The Issue The issues determined in this proceeding are whether Respondent engaged in construction contracting without a license as alleged in the Amended Administrative Complaint; and, if so, the appropriate penalty.
Findings Of Fact Parties Petitioner is the state agency responsible for regulating the practice of construction contracting pursuant to section 20.165 and chapters 455 and 489, Florida Statutes. Petitioner has jurisdiction over the unlicensed practice of construction contracting pursuant to sections 455.227, 455.228, and 489.13. At all times material to this matter, Respondent was the owner of Advanced Connections, LLC. Neither he nor his company is licensed, registered, or certified to perform construction contracting services in Florida. Respondent holds only certification to perform backflow preventer testing. At the heart of this case is whether Respondent may perform backflow preventer repair without a license, certification, or registration. Facts Related to Work Performed It is undisputed that Respondent performed repair of backflow preventers for customers in Tallahassee, Florida. On July 25, 2014, Respondent performed a backflow prevention assembly test on two existing backflow preventers at Old Enrichment Center located at 2344 Lake Bradford Road, Tallahassee, Florida 32301. Respondent provided an invoice to Old Enrichment Center following the backflow test, which described the work performed as follows: “I was able to repair both units and they are Functioning [sic] properly. I had to replace one additional part on, AS #10896, the #2 check cage was cracked. Thank you For [sic] your business. Don’t forget to cover the backflows.” The invoice reflected that Respondent was compensated $343.00 for the worked performed and materials. On August 20, 2014, Respondent performed a backflow test on an existing backflow preventer for Li-Ping Zhang at a property located at 2765 West Hannon Hill Drive, Tallahassee, Florida 32309. Respondent provided an invoice to the customer describing the outcome of the test, and he provided an estimate for repair as follows: Invoice: Thank For this opportunity to serve you. The unit is failing. The #1 check valve is leaking across it. That means it is not holding pressure. The Manufacture of flowmatic no longer makes parts for your unit. But my supplier does have a repair kit available. Due to the Fact are no longer made for your device it may be better to have the unit replaced with a Wilkins 975-XL. Please See Quote * * * Quote for repair: Part: Complete Rubber Kit-$30.00 Labor: This unit may not be repairable due to the fact that there is a limited supply of parts. If there is damage to the #1 Check. I will not be able to repair the unit. If that happens I can return the parts but a labor charge would still remain. Please call with any questions. Thank you. (Quoted text from invoice without correction of grammar.) Respondent ultimately performed the repair on August 25, 2014. The invoice issued to Li-Ping Zhang reflected service provided as “[t]he repair was a success. The unit is Passing [sic]. Paid Cash $115.00 8.25.14 — signed Ian.” Both invoices include the Respondent’s company name, Advanced Connections, LLC. There was no evidence presented of financial or property harm caused by Respondent’s actions. On or about February 2, 2015, Petitioner received a complaint from City of Tallahassee filed against Respondent for his repair of backflow preventers in Tallahassee, Florida. Petitioner commenced an investigation into Respondent’s actions through its unlicensed activity investigation unit. At the conclusion of the investigation, Petitioner filed an Administrative Complaint alleging Respondent engaged in construction contracting without a license. Respondent disagrees with Petitioner and argues that he is eligible for an exemption under section 489.103(9), commonly known as the “handyman” exemption. Life-Safety Matter Respondent’s eligibility for the exemption hinges upon whether repair of a backflow preventer is considered a life- safety matter. The Florida Building Code provides minimum standards for building construction to “safeguard the public health, safety and general welfare.” See § 101.3, Florida Building Code, Building. The Florida Building Code, Plumbing, applies to “the installation, alteration, repair and replacement of plumbing systems, including fixtures, fittings and appurtenances where connected to a water or sewage system . . . .” See § 101.4.3, Florida Building Code, Building. The plumbing chapter of the Florida Building Code defines a backflow preventer as a device or means to prevent backflow of water from flowing from one system into the potable water system.2/ A potable water supply system shall be maintained in such a manner so as to prevent contamination from non-potable liquids, solids, or gases being introduced into the potable water supply through cross-connections or any other piping connections to the system. § 608.1 Building Code, Plumbing. To further explain the purpose of backflow preventers, Petitioner offered Frank Hagen as a plumbing expert. Mr. Hagen, who has 42 years of plumbing experience, has been licensed in Florida since 1981 and is also licensed in Georgia. He holds a certification in backflow preventer testing (issued by the University of Florida TREEO Center) and backflow preventer repair. Mr. Hagen has regularly conducted on-the-job plumbing training for 36 years. Mr. Hagen was accepted as a plumbing expert. Mr. Hagen testified that a backflow preventer is a life-safety device. He explained that this reference is accepted throughout the plumbing industry because the backflow preventer protects water systems by preventing chemicals and poisons from entering the public water system. Mr. Hagen provided examples of potential outcomes if a backflow preventer fails (e.g., three children died as a result of drinking water from a water hose where poison in the sprinkler system contaminated the water). Mr. Hagen also testified that only a licensed plumber is authorized to perform backflow repairs. Mr. Hagen’s testimony is credible. John Sowerby, P.E., a licensed professional engineer for 35 years, who previously worked in the Department of Environmental Protection’s (DEP) Source of Drinking and Water Program, also testified regarding the nature of backflow preventers. He testified that backflow preventers protect public health because they prevent contamination of potable water systems (i.e., water that is satisfactory for human consumption). Mr. Sowerby’s testimony is also found to be credible. Respondent’s testimony that a backflow preventer is not a life-safety fixture, is not supported by the evidence. Respondent testified that backflow preventers are “plumbing fixtures” that are installed between the public water supply line and the private water supply line. Respondent also testified that if a backflow preventer fails, it could cause contamination of the public water supply and public health would be at risk. More importantly, the applicable building codes and the testimony of Mr. Hagen and Mr. Sowerby establish that backflow preventers prevent contamination of public water supply and protect public health. Given that backflow preventers safeguard public health by protecting the public water supply, they involve life-safety matters. The Department has incurred investigative costs in the amount of $415.95 related to this matter. Ultimate Findings of Fact Respondent’s repair of a backflow preventer on a water service line is a life-safety matter and as a result, Respondent is not eligible for an exemption under section 489.103(9). The evidence is clear and convincing that Respondent’s repair of a backflow preventer at the two properties referenced herein constituted the practice of construction contracting without a license. As a result, Respondent is guilty of unlicensed contracting, as charged in Counts I and II of the Amended Administrative Complaint.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Business and Professional Regulation issue a final order that: Finds Respondent guilty of unlicensed contracting in violation of section 489.13(1), as alleged in Counts I and II of the Amended Administrative Complaint; Imposes an administrative fine of $6,000 ($3,000 for each count); and Requires Mr. Tuttle to pay the Department’s investigative costs of $415.95. DONE AND ENTERED this 26th day of October, 2016, in Tallahassee, Leon County, Florida. S YOLONDA Y. GREEN 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 October, 2016.
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.
The Issue The issue for consideration in this matter is whether Respondent’s license as a water well contractor should be disciplined because of the matters alleged in the Administrative Complaint and Order entered herein by the District.
Findings Of Fact At all times pertinent to the issues herein, the Southwest Florida Water Management District (SWFWMD) was the state agency responsible for the conservation, protection, management, and control of water resources within its boundaries, and consistent therewith, the licensing of water wells therein; and for the licensing and regulation of water wells and water well contractors within the district. The three wells in issue herein were within the jurisdiction of the Petitioner, and Respondent was a water well contractor licensed by the District. On June 4, 1998, Respondent signed a contract with Karen Anne Grant, to drill a four-inch domestic water well on her property located at 33442 Larkin Road, Dade City, Florida. The property, on which Ms. Grant was building a residence, was a part of a pre-existing citrus grove. After application by the Respondent, SWFWMD issued WCP No. 606175.01 to him on June 1, 1998, and Respondent began construction of the well on June 15, 1998. His application reflected the well was to be drilled using the cable-tool method. Construction was completed on the well on or about July 7, 1998, but because the well was vandalized during construction by the dropping of an unknown substance (probably a piece of casing) down the well, the well was unsatisfactory and was not used. Respondent attempted to repair the well but was unable to do so. Respondent claimed the well was unusable and he would have to drill another one. Although he did not obtain a permit to close the well, he subsequently did so. He was paid $5,375.00 to dig this Well (No. 1). Because of the failure of Well No. 1, Respondent applied to the District for and received WCP No. 613349.01 on December 9, 1998, to construct a second four-inch water well on Ms. Grant's property. This was Well No. 2. He began construction that day and completed it on January 27, 1999. From the time of its initial use, Well No. 2 produced water which contained unacceptable amounts of sediment, debris, and sand. In addition to the unsatisfactory quality of the water it produced, Well No. 2 also failed to produce a sufficient quantity of water for domestic potable water use or grove irrigation. Respondent admitted to Ms. Grant that Well No. 2 was not satisfactory for grove irrigation, and in an effort to fix the water quality problem, installed a sand filter and sedimentation tank. Well No. 2 was not properly closed. It was covered with a PVC cap instead of a tamper-resistant watertight cap or valve as required, and Respondent did not properly seal the upper terminus of the well. Without obtaining a third WCP, on February 25, 1999, Respondent started construction of a third well on the Grant property. Respondent contends WCP No. 613349.01, pulled for Well No. 2, was not for that well but for Well No. 3. He argues that the second well was so close to the first well that he did not feel another permit was required. Though Well No. 3 was completed and produces water, the water quality is poor. It contains sand, sediment, debris, and rock, which results in clogging of plumbing fixtures at the Grant home. In addition, the volume of water produced is insufficient for comfortable home use. Well No. 3 is open down to 178 feet below land surface, beyond which point it is obstructed by sand. Use of a diagnostic tool available to the District reveals that the sand seems to be coming from around the well casing. Ms. Grant initially contracted with Respondent to dig her well in June 1998. Although Petitioner disputes it, the location of the well near the new house she was building was, she claims, by mutual agreement. Respondent did not express any dissatisfaction with the location of this or either of the other wells, He said he was familiar with the area and had worked all around there. Respondent started work on Well No. 1 on June 15, 1998 and it was completed on July 2, 1998. The house was not yet completed, and electric service had not been installed, though it was being arranged for. Before the well could be put in operation, however, Respondent claimed it was vandalized and his equipment, which he had left at the site, stolen. At this point, Respondent told Ms. Grant that he had run into an obstruction which he believed was pipe which had been dropped into the well at more than 100 feet. He said he had tried to get it out, but could not, and had to drill another well. The casing of Well No. 1 was not cut off at that time. Ms. Grant later discovered it had been cut off and plugged, but she does not know who did that. Ms. Grant used Well No. 2, which was located about 20 to 30 feet west of Well No. 1, for just about two months but was never satisfied with the amount or quality of the water it produced. Not only was the water quality low, but there was also insufficient volume for grove irrigation, one of the intended uses of which she had advised Respondent. When Grant complained to Respondent about the water quality, he suggested she run hoses constantly to clear the sand out. In February, 1999, just after Ms. Grant contacted the District to complain, Respondent said he would come by to cap Well Nos. 1 and 2, and start Well No. 3. On February 25, 1999, Respondent started Well No. 3 at a site about 200 feet north of Well Nos. 1 and 2, agreed upon by the parties after some discussion, and on March 5, 1999, he completed it. Respondent billed Ms. Grant $3,271 for this well, in addition to the $5,375 paid for Well No. 1 and the $4,585 paid for Well No. 2. Whereas the builder paid for the first two wells, Ms. Grant paid for Well No. 3, but she had the same problems with Well No. 3 that she had had with the prior two wells. An irrigation company called in to see what could be done to get water to the citrus grove indicated there was too much sediment in the water and not enough flow. About a year after Well No. 3 was completed, the Grants noticed the water pressure was dropping, and when they went to the well site, they noticed the pump was constantly running. As a result, they called another well driller who pulled the pump and replaced the impellers. After that, Ms. Grant contacted Respondent about the fact that the wells he had drilled had never worked properly. All he would recommend was to keep the hoses running. He indicated he would try to develop the well to rid it of debris but when he tried, he was unsuccessful. As a result of the situation with the three wells, the Grants had no water to their home; the pumps they installed were destroyed; they were unable to irrigate their 8-acre citrus grove; they suffered a resultant loss of income; and, they were forced to drill a fourth well. When Well No. 1 was closed, the casing was cut off at or below ground level. It did not extend one foot above the land surface, nor was the casing capped or sealed with a tamper- resistant watertight cap or valve. Examination of the well site by Sharon Lee Vance, then a technician IV for the District, on May 25, 1999, based on a complaint filed by Ms. Grant, revealed that the water quality was poor - cloudy with excessive sand and rock particles. Ms. Vance tried to contact Respondent, whose name appeared on the permit as contact, by phone but always got his voice mail. Though she left messages requesting him to call back, he never did. Ms. Vance went back to the Grant site in July 1999 in the company of other District personnel. At this visit, Ms. Vance learned there were two wells. She located both and found that Well No. 1 was buried. When she first saw that well, she noted that it had been cut off below the surface, a fence post had been driven into the top, and the well had been buried. In Ms. Vance's discussions with Ms. Grant about this well, Ms. Grant categorically denied she was the one who cut off the top of Well No. 1 or buried it. She does not have access to the cutting equipment used to cut off the top of the well. Such equipment, however, is commonly used by well contractors. It was obvious to Ms. Vance that Well No. 1 had several problems. It was clearly not suitable for its intended use because it was cut off below ground level and was obstructed. It had not been properly abandoned. Though she dug down approximately one-and-a-half feet all the way around the casing, she could find no evidence of bentonite or any other approved closing medium. Even though Respondent now claims the second permit he pulled was not for Well No. 2 but for Well No. 3 instead, the permit itself appears to authorize the construction of Well No. Ms. Vance found several problems with this well, also. It was not properly sealed with bentonite or any other properly approved closure medium; a PVC cap had been applied to the top instead of a waterproof or tamperproof cap, and the PVC cap was cracked; the well was not suitable for its intended purpose because it was obstructed and produced both insufficient and poor quality water; and it was not properly abandoned. Ms. Vance observed a metal plate placed around the well top. She does not know what purpose it was to serve, but based on her experience and her examination of the site, she believes it was placed there to keep the casing from falling into the well. Notwithstanding, Ms. Vance's opinion that the second permit was for Well No. 2, Respondent contends he believed the permit for Well No. 1 was adequate to permit drilling of Well No. 2 without a new permit. Though his belief is incorrect, he admitted to obtaining a permit for Well No. 3. Therefore, it is found that Well No. 2 was not properly permitted. Well No. 3 was permitted. The water in Well No. 3 was not of good quality. She examined the sand filter which had been installed by the Respondent and found it to be full of sand. So was the settling tank. She also noted debris and unusual sediment around the well head. Based on water samples taken at the well, and the observations made, it was clear to Ms. Vance that the well was not properly seated and was pumping sand. Further, the well casing did not extend down to the static water level, and the well was not properly permitted. Ms. Vance further noted that the water from Well No. 3, in addition to the excessive sand, also had large pieces of rock and chunks of clay in it. This was unusual and indicated to her that there was a problem with the well's construction. The casing integrity as not good, which permitted an infusion of contaminant into the well. This condition is not unusual during the first day or so of a well's operation, but it usually clears up after that. In this case, it did not. Ms. Vance admits she does not know who cut Well No. 1 off below ground level. She knows the well was not properly abandoned as required by rule, however, because it was not properly grouted with neat cement grout or bentonite. She dug down beside the well for a total of two and a half feet without seeing any evidence of grout or bentonite. The fact that the well had pipe dropped into it, and the existence of the cutting off of the pipe below ground, made it inappropriate for the intended purpose of providing water for the home. Ms. Vance she does not know who cut off the pump; Ms. Grant does not know who cut off the pipe; and Respondent denies having done it. Though the work was clearly done by someone with access to well drilling tools, Respondent was not the only driller to work at the site. Therefore, it cannot be found that Respondent cut the pipe off below ground. It is clear, however, that Respondent failed to properly abandon and close Well No. 1, when he found it unusable, and it was his responsibility to do so. Well No. 2 also was not properly sealed by Respondent, according to Ms. Vance. A proper seal would include a good cap, not a cracked PVC cap, which would suffice only as a temporary cap. A proper cap would be one that is water tight and could not be readily removed. Ms. Vance admits she does not know who cracked the existing cap - only that it is cracked. This well, too, did not produce water fit for its intended purpose because of the existence of the tools which had been dropped into it. A permit was not obtained to abandon it. Under all these circumstances, Ms. Vance did not attempt to determine if it would produce sufficient water. Finally, Ms. Vance concluded that Well No. 3 was not properly seated. According to rule, the casing has to seat to or below the static water level. Based on the debris in the water drawn from this well, she was satisfied this well was not properly cased. Mack Pike, a water resources technician III for the District, does much of the well logging for the District. The equipment he uses goes to the bottom of the well and shows the diameter up to the point where the casing usually starts. Among other items, he uses a camera, which is what he used on the wells in issue here. On July 22, 1999, he went to the Grant property to look at Well Nos. 1 and 2. His first efforts to get into these wells were unsuccessful, so he stopped his effort and returned on May 10, 2000 with the camera. On May 17, 2000, he also ran the camera down all three wells. In Well No. 3 he found the pump at 176 feet. He found Well No. 1 cut off about one and a- half feet below ground level, with a log jammed into the casing top down to the level of the casing. The pipe had been cut with a torch, but the casing had not been properly sealed with bentonite. Use of the log to stuff the pipe was an improper seal. He found the well open below the log down to 128 feet, but obstructed below that. There was no water in the well. Respondent adamantly insists he used bentonite in all three wells, but since no trace of it was found in any of the wells by Mr. Pike or Ms. Vance, it is found that he did not. At Well No. 2, Mr. Pike found a welded slab around the pipe to keep the casing from falling in. The cap was cracked and was no good. The camera showed the well was closed off. He hit sand at 158 feet. The presence of sand indicated to Mr. Pike that the casing was not properly sealed. The well was unusable. Mr. Pike did not examine Well No. 3 until after he opened the sediment tank and found sand which appeared to have come from the surface. If the casing had been properly sealed, there should have been no surface sand. This means that the well was not properly seated. Respondent has been a licensed well contractor since 1989 and has drilled approximately 300 wells since that time. Though he claims he suggested alternate locations for the wells to Ms. Grant, she insisted the well be placed near her irrigation line. Respondent claims he was against this because the site was a transition area which raised the possibility of the pipe bending. Notwithstanding the advice he got from others regarding the siting of the wells, he agreed to place the well where Ms. Grant wanted it. Respondent claims he dug the first well and installed the pump, but the power was insufficient to run it. As a result, he pulled out the pump and told Ms. Grant that when she got the proper power to run it, he'd come back and reinstall the pump. It was when he returned to the site in response to her call that he found that the site of Well No. 1 had been vandalized. Though he recommended the well be abandoned, Ms. Grant did not want to do that, so he moved over 20 feet and started to drill again. He categorically denies having cut off the casing of Well No. 1 below ground level. It has been found that the evidence shows Respondent that cut the pipe on Well No. 1, is insufficient. Mr. Holt admits he did not seek a permit for this second well because his understanding was that one could drill like wells on the same premises without abandoning the pre- existing wells. He drilled the second well which, he claims, produced water for five to six months. However, it was impossible to stop the sand from infiltrating the well, and the well was not producing sufficient water to irrigate the grove. Because the water produced by Well No. 2 was insufficient in quantity to use the 5-horsepower pump called for in the contract, Respondent replaced it with a one and a-half horsepower pump. According to Respondent, he and Ms. Grant discussed where to site Well No. 3. Finally, Ms. Grant agreed to move it up the hill on which Respondent wanted to site it, as this would accommodate her irrigation system. Respondent was not comfortable with this because it was on the slope too close to the others, but he went along with it. As Well No. 3 was being constructed, Respondent discussed with Ms. Grant the need to close Well Nos. 1 and 2. She did not want to pay for the closings, so he decided to cap the existing wells. As a result, Well No. 2 is still a viable well, and though it will not irrigate the grove, it will, Respondent claims, provide sufficient water for the house. He admits placing the PVC cap on Well No. 2, but claims it was not cracked when installed. He also admits to placing the plate around the top of Well No. 2 because the drive shoe was bent. It broke off, and he was afraid if he did not reinforce the area as he had the casing would collapse when he tried to ream out the drive shoe to recover it. At the 126-foot mark of Well No. 3, Respondent hit a boulder through which the drill would not go. At that time, the hole below the casing was still good with no infusion. Respondent installed a pump and drew water, but, the pump soon began to pull sand. Respondent installed a filter, but it was insufficient. He ultimately drilled through the rock and placed the pump at 178 feet. That well is currently being used. Respondent claims that all wells in that area pull sand to some degree. He insists that Ms. Grant's wells just pull too much. He claims he could have quit, but because of his relationship with the builder, he felt obligated to drill a working well for Ms. Grant. Anthony Gilboy, who has been with the District for 20 years, is currently the District's manager of well construction. He is familiar with the statutes and the rules of the District relating to water well construction and abandonment. According to Mr. Gilboy, they are loose enough to permit some latitude in their application. There is a freedom to amend methodology where circumstances so dictate. A licensed water well contractor is required to obtain a permit to construct a water well. Once a permit is drawn, if the well needs to be changed, the permittee must apply for an amendment and then plug the old well consistent with District guidelines. Plugging is critical to prevent potential contamination of water and to preserve it. Rule 40D-3.042, Florida Administrative Code, permits multiple (up to 8) wells under a single permit for similar types of wells that have diameters of 4 inches or less, but not domestic water wells. There are different ways to drill a water well. One is by cable-tool drill in which a bit is hammered into the rock. As the casing is being driven down into the ground, it holds back the sediment. Another method involves the use of a rotary drill which employs water and bentonite to hold back sediment. It is possible to tell whether bentonite was used in the drilling process just by looking at the well. The bentonite adheres to the well casing and looks different from the surrounding soil. In fact, there is no soil appearing naturally in Florida that looks like bentonite. In the instant case, Respondent applied to use the cable-tool method. Bentonite traces were not found at the sites. When a well is drilled, the casing is to be poured in segments as drilling progresses. When a well is to be abandoned, one approved method of doing so involves the use of bentonite, a type of clay which swells to about 10 to 15 times its volume in dry form. Studies done by the District in conjunction with the University of Florida show that over all, bentonite is a better seal than natural soil, and it prevents surface water from settling down the side of the casing. Rule 40D-3.517(3), Florida Administrative Code, requires bentonite's use for this purpose, and a rule of the Department of Environmental Protection, though not specifically mentioning bentonite, requires that casings be sealed. The casing of a water well is used to seal off any unconsolidated materials. Rule 62-532, Florida Administrative Code, requires the casing be extended into the static water level at the time the well is drawn. If a well is not sealed, debris and sand can slide into the well and damage the pump and other equipment. If debris is seen, it usually means the casing was not sealed properly. After a well is completed, the rules of the District and the Department, Rules 40D-3.521(2) and 62-532.500(3)(a)4, Florida Administrative Code, respectively, require the upper part of the well to be sealed off to prevent infusion of contaminants. The seal must be tamper-proof and permanent. A fence post is not acceptable, nor is a cracked PVC cap. In addition, the upper terminus of a private well must extend at least 1 foot above the land surface. The purpose of this requirement is to allow the well to be found, and to prevent infusion of contaminant. (Rule 40D-3.53(2), Florida Administrative Code) According to Rule 62-532-500(4), Florida Administrative Code, all abandoned or incomplete wells must be plugged from top to bottom with grout (neat cement). The Rule and Stipulation 39 of the permit provide that the well drilling contractor is responsible for proper abandonment of a well. This is not conditioned on the willingness of the owner to pay. The contractor has the responsibility to do it. An abandoned well is one which the use of which has been permanently discontinued or which is so in need of repair as to be useless. These determinations must be made by the District, hence the need for the permit. In the instant case it was determined that Well Nos. 1 and 2 were not suited for their intended purpose, and they should have been properly abandoned. The process for well abandonment is not complex, but it does require the obtaining of a permit. At least 24 hours in advance of initiation of the plugging process, the contractor must advise the District that the process will be implemented. Thereafter, the well hole is filled with neat cement or bentonite grout. To abandon a well by any other method would require a variance from the District. Neither permit nor variance was sought as to Well Nos. 1 and 2. The standards adopted by the Department and the Water Management Districts are statewide in application. Construction of a water well without first obtaining a permit is classified as a major violation. The failure to properly abandon a well or the failure to use bentonite or neat cement in well closure are also major violations. Failure to construct a well so that the casing extends below the static water level is a major violation. Failure to seat or seal a casing into rock formation is a major violation. Failure to place a water-tight seal and failure to extend well casing at least one foot above the ground level are both major violations. Penalties may be assessed for these violations according to a schedule set out in the Department rules. However, these penalties may be adjusted based on such factors as the economic benefit to the contractor of his non-compliance; his history of non-compliance; the negligence or willfulness of his actions; and whether he acted in good faith. Under the circumstances of this case, Mr. Gilboy is of the opinion that the actions proposed by the District are appropriate.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is recommended that Respondent, Fletcher Holt be ordered to pay an administrative fine of $4,600; that 46 points be assessed against his water well contractor's license; and that he be required to properly abandon Well Nos. 1, 2, and 3, which he drilled on the Grant property. DONE AND ENTERED this 18th day of July, 2000, in Tallahassee, Leon County, Florida. ARNOLD H. POLLOCK 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 18th day of July, 2000. COPIES FURNISHED: Onofre Cintron, Esquire 305 North Parson Avenue Brandon, Florida 33510 Margaret M. Lytle, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 E. D. "Sonny" Vergara, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Kathy C. Carter, Agency Clerk Office of General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Station 35 Tallahassee, Florida 32399-3000
The Issue The issue is whether Respondent should correct a health violation and have a $500.00 fine imposed for violating an agency rule and statute, as alleged in the Citation for Violation issued by Petitioner on December 22, 1999.
Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: This case involves an allegation that Respondent, Steve DeLuca, violated an agency regulation and statute by making repairs to a drainfield on property located at 1444 East New York Avenue, Deland, Florida, without obtaining the necessary permits from the Volusia County Department of Health (Health Department). That department is under the direction and control of Petitioner, Department of Health (Department). Respondent denies the charge and, as clarified for the first time at hearing, contends that the repairs were minor in nature and thus did not require a permit, no authorization was given to the excavation firm which performed the repairs, and the Citation was not issued to the actual owner of the property. On October 29, 1999, William N. VanderLugt (Vanderlugt), a Health Department environmental specialist, received a complaint regarding a septic tank repair being undertaken at 1430 East New York Avenue, Deland, Florida. During the course of inspecting that property, Vanderlugt observed excavation activities on the drainfield located next door at 1444 East New York Avenue. More specifically, Vanderlugt observed an area in the back yard approximately 6 feet by 20 feet in size which had been recently excavated and a large pile of sand nearby. In the excavated site, he saw a rock bed of the size commonly used in drainfields, "clean" and "newly installed" rocks, and a "black paper" covering a part of the rocks. Therefore, he concluded that the excavating firm had just installed a new rock drainfield. This type of activity constitutes a repair to an existing drainfield and requires that such work be performed by a licensed septic tank contractor. It also requires that appropriate permits be obtained from the Health Department. Although Respondent contended that the work was merely to correct a "minor structural flaw" which would not require a permit, Vanderlugt's testimony is more persuasive on this issue, and it is found that a more substantial repair to the drainfield was made. Further inquiry by Vanderlugt revealed that no permits had been obtained for the repair of a drainfield from the Health Department by the excavating company, Collier Enterprises. After a brief conversation with a Collier Enterprises employee, the substance of which is hearsay in nature and cannot be used, Vanderlugt visited the offices of Delco Oil Company and spoke with Respondent, who is employed by that firm. In doing so, Vanderlugt was under the impression that Respondent owned the property in question. During his brief conversation with Repondent, Vanderlugt pointed out that he had to issue a citation because no permit had been obtained for the work at the property in question. DeLuca responded with words to the effect that "they [Collier Enterprises] broke a pipe and they fixed what they broke." Apparently, there was no discussion as to whether Respondent or someone else actually owned the property. Vanderlugt returned to the property in question and performed a second inspection on November 3, 1999. Because no permits had been obtained by that date, and the drainfield site had been covered, a recommendation for a citation was prepared by Vanderlugt. A Citation for Violation was later issued by the Department on December 22, 1999, alleging that Respondent had failed to obtain permits before making a drainfield repair. The Citation was delivered to Respondent at Delco Oil Company. Because Collier Enterprises was not licensed to perform the work, it was given a first violation "warning" letter by the Health Department, as required by a Department rule. During later meetings with Respondent and others, Vanderlugt learned that the actual owner of the property in question was Deluca Properties, Inc., and not Steve DeLuca. For some reason, however, the Department declined to amend its citation and charge the actual owner with the alleged violation. Although Petitioner asserted at hearing and in its Proposed Recommended Order that Respondent is the owner's registered agent, there is no competent evidence of record to support this assertion. According to the general manager of Delco Oil Company, which is apparently owned by Steve Deluca and others, no permission was given to the excavating company to make any repairs. Indeed, Deluca Properties, Inc. has a licensed septic tank contractor who makes all septic tank repairs, when needed.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Health enter a final order dismissing the Administrative Complaint for lack of jurisdiction. DONE AND ENTERED this 14th day of June, 2000, in Tallahassee, Leon County, Florida. DONALD R. ALEXANDER 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 14th day of June, 2000. COPIES FURNISHED: Angela T. Hall, Agency Clerk Department of Health Bin A02 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1703 Charlene J. Petersen, Esquire Department of Health 420 Fentress Boulevard Daytona Beach, Florida 32114 Christopher R. Ditslear, Esquire Post Office Box 41 Deland, Florida 32721-0041 William W. Large, General Counsel Department of Health Bin A02 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1701
Findings Of Fact At all times pertinent to the issues herein, the Southwest Florida Water Management District had permitting authority for the issuance of consumptive use permits in the area in which Respondent, El Jobean, proposes to sink its irrigation well. On December 12, 1988, El Jobean submitted a consumptive use permit application to sink a new well for the purpose of irrigation of a golf course to be developed on the property it owns in Sarasota County. The well is to be located in the NE 1/4 of the NE 1/4 of Section 32, Township 365, Range 20R, in Sarasota County, Florida near the southern boundary of an irregularly shaped piece of property consisting of approximately 855 acres, owned by the applicant, which extends over Sections 28, 29, 32 and 33, Township 365, Range 20E. Respondent proposed to sink a 10 inch diameter well to a total depth of approximately 900 feet with casing in the well now to extend down to 300 feet, with a pump capacity of 1,000 GPM. The golf course to be irrigated is to encompass approximately 190 acres. The applicant requested authority to withdraw an average of 600,000 GPD with a limitation of a maximum of 1,440,000 GPD. The application was properly staffed by the District. In the staff report on the application, the average daily use limitation was expanded to 707,000 GPD; consumptive use was raised from 0 to 139,000 GPD; and maximum daily consumption was reduced from 1,440,000 GPD to 1,240,000 GPD. These changes were due to correction of arithmetic errors in the application and were accepted by the applicant. The ultimate recommendation of the staff was for approval of a 6 year permit, subject to certain conditions outlined in subparagraph I of the staff report. These special conditions require the provision and use of flow measuring devices to maintain an accurate record of the water withdrawn; the maintenance of flow records and the providing of periodic reports to the District; the collection and analyzing of water quality of samples taken from the well to measure the appropriate parameters for chlorides, sulfates, and total dissolved solids; the reporting of the results of these samplings and a description of the sampling and analytical methodologies employed; and a requirement that the permittee investigate the feasibility of supplementing and/or substituting drawn water with treated sewage affluent. After the staff report was submitted, proper notice of the District's intent to issue the permit was published. Based on that notice, protests were filed both by Miakka and Mr. Bishop. The area in question is located within the Manasota Basin which, itself, is located within the Southern West-Central Florida Ground Water Basin, (SWCFGWB), which encompasses all of Pasco, Hillsborough, Manatee, Sarasota, Polk, Hardee, and DeSoto Counties, and parts of Lee, Glades, Charlotte and Highlands Counties. The SWCFGWB sits atop several aquifers which include the Floridian Aquifer, two Intermediate aquifers, and the Surficial Aquifer. The Floridian Aquifer is the deepest and the Surficial Aquifer is on the top. The Miakka Community Club is a Florida corporation made up of residents of the pertinent area whose primary function is to preserve and conserve the rural nature and spirit of the Northeast section of Sarasota County. The club performs this function through educational programs, community activities, and participation in the legislative process. Miakka urges denial of the permit sought by El Jobean based on its membership's belief that the property owners whose property is in the immediate vicinity of the proposed well will be adversely affected if El Jobean is permitted to sink its well and withdraw water from it. The club membership believes that approval of El Jobean's well will result in contamination of existing personal water wells due to excessive use by El Jobean; potential contamination of Sarasota County's future drinking water sources which include the capital Ringling,/MacArthur tract and the Myakka River; reduction of property values; and destruction of personal resources. Petitioner also urges that since the proposed golf course will be a part of a private club for the use of members only, in which membership will be limited, there is no public benefit derived from the approval of and sinking of the well in question. Petitioner also contends that during the periods of severe water shortage as are being currently experienced, permission to sink a well of this size to draw water in of the magnitude expressed in the application, would be counterproductive and detrimental to the interests of the other property owners in the area. In support of its claim, Petitioner presented the testimony of two homeowners from the area, Mr. Richardson and Ms. Mustico. Mr. Richardson, whose well is 183 feet deep, has had several problems with his well even without the instant drilling. In 1974, and subsequent thereto, he has had to go deeper with a suction pipe because the water has dropped below the level of the tail pipe. Ms. Mustico's 160 foot deep well, with 80 feet of casing, is used to supply water for the home. She also has other wells for watering her lawn and for livestock, one of which goes down 500 feet. She is concerned that the well proposed by El Jobean will adversely impact her ability to draw water from her wells because, she believes, the water level from which her water is drawn will drop. In the past, her primary well has gone dry and the wells of several neighbors have gone dry as well. Through maps and other documentation taken from the Ground Water Resource Availability Inventory for Sarasota County, Florida, prepared by the District in March 1988, Petitioner has established that areas of significant groundwater withdrawal within the SWCFGWB occur in Hillsborough, Manatee, Polk, Hardee, DeSoto and Highlands Counties. With the exception of an extremely small portion of Sarasota County located contiguous to Manatee County, there appear to be no areas of major ground water withdrawal currently existing in Sarasota County. The majority of the major municipal well fields within the pertinent basin that are located within Sarasota County, extend down to the Intermediate and Surficial Aquifers with only 3 extending through the lower Intermediate into the Floridan Aquifer. These include the Verna well field located in the northeast corner of Sarasota County where it abuts Manatee County; the Sarasota County well field located in northwest Sarasota County near the Manatee County line; and the Sorrento Utility, Inc., well field which is located near the Gulf Coast, approximately two-fifths of the way down between the Manatee and Charlotte County lines. With the exception of the Verna well field, all the municipal well fields in Sarasota County appear to be reverse osmosis systems and as of 1987, there were 28 reverse osmosis systems located within Sarasota County. Most are relatively small in their output measured in millions of gallons per day. With the exception of 3 public supply wells, 2 of which are permitted an average annual pumpage greater than 100,000 GPD and 1 of which is permitted less, all of the permitted public supply well fields in Sarasota County are located west and south of 1-75 as it extends from the Manatee County line in the north to the Charlotte County line in the south. The El Jobean well would be located east of the line, in that area occupied by the 3 public supply wells. Generalized recharge areas for the upper Floridan Aquifer in the groundwater basin in issue here have been categorized from "high", with a rate of more than 10 inches per year, to "Generally none", with a recharge rate at 0. In 1980, the high recharge rates existed in the north-central part of Pasco, the eastern part of Polk County, and the northeastern part of Highlands County. Sarasota County is in an area wherein the recharge rate was either very low or generally none. In September 1986, the high recharge rate was found in a very small area of northeastern Pasco County, and small areas in both Polk and Highlands Counties. Sarasota County, for the most part, was classified as having no recharge. In May 1987, the high recharge rates were, again, a small area in eastern Pasco County, a small area in northeastern Hillsborough County, a small area in southeastern Polk and northwestern Highlands Counties, and a minuscule area in central Pinellas County. Again, Sarasota County had a recharge rate of 0. Generalized estimated, calibrated, model-derived recharge and discharge values for the upper Floridan Aquifer in the ground water basin in issue here, as they pertain to Sarasota County, reflect positive 2 recharge to negative 1 discharge inches per year. Historically, however, the northeast portion of Sarasota County, where the El Jobean well in question would be located, evaluated by various individuals or agencies periodically from 1980 through 1988, reflects a recharge of anywhere from 0 to 2 inches per year. None of this documentation was supplemented, however, by direct testimony by an individual knowledgeable in this area, and Petitioner's main thrust appears to be an unsubstantiated fear that the sinking of El Jobean's well will have a negative impact on its membership's wells. Admittedly, the residents in the area in question all rely on private wells for the majority of their water supply, other than through the catchment of rainwater, which is insignificant. It was also established that the area has been undergoing a severe water shortage and that conservation measures have been mandated. On the other hand, El Jobean presented the testimony of a hydrogeologist, Mr. Moresi, who has extensive experience with the modeling process used to determine water consumption and recharge in southwest Florida and Sarasota County. The aquifer system in Florida is made up of water bearing limestone layers below the surficial sand base. This aquifer system underlays the various zones throughout the state and reflects a surficial aquifer extending from ground level down approximately 70 feet to a confining bed which separates it from the lower strata. This top confining bed is approximately 20 feet thick, and below it is the Tamiami-Upper Hawthorn Aquifer, which is between 100 and 200 feet deep and which rests on another confining bed somewhat thicker than the upper one. Below the second confining bed is the Lower Hawthorn-Upper Tampa Aquifer which extends approximately from the 250 foot to the 450 foot level at the Manatee County line, and between the 320 foot and the 710 foot level at the Charlotte County line. Another confining bed lays between this aquifer and the Floridan Aquifer which starts at the 500 foot level and goes down well below the 900 foot level in the north and extends from the 730 foot level down in the south. The confining bed below the surficial aquifer is made up of a clay material which retards the movement of water from one aquifer to another. The surficial aquifer is porous and saturated with water from the water table down. Since the confining beds are far less porous than the aquifers they separate, water moves much more slowly through them. The lower aquifers are made up of limestone and are also porous and contain water. The Tamiami-Upper Hawthorn formation consists of limestone and clay, but is water bearing. The Lower Hawthorn-Upper Tampa formation is similar and both make up the intermediate aquifer below which is the lower confining bed followed by the Floridan aquifer. Respondent's well would be cased in steel down to an area approximately 100 feet into the Floridan Aquifer, through the Lower Hawthorn- Upper Tampa Aquifer and through the lower confining bed. Since the well would be cased to well below the lower confining bed, water existing in the upper aquifers, would be prevented from being drawn down by operation, of the Respondent's well either directly or by settling down to replace the water drawn out. Generally, the deeper a well is drilled, the worse the quality of the water, and it becomes less potable. The Floridan Aquifer produces far more copious quantities of water than do the intermediate aquifers. However, since it is cheaper to drill to the intermediate zones as the wells need not be so deep, and since the water there is better, most domestic wells go no deeper than these aquifers. They go down approximately 150 to 180 feet. The pressure in each level is separate from and different from that in the other aquifers. The upper intermediate system generally has a lower pressure than the lower intermediate system. As a result, water from the lower intermediate system tends to leak upward toward the upper intermediate aquifer, rather than the reverse. In addition, a recent survey tends to show that the Floridan aquifer also tends to leak upward into the lower intermediate level. It also shows that leakage through the confining beds amounts to .002 GPD per cubic foot of aquifer. Petitioner claims that since the lower water is of lesser quality, and since withdrawal of water from the upper layers would promote leakage upward, thereby adding lower grade water to the better grade upper water, there could be a diminishment in upper level water quality as a result of water being drawn from the upper levels. However, according to Mr. Moresi, the .002 figure is so small it would result in an infinitesimally small drawdown of water level from the upper intermediate level aquifer and the potential for compromise of the water quality therein is remote. Clearly, this is not the result of drawing water from the Floridan Aquifer as the well in question would do but more the result of the residential wells extending into the upper levels. The District ran a model for the proposed El Jobean well (a Jacob- Hantush model) which showed that drawdown at the wellhead would be just over 2 feet. This means that use of the Respondent's well would reduce the water level in the Floridan Aquifer at the well head by 2 feet. However, this drawdown is shown to decrease rapidly out to where, at distance, it is almost immeasurable. In fact, drawdown of the Floridan Aquifer at 24,000 feet from the well head (approximately 4.5 miles) would be .1 feet, slightly or 1 inch. The .1 foot drawdown relates to the lowest (Floridan) aquifer and the resultant drawdown in the upper intermediate aquifer, into which the majority of residential wells are sunk, would be relatively undetectable. Since the Petitioner's wells, at their deepest, go only into the upper intermediate level, and would be separated by 2 confining beds from the Floridan Aquifer, the impact on the domestic wells at 2 miles from the El Jobean wellhead would be immeasurable. Even at 1 mile, there would be minimal drawdown in the Floridan Aquifer and almost none in the upper intermediate aquifer. The potentiometric surface of the intermediate layer would not be adversely affected, nor would that of the surface water. Recognizing the potential for saltwater intrusion which occurs all along the coast, based on his studies, Mr. Moresi concluded that the well in question here would not induce significant saltwater intrusion. He concluded as well that the permit is consistent with the requirements of the District rule; that the amount permitted for the use of irrigation of the golf course is reasonable, assuming a golf course is a reasonable and appropriate use of water; that the withdrawal by the well in issue would not have an adverse impact on users outside the property on which the well was located; that it would not impact existing users; that there is no other water available for the purpose intended; that the water taken from the Floridan Aquifer under this permit may be potable but is of poor quality; and that the applicant met rule standards. Mr. Moresi also discussed the possible cumulative impact of the proposed well when operated along with the currently existing wells. If there are other drawdowns from the same cone into which El Jobean's well would be sunk, the withdrawals would be cumulative. However, as best he can determine, the only other significant drawdown from the cone pertinent here is that of the Verna well field. In his opinion, that well field's drawdown, which is from the northeast, would not be significant even when considered with the El Jobean well. Mr. Moresi was also satisfied that while the confining bed separating the surficial aquifer from the next lower level might be disturbed, the deeper one goes, the less likely there is to be mixing of aquifers. The only instance where water could move from one level to another as a result of the well is where there is no casing on the bore hole. In the instant case, plans call for, and permit conditions require, the well to be cased to below the lowest confining bed. Consequently, there should be no upward or downward flow of water as a result of the bore. Mr. Tyson, who worked on the evaluation of El Jobean's application for permit, was of the opinion that the amount of water requested by El Jobean in its application was appropriate for a golf course. This does not mean that a golf course is an appropriate use of the property. The special conditions imposed on the granting of the permit by the District are designed to reduce any impact possibly caused by the permitted activity. The Jacob-Hantush model used in analysis of the instant application is considered to be a conservative tool and showed minimal drawdown at all property boundaries. The use of other models in this case was considered neither necessary nor appropriate. Mr. Tyson considers the proposed permit a reasonable beneficial use as defined in the Florida Administrative Code and statutes because it proposes use of reasonable amounts of water and the models indicate no unfavorable impact. Based on the past practice of permitting golf courses with subdivisions, he feels the proposed use is reasonable. He concludes, therefore, that it is in the public interest to grant this permit. In his opinion, the permit will not interfere with legal existing uses and meets all statute and rule requirements. Considering the evidence as a whole, it is found that petitioner has presented insufficient evidence to support its claim that approval and operation of El Jobean's well as proposed would have an adverse impact on the property owners. It's concerns are no doubt sincere, but these concerns are not sufficiently confirmed by evidence of record. At the hearing, the parties stipulated that if the permit were granted, it would be modified by the addition of two conditions: The proposed well shall be constructed with a minimum of 600 feet of casing so as to prevent the unauthorized interchange of water between water bearing zones in order to prevent the deterioration of water quality in the shallower zones. If the well cannot be properly completed to prevent such an unauthorized interchange of water, the well shall be abandoned and plugged in accordance with Rule 17-21.10(2)(c), F.A.C.. Upon completion of the well, a copy of the well construction completion report shall be sent to the District. The permittee shall line the bottom of the pond that will be used as the irrigation source, with clay to a thickness equal to 1.5 feet.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that the Southwest Florida Water Management District enter a Final Order issuing Consumptive Use Permit Number 209458, as modified by the conditions stipulated to at the hearing held herein on June 7, 1989, and outlined in Finding of Fact Number 27 herein, to El Jobean Philharmonic Group, Inc. RECOMMENDED this 9th day of August, 1989 at Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of Division of Administrative Hearings this 9th day of August, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 88-1176 The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. For the Petitioner: Not a Finding of Fact but a statement of the ultimate issue of fact. Accepted and incorporated herein. 3-6. Accepted and incorporated herein. 7-12. Accepted and incorporated herein. Accepted as indicating original conditions. The parties stipulated to additional conditions at the hearing. Accepted. 15 & 16. Accepted and incorporated herein. 17-33. Accepted and incorporated herein as pertinent. 34 & 35. Accepted. 36 & 37. Accepted. 38 & 39. Redundant. 40-43. Accepted. 44. Accepted. 45-51. Accepted. 52 & 53. Accepted. 54-56. Accepted. 57 & 58. Accepted and incorporated herein. 59-66. Accepted. 67-75. Accepted and incorporated herein. 76 & 77. Accepted and incorporated herein. 78. Accepted. 79-84. Accepted. Accepted and incorporated herein. Rejected. 87 & 88. Accepted. 89-93. Accepted and incorporated herein. Accepted. Accepted in the natural source sense suggested by Petitioner. 96-99. Accepted and incorporated herein. 100 & 101. Accepted and incorporated herein. 102-105. Accepted and incorporated herein. 106. Accepted. 107 & 108. Accepted. 109 & 110. Accepted. For the Respondents: 1 & 2. Stipulation between the parties accepted and incorporated herein. 3-6. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence except for the second sentence which is incorporated herein as a Finding of Fact. Not a Finding of Fact but a comment on the evidence. 9-11. Accepted and incorporated herein. 12. Accepted. 13-16. Accepted and incorporated herein. 17. Accepted and incorporated herein. 18 & 19. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. 22-26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29. Accepted. 30-32. Accepted and incorporated herein. 33-40. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Not a Finding of Fact but a Conclusion of Law. COPIES FURNISHED: Becky Ayech Personal Representative Miakka Community Club 421 Verna Rd. Sarasota, Florida 34240 Douglas Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Edward B. Helvenston, Esquire Assistant General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609 6899
The Issue The issue to be determined in this case is whether Respondents, United States Sugar Corporation (“USSC”), Sugar Farms Co-op (“SFC”), and Sugar Cane Growers Cooperative of Florida (“SCGC”) (collectively “the Applicants”) are entitled to the Everglades Works of the District permits (“WOD Permits”), issued to them by the South Florida Water Management District (“District”).
Findings Of Fact The Parties Audubon is a not-for-profit organization dedicated to restoring and conserving natural ecosystems, focusing on birds and their habitats. Audubon has a substantial interest in the protection of the Everglades and other ecosystems in the area. Audubon’s interest is affected by the proposed agency action because the WOD Permits authorize agricultural discharges that affect these ecosystems. The District is a Florida public corporation with the authority and duty to administer regulatory programs in chapter 373, and Florida Administrative Code Title 40E, including a program for regulating discharges from the Everglades Agricultural Area (“EAA”) into works of the District. The EAA is located south of Lake Okeechobee and comprises about 570,000 acres. The majority of EAA agriculture is sugarcane, with some row crops, such as radishes, leafy vegetables, and corn, and turf sod. During fallow periods, rice is also grown. The Applicants are owners and lessees of agricultural lands in the EAA. Background Some essential background for this case is set forth in rule 40E-63.011: The Everglades is a unique national resource. It has a high diversity of species, and provides habitat for large populations of wading birds and several threatened and endangered species, including wood storks, snail kites, bald eagles, Florida panthers, and American crocodiles. Large portions of the northern and eastern Everglades have been drained and converted to agricultural or urban land uses. Only 50% of the original Everglades ecosystem remains today. The remainder is the largest and most important freshwater sub-tropical peatland in North America. The remaining components of the historic Everglades are located in the Water Conservation Areas (WCAs) and Everglades National Park (ENP). ENP and Loxahatchee National Wildlife Refuge (WCA 1) are Outstanding Florida Waters, a designation which requires special protection for the resource. Large portions of the Everglades ecosystem have evolved in response to low ambient concentrations of nutrients and seasonal fluctuations of water levels. Prior to creation of the Everglades Agricultural Area (EAA), nitrogen and phosphorus were mainly supplied to large areas only in rainfall. Phosphorus is the primary limiting nutrient throughout the remaining Everglades. Sawgrass has lower phosphorus requirements than other species of Everglades vegetation. A substantial portion of EAA nutrients is transported to the remaining Everglades either in dissolved or in particulate form in surface waters. The introduction of phosphorus from EAA drainage water has resulted in ecological changes in substantial areas of Everglades marsh. These changes are cultural eutrophication, which is an increase in the supply of nutrients available in the marsh. The increased supply of phosphorus in Everglades marshes has resulted in documented impacts in several trophic levels, including microbial, periphyton, and macrophyte. The areal extent of these impacts is increasing. In 1988, the United States sued the District and the Florida Department of Environmental Regulation, now the Department of Environmental Protection (“DEP”), in federal court, alleging that the agencies failed to enforce Florida’s water quality standard for nutrients in waters of Loxahatchee Wildlife Refuge and Everglades National Park. The principal pollutant of concern was phosphorus. Audubon, USSC, and certain members of SCGC and SFC intervened in the federal case. In February 1992, the parties resolved their dispute through a settlement agreement approved by the federal court (“the Consent Decree”). The Consent Decree required the District and DEP to take action to meet water quality standards by December 31, 2002. At that time, the nutrient water quality standard was a narrative standard, prohibiting the discharge of nutrients so as to cause “an imbalance in natural populations of aquatic flora and fauna.” The Consent Decree directed the District to construct 34,700 acres of stormwater treatment areas (“STAs”) so that nutrient-laden surface water discharged from the EAA could be treated before discharge to the Everglades Protection Area (“EvPA”), which includes Loxahatchee Wildlife Refuge, Everglades National Park, and the Water Conservation Areas. STAs are large freshwater wetlands which remove phosphorus from the water column through physical, chemical, and biological processes such as sedimentation, precipitation, plant growth, and microbial activity. The first STAs were constructed and in operation in 1993. The Applicants operate in the S-5A Basin within the EAA. Their surface water is conveyed to STA-1W for treatment before being discharged to the EvPA. The Consent Decree required the District to initiate a regulatory program by 1992 to require permits for discharges from internal drainage systems (farms) in the EAA. The regulatory program was to be based on agricultural best management practices (“BMPs”). The goal of the program, as stated in the Consent Decree, was to reduce phosphorus loads from the EAA by 25 percent over the base period (1979-1988). In 1992, the District promulgated rule chapter 40E-63, which required EAA farmers to obtain WOD permits and to implement agricultural BMP plans. The BMP plans address fertilizer use and water management. Permittees must also implement a water quality monitoring plan. The rules require reduction of the total phosphorus loads discharged from the EAA Basin, as a whole, by 25 percent from historic levels. See Fla. Admin. Code R. 40E-63.101. If the EAA, as a whole, is in compliance, individual permittees are not required to make changes to their operations. See Fla. Admin. Code R. 40E-63.145(3)(d). If the 25 percent reduction requirement is not met, the rule contemplates that individual permittees in the EAA would have to reduce nutrient loads in their discharges. See Fla. Admin. Code R. 40E-63.145(3)(e).1/ The Consent Decree also required the District to obtain permits from the Department for discharges from the STAs to the EvPA and to conduct research and adopt rules to “numerically interpret” the narrative standard. In 1994, the Florida Legislature enacted the Everglades Forever Act (“the Act”), chapter 94-115, Laws of Florida, which is codified in section 373.4592. The Legislature authorized the district to proceed expeditiously with implementation of the Everglades Program. See § 373.4592(1)(b), Fla. Stat. The “Everglades Program” means the program of projects, regulations, and research described in the Act, including the Everglades Construction Project. The Everglades Construction Project involved the construction of 40,452 acres of STAs, which is 5,350 acres more than was required by the federal Consent Decree. The Act acknowledged the BMP regulatory program for the EAA that the District had established in rule chapter 40E-63, and stated: Prior to the expiration of existing permits, and during each 5-year term of subsequent permits as provided for in this section, those rules shall be amended to implement a comprehensive program of research, testing, and implementation of BMPs that will address all water quality standards within the EAA and Everglades protection Area. See § 373.4592(4)(f)2., Fla. Stat. The Act required DEP to issue permits to the District to construct, operate, and maintain the STAs. See § 373.4592(9)(e), Fla. Stat. The Act required development of a numeric water quality phosphorus standard for the EvPA by 2003. See § 373.4592(4)(e), Fla. Stat. The Act set the goal of achieving the phosphorus standard in all parts of the EvPA by December 31, 2006. In June 1995, modifications were made to the Consent Decree. The deadline for achieving water quality standards in the EvPA was changed from December 31, 2002, to December 31, 2006. The STAs were increased from 34,700 acres to 40,452 acres. The chronological developments outlined above indicate the intent of the Legislature and the parties to the Consent Decree to conform state law and the Consent Decree to each other. In 2001, DEP initiated rulemaking that lead to its adoption of the Phosphorus Rule, rule 62-302.540, in 2003. The rule set a numeric phosphorus criterion for the EvPA of 10 parts per billion (“ppb”), applied through a four-part test in which attainment is determined separately for “unimpacted” and “impacted areas” of the EvPA. See Fla. Admin Code R. 62- 302.540(4). In conjunction with this rulemaking, the DEP and District developed the Everglades Protection Area Tributary Basins Long Term Plan for Achieving Water Quality Goals (“Long- Term Plan”) in March 2003. The Long-Term Plan provided remedial measures and strategies divided into pre-2006 projects and post- 2006 projects. The pre-2006 projects included structural and operational modifications to the existing STAs, implementation of agricultural and urban BMPs in areas outside the EAA or C-139 basins, and construction of several restoration projects congressionally mandated by the Comprehensive Everglades Restoration Plan. Modeling of treatment capabilities of the STAs after implementation of the pre-2006 projects predicted that the 10 ppb standard for phosphorus could be achieved, but not consistently. Therefore, the Long-Term Plan required the District to identify and evaluate methods to improve phosphorus reductions, and if the phosphorus criterion was not achieved by December 31, 2006, to implement post-2006 modifications and improvements. The post- 2006 strategies include projects to expand and improve the STAs. They do not include changes to the BMP program. In 2003, the Legislature substantially amended the Act. It incorporated the Long-Term Plan into the Act, finding that it “provides the best available phosphorus reduction technology based on a combination of the BMPs and STAs.” § 373.4592(3)(b), Fla. Stat. The Long-Term Plan contemplates maintenance of the BMP program in the EAA, with refinements derived from BMP research. Recent Conditions and Events As previously stated, chapter 40E-63 requires the total phosphorus load from the EAA to be reduced by not less than 25 percent from historic levels. Since full implementation of the BMP regulatory program, annual phosphorus loads have been reduced by approximately 50 percent. Despite the efforts and projects undertaken, the phosphorus standard was not being achieved as of December 31, 2006, in all parts of the EvPA. In 2007, the DEP issued a permit to the District for discharges from the STAs to the EvPA (referred to as the “Everglades Forever Act” or “EFA permit”). The permit required the District to design and construct several regional water management projects, including structural enhancements to STA-1W, and the construction of 6,800 acres of additional STAs. The permit and its compliance schedules provided interim relief through 2016 from the water quality based effluent limitation (WQBEL) necessary to achieve the 10 ppb phosphorus standard. The 2007 EFA permit was not challenged by Audubon or any other entity. The District, DEP, and the United States Environmental Protection Agency began working together in 2010 to develop new strategies for achieving compliance with the phosphorus standard in the EvPA. The agencies determined that compliance could be achieved by expanding the STAs by 7,300 acres (6,500 acres would be added to STA-1W) and constructing flow equalization basins to store up to 110,000 acre feet of stormwater runoff. These basins are designed to attenuate peak flows into the STAs in order to improve the processes that remove phosphorus. In September 2012, DEP issued the District a new EFA permit, which authorized continued operation of the District’s S-5A pump station, STA-1W, and the related conveyance systems by which stormwater runoff from the S-5A Basin is ultimately discharged to the EvPA. The permit was issued with a Consent Order, requiring the District to expand STA-1W by 6,500 acres of effective treatment area in accordance with a timeline and the District’s Restoration Strategies. The 2012 EFA Permit and Consent Order were not challenged by Audubon or any other entity. In 2013, the Legislature amended the Act again. The Act’s reference to the Long-Term Plan was revised to include the District’s Restoration Strategies Regional Water Quality Plan, which called for expanding the STAs and constructing flow equalization basins. See § 373.4592(2)(j), Fla. Stat. The Legislature added a finding that “implementation of BMPs, funded by the owners and users of land in the EAA, effectively reduces nutrients in waters flowing into the Everglades Protection Area.” See § 373.4592(1)(g), Fla. Stat. The 2013 amendments indicated the Legislature’s intent to codify into law the strategies developed by the District and other regulatory agencies to achieve water quality standards in the EvPA. Those strategies do not materially change the BMP program in the EAA. The Act and the rules of the District create programs for achieving restoration of the EvPA that rely heavily on the STAs. Over the years, the STAs have repeatedly been enlarged and enhanced. In contrast, the requirement for farmers in the EAA to reduce their phosphorus loading by 25 percent has not changed in 21 years. It is beyond the scope of this proceeding to question the wisdom of the programs that have been established by statute and rule. Whether Additional Water Quality Measures Are Required A principal dispute in this case is whether the WOD Permits must include additional water quality measures to be implemented by the Applicants. Section 373.4592(4)(f)4. provides that, as of December 31, 2006, all EAA permits shall include “additional water quality measures, taking into account the water quality treatment actually provided by the STAs and the effectiveness of the BMPs.” Audubon asserts that the requirement for additional water quality measures has been triggered. The District does not interpret the statute as requiring additional water quality measures under current circumstances. The interpretation of the statute is primarily a disputed issue of law and is addressed in the Conclusions of Law. There, it is concluded that additional water quality measures are not required. Whether the BMP Plans are Adequate Audubon contends that the WOD Permits should be denied because the Applicant’s existing BMP plans are not “tailored” to particular soils, crops, and other conditions. This contention is based on section 373.4592(4)(f)2.c., which states in relevant part: BMPs as required for varying crops and soil types shall be included in permit conditions in the 5-year permits issued pursuant to this section. Audubon showed that the Applicants have similar BMP plans for the thousands of acres covered in the three WOD Permits, and contends that this similarity proves that BMPs are not being tailored to specific farm conditions. However, soils and crops are similar throughout the EAA. The soils of the EAA are almost entirely muck soils and the primary crop is sugarcane with some corn or other vegetable rotated in. The Applicants use many of the same BMPs because they have similar soils and grow similar crops. There are three main categories of BMPs implemented in the EAA: nutrient and sediment control BMPs, particulate matter and sediment control BMPs, and water management BMPs. See Fla. Admin. Code R. 40E-63.136, Appendix A2. The BMPs proposed by the Applicants are based on research in the EAA and recommendations specifically for EAA soils and the crops grown there. The Applications do not identify the specific BMPs that will be implemented, but only the number of BMPs that will be selected from each of the BMP categories (i.e., sediment control). The Applicants must use BMPs on the District’s list of approved BMPs unless an alternative BMP is requested and approved. The lack of greater detail was explained as necessitated by the need for flexibility during the life of the permit to adapt BMPs to varied crops and conditions. Audubon does not believe the BMP plans are tailored enough, but there is no rule criterion for determining how tailored BMP plans must be, except they must achieve the overall goal of reducing phosphorus loading in discharges from the EAA by at least 25 percent. This goal is being achieved.2/ Audubon did not show that any particular BMP being used by an Applicant was the wrong BMP for a particular soil and crop, or identify the BMP that Audubon believes should be used. Audubon failed to prove that the Applicants’ BMP plans do not meet applicable requirements. Whether the Applications Are Complete Audubon contends that the WOD Permits must be denied because the Applications are incomplete. Many of Audubon’s completeness issues deal with minor discrepancies of a type that are more appropriately resolved between the District and applicants, not violations of criteria that are likely to affect a third party’s interest in environmental protection. Rule 40E-63.130 lists the requirements for a permit application for activities in the EAA Basin. An Application Guidebook is incorporated into chapter 40E-63, which contains instructions for completing the application. For applications to renew a permit, the practice of the District is to not require the resubmittal of information that was previously submitted to the District and which has not changed. The Application Guidebook explains this practice. The Applicants supplemented their applications at the final hearing to provide information that Audubon claimed was omitted from the Applications.3/ Audubon contends that the Applications are incomplete because some application forms are not dated and other forms are not signed by appropriate entities. The District explained its rule interpretation and practices associated with the forms. Additional signatures and dates were submitted at the final hearing. Audubon failed to demonstrate that the Applications are incomplete based on the identity of the persons who signed application forms or the lack of dates. Audubon contends the Applications are incomplete because copies of contracts or agreements are not included as required by rule 40E-63.132(3). Audubon failed to prove that contracts and agreements exist that were not included. Audubon contends the Applications are incomplete because they do not contain a completed Form 0779, entitled “Application For A Works Of The District Permit,” as required by rule 40E-63.132(5). In some cases, the information for Form 0779 had been previously submitted and was unchanged, so the District did not require it to be resubmitted for the permit renewal. Additional information was provided at the final hearing. Audubon failed to prove that the Applications are incomplete based on missing information on Form 0779. Audubon contends that the Applications are incomplete because documentation regarding leased parcels was missing. Pursuant to rule 40E-63.130(1)(a), individual permit applications must be submitted by the owner of the land on which a structure is located and any entity responsible for operating the structure, and the permit application must include the owners of all parcels which discharge water tributary to the structure. Applications may be submitted by a lessee if the lessee has the legal and financial capability of implementing the BMP Plan and other permit conditions. The District explained that when applications are submitted by a lessee who will be the permittee or co-permittee, the District requires the lessee to be a responsible party for the entire term of the permit, which is five years. If the lessee is a not a co-permittee, the District does not require information about the lease and does not require the lessee’s signature. If the lessee is a co-permittee, but the lease expires during the term of the permit, the District requires the applicant to modify the permit when the lease expires. Audubon failed to prove that the Applications are incomplete based on lease information Audubon contends that the Applications are incomplete because they fail to show that the Applicants participated in an education and training program as required by rule 40E- 63.136(1)(g). The preponderance of the evidence shows that the Applicants participated in education and training programs. Audubon failed to prove that the Applications are incomplete for any of the reasons raised in its petition for hearing or advanced at the final hearing. Water Quality Standards in the EAA Audubon presented some evidence of algal accumulations in ditches and canals, but the evidence was insufficient to prove the Applicants are violating water quality standards applicable in the EAA. Summary Audubon failed to carry its burden to prove that the Applicants are not entitled to the WOD Permits.
Recommendation Based on the foregoing Findings of Facts and Conclusions of Law, it is RECOMMENDED that South Florida Water Management District issue Permit Nos. 50-00031-E, 50-00018-E, and 50-00047-E. DONE AND ENTERED this 10th day of February, 2014, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 10th day of February, 2014.
The Issue The issues in this case are whether penalties should be imposed and investigative costs and expenses assessed against Respondent for water supply system violations; and, if so, the amount of the penalties and assessments.
Findings Of Fact Respondent, Premier Construction Group, Inc., owns and operates a water treatment plant and associated piping in a commercial building it owns and leases at 2315 Highway 41 North in Inverness. The water treatment plant consists of a 500- gallon tank that holds groundwater pumped from a well. The water in the tank is treated with chlorine and distributed throughout the building for potable water use. The water system serves 25 or more people daily for at least 60 days a year and serves the same people for over six months a year. Respondent owned and operated the water system for 18 and a half years with no violations. Respondent hired a licensed water treatment plant operator to monitor and ensure compliance with applicable DEP rules. In August 2009, Respondent’s licensed operator increased his price substantially. Rick Suggs, as Respondent’s owner and president, disputed the increase and asked the licensed operator to reconsider. Family obligations then required Mr. Suggs to travel to South Carolina for an extended period of time, and Respondent did not attend to the matter further. By the end of August 2009, Respondent’s licensed operator notified DEP that he would no longer be servicing Respondent’s water system as of the end of the month. On August 24, 2009, DEP mailed Respondent a letter relaying this information and putting Respondent on notice that a new licensed operator would have to be hired for September. Notwithstanding Respondent’s communications with its licensed operator and DEP in August, Respondent did not hire a new licensed operator. Mr. Suggs testified that Respondent did not know its licensed operator actually quit until later in September. When this was brought to Mr. Suggs’ attention, he instructed his office manager to hire a replacement. Respondent thought the matter was resolved, but the supposed replacement did not proceed with the work. While Respondent was without a licensed operator, the residual chlorine in the system dropped to zero when tested by DEP on September 17, 24, and 30 and on October 7 and 13, 2009. As a result, the water system did not comply with disinfection requirements during September and October 2009. Respondent did not notify DEP of its failure to comply with disinfection requirements in September and October 2009. No monthly operation reports were submitted to DEP for Respondent’s water system for September or October 2009. No bacteriological samples were collected from Respondent’s water system for the months of September and October 2009. Respondent did not notify DEP of its failure to collect bacteriological samples in September and October 2009. While without a licensed operator, Respondent did not provide public notification of its failure to collect bacteriological samples in September and October 2009. Well into October 2009, Respondent became aware that the supposed replacement licensed operator was not doing work for Respondent. Mr. Suggs hired a replacement licensed operator named Mike Watson, who began servicing Respondent’s water system on November 17, 2009. Public notification of Respondent’s failure to collect bacteriological samples in September and October 2009 was given on November 25, 2009. On December 11, 2009, Respondent submitted a completed DEP Form 62-555.900(22), Certification of Delivery of Public Notice, as to its failure to notify the public of its failure to collect bacteriological samples in September and October 2009. By not having a licensed operator in September and October 2009, Respondent saved $332. By not having bacteriological samples collected and tested in September and October 2009, Respondent saved $60. There was evidence that DEP spent approximately $678 investigating and enforcing the violations. More may have been spent, but no evidence of any additional costs or expenses was presented. There was no evidence of any other water treatment violations by Respondent after October 2009. Although there was a potential that the violations could have posed a health threat, there was no evidence that the public’s health actually was threatened by Respondent’s violations. The water system was tested on November 18, 2009, and did not have any coliform bacteria. The NOV includes corrective actions (essentially coming into and staying in compliance), which Respondent already has taken. The NOV requests that penalties be paid within 30 days by cashier’s check or money order made payable to the “State of Florida Department of Environmental Protection” and including the notations OGC File No. 09-3847-09-PW and “Ecosystem Management and Restoration Trust Fund” to be mailed to DEP’s Southwest District office at 13051 North Telecom Parkway, Temple Terrace, Florida 33637. Respondent believes the penalties sought by DEP in this case are excessive. Mr. Suggs cited Respondent’s clean record for 18 and a half years, his personal and financial difficulties during the two months when the violations occurred, and his responsiveness in correcting violations beginning in November 2009. Mr. Suggs testified that, during mediation, DEP informed him that the penalties could have totaled $115,000 if an unexplained “matrix” had been used to calculate the penalties. Mr. Suggs thought $115,000 was “ludicrous.” Mr. Suggs also requests that the lesser penalties sought in the NOV be further reduced, especially considering that Respondent paid a lawyer $2,800 for representation earlier in the proceeding, until the lawyer withdrew from the case.
The Issue Whether the applicants own the property in question? Whether the project would comply with the criteria of the South Florida Water Management District contained in Basis of Review for Surface Water Management Systems, specifically Sections 3.1.3 and 3.2? Whether flood protection would be inadequate or septic tanks unsuitable or whether the public health and safety would be compromised or the ultimate purchasers be deprived of usage of the property due to inundation in violation of Chapter 373, Florida Statutes (1981), or Rule 40E-4.301(1), Florida Administrative Code?
Findings Of Fact Ms. Williamson and Messrs. Leggett and Collins hold in fee simple a triangular 117.24-acre parcel in Okeechobee County as tenants in common under a warranty deed executed in their favor by one W. C. Sherman. They propose to develop the property as a trailer park (complete with airstrip) large enough to accommodate 109 trailers. To this end, soil would be dug up from the center of the property and used to raise the elevation of the surrounding land above the 100-year floodplain. (T. 47) The applicants have a dredging permit from the Department of Environmental Regulation authorizing them to excavate 629,889 cubic yards. They are proposing to dig to a depth of 76 feet below ground. This would create an 18-acre body of water ("Poe's Lake") which would overflow a V-notched weir into a county canal. The county canal would take the water to C- 38, one of the large canals to which the Kissimmee River has been relegated, at a point about 18 miles upstream from Lake Okeechobee. Runoff would wash over residential lots and roadways; the site would be graded to assure drainage into Poe's Lake. The minimum road crest elevation would be 30 feet NGVD ("[a]round twenty-nine feet" T.52), as compared to the control elevation for surface waters of 28.5 feet NGVD. WATER QUALITY The developers plan septic tanks for wastewater treatment. At the close of all the evidence, counsel for the applicants stated that sanitary sewers could be installed instead. Respondents' Proposed Recommended Order, p. With all the housing units in use, at least 10,900 gallons of effluent would seep into the ground from the tanks daily. There would be some evapotranspiration, but all the chemicals dissolved in the effluent would eventually end up in the groundwater. During the dry season, septic tank effluent would cause mounding of the groundwater and some groundwater movement toward, and eventual seepage into, Poe's Lake. The eventual result would be eutrophication and the growth of algae or macrophytes on the surface of Poe's Lake. This would cause dissolved oxygen violations in Poe's Lake. Discharges from the lake would inevitably occur, aggravating the situation in C-38, which already experiences dissolved oxygen levels below 5.0 milligrams per liter in the rainy summer months. Some fraction of the nutrients in the effluent from the septic tanks would ultimately reach Lake Okeechobee itself. The sheer depth of the excavation would create another water quality problem. Under the anaerobic conditions that would obtain at the bottom of Poe's Lake, bacteria acting on naturally occurring sulfates would produce hydrogen sulfide, ammonia and various other reduced organic nitrogen compounds. These substances are toxic to human beings and would, in some indeterminate quantity, enter the groundwater from Poe's Lake. This would affect the taste and perhaps the potability of water from any well nearby. It would be "possible to design a better system where there would be nutrient removal and a greatly reduced probability of violation of the dissolved oxygen criterion and obviation of the potential for ground water contamination." (T. 200) Installation of a baffle on the weir would serve to prevent buoyant debris from entering surface waters of the state. BASIS OF REVIEW Official recognition was taken of the "Basis of Review for Surface Water Management Permit Applications Within the South Florid Water Management District," parts of which all parties agree pertain in the present proceedings. Among the criteria stated in this document are: 3.1.3 Waste and Wastewater Service - Potable water and wastewater facilities must be identified. The Applicant for a Surface Water Management Permit must provide information on how these services are to be provided. If wastewater disposal is accomplished on-site, additional information will normally be requested regarding separation of waste and storm systems. 3.2.1.4 Flood protection - Building floors shall be above the 100 year flood elevations, as determined from the most appropriate information, including Federal Flood Insurance Rate Maps. Both tidal flooding and the 100 year, 3 day storm event shall be considered in determining elevations. b. Commercial and industrial projects to be subdivided for sale are required to have installed by the permittee, as a minimum, the required water quality system for one inch of runoff detention or one half inch of runoff retention from the total developed site. State standards - Projects shall be designed so that discharges will meet State water quality standards, as set forth in Chapter 17-3, Retention/detention criteria - Retention and/or detention in the overall system, including swales, lakes, canals, greenways, etc., shall be provided for one of the three following criteria or equivalent combinations thereof . . . Wet detention volume shall be provided for the first inch of runoff from the developed project, or the total runoff from a 3-year, 1-hour rainfall event, whichever is greater. Dry detention volume shall be provided equal to 75 percent of the above amounts computed for wet detention. Retention volume shall be provided equal to 50 percent of the above amounts computed for wet detention. 3.2.4.1 Discharge structures should include gratings for safety and maintenance purposes. The use of trash collection screens is desirable. Discharge structures shall include a "baffle" system to encourage discharge from the center of the water column rather than the top or bottom. 3.2.4.4.2 b. Control elevations should be no higher than 2 feet below the minimum road centerline elevation in the area served by the control device in order to protect the road subgrade. Simply detaining runoff before discharging it offsite will not insure that the water quality standards set forth in Chapter 17-3 will be met. Whether the standards are met depends on, among other things, the composition of the runoff. FWF'S INTEREST Among the purposes of the FWF, as stated in its charter, Shall be to further advance the cause of conservation in environmental protection, to perpetuate and conserve fish and wildlife, oil, water, clean air, other resources of the State and so manage the use of all natural resources, that this generation and posterity will receive the maximum benefit from the same. (T. 248-9) Four or five thousand Floridians belong to FWF. FWF members "make use" (T. 250) of the waters of Lake Okeechobee, the Kissimmee River and specifically of the waters in C-38. PROPOSED FINDINGS CONSIDERED The applicants and FWF filed post hearing memoranda and proposed recommended orders including proposed findings of fact which have been considered in preparation of the foregoing findings of fact. They have been adopted, in substance, for the most part. To the extent they have been rejected, they have been deemed unsupported by the weight of the evidence, immaterial, cumulative or subordinate.
Recommendation Upon consideration of the foregoing, it is RECOMMENDED: That SFWMD deny the pending application for surface water management permit. DONE and ENTERED this 29th day of November, 1983, in Tallahassee, Florida. ROBERT T. BENTON II, Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 29th day of November, 1983. COPIES FURNISHED: Dennis J. Powers, Esquire Gunster, Yoakley, Criser & Stewart 400 South County Road Palm Beach 33480 Terrell K. Arline, Esquire 325-C Clematis Street West Palm Beach, Florida 33401 Irene Kennedy Quincey, Esquire 3301 Gun Club Road West Palm Beach, Florida 33406 Charles P. Houston, Esquire 324 Datura Street, Suite 106 West Palm Beach, Florida 33401
The Issue The issue is whether Respondent's water use permit should be revoked for nonuse of the permit for a period of two years or more.
Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Background The District is a state agency charged with the responsibility of issuing water use permits under Chapter 373, Florida Statutes, and Florida Administrative Code Chapter 40B- 2 for the geographic area under its statutory jurisdiction. Alachua County is within that geographic jurisdiction. Respondent is a Florida corporation with offices at 700 Northwest Cheeota Avenue, High Springs, in northern Alachua County. It owns approximately 700 acres in High Springs (west of Interstate Highway 75) on which it operates a church retreat and summer camping and recreational facility known as Camp Kulaqua. The property surrounds, and is contiguous to, Hornsby Spring, a first-order magnitude spring (having a flow rate of 100 CFS or greater) which, under normal conditions, discharges into the nearby Santa Fe River. Hornsby Spring is one of 296 documented springs within the District's jurisdiction. After receiving an overture from a representative of a private water bottling company, on September 28, 1999, Respondent filed an application for a General Water Use Permit in Township 7 South, Range 17 East, Section 26, in High Springs. In its application, Respondent represented that it desired a daily allocation of 2,000,000 gallons; that it intended to install two 12-inch wells, each having a capacity of 1,400 gallons per minute, just east of, and upgradient from, Hornsby Spring; and that all water withdrawals would be used in conjunction with a privately-owned commercial spring water bottling facility to be located on its property. The application also represented that the facility would employ 36 persons and operate 168 hours per week. The application was reviewed by a former District hydrogeologist, William H. Kirk. During the review process, and in response to Mr. Kirk's request for more information, Respondent provided a comparison of the requested allocation with the overall flow of Hornsby Spring. This was because Mr. Kirk was concerned that the requested allocation was "a bit high," and he wanted to ensure that the issuance of the permit would not cause harm to, or adversely affect, the water resources. Under a professional guideline that Mr. Kirk used, if the applicant could show that the cumulative amount being withdrawn was to be less than ten percent of what the available data showed to be the mean spring flow, the District would consider it to be "an acceptable impact." Notwithstanding Mr. Kirk's use of this guideline, the District points out that there is no District rule or policy sanctioning the ten percent rule, and at hearing it denied that this standard is used by the District in assessing water use applications. Further, the Permit itself does not refer to a relationship between spring flow and the size of the allocation. Even so, this analysis was considered by Mr. Kirk in determining whether Respondent had given reasonable assurance that the spring would not be impacted. In its response to the request for additional information, Respondent reduced its requested allocation to 750,000 gallons per day and indicated that if a bottling plant were to be constructed on its property, approximately 700,000 gallons of the total allocation would be consumed in "bulk transfer and bottling," with the remainder for camp use. More specifically, Respondent indicated that it would allocate 490,000 gallons per day for bulk transport, 210,000 gallons per day for spring bottling water, and 50,000 gallons per day for incidental uses at its property. By reducing the allocation from 2,000,000 gallons per day to 750,000 gallons per day, Respondent's requested average daily allocation represented only 0.4 percent of the average daily spring flow as measured over the last 28 years. The reduced allocation satisfied Mr. Kirk's concern that Respondent demonstrate a reasonable demand and a reasonable need for that allocation, and he recommended approval of the application.2 On February 25, 2000, the District approved the application and issued Water Use Permit No. 2-99-00130 (Permit).3 The Permit authorizes an average daily withdrawal of 0.7500 million gallons per day (750,000 gallons per day) or a maximum daily withdrawal and use of 0.7500 million gallons per day with an annual allocation not to exceed 273.750 million gallons (273,750,000 gallons) per calendar year in conjunction with the operation of a privately-owned water bottling plant. The Permit expires on February 25, 2020. After the Permit was issued, under the regulatory process in place, Respondent was required first to obtain a permit for a temporary test well which would be used to collect information concerning the site of the proposed activity, and to then file an application for permits authorizing the construction and operation of the two 12-inch production wells. The Permit contains a number of conditions, two of which require a brief comment. First, Condition No. 2 provides that "[t]his permit is classified as unconfined [F]loridan aquifer for privately owned bottled water plant." This means that all water withdrawals must be made from the unconfined Floridan aquifer, as opposed to the spring head of Hornsby Spring. (Respondent's proposed siting of its two production wells 660 yards east of the spring is consistent with this provision.) Second, Condition No. 4 provides that "[t]he permittee shall submit daily pumpage records on a monthly basis to the [District]." Pumpage reports are filed by permittees so that the District can determine whether the permit is actually being used, and if so, to ensure that the amount of water being withdrawn under the permit does not exceed the authorized allocation. As it turned out, pumpage reports were never filed by Respondent. (However, the record shows that the District has never strictly enforced this requirement for any permittee.) In late 2002, the District staff undertook a review of the nine water bottling permit holders within its jurisdiction, including Respondent. That category of permit holders was selected for review because of the small number of permits and the limited resources of the District staff. (In all, the District has probably issued several thousand permits to other types of users.) On February 4, 2003, the District served its Complaint under the authority of Sections 120.60 and 373.243, Florida Statutes, and Florida Administrative Code Rule 40B-2.341. As grounds for revoking the permit, the District alleged that there was "non-use of the water supply allowed by the permit for a period of two (2) years or more." Although Respondent contends that it should have been given an opportunity to correct the nonuse allegation before the Complaint was issued, nothing in the Administrative Procedure Act or District rules requires that this be done. Until the issuance of the Complaint against Respondent in early 2003, and similar Complaints against eight other permit holders at the same time, the District had never invoked this statutory provision.4 There is no evidence to support Respondent's contention that the Complaints were issued for "purely political reasons." On March 4, 2003, Respondent requested a formal hearing challenging the District's proposed action. In the parties' Pre-Hearing Stipulation, the issues have been broadly described as follows: whether Section 373.243(4), Florida Statutes, is to be strictly or liberally construed; whether Respondent's nonuse is based upon extreme hardship for reasons beyond its control; and whether the District is equitably estopped from permit revocation. (According to the District, even if the Permit is revoked, such revocation is without prejudice to Respondent reapplying for, and receiving, another permit so long as it meets all applicable requirements.) Equitable Estoppel Respondent first contends that the District is estopped from revoking its Permit on the theory that, under the circumstances here, the doctrine of equitable estoppel applies. For that doctrine to apply, however, Respondent must show that the District made a representation as to a material fact that is contrary to a later asserted position; that Respondent relied upon that representation; and that the District then changed its position in a manner that was detrimental to Respondent. See, e.g., Salz v. Dep't of Admin., Div. of Retirement, 432 So. 2d 1376, 1378 (Fla. 3d DCA 1983). The District issued Respondent's Permit on the condition that Respondent operate in conformity with all pertinent statutes and regulations. This finding is consistent with language on the face of the Permit, which states that the Permit "may be permanently or temporarily revoked, in whole or in part, for the violation of the conditions of the permit or for the violation of any provision of the Water Resources Act and regulations thereunder." Respondent relied on the District's representation that it could use the Permit so long as it complied with all statutes and regulations. In reliance on that representation, in addition to staff time, after its Permit was issued, Respondent expended "somewhere around" $70,000.00 to $74,000.00 for conducting water quality testing; sending cave divers underground to ascertain the correct location of the portion of the aquifer on which to place its production wells; drilling a 6-inch test well in August 2000; obtaining the City of High Springs' approval in March 2000 for industrial zoning on a 10-acre tract of land on which to site a "water plant"; and engaging the services of a professional who assisted Respondent in "seeking out businesses and getting the right qualifications of the spring water to make sure that it was a marketable water." The District has never asserted anything different from its original position: that if Petitioner complied with all statutes and rules, it could continue to lawfully make water withdrawals under its Permit. The issuance of the Complaint did not represent a change in the District's position. Because a change in position in a manner that was detrimental to Respondent did not occur, the necessary elements to invoke the doctrine of equitable estoppel are not present. Was the Permit Used? A preliminary review by District staff indicated that Respondent had never filed the daily pumpage reports on a monthly basis and had never requested permits authorizing the construction of the two 12-inch production wells. These preliminary observations were confirmed at final hearing, along with the fact that Respondent has never entered into an agreement with a water bottling company (although draft agreements were once prepared); that Respondent has never constructed a water bottling facility; and that no operations were ever conducted under the Permit. Therefore, the evidence supports a finding that Respondent did not use its Permit for the two-year period after it was issued, as alleged in the Complaint. Respondent's contention that the evidence fails to support this finding belies the evidence of record. In an effort to show that it actually used the Permit, Respondent points out that in August 2000 it applied for, and received a permit to construct, an unmetered 6-inch test well in association with its General Water Use Permit. (Respondent sometimes erroneously refers to the test well as a test production well. This is incorrect as the well is a test well, and not a production well.) After the test well was installed, at some point Respondent says it began withdrawing approximately 50,000 gallons per day of water from that well for incidental uses associated with the operation of Camp Kulaqua.5 These withdrawals were made on the assumption that the test well permit fell under the broad umbrella of the General Water Use Permit. (Respondent also has a permitted 6- inch diameter well and an unregulated 4-inch well on its premises, both of which are used for water supply needs at Camp Kulaqua.) It is true, as Respondent asserts, that its Permit authorized incidental withdrawals of up to 50,000 gallons per day for unspecified uses at Camp Kulaqua. However, these withdrawals are authorized under the General Water Use Permit and not the test well permit. The two permits are separate and distinct. On the one hand, a test well is intended to be temporary in nature and used only for the purpose of test well development and collecting information regarding the height of the aquifer and water quality at the site of the proposed activity. Conversely, withdrawals for any other purpose, even incidental, must be made from the production wells, which are only authorized by the General Water Use Permit. Before a test well can be used for normal consumptive purposes, the permit holder must seek a modification of the permit to include it as a part of its general water use permit. Here, no such modification was sought by Respondent, and no authorization was given by the District. Therefore, Respondent's incidental water uses associated with its test well cannot be counted as "uses" for the purpose of complying with the use requirement in Section 373.243(4), Florida Statutes. In light of the District's credible assertion to the contrary, Respondent's contention that it is common practice to lawfully withdraw water from a test well for incidental consumptive purposes has been rejected. (It is noted, however, that the District has not charged Respondent with violating the terms of its test well permit.) Extreme Hardship Under Section 373.243, Florida Statutes (which was enacted in 1972), the District is authorized to revoke a water use permit "for nonuse of the water supply allowed by the permit for a period of 2 years." However, if the user "can prove that his or her nonuse was due to extreme hardship caused by factors beyond the user's control," revocation of the permit is not warranted. The phrase "extreme hardship caused by factors beyond the user's control" is not defined by statute or rule. In the context of this case, however, the District considers an extreme hardship to occur under two scenarios. First, if the aquifer level has dropped so low due to drought conditions that a permit holder cannot access the water through its well, its nonuse is excusable. Alternatively, if an emergency order has been issued by the District directing permit holders (including Respondent) to stop pumping due to certain conditions, an extreme hardship has occurred. (Presumably, a severe water shortage would precipitate such an order.) In this case, the District issued a water shortage advisory, but not an emergency order, due to a "severe drought," indicating that users could still pump water, but were encouraged to voluntarily reduce their usage. This advisory remained in effect from the summer of 1998 until the spring of 2003, when a severe drought ended. However, no emergency order was ever issued by the District. Respondent contends that its nonuse was due to an extreme hardship caused by factors beyond its control. More specifically, it argues that a severe drought occurred in Alachua County during the years 1998-2003, and that under these conditions, federal regulations prevented it from withdrawing water for bottling purposes, which was the primary purpose for securing a permit. Further, even if it had withdrawn water during these drought conditions, such withdrawals could have adversely impacted Hornsby Spring and constituted a violation of a District requirement that water resources not be adversely impacted. Because an investment of several hundred thousand dollars was required to drill and install the two production wells, Respondent contends it was not financially prudent to make that type of investment and begin operations until normal spring conditions returned. These contentions are discussed in greater detail below. Around September 7, 1999, a representative of a water bottling company first approached Respondent about the possibility of the two jointly operating a water bottling plant and/or transporting water in bulk from Respondent's property. Prompted by this interest, less than three weeks later Respondent filed its application for a water use permit (although at that time it did not mention on the application that off-site bulk transfers would occur), and a permit was eventually issued in February 2000. Later, and through a professional firm it employed, Respondent had discussions with representatives of several bottling companies, including Great Springs Waters of America (Great Springs) and Perrier Group of America. Apparently, these more serious discussions with a potential suitor did not take place until either late 2000 or the spring of 2001. Periodic measurements taken by District staff at Hornsby Spring reflected natural drought conditions from April 2000 to April 2003. As noted earlier, this was the product of a "severe drought" which took place between the summer of 1998 and the spring of 2003; the drought was one of a magnitude that occurs only once in every 50 to 100 years. During the years 2000 through 2002, the spring had zero flow or was barely flowing much of the time.6 Had Respondent pumped water during 20 out of the 24 months after the Permit was issued, it could have potentially violated the requirement that it not harm Hornsby Spring. This fact is acknowleged by a District witness who agreed that if the "spring is not flowing, . . . [pumping] would have an [adverse] impact." Even as late as October 2003, the spring had tannic discoloration caused by the lengthy drought conditions. The parties agree, however, that there is no water shortage in the District at the present time. To illustrate the difficulty that it experienced in obtaining a joint venture partner for water bottling purposes, Respondent established that in the spring of 2001, a Great Springs representative visited the site when the spring was "barely flowing." For obvious reasons, Respondent could not "bring a party there who would want to enter into a business [agreement]" under those conditions. These same conditions remained in effect during most of the two year period. The District points out, however, that even though the spring was low or barely flowing, so long as the aquifer itself was not too low, Respondent could still withdraw water from the aquifer, since Condition 2 of the Permit authorizes withdrawals from the aquifer, and not the spring. The reason for this apparent anomaly is that when a spring ceases to flow, the aquifer has simply dropped below the level of the spring vent; even under these circumstances, however, there may still be a substantial quantity of water in the aquifer available for pumping. Assuming that it could still lawfully pump water when the spring was dry or barely flowing without causing adverse impacts to the spring, Respondent was still subject to federal regulations which govern the bottling of spring water. See Title 21, Part 165, C.F.R. For spring water to be marketed as bottled "spring water," 21 C.F.R. § 165.119(2)(vi) requires that the water "be collected only at the spring or through a bore hole tapping the underground formation feeding the spring." This means that the bore hole had to be physically connected with the cave system feeding Hornsby Spring or produce water of the same quality as that discharging from the spring. The regulation goes on to provide that "[i]f spring water is collected with the use of an external force [such as by a pump], water must continue to flow naturally to the surface of the earth through the spring's natural orifice." While this regulation obviously does not prohibit Respondent from pumping water, since that authority lies within the District's exclusive jurisdiction, it does provide that in order to use spring water for bottling purposes, the water must continue to flow naturally from the aquifer to the spring. If it does not, the water cannot be used for this purpose. Because Hornsby Spring had zero flow for parts of 2001 and 2002, and severely reduced flows during most of the other time during the two-year period ending February 2002, Respondent was effectively prevented by the foregoing regulation from using the water for bottling purposes. Therefore, Respondent's nonuse was due to extreme hardship caused by factors beyond its control -- a severe drought lasting throughout the two-year period after the Permit was issued, and federal regulations which prevented it from using water for the purpose for which the Permit was issued. Thus, the nonuse is excusable.
The Issue The issues are whether Respondent violated Rule 62-532.500(2)(d)1., Florida Administrative Code, by failing to seat a well casing in a rock layer or other such consolidated formation, and if so, what penalty should be imposed.
Findings Of Fact Respondent is charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries. Respondent's duties include the regulation of water wells and water well contractors. Respondent is a water well contractor. As such, he holds Water Well Contractor License No. 2215. On September 25, 1997, Petitioner issued Respondent Well Construction Permit No. 597679.01. The permit gave Petitioner permission to construct a water well, four-inches in diameter, on property owned by Rex Hobbs in Pasco County. Respondent subsequently constructed the water well on the property owned by Mr. Hobbs, using the cable tool construction method. Respondent completed construction of the well on or about October 20, 1997. After the well was constructed, Mr. Hobbs complained to Respondent on several occasions that the well was producing sand, rock, and other debris. Respondent made no attempt to repair the well. In May or June of 1998, Mr. Hobbs filed a complaint with Petitioner regarding the construction of the well on his property. Petitioner's subsequent field investigation did not reveal a significant amount of sediment in the well water. Mr. Hobbs filed a second complaint with Petitioner in the summer of 1998, insisting that the water from his well contained an excess amount of sediment. Petitioner's second field investigation revealed an abnormal amount of sediment in the well water. On July 9, 1998, Petitioner issued a Notice of Violation, advising Respondent that he had violated Rule 40D-3.037(1), Florida Administrative Code, by failing to seat the casing of the Hobbs well into a consolidated formation. Water from the Hobbs well contains sediments including sand, rock, and other debris. These sediments interfere with the operation of plumbing, appliances, and irrigation devices, which utilize water supplied by the well. The quality of the well water produced by the Hobbs water well is unacceptable. The total depth of the Hobbs well is 131 feet below land surface. The well is cased to 42 feet below land surface. The water pump is set at 84 or 86 feet below land surface. The static water level was 58.2 feet below the land surface. The geologic formation at the end of the casing of the well contains gray clay, yellow clay, limerock, and sand. The end of the casing is not seated in a layer of rock or other consolidated formation. There is no persuasive testimony to the contrary. The area in which the well is located is geologically unstable. Wells in that area generally require 84 feet of casing. Respondent admitted at the hearing that the well is producing sand and needs more "pipe." Failure to seat a well casing into a consolidated formation is a major violation under the Florida Department of Environmental Protection's Water Well Contractor Disciplinary Guidelines and Procedures Manual. Respondent has entered into three previous Consent Orders with Petitioner to resolve permitting and construction violations.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED: That Petitioner enter a final order requiring Respondent to pay an administrative fine in the amount of $500 and assessing five points against his water well contractor's license. DONE AND ENTERED this 18th day of August, 1999, in Tallahassee, Leon County, Florida. SUZANNE F. HOOD 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 18th day of August, 1999. COPIES FURNISHED: Margaret M. Lytle, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Tony Holt 6145 Durant Road Durant, Florida 33530 E. D. Sonny Vegara, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899
