slab surrounding the well casing has been broken exposing the system to possible contamination. This condition has existed since at least February, 1979. These facts show a violation of Rule 17-22.106(2)(c)2.e., Florida Administrative Code. Count V. The Respondent`s water system has no flow meter for accurately measuring the volume of water distributed by the public water system. This condition has existed since at least February, 1979. These facts show a violation of Rule 17-22.106(3)(g), Florida Administrative Code. Count VI. The Petitioner has incurred costs and expenses in the amount of $57.22 in the course of investigating the case and is entitled to be reimbursed pursuant to Subsection 403.860(3), Florida Statutes.
Findings Of Fact This case is presented for consideration based upon the Notice of Violation and Order of Correction filed by the Secretary of the State of Florida, Department of Environmental Regulation, on August 24, 1979. The action is taken against Arnold H. Parker, an individual who resides in Escambia County, Florida. On September 17, 1979, the Respondent, Parker, by and through his counsel answered the allegations of the Petitioner and requested a Subsection 120.57(1), Florida Statutes, hearing. The request for hearing was granted and on December 6, 1979, in Florida, a formal hearing was held to consider the Petitioner's complaint. (The essential elements of that complaint are reflected in the synopsis reported in the Issue statement of this Recommended Order.) The facts reveal that Daniel C. Walker, an employee of Petitioner, went to Perdido Key, Escambia County, Florida, in February, 1979, for the purpose of inspecting a water system owned and operated by the Respondent and to ascertain the number of service connections associated with the system. When Walker arrived at the location of the Respondent's well, he observed that the above-ground equipment utilized in pumping the water out of the ground was housed in a building. This building had a hole in the roof and the concrete slab surrounding the well casing was broken at the surface allowing for possible contamination by influent. At the time of the inspection a device for introducing chlorine into the extracted water was noted but that device was not connected and no chlorine residual was found in the water system. The water system was not being operated by a certified operator within the meaning of Rule 17-22.107(3)(b), Florida Administrative Code. In addition, the Respondent had not submitted operational reports to the Petitioner since April, 1978. The reports referred to are those reports required by Rule 17- 22.111(2), Florida Administrative Code. While Walker was at the general location of the well in onestion, he observed forty individual lots on which various types of trailers, campers and mobile homes could be found. Walker did not determine if persons were living in these shelters and he does not recall seeing persons in the area of the lots. The witness, Walker, did not observe any restaurant or public food establishment in the area of the well house and lots. On September 25, 1979, Robert Court, another employee of the Petitioner, went to the site of the well house and lots. At that time he counted thirty-two trailers, campers and mobile homes and each of those shelters had a service connection from the well of the Respondent located somewhere on the lot where the shelter was found. The service connection was in the form of a spigot. Court observed several people in the north-east section of the general area which is constituted of the well location and lots. Court returned to the location on November 30, 1979, and in a random survey saw approximately thirty-two trailers, campers and mobile hones. Subsequent to the visits of the employees, the Notice of Violation and Order of Correction was prepared by the enforcement section of the Petitioner and the cost of that preparation was $57.22. The Respondent, Arnold H. Parker, testified in the course of the hearing and his testimony established that there are nine persons who live in the area of the well on a year-round basis and these persons are served by the well during that period of time. Of the nine persons one family, the family of the Respondent, lives in a mobile home and the family is constituted of three persons, the Respondent, his wife and son. In a second mobile home the Respondent's daughter and her husband are found to reside. The final group of persons constituted of the nine full-time residents are the Respondent's daughter, her husband and two children in a third mobile home. Each lot on which the three mobile homes are found is served by a service connection. The remaining lots at the location in question were subdivided approximately two years prior to the hearing date and sold separately with the exception of the three lots where the nine permanent residents reside and two lots where other children of the Respondent resided prior to the February, 1979, inspection by the Petitioner's employee. Respondant sold twenty-four mobile home lots and twelve camper sites to persons other than family members and each of the mobile home lots and camper sites has a service connection to the well. Those persons who use the water system other than the nine permanent residents, use the system from mid-March through mid-September in the calendar year. During that time of usage, there are two families at two separate lots who come down during the week and use the water supply. The number of members in those families was not indicated in the course of the hearing. The balance of the persons using the water supply, excluding the above-mentioned two families and the nine permanent residents, use the shelters for vacation purposes and on the weekend. Some of this latter group would be vacationing in their summer home for a period as long as two weeks. The highest number of persons using the water from the well during the vacation period would be approximately forty persons during holiday weekends in the vacation cycle. From the testimony of the Respondent there would never be more than ten days during the vacation period in which twenty-five or more persons would be utilizing the water supply from the well. The water is brought into the trailers, campers and mobile hones by hoses attached to the spigot service connections and the hoses are removed when the individual owners are not in attendance. The lot owners who are served by the water system of the Respondent pay a fee of $18.00 a year, which the Respondent uses to repair the well pump, for pipe and for the cost of electricity to run the well. The well generating device is a two-horsepower electric pump and the well source is tapped by a two-inch service pipe. A one-half-inch line runs from the main to the service connectors (spigot). After the inspection of February, 1979, the Respondent repaired the broken slab around the well casing and these repairs were made in March or April, 1979. The repairs were depicted in the Respondent's Exhibits 1 and 2 admitted into evidence which are photographs of the well casing after the repair.
Recommendation It is recommended that the action taken by the Petitioner against Respondent pursuant to the Notice of Violation and the Order for Corrective Action be dismissed, to include the Petitioner's claim for costs and expenses. DONE AND ENTERED this 7th day of January, 1980, in Tallahassee, Florida. CHARLES C. ADAMS, Hearing Officer Division of Administrative Hearings Room 101, Collins Building Tallahassee, Florida 32301 (904) 488-9675 COPIES FURNISHED: William Hyde, Esquire Department of Environmental Regulation 2600 Blair Stone Read Tallahassee, Florida 32301 Barne J. Morain, Esquire 113 North Palafox Street Pensacola, Florida 32501
The Issue The issues for determination in this case are whether Respondent Jeffrey Hill should pay the administrative penalty and investigative costs, and should undertake the corrective actions that are demanded by the Florida Department of Environmental Protection (“Department”) in its Notice of Violation, Orders for Corrective Action, and Civil Penalty Assessment (“NOV”).
Findings Of Fact Respondent is the owner and operator of a community water system and its associated piping, designated PWS No. 2124409, located on parcel ID No. 03-4S-17-07486-001 on Country Club Road, in Lake City, Columbia County, Florida (“the property”). Respondent is a “person” as defined in section 403.852(5), Florida Statutes. Respondent is a “supplier of water” as defined in section 403.852(8). The water system is a “public water system” and a “community water system” as defined in sections 403.852(2) and (3), respectively. The community water system is a Category V, Class D water system with a capacity of 28,800 gallons per day that supplies between 25 and 3,300 people, using groundwater as its source. Count I Count I of the NOV charges Respondent with failure to sample for nitrate and nitrite in 2012 and 2013, which was admitted by Respondent. Count II Count II of the NOV charges Respondent with failure to sample for primary inorganic contaminants for the 2011-2013 compliance period, which was admitted by Respondent. Count III Count III of the NOV charges Respondent with failure to analyze for secondary contaminants in the 2011-2013 compliance period, which was admitted by Respondent. Count IV Count IV of the NOV charges Respondent with failure to sample for volatile organic contaminants in the 2011-2013 compliance period, which was admitted by Respondent. Count V Count V of the NOV charges Respondent with failure to sample for synthetic organic contaminants in the 2011-2013 compliance period, which was admitted by Respondent. Count VI Count VI of the NOV charges Respondent with failure to sample for total coliform from June 2013 to date, which was admitted by Respondent. Count VII Count VII of the NOV charges Respondent with failure to employ an operator for the system since May 2013, which was admitted by Respondent. Count VIII Count VIII of the NOV charges Respondent with failure to submit test results required by Florida Administrative Code Chapter 62-550, and failure to file a monthly operation report since April 2013, which was admitted by Respondent. Count IX Count IX of the NOV charges Respondent with failure to issue Tier 3 notices in May 2013 and March 2014, advising customers of the failure to monitor for certain contaminants, which Respondent admitted. Count X Count X of the NOV charges Respondent with failure to provide a consumer confidence report to his customers in 2012 and 2013, which was admitted by Respondent. Count XI In Count XI of the NOV, the Department states that it incurred $530 in investigative costs related to this enforcement matter, which is admitted by Respondent.
The Issue The issue to be determined in this case is whether the City of Tarpon Springs (“City”) is entitled to a industrial wastewater facility permit for its proposed discharge of demineralization concentrate into the Gulf of Mexico adjacent to Pasco County, Florida.
Findings Of Fact The Parties Henry Ross is a resident of Tarpon Springs. In his petition for hearing, he alleges that he is a recreational fisherman and a "consumer of fish taken from the area" where the proposed wastewater discharge would occur. He presented no evidence at the final hearing to prove these allegations. Neither the City or the Department stipulated to facts that would establish Ross's standing. The City of Tarpon Springs is a municipality in Pinellas County and the applicant for the industrial wastewater permit that is challenged by Ross. The Department is the agency charged by law with the duty, and granted the power, to regulate the discharge of pollutants into waters of the State. The Proposed Permit - General Due to the cost of obtaining potable water from Pinellas County Utilities, the City decided to look for another source of drinking water. In February 2004, an alternative water supply plan was developed by the City’s Office of Public Services which analyzed potable water supply options. It determined that the withdrawal and treatment of brackish groundwater represented the best option for the City. The proposed permit authorizes the City to discharge industrial wastewater into waters of the State. The wastewater is demineralization concentrate, which is produced when RO technology is used to remove salts from brackish water to convert it to potable water. The wastewater would be produced in conjunction with the operation of a not-yet-constructed WTP that would supply public drinking water to the residents of the City. The City must also obtain a consumptive use permit from the Southwest Florida Water Management District for the proposed withdrawal of groundwater. Whether the Town is entitled to a consumptive use permit is not at issue in this proceeding. The industrial wastewater permit would authorize a maximum daily discharge of 2.79 million gallons per day ("mgd") of RO concentrate. The initial operation of the WTP, however, is expected to discharge 1.05 mgd. The RO concentrate would be transported via a force main from the WTP in the City to an outfall in Pasco County. The outfall would discharge the wastewater into a canal which is already being used for the discharge of cooling water from Progress Energy Florida, Inc.’s Anclote Power Generation Facility. The outfall would be 50 feet north of the point in the canal where Progress Energy is required to demonstrate compliance with its own permitting requirements, so as not to interfere with Progress Energy's ability to demonstrate compliance. There is a floating barrier in the channel north of the proposed point of discharge, and a fence along the side of the canal, to prevent swimmers, boaters, and persons on foot from getting near the Progress Energy power plant. The floating barrier and fence would also prevent swimmers, boaters, or pedestrians from reaching the proposed discharge outfall and the area of the canal where the discharge will initially mix. After being discharged into the canal, the wastewater would become diluted and flow northward, out of the canal and into the open waters of the Gulf. The prevailing currents in area would most often force the wastewater south toward Pinellas County and the mouth of the Anclote River. To determine the characteristics of the wastewater, the City's consultants collected water from the three proposed well fields for the new WTP and ran the water through a small, pilot-scale RO unit to generate an RO concentrate that is representative of the proposed RO discharge. It was determined that eight constituents of the wastewater would likely be present in concentrations that would exceed applicable state water quality standards: aluminum, copper, iron, gross alpha (a radioactivity measurement), total radium, selenium, nickel, and zinc. The Mixing Zones The Department may authorize mixing zones in which a wastewater discharge is allowed to mix with the receiving waters. See Fla. Admin. Code R. 62-4.244. Within the mixing zone, certain minimum water quality criteria must be met. At the outer boundary of the mixing zone, the applicable state water quality standards must be met. In this case, the water quality standards for Class III marine waters are applicable. The City's consultants analyzed the wastewater, receiving waters, and other factors and used an analytical model to simulate a number of mixing scenarios. In cooperation with Department staff, a separate mixing zone was established for each of the eight constituents that are not expected to meet water quality standards at the outfall. The largest mixing zone, for copper, is 1,483.9 square meters. The smallest mixing zone, for nickel, is 0.7 square meters. The mixing zones are conservatively large to assure sufficient mixing. Under most conditions, the mixing is expected to occur in a smaller area. Toxicity Analysis Among the minimum criteria that must be met within a mixing zone is the requirement to avoid conditions that are acutely toxic. See Fla. Admin Code R. 62-302.500(1)(a). A wastewater discharge is tested for potential acute toxicity by exposing test organisms to the undiluted discharge and determining whether more than 50 percent of the organisms die within a specified time period. The test organisms, mysid shrimp and silverside minnow, are sensitive species. Therefore, when a discharge is not acutely toxic to these organisms, it can be reasonably presumed that the discharge would not harm the native organisms in the receiving waters. The acute toxicity test for the proposed RO concentrate indicated zero toxicity. The Department requested that the City also analyze the potential chronic toxicity of the proposed discharge. A wastewater discharge shows chronic toxicity if exposure to the discharge adversely affects the growth and weight of the test organisms. The tests performed on the representative discharge showed that the proposed discharge of RO concentrate would not create chronic toxicity in the mixing zones. Petitioner’s expert witness, Ann Ney, did not review the toxicity analyses or other water quality data that were submitted to the Department by the City. However, she expressed a general concern about a salty discharge that could create stratification in the canal with higher salinity at the bottom of the canal that might be hypoxic (little or no dissolved oxygen). The more persuasive evidence shows that salinity stratification, or a hypoxic condition, is unlikely to occur. The proposed permit requires the City to conduct quarterly chronic toxicity tests. The permit also requires the City to periodically test the water and sediments for any unexpected cumulative effects of the discharge. Evaluation of Disposal Options Florida Administrative Code Rule 62-620.625(6) requires that an applicant for a permit to discharge demineralization concentrate must investigate disposal options potentially available in the project area. The City evaluated blending the discharge concentrate with the City's re-use water irrigation program or with the City’s domestic wastewater discharge into the Anclote River. The RO concentrate was too salty for irrigation use and there was an inadequate volume of domestic wastewater available throughout the year. In addition, the Anclote River is an Outstanding Florida Water and, therefore, is afforded the highest water quality protection under Department rules. See Fla. Admin. Code R. 62-4.242(2). The City also looked at underground injection but that was economically unreasonable and there was concern about upward migration of the discharge. It was economically unreasonable to discharge the concentrate farther out into the Gulf. Anti-degradation Analysis For a proposed new discharge, a permit applicant must demonstrate that the use of another discharge location, land application, or recycling that would avoid the degradation of water quality is not economically and technologically reasonable. See Fla. Admin. Code R. 62-4.242(1)(d). As discussed above, the City investigated other disposal options, but they were not economically or technologically reasonable. An applicant for a permit authorizing a new discharge must demonstrate that any degradation is desirable under federal standards and under circumstances that are clearly in the public interest. See Fla. Admin. Code R. 62-302.300(17). In determining whether a proposed discharge is desirable under federal standards and under circumstances that are clearly in the public interest, the Department is required by Rule 62-4.242(1)(b) to consider the following factors: Whether the proposed project is important to and is beneficial to public health, safety or welfare (taking into account the policies set forth in Rule 62-302.300, F.A.C., and, if applicable, Rule 62-302.700, F.A.C.); and Whether the proposed discharge will adversely affect conservation of fish and wildlife, including endangered or threatened species, or their habitats; and Whether the proposed discharge will adversely affect the fishing or water-based recreational values or marine productivity in the vicinity of the proposed discharge; and Whether the proposed discharge is consistent with any applicable Surface Water Improvement and Management Plan that has been adopted by a Water Management District and approved by the Department. The proposed project is important to and is beneficial to public health, safety or welfare because it would provide drinking water for the public. In addition, the treatment and use of brackish groundwater converts otherwise unusable water into a valuable resource. The use of brackish water avoids the use of water in the surficial aquifer that is used by natural systems, such as wetlands. The Florida Legislature has found that the demineralization of brackish water is in the public interest, as expressed in Section 403.0882, Florida Statutes (2010): The legislature finds and declares that it is in the public interest to conserve and protect water resources, provide adequate supplies and provide for natural systems, and promote brackish water demineralization as an alternative to withdrawals of freshwater groundwater and surface water by removing institutional barriers to demineralization and, through research, including demonstration projects, to advance water and water by-product treatment technology, sound waste by-product disposal methods, and regional solutions to water resources issues. The proposed discharge would not adversely affect conservation of fish and wildlife. Because the discharge is not toxic to sensitive test organisms provides reasonable assurance that the native fish and other aquatic life would not be adversely affected by the discharge. The only identified threatened or endangered species that frequents the canal waters is the endangered Florida Manatee. Manatees use the canal because of its relatively warm waters. Manatees come to the surface to breathe and they drink fresh water. There is no reason to expect that a manatee moving through the mixing zones would be adversely affected by the RO concentrate. The Florida Fish and Wildlife Conservation Commission, which has primary responsibility for the protection of endangered and threatened species, did not object to the proposed permit. Manatees and many other aquatic species use seagrasses as food or habitat. There are no seagrasses in the area of the canal into which the RO concentrate would be discharged, but there are dense seagrass beds nearby. The proposed discharge would have no effect on the seagrasses in the area. The proposed discharge would not adversely affect fishing or water-based recreational values or marine productivity in the vicinity of the proposed discharge. Because the proposed discharge is non-toxic and would meet Class III water quality standards before reaching the closest areas where humans have access to the canal and Gulf waters, there is no reason to believe that the proposed discharge would be harmful to humans. The proposed discharge would not adversely affect recreational activities, such as swimming, boating, or fishing. Petitioner presented the testimony of two fishermen about fishing resources and water flow in the area, but no evidence was presented to show how the proposed discharge would reduce marine productivity. Petitioner contends that the proposed discharge would adversely affect the Pinellas County Aquatic Preserve. However, the aquatic preserve is two miles away. The proposed discharge would probably be undetectable at that distance. It would have no effect on the waters or other resources of the aquatic preserve. With regard to the requirement that the proposed discharge be consistent with an adopted and approved Surface Water Improvement and Management Plan for the area, there is no such plan.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law it is RECOMMENDED that the Department issue a final order determining that Petitioner lacks standing, and approving the issuance of the industrial wastewater facility permit to the City. DONE AND ENTERED this 16th day of December, 2010, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 16th day of December, 2010. COPIES FURNISHED: Nona R. Schaffner, Esquire Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Station 35 Tallahassee, Florida 32399-3000 Thomas J. Trask, Esquire Frazer, Hubbard, Brandt & Trask, LLP 595 Main Street Dunedin, Florida 34698 Henry Ross 1020 South Florida Avenue Tarpon Springs, Florida 34689 Lea Crandall, Agency Clerk Department of Environmental Protection Douglas Building, Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Tom Beason, General Counsel Department of Environmental Protection Douglas Building, Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Mimi Drew, Secretary Department of Environmental Protection Douglas Building 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000
The Issue This is a procurement protest. The ultimate issue is whether the Respondent’s award of the "Agreement for the Construction and Operation of a Seawater Desalination Plant and Water Purchase Agreement" ("WPA") to Intervenor, S & W Water, LLC ("S&W") on July 19, 1999, is contrary to Tampa Bay Water's (TBW’s) governing statutes, its rules or policies, or the proposal specifications, or is clearly erroneous, contrary to competition, arbitrary, or capricious. Additional issues presented for decision are: (1) whether Petitioner has standing to maintain this protest; and (2) whether, by participating in the procurement process, Petitioner has waived or is estopped from claiming irregularities arising out of that process.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is recommended that TBW enter a Final Order denying Petitioner's Formal Protest. Jurisdiction is reserved for consideration of S&W's request for a determination of improper purpose under Section 120.595(1), Florida Statutes, if such request is made by motion within 10 days from the issuance of this Recommended Order. DONE AND ENTERED this 25th day of October, 1999, in Tallahassee, Leon County, Florida. J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 25th day of October, 1999. COPIES FURNISHED: Charles W. Pittman, Esquire 400 North Tampa Street Suite 1040 Tampa, Florida 33602 Richard A. Harrison, Esquire John W. Wilcox, Esquire Allen, Dell, Frank & Trinkle, P.A. Post Office Box 2111 Barnett Plaza, Suite 1240 101 E. Kennedy Boulevard Tampa, Florida 33601-2111 Donald D. Conn, General Counsel Tampa Bay Water 2535 Landmark Drive Suite 211 Clearwater, Florida 33761-3950 John H. Rains, III, Esquire Annis, Mitchell, Cockey, Edwards & Roehn, P.A. Post Office Box 3433 One Tampa City Center, Suite 2100 Tampa, Florida 33601
Findings Of Fact The parties stipulated, and it is so found, that Petitioner, DER, has jurisdiction over both the issues and the Respondents Dey and KWC. KWC owns and operates a water system which supplies water to both residential and commercial customers in the City of Keystone Heights, Florida. Virginia Key is the President of KWC, a member of the Board of Directors of the corporation, and one of the five stockholders. The other stockholders are her sisters. The five sisters are the daughters of the late G. E Wiggins, and inherited the company from him at his death in 1969. Mr. Wiggins developed the water company in the 1920's and operated it until his death. KWC came under the jurisdiction of the Florida Public Service Commission (PSC) just prior to Mr. Wiggins' death. At that time, pursuant to a PSC requirement, it was assessed and valued at a sum in excess of $250,000.00 by a consultant firm hired for the purpose. As of late November, 1984, KWC served approximately 752 residential customers which, when multiplied by an average 2.5 persons per family factor, results in a total of approximately 1,880 residential inhabitants served by the water system. In addition, the system serves 105 commercial customers. It is impossible to estimate with any reasonable degree of accuracy the number of individuals involved in the commercial service. The system consists of three wells drilled in 1940, 1946, and 1960 to a depth of 350, 450, and 492 feet respectively. Total yield from the three wells is normally 1,350 gallons per minute. The wells are generally well protected against surface water infusion, are normally not subject to inundation, and have had no salt water infiltration problems in the past. At the present time, well number 2, drilled in 1946, with a 350 gpm yield is out of service. The water, when pumped from the ground, is stored in two tanks-one with a 60,000 gallon capacity and the other with a capacity of 800 gallons. Both tanks are steel. Chlorine is added to the water in each storage situation by a hyper-chlori- nation system before the water is sent to the storage tank. The distribution system is made up of 6" and 2" diameter pipe. In March, 1984, two different inspections of the water system, done by, in one case, an environmental specialist and in the other, an Engineer I with DER, revealed several deficiencies in the maintenance and operation of the system all of which constitute violations of DER rules. Specifically, these include (1) failure to provide an auxiliary power source in the event the main pumping capability of the system is lost, (Rule 17-22.106 (3)(a); (2) failure to utilize for the system an operator certi- fied by the state with a Class C license, (Rule 17-22.107(3)(b); (3) failure to maintain a free chlorine residual in the water of at least 0.2 ppm in the system, (Rule 17-22.106(3)(c); (4) failure to maintain a minimum pressure of 20 ppi in the distribution system, (Rule 17-22.106(3)(f); (5) failure to have a gas chlorination facility, (Rule 17-22.106(3)(d); and (6) failure to obtain proper permits to expand the distribution system, (Rule 17-22.108 (1)(b) Rule 17-22, F.A.C., sets up requirements for safe drinking water and was designed to establish guidelines and standards for facilities and water and to bring water into compliance with the Federal Act. Twenty ppi of pressure in the system was adopted as a standard minimum for residual pressure to protect against outside contaminants getting into the water system. Such contaminants could come from ground water, leaks, and water in storage tanks attached to the system such as toilet tanks, being aspirated into the system. Also a certain amount of pressure is required to operate appliances. Normally minimum pressure is found in areas at the edge of the system and in those areas where inadequate chlorination is located. They interact and both pressure and chlorinization are required. Chlorine can be injected into the system generally in two ways: the first is through gas chlori- nation and the second, through hyper-chlorinization as is used in the instant system. The effectiveness of hyper-chlorinization is limited, however, by the size of the system. Basically, hyper- chlorinization is effective when the demand in the system for pressure is no more than 10 ppi. Above this, gas chlorinization is necessary. As late as January 4, 1985, Mr. Dykes went to Keystone Heights to test the system. His tests showed that 11.9 ppi is the average daily flow per 24 hours for the last 12 months. Since this figure is above 10 ppi, in his opinion, a gas chlorinization system would be needed. Chlorine is used to purify water because it has been shown, through long use, to prevent disease. The requirement for a residual chlorine level in water, therefore, is consistent with that concept to insure chlorine is always in the water in sufficient quantity to prevent disease. Respondent's plant has less than the 0.2 residual that is required under the rule. This insufficiency is caused by the inadequate chlorinization system which has insufficient capacity to provide the appropriate amount of chlorine. At the current level, it is providing only approximately 60 percent of the needed chlorine. To correct this deficiency Mr. Dykes recommends installation of a gas chlorinization system. In addition, the pneumatic tank storing the water from the number 3 well does not give sufficient detention time to allow for appropriate reaction of the chlorine contained in the water before the water is released into the distribution system. Another factor relating to the lack of adequate pressure in the system is the fact that, in Mr. Dykes' opinion, too much of the system is made up of 2" diameter water line. A line of this small diameter prevents the maintenance of adequate pressure especially in light of the fact that there are numerous old lines in the system some with corrosion and scale in them which tends to reduce pressure. This latter factor would be prevalent even in the 6" lines. The current plant manager, Mr. Cross, who has been with Respondent for approximately 4 years is, with the exception of one part time employee, the only operations individual associated with the plant. As such, he repairs the meters and the lines, checks the pumps, the chlorinator, and checks and refills the chlorine reservoir on a seven day a week basis. Be learned the operation of the plant from his precedessor, Mr. Johnson, an unlicensed operator who was with the company for 10 years. Mr. Cross has a "D" license which he secured last year after being notified by DER that a license was required. It was necessary for him to get the "D" license before getting the required "C" license. At the present time, he is enrolled to take courses leading toward the "C" license. At the present time, however, he is not, nor is anyone else associated with KWC, holding a license as required. The rule regarding auxiliary power provides that all community systems serving 350 or more persons shall have standby pumping capability or auxiliary power to allow operation of the water treatment unit and pumping capability of approximately one-half the maximum daily system demand. Respondent has admitted that the system is not equipped with an auxiliary power source and it has already been established that more than 350 persons are served by the system. Respondent also admits that subsequent to November 9, 1977, it constructed main water lines for the system which required the obtaining of a permit from either the Petitioner or the county health unit. Respondent admits that it did not obtain or possess a permit to do the additional construction referenced above from either DER or the Clay County Health Department prior to the construction of the water lines referenced. The inspections referenced above, which identified the problems discussed herein, were accomplished by employees of Petitioner, DER, at a stipulated cost of $898.10. Respondent contends, and there is no evidence to the contrary, that there have been no complaints of contaminated water and that the monthly water samples which Mr. Cross forwards to the Clay County Health Department have been satisfactory. Mr. Cross also indicates that a September, 1983 DER analysis of water samples taken from the system was satisfactory. However, bacteriological analysis reports on water collected from Respondent's system on July 11 and 27, 1983, reflect unsatisfactory levels of either coliform or non-coliform bacteria in the water requiring resubmission of test samples. Respondent also contends that no one has ever gotten sick or died from the water furnished by the system and there is, in fact, no evidence to show this is not true. Even though so far as is known, no one has ever been made sick from the water in the system, in Mr. Dykes' opinion, the risk is there. As a result of the defects identified in this system, insufficient chlorine is going into the system to meet reasonable health standards. Though this does not mean that the water is now bad, it does mean that at any time, given a leak or the infusion of some contaminant, the water could become bad quickly, and the standard established by rule is preventive, designed to insure that even in the case of contamination, the water will remain safe and potable. Respondent does not deny that it is and has been in violation of the rules as set out by the Petitioner. It claims, however, that it does not have sufficient funds available to comply with the rules as promulgated by DER. Respondent has recently filed a request for variance under Section 403.854, Florida Statutes, setting forth as the basis for its request that it does not have the present financial ability to comply with any of the suggested or recommended corrective actions to bring its operation into compliance with the rules. Mr. Protheroe, the consulting engineer who testified for Respondent has not evaluated the system personally. His familiarity with it is a result of his perusal of the records of the company and the Petitioner. Based on his limited familiarity with the system, he cannot say with any certainty if it can be brought into compliance with, for example, the 20 ppi requirement. There are too many unknowns. If, however, the central system was found to be in, reasonably good shape, in his opinion, it would take in excess of $100,000.00 to bring it within pressure standards. To do so would require replacement of the 2" lines, looping the lines, and cleaning and replacing some central system lines as well. In his opinion, it would take three months to do a complete and competent analysis of the system's repair needs. Once that was done, he feels it would take an additional three months to bring the plant into compliance with DER requirements. Other repairs, such as those to the lines outside the plant, would take longer because some are located in the downtown area and have interfaced with other utilities. This could take from three to four months if the money were available to start immediately. Here, however, it has been shown that it is not. Consequently, to do the study and then, if possible, procure the funds required, could take well in excess of six months or so. Mr. Protheroe contends, and there is little if any evidence to indicate to the contrary, that to replace the current system with a new one entirely as it is currently constituted would cost at least $250,000.00. However, in his opinion, no one would ever put in a new system similar to the one currently there. He cannot say how much it would cost to buy the system and make the necessary corrections to it to rectify the deficiencies. His familiarity with the system is not sufficiently complete to do this. He cannot say exactly how much the system is worth in its current state, but he is satisfied that it is worth more than $65,000.00. In that regard, Mrs. Dey indicated that in her opinion, the fair market value of the system is currently at $250,000.00. At the present time, there are current outstanding loans in excess of $9,000.00 at 16 percent interest. This current loan basis has been reduced from a higher figure. In 1977, the company borrowed $15,000.00 at 9 percent. In 1981, it borrowed $5,000.00 more at 18 percent. In 1982, the loans were consolidated at an increased rate of 16 percent and the officers have been advised by their current creditors that they cannot borrow any more money for the system in its current state. They would sell the system if a reasonable price could be realized. However, any inquiries on prospective purchases have been chilled by a low rate base assigned by the PSC. In that regard, the City of Keystone Heights offered to purchase the system for $59,000.00. This offer was declined as being unreasonable. Nonetheless, in light of the low rate base assigned by the PSC in its order issued on December 21, 1981 of slightly over $53,000.00 the offer by the city of $59,000.00 is not completely out of line. A certified public accountant, in KWC's December 31, 1983 financial report assigned a valuation of approximately $62,000.00, again a figure only slightly higher than that offered by the city, but substantially less than the $175,000.00 price asked of the city by Respondent Dey and her sisters. Mrs. Dey indicated that to the best of her knowledge the PSC denied rate increases for the purposes of improvements. In the presentation before the commission, respondents relied exclusively on the services of their attorney and accountant. Evidence from Mr. Lowe, of the PSC, however, indicates that KWC has never requested a rate increase to finance any of the improvements called for here. In the PSC order referred to above, Respondent was awarded a 12.25 percent rate of return on its rate base. This figure was an amalgam of a more than 13 percent rate on equity and a lesser figure for cost of doing business, including debt. At the time of that hearing, however, the debt cost was based on a 9 percent interest figure. The 16 percent interest figure came afterwards and no hearing has been requested based on the higher interest rate and it is so found.
Recommendation Based on the foregoing findings of fact and conclusion of law, it is, therefore: RECOMMENDED that Respondents Virginia W. Day and the Keystone Water Company be ordered to comply with the Orders for Corrective Action previously filed herein to bring the water system in question in compliance with the Florida Safe Water Drinking Act without delay or suffer the penalties for non- compliance called for by statute and, in addition, pay costs of investigation in the amount of $898.16. RECOMMENDED in Tallahassee, Florida this 19th day of February, 1985. ARNOLD H. POLLOCK Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 19th day of February, 1987. COPIES FURNISHED: Debra A. Swim, Esquire Assistant General Counsel Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32301 John E Norris, Esquire 10 North Columbia Street Lake City, Florida 32055 Victoria Tschinkel, Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301
The Issue This case presents two questions for consideration. The first question concerns the Petitioners' contention that the grant of the permit at issue must be considered contemporaneously with the matters of file in the application made by the Respondent, The Deltona Corporation, with the Respondent, State of Florida, Department of Environmental Regulation, File No. 64-24208, pending before the Department. From the point of view of the Petitioners, should this contemporaneous review process be afforded, then the current permit would not be granted due to the alleged deficiencies associated with the application, File No. 64-24208. The second question to be answered in this case concerns the dispute between the Respondents on the issue of water quality monitoring as a condition to granting the permit sought herein. The Respondent Department would have the applicant monitor in six lakes in the area of the project and the applicant would restrict its monitoring activity to three lakes in the project area. The Petitioners support the Department in its position on the monitoring question. 1/
Findings Of Fact The Respondent, The Deltona Corporation, has made application with the Respondent, State of Florida, Department of Environmental Regulation, to effect drainage system improvements to a land locked conveyance network which consists of the enlargement and regrading 990 lineal feet of existing channel cross- section and the installation of additional culverts and control structures at road crossings. The project also involves repairs and replacement of a damaged culvert. The work would be accomplished by land based equipment transported to the work site by existing overland routes. The excavated sand fill would be placed on upland property owned by The Deltona Corporation. The details of the project and data related to the geographical area may be found in the Joint Exhibit I admitted into evidence. The date of the application for permit is December 12, 1979. On January 25, 1980, the Department of Environmental Regulation sent out a notice of the pending review by the Department of the permit application. After receipt of that notice, attorney for the Petitioners, on February 12, 1980, wrote to the Department expressing the objection to the project made by property owners in the area of the project site, together with a list of those owners found in an attached Petition of owners' names and addresses. A copy of this letter and attached Petition may be found as Joint Exhibit No. VII admitted into evidence. Subsequent to the receipt of the statement of objections, the Department issued a construction permit dated April 30, 1980, subject to conditions. A copy of this permit may be found as Joint Exhibit No. VIII admitted into evidence. The Petitioners, through their counsel, then filed a formal petition dated May 6, 1980, which was the vehicle utilized in establishing the details of this dispute and was the basis for the Department Secretary forwarding the case to the Division of Administrative Hearings for consideration by a hearing officer in keeping with the provisions of Section 120.57, Florida Statutes. The hearing was conducted on October 16, 1980, and the Petitioners' position was more specifically defined in the course of that hearing and the claim as described in the issue statement of this order constitutes the substance of the Petitioners' position. 2/ Joint Exhibit No. I; petitioners' Exhibit No. 1 and Respondent Deltona's Exhibits 1, 2 and 4 constitute sketches and aerial photographs of the general project area. Joint Exhibit No. 1 identifies the work area with more particularity. Respondent's Exhibit No. 2 indicates the desired flow pattern of the water through the various lake systems and indicates whether the flow is by gravity flow or pump flow. This drawing depicts the proposed channels and structural improvements that would be involved. The Department has indicated that all the regulatory concerns which it has about the project associated with Permit No. 64-26478-4E, the permit in question, have been adequately addressed, subject to the conditions set forth in the permit document. Joint Exhibit Nos. V and VI; Respondent Deltona's Exhibit Nos. 5, 6 and 7; and the Petitioners Exhibit No. 2 are exhibits pertaining to water quality concerns, to include sample results. The testing and other information provided indicates that the project as contemplaced, would meat the regulatory parameters set forth in Chapter 403, Florida Statutes, and Chapters 17-3 and 17-4, Florida Administrative Code. The Department in expressing its concern that continued water quality monitoring be conducted has indicated that it feels that future periodic monitoring should be done in Jenkins Pond, Lake Big, Lake Diana, McGarity Lake, Sidney Lake and Lake Mitnik. The Respondent Deltona would only conduct this monitoring in the first three lakes named. By looking at the Respondent Deltona's Exhibit No. 2, it could be seen that all of the aforementioned lakes would be in the same basic flow pattern. Of the system of lakes, the area around McGarity Lake is the most highly developed and and has the greatest potential for causing unacceptable pollution. That pollution could be carried through the other lakes within the system as described in view of the potential of the system, if the project is built, to convey a greater volume of water at a higher rate of flow. A more expansive water quality monitoring system within six lakes as opposed to three lakes would increase the opportunity to discover potential hazards from pollutant at an earlier data. This is particularly so by using lakes such as McGarity Lake where there is a higher level of developmental build-out.
The Issue The issue in this case is whether Niagara Bottling Company, LLC (Niagara), is entitled to Consumptive Use Permit (CUP) No. 114010 issued by the St. Johns River Water Management District (District), which authorizes Niagara to withdraw and use 484,000 gallons per day (gpd) of groundwater to produce bottled water at a facility in Lake County.
Findings Of Fact The Parties Groveland is a municipal corporation located in Lake County. Niagara is a water bottling company registered to do business in Florida. Niagara currently owns and operates six water bottling facilities in the United States, including a bottling facility in unincorporated Lake County, northwest of Groveland. Niagara currently operates one bottling line at its Groveland facility, which can be used to bottle either spring water or purified water. The District is a special taxing district created by the Florida Water Resources Act of 1972, with jurisdiction over a sixteen-county area that includes Groveland and the site of Niagara’s proposed water withdrawal. The District administers a permitting program for the consumptive use of water. The Proposed Permit The top geologic layer in the region is the surficial aquifer, which starts at the ground surface and extends down about 50 feet to the Intermediate Confining Unit. Below the Intermediate Confining Unit is the Upper Floridan Aquifer, which starts at a depth of about 150 feet and extends downward to about 550 feet below the ground surface. Below the Upper Floridan Aquifer is the Middle Semi-Confining Unit, which extends down another 450 feet. Below the Middle Semi-Confining Unit is the Lower Florida Aquifer, which extends down to about 2,200 feet below sea level. Nearly all of the groundwater withdrawn for consumptive uses in central Florida comes from the Upper Floridan Aquifer. Groveland’s public water supply wells, for example, withdraw water from the Upper Floridan Aquifer. The proposed CUP authorizes Niagara to withdraw 484,000 gpd from the Upper Floridan Aquifer to produce bottled water. The CUP authorizes the installation of three water supply wells for the facility: a 16-inch production well, a 16-inch backup well, and a 4-inch supply well for domestic uses at Niagara’s facility. Of the 484,000 gpd that Niagara would withdraw, approximately 454,000 gpd would be treated and bottled as “purified water” and approximately 30,000 gpd would be used for cooling some of the equipment used in the bottling process. Under federal regulations, bottled water sold as purified water must meet certain maximum contaminant levels, including a total dissolved solids (TDS) level of less than 10 parts per million. By regulation, purified water is distinct from tap water and from bottled spring water. Niagara would treat the groundwater by filtration and reverse osmosis (RO), primarily to remove TDS. At a customer’s request, minerals can be added to the water to enhance taste. Also before the water is bottled, it disinfected with ozone. The RO process at the Niagara facility is projected to turn 454,000 gpd of groundwater into about 363,000 gpd of purified drinking water for bottling and 91,000 gpd of RO concentrate/wastewater. Reject water from the cooling water system would add some additional wastewater. Niagara has arranged to send its RO concentrate to the Frozen Grove Wastewater Treatment Facility to be blended and used for irrigation at the Mission Inn Golf and Tennis Resort in Howey-in-the-Hills. The City of Minneola has also agreed to take Niagara’s RO concentrate. Niagara and the District requested that the proposed CUP be modified to add the City of Minneola wastewater treatment facility as an alternative recipient for Niagara’s RO concentrate. Niagara and the District propose the following change to Condition 10 of the Technical Staff Report: Withdrawals of groundwater from Well Nos. 1 (GRS Id No 145009) and 2 (GRS Id No 145010 for commercial/industrial type use shall not be initiated until Niagara Bottling LLC and the Frozen Grove WWTF or alternatively Niagara Bottling LLC and the City of Minneola WWTF have obtained all necessary permits to create and use the blend of process waste water (R/O concentrate) and reclaimed water for irrigation, as described in Attachment 4 of the application materials submitted to the District on May 9, 2008 for the Frozen Grove WWTF and the material submitted to the District on March 4, 2009 for the City of Minneola WWTF. The permittee shall provide documentation to the District that the necessary permits have been obtained within 30 days of initiating withdrawals of groundwater for commercial/industrial type use from Well Nos. 1 (GRS Id No 145009) and 2 (GRS Id No 145010). The proposed CUP includes a conservation plan with provisions for monitoring water use, repairing leaks, conducting quality assurance inspections, using totalizing flow meters, and minimizing spillage. Niagara’s proposed CUP contains conditions for environmental monitoring. Niagara would be required to collect water level and rainfall data, and basic vegetation and soils conditions at Lake Arthur. Lake Arthur was selected for monitoring because hydrologic modeling indicated that Niagara’s greatest potential impact to the water table was near Lake Arthur. The monitoring is intended to detect any unexpected adverse environmental impacts caused by Niagara’s proposed withdrawal so that they can be addressed. The proposed permit has an expiration date of December 31, 2013. Stipulations and Withdrawn Claims Before the final hearing, Groveland withdrew a number of allegations made in its Second Amended Petition for Hearing. Groveland stated that its intent was to withdraw the claims that its substantial interests were affected by Niagara’s proposed groundwater withdrawal. Groveland no longer contends that it would be specially injured by the proposed water use. In the parties’ Joint Pre-Hearing Stipulation, Groveland stipulated that Niagara’s proposed water use would not interfere with any legal uses of water. Groveland also stipulated that Niagara’s proposed use would not cause adverse or significant impacts to lake stages or vegetation, would not impact adjacent land uses, would not cause significant saline water intrusion, would not cause or contribute to flood damage, would not harm the quality of the water source, would not cause or contribute to a violation of state water quality standards, would not impact minimum flows and levels established by the District, would not cause the water table or aquifer potentiometric surface to be lowered so that lake stages or vegetation would be adversely and significantly affected, would not affect spring flows or water levels, and would not use water reserved by the District from consumptive use. The record evidence supports the stipulations identified above. Economic and Efficient Utilization The Upper Floridan Aquifer is capable of producing the requested amount of water. Florida Administrative Code Rule 40C-2.301(4)(a) and Section 10.3(a) of the Applicant’s Handbook require that a water use be in such quantity as is necessary for economic and efficient utilization. The District’s determination of economic necessity focuses on preventing “water banking,” which is securing rights to water in excess of an applicant’s actual needs, for possible future use. Niagara’s 484,000 gpd allocation is based on the peak maximum daily output of the processing equipment operating at 74 percent capacity, which is the average capacity that Niagara achieves at its bottling facilities. Groveland contends that the consumer demand for bottled water could be met by other water bottlers and, therefore, there is no need for Niagara’s proposed withdrawal. However, no statute or rule requires Niagara to demonstrate that this particular CUP is the only means to meet the consumer demand for bottled water. The District’s evaluation of need focuses on the applicant’s need for the requested volume of water. In determining whether a requested use of water is necessary, the District does not evaluate the appropriateness of the associated business or activity, but only whether the applicant can reasonably be expected to use the requested volume of water, and do so efficiently based on industry standards. The evidence presented regarding the bottled water market and Niagara’s position in the market was sufficient to demonstrate that the requested volume of water is necessary through the duration of the CUP. The 30,000 gpd that Niagara would use for its cooling system is a reasonable amount of the water for that purpose. The technology to be used at Niagara’s facility is state-of-the- art, using constant online monitoring to reduce reject water. The cooling equipment and its operation have been designed to minimize water use. RO is the industry treatment standard for production of purified bottled water. It is the most cost-efficient treatment method in terms of energy use and water consumption. The proposed RO equipment and its operational parameters are designed to optimize treatment efficiencies. The volume of RO concentrate that would be produced depends on the TDS levels in the groundwater. The estimate of 91,000 gpd of RO concentrate is conservatively high, based on the TDS levels in groundwater samples. The actual volume of RO concentrate produced by Niagara could be smaller. Groveland was critical of Niagara’s wastewater volume, contending that the conversion of 91,000 gpd of groundwater to wastewater is inefficient and contrary to the public interest. The fact that Niagara’s bottling process would produce 91,000 gpd of wastewater does not make it inefficient. Nearly every commercial and industrial water use has a wastewater component. In the context of water bottling processes and water treatment systems, Niagara’s operation is efficient. Groveland asserts that sending Niagara’s RO concentrate to the Mission Inn golf course or the City of Minneola for irrigation purposes is inefficient because a large portion of irrigation water is usually lost to evaporation and does not recharge the aquifer. This assertion fails to account for the fact that every gallon of RO concentrate used for irrigation reduces by one gallon the volume of groundwater that would otherwise be withdrawn for irrigation. Using Niagara’s wastewater for irrigation contributes to the efficiency of Niagara’s proposed use. There is typically a deficit of reclaimed water from public wastewater treatment systems in the summer when the demand for reclaimed water for irrigation and other purposes increases. Niagara’s supply of RO concentrate, however, would remain constant throughout the year. Mission Inn and Minneola would benefit if they were able to use Niagara’s RO concentrate. Niagara’s conservation plan for water use at its facility is equal to or better than the conservation plans incorporated into the CUPs that the District has issued to other beverage bottlers. Niagara’s proposed use was shown to be of such a quantity as is necessary for economic and efficient utilization. Sources of Lower Quality Water Florida Administrative Rule 40C-2.301(4)(f) states that reclaimed water must be used if it is “readily available.” Section 10.3(g) of the Applicant’s Handbook requires that the “lowest acceptable quality water source, including reclaimed water or surface water” must be used for a consumptive use, unless the applicant demonstrates that the use of a lower quality water source is not economically, environmentally, or technologically feasible. The requirement to use a lower water quality source, however, is not applicable when the water is for “direct human consumption” or human food preparation. § 10.3(g), Applicant’s Handbook. Groveland argues that the word “direct” should mean unaltered and, therefore, Niagara’s bottled water is not intended for direct human consumption because the water is treated before it is bottled. The District, however, does not interpret or apply the term “direct human consumption” to mean drinking water directly from the source without treatment. In the case of the water delivered to households and businesses by public water suppliers, which also must be treated before it is delivered, the District regulates the water as being for direct human consumption. The fact that Niagara would filter the groundwater, apply RO treatment, add acid to prevent mineral buildup in the RO equipment, and add minerals for taste if requested by customers, does not disqualify Niagara’s bottled water as being for direct human consumption. Because 454,000 gpd of Niagara’s proposed water withdrawal would be processed for direct human consumption, Niagara did not have to seek to use a source of lower water quality for that volume. The requirement to use available sources of lower quality water would apply to the 30,000 gpd that Niagara intends to use for cooling. There are technical and economic problems associated with using water of lower quality for the cooling process at the Niagara facility because higher TDS levels would damage the cooling equipment. Using water with higher TDS levels would also require greater volumes of water to achieve cooling. Niagara’s cooling system is designed to reject water when the dissolved solids reach a certain high level, and to replace the reject water with fresh water. Operating at higher dissolved solid levels would cause the system to reject water more frequently, so greater volumes of water would be needed for cooling and greater volumes of wastewater would be generated. Using surface water from the St. Johns River, which has TDS levels much higher than in the groundwater, would require twice as much water to operate Niagara’s cooling system. In addition, a 44-mile pipeline would be needed to convey water from the St. Johns River to the Groveland facility, which would involve much higher costs. Seawater has even higher TDS levels and would require desalinization and a different cooling system. Using seawater would require much greater volumes of water for treatment and cooling. Disposal of the brine concentrate generated by the treatment process would create additional costs. The use of seawater would require the construction of a 120-mile pipeline, which would involve large capital and operating costs. Groveland insists that the much higher costs associated with these sources of lower quality water are still economically feasible for Niagara based on Niagara’s projected income from its bottling operations. The District does not determine feasibility based on the balance sheet of the individual permit applicant. The District evaluates relative costs of alternative sources in the context of normal practices and expected benefits. Reliable volumes of reclaimed water to use in Niagara’s cooling system are not readily available to Niagara from domestic wastewater treatment facilities in the area. The spring water sources that Niagara is currently using are not sources of lower quality water. These sources are of equivalent quality to the groundwater that Niagara proposes to withdraw. Groveland contends that Niagara did not investigate the quality of the Lower Floridan Aquifer as a potential source of lower water quality water for Niagara’s proposed use. Groveland believes, but did not prove, that the Lower Floridan has lower quality water. Studies conducted by the U.S. Geological Survey indicate that the water quality of the Lower Floridan Aquifer is about the same or better quality than the quality of the water in the Upper Floridan Aquifer. Water quality data from a Lower Floridan well in the vicinity also indicates that the quality of the water in the Lower Floridan is as good as, or better than, the water quality in the Upper Floridan in this area. Withdrawals from the Lower Floridan create a risk of saline water intrusion into the fresh portion of the Lower Floridan or Upper Floridan. Niagara demonstrated that it is not technically nor economically feasible to use a source of lower quality water for its cooling water. Individual Effect on Wetlands and Lakes To identify the “zone of influence” of Niagara’s proposed withdrawal of water and to assess the individual and cumulative effects of the drawdown associated with the withdrawal, Niagara’s consulting hydrogeologist used a steady- state numerical groundwater model developed by the District, known as the East Central Florida (ECF) groundwater model. It is a steady-state model, which produces a value that represents a long-term average effect. The ECF model predicts the level of drawdown in the surficial aquifer. The model assumes that wetlands and other surface waters are directly connected to the surficial aquifer so that a given drawdown of the surficial aquifer causes the same drawdown of the water levels in wetlands and other surface waters. The ECF model is calibrated to water level data from 1995. A drawdown predicted by the model is a drawdown from 1995 water levels. The ECF model results are graphically depicted as drawdown contours that are overlaid on aerial photography. The District considers the condition and functions of the surface waters in and around the withdrawal site to determine how they might be affected by a predicted drawdown. The dominant surface waters in the area of the proposed withdrawal are sand hill lakes. There are few wetlands. In sand hill lake systems, water table levels fluctuate widely, as much as eight or ten feet. Consequently, these systems are colonized by herbaceous plants that are adapted to widely fluctuating water levels. The wetlands and lakes in the area are not currently showing signs of environmental harm as a result of existing groundwater withdrawals. Niagara’s modeling predicted that the proposed water withdrawal, by itself, would cause a maximum drawdown in the surficial aquifer of 0.1 feet, except for one small area where the predicted drawdown was 0.2 feet. All the expert witnesses were in agreement that Niagara’s drawdown, by itself, is unlikely to cause environmental harm. In fact, the impacts of such a small drawdown on the physical conditions or functions of wetlands or lakes in the area would probably be impossible to detect. Cumulative Effect on Wetlands and Lakes For the analysis of cumulative impacts, the ECF model takes into account all permitted withdrawals for the year 2013, because that is the key year for the regulation of water uses in the Central Florida Coordination Area (CFCA), which includes the site of Niagara’s bottling facility. The CFCA is discussed in greater detail later in this Recommended Order. The ECF model predicated that the cumulative surficial aquifer drawdown within the area of influence of Niagara’s proposed withdrawal would be less than one foot except for one small area where the drawdown is predicted to be 1.1 feet. Niagara submitted an environmental assessment report, the Lotspeich report, with its permit application. The Lotspeich report concluded that no ecological harm would be caused by Niagara’s proposed withdrawal. Subsequently, Niagara’s consulting ecologist, Dr. Shirley Denton, who has extensive experience with the effects of drawdowns on wetlands and other surface waters, reevaluated the potential effects of Niagara’s proposed withdrawal. Dr. Denton visited all of the natural systems in the field. It was her opinion that the cumulative drawdown would not cause unacceptable harm to these natural systems. The District’s environmental expert agreed with Dr. Denton. In the Central Florida sand hill lakes area, a drawdown of this magnitude is not an uncommon cumulative impact from groundwater withdrawals that the District has determined to be acceptable. Groveland presented the testimony of Dr. Jay Exum who opined that the cumulative drawdown in the area of Niagara’s proposed withdrawal would adversely impact wetlands. Dr. Exum’s opinion was based on his prediction that the cumulative drawdown would result in a substantial reduction in the size of the wetlands in the area. However, his opinion about the loss of wetland acreage is not persuasive because of the unconventional methodology2/ that he used and the unreasonable assumptions upon which his opinion was based. Dr. Exum reviewed land cover maps of Lake County, calculated the size and topography of eight wetlands in the area (only one was within Niagara’s zone of influence), came up with an estimated reduction in wetland acreage for these wetlands, and then extrapolated from that number a prediction of the total area of wetlands within Niagara’s area of influence that would be lost as a result of the cumulative drawdown. Dr. Exum did not account for the fact that the wetlands and lakes in the area already reflect most of the cumulative drawdown. The cumulative drawdown predicted by the modeling is not a drawdown below today’s average water levels; it is a drawdown below 1995 levels. In addition, Dr. Exum assumed that a drawdown in the surficial aquifer of .5 foot will cause the future loss of the vegetation at the outer edges of a wetland in an amount that can be calculated simply by determining how much area .5 feet of water would occupy. That assumption would only apply in a hypothetical, unnatural situation where water levels are constant and the wetland vegetation will not survive if the water table drops .5 feet. However, the actual situation is that the water table fluctuates widely in these natural systems and the vegetation is adapted to the fluctuations. The area “formerly” occupied by the .5 feet of water could still be inundated frequently enough to sustain the vegetation. Dr. Exum’s opinion about the environmental effects that would be caused by the cumulative drawdown of the surficial aquifer was given less weight than the opinions offered by Niagara’s and the District’s ecologists because Dr. Exum has little or no prior experience with the effects of drawdowns on natural systems. Dr. Exum’s professional experience is almost entirely with the impacts associated with construction activities in or near wetlands, which would not acquaint him with the unique, long-term responses of natural systems to water table drawdowns caused by groundwater withdrawals. Dr. Denton, who has over 25 years of experience with monitoring wetlands affected by groundwater withdrawals, stated that drawdowns in the surficial aquifer do not usually cause reductions in the size of a wetlands. The more persuasive evidence in the record demonstrates that Niagara’s proposed withdrawal would not cause adverse impacts to wetlands on an individual or a cumulative basis. Niagara provided reasonable assurance that any environmental harm caused by the proposed use has been reduced to an acceptable amount. The five-year duration of the permit is reasonable and appropriate. Public Interest Section 9.3 of the Applicant’s Handbook defines “public interest” as: those rights and claims on behalf of the people in general. In examining whether an application is consistent with the public interest, the District considers whether a particular use of water is going to be beneficial or detrimental to the overall collective well-being of the people or to the water resource in the area, the District and the State. The policy and practice of the District has been to limit its public interest analysis to matters directly related to water resources and the management of those resources. Other matters, such as vehicle traffic generated by the applicant, are not considered by the District. Groveland suggests that Niagara’s proposed use, and perhaps all commercial/industrials uses, are less important and worthy than public water supply uses like its own, and should not be allowed to take water that a public water supplier might need in the future. As discussed in the Conclusions of Law, all reasonable beneficial uses of water are equal under Chapter 373, except in certain contexts which are not applicable here. Commercial and industrial activities that make consumptive uses of water, when conducted in conformance with regulations established to efficiently use and protect the water resources, are generally beneficial to the collective well-being of the people. Groveland also claims that Niagara’s CUP is not in the public interest because a portion of Niagara’s bottled water will be shipped out of Florida. Although Niagara cannot project precisely the amount of bottled water that would end in the hands of consumers residing out-of-state, an estimate of 20 percent was given. For beverage bottlers or any other commercial or industrial water users that incorporate water into their products, the District deems the location of the water use to be where the water is bottled or incorporated into the products. The District does not look to where products are ultimately purchased by a retail consumer. Therefore, the District did not consider the fact that a portion of Niagara’s bottled water would be consumed outside of Florida as a factor in the District’s determination of whether the proposed water use is in the public interest. Niagara’s withdrawal is within the Central Florida Coordination Area (CFCA), an area covering parts of the jurisdiction of three water management districts and which includes the City of Groveland and the site of Niagara’s proposed water withdrawal. The CFCA is a highly productive area for groundwater withdrawals, but the water management districts have determined that it does not have sufficient water to serve water needs above the levels that have been allocated through the year 2013. To protect the water resources of the CFCA, rules were adopted to require public water suppliers and other water users within the CFCA to use “supplemental water supplies” to meet their increases in demand after 2013. Supplemental water supplies are identified in the CFCA rules as reclaimed water, stormwater, surface water, and seawater desalinization. Niagara is not requesting additional water above its 2013 demand and, therefore, is not subject to the restrictions imposed by the various CFCA rules. Nevertheless, the District treated Niagara’s location within the CFCA as a matter affecting the public interest. The District determined that it was inconsistent with the public interest to allow Niagara to withdraw groundwater in the CFCA unless Niagara was required to participate in the development of supplemental water supplies. Therefore, Niagara is required by “Other Condition” 14 in the District’s Technical Staff Report, to identify potential partners for the development of supplemental water supply projects, determine the viability of developing the partnerships, evaluate potential supplemental water supply projects available, and submit a comprehensive written report evaluating whether identified projects are feasible future water supply sources for Niagara. The District imposed a permit expiration date of December 31, 2013, to enable the District and Niagara to reevaluate Niagara’s ability to use a lower quality water source after that date. Groveland does not believe the conditions imposed by the District go far enough and asserts that Niagara’s water withdrawal from the CFCA is still contrary to the public interest. Niagara’s proposed withdrawal is also within a Priority Water Resource Caution Area (PWRCA) designated by the District. The District designates priority water resource caution areas as part of its water supply 20-year planning process. In the PWRCA, the District has determined that there is inadequate groundwater in the Floridan Aquifer to meet all existing and future water needs, without having unacceptable impacts on the water resources. The District stated that the designation of a priority water resource caution area is strictly a planning tool and does not preclude the issuance of permits. CUPs are commonly issued for proposed withdrawals in priority water resource caution areas in the District.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the District enter a final order granting Consumptive Use Permit No. 114010 with the conditions specified in the Technical Staff Report and the additional condition proposed by the District and Niagara and set forth in paragraph 12, above. DONE AND ENTERED this 7th day of August, 2009, in Tallahassee, Leon County, Florida. BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 7th day of August, 2009.
The Issue The issue for consideration herein is whether Sarasota County Utilities should be issued a consumptive use permit to draw water from the 14 wells in issue here located in Sarasota County.
Findings Of Fact At all times pertinent to the issues herein, the Respondent, District, was the state agency responsible for themanagement of water resources within its area of geographical jurisdiction. Included therein was the responsibility for the permitting of consumptive water use. The Respondent, Sarasota County, is a political subdivision of the State of Florida and operates a public utilities division which is charged with meeting, among other things, the potable water needs of the residents of the County. Petitioners Wyatt S. Bishop and Joan Jones are both residents of Sarasota County and both draw their potable water from wells which utilize the aquifers pertinent to the wells for which the permit in issue here relate. Mr. Bishop lives approximately 7.5 miles north of the Carlton Reserve, the property on which the wells in issue are located, and Ms. Jones lives approximately 7 miles from the Reserve, but in a different direction. Sarasota County filed an application for a consumptive use permit with the District on January 28, 1987 requesting an average daily withdrawal of 10.71 million gallons per day, (mgd), and a peak monthly withdrawal of 15.55 mgd. This application, assigned number 208836.00, was, over the next three years, amended by the County four separate times. These amendments reflected revised water demand determinations and were submitted to provide additional information requested by the District. The District issued a preliminary staff report and proposed intent on March 26, 1991 reflecting an approved withdrawal in the amount of 7.28 mgd average daily withdrawal and 11.1 mgd peak monthly withdrawal. These figures were revised, however, byan amendment by the District on July 8, 1991, and as amended, authorize 7.303 mgd average daily withdrawal and 9.625 mgd peak monthly withdrawal. The County's application was reviewed by an experienced hydrologist in the District office with extensive permit review experience who utilized, in his evaluation of the permit, the pertinent District rules and policies. By way of background, to more easily understand the circumstances here, Sarasota entered into a contract with Manatee County in 1973 which called for the latter to provide up to 10 mgd of water for a period of 40 years, up to and including the year 2013. However, in 1979, Manatee County's utilities director advised Sarasota County that it, Sarasota County, could not continue to rely on Manatee County's water after the expiration of the current contract, and would, therefore, have to become self sufficient in water. Since the MacArthur tract, now known as the Carlton Reserve, had just recently been identified by, inter alia, the United States Geological Service as a potential long term water source for Sarasota County, after Manatee County advised Sarasota County of its future expectations, Sarasota County and the Manasota Basin Board hired a consulting firm to conduct hydrological testing on the Carlton Reserve. This study concluded that the Reserve had sufficient water resources to satisfy the needs of the unincorporated areas of Sarasota County for an extended time into the future. In 1985, because of its increased water needs and thetime necessary to complete required studies on the utilization of the Myakka River, a surface water resource, Sarasota County concluded that it was suffering a water supply shortage and entered into a supplemental contract with Manatee County to provide 2 million gallons of water per day over a 5 year period which would expire in 1990. Sarasota County had not, however, been idle with regard to the investigation of other water resources. Studies done included not only the Myakka River mentioned above but a reservoir owned by the City of Bradenton, and the Peace River. Nonetheless, it was determined that the Carlton Reserve was the best source available overall, and in 1987, the County filed the application in issue here. The permit was under consideration for approximately 3 1/2 years before the initial decision by the District to grant it. During that time the County experienced a significant deficiency in its water sources and found it necessary, on February 5, 1991, to enter into another contract with Manatee County to supply an addition 5 mgd. Terms of that contract clearly indicate the expectations of both parties that Sarasota County will take reasonable steps to develop its own water resources. It is not as though Sarasota County sat quietly in the interim, however, and allowed the situation to develop. A building moratorium to halt additional construction was proposed and as a result, economic forces in the County indicated a potential loss of jobs to County residents. None of this would be desirable from an economicstandpoint. In the course of the permit application process, 12 test wells were sunk to conduct aquifer pump tests; to assess water quality, amounts and availability, aquifer characteristics and drawdown; and to determine the impact of withdrawal on water quality. Eight of these 12 wells are located on the Carlton Reserve. The other 4 are located on property owned by the MacArthur Foundation which is contiguous to the Carlton Reserve property and from which Sarasota has a right by easement to draw water. The 2 wells yet to be constructed will be on Sarasota County property. Sarasota County currently receives 10 mgd of water under its contract with Manatee County; an additional 5 mgd under the February 5, 1991 contract; 2 mgd from the University wellfield, (with a peak withdrawal rate of 3 mgd); and .9 mgd from the Sorrento wellfield, (with a peak withdrawal rate of 1.1 mgd). This latter source is only producing currently .6 mgd of potable water due to constraints imposed by the water treatment requirements. Taken together, the current Sarasota County supply constitutes 18.6 mgd. The above does not take into account the County's agreement with the City of Sarasota calling for the purchase of up to 2 mgd. Since this source is not reliable, it is not included in the total, and the City is not considered an available water source. In addition, the District and Sarasota County stipulated on July 15, 1991 that within 30 days, the County would apply tophase out routine water production from the Sorrento wellfield, relying on it only in emergency situations with District consent. For this reason, it, too, is not considered an available water supply source. These currently existing sources, with modifications as described, will be the primary sources of potable water provided to 6 major service areas in Sarasota County when the County's water treatment plant and transmission system are complete in 1993. In attempting to define the County's future water requirements, two major criteria were considered. The first was the County's historical water demand, and the second, modifying it, relates to the demand arising as a result of new water users being added to the system as a result of the County's capital improvements and acquisition program. Water resources are not unlimited. Current resources come primarily from Manatee County and there are constraints on this supply as it is made available to Sarasota County. For example, the 10 mgd contract expires in 2013. The 5 mgd contract expires in 2001. Though the latter is subject to renewal, renewal is contingent upon the availability of water supply at that time, and that is not a sure thing. It can, therefore, readily be seen that 15 out of the 18.6 mgd routinely available now comes from Manatee County, and those sources are not perpetual. In addition, it is conceivable that Manatee County may pre-blend the water it delivers to Sarasota County with water of lesser quality, so that the delivered water may exceed the total dissolved solids standard of 500 ppm for potable water. If thewater from Manatee County were reduced to that quality, the University wellfield supply, which currently exceeds standards itself, and which relies on blending with better quality Manatee County water to be potable, would also be removed as a source of potable water to Sarasota County. In order to comply with the provisions of Section 373.171, Florida Statutes, which requires the District to regulate the use of water by apportionment, limitation, or rotating uses, to obtain the most beneficial use of water resources and to protect the public health, safety and welfare, the District analyzed the available water sources and determined that Sarasota County relies upon its 10 mgd supply from Manatee County and the 2 mgd supply from University wellfield to constitute 12 mgd usable water. The 5 mgd from Manatee County would be used only in an emergency situation, and the Sorrento wellfield would be abandoned. Future water demands must be predicted relying in great part upon an historic record of prior water use. Utilizing a statistical procedure called linear regression, a methodology accepted by the District, indicated a water demand figure for the period from 1992 to 1997 based upon six use points extending from 1985 to 1990. These use records reflected a low of 9.733 mgd and a high of 12.808 mgd, the former being in 1985 and the latter in 1990. In addition, the County estimated that its capital improvement program would add between 10 and 12 thousand customers who presently use private wells, whose water use would constitute approximately 2 mgd of additional demand. The County's program toacquire some 42 private franchises now serving customers would add an additional demand of 2 mgd. Taken together, these programs would add in approximately 1.8 mgd per year to the need assessment, and it would therefore appear that by 1997, the County's average daily demand, considering all new users, would be 17.84 mgd. The water to be drawn from the Carlton Reserve is not currently potable and will require some form of treatment to render it so. Sarasota County proposes to use the Electrodialysis Reversal process, (EDR), because, in the County's judgement, it is more efficient than others such as reverse osmosis and ion exchange. Whereas EDR is rated at up to 85% efficient, the others range between 50% to 75% efficient. In that regard, in order to determine the maximum amount of water to be drawn, providing a safety factor for a treatment plant operation that is not working up to peak capacity in computing the water needs, the EDR process was determined to be no more than 80% efficient. Factoring in that efficiency potential, when the 1997 average daily demand is subtracted from the County's projected water capacity, the withdrawal need in 1997 is determined to be 7.303 mgd. However, as a part of its permitting process, the County also calculated its peak month daily demand. This is a figure which represents the maximum amount permitted to be drawn on a daily basis during the peak demand period. This peak period was determined under Section b 3.2 of the District's Basis of Review by taking the 1989 daily flow and using a sliding 31 day calendar to determine the highest historical 31 day flow. Thisresulted in a peak month coefficient of 6.16 which was then multiplied by the 1997 average daily demand of 17.842 mgd which resulted in a peak month daily demand of 20.7 mgd. When existing water supplies are removed and the 80% EDR treatment process factor is applied, the amount of raw water needed from the wellfield in issue on a peak monthly basis would be 9.625 mgd. This peak monthly basis figure is considered because of the intermittent periods of low rainfall and high water demand within the County. Accepting the 1.8 gpd yearly increase; the peak factor of 1.16; and the assumed water supply capacity of 18.6 mgd; Sarasota County's need will exceed its available supplies by 1993. In fact, the County is already experiencing low water pressure in part of its service area during peak demand periods. County experts estimate that without the requested water from the Carlton Tract, Sarasota County can expect to experience dry periods as early as 1993 during the periods of peak water usage, generally between April and June. For the above reason, when the application and its supporting information was reviewed by Mr. Basso, the District hydrologist with extensive experience reviewing more than 300 water use application, he determined that the water supplies requested are necessary to meet the County's certain reasonable demand, and that this meets the criteria set out in Rule 40D - 2.301(1)(a), F.A.C. Turning to the issue of hydrologic and environmental impacts, the District's Basis For Review of Water Permit Applications provides for the use of a "water use model" inevaluating water needs and the appropriateness of a proposed withdrawal. In preparing its submittal to the District, Sarasota County performed certain tests and modeling to derive the statistical and scientific information used in support of its application. Specifically it used the USGS' MODFLOW model utilizing information obtained from the pump tests run on the wells in the pertinent areas. Consistent with the District's rule, the water data and aquifer drawdown were determined by simulated pumping. The tests run also provided the information on water quality in the aquifer and physical characteristics including transmissivity, storage coefficient, specific yield and leakance between aquifers. This data also helped in defining the hydrogeologic framework of the Carlton Reserve. The Carlton Reserve's hydrogeology listed in descending order from the surface, includes a surficial aquifer which varies in depth between 19 and 70 feet across the Reserve; a semi-confining clay unit separating it from the intermediate aquifer; the upper intermediate and lower intermediate aquifer which range in depth from 140 to 180 feet across the Reserve; another confining layer, and the Upper and Lower Floridan aquifers. The hydrology and groundwater modeling expert who constructed the model used in Sarasota County's permit application concluded that the water table drawdown at the Reserve property boundary in the surficial aquifer would be less than .3 of a foot; less than .4 of a foot in the intermediate aquifer; and 2.9 feet in the Upper Florida aquifer. The water to be drawn consistentwith this instant permit, if approved, would come from the Upper Floridan aquifer on the Reserve. The County's experts were conservative in the assumptions used in the groundwater model. It was assumed there would be no lateral water flow into the model area and no recharge. In addition, the model called for all pumps to run simultaneously at a maximum drawdown of 12.65 mgd for 90 days rather than at the requested quantity of 9.625 mgd. Utilization of these assumptions provided a scenario wherein "severe" impacts would be encountered. Based on the testing and the modeling done, expert opinion was that there would be no quantity or quality changes that would adversely effect water resources including ground and surface water. This meets the criteria of Rule 40D-2.301. This opinion was concurred in the District's hydrology expert. Nonetheless, in its proposed approval, the District has imposed special permitting conditions which require the County to monitor, analyze, and report water quality and water table level information to the District on a monthly and annual basis. When it evaluates the information supplied by an applicant relating to ground water monitoring, the District is required to consider certain presumptions set forth in its Basis For Review. For example, the District presumes that if there is a drawdown of more than 1 foot in the surficial aquifer at a wetland, adverse environmental impacts will occur. In the instant case, the County model concluded that the actual drawdown in the surficial aquifer at the Carlton Reserve is less than .6 of onefoot and, therefore, there should be no adverse environmental impact resulting from the withdrawal. Nonetheless, the County has developed several plans designed to provide information on environmental impacts which will continuously monitor such parameters as rainfall and evaporation, wetlands hydroperiod changes and vegetative changes in the wetlands to detect any changes which might be attributed to the water pumping. These plans have been made special conditions to the water use permit, and in the opinion of the County's ecology and hydrology expert, would enable the County to adequately monitor and detect any pertinent changes to the pertinent factors concerned on the Carlton Reserve. If wetland changes are detected, a contingency plan will be in effect which will require an alteration of pumping schedules or other action to minimize any adverse impacts. The District expert in wetlands and wildlife habitat has opined that these measures, with which he is familiar, are adequate to insure that adverse impacts to the wetlands will not occur. This is consistent with the provisions of Rule 40D-2.301(1). As was stated previously, the water to be drawn pursuant to this permit will be drawn from the Upper Floridan aquifer. This water is not potable but is treatable and is the lowest quality water which can be economically used by the County. Water of a lower quality does exist in the Lower Florida aquifer, but it is not economically treatable, and, in addition, use of this Lower Floridan aquifer might cause vertical movement of the poorer quality water into the upper strata. For all practical purposes,then, the lowest quality water available to it will be used by the County and this is consistent with the District's basis for review. Expert testimony indicates that saline water will not be infused into the Upper Floridan aquifer. Salt water intrusion generally occurs when groundwater is brought to a level below sea level. Even at the point of maximum actual drawdown as a result of pumping on the Reserve, the fresh water level will remain at least 20 feet above sea level, and as a result of the difference in water level, no saline water intrusion into the fresh water supply will occur even though salt water intrusion can also occur as a result of upward vertical movement of lower quality water due to withdrawal. The District's hydrologist and reviewing official also concluded that because of the confining layer below the aquifer from which water will be withdrawn, there would not be any significant upward movement of lesser quality water. The District's basis of review also envisions an aquifer pollution if a proposed withdrawal would spread an identified contamination plume. Here no contamination has been identified in the area from which the water will be drawn, and therefore, contamination would not be spread. The Basis for Review also infers there will be adverse impact to off site land if there is a significant drawdown of surface water bodies or if damage to crops or other vegetation can be expected. Here, the water table drawdown at the boundary of the Carlton Reserve is anticipated at less than .3 of one foot and any drawdown further out from the Reserve can be expected tobe even less. As a result, no adverse impact to existing off site land useage is expected. With regard to Rule 40D-2.301(1)(i), relating to an adverse impact on existing legal uses, the District presumes that no adverse impact will exist if the drawdown in the water table is no more than 2 feet at an affected well, or the potentiometric surface at the well is not lowered by more than 5 feet. Here, again applying the County's groundwater modeling demonstrates that the drawdown at its worst, in the Upper Floridan aquifer, would be no more than 2.9 feet at the Reserve boundary and much less at the Petitioners' wells. Both Mr Bishop's and Ms. Jones' wells are approximately 7.5 and 7 miles, respectively, from the closest well on the Reserve property. Ms. Jones' well is drilled into the intermediate aquifer which is above that which the County proposes to use and should not be impacted. Mr. Bishop draws water from the intermediate and surficial aquifers, both of which are above the Upper Florida aquifer identified for use here, and the groundwater modeling would suggest that his well would not be impacted either. Sarasota County's application contains reference to numerous proposals for water conservation measures which it intends to implement or has already implemented. It has adopted ordinances to enforce the District's watering restrictions and is currently implementing a block inverted use rate structure to promote conservation. It has developed programs for use in the schools outlining water conservation efforts and is developing programs topromote the increased use of treated waste water for golf course irrigation. The requirement for a water conservation plan such as is described and envisioned by the County is a condition of the water use permit proposed, and in addition, the County has adopted an Ordinance, (90-38) which modifies its building code to require installation of water conservation devices in new buildings erected in the County. It has developed proposals for conservation measures such as water auditing, meter testing, leak detection, system looping, and pressure reduction, and has selected the EDR process of water purification as the most efficient use of groundwater resources. Petitioner, Bishop, testified to his belief that approval of this permit and the resultant water withdrawal on the Carlton Reserve would necessitate an expansion of the boundaries of the District's Eastern Tampa Bay Water Use Caution Area to a point where his property would be encompassed therein. In support of his position, Mr. Bishop offered a notice to the effect that new ground water withdrawals would not be permitted within a certain "most impacted area" within the caution area. There was, however, no independent evidence from hydrologists, geologists, or other conservationists, or individuals familiar with the water conservation process, to support Mr. Bishop's contention that either the boundaries would be expanded or that withdrawal of the proposed permitted amounts of water from the Carlton Reserve would cause the boundaries to be expanded. By the same token, Mr. Bishop's contention that theproposed withdrawal from the wells here in issue would adversely effect his ability to draw water from his existing well was not supported by any expert testimony or documentary evidence tending to support or confirm his contention. He had no evidence tending to contradict the County's and District's experts, all of whom indicated there would be no adverse impact on the environment or water resources as a result of the instant permit. Similarly, neither Petitioner offered any evidence of a demonstrative nature that would draw any connection between the proposed permitted withdrawals and potential salt water intrusion and water level drawdown in their wells. The County introduced construction permits issued by its own health department covering 8 of the 12 wells which have been drilled on the Carlton Reserve as test wells. These wells were clearly sunk pursuant to an agreement between the District and the County's public health unit which delegates authority for water well construction permitting to the County. Taken together the documentation indicates that these 12 wells on the Reserve were installed and permitted pursuant to and consistent with appropriate permitting processes, and the testimony of Mr. Bassarab, the County's expert who oversaw the installation of the wells, reflects they are appropriately grouted and sealed. Therefore, there will be no mixing of lower quality water from the lower portion of the Floridan aquifer with the better quality water from the upper portion of that aquifer. The County's evidence clearly refutes the allegation by Mr. Bishop that the 12 test wells currently existingon the Carlton Reserve were neither permitted nor inspected as required by the District. County Commissioner Hill, who testified on behalf of the Petitioners, indicated that the wells applied for here are unnecessary and an inappropriate expenditure of County funds. She claimed there are other valid sources of water available to the County, including that extracted from excavated shell pits and seawater from the Gulf of Mexico which could be treated and desalinated. The Commissioner's comments as to alternate sources are not specifically rebutted. However, she is neither an expert in hydrology or hydrogeology, and her testimony is not persuasive. While other water sources may exist, the better evidence clearly indicates that those sources are not sufficient to meet the County's needs or are otherwise inappropriate for use by the County in sufficient quantity to satisfy those needs.
Recommendation Based on the foregoing Findings of fact and Conclusions of Law, it is, therefore: RECOMMENDED that consumptive water use permit No. 208836.00, providing for authorized quantities as outlined in the intent to issue, subject to conditions contained therein, be issued to Sarasota County. RECOMMENDED in Tallahassee, Florida this 5th day of September, 1991. ARNOLD H. POLLOCK Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 5th day of September, 1991. APPENDIX TO RECOMMENDED ORDER 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 PETITIONERS: Rejected as not supported by the evidence. Accepted. Accepted. - 8. Resolved against the Petitioners on the basis information presented by Respondents. 9.- 13. Accepted and incorporated herein. 14. - 16. Accepted and incorporated herein. Accepted and incorporated herein. & 19. Accepted and incorporated herein. 20. - 23. Accepted. Accepted but not dispositive of any issue. Accepted. & 27. Noted as citation of authority. Rejected. & 30. Accepted as restatements of evidence but not as Findings of Fact. 31. Irrelevant. 32. Rejected 33. & 34. Not a error is, in fact, it is such. 35. - 38. Irrelevant. 39. - 43. Accepted. 44. Accepted. 45. Rejected. 46. Accepted and incorporated herein. 47. & 48. Rejected as a mere citation of testimony. 49. Not understandable. Not a Finding of Fact. 50. Accepted. 51. Evidence is acceptable. 52. Not sufficiently specific to rule upon. 53. Not proven. 54. Not specific. 55. & 56. Rejected. FOR THE RESPONDENTS: 1. - 4. Accepted and incorporated herein. 5. & 6. Accepted and incorporated herein. 7. & 8. Accepted and incorporated herein. 9. - 14. Accepted and incorporated herein. 15. - 17. Accepted and incorporated herein. 18. - 21. Accepted and incorporated herein. 22. & 23. Accepted and incorporated herein. Accepted. - 27. Accepted and incorporated herein. 28. & 29. Accepted and incorporated herein. 30. - 32. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. Accepted. - 37. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. - 43. Accepted and incorporated herein. Accepted. Accepted and incorporated herein, - 48. Accepted and incorporated herein. Accepted - not a Finding of Fact. Accepted and incorporated in substance herein. Not correct as stated. Sarasota County will not be withdrawing saline water from the upper Floridan aquifer. The remaining discussion is accepted. Accepted and utilized. & 54. Accepted. Accepted and incorporated herein. Accepted. - 59. Accepted and incorporated herein. 60. Accepted. 61 - 63. Not Findings of Fact but comments on the evidence. Accepted and incorporated herein. & 66. Not Findings of Fact. COPIES FURNISHED: Wyatt S. Bishop, Jr. 5153 Tucumcari Trail Sarasota, Florida 34241 Joan Jones 719 East Baffin Road Venice, Florida 34293 William A. Dooley, Esquire Nelson, Hesse, Cyril, Smith, Widman, Herb, Causey & Dooley 2070 Ringling Blvd. Sarasota, Florida 34237 Cathy Sellers, Esquire Steel, Hector & Davis 215 S. Monroe Street Tallahassee, Florida 32301-1804 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Edward B. Helvenston, Esquire Vivian Arenas, Esquire SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
