The Issue The issue for consideration herein is whether Sarasota County Utilities should be issued a consumptive use permit to draw water from the 14 wells in issue here located in Sarasota County.
Findings Of Fact At all times pertinent to the issues herein, the Respondent, District, was the state agency responsible for themanagement of water resources within its area of geographical jurisdiction. Included therein was the responsibility for the permitting of consumptive water use. The Respondent, Sarasota County, is a political subdivision of the State of Florida and operates a public utilities division which is charged with meeting, among other things, the potable water needs of the residents of the County. Petitioners Wyatt S. Bishop and Joan Jones are both residents of Sarasota County and both draw their potable water from wells which utilize the aquifers pertinent to the wells for which the permit in issue here relate. Mr. Bishop lives approximately 7.5 miles north of the Carlton Reserve, the property on which the wells in issue are located, and Ms. Jones lives approximately 7 miles from the Reserve, but in a different direction. Sarasota County filed an application for a consumptive use permit with the District on January 28, 1987 requesting an average daily withdrawal of 10.71 million gallons per day, (mgd), and a peak monthly withdrawal of 15.55 mgd. This application, assigned number 208836.00, was, over the next three years, amended by the County four separate times. These amendments reflected revised water demand determinations and were submitted to provide additional information requested by the District. The District issued a preliminary staff report and proposed intent on March 26, 1991 reflecting an approved withdrawal in the amount of 7.28 mgd average daily withdrawal and 11.1 mgd peak monthly withdrawal. These figures were revised, however, byan amendment by the District on July 8, 1991, and as amended, authorize 7.303 mgd average daily withdrawal and 9.625 mgd peak monthly withdrawal. The County's application was reviewed by an experienced hydrologist in the District office with extensive permit review experience who utilized, in his evaluation of the permit, the pertinent District rules and policies. By way of background, to more easily understand the circumstances here, Sarasota entered into a contract with Manatee County in 1973 which called for the latter to provide up to 10 mgd of water for a period of 40 years, up to and including the year 2013. However, in 1979, Manatee County's utilities director advised Sarasota County that it, Sarasota County, could not continue to rely on Manatee County's water after the expiration of the current contract, and would, therefore, have to become self sufficient in water. Since the MacArthur tract, now known as the Carlton Reserve, had just recently been identified by, inter alia, the United States Geological Service as a potential long term water source for Sarasota County, after Manatee County advised Sarasota County of its future expectations, Sarasota County and the Manasota Basin Board hired a consulting firm to conduct hydrological testing on the Carlton Reserve. This study concluded that the Reserve had sufficient water resources to satisfy the needs of the unincorporated areas of Sarasota County for an extended time into the future. In 1985, because of its increased water needs and thetime necessary to complete required studies on the utilization of the Myakka River, a surface water resource, Sarasota County concluded that it was suffering a water supply shortage and entered into a supplemental contract with Manatee County to provide 2 million gallons of water per day over a 5 year period which would expire in 1990. Sarasota County had not, however, been idle with regard to the investigation of other water resources. Studies done included not only the Myakka River mentioned above but a reservoir owned by the City of Bradenton, and the Peace River. Nonetheless, it was determined that the Carlton Reserve was the best source available overall, and in 1987, the County filed the application in issue here. The permit was under consideration for approximately 3 1/2 years before the initial decision by the District to grant it. During that time the County experienced a significant deficiency in its water sources and found it necessary, on February 5, 1991, to enter into another contract with Manatee County to supply an addition 5 mgd. Terms of that contract clearly indicate the expectations of both parties that Sarasota County will take reasonable steps to develop its own water resources. It is not as though Sarasota County sat quietly in the interim, however, and allowed the situation to develop. A building moratorium to halt additional construction was proposed and as a result, economic forces in the County indicated a potential loss of jobs to County residents. None of this would be desirable from an economicstandpoint. In the course of the permit application process, 12 test wells were sunk to conduct aquifer pump tests; to assess water quality, amounts and availability, aquifer characteristics and drawdown; and to determine the impact of withdrawal on water quality. Eight of these 12 wells are located on the Carlton Reserve. The other 4 are located on property owned by the MacArthur Foundation which is contiguous to the Carlton Reserve property and from which Sarasota has a right by easement to draw water. The 2 wells yet to be constructed will be on Sarasota County property. Sarasota County currently receives 10 mgd of water under its contract with Manatee County; an additional 5 mgd under the February 5, 1991 contract; 2 mgd from the University wellfield, (with a peak withdrawal rate of 3 mgd); and .9 mgd from the Sorrento wellfield, (with a peak withdrawal rate of 1.1 mgd). This latter source is only producing currently .6 mgd of potable water due to constraints imposed by the water treatment requirements. Taken together, the current Sarasota County supply constitutes 18.6 mgd. The above does not take into account the County's agreement with the City of Sarasota calling for the purchase of up to 2 mgd. Since this source is not reliable, it is not included in the total, and the City is not considered an available water source. In addition, the District and Sarasota County stipulated on July 15, 1991 that within 30 days, the County would apply tophase out routine water production from the Sorrento wellfield, relying on it only in emergency situations with District consent. For this reason, it, too, is not considered an available water supply source. These currently existing sources, with modifications as described, will be the primary sources of potable water provided to 6 major service areas in Sarasota County when the County's water treatment plant and transmission system are complete in 1993. In attempting to define the County's future water requirements, two major criteria were considered. The first was the County's historical water demand, and the second, modifying it, relates to the demand arising as a result of new water users being added to the system as a result of the County's capital improvements and acquisition program. Water resources are not unlimited. Current resources come primarily from Manatee County and there are constraints on this supply as it is made available to Sarasota County. For example, the 10 mgd contract expires in 2013. The 5 mgd contract expires in 2001. Though the latter is subject to renewal, renewal is contingent upon the availability of water supply at that time, and that is not a sure thing. It can, therefore, readily be seen that 15 out of the 18.6 mgd routinely available now comes from Manatee County, and those sources are not perpetual. In addition, it is conceivable that Manatee County may pre-blend the water it delivers to Sarasota County with water of lesser quality, so that the delivered water may exceed the total dissolved solids standard of 500 ppm for potable water. If thewater from Manatee County were reduced to that quality, the University wellfield supply, which currently exceeds standards itself, and which relies on blending with better quality Manatee County water to be potable, would also be removed as a source of potable water to Sarasota County. In order to comply with the provisions of Section 373.171, Florida Statutes, which requires the District to regulate the use of water by apportionment, limitation, or rotating uses, to obtain the most beneficial use of water resources and to protect the public health, safety and welfare, the District analyzed the available water sources and determined that Sarasota County relies upon its 10 mgd supply from Manatee County and the 2 mgd supply from University wellfield to constitute 12 mgd usable water. The 5 mgd from Manatee County would be used only in an emergency situation, and the Sorrento wellfield would be abandoned. Future water demands must be predicted relying in great part upon an historic record of prior water use. Utilizing a statistical procedure called linear regression, a methodology accepted by the District, indicated a water demand figure for the period from 1992 to 1997 based upon six use points extending from 1985 to 1990. These use records reflected a low of 9.733 mgd and a high of 12.808 mgd, the former being in 1985 and the latter in 1990. In addition, the County estimated that its capital improvement program would add between 10 and 12 thousand customers who presently use private wells, whose water use would constitute approximately 2 mgd of additional demand. The County's program toacquire some 42 private franchises now serving customers would add an additional demand of 2 mgd. Taken together, these programs would add in approximately 1.8 mgd per year to the need assessment, and it would therefore appear that by 1997, the County's average daily demand, considering all new users, would be 17.84 mgd. The water to be drawn from the Carlton Reserve is not currently potable and will require some form of treatment to render it so. Sarasota County proposes to use the Electrodialysis Reversal process, (EDR), because, in the County's judgement, it is more efficient than others such as reverse osmosis and ion exchange. Whereas EDR is rated at up to 85% efficient, the others range between 50% to 75% efficient. In that regard, in order to determine the maximum amount of water to be drawn, providing a safety factor for a treatment plant operation that is not working up to peak capacity in computing the water needs, the EDR process was determined to be no more than 80% efficient. Factoring in that efficiency potential, when the 1997 average daily demand is subtracted from the County's projected water capacity, the withdrawal need in 1997 is determined to be 7.303 mgd. However, as a part of its permitting process, the County also calculated its peak month daily demand. This is a figure which represents the maximum amount permitted to be drawn on a daily basis during the peak demand period. This peak period was determined under Section b 3.2 of the District's Basis of Review by taking the 1989 daily flow and using a sliding 31 day calendar to determine the highest historical 31 day flow. Thisresulted in a peak month coefficient of 6.16 which was then multiplied by the 1997 average daily demand of 17.842 mgd which resulted in a peak month daily demand of 20.7 mgd. When existing water supplies are removed and the 80% EDR treatment process factor is applied, the amount of raw water needed from the wellfield in issue on a peak monthly basis would be 9.625 mgd. This peak monthly basis figure is considered because of the intermittent periods of low rainfall and high water demand within the County. Accepting the 1.8 gpd yearly increase; the peak factor of 1.16; and the assumed water supply capacity of 18.6 mgd; Sarasota County's need will exceed its available supplies by 1993. In fact, the County is already experiencing low water pressure in part of its service area during peak demand periods. County experts estimate that without the requested water from the Carlton Tract, Sarasota County can expect to experience dry periods as early as 1993 during the periods of peak water usage, generally between April and June. For the above reason, when the application and its supporting information was reviewed by Mr. Basso, the District hydrologist with extensive experience reviewing more than 300 water use application, he determined that the water supplies requested are necessary to meet the County's certain reasonable demand, and that this meets the criteria set out in Rule 40D - 2.301(1)(a), F.A.C. Turning to the issue of hydrologic and environmental impacts, the District's Basis For Review of Water Permit Applications provides for the use of a "water use model" inevaluating water needs and the appropriateness of a proposed withdrawal. In preparing its submittal to the District, Sarasota County performed certain tests and modeling to derive the statistical and scientific information used in support of its application. Specifically it used the USGS' MODFLOW model utilizing information obtained from the pump tests run on the wells in the pertinent areas. Consistent with the District's rule, the water data and aquifer drawdown were determined by simulated pumping. The tests run also provided the information on water quality in the aquifer and physical characteristics including transmissivity, storage coefficient, specific yield and leakance between aquifers. This data also helped in defining the hydrogeologic framework of the Carlton Reserve. The Carlton Reserve's hydrogeology listed in descending order from the surface, includes a surficial aquifer which varies in depth between 19 and 70 feet across the Reserve; a semi-confining clay unit separating it from the intermediate aquifer; the upper intermediate and lower intermediate aquifer which range in depth from 140 to 180 feet across the Reserve; another confining layer, and the Upper and Lower Floridan aquifers. The hydrology and groundwater modeling expert who constructed the model used in Sarasota County's permit application concluded that the water table drawdown at the Reserve property boundary in the surficial aquifer would be less than .3 of a foot; less than .4 of a foot in the intermediate aquifer; and 2.9 feet in the Upper Florida aquifer. The water to be drawn consistentwith this instant permit, if approved, would come from the Upper Floridan aquifer on the Reserve. The County's experts were conservative in the assumptions used in the groundwater model. It was assumed there would be no lateral water flow into the model area and no recharge. In addition, the model called for all pumps to run simultaneously at a maximum drawdown of 12.65 mgd for 90 days rather than at the requested quantity of 9.625 mgd. Utilization of these assumptions provided a scenario wherein "severe" impacts would be encountered. Based on the testing and the modeling done, expert opinion was that there would be no quantity or quality changes that would adversely effect water resources including ground and surface water. This meets the criteria of Rule 40D-2.301. This opinion was concurred in the District's hydrology expert. Nonetheless, in its proposed approval, the District has imposed special permitting conditions which require the County to monitor, analyze, and report water quality and water table level information to the District on a monthly and annual basis. When it evaluates the information supplied by an applicant relating to ground water monitoring, the District is required to consider certain presumptions set forth in its Basis For Review. For example, the District presumes that if there is a drawdown of more than 1 foot in the surficial aquifer at a wetland, adverse environmental impacts will occur. In the instant case, the County model concluded that the actual drawdown in the surficial aquifer at the Carlton Reserve is less than .6 of onefoot and, therefore, there should be no adverse environmental impact resulting from the withdrawal. Nonetheless, the County has developed several plans designed to provide information on environmental impacts which will continuously monitor such parameters as rainfall and evaporation, wetlands hydroperiod changes and vegetative changes in the wetlands to detect any changes which might be attributed to the water pumping. These plans have been made special conditions to the water use permit, and in the opinion of the County's ecology and hydrology expert, would enable the County to adequately monitor and detect any pertinent changes to the pertinent factors concerned on the Carlton Reserve. If wetland changes are detected, a contingency plan will be in effect which will require an alteration of pumping schedules or other action to minimize any adverse impacts. The District expert in wetlands and wildlife habitat has opined that these measures, with which he is familiar, are adequate to insure that adverse impacts to the wetlands will not occur. This is consistent with the provisions of Rule 40D-2.301(1). As was stated previously, the water to be drawn pursuant to this permit will be drawn from the Upper Floridan aquifer. This water is not potable but is treatable and is the lowest quality water which can be economically used by the County. Water of a lower quality does exist in the Lower Florida aquifer, but it is not economically treatable, and, in addition, use of this Lower Floridan aquifer might cause vertical movement of the poorer quality water into the upper strata. For all practical purposes,then, the lowest quality water available to it will be used by the County and this is consistent with the District's basis for review. Expert testimony indicates that saline water will not be infused into the Upper Floridan aquifer. Salt water intrusion generally occurs when groundwater is brought to a level below sea level. Even at the point of maximum actual drawdown as a result of pumping on the Reserve, the fresh water level will remain at least 20 feet above sea level, and as a result of the difference in water level, no saline water intrusion into the fresh water supply will occur even though salt water intrusion can also occur as a result of upward vertical movement of lower quality water due to withdrawal. The District's hydrologist and reviewing official also concluded that because of the confining layer below the aquifer from which water will be withdrawn, there would not be any significant upward movement of lesser quality water. The District's basis of review also envisions an aquifer pollution if a proposed withdrawal would spread an identified contamination plume. Here no contamination has been identified in the area from which the water will be drawn, and therefore, contamination would not be spread. The Basis for Review also infers there will be adverse impact to off site land if there is a significant drawdown of surface water bodies or if damage to crops or other vegetation can be expected. Here, the water table drawdown at the boundary of the Carlton Reserve is anticipated at less than .3 of one foot and any drawdown further out from the Reserve can be expected tobe even less. As a result, no adverse impact to existing off site land useage is expected. With regard to Rule 40D-2.301(1)(i), relating to an adverse impact on existing legal uses, the District presumes that no adverse impact will exist if the drawdown in the water table is no more than 2 feet at an affected well, or the potentiometric surface at the well is not lowered by more than 5 feet. Here, again applying the County's groundwater modeling demonstrates that the drawdown at its worst, in the Upper Floridan aquifer, would be no more than 2.9 feet at the Reserve boundary and much less at the Petitioners' wells. Both Mr Bishop's and Ms. Jones' wells are approximately 7.5 and 7 miles, respectively, from the closest well on the Reserve property. Ms. Jones' well is drilled into the intermediate aquifer which is above that which the County proposes to use and should not be impacted. Mr. Bishop draws water from the intermediate and surficial aquifers, both of which are above the Upper Florida aquifer identified for use here, and the groundwater modeling would suggest that his well would not be impacted either. Sarasota County's application contains reference to numerous proposals for water conservation measures which it intends to implement or has already implemented. It has adopted ordinances to enforce the District's watering restrictions and is currently implementing a block inverted use rate structure to promote conservation. It has developed programs for use in the schools outlining water conservation efforts and is developing programs topromote the increased use of treated waste water for golf course irrigation. The requirement for a water conservation plan such as is described and envisioned by the County is a condition of the water use permit proposed, and in addition, the County has adopted an Ordinance, (90-38) which modifies its building code to require installation of water conservation devices in new buildings erected in the County. It has developed proposals for conservation measures such as water auditing, meter testing, leak detection, system looping, and pressure reduction, and has selected the EDR process of water purification as the most efficient use of groundwater resources. Petitioner, Bishop, testified to his belief that approval of this permit and the resultant water withdrawal on the Carlton Reserve would necessitate an expansion of the boundaries of the District's Eastern Tampa Bay Water Use Caution Area to a point where his property would be encompassed therein. In support of his position, Mr. Bishop offered a notice to the effect that new ground water withdrawals would not be permitted within a certain "most impacted area" within the caution area. There was, however, no independent evidence from hydrologists, geologists, or other conservationists, or individuals familiar with the water conservation process, to support Mr. Bishop's contention that either the boundaries would be expanded or that withdrawal of the proposed permitted amounts of water from the Carlton Reserve would cause the boundaries to be expanded. By the same token, Mr. Bishop's contention that theproposed withdrawal from the wells here in issue would adversely effect his ability to draw water from his existing well was not supported by any expert testimony or documentary evidence tending to support or confirm his contention. He had no evidence tending to contradict the County's and District's experts, all of whom indicated there would be no adverse impact on the environment or water resources as a result of the instant permit. Similarly, neither Petitioner offered any evidence of a demonstrative nature that would draw any connection between the proposed permitted withdrawals and potential salt water intrusion and water level drawdown in their wells. The County introduced construction permits issued by its own health department covering 8 of the 12 wells which have been drilled on the Carlton Reserve as test wells. These wells were clearly sunk pursuant to an agreement between the District and the County's public health unit which delegates authority for water well construction permitting to the County. Taken together the documentation indicates that these 12 wells on the Reserve were installed and permitted pursuant to and consistent with appropriate permitting processes, and the testimony of Mr. Bassarab, the County's expert who oversaw the installation of the wells, reflects they are appropriately grouted and sealed. Therefore, there will be no mixing of lower quality water from the lower portion of the Floridan aquifer with the better quality water from the upper portion of that aquifer. The County's evidence clearly refutes the allegation by Mr. Bishop that the 12 test wells currently existingon the Carlton Reserve were neither permitted nor inspected as required by the District. County Commissioner Hill, who testified on behalf of the Petitioners, indicated that the wells applied for here are unnecessary and an inappropriate expenditure of County funds. She claimed there are other valid sources of water available to the County, including that extracted from excavated shell pits and seawater from the Gulf of Mexico which could be treated and desalinated. The Commissioner's comments as to alternate sources are not specifically rebutted. However, she is neither an expert in hydrology or hydrogeology, and her testimony is not persuasive. While other water sources may exist, the better evidence clearly indicates that those sources are not sufficient to meet the County's needs or are otherwise inappropriate for use by the County in sufficient quantity to satisfy those needs.
Recommendation Based on the foregoing Findings of fact and Conclusions of Law, it is, therefore: RECOMMENDED that consumptive water use permit No. 208836.00, providing for authorized quantities as outlined in the intent to issue, subject to conditions contained therein, be issued to Sarasota County. RECOMMENDED in Tallahassee, Florida this 5th day of September, 1991. ARNOLD H. POLLOCK Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 5th day of September, 1991. APPENDIX TO RECOMMENDED ORDER The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on all of the Proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONERS: Rejected as not supported by the evidence. Accepted. Accepted. - 8. Resolved against the Petitioners on the basis information presented by Respondents. 9.- 13. Accepted and incorporated herein. 14. - 16. Accepted and incorporated herein. Accepted and incorporated herein. & 19. Accepted and incorporated herein. 20. - 23. Accepted. Accepted but not dispositive of any issue. Accepted. & 27. Noted as citation of authority. Rejected. & 30. Accepted as restatements of evidence but not as Findings of Fact. 31. Irrelevant. 32. Rejected 33. & 34. Not a error is, in fact, it is such. 35. - 38. Irrelevant. 39. - 43. Accepted. 44. Accepted. 45. Rejected. 46. Accepted and incorporated herein. 47. & 48. Rejected as a mere citation of testimony. 49. Not understandable. Not a Finding of Fact. 50. Accepted. 51. Evidence is acceptable. 52. Not sufficiently specific to rule upon. 53. Not proven. 54. Not specific. 55. & 56. Rejected. FOR THE RESPONDENTS: 1. - 4. Accepted and incorporated herein. 5. & 6. Accepted and incorporated herein. 7. & 8. Accepted and incorporated herein. 9. - 14. Accepted and incorporated herein. 15. - 17. Accepted and incorporated herein. 18. - 21. Accepted and incorporated herein. 22. & 23. Accepted and incorporated herein. Accepted. - 27. Accepted and incorporated herein. 28. & 29. Accepted and incorporated herein. 30. - 32. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. Accepted. - 37. Accepted and incorporated herein. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. - 43. Accepted and incorporated herein. Accepted. Accepted and incorporated herein, - 48. Accepted and incorporated herein. Accepted - not a Finding of Fact. Accepted and incorporated in substance herein. Not correct as stated. Sarasota County will not be withdrawing saline water from the upper Floridan aquifer. The remaining discussion is accepted. Accepted and utilized. & 54. Accepted. Accepted and incorporated herein. Accepted. - 59. Accepted and incorporated herein. 60. Accepted. 61 - 63. Not Findings of Fact but comments on the evidence. Accepted and incorporated herein. & 66. Not Findings of Fact. COPIES FURNISHED: Wyatt S. Bishop, Jr. 5153 Tucumcari Trail Sarasota, Florida 34241 Joan Jones 719 East Baffin Road Venice, Florida 34293 William A. Dooley, Esquire Nelson, Hesse, Cyril, Smith, Widman, Herb, Causey & Dooley 2070 Ringling Blvd. Sarasota, Florida 34237 Cathy Sellers, Esquire Steel, Hector & Davis 215 S. Monroe Street Tallahassee, Florida 32301-1804 Peter G. Hubbell Executive Director Southwest Florida Water Management District 2379 Broad Street Brooksville, Florida 34609-6899 Edward B. Helvenston, Esquire Vivian Arenas, Esquire SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
The Issue The issues are whether the proposed amendment to Rule 40E- 2.041(1), Florida Administrative Code, exceeds the agency's grant of rulemaking authority; enlarges, modifies, or contravenes the specific law implemented; or is vague, fails to establish adequate standards for agency discretion, and vests unbridled discretion in the agency.
Findings Of Fact Based upon all of the evidence, the following findings of fact are determined: Petitioner, Osceola Fish Farmers Association, Inc. (OFFA), is a non-profit corporation whose members consist of tropical fish farmers in Osceola County, Florida. The parties have stipulated that OFFA has standing to bring this action. Respondent, South Florida Water Management District (District or Respondent), is a public corporation operating pursuant to Chapter 373, Florida Statutes, with its principal office in West Palm Beach, Florida. Among other things, the District has the authority to regulate the uses of water within its geographic boundaries, including Osceola County. On an undisclosed date, the District began test drawdowns (a lowering of the elevation of the water through control structures) in the Alligator Chain of Lakes just east of St. Cloud in Osceola County, where OFFA's members are engaged in tropical fish farming. The drawdowns were undertaken for the purpose of allowing the Florida Fish and Wildlife Conservation Commission (FFWCC) to conduct demucking activities in the lakes to enhance aquatic habitat. Prior to beginning work, the FFWCC obtained an Environmental Resource Permit from the Department of Environmental Protection (DEP). However, the District did not require either itself or the FFWCC to obtain a consumptive use permit on the theory that a lake drawdown for demucking activities was not a consumptive use and therefore did not require a permit. In an effort to halt future scheduled drawdowns, OFFA participated in a United States Army Corps of Engineers proceeding which culminated in the preparation of an Economic Impact Statement for FFWCC's drawdowns; filed a complaint with DEP under Section 373.219(2), Florida Statutes, alleging that an unlawful consumptive use (without a permit) was taking place (which complaint was found to be insufficient); filed an action for injunctive relief in circuit court under Section 403.412, Florida Statutes (which was dismissed or dropped for undisclosed reasons); and finally initiated a proceeding against the District under Section 120.56(4), Florida Statutes, alleging that the District had adopted "an incipient non-rule policy of exempting lake 'drawdowns' from water use permitting requirements" (DOAH Case No. 00-3615RU). To avoid the consequences of an adverse ruling in the latter action, the District began rulemaking proceedings to adopt an amendment to Rule 40E-2.041(1), Florida Administrative Code, to codify its policy relative to lake drawdowns. As amended, the rule reads as follows: Unless expressly exempt by law or District rule, a water use permit must be obtained from the District prior to any use or withdrawal of water. The drawdown of lakes for environmental, recreational, or flood control purposes is not regulated by Chapter 40E-2 or 40E-20, F.A.C. (Underscored language represents amended language). Petitioner has challenged only the amendment, and not the existing rule. The effect of the rule is obvious - a lake drawdown for one of the three stated purposes in the rule will not require a permit, while all other lake drawdowns will. As specific authority for the proposed amendment, the District cites Sections 373.044 and 373.113, Florida Statutes. The former statute authorizes the District to "adopt rules pursuant to [Chapter 120] to implement the provisions of this chapter," while the latter statute authorizes it to "adopt rules pursuant to [Chapter 120] to implement the provisions of law conferring powers or duties upon it." The District has cited Sections 373.103(1), 373.219, and 373.244, Florida Statutes, as the specific laws being implemented. The first statute provides that if specifically authorized by DEP, the District has the authority to "administer and enforce all provisions of this chapter, including the permit systems established in parts II, III, and IV of [Chapter 373], consistent with the water implementation rule"; the second statute provides in relevant part that the District may "require such permits for consumptive use of water and may impose such reasonable conditions as are necessary to assure that such use is consistent with the overall objectives of the district or department and is not harmful to the water resources of the area"; and the third statute provides for the issuance of temporary permits while a permit application is pending. In regulating the uses of water within its boundaries, the District administers a comprehensive consumptive water use permit program under Part II, Chapter 373, Florida Statutes. Both parties agree that under Section 373.219(1), Florida Statutes (2000), all "consumptive uses" of water require a permit, except for the "domestic consumption of water by individual users," which use is specifically exempted by the same statute. The global requirement for permits is also found in Rule 40E-2.041 (the rule being amended), as well as Rule 40E- 1.602(1), which provides in relevant part that unless expressly exempted by statute or rule, "[a] water use individual or general permit pursuant to Chapters 40E-2 or 40E-20, F.A.C., must be obtained prior to use or withdrawal of water " The term "consumptive uses" is not defined by statute, but the District has promulgated a rule defining that term. By Rule 40E-2.091, Florida Administrative Code, the District has adopted by reference a document known as the "Basis for Review for Water Use Permit Applications with the South Florida Water Management District." Section 1.8 of that document contains definitions of various terms used in the permitting program, including "consumptive use," which is defined as "[a]ny use of water which reduces the supply from which it is withdrawn or diverted." The District's policy for lake drawdowns, as proposed in the rule amendment, is inconsistent with this definition. On this disputed issue, Petitioner's evidence is accepted as being the most persuasive, and it is found that a lake drawdown for any purpose is a consumptive use of water. Section 373.219(1), cited as a specific law being implemented, provides that the District "may require such permits for consumptive use of water and may impose such reasonable conditions as are necessary to assure such use is consistent with the overall objectives of the district and department and is not harmful to the water resources of the area." The District construes this language as authorizing it to decide which uses of water are a "consumptive use," and which are not, and to implement a rule which codifies those decisions relative to lake drawdowns. Not surprisingly, Petitioner views the statute in a different manner and argues that the statute simply allows the District to create a permit program that is consistent with Chapter 373; that under the law a permit is required for all consumptive uses, including lake drawdowns; and that the District has no authority to carve out an exception for a lake drawdown from the permitting process, no matter what the purpose. As noted above, the District has identified three instances (for environmental, recreational, and flood control purposes) when a lake drawdown does not require a consumptive use permit. These terms are not so vague that a person of common intelligence would have difficulty understanding them. However, the proposed rule contains no prescribed standards to guide the District in its administration of the rule.
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
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
Findings Of Fact Upon consideration of the oral and documentary evidence adduced at the hearing, the following relevant facts are found: Respondent owns real property located in Township 2 North, Range 7 East, Section 32, in Madison County, Florida, that has surface water flowing through it and is encompassed within what is defined as "wetlands." Respondent is in control and possession of the property in question and all work on the property that is material to this proceeding is under the control or direction of the Respondent. There were access roads on the property as early as 1973 as reflected by Respondent's exhibit 2, a 1973 aerial photograph, but the width of the roads or the existence of ditches or culverts cannot be determined from the photograph. Petitioner's exhibit 2, a 1981 aerial photograph, shows the roads still in existence in 1981 but the width of the roads or existence of ditches or culverts cannot be determined from the photograph. Sometime before the Respondent purchased the property and began construction to expand the roads, ditches and culverts were in place; however, there was no evidence as to when the ditches and culverts came to be in place. A 1976 survey of the property reflects 60 foot roads which were to provide access to platted but unrecorded lots. These roads had not been constructed when Respondent purchased the property or began construction to expand the roads. The newly constructed portions of the road indicates an attempt to build the roads in accordance with the 1976 survey. The previously existing roads attempted to follow the natural contour of the land and as a result were not always straight, and only had a negligible effect on the flow or storage of surface water in regard to the property. Sometime around October 1987, Respondent began to rebuild and construct roads on the property by straightening existing curves, removing fill material from adjacent wetlands to widen and heighten the existing roadbed or construct a new roadbed, and to increase the depth and width of existing ditches or dig new ditches. The initial portion of the existing road providing access to the property from the county graded road has been substantially rebuilt with portion of the roadbed being 40 to 43 feet wide. Ditches along this portion of the roadbed have had their width increased up to 14 feet and their depth increased up to 6 and 8 feet. Other portions of the road has been expanded beyond the previously existing roadbed by increasing the width and height of the roadbed. The increased size of the ditches and the expanded roadbed has increased the interception of surface water above that already being intercepted by the previous roadbed and ditches and, as a result, there is an increased amount of surface water impounded or obstructed. The effect is that surface water is removed from Respondent's property at a faster rate than before road construction began and, as a result, sheet flow of surface water is decreased which diminishes the storage of surface water on the property. Although new culverts were installed during road construction, there was insufficient evidence to show that these new culverts were in addition to the culverts already in place or if they replaced old culverts. There was insufficient evidence to show that the new culverts allowed water to flow in a different direction or be removed from the property at a faster rate than before or if they impounded or obstructed surface water more so than before. The previously existing roads had sufficiently served an earlier timber harvest on the property and, by Respondent's own testimony, were sufficient for his ongoing hog and goat operation. The extensive rebuilding and constructing of roads in this case was neither necessary nor a customary practice for construction of farm access roads in this area. Respondent is engaged in the occupation of agriculture in that he has a bona fide hog and goat operation. However, Respondent's silviculture occupation is somewhat limited in that he is presently harvesting the timber but shows no indication of replanting or continuing the forestry operation upon completing the present harvesting operation. The extensive rebuilding and constructing of roads in this case goes beyond what is necessary or is the customary practice in the area for a hog or goat operation or forestry operation such as Respondent's and is inconsistent with this type of agriculture or silviculture occupation. Respondent has never applied for nor received a surface water management permit from the Petitioner even though the Petitioner has informed Respondent that a permit was required for the work being done on his property. The present alteration of the topography of the land by Respondent has obstructed and impounded surface water in such a fashion that the interruption of the sheet flow of surface water has been increased, causing the storage of surface water on the property to be diminished. At the present time, Respondent has been enjoined by the Circuit Court of Madison County, Florida, from any further activity on this project. However, should Respondent be allowed to complete this project, it is evident that the sole and predominant purpose would be to impound and obstruct the sheet flow of surface water and diminish the storage of surface water on the property in question.
Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence of record and the candor and demeanor of the witnesses, it is, therefore, RECOMMENDED that the Petitioner, Suwannee River Management District, enter a Final Order requiring Respondent, Norman Leonard, to: (a) remove all unauthorized fill material placed within jurisdictional wetlands and return those areas to predevelopment grades and revegetate with naturally occurring local wetlands species to prevent erosion; (b) back fill excavated swale ditches, return road beds and excavated ditches to predevelopment condition and grades and seed disturbed non-wetland areas with a 50:50 mix of bahia and rye grass and; (c) refrain from any other development until and unless a required permit is obtained for such development. Respectfully submitted and entered this 13th day of February, 1989, in Tallahassee, Leon County, Florida. WILLIAM R. CAVE Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 13th day of February, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE NO. 88-1445 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 in this case. Specific Rulings on Proposed Findings of Fact Submitted by Petitioner 1. Adopted in Finding of Fact 1. 2.-3. Adopted in Finding of Fact 2. 4.-7. Are unnecessary findings for this Recommended Order. Adopted in Finding of Fact 18. Adopted in Finding of Fact 19. Adopted in Finding of Fact 10. Adopted in Finding of Fact 11. Subordinate to the facts actually found in this Recommended Order. Adopted in Finding of Fact 11. Adopted in Finding of Fact 12. Rejected as conclusions of law. Adopted in Findings of Fact 3 and 4. Adopted in Finding of Fact 8. Adopted in Finding of Fact 9. Adopted in Finding of Fact 9. Adopted in Finding of Fact 8. Adopted in Finding of Fact 6. Adopted in Finding of Fact 7. Adopted in Finding of Fact 6. Adopted in Finding of Fact 10. Adopted in Findings of Fact 15 and 17. 26.-29. Adopted in Finding of Fact 12. 30. Adopted in Finding of Fact 13. 31.-32. Subordinate to facts actually found in this Recommended Order. Adopted in Finding of Fact 12. Adopted in Finding of Fact 16. 35.-38. Subordinate to facts actually found in this Recommended Order. 39.-42. Rejected as not being relevant or material. Specific Rulings on Proposed Findings of Fact Submitted by Respondent 1. The first paragraph adopted in Finding of Fact 16. The balance is rejected as a conclusion of law. 2.-3. Rejected as not being relevant or material. Not a finding of fact but a statement of testimony. However, it is subordinate to facts actually found in this Recommended Order. Rejected as not supported by substantial competent evidence in the record. The more credible evidence is contrary to this finding. COPIES FURNISHED: Janice F. Baker, Esquire Post Office Box 1029 Lake City, Florida 32056-1029 Norman Leonard, Pro Se Route 2, Box 172-D Live Oak, Florida 32060 Donald O. Morgan Executive Director Suwannee River Water Management District Route 3, Box 64 Live Oak, Florida Dale H. Twachtmann, Secretary Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32399-2400
Findings Of Fact This application is a request for a consumptive water use permit for six wells at the following locations: LATITUDE LONGITUDE 28 degrees 20' 50" 82 degrees 41' 36" (hereinafter referred to as Garden Terrace No.1) 28 degrees 20' 50" 82 degrees 41' 35" (hereinafter referred to as Garden Terrace No.2) 28 degrees 20' 55" 82 degrees 39' 11" (hereinafter referred to as Parkwood Acres No.1) 28 degrees 21' 20" 82 degrees 39' 11" (hereinafter referred to as Parkwood Acres No.2) 28 degrees 21' 49" 82 degrees 38' 56" (hereinafter referred to as New Well No.1) 28 degrees 21' 50" 82 degrees 38' 56" (hereinafter referred to as New Well No.2) Although included in the application, it appears from the record of this proceeding that Garden Terrace No. 1 is to be abandoned by applicant upon completion of its new facilities and therefore is not intended for inclusion in any consumptive water use permit issued pursuant hereto. Further, it appears from the records that the applicant intends to use Garden Terrace No. 2 as an emergency standby supply well only and therefore its average daily withdrawal as reflected on the application is not intended to be included in a consumptive water use permit issued pursuant hereto. Therefore, with those amendments the application seeks, from a total of five wells, a maximum daily withdrawal of 1,501,000 gallons and an average daily withdrawal of 650,000 gallons. The use of this water is for public water supply and appears to be a reasonable, beneficial use consistent with the public interest and not interfering with any legal use of water existing at the time of the application. Further, according to testimony of the staff of the Southwest Florida Water Management District it does not appear that any of the matters set forth in Subsection 16J-2.11(2), (3) or (4), F.S., exist so as to require the denial of this permit. The staff recommendation is that this permit be granted for a maximum daily withdrawal of 1.50 million gallons per day and an average daily withdrawal of .650 million gallons per day. The staff recommendations are subject to the following conditions: That all individual connections to the system be metered. That the permittee shall install totalizing flow meters of the propeller driven type on all withdrawal points covered by this permit with the exception of those wells which are currently gaged together using a single meter. That the permittee shall submit to the District a record of his pumpage for each meter. Said pumpage shall be read on a monthly basis and submitted quarterly to the District by April 15, July 15, October 15, and January 15, for each preceding calendar quarter. That the permittee have water samples from all wells permitted analyzed for chloride on a monthly basis and results submitted to the District by April 15, July 15, October 15 and January 15 for each preceding calendar quarter. That to promote good water management and avoid salt water intrusion that the water be withdrawn at an average of .217 million gallons per day from each of the three following wells: Parkwood Acres Well No. 1, Parkwood Acres Well No. 2, and New Well No. 1. New Well No. 2 shall be operated only to meet peak demand. That Garden Terrace Well No. 2 be used only as an emergency standby well. The applicant entered no objections to the conditions set forth above nor were there any objections from members of the public to the issuance of this consumptive water use permit.
Recommendation It is hereby RECOMMENDED that a consumptive use permit be issued for the five subject wells for the withdrawal of 1.30 mgd maximum daily withdrawal and .65 mgd, average daily withdrawal subject to the conditions set forth in paragraph 4 above. DONE and ORDERED this 15th day of July, 1976, in Tallahassee, Florida. CHRIS H. BENTLEY, Hearing Officer Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304 (904) 488-9675 COPIES FURNISHED: Jay T. Ahern, Esquire Southwest Florida Water Management District P.O. Box 457 Brooksville, Florida 33512 Delmar Water Corporation 731 West Main Street New Port Richey, Florida 33552
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 THE PARTIES CMI is a Florida corporation authorized to do business in Florida. CMI owns a mine site as is depicted in the permit application, which mine site is known as "Pine Level". Alan R. Behrens owns residential property approximately two miles from Pine Level, which abuts Horse Creek. He maintains an individual well for domestic and other purposes, and is a substantially affected person under the statute. Charlotte County is a government entity and a political subdivision of the State of Florida, and is a substantially affected person under the statute. The City of North Port is an incorporated municipality of the State of Florida, and is a substantially affected person under the statute. The Environmental Confederation (ECOSWF), a citizens group, is a substantially affected person under the statute. The District is the agency with the responsibility for reviewing and ruling upon CMI's water use permit application. APPLICATION AND PROCESS CMI proposes to operate a phosphate mine facility at "Pine Level" ("site"). The site is located approximately seven miles west of Arcadia, DeSoto County, Florida. The mine reserves at the site are approximately 17,700 acres. 9,000 to 10,000 acres are projected for mining. In 1978, Consumptive Use Permit No. 200103, was issued and in 1986, the current owners purchased the corporation which held the permit, and changed the name of the corporation to CMI. The Industrial Water Use Permit has not been used since it was issued to a prior owner of the site, and provided for average daily withdrawals of 13.6 mgd from wells. In 1984, this permit was renewed and modified to provide for average daily withdrawals of 12.8 mgd from deep wells. The groundwater withdrawals currently sought by CMI is 6.9 million gallons per day ("mgd") average daily withdrawal, which totals include 5.1 mgd from deep wells for use in the amine flotation process and 1.7 mgd for sealing the matrix slurry pumps. This reduction to 6.9 mgd in permitted withdrawals is a significant reduction. In addition, the proposed permit allows 3.7 mgd to be withdrawn from the surficial aquifer by dewatering mine cuts. In November, 1990, CMI submitted an application for renewal. In November 1991, CMI submitted to the District a revised Water Use Application No. 200103.02 ("application") to renew and modify the existing water use permit. The District requested more information, and CMI provided additional information and supplemental responses to aid in the review and evaluation of the application. The District prepared and submitted a Notice of Intent to Issue Permit and the District staff has prepared a "draft" Permit No. 200103.02 authorizing the withdrawal of the quantities requested in the application with certain conditions. In addition to renewal and modification of the water use permit, which is the subject of this proceeding, CMI will be required to participate in numerous regulatory reviews and permitting procedures (i.e. a development of regional impact evaluation, a federal environmental impact statement, federal approvals under the Clean Water Act [including a national pollutant discharge elimination system ("NPDES") permit], and a conceptual reclamation plan review) before CMI may commence mining, and consequently, begin any withdrawal of water. The mining process will utilize large walking draglines to excavate over burden and stack it beside the active mining area for land reclamation. The ore material called "matrix" will be dug up by the draglines, placed into an earthen pit where it will be slurried with a high pressure water jet. A pump will pick up this slurried matrix material, pump it back to the processing plant where it will first go through various separation devices, including screens and cyclones. The course material termed "pebble" will be separated and parts of that will be directly saleable as a product. The bulk of the phosphate product is contained in intermediate-sized material called concentrate feed. The concentrate feed consists of ore and sand. The ore is separated from the sand in a process called "flotation". The flotation process is a two stage process that ends up separating the tailings sand, which can then go back to the sand-clay flocculation and mixing units, and be pumped out ultimately for land reclamation back in the mine-out areas. The phosphate product which is called "wet rock", is placed in storage bins where it can drain, and be loaded onto rail cars for shipment. The "amine flotation process" is the second stage of flotation where sand and phosphates are separated. This process requires clean water for the amine flotation phase, because any amount of contaminants, including organic reagents, will adversely affect the process. Any mineral particles must be removed so that the amine may attach itself to the phosphate. Any contaminants will destroy or significantly and adversely affect not only the phosphate recovery, but the entire flotation process. Deep well water is requested for use in the amine flotation process because it is clean. All phosphate mines in Florida currently rely on deep well water. 5.2 mgd is the minimum amount of "clean" water needed to assure efficient processing of the amine flotation process of the mine beneficiation plant. Deep well withdrawals are also commonly used for the purpose of sealing or protecting the packing of pumps at various points in the mine system in order to avoid damage to the equipment. These wells are often referred to as "sealing water wells". The Pine Level mine will require 1.7 mgd for this purpose. Water for the sealing water wells must be clean and clear in order to effectively seal pumps for leaks. The Pine Level project will provide 400-500 construction jobs during the construction period. It will provide approximately 200 full-time jobs with an annual payroll of about five million dollars once it is in operation. It will result in about one thousand additional jobs providing services to the development. It will pay in excess of one million dollars a year to DeSoto County in ad valorem taxes. TECHNICAL CRITERIA The water use is a reasonable and beneficial use. 5.2 mgd groundwater withdrawal is "necessary to fill a certain reasonable demand." The technical criteria relating to water level or rates of flow impacts set forth in Rule 40D-2.301(1)(d), Florida Administrative Code, are not applicable in this proceeding because the District has not established any regulatory levels or rates of flow for the area encompassed by the application. In addition, this presumption only addresses surface water withdrawals. Phosphate mining is a beneficial activity and is consistent with the public interest. There is no significant risk of salt water intrusion. The water use withdrawal will not degrade the water quality in the aquifer by causing any contamination plume to spread. There have been no contaminant plumes identified on site. GROUNDWATER IMPACTS There is sufficient ground water at the site of a suitable quality and quantity to support the proposed phosphate mining and beneficiation activities. The local hydrogeology at the site consists of an upper layer known as the surficial aquifer. Rain penetrates the surficial aquifer to flow vertically to the water table. The water that is not consumed by vegetation at this layer will flow either to a nearby stream channel or will leak down through a semi- confining layer. The water continues to seep vertically into the lower underlying limestone aquifers. There are three limestone water-bearing layers: the intermediate, the Suwannee or Upper Floridan, and the Avon Park or Lower Floridan aquifers, respectively. The intermediate and the underlying Suwannee aquifer are separated by another semi-confining layer. Likewise, the Avon Park aquifer and the Suwannee aquifer are separated by another semi-confining layer. At the site, wells in the intermediate aquifer will draw water to seal the bearings on the matrix slurry pumps. There will be one deep well in the Suwannee and one deep well in the Avon Park to draw for the beneficiation plant. The groundwater modeling performed by CMI simulated the four aquifers, that is, the surficial aquifer and each of the three limestone aquifers. An Aquifer Performance Test ("APT") was performed at the site. The data generated from the APT was used to calculate various aquifer parameters, for example, transmissivity, storage coefficient, and leakiness. This information was then used in setting up the groundwater flow model that ultimately was incorporated into the application. During the District staff's review of the application, the deep well withdrawal quantities requested by CMI were compared with approximately 6 other phosphate mines of comparable size, acreage, and type of operation. As a result of this comparison, the staff found CMI's requested use to be less than the other six phosphate mines. The use of recycled water in the amine flotation process in place of deep well water in the past by CMI has proven unsuccessful because a constant temperature and a constant ph level could not be maintained with recycled water, and recycled water contains traces of fatty acids and oils, which also negatively affect the amine flotation process. C.F. Industries, Inc., has been operating a phosphate mine in Hardee County, Florida, since 1978. C.F. Industries, Inc., has since 1983 at the Hardee County mine, successfully substituted recirculation water for deep well water for operation of the amine flotation circuit on a routine basis. C.F. Industries, Inc., presently plans to employ substitution of some recirculation water for deep well water in a new yet-to-be permitted mine. C.F. Industries, Inc., at its existing Hardee County mine requires use of deep well water for start-up purposes to "charge" the system. C.F. Industries, Inc., at its existing mine, uses deep well water to respond to abnormal operational conditions, including excessive rainfall events, when the quality of the normal recirculation water is not suitable for substitution of deep well water. Neither CMI, nor District staff was aware prior to hearing, that the C.F. mine was successfully substituting recycled water for deep well water in the amine flotation process. At the time of making the representations to the District about necessary water quality requirements of the flotation process, CMI had a study, entitled, Amine Water Evaluation, Pine Level Project, July 27, 1984, ("Pilot Plant Study"), which concluded that deep well pumping and discharge could be reduced by use of water drawn from mine cuts. The Pilot Plant study was site specific to CMI's proposed phosphate mine. The Pilot Plant study bench tests were verified in the same pilot plant facility CMI uses to verify the grade of ore on the Pine Level Site. The Pilot Plant study or its results were known to CMI officials or experts involved in the permit application at issue in this case. CMI did not inform District staff of the existence or conclusions of the Pilot Plant study. The Pilot Plant study indicates that CMI could reduce its water usage by substituting water from mine cuts for deep well water. CMI did no studies to determine if the substitution of mine cut water for deep well water, as suggested by the Pilot Plant Study, was feasible to implement. SURFACE WATER IMPACTS The phosphate ore (matrix), is extracted by an excavation machine called a "dragline", which opens mining cuts of approximately 32 to 35 feet in depth, 330 feet wide, and up to 4,000 feet long. Seepage occurs into the mine cuts from the water table, and must be pumped out in order to see and extract the matrix. This dewatering is also necessary to protect the draglines against slope stability problems. Water pumped out of the mining cuts is introduced into the mine water recirculation system which is operated for purposes of collecting and recycling water within the mine complex. The matrix that is extracted from the mining cut is placed in a shallow excavation near the cut, and is converted to a slurry and, thereafter, transported hydraulically to the mine processing (or "beneficiation") plant. The beneficiation plant uses considerable quantities of water, utilizing supplies from within the mine system (i.e. surface water) and water from deep wells. Sand tailings and sand and clay mixture are by-products of the mining process. Recycled water is used to transport waste clay and sand from the plant to the disposal and reclamation areas. Reclamation takes 1-2 years for areas reclaimed with sand tailings and 5-6 years for areas reclaimed with a sand-clay mixture. Groundwater that is used in the processing plant is recycled. Water within the mine is recycled a number of times, and CMI's proposal calls for 90 percent of the total mine demand to be satisfied by this recirculation system and approximately 96 percent of the water used is recyclable water. DEWATERING AND WATER BALANCE CMI's mine pit dewatering activities result in the withdrawal of water from the surficial aquifer. A "water balance" demonstrates that requested quantities relate to reasonable mining, processing, and dewatering needs. The "water balance" for the mining operation evidences a balance between sources and uses/losses. The sources of water in the CMI water balance that input to the mining operation include groundwater from wells (6.9 mgd), mine cut dewatering or water table drainage (3.7 mgd), and collected rainfall (3.1 mgd). Uses and losses associated with the mining operation include water retained in clays (6.7 mgd), water shipped with final product (.7 mgd), evapotranspiration and evaporation (3.0 mgd), water used for agricultural irrigation (5.0 mgd), and water seeping from the Mine Water Surge Area ("MWSA") (1.2 mgd). The water balance matrix moisture component of 2.9 mgd is not a withdrawal of water for water use permitting purposes. The District's modeling of the impacts resulting from mine cut dewatering resulted in a finding of 2.34 MGD as opposed to the 3.7 mgd derived by CMI. For calculation purposes, rainfall is collected at the rate of 3,974 gallons per acre per day. CMI calculates that it will collect 3.1 mgd of rainfall, and use it in its recirculation system. The 3.1 mgd calculation is based on the amount of rain that will fall on 600 acres of mine water surge area, 80 acres of plant site, and two 50 acre mine cuts. CMI plans to mine 450 acres each year at the Pine Level Site over a period of 22 years. Runoff over disturbed areas on the CMI mine site must be captured, and will become part of the recirculation system. Assuming only one year of disturbed area during the permit term, CMI has failed to account for nearly 1.8 mgd in its water balance (450 acres x 3,974 gallons/acre/day). CMI plans to pump any rainfall collected from all disturbed areas to the mine water surge area (MWSA). CMI has not included any acres of disturbed area in its calculations of the amount of rainfall it will collect for the current permit. CMI has not submitted a mine plan. Without a mine plan, the number of disturbed acres cannot be determined. Because CMI's water balance does not include rainfall collected over disturbed areas, the water balance is incorrect. The rainfall collected from the disturbed areas will increase the amount of water that CMI will need to discharge or use for agricultural purposes. Excavation of the Mine Water Surge Area will cause dewatering of the surficial aquifer. No analysis was done of how much dewatering of the surficial aquifer will occur as a result of the excavation of the MWSA, or of the potential impacts to wetlands as a result of the dewatering activities. The District's one foot draw down presumption applies to dewatering as well as to groundwater pumping. The proposed dewatering setback from wetlands was set at 660 feet. The 660 foot setback distance is in lieu of mitigation if CMI wishes to mine within the setback distance, it will be required to implement mitigation procedures. Dewatering draw downs in the surficial aquifer as great as six and one-half to seven feet could occur on the CMI site at 660 feet from a mine cut under dry weather conditions. At 660 feet, the predicted draw down is nearly one and one-half feet using a mine pit depth of 26 feet, based on a three foot water table and a 29 foot average mine cut depth for the area expected to be mined during the term of the permit. Actual mine cut depths during the term of the permit would be as deep as thirty-seven feet which result in a draw down in the aquifer that is greater than one and on-half feet. Combining the dewatering calculations with the surficial aquifer draw downs resulting from CMI's planned well pumping from the intermediate and Floridian aquifers result in greater than predicted draw downs. CMI's water balance did not account for changes in water needs due to variability of the ore body. WATER QUALITY CMI has not demonstrated that the water quantities requested for the operation of the phosphate mine and beneficiation plant, and land reclamation and water handling will utilize the lowest water quality to the greatest extent practicable. Nevertheless, the Pine Level mine is innovative in comparison to other operating mines. It proposes to reduce its groundwater requirement by increasing the amount of recycled water used in the amine flotation process; employ an innovative sand/clay mixing technique for land reclamation, thus eliminating the need for conventional large, above-ground day settling areas or slime ponds; and use surplus water for irrigation of agricultural crops or pasture. CMI plans to mine the Pine Level Site for a period of 22 years. For phosphate mines, neither DNR, nor SWFWMD analyze impacts with respect to surface water during the mining process. For phosphate mines, no state agency looks at off-site surface water impacts from the standpoint of draw downs, with the possible exception of cities and counties. The District has not required CMI to submit an application for the management and storage of surface waters permit, since the District staff believes that phosphate mines are exempt from obtaining any MSSW permit from the District. A gap exists in the regulatory scheme for phosphate mines with respect to the reduction of surface water flows during the mining process if SWFWMD exempts phosphate mines from obtaining an MSSW permit. INTERFERENCE WITH EXISTING LEGAL USERS The City of North Port is an existing legal user of water. The City of North Port has a public water supply facility which draws its water from the Big Slough. The Big Slough normally gets a portion of its flow from high quality water in the surficial aquifer. CMI's proposed Pine Level phosphate mine is located in the watersheds which feed the Big Slough and the Peace River. In the initial years of the mine, virtually all of the collected rainfall will be diverted from the Big Slough watershed. No analysis has been done to see how dewatering might affect the City of North Port. Any significant reduction in flow to the City of North Port's facility during the low flow season will interfere with North Ports existing legal use of water. Diversion of 3.1 mgd of rainfall from the Big Slough will have an adverse impact on the City of North Port's water facility. The City of North Port is currently under a consent agreement with the Florida Department of Environmental Regulation because the water supplied by its facility violates drinking water quality standards for sulfates and total dissolved solids ("TDS") regularly during periods of low flow in the Big Slough. The MWSA, the plant area and the initial mining areas are primarily within the Big Slough drainage area. Seepage of 1.2 mgd from the MWSA will flow into the Big Slough. The only analysis done of the quality of the seepage from the MWSA was a rough analysis which showed that sulfates will likely be around 550 grams per liter. The legal standard for sulfates in drinking water is 250 grams per liter. Seepage from the MWSA will be high in total dissolved solids ("TDS") since a good portion of it was pumped from deep wells which have very high levels of TDS. No analysis was done of the potential of this seepage water to interfere with North Port's facility. Charlotte County is an existing legal user of water whose water supply is drawn from the Peace River downstream from the proposed CMI phosphate mine at Pine Level. Discharge of 5.0 mgd from the Pine Level mine could adversely affect Charlotte County's drinking water facility located on the Peace River. AGRICULTURAL USE CMI proposes to use 5.0 MGD of surplus water for irrigation of pasture grasses for cattle. CMI has not conducted any specific tests to determine the feasibility of using the discharge or the quality of the water that they plan to use for agricultural irrigation. The water for irrigation will be drawn out of the mine water surge area. The determination of whether the 5.0 mgd discharge can be used for agricultural irrigation has been postponed. The staff's position is that the proposed special conditions provide reasonable assurances that the discharge will comply with the requirements of the Basis for Review. WETLANDS Isolated wetlands occur throughout the CMI mine site. The isolated wetlands on the CMI property provide habitat for endangered and threatened species. Sandhill Cranes and Wood Storks, both threatened or endangered species, were sighted on the CMI property by wetlands experts during their site visit prior to the hearing. Small isolated wetlands on CMI property would be adversely affected by less than a one foot draw down. Wetland peat soils oxidize if exposed to the air. Oxidation results in subsidence of the wetland soils, which adversely impacts wetlands. Too much water as well as too little water can adversely impact wetlands. The combined effects of aquifer pumping and dewatering planned at the CMI site will adversely affect wetlands. No analysis was completed of the impacts to wetlands as a result of the combined effects of dewatering and pumping from the aquifer. No information regarding the normal range of wetland hydroperiods for preserved wetlands or other onsite unmined wetlands was introduced. No information was provided regarding the habitat functions provided by the wetlands on the CMI site either for threatened or endangered species or otherwise. ENVIRONMENTAL IMPACT The Applicant did not provide reasonable assurance that the water use will not cause unacceptable adverse impacts to environmental features on or off- site. The Applicant did not provide reasonable assurances that the water use will not have an adverse impact to surface water bodies such as lakes, ponds, impoundments, springs, streams, canals, estuaries or other water courses. The Applicant did not provide reasonable assurances that there will be no adverse environmental impact to wetlands, lakes, streams, estuaries, fish, and wildlife or other natural resources. The Applicant did not provide reasonable assurances that there will be no adverse impacts to the surface water system or vegetation as a result of groundwater withdrawal. The Applicant did not provide reasonable assurances that the water use will not have an adverse impact by altering or impairing the habitat of threatened or endangered species. The Applicant did not provide reasonable assurances that the projected draw downs will not result in any adverse impact to any protected or non-protected plant or animal species. The Applicant did not provide reasonable assurances that the water use will not have an adverse environmental impact to wetlands.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Governing Board of Southwest Florida Water Management District enter a Final Order DENYING the issuance of a Water Use Permit to the Applicant, CMI. DONE and ENTERED this 20th day of April, 1993, in Tallahassee, Florida. DANIEL M. KILBRIDE Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 20th day of April, 1993. APPENDIX The following constitutes my specific rulings, in accordance with section 120.59, Florida Statutes, on proposed findings of fact submitted by the parties. Proposed findings of fact submitted by Petitioner. Accepted in substance: paragraphs - 13, 14, 15, 21, 24, 31, 35, 38, 70, 71, 73, 75, 91, 97, 100, 104, 105, 114, 115, 116, 125, 126, 127, 128, and 129. Rejected as subsumed or irrelevant and immaterial: paragraphs - 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 16, 17, 19, 20, 22, 23, 25, 27, 28, 29, 30, 33, 34, 36, 37, 37A, 39 40, 43, 44, 45, 48, 49, 50, 51, 52, 53, 54, 55, 56, 57, 58, 59, 60, 61, 62, 63, 64, 65, 66, 67, 68, 72, 74, 76, 77, 78, 79, 80, 81, 82, 83, 84, 85, 86,87, 92, 93, 94, 95, 96, 98, 99, 101, 102, 103, 106A, 106, 107, 108, 109, 110, 111, 112, 113, 117, 120, 121, 122, 123, 124, 130, 131, 132, 133, and 134. Rejected as against the greater weight of the evidence: paragraphs - 18, 26, 32, 41, 42, 46 (omitted), 47 (omitted), 69, 88 (omitted), 89 (omitted), 90 (omitted), 118 (omitted), 119 (omitted), and 135 (omitted). Proposed findings of fact submitted by Petitioner, Charlotte County. Accepted in substance: paragraphs - 1, 2, 7, 18, 19, 20, 22, 25, 28, 29, 36, 40, 41, 51, 59, and 62. Rejected as argument, subsumed or irrelevant and immaterial: paragraphs - 3, 4, 5, 6, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 21, 23, 24, 26, 27, 30, 31, 32, 33, 34, 35, 37, 38, 39, 42, 45, 46, 47, 48, 49, 50, 52, 53, 54, 55, 56, 57, 58, 60, and 61. Rejected as hearsay: paragraphs - 43 and 44. Proposed findings of fact submitted by Petitioner, City of North Port. Accepted in substance: paragraphs - 1, 2, 3, 5, 6, 7, 9, 19, 20, 21, 22, 24(in part), 25, 26, 27, 28, 29, 30, 31, 32, 34, 35, 36, 37, 38, 39, 40, 41, 42, 45, 47, 48, 49(in part), 50, 51, 52, 53, 54, 56, 57(in part), 58, 59, 60, 61, 63(in part), 65, 66, 67, 68, 69, 70, 71, 72, 73, 74, 75, 78, 79, 80, 83, 84, 85, 86(in part), 87, 92, 93, 95, 96, 99, 104, 107, 108(in part), 109(in part), 112, 113, 114, 115, 116, 120, 122, 123, 126, 138, 139, 140, 141, 142, 143(in part), 144, 150, 153, 154, 155, 156, 159, 167, 168, 170, 171, 172, 173, 176, 177, 179, 180, 187, 193, 194, 195, 197, 198, 199, 200, 201, 202, 204, 205. Rejected as argument, subsumed or irrelevant and immaterial: paragraphs - 4(contained in Preliminary Statement), 8, 10, 11, 12, 13, 14, 15, 16, 17, 18, 23, 24(in part), 33, 43, 44, 46, 49(in part), 55, 57(in part), 62, 63(in part), 64, 76, 77, 81, 82, 86(in part), 88, 89, 90, 91, 94, 97, 98, 100, 101, 102, 103, 105, 106, 108(in part), 109 (in part), 110, 111, 117, 118, 119, 121, 124, 125, 127, 128, 129, 130, 131, 132, 133, 134, 135, 136, 137, 143(in part), 145, 146, 147, 148, 149, 151, 152, 157, 158, 160, 161, 162, 163, 164, 165, 166, 169, 174, 175, 178, 181, 182, 183, 184, 185, 186, 188, 189, 190, 191, 192, 196, 203, 206, 207, 208, 209, 210, 211, 212, 213, 214, 215, 216, 217. Proposed findings of fact submitted by Respondent/Petitioner Consolidated Minerals, Inc. and Southwest Florida Water Management District. Accepted in Substance: paragraphs - 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 14, 17, 18, 19, 20, 21, 22(in part), 23, 24, 25(in part), 26, 27(in part), 28, 29(in part), 32, 33(in part), 39, 40, 41, 42, 43, 44, 45, 46, 47, 49, 50, 52(in part), 53, 54, 55, 56, 57(in part), 58, 62, 71, 82, 85, 87, 88, 91, 92(in part), 93, 94(in part), 95(in part), 96(in part), 97(in part), 100(in part), 101, 115, 119, 120, 123, 124(in part), 125(in part), 126(in part), 127(in part), 130(in part), 133(in part), 137, 138(in part), 139, 145. Rejected as argument, subsumed, or irrelevant and immaterial: paragraphs - 12, 13, 15, 16, 31, 36, 37, 38, 48, 51, 52(in part), 57(in part), 59, 60, 63, 80, 81, 83, 84, 86, 90, 94(in part), 105, 106, 107, 108, 109, 110, 111, 112, 113, 114, 116, 117, 118, 124(in part), 126(in part), 127(in part), 130(in part), 134, 135, 136, 138(in part), 140, 141, 142, 143. Rejected as against the greater weight of evidence: paragrahs - 22(in part), 25(in part), 27(in part), 29(in part), 30, 33(in part), 34, 35, 61, 64, 65, 66, 67, 68, 69, 70, 72, 73, 74, 75, 76, 77, 78, 79, 89, 92(in part), 95(in part), 96(in part), 97(in part), 98, 99, 100(in part), 102, 103, 121, 122, 125(in part), 128, 129, 131, 132, 133(in part), 144. Proposed findings of fact submitted by Petitoner, Environmental Confederation of Southwest Florida, Inc. Accepted in substance: paragraphs - 1, 2, 3, 4 6, 7, 17, 22, 26, 27, 28, 29, 30, 33(in part), 34, 35, 39(in part) 41, 42, 43, 45, 48, 53, 56, 57, 59, 60, 61, 62, 71, 73, 80, 81, 82, 85, 86, 87, 92(in part), 106, 107, 110, 112, 113, 114, 115, 116, 117, 121, 122, 123, 124, 125, 126, 127, 128, 129, 130, 131, 132, 133, 134, 135, 136, 137, 138, 139(in part), 140, 141, 142, 143, 144, 145, 148, 149, 150, 151, 152, 154, 155, 157, 158, 162, 163, 164, 165. Rejected as argument, subsumed, or irrelevant and immaterial: paragraphs - 5, 8, 9, 10, 11, 12, 13, 14, 15, 16, 18, 19, 20, 21, 23, 24, 25, 31, 32 33(in part), 36, 37, 38, 39(in part), 46, 47, 49, 50, 51, 52, 55, 58, 63, 64, 65, 66, 67, 68, 70, 72, 74, 75, 76, 77, 78, 79, 83, 84, 88, 89, 90, 91, 92(in part), 93, 94, 95, 96, 97, 98, 99, 100, 101, 102, 103, 104, 105, 108, 109, 111, 118, 119, 120, 146, 147, 153, 156, 159, 160, 161, 166, 167, 168. Rejected as against the greater weight of evidence: paragraphs - 44, 54, 69, 139(in part). COPIES FURNISHED: Rory C. Ryan, Esquire Roger W. Sims, Esquire HOLLAND & KNIGHT Suite 2600 200 S. Orange Avenue P. O. Box 1526 Orlando, Florida 32802 Vivian Arenas, Esquire Assistant General Counsel Southwest Florida Water Management District 2379 Broad St. Brooksville, Florida 34609 Mr. Alan R. Behrens Route 2, Box 725-A-32 Arcadia, Florida 33821 Matthew G. Minter, Esquire County Attorney 18500 Murdock Cr. Port Charlotte, Florida 33948-1094 David M. Levin, Esquire ICARD, MERRILL, CULLIS, TIMM, FUREN & GINSBURG PO Box 4195 Sarasota, Florida 34237 Kenneth B. Wright, Esquire Sierra Club Legal Defense Fund PO Box 1329 Tallahassee, Florida 32302 Peter G. Hubbell Executive Director 2379 Broad Street Brooksville, Florida 34609-6899
The Issue The issues presented in this matter concern the request by the Petitioner to be granted a management and storage of surface waters permit by Respondent. Respondent proposes to deny the permit based upon the perception that the activities contemplated by Petitioner: (1) are not consistent with the public interest as envisioned by Section 373.016, Florida Statutes, and 40C- 4.301(1)(b), Florida Administrative Code, (2) are not a reasonable and beneficial activity, per Section 40C-4.301(1)(a), Florida Administrative Code, alter the peak discharge rate of runoff from the proposed activity or the downstream peak stage or duration for the 1 in 10 year design storm, per Section 40C-4.301(3)(a), Florida Administrative Code, (4) cause an increase in velocity or flood stage on lands other than those owned, leased, or otherwise controlled by the applicant for the design storm, per Section 40C-4.301(3)(b), Florida Administrative Code, (5) cause an increase in flow or stage such that it would adversely affect lands other than those owned, leased, or otherwise controlled by the applicant, per Section 40C-4.301(3)(c), Florida Administrative Code. 1/
Findings Of Fact A predecessor applicant had requested permission to construct and operate the water management system which is the subject of this controversy. The approximate acreage involved was 197 acres in Lake County, Florida. This acreage and requested activity was subject to the regulatory requirements of St. Johns River Water Management District. Clay Island Farms, Inc., hereinafter referred to as CIF, was substituted for the initial applicant and this matter has been litigated before the Division of Administrative Hearings on the continuing application of the Petitioner. The permit application number is 4- 8089. This application was considered with application number 4-8088, pertaining to property owned by A. Duda and Sons, Inc. Subsequently, the latter application shall be referred to as the Duda request for permit. Certain additional information was sought by Respondent from the applicants, CIF and Duda, in the permit review, by correspondence dated October 2, 1981. A copy of that correspondence may be found as Petitioner's Exhibit No. 16 admitted into evidence. In particular, CIF was requested to prepare pre and post-development runoff rates in the 1 in 10, 1 in 25,and 1 in 100-year storms, to include stage-storage and stage-discharge rates for any and all retention facilities within the project design. Petitioner's Composite Exhibit No. 1 admitted into evidence contains a copy of the engineering report by CIF which are CIF's responses to the request for information. The date of the engineering report is July 12, 1982. The CIF application, as originally envisioned, called for the construction of exterior and interior ditches to be placed around a dike of 71 feet MSL elevation. The dike would enclose a proposed farm operation of approximately 197 acres, should the permit be granted. Within that 197 acre plot, would be found numerous drainage ditches to include major ditches and minor arterial ditches. The purpose of those ditches found in the 197 acres would be to serve as a conveyance for rainfall runoff. The system of conveyance would be connected to an existing conveyance system already in place and related to farm operations of A. Duda and Sons. The runoff would be eventually placed in a retention pond and at times discharged from that retention pond or basin into Lake Apopka by means of gravity flow. The particulars of the development of the 197 acre plot and its service dike, canals, and ditches are more completely described in Petitioner's Exhibit No. 1, which is the engineering report for the surface water management permit application. The CIF application was reviewed by the staff of the Respondent. Recommendation was made to deny the permit. Details of that denial may be found in Respondent's Exhibit No. 1. In the face of the denial, CIF requested an administrative hearing. This request was made on August 27, 1982, by petition for formal Subsection 120.57(1), Florida Statutes, hearing to determine Petitioner's entitlement to the requested permit. St. Johns River Water Management District, in the person of its governing board, determined to refer this matter to the Division of Administrative Hearings to conduct the formal proceeding and the request for the assignment of a hearing officer was received by the Division on September 13, 1982, leading to the final hearing in this cause. During the course of the final hearing, the CIF permit application was modified in a fashion which reduced the amount of acreage sought for cultivation. Now, approximately 122 acres would be farmed per the amended proposal. A general depiction of the design of the project in its amended form may be found in the engineer's sheet, which is Petitioner's Exhibit No. 20 admitted into evidence. When contrasted with the engineering drawings set out in Petitioner's Composite Exhibit No. 1, the new design is essentially the same as contemplated in the original permit application, on a lesser scale. Other than dimensions, the basic concepts of the CIF operation would remain the same under the amended proposal. At present, Petitioner proposes to remove the vegetation which covers the subject 122 acre plot and to conduct a muck farming operation. That vegetation is mostly mixed hardwood with the primary species being red maple. The soil in this area is constituted of monteverde muck, which is conducive to the production of corn and carrots, the crops which Petitioner would plant, to prepare the land for the operation, the system of ditches dikes and canals described would be installed following the cleaning, draining, and leveling of the 122 acres. Petitioner's Exhibit No. 10 admitted into evidence depicts land which has been cultivated and the subject 122 acres in its undisturbed state. Petitioner's Exhibit No. 4 admitted into evidence shows the overall CIF area is outlined in red, except for its southerly extent, which carries a red and yellow line on the exhibit. This exhibit depicts Wolfshead Lake which is a small interior lake in the southeastern corner of the overall CIF property. The yellow line in the middle of the CIF property represents, the location of a former north-south canal. The westernmost north-south reach, which is shown with a red line, depicts a canal which runs north from Wolfshead Lake into the existing Duda system of canals and ditches. The Duda operation has attempted to plug that north-south canal on the western fringe to stop the flow from the area of Wolfshead Lake, but has been unsuccessful and the water still enters the Duda farm ditches and canals. In the 1940's and early 1950's, the CIF property had been partially developed for a cattle operation and truck farming. Those canals, as described before, were installed, together with the diagonal yellow line on Petitioner's Exhibit 4, which represents a canal that was built with an axis running northeast and southwest. In addition, there was a centrally placed east-west canal and a slough running from Wolfshead Lake in a southeasterly direction. The slough is still there, although water that might be diverted from the Wolfshead Lake area into the slough is flowing north in the westerly north-south canal at present. If the project were allowed, most of the water flowing in and around the Wolfshead Lake would be introduced into the slough and from there exit to Lake Apopka. The center north-south canal and the interior east-west canal, together with the diagonal canal, are not in operation at present. The center north-south-canal would become the approximate eastern boundary of the 122 acres with the western north-south canal representing the approximate western boundary of the 122 acre plot. The northern boundary of the CIF property is constituted of an east-west canal which is part of the present Duda system. This is the only one of the canals associated with the former farming operation on the CIF property which is part of any maintained system of conveyances presently in existence. Approximately 1,000 acres are being farmed by Duda and Sons in property north of the proposed project. The Duda permit application, 4-8088 as granted, is described in Petitioner's Exhibit No. 13 which is a copy of the permit. This acreage is generally found to the northwest of the CIF plot, and would allow an additional 300 acres to be farmed in that muck area, on land which has been cleared for the most part and/or which has an elevation predominantly above 68.5 feet MSL. Eighty acres of the proposed Duda permit application was denied based upon the fact that it had not been cleared prior to the Duda permit application and in consideration of the amount of the 80 acre segment which lies below 68.5 feet MSL. The elevation 68.5 feet MSL represents the flood plain for the 1 in 10 year rainfall event for Lake Apopka. The area of the Duda permit is depicted on Petitioner's Exhibit No. 4 and outlined on that exhibit with lines of green and yellow at the southern end, green and yellow and red and yellow on its western flanks, red at the north end and by red on the east side, together with a Duda drainage ditch, which runs north from the terminus of the north-south drainage ditch coming from Wolfshead Lake and the east-west drainage ditch at the northern extent of the CIF property. Exhibit No. 4 was made prior to clearing operations depicted in Petitioner's Exhibit No. 10 and that letter exhibit is a more correct indication of the appearance of the new Duda permit property today. A green diagonal line running northwest and southeast intersecting with a line running east-west and a line running north-south depicts the approximate part of the 80 acres, which lies below 68.5 feet MSL, as shown in Petitioner's Exhibit No. 4. Farm operations, in keeping with the authority of Permit No. 4-8088, have not commenced. If the CIF permit application is successful, the original 1,000 acres, approximately 300 acre area of the Duda permit and the 122 acres of CIF, would be tied in by a system of conveyance ditches or canals allowing the interchange and transport of water through and around the three farm areas. The existing retention pond would be expanded to accommodate the additional farm acreage. The Petitioner is willing to increase the present retention pond to a design capacity which would equal one acre of basin for each ten acres of farm land, at the place in time when all three elements of the muck farm operation were under way. This again pertains to the existing 1,000 acres, the approximately 300 acre recent Duda permit, and the 122 acres related to the CIF application. With the addition of the CIF acreage, when water in the ditches reached 67.1 feet MSL, this would cause the engagement of a 40,000 GPM pump allowing the ditch water influent into the retention pond. The pump automatically would shut off at any time the water level in the access ditches to the pond dropped below 61 feet MSL. The primary purpose of the retention pond is to make water available for irrigation of crops, in its present state, and as contemplated with the addition of the CIF project. The pond does and would detain farm water for a period of about a day allowing the settling out of certain nutrients which are in particulate form. The existing pond and in its expanded form does not and would not filter nutrients which have been dissolved and have become a part of the water column. At times of high incidence of rainfall, when the crops are inundated with water for a 48-hour period of time, the retention pond is now designed and as contemplated by the addition of the CIF farm land, would allow for the discharge of effluent into Lake Apopka through two discharge culverts. The discharge is by means of gravity through an adjustable riser system. The retention pond as presently designed and as contemplated in its expansion has established the height at which water would be released from the retention pond into Lake Apopka through the riser at 68 feet MSL. The occasion of high incidence of rainfall occurs during the normal rainy season in a given year. Discharge could also be expected in the 1 in 10 year, 24hour storm event. During that storm event or design, Lake Apopka would rise to a level of 68.54 feet MSL, a level which would correspond to the 10year flood plain. Whether in the pre or post-development phase of the 122 acres, waters from that acreage would be discharged during the course of the storm through culverts leading from the retention pond into Lake Apopka. This process would continue until the gravity flow stopped at the moment where the water level in the pond and the water level in Lake Apopka adjacent to the discharge culverts achieved equilibrium of elevation. At that point in time, the gravity flow or discharge from the retention basin would cease, there no longer being a positive gradient from the detention pond to Lake Apopka. There will be some amount of discharge in the 24-hour storm event through the culverts at the retention pond either in the pre or post-development phases of the project, because, at present, the western most north-south ditch, which is found at the western boundary of the CIF property, allows water to flow north into the present Duda ditch system, water which has fallen on the 122 acres in question. From the ditch system, that water finds its way into the retention pond and thus into the lake. The contemplated system to be installed with the 122 acres at build-out would also allow water from the 122 acres to go through a system of conveyances and to the retention pond and from there into Lake Apopka. Although considerable testimony was presented by both parties on the subject of comparing pre-development and post-development peak discharge rates of runoff from the proposed activity, in the 1 in 10 year, 24-hour storm design or event, neither party has satisfactorily proven the dimensions of the pre-development and post-development peak discharge rates of runoff from the proposed activity. This determination is made having reviewed the testimony and the exhibits in support of that testimony. Notwithstanding a lack of proof of this differential with exactitude, it has been shown by the testimony and exhibits that the post- development peak discharge rate of runoff in the 1 in 10 year, 24-hour design storm or event can be expected to exceed that of the pre-development rate. On the associated topic of the ability of the post-development design to accommodate the differential in peak discharge rate of runoff between pre- development and post-development, Petitioner has failed to establish this proof. The modeling that was done by the Petitioner, in an effort to depict the differential as 10 acre feet with an available capacity of attenuation approximating 26 acre feet within the system of ditches, is not convincing. Nor has petitioner shown that there is sufficient storage in the retention pond, in the course of the storm event. The data offered in support of Petitioner's position does not sufficiently address accommodation of the drainage from areas surrounding the 122 acres in question, which are not part of the Duda system; the amounts of water already found in the system of ditches and canals at the onset of the storm event; the amount of water located on the crops at the onset of the storm event, which would have to be removed; and the amount of water already found in the retention pond at the time of the storm event. During the 1 in 10 year 24-hour storm, the CIF 122 acres will be protected by the 71-foot MSL dike, in that the expected elevation of Lake Apopka would not exceed 68.54 feet MSL. The dike would also protect the 122 acres in the 25, 50, and 100-year, 24-hour storm events whose elevations are anticipated to be 68.98, 69.28, and 69.56 feet MSL, respectively. As a consequence, an increase in flood stage would occur on lands other than those controlled by CIF. The amount of increase in flood stage would be approximately .046 inches during the 1 in 10 year storm, and an increasingly greater amount for the larger storms. It was not established where the amount of water which could not be staged on the 122 acres would be brought to bear through the surface flow on the 31,000 acres of water which constitute Lake Apopka. Nonetheless, that water could be expected to increase the flood stage on lands other than those of the Applicant. Possibly the dikes protecting the muck farms on the northern side of Lake Apopka could be influenced by the .046 inches in elevation due to the forces associated with the 1 in 10 year storm event, such as winds and movement of the water in the lake. This is true, notwithstanding the fact that the design goal of the dikes in the area is 71 feet MSL. The dikes are constituted of muck and are susceptible to overtopping, erosion, or blowout. By history, there have bean dike failures in the northern end of Lake Apopka, and associated increases in stage or flood stage. This incremental increase in water level in the 1 in 10 year storm event, due to the CIF development, when considered in the context with the other influences of that storm event, could possibly be the determining incident leading to dike failure in the northern perimeter of Lake Apopka. However, given the history of dike failures, prior to this potential loss of the storage area on the applicant's property, it has not been shown that the proximate cause of dike failure in the 1 in 10 year storm could be expected to be the contribution of an additional .046 inches of water on the lake surface. Those failures existed prior to the potential for the addition of water and were the result of inadequate maintenance of a structure which demanded a better quality of attention. Nonetheless, the additional amount of water could be expected to exacerbate the extent of a dike breach in any 1 in 10 year storm event that occurred subsequent to the development of the CIF 122 acres. In summary, the likelihood that the increase in elevation of water caused by the loss of storage on the subject property will be the critical event that causes a dike failure is not accepted. A dike could breach because of the influence of the storm even itself, without regard for the incremental increases in water elevation due to loss of water storage on the CIF property. The poor condition of some dikes due to less than adequate design or maintenance, would promote that dike failure and be exacerbated to the extent of more water being introduced on that property through the incremental amount of increase due to loss of storage on the CIF property. The dike failure circumstance in and of itself would not be sufficient to deny the permit application; however, the applicant had the burden of addressing the possible problem of increases in stage or flood stage on other properties, not its own, which are not protected by dikes. This showing was not made by the applicant, notwithstanding the fact that an increase in stage or flood stage could be expected to occur on property fronting Lake Apopka, which property is not protected by any form of artificial barrier. The installation of the protective dike aground the 122 areas of the CIF property in the 1 in 10 year design storm and potentially at times of lesser rainfall events, could be expected to increase the stage or flood stage on lands unprotected by dikes and thereby adversely affect lands other than those controlled by the applicant. Most of the 122 acres and the property to the east of that development and a portion of the undeveloped 80 acres in the recent Duda permit would be inundated in the 1 in 10 year storm event, prior to development. This is true because the elevation of much of that property is approximately 67.5 foot MSL. During the 1 in 10 year storm event, it would store approximately one foot of water, as presently constituted. It could also be expected to be inundated on an average of approximately once in two years. Lake Apopka is a part of a controlled system of lakes known as the Oklawaha River chain of lakes. Respondent regulates the water level in that chain of lakes by operation of a lock on the Apopka-Beauclair canal. The maximum desirable elevation of 67.5 feet MSL for Lake Apopka is a part of the regulation schedule found in Respondent's Exhibit No. 2 admitted into evidence. In the 1 in 10 year or better storm event, the Apopka-Beauclair system could not draw down the surface water at a rate faster than 27 days per foot, even assuming the lock was fully open to flow. Consequently, those properties that were suffering an, increase in flood stage on their surface could not expect to gain prompt relief through the regulation of waters in the Oklawaha River chain of lakes. Lake Apopka is an hyper-eutrophic lake. Although it is classified as Class III water body (ambient water quality) within the meaning of Section 17- 3.161, Florida Administrative Code, it fails to match that classification in terms of its actual water quality. This is as a consequence of its highly eutrophic state, brought about by the age of the lake and the contributions of man. Some of the contributors to the eutrophication have been removed from the lake area and water quality has improved. Those facilities removed were sewage treatment and citrus processing plants around the Lake Apopka rim. The muck farms remain and the quality of the water in the retention basins or ponds when compared to the receiving waters of Lake Apopka is similar in nature. Consequently, the receiving waters are not enhanced in their water quality when the retention ponds discharge water into Lake Apopka. As stated before, the retention ponds do not have as their primary purpose the treatment of water. Any water quality improvement is a secondary function of the retention pond. The retention ponds do improve the water somewhat, as described, and are adequately sized to fulfill that partial cleansing. Whether the water quality in Lake Apopka would ever improve sufficiently to allow Lake Apopka to become a more diversified habitat for fish and wildlife is not certain, even if all contributing discharges of pollutants were curtailed, to include the discharge of water from the muck farms with its high nutrient loads. Nonetheless, Lake Apopka cannot accomplish the recovery if the effluent from the muck farms continues to be introduced into the lake with the present constituents found in the water. Out of concern for the water quality in Lake Apopka, officials of the University of Florida have conducted experiments on nutrient removal which they hoped would approximate the quality of removal accomplished by transitional vegetation and swamp. (The 122 acres at issue and the western and eastern adjoining property are constituted of these water treatment zones.) This experiment of nutrient removal through use of retention ponds calls for the retention of the muck farm water for a period of six days allowing settlement of particulates and for the vegetation within those experimental retention basins to uptake dissolved nutrients. Several types of vegetation are used to gain a better quality of nutrient uptake add the vegetation is harvested every six to eight weeks to improve that performance. The experiment has shown that the quality of water discharged from the ponds utilized by the University of Florida was comparable in its quality to the natural wetlands system water discharge. The natural wetlands discharge is of a better quality than the receiving waters. Unlike the university experiment, the pond contemplated by CIF primarily emphasizes detention for a shorter period of time than was used in the experiment and allows highly eutrophic water to be mixed with that quality of water already found in Lake Apopka. The only exception to that comment is that water flowing from Wolfshead Lake, which is south of the proposed 122 acres, is a high quality of water, and through the project as contemplated, this water would be directly introduced into Lake Apopka through a flow over a natural wetlands system. This is in opposition to the present situation where the water from Wolfshead Lake flows primarily to the north through an existing canal and is mixed with water from the muck farm and is, therefore, of the eutrophic character as opposed to the high quality character. The Duda permit, which was issued, would allow the introduction of water which is similar in character to the water of Lake Apopka, through the system of ditch conveyances, placement in the retention pond, and at times, flow to the lake. In its effect, the nutrient loading which occurs by introduction of waters from that new farm, would be similar to that proposed in the CIF project. The fact of this similarity does not prohibit the district from evaluating water quality matters on the occasion of the CIF permit decision. Should the 122 acres be converted from natural vegetation to a muck farm, wildlife and fish habitat would be adversely impacted. The habitat provided by the plot is in scarce supply and is essential to the maintenance of a diversified fish population. The hardwood swamp, which is part of and adjacent to the 122 acres of the CIF application, supports benthic invertebrates, which are a food source for game fish. The type of vegetation found in the lake, due to its eutrophic state, is plankton and one of the by- products of the reproduction of that plant through the process and respiration is the destruction of the fish population. This occurs in the summer months. The plankton has replaced the emergent and submergent vegetation which once covered as much as two-thirds of Lake Apopka and now represents .05 percent of the lake. As a consequence, game fish have diminished over a period of years with plankton feeding fish predominating. Consequently, the fish population is less diverse and the removal of the vegetation becomes a significant contributor to the imbalance in fish population.
