Findings Of Fact The Petitioner, Responsible Growth Management, Inc., is a not-for- profit corporation conceived and organized for the purpose of monitoring local governments within the geographic boundaries of Lee County for compliance with the requirements of the Florida Growth Management Act. Its members are residents of Lee County. Some of its members obtain their potable water from sources protected by Lee County Ordinance No. 89-30, as amended by Ordinance 90- 40 and 90-46, collectively referred to as the Wellfield Protection Ordinance (WPO). Other members obtain their potable water from sources the Petitioner contends are not protected by the WPO. The Petitioner contends that, for several reasons, the WPO is not consistent with the Lee County comprehensive plan. The Lee Plan Goal 41 of the Lee County comprehensive plan (the Lee Plan) provides in pertinent part: GOAL 41: GROUNDWATER. To protect the county's groundwater supplies from those activites having the potential for depleting or degrading those supplies. OBJECTIVE 41.1: WELLFIELD PROTECTION. By 1990 the county shall adopt a wellfield protection ordinance to provide regulations protecting the quality of water flowing into potable water wellfields. POLICY 41.1.1: The proposed wellfield protection ordinance shall be based on reliable technical data to ensure that adequate protection is provided. POLICY 41.1.2: The wellfield protection ordinance shall be amended whenever better technical data is developed and whenever additional potable wellfields are proposed. POLICY 41.1.3: The staff hydrogeologist shall review and comment on all development applications near public utility potable water wellfields, with particular attention to proposed land uses within a 10-year travel time from the well- heads. Goal 85 of the Lee Plan provides: GOAL 85: WATER QUALITY AND WASTEWATER. To ensure that water quality is maintained or improved for the protection of the environ- ment and people of Lee County. OBJECTIVE 85.1: Maintain high water quality, meeting or ex- ceeding state and federal water quality standards. POLICY 85.1.1: Sources of water pollution shall be identi- fied, controlled, and eliminated wherever feasible. POLICY 85.1.2: New development and additions to existing development shall not degrade surface and ground water quality. POLICY 85.1.3: The design, construction, and maintenance of artifical drainage systems shall provide for retention or detention areas and vegetated swale systems that minimize nutrient loading and pollution of freshwater and estuarine systems. POLICY 85.1.4: Developments which have the potential of lower- ing existing water quality below state and federal water quality standards shall provide standardized appropriate monitoring data. POLICY 85.1.5: New developments shall demonstrate compliance with all applicable federal, state, and local water quality standards. POLICY 85.1.6: No garbage or untreated sewage shall be dis- charged into coastal and interior surface waters. POLICY 85.1.7: The county shall initiate a wellfield protec- tion program to prevent the contamination of shallow wells by pollutant generating develop- ment including surface water runoff (see Goal 41). POLICY 85.1.8: Valid permits and inspection shall be required prior and subsequent to drilling operations for wells, elevator shafts, foundation holes, and test borings. POLICY 85.1.9: The county shall participate in a program to plug improperly constructed wells which are detrimental to ground water resources. Goal 87 of the Lee Plan provides in pertinent part: GOAL 87: WATER RESOURCES. To conserve, manage, protect, and improve the natural hydrologic system of Lee County to insure continued water resource availability. OBJECTIVE 87.1: WATER SUPPLIES. Insure water supplies of sufficient quantity and quality to meet the present and projected demands of all consumers and the environment, based on the capacity of the natural systems. POLICY 87.1.1: Natural water system features which are essen- tial for retention, detention, purification, runoff, recharge, and maintenence of stream flows and groundwater levels shall be iden- tified, protected, and managed. POLICY 87.1.2: The county shall recognize and encourage water and wastewater management, provided that such management does not exceed the natural assimi- lative capacity of the environment or appli- cable health standards. Appropriate water and wastewater management includes, but is not limited to, groundwater and aquifer recharge, spray or drip irrigation, gray-water systems, agricultural production, and other recycling techniques. POLICY 87.1.3: Freshwater resources shall be managed in order to maintain adequate freshwater supplies during dry periods and to conserve water. POLICY 87.1.4: Development designs shall provide for maintain- ing surface water flows, groundwater levels, and lake levels at or above existing conditions. POLICY 87.1.5: The county shall cooperate with the United States Geological Survey, South Florida Water Management District, and state agencies to develop an area-wide water resources plan emphasizing planning and management of water resources on the basis of drainage basins; and addressing the needs of the existing and potential built environment, natural hydro- logic system requirements, and freshwater flow impacts on estuarine systems. POLICY 87.1.6: The county shall continue to support a moni- toring program of existing baseline conditions of water resources. POLICY 87.1.7: The county shall cooperate fully with emer- gency water conservation measures of the South Florida Water Management District. The WPO Lee County Ordinance 89-30 provides for potable water wellfield protection. It establishes wellfield protection zones and sets out a protection zone map: showing the location on the ground of the outer limits of protection zones for present public utility potable water supply wells and wellfields which are permitted to pump 1,000,000 gallons of water per day or more. The Florida Cities-Waterway Estates Wellfield shall not be included within the protections established by this ordinance or depicted on the Protection Zone Maps. Chapter 10 of the ordinance is a "sunset provision" confirming that the ordinance was adopted "for the purpose of providing interim protection to existing potable water wellfields which are permitted to pump one million gallons of water or more per day" and explaining: The County is engaged in the creation of a Raw Water Management Authority to insure the protection of the public potable water supply. Potable water wellfields make up a portion of the available public potable water supply. In adopting this ordinace, the Board has taken the first step toward creating such an author- ity and providing an overall program for the protection of the public water supply. The wellfield protection ordinance is conceived as a part of that program. In order to insure that the wellfield protec- tion efforts of the County are incorporated into any overall program to protect the public potable water supply this ordinance shall expire and be of no further force and effect as to any acts occurring on or after September 1, 1991. The data and analysis supporting the Lee Plan clearly was based on the assumption of a 1 MGD threshhold. 5/ Section 4.05 of the Ordinance provides: Certain existing or proposed public and quasi-public land uses and activities may be declared exempt from the provisions of this Ordinance by the Board of County Commission- ers. This exemption shall be granted only upon a finding made by the Board in a public meeting that the existing or proposed land use or activity serves a public need which overrides the intent and purpose of this Ordinance and that it would be economically impractical or scientifically impossible for the land use or activity to comply with the requirements of this Ordinance or be relo- cated to an area outside of the protection zones established by this Ordinance. When declaring such an exemption, the Board of County Commissioners shall limit it to the extent necessary to enable the existing or proposed public or quasi-public land use or activity in question to be conducted within a protection zone while still serving the intent and prupose of this Ordinance to the extent which is economically practical and scientifi- cally possible. The Board may attach any con- ditions to the grant of any exemption that it deems appropriate. Section 3.01 of the Ordinance states: Four types of Protection Zone[s] have been established using scientific criteria relating to the physical characteristics of the water supply aquifer and the transport gradients caused by either natural forces or induced pumpage of the wellfields (see Appendix A)." The transport times associated with the Pro- tection Zones are designed so as to allow adequate time to carry out mitigating proce- dures to prevent wellfield contamination in the event of spillage of any Regulated Substance. Section 3.01.A. establishes and defines Protection Zone 1 as: "All land situated between the well(s) and the water table aquifer 6-month travel time zone demarcation." Section 3.01.B. establishes and defines Protection Zone 2 as: "All land situated between the well(s) and the planar geometric union of the largest of the following three travel time zones: Water table aquifer 1-year travel time zone demarcation. Lower Tamiami 1-year travel time zone demarcation. Sandstone 1-year travel time zone demarcation. Section 3.01.C. establishes and defines Protection Zone 3 as: "All land situated between the well(s) and the planar geometric union of the largest of the following three travel time zones: Water table 1-year travel time zone demar- cation and the water table aquifer 5-year travel time zone demarcation. Sandstone aquifer 1-year travel time zone demarcation and the Sandstone aquifer 5-year travel time zone demarcation. Lower Tamiami 1-year travel time zone demarcation and the Lower Tamiami 5-year travel time zone demarcation. Section 3.01.D. establishes and defines Protection Zone 4 as: "All land situated between the well(s) and the planar geometric union of the largest of the following three travel time zones: Water table 5-year travel time zone demar- cation and the water table 10-year travel time zone demarcation. Sandstone 5-year travel time zone demarca- tion and the Sandstone 10-year travel time zone demarcation. Lower Tamiami 5-year travel time zone demar- cation and the Lower Tamiami 10-year travel time zone demarcation. Section 3.02.B. of the Ordinance provides essentially that, where the location of property and buildings is within more than one protection zone, the most restrictive protective zone applies. Section 4.04 of the Ordinance prohibits liquid waste and solid waste disposal in Protection Zones 1, 2, and 3. In those zones, it also prohibits wastewater effluent disposal, except for public access reuse of reclaimed water and land application (under the conditions set forth and as defined in Chapter 17-610, Part III, F.A.C.). As for the exception, it provides: "Where public access reuse is permitted the chloride content shall be no greater than 500 mg/l." In Protection Zones 1 and 2, it also prohibits "the use handling, production, or storage of Regulated Substances [defined in Section 4.03 of the Ordinance] associated with land uses or activities regulated by this Ordinance in quantities greater than those set forth in Section 4.02.A." and "[e]arth mining within a five hundred foot (500') radius of an existing wellhead." The only prohibition in Protection Zone 4 is against "any activity regulated by this ordinance which stores, handles, uses, or produces any Regulated Substance, in quantities greater than those set forth in Section 4.02.A., which does not obtain a valid operation permit as set forth in Section 6.02." Thus, the Ordinance does not by its terms prohibit landfills, sludge disposal or rapid rate percolation ponds in Zone 4. Section 4.03 of the Ordinance, entitled "Regulated Hazardous or Toxic Substances," defines regulated substances in part in terms of federal and state regulations that are referenced, but not reproduced, in the ordinance. Section 4.02 of the Ordinance provides that it applies only to a particular land use or activity, whether that land use or activity is classified as a residential or commercial use, when either the aggregate sum of all quantities of any one Regulated Substance, or the aggregate sum of all Regulated Substances, on a given parcel or in a certain building exceeds one hundred and ten (110) gallons if the substance is liquid, or one thousand, one hundred and ten (1,110) pounds if said substance is solid. It also provides that the Ordinance applies to all storage facilities for petroleum products which are not regulated by Section 376.317, Florida Statutes, or Chapter 17-61, Florida Administrative Code. Section 4.04 of the Ordinance also provides that, within the protection zones: "Any stormwater or surface water discharge . . . shall conform to existing S.F.W.M.D. and F.D.E.R. rules or as they may be amended or replaced." Under Section 4.04 of the Ordinance, "partially treated sewage from residential septic tank systems" are not regulated in any of the protection zones. Section 4.05.B.5. of the Ordinance provides an: Exemption for Retail Sales Activities. Retail sales establishments that store and handle Regulated Substances for resale in their original unopened containers shall be exempt from the prohibition in Sub-Sections 4.04.A.1. and 2. provided that those estab- lishments obtain an Operating Permit pursuant to Section 6.02. No operating permit is re- quired in Protection Zones 3 and 4. Other Relevant Facts The WPO's Coverage. The support documentation in support of the Lee Plan was based on the assumption of a 1 MGD threshhold. The evidence as a whole does not suggest that was it contemplated at any time prior to adoption that the Lee Plan would require a wellfield protection ordinance that protects all potable water wellfields. 6/ Although the documentation in support of the Lee Plan focuses on wellfields permitted to pump 1 MGD or more and serves an indication that the Lee Plan does not require all potable wellfields to be covered by a protection ordinance, nothing in the Lee Plan or the supporting documentation establishes a clear intention to require the same protections for all wellfields permitted to pump 1 MGD or more. The focus of the WPO is on the protection of wellfields from contamination from the ground surface. Two wellfields permitted to pump more than 1 MGD are not covered by those protections. They pump from deep aquifers. The confining layers above those aquifers protect them from contamination from the ground surface. Other parts of the WPO, and other regulatory programs, require that abandoned wells that could possibly serve as a conduit for contamination into those aquifers be properly grouted so as to prevent contamination from the ground surface. As a result, they are adequately protected. 7/ The Florida Cities-Waterway Estates wellfield pumps from both the surficial aquifer and from a deeper aquifer known as the mid-Hawthorn. The confining layers above the mid-Hawthorn aquifer protect it from contamination from the ground surface. Other parts of the WPO, and other regulatory programs, require that abandoned wells that could possibly serve as a conduit for contamination into the mid-Hawthorn be properly grouted so as to prevent contamination from the ground surface. As for the wells pumping from the surficial aquifer, no party presented evidence on which findings of fact can be made on the issue whether it is fairly debatable to exclude the Florida Cities- Waterways wellfield from the WPO's protections against contamination from the ground surface. There was no evidence on which a finding can be made as to why they were excluded from the greater protections the WPO affords to other wellfields permitted to pump 1 MGD or more. 8/ The evidence was that 90% to 95% of Lee County's potable water supply is either covered by the WPO, with its 1 MGD threshhold and exclusion of the Florida Cities-Waterway Estates wellfield, or pumps from deep aquifers that do not need the WPO's protections from contamination from the ground surface. The Department of Environmental Regulation's so-called G regulations adopted in 1986 utilize a 100,000 gallon a day threshhold for coverage. This threshhold was selected to coincide with the jurisdiction of, and to extend coverage to all wells requiring a permit from, Florida's water management districts. The G-I regulations were successfully challenged and still are not in effect. The federal Environmental Protection Agency recently has criticized the G Although it is written in general terms to leave open the possibility of other similar applications, the evidence reflects that the primary purpose of the Section 4.05 exemption for "certain existing or proposed public and quasi- public land uses and activities" is to acknowledge and permit consideration to be given to the practical impact of possible future expansion of the regional airport located in Lee County. Since there are wellfields in the vicinity that possibly could be impacted by such an expansion, the exemption acknowledges that it might be more sensible, feasible, practical and economical to replace the wellfields than to move the regional airport. If this happens and, on a case- by-case basis, the County utililizes the exemption provision, it may be necessary to phase out the wellfields and to allow some degradation of parts of the wellfield, subject to close monitoring pending complete replacement of the wellfields. Alleged Inadequate Regulation of Pollution Sources. Rock and sand mine operations, which are prohibited within 500' of a wellhead, create open, water-filled holes in the ground. As the Petitioner correctly points out, mining operations can thereby create direct conduits that can lead contaminants to underlying aquifers. But there is evidence in the record to justify the WPO's treatment of rock and sand mines on several bases: first, these mines are regulated on a case-by-case basis through a permitting process; second, mines that have been permitted are relatively shallow and reach into, but do not penetrate, the layer confining the aquifers in the vicinity of the mines that are sources of potable water; third, the County has required as a condition of these permits that the pits be prohibited from serving as storm water retention ponds in the future so as to prevent contaminants from gaining entry to the potential conduit; and, finally, the evidence provides assurances that, even if contaminants somehow find their way into the pits, their concentrations would be low enough that sufficient "head" to penetrate the confining layers would not be generated. The WPO does not prohibit "zones of discharge." A "zone of discharge" is a deliberate decision on the part of a regulatory agency to utilize a limited part of the groundwater as part of the process of diluting contaminants. There was some expert testimony that, in a general and theoretical or academic sense, the concept of a "zone of discharge" is inconsistent with wellfield protection. They are not permitted in DER's G The WPO permits landfills, sludge disposal and rapid rate infiltration ponds in Protection Zone 4 (delineated by the ten-year travel time). The evidence was that landfills, at least, are subject to Department of Environmental Regulation (DER) and other regulation and permitting requirements that would provide adequate wellfield protection. There was no evidence or argument presented by any party to clarify how the other activities--sludge disposal and rapid rate infiltration ponds--are regulated. The Petitioner's evidence in general did not address the existence or absence of regulations (both County and other regulatory agencies) pertaining to the various activities of which it complains to rule out the possibility that they might meet the objectives and policies of the Lee Plan. The WPO does not contain its own stormwater regulations. Instead, it provides: "Any stormwater or surface water discharge . . . shall conform to existing S.F.W.M.D. and F.D.E.R. rules or as they may be amended or replaced." The Petitioner offered, as evidence in support of its position that the DER and SFWMD stormwater regulations are inadequate, expert testimony to the effect that the DER and SFWMD regulations are "performance standards," not "directed to groundwater monitoring, and it's not quality impact related." A "performance standard" requires certain things to be done with stormwater in the expectation that groundwater contamination would be eliminated or minimized. The Petitioner's witnesses related that DER decided that "protection of public water supply has to be protected to above and beyond a performance standard" and opted for specific water quality criteria in its G-I groundwater. But nothing in the Lee Plan requires utilization of the G-I rule approach, and the Petitioner's expert did not opine that failure to do so would render the WPO inconsistent with the Lee Plan. The Section 4.05.B.5 retail sales exemption presents a risk of contamination of a wellfield, but the risk is low. In all likelihood, it would take a fire or some other similar catastrophe for the possibility of actual harm to a wellfield to materialize from the small risk involved. Other County Measures Relevant to the WPO. The County has several programs, other than the WPO, and in addition to the Raw Water Management Authority mentioned in the WPO, 9/ that impact wellfield protection. It has a program to encourage (and in some cases require) the reduction and elimination of the use of septic tanks and package sewage plants. It is building a new sewer district. It has taken over the from DER the function of inspecting the installation of underground storage tanks and the remediation (clean up and repair) of tanks storing liquid petroleum products in an attempt to do the job better. There also was evidence that the County has restricted density in potential future wellfield locations and their recharge areas to one unit per ten acres. (The Petitioner's own witness testified that, other than an outright ban on septic tanks, density reduction is the only way to address the problem of septic tanks.
The Issue Whether the Petitioner is entitled to the issuance of a water vending machine permit for a machine located at Herman's Meat Market, Nokomis, Florida, under the provisions of Section 381.295, Florida Statutes.
Findings Of Fact A water vending machine located at Herman's Meat Market, 227 West Albee Road, Nokomis, Florida, operating from a non-community water supply came to the attention of the Department's water vending machine permitting personnel in Tallahassee on March 9, 1987. At that time, Frank Dowdney, on behalf of Bottled Water Vending of Florida, had made application for issuance of a water vending machine permit at that location. Upon request of the Department in June, 1987, Mr. Dowdney had the well water tested to determine whether the water met community public water supply system standards as required in Chapter 10D-22.004(5) Florida Administrative Code. The water failed to meet the minimum standards as determined by the lab report dated July 22, 1987 of Thornton Laboratories Inc. There were four areas of deficiency, specifically, turbidity, radionuclides, iron, and total dissolved solids (T.D.S.). Mr. Dowdney did not provide any additional test results to the Department and did not receive a permit from the Department for this location. Subsequent to Mr. Dowdney's death in the fall of 1987, the water vending machine location at Herman's Meats was operated by Glacier Water Vending. In the summer of 1988, an agent of Glacier Water had notified departmental permitting personnel that the machine at this location was not in operation. Glacier Water Vending never requested a permit for this location. On September 7, 1988, Mr. McKinney, President of the Petitioner Clean Water Systems, Inc., became the operator of a new water vending machine at the Herman's Meats Location. Mr. McKinney submitted an application for a permit on September 6, 1988, which was denied on November 3, 1988. The reason for denial was that the water source at Herman's Meats had not been shown to be in compliance with community public water system standards. Neither Mr. McKinney nor Clean Water Systems, Inc., though aware of the predecessor operators at this location, had any ownership interest and had not been an employee of either Bottled Water Vending of Florida or Glacier Water Vending. A reverse osmosis system which had been installed on the source line from the well to the water vending machine subsequent to the 1987 testing was removed by Robert Miller of Glacier Water Vending. Mr. McKinney installed a new reverse osmosis system on the source line on September 7, 1988. The source water for a vending machine is the water just prior to entering the machine, which includes the well and any treatment processes between the well and the machine. The source water for Petitioner's vending machine has been processed through chlorination and one reverse osmosis system. This source water must meet minimum standards established for community public water supply systems. There are many different types of reverse osmosis systems. In general, a reverse osmosis system is a purification process intended to improve water quality. The degree of improvement in product water is affected by many factors including, but not limited to, feed water mineral concentration, feed pressure, feed water temperatures and Ph. It cannot be assumed that minimum water quality standards are being met just because a reverse osmosis system has been installed. The Department has no obligation to provide and/or pay for the chemical testing that is a prerequisite to the issuance of this water vending machine permit. Department personnel do perform required bacteriological and nitrate testing on the non-community well at Herman's Meats. There has been a pattern of noncompliance for bacteriological and chlorine residual levels at this location. The Department does not perform water vending machine testing at Herman's Meats and would only do so if there was a complaint. At the time of the hearing, there had been no complaints about the vended water there. The Petitioner has provided no test results from a state certified lab to the Department. The Petitioner has provided to the Department only test results from his own testing efforts which relate only to the total dissolved solids (T.D.S.) category. The test results generated by Mr. McKinney are not adequate for departmental permitting purposes. The only state certified chemical test results available to the Department on this location show that the source water did not meet minimum standards for community public water supply systems in 1987.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that Petitioner's application for a water vending machine permit be DENIED. DONE AND ENTERED this 3rd day of October, 1989, in Tallahassee, Leon County, Florida. DANIEL M. KILBRIDE Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 3rd day of October, 1989. APPENDIX TO RECOMMENDED ORDER, CASE NO. 89-0668 The following constitutes my specific rulings, in accordance with section 120.59, Florida Statutes, on findings of fact submitted by the parties. Respondent's Findings of Fact Accepted-paragraphs 1-11. Rejected-paragraph 11 is covered in the Preliminary Statement Petitioner's Findings of Fact Accepted-paragraph 7 (in substance) Rejected-paragraph 1 - irrelevant paragraph 2 - against the weight of the evidence or subordinate paragraph 3 - insufficient proof (first subparagraph); uncorroborated hearsay (second subparagraph); subordinate (third, fourth and fifth subparagraphs) paragraph 4 - argumentative and uncorroborated 5,8 (sic) hearsay and 10 paragraph 6 - insufficient proof COPIES FURNISHED: Eugenie G. Rehak, Esquire Health Program Attorney Department of Health and Rehabilitative Services 12381 South Cleveland Avenue Suite 501 Fort Myers, Florida 33907 Lew McKinney, President Clean Water Systems, Inc. 250 Warfield Avenue Venice, Florida 34292 Sam Power Clerk Department of Health and Rehabilitative Services 1323 Winewood Boulevard Tallahassee, Florida 32399-0700 Gregory L. Coler Secretary Department of Health and Rehabilitative Services 1323 Winewood Boulevard Tallahassee, Florida 32399-0700 John Miller General Counsel Department of Health and Rehabilitative Services 1323 Winewood Boulevard Tallahassee, Florida 32399-0700
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 Upon consideration of the oral and documentary evidence adduced at the hearing; the following facts relevant to the issue presented for determination are found: The prime complaint heard from petitioner's customers who testified at the hearing was the objectionable odor of the water received in their homes. The water was described as smelling like chlorine or like sewer, swamp or sulphur water. Such an objectionable odor affects the water's taste, and several customers testified that they were compelled to use filters to make the water bearable to drink. Another witness testified that the water tasted like quinine. Other complaints regarding the quality of water provided by petitioner to its customers included the presence of debris, such as sand, silt or dirt, in the water, the staining of white sinks by the water and inadequate water pressure. Complaints with regard to the service provided by petitioner to its customers were also voiced. These complaints included interruptions in water service without prior notice, the presence of air in the water lines and the necessity of making long-distance telephone calls to Orlando when inquiring about their bills. One customer testified that even though he had paid for a temporary disconnection of his water when he was away from his residence, he was still billed a minimum charge for service. Several customers testified that petitioner's office personnel failed to timely or adequately respond to their complaints or inquiries regarding their bills. Charles Sweat, the vice president of operations for petitioner's fifty- one systems in eight counties, visits each of the systems at least once a month. At the time that petitioner took over the operation of the Intercession City water system in 1977, the system was under citation by the Department of Environmental Regulation for inadequate chlorination of the water. The Department of Environmental Regulation does have a minimum requirement as to the amount of chlorine which must be added to the water. Petitioner corrected this deficiency and the citation was removed. Neither of the two water systems involved in this proceeding - Intercession City and Tropical Park - are presently under citation by any state or local regulatory agency. Analyses of monthly laboratory samples of water from the Intercession City and the Tropical Park systems indicate that the water quality will meet the Department of Environmental Regulation's secondary drinking water standards which went into effect on January 13, 1981. Petitioner now provides a toll-free telephone number which Osceola County customers may use to call Orlando. Notice of this toll-free number was included in the water bills sent to customers in September or October of 1980. A log is maintained by petitioner of all interruptions of water service. On one occasion occurring on March 3, 1980, there was a water outage. The outage was caused by low temperatures freezing the pressure switch at a time when it was at a high pressure level. When there was no pressure, the switch, being frozen, was incapable of sending an on-signal to the pump. It was necessary for petitioner to use torches to thaw out the pipes to make the system work properly. Cold weather sufficient to cause such an effect rarely occurs in Florida. On January 16, 1981, there was an interruption in service caused by the county cutting a water line. Another interruption of service occurred on January 18, 1981. This was caused by the malfunction of an air release valve which releases excess air from the pressure tank. Air was eventually caused to go into the distribution system and consequently into the homes of the customers. Petitioner's personnel have been instructed to watch this type of situation more carefully and more often. Petitioner's vice president of operations was not aware of recent complaints from customers concerning air problems, but testified that he would immediately and personally follow up on the problem.
Recommendation Based upon the findings of fact and conclusions of law recited herein, it is RECOMMENDED that the quality of water service provided by petitioner to its customers in Osceola County be found to be satisfactory and that no adverse consequences be imposed upon the petitioner in its application for a rate increase as a result of the quality of its service. Respectfully submitted and entered this 22nd day of April, 1981, in Tallahassee, Florida. DIANE D. TREMOR, Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 22nd day of April, 1981. COPIES FURNISHED: R.M.C. Rose Myers, Kaplan, Levinson, Kenin and Richards Suite 103, 1020 Lafayette Street Tallahassee, Florida 32301 Jack Shreve Public Counsel Room 4 - Holland Building Tallahassee, Florida 32301 M. Robert Christ Legal Department Florida Public Service Commission 101 East Gaines Street Tallahassee, Florida 32301 Steve Tribble, Clerk Public Service Commission 101 East Gaines Street Tallahassee, Florida 32301
Findings Of Fact The parties stipulated, and it is so found, that Petitioner, DER, has jurisdiction over both the issues and the Respondents Dey and KWC. KWC owns and operates a water system which supplies water to both residential and commercial customers in the City of Keystone Heights, Florida. Virginia Key is the President of KWC, a member of the Board of Directors of the corporation, and one of the five stockholders. The other stockholders are her sisters. The five sisters are the daughters of the late G. E Wiggins, and inherited the company from him at his death in 1969. Mr. Wiggins developed the water company in the 1920's and operated it until his death. KWC came under the jurisdiction of the Florida Public Service Commission (PSC) just prior to Mr. Wiggins' death. At that time, pursuant to a PSC requirement, it was assessed and valued at a sum in excess of $250,000.00 by a consultant firm hired for the purpose. As of late November, 1984, KWC served approximately 752 residential customers which, when multiplied by an average 2.5 persons per family factor, results in a total of approximately 1,880 residential inhabitants served by the water system. In addition, the system serves 105 commercial customers. It is impossible to estimate with any reasonable degree of accuracy the number of individuals involved in the commercial service. The system consists of three wells drilled in 1940, 1946, and 1960 to a depth of 350, 450, and 492 feet respectively. Total yield from the three wells is normally 1,350 gallons per minute. The wells are generally well protected against surface water infusion, are normally not subject to inundation, and have had no salt water infiltration problems in the past. At the present time, well number 2, drilled in 1946, with a 350 gpm yield is out of service. The water, when pumped from the ground, is stored in two tanks-one with a 60,000 gallon capacity and the other with a capacity of 800 gallons. Both tanks are steel. Chlorine is added to the water in each storage situation by a hyper-chlori- nation system before the water is sent to the storage tank. The distribution system is made up of 6" and 2" diameter pipe. In March, 1984, two different inspections of the water system, done by, in one case, an environmental specialist and in the other, an Engineer I with DER, revealed several deficiencies in the maintenance and operation of the system all of which constitute violations of DER rules. Specifically, these include (1) failure to provide an auxiliary power source in the event the main pumping capability of the system is lost, (Rule 17-22.106 (3)(a); (2) failure to utilize for the system an operator certi- fied by the state with a Class C license, (Rule 17-22.107(3)(b); (3) failure to maintain a free chlorine residual in the water of at least 0.2 ppm in the system, (Rule 17-22.106(3)(c); (4) failure to maintain a minimum pressure of 20 ppi in the distribution system, (Rule 17-22.106(3)(f); (5) failure to have a gas chlorination facility, (Rule 17-22.106(3)(d); and (6) failure to obtain proper permits to expand the distribution system, (Rule 17-22.108 (1)(b) Rule 17-22, F.A.C., sets up requirements for safe drinking water and was designed to establish guidelines and standards for facilities and water and to bring water into compliance with the Federal Act. Twenty ppi of pressure in the system was adopted as a standard minimum for residual pressure to protect against outside contaminants getting into the water system. Such contaminants could come from ground water, leaks, and water in storage tanks attached to the system such as toilet tanks, being aspirated into the system. Also a certain amount of pressure is required to operate appliances. Normally minimum pressure is found in areas at the edge of the system and in those areas where inadequate chlorination is located. They interact and both pressure and chlorinization are required. Chlorine can be injected into the system generally in two ways: the first is through gas chlori- nation and the second, through hyper-chlorinization as is used in the instant system. The effectiveness of hyper-chlorinization is limited, however, by the size of the system. Basically, hyper- chlorinization is effective when the demand in the system for pressure is no more than 10 ppi. Above this, gas chlorinization is necessary. As late as January 4, 1985, Mr. Dykes went to Keystone Heights to test the system. His tests showed that 11.9 ppi is the average daily flow per 24 hours for the last 12 months. Since this figure is above 10 ppi, in his opinion, a gas chlorinization system would be needed. Chlorine is used to purify water because it has been shown, through long use, to prevent disease. The requirement for a residual chlorine level in water, therefore, is consistent with that concept to insure chlorine is always in the water in sufficient quantity to prevent disease. Respondent's plant has less than the 0.2 residual that is required under the rule. This insufficiency is caused by the inadequate chlorinization system which has insufficient capacity to provide the appropriate amount of chlorine. At the current level, it is providing only approximately 60 percent of the needed chlorine. To correct this deficiency Mr. Dykes recommends installation of a gas chlorinization system. In addition, the pneumatic tank storing the water from the number 3 well does not give sufficient detention time to allow for appropriate reaction of the chlorine contained in the water before the water is released into the distribution system. Another factor relating to the lack of adequate pressure in the system is the fact that, in Mr. Dykes' opinion, too much of the system is made up of 2" diameter water line. A line of this small diameter prevents the maintenance of adequate pressure especially in light of the fact that there are numerous old lines in the system some with corrosion and scale in them which tends to reduce pressure. This latter factor would be prevalent even in the 6" lines. The current plant manager, Mr. Cross, who has been with Respondent for approximately 4 years is, with the exception of one part time employee, the only operations individual associated with the plant. As such, he repairs the meters and the lines, checks the pumps, the chlorinator, and checks and refills the chlorine reservoir on a seven day a week basis. Be learned the operation of the plant from his precedessor, Mr. Johnson, an unlicensed operator who was with the company for 10 years. Mr. Cross has a "D" license which he secured last year after being notified by DER that a license was required. It was necessary for him to get the "D" license before getting the required "C" license. At the present time, he is enrolled to take courses leading toward the "C" license. At the present time, however, he is not, nor is anyone else associated with KWC, holding a license as required. The rule regarding auxiliary power provides that all community systems serving 350 or more persons shall have standby pumping capability or auxiliary power to allow operation of the water treatment unit and pumping capability of approximately one-half the maximum daily system demand. Respondent has admitted that the system is not equipped with an auxiliary power source and it has already been established that more than 350 persons are served by the system. Respondent also admits that subsequent to November 9, 1977, it constructed main water lines for the system which required the obtaining of a permit from either the Petitioner or the county health unit. Respondent admits that it did not obtain or possess a permit to do the additional construction referenced above from either DER or the Clay County Health Department prior to the construction of the water lines referenced. The inspections referenced above, which identified the problems discussed herein, were accomplished by employees of Petitioner, DER, at a stipulated cost of $898.10. Respondent contends, and there is no evidence to the contrary, that there have been no complaints of contaminated water and that the monthly water samples which Mr. Cross forwards to the Clay County Health Department have been satisfactory. Mr. Cross also indicates that a September, 1983 DER analysis of water samples taken from the system was satisfactory. However, bacteriological analysis reports on water collected from Respondent's system on July 11 and 27, 1983, reflect unsatisfactory levels of either coliform or non-coliform bacteria in the water requiring resubmission of test samples. Respondent also contends that no one has ever gotten sick or died from the water furnished by the system and there is, in fact, no evidence to show this is not true. Even though so far as is known, no one has ever been made sick from the water in the system, in Mr. Dykes' opinion, the risk is there. As a result of the defects identified in this system, insufficient chlorine is going into the system to meet reasonable health standards. Though this does not mean that the water is now bad, it does mean that at any time, given a leak or the infusion of some contaminant, the water could become bad quickly, and the standard established by rule is preventive, designed to insure that even in the case of contamination, the water will remain safe and potable. Respondent does not deny that it is and has been in violation of the rules as set out by the Petitioner. It claims, however, that it does not have sufficient funds available to comply with the rules as promulgated by DER. Respondent has recently filed a request for variance under Section 403.854, Florida Statutes, setting forth as the basis for its request that it does not have the present financial ability to comply with any of the suggested or recommended corrective actions to bring its operation into compliance with the rules. Mr. Protheroe, the consulting engineer who testified for Respondent has not evaluated the system personally. His familiarity with it is a result of his perusal of the records of the company and the Petitioner. Based on his limited familiarity with the system, he cannot say with any certainty if it can be brought into compliance with, for example, the 20 ppi requirement. There are too many unknowns. If, however, the central system was found to be in, reasonably good shape, in his opinion, it would take in excess of $100,000.00 to bring it within pressure standards. To do so would require replacement of the 2" lines, looping the lines, and cleaning and replacing some central system lines as well. In his opinion, it would take three months to do a complete and competent analysis of the system's repair needs. Once that was done, he feels it would take an additional three months to bring the plant into compliance with DER requirements. Other repairs, such as those to the lines outside the plant, would take longer because some are located in the downtown area and have interfaced with other utilities. This could take from three to four months if the money were available to start immediately. Here, however, it has been shown that it is not. Consequently, to do the study and then, if possible, procure the funds required, could take well in excess of six months or so. Mr. Protheroe contends, and there is little if any evidence to indicate to the contrary, that to replace the current system with a new one entirely as it is currently constituted would cost at least $250,000.00. However, in his opinion, no one would ever put in a new system similar to the one currently there. He cannot say how much it would cost to buy the system and make the necessary corrections to it to rectify the deficiencies. His familiarity with the system is not sufficiently complete to do this. He cannot say exactly how much the system is worth in its current state, but he is satisfied that it is worth more than $65,000.00. In that regard, Mrs. Dey indicated that in her opinion, the fair market value of the system is currently at $250,000.00. At the present time, there are current outstanding loans in excess of $9,000.00 at 16 percent interest. This current loan basis has been reduced from a higher figure. In 1977, the company borrowed $15,000.00 at 9 percent. In 1981, it borrowed $5,000.00 more at 18 percent. In 1982, the loans were consolidated at an increased rate of 16 percent and the officers have been advised by their current creditors that they cannot borrow any more money for the system in its current state. They would sell the system if a reasonable price could be realized. However, any inquiries on prospective purchases have been chilled by a low rate base assigned by the PSC. In that regard, the City of Keystone Heights offered to purchase the system for $59,000.00. This offer was declined as being unreasonable. Nonetheless, in light of the low rate base assigned by the PSC in its order issued on December 21, 1981 of slightly over $53,000.00 the offer by the city of $59,000.00 is not completely out of line. A certified public accountant, in KWC's December 31, 1983 financial report assigned a valuation of approximately $62,000.00, again a figure only slightly higher than that offered by the city, but substantially less than the $175,000.00 price asked of the city by Respondent Dey and her sisters. Mrs. Dey indicated that to the best of her knowledge the PSC denied rate increases for the purposes of improvements. In the presentation before the commission, respondents relied exclusively on the services of their attorney and accountant. Evidence from Mr. Lowe, of the PSC, however, indicates that KWC has never requested a rate increase to finance any of the improvements called for here. In the PSC order referred to above, Respondent was awarded a 12.25 percent rate of return on its rate base. This figure was an amalgam of a more than 13 percent rate on equity and a lesser figure for cost of doing business, including debt. At the time of that hearing, however, the debt cost was based on a 9 percent interest figure. The 16 percent interest figure came afterwards and no hearing has been requested based on the higher interest rate and it is so found.
Recommendation Based on the foregoing findings of fact and conclusion of law, it is, therefore: RECOMMENDED that Respondents Virginia W. Day and the Keystone Water Company be ordered to comply with the Orders for Corrective Action previously filed herein to bring the water system in question in compliance with the Florida Safe Water Drinking Act without delay or suffer the penalties for non- compliance called for by statute and, in addition, pay costs of investigation in the amount of $898.16. RECOMMENDED in Tallahassee, Florida this 19th day of February, 1985. ARNOLD H. POLLOCK Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 19th day of February, 1987. COPIES FURNISHED: Debra A. Swim, Esquire Assistant General Counsel Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32301 John E Norris, Esquire 10 North Columbia Street Lake City, Florida 32055 Victoria Tschinkel, Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301
The Issue The issue for consideration at the hearing was whether the Respondent, Roger Harloff, should be issued a consumptive use permit to withdraw and use ground water from the wells on his property, and if so, in what amount and under what conditions.
Findings Of Fact Respondent, Roger Harloff, owns several farms in southeastern Manatee County, Florida which, taken together, make up an irregular 8,500 acre tract located approximately 2 1/2 miles north of the City of Sarasota's Verna Wellfield. Mr. Harloff grows vegetables on much of this tract, of which approximately 1,500 acres is devoted to tomatoes. This tomato crop is the prime crop produced by Mr. Harloff, and provides the raw material for the Harloff packing plant which is dependent upon the tomato crop in order to stay in business. Mr. Harloff also operates a plant nursery at which he produces many if not most of the seedling plants utilized in his vegetable growing operations. In order to be economically feasible and remain operative, Mr. Harloff must farm approximately 3,800 acres during the Spring growing season and approximately 3,000 acres during the Fall. These acres are made up of tomatoes and other vegetables. The packing plant and the plant nursery are dependent upon the farm operation and without adequate water, the farm operation cannot be successfully carried on. In September 1988, Mr. Harloff applied to the District for a consumptive use permit to withdraw water from twelve wells located on his property, requesting an annual average rate of 12,995,606 gpd, and a maximum daily rate of 47,520,000 gpd. The consumptive use permit application filed by Mr. Harloff was assigned District Number 204467.04. After evaluation of the application in conjunction with its needs and policies, the District issued a staff report and proposed agency action on the application which recommended issuance of the permit authorizing water to be drawn from the 12 wells at a rate approximating that requested in the application. Thereafter, the City of Sarasota, which operates the nearby Verna Wellfield, considering that the proposed withdrawal would have a substantial adverse impact on its wellfield operations, filed a Petition for Formal Administrative Hearing objecting to the issuance of the permit to Mr. Harloff. Though Mr. Harloff has owned much of the property which make up the 8,500 acre tract in question here, at the time of his application, he did not own, but had under contract, a substantial portion. He closed on the purchase of that remainder after he received notice of the District's intention to issue the permit in question but prior to the City's filing its Petition For Formal Hearing. The purchase price of the property in question was $9,000,000.00 which carries an interest payment on the financed portion of $52,000.00 per month. The wells pertinent to the issues in this proceeding are as follows: # Cons. Depth Cas. Lin. Diam. Cap. Loc. 1 1978 1185' 200' 220-490' 12" 2000 gpm SE 2. 1988 1320' 210' 210-480' 16" 3000 gpm SE 9. 1974 1130' 390' 16" 3000 gpm C 10. 1976 1232' 231' 283-400' 16" 3000 gpm NW 11. 1979 1120' 210' 260-480' 12" 2000 gpm NW 12. 1976 1180' 480' 12" 2000 gpm SW 3. 1989 1434' 460' 16" 3000 gpm SE 5. 1989 1374' 610' 16" 3000 gpm W 8. 1989 1292' 548' 16" 3000 gpm NW 13. 1989 1310' 635' 16" 2000 gpm NE Well No. 8 was used as the pump test well for the constant rate discharge test and Well No. 13 was the deep observation well for that test. Wells 1, 2, 9, 10, 11, and 12 have all been previously permitted by the District and No's 1, 2, 9 and 10 are currently permitted under two other permits, while 11 and 12 were permitted under a different permit. Wells No. 3, 5, 8 and 13 have been authorized for construction but not, as yet, to produce water. Wells 4, 6 and 7 have not yet been constructed. The intention is to drill them to a depth of 1,300 feet and case them to 600 feet. Each will have a pump capacity of 3,000 gpm. Number 4 will be in the southeast portion of the tract, number 6 in the central portion, and number 7 will be located just north of number 6. Wells 1, 2, 9, and 10 currently have a combined permitted maximum daily rate of 13,680,000 gallons under permits number 204467.03 for 1 and 2, and 204630 for 9 and 10. The former was issued on December 29, 1987 and will expire on December 29, 1993, and the latter, issued on October 7, 1981, will expire on that same day in 1991. The permit previously issued for wells 11 and 12 authorized withdrawal at a maximum daily rate of 2,160,000 gallons. That permit, number 204374, expired on September 9, 1986 and was not renewed. After the City filed its Petition challenging Mr. Harloff's proposed permit, Mr. Harloff, on June 26, 1989, filed an amended application to withdraw water at an average annual rate of 10.99 mgd and a maximum daily rate of 48.96 million gallons. This amended application refers to an additional proposed well, Number 13. The District, however, had previously approved wells 3 - 8 and 13, and pursuant to this authorization, wells 3, 5, 8, and 13 were built. Mr. Harloff submitted additional amendments to his application on August 7 and 9, 1989. The former requests a seasonal average daily rate of 25.34 mgd and a seasonal maximum daily rate of 32.79 mgd. The latter requests a seasonal average rate of 26.18 mgd, an annual average rate of 15.18 mgd, and a seasonal maximum rate of 31.56 mgd. In that regard, a seasonal rate is the same as an annual rate, (average or maximum) when applied to a growing season as opposed to a year. The additional amendments to the application were evaluated by District staff who, on August 18, 1989, issued a revised staff report and a proposal to issue to Mr. Harloff a consumptive use permit authorizing an average annual withdrawal of 11.1. mgd, an average seasonal withdrawal of 15.6 mgd, and a seasonal maximum withdrawal of 20.1 mgd. The proposed permit also contains terms and conditions which, the District contends, will, inter alia, permit Mr. Harloff to withdraw more water than he is currently authorized without additional adverse impact on the City's Verna Wellfield. It is to some of these terms and conditions that Mr. Harloff objects. Since the issuance of the revised staff report and intent to issue, the parties have negotiated on the various terms and conditions in question and have agreed to some and the amendment of others. Mr. Harloff has no objection to conditions number 1, 2, 3, 7 - 14, 23, 24, 26, 28 - 30, 32, and 34 & 35. The parties agree that other conditions, as indicated herein, should be amended as follows: Condition 19, on the third line, should be changed to read, " up to 20 inches tapering to 12 inches." Condition 22, on the second line, should be changed from "30 days" to "10 days". Condition 25, on the first line, should be changed from "within 60 days" to within 120 days". Condition 31, on the third line, starting with "following month" should be changed to "following months: January, April, July and October". Also, under Sampling Frequency, "Monthly" should be changed to "Quarterly". Condition 33, on the ninth line, insert the work "economically" before the word "feasible" in the phrase "specific operation and irrigation improvements are feasible". Mr. Harloff objects to conditions 4, 5, 15 - 17, 20 & 27. He does not object to the proposed new standards for new wells. Taken together, the parties then disagree only on the requirement for abandonment or refurbishment of existing wells and the quantities of water Mr. Harloff will be allowed to draw. The City supports the District's position on both issues. The City of Sarasota owns and operates a public water system to serve between 50 to 75 thousand people located in Sarasota County. The primary source of water for this system is the Verna Well field which is also owned by the City and which accounts for approximately 60 percent of the City's water needs. The City also operates a reverse osmosis, (R.O.) water desalinization facility, and has back-up wells at St. Armond Key and at the Bobby Jones Wellfield. The Verna Wellfield is located about 17 miles east of the Sarasota city limits on approximately 2,000 acres of land in northeastern Sarasota County. It consists of two tracts of land: Part "A", which is approximately 1/2 mile wide by 4 miles long; and Part "B", which is approximately 1 mile square located about 500 feet southeast of Part "A". The Verna Wellfield's permitted allocation is based on whether the R.O. facility is producing at capacity. If it is, the Verna daily allocation is 7 mgd, and if not, 9.5 mgd. The R.O. facility's capacity is 4.5 mgd and the backup wells have a capacity of 1.7 mgd. The wellfield contains 39 permitted production wells, 30 of which are in Part "A" and 9 of which are in Part "B." One of them, well 30, is currently inactive. The wellfield has been in operation as a part of the City's public water system since September 1966. When the Verna Wellfield was constructed in 1965-1966, its original design specified casing on most wells down to 140 feet with pump bowl settings at 125 feet. Each pump was to have a total dynamic head, (TDH) of 200 feet. Over the years, the City has decreased the TDH of the pumps at Verna from 200 feet to 175 feet. This has resulted in a reduction of the pumps' ability to produce water with sufficient pressure to carry it to the discharge point. This decline has been caused by an increase in withdrawal of water regionally, and not solely because of withdrawals from the Verna Well field. Verna is impacted by the use of water outside the boundaries of the wellfield. The City has an ongoing program calling for the refurbishment of 2 to 3 wells per year at the Verna Wellfield. It is the City's intent to convert the pumps to 200 feet TDH on all well refurbishments in the future. In August 1977, a program requiring permits for the consumptive use of water was implemented in both Sarasota and Manatee Counties. At that time, the Verna Wellfield had a production rate of 6.9 mgd annual average daily rate. On January 6, 1978, the City applied for a permit for Verna and on April 3, 1979, the District issued permit number 27804318 to allow the City to draw water from the Verna Wellfield. The City applied for a renewal of that permit in October 1983 and thereafter, in January 1985, the District authorized the continued withdrawal of water from Verna by the issuance of permit 204318 which, at Condition 18, placed limitations on the City's use of water from the wellfield. Specifically, the permit limited withdrawals from Verna to: ...6,000,000 gallons per day average and 7,000,000 gallons per day maximum, except during those times when ... [the R.O. process is reduced or to facilitate maintenance or repairs]. At such times, ... [withdrawals) may be increased to provide additional supplies not to exceed 8,000,000 gallons per day average annual and 9,500,000 gallons per day maximum. This condition clearly provides for additional supplies to be drawn to increase the Verna Well field production to a total of 8,000,000 and 9,500,000 mgd, respectively, not in addition to the regular permitted amount, by those quantities. The City's permit has been neither suspended nor revoked nor is any violation enforcement action currently under way. The current permit expires January 9, 1991. The water pumped from the Verna wells is held in a 1,000,000 gallon reservoir at the wellfield. This reservoir, which is topped at approximately 22 to 23 feet, electronically controls the pumping activity at the well field by turning on and shutting off pumps, in series, as the water level in the reservoir rises and falls. The water, when needed, is transmitted to another reservoir near the City's treatment plant in downtown Sarasota by gravity flow through a 30" diameter, 92,000 foot long pipe. The flow rate is approximately 5,000 gpm normally. When the treatment plant needs more water, a pump at the well field forces the flow at a rate of between 7,200 to 8,200 gpm, depending upon the level of water in the receiving reservoir. A flow of 8,200 gpm would draw 11.8 mgd from the wellfield. The operating capacity of the Verna Wellfield, in August 1988, was 17.9 mgd. Harloff's experts assert, and there is no concrete evidence to rebut it, that if all wells at Verna were pumping during a 24 hour period in May 1989, the reservoir could have been maintained at full level. However, though there is a manual override of the automatic reservoir/pump control system, it is unrealistic and unwise to expect full production on a 24 hour basis for any lengthy time period. Water under both Mr. Harloff's property and the Verna Well field is found at various levels known by different names. These include, in order of descent, the Surficial Aquifer, the Intermediate Aquifer, the Upper Floridan Aquifer, and the Lower Floridan Aquifer. The Surficial Aquifer extends from the surface down to between 20 and 60 feet below the surface. A 20 foot thick bed of clay separates the water in this aquifer from that in the aquifer immediately below it, the Intermediate Aquifer, which extends from approximately 80 feet down to approximately 420 feet below the surface. In the lower part of the Intermediate Aquifer, permeability decreases until a confining unit separating the bottom of the Intermediate Aquifer from the top of the Upper Floridan Aquifer is formed. There is such a confining unit between 420 and 500 feet. There is no well-defined confining unit between the Upper and Lower Floridan Aquifers. There is, however, a substantial difference in the transmissivity in each zone. "Transmissivity" is defined as the amount of water that will exist through a section of the aquifer that is the same width from the top to the bottom. The lower the transmissivity rate, the deeper the cone and the narrower the radius of effect. The higher the rate, the shallower the cone and the broader the radius. The Lower Floridan Aquifer has an extremely high transmissivity. Its top is found at a range of from 1,050 to 1,200 feet below the surface on Mr. Harloff's property. The water from the Upper Floridan Aquifer is of higher quality than that in the Lower. It is more readily usable for drinking than that in the Lower, but the Lower water is quite acceptable for agricultural purposes. What confining layer exists between the Upper and Lower Floridan Aquifers is made up of relatively impermeable anhydrides and gypsum. Because of this, there is little likelihood of the highly mineralized water from the Lower Floridan Aquifer rising into the better quality water in the Upper. If, therefore, water for agricultural purposes is drawn from the Lower Floridan Aquifer, with its high transmissivity and narrower cone radius, and if the wells utilized to procure this water are cased down to within the Lower aquifer, there is little chance of a negative impact on the better quality water, used for drinking by the City, within the Upper Floridan and Intermediate Aquifers. Mr. Hardin, an expert geologist and hydrogeologist testifying for Mr. Harloff, concluded, utilizing certain commonly accepted computer models, that Mr. Harloff's requested additional withdrawals would not have a significant effect on the Verna Wellfield's ability to produce water sufficient for the City's needs. This conclusion was based on 1989 seasonal use figures including an average rate of 21.95 mgd, a maximum rate of 27.04 mgd, and a maximum rate of 29 mgd under a "run time" calculation and the fact that during that period, the City was able to pump at least its permitted quantity from its wells at Verna. The City and the District do not accept this conclusion as reasonable, however, because, they claim, the withdrawal figures cited are not meter readouts but estimates based on the number of acres farmed and the number of pump operating hours during the period in question. The City's experts contend the data used by Hardin and Prochaska in their opinions is not that which other experts in the field would reasonably rely upon. They do not appear to be unrealistic, however, and, therefore, Mr. Hardin's opinion is accepted as but one factor to be considered. On the other hand, Mr. Anderson, also a Harloff expert hydrogeologist, claims the requested withdrawals would result in only an additional 1.7 foot drawdown in the Upper Floridan Aquifer underlying the Northeast corner of the Verna Well field. To be sure, this is only one small portion of the wellfield in issue. There has, however, been a continuing history of declining groundwater levels in this area over the past several years. After the 1975 drought, the City started to experience declining water levels at Verna which, because of the reduction in ability to produce water, required a lowering of the pump elements in some wells, and also caused the City to develop an R.O. facility in an effort to reduce dependence on well water. This drop in capability occurred again during the 1985 drought and this time the City modified the pump motors to shut off prior to cavitation and initiated a schedule of operating times for wells, so that water is drawn from different and geographically separated areas in a sequence designed to allow periodic regeneration of an area's supply. Nevertheless, water supply remains a concern at Verna, and the problems previously experienced continue to occur during periods of drought. In May 1989, the Verna Wellfield was periodically "unable" to meet it's short term peak demands at times even though all operating wells were pumping. This means that at the times in question, more water was being drawn from the Verna reservoir than could be replaced by pumping activities. It does not mean that the reservoir ran dry and water could not be furnished to the treatment plant. However, this condition is serious and indicative of a more serious shortage in the future unless appropriate safeguards are instituted. Mr. Balleau, the City's expert in hydrology and hydrogeology, and the District's experts all believe the Verna Wellfield is in trouble. It is operating well beyond its design range and the imposition of additional demands on it would seriously and adversely affect its ability to produce water. This position is supported by the facts and found to be accurate. There appear to be several options open to the City to contend with the Verna problem potential. These include: drill deeper wells at Verna to tap the Lower Floridan Aquifer. (This will produce the lower quality water found there and require additional treatment facilities. construct a linear wellfield along the pipeline from Verna to the treatment facility. (This will require additional permitting to draw the water, high construction and operating costs, and still result in low quality water requiring treatment. redevelop the downtown wells currently supplying the R.O. facility. (This will require satisfaction of regulatory issues, adversely impact on the users of the upper aquifers, possibly result in poor water quality and in contamination from nearby landfills.) develop a new well field southeast of Verna. (This will experience regulatory issues and high construction costs, with an unknown water quality result.) buy water from Manatee County. (This is expensive, may result in transmission and compatibility problems, and would be only a short term solution. lower pump assemblies; replace existing pumps and modify the pump circuits. (These are all unreliable, short term solutions of minimal benefit.) Mr. Harloff and the City/District disagree on the appropriate amount of water needed for the successful growing of the crops produced by his operations. Both agree, however, that the heaviest demands for water come in the spring growing season including April and May. Tomatoes require the most water. Peppers require nearly as much. This is because the short root systems require a higher water table in the soil to supply needed moisture. In its analysis of Mr. Harloff's application, the District, referring to tables developed for the purpose of allocation and relating to Harloff's watering history during the period from August 15, 1988 to June 7, 1989, subtracted the fall season recorded application of 20.7 acre-inches from the total 10 month figure of 50.92 acre-inches and concluded he would need 30.22 acre-inches for peppers during the spring, 1989 season. Unless shown to be totally unreasonable, however, (not the case here), the applicant's water need figures should be accepted. Mr. Harloff's operation constitutes an important part of Manatee County's agricultural economy, and agriculture utilizes 68.9 percent of the land in the county. Agricultural products sold in Manatee County in 1987 were valued at $145,655,000.00, which ranked Manatee County third among all Florida counties in vegetable production. Agriculture is the fourth largest employer in Manatee County, employing an average of 4,692 people per month. Through his farm operation alone, Harloff employes as many as 1,050 people, with 200 employed on a full-time basis. Experts estimate that the loss of the Harloff operation would cause a reduction of between 16 and 18 million dollars in agricultural sales in the county with an additional loss in jobs and income to his suppliers. This estimate is not at all unreasonable. Florida produces approximately 95 percent of all tomatoes grown in this country for the fresh tomato market during the winter growing season. Tomatoes are the single largest vegetable crop grown in the state and accounted for 39.7 percent of the total value of vegetables produced in Florida during the 1987-1988 growing season. Mr. Harloff produced 4.8 percent of the total shipment of tomatoes from this state during that period. Water, primarily through irrigation, is an indispensable portion of the farming operation for this crop. Mr. Harloff currently irrigates the majority of his non-citrus crops by use of a "semi-closed ditch irrigation system", as opposed to a "drip system." The drip system is considerably more efficient than the semi-closed system having an efficiency rating, (amount of water actually used by the plants) of between 80 to 90 percent, as opposed to 40 to 60 percent for the other. While Mr. Harloff could reduce his water needs considerably and achieve substantial savings on pump fuel by conversion to a drip system for all or a part of his crops, such an undertaking would be quite costly. One of the conditions proposed by the District for the approval of Harloff's permit, as amended, is the refurbishment of several of the existing wells utilized by Mr. Harloff to make them more efficient and to promote the withdrawal of water from the Lower Floridan Aquifer, in which there appears to be adequate water and from which the Verna Well field does not draw. Currently, Mr. Harloff has seven wells which do not meet the standards of this proposed condition. They are not drilled to 1,300 feet below mean sea level and are not cased to 600 feet. To bring these wells into compliance, they would have to be drilled to the 1,300 foot level, or to a level which has a specific capacity of 400 gpm, and the casings in each would have to be extended to 600 feet. Extending the casings would be a complicated procedure and Harloff's experts in the area cannot guarantee the procedure would successfully achieve the desired end. Assuming the retrofit was successful, the cost of the entire process would be approximately $15,000.00 to $16,000.00 per well. In addition, the process would, perforce, require reducing the diameter of the well from 10 to 8 inches, thereby necessitating increasing the pump capacity to produce sufficient water. The cost of this is substantial with an appropriate new pump costing somewhere between $10,000.00 and $15,000.00 each. Consequently, the anticipated cost of bringing the existing wells up to condition standards would be between $25,000.00 to $31,000.00 per well, while the cost of constructing a new well is between $40,000.00 and $50,000.00 per well. Mr. Harloff feels it would be more prudent for him to replace the existing wells rather than to retrofit them. This may be correct. Harloff experts also claim that extending the casings on the existing wells down to 600 feet would not provide a significant benefit to the aquifer nor cause any significant reduction in drawdown impact at Verna. The District and City experts disagree and, taken on balance, caution and the interests of the public indicate that a conservative approach is more appropriate. While Mr. Harloff proposes to convert the areas served by wells 1, 9, 11, and 12 to the growing of citrus which requires much less water than tomatoes, this would not be sufficient mitigation to offset the need for some modification if large amounts of water will still be drawn. The entire area under the District's jurisdiction has been experiencing a water shortage due to a lack of rainfall. As a result, in June 1989, the District adopted a resolution identifying an area, including the area in question here, as a "water use caution area." This was done because the Floridan Aquifer has been subjected to large seasonable drawdowns of the potientiometric surface, the level to which water in a confined aquifer can rise in a well which penetrates that acquifer. This drawdown is directly related to increased water use in the area, much of which is for agricultural purposes. As a result of the District's action, special conditions on well construction for consumptive use applicants have been imposed on a permit by permit basis to insure, as much as possible, that the applicant uses the lowest quality water appropriate for his intended purpose. These conditions are not unreasonable. While accepting the District's and City's conclusion that his wells, if permitted, would have some impact on the Verna Wellfield, Mr. Harloff does not concede that the impact is significant. Specifically, the difference in impact resulting from an increase from his currently permitted use of 13.68 mgd seasonal maximum and his requested use of 31.56 mgd seasonal maximum for wells 1, 2, 9, and 10 would be a maximum increased drawdown of 1.1 feet at the Intermediate aquifer and 1.8 feet at the Upper Floridan Aquifer. Both figures relate to that portion of the wellfield found in the northeast corner of Part A. If the anticipated usage for crops predicted by Mr. Harloff's experts for the spring of 1989 is accurate, the drawdown would be 0.2 feet for the intermediate aquifer and 0.4 feet for the Upper Floridan Aquifer measured at the northeast corner of Part B of the Verna We1lfield. Harloff's experts contend that additional impacts for the spring of 1989 included, the increased usage will not have a significant effect on Verna's ability to produce its permitted daily maximum withdrawal of 9.5 mgd. While this is an educated speculation, it should be noted that during May 1989, the Verna field was able to produce up to 8.3 mgd without using all wells during any 24 hour period. This does not consider, however, the problems encountered by the City as indicated by the wellfield personnel, and the fact that some of the City wells are not pumping water.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that Roger Harloff be issued a consumptive use permit, No. 204467.04, as modified, to reflect authorization to draw 15.18 mgd annual average, not to exceed 31.56 mgd seasonal maximum, conditioned upon compliance with the conditions found in the conditions portion of the permit, as modified to conform to the quantities as stated herein, and to include those requirements as to acre-inch and crop-acre limitations, well usage and abandonment schedules, well modification standards, and record keeping, as are contained therein. RECOMMENDED this 5th day of December, 1989, in Tallahassee, Florida. ARNOLD H. POLLOCK, 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 5th day of December, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE No. 89-0574 The following constitutes my specific rulings pursuant to s. 120.59(2), Florida Statutes, on all of the proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONER: City of Sarasota, joined by the District 1 & 2. Accepted and incorporated herein. 3. Accepted and incorporated herein. 8-12. Accepted and incorporated herein. 13. Accepted and incorporated herein. 14-22. Accepted and incorporated herein. 23-25. Accepted and incorporated herein. 26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29-33. Accepted and incorporated herein. Not a Finding of Fact but a statement of party position. & 36. Accepted. 37. & 38. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not a Finding of Fact but a comment on opponent's satisfaction of its burden of proof. 42-44. Accepted and incorporated herein. Accepted and incorporated herein. Rejected as a misstatement of fact. Water service was never interrupted. The deficiency was in the City's inability to keep its wellfield reservoir filled. 47-54. Accepted and incorporated herein. Accepted and incorporated herein. Rejected for the reasons outlined in 41. 57-62. Accepted and incorporated herein. 63. Rejected for the reasons outlined in 41. 64-66. Accepted and incorporated herein. Rejected for the reasons outlined in 41. Rejected. & 70. Accepted and incorporated herein. 71. & 72. Accepted and incorporated herein. 73. Accepted and incorporated herein. 74 & 75. Accepted and incorporated herein. Accepted. Not a Finding of Fact but a statement of party position. Rejected. Accepted. Irrelevant. 81-84. Rejected. 85. & 86. Accepted and incorporated herein. 87 & 88. Accepted and incorporated herein. 89. Accepted and incorporated herein. 90 & 91. Accepted and incorporated herein. 92. & 93. Accepted and incorporated herein. FOR THE RESPONDENT: Roger Harloff 1-9. Accepted and incorporated herein. 10-13. Accepted and incorporated herein. 14 & 15. Accepted and incorporated herein. 16-25. Accepted and incorporated herein. 26-28. Accepted and incorporated herein. 29 & 30. Accepted. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not proven. 35 & 36. Accepted and incorporated herein. 37 & 38. Accepted and incorporated herein. 39-41. Accepted and incorporated herein. 42 & 43. Accepted and incorporated herein. 44. Accepted. 45 & 46. Accepted and incorporated herein. 47 & 48. Accepted and incorporated herein. 49. Accepted. 50 & 51. Accepted and incorporated herein. Accepted. Accepted. Accepted. & 56. Accepted and incorporated herein. 57. Accepted. 58-60. Accepted and incorporated herein. 61 & 62. Accepted and incorporated herein. Rejected as unproven. Accepted. Accepted and incorporated herein. Accepted. 67-68. Accepted. Not a Finding of Fact but an interpretation of party po Accepted. Rejected. 72 & 73. Accepted. COPIES FURNISHED: Edward P. de la Parte, Jr., Esquire de la Parte, Gilbert and Gramovot, P.A. 705 East Kennedy- Blvd. Tampa, Florida 33602 Edward B. Helvenston, Esquire SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899 Douglas P. Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Peter G. Hubbell Executive Director SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
Findings Of Fact Respondent/Applicant, North Orlando Water and Sewer Company, filed an application on August 11, 1981, with Respondent, Department of Environmental Regulation, seeking a permit to authorize the construction of sewage effluent disposal ponds in Winter Springs, Seminole County, Florida. On August 16, 1981, the Department advised the Applicant that additional information was required. This information was supplied by Applicant on September 11, 1981. After reviewing the application and supplemental information, the Department determined that Applicant had provided reasonable assurance that the proposed percolation ponds would not adversely affect waters of the State and thereafter issued Permit No. DC59-46435 on September 22, 1981, authorizing the construction of the requested activity. Petitioners are owners of the property on which one of the disposal ponds is to be constructed. On June 12, 1981, Applicant instituted condemnation proceedings in Circuit Court for Seminole County under Chapters 73, 74 and 361, Florida Statutes, seeking to condemn the property so that the facilities could be constructed. The suit remains pending until all necessary permits from the Department are acquired by Applicant. The parties agree that based on plans, test results and other information, the construction of the proposed installation will not discharge, emit, or cause pollution in contravention of Department standards, rules or regulations. The permit was issued without formal public notice. However, it falls under the class of permits enumerated in Rule 17-1.62(3)(a), Florida Administrative Code. That rule makes publication of a notice discretionary on the part of the Department, and no abuse of discretion was shown. Item D(i) on page 7 of the application requires that the Applicant "[i]ndicate the number of potable water supply wells within 500 feet of effluent disposal area, the depths of these wells and their approximate distances from the disposal area." Applicant answered "None". There are no public potable water supply wells within 500 feet of the effluent disposal area. There are several private potable water supply wells within 500 feet of the pond but adequate buffer zones between these private potable water supply wells and the actual effluent disposal area exist. Moreover, Petitioners' expert witness conceded that seepage would be minimal, should not be a concern, and the failure to list the private wells on the application had no effect on the substantive merits of the application. Applicant construed the term "potable water supply wells" to mean only public wells since DER has no jurisdiction over private wells. For this reason, it answered the question in the manner that it did. The Department concurs in this interpretation.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that Permit No. DC59-46435 be issued to Applicant, North Orlando Water and Sewer Company. DONE and ENTERED this 23rd day of July, 1982, in Tallahassee, Florida. DONALD R. ALEXANDER Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 23rd day of July, 1982.
The Issue The issue in the case is whether the Petitioner's employment position was properly reclassified from Career Service to Selected Exempt Service pursuant to Section 110.205(2)(x), Florida Statutes (2001).
Findings Of Fact Beginning on April 23, 2001, and at all times material to this case, the Petitioner was employed by the Hillsborough County Health Department as a Professional Engineer III, a position requiring state registration in accordance with Chapter 471, Florida Statutes (2001). The job announcement related to the Petitioner's employment states that the position "oversees" the drinking water program and engineering-related activities. The position was responsible for management of "Safe Drinking Water" permitting and compliance enforcement program entailing a variety of duties, including planning, organizing, and coordinating work assignments. According to organizational charts before and after the date of the reclassification of the position, the Professional Engineer III position had direct supervision of four employment positions, and indirect supervision of eight additional positions that reported to one of the Petitioner's direct employees. The position of Professional Engineer III includes a substantial amount of engineering review responsibilities, and is charged with direct supervision of the Safe Drinking Water Act program staff and Limited Use Drinking Water program staff. The position description categorized the job responsibilities as "regulatory," "supervising/training," "enforcement," "policies and procedures," "record keeping," "education," and "committees/other duties." Review of the specific duties indicates that the Petitioner's supervisory responsibilities were included within several of the categories. Included within the "regulatory" category was "[e]nsures staff conduct field inspections of public water systems. . . . Supervisor is responsible and accountable for field staff." Included within the "supervising/training" category were the following duties: Supervises Engineers to ensure all programs in the Safe Drinking Water Program are completed according to the agreement with DEP and the policies and procedures of the Department of Health. Supervises an Environmental Supervisor II to ensure that all programs in the Limited Use Drinking Water Program and Private Drinking Water Program are completed according to the F.S., F.A.C. and county regulations. Supervises staff review of engineer's plans. Supervises and reviews the preparation of non-compliance letters written by staff regarding enforcement actions. Provide training to new Health Department staff in all aspects of EHS at least once a year (standardized presentation). Perform field inspections (documented) with personnel on a quarterly basis to evaluate staff performance and for Quality Improvement (QI) in accordance with office policy. Telephone regulated facilities each quarter to determine customer satisfaction . . . in accordance with office policy. Develop training modules for specific program areas (public drinking water systems) and maintain them accurate and current. Provide those training modules to new EH staff and twice a year to existing EH staff. Assign staff to special work areas as necessary and perform field inspections (staff shortages, vacation/leave time, and natural disaster). Evaluate personnel's work, plan work load, special tasks to include efficiency. Included within the "enforcement" category were the following duties: Reviews appropriate enforcement activities generated by staff and assure timely progress of formal enforcement from compliance to enforcement. Ensures the time progress of enforcement cases by working closely with the compliance section of the Public Drinking Water Program in bringing non-compliant clients into enforcement. Follow up on violations of FAC and/or FS and ensure compliance is achieved or enforcement action is taken. Included within the "policies and procedures" category was the responsibility to "[r]eview daily activity reports and corresponding paperwork each day." The Petitioner was responsible for managing the daily workflow of the office. He planned, directed, and reviewed the work performed by his employees. The Petitioner was responsible for the evaluation of all employees under his direct supervision, including newly hired probationary employees. The Petitioner was responsible for review of the evaluations for employees for whom he had indirect supervisory duties, and he also provided his own independent evaluation of their performance. The Petitioner was responsible for the discipline of employees. At one point he had to counsel an employee who was consistently late to arrive for work. The Petitioner was also responsible for seeking qualified applicants for position openings. He was responsible for initiating the employment process. He chose the panel that interviewed applicants, designed the interview questions, participated in interviews, and made the final recommendation as to the person hired. He had the authority to decline to fill an open position if he deemed that the applicants lacked sufficient qualification. The Petitioner claims that the majority of his time was spent in review of permit applications and related engineering tasks. The evidence fails to support the assertion. The Petitioner's claim appears to essentially relate to a period of time subsequent to the July 1, 2001, reclassification of the position. During the time between his initial employment and the date of the position reclassification, the Petitioner was primarily a supervisory employee and had little, if any, permit review responsibilities. The office was fully staffed with other employees who were directly responsible for review of permit applications and related field reviews. In autumn of 2001, after the position was reclassified, the office began to lose employees, resulting in an increased workload for the remaining workers. At this point, the Petitioner began to undertake a substantial role in the actual review of permit applications in addition to his supervisory duties. Nonetheless, the Petitioner remained responsible for supervision of remaining employees. The Petitioner was also responsible for filling the vacant positions.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Education enter a Final Order finding that the "Professional Engineer III" position held by Raymond Van Loon on July 1, 2001, was properly classified into the Selected Exempt Service. DONE AND ENTERED this 21st day of April, 2004, in Tallahassee, Leon County, Florida. S WILLIAM F. QUATTLEBAUM 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 21st day of April, 2004. COPIES FURNISHED: Stephen W. Foxwell, Esquire Department of Health 4052 Bald Cypress Way, Bin A02 Tallahassee, Florida 32399-1703 Aaron J. Hilligas, Esquire AFSCME Council 79 3064 Highland Oaks Terrace Tallahassee, Florida 32301 Maria N. Sorolis, Esquire Allen, Norton & Blue, P.A. 324 South Hyde Park Boulevard Hyde Park Plaza, Suite 350 Tampa, Florida 33606 Jerry G. Traynham, Esquire Patterson & Traynham Post Office Box 4289 315 Beard Street Tallahassee, Florida 32315 William E. Large, General Counsel Department of Health 4052 Bald Cypress Way, Bin A02 Tallahassee, Florida 32399-1701 R. S. Power, Agency Clerk Department of Health 4052 Bald Cypress Way, Bin A02 Tallahassee, Florida 32399-1701
The Issue As reflected in the parties' prehearing stipulation filed on August 28, 1991, the issue in this case is whether the St. Johns River Water Management District (SJRWMD) should approve South Brevard Water Authority's (SBWA) consumptive use permit (CUP) application. The SBWA is seeking permission to withdraw an annual average daily rate of 18.8 million gallons (mgd) and a maximum daily rate of 21.4 mgd. The District proposes to grant the permit with specified conditions. Petitioners challenge the issuance of the permit, alleging that applicable requirements of Chapter 373, F.S. and Chapter 40C-2, F.A.C. and other applicable law are not met. The standing of Petitioners, other than Osceola County, is at issue. Also at issue is whether the relevant criteria include consideration of the adequacy of existing sources of water, and the consideration of costs of utilizing existing sources versus the cost of the proposed new source of water.
Findings Of Fact The Parties The applicant, South Brevard Water Authority (SBWA) was created by special act of the legislature, Chapter 83-375, Laws of Florida. Its principal office is located in Melbourne, Brevard County, Florida. Its general mission is described in Section 1, of Chapter 83-375, Laws of Florida, as amended by Chapter 87-481, Laws of Florida: Section 1. It is hereby declared and determined by the Legislature that a regional water authority is the most responsive, efficient, and effective local government entity to secure, operate, and maintain an adequate, dependable, and safe water supply for the district and customers of the district. It is the intent of the Legislature that such regional water authority possess the full power and authority to implement, finance, and operate a single coordinated program of water supply transmission and distribution to meet the future quantity and quality needs of the district and for customers of the district. There is a paramount public need to develop a safe, reliable, and energy-efficient source of public water for the district residents and to contruct the wellfields, transmission lines, and other facilities necessary to supply such water. The St. Johns River Water Management District (SJRWMD or District) is an agency created pursuant to Chapter 373, F.S. in charge of regulating consumptive uses of water in a 19-county area of the State of Florida, including all of Brevard and part of Osceola County. The geographical boundaries of the District are described in Section 373.069(2)(c), F.S. Osceola County is a political subdivision of the state, west of, and contiguous to, south Brevard County. The Corporation of the President of the Church of Jesus Christ of Latter Day Saints (Deseret) is a Utah corporation authorized to conduct business in the State of Florida. Deseret owns real property in Osceola County to the north and east of the proposed wellfield. Deseret possesses a valid consumptive use permit authorizing the withdrawal of water for this property. East Central Florida Services (ECFS) does not own land or possess a consumptive use permit (CUP). Its purpose is to take over the water management program for the Deseret property. It has applied to the Public Service Commission for certification. Notwithstanding the parties' stipulation that "Triple E Corporation" and "Triple N Corporation" own real property in Osceola County near the proposed wellfield (prehearing stipulation, filed 8/28/91, p. 5), no such corporations are registered in the State of Florida. The lands identified as Triple E and Triple N are owned by multiple parties through trusts, primarily managed by Maury L. Carter, one of the owners. Neither Triple E nor Triple N properties have CUP's. The properties are used for agricultural purposes and the Triple N property has a well and recreational camp. The Site of the Proposed Use The proposed wellfield is located on property owned by the SJRWMD, the Bull Creek Wildlife Management Area (BCWMA), located entirely in eastern Osceola County. The BCWMA is comprised of 22,206 acres within the drainage area of the St. Johns River. The northern third of the management area is drained by Crabgrass Creek, and the southern two-thirds is drained by Bull Creek. The easternmost boundary is located approximately one mile from the Brevard County boundary. Currently all 22,206 acres of the BCWMA are under lease to the Florida Game and Fresh Water Fish Commission, which agency manages the area as a public recreation facility for hunting, fishing, hiking, horseback riding, camping and archeological studies. The sparsely populated area has historically been used for logging and cattle grazing. It was acquired for a detention area and it currently provides nonstructural flood protection. Its surface topography is relatively flat, with uplands and wetlands separated by only inches in vertical elevation. Upland communities include pine flatwoods, saw palmetto prairies, pine savannahs and sand oaks. Wetland communities include cypress domes, mixed shallow marshes, sawgrass marsh, wet prairies and transitional prairies. The BCWMA is classified as a "conservation area" in the District's current adopted Five Year Land Plan which summarizes the agency's land acquisition and management policies. A "conservation area" is defined as "...an area acquired for water resource conservation and protection in an environmentally-acceptable manner". The term includes water supply areas, including areas for public wellfield location. (Osceola Co. exhibit #33, p. 15) Facilities Associated with the Proposed Consumptive Use Although the precise siting of the wells has not been established, the wellfield will be located at the northern end of the BCWMA, east-west into a "panhandle" area, and extending south, for an inverted "L" shape. The wellfield will consist of 12 production wells in 2000 ft. intervals. Wells 1-9 will lie along an east-west axis adjacent to Crabgrass Creek, while wells 10-12 will lie along a north-south axis below well 9, the eastern-most well. The capacity of each well is designed at 3,000 gallons per minute or approximately 4.30 million gallons a day (mgd). Each well consists of 20" diameter casing pipe extending 700' below the ground surface. From there, an open hole for production will extend another 250 feet in depth. A small, 20 ft. by 30 ft., concrete building will enclose the motor and other equipment associated with each well, in order to eliminate vandalism and to baffle the noise. The wells will be sited to avoid jurisdictional wetlands. In addition to the production wells, monitoring wells will be constructed to comply with permit conditions. Because the water drawn from the proposed wellfield will exceed potable standards, reverse osmosis (RO) desalinization treatment is required. A below ground header pipeline will carry raw water from the wellfield to an RO treatment facility in Brevard County. The RO treatment facility will process 75 percent of water coming from the wellfield, 85 percent of which is recovered as finished water, and 15 percent of which is disposed of as brine by deep well injection. The 25 percent of raw water which bypasses the treatment process will be blended with the finished water to yield water which meets drinking water standards for chloride levels. The yield is anticipated to be 16.67 mgd on an average day and 18.9 mgd on a maximum day. However, the finished water yield could be higher if raw water quality permits greater blending and less reject water. On the finished water side, the water will need to be treated again to assure that it will be compatible with water from the City of Melbourne plant. Failure to balance the blended waters chemically could result in corrosion of pipes, leaching of pipes, discoloration, rusty water, and odorous water. A proper process, therefore, is essential and is highly sophisticated. From the treatment facility the water will travel in underground pipes, beneath the St. Johns River, beneath I-95 and east to the Melbourne distribution system. From there some water is anticipated to travel south to connect to the General Development Utilities (GDU) system. Hydrogeologic Characteristics of the Site For modelling purposes, the aquifer system in the region is represented by sequential layers of differing characteristics in the flow and movement of water. The SBWA model contains 6 layers; the Osceola model contains 7 layers. In both models, layer 1 corresponds to the surficial (water table) aquifer; layer 2 corresponds to the Hawthorn formation (the upper confirming layer); layer 3 is the Upper Floridan aquifer; layer 4 describes the 200 ft. thick portion of the Upper Floridan called the "production zone"; layer 5 in the SBWA model is approximately 450 ft. thick and is called a confining unit; Osceola's consultants consider this layer less permeable or semi-confirming; layer 6 is the lower Floridan; and layer 7 in the Osceola model is the bottom reaches of the lower Floridan. The surficial aquifer consists of sand and shell deposits and extends to a depth of approximately 100 feet below land surface. The surficial aquifer is capable of producing small to moderate amounts of water for domestic uses. The Hawthorn is an interbedded formation consisting of clay, limestone and phosphate. Due to its extremely low permeability, this layer restricts both the vertical and horizontal movement of water. The Hawthorn is thicker in Central Florida than in other portions of the state. At the BCWMA the thickness of the Hawthorn ranges from 240 feet in the area northwest of the management area to 80 feet in the southeastern portion of the management area. The upper Floridan Aquifer at the BCWMA, as characterized by the SBWA's consultant and based on site specific data, extends from the base of the Hawthorn to a depth of approximately 900 feet below land surface. That portion of the upper Floridan Aquifer between the bottom of the Hawthorn and 700 feet below land surface consists of fine grained limestone with relatively low permeability. This zone corresponds with layer 3 in the groundwater modeling done by the SBWA. The portion of the upper Floridan between the bottom of the Hawthorn and 700 feet below land surface is less capable of producing water than the portions below this level. That portion of the upper Floridan Aquifer between 700 feet and 900 feet of depth consists of hard dolomites. Dolomitic zones are the most productive zones of water within the Floridan in this part of the state because these formations contain solution fractures and cavities. This zone corresponds with layer 4 in the groundwater modeling done by the SBWA. Several researchers and modelers have suggested the existence of a zone, variously referred to as a semi-confining unit, a zone of lower permeability or a middle semi-confining unit, located between the upper and lower Floridan Aquifer. This area between 900 feet and 1350 feet below land surface consists largely of hard dolomites similar in nature to those in the zone immediately above it. This zone corresponds to layer 5 in the groundwater modeling done by SBWA. Previous regional modeling efforts have utilized model derived values to describe the middle semi-confining unit rather than site specific information showing the location, thickness or hydrogeological characteristics of the zone. Site specific data tends to confirm the lower permeability of this zone relative to the layers above and below it. Site specific data consists of a core sample, mineral content observed during the drilling of the test monitor well, and a Neumann-Witherspoon ratio analysis conducted during the aquifer performance test. The area between 1350 feet and 1450 feet below land surface also consists of dolomites but with greater permeability and greater transmissivity (the measure of an aquifer's ability to transmit water in a horizontal direction). This area corresponds to layer 6 in the groundwater modeling done by the SBWA. No site specific data exists beneath 1483 feet, representing the total depth of test well TM. Regional data does exist which characterizes the areas from 1500 feet below land surface to the bottom of the lower Floridan Aquifer as consisting of zones of varying lithology, and varying permeabilities. This zone which corresponds to layer 7 in the groundwater modeling done by Osceola County is not homogeneous or uniform over its entire thickness according to available regional data, consisting of geologic reports of deep wells in the east-central Florida area. All parties agree that in the area of the proposed wellfield, horizontal movement of water in the Floridan aquifer is from west, where the greatest recharge occurs along the Lake Wales Ridge, to east, where there is little or no recharge. Water quality in the upper Floridan as measured by chloride concentrations deteriorates as one moves from west to east. The Floridan aquifer beneath the BCWMA represents a transition zone between the recharge area to the west and high saline formation waters in the east. The dominant geochemical components in water beneath the BCWMA are biocarbonates. Water quality, as measured by chloride concentrations, also deteriorates with depth. Chloride concentrations, based on data derived from the drilling of well TM at the BCWMA, increase gradually from 306 milligrams per liter (mgl) at 410 feet, to 658 mgl at 1473 feet below land surface. Chloride concentrations increase abruptly to 1980 mgl in well TM at 1483 feet of depth. Evidence is inconclusive as to whether all of the proposed production wells will draw water exceeding 250 mgl in chloride concentrations. It is undisputed that most will, but chloride contours initially provided by SBWA's consultant indicate that the southernmost wells may produce water between 150 and 250 mgl. A comprehensive aquifer performance test (APT) was conducted at the BCWMA by the SBWA's consultant, Post, Buckley Schuh, and Jernigan, Inc. (PBSJ). The test was designed by the staff of the SJRWMD in consultation with the U.S. Geological Survey (USGS). This test yielded data which enabled PBSJ to calculate several aquifer characteristics for use in the groundwater modeling which was later done by SBWA's modeling consultant, Environmental Science and Engineering, Inc. (ESE). Eight wells were utilized in connection with the APT conducted at the BCWMA in January and February 1990. Three of the wells were dual zone monitoring wells capable of monitoring events in two different geologic units simultaneously. Three wells, including the test production well (TP) were open to the interval between 700 and 900 feet below land surface which was identified by the SBWA as the production zone. Typically APT's are run for 12 to 72 hours in Florida. Well TP was pumped for approximately 10 days at a rate equivalent to that expected during actual production while observations were made of water levels in all wells, including three off-site wells (the Holopaw test well, the Kempfer well and the Bruner well). All of the information the SBWA needed from the APT was obtained in the first hours of the test. Water levels in the area monitored during the APT ceased dropping due to pumpage within 1 hour after the pumping started. Three different analytical models were used to calculate a transmissivity value for the production zone, utilizing data derived during the APT. The result showed transmissivity in this zone to be approximately 2 million gallons per foot per day. This is a very high transmissivity value indicating a comparatively prolific aquifer, capable of producing the volumes of water requested in the application. As transmissivity increases, the cone of depression associated with pumpage tends to flatten out and be less steep. The cone of depression extends further out, creating a wider area of drawdown. Hydraulic conductivity is the measure of an aquifer's resistance to flow either in a vertical (KV) or horizontal (KH) direction. Two methods were used to calculate the hydraulic conductivity of the Hawthon Formation by PBSJ: laboratory analysis of a core sample taken from this unit, and a bail test (measuring an increase in water level over time) conducted on a well on site by the SJRWMD. Two different methods were used by PBSJ to calculate the hydraulic conductivity of layer 5: laboratory analysis of a core sample taken from that zone, and the Neuman-Witherspoon ratio analysis method. Porosity is the void space in porous media through which transport of particles, such as chlorides, can occur. Effective porosity has an impact on the ability of saline or dense water to move upward from depth toward a pumping well. The lower the effective porosity within an aquifer, the greater the potential for upconing of saline water within that aquifer. Effective porosity for layers 4 and 5 was calculated using two different methods, those being laboratory analysis of core samples taken from these zones, and analysis of acoustic logs generated during the APT. Each of these methods is accepted in the field of hydrogeology. Anticipated Impacts to Groundwater Levels and Flows as a Result of the Proposed Consumptive Use A numeric groundwater flow model is a computer code representing the groundwater flow process. Both SBWA and Osceola used numeric groundwater flow models developed by their consultants to predict and simulate the impacts associated with withdrawals proposed in the application. The SBWA used a finite difference model called INTERSAT for its simulations. INTERSAT is a widely used and accepted groundwater flow model. The model was run by ESE for the SBWA in the impact or drawdown mode. Drawdown or impact models simulate changes in water levels in response to a stress such as a pumping well. Drawdown models are an accepted and frequently used method to evaluate wellfield stress, particularly in association with a CUP application. ESE and PBSJ utilized several analytical models to first determine and later to verify the area to which the boundaries of their model would extend. The radius of influence of a well or wellfield is the distance from the center of pumpage extending out to where drawdowns caused by that pumpage reach zero. The boundary for a numeric groundwater model should be set at, or beyond, the radius of influence of the pumpage being simulated by the model. Based on the analytical models run by ESE and PBSJ the radius of influence of the wellfield proposed in the application is 43,000 to 45,000 feet. The approximate distances of the boundaries set in INTERSAT model from well TP were 50,000 feet to the east, 40,000 feet to the west, 40,000 feet to the north and 50,000 feet to the south. The INTERSAT model covers a total area of 320 square miles. This size falls somewhere between a regional model and a local model, and is adequate in size to address the impacts associated with the proposed withdrawals. The vertical boundary of SBWA's model extends to 1450 feet below land surface and, as stated above, is divided into 6 layers. The 1450 feet depth generally coincides with the limits of site specific data generated during the APT. The six layers in the SBWA flow model coincide with the six distinct geologic units identified by PBSJ in their APT report. The site specific data generated by the APT was utilized, along with other regional modeling studies, to arrive at a set of "conservative" aquifer parameters to be utilized in the INTERSAT model. "Conservative" parameters for purposes of this application are those which would tend to overpredict drawdown in the surficial aquifer and the production zone, while allowing for more upconing of dense water from the bottom of the model. The selection of "conservative" aquifer parameters by SBWA involved taking site specific values, comparing them with the ranges of values reported in the other available regional models and selecting values which, while still within the range of reported values used in other studies, would tend to show greater impacts for the areas of primary concern than the site specific values. Every aquifer parameter utilized in SBWA's groundwater flow model falls within the range of values reported in at least one of the groundwater modeling studies previously done in this region. The size of the grids utilized in the SBWA model were 500 feet by 500 feet within the vicinity of the wellfield. Grid sizes expand as one moves toward the outer boundaries of the model. The fineness of the grids used by ESE, particularly in the wellfield area, allows for accurate representation and resolution of surface water features, impacts in the production zone and for evaluating the effects of saltwater upcoming in the transport model also done by ESE. Within the radius of influence of the proposed wellfield, there are no existing wells in layers 5 or 6. The ESE model simulations for 18.8 mgd pumpage predict a maximum drawdown in the surficial aquifer (layer 1) of 0.14 feet centered primarily within the BCWMA. At a distance of 1 mile from the wellfield the impact drops to 0.12 feet. None of the existing legal users of water in layer 1 within the radius of influence of the proposed wellfield will suffer a ten percent or greater reduction in withdrawal capacity from their wells solely as a result of the proposed withdrawals, since 10 percent reduction would require at least 3 feet of drawdown. The ESE model simulations predict a maximum drawdown caused by the proposed pumpage of 4.5 feet in layer 3 centered along the alignment of wells and primarily within the BCWMA. At a distance of 2 miles, the drawdown drops to 2 feet. At the Brevard-Osceola County line the drawdown in layer 3 is approximately .5 feet. Petitioner Deseret's flowing wells are drilled in layer 3 and are located within the area where a drawdown of 1 foot is predicted in layer 3 by the ESE model. Deseret uses its property for a cow/calf ranching operation and has approximately 32,000 head of cows. Deseret uses 39 flowing wells east of state road 192 to irrigate pasture, water cattle and supply drinking water. Deseret possesses a valid CUP for a portion of the total flow capacity from those wells. Seasonally, the wells flow at different rates, but they are most relied upon in dry conditions when the natural flow would be decreased. It is unlikely that the proposed SBWA withdrawals will stop the flow of any of Deseret's wells; and it is unlikely that the flow will be reduced by more than 10 percent. Deseret and Osceola's consultants do predict a greater drawdown and opine that approximately 12 of Deseret's wells will cease flowing as a result of the SBWA withdraw As addressed below, the modelling by Petitioner's consultants, upon which those predictions are based, is less reliable than that of SBWA's consultants. If the effects are greater than predicted, mitigation in the form of installation of pumps is possible, albeit inconvenient and expensive. Mitigation would have to be provided by the applicant, SBWA. The drawdowns predicted by the ESE model for layer 4 are not significantly different from those for layer 3. It is anticipated that no legal user of water within the radius of influence of the proposed wellfield will suffer a 10 percent or greater reduction in withdrawal capacity for its wells, as a result of SBWA's proposed withdrawals. Petitioners' consultants, Hartman and Associates, (Hartman) modeled a significantly larger (4900 square miles) and deeper (3000 feet) area than did SBWA. The model makes its predictions based on one data point for every 49 square miles within the modeled area. Petitioners utilized much larger model grids in the wellfield area (2000 feet by 2000 feet) than did the SBWA. Grid of this size lacks the resolution necessary to evaluate wellfield impacts. Petitioners selected their aquifer parameters from another regional modeling study done in 1985 rather than using site specific data. Those parameters were then adjusted or calibrated until a match was obtained to a computer created potentiometric surface which was supposed to reflect the potentiometric surface for May 1990, an uncharacteristically dry period. The created potentiometric surface to which Hartman calibrated its model varies greatly from the potentiometric surface as reflected in the actual data points from which USGS derives its potentiometric surface maps. While no model is perfect, and actual data is preferable, in the absence of all the actual data that is needed, the ESE model is a more credible predictor of drawdowns. Anticipated Impacts to Groundwater Quality as a Result of the Proposed Consumptive Use Solute transport models are computer models designed to simulate the movement of mass, in this case -- chlorides -- through a groundwater flow system. These models are linked to, and are dependent on flow fields generated by groundwater flow models. In order to predict changes in water quality anticipated to occur as a result of its proposed withdrawals, SBWA's consultants used a solute transport model called HST3D. Developed by the USGS, this model is widely used and accepted. For simulations using the HST3D model, SBWA used the flow field and a portion of the grid generated by its INTERSAT groundwater flow model. The HST3D simulations run by ESE utilized a cross section of the INTERSAT model grid extending through row 26 of that grid, which is the row containing the line of 9 proposed wells running on an east-west axis. Use of a cross sectional grid is an appropriate method by which to examine salt water intrusion. Upconing, to the extent that it will occur as a result of the proposed pumpage, would be greatest within the cross section containing the 9 wells. The cross section extends two miles through the wellfield to the west. As chloride concentrations in water increase, the density of the water increases. Density can retard the degree of upconing when chloride concentrations are as low as 1000-2000 parts per million and becomes significant at 3000-5000 parts per million. Failure of a model to consider density effects, when appropriate, would tend to overstate upconing. HST3D does consider density effects. SBWA's consultant ran several simulations with the HST3D model to predict changes that would occur as a result of the proposed pumpage in chloride concentrations over 7, 14 and 30 year time periods. These simulations utilized the same aquifer parameters as the INTERSAT model together with the effective porosity values derived from site specific data. Assuming a starting chloride concentration of 1000 mgl at the bottom of layer 5, the measured concentration at that level in well TM on the BCWMA site, after 30 years of pumpage at 18.8 mgd, the chloride concentrations in layer 4 would increase by only 100 mgl. The simulations for 7 years of pumpage which is the duration of the proposed permit, show that the predicted increase in chloride levels would be substantially less than 100 mgl. Other HST3D simulations were run by SBWA for a pumpage rate of 35 mgd utilizing beginning chloride concentrations of 5,000 mgl and 10,000 mgl, respectively at the bottom of layers. The results did not show any significant changes in chloride concentrations in layer 4 over and above those shown when a lower starting chloride concentration was assumed. In a circumstance where, as here, the chloride concentrations in the zone from which water is proposed to be withdrawn exceeds secondary drinking water standards (250 mgl), the SJRWMD evaluates the existing legal water uses within the area that would be impacted by the proposed use. If it is determined that the increase in chloride concentrations caused by a proposed use would detrimentally affect other existing legal users or the applicant, only then is the increase deemed to be "significant". Within the layers of the aquifer which would experience increases in chloride concentrations as a result of the proposed withdrawal, layers 4, 5 and 6, no existing users of water would be detrimentally affected. Petitioner Deseret's closest wells to the proposed wellfield are in layer 3 where chloride levels will not be affected by the proposed wellfield within the 7 year duration of the proposed permit or even beyond that period. Further, the use Deseret makes of the water from the wells in closest proximity to the proposed wellfield, pasture irrigation, can tolerate significantly higher chloride concentrations than will exist even directly beneath the wellfield in level 4 after 30 years of pumping. Use of water for public supply purposes is considered by SJRWMD to be in the public interest. Utilization of the water beneath BCWMA for public supply purposes, even with some increase in chloride concentrations in the source of the water over the life of the permit, does not on balance detrimentally affect the public interest. Two different solute transport models were done by Petitioners' consultants, one a numeric model and the other an analytical model. The numeric model done by Hartman, RANDOMWALK, does not predict changes in chloride concentrations within an aquifer, but rather tracks movement of particles. RANDOMWALK does not account for density effects. The analytical model done by Prickett for the Petitioners relies on assumptions, many of which are not met in the aquifer system at BCWMA. Those assumptions relate to uniformity of the system, for example: porosity and permeabilities, and lack of regional gradients. The solute transport models utilized by the Petitioners are less reliable for predicting water quality changes resulting from the proposed pumpage than the model utilized by the SBWA. Salt water intrusion is a dramatic increase of chloride levels in an aquifer layer. The saline water encroachment which occurs from the wellfield stress will be in the lower confining unit. There will be limited degradation in the lower part of the production zone. The wellfield will not induce significant lateral intrusion from the east. There will not be any dramatic changes in chlorides. The movement of the chlorides is confined to the locality of the wellfield. Most of the movement is vertical and is of limited increase. The proposed Bull Creek withdrawals will not aggravate any currently existing salt water intrusion problems. The reject brine water from the RO treatment plant will be disposed of in deep injection wells in Brevard County. These injection wells would deposit the brine into a receiving body of water in the Oldsmar geologic formation. The brine reject will have a total dissolved solids (TDS) concentration of approximately 7,000 mgl. The receiving water into which the brine will be injected approximates sea water, with TDS concentrations in the range of 36,000 mgl. The receiving body will obviously not be further degraded. Environmental Impacts of the Proposed Consumptive Use District staff, SBWA consultants and Osceola's consultants independently conducted onsite field investigations of the BCWMA to evaluate the vegetative communities and land uses which exist on site. Each consultant prepared a habitat map identifying the various vegetative communities found at the site. While relatively pristine, the BCWMA has been logged and grazed by cattle in the past. The impacts of man's activities have been remediated by ceasing the activity. There are few permanent incursions, such as roads, canals and buildings. The area is a very diverse landscape, with a mosaic of different types of plant communities. There are various upland and wetland habitats. The variety of wetlands are forested and non-forested, deep and shallow, open and closed. These wetlands perform important functions, including water storage and purification, aquifer recharge, flood control, and provision of food sources and habitat for wildlife, and they are "factories" for producing the materials needed by many higher organisms. The wetlands on site are structurally complex and are good habitat for macro- invertebrates and the fish and higher organisms that feed on them. A number of these wetlands are shallow, isolated wetlands. During periods of inundation, when the wetlands fill up with water and interconnect with the Bull Creek drainage system, the system exports various organisms to the wetlands. Fish that are live bearers move into isolated wetlands during periods of inundation, and they and their offspring become a source of food for birds. Fish species that lay eggs can withstand desiccation (total drying out) can survive the temporary drying of wetlands, but live bearers must repopulate during periods of inundation. The mixed wetland hardwoods on site contain a diversity of bugs, crawfish, mayflies, damsel flies, midges, and snails. Some of these are important food sources for higher organisms. The apple snail, for example, is an important food source for such birds as the limpkin and the endangered snail kite, and its eggs are food for crawfish and other organisms. The biological communities that exist in the wetlands and uplands at the site are determined by a number of factors, including the depth and duration of the hydroperiod, soils, climate, temperature, and availability of sunlight. These communities and their habitats will react to changes in light, water, temperature, and many other subtle effects, causing changes in plant diversity and structure, the areal extent of certain types of habitats and wetlands, and utilization by wildlife. Natural fluctuations in the hydroperiod also cause these changes, generally from the exterior edges of a wetland to the interior. The wetlands in the BCWMA have been able to withstand the natural drought and flood periods, or they wouldn't be there today. Periodic burning is essential to the health of ecosystems such as in the Bull Creek area. Fires reduce the prevalence of species less tolerant to fire, allow other species to strengthen their presence, return organic material to the soil, and reduce the fuel available for wild fires. Originally occurring naturally as a result of lightening strikes, prescribed burns are now undertaken by agencies such as the Division of Forestry and the Game and Fresh Water Fish Commission to replicate the beneficial functions of natural periodic burning. Fire management is used as a land management technique at BCWMA and continued fire management at the BCWMA will maintain a natural ecological setting typical of Florida. Slight variations in elevation which mark the difference between wetlands and uplands can result in utilization of the areas by different animal communities. Where different types of plant communities meet, an "ecotone" is created. Where an ecotone exists, the "edge effect" of the competition between the two communities occurs. The result of the edge effect is higher plant and animal species diversity, which is extremely important to the natural community. Some animals make specific use of the ecotone for habitat and food resources. Many amphibians, frogs in particular, live in the ecotone. Some birds will not roost in the upland forests but will roost in the edge of the forest adjacent to wetlands. Wetlands in the BCWMA are connected to the remainder of the Bull Creek system through groundwater resources. Their biological and ecological communities are also connected as the same organisms move throughout the system. Isolated wetlands also exhibit a "moving edge" effect, where changes in the surface water and water table levels cause different plants, or plants at different levels of maturity, to exist in the wetland and its perimeter. This increases the productivity of the wetland by making it attractive to a wider variety of plant and animal species. If the expansion and contraction of isolated wetlands is reduced by lowered water levels, the smaller wetlands would exhibit a reduced edge effect, and the cumulative effect of this reduction over time would disrupt the functioning of the wetland-upland system. Isolated wetland systems are more sensitive to drawdowns in the surficial aquifer than connected wetland systems because the drainage area contributing water to the wetland system is smaller. Isolated herbaceous wetland communities are the most sensitive of the vegetative communities on BCWMA to drawdowns in the surficial aquifer. The surficial aquifer fluctuates naturally as much as five feet annually. Rainfall is the primary source of water for the surficial aquifer. Water levels in the surficial aquifer respond very quickly to rainfall events. Hydroperiods of the wetland systems in the BCWMA respond to rainfall and surficial aquifer levels. The wetland hydroperiods vary from year to year, and wetland ecosystems have adopted to those annual changes. But a groundwater withdrawal from the surficial aquifer in the Bull Creek area would cause a corresponding lowering of the surface water level, since the wetlands are not "perched", or separated from the aquifer by a confining layer. A drawdown would lower water levels throughout the hydroperiod, under both high water and low water conditions, with a more pronounced effect during the dry season and drought periods. Some of the over twenty threatened and endangered plant species present at Bull Creek grow in shallow, marginally wet areas. Changes in even a few inches of groundwater would cause these plant species to be retarded in growth, and their abundance would decrease or they would die out at the site. Many of the wetlands are shallow, broad, sloping areas, and groundwater elevation changes of just a few inches will cause changes in the areal extent of these wetlands. Even the .14 foot drawdown predicted by SBWA's modeling would affect shallow inundated or saturated systems by changing the moisture level at the surface, particularly by affecting the lowest water levels. Changes in the vegetative composition of wetlands will affect the macro-invertebrate characteristics of a site. For example, as water levels change, the density of the vegetation (in terms of number of plant stems per acre) can decrease, leaving fewer places for the macro-invertebrates to hide, and the populations of macro-invertebrates will decrease through predation. As food sources, habitat and breeding grounds decrease, those animal species that can relocate will attempt to do so. Relocation can adversely affect the survival of the species; for example, a wood stork unable to find a particular food upon which it is dependent at a particular interval in its life cycle may abandon its nest and its young. Animals that attempt to relocate may find that there is not a suitable similar habitat available, making their attempt to adjust to the change in their environment unsuccessful. The proposed use will not significantly affect the stages or vegetation of the upland communities at the BCWMA because they are not as dependent on saturation or inundation as a wetland community. Forested wetland systems, be they isolated or connected, will not be influenced by a drawdown of the magnitude predicted by SBWA for the surficial aquifer. Forested systems have deep root zones and the canopy provides shading to the strata below. Forested systems are able to tolerate natural changes in hydrology. The SBWA assessment does not offer any detailed cataloguing of the plant and animal communities on site, or a description of how the systems operate or interface with each other. It does not provide sufficient information to be able to assess the impacts of the proposed wellfield on these systems. There was insufficient information presented by the applicant to conclude that the environmental harm to be caused by operation of a wellfield at the BCWMA has been reduced to an acceptable level. The applicant relied on the fact that drawdowns in the surficial aquifer will be minimal, without fully considering the impact of those minimal drawdowns on a fragile wetland ecosystem during a dry period. Water Demand The SBWA was created by special act in 1983 as a dependent special district for the purpose of developing regional water supplies and transmission of water to water distribution systems. In its existence so far, its labors have been in the former, and none in the latter category. Efforts to develop a regional water supply have been frustrated by litigation, by reluctance of local public systems to give up their authority and by delays in pursuing and processing CUP applications, two of which are still pending, in addition to the instant application. The City of Melbourne's public water system provides water to Melbourne, Palm Bay and West Melbourne, and to some unincorporated areas surrounding Melbourne. It also supplies water to the area called south beaches, comprised of the Brevard County area south of Patrick Air Force Base, including Satellite Beach, Melbourne Beach, Indiatlantic and Indian Harbor Beach. The current water supply is Lake Washington, which is part of the chain of lakes on the St. Johns River. The city of Melbourne was granted a CUP on January 15, 1991, for withdrawals from Lake Washington, ranging from 27.15 million gallons maximum daily withdrawals in 1991 to 21.7 million gallons maximum daily withdrawals in 1998. In addition, Melbourne has planned a new facility and has the CUP to withdraw 8.13 million gallons a day from the Floridan Aquifer commencing in 1993. After reverse osmosis treatment, the groundwater withdrawal will yield 6.5 million gallons a day finished water, making up the difference from reduced withdrawals from Lake Washington. Approximately 56 potable water systems have been identified by SBWA in South Brevard, south of the Pineda Causeway. Almost all are small private systems. Besides Melbourne, the other major water supplier in the area is General Development Utilities (GDU), serving the City of Palm Bay. GDU's CUP expires in 1993 with an average daily withdrawal of 6.5 mgd and maximum daily withdrawal of 8.5 mgd. It has ample capacity until 1996, and beyond to the year 2000, if an additional Department of Environmental Regulation capacity rating is obtained. The total capacity of the two major existing facilities is approximately 30 mgd and total existing consumptive use quantities (including existing CUPs with expiration dates varying from 1993 to 1998) approach 40 mgd. The current SBWA water master plan assumes that existing sources need replacing. More specifically, SBWA, if this CUP is granted, seeks to replace Lake Washington as the primary source of water in the area with the groundwater obtained from the BCWMA wellfield. An agreement between the City of Melbourne and SBWA provides that the City will initially purchase 8 mgd, plus all future needs of water from the SBWA. This 8 mgd would be used by Melbourne prior to using its 6.5 mgd finished water from the RO facility, and the RO water would be used prior to withdrawals from Lake Washington. The agreement, dated January 9, 1991, acknowledges the need for, and specifically authorizes improvements to Melbourne's Lake Washington Water Treatment Plant, including the conversion of the existing high service pumping station to a low service pumping station with average daily capacity of 20 mgd and maximum capacity of 25 mgd. (SBWA Ex. 49) GDU is a private utility and currently is outside the jurisdiction of the SBWA. General Development Corporation is in receivership and the City of Palm Bay is negotiating for purchase of the utility. If the purchase is successful, the supply will become publicly owned and subject to the jurisdiction of the SBWA. The City of Palm Bay is not bound to purchase GDU at any price, and the requirement that it would shut down its newly purchased facility to receive water from SBWA is a disincentive to the acquisition. In the meantime, GDU has no incentive to reduce CUP capacity and devalue its facility. GDU's service has been uninterrupted and reliable. Contamination to the surface aquifer utilized by GDU has been successfully treated. Although septic tanks proliferate in Palm Bay, their location, as well as the presence of confining layers in the surficial aquifer, reduce the susceptibility of GDU wells to contamination from septic tanks. The applicant's concerns about unreliability and safety of Lake Washington as a continued water source are unsubstantiated by the weight of evidence in this proceeding. Surface water facilities have been used in Florida since before the turn of the century and no major facility has ever been off-line one day due to raw water contamination. Nor has any major Florida surface water plant ever been sabotaged. There is a greater chance in Florida of problems with pipeline failures, and the miles of pipes planned to transmit ground water from Bull Creek east to SBWA consumers increase the chances of those problems. Recently, the SJRWMD Upper Basin Project has significantly improved the water quality and quantity in Lake Washington through restoration of marshlands in the upper basin and capping flowing wells. Restored marsh areas will allow for additional removal of nutrients and provide an additional storage to the Lake Washington/Upper Basin system, significantly improving safe yield quantities. Comparisons of concentrations of raw water chlorides and total dissolved solids for the drought years of 1989 and 1990, show significant reductions for the latter time frame. Recent evaluations indicate that Lake Washington would be acceptable in terms of chlorides and TDS concentrations for a 35 mgd withdrawal, even during 50 and 100 year droughts. Water quality improvements to Lake Washington can be directly related to the Upper Basin project. Trihalomethanes are regulated by the Safe Drinking Water Act. They are produced by the disinfection process of treating raw water with chlorines, and they are carcinogenic. A previously experienced problem at the Melbourne plant has been corrected with operational changes. As recently as 1988, an internal staff report by SJRWMD staff provided: Lake Washington has been a reliable source of public water supply since 1960 and can remain so in the future with the continuation of sound basin planning and watershed management by the St. John's river Water Management District. The quality of the raw water from Lake Washington is subject to annual and seasonal variations that make the treatment process more difficult, and the quality of the delivered water less consistent, than would be the case with a groundwater supply. A supplemental water source near Lake Washington would improve the quality of the water delivered to the users, would increase the total volume that could be taken from the lake in times of stress, and would provide a reliable alternative in case of emergency. The upper zone of the Floridan Aquifer within south Brevard County has the potential to supply a significant portion of the area's future water needs with existing low-pressure, reverse osmosis technology at a cost that is comparable to current supplies.
Recommendation Based on the foregoing, it is hereby, recommended that the SBWA application for CUP be denied. RECOMMENDED this 12th day of March, 1992, in Tallahassee, Leon County, Florida. MARY CLARK 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 12th day of March, 1992. APPENDIX TO RECOMMENDED ORDER, CASE NOS. 91-1779, 91-1780, & 91-1781 The following constitute disposition of the findings of fact proposed by each party. Petitioner, Osceola County These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-5, 7-8, 14, 21-22, 24-25, 27-28, 30, 32, 35, 62-65, 73, 104, 113, 116-125, 127, 129-130, 132-138, 140, 154, 157-158, 164, 167-168, 183, 186, 189, 191-195, 197-200, 202-204, 209, 212. These findings are rejected as contrary to or unsupported by the weight of evidence: 37-38, 48, 51, 53, 56, 66, 79-81, 84-90, 92-94, 102-103, 105-107, 110-112, 115, 128, 171-172, 212(d), (f) and (g), 213-214. These findings are rejected as cumulative, unnecessary or irrelevant: 6, 9- 13, 15-20, 23, 26, 29, 31, 33-34, 36, 39-47, 49-50, 52, 54-55, 57-61, 67-72, 74- 78, 82-83, 91, 95-101, 108-109, 114, 126, 131, 139, 141-153, 155-156, 159-163, 165-166, 169-170, 173-182, 184-185, 190, 196, 201, 205-208, 210-211, 212(e), 215. Petitioners, Triple E, Triple N, East Central Florida Services, Inc., and Deseret These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-6, 8-9, 16-20, 22-25, 27-28, 30-31, 50- 56, 59-60. These findings are rejected as contrary to or unsupported by the weight of evidence: 7, 12, 32, 34-37, 40, 42, 44, 48, 49, 58. These findings are rejected as cumulative, unnecessary or irrelevant: 10- 11, 13-15, 21, 26, 29, 33, 38-39, 41, 43, 45-47, 57, 61-63. Respondent, South Brevard Water Authority These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-6, 9-11, 13, 16-24, 28, 30-34, 36, 38, 46-48, 61, 64, 70, 72-74, 90-91, 94-98, 105-108, 110-111, 113, 115-116, 121, 126-129, 133, 149, 152, 157, 169, 179, 181-190, 192-194. These findings are rejected as contrary to or unsupported by the weight of evidence: 41, 130-132, 156, 158, 167, 174, 177. These findings are rejected as cumulative, unnecessary or irrelevant: 7-8, 12, 14-15, 25-27, 29, 35, 37, 39-40, 42-45, 49-60, 62-63, 65-69, 71, 75-89, 92- 93, 100-104, 109, 112, 114, 117-120, 122-125, 134-148, 150-151, 153-155, 159- 166, 168, 170-173, 175-176, 178, 180, 191. Respondent, St. Johns River Water Management District These findings have been adopted in full or in substantial part in the recommended order submitted herewith: 1-8, 10-22, 24-36, 38-44, 47-62, 64-88, 90, 92-116, 118-122, 124-130, 132-142, 144-151, 159-160, 164, 166-167, 169, 171, 174-175, 177, 193-196, 198, 202, 206. These findings are rejected as contrary to or unsupported by the weight of evidence: 131 (the conclusion), 153-154, 156-157, 161-162, 197, 204, 207. These findings are rejected as cumulative, unnecessary or irrelevant: 9, 23, 37, 45-46, 63, 89, 91, 117, 123, 143, 150, 152, 155, 158, 163, 165, 168, 170, 172-173, 176, 178-192, 199-201, 203, 208-210. COPIES FURNISHED: Segundo J. Fernandez, Esquire Scott Shirley, Esquire OERTEL, HOFFMAN, FERNANDEZ & COLE, P.A. Post Office Box 6507 Tallahassee, FL 32314-6507 Douglas P. Manson, Esquire BLAIN & CONE, P.A. 202 Madison Street Tampa, FL 33602 Clifton A. McClelland, Esquire POTTER, McCLELLAND, MARKS & HEALY, P.A. Post Office Box 2523 Melbourne, FL 32902-2523 Wayne Flowers, Esquire Nancy B. Barnard, Esquire St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429 Neal D. Bowen, County Attorney Osceola County Room 117 17 South Vernon Avenue Kissimmee, FL 32741 Carol Browner, Secretary Dept. of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400 Daniel H. Thompson, General Counsel Dept. of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400
The Issue The issues determined in this proceeding are whether Respondent engaged in construction contracting without a license as alleged in the Amended Administrative Complaint; and, if so, the appropriate penalty.
Findings Of Fact Parties Petitioner is the state agency responsible for regulating the practice of construction contracting pursuant to section 20.165 and chapters 455 and 489, Florida Statutes. Petitioner has jurisdiction over the unlicensed practice of construction contracting pursuant to sections 455.227, 455.228, and 489.13. At all times material to this matter, Respondent was the owner of Advanced Connections, LLC. Neither he nor his company is licensed, registered, or certified to perform construction contracting services in Florida. Respondent holds only certification to perform backflow preventer testing. At the heart of this case is whether Respondent may perform backflow preventer repair without a license, certification, or registration. Facts Related to Work Performed It is undisputed that Respondent performed repair of backflow preventers for customers in Tallahassee, Florida. On July 25, 2014, Respondent performed a backflow prevention assembly test on two existing backflow preventers at Old Enrichment Center located at 2344 Lake Bradford Road, Tallahassee, Florida 32301. Respondent provided an invoice to Old Enrichment Center following the backflow test, which described the work performed as follows: “I was able to repair both units and they are Functioning [sic] properly. I had to replace one additional part on, AS #10896, the #2 check cage was cracked. Thank you For [sic] your business. Don’t forget to cover the backflows.” The invoice reflected that Respondent was compensated $343.00 for the worked performed and materials. On August 20, 2014, Respondent performed a backflow test on an existing backflow preventer for Li-Ping Zhang at a property located at 2765 West Hannon Hill Drive, Tallahassee, Florida 32309. Respondent provided an invoice to the customer describing the outcome of the test, and he provided an estimate for repair as follows: Invoice: Thank For this opportunity to serve you. The unit is failing. The #1 check valve is leaking across it. That means it is not holding pressure. The Manufacture of flowmatic no longer makes parts for your unit. But my supplier does have a repair kit available. Due to the Fact are no longer made for your device it may be better to have the unit replaced with a Wilkins 975-XL. Please See Quote * * * Quote for repair: Part: Complete Rubber Kit-$30.00 Labor: This unit may not be repairable due to the fact that there is a limited supply of parts. If there is damage to the #1 Check. I will not be able to repair the unit. If that happens I can return the parts but a labor charge would still remain. Please call with any questions. Thank you. (Quoted text from invoice without correction of grammar.) Respondent ultimately performed the repair on August 25, 2014. The invoice issued to Li-Ping Zhang reflected service provided as “[t]he repair was a success. The unit is Passing [sic]. Paid Cash $115.00 8.25.14 — signed Ian.” Both invoices include the Respondent’s company name, Advanced Connections, LLC. There was no evidence presented of financial or property harm caused by Respondent’s actions. On or about February 2, 2015, Petitioner received a complaint from City of Tallahassee filed against Respondent for his repair of backflow preventers in Tallahassee, Florida. Petitioner commenced an investigation into Respondent’s actions through its unlicensed activity investigation unit. At the conclusion of the investigation, Petitioner filed an Administrative Complaint alleging Respondent engaged in construction contracting without a license. Respondent disagrees with Petitioner and argues that he is eligible for an exemption under section 489.103(9), commonly known as the “handyman” exemption. Life-Safety Matter Respondent’s eligibility for the exemption hinges upon whether repair of a backflow preventer is considered a life- safety matter. The Florida Building Code provides minimum standards for building construction to “safeguard the public health, safety and general welfare.” See § 101.3, Florida Building Code, Building. The Florida Building Code, Plumbing, applies to “the installation, alteration, repair and replacement of plumbing systems, including fixtures, fittings and appurtenances where connected to a water or sewage system . . . .” See § 101.4.3, Florida Building Code, Building. The plumbing chapter of the Florida Building Code defines a backflow preventer as a device or means to prevent backflow of water from flowing from one system into the potable water system.2/ A potable water supply system shall be maintained in such a manner so as to prevent contamination from non-potable liquids, solids, or gases being introduced into the potable water supply through cross-connections or any other piping connections to the system. § 608.1 Building Code, Plumbing. To further explain the purpose of backflow preventers, Petitioner offered Frank Hagen as a plumbing expert. Mr. Hagen, who has 42 years of plumbing experience, has been licensed in Florida since 1981 and is also licensed in Georgia. He holds a certification in backflow preventer testing (issued by the University of Florida TREEO Center) and backflow preventer repair. Mr. Hagen has regularly conducted on-the-job plumbing training for 36 years. Mr. Hagen was accepted as a plumbing expert. Mr. Hagen testified that a backflow preventer is a life-safety device. He explained that this reference is accepted throughout the plumbing industry because the backflow preventer protects water systems by preventing chemicals and poisons from entering the public water system. Mr. Hagen provided examples of potential outcomes if a backflow preventer fails (e.g., three children died as a result of drinking water from a water hose where poison in the sprinkler system contaminated the water). Mr. Hagen also testified that only a licensed plumber is authorized to perform backflow repairs. Mr. Hagen’s testimony is credible. John Sowerby, P.E., a licensed professional engineer for 35 years, who previously worked in the Department of Environmental Protection’s (DEP) Source of Drinking and Water Program, also testified regarding the nature of backflow preventers. He testified that backflow preventers protect public health because they prevent contamination of potable water systems (i.e., water that is satisfactory for human consumption). Mr. Sowerby’s testimony is also found to be credible. Respondent’s testimony that a backflow preventer is not a life-safety fixture, is not supported by the evidence. Respondent testified that backflow preventers are “plumbing fixtures” that are installed between the public water supply line and the private water supply line. Respondent also testified that if a backflow preventer fails, it could cause contamination of the public water supply and public health would be at risk. More importantly, the applicable building codes and the testimony of Mr. Hagen and Mr. Sowerby establish that backflow preventers prevent contamination of public water supply and protect public health. Given that backflow preventers safeguard public health by protecting the public water supply, they involve life-safety matters. The Department has incurred investigative costs in the amount of $415.95 related to this matter. Ultimate Findings of Fact Respondent’s repair of a backflow preventer on a water service line is a life-safety matter and as a result, Respondent is not eligible for an exemption under section 489.103(9). The evidence is clear and convincing that Respondent’s repair of a backflow preventer at the two properties referenced herein constituted the practice of construction contracting without a license. As a result, Respondent is guilty of unlicensed contracting, as charged in Counts I and II of the Amended Administrative Complaint.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Business and Professional Regulation issue a final order that: Finds Respondent guilty of unlicensed contracting in violation of section 489.13(1), as alleged in Counts I and II of the Amended Administrative Complaint; Imposes an administrative fine of $6,000 ($3,000 for each count); and Requires Mr. Tuttle to pay the Department’s investigative costs of $415.95. DONE AND ENTERED this 26th day of October, 2016, in Tallahassee, Leon County, Florida. S YOLONDA Y. GREEN Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 26th day of October, 2016.
