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JOSEPH SMITH, LENA SMITH, EUGENE COLWELL, ANNA COLWELL, JERRY HARRIS, AND BRENDA HARRIS vs ST. JOHNS RIVER WATER MANAGEMENT DISTRICT, 94-000544 (1994)
Division of Administrative Hearings, Florida Filed:Ocala, Florida Jan. 31, 1994 Number: 94-000544 Latest Update: Nov. 01, 1994

Findings Of Fact The Parties. The Petitioners, Joseph and Lena Smith, Eugene and Anna Colwell, and Jerry and Brenda Harris, are littoral owners and operators of sports fishing facilities on Orange Lake, a freshwater body of approximately 7,000 acres of open water and 15,000 acres of associated wetlands, whose southern margin constitutes the boundary between Alachua and Marion Counties in north central Florida. Respondent, the St. Johns River Water Management District (hereinafter referred to as the "District"), is a special taxing district created by Chapter 373, Florida Statutes, charged with the statutory responsibility for the management of water and related land resources; the promotion of conservation, development, and proper utilization of surface and ground water; and the preservation of natural resources, fish and wildlife, pursuant to Chapter 373, Florida Statutes. Intervenor, the Sierra Club, Inc. (hereinafter referred to as "Sierra"), is a not-for-profit California corporation registered to do business within the State of Florida. Sierra is an international corporation whose purpose is to explore, enjoy and protect the natural resources of the earth. Intervenor, Florida Defenders of the Environment, Inc. (hereinafter referred to as "Florida Defenders"), is a not-for-profit Florida corporation whose purpose is to preserve and restore Florida's natural resources. Intervenor, the Florida Department of Environmental Protection (hereinafter referred to as "DEP"), is an agency of the State of Florida charged with the responsibility of controlling and prohibiting pollution of the air and water of the State of Florida. See Chapter 403, Florida Statutes. DEP is also charged with responsibility for management of the Paynes Prairie State Preserve. Section 373.026, Florida Statutes. Intervenor, the Attorney General of the State of Florida (hereinafter referred to as the "Attorney General"), sits as a Trustee of the sovereignty submerged lands of the State and as one of the legal owners of the State's property including the Paynes Prairie State Preserve. The Challenged Rules. The District issued an order on November 7, 1993, authorizing the publication of a notice of intent to amend Chapter 40C-2, Florida Administrative Code, by adopting proposed Rule 40C-2.302, Florida Administrative Code, and amending Rule 40C-2.051(6), Florida Administrative Code (hereinafter jointly referred to as the "Challenged Rules"). Proposed Rule 40C-2.302, Florida Administrative Code (hereinafter individually referred to as the "Reservation Rule"), provides: 40C-2.302 Reservation of Water From Use. The Governing Board finds that reserving a certain portion of the surface water flow through Prairie Creek and Camps Canal south of Newnans Lake in Alachua County, Florida, is necessary in order to protect the fish and wildlife which utilize the Paynes Prairie State Preserve, in Alachua County, Florida. The Board therefore reserves from use by permit applicants that portion of surface water flow in Prairie Creek and Camps Canal that drains by gravity through an existing multiple culvert structure into Paynes Prairie. this reservation is for an average flow of [35] cubic fee per second (23 million gallons per day_ representing approximately forty five per cent (45 percent) of the calculated historic flow of surface water through Prairie Creek and Camps Canal. The specific authority for the Reservation Rule is Sections 373.044, 373.113, 373.171, 373.216 and 373.219, Florida Statutes. The law implemented by the Reservation Rule is Sections 373.219 and 373.223, Florida Statutes. The proposed amendment to Rule 40C-2.051, Florida Administrative Code (hereinafter individually referred to as the "Exemption Rule"), provides, in pertinent part: 40C-5.2.051 Exemptions. No permit shall be required under the provisions of this rule for the following water uses: through (5) No change (6) Water, whether withdrawn or diverted, when used for purposes of protection of fish and wildlife or the public health and safety when and where the Governing Board has, by regulation, reserved said water from use by permit applicant pursuant to Subsection 373.223(3), F.S. The specific authority for the Exemption rule is Sections 373.044, 373.113 and 373.171, Florida Statutes. The law implemented by the Exemption Rule is Sections 373.103, 373.171, 373.216, 373.219, 403.501 et seq. and 288.501 et seq., Florida Statutes. Orange Creek Basin. Orange Creek Basin is the name given to the hydrological features of approximately 400 square miles of Alachua, Putnam and Marion Counties, Florida. Orange Creek Basin is a major sub-basin of the Lower Ocklawaha River Basin. Surface water in the Orange Creek Basin flows generally in a north to south direction Orange Creek Basin is made up of several sub-basins, including Newnans Lake, Paynes Prairie, Orange Lake and Lochloosa Lake sub-basins. Surface water within the approximately 100 square miles of Newnans Lake sub-basin drains into Newnans Lake. When sufficiently high, water in Newnans Lake discharges over a weir structure from the southern end of the lake into Prairie Creek. The weir structure at the southern end of Newnans Lake may be adjusted to control the amount of water flowing into Prairie Creek. The weir was installed in 1966. It was adjusted by the Florida Game and Freshwater Fish Commission in 1976. Water flows south into Prairie Creek, the south and southwest through Prairie Creek to two man-made structures. The first is a gated culvert structure consisting of 3 Culverts (the "Camps Canal Culverts"), through which some of the Prairie Creek water enters Paynes Prairie. The second man-made feature is a levee and a canal named Camps Canal. The levee diverts water in Prairie Creek, which does not flow into Paynes Prairie by gravity, through Camps Canal to the south to the River Styx, which flows into Orange Lake. If the elevation of surface water in Prairie Creek exceeds 58.91 feet National Geodetic Vertical Datum (hereinafter referred to as "NGVD"), a portion of the volume of Prairie Creek will flow, by gravity, into Paynes Prairie through the Camps Canal Culverts. The Paynes Prairie sub-basin covers an area of approximately 49 square miles. Surface water in this sub-basin drains into a natural geological feature known as Alachua Sink. Surface water in the approximately 56 square mile Orange Lake sub- basin flows into Orange Lake. Surface water flows out of Orange Lake through Orange Creek. Outflow is controlled by Orange Lake Dam. The Orange Lake Dam has a fixed crest elevation of 58 feet NGVD. Water levels in Orange Lake must exceed 58 feet NGVD before there is surface water outflow from Orange Lake. Surface water within the approximately 75 square mile Lochloosa Lake sub-basin drains into Lochloosa Lake. Lochloosa Lake has two outlets: Lochloosa Slough in the east and Cross Creek in the south. Cross Creek connects Lochloosa Lake to Orange Lake. Paynes Prairie State Preserve. Prior to the construction of the weir at the outlet from Newnans Lake to Prairie Creek, all surface water from Newnans Lake flowed from Newnans Lake to Prairie Creek unimpeded. Prior to 1927 all surface water in Prairie Creek flowed south into an area known as Paynes Prairie. Paynes Prairie is located in Alachua County. All water in Prairie Creek entered Paynes Prairie and flowed across Paynes Prairie to Alachua Sink. Alachua Sink is a natural geological feature located in the north- central portion of Paynes Prairie. At Alachua Sink surface water enters the Florida aquifer. In 1927 a levee was constructed around the eastern boundary of Paynes Prairie, and Camps Canal was excavated in order to divert water from Paynes Prairie. Due to the levee, water in Prairie Creek was diverted into Camps Canal beginning in approximately 1927. The water flowed into the River Styx and then into Orange Lake. Canals and levees were also constructed within Paynes Prairie to convey surface water in Paynes Prairie into Alachua Sink and Camps Canal. The modifications to Paynes Prairie made in 1927 were intended to drain Paynes Prairie so that the land could be utilized for agricultural purposes, including the raising of cattle. Paynes Prairie continued to be used primarily for the raising of cattle between 1927 and early 1970. In 1970, the State of Florida began acquiring parts of Paynes Prairie. Property acquired by the State was used to create the Paynes Prairie State Preserve (hereinafter referred to as the "Preserve"). Land is still being acquired by the State. The Preserve currently consists of approximately 20,600 acres. Approximately 18,000 acres of the Preserve were acquired within the first 4 years after acquisitions by the State began. Approximately 12,000 acres are considered wetlands. Two major highways, U.S. Highway 441 and Interstate 75 run north-south across the middle and western portion of Paynes Prairie. U.S. 441 was constructed in 1927 and I-75 was constructed in 1964. In 1975 the State of Florida's Department of Natural Resources (which is now DEP) breached the levee at Camps Canal in order to restore part of the water flow from Prairie Creek to the Preserve. In 1979 flashboard riser Culverts were placed in the breach in the Camps Canal levee. In 1988 the Camps Canal Culverts were constructed. The Preserve, a unique land feature, was designated a National Natural Landmark in 1974 by the United States Department of the Interior. No consumptive use permit concerning water that flows into Paynes Prairie or the Preserve has been issued by the District. No consumptive use permits have been issued by the District for surface water withdrawals from Newnans Lake, Prairie Creek or Orange Creek. The Current General Hydrologic Condition of the Preserve. The Preserve is one of the largest continuous wetland systems in Florida and the Southeastern United States. The Preserve and Paynes Prairie constitute one of the largest wetland areas formed by the collapse of a sinkhole, Alachua Sink. Since 1975, at least some water has flowed into the Preserve from Prairie Creek through the Camps Canal Culverts and its predecessors. The "inverts" of the Prairie Creek-Camps Canal Culverts are above the creek-canal bottom. This means that if water in Prairie Creek does not reach a certain level, no water will flow through the Camps Canal Culverts into the Preserve. Under these conditions, all water in Prairie Creek will flow through Camps Canal and eventually to Orange Lake. The amount of water flowing through the Camps Canal Culverts is also limited to a maximum amount due to the size of the Culverts. The exact amount of water that may flow through the Camps Canal Culverts into the Preserve depends on the amount of water in Prairie Creek coming from Newnans Lake and the capacity of the Culverts to move the water. Water flowing into the Preserve through the Camps Canal Culverts constitutes approximately 50 percent of the surface water entering the Preserve. After water flows into the Preserve through the Camps Canal Culverts it flows in a broad, shallow path, referred to as "sheetflow," over the eastern portion of the Preserve. The sheetflow from Camps Canal Culverts creates approximately 550 to 600 acres of shallow marsh community. The water eventually flows into an area known as Alachua Lake in the central portion of the Preserve. Water discharging from Alachua Lake flows through a water control structure consisting of four gated Culverts, known as the Main Structure, into Alachua Sink. Water also enters the Preserve from the north through a tributary known as Sweetwater Branch. Water flows through Sweetwater Branch into Alachua Sink. Sweetwater Branch is channelized over its entire length, preventing water from reaching into the Preserve or Alachua Lake. The District's Purpose in Adopting, and the District's Interpretation of, the Challenged Rules. The District's intent in adopting the Challenge Rules was to reserve water which the District had concluded is required for the protection of fish and wildlife in Paynes Prairie. The District is attempting to carry out its intent by providing in the Reservation Rule that whatever amount of water that may flow through the Camps Canal Culverts by gravity into the Preserve may not be used for other purposes. The District is further attempting to carry out its intent by providing in the Exemption Rule that any amount of water that has been reserved by the District because it is required for the protection of fish and wildlife pursuant to Section 373.223(3), Florida Statutes, exempt from the consumptive use permit process. The Reservation Rule is not intended to reserve a specific quantity of water for the Preserve. Rather, the Reservation Rule reserves only that amount of water that flows through the Camps Canal Culverts by force of gravity. The intent is allow the natural existing hydrologic regime of the Preserve to continue. The quantity of the water reserved by the Reservation Rule is identified, in part, as follows: The Governing Board finds that reserving a certain portion of the surface water flow through Prairie Creek and Camps Canal south of Newnans Lake in Alachua County, Florida, is necessary in order to protect the fish and wildlife which utilize the Paynes Prairie State Preserve, in Alachua County, Florida. The Board therefore reserves from use by permit applicants that portion of surface water flow in Prairie Creek and Camps Canal that drains by gravity through an existing multiple culvert structure into Paynes Prairie. . . . [Emphasis added]. The last sentence of the Reservation Rule goes on to proved: This reservation is for an average flow of [35] cubic feet per second (23 million gallons per day) representing approximately forty five per cent (45 percent) of the calculated historic flow of surface water through Prairie Creek and Camps Canal. This portion of the Reservation Rule was not included by the District to establish a minimum and/or maximum quantity of water that is being reserved for the protection of fish and wildlife in the Preserve. This portion of the Reservation Rule represents a very condensed summary of the historical hydrologic data relied upon by the District in deciding to reserve water for the Preserve's fish and wildlife. The Exemption Rule was intended to make clear that anytime the District reserves water which it determines is required to protect fish and wildlife or the public safety, that no consumptive use permit is necessary. The District's Determination that Water is Necessary for the Protection of Fish and Wildlife in Paynes Prairie. In reaching its decision that the quantity of water flowing through the Camps Canal Culverts by force of gravity into the Preserve is required for the protection of the fish and wildlife of the Preserve, the District relied upon a study of the Orange Creek Basin which District staff had begun in the 1980s. There were three objectives for the Orange Creek Basin study: (a) the first objective of the study was to develop a predictive hydrologic model that could be used to predict water levels throughout the basin and the water courses that connect the various major lakes and prairie systems; (b) the second objective of the Orange Creek Basin study was to develop environmental and hydrologic criteria that could be used to evaluate the environmental impacts of different water management alternatives in the basin; and (c) the third objective was to look at alternatives for management of water within the District. Substantial evidence concerning the manner in which the Orange Creek Basin study was conducted, the results of the study and the rationale for the District's conclusion that the quantity of water flowing through the Camps Canal Culverts by force of gravity is required to protect the fish and wildlife of the Preserve was presented during the final hearing of this case by the District. The evidence presented by the District to support a finding that the quantity of water flowing through the Camps Canal Culverts by force of gravity is required to protect the fish and wildlife of the Preserve was not rebutted by competent subs by the Petitioners. The only witness called by the Petitioners was an expert in hydrology. The Petitioners' expert only suggested that he had questions about the District's hydrologic study. He was unable, however, to testify that the hydrologic study relied on by the District was unreasonable or inaccurate. The Petitioners also offered no evidence to counter the testimony of the District's expert on the environment of Paynes Prairie. The testimony of the District's expert proved that, even without the results of the hydrologic study conducted by the District, the evidence concerning the Preserve's environment supports a finding that the water reserved by the Reservation Rule is required for the protection of fish and wildlife. Generally, the evidence proved that, if the water being reserved is not continued to allow to flow naturally into the Preserve, the range of water fluctuations and the resulting natural impact of the environment of the Preserve will not be achieved. There exist in the Preserve currently, a range of plant communities and fish and wildlife. The nature of those communities, fish and wildlife depends on the amount of water in the communities. The communities range from those existing in of upland areas, which have the lowest levels of water, down to deep marshes, where water levels are the greatest. In between are emergent marsh (also called "shallow marsh"), cypress swamps, mixed scrub-shrub wetland, wet prairie, old filed, hudric forest, mesic forest and xeric community. The various types of communities are is a state of fluctuation depending on the levels of water flowing into the Preserve. The evidence presented by the District, and was uncontroverted by the Petitioners, proved that these fluctuations are environmentally desirable; that natural fluctuations of water levels in the Preserve are required for the protection of fish and wildlife. It is for this reason, therefore, that the District decided to reserve the amount of water flowing by gravity through the Camps Canal Culverts, and not some specified volume. The Rationale for the District's Finding that Water is Required for the Protection of Fish and Wildlife. Although the District and some of the Intervenors have prosed several findings of fact that support the ultimate finding of fact that the water reserved by the Reservation Rule is required to protect fish and wildlife. Those findings of fact are subordinate to the ultimate relevant fact in this case. Therefore, rather than rewrite all of those subordinate facts, the District's subordinate findings of fact (which cover those subordinate findings suggested by the Intervenors) will be quoted and adopted in this Final Order. The findings of fact of the District quoted and adopted herein which relate to the hydrologic portion of the are as follows. The findings have been modified to reflect terms used throughout this Final Order. The findings of the District adopted are District findings of fact 44 through 74: Surface water hydrologic models are a tool used by water resource professionals to enable them to simulate or calculate certain characteristics of a hydrologic system from data that relates to or is collected from within that system. T. 65, 66, 90, 91, 779. In this basin, the staff of the District developed a surface water model in order to calculate anticipated water levels and discharge volumes at various points throughout the basin expected to be associated with several alternative water management strategies. T. 90, 91, SJ Ex 1 p 27. The specific model used by the District is the Streamflow Synthesis and Reservoir Regulation (SSARR) mathematical model, developed by the U.S. Army Corps of Engineers. This particular model is generally accepted and used in the field of hydrology for the purposes for which it was used here by the District staff. T. 90, 91, SJ Ex 1 p 27. The model combines two types of data, the first of which are "fixed basin parameters" such as drainage area, soil moisture run-off relationships, and storage capacity of the water bodies in the basin. Fixed basin parameters do not change over time. T. 98, 99, SJ Ex 1 pp 32-37. The second type of data used by the model is "time series" data such as rainfall, evaporation, lake elevations and discharges at several points throughout the basin. Time series data does change over time. T. 98, 99, SJ Ex 1 pp 38-40. Rainfall data for the basin is the most important input element for the model because rainfall drives the system from a hydrologic perspective. T. 95. Rainfall data from 5 recording stations scattered over the basin were utilized, with one station located at the University of Florida in Gainesville yielding data for more than 50 years, although only data for the 50 year period from 1942-1991 was used in the model. T. 96, 97, SJ Ex 1 pp 38, 39, 62, 175. The other 4 rainfall recording stations used in the model have recorded rainfall for periods ranging from 11 years to 37 years. SJ Ex 1 p 39. In a basin the size of the Orange Creek Basin, day to day rainfall amounts may vary from one recording station to another, however, on an annualized basis, rainfall amounts are relatively consistent between the rainfall recording stations utilized in the District's model. T. 97, 98, 184, 727. Both the number and location of rainfall recording stations used for the model are adequate to characterize rainfall for the basin. T. 97, 98, 184. Fifty years of hydrologic data were utilized by the District in the model, because corresponding records existed for rainfall, lake levels, and discharge for this period of time. In addition, a 50 year period is more likely to exhibit a full range of hydrologic conditions, such as droughts and floods, than a shorter increment of time would. T. 104. The model utilizes both the fixed basin parameters and the time series data to calculate an associated lake level for any of the lakes in the basin or a discharge measurement at one of several points in the basin for any particular day during the 50 year period represented by the hydrologic data on which the model is based. T. 98-100. The model was initially run to calculate several hydrologic values with existing conditions in place. Existing conditions, for purposes of comparison with other alternatives, assumes the Newnans Lake weir to be in place, the gates to the Camps Canal Culverts to be in an open position and the gates to the main structure Culverts in the Preserve to be in an open position. T. 99, SJ Ex 1 p 83. For all scenarios examined, the model assumes existing land uses to be in place, in all years simulated, in order to allow consistent comparisons of hydrologic conditions over the 50 years for which data was available. T. 134, 135. In the "existing conditions" scenario the model calculates the volume of water discharging from Newnans Lake southward into Prairie Creek for each day during the 50 year period from 1942-1991. T. 100. Discharge measurements were made by District staff at the downstream end of the Camps Canal Culverts from which a rating curve was developed for the structure. T. 101, 102, SJ Ex 1 pp 33, 36. A rating curve is a means by which the flow capacity of a water control structure such as a culvert may be calculated. T. 101, 102. Using the rating curve developed by District staff for the Camps Canal Culverts, the model, having calculated the volume of water moving from Newnans Lake into Prairie Creek, can then calculate the volume of water passing through the Culverts at the Camps Canal Culverts into the Preserve versus the volume moving on southward through Camps Canal to Orange Lake for each day or year during the 50 year period from 1942-1991. T. 101, 102, SJ Ex 1 p 84, Appendix Table E-45. Having calculated the annual volume of surface water entering the Preserve and the annual volume moving into and through Camps Canal to Orange Lake for each of the 50 years between 1942- 1991, District staff then divided the 50 year totals for each by 50 to arrive at a yearly average volume of water going to the Preserve versus a yearly average volume going through Camps Canal to Orange Lake, under existing conditions. T. 101-104, SJ Ex 1 p 84, Appendix Table E-45. Based on the volumes calculated for the 50 year period between 1942-1991, on average, 45 percent of Prairie Creek flow enters Preserve through the Camps Canal Culverts under existing conditions. This equates to 35 cubic feet per second (cfs), or 23 million gallons per day (mgd). T. 103, 605, 606, SJ Ex 1 p 84, Appendix Table E-45. Also based on the volumes calculated for the 50 year period between 1942-1991, on average, 55 percent of Prairie Creek flow goes into Camps Canal and moves on southward to the River Styx and then to Orange Lake under existing conditions. T. 103, SJ Ex 1 Appendix Table E-45. Making a calculation of flow based on 50 years of historic hydrologic data does not guarantee that the next 50 years will be identical to the period during which the calculation was developed, however, it is reasonable to assume that the next 50 years will be statistically similar to the previous 50 years and that hydrologic conditions, on average, will be the same. T. 104, 143. Both the general methodology and the specific model used by the District to quantify the average volume of flow entering the Preserve under existing conditions, which also represents the volume of flow which the rule would reserve for fish and wildlife which use the Preserve, are based on logic and accepted scientific principles. T. 90, 91, 97, 102, 128, 729. The rule in issue does not reserve a specific amount of water for the protection of fish and wildlife using the Preserve, rather, it reserves the amount which will flow by gravity through the existing Camps Canal Culverts with the gates in an open position, which will in essence, maintain the existing volume of flow into the Preserve. T. 604, 605, 624. Thirty-five cfs does not necessarily represent the specific volume of water that will flow into Preserve on a given day, rather, the specific volume would be dependent on hydrologic conditions on that given day. T. 105, 106. Nevertheless, 45 percent of flow, or 35 cfs, or 23 mgd, represents a reasonably accurate calculation, based on the data available, of the average volume of Prairie Creek flow which will enter the Preserve by gravity pursuant to the Reservation Rule. T. 101- 104, 638, SJ Ex 1. With the existing conditions hydrologic regime which the Reservation Rule would continue in place, the model calculates that the mean elevation of Orange Lake would be 57.26 feet NGVD. T. 121, 122, SJ Ex 8 (arithmetic mean). If no Prairie Creek flow were allowed to enter the Preserve and all of its flow went to Orange Lake, the model calculates the mean elevation of Orange Lake to be 57.51 feet NGVD. T. 121, 122, SJ Ex 8 (arithmetic mean). Thus, the mean elevation of Orange Lake rises by only 0.25 feet when all of the Prairie Creek flow is diverted to Orange Lake. SJ Ex 8. The impact of a 0.25 feet change in the mean elevation of Orange Lake from a hydrologic perspective is small given the 11 feet fluctuation in elevations that has occurred naturally over time in the lake. T. 125. By contrast, if no Prairie Creek flow were allowed to enter the Preserve and all of its flow went to Orange Lake, the mean elevation of water levels within the Preserve, as calculated by the model, would decline by 0.65 feet. SJ Ex 7. Eliminating all Prairie Creek flow from the Preserve would decrease the amount of wetted acreage in the central portion of the prairie by up to 2400 acres. T. 203, SJ Ex 1 p 131, SJ Ex 6. In addition, the acreage wetted in the eastern lobe of the Preserve by the sheetflow of Prairie Creek water as it moves from the Camps Canal Culverts to Alachua Lake would also be eliminated. T. 116, SJ Ex 1 p 131. The findings of fact of the District quoted and adopted herein which relate to the environment of, and the alternative course of action considered for, the Preserve are as follows. The findings have been modified to reflect terms used throughout this Final Order. The findings of the District adopted are District findings of fact 79 through 127: The eastern and western lobes of the Preserve are approximately the same elevation and have similar gradients; however, the plant communities within the eastern lobe differ from the plant communities in the western lobe. The plant community within the eastern lobe is predominantly a shallow marsh community while the plant community within the western lobe varies from wet prairie to old field. T. 262, 263; SJ Exs 3, 10B, 10H. For the western lobe of the Preserve, consisting of the area west of U.S. Highway 441, rainfall is the only source of water except when extremely high water levels occur in Alachua Lake. T. 263, 272. When extremely high water levels occur on Alachua Lake water can backflow through the culverts under U.S. Highway 441 and Interstate Highway 75 and inundate the western lobe. T. 272. The eastern lobe of the Preserve is dependent upon sheetflow from Prairie Creek for its source of water. T. 263. Prior to the construction of Cones Levee the sheetflow from Prairie Creek inundated approximately 1,200 acres of the eastern lobe. Today, however, sheetflow inundates directly 600 acres and indirectly another 600 acres in the eastern lobe. T. 264, 265; SJ Ex 10B. Without the Prairie Creek sheetflow, the biological character of the eastern lobe would change to resemble the more terrestrial nature of the western lobe. T. 263, 272, 518. The fish and wildlife inhabiting the Preserve are totally dependent upon its surface water hydrology. T. 276. Of the 21 species of plants living within the Preserve that are listed by the federal government or the State of Florida as endangered, threatened or species of special concern, four species are wetland species. T. 268, 358, 359, 360. Twenty species of animals living on the Preserve are listed by the federal government or the State of Florida as endangered, threatened or species of special concern. Seventeen of these species are wetland dependent. T. 269. Birds, including a number of species listed as endangered or threatened such as great blue herons, woodstorks, anhingas, limpkins, sandhill cranes and ospreys, use the shrub communities around Alachua Lake, the cypress swamp in the eastern lobe and other areas of the eastern lobe for breeding, nesting, and foraging. T. 269, 270, 271, 277, 364, 365. Several species of migratory ducks overwinter in the central area of the Preserve, particularly in the shrub wetland communities around Alachua Lake. Without the flow of water from Prairie Creek the open water in Alachua Lake would be lost and consequently, the overwintering habitat for the ducks would be lost. T. 240, 270, 518. Immature bald eagles use the eastern lobe wetlands for foraging. T. 270. Additionally, the northern harrier, American kestrel and peragrine falcon use wetlands within the Preserve as foraging habitat. T. 364, 365. Mammals, such as river otters, brown water rat, bobcats, bats and long-tailed weasels, use the wetlands within the Preserve, and the eastern lobe particularly, as breeding, nesting, and/or foraging habitat. Reptiles, such as the American alligator, live in the Preserve. T. 270-271, 375, 377-378; SJ Ex 14. The diversity and abundance of animals living in or using the Preserve is greater in the eastern lobe and central area than the western lobe. T. 273, 274. Different species of birds frequent the western lobe. Typically, species more indicative of a drier terrestrial environment are found in the western lobe. T. 272. If the Prairie Creek flow is diverted from the Preserve, the eastern lobe would be driven towards a drier, terrestrial habitat and the functions of the eastern lobe wetlands would be totally lost. T. 277. The sheetflow across the eastern lobe is a unique feature of the Preserve, and without this sheetflow animals such as the endangered brown water rat would not live there. T. 277. Without the Prairie Creek sheetflow, animals dependent on Alachua Lake and the wetlands, such as the brown water rat and the woodstork, would have to find other areas to live, forage, breed and nest due to the loss of wetlands and open water habitat. T. 277, 518. When the water levels in the Preserve are low and wetlands are lost, the birds that depend on the wetlands for nesting will not nest in the Preserve nor elsewhere. T. 532. The wetland communities within the Preserve require a range of water level fluctuations which includes periods of high water levels, average water levels and low water levels. Wetlands must remain wet long enough to exclude upland plants and to conserve hydric soils, yet sufficiently dry often enough to allow germination of wetland plants and the compaction and oxidation of flocculent sediments. T. 293, 294, 298, 299, 310, 311; SJ Ex 1 pp. 23-25. Periods of high water levels maintain lower swamp and shallow marsh habitats, facilitate the dispersal of the seeds of wetland plants, allow wetland species that normally occur at lower elevations to move up into the forested communities, prevent the encroachment of upland species into the upper wetland area, and advance the transportation of organic matter from uplands to wetlands. Inundation of the floodplain and forested communities provide nesting, spawning, refugia, and foraging habitat for fish and other aquatic organisms. T. 294, 296, 310, 311; SJ Ex 1 pp 23- 25. The frequency, timing and duration of high water levels influence the composition and survival of wetland forests. T. 310, 311; SJ Ex 1 p 23. Periods of average water levels create and maintain organic soils and maintain wetland habitat for wetland dependent wildlife. T. 293, 297; SJ Ex 1 p 25. Periods of low water levels rejuvenate floodplain wetlands by allowing seed germination and growth of wetland plants. Seeds of many wetland plant species require saturated soils without standing water in order to germinate. T. 291, 293, 298, 299; SJ Ex 1 pp 24, 25. Periods of low water levels increase the rate of aerobic microbial breakdown and decomposition of organic sediments, and allows the consolidation and compaction of flocculent organic sediments. The consolidation, compaction and decomposition of flocculent organic sediments improves substrates for fish nesting and seed germination. T. 298, 299; SJ Ex 1 pp 24-25. Upland animals use the wetlands during periods of low water levels for foraging and breeding. T. 298, 299. Three elevation transects were used by District staff to identify the elevations of plant communities on the Preserve and develop environmental criteria for the Preserve floodplain. T. 302, 305-306; SJ Ex 1 pp 26, 27, 31, 60. Ecological criteria were developed by District staff to accommodate the hydroperiod requirements of lake and wetland biota. The ecological criteria consisted of hydrologic duration, i.e. how long an area is flooded; and recurrence intervals, i.e. how often an area is flooded. T. 304, 309; SJ Ex 1 pp 23, 61. Maintaining appropriate hydrologic durations and recurrence intervals for plant communities enables the plant communities to support populations of fish and wildlife. T. 307, 312. The District identified the following five significant water management levels: infrequent high water level, frequent high water level, minimum average water level, frequent low water level, and infrequent low water level. The water management levels characterize zones along the elevation gradient of the Preserve. T. 307, 308; SJ Ex 1 p 61. The five different recurrence intervals and the associated hydrologic durations became the hydrologic criteria used by District staff for the water management levels. T. 312. The District evaluated six water management alternatives for the Preserve: the "existing conditions" alternative which simulated the current morphometry of the Paynes Prairie sub-basin; the "total restoration" alternative, under which all the Prairie Creek flow is restored to Paynes Prairie; the "50/50 management" alternative, under which the inflow capacity at the Camps Canal Culvert is reduced by 50 percent and the outflow capacity at the main structure at Alachua Lake is reduced by 50 percent; the "elevation threshold" alternative, under which when the water level at Newnans lake is at 66 feet NGVD or above and the water level at Orange Lake is at 56 feet NGVD or below, then the inflow structure at Camps Canal Culvert is reduced by 50 percent while the outflow capacity at the main structure is maintained at 100 percent; the "Sweetwater Branch" alternative, under which flow from Prairie Creek is replaced by Sweetwater Branch flow; and the "no restoration" alternative, under which the entire flow from Prairie Creek is diverted to Orange Lake. T. 313, 314; SJ Ex 1 p 119. Based upon the hydrologic durations and recurrence intervals defined by the ecologic criteria, the District determined five water management levels for each water management alternative. SJ Ex 1 p 61. The five water management levels and the associated recurrence intervals and hydrologic durations form a fluctuation management regime. The fluctuation management regime for each water management alternative was evaluated with respect to the existing biological features of the aquatic and wetland communities of the Paynes Prairie sub-basin. SJ Ex 1 pp 61, 124, 125. Under the total restoration alternative the water levels on the Preserve would rise thereby improving the hydrologic regime on the prairie, but the possibility of flooding and damaging U.S. Highway 441 would also increase. The minimum average water level of Orange Lake would decrease by 0.67 feet. T. 331, 333; SJ Ex 1 pp 125-130; SJ Ex 8. The no restoration alternative would not satisfy all the hydrologic criteria. The minimum average water level on the Preserve would decrease by 1.01 feet under this alternative. Under this alternative the acreage inundated by the minimum average water level is reduced by approximately 2,400 acres. Additional wetland acres are lost due to the absence of the Prairie Creek sheetflow across the eastern lobe. The minimum average water level in Orange Lake would increase by 0.16 of a foot. T. 324, 334-336; SJ Ex 1 pp 124, 125, 131; SJ Ex 8. Eliminating the flow of Prairie Creek into Paynes Prairie would be detrimental to the current and future biological conditions on the Preserve. SJ Ex 1 p 131. Under the 50/50 management alternative the average flow from Prairie Creek would be reduced from 45 percent to 22.5 percent and the outflow to Alachua Sink would be reduced by 26 percent. T. 337; SJ Ex 1 p 131. The high water levels and the low water levels increase slightly within the Preserve and Orange Lake under the 50/50 management alternative; however, the residence time of water and the concentration of nutrients, including phosphorous and nitrogen, would increase thereby degrading water quality within the Preserve. T. 338, 340, 341; SJ Ex 1 pp 124, 125, 127, 128, 131, 132; SJ Exs 7 and 8. The reduction of sheetflow from Prairie Creek under the 50/50 management alternative would adversely affect the wetlands in the eastern lobe. SJ Ex 1 p 132. Under the elevation threshold management alternative water levels within the Preserve would decrease. The Preserve would receive less water during some periods of naturally high flows reducing the duration and frequency of inundation in the eastern lobe wetlands and, therefore, negatively impacting wildlife dependent upon seasonal high flows. T. 344; SJ Ex 1 p 133; SJ Ex 7. The flow provided by Sweetwater Branch provides approximately 15 percent of the Preserve's average inflow, whereas Prairie Creek provides approximately 50 percent of the Preserve's average inflow. T. 346. Sweetwater Branch is more or less confined to a channel and discharges into Alachua Sink bypassing the Preserve and its eastern lobe. T. 347. Under the Sweetwater Branch alternative the eastern lobe would be deprived of the sheetflow essential to the maintenance of wetlands and the wildlife in the eastern lobe. The eastern lobe would dry out and the plant communities would change to old field or wet prairie. The functions of the plant communities to wildlife would also change under this alternative. T. 347. The Sweetwater Branch alternative would not support fish and wildlife in the eastern lobe of the Preserve. T. 347. The water quality of Sweetwater Branch is poor. Sweetwater Branch has higher concentrations of nitrogen and phosphorous than Prairie Creek. If the nutrient-rich Sweetwater Branch water was diverted onto the Preserve the types and abundances of vegetative communities would change from native vegetation to monocultures of nuisance vegetation that thrive in nutrient-rich environments. T. 346-349; SJ Ex 1 pp 133-134. The existing conditions alternative provides over the long term an average of approximately 45 percent of the Prairie Creek flow by gravity flow through the Camps Canal Culvert to the Preserve. T. 355, 356; SJ Ex 1 p 121. Under the existing conditions alternative, the five hydrologic criteria for both the Preserve and Orange Lake are met and the water level elevations meet the desired recurrence intervals and hydrologic durations. T. 324, 350, 351. The fluctuation management regime provided by the existing conditions alternative partially restores sheetflow from Prairie Creek to the Preserve in sufficient, but fluctuating, water quantities necessary to maintain habitat for fish and wildlife within the eastern lobe. T. 350, 351. It is essential for the protection of the fish and wildlife that utilize and depend upon the Preserve to maintain the flow of Prairie Creek into the Preserve. T. 351, 517. The Preserve needs flow from Prairie Creek in volumes reserved by the proposed rule to protect its fish and wildlife. T. 351. The management levels established by the environmental criteria used for each of the water bodies in the basin will continue to be met in Orange Lake with an average of 45 percent of Prairie Creek flow going to the Preserve and 55 percent going to Orange Lake. T. 432, SJ Ex 1 pp 127, 134, 146. Based upon the substantial and uncontroverted evidence in this case, it is concluded that the water reserved by the Reservation Rule is required for the protection of fish and wildlife of the Preserve.

Florida Laws (12) 1.01120.54120.56120.57373.026373.044373.103373.171373.216373.219373.223403.501 Florida Administrative Code (2) 40C-2.05140C-2.302
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CARLOS M. BERUFF vs SOUTHWEST FLORIDA REGIONAL PLANNING COUNCIL, 99-004159 (1999)
Division of Administrative Hearings, Florida Filed:Bradenton, Florida Oct. 04, 1999 Number: 99-004159 Latest Update: Mar. 15, 2002

The Issue The issue is whether Petitioner is entitled to an environmental resource permit for a surface water management system and the alteration of a wetland in connection with the construction of two warehouses, paved parking and loading areas, a detention pond, and enhancement of the remainder of the existing wetland. If not otherwise entitled to the permit, an additional issue is whether Petitioner is entitled to the permit through an exemption, waiver, or variance from the standard requirements for mitigation.

Findings Of Fact Background Petitioner Carlos M. Beruff, as Trustee under Florida Land Trust No. 22 dated March 30, 1989 (Petitioner), purchased 85 acres of land in Manatee County for $1.2 million in May 1989. (All acreages are approximate.) The east boundary of the 85-acre parcel consists of about 1700 feet of frontage along U.S. Route 301. One month after the purchase, Petitioner sold 70 of the 85 acres for $1.6 million. In the intervening month, Petitioner incurred no significant expenses for development or marketing, although the development and marketing expertise of Carlos Beruff facilitated the $1.6 million sale. The 70 acres that were sold included the frontage on U.S. Route 301. The 15 acres remaining after the sale comprise two tracts of 9 and 5.88 acres. In these cases, Petitioner seeks an environmental resource permit (ERP) for activities involving the 5.88-acre parcel (Site). The 9-acre parcel occupies the northwest corner of the 85-acre parcel. The Site, which was platted in 1911, is the only noncontiguous land constituting the 85-acre parcel; it is 450 feet south of the remainder of the 85-acre parcel. The sole parcel between the Site and the remainder of the 85- acre parcel was originally owned by Lowe's and is now owned by Cheetah Technologies (Cheetah Parcel). The 5.88-acre Site is subject to a road right-of-way of 0.32 acres in favor of the Cheetah Parcel. Of the remaining 5.56 acres, 4.66 acres are wetland and 0.9 acres are upland. The 0.9 acres of upland are subject to an access easement of 0.42 acres, also in favor of the Cheetah Parcel, so the net available upland acreage is only 0.48 acres. The Cheetah Parcel occupies the northwest corner of U.S. Route 301 and Saunders Road (also known as 63rd Avenue East). The Site is immediately west and south of the Cheetah Parcel and occupies the northeast corner of Saunders Road and 24th Street East (also known as Arlin Road). The Site is about 530 feet west of the intersection of U.S. Route 301 and Saunders Road. U.S. Route 301 is a major arterial, and Saunders Road is at least a major collector road. The Site contains about 600 feet of frontage along Saunders Road and 465 feet of frontage along 24th Street East. The Site is in unincorporated Manatee County roughly midway between downtown Bradenton and downtown Sarasota. Saunders Road crosses a north-south railroad line approximately one-half mile west of the Site and Bowlees Creek about 650 feet west of the railroad track. The 9-acre parcel still owned by Petitioner is about 350 feet north-south by 1250 feet east-west. The western boundary of the 9-acre parcel runs along the east side of the railroad line. Like the other parcels involved in this case, the 9-acre parcel drains into Bowlees Creek. The Site is in an area characterized by industrial land uses, including warehouses, a junkyard, an industrial center, and a bakery. A halfway house for persons recently released from prison is located one-quarter mile to the west of the Site. The Site is zoned HM (heavy manufacturing), which is a limited, and thus valuable, zoning category in Manatee County. Respondent has issued three relatively recent surface water management permits that are relevant to these cases: a 1986 permit for the development of the Cheetah Parcel (Cheetah Permit), a 1988 permit for the widening of Saunders Road from two to four lanes (Saunders Road Permit), and a 1989 permit for the construction of a commercial park north of the Site known as 301 Park of Commerce (301 Permit). Bowlees Creek runs from north to south, emptying into Sarasota Bay across from Longboat Key. Sarasota Bay is an Outstanding Florida Water. Bowlees Creek drains a nine square-mile basin, which is about 21-25 percent developed. The Bowlees Creek basin is an open drainage basin. Due to flooding problems, Manatee County has imposed special limitations upon development within the Bowlees Creek basin. Among these limitations is that the rate of post- development runoff must be less than the rate of pre- development runoff--up to 50 percent less, according to expert witnesses for both sides (Lawrence Weber, Tr. Vol. III, pp. 118-19; and Daryl Flatt, Tr. Vol. IV, p. 230). By stipulation, the Site is at the extreme eastern end of the Bowlees Creek basin. In fact, the Site may have historically drained into Bowlees Creek and will drain into Bowlees Creek after, as described below, the northwest window is added to the surface water management system. In 1993 or 1994, Petitioner began the process of developing the Site following the sale five years earlier of the larger 70-acre parcel. Mr. Beruff has been in the development business for 20 years. His career began in 1980 when Mr. Beruff became an employee for U.S. Homes and Modern Builders; he became self-employed in 1984. Mr. Beruff has developed seven commercial and ten residential developments. Application Process Deciding to pursue warehouse development for the Site, Petitioner initiated the development process by hiring an engineer and environmental consultant. With the assistance of these consultants, Petitioner prepared its application for an ERP. By application dated October 9, 1998, and filed November 13, 1998, Petitioner requested that Respondent issue an individual ERP for the construction on the Site of a surface water management system in connection with the construction of two warehouse buildings, paved parking and loading areas, and a detention pond, as well as the enhancement of the remainder of the existing wetland (Application). The Application states that the total building, parking, and loading areas would be 58,026 square feet and that wetlands constitute 3.37 acres of the 5.88-acre Site. The site plan attached to the Application shows a "wetland preservation & enhancement" area of 1.592 acres at the north end of the Site. To the south, toward Saunders Road, are two buildings with paved parking and loading areas. On the southwest corner is a "stormwater treatment & attenuation" area. After several discussions with Respondent's staff, Petitioner modified the proposed development. In its latest revision, the footprint of the proposed development would occupy 2.834 acres of wetland, leaving 1.826 acres of wetland. On November 13, 1998, Petitioner filed a Petition for Exemption, Waiver or Variance as to Mitigation Requirements, seeking an exemption, waiver, or variance from all laws requiring offsite mitigation or additional onsite mitigation for the portion of the wetland that would be destroyed by the proposed development. Drainage At present, the Site receives runoff from a total of 27 acres. The offsite contributors of runoff are the Cheetah Parcel and a segment of Saunders Road east of 21st Street East. These locations have drained into the Site for hundreds of years. In general, drainage raises two distinct issues: water quality and water quantity. For an open drainage basin, the issue of water quantity expresses itself primarily in runoff discharge rate, although historic basin storage is also an issue. As discussed in the Conclusions of Law, the Respondent's Basis of Review identifies different storm events to which applicants must design different components of surface water management systems. For water quantity, the system may release no more than the permitted discharge rate in the design storm, which is the 25-year, 24-hour storm event. At present, the design storm would produce about eight inches of rain, although the same design storm, due to a different model or modeling assumptions, produced 9.5 inches of rain at the time of the issuance of the permit for the Cheetah Parcel. (The practical effect of this change in the calculation of the design storm is that the quantitative capacity of the surface water management system of the Cheetah Parcel is nearly 20 percent greater than would be required today.) For water quality, the system must capture the first inch of runoff (sometimes only the first half-inch of runoff, depending on the type of system and receiving waterbody). In contrast to the relatively infrequent 25-year storm, approximately 90 percent of the storms in Respondent's jurisdiction produce no more than one inch of runoff. The underlying premise is that the first inch of runoff contains nearly all of the contaminants that will be flushed from impervious surfaces. The Cheetah surface water management system features a wetland and a retention pond along the north property line of the Site. The Cheetah pond and wetland attenuate runoff before allowing it to drain south onto the Site. The Cheetah surface water management system also includes a swale running north along 24th Street East to take runoff eventually to Bowlees Creek. The Saunders Road surface water management system discharging onto the Site consists largely of an underground, offline storage and attenuation system that stores excess runoff, as compared to pre-development rates, in lateral pipes off a weir. Nothing in the record suggests that the surface water management systems authorized by the Cheetah Permit or the Saunders Road Permit fail to provide reasonable assurance that the discharged runoff is of satisfactory water quality. Following their respective permits in 1986 and 1988, respectively, the rates of discharge of runoff from the Cheetah Parcel and Saunders Road were no greater post- development than they had been pre-development. The Cheetah Parcel post-development and pre-development discharge rates were both 10.6 cubic feet per second (cfs). The Saunders Road post-development and pre-development discharge rates were both 32.4 cfs. In issuing the 301 Permit, Respondent authorized the construction of a drainage system that would take runoff north along 24th Street East and then west, eventually emptying into Bowlees Creek. Conforming to the previous drainage system, the new system replaced an open ditch with underground stormwater pipes. Of particular relevance to the Site, two prominent features of the system authorized by the 301 Permit were windows in the vicinity of the southwest and northwest corners of the Site (Southwest Window and Northwest Window). A window is an opening in the wall of a hardened structure whose purpose includes drainage. The opening is constructed at a certain elevation and a certain size to allow specified volumes or rates of water to pass into the structure and then offsite. The 301 Permit authorized the construction of a swale along the southwest corner of the Site to direct runoff discharging from the Saunders Road system into the Southwest Window. This swale has been construed. However, several problems have precluded the construction of the Southwest Window, probably permanently. The most serious problem, from an engineering perspective, is the failure to lay the stormwater pipe along 24th Street East at the proper depth. The stormwater pipe was erroneously installed at an elevation of 15.32 feet National Geodetic Vertical Datum (NGVD), and the Southwest Window was to have been cut at a control elevation of 14.75 feet NGVD. The discharge elevation of the Saunders Road outlet precludes raising the control elevation of the Southwest Window sufficiently to allow gravity drainage into the stormwater pipe. Exacerbating the discrepancy among the as-built elevations of the three structures is what appears to be a design problem belatedly recognized by Respondent. Respondent is justifiably concerned that the Southwest Window, at a control elevation of 14.75 feet NGVD, would draw down the water elevation of the Site's wetland, which is at a wet season elevation of 16.5 feet NGVD (now actually 17 feet NGVD, possibly due to the absence of the Southwest Window). A third problem with the Southwest Window is that the southwest corner of the Site was not historically a point of discharge, so the Southwest Window would deprive the Site's wetland of runoff. Fortunately, neither the Southwest nor the Northwest Window is essential for the proper operation of the surface water management system of 301 Park of Commerce, which largely depends on a series of lakes for treatment and attenuation. The Northwest Window was to be at elevation 16.5 feet NGVD, and its construction would provide needed drainage for the Site. In general, the Northwest Window does not raise the same concerns as does the Southwest Window. The Northwest Window is in the vicinity of the historic point of discharge for the Site and replaces a ditch permitted for the Cheetah Parcel to take runoff north along 24th Street East. The Northwest Window would also alleviate a standing-water problem at the northwest corner of the Site. However, Manatee County, which controls the right- of-way on which the Northwest Window is located and is responsible for its construction and maintenance, has discovered that it lacks a sufficient property interest to access the Northwest Window. The County has since initiated the process by which it can obtain the necessary interest, and, once completed, the County will cut the Northwest Window into the existing structure. Due to the role of the Northwest Window in draining the runoff in the area, including the Site, the Application reincorporates the Northwest Window, as it should have been constructed pursuant to the 301 Permit. Although the Cheetah and Saunders Road permits resulted in greater runoff volume entering the Site, more importantly to area drainage, these permits did not result in greater runoff rates and or in a deterioration in runoff water quality. Likewise, the failure to construct the Southwest Window and Northwest Window is not especially relevant to area drainage, nor is the likely inability ever to construct the Southwest Window. Far more important to area drainage is the fact that Petitioner proposes that the Site, post-development, would produce a runoff rate of 10.6 cfs, as compared to a pre-development runoff rate of 7 cfs. A serious adverse impact to area drainage, the proposed activity increases the runoff rate by 50 percent in a floodprone, 80-percent builtout basin--a basin of such sensitivity that Manatee County is imposing a post-development requirement of substantially reduced runoff rates. The cumulative impacts of the proposed development, together with existing developments, would be to cause substantial flooding of the Bowlees Creek basin. Petitioner's expert attempted to show that the runoff from the Site, which is at the extreme eastern end of the Bowlees Creek basin, would be delayed sufficiently so as not to exacerbate flooding. Respondent's expert thoroughly discredited this testimony due, among other things, to its reliance upon obsolete data and an unrealistic limitation upon the assumption of the direction of travel of storms. Similarly, Petitioner failed to prove that the authorized discharge rate for the 301 Permit is 42 cfs. This assertion is most succinctly, though not exclusively, rebutted by the fact that the 42-inch pipe can only accommodate 18 cfs. Even if the 42-inch pipe could accommodate a substantially greater runoff rate, Petitioner's expert would have erroneously inferred a permitted discharge rate from this increased capacity without negating the possibility that other structures in the 301 surface water management system effectively reduced the rate or that oversized structures existed to accommodate higher runoff rates in storms greater than the design storm. In addition to increasing the runoff rate by 50 percent, Petitioner's proposal would also reduce the historic basin storage by over 40 percent. Displaced basin storage moves downstream, increasing flood levels from fixed storm events. At present, the Site provides 8.68 acre-feet of historic basin storage. The Application proposes to replace this storage with storage in the wetland and retention pond totaling only 4.9 acre-feet. The loss of 3.8 acre-feet of basin storage means that this additional volume of water would, post-development, travel down Bowlees Creek. A final drainage deficiency in Petitioner's proposal arises out of a berm's proposed outside of the Northwest Window. A one-foot bust in the survey of Petitioner's expert would have resulted in this berm preventing runoff from entering the Site from the Cheetah Parcel, as runoff presently does. Respondent's expert suggested several possible alternatives that might result in a permittable project with respect to post-development runoff rates (the record is silent as to the effect of these alternatives upon historic basin storage, although it would seem that they would add storage). Reducing the area of destroyed wetlands to one acre would probably reduce the excess of post-development runoff rate to 1-2 cfs. Petitioner could then obtain offsetting attenuation through a variety of means, such as by obtaining an easement to use the wetland on the Cheetah Parcel, constructing an attenuation pond on the 9-acre parcel, or constructing underground vaults in the filled area of the wetland on the Site. Wetlands Except for the road right-of-way, the Site is undeveloped and forested. The presence of 25-year-old red maples militates against attributing the transition from an herbaceous to a forested wetland to the failure to install the Northwest and Southwest windows. More likely, this transition to the sub-climax species of red maple and willow (in the absence of a cypress source) is due to the repression of fire on the Site. Experts for the opposing sides differed sharply in their biological assessments of the wetland. Petitioner's expert described a stressed wetland whose impenetrable thicket provided habitat only to a lone rat and swarm of mosquitoes. Respondent's expert described a robust wetland featuring a luxuriant overstory of red maple and Carolina willow; an rich understory of ferns, and diverse wildlife ranging from birds in the air (direct evidence); fish, snails, and tadpoles in a small pond (direct evidence); and squirrel and opossum (indirect evidence) scampering (indirect evidence) among the buttonbush, elderberry, and wax myrtle (direct evidence). Undoubtedly, the wetland has been stressed; approximately 30 percent of the wetland vegetation is Brazilian pepper, which is a nuisance exotic. However, the wetland is well hydrated. Issuance of the Cheetah Permit was predicated, in part, upon the rehydration of the wetland on the Site. With the issuance of the Cheetah Permit and especially the Saunders Road Permit, the quality of water entering the wetland has improved by a considerable amount. As already noted, added volumes of runoff are entering the wetland since the issuance of these two permits, although post-development runoff rates are the same as pre-development runoff rates. On balance, the wetland is functioning well in providing habitat and natural drainage functions. Giving due weight to the current condition of the wetland, the enhancement offered by Petitioner does not approach offsetting the loss of wetland area. In return for destroying 2.83 acres of the wetland, Petitioner proposed the enhancement of the remaining 1.83 acres by removing exotic species to no more than 10 percent of the total vegetation. The mitigation is plainly insufficient because of the level of functioning of the entire wetland at present. Additionally, Petitioner has failed to demonstrate that the Brazilian pepper, which is the major nuisance exotic occupying the Site, is evenly distributed; to the contrary, it is present mostly outside the wetland, along a berm just outside of the wetland. The lack of seedlings and old specimens suggests that the Brazilian pepper population may not be stable and may itself be stressed. Petitioner's failure to show that the remaining wetland area has more than 10 percent infestation or is likely to suffer additional infestation further undermines the effectiveness of the proposed mitigation. Respondent has never issued an ERP for a proposed activity involving the alteration of wetlands when the enhancement mitigation ratio is as low as .65:1, as Petitioner proposes. In general, Respondent requires higher mitigation ratios when proposals involve wetlands enhancement, rather than wetlands creation, because the wetlands to be enhanced are already functioning--in these cases, at a relatively high level. Although Petitioner has been unwilling to consider such alternatives, numerous alternatives exist for offsite mitigation or mitigation banking, if insufficient area exists for adequate onsite mitigation. Lastly, Petitioner devoted considerable effort at hearing to portraying Respondent's handling of the Application as flawed and unfair. However, the evidence does not support these assertions. Most strikingly, Respondent's staff treated the drainage windows inconsistently, to the benefit of Petitioner. They treated the Northwest Window as installed for the purpose of calculating the pre-development runoff discharge rate to Bowlees Creek. Until the Northwest Window is installed, the actual rate is even lower. This approach is justifiable because the Northwest Window will be installed at some point. On the other hand, Respondent's staff ignored the higher wetland elevation on the Site, presumably resulting from the absence of the Southwest Window. However, this approach, which benefits Petitioner in calculating wetland drawdown effects, is unjustifiable because the Southwest Window probably will never be installed. Petitioner's specific complaints of unfair treatment are unfounded. For example, Petitioner suggested that Respondent credited Lowe's with wetland acreage for the littoral shelf of its wetland, but did not do so with the wetland on the Site. However, Petitioner produced no evidence of similar slopes between the two shelves, without which comparability of biological function is impossible. Additionally, Petitioner ignored the possibility that, in the intervening 14 years, Respondent may have refined its approach to wetland mitigation. Although occurring at hearing, rather than in the application-review process, Respondent's willingness to enter into the stipulation that the Site presently drains into Bowlees Creek, despite recent data stating otherwise, was eminently fair to Petitioner. Absent this stipulation, Respondent would have been left with the formidable prospect of providing reasonable assurance concerning drainage into the floodprone Bowlees Creek when the post-development rate was 10.6 cfs and the pre-development rate was 0 cfs.

Recommendation Based on the foregoing, it is RECOMMENDED that Respondent deny Petitioner's application for an environmental resource permit and for an exemption, variance, or waiver. DONE AND ENTERED this 29th day of February, 2000, in Tallahassee, Leon County, Florida. ___________________________________ ROBERT E. MEALE 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 29th day of February, 2000. COPIES FURNISHED: S. W. Moore Tracey B. Starrett Brigham. Moore, Gaylord, Schuster, Merlin & Tobin, LLP 100 Wallace Avenue, Suite 310 Sarasota, Florida 34237-6043 Mark F. Lapp Jack R. Pepper Assistant General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609 E. D. "Sonny" Vergara Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899

Florida Laws (17) 120.54120.542120.569120.57267.061373.042373.086373.403373.406373.413373.414373.416373.421380.06403.031403.061403.201 Florida Administrative Code (6) 40D-4.09140D-4.30140D-4.30240D-40.30162-302.30062-4.242
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PHILLIP LOTT vs CITY OF DELTONA AND ST. JOHNS RIVER WATER MANAGEMENT DISTRICT, 04-002406 (2004)
Division of Administrative Hearings, Florida Filed:Deltona, Florida Jul. 12, 2004 Number: 04-002406 Latest Update: Jul. 25, 2005

The Issue The issue is whether the applicant for an Environmental Resource Permit ("ERP"), the City of Deltona ("City" or "Applicant"), has provided reasonable assurance that the system proposed complies with the water quantity, environmental, and water quality criteria of the St. Johns River Water Management District's ("District") ERP regulations set forth in Florida Administrative Code Chapter 40C-4, and the Applicant's Handbook: Management and Storage of Surface Waters (2005).

Findings Of Fact The District is a special taxing district created by Chapter 373, Florida Statutes, charged with the duty to prevent harm to the water resources of the District, and to administer and enforce Chapter 373, Florida Statutes, and the rules promulgated thereunder. The City of Deltona is a municipal government established under the provisions of Chapter 165, Florida Statutes. The Lake Theresa Basin is comprised primarily of a system of interconnected lakes extending from Lake Macy in the City of Lake Helen to the Butler Chain of Lakes (Lake Butler and Lake Doyle). The Lake Theresa Basin is land-locked and does not have a natural outfall to Lake Monroe and the St. Johns River. In 2003, after an extended period of above-normal rainfall in the Deltona area, the lakes within the land-locked Lake Theresa Basin staged to extremely high elevations that resulted in standing water in residential yards, and rendered some septic systems inoperable. Lake levels within the Lake Theresa Basin continued to rise and were in danger of rising above the finished floor elevations of some residences within the basin. On March 25, 2003, the District issued an Emergency Order (F.O.R. No. 2003-38) authorizing the construction and short-term operation of the Lake Doyle and Lake Bethel Emergency Overflow Interconnection. Since wetland and surface water impacts would occur, the Emergency Order required the City of Deltona to obtain an ERP for the system. The project area is 4.1 acres, and the system consists of a variable water structure on the west shore of Lake Doyle connected to a series of pipes, swales, water control structures, and wetland systems which outfall to a finger canal of Lake Bethel, with ultimate discharge to Lake Monroe and the St. Johns River. The first segment of the system extends downstream from the weir structure on the west shore of Lake Doyle via a pipe entrenched in the upland berm of the Sheryl Drive right-of-way. The pipe passes under Doyle Road and through xeric pine-oak uplands to the northeast shore of a large (approximately 15 acres) deepwater marsh. Water flows south through the deepwater marsh where it outfalls through four pipes at Ledford Drive. Two of the four pipes are overflow structures, controlled by canal gates. The pipes at Ledford Drive discharge into a ditch and into a large (greater than 20 acres) shallow bay swamp. The south end of the bay swamp is defined (and somewhat impounded) by a 19th Century railroad grade. Water flows through the bay swamp where it outfalls through five pipes at the railroad grade. Three of the five pipes are overflow structures, controlled by channel boards. The pipes at the railroad grade discharge to a 1500-foot long finger canal that was dug some time during the period 1940-1972 from the north central shore of Lake Bethel. The overflow interconnection system has three locations whereby the system can be shut down: 1) Lake Doyle--a control weir, controlled by three sluice gates; 2) Ledford Drive--two thirty-inch reinforced concrete pipes, controlled by canal gates; and 3) railroad grade--three thirty-inch reinforced concrete pipes, controlled by channel boards (collectively referred to as "Overflow Structures"). The Overflow Structures are designed to carry the discharge of water from Lake Doyle to Lake Bethel. With the Overflow Structures closed the system returns to pre-construction characteristics, meaning there will be no increase or decrease in the quantity or quality of water throughout the path of the system as a result of the project. An unequivocal condition of the permit is that the system would operate with all of the Overflow Structures closed. As an added assurance, the City proposes to place a brick and mortar plug in the Lake Doyle weir structure outfall pipe to prevent any discharge from the weir. The City has submitted to the District preliminary plans for a future phase in which the system would be modified for the purpose of alleviating high water levels within the Lake Theresa Basin when the water level in Lake Doyle rises above an elevation of 24.5 feet. The District shall require a separate permit application to be submitted for such future plans. Petitioner, Barbara Ash, has lived on Lake Theresa for 19 years. Ms. Ash lives upstream from the area of the weir that will be plugged in accordance with the ERP. She does not trust either the City of Deltona to comply with or the District to enforce the conditions of the ERP applied for by the City. Petitioner, Barbara Ash, also served as the qualified representative for Petitioners, Francell Frei, Bernard J. and Virginia Patterson, and Ted and Carol Sullivan. Ms. Ash represented that Ms. Frei has lived on Lake Theresa for 12 years, and both the Pattersons and the Sullivans live on Lake Louise, which is within the area of concern in this proceeding. Petitioner, Diana Bauer, has lived on Lake Theresa since February 2004. She fears that the lake will become too dry if the system is allowed to flow. She also believes the wildlife will be adversely affected if the water levels are too low since many species need a swampy or wet environment to thrive. She fears her property value will decrease as a result of the approval of the ERP. She also does not trust either the City to comply with or the District to enforce the conditions of the ERP. Petitioner, Howard Ehmer, lives two to three hundred yards down Lake Theresa from Ms. Bauer. He is concerned about the lake bed being too dry and attracting people on all terrain vehicles who enjoy driving around the lake bottom. He is concerned about his property value decreasing if the lake bed is dry. Further, when the lake level is too low, people cannot enjoy water skiing, boating, and fishing on Lake Theresa. Petitioner, Phillip Lott, a Florida native, has also owned and lived on property abutting Lake Theresa since 1995. Mr. Lott has a Ph.D. in plant ecology, and M.P.A. in coastal zone studies, an M.B.A. in international business, and a B.S. in environmental resource management and planning. Mr. Lott has been well acquainted with the water levels on Lake Theresa for many years. Based upon his personal observations of the lake systems in the Deltona area over the years, Mr. Lott has seen levels fluctuate greatly based upon periods of heavy and light rainfall. Mr. Lott is concerned that the District will permit the City to open the weir to let water flow through the system and cause flooding in some areas and low water levels in other areas. He fears that the District will allow the water to flow and upset the environmental balance, but he admits that this ERP application is for a closed system that will not allow the water to flow as he fears. Mr. Lott similarly does not trust the City to comply with and the District to enforce the conditions of the ERP. Petitioners, James E. and Alicia M. Peake, who were represented by Steven L. Spratt at hearing as their qualified representative, live on Lake Louise, which is interconnected with the Lake Theresa basin. The Peakes are concerned that if the level of Lake Louise drops below 21 feet, nine inches, they will not be able to use the boat launch ramps on the lake. Petitioner, Steven L. Spratt, also lives on Lake Louise, and is concerned about the water levels becoming so low that he cannot use the boat launch on the lake. He has lived on the lake since 2000, and remembers when the water level was extremely low. He fears that approval of the ERP in this case will result in low levels of water once again. Petitioner, Gloria Benoit, has live on Lake Theresa for two years. She also enjoys watching recreational activities on the lake, and feels that approval of the ERP will devalue her lakefront property. Ms. Benoit appeared at the first day of the hearing, but offered no testimony on her behalf. J. Christy Wilson, Esquire, appeared prior to the final hearing as counsel of record for Petitioners, Steven E. Larimer, Kathleen Larimer, and Helen Rose Farrow. Neither Ms. Wilson nor any of the three Petitioners she represented appeared at any time during the hearing, filed any pleadings seeking to excuse themselves from appearing at the final hearing, or offered any evidence, testimony, pre- or post- hearing submittals. Petitioner, Gary Jensen, did not appear at hearing, did not file any pleadings or papers seeking to be excused from appearing at the final hearing, and did not offer any evidence, testimony, pre- or post-hearing submittals. Both the City and the District recognize that areas downstream from the project site, such as Stone Island and Sanford, have experienced flooding in the past in time of high amounts of rainfall. The system proposed by the City for this ERP will operate with the overflow structures closed and a brick and mortar plug in the outfall pipe to prevent water flow from Lake Doyle to Lake Bethel. So long as the overflow structures are closed, the system will mimic pre-construction flow patterns, with no increase in volume flowing downstream. The District has considered the environment in its proposed approval of the ERP. The area abutting the project is little urbanized and provides good aquatic and emergent marsh habitat. With the exception of the western shore area of the deepwater marsh ("west marsh area"), the bay swamp and remaining deepwater marsh area have good ecological value. In the 1940's, the west marsh area was incorporated into the drainage system of a poultry farm that occupied the site. This area apparently suffered increased nutrient influxes and sedimentation that contributed to a proliferation of floating mats of aquatic plants and organic debris. These tussocks reduced the deepwater marsh's open water and diminished the historical marsh habitat. Water under the tussocks is typically anoxic owing to total shading by tussocks and reduced water circulation. Thick, soft, anaerobic muck has accumulated under the matted vegetation. Exotic shrubs (primrose willow Ludwigia peruvania) and other plants (cattails Typha spp.) dominate the tussocks. The construction of the project, from the 2003 Emergency Order, resulted in adverse impacts to 1.3 acres of wetlands having moderately high- to high ecological value and 0.2 acres of other surface waters. The 0.2 acre impact to other surface waters was to the lake bottom and the shoreline of Lake Doyle where the weir structure was installed. The 0.3 acres of wetland impacts occurred at the upper end of the deepwater marsh where the pipe was installed. The largest wetland impact (1.0 acre) was to the bay swamp. The bay swamp is a shallow body dominated by low hummocks and pools connected inefficiently by shallow braided channels and one acre is filled with a 1-2 foot layer of sediment following swamp channelization. Disturbance plants (e.g., primrose willow, Ludwigia peruvania, and elderberry Sambucus Canadensis) now colonize the sediment plume. Pursuant to the District's elimination and reduction criteria, the applicant must implement practicable design modifications, which would reduce or eliminate adverse impacts to wetlands and other surface waters. A proposed modification, which is not technically capable of being done, is not economically viable, or which adversely affects public safety through endangerment of lives or property is not considered "practicable." The City reduced and/or eliminated the impacts to the lake bottom and shoreline of Lake Doyle and deepwater marsh, to the extent practicable. The impacts were the minimum necessary to install the weir structure and pipe for the system; the weir structure and pipe were carefully installed on the edges of the wetland and surface water systems, resulting in a minimum amount of grading and disturbance. To compensate for the loss of 1.3 acres of wetlands and 0.2 acres of other surface waters, the City proposes to preserve a total of 27.5 acres of wetlands, bay swamp, marsh, and contiguous uplands. Included in this 27.5 acres are 6.4 acres of the west marsh, which are to be restored. The parties stipulated that the mitigation plan would adequately compensate for losses of ecological function (e.g. wildlife habitat and biodiversity, etc.) resulting from the project. Water quality is a concern for the District. Lake Monroe is included on the Florida Department of Environmental Protection's verified list of impaired water bodies for nitrogen, phosphorous, and dissolved oxygen. Water quality data for Lake Monroe indicate the lake has experienced high levels of nitrogen and phosphorous and low levels of dissolved oxygen. Prior to construction of the project, there was no natural outfall from the Lake Theresa Basin to Lake Monroe and therefore no contribution from this basin to nitrogen and phosphorous loadings to Lake Monroe. Lake Colby, Three Island Lakes (a/k/a Lake Sixma), and the Savannah are surface waters within the Lake Theresa Basin for which minimum levels have been adopted pursuant to Florida Administrative Code Chapter 40C-8. The system will operate with the overflow structures closed and a brick and mortar plug in the outfall pipe to prevent water flow from Lake Doyle to Lake Bethel, resulting in no outfall from the Theresa Basin to Lake Monroe. Minimum flows established for surface waters within the Lake Theresa Basin will not be adversely impacted. Under the first part of the secondary impact test, the City must provide reasonable assurance that the secondary impacts from construction, alteration, and intended or reasonable expected use of the project will not adversely affect the functions of adjacent wetlands or surface waters. The system is designed as a low intensity project. As proposed, little activity and maintenance are expected in the project site area. The reasonably expected use of the system will not cause adverse impacts to the functions of the wetlands and other surface waters. None of the wetland areas adjacent to uplands are used by listed species for nesting or denning. In its pre-construction state, the project area did not cause or contribute to state water quality violations. Under the second part of the secondary impact test, the City must provide reasonable assurance that the construction, alteration, and intended or reasonably expected uses of the system will not adversely affect the ecological value of the uplands to aquatic or wetland dependent species for enabling existing nesting or denning by these species. There are no listed threatened or endangered species within the project site area. Under the third part of the secondary impact test, and as part of the public interest test, the District must consider any other relevant activities that are closely linked and causally related to any proposed dredging or filling which will cause impacts to significant historical and archaeological resources. When making this determination, the District is required, by rule, to consult with the Division of Historical Resources. The Division of Historical Resources indicated that no historical or archaeological resources are likely present on the site. No impacts to significant historical and archaeological resources are expected. Under the fourth part of the secondary impact test, the City must demonstrate that certain additional activities and future phases of a project will not result in adverse impacts to the functions of wetlands or water quality violations. The City has submitted to the District preliminary plans for a future phase in which the system would be modified for the purpose of alleviating high water levels within the Lake Theresa Basin when the level in Lake Doyle rises above an elevation of 24.5 feet. Based upon the plans and calculations submitted, the proposed future phase, without additional measures, could result in minor increases in the loadings of nitrogen and phosphorous to Lake Monroe. Lake Monroe is included on the Florida Department of Environmental Protection's verified list of impaired water bodies due to water quality data indicating the lake has experienced high levels of nitrogen and phosphorous, and low levels of dissolved oxygen. Under this potential future phase, there would be an outfall from the Lake Theresa Basin to Lake Monroe. To address the impact on water quality of this potential future phase, the City has submitted a loading reduction plan for nitrogen, phosphorous, and dissolved oxygen. The plan includes compensating treatment to fully offset the potential increased nutrient loadings to Lake Monroe. Specifically, the loading reduction plan includes: Construction and operation of compensating treatment systems to fully offset anticipated increased nutrient loadings to Lake Monroe. Weekly water quality monitoring of the discharge from Lake Doyle for total phosphorous and total nitrogen. A requirement that the overflow structure be closed if the total phosphorous level reaches 0.18 mg/l or higher or the total nitrogen level reaches 1.2 mg/l or higher in any given week and will remain closed until levels fall below those limits. The implementation of these water quality mitigation measures will result in a net improvement of the water quality in Lake Monroe for nitrogen, phosphorous, or dissolved oxygen. The future phase was conceptually evaluated by the District for impacts to wetland functions. The future phase as proposed could result in adverse impacts to wetland functions. Operation of the system with the overflow structures open could impact the bay swamp and deepwater marsh. The City has demonstrated that any adverse impacts could be offset through mitigation. Based upon the information provided by the City and general engineering principles, the system is capable of functioning as proposed. The City of Deltona will be responsible for the operation, maintenance, and repair of the surface waster management system. A local government is an acceptable operation and maintenance entity under District rules. The public interest test has seven criteria. The public interest test requires the District to evaluate only those parts of the project actually located in, on, or over surface waters or wetlands, to determine whether a factor is positive, neutral, or negative, and then to balance these factors against each other. The seven factors are as follows: the public health, safety, or welfare of others; conservation of fish and wildlife and their habitats; fishing, recreational value, and marine productivity; temporary or permanent nature; 5) navigation, water flow, erosion, and shoaling; 6) the current condition and relative value of functions; and 7) historical and archaeological resources. There are no identified environmental hazards or improvements to public health and safety. The District does not consider impacts to property values. To offset any adverse impacts to fish and wildlife and their habitats, the City has proposed mitigation. The areas of the project in, on, or over wetlands do not provide recreational opportunities. Construction and operation of the project located in, on, or over wetlands will be permanent in nature. Construction and operation of the project located in, on, or over wetlands will not cause shoaling, and does not provide navigational opportunities. The mitigation will offset the relative value of functions performed by areas affected by the proposed project. No historical or archaeological resources are likely on the site of the project. The mitigation of the project is located within the same drainage basin as the project and offsets the adverse impacts. The project is not expected to cause unacceptable cumulative impacts.

Recommendation Based upon the Findings of Fact and Conclusions of Law, it is RECOMMENDED that a Final Order be entered granting the City of Deltona's application for an environmental resource permit with the conditions set forth in the Technical Staff Report, and dismissing the Petitions for Formal Administrative Hearing filed by Gary Jensen in Case No. 04-2405, and by Steven E. Larimer, Kathleen Larimer, and Helen Rose Farrow in Case No. 04-3048. DONE AND ENTERED this 27th day of May, 2005, in Tallahassee, Leon County, Florida. S ROBERT S. COHEN 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 27th day of May, 2005. COPIES FURNISHED: George Trovato, Esquire City of Deltona 2345 Providence Boulevard Deltona, Florida 32725 Diana E. Bauer 1324 Tartan Avenue Deltona, Florida 32738 Barbara Ash, Qualified Representative 943 South Dean Circle Deltona, Florida 32738-6801 Phillip Lott 948 North Watt Circle Deltona, Florida Howard Ehmer Nina Ehmer 32738-7919 1081 Anza Court Deltona, Florida 32738 Francell Frei 1080 Peak Circle Deltona, Florida 32738 Bernard T. Patterson Virginia T. Patterson 2518 Sheffield Drive Deltona, Florida 32738 Kealey A. West, Esquire St. Johns River Water Management District 4049 Reid Street Palatka, Florida 32177 J. Christy Wilson, Esquire Wilson, Garber & Small, P.A. 437 North Magnolia Avenue Orlando, Florida 32801 Gloria Benoit 1300 Tartan Avenue Deltona, Florida 32738 Gary Jensen 1298 Tartan Avenue Deltona, Florida 32738 James E. Peake Alicia M. Peake 2442 Weatherford Drive Deltona, Florida 32738 Steven L. Spratt 2492 Weatherford Drive Deltona, Florida 32738 Ted Sullivan 1489 Timbercrest Drive Deltona, Florida 32738 Kirby Green, Executive Director St. Johns River Water Management District 4049 Reid Street Palatka, Florida 32177

Florida Laws (3) 120.569120.57373.086 Florida Administrative Code (6) 40C-4.30140C-4.30240C-4.33140C-4.75162-302.30062-4.242
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JACK SALTIEL AND TERRI SALTIEL vs JAMES N. NASH, JANICE E. NASH, AND DEPARTMENT OF ENVIRONMENTAL REGULATION, 91-007972 (1991)
Division of Administrative Hearings, Florida Filed:Tallahassee, Florida Dec. 11, 1991 Number: 91-007972 Latest Update: Oct. 13, 1992

The Issue Whether the Department of Environmental Regulation should grant a dredge and fill permit to James N. and Janice E. Nash authorizing removal of eleven cubic yards of soil, installation of five 24-inch culverts in lieu of two 18- inch culverts, and placement of 19 cubic yards of limerock in and around the bed of an unnamed creek near the point it reaches the Alford Arm of Lake Lafayette in Leon County, Florida?

Findings Of Fact More than a thousand acres in eastern Leon County comprise the drainage basin giving rise to the unnamed stream that intermittently wends its way across the Alvarez property, crosses the 30-foot wide "tongue" of the Nashes' lot, and traverses the Saltiels' land on its way to the Alford Arm of Lake Lafayette (unless it reaches Alford Arm earlier because rain or other conditions have raised the lake, moving the water's edge upland.) Although neighbors allow them ingress and egress by another route, when flooding makes the roadway impassable, Mr. and Mrs. Nash have no legal right of access other than by the private road which crosses the intermittent stream. In addition to wetlands on either side, part of the streambed, 15 feet wide where it meets the roadway, was originally filled in 1968, when the private drive was built. The strip of land, 30 feet wide and 700 feet long that underlies most of the private road, joins the part of the parcel where the Nashes' house stands to Deep Wood Trail, the public thoroughfare which the private road enters. Leaving a car on the Deep Wood Trail side of the stream, wading across to the other side, and hiking to the house pose difficulties for Mr. Nash, who has muscular dystrophy. Under some conditions, the roadbed acts as a dam. When the lake is low, water flowing downstream may be impeded. When the lake is high, backwater moving in the other direction may be impeded. Of the two culverts installed when the private road was constructed, each with a diameter of 18 inches, only one permits water to flow through now, and even it is partially clogged. When Lake Lafayette rises above 45.3 feet NGVD, Alford Arm spills over the terrain between it and the Nashes' road, and reverses the flow in the streambed where it intersects the roadway. The "invert of the stream at the subject crossing [is] 44.3 feet [NGVD]." T.402. The roadbed is submerged in the vicinity of the stream when Alford Arm rises above 46.7 feet NGVD. The Nashes propose to excavate the streambed (about two and a half feet deep in the natural channel on either side of the existing fill) where it crosses (diagonally) the Nashes' private road, remove the existing culverts together with the soil in which they are embedded, install five culverts, each 24 inches in diameter, in their stead, install cement bag riprap at the ends of the culverts, remove 11 cubic yards of dirt from a 205' by 10' wide section of existing road surface and replace with 19 cubic yards of lime rock surface, Nashes' Exhibits Nos. 5 and 6, realigning the roadway slightly (to avoid the existing encroachment on the Saltiels' property) and increasing the roadbed's elevation over a 205-foot stretch by no more than four inches. Five trees are to be removed, but other trees are to be protected "by tree protection barricades." Nashes' Exhibit No. 7A. Filter fences upstream and down would contain turbidity during construction. The plan is to lay sod and plant grass seed afterwards in order to prevent erosion. Larger culverts would permit the flow of a greater volume of water at lower velocity, more closely approximating the natural regime and reducing scour or erosion downstream. Even when water levels exceeded the elevation of the existing roadbed, more water than the existing culverts can accommodate could move through the proposed replacement culverts, and at a slower velocity. At water levels above the existing grade and below the proposed, slightly higher grade, however, the four inches or less of limerock added to the roadbed would act as a (presumably somewhat porous) barrier to flows that could now move over the roadway unimpeded. The proposed improvements would have no discernible effect on water levels whenever Alford Arm overtopped the roadbed. Ted L. Biddy, the professional engineer called as a witness by the Nashes, testified that a 25-year return two-hour storm would raise water immediately upstream of the roadway, when runoff concentrated there, to levels above the existing roadway grade, assuming that the drainage basin was saturated at the time of the rainfall and that all ponds within the basin were full, but that the level of Lake Lafayette was at or below 45.3 feet NGVD. T.489. "Ordinary high water for Alford Arm is 45.7 [feet NGVD.]" T.486. On this record, it can only be a matter of speculation how often (if ever) a 25-year return, two-hour storm might be expected to occur after rainfall has saturated the ground and filled all ponds in the drainage basin without raising the lake above 45.3 feet NGVD. The wet conditions Mr. Biddy assumed already to obtain in the drainage basin at the time of the hypothetical storm seem unlikely to coincide with the low lake level assumed to occur simultaneously. Alford Arm's 100-year flood level is 51 feet NGVD, "50.25 for the 25 year flood or rainfall, and elevation 49.9 for the 10 year storm water event." T.425. In any event, flooding of the Saltiels' property attributable to the proposed raising of the roadway would last only a matter of hours every quarter of a century according to Mr. Biddy, and would represent temporary diversion of water that would otherwise have flooded their property downstream of the roadway. Even then, no house or structure on the Saltiels' property would be affected nor any part of their property not within the 100-year flood plain. At all water levels below the existing roadway grade, the overwhelmingly more frequent condition, larger culverts would prevent or diminish flooding that might otherwise reach the Saltiels' property upstream of the roadway. By impeding flows downstream, the roadway affords some solids suspended in the water an opportunity to precipitate, instead of being borne on into Alford Arm. Under certain conditions, the larger culverts proposed by the Nashes would reduce time for particulate matter to settle upstream of the roadway; the greater volume of flow through larger culverts would reduce the time water was impounded upstream. Uncontroverted expert testimony established, however, that any increase in turbidity in water reaching Alford Arm would not violate applicable standards.

Recommendation It is, accordingly, RECOMMENDED: That DER issue a dredge and fill permit to Mr. and Mrs. Nash for the project described in their application on the conditions stated in the notice of intent to issue. DONE and ENTERED this 28th day of August, 1992, in Tallahassee, Florida. ROBERT T. BENTON, II Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 28th day of August, 1992. APPENDIX Petitioners' proposed findings of fact Nos. 2 and 10 have been adopted, in substance, insofar as material. With respect to petitioners' proposed finding of fact No. 1, what knowledge petitioners are charged with is a matter of law. Petitioners' proposed findings of fact Nos. 3, 4, 7, 8, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27, 28, 29 and 31 pertain to subordinate matters. Petitioners' proposed findings of fact Nos. 5, 6 and 32 pertain to immaterial matters as does petitioners' proposed finding of fact No. 9. Only the dredge and fill permit DER proposes to grant the Nashes is at issue. With respect to petitioners' proposed finding of fact No. 30, the calculations of both Mr. Flatt and Mr. Biddy seem to be flawed. With respect to petitioners' proposed finding of fact No. 33, it is not clear that the proposed project would increase the flooding on the Saltiels' property significantly. Temporally de minimis, the change might amount only to relocating the flooding. With respect to petitioners' proposed finding of fact No. 34, see finding of fact No. 12. With respect to petitioners' proposed finding of fact No. 35, larger culverts will decrease the velocity of the flow through the culverts. Petitioners' proposed finding of fact No. 36 is immaterial because it does not relate to any applicable rule or statutory standard. With respect to the individual respondents' and intervenor's (applicants') proposed findings of fact Nos. 1 and 2, the application does not specify dredge and fill. The applicants' proposed findings of fact Nos. 3, 4, 5, 7, 8, 10, 17, 18, 19, 20 and 32 have been adopted, in substance, insofar as material. With respect to the applicants' proposed finding of fact No. 6, backwater flows at levels above 45.3 feet NGVD. With respect to the applicants' proposed finding of fact No. 9, the OHW is 45.7 feet NGVD. With respect to the applicants' proposed finding of fact No. 11, testimony so implied. With respect to the applicants' proposed finding of fact No. 12, Mr. Nash suffers from muscular dystrophy. The applicants' proposed findings of fact Nos. 14 and 15 pertain to subordinate matters. With respect to the applicants' proposed finding of fact No. 16, the only testimony regarding flooding concerned the critical 25-year return storm. With respect to DER's proposed findings of facts Nos. 1 and 2, the application does not specify dredge and fill. With respect to DER's proposed finding of fact No. 3, backflows begin at 45.3 feet NGVD. With respect to DER's proposed finding of fact No. 4, not all fill would be removed. With respect to DER's proposed finding of fact No. 5, testimony so implied. With respect to DER's proposed finding of fact No. 6, no statute or rule specifies a design storm. DER's proposed finding of fact No. 7 is really a conclusion of law. With respect to DER's proposed finding of fact No. 8, less settling may result in more suspended solids under some conditions. DER's proposed findings of fact Nos. 9, 10, 11 and 12 have been adopted, in substance, insofar as material. DER's proposed finding of fact No. 13 is immaterial to the merits. COPIES FURNISHED: John A. Barley P.O. Box 10166 Tallahassee, FL 32302 Donna H. Stinson Moyle, Flanigan, Katz, Fitzgerald & Sheehan, P.A. 118 North Gadsden Street Suite 100 Tallahassee, FL 32301 Candi E. Culbreath Patricia Comer 2600 Blair Stone Road Tallahassee, FL 32399-2400 Carlos Alvarez c/o Hopping, Boyd, Green & Sams 123 South Calhoun Street Tallahassee, FL 32301 Daniel H. Thompson, General Counsel Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, FL 32399-2400 Carol Browner, Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, FL 32399-2400

Florida Laws (2) 120.57267.061
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COLLIER CATTLE CORPORATION AND TROPICAL RANCH PROPERTIES, INC. vs SOUTH FLORIDA WATER MANAGEMENT DISTRICT AND DEPARTMENT OF ENVIRONMENTAL PROTECTION, 97-001682 (1997)
Division of Administrative Hearings, Florida Filed:Naples, Florida Apr. 04, 1997 Number: 97-001682 Latest Update: Sep. 28, 1998

The Issue The issue is whether Respondent South Florida Water Management District is entitled to an environmental resource permit from Respondent Department of Environmental Protection to construct a weir in Collier County on the Merritt Canal about 3600 feet south of Interstate 75 for the purpose of extending the hydroperiod on the Florida Panther Federal Wildlife Refuge.

Findings Of Fact Proposed Permit On April 17, 1996, Respondent South Florida Water Management District (District) filed with Respondent Department of Environmental Protection (DEP) an application for the construction of a water-control structure in the Merritt Canal. The stated purpose of the structure, which is a weir, is to extend the hydroperiod of the Lucky Lake Strand. The application states that the District is the owner of a drainage easement covering the land proposed as the site of the weir. According to the application, Collier County, in which the Merritt Canal lies, originally held the drainage easement. The District later adopted the Merritt Canal as a "Works of the District," which transferred operational responsibility for the canal from the County to the District. (A sub-unit of the District, the Big Cypress Basin Board has jurisdiction for District projects of the type involved in this case. References to the District shall include the Big Cypress Basin Board.) The application requests a permit to construct an adjustable sheet-pile weir within the 80-foot Merritt Canal right-of-way. The application accurately describes the Merritt Canal as a Class III waterbody that is not an Outstanding Florida Water. By Notice of Intent to Issue Environmental Resource Permit dated January 29, 1997 (NOI), DEP proposed to issue an environmental resource permit (ERP) to the District for the construction of the Lucky Lake Strand Water Control Structure. The structure would be an adjustable weir with operating levels of 7.0 feet National Geodetic Vertical Datum (NGVD) in the wet season and 9.5 feet NGVD in the dry season. As stated in the NOI, the Merritt Canal is 12 miles long and one of four main north-south canals within a larger system of 183 miles of canals--all Class III waters-- constructed in the 1960s by Gulf American Land Corporation to drain wetlands for development of the Southern Golden Gate Estates area. These four north-south canals drain water south through the Faka Union Canal and into Faka Union Bay, which is part of the 10,000 Islands/Cape Romano Aquatic Preserve. The preserve contains Class II Outstanding Florida Waters. The NOI notes that the U.S. Fish and Wildlife Service (FWS) and District entered into an agreement in September 1994 to construct two weirs in the Merritt Canal "to partially restore historic hydroperiods into two major wetland features within the federally owned lands of the USFWS Florida Panther National Wildlife Refuge, Lucky Lake Strand and Stumpy Strand (Class III Outstanding Florida Waters)." As stated in the NOI, these federally owned wetlands constitute over 3000 acres of cypress and mixed swamps, wet prairies, marshes, and ponds. The NOI relates that FWS staff proposed the project to counteract "subtle vegetational changes and accelerated pond draw-downs [that] were taking place in the strands as a result of shortened hydroperiods caused by a three-year drought, I-75 widening activities, and subsequent canal modifications." The NOI correctly states that water in the wet season historically flowed southerly through Stumpy Strand, Lucky Lake Strand, and Picayune Strand, before entering the larger Fakahatchee Strand. Lucky Lake Strand narrows to 1000 feet at its south end, which is at Interstate 75 (I-75). The NOI accurately asserts that the construction of the Merritt Canal and the I-75 borrow canals combined to draw down the upstream wetlands, thus reducing their hydroperiods. The effect of the Merritt Canal is reportedly significant because of its confluence with the southern tip of Lucky Lake Strand. The NOI discloses that the original agreement between the District and FWS called for the construction of two weirs south of I-75, one at the headwaters of the Merritt Canal and another about 1800 feet downstream in the Merritt Canal. However, the proposed permit eliminates one weir, whose function was performed by plugs in the north I-75 borrow canal, and relocates the remaining proposed weir about 3600 feet south of I-75, rather than immediately south of I-75, reportedly because of difficulties in accessing the proposed weir at I-75. The NOI states that the Merritt Canal is within the 80-foot drainage easement originally acquired by Collier County. The uplands adjacent to the weir are reportedly owned by DEP. The NOI describes the proposed weir as a sheet pile weir with adjustable partitions. As proposed, during the wet season, the District would start to open the gates at 7 feet NGVD and start to close them at 6.5 feet NGVD. During the dry season, the District would start to open the gates at 9.8 feet NGVD and start to close them at 9.3 feet NGVD. Also, the proposed permit would anticipate that the District would dredge the canal to a trapezoidal cross-section having a bottom elevation of -1.5 feet NGVD and a width of about 49 feet at the weir and transitioning to 20-foot bottom widths upstream and downstream of the weir. According to the NOI, the purpose of the proposed weir is to reduce over-drainage of the upstream wetlands in Lucky Lake and Stumpy Strands by extending the hydroperiod further into the dry season. No increase in water levels during the wet season is expected. Although the historic extended hydroperiod is not expected to be achieved, the weir structure is expected to improve current conditions to the upstream wetlands. Holding back water in these wetlands [is] also expected to improve water quality downstream by removal of excess nutrient, sediments, and chemicals. Wildlife values are expected to be enhanced in preferred waterfowl and wading bird habitat, including areas for the endangered wood stork and threatened bald eagle. Forage areas are also expected to be improved for white-tailed deer and other wildlife species which are essential prey for the endangered Florida panther. Aquifer recharge is also expected as the ground water reserves will be raised by raising the canal water levels, while maintaining the existing level of flood protection for adjacent private landowners. The NOI states that FWS will monitor post- construction environmental conditions and will recommend to the District adjustments to the weir elevations. The NOI reports that the District will be the "main operator" of the weir to adjust elevations to maintain flood control for adjacent lands. The NOI adds: The project was designed so as not to decrease the peak discharge capacity in the canal or increase flood stages in the Upper Merritt Canal watershed. Hydraulic modeling by the District indicates that there will be no additional surface water flooding to private property as a result of the project, and the current level of service will be maintained. Based on this analysis, the NOI concludes that the District has provided reasonable assurance that the proposed activity will comply with Part IV, Chapter 373, Florida Statutes, and the underlying rules, including Chapter 62-330 and Rules 40E-4.301 and 40E-4.302, Florida Administrative Code. The NOI states that the District has demonstrated that the activity is clearly in the public interest, pursuant to Section 373.414(1)(a), Florida Statutes. The proposed permit conforms to the NOI's description. Specific Condition 13 sets the fixed crest of the proposed weir at 4.5 feet NGVD and the width of the weir at 48 feet. Although the proposed permit is nowhere explicitly conditioned on a successful wetland enhancement project, Specific Condition 12 states that "the" wetland enhancement project shall be considered successful if, after five years, Lucky Lake Strand and Stumpy Strand display wetland- appropriate vegetation and the "viability of adjacent upland sites [is] not negatively impacted by increased ground water or surface water levels resulting from the authorized project." Specific Condition 17 requires the District to document the operation of the gates and notify DEP, within three days, whenever any of the permitted elevations are exceeded. Annually, the District must supply DEP detailed data and analysis of the operational history of the weir, including "reasons for going to nonstandard operation and a narrative description of the effectiveness of initiating the nonstandard operation to include areas not flooded (or flooded, if applicable) and other associated impacts." During the final hearing, the District proposed, and DEP approved, a modification of Specific Condition 18. As modified, Specific Condition 18 requires the District to "monitor the effects of the operation" of the weir, pursuant to the revised monitoring plan incorporated by reference into this condition. The revised monitoring plan, which is dated November 12, 1997, alters the original monitoring plan by adding two sites for the installation of water-table wells. One of the new sites (Site A) is 1200 feet north of the weir, and the other new site (Site B) is 1200 feet north and 2000 feet west of the weir. These are the only water-table monitoring devices. Five other sites are surface-water monitoring sites. Three of the these sites are in the Merritt Canal: one immediately upstream of the weir, one immediately downstream of the weir, and one farther upstream at I-75. The other two surface-water monitoring sites are farther upstream. One is in Lucky Lake about 1.75 miles north of the weir, and the other is about three miles northeast of Lucky Lake. Three other sites are rainfall-monitoring sites. Two rainfall-monitoring sites are north of the weir. The site just north of I-75 is at the Ford Motor Company test track, which is immediately west of Lucky Lake and Stumpy Strands, and the site more directly north of the Merritt Canal is about ten miles north of I-75. Specific Condition 18 states the frequency with which someone (presumably a District employee or contractor) is to collect the data from these 10 monitoring sites, but contains no performance criteria. The monitoring plan thus commits the District to collecting data, but not to analyzing the data, nor, more importantly, taking specified actions when certain performance parameters are exceeded. Neither the revised monitoring plan nor the application in any way commits the District to using the data collected from the revised monitoring plan to develop a set of criteria, based on rainfall amounts, groundwater levels, and surface water levels, to fine-tune the operation of the gates so as not to exacerbate present flooding. Nothing in the revised monitoring plan or the application suggests that the District will use the data collected from the revised monitoring plan to identify more clearly the relationships between storm events and water levels to understand better the relationship between flooding, on the one hand, and the existence of the proposed weir and the operation of its gates. Faka Union Canal Watershed and Southern Golden Gate Estates What is now known as the Faka Union Canal Watershed historically covered about 234 square miles. It ran from an area about four miles north of what is now known as Immokalee Road south in a widening expanse that approached 12 miles at what is now U.S. Route 41. It then ran south until it emptied into the Gulf of Mexico at Faka Union Bay in what is now the Cape Romano Ten Thousand Islands State Aquatic Preserve east of Marco Island. Land alterations due to road and canal construction and urban and agricultural development eventually reduced the Faka Union Canal Watershed to about 189 square miles. Most noticeably, these changes narrowed the drainage area at U. S. Route 41 from almost 12 miles to little more than the width of the Faka Union Canal. The Faka Union Canal Watershed is characterized by low relief and poorly defined drainage patterns. At the north boundary of the watershed, which now ends at Immokalee Road, the elevation reaches 24 feet NGVD. Twenty-eight miles to the south, at the outlet of the basin, the elevation is two feet NGVD. The water flows generally in a southwest direction. Historically, water ran slowly through the watershed in sheetflow several miles wide and a few inches to a few feet deep. Drainage concentrated in slightly lower sloughs and strands, which generally dried out in the dry season. Historically, the watershed featured flat, swampy lands containing cypress trees, islands of pine forests, and wet and dry prairies. Prior to development, much of the watershed remained inundated by several feet of water during the five- month wet season (roughly from mid-May through mid-October). In this undisturbed state, the prominent features of the watershed were the storage of runoff in depressional areas, attenuated peak flows, and a longer hydroperiod into the dry season. In the early 1960s, Gulf American Land Corporation subdivided a 173 square-mile area in Collier County into many thousands of lots as small as 1.25 acres. The development was Golden Gate Estates. The portion of Golden Gate Estates south of I-75 is known as Southern Golden Gate Estates. Golden Gate Estates is west of the Merritt Canal. Gulf American's purpose in dredging the 183-mile canal system was to allow it to market as land, available for continuous occupation, subdivided lots superimposed over an area that was land during the dry months and water during the wet months. To achieve this objective, Gulf American Land Corporation constructed one group of canals that drains to the west and another group of canals drains to the south into the Faka Union Canal. Gulf American dredged the canals draining to the south, which form the Faka Union Canal System, from 1968 through 1971. Four north-south canals spaced two miles apart drain Southern Golden Gate Estates and the portion of the Faka Union Canal Watershed north of I-75. From west to east, the canals are the Miller Canal, Faka Union Canal, Merritt Canal, and Prairie Canal. Only the two westerly canals run north of I-75. The Miller Canal extends almost seven miles north of I-75, and the Faka Union Canal extends about 14 miles north of I-75. The Merritt Canal starts in the immediate vicinity of I-75, and the Prairie Canal starts about two miles south of I-75. The average excavated depth of the four canals is about ten feet from the top of the bank to the bottom of the channel. Given the relatively close proximity of the water table to the surface in this area, excavation to these depths thus established a direct hydraulic connection with the surficial aquifer. The canals are large, ranging from 45 to over 200 feet wide. Although unable to convey without flooding the water from even a ten-year storm event, which is the level of service standard set by Collier County for Southern Golden Gate Estates, the Faka Union Canal system has nonetheless severely impacted the water resources of Collier County. According to the Hydrologic Restoration of Southern Golden Gate Estates, prepared in February 1996 by the Big Cypress Basin Board (Southern Golden Gate Estates Restoration Plan): . . . Construction of the canals has led to both increased volumes and rates of runoff from the watershed which has had lasting effects on the area's water supply, vegetation, wildlife, and coastal estuaries. The canals intercept large volumes of surface and subsurface flow and quickly divert them to the Faka Union Bay and the Ten Thousand Island Estuary of the Gulf of Mexico resulting in less surface water available for storage. Since groundwater recharge is achieved primarily through infiltration from surface detention storage, reduced groundwater recharge threatens both groundwater supply for the region and the natural barrier to salt water intrusion. Continued overdrainage has caused an eventual lowering of the groundwater table. This has caused vegetation to change from wetland dominant to transitional and upland systems with invasive exotic species. The extreme dry conditions caused by overdrainage have resulted in more frequent and more intense wildfires with a greater destructive impact on vegetation. The increased runoff rate has had severe effects on the receiving estuaries. Historically, the estuaries would receive broad, slow moving sheets of water that were capable of carrying essential nutrients but not high sediment loads. This has been replaced with point loads of freshwater at the Faka Union Canal outlet that push salinity levels down and result in freshwater discharge shocks throughout the Ten Thousand Island Estuary. The increased runoff rate drains the area quickly and does not allow the hydroperiods necessary to sustain wetland vegetation. . . . Southern Golden Gate Estates Restoration Plan, pages 8-9. The major roadway affecting the Faka Union Canal Watershed is State Road 84, which was a two-lane road constructed in 1966. In 1990, construction was completed transforming State Road 84 into four-lane I-75. These road projects have hastened drainage of the lands to the north of I-75 and east of the Faka Union Canal. The land north of the Merritt Canal is largely undeveloped. If one were to extend the Merritt Canal due north of I-75, it would run through the middle of Lucky Lake Strand and much of Stumpy Strand, which is immediately to the north of Lucky Lake Strand. Agricultural land owned by Collier Enterprises is just north of the Ford Motor Company test track and immediately west of Lucky Lake Strand. Agricultural land owned by Baron Collier Company is immediately north of Stumpy Strand. This imaginary extension of Merritt Canal would mark the west boundary of the Florida Panther National Wildlife Refuge, which was established in June 1989. The Florida Panther National Wildlife Refuge constitutes 26,000 relatively undisturbed acres immediately north of I-75. Intervenor Clifford Fort owns property south of the refuge on the south side of I-75. The Florida Panther National Wildlife Refuge features mostly wetlands, oak hammocks, pine flatwoods, and prairies. The refuge receives runoff from stormwater and possibly agricultural pumping of the water table from the adjacent farmland. In addition to draining into the headwaters of the Merritt Canal near the southwest corner of the refuge, the refuge also drains into the northerly borrow canal running along the north side of I-75. In the vicinity of the Merritt Canal, the four borrow canals running along the north and south sides of I-75, on both sides of the Merritt Canal, drain in the direction of the Merritt Canal. Listed species using the Florida Panther National Wildlife Refuge include the Florida panther, Florida black bear, wood stork, roseate spoonbill, limpkin, and Eastern Indigo snake. In October 1995, an inordinate amount of rain fell in the area. Attracted by the increased water depths, which more closely approximated historic conditions, 75 wood storks nested in the Lucky Lake Strand; in drier years, wood storks do not nest in the strand. Lucky Lake Strand occupies the southwest corner of the Florida Panther National Wildlife Refuge. Lucky Lake and two other ponds are present in this area. When full, Lucky Lake and one of the ponds are about 50 meters wide, and the third pond is about half of this width. During the dry season, a person can throw a stone across any of the ponds. Historically, Lucky Lake and Stumpy strands passed surface water into the Picayune Strand, which is west of the Merritt Canal and south of I-75, from which the water ran into the Fakahatchee Strand. Lucky Lake Strand presently narrows to about 1000 feet at I-75. The hydrologic connection between the outlet of Lucky Lake Strand and the headwaters of the Merritt Canal has contributed significantly to the overdrainage of these two strands, which occupy a significant area within the federal refuge. The FWS wildlife biologist stationed at the Florida Panther National Wildlife Refuge reported in a habitat assessment report prepared in August 1996 that four ponds in the strand dried out by December so that they could not sustain fish or provide feeding habitat for birds. Permitting Criteria Public Health, Safety, or Welfare or Others' Property One of the main disputes between the parties is the affect of the proposed weir on flooding. This case is largely about flooding or, more generally, the amount of water to be stored for a specified period of time. Petitioners and Intervenors fear that the District's effort will cause flooding to areas south of I-75 and east and west of the Merritt Canal. Occupying property within a vast area whose natural drainage patterns have been greatly disrupted, Petitioners and Intervenors justifiably fear the ravages of flood and fire. Although this area was undoubtedly subject to these hazards prior to man's alteration of the natural landscape, large- scale alterations to natural drainage in Southwest Florida have artificially heightened the risk presented by these natural hazards. Destructive flooding follows the inhabitation of areas historically devoted to the storage of considerable volumes of water; the flooding is exacerbated where, as here, natural drainage features have been replaced by artificial facilities that are inadequate for both the natural flows and the new, artificial flows generated by development. Although inadequate for the natural and artificial flows generated by even design storm events, the artificial drainage facilities nevertheless change historic drainage rates, accelerating the rate and volume of natural drainage and shortening the hydroperiod. In this manner, the artificial drainage facilities contribute to the desiccation of previously saturated soils and foster conditions suitable for dangerous fires. Initially, Petitioners and Intervenors contend that the District seeks approval of the proposed weir as an indirect means of implementing the Southern Golden Gate Estates Rehydration Plan. Little evidence supports this concern. The Southern Golden Gate Estates Rehydration Plan outlines several alternatives for the proposed rehydration of Southern Golden Gate Estates. The preferred alternative does not call for a weir at the proposed location. The purpose of the proposed weir is to rehydrate an area north of the Southern Golden Gate Estates. As discussed below, the role of the proposed weir in rehydrating Southern Golden Gate Estates appears insubstantial to the point of nonexistent. Focusing on the location of the proposed weir over half of a mile downstream from the southernmost part of the area intended to be rehydrated, Petitioners and Intervenors dispute the stated purpose of the project, focusing on the District's earlier relocation of the proposed weir from positions just north and then just south of I-75 to its present position a half-mile farther to the south. The District did nothing to allay this concern of Petitioners and Intervenors when its employees could not provide a reasonably detailed explanation of the process by which someone moved the proposed site to the south. From the District's evidence, one would infer that the decision to relocate the proposed weir to the south spontaneously emerged, without human sponsor, in the course of bureaucratic decisionmaking. The District asserted that the northerly sites were impractical due to access problems. However, the District made little, if any, real effort to see if the Department of Transportation would allow access to these more northerly sites--one of which the District might be able to access without the consent of the Department of Transportation. The record does not reveal why the District relocated the proposed weir to its present location, considerably south of its initial two locations at I-75. Again, though, the evidence does not support the contention of Petitioners and Intervenors that the relocation decision was part of a private plan among District employees to incorporate the proposed weir as part of a more ambitious project to rehydrate Southern Golden Gate Estates. Nor does the evidence establish, as Petitioners and Intervenors contend, that the relocation decision was driven by the concerns of three influential landholders to the north of I-75--Collier Enterprises, Barron Collier Company, and Ford Motor Company. These three landholders approved the proposed weir in its present location over a half-mile to the south of its original locations and may have expressed concern that the original locations at I-75 would unreasonably raise the risk of flooding their land and business and agricultural activities to the north of I-75. If the District's real reason for relocating the proposed weir was due to objections from these landowners to the north of I-75, this reason would not itself help Petitioners and Intervenors. If the District acceded to the demands of these landowners to the north, it does not necessarily follow that the District lacked confidence in its flood calculations. A relocation decision under these circumstances would have as likely reflected political, as scientific, concerns. Additionally, if the District moved the proposed weir at the insistence or suggestion of the landowners to the north, any flooding concerns voiced by these landowners raise different issues from the flooding concerns raised by Petitioners and Intervenors. Owners of land immediately to the north and west of the federal refuge are more directly within the area of the intended effects than are Petitioners and Intervenors. More substantially, Petitioners and Intervenors claim that the proposed activity is so negligently designed or will be so negligently operated as to result in heightened and more frequent flooding of areas to the west and east of the proposed weir. The District's record in operating weirs in Collier County is not flawless. In recent years, the District constructed and maintained a weir with unlawfully high gates and did not correct the noncompliant water-control structure for several months after first learning of the violation. However, this appears to have been an isolated violation. The division of responsibility between the District and Collier County for the maintenance of drainage canals is based on whether the canal is a primary or secondary drainage facility. The District has assumed responsibility for all of the primary drainage facilities in Collier County. Surprisingly, though, the record reveals no master map or index of the primary drainage facilities and at least the larger nonprimary drainage facilities. However, Petitioners and Intervenors failed to show that any confusion concerning maintenance responsibilities that may exist between the District and Collier County would appreciably raise the probabilities that the District would operate the proposed weir in such a way as to exacerbate present flooding concerns. The District and Collier County agree that the District has jurisdiction over the Merritt Canal. Petitioners and Intervenors have also failed to show that any confusion concerning secondary-drainage contributions that may exist between the District and Collier County would have a substantial impact on the successful operation of the proposed weir. The most significant claim raised by Petitioners and Intervenors asserts that the District failed to provide reasonable assurance that the proposed weir would not exacerbate flooding. Although the weir gates would be closed only during the dry season, the proposed activity requires analysis of the risk of heightened water elevations upstream of the proposed weir. In theory, flooding could result from the effects of the weir even when the gates are open, as well as the possibility of an extreme storm event during the dry season. Expert witnesses on both sides clashed over whether the design of the proposed weir was sufficient not to exacerbate existing levels, rates, and frequencies of flooding of adjacent uplands. The crucial feature over which the experts disagreed was the spoil banks running along the canal. When the Merritt Canal was constructed, the spoil was dumped along the banks. In the ensuing years, vegetation colonized and stabilized the spoil banks, which now function as levees. The expert witness called by Petitioners and Intervenors disregarded the spoil banks in his calculations. His lack of confidence in the opposing expert witness's use of top-of-bank elevations was partly justified for the reasons stated below. Although a minor point, part of the argument of Petitioners and Intervenors' expert witness proved too much by asserting that levees cannot maintain water levels higher inside the levee than the existing ground elevation outside the levee. On the other hand, in showing that the proposed weir would not exacerbate flooding, the District's expert witness relied, not entirely justifiably, on the top-of-bank elevations. The District took only spot elevations of the spoil bank and then assumed that these elevations prevailed along the entire 3600 feet of canal upstream of the weir. The District did not inspect the upstream banks for unpermitted culverts, of which at least one was discovered during the lengthy hearing in this case. There is a possibility of material differences in elevations along the spoil banks. These spoil banks were not constructed to a specified elevation; they were an excavation byproduct that was haphazardly deposited beside the excavated canal. Additionally, the record suggests that this general area has been the site of unpermitted works, such as the installation of a culvert and creation of unpermitted canal plugs. In the months over which the hearing took place, Petitioners and Intervenors alertly found a culvert breaching the spoil bank upstream of the proposed weir. At least one of their representatives demonstrated superior familiarity with the spoil bank over the familiarity demonstrated by the District's representatives. It is a fair inference that, if the spoil bank was substantially missing at any point upstream of the proposed weir, Petitioners and Intervenors would have brought such evidence to the hearing. The absence of such evidence, coupled with the reasonable inferences that may be drawn from the concededly more cursory investigation of the site by the District, precludes a finding that the spoil bank is substantially missing at any material point so as to warrant the use of ground elevations, as used by the expert witness called by Petitioners and Intervenors. At best, from the perspective of Petitioners and Intervenors, the record supports the finding that the spoil banks may not be as continuously as high as the District posits, but they are not nearly as low (i.e., nonexistent) at any point as Petitioners and Intervenors contend. The two experts also disagreed over two subordinate inputs used in running the flood calculations. The expert called by Petitioners and Intervenors claimed that initial tailwaters (i.e., water elevations downstream of the weir) in excess of 8.53 feet were appropriate. Although the canal has experienced historically higher tailwaters than 8.53 feet, the expert did not explain adequately why such higher tailwaters should be used in running the model, especially since flood calculations are not used to predict flooding conditions in all storms, such as a 1000-year storm. Absent a showing that tailwater in excess of 8.53 feet would be present at the relevant time preceding or during the design storm event, the expert called by Petitioners and Intervenors failed to show why the District's tailwater input was unreasonable. On the other hand, the District's expert claimed that the model required an adjustment to the friction factor or Manning's N coefficient. This adjustment, which decreased the friction factor by an order of magnitude, approximated a bottom that was many times smoother than the actual bottom of the Merritt Canal. The District's expert did not explain adequately why the lower friction factor should be used in running the model, and he frankly did not demonstrate the same familiarity with this friction factor as did the expert called by Petitioners and Intervenors. The most likely inference is that the District's expert erred in making this adjustment. There was another controversy between the parties regarding a subordinate input for the flooding calculations. Petitioners and Intervenors raised the possibility that agricultural discharges from the Collier properties adjacent to the federal refuge, which the District ignored in its calculations, might further undermine any assurances as to flooding. This could have been useful information if developed in the record, but the record permits no basis to quantify the value of this additional discharge or ascertain its timing relative to wet and dry seasons and storm events, if in fact this agricultural discharge takes place at all. Also, offsetting any such discharge would be two factors: the District ran its calculations assuming a runoff rate 25 percent greater than that appropriately used by the Florida Department of Transportation for modeling the design storm event, and the District ignored the plugs in the I-75 borrow canals, which attenuate the runoff into the Merritt Canal. Although Petitioners and Intervenors incorrectly inputted ground elevation in place of the top-of-bank elevation--when the best elevation is somewhere in between these two values--their expert's calculations are useful for illustrating a scenario that, for this reason, exceeds the worst-case scenario. Again, this is an illustration of a scenario that predicts greater flooding than reasonably should be predicted because, in actuality, the restraining elevation is higher than ground elevation. Using the 8.53-feet initial value for tailwater, Petitioners' Exhibit 27 illustrates the different water elevations resulting from running the model with and without the excessive reduction of the friction factor. Petitioners Exhibit 27 illustrates the effect of the design storm on upstream water elevations with the gates open. Petitioners Exhibit 27 ignores the spoil banks and instead uses prevailing ground elevations. At the site of the proposed weir, the canal bottom is at about -1.5 feet NGVD. The proposed weir would add fixed barriers up to an elevation of 5.0 feet NGVD; the adjustable gates would, when closed, extend the barrier from 5.0 feet NGVD to 9.5 feet NGVD. Approximate existing ground elevation averages about 10 feet NGVD downstream of I-75, with one dip to below 9 feet NGVD about 600 feet downstream of I-75. For about 6000 feet upstream of I-75, where there is no spoil bank whatsoever, the average ground elevation, outside of the slough, is about 13 feet. The slough bottom in this area gently slopes from about 9 feet NGVD to 10 feet NGVD. Ignoring the spoil bank, Petitioners Exhibit 27 predicts flooding in two major areas in the design storm event, even with the gates open. One of these is about 300 feet long, starting about 400 feet downstream of I-75. The other is at least 300 feet long, starting near the northern extreme of the modeled area and running off the modeled area. The District did not survey in detail the spoil bank along the 300 feet downstream of I-75. There is no spoil bank upstream of I-75 because there is no dredged canal. The water elevation about 400 feet downstream of I-75 would be almost one foot greater than the ground elevation. The water elevation about 6000 feet upstream of I-75 will be as much as half of a foot greater than the ground elevation. At the more downstream point, the actual water elevation would exceed the District's projection by nearly three-quarter of one foot. At the more upstream point, the actual water elevation would exceed the District's projection by over 1.5 feet. Although the record could have been better developed on this important point, there is reasonable assurance that the existing spoil-bank elevations are sufficient to contain these flood elevations predicted by the expert called by Petitioners and Intervenors. Petitioners and Intervenors claimed that the District could achieve its stated purpose of extending the hydroperiod in the Florida Panther National Wildlife Refuge without increasing the risk or extent of flooding of adjacent uplands. Petitioners and Intervenors suggested that the District repair an existing plug in the Merritt Canal just south of I-75. (This "plug" is actually the original ground surface, which evidently was undisturbed during the construction of I-75. Given the excavation of canals on both sides of what is now a narrow strip of earth, the land resembles a plug, and this recommended order refers to it as a plug, although this term is descriptive only of the feature's present appearance, not its method of creation.) There are actually six plugs--again, in the broad sense of the word--in the vicinity of the junction of the Merritt Canal and I-75. Two plugs interrupt the flow into the Merritt Canal of the borrow canals to the north of I-75. Two plugs likewise interrupt the flow into the Merritt Canal of the borrow canals to the south of I-75. The last two plugs are in the Merritt Canal, a few feet north and south of I-75. Repairing the plug immediately south of I-75 would raise the water elevation by about 1.3 feet under the I-75 bridge. By about 2000 feet upstream of I-75, there is no significant difference between the water elevation using the model of Petitioners and Intervenors' expert for the proposed weir 3600 feet downstream of I-75 and the water elevation for the proposed plug repair just south of I-75. Repairing the plugs would have reduced the water elevation downstream of I- 75 by less than one half of a foot. Petitioners, Intervenors, and their expert have proposed a promising alternative to the proposed weir. The alternative appears to serve the stated purpose of the proposed activity at least as well as the proposed weir would, if not somewhat better due to its closer proximity to the targeted federal refuge, and the alternative project would cost much less to construct, maintain, and operate. The restorative nature of the work would probably relieve the District of the necessity of obtaining a permit. Perhaps the prospect of such work might motivate other state and federal agencies to grant the District access to the area at I-75 to build the weir at one of its first two locations. However, the issue is whether the District has provided reasonable assurance for the activity that it has proposed. As to flooding, the District has provided reasonable assurance that the proposed activity will not exacerbate flooding during the design storm events or even more severe storm events. Even assuming an absence of reasonable assurance as to flooding, the first criterion requires consideration of whether the proposed activity would adversely affect the public health, safety, and welfare or the property of others. Extending the hydroperiod of the federal refuge protects the property of others by reducing the period of time that the turf is dried out. This provides a wide range of environmental protection, including protection against the risk of fire caused by excessive drainage, for the federal refuge and other property in the area. Retarding the artificially high rate of drainage will improve water quality in at least two respects. The proposed weir will retard and reduce the nutrients conveyed down the canal and into the estuary into which it eventually empties. The proposed weir will also tend to restore somewhat the rate and timing of historic freshwater inputs on which the viability of the estuary and its inhabitants depends. Concerns about public health, safety, and welfare, as well as the property of others, cannot be severed from these broadscale environmental benefits to be derived from the proposed activity. Public health concerns are tied to these considerations. Thus, even if the District had failed to provide reasonable assurance as to flooding alone, the District has provided reasonable assurance that, on balance, the proposed weir will not adversely affect the matters set forth in the first criterion. Conservation of Fish and Wildlife, Including Endangered or Threatened Species, or Their Habitats The proposed weir will serve the conservation of a wide range of flora and fauna, as well as their wetlands habitat, within the targeted federal refuge. These species include listed species. The evidence does not support a finding that extending the hydroperiod of the federal refuge would in any way disturb the Florida panther. Navigation, Flow of Water, or Harmful Erosion or Shoaling The proposed weir will have not adversely affect navigation or the flow of water within the canal, and it will not cause erosion or shoaling. Fishing or Recreational Values or Marine Productivity in the Vicinity of the Activity The proposed weir will not adversely affect fishing or recreational values or marine productivity in the vicinity of the proposed weir. To the contrary, the proposed weir will enhance these values in the immediate vicinity of the proposed weir and downstream at the estuary at the mouth of the Merritt Canal. Temporary or Permanent Nature The proposed weir will be of a permanent nature. Significant Historic and Archaeological Resources The record provides no basis for a finding that the proposed weir jeopardizes significant historic and archaeological resources. Current Condition and Relative Value of Functions of Areas Affected by the Proposed Activity The federal refuge is functioning well environmentally, despite the adverse impact of dramatic disruptions of the natural drainage regime. The value of these functions is high. Likewise, the receiving estuarine waters are functioning well, despite the adverse impact of dramatic disruptions of the natural drainage regime. Extending the hydroperiod of the federal refuge will partially offset these historic disruptions. Thus, the proposed weir will assist in the functioning of natural systems that are now functioning well, but could use some help. Public Interest The proposed weir is not in an Outstanding Florida Water. Thus, the question is whether the proposed activity is not contrary to the public interest. The District has provided reasonable assurances as to the preceding seven criteria sufficient to demonstrate that, on balance, the proposed activity is not contrary to the public interest. Cumulative Impacts There is no evidence that the proposed weir will cause any adverse cumulative impacts upon wetlands or surface waters. Other Criteria The District has proved that the proposed weir would not violate any water quality standards. To the contrary, any effect from the proposed activity would be to improve water quality, especially downstream at the estuary. The restoration of conditions more typical of historic drainage would allow more nutrients to be captured upstream and would tend to restore the historic timing and volume of freshwater inputs into the estuary. For the reasons set forth above, the District has also provided reasonable assurance that the proposed activity meets the 11 criteria contained in Rule 40E-4.301, which largely duplicate the seven criteria discussed above, and the relevant provisions of the Basis of Review. It is true that the monitoring provisions are largely illusory because they provide no quantifiable parameter beyond which the District must take specified action. In other words, at best, the monitoring provisions assure that the District will collect post-operational flooding data, but they do not promise that the District will take any action if certain levels of flooding take place. However, the monitoring provisions are of little importance given the factual findings concerning flooding, as discussed above, and the legal requirements of the Basis of Review, as discussed below.

Recommendation It is RECOMMENDED that the Department of Environmental Protection enter a final order granting the permit for the construction of the proposed weir about 3600 feet south of I-75 in the Merritt Canal. DONE AND ENTERED this 25th day of June, 1998, in Tallahassee, Leon County, Florida. ROBERT E. MEALE 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 Filed with the Clerk of the Division of Administrative Hearings this 25th day of June, 1998. COPIES FURNISHED: James W. McDonald, Jr., Esquire McDonald & Associates Community Plaza, Suite 306 15600 Southwest 288th Street Homestead, Florida 33030 A. Glenn Simpson Qualified Representative 5961 22nd Avenue Southwest Naples, Florida 34116 Marcy I. LaHart Associate Attorney South Florida Water Management District 3301 Gun Club Road West Palm Beach, Florida 33416-4680 Francine M. Ffolkes Assistant General Counsel Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Walter R. Shaw, Sr., pro se 1400 Northwest 62nd Avenue Sunrise, Florida 33313-6138 Cliffort L. Fort 8410 Northwest 16th Street Pembroke Pines, Florida 33024 Kathy Carter, Agency Clerk Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 F. Perry Odom, General Counsel Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000

Florida Laws (4) 120.57267.061373.413373.414 Florida Administrative Code (6) 40E -4.30140E-4.30140E-4.30262 -330.10062 -330.20062-330.200
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PEYTON Z. PEEBLES, JR. vs DEPARTMENT OF ENVIRONMENTAL REGULATION, 89-003725 (1989)
Division of Administrative Hearings, Florida Filed:Gainesville, Florida Jul. 12, 1989 Number: 89-003725 Latest Update: Feb. 27, 1990

The Issue The ultimate issue for determination is whether the Petitioner has met the requirements of Sections 403.918 and 403.919, Florida Statutes, for the issuance of a dredge and fill permit within the waters of the State of Florida.

Findings Of Fact The Department takes exception to the Hearing Officer's statement in Finding of Fact No. 5 that the fill "over time will become inhabited by the types of life which live at the edge of the water and land." The Department argues that the record contains no competent, substantial evidence to support such a finding of fact. The law prohibits me, as agency head, from rejecting any finding of fact in a recommended order that is supported in the record by competent, substantial evidence, but I can and should reject findings of fact which are not supported in the record by competent, substantial evidence. Section 120.57(1)(b)10., Florida Statutes. In this case I must agree with the exception. A review of the entire record reveals no competent, substantial evidence to support the finding of fact. The only record evidence remotely bearing on the matter is that portion of the testimony of Dr. Peebles where he stated that "there probably are some small animals and little salamanders and whatever that live in that area, but I don't believe that they would all die. I think they migrate out into the other natural area that I'm leaving." (Tr. at 21) 2/ This testimony does not support the finding of fact, and the record contains no other evidence even remotely bearing on the matter. Therefore, I reject this finding of fact and accept the exception of the Department. The Department next takes exception to Finding of Fact No. 11 in which the Hearing Officer states that "However, this effect [on the life cycle of fish] will be minimal and would not itself cause significant damage to fishing or the lake." Once again, the Department contends that there is no competent, substantial evidence in the record to support the finding. Dr. Peebles testified: I can't honestly believe that me filling 14.3 percent, of my frontage is going to effect the health, safety, welfare and property of other people. The same goes for . . . whether the project will adversely affect the conservation of fish and wildlife, including endangered or threatened species, or their habitats. Now, this is a case where to argue that on a factual basis would require expert witnesses that would say yes and others that would say no. I think we would find conflicts on all of these subjects. (Tr. at 19) Dr. Peebles also testified that "14.3 percent of the shoreline for the use of the owner is not a serious thing. So I don't think any far reaching serious impacts will occur by granting [the permit]." (Tr. at 75) The only other statement in the record which arguably supports the finding of fact is a statement made by Dr. Peebles while questioning the Department's witness. There Dr. Peebles stated that "I know for a fact -- I'm a fisherman. I fish in the lake. It's a good fishing lake, and with all the construction that's already taken place you've still got good water quality." (Tr. at 70-71) Whether the proposed project and the cumulative impact of reasonably expected future similar projects will have a minimal or significant impact on fishing and the lake is an area requiring specialized knowledge, skill, experience or training. Although the lay opinion of Dr. Peebles may be helpful in supporting expert testimony, lay opinion standing alone may not under law establish what the impacts would be. Dr. Peebles acknowledges that he is not an expert in ecology or the environment, and admits that expert testimony is needed to determine whether granting the permit will adversely affect the conservation of fish and wildlife. (Tr. at 19) Therefore, Dr. Peebles' opinion that there will be no adverse effect on conservation of fish and wildlife (Tr. at 19) and that the filling of "14.3 percent" of the shoreline for the use of the owners will not have "any far reaching serious impacts" (Tr. at 75) is not supported by expert testimony and is not sufficient evidence to support the finding of fact. Section 90.701(2), Florida Statutes; Ehrhardt, Florida Evidence 387 (2d ed. 1984); Husky Industries v. Black, 434 So. 2d 988, 992 (Fla. 4th DCA 1983) ("Expert testimony is not admissible at all unless the witness has expertise in the area in which his opinion is sought.") Furthermore, the statement that Dr. Peebles made while questioning the Department's witness is not evidence. To the extent that it might be liberally construed as evidence in view of the fact that he was not represented by counsel, the existing fishing quality of the lake is not relevant to the impact of future filling of wetlands around the lake. On the other hand, Mr. Jeremy Tyler, accepted as an expert in the areas of the environment and water quality, (Tr. at 52) testified that the cumulative impact of granting Dr. Peebles' permit and similar permits reasonably expected would result in an adverse impact on conservation of fish and wildlife, (Tr. 35-41, 49-51, 54-55) and ultimately would result in a violation of water quality standards. (Tr. at 60, 64 and 69) Therefore, not only is there no competent, substantial evidence in the record to support the finding of fact, but there is uncontroverted expert testimony to the contrary Therefore, I accept this exception. The Department also takes exception to any implication in Finding of Fact No. 11 that the Department's only concern is with cumulative impacts. I do not read the Recommended Order as making any such implied finding. The record shows that the Department concluded that reasonable assurance had been provided that the instant project, standing alone, would not result in water quality violations, (Tyler, Tr. at 51, 60, 64) but that water quality violations will occur and the project is contrary to the public interest when the cumulative impact of reasonably expected future permit applications are taken into consideration. (Tyler, Tr. at 35-41, 49-51, 54-55, 60, 64 and 69) This does not suggest that the Department's only concern in such permitting decisions is cumulative impacts. It only means that under the facts of this application, the only remaining concern is the cumulative impact of reasonably expected future permit applications. The exception is rejected. The Department takes exception to Finding of Fact No. 12 to the extent that the statement "Mitigation of the impacts to fishing is not practical" implies that the only negative impact of the proposed project is to fishing. As noted in my discussion of Point 3 above, the record contains competent, substantial evidence that when the cumulative impacts of reasonably expected future projects are considered, water quality violations will result and the proposed project will be contrary to the public interest. I have reviewed the entire record and find no competent, substantial evidence to support a finding that the impact of the proposed project and cumulative impact of reasonably expected future projects would be limited to fishing quality. To the extent that the Recommended Order implies such a limited impact I reject the implication and accept the exception. The Department's final exception to findings of fact argues that Finding of Fact No. 14 improperly implies that the proposed project would not impair water quality. Finding of Fact No. 14 states, "The amount of fill proposed in this application would not place the lake at risk or impair fishing; however, if additional such permits are approved it may at some point impair the waters and fishing." Although some semantic difficulties arise out of the Hearing Officer's use of the terms "place the waters at risk" and "impair the waters," the finding of fact is consistent with - testimony of Mr. Tyler that reasonable assurance had been provided that this proposed project, standing alone, would not violate water quality standards. (Tr. at 51) The finding is also consistent with the testimony that when the cumulative impact of this project and similar reasonably expected projects are considered, reasonable assurance had not been provided that water quality standards will not be violated and that the project is not contrary to the public interest. (Tr. at 60, 64 and 69) However, the impact of the project on the water quality of the lake is a matter that requires expert testimony. As in the case with the impact on conservation of fish and wildlife discussed above, Dr. Peebles introduced no expert testimony regarding the impact of the project on water quality. On the other hand, the Department's expert witness testified that although reasonable assurance had been provided that the project, standing alone, would not violate water quality standards, (Tyler, Tr. at 51) he also testified that the project by itself would have some adverse impact on water quality. (Tyler, Tr. at 51) Therefore, any implication that the project by itself would not impair the water quality of the lake lacks support in competent, substantial evidence and is contrary to unrebuted expert testimony. To the extent the Hearing Officer's finding implies that the project will not impair water quality, such a finding can not affect the outcome of this case because impairment of water quality is not a proper legal criterion for deciding whether to grant or deny the permit. The proper criterion is whether reasonable assurance has been provided that the project will not violate water quality standards. Cf. Houle v. Department of Environmental Regulation, 10 FALR 3671 (DER Final Order, June 13, 1988), per curiam aff'd, 538 So.2d 1257 (Fla. 1st DCA 1989); Brown v. Dept. of Environmental Regulation, 9 FALR 1871, 1875 (DER Final Order, March 27, 1987), per curiam aff'd, 531 So.2d 173 (Fla. 4th DCA 1988). Since the implied statement of the Hearing Officer does not affect the outcome of this case, any error is harmless and I reject the exception. RULINGS ON EXCEPTIONS TO CONCLUSIONS OF LAW Burden of Proof The Department contends that the Hearing Officer erred in not placing the burden of proof on Mr. Peebles to show that the project is not contrary to the public interest when the cumulative impact of reasonably expected similar future projects are taken into consideration. An applicant for a permit has the burden of proof or persuasion to show entitlement to the permit. Florida Department of Transportation v. J.W.C. Co., 396 So.2d 778 (Fla. 1st DCA 1981). In order to show entitlement to a dredge and fill permit, an applicant must show that he has provided reasonable assurance that water quality standards will not be violated and that the project is not contrary to the public interest, and both of those tests must take into consideration the cumulative impacts of similar projects which are existing, under construction, or reasonably expected in the future. Sections 403.918(1), (2) and 403.919, Florida Statutes; Caloosa Property Owners' Ass'n v. Dept. of Environmental Regulation, 462 So.2d 523 - (Fla. 1st DCA 1985). 3/ The applicant's burden of proof includes the burden of giving reasonable assurance that cumulative impacts do not cause a project to be contrary to the public interest or to violate water quality standards. Concerned Citizens League of America, Inc., v. IMC Fertilizer, Inc., et al., 11 FALR 4237, 4244 (DER Final Order, March 29, 1989); Brown v. Dept. of Environmental Regulation, 9 FALR at 1877. At the hearing, the Department introduced expert testimony that reasonable assurance had not been provided that the project would not cause violations of water quality standards and was not contrary to the public interest when the cumulative impact of reasonably expected future projects were considered. (Tyler, Tr. at 35-41, 49-51, 54-58, 60, 64 and 69) Dr. Peebles, who bore the burden of persuasion, introduced no competent, substantial evidence to show that when cumulative impacts had been considered the necessary reasonable assurances had been provided. 4/ Dr. Peebles argues that his project will only fill in 14.3 percent of his shoreline, and only increase the percentage of the lake's wetlands that have been filled to 31.6 percent from the already existing 30 percent. However, it is not the incremental increase that causes the project to be not permittable, it is the cumulative impact of reasonably expected future projects, and Dr. Peebles failed to carry his burden of persuasion as to the cumulative impacts. Since Dr. Peebles did not carry his burden of persuasion he was not entitled to the permit as a matter of law, and the Hearing Officer erred in concluding that the permit should issue. Therefore, the Department's exception is accepted. Cumulative Impacts The Department takes exception to the Hearing Officer's conclusion of law that: Application of the cumulative effect principle denies the applicant a permit because of the destruction of wetlands by other landowners. The lack of emphasis on enforcement creates a disincentive to comply with the state's regulation of the waters. If those landowners who illegally filled the waters of the state were required to restore the wetlands they destroyed, then new applicants also could fill small portions of wetlands to enhance their use of their property without worrying about cumulative effects. (Recommended Order at 6) At this point it may be helpful to explain the role of cumulative impact analysis. The Department is required to take into consideration the cumulative impacts of similar projects which are existing, under construction, or reasonably expected in the future. Section 403.919, Florida Statutes; Brown v. Department of Environmental Regulation, 9 FALR 1871, 1876 (DER Final Order, March 27, 1987) (cumulative impact analysis is mandatory). Cumulative impact is not a third test, but rather a factor to be considered in determining whether reasonable assurance has been provided that the project will not result in violations of water quality standards and will not be contrary to the public interest. Concerned Citizens League of America, Inc. v. IMC Fertilizer Inc., 11 FALR 4237 (DER Final Order, March 29, 1989). As my predecessor Secretary Tschinkel observed: Without the ability to consider long-term impacts of a project (in combination with similar projects in the area considered "reasonably likely"), DER would be helpless to prevent gradual worsening of water quality and piece-meal elimination of biological resources inflicted by a proliferation of small projects. Morales v. Department of Environmental Regulation, 7 FALR 4786 (DER Final Order, September 18, 1985). The cumulative impact doctrine was originally developed as policy by the Department. It was subsequently codified by the Legislature in 1984 as Section 403.919, Florida Statutes. Chipola Basin Protective Group, Inc. v. Dept. of Environmental Regulation, 11 FALR 467, 476 (DER Final Order, December 29, 1988). - The doctrine was approved by the courts in Caloosa Property Owners Association v. Department of Environmental Regulation, 462 So.2d 523 (Fla. 1st DCA 1985). The cumulative impact statute, Section 403.919, is entitled "Equitable distribution." As the title suggests, the purpose of cumulative impact analysis is to distribute equitably that amount of dredging and filling activity which may be done without resulting in violations of water quality standards and without being contrary to the public interest. In order to determine whether the allocation to a particular applicant is equitable, the determination of the cumulative impacts is based in part on the assumption that reasonably expected similar future applications will also be granted. It does not necessarily follow, however, that all similar future applications must be granted if the current application is granted. Although the Department must be consistent in its permitting decisions to the extent possible and consistent with the public interest, (Rule 17-103.160, Fla. Admin. Code) each future application must stand on its own merit and must provide anew the necessary reasonable assurances subject to cumulative impact analysis. Manasota- 88, Inc, v. Agrico Chemical Co., et al., 90 ER FALR 043 (DER Final Order 1 February 19, 1990). In this case Dr. Peebles argued and the Hearing Officer concluded that the application of cumulative impact analysis is inequitable because previous unpermitted and allegedly illegal filling of wetlands around the lake now results in permits being denied which would have been granted but for the previous filling. There was testimony that about 30 percent of the original wetlands around the lake had been filled in the past, (Tyler, Tr. at 67) that all of the past filling was unpermitted, and that some of it may have been illegal. (Tyler, Tr. at 46, 61-62, 66-67, 72) However, the record contains no competent, substantial evidence showing how much, if any, previous filling was illegal. Furthermore, Section 403.919(2) requires the Department to consider the impacts of "projects which are existing", and does not draw a distinction between legal or illegal projects. As to the Hearing Officer's recommendation that cumulative impacts not be considered in this application, I note that Section 403.919, Florida Statutes mandates that such an analysis be conducted for every dredge and fill permit. Section 403.919 states that "The department in deciding whether to grant or deny a [dredge and fill] permit for an activity which will affect waters, shall consider [cumulative impacts]." See also Brown, supra, 9 FALR at 1876 (cumulative impact analysis is mandatory). Therefore, to the extent that the Hearing Officer is recommending cumulative impact analysis not be applied to Dr. Peebles' application, the recommendation is contrary to the law and must be rejected. The issue then remains of how past fill, whether legal or illegal, should be considered in the cumulative impact analysis. The Hearing Officer's recommendation in effect would require the Department to conduct a cumulative impact analysis under the assumption that previously filled wetlands should be treated as functioning wetlands. If I were to accept this view it would require the Department to take enforcement action in every case or abandon the protection of water quality of certain waters of the state. Such an interpretation would strip from the Department's hands the ability to exercise its discretion in allocating its limited enforcement resources, and result in the Department's enforcement priorities being set by permit applicants rather than by the Department. I note that the record contains competent, substantial evidence that the Department lacks sufficient resources to enforce every violation, (Tyler, Tr. at 45) although such a fact scarcely needs proof. Acceptance of the Hearing Qfficer's recommendation would place the Department in the dilemma of having to choose to withdraw enforcement resources from more environmentally significant projects or to abandon altogether the protection of less significant projects. Acceptance of the Hearing Officer's conclusion of law would also result in requiring the Department in all cases to determine whether violations had occurred and to take enforcement action for prior violations before it could consider cumulative impacts. Aside from the lack of sufficient enforcement resources, such enforcement' proceedings seldom, if ever, could be commenced and completed within the 90 days within which the Department must act on an application. Section 403.0876, Florida Statutes. The result would in effect limit the scope of Section 403.919 to pristine water bodies, and render the statute largely meaningless. I cannot accept that the Legislature intended such interpretations of Section 403.919, Florida Statutes. Although the result of the application of cumulative impact analysis to the facts of this case may seem harsh, the record indicates that Dr. Peebles may still obtain access the waters of the lake by means of a private dock that would not even require a permit if it had 1000 square feet or less of surface area and met the other provisions of Rule 17-312.050(1)(d), Fla. Admin. Code. Dr. Peebles' existing planned dock is 452 square feet. Therefore, Dr. Peebles could extend that portion of the dock that bridges the wetlands to the uplands by an additional 548 square feet of surface area. For example, the four foot wide bridge to the dock could be extended an additional 137 feet, which is more than enough to reach the upland portion of the lot. (Joint Exhibit No. 1) For the reasons state above, I reject the Hearing Officer's conclusion of law and accept the exception. Public Interest Test The Department also takes exception to the Hearing Officer's conclusion that the project is not contrary to the public interest. In conducting the public interest test the Department must balance the criteria as specified by the Legislature. Section 403.918(2)(a) states: In determining whether a project is not contrary to the public interest, or is clearly in the public interest, the department shall consider and balance the following criteria: Whether the project will adversely affect the public health, safety, or welfare or the property of others; Whether the project will adversely affect the conservation of fish and wildlife, including endangered or threatened species, or their habitats; Whether the project will adversely affect navigation or the flow of water or cause harmful erosion or shoaling; Whether the project will adversely affect the fishing or recreational values or marine productivity in the vicinity of the project; Whether the project will be of a temporary or permanent nature; Whether the project will adversely affect or will enhance significant historical and archaeological resources under the provisions of 5.267.061; and The current condition and relative value of functions being performed by areas affected by the proposed activity. The Department introduced evidence that criteria 1, 3 and 6 were neutral, (Tyler, Tr. at 54-56) that criteria 2, 4, 5 and 7 were negative, (Tyler, Tr. at 35-36, 54, 56, 57) and that when all the criteria were balanced there was a negative value to the project. (Tyler, Tr. at 57-58) Dr. Peebles argued at the hearing and in his response to exceptions that the Department's methodology in weighing each criteria in the public interest balancing test is incorrect. I disagree, and note that Dr. Peebles bore the burden of proof on the public interest test, and was free to introduce competent, substantial evidence on each criteria. As discussed in Part II above, Dr. Peebles did not introduce any competent, substantial evidence as to any of the above. The Hearing Officer's conclusion of law lacks competent, substantial evidence to support it, and is contrary to unrebuted competent, substantial evidence. Therefore, I reject this conclusion of law.

Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence of record, the candor and demeanor of the witnesses, and the pleadings and arguments of the parties, it is, therefore, RECOMMENDED that the application of Petitioner to place fill in the waters of the state be approved in accordance with the drawings submitted with the application. DONE and ENTERED this 28th day of February, 1990, in Tallahassee, Leon County, Florida. STEPHEN F. DEAN, Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida1 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 28th day of February, 1990. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 89-3725 The Agency filed proposed findings of fact which were read and considered. The Agency's findings were adopted or rejected for the reasons indicated as follows: Paragraphs 1-10 Adopted Paragraph 11 Adopted that it will damage fishing; however, this damage will be insignificant and will not truly affect tee fishing on the lake. Paragraph 12 Adopted The Applicant's letter was read and considered as oral argument on the issues presented at hearings. COPIES FURNISHED: Mr. Dale H. Twachtmann Secretary Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Daniel H. Thompson, Esq. Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Dr. Peyton Z. Pebbles, Jr. 6527 Northwest 42nd Place Gainesville, FL 32606 William H. Congdon, Esq. Office of General Counsel Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 =================================================================

Florida Laws (3) 120.68403.087690.701
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AUDUBON SOCIETY OF SOUTHWEST FLORIDA vs. LEE COUNTY BOARD OF COUNTY COMMISSIONERS AND DEPARTMENT OF ENVIRONMENTAL REGULATION, 81-002307 (1981)
Division of Administrative Hearings, Florida Number: 81-002307 Latest Update: Jul. 07, 1982

Findings Of Fact On April 2, 1981, Lee County applied to DER for a permit to construct an extension of Colonial Boulevard east to State Road 82B by dredging 4,600 cubic yards of material landward of the ordinary high water mark, and by depositing 83,000 cubic yards of fill landward of the ordinary high water mark in an area of Lee County known as the Six Mile Cypress Strand or Six Mile Cypress Slough. The permit application was made by Lee County on standard DER forms which would have been appropriate for an application under either or both Chapters 253 or 403, Florida Statutes. Additionally, Lee County tendered a permit application fee to DER sufficient to cover the cost of an application under both statutes. After review of the application, DER determined that it had no jurisdiction under Chapter 253, Florida Statutes, and refunded to Lee County that portion of the permit application fee required for a Chapter 253 permit. As indicated above, Lee County's application, on its face, reflected that no fill material or dredging was proposed waterward of the ordinary high water mark. The Six Mile Cypress Strand is a meandering swamp, approximately 44,000 acres in size, dominated by cypress trees. At periods of high water the waters of the swamp empty into Ten Mile Canal, an artificial water body which connects to Estero Bay by way of Mullock Creek, a natural stream. All water bodies involved in this proceeding are classified as Class III waters. Six Mile Cypress Strand functions as a major aquifer recharge area for the eastern central portion of Lee County. The area drained by the Strand receives approximately 54 inches of rainfall annually. The wetland vegetation and uneven contours of the Strand allow the assimilation of nutrients and reduction in turbidity and erosion which could otherwise adversely affect downstream waters. The drainage area north of the proposed project consists of approximately 5,000 acres, or 11 percent of the total drainage basin served by the Strand. The proposed roadway would cross the Strand through a corridor which contains three cypress heads, or flag ponds. These ponds generally retain water during dry periods and support a more diverse community of aquatic life than those portions of the Strand which become completely dry. At the time of final hearing in this cause, these ponds exhibited dry season characteristics and contained less than one foot of water in their deepest portions. During low water periods the Strand itself may be virtually dry except for standing water in the vicinity of cypress heads and flag ponds. Only during the rainy season, which occurs during approximately four months of the year, does the Strand contain standing water. During high water periods, however, water may flow continuously throughout the length of the Strand. During these latter periods, canoes and other such small water craft may be able to negotiate portions of the Strand. No evidence was presented, however, which would indicate that the Strand is now or has ever been utilized, or is susceptible to utilization, for commercial boat traffic. The lands in the Strand over which Lee County proposes to build the roadway were conveyed by the Trustees of the Internal Improvement Trust Fund to private ownership after having been acquired from the federal government under the Swamp and Overflow Grant Act of 1850. The Strand was not meandered in the original government survey of the area, and, in fact, the surveyor's field notes reflect that the area of the Strand was densely vegetated and crossed by several roads, including one crossing the section line in the same vicinity proposed for the Colonial Boulevard extension. The existence of this last referenced road is corroborated by biological evidence presently existing on the site, and from examinations of full infrared aerial photography of the area. It is approximately nine miles from the Strand to the nearest meander line contained in the original government survey. Further, evidence of record in this proceeding establishes that water craft may not presently be navigated from Estero Bay into the Strand because of man-made barriers, and no record evidence establishes that such navigation would have been possible at the time of Florida's admission to statehood in 1845 when the stream presumably was in its natural condition. The Department of Natural Resources was notified in accordance with DER policy, of the pendency of Lee County's application, and asserted no claim of ownership over sovereignty lands in the area of the proposed project. The design for the proposed roadway includes a system of collector and spreader swales on the upstream and downstream sides of the Strand, respectively, connected by large culverts to be located beneath the roadway. The swales and culverts are intended to minimize interruption of the Strand's hydroperiod, the natural fluctuation and flow of waters within the affected portion of the Strand. A vegetated swale system paralleling the roadway is also included in the proposed roadway design to provide treatment and nutrient uptake from storm water runoff generated from the surface of the roadway. In addition, the toe of the slope of the roadway will be replanted with native vegetation, and the edge of the fill area will be meandered to save some existing vegetation. It is anticipated that the roadway could result in runoff containing from .17 to .18 pounds per day of nitrogen, and from .01 to .07 pounds per day of phosphate. The grassy swales proposed for inclusion in the project design have the capability of assimilating from 1.8 to 3.6 pounds of these nutrients per day, thereby ensuring a significant safety factor. It can also reasonably be anticipated that the swale areas are capable of absorbing any BOD loading from the roadway surface. As a result, it can reasonably be anticipated that the construction of the project will not result in the discharge of nutrients into the Strand, and that any heavy metals will be bound in organic sediments and not result in degradation of existing water quality. Ambient water conditions in the Strand show low dissolved oxygen content together with high biochemical oxygen demand, neither of which should be exacerbated by construction of the project. No violation of water quality criteria relating to herbicides is anticipated in view of Lee County's commitment at final hearing in this cause to control vegetation by way of mowing instead of by the use of herbicides. The proposed construction will, of course, destroy aquatic vegetation in the area lying in the path or "footprint" of the roadway itself, consisting of approximately seven and one-half acres, three acres of which are predominantly cypress. However, because of the design features of the proposed roadway, including grass, collector and spreader swales and the culvert system, the anticipated impact on the hydroperiod upstream and downstream of the project, and thereby the effect on aquatic vegetation and water quality will not be significant. Construction fabric will be used to allow the road surface to be supported without demucking, thus minimizing turbidity during construction periods, although it is intended that construction be conducted during the dry season, thereby further reducing the potential for turbidity violations. Further, the detention swales which are to be equipped with French drains are designed to retain the first inch of rainfall. Culverts to be constructed on the roadway are designed to accommodate a 50-year, 24-hour storm event. The Secretary of DER issued the subject permit on August 18, 1981, without any prior notice of intent. ASSWF received notice of DER's action in the form of a complete copy of the permit on August 27, 1981. On September 2, 1981, ASSWF filed its petition requesting a formal Section 120.57(1), Florida Statutes, hearing. This petition was received by DER on September 8, 1981. ASSWF and Audubon, and the members of these organizations, use the Six Mile Cypress Strand in the vicinity of the proposed project for field trips and environmental education activities which will be impacted should the project be approved. In addition, Audubon owns property within the Strand which may also be affected by the proposed project if permitted. Intervenors, Community Council and Lehigh Acres of Florida, Inc., Ralph Marciano, Claudia Tipton and H. Mark Strong requested to be granted party status in this proceeding in support of the application. Ralph Marciano owns a business allegedly limited because of the present poor highway access to the business center of the city. Claudia Tipton owns an electrical construction business alleged to be seriously hampered because of extended transportation time in emergency trips. H. Mark Strong is a retired fire marshal and contends that paramedics are seriously hampered in transporting emergency patients to the community hospital located in Fort Myers. The Community Council of Lehigh Acres was formed to serve as a council representing the entire community of Lehigh Acres on problems and projects affecting the health, welfare, growth and prosperity of Lehigh Acres. Essentially, these intervenors assert that the general public welfare and, in some cases, their own personal business interests, will be enhanced by building the proposed roadway, thereby enhancing vehicular access to various portions of the community.

Florida Laws (3) 120.57403.087403.412
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VINCENT J. WOEPPEL vs DEPARTMENT OF ENVIRONMENTAL REGULATION, 92-004063 (1992)
Division of Administrative Hearings, Florida Filed:Lake Wales, Florida Jul. 06, 1992 Number: 92-004063 Latest Update: Apr. 16, 1993

Findings Of Fact On December 12, 1991, Petitioner applied to the Respondent for a permit/water quality certification to grade and level, in stages, approximately 20,000 square feet or 0.45 acres of lake front to remove and prevent the formation of berms and depressions in the exposed lake bottom adjacent to his property. The project site is located at 3955 Placid View Drive which lies along the shoreline of Lake Placid, a natural waterbody in Highlands County, Section 24, Township 37 South, Range 29 East. Lake Placid is not an aquatic preserve, and is not an outstanding Florida water. It has been designated as a Class III waterbody. Petitioner's unsubdivided lot lies at the western end of Lake Placid. The shoreline measures approximately 203 feet. The western lot line also measures 203 feet, and fronts on Placid View Drive. The water level of Lake Placid has receded in recent years which allows large expanses of what was historically lake bottom to become beaches, lawns, and areas of habaceous marsh. The specific project which the Petitioner proposes calls for the leveling of the berms and depressions which form on the exposed lake bottom from collected water, which stagnates and permits various noxious creatures, including mosquitoes, to breed in them. The berms and depressions are approximately six inches high or deep and between one and three feet wide, and generally extend the length of the shoreline. The proposed area affected is approximately 20,000 square feet or 0.45 acres of lake front, although Petitioner proposes to actually level a much smaller area in stages of approximately 2,000 square feet on an "as needed" basis. No material other than sod in the beach area is proposed to be brought from or removed to off-site locations. Petitioner is highly sensitive to mosquito bites. The area proposed for leveling was previously cleared of vegetation without authorization. Very little revegetation of the shoreline has occurred since the area was cleared. Vegetation colonizing the beach, at present, includes pennyworts (Centella asiatica and Hydrocotyle umbellata) and water- hyssops (Bacopa sp.) Blue green algae was observed in the depressions which have formed along the shore since the clearing. Fauna observed on-site included gulls (Larus sp.), small fish in the adjacent lake shallows, and water-boatmen (Order Hemiptera) in the depressions. An area landward of the wetlands considered here was also cleared previously and is proposed to be seeded. An adjacent, uncleared shoreline was vegetated with primrose willow (Ludwigia sp.), cattail (Typha sp.), flat sedge (Cyperus odorata), and other wetland species for an almost 100% plant coverage. The Petitioner proposes to use a small tractor in leveling of the shore which will cause turbidity in the lake water. No turbidity controls were proposed by the Petitioner. Petitioner failed to provide reasonable assurances that the turbidity caused by the earthmoving equipment in areas presently above water would not cause degradation of water quality in Lake Placid; would not contribute to the long-term degradation of water quality in the lake caused by upland runoff that would flow into the lake without benefit of retention or filtration by shoreland vegetation (freshwater herbaceous habitat) which would be permanently removed under Petitioner's proposal. Nutrients such a nitrogen and phosphorus and pollutants such as pesticides, herbicides and other chemicals commonly used in lawn and garden care would be included in the runoff, and would have an adverse impact on fishing and marine productivity in the lake. The project would have a minor adverse impact on erosion and soil stabilization in the area surrounding the lake. Petitioner has failed to provide reasonable assurance that the proposed project is not contrary to the public interest. Petitioner can mitigate the project by eliminating the use of heavy equipment and substitute hand equipment to smooth out ruts, berms and depressions in jurisdictional areas.

Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Petitioner's application for Wetland Resource Regulation permit be DENIED. DONE and ENTERED this 8th day of March, 1993, in Tallahassee, Florida. DANIEL M. KILBRIDE Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings ths 8th day of March, 1993. COPIES FURNISHED: Francine M. Ffolkes, Esquire Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32399-2400 Mr. Vincent J. Woeppel 3955 Placid View Drive Lake Placid, Florida 33852 Daniel H. Thompson Department of Environmental Regulation Acting General Counsel Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32399-2400 Virginia B. Wetherell Secretary Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32399-2400

Florida Laws (3) 120.57211.32267.061
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J. C. BASS; BASS RANCH, INC.; AND OKEECHOBEE COUNTY vs. COQUINTA WATER MANAGEMENT DISTRICT AND SOUTH FLORIDA WATER MANAGEMENT DISTRICT, 78-000181 (1978)
Division of Administrative Hearings, Florida Number: 78-000181 Latest Update: Nov. 14, 1978

Findings Of Fact On September 13, 1977, SFWMD advised Coquina by letter that "[a]t its September 8, 1977 meeting the Governing Board of this District gave Conceptual Approval of [Coquina's] surface water management plan . . . subject to the four special conditions found on page 15 of the District's staff report. . . [and an] additional special condition Joint exhibit No. 5. The first special condition found on page 15 of the District's staff report requires that complete construction plans be submitted, including "supporting calculations for all design elements not already submitted and any other plans necessary to assure adherence to the concept plan." Joint exhibit No. 2, page 15. The plan approved by SFWMD is designed to lower the water table in a 22 square mile area northwest of Lake Okeechobee in Okeechobee County. In its natural state, the land lies under water for part of the year. The corporate owner of the land has plans to subdivide it and sell residential lots, beginning with the four contiguous sections as to which the present application for a construction permit has been made. These four sections (phase I) lie north and south of each other in the western portion of the larger tract. The proposed construction would consist of digging ditches or swales paralleling existing and planned roads; building intersecting collector swales running north and south; installing ditch checks where swales intersect; dredging a retention pond into which the collector swales could empty at the south end of the phase I tract; digging an outfill ditch to channel water leaving the retention area for Ash Slough; and erecting a weir, between the retention area and the slough. Culverts through the weir would be equipped "with standard flash board risers in which the water level is regulated by stop logs which can be added or removed," Coquina's exhibit No. 1, p. 10, and the culverts would ordinarily serve as the route by which water from the retention area would reach Ash Slough. Under extremely wet conditions, however, water from the retention area could overflow the weir. The intervening petitioners own land on Ash Slough downstream from the retention area and adjacent to the southern boundary of the phase I tract. No formal studies of the likely effects of the proposed construction downstream were undertaken by Coquina or by SFWMD in evaluating Coquina's application. The surface water management plan given conceptual approval by SFWMD provides: The quantity of runoff flowing to the south through existing sloughs will be controlled to protect the downstream areas against flooding whereas at the present there is no control. The amount flowing to the existing sloughs to the south during the 25 yr. design storm will be limited to the amount flowing to those sloughs before any development takes place. Lesser storms will be more completely retained on the property. Controlled discharge will be provided from retention areas to the existing sloughs for the purpose of nourishing these streams. Coquina's exhibit No. 1, p. 1. (Emphasis supplied) Since no records of the amount of discharge to Ash Slough "before any development" are in existence, certain assumptions and estimates were made. One such assumption on which the application for construction permit proceeds is that the phase I tract all drains to the south, in its present state. In fact, some of the water now leaving the phase I tract travels in a westerly direction and never enters Ash Slough, at least under some weather conditions. If the proposed construction is accomplished, the phase I tract would all drain to the south through Ash Slough. As things now stand, a significant amount of water leaves the phase I tract by evapotranspiration. If the water table were lowered two and a half feet, which is what Coquina proposes, less water would leave the phase I tract by evapotranspiration, leaving more water to flow over the ground. In estimating the quantity of the anticipated discharge to Ash Slough, if the proposed construction takes place, it is necessary to take into account drainage onto the phase I tract from adjoining lands. Coquina has failed to furnish plans and supporting calculations sufficient to insure that the proposed construction will not increase the amount of flow to Ash Slough during the 25 year design storm. Increased flow to Ash Slough would aggravate downstream landowners' drainage problems, unless the slough could handle the additional flow, a question which the application does not address. The foregoing findings of fact should be read in conjunction with the statement required by Stuckey's of Eastman, Georgia v. Department of Transportation, 34O So.2d 119 (Fla. 1st DCA 1976), which is attached as an appendix to the recommended order.

Recommendation Upon consideration of the foregoing, it is RECOMMENDED: That SFWMD deny Coquina's application for construction permit. DONE and ENTERED this 14th day of November, 1978, in Tallahassee, Florida. ROBERT T. BENTON, II Hearing Officer Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304 (904) 488-9675 APPENDIX Paragraph one of intervening Bass petitioners' proposed findings of fact has been adopted, in substance, insofar as relevant, except that the evidence did not demonstrate that downstream landowners would in fact be harmed. Paragraphs two, three, four, five, six and seven of intervening Bass petitioners' proposed findings of fact have been adopted, in substance, insofar as relevant. Paragraph one of respondent Coquina's proposed findings of fact has been adopted, in substance, insofar as relevant, except for the date of the application. Paragraphs two, three, four, five, six, seven, eight, nine and thirteen of respondent Coquina's proposed findings of fact have been adopted in substance, insofar as relevant. Paragraph ten of respondent Coquina's proposed findings of fact stated a conclusion of law, in part. While "testimony was presented that the construction of Phase I would have no substantial adverse affect [sic] on surrounding properties," the evidence as a whole did not establish this fact. Paragraphs eleven and twelve of respondent Coquina's proposed findings of fact have not been adopted because they were not established by the evidence, except for subparagraph eleven (f), which was proven. COPIES FURNISHED: John Henry Wheeler, Esquire South Florida Water Management District Post Office Box V West Palm Beach, Florida 33402 Robert Birenbaum, President Viking Communities Corporation (Coquina Water Management District) 123 Northeast 70 Street Miami, Florida 33138 Kyle S. Van Landingham, Esquire County Attorney Okeechobee County Courthouse Okeechobee, Florida 33472 Andrew B. Jackson, Esquire J.C. Bass & Bass Ranch, Inc. Post Office Box 488 Lake Placid, Florida 33852 Emerson Allsworth, Esquire 1177 Southeast Third Avenue Ft. Lauderdale, Florida 33316 Mr. Bob Wittenberg Division of Florida Land Sales and Condominiums The Johns Building 725 South Bronough Street Tallahassee, Florida 32304 Dr. Patrick M. McCaffrey Kissimmee Coordinating Council 2600 Blair Stone Road Tallahassee, Florida 32301 Mr. George Stansbury Central Florida Regional Planning Council Post Office Box 2089 Bartow, Florida 33830

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