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HILLSBOROUGH COUNTY AND WASTE MANAGEMENT, INC., OF FLORIDA vs. DEPARTMENT OF ENVIRONMENTAL REGULATION, 80-002167 (1980)
Division of Administrative Hearings, Florida Number: 80-002167 Latest Update: Oct. 08, 1981

Findings Of Fact The site of the proposed landfill is located near Seffner, Florida, and is northwest of and adjacent to two previously used landfill sites. The proposed site meets all zoning requirements, is not located in the vicinity of an airport so as to be subject to Federal Aviation Administration regulations, and no natural or artificial body of water is located within 200 feet of the site. Inasmuch as the operation of the earlier used landfills created much of the opposition presented at this hearing, a short history of Hillsborough County's landfill operation follows. Hillsborough County opened the old Taylor Road landfill, a tract containing 42 acres, in 1976 and closed it in 1980 when it became full. The old Taylor Road landfill site abuts to the southeast the site being applied for it these proceedings. In 1977, pursuant to a consent decree between the City of Tampa and the Federal Environmental Protection Agency (petitioners' Exhibit 14) , the City of Tampa's incinerator, at which most of the solid waste in Hillsborough County was disposed, was ordered closed by 1979. The City of Tampa engaged consultants to locate an acceptable site for use as a sanitary landfill. In 1978, Hillsborough County, pursuant to an agreement with the City of Tampa (Petitioners' Exhibit 15), assumed the responsibility for solid waste disposal throughout Hillsborough County. Thereafter, it was determined that the best site, from an ecological point of view, was adjacent to the old Taylor Road landfill. Prior to obtaining DER approval to expand this site, the selection of which the County Commission approved in April 1979, time for closing the incinerator was running out and the County was given permission to utilize a 10.6 acre borrow pit, adjacent to and west of the old Taylor Road site, which bad been given to the County by the State Department of Transportation. This approval was given by DER in January 1980. When Hillsborough County assumed the responsibility for waste disposal throughout the County, waste from Temple Terrace and Plant City was added which waste had not been disposed of by the City of Tampa incinerator. The County entered into a contract with Waste Management Inc., a large company specializing in developing and operating waste disposal facilities in many parts of the United States and abroad, to design and operate Hillsborough Heights Sanitary Landfill. The 10.6 acre site would quickly be filled so it was necessary for the County to `reapply to DER for a permit to operate a landfill capable of serving the County until 1984. At that time, modification to the incinerator to comply with clean air standards and operate as an energy recovery unit will be complete and it can be restored to operation. Before that hearing was held the 10.6 acre site filled, and it became necessary for the County to request an emergency permit from DER to operate a landfill on part of the proposed site. Following a hearing on this request, DER issued an order in July 1980, authorizing Hillsborough County to operate a sanitary landfill on 41.5 acres adjacent to the old Taylor Road landfill and the 10.6 acre borrow pit site. By the application here under consideration, as modified by Stipulation and Settlement Agreement, the Petitioners are seeking to expand this 41.5 acre site to 64 acres, thereby adding 22.5 acres to the already approved site. Two thousand tons of solid waste are deposited at this site daily, six days a week. The primary concern respecting a sanitary landfill in the proposed location is the potential for pollution of the Floridan aquifer which underlies this site and the fact that the site is located in a karst area. Unless an impervious surface lies naturally or is constructed between the base of the proposed landfill and the Floridan aquifer, pollution of the aquifer could occur should leachate from the site accumulate and percolate to the aquifer. All of Hillsborough County and much of Florida is underlain by limestone containing karst features. One unfortunate characteristic of the karst formation is the potential for the limestone to dissolve thereby creating cavities into which the surface overburden falls to create a sinkhole. Some liquids, including leachate, will dissolve limestone, thereby creating cavities into which the overburden can fall. This risk is reduced by the thickness of the clay layer over the limerock which inhibits the entry of surface water into the aquifer. The proposed site has a basal clay from five feet to twenty feet thick above the limerock. However, this base clay is not believed to be continuous throughout the site to this minimum thickness due to sand columns, pinnacles and other anomalies that have formed. Petitioners propose to remove some 35 to 45 feet of the overlying sand and intermediate clay down to the base clay to form the pit into which waste will be deposited. The thickness of this base clay over the limerock will then be tested. If at least five feet of clay is not over the limestone, Petitioners will install a minimum of five feet of recompacted clay liner with a density of at least 2.5 - X 10 (to the seventh power) cm/sec. over the bottom of the landfill. Impervious sidewalls around the edges of the landfill will be constructed of either a minimum of five feet of compacted lay or of Hypalon, a synthetic sidewall liner material, in accordance with the Stipulation Agreement. If Hypalon is used, it will be covered with at least two feet of soil before waste is put in the landfill. Petitioners will install a leachate collection system for monitoring and removing, if necessary, leachate that may collect in the bottom of this landfill. Perimeter ditches will be constructed around the bottom of the landfill with the floor of the landfill sloped toward the perimeter ditches. These ditches will contain perforated pipe to conduct leachate to sumps from which the leachate can be removed. Should leachate be generated before the landfill is closed, the leachate will be extracted by pumping; and discharged for absorption by solid waste at the landfill, or trucked to a treatment plant for processing. After each day's operations at this landfill, at least six inches of soil will be placed over the compacted solid waste accepted that day. This should provide reasonable protection for rodents and insects. Final soil coverage to be used as a top liner for this landfill will consist of at least eighteen inches of compacted clayey soil overlain by six inches of loosely compacted soil in order to provide a final cover to minimize infiltration of surface water runoff. The final surface of the landfill will be graded and sloped so rainfall will not puddle on the landfill but run off to the perimeter of the landfill. Thus, when completed, the deposited waste will be encased in a relatively impermeable container on all surfaces. Perimeter ditches will be installed to keep surface waters out of the landfill, and these ditches will be lined with 18 inches of clay to inhibit seepage of water to the landfill from these ditches. The ditches will discharge into holding ponds located south and southwest of the site. Surface waters in this vicinity flow south to southwesterly. Access to the landfill will be controlled by a perimeter fence and entry gate which will be manned during all hours of operation and locked when not manned. Disposal of hazardous or infectious waste will not be allowed. Spotters will be stationed at the dump site to inspect waste entering the site and to detect any hazardous or infectious waste that may reach the landfill. Household wastes will be accepted and these may include small quantities of paints, insecticides and other material that in large quantities would be considered hazardous. Litter will be controlled by temporary fencing or portable litter fences. Bare limestone exposed by excavation will be protected from flow of water from the active landfill area by berms until such time as the limestone is covered by the five feet of compacted base clay. During excavation of the landfill, a geologist or hydrologist will be stationed at the site by the operator of the landfill to determine the nature and extent of earth materials encountered. Anomalies found during excavation will be recorded and reported. This will serve to insure the impervious five feet clay base between the landfill and the limestone. Methane gas control will be provided by the base clay underlying the landfill, the liners to be constructed around the landfill perimeter, and the clay soil cover. Rising gas will vent through the soil cover. If odor problems occur, gas vents will be installed at the high point of the landfill to provide a controlled path for these gases which can then be flared. Groundwater monitoring wells will be installed around the perimeter of the site to detect any leachate which may escape. Wells upgrade of the site will be installed to determined whether metals or other impurities detected in the downgrade monitoring wells come from the landfill or are in the groundwater before it gets to the landfill. The geology of the site is complex. Numerous test borings have been taken in the 218.6 acre tract, sinkholes in the area have been studied, special photographs of the site have been taken to show where changes and moisture in soil occur as well as other geologic features. All available information shows the 64 acre parcel in the southern part of the 218.6 acre site to be the safest in the site from a catastrophic subsidence (sinkhole) Although the Intervenors contend that the site is subject to sinkholes, no credible evidence was presented that this site is more subject to a catastrophic subsidence than is the remainder of Hillsborough County. Competent evidence was presented that a sinkhole is less likely to develop at the proposed 64 acre site than in other areas of Hillsborough County. Intervenors' and the public witnesses' primary complaint and vehement opposition to the granting of the permit here requested stem largely from the manner in which the predecessor landfills in this area have been operated; and rightly so. Infectious waste has been dumped on the site on several occasions; inadequate daily cover has been provided; dogs have roamed the site; birds have been killed by insecticides dumped on the site; papers have blown over the site; surface waters from the site have been pumped outside the site in such a manner that well water could be contaminated; inadequate precautions have been taken to prevent rodent and insect infestation of the site; and unpleasant odors have emanated from the site. These complaints go to conditions that existed in the past; they are not necessarily harbingers of things to come. Hillsborough County's lease law should preclude dogs roaming the site. Strict adherence to the conditions of the permit will eliminate the vast majority of those complaints.

Florida Laws (1) 403.707
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ANGELO'S AGGREGATE MATERIALS, LTD., D/B/A ANGELO'S RECYCLED MATERIALS vs DEPARTMENT OF ENVIRONMENTAL PROTECTION, 09-001543 (2009)
Division of Administrative Hearings, Florida Filed:Temple Terrace, Florida Mar. 23, 2009 Number: 09-001543 Latest Update: Sep. 16, 2013

The Issue The issue to be determined in this proceeding is whether Angelo's Aggregate Materials, LTD ("Angelo's") is entitled to permits from the Department of Environmental Protection ("Department") to construct and operate a Class I landfill in Pasco County.

Findings Of Fact The Parties The Department is the state agency with the power and duty under chapter 403, Florida Statutes, to review and take action on applications for permits to construct and operate solid waste management facilities, including landfills. Angelo's is a Florida limited partnership authorized to conduct business under the name Angelo's Recycled Materials. Angelo's filed the permit applications which are the subject of this proceeding. Angelo's owns the property on which the proposed landfill would be constructed and operated. Crystal Springs Preserve is a Florida corporation that owns approximately 525 acres in Pasco County, Florida on which is located Crystal Springs, a second magnitude spring that flows into the Hillsborough River. The property is about 10 miles south of Angelo's proposed landfill site. Crystal Springs Preserve's primary business activities are selling spring water for bottling for human consumption and operating an environmental education center that focuses on Crystal Springs and the Hillsborough River. Crystal Springs Preserve hosts approximately 50,000 visitors annually at the environmental education center. Crystal Springs Preserve holds a water use permit which authorizes it to withdraw up to 756,893 gallons of water per day (annual average) from Crystal Springs for production of bottled water. The water is transported about three miles to a water bottling facility operated by Nestlé. Nestlé is a private corporation engaged in the business of bottling and selling spring water. Nestlé purchases spring water from Crystal Springs Preserve. Nestlé's "Zephyrhills Spring Water" brand is composed of approximately 90 percent Crystal Springs water and 10 percent Madison Blue Spring water. The only water treatment applied by Nestlé is filtering the water to remove gross contaminants and passing the water through ultraviolet light or ozone to kill any potential bacteria before bottling. Nestlé has established "norms" for its spring water and would not be able to use the water from Crystal Springs if its chemical composition varied significantly from the norms. WRB is a Florida corporation that owns 1,866 acres in Pasco County known as Boarshead Ranch. Boarshead Ranch is adjacent to the east and south of Angelo’s property and is approximately 3,000 feet from the proposed landfill at its closest point. Boarshead Ranch is currently being used for agricultural, recreational, residential, and conservation purposes, including wildlife management. Nearly all of Boarshead Ranch is subject to a conservation easement held by the Southwest Florida Water Management District (SWFWMD). The conservation easement allows WRB to continue agricultural operations. Numerous agricultural water wells are located on Boarshead Ranch. WRB holds a water use permit which authorizes the withdrawal of 820,000 gallons per day (gpd) (annual average) for a number of uses, including production of agricultural products, animal drinking water, and personal use. The City of Zephyrhills is located in Pasco County and is a municipal corporation. Zephyrhills' water service area encompasses Zephyrhills and portions of Pasco County. Zephyrhills owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Zephyrhills holds a water use permit which authorizes nine potable water supply wells with a combined withdrawal of 2.9 million gallons per day ("mgd") (annual average). Zephyrhills has two new production wells located about two miles southeast of the proposed landfill. The City of Tampa owns and operates the David L. Tippin Water Treatment Plant, the Hillsborough River dam, and the City of Tampa reservoir on the Hillsborough River. Flows from Crystal Springs make up a substantial amount of the water in the Hillsborough River, especially during drought conditions when the spring flow accounts for about 50 percent of the flow. The City of Tampa holds a water use permit which authorizes the withdrawal 82 mgd (annual average). The City of Tampa owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Carl Roth, Marvin Hall, and Louis Potenziano own property in Pasco County near the proposed landfill site. Roth's property is 3.5 miles west of the proposed landfill site; Hall's property is located approximately one mile southwest of the site; and Potenziano's property is 1.6 miles to the south/southeast of the site. Roth, Hall, and Potenziano have water wells on their properties. The record does not establish that John Floyd owns property in the area. Floyd and Associates, Inc., owns about 55 acres in the area and holds a water use permit authorizing the withdrawal of water for agricultural uses. The Stipulated Agreement On March 1, 2010, Angelo's filed with DOAH a "Stipulated Agreement" signed by all parties. The Stipulated Agreement states in relevant part: Angelo's shall provide a final design, revised complete permit application and site investigation (referred to jointly as "Revised Submittal") to DEP with copies to all Parties and DEP shall make a completeness determination prior to this proceeding being set for a new final hearing date. * * * Angelo's shall not revise its permit application or supporting information beyond the Revised Submittal prior to or during the final hearing except in response to issues raised by DEP. It appears that the Aligned Parties did not remember the Stipulated Agreement until the commencement of the final hearing. They did not object before then to any of the evidence which Angelo's had prepared or intended to prepare for hearing on the basis that it violated the terms of the Stipulated Agreement. At the commencement of the hearing, Nestlé argued that the Stipulated Agreement barred Angelo's from revising its application or presenting new support for its project at the final hearing. The Stipulated Agreement is unusual and the necessity for Angelo's to make any concessions to the Aligned Parties in order to obtain their agreement to an abeyance was not explained. Allowing an applicant time to amend a permit application is usually good cause for an abeyance. The Stipulated Agreement allowed Angelo's to continue to respond to issues raised by the Department. Angelo's contends that all of the evidence it presented at the final hearing qualifies as a response to issues raised by the Department. The Proposed Landfill Angelo's applied to construct and operate a Class I landfill with associated buildings and leachate holding tanks. Application No. 22913-001-SC/01 corresponds to the construction permit application and Application No. 22913-001-SO/01 corresponds to the operation permit application. A Class I landfill is a landfill authorized to receive Class I waste, which is solid waste from households and businesses. Class I waste does not include hazardous waste, yard waste, or construction and demolition debris. See Fla. Admin. Code R. 62-701.200(13) and (14). The proposed landfill would be approximately 30 acres in size. It is part of a 1,020-acre parcel owned by Angelo's that is west of County Road 35 and south of Enterprise Road in Pasco County. The site is currently leased for cattle grazing and hay and sod production. There are also spray fields, orange groves, and a pond on the 1,020-acre parcel. Angelo's would construct the landfill by first clearing the 30-acre site. It would then excavate and fill to create the design subgrade or floor of the landfill with slopes required for the liner system. The subgrade would be compacted with a vibratory roller. After the subgrade compaction, the grouting plan would be implemented. The grouting plan calls for grouting 39 subsurface locations on the site that have voids, loose soils, or other unstable characteristics. A liner system would be installed after the grouting is completed and the subgrade is finished. From the bottom upward, the liner system would begin with a 12-inch layer of clay, over which a reinforcement geotextile would be installed, followed by another 12-inch layer of clay. This reinforcement geotextile is in addition to the double liner system required by Department rule. Its purpose is to maintain the integrity of the liner system in the event that a sinkhole occurs beneath the landfill. Installed above the reinforcement geotextile and clay layer would be a 60-millimeter high-density polyethylene ("HDPE") geomembrane, followed by a HDPE drainage net. These last two components comprise the secondary leachate collection system. Above the HDPE drainage net would be the primary leachate collection system, consisting of another 60-millimeter HDPE geomembrane and HDPE drainage net, followed by a geotextile, then a 12-inch sand layer for drainage, and an additional 12-inch sand layer for protection against puncture of the HDPE liner. A 48-inch layer of selected waste, free of items that could puncture the liner, would be the first waste placed over the primary leachate collection system. "Leachate" is "liquid that has passed through or merged from solid waste and may contain soluble, suspended, or miscible materials." See Fla. Admin. Code R. 62-701.200(66). Leachate would be collected through a system of perforated pipes that empty into a sloping trench with a leachate collection pipe. The leachate collection pipe would run down the center of the landfill to the lowest point where a pump would send the collected leachate through a force main 0.25 miles to storage tanks. Five above-ground storage tanks would be installed on a concrete pad with capacity to store 90,000 gallons of leachate. The stored leachate would be periodically transported to an offsite location, such as a wastewater treatment facility, for disposal. Sinkholes and Karst The terms "sinkhole" and "sinkhole activity" are not defined by Department rule, but the statutory definitions in chapter 627, a chapter dealing with insurance coverage for homes and other buildings, are generally consistent with the scientific meanings of these terms. The term "sinkhole" is defined in section 627.706(2)(h) as: a landform created by subsidence of soil, sediment, or rock as underlying strata are dissolved by groundwater. A sinkhole forms by collapse into subterranean voids created by dissolution of limestone or dolostone or by subsidence as these strata are dissolved. The term "sinkhole activity" is defined in section 627.706(2)(i) as: settlement or systematic weakening of the earth supporting the covered building only if the settlement or systematic weakening results from contemporaneous movement or raveling of soils, sediments, or rock materials into subterranean voids created by the effect of water on a limestone or similar rock formation. Sinkholes occur throughout Florida. There have been many reported and confirmed sinkholes in Pasco County. The more common type of sinkhole that has occurred on the Brooksville Ridge is a "cover subsidence" sinkhole, which is caused by voids in the limestone and the downward movement--"raveling"--of overlying soils into the cavity. Eventually, the loss of soils in the raveling zone will propagate upward until the soils at the ground surface also move downward and a depression is formed at the surface. Cover subsidence sinkholes develop slowly and are usually small, less than ten feet in diameter. Less common are "cover collapse" sinkholes, which can form in a matter of days or hours as the result of the collapse of the "roof" of a dissolved cavity in the limestone. These sinkholes are usually large and deep. The occurrence of a sinkhole does not always mean that areas near the sinkhole are unstable. However, the occurrence of a sinkhole is reasonable cause for concern about the stability of nearby areas and a reasonable basis for the Department to require thorough geologic investigations. "Karst" refers to limestone that is undergoing dissolution and it is common in Florida. A sinkhole forms in karst. "Epikarst" is limestone that was weathered while exposed above sea level millions of years ago before being submerged again. It is generally softer and more permeable than unweathered limestone. "Paleokarst" refers to karst that is very old in geologic time. Paleosinks are old sinkhole features in the paleokarst. A paleosink may no longer be unstable because it has been filled in for thousands or millions of years. A "lineament," or a "photolineament," is a relatively straight line seen in the topography or aerial photographs of the ground surface in an area. It might be defined by soil color, sloughs, ponds, wetlands, or other land features that follow a linear path. Lineaments are sometimes, but not always, associated with subsurface fractures in the bedrock where one would expect to also find active karst, sinkholes, and relatively rapid groundwater flow. Even where there is no lineament, there can be fractures in limestone that, when extensive enough, will allow for "fractured," "preferential," or "conduit flow" of groundwater. Fractured flow can occur in a small area or may go on for miles. Springs in Florida are usually associated with fractured flow or conduit flow that allows groundwater to move through the aquifer a long distance relatively rapidly, in weeks rather than decades. Geotechnical Investigation The Department's rules require subsurface conditions to be explored and described, including soil stratigraphy, soft ground, lineaments, and unstable areas, but the rules do not require the application of any particular geologic testing technique. An applicant's testing program is primarily a function of the professional judgment of the applicant’s geologist in cooperation with Department staff. The amount of geological testing done by Angelo's during its initial testing was similar to what was done for recent landfill applications. Angelo's conducted additional testing to respond to Department concerns and to prepare for the final hearing in this case, making the total amount of testing at Angelo's proposed site more extensive than is usual for a proposed landfill. The geologic investigation conducted by Angelo's experts to determine subsurface features, including any sinkholes, employed several technologies. Split Spoon Penetrometer Test (SPT) or SPT borings were drilled with a drill rig that advances a split spoon sampler into the ground with a 140 pound hammer. The hammer is dropped 30 inches and the number of blows required to drive the sampler each successive 12 inches is referred to as the "N" value and indicates soil strength and density. The higher the N value, the denser the soil. When the material is so dense the drill rod cannot (essentially) be hammered deeper, the N value is shown as "R," which stands for "refusal." SPT Bore logs also note any observed "weight of hammer," "weight of rod," or "loss of circulation." These terms describe areas where the drilling encounters very soft material or voids. Weight of rod, for example, means the weight of the drilling rod, by itself, with no hammer blow, was enough to cause the rod to fall deeper through the soil or rock. Cone Penetrometer Test ("CPT") borings were also conducted. CPT borings are relatively shallow, performed with a hand-held rod and special tip that the operator pushes into the ground. The CPT equipment continuously measures and records tip resistance and sleeve resistance as the rod moves downward through soils. It is helpful in some applications, but is less precise in determining soil type, strength, and compressibility than SPT borings and cannot be used to explore deep zones. Ground penetrating radar ("GPR") studies were used. GPR equipment transmits pulses of radio frequency waves into the ground. The manner in which the radio waves are reflected indicates the types of soil and rock encountered. It can also detect cavities and other features that would suggest karst activity. When the GPR identifies geologic features of interest, they can be further investigated with SPT borings. Another investigative tool used by Angelo's was Multiple Electrode Resistivity ("MER"). MER uses a grid of wires and electrodes and the equipment interprets the resistivity of electrical signals transmitted through the subsurface. MER data can be displayed in a two dimensional or three dimensional format, depending on the software program that is used to process the data. Like GPR, MER is useful for indentifying geologic features of interest that can be further explored with SPT borings. However, GPR generally has good resolution only near the ground surface, while MER has good resolution to a depth of 100 feet. The Regional Geology The proposed site is in a geologic transition zone on the eastern flank of a regional, geological feature known as the Brooksville Ridge. It is a transition zone for both the Suwannee Limestone and Hawthorn Group. The Brooksville Ridge was formed when it was part of the coastline. In its geologic past, the Brooksville Ridge experienced sea level changes, weathering, erosion of sediments, and beach reworking. The general layering of geologic features on the Brooksville Ridge, from the top down, begins with topsoil and a layer of sand. Under the sand layer is the Hawthorn Group, an older geologic layer consisting of a heterogeneous mix of limestone, clays, and sands which generally range in depth from slightly under 60 feet to 80 feet or more. It was formed by river and wind erosion, flushing, and re-deposition in a beach dune environment. Below the Hawthorn Group is the Suwannee Limestone Formation, which is present throughout eastern Pasco County. The upper surface of the Suwannee Limestone Formation is undulating, due to a gradual chemical weathering of its upper surface, representing a "paleokarst environment." Underlying the Suwannee Limestone Formation is the Ocala Limestone Formation. It extends throughout most of Florida. It is composed of nearly pure limestone and is considered the Floridan Aquifer. It extends across the site’s subsurface. Angelo's used the Florida Geologic Survey's data base to determine there are six sinkholes within five miles of the proposed landfill. A seventh sinkhole, not in the data base, is the 15- foot sinkhole at the Angelo's Enterprise Road Facility landfill, a Class III landfill (yard waste and construction and demolition debris) about a mile northwest of the proposed site. Angelo's contends that the sinkhole at its Class III landfill was "induced" during construction of the facility by the diversion of stormwater runoff to an area where overburden had been removed. The average diameter of the seven sinkholes is 11.9 feet. The Geology of the Proposed Site Rule 62-701.410(2)(c) requires a geotechnical site investigation and report, which shall: Explore and describe subsurface conditions including soil stratigraphy and ground water table conditions; Explore and address the presence of muck, previously filled areas, soft ground, lineaments, and sinkholes; Evaluate and address fault areas, seismic impact zones, and unstable areas as described in 40 C.F.R. 258.13, 258.14 and 258.15; Include estimates of the average and maximum high ground water table across the site; and Include a foundation analysis to determine the ability of the foundation to support the loads and stresses imposed by the landfill. It may include geotechnical measures necessary to modify the foundation to accommodate the imposed loads and stresses. The foundation shall be analyzed for short-term, end of construction, and long-term stability and settlement conditions. Considering the existing or proposed subgrade conditions and the landfill geometry, analysis shall include: Foundation bearing capacity; Subgrade settlements, both total and differential; and Subgrade slope stability. Angelo's conducted a geotechnical site investigation, but it was not adequate, as discussed below and in sections I. and J. The proposed landfill site is geologically complex, having features that are discontinuous horizontally and vertically. The site has karst features or areas where the limestone has dissolved. There is a clay layer in some areas, but it is not continuous and its depth and thickness vary. There are deposits of hard and soft sands at various depths. There are pinnacles of limestone surrounded by softer materials. Photographs from a quarry called the Vulcan Mine, located on the western flank of the Brooksville Ridge, show exposed features in the top 20 to 30 feet of the Suwannee Limestone in the region. The features at the Vulcan Mine are roughly similar to features at the Angelo's site. There are a number of shallow depressions on the surface of the ground on the Angelo's site. The origin and significance of these depressions was a matter of dispute. The Aligned Parties believe they represent sinkhole activity, but the evidence presented did not rise to the level of proof. However, Angelo's did not prove they were unassociated with geotechnical issues that could affect the proposed landfill. Angelo's offered no reasonable explanation for the depressions. Determining the exact cause of the depressions may not be possible even with more extensive investigation, but it was Angelo's responsibility as the permit applicant, pursuant to rule 62-701.410(2)(c), to make a greater effort to account for them. Angelo's initial permit application identified two intersecting lineaments on Angelo's property, based on aligned lowlands, enclosed valleys, and ponds. Angelo's contends the lineaments do not reflect an unstable subsurface or fractured limestone. The Aligned Parties contend that the lineaments are regional features and reflect fractures in the bedrock. They also contend that the onsite pond, which is located along the lineament, is an old sinkhole. The Aligned Parties did not prove the proposed landfill site is above an area of fractured bedrock, but the evidence presented by Angelo's was incomplete and insufficient to show there are no fractures. The limestone on the site was not adequately investigated for voids and fractures. Angelo's did not refute the possibility that the lineaments reflect a significant subsurface feature that could affect both site stability and groundwater movement. The Regional and Local Hydrogeology Rule 62-701.410(1) requires a hydrogeological investigation and site report, which shall: Define the landfill site geology and hydrology and its relationship to the local and regional hydrogeologic patterns including: Direction and rate of ground water and surface water flow, including seasonal variations; Background quality of ground water and surface water; Any on site hydraulic connections between aquifers; For all confining layers, semi-confining layers, and all aquifers below the landfill site that may be affected by the landfill, the porosity or effective porosity, horizontal and vertical permeabilities, and the depth to and lithology of the layers and aquifers; and Topography, soil types and characteristics, and surface water drainage systems of the site and surrounding the site. Include an inventory of all the public and private water wells within a one-mile radius of the proposed landfill site. The inventory shall include, where available: The approximate elevation of the top of the well casing and the depth of each well; The name of the owner, the age and usage of each well, and the estimated daily pumpage; and The stratigraphic unit screened, well construction technique, and static water levels of each well. Identify and locate any existing contaminated areas on the landfill site. Include a map showing the locations of all potable wells within 500 feet of the waste storage and disposal areas to demonstrate compliance with paragraph 62- 701.300(2)(b), F.A.C. Angelo's conducted a hydrogeological investigation, but it was not adequate, as discussed below. Angelo's and the Aligned Parties disputed the hydrogeological characteristics of the proposed landfill site and region. The principal disputes related to the direction and velocity of groundwater flow. Angelo's contends that groundwater flows from the landfill site to the west, making the proposed landfill site part of the Withlacoochee River groundwater basin. The Aligned Parties contend that groundwater flows south toward Crystal Springs and, therefore, the site is within the "springshed" of Crystal Springs. A United States Geological Survey map of the Crystal Springs springshed shows Angelo's proposed landfill site within the springshed. A springshed study done for SWFWMD also indicates the site is within the Crystal Springs springshed, but the District has not always been consistent in its statements about the groundwater basin boundaries in this area. A water chemistry analysis of the groundwater in the area of Angelo's proposed landfill indicates that the site is an area of higher recharge and within the Crystal Springs springshed. The springshed boundary can shift, depending on rainfall. Angelo's hydrogeological evidence was not sufficient to refute the reasonable possibility that the proposed landfill site is within the Crystal Springs springshed. Therefore, the Department's determination whether Angelo's has provided reasonable assurances must account for the threat of contamination to Crystal Springs and the other public and private water supply sources to the south. There are no creeks or streams and only a few lakes in the area between Crystal Springs and the Angelo's site. The absence of surface runoff features indicates it is an area of high recharge to the groundwater. Crystal Springs is in an area of conduit flow. The hydrologic investigation conducted by Angelo's was not thorough enough to characterize surficial aquifer flow and flow between aquifers. The preponderance of the evidence shows more groundwater recharge to the Floridan Aquifer in the area than estimated by Angelo's. Angelo's hydrogeological investigation was inadequate to refute the possibility of fractured flow or rapid groundwater movement at the proposed landfill site. Angelo's contends there is a continuous clay confining layer that would prevent contamination from moving into deep zones, but the preponderance of the evidence shows discontinuity in the clay and large variations in thickness and depth. The landfill's impermeable liner will impede water movement downward from the landfill, but groundwater will still recharge from outside the landfill to carry any contaminants deeper. If fractured flow or conduit flow extends south from the proposed landfill site, any leachate released into the groundwater beneath the landfill could travel rapidly toward the water supply sources of the City of Zephyrhills, Crystal Springs, Nestlé, and the City of Tampa. Whether the Proposed Landfill is in an Unstable Area Rule 62-701.200(2)(a) prohibits the storage or disposal of solid waste "[i]n an area where geological formations or other subsurface features will not provide support for the solid waste." However, the Department has adopted by reference a federal regulation, 40 C.F.R. 258.15, which allows a landfill to be constructed in a geologically unstable area if the permit applicant can demonstrate that engineering measures are incorporated into the design to ensure that the integrity of the landfill’s structural components "will not be disrupted." The parties presented evidence on many disputed issues of fact at the final hearing, but most of the case involved two ultimate questions: whether the proposed landfill site is unstable and, if so, whether Angelo's has proposed measures that would eliminate the unstable conditions and make the site suitable for a landfill. as: An "unstable area" is defined in 40 C.F.R. § 258.15 A location that is susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from a landfill. Unstable areas can include poor foundation conditions, areas susceptible to mass movements, and Karst terrains. There is overwhelming evidence that the proposed landfill site is an unstable area. A considerable amount of evidence presented by Angelo's supports this finding. For example, Angelo's experts agreed there are loose soils, evidence of raveling, and sinkhole activity. These conditions make the site susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from the proposed landfill. The Department's landfill permitting staff requested a sinkhole risk assessment from the Florida Geologic Survey ("FGS"). The State Geologist and Director of the FGS, Dr. Jonathan Arthur, believes the potential for sinkhole formation at the proposed site is moderately high to high. That potential is consistent with the characterization of the area as unstable. Whether the Proposed Engineering Measures Are Adequate Because the site is unstable, Angelo’s must demonstrate that engineering measures have been incorporated into the landfill's design to ensure that the integrity of its structural components will not be disrupted. See 40 C.F.R. § 258.15(a). The engineering measures proposed by Angelo's are discussed below. Because it was found that Angelo's hydrogeological and geotechnical investigations were not sufficient to characterize all potentially unstable features of the subsurface, it was not demonstrated that the proposed engineering measures would overcome the instability and make the site suitable for a landfill. Roller Compaction Angelo's would use roller compaction on the graded floor of the landfill to compact the soils to a depth of about five feet and eliminate any voids within that depth. The Aligned Parties did not contradict Angelo's evidence that its proposed roller compaction will be done in a manner exceeding what the Department usually requires as far as roller force and the number of roller "passes." However, roller compaction will not affect deep voids. Liner System In order to ensure that the landfill’s liner system components will not be disrupted in the event of a sinkhole, Angelo’s proposes to include the reinforcement geotextile discussed above. The Department previously approved the use of geotextile reinforcement, combined with grouting, to demonstrate site stability for the Hernando County Northwest Landfill, which had a comparable risk of sinkhole formation according to the Department. The reinforcement geotextile can span a 15-foot diameter sinkhole without failure. As found above, the average diameter of the seven sinkholes within five miles of the proposed landfill is 11.9 feet. Angelo's proved that the proposed liner system meets all applicable criteria, except the requirement of rule 62- 701.400(3)(a) that the liner be installed upon a geologically stable base. Grouting Plan Angelo's grouting plan would be implemented to fill voids and stabilize areas of loose or weak material. The grouting plan was first designed to grout all locations where there was a Weight of Hammer, Weight of Rod, Loss of Circulation, or loose sands, as indicated by a low blow count. Angelo's revised the grout plan to include several more areas of concern identified later, for a total of 39 locations. Each grout location would have seven grout points, one in the center and six others equally-spaced on a ten-foot radius from the center. If more than ten cubic yards of grout is needed, additional grout points further outward would be injected until the void or loose soils are filled or stabilized. Although Angelo's proposes to grout every boring of concern, that still ties the integrity of the grouting plan to the thoroughness of the borings. The geologic evidence indicates that there are unstable areas which the grouting plan does not address. The Aligned Parties' MER analysis was persuasive in identifying potential areas of instability that were omitted from Angelo's investigation and from its grouting plan. There are other unstable areas existing on the site that should be grouted or otherwise engineered to provide support for the landfill. The grouting plan does not provide reasonable assurance that the integrity of the structural components of the landfill will not be disturbed. Other Issues Raised by the Aligned Parties The Aligned Parties raise a number of other issues, some of which begin with the assumption that the site is unstable and a large sinkhole would form at the landfill. This sometimes mixes issues inappropriately. It has been found that Angelo's did not provide reasonable assurance that the site will support the proposed landfill, but other project elements must be reviewed on their own merits where possible, assuming the site was engineered for stability. Leachate Collection System There is a single leachate collection trench in the center of the two landfill cells, which makes the landfill operate much like a single cell. The two halves of the cell slope toward the center, so that leachate will drain to the leachate collection trench, and the entire landfill slopes to the west, so that the trench will drain to a sump from which the leachate is pumped to storage tanks. At full capacity, the landfill will generate about 40,000 gallons of leachate per day. Careful cutting and grading of the earth is necessary to create the slopes that are essential to the proper functioning of the project’s leachate collection system. Settlement analyses are necessary to assure that the slopes are maintained. Rule 62-701.410(2)(e) requires a foundation analysis which must include a study of "subgrade settlements, both total and differential." "Total settlement" refers to the overall settlement of a landfill after construction and the loading of solid waste. "Differential settlement" compares settlement at two different points. Angelo's did not meet its burden to provide reasonable assurance on this point. The settlement analysis conducted by Angelo's was amended two or three times during the course of the final hearing to account for computational errors and other issues raised by the Aligned Parties. The analysis never came completely into focus. The final analysis was not signed and sealed by a professional engineer. The settlement analysis is dependent on the geologic analysis, which is inadequate. Without adequate settlement and geologic analyses, it cannot be determined that leachate collection would meet applicable criteria. Storage Tanks The Aligned Parties contend that the leachate storage tanks cannot be supported by the site. Because it was found that Angelo's geologic investigation was not adequate to identify all unstable areas, it is also found that Angelo's failed to provide reasonable assurance that the site would support the leachate storage tanks. In all other respects, the Aligned Parties failed to refute Angelo's demonstration that the storage tanks would meet applicable criteria. Groundwater Monitoring Plan The Aligned Parties contend that there is an insufficient number of monitor wells proposed by Angelo's to detect a leak from the landfill and the wells are too shallow. Because it was found that Angelo's did not adequately characterize the geology and hydrology of the proposed landfill site, the monitoring plan does not provide reasonable assurance of compliance with applicable criteria. Cell Design The Aligned Parties contend that the "mega-cell" design proposed by Angelo's provides less flexibility to respond to and isolate landfill problems than other landfill designs with smaller cells, and the mega-cell design could generate more leakage. No evidence was presented to show whether Angelo's design was one that had been approved or rejected in the past by the Department. Although it is not the best landfill design, the Aligned Parties did not show that the proposed design violates any permitting criteria. Operation and Closure The evidence presented by the Aligned Parties in support of their issues regarding the operation of the proposed landfill, such as noise, odor, and traffic, was not sufficient to refute Angelo's evidence of compliance with applicable criteria, with one exception: Angelo's has not provided an adequate contingency plan to show how it would respond to a sinkhole or other incident that required the landfill to be shut down and repaired. Assuming the site was engineered to support the landfill, there is nothing about the Closure Plan that the Aligned Parties showed does not meet applicable criteria.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Environmental Protection deny Angelo's Permit Application Nos. 22913-001-SC/01 and 22913- 002-SO/01. DONE AND ENTERED this 28th day of June, 2013, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 28th day of June, 2013. COPIES FURNISHED: Carl Roth, Qualified Representative 8031 Island Drive Port Richey, Florida 34668-6220 Christopher M. Kise, Esquire Foley and Lardner, LLP 106 East College Avenue, Suite 900 Tallahassee, Florida 32301-7732 Wayne E. Flowers, Esquire Lewis, Longman and Walker, P.A. Suite 150 245 Riverside Avenue Jacksonville, Florida 32202-4931 Janice M. McLean, Esquire City of Tampa 7th Floor 315 East Kennedy Boulevard Tampa, Florida 33602-5211 Joseph A. Poblick, Esquire City of Zephyrhills 5335 8th Street Zephyrhills, Florida 33542-4312 Doug Manson, Esquire William Bilenky, Esquire Brian A. Bolves, Esquire Manson Bolves, P.A. 1101 West Swann Avenue Tampa, Florida 33606-2637 Jacob D. Varn, Esquire Linda Loomis Shelley, Esquire Karen A. Brodeen, Esquire Fowler, White, Boggs, P.A. 101 North Monroe Street, Suite 1090 Tallahassee, Florida 32302-1547 David Smolker, Esquire Smolker, Bartlett, Schlosser, Loeb and Hinds, P.A. Suite 200 500 East Kennedy Boulevard Tampa, Florida 33602-4936 Stanley Warden, Esquire Christopher Dale McGuire, Esquire Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 William D. Preston, Esquire William D. Preston, P.A. 4832-A Kerry Forest Parkway Tallahassee, Florida 32309-2272 Herschel T. Vinyard, Jr., Secretary Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Matthew Z. Leopold, General Counsel Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Lea Crandall, Agency Clerk Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000

CFR (6) 0 CFR 25840 CFR 25840 CFR 258.1340 CFR 258.1440 CFR 258.1540 CFR 258.15(a) Florida Laws (6) 120.52120.57120.68258.15403.707627.706 Florida Administrative Code (6) 62-701.20062-701.22062-701.32062-701.34062-701.40062-701.410
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CARL ROTH, JOHN FLOYD, LOUIS POTENZIANO, AND MARVIN HILL vs ANGELO`S AGGREGATE MATERIALS, LTD., D/B/A ANGELO`S RECYCLED MATERIALS AND DEPARTMENT OF ENVIRONMENTAL PROTECTION, 09-001544 (2009)
Division of Administrative Hearings, Florida Filed:Temple Terrace, Florida Mar. 23, 2009 Number: 09-001544 Latest Update: Sep. 16, 2013

The Issue The issue to be determined in this proceeding is whether Angelo's Aggregate Materials, LTD ("Angelo's") is entitled to permits from the Department of Environmental Protection ("Department") to construct and operate a Class I landfill in Pasco County.

Findings Of Fact The Parties The Department is the state agency with the power and duty under chapter 403, Florida Statutes, to review and take action on applications for permits to construct and operate solid waste management facilities, including landfills. Angelo's is a Florida limited partnership authorized to conduct business under the name Angelo's Recycled Materials. Angelo's filed the permit applications which are the subject of this proceeding. Angelo's owns the property on which the proposed landfill would be constructed and operated. Crystal Springs Preserve is a Florida corporation that owns approximately 525 acres in Pasco County, Florida on which is located Crystal Springs, a second magnitude spring that flows into the Hillsborough River. The property is about 10 miles south of Angelo's proposed landfill site. Crystal Springs Preserve's primary business activities are selling spring water for bottling for human consumption and operating an environmental education center that focuses on Crystal Springs and the Hillsborough River. Crystal Springs Preserve hosts approximately 50,000 visitors annually at the environmental education center. Crystal Springs Preserve holds a water use permit which authorizes it to withdraw up to 756,893 gallons of water per day (annual average) from Crystal Springs for production of bottled water. The water is transported about three miles to a water bottling facility operated by Nestlé. Nestlé is a private corporation engaged in the business of bottling and selling spring water. Nestlé purchases spring water from Crystal Springs Preserve. Nestlé's "Zephyrhills Spring Water" brand is composed of approximately 90 percent Crystal Springs water and 10 percent Madison Blue Spring water. The only water treatment applied by Nestlé is filtering the water to remove gross contaminants and passing the water through ultraviolet light or ozone to kill any potential bacteria before bottling. Nestlé has established "norms" for its spring water and would not be able to use the water from Crystal Springs if its chemical composition varied significantly from the norms. WRB is a Florida corporation that owns 1,866 acres in Pasco County known as Boarshead Ranch. Boarshead Ranch is adjacent to the east and south of Angelo’s property and is approximately 3,000 feet from the proposed landfill at its closest point. Boarshead Ranch is currently being used for agricultural, recreational, residential, and conservation purposes, including wildlife management. Nearly all of Boarshead Ranch is subject to a conservation easement held by the Southwest Florida Water Management District (SWFWMD). The conservation easement allows WRB to continue agricultural operations. Numerous agricultural water wells are located on Boarshead Ranch. WRB holds a water use permit which authorizes the withdrawal of 820,000 gallons per day (gpd) (annual average) for a number of uses, including production of agricultural products, animal drinking water, and personal use. The City of Zephyrhills is located in Pasco County and is a municipal corporation. Zephyrhills' water service area encompasses Zephyrhills and portions of Pasco County. Zephyrhills owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Zephyrhills holds a water use permit which authorizes nine potable water supply wells with a combined withdrawal of 2.9 million gallons per day ("mgd") (annual average). Zephyrhills has two new production wells located about two miles southeast of the proposed landfill. The City of Tampa owns and operates the David L. Tippin Water Treatment Plant, the Hillsborough River dam, and the City of Tampa reservoir on the Hillsborough River. Flows from Crystal Springs make up a substantial amount of the water in the Hillsborough River, especially during drought conditions when the spring flow accounts for about 50 percent of the flow. The City of Tampa holds a water use permit which authorizes the withdrawal 82 mgd (annual average). The City of Tampa owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Carl Roth, Marvin Hall, and Louis Potenziano own property in Pasco County near the proposed landfill site. Roth's property is 3.5 miles west of the proposed landfill site; Hall's property is located approximately one mile southwest of the site; and Potenziano's property is 1.6 miles to the south/southeast of the site. Roth, Hall, and Potenziano have water wells on their properties. The record does not establish that John Floyd owns property in the area. Floyd and Associates, Inc., owns about 55 acres in the area and holds a water use permit authorizing the withdrawal of water for agricultural uses. The Stipulated Agreement On March 1, 2010, Angelo's filed with DOAH a "Stipulated Agreement" signed by all parties. The Stipulated Agreement states in relevant part: Angelo's shall provide a final design, revised complete permit application and site investigation (referred to jointly as "Revised Submittal") to DEP with copies to all Parties and DEP shall make a completeness determination prior to this proceeding being set for a new final hearing date. * * * Angelo's shall not revise its permit application or supporting information beyond the Revised Submittal prior to or during the final hearing except in response to issues raised by DEP. It appears that the Aligned Parties did not remember the Stipulated Agreement until the commencement of the final hearing. They did not object before then to any of the evidence which Angelo's had prepared or intended to prepare for hearing on the basis that it violated the terms of the Stipulated Agreement. At the commencement of the hearing, Nestlé argued that the Stipulated Agreement barred Angelo's from revising its application or presenting new support for its project at the final hearing. The Stipulated Agreement is unusual and the necessity for Angelo's to make any concessions to the Aligned Parties in order to obtain their agreement to an abeyance was not explained. Allowing an applicant time to amend a permit application is usually good cause for an abeyance. The Stipulated Agreement allowed Angelo's to continue to respond to issues raised by the Department. Angelo's contends that all of the evidence it presented at the final hearing qualifies as a response to issues raised by the Department. The Proposed Landfill Angelo's applied to construct and operate a Class I landfill with associated buildings and leachate holding tanks. Application No. 22913-001-SC/01 corresponds to the construction permit application and Application No. 22913-001-SO/01 corresponds to the operation permit application. A Class I landfill is a landfill authorized to receive Class I waste, which is solid waste from households and businesses. Class I waste does not include hazardous waste, yard waste, or construction and demolition debris. See Fla. Admin. Code R. 62-701.200(13) and (14). The proposed landfill would be approximately 30 acres in size. It is part of a 1,020-acre parcel owned by Angelo's that is west of County Road 35 and south of Enterprise Road in Pasco County. The site is currently leased for cattle grazing and hay and sod production. There are also spray fields, orange groves, and a pond on the 1,020-acre parcel. Angelo's would construct the landfill by first clearing the 30-acre site. It would then excavate and fill to create the design subgrade or floor of the landfill with slopes required for the liner system. The subgrade would be compacted with a vibratory roller. After the subgrade compaction, the grouting plan would be implemented. The grouting plan calls for grouting 39 subsurface locations on the site that have voids, loose soils, or other unstable characteristics. A liner system would be installed after the grouting is completed and the subgrade is finished. From the bottom upward, the liner system would begin with a 12-inch layer of clay, over which a reinforcement geotextile would be installed, followed by another 12-inch layer of clay. This reinforcement geotextile is in addition to the double liner system required by Department rule. Its purpose is to maintain the integrity of the liner system in the event that a sinkhole occurs beneath the landfill. Installed above the reinforcement geotextile and clay layer would be a 60-millimeter high-density polyethylene ("HDPE") geomembrane, followed by a HDPE drainage net. These last two components comprise the secondary leachate collection system. Above the HDPE drainage net would be the primary leachate collection system, consisting of another 60-millimeter HDPE geomembrane and HDPE drainage net, followed by a geotextile, then a 12-inch sand layer for drainage, and an additional 12-inch sand layer for protection against puncture of the HDPE liner. A 48-inch layer of selected waste, free of items that could puncture the liner, would be the first waste placed over the primary leachate collection system. "Leachate" is "liquid that has passed through or merged from solid waste and may contain soluble, suspended, or miscible materials." See Fla. Admin. Code R. 62-701.200(66). Leachate would be collected through a system of perforated pipes that empty into a sloping trench with a leachate collection pipe. The leachate collection pipe would run down the center of the landfill to the lowest point where a pump would send the collected leachate through a force main 0.25 miles to storage tanks. Five above-ground storage tanks would be installed on a concrete pad with capacity to store 90,000 gallons of leachate. The stored leachate would be periodically transported to an offsite location, such as a wastewater treatment facility, for disposal. Sinkholes and Karst The terms "sinkhole" and "sinkhole activity" are not defined by Department rule, but the statutory definitions in chapter 627, a chapter dealing with insurance coverage for homes and other buildings, are generally consistent with the scientific meanings of these terms. The term "sinkhole" is defined in section 627.706(2)(h) as: a landform created by subsidence of soil, sediment, or rock as underlying strata are dissolved by groundwater. A sinkhole forms by collapse into subterranean voids created by dissolution of limestone or dolostone or by subsidence as these strata are dissolved. The term "sinkhole activity" is defined in section 627.706(2)(i) as: settlement or systematic weakening of the earth supporting the covered building only if the settlement or systematic weakening results from contemporaneous movement or raveling of soils, sediments, or rock materials into subterranean voids created by the effect of water on a limestone or similar rock formation. Sinkholes occur throughout Florida. There have been many reported and confirmed sinkholes in Pasco County. The more common type of sinkhole that has occurred on the Brooksville Ridge is a "cover subsidence" sinkhole, which is caused by voids in the limestone and the downward movement--"raveling"--of overlying soils into the cavity. Eventually, the loss of soils in the raveling zone will propagate upward until the soils at the ground surface also move downward and a depression is formed at the surface. Cover subsidence sinkholes develop slowly and are usually small, less than ten feet in diameter. Less common are "cover collapse" sinkholes, which can form in a matter of days or hours as the result of the collapse of the "roof" of a dissolved cavity in the limestone. These sinkholes are usually large and deep. The occurrence of a sinkhole does not always mean that areas near the sinkhole are unstable. However, the occurrence of a sinkhole is reasonable cause for concern about the stability of nearby areas and a reasonable basis for the Department to require thorough geologic investigations. "Karst" refers to limestone that is undergoing dissolution and it is common in Florida. A sinkhole forms in karst. "Epikarst" is limestone that was weathered while exposed above sea level millions of years ago before being submerged again. It is generally softer and more permeable than unweathered limestone. "Paleokarst" refers to karst that is very old in geologic time. Paleosinks are old sinkhole features in the paleokarst. A paleosink may no longer be unstable because it has been filled in for thousands or millions of years. A "lineament," or a "photolineament," is a relatively straight line seen in the topography or aerial photographs of the ground surface in an area. It might be defined by soil color, sloughs, ponds, wetlands, or other land features that follow a linear path. Lineaments are sometimes, but not always, associated with subsurface fractures in the bedrock where one would expect to also find active karst, sinkholes, and relatively rapid groundwater flow. Even where there is no lineament, there can be fractures in limestone that, when extensive enough, will allow for "fractured," "preferential," or "conduit flow" of groundwater. Fractured flow can occur in a small area or may go on for miles. Springs in Florida are usually associated with fractured flow or conduit flow that allows groundwater to move through the aquifer a long distance relatively rapidly, in weeks rather than decades. Geotechnical Investigation The Department's rules require subsurface conditions to be explored and described, including soil stratigraphy, soft ground, lineaments, and unstable areas, but the rules do not require the application of any particular geologic testing technique. An applicant's testing program is primarily a function of the professional judgment of the applicant’s geologist in cooperation with Department staff. The amount of geological testing done by Angelo's during its initial testing was similar to what was done for recent landfill applications. Angelo's conducted additional testing to respond to Department concerns and to prepare for the final hearing in this case, making the total amount of testing at Angelo's proposed site more extensive than is usual for a proposed landfill. The geologic investigation conducted by Angelo's experts to determine subsurface features, including any sinkholes, employed several technologies. Split Spoon Penetrometer Test (SPT) or SPT borings were drilled with a drill rig that advances a split spoon sampler into the ground with a 140 pound hammer. The hammer is dropped 30 inches and the number of blows required to drive the sampler each successive 12 inches is referred to as the "N" value and indicates soil strength and density. The higher the N value, the denser the soil. When the material is so dense the drill rod cannot (essentially) be hammered deeper, the N value is shown as "R," which stands for "refusal." SPT Bore logs also note any observed "weight of hammer," "weight of rod," or "loss of circulation." These terms describe areas where the drilling encounters very soft material or voids. Weight of rod, for example, means the weight of the drilling rod, by itself, with no hammer blow, was enough to cause the rod to fall deeper through the soil or rock. Cone Penetrometer Test ("CPT") borings were also conducted. CPT borings are relatively shallow, performed with a hand-held rod and special tip that the operator pushes into the ground. The CPT equipment continuously measures and records tip resistance and sleeve resistance as the rod moves downward through soils. It is helpful in some applications, but is less precise in determining soil type, strength, and compressibility than SPT borings and cannot be used to explore deep zones. Ground penetrating radar ("GPR") studies were used. GPR equipment transmits pulses of radio frequency waves into the ground. The manner in which the radio waves are reflected indicates the types of soil and rock encountered. It can also detect cavities and other features that would suggest karst activity. When the GPR identifies geologic features of interest, they can be further investigated with SPT borings. Another investigative tool used by Angelo's was Multiple Electrode Resistivity ("MER"). MER uses a grid of wires and electrodes and the equipment interprets the resistivity of electrical signals transmitted through the subsurface. MER data can be displayed in a two dimensional or three dimensional format, depending on the software program that is used to process the data. Like GPR, MER is useful for indentifying geologic features of interest that can be further explored with SPT borings. However, GPR generally has good resolution only near the ground surface, while MER has good resolution to a depth of 100 feet. The Regional Geology The proposed site is in a geologic transition zone on the eastern flank of a regional, geological feature known as the Brooksville Ridge. It is a transition zone for both the Suwannee Limestone and Hawthorn Group. The Brooksville Ridge was formed when it was part of the coastline. In its geologic past, the Brooksville Ridge experienced sea level changes, weathering, erosion of sediments, and beach reworking. The general layering of geologic features on the Brooksville Ridge, from the top down, begins with topsoil and a layer of sand. Under the sand layer is the Hawthorn Group, an older geologic layer consisting of a heterogeneous mix of limestone, clays, and sands which generally range in depth from slightly under 60 feet to 80 feet or more. It was formed by river and wind erosion, flushing, and re-deposition in a beach dune environment. Below the Hawthorn Group is the Suwannee Limestone Formation, which is present throughout eastern Pasco County. The upper surface of the Suwannee Limestone Formation is undulating, due to a gradual chemical weathering of its upper surface, representing a "paleokarst environment." Underlying the Suwannee Limestone Formation is the Ocala Limestone Formation. It extends throughout most of Florida. It is composed of nearly pure limestone and is considered the Floridan Aquifer. It extends across the site’s subsurface. Angelo's used the Florida Geologic Survey's data base to determine there are six sinkholes within five miles of the proposed landfill. A seventh sinkhole, not in the data base, is the 15- foot sinkhole at the Angelo's Enterprise Road Facility landfill, a Class III landfill (yard waste and construction and demolition debris) about a mile northwest of the proposed site. Angelo's contends that the sinkhole at its Class III landfill was "induced" during construction of the facility by the diversion of stormwater runoff to an area where overburden had been removed. The average diameter of the seven sinkholes is 11.9 feet. The Geology of the Proposed Site Rule 62-701.410(2)(c) requires a geotechnical site investigation and report, which shall: Explore and describe subsurface conditions including soil stratigraphy and ground water table conditions; Explore and address the presence of muck, previously filled areas, soft ground, lineaments, and sinkholes; Evaluate and address fault areas, seismic impact zones, and unstable areas as described in 40 C.F.R. 258.13, 258.14 and 258.15; Include estimates of the average and maximum high ground water table across the site; and Include a foundation analysis to determine the ability of the foundation to support the loads and stresses imposed by the landfill. It may include geotechnical measures necessary to modify the foundation to accommodate the imposed loads and stresses. The foundation shall be analyzed for short-term, end of construction, and long-term stability and settlement conditions. Considering the existing or proposed subgrade conditions and the landfill geometry, analysis shall include: Foundation bearing capacity; Subgrade settlements, both total and differential; and Subgrade slope stability. Angelo's conducted a geotechnical site investigation, but it was not adequate, as discussed below and in sections I. and J. The proposed landfill site is geologically complex, having features that are discontinuous horizontally and vertically. The site has karst features or areas where the limestone has dissolved. There is a clay layer in some areas, but it is not continuous and its depth and thickness vary. There are deposits of hard and soft sands at various depths. There are pinnacles of limestone surrounded by softer materials. Photographs from a quarry called the Vulcan Mine, located on the western flank of the Brooksville Ridge, show exposed features in the top 20 to 30 feet of the Suwannee Limestone in the region. The features at the Vulcan Mine are roughly similar to features at the Angelo's site. There are a number of shallow depressions on the surface of the ground on the Angelo's site. The origin and significance of these depressions was a matter of dispute. The Aligned Parties believe they represent sinkhole activity, but the evidence presented did not rise to the level of proof. However, Angelo's did not prove they were unassociated with geotechnical issues that could affect the proposed landfill. Angelo's offered no reasonable explanation for the depressions. Determining the exact cause of the depressions may not be possible even with more extensive investigation, but it was Angelo's responsibility as the permit applicant, pursuant to rule 62-701.410(2)(c), to make a greater effort to account for them. Angelo's initial permit application identified two intersecting lineaments on Angelo's property, based on aligned lowlands, enclosed valleys, and ponds. Angelo's contends the lineaments do not reflect an unstable subsurface or fractured limestone. The Aligned Parties contend that the lineaments are regional features and reflect fractures in the bedrock. They also contend that the onsite pond, which is located along the lineament, is an old sinkhole. The Aligned Parties did not prove the proposed landfill site is above an area of fractured bedrock, but the evidence presented by Angelo's was incomplete and insufficient to show there are no fractures. The limestone on the site was not adequately investigated for voids and fractures. Angelo's did not refute the possibility that the lineaments reflect a significant subsurface feature that could affect both site stability and groundwater movement. The Regional and Local Hydrogeology Rule 62-701.410(1) requires a hydrogeological investigation and site report, which shall: Define the landfill site geology and hydrology and its relationship to the local and regional hydrogeologic patterns including: Direction and rate of ground water and surface water flow, including seasonal variations; Background quality of ground water and surface water; Any on site hydraulic connections between aquifers; For all confining layers, semi-confining layers, and all aquifers below the landfill site that may be affected by the landfill, the porosity or effective porosity, horizontal and vertical permeabilities, and the depth to and lithology of the layers and aquifers; and Topography, soil types and characteristics, and surface water drainage systems of the site and surrounding the site. Include an inventory of all the public and private water wells within a one-mile radius of the proposed landfill site. The inventory shall include, where available: The approximate elevation of the top of the well casing and the depth of each well; The name of the owner, the age and usage of each well, and the estimated daily pumpage; and The stratigraphic unit screened, well construction technique, and static water levels of each well. Identify and locate any existing contaminated areas on the landfill site. Include a map showing the locations of all potable wells within 500 feet of the waste storage and disposal areas to demonstrate compliance with paragraph 62- 701.300(2)(b), F.A.C. Angelo's conducted a hydrogeological investigation, but it was not adequate, as discussed below. Angelo's and the Aligned Parties disputed the hydrogeological characteristics of the proposed landfill site and region. The principal disputes related to the direction and velocity of groundwater flow. Angelo's contends that groundwater flows from the landfill site to the west, making the proposed landfill site part of the Withlacoochee River groundwater basin. The Aligned Parties contend that groundwater flows south toward Crystal Springs and, therefore, the site is within the "springshed" of Crystal Springs. A United States Geological Survey map of the Crystal Springs springshed shows Angelo's proposed landfill site within the springshed. A springshed study done for SWFWMD also indicates the site is within the Crystal Springs springshed, but the District has not always been consistent in its statements about the groundwater basin boundaries in this area. A water chemistry analysis of the groundwater in the area of Angelo's proposed landfill indicates that the site is an area of higher recharge and within the Crystal Springs springshed. The springshed boundary can shift, depending on rainfall. Angelo's hydrogeological evidence was not sufficient to refute the reasonable possibility that the proposed landfill site is within the Crystal Springs springshed. Therefore, the Department's determination whether Angelo's has provided reasonable assurances must account for the threat of contamination to Crystal Springs and the other public and private water supply sources to the south. There are no creeks or streams and only a few lakes in the area between Crystal Springs and the Angelo's site. The absence of surface runoff features indicates it is an area of high recharge to the groundwater. Crystal Springs is in an area of conduit flow. The hydrologic investigation conducted by Angelo's was not thorough enough to characterize surficial aquifer flow and flow between aquifers. The preponderance of the evidence shows more groundwater recharge to the Floridan Aquifer in the area than estimated by Angelo's. Angelo's hydrogeological investigation was inadequate to refute the possibility of fractured flow or rapid groundwater movement at the proposed landfill site. Angelo's contends there is a continuous clay confining layer that would prevent contamination from moving into deep zones, but the preponderance of the evidence shows discontinuity in the clay and large variations in thickness and depth. The landfill's impermeable liner will impede water movement downward from the landfill, but groundwater will still recharge from outside the landfill to carry any contaminants deeper. If fractured flow or conduit flow extends south from the proposed landfill site, any leachate released into the groundwater beneath the landfill could travel rapidly toward the water supply sources of the City of Zephyrhills, Crystal Springs, Nestlé, and the City of Tampa. Whether the Proposed Landfill is in an Unstable Area Rule 62-701.200(2)(a) prohibits the storage or disposal of solid waste "[i]n an area where geological formations or other subsurface features will not provide support for the solid waste." However, the Department has adopted by reference a federal regulation, 40 C.F.R. 258.15, which allows a landfill to be constructed in a geologically unstable area if the permit applicant can demonstrate that engineering measures are incorporated into the design to ensure that the integrity of the landfill’s structural components "will not be disrupted." The parties presented evidence on many disputed issues of fact at the final hearing, but most of the case involved two ultimate questions: whether the proposed landfill site is unstable and, if so, whether Angelo's has proposed measures that would eliminate the unstable conditions and make the site suitable for a landfill. as: An "unstable area" is defined in 40 C.F.R. § 258.15 A location that is susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from a landfill. Unstable areas can include poor foundation conditions, areas susceptible to mass movements, and Karst terrains. There is overwhelming evidence that the proposed landfill site is an unstable area. A considerable amount of evidence presented by Angelo's supports this finding. For example, Angelo's experts agreed there are loose soils, evidence of raveling, and sinkhole activity. These conditions make the site susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from the proposed landfill. The Department's landfill permitting staff requested a sinkhole risk assessment from the Florida Geologic Survey ("FGS"). The State Geologist and Director of the FGS, Dr. Jonathan Arthur, believes the potential for sinkhole formation at the proposed site is moderately high to high. That potential is consistent with the characterization of the area as unstable. Whether the Proposed Engineering Measures Are Adequate Because the site is unstable, Angelo’s must demonstrate that engineering measures have been incorporated into the landfill's design to ensure that the integrity of its structural components will not be disrupted. See 40 C.F.R. § 258.15(a). The engineering measures proposed by Angelo's are discussed below. Because it was found that Angelo's hydrogeological and geotechnical investigations were not sufficient to characterize all potentially unstable features of the subsurface, it was not demonstrated that the proposed engineering measures would overcome the instability and make the site suitable for a landfill. Roller Compaction Angelo's would use roller compaction on the graded floor of the landfill to compact the soils to a depth of about five feet and eliminate any voids within that depth. The Aligned Parties did not contradict Angelo's evidence that its proposed roller compaction will be done in a manner exceeding what the Department usually requires as far as roller force and the number of roller "passes." However, roller compaction will not affect deep voids. Liner System In order to ensure that the landfill’s liner system components will not be disrupted in the event of a sinkhole, Angelo’s proposes to include the reinforcement geotextile discussed above. The Department previously approved the use of geotextile reinforcement, combined with grouting, to demonstrate site stability for the Hernando County Northwest Landfill, which had a comparable risk of sinkhole formation according to the Department. The reinforcement geotextile can span a 15-foot diameter sinkhole without failure. As found above, the average diameter of the seven sinkholes within five miles of the proposed landfill is 11.9 feet. Angelo's proved that the proposed liner system meets all applicable criteria, except the requirement of rule 62- 701.400(3)(a) that the liner be installed upon a geologically stable base. Grouting Plan Angelo's grouting plan would be implemented to fill voids and stabilize areas of loose or weak material. The grouting plan was first designed to grout all locations where there was a Weight of Hammer, Weight of Rod, Loss of Circulation, or loose sands, as indicated by a low blow count. Angelo's revised the grout plan to include several more areas of concern identified later, for a total of 39 locations. Each grout location would have seven grout points, one in the center and six others equally-spaced on a ten-foot radius from the center. If more than ten cubic yards of grout is needed, additional grout points further outward would be injected until the void or loose soils are filled or stabilized. Although Angelo's proposes to grout every boring of concern, that still ties the integrity of the grouting plan to the thoroughness of the borings. The geologic evidence indicates that there are unstable areas which the grouting plan does not address. The Aligned Parties' MER analysis was persuasive in identifying potential areas of instability that were omitted from Angelo's investigation and from its grouting plan. There are other unstable areas existing on the site that should be grouted or otherwise engineered to provide support for the landfill. The grouting plan does not provide reasonable assurance that the integrity of the structural components of the landfill will not be disturbed. Other Issues Raised by the Aligned Parties The Aligned Parties raise a number of other issues, some of which begin with the assumption that the site is unstable and a large sinkhole would form at the landfill. This sometimes mixes issues inappropriately. It has been found that Angelo's did not provide reasonable assurance that the site will support the proposed landfill, but other project elements must be reviewed on their own merits where possible, assuming the site was engineered for stability. Leachate Collection System There is a single leachate collection trench in the center of the two landfill cells, which makes the landfill operate much like a single cell. The two halves of the cell slope toward the center, so that leachate will drain to the leachate collection trench, and the entire landfill slopes to the west, so that the trench will drain to a sump from which the leachate is pumped to storage tanks. At full capacity, the landfill will generate about 40,000 gallons of leachate per day. Careful cutting and grading of the earth is necessary to create the slopes that are essential to the proper functioning of the project’s leachate collection system. Settlement analyses are necessary to assure that the slopes are maintained. Rule 62-701.410(2)(e) requires a foundation analysis which must include a study of "subgrade settlements, both total and differential." "Total settlement" refers to the overall settlement of a landfill after construction and the loading of solid waste. "Differential settlement" compares settlement at two different points. Angelo's did not meet its burden to provide reasonable assurance on this point. The settlement analysis conducted by Angelo's was amended two or three times during the course of the final hearing to account for computational errors and other issues raised by the Aligned Parties. The analysis never came completely into focus. The final analysis was not signed and sealed by a professional engineer. The settlement analysis is dependent on the geologic analysis, which is inadequate. Without adequate settlement and geologic analyses, it cannot be determined that leachate collection would meet applicable criteria. Storage Tanks The Aligned Parties contend that the leachate storage tanks cannot be supported by the site. Because it was found that Angelo's geologic investigation was not adequate to identify all unstable areas, it is also found that Angelo's failed to provide reasonable assurance that the site would support the leachate storage tanks. In all other respects, the Aligned Parties failed to refute Angelo's demonstration that the storage tanks would meet applicable criteria. Groundwater Monitoring Plan The Aligned Parties contend that there is an insufficient number of monitor wells proposed by Angelo's to detect a leak from the landfill and the wells are too shallow. Because it was found that Angelo's did not adequately characterize the geology and hydrology of the proposed landfill site, the monitoring plan does not provide reasonable assurance of compliance with applicable criteria. Cell Design The Aligned Parties contend that the "mega-cell" design proposed by Angelo's provides less flexibility to respond to and isolate landfill problems than other landfill designs with smaller cells, and the mega-cell design could generate more leakage. No evidence was presented to show whether Angelo's design was one that had been approved or rejected in the past by the Department. Although it is not the best landfill design, the Aligned Parties did not show that the proposed design violates any permitting criteria. Operation and Closure The evidence presented by the Aligned Parties in support of their issues regarding the operation of the proposed landfill, such as noise, odor, and traffic, was not sufficient to refute Angelo's evidence of compliance with applicable criteria, with one exception: Angelo's has not provided an adequate contingency plan to show how it would respond to a sinkhole or other incident that required the landfill to be shut down and repaired. Assuming the site was engineered to support the landfill, there is nothing about the Closure Plan that the Aligned Parties showed does not meet applicable criteria.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Environmental Protection deny Angelo's Permit Application Nos. 22913-001-SC/01 and 22913- 002-SO/01. DONE AND ENTERED this 28th day of June, 2013, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 28th day of June, 2013. COPIES FURNISHED: Carl Roth, Qualified Representative 8031 Island Drive Port Richey, Florida 34668-6220 Christopher M. Kise, Esquire Foley and Lardner, LLP 106 East College Avenue, Suite 900 Tallahassee, Florida 32301-7732 Wayne E. Flowers, Esquire Lewis, Longman and Walker, P.A. Suite 150 245 Riverside Avenue Jacksonville, Florida 32202-4931 Janice M. McLean, Esquire City of Tampa 7th Floor 315 East Kennedy Boulevard Tampa, Florida 33602-5211 Joseph A. Poblick, Esquire City of Zephyrhills 5335 8th Street Zephyrhills, Florida 33542-4312 Doug Manson, Esquire William Bilenky, Esquire Brian A. Bolves, Esquire Manson Bolves, P.A. 1101 West Swann Avenue Tampa, Florida 33606-2637 Jacob D. Varn, Esquire Linda Loomis Shelley, Esquire Karen A. Brodeen, Esquire Fowler, White, Boggs, P.A. 101 North Monroe Street, Suite 1090 Tallahassee, Florida 32302-1547 David Smolker, Esquire Smolker, Bartlett, Schlosser, Loeb and Hinds, P.A. Suite 200 500 East Kennedy Boulevard Tampa, Florida 33602-4936 Stanley Warden, Esquire Christopher Dale McGuire, Esquire Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 William D. Preston, Esquire William D. Preston, P.A. 4832-A Kerry Forest Parkway Tallahassee, Florida 32309-2272 Herschel T. Vinyard, Jr., Secretary Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Matthew Z. Leopold, General Counsel Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Lea Crandall, Agency Clerk Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000

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NESTLE WATERS NORTH AMERICA, INC. vs ANGELO`S AGGREGATE MATERIALS, LTD., D/B/A ANGELO`S RECYCLED MATERIALS AND DEPARTMENT OF ENVIRONMENTAL PROTECTION, 09-001546 (2009)
Division of Administrative Hearings, Florida Filed:Temple Terrace, Florida Mar. 23, 2009 Number: 09-001546 Latest Update: Sep. 16, 2013

The Issue The issue to be determined in this proceeding is whether Angelo's Aggregate Materials, LTD ("Angelo's") is entitled to permits from the Department of Environmental Protection ("Department") to construct and operate a Class I landfill in Pasco County.

Findings Of Fact The Parties The Department is the state agency with the power and duty under chapter 403, Florida Statutes, to review and take action on applications for permits to construct and operate solid waste management facilities, including landfills. Angelo's is a Florida limited partnership authorized to conduct business under the name Angelo's Recycled Materials. Angelo's filed the permit applications which are the subject of this proceeding. Angelo's owns the property on which the proposed landfill would be constructed and operated. Crystal Springs Preserve is a Florida corporation that owns approximately 525 acres in Pasco County, Florida on which is located Crystal Springs, a second magnitude spring that flows into the Hillsborough River. The property is about 10 miles south of Angelo's proposed landfill site. Crystal Springs Preserve's primary business activities are selling spring water for bottling for human consumption and operating an environmental education center that focuses on Crystal Springs and the Hillsborough River. Crystal Springs Preserve hosts approximately 50,000 visitors annually at the environmental education center. Crystal Springs Preserve holds a water use permit which authorizes it to withdraw up to 756,893 gallons of water per day (annual average) from Crystal Springs for production of bottled water. The water is transported about three miles to a water bottling facility operated by Nestlé. Nestlé is a private corporation engaged in the business of bottling and selling spring water. Nestlé purchases spring water from Crystal Springs Preserve. Nestlé's "Zephyrhills Spring Water" brand is composed of approximately 90 percent Crystal Springs water and 10 percent Madison Blue Spring water. The only water treatment applied by Nestlé is filtering the water to remove gross contaminants and passing the water through ultraviolet light or ozone to kill any potential bacteria before bottling. Nestlé has established "norms" for its spring water and would not be able to use the water from Crystal Springs if its chemical composition varied significantly from the norms. WRB is a Florida corporation that owns 1,866 acres in Pasco County known as Boarshead Ranch. Boarshead Ranch is adjacent to the east and south of Angelo’s property and is approximately 3,000 feet from the proposed landfill at its closest point. Boarshead Ranch is currently being used for agricultural, recreational, residential, and conservation purposes, including wildlife management. Nearly all of Boarshead Ranch is subject to a conservation easement held by the Southwest Florida Water Management District (SWFWMD). The conservation easement allows WRB to continue agricultural operations. Numerous agricultural water wells are located on Boarshead Ranch. WRB holds a water use permit which authorizes the withdrawal of 820,000 gallons per day (gpd) (annual average) for a number of uses, including production of agricultural products, animal drinking water, and personal use. The City of Zephyrhills is located in Pasco County and is a municipal corporation. Zephyrhills' water service area encompasses Zephyrhills and portions of Pasco County. Zephyrhills owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Zephyrhills holds a water use permit which authorizes nine potable water supply wells with a combined withdrawal of 2.9 million gallons per day ("mgd") (annual average). Zephyrhills has two new production wells located about two miles southeast of the proposed landfill. The City of Tampa owns and operates the David L. Tippin Water Treatment Plant, the Hillsborough River dam, and the City of Tampa reservoir on the Hillsborough River. Flows from Crystal Springs make up a substantial amount of the water in the Hillsborough River, especially during drought conditions when the spring flow accounts for about 50 percent of the flow. The City of Tampa holds a water use permit which authorizes the withdrawal 82 mgd (annual average). The City of Tampa owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Carl Roth, Marvin Hall, and Louis Potenziano own property in Pasco County near the proposed landfill site. Roth's property is 3.5 miles west of the proposed landfill site; Hall's property is located approximately one mile southwest of the site; and Potenziano's property is 1.6 miles to the south/southeast of the site. Roth, Hall, and Potenziano have water wells on their properties. The record does not establish that John Floyd owns property in the area. Floyd and Associates, Inc., owns about 55 acres in the area and holds a water use permit authorizing the withdrawal of water for agricultural uses. The Stipulated Agreement On March 1, 2010, Angelo's filed with DOAH a "Stipulated Agreement" signed by all parties. The Stipulated Agreement states in relevant part: Angelo's shall provide a final design, revised complete permit application and site investigation (referred to jointly as "Revised Submittal") to DEP with copies to all Parties and DEP shall make a completeness determination prior to this proceeding being set for a new final hearing date. * * * Angelo's shall not revise its permit application or supporting information beyond the Revised Submittal prior to or during the final hearing except in response to issues raised by DEP. It appears that the Aligned Parties did not remember the Stipulated Agreement until the commencement of the final hearing. They did not object before then to any of the evidence which Angelo's had prepared or intended to prepare for hearing on the basis that it violated the terms of the Stipulated Agreement. At the commencement of the hearing, Nestlé argued that the Stipulated Agreement barred Angelo's from revising its application or presenting new support for its project at the final hearing. The Stipulated Agreement is unusual and the necessity for Angelo's to make any concessions to the Aligned Parties in order to obtain their agreement to an abeyance was not explained. Allowing an applicant time to amend a permit application is usually good cause for an abeyance. The Stipulated Agreement allowed Angelo's to continue to respond to issues raised by the Department. Angelo's contends that all of the evidence it presented at the final hearing qualifies as a response to issues raised by the Department. The Proposed Landfill Angelo's applied to construct and operate a Class I landfill with associated buildings and leachate holding tanks. Application No. 22913-001-SC/01 corresponds to the construction permit application and Application No. 22913-001-SO/01 corresponds to the operation permit application. A Class I landfill is a landfill authorized to receive Class I waste, which is solid waste from households and businesses. Class I waste does not include hazardous waste, yard waste, or construction and demolition debris. See Fla. Admin. Code R. 62-701.200(13) and (14). The proposed landfill would be approximately 30 acres in size. It is part of a 1,020-acre parcel owned by Angelo's that is west of County Road 35 and south of Enterprise Road in Pasco County. The site is currently leased for cattle grazing and hay and sod production. There are also spray fields, orange groves, and a pond on the 1,020-acre parcel. Angelo's would construct the landfill by first clearing the 30-acre site. It would then excavate and fill to create the design subgrade or floor of the landfill with slopes required for the liner system. The subgrade would be compacted with a vibratory roller. After the subgrade compaction, the grouting plan would be implemented. The grouting plan calls for grouting 39 subsurface locations on the site that have voids, loose soils, or other unstable characteristics. A liner system would be installed after the grouting is completed and the subgrade is finished. From the bottom upward, the liner system would begin with a 12-inch layer of clay, over which a reinforcement geotextile would be installed, followed by another 12-inch layer of clay. This reinforcement geotextile is in addition to the double liner system required by Department rule. Its purpose is to maintain the integrity of the liner system in the event that a sinkhole occurs beneath the landfill. Installed above the reinforcement geotextile and clay layer would be a 60-millimeter high-density polyethylene ("HDPE") geomembrane, followed by a HDPE drainage net. These last two components comprise the secondary leachate collection system. Above the HDPE drainage net would be the primary leachate collection system, consisting of another 60-millimeter HDPE geomembrane and HDPE drainage net, followed by a geotextile, then a 12-inch sand layer for drainage, and an additional 12-inch sand layer for protection against puncture of the HDPE liner. A 48-inch layer of selected waste, free of items that could puncture the liner, would be the first waste placed over the primary leachate collection system. "Leachate" is "liquid that has passed through or merged from solid waste and may contain soluble, suspended, or miscible materials." See Fla. Admin. Code R. 62-701.200(66). Leachate would be collected through a system of perforated pipes that empty into a sloping trench with a leachate collection pipe. The leachate collection pipe would run down the center of the landfill to the lowest point where a pump would send the collected leachate through a force main 0.25 miles to storage tanks. Five above-ground storage tanks would be installed on a concrete pad with capacity to store 90,000 gallons of leachate. The stored leachate would be periodically transported to an offsite location, such as a wastewater treatment facility, for disposal. Sinkholes and Karst The terms "sinkhole" and "sinkhole activity" are not defined by Department rule, but the statutory definitions in chapter 627, a chapter dealing with insurance coverage for homes and other buildings, are generally consistent with the scientific meanings of these terms. The term "sinkhole" is defined in section 627.706(2)(h) as: a landform created by subsidence of soil, sediment, or rock as underlying strata are dissolved by groundwater. A sinkhole forms by collapse into subterranean voids created by dissolution of limestone or dolostone or by subsidence as these strata are dissolved. The term "sinkhole activity" is defined in section 627.706(2)(i) as: settlement or systematic weakening of the earth supporting the covered building only if the settlement or systematic weakening results from contemporaneous movement or raveling of soils, sediments, or rock materials into subterranean voids created by the effect of water on a limestone or similar rock formation. Sinkholes occur throughout Florida. There have been many reported and confirmed sinkholes in Pasco County. The more common type of sinkhole that has occurred on the Brooksville Ridge is a "cover subsidence" sinkhole, which is caused by voids in the limestone and the downward movement--"raveling"--of overlying soils into the cavity. Eventually, the loss of soils in the raveling zone will propagate upward until the soils at the ground surface also move downward and a depression is formed at the surface. Cover subsidence sinkholes develop slowly and are usually small, less than ten feet in diameter. Less common are "cover collapse" sinkholes, which can form in a matter of days or hours as the result of the collapse of the "roof" of a dissolved cavity in the limestone. These sinkholes are usually large and deep. The occurrence of a sinkhole does not always mean that areas near the sinkhole are unstable. However, the occurrence of a sinkhole is reasonable cause for concern about the stability of nearby areas and a reasonable basis for the Department to require thorough geologic investigations. "Karst" refers to limestone that is undergoing dissolution and it is common in Florida. A sinkhole forms in karst. "Epikarst" is limestone that was weathered while exposed above sea level millions of years ago before being submerged again. It is generally softer and more permeable than unweathered limestone. "Paleokarst" refers to karst that is very old in geologic time. Paleosinks are old sinkhole features in the paleokarst. A paleosink may no longer be unstable because it has been filled in for thousands or millions of years. A "lineament," or a "photolineament," is a relatively straight line seen in the topography or aerial photographs of the ground surface in an area. It might be defined by soil color, sloughs, ponds, wetlands, or other land features that follow a linear path. Lineaments are sometimes, but not always, associated with subsurface fractures in the bedrock where one would expect to also find active karst, sinkholes, and relatively rapid groundwater flow. Even where there is no lineament, there can be fractures in limestone that, when extensive enough, will allow for "fractured," "preferential," or "conduit flow" of groundwater. Fractured flow can occur in a small area or may go on for miles. Springs in Florida are usually associated with fractured flow or conduit flow that allows groundwater to move through the aquifer a long distance relatively rapidly, in weeks rather than decades. Geotechnical Investigation The Department's rules require subsurface conditions to be explored and described, including soil stratigraphy, soft ground, lineaments, and unstable areas, but the rules do not require the application of any particular geologic testing technique. An applicant's testing program is primarily a function of the professional judgment of the applicant’s geologist in cooperation with Department staff. The amount of geological testing done by Angelo's during its initial testing was similar to what was done for recent landfill applications. Angelo's conducted additional testing to respond to Department concerns and to prepare for the final hearing in this case, making the total amount of testing at Angelo's proposed site more extensive than is usual for a proposed landfill. The geologic investigation conducted by Angelo's experts to determine subsurface features, including any sinkholes, employed several technologies. Split Spoon Penetrometer Test (SPT) or SPT borings were drilled with a drill rig that advances a split spoon sampler into the ground with a 140 pound hammer. The hammer is dropped 30 inches and the number of blows required to drive the sampler each successive 12 inches is referred to as the "N" value and indicates soil strength and density. The higher the N value, the denser the soil. When the material is so dense the drill rod cannot (essentially) be hammered deeper, the N value is shown as "R," which stands for "refusal." SPT Bore logs also note any observed "weight of hammer," "weight of rod," or "loss of circulation." These terms describe areas where the drilling encounters very soft material or voids. Weight of rod, for example, means the weight of the drilling rod, by itself, with no hammer blow, was enough to cause the rod to fall deeper through the soil or rock. Cone Penetrometer Test ("CPT") borings were also conducted. CPT borings are relatively shallow, performed with a hand-held rod and special tip that the operator pushes into the ground. The CPT equipment continuously measures and records tip resistance and sleeve resistance as the rod moves downward through soils. It is helpful in some applications, but is less precise in determining soil type, strength, and compressibility than SPT borings and cannot be used to explore deep zones. Ground penetrating radar ("GPR") studies were used. GPR equipment transmits pulses of radio frequency waves into the ground. The manner in which the radio waves are reflected indicates the types of soil and rock encountered. It can also detect cavities and other features that would suggest karst activity. When the GPR identifies geologic features of interest, they can be further investigated with SPT borings. Another investigative tool used by Angelo's was Multiple Electrode Resistivity ("MER"). MER uses a grid of wires and electrodes and the equipment interprets the resistivity of electrical signals transmitted through the subsurface. MER data can be displayed in a two dimensional or three dimensional format, depending on the software program that is used to process the data. Like GPR, MER is useful for indentifying geologic features of interest that can be further explored with SPT borings. However, GPR generally has good resolution only near the ground surface, while MER has good resolution to a depth of 100 feet. The Regional Geology The proposed site is in a geologic transition zone on the eastern flank of a regional, geological feature known as the Brooksville Ridge. It is a transition zone for both the Suwannee Limestone and Hawthorn Group. The Brooksville Ridge was formed when it was part of the coastline. In its geologic past, the Brooksville Ridge experienced sea level changes, weathering, erosion of sediments, and beach reworking. The general layering of geologic features on the Brooksville Ridge, from the top down, begins with topsoil and a layer of sand. Under the sand layer is the Hawthorn Group, an older geologic layer consisting of a heterogeneous mix of limestone, clays, and sands which generally range in depth from slightly under 60 feet to 80 feet or more. It was formed by river and wind erosion, flushing, and re-deposition in a beach dune environment. Below the Hawthorn Group is the Suwannee Limestone Formation, which is present throughout eastern Pasco County. The upper surface of the Suwannee Limestone Formation is undulating, due to a gradual chemical weathering of its upper surface, representing a "paleokarst environment." Underlying the Suwannee Limestone Formation is the Ocala Limestone Formation. It extends throughout most of Florida. It is composed of nearly pure limestone and is considered the Floridan Aquifer. It extends across the site’s subsurface. Angelo's used the Florida Geologic Survey's data base to determine there are six sinkholes within five miles of the proposed landfill. A seventh sinkhole, not in the data base, is the 15- foot sinkhole at the Angelo's Enterprise Road Facility landfill, a Class III landfill (yard waste and construction and demolition debris) about a mile northwest of the proposed site. Angelo's contends that the sinkhole at its Class III landfill was "induced" during construction of the facility by the diversion of stormwater runoff to an area where overburden had been removed. The average diameter of the seven sinkholes is 11.9 feet. The Geology of the Proposed Site Rule 62-701.410(2)(c) requires a geotechnical site investigation and report, which shall: Explore and describe subsurface conditions including soil stratigraphy and ground water table conditions; Explore and address the presence of muck, previously filled areas, soft ground, lineaments, and sinkholes; Evaluate and address fault areas, seismic impact zones, and unstable areas as described in 40 C.F.R. 258.13, 258.14 and 258.15; Include estimates of the average and maximum high ground water table across the site; and Include a foundation analysis to determine the ability of the foundation to support the loads and stresses imposed by the landfill. It may include geotechnical measures necessary to modify the foundation to accommodate the imposed loads and stresses. The foundation shall be analyzed for short-term, end of construction, and long-term stability and settlement conditions. Considering the existing or proposed subgrade conditions and the landfill geometry, analysis shall include: Foundation bearing capacity; Subgrade settlements, both total and differential; and Subgrade slope stability. Angelo's conducted a geotechnical site investigation, but it was not adequate, as discussed below and in sections I. and J. The proposed landfill site is geologically complex, having features that are discontinuous horizontally and vertically. The site has karst features or areas where the limestone has dissolved. There is a clay layer in some areas, but it is not continuous and its depth and thickness vary. There are deposits of hard and soft sands at various depths. There are pinnacles of limestone surrounded by softer materials. Photographs from a quarry called the Vulcan Mine, located on the western flank of the Brooksville Ridge, show exposed features in the top 20 to 30 feet of the Suwannee Limestone in the region. The features at the Vulcan Mine are roughly similar to features at the Angelo's site. There are a number of shallow depressions on the surface of the ground on the Angelo's site. The origin and significance of these depressions was a matter of dispute. The Aligned Parties believe they represent sinkhole activity, but the evidence presented did not rise to the level of proof. However, Angelo's did not prove they were unassociated with geotechnical issues that could affect the proposed landfill. Angelo's offered no reasonable explanation for the depressions. Determining the exact cause of the depressions may not be possible even with more extensive investigation, but it was Angelo's responsibility as the permit applicant, pursuant to rule 62-701.410(2)(c), to make a greater effort to account for them. Angelo's initial permit application identified two intersecting lineaments on Angelo's property, based on aligned lowlands, enclosed valleys, and ponds. Angelo's contends the lineaments do not reflect an unstable subsurface or fractured limestone. The Aligned Parties contend that the lineaments are regional features and reflect fractures in the bedrock. They also contend that the onsite pond, which is located along the lineament, is an old sinkhole. The Aligned Parties did not prove the proposed landfill site is above an area of fractured bedrock, but the evidence presented by Angelo's was incomplete and insufficient to show there are no fractures. The limestone on the site was not adequately investigated for voids and fractures. Angelo's did not refute the possibility that the lineaments reflect a significant subsurface feature that could affect both site stability and groundwater movement. The Regional and Local Hydrogeology Rule 62-701.410(1) requires a hydrogeological investigation and site report, which shall: Define the landfill site geology and hydrology and its relationship to the local and regional hydrogeologic patterns including: Direction and rate of ground water and surface water flow, including seasonal variations; Background quality of ground water and surface water; Any on site hydraulic connections between aquifers; For all confining layers, semi-confining layers, and all aquifers below the landfill site that may be affected by the landfill, the porosity or effective porosity, horizontal and vertical permeabilities, and the depth to and lithology of the layers and aquifers; and Topography, soil types and characteristics, and surface water drainage systems of the site and surrounding the site. Include an inventory of all the public and private water wells within a one-mile radius of the proposed landfill site. The inventory shall include, where available: The approximate elevation of the top of the well casing and the depth of each well; The name of the owner, the age and usage of each well, and the estimated daily pumpage; and The stratigraphic unit screened, well construction technique, and static water levels of each well. Identify and locate any existing contaminated areas on the landfill site. Include a map showing the locations of all potable wells within 500 feet of the waste storage and disposal areas to demonstrate compliance with paragraph 62- 701.300(2)(b), F.A.C. Angelo's conducted a hydrogeological investigation, but it was not adequate, as discussed below. Angelo's and the Aligned Parties disputed the hydrogeological characteristics of the proposed landfill site and region. The principal disputes related to the direction and velocity of groundwater flow. Angelo's contends that groundwater flows from the landfill site to the west, making the proposed landfill site part of the Withlacoochee River groundwater basin. The Aligned Parties contend that groundwater flows south toward Crystal Springs and, therefore, the site is within the "springshed" of Crystal Springs. A United States Geological Survey map of the Crystal Springs springshed shows Angelo's proposed landfill site within the springshed. A springshed study done for SWFWMD also indicates the site is within the Crystal Springs springshed, but the District has not always been consistent in its statements about the groundwater basin boundaries in this area. A water chemistry analysis of the groundwater in the area of Angelo's proposed landfill indicates that the site is an area of higher recharge and within the Crystal Springs springshed. The springshed boundary can shift, depending on rainfall. Angelo's hydrogeological evidence was not sufficient to refute the reasonable possibility that the proposed landfill site is within the Crystal Springs springshed. Therefore, the Department's determination whether Angelo's has provided reasonable assurances must account for the threat of contamination to Crystal Springs and the other public and private water supply sources to the south. There are no creeks or streams and only a few lakes in the area between Crystal Springs and the Angelo's site. The absence of surface runoff features indicates it is an area of high recharge to the groundwater. Crystal Springs is in an area of conduit flow. The hydrologic investigation conducted by Angelo's was not thorough enough to characterize surficial aquifer flow and flow between aquifers. The preponderance of the evidence shows more groundwater recharge to the Floridan Aquifer in the area than estimated by Angelo's. Angelo's hydrogeological investigation was inadequate to refute the possibility of fractured flow or rapid groundwater movement at the proposed landfill site. Angelo's contends there is a continuous clay confining layer that would prevent contamination from moving into deep zones, but the preponderance of the evidence shows discontinuity in the clay and large variations in thickness and depth. The landfill's impermeable liner will impede water movement downward from the landfill, but groundwater will still recharge from outside the landfill to carry any contaminants deeper. If fractured flow or conduit flow extends south from the proposed landfill site, any leachate released into the groundwater beneath the landfill could travel rapidly toward the water supply sources of the City of Zephyrhills, Crystal Springs, Nestlé, and the City of Tampa. Whether the Proposed Landfill is in an Unstable Area Rule 62-701.200(2)(a) prohibits the storage or disposal of solid waste "[i]n an area where geological formations or other subsurface features will not provide support for the solid waste." However, the Department has adopted by reference a federal regulation, 40 C.F.R. 258.15, which allows a landfill to be constructed in a geologically unstable area if the permit applicant can demonstrate that engineering measures are incorporated into the design to ensure that the integrity of the landfill’s structural components "will not be disrupted." The parties presented evidence on many disputed issues of fact at the final hearing, but most of the case involved two ultimate questions: whether the proposed landfill site is unstable and, if so, whether Angelo's has proposed measures that would eliminate the unstable conditions and make the site suitable for a landfill. as: An "unstable area" is defined in 40 C.F.R. § 258.15 A location that is susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from a landfill. Unstable areas can include poor foundation conditions, areas susceptible to mass movements, and Karst terrains. There is overwhelming evidence that the proposed landfill site is an unstable area. A considerable amount of evidence presented by Angelo's supports this finding. For example, Angelo's experts agreed there are loose soils, evidence of raveling, and sinkhole activity. These conditions make the site susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from the proposed landfill. The Department's landfill permitting staff requested a sinkhole risk assessment from the Florida Geologic Survey ("FGS"). The State Geologist and Director of the FGS, Dr. Jonathan Arthur, believes the potential for sinkhole formation at the proposed site is moderately high to high. That potential is consistent with the characterization of the area as unstable. Whether the Proposed Engineering Measures Are Adequate Because the site is unstable, Angelo’s must demonstrate that engineering measures have been incorporated into the landfill's design to ensure that the integrity of its structural components will not be disrupted. See 40 C.F.R. § 258.15(a). The engineering measures proposed by Angelo's are discussed below. Because it was found that Angelo's hydrogeological and geotechnical investigations were not sufficient to characterize all potentially unstable features of the subsurface, it was not demonstrated that the proposed engineering measures would overcome the instability and make the site suitable for a landfill. Roller Compaction Angelo's would use roller compaction on the graded floor of the landfill to compact the soils to a depth of about five feet and eliminate any voids within that depth. The Aligned Parties did not contradict Angelo's evidence that its proposed roller compaction will be done in a manner exceeding what the Department usually requires as far as roller force and the number of roller "passes." However, roller compaction will not affect deep voids. Liner System In order to ensure that the landfill’s liner system components will not be disrupted in the event of a sinkhole, Angelo’s proposes to include the reinforcement geotextile discussed above. The Department previously approved the use of geotextile reinforcement, combined with grouting, to demonstrate site stability for the Hernando County Northwest Landfill, which had a comparable risk of sinkhole formation according to the Department. The reinforcement geotextile can span a 15-foot diameter sinkhole without failure. As found above, the average diameter of the seven sinkholes within five miles of the proposed landfill is 11.9 feet. Angelo's proved that the proposed liner system meets all applicable criteria, except the requirement of rule 62- 701.400(3)(a) that the liner be installed upon a geologically stable base. Grouting Plan Angelo's grouting plan would be implemented to fill voids and stabilize areas of loose or weak material. The grouting plan was first designed to grout all locations where there was a Weight of Hammer, Weight of Rod, Loss of Circulation, or loose sands, as indicated by a low blow count. Angelo's revised the grout plan to include several more areas of concern identified later, for a total of 39 locations. Each grout location would have seven grout points, one in the center and six others equally-spaced on a ten-foot radius from the center. If more than ten cubic yards of grout is needed, additional grout points further outward would be injected until the void or loose soils are filled or stabilized. Although Angelo's proposes to grout every boring of concern, that still ties the integrity of the grouting plan to the thoroughness of the borings. The geologic evidence indicates that there are unstable areas which the grouting plan does not address. The Aligned Parties' MER analysis was persuasive in identifying potential areas of instability that were omitted from Angelo's investigation and from its grouting plan. There are other unstable areas existing on the site that should be grouted or otherwise engineered to provide support for the landfill. The grouting plan does not provide reasonable assurance that the integrity of the structural components of the landfill will not be disturbed. Other Issues Raised by the Aligned Parties The Aligned Parties raise a number of other issues, some of which begin with the assumption that the site is unstable and a large sinkhole would form at the landfill. This sometimes mixes issues inappropriately. It has been found that Angelo's did not provide reasonable assurance that the site will support the proposed landfill, but other project elements must be reviewed on their own merits where possible, assuming the site was engineered for stability. Leachate Collection System There is a single leachate collection trench in the center of the two landfill cells, which makes the landfill operate much like a single cell. The two halves of the cell slope toward the center, so that leachate will drain to the leachate collection trench, and the entire landfill slopes to the west, so that the trench will drain to a sump from which the leachate is pumped to storage tanks. At full capacity, the landfill will generate about 40,000 gallons of leachate per day. Careful cutting and grading of the earth is necessary to create the slopes that are essential to the proper functioning of the project’s leachate collection system. Settlement analyses are necessary to assure that the slopes are maintained. Rule 62-701.410(2)(e) requires a foundation analysis which must include a study of "subgrade settlements, both total and differential." "Total settlement" refers to the overall settlement of a landfill after construction and the loading of solid waste. "Differential settlement" compares settlement at two different points. Angelo's did not meet its burden to provide reasonable assurance on this point. The settlement analysis conducted by Angelo's was amended two or three times during the course of the final hearing to account for computational errors and other issues raised by the Aligned Parties. The analysis never came completely into focus. The final analysis was not signed and sealed by a professional engineer. The settlement analysis is dependent on the geologic analysis, which is inadequate. Without adequate settlement and geologic analyses, it cannot be determined that leachate collection would meet applicable criteria. Storage Tanks The Aligned Parties contend that the leachate storage tanks cannot be supported by the site. Because it was found that Angelo's geologic investigation was not adequate to identify all unstable areas, it is also found that Angelo's failed to provide reasonable assurance that the site would support the leachate storage tanks. In all other respects, the Aligned Parties failed to refute Angelo's demonstration that the storage tanks would meet applicable criteria. Groundwater Monitoring Plan The Aligned Parties contend that there is an insufficient number of monitor wells proposed by Angelo's to detect a leak from the landfill and the wells are too shallow. Because it was found that Angelo's did not adequately characterize the geology and hydrology of the proposed landfill site, the monitoring plan does not provide reasonable assurance of compliance with applicable criteria. Cell Design The Aligned Parties contend that the "mega-cell" design proposed by Angelo's provides less flexibility to respond to and isolate landfill problems than other landfill designs with smaller cells, and the mega-cell design could generate more leakage. No evidence was presented to show whether Angelo's design was one that had been approved or rejected in the past by the Department. Although it is not the best landfill design, the Aligned Parties did not show that the proposed design violates any permitting criteria. Operation and Closure The evidence presented by the Aligned Parties in support of their issues regarding the operation of the proposed landfill, such as noise, odor, and traffic, was not sufficient to refute Angelo's evidence of compliance with applicable criteria, with one exception: Angelo's has not provided an adequate contingency plan to show how it would respond to a sinkhole or other incident that required the landfill to be shut down and repaired. Assuming the site was engineered to support the landfill, there is nothing about the Closure Plan that the Aligned Parties showed does not meet applicable criteria.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Environmental Protection deny Angelo's Permit Application Nos. 22913-001-SC/01 and 22913- 002-SO/01. DONE AND ENTERED this 28th day of June, 2013, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 28th day of June, 2013. COPIES FURNISHED: Carl Roth, Qualified Representative 8031 Island Drive Port Richey, Florida 34668-6220 Christopher M. Kise, Esquire Foley and Lardner, LLP 106 East College Avenue, Suite 900 Tallahassee, Florida 32301-7732 Wayne E. Flowers, Esquire Lewis, Longman and Walker, P.A. Suite 150 245 Riverside Avenue Jacksonville, Florida 32202-4931 Janice M. McLean, Esquire City of Tampa 7th Floor 315 East Kennedy Boulevard Tampa, Florida 33602-5211 Joseph A. Poblick, Esquire City of Zephyrhills 5335 8th Street Zephyrhills, Florida 33542-4312 Doug Manson, Esquire William Bilenky, Esquire Brian A. Bolves, Esquire Manson Bolves, P.A. 1101 West Swann Avenue Tampa, Florida 33606-2637 Jacob D. Varn, Esquire Linda Loomis Shelley, Esquire Karen A. Brodeen, Esquire Fowler, White, Boggs, P.A. 101 North Monroe Street, Suite 1090 Tallahassee, Florida 32302-1547 David Smolker, Esquire Smolker, Bartlett, Schlosser, Loeb and Hinds, P.A. Suite 200 500 East Kennedy Boulevard Tampa, Florida 33602-4936 Stanley Warden, Esquire Christopher Dale McGuire, Esquire Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 William D. Preston, Esquire William D. Preston, P.A. 4832-A Kerry Forest Parkway Tallahassee, Florida 32309-2272 Herschel T. Vinyard, Jr., Secretary Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Matthew Z. Leopold, General Counsel Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Lea Crandall, Agency Clerk Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000

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WRB ENTERPRISES, INC. vs ANGELO`S AGGREGATE MATERIALS, LTD., D/B/A ANGELO`S RECYCLED MATERIALS AND DEPARTMENT OF ENVIRONMENTAL PROTECTION, 09-001545 (2009)
Division of Administrative Hearings, Florida Filed:Temple Terrace, Florida Mar. 23, 2009 Number: 09-001545 Latest Update: Sep. 16, 2013

The Issue The issue to be determined in this proceeding is whether Angelo's Aggregate Materials, LTD ("Angelo's") is entitled to permits from the Department of Environmental Protection ("Department") to construct and operate a Class I landfill in Pasco County.

Findings Of Fact The Parties The Department is the state agency with the power and duty under chapter 403, Florida Statutes, to review and take action on applications for permits to construct and operate solid waste management facilities, including landfills. Angelo's is a Florida limited partnership authorized to conduct business under the name Angelo's Recycled Materials. Angelo's filed the permit applications which are the subject of this proceeding. Angelo's owns the property on which the proposed landfill would be constructed and operated. Crystal Springs Preserve is a Florida corporation that owns approximately 525 acres in Pasco County, Florida on which is located Crystal Springs, a second magnitude spring that flows into the Hillsborough River. The property is about 10 miles south of Angelo's proposed landfill site. Crystal Springs Preserve's primary business activities are selling spring water for bottling for human consumption and operating an environmental education center that focuses on Crystal Springs and the Hillsborough River. Crystal Springs Preserve hosts approximately 50,000 visitors annually at the environmental education center. Crystal Springs Preserve holds a water use permit which authorizes it to withdraw up to 756,893 gallons of water per day (annual average) from Crystal Springs for production of bottled water. The water is transported about three miles to a water bottling facility operated by Nestlé. Nestlé is a private corporation engaged in the business of bottling and selling spring water. Nestlé purchases spring water from Crystal Springs Preserve. Nestlé's "Zephyrhills Spring Water" brand is composed of approximately 90 percent Crystal Springs water and 10 percent Madison Blue Spring water. The only water treatment applied by Nestlé is filtering the water to remove gross contaminants and passing the water through ultraviolet light or ozone to kill any potential bacteria before bottling. Nestlé has established "norms" for its spring water and would not be able to use the water from Crystal Springs if its chemical composition varied significantly from the norms. WRB is a Florida corporation that owns 1,866 acres in Pasco County known as Boarshead Ranch. Boarshead Ranch is adjacent to the east and south of Angelo’s property and is approximately 3,000 feet from the proposed landfill at its closest point. Boarshead Ranch is currently being used for agricultural, recreational, residential, and conservation purposes, including wildlife management. Nearly all of Boarshead Ranch is subject to a conservation easement held by the Southwest Florida Water Management District (SWFWMD). The conservation easement allows WRB to continue agricultural operations. Numerous agricultural water wells are located on Boarshead Ranch. WRB holds a water use permit which authorizes the withdrawal of 820,000 gallons per day (gpd) (annual average) for a number of uses, including production of agricultural products, animal drinking water, and personal use. The City of Zephyrhills is located in Pasco County and is a municipal corporation. Zephyrhills' water service area encompasses Zephyrhills and portions of Pasco County. Zephyrhills owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Zephyrhills holds a water use permit which authorizes nine potable water supply wells with a combined withdrawal of 2.9 million gallons per day ("mgd") (annual average). Zephyrhills has two new production wells located about two miles southeast of the proposed landfill. The City of Tampa owns and operates the David L. Tippin Water Treatment Plant, the Hillsborough River dam, and the City of Tampa reservoir on the Hillsborough River. Flows from Crystal Springs make up a substantial amount of the water in the Hillsborough River, especially during drought conditions when the spring flow accounts for about 50 percent of the flow. The City of Tampa holds a water use permit which authorizes the withdrawal 82 mgd (annual average). The City of Tampa owns, operates, and maintains a water distribution and transmission system of pipes, pump stations, and storage tanks within the City and its service area. Carl Roth, Marvin Hall, and Louis Potenziano own property in Pasco County near the proposed landfill site. Roth's property is 3.5 miles west of the proposed landfill site; Hall's property is located approximately one mile southwest of the site; and Potenziano's property is 1.6 miles to the south/southeast of the site. Roth, Hall, and Potenziano have water wells on their properties. The record does not establish that John Floyd owns property in the area. Floyd and Associates, Inc., owns about 55 acres in the area and holds a water use permit authorizing the withdrawal of water for agricultural uses. The Stipulated Agreement On March 1, 2010, Angelo's filed with DOAH a "Stipulated Agreement" signed by all parties. The Stipulated Agreement states in relevant part: Angelo's shall provide a final design, revised complete permit application and site investigation (referred to jointly as "Revised Submittal") to DEP with copies to all Parties and DEP shall make a completeness determination prior to this proceeding being set for a new final hearing date. * * * Angelo's shall not revise its permit application or supporting information beyond the Revised Submittal prior to or during the final hearing except in response to issues raised by DEP. It appears that the Aligned Parties did not remember the Stipulated Agreement until the commencement of the final hearing. They did not object before then to any of the evidence which Angelo's had prepared or intended to prepare for hearing on the basis that it violated the terms of the Stipulated Agreement. At the commencement of the hearing, Nestlé argued that the Stipulated Agreement barred Angelo's from revising its application or presenting new support for its project at the final hearing. The Stipulated Agreement is unusual and the necessity for Angelo's to make any concessions to the Aligned Parties in order to obtain their agreement to an abeyance was not explained. Allowing an applicant time to amend a permit application is usually good cause for an abeyance. The Stipulated Agreement allowed Angelo's to continue to respond to issues raised by the Department. Angelo's contends that all of the evidence it presented at the final hearing qualifies as a response to issues raised by the Department. The Proposed Landfill Angelo's applied to construct and operate a Class I landfill with associated buildings and leachate holding tanks. Application No. 22913-001-SC/01 corresponds to the construction permit application and Application No. 22913-001-SO/01 corresponds to the operation permit application. A Class I landfill is a landfill authorized to receive Class I waste, which is solid waste from households and businesses. Class I waste does not include hazardous waste, yard waste, or construction and demolition debris. See Fla. Admin. Code R. 62-701.200(13) and (14). The proposed landfill would be approximately 30 acres in size. It is part of a 1,020-acre parcel owned by Angelo's that is west of County Road 35 and south of Enterprise Road in Pasco County. The site is currently leased for cattle grazing and hay and sod production. There are also spray fields, orange groves, and a pond on the 1,020-acre parcel. Angelo's would construct the landfill by first clearing the 30-acre site. It would then excavate and fill to create the design subgrade or floor of the landfill with slopes required for the liner system. The subgrade would be compacted with a vibratory roller. After the subgrade compaction, the grouting plan would be implemented. The grouting plan calls for grouting 39 subsurface locations on the site that have voids, loose soils, or other unstable characteristics. A liner system would be installed after the grouting is completed and the subgrade is finished. From the bottom upward, the liner system would begin with a 12-inch layer of clay, over which a reinforcement geotextile would be installed, followed by another 12-inch layer of clay. This reinforcement geotextile is in addition to the double liner system required by Department rule. Its purpose is to maintain the integrity of the liner system in the event that a sinkhole occurs beneath the landfill. Installed above the reinforcement geotextile and clay layer would be a 60-millimeter high-density polyethylene ("HDPE") geomembrane, followed by a HDPE drainage net. These last two components comprise the secondary leachate collection system. Above the HDPE drainage net would be the primary leachate collection system, consisting of another 60-millimeter HDPE geomembrane and HDPE drainage net, followed by a geotextile, then a 12-inch sand layer for drainage, and an additional 12-inch sand layer for protection against puncture of the HDPE liner. A 48-inch layer of selected waste, free of items that could puncture the liner, would be the first waste placed over the primary leachate collection system. "Leachate" is "liquid that has passed through or merged from solid waste and may contain soluble, suspended, or miscible materials." See Fla. Admin. Code R. 62-701.200(66). Leachate would be collected through a system of perforated pipes that empty into a sloping trench with a leachate collection pipe. The leachate collection pipe would run down the center of the landfill to the lowest point where a pump would send the collected leachate through a force main 0.25 miles to storage tanks. Five above-ground storage tanks would be installed on a concrete pad with capacity to store 90,000 gallons of leachate. The stored leachate would be periodically transported to an offsite location, such as a wastewater treatment facility, for disposal. Sinkholes and Karst The terms "sinkhole" and "sinkhole activity" are not defined by Department rule, but the statutory definitions in chapter 627, a chapter dealing with insurance coverage for homes and other buildings, are generally consistent with the scientific meanings of these terms. The term "sinkhole" is defined in section 627.706(2)(h) as: a landform created by subsidence of soil, sediment, or rock as underlying strata are dissolved by groundwater. A sinkhole forms by collapse into subterranean voids created by dissolution of limestone or dolostone or by subsidence as these strata are dissolved. The term "sinkhole activity" is defined in section 627.706(2)(i) as: settlement or systematic weakening of the earth supporting the covered building only if the settlement or systematic weakening results from contemporaneous movement or raveling of soils, sediments, or rock materials into subterranean voids created by the effect of water on a limestone or similar rock formation. Sinkholes occur throughout Florida. There have been many reported and confirmed sinkholes in Pasco County. The more common type of sinkhole that has occurred on the Brooksville Ridge is a "cover subsidence" sinkhole, which is caused by voids in the limestone and the downward movement--"raveling"--of overlying soils into the cavity. Eventually, the loss of soils in the raveling zone will propagate upward until the soils at the ground surface also move downward and a depression is formed at the surface. Cover subsidence sinkholes develop slowly and are usually small, less than ten feet in diameter. Less common are "cover collapse" sinkholes, which can form in a matter of days or hours as the result of the collapse of the "roof" of a dissolved cavity in the limestone. These sinkholes are usually large and deep. The occurrence of a sinkhole does not always mean that areas near the sinkhole are unstable. However, the occurrence of a sinkhole is reasonable cause for concern about the stability of nearby areas and a reasonable basis for the Department to require thorough geologic investigations. "Karst" refers to limestone that is undergoing dissolution and it is common in Florida. A sinkhole forms in karst. "Epikarst" is limestone that was weathered while exposed above sea level millions of years ago before being submerged again. It is generally softer and more permeable than unweathered limestone. "Paleokarst" refers to karst that is very old in geologic time. Paleosinks are old sinkhole features in the paleokarst. A paleosink may no longer be unstable because it has been filled in for thousands or millions of years. A "lineament," or a "photolineament," is a relatively straight line seen in the topography or aerial photographs of the ground surface in an area. It might be defined by soil color, sloughs, ponds, wetlands, or other land features that follow a linear path. Lineaments are sometimes, but not always, associated with subsurface fractures in the bedrock where one would expect to also find active karst, sinkholes, and relatively rapid groundwater flow. Even where there is no lineament, there can be fractures in limestone that, when extensive enough, will allow for "fractured," "preferential," or "conduit flow" of groundwater. Fractured flow can occur in a small area or may go on for miles. Springs in Florida are usually associated with fractured flow or conduit flow that allows groundwater to move through the aquifer a long distance relatively rapidly, in weeks rather than decades. Geotechnical Investigation The Department's rules require subsurface conditions to be explored and described, including soil stratigraphy, soft ground, lineaments, and unstable areas, but the rules do not require the application of any particular geologic testing technique. An applicant's testing program is primarily a function of the professional judgment of the applicant’s geologist in cooperation with Department staff. The amount of geological testing done by Angelo's during its initial testing was similar to what was done for recent landfill applications. Angelo's conducted additional testing to respond to Department concerns and to prepare for the final hearing in this case, making the total amount of testing at Angelo's proposed site more extensive than is usual for a proposed landfill. The geologic investigation conducted by Angelo's experts to determine subsurface features, including any sinkholes, employed several technologies. Split Spoon Penetrometer Test (SPT) or SPT borings were drilled with a drill rig that advances a split spoon sampler into the ground with a 140 pound hammer. The hammer is dropped 30 inches and the number of blows required to drive the sampler each successive 12 inches is referred to as the "N" value and indicates soil strength and density. The higher the N value, the denser the soil. When the material is so dense the drill rod cannot (essentially) be hammered deeper, the N value is shown as "R," which stands for "refusal." SPT Bore logs also note any observed "weight of hammer," "weight of rod," or "loss of circulation." These terms describe areas where the drilling encounters very soft material or voids. Weight of rod, for example, means the weight of the drilling rod, by itself, with no hammer blow, was enough to cause the rod to fall deeper through the soil or rock. Cone Penetrometer Test ("CPT") borings were also conducted. CPT borings are relatively shallow, performed with a hand-held rod and special tip that the operator pushes into the ground. The CPT equipment continuously measures and records tip resistance and sleeve resistance as the rod moves downward through soils. It is helpful in some applications, but is less precise in determining soil type, strength, and compressibility than SPT borings and cannot be used to explore deep zones. Ground penetrating radar ("GPR") studies were used. GPR equipment transmits pulses of radio frequency waves into the ground. The manner in which the radio waves are reflected indicates the types of soil and rock encountered. It can also detect cavities and other features that would suggest karst activity. When the GPR identifies geologic features of interest, they can be further investigated with SPT borings. Another investigative tool used by Angelo's was Multiple Electrode Resistivity ("MER"). MER uses a grid of wires and electrodes and the equipment interprets the resistivity of electrical signals transmitted through the subsurface. MER data can be displayed in a two dimensional or three dimensional format, depending on the software program that is used to process the data. Like GPR, MER is useful for indentifying geologic features of interest that can be further explored with SPT borings. However, GPR generally has good resolution only near the ground surface, while MER has good resolution to a depth of 100 feet. The Regional Geology The proposed site is in a geologic transition zone on the eastern flank of a regional, geological feature known as the Brooksville Ridge. It is a transition zone for both the Suwannee Limestone and Hawthorn Group. The Brooksville Ridge was formed when it was part of the coastline. In its geologic past, the Brooksville Ridge experienced sea level changes, weathering, erosion of sediments, and beach reworking. The general layering of geologic features on the Brooksville Ridge, from the top down, begins with topsoil and a layer of sand. Under the sand layer is the Hawthorn Group, an older geologic layer consisting of a heterogeneous mix of limestone, clays, and sands which generally range in depth from slightly under 60 feet to 80 feet or more. It was formed by river and wind erosion, flushing, and re-deposition in a beach dune environment. Below the Hawthorn Group is the Suwannee Limestone Formation, which is present throughout eastern Pasco County. The upper surface of the Suwannee Limestone Formation is undulating, due to a gradual chemical weathering of its upper surface, representing a "paleokarst environment." Underlying the Suwannee Limestone Formation is the Ocala Limestone Formation. It extends throughout most of Florida. It is composed of nearly pure limestone and is considered the Floridan Aquifer. It extends across the site’s subsurface. Angelo's used the Florida Geologic Survey's data base to determine there are six sinkholes within five miles of the proposed landfill. A seventh sinkhole, not in the data base, is the 15- foot sinkhole at the Angelo's Enterprise Road Facility landfill, a Class III landfill (yard waste and construction and demolition debris) about a mile northwest of the proposed site. Angelo's contends that the sinkhole at its Class III landfill was "induced" during construction of the facility by the diversion of stormwater runoff to an area where overburden had been removed. The average diameter of the seven sinkholes is 11.9 feet. The Geology of the Proposed Site Rule 62-701.410(2)(c) requires a geotechnical site investigation and report, which shall: Explore and describe subsurface conditions including soil stratigraphy and ground water table conditions; Explore and address the presence of muck, previously filled areas, soft ground, lineaments, and sinkholes; Evaluate and address fault areas, seismic impact zones, and unstable areas as described in 40 C.F.R. 258.13, 258.14 and 258.15; Include estimates of the average and maximum high ground water table across the site; and Include a foundation analysis to determine the ability of the foundation to support the loads and stresses imposed by the landfill. It may include geotechnical measures necessary to modify the foundation to accommodate the imposed loads and stresses. The foundation shall be analyzed for short-term, end of construction, and long-term stability and settlement conditions. Considering the existing or proposed subgrade conditions and the landfill geometry, analysis shall include: Foundation bearing capacity; Subgrade settlements, both total and differential; and Subgrade slope stability. Angelo's conducted a geotechnical site investigation, but it was not adequate, as discussed below and in sections I. and J. The proposed landfill site is geologically complex, having features that are discontinuous horizontally and vertically. The site has karst features or areas where the limestone has dissolved. There is a clay layer in some areas, but it is not continuous and its depth and thickness vary. There are deposits of hard and soft sands at various depths. There are pinnacles of limestone surrounded by softer materials. Photographs from a quarry called the Vulcan Mine, located on the western flank of the Brooksville Ridge, show exposed features in the top 20 to 30 feet of the Suwannee Limestone in the region. The features at the Vulcan Mine are roughly similar to features at the Angelo's site. There are a number of shallow depressions on the surface of the ground on the Angelo's site. The origin and significance of these depressions was a matter of dispute. The Aligned Parties believe they represent sinkhole activity, but the evidence presented did not rise to the level of proof. However, Angelo's did not prove they were unassociated with geotechnical issues that could affect the proposed landfill. Angelo's offered no reasonable explanation for the depressions. Determining the exact cause of the depressions may not be possible even with more extensive investigation, but it was Angelo's responsibility as the permit applicant, pursuant to rule 62-701.410(2)(c), to make a greater effort to account for them. Angelo's initial permit application identified two intersecting lineaments on Angelo's property, based on aligned lowlands, enclosed valleys, and ponds. Angelo's contends the lineaments do not reflect an unstable subsurface or fractured limestone. The Aligned Parties contend that the lineaments are regional features and reflect fractures in the bedrock. They also contend that the onsite pond, which is located along the lineament, is an old sinkhole. The Aligned Parties did not prove the proposed landfill site is above an area of fractured bedrock, but the evidence presented by Angelo's was incomplete and insufficient to show there are no fractures. The limestone on the site was not adequately investigated for voids and fractures. Angelo's did not refute the possibility that the lineaments reflect a significant subsurface feature that could affect both site stability and groundwater movement. The Regional and Local Hydrogeology Rule 62-701.410(1) requires a hydrogeological investigation and site report, which shall: Define the landfill site geology and hydrology and its relationship to the local and regional hydrogeologic patterns including: Direction and rate of ground water and surface water flow, including seasonal variations; Background quality of ground water and surface water; Any on site hydraulic connections between aquifers; For all confining layers, semi-confining layers, and all aquifers below the landfill site that may be affected by the landfill, the porosity or effective porosity, horizontal and vertical permeabilities, and the depth to and lithology of the layers and aquifers; and Topography, soil types and characteristics, and surface water drainage systems of the site and surrounding the site. Include an inventory of all the public and private water wells within a one-mile radius of the proposed landfill site. The inventory shall include, where available: The approximate elevation of the top of the well casing and the depth of each well; The name of the owner, the age and usage of each well, and the estimated daily pumpage; and The stratigraphic unit screened, well construction technique, and static water levels of each well. Identify and locate any existing contaminated areas on the landfill site. Include a map showing the locations of all potable wells within 500 feet of the waste storage and disposal areas to demonstrate compliance with paragraph 62- 701.300(2)(b), F.A.C. Angelo's conducted a hydrogeological investigation, but it was not adequate, as discussed below. Angelo's and the Aligned Parties disputed the hydrogeological characteristics of the proposed landfill site and region. The principal disputes related to the direction and velocity of groundwater flow. Angelo's contends that groundwater flows from the landfill site to the west, making the proposed landfill site part of the Withlacoochee River groundwater basin. The Aligned Parties contend that groundwater flows south toward Crystal Springs and, therefore, the site is within the "springshed" of Crystal Springs. A United States Geological Survey map of the Crystal Springs springshed shows Angelo's proposed landfill site within the springshed. A springshed study done for SWFWMD also indicates the site is within the Crystal Springs springshed, but the District has not always been consistent in its statements about the groundwater basin boundaries in this area. A water chemistry analysis of the groundwater in the area of Angelo's proposed landfill indicates that the site is an area of higher recharge and within the Crystal Springs springshed. The springshed boundary can shift, depending on rainfall. Angelo's hydrogeological evidence was not sufficient to refute the reasonable possibility that the proposed landfill site is within the Crystal Springs springshed. Therefore, the Department's determination whether Angelo's has provided reasonable assurances must account for the threat of contamination to Crystal Springs and the other public and private water supply sources to the south. There are no creeks or streams and only a few lakes in the area between Crystal Springs and the Angelo's site. The absence of surface runoff features indicates it is an area of high recharge to the groundwater. Crystal Springs is in an area of conduit flow. The hydrologic investigation conducted by Angelo's was not thorough enough to characterize surficial aquifer flow and flow between aquifers. The preponderance of the evidence shows more groundwater recharge to the Floridan Aquifer in the area than estimated by Angelo's. Angelo's hydrogeological investigation was inadequate to refute the possibility of fractured flow or rapid groundwater movement at the proposed landfill site. Angelo's contends there is a continuous clay confining layer that would prevent contamination from moving into deep zones, but the preponderance of the evidence shows discontinuity in the clay and large variations in thickness and depth. The landfill's impermeable liner will impede water movement downward from the landfill, but groundwater will still recharge from outside the landfill to carry any contaminants deeper. If fractured flow or conduit flow extends south from the proposed landfill site, any leachate released into the groundwater beneath the landfill could travel rapidly toward the water supply sources of the City of Zephyrhills, Crystal Springs, Nestlé, and the City of Tampa. Whether the Proposed Landfill is in an Unstable Area Rule 62-701.200(2)(a) prohibits the storage or disposal of solid waste "[i]n an area where geological formations or other subsurface features will not provide support for the solid waste." However, the Department has adopted by reference a federal regulation, 40 C.F.R. 258.15, which allows a landfill to be constructed in a geologically unstable area if the permit applicant can demonstrate that engineering measures are incorporated into the design to ensure that the integrity of the landfill’s structural components "will not be disrupted." The parties presented evidence on many disputed issues of fact at the final hearing, but most of the case involved two ultimate questions: whether the proposed landfill site is unstable and, if so, whether Angelo's has proposed measures that would eliminate the unstable conditions and make the site suitable for a landfill. as: An "unstable area" is defined in 40 C.F.R. § 258.15 A location that is susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from a landfill. Unstable areas can include poor foundation conditions, areas susceptible to mass movements, and Karst terrains. There is overwhelming evidence that the proposed landfill site is an unstable area. A considerable amount of evidence presented by Angelo's supports this finding. For example, Angelo's experts agreed there are loose soils, evidence of raveling, and sinkhole activity. These conditions make the site susceptible to natural or human-induced events or forces capable of impairing the integrity of some or all of the landfill structural components responsible for preventing releases from the proposed landfill. The Department's landfill permitting staff requested a sinkhole risk assessment from the Florida Geologic Survey ("FGS"). The State Geologist and Director of the FGS, Dr. Jonathan Arthur, believes the potential for sinkhole formation at the proposed site is moderately high to high. That potential is consistent with the characterization of the area as unstable. Whether the Proposed Engineering Measures Are Adequate Because the site is unstable, Angelo’s must demonstrate that engineering measures have been incorporated into the landfill's design to ensure that the integrity of its structural components will not be disrupted. See 40 C.F.R. § 258.15(a). The engineering measures proposed by Angelo's are discussed below. Because it was found that Angelo's hydrogeological and geotechnical investigations were not sufficient to characterize all potentially unstable features of the subsurface, it was not demonstrated that the proposed engineering measures would overcome the instability and make the site suitable for a landfill. Roller Compaction Angelo's would use roller compaction on the graded floor of the landfill to compact the soils to a depth of about five feet and eliminate any voids within that depth. The Aligned Parties did not contradict Angelo's evidence that its proposed roller compaction will be done in a manner exceeding what the Department usually requires as far as roller force and the number of roller "passes." However, roller compaction will not affect deep voids. Liner System In order to ensure that the landfill’s liner system components will not be disrupted in the event of a sinkhole, Angelo’s proposes to include the reinforcement geotextile discussed above. The Department previously approved the use of geotextile reinforcement, combined with grouting, to demonstrate site stability for the Hernando County Northwest Landfill, which had a comparable risk of sinkhole formation according to the Department. The reinforcement geotextile can span a 15-foot diameter sinkhole without failure. As found above, the average diameter of the seven sinkholes within five miles of the proposed landfill is 11.9 feet. Angelo's proved that the proposed liner system meets all applicable criteria, except the requirement of rule 62- 701.400(3)(a) that the liner be installed upon a geologically stable base. Grouting Plan Angelo's grouting plan would be implemented to fill voids and stabilize areas of loose or weak material. The grouting plan was first designed to grout all locations where there was a Weight of Hammer, Weight of Rod, Loss of Circulation, or loose sands, as indicated by a low blow count. Angelo's revised the grout plan to include several more areas of concern identified later, for a total of 39 locations. Each grout location would have seven grout points, one in the center and six others equally-spaced on a ten-foot radius from the center. If more than ten cubic yards of grout is needed, additional grout points further outward would be injected until the void or loose soils are filled or stabilized. Although Angelo's proposes to grout every boring of concern, that still ties the integrity of the grouting plan to the thoroughness of the borings. The geologic evidence indicates that there are unstable areas which the grouting plan does not address. The Aligned Parties' MER analysis was persuasive in identifying potential areas of instability that were omitted from Angelo's investigation and from its grouting plan. There are other unstable areas existing on the site that should be grouted or otherwise engineered to provide support for the landfill. The grouting plan does not provide reasonable assurance that the integrity of the structural components of the landfill will not be disturbed. Other Issues Raised by the Aligned Parties The Aligned Parties raise a number of other issues, some of which begin with the assumption that the site is unstable and a large sinkhole would form at the landfill. This sometimes mixes issues inappropriately. It has been found that Angelo's did not provide reasonable assurance that the site will support the proposed landfill, but other project elements must be reviewed on their own merits where possible, assuming the site was engineered for stability. Leachate Collection System There is a single leachate collection trench in the center of the two landfill cells, which makes the landfill operate much like a single cell. The two halves of the cell slope toward the center, so that leachate will drain to the leachate collection trench, and the entire landfill slopes to the west, so that the trench will drain to a sump from which the leachate is pumped to storage tanks. At full capacity, the landfill will generate about 40,000 gallons of leachate per day. Careful cutting and grading of the earth is necessary to create the slopes that are essential to the proper functioning of the project’s leachate collection system. Settlement analyses are necessary to assure that the slopes are maintained. Rule 62-701.410(2)(e) requires a foundation analysis which must include a study of "subgrade settlements, both total and differential." "Total settlement" refers to the overall settlement of a landfill after construction and the loading of solid waste. "Differential settlement" compares settlement at two different points. Angelo's did not meet its burden to provide reasonable assurance on this point. The settlement analysis conducted by Angelo's was amended two or three times during the course of the final hearing to account for computational errors and other issues raised by the Aligned Parties. The analysis never came completely into focus. The final analysis was not signed and sealed by a professional engineer. The settlement analysis is dependent on the geologic analysis, which is inadequate. Without adequate settlement and geologic analyses, it cannot be determined that leachate collection would meet applicable criteria. Storage Tanks The Aligned Parties contend that the leachate storage tanks cannot be supported by the site. Because it was found that Angelo's geologic investigation was not adequate to identify all unstable areas, it is also found that Angelo's failed to provide reasonable assurance that the site would support the leachate storage tanks. In all other respects, the Aligned Parties failed to refute Angelo's demonstration that the storage tanks would meet applicable criteria. Groundwater Monitoring Plan The Aligned Parties contend that there is an insufficient number of monitor wells proposed by Angelo's to detect a leak from the landfill and the wells are too shallow. Because it was found that Angelo's did not adequately characterize the geology and hydrology of the proposed landfill site, the monitoring plan does not provide reasonable assurance of compliance with applicable criteria. Cell Design The Aligned Parties contend that the "mega-cell" design proposed by Angelo's provides less flexibility to respond to and isolate landfill problems than other landfill designs with smaller cells, and the mega-cell design could generate more leakage. No evidence was presented to show whether Angelo's design was one that had been approved or rejected in the past by the Department. Although it is not the best landfill design, the Aligned Parties did not show that the proposed design violates any permitting criteria. Operation and Closure The evidence presented by the Aligned Parties in support of their issues regarding the operation of the proposed landfill, such as noise, odor, and traffic, was not sufficient to refute Angelo's evidence of compliance with applicable criteria, with one exception: Angelo's has not provided an adequate contingency plan to show how it would respond to a sinkhole or other incident that required the landfill to be shut down and repaired. Assuming the site was engineered to support the landfill, there is nothing about the Closure Plan that the Aligned Parties showed does not meet applicable criteria.

Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Environmental Protection deny Angelo's Permit Application Nos. 22913-001-SC/01 and 22913- 002-SO/01. DONE AND ENTERED this 28th day of June, 2013, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 28th day of June, 2013. COPIES FURNISHED: Carl Roth, Qualified Representative 8031 Island Drive Port Richey, Florida 34668-6220 Christopher M. Kise, Esquire Foley and Lardner, LLP 106 East College Avenue, Suite 900 Tallahassee, Florida 32301-7732 Wayne E. Flowers, Esquire Lewis, Longman and Walker, P.A. Suite 150 245 Riverside Avenue Jacksonville, Florida 32202-4931 Janice M. McLean, Esquire City of Tampa 7th Floor 315 East Kennedy Boulevard Tampa, Florida 33602-5211 Joseph A. Poblick, Esquire City of Zephyrhills 5335 8th Street Zephyrhills, Florida 33542-4312 Doug Manson, Esquire William Bilenky, Esquire Brian A. Bolves, Esquire Manson Bolves, P.A. 1101 West Swann Avenue Tampa, Florida 33606-2637 Jacob D. Varn, Esquire Linda Loomis Shelley, Esquire Karen A. Brodeen, Esquire Fowler, White, Boggs, P.A. 101 North Monroe Street, Suite 1090 Tallahassee, Florida 32302-1547 David Smolker, Esquire Smolker, Bartlett, Schlosser, Loeb and Hinds, P.A. Suite 200 500 East Kennedy Boulevard Tampa, Florida 33602-4936 Stanley Warden, Esquire Christopher Dale McGuire, Esquire Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 William D. Preston, Esquire William D. Preston, P.A. 4832-A Kerry Forest Parkway Tallahassee, Florida 32309-2272 Herschel T. Vinyard, Jr., Secretary Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Matthew Z. Leopold, General Counsel Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Lea Crandall, Agency Clerk Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000

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TAYLOR ROAD CIVIC ASSOCIATION, INC. vs. HILLSBOROUGH COUNTY AND DEPARTMENT OF ENVIRONMENTAL REGULATION, 79-002269 (1979)
Division of Administrative Hearings, Florida Number: 79-002269 Latest Update: May 14, 1980

Findings Of Fact On February 1, 1977, DER issued an operation permit to Respondent Hillsborough County for the operation of a solid waste disposal facility (sanitary landfill) with an area of 42 acres, located at Taylor Road and Sligh Avenue in the northeast portion of Hillsborough County. The permit was effective for a period of two years and contained various conditions which required the permittee to abide by applicable rules of the DER. The conditions also specified that water samples from monitoring wells and from any waters discharged from the site should be taken and analyzed to determine water quality and such analysis submitted to the Hillsborough County Environmental Protection Commission (HCEPC) acting as the agent for DER within Hillsborough County. The conditions further prohibited open burning at the site without prior approval, control of any objectionable odors, provision for sufficient equipment, and controlled access to the site. (Exhibit 22) In December 1978, Hillsborough County applied for renewal of its operation permit until February 1, 1980. The application and accompanying letter showed that the county wished to operate the site as a "high rise land fill" due to the fact that dirt accumulated from trench excavation had raised the ground level approximately ten feet. In July, 1979, after submission of requested additional information to DER during the preceding months, the county director of solid wastes submitted closeout plans for the landfill to DER and advised that they were filing a permit application for a new landfill to the east of the current site, utilizing a borrow pit area which had been transferred to the county by the State Department of Transportation. Thereafter, by letter of October 23, 1979, the Hillsborough County Administrator requested that DER consider the previous application for renewal of its operating permit to be withdrawn and that the application be viewed as one for a temporary operating permit. (Exhibit 1) During the month of August 1979, several inspections of the existing landfill were made by DER, HCEPC, and Regional EPA personnel. A series of memos prepared by the agency personnel reflected that various violations of DER rules governing landfills had been found during the course of the inspections. These included uncontrolled ponding of water in low areas on the site, failure to control the runoff of surface water, lack of adequate control to prevent unauthorized access to the site, failure to provide the requisite six inches of daily cover over the compacted waste, lack of proper ground water monitoring, and destruction of several wells by heavy equipment, and frequent breakdown of equipment used at the site. Residents living nearby or adjacent to the landfill have observed ponding, uncontrolled runoff, and unauthorized personnel on the site. They have experienced a high incidence of rats, birds and flies on their property and have seen septic tank waste trucks at the landfill. They further have noted uncovered garbage and have seen waste flow from the landfill into the area of Interstate Highway 4 which borders the south portion of the site. The State Department of Transportation has also made complaints to the county concerning dirt and debris on the interstate right-of-way. In a letter to DER, dated October 2, 1979, the county director of public utilities and safety responded to the various complaints and alleged violations. He acknowledged the validity of a number of the problems and indicated the corrective action that had or would be taken to prevent recurrence. (Testimony of Brantner, Warner, Smoot, Exhibit 8, supplemented Exhibits 10-15, 20, 23) By letter of October 23, 1979, DER's Southwest District manager issued Notice of Intent to issue a temporary operation permit for the high-rise landfill pursuant to Section 403.087, Florida Statutes, and Sections 17-4.07, Florida Administrative Code, with an expiration date of February 1, 1980. The stated reasons for the proposed issuance of the permit were because the facility did not qualify for an operation permit, but the applicant was making bona fide efforts to provide an acceptable alternate waste disposal system, and that the permit would allow time to establish a five-year monitoring program to ensure that the site had stabilized and was not a significant water pollution source. Conditions attached to the proposed permit were such as to reasonably preclude the recurrence of past violations with regard to daily cover, controlling access to the site, establishment of a gas monitoring program, and installation of additional monitoring wells for periodic sampling as to water quality. A compliance schedule was stated which required the submission of plans to accomplish the requirements of the permit and such schedule called for the cessation of all filling operations by February 1, 1980 and commencement of the closeout operation on March 1, 1980. The petitions for hearing herein were thereafter filed with DER and referred to this Division on November 15, 1979. (Exhibit 3) In December, 19.79, DER received notification from the regional office of the United States Environmental Protection Agency that volatile organic analysis on well supply samples from private residences in the vicinity of the landfill indicated a potential health risk and that the agency had therefore advised the well owners not to drink the water. Inspections of the landfill in mid-January 1980 by DER and HCEPC personnel showed that solid waste was not being adequately covered on a daily basis and that ponding of water in various areas was observed. The county attributed the ponding to heavy rainfall during the period, but claimed that the waste had been covered on a daily basis although the heavy equipment had scattered paper and other debris through the cover soil in view of the sticky nature of the clayey soil. (Exhibits 6, 16-18) After Hillsborough County officials became aware of the EPA well tests, a private consulting firm of ground water hydrologists and geologists was employed by the county to undertake a water quality analysis of the round water in and around the landfill. The program commenced in late December 1979, and a preliminary assessment of ground water quality was submitted in February 1980. Water samples were taken from private wells adjoining the landfill and from a well within the landfill itself. Analysis of the samples led to preliminary conclusions that organic and inorganic constituents of samples from within the landfill correlated well with those wells adjacent to the landfill, thereby suggesting landfill leachate as a source of contaminants. However, the consultants are of the opinion that several wells which exhibited traces of organic but no discernible inorganic contaminants may be affected by sources of contamination not related to landfill leachate, such as petroleum products, septic tank cleaners, and other household products. It was found that inadequate regional and site specific hydrogeologic data was available upon which to base a complete statistical analysis. It was further found that the wells used in the study were "uncontrolled" and therefore did not represent a valid basis for determining the origin of their contamination. Further study is planned which will involve testing of samples from twenty new monitoring wells designed to determine the rate of movement and attenuation of leachate. The results of such study will be available within five or six months. Although it is generally agreed that ground water flows in a southwesterly direction at the site, more information is required to ascertain the precise direction of flow. At the present time surface water falling on the landfill flows toward a county owned borrow pit to the southwest of the landfill. (Testimony of Schreuder, Becker, Bush, Exhibits 7, 19) The closing plans for the landfill site provide for surface water to be channeled away from the area and directed through swales to travel in the natural direction to the west. A final two-foot cover of soil will be place over completed cells and a three and one-half foot cover of compacted soil will be placed on side slopes of the landfill. Such final cover and grading of the area is designed to preclude infiltration of surface water. Trees will be planted around the periphery of the area and trenches will be dug to force any gases upward to a high point where an exhaust will be placed. Soil borings show that there is an extensive layer of clay at the bottom of the landfill but the permeability of this material is unknown. The solid waste cells are at a maximum of 40 feet below the ground surface and the average height of the compacted waste above ground surface is approximately 28 feet. The county permanently ceased accepting solid waste at the landfill on February 11, 1980, and has commenced closing operation to a minimal degree. As a result of the fact that solid waste is no longer being accepted, the intended elevation to be reached in the southern portion of the site will not take place and accordingly the closing plan will have to be revised in that respect. It is estimated that closing will take approximately one year to accomplish. Upon final closing with vegetative cover and proper grading, it is anticipated that pending and vector problems will be resolved. At the present time, inadequate fencing exists around the boundaries of the landfill. (Testimony of Bush, Becker, Exhibits 2- 21) In recognition of the fact that Hillsborough County ceased using the landfill for disposal of solid waste, the county and DER entered into a written stipulation, dated February 25, 1980, confirming this fact and revising special conditions to the proposed temporary operating permit. These conditions included a proviso that the proposed permit would expire three years from the date of issuance to permit a long-term monitoring and surveillance program to be conducted until the site has stabilized and is not a significant water pollution source. The conditions also call for the county to establish an acceptable program for monitoring gases at different points within the landfill, to control access to the site, and to complete the study to determine the extent and source of any infiltration of foreign substances into the ground water from the site. In addition, the conditions would require the county to submit an acceptable plan for long-term monitoring of ground water, including the installation of additional monitoring wells if required. It also provides that the final closeout of the site shall be completed within one year from the date of the final order and that such closeout shall be completed in accordance with applicable law and in accordance with previous closeout plans to the extent made possible by final elevations. (Exhibit 4)

Recommendation That the applicant Hillsborough County be issued a temporary operating permit for the closing of the landfill specified in the application. DONE and ENTERED this 26th day of March, 1980, in Tallahassee, Florida. THOMAS C. OLDHAM Hearing Officer Division of Administrative Hearings 101 Collins Building Tallahassee, Florida 32301 (904) 488-9675 COPIES FURNISHED: Honorable Jacob Varn Morris W. Milton, Esquire Secretary, Department of Douglas A. Mulligan, Esquire Environmental Regulation Post Office Box 13517 2600 Blair Stone Road St. Petersburg, Florida 33713 Tallahassee, Florida 32301 Alfred W. Clark, Esquire Vincent L. Nuccio, Jr., Esquire Department of Environmental Post Office Box 1110 Regulation Tampa, Florida 35601 2600 Blair Stone Road Tallahassee, Florida 32301 Gene T. Hall, Esquire Elliot Dunn, Esquire 209 East Robertson Street Post Office Box 1110 Brandon, Florida 33511 Tampa, Florida 33601 Richard S. Smoot Ronald Frink, President Post Office Box 682 Florida Water Well Association Seffner, Florida 33584 Post Office Box 11648 Tampa, Florida 33680

Florida Laws (5) 403.087403.088403.703403.7077.08
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KENNETH C. WILLIAMS, JOSEPH KAISER, ET AL. vs. DEPARTMENT OF ENVIRONMENTAL REGULATION, 76-001250 (1976)
Division of Administrative Hearings, Florida Number: 76-001250 Latest Update: Jun. 08, 1977

Findings Of Fact Respondent, Textron Petroleum Products Company, Inc., has applied for a construction permit to construct a sanitary landfill in Sections 3 and 10, Township 1 North, Range 2 East, Leon County, Florida. The proposed site consists of ninety (90) acres and is approximately 2,000 feet from U.S Highway 90 at Its closest point to that highway. The application is in proper form and contains all information required by the Department of Environmental Regulation. towns and areas to be served by the application are the City," of Tallahassee and Leon County. The facility is designed to serve a population of 135,000 people. Although evidence was presented for the purpose of showing that the City of Tallahassee and Leon County, as governmental entities, do not intend to use the proposed sanitary landfill as an "official" landfill site for those governmental bodies, this evidence did not establish that the area to be served and the population to be served by the proposed sanitary landfill is other than that stated above. The applicant, Textron Petroleum Products Company, Inc. does not have a franchise from any county, municipality or other governmental agency with regard to solid waste resource recovery and management responsibilities. The applicant, Textron Petroleum Products Company, Inc., had not, at the time of hearing, posted a performance bond or other approved security with the agency within whose jurisdiction the proposed site is located. The "owner" as that term is used in Section 17-4.21(1)(d), F.A.C., is the applicant, Textron Petroleum Products Company, Inc. The unrebutted evidence presented,at hearing established that the applicant has a net worth of $1 million and is financially responsible. The evidence presented did not establish any violation of the State Resource Recovery And Management Program set out in Part II, Chatper 17-7, F.A.C. There is a public supply well located in the Homestead Ridge area. This system serves 38 or more customers at an averave rate of about 200,000 gallons per month. The well is located more than 2,700 feet from the site boundary of the proposed sanitary landfill. As found by the Northwest Florida Water Management District, even if the consumption of that well system were increased to 2.16 million gallons of water per month, the drawdown at a radius of 2,000 feet would be 0.13 feet. Therefore, it was concluded that the cone of influence of the public water supply does not extend under the proposed sanitary landfill site. As a condition for issuance of a construction permit the Department of Environmental Regulation proposes the requirement of a monitoring system of wells which would include a deep well located between the proposed site and the Homestead Ridge public supply, the purpose of which would be to detect the potential intrusion of leachate or other contaminants into the public water supply from the sanitary landfill. It is improbable that the proposed sanitary landfill will produce any significant quantity of leachate. However, the application proposes that if monitoring indicates that lechate control is needed, a well point system will be installed in the completed cells and underground pipe drains installed in the new cells. It further provides that, dependent upon the quantities involved, the leachate.will be transported to the City of Tallahassee Sewage Treatment Facilities for disposal or it will be treated on-site by transporting the leachate to the settling pond which will at that time be equipped with suitable aeration and chlorination equipment for treatment of the leachate. The proposed design of the sanitary landfill provides that all final discharge from the sedimentatlon pond will conform to the water quality standards set out in Chapter 17-3, F.A.C, even though this may require the constrjction of treatment equipment by the applicant. The application, at pages 12 and 14,.provides for the equipment to be used on-site in the operation of the proposed sanitary landfill as well as for the method of providing adequate site supervision. No evidence was presented showing these provisions to be other than adequate. The evidence presented did not establish that the utilization of U.S. Highway 90 by vehicles transporting waste to the proposed sanitary landfill would create any unusual 0rincreased traffic and safety hazard. The application, at page 3, proposed the installation of electronic signalization equipment to alleviate any hazard which might be created by traffic using the proposed site. No evidence was presented showing this proposal to be inadequate. According to a letter to Mr. James Barrineau, Leon County Department of Pollution Control, from Mr. Mark Stamps, Assistant Zoning Director, Tallahassee Leon County Planning Department, the proposed site is currently zoned Agricultural 2. The letter further states that an Agricultural 2 zoning allows a sanitary landfill as a permitted use. A small portion of the proposed sanitary landfill site is open to public view from,U.S. Highway 90 which is a major thoroughfare. It was estimated by a witness that the distance to the proposed site from that section of U.s. Highway 90 from which the site was open to public view was one (1) mile. An examination of the plot plan of.the proposed site contained in the application shows that at the closest point, the site boundary is approximately 2,000 feet from U.5 Highway 90. The site is screened from public view from most places on Highway 90 by the existing topography and ground cover.

Florida Laws (4) 403.702403.706403.7147.04
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ROBERT G. COLLINS vs. G. W. ELLSWORTH, PASCO COUNTY BOARD OF COUNTY COMMISSIONERS, AND DEPARTMENT OF ENVIRONMENTAL REGULATION, 89-000577 (1989)
Division of Administrative Hearings, Florida Number: 89-000577 Latest Update: May 23, 1989

The Issue The issue in this case is whether Pasco County's application for a permit to construct a Class III landfill should be approved by the Department of Environmental Regulation (Department). Pasco County called Robert Hauser, Jr., who was accepted as an expert in sanitary landfills, and the Department called Kim Ford, who was accepted as an expert in professional engineering with expertise in solid waste. Petitioner Collins testified on behalf of the Petitioners. Two exhibits were received on behalf of Pasco County and two on behalf of the Petitioners. One exhibit offered by Petitioners (P-3) was rejected. No transcript of the hearing was filed. The parties were given ten days following the hearing to file their proposed recommended orders, including proposed findings of fact. A ruling on each timely filed proposed finding of fact is included in the Appendix to this Recommended Order.

Findings Of Fact Pasco County filed an application with the department on or about January 29, 1983, to construct a Class III sanitary landfill. The location of the landfill would be near Hays Road and County Road 52, near Aripeka, in Pasco County, Florida. Pasco County owns the property on which the landfill would be located. After review, the Department issued an Intent to Issue on or about December 2, 1988, by which it proposed to issue Permit No. SC 51-144683 to Pasco County. The proposed landfill site is approximately 60 acres in size, with 20 acres to be used for disposal of household trash, yard trash consisting of grass clippings and other vegetative matter resulting from landscape maintenance or land clearing operations, construction or demolition debris, paper, cardboard, cloth, glass, street sweepings, vehicle tires, and other nonputrescible materials. Pasco County will install a 60 mil thick, high density polyethylene synthetic liner with a leachate collection system which is designed to eliminate discharge to the Floridan Aquifer within the landfill boundaries. An extensive geotechnical investigation of subsurface conditions at the site was conducted by the County's consultants in order to determine the suitability of the site for a Class III landfill, and to evaluate the ability of the site to provide an adequate foundation for the facility. Soil boring and ground penetrating radar were used. It was established that the site is of relatively uniform stratigraphy, characterized by a uniform layer of surficial sand, a reasonably continuous clay semi-confining layer from six to ten feet thick, under which lies the limestone groundwater bearing formation known as the Floridan Aquifer. The hydrogeological survey conducted by the County included a foundation analysis which demonstrates that the subgrade will support loads and stresses imposed by the proposed landfill. It also has a low potential for sinkhole development, and the synthetic liner and leachate collection system are reasonable mitigation steps which address sinkhole potentials. Pasco County's application includes a surface water management system, which has already received approval from the Southwest Florida Water Management District, and which is adequate to control surface water discharged from the Class III landfill site. The groundwater monitoring plan included in the application provides for no less that 10 pairs of monitor wells to be located approximately 100 feet from the boundary of the proposed landfill area. This meets the requirements of the Department, and is adequate to monitor both the surficial and Floridan Aquifer, and to provide early detection of any discharges to the groundwater. Reasonable assurances have been provided, through site specific geotechnical analysis and enhanced design features, that the site can be developed and operated as a Class III landfill without adverse impact to the Floridan Aquifer, despite the fact that the site is located in an area designated by the Southwest Florida Water Management District as a high recharge area. The County has demonstrated that it has the financial ability to construct, operate and close this Class III landfill in accordance with the Department's rules. The operations plan included in the County's application establishes the County's ability to operate the proposed landfill in accordance with rules of the Department. The proposed design of Pasco County's proposed Class III landfill offers reasonable assurances that the Department's standards will be met, and in fact, the design as proposed by the County exceeds the standards required by the Department for a Class III landfill, in that this project includes a liner and leachate collection system which are not mandatory. Competent substantial evidence was not presented by the Petitioners to establish that they would be substantially affected, or affected in any way, from the construction and operation of this Class III landfill.

Recommendation Based upon the foregoing, it is recommended that the Department issue Permit NO. SC 51-144683 to Pasco County. DONE AND ENTERED this 23rd of May, 1989 in Tallahassee, Florida. DONALD D. CONN Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 Filed with the Clerk of the Division of Administrative Hearings this 23rd day of May, 1989. APPENDIX The Petitioners did not file Proposed Findings of Fact. Rulings on Pasco County's Proposed Findings of Fact: 1. Adopted in Finding of Fact 3. 2-4. Adopted in Finding of Fact 5. 5. Adopted in Finding of Fact 4. 6-8. Adopted in Finding of Fact 6. 9. Adopted in Finding of Fact 11. 10-11. Adopted in Finding of Fact 7. 12. Adopted in Finding of Fact 10. 13-14. Adopted in Finding of Fact 8. 15. Adopted in Finding of Fact 9. Rulings on the Department's Proposed Findings of Fact: Adopted in Findings of Fact 1, 2. Rejected since this is a conclusion of law. Adopted in Finding of Fact 3. Adopted in Findings of Fact 4, 5, 11. Adopted in Finding of Fact 11. Adopted in Finding of Fact 7. Adopted in Finding of Fact 6. Adopted in Finding of Fact 7. Adopted in Finding of Fact 10. Adopted in Finding of Fact 9. Adopted in Finding of Fact 8. COPIES FURNISHED: Robert G. Collins 1750 Blue Heron Lane Spring Hill, FL 34610 Robert D. Odell 12636 Box Drive Rolling Oaks Estates Hudson, FL 34667 J. Ben Harrill, Esquire 7530 Little Road, Room 203 New Port Richey, FL 34654 Richard T. Donelan, Jr., Esquire Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Daniel H. Thompson, Esquire Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Dale Twatchmann, Secretary Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400

Florida Laws (1) 120.57
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SOUTHEAST HILLSBOROUGH CIVIC ASSOCIATION, INC. vs. HILLSBOROUGH COUNTY AND DEPARTMENT OF ENVIRONMENTAL REGULATION, 83-002378 (1983)
Division of Administrative Hearings, Florida Number: 83-002378 Latest Update: Dec. 30, 1983

Findings Of Fact The Petitioner, Southeast Hillsborough Civic Association, Inc. (SEHCA), is a corporate entity. The majority of its members reside in southeast Hillsborough County in the vicinity of the proposed landfill site. The Respondent, Department of Environmental Regulation (DER), is a state agency charged with regulating the construction and operation of sanitary landfills pursuant to Chapter 403, Florida Statutes, and Chapters 17-3, 17-4, 17-7, 17-9 and 17-25.04(5), Florida Administrative Code. The Respondent, Hillsborough County, Florida, is a political subdivision of the State of Florida. It is a local government entity which serves the areas within its geographical boundaries with traditional types of government services designed to promote and protect the public health, safety and welfare, including the collection and disposal of solid waste. Hillsborough County currently disposes of its solid waste at the Hillsborough Heights Landfill. The Hillsborough Heights Landfill is, however, nearing capacity, and the County is under a mandate, pursuant to a stipulation and settlement agreement executed with DER, to close the Hillsborough Heights Landfill by October 31, 1984. Accordingly, Hillsborough County must put in train the initial phases of construction of a new sanitary landfill in early 1984, once an appropriate site in terms of environmental considerations and other considerations is approved and the appropriate construction and operating permits issued. In August 1981, with a view toward the upcoming necessity to obtain a new sanitary landfill site, Hillsborough County hired the consulting and engineering firm of Camp, Dresser and McKee (CDM) to assist Hillsborough County in studying, identifying, evaluating, and ultimately selecting a new sanitary landfill site. CDM is an engineering consulting firm employing a team of engineers that specialize in the technical aspects of solid waste disposal and management and related landfill design and construction. Ardaman and Associates, Inc. (Ardaman), is an engineering and geotechnical consulting firm with extensive experience in geotechnical investigation and engineering pertinent to the construction of solid waste disposal facilities in Florida and elsewhere in the world. It employs engineers specializing in those functions. CDM and Ardaman, as well as certain Hillsborough County employees, conducted a detailed investigation of the subject site, collecting numerous soil samples and installing 22 monitoring or inspection wells. A multitude of analyses and tests were performed on the soil and water samples taken with the resulting information being used to prepare the designs for the landfill and concomitant data incorporated in the permit applications sub judice. On February 28, 1983, Hillsborough County filed an application for DER permits to construct and operate a solid waste resource recovery and management facility, as well as accompanying permit applications for the dredge and fill activities and storm water discharge facilities involved. After an extensive review process by DER in conjunction with the Hillsborough County Environmental Protection Commission (HCEPC) as well as the Southwest Florida Water Management District (SWFWMD), and after further responses and information in response to DER inquiry were filed by the permit applicant, DER gave notice of its intent to issue the permits to Hillsborough County for the proposed landfill, storm water drainage system, and related dredge and fill activity. The Petitioner, SEHCA, timely requested an administrative hearing concerning its opposition to the issuance of these permits. The proposed landfill will serve all the unincorporated portions of Hillsborough County, as well as the cities of Tampa, Temple Terrace, and Plant City. The current population of the County is approximately 650,000. The population of the County is expected to grow to 950,000 by the year 2000, and 1,375,000 by the year 2020. The landfill is expected to provide for the waste disposal needs of the County for a minimum of 34 to a maximum of 40 years and is proposed to be the County's only landfill until approximately the year 2020. The proposed landfill would occupy approximately 175 acres out of a total of 1,100 acres at the proposed site, such that there is land available at the site that can be used for landfill purposes after the ultimate completion of the landfill at issue herein. Hillsborough County must presently dispose of approximately 2,000 tons of solid waste per day, or approximately 650,000 tons per year. By the year 2015, the County will be required to dispose of in excess of a million tons of solid waste per year. The proposed landfill would receive only nonhazardous, solid waste. It would not accept hazardous or toxic waste, infectious material, hospital waste, liquid waste, septic tank or sewer plant sludges, or similar toxic or hazardous material. The material placed in the landfill would consist of only domestic waste, debris from demolition, construction debris, and other nonhazardous items. In 1987, Hillsborough County and the City of Tampa will both have resource recovery incineration facilities in operation. These facilities will burn approximately 85 percent of the solid waste generated in Hillsborough County and the City of Tampa, with concomitant energy generation. After these resource recovery facilities are placed in operation, the proposed landfill would receive mostly ash from the resource recovery incineration process, as well as some nonburnable waste such as construction debris and demolition debris, and any solid waste which may be generated by the various cities and County which exceeds the capacity of the resource recovery incineration facilities. Thus, since the resource recovery facilities will reduce the volume of the County's solid waste to ash, that volume entering the landfill will be reduced by as much as 90 percent by 1987 or shortly thereafter. The Site The landfill site is in a remote area of southeast Hillsborough County approximately 25 miles from downtown Tampa. The site is two miles northwest of the community of "Picnic," which lies at the intersection of County Road 39 and County Road 672. The nearest paved county road is approximately a half-mile from the site. The site contains approximately 1,100 acres of land within the boundaries. The remainder of the property in excess of the 175 acres used for the proposed landfill will be used for buffer zones, borrow areas, and ancillary facilities as well as land which could be used for an additional landfill facility in the remote future. Hillsborough County also has acquired land to be used as a buffer zone on the southeast corner of the site and land which will be used for the access road to the landfill from County Road 672. The site is located in a large phospate mine, which was started in 1945 and abandoned since 1965. The site is surrounded by a buffer zone consisting of citrus groves, woods, rangeland, and other phosphate mining areas. The orange groves and trees on the southern side of the property create an effective visual barrier between the site and the nearest public road. The closest residence is in excess of 1,000 feet from the site boundary and at a greater distance from the actual landfill site, which lies some distance inside the site boundary. The two closest homes, lying slightly over 1,000 feet and approximately 1,500 feet from the subject property boundaries, both use deep wells in the Floridan Aquifer for potable water. There are only 17 to 20 residences within a mile of the property boundary. Most of these homes are located south of the landfill site along County Road 672. A few additional residences are located a mile or more from the site east along Counts Road 39. The character of the land within several miles of the site is essentially rural, with no large residential subdivisions or commercial development within several miles of the site. The County zoning at the site is "A" and "AA," and is such that a government-owned and operated landfill will be permitted in both of these zoning districts. Landfill Design The design of the landfill includes three major components: a clay liner; a permanent leachate collection system; and a storm water drainage system. The landfill will be built on an unmined clay settling area which was constructed and filled with clay during the former mining operation on the site. Starting in 1945, clay from the phosphate mine was pumped into the settling area together with water obtained by the mining operation from deep wells in the Floridan Aquifer. It was pumped into the clay settling area in a liquid or semi-liquid state and allowed to consolidate and solidify. The clay will provide an appropriate liner for the bottom of the landfill. The site investigation by Ardaman reveals that the clay has a very low permeability (10- 8, or .00000001 cm. per second). The landfill and solid waste deposited therein will be placed only in areas with a minimum thickness of clay liner of at least four feet. The clay liner ranges in thickness at the precise landfill site from a minimum of four feet, up to 21 feet. In comparison, many landfills of acceptable design have a liner of 18 inches to two feet thick. By limiting the landfill to areas where the clay is a minimum of four feet in thickness, the liner's depth and continuity across the landfill is assured in terms of providing protection for groundwater resources from landfill leachate percolation. The clay will prevent leachate (water percolating through the landfill which picks up suspended or dissolved pollutants from the solid waste) from moving out of the landfill. Due to the clay's extremely low permeability there is an insignificant likelihood of any leachate ever escaping through the clay liner. As the construction of the landfill progresses, the clay will settle and further consolidate under the weight of the refuse. The clay will then in effect form a large bowl that will collect leachate. To insure the structural stability of the clay underlying the landfill, the landfill will be built in several phases. A planned sequence of "loading" operations will be carried out to allow the clay to settle in a carefully controlled manner. Ardaman's calculations in evidence establish that the sequence of loading operations will have a large safety factor in that the structural strength of the clay will be greater than necessary to support the weight of the proposed landfill. As the clay consolidates, the water in the clay will be squeezed out, and approximately one-half of the groundwater in the clay at the present time will migrate upward into the leachate collection system. The other 50 percent or so of the water content of the clay will migrate in a downward direction into the surficial groundwater aquifer over a period of the entire 40-year estimated life of the landfill. Since water will be flowing upward from the clay into the leachate collection system, it was undisputed that leachate will not be able to flow downward into the clay during the active life of the landfill because of the positive, upward hydraulic head developed (aside from the impermeable nature of the clay). The leachate will thus be somewhat diluted by the groundwater migrating upward from the clay liner. The leachate will be automatically pumped out of a collection sump as long as the landfill operation is going on and after it is completed. Once the landfilling operations are completed, the landfill will be covered with a clay or "synthetic cap" to prevent any water from entering the landfill and forming leachate in the future after the landfill operation is phased out. Should any leachate enter the clay liner, the clay would act as a filter and partial treatment medium for any liquid that moves through it. For example, clay will remove heavy metals from the leachate such that the fluid emerging ultimately from the bottom of the clay liner would be filtered and partially treated. Thus, the clay liner has very low permeability, is continuous and homogenous, and provides long-term protection for ground and surface waters by preventing any leachate from escaping from the landfill itself. Leachate Collection System A permanent leachate collection system will be used in the operation of the landfill. The system is designed to collect and remove all leachate resulting from percolation of rainfall through the refuse in the landfill before it can percolate to groundwater or move in a lateral direction so as to enter the ground or surface waters of the state. The leachate collection system is based on conservative design assumptions, in that it is designed to collect and remove all water moving up from the clay as the clay liner consolidates, as well as water which has moved downward through the landfill. The water will move into the leachate collection system for the entire 40-year life of the landfill and beyond, but the design parameters for the leachate collection system were based upon the conservative assumption that all the water from the clay-settling area would migrate upward into the leachate collection system during the first ten years of landfill operations. Thus, the calculations upon which the leachate collection system design was predicated included this intentionally inflated prediction about the amount of leachate that will be generated and handled by the system. The amount of leachate actually produced will be substantially less than the amount predicted and the leachate collection system was shown to be based on sound engineering principles. The leachate collection system will be constructed by placing from three to eight feet of sand over the clay liner of the landfill. Trenches two feet wide by two feet deep will then be dug at 200-foot intervals and filled with drainfield rock averaging 1 1/2 inches in diameter. The trenches thus serve as conduits to collect leachate percolating downward through the landfill refuse and drain it to a central sump where the leachate will be pumped out by automatic pumps which operate when the leachate level in the sump reaches a certain height. Backup pumping capacity is provided to avoid overflow of leachate out of the sump and out of the side of the landfill in the event of mechanical breakdown. No leachate is expected to be generated for approximately the first three years of landfill operation since the refuse will act in the nature of a sponge to soak up and retain water entering the landfill for approximately that period of time. Once leachate is produced and collected in the sump, however, it will be pumped into active areas of landfill for recirculation through the landfill. Recirculating leachate was established to be an acceptable form of pretreatment or partial treatment for leachate. Recirculation by percolating leachate back through the refuse in the landfill evaporates some water and causes some of the pollutants to be absorbed by the refuse and soil in the landfill, reducing the total amount of leachate produced which must be removed from the landfill site. In the instant situation, any excess liquid leachate will be pumped out of the sumps, stored in storage tanks and periodically removed and trucked to a county wastewater treatment facility for treatment. Wastewater treatment plants of the secondary treatment mode are capable of adequately treating landfill leachate. The County, however, expressed a willingness to construct a treatment plant at the landfill site for specifically treating leachate from the landfill as an alternative to trucking leachate to a nearby county wastewater treatment plant should this method be more efficacious in preventing landfill leachate causing a deleterious effect on surface waters of the state, either at the landfill site or as a component of effluent from a nonspecifically designed wastewater treatment plant. Storm Water Drainage System In addition to the actual construction permit application for the landfill itself, the county has submitted an application for construction and operation of a storm water drainage system to be used in conjunction with the landfill operation. The DER performance standards for storm water drainage systems are contained in Rule 17-25.04(5), Florida Administrative Code. In effect, such a storm water system must drain and filter runoff from the first one inch of rainfall which falls on a given area within 72 hours. This rule presumes that such a capacity provides reasonable assurances that all applicable DER water quality standards will thus be met. In point of fact, it was established that primary pollutants carried by storm water runoff are flushed from the surface of land and in effect "bound up" in the first one-half inch of rainfall. The proposed storm water system to be used in conjunction with the landfill will meet this performance standard. It was undisputed that the storm water system will indeed collect, detain, and filter the runoff from the first inch of rainfall within 72 hours at the site. The system can handle and filter larger amounts of rainfall and, indeed, when initially installed, the system will filter runoff from the first inch of rainfall occurring within 24 to 36 hours. The storm water drainage system is designed to keep storm water completely separate and physically apart from the landfill itself and thus to prevent leachate from entering the storm water drainage system and vice versa. Rainwater falling on the active landfill itself will move through the landfill vertically, percolate through the refuse and soil, and be collected as leachate in the leachate collection system, with subsequent treatment. Rainfall falling on the surrounding portions of the landfill site will not contact refuse, but, rather, will flow laterally into the storm water drainage system basins, where it will be filtered to remove silt, sediment, and other degradatory materials. Thus, the water entering the storm water system will be rainwater, together with any sediments or other materials nicked up during the course of its drainage over soil and land, with no contact with refuse or related pollutants. The filter medium in the storm water basins will consist of clean sand. The basins will consist of berm walls and at least two feet of clean sand in the bottom as the filter medium. The approximately six basins and drainage swales will serve as a filtration-treatment mode, as well as retention ponds, as a method of storm water treatment. A drainage swale will be used to filter storm water runoff from the access road. This method of storm water filtration and treatment has been shown to be acceptable on other landfills similarly designed and to be the most effective method of filtration and treatment of storm water related to such a landfill operation. The storm water system will thus reduce the potential for pollution in the streams near the site which will receive the filtered storm water after it is ultimately discharged from the basins and retention ponds and swales. Presently, the sand, sediment, clay, and other materials on the site are washed into the streams by storms. After the landfill is constructed and operating, the storm water flowing off the sites will also be filtered and treated in accordance with DER standards. Particulate matter in the storm water runoff will be collected in the basins. Periodic monitoring of the effectiveness of the storm water treatment basins and swales should be performed to ensure the filter medium continues to function effectively as opposed to becoming clogged with silt deposits with resultant overflow of unfiltered storm water over the tops of the basin berms. Water Quality Hillsborough County has conducted a ground and surface water monitoring program to evaluate the existing water quality at the site. This was done through the installation of monitoring wells and concomitant sampling of the water in those wells for water quality parameters in accordance with DER rules. The ground and surface water at the site will be regularly monitored throughout the life of the landfill through the use of monitor wells and other means. Parenthetically, it should be noted that the DER rules require a minimum of three monitor wells to be installed at Class I landfills such as this. Hillsborough County has installed nine monitor wells and performed evaluation and testing of water quality of water samples collected from all nine of those wells. That monitoring program included tests for "indicators," that is, substances that would reveal whether a need for further testing existed. Such tests were performed both at the groundwater monitoring well sites, as well as surface water sampling locations over the entire landfill site. The tests indicated elevated concentrations of total organic carbon in the groundwater. Steve Boyes, an employee of DER, was tendered and accepted as an expert on water quality at phosphate mine sites. He established that the total organic carbon concentrations found in certain groundwater samples came from naturally occurring organic material in the groundwater. Test data supported that conclusion. The wells with elevated levels of total organic carbon collected water from an area in the soil which contained roots and other decomposing organic matter. The organic carbon concentration noted in certain groundwater monitoring wells is a naturally occurring instance. There is no DER water quality standard extant in the rules for total organic carbon. It was not demonstrated to have any deleterious effect on human health, and the installation and operation of the landfill was not shown to cause or enhance any deleterious effect on surface or ground waters of the state (or its citizens) which might be occasioned by the elevated carbon concentrations in groundwater at portions of the site. The phosphate mine which formerly operated at the subject site was known as the Boyette Washer Mine. Initially, in the first years of its operation, it used what is called a "single stage washing process" to separate the phosphate from clay. In this process, the clay, sand, and phosphate were separated simply by hydraulic means, that is, being washed with water from deep wells in the Florida Aquifer. The clay and water was then pumped into a clay- settling area. No chemicals were used for separation of the phosphate in this process. The clay-settling area in which the clay and process water was pumped is now the subject landfill site, the clay being naturally consolidated over time and which will be further consolidated in the construction process of the landfill into the "clay liner." After several years (approximately in 1955), the mine operators built a first-stage flotation plant which used caustic soda, tall oil (fatty acids), and fuel oil to separate the fine clay materials from the phosphate. Tom Holland, a witness for the Petitioner, worked as the mine supervisor for a substantial number of years. He established that most of the clay discharge in the clay-settling area came from the washer process as opposed to the flotation process. The clay-settling area was almost full of clay before the flotation plant began operation. Dr. Garlanger is a former professor at the Massachusetts Institute of Technology and was tendered and accepted as an expert witness on clay waste disposal. He presented a study of water quality data collected from six phosphate mines using the same treatment processes. Clay samples were taken out of these similar or typical phosphate mines for purposes of comparison to the water-clay characteristics of landfill sites. For purposes of that study, the water was squeezed from clay taken from those six representative clay-settling areas. The data from those sites showed that normally the water embodied in the clay meets the Department's primary and secondary drinking water standards. At the proposed landfill site, the water squeezed from clay samples taken from the bottom of the clay-settling area would be the same or better quality than those from other mine locations, since only clay and water were pumped into the settling area for several years before any flotation process was begun at the mine. During that time the only substances going into the bottom of the clay- settling area were clay and drinking water obtained from deep wells in the Florida Aquifer, the primary source of potable drinking water for this portion of the state. Thus, any water migrating downward from the bottom of the clay- settling area, or clay liner, would be uncontaminated water which meets drinking water standards, inasmuch as the high impermeability of the clay liner would prevent pollutants migrating from above in the form of landfill leachate. It would be a better quality than the water collected at the six other mine sites because the samples collected from those clay-settling areas were collected at the top and thus contained the process water from the flotation plants at those mines. Even so, those samples still met DER's primary and secondary drinking water standards. Data collected from this landfill site confirms these findings. Hillsborough County performed water quality analyses for "priority pollutants" on water samples taken from a number of locations around the site. These analyses were designed to identify any pollutant which might have been deposited at the site in the mines' process water, including benzine and kerosene compounds. Hundreds of analyses were performed, and all of the priority pollutant tests were negative. There are no priority pollutants such as benzine or kerosene in the groundwater at the landfill site. The results of this detailed investigation, in evidence, establish that the quality of water in the clay at the site, if squeezed out of the bottom of the clay liner in the present clay-settling area of the old mine, will not contribute to any water quality violations of pertinent rules. To ensure this result, the County has agreed to regularly monitor and test the ground and surface water at the site throughout the life of the landfill. The Petitioner presented no contrary water quality data. Two lay witnesses living near the site have fished in the mine-cut lakes near the landfill site, but which are not involved in the landfill construction and operation. These witnesses have noted a kerosene-like flavor in fish consumed which were caught from these "mine-cut lakes." The cause of that peculiar taste in the fish was not demonstrated, and no evidence was presented to establish that the taste was caused by water from the clay-settling area, which is the only part of the former phosphate mine site involved in this proceeding. Radioactivity In the course of performance of the water quality analyses referred to above, the radioactivity in the groundwater at the site was evaluated. Levels of radium 226 in the filtered water sample were within DER standards. There were, however, elevated levels of gross alpha radiation in two of the test wells. Dr. Emmett Bolch, a professor of radiation-related studies at the University of Florida, and Dr. John Garlanger established that the elevated levels of gross alpha radiation are caused by naturally occurring deposits of radioactive minerals in the "leach zones" on top of the "Bone Valley formation" lying beneath the landfill site. The leach zone is the weathered, fissured surface of this Bone Valley formation, which was weathered during exposure to the atmosphere and elements at remote geologic times. Radioactive minerals were then deposited by alluvial action in the fissured surface, and at later geologic times, the leach zone of the Bone Valley phosphate-bearing formation was covered with sand, silt, and other materials. The Petitioner's expert witness agreed that gross alpha radiation in the groundwater was a naturally occurring phenomenon. Excessive levels of gross alpha radiation do not typically occur in clay-settling areas such as the one where the landfill would be built. Dr. Bolch has substantial experience with the study of radiation levels at phosphate mines throughout Florida. The radiation level in water contained in clay- settling areas is normally well within the applicable Department standards, but, in any event, the radioactive material in clay-settling areas is primarily bound up in the particles and sediment. Once water moves through the ground in clay- settling areas, these radioactive particles are filtered out, thus no significant level of radioactivity could leave the clay-settling area in the groundwater. Although unfiltered samples containing radioactive sediment and particles may demonstrate elevated radioactivity, filtered water samples from clay-settling areas routinely meet DER standards for radiation. These filtered samples of water are more representative of typical drinking water which citizens would obtain from the surficial aquifer, to the extent that they use shallow wells. This thesis by Drs. Bolch and Garlanger is factually established by the water quality data obtained at the instant site. Test Hole 28, one of the County's monitor wells, is located hydrologically down-gradient from the clay- settling area. Water flows from the clay-settling area and passes through Test Hole 28. The water quality in Test Hole 28 is representative of the water quality in the clay-settling area. Nonetheless, the filtered sample collected from Test Hole 28 on October 14, 1983, contained 11.6 pci/liter of gross alpha radiation [see Exhibit 84(c)]. This is well within the DER standard of 15 pci/liter. Thus, the water quality tests for these sites establish that groundwater flowing out of the clay-settling area does not contain elevated levels of gross alpha radiation. On the other hand, high levels of gross alpha were found in Test Hole 22, which lies up-gradient (hydrologically upstream) from the clay-settling area. Since the water from a clay-settling area would not flow in an uphill direction, the high gross alpha content in Test Hole 22 would not have come from the clay-settling area, nor would the higher level of radiation found in that test hole leave the clay-settling area and migrate off the landfill site. It is noteworthy that Test Hole 22 is located on land that has not been mined. The higher level of radiation found in that well is clearly naturally-occurring, and its concentration has not been enhanced by any man-made technological process. Accordingly, it has been established that the water coming from the bottom of the clay liner will meet DER primary and secondary drinking water standards. It will not have elevated levels of radioactivity. Steve Boyes, a DER hydrologist and expert witness on groundwater impacts of the phosphate mining process, established that there is a very low, extremely remote possibility that the landfill will ever have any effect on any drinking water supply. Operation and Maintenance of Landfill Most of the refuse was brought to the landfill in a closed transfer truck from transfer stations set up by the County. The refuse will be inspected at the transfer station before it is loaded on the trucks for transportation to the landfill. At the entrance to the landfill, trucks will be weighed and inspected for chemical or hazardous wastes which cannot be placed in the landfill and then will he directed to the active "working face" of the landfill. Two full-time employee-inspectors will be on duty at the working face to visually inspect the refuse as it is placed on the landfill. The refuse will be spread across the working face and compacted in layers. At the end of the working day, at least six inches of daily cover material will be placed over the refuse. A 12-inch layer of intermediate cover material will be placed over areas not to be used again for several months. After an area of "lift" has been filled to its maximum elevation, a two-foot layer of final, permanent cover will be placed over it. All cover material is available on the site. The daily cover material will consist primarily of sand obtained from the sand tailings pile at the mine site. The sand material was established to be an appropriate daily cover material. It is readily workable and, unlike clay, can be used under adverse weather conditions, such as prolonged rainfall. A sand-clay mix would not be an adequate cover material for daily use; it is not as easily workable, especially when wet, and would create a relatively impermeable cap, which could cause methane to build up beneath it in the landfill. When a new lift or cell is built on the landfill, additional refuse is placed over the preceding daily cover. If sand is used for daily cover, any leachate in the new material can readily pass through the sand and appropriately enter the leachate collection system. If a sand-clay or all-clay mix were used, the leachate would not be able to percolate downward and would form pockets or pools at various levels in the landfill rather than flowing downward into the leachate collection system. These pools of leachate would then break out of the sides of the landfill and possibly pollute surface waters of the state by entry into the storm water system or otherwise. Routine maintenance practices at the landfill will prevent potential problems such as this from developing. Regular frequent inspections will be made around the entire landfill. Movable litter fences will be erected around the working face to retard dispersal of windblown litter. Work crews will regularly pick up any litter on access roads, which problem will largely be prevented initially through the use of covered trucks for transportation of refuse into the landfill. The storm water basin and drainage system must be regularly inspected and maintained to prevent sedimentation clogging. The most likely operational problems typically occurring at such a landfill can largely be prevented by regular inspection and routine maintenance. In this connection, the sanitary engineer's office of the county should maintain a qualified county employee in sanitary landfill operations to oversee the correct operation of the landfill, especially if operation of the landfill is performed by a private contractor or agent. Methane Gas As organic material such as discarded food, grass clippings, etc., decomposes, it produces methane gas. The ash and residue from the resource recovery facilities, once they become operational, will not produce methane gas when deposited in the landfill, since that refuse would already be burned. Since there will be limited amounts of organic solid waste going into the landfill after 1987, the potential for methane gas generation is limited. The daily cover material of sand is highly permeable and will allow methane gas generated to escape to the atmosphere in a harmless fashion. If methane gas is seen to accumulate in an adverse manner inside the landfill, the County will construct vents at appropriate locations on the landfill to allow methane to escape to the atmosphere. As established by Dr. Urone, the Petitioner's own expert on air pollution, the release of methane gas to the atmosphere will not violate any air quality standards or cause human health problems. Odor Odor at landfills is caused by decomposition of organic matter. As in the case of methane gas, the potential for odor generation will be greatly reduced after 1987 because the landfill will only receive limited quantities of unburned organic waste. Potential odor problems at landfills normally are eliminated by appropriate and regular application of the daily cover material over the refuse. If daily cover material is properly used, there will be no noticeable odor beyond the site boundary of the landfill. The applicant should be required, as a condition to a grant of the subject permits, to agree to weekly inspections by both the Hillsborough County Environmental Protection Commission and/or DER to ensure that the landfill is operated in compliance with all the permit conditions, including the condition that odor be unnoticeable beyond the site boundary. If an odor problem develops, the Department should require Hillsborough County to place additional thicknesses of cover material over the solid waste daily, as well as to require a different cover material should the sand cover material prove inappropriate. Dust Control Dust control of the site will be accomplished by water spraying which will be used on access roads, working roads within the landfill itself, and at the working face and all construction areas. The roads on the site will be paved or coated with soil cement to reduce airborne dust. Further, the size of the working face and the borrow area will be kept to a minimum to reduce the potential for airborne dust. Petitioner's expert on air pollution, Dr. Urone, acknowledged that these standard, well-known dust control practices would be sufficient to control airborne dust problems. Airborne Radiation Hillsborough County's radiation expert, Dr. Bolch, calculated the potential radiation caused by dust emissions at the site due to landfill operations. His calculations are based on a "worse case" scenario concerning dust-borne radiation emissions. Radiation from dust emissions at the landfill site will be insignificant. Currently, radon gas is released from the clay- settling area and the sand tailings pile. When the landfill is built, however, the sand and clay obtained from the sand tailings pile and clay in the clay liner will be buried at the bottom of the landfill, except for the sand deposited as daily cover at the current working face. By the burying of the other sand and clay used in the landfill beneath the landfill, the landfill itself will actually create a barrier to prevent radon gas from entering the atmosphere beyond that minute amount present in the daily cover material on an active landfill "lift." Thus, the landfill will actually somewhat reduce the current radon gas emissions naturally occurring at the site. The radon gas was not demonstrated to have any health impact on people working at the site nor on surrounding residents. Nor were existing levels of gamma radiation at the site shown to have any human health impact. Sink Holes The likelihood of a sink hole occurrence at the proposed landfill is very low. Dr. John Garlanger of Ardaman and Associates was accepted without objection as an expert in the area of soil mechanics, clay waste disposal, hydrogeology, and sink hole formation. He is a member of the advisory board for sink hole research at the University of South Florida and has published numerous papers and articles on the remediation of sink holes and their causes. He directed the subsurface hydrogeologic investigation at the landfill site preparatory to filing the permit applications. The overburden soil at the immediate site of the landfill is approximately 22 feet thick, with the phosphate bearing Bone Valley formation underlying that, for a depth of approximately 20 feet. Below that formation is the dense Hawthorne formation of an approximate 105-foot thickness, before the Tampa Limestone strata, which encompasses the Floridan Aquifer, is reached. Because of the great thickness of the Hawthorne formation, which is quite dense and which serves to protect the limestone underlying it from fissure development caused by percolation of ground water (which can ultimately result in sink hole formation), there is a scant likelihood of sink holes developing beneath or in the immediate vicinity of the landfill which could cause a deleterious impact on ground water supplies in the area. The likelihood of a sink hole developing at the proposed site is much lower than in other areas of Hillsborough County to the north, northeast, and northwest. The fact is corroborated by the investigation of Southwest Florida Water Management District which establishes that indeed the site has a low potential for sink hole development (DER Exhibit 5). 2/ Dredge and Fill Activities The proposed dredge and fill activities at the landfill consist of the installation of several culverts for road crossings and similar minor activities. The proposed activities were designed to minimize any potential impacts on state waters. Hillsborough County will use turbidity curtains and other recognized techniques for controlling erosion, sedimentation and other impacts from these activities. In this regard, there is no contiguous connection between the clay-settling area where the landfill will be constructed and any surface water body. A culvert is located passing through a berm or dike on the southwest side of the clay-settling area, but the culvert only discharges water on rare occasions of extreme rainfall. The vegetation near the culvert shows that the rainwater standing on the clay-settling area rarely rises to a level which would cause a discharge from that basin. Similarly, with regard to the lakes on the southeast side of the county's property, which are not involved in the area of the proposed landfill construction and operation, there is no contiguous surface water connection between those lakes and the surface waters located off the site. There is some groundwater seepage from the foot of a dike, but no regular flow over the top of the dike connecting to any surface water body was established. In any event, the proposed activities would have no significant short- or long-term adverse impacts on water quality. The Petitioner relied on the testimony of two expert witnesses, Drs. Carnahan and Urone. Drs. Carnahan and Urone collected no soil, water, or air samples and performed no laboratory tests nor independent calculations or analyses. Dr. Carnahan read the permit application less than a week before the final hearing and visited the site only on the day before his testimony. Dr. Urone never visited the landfill site. Dr. Urone was proffered as an expert in air pollution, but he has no prior experience with the construction and operation of landfills in terms of their air pollution potential. Dr. Urone opines that there could be a potential odor problem at the landfill, but has done no analysis or investigation regarding this potential problem at the subject landfill site, or any other similar landfill, to calculate the amount of potential odor which could be generated. He admittedly is not an expert concerning the use of soil cover to control odors at landfills. He refrained from expressing an opinion about the suitability of the proposed daily, intermediate, and final soil covers. Further, Dr. Urone acknowledges that the methane gas in itself, in the concentrations to be expected from such a landfill, would have no significant impact on air quality. He further admitted he was unable to estimate what would occur at the subject site in terms of airborne dust emissions, but acknowledged that they could be controlled by using well-known dust control techniques such as those found above. Finally, Dr. Urone admits that if the landfill was operated in a manner described in the permit application documents which he reviewed, then there should be no health problem as that is defined by current health standards, nor did he expect any violation of air quality standards. Based on a limited review of the permit application materials, both Drs. Carnahan and Urone expressed only general concerns about the effects of the proposed project. Finally, Dr. Carnahan admitted the thoroughness of the investigation and site evaluation performed by Respondent's expert witnesses in these subject areas and did not dispute the result of their investigations (in evidence). Thus, the testimony of the expert witnesses presented by the County in the above subject areas is accepted.

Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence in the record, the candor and demeanor of the witnesses, and the pleadings and arguments of the parties, it is, therefore, RECOMMENDED: That the Department of Environmental Regulation issue permits to Hillsborough County for the construction and operation of the proposed Southeast Hillsborough County landfill and for the attendant storm water drainage system and dredge and fill operations, subject to the following conditions: That the Hillsborough County Environmental Protection Commission and/or DER ensure that the landfill operation is inspected by duly qualified personnel on a weekly basis; That the county have a qualified employee on the site daily to ensure that the landfill and storm water drainage system is being consistently operated properly; That the Department should take background water samples from wells of the residents living within one mile of the site before construction and operation of the landfill commences to establish background data by which to measure the quality and safety of the later landfill operation in terms of any impacts on groundwater quality, which water quality should be periodically monitored in a similar manner thereafter. DONE AND ENTERED this 29th day of December, 1983, at Tallahassee, Florida. P. MICHAEL RUFF Hearing Officer Division of Administrative Hearings Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 FILED with the Clerk of the Division of Administrative Hearings this 30th day of December, 1983. COPIES FURNISHED: Thomas W. Reese, Esquire 123 Eighth Street, North St. Petersburg, Florida 33701 William W. Deane, Esquire Douglas MacLaughlin, Esquire Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32301 Jacob D. Varn, Esquire David S. Dee, Esquire Suite 410, Lewis State Bank Building Post Office Drawer 190 Tallahassee, Florida 32302 Ms. Victoria Tschinkel Secretary Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32301

Florida Laws (9) 120.57403.031403.088403.182403.7045403.707404.0517.0390.203
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