The Issue The issue for determination in this case is whether Florida Administrative Code Rule 62-302.300(6) is an invalid exercise of delegated legislative authority because the rule is vague, fails to establish adequate standards for agency decisions, or vests unbridled discretion in the agency.
Findings Of Fact The Parties The Department is the state agency authorized under Chapter 403, Florida Statutes, to regulate discharges of industrial wastewater to waters of the state. Under a delegation from the United States Environmental Protection Agency, the Department administers the National Pollution Discharge Elimination (NPDES) permitting program in Florida. The Department promulgated the rules in Florida Administrative Code Title 62 that are applicable to the permitting of wastewater discharges. FOPB is a non-profit Alabama corporation established in 1988 whose members are interested in protecting the water quality and natural resources of Perdido Bay. FOPB has approximately 450 members. About 90 percent of the members own property adjacent to Perdido Bay. James Lane is the president of FOPB. Jacqueline Lane and James Lane live on property adjacent to Perdido Bay. IP owns and operates a paper mill in Cantonment, Escambia County, Florida. IP is the applicant for the Department authorizations that are the subject of DOAH Case Nos. 08-3922 and 08-3923. Background When this rule challenge was filed, DOAH Cases Nos. 08-3922 and 08-3923 (the permit cases) involved challenges by these same Petitioners to four Department authorizations for IP: an NPDES permit, a Consent Order, an approved exemption for the experimental use of wetlands pursuant to Florida Administrative Code Rule 62-660.300, and a waiver related to the experimental use of wetlands. IP later withdrew its request for the experimental use of wetlands exemption and the related waiver. Petitioners were ordered to show cause why their claim regarding the invalidity of Florida Administrative Code Rule 62- 660.300 was not rendered moot by IP’s withdrawal of its request for the exemption. Subsequently, the challenge to the validity of Florida Administrative Code Rule 62-660.300 was dismissed as moot. At the commencement of the final hearing on June 22, 2009, FOPB and James Lane announced that they were withdrawing their rule challenges except with respect to Florida Administrative Code Rule 62-302.300(6), and that the only legal ground being asserted for the invalidity of the rule is that it is vague and vests unbridled authority in the Department. Petitioners’Standing Jacqueline Lane, James Lane and a substantial number of the members of FOPB swim, boat, and make other uses of Perdido Bay. Perdido Bay would be affected by IP's wastewater effluent. The challenged rule was applied by the Department to determine that IP's proposed industrial wastewater discharge was in the public interest. The Challenged Rule Florida Administrative Code Rule 62-302.300, is entitled "Findings, Intent, and Antidegradation Policy for Surface Water Quality." Subsection (6) of the rule states: Public interest shall not be construed to mean only those activities conducted solely to provide facilities or benefits to the general public. Private activities conducted for private purposes may also be in the public interest. Most of the permits that are issued by the Department are issued to private entities whose primary purposes are personal uses or the production of private incomes and profits, rather than solely to provide facilities or benefits to the general public.
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.
Findings Of Fact Petitioner, Department of Health and Rehabilitative Services, is the state agency charged with regulating waste water treatment facilities and any sanitary nuisance which may emanate as a result of such operations pursuant to Chapters 381 and 386, Florida Statutes. Respondent, Larry G. Delucenay d/b/a Madhatter Utilities, Inc., owns and operates the Foxwood Waste Water Treatment Plant which is permitted and certified by the Department of Environmental Regulation. Respondent, in operating the Foxwood system, discharges its treated effluent water by means of two percolation ponds and a drip field located adjacent to the Cypress Cove Subdivision in Pasco County, Florida. Respondent owns and controls percolation ponds which are located adjacent to the Cypress Cove Subdivision and pumps human waste from a sewage treatment plant to percolation ponds in the Cypress Cove Subdivision. Respondent's percolation ponds are located approximately 50 ft. west of several residences and the ponds are accessible to the public. The ponds are elevated from 3 ft. to 5 ft. above the adjacent residential lots in the subdivision. However, there is a sand berm approximately 8 ft. high with a 12 yd. base which serves as a barrier between the percolation ponds and the Cypress Cove residences. On August 5, 1991, environmental health specialist Burke observed liquid flowing through the sand berm. He also observed erosion patterns in the sand on the berm which indicated liquid was flowing through it. Mr. Burke, while in the company of two other employees of Petitioner, observed liquid flowing from the percolation ponds onto Lake Floyd Drive to the south of the ponds. An improperly designed nearby lake exacerbated the flooding into Lake Floyd Drive. Respondent's waste water treatment system is designed according to the manufacturer's specifications. Pasco County allowed a number of developments to be built in the area without an adequate drainage system which adversely impacts Respondent's system to the point whereby untreated drainage outfall is draining into the southeast areas in Cypress Cove. Specifically, Respondent's pond #4 is designed to handle a water level up to 67.33 ft. During the investigation of the case, the water level in that pond was approximately 3 1/2 ft. higher than the designed capacity and was therefore causing overflow into the southeast areas of the development. (Respondent's Exhibits A, B and C.) Noteworthy also was the fact that a developer failed to complete a connection which has impacted Respondent's percolation pond and has forced the water to rise approximately 9 ft. higher than the designed capacity which has resulted in an overflow approximately 3 ft. to 4 ft. into the neighboring subdivision. As a result of the overflow, waste water spills over the percolation ponds and prevents the water from draining through the berms as designed. Petitioner's consulting engineer, Robert William Griffiths, credibly testified that a number of agencies having oversight responsibility such as Pasco County, the Southwest Florida Water Management District and the Department of Environmental Regulation, mandated that the drainage system be completed prior to the entire build-up of Cypress Cove. Despite the mandate, the drainage system was not completed and the County allowed the development to continue. Respondent is properly treating and chlorinating sewage in its plant which complies with Petitioner's requirements for the treatment of sewage in systems designed such as Respondent's. Respondent properly treats sewage flowing through its ponds and its berms are properly maintained. As early as October 1989, Respondent consulted and retained an engineer, Gerald E. Towson, who was commissioned to investigate the specifics of designing a waste water treatment plant based on concerns raised by the Department of Environmental Regulation (DER). As a result of that charge, Towson investigated the area and observed flooding and the stormwater runoff in the Cypress Cove neighborhood and attempted to find a solution to alleviate the problem. Consultant Towson also investigated Respondent's treatment plant to determine if the system was functioning as designed. Based on his observation and inspection of the treatment facility, the facility was operating as it was designed and properly filters and treats the effluent. However, based on Respondent's inability to control the stormwater runoff in the neighborhood created by the excess buildup, Towson concluded that there was no workable solution to the problem. As a result of Towson's inability to find a workable solution to handle the concerns raised by DER, Respondent suggested that Towson locate another wastewater treatment site which he found in a surrounding area. Respondent negotiated a lease arrangement with the landowner and initiated the permit process with DER. After the completion of numerous documents and engineering studies required by the Department of Environmental Regulation, Respondent was able to get the leased site permitted by DER as a slow drip irrigation system during March 1991. However, while construction of the system was scheduled to start during March 1991, as a result of vigorous protests from area neighbors, construction was delayed. Respondent thereafter investigated several sites but was unable to fine a suitable area near Cypress Cove. Towson completed a lengthy and cumbersome process in getting Respondent's construction application processed by DER. Initially the application was filed and following a DER review, a Notice of Intent to Issue was given. Hillsborough County thereafter reviewed the project and following their review, Hillsborough County issued its Notice of Intent to Grant and public notice was given. Based on Respondent's inability to comply with the neighbor's concerns regarding setback problems, DER withdrew its permit during May of 1991. Thereafter, Petitioner became involved in connecting with the Pasco County Public System. That connection was ultimately made and the County gave its approval following a delay based on a review occasioned by an employee who had been on vacation. Upon getting the approval, Petitioner ordered the equipment from a supplier which included installation of a magnetic meter and the necessary hookups into the Pasco County System. A "phased in" connection has been completed and the stormwater runoff problem has been abated. When the problems raised by DER and ultimately Petitioner was first brought to Respondent's attention, Pasco County did not have the capacity to handle the hookups required by Respondent's system. Respondent, has been involved in the installation of waste water treatment plants since 1967. Respondent is qualified as a Class "A" Licensee Waste Water Operator. He has been accepted as an expert in numerous administrative hearings. Respondent purchased the Foxwood System during 1982. Respondent utilized a 13 acre tract near Lake Floyd Drive. The system was licensed and designed with a flow capacity of 300,000 plus gallons per day. During the time when the Administrative Complaint was issued, the flow capacity was 220,000 gallons per day. The storm water system which was to have been completed by developers in the area was not connected to the public system and the County granted numerous other permits to daycare centers and several parking lots were constructed for other newly constructed commercial buildings in the area. As a result of the excess runoff created by the development in the area, Respondent's system was impacted and the water level was raised in the percolation ponds to the point whereby an overflow resulted. Petitioner adduced no evidence which showed that any physical or emotional harm resulted from the runoff. At all times while the concerns were being raised by Petitioner and other oversite agencies, the effluents in Respondent's systems were properly treated. Respondent vigorously attempted to abate the runoff created by the excess buildup in the area despite the fact that the problem was raised by Pasco County and over which Respondent had no control. Throughout the process of attempting to find alternate solutions and ultimately getting permitting approval to start construction of an alternative waste water treatment system, Respondent operated in good faith. When no alternate site became available, Respondent initially made application to connect with Pasco County System and that connection has now been made.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that: Petitioner enter a Final Order dismissing the Administrative Complaint herein in its entirety. DONE and ENTERED this 29 day of April, 1992, in Tallahassee, Leon County, Florida. JAMES E. BRADWELL 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 29 day of April, 1992. COPIES FURNISHED: THOMAS W CAUFMAN ESQ HRS DISTRICT V LEGAL OFFICE 11351 ULMERTON RD - STE 407 LARGO FL 34648 RANDALL C GRANTHAM ESQ COTTERILL GONZALEZ & GRANTHAM 1519 N MABRY - STE 100 LUTZ FL 33549 RICHARD S POWER AGENCY CLERK DEPT OF HEALTH AND REHABILITATIVE SERVICES 1323 WINEWOOD BLVD TALLAHASSEE FL 32399 0700 JOHN SLYE ESQ/GENERAL COUNSEL DEPT OF HEALTH AND REHABILITATIVE SERVICES 1323 WINEWOOD BLVD TALLAHASSEE FL 32399 0700
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 Petitioner Ferncrest Utilities, Inc. owns and operates a sewage treatment plant at 3015 Southwest 54th Avenue, Fort Lauderdale, Florida. It presently services the needs of a population of about 2500 primarily located in three trailer parks, certain warehouses, a 153 room hotel, and several other business establishments. The plant was constructed and operated by a lessee of Petitioner's owners, but, in July 1979, Petitioner became the owner and operator of the facility. At that time, it was determined necessary to secure new operators and upgrade the plant equipment and method of process in order to properly service the existing and anticipated future number of customers in the area covered by a Public Service Commission franchise. Although the plant had been operating at a permitted capacity of 0.25 million gallons per day (MGD), Petitioner planned to expand the capacity to 0.60 MGD by modifying the aeration tank, and adding tertiary sand filters and equipment for clarification. Upon assuming control of the plant, Petitioner found that the 0.25 MGD permitted capacity had been exceeded by approximately 120,000 gallons per day for a number of years. Petitioner estimates that a population of 6,000 could be served under its new proposed design capacity. (Testimony of Forman, Exhibit 1) Pursuant to Petitioner's application for a construction permit, dated May 25, 1979, to modify the existing treatment plant, Respondent issued permit No. DC06-21789 on August 6, 1979. The permit specified that it was for construction of additional tank capacity for an existing 0.25 MGD wastewater treatment plant intended to approve effluent quality, and further stated that plant design capacity would remain at that figure. A subsequent letter from Respondent's subdistrict manager to Petitioner on January 15, 1980, stated that an evaluation of the quality of the surface waters receiving the plant discharge and the effect of such increased discharge would have to be made before processing a request for an increase in permitted flow. (Exhibit 7) On February 8, 1980, Respondent issued a temporary operating permit for Petitioner to temporarily operate a 0.25 MGD contact stabilization sewage treatment plant, including additional tank capacity and tertiary filtration. Specific conditions attached to the permit stated that it was issued to give the permittee a reasonable period of time to complete construction of the modification outlined in DER Permit DC06-21789 and for subsequent assessment of the effects of discharge on receiving waters. The conditions further required that the facility continue to achieve 90 percent removal of BOD5 and total suspended solids at all times with specified average daily discharges of such substances. Another condition required that the effluent from the plant be adequately chlorinated at all times so as to yield the minimum chlorine residual of 0.5 parts per million after a minimum contact period of 15 minutes. (Exhibit 8) Thereafter, on July 21, 1980, petitioner filed the instant application for an operation permit for the facility at a design capacity of 0.60 MGD. On October 7, 1980, Petitioner filed a certificate of completion of construction. By letter of December 16, 1980, Respondent's South Florida Subdistrict Manager advised Petitioner that the application for an operating permit had been denied for the reason that monitoring of the Class III receiving waters by the Broward County Environmental Quality Control Board indicated that the dissolved oxygen concentration was frequently below the minimum of 5 milligrams per liter required by Section 17-3.161(1), Florida Administrative Code, and that Petitioner's plant contributed to the substandard conditions in those waters. Petitioner thereafter requested a Section 120.57(1), F.S., hearing. (Exhibits 1-2, 4, 8) Petitioner's plant discharges into the North New River Canal through a six inch effluent pipe. The canal extends from Lake Okeechobee to the intracoastal waterway approximately five miles in distance from the point of discharge of Petitioner's plant. Monitoring of water quality in the canal for the past several years by the Broward County Environmental Quality Control Board shows that the dissolved oxygen concentrations at various sampling stations have ranged from below one part per million to in excess of five parts per million, depending upon the season of the year. However, at no station did the dissolved oxygen concentration reach an average of five parts per million. In addition, the tests also showed that BOD5 is generally low in the canal waters. (Testimony of Mazzella, Exhibits 1, 3, 5) Petitioner's modified plant is now capable of treating 0.60 MGD and meets current basic state requirements of 90 percent (secondary) removal of BOD and total suspended solids. In fact, the plant has tertiary treatment and can consistently operate at a level of 95 percent treatment. The data submitted by the applicant as to effluent water quality characteristics showed removal of 98 percent BOD, 97 percent suspended solids, 50 percent total nitrogen, and 25 percent total phosphorus with an average chlorine residual in the effluent of 0.2 parts per million. The dissolved oxygen level in the effluent has been established at 6.5 milligrams per liter. (Testimony of Hermesmeyer, Dodd, Exhibit 1) Respondent's district personnel took one 24-hour sample of the effluent from Petitioner's plant in March 1981 and determined that a concentrate of 14.6 milligrams per liter of ammonia was being discharged to receiving waters. Respondent therefore determined that the dissolved oxygen levels of the canal would be further degraded because approximately 48 to 50 parts per million of dissolved oxygen would be necessary to offset the effects of oxygen removal resulting from the ammonia discharge. Respondent further found that, although the effluent from the plant had 6.5 milligrams per liter of dissolved oxygen, the amounts of phosphorus and nitrogen being discharged could lead to algal blooms and consequent eventual eutrophication of its waters. Respondent's reviewing personnel therefore considers that there would be negative impacts upon the receiving waters if Petitioner discharged its prior licensed capacity of 250,000 gallons per day, and that a discharge of 600,000 gallons per day would double such impacts. Respondent's personnel therefore believes that although Petitioner's facility meets the basic secondary treatment requirements of Rule 17-6.01, Florida Administrative Code, it does not meet the water quality-based effluent limitation specified in Rule 17-6.10. In order to meet such requirements, it would be necessary to redesign the plant for more efficient removal of nutrients or to redirect the discharge. (Testimony of Mazzella) Other facilities adjacent to or near the North New River Canal discharge directly or indirectly into the canal waters and contribute to an unknown degree to the poor quality of the canal waters. Additionally, agricultural use of land produces stormwater runoff containing fertilizer residue into the canal in an unknown amount. A sewage treatment plant operates at optimum level of treatment when it discharges at about 50 percent of its treatment capacity. (Testimony of Mazzella) In 1983, Broward County will require Petitioner's plant to conform to state advanced waste treatment criteria which will provide for additional removal of nitrogen and phosphorus from effluent. To meet this requirement, Petitioner, plans to investigate the possibilities of utilizing a landlocked lake on its property near the treatment plant as a seepage pond. Although Petitioner's plant is identified in area regional plans to be diverted to the Hollywood wastewater treatment plant in the future, there is presently no target date for tying in to such a regional facility. (Testimony of Hermesmeyer, Exhibit 1)
Recommendation That Respondent issue a permit to Petitioner for the operation of its sewage treatment plant, with appropriate conditions as designed to protect the receiving waters. DONE and ENTERED this 27th day of May, 1981, in Tallahassee, Florida. THOMAS C. OLDHAM Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 27th day of May, 1981. COPIES FURNISHED: Alfred Clark, Esquire Deputy General Counsel Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 Martin S. Friedman and R.M.C. Rose, Esquires Myers, Kaplan, Levinson, Kenin and Richards 1020 East Lafayette Street Tallahassee, Florida 32301 Honorable Victoria Tschinkel Secretary, Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 =================================================================
The Issue The issue to be determined by this Order is whether the Request for Administrative Hearing filed by Petitioner with the Department of Environmental Protection (“DEP”) on February 15, 2013, was timely1/ and, if not, whether the application of the doctrine of equitable tolling would serve to relieve Petitioner of the consequences of having failed to file a petition for hearing within the time allotted by applicable notice provisions.
Findings Of Fact The Parties Petitioner, SRQUS, LLC, is an active Florida, limited- liability corporation, and is the owner of submerged lands and adjacent upland property contiguous to Sarasota Bay. Petitioner is a closely held entity, the only members being Achim and Erika Ginsberg-Klemmt. Respondent, Department of Environmental Protection, is an agency of the State of Florida having jurisdiction for permitting Municipal Separate Storm Sewer Systems (MS4), including duties as a federally-approved state program for the implementation of the Federal National Pollutant Discharge Elimination System (NPDES) Program, pursuant to authority conferred under section 403.0885, Florida Statutes. Respondents, Sarasota County, City of Sarasota, City of Venice, Town of Longboat Key, and Department of Transportation (“DOT”) (collectively the “Applicants”) are responsible for certain existing stormwater point-source discharges to waters of the state from those portions of MS4 facilities owned or operated by one or more of the individual Applicants. The DEP issued a notice of proposed agency action to issue a renewal of an existing MS4 Permit to the Applicants. On January 30, 2013, Sarasota County arranged for the notice to be published in the Sarasota Herald-Tribune, which is a newspaper of general circulation in Sarasota County. The notice provided as follows: STATE OF FLORIDA DEPARTMENT OF ENVIRONMENTAL PROTECTION NOTICE OF INTENT TO ISSUE PERMIT AND REQUEST FOR ADMINISTRATIVE HEARING The Department of Environmental Protection gives notice of its intent to issue a permit to Sarasota County, 1660 Ringling Boulevard, Sarasota, Florida 34236 within its jurisdiction and including the following co- permittees: Florida Department of Transportation District One, Town of Longboat Key, City of North Port, City of Sarasota, and City of Venice, for renewal of a Municipal Separate Storm Sewer System [MS4] permit. Any person whose substantial interests are affected by the proposed permitting decision of the Department may petition for an administrative hearing in accordance with Sections 120.569 and 120.57 of the Florida Statutes (F.S.). The petition must contain the information set forth below and must be filed (received) in the Department of Environmental Protection, Office of General Counsel, Mail Station 35, 3900 Commonwealth Boulevard, Tallahassee, Florida 32399-3000. Petitions must be filed within fourteen days of publication of this public notice or within fourteen days of receipt of the notice of intent, whichever occurs first. A petitioner must mail a copy of the petition to the applicant at the address indicated above, at the time of filing. The failure of any person to file a petition [or a request for mediation, as discussed below] within the appropriate time period shall constitute a waiver of that person?s right to request an administrative determination (hearing) under Sections 120.569 and 120.57, F.S., or to intervene in this proceeding and participate as a party to it. Any subsequent intervention will be only at the discretion of the presiding officer upon the filing of a motion in compliance with Rule 28-5.207 of the Florida Administrative Code. A petition must contain the following information: The name, address and telephone number of each petitioner, the Department Permit Number and the county in which the MS4 is located; A statement of how and when each petitioner received notice of the Department?s action; A statement of how each petitioner?s substantial interests are affected by the Department?s action; A statement of the material facts disputed by the petitioner, if any; A statement of facts that the petitioner contends warrant reversal or modification of the Department?s action; A statement of which rules or statutes the petitioner contends require reversal or modification of the Department?s action; and A statement of the relief sought by the petitioner, stating precisely the action that the petitioner wants the Department to take. Because the administrative hearing process is designed to formulate final agency action, the filing of a petition means that the final action of the Department may be different from the position taken by it in the notice of intent. Persons whose substantial interests will be affected by any such final decision of the Department on the permit revision have the right to petition to become a party to the proceeding, in accordance with the requirements set forth above. Mediation under Section 120.573, F.S. is not available for this proceeding. The permit application file and supporting data are available for public inspection during normal business hours, 8:00 a.m. to 5:00 p.m., Monday through Friday, except legal holidays, at Department of Environmental Protection, NPDES Stormwater Section, 2600 Blair Stone Rd. Room 560, Tallahassee, Florida 32399-2400, phone number (850) 245-8430. Date of pub. January 30, 2013. Because a portion of the Town of Longboat Key extends into Manatee County, the Town of Longboat Key arranged for the notice to be published in the Bradenton Herald, which is a newspaper of general circulation in Manatee County. The notice was published on February 4, 2013. The substance of the notice, except for the date of publication, was identical to that published in the Sarasota Herald-Tribune. Neither Petitioner, nor its representatives, saw either of the published notices prior to the filing of the Petition. On or about February 8, 2012, as a result of the filing of a pre-hearing stipulation in related litigation involving an Environmental Resource Permit (“ERP”) issued by the Southwest Florida Water Management District (“SWFWMD”), Petitioner became aware of the existence of the MS4 Permit. Erika Ginsberg-Klemmt obtained a copy of the permit online, and on February 12, 2013, sent an e-mail to employees of the DEP Ft. Myers? office expressing her general concern with water quality from the disputed stormwater outfall. She expressed her belief that Sarasota County was in violation of the existing MS4 permit, and requested that the recipients of her e-mail “[p]lease be so kind as to look into this matter and let us know what could be done to prevent this unacceptable condition to continue unchecked like it did in the past.” The e-mail did not request any information regarding the MS4 Permit renewal application, nor did it request any information regarding notices or deadlines related to the application. On February 13, 2013, Christopher Wright, a consultant for Petitioner, called the DEP to gather information and do some “legwork” related to Petitioner?s challenge to the SWFWMD?s ERP. The purpose of the call was to determine if information submitted to the DEP in conjunction with the MS4 application, particularly drainage basin maps, could have been of use in the SWFWMD litigation. Mr. Wright spoke with DEP employee, Heather Ritchie, regarding the drainage basin maps that had been submitted to the DEP. During the course of their discussion, Ms. Ritchie advised Mr. Wright that a Notice of Intent to issue the MS4 Permit had been issued by the DEP. However, Ms. Ritchie did not know when Sarasota County had published the notice or when the deadline for challenging the proposed agency action was to run. In short, Ms. Ritchie expressed to Mr. Wright that “she didn?t know what the status of things were.” The discussion then went back to the primary substance of the call, which was watersheds and discharge points. Ms. Ritchie agreed to provide Mr. Wright with an electronic copy of a drainage map from the MS4 Permit file. At 12:43 p.m., on February 13, 2013, Ms. Ritchie sent a map to Mr. Wright via e-mail, and indicated that “[i]f you have additional questions or comments, you may call or e-mail me.” Later on the afternoon of February 13, 2013, Mr. Wright decided that he should ask Ms. Ritchie for a copy of the Notice of Intent. At 5:59 p.m., on February 13, 2013, after the close of business for the day, Mr. Wright wrote to Ms. Ritchie thanking her for her “rapid response to my inquiry today,” and providing her with comments on various basin areas and discharge structures. Mr. Wright concluded his e-mail by stating that “at this time I would also like to request a copy of the Notice of Intent to Issue the MS4 Permit.” The next morning, February 14, 2013, Ms. Ritchie provided Mr. Wright with the Notice of Intent to Issue the MS4 Permit as requested. Later that morning, Mr. Wright inquired as to the time for filing a challenge to the permit. Ms. Ritchie replied at 2:34 p.m. that afternoon that the MS4 Permit “was publicly noticed by the county on January 30th with a 14 day window. The window closed yesterday.” There is no evidence that Ms. Ritchie had any specific information as to the date of publication or the deadline for filing a challenge prior to that communication with Mr. Wright. Petitioner filed the Petition on February 15, 2013. The disputes identified in the Petition were directed exclusively at a 46-acre drainage basin in downtown Sarasota, and a related discharge structure that discharges stormwater from the basin to Sarasota Bay just south of the intersection of U.S. Highway 41 and Fruitville Road. The disputed basin and discharge point are located in Sarasota County.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that Respondent, Department of Environmental Protection, issue a final order dismissing Petitioner?s Request for Hearing and Amended Petition for FLS000004-004 on the ground that the Petition was not timely filed. DONE AND ENTERED this 18th day of October, 2013, in Tallahassee, Leon County, Florida. S E. GARY EARLY 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 18th day of October, 2013.
The Issue Whether General Water Use Permit (WUP) Number 20012185.000 (Permit) meets the conditions for issuance as established in Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, and should be issued to Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc.
Findings Of Fact The Parties DCAP is not-for-profit corporation incorporated in the State of Florida. Behrens is the President of DCAP. See also Findings of Fact 63-77. Farmland Hydro is a Delaware Limited Partnership authorized to transact business in Florida, and is the owner of the property leased by Basso/Redland, which is the subject of this WUP. Frank T. Basso, Jr., is a third generation farmer, who operates as Redland Growers Exchange, and seeks a General WUP to authorize groundwater withdrawals for crop irrigation. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries pursuant to Chapter 373, Florida Statutes, and the rules promulgated thereunder as Chapter 40D, Florida Administrative Code. The Proposed Water Use An Application for a General WUP was submitted by Farmland Hydro and Basso, as co-applicants, and received by the District on April 11, 2001. After receipt of additional information, the Application was deemed complete on October 22, 2001. The Applicants seek a General WUP to authorize a new water use for the irrigation of 140 acres for the production of both Spring and Fall row crops, using a seepage-with-mulch irrigation system.1 Basso plans to grow tomatoes and/or peppers in the Spring, and squash and/or cucumbers in the Fall. Crop planting for both seasons will be phased-in over a one-month period. Water allocation quantities are calculated on a weekly phase-in basis of approximately 35 acres for each planting date. The total time that the parcel will be in use for farming, to include planting and harvesting for each crop, is approximately six months per year. The subject parcel is part of a 250-acre tract known as the Brushy Creek Tract and is located in Hardee County approximately two miles south of the town of Ona; approximately two miles south of the intersection of U.S. Highway 64 and County Road 663; and is within the Southern Water Use Caution Area (SWUCA). The subject parcel currently does not contain a water well. The Brushy Creek Tract is a larger parcel of approximately 1,230 acres leased from Farmland Hydro by Redland and also by Parker Farms for cattle grazing, farming, and hunting. The subject parcel is used for cattle grazing and is surrounded by land owned by Farmland Hydro and used for either cattle grazing or agricultural row crops. Farmland Hydro also operates an additional approximately 1,941 acres of property near the subject parcel, which is used for citrus groves. Farmland Hydro has consumptive WUPs for this property. The closest existing legal user to the proposed Basso well site is another well on the Farmland Hydro property. As is generally done with vegetable crop production in Florida, vegetable crops grown on the Farmland Hydro property are grown in rotation with pasture, and have been rotated in this manner for many years. Typically, farmers have farmed a piece of land for one, two or three years and then, to avoid the buildup of insects and diseases, have allowed the land to revert to pasture and have moved on to another field for crop production. The subject parcel for which the WUP is being sought will be similarly treated. Crop rotation is an important agricultural best management practice that is used to address pest management, soil conservation, and maximizing nutrients for obtaining favorable crop production. Soil conservation is important to Basso, notwithstanding that there is a response in the Application that no approved Soil Conservation Service plan exists for the operation included in the Application. If the WUP is issued and the subject parcel is placed into crop production, another parcel of land will be taken out of crop production by Basso, resulting in the discontinuation of another permitted well. As a result, the issuance of this WUP will not result in a "water use change." Determination of Reasonable Demand/Allocated Quantities In determining whether a proposed water use is reasonable-beneficial and in the public interest, the District calculates the appropriate permit quantities for the particular water use, which is a function of demonstrated need, or demand for water; efficiency of the water treatment and distribution systems; whether water is sold or transferred to other entities; whether acceptable water can be acquired from lower quality sources; and whether conservation practices are employed. District Basis of Review (BOR), page B3-1. The reasonable need for agricultural water use is generally composed of one or more demand components, depending upon the specific agricultural use. "Typically, the reasonable need for irrigation water uses is equal to the supplemental crop requirement divided by the system efficiency or the system design capacity, whichever is less." "The supplemental crop requirement is the amount of water needed for a particular crop beyond the amount of water provided by effective rainfall." The supplemental crop requirement is generally determined by using the Agricultural Water Use Calculation Program (AGMOD) Version 2.1, which is based on the modified Blaney-Criddle method. This program takes into account site specific information such as crop type, growing period, evapotranspiration rate, soil type, rainfall, irrigation method and number of irrigated areas. "In most cases, the supplemental irrigation requirement is determined for a 2 in 10-year drought condition." The AGMOD program determines an inch-application rate which, when applied to the number of acres to be irrigated, results in a calculation of total annual average and peak monthly quantities for the proposed water use. District BOR, pages B3-4 and 3-5. See also District Water Use Design Aids, pages C4-1 through C4-7. In determining the allocated quantities, or reasonable demand for water, the District seeks to avoid both over- allocating water and under-allocating water for the specific crop intended, to ensure that the permitted amount is sufficient for the "2 in 10-year drought condition." Consequently, the allocated quantities arrived at by District staff through use of the AGMOD methodology may be different from the quantities indicated on an applicant's initial application, which are generally estimated without benefit of an agricultural water use calculation program. The AGMOD program was used to calculate water use quantities for the proposed water use. The allocated quantities for Basso's proposed use are 454,000 gallons per day (gpd) on an annual average basis and 1,241,000 gpd, as a peak month quantity. No quantities were requested or allocated for crop protection. See Finding of Fact 52. Modeling for Simulated Impacts As part of the application review process, the District evaluates potential impacts to existing legal uses of water, the water resources and environmental features that may result from the proposed groundwater withdrawals. To assist in the review process, analytical and numerical models, which incorporate best available hydrogeologic parameters for the area being considered for a permit, are used to simulate drawdowns for the withdrawal of the proposed quantities. The results of these simulations are used in the evaluation of potential impacts to assess whether the application meets the conditions for issuance. The District undertook simulation modeling of the potential effects of the proposed water withdrawals to be authorized by the permit. The allocated quantities were entered into the MODFLOW 387 groundwater flow model, which is a three- layer model developed by the U.S. Geological Survey and is the generally accepted model for this purpose. Model layers were set up to represent the surficial, intermediate, and Upper Floridan aquifers. (The Applicants seek to pump water solely from the Upper Floridan Aquifer.) There are limitations to the model in that the model assumes a homogeneous isotropic aquifer, with no preferred flow direction. In actuality, there is variability in the geology of the area. Modeling is intended to serve as a screening tool for assessing localized impacts anticipated from a proposed water use and is based upon the best available information. As distance from the proposed withdrawal site increases, the reliability of the modeling decreases, due to the variability in the geology and other parameters or boundary conditions that can affect the model. Use of the MODFLOW groundwater model allows the District to look at potential impacts at the site, and in the proximity of the site, and assists the District in assessing possible cumulative impacts associated with a proposed use. To assist in assessing potential impacts from the proposed use, a Peak Month modeling simulation was undertaken by the District, which simulates the effect of pumping the proposed Peak Month withdrawal rate of 1,241,000 gpd for 90 consecutive days, with no recharge to the aquifer systems. The model essentially presents a worst case scenario that is a more severe prediction than what is actually likely to occur from the permitted use under normal conditions. Simulating the period of greatest demand on the hydrologic system is likely to provide maximum protection to existing legal water users and the water resources. The Peak Month simulation undertaken by the District predicts drawdowns in the potentiometric surface of the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site; less than 1.4 feet at the nearest property boundary (approximately 1,250 feet from the proposed withdrawal site); and less than 1.2 feet at the nearest existing legal user (a Farmland Hydro well approximately 3,500 feet from the proposed withdrawal site). These numbers did not raise a concern for District staff. ("Potentiometric surface" is "a surface defined by the level to which water rises in an open pipe that is constructed into or all the way through an artesian aquifer. This is measured in feet relative to NGVD or sea level. The level to which water rises inside this open pipe is a function of the pressures on the water in the artesian aquifer." District BOR, page B-xii.) The Peak Month simulation predicts drawdowns in the intermediate aquifer of approximately 0.9 feet at the proposed withdrawal site, and less than 0.9 feet at the property boundary, and at the nearest existing legal user. The Peak Month simulation predicts drawdowns in the water level of the surficial aquifer (water table) of approximately 0.01 feet or less at the proposed withdrawal site, property boundary and nearest existing legal user. Based upon the Peak Month simulations, the District reasonably determined that further cumulative impact modeling was not necessary in order to assess localized cumulative impacts resulting from the proposed use. To assess regional cumulative impacts, the District evaluated Regional Observation Monitoring Program (ROMP) data and found no significant trends in withdrawals in recent years, other than a slight decline attributed to the recent drought. Conditions of Issuance of the Proposed Permit In order to obtain a water use permit, an applicant must establish that the proposed use of water is a reasonable- beneficial use, will not interfere with any existing legal use of water, and is consistent with the public interest, by providing reasonable assurance, on both an individual and cumulative basis, that the water use meets the conditions for issuance as specified in Section 373.223(1), Florida Statutes, and Rule 40D-2.301, Florida Administrative Code. A permit must be obtained from the District prior to withdrawing water, where the withdrawal is from a well having an outside diameter of six inches or more at land surface, where the annual average withdrawal from all sources is 100,000 gpd or greater, or where the total combined withdrawal capacity from all sources is greater than or equal to 1 mgd. The proposed water use falls within these parameters. Rule 40D-2.041(1)(b) and (c), Florida Administrative Code. The quantities allocated for the proposed use have been determined by the District to be necessary to fulfill a certain reasonable demand, for the reasons specified herein. To assist in assessing impacts, the District utilizes a network of ROMP wells to obtain basic groundwater monitoring data over time and to help characterize the lithology, stratigraphy, aquifer depths, water levels and, in some cases, water quality for the various water resources. Data obtained from the ROMP and other wells is compiled to ascertain aquifer characteristics within the District and is also integrated into the District's modeling efforts pertaining to proposed water uses. ROMP well No. 31 is located just off the northeast corner of the Basso site. Having a ROMP well adjacent to the Basso site increases confidence in the specific geological information being used in the groundwater model to assess potential impacts from the proposed uses. ROMP well No. 17 is located approximately 1/2 mile from DCAP member Behren's well. Data from both wells were considered in assessing potential impacts from the proposed water use. Based on available information, the possible sources of groundwater for the proposed use at the Basso site are the surficial aquifer, intermediate aquifer, and the Upper Floridan Aquifer systems. To ensure sufficient quantities of water for the proposed use and to avoid potential impacts to environmental features, such as wetlands and surface waters, the District will require the proposed use to limit withdrawals to solely the Upper Floridan Aquifer. By examining stratigraphic cross sectional information generated from the ROMP wells, particularly ROMP No. 31 well, which is in close proximity to the Basso site, District staff were able to determine, with reasonable certainty, the approximate depths of the aquifers at the Basso well site. To ensure that the well will be open solely to the Upper Floridan Aquifer, the permit requires the Basso well to have a minimum of 400 feet of casing, with an estimated well depth of 1,000 feet. Based upon available information concerning the construction of other wells in the vicinity of the proposed Basso well, the District is reasonably assured that a well cased for a minimum of 400 feet will draw water only from the Upper Floridan Aquifer and will minimize the potential for water to move between the aquifers through the well. The well construction requirements imposed for Basso's well are in line with the best available stratigraphic information and with known construction of wells in the area. By casing the well to a depth of 400 feet and due to the extremely low leakage of the intermediate confining unit, the intermediate and surficial aquifers will be buffered from impacts associated with the proposed use. The District will deny a water use permit application if the proposed withdrawal of water, together with other withdrawals, would cause an unmitigated adverse impact on a legal water withdrawal existing at the time of the application. The District considers an adverse impact "to occur when the requested withdrawal would impair the withdrawal capacity of an existing legal withdrawal to a degree that the existing withdrawal would require modification or replacement to obtain the water it was originally designed to obtain." District BOR, page B4-14. Based upon an assessment of individual and cumulative regional information, there are no existing legal uses of water that will be adversely impacted as a result of the proposed withdrawals. Based upon an assessment of individual and cumulative regional information, no quantity or quality changes that adversely impact the water resources, including both surface and groundwaters, are anticipated from the proposed withdrawals. The District requires that consideration be given to the lowest water quality available, which is acceptable for the proposed use. Lower quality water includes reclaimed water, collected stormwater, recovered agricultural tailwater, saline water or other sources. District BOR, page B4-12. For the proposed water use, there is no viable lower quality water source and no reclaimed water available near the site to use as an alternative to groundwater pumping. The Applicants are proposing to use the lowest quality water that is available. There are no known concerns regarding the quality of water in the Upper Floridan Aquifer at this location in Hardee County. Restricting the proposed water use to the Upper Floridan Aquifer will not cause water quality concerns or result in pollution to any of the aquifers. Simulated drawdowns to the Upper Floridan Aquifer of approximately 2.6 feet at the proposed withdrawal site, less than 1.4 feet at the nearest property boundary, and less than 1.2 feet at the nearest permitted well, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the intermediate aquifer of 0.9 feet at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, provide reasonable assurance that adverse impacts will not occur from the proposed water use. Simulated drawdowns to the surficial aquifer of 0.01 feet or less at the proposed withdrawal site, and less as the distance from the proposed withdrawal site increases, constitute a nearly undetectable impact to the surficial aquifer, which is not an adverse impact. The modeling simulations demonstrate that the proposed withdrawals will have no significant effect on the surficial aquifer and, therefore, will not cause adverse impacts to environmental features such as wetlands, lakes, streams, fish and wildlife, or other natural resources. None of the simulated drawdowns are considered to be predictions of adverse impacts, not even in the localized vicinity of the well site. Mr. Jackson explained that because the localized modeling simulations were small or insignificant and showed no adverse impacts, cumulative modeling is not considered necessary. Reasonable assurance on a cumulative basis is determined by assessing the potential localized impacts in conjunction with existing cumulative data for the region, such as the available ROMP data and hydrographs, which depict the existing regional condition, taking into account, on a cumulative basis, all existing uses as well as rainfall conditions and climate. Based on an assessment of the cumulative data and the modeling for individualized impacts, and applying professional judgment, District staff reasonably concluded that the proposed water use presents no concerns that it will cause, on either an individual or a cumulative basis, adverse impacts to the water resource or existing legal uses. Minimum flows and levels have not been established by the District for the area where the proposed use is located. (The parties stipulated that the District has not established minimum flows and levels pursuant to Section 373.042, Florida Statutes, for the Southern Water Use Caution Area (SWUCA)). Therefore, Rule 40D-2.301(1)(d), Florida Administrative Code, (requirements for minimum flows and levels), is not applicable to the proposed permit. The proposed use presents no concerns for saline water intrusion. The proposed use raises no concerns regarding causing pollution to the aquifer. There are no offsite land uses that will be adversely impacted as a result of this permit. Basso currently uses best management practices for water conservation in his ongoing farming operations, and intends to use such practices with the new farming operation authorized under the permit. In keeping with such practices, irrigation is stopped when the water reaches the end of the watering ditch. Basso uses seepage irrigation and tries to regulate the ditches so that there is a minimum, if no, runoff. Also, a watering cycle generally lasts from three to seven days before irrigation has to be resumed. Any runoff goes into "filtering ponds, before reaching ditches or creeks" in its raw content. Basso does not intend to farm during months of likely frost so no separate allocation for frost/freeze protection was requested or needed. Given these irrigation practices, water is not reasonably expected to be wasted. All necessary and feasible agricultural water conservation activities will be implemented upon issuance of the WUP. In addition, Specific Condition No. 3 of the proposed WUP requires the incorporation of best water management practices in all irrigation practices. The proposed use presents no concerns that it will otherwise be harmful to the water resource. The Applicants have met all the requirements for issuance of a WUP. Southern Water Use Caution Area The proposed water use site is located within the SWUCA. The District established the SWUCA as a means of addressing on a regional scale concerns about long-term impacts to the water resource. Water use caution areas were created in recognition of regional water concerns. There have been drought conditions in the area which have caused reduced aquifer levels. The proposed water use site is not within the "Most Impacted Area" (MIA), which is located approximately 18 miles to the west of the site in Manatee County, nor within the "East Tampa Bay Water Use Cautionary Area" (ETB WUCA), which is approximately six miles to the west of the proposed site, also in Manatee County. (The SWUCA includes the MIA and ETB WUCA.) Pending final adoption of rules for the SWUCA, the District will continue to issue WUPs for proposed water uses that meet the conditions for issuance. The District cannot treat new uses and existing renewal uses any differently when considering the issuance of a permit. Once SWUCA rules and minimum flows and levels are established, the District expects to rely on a more regional approach to address long-term cumulative impacts over the entire use caution area, instead of relying on a permit-by-permit basis to address regional concerns. Standard Condition No. 9 of the proposed WUP requires the permittee to cease or reduce withdrawals as directed by the District, if water levels in the aquifers fall below the minimum levels established by the District Governing Board. The proposed withdrawal will use a seepage with mulch irrigation method, which has a 50 percent efficiency level. See footnote 1. This is the minimum efficiency level currently required for agricultural WUPs within the SWUCA, which approve the use of this irrigation method. As SWUCA rules come into effect, a higher percentage efficiency level probably will be required, as is now required in the Eastern Tampa Bay Water Use Caution Area and also in the Highlands Ridge Water Use Caution Area. Consequently, Standard Condition No. 11 of the proposed WUP requires that, when SWUCA rules are implemented, the permittee must comply with any higher efficiency level or other special regulation that may be required for the SWUCA area. DCAP's Challenge to the Proposed WUP DCAP does not keep official membership records. It does not maintain any list of current members. According to Behrens, there are five members of the board of directors. DCAP does not hold corporate meetings, annual meetings or maintain corporate records. Members do not meet. There are no means to document the existence of members for this organization. Behrens is a member of DCAP. He has owned five acres adjoining the west side of Horse Creek (in DeSoto County) since 1985. Behrens complains that the District does not look at the cumulative effect on his well and other people he knows, such as George Chase. Behrens is concerned with any lowering of the water level in the area, including Horse Creek. He believes that approval of wells in the area, including the proposed well, is the straw that is breaking the camel's back. Mr. Chase shares this view. Behrens relies on an artesian free-flowing, two-inch diameter well, for domestic water use, located in the intermediate aquifer, approximately 150 feet deep. (Behrens' well is approximately 18-20 miles from the proposed Basso well.) For most of the time he has lived there, the well had an electric pump for obtaining water. Approximately one year ago, the pump went bad, and a replacement system has not been installed. Currently, Behrens has no pump on the well, and in dry periods, has to obtain water for domestic uses from nearby Horse Creek, which is low during the dry season. (Behrens depends on Horse Creek to pursue his recreation, wildlife, and aesthetic values.) Having a flowing artesian well will enable him to obtain water from the well without having to install an electrical pump, a situation which is desired by Behrens, in part, because the property is in a flood plain and experiences frequent flooding and electrical outages. Not all artesian wells flow. Artesian wells are completed into confined aquifers in which the water in a tightly cased well, will rise to a level above the formation being measured. Water would have to rise above the land surface to be a flowing well. For a well to be artesian, the well must be under confined pressure. For a well drawing water from a confined aquifer, such as the intermediate or the Upper Floridan Aquifer systems, the measured water level in the well is a reflection of the amount of potentiometric pressure in the well. This level can be affected just as much by the amount of recharge as it can by the amount of water withdrawals. There is no evidence that the proposed water use will adversely impact the flowing nature of either Behrens' or Chase's well. The evidence demonstrates that the proposed water use will not adversely impact Behrens' well. George Chase is a member of DCAP. Mr. Chase lives in Arcadia, DeSoto County, Florida. His property is adjacent to the Peace River. Mr. Chase's well is a two-inch diameter well, believed to be about 150 feet deep and equipped with a 12-volt DC solar-powered pump. Mr. Chase has in the past relied on artesian pressure within the confined intermediate aquifer to supply water to his solar-powered home. The solar-powered pump assists in supplying water to the home. In recent years, Mr. Chase has experienced low water pressure in his well. In Spring 2000, Mr. Chase contacted the District to complain that when an adjacent citrus grove was irrigating the groves, it appeared to affect the water level in his well such that the well's ability to flow was impacted. (According to Mr. Chase, his neighbors have had problems obtaining sufficient water from their wells and reaching water with standard pumps.) This citrus grove is an existing legal user of water that pre-existed Mr. Chase's well. In recent years, numerous domestic wells have been constructed in the vicinity of the Chase home that are large diameter wells utilizing submersible pumps with 110-volt AC power. These wells are more efficient at producing water than the type of well and pump being used by Mr. Chase, are located within a few hundred feet of Mr. Chase's well, and are open to the intermediate aquifer as is the Chase well. Based upon the District's experience in other areas, where there is a cluster of domestic wells drawing from the same intermediate aquifer, such adjacent wells have a much greater impact on each other than do other more distant wells, such as the previously discussed citrus irrigation wells, that are open solely to the confined Upper Floridan Aquifer System. This conclusion is based upon monitoring of the ROMP sites in the affected areas. Mr. Chase's well is approximately ten miles from the proposed withdrawal site. There is no basis to conclude that the proposed water use will cause any adverse impacts to Mr. Chase's well. DCAP members' interests are not affected any differently by the proposed use than are the interests of the general public. DCAP has produced no evidence to support its assertion that the issuance of this permit will result in lowered water levels in the Horse Creek and Peace River or other surface waters. DCAP has produced no evidence to support its assertion that the permit will cause adverse impacts to surface water flows or surface waters or to environmental features such as vegetation, fish, and wildlife. DCAP has produced no evidence that its substantial interests are affected by the proposed agency action.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that Southwest Florida Water Management District enter a final order: Determining that Farmland Hydro Limited Partnership and Frank T. Basso, Jr. and Redland Growers Exchange, Inc., have satisfied the requirements of Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, regarding conditions for issuance of WUPs;3 Issuing proposed General Water Use Permit No. 20012185.000, as set forth in District Exhibit No. 4; and Finding that DCAP lacks standing to challenge the issuance of the permit. DONE AND ENTERED this 3rd day of June, 2002, in Tallahassee, Leon County, Florida. CHARLES A. STAMPELOS Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 3rd day of June, 2002.
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 Whether the Respondent committed the violations alleged in the Administrative Complaint dated January 8, 1999, and, if so, the penalty which should be imposed.
Findings Of Fact Based on the oral and documentary evidence presented at the final hearing and on the entire record of this proceeding, the following findings of fact are made: The Department of Health, including the county health departments such as the St. Lucie County Health Department ("County Health Department"), are responsible for supervising and controlling limited use public water systems. Section 381.0062(3), Florida Statutes (1997). Mr. Gorman is the owner of three duplexes located at 120 and 122 Laidback Way, Fort Pierce, Florida; 140 and 142 Laidback Way, Fort Pierce, Florida; and 160 and 162 Laidback Way, Fort Pierce, Florida. The duplexes were built in 1982 and 1983 and each contains two units which are available for rent. Water is piped into each duplex from a well located on the property. The wells providing water to 120 and 122 Laidback Way and to 140 and 142 Laidback Way were inspected by the Department of Health and Rehabilitative Services in May 1994 and found to be satisfactory pending results of water tests. Two-day bacteriological analyses were conducted on May 2 and 3, 1994, on the wells serving these two properties, and the results were satisfactory. 3/ The 1994 inspection report for the well serving the property at 120 and 122 Laidback Way reflects that it had the following equipment: a one-half horsepower pump; a 30-gallon "p tank"; a 20-gallon water softener filter; and a 30-gallon brine tank. The 1994 inspection report for the well serving the property at 140 and 142 Laidback Way reflects that it had the following equipment: a one-half horsepower pump; a 20-gallon "p. tank"; a 25-gallon water softener filter; and a 40-gallon brine tank. In a letter dated August 21, 1998, the County Health Department notified Mr. Gorman that he needed to submit the application enclosed with the letter and a $140.00 fee to bring the "permit" to current status for the property located at 140 and 142 Laidback Way. The letter was inartfully composed and conveyed incomplete information regarding the nature of the permit. The letter did, however, contain reference to "Chapter" 381.0062, Florida Statutes, and Chapter 64E-8, Florida Administrative Code, and it also provided notification that Chapter 64E-8 required quarterly sampling of limited use public water systems for bacteria and a lead and nitrate test every three years. The County Health Department sent Mr. Gorman an identical notice, dated August 21, 1998, regarding the property located at 160 and 162 Laidback Way. The County Health Department sent Mr. Gorman a somewhat different letter, dated August 31, 1998, regarding the "Limited Use Public Water Systems" for the property located at 120 and 122 Laidback Way. The letter notified Mr. Gorman that his permit to operate the "referenced water system has expired as of September 30, 1998." The letter reiterated the information contained in the August 21 letter and requested in addition that Mr. Gorman submit "a minimum 8.5 x 11 inch site plan of the system, drawn to scale, that accurately identifies the location of the source of water in relation to property boundaries and contaminant sources, i.e., well must be 75 feet from septic system, etc." and an "[e]quipment list: pump, tank, softener, automatic chlorinate, etc., manufacturer, model #, and capacity." Finally, Mr. Gorman was notified of the permitting and testing fees and told that the "[a]pplication with required site and equipment information must be submitted with necessary fees within 30 days receipt of this notification." Mr. Gorman responded with a letter dated October 16, 1998, in which he posed several questions to the County Health Department: Do you understand that these are duplexes? Are all rental properties including single family subject to these regulations? Can you give me a valid reason why rental units of two units or more should be subject to quarterly bacterial testing (I believe the statute only authorizes it annually) and not all other residential properties, public facilities or otherwise that might use well water? Mr. Gorman requested a response to his questions but did not provide the information, applications, and permit fees requested in the letters dated August 21 and August 31. In a letter dated December 14, 1998, sent certified mail with return receipt requested and referenced as a Notice of Violation, the County Health Department notified Mr. Gorman that he was operating limited use community public water systems without a permit at 120 and 122, 140 and 142, and 160 and 162 Laidback Way and that he had not provided the following required information: Signed, dated application form. An operation permit fee of $75.00 for the initial permit. A site plan of the property that accurately identifies the location of the well in relation to property, boundaries and contaminant sources such as septic tank systems. Capacity/size, model and brand information on system components. Well completion report if available or year well was installed if known. Required chemical analysis results (lead and nitrate). Initial satisfactory two-day source (well) water and system water bacteriological tests results. Mr. Gorman was told to contact Bruce McLeod within five days of receipt of the notice. Although Mr. Gorman received the notice on December 16, 1998, he did not respond. The County Health Department had not, as of the final hearing, received any reports of illness attributable to the water from the wells at the subject properties, and it does not have any reason to believe that the wells are contaminated. Mr. Gorman had not, as of the final hearing, submitted the applications, permit fees, or information requested by the County Health Department, and he had no operating permits for the wells providing water to the subject properties. The evidence presented in this case is sufficient to establish that the wells providing water to the three duplexes owned and rented by Mr. Gorman each contains two rental units and are limited use community public water systems. Mr. Gorman must have operating permits for the wells providing water to these properties.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Health enter a final order: Finding that Robert J. Gorman is guilty of three violations of Section 381.0062, Florida Statutes (1997), because he failed to obtain operating permits for the limited use community public water systems he maintains at 120 and 122, 140 and 142, and 160 and 162, Laidback Way, Fort Pierce, Florida; and Imposing an administrative fine in the amount of $1500.00, or $500.00 for each of the three violations. DONE AND ENTERED this 25th day of June, 1999, in Tallahassee, Leon County, Florida. PATRICIA HART MALONO 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 June, 1999.