Findings Of Fact Application No. 76-00292 is for a consumptive use permit for one well located in the Green Swamp, Lake County. The water withdrawn is to be used for industrial purposes. The application seeks a total withdrawal of 3.642 million gallons per day average annual withdrawal and 5.112 million gallons maximum daily withdrawal. This withdrawal will be from one well and a dredge lake and constitutes in its entirety a new use. The consumptive use, as sought, does not exceed the water crop as defined by the district nor otherwise violate any of the requirements set forth in Subsections 16J-2.11(2) , (3) or (4), Florida Administrative Code. The Southwest Florida Water Management District's staff recommends issuance of a permit with the following conditions: That the applicant shall install totalizing flowmeters of the propeller-driven type on the subject well. The applicant shall record the pumpage from the subject well on a weekly basis and submit a record of that pumpage to the district quarterly beginning on January 15, 1977. The permit shall expire on December 31, 1980. The procedural requirements of Chapter 373, Florida Statutes, and the rules promulgated pursuant thereto, have been complied with as they pertain to this application. The intended consumptive use appears to be a reasonable, beneficial use which is consistent with the public interest and will not interfere with any legal use of water existing at the time of the application.
Recommendation It is hereby RECOMMENDED that a consumptive water use permit in the amounts and manner sought for by the subject application be issued subject to the conditions set forth in paragraph 3 above. ENTERED this 5th day of October, 1976, in Tallahassee, Florida. CHRIS H. BENTLEY Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Florida Rock Industries, Inc. Staff Attorney Post Office Box 4667 Southwest Florida Water Jacksonville, Florida Management District Post Office Box 457 Brooksville, Florida 33512
The Issue The issue in this case is whether the portion of Consumptive Use Permit (CUP) Application Number 97106 seeking an allocation of 499,000 gallons per day (gpd) of groundwater for commercial/industrial uses (supply bulk water to bottling plants) meets the conditions for issuance as established in Section 373.223, Florida Statutes, Florida Administrative Code Rule 40C-2.301, and the Applicant’s Handbook, Consumptive Uses of Water.1 The County does not oppose or contest the portion of the CUP application authorizing use of 6.0 million gpd of surface water for limerock mining operations.
Findings Of Fact The Parties The County is a political subdivision of the State of Florida. The County operates a water supply utility that supplies water for a variety of uses, including providing untreated water, in bulk, for bottling purposes. The County is currently engaged in a long-range planning effort designed to assess water supply demands and sources to supply those demands in the County over the next 50 years. The County also has completed a study of the two major springs in the County (Rainbow Springs and Silver Springs), and the County’s Board of County Commissioners is in the process of enacting certain recommendations contained in the study. The well for the proposed CUP allocation is located on approximately 160 acres in northern Marion County. Hastings and Greene's father owned the property from 1978 until the latter's death. In 1993, the latter's interest was transferred to Greene and two brothers, who now hold title to the property along with Hastings. The District is a special taxing district created by Chapter 373, Florida Statutes, and is charged with the duty to prevent harm to water resources of the District, and to administer and enforce Chapter 373, Florida Statutes, and the rules promulgated thereunder. The District has implemented Chapter 373, Florida Statutes, in part, through the adoption of Rule Chapters 40C-2 and 40C-20, and the Applicant’s Handbook, Consumptive Uses of Water. Historic Uses of Water on the Mine Site Since the 1980s, the property where the proposed withdrawals will occur has been used for mining of limerock and has been known as the “Black Sink Mine." A ten-inch diameter well has been located on the Black Sink Mine property for 35 years. The well was originally used to provide water to augment water levels in canals in and around the Black Sink Mine property. Later the well was used to irrigate watermelons grown on the property before the mining operation began. The limerock mining operation at Black Sink Mine uses approximately 6 million gpd of surface water. The mine pit at the site is divided by an earthen berm that separates a larger, previously mined area from a smaller area where active mining is occurring. Surface water is pumped from the actively mined portion of the pit to the larger, previously mined portion of the pit, to enable mining of the limerock material to be conducted at levels below the water table. Dewatering is necessary in order to remove the limerock. A majority of the property is mined to a depth of 55 feet below land surface. The limerock material extracted from the site is transported by trucks from the site, approximately 100 trucks per day, to various sites across North Florida. The Need for the Proposed Use of Groundwater If mining of limerock continues at the current pace, the limerock material at the Black Sink Mine will be exhausted within a year. Recognizing that the productive use of the property for limerock mining was nearing an end, Greene and Hastings began exploring other potential uses for the property, including use of the existing well on the property for production of bottled water. To explore the feasibility of producing water for bottling from the existing well, in 2004 Greene and Hastings engaged an engineering firm with expertise in water resources to conduct a hydrogeologic study of the mine property and well. The results of the study, showing water of sufficient quality and quantity for production of bottled water, motivated Greene and Hastings to submit the CUP application which was the subject of the hearing. The study also determined that water withdrawn from the well could be marketed as spring water. Greene and Hastings also determined through market research that the demand for bottled water has increased at the rate of ten percent per year for the last 4-5 years and that Florida bottlers were interested in purchasing water from the well on the mine site in bulk for bottling. In order to provide reasonable assurance that the water use proposed by Greene and Hastings is in such quantity as is necessary for economic and efficient utilization, Greene and Hastings must show that the amount to be used is consistent with what would typically be required for the activity being supplied; that the water will be used efficiently with loss or waste minimized; and that there is a demonstrated need for the water proposed for allocation. To demonstrate a need for the 499,000 gpd of groundwater requested in the application for an allocation of 499,000 gpd of groundwater, Greene and Hastings provided letters from two businesses engaged in bottling of water stating an intent to purchase specific quantities of water produced from the Greene and Hastings well should the CUP be granted. One of the letters of intent came from a bottler in Jacksonville, Florida, stating its intention to initially purchase 100,000 gpd of Greene and Hastings’s water. The other was from a bottler in Stuart, Florida, dated January 9, 2006, stating its intention to purchase 125,000 gpd of water from Greene and Hastings within “the next 12-24 months.” Based on these letters Greene and Hastings initially requested an allocation of 200,000 gpd of groundwater for the first year of the permit. Prior to completion of the CUP application, Greene and Hastings learned that because the Stuart bottler’s facility was located outside the geographic boundaries of the District, to transport water from the Black Sink Mine to the Stuart facility would require additional data and information related to inter- district transfers of groundwater. Greene and Hastings elected to reduce the requested allocation for the first year of the permit to 100,000 gpd, relying on the letter from the Jacksonville bottler. Based on the current market demand for bottled water, and based on the fact that there are other bottlers of water within the boundaries of the District purchasing water for bottling, it is reasonable to conclude that Greene and Hastings can sell 499,000 gpd of water from the well on the Black Sink Mine property by the end of the fifth year of the proposed CUP. These facts support the conclusion that there is a need for the amount of water requested by Greene and Hastings. In addition, the permit is conditioned to require a compliance review at five-year intervals during the term of the permit. Should Greene and Hastings not be successful in selling the full 499,000 gpd allocated by the fifth year of the permit, the District has the ability as part of the five-year compliance review to modify the permit to reduce the allocation based on the amount of water actually used for bottled water. Efficiency of the Proposed Use of Water The production of water in bulk for shipment to a bottler is a highly efficient use of water. There is very little if any water lost in the withdrawal and loading of the water; almost all the water goes to the end product. The evidence establishes that the use proposed by Greene and Hastings is an efficient use of water. Potential Impacts from the Proposed Groundwater Allocation The source of the groundwater proposed for use by Greene and Hastings is the Floridan aquifer. Because there is no confining layer in the vicinity of the Black Sink Mine that would retard movement of water between the Upper Floridan aquifer and the surficial aquifer, both the Upper Floridan aquifer and the surficial aquifer essentially behave as one unit. Thus, any drawdown in the surficial aquifer associated with groundwater withdrawals at this location will be the same as the related drawdown in the Upper Floridan aquifer as a result of groundwater withdrawals. The Floridan aquifer is capable of producing the amount of groundwater requested by Greene and Hastings in the application. To assess the level of drawdown expected to occur in both the Floridan aquifer and the surficial aquifer as a consequence of the proposed groundwater withdrawals, Greene and Hastings engaged a consultant, Andreyev Engineering, Inc., to run a groundwater model to simulate the proposed withdrawal and predict the anticipated drawdown. The groundwater model selected for use for this application was the North Central Florida Regional Groundwater Flow Model, a model developed for the District by the University of Florida for use in Marion County and surrounding areas. This model is an accepted and reliable tool for predicting aquifer drawdown associated with groundwater withdrawals at the location of the withdrawals proposed in this application and is used extensively by the District in its CUP program. To simulate the drawdown associated with the withdrawal of 499,000 gpd from the Florida aquifer, Greene and Hastings’s consultant inserted a pumping well in the model grid where the Black Sink Mine is located. The model then simulated pumping from the well at 499,000 gpd. The model results are graphically depicted on maps showing drawdown contours overlain on the Black Sink Mine Site, illustrating the level of drawdown in the aquifer and the distance the level of drawdown extends out from the well site. The model predicts a drawdown of 0.03 feet in the Floridan and surficial aquifers in the immediate vicinity of the well on the Black Sink Mine property, and a drawdown of 0.02 feet in the Floridan and surficial aquifers extending out to a distance of approximately 5,000 feet from the well, less than 1/3 of an inch of drawdown. The model results represent a reasonable estimation of the drawdown that will occur as a consequence of withdrawal of 499,000 gpd of groundwater at the Black Sink Mine as proposed in the application. The impact of the 0.02-0.03 foot drawdown predicted by the model was variously characterized by the experts who testified at the final hearing as “not practically measurable,” an “insignificant impact,” “very small,” or “de minimus.” The use of water proposed by Greene and Hastings will not cause significant saline water intrusion, nor will it further aggravate any existing saline water intrusion problems. The use of water proposed by Greene and Hastings will not induce significant saline water intrusion to such an extent as to be inconsistent with the public interest. Because the predicted drawdown is so small, it will not interfere with any existing legal uses of water. Neither will the predicted drawdown cause serious harm to the quality of the source of the water proposed for use by Greene and Hastings. With regard to the issue of interference with existing legal users, the County argued that the District should have considered whether there is sufficient groundwater available to meet all projected needs for water in the County during the 20- year term of the permit, as well as the additional cost County citizens will need to bear to secure alternative water supplies as a result of any future shortfalls in available groundwater. The County projects, based on planning estimates, that use of groundwater to supply all anticipated uses of water in the County will be limited within 20-30 years from the present. Such “limits” would not become an issue until after the Greene and Hastings permit expires. Thereafter, water users in the County will have to rely on alternative water sources, conservation, reuse of reclaimed water, and surface water. The anticipated growth in demand in the County’s planning estimates includes anticipated growth in the commercial/industrial category of uses. The County’s estimated limits on groundwater use will occur whether or not the CUP requested by Greene and Hastings is approved. The District does not base its permitting decisions on a pending CUP application on the possibility that the source of water may become limited at some future time for water uses not presently permitted, provided the application meets all permitting criteria. The District allocates water for recognized beneficial uses of water, such as commercial/industrial uses, as long as the water is available and the application meets District criteria. The District allocates water as long as an allocation does not cause harm to the resource. Based on these facts, the proposed use of water by Greene and Hastings will not interfere with any existing legal use of water. No Evidence of Economic or Environmental Harm Because the predicted drawdown associated with the proposed use of water is so small, and because no impacts are anticipated on any surrounding properties or water uses, Greene and Hastings have provided reasonable assurance that any economic harm caused by the proposed use has been reduced to an acceptable amount. For purposes of determining whether an applicant has provided reasonable assurance that any environmental harm caused by a proposed use of water is reduced to an acceptable amount, the District examines modeling results showing the level of drawdown predicted for the use and also examines the resources in and around the site of a withdrawal to determine the likely impact of the drawdown predicted for the withdrawal on those resources. The District’s environmental scientists examined the Black Sink Mine site and the surrounding landscape and determined that, based on the characteristics of the landscape in and around the site of the proposed withdrawal and based on the negligible drawdown impact predicted for the proposed water use in both the Floridan and surficial aquifers, there will be no environmental harm resulting from the allocation of groundwater contained in the CUP. The use of water proposed by Greene and Hastings will not cause damage to crops, wetlands, or other types of vegetation. The use of water proposed by Greene and Hastings will not cause the water table to be lowered so that stages or vegetation will be adversely and significantly affected on lands other than those owned, leased, or otherwise controlled by Greene and Hastings. The CUP will not use water that the District has reserved pursuant to Section 373.223(3), Florida Statutes, and Rule 40C-2.301(4). No Impact on Established Minimum Flows or Levels No minimum surface or groundwater levels or surface water flows have been established by the District pursuant to Rule Chapter 40C-8 for any of the water bodies in Marion County that may be affected by the proposed water use. The closest water body for which the District has established a minimum flow is the St. Johns River at the State Road 44 bridge located more than 50 miles from the Black Sink Mine property. The closest water body for which the District has established a minimum level is Star Lake in Northwest Putnam County, more than nine miles from the mine site. Because of the distance of these water bodies from the withdrawal site and because of the negligible drawdown expected to be caused by the proposed use of water, the use will not cause an established minimum flow or level to be exceeded during the term of the permit. Other Reasonable-Beneficial Use Considerations All available conservation measures that are economically, environmentally, and technically feasible are proposed for implementation in the application by Greene and Hastings for the uses proposed by them. Greene and Hastings submitted to the District, as part of the application, a conservation plan that complies with the requirements of A.H. Section 10.3(e). Reclaimed water, as defined in the District’s rules, is not currently available to be used in place of the water proposed for use by Greene and Hastings in the application. The use of water proposed by Greene and Hastings in the application will not cause or contribute to a violation of water quality standards in receiving waters of the state. The use of water proposed by Greene and Hastings in the application will not cause or contribute to flood damage. The Use is Consistent With the Public Interest With regard to the determination of whether reasonable assurance was provided that the proposed use is consistent with the public interest, the County contends that: 1) Greene and Hastings must show that any necessary approvals required by the County’s Comprehensive Plan and/or its LDRs for use of the site for producing bottled water have been obtained; 2) that the District did not properly consider the effect of existence of lawn watering restrictions affecting citizens in the County in evaluating the application; and 3) that the District should have considered the amount of money the applicant may stand to gain from the use of the water requested in the application. In examining whether an application is consistent with the public interest, the District considers whether a particular use of water is going to be beneficial or detrimental to the people of the area and to water resources within the state. In this inquiry, the District considers whether the use of water is efficient, whether there is a need for the water requested, and whether the use is for a legitimate purpose; and the inquiry focuses on the impact of the use on water resources and existing legal users. Sale of water for bottling for human consumption is recognized by the District as a legitimate, beneficial economic enterprise. Use of water for human consumption is among the highest and best uses permitted by the District. For reasons outlined above in the Recommended Order, there are no detrimental impacts that will result from this use of water. The District does not consider whether local government approvals have been obtained prior to issuance of a CUP for purposes of determining whether the application is consistent with the public interest. Neither does the District consider impacts related to local roads from trucks transporting the water or other impacts not related to water resources. No such requirements are included in the District’s adopted permitting criteria. There are no water shortage orders in effect in the District at present. In evaluating a CUP application, the District considers whether its permitting criteria will be met during periods of normal weather as well as during periods of drought. Withdrawals authorized in CUPs can be restricted by order of the District during periods of water shortage, such as droughts. Thus, the possibility of a water shortage order being entered in the County in the future, or the fact that such orders may have been in effect there in the past, does not mean the application is not consistent with the public interest. The District critically examines the efficiency of all water uses for purposes of enacting its regulatory requirements regarding CUPs and in evaluating CUP applications. The District has adopted restrictions on landscape irrigation (which apply to all such users throughout the District’s jurisdiction, not just in Marion County) limiting landscape irrigation to no more than two days per week. The limitations on landscape irrigation exist because this type of use has been determined to be a highly inefficient, wasteful use of water without such restrictions. By contrast, the use of water proposed by Greene and Hastings is a highly efficient use of water, resulting in little or no loss or waste of water. The District does not consider the level of financial gain or benefit an applicant will derive from a permitted use of water for purposes of determining whether the proposed use is consistent with the public interest. Most, if not all permitted users of water derive some level of economic benefit from the water they use, and the District’s rule criteria do not provide standards for evaluating such gain or that otherwise limit the amount of such gain. For the foregoing reasons, the Applicant has provided reasonable assurance that the use of water proposed in the application is consistent with the public interest. Groundwater is the Lowest Quality Source for this Use The County contends that groundwater is not the lowest quality source of water available for the use proposed by Greene and Hastings, in that surface water from the mine pit on the site could be treated and used for bottling in place of groundwater. From the testimony, it is clear that Greene and Hastings’s ability to market water for bottling from the Black Sink Mine is dependent on such water being capable of being labeled as spring water, and on such water being delivered without having gone through any treatment processes. The testimony also establishes that because of the connection between the surficial aquifer and the Upper Floridan aquifer at the site, using surface water instead of groundwater to supply the proposed use would result in little if any reduction in impacts to the Floridan aquifer. More importantly, because the application proposes use of water for direct human consumption, the District’s rules do not require use of a lower quality source of water. For the foregoing reasons, groundwater is the lowest quality source of water suitable for use for bottled water for human consumption. The District’s Noticing Was Adequate and Appropriate The District provided notice of its receipt of the Greene and Hastings CUP application by publishing notice in the Ocala Star-Banner, a newspaper of general circulation in Marion County, on January 25, 2005, with an amended notice being published on February 16, 2005, and also by letters to the County dated January 20, 2005, and February 10, 2005. In each notice, the location of the proposed use was identified by section, township, and range. The County responded to the notices by sending a letter of objection to the application dated February 14, 2005. Thus, the County received sufficient information regarding the location of the proposed use to enable it to prepare and file a letter of objection to the application, and suffered no prejudice as a consequence of the notice. The District provided personal notice of its intent to issue a CUP to Greene and Hastings by letter dated April 5, 2006. In this notice, the location of the proposed use was identified by section, township, and range. The County responded by filing petitions that have resulted in this proceeding. Thus, the County received sufficient notice of the location of the use addressed in the District’s intent to issue to enable it to initiate administrative proceedings regarding the permit, and suffered no prejudice as a consequence of the notice.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the District enter an order granting CUP No. 97106 to Greene and Hastings with the conditions recommended in the District’s Technical Staff Report. DONE AND ENTERED this 9th day of January, 2007, in Tallahassee, Leon County, Florida. S J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 9th of January, 2007.
The Issue The issue for consideration in this case is whether the Respondent, Hi Hat Cattle and Grove, should be issued water use permit 204387.03, to withdraw groundwater from the wells on its property, and if so, in what amount and under what conditions.
Findings Of Fact At all times pertinent to the issues herein, the Respondent, District, was the state agency responsible for the permitting of consumptive water use within its area of geographical jurisdiction. The Respondent, Hi Hat, is a family owned farming and ranching operation in eastern Sarasota County with water wells on its property. The Intervenor, City of Sarasota, is a municipality in Sarasota County which operates wells in the general area of those operated by Hi Hat, and which has an agreement with Hi Hat for the latter's use of treated wastewater pumped from the city's treatment plant to Hi Hat Ranch. The Petitioner, Wyatt S. Bishop, Jr., is a property owner and resident of Sarasota County whose property is located near the Hi Hat Ranch, and whose potable water is drawn from a well on his property which utilizes both the surficial and intermediate aquifers which are penetrated by the wells on Hi Hat Ranch. Hi Hat Ranch consists of 11,000 acres owned by Hi Hat Cattle and Grove, the family owned business which operates it, and an additional 3,227 acres leased from the City of Sarasota. Agricultural operations, including citrus farming, truck farming, sod farming, and grazing have been conducted on the ranch since the mid 1940's. In February, 1990, Hi Hat applied to the District for a permit to withdraw and use water from some 14 wells located on its property. It requested an annual average of 6,267,000 gallons per day, (gpd), and a peak monthly rate of 32, 668,000 gpd. Upon receipt by the District, the application was assigned a number, (204387.03), and was submitted for evaluation by the District staff for conformity with applicable District rules and policies. When the staff evaluation was completed, the District issued a staff report and proposed staff agency action in which it indicated its intention to issue a permit authorizing water to be drawn from the wells at a rate of 6,570,000 gpd, average annual, a peak monthly rate of 14,300,000 gpd, and a maximum daily rate of 5,210,000 gpd. In conducting its evaluation, the District staff relied upon the District's Basis of Review For Water Use Permit Applications which contains within it the provision for use of a "water use model" in assessing the need and appropriateness of water withdrawal amounts. This model, known as the Blaney- Criddle Model considers numerous factors in the evaluation, including rainfall, soil characteristics, irrigation methods used, and proposed crop types, all in an effort to determine a reasonable estimate of the applicant's supplemental water needs. Hi Hat's application was evaluated primarily by Marie Jackson, a Hydrologist III employed by the District, and an expert in hydrology, who has, over the years, reviewed between 350 and 400 permit applications, of which approximately 90 percent have been for agriculture. She is, therefore, quite familiar with the specifics of agricultural water use needs. Her evaluation of Hi Hat's application was done in the same manner as the others she has done and utilized the same tests, measurements and factors for consideration in arriving at her conclusion. In its application, a renewal with modification sought to increase average annual quantities due to a change in crop plans, Hi Hat indicated that its criteria for water use was based on certain agricultural uses and application rates. These included: low volume under tree spray irrigation of 778 acres of citrus at an application rate of 17.2 inches/year plus one inch/year for frost and freeze protection. open ditch irrigation of 135 acres of sod at an application rate of 30 inches/year. open ditch irrigation of 1,367 acres of improved pasture at an average application rate of 26.6 inches/year. overhead spray irrigation of 1,200 acres of improved pasture at an application rate of 20.3 inches/year. open ditch irrigation of 110 acres of spring peppers at an application rate of 30.0 inches/crop, and open ditch irrigation of 110 acres of fall peppers at an application rate of 45.2 inches/crop. Applicant also stipulated that the peak monthly quantities that it requested would be utilized for pasture, sod and citrus irrigation during the month of May. The proposed maximum quantities were for frost and freeze protection of citrus only. In January, 1989, Hi Hat entered into a contract with the City of Sarasota under which the City was obligated to deliver reclaimed water from its wastewater treatment plant to a "header" located on the ranch which thereafter distributes the water through pipes to "turnouts" located at various high points on the property. From these, the water is then discharged into a system of ridges and furrows for distribution of the water across the needed area. The reclaimed water is used to irrigate approximately 5,403 acres of ranchland. The Contract provides for minimum and maximum amounts of water to be delivered as well as for water quality standards which must be met. In periods of adequate rainfall, when irrigation is not required, any treated wastewater which is not needed is stored in a 185 million gallon holding pond on City property located adjacent to the ranch. When needed, water can be fed into the wastewater distribution system described above from the holding pond. This reclaimed water, whether from the pond or direct from the header, can also be utilized to irrigate citrus crops, but this requires a filter system which has not yet been able to operate properly. Therefore, no reclaimed water has yet to be utilized for citrus irrigation on the ranch. At an average annual flow of 6.2 million gallons per day, the pond has the capacity to hold enough treated water for almost 30 days. Not all wells on Hi Hat Ranch are active wells. Several of the wells are classified as standby wells which are intended to be used only to back up the reclaimed water delivery system and are located, normally, beside the "turnouts." In the event the reclaimed water is not available from the city, the standby wells can be utilized to provide water to the ridge and furrow system used to irrigate pasture land. The standby wells are numbers 1, 6, 7, 11, 13, 14, and 15. Well number 5, also identified as a standby well in the staff report and in the draft permit was mistakenly so identified. The draft permit contains several special conditions which impact on the drawing of water under the terms of the permit. Significant among these is Special Condition 33 which prohibits the withdrawal of water from any of the standby wells unless the reclaimed water supply from the city is interrupted. Special Condition 27 requires the installation of a flow meter on any standby well that becomes active as a result of permanent discontinuance of the reclaimed water supply. With regard to flow meters, Special Condition 22 requires flow meters on all of Hi Hat's wells. Ms. Jackson, however, indicated this was in error and has recommended that the standby wells be deleted from that Special Condition. When that is done, only those wells actively producing water on a regular basis would require the installation of flow meters. In its analysis of the application for permit, the District staff considered several factors pertinent to the impact the well would have on the water supply in the area and its effect on other users. These factors include hydrologic impacts, well condition, the history of water use at the ranch, the reliability of the reclaimed water system and its ability to provide a uniform source, and the city's water reuse policy. Addressing each individually, and starting with the hydrologic impact of the withdrawal of the requested amounts, the District considered the nature of the existing wells and how they are constructed and maintained. The District assumed, because the data regarding the construction of the existing wells was incomplete and insufficient to properly disclose the status of casing on each well, that they were shallow cased. As a result, the calculations incorporating this assumption indicate a situation that would occur in its most aggravated form. The parties agreed that Hi Hat's wells are shallow cased and probably go no deeper than 90 feet. To determine, as much as possible, the projected drawdowns in the surficial and intermediate aquifers that might be expected if Hi Hat withdrew the amounts of water proposed, the District utilized the "MODFLOW" computer model which factors in simultaneous peak withdrawals from all 14 of the wells along with a 90 day no rainfall drought condition. This, too, contributes to a worst case scenario, and the resultant figures are considered to be conservative estimates of the hydrologic impact of the water withdrawal. Notwithstanding, the application of this computer model resulted in the indication that, as to the surficial aquifer, the drawdown at Mr. Bishop's property located approximately one half mile from the ranch border, would be no more than .055 feet. Since normal fluctuations in the surficial aquifer during the course of the year can be as much as 6 feet, the projected drawdown as a result of Hi Hat's withdrawals was considered insignificant. Applying the same assumptions and utilizing the same computer model as it relates to the intermediate aquifer resulted in an indication of a drawdown of no more than 2.3 feet at Mr. Bishop's property. Since annual fluctuation in the intermediate aquifer can range from 15 to 20 feet normally, the District considers that any reduction of less than five feet in the intermediate aquifer is insignificant. The permit held by Hi hat currently allows for the withdrawal of more water than would be withdrawn under the proposed permit as conditioned and is consistent with the proposed reduction in allowable withdrawals. Considering that factor, as well as the prohibition against withdrawals from standby wells as long as reclaimed water is available, the actual impact of the water withdrawals consistent with the proposed permit would be substantially less than the computed prediction which includes production from all wells. Drawdown contours are defined across the entire effected area. One of the levels is a 4 foot contour, and when a computer simulation indicates that the 4 foot contour includes a withdrawal previously or otherwise permitted, the District will generally conduct a cumulative impact analysis. In this case, however, since there was only one golf course well within the area circumscribed by the 4 foot contour line, and since this withdrawal was too small to have effected an evaluation, it was not done. The condition of the wells on the Hi Hat Ranch has some bearing on whether or not the application for additional withdrawal of water should be granted. These wells are almost 30 years old, having been drilled in the 1960's. As a result, there is little information available regarding their construction detail. This is not necessarily unusual for agricultural wells, and there is evidence that there are many similar wells in use within the District. The reason for this is that at the time the wells were drilled, information regarding their depth, casing and other matters were not required to be kept or reported. However, there is no indication the wells are in any way violative of well construction criteria and their use has been authorized continuously since 1977. When he prepared Hi Hat's application, Mr. Turner included much the same information regarding the wells as pertains as to depth and diameter which he had previously submitted in earlier applications and which had been accepted. In each case, casing depths had been reported as unknown. Notwithstanding the information contained in some old well logs relative to only a few of Hi Hat's wells, this information is in no way definitive and it is difficult to describe anything specific with the majority of these wells. Nonetheless, as already found, it is stipulated that most are approximately 90 feet deep. It is reasonable to assume that the existing wells, however, are cased only to a shallow depth, and that in many cases, the existing casings have corroded away, either totally or in part. This can cause an intermixing of water from the separate aquifers, but whether this is in fact happening depends upon factors specific to that particular well. Petitioner did not present any evidence to show that as a result of the condition of Hi Hat's wells, any degradation is occurring in the more potable, surficial aquifer as a result of intermixing with water from the intermediate aquifer on or around the Hi Hat Ranch. In Ms. Jackson's opinion, and there appears to be no evidence to contradict it, the amount of drawdown which would occur as a result of maximum pumping at Hi Hat Ranch would not be sufficient to cause poorer quality water from the Floridan aquifer to percolate upward (upcone) into the better quality water of the two upper aquifers even during drought conditions. By the same token, there is no evidence that drawdown would encourage or permit salt water intrusion. Petitioner attempted to show by the records kept on the various Hi Hat wells that many of them have been abandoned and are no longer operative and should not be allowed to fall within the parameters of this permit. He testified clearly that over the years, the level of water in his potable water well has lowered and presumed that this was the result of increased water usage by other entities which draw from the aquifer into which his well is sunk. Water level, however, depends upon numerous factors, of which usage is only one. Others include recharging of the aquifer and the amount of rainfall and other recharge sources not only in the immediate area but across the large area which feeds the aquifer. Mr. Bishop did not present any evidence showing a causal connection between the lowering of the water in his well, or the degradation in water quality he claims to have experienced, and either the drawdown caused by Hi Hat's operation or by aquifer intermixing. He indicated, and it is not disputed, that within the past year, he has had to take measures to improve the water quality in his potable well, but, again, he has not presented any evidence to show this was caused by Hi Hat's ground water withdrawals. In its long range planning, the District intends to implement a program to rehabilitate old wells, and when that program is implemented, almost every agricultural well within the District may require recasing or redrilling. This program will not be implemented for several years, however. In an effort, however, to insure that all reasonable precautions are taken to see that approval of any petition for withdrawal does not have an unacceptable adverse impact on the water needs of the surrounding community, in its analysis of this application, and in all cases, the District makes certain assumptions when adequate empirical data is not available. In this case, pertaining to the unavailability of information regarding Hi Hat's wells, the District assumed that all wells were shallow cased, and this placed the application in the worst possible light. Shallow cased wells allow more upconing and aquifer intermixing. Nonetheless, the amount of water permitted to Hi Hat, even if not used, could impact on Mr. Bishop and other adjoining owner's use of additional water as a result of a possible change to their permitted quantities. However, to compensate for this, the District has also included a special condition, (#26), which requires Hi Hat to log all 14 of its wells within the term of the permit, (7 years), which will require at least 2 wells be done each year. The cost of that action will be between $800 and $2500 per well. Another condition, (#31), requires Hi Hat to look into any complaint from adjacent property owners regarding adverse impacts due to water withdrawal, to report the results of its inquiry to the District, and to mitigate, as much as possible, all adverse impacts due to its withdrawal. Mr. Bishop claimed, and introduced evidence purporting to demonstrate, that many of the wells on the Hi Hat Ranch, which are covered by the permit applied for here, are no longer in use and have been abandoned. In response, Mr. Turner, who has been actively engaged in the ranch's operations for at least the past four years, indicates from his personal knowledge, that all 14 wells included in the permit applied for have been operated within the past two years, and all are capable of producing water. It is so found. Not all wells, however, have been operated at all times. Crop rotation and a varying need for groundwater has resulted in some wells not being used at some times. This is, of course, commonplace in agriculture and to be expected as a result of crop planning programs. Admittedly, an accurate figure for the amount of water which has been withdrawn from the 14 wells cannot be established because these wells do not have, and were not required to have, flow meters. Two of the wells were fitted with hour meters in January, 1989, but because the capacity of the pumps on those wells is variable, a precise estimate of volume pumped cannot be determined. The meters measured only the number of hours the pumps were in operation and not the amount of water passed through the pumps. Evidence was presented, however, to show that wells have been utilized at the ranch since the 1960's, and in 1977, some 14 years ago, following District implementation of a consumptive water use permit program, the ranch first applied for water withdrawal permits. These permits have been renewed as required and all water usage since the implementation of the program has been permitted. Turning to the reclaimed water supply, the delivery system, incorporating a program to pump reclaimed water from the treatment plant all the way back out to the ranch site, is subject to material failure and operator error, and either one can occur at any number of places along the system route. Each could result in interruption of the delivery of the reclaimed water to the ranch. The system is far more complex than would be the use of on-site wells for delivery of ground water. One two week shutdown in the system was occasioned by a major pipe failure as a result of pressure building up in the pipes. Were it not for the fact that a contractor was already at the ranch with replacement parts on hand to effect expeditious repair of the system, the shutdown could have lasted considerably longer than it did. This is not the only interruption, however. Several main line leaks and valve problems have caused the system to be shut down on several occasions for short periods of time. The filter system required for the water destined for the citrus area is problematical, and so far this area of the ranch has not received any reclaimed water in the 10 months the system has been in operation. Mr. Bishop argues that the wet weather holding pond is a solution to the reliability problems with the pipe line, but the pond has had problems of its own. Sand in the water, which comes from the holding pond, has been the primary difficulty in the filter system for the citrus area, and algae growth in that pond has the potential to create other filter problems. Delivery of the water from the pond is not accomplished by a gravity system, but instead, requires the use of pumps powered by an electric motor. In the event of a power failure, this source would be unavailable. Discounting all of the above, however, and assuming, arguendo, that all systems were in top operating condition, the fact remains that the delivery system from the pond to the distribution system is not adequate to supply the amount of water that would be necessary to have an effective freeze protection program. In any case, the reclaimed water supply is not the panacea for all water shortage problems experienced at Hi Hat Ranch. In the first place, the quality of the reclaimed water is generally lower than that of the groundwater which would come from wells on the ranch. Also, the City's treatment process does not remove from the water all the pollutants that are of concern to the farm operators. For one thing, total dissolved solids in the reclaimed water are considerably higher than in the ground water, and high dissolved solid levels can be harmful to citrus crops. In fact, the Institute of Food and Agricultural Sciences recommends that citrus irrigation water not exceed total dissolved solid ranges of from 1000 to 1500 milligrams per liter, (mpl). Testing done on the reclaimed water delivered to Hi Hat Ranch showed it averaged between 1200 and 1500 mpl. Though within recommended parameters, it was toward the high end. Further, reclaimed water is not totally interchangeable with ground water for all agricultural purposes. It cannot, by law, be applied to certain types of ground crops such as melons, nor can it be used for overhead citrus irrigation. There is also a restriction on the use of reclaimed water for pastures on which dairy cattle will be grazed. This all results in a restriction on the options available to the farmer who chooses to use reclaimed water in his irrigation plan. As a result, many farmers try not to use reclaimed water if they have access to adequate amounts of groundwater from on- site wells. Notwithstanding all the above, the parties agree that the use of reclaimed water for irrigation purposed is in the public interest. The District encourages it but nonetheless concedes that even with the availability of reclaimed water, a farmer should have access to wells on his property, in a standby capacity, as an alternative source of water to support his farming activities. Not only that, the agreement between the City and Hi Hat provides for Hi Hat to maintain its water use permit even while receiving reclaimed water from the City. Hi Hat is not the only farm operation with whom the City has negotiated in a effort to expand its wastewater distribution program. It has found in those negotiations, that most farm producers are not willing to rely totally on reclaimed water for all their irrigation needs, and it has concluded that were it mandatory that a farmer give up his on-site ground water withdrawals in order to utilize reclaimed water for a part of his needs, most would be reluctant to use it at all. This would seriously interfere with the City's ability to dispose of its surplus reclaimed water consistent with its policy. Even though Hi Hat's property lies within the Eastern Tampa Bay Water Use Cautionary Area, the rule pertaining thereto is inapplicable to Hi Hat because Hi Hat filed its application for permit, which was deemed complete, prior to the adoption of the rule. Nonetheless, water use officials agree that the proposed permit is consistent with the rule emphasis on the use and reuse of reclaimed water, and the District does not object to backup wells being permitted as supportive of the District's desire to keep ground water within the ground.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that Hi Hat Cattle and Grove be issued water use permit No. 204387.03, within the limits of the authorized quantities as indicated in the intent to issue, subject to conditions contained therein; except that the permit be amended to show well No. 5 as a non-standby well, and to delete standby wells from the terms and requirements of Special Condition 22. RECOMMENDED this 17th day of May, 1991, in Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 17th day of May, 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 PETITIONER: Accepted Accepted and incorporated herein. Accepted and incorporated herein. - 6. Accepted and incorporated herein. 7. - 11. Accepted. - 15. Accepted and incorporated herein. Accepted. Accepted. & 19. Accepted and incorporated herein. - 22. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. - 28. Accepted and incorporated herein. Accepted and incorporated herein. Rejected. She testified that Condition 28 of the permit provides this. Accepted. Accepted. Accepted and incorporated herein. Accepted. & 36. Accepted. Rejected as not supported by the evidence except that the method permitted was the method being used. - 40. Accepted. Ms. Jackson indicated she "assumed" some wells were drilled into the Florida aquifer. Rejected. Accepted as qualified by the comment, "depending on the respective potentiometric heads." - 47. Accepted. Accepted but incomplete. This is because they did not feel it was necessary under the circumstances. - 51. Accepted. Accepted. Accepted. Accepted. Accepted. Accepted and incorporated herein. Accepted. Redundant. - 61. Accepted. - 66. Accepted and incorporated herein. Accepted. More a restatement of testimony than a Finding of Fact Accepted and incorporated herein. & 71. Accepted and incorporated herein. - 74. Accepted. Accepted. First sentence accepted. Second portion rejected since cited case involves active wells versus standby, as here. The comparison made is accepted. The conclusion drawn as to validity is rejected. & 79. Accepted. FOR THE RESPONDENTS AND INTERVENOR: & 2. Accepted and incorporated herein. Accepted and incorporated herein. Accepted and incorporated herein. & 6. Accepted and incorporated herein. 7. - 10. Accepted and incorporated herein. 11. - 13. Accepted and incorporated herein. - 17. Accepted and incorporated herein. Accepted. Accepted. Accepted and incorporated herein. Accepted and incorporated herein. & 23. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not a Finding of Fact but a comment on the evidence. 27. Accepted. 28. & 29. Accepted and incorporated herein. 30. - 33. Accepted and incorporated herein. 34. - 37. Accepted and incorporated herein. 38. Accepted. 39. Accepted. 40. - 42. Accepted and incorporated herein. Accepted and incorporated herein, & 45. Accepted. 46. & 47. Accepted and incorporated herein. COPIES FURNISHED: Wyatt S. Bishop 5153 Tucumcari Trail Sarasota, Florida 34241 Bram D.E. Canter, Esquire Haben, Culpepper, Dunbar & French, P.A. 306 N. Monroe Street Tallahassee, Florida 32301 Edward B. Helvenston, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Barbara B. Levin, Esquire de la Parte & Gilbert 705 East Kennedy Blvd. Tampa, Florida 33602 Peter G. Hubbell Executive Director SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
The Issue The issue in this case is whether Water Use Permit (WUP) Application Number 20009478.005 meets the conditions for issuance as established in Section 373.223, Florida Statutes (2001), Florida Administrative Code Rule 40D-2.301 (April 2001), and the District’s Basis of Review for Water Use Permit Applications.
Findings Of Fact The Parties Petitioner, Alan Behrens, owns real property and a house trailer located at 4070 Southwest Armadillo Trail, in Arcadia, Florida. Behrens uses a two-inch well as the primary source of running water for his trailer. Boran and his family operate a ranch and sod farm in Arcadia, Florida, under the limited partnership of Boran Ranch and Sod, Ltd. Boran uses several different on-site wells to irrigate the farm. See Findings 12-17, infra. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries pursuant to Chapter 373, Florida Statutes, and Florida Administrative Code Rule Chapter 40D. Permit History Boran’s property is a little over 1,000 acres in size, on which he has raised cattle and grown sod for approximately the past four years. Before Boran owned the property, its prior occupants used the land for growing fall and spring row crops (primarily tomatoes). Boran's cattle and sod farm uses less water than was used by previous owners and occupants. In 1989, the original permit holders could make annual average daily withdrawals of 309,000 gallons but also were allowed a maximum daily withdrawal of 6,480,000 gallons. In 1992, the permitted withdrawals increased to an annual average daily quantity of 2,210,000 gallons, with a peak monthly limit of 3,596,000 gallons per day. On December 14, 1999, Boran received an agricultural water use permit (WUP No. 20009478.004) from the District. This current existing permit expires on December 14, 2009. The current permit grants Boran the right to withdraw groundwater for his agricultural use in the annual average daily quantity of 1,313,000 gallons, and with a peak month daily quantity of 3,177,000 gallons. On September 11, 2000, Boran filed an application to modify his existing water use permit. Modification of Boran's existing permit does not lengthen the term of the permit, and the scope of the District's review was limited to those features or changes that are proposed by the modification. The proposed modification would allow Boran to increase his annual average daily quantity by 175,000 gallons, and increase the peak month daily quantity by 423,900 gallons, for the irrigation of an additional 129 acres of sod. With the proposed increase, the new annual average daily quantity will be 1,488,000 gallons, and the new peak month daily quantity will be 3,600,900 gallons. The proposed modification also provides for the construction of an additional well (DID #6) on the southeastern portion of property, which will withdraw groundwater from the upper Floridan aquifer. The proposed agency action also entails a revision of the irrigation efficiency rating for the entirety of Boran Ranch. Irrigation efficiency refers to the ability to direct water to its intended target, which in this case means the root zone of the sod, without losing water to evaporation and downward seepage. Under the proposed permit modification, Boran will increase the entire farm’s water efficiency from 65 percent to 75 percent. As discussed further in the Conditions for Issuance section infra, the District's AGMOD modeling program uses this efficiency rating as part of its determination of the appropriate quantities for withdrawals. The higher the efficiency rating, the less water received under a permit. Because the efficiency rating increased, the application rate for water decreased from 42" per year to 36.4" per year for the entire Boran Ranch. Boran's Wells There are six well sites (labeled according to District identification numbers, e.g., DID #3) existing or proposed on Boran’s property. DID #1 is an eight-inch well located in the northeastern portion of the property. DID #1 provides water solely from the intermediate aquifer. DID #2 is an eight-inch well located in the middle of the property. DID #2 withdraws water from both the intermediate and upper Floridan aquifers. Both DID #1 and DID #2 were installed in 1968, and predate both the first water use permit application for the farm and the District's water use regulatory system. DID #4 is a twelve-inch well located in the north- central part of the property and solely taps from the upper Floridan aquifer. DID #4 had already been permitted and constructed as of the date of the proposed modification application at issue in this case. DID #3 and DID #5 are twelve-inch wells which have already been permitted for the southern and northern portions of the property, respectively, but have not yet been constructed. Both wells will withdraw water only from the upper Floridan aquifer. DID #6 is a proposed twelve-inch well to be located on the southeastern portion of the property and to irrigate an additional area of sod. DID #3, #5, and #6 will all be cased to a depth of approximately 540 feet, and only open to the upper Floridan aquifer to a depth of approximately 940 feet. By casing the well with pipe surrounded by cement, these wells will be sealed off to all aquifers above 540 feet, including the intermediate aquifer. All the wells on the property are used to irrigate sod. The wells have artesian flow, but utilize diesel pumps to provide consistent flow pressure year-round throughout the fields (some of which can be a mile and a half from a well). Since running the pumps costs money, there is an economic incentive not to over-irrigate. In addition, over-irrigation can lead to infestations of fungi and insects, and eventually cause the grass to rot and die. As a result, the fields receive irrigation only when dry areas in the fields appear and the grass begins to wilt. Boran Ranch Operations and Management Practices Boran Ranch primarily grows three kinds of grasses: St. Augustine Floratam; St. Augustine Palmetto; and Bahia. (Boran also is experimenting on a smaller scale with common paspalum and common Bermuda.) The Bahia grass, which is what also grows in the ranch's cattle pasture, does not require irrigation; the St. Augustine grasses are less drought- resistant and require irrigation at times. The majority of the sod sold to residential installers (who ordinarily work for landscape companies) is a St. Augustine grass. Commercial or governmental roadside installations favor Bahia. Currently, Boran sells more Bahia than St. Augustine. But market demand determines which types of grass are produced on the farm. As residential use and demand for St. Augustine in southwest Florida increases, so would the proportion of the farm used for growing St. Augustine grass. Boran grows sod year-round because of a large demand for the product in Ft. Myers and Cape Coral, and to a lesser extent in Punta Gorda and Port Charlotte. Sod helps control erosion and is considered to have aesthetic value. There also was some evidence that sod lowers the ambient temperatures, as compared to bare dirt; but the evidence was not clear how sod would compare to other ground cover in lowering temperatures. When subsurface seepage irrigation is being used, a sod field must be disked and "laser-leveled" to the proper elevation, with a slight slope created in the field to help ensure proper irrigation and drainage, before it can be used for sod production. The fields are laser-leveled before the irrigation system is installed and the crop is planted. The perforated irrigation supply lines of Boran Ranch’s subsurface irrigation system, also known as the "tile," run the opposite direction of the slope of the field and perpendicular to the main irrigation line. Once the subsurface irrigation system is installed, the field receives sprigs of sod, which are then watered and "rolled" to pack them into the ground. Approximately three months after a field has been rolled, the new sod is then periodically fertilized, sprayed and mowed. Sod takes approximately one year to grow before it may be harvested. The sod at Boran Ranch is harvested via tractor with a "cutter" on its side, which cuts underneath the grass, lifts it up onto a conveyor belt, and then onto a pallet for shipping. There are four different types of irrigation systems used for growing sod in Florida: (1) pivot systems which rely on sprinklers attached to overhead lines that rotate around a fixed point; (2) overhead rain guns which utilize motorized hydraulic pressure to spray a field; (3) above-ground seepage; and (4) subsurface irrigation systems (which can also be used to drain excess water from fields during large rain events). The most efficient irrigation system used for sod in Florida is the subsurface irrigation system. Boran Ranch first started the subsurface irrigation system approximately four years ago. Since that time, Boran Ranch has converted almost all its fields to the subsurface irrigation system, at a cost of approximately $1150 to $1350 per acre. As a result of this conversion process, Boran Ranch now uses less water per acre of sod. The subsurface irrigation system delivers water from a well to a water control structure (also known as the "box") via the imperforated main irrigation line. The perforated lines of the "tile" are connected to this main irrigation line at a 90-degree angle. The largest portion of the "box" sits underground. Once the water in the main irrigation line reaches the "box," water builds up behind removable boards contained in the box, creating the backpressure which forces water out into the tile. Water flows out from the tile to maintain the water table level at or near the root zone of the sod. Subsurface irrigation systems only function on property that has a hardpan layer beneath the soil. The hardpan layer acts as a confining unit to minimize the downward seepage of water, thereby allowing the subsurface irrigation system to work efficiently. Behrens questioned whether Boran Ranch has the necessary hardpan based on Todd Boran's reliance on hydrogeologists for this information. But the expert testimony of Boran's hydrogeology consultant and the District's hydrogeologist confirmed Todd Boran's understanding. Typically, the highest board in the box has the same height as the top of the field. Once the water level inside the box surpasses the height of the last board, water will spill over that board into the remainder of the box and then out another main irrigation line to the next box and set of tiles. By removing some of the boards in the box, Boran can bypass irrigating certain sections of his fields in favor of other areas. Excess water from the fields flows into field ditches which lead to wetlands on the property. If water leaves the wetlands during episodes of heavy rains, it flows downstream to the Peace River. Conditions for Issuance Boran Ranch is located in southwestern DeSoto County, in an area designated by the District as the Southern Water Use Caution Area (SWUCA). The District created the SWUCA, which covers 5,000 square miles, after first determining that the groundwater resources of eastern Tampa Bay and Highlands Ridge regions were stressed and creating the Eastern Tampa Bay Water Use Caution Area (ETBWUCA) and Highlands Ridge Water Caution Area (HRWUCA). Both the ETBWUCA and the HRWUCA are contained within the larger boundaries of the SWUCA. Within the ETBWUCA is an area along the coasts of portions of Hillsborough, Manatee, and Sarasota counties known as the Most Impacted Area (MIA). Special permitting rules exist for new projects located within the ETBWUCA, HRWUCA, and MIA, but not within the remainder of the "undifferentiated" SWUCA. Boran Ranch is located in this "undifferentiated" area of the SWUCA. Behrens took the position that Boran should not be permitted any additional water use until special permitting rules are promulgated for the "undifferentiated" SWUCA. But Behrens could cite no authority for such a moratorium. Meanwhile, the more persuasive evidence was that no such moratorium would be reasonable or appropriate. The evidence proved that the quantities authorized by the proposed modification are necessary to fulfill a certain reasonable demand, as required by Rule 40D- 2.301(1)(a). Boran sought additional water quantities through the permit modification application in order to irrigate an additional 129 acres of its sod farm. The application reflects a need for additional water, associated with additional acreage added to the farm. Boran used the District's AGMOD spreadsheet model, which is based on a mathematical methodology known as the modified Blainey-Criddle method, to determine the reasonable quantities for Boran's specific agricultural use. AGMOD inputs into its computations the following variables: (1) geographic location of the proposed use; (2) type of crop grown; (3) irrigation (efficiency); (4) pump capacity; (5) soil type; and (6) number of acres to be irrigated. AGMOD is a generally accepted tool used for determining the allocation of water quantities for agricultural use. In the instant case, the AGMOD calculations incorporated 87 years of rainfall data and its results reflect the quantities necessary in the event of a two-in-ten-year drought. Similarly, the AGMOD calculations in the instant case take into account the change in irrigation efficiency from 65 percent to 75 percent. Behrens suggested that Boran should not be allowed to use any more water until minimum flows and levels are established for the intermediate aquifer in the vicinity. However, Behrens could cite no authority for imposing such a moratorium. Meanwhile, the more persuasive evidence was that no such moratorium would be reasonable or appropriate. See Finding 49 and Conclusion 86, infra. Behrens also suggested that inputs to AGMOD should assume more Bahia and less St. Augustine grass so as to reduce the resulting amount of reasonable demand. He also suggested that Boran's reasonable demand should not take into account possible future increases in St. Augustine grass production based on possible future market demand increases. But it does not appear that the District requires an applicant to differentiate among various types of grasses when inputting the crop type variable into the AGMOD model for purposes of determining reasonable demand. See Water Use Permit Information Manual, Part C, Design Aids (District Exhibit 2C), Table D-1, p. C4-9. The evidence proved that Boran demonstrated that the proposed use will not cause quantity or quality changes that adversely impact the water resources, on either an individual or cumulative basis, including both surface and ground waters, as required by Rule 40D-2.301(1)(b). Data from water quality monitoring reports indicate that water quality at Boran Ranch and in the region has remained fairly consistent. There were no statistically significant declining trend in water levels in the region. Behrens admitted that water quality in his well has been consistently good. One apparent increase in total dissolved solids and chlorides in DID #1 was explained as being a reporting error. Boran inadvertently reported some findings from DID #2 as coming from DID #1. Until the error was corrected, this made it appear that water quality from DID #1 had decreased because, while DID #1 is open only to the intermediate aquifer, DID #2 is open to both the intermediate aquifer and the upper Florida aquifer, which has poorer water quality. Both Boran and the District used the MODFLOW model, a generally accepted tool in the field of hydrogeology, to analyze withdrawal impacts. The purpose of modeling is to evaluate impacts of a proposed use on the aquifer tapped for withdrawals, and any overlying aquifers including surficial aquifers connected to lakes and wetlands. MODFLOW uses mathematics to simulate the different aquifer parameters for each production unit determined from aquifer performance testing. During the permit application process, both Boran and the District conducted groundwater modeling by simply adding the proposed new quantities to models developed for Boran's permit application in 1999. The models were comparable but not identical; the District's model was somewhat more detailed in that it separated predicted drawdowns into more aquifer producing units. Both models satisfied the District that the proposed modification would have no adverse impact on water resources. After the challenge to the Proposed Agency Action, the District created a new model to assess the impact of only the additional quantities requested by the modification. This new model added some aquifer parameters obtained from Regional Observation Monitoring Program (ROMP) well 9.5, which was constructed very close to the Boran Ranch in 1999. (Information from ROMP 9.5 was not available at the time of the earlier models.) The new model allowed the District to limit the scope of its review to those changes proposed by the modification. The results of this model show that impacts are localized and that most are within the confines of Boran’s property. The greatest impacts resulting from the proposed modification would occur in the Suwannee Limestone producing unit (the upper-most portion of the upper Floridan aquifer), the unit to be tapped by DID #6. The confining unit above the upper Floridan aquifer in this region of DeSoto County is approximately 300-400 feet thick, and impacts on the intermediate aquifer, which is above this confining unit, are much less. When the District's new model was run for peak monthly withdrawals (423,900 gpd for 90 days), the model's 1.0 foot drawdown contour was contained within the confines of Boran’s property, and the 0.1 foot drawdown contour extended only approximately two miles out from the well node of DID #6. Atmospheric barometric changes can cause fluctuations in aquifer levels that exceed a tenth of a foot. As minimal as these modeled impacts appear to be, they are larger than would be expected in reality. This is because, for several reasons, MODFLOW is a conservative model- -i.e., impacts modeled are greater than impacts that would be likely in actuality. First, MODFLOW is a mathematical, asyntopic model. This means it models very gradually decreasing drawdowns continuing over long distances as predicted drawdowns approach zero. This tends to over-predict impacts at greater distances from the withdrawal. In reality, the heterogeneity or discontinuity of confining units cuts down on drawdown effects. The steepest drawdowns occur at a well node and then decline relatively rapidly with distance. Second, several model inputs are conservative. The annual average quantities for water use generated under the AGMOD methodology is based on a two-in-ten-year drought year. The peak month quantity applies to the three driest months within the two-in-ten-year drought period. The MODFLOW model applies this 90-day peak usage continuous pumping under AGMOD and conservatively assumes no rainfall or recharge to the aquifers during this period. Both of these are extremely conservative assumptions for this region of Florida. The District's determination of reasonable assurances "on both an individual and a cumulative basis" in water use permit cases only considers the sum of the impact of the applicant's proposal, together with all other existing impacts (and perhaps also the impacts of contemporaneous applicants). The impacts of future applicants are not considered. This differs from the cumulative impact review under Part IV of Chapter 373 (environmental resource permitting). See Conclusions 80-84, infra. Modeling is a component of the District’s assessment of impacts on a cumulative basis. In addition, the District reviewed and assessed hydrographs of the potentiometric surface from nearby ROMP wells, water quality data, permit history of the Boran site, and regional hydrologic conditions. The hydrographs represent the accumulation of all impacts from pumpage in the area and show stable groundwater levels in the region. Water quality also is stable, with no declining trends. The permit history indicates that permitted withdrawals on the Boran site have declined. For all of these reasons, the evidence was that Boran's proposed withdrawals would create no adverse impacts on water resources on a cumulative basis. The evidence proved that the proposed agency action will not cause adverse environmental impacts to wetlands, lakes, streams, estuaries, fish and wildlife, or other natural resources, as required by Rule 40D-2.301(1)(c). Due to the significant confinement between the source aquifers and the surficial aquifer and surface water bodies, the modeling results show no adverse impact to the surficial aquifer, and no adverse impact to wetlands, streams, estuaries, fish and wildlife, or other natural resources. The evidence was that there are no minimum flows or levels set for the area in question. Furthermore, Standard Condition 9 of the Proposed Agency Action requires Boran to cease or reduce withdrawals as directed by the District if water levels should fall below any minimum level later established by the District. The more persuasive evidence was that the requirements of section 4.3 of the District's Basis of Review have been met. (A moratorium on water use permits until establishment of minimum flows and levels would be neither reasonable nor appropriate.) The evidence proved that the proposed use will utilize the lowest water quality he has the ability to use, as required by Rule 40D-2.301(1)(e), because the new withdrawals are exclusively from the upper Floridan aquifer, which has poorer quality than the intermediate aquifer. Deeper aquifers cannot be used because the water quality is poorer than the upper Floridan aquifer, and it is technically and economically infeasible to use it for agricultural purposes. Behrens suggests that Boran should be required to discontinue all withdrawals of higher quality water from the intermediate aquifer as part of the proposed modification. While an offer to do so might be welcomed (as was Boran's offer to install subsurface seepage irrigation and apply the higher efficiency percentage to the entire Boran Ranch), Behrens could cite no authority for imposing such a condition; and the more persuasive evidence was that imposition of such a condition would be neither reasonable nor appropriate under the circumstances of this case. The evidence proved that the proposed use will not significantly induce saline water intrusion, as required by Rule 40D-2.301(1)(f), because the model results show that the drawdown contours do not approach anywhere near the ETBWUCA or MIA areas. Boran's Ranch is located approximately 21 miles from the MIA boundary and 10.8 miles from ETBWUCA boundary. Further, Boran must monitor the water quality in DID #1 and DID #4 and document any changes in water quality as a result of the withdrawals. The parties have stipulated that the proposed use meets the requirements of Rule 40D-2.301(1)(g) and will not cause pollution of the aquifer. The evidence proved that the proposed use will not adversely impact offsite land uses existing at the time of the application, as required by Rule 40D-2.301(1)(h), because the modeling showed no impact to the surficial aquifer or land use outside Boran Ranch. The confinement between the point of withdrawal and the surface is too great to impact offsite land uses in the instant case. The evidence proved that the proposed use will not adversely impact any existing legal withdrawal, as required by Rule 40D-2.301(1)(i), based on the ROMP hydrographs and modeling showing minimal drawdowns outside the boundaries of Boran Ranch. Behrens claims that Boran's proposed modification will adversely impact his well, which is approximately 3.5 miles northeast of the northeast corner of the Boran property and over four miles away from DID #6. But the greater weight of the evidence was to the contrary. (The wells of other DCAP members were even further away, making impacts even less likely.) Behrens has no independent knowledge of the depth of his two-inch well but believes it is approximately 150 feet deep, which would place it within the intermediate aquifer. In view of the consistent quality of Behrens' well water, and the nature of his well construction, it is most likely that Behrens' well does not penetrate the confining layer between the intermediate aquifer and the upper Floridan aquifer. If 150 feet deep, Behrens' well would not extend into the deepest producing unit of the intermediate aquifer (PZ-3); rather, it would appear to extend into the next deepest producing unit of the intermediate aquifer (PZ-2). But it is possible that Behrens' well cross-connects the PZ-2 and the shallowest producing unit of the intermediate aquifer (PZ-1). (The evidence did not even rule out the possibility that Behrens' well also is open to the surficial aquifer.) Assuming that Behrens' well is open to the PZ-2 only, conservative MODFLOW modeling predicts no impact at all from the proposed modification. (Behrens' well would be outside the zero drawdown contour.) Meanwhile, hydrographs of PZ-2 from nearby ROMP wells show marked fluctuations (five-foot oscillations) of the potentiometric surfaces in producing units of the intermediate aquifer. These fluctuations appear to coincide with increased pumping out of the intermediate aquifer. These fluctuations in the potentiometric surface are not being transmitted up from the upper Floridan aquifer or down from the surficial aquifer. The potentiometric surface in those aquifers do not exhibit matching fluctuations. It appears that the intermediate aquifer is being impacted almost exclusively by pumping out of that aquifer. (This evidence also confirms the integrity of the relatively thick confining layer between the intermediate and the upper Floridan aquifers, which serves to largely insulate Behrens' well from the influence of pumping out of the upper Floridan.) Behrens seems to contend that, in order to determine adverse impacts on a cumulative basis, the impact of Boran's entire withdrawal, existing and proposed, which is modeled conservatively at approximately 0.3 feet, must be considered. But the District considers an adverse impact to an existing legal withdrawal to consist of an impact large enough to necessitate modification to the producing well in order for it to continue to function as intended. The greater weight of the evidence was that the well on Behrens' property was not designed to be a free-flowing well but was designed to use a pump to operate as intended. At the time Behrens purchased his property, there was a well and a non-functioning pump on the property. Even at the beginning of his ownership, he did not always have running water without a functioning pump. In approximately 1986 or 1987, Behrens installed a new electric pump because it allowed the well to produce more water. After installation of the pump, Behrens raised his trailer an additional five feet (to guard against flooding) which caused it to be approximately ten feet high, meaning the water had to travel that much farther against gravity to reach Behrens' faucets. For most of the time that he has owned the property, Behrens has used a pump on the well. Behrens installed a check valve to allow him to turn off the pump. Sometimes during storm or flood conditions, electric power failed or was cut off, and Behrens was forced to rely solely on artesian flow, which was sometimes adequate in flood conditions during the rainy season. At other times when artesian flow was adequate, Behrens would turn off the pump and rely solely on artesian flow. But it also was sometimes necessary for Behrens to use the pump to get adequate water flow. During the summer of 2001, Behrens' pump failed, and he had to rely solely on artesian flow. As in prior years, artesian flow was sometimes inadequate. In order to be able to get at least some artesian flow for the maximum amount of time, Behrens lowered the spigot on his well by about two feet. Although Behrens is aware that the iron casing of his well could corrode over time, he has never called a licensed well driller or other contractor to inspect his well. Behrens did not test his own well for possible blockage that would result in a lower yield. Furthermore, Behrens admits that his whole outdoor water system needs to be completely replaced. The evidence proved that the proposed use will incorporate water conservation measures, as required by Rule 40D-2.301(1)(k), based on the water conservation plan submitted to the District, installation of a state-of-the-art irrigation system, increase in efficient use of the water, and decrease in the application rate. (Behrens' arguments that Boran has been allowed to use too much water and his question as to the existence of hardpan underlying Boran's fields already has been addressed. See Findings 27 and 35, supra.) The parties have stipulated that Boran has demonstrated that the proposed use will incorporate reuse measures to the greatest extent practicable, as required by Rule 40D-2.301(1)(l). The evidence proved that the proposed use will not cause water to go to waste, as required by Rule 40D-2.301(m), because the irrigation method is the most efficient system that is economically and technically feasible available for sod. (Behrens' question as to the existence of hardpan underlying Boran's fields already has been addressed. See Finding 27, supra.) The evidence proved that the proposed use will not otherwise be harmful to the water resources of the District, as required by Rule 40D-2.301(1)(n), based on the review of all other permit criteria. Propriety of Behrens' Purpose Behrens did not review the District's permit file on Boran's application before he filed his petition. The evidence suggested that he traveled to the District's Sarasota office for that purpose but found on his arrival that the complete permit file was not available for inspection there. Because of the filing deadline, he did not find time to make another attempt to review the permit file of record before he filed his petition. Behrens also did not contact Boran, the District or anyone else with any questions about the proposed agency action before filing his petition. He also did not visit Boran’s property, and made no inquiry as to the irrigation system employed by Boran. Behrens also did not do any additional legal research (beyond what he had done in connection with other water use permit proceedings) before filing his petition. Behrens believed he had all the information he needed to file his petition. Behrens has previously filed at least one unsuccessful petition challenging the District’s issuance of a water use permit. See Behrens v. Southwest Fla. Water Management Dist., DOAH Case No. 00-4801 (DOAH Jan. 29, 2001). DCAP, with Behrens acting as its president, has previously filed at least three unsuccessful petitions challenging the District’s issuance of a water use permit. See, e.g., DeSoto Citizens Against Pollution, Inc. v. Farmland Hydro Limited Partnership, DOAH Case No. 02-232 (Southwest Fla. Water Man. Dist. June 25, 2002); DeSoto Citizens Against Pollution, Inc. v. Southwest Fla. Water Management Dist., DOAH Case No. 01- 3056 (DOAH Aug. 22, 2001); DeSoto Citizens Against Pollution, Inc. v. Southwest Fla. Water Management Dist., DOAH Case No. 01-2917 (DOAH Sept. 24, 2001). However, none of those proceedings involved a project at the Boran site. It is found that, under the totality of circumstances, Behrens' and DCAP's participation in this proceeding was not for an improper purpose--i.e., not primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of Boran's permit modification. While a reasonable person would not have raised and pursued some of the issues raised by Behrens and DCAP in this proceeding, it cannot be found that all of the issues they raised were frivolous or that their participation in this proceeding was for an improper purpose. It appears that Behrens based his standing in part on the requirement in Rule 40D-2.301(1)(i) that Boran provide reasonable assurances that the proposed use will not adversely impact an existing legal withdrawal to be provided "on both an individual and a cumulative basis.” (Emphasis added.) Not unreasonably, Behrens argued that this requirement allowed him to base his standing on alleged injuries from all of Boran's withdrawals, existing and proposed, which would create a 0.3- foot drawdown on his well. While his argument is rejected, it cannot be found to be frivolous or made for improper purpose. Behrens' argument that Boran did not meet Rule 40D- 2.301(1)(i) was based on the 0.3-foot drawdown and his position that his well was designed to be artesian free- flowing. While Behrens' proposed finding was rejected, the position he took is not found to be frivolous or taken for improper purpose. Several other arguments made and positions taken by Behrens have been rejected. See Findings 27, 34, 35, and 51, supra, and Conclusions 86-87, infra. But they cannot all be found to have been frivolous or made and taken for improper purpose.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the District enter an order granting Boran’s water use permit application number 20009478.005; and denying the motions for attorney's fees and costs under Section 120.595(1), Florida Statutes. Jurisdiction is reserved to enter a final order on the part of the motions for sanctions under Section 120.569(2)(e). DONE AND ENTERED this 29th day of July, 2002, in Tallahassee, Leon County, Florida. Hearings Hearings ___________________________________ J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative 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 29th day of July, 2002. COPIES FURNISHED: Alan R. Behrens, President DeSoto Citizens Against Pollution, Inc. 4070 Southwest Armadillo Trail Arcadia, Florida 34266 Mary Beth Russell, Esquire Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Douglas P. Manson, Esquire Carey, O'Malley, Whitaker & Manson, P.A. 712 South Oregon Avenue Tampa, Florida 33606 E.D. "Sonny" Vergara, Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899
Findings Of Fact At all times pertinent to the issues herein, Respondent, Cargill, a Delaware corporation authorized to do business in Florida which owned and operated a phosphate mine near Fort Meade, located in Polk County Florida. Petitioner, Gloria Elder, owns residential property adjoining the Fort Meade Mine on which she maintains an individual water well for domestic and other purposes. The Respondent, District, has the responsibility for regulating the consumption and conservation of ground and surface water within its jurisdictional limits, including the well in question. For a period prior to December, 1990, Cargill had been operating under consumptive use permit No. 202297.04, issued by the District, which provided for average daily withdrawals of 12.0 MGD from wells on its property. In addition to the 12.0 MGD, Cargill also was utilizing an additional 3.3 MGD for mine pit and surficial aquifer dewatering activities which did not have to be reflected in the permit but which were lawful uses. In December, 1990, Cargill submitted its application to renew the existing water use permit with a modification including the 3.3 MGD previously being used but not officially permitted. No additional water would be drawn from the permitted wells as the newly applied for 15.3 MGD was the total of the 12 MGD and 3.3 MGD previously permitted and lawfully used. After reviewing the additional information requested of Cargill pertaining to this application, the District published its Notice of Proposed Agency Action for approval of the permit. The proposed permit authorizes withdrawal of the amount requested in the application, 15.3 MGD, the exact same amount actually withdrawn under the prior permit. As a part of the proposed permit the District imposed two special conditions. These conditions, 12 and 13, require Cargill to conduct its dewatering activities no closer than 1,500 feet to any property boundary, wetlands, or water body that will not be mined or, in the alternative, to mitigate pursuant to conditions 12 and 13 any activities conducted within the 1,500 foot setback. There are no reasonable alternatives to Cargill's request. The mining process in use here utilizes a water wash of gravel-size phosphate ore particles out of accompanying sand and clay. The water used for this purpose is recycled and returned to the washer for reuse. The resulting phosphate ore mix, matrix, is transported with water in slurry form to the refining plant. This system in the standard for phosphate mining in the United States. Once at the plant, the slurry is passed through an amine flotation process where the sand and phosphates are separated. This process requires clean water with a constant Ph balance and temperature which can be retrieved only from deep wells. Even though the permit applied for here calls for an average daily withdrawal of 15.3 MGD, typically the Cargill operation requires about 10.08 MGD from deep wells. This is a relatively standard figure within the industry. Approximately 92 percent of the water used at the site in issue is recycled. However, recycled water is not an acceptable substitute for deep well water because it contains matters which interfere with the ability of the chemical reagents utilized in the process to react with the phosphate rock. Therefore, the quantity sought is necessary and will support a reasonable, complete mining operation at the site. The Cargill operation is accompanied by a strenuous reclamation operation. Land previously mined near the Petitioner's property has been reclaimed, contoured, re-grassed and re-vegetated. This project was completed in 1990. No evidence was introduced showing that Cargill's operation had any adverse effect on the Elders' well. Water samples were taken from that well at the Petitioner's request in May, 1991 in conjunction with the investigation into a previous, unrelated complaint. These samples were submitted to an independent laboratory for analysis which clearly demonstrated that the minerals and other compounds in the water from the Petitioner's well were in amounts well below the detection level for each. Only the iron level appeared elevated, and this might be the result of deterioration of the 18 year old black iron pipe casing in the well. Another possible explanation is the fact that iron is a common compound in that part of the state. In any case, the installation of a water softener would remove the iron, and there is no indication the water would have any unacceptable ecological or environmental impacts in the area either on or off the site. No other residents in the area have complained of water quality problems. Petitioner claims not only that Cargill's operation would demean her water quality but also that its withdrawal will cause a draw down in the water level in her well. This second matter was tested by the District using the McDonald-Haurbaugh MODFLOW model which is well recognized and accepted within the groundwater community. The model was applied to the surficial, intermediate, and upper Floridan aquifers and indicated the draw down at the property boundary would be less than one foot in the surficial aquifer and less than four feet in the intermediate aquifer. The model also showed the draw down at the Petitioner's well would be less than three feet, which is well within the five foot criteria for issuance of a consumptive use permit under the appropriate District rules. This evidence was not contradicted by any evidence of record by Petitioner. All indications are that the water use proposed is both reasonable and beneficial, is consistent with the public interest, and will not interfere with any existing legal use of water.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore recommended that WUP Permit No. 202297.05 be renewed as modified to reflect approval of 15.3 MGD average daily withdrawal. Jurisdiction will remain with the Hearing Officer for the limited purpose of evaluating the propriety of an assessment of attorney's fees and costs against the Petitioner and the amount thereof. RECOMMENDED this 29th day of April, 1993, in Tallahassee, Florida. ARNOLD H. POLLOCK Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 29th day of April, 1993. COPIES FURNISHED: Joseph N. Baron, Esquire 3375-A U.S. Highway 98 South Lakeland, Florida 33803 Rory C. Ryan, Esquire 200 South Orange Avenue Suite 2600 Post office Box 1526 Orlando, Florida 32801 Martin D. Hernandez, Esquire Richard Tschantz, Esquire 2379 Broad Street Brooksville, Florida 34609 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899
The Issue The matter to be resolved by this Recommended Order concerns the Petitioner's Notice of Violation and Order of Corrective Action filed against the Respondent on the subject of alleged violations by the Respondent of the "Florida Safe Drinking Water Act", Sections 403.850 through 403.864, Florida Statutes. Within this complaint document there are six counts constituted of the following allegations: Count I. The Respondent does not continually apply effective disinfection measures to the water distributed to the service connections of the Respondent's water system. Respondent's water system has chlorination equipment installed but a chlorine residual is not continually maintained. This condition has existed since at least February, 1979. These facts show a violation of Rule 17- 22.106(3)(c), Florida Administrative Code. Count II. The Department has not received reports from the Respondent which contain information about the operation and maintenance of the water system. This condition has existed since at least April, 1978. These facts show a violation of Rule 17-22.111(2), Florida Administrative Code. Count III. The Respondent's water system has a daily flow of more than 2,500 gallons per day but less than 0.1 million gallons per day. The operation, maintenance and supervision, if any, of the water system is not performed by a person who has passed an examination that entitled such person to be a certified operator. This condition has existed since at least April, 1978. These facts show a violation of Rule 17-22.107(3)(b), Florida Administrative Code. Count IV. The slab surrounding the well casing has been broken exposing the system to possible contamination. This condition has existed since at least February, 1979. These facts show a violation of Rule 17-22.106(2)(c)2.e., Florida Administrative Code. Count V. The Respondent`s water system has no flow meter for accurately measuring the volume of water distributed by the public water system. This condition has existed since at least February, 1979. These facts show a violation of Rule 17-22.106(3)(g), Florida Administrative Code. Count VI. The Petitioner has incurred costs and expenses in the amount of $57.22 in the course of investigating the case and is entitled to be reimbursed pursuant to Subsection 403.860(3), Florida Statutes.
Findings Of Fact This case is presented for consideration based upon the Notice of Violation and Order of Correction filed by the Secretary of the State of Florida, Department of Environmental Regulation, on August 24, 1979. The action is taken against Arnold H. Parker, an individual who resides in Escambia County, Florida. On September 17, 1979, the Respondent, Parker, by and through his counsel answered the allegations of the Petitioner and requested a Subsection 120.57(1), Florida Statutes, hearing. The request for hearing was granted and on December 6, 1979, in Florida, a formal hearing was held to consider the Petitioner's complaint. (The essential elements of that complaint are reflected in the synopsis reported in the Issue statement of this Recommended Order.) The facts reveal that Daniel C. Walker, an employee of Petitioner, went to Perdido Key, Escambia County, Florida, in February, 1979, for the purpose of inspecting a water system owned and operated by the Respondent and to ascertain the number of service connections associated with the system. When Walker arrived at the location of the Respondent's well, he observed that the above-ground equipment utilized in pumping the water out of the ground was housed in a building. This building had a hole in the roof and the concrete slab surrounding the well casing was broken at the surface allowing for possible contamination by influent. At the time of the inspection a device for introducing chlorine into the extracted water was noted but that device was not connected and no chlorine residual was found in the water system. The water system was not being operated by a certified operator within the meaning of Rule 17-22.107(3)(b), Florida Administrative Code. In addition, the Respondent had not submitted operational reports to the Petitioner since April, 1978. The reports referred to are those reports required by Rule 17- 22.111(2), Florida Administrative Code. While Walker was at the general location of the well in onestion, he observed forty individual lots on which various types of trailers, campers and mobile homes could be found. Walker did not determine if persons were living in these shelters and he does not recall seeing persons in the area of the lots. The witness, Walker, did not observe any restaurant or public food establishment in the area of the well house and lots. On September 25, 1979, Robert Court, another employee of the Petitioner, went to the site of the well house and lots. At that time he counted thirty-two trailers, campers and mobile homes and each of those shelters had a service connection from the well of the Respondent located somewhere on the lot where the shelter was found. The service connection was in the form of a spigot. Court observed several people in the north-east section of the general area which is constituted of the well location and lots. Court returned to the location on November 30, 1979, and in a random survey saw approximately thirty-two trailers, campers and mobile hones. Subsequent to the visits of the employees, the Notice of Violation and Order of Correction was prepared by the enforcement section of the Petitioner and the cost of that preparation was $57.22. The Respondent, Arnold H. Parker, testified in the course of the hearing and his testimony established that there are nine persons who live in the area of the well on a year-round basis and these persons are served by the well during that period of time. Of the nine persons one family, the family of the Respondent, lives in a mobile home and the family is constituted of three persons, the Respondent, his wife and son. In a second mobile home the Respondent's daughter and her husband are found to reside. The final group of persons constituted of the nine full-time residents are the Respondent's daughter, her husband and two children in a third mobile home. Each lot on which the three mobile homes are found is served by a service connection. The remaining lots at the location in question were subdivided approximately two years prior to the hearing date and sold separately with the exception of the three lots where the nine permanent residents reside and two lots where other children of the Respondent resided prior to the February, 1979, inspection by the Petitioner's employee. Respondant sold twenty-four mobile home lots and twelve camper sites to persons other than family members and each of the mobile home lots and camper sites has a service connection to the well. Those persons who use the water system other than the nine permanent residents, use the system from mid-March through mid-September in the calendar year. During that time of usage, there are two families at two separate lots who come down during the week and use the water supply. The number of members in those families was not indicated in the course of the hearing. The balance of the persons using the water supply, excluding the above-mentioned two families and the nine permanent residents, use the shelters for vacation purposes and on the weekend. Some of this latter group would be vacationing in their summer home for a period as long as two weeks. The highest number of persons using the water from the well during the vacation period would be approximately forty persons during holiday weekends in the vacation cycle. From the testimony of the Respondent there would never be more than ten days during the vacation period in which twenty-five or more persons would be utilizing the water supply from the well. The water is brought into the trailers, campers and mobile hones by hoses attached to the spigot service connections and the hoses are removed when the individual owners are not in attendance. The lot owners who are served by the water system of the Respondent pay a fee of $18.00 a year, which the Respondent uses to repair the well pump, for pipe and for the cost of electricity to run the well. The well generating device is a two-horsepower electric pump and the well source is tapped by a two-inch service pipe. A one-half-inch line runs from the main to the service connectors (spigot). After the inspection of February, 1979, the Respondent repaired the broken slab around the well casing and these repairs were made in March or April, 1979. The repairs were depicted in the Respondent's Exhibits 1 and 2 admitted into evidence which are photographs of the well casing after the repair.
Recommendation It is recommended that the action taken by the Petitioner against Respondent pursuant to the Notice of Violation and the Order for Corrective Action be dismissed, to include the Petitioner's claim for costs and expenses. DONE AND ENTERED this 7th day of January, 1980, in Tallahassee, Florida. CHARLES C. ADAMS, Hearing Officer Division of Administrative Hearings Room 101, Collins Building Tallahassee, Florida 32301 (904) 488-9675 COPIES FURNISHED: William Hyde, Esquire Department of Environmental Regulation 2600 Blair Stone Read Tallahassee, Florida 32301 Barne J. Morain, Esquire 113 North Palafox Street Pensacola, Florida 32501
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 is whether Respondents should be subject to civil penalties and required to submit a Compliance Plan for the reasons stated in the Administrative Complaint and Order filed on January 8, 2002.
Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Background In this enforcement action, Petitioner, Southwest Florida Water Management District (District), proposes to assess civil penalties against, and require a compliance plan from, Respondents, Balm Associates, Inc. (Balm) and Goodson Farms, Inc. (Goodson), on the grounds that from March 1999 through July 2001 they made water withdrawals from certain property in Hillsborough County, Florida, without a water use permit, and after a permit was obtained in August 2001, they continued to exceed the annual average daily withdrawals authorized under the permit through the month of November 2001, or just prior to the preparation and issuance of the Administrative Complaint and Order (Complaint).1 While not denying that excessive pumpages may have occurred, and that a permit was not obtained until August 2001, Balm points out that it is the owner-lessor of the property and not the consumptive user of the water, and contends that the District has no authority to enforce its rules against, and recover civil penalties from, the non-user of the water. In its request for a hearing, Goodson did not specifically dispute the allegation that it consumed water without a permit, or exceeded the withdrawal limits under the new permit, but contended instead that the limits were unrealistic and should be modified. At the final hearing, however, Goodson disputed the accuracy of the water consumption figures used in the Complaint. The District is the administrative agency charged with the responsibility to conserve, protect, manage, and control water resources within its boundaries and to administer and enforce Chapter 373, Florida Statutes. Balm is a corporation registered to do business in the State of Florida. Its mailing address is 2101 Huntington Avenue, Sarasota, Florida 34232. It owns approximately 220 acres of land in Section 28, Township 31 South, Range 21 East, in Hillsborough County, Florida, which is the site of the alleged wrongdoing. Goodson is a corporation registered to do business in the State of Florida. Its mailing address is Post Office Box 246, Balm, Florida 33503. Goodson is in the farming business and operates a total of 13 farms, including the farm at issue in this proceeding. Permit Requirements Under Rule 40D-2.041(1), Florida Administrative Code, a water use permit is required whenever total withdrawal capacity from any source or combined sources is greater than or equal to 1,000,000 gallons per day (gpd); annual average withdrawal from any source or combined sources is greater than or equal to 100,000 gpd; or withdrawal is from a well having an outside diameter of 6 inches or more at the surface. Rule 40D-2.351(1), Florida Administrative Code, provides that a permittee must notify the District within 30 days of the sale or conveyance of permitted water withdrawal facilities or the land on which the facilities are located. The same rule also provides that where a permit has been issued to a party whose ownership or legal control of the permitted water withdrawal facilities subsequently ends, the party who assumes control over the facilities may apply to transfer the permit to himself or herself up to the renewal date of the transferor's permit. Finally, Rule 40D-2.351(2), Florida Administrative Code, provides that until a permit is transferred or a new permit is obtained, the party subsequently controlling the permitted water withdrawal facilities will be in violation of District rules for making withdrawals without the required permit. History of Permits on the Property On September 29, 1989, the District issued Water Use Permit No. 207135.001 (the .001 permit) to James Brown (Brown) and B & T Growers Partnership (B & T) for water withdrawals from one well for agricultural purposes on Balm's property. The .001 permit authorized annual average withdrawals of 102,000 gpd of groundwater for agricultural irrigation. On August 29, 1990, the District adopted new rules applicable to District permits within the Eastern Tampa Bay Water Use Caution Area (ETBWUCA). The .001 permit was within the ETBWUCA, and Brown and B & T were provided with a Notice of Permit Modification and new Permit Conditions. The new conditions became effective November 15, 1990. New Condition No. 5 provided that By July 31, 1995, all permitted withdrawal points shall be equipped with totalizing flow meters or other measuring devices as approved in writing by the Director, Resource Regulation Department. Such devices shall have and maintain accuracy within five percent of the actual flow installed. On December 14, 1992, the District approved the transfer of the .001 permit from Brown and B & T to B. Kenda Produce. The Unpermitted Water Withdrawals On June 30, 1997, Goodson entered into a two-year agricultural lease with Balm to use a portion of the property, including acreage previously used by B. Kendra Produce. At the time the lease was entered into, neither Respondent applied to the District to have the .001 permit transferred from B. Kendra Produce. It can be reasonably inferred from the evidence that after the first lease expired, the parties continued to execute new lease agreements at least through the time of the hearing. The portion of the property which Goodson leased and farmed is referred to as the "Sweat Loop Farm" and consists of approximately 100 acres. There is one well with an outside diameter of 10 inches at the surface located on the Sweat Loop Farm. The well's total withdrawal capacity is approximately 1,500 gallons per minute (gpm), which is over 1,000,000 gpd. Thus, withdrawals from the well required a water use permit. As noted earlier, Goodson operates a total of 13 farms on approximately 2,500 acres of land. There are approximately 15 wells on all 13 farms, including the Sweat Loop Farm. Michael E. Hare, an irrigation supervisor who is responsible for the irrigation of all 13 of Goodson's farms, installed a total of approximately 8 meters on the farms, including the meter on the Sweat Loop Farm. A totalizing flow meter, which was made by MiCrometer, was installed at the Sweat Loop Farm in June 1997. Mr. Hare acknowledged that he was familiar with MiCrometer meters and would be aware if the MiCrometer flow meter on the Sweat Loop Farm was not functioning properly. Whenever metering devices on the various Goodson farms have malfunctioned in the past, Mr. Hare has taken the malfunctioning meter to a metering company to be fixed. Goodson began irrigating the Sweat Loop Farm in June 1997. Since that time, Goodson has been the sole water user of the well on the farm. In March 1999, Goodson began submitting to the District monthly pumpage reports for the groundwater withdrawals on the Sweat Loop Farm. Although some unmeasured withdrawals presumably occurred prior to March 1999, the Complaint does not identify these as being a violation. Mr. Hare and other supervisors are responsible for collecting the meter readings which go on the monthly pumpage reports and providing them to the District. The information on the reports includes the permit number; the last month's meter reading; the current month's meter reading; the total gallons of water pumped for the current month; the meter total; and the meter factor. To determine the average daily withdrawal on the Sweat Loop Farm, the District relied upon the calculations provided by Goodson as to the total gallons of water pumped for the month and divided this number by 30 days. From March 1999 through July 2001, these quantities were as follows: MONTH/YEAR AVERAGE DAILY PUMPAGE March 1999 April 1999 531,487 No data available May 1999 364,930 June 1999 0 July 1999 0 August 1999 57,410 September 1999 49,563 October 1999 222,667 November 1999 250,667 December 1999 755,003 January 2000 689,433 February 2000 695,073 March 2000 544,427 April 2000 305,153 May 2000 597,720 June 2000 0 July 2000 62,120 August 2000 86,370 September 2000 123,233 October 2000 602,020 November 2000 409,550 December 2000 145,823 January 2001 957,690 February 2001 890,213 March 2001 391,280 April 2001 467,640 May 2001 617,177 June 2001 0 July 2001 0 Under Rule 40D-2.041(1)(a)-(c), Florida Administrative Code, a water use permit was required for Goodson's withdrawals since the well's total withdrawal capacity is approximately 1,500 gpm, which is greater than 1,000,000 gpd; the annual average withdrawals exceeded 100,000 gpd; and the well has an outside diameter of 10 inches at the surface. The withdrawals on the Sweat Loop Farm were not authorized by the .001 permit since neither Goodson or Balm was a permittee under the permit. Even if Goodson could rely on the permit, which it cannot, pumpage data provided by Goodson reflects that the water withdrawals (except for nine months) were in excess of that authorized by the permit. On June 16, 2000, the District mailed a Notice of Non-Compliance for excessive water withdrawals to Goodson. The Notice indicated that if the pumpage values submitted by Goodson were incorrect, Goodson was to explain the error and provide corrected quantities. On June 26, 2000, the District received a written response to the Notice of Non-Compliance from the superintendent of the Sweat Loop Farm who indicated that the pumpage values were correct, and that the excess usage was due to a "serious drought condition" which had caused a "significant financial hardship on [the] farm." The response also indicated that Goodson would contact Mr. Haftel, owner of Balm, to request that he "revise the water use permit for spring crops." On November 22, 2000, the District mailed Goodson a Notice of Violation indicating that the quantities authorized by the .001 permit were still being exceeded and that the District might seek monetary penalties if Goodson failed to come into compliance within 30 days. Despite the foregoing Notice, Goodson continued to make withdrawals without a permit and in excess of the quantities formerly authorized under the .001 permit until August 2001 when a new permit was finally obtained. Issuance of a New Water Use Permit On January 2, 2001, the District received an application for a General Water Use Permit seeking to modify the .001 permit to increase the withdrawal quantities and to transfer the permit from B. Kendra Produce to Balm. "Seymour Haftel/ Balm Associates, Inc." was listed as the applicant, and "Donn Goodson" from " Goodson Farms" was listed as the contact or consultant. Mr. Haftel signed the application on behalf of Balm. Goodson assisted Balm in securing the permit for the Sweat Loop Farm because Goodson wanted more water for irrigation purposes. Section 2.1 of the Basis of Review for Water Use Permit Application, adopted and incorporated by reference by Rule 40D-2.091, Florida Administrative Code, provides that "[a]pplications for leased property, except property leased from the District, must be either a joint application in the name of the lessee and the property owner(s) or be only in the name of the property owner(s)." In a Request for Additional Information mailed to Balm on January 29, 2001, the District asked whether Goodson should be listed as co-applicant on the application. On April 27, 2001, Balm submitted a response which indicated that Goodson should not be listed as co-applicant. On August 6, 2001, the District issued Water Use Permit No. 200007135.002 (the .002 permit) to Seymour Haftel/Balm Associates, Inc. authorizing an increase in the annual average withdrawals to 224,300 gpd. The permit had an expiration date of September 29, 2009. The permit contained a number of special conditions, none of which were challenged by Balm. Unauthorized Withdrawals Under the .002 Permit Special Condition No. 2 of the .002 permit requires in part that the permittee: continue to maintain and operate the existing non-resettable, totalizing flow meter(s), or other flow measuring device(s) as approved by the Regulation Department Director, Resource Regulation, for District ID No(s), Permittee ID No(s)[,] G-1. Such device(s) shall maintain an accuracy within five percent of the actual flow as installed. Total withdrawal and meter readings from each metered withdrawal shall be recorded on a monthly basis and reported to the Permit Data Section, Records and Data Department, (using District forms) on or before the tenth day of the following month. In the event a permittee chooses not to use a totalizing flow meter, as required by Special Condition No. 2, the District will review information provided by the measuring device's manufacturer to determine if the measuring device would maintain a five percent accuracy as required by the Condition. The meters have to be monitored and calibrated periodically for accuracy. It is the permittee's responsibility to comply with the conditions of the permit, including Special Condition No. 2, which requires the submittal of accurate pumpage reports. Goodson submitted the meter readings on behalf of Balm beginning in September 2001, which covered the withdrawals for the month of August 2001. The District relied on the meter readings submitted by Goodson to determine the annual average daily pumpage calculation for the .002 permit. The calculation is a running 12-month average, whereby each month the annual average daily quantity is recalculated based on the previous 12-month pumpage. The running annual average daily pumpage and percentage of pumpage which exceeded the .002 permit from August 2001 through May 2002 are as follows: MONTH/YEAR ANNUAL AVERAGE DAILY PUMPAGE PERCENTAGE OVERPUMPED August 2001 378,462 69 percent September 2001 382,622 71 percent October 2001 376,687 68 percent November 2001 383,008 71 percent December 2001 379,212 69 percent January 2002 327,343 46 percent February 2002 321,530 43 percent March 2002 350,701 56 percent April 2002 356,013 59 percent May 2002 338,131 51 percent As the foregoing data reflects, the withdrawals from the Sweat Loop Farm were in excess of that authorized by the .002 permit from August 2001 through May 2002.
Recommendation Based on 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 Respondents are guilty of the charges in its Administrative Complaint and Order except as concluded in paragraph 48 above and endnote 2 below; that Respondents be required to submit an acceptable written plan (Compliance Plan) to the District for its consideration and approval within fourteen days after entry of the final order; that the Compliance Plan describe how Respondents shall achieve full compliance with the .002 permit; that the Compliance Plan include reductions in withdrawals, water conservation measures, and development and utilization of alternative resources; that the Compliance Plan establish deadlines for implementation and completion of corrective actions; that full compliance be achieved within 120 days after entry of the final order; and that any failure of Respondents to comply with any provision of the Compliance Plan shall constitute a violation of the final order. DONE AND ENTERED this 30th day of July, 2002, in Tallahassee, Leon County, Florida. ___________________________________ DONALD R. ALEXANDER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 30th day of July, 2002.
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.
Findings Of Fact Petitioner seeks to irrigate 450 acres of pasture land. In preparing its application Petitioner consulted the soil conservation office to obtain the amount of water required under extreme drought conditions. Petitioner's maximum pumping capacity is 2,500 gallons per minute, 108 million gallons per month, or 5.56 gallons per acre per minute. The longest period in which applicant recalls running its pumps continuously was 3 weeks. This occurred during a drought period and after the pumps had been out of operation for an extended period. During normal drought conditions Petitioner would expect to run its pumps 18 days per month. At the pumping capacity available to Petitioner this would amount to 64.8 million gallons of water per month. The maximum monthly allocation recommended by Respondent was 66 million gallons. The source of water from which an allocation is sought is the Florida aquifer and none of the water removed therefrom by this Petitioner will return. The Florida aquifer for which the water herein requested will be obtained is presently being mined, i.e. more water is being withdrawn therefrom than is going back into the aquifer. In evaluating the application the C&SFCD engineer took the 30 to 40 years annual rainfall, the consumptive water use for the crops to be grown and the difference between these figures as the annual supplemental irrigation required. Correcting these figures for evapotranspiration rates and allowing for drought conditions occurring 2 out of 10 years the figures of 66.5 million gallons, or 263 acre feet per month maximum usage was reached. Respondent proposed two special conditions upon the Petitioner. One, that Petitioner submit a water quality analysis from the pump discharge in May and October of each year. The second condition was that a measuring device be installed upon the pump to measure the amount of water pumped. The water quality analysis will cost Petitioner approximately $70 per year for the test alone. An hours of operation clock on the pump will suffice for the water measuring device.
