The Issue The issue is whether Respondent's water use permit should be revoked for nonuse of the permit for a period of two years or more.
Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Background The District is a state agency charged with the responsibility of issuing water use permits under Chapter 373, Florida Statutes, and Florida Administrative Code Chapter 40B- 2 for the geographic area under its statutory jurisdiction. Alachua County is within that geographic jurisdiction. Respondent is a Florida corporation with offices at 700 Northwest Cheeota Avenue, High Springs, in northern Alachua County. It owns approximately 700 acres in High Springs (west of Interstate Highway 75) on which it operates a church retreat and summer camping and recreational facility known as Camp Kulaqua. The property surrounds, and is contiguous to, Hornsby Spring, a first-order magnitude spring (having a flow rate of 100 CFS or greater) which, under normal conditions, discharges into the nearby Santa Fe River. Hornsby Spring is one of 296 documented springs within the District's jurisdiction. After receiving an overture from a representative of a private water bottling company, on September 28, 1999, Respondent filed an application for a General Water Use Permit in Township 7 South, Range 17 East, Section 26, in High Springs. In its application, Respondent represented that it desired a daily allocation of 2,000,000 gallons; that it intended to install two 12-inch wells, each having a capacity of 1,400 gallons per minute, just east of, and upgradient from, Hornsby Spring; and that all water withdrawals would be used in conjunction with a privately-owned commercial spring water bottling facility to be located on its property. The application also represented that the facility would employ 36 persons and operate 168 hours per week. The application was reviewed by a former District hydrogeologist, William H. Kirk. During the review process, and in response to Mr. Kirk's request for more information, Respondent provided a comparison of the requested allocation with the overall flow of Hornsby Spring. This was because Mr. Kirk was concerned that the requested allocation was "a bit high," and he wanted to ensure that the issuance of the permit would not cause harm to, or adversely affect, the water resources. Under a professional guideline that Mr. Kirk used, if the applicant could show that the cumulative amount being withdrawn was to be less than ten percent of what the available data showed to be the mean spring flow, the District would consider it to be "an acceptable impact." Notwithstanding Mr. Kirk's use of this guideline, the District points out that there is no District rule or policy sanctioning the ten percent rule, and at hearing it denied that this standard is used by the District in assessing water use applications. Further, the Permit itself does not refer to a relationship between spring flow and the size of the allocation. Even so, this analysis was considered by Mr. Kirk in determining whether Respondent had given reasonable assurance that the spring would not be impacted. In its response to the request for additional information, Respondent reduced its requested allocation to 750,000 gallons per day and indicated that if a bottling plant were to be constructed on its property, approximately 700,000 gallons of the total allocation would be consumed in "bulk transfer and bottling," with the remainder for camp use. More specifically, Respondent indicated that it would allocate 490,000 gallons per day for bulk transport, 210,000 gallons per day for spring bottling water, and 50,000 gallons per day for incidental uses at its property. By reducing the allocation from 2,000,000 gallons per day to 750,000 gallons per day, Respondent's requested average daily allocation represented only 0.4 percent of the average daily spring flow as measured over the last 28 years. The reduced allocation satisfied Mr. Kirk's concern that Respondent demonstrate a reasonable demand and a reasonable need for that allocation, and he recommended approval of the application.2 On February 25, 2000, the District approved the application and issued Water Use Permit No. 2-99-00130 (Permit).3 The Permit authorizes an average daily withdrawal of 0.7500 million gallons per day (750,000 gallons per day) or a maximum daily withdrawal and use of 0.7500 million gallons per day with an annual allocation not to exceed 273.750 million gallons (273,750,000 gallons) per calendar year in conjunction with the operation of a privately-owned water bottling plant. The Permit expires on February 25, 2020. After the Permit was issued, under the regulatory process in place, Respondent was required first to obtain a permit for a temporary test well which would be used to collect information concerning the site of the proposed activity, and to then file an application for permits authorizing the construction and operation of the two 12-inch production wells. The Permit contains a number of conditions, two of which require a brief comment. First, Condition No. 2 provides that "[t]his permit is classified as unconfined [F]loridan aquifer for privately owned bottled water plant." This means that all water withdrawals must be made from the unconfined Floridan aquifer, as opposed to the spring head of Hornsby Spring. (Respondent's proposed siting of its two production wells 660 yards east of the spring is consistent with this provision.) Second, Condition No. 4 provides that "[t]he permittee shall submit daily pumpage records on a monthly basis to the [District]." Pumpage reports are filed by permittees so that the District can determine whether the permit is actually being used, and if so, to ensure that the amount of water being withdrawn under the permit does not exceed the authorized allocation. As it turned out, pumpage reports were never filed by Respondent. (However, the record shows that the District has never strictly enforced this requirement for any permittee.) In late 2002, the District staff undertook a review of the nine water bottling permit holders within its jurisdiction, including Respondent. That category of permit holders was selected for review because of the small number of permits and the limited resources of the District staff. (In all, the District has probably issued several thousand permits to other types of users.) On February 4, 2003, the District served its Complaint under the authority of Sections 120.60 and 373.243, Florida Statutes, and Florida Administrative Code Rule 40B-2.341. As grounds for revoking the permit, the District alleged that there was "non-use of the water supply allowed by the permit for a period of two (2) years or more." Although Respondent contends that it should have been given an opportunity to correct the nonuse allegation before the Complaint was issued, nothing in the Administrative Procedure Act or District rules requires that this be done. Until the issuance of the Complaint against Respondent in early 2003, and similar Complaints against eight other permit holders at the same time, the District had never invoked this statutory provision.4 There is no evidence to support Respondent's contention that the Complaints were issued for "purely political reasons." On March 4, 2003, Respondent requested a formal hearing challenging the District's proposed action. In the parties' Pre-Hearing Stipulation, the issues have been broadly described as follows: whether Section 373.243(4), Florida Statutes, is to be strictly or liberally construed; whether Respondent's nonuse is based upon extreme hardship for reasons beyond its control; and whether the District is equitably estopped from permit revocation. (According to the District, even if the Permit is revoked, such revocation is without prejudice to Respondent reapplying for, and receiving, another permit so long as it meets all applicable requirements.) Equitable Estoppel Respondent first contends that the District is estopped from revoking its Permit on the theory that, under the circumstances here, the doctrine of equitable estoppel applies. For that doctrine to apply, however, Respondent must show that the District made a representation as to a material fact that is contrary to a later asserted position; that Respondent relied upon that representation; and that the District then changed its position in a manner that was detrimental to Respondent. See, e.g., Salz v. Dep't of Admin., Div. of Retirement, 432 So. 2d 1376, 1378 (Fla. 3d DCA 1983). The District issued Respondent's Permit on the condition that Respondent operate in conformity with all pertinent statutes and regulations. This finding is consistent with language on the face of the Permit, which states that the Permit "may be permanently or temporarily revoked, in whole or in part, for the violation of the conditions of the permit or for the violation of any provision of the Water Resources Act and regulations thereunder." Respondent relied on the District's representation that it could use the Permit so long as it complied with all statutes and regulations. In reliance on that representation, in addition to staff time, after its Permit was issued, Respondent expended "somewhere around" $70,000.00 to $74,000.00 for conducting water quality testing; sending cave divers underground to ascertain the correct location of the portion of the aquifer on which to place its production wells; drilling a 6-inch test well in August 2000; obtaining the City of High Springs' approval in March 2000 for industrial zoning on a 10-acre tract of land on which to site a "water plant"; and engaging the services of a professional who assisted Respondent in "seeking out businesses and getting the right qualifications of the spring water to make sure that it was a marketable water." The District has never asserted anything different from its original position: that if Petitioner complied with all statutes and rules, it could continue to lawfully make water withdrawals under its Permit. The issuance of the Complaint did not represent a change in the District's position. Because a change in position in a manner that was detrimental to Respondent did not occur, the necessary elements to invoke the doctrine of equitable estoppel are not present. Was the Permit Used? A preliminary review by District staff indicated that Respondent had never filed the daily pumpage reports on a monthly basis and had never requested permits authorizing the construction of the two 12-inch production wells. These preliminary observations were confirmed at final hearing, along with the fact that Respondent has never entered into an agreement with a water bottling company (although draft agreements were once prepared); that Respondent has never constructed a water bottling facility; and that no operations were ever conducted under the Permit. Therefore, the evidence supports a finding that Respondent did not use its Permit for the two-year period after it was issued, as alleged in the Complaint. Respondent's contention that the evidence fails to support this finding belies the evidence of record. In an effort to show that it actually used the Permit, Respondent points out that in August 2000 it applied for, and received a permit to construct, an unmetered 6-inch test well in association with its General Water Use Permit. (Respondent sometimes erroneously refers to the test well as a test production well. This is incorrect as the well is a test well, and not a production well.) After the test well was installed, at some point Respondent says it began withdrawing approximately 50,000 gallons per day of water from that well for incidental uses associated with the operation of Camp Kulaqua.5 These withdrawals were made on the assumption that the test well permit fell under the broad umbrella of the General Water Use Permit. (Respondent also has a permitted 6- inch diameter well and an unregulated 4-inch well on its premises, both of which are used for water supply needs at Camp Kulaqua.) It is true, as Respondent asserts, that its Permit authorized incidental withdrawals of up to 50,000 gallons per day for unspecified uses at Camp Kulaqua. However, these withdrawals are authorized under the General Water Use Permit and not the test well permit. The two permits are separate and distinct. On the one hand, a test well is intended to be temporary in nature and used only for the purpose of test well development and collecting information regarding the height of the aquifer and water quality at the site of the proposed activity. Conversely, withdrawals for any other purpose, even incidental, must be made from the production wells, which are only authorized by the General Water Use Permit. Before a test well can be used for normal consumptive purposes, the permit holder must seek a modification of the permit to include it as a part of its general water use permit. Here, no such modification was sought by Respondent, and no authorization was given by the District. Therefore, Respondent's incidental water uses associated with its test well cannot be counted as "uses" for the purpose of complying with the use requirement in Section 373.243(4), Florida Statutes. In light of the District's credible assertion to the contrary, Respondent's contention that it is common practice to lawfully withdraw water from a test well for incidental consumptive purposes has been rejected. (It is noted, however, that the District has not charged Respondent with violating the terms of its test well permit.) Extreme Hardship Under Section 373.243, Florida Statutes (which was enacted in 1972), the District is authorized to revoke a water use permit "for nonuse of the water supply allowed by the permit for a period of 2 years." However, if the user "can prove that his or her nonuse was due to extreme hardship caused by factors beyond the user's control," revocation of the permit is not warranted. The phrase "extreme hardship caused by factors beyond the user's control" is not defined by statute or rule. In the context of this case, however, the District considers an extreme hardship to occur under two scenarios. First, if the aquifer level has dropped so low due to drought conditions that a permit holder cannot access the water through its well, its nonuse is excusable. Alternatively, if an emergency order has been issued by the District directing permit holders (including Respondent) to stop pumping due to certain conditions, an extreme hardship has occurred. (Presumably, a severe water shortage would precipitate such an order.) In this case, the District issued a water shortage advisory, but not an emergency order, due to a "severe drought," indicating that users could still pump water, but were encouraged to voluntarily reduce their usage. This advisory remained in effect from the summer of 1998 until the spring of 2003, when a severe drought ended. However, no emergency order was ever issued by the District. Respondent contends that its nonuse was due to an extreme hardship caused by factors beyond its control. More specifically, it argues that a severe drought occurred in Alachua County during the years 1998-2003, and that under these conditions, federal regulations prevented it from withdrawing water for bottling purposes, which was the primary purpose for securing a permit. Further, even if it had withdrawn water during these drought conditions, such withdrawals could have adversely impacted Hornsby Spring and constituted a violation of a District requirement that water resources not be adversely impacted. Because an investment of several hundred thousand dollars was required to drill and install the two production wells, Respondent contends it was not financially prudent to make that type of investment and begin operations until normal spring conditions returned. These contentions are discussed in greater detail below. Around September 7, 1999, a representative of a water bottling company first approached Respondent about the possibility of the two jointly operating a water bottling plant and/or transporting water in bulk from Respondent's property. Prompted by this interest, less than three weeks later Respondent filed its application for a water use permit (although at that time it did not mention on the application that off-site bulk transfers would occur), and a permit was eventually issued in February 2000. Later, and through a professional firm it employed, Respondent had discussions with representatives of several bottling companies, including Great Springs Waters of America (Great Springs) and Perrier Group of America. Apparently, these more serious discussions with a potential suitor did not take place until either late 2000 or the spring of 2001. Periodic measurements taken by District staff at Hornsby Spring reflected natural drought conditions from April 2000 to April 2003. As noted earlier, this was the product of a "severe drought" which took place between the summer of 1998 and the spring of 2003; the drought was one of a magnitude that occurs only once in every 50 to 100 years. During the years 2000 through 2002, the spring had zero flow or was barely flowing much of the time.6 Had Respondent pumped water during 20 out of the 24 months after the Permit was issued, it could have potentially violated the requirement that it not harm Hornsby Spring. This fact is acknowleged by a District witness who agreed that if the "spring is not flowing, . . . [pumping] would have an [adverse] impact." Even as late as October 2003, the spring had tannic discoloration caused by the lengthy drought conditions. The parties agree, however, that there is no water shortage in the District at the present time. To illustrate the difficulty that it experienced in obtaining a joint venture partner for water bottling purposes, Respondent established that in the spring of 2001, a Great Springs representative visited the site when the spring was "barely flowing." For obvious reasons, Respondent could not "bring a party there who would want to enter into a business [agreement]" under those conditions. These same conditions remained in effect during most of the two year period. The District points out, however, that even though the spring was low or barely flowing, so long as the aquifer itself was not too low, Respondent could still withdraw water from the aquifer, since Condition 2 of the Permit authorizes withdrawals from the aquifer, and not the spring. The reason for this apparent anomaly is that when a spring ceases to flow, the aquifer has simply dropped below the level of the spring vent; even under these circumstances, however, there may still be a substantial quantity of water in the aquifer available for pumping. Assuming that it could still lawfully pump water when the spring was dry or barely flowing without causing adverse impacts to the spring, Respondent was still subject to federal regulations which govern the bottling of spring water. See Title 21, Part 165, C.F.R. For spring water to be marketed as bottled "spring water," 21 C.F.R. § 165.119(2)(vi) requires that the water "be collected only at the spring or through a bore hole tapping the underground formation feeding the spring." This means that the bore hole had to be physically connected with the cave system feeding Hornsby Spring or produce water of the same quality as that discharging from the spring. The regulation goes on to provide that "[i]f spring water is collected with the use of an external force [such as by a pump], water must continue to flow naturally to the surface of the earth through the spring's natural orifice." While this regulation obviously does not prohibit Respondent from pumping water, since that authority lies within the District's exclusive jurisdiction, it does provide that in order to use spring water for bottling purposes, the water must continue to flow naturally from the aquifer to the spring. If it does not, the water cannot be used for this purpose. Because Hornsby Spring had zero flow for parts of 2001 and 2002, and severely reduced flows during most of the other time during the two-year period ending February 2002, Respondent was effectively prevented by the foregoing regulation from using the water for bottling purposes. Therefore, Respondent's nonuse was due to extreme hardship caused by factors beyond its control -- a severe drought lasting throughout the two-year period after the Permit was issued, and federal regulations which prevented it from using water for the purpose for which the Permit was issued. Thus, the nonuse is excusable.
Findings Of Fact The property has been annexed into the Acme Improvement District (Intervenor) by Special Act of the Florida Legislature. Petitioner purchased 487.7 acres of this tract from private owners in 1954. Subsequently, Petitioner purchased 653.59 acres from the Trustees of the Internal Improvement Fund of the State of Florida on or about March 4, 1960. The balance of the land constituting the property is a 224 acre hiatus tract owned by Marshall Brown with whom Petitioner has an agricultural use agreement. A parcel of Petitioner's land within the property includes a commercial lease to Malrite Corporation for siting a television antenna, consisting of 111 acres in the southeast corner of the property. This area is within the permit application. The tract is otherwise undeveloped and is currently submerged or semi- submerged during much of the year. Petitioner's development plan envisions drainage of this tract and use of the property for cultivation. The property is bounded on the north by Acme Improvement District, on the east by a subdivision called Homeland, on the west by Water Conservation Area #1, also known as the Loxahatchee Refuge, and on the south by undeveloped lands. The boundaries of the Loxahatchee Refuge actually encroach by approximately 300 feet into the property. The property development plan, which is the basis of this application, was prepared by the engineering firm Gee and Jensen. This plan calls for the creation of a 240 acre reservoir of a proposed 3 foot maximum depth. This reservoir would hold the internal stormwater runoff for subsequent agricultural irrigation. Perimeter dikes are to be constructed to prevent surface water runoff from outside areas entering the project and perimeter ditches are to be developed for the deliverance of stormwater runoff from the internal agricultural system to proposed pump stations located at the southwest corner of the development area. On the northwest corner of the proposed reservoir, the existing Acme Improvement District pump station No. 2 would be increased in capacity by 27,000 gallons per minute. Under Acme's charter and its statutory annexation of the property, the proposed reservoir and water management works would become a unit of development controlled by Acme. Under Petitioner's agreement with the hiatus tract owner, Acme would be the exclusive manager and operator of the proposed system, and the property would become an integral part of Acme's water management system. The Acme Water Improvement District is not solely an agricultural support enterprise but serves the various uses which may evolve within its boundaries. The area is currently zoned for limited residential development as well as agricultural. The television antenna facility located on the property is an example of a non-agricultural use. Petitioner's surface water management system is proposed to discharge into the Acme system, which in turn discharges offsite. Discharge into the Acme system is of a limited nature, but the system is designed to discharge for successive days under wet conditions. The design discharge is not limited to an extreme rainfall event but would probably occur during the traditional hydrologic cycle of south Florida. Under conditions which reflect actual rainfall over the past 20 years, the proposed surface water management system would have discharged 19 out of 20 years into the Water Conservation Area (Loxahatchee Refuge). In some years this discharge would have continued for approximately three months. The unrebutted testimony of expert witnesses called by Respondent established that the entire 1,393 acre tract referred to herein as "the property" is a freshwater wetland habitat. The western half is emergent marsh land, while the eastern half is forested with woody species. The wetlands on the property form a valuable wildlife habitat. Environmentally, they are in excellent condition. This area has not been adversely affected by drainage, fire or exotic species. These marshes also have good habitat diversity. The populations of aquatic invertebrates and forage fishes that are produced in these Everglades marshes are utilized by the many species of wading birds that feed in these wetlands. The proposed project will adversely affect wildlife species, including a variety of wading birds which will likely be unable to relocate. While this is undesirable from an environmental standpoint, conversion of this land would provide benefits from an agricultural standpoint, and would create additional water recreational facilities.
Recommendation From the foregoing, it is RECOMMENDED: That Respondent enter a final order denying the application. DONE and ORDERED this 30th day of November, 1983, in Tallahassee, Florida. R. T. CARPENTER 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 30th day of November, 1983.
The Issue In their Prehearing Stipulation, the parties described the nature of the controversy as follows: This matter involves a challenge to a Technical Staff Report and Recommendation made by Respon- dent's staff on a consumptive use permit applica- tion for water submitted to Respondent by Petitioner. Petitioner owns a recreational facility where water is being used. The Staff Report recommends that certain conditions be imposed upon the permit proposed to be issued to Petitioner placing limitations on the amount of water which may be consumed by Petitioner and requiring Petitioner to report on numbers of persons utilizing Respondent's facility. In that same stipulation, the parties described their respective positions as follows: Petitioner's Position: The present use of water at the Wekiva Falls Resort is a reasonable beneficial use which should not be reduced or limited by permit conditions. The standpipes through which the water flows are not wells and therefore should not be subject to any regulation by Respondent. The placement of the standpipes did not increase the flow of water but rather captured the already existing flow from natural springs which existed on the property prior to the placement of the standpipes. Petitioner feels his use does not come within the permitting power of Respondent, and that if it does, its use should be allowed to continue without any reductions in flow. Respondent's Position: After review of Petitioner's consumptive use permit application for the use of water emanating from two standpipes, one twenty-four (24) inches in diameter and the other fourteen inches in diameter, the staff of the District determined that the standpipes were wells subject to the District's regulation under Chapter 40C-2, Florida Administrative Code, and recommended approval of the permit with certain conditions requiring a reduction in flow during certain low or non-use periods. This matter arose from Petitioner's application to the District for a consumptive use permit that would allocate water to the Petitioner from water flowing from a 24-inch metal pipe and a 14-inch metal pipe for use at Petitioner's campground. The District maintains that, not only is the water that is drawn from the metal pipes and used at the campground regulated pursuant to Part II of Chapter 373, Florida Statutes, but also that the remaining water that flows from the two metal pipes and is used by Petitioner to maintain a swimming area is regulated pursuant to Part II of Chapter 373, Florida Statutes. The Petitioner has not applied for an allocation of water for maintaining the swimming area. Even though the Petitioner has not applied for such an allocation, the use of water for maintaining the swimming area has been evaluated because the Petitioner maintained that, even if the water used to maintain the swimming area is regulated pursuant to Part II of Chapter 373, Florida Statutes, the flow of water from the metal pipes should not be restricted in any fashion from the ongoing flow. Thus, the issues presented are whether the application that was applied for should be granted, whether the Petitioner has to apply for an additional allocation in order to continue using water to maintain the swimming area, and what, if an additional allocation is sought, the permit would be. In their Prehearing Stipulation the parties also agreed to the following issues of law. The Division of Administrative Hearings has jurisdiction over the subject matter of and the parties to this proceeding subject to Section 120.57(1), Florida Statutes. To the extent the standpipes located on Petitioner's property are determined to be wells, they are governed by and subject to the provisions of Chapter 373, Florida Statutes, and Chapter 40C-2, Florida Administrative Code. The procedural rules which apply to this proceeding are Chapters 40C-1, 28-5, and 22-I, Florida Administrative Code. The parties also agreed to the following as being the ultimate issues of fact which remained to be litigated. Whether the two standpipes constitute an excavation that was drilled, cored, washed, driven, dug, jetted, or otherwise constructed with the intended use of such excavation to be for the location, acquisition, development, or artificial recharge of water. Whether the continued use by Petitioner of water at pre-permit levels is a use of water in a quantity necessary for economic and efficient utilization for a purpose and in a manner which is both reasonable and consistent with the public interest. Whether the continued use of water by Petitioner at pre-permit levels would increase the danger of saline water encroachment. Whether a reduction in flow of water will result in a reduction in water quality for the uses made of the water by Petitioner. Whether a reduction in flow of water would have adverse impacts on the quality of water in the Wekiva River. Subsequent to the hearing, a transcript of the proceedings at hearing was filed on December 22, 1986, and, pursuant to request of the parties, they were allowed 30 days from that date within which to file their proposed recommended orders. Both parties filed proposed recommended orders containing proposed findings of fact and conclusions of law. The proposed recommended orders have been carefully considered and a specific ruling on each proposed finding of fact submitted by each party is contained in the Appendix which is attached to and incorporated into this Recommended Order.
Findings Of Fact Based on the stipulations of the parties, on the exhibits received in evidence, and on the testimony of the witnesses at the hearing, I make the following findings of fact. Findings based on admissions in prehearing stipulation Petitioner is a private individual who owns and does business as the Wekiva Falls Resort in Lake County, Florida. Respondent, a special taxing district created by Chapter 373, Florida Statutes, is charged with the statutory responsibility of the administration and enforcement of permitting programs pursuant to Part II of Chapter 373, Consumptive Uses of Water, specifically Sections 373.219 and 373.223, Florida Statutes, and Chapter 40C-2, Florida Administrative Code. The District is the agency affected in this proceeding. The District has assigned Petitioner's permit application, which is the subject of this proceeding, the permit number 2-069-0785AUS. On September 4, 1985, Petitioner submitted to Respondent a CUP application number 2-069-0785AUS to withdraw water from two wells, one 14 inches in diameter and the other 24 inches in diameter, located on Petitioner's property in Lake County, Florida. The water which flows from the two standpipes flows through a creek which was improved by Petitioner, said creek having as its terminus the Wekiva River. The standpipes were put in place by Petitioner or his authorized agents or employees in 1972. The area of the Wekiva River into which the creek leading from the two standpipes flows has been designated as an aquatic preserve and an "Outstanding Florida Water." On May 23, 1986, Respondent's staff gave notice of its intent to recommend approval with conditions of Petitioner's CUP application number 2-069- 0785AUS. Petitioner's Petition for Administrative Hearing was timely filed with the District. Findings based on evidence at hearing Petitioner filed his CUP application on September 4, 1985, one week in advance of the September 11, 1985, deadline for existing users of water to file applications which would establish and protect their existing user status. Petitioner's application requests an allocation of 31.7 million gallons per year (mgy) for the following uses: 8 per cent for cooling and air conditioning, 3 per cent for outside use, and 89 per cent for commercial and industrial use. Petitioner has made no application for any allocation of water for water based recreation. The Wekiva Falls Resort property consists of approximately 140 acres stretching 4800 feet in length between Wekiva River Road and the Wekiva River. The property is located along the Wekiva River between State Road 46 and the Orange County, Florida, line. Seminole County, Florida, is on the opposite side of the Wekiva River from the subject property. Petitioner purchased the subject property in 1968. At that time it was a heavily overgrown rural tract. Petitioner observed a stream which came under Wekiva River Road, passing through seven culverts, and running the length of the property to the Wekiva River. This stream carries runoff from Petitioner's property as well as runoff from areas west of the property on the opposite side of Wekiva River Road. At a point approximately midway between the Wekiva River and Wekiva River Road, along the stream, a depressional area was located by Petitioner, through which the stream flowed. Petitioner observed that more water was flowing downstream from the depressional area than upstream. Petitioner's property is located in an area of natural artesian flow where springs or seeps are not uncommon. Because the area in which the subject property is located is one of natural artestian flow, it is likely that a surficial seep of water existed in the depressional area which generated a flow of water. None of the available geological or hydrogeological information or data would indicate the existence of a spring or springs on this site prior to the drilling undertaken by Petitioner. At the time the first well was drilled by Dick Joyce Well Drilling, Inc., no spring was observed by the driller. Further, in conversations with the Executive Director of the District in 1974, no mention was made by the Petitioner of the existence of a spring or springs at the site prior to drilling. On July 17, 1969, Petitioner measured the stream flow and calculated same to be 23.97 cubic feet per second. The methodology utilized by Petitioner in measuring the stream flow in its natural state was an accepted methodology. However, this measurement did not discriminate between the water flowing into the depressional area from the stream carrying runoff from the lands upstream of the depressional area and the water originating from surficial seeps in the depressional area. Thus, this amount cannot be utilized or relied upon as a measurement of the amount of water emanating from seeps in the depressional area before drilling was undertaken by Petitioner. Nevertheless, other evidence indicates that the total volume of water flowing from Petitioner's property into the Wekiva River was probably substantially the same both before and after the installation of the two wells on Petitioner's property. In any event, the installation of Petitioner's wells does not appear to have increased the flow of the Wekiva River downstream of where Wekiva Canoe Creek discharges. In undertaking the development of his property as a resort/campground/recreational vehicle facility, Petitioner dug out the depressional area and used a dragline to open up the creek from the depressional area downstream to the Wekiva River. At a point approximately 200 feet west of the Wekiva River, Petitioner dredged a wide area to construct a marina with access through the creek to the Wekiva River. In an effort to obtain a controlled flow of water, Petitioner contracted Dick Joyce of Dick Joyce Well Drilling Inc. to drill a well fourteen inches in diameter at a site along the bank of the depressional area designated by Petitioner. The well was drilled by Joyce in August of 1972. The well was drilled using a cable rig to a depth of 107 feet, with casing being driven to a depth of 58 feet. The drilling procedure excavated a hole in the ground, penetrated rock, and resulted in the flow of ground water to land surface. The top of the 14-inch well extends 4 to 5 feet above land surface. In a further effort to obtain a controlled flow of water, Petitioner subsequently contracted Central Florida Drillers to drill a second well, twenty- four (24) inches in diameter. This well was drilled in 1973 along the bank of the depressional area, at a spot identified by Petitioner, in the same general vicinity as the previously drilled 14-inch well. The well was also drilled using a cable rig to a depth of 120 feet with casing being driven to a depth of 84.7 feet. The drilling procedure excavated a hole in the ground, penetrated rock, and resulted in the flow of ground water to land surface. The top of the 24-inch well extends 5 feet above land surface. Central Florida Well Drillers Inc. prepared and maintained a driller's log of the 24-inch well, recording the composition of the stratigraphic column through which the drilling equipment passed. The lithology shown in the stratigraphic column is indicative of the geology normally found in a well drilled in this geographical area. The log shows penetration of the normal stratigraphic column for this area and does not show a spring bore that had been filed in by materials at an earlier date. The drilling of the two wells by Petitioner substantially altered the natural conditions on the property as they existed prior to 1972. The top of the Floridan aquifer in the geographical region in which Petitioner's wells are located is encountered at depths ranging from 50 to 100 feet below land surface. The amount of water flowing from the wells has been variously reported and calculated since the wells were installed. Petitioner's promotional materials, which bill the resort as home of the "world's largest flowing well," asserts the maximum free flow capacity to be 72 million gallons per day (mgd). At another point in time, flow from the larger well was said to be 28.8 mgd and the flow from the smaller well 11.5 mgd. Respondent's staff, in preparing its technical staff report, calculated the total flowage from the two wells to be 18 mgd. In his application for a permit to operate a public bathing facility filed with the Florida Department of Health and Rehabilitative Services (HRS), Petitioner indicated the total flowage to be 16 mgd. For purposes of the determination to be made by this Order, the parties stipulated at the hearing to a total flowage figure of 12.47 mgd. Petitioner has operated and continues to operate the facility as a campground and water based recreational site. The central theme of the use of Petitioner's property is the recreational use of water. The water based recreation includes swimming, boating, tubing, and fishing, and is centered around the two flowing wells. The designated swimming area extends from a retaining wall located just west of the westernmost of the two wells to a footbridge which crosses Canoe Creek west of the Marina. The supply of water for recreational use comes primarily from the two wells. The stream which originally existed on the property and which carries runoff from the more western part of Petitioner's property and from off-site enters the designated swimming area at the retaining wall on its westernmost edge. The water which comes from this stream and which is introduced into the western end of the swimming area contains high levels of bacteria and coliforms. Between the hours of 6:00 a.m. and 6:00 p.m., Petitioner operates a sump pump which redirects this high coliform water eastward around a major portion of the swimming area to a point still within the swimming area. For the remaining twelve hours per day, this high bacteria, high coliform water is allowed to flow directly into the swimming area. Petitioner could reduce the level of bacteria and coliforms in the swimming area by simply operating the sump pump for 24 hours a day and/or introducing the water so pumped back into Canoe Creek at a point further downstream east of the designated swimming area. In addition, runoff from a storm drain which was constructed by Lake County, Florida, as a result of an easement granted to them by Petitioner, enters Canoe Creek at a point downstream from the wells but east of the footbridge, within the designated swimming area. When stormwater is conveyed through this storm drain, it also introduces coliforms into the swimming area at the point where the storm drain intersects Canoe Creek. The gate valves on each of the two wells are frozen in a completely open position. The wells are presently flowing at maximum capacity 24 hours a day without regard to whether the facility is being used or not. Petitioner does not presently have the capability to incrementally control the flow of water, short of utilizing a plug to completely shut off the flow of water from one or the other or both of the two wells. Petitioner does, however, have the capability of installing a hydraulic cylinder remote control system in the wells which would allow him to control the flow of water incrementally from the wells via a phone line. The use of Petitioner's facility varies by season, month, day of the week, and time of day, and according to weather conditions on a particular day. Although Petitioner did not have records available showing the number of persons utilizing a particular part of the facility for a particular purpose on a particular day, most of Petitioner's revenue, at least during the summer months, is generated by day use swimmers and picnickers. The swimming facility is most heavily used during daylight hours in the summer months. More customers use the swimming facilities on Saturday and Sunday than during the weekdays. Use is lower during the winter months and during times of inclement weather such as cloudy or rainy days. The evidence fails to show the average number of bathers who use Petitioner's facilities at any particular season or during any particular weather conditions. Petitioner holds a Swimming Pool-Bathing Place Operating Permit for the swimming area issued by the Florida Department of Health and Rehabilitative Services pursuant to Section 10D-5.120, Florida Administrative Code. Responsibility for enforcement of these administrative regulations is with the Lake County, Florida, Public Health Unit. Petitioner's permit allows him to have a maximum swimming pool population of 2000 bathers per day, but there is no evidence that he has ever had that many bathers on a single day since he received the permit. There are two primary water quality parameters which Petitioner is required to maintain within the swimming area, which are delineated in Rule 10D- 5.120, Florida Administrative Code. The first is a flow-through requirement of 500 gallons of water per anticipated bather per 24 hours. On a day when the swimming facility is being utilized by the maximum number of bathers allowable, 2000, the flow requirement for that day would then be one million gallons. For any day when the bathing population fell below 2000, the gallon flow-through requirement would be proportionately reduced. The second water quality parameter Petitioner is required to maintain relates to coliform densities. High coliform count can result in serious illness. The coliform density in the swimming area must not exceed 1000 most probable number of coliform organisms per 100 milliliters. Coliform levels in the swimming area at any given time are dependent upon several variable factors. Among these factors is the number of coliforms being introduced into the swimming area. As has previously been discussed, when the sump pump which reroutes high coliform water around the upper part of the swimming area is not operating, the number of coliforms would increase. Also during periods of rainfall, coliforms are washed into the swimming area in runoff which enters from overland and through the storm drain which enters the lower part of the swimming area. Temperature is a variable factor which affects coliform levels. As temperatures increase, bacteria multiply more rapidly, and thus coliform levels increase. The number of human beings utilizing the water at a given time impacts coliform levels in that, since humans are producers of coliforms, when greater numbers of humans are in the water, higher coliform levels would normally result. These factors coalesce in that high temperatures normally occur during the summer months which contain the days of most intense usage, and thus high coliform levels would be expected during these times if all other factors remain constant. Conversely, during the winter months, when facility usage is lowest and temperatures are lowest, lower coliform levels would be expected. One additional variable factor which affects coliform levels is the amount of water flowing through the swimming area. Water dilutes any contaminants or pollutants that come into the system. Petitioner attempted to show a correlation between rate of flow and coliform levels in excess of 1000 parts per 100 milliliters (ppm). (Petitioner's Exhibit #1) However, because the date collected did not control for and did not take into account the presence or non-presence of the variable factors which affect coliform levels, no conclusions could be reached regarding whether water quality could be maintained in the swimming area in accordance with HRS standards, with periodic adjustments to flow from the wells. No competent substantial evidence was offered to show that periodic adjustments to flow would prevent Petitioner from meeting HRS standards for water quality and therefore prevent Petitioner's continuing the operation of his public bathing facility. The original permit application filed by Petitioner only requested an allocation of 31.7 million gallons per year (mgy), this amount being only the water utilized for the campground. The construction of Petitioner's potable water supply for the campground was approved by the Florida Department of Environmental Regulation and meets all water quality standards applicable to the campground. Although the water used for the campground comes from a pipe connected to the 24-inch well, this request for water is not related to and does not account for the water which flows from the wells into the swimming area and out through Canoe Creek and is used for recreational purposes. The technical staff report (TSR) prepared by Respondent's staff recommends granting an allocation of 31.7 mgy of water to Petitioner for commercial and household uses (to supply the campground) and an allocation of 2.55 billion gallons per year (bgy) of water for recreational uses. The recommended allocation for recreational use breaks down to an average daily use of 7 million gallons per day (mgd), representing a 44 per cent reduction in the amount of water presently flowing from the wells for recreational purposes. The TSR further recommends a maximum daily use for any one day of the year of 18 million gallons of water. This recommendation actually exceeds the present production capacity of the wells. The TSR further recommends that the overall 44 per cent reduction in use of water for recreational purposes be achieved by adjustment of well discharges during non-use periods each day and seasonal non-use periods when bathing and marina use are minimal. This would require installation of operable valves on each of the wells as is also recommended in the TSR. Subject to the limitation imposed by the annual allocation and subject to the maximum daily allocation, Petitioner would make the flow adjustments as conditions warrant and as he sees fit. The Floridan aquifer in the region surrounding Petitioner's property is not expansive; thus there is a maximum amount of water which can be stored within it. Water will tend to discharge at some point within the system when flow is stopped at another point. The drawdown effect on the potentiometric head caused by the 24-inch well after flowing for a period of twenty-four hours can be calculated to extend up to two miles west of that well and further to the east. The excess water flowing through Petitioner's wells, over and above that required for recreational purposes, could be tapped and used by other potential consumers of water within the same vicinity, if Petitioner reduced the flow from his wells. Underlying the Floridan aquifer in the Wekiva River Basin Area is a layer of saline water, the degree of salinity being measured by the chloride concentrations in said water. This underlying saline water is relic sea water and is not salt water being pulled in from the oceans. When water is discharged from the Floridan aquifer and potentiometric pressures are thereby reduced, saline water is allowed to move upward and closer to the Floridan aquifer, resulting in higher chloride concentrations in the water discharged from the Floridan aquifer. The converse is also true. Reductions in discharge tend to increase potentiometric pressures which, in turn, would push the saline water further away from the Floridan aquifer. Chloride concentrations are the basic measurement of water quality. In measuring chloride concentrations in water, 250 milligrams of chloride per liter of water is the significant figure because this measuring point is the highest concentration of chloride that is recommended for public drinking water supplies. Data has been collected regarding chloride concentrations in water taken from the Floridan aquifer beneath the Wekiva River basin and shows significant changes during the period from 1973 to 1986. In a United States Geological Survey (USGS) study of water quality in the Floridan aquifer beneath the Wekiva River basin, conducted in 1973-74, an area or isochlor of water with chloride concentrations exceeding 250 (ppm) was identified. Petitioner's wells were included in this study, and the chloride level in his wells was measured at 230 ppm. The isochlor depicting water with chloride concentrations exceeding 250 ppm extended southward to a point north of Petitioner's property. A follow-up study begun in 1986 shows that the area or isochlor of water with chloride concentrations exceeding 250 ppm has extended itself, moving southward to include and pass the Petitioner's wells, past the Lake County border line which lies to the south of Petitioner's property and into Orange County, Florida. In 1986 Petitioner's wells produced water which measured 296 ppm and 312 ppm respectively. Because the 1986 study was not complete as of the time of hearing, no clear determinations can be made as to the extent to which the Petitioner's wells have contributed to the southward migration of the 250 mg/1 of chloride base line. At a minimum, the withdrawals of water from Petitioner's wells is having a localized impact in the immediate vicinity of those wells. Reduction of the flows from Petitioner's wells would, at a minimum, result in an improvement in the chloride levels in a localized area. That improvement in conjunction with similar improvements at other wells in the area could ultimately result in a more regional improvement of the chloride levels. Because of the factors observed indicating a deterioration of the aquifer systems in the face of increased demand, Respondent's staff has created Special Condition Zones in an effort to identify areas within the Wekiva River basin where hydrologic conditions warrant concern and special attention. Zone One, in which Petitioner's property is located, is the area of greatest concern because of observed changes within the hydrologic regime. Special permit conditions have been created for these zones to insure that no more water than is needed for a specific purpose is allocated to any user in the area. The flows from Petitioner's wells provide a benefit to the Wekiva River by diluting the pollutants which flow into the river. The cascading water from the standpipes aerates the water, which in turn increases the oxygen levels which is of benefit to the invertebrates, fish, and other animals that live in the water. The flows from Petitioner's wells account for approximately six or seven per cent of the flow of the Wekiva River at the gauging station at State Road 46. Nevertheless, no persuasive competent substantial evidence was offered to show that an overall 44 per cent reduction in flow from Petitioner's wells would in any significant way impact the quality of water in the Wekiva River. The District staff recommended that numerous "standard general conditions" and numerous "other conditions" which relate specifically to this project be incorporated in Petitioner's CUP permit. Those conditions are set forth at length in Respondent's Exhibit No. 6 and it would serve no useful purpose to repeat them all here.
The Issue Whether the application of Telegraph Cypress Water Management District to modify an existing surface water management system permit should be granted.
Findings Of Fact The South Florida Water Management District (District) is a public corporation in the State of Florida existing pursuant to Chapter 25270, Laws of Florida, 1949, and operating pursuant to Chapter 373, Florida Statutes, and Chapter 40E, Florida Administrative Code. The District is a multipurpose water management agency with principal offices in West Palm Beach, Florida. Telegraph Cypress Water Management District (TCWMD) is a water control district organized pursuant to Chapter 298, Florida Statutes. Agricultural operations have been conducted within the TCWMD for more than 30 years by the landowner, Babcock Florida Company. The TCWMD is the permittee of record. James D. English, Jr., owns, along with other members of his family, an orange grove and pasture in Lee County, Florida. The English family has owned the property for approximately 120 years. On November 10, 1992, James D. English, Jr., and the Panacea Timber Company filed a petition for formal administrative hearing challenging the District's intent to issue SWM Permit Modification No. 08-00004-S. Cypress Creek Partnership is a Florida General Partnership of which James D. English, Jr., is a principal. The partnership engages in agricultural activities in Lee County, Florida. The Alva Cemetery, Inc., is a Florida not-for-profit corporation which owns and manages a cemetery facility in Lee County Florida. The cemetery has been in active use for approximately 120 years. In recent years, Alva Cemetery has experienced occasions of excess water encroaching onto the cemetery property. On November 12, 1992, Alva Cemetery, Inc., filed a petition for administrative hearing challenging the District's intent to issue SWM Permit Modification No. 08-00004-S. James D. English, Jr., Cypress Creek Partnership and Alva Cemetery, Inc., are herein referred to as Petitioners. The TCWMD and the Petitioner English share a common property boundary. The Alva Cemetery is surrounded by the English property. All lands involved in this matter historically drain towards the Caloosahatchee River. The TCWMD includes approximately 89,120 acres of land located in Charlotte and Lee Counties, Florida. The land uses within the TCWMD include agricultural, cattle, and timber operations. Generally, the fields have been leased to third party farmers who use the field for several years. When the fields are not actively farmed, they are returned to a fallow state and used as pasture land until fertility is restored at which time they are reactivated for farming. Active farms fields are generally surrounded by a perimeter ditch and dike system. Pumps may be used to water and de-water the fields. When the field is returned to a fallow state, the ditch and dike system are not maintained and become less prominent either by action of weather or by intent. Pumps are not present. All of the TCWMD lies generally north to northwest of the property owned by the Petitioners. Surface waters flow onto the Petitioners' lands from the north. The Telegraph-Cypress system is unique and is the largest of its kind in South Florida Water Management District jurisdiction. The TCWMD system includes storage/detention facilities, control structures, pumping stations and an extensive network of internal canals. There are nine separate water management basins within the TCWMD. The Petitioners asserted that the water management basins identified by the District and the TCWMD are incorrect. The greater weight of the evidence establishes that the District's identification and delineation of the nine basins is based on historical hydrologic characteristics of the TCWMD and is a reasonable determination of basin boundaries. The land encompassed by the instant application for permit modification includes three of the nine basins and encompasses approximately 51,400 acres of the TCWMD. Surface water discharge from the relevant farm fields flows via the internal canal network and sheet flow to the three common detention basins: Telegraph Swamp, North Telegraph Swamp ("Telegraph North") and Curry Lake. The Telegraph North basin lies to the north of and discharges into the Telegraph Swamp basin and includes 13,799 acres of which 4,094 acres are farm fields. The drainage into the Curry Lake basin does not impact either the Telegraph North or Telegraph Swamp basins or the Petitioners' properties. The evidence establishes that as to the Telegraph North and Curry Lake drainage basins, the permit modification meets applicable permitting criteria. There is no credible evidence to the contrary. Telegraph Swamp is the largest of the three relevant detention systems. The Telegraph Swamp basin includes a total of 32,707 acres of which 4,381 acres are farm fields. Telegraph Swamp is a 4,390-acre wetland vegetated by cypress trees and sawgrass, with a base of muck soils, humus, topsoil, leaf litter and other organic material. Located at the south end of Telegraph Swamp are surface water management control structures (the Big Island Dike) built in 1975 and permitted in the original 1980 permit. The structures include three broad-crested weirs and one flash-board weir. Telegraph Swamp has been compared to a "sponge" capable of absorbing vast quantities of surface water discharges within the TCWMD before the control structures at the south end of the swamp are over-topped. Water discharged from the control structures flows through canals and creeks to the Caloosahatchee River. During storm events water is discharged over the control structures and into a swamp area south of Big Island Dike. From there, the water flows southerly, into Telegraph Creek, Big Island Canal and Cypress Creek and then into the Caloosahatchee. The Petitioners expressed concern that TCWMD could inappropriately discharge water from the control gates in the Telegraph Swamp weir. Based on evidence admitted at the hearing, the permit modification should include the following special condition: Discharge structures in the Telegraph Swamp basin shall remain fixed so that discharge cannot be made below the control elevations, except that structure gates and weirs may only be removed during emergency conditions upon notification to and consent by the District's Fort Myers Service Center regulatory area manager or designee. The Basis of Review for Surface Water Management Permit Applications within the South Florida Water Management District--September 1989, incorporated into Chapter 40E, Florida Administrative Code, provides the applicable water quantity permitting criteria relevant to this proceeding. The Petitioners assert that the control gates are required to be locked in accordance with Basis of Review section 3.2.4.1.b, which states: Discharge structures shall be fixed so that discharge cannot be made below the control elevation, except that emergency devices may be installed with secure locking devices. Either the District or an acceptable govern- mental agency will keep the keys for any such devices. The Petitioners are correct. The rule requires secure locking devices. Such condition should be added to the permit The keys may remain with the TCWMD as "an acceptable governmental agency." In 1980, the District issued Surface Water Management Permit No. 08- 00004-S for the TCWMD to operate an existing surface water management system for an existing agricultural operation. The 1980 permit specifically authorizes "[o]peration of a water management system serving 89,120 acres of agricultural lands by a vast network of internal drainage and irrigation canals, a major dike, a major canal and 4 water control structures discharging via small tributary creeks and sloughs into the Caloosahatchee River." Although the permit has been subsequently modified, the authorization to operate the system has not been amended. While District enforcement staff have occasionally noted "performance deficiencies" on the TCWMD property, there have been no permit violations by the permittee. Deficiencies which have been called to the TCWMD's attention have been resolved. Special condition number five to the 1980 permit provides that "[d]ischarges of water onto adjacent lands may be continued to the extent that increased problems are not caused by such discharges." The Petitioners assert that the District has failed to acknowledge that water discharged from the Telegraph Cypress system flows into the Cypress Creek canal and has failed to consider the impact on the Cypress Creek receiving body. However in the staff report to the 1980 permit states as follows: The Telegraph Cypress basin has three major drainage outlets. These are Trout Creek on the west, Telegraph Creek in the center and Cypress Creek to the east. There is a fourth outlet in the northeastern corner of the property known as Jack's Branch, however, this outlet is small compared to the three major ones. Much of Telegraph's southeastern area was previously drained by Spanish Creek and County Line Canal. This historical drainage pattern was blocked when a company which is presently known as Golden Grove constructed a dike across their northern boundary. This dike causes increased flow in a westerly direction around the west end of the dike, thence southerly towards Cypress Creek. This increased flow has caused excess water problems to property owners downstream. In addition, the dike has blocked virtually all flow to Spanish Creek. The evidence fails to establish that, as asserted by the Petitioners, the District has failed to acknowledge the discharge of water to Cypress Creek or to consider the condition of the Cypress Creek receiving body. In the instant case, the condition of the Cypress Creek receiving body was not re- addressed because the permit modification being sought will cause no additional adverse impacts on existing conditions. Although not individually numbered and identified in the original 1980 permit, the evidence establishes that in 1980, all of the farm fields which are subject to this permit modification application were in existence. The applicant seeks no new water control structures. Other than that required to reactivate fallow farm fields, there is no new construction proposed in the instant application. The Petitioners assert that the instant permit modification application will result in construction of new farm fields. The evidence is contrary to the assertion. Proposed permit special condition No. 10 states that the permit does not include the construction of any new farm fields. The farm fields covered in the staff report would be permitted for reactivation from a fallow state without further permitting activity in the future, and without individual retention for each farm field. The modifications to the original 1980 permit have increased the total farm land area. There is no evidence that, except as specifically permitted and approved by the District, there has been alteration of historical discharge rates or routes. There has been considerable confusion regarding the permitting status of the operations as farm fields have been reactivated. Such reactivation entails grading and leveling fields, reconstruction of ditches and dikes and installation of pumping equipment. In order to provide for standardization in farm field reactivation, and to better monitor such activities, the District requested that the TCWMD seek to modify the existing permit. On February 8, 1991, the TCWMD submitted an application to modify the existing permit for the purpose of reactivating the existing farm fields located within the Telegraph North, Telegraph Swamp, and Curry Lake drainage basins. The proposed SWM permit modification authorizes the continued use of the previously permitted surface water management system for existing active and fallow farm fields and allows the reactivation of currently fallow farm fields without further permit modification by the District. Proposed SWM permit special condition No. 16 states that the District requires notification in letter form 30 days prior to all farm field reactivation activities. The proposed modification of the permit will provide the District with an enhanced ability to inspect the reactivated farm fields. Inherent in such reactivation is ditching and diking of the fields. Such operations have been authorized since the 1980 permit was issued. The work associated with field reactivation will be conducted in accordance with existing design criteria as set forth in the application. Based on evidence admitted at the hearing, the permit modification should include the following special condition: Ditches and dikes associated with the farm fields encompassed by this authorization shall be constructed/maintained in conformance with the "Typical Field Layout And Detail Sheet," revised 10/12/93. The evidence establishes that the operations of the TCWMD as proposed by the permit modification application are within the authorization of the existing permit as previously modified. Otherwise stated, the award of this modification will have no substantial impact on the operation of the permitted surface water management system. The modification will result in no additional discharge of surface water from the control structures. The District has established water quantity criteria intended to insure that adverse impacts do not occur due to excess discharge. (Based upon the Hearing Officer's ruling on a District's Motion in Limine, water quality issues were not addressed at hearing.) The criteria are set forth at Chapter 40E-4.301, Florida Administrative Code, and in the Basis of Review. In relevant part, the District criteria require an applicant to provide reasonable assurances that the surface water management system provides adequate flood drainage and protection, that the system will not cause adverse water quantity impacts on receiving waters and adjacent lands, and that the system will not cause adverse impacts on surface and groundwater levels and flows. Modification of a permit must not result in additional adverse off-site impacts. In this case, reasonable assurances have been provided that the proposed modification will not exacerbate the historical and current drainage conditions. The permit modification application at issue does not propose to alter the rates or routes of water currently authorized for discharge from Telegraph Swamp. Reactivation of the farm fields will not impact receiving bodies in any manner different from that which presently exists under previous permits. In providing reasonable assurances, the TCWMD analyzed the water storage capacity available in the detention basins, performed flood routing projections and calculated peak discharge rates for the permit area. As required by the district, the TCWMD utilized a standard hypothetical 25-year/3- day storm event in order to determine whether sufficient capacity was available to handle the resulting stormwater. The projections provide reasonable assurances that the common detention areas have the capacity to provide adequate flood drainage and protection and are accepted. Rule 40E-4.091(1)(a), Florida Administrative Code, incorporates by reference a document identified as the "Basis of Review for Surface Water Management Permit Applications within the South Florida Water Management District--September 1989" Section 3.2.1.2.b requires that: the proposed project modification must meet the allowable discharge rate; and the allowable discharge rate for a previously permitted project is that which was set in the previous permit. The TCWMD prepared and submitted discharge calculations establishing that the post-development discharges will not exceed the discharge rate previously accepted by the District. Since 1984, the District has previously accepted a peak allowable discharge rate of 39 cubic feet per second per square mile (csm). The csm figure is based upon the historical TCWMD discharge rate within the Caloosahatchee River basin. As previously stated, reactivation of the farm fields will not impact the receiving bodies in any manner different from that which presently exists under previous permits. The District asserts that the 39csm discharge rate has been "permitted" since the 1984 modification was approved. The Petitioner asserts that the 39csm discharge rate has never been "permitted" by the District. The evidence establishes that since the 1984 application for permit modification, the discharge rate of 39csm has been utilized by TCWMD and has been accepted by the District, but that the actual permits do not specifically identify the discharge rate as 39csm. In projecting discharge rates, the TCWMD used a time of concentration of one hour. The time of concentration (T.O.C.) is the time in which water would move from the farm fields to the control structure in each sub-watershed. Otherwise stated, a projected T.O.C. of one hour means that the storm water would move from the field to the control structure in one hour. The T.O.C. of one hour is a conservative estimate and likely substantially overestimates the speed at which the water will move. The three basin areas contain a total of more than 80 square miles. Water will travel an average distance of two miles from field to detention basin through ditches, swales and existing low areas. Again conservatively, the TCWMD did not include projected travel time through such conveyances, resulting in a longer T.O.C. and resulting in a higher peak discharge rate than is probable. Although there appeared to be some confusion on the part of the District staff as to the application of the T.O.C. by the TCWMD, the TCWMD engineer who performed the calculation testified at hearing and was qualified as an expert witness in civil engineering, hydrology and surface water management. His testimony and projections are reasonable and are credited. Proposed SWM permit modification special condition No. 11 states that farm field discharge shall be directed to and conveyed via existing ditches, wetlands and/or sheetflow areas per existing site conditions. No new outfall ditches are permitted under this modification. Flood routings were calculated assuming all farm fields would be activated simultaneously and pumping the maximum capacity of 390 gallons per minute per acre (the equivalent of 20-21 inches of surface water pumped from each field daily). It is highly unlikely that all farm fields would be active simultaneously or that stormwater would continue to fall with such velocity to permit continued pumping at maximum capacity for an extended period. Even based on the conservative assumptions utilized by the TCWMD engineers, the projected peak discharge rate at the Telegraph Swamp control structure is 37csm to 38.5csm, within the maximum of 39csm previously accepted by the District. The computer modeling performed by the TCWMD engineer in calculating the peak discharge rate is accepted as reasonable. The TCWMD did not include offsite inflow in its analysis of projected capacity or discharge rates. There is anecdotal evidence that on occasion, water may flow into TCWMD from Jack's Branch or from across roadways to the north and west of the TCWMD; however, given the vast storage capacity of the TCWMD detention areas, there is no evidence that the quantity of offsite inflows is of such significance as to render the TCWMD projections unreasonable. As previously stated, the TCWMD calculations are reasonable and are accepted. The evidence establishes that the peak discharge rate resulting from approval of the instant permit modification will not exceed 39csm. The Petitioners offered their own peak discharge rate calculations, based on a "worst possible case scenario." The assumptions on which the Petitioners' projections are based are unreasonable and are rejected. Based on recommendations received at the hearing, the permit modification should include the following special condition: Pumped discharge from farm fields for which pumps are not currently installed shall be limited to 75 gallons per minute per acre of farmed area. Pumps are currently installed in fields number 7, 8, 9, 10, 12, 14, 15, 24 north and south, 28, east half of 34, 64, 67, 68, 69 and 80. The Petitioners assert that the system is currently causing adverse impacts to their properties in the form of flooding. The greater weight of the evidence establishes that the system presently does not cause adverse water quantity impacts on receiving waters and adjacent lands, and does not cause adverse impacts on surface and groundwater levels and flows. The evidence establishes that award of the application for permit modification will not adversely alter the current operations. It is clear that the Petitioners have been impacted by changes in the historical drainage patterns in the area; however, such changes had substantially occurred by 1980 when the original permit was issued. The greater weight of the credited evidence establishes that such impacts are not the result of the activities authorized in the original 1980 permit and in subsequent modifications, but instead are the result of unrelated actions by third parties not involved in this administrative proceeding. There is no credible evidence that the permit modification sought in the instant proceeding will adversely affect the Petitioners. The 1980 permit addresses existing water quantity problems in the area of the TCWMD project. For example, the construction of the Golden Grove Dike resulted in blockage of historical drainage towards Spanish Creek and the diversion of excess waters into Cypress Creek. During the 1980's the District required that culverts be installed in the Golden Grove Dike which eventually restored some surface water flow through the dike construction and on towards the south, although during some storm events water flow continues around the dike and into Cypress Creek. The Petitioners offered anecdotal evidence as to reduced water flows in some local creeks and increased flows thorough Cypress Creek. The Respondent offered evidence indicating that water flow through Cypress Creek may be less than 30 years ago, due to the digging of a canal between Spanish Creek and Cow Slough and the extension of the Clay Gully Canal's diversion of water into Telegraph Swamp. None of the evidence on this point was persuasive, however it is not relevant. Clearly, the instant permit modification application will not adversely affect the existing situation in the receiving bodies. The Petitioners assert that other receiving waterways have become clogged with vegetation, debris or soil, have accordingly reduced capacities, and are unable to accommodate historical discharge levels. Based on the lack of capacity, the Petitioners suggest that waters move towards the eastern portion of Telegraph Swamp and are discharged, flow towards, into and over the banks of Cypress Creek, and flood their properties. The TCWMD conducted a study of backwater profiles based upon credited field data. The study is found to be reasonable and is credited. Based upon the study, approximately 90 per cent of the water discharged from Telegraph Swamp is conveyed to the Caloosahatchee via Big Island Canal, Telegraph Creek and the swamp area south of the control structure. The remaining 10 per cent of the water enters the Bullhead Strand-Lightered Canal-Cypress Creek watercourse. Water flows from Telegraph Swamp into Cypress Creek via Bullhead Strand and the South Lightered Canal, however, the canal has become so restricted by vegetation that it provides little direct water flow between the strand and the creek and is more properly regarded as an area of enhanced sheet flow. The evidence does not establish that the surface water traveling from Bullhead Strand to Cypress Creek is of significance. Coupled with the existence of the Big Island Canal (which connects Telegraph Swamp to Telegraph Creek) it is unlikely that post-development surface water discharged from the Telegraph Swamp into Cypress Creek exceeds pre-development discharges. The Petitioners claim that two culverts in the Big Island canal restrict the flow of water through the canal and result in increased discharge to the east and to Cypress Creek. The greater weight of the evidence establishes that during period of time when the culverts are unable to accommodate water flow, the water travels into a broad flood plain, around the culverts and returns to the Big Island Canal. The evidence establishes that the proposed modification will not result in additional adverse off-site impacts. The adverse conditions affecting Cypress Creek existed at the time of the 1980 permit and are addressed in the staff report to that permit and to subsequent permit modifications. There is no credible evidence that modification of the permit as sought in this case will result in adverse impacts beyond those which have existed at the time of the award of the original permit. The Petitioners assert that the fields included within the permit modification application lack individual retention areas. The lack of individual detention areas is immaterial in this case where sufficient downstream detention capacity is available through the common detention areas. The Petitioners asserts that the Telegraph Swamp is an "above-ground impoundment" and that as such is fails to comply with requirements related to such water storage systems. The Telegraph Swamp is not a typical "above-ground impoundment" as that term is routinely applied by the District. The regulations addressed by the Petitioners clearly state that they are not intended to be inclusive and are intended to provide guidelines and basic performance criteria for commonly encountered south Florida situations. Telegraph Swamp is not a commonly encountered south Florida situation. There is no evidence that the decision not to apply the "above-ground impoundment" regulations to the Telegraph Swamp is unreasonable. The Petitioner suggest that the TCWMD application for permit modification is deficient and fails to provide information in compliance with the Basis of Review. The Basis of Review is directed towards applications for new construction. The District reasonably does not interpret the all elements of the Basis of Review to apply to existing operations. The original staff report for this permit modification application fails to acknowledge that Cypress Creek is a receiving body. However, as stated previously, the 1980 application and subsequent modifications have clearly addressed the fact that Telegraph Swamp waters discharge to Cypress Creek via intervening waterways. The failure to include the reference in the staff report to this application for modification is irrelevant.
Recommendation Based on the foregoing, it is hereby RECOMMENDED that the South Florida Water Management District enter a Final Order issuing Surface Water Management Permit Modification No. 08-00004-S including the additional permit conditions set forth herein, to the Telegraph Cypress Water Management District. DONE and RECOMMENDED this 1st day of April, 1994 in Tallahassee, Florida. WILLIAM F. QUATTLEBAUM Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 1st day of April, 1994. APPENDIX TO RECOMMENDED ORDER, CASES NO. 92-6900 and 92-6901 To comply with the requirements of Section 120.59(2), Florida Statutes, the following constitute rulings on proposed findings of facts submitted by the parties. Petitioners James D. English and Cypress Creek Partnership The proposed findings of fact submitted by Petitioners James D. English and Cypress Creek Partnership consist of unnumbered paragraphs. Pages forty-five through fifty-nine of the proposed findings of fact submitted by Petitioners James D. English and Cypress Creek Partnership were stricken as set forth in the Order On Motion To Strike issued March 29, 1994. The paragraphs of pages five through forty-four of the proposed findings of fact submitted by Petitioners James D. English and Cypress Creek Partnership have been consecutively numbered and are accepted as modified and incorporated in the Recommended Order except as follows: 1-2. Rejected, argument, not findings of fact. 7-9. Rejected, argument, not findings of fact. The staff report is not dispositive. 10-12. Rejected. The greater weight of the evidence establishes that, although the 39csm figure is not set forth in the permit, as of the 1984 modification, the TCWMD calculations have been based on a peak discharge rate of 39csm and that the District has accepted the calculations previously. The applicable criteria in the instant case require that the allowable discharge rate for a previously permitted project is that which was set in the previous permit. 13. Rejected, recitation of testimony is not finding of fact. 15-16. Rejected, argument, not finding of fact, irrelevant, cumulative. 17-18. Rejected, recitation of testimony is not finding of fact. 19. Rejected, contrary to the greater weight of credible and persuasive evidence which establishes that 39csm has been the peak discharge rate accepted by the District since 1984. The flow rate projected by the TCWMD does not exceed the accepted peak discharge rate. 24. Rejected, recitation of testimony is not finding of fact. 26-28. Rejected, recitation of testimony is not finding of fact. 29-30. Rejected, argument, not finding of fact. Rejected, irrelevant. Rejected, argument, not finding of fact. Rejected, irrelevant. The greater weight of the credible and persuasive evidence establishes that 39csm has been the District's accepted peak discharge rate and that this modification will not result in peak discharge rates in excess of that which has been previously accepted. Rejected, not supported by the greater weight of credible and persuasive evidence. The assumptions underlying the Petitioners' calculation of theoretical maximum discharge are rejected as unreasonable. Rejected, unnecessary. 36-45. Rejected, irrelevant. The anecdotal evidence fails to establish that offsite inflows are of such quantity as to render the TCWMD projections unreasonable. The proposed findings also consist of recitation of testimony or argument and are not findings of fact. 46-52. Rejected, contrary to the greater weight of credible and persuasive evidence. The evidence fails to establishes that the swamp is an "above-ground impoundment" as that term is routinely applied by the District. The proposed findings also consist of recitation of testimony or argument and are not findings of fact. 53-67. Rejected, irrelevant. An applicant for a permit modification is not required to supply every item on the checklist. An application for a modification to an existing permit often need not contain all the items described. 69. Rejected, cumulative. 70-71. Rejected, argument, not finding of fact. 72-81. Rejected, not supported by the greater weight of credible and persuasive evidence which establishes that the identification and delineation of the nine basins is based on historical hydrologic characteristics of the TCWMD and is a reasonable determination of basin boundaries. The proposed findings also consist of recitation of testimony or argument and are not findings of fact. 82. Rejected, subordinate. 83-85. Rejected, irrelevant. The confusion on the part of District staff as to what T.O.C. was utilized by the TCWMD engineer is irrelevant. This proceeding is not a review of preliminary staff activity. The applicant must establish entitlement to the permit at the hearing. 86-87. Rejected, recitation of testimony is not finding of fact. Rejected. The confusion on the part of District staff as to what T.O.C. was utilized by the TCWMD engineer is irrelevant. Rejected, unnecessary. Rejected, recitation of testimony is not finding of fact. 91-94. Rejected, irrelevant, the discharge projections calculated by the TCWMD as explicated at the hearing are credited. In any event, the evidence establishes that this modification will result in no additional discharge of surface water from the control structures. 95-97. Rejected, irrelevant. The evidence establishes that this modification will result in no additional discharge of surface water from the control structures. Petitioner Alva Cemetery Petitioner Alva Cemetery's proposed findings of fact are accepted as modified and incorporated in the Recommended Order except as follows: 2. Rejected, not supported by the greater weight of credible and persuasive evidence. 4-5. Rejected, irrelevant. Rejected, irrelevant. This is a de novo hearing, not a review of preliminary staff work. The evidence at hearing establishes that the permit modification will not cause additional adverse affect on existing receiving bodies. Rejected, irrelevant. The evidence fails to establish that Hall Creek and Fichter Creek are receiving bodies of such capacity that their omission from staff report is material. Rejected, irrelevant. Rejected, irrelevant. The evidence fails to establish that offsite inflows are of such quantity as to be relevant. 11. Rejected, not supported by the greater weight of credible and persuasive evidence. The Applicant's analysis is credited. As to T.O.C., even the less conservative T.O.C. projections indicate a peak discharge rate within that previously accepted by the District. 12-13. Rejected, irrelevant. Rejected, irrelevant. Such return overflows are unnecessary in this situation where the detention areas have the capacity to provide adequate flood drainage and protection. Rejected, not supported by the greater weight of credible and persuasive evidence. Rejected, not supported by the greater weight of credible and persuasive evidence. 18-20. Rejected, cumulative. 21. Rejected, immaterial. There is no evidence that this permit modification application will cause additional adverse impact on receiving bodies. The failure to address nonexistent impacts is immaterial. Rejected, errors in staff report are irrelevant. The evidence admitted at hearing is accepted as correct. First paragraph is rejected, cumulative. Second paragraph is rejected, not supported by the greater weight of credible and persuasive evidence. Rejected, anecdotal testimony is not supported by the greater weight of credible and persuasive evidence. Rejected. The greater weight of credible and persuasive evidence establishes that all farm fields affected by this permit modification application were in existence by the 1980 permit. Rejected, not supported by the greater weight of credible and persuasive evidence. The assumptions underlying the Petitioners' calculation of theoretical maximum discharge are rejected as unreasonable. Rejected, irrelevant. The greater weight of credible and persuasive evidence fails to establish that the cemetery flooding is related to actions by the TCWMD. Further, the evidence fails to establish that, even if the flooding was related to the TCWMD, the instant permit modification application will cause additional adverse impacts. Respondent Telegraph Cypress Water Management District Respondent Telegraph Cypress Water Management District's proposed findings of fact are accepted as modified and incorporated in the Recommended Order except as follows: 18. Rejected, subordinate. 19-20. Rejected, not credited and unnecessary. Rejected as to assertion that the 39csm discharge rate was set in the 1984 permit modification, not supported by the evidence. Review of the document admitted into evidence as the 1984 modification fails to reveal that the figure of 39csm is set forth therein. Rejected, cumulative. Rejected, unnecessary. Respondent South Florida Water Management District Respondent South Florida Water Management District's proposed findings of fact are accepted as modified and incorporated in the Recommended Order except as follows: 30. Rejected as to assertion that the 39csm discharge rate was set in the 1984 permit modification, not supported by the evidence. Review of the document admitted into evidence as the 1984 modification fails to reveal that the figure of 39csm is set forth therein. Pages 17-19 of the Proposed Recommended Order set forth revisions to the staff report which originally form the basis for the preliminary agency action in this matter. As the hearing is a de novo review of this matter, it is unnecessary for this Recommended Order to address the revision of the staff report, which has limited probative value. COPIES FURNISHED: Tilford C. Creel Executive Director South Florida Water Management District Post Office Box 24680 West Palm Beach, Florida 33416 Melville G. Brinson, Esquire 1415 Hendry Street Fort Myers, Florida 33902 Frank A. Pavese, Sr. Esquire 1833 Hendry Street Fort Myers, Florida 33902 Scott Barker, Esquire Post Office Box 159 Fort Myers, Florida 33902 John J. Fumero, Esquire Toni M. Leidy, Esquire South Florida Water Management District 3301 Gun Club Road West Palm Beach, Florida 33416
The Issue Whether Bay County has demonstrated its entitlement to the Permit?
Findings Of Fact The Ecologically Diverse Florida Panhandle With its high diversity of species and richness in endemic plants, the Florida Panhandle has been identified as one of six continental "biodiversity hot spots" north of Mexico. It has more species of frogs and snakes, for example, than any other equivalently-sized area in the United States and Canada and has botanical species that do not exist anywhere else in the Coastal Plain, one of the three floristic provinces of the North Atlantic American Region. The biodiversity stems from a number of factors. The Panhandle was not glaciated during the Pleistocene Period. Several major river systems that originate in the southern Appalachian Mountains terminate on the Panhandle's Gulf Coast. Its temperate climate includes relatively high rainfall. These factors promote or produce plentiful sources of surface and groundwater that encourage botanical and zoological life and, in turn, a diverse ecology. When compared to the rest of Florida, the Panhandle is relatively free from man-made impacts to its water resources. Until recently, the population growth rate lagged behind much of the state. Despite a rapid increase in the population in the late 1990s into the early part of the twenty-first century, it remains much less densely populated than areas in the I-4 Corridor and coastal peninsular Florida to the south. The Panhandle can be divided into physiographic areas of geological variation that are highly endemic; a substantial number of plant and animal species found in these areas are found nowhere else in the world. One of these areas is of central concern to this case. Located in southern Washington County and northern Bay County, it is known as the Sand Hill Lakes Area. The Sand Hill Lakes Area The Sand Hill Lakes Area (the "Area") is characterized by unusual geology that produces extraordinary ecological value. With few exceptions (see findings related to Dr. Keppner's flora and fauna inventories on the NTC/Knight Property below), the Area has not been extensively studied. The data on biological communities and water levels that exist, sparse as it is, has been obtained from historic aerials dating to 1941. The aerials are of some use in analyzing lakes and surface waters whose source is the Surficial Aquifer, but they are of limited value otherwise. They are not of use in determining the level in the Surficial Aquifer. Nor are they of assistance in determining river height when the banks of the river are covered by hardwood forest canopy. The resolution of the aerials is insufficient to show details of the various ecosystems. They do not show pitcher plants, for example, that exist at the site of hillside seepage bogs common in the Area. An aspect of the Area that the aerials do reveal is its many karst features on the surface of the land. Karst lakes and sinkholes dominate the Area and are a component of its highly unusual geology which is part of a larger system: the Dougherty Karst Plain. The Dougherty Karst Plain is characterized by numerous karst features: springs, caverns, sinkhole lakes, and sinkholes. Sinkholes In Florida, there are three types of sinkholes: cover subsidence, cover collapse, and "rock" or "cavern" collapse. Of the three, cover subsidence sinkholes are the most common in the state. Cover subsidence sinkholes form as the result of processes that occur on the surface. A cover subsidence sinkhole is usually a shallow pan typically not more than a few feet deep. Found throughout Central and South Florida, they are the most common type of sinkholes in most of peninsular Florida. In contrast, the other two major types of sinkholes (cover collapse and cavern collapse) occur as the result of processes below the surface that cause collapse of surface materials into the substrata. Both types of "collapse" sinkholes are found in the Area, but cover collapse is the more common. Cavern collapse sinkholes are relatively rare. Typical of the Area, cover subsidence sinkholes are not found on the NTC/Knight Property. The NTC/Knight Property The majority of the NTC/Knight Property is in Washington County, but the property straddles the county line so that a smaller part of it is in northern Bay County. All of the NTC/Knight Property is within the Area. The District recognizes that the NTC/Knight Property contains natural resources of extraordinary quality as does the Area generally. Over the three years that preceded the hearing, Dr. Keppner, an NTC/Knight expert, conducted extensive inventories of the flora and fauna on NTC/Knight Property. Dr. Keppner's inventory showed the NTC/Knight Property supports more than 500 species of vascular plants (flora with a system of tubes within the stem, phloem, and the xylem that exchange materials between the roots and leaves) and 300 species of animals. Among them are at least 28 vascular plants and six animals listed as imperiled (threatened or endangered) by state or federal agencies. At least 22 of the imperiled species of vascular plants and eight of the imperiled species of animals are located within an area expected to be affected by the Wellfield for which Bay County seeks the permit modification. For example, at Big Blue Lake alone where impacts were predicted by NTC/Knight experts to take place, the following imperiled plant species are found: Smoothbark, St. John's Wort, Kral's Yelloweyed Grass, Quilwort Yelloweyed Grass, Threadleaf Sundew, Panhandle Meadowbeauty, and Crystal Lake Nailwort. In addition to the Keppner inventory, NTC/Knight commissioned other studies to determine the nature of the sinkholes and whether they are connected to the Floridan Aquifer. NTC/Knight's experts determined that the property contains cover collapse and a few cavern collapse sinkholes that connect to the Floridan Aquifer. Despite evidence to the contrary submitted by the District and Bay County, the NTC/Knight determinations are accepted as facts for a number of reasons, including the lineup of the sinkholes and sinkhole lakes along identified photo-lineaments and the distribution of them in patterns that are not random. A District study using a dye test, moreover, confirmed conduit flow exists in the Area just east of the NTC/Knight Property. With regard to the distribution of the sinkholes and sinkhole lakes on the NTC/Knight Property, Dr. Sam Upchurch used the term "String of Pearls" to describe multiple sinkholes that exist along the edges of several lakes on the property. When sinkholes closer to the center of a lake are clogged or plugged with sediment and debris, the lakes continue to leak around the plugs which causes new sinkholes to form along the edge of the plugs. Examples of the "String of Pearls" formation on the edges of existing lakes are found at White Western and Big Blue Lakes on the NTC/Knight Property and at Crystal Lake nearby in Washington County. The multiple sinkholes bordering the edge of Big Blue Lake are examples of cover collapse sinkholes that, in geological terms, are relatively young as evidenced by their steep sides. In a karst area such as the Area, there is preferential flow in the conduits because of the difference of efficiency of transmission of water flowing through a porous medium of rock compared to that flowing though a conduit. Absent pumping in the Wellfield, the underlying aquifers are relatively stable. If the requested pumping does not take place, it is likely the stability will remain for a substantial period of time. It is not known with precision what will happen in the long term to the karst environment should pumping occur at the Wellfield at the rate the District proposes. When pumping occurs, however, water in the Area affected by the Wellfield will move toward the Wellfield. "[A]s it does[,] you may get some turbulent flow or vorticity in the water." Tr. 1391, (emphasis supplied). At some point, a change in the potentiometric surface and loss of buoyancy will most likely occur. This leads to concerns for Dr. Upchurch from two perspectives: One . . . is that if there is a[n affected] sinkhole lake [on the surface,] it may induce downward flow . . . the other . . . is that if it breaks the plug it may either create a new sinkhole or create a substantial drop in the level of water in the lake . . . which drains periodically, not necessarily because of a wellfield, but because that plug breaks. Id. In the first instance, lake levels could be reduced significantly. In the second, a new sinkhole could be created or the water level could drop dramatically as occurred at Lake Jackson in Tallahassee. Sand Hill Lakes Wetlands The Area contains a number of wetland communities. These include hillside seepage bogs, steepheads, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and creeks and streams in forested wetlands. A number of these wetlands occur on the NTC/Knight Property within the zone of influence in the Surficial Aquifer predicted by NTC/Knight's experts employing a model known as the "HGL Model." The wetland systems on the NTC/Knight Property are diverse, by type, plant species composition, and richness. This remarkable diversity led the District to recognize that the NTC/Knight Property contains lakes of nearly pristine quality, interconnected karst features, and endemic steephead ravines, all of which are regionally significant resources of extraordinary quality. The Area's wetlands also include many streams, among them Pine Log Creek, the majority of which is located on the NTC/Knight Property. Significant recharge to the Floridan Aquifer occurs on NTC/Knight Property. To the west, north, and east of the NTC/Knight Property are major concentrations of Floridan Aquifer springs that are crucial to the quality and character of regional surface water systems, including the Choctawhatchee River, Holmes Creek, and Econfina Creek systems. All of these surficial systems are dependent on the groundwater resources of the Area. The Area's Hillside Seepage Bogs Hillside seepage bogs are marsh-like wetland usually located on gentle slopes of the sides of valleys. They form when the Surficial Aquifer intercepts the sloping landscape allowing water to seep onto the sloped surface. The plant communities in the bogs are dominated by a great number and variety of herbaceous plants that prefer full sun. Among them are carnivorous plants. These unusual plants include the Trumpet and White-Topped pitcher plants as well as other varieties of pitcher plants. Inundation or saturation for extended periods of time is necessary for pitcher plants and most of the rest of the plant communities found in the bogs to thrive and to fend off invasion by undesirable species. Hillside seepage bogs are valued because they are among the most species-rich communities in the world. A reduction in water levels in the bogs below the root zone of associated plants will kill the plant communities that live in them and pose a threat to the continued existence of the bogs. Hillside seepage bogs were once abundant in pre- settlement Florida, but their expanse has been greatly reduced. They are now estimated to only occupy between one and five percent of their original range. On NTC/Knight Property, they have been spared to a significant degree. Numerous hillside seepage bogs continue to exist on the NTC/Knight Property primarily along the margin of Botheration Creek and its tributaries. The Area's Steepheads Steepheads are unique wetland systems. Found around the globe, they are usually regarded as a rarity. More than 50 percent of the steepheads that exist in the world are in a narrow latitudinal band that extends from Santa Rosa County in the west to Leon County in the east, a major section of the Florida Panhandle. Steepheads occur in deep sandy soils where water originating in the Surficial Aquifer carries away sand and cuts into sandy soils. The seepage emerges as a "headwater" to create a stream that conveys the water from the steephead into a river, or in some rare circumstances, into a karst lake. Over time, flow of the seepage waters results in deep, amphitheater- shaped ravines with steep valley side walls. Steepheads are important to the ecologies of the areas in which they occur. They provide habitat for a number of Florida endemic animals and plants believed to be relics of once-abundant species. Water that emerges from a steephead is perennial. Because the steep slopes of the steephead have not been disturbed over a long period of time, the water remains at a relatively constant temperature, no matter the season. Sampling of aquatic invertebrates at the Russ Pond and Tiller Mill Steepheads on the NTC/Knight Property found 41 and 33 distinct taxa, respectively, to inhabit the steepheads. Among them were a number of long-lived taxa. Their presence is consistent with the hallmark of a steephead: perennial flow of water at a relatively constant temperature. Most of the known steepheads flow into streams or rivers. Between six and ten within the Area, however, flow into Sand Hill Lakes. They have no direct connection to any surface drainage basin, thereby adding to their uniqueness. The level in the Surficial Aquifer has a direct impact on where and to what extent seepage flows from the sidewalls of a steephead. The Area's Sphagnum Bogs Sphagnum moss grows in many locations within the landscape and requires moisture. Where there is a large amount of sphagnum moss, it can form a unique community known as a sphagnum bog that is capable of supporting unique plant and animal populations. In the Area, these sphagnum bogs form along the valley sidewalls of steephead ravines and are fed by Surficial Aquifer seepage from the sidewall of the ravine. These sphagnum bogs support unique plant and animal communities, including a salamander discovered by Dr. Means that is new to science and so far only known to exist in sphagnum bogs in the Florida Panhandle. The Area's Sinkhole Lakes and their Littoral Seepage Slopes Sand Hill Lakes are nutrient poor, or "oligotrophic," receiving most of their nutrient inputs through exchange with the plant and animal communities on the adjacent littoral shelves during periods of high water levels. Fluctuating water levels in the Sand Hill Lakes allow a littoral zone with many different micro-habitats. Areas closest to the lakes are inundated regularly, but higher areas of the littoral zone are generally dry and inundated only every ten or 20 years -- just often enough to prevent encroachment of trees. In a few instances, portions of the littoral zones are inundated by seepage from the Surficial Aquifer. Above the normal low water of the Sand Hill Lakes, the littoral shelf occurs along a low gradient. As the littoral shelf transitions into the lake bottom and toward the deeper parts of the lake, there is an inflection point, where the gradient of the lake bottom becomes much steeper than the littoral shelf. If lake water levels fall below that natural inflection point, gully erosion will occur. The flow of water will be changed along the littoral shelf from seepage sheet flow over a wide expanse to water flowing down gullies in a concentrated stream. This change in flow will result in a loss of area needed by certain seepage dependent plants and animals as well as increased sedimentation from erosion. Big Blue Lake is unique because it boasts the largest known littoral zone seepage area of any Sand Hill Lake. The seepage zone along Big Blue Lake supports a number of rare plant species, including the Thread-Leaf Sundew, Smoothed Barked St. Johns Wort, and Crystal Lake Nailwort. The Area's Temporary Ponds Temporary ponds are small isolated water bodies that generally have no surface water inlet or outlet. Typically very shallow, they are sometimes wet and sometimes dry. Temporary ponds can range from basins that have continuous water for three to five years, to basins that have standing water for a month or two, every two to four years. These conditions limit their occupation by fish and, therefore, provide ideal conditions for amphibian reproduction which only occurs when water levels are maintained long enough to complete a reproductive cycle. In the Area, temporary ponds are a direct expression of the Surficial Aquifer and contain no known restrictive layer that might cause water to be "perched" above the Surficial Aquifer. Temporary ponds are critical to the viability of amphibian populations and support high amphibian biodiversity. A given pond can contain between five and eight species of salamander, and between 12 and 15 species of frogs. There has been a decline recently in the population of frogs and other amphibians that depend upon temporary ponds. The decline is due in part to ditching and other anthropogenic activities that have altered the hydrology of temporary ponds. Temporary ponds have a higher likelihood of being harmed by a drawdown than larger, connected wetlands systems. Lowered Surficial Aquifer water levels would lower water levels in temporary ponds and, thereby, threaten amphibian reproduction. Creeks/Streams in Forested Wetlands Streams are classified on the basis of the consistency of flowing water, including perennial (always flowing), intermittent (flowing part of the year), and ephemeral (flowing only occasionally during rain events). The type of stream flow is important because movement of water is essential to support aquatic systems in stream habitats. The NTC/Knight Property includes a number of stream systems, including Botheration Creek and Pine Log Creek. Botheration Creek is fed by groundwater discharge and originates, in large part, on the NTC/Knight Property. Botheration Creek flows from east to west until it intersects Pine Log Creek on the southwest part of the NTC/Knight Property. Botheration Creek provides Pine Log Creek with approximately 89 percent of Pine Log Creek's flow. From the confluence, Pine Log Creek flows south and west into the Pine Log State Forest and eventually joins the Choctawhatchee River. Botheration Creek contains high quality water and a diverse mix of aquatic invertebrates and fish. Sampling at a stage recorder located approximately two miles west of the eastern boundary of the NTC/Knight Property ("BCS-01") identified 46 taxa of macroinvertebrates, including six long- lived taxa, and mussels. The water level in Botheration Creek at BCS-01 was measured to be between 0.1 and 0.32 feet by four measurements taken from October 2010 to July 2011. Nonetheless, the presence of long-lived taxa and mussels indicates that, at BCS-01, Botheration Creek is a perennial stream. Carbon export from streams provides nutrients that feed the stream system. Headwater streams like Botheration Creek and its tributaries are essential to carbon export. For carbon export to occur, a stream must have out-of-bank flood events regularly to promote nutrient exchange with the flood plain. Bay County and its Water Supply Prior to 1961, the County obtained its public water supply from wellfields located near downtown Panama City. The wellfields drew from the Floridan Aquifer. An assessment of the pre-1961 groundwater pumping appears in a District Water Supply Assessment released in June 1998. In summary, it found that near Panama City, the potentiometric surface was substantially depressed by the pumping. Due to the threat of saltwater intrusion, the Deer Point Lake Reservoir (the "Reservoir") was constructed as an alternate water supply. A local paper mill, the city of Panama City, and Tyndall Air Force Base, all began to obtain public supply water from the Reservoir. Six years after the construction of the Reservoir, the Floridan Aquifer's water levels had rebounded to pre-pumping levels. See NTC/Knight Ex. 93 at 69. The authorization for the Reservoir began in the 1950's when the Florida Legislature passed a series of laws that granted Bay County authority to create a saltwater barrier dam in North Bay, an arm of the St. Andrews Bay saltwater estuary. The laws also allowed Panama City to develop and operate a surface freshwater reservoir to supply water for public use. The Deer Point Lake Dam (the "Dam") was built in 1961 from metal sheet piling installed across a portion of North Bay. The Dam created the Reservoir. The watershed of the Reservoir includes portions of Jackson, Calhoun, Washington, and Bay Counties and covers approximately 438 square miles. The Reservoir receives freshwater inflow from several tributaries, including Econfina Creek, Big Cedar Creek, Bear Creek/Little Bear Creek, and Bayou George Creek, totaling about 900 cubic feet per second ("cfs") or approximately 582 MGD. The volume of inflow would increase substantially, at least two-fold, during a 100-year storm event. The Dam is made of concrete and steel. Above it is a bridge and two-lane county road roughly 11.5 feet above sea level. The bridge is tied to the Dam by pylons. The top of the Dam is 4.5 feet above sea level, leaving a distance between the Dam and the bridge bottom of about seven feet. There is an additional structure above the Dam that contains gates, which swing open from the force of water on the Reservoir's side of the Dam. Capable of releasing approximately 550 MGD of freshwater into the saltwater bay, the gates keep the level of the Reservoir at about five feet above sea level. The height of the Dam and the gate structure leaves a gap between the bottom of the bridge deck and the top of the structure of "somewhere between 12 and 14 inches, a little better than a foot." Tr. 140. If storm surge from the Gulf of Mexico and St. Andrew's Bay were to top the Dam and the gate structure, the gap would allow saltwater to enter the Reservoir. The gates and the Dam structure are not designed to address storm surge. The Dam is approximately four feet thick and roughly 1,450 feet long. The 12-to-14 inch gap extends across the length of the Dam. With normal reservoir levels, the volume of water it contains is approximately 32,000-acre-feet or roughly 10.4 billion gallons. Bay County needs to drawdown the lake level for fish and wildlife purposes, the control of aquatic growth, and weed control. In winter, FWS prescribes a 45-day period of time to draw down the lake to expose the banks to kill vegetation. The last time the lake was drawn down by the County, the water level dropped approximately three feet, from five feet above sea level to two feet above sea level. This process took approximately six days and 16 hours, or approximately 53 hours/foot. Repair of the Dam and its Maintenance The Dam has been repaired three times. The last repair was following Hurricane Opal which hit the Florida Panhandle in the fall of 1995. During Hurricane Opal, "saltwater . . . entered . . . the [R]eservoir . . . [t]hat took 20-some days to flush out . . . ." Tr. 135. No evidence was presented regarding the Dam's vulnerability from the perspective of structural integrity during normal or emergency conditions. Other than the inference drawn from Mr. Lackemacher's testimony that Hurricane Opal damaged the Dam in 1995, no evidence was presented to suggest that the Dam's structure is vulnerable to damage caused by a storm surge, wave effect or other conditions caused by a storm of any magnitude. After the last of the three repairs, Bay County implemented a detailed maintenance program. Based upon the latest inspection reports, the Dam is in good condition and structurally sound. No work other than routine inspection and maintenance is currently planned. The 1991 Agreement and the WTP Bay County's current withdrawal of water from the Reservoir is based on a 1991 agreement between Bay County and the District (the "1991 Agreement"). See Joint Ex. Vol. II, Tab K. The 1991 Agreement allows Bay County after the year 2010 to withdraw 98 MGD (annual average) with a maximum daily withdrawal of 107 MGD. The 1991 Agreement, still in effect, authorizes Bay County to withdraw enough water from the Reservoir to meet its needs through 2040. Water for public supply is withdrawn from the Reservoir by a water utility pump station (the "Pump Station") located a short distance from the Dam in Williams Bayou. The water is piped to the water utility's treatment plant (the "Water Treatment Plant") five miles away. The Water Treatment Plant treats 60 MGD. Following treatment, the water is distributed to Bay County's wholesale and retail customers. The Reservoir water available to Bay County utilities is more than adequate to fulfill the water consumption demands of Bay County's system through a 20-year permit horizon. The transmission line between the Pump Station and the Water Treatment Plant has fittings that were designed to allow transmission of groundwater withdrawn from groundwater wells to be located along the transmission line to the Water Treatment Plant to provide a backup supply for the Reservoir. Bay County's Current Use of Potable Water The amount of water consumed by Bay County utility customers has declined over the last five years. Bay County's current use of water, based upon the average of the 13 months prior to the hearing, was 24.5 MGD, an amount that is only 25 percent of the water allocation authorized by the 1991 Agreement. There are approximately 560,000 linear feet of main transmission lines in Bay County with small service lines accounting for another several hundred thousand linear feet. Bay County furnishes water directly to approximately 6,000 retail customers in areas known as North Bay, Bay County, and the former Cedar Grove area, which is now part of Bay County. Wholesale customers include Panama City Beach, Panama City, Mexico Beach, Callaway, Parker, Springfield, and parts of Lynn Haven. The County also furnishes potable water to Tyndall Air Force Base. Lynn Haven does have some water supply wells; however, Bay County still supplements this water supply by approximately 30 percent. No other cities serviced by Bay County produce their own water. Bay County has a population of approximately 165,000- 170,000 permanent residents, which includes residents of the cities. The Bay County area experiences seasonal tourism. From spring break to July 4th, the population can grow to more than 300,000. The users of Bay County's drinking water supplies include hospitals, Tyndall Air Force Base, and the Naval Support Activity of Panama City ("NSA"). The County has 178 doctor's offices, 56 dental offices, 29 schools, 21 fire departments, 12 walk-in-clinics, six nursing and rehabilitation homes, six major employers, three colleges and universities, and two major hospitals, all which are provided drinking water by Bay County. Panama City Beach is the community which has the highest water use. Panama City Beach's average daily use is approximately 12 MGD. The peak day of usage for all of Bay County's customers over the 13 months prior to the hearing was 40 MGD. Bay County sells water to community water utility systems referred to as a "consecutive system." They include Panama City Beach, Panama City, and Mexico Beach. Bay County's request for 30 MGD contemplates provision of water for all essential and non-essential water uses occurring within the consecutive system. Bay County and the consecutive systems are subject to the District's regulations regarding emergency water use restrictions which typically restrict the non-essential use of water during water shortage emergencies. Hurricanes, Train Wrecks, and Post-9/11 America At the District's recommendation, Bay County has been considering a backup potable water source since the mid-1980's. Bay County's main concern is that it has inadequate alternatives to the Reservoir should it be contaminated. Contamination to date has been minimal. In the period of time after the 1961 creation of the Reservoir to the present, the Dam and the Reservoir have suffered no major damage or impacts from a tropical storm. No tropical storm since 1961 has disrupted Bay County's ability to provide potable water. Even Hurricane Opal in 1995 did not disrupt the water supply. Recent hurricane activity in the Gulf of Mexico, however, has aroused the County's fears. Should a storm of sufficient magnitude make landfall in proximity to the Dam, there is potential for saltwater contamination of the Reservoir from storm surge or loss of impounded freshwater due to damage to the Dam. Mr. Lackemacher, assistant director of the Bay County Utility Department and manager of the water and wastewater divisions of the department, has experience with other hurricanes in Palm Beach, Florida, and Hurricane Hugo in Myrtle Beach, South Carolina, during which water utilities suffered disruption of their distribution systems. The experience bolsters his concern about the damage a storm could cause Bay County's source of public water supply. Bay County's intake structure at Williams Bayou is approximately one mile away from the Dam. The location of the Pump Station puts it at risk for damage from a strong storm or hurricane. There is a rail line near the Reservoir. It runs along Highway 231 and over creeks that flow into the Reservoir, including the Econfina Creek. The rail line is known as "Bayline." Bayline's most frequent customers are the paper mill and the Port of Panama City. Not a passenger line, Bayline is used for the transport of industrial and chemical supplies. In 1978, a train derailment occurred on tracks adjacent to creeks that feed the Reservoir. The derailment led to a chlorine gas leak into the atmosphere. There was no proof offered at hearing of contamination of the Reservoir. There has never been a spill that resulted in a hazardous chemical or pollutant being introduced into the Reservoir. Bay County has not imposed restrictions on the type of vehicles that are allowed to use, or the material that may pass over, the county road on the bridge above the Dam. Nonetheless, in addition to saltwater contamination, Bay County also bases the need for an alternative water source on the possibility of a discharge into the Reservoir of toxic substances from a future train derailment. Bay County is also concerned about contamination of the Reservoir from a terrorist attack. In short, Bay County is concerned about "anything that could affect the water quality and water in Deer Point Lake." Tr. 184. The concerns led Bay County to file its application for the Wellfield on lands currently owned by the St. Joe Company. Consisting of ten wells spaced over an area of approximately ten square miles, the Wellfield would have a capacity of 30 MGD. Bay County's application was preceded by the development of the District's Region III Regional Water Supply Plan and efforts to acquire funding. Funding for the Wellfield and the Region III Regional Water Supply Plan Shortly after the commencement of the planning for the Wellfield, the District, in May 2007, authorized the use of funds from the State's Water Protection and Sustainability Trust Fund ("WPSTF"). The WPSTF is intended for development of alternative water supplies. In cooperation with the District, Bay County began drilling a test well followed by analyses to evaluate the water for potable suitability. In October of the same year, the District passed a resolution to request the Department of Environmental Protection to release $500,000 from the WPSTF to the District for local utilities in Bay and Escambia Counties for "Water Resource Development." NTC/Knight Ex. 195, p. 2. The amount was to be used "to provide funding for implementation of alternative water supply development and water resource developments projects pursuant to sections 403.890 and 373.1961, F.S." Id., p. 1. In February 2008, the District began a process to develop a regional water supply plan for Bay County. If the Wellfield were designated in the applicable regional water supply plan as "nontraditional for a water supply planning region," then it would meet the definition of "alternative water supplies" found in section 373.019(1), Florida Statutes. "In evaluating an application for consumptive use of water which proposes the use of an alternative water supply project as described in the regional water supply plan," the District is mandated "to presume that the alternative water supply is consistent with the public interest " § 373.223(5). Whether the Wellfield is to be presumed to be in the public interest depends on whether the application proposes the use of an alternative water supply project as described in the District's Region III Water (Bay County) Water Supply Plan adopted in 2008. The 2008 RWSP Pursuant to the process commenced in February, the District in August 2008 produced the Region III (Bay County) Regional Water Supply Plan (the "2008 RWSP"). In a section entitled "Identification of Alternative Water Supply Development Projects," the 2008 RWSP provides the following: "All of the water supply development projects identified in Table 4 are interrelated and considered alternative, nontraditional water supply development projects." NTC/Knight Ex. 187 at 14. Table 4 of the 2008 RWSP does not specifically identify the Wellfield. It identifies three projects in general terms. The first of the three (the only one that arguably covers the Wellfield) shows "Bay County Utilities" as the sole entity under the heading "Responsible Entities." Id. at 13. The project is: "Inland Ground Water Source Development and Water Supply Source Protection." Id. Under the heading, "Purpose/Objective," the Table states for the first project, "Develop inland alternative water supply sources to meet future demands and abate risks of salt water intrusion and extreme drought." Id. The Table shows "Estimated Quantity (MGD)" to be "10.0." Id. (In July 2008, the District's executive director informed Bay County that the Wellfield could produce 10 MGD.) The "Time Frame" is listed as 2008-12, and the "Estimated Funding" is "$5,200,000 WPSPTF" and "$7,800,000 Local, NWFWMD." Id. While not specifically identified in the 2008 RWSP, Table 4's project description supports a finding that the Wellfield is, in fact, one of the inland alternative water supply sources. The 2008 RWSP, therefore, designates the Wellfield as a "nontraditional" water supply source for Region III.4/ (The Wellfield also, therefore, meets the definition of "[a]lternative water supplies" in section 373.019(1). The demonstration of a prima facie case by Bay County and the District, however, make the applicability of the presumption a moot point. See Conclusions of Law, below.) Water Supply Assessments and Re-evaluations Development of a regional water supply plan by the governing board of each water management district is mandated "where [the governing board] determines that existing and reasonably anticipated sources of water are not adequate to supply water for all existing and future reasonable-beneficial uses and to sustain the water resources and related natural systems for the planning period." § 373.709(1), Fla. Stat. (the "Regional Water Supply Planning Statute"). The District determined in its 1998 District Water Supply Assessment ("WSA") for Region III (Bay County) that the existing and reasonably anticipated water sources are adequate to meet the requirements of existing legal users and reasonably anticipated future water supply needs of the region through the year 2020, while sustaining the water resource and related natural systems. See NTC/Knight 93 at 79. In 2003, Ron Bartel, the director of the District's Resource Management Division, issued a memorandum to the Governing Board (the "2003 Re-evaluation Memorandum"), the subject of which is "Regional Water Supply Planning Re- evaluation." NTC/Knight 95 (page stamped 42). The 2003 Re-evaluation Memorandum sets out the following with regard to when a "water supply plan" is needed: The primary test we have used for making a determination that a water supply plan was "not needed" for each region is that projected consumptive use demands for water from major water users do not exceed water available from traditional sources without having adverse impacts on water resources and related natural systems. Similarly, regional water supply planning is initiated "where it is determined that sources of water are not adequate for the planning period (20) years to supply water for all existing and reasonable-beneficial uses and to sustain the water resources and related natural systems." Id. With regard to the need for a Water Supply Plan for Bay County the 2003 Re-evaluation Memorandum states: [I]n Bay County (Region III), sufficient quantities have been allocated for surface water withdrawal from Deer Point Lake Reservoir through the District's consumptive use permitting program extending through the year 2040. In this area, the District is also scheduled to complete a minimum flow and level determination for the lake by the year 2006. This determination will be useful for deciding if additional water supply planning is needed before the permit expires in 2040. Id. (page stamped 43). The 2008 RWSP's designation of the Wellfield is justified in the minutes of the Governing Board meeting at which the 2008 RWSP's approval took place: While the reservoir has largely replaced the use of coastal public supply wells historically impacted by saltwater intrusion, there remain challenges within the region that make development and implementation of a Regional Water Supply Plan (RWSP) appropriate. Development of alternative water supplies would diversify public supply sources and help drought-proof the region through establishment of facility interconnections. Development of alternative supplies would also minimize vulnerability associated with salt water potentially flowing into the reservoir during major hurricane events. Id., p. 3 of 4. The adoption of the 2008 RWSP was followed in December 2008 by the District's 2008 Water Supply Assessment Update. The update is consistent with the earlier determinations of the adequacy of the Reservoir as a water supply source for the foreseeable future (in the case of the update, through 2030). The update also voices the concern about water quality impacts from storm surge. The update concludes with the following: In Region III, the existing and reasonably anticipated surface water resources are adequate to meet the requirements of existing and reasonably anticipated future average demands and demands for a 1-in-10 year drought through 2030, while sustaining water resources and related natural systems. However, the major concern for potential water quality impacts is that resulting from hurricane storm surge. A Regional Water Supply Plan (NWFWMD 2008) has recently been prepared for Region III to address concerns associated with existing surface water systems. NTC/Knight Ex. 101, p. 3-41. The Parties Washington County is a political subdivision of the State of Florida. Washington County is located directly north of Bay County and the Wellfield and within one mile of some of the proposed wells. Washington County includes thousands of wetlands and open water systems. Because of the hydro-geologic system in the area of the Wellfield, if there are wetland, Surficial Aquifer, and surface water impacts from the withdrawal under the Permit, it is likely that impacts will occur in Washington County. Washington County has a substantial interest in protection, preservation, and conservation of its natural resources, including lakes, springs, and wetlands, and the flora and fauna that depend on these water resources, especially endangered flora and fauna. Washington County has a substantial interest in the protection of all water resources in Washington County because of the close relationship between surface waters, groundwater, and the potable water supply used by Washington County residents. NTC/Knight is the owner of approximately 55,000 acres of land located in northern Bay County and southern Washington County. The NTC/Knight Property includes thousands of acres of wetlands and open waters, including Sand Hill Lakes, steepheads, hillside seepage bogs, sphagnum bogs, littoral seepage slopes around certain Sand Hill Lakes, temporary ponds, and forested wetlands. A large portion of the NTC/Knight Property is directly adjacent to the Wellfield and within the HGL Model projected drawdown contour. Based on the projected amount of drawdown from pumping at the proposed average rate of 5 MGD, the 0.5 projected drawdown contour predicted by the HGL Modeling Report (see Finding of Fact 121, below) extends over thousands of acres of the property. NTC/Knight has a substantial interest in the protection of the surface and groundwater directly on, under, and adjacent to its property. The water supports the numerous ecosystems of extraordinary value located on the property. James Murfee and Lee Lapensohn are individuals, who reside in Bay County on property fronting on and beneath Tank Pond approximately five miles from the Wellfield. Petitioners Murfee and Lapensohn have a well which extends into the Intermediate Aquifer. The Murfee and Lapensohn properties are within the HGL Model projected drawdown contour. Petitioners Murfee and Lapensohn have a substantial interest in the protection of their drinking water supply well and the surface waters directly on and adjacent to their properties. Bay County, the applicant, is a political subdivision of the State of Florida. The District is a water management district created by section 373.069(1). It has the responsibility to conserve, protect, manage, and control the water resources within its geographic boundaries. See § 373.069(2)(a), Fla. Stat. Section 120.569(2)(p), Florida Statutes Section 120.569(2)(p), in pertinent part, provides: For any proceeding arising under chapter 373, chapter 378, or chapter 403, if a nonapplicant petitions as a third party to challenge an agency’s issuance of a license, permit, or conceptual approval, the order of presentation in the proceeding is for the permit applicant to present a prima facie case demonstrating entitlement to the license, permit, or conceptual approval, followed by the agency. This demonstration may be made by entering into evidence the application and relevant material submitted to the agency in support of the application, and the agency’s staff report or notice of intent to approve the permit, license, or conceptual approval. Subsequent to the presentation of the applicant’s prima facie case and any direct evidence submitted by the agency, the petitioner initiating the action challenging the issuance of the license, permit, or conceptual approval has the burden of ultimate persuasion and has the burden of going forward to prove the case in opposition to the license, permit, or conceptual approval through the presentation of competent and substantial evidence. The permit applicant and agency may on rebuttal present any evidence relevant to demonstrating that the application meets the conditions for issuance. Paragraph (p) was added to section 120.569(2) in the 2011 Session of the Florida Legislature. Accordingly, the final hearing commenced with the Bay County and the District's presentation of its prima facie case by submitting the application, supporting documentation, and the District's approval of the application. Respondents also presented the testimony of four witnesses in the hearing's first phase. Phase I of the Final Hearing: Bay County's Application, Supporting Documents, the District's Approval and Supporting Testimony The Application File At the final hearing, Bay County and the District offered the "application file," marked as Joint Exhibit Binder Volumes I-IV (the "Application File") in the hearing's first phase. It was admitted into evidence. A document entitled "Alternate Water Supply Report - Bay County Water Division" dated May 20, 2008 (the "Hatch Mott MacDonald Report") is contained in the Application File. See Joint Ex. Vol. I, Tab B. The Hatch Mott MacDonald Report is a preliminary evaluation of a wellfield with 22 wells, an "initial phase . . . [of] five (5) wells producing 5 MGD and the final phase . . . [of] 17 wells, producing 25 MGD." Id. at 1. The evaluation includes the gathering of information, a recommendation for the best method of treatment, an analysis of whether individual well sites or a centralized site would be superior, a hydraulic model and analysis, and the potential construction and operation costs. The report concludes in its Executive Summary: HMM's preliminary results, based upon water analysis of Well No. 1, indicate that only disinfection will be required for potable water treatment. Additionally, the hydraulic analysis indicated that the wells are capable of providing the initial 5 MGD and future 25 MGD to the proposed connection point along Highway 388 without re-pumping. Adequate storage for fire protection should be considered at current and future service areas. The use of chlorine gas at each well site during the initial phase had the lowest present worth of $16,770,270; that is, the smallest amount of funds needed today to build, operate, and maintain the system. The use of chlorine gas at each well in the final phase had a present worth of $41,245,118, only slightly more than the present worth of $40,834,245 for on-site Id. generation of disinfectant at three (3) central facilities. The Application File contains a response to a District request for additional information (the "2009 RAI Response") submitted by the Bay County Services Utility Director and received by the District in September 2009. See Joint Ex. Vol. II, Tab K. The 2009 RAI Response contains the 1991 Agreement and numerous other documents. Among them is a report prepared by HydroGeoLogic, Inc. ("HGL") entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" dated September 2009 (the "2009 HGL Modeling Report"). The report predicts impacts that would be created to the surrounding aquifers as a result of the Wellfield pumping, but recommends that additional data be obtained. The Application File contains the District's Notice dated March 25, 2010. See Joint Ex. Vol. III, Tab B. Attached to the Notice is a draft of the Permit and a staff report from the District recommending approval with conditions. Condition 11 of the Permit's standard conditions obligates Bay County to mitigate any significant adverse impacts caused by withdrawals and reserves the right to the District to curtail permitted withdrawal rates "if the withdrawal causes significant adverse impact on the resource and legal uses of water, or adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. III, Tab B, p. 3 of 17. Attachment A to the Permit requires conditions in addition to the standard conditions contained in the body of the Permit. Paragraph 12 of Attachment A, for example, requires that Bay County implement and maintain a water and conservation efficiency program with a number of goals. Attachment B to the Permit requires a monitoring and evaluation program and wetland monitoring of adjacent properties to determine if the pumping causes adverse impacts to wetland areas, including habitat and species utilization. The Application File contains a revised modeling report also entitled "Groundwater Model Development for the Assessment of a New Wellfield in Bay County, Florida" (the "2011 Revised HGL Modeling Report" or the "HGL Model Report"). See Joint Ex. Vol. III, Tab P. The 2011 Revised HGL Modeling Report predicts impacts of the pumping of the Wellfield on the Upper Floridan Aquifer and the Surficial Aquifer. The HGL Model is based on an adaptation of an original model first developed by the U.S. Geological Survey (USGS) and then further adapted by HGL. The adapted model is known as MODFLOW-SURFACT. The MODFLOW-SURFACT Model has been used in excess of 600 applications and is used worldwide. The HGL Model predicted impact from pumping when wellfield pumping achieves a "steady state." Steady state impact is achieved after 10-12 years of constant pumping. The impact and the area of impact is depicted on Figure 5.1b(1) of the 2011 Revised HGL Modeling Report. The predicted drawdown of the Surficial Aquifer is predicted to be six inches (0.5 ft) within the areas indicated. The Application File shows that the permit was revised twice. Ultimately, a Second Revised Notice of Proposed Agency Action dated July 22, 2011, was issued by the District. Attached to the Second Revised NOPAA is the District's Permit. See Joint Ex. Vol. IV, Tab U. A revised Staff Report from the District dated July 18, 2011, is also included in Volume IV of the joint exhibits. See id., Tab Q. The Permit as supported by the staff report allows an average daily withdrawal of 5 MGD, a maximum daily withdrawal of 30 MGD for no more than 60 days per year (with a maximum of 52 consecutive days), and a maximum monthly amount of 775 million gallons. See Joint Ex. Vol. IV, Tab U. The Permit also includes the LTEMP jointly prepared by the Applicant and the District. See id., Attachment B. The Permit requires Bay County to "mitigate any significant adverse impact caused by withdrawals . . . on the resource and legal water withdrawals and uses, and on adjacent land use, which existed at the time of the permit application." Joint Ex. Vol. IV, Tab R, p. 3 of 11. If the District receives notice of an impact from the existing legal user, it contacts the utility. "Within 72 hours [the utility has] a well contractor out there and they have determined what the problem is." Tr. 615. There are no time requirements for the resolution of the impact or any other resolution procedures in the Permit. Definitions of Emergency and Maintenance Amounts The Permit does not include a definition of when the Reservoir may be considered to be unavailable as a public water supply. That determination is left to Bay County. The Permit does not set a withdrawal limit lower than the limits detailed above for maintenance of the Wellfield. There is one set of withdrawal limits. They apply irrespective of the purpose of the withdrawals, that is, whether for backup in an emergency, maintenance, or some other purpose that falls under Public Supply or Industrial Use. Conditions and Monitoring Requirements Bay County is required to mitigate any significant adverse impacts on resources and legal water withdrawals and uses caused by the County's withdrawal from the Wellfield. In addition, the District reserves the right to curtail permitted withdrawal rates if Bay County's withdrawal causes adverse impacts on local resources and legal uses of water in existence at the time of the permit application. In the event of a declared water shortage, the Permit requires Bay County to make water withdrawal reductions ordered by the District. In addition, the District may alter, modify, or deactivate all or parts of the Permit. Attachment A to the Permit, states: The Permittee shall not exceed total, combined groundwater and surface water (authorized in Individual Water Use Permit No. 19910142) withdrawals of an average daily withdrawal of 98,000,000 gallons, a maximum daily withdrawal of 107,000,000 gallons and a maximum monthly withdrawal of 2,487,750,000 gallons. Joint Ex. Vol. IV, Tab U, p. 4 of 11. The inclusion of "surface water" in the condition covers withdrawals from the Reservoir. The combination of actual withdrawals from the Wellfield and actual withdrawals from the Reservoir, therefore, means that Bay County may not exceed the limitations of the withdrawals authorized by the 1991 Agreement. Attachment A to the Permit further explains how Bay County must mitigate harm caused by groundwater withdrawals. The Permittee, within seven days of determination or notification by the District that the authorized groundwater withdrawal is causing harm to the resources, shall cease or reduce, as directed by the District, its pumping activity. The Permittee shall retain the services of a qualified, licensed professional to investigate allegations of interference with an existing, legal groundwater use. The Permittee shall ensure their chosen contractor investigates the alleged interference within 72 hours of the allegation being made. If it is determined that the use of a well has been impaired as a result of the Permittee's operation, the Permittee shall undertake the required mitigation or some other arrangement mutually agreeable to the Permittee and the affected party. The Permittee shall be responsible for the payment of services rendered by the licensed water well contractor and/or professional geologist. The Permittee, within 30 days of any allegation of interference, shall submit a report to the District including the date of the allegation, the name and contact information of the party making the allegation, the result of the investigation made and any mitigation action undertaken. Joint Ex. Vol. IV, Tab U, Attachment A, p. 4 of 11. Bay County is also required, within two years from the Permit's issuance, to submit to the District for review and approval a contingency plan to mitigate potential impacts. The County must wait one full year prior to commencing withdrawal of groundwater for production purposes. During the one-year period, the County must complete groundwater, surface water, and wetland monitoring. The requirements of the mandatory monitoring are found in Attachment B of the Permit, LTEMP. See Joint Ex. Vol. IV, Tab U, Attachment B. The LTEMP "is designed to track trends in ecological and hydrological conditions caused by naturally occurring fluctuations in rainfall, which may affect ground and surface water hydrologic conditions; and to identify potential effects caused by wellfield pumping." Joint Ex. Vol. IV, Tab U, Attachment B at 1. If a substantive deviation occurs from predictions made by the HGL Modeling, or if any other hydrologic or ecologic changes due to the withdrawals are observed at monitoring sites, the District is required to review and, in consultation with Bay County, appropriately revise the LTEMP as necessary with the aim that the monitoring will assure that the conditions for issuance of the Permit are being met. Testimony in Support of the Application In addition to the documentary evidence offered in the first phase of the proceeding, Bay County and the District presented the testimony of several witnesses. These witnesses testified as to background and the 2008 RWSP, the vulnerability of the Reservoir to saltwater contamination from storm surge, and the basis for the District's decision. Vulnerability to Storm Surge There is a one percent chance every year of a 100- year storm event. Flood Insurance Rates Maps ("FIRMS") show that the 100-year water level (the level of storm surge in a 100-year storm event) at the Dam will reach 11 feet NAVD, two feet above the top of the gate structure above the Dam. The Federal Emergency Management Agency ("FEMA") and the National Weather Service ("NWS") have developed the Sea, Lake, and Overland Surge from Hurricanes ("SLOSH") model, which estimates storm surge depths resulting from historical, hypothetical, or predicted hurricanes. A Florida Department of Emergency Management's SLOSH model of the Panama City area shows maximum surge levels for Storm Categories 1, 2, 3, 4, and 5, in NAVD feet as 3.3, 5.8, 10.8, 14.1, and 18.1, respectively. The SLOSH model, in all likelihood, is a low estimation. It is reasonable to expect surge levels in a Category 3 hurricane that passes directly over the Dam, for example, to be higher than 10.8 feet NAVD predicted by the SLOSH model at the Dam. According to the National Oceanic and Atmospheric Administration's ("NOAA") database, 43 tropical storms and hurricanes have passed within 200 miles of the Reservoir between 1970 and 2010 and 20 have come within 100 miles. None have made landfall closer than 40 miles away from the Dam. Of the 20 storms passing within 100 miles of the Reservoir, four have reached Category 3 strength or higher: Eloise, Elena, Opal, and Dennis. In 2004, Hurricane Ivan made landfall over 100 miles to the west of the Dam and raised water levels near the Dam to nearly five feet NAVD. The following year, Hurricane Dennis made landfall 76 miles to the west of the Dam. Dennis produced a surge level of nearly four feet NAVD near the Dam. "Hurricane Eloise (1975) made landfall 40 miles west of Panama City and produced water levels 15 ft above normal at Panama City ([citation omitted]). However, the storm passed through the area quickly and does not appear to have significantly affected the dam." Bay County Ex. 1, p. 3 of 9. Hurricane Opal made landfall 86 miles west of Panama City Beach and produced water levels of about 8.3 feet NAVD near the Dam. The storm surge did not overtop the gate structure above the Dam, but the gates were jammed by debris. "[C]hloride levels rose above 50 ppm at the intake pumps and two to three times above normal background levels of 8 to 10 ppm 'almost one mile up-reservoir.'" Id. The levels of chloride were "still well within drinking water limits," tr. 434, of 250 parts-per- million (ppm). Hurricane Katrina made landfall in 2005 more than 200 miles west of the Reservoir with storm surges higher than 20 feet. Katrina produced surge levels of five feet above normal tide levels in Bay County. The rate and amount of saltwater that would enter the Reservoir depends on the height of the storm surge above the Dam. The 100-year surge levels could remain above the top of the Dam for three or more hours. Such an event would introduce approximately 56,200,000 cubic feet or 1,290 acre-feet of saltwater into the Reservoir, even if the Dam were to remain intact (undamaged) and the tide gates remain closed. The salinity levels bay-side of the dam are generally 23,000 to 33,000 ppm. It is reasonable to expect that in the event of a 100-year storm event, much of the storm surge would come directly from the Gulf of Mexico, which has higher salinity levels. With the Dam intact, the introduction of 1,290 acre- feet of saltwater at 33,000 ppm would raise the average chloride concentration in the Reservoir to at least 800 ppm, more than three times the maximum drinking water chloride level of 250 ppm. Assuming the Dam remained intact during a 100-year storm event, freshwater added over time to the lake from the streams and aquifer will dilute the elevated lake chloride level and restore the lake water to a level fit for human consumption. The USGS has measured stream flow at Deer Point Lake and estimated the lake receives an average of 600 million gallons of freshwater per day or 900 cfs. Post-Opal rates were estimated at 1,500 cfs by the District. Given the estimated volume of saltwater introduced to the lake, at an inflow rate equal to the estimated post- hurricane freshwater inflow rate, Bay County's expert, Dr. Miller, estimated it would take at least two weeks to reduce salinity in the lake to drinkable levels. The inflow rate, however, is not certain. Dr. Miller estimated it is reasonable to expect that it could take anywhere from two weeks to two months for the lake to recover from the saltwater intrusion depending on the variation in the inflow rate. Nonetheless, Dr. Miller assumed that the saltwater from storm surge entering the Reservoir would mix in a uniform matter. There would be "quite a bit of mixing in a storm," tr. 485, of saltwater topping the Dam and freshwater in the Dam. But there would also be stratification due to the sinking of denser saltwater and the rising in the water column of freshwater. The above estimations assume the bridge and Dam remain intact during a major storm. The Dam and tide gates act as a solid barrier, protecting the lake from saltwater in the bay. If rainfall rises in the lake prior to a surge, the tide gates would open to release water, becoming vulnerable to damage or jamming by debris as occurred during Hurricane Opal. In the event of storm surge bringing saltwater into the Reservoir, the opening of the tide gates will assist the Reservoir in reaching chloride levels below 250 ppm provided the tide gates operate properly. Dr. Janicki, an NTC/Knight expert, used the Environmental Fluid Dynamics Code hydrodynamic model ("EFDC Model") to simulate the effects of control structures and water withdrawals on the Reservoir. Taking into consideration the factors Dr. Janicki considered relevant, he predicted that chloride levels, in the event of storm surge from a Category 3 hurricane overtopping the Dam, would only exceed 250 ppm, the drinking water standard, for approximately 3.4 days. Dr. Janicki's prediction, however, was flawed. He added too little saltwater to the lake in the event of contamination from storm surge. He assumed that saltwater would be flushed too soon from the Reservoir following contamination. He did not account for the effects of waves in his model. His model was not in accord with data for Hurricane Opal and the chloride levels near the Dam taken by Bay County after Opal. If the bridge and Dam were severely damaged, more saltwater could enter the lake. With severe damage to the Dam, the Reservoir would be exposed to normal tides. Restoration would not begin until the Dam and bridge had been fully repaired. If an event were catastrophic, the Reservoir could be offline for a lengthy period of time. The Basis for the District's Decision Bay County's reliance on the Reservoir for water for the majority of the population led the District in the mid-1980s to encourage the County to obtain a backup supply. After the District turned down several requests for withdrawals of up to 30 MGD for every day of the year, the District ultimately approved what is reflected in the Permit. The justification for the permitted withdrawal is as a backup supply in the event the Reservoir becomes unavailable and for maintenance of the system and recoupment of its cost. With regard to maintenance, the District attempted to obtain information from Bay County as to appropriate withdrawal limitations. The attempts were abandoned. Despite repeated requests by the District, Bay County did not provide the amount of water needed to be withdrawn for maintenance since it did not have "infrastructure specifics," tr. 552, needed to provide the District with a numeric limit. In contrast to the amount needed for maintenance, the District found Bay County to have demonstrated that it needs 30 MGD when the Reservoir is offline and that it is reasonable for the County to need 30 MGD up to 60 days per year. The District determined that the Bay County's application met the requirements for the issuance of a consumptive use permit found in section 373.221(1)(a)-(c). In determining whether approval of the application is in the public interest, the District did not presume that it is in the public interest on the basis of the designation in the 2008 RWSP of an inland groundwater source as an alternative water supply. The District determined that it is in the public's interest for Bay County to have a reliable and safe water supply source as a backup to the Reservoir irrespective of the statutory presumption. Nonetheless, the District maintains in this proceeding that the presumption applies. The District also applied the 18 criteria test for finding a reasonable-beneficial use found in Florida Administrative Code Rule 62-40.410(a)-(r) and determined that the application should be approved. Petitioners' Case in Opposition Washington County (Petitioner in Case No. 10-2983), NTC/Knight (Petitioner in Case No. 10-2984), and Messrs. Murfee and Lapensohn (Petitioners in Case No. 10-10100) filed individual petitions for formal administrative hearing. Although not identical, the petitions share the similarity that, in essence, each alleges that Bay County failed to establish that the proposed use of water meets the statutory and rule criteria for obtaining a permit for the consumptive use of water. For example, among the many issues listed under the heading "Disputed Issues of Material Fact and Law" in Washington County's Petition for Formal Administrative Hearing is "[w]hether Bay County has provided reasonable assurance that its proposed use of water is a reasonable-beneficial use as defined in section 373.019, Florida Statutes." See p. 5 of the Washington County petition. In like fashion, the Washington County petition and the other two petitions allege that the issues are whether Bay County provided reasonable assurance that it meets the other statutory criteria in section 373.223, and the applicable rule criteria that must be met by an applicant in order for the District to issue a permit for the consumptive use of water. The Petitioners' cases focused on five topics: 1) the limitations of the HGL Model; 2) the likelihood of impacts to wetlands and the failure of the monitoring plan to provide reasonable assurance that the District's monitoring under the plan will succeed in detecting harm to wetlands caused by the withdrawals; 3) the reasonable-beneficial nature of the proposed use of the permit, including the vulnerability of the Reservoir; 4) interference with presently existing legal users; and 5) the feasibility of alternative sources. Bay County and the District offered evidence on rebuttal to meet the Petitioners' cases. Surrebuttal was conducted by Petitioners. Modeling Groundwater models "represent what is happening in very complex physical systems." Tr. 1495. Typically, the data used by models is not sufficient to obtain a completely accurate representation. The models depend on specific data points such as information from boreholes or water level measurements that do not reveal everything that is occurring in the complex system and, therefore, are not enough to support completely accurate model predictions. As explained by Dr. Guvanasen, Bay County and the District's expert, in order to reach a representation of the entire system when the data available from boreholes and measurements is insufficient, which is typically the case, the modeler must "extrapolate a lot of information and use other knowledge of other events." Id. The "knowledge of other events" that the HGL Model used included Dr. Scott's knowledge of the karst environment in the Panhandle of Florida, the mapping of Bay and Washington County geology by the Florida Geological Society, and Dr. Upchurch's knowledge of karst topography. The HGL results of the available data and the extrapolations were placed into a mathematical model (the HGL Model) that considered the withdrawals at issue to determine the response of the system to the additional stress of the withdrawals. Mathematical models like the HGL Model lead to "non- unique solutions" in which "no model . . . is exactly 100 percent correct . . . ." Tr. 1635. Modeling results, therefore, are subject to changes as additional data is collected that demand a better representation than the model provided prior to the data's collection and analysis. HGL Modeling for this case provides examples of non- unique solutions. HGL "built a model twice . . . and got two different sets of answers." Tr. 1633. Besides the recommendation that more data be obtained after the first HGL Model results, the model was not satisfactorily calibrated and the model was recalibrated for the Revised HGL Modeling results. Mr. Davis, NTC/Knight's expert, conducted additional modeling work (the "Davis Modeling"). Using the HGL Model and additional data concerning the NTC/Knight Property, Mr. Davis found drawdowns would occur over a similar but greater area than shown in the 2011 Revised HGL Modeling Report. (Compare NTC/Knight Ex. 31 at 2 to Joint Ex. Vol. III, Tab P, Figure 51b(1).) The Davis Modeling drawdowns, moreover, ranged up to 0.8 feet, 60 percent more than the 0.5 feet determined by the second HGL Modeling results. In the area of Big Blue Lake, for example, the drawdown contours produced by the Davis Model were either 0.6 feet or 0.7 feet, 20 to 40 percent more than the 0.5 feet produced by the second HGL Modeling results. See NTC/Knight Ex. 31 at 2. Asked to rank the modeling results between the first HGL Model run, the second HGL Model run, and his own results, Mr. Davis was unable to say which was better because of the sparseness of the data. Mr. Davis opined that he could conduct another "dozen more model runs," but without additional data he would be "hard pressed" to be able to say which run was more accurate. Tr. 1633. In Mr. Davis' opinion there remain significant uncertainties that cannot be resolved without more data. Inadequate data "precludes . . . reasonable assurance as to exactly where the impacts will travel and exactly what the magnitude of those impacts will be . . . ." Tr. 1637. Ecological Impacts Bruce A. Pruitt, Ph.D., was accepted as an expert in hydrology, soil science, fluvial geomorphology, and wetland sciences. Dr. Pruitt mapped the soil types on the NTC/Knight Property using the Natural Resource Conservation Service ("NRCS") Web Soil Survey and tested soil types by hand-auguring in wetland areas. He characterized the various soil-types on the property by drainage class (relative wetness of the soil under natural conditions) and hydraulic conductivity (permeability). Dr. Pruitt ranked the vulnerability of wetlands within the zone of drawdown predicted by the HGL Model as "very high," "high," or "moderate." The categories were based on the presence of threatened and endangered species, Florida Natural Area Inventor ("FNAI") habitat designation, and the hydrology of the wetland. He assumed that if the water level in the Surficial Aquifer were to be drawn down by 0.3 feet or 0.4 feet then the water level in the seepage bogs at Botheration Creek would be drawn down by the same amount. Wetlands with a vulnerability classification of "very high" will suffer an adverse impact at a drawdown level of 0.2 feet; those at "high" at 0.3 feet and those at "moderate" at 0.5 feet in times of drought. Dr. Pruitt calculated wetland acreage by type using the Florida Cover Classification System. He assigned vulnerability rating for the wetlands within the Surficial Aquifer drawdown contours generated by the HGL Model. Based on Dr. Pruitt's calculations, a total of approximately 4,200 acres of wetlands are likely to be harmed by the predicted drawdown. A majority of these wetlands are located in Washington County. Based on Dr. Pruitt's analysis, it is likely that the NTC/Knight Property contains 1,981 acres of "very highly" vulnerable wetlands; 1,895 acres of "highly" vulnerable wetlands; and 390 acres of "moderately" vulnerable wetlands, which are likely to be harmed by the drawdown in times of drought. In reaching his opinion about the quantification of acres of wetlands likely to be harmed, Dr. Pruitt applied the Florida Uniform Mitigation Assessment Method ("UMAM"). UMAM was designed to address compensatory mitigation in dredge and fill cases. It was not designed for consumptive water use cases. In contrast and damaging to its case of reasonable assurance that natural systems will not be significantly affected, the District did not conduct an analysis to determine loss of wetland function resulting from operation under the Permit. Nor did it determine how much drawdown the affected wetlands could tolerate before they were harmed. Rather than conducting such an analysis, the District chose to rely on implementation of the LTEMP to cure any harm that might be down by drawdown to the Surficial Aquifer. The District and Bay County's wetland scientists opined that there might be a less permeable restrictive layer maintaining water levels above the Surficial Aquifer on the NTC/Knight Property. Dr. Pruitt acknowledged that the NTC/Knight Property had scattered clay layers beneath the surface. It is possible, therefore, that some of the wetland areas he identified as subject to harm have restrictive features under them which would hold water and resist dehydration. In his hand-auguring, however, Dr. Pruitt found no evidence of a less permeable layer. The auguring only went to a depth of three feet and would have to go to a depth of two meters to be definitive. Furthermore, Dr. Pruitt found no evidence of a less permeable layer from well drillings. The District and Bay County did not prove that there is, in fact, such a restrictive layer. NTC/Knight collected water-level data from shallow hand-augured wells and stage recorders at the Botheration Creek Hillside Seepage Bog. The data demonstrate that the water level in the shallow, hand-augured wells at the Botheration Creek Bog is a direct reflection of the level of the Surficial Aquifer. The Surficial Aquifer at the Botheration Creek Bog was approximately 95.5 feet NAVD, over 35 feet higher than at Big Blue Lake and the highest measured level south of Big Blue Lake. The Botheration Creek Hillside Seepage Bog is located between the 0.3 and 0.4 foot Surficial Aquifer drawdown contours predicted by the HGL Model. Based on the HGL Model, the District and Bay County's experts estimated the Surficial Aquifer drawdown at this bog would be 0.39 feet. During the approximately one year of NTC/Knight's water-level recording, a drawdown of 0.39 feet would have reduced the frequency and duration of inundation at this bog significantly. For example, an analysis of the approximately one year of data collected by NTC/Knight shows that at the intermediate water-level recorder location in the bog, one 29-day period of inundation would have been reduced to just nine days and that further down gradient in the bog, none of the five instances when the bog was inundated would have occurred. This is consistent with Dr. Pruitt's vulnerability assessment, which finds that the vulnerability of the hillside seepage bogs to drawdown is "very high," that is, these systems are likely to be harmed in times of drought at drawdown levels in the Surficial Aquifer of 0.2 feet or greater. A drawdown of 0.3-0.4 feet in the Surficial Aquifer at the hillside seepage bog along Botheration Creek increases the likelihood that the hillside seepage bogs along Botheration Creek will be lost in times of drought. The littoral shelves of Sand Hill Lakes typically occur along a low gradient above the normal low water level of the lakes. The existence of the shelf promotes seepage sheet flow along a wide expanse. The drawdown will change the flow from seepage sheet flow to concentrated stream flow within gullies. The erosion and increased sedimentation produced by the greater force of the water in the gullies will cause a loss of area needed by certain seepage dependent plants and animals. If Big Blue Lake were to be drawn down by the 0.71 feet predicted by Mr. Davis, the location of the seepage would move down 0.71 feet vertically and an estimated 24.5 feet horizontally. The result would be a reduction in the littoral shelf conducive to seepage-dependent plant communities by approximately nine acres. The impact would likely be significant since the seepage zone is in an area of "very high" vulnerability according to Dr. Pruitt. Between October 2010 and July 2011, NTC/Knight took four measurements of water level at "BCS-01," a stage recorder in Botheration Creek. The measurements showed the water level in the creek at that point to be 0.1 to 0.32 feet. NTC/Knight also sampled for taxa of macroinvertebrates in the reach of the creek. NTC/Knight identified 46 taxa, including mussels and six long-lived taxa. The presence of the long-lived taxa and mussels indicate that the reach of the creek in the vicinity of the stage recorder should be considered to be a perennial stream. Botheration Creek is high-quality water and, as shown by NTC/Knight's sampling, it contains a diverse mix of aquatic invertebrates and fish. A drop in the level of Botheration Creek of 0.2 feet predicted by the HGL Model would have caused the creek to go dry at BCA-01 during three of the four dates on which the water level was measured. Such a drop would convert the reach of the creek in the vicinity of the stage recorder from a perennial to an intermittent stream and would eliminate the reach's viability for long-lived taxa. Similarly, upstream reaches that are intermittent would become ephemeral (streams that flow only during periods of high rainfall). If the Wellfield becomes fully operational as allowed by the Permit, there will be a reduction in the Surficial Aquifer at Botheration Creek of between 0.2 and 0.3 feet. The reduction in the aquifer will reduce flow in Botheration Creek, reduce the volume downstream, including in Pine Log Creek, and reduce out-of-bank flood frequency and duration. The result will be a reduction in nutrients delivered downstream and to the floodplain to the detriment of plants and animal life that depend on them. Additionally, other reaches of the creek that have perennial flow will be converted to intermittent streams and reaches that are intermittent will become ephemeral. The result will be the elimination of plant and animal species currently living in these portions of the creek. The impact of the HGL Model predicted drawdown to steepheads depends on the individual steephead and the drawdown contour at its location and the amount of rainfall. Four steepheads on the NTC/Knight Property could suffer impacts similar to the impact at Russ Steephead to which Dr. Pruitt assigned a high probability of impact. Russ Steephead is located on the NTC/Knight Property above Russ Pond. NTC/Knight installed Surficial Aquifer wells at Russ Steephead between the HGL Model's predicted 0.5 and 0.6 foot Surficial Aquifer drawdown contours. NTC/Knight also installed a stage recorder just downstream from the steephead. During drought, NTC/Knight observed a loss of flow from the sidewall seepage areas and in the Russ Steephead Stream. If the Surficial Aquifer at Russ Pond were to be drawn down by 0.5-0.6 feet, the sidewalls of the Russ Steephead Stream and the stream itself would lose flow in times of drought. The loss of flow would lead to oxidation and loss of organic materials in the stream channel and flood plain, resulting in soil subsidence. If the water level at the terminus of the Russ Steephead Stream were drawn down, headward down cutting in the stream channel would be induced. In such a case, in the words of Dr. Pruitt, "there is a high probability that if drawdown occurs and . . . over a long period of time," the process will make the steephead "look more like a gully . . . ." Tr. 2120. The drawdown will also reduce the frequency and duration of inundation of the sphagnum bogs in the four steepheads likely to be affected by the drawdown. The bogs and the associated animals that depend upon them would be lost. Dr. Means identified a number of temporary ponds within HGL's predicted drawdown of the Surficial Aquifer. Nine were between the 0.3 and 0.6 foot drawdown contour, and two were between the 0.6 and 0.7 foot drawdown contours. These ponds and plant and animal communities dependent upon them would likely be harmed by the drawdowns. Mr. Cantrell offered testimony to rebut the Petitioners' case on wetland impacts. His testimony was based on an evaluation of aerial photography, site visits to the Wellfield, and a one-day trip to the NTC/Knight Property. It is Mr. Cantrell's opinion that if the NTC/Knight Property were to drain, it would be because of a surface water drainage system, such as ditching, not because of drawdown in the Surficial Aquifer caused by operation of the Wellfield. Mr. Cantrell's opinion is that because the Area has been subjected to a wide range of fluctuations in water levels and the wetland systems have survived, operation of the Wellfield will not have significant impacts. Mr. Cantrell's opinion, however, overlooks the effect of constant drawdown during times of severe drought. That wetlands have survived severe drought in the past does not mean they will survive severe drought conditions exacerbated by drawdown caused by operation of the Wellfield. Monitoring Special condition 19 of the Permit requires Bay County to implement the LTEMP after the Permit is issued. The LTEMP requires Bay County to establish a monitoring network, but does not provide the location of any particular monitoring site. Sites identified in the LTEMP are recommended, but the ability to use a particular site is dependent on field verification of suitability and authorization by the landowner. Over half the area designated in the LTEMP from the HGL Model's projected 0.5 foot drawdown in the Surficial Aquifer is located on the NTC/Knight Property. It will be necessary, therefore, to include sites on the NTC/Knight Property in the ultimate environmental monitoring network. The LTEMP's recommended sites do not include monitoring of some of the most susceptible wetland systems: temporary ponds, the Botheration Creek hillside seepage bogs, and the perennial headwaters of Botheration Creek. Without this monitoring, the LTEMP will be unable to detect whether these systems are harmed by withdrawals. The Permit and LTEMP require no more than one-year of baseline data to be collected prior to initiation of water withdrawals. The proposed monitoring time is inadequate to create a sufficient record for use in determining whether a reduction in water levels is attributable to water withdrawals or natural phenomena, such as drought. Baseline monitoring should be conducted for a sufficient duration to ensure that a full range of wet and dry years is captured. The LTEMP describes the types of data that are to be collected. A missing component is sampling for frogs, salamanders, and other amphibians that are sensitive to changes in hydrologic regimes and which depend upon infrequent periods of inundation in order to breed. This type of faunal sampling is particularly important in the temporary ponds and seepage environments. Without sampling for the presence of these species, the LTEMP will be unable to determine whether these populations have been harmed by withdrawals. The LTEMP includes a number of "triggers," that if tripped, require the preparation of an auxiliary report. A number of these triggers make reference to changes in water levels at the level of "significant deviation," an undefined term. More importantly, the LTEMP fails to require any statistical analysis. Without it, the LTEMP will be inadequate to establish whether a reduction in water levels is caused by water withdrawals or another cause. Similarly, other triggers lack sufficient detail to determine when they are tripped, such as those that refer to downward movement of plants. Finally, even if one of these triggers is tripped and an auxiliary report is prepared, nothing in the Permit or LTEMP sets forth the circumstances under which withdrawals would need to be curtailed and by what amount. The purpose of the LTEMP is to determine whether withdrawals are causing harm to the wetlands within the vicinity of the Wellfield. The LTEMP fails to provide reasonable assurance that it will succeed in achieving its purpose. Reasonable-Beneficial Use Use if the Reservoir is Unavailable In the event of Reservoir unavailability, Bay County is likely to need much less than 30 MGD. The need is likely to fall between 7.42 MGD and 9.71 MGD for the current population. In 2013, the need is likely to fall between 9.40 MGD and 12.29 MGD. See NTC/Knight Ex. 5, p. 4 of 4. The Permit, however, does not limit Bay County to emergency or backup use. While Bay County might voluntarily limit withdrawals to emergency use or backup supply, it has unfettered discretion to determine what constitutes an emergency or the necessity for a backup supply. The Permit is also not restricted to essential uses. Authorization of 30 MGD provides more than Bay County's current average daily demand for potable water. If the Permit restricted the use to essential uses, the authorization would be far less than 30 MDG. The District commissioned King Engineering to assist in development of a "Coastal Water Systems Interconnect Project" (the "Interconnect Project"). On average, the utilities subject to the Interconnect Project estimated that 42 percent of the average daily demand is dedicated to essential uses with the remaining 58 percent going to non-essential uses. Consistent with the estimate, the Project set a target of 50 percent of average daily demand to be allowed for use in an emergency. None of the information from the Interconnect Project, however, was used by the District in setting the limits of withdrawal in the Permit. b. Daily Use Bay County claims the 5 MGD annual average allocation under the Permit is needed for several reasons, principally the maintenance of pumps. Bay County's justification for 5 MGD is found in testimony from Mr. Lackemacher and a document he authored entitled, "Confidential Draft for Internal Use Only 5 MGD Pumping Rate" (the "Lackemacher Confidential Draft"), admitted as Bay County Ex. 24. Mr. Lackemacher's testimony follows: A. The fact is that there are no absolute knowns when we're talking about what needs to be. Q. What do you mean? A. Well, here we have a document [Bay County Ex. 24] where I talk about rationalization for 5 million gallons a day, why we would need it, mechanical reasons, financial reasons, regulatory reasons. I always felt that it was very difficult to justify a number. I don't know. We haven't designed the system. We haven't got all of the wells in. We don't know what their specific yields are. There's unknowns here. So do we need 2 million gallons a day or 5 million gallons a day? I don't know. I don't know that. But here is the rationalization for 5 million if that's in fact what we need. We may very well find out that we don't need 5 million gallons a day. Q. Is that because you don't know the precise locations of the well and how they're going to be piped and distributed? A. That's absolutely true. Q. Well, did you in this report, Exhibit 24, did you make some reasonable assumptions? A. I based it on some of the values as you discussed or as I pointed out earlier from Hatch Mott MacDonald's preliminary design. * * * Q. And do you feel confident that your analysis supported that in the area of 5 million gallons a day is what would be needed to operate the wellfield? A. Yes. And that's why the paper was generated that [is] a justification for 5 million gallons a day, here's what we think we would need. Tr. 209-10. The Lackemacher Confidential Draft is a one-page, written justification for the 5 MGD. Based on the Hatch Mott McDonald Report, see tr. 210, it considers regulatory, mechanical and financial factors. It is not supported, however, by engineering analysis. Any financial analysis found in the Hatch Mott McDonald Report, moreover, is far from complete. The factors taken into consideration are recited in the most general of terms. For example, of four such factors, the document lists the second as: "All water pumps are designed to run - turning pumps on and off is not the best situation for the overall electrical efficiency or the mechanicals of a pump." Bay County Ex. 24. Consistent with Mr. Lackemacher's testimony, the document concludes that the amount of water needed to run each well is unknown. The financial justification is based on costs shown in the Hatch Mott MacDonald Report for construction and operation of 22 wells, ten more wells than are contained in the Wellfield and without any analysis of revenue to recoup the costs. The financial justification is a bare conclusion on the part of Mr. Lackemacher: We cannot afford to operate a well field at a financial loss, based on this fact alone we would have to pump a minimum of 4.49 MGD. Combined with the fact that we don't know what volumes of water have to be turned over to ensure water quality 5 MGD seems quite reasonable. Bay County Ex. 24. The Lackemacher Confidential Draft is dated May 17, 2011. It was not part of Bay County's Application nor was it submitted to the District prior to the decision to issue the Permit. Although the District attempted to obtain information from Bay County about what was needed for maintenance, Bay County did not provide it. As Mr. Gowans testified, "[t]hen I finally told staff, [s]top asking, we're not going to get the numbers . . . ." Tr. 552. The District performed no analysis to determine the minimum amount of water needed to maintain the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Phillip Waller, an engineer accepted as an expert in the design and construction of potable water systems, including groundwater wells, surface water, and transmission and distribution of drinking water. Mr. Waller testified that if the wells were connected to a central treatment system, there would not be the need to flush the pipeline for disinfection prior to use of the well in an emergency. Only 2.4 million gallons per year or 6,500 gallons per day would be needed to maintain optimum operating conditions, an amount far less than 5 MGD. Mr. Waller's experience when groundwater is used as a backup, moreover, is that they are operated periodically. While prudent to periodically operate backup wells especially in advance of hurricane season, vertical pumps in wells, unlike horizontal pumps, do not have a need for frequent operation because of even force distribution. They certainly do not need to be continuously operated. "In fact, wells routinely are idle for months at a time." Tr. 1123. Interference with Existing Legal Users In its Revised Staff Report dated July 18, 2011, the District wrote: Nearby Users: Under the most intensive pumping activity, drawdown in the Upper Floridan Aquifer is predicted to be approximately 15 feet in the vicinity of the nearest private wells. Water level declines of this magnitude may cause water levels to fall below the level of the pump intake in some privately-owned wells. Joint Ex. Vol. IV, Tab Q, p. 4. The District's high estimate of the number of wells used by existing legal users that might suffer impacts approaches 900. The exact number or whether any existing legal users would be likely to suffer impacts was not proven. Alternatives Groundwater wells, if installed and attached to the fitting in the existing transmission line that delivers water from the Pump Station to the Water Treatment Plant, could serve as backup to the Reservoir. Bay County did not conduct a study of whether groundwater in the area of the transmission line was adequate to serve as an alternative. Mr. Waller, on behalf of NTC/Knight and Washington County, on the other hand, testified that the transmission line could support ten wells with a capacity of 10 MGD and could be constructed at a cost of $12 million, far less than the Wellfield. The area of the transmission line is in an area identified by the District as acceptable for the creation of potable water wells. The area does not present a significant risk of saltwater intrusion if not used continuously. The water meets the drinking water requirements for the Department of Environmental Protection and the Department of Health. The existing transmission line alternative is located near the existing raw water supply line which minimizes the need for additional piping. There is sufficient length along the existing raw water pipeline to accommodate ten wells. The existing transmission line alternative, therefore, has significant potential to succeed as a water supply backup to the Reservoir. NTC/Knight and Washington County, through Mr. Waller, also proposed another alternative: an intake at Bayou George. Near Highway 231, the main pipeline from the intake would run along public right-of-way. North of the existing intake in Williams Bayou and three miles north of the Dam, the proposed intake would be less susceptible to contamination from storm surge. Neither Bay County nor the District presented a thorough analysis of any alternative to the Wellfield. In contrast, NTC/Knight and Washington County presented the testimony of Mr. Waller that there are two alternatives that could be constructed at much less cost than the Wellfield and that have significant potential of providing backup supply.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Northwest Florida Water Management District enter a final order that denies the application of Bay County for the individual water use permit at issue in this proceeding. DONE AND ENTERED this 26th day of July, 2012, in Tallahassee, Leon County, Florida. S DAVID M. MALONEY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 26th day of July, 2012.
The Issue The issues for determination in this proceeding, are as follows: Whether St. Johns' Rules 40C-2.301(4)(d), and (i), F.A.C. [adopted, as well, in the Applicant's Handbook as Sections 10.3(D),(H) and (I)] are invalid exercises of delegated legislative authority, because of vagueness and arbitrariness. because, to the extent water quality is regulated, St. Johns has exceeded its statutory authority. Whether St. Johns utilizes an unwritten, and, therefore, invalid rule for determining allowable parts per million of phosphorus and nitrogen. Whether St. Johns' policy of reliance on Department of Environmental Regulation (DER) Rule Chapter 17-3, F.A.C., constitutes an invalid rule. MATERIAL ADMISSIONS AND STIPULATIONS In Stipulations filed at or before the hearings on November 22, 1988 and February 27, 1989, the parties have agreed as follows: Zellwood Drainage and Water Control District and the individual Petitioners in this case have standing to bring this Section 120.56, F.S., rule challenge. Zellwood filed a timely consumptive use permit application with St. Johns, as an existing use. St. Johns classified the application as one for an existing use. The review of the application occurred in December 1985. The sole basis of St. Johns' recommended denial is Zellwood's alleged non-compliance with Rules 40C-2.301(4)(d), (h), and (i), F.A.C., and those same provisions found in Section 10.3(D), (H) and (I) of the Applicant's Handbook. The factual basis of St. Johns' denial of Zellwood's consumptive use permit application is the quality of the water discharged into Lake Apopka and the effect the discharge has on the lake. In its admissions filed at the February 27, 1989 hearing, St. Johns admits that unless an applicant has an operation permit issued by DER, St. Johns uses the State Water Quality standards in Chapter 17-3, F.A.C. (DER's rule) in deciding whether a use of water causes serious harm to the water quality of source or receiving waters, pursuant to Rules 40C-2.301(4)(h) and (i), F.A.C., and whether a use of water has reduced environmental or economic harm to an acceptable amount pursuant to Rule 40C-2.301(4)(d), F.A.C.
Findings Of Fact Petitioner, Zellwood Drainage and Water Control District was created as a special district in Orange County, Florida, by act of the Legislature, Chapter 20714, Laws of Florida, in 1942. The district is located south and west of the town of Zellwood, along the northeast shore of Lake Apopka, and comprises approximately 8700 acres. The district is governed by a board of governors; William Rex Clonts, Jr. is currently Chairman. Plainly stated, the purpose of the district is to make its lands suitable for farming by maintaining pumps, canals, a dike, roads and other improvements. The land within the district is lower than the level of the lake and surrounding land. Without drainage, the land could not be farmed. The individual petitioners are farmers owning land and farms within the district. There are approximately twelve farms, primarily family-owned, growing broccoli, carrots, celery, leaf lettuce, radishes, greens, sweet corn and sod. The farms within the district, utilizing the improvements of the district, pump water from Lake Apopka for nematode control and for irrigation in times of dry seasons. Except when the water is allowed to evaporate off the fields, water is then discharged back into Lake Apopka. Water is also discharged for flood control. When water is used as described above, it moves across the lands and it tends to pick up nutrients depending on the composition of the soil and the concentrations of the soil in the water. Almost every consumptive use of water has an associated discharge. From a regulatory standpoint, water quality and water quantity are intertwined. Both withdrawal from and discharge to a waterbody can degrade the water quality of that body. The only consumptive use permit applications denied by St. Johns on the basis of the quality of the discharge water are Zellwood's, Duda Farms', and other neighbors of Zellwood near Lake Apopka. However, in cases other than these St. Johns has recognized water quality problems and has issued water use permits with conditions which would help remedy the problem. When reviewing a consumptive use permit application such as Zellwood's, St. Johns applies, among others, these relevant provisions of its Rule 40C- 2.301, F.A.C.: 40C-2.301 Conditions for Issuance of Permits. To obtain a consumptive use permit for a use existing on the effective date of implementation, the applicant shall apply for a permit under the provisions of Section 373.226, Florida Statutes, and Rule 40C- 2.04(2), Florida Administrative Code, and shall establish that it is a reasonable beneficial use and is allowable under the common law of Florida. * * * The following criteria must be met in order for a use to be considered reasonably beneficial: The use must be such quantity as is necessary for economic and efficient utilization. The use must be for a purpose that is both reasonable and consistent with the public interest. The source of the water must be capable of producing the requested amounts of water. The environmental or economic harm caused by the consumptive use must be reduced to an acceptable amount. To the degree which is financially environmentally, and socially practicable, available water conservation and reuse measures shall be used or proposed for use. The consumptive use should not cause significant saline water intrusion or further aggravate currently existing saline water intrusion problems. The consumptive use should not cause or contribute to flood damage. The water quality of the source of the water should not be seriously harmed by the consumptive use. The water quality of the receiving body of water should not be seriously harmed by the consumptive use. A valid permit issued pursuant to Rule 17-4.240 or Rule 17- 4.260, Florida Administrative Code, shall establish a presumption that this criterion has been met. (emphasis added) Rules 17-4.240 and 17-4.260, F.A.C. are DER rules relating to operation permits for water pollution sources, and permits for sewage works, respectively. Zellwood contends that the standards in 40C-2.301(4)(d), (h) and (i), F.A.C., above, have no scientific meaning, do not put the applicant on notice as to what discharge would be permitted, and leave too much discretion to the agency. Sanford "Sandy" Young is an environmental consultant who testified on behalf of Zellwood. He specializes in limnology, the study of physical, chemical and biological aspects of fresh water. Young claims that the language of the rules is too vague to allow him to advise a client. He contrasts these rules with the DER water quality standards in Chapter 17-3, F.A.C., adopted by the Environmental Regulation Commission, which do include specific numbers where possible. St. John's department of resource management is responsible for reviewing and processing permit applications, including applications for consumptive use permits. In addition to using its own staff of engineers, hydrologists, and environmental specialists, the Department consults with its sister department of water resources, the district's program and research department, for additional technical expertise. On matters related to water quality, St. Johns' staff also consults with DER staff. St. Johns uses the provisions of DER rule Chapter 17-3 to measure the "serious harm" referenced in St. Johns' rules. Rule 17-3.121(19), F.A.C., sets the standard for nutrients in surface waters classified as Class III, such as Lake Apopka, as follows: (19) Nutrients - In no case shall nutrient concentrations of a body of water be altered so as to cause an imbalance in natural populations of aquatic flora and fauna. The nutrient standard provided in Rule 17-3.121, F.A.C., above, requires a site specific determination of the volume and concentrations of the nutrients that are discharged. The point at which an imbalance would be created is different from different bodies of water. Nutrients behave in a very site specific fashion, and in order to derive a scientific estimate of nutrient criteria for a specific body of water, the characteristics of that body have to be taken into account. It would be impossible to develop a numerical standard which would apply to all. The nutrient standard in Rule 17C-3.121, F.A.C. is applied, therefore, on a case-by-case basis. In permit application review, when there is not sufficient time to do actual field samplings and to run an exhaustive model of nutrient loading, the staff relies on available data, available literature and what is provided in the application itself, to make a recommendation to the district board regarding approval or denial. The staff's recommendation as to Zellwood was based on published literature on Lake Apopka and its existing water quality conditions and on available data from consultants on the quality and quantity of discharge and quantity from the Zellwood farms. As a rule of thumb, in this case, and not as an official district policy, the staff felt that .1 milligram per liter phosphorus, and 2 milligrams per liter nitrogen, would be an acceptable working level for discharge into Lake Apopka. That level itself would also depend on the amount of water being discharged. The .1 milligram and 2 milligrams level assumes a discharge of 20 billion gallons per year. The staff, in establishing such levels in consumptive use permits, strives to establish a discharge that will not contribute to the water quality of the receiving body staying below Class III standards (when that Class has been designated by DER). St. Johns has not adopted the nutrient level described above as a rule, but neither does it apply the level generally to other permit applications. Without a given volume of water, without knowledge of the ecological state of the receiving body, it is impossible to determine whether a given nutrient concentration, such as the parts per liter of nitrogen and phosphorus described above, would cause an imbalance of natural flora and fauna in the receiving body. St. Johns has adopted Rules 40C-2.301(4)(d), (h) and (i), F.A.C., in accordance with the rulemaking provisions of Section 120.54, F.S. In addition, Chapter 40C-2, F.A.C., has been reviewed by DER and accepted without objection as consistent with Chapter 17-40, F.A.C., the state water policy, and other applicable statutory standards.
The Issue The issue for consideration herein is whether Sarasota County Utilities should be issued a consumptive use permit to draw water from the 14 wells in issue here located in Sarasota County.
Findings Of Fact At all times pertinent to the issues herein, the Respondent, District, was the state agency responsible for themanagement of water resources within its area of geographical jurisdiction. Included therein was the responsibility for the permitting of consumptive water use. The Respondent, Sarasota County, is a political subdivision of the State of Florida and operates a public utilities division which is charged with meeting, among other things, the potable water needs of the residents of the County. Petitioners Wyatt S. Bishop and Joan Jones are both residents of Sarasota County and both draw their potable water from wells which utilize the aquifers pertinent to the wells for which the permit in issue here relate. Mr. Bishop lives approximately 7.5 miles north of the Carlton Reserve, the property on which the wells in issue are located, and Ms. Jones lives approximately 7 miles from the Reserve, but in a different direction. Sarasota County filed an application for a consumptive use permit with the District on January 28, 1987 requesting an average daily withdrawal of 10.71 million gallons per day, (mgd), and a peak monthly withdrawal of 15.55 mgd. This application, assigned number 208836.00, was, over the next three years, amended by the County four separate times. These amendments reflected revised water demand determinations and were submitted to provide additional information requested by the District. The District issued a preliminary staff report and proposed intent on March 26, 1991 reflecting an approved withdrawal in the amount of 7.28 mgd average daily withdrawal and 11.1 mgd peak monthly withdrawal. These figures were revised, however, byan amendment by the District on July 8, 1991, and as amended, authorize 7.303 mgd average daily withdrawal and 9.625 mgd peak monthly withdrawal. The County's application was reviewed by an experienced hydrologist in the District office with extensive permit review experience who utilized, in his evaluation of the permit, the pertinent District rules and policies. By way of background, to more easily understand the circumstances here, Sarasota entered into a contract with Manatee County in 1973 which called for the latter to provide up to 10 mgd of water for a period of 40 years, up to and including the year 2013. However, in 1979, Manatee County's utilities director advised Sarasota County that it, Sarasota County, could not continue to rely on Manatee County's water after the expiration of the current contract, and would, therefore, have to become self sufficient in water. Since the MacArthur tract, now known as the Carlton Reserve, had just recently been identified by, inter alia, the United States Geological Service as a potential long term water source for Sarasota County, after Manatee County advised Sarasota County of its future expectations, Sarasota County and the Manasota Basin Board hired a consulting firm to conduct hydrological testing on the Carlton Reserve. This study concluded that the Reserve had sufficient water resources to satisfy the needs of the unincorporated areas of Sarasota County for an extended time into the future. In 1985, because of its increased water needs and thetime necessary to complete required studies on the utilization of the Myakka River, a surface water resource, Sarasota County concluded that it was suffering a water supply shortage and entered into a supplemental contract with Manatee County to provide 2 million gallons of water per day over a 5 year period which would expire in 1990. Sarasota County had not, however, been idle with regard to the investigation of other water resources. Studies done included not only the Myakka River mentioned above but a reservoir owned by the City of Bradenton, and the Peace River. Nonetheless, it was determined that the Carlton Reserve was the best source available overall, and in 1987, the County filed the application in issue here. The permit was under consideration for approximately 3 1/2 years before the initial decision by the District to grant it. During that time the County experienced a significant deficiency in its water sources and found it necessary, on February 5, 1991, to enter into another contract with Manatee County to supply an addition 5 mgd. Terms of that contract clearly indicate the expectations of both parties that Sarasota County will take reasonable steps to develop its own water resources. It is not as though Sarasota County sat quietly in the interim, however, and allowed the situation to develop. A building moratorium to halt additional construction was proposed and as a result, economic forces in the County indicated a potential loss of jobs to County residents. None of this would be desirable from an economicstandpoint. In the course of the permit application process, 12 test wells were sunk to conduct aquifer pump tests; to assess water quality, amounts and availability, aquifer characteristics and drawdown; and to determine the impact of withdrawal on water quality. Eight of these 12 wells are located on the Carlton Reserve. The other 4 are located on property owned by the MacArthur Foundation which is contiguous to the Carlton Reserve property and from which Sarasota has a right by easement to draw water. The 2 wells yet to be constructed will be on Sarasota County property. Sarasota County currently receives 10 mgd of water under its contract with Manatee County; an additional 5 mgd under the February 5, 1991 contract; 2 mgd from the University wellfield, (with a peak withdrawal rate of 3 mgd); and .9 mgd from the Sorrento wellfield, (with a peak withdrawal rate of 1.1 mgd). This latter source is only producing currently .6 mgd of potable water due to constraints imposed by the water treatment requirements. Taken together, the current Sarasota County supply constitutes 18.6 mgd. The above does not take into account the County's agreement with the City of Sarasota calling for the purchase of up to 2 mgd. Since this source is not reliable, it is not included in the total, and the City is not considered an available water source. In addition, the District and Sarasota County stipulated on July 15, 1991 that within 30 days, the County would apply tophase out routine water production from the Sorrento wellfield, relying on it only in emergency situations with District consent. For this reason, it, too, is not considered an available water supply source. These currently existing sources, with modifications as described, will be the primary sources of potable water provided to 6 major service areas in Sarasota County when the County's water treatment plant and transmission system are complete in 1993. In attempting to define the County's future water requirements, two major criteria were considered. The first was the County's historical water demand, and the second, modifying it, relates to the demand arising as a result of new water users being added to the system as a result of the County's capital improvements and acquisition program. Water resources are not unlimited. Current resources come primarily from Manatee County and there are constraints on this supply as it is made available to Sarasota County. For example, the 10 mgd contract expires in 2013. The 5 mgd contract expires in 2001. Though the latter is subject to renewal, renewal is contingent upon the availability of water supply at that time, and that is not a sure thing. It can, therefore, readily be seen that 15 out of the 18.6 mgd routinely available now comes from Manatee County, and those sources are not perpetual. In addition, it is conceivable that Manatee County may pre-blend the water it delivers to Sarasota County with water of lesser quality, so that the delivered water may exceed the total dissolved solids standard of 500 ppm for potable water. If thewater from Manatee County were reduced to that quality, the University wellfield supply, which currently exceeds standards itself, and which relies on blending with better quality Manatee County water to be potable, would also be removed as a source of potable water to Sarasota County. In order to comply with the provisions of Section 373.171, Florida Statutes, which requires the District to regulate the use of water by apportionment, limitation, or rotating uses, to obtain the most beneficial use of water resources and to protect the public health, safety and welfare, the District analyzed the available water sources and determined that Sarasota County relies upon its 10 mgd supply from Manatee County and the 2 mgd supply from University wellfield to constitute 12 mgd usable water. The 5 mgd from Manatee County would be used only in an emergency situation, and the Sorrento wellfield would be abandoned. Future water demands must be predicted relying in great part upon an historic record of prior water use. Utilizing a statistical procedure called linear regression, a methodology accepted by the District, indicated a water demand figure for the period from 1992 to 1997 based upon six use points extending from 1985 to 1990. These use records reflected a low of 9.733 mgd and a high of 12.808 mgd, the former being in 1985 and the latter in 1990. In addition, the County estimated that its capital improvement program would add between 10 and 12 thousand customers who presently use private wells, whose water use would constitute approximately 2 mgd of additional demand. The County's program toacquire some 42 private franchises now serving customers would add an additional demand of 2 mgd. Taken together, these programs would add in approximately 1.8 mgd per year to the need assessment, and it would therefore appear that by 1997, the County's average daily demand, considering all new users, would be 17.84 mgd. The water to be drawn from the Carlton Reserve is not currently potable and will require some form of treatment to render it so. Sarasota County proposes to use the Electrodialysis Reversal process, (EDR), because, in the County's judgement, it is more efficient than others such as reverse osmosis and ion exchange. Whereas EDR is rated at up to 85% efficient, the others range between 50% to 75% efficient. In that regard, in order to determine the maximum amount of water to be drawn, providing a safety factor for a treatment plant operation that is not working up to peak capacity in computing the water needs, the EDR process was determined to be no more than 80% efficient. Factoring in that efficiency potential, when the 1997 average daily demand is subtracted from the County's projected water capacity, the withdrawal need in 1997 is determined to be 7.303 mgd. However, as a part of its permitting process, the County also calculated its peak month daily demand. This is a figure which represents the maximum amount permitted to be drawn on a daily basis during the peak demand period. This peak period was determined under Section b 3.2 of the District's Basis of Review by taking the 1989 daily flow and using a sliding 31 day calendar to determine the highest historical 31 day flow. Thisresulted in a peak month coefficient of 6.16 which was then multiplied by the 1997 average daily demand of 17.842 mgd which resulted in a peak month daily demand of 20.7 mgd. When existing water supplies are removed and the 80% EDR treatment process factor is applied, the amount of raw water needed from the wellfield in issue on a peak monthly basis would be 9.625 mgd. This peak monthly basis figure is considered because of the intermittent periods of low rainfall and high water demand within the County. Accepting the 1.8 gpd yearly increase; the peak factor of 1.16; and the assumed water supply capacity of 18.6 mgd; Sarasota County's need will exceed its available supplies by 1993. In fact, the County is already experiencing low water pressure in part of its service area during peak demand periods. County experts estimate that without the requested water from the Carlton Tract, Sarasota County can expect to experience dry periods as early as 1993 during the periods of peak water usage, generally between April and June. For the above reason, when the application and its supporting information was reviewed by Mr. Basso, the District hydrologist with extensive experience reviewing more than 300 water use application, he determined that the water supplies requested are necessary to meet the County's certain reasonable demand, and that this meets the criteria set out in Rule 40D - 2.301(1)(a), F.A.C. Turning to the issue of hydrologic and environmental impacts, the District's Basis For Review of Water Permit Applications provides for the use of a "water use model" inevaluating water needs and the appropriateness of a proposed withdrawal. In preparing its submittal to the District, Sarasota County performed certain tests and modeling to derive the statistical and scientific information used in support of its application. Specifically it used the USGS' MODFLOW model utilizing information obtained from the pump tests run on the wells in the pertinent areas. Consistent with the District's rule, the water data and aquifer drawdown were determined by simulated pumping. The tests run also provided the information on water quality in the aquifer and physical characteristics including transmissivity, storage coefficient, specific yield and leakance between aquifers. This data also helped in defining the hydrogeologic framework of the Carlton Reserve. The Carlton Reserve's hydrogeology listed in descending order from the surface, includes a surficial aquifer which varies in depth between 19 and 70 feet across the Reserve; a semi-confining clay unit separating it from the intermediate aquifer; the upper intermediate and lower intermediate aquifer which range in depth from 140 to 180 feet across the Reserve; another confining layer, and the Upper and Lower Floridan aquifers. The hydrology and groundwater modeling expert who constructed the model used in Sarasota County's permit application concluded that the water table drawdown at the Reserve property boundary in the surficial aquifer would be less than .3 of a foot; less than .4 of a foot in the intermediate aquifer; and 2.9 feet in the Upper Florida aquifer. The water to be drawn consistentwith this instant permit, if approved, would come from the Upper Floridan aquifer on the Reserve. The County's experts were conservative in the assumptions used in the groundwater model. It was assumed there would be no lateral water flow into the model area and no recharge. In addition, the model called for all pumps to run simultaneously at a maximum drawdown of 12.65 mgd for 90 days rather than at the requested quantity of 9.625 mgd. Utilization of these assumptions provided a scenario wherein "severe" impacts would be encountered. Based on the testing and the modeling done, expert opinion was that there would be no quantity or quality changes that would adversely effect water resources including ground and surface water. This meets the criteria of Rule 40D-2.301. This opinion was concurred in the District's hydrology expert. Nonetheless, in its proposed approval, the District has imposed special permitting conditions which require the County to monitor, analyze, and report water quality and water table level information to the District on a monthly and annual basis. When it evaluates the information supplied by an applicant relating to ground water monitoring, the District is required to consider certain presumptions set forth in its Basis For Review. For example, the District presumes that if there is a drawdown of more than 1 foot in the surficial aquifer at a wetland, adverse environmental impacts will occur. In the instant case, the County model concluded that the actual drawdown in the surficial aquifer at the Carlton Reserve is less than .6 of onefoot and, therefore, there should be no adverse environmental impact resulting from the withdrawal. Nonetheless, the County has developed several plans designed to provide information on environmental impacts which will continuously monitor such parameters as rainfall and evaporation, wetlands hydroperiod changes and vegetative changes in the wetlands to detect any changes which might be attributed to the water pumping. These plans have been made special conditions to the water use permit, and in the opinion of the County's ecology and hydrology expert, would enable the County to adequately monitor and detect any pertinent changes to the pertinent factors concerned on the Carlton Reserve. If wetland changes are detected, a contingency plan will be in effect which will require an alteration of pumping schedules or other action to minimize any adverse impacts. The District expert in wetlands and wildlife habitat has opined that these measures, with which he is familiar, are adequate to insure that adverse impacts to the wetlands will not occur. This is consistent with the provisions of Rule 40D-2.301(1). As was stated previously, the water to be drawn pursuant to this permit will be drawn from the Upper Floridan aquifer. This water is not potable but is treatable and is the lowest quality water which can be economically used by the County. Water of a lower quality does exist in the Lower Florida aquifer, but it is not economically treatable, and, in addition, use of this Lower Floridan aquifer might cause vertical movement of the poorer quality water into the upper strata. For all practical purposes,then, the lowest quality water available to it will be used by the County and this is consistent with the District's basis for review. Expert testimony indicates that saline water will not be infused into the Upper Floridan aquifer. Salt water intrusion generally occurs when groundwater is brought to a level below sea level. Even at the point of maximum actual drawdown as a result of pumping on the Reserve, the fresh water level will remain at least 20 feet above sea level, and as a result of the difference in water level, no saline water intrusion into the fresh water supply will occur even though salt water intrusion can also occur as a result of upward vertical movement of lower quality water due to withdrawal. The District's hydrologist and reviewing official also concluded that because of the confining layer below the aquifer from which water will be withdrawn, there would not be any significant upward movement of lesser quality water. The District's basis of review also envisions an aquifer pollution if a proposed withdrawal would spread an identified contamination plume. Here no contamination has been identified in the area from which the water will be drawn, and therefore, contamination would not be spread. The Basis for Review also infers there will be adverse impact to off site land if there is a significant drawdown of surface water bodies or if damage to crops or other vegetation can be expected. Here, the water table drawdown at the boundary of the Carlton Reserve is anticipated at less than .3 of one foot and any drawdown further out from the Reserve can be expected tobe even less. As a result, no adverse impact to existing off site land useage is expected. With regard to Rule 40D-2.301(1)(i), relating to an adverse impact on existing legal uses, the District presumes that no adverse impact will exist if the drawdown in the water table is no more than 2 feet at an affected well, or the potentiometric surface at the well is not lowered by more than 5 feet. Here, again applying the County's groundwater modeling demonstrates that the drawdown at its worst, in the Upper Floridan aquifer, would be no more than 2.9 feet at the Reserve boundary and much less at the Petitioners' wells. Both Mr Bishop's and Ms. Jones' wells are approximately 7.5 and 7 miles, respectively, from the closest well on the Reserve property. Ms. Jones' well is drilled into the intermediate aquifer which is above that which the County proposes to use and should not be impacted. Mr. Bishop draws water from the intermediate and surficial aquifers, both of which are above the Upper Florida aquifer identified for use here, and the groundwater modeling would suggest that his well would not be impacted either. Sarasota County's application contains reference to numerous proposals for water conservation measures which it intends to implement or has already implemented. It has adopted ordinances to enforce the District's watering restrictions and is currently implementing a block inverted use rate structure to promote conservation. It has developed programs for use in the schools outlining water conservation efforts and is developing programs topromote the increased use of treated waste water for golf course irrigation. The requirement for a water conservation plan such as is described and envisioned by the County is a condition of the water use permit proposed, and in addition, the County has adopted an Ordinance, (90-38) which modifies its building code to require installation of water conservation devices in new buildings erected in the County. It has developed proposals for conservation measures such as water auditing, meter testing, leak detection, system looping, and pressure reduction, and has selected the EDR process of water purification as the most efficient use of groundwater resources. Petitioner, Bishop, testified to his belief that approval of this permit and the resultant water withdrawal on the Carlton Reserve would necessitate an expansion of the boundaries of the District's Eastern Tampa Bay Water Use Caution Area to a point where his property would be encompassed therein. In support of his position, Mr. Bishop offered a notice to the effect that new ground water withdrawals would not be permitted within a certain "most impacted area" within the caution area. There was, however, no independent evidence from hydrologists, geologists, or other conservationists, or individuals familiar with the water conservation process, to support Mr. Bishop's contention that either the boundaries would be expanded or that withdrawal of the proposed permitted amounts of water from the Carlton Reserve would cause the boundaries to be expanded. By the same token, Mr. Bishop's contention that theproposed withdrawal from the wells here in issue would adversely effect his ability to draw water from his existing well was not supported by any expert testimony or documentary evidence tending to support or confirm his contention. He had no evidence tending to contradict the County's and District's experts, all of whom indicated there would be no adverse impact on the environment or water resources as a result of the instant permit. Similarly, neither Petitioner offered any evidence of a demonstrative nature that would draw any connection between the proposed permitted withdrawals and potential salt water intrusion and water level drawdown in their wells. The County introduced construction permits issued by its own health department covering 8 of the 12 wells which have been drilled on the Carlton Reserve as test wells. These wells were clearly sunk pursuant to an agreement between the District and the County's public health unit which delegates authority for water well construction permitting to the County. Taken together the documentation indicates that these 12 wells on the Reserve were installed and permitted pursuant to and consistent with appropriate permitting processes, and the testimony of Mr. Bassarab, the County's expert who oversaw the installation of the wells, reflects they are appropriately grouted and sealed. Therefore, there will be no mixing of lower quality water from the lower portion of the Floridan aquifer with the better quality water from the upper portion of that aquifer. The County's evidence clearly refutes the allegation by Mr. Bishop that the 12 test wells currently existingon the Carlton Reserve were neither permitted nor inspected as required by the District. County Commissioner Hill, who testified on behalf of the Petitioners, indicated that the wells applied for here are unnecessary and an inappropriate expenditure of County funds. She claimed there are other valid sources of water available to the County, including that extracted from excavated shell pits and seawater from the Gulf of Mexico which could be treated and desalinated. The Commissioner's comments as to alternate sources are not specifically rebutted. However, she is neither an expert in hydrology or hydrogeology, and her testimony is not persuasive. While other water sources may exist, the better evidence clearly indicates that those sources are not sufficient to meet the County's needs or are otherwise inappropriate for use by the County in sufficient quantity to satisfy those needs.
Recommendation Based on the foregoing Findings of fact and Conclusions of Law, it is, therefore: RECOMMENDED that consumptive water use permit No. 208836.00, providing for authorized quantities as outlined in the intent to issue, subject to conditions contained therein, be issued to Sarasota County. RECOMMENDED in Tallahassee, Florida this 5th day of September, 1991. 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 September, 1991. APPENDIX TO RECOMMENDED ORDER The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONERS: Rejected as not supported by the evidence. Accepted. Accepted. - 8. Resolved against the Petitioners on the basis information presented by Respondents. 9.- 13. Accepted and incorporated herein. 14. - 16. Accepted and incorporated herein. Accepted and incorporated herein. & 19. Accepted and incorporated herein. 20. - 23. Accepted. Accepted but not dispositive of any issue. Accepted. & 27. Noted as citation of authority. Rejected. & 30. Accepted as restatements of evidence but not as Findings of Fact. 31. Irrelevant. 32. Rejected 33. & 34. Not a error is, in fact, it is such. 35. - 38. Irrelevant. 39. - 43. Accepted. 44. Accepted. 45. Rejected. 46. Accepted and incorporated herein. 47. & 48. Rejected as a mere citation of testimony. 49. Not understandable. Not a Finding of Fact. 50. Accepted. 51. Evidence is acceptable. 52. Not sufficiently specific to rule upon. 53. Not proven. 54. Not specific. 55. & 56. Rejected. FOR THE RESPONDENTS: 1. - 4. Accepted and incorporated herein. 5. & 6. Accepted and incorporated herein. 7. & 8. Accepted and incorporated herein. 9. - 14. Accepted and incorporated herein. 15. - 17. Accepted and incorporated herein. 18. - 21. Accepted and incorporated herein. 22. & 23. Accepted and incorporated herein. Accepted. - 27. Accepted and incorporated herein. 28. & 29. Accepted and incorporated herein. 30. - 32. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. Accepted. - 37. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. - 43. Accepted and incorporated herein. Accepted. Accepted and incorporated herein, - 48. Accepted and incorporated herein. Accepted - not a Finding of Fact. Accepted and incorporated in substance herein. Not correct as stated. Sarasota County will not be withdrawing saline water from the upper Floridan aquifer. The remaining discussion is accepted. Accepted and utilized. & 54. Accepted. Accepted and incorporated herein. Accepted. - 59. Accepted and incorporated herein. 60. Accepted. 61 - 63. Not Findings of Fact but comments on the evidence. Accepted and incorporated herein. & 66. Not Findings of Fact. COPIES FURNISHED: Wyatt S. Bishop, Jr. 5153 Tucumcari Trail Sarasota, Florida 34241 Joan Jones 719 East Baffin Road Venice, Florida 34293 William A. Dooley, Esquire Nelson, Hesse, Cyril, Smith, Widman, Herb, Causey & Dooley 2070 Ringling Blvd. Sarasota, Florida 34237 Cathy Sellers, Esquire Steel, Hector & Davis 215 S. Monroe Street Tallahassee, Florida 32301-1804 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Edward B. Helvenston, Esquire Vivian Arenas, Esquire SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
The Issue The issue concerns the entitlement of GJPS Lukas, Inc. to be granted a consumptive use of water permit from the St. Johns River Water Management District. See Chapter 373, Florida Statutes, and Chapter 40C-2, Florida Administrative Code.
Findings Of Fact On December 7, 1990, the Applicant applied for a consumptive use of water permit under application no. 2-127-0808AN as submitted to St. Johns. The Applicant asked that it be allowed to withdraw water from the Floridian aquifer to irrigate a 240 acre sod farm by the use of four wells and a pipeline ditch irrigation system. This was a new use. On January 9, 1991, St. Johns prepared a technical staff report recommending approval of the application. Petitioner was provided notice of this pending disposition on January 15, 1991 leading to his protest to the grant of the permit. Petitioner's property is adjacent to the Applicant's property. Petitioner has a well which he uses for domestic water needs which is in the vicinity of the proposed project. He also has a commercial fish operation with a number of fish ponds including fresh water ponds. Both these uses may potentially be affected by the proposed consumptive water use contemplated by the Applicant. St. Johns calculated that the irrigation of 240 acres of sod, by calculation using the modified Blaney-Criddle formula pertaining to evapotranspiration, calls for a maximum extraction of 169.4 million gallons a year. In any one month the amount withdrawn should not exceed 37.4 million gallons. The Floridian aquifer at the place where the Applicant proposes to draw water is capable of the production of 169.4 million gallons of water per year and 37.4 million gallons per month without promoting environmental or economic harm. Extraction of this water for purposes of irrigation is an acceptable arrangement in that no wastewater treatment plants are within a five mile radius of the site of the proposed use. Therefore it would not be economically, technically or environmentally feasible for the Applicant to use reclaimed wastewater as a source for its irrigation needs. The aquifer in that area is stable. There was no showing in the hearing by competent evidence that saline water intrusion problems now exist in the area of the proposed site of withdrawal. There was no showing that the withdrawal of as much as 169.4 million gallons per year would cause a saline water intrusion problem. The fields where the Applicant intends to apply the extracted water for irrigation purposes are surrounded by a system of ditches and water control structures to confine the water as applied to the sod and any mixing of that water with any surface or subsurface waters that are contributed by rain events. The ditches and control structures keep the water on the property and prevent flooding downgradient of the subject property. As a consequence flood damage on adjacent properties is not to be expected. On a related issue, the ditches and control structures will prevent water from discharging into receiving bodies of water and thereby degrading water in those receiving bodies such as the fish ponds operated by the Petitioner. The water quality of the Floridian aquifer will not be harmed by the activities of the Applicant in withdrawing this water. In the worse circumstances the well used by the Petitioner will be affected by the Applicant extracting the water from the aquifer to the extent of .25 to .4 drawdown in feet in the well the Petitioner uses. This is not a substantial impediment to the Petitioner's ability to withdraw needed water from the well he uses. The Floridian aquifer in the area in question is semi-confined. The four wells that would be used in withdrawing water for the Applicant's purposes will extract the water at 110 feet below the surface. Between that level and the surface are three confining areas of clay totaling approximately 40 feet in thickness. Those confining units of clay would protect the water at the surface when the Applicant withdraws water and induces a gradient. In particular, the nature of the stratification in the soils in the area in question and the topography are such that the Petitioner's fish ponds, when taking into account the distance between the Applicant's operation and those fish ponds, the clay confining units and the gradient between the Applicant's property and the Petitioner's fish ponds, would not lead to a reduction in the water levels of the Petitioner's fish ponds when the water was extracted by the Applicant. The proposed use by the Applicant would not require invading another use reserved by a permit issued from St. Johns. St. Johns has not established minimum levels or rates of flow for the surface water in the area where the Applicant proposes to extract the water. Nor has St. Johns established a minimum level for a water table aquifer or a minimum potentiometric surface water for an aquifer in the area where the Applicant proposes to extract the water. The surficial aquifer water table beneath the property where the Applicant intends to apply the extracted water should not be raised inordinately should the Applicant follow the best management practice as recommended as special condition No. 9 to the Consumptive Use Technical Staff Report pertaining to this project. Nonetheless if the water table beneath the Applicant's property were to be raised to a level which is too high or if the activities by the Applicant would result in excessive surface water runoff the ditches and water control structures that isolate the Applicant's property would prevent the water level in the Petitioner's fish pond from being increased by the Applicant's proposed activities. The application of the extracted water and the expected flow pattern of water applied to the surface and control of that water is set out in St. Johns' Exhibit No. 5 and described in the testimony of Jack Caldwell Lawrence, Jr., employee of St. Johns and an expert in geology and hydrology. See pages 61 and 62 of the transcript. Concerning water quality in the Petitioner's fish pond, it will not be affected by the Applicant's proposed activities in extracting the water. The gradients and distances between the Petitioner's fish pond and the Applicant's fields do not allow surface water or water in the surficial aquifer, which is groundwater above the confining clay unit, to flow from the Applicant's fields into the Petitioner's fish ponds. Again the ditches and control structures related to the project offer additional protection against a compromise to the water quality in the Petitioner's fish ponds. The Technical Staff Report on this project is an apt description of the project and the necessary conditions to granting a permit which would protect the public and environment. One modification has been made to that report and that modification is appropriate. It changes the intended disposition from one of allowing surface water from the onsite management system to be used as the primary irrigation supply with the Floridian aquifer serving as a supplementary source to one in which the Applicant would not use the onsite management system as a water supply source but would use the onsite management system simply as a discharge holding area.
Recommendation Based upon the facts found and the conclusions of law reached, it is, RECOMMENDED: That a Final Order be entered which approves the application for consumptive use of water subject to the conditions set forth in the Technical Staff Report, excepting the need to have the Applicant utilize water from the onsite management system as the primary source of irrigation of its sod. DONE and ENTERED this 4th day of November, 1991, in Tallahassee, Florida. CHARLES C. ADAMS, 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 4th day of November, 1991. APPENDIX TO RECOMMENDED ORDER The following discussion is made of the suggested facts set forth in the proposed recommended orders. Petitioner's Facts Paragraphs 1-6 are subordinate to facts found. Concerning Paragraph 7, Petitioner does not have standing to take issue with the quality of notice provided to other adjacent landowners. As to Paragraph 8, the witness had sufficient understanding of the location and nature of the surficial or sand aquifer and the clay confining units to have his testimony credited. As to Paragraph 9 the fact that the witness is unaware of the exact depth of the Petitioner's fish pond does not cause his testimony to be disregarded in deciding that the fish ponds would not be negatively impacted by the activities contemplated in this permit application. As to Paragraph 10, this proposed fact is inconsequential given the de novo nature of this proceeding. As to Paragraph 11, see discussion of Paragraph 7. As to Paragraph 12, it is rejected. As to Paragraph 13, that knowledge was not necessary in determining the outcome here. As to Paragraph 14, it is accepted in hypothetical terms, however, no showing was made that chlorides would increase in this instance and adversely affect the Petitioner's fish based upon the evidence adduced at hearing. As to Paragraph 15, the soil samples from Petitioner's property are inclusive and less reliable that the description of soil in the general area as set forth by the witness for St. Johns. COPIES FURNISHED: Clayton D. Simmons, Esquire Stenstrom, Mackintosh, Julian, Colbert, Whigham and Simmons, P.A. 200 West First Street, Suite 22 Sanford, FL 32772-4848 Michael D. Jones, Esquire 996 Westwood Square, Suite 04 Oviedo, FL 32765 Michael D. Jones, Esquire Post Office Box 3567 Winter Springs, FL 32708 Eric T. Olsen, Esquire St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429 Henry Dean, Executive Director St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429
The Issue The issue presented for decision in this case is whether Respondent, the Southwest Florida Water Management District (the "District"), should issue Water Use Permit ("WUP") No. 20005687.003 to Dr. Thomas E. Kelly, pursuant to the terms of the proposed permit issued on April 11, 2001.
Findings Of Fact Based on the oral and documentary evidence adduced at the final hearing and the entire record in this proceeding, the following findings of fact are made: PARTIES Petitioner Becky Ayech is a resident of Sarasota County and a citizen of the State of Florida. The District is a water management district in the State of Florida created pursuant to Section 373.069(1)(d) and (2)(d), Florida Statutes. The District is the governmental agency charged with the responsibility and authority to review and act upon water use permit applications, pursuant to Chapter 373, Part II, Florida Statutes, and Chapters 40D-1 and 40D-2, Florida Administrative Code. Dr. Thomas E. Kelly is the owner of the real property in Sarasota County on which Pop's Golf and Batting Center is located, and as such is recognized as the applicant for and holder of any WUP issued for the property. Pursuant to a 50- year lease with Dr. Kelly, Ralph Perna owns and operates Pop's Golf and Batting Center and is the person who would be responsible for day-to-day compliance with the terms of the WUP at issue. Neither Dr. Kelly nor Mr. Perna formally intervened in this proceeding. THE PROPOSED PERMIT The proposed permit is for irrigation and sanitary uses at a golf driving range and batting cage facility called Pop's Golf and Batting Center, on Fruitville Road in Sarasota County. The site leased by Mr. Perna comprises approximately 30 acres, of which the westward 15 acres is taken up by the Pop's facility. The eastern 15 acres is heavily wooded, overgrown with brush, and contains a five-acre lake. The majority of the 15 acres used by Pop's is taken up by the landing area for the driving range. Near the front of the facility are a tee box and putting green sown with Bermuda grass. This grassy area, about six-tenths of an acre, is the only part of the 30-acre property requiring irrigation, aside from some landscape plants in front of the business office. The landing area is not watered and is not even set up for irrigation. The Pop's facility is in a low-lying area historically prone to flooding. For this reason, the tee box, putting green, and business office are elevated about two and one-half feet higher than the landing area. This elevation also serves the esthetic purpose of allowing golfers to follow the flight of their drives and watch the balls land. The proposed WUP is a renewal of an existing permit. The existing permit is premised on the property's prior use for agriculture, and permits withdrawals of 34,000 gpd on an average annual basis and 99,000 gpd on a peak monthly basis. The renewal would authorize withdrawals of 1,700 gpd on an average annual basis and 4,400 gpd on a peak monthly basis, reductions of 95 percent and 96 percent, respectively. "Average annual" quantity is the total amount of water withdrawn over the course of one year. This quantity is divided by 365 to arrive at the allowable gallons per day. "Peak monthly" quantity is the amount of water allowed to be withdrawn during the driest month of the year. This quantity is divided by 30 to arrive at the allowable gallons per day. Pop's draws water from two wells on the property. A six-inch diameter well, designated District Identification No. 1 ("DID 1"), is used for irrigation of the tee box and putting green. A four-inch diameter well, designated District Identification No. 3 ("DID 3"), is used to supply water to the two restrooms at the facility. THE PERMIT CONDITIONS The proposed WUP includes the following basic information: the permittee's name and address; the permit number; the date the permit application was filed; the date the permit was issued; the expiration date of the proposed permit; the property location; the quantity of water to be permitted; the withdrawal locations; and the water use classification proposed pursuant to the District's permit application. The District's permit application provides the applicant with the following five choices regarding proposed water use: Public Supply; Industrial or Commercial; Recreation or Aesthetic; Mining or Dewatering; and Agriculture. The proposed permit in this case has been classified as Recreation or Aesthetic. The proposed WUP would allow the permittee to withdraw from DID 1 an average of 1,600 gpd, with a peak monthly withdrawal of 4,200 gpd, and to withdraw from DID 3 an average of 100 gpd, with a peak monthly withdrawal of 200 gpd. The proposed WUP contains four Special Conditions. Relevant to the issues raised in this proceeding, Special Condition No. 3 requires the permittee to incorporate best water management practices, to limit daytime irrigation to the greatest extent practicable, to implement a leak detection and repair program, to conduct a system-wide inspection of the irrigation system at least once per year, and to evaluate the feasibility of improving the efficiency of the current irrigation system. Special Condition No. 4 requires the permittee to submit a conservation plan no later than April 30, 2006. The plan must address potential on-site reuse of water and external sources of reuse water. The proposed WUP also contains 16 Standard Conditions. Standard Condition No. 2 reserves the District's right to modify or revoke the WUP following notice and a hearing, should the District determine that the permittee's use of the water is no longer reasonable and beneficial, consistent with the public interest, or if the water use interferes with an existing legal use of water. Standard Condition No. 3 provides that the permittee may not deviate from the terms of the WUP without the District's written approval. Standard Condition No. 4 provides that, if the District declares a water shortage pursuant to Chapter 40D-21, Florida Administrative Code, the District may alter, modify, or declare inactive all or any part of the proposed WUP as necessary to address the water shortage. Standard Condition No. 5 provides that the District will collect water samples from DIDs 1 and 3, or require the permittee to submit water samples to the District, if the District determines there is a potential for adverse impacts to water quality. Standard Condition No. 9 provides that the District may require the permittee to cease or reduce its withdrawals if water levels in aquifers fall below minimum levels established by the District. Standard Condition No. 11 provides that the District may establish special regulations for Water Use Caution Areas ("WUCAs"), and that the permit will be subject to such regulations upon notice and a reasonable period to come into compliance. Standard Condition No. 12 requires the permittee to install flow metering or other measuring devices to record withdrawal quantities, when the District deems it necessary to analyze impacts to the water resource or existing users. CONDITIONS FOR ISSUANCE OF PERMIT Generally, the miniscule withdrawals proposed by Pop's would not fall within the District's permitting authority, which mostly confines itself to withdrawals of 100,000 gpd or more. However, Rule 40D-2.041(1)(c), Florida Administrative Code, requires a permit for any withdrawal from a well having an outside diameter of six inches or more at the surface. DID 1 has an outside diameter of six inches. An applicant for a WUP must demonstrate that the proposed use of water is reasonable and beneficial, is in the public interest, and will not interfere with any existing legal use of water, by providing reasonable assurances on both an individual and a cumulative basis that the proposed use of water satisfies the 14 specific conditions set forth in Rule 40D-2.301(1)(a)-(n), Florida Administrative Code, identified in the subheadings below. Necessary to Fulfill a Certain Reasonable Demand Pop's is open for business twelve hours per day. During the summer months, it averages 100 customers per day. The tee box and putting green at Pop's are heavily used. When golfers hit balls from the tee box, they make small gouges, or divots, in the Bermuda grass. These divots are later filled with sand, and the grass naturally grows over them. Irrigation is essential to the health of the Bermuda grass, allowing the application of fertilizer and chemicals to treat for pests and fungus. The tee box and putting green are watered as little as possible, because over-watering can itself lead to fungus problems with the Bermuda grass. The District uses an irrigation allocation computer program called AGMOD to determine reasonable average annual and peak monthly quantities for irrigation in an objective and consistent manner. Data on the pump capacity, soil type, the area to be irrigated, and its geographic location are input, and AGMOD allocates a quantity of water sufficient to irrigate for the driest 20 percent of the time, based on 75 years of historic rainfall data. The AGMOD program allows quantities for irrigation of the fairways of a typical golf course; however, Pop's does not have fairways and thus the proposed permit does not authorize any water for such irrigation. The District's expert, David Brown, credibly testified that the amounts allocated under this permit are conservative because the area to be irrigated is a high traffic area, because the irrigation methodology employed by Pop's ensures that 75 percent of the water withdrawn from DID 1 will get to the grass, because of the fertilizers and chemicals necessary to maintain and repair the grass, and because of the elevation of the area to be watered. Mr. Brown testified that the AGMOD model uses native soil types, not the fill used to elevate the tee box and putting green, and therefore the soil for the elevated areas will likely require more water and drain more quickly than AGMOD indicated. The quantities allocated for withdrawals from DID 3 on an average annual and peak monthly basis are necessary to fulfill the demand associated with the use of the two restrooms by Pop's employees and customers. In summary, the amounts of water authorized for withdrawal under the proposed permit are no more than necessary to fulfill a certain reasonable demand. Quantity/Quality Changes Adversely Impacting Resources The evidence at the hearing established that the operation of DIDs 1 and 3 pursuant to the terms of the proposed WUP will cause no quality or quantity changes adversely impacting the water resources. The proposed withdrawal amounts constitute a decrease of 95 percent on an average annual basis and of 96 percent on a peak monthly basis from the existing permit. The District reasonably presumes that decreases in permitted withdrawal amounts will not cause quantity or quality changes that will adversely impact the water resources. Nonetheless, Mr. Brown performed groundwater modeling to confirm that the District's presumption was correct in this case. The first step in model development is to study the geology at the site being studied. Mr. Brown looked at detailed information from surrounding WUPs and geographic logs to arrive at a "vertical" view of the stratigraphic column in place at Pop's, giving him an idea of which zones below Pop's produce water and which zones confine water and impede its movement between the producing units. Mr. Brown then looked to site-specific aquifer test information from other permits to give him an idea of the "horizontal" continuity of the system across the area under study. The hydrogeologic profile at Pop's contains five different aquifer production zones separated by confining units of clay or dense limestone. Moving downward from the surface, the production zones are the surficial aquifer, zones called Production Zone 2 ("PZ-2") and Production Zone 3 ("PZ- 3") within the intermediate aquifer, and the Suwannee limestone and Avon Park limestone layers within the Upper Floridan aquifer system. DID 3 has approximately 96 feet of casing and a total depth of approximately 195 feet. It draws water from PZ-2, the upper production zone of the intermediate aquifer. DID 1 was built before the District assumed regulation of well construction and consumptive water use; therefore, the District does not possess specific information as to its construction. Mr. Brown reviewed historical documents, including a 1930s report by the United States Geological Survey ("U.S.G.S.") about irrigation wells drilled in the location now occupied by Pop's. Mr. Brown's review led him to a reasonable conclusion that DID 1 has approximately 75 to 100 feet of casing and is drilled to a total depth of 600 to 700 feet below land surface. The District's water level measurements confirmed Mr. Brown's judgment, indicating that the well penetrates only through the Suwannee limestone formation in the Upper Floridan aquifer. His hydrogeological findings in place, Mr. Brown proceeded to perform a number of analyses using a five-layer groundwater model based on the "Mod-Flow EM" program developed by the U.S.G.S. to determine whether the withdrawals authorized by the proposed WUP would have any adverse impacts on water resources. The model's five layers simulated the five aquifer zones found in the area of Pop's. Mr. Brown performed simulations to predict the effect of the combined pumping of DID 1 and DID 3 at 1,700 gpd on a steady state basis and at 4,400 gpd for a period of 90 days. A "steady state" model assumes continuous pumping at the stated quantity forever. The scenario for pumping 4,400 gpd for 90 days is called a "transient" model, and simulates the effect of continuous pumping at the peak month quantity, without replenishment of the water source, for the stated period. Both the steady state and transient models used by Mr. Brown were conservative, in that it is unlikely that their scenarios would actually occur at Pop's. The modeling predicted that Pop's withdrawals would have no effect on the surficial aquifer or on the deep Avon Park limestone formation. Because DID 1 is likely to open to the PZ-2, PZ-3, and Suwannee limestone production zones, Mr. Brown analyzed the steady state and transient conditions for each zone. The greatest effect predicted by any of the modeling runs was a drawdown in water levels of approximately two-hundredths of a foot in the PZ-3 and Suwannee limestone zones. This drawdown would extend no farther than the boundary of Pop's property. All of the predicted drawdowns were smaller than the natural fluctuations in water levels caused by changes in barometric pressure. Thus, any possible effects of withdrawals at the quantities proposed in the WUP would be lost in the background noise of the natural water level fluctuations that occur in all confined aquifers. The water level or pressure within subterranean production zones is referred to as the "head." For water to move from one zone to another, there must be a difference in head between the zones. The evidence established that groundwater quality declines with depth at the Pop's site, but that the heads in the PZ-2, PZ-3, and Suwannee limestone production zones are essentially the same in that area. The similarity in heads means that there is no driving force to move water between the zones and thus no potential for adverse water quality changes caused by DID 1's being open to multiple production zones. In summary, the amounts of water authorized for withdrawal under the proposed permit will not cause quantity or quality changes which adversely impact the water resources, including both surface and ground waters. Adverse Environmental Impacts to Wetlands, Lakes, Streams, Estuaries, Fish and Wildlife, or Other Natural Resources Mr. Brown's model indicated there would be no drawdown from the surficial aquifer, where there would be the potential for damage to water related environmental features and/or the fish and wildlife using those features as habitat. Petitioner offered no evidence indicating that the proposed water use will cause adverse environmental impacts. Deviation from Water Levels or Rates of Flow The District has not established minimum flows or levels for the area including Pop's. Therefore, Rule 40D- 2.301(1)(d), Florida Administrative Code, is not applicable to this WUP. Utilization of Lowest Quality of Water Ninety percent of the water withdrawn from DID 1 will come from the Suwannee limestone formation and is highly mineralized and of lower quality than the water in PZ-2 or PZ- 3. DID 3 draws its water from PZ-2. As noted above, DID 3 provides water to the two restrooms on the premises of Pop's. Because its water is used in the public restrooms, DID 3 is considered a limited public supply well, the water from which must meet potable standards. Mr. Brown testified that, though PZ-2 provides water of higher quality than do the zones beneath it, that water only barely meets potable standards. Lower quality water than that obtained from PZ-2 would require extensive treatment to meet potable standards. Reuse or reclaimed water is unavailable to Pop's under any rational cost-benefit analysis. There is a reclaimed water transmission network in Sarasota County, but the nearest point of connection is more than one mile away from Pop's. The wetland lake on Pop's site is unsuitable because extensive land clearing, pipeline construction, and intensive filtration would be required to use its water. Such a project would not be technically or economically feasible for the small amount of water in question. The evidence establishes that Pop's will utilize the lowest quality water available. Saline Water Intrusion The evidence demonstrated that the proposed use will not significantly induce saline water intrusion. Saline water intrusion occurs in the Avon Park limestone formation. Withdrawals must cause a drawdown in the Avon Park formation to further induce saline water intrusion. DID 1 does not penetrate into the Avon Park formation. Mr. Brown's modeling indicated that the withdrawals allowed under the proposed WUP will not cause any drawdown in the Avon Park formation. Pollution of the Aquifer The proposed use will not cause pollution of the aquifer. As noted above, absent a difference in head or some driving force, there is no potential for water to be exchanged between the confined producing zones. Any small quantity that might be exchanged due to the pumping of the well would be removed by the same pumping. There is no potential for pollution of the aquifer by storm water moving through DID 1 or DID 3 because there is no head differential or driving force to move storm water down into the wells. The District's historic water level measurements indicated that during the rainy season, when the site is most likely to be inundated, water levels in the wells are 0.15 feet above land surface. The well structures extend at least one foot above ground level and are sealed with plates and gaskets. Adverse Impacts to Existing Off-site Land Uses The proposed use will not adversely impact off-site land uses. The District's reasonable practice, when authorizing renewal of the permit for an existing well, is to consider off-site impacts only where the applicant seeks to increase withdrawal amounts. In this case, the applicant is requesting a substantial decrease in the amount of withdrawals allowed under the renewed WUP. Adverse Impacts to Existing Legal Withdrawals The proposed use will not adversely affect any existing legal withdrawals of water. The District's reasonable practice, when authorizing renewal of the permit for an existing well, is to consider adverse impacts to existing legal withdrawals only where the applicant seeks to increase withdrawal amounts. In this case, the applicant is requesting a substantial decrease in the amount of withdrawals allowed under the renewed WUP. As noted above, Mr. Brown's modeling indicated that any drawdowns caused by these withdrawals are so small as to be lost within the natural fluctuations of water levels in the aquifer, even at the edge of Pop's 30-acre site. Petitioner's well is more than ten miles away from the wells at Pop's. Utilization of Local Resources to Greatest Extent Practicable The proposed use of water will use local resources to the greatest extent practicable, because the water withdrawn pursuant to the permit will be used on the property where the withdrawal occurs. Water Conservation Measures The proposed use of water incorporates water conservation measures. Pop's uses a commercial irrigation system with low volume misters, spray tips and sprinkler heads, and a rain gauge that automatically shuts down the system if one-eighth to one-quarter inch of rain falls. Mr. Perna testified that the automatic shutdown system rarely has the opportunity to work, because he manually shuts down the system if the weather forecast calls for rain. Mr. Perna testified that the typical golf range irrigates from 30 to 45 minutes per sprinkler head. Pop's irrigates roughly eight minutes per head. Overwatering can cause fungus on the Bermuda grass, giving Pop's a practical incentive to minimize irrigation. Pop's irrigates only the high traffic areas of the tee box and putting green, not the landing area. In its Basis of Review, the District has adopted a water conservation plan for golf courses located in the Eastern Tampa Bay Water Use Caution Area ("WUCA"). Basis of Review 7.2, subsection 3.2. Pop's is located in the Eastern Tampa Bay WUCA, and has implemented the items that golf courses are required to address in their conservation plans. Reuse Measures Given the small total irrigated area and the efficiency of the irrigation methods employed by Pop's, there is no realistic opportunity to capture and reuse water on the site. There is no reuse water realistically available from other sources. Thus, Pop's incorporates reuse measures to the greatest extent practicable. Waste Given the reduction in permitted quantities and the limited scope of the irrigation, the proposed use will not cause waste. Otherwise Harmful to District Resources No evidence was presented that the use of this water by Pop's will otherwise harm the water resources of the District. PETITIONER'S EVIDENCE Petitioner testified on her own behalf and presented the testimony of Ellen Richardson. Ms. Richardson testified that she had once seen a sprinkler running at Pop's during a rainfall, though she conceded that it had just begun to rain when she saw it. Ms. Richardson also testified that she had more than once seen sprinklers running at Pop's during daylight hours. However, Mr. Brown testified that some daytime irrigation is permissible under the District's watering restrictions, where heat stress and applications of fertilizers and chemicals make daytime watering necessary. These conditions applied to Pop's. Petitioner's chief concern was with her own well. Since the late 1980s, she has experienced intermittent water outages. The District has repeatedly worked with Petitioner on her well problems, and Petitioner feels frustrated at the District's inability to solve them. However, the District's evidence established that Petitioner's problems with water levels in her own well could not possibly be caused or exacerbated by the withdrawals at Pop's, ten miles away. To the extent that the renewal of this WUP will result in drastic decreases in permitted withdrawals, Petitioner's position would be improved even accepting her theory that these withdrawals have some impact on her well. In her petition, Petitioner alleged that there were disputed issues of material fact as to eight of the fourteen permitting criteria discussed above. While she engaged in spirited cross-examination of the District's witnesses, Petitioner offered no affirmative evidence showing that the any of the conditions for issuance of permits were not met. Petitioner's chief attack was that Rule 40D- 2.301(1), Florida Administrative Code, requires "reasonable assurances" that the permittee will fulfill the listed conditions, and that the applicant here could not supply "reasonable assurances" because of his long history of failure to comply with the conditions of prior permits. As evidence, Petitioner offered the District's historic record of this permit, which indeed was replete with correspondence from the District requesting records related to pumpage and water quality, and apparent silence from Dr. Kelly in reply. However, the record also explains that the failure to provide data was not the result of obduracy, but because farming had ceased on the property. When the less water intensive use of the driving range commenced approximately nine years ago, the owner ceased monitoring activities. The District, under the impression that farming was still taking place on the property, continued to request pumpage and water quality data for several years after the conversion. It appears from the record that Dr. Kelly, an absentee landlord, simply did not bother to respond. Dr. Kelly's past discourtesy does not rise to the level of calling into question the reasonable assurances provided in this permit renewal application, particularly where the lessee, Mr. Perna, has every reason to ensure that the conditions of the WUP are fulfilled. The evidence did not prove that Petitioner participated in this proceeding for an improper purpose--i.e., primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of licensing or securing the approval of the permit renewal application. To the contrary, the evidence was that Petitioner participated in this proceeding in an attempt to raise justifiable issues as to why the permit renewal application should not be granted. In particular, Petitioner raised an important policy issue as to whether an applicant's history of failure to comply with permit conditions should be considered by the District in assessing the reasonableness of the applicant's assurances of future compliance. The District contended that the applicant's compliance history is irrelevant. While the District ultimately prevailed on the substantive issue, its procedural claim of irrelevance was rejected, and Petitioner was allowed to attempt to prove her contention as to Dr. Kelly's noncompliance. It is not found that Petitioner's litigation of this claim was frivolous.
Recommendation Upon the foregoing Findings of Fact and Conclusions of Law, it is recommended that the Southwest Florida Water Management District enter a final order determining that Dr. Thomas E. Kelly has satisfied the requirements of Section 373.223, Florida Statutes, and Rule 40D-2.301, Florida Administrative Code, regarding conditions for issuance of water use permits, and that the District issue Water Use Permit No. 20005687.003 to Dr. Thomas E. Kelly. DONE AND ENTERED this 27th day of November, 2001, in Tallahassee, Leon County, Florida. ___________________________________ LAWRENCE P. STEVENSON Administrative Law Judge Division of Administrative Hearings 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 this 27th day of November, 2001. COPIES FURNISHED: Becky Ayech 421 Verna Road Sarasota, Florida 34240 Jack R. Pepper, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34604 E. D. "Sonny" Vergara, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899
