The Issue This is a procurement protest. The ultimate issue is whether the Respondent’s award of the "Agreement for the Construction and Operation of a Seawater Desalination Plant and Water Purchase Agreement" ("WPA") to Intervenor, S & W Water, LLC ("S&W") on July 19, 1999, is contrary to Tampa Bay Water's (TBW’s) governing statutes, its rules or policies, or the proposal specifications, or is clearly erroneous, contrary to competition, arbitrary, or capricious. Additional issues presented for decision are: (1) whether Petitioner has standing to maintain this protest; and (2) whether, by participating in the procurement process, Petitioner has waived or is estopped from claiming irregularities arising out of that process.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is recommended that TBW enter a Final Order denying Petitioner's Formal Protest. Jurisdiction is reserved for consideration of S&W's request for a determination of improper purpose under Section 120.595(1), Florida Statutes, if such request is made by motion within 10 days from the issuance of this Recommended Order. DONE AND ENTERED this 25th day of October, 1999, in Tallahassee, Leon County, Florida. J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 25th day of October, 1999. COPIES FURNISHED: Charles W. Pittman, Esquire 400 North Tampa Street Suite 1040 Tampa, Florida 33602 Richard A. Harrison, Esquire John W. Wilcox, Esquire Allen, Dell, Frank & Trinkle, P.A. Post Office Box 2111 Barnett Plaza, Suite 1240 101 E. Kennedy Boulevard Tampa, Florida 33601-2111 Donald D. Conn, General Counsel Tampa Bay Water 2535 Landmark Drive Suite 211 Clearwater, Florida 33761-3950 John H. Rains, III, Esquire Annis, Mitchell, Cockey, Edwards & Roehn, P.A. Post Office Box 3433 One Tampa City Center, Suite 2100 Tampa, Florida 33601
Findings Of Fact Background In 1983, Concerned Citizens of Citrus County, Inc. (Concerned Citizens), an intervenor in this case, filed a petition toe initiate rulemaking for single source reclassification of groundwater under the existing provisions of Rule 17-3.403, Florida Administrative Code (F.A.C.). In this manner, Concerned Citizens sought to have existent potable waters in Pinellas, Hillsborough, Pasco, Hernando, and Citrus Counties classified Class G-I groundwater, and to thereby provide them the most stringent water quality protection accorded groundwaters of the state. At a public meeting in February 1985, the Environmental Regulation Commission (ERC) deferred action on the petition of Concerned Citizens, and directed the Department of Environmental Regulation (Department) to review the existing G-I rule, prepare proposed revisions, and present its recommendations to the ERC. Following the ERC directive, the Department held numerous public meetings and workshops to explore different approaches to groundwater protection. As a consequence, it prepared the proposed revisions to Rules 17-3.021, 17-3.403, 17-3.404, and 17- 4.245, F.A.C., at issue in these proceedings. On October 31, 1986, the Department duly noticed the proposed rules in volume 12, number 44, of the Florida Administrative Weekly. The notice interested parties that a public hearing would be held on December 16, 1986, before the ERC. 1/ On December 16-17, 1986, the ERC held a public hearing at which time it considered the rules recommended by the Department. During the course of this meeting, the ERC approved and adopted the rules with certain changes. These changes were duly noticed in volume 13, number 3, of the Florida Administrative Weekly on January 16, 1987. Petitioners and Intervenors Petitioners, Adam Smith Enterprises, Inc., and Alliance for Rational Groundwater Rules (Case No. 86-4492RP), and Petitioners Aloha Utilities, Inc.; Interphase, Inc.; Phase 1 Homes, Inc.; A.C. & R., Inc.; Tahitian Development, Inc.; Great Cypress Mobile Village, Inc.; and Barrington, Ltd. (Case No. 86- 4705R), filed timely petitions to challenge the validity of the proposed rules, which petitions were consolidated for hearing. Petitions for leave to intervene were granted on behalf of Florida Electric Power Coordinating Group, Inc.; Florida Land Council, Inc.; and Pasco County. These Intervenors' interests were aligned with those of petitioners. Petitions for leave to intervene were a1so granted on behalf of West Coast Regional Water Supply Authority and Concerned Citizens of Citrus County, Inc. These Intervenors' interests were aligned with those of the Department and the ERC. Petitioner, Adam Smith Enterprises, Inc. (Adam Smith), is the owner/developer of a 3,800-acre development of regional impact (DRI) to be known as Trinity Communities. This development, which has been in the acquisition and planning stages for almost 5 years, is currently undergoing DRI review and Adam Smith anticipates that it will receive its development order by September 1987. The Trinity Communities development is located predominately in Pasco County, with just over 250 acres of its lands located in Pinellas County. These properties are predominately open pasture land, and are bordered on the north, east and west by roads and on the south by Hillsborough and Pinellas Counties. As proposed, the Trinity Communities development will include 1100 acres of parks, golf courses, and other open areas. The remaining lands will be developed to accommodate 9500 dwelling units, as well as industrial and commercial uses to service the community, over a 20-year period. At today's market value, the property represents an investment of approximately 28 million dollars. Abutting the Trinity Communities development is the Eldridge-Wilde Well Field. This well field is covered by consumptive use permits issued by the Southwest Florida Water Management District (SWFWMD), and contains major public community drinking water supply wells as defined by the rules at issue in this proceeding. Of these wells, 5 are located within 9.63 feet and 181.5 feet of the proposed development's property line, and 5 are located with 204.72 fee and 297.5 feet of its property line. Petitioner, Alliance for Rational Groundwater Rules (Alliance), is an association of landowners who united to educate themselves about the proposed rules. The proof failed, however, to establish whether Alliance had ever elected any officers or directors, or the magnitude of its membership. Consequently, the proof failed to establish that a substantial number of its members, although not necessarily a majority, were substantially affected by the proposed rules, and that the relief requested by it was of a type appropriate for it to receive on behalf of its members. Petitioner, Aloha Utilities, Inc. (Aloha Utilities), is a utility certified by the Florida Public Service Commission to provide water and sewer service to two separate service areas in southern Pasco County. Currently, Aloha Utilities operates an 850,000 gallon per day (gpd) sewage treatment facility (Aloha Gardens) and a 1.2 million gpd sewage treatment plant (Seven Springs). It also operates 10-11 producing wells, at least 7 of which are permitted by SWFWMD to withdraw at least 100,000 gpd. One of these wells is located approximately 1/4-1/2 mile from an Aloha Utility sewage treatment plant. At least 3 of Aloha Utilities' wells which are permitted to withdraw 100,000 gpd or more, will service or are servicing the Riverside projects and Aloha Gardens Unit Number 12 project discussed infra. Consequently, the proof establishes that Aloha Utilities operates a major public community drinking water supply system as defined by the subject rules. The Aloha Gardens facility is under a Department order to expand its effluent disposal capacity. To satisfy the Department's order and the need for increased disposal capacity, Aloha Utilities commenced condemnation proceedings 8-12 months ago to secure the needed property. While the condemnation proceeding is not yet completed, Aloha Utilities has already expended considerable sums for engineering studies and attorney's fees in its efforts to acquire the property. That property is located approximately 1/2 mile from an existing well that is permitted for an average daily flow of at least 100,000 gpd. The effluent disposal capacity of the Seven Springs facility is also being expanded to meet existing and future demand. In April 1987, Aloha Utilities acquired a 27-28 acre parcel of land immediately adjacent to its existing facility. Upon these lands, Aloha Utilities proposes to construct percolation ponds, a rapid rate land application effluent disposal process. As sited, these ponds would be located 1/2 to 3/4 of a mile from a well permitted for an average daily flow of 100,000 gallons or more. 2/ Petitioners, Interphase, Inc., Phase 1 Homes, Inc., and Tahitian Development, Inc., are corporations with common management which are developing three separate but geographically proximate projects in Pasco County. These projects will be, or are, serviced by Aloha Utilities. Interphase, Inc., is the owner/developer of a 100- acre tract known as Riverside Village Unit Number Four. This property is currently being developed to include 57 acres dedicated to single family use and 43 acres dedicated to multifamily use, and will require the installation of stormwater facilities and underground sewage transportation facilities. Two wells of Aloha Utilities that are permitted for an average daily flow of 100,000 gallons or more are located 1/2 mile and 1/3 mile, respectively, from this development. Interphase, Inc., is also the owner of a 17-acre parcel of vacant land in Pasco County that is zoned commercial. This property is located within 400 feet of Aloha Utilities' Seven Springs sewer treatment plant, and its development will require the installation of underground sewage transportation facilities. Phase 1 Homes, Inc., is the owner/developer of a project known as Riverside Village Townhouses. This project is fully developed and is currently serviced by Aloha Utilities. Located within 1/2 mile of the development are two wells of Aloha Utilities that are permitted for an average daily flow of 100,000 gallons or more. Tahitian Development, Inc., is the owner/developer of a 40-acre tract known as Riverside Villas. Twenty of these acres have been developed and some of the units sold. The remaining 20 acres are currently under development. In developing its remaining 20 acres, Tahitian Development would be required to install stormwater drainage systems and sewage transportation lines to connect with Aloha Utilities. Located within 1/2 mile of the development are wells of Aloha Utilities that are permitted for an average daily flow of 100,000 gallons or more. Tahitian Development also owns a 40-acre parcel in Orange County which it plans to develop for light industrial uses such as an industrial park or an office complex. Such development would result in at least a 40 percent impervious surface, including building tops, within that 40-acre parcel, and require the installation of a sewage transportation system and a stormwater drainage system. Petitioner, A.C. & R., Inc., is the owner/developer of a project in Pasco County known as Aloha Gardens Unit Number 12. The project, which currently is represented by 40-50 developed lots, is located just north of the Aloha Gardens sewage treatment facility, and is serviced by Aloha Utilities. Located within 1/2 mile of the development that is permitted for an average daily flow of 100,000 gallons or more. Petitioner, Great Cypress Mobile Village, Inc., is the owner/developer of a 149 unit mobile home park in Pasco County. Twenty of these units are completed and ready for occupancy. Completion of the project will require the installation of additional sewer lines. Located at the interior of the property is a sewage treatment plant owned by Northern Utilities which services the project, and within 600 feet of the project's boundary there is a well which services that utility. The capacity of that well was not, however, demonstrated in these proceedings, nor was it shown whether such well was part of a community water system. Petitioner, Barrington, Ltd. is a party of unknown capacity, origin, or interest. No evidence was presented on its behalf to demonstrate that its substantial interests would be affected by the proposed rules. Intervenor, Florida Electric Power Coordinating Group, Inc. (FCG), a Florida corporation, is an association of Florida's electric utilities, and is composed of 37 members. The FCG has, as part of its internal organization, an environmental committee whose purpose is to participate in regulatory development and provide mutual member assistance with regard to water related matters. This committee was authorized by the FCG executive committee to participate in the development of the rules at issue in these proceedings, as well as Intervene in these proceedings, to represent and protect the interests of FCG members. The FCG participated in the development of the subject rules by the Department, and was granted full party status by the ERC during that rulemaking process. The members of FCG are owners and operators of electric power generating facilities. These facilities“ include the power plant and ancillary facilities such as substations. Incident to the operation of these facilities are wastewater discharges associated with the production of electricity and stormwater discharges. One of these facilities, Gainesville Regional Utilities' Deer Haven generating station is located across Highway 441 from a major community drinking water supply well. Intervenor, Florida Land Council, Inc., a Florid corporation, is composed of 12 primary members who own large tracts of land in interior Florida, and who are engaged primarily in agribusiness. The Land Council's purpose is to protect the asset value of its members property and, because of that purpose, it is concerned with environmental regulations, growth management regulations, land use regulations, and comprehensive planning. To protect its interests, the Land Council sought leave to intervene in these proceedings. There was, however, no proof that any lands owned by any member of the Land Council were proximate to any major public community drinking water well. Intervenor, Pasco County, is the owner/operator of 25 wastewater treatment plants with capacities In excess of 100,000 gallons per day, and has under construction, or in the design stage, additional facilities with capacities in excess of 100,000 gallons per day. The construction of these new facilities will require the installation of new lines for the collection of wastewater. Pasco County's current, as well as its planned, wastewater treatment facilities will utilities a rapid rate land application effluent disposal process. Within a mile of any wastewater treatment plan operated by Pasco County can be found a major public community drinking water well as defined by the rules at issue in these proceedings. Pasco County also owns and operates wells within the county with permitted withdrawal rates exceeding 100,000 gpd, and participates in the ownership and management of their wells with permitted withdrawal rates exceeding 100,000 gpd through West Coast Regional Water Supply Authority. Pasco County currently has plans to add new production wells in the county with an average daily pumpage in excess of 100,000 gallons per day. Intervenor, West Coast Regional Water Supply Authority (West Coast), is an interlocal government body created in 1974 to develop, store, and supply water to its member governments so that all citizens within the areas served by the authority may be assured an adequate supply of water. Member governments served by WCRWSA are Hillsborough County, Pasco County, and the cities of St. Petersburg and Tampa. Wellfields operated by West Coast are the Starkey Wellfield located in west central Pasco County, which serves the citizens of New Port Richey and Pasco County; the South-Central Hillsborough Regional Wellfield located in south-central Hillsborough County, which serves the citizens of Hillsborough, County; the crossbar Ranch Wellfield located in north-central Pasco County, which principally serves the citizens of Pinellas, County; the Cypress Creek Wellfild located in south-central Pasco County, which serves the citizens of Hillsborough, Pinellas, and western Pasco Counties and the City of St. Petersburg; the Northwest Hillsborough Wellfield located in northwest Hillsborough County, which serves the citizens of Hillsborough County; the Section 21 Wellfield located in northwest Hillsborough County, which serves the citizens of the City of St. Petersburg; and, the Come-Odessa Wellfield located in northwest Hillsborough County, which serves the citizens of the City of St. Petersburg. 3/ Each of the wellfields operated by West Coast are public community water systems, and contain wells permitted to withdraw in excess of 100,000 gallons per day. Collectively, these wellfields serve a total population of 800,000 persons. Intervenor, Concerned Citizens of Citrus County, Inc. (Concerned Citizens), is a not-for-profit corporation, was chartered in 1981, and has 350 members who obtain their drinking water from operational community water supply wells permitted for over 100,000 gallons per day in Inverness, Crystal River, Floral City, Sugar Mill Woods, Beverly Hills, and Rolling Oaks, Citrus County, Florida. The purpose of Concerned Citizens is to protect the natural resources of Citrus County through planning and zoning regulations, and local and state legislation and regulations. It was granted party status by the ERC. General aspects of the proposed rules The proposed rules establish new eligibility criteria for designation of an aquifer segment as Class G-I groundwater. Under the existing rule, the ERC could reclassify an aquifer or portion of an aquifer as G-I within specified boundaries upon a finding that: The aquifer or portion of the aquifer is the only reasonably available source of potable water to a significant segment of the population; and The designated use is attainable, upon consideration of environmental, techological, water quality, institutional, and social and economic factors. Under the proposed revisions, an aquifer segment could be classified by the ERC as G-I provided it was: ...within the zones of protection of a major public community drinking water supply well(s) or wellfield(s) withdrawing water from unconfined aquifers or from leaky confined aquifer... and, upon consideration of: ...environmental, technologial, water quality, institutional (including local land use comprehensive plans), public health, public interest, social and economic factors. As with thee existing rule, the proposed rules require that rulemaking procedures be followed to actually designate a G-I aquifer or aquifer segment at any particular location. The scheme envisioned by the proposed rules is to provide protection to "major community drinking water supply wells", community water systems that are permitted by consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater, by preventing contaminants from entering the groundwater within a circumscribed radius of the wells. To accomplish this purpose, the proposed rules establish a methodology whereby two zones of protection would be established around such wells if they were withdrawing waters from unconfined aquifers (an aquifer exposed to the atmosphere) or leaky confined aquifers (an aquifer in which groundwater moves vertically from the water table to the top of the aquifer in five years or less). The first zone (the inner zone) would be based on a fixed radius of 200 feet. The second zone (the outer zone) would be based on a radius, calculated under the rule's methodology, of 5 years groundwater travel time. Within the inner zone, discharges would be prohibited. Within the outer zone, certain developments which discharge to groundwater would be prohibited or restricted. A major emphasis of the proposed rules is to restrict discharges to groundwater within the zones of protection. For example, the rules eliminate the zone of discharge within the zones of protection, and require that new discharges to groundwater of treated domestic effluent meet the groundwater criteria specified in rule 17-3.404, F.A.C., prior to discharge. 4/ Additionally, such wastewater treatment facilities would be required to pre-treat industrial wastewater, provide daily monitoring to insure proper treatment plant process control, and provide 24 hour a day attendance of a wastewater operator under the general supervision of a Class A certified wastewater operator. New underground lines for the transport of domestic raw wastewater would be required to be constructed so that no more than 50 gallons per inch of pipe diameter per mile per day could leak into the ground. Within the 5 year zone of protection, there are no restrictions on stormwater discharges for residential developments. However, discharges from new stormwater facilities serving an area forty acres or larger with a forty percent impervious surface, excluding building tops, are required to monitor the discharge. Construction and operation of new sanitary landfills would be prohibited. As previously noted, to be eligible for reclassification as a G-I aquifer, the aquifer or aquifer segment under consideration must be leaky confined or unconfined. Whether the aquifer is leaky confined or not will be determined through application of the "Vv" and "Tv" formulae contained in the proposed rules, and the zones of protection will be established by reference to the "r" formula contained in the proposed rule. To date, neither the Department nor any party has applied the "Vv" and "Tv" formulae to identify wells hat are withdrawing from unconfined or leaky confined aquifers, nor has anyone delineated any zones of protection by application of the "r" formula. The Department has, however, identified those areas of the state at which it is likely that major community drinking water supply wells are withdrawing from such aquifers. Based on this identification, the Department has contracted with the U.S. Geological Survey (USGS) to "map" the Middle-Gulf region (Pinellas, Hillsborough, Pasco, Hernando, and Citrus Counties) by applying the "Vv" and "Tv" formulas to each well permitted to withdraw 100,000 gpd or more to determine if it is withdrawing from such aquifers and, if so, to delineate proposed zones of protection around such wells or wellfields through application of the "r" formula. The USGS is currently mapping the Middle-Gulf region. Pertinent to this case, the Department has identified all of Pasco and Pinellas Counties, the northern half of Hillsborough County, and most of Orange County including Orlando, as areas within which wells are most probably withdrawing from unconfined or leaky confined aquifers, and for which aquifers the Department will seek G-I reclassification. Under the circumstances, the parties have established, except as heretofore noted, that there is a reasonable likelihood that the proposed rules will substantially affect their interests. The rule challenge The gravamen of the protestant's challenge is that certain definitions and formulae continued within the proposed rule are vague, ambiguous, or not supported by fact or logic. The Protestants' also challenge the adequacy of the economic impact statement. The Protestants concerns are addressed below. Definitions Rule 17-3.021, as amended, would define "Confined Aquifer", "Leaky Confined Aquifer", and "Unconfined Aquifer", as follows: (7) "Confined Aquifer" shall mean an aquifer bounded above and below by impermeable beds or by beds of distinctly lower permeability than that of the aquifer itself. For the purpose of G-I, it shall mean an aquifer confined from above by a formation(s) which restricts the movement of groundwater vertically from the water table to the top of the confined aquifer for a period of more than five years * * * (16) "Leaky Confined Aquifer" shall mean, for the purposes of G-I, an aquifer confined from above by a formation(s) which allows groundwater to move vertically from the water table to the top of the leaky confined aquifer in five years or less. * * * (34) "Unconfined Aquifer" shall mean an aquifer other than a confined aquifer. For the purpose of G-I it shall mean an aquifer other than a confined or leaky confined aquifer. 5/ Protestants contend that the definition of "confined aquifer" and "leaky confined aquifer" are vague and meaningless because they are "defined by use of the phrase being defined". Accordingly, they conclude that proposed rule 17-3.021(7) and (16) must fall because they are without thought and reason, irrational and vague. Protestants further contend that since the definitions of "confined aquifer" and "leaky confined aquifer" are flawed, proposed rule 17-3.021(34), which defines unconfined aquifer, must also fall. The Protestants' contentions are not persuasive. If one were restricted to the definition of "confined", "leaky confined" and "unconfined" aquifer to glean their meaning, the rules might be considered vague. However, these definitions are, as they specifically provide, "for the purpose of G-I" and they must be read in context with the balance of the rule. When so read, it is apparent that "top of the confined aquifer" or "top of the leaky confined aquifer" is the top of the aquifer that has been calculated as confined or leaky through manipulation of the "Vv" and "Tv" formulae. Under the circumstances, the subject definitions are not vague, arbitrary or capricious. Proposed rule 17-3.021(20) provides: "New Discharge" shall mean, for the purpose of G-I, a discharge from a new installation; or a discharge from an existing permitted installation that has been altered, after the effective date of G-I reclassification, either chemically, biologically, or physically or that has a 211 22 different point of discharge, and which causes a significantly different impact on groundwater. Protestants contend that the definition of "new discharge" is vague, arbitrary and capricious because existing installations would be classified as new dischargers, and subject to the more stringent requirements of the proposed rules, whether the alteration of their discharge significantly improved or adversely affected groundwater. As proposed, the rule would so define new discharge, and it is not vague or ambiguous. The proof demonstrated, however, that the Department only proposed to define, as new dischargers, those existing installations whose altered discharge caused a significantly different negative impact on groundwater. The Department conceded this point, and offered no proof to demonstrate the reasonableness of classifying existing installations that improve their discharge as new discharges. Under the circumstances, proposed rule 17-3.021(20) is arbitrary and capricious. Proposed rule 17-3.021(35) defines "underground storage facility or underground transportation facility as follows: "Underground storage facility" or "underground transportation facility" shall mean that 10 percent or more of the facility is buried below the ground surface. This proposed rule is, however, only pertinent to proposed rule 17-4.245, which addresses the permitting and monitoring requirements for installations discharging to groundwater. Pertinent to this case, proposed rules 17-4.245(3)(c) and (d) establish construction requirements for the following facilities within the five year zone of protection: Underground storage facilities. An underground storage facility includes any enclosed structure, container, tank or other enclosed stationary devices used for storage or containment of pollutants as defined in Section 376.301(12), F.S. or any contaminant as defined in Sect ion 403.031(1), F.S. Nothing in this paragraph is intended to include septic tanks, enclosed transformers or other similarly enclosed underground facilities.... Underground facilities for transportation of wastewater or pollutants as defined in Section 376.301(12), F.S. or any contaminant as defined in Section 403.031(1), F.S. excluding natural and liquified petroleum gas. Underground facilities for transportation of waste effluent or pollutants or contaminants include piping, sewer lines, and ducts or other conveyances to transport pollutants as defined in Section 376.301(12), F.S., and contaminants as defined in Section 403.031(1), F.S.... Protestants contend that the proposed rules are contained in two separate chapters of the Florida Administrative Code with no bridge between them. Under such circumstances, they contend the rules fail to adequately define either facility in either chapter, and that the rules are therefore vague, arbitrary and capricious. Protestants' contention is not persuasive. Proposed rule 17-3.021(35) defines "underground storage facility" or "underground transportation facility" as meaning that 10 percent or more of the facility is buried below the ground surface. Proposed rules 17-4.245(3)(c) and (d) address what type of facility is included within the terms "underground storage facility" and "underground transportation facility." Notably, Rule 17-4.021, F.A.C., provides: Definitions contained in other chapters of the Department's rules may be utilized to clarify the meaning of terms used herein unless such terms are defined in Section 17-4.020, F.A.C., or transfer of such definition would defeat the purpose or alter the intended effect of the provisions of this chapter. Under the circumstances of this case, the rules are appropriately read together. So read, the construction requirements for "underground storage facilities" and "underground transportation facilities", as required by proposed rule 17-4.245(3)(c) and (d), are applicable if 10 percent or more of the containment device used for the storage or transport of pollutants is buried below the ground surface, and the proposed rules are not vague, arbitrary or capricious. Proposed rule 17-3.021(39) defines "Zones of Protection" as follows: "Zones of Protection" shall mean two concentric areas around a major public community drinking water supply well(s) or wellfield(s) drawing from a G-I aquifer whose boundaries are determined based on radii from the well or wellfields of 200 feet and five years groundwater travel time respectively. Protestants contend that the definition of "Zones of Protection" is vague, arbitrary and capricious because nowhere within the proposed rules is "G-I aquifer" defined. protestants' contention is not persuasive. Proposed rules 17-3.403(1) and (7) adequately explain what is meant by "G-I aquifer", and proposed rule 17-3.403(8) sets forth the metodology for calculating the zones of protection. The definition of "Zones of Protection", set forth in proposed rule 17-3.02(39) is not vague, arbitrary or capricious, because of any failure to define "G-I aquifer." Mapping Priorities When considering whether to reclassify an aquifer or aquifer segment as G-I, proposed rule 17-3.403(5)(e)2 requires that the aquifer or aquifer segment: Be specifically mapped and delineated by the Department on a detailed map of a scale which would clearly depict the applicable zones of protection. Maps will be grouped and submitted for reclassification generally on a regional basis. Mapping priorities shall follow the Commission directive of February 27, 1985. The remaining areas of the state will be mapped by the Department as time and resources allow. The mapping priority directive referred to in purposed Rule 17-3.403(5)(e)2a, was an oral directive of the ERC that Pinellas, Hillsborough, Pasco, Hernando, and Citrus Counties, referred to as the Middle-Gulf region, be mapped first. That directive has not been reduced to writing and, consequently, a copy thereof has never been available for inspection. Categories of G-I Aquifers and determination of zones and protection Proposed rules 17-3.403(7) and (8), respectively, set forth the eligibility criteria for reclassification as G-I aquifers and the methodology whereby the boundaries of the zones of protection are established. To this end, proposed rule 17- 3.403 (7) provides: Categories of G-I aquifers. For aquifers or aquifer segments to be eligible for potential reclassification as G-I aquifers one of the following criteria must be met: That the aquifer or aquifer segment under consideration be within the zones of protection of a major public community drinking water supply well(s) or wellfield(s) withdrawing water from unconfined aquifers or from leaky confined aquifers.... (b)(. reserved.) Proposed rule 17-3.403(8) provides: Determination of the boundaries of the zones of protection. (a) The boundaries of the zones of protection shall be based on radii from the wellhead or wellfield (if closely clustered, so that the five year zones of protection are overlapping) measured in 200 feet for the inner zone and five years for the outer zone. The radius of the outer zone shall be determined using the following formula: percent.x4n where Q = permitted average daily flow from the well (measured in cubic feet per day); T = five years (1825 days); 3.14 = mathematical constant pi; r = radius (feet); h distance from the top of the producing aquifer to the bottom of the hole (feet); n effective porosity. Protestants contend that the foregoing provisions of the proposed rules are vague, arbitrary and capricious because the wells that would be subject to and around which a zone of protection would be established cannot be identified or, if identifiable, do not comport with the Department's intent or interpretation. Protestant's concerns are not without merit. To be eligible for consideration as a G-I aquifer, proposed rule 17-3.403(7) requires that the aquifer segment be within the zones of protection of a "major public community drinking water supply well(s) or wellfield(s). Proposed rule 17- 3.021(17) provides that "major public community drinking water supply" shall mean: those community water systems as defined in Section 17-22.103(5), F.A.C., that are permitted by consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater. Community water system" is defined by Section 17-22.103(5) as: a public water system which serves at least IS service connections used by year- round residents or regularly serves at least 25 year-round residents. Facially then, the proposed G-I rules are applicable to "community water system" that hold a consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater", and which are withdrawing from unconfined or leaky confined aquifers. Notably, the rule does not ascribe the 100,000 gpd permitted rate of withdrawal to each well, but to a permit held by a community water system. Accordingly, under the literal reading of the proposed rules, each well covered by the consumptive use permit would be subject to a zone of protection regardless of its individually permitted rate, so long as it was withdrawing from an unconfined or leaky confined aquifer. While there may be legitimate reasons to designate zones of protection around wells, regardless of their individual permitted rate when the community water system holds a consumptive use permit to withdraw groundwater at a 100,000 gpd average, the Department advanced none. To the contrary, the Department contended that zones of protection were only to be established around a well that was permitted to withdraw an average daily amount of 100,000 gallons or greater. Under the circumstances, the provisions of proposed rules 17-3.403(7) and (8) are arbitrary and capricious. 6/ The "Vv" and "Tv" formulae Proposed rule 17-3.403(7)(a) prescribes the methodology where by vertical travel time will be calculated, and therefore whether a particular aquifer will be classified as confined or leaky confined. To this end, the proposed rule provides: ... Determination of vertical travel time for leaky confinement will be by application of the following formulae: Vv= Kv h/nl where: Vv= vertical velocity (feet/day). Kv= vertical hydraulic conductivities of the surficial aquifer and underlying confining bed materials (feet/day). h= head difference between water table in the surficial aquifer and the potentiometric surface of the producing aquifer (feet). n = effective porosities of the surficial aquifer and underlying confining bed materials. 1 = distance from the water table to the top of the producing aquifer (feet). Tv= 1/Vv 365 where: Tv= vertical travel time (years). 1 = same as above. Vv= same as above. The "Vv" formula and the "Tv" formula are valid formulae, and are commonly used by hydrogeologists to calculate the vertical velocity and vertical travel time of groundwater. As proposed, the formulae present a reasonable methodology for computing the vertical velocity and vertical travel time of groundwater if the well is producing from one aquifer. The formulae cannot, however, as hereafter discussed, be reasonably applied if tee well is producing from multiple aquifers or if another aquifer intervenes between the surf aquifer and the producing aquifer. While not the most prevalent occurrence in the state wells in the Middle-Gulf regions often do penetrate more than one aquifer and do produce water from more than one aquifer. The rule defines the "Kv" element of the "Vv" formula as the "vertical hydraulic conductivities of the surficial aquifer and underlying confining bed materials (feet/day)." This is a reasonable definition and will produce a scientifically valid result provided the well does not penetrate multiple aquifers. Should the well penetrate multiple aquifers, the values derived for vertical velocity ("Vv") and vertical travel time ("Tv") will not be accurate since the hydraulic conductivities of the intervening aquifers are not, by the rule definition, factored into the calculation of "Kv". Under such circumstances, whether an aquifer was classified as confined or leaky confined would not be determined by a valid "Kv" but, rather, by chance. Protestants also contend that the rule is vague, arbitrary and capricious because it does not specify the methodology by which "Kv" is to be calculated. There are, however, methodologies commonly accepted by hydrogeologists to derive a scientifically valid "Kv", whether the well penetrates one or more than one aquifer. The infirmity of the rule is not its failure to specify a methodology, but its to include data necessary to produce a meaningful result. The rule defines the "n" element of the Vv formula as "effective porosities of the surficial aquifer and underlying confining bed materials." This is a reasonable definition and will, though the application of commonly accepted methodologies, produce a scientifically valid result. 7/ The rule defines the element "Delta h" in the Vv formula as the "head difference between the water table in the surficial aquifer and the potentiometric surface of the producing aquifer (feet)", and defines the element "1" as the "distance from the water table to the top of the producing aquifer (feet)." These elements are utilized in the formula to calculate a gradient, and must be measured using the same points of reference to yield a meaningful result. To this end, the proof demonstrates that the definitions are reasonable since they utilize the same points of reference, and that when applied in accordance with accepted hydrogeologic practice will produce a scientifically valid gradient. (See Department exhibit 7). Protestants contend, however, that the definitions of "Delta h" and "1" are vague, arbitrary and capricious because they do not specify when the measurements should be made, do not define "producing aquifer", and do not define "top" of the producing aquifer. For the reasons that follow, Protestants' contentions are found to be without merit. While a water table is a dynamic surface subject to frequent, if not daily fluctuation, resulting from variations in rainfall and the demands of man, and while a potentiometric surface is likewise a dynamic elevation that changes with time and season, protestants failed to demonstrate that there was any particular date or dates that would be most appropriate to make such calculations. Rather, protestants contended that unless such measurements were taken contemporaneously, any derivation of "Delta h" and "1" would not be reliable. While such might be the case, the rule does not mandate a divergence from the accepted hydrogeologic practice of taking such measurements contemporaneously. While the rule does not define "producing aquifer," it is an accepted hydrogeologic term and not subject to confusion. The only confusion in this case was the introduction of the issue of multiple producing aquifers and protestants' contentions that this rendered the Vv formula vague, arbitrary and capricious since it did not factor in such a consideration. Protestants' contention does not, however render the term "producing aquifer" vague. The sole purpose of the Vv and Tv formulas are to determine whether the aquifer from which water is being produced is leaky confined. To establish this, the formulae are applied to calculate whether the vertical travel time is five years or less. If a well is withdrawing water from more than one aquifer it may be necessary to calculate Vv and Tv for each aquifer to discern which of those aquifers are within the 5 year vertical travel time threshold, and therefore subject to G-I reclassification. To this end the rule is not vague, and would adequately address the multiple producing aquifer scenario. While the rule doe not define "top" of the producing aquifer, this term is an accepted hydrogeologic term and is not subject to confusion. In application there may, however, be disagreements among hydrogeologists as to where this line should be established because geologic boundaries are fine gradations, and not sharp lines which would lend themselves to the designation of precise points of reference. This is not, however, a failure of the rule, but a peculiarity of nature, and is subject to scientific proof. Notably, protestants did not demonstrate that "top" of the producing aquifer could be defined with reference to a fixed point. Under the circumstances, "top" of the producing aquifer is a reasonable reference point. Zones of Protection Proposed rule 17-3.408 provides: Determination of the boundaries of the zones of protection shall be based on radii from the wellhead or wellfield (if closely clustered, so that the five year zones of protection are overlapping), measured in 200 feet for the inner zone and five years for the outer zone. The radius of the outer zone shall be determined using the following formula: QT 2 3.14 hn where Q = permitted average daily flow from the well (measured in cubic feet per day); T = five years (1825 days); 3.14 = mathematical constant pi; r = radius (feet); h distance from the top of the producing aquifer to the bottom of the hole (feet); n effective porosity. For the purpose of this calculation the following effective porosities for representative Florida aquifers will be used: Floridan .05 Sand and Gravel .2 Biscayne .15 Surficial .2 The Department shall use more site-specific values for "Q", "n", or "h" when available for designation of the zones of protection by the Commission. Proposed rule 17-3.403(8)(a) provides that the inner zone of protection shall be based on a radius from the wellhead or wellfilled, as appropriate, of 200 feet. While denoted as an arbitrary radius, the 200 foot radius was not derived without fact or reason. Rather, it was a result reached at the workshops after consideration of existing regulations that establish buffer zones of 200-500 feet between a public water supply and a pollution source. Conceptually, the 200 foot zone was adopted because it is so small and so close to the well that it essentially constituted a zone of protection of the well head by preventing contaminants from moving into the well opening directly or the annular space around the well casing. Accordingly, the 200 foot zone has a reasonable basis. Its actual delineation is, however, as flawed as that of the five year zone discussed infra. The "r" formula defines the outer zone of protection, and calculates it as a radius equal to the distance groundwater would flow in five years toward the well. The basis for the "r" formula is the formula used to calculate the volume of a cylinder. That formula, V = pi r2 h, yields a simple volumetric measurement without any consideration of velocity. By the introduction of the element "n" (effective porosity), the "r" formula introduces a velocity component which would, properly applied, produce a radius equal to the distance groundwater would flow in 5 years. 8/ As proposed, however, the rule would establish a meaningless line around a well. Under the proposed rule, the Department would calculate "r" based on specified effective porosities ("n") for the Floridan, Biscayne, sand and gravel, and surficial aquifers absent site specific data. The Department is, however, under no requirement to generate site specific data, and currently is mapping the Middle-Gulf region based on the values established by the rule. Absent chance, the areas mapped will bear no relationship to groundwater travel time. The lithology of an aquifer and the surrounding layers is varied and diverse, and directly affects the direction and velocity of groundwater flow. By assuming "n", the "r" formula ignores the varied lithology, and produces a radius that would seldom, if ever, represent the actual rate at which groundwater moved toward any well. 9/ The zone thus circumscribed is an illusion since the groundwaters and contaminants within it may move at a rate significantly greater than or less than 5 years travel time. Notably, the Department has conducted no study or test to validate its proposed methodology. The element "Q" in the "r" formula is defined as the "permitted average daily flow from the well (measured in cubic feet per day)." Protestants contend that such definition is vague, arbitrary and capricious because the Department proposes to rely on consumptive use permits issued by the various water management districts to derive "Q", and such permits would not necessarily provide the requisite data. While the proof demonstrates that "Q" cannot always be derived by reference to a consumptive use permit, this does not render the definition of "Q" vague, arbitrary, or capricious. Rather, "Q" is a factual matter, and subject to a factual derivation through reference to consumptive use permits and other site specific data. The element "T" in the "r" formula is defined as "five years (1825) days." By its inclusion, the Department proposes to circumscribe the outer zone of protection at five years groundwater travel time. The concept of a zone of protection is premised on the theory that restrictions should be placed on discharges to groundwater within an area proximate to a public water supply for public health and safety concerns. The five year standard, which is found throughout the rules, was based on the theory that if a contaminant was introduced to groundwater a period of time should be allowed to discover the contamination and remove it or make provision for an alternate water supply before the contaminant reached the public water supply. The five years proposed by the rule was not, however, founded on fact or reason. During the workshops that under scored the proposed rule, the time factor was the subject of considerable discussion and ranged from less than two years to greater than ten years. Based on its own in-house search, the Department initially proposed a 10-year standard. That search revealed that it took 10 to 15 years between the time a contaminant was discovered and cleanup could commence, and between seven and eight years between the time a contaminant was introduced into groundwater and it discovery. Notwithstanding the results of its own in-house search, the Department, in the face of debate, elected to "compromise" and propose a five-year standard. Such standard was not the result of any study to assess its validity, and no data, reports or other research were utilized to derive it. In sum, the five- year standard was simply a "compromise", and was not supported by fact or reason. As previously noted, the lithology of an aquifer and the surrounding layers is varied and diverse, and directly affects the direction and velocity of groundwater flow. The effective porosity of those materials in the Floridan aquifer canvary from to .4 at various places. The rule proposes, however, to use an effective porosity for the Floridan aquifer of .05 to establish "r." The value ascribed to "n" is a critical value, as previously discussed in paragraph 65. It also has a profound impact on the aeral extent of the zone of protection. For example, assuming "Q" equals 3 million gallons and "h" equals 600 feet, an "n" of .02 would result in a radius of 4,406 feet or 1,400 acres, an "n" of .03 would result in a radius of 3,578 fee or 934 acres, an "n" of .05 would result in a radius of 2,787 feet or 560 acres, and an "n" of .2 would result in a radius of 1,393 feet or 140 acres. While an effective porosity of 05 for the Floridan aquifer may be a reasonable value at a particular site, it is not a value that can be reasonably ascribed to the Floridan in general. For this reason, and the reasons heretofore set forth, the rule's specification of an effective porosity of .05 for the Floridan aquifer is unreasonable. Proposed rule 17-3.403(8)(a), sets forth the manner in which the zones of protection will be drawn around a well or wellfield. That proposed rule provides: For well fields whose individual zones of protection overlap due to clustering, a single zone of protection will be calculated in the following manner: Using the permitted average daily withdrawal rate of the wells with overlapping zones of protection, the area on the surface overlying the aquifer equal to the sum of the areas of the five year zones of protection of the individual wells, shall be used to define the area which encircles the perimeter of the wellfield. In cases where a zone of protection of a single well protrudues beyond the calculated perimeter or when the configuration of the wellfield is irregular, the perimeter will be shaped to accommodate the configuration. The surface are encircling the perimeter of the wellfield shall not exceed the total surface area of the overlapping zones of protection for individual wells. In the case of unclustered wells within a wellfield, individual zones of protection around each well will be calculated. As previously discussed, the proposed G-I rules are facially applicable to "community water systems" that hold a " consumptive use permit to withdraw an average daily amount of 100,000 gallons or greater of groundwater," and which are withdrawing from unconfined or leaky confined aquifers. Under proposed rule 1773.403(8)(a), the five-year zone of protection would be drawn around each of these wells. If the wells are located so close to each other that the five year zones of protection are overlapping (clustered), those wells would be deemed a wellfield by rule definition and a five year zone of protection would be established around it. The proposed rule's description at how to determine and configure a zone of protection around a wellfield is however, vague and ambiguous. While the rule provides that when the configuration of the wellfield is "irregular", the perimeter will be shaped to accommodate the configuration", it sets forth no standard by which the perimeter will be established. Effectively, the rule vests unbridled discretion in the Department to establish the configuration of a wellfield. The Economic Impact Statements Pursuant to the mandate of Section 120.54(2), Florida Statutes, the Department prepared economic impact statements for the proposed revisions to Chapters 17-3 and 17-4, Florida Administrative Code. The economic impact statements were prepared by Dr. Elizabeth Field, the Department's chief economist, an expert in economics. Dr. Field developed the economic impact statements by examining the proposed rules and discussing their potential impact with Department staff. Additionally, Dr. Field attended the public workshops that were held concerning the proposed rules, and solicited input from those participants. The Florida Home Builders Association and the Florida Petroleum Council submitted data for her consideration, but none of the petitioners, although some were represented at such workshops, responded to her requests for information. The economic impact statements prepared by Dr. Field to address the proposed rules conclude that, apart from the cost to the Department for mapping, there are no direct costs or economic benefits occasioned by the rules. Dr. Field's conclusion was premised on the fact that the proposed rules only establish the eligibility criteria for reclassification of an aquifer to G-I and the standards for discharge to that aquifer. Under the proposed rules, further rulemaking would be required to actually designate a specific aquifer as G-I, and delineate a zone of protection. 10/ Pertinent to this case, proposed rule 17-3.403, provides: The intent of establishing G-I eligibility criteria is to determine which aquifer or aquifer segments qualify for potential reclassification to G-I aquifers. Adoption of these criteria does not imply nor does it designate aquifer or aquifer segments as G-I. Such designation can only be achieved through reclassification by the Commission after eligible segments have been mapped by the Department. (6)... the following procedure shall be used to designate Class G-I aquifers: Rulemaking procedures pursuant to Chapter 17-102, F.A.C., shall be followed; Fact-finding workshops shall be held in the affected area; All local, county, or municipal governments, water management districts, state legislators, regional water supply authorities, and regional planning councils whose districts or jurisdictions include all or part of a proposed G-I aquifer shall be notified in writing by the Department at least 60 days prior to the workshop; A prominent public notice shall be placed in an appropriate newspaper(s) of general circulation in the area of the proposed G-I aquifer at least 60 days prior to the workshop. The notice shall contain a geographic location map indicating the area of the zones of protection and a general description of the impact of reclassification on present and future discharges to groundwater. A notice of a G-I workshop shall be published in the Florida Administrative Weekly prior to the workshop(s). At least 180 days prior to the Commission meeting during which a particular zone of protection will be considered for reclassification, the Department will provide notice in the Florida Administrative Weekly and appropriate newspaper(s) of the intended date of the Commission meeting. The Commission may reclassify an aquifer or aquifer segment as a G-I aquifer within specified boundaries upon consideration of environmental, technological, water quality, institutional (including local land use comprehensive plans), public health, public interest, social and economic factors. When considering a reclassification an aquifer or aquifer segment shall: ....(Be within the zones of protection of a major public community drinking water supply well(s) or wellfield(s) withdrawing water from unconfined or from leaky confined aquifers.).... Be specifically mapped and delineated by the Department on a detailed map of a scale which would clearly depict the applicable zones or protection. Maps will be grouped and submitted for reclassification generally on a regional basis. Mapping priorities shall follow the Commission directive of February 27, 1985. The remaining areas of the state will be mapped by the Department as time and resources allow. (Emphasis added). While, if and when applied, the proposed rules would certainly have a direct economic impact as a consequence of a reclassification of an aquifer to G-I and the designation of a zone of protection, as well as the standards for discharge to that aquifer, such costs at this stage are not direct or are not quantifiable. When mapped and the zones of protection identified, a reasonable assessment of the economic cost or benefit of the proposal can be addressed. This is specifically reserved by the Commission whereby its decision to reclassify an aquifer as G-I will, pursuant to proposed rule 17-3.403(6) follow rule making procedures and be based on consideration of economic factors. This result obtains whether the affected party is a small business or some other entity. In reaching the conclusion that the economic costs or benefits of the proposed rules, apart from the cost of mapping, do not at this stage have a direct or quantifiable impact, I have not overlooked the "announcement effect" that is occasioned by the announcement of a governmental agency to regulate an activity. Such announcement certainly has a chilling effect on the community that may reasonably be impacted. The economic impact is, however, speculative or not quantifiable in the instant case. Further, the proof does not demonstrate any incorrectness or unfairness in the proposed adoption of the rules occasioned by the EIS prepared in this case.
Findings Of Fact At all times pertinent to the issues herein, the Southwest Florida Water Management District had permitting authority for the issuance of consumptive use permits in the area in which Respondent, El Jobean, proposes to sink its irrigation well. On December 12, 1988, El Jobean submitted a consumptive use permit application to sink a new well for the purpose of irrigation of a golf course to be developed on the property it owns in Sarasota County. The well is to be located in the NE 1/4 of the NE 1/4 of Section 32, Township 365, Range 20R, in Sarasota County, Florida near the southern boundary of an irregularly shaped piece of property consisting of approximately 855 acres, owned by the applicant, which extends over Sections 28, 29, 32 and 33, Township 365, Range 20E. Respondent proposed to sink a 10 inch diameter well to a total depth of approximately 900 feet with casing in the well now to extend down to 300 feet, with a pump capacity of 1,000 GPM. The golf course to be irrigated is to encompass approximately 190 acres. The applicant requested authority to withdraw an average of 600,000 GPD with a limitation of a maximum of 1,440,000 GPD. The application was properly staffed by the District. In the staff report on the application, the average daily use limitation was expanded to 707,000 GPD; consumptive use was raised from 0 to 139,000 GPD; and maximum daily consumption was reduced from 1,440,000 GPD to 1,240,000 GPD. These changes were due to correction of arithmetic errors in the application and were accepted by the applicant. The ultimate recommendation of the staff was for approval of a 6 year permit, subject to certain conditions outlined in subparagraph I of the staff report. These special conditions require the provision and use of flow measuring devices to maintain an accurate record of the water withdrawn; the maintenance of flow records and the providing of periodic reports to the District; the collection and analyzing of water quality of samples taken from the well to measure the appropriate parameters for chlorides, sulfates, and total dissolved solids; the reporting of the results of these samplings and a description of the sampling and analytical methodologies employed; and a requirement that the permittee investigate the feasibility of supplementing and/or substituting drawn water with treated sewage affluent. After the staff report was submitted, proper notice of the District's intent to issue the permit was published. Based on that notice, protests were filed both by Miakka and Mr. Bishop. The area in question is located within the Manasota Basin which, itself, is located within the Southern West-Central Florida Ground Water Basin, (SWCFGWB), which encompasses all of Pasco, Hillsborough, Manatee, Sarasota, Polk, Hardee, and DeSoto Counties, and parts of Lee, Glades, Charlotte and Highlands Counties. The SWCFGWB sits atop several aquifers which include the Floridian Aquifer, two Intermediate aquifers, and the Surficial Aquifer. The Floridian Aquifer is the deepest and the Surficial Aquifer is on the top. The Miakka Community Club is a Florida corporation made up of residents of the pertinent area whose primary function is to preserve and conserve the rural nature and spirit of the Northeast section of Sarasota County. The club performs this function through educational programs, community activities, and participation in the legislative process. Miakka urges denial of the permit sought by El Jobean based on its membership's belief that the property owners whose property is in the immediate vicinity of the proposed well will be adversely affected if El Jobean is permitted to sink its well and withdraw water from it. The club membership believes that approval of El Jobean's well will result in contamination of existing personal water wells due to excessive use by El Jobean; potential contamination of Sarasota County's future drinking water sources which include the capital Ringling,/MacArthur tract and the Myakka River; reduction of property values; and destruction of personal resources. Petitioner also urges that since the proposed golf course will be a part of a private club for the use of members only, in which membership will be limited, there is no public benefit derived from the approval of and sinking of the well in question. Petitioner also contends that during the periods of severe water shortage as are being currently experienced, permission to sink a well of this size to draw water in of the magnitude expressed in the application, would be counterproductive and detrimental to the interests of the other property owners in the area. In support of its claim, Petitioner presented the testimony of two homeowners from the area, Mr. Richardson and Ms. Mustico. Mr. Richardson, whose well is 183 feet deep, has had several problems with his well even without the instant drilling. In 1974, and subsequent thereto, he has had to go deeper with a suction pipe because the water has dropped below the level of the tail pipe. Ms. Mustico's 160 foot deep well, with 80 feet of casing, is used to supply water for the home. She also has other wells for watering her lawn and for livestock, one of which goes down 500 feet. She is concerned that the well proposed by El Jobean will adversely impact her ability to draw water from her wells because, she believes, the water level from which her water is drawn will drop. In the past, her primary well has gone dry and the wells of several neighbors have gone dry as well. Through maps and other documentation taken from the Ground Water Resource Availability Inventory for Sarasota County, Florida, prepared by the District in March 1988, Petitioner has established that areas of significant groundwater withdrawal within the SWCFGWB occur in Hillsborough, Manatee, Polk, Hardee, DeSoto and Highlands Counties. With the exception of an extremely small portion of Sarasota County located contiguous to Manatee County, there appear to be no areas of major ground water withdrawal currently existing in Sarasota County. The majority of the major municipal well fields within the pertinent basin that are located within Sarasota County, extend down to the Intermediate and Surficial Aquifers with only 3 extending through the lower Intermediate into the Floridan Aquifer. These include the Verna well field located in the northeast corner of Sarasota County where it abuts Manatee County; the Sarasota County well field located in northwest Sarasota County near the Manatee County line; and the Sorrento Utility, Inc., well field which is located near the Gulf Coast, approximately two-fifths of the way down between the Manatee and Charlotte County lines. With the exception of the Verna well field, all the municipal well fields in Sarasota County appear to be reverse osmosis systems and as of 1987, there were 28 reverse osmosis systems located within Sarasota County. Most are relatively small in their output measured in millions of gallons per day. With the exception of 3 public supply wells, 2 of which are permitted an average annual pumpage greater than 100,000 GPD and 1 of which is permitted less, all of the permitted public supply well fields in Sarasota County are located west and south of 1-75 as it extends from the Manatee County line in the north to the Charlotte County line in the south. The El Jobean well would be located east of the line, in that area occupied by the 3 public supply wells. Generalized recharge areas for the upper Floridan Aquifer in the groundwater basin in issue here have been categorized from "high", with a rate of more than 10 inches per year, to "Generally none", with a recharge rate at 0. In 1980, the high recharge rates existed in the north-central part of Pasco, the eastern part of Polk County, and the northeastern part of Highlands County. Sarasota County is in an area wherein the recharge rate was either very low or generally none. In September 1986, the high recharge rate was found in a very small area of northeastern Pasco County, and small areas in both Polk and Highlands Counties. Sarasota County, for the most part, was classified as having no recharge. In May 1987, the high recharge rates were, again, a small area in eastern Pasco County, a small area in northeastern Hillsborough County, a small area in southeastern Polk and northwestern Highlands Counties, and a minuscule area in central Pinellas County. Again, Sarasota County had a recharge rate of 0. Generalized estimated, calibrated, model-derived recharge and discharge values for the upper Floridan Aquifer in the ground water basin in issue here, as they pertain to Sarasota County, reflect positive 2 recharge to negative 1 discharge inches per year. Historically, however, the northeast portion of Sarasota County, where the El Jobean well in question would be located, evaluated by various individuals or agencies periodically from 1980 through 1988, reflects a recharge of anywhere from 0 to 2 inches per year. None of this documentation was supplemented, however, by direct testimony by an individual knowledgeable in this area, and Petitioner's main thrust appears to be an unsubstantiated fear that the sinking of El Jobean's well will have a negative impact on its membership's wells. Admittedly, the residents in the area in question all rely on private wells for the majority of their water supply, other than through the catchment of rainwater, which is insignificant. It was also established that the area has been undergoing a severe water shortage and that conservation measures have been mandated. On the other hand, El Jobean presented the testimony of a hydrogeologist, Mr. Moresi, who has extensive experience with the modeling process used to determine water consumption and recharge in southwest Florida and Sarasota County. The aquifer system in Florida is made up of water bearing limestone layers below the surficial sand base. This aquifer system underlays the various zones throughout the state and reflects a surficial aquifer extending from ground level down approximately 70 feet to a confining bed which separates it from the lower strata. This top confining bed is approximately 20 feet thick, and below it is the Tamiami-Upper Hawthorn Aquifer, which is between 100 and 200 feet deep and which rests on another confining bed somewhat thicker than the upper one. Below the second confining bed is the Lower Hawthorn-Upper Tampa Aquifer which extends approximately from the 250 foot to the 450 foot level at the Manatee County line, and between the 320 foot and the 710 foot level at the Charlotte County line. Another confining bed lays between this aquifer and the Floridan Aquifer which starts at the 500 foot level and goes down well below the 900 foot level in the north and extends from the 730 foot level down in the south. The confining bed below the surficial aquifer is made up of a clay material which retards the movement of water from one aquifer to another. The surficial aquifer is porous and saturated with water from the water table down. Since the confining beds are far less porous than the aquifers they separate, water moves much more slowly through them. The lower aquifers are made up of limestone and are also porous and contain water. The Tamiami-Upper Hawthorn formation consists of limestone and clay, but is water bearing. The Lower Hawthorn-Upper Tampa formation is similar and both make up the intermediate aquifer below which is the lower confining bed followed by the Floridan aquifer. Respondent's well would be cased in steel down to an area approximately 100 feet into the Floridan Aquifer, through the Lower Hawthorn- Upper Tampa Aquifer and through the lower confining bed. Since the well would be cased to well below the lower confining bed, water existing in the upper aquifers, would be prevented from being drawn down by operation, of the Respondent's well either directly or by settling down to replace the water drawn out. Generally, the deeper a well is drilled, the worse the quality of the water, and it becomes less potable. The Floridan Aquifer produces far more copious quantities of water than do the intermediate aquifers. However, since it is cheaper to drill to the intermediate zones as the wells need not be so deep, and since the water there is better, most domestic wells go no deeper than these aquifers. They go down approximately 150 to 180 feet. The pressure in each level is separate from and different from that in the other aquifers. The upper intermediate system generally has a lower pressure than the lower intermediate system. As a result, water from the lower intermediate system tends to leak upward toward the upper intermediate aquifer, rather than the reverse. In addition, a recent survey tends to show that the Floridan aquifer also tends to leak upward into the lower intermediate level. It also shows that leakage through the confining beds amounts to .002 GPD per cubic foot of aquifer. Petitioner claims that since the lower water is of lesser quality, and since withdrawal of water from the upper layers would promote leakage upward, thereby adding lower grade water to the better grade upper water, there could be a diminishment in upper level water quality as a result of water being drawn from the upper levels. However, according to Mr. Moresi, the .002 figure is so small it would result in an infinitesimally small drawdown of water level from the upper intermediate level aquifer and the potential for compromise of the water quality therein is remote. Clearly, this is not the result of drawing water from the Floridan Aquifer as the well in question would do but more the result of the residential wells extending into the upper levels. The District ran a model for the proposed El Jobean well (a Jacob- Hantush model) which showed that drawdown at the wellhead would be just over 2 feet. This means that use of the Respondent's well would reduce the water level in the Floridan Aquifer at the well head by 2 feet. However, this drawdown is shown to decrease rapidly out to where, at distance, it is almost immeasurable. In fact, drawdown of the Floridan Aquifer at 24,000 feet from the well head (approximately 4.5 miles) would be .1 feet, slightly or 1 inch. The .1 foot drawdown relates to the lowest (Floridan) aquifer and the resultant drawdown in the upper intermediate aquifer, into which the majority of residential wells are sunk, would be relatively undetectable. Since the Petitioner's wells, at their deepest, go only into the upper intermediate level, and would be separated by 2 confining beds from the Floridan Aquifer, the impact on the domestic wells at 2 miles from the El Jobean wellhead would be immeasurable. Even at 1 mile, there would be minimal drawdown in the Floridan Aquifer and almost none in the upper intermediate aquifer. The potentiometric surface of the intermediate layer would not be adversely affected, nor would that of the surface water. Recognizing the potential for saltwater intrusion which occurs all along the coast, based on his studies, Mr. Moresi concluded that the well in question here would not induce significant saltwater intrusion. He concluded as well that the permit is consistent with the requirements of the District rule; that the amount permitted for the use of irrigation of the golf course is reasonable, assuming a golf course is a reasonable and appropriate use of water; that the withdrawal by the well in issue would not have an adverse impact on users outside the property on which the well was located; that it would not impact existing users; that there is no other water available for the purpose intended; that the water taken from the Floridan Aquifer under this permit may be potable but is of poor quality; and that the applicant met rule standards. Mr. Moresi also discussed the possible cumulative impact of the proposed well when operated along with the currently existing wells. If there are other drawdowns from the same cone into which El Jobean's well would be sunk, the withdrawals would be cumulative. However, as best he can determine, the only other significant drawdown from the cone pertinent here is that of the Verna well field. In his opinion, that well field's drawdown, which is from the northeast, would not be significant even when considered with the El Jobean well. Mr. Moresi was also satisfied that while the confining bed separating the surficial aquifer from the next lower level might be disturbed, the deeper one goes, the less likely there is to be mixing of aquifers. The only instance where water could move from one level to another as a result of the well is where there is no casing on the bore hole. In the instant case, plans call for, and permit conditions require, the well to be cased to below the lowest confining bed. Consequently, there should be no upward or downward flow of water as a result of the bore. Mr. Tyson, who worked on the evaluation of El Jobean's application for permit, was of the opinion that the amount of water requested by El Jobean in its application was appropriate for a golf course. This does not mean that a golf course is an appropriate use of the property. The special conditions imposed on the granting of the permit by the District are designed to reduce any impact possibly caused by the permitted activity. The Jacob-Hantush model used in analysis of the instant application is considered to be a conservative tool and showed minimal drawdown at all property boundaries. The use of other models in this case was considered neither necessary nor appropriate. Mr. Tyson considers the proposed permit a reasonable beneficial use as defined in the Florida Administrative Code and statutes because it proposes use of reasonable amounts of water and the models indicate no unfavorable impact. Based on the past practice of permitting golf courses with subdivisions, he feels the proposed use is reasonable. He concludes, therefore, that it is in the public interest to grant this permit. In his opinion, the permit will not interfere with legal existing uses and meets all statute and rule requirements. Considering the evidence as a whole, it is found that petitioner has presented insufficient evidence to support its claim that approval and operation of El Jobean's well as proposed would have an adverse impact on the property owners. It's concerns are no doubt sincere, but these concerns are not sufficiently confirmed by evidence of record. At the hearing, the parties stipulated that if the permit were granted, it would be modified by the addition of two conditions: The proposed well shall be constructed with a minimum of 600 feet of casing so as to prevent the unauthorized interchange of water between water bearing zones in order to prevent the deterioration of water quality in the shallower zones. If the well cannot be properly completed to prevent such an unauthorized interchange of water, the well shall be abandoned and plugged in accordance with Rule 17-21.10(2)(c), F.A.C.. Upon completion of the well, a copy of the well construction completion report shall be sent to the District. The permittee shall line the bottom of the pond that will be used as the irrigation source, with clay to a thickness equal to 1.5 feet.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that the Southwest Florida Water Management District enter a Final Order issuing Consumptive Use Permit Number 209458, as modified by the conditions stipulated to at the hearing held herein on June 7, 1989, and outlined in Finding of Fact Number 27 herein, to El Jobean Philharmonic Group, Inc. RECOMMENDED this 9th day of August, 1989 at Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of Division of Administrative Hearings this 9th day of August, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 88-1176 The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. For the Petitioner: Not a Finding of Fact but a statement of the ultimate issue of fact. Accepted and incorporated herein. 3-6. Accepted and incorporated herein. 7-12. Accepted and incorporated herein. Accepted as indicating original conditions. The parties stipulated to additional conditions at the hearing. Accepted. 15 & 16. Accepted and incorporated herein. 17-33. Accepted and incorporated herein as pertinent. 34 & 35. Accepted. 36 & 37. Accepted. 38 & 39. Redundant. 40-43. Accepted. 44. Accepted. 45-51. Accepted. 52 & 53. Accepted. 54-56. Accepted. 57 & 58. Accepted and incorporated herein. 59-66. Accepted. 67-75. Accepted and incorporated herein. 76 & 77. Accepted and incorporated herein. 78. Accepted. 79-84. Accepted. Accepted and incorporated herein. Rejected. 87 & 88. Accepted. 89-93. Accepted and incorporated herein. Accepted. Accepted in the natural source sense suggested by Petitioner. 96-99. Accepted and incorporated herein. 100 & 101. Accepted and incorporated herein. 102-105. Accepted and incorporated herein. 106. Accepted. 107 & 108. Accepted. 109 & 110. Accepted. For the Respondents: 1 & 2. Stipulation between the parties accepted and incorporated herein. 3-6. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence except for the second sentence which is incorporated herein as a Finding of Fact. Not a Finding of Fact but a comment on the evidence. 9-11. Accepted and incorporated herein. 12. Accepted. 13-16. Accepted and incorporated herein. 17. Accepted and incorporated herein. 18 & 19. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. 22-26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29. Accepted. 30-32. Accepted and incorporated herein. 33-40. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. Not a Finding of Fact but a Conclusion of Law. COPIES FURNISHED: Becky Ayech Personal Representative Miakka Community Club 421 Verna Rd. Sarasota, Florida 34240 Douglas Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Edward B. Helvenston, Esquire Assistant General Counsel Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609 6899
The Issue The issue in this case is whether a variance for a reduced setback from Petitioner's well to Respondent Allen C.D. Scott, II's (Scott) septic system should be granted by the Department of Health.
Findings Of Fact Allen C.D. Scott, II, owns property designated as Lot 13, Block 11, Vilano Beach Subdivision, 40 Viejo Street in St. Johns County, Florida. Mr. Scott's property is undeveloped, except for a drinking water well located in the northwest quadrant of his property. The well was installed within the past year. There are residential homes on the north, south, and west sides of the property. The beach is on the east of the property. The property is 50 feet wide and 125 feet deep. The property is not served by a public or private utility; thus, Mr. Scott must provide his own drinking water well and septic system. Mr. Scott purchased the property from Alexander A. Morese, Jr. Mr. Scott was Morese's attorney of record for issues concerning this property and the proposed septic tank system. The neighboring property to the north of Mr. Scott's property is owned by Petitioner, May Bobbitt. Petitioner has two wells on her property. A fairly recently-installed drinking water well and an irrigation well. The irrigation well, is located 30 feet from a site on Mr. Scott's property proposed for an on-site septic system. The location of the proposed septic tank is less than the required setback from a septic system to an irrigation well of 50 feet. The potable drinking water well is 225 feet deep, pit- cased and terminates in the Floridan aquifer. It is within 65 feet of Ms. Bobbitt's septic tank system and is located 50 feet from the proposed site of Mr. Scott's septic system. The location of the proposed septic tank is less than the required setback from a potable drinking water well to a septic system of 75 feet. The initial permit for Ms. Bobbitt's drinking water well was denied based on its proximity to her septic tank. Ms. Bobbitt challenged the denial in an informal proceeding before DOH (DOH case number 97-023H). Mr. Morese played some role in that proceeding. In the meantime, the initial septic tank permit application filed by Mr. Morese was denied by DOH based on the location of Ms. Bobbitt's drinking water well. Mr. Morese appealed the denial to the DOAH Case No. 98-3283. Sometime in late 1997, DOH granted Ms. Bobbitt a variance for a 65-foot setback distance from her drinking water well to her septic system. The variance resulted after settlement of the administrative actions involving May Bobbitt and Mr. Morese's permitting her well and Mr. Morese's septic tank. The variance was granted because the construction of the well prevents contamination of the well from the septic system. Both cases were separately terminated. On November 5, 1997, Mr. Morese applied to DOH for a variance to reduce the setback distances from Petitioner's two wells to Mr. Morese's proposed septic system. Since Mr. Morese's property was 50 feet wide and Mr. Morese desired to build a two-bedroom home on the property, there was limited area available to construct the septic system. The proposed septic system is located in the only area available for such a system and is the same location proposed by Respondent Scott. A sign was posted on Mr. Morese's property notifying Ms. Bobbitt of Mr. Morese's variance request. The variance committee recommended approval of the Morese variance with specific provisos at their December 1997, meeting. Dr. Richard Hunter, Department of Health Deputy State Health Officer, approved the variance with provisos by letter to Mr. Morese on December 17, 1997. The letter stated the approval as follows: The onsite sewage treatment and disposal system shall be set back from the irrigation well on lot 14 by the maximum distance attainable but not less than 30 feet when installed. The onsite sewage treatment and disposal system shall be set back from the drinking water supply well on lot 14 by the maximum distance attainable but not less than 50 feet when installed. The onsite sewage treatment and disposal system drainfield elevation shall be based on a seasonal high water table no lower than 12 inches below existing grade based on William G. Harb's report of November 13, 1997. The variance approval was not challenged by Petitioner or any other neighbor. The variance was granted for a period of one year from the date of Dr. Hunter's letter. As indicated, Allen C.D. Scott, II, purchased the property from Mr. Morese. When Mr. Scott purchased the property from Mr. Morese, the variance was transferred to Mr. Scott. After Mr. Scott purchased the property, he hired an engineer to assist him in securing a Department of Environmental Protection (DEP) coastal construction control permit. The permit was finally issued on May 13, 1999. The variance granted Mr. Morese and subsequently transferred to Mr. Scott expired December 18, 1998. Thus, by the time Mr. Scott obtained his DEP permit to put fill on his property in order to construct his septic system, the variance for reduced setbacks from Petitioner's wells had expired. On June 14, 1999, Mr. Scott applied to DOH for a variance to reduce the required setbacks from Petitioner's irrigation and drinking water wells to his proposed septic system. Mr. Scott's variance application requested the exact same setbacks that Mr. Morese had been granted in December 1997. For the same reasons the variance review committee recommended approval of the Morese the committee recommended approval of the Scott variance. Dr. Sharon Heber, Director of Environmental Health, DOH, granted the variance by letter on July 2, 1999. The letter contained the same provisions as Mr. Morese received in December 1997. The evidence demonstrated that the requested variance would not adversely impact anyone's health or degrade ground or surface waters. Moreover, the evidence showed that the variance met all other Department criteria for an onsite sewage disposal system. Don Hallman, professional engineer, testified that the pit casing of Ms. Bobbitt's well provides an additional layer of protection from contamination sources. He further explained that Petitioner's deep well was cased in a consolidated formation which furnished protection from surface and lateral contaminants. Mike Turner testified that he has permitted and/or had experience with two thousand or more wells in his job with the St. Johns Water Management District. He stated unequivocally that Ms. Bobbitt's deep, pit-cased well was in no more danger from contamination from Scott's septic system, 50 feet away, than it is from the 65-foot reduced setback distance to her own septic system. Given these facts, Respondent is entitled to a variance for his proposed septic tank system.
Recommendation Based upon the findings of fact and conclusions of law, it is RECOMMENDED: That the variance should be granted by the Department of Health and Petitioner's challenge dismissed. DONE AND ENTERED this 8th day of June, 2000, in Tallahassee, Leon County, Florida. DIANE CLEAVINGER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 8th day of June, 2000. COPIES FURNISHED: Charlene J. Petersen, Esquire Department of Health 420 Fentress Boulevard Daytona Beach, Florida 32114 May Bobbitt 41 Zamora Street St. Augustine, Florida 32095 Allen C. D. Scott, II, Esquire 101 Orange Street St. Augustine, Florida 32084 Angela T. Hall, Agency Clerk Department of Health Bin A02 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1703 William Langue, General Counsel Department of Health Bin A02 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1701 Dr. Robert G. Brooks, Secretary Department of Health Bin A00 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1701
The Issue Whether Gar-Con's revised application for a permit to construct a sewage plant, and soakage trenches to dispose of the effluent, should be granted?
Findings Of Fact Eight to ten miles south of Melbourne Beach and 8.3 miles north of Sebastian Inlet, Gar-Con plans to develop a parcel of land stretching west from the Atlantic Ocean, across Highway A1A, to the Indian River. Gar-Con expects to build a motel and residential complex complete with tennis courts, parking garage, water treatment plant and the sewage treatment facility for which a construction permit is sought in these proceedings. The sewage treatment plant would be built on a site 480 feet west of Highway A1A and 90 feet south of Gar-Con's northern property line, at an elevation of 11 or 12 feet above mean sea level. Ocean Way Water and Sewer Association, Inc. is to be organized as a nonprofit corporation to own and operate the wastewater treatment facility. The Public Service Commission, through the director of its water and sewer treatment, has taken the position that the proposed "sewer system will fall within the exemption described in Section 367.022(7), Florida Statutes." DER's Composite Exhibit A. PACKAGE PLANT PROPOSED The facility Gar-Con proposes is designed to treat 100,000 gallons of sewage daily, which is the estimated "total flow" (T. 75) the sanitary engineer who designed the system anticipates from the development. Sewage generated by the development would flow to the plant, through a bar rack designed to remove rags and other large objects, and into aeration tanks where, over a 24 hour period, interaction with air and a biological mass would supply oxygen and cause the formation of biological floccules. The flocculant sewage would then move to a clarifier hopper. During its five hour stay there, solids which were not earlier segregated as the sewage moved over a weir into the clarifier, would be precipitated and removed. The clear, residual liquid would be pumped through one of two sand filters (each of which would also have granular activated carbon and be capable of filtering 100,000 gallons daily) into one of two chlorine contact chambers where a gas chlorinator would introduce chlorine for an hour. Under ordinary circumstances, the chlorinated effluent would then be pumped into one of two soakage trenches. The soakage trenches, each designed for use every other week, are to be gravel-filled ditches covered over first with felt paper, then with compacted fill. The gravel would lie at least one foot beneath the surface of the ground in a space ten feet wide and three feet deep stretching the 940 foot length of each soakage trench. Punctured like sieves, two six-inch PVC pipes would run through the gravel, sweating effluent from their pores. There is also a plan to dig a percolation pond or grassed swale five feet deep, 120 feet long and 80 feet wide near the wastewater treatment plant, which could serve as a receptacle for effluent, in case of "a 1:10 year storm or when the filters are down and/or if soakage trenches would need repair." Gar- Con's Exhibit 2-A. It would hold about 100,000 gallons. The solids caught by the weir, those extracted in the clarifying process, and those recovered from backwashing the filters would serve as catalyst for the aeration process as needed. Excess sludge, about 3,000 pounds monthly, would undergo "aerobic digestion," before being removed to Brevard County's Central Disposal Facility on Adamson Road, for disposal there. Gar- Con's Exhibit No. 7. Primary and secondary drinking water standards would be met by the effluent as it left the plant (although the engineer who designed the system would not drink the effluent himself), except that, from time to time, nitrate concentrations might reach 12 milligrams per liter, and except in the "event that a homeowner might put some type of [inorganic toxic or carcinogenic] material into the sewer system." (T. 86) The biological oxygen demand (BOD) would be ten milligrams per liter; suspended solids would probably amount to about five milligrams per liter; pH would probably be slightly under seven; nitrates would average approximately eight milligrams per liter but would "peak out at certain times during the year, for maybe extended periods up to two months, at twelve milligrams per liter," (T. 80); and there would be a chlorine residual after 60 minutes of two milligrams per liter. AMBIENT WATERS There would be no direct discharge to the Atlantic Ocean, Indian River or any other body of surface water, nor would any indirect effect on surface waters be measurable. No body of surface water lies within 500 feet of the site proposed for the plant and soakage trenches. Potable groundwater underlies the site; the groundwater table slopes toward the Atlantic Ocean, 9.5 to 12.5 feet below ground. "[D]uring the traditional rainy season," Gar-Con's Exhibit 2B, Attachment, p.3, the groundwater may rise to within seven feet of the surface. The PVC pipes in the soakage trenches are to be placed two and a half feet deep. As effluent percolated through the sandy soil, there would be "mounding" of the groundwater underneath the soakage trenches, and dispersal in all directions. Surface flow is to be diverted from the soakace trenches so that only rainwater falling directly on them would percolate down through the gravel beds. Taking soil characteristics into account, and assuming a "water table depth" of 20 feet, an engineer retained by Gar-Con predicted that "the maximum expected groundwater rises beneath the east and west trenches are 2.4 and 2.1 feet, respectively under a loading of 100,000 gpd for a period of 7 days." Gar-Con's Exhibit No. 3. The water table depth, "the height, the top of the groundwater from the first restrictive layer," (T. 172), is probably more like 40 feet than 20, which accounts in part for the "conservatism" of the mounding predictions. Under very severe weather conditions (a 100 year storm), groundwater would rise as high as the bottom of the trenches making them unavailable to receive effluent, but the effluent would not be forced above ground. In a 100 year flood, water would be expected to rise to seven feet above mean sea level. Under such conditions, people could be expected to evacuate the area. In a 25 year storm, the system could be expected to continue to function. Groundwater to the north and east of the proposed site was sampled, and the samples were analyzed. The water to the north had 380 milligrams of chlorides per liter and the water to the east had 450 milligrams of chlorides per liter. As it left the proposed treatment plant, the effluent would contain approximately 150 milligrams of chlorides per liter. SOUND AND LIGHT Lights like those used as street lights are to be installed at four places in the wastewater treatment plant. A timer, which can be overridden, would turn the lights on at dusk and off at eleven o'clock at night. The lights would illuminate the plant adequately. Pumps would move sewage to and through the proposed plant. Most of the pump motors would be submerged and unable to be heard. Two electric blowers, a flow meter and a totalizer would also have electrical motors. The blowers and the blower motors are to be equipped with insulated fiberglass covers and the blowers would also have intake and double outlet silencers. Four feet from the plant the noise of the motors would be comparable to that of a home air conditioning unit. At the nearest residence the noise level would scarcely exceed background noise. At hearing, Gar-Con revised its application and agreed to install an emergency generator which would also be encased in insulated housing and is to be equipped with a muffler. AEROSOL AND ODOR Unless the proposed plant loses electric power for 24 hours or longer, no offensive odors would emanate from it. The bar rack and weirs would be regularly hosed down. Against the possibility of a power failure, Gar-Con agreed at hearing to install permanently an emergency generator with sufficient capacity to keep both the wastewater treatment plant and the water treatment plant it plans to build operable. No aerosol drift is foreseen. The surface of the liquid In the aeration tanks would be 1.4 feet below the top of the rim. Walkways four feet wide along the inside perimeters of the aeration holding tanks would prevent dispersal of most of aerosol. A decorative hedge around the treatment plant, which would eventually be 15 feet high, is a final fail-safe. WELLS To the north are two shallow wells within 500 feet of the site proposed for the wastewater treatment plant. Both wells belong to Kel Fox, who wrote Gar-Con that he had no objection to their proposed wastewater treatment facility in light of Gar-Con's agreement to furnish drinking water to existing facilities on his property and reimburse him expenses incurred in disconnecting the two shallow wells. Gar-Con's Exhibit 2E. There is a deep well within 500 feet to the south. DER and Gar-Con have entered into the following stipulation, dated September 2, 1983: Existing Wells. Prior to the operation of its waste water treatment plant, Gar-Con will offer to supply drinking water at a reasonable cost to owners of property on which are located operational or approved shallow drinking water wells that are within 500 feet of Gar-Con's land application site. Gar-Con will make this offer to all such owners known to it prior to the operation of its plant. Gar-Con will further offer to provide reasonable compensation to such owners to disconnect their shallow wells. Gar-Con will endeavor to arrange for provision of drinking water to these owners and the disconnection of those wells prior to the operation of its plant. Future Wells. Should nearby individual (non-corporate) property owners propose to construct shallow drinking wells located within 500 feet of Gar-Con's land application site after Gar-Con begins operation of its waste water treatment plant, Gar-Con also will offer to supply them with drinking water at a reasonable cost and to provide reasonable compensation to them to disconnect those wells. However, Gar-Con shall have no obligation to make any such offer to owners of future wells if sampling of monitoring wells located at or near its external property line indicates that the groundwater meets the primary drinking water standards and, after July 1, 1985, the secondary drinking water standards listed in Florida Administrative Code Rule 17-22.104. Gar-Con agrees to record a master notice of restriction barring future owners of lots within the Ocean Way development, which are owned by Car-Con at the time of permit issuance, from installing shallow drinking water wells on such property or otherwise using the shallow aquifer beneath their property as a source for irrigation or for potable water, so long as use of the proposed sewage disposal system continues, and the Department has not found that this restriction is unnecessary. This restriction, which shall be a covenant running with the land, further shall require future owners to purchase water from Gar-Con or any successor owner of the development's water system if Gar-Con or the successor provides water service. These restrictions also shall be contained in all other appropriate documents of title. In addition, Gar-Con plans to create a non-profit water and sewer association to own and control the development's water and sewer system. Gar-Con will include in the Articles of Incorporation of this association a requirement that all property owners served by the system must be members of the Association. Gar-Con is entitled to a zone of discharge extending to its current property line with the exception that the zone of discharge shall not include the area contained within a 100' radius of Gar-Cons's proposed water supply wells. DER Staff concurs that the above conditions, in conjunction with the sewage treatment and disposal system and the groundwater monitoring program proposed by the applicant, to meet the requirements of Chapter 17-4, F.A.C. will provide reasonable assurance that existing and future off-site and on-site property owners will be protected from any adverse effects that might result from the operation of the proposed sewage treatment disposal system. Petitioner's Exhibit No. 10. There are to be a half dozen monitoring wells to allow sampling of the groundwater at strategic points in the shallow aquifer. NATURAL RESOURCES Turtles nest in the general vicinity but off the site of the proposed project. Construction and operation of the proposed waste water treatment facility would have no impact on the turtles apart from making it possible for more people to live closer to where they nest.
The Issue Whether the Respondent committed the violations alleged in the Administrative Complaint dated January 8, 1999, and, if so, the penalty which should be imposed.
Findings Of Fact Based on the oral and documentary evidence presented at the final hearing and on the entire record of this proceeding, the following findings of fact are made: The Department of Health, including the county health departments such as the St. Lucie County Health Department ("County Health Department"), are responsible for supervising and controlling limited use public water systems. Section 381.0062(3), Florida Statutes (1997). Mr. Gorman is the owner of three duplexes located at 120 and 122 Laidback Way, Fort Pierce, Florida; 140 and 142 Laidback Way, Fort Pierce, Florida; and 160 and 162 Laidback Way, Fort Pierce, Florida. The duplexes were built in 1982 and 1983 and each contains two units which are available for rent. Water is piped into each duplex from a well located on the property. The wells providing water to 120 and 122 Laidback Way and to 140 and 142 Laidback Way were inspected by the Department of Health and Rehabilitative Services in May 1994 and found to be satisfactory pending results of water tests. Two-day bacteriological analyses were conducted on May 2 and 3, 1994, on the wells serving these two properties, and the results were satisfactory. 3/ The 1994 inspection report for the well serving the property at 120 and 122 Laidback Way reflects that it had the following equipment: a one-half horsepower pump; a 30-gallon "p tank"; a 20-gallon water softener filter; and a 30-gallon brine tank. The 1994 inspection report for the well serving the property at 140 and 142 Laidback Way reflects that it had the following equipment: a one-half horsepower pump; a 20-gallon "p. tank"; a 25-gallon water softener filter; and a 40-gallon brine tank. In a letter dated August 21, 1998, the County Health Department notified Mr. Gorman that he needed to submit the application enclosed with the letter and a $140.00 fee to bring the "permit" to current status for the property located at 140 and 142 Laidback Way. The letter was inartfully composed and conveyed incomplete information regarding the nature of the permit. The letter did, however, contain reference to "Chapter" 381.0062, Florida Statutes, and Chapter 64E-8, Florida Administrative Code, and it also provided notification that Chapter 64E-8 required quarterly sampling of limited use public water systems for bacteria and a lead and nitrate test every three years. The County Health Department sent Mr. Gorman an identical notice, dated August 21, 1998, regarding the property located at 160 and 162 Laidback Way. The County Health Department sent Mr. Gorman a somewhat different letter, dated August 31, 1998, regarding the "Limited Use Public Water Systems" for the property located at 120 and 122 Laidback Way. The letter notified Mr. Gorman that his permit to operate the "referenced water system has expired as of September 30, 1998." The letter reiterated the information contained in the August 21 letter and requested in addition that Mr. Gorman submit "a minimum 8.5 x 11 inch site plan of the system, drawn to scale, that accurately identifies the location of the source of water in relation to property boundaries and contaminant sources, i.e., well must be 75 feet from septic system, etc." and an "[e]quipment list: pump, tank, softener, automatic chlorinate, etc., manufacturer, model #, and capacity." Finally, Mr. Gorman was notified of the permitting and testing fees and told that the "[a]pplication with required site and equipment information must be submitted with necessary fees within 30 days receipt of this notification." Mr. Gorman responded with a letter dated October 16, 1998, in which he posed several questions to the County Health Department: Do you understand that these are duplexes? Are all rental properties including single family subject to these regulations? Can you give me a valid reason why rental units of two units or more should be subject to quarterly bacterial testing (I believe the statute only authorizes it annually) and not all other residential properties, public facilities or otherwise that might use well water? Mr. Gorman requested a response to his questions but did not provide the information, applications, and permit fees requested in the letters dated August 21 and August 31. In a letter dated December 14, 1998, sent certified mail with return receipt requested and referenced as a Notice of Violation, the County Health Department notified Mr. Gorman that he was operating limited use community public water systems without a permit at 120 and 122, 140 and 142, and 160 and 162 Laidback Way and that he had not provided the following required information: Signed, dated application form. An operation permit fee of $75.00 for the initial permit. A site plan of the property that accurately identifies the location of the well in relation to property, boundaries and contaminant sources such as septic tank systems. Capacity/size, model and brand information on system components. Well completion report if available or year well was installed if known. Required chemical analysis results (lead and nitrate). Initial satisfactory two-day source (well) water and system water bacteriological tests results. Mr. Gorman was told to contact Bruce McLeod within five days of receipt of the notice. Although Mr. Gorman received the notice on December 16, 1998, he did not respond. The County Health Department had not, as of the final hearing, received any reports of illness attributable to the water from the wells at the subject properties, and it does not have any reason to believe that the wells are contaminated. Mr. Gorman had not, as of the final hearing, submitted the applications, permit fees, or information requested by the County Health Department, and he had no operating permits for the wells providing water to the subject properties. The evidence presented in this case is sufficient to establish that the wells providing water to the three duplexes owned and rented by Mr. Gorman each contains two rental units and are limited use community public water systems. Mr. Gorman must have operating permits for the wells providing water to these properties.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Health enter a final order: Finding that Robert J. Gorman is guilty of three violations of Section 381.0062, Florida Statutes (1997), because he failed to obtain operating permits for the limited use community public water systems he maintains at 120 and 122, 140 and 142, and 160 and 162, Laidback Way, Fort Pierce, Florida; and Imposing an administrative fine in the amount of $1500.00, or $500.00 for each of the three violations. DONE AND ENTERED this 25th day of June, 1999, in Tallahassee, Leon County, Florida. PATRICIA HART MALONO Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 25th day of June, 1999.
The Issue The issue in this case is whether a variance for a reduced setback of four feet from Petitioner's well to a building pad treated with pesticide should be denied by the Department of Health.
Findings Of Fact Petitioner resides on property consisting of 7.5 acres at 3665 Darby Road, New Smyrna Beach, Volusia County, Florida. Since Petitioner receives no public utility service at his home, he has a septic system and potable drinking water well on his property. However, Petitioner's family does not drink the water from the well. The family purchases bottled water for drinking purposes. The well water is used for other household purposes, such as cleaning and bathing. There are other locations on Petitioner's property for a well. The evidence demonstrated that Petitioner has or had alternative locations for the well. Petitioner built a 1681 square foot barn utilizing an old concrete foundation from a previous barn. Petitioner's well is located in the southwest corner of the old barn's foundation and four feet from the new barn's foundation. The building plans for the barn, submitted to Volusia County, clearly indicated the location of Petitioner's well within four feet of the new barn's foundation. Even with this information Volusia County issued a building permit for the new barn. There were other locations for the barn on Petitioner's property which Petitioner would have utilized had he known of the setback requirements when he first permitted his barn. Volusia County required the new barn's foundation to be elevated. In order to elevate the sub-floor for the new barn's foundation, Petitioner placed a layer of visqueen on the sub- floor, or old concrete floor of the old barn, then added a layer of sand and poured concrete on top of the sand layer. The sand layer is encased in concrete. The concrete encasement does not necessarily prevent leaks from above given the porous nature of concrete. Additionally, the condition of the old barn floor, i.e. whether it has cracks, is not known. The Volusia County building code requires that the soil under a foundation be treated for termites. After Petitioner's contractor added the sand layer, he spread one four-pound bag of 90 percent Sevin dust, a common garden pesticide, on top of the sand. The application rate was within normal application rates for the barn area. The Sevin dust was not applied with any pressure to force penetration into the soil. More than seven days later the contractor poured the new concrete foundation on the pesticide-treated sand layer. The label on the Sevin dust package indicates that 10 percent Sevin dust may be applied to vegetables up to the day of harvest and in some instances 3 to 7 days before harvest, depending on the type of crop. However, the package does not indicate that a treated crop is edible for human consumption without first washing the crop or other processing of the crop. Therefore, a lack of danger from contamination has not been shown. Indeed, the evidence did not show that health would not be adversely affected by use of Petitioner's well given this major deviation from the setback requirements and the soil in the area. A Volusia County building inspector informed Petitioner's contractor that the close proximity of Petitioner's potable well to the area treated with pesticide was a violation of state health codes and could not be approved because the well did not meet the requirement of having a 25-foot separation from soil treated with pesticide. The contractor informed Steve Baur, a Department of Health employee, about the violation. The deviation of 21 feet from the 25-foot setback requirement is a major deviation. Petitioner applied to DOH for a variance to allow him to utilize his potable drinking water well. Petitioner's variance application was denied by the variance committee and Dr. Sharon Heber, Department of Health Environmental Health Director, for the following reasons: Section 64E-8.009(2), F.A.C., allows the granting of variances to 'prevent excessive hardship only in cases involving a minor deviation from established standards when the hardship was not intentionally caused by the applicant, where no reasonable alternative exists, and where proper use of the system will not adversely affect public health.' According to information supplied by the Volusia County Health Department, the treated slab is located 4 feet from the existing well. This is a major deviation from the established standards. The well completion report for the existing well indicates coarse shell starting at 10 feet and continuing down to 60 feet. This material provides no filtration and/or confinement for the pesticide.
Recommendation Based upon the findings of fact and conclusions of law, it is RECOMMENDED: That the Department of Health enter a final order denying Petitioner's request for a variance. DONE AND ENTERED this 14th day of June, 2000, in Tallahassee, Leon County, Florida. DIANE CLEAVINGER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 14th day of June, 2000. COPIES FURNISHED: Charlene J. Petersen, Esquire Department of Health 420 Fentress Boulevard Daytona Beach, Florida 32114 Edward N. Pollack 3665 Darby Road New Smyrna Beach, Florida 32168 Angela T. Hall, Agency Clerk Department of Health Bin A02 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1703 William Langue, General Counsel Department of Health Bin A02 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1701 Dr. Robert G. Brooks, Secretary Department of Health Bin A00 2020 Capital Circle, Southeast Tallahassee, Florida 32399-1701
The Issue Whether SFP's revised application for a permit to construct a sewage treatment plant with percolation ponds should be granted or, for failure of SFP to give reasonable assurances that the plant will not cause pollution significantly degrading the waters of Gator Cove, be denied?
Findings Of Fact About 1,500 feet from Santa Fe Lake's Gator Cove, SFP proposes to build an extended aeration package sewage treatment plant to serve a "private club with restaurant and overnight accommodations," SFP's Exhibit No. l, to be built between the plant and the lake, on the western shore of Santa Fe Lake, just south of the strait or pass connecting Santa Fe Lake and Little Santa Fe Lake. The site proposed for the waste water treatment plant lies at approximately 177 or 178 feet above sea level, north of Earleton on county road N.E. 28 near State Road 200A, some three miles north of State Road 26, in unincorporated Alachua County, Section 33, Township 8 South, Range 22 East. SFP's Exhibit No. 1. Santa Fe Lake, also called Lake Santa Fe, and Little Santa Fe Lake, also called Little Lake Santa Fe, are designated outstanding Florida waters by rule. Rule 17-3.041(4)(i), Florida Administrative Code. Lake Santa Fe "is . . . the sixth largest non-eutrophic lake in the State of Florida . . . [and] the last remaining large non-eutrophic lake in Alachua County." (0.367). Recreation is a "beneficial use" of these waters. The Lakes Santa Fe are at an elevation of approximately 140 feet above sea level, and their level varies within a range of four feet. Input The proposed plant is to treat sewage generated by staff, by diners at a 150-seat restaurant, and by inhabitants of 150 lodge or motel rooms, comprising 100 distinct units. On the assumptions that 150 rooms could house 275 persons who would generate 75 gallons of sewage a day for a daily aggregate of 20,625 gallons, and that a 150-seat restaurant would generate 50 gallons of sewage per seat per day, full occupancy is projected to engender 28,125 gallons of sewage per day. This projection is based on unspecified "D.E.R. criteria; (5.35) which the evidence did not show to be unreasonable. Full occupancy is not foreseen except around the Fourth of July, Labor Day and on other special occasions. An annual average flow of between 15 and 20,000 or perhaps as low as 13,000 gallons per day is envisioned. (S.38) The proposed plant is sized at 30,000 gallons per day in order to treat the peak flow forecast and because package plants are designed in 5,000 gallon increments. Sluice-gate valves and baffling are to permit bypassing one or more 5,000 gallon aeration units so plant capacity can be matched to flow. The composition of the sewage would not be unusual for facilities of the kind planned. As far as the evidence showed, there are no plans for a laundry, as such, and "very little laundry" (S.37) is contemplated. The health department would require grease traps to be installed in any restaurant that is built. Gravity would collect sewage introduced into 2,000 feet of pipe connecting lodging, restaurant and a lift station planned (but not yet designed) for construction at a site downhill from the site proposed for the water treatment plant. All sewage reaching the proposed treatment plant would be pumped 3,000 feet from the lift station through a four-inch force main. Influent flow to the treatment plant could be calculated by timing how long the pump was in operation, since it would "pump a relatively constant rate of flow." (S.39) Treatment Wastewater entering the plant would go into aeration units where microorganisms would "convert and dispose of most of the incoming pollutants and organic matter." (S.40) The plant would employ "a bubbler process and not any kind of stirring-type motion . . . [so] there should be very little:; aerosol leaving the plant," (S.42) which is to be encircled by a solid fence. Electric air blowers equipped with mufflers would be the only significant source of noise at the proposed plant, which would ordinarily be unmanned. If one blower failed, the other could run the plant itself. A certified waste water treatment plant operator would be on site a half-hour each week day and for one hour each weekend. SFP has agreed to post a bond to guarantee maintenance of the plant for the six months' operation period a construction permit would authorize. (0.63) The proposed plant would not "create a lot of odor if it's properly maintained." Id. The specifications call for a connection for an emergency portable generator and require that such a generator be "provide[d] for this plant. . . ." (S. 43). The switch to emergency power would not be automatic, however. A settling process is to follow extended aeration, yielding a clear water effluent and sludge. Licensed haulers would truck the sludge elsewhere for disposal. One byproduct of extended aeration is nitrate, which might exceed 12 milligrams per liter of effluent, if not treated, so an anoxic denitrification section has been specified which would reduce nitrate concentrations to below 12 milligrams per liter, possibly to as low as 4 or 5 milligrams per liter. Before leaving the plant, water would be chlorinated with a chlorinator designed to use a powder, calcium hypochlorite, and to provide one half part per million chlorine residual in the effluent entering the percolation ponds. A spare chlorine pump is to be on site. The effluent would meet primary and secondary drinking water standards, would have 20 milligrams or less per liter of biochemical oxygen demand or, if more, no more than ten percent of the influent's biochemical oxygen demand, and total suspended solids would amount to 20 milligrams or less per liter. (5.294- 295). Half the phosphorous entering the plant would become part of the sludge and half would leave in the effluent. Something like ten milligrams per liter of phosphorous would remain in the effluent discharged from the plant into the percolation ponds. (5.202). Although technology for removing more phosphorous is available (S.298, 0.170-171), SFP does not propose to employ it. Allen flocculation treatment followed by filtration could reduce phosphorous in the effluent to .4 milligrams per liter, but this would increase the cost of building the treatment plant by 30 to 40 percent; and operational costs would probably increase, as well, since it would be necessary to dispose of more sludge. (0.170-172). SFP did agree to accept a permit condition requiring it to monitor phosphorous levels in groundwater adjacent to the proposed plant. (0.63). Land Application Three percolation ponds are planned with an aggregate area of 30,000 square feet. At capacity, the plant would be producing a gallon and a half of effluent a day for each square foot of pond bottom in use. The ponds are designed in hopes that any two of them could handle the output of effluent, even with the plant at full capacity, leaving the third free for maintenance. The percolation ponds would stand in the lakes' watershed, in an area "of minimal flooding, (S.30) albeit outside the 100-year flood plain. Santa Fe Lake, including Gator Cove, and Little Santa Fe Lake are fed by groundwater from the surficial aquifer. All effluent not percolating down to levels below the surficial aquifer or entering the atmosphere by evapotranspiration would reach the lake water one way or another sooner or later. If percolation through the soils underneath the percolation ponds can occur at the rate SFP's application assumes, effluent would not travel overland into Lake Santa Fe except under unusually rainy conditions, which would dilute the effluent. Whether the planned percolation ponds would function as intended during ordinary weather conditions was not clear from the evidence, however. In the event the ponds overflowed, which, on SFP's assumptions, could be expected to happen, if peak sewage flaw coincided with weather more severe than a 25-year rainfall, effluent augmented by rainwater would rise to 179.87 NGVD (S.34), then overflow a series of emergency weirs connecting the ponds, flow through an outfall ditch, drain into a depression west of the ponds, enter a grassed roadside ditch, and eventually reach Lake Santa Fe after about a half a mile or so of grass swales. (5.69). Sheet flow and flow through an ungrassed gulley in the direction of Gator Cove (0.154) are other possible routes by which overflowing waters might reach the lake. (0.263). Since the facilities the plant is designed to serve are recreational, wet weather would discourage full use of the facilities and therefore full use of the water treatment system. Effluent traveling over the surface into Gator Cove would wash over vegetation of various kinds. Plants, of course, do take up phosphorous, but they don't do it forever, and if you leave a plant system alone, it will come to a steady state in which there is no net storage of phosphorous in the plant material. (0.166) Whether by sheet flow or by traversing swales, overland flow would reach Gator Cove within hours. Effluent traveling through the surficial aquifer would not reach the lake for at least five years. (S.238-9). It could take as long as 45 years. (0.316). In the course of the effluent's subterranean passage, the soil would take up or adsorb phosphorous until its capacity to do so had been exhausted. In addition, interaction with certain chemicals found in the soil, primarily calcium, precipitates phosphorous dissolved in groundwater. As between adsorption and precipitation, the former is much more significant: "[W]ith a three-meter distance you can expect at least 70 to 80 percent removal of phosphorous just by a a[d] sorption alone." (0.21). Precipitated phosphorous does not return to solution, unless the soil chemistry changes. (0.19) Adsorption, however, is reversible, although not entirely, because of the "hysteresis phenomenon." (0.19) Eventually, a kind of dynamic equilibrium obtains to do with the binding of the phosphorous to soil constituents, binding or precipitation of phosphorous. At some point . all of the binding sites become saturated . [and] the amount of phosphorous leaving, into the lake really, will be equal to the amount of phosphorous going into the the system. When there is no more place to store the phosphorous in the ground, then the output is equal to the input and that is called the steady state. (0.161) Although precipitation of phosphorous would not reach steady state under "conditions that render the phosphorous-containing compound insolu[]ble," (0.168) these conditions were not shown to exist now "much less . . . on into perpetuity." Id. Spring Seep A third possible route by which the effluent might reach lake waters would begin with percolation through the sand, which is to be placed on grade and on top of which the percolation ponds are to be constructed. Underground, the effluent would move along the hydraulic gradient toward the lake unless an impeding geological formation (an aquiclude or aquitard) forced it above ground lakeward of the percolationi ponds. In this event, the effluent would emerge as a man-made spring and complete its trip to Gator Cove, or directly to the lake, overland. The evidence demonstrated that a spring seep of this kind was not unlikely. Relatively impermeable clayey soils occur in the vicinity. A more or less horizontal aquitard lies no deeper than four or five feet below the site proposed for the percolation ponds. Conditions short of an actual outcropping of clayey sand could cause effluent mounding underground to reach the surface. Nor did the evidence show that an actual intersection between horizontal aquitard and sloping ground surface was unlikely. Such a geological impediment in the effluent's path would almost surely give rise to a spring seep between the pond site and the lakes. In the case of the other percolation ponds in this part of the state that do not function properly, the problem is n [U] sually an impermeable layer much too close to the bottom of the pond," (S.179), according to Mr. Frey, manager of DER's Northeast District. Phosphorous in effluent travelling by such a mixed route would be subject to biological uptake as well as adsorption and precipitation, but again a "steady state" would eventually occur. On Dr. Bothcher's assumptions about the conductivity of the clayey sand (or sandy clay) lying underneath the topsoil, the effluent would accumulate as a mound of groundwater atop the clay unit, and seep to the surface in short order; and "after a matter of probably weeks and maybe months, it would be basically of the quality of the water inside of the percolation pond." (0.278). More Phosphorous in Gator Cove The total annual phosphorous load from all existing sources "to the lake" has been estimated at 2,942 kilograms. Assuming an average effluent flow of 17,000 gallons per day from the proposed plant, "the total phosphorous load [from the proposed plant] will be 235 kilograms per annum," (0.16), according to Dr. Pollman, called by SFP as an expert in aquatic chemistry. Even before any steady state condition was reached, 20.75 to 41.5 kilograms of phosphorous, or approximately one percent of the existing total, would reach the lake annually from the proposed plant, on the assumptions stated by Dr. Pollman at 0.22-23 (90 to 95 percent removal of phosphorous in the soils and average daily flow of 30,000 gallons). Santa Fe Lake is more than two miles across and two miles long, and Little Santa Fe Lake, which may be viewed as an arm of Santa Fe Lake, is itself sizeable, with a shoreline exceeding two miles. But Gator Cove is approximately 200 yards by 100 yards with an opening into Santa Fe Lake only some 50 to 75 yards wide. (0.154). On a site visit, Dr. Parks observed "luxuriant growth of submerged plants" (0.154), including hydrilla, in Gator Cove. If a one percent increase in phosphorous were diffused evenly throughout the more than eight square miles Santa Fe Lake covers, there is no reason to believe that it would effect measurable degradation of the quality of the water. Some nutrients are beneficial, and the purpose of classifying a lake is to maintain a healthy, well-balanced population of fish and wildlife. It's hard to see how 1.4 percent increase would lower the ambient quality. But . . . seepage into Gator Cove, which is a much more confined place [100 by 200 yardsj [would make it] quite probable that there would be a lowering of ambient water quality in the site . R] educed dispersion . . . in this cove would allow . . . phosphorous to build up. (0.156) Overland effluent flow to Gator Cove would increase concentrations of phosphorus there, with a consequent increase in the growth of aquatic plants, and the likely degradation of waters in the Cove, unless rapid and regular exchange of lake and cove waters dispersed the phosphorous widely, promptly upon its introduction Except for testimony that wind-driven waves sometimes stir up phosphorous laden sediments on the bottom, the record is silent on the movement of waters within and between Lake Santa Fe and Gator Cove. The record supports no inference that phosporous reaching Gator Cove would be dispersed without causing eutrophic conditions significantly degrading the water in the Cove. Neither does the record support the inference, however, that effluent moving underground into the lakes would enter Gator Cove. On this point, Dr. Bottcher testified: [T]he further away from the lake that you recharge water the further out under a lake that the water will be recharging into the lake; gives it a longer flow . . . it's going to migrate and come up somewhat out into the lake. (0.281-2) Phosphorous in the quantities the treatment plant would produce, if introduced "somewhat out into the lake" would probably not degrade water quality significantly, notwithstanding testimony to the contrary. (0.349, 354). Sands and Clays DER gave notice of its intent to deny SFP's original application because SFP proposed to place the pond bottoms approximately two and a half feet above an observed groundwater table. Placement in such proximity to groundwater raised questions about the capacity of the ground to accept the effluent. In its revised application, SFP proposes to place sand on the existing grade and construct percolation ponds on top of the sand. By elevating the pond bottoms, SFP would increase the distance between the observed groundwater table and pond bottoms to 5.2 feet. (S.256, 257). This perched water table, which is seasonal, is attributable to clayey sand or sandy clay underlying the site proposed for the percolation ponds. Between January 9, 1985, and January 17, 1985, "following a fairly dry antecedent period," (S.229) Douglas F. Smith, the professional consulting engineer SFP retained to prepare the engineering report submitted in support of SFP's permit applications, conducted six soil borings in the vicinity of the site proposed for the plant. One of the borings (TB 5) is in or on the edge of a proposed percolation pond and another (TB 4) is slightly to the north of the proposed pond site. Three (TB 1, 2 and 3) are east of the proposed pond site at distances ranging up to no more than 250 feet. The sixth is west of the proposed site in a natural depression. Mr. Smith conducted a seventh test boring under wetter conditions more than a year later a few feet north of TB 4. Finally, on September 5, 1986, during the interim between hearing days, Mr. Smith used a Shelby tube to obtain a soil sample four to six feet below grade midway between TB 4 and TB 5. 1/ The sites at which samples were taken are at ground elevations ranging from 173 to 178 feet above sea level. From the original borings and by resort to reference works, Mr. Smith reached certain general conclusions: The top four feet or so at the proposed pond site consists of silty sand, 17 percent silt and 83 percent quartz sand. This topsoil lies above a two-foot layer of clayey sand, 20 percent clay, 6 percent silt and 74 percent sand. Below the clayey sand lies a layer some eight feet thick of dense, silty sand, 23 percent silt, 7 percent clay and 70 percent sand, atop a one and one-half foot layer of clayey sand, separating loose, quartz sands going down 40 feet beneath the surface from what is above. These formations "are very heterogeneous, in the sense of the position and occurrence of the clay layers or the sandy layers . . .," (0.230) and all occur within the surficial aquifer. "There are layers of clay within it, and so perched water tables are rather common." (0.225). In March of 1986, the regional water table was some 17 feet down. SFP Exhibit 1B. Below the surficial aquifer lie the Hawthorne formation and, at a depth of 110 feet, the limestone of the Floridan aquifer. The soils above the Hawthorne formation are not consolidated. (S.254, 255). Conductivity Measurements The applicant offered no test results indicating the composition or conductivity of soils lying between the easternmost test boring and Gator Cove, some 1,200 feet distant. No tests were done to determine the conductivity of the deeper layer of clayey sand beneath the site proposed for the ponds. Tests of a sample of the topsoil in TB 7 indicated horizontal permeability of 38.7 feet per day and vertical permeability of six feet per day. On the basis of an earlier test of topsoil in TB 3, "hydraulic conductivity of the surface soils was measured to be 8.2 feet per day. . . ." SFP's Exhibit No. 1B. From this measurement, vertical hydraulic conductivity was conservatively estimated at .82 feet (9.84 inches) per day. Id. The design application rate, 2.41 inches per day, is approximately 25 percent of 9.84 inches per day. Id. The initial test done on a sample of the clayey sand, which lay beneath the topsoil at depths of 3.5 to 5.5 feet, indicated a permeability of 0.0001 feet per day. Thereafter, Mr. Smith did other testing and "made some general assumptions" (S. 235) and concluded that "an area-wide permeability of this clayey sand would be more on the order of 0.0144 feet per day." (S. 234). Still later a test of the sample taken during the hearing recess indicated hydraulic conductivity of 0.11 feet per day. SFP's Exhibit No. 10. The more than thousandfold increase in measured conductivity between the first laboratory analysis and the second is attributable in some degree to the different proportions of fines found in the two samples. The soil conductivity test results depend not only on the composition of the sample, but also on how wet the sample was before testing began. Vertical Conductivity Inferred On March 6, 1986, ground water was observed on the site about two and a half feet below the surface. SFP's expert, Mr. Smith, concluded that it was "essentially a 1.5 foot water table, perched water table over the clay." (0.422). There was, however, groundwater below, as well as above, the clay. On March 12, 1986, the water table at this point had fallen six inches. In the preceding month rainfall of 5.9 inches had been measured in the vicinity, after 5.1 inches had been measured in January of 1986, but in November and December of 1985 "there was a total of 0.6 inches of rainfall." (0.421). Later in the year, notwithstanding typically wet summer weather, no water table was measured at this point. From this Mr. Smith concluded that, once the clayey sand layer is wetted to the point of saturation, conductivity increases dramatically. If that were the case, a more or less steady stream of effluent could serve to keep the clayey sand wetted and percolation at design rates should not be a problem. But Dr. Bottcher, the hydrologist and soil physicist called as a witness for the Association, testified that the six- inch drop over six days could be attributed, in large part, to evapotranspiration. He rejected the hypothesis that the clayey sand's conductivity increased dramatically with saturation, since "the actual water table was observed . about three weeks after the very heavy rainfall had stopped" (0.290) and had probably been present for at least a month; and because the soil survey for Alachua County reports that perched water tables ordinarily persist for two months (0.227) in this type of soil. Certain soils' hydraulic conductivity does diminish with dessication, but such soils usually regain their accustomed conductivity within hours of rewetting. Dr. Bottcher rejected as unrealistically optimistic the assumption SFP's expert made about the conductivity of the clayey sand on grounds that "the conductivity that . . . [SFP] used, if you went out there you couldn't perch a water table for a month." (0.277). In these respects, Dr. Bottcher's testimony at hearing has been credited. In the opinion of the geologist who testified on behalf of the Association, Dr. Randazzo, a minimum of seven or eight additional augur borings in "definitive patterns to the northeast and to the northwest" (0.240) to depths of 15 to 20 feet, with measurements within each augur boring every two feet, are necessary to determine "how permeable the soils are and how fast the waters would move through them." (0.240). This testimony and the testimony of the soil physicist and others to the same general effect have been credited, and Mr. Smith's testimony that no further testing is indicated has been rejected. Wet Ground In the expert opinion of a geologist who testified at hearing, "it is reasonable to assume that saturation conditions of the surficial aquifer in this area can be achieved," (0.238) even without adding effluent from a wastewater treatment plant. The evidence that soils in the vicinity of the site have a limited capacity to percolate .water came not only from engineers and scientists. Charles S. Humphries, the owner of the property 150 feet from the proposed percolation site, "put a fence post line . . . every ten feet, and every ten feet [he] hit clay." (0.372). Three quarters of an inch of rain results in waters standing overnight in neighboring pastures. In parts of the same pastures, rain from a front moving through "will stay for a week or so." (0.373). It is apparent that the area cannot percolate all the rainfall it receives. This is the explanation for the gully leading down toward Gator Cove. Six-feet deep (0.377), "the gully is a result of natural surface runoff." (0.263).
Findings Of Fact In approximately 1987, the Petitioner purchased land in Pinellas County, of which approximately 85 percent lies within jurisdictional wetlands. (The jurisdictional wetlands approximate the surface water mean high water line.) Some of the wetlands will have to be filled in order to construct a residential dwelling on the property. The nearest public sewer connection is over a mile away from the Petitioner's property. The only reasonable alternative for the treatment of residential sewerage is an onsite sewage treatment and disposal system. The only reasonable alternative for construction of an onsite sewage treatment and disposal system on the property would require a drainfield to be located well within 75 feet of the jurisdictional wetlands, which are surface waters of the State. In fact, the proposed drainfield would have to be as close as six to twelve feet from the jurisdictional wetlands in most places. In addition, there is a drainage ditch along the road on the western boundary of the Petitioner's property. The drainage ditch contains water for extended periods of time in the rainy summer months. The drainfield for the Petitioner's proposed onsite sewage treatment and disposal system would be approximately 21 feet from the drainage ditch. In other words, a 75 foot setback from the drainage ditch would overlap the 75 foot setback from the jurisdictional wetlands. Although the Petitioner's proposed onsite sewage treatment and disposal system is designed to function without failing during such conditions, parts of the drainfield can be expected to be inundated during the rainy season. In effect, as a result of rainfall and runoff during rainy weather, the water from the wetlands and the drainage ditch would be expected to overflow the jurisdictional line and the ditch banks and inundate parts of the drainfield. There would be a direct connection between the waters inundating the drainfield and the surface waters of the wetland and of the drainage ditch. The Petitioner proposes to have, and several neighbors have, potable water wells to supply drinking water. There are sinkholes all over the area of the Petitioner's property. It is not known whether there is a sinkhole on the Petitioner's property, but it is well known that sinkholes are common in cypress head swamps like the wetlands on the Petitioner's property. If there is a sinkhole, or if one develops, it could act as a direct conduit from the surface water to the aquifer from which the private drinking water wells in the area draw water. Contamination from the Petitioner's drainfield then would be able to contaminate the drinking water. Potential fecal coliform contamination of the surface waters adjacent to the Petitioner's proposed drainfield (both the wetlands and the drainage ditch) also could pose a public health threat. The County recently has disposed of digested sludge in the vicinity of the Petitioner's site (i.e., within approximately a mile away). (It is not clear from the evidence whether this still is taking place.) However, under applicable Department of Environmental Protection rules, the sludge was being applied to pasture at least 300 feet from cypress heads, and the County also was required to meet other environmental controls and regulations for that kind of disposal. The Petitioner's evidence did not prove that discharge from his proposed onsite sewage treatment and disposal system will not adversely affect the health of the Petitioner or the public or that it will not significantly degrade the groundwater or surface waters.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is recommended that the Department of Health and Rehabilitative Services (HRS) enter a final order denying the Petitioner's application for a variance. RECOMMENDED this 14th day of March, 1994, in Tallahassee, Florida. J. LAWRENCE JOHNSTON Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 14th day of March, 1994. COPIES FURNISHED: R. Patrick Mirk, Esquire Post Office Box 10598 Tampa, Florida 33679-0598 David Jon Fischer, Esquire Assistant District Legal Counsel Department of Health and Rehabilitative Services 11351 Ulmerton Road Largo, Florida 34648 Robert L. Powell Agency Clerk Department of Health and Rehabiltiative Services 1323 Winewood Blvd. Tallahssee, Florida 32399-0700 Kim Tucker, Esquire General Counsel Department of Health and Rehabiltiative Services 1323 Winewood Blvd. Tallahssee, Florida 32399-0700
Findings Of Fact Tim Youngquist is a licensed water well contractor, holding Florida license #2172, and is principal of Youngquist Brothers, Inc. The South Florida Water Management District, operating pursuant to Chapter 373, Florida Statutes, and Chapter 40E, Florida Administrative Code, is responsible for the permitting and regulation of nonexempt water well drilling within the District's geographical jurisdiction. Unless specifically exempted from permitting requirements, each well must be separately permitted prior to construction. Due to the unique characteristics of wells, well construction permits are issued separately for each individual well and are not issued on a site basis. The Respondent, in the summer of 1990, contracted with the City of Fort Myers, Florida, to construct twenty public water supply wells and eight monitoring wells, all located within the existing city well field site. The Respondent was responsible for compliance with all applicable permit requirements. On December 19, 1990, the Respondent obtained the appropriate city permit for the drilling operation, but did not at that time apply for or obtain any permits as required by the Petitioner. The City of Fort Myers permits wells in compliance with the Standard Plumbing Code, but does not have a well construction ordinance. The city permit does not substitute for the Petitioner's well construction permits. On April 9, 1990, the Petitioner received an inquiry from a representative of the Lee County Health Department as to whether the Respondent had obtained well construction permits from the Petitioner. At that time, there had been no application for the permits submitted to the Petitioner by the Respondent. On April 10, 1990, Don Douglas, Youngquist Brothers manager for the Fort Myers city wells project, contacted the Petitioner and inquired as to the method for obtaining permits for the well construction. Mr. Douglas was advised to immediately cease any well construction operations at the City of Fort Myers well field pending receipt of the appropriate permits. On April 11, 1991, Petitioner's staff inspected the City of Fort Myers well field site, and observed six newly- completed public supply wells on the site. Petitioner's staff again instructed Respondent's representative to cease any further activity. There is no evidence that, subsequent to the Petitioner's directions to cease operations at said site, any additional construction activities occurred. On April 16, 1991, Petitioner's staff again inspected the City of Fort Myers well field site, and observed three additional public supply wells on the site, two of which were surface-cased with the third well appearing to be completed. On May 23, 1991, a Notice of Violation (NOV) was issued to Youngquist citing the failure to obtain well construction permits for the seven completed public water supply wells and the failure to provide notice to the Petitioner 24 hours in advance of the placement of grout in the annular spaces of the seven wells. The Petitioner's staff determined that the extent of the two surface- cased wells construction did not prohibit appropriate inspection even though the wells would also require permitting. As stated in the NOV, the Petitioner sought a fine of $5,000 for the violations. Further, because the Petitioner's staff was first informed by the Respondent's representative that there were six wells completed on site when in fact there were nine, the NOV sought the imposition of a 20% penalty applied to the $5,000, and the suspension of Respondent's well drilling license. Subsequent to the issuance of the NOV, the Petitioner's staff met with Respondent's project manager to discuss the matter. At that time, it was determined that there actually were only six fully completed public water supply wells and three additional surface-cased but incomplete public water supply wells. The Petitioner dropped the proposed 20% penalty and suspension of Youngquist's license. However, subsequent to this discussion, the parties could not resolve the dispute and an Administrative Complaint was filed. 1/ Six individual well construction permits are required for the six completed public water supply wells located at the City of Fort Myers well field. The evidence establishes that the Respondent constructed and completed the six public water supply wells without obtaining the appropriate permits from the Petitioner. The failure to obtain the six permits constitutes six separate violations. The evidence establishes that, in completing the wells, the Respondent failed to notify the Petitioner 24 hours in advance of placement of grout in the annular spaces of the six completed wells. The failure to notify the Petitioner 24 hours in advance of placement of grout in the annular spaces of the six completed wells constitutes six separate violations. There is no evidence that, prior to initiation of the well construction activities and prior to the discovery of the violations by Petitioner's staff, the Respondent made any attempt to comply with the permitting requirements of the Petitioner.
Recommendation Based on the foregoing, it is hereby RECOMMENDED that the South Florida Water Management District enter a Final Order imposing an administrative fine of $4,500.00 against Tim Youngquist. DONE and RECOMMENDED this 14th day of January, 1992, in Tallahassee, Florida. WILLIAM F. QUATTLEBAUM Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 14th day of January, 1992.
