Findings Of Fact The applicant proposes, on the west shore of the Indian River to: (1) Dredge an access channel 3' deep, 801 wide, and 1,500' long, Construct a vertical seawall of 600 linear feet along the waterward side of the proposed fill area, and Disposit some 4,000 cubic yards of spoil in a 200' x 400' area enclosed by the seawall. This proposed seawall will be in line with and connect to an existing seawall along the adjacent north property. A hydraulic dredge and a silt screen will be used during dredging operation. Petitioner acquired the submerged lands fronting his property on the west bank of the Indian River at Melbourne, Florida to the bulkhead line, by purchase from the Trustees of the Internal Improvement Trust Fund (IITF) in 1963 and 1964. The submerged land just north of Petitioner's property was likewise acquired from the Trustees, bulkheaded and filled, circa 1963 where a commercial marina is now operated by one Rathman. Indian River in the vicinity of Melbourne has become in the nature of a basin by reason of the Eau Gallie Causeway to the north and the Melbourne Causeway to the south. These causeways have materially reduced the flushing of this stretch of the Indian River and increased the turbidity of the water. Normal turbidity of the Indian River in the vicinity of the lands here involved is such that the bottom cannot be seen at depths greater than 1.5 to 2 feet. Surface drainage from U.S. 1, which runs just west of Shablowski`s property, and an area of some 5 square miles just west of U.S. 1 runs into the Indian River through culverts just north and south of Petitioner's property. No evidence was submitted that this surface runoff goes through debris or settling traps before being discharged into the Indian River. Rathman's marina and the area there filled is bounded on the south by a bulkhead normal to the shoreline of Indian River and extending into the river some 200 feet. This creates a pocket where some debris accumulates on the north end of Petitioner's property. Granting the applied for permit would result in moving this pocket 400 feet to the south. Although the Indian River, between the causeways above noted, is in an ecologically stressed condition due primarily to the effects of the causeways and the surface water drainage into Indian River, it is not dead. Cuban Shoalweed grows in the shallow water areas of the Indian River (less than 3 feet deep) and provides a source of food to the marine life in the area. The submerged lands owned by Petitioner are sparsely covered (10 percent to 25 percent) with patches of Cuban Shoalweed. The area proposed for filling has an average depth of approximately 1.5 feet with some areas near the eastern edge of the property having depths of up to 3.5 feet. However, these are primarily holes or former channels. A significant amount of animal life exists on the property in question. These consist of blue crabs and numerous small fishes such as silversides, mojarra, needlefish, mullet, sheepshead, leather jack and snook. Benthic samples collected include polychaetes, amphipods, sphaeromid isopods, cumaceans, small shrimp, gem clams, paper mussels, gobies and pipe fish. Petitioner's proposal to dredge an access channel 3 feet deep, 80 feet wide, and 1500 feet long from the eastern edge of the property riverward will not have a significant adverse impact on marine biological resources or water quality. (Exhibit 3). Silt screens will be used in connection with the hydraulic dredging and the shallow depths to which Petitioner proposes to dredge will not cause permanent damage to the bottom grasses, if any, in the dredged area. The vertical bulkhead proposed by Petitioner would increase the possibility of scouring in the areas; however Petitioner agreed at the hearing to install rip rap along this bulkhead. This will eliminate scouring and promote the propagation of marine life. Granting the application will result in the loss of approximately 2 acres of moderately productive bottom land in the Indian River, or approximately 0.1 percent of the total area of the Indian River in the basin between the two causeways. Respondent generally acknowledges that filling of the area in question will not have a significant effect upon the ecology of the area; however, if others also fill productive bottom lands the cumulative effect could be significant. Petitioner has not determined the use to which the property will be put if the application is granted. At such time as construction is instituted DER can establish requirements for surface water runoff containment to protect the receiving waters.
The Issue The issue for consideration at the hearing was whether the Respondent, Roger Harloff, should be issued a consumptive use permit to withdraw and use ground water from the wells on his property, and if so, in what amount and under what conditions.
Findings Of Fact Respondent, Roger Harloff, owns several farms in southeastern Manatee County, Florida which, taken together, make up an irregular 8,500 acre tract located approximately 2 1/2 miles north of the City of Sarasota's Verna Wellfield. Mr. Harloff grows vegetables on much of this tract, of which approximately 1,500 acres is devoted to tomatoes. This tomato crop is the prime crop produced by Mr. Harloff, and provides the raw material for the Harloff packing plant which is dependent upon the tomato crop in order to stay in business. Mr. Harloff also operates a plant nursery at which he produces many if not most of the seedling plants utilized in his vegetable growing operations. In order to be economically feasible and remain operative, Mr. Harloff must farm approximately 3,800 acres during the Spring growing season and approximately 3,000 acres during the Fall. These acres are made up of tomatoes and other vegetables. The packing plant and the plant nursery are dependent upon the farm operation and without adequate water, the farm operation cannot be successfully carried on. In September 1988, Mr. Harloff applied to the District for a consumptive use permit to withdraw water from twelve wells located on his property, requesting an annual average rate of 12,995,606 gpd, and a maximum daily rate of 47,520,000 gpd. The consumptive use permit application filed by Mr. Harloff was assigned District Number 204467.04. After evaluation of the application in conjunction with its needs and policies, the District issued a staff report and proposed agency action on the application which recommended issuance of the permit authorizing water to be drawn from the 12 wells at a rate approximating that requested in the application. Thereafter, the City of Sarasota, which operates the nearby Verna Wellfield, considering that the proposed withdrawal would have a substantial adverse impact on its wellfield operations, filed a Petition for Formal Administrative Hearing objecting to the issuance of the permit to Mr. Harloff. Though Mr. Harloff has owned much of the property which make up the 8,500 acre tract in question here, at the time of his application, he did not own, but had under contract, a substantial portion. He closed on the purchase of that remainder after he received notice of the District's intention to issue the permit in question but prior to the City's filing its Petition For Formal Hearing. The purchase price of the property in question was $9,000,000.00 which carries an interest payment on the financed portion of $52,000.00 per month. The wells pertinent to the issues in this proceeding are as follows: # Cons. Depth Cas. Lin. Diam. Cap. Loc. 1 1978 1185' 200' 220-490' 12" 2000 gpm SE 2. 1988 1320' 210' 210-480' 16" 3000 gpm SE 9. 1974 1130' 390' 16" 3000 gpm C 10. 1976 1232' 231' 283-400' 16" 3000 gpm NW 11. 1979 1120' 210' 260-480' 12" 2000 gpm NW 12. 1976 1180' 480' 12" 2000 gpm SW 3. 1989 1434' 460' 16" 3000 gpm SE 5. 1989 1374' 610' 16" 3000 gpm W 8. 1989 1292' 548' 16" 3000 gpm NW 13. 1989 1310' 635' 16" 2000 gpm NE Well No. 8 was used as the pump test well for the constant rate discharge test and Well No. 13 was the deep observation well for that test. Wells 1, 2, 9, 10, 11, and 12 have all been previously permitted by the District and No's 1, 2, 9 and 10 are currently permitted under two other permits, while 11 and 12 were permitted under a different permit. Wells No. 3, 5, 8 and 13 have been authorized for construction but not, as yet, to produce water. Wells 4, 6 and 7 have not yet been constructed. The intention is to drill them to a depth of 1,300 feet and case them to 600 feet. Each will have a pump capacity of 3,000 gpm. Number 4 will be in the southeast portion of the tract, number 6 in the central portion, and number 7 will be located just north of number 6. Wells 1, 2, 9, and 10 currently have a combined permitted maximum daily rate of 13,680,000 gallons under permits number 204467.03 for 1 and 2, and 204630 for 9 and 10. The former was issued on December 29, 1987 and will expire on December 29, 1993, and the latter, issued on October 7, 1981, will expire on that same day in 1991. The permit previously issued for wells 11 and 12 authorized withdrawal at a maximum daily rate of 2,160,000 gallons. That permit, number 204374, expired on September 9, 1986 and was not renewed. After the City filed its Petition challenging Mr. Harloff's proposed permit, Mr. Harloff, on June 26, 1989, filed an amended application to withdraw water at an average annual rate of 10.99 mgd and a maximum daily rate of 48.96 million gallons. This amended application refers to an additional proposed well, Number 13. The District, however, had previously approved wells 3 - 8 and 13, and pursuant to this authorization, wells 3, 5, 8, and 13 were built. Mr. Harloff submitted additional amendments to his application on August 7 and 9, 1989. The former requests a seasonal average daily rate of 25.34 mgd and a seasonal maximum daily rate of 32.79 mgd. The latter requests a seasonal average rate of 26.18 mgd, an annual average rate of 15.18 mgd, and a seasonal maximum rate of 31.56 mgd. In that regard, a seasonal rate is the same as an annual rate, (average or maximum) when applied to a growing season as opposed to a year. The additional amendments to the application were evaluated by District staff who, on August 18, 1989, issued a revised staff report and a proposal to issue to Mr. Harloff a consumptive use permit authorizing an average annual withdrawal of 11.1. mgd, an average seasonal withdrawal of 15.6 mgd, and a seasonal maximum withdrawal of 20.1 mgd. The proposed permit also contains terms and conditions which, the District contends, will, inter alia, permit Mr. Harloff to withdraw more water than he is currently authorized without additional adverse impact on the City's Verna Wellfield. It is to some of these terms and conditions that Mr. Harloff objects. Since the issuance of the revised staff report and intent to issue, the parties have negotiated on the various terms and conditions in question and have agreed to some and the amendment of others. Mr. Harloff has no objection to conditions number 1, 2, 3, 7 - 14, 23, 24, 26, 28 - 30, 32, and 34 & 35. The parties agree that other conditions, as indicated herein, should be amended as follows: Condition 19, on the third line, should be changed to read, " up to 20 inches tapering to 12 inches." Condition 22, on the second line, should be changed from "30 days" to "10 days". Condition 25, on the first line, should be changed from "within 60 days" to within 120 days". Condition 31, on the third line, starting with "following month" should be changed to "following months: January, April, July and October". Also, under Sampling Frequency, "Monthly" should be changed to "Quarterly". Condition 33, on the ninth line, insert the work "economically" before the word "feasible" in the phrase "specific operation and irrigation improvements are feasible". Mr. Harloff objects to conditions 4, 5, 15 - 17, 20 & 27. He does not object to the proposed new standards for new wells. Taken together, the parties then disagree only on the requirement for abandonment or refurbishment of existing wells and the quantities of water Mr. Harloff will be allowed to draw. The City supports the District's position on both issues. The City of Sarasota owns and operates a public water system to serve between 50 to 75 thousand people located in Sarasota County. The primary source of water for this system is the Verna Well field which is also owned by the City and which accounts for approximately 60 percent of the City's water needs. The City also operates a reverse osmosis, (R.O.) water desalinization facility, and has back-up wells at St. Armond Key and at the Bobby Jones Wellfield. The Verna Wellfield is located about 17 miles east of the Sarasota city limits on approximately 2,000 acres of land in northeastern Sarasota County. It consists of two tracts of land: Part "A", which is approximately 1/2 mile wide by 4 miles long; and Part "B", which is approximately 1 mile square located about 500 feet southeast of Part "A". The Verna Wellfield's permitted allocation is based on whether the R.O. facility is producing at capacity. If it is, the Verna daily allocation is 7 mgd, and if not, 9.5 mgd. The R.O. facility's capacity is 4.5 mgd and the backup wells have a capacity of 1.7 mgd. The wellfield contains 39 permitted production wells, 30 of which are in Part "A" and 9 of which are in Part "B." One of them, well 30, is currently inactive. The wellfield has been in operation as a part of the City's public water system since September 1966. When the Verna Wellfield was constructed in 1965-1966, its original design specified casing on most wells down to 140 feet with pump bowl settings at 125 feet. Each pump was to have a total dynamic head, (TDH) of 200 feet. Over the years, the City has decreased the TDH of the pumps at Verna from 200 feet to 175 feet. This has resulted in a reduction of the pumps' ability to produce water with sufficient pressure to carry it to the discharge point. This decline has been caused by an increase in withdrawal of water regionally, and not solely because of withdrawals from the Verna Well field. Verna is impacted by the use of water outside the boundaries of the wellfield. The City has an ongoing program calling for the refurbishment of 2 to 3 wells per year at the Verna Wellfield. It is the City's intent to convert the pumps to 200 feet TDH on all well refurbishments in the future. In August 1977, a program requiring permits for the consumptive use of water was implemented in both Sarasota and Manatee Counties. At that time, the Verna Wellfield had a production rate of 6.9 mgd annual average daily rate. On January 6, 1978, the City applied for a permit for Verna and on April 3, 1979, the District issued permit number 27804318 to allow the City to draw water from the Verna Wellfield. The City applied for a renewal of that permit in October 1983 and thereafter, in January 1985, the District authorized the continued withdrawal of water from Verna by the issuance of permit 204318 which, at Condition 18, placed limitations on the City's use of water from the wellfield. Specifically, the permit limited withdrawals from Verna to: ...6,000,000 gallons per day average and 7,000,000 gallons per day maximum, except during those times when ... [the R.O. process is reduced or to facilitate maintenance or repairs]. At such times, ... [withdrawals) may be increased to provide additional supplies not to exceed 8,000,000 gallons per day average annual and 9,500,000 gallons per day maximum. This condition clearly provides for additional supplies to be drawn to increase the Verna Well field production to a total of 8,000,000 and 9,500,000 mgd, respectively, not in addition to the regular permitted amount, by those quantities. The City's permit has been neither suspended nor revoked nor is any violation enforcement action currently under way. The current permit expires January 9, 1991. The water pumped from the Verna wells is held in a 1,000,000 gallon reservoir at the wellfield. This reservoir, which is topped at approximately 22 to 23 feet, electronically controls the pumping activity at the well field by turning on and shutting off pumps, in series, as the water level in the reservoir rises and falls. The water, when needed, is transmitted to another reservoir near the City's treatment plant in downtown Sarasota by gravity flow through a 30" diameter, 92,000 foot long pipe. The flow rate is approximately 5,000 gpm normally. When the treatment plant needs more water, a pump at the well field forces the flow at a rate of between 7,200 to 8,200 gpm, depending upon the level of water in the receiving reservoir. A flow of 8,200 gpm would draw 11.8 mgd from the wellfield. The operating capacity of the Verna Wellfield, in August 1988, was 17.9 mgd. Harloff's experts assert, and there is no concrete evidence to rebut it, that if all wells at Verna were pumping during a 24 hour period in May 1989, the reservoir could have been maintained at full level. However, though there is a manual override of the automatic reservoir/pump control system, it is unrealistic and unwise to expect full production on a 24 hour basis for any lengthy time period. Water under both Mr. Harloff's property and the Verna Well field is found at various levels known by different names. These include, in order of descent, the Surficial Aquifer, the Intermediate Aquifer, the Upper Floridan Aquifer, and the Lower Floridan Aquifer. The Surficial Aquifer extends from the surface down to between 20 and 60 feet below the surface. A 20 foot thick bed of clay separates the water in this aquifer from that in the aquifer immediately below it, the Intermediate Aquifer, which extends from approximately 80 feet down to approximately 420 feet below the surface. In the lower part of the Intermediate Aquifer, permeability decreases until a confining unit separating the bottom of the Intermediate Aquifer from the top of the Upper Floridan Aquifer is formed. There is such a confining unit between 420 and 500 feet. There is no well-defined confining unit between the Upper and Lower Floridan Aquifers. There is, however, a substantial difference in the transmissivity in each zone. "Transmissivity" is defined as the amount of water that will exist through a section of the aquifer that is the same width from the top to the bottom. The lower the transmissivity rate, the deeper the cone and the narrower the radius of effect. The higher the rate, the shallower the cone and the broader the radius. The Lower Floridan Aquifer has an extremely high transmissivity. Its top is found at a range of from 1,050 to 1,200 feet below the surface on Mr. Harloff's property. The water from the Upper Floridan Aquifer is of higher quality than that in the Lower. It is more readily usable for drinking than that in the Lower, but the Lower water is quite acceptable for agricultural purposes. What confining layer exists between the Upper and Lower Floridan Aquifers is made up of relatively impermeable anhydrides and gypsum. Because of this, there is little likelihood of the highly mineralized water from the Lower Floridan Aquifer rising into the better quality water in the Upper. If, therefore, water for agricultural purposes is drawn from the Lower Floridan Aquifer, with its high transmissivity and narrower cone radius, and if the wells utilized to procure this water are cased down to within the Lower aquifer, there is little chance of a negative impact on the better quality water, used for drinking by the City, within the Upper Floridan and Intermediate Aquifers. Mr. Hardin, an expert geologist and hydrogeologist testifying for Mr. Harloff, concluded, utilizing certain commonly accepted computer models, that Mr. Harloff's requested additional withdrawals would not have a significant effect on the Verna Wellfield's ability to produce water sufficient for the City's needs. This conclusion was based on 1989 seasonal use figures including an average rate of 21.95 mgd, a maximum rate of 27.04 mgd, and a maximum rate of 29 mgd under a "run time" calculation and the fact that during that period, the City was able to pump at least its permitted quantity from its wells at Verna. The City and the District do not accept this conclusion as reasonable, however, because, they claim, the withdrawal figures cited are not meter readouts but estimates based on the number of acres farmed and the number of pump operating hours during the period in question. The City's experts contend the data used by Hardin and Prochaska in their opinions is not that which other experts in the field would reasonably rely upon. They do not appear to be unrealistic, however, and, therefore, Mr. Hardin's opinion is accepted as but one factor to be considered. On the other hand, Mr. Anderson, also a Harloff expert hydrogeologist, claims the requested withdrawals would result in only an additional 1.7 foot drawdown in the Upper Floridan Aquifer underlying the Northeast corner of the Verna Well field. To be sure, this is only one small portion of the wellfield in issue. There has, however, been a continuing history of declining groundwater levels in this area over the past several years. After the 1975 drought, the City started to experience declining water levels at Verna which, because of the reduction in ability to produce water, required a lowering of the pump elements in some wells, and also caused the City to develop an R.O. facility in an effort to reduce dependence on well water. This drop in capability occurred again during the 1985 drought and this time the City modified the pump motors to shut off prior to cavitation and initiated a schedule of operating times for wells, so that water is drawn from different and geographically separated areas in a sequence designed to allow periodic regeneration of an area's supply. Nevertheless, water supply remains a concern at Verna, and the problems previously experienced continue to occur during periods of drought. In May 1989, the Verna Wellfield was periodically "unable" to meet it's short term peak demands at times even though all operating wells were pumping. This means that at the times in question, more water was being drawn from the Verna reservoir than could be replaced by pumping activities. It does not mean that the reservoir ran dry and water could not be furnished to the treatment plant. However, this condition is serious and indicative of a more serious shortage in the future unless appropriate safeguards are instituted. Mr. Balleau, the City's expert in hydrology and hydrogeology, and the District's experts all believe the Verna Wellfield is in trouble. It is operating well beyond its design range and the imposition of additional demands on it would seriously and adversely affect its ability to produce water. This position is supported by the facts and found to be accurate. There appear to be several options open to the City to contend with the Verna problem potential. These include: drill deeper wells at Verna to tap the Lower Floridan Aquifer. (This will produce the lower quality water found there and require additional treatment facilities. construct a linear wellfield along the pipeline from Verna to the treatment facility. (This will require additional permitting to draw the water, high construction and operating costs, and still result in low quality water requiring treatment. redevelop the downtown wells currently supplying the R.O. facility. (This will require satisfaction of regulatory issues, adversely impact on the users of the upper aquifers, possibly result in poor water quality and in contamination from nearby landfills.) develop a new well field southeast of Verna. (This will experience regulatory issues and high construction costs, with an unknown water quality result.) buy water from Manatee County. (This is expensive, may result in transmission and compatibility problems, and would be only a short term solution. lower pump assemblies; replace existing pumps and modify the pump circuits. (These are all unreliable, short term solutions of minimal benefit.) Mr. Harloff and the City/District disagree on the appropriate amount of water needed for the successful growing of the crops produced by his operations. Both agree, however, that the heaviest demands for water come in the spring growing season including April and May. Tomatoes require the most water. Peppers require nearly as much. This is because the short root systems require a higher water table in the soil to supply needed moisture. In its analysis of Mr. Harloff's application, the District, referring to tables developed for the purpose of allocation and relating to Harloff's watering history during the period from August 15, 1988 to June 7, 1989, subtracted the fall season recorded application of 20.7 acre-inches from the total 10 month figure of 50.92 acre-inches and concluded he would need 30.22 acre-inches for peppers during the spring, 1989 season. Unless shown to be totally unreasonable, however, (not the case here), the applicant's water need figures should be accepted. Mr. Harloff's operation constitutes an important part of Manatee County's agricultural economy, and agriculture utilizes 68.9 percent of the land in the county. Agricultural products sold in Manatee County in 1987 were valued at $145,655,000.00, which ranked Manatee County third among all Florida counties in vegetable production. Agriculture is the fourth largest employer in Manatee County, employing an average of 4,692 people per month. Through his farm operation alone, Harloff employes as many as 1,050 people, with 200 employed on a full-time basis. Experts estimate that the loss of the Harloff operation would cause a reduction of between 16 and 18 million dollars in agricultural sales in the county with an additional loss in jobs and income to his suppliers. This estimate is not at all unreasonable. Florida produces approximately 95 percent of all tomatoes grown in this country for the fresh tomato market during the winter growing season. Tomatoes are the single largest vegetable crop grown in the state and accounted for 39.7 percent of the total value of vegetables produced in Florida during the 1987-1988 growing season. Mr. Harloff produced 4.8 percent of the total shipment of tomatoes from this state during that period. Water, primarily through irrigation, is an indispensable portion of the farming operation for this crop. Mr. Harloff currently irrigates the majority of his non-citrus crops by use of a "semi-closed ditch irrigation system", as opposed to a "drip system." The drip system is considerably more efficient than the semi-closed system having an efficiency rating, (amount of water actually used by the plants) of between 80 to 90 percent, as opposed to 40 to 60 percent for the other. While Mr. Harloff could reduce his water needs considerably and achieve substantial savings on pump fuel by conversion to a drip system for all or a part of his crops, such an undertaking would be quite costly. One of the conditions proposed by the District for the approval of Harloff's permit, as amended, is the refurbishment of several of the existing wells utilized by Mr. Harloff to make them more efficient and to promote the withdrawal of water from the Lower Floridan Aquifer, in which there appears to be adequate water and from which the Verna Well field does not draw. Currently, Mr. Harloff has seven wells which do not meet the standards of this proposed condition. They are not drilled to 1,300 feet below mean sea level and are not cased to 600 feet. To bring these wells into compliance, they would have to be drilled to the 1,300 foot level, or to a level which has a specific capacity of 400 gpm, and the casings in each would have to be extended to 600 feet. Extending the casings would be a complicated procedure and Harloff's experts in the area cannot guarantee the procedure would successfully achieve the desired end. Assuming the retrofit was successful, the cost of the entire process would be approximately $15,000.00 to $16,000.00 per well. In addition, the process would, perforce, require reducing the diameter of the well from 10 to 8 inches, thereby necessitating increasing the pump capacity to produce sufficient water. The cost of this is substantial with an appropriate new pump costing somewhere between $10,000.00 and $15,000.00 each. Consequently, the anticipated cost of bringing the existing wells up to condition standards would be between $25,000.00 to $31,000.00 per well, while the cost of constructing a new well is between $40,000.00 and $50,000.00 per well. Mr. Harloff feels it would be more prudent for him to replace the existing wells rather than to retrofit them. This may be correct. Harloff experts also claim that extending the casings on the existing wells down to 600 feet would not provide a significant benefit to the aquifer nor cause any significant reduction in drawdown impact at Verna. The District and City experts disagree and, taken on balance, caution and the interests of the public indicate that a conservative approach is more appropriate. While Mr. Harloff proposes to convert the areas served by wells 1, 9, 11, and 12 to the growing of citrus which requires much less water than tomatoes, this would not be sufficient mitigation to offset the need for some modification if large amounts of water will still be drawn. The entire area under the District's jurisdiction has been experiencing a water shortage due to a lack of rainfall. As a result, in June 1989, the District adopted a resolution identifying an area, including the area in question here, as a "water use caution area." This was done because the Floridan Aquifer has been subjected to large seasonable drawdowns of the potientiometric surface, the level to which water in a confined aquifer can rise in a well which penetrates that acquifer. This drawdown is directly related to increased water use in the area, much of which is for agricultural purposes. As a result of the District's action, special conditions on well construction for consumptive use applicants have been imposed on a permit by permit basis to insure, as much as possible, that the applicant uses the lowest quality water appropriate for his intended purpose. These conditions are not unreasonable. While accepting the District's and City's conclusion that his wells, if permitted, would have some impact on the Verna Wellfield, Mr. Harloff does not concede that the impact is significant. Specifically, the difference in impact resulting from an increase from his currently permitted use of 13.68 mgd seasonal maximum and his requested use of 31.56 mgd seasonal maximum for wells 1, 2, 9, and 10 would be a maximum increased drawdown of 1.1 feet at the Intermediate aquifer and 1.8 feet at the Upper Floridan Aquifer. Both figures relate to that portion of the wellfield found in the northeast corner of Part A. If the anticipated usage for crops predicted by Mr. Harloff's experts for the spring of 1989 is accurate, the drawdown would be 0.2 feet for the intermediate aquifer and 0.4 feet for the Upper Floridan Aquifer measured at the northeast corner of Part B of the Verna We1lfield. Harloff's experts contend that additional impacts for the spring of 1989 included, the increased usage will not have a significant effect on Verna's ability to produce its permitted daily maximum withdrawal of 9.5 mgd. While this is an educated speculation, it should be noted that during May 1989, the Verna field was able to produce up to 8.3 mgd without using all wells during any 24 hour period. This does not consider, however, the problems encountered by the City as indicated by the wellfield personnel, and the fact that some of the City wells are not pumping water.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, therefore: RECOMMENDED that Roger Harloff be issued a consumptive use permit, No. 204467.04, as modified, to reflect authorization to draw 15.18 mgd annual average, not to exceed 31.56 mgd seasonal maximum, conditioned upon compliance with the conditions found in the conditions portion of the permit, as modified to conform to the quantities as stated herein, and to include those requirements as to acre-inch and crop-acre limitations, well usage and abandonment schedules, well modification standards, and record keeping, as are contained therein. RECOMMENDED this 5th day of December, 1989, in Tallahassee, Florida. ARNOLD H. POLLOCK, Hearing officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 5th day of December, 1989. APPENDIX TO RECOMMENDED ORDER IN CASE No. 89-0574 The following constitutes my specific rulings pursuant to s. 120.59(2), Florida Statutes, on all of the proposed Findings of Fact submitted by the parties to this case. FOR THE PETITIONER: City of Sarasota, joined by the District 1 & 2. Accepted and incorporated herein. 3. Accepted and incorporated herein. 8-12. Accepted and incorporated herein. 13. Accepted and incorporated herein. 14-22. Accepted and incorporated herein. 23-25. Accepted and incorporated herein. 26. Accepted and incorporated herein. 27 & 28. Accepted and incorporated herein. 29-33. Accepted and incorporated herein. Not a Finding of Fact but a statement of party position. & 36. Accepted. 37. & 38. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not a Finding of Fact but a comment on opponent's satisfaction of its burden of proof. 42-44. Accepted and incorporated herein. Accepted and incorporated herein. Rejected as a misstatement of fact. Water service was never interrupted. The deficiency was in the City's inability to keep its wellfield reservoir filled. 47-54. Accepted and incorporated herein. Accepted and incorporated herein. Rejected for the reasons outlined in 41. 57-62. Accepted and incorporated herein. 63. Rejected for the reasons outlined in 41. 64-66. Accepted and incorporated herein. Rejected for the reasons outlined in 41. Rejected. & 70. Accepted and incorporated herein. 71. & 72. Accepted and incorporated herein. 73. Accepted and incorporated herein. 74 & 75. Accepted and incorporated herein. Accepted. Not a Finding of Fact but a statement of party position. Rejected. Accepted. Irrelevant. 81-84. Rejected. 85. & 86. Accepted and incorporated herein. 87 & 88. Accepted and incorporated herein. 89. Accepted and incorporated herein. 90 & 91. Accepted and incorporated herein. 92. & 93. Accepted and incorporated herein. FOR THE RESPONDENT: Roger Harloff 1-9. Accepted and incorporated herein. 10-13. Accepted and incorporated herein. 14 & 15. Accepted and incorporated herein. 16-25. Accepted and incorporated herein. 26-28. Accepted and incorporated herein. 29 & 30. Accepted. Accepted and incorporated herein. Accepted. Accepted and incorporated herein. Not proven. 35 & 36. Accepted and incorporated herein. 37 & 38. Accepted and incorporated herein. 39-41. Accepted and incorporated herein. 42 & 43. Accepted and incorporated herein. 44. Accepted. 45 & 46. Accepted and incorporated herein. 47 & 48. Accepted and incorporated herein. 49. Accepted. 50 & 51. Accepted and incorporated herein. Accepted. Accepted. Accepted. & 56. Accepted and incorporated herein. 57. Accepted. 58-60. Accepted and incorporated herein. 61 & 62. Accepted and incorporated herein. Rejected as unproven. Accepted. Accepted and incorporated herein. Accepted. 67-68. Accepted. Not a Finding of Fact but an interpretation of party po Accepted. Rejected. 72 & 73. Accepted. COPIES FURNISHED: Edward P. de la Parte, Jr., Esquire de la Parte, Gilbert and Gramovot, P.A. 705 East Kennedy- Blvd. Tampa, Florida 33602 Edward B. Helvenston, Esquire SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899 Douglas P. Manson, Esquire Blain & Cone, P.A. 202 Madison Street Tampa, Florida 33602 Peter G. Hubbell Executive Director SWFWMD 2379 Broad Street Brooksville, Florida 34609-6899
The Issue The issue in this case was whether the Respondent, City of Cape Coral (City), was entitled to an Individual Environmental Resource Permit (Permit) that would allow removal of the Chiquita Boat Lock (Lock) and associated uplands, and installation of a 165-foot linear seawall in the South Spreader Waterway in Cape Coral, Florida.
Findings Of Fact Based on the parties' stipulations and the evidence adduced at the final hearing, the following findings of fact are made: The Parties The Department is the administrative agency of the State of Florida statutorily charged with, among other things, protecting Florida's water resources. As part of the Department's performance of these duties, it administers and enforces the provisions of chapter 373, part IV, Florida Statutes, and the rules promulgated thereunder in the Florida Administrative Code. Pursuant to that authority, the Department determines whether to issue or deny applications for environmental resource permits. The City is a Florida municipality in Lee County. The City is the applicant for the Permit allowing the removal of the Lock and installation of a seawall (Project). The Project is located within the geographic boundary of the City. The South Spreader Waterway is a perimeter canal separating the City's canal system from shoreline wetlands to the west and south, which run the length of Matlacha Pass to the mouth of the Caloosahatchee River at San Carlos Bay.1/ The Association is a Florida non-profit corporation that was created in 1981. The Association was created to safeguard the interests of its members. The Association has approximately 150 members who reside in Matlacha and Matlacha Isles, Florida. A substantial number of its members have substantial interests in the use and enjoyment of waters adjacent to and surrounding Matlacha. The Association's members were particularly interested in protecting the water quality of the surface waters in the area. Matlacha is an island community located to the northwest of Cape Coral, the South Spreader Waterway, and the Lock. Matlacha is located within Matlacha Pass Aquatic Preserve. Matlacha Pass is classified as a Class II waterbody designated for shellfish propagation or harvesting, and is an Outstanding Florida Water (OFW). See Fla. Admin. Code R. 62-02.400(17)(b)36; 62-302.700(9)(h). Petitioner, Karl Deigert, is a resident and property owner in Matlacha. Mr. Deigert is the president of the Association. Mr. Deigert’s house in Matlacha is waterfront. He holds a captain’s license and has a business in which he gives sightseeing and ecological tours by boat of the waters around Matlacha. He fishes in the waters around his property and enjoys the current water quality in the area. He is concerned that removal of the Lock would have negative effects on water quality and would negatively impact the viability of his business and his enjoyment of the waters surrounding Matlacha. Petitioner, Melanie Hoff, is a resident and property owner in St. James City. St. James City is located to the southwest of Cape Coral. Ms. Hoff’s property is located within five nautical miles of the Lock. Ms. Hoff engages in various water sports and fishes in the waters around her property. She moved to the area, in part, for the favorable water quality. She is concerned that removal of the Lock would negatively impact water quality and her ability to use and enjoy waters in the area. Petitioner, Robert S. Zarranz, is a resident and property owner in Cape Coral. Mr. Zarranz’s house in Cape Coral is waterfront. He is an avid fisherman and boater. He is concerned that removal of the Lock would negatively impact water quality, and that the quality of fishing in the area would decline as a result. Petitioner, Yolanda Olsen, is a resident and property owner in Cape Coral. Ms. Olsen’s house in Cape Coral is waterfront. She enjoys watersports and birdwatching in the areas around her property. She is concerned that removal of the Lock would negatively impact water quality, and that her ability to enjoy her property and the surrounding waters would suffer as a result. Petitioner, Jessica Blanks, is a resident and property owner in Cape Coral. Ms. Blanks’ house in Cape Coral is waterfront. She is concerned that removal of the Lock would negatively impact water quality, and that her ability to enjoy her property and the surrounding waters would suffer as a result. Petitioner, Joseph Michael Hannon, is a resident and property owner in Matlacha. Mr. Hannon is a member of the Association. He enjoys boating, fishing, and kayaking in the waters surrounding Matlacha. He is concerned that removal of the Lock would negatively impact water quality, and that his ability to enjoy his property and the surrounding waters would suffer as a result. Petitioner, Debra Hall, did not appear at the final hearing and no testimony was offered regarding her standing. The Project and Vicinity The Project site is 0.47 acres. At the Lock location, the South Spreader Waterway is 200 feet wide, and includes a 125-foot wide upland area secured by two seawalls, the 20-foot wide Lock, a 32-foot wide upland area secured by one seawall, and 23 feet of mangrove wetlands. The Lock is bordered to the north by property owned by Cape Harbour Marina, LLC, and bordered to the south by mangrove wetlands owned by the state of Florida. The 125-foot wide upland area and the 20-foot wide Lock form a barrier separating the South Spreader Waterway from the Caloosahatchee River. The preponderance of the competent substantial evidence established that the South Spreader Waterway behind the Lock is not tidally influenced, but would become tidally influenced upon removal of the Lock. Joint Exhibit 1 at p. 46. The City proposes to remove the Lock and one of the seawalls, reducing the 125-foot upland area to 20 feet. The proposed future condition of the area would include 125 feet of open canal directly connecting the South Spreader Waterway with the Caloosahatchee River. Joint Exhibit 1 at p. 47. The primary purpose of the Lock's removal is to alleviate safety concerns related to boater navigation. The Project's in-water construction includes demolition and removal of the existing Lock, removal of existing fill in the 125-foot upland area, removal of existing seawalls, and construction of replacement seawalls. The City would employ Best Management Practices (BMPs) throughout the course of the Project, including sediment and erosion controls such as turbidity barriers. The turbidity barriers would be made of a material in which manatees could not become entangled. All personnel involved with the Project would be instructed about the presence of manatees. Also, temporary signs concerning manatees would be posted prior to and during all in-water project activities. History of the South Spreader Waterway In the mid-1970's, the co-trustees of Gulf American Corporation, GAC Properties Credit, Inc., and GAC Properties, Inc., (collectively GAC) filed for after-the-fact permits from the Department's predecessor agency (DER), for the large dredge and fill work project that created the canal system in Cape Coral. In 1977, DER entered into CO 15 with GAC to create the North and South Spreader Waterways and retention control systems, including barriers. The Lock was one of the barriers created in response to CO 15. The Spreader Waterways were created to restore the natural hydrology of the area affected by GAC's unauthorized dredging and filling activity. The Spreader Waterways collected and retained surface runoff waters originating from the interior of Cape Coral's canal system. The South Spreader Waterway was not designed to meet water quality standards, but instead to collect surface runoff, then allow discharge of the excess waters collected over and through the mangrove wetlands located on the western and southern borders of the South Spreader Waterway. This fresh water flow was designed to mimic the historic sheet flow through the coastal fringe of mangroves and salt marshes of the Caloosahatchee River and Matlacha Pass estuaries. The fresh water slowly discharged over the coastal fringe until it finally mixed with the more saline waters of the estuaries. The estuarine environments located west and south of the Lock require certain levels of salinity to remain healthy ecosystems. Restoring and achieving certain salinity ranges was important to restoring and preserving the coastal fringe. In 1977 GAC finalized bankruptcy proceedings and executed CO 15. CO 15 required GAC to relinquish to the state of Florida the mangrove wetlands it owned on the western and southern borders of the South Spreader Waterway. This land grant was dedicated by a warranty deed executed in 1977 between GAC and the state of Florida. The Petitioners' expert, Kevin Erwin, worked as an environmental specialist for DER prior to and during the construction of the Spreader Waterways. Mr. Erwin was DER's main representative who worked with the GAC co-trustees to resolve the massive dredge and fill violation and design a system to restore the natural hydrology of the area. Mr. Erwin testified that the Lock was designed to assist in retention of fresh water in the South Spreader Waterway. The fresh water would be retained, slowed down, and allowed to slowly sheet flow over and through the coastal fringe. Mr. Erwin also testified that the South Spreader Waterway was not designed to allow direct tidal exchange with the Caloosahatchee River. In Mr. Erwin's opinion, the South Spreader Waterway appeared to be functioning today in the same manner as originally intended. Breaches and Exchange of Waters The Department's second amended notice of intent for the Project, stated that the Project was not expected to contribute to current water quality violations, because water in the South Spreader Waterway was already being exchanged with Matlacha Pass and the Caloosahatchee River through breaches and direct tidal flow. This second amended notice of intent removed all references to mitigation projects that would provide a net improvement in water quality as part of the regulatory basis for issuance of the permit. See Joint Exhibit 1 at pp. 326-333. The Department's witnesses testified that waters within the South Spreader Waterway currently mix with waters of the Caloosahatchee River when the Lock remains open during incoming and slack tides. A Department permit allowed the Lock to remain open during incoming and slack tides. Department witness, Megan Mills, the permitting program administrator, testified that she could not remember the exact date that permit was issued, but that it had been "a couple years." The location of breaches in the western and southern banks of the South Spreader Waterway was documented on another permit's drawings and pictures for a project titled "Cape Coral Spreader Waterway Restoration." See Cape Coral Ex. 9. Those documents located three breaches for repair and restoration identified as Breach 16A, Breach 16B, and Breach 20. The modeling reports and discussion that support the City's application showed these three breaches connect to Matlacha Pass Aquatic Preserve. Breach 20 was described as a connected tidal creek. Breach 16A and 16B were described as allowing water movement between Matlacha Pass and the South Spreader Waterway only when relatively high water elevations occurred in Matlacha Pass or in the South Spreader Waterway. The Department's water quality explanation of "mixing," was rather simplistic, and did not consider that the waterbody in which the Project would occur has three direct connections with an OFW that is a Class II waters designated for shellfish propagation or harvesting. Such a consideration would require the Department to determine whether to apply the OFW permitting standards, and the Class II waters permitting criteria in section 10.2.5 of the Environmental Resource Permit Applicant's Handbook, Volume I. See Fla. Admin Code R. 62-330.302(1)(a); 62-4.242(2); and 62-302.400(17)(b)36. The Caloosahatchee River, at its entrance to the South Spreader Waterway, is a Class III waters restricted for shellfish harvesting. The mouth of the Caloosahatchee River is San Carlos Bay, which is a Class II waters restricted for shellfish harvesting. There was no evidence that the Department's regulatory analysis considered that the waterbody in which the Project would occur directly connects to Class III waters that are restricted for shellfish harvesting, and is in close proximity to Class II waters that are restricted for shellfish harvesting. See Fla. Admin. Code R. 62-302.400(17)(b)36. and 62-330.302(1)(c).2/ Total Nitrogen The City's expert, Anthony Janicki, Ph.D., testified that nitrogen concentrations in the Caloosahatchee River were higher than in the South Spreader Waterway in the years 2017 and 2018. Thus, he opined that if the Lock is removed, water from the South Spreader Waterway would not negatively impact the Caloosahatchee River. However, the City's application was supported by an analysis, with more than a decade of monitoring data, which showed nitrogen concentration values were comparable inside the South Spreader Waterway and in the Caloosahatchee River. Dr. Janicki also used the Department's Hydrologic Simulation Program – FORTRAN (HSPF) watershed model to estimate the Total Nitrogen (TN) loading that would enter the Caloosahatchee River through the Chiquita Lock. Dr. Janicki estimated that TN loading to the Caloosahatchee River, after removal of the Chiquita Lock, would amount to 30,746 pounds per year. The Caloosahatchee River is listed as impaired for nutrients and has a TN Total Maximum Daily Load (TMDL) that was set by the Department in 2009. Dr. Janicki opined that removing the Lock would not result in adverse impacts to the surrounding environment. But the Petitioners obtained his concession that his opinion was dependent on the City's completion of additional water quality enhancement projects in the future as part of its obligations under the Caloosahatchee Estuary Basin Management Action Plan (BMAP) for achieving the TN TMDL. Dr. Janicki additionally testified that the potential TN loading to the Caloosahatchee River did not anticipate an actual impact to the River's water quality because the TN loads from the South Spreader Waterway were already factored into the 2009 TMDL. He essentially testified that the Lock's removal was anticipated and was factored into the model when the TMDL was established in 2009. Thus, the Petitioners proved by a preponderance of the competent and substantial evidence that the Department and the City were not aligned regarding how the City's application would provide reasonable assurances of meeting applicable water quality standards. The Petitioners proved by a preponderance of the competent and substantial evidence that the City relied on future projects to provide reasonable assurance that the removal of the Lock would not cause or contribute to violations of water quality standards in the Caloosahatchee River and the Matlacha Pass Aquatic Preserve. The Petitioners proved by a preponderance of the competent and substantial evidence that the Department relied on a simplistic exchange of waters to determine that removal of the Lock would not cause or contribute to violations of water quality standards in the Caloosahatchee River and the Matlacha Pass Aquatic Preserve. Water Quantity and Salinity The engineering report that supports the City's application stated that when the Lock is removed, the South Spreader Waterway behind the Lock will become tidally influenced. With the Lock removed, the volume of daily water fluxes for the South Spreader Waterway would increase from zero cubic meters per day to 63,645 cubic meters per day. At the location of Breach 20, with the Lock removed, the volume of daily water fluxes would drastically decrease from 49,644 cubic meters per day to eight cubic meters per day. Dr. Janicki testified that Breach 20 was connected to a remnant tidal creek that meanders and eventually empties into an embayment. The evidence demonstrated that the embayment is Punta Blanca Bay, which is part of the Matlacha Pass Aquatic Preserve. Dr. Janicki opined that Breach 20 was an area of erosion risk and sediment transport into downstream mangroves that would be significantly reduced by removing the Lock. He explained that the reductions in flow would result in reductions in velocities through Breach 20 and in the South Spreader Waterway itself. Mr. Erwin testified that Breach 20 was not a "breach."3/ He described it as the location of a perpendicular intersection of the South Spreader Waterway with a small tidal creek, which connected to a tidal pond further back in the mangroves. Mr. Erwin testified that an "engineered sandbag concrete structure" was built at the shallow opening to limit the amount of flow into and out of this tidal creek system. But it was also designed to make sure that the tidal creek system "continued to get some amount of water." As found above, Lock removal would drastically reduce the volume of daily water fluxes into and out of Breach 20's tidal creek system. Mr. Erwin also testified that any issues with velocities or erosion would be exemplified by bed lowering, siltation, and stressed mangroves. He persuasively testified, however, that there was no such evidence of erosion and there were "a lot of real healthy mangroves." Mr. Erwin opined that removal of the Lock would cause the South Spreader Waterway to go from a closed, mostly fresh water system, to a tidal saline system. He described the current salinity level in the South Spreader Waterway to be low enough to support low salinity vegetation and not high enough to support marine organisms like barnacles and oysters. The City's application actually supports this opinion. Using the Environmental Fluid Dynamics Code (EFDC) model developed by Dr. Janicki for this Lock removal project, comparisons were made describing the salinity distribution within the South Spreader Waterway. The model was run with and without the Lock, for both a wet and dry year. Dr. Janicki testified, and the model showed, that removal of the Lock would result in increased salinity above the Lock and decreased salinity downstream of the Lock. However, he generally opined that the distribution of salinities was well within the normal ranges seen in this area. The City's application also concluded that the resultant salinities did not fall outside the preferred salinity ranges for seagrasses, oysters, and a wide variety of fish taxa. However, Dr. Janicki did not address specific changes in vegetation and encroachment of marine organisms that would occur with the increase in salinity within the South Spreader Waterway. Secondary Impacts to the Mangrove Wetlands Mr. Erwin testified that the mangroves located on the western and southern borders of the South Spreader Waterway are currently in very good health. He additionally testified that loss of the current fresh water hydraulic head and an increase in salinity within the South Spreader Waterway would negatively impact the health of the mangrove wetlands. In addition, the City's application stated that removing the Lock would result in a drop in the water level of one to one and a half feet within the South Spreader Waterway. Mr. Erwin credibly and persuasively testified that a drop in water level of only a few inches would have negative effects on the health of mangroves, and that a drop of a foot could result in substantial mangrove die-off. Mr. Erwin testified that the mangrove wetlands adjacent to the South Spreader Waterway consist of a variety of plants and algae in addition to mangroves. He described the wetlands as a mangrove community made up of different types of mangroves, and epiphytic vegetation such as marine algae. This mangrove community provides habitat for a "wide range of invertebrates." He further testified that these plants and algae uptake and transform the nutrients that flow over and through the mangrove wetlands before they reach the receiving waters. Thus, the mangrove wetlands on the western and southern borders of the South Spreader Waterway serve to filter nutrients out of the water discharged from the Waterway before it reaches Matlacha Pass and the Caloosahatchee River. Mr. Erwin's credible and persuasive testimony was contrary to the City's contention that Lock removal would not result in adverse impacts to the mangrove wetlands adjacent to the South Spreader Waterway. The City and the Department failed to provide reasonable assurances that removing the Lock would not have adverse secondary impacts to the health of the mangrove wetlands community adjacent to the South Spreader Waterway. Impacts to Fish and Wildlife, Including Endangered and Threatened Species The Florida Fish and Wildlife Conservation Commission (FWC) reviewed the City's application and determined that if BMPs for in-water work were employed during construction, no significant adverse impacts on fish and wildlife were expected. For example, temporary signs concerning manatees would be posted prior to and during all in-water project activities, and all personnel would be instructed about the presence of manatees. The FWC determination only addressed direct impacts during in-water construction work. The City's application contained supporting material that identified the major change resulting from removal of the Lock that may influence fish and wildlife in the vicinity of the Project, was the opportunity for movement to or from the South Spreader Waterway canal system. Threatened and endangered species of concern in the area included the Florida manatee and the smalltooth sawfish. The City's application stated that literature review showed the smalltooth sawfish and the Florida manatee utilized non-main-stem habitats, such as sea-wall lined canals, off the Caloosahatchee River. The City cited studies from 2011 and 2013, which showed that non-main-stem habitats were important thermal refuges during the winter, and part of the overall nursery area for smalltooth sawfish. The City concluded that removal of the Lock "would not be adverse, and would instead result in increased areas of useable habitat by the species." However, the Petitioner's expert witness, John Cassani, who is the Calusa Waterkeeper, testified that there is a smalltooth sawfish exclusion zone downstream of the Lock. He testified that the exclusion zone is a pupping area for smalltooth sawfish, and that rapid salinity fluctuations could negatively impact their habitat. The City also concluded that any impacts to the Florida manatee would not be adverse, "and would instead result in increased areas of useable habitat by the species, as well as a reduction in risk of entrapment or crushing in a canal lock system." At the same time, the City acknowledged that "watercraft collision is a primary anthropogenic threat to manatees." The City's literature review included a regional assessment by FWC's Fish and Wildlife Research Institute (FWRI) from 2006. Overall, the FWRI report concluded that the mouth of the Caloosahatchee River, at San Carlos Bay, was a "hot spot" for boat traffic coinciding with the shift and dispersal of manatees from winter refugia. The result was a "high risk of manatee- motorboat collisions." In addition, testimony adduced at the hearing from an 18-year employee of Cape Harbour Marina, Mr. Frank Muto, was that Lock removal would result in novice boaters increasing their speed, ignoring the no-wake and slow-speed zones, and presenting "a bigger hazard than the [L]ock ever has." Boater Navigation Concerns Oliver Clarke was the City’s principal engineer during the application process, and signed the application as the City's authorized agent. Mr. Clarke testified that he has witnessed boater congestion at the Lock. He also testified that lack of boating experience and weather concerns can exacerbate the boater congestion issues at the Lock. Petitioners presented the testimony of Mr. Frank Muto, the general manager of Cape Harbour Marina. Mr. Muto has been at the Cape Harbour Marina for 18 years. The marina has 78 docks on three finger piers along with transient spots. The marina is not currently subject to tidal flows and its water depth is between six and a half and seven and a half feet. He testified that they currently have at least 28 boats that maintain a draft of between four and a half and six feet of water. If the water depth got below four feet, those customers would not want to remain at the marina. Mr. Muto further testified that the Lock was in place when the marina was built, and the marina and docks were designed for an area with no tidal flow. Mr. Muto also testified that he has witnessed several boating safety incidents in and around the Lock. He testified that he would attribute almost all of those incidents to novice boaters who lack knowledge of proper boating operations and locking procedures. Mr. Muto additionally testified that there is law enforcement presence at the Lock twenty-four hours a day, including FWC marine patrol and the City's marine patrol.
Conclusions For Petitioners: J. Michael Hannon, Qualified Representative 2721 Clyde Street Matlacha, Florida 33993 John S. Turner, Esquire Peterson Law Group Post Office Box 670 Fort Myers, Florida 33902 For Respondent City of Cape Coral: Craig D. Varn, Esquire Amy Wells Brennan, Esquire Manson Bolves Donaldson Varn, P.A. 106 East College Avenue, Suite 820 Tallahassee, Florida 32301 Steven D. Griffin City of Cape Coral Assistant City Attorney Post Office Box 150027 Cape Coral, Florida 33915-0027 For Respondent Department of Environmental Protection: Kirk Sanders White, Esquire Department of Environmental Protection Mail Station 35 3900 Commonwealth Boulevard, Tallahassee, Florida 32399-3000
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is, RECOMMENDED that: The Department of Environmental Protection enter a final order denying Individual Environmental Resource Permit Number 244816-005 to the City of Cape Coral for removal of the Chiquita Boat Lock. The final order deny Petitioners' request for an award of attorney's fees and costs. DONE AND ENTERED this 12th day of December, 2019, in Tallahassee, Leon County, Florida. S FRANCINE M. FFOLKES 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 12th day of December, 2019.
The Issue This case involves a challenge to St. Johns River Water Management District’s (District or SJRWMD) intended issuance of an Environmental Resource Permit (ERP) granting the City's Application No. 4-127-97380-1, for the construction and operation of a surface water management system for a retrofit flood-relief project known as Drysdale Drive/Chapel Drive Drainage Improvements consisting of: excavation of the Drysdale Drive pond (Pond 1); improvement to the outfall at Sterling Lake; and the interconnection of Pond 1 and four existing drainage retention areas through a combination of pump stations and gravity outfalls (project or system). The issue is whether the applicant, the City of Deltona (City or Deltona), has provided reasonable assurance the system complies with the water quantity, environmental, and water quality criteria of the District’s ERP regulations set forth in Chapter 40C-4, Florida Administrative Code,1 and the Applicant’s Handbook: Management and Storage of Surface Waters (2005) (A.H.).2
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the St. Johns River Water Management District enter a final order issuing to the City of Deltona an ERP granting the City's Application No. 4-127-97380-1, subject to the conditions set forth in the Technical Staff Report. DONE AND ENTERED this 17th day of March, 2006, in Tallahassee, Leon County, Florida. S J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 17th day of March, 2006.
The Issue The issue to be determined in this case is whether the Respondents, Florida Department of Transportation (“FDOT”) and Palm Beach County (also referred to as “the Applicants”), are entitled to the issuance of an Environmental Resource Permit (“ERP”) to construct an extension of State Road 7 (“SR 7”) and its associated surface water management system in Palm Beach County.
Findings Of Fact The Parties The City is a municipality incorporated under Florida law. The District is a regional agency with the authority to regulate the construction, operation, and maintenance of any surface water management system pursuant to chapter 373, Part IV, Florida Statutes, and Florida Administrative Code Titles 40E and 62. FDOT is an agency of the state of Florida charged with the establishment, maintenance, and regulation of public transportation. It is a co-applicant for the ERP permit. Palm Beach County is a political subdivision of the State of Florida, and is a co-applicant for the ERP permit. Background State Road 7 Extension The ERP was issued by the District for an 8.5-mile extension of SR 7 between Okeechobee Boulevard and Northlake Boulevard in Palm Beach County. The purpose of the proposed roadway is to relieve traffic now moving through rural residential areas and two large residential developments known as The Acreage and Jupiter Farms. The proposed roadway would also improve hurricane evacuation by providing additional capacity and connectivity, and reduce emergency response time in the rural residential areas. The proposed roadway alignment was selected by FDOT after a multiyear corridor study under a National Environmental Protection Policy Act process. Four corridors were considered using federal selection criteria that addressed social, environmental, property, physical, and financial impacts. There are two segments of the proposed roadway covered by the ERP. The southern segment would add two more lanes to the existing two-lanes of SR 7 from Okeechobee Boulevard North to 60th Street North, just south of the M-Canal. This segment is 4.4 miles long. The southern segment is not at issue in this case. The northern segment would extend four lanes of SR 7 east from 60th Street North about one mile, and then north 3.1 miles to Northlake Boulevard. This is the roadway segment challenged by Petitioner. Hereafter, all references to “the Project” are to the northern segment. The Project includes a raised roadway, median, sidewalks, bike lanes, and stormwater swales. It also includes a bridge over the M-Canal and a bridge over a water control outfall. The Project would be constructed in an existing right- of-way (“ROW”). FDOT owns a ROW that is approximately 200 feet wide. The County owns an adjacent 120-foot-wide ROW, so that the total width of the Project ROW is 320 feet. Running north/south within the ROW is a dirt service road, a ditch, and a fence. Much of the vegetation in the ROW is dominated by invasive and exotic plant species, including Melaleuca, Carolina Willow, Brazilian Pepper, and Australian Pine. The Ibis Development West of the Project ROW is the 1,958-acre Ibis Golf and Country Club residential development (“Ibis”). In 1989, an ERP was issued for Ibis’ surface water management system (“the Ibis system”). The Ibis system includes almost 300 acres of interconnected lakes that provide water management and water quality treatment for Ibis. The 1989 permit required the Ibis system to be sized to receive and treat runoff from a segment of Northlake Boulevard and from an existing two-lane road off of Northlake Boulevard that serves the commercial area of Ibis, which is directly north of the Ibis residential area. The Ibis system was also required to receive and provide water treatment and storage for the stormwater runoff from 46.8 acres of the ROW for SR 7. The parties introduced evidence about modifications to the 1989 permit, which the City contends reduced the treatment capabilities of the system. It is found from the preponderance of the evidence that the original system and its modifications continued to meet design requirements to store and treat future runoff from 46.8 acres of the SR 7 ROW.1/ When the water in the Ibis lakes reaches elevation 17.5 feet NGVD (National Geodetic Vertical Datum), pumps at two pump stations at the south end of Ibis begin pumping water over a berm into Ibis Preserve, a 366-acre natural area directly south of Ibis. Water is retained in Ibis Preserve unles it exceeds an elevation of 18.5 feet, when it then passes over an outfall structure into the Grassy Waters Everglades Preserve (“Grassy Waters”) to the east. Ibis Preserve provides additional water quality treatment for the water pumped from Ibis, but this additional treatment was not part of the calculation of water quality management for Ibis. The Ibis system was required to meet District permitting criteria before discharge to Ibis Preserve. The North Palm Beach County Improvement District (“Improvement District”) owns and has operational and maintenance responsibility for the Ibis system. It also owned and managed Ibis Preserve, but transferred ownership and management of Ibis Preserve to the City in 2004. Grassy Waters/Water Catchment Area To the east of the Project is the City-owned “Water Catchment Area,” which covers about 14,700 acres or 23 square miles. The Water Catchment Area is owned by the City and is part of its public drinking water supply system. Water in the Water Catchment Area flows to Lake Mangonia where it is withdrawn, treated, and then delivered to residents and businesses in the City, the Town of Palm Beach, and the Town of South Palm Beach. There is a statement in the Project application that Grassy Waters refers only to the open water marsh within the Water Catchment Area. The Water Catchment Area includes other habitat types besides open marsh. Most of the information in the record indicates that Grassy Waters and the Water Catchment Area have the same boundaries. Therefore, in this Recommended Order, Grassy Waters and the Water Catchment Area are treated as being two names for the same area. Grassy Waters was once connected to the Everglades and large portions of it have the same characteristics, being an open water marsh with an extended hydroperiod. It is oligotrophic, meaning it is low in nutrients and has an ecosystem adapted to low nutrient conditions. It was undisputed that most areas of Grassy Waters are of high or even pristine environmental quality. Grassy Waters has periphyton, an assemblage of algae that only survive in phosphorous levels of less than 10 parts per billion (“ppb”). Periphyton is the base of the food chain in the open water marsh area of Grassy Waters and is consumed by apple snails and many invertebrates and fish. Grassy Waters has a visitor and nature center and provides recreational opportunities, such as canoeing, hiking, and bird watching. There appeared to be disagreement about whether the Project ROW is located in Grassy Waters or adjacent to it. The ROW is not within Grassy Waters, it is adjacent. However, the wetlands and other surface waters within the ROW are hydrologically connected to Grassy Waters. In the western part of Grassy Waters, which ends at the Project ROW, there are hammock islands and hydric pine flatwoods. The City contends these areas and the rest of the ROW were historically open water marsh, but were changed by human activities. The more persuasive evidence is that this western area was not all open marsh, historically. It was an area of natural transition from open water marsh to other habitat types. Ibis Impacts to Grassy Waters The parties disputed whether the Ibis system is a “failed system.” This is not a technical or defined term. The relevant issue is whether the Ibis system is operating in conformance with the requirements of its permit. The City contends the Ibis lakes are eutrophic and that sediment accumulation in the lakes is releasing phosphorus back into the water, which ends up in Grassy Waters. However, the City’s expert witness, Dr. Harper, admitted that the phosphorus concentration being discharged from the Ibis system, about 40 ppb, is typical for surface water management systems serving large residential developments, although that concentration is at the high end of the range. The phosphorus concentration is closer to 30 ppb in discharges from Ibis Preserve into Grassy Waters, showing that Ibis Preserve provides additional treatment to the waters coming out of Ibis. The characterization of the nutrient loading from the Ibis system as “typical” did not address the additional nutrients in the drainage that the Ibis system is required to accept from the SR 7 ROW. The record does not show that the nutrient concentrations from the Ibis system would still be typical if all of the ROW drainage were added without pre-treatment, as was contemplated by the 1989 Ibis permit. Because Grassy Waters is an oligotrophic ecosystem, it can be adversely affected by phosphorus levels above 10 ppb. When phosphorus is introduced into an oligotrophic system in concentrations over 10 ppb, the system begins to change to denser wetland vegetation, which can include invasive and nuisance species, such as cattail. There is denser vegetation and cattails in Grassy Waters near the Ibis Preserve outfall. There is also more phosphorus in sediments near the outfall. These effects decrease with distance from the outfall, but some effects were detected as far as a half mile from the outfall. The City’s expert witness, Dr. Gaiser, testified that periphyton is dissolved by high nutrient levels and replaced by weedy algae. She found adverse effects on periphyton near the outfall. Dr. Gaiser also found microcystis near the outfall. Microcystis is a toxic algae caused by high elevations of phosphorous. Microcystis comprised over 10 percent of the cell density of the algal community near the outfall. The District’s witness, Mr. Waterhouse, conceded that there is a problem with nuisance vegetation at the discharge point into Grassy Waters. He said the District was not aware of the problem before information was developed for this case. No evidence was presented about what consideration the District gave in 1989, when Ibis was permitted, to the potential adverse impacts of discharging phosphorus into the oligotrophic ecosystem of Grassy Waters. Based on the evidence that a phosphorus concentration of 30 ppb is expected for this kind of surface water management system, it must be concluded that the Ibis system was not designed to prevent harm to oligotrophic receiving waters. Respondents presented evidence to show that phosphorus loadings from the M-Canal could be the cause of the adverse impacts found near the Ibis Preserve outfall. The M-Canal was constructed by the City for the primary purpose of delivering water from Lake Okeechobee, via connection to the L-8 Canal, to the Water Catchment Area for public water supply. For most of its length, the M-Canal runs through Grassy Waters. The City generally maintains the water level in the M-Canal below the elevation of Grassy Waters so water in the canal will not flow into Grassy Waters. However, on some occasions, water flows from the M-Canal into Grassy Waters. High phosphorus concentrations have been recorded in the M-Canal; as high as 300 ppb. Nuisance vegetation is growing in the area where the M-Canal connects to the Water Catchment Area. The preponderance of the evidence establishes that the adverse impacts described by the City’s experts in the area of the Ibis Preserve outfall are caused primarily by discharges from Ibis Preserve. There are three other developments adjacent to Grassy Waters that occasionally discharge to Grassy Waters. These discharges are likely to contain some nutrients, but the amount of nutrients and their effects, if any, on Grassy Waters were not described in the record. The Water Catchment Area is a Class I waterbody because it is used for public water supply. The water quality standard for phosphorus and other nutrients in a Class I waterbody is set forth in Florida Administrative Code Rule 62-302.530(48)(b): In no case shall nutrient concentrations of a body of water be altered so as to cause an imbalance in natural populations of aquatic flora or fauna. Grassy Waters was designated by the Department of Environmental Protection (“DEP”) as a stream. Rule 62-302.531(2)(c) states that the narrative criterion “shall be interpreted as being achieved in a stream segment where information on chlorophyll a levels, algal mats or blooms, nuisance macrophyte growth, and changes in algal species composition indicates there are no imbalances in flora or fauna.” The City presented some evidence regarding nuisance macrophyte growth and changes in algal species composition in Grassy Waters near the Ibis Preserve outfall. Little evidence was presented regarding the practice of DEP or the District in the application of the narrative nutrient standard, but the preponderance of the evidence indicates the agency practice is to consider a stream segment as a whole to determine whether it exhibits an imbalance in natural populations of aquatic flora and fauna.2/ During the course of this proceeding, the District issued administrative complaints against the Improvement District and the City, which include Orders for Corrective Action. The complaints were issued pursuant to section 373.119, Florida Statutes, which authorizes such action when a water management district believes that a violation of any provision of chapter 373 or district rule has occurred. However, at the final hearing, the District was reluctant to say the Improvement District had violated any law or permit condition. The Improvement District did not challenge the enforcement action against it and, therefore, the District’s enforcement order became final. The Improvement District is required to address the accumulation of sediment in the Ibis Lakes, develop a nutrient source control plan, eliminate and reduce the use of herbicides containing copper sulfate, and reassess pumping schedules. There is no target nutrient limit specified in the District’s Orders for Corrective Action. The District’s enforcement action against the City seeks to require the City to increase secondary treatment and retention in Ibis Preserve, provide a plan to remove the exotic/invasive vegetation at the outfall, provide a vegetation monitoring plan, and develop source control measures for residential developments that discharge into Grassy Waters. The City challenged the enforcement action and it remains pending. Snail Kites The Everglades snail kite gets its name from its primary food, the apple snail. In the Everglades, snail kites also feed on an exotic island snail, which occurs there in about equal numbers as apple snails. There was no evidence presented that there are exotic island snails in Grassy Waters. Snail kite habitat is dependent on conditions conducive to apple snails, which are the open marsh and oligotrophic conditions where periphyton flourish. If a sufficient number of apple snails are present, snail kites will find suitable nesting nearby. Dense wetland vegetation is not good forage for snail kites because, even if apple snails are present, the apple snails will be difficult or impossible for the snail kites to see. Dr. Welch, who was the state snail kite conservation coordinator at the Florida Fish and Wildlife Conservation Commission and wrote the snail kite management plan for Florida, testified for the District, where he is now employed as a senior scientist. He said field surveys of snail kite nests in Grassy Waters indicate their numbers are relatively low compared to other areas where snail kites are found. There were only ten successful nests (eggs laid) observed from 2000 to 2016. The City’s Everglades expert, Dr. Lodge, speculated that the low nest counts could be due to difficulty in seeing the nests, but he was not familiar with the survey techniques used and, therefore, his opinion that the numbers could be materially underestimated is not credited. Snail kites nest throughout the Water Catchment Area, but primarily in the open marsh areas of the central and eastern portions of the Water Catchment Area. Over 90 percent of snail kite nests are more than a mile from the Project ROW. Dr. Lodge said there are four snail kite nests within 800 feet of the Project, but he was not more specific about their locations. Most nests are closer to Northlake Boulevard, State Road 710, and the Florida Turnpike. The major factor that adversely affects successful nesting by snail kites and production of offspring is predation, usually by raccoons and rat snakes. “Cold snaps” and drought are also factors. Impacts of The Proposed Project Water Quantity Impacts Water storage for the Project, which was going to be handled in the Ibis system under the 1989 Ibis permit, would be provided in the roadside swales. The Project is designed to retain water volumes greater than typically required for roadways. Stormwater would not flow out of the Project into the Ibis system except in unusually large storm events, in excess of six inches of rainfall. The City did not dispute the Project’s compliance with the applicable water quantity criteria in the District rules. Water Quality Impacts To address the City’s concerns about adverse impacts caused by the Ibis system, the Applicants expanded the roadside swales by ten feet and raised the outfall elevation by 0.05 feet. With these modifications, the Project would provide water quality treatment for its stormwater and no longer rely on the Ibis system for treatment. The swales would provide treatment in excess of the treatment required by District rules. Respondents contend that, when the treatment provided by the Ibis system is added, the total treatment provided for the Project stormwater is more than twice as much as required by District rules. The City, on the other hand, claims that no additional water quality treatment can be provided by the Ibis system because the Ibis Lakes are eutrophic. The preponderance of the evidence supports a finding that Project runoff to the Ibis system would receive additional water quality treatment in the Ibis system and in Ibis Preserve before flowing to Grassy Waters. The effect of the Project’s on-site treatment of its stormwater is that the amount of nutrients that would otherwise flow into the Ibis system from SR 7 would be reduced. Therefore, the effect of the Project is to reduce the nutrient load that the Improvement District was permitted to discharge to Ibis Preserve and Grassy Waters. The City did not dispute the Applicants’ evidence that the Project exceeds the District’s design criteria for water quality. The City focused instead on its contention that, despite its compliance with water quality design criteria, the Project would result in additional nutrient loading to Grassy Waters, which would cause additional adverse impacts to its flora and fauna. The Applicants and the City performed nutrient loading analyses even though such analyses are only required by the District when the receiving waters have been designated by the Department as “impaired” by nutrients or in the case of certain other specially designated waters. Grassy Waters does not have any of these special designations. The Applicants’ nutrient loading analysis concluded that the post-development loading of phosphorus and nitrogen from the Ibis system would be less than the pre-development condition, so there would be a net decrease in nutrients discharged into Grassy Waters. Petitioner’s expert witness, Dr. Harper, believes the Project would increase nutrient loading to Grassy Waters, even if stormwater from the Project did not carry additional nutrients, because the increased volume of water moving through the Ibis system would entrain more nutrients from sediments in the Ibis lakes. Dr. Harper believes the Project would also cause nutrient loading via groundwater seepage through the roadway swales into Grassy Waters. The preponderance of the evidence does not support his opinion that groundwater seepage would cause additional nutrient loading.3/ Dr. Harper believes another source of nutrient loading from the Project would be from surface flow down the roadway embankments. On the eastern embankment, this flow would enter the mitigation area 150 feet from Grassy Waters. Dr. Harper’s estimated total loading from all sources is not persuasive. The estimate gives a false sense of precision. It is based on a number of variable assumptions, some of which are not widely known or in use by experts in the field. In addition, Dr. Harper’s opinion did not appear to appropriately account for the modifications to the Project’s storage capacity. Dr. Harper’s estimated loading was not translated into physical effects in Grassy Waters. The Applicants’ estimate of total nutrient loading also gives a false sense of precision, but it is based on a well-known and widely used methodology. The City failed to prove that the Project would result in more nutrient loading to Grassy Waters than is currently contributed by the ROW. Because the Project would not rely on the Ibis system for stormwater treatment, the Project would reduce the loading that the Improvement District was permitted to discharge to Grassy Waters. To address potential vehicular spills into Grassy Waters, FDOT produced a Spill Response Plan. The swales would capture and contain any material spilled on the roadway or swale. The curb and gutter, a guardrail, gravity wall, and fence also provide protection against spills. The bridge over the M-Canal would use a 54-inch traffic barrier, which is higher than FDOT specifications for the design speed for the bridge. The City did not present evidence to show that the protective measures proposed by the Applicants are less than what is usually considered adequate under similar circumstances, or fails to meet a relevant safety standard. Wetland Impacts Direct Impacts The Project would directly impact 52.37 acres of wetlands and 7.86 acres of surface waters. The impacted wetlands are fresh water marsh, mixed shrubs, and hydric pine flatwoods. The surface waters affected consist of vegetated ditches and un- vegetated channels or canals. The impacted wetlands include 11.77 acres of freshwater marsh. The impacted surface waters are ditches. Most of these wetlands are disturbed and their functional values have been reduced. Secondary Impacts District rules require an applicant to account for the secondary impacts caused by a project that could adversely affect the functions of adjacent wetlands or other surface waters. The Applicant’s Handbook defines secondary impacts to include impacts on wetland functions, water quality, and endangered species, including impacts on areas needed by endangered species for foraging. Part of the Applicants’ assessment of secondary impacts of the Project was made by reviewing the effects of the Acreage Reliever Road on Pond Cypress Preserve, a 1,737-acre conservation area managed by the County that is immediately south of the proposed Project. The County has been monitoring the effect of the Acreage Reliever Road on hydrology, vegetation, and species compensation ever since the road was built. The County found no adverse secondary impacts caused by the road. The species that use the wetlands near the road, including wading birds, appear to be unaffected by the road. The scoring of secondary impacts for the Projects, using the Uniform Mitigation Assessment Methodology (“UMAM”), was conservative, meaning that assumptions were made at the high side of the potential range of impacts. This resulted in more mitigation being required. The Applicants claim the Project would “maintain a 300-foot buffer between the project’s construction boundary and [Grassy Waters].” This appears to be a misstatement. The Applicants’ combined ROW is only 320 feet wide. Going east from the limits of construction, it is 160 feet to Grassy Waters. The Project’s buffer is 160 feet wide. The District accounted for secondary impacts to wetland dependent species, including snail kites, from noise and lights that might discourage use of the area. The Project would provide a tree buffer that will reduce noise and light impacts to Grassy Waters. The roadway lighting plan is also intended to reduce light penetration into Grassy Waters. Most of the threatened and endangered bird species are tolerant of roadways for foraging and roosting, but not for nesting. Section 10.2.7 requires the Applicants to provide reasonable assurances that any future phase of a project or project-related activities will not result in adverse impacts to the functions of wetlands or water quality violations. The Applicants satisfied this requirement by releasing of FDOT ROW north and south of the Project. Cumulative Impacts An applicant must provide reasonable assurance that a regulated activity will not cause unacceptable cumulative impacts upon wetlands and other surface waters within the same drainage basin as the regulated activity for which a permit is sought. Some of the proposed mitigation for the Project is out- of-basin. If an applicant proposes to mitigate impacts in another drainage basin, District rules require consideration of factors such as “connectivity of waters, hydrology, habitat range of affected species, and water quality” to determine whether there are unacceptable cumulative impacts. The Project is located in the eastern Palm Beach County Basin, which has approximately 21,000 acres of wetlands. About 89 percent of the wetlands in the basin are publicly-owned conservation lands, which means their wetland functions will continue into the future. The cumulative impact analysis was conservative, meaning that the actual impacts are likely to be fewer. Petitioner contends that Respondents’ cumulative impact analysis did not account for the unique nature of the Grassy Waters ecosystem as the only remaining low nutrient oligotrophic wetland in the region. The preponderance of the evidence shows that the historical wetland types in the Project area were not all like the open marsh found in the central and eastern portion of Grassy Waters. Respondents accounted for the loss of open water marsh that would be caused by the Project. On-Site Mitigation There would be 52.4 acres of on-site mitigation within a 160-foot-wide strip of land along the eastern limits of proposed construction. This area of the ROW would be managed by removing or treating the exotic vegetation, such as Brazilian Pepper and Maleleuca. Removing the exotic vegetation seed source would prevent further spread of these nuisance species into Grassy Waters. Where native habitats have been altered with ditches and berms, the land would be graded to create a slope from the limits of construction eastward to the edge of the ROW. The eastern elevation would be similar to the adjacent marsh or hydric pine areas of Grassy Waters. Then, native vegetation would be planted. The habitats enhanced, restored, or created would include freshwater marsh, hydric pine flatwoods and mixed forested wetlands, including cypress. The planting of mixed, forested species would provide sound and light buffering for snail kites and other species in Grassy Waters. Two wildlife passages would be created underneath the Project with fencing designed to direct wildlife to use the wildlife passages. Slats would be placed in the roadway fencing to prevent small animals from going through the fence and onto the roadway. The on-site mitigation was scored using UMAM and determined to result in functional gain. The UMAM analysis was conservative, meaning that the actual functional gain is likely to be greater. The City did not contest the UMAM scoring. Off-site Mitigation FDOT is applying mitigation credits from 210 acres at the Pine Glades Natural Area (“Pine Glades”) to offset impacts to 15.7 acres of herbaceous marsh and 26.78 acres of forested wetland impacts. Pine Glades is a regional off-site mitigation area located in the Loxahatchee River Basin and is owned and operated by Palm Beach County. Pine Glades consists of a mix of wet prairie, depression marshes, hydric pine flatwoods, and mesic flatwoods. The restoration work in Pine Glades has already been completed. Pines Glades implements a detailed management plan that provides regional ecological value. Robbins testified that Pine Glades has similar habitats to Grassy Waters. Pine Glades has periphyton, apple snails, snail kites, wood storks, and sand hill cranes. Pine Glades has some areas with oligotrophic conditions. Additional off-site mitigation to offset 52 acres of wetland impacts caused by the Project would be provided at the DuPuis Reserve (“DuPuis”). DuPuis is a regional off-site mitigation area located between the L-8 Canal and the C-44 Canal in western Palm Beach and Martin Counties, and is owned and operated by the District. DuPuis would provide mitigation with 34.71 acres of herbaceous wetlands and 43.8 acres of forested wetlands. DuPuis is appropriate to offset the impacts associated with the Project because it provides similar habitats with similar values of functions for similar wildlife. DuPuis implements a detailed management plan that provides regional ecological value. The City argues that there is little similarity between the Grassy Waters ecosystem and Pine Glades or DuPuis, so the mitigation there cannot offset the unique assemblage of plants and animals that would be lost in Grassy Waters. It is unnecessary for Pine Glades and DuPuis to be dominated by open water marshes like Grassy Waters. It is only necessary that they have some of these areas to offset Project impacts to open water marsh. Proposed snail kite mitigation would provide 52.5 more acres of snail kite habitat than would be directly impacted by the Project. The mitigation for snail kites will be located in FDOT ROW adjacent to the Project, south of the M-Canal, and north of Northlake Blvd. Erwin expressed concern about fragmentation of the ecosystems that would be caused by the Project. The areas that would be affected by the Project have already been fragmented by berms, ditches, and fences. Grassy Waters is surrounded by berms, a canal, and highways. The Project would cause fragmentation, like all roads. However, the fragmentation was reduced where practicable, and the City did not show that the roadway would cause the loss of any significant “greenway” now used by wildlife. Snail Kite Impacts Section 10.2.2(a) requires an applicant to provide reasonable assurances that a proposed activity would not impact wetlands and other surface waters so as to reduce the abundance and diversity of listed species. Snail kites, wood storks, sandhill cranes, white ibises, and little blue herons are listed species that have been observed within the Project corridor. As explained in the Conclusions of Law, the UMAM process is designed to mitigate for wetland functional losses, not snail kite functional losses. However, the potential impact to any listed species warrants close attention to the issue of whether function-for-function wetland mitigation would be provided. There will be 11.5 acres of direct impacts to snail kite habitat within the footprint of the Project area. Dr. Welch believes secondary impacts to wetland functions associated with snail kites could extend 800 feet east of the ROW. Mitigation for snail kites would be located in the Rangeline corridor south of the M-Canal and north of Northlake Boulevard. Dr. Welch estimated there were about 64 acres of snail kite habitat in the Rangeline corridor similar to the 11.5 acres of habitat located in the Project footprint. Dr. Welch conceded that he has no evidence that snail kites currently use the Rangeline, but he believes the habitat is suitable and is appropriate mitigation. Petitioner claims there are studies of “similar birds” indicating that snail kites avoid highways due to noise. However, the studies were not of similar birds. More weight is given to Dr. Welch’s testimony that snail kites are not particularly sensitive to roadway noise. Dr. Welch stated that Pine Glades would likely have value for snail kites because it is near the Hungryland Wildlife Management Area, which has the same number of successful snail kite nests as Grassy Waters. The City contends that Pine Glades is too far away from Grassy Waters to mitigate Project impacts to snail kites. However, snail kites range long distances to forage; several hundred miles in a few days. Satellite telemetry of snail kites shows snail kites from Grassy Waters are using Pine Glades for feeding. Dr. Welch reviewed snail kite nesting data to determine whether roads deterred nesting and found that snail kites frequently nested within 500 feet of major roadways. Dr. Welch refuted the idea that Grassy Waters provided snail kite refuge during drought conditions, because Grassy Waters is also subject to drought conditions that adversely affect snail kites. There are conditions in the permit to limit potential impacts to snail kites during construction of the Project. If snail kite nesting is observed within 1,640 feet of construction, all Project construction must cease. Thereafter, monitoring of the nest and notification of the U.S. Fish and Wildlife Service is required. Construction cannot resume until that nest has been considered finished. FDOT would place a conservation easement over 82.6 acres in the FDOT ROW between Okeechobee Boulevard and the M-Canal, south of the Project area that is the subject of this proceeding. The conservation easement would maintain connectivity between the Pond Cypress Natural Area and Grassy Waters and ensure that no future southern extension of the roadway will be constructed. A conservation easement would be placed on the FDOT ROW between Northlake Boulevard and SR 710, an area of approximately 43.5 acres. Preserving this area protects a hydrologic connection between Loxahatchee Slough Natural Area and Grassy Waters. It also ensures no future northern extension of the roadway. A conservation easement would be placed on a portion of the FDOT ROW between SR 710 and Jupiter Farms, an area of 44.5 acres. This section of ROW is in the Loxahatchee Slough and the release of the ROW would be a direct benefit to Loxahatchee Slough. The preservation of these areas would benefit fishing and recreational values in the Pond Cypress Natural Area, Grassy Waters, and the Loxahatchee Slough Natural Area. These conservation areas did not receive UMAM credits to reduce the wetland acreage needed to offset wetland functional losses, but they were included in the mitigation credit for benefits to snail kites and other wildlife. Summary The preponderance of the evidence established that the proposed mitigation offsets the impacts to wetlands and other surface waters that would be caused by the Project and exceeds the requirements of District rules. Practicable Design Modifications District rules require an applicant to consider alternatives that would avoid or reduce wetland impacts. The City claims the Applicants failed to comply with this rule because FDOT selected a roadway corridor that was expected to have greater environmental impacts than some of the other three corridors that were being considered. As explained in the Conclusions of Law, this argument is misplaced. The District’s review of the Applicants’ measures to avoid or minimize wetland impacts was appropriately confined to Corridor 3, the corridor selected by FDOT where the Project is proposed. The Applicants reduced and eliminated impacts of the Project in several ways. For example, the footprint of the road was narrowed from six lanes to four lanes, wildlife underpasses were provided, retaining walls were used to narrow stormwater features, the median was reduced in size, and the design speed limit was reduced for the bridge at the M-Canal crossing. Under two circumstances, District rules allow an applicant to avoid the requirement to implement practicable design modifications to reduce or eliminate wetland impacts, which are referred to as the “opt-out” provisions. Section 10.2.1.2, Volume I, of the Applicant’s Handbook (“A.H.”) provides: The ecological value of the functions provided by the area of wetland or other surface water to be adversely affected is low, based on a site specific analysis using the factors in section 10.2.2.3, below, and the proposed mitigation will provide greater long term ecological value than the area of wetland or other surface water to be adversely affected, or The applicant proposes mitigation that implements all or part of a plan that provides regional ecological value and that provides greater long term ecological value than the area of wetland or other surface water to be adversely affected. The District determined that the Applicants meet both tests. The preponderance of the evidence supports the District’s determination. The ecological value of the functions provided by the affected wetlands and surface is low and the proposed mitigation would provide greater long-term ecological value than the area being impacted. Pine Glades and DuPuis are part of a plan to restore the ecological value of Northern Palm Beach County and create an “ocean to lake” system of preserves and natural areas.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the South Florida Water Management District enter a final order approving Permit Number 50-05422-P on the terms and conditions set forth in the amended Staff Report, and the complete application for the Permit. DONE AND ENTERED this 31st day of March, 2017, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER 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 31st day of March, 2017.
The Issue Whether the activities conducted on respondent's property required a dredge/fill permit and whether respondent violated the conditions of the permit issued on February 15, 1985.
Findings Of Fact Respondent is the record holder of a parcel of land located within Section 35, Township 45, South, Range 21 East, in Lee County, Florida. Respondent's property is contiguous to Pine Island Sound, a Class II, Outstanding Florida Water. Maureen Powers, an Environmental Specialist with the Department initially inspected respondent's property on May 23, 1984, after the Department received an anonymous complaint that someone was clearing away mangroves on the property. Ms. Powers-discovered that an earthen-fill road had been constructed on the property, and a portion of the road, 24' x 43'; was located within the landward extent of the state's waters. The determination that the portion of the road was within the Department's jurisdiction was based on the dominance of black and white mangroves. There had been recent mangrove cutting in the area, and a pile of vegetative debris, the result of the cutting, had been placed in the jurisdictional wetlands contiguous to Pine Island Sound. On June 1, 1984, Ms. Powers met with respondent in Langley Adair's office to discuss the violations observed on May 23, 1984, and to discuss the resolution of these violations. Respondent agreed to remove all of the earthen fill and vegetative debris that he had deposited within the jurisdictional wetlands. He agreed to refrain from any further work within the jurisdictional area prior to receiving a permit from the department. He also agreed to open up a flow channel in the berm along Pine Island Sound to restore circulation to the area. On July 11, 1984, Ms. Powers conducted an on-site inspection and discovered that the vegetative debris and the fill material had not been removed. Further, it was apparent that respondent's proposed home site, outlined by string and stakes, was submerged and directly connected by water to Pine Island Sound. The water standing on the property covered a portion of the fill area. On August 8, 1984, another inspection was performed, and it was discovered that respondent still had not removed the fill materials. The condition of the property was essentially the same as it had been on July 11, 1984. By letter dated August 20, 1984, respondent was again notified of the violations and reminded that he had agreed on June 1, 1984, to remove the vegetative and earthen fill. Respondent was informed that he needed to remove the fill materials within 30 days of receipt of the letter in order to avoid further enforcement action. On September 5, 1984, Ms. Powers again inspected the property and found that the proposed homesite and a portion of the fill were still submerged, that the water connected directly with Pine Island Sound and the fill materials had not been removed. Also apparent was a flume of milky white water which originated at the toe of the fill and continued into Pine Island Sound. Water samples were taken which revealed that the erosion of the unauthorized fill was resulting in a violation of state surface water quality criteria, specifically, turbidity1 greater than 29 Nephelometric Turbidity Units above natural background. The background sample, taken upstream from the site of the discharge, had a value of 5.2 turbidity units. The water sample taken two feet from the toe of the fill had a value of 69 turbidity units, and the sample from Pine Island Sound waterward of the mangrove fringe had a value of 46 turbidity units. On October 9, 1984, a letter was sent to respondent which pointed out that the earthen and vegetative fill had not been removed and notifying respondent that erosion of the earthen fill into the waters of Pine Island Sound had resulted in violation of surface water quality criteria. Respondent was requested to immediately cease and desist from all unauthorized. activity under the Department's jurisdiction. To clarify the situation, original photos of the site were sent with the letter which showed the earthen fill, the vegetative debris, and the turbid water leaving the site. A diagram of the site was also included to show the location fill materials that were to have been removed. On October 25, 1984, Ms. Powers met with Mr. Decker at the site. Ms. Powers showed respondent the earthen fill and vegetative debris that should have been removed. Ms. Powers noted that the waterward 23' x 24' section of the earthen fill had become heavily colonized by black mangrove seedings and, therefore, excepted that portion of the fill from the removal requirement so that the seedlings would not be disturbed. Mr. Decker stated that he would remove the unauthorized fill within two weeks. Meanwhile, apparently in September, respondent had submitted a permit application. Mr. Beaver was the field inspector assigned by DER to evaluate the application and make a recommendation on the feasibility of the project to the dredge and fill supervisor. On October 8, 1984, Mr. Beaver performed the field inspection at the site, and on October 23, 1984, issued his permit application appraisal recommending that the application be denied. Mr. Beaver recommended that the project be reconsidered for a permit if, among other things, the house site were removed from the landward extent of the state waters and located in the uplands, the septic tank were removed from the low lying portions of the site, and previously cut areas were allowed to regrow in native vegetation. On November 15, 1984, Mr. Beaver met with Mr. Decker and Mr. Cantrell, the district supervisor of dredge and fill, to discuss the project. Mr. Cantrell asked how the project could be modified so that Mr. Decker could have his house in the location where he wanted it. Mr. Beaver suggested a stilt, elevated house with a small fill pad that would allow access to the entrance of the house. The house would have to be elevated -enough so that revegetation of wetland plants could occur underneath the house structure and water flow could be maintained. On November 19, 1984, Ms. Powers and Mr. Beaver met Mr. Decker at the property. Ms. Powers and Mr. Beaver staked the DER jurisdiction line and marked the proposed location of Mr. Decker's boardwalk. Mr. Decker asked about placing wood chip mulch on the wetlands on his property in order to beautify the area. Mr. Decker was informed that wood chip mulch was considered vegetative fill and would require modification of his permit application. Subsequent to the meeting of November 15 and the on- site inspection of November 19, Mr. Decker modified his project. However, wood chip mulch was not mentioned. On December 7, 1984, Mr. Beaver recommended that the application be approved subject to specified conditions, which were ultimately incorporated into the permit. On December 11, 1984, Ms. Powers inspected the site and discovered that a large pile of wood chips had been placed on the northeast end of the fill road waterward of the jurisdiction line. The vegetative debris and earthen fill that had previously been on the project had not been removed. Respondent was notified of the violations by a Cease and Desist letter dated January 4, 1985. The letter pointed out that respondent had been told specifically that wood chip mulch was considered vegetative fill and that dredge/fill permit would be required prior to the placement of any fill material. On February 5, 1984, respondent met with DER, officials to discuss the violations. Mr. Decker stated that the fill had been removed as requested. The Department informed Mr. Decker that an inspection would be performed and, if the fill had not been removed, the Department would pursue formal enforcement action. On February 7, 1985, the site was inspected none of the fill material had been removed. A subsequent inspection on February 20, 1985, revealed that the wood chips had been spread throughout the jurisdictional wetlands. On February 15, 1985, respondent received a permit to fill and to construct a dock and boardwalk. The specific conditions of the permit include the following: 2. A 20' x 16' - 4" fill pad shall be the only fill placed waterward of the jurisdictional line. This fill pad will be composed of clean sand and have the banks stabilized by a riprap revetment with a slope not greater than 2H:1V. * * * The house and all associated structures shall be built upon stilts with concrete footings and/or wooden pilings. On-site turbidity control devices shall be installed and properly maintained to localize turbidity impacts to the construction area. * * * All vegetative debris, trash and spoil material resulting from concrete footing placement shall be removed from the landward extent of State Waters as defined by the jurisdiction line staked by the DER. Upon completion of construction, non- filled areas beneath the stilt house and associated structures shall be returned to original grade if they were altered by construction. Wetland vegetation shall be planted in the previously cleared area and mangroves removed by construction activities shall be replaced on a 2 for 1 basis with 80% survival over a three year period. * * * 11. The project shall comply with applicable State Water Quality Standards, namely: 17-3.051 - Minimum Criteria for All Waters at All Times and All Places. 17-3.061 - Surface Waters: General Criteria 17-3.111 - Criteria - Class II Waters Shellfish Propagation or Harvesting, Surface Waters General Conditions 2 and 5 of the permit provide: 2. This permit is valid only for the specific processes and operation applied for and indicated in the approved drawings or exhibits. Any unauthorized deviation from the approved drawings, exhibits, specifications, or conditions of this permit may constitute grounds for 81' filled area was located within the landward extent of the state waters. 19. Respondent has violated several conditions of the permit issued February 15, 1985. Specific Condition #2 provided that the 20' x 16' fill pad would be "the only fill placed waterward of the jurisdictional line." Instead, respondent filled an area approximately 78' x 81' to an average height of about 2\', totaling approximately 585 cubic yards of fill. The fill was non-native fill brought onto the site. The permit did not authorize fill for a septic tank in the revocation and enforcement action by the department. 5. This permit does not relieve the permittee from liability for harm or injury to human health or welfare, animal, plant or aquatic life or property and penalties therefor caused by the construction or operation of this permitted source, nor does it allow the permittee to cause pollution in contravention of Florida Statutes and department rules, unless specifically authorized by an order from the department. On March 19, 1985, an inspection of the property revealed that Mr. Decker had totally ignored the conditions of his permit. Rather than a fill pad of 20' x 16', respondent had filled an area approximately 78' x 81'.2 The fill was unstabilized, and no turbidity control devices were in place. Fill material had been used to construct a earthen berm across a natural flow channel, blocking the flow of water onto the property. Further, the vegetative debris resulting from the construction of the boardwalk had been deposited in the mangrove wetlands. On March 22, 1985, a Notice of Violation and. Orders for Corrective Action was sent to the respondent. Respondent received the notice on or about March 26, 1985. The landward extent of the state waters on respondent's property, the area in which a DER permit is required for dredging and filing, was determined by the presence of red mangroves (Rhizophora mangle), black mangroves (Avicennia germinans), and saltwort (Basis maritime) as the dominant species. The jurisdiction line was originally staked on November 19, 1984, and was reestablished on April 23, 1985, from remaining landmarks, due to the original markers being removed. The 78' x81' filled area was located within the landward extent of the state waters. Respondent has violated several conditions of the permit issued February 15, 1985. Specific Condition #2 provided that the 20' x 16' fill pad would be "the only fill placed waterward of the jurisdictional line." Instead, respondent filled an area approximately 78' x 81' to an average height of about 21/2', totaling approximately 585 cubic yards of fill. The fill was non-native fill brought onto the site. The permit did not authorize fill for a septic tank in the jurisdictional wetlands, but respondent placed a septic tank and drainfield in that area.3 By filling an area several times the size of the area authorized, respondent has seriously violated the conditions of the permit. A fill area of the size that now exists eliminates the habitat and water quality functions that the area historically performed. Respondent has violated Specific Condition #4, which required that the house and associated structures be built on stilts. The purpose of such a requirement is to preserve undisturbed the existing substrate, which constitutes the base of the food chain, and to allow for a free flow of water across the site, which is essential to the health of the mangrove system. Respondent not only filled an area larger than his proposed house, he poured a solid, continuous, concrete foundation on top of the fill, which would prevent the flow of water should the water rise high enough to come onto the filled area.4 By filling the area, destroying the substrate, and preventing the flow of water into the area, respondent has violated Specific Condition #4 of the permit. Respondent violated Specific Condition #5 of his permit in that respondent failed to install any turbidity control devices. Turbidity control devices of some sort are necessary in a fill area such as the one in this case. Turbidity screens or staked hay bales could have been used. Respondent also violated Specific Condition #8. Construction debris and vegetative debris were located throughout the area. Although respondent technically has not violated Specific Condition #9, in that it requires acts to be performed "upon completion of construction", respondent has made compliance with that provision an impossibility because he has filled the "non- filled areas beneath the stilt house" and therefore there are no "non-filled areas" to return to original grade. Respondent has never requested that his permit conditions and requirements be modified. By his actions, respondent has repeatedly shown a complete disregard for the requirements of the law, and he has totally ignored the conditions set forth in the permit. Mr. Decker was not qualified as an expert and I did not find him to be a credible witness. The reasonable costs and expenses incurred by the Department in relation to the enforcement aspects of this action are $866.17. These costs and expenses were incurred by the Department in its effort to control and abate pollutants and to restore the waters and property of the state to their former condition.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the respondent's permit, number 360902245, be revoked that the respondent be ordered to make payment to the Department in the amount of $866.17 for costs and expenses incurred by the state and that the following corrective action be ordered: Respondent shall within thirty (30) days, remove all unauthorized fill material placed within the area of Department jurisdiction. Prior to initiating the fill removal respondent shall arrange for Department personnel to stake the area to be restored. All areas shall be restored to the elevation and soil conditions which existed prior to the placement of fill material. Respondent shall take all necessary precautions to ensure that state water quality standards are not violated during the restoration work. Respondent shall not disturb adjacent areas within the jurisdiction of the Department unless approved by the Department in writing. DONE and ENTERED this a 24th day of January, 1986, in Tallahassee, Leon County, Florida. DIANE A. GRUBBS Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 FILED with the Clerk of the Division of Administrative Hearings this 24th day of January, 1986.
The Issue The issues to be determined in this proceeding are: whether the challengers have standing; and (2) whether Proposed Rule 40E-8.221(2) is an invalid exercise of delegated legislative authority.
Findings Of Fact Based on the parties' stipulations and the evidence adduced at the final hearing, the following findings of fact are made: The Parties The District is a government entity existing and operating pursuant to chapter 373, Florida Statutes, as a multi- purpose water management district. The District has the power and duty to adopt MFLs consistent with the provisions of part I of chapter 373. Sanibel is a barrier island sanctuary in Lee County and a duly-formed municipality with a population of more than 6,000. Sanibel is situated at the mouth of the Caloosahatchee River, within the Caloosahatchee's greater estuarine area. Sanibel is known primarily for its natural beauty, including clear blue waters, shell beaches, world-class sport fisheries, and wildlife refuges. That is why tourists come from around the globe to visit Sanibel, and why Sanibel's residents move and remain there. Sanibel actively participated in the rulemaking process for the Proposed Rule from its inception. Sanibel submitted two technical comment letters to the District during the development of the Proposed Rule. Sanibel's natural resources director, James Evans, attended numerous public and technical meetings associated with the development of the Proposed Rule, speaking on the record at each of the public meetings prior to the adoption hearing by the District's governing board. The Town, located on Estero Island in Lee County, is also a barrier island community and duly-formed municipality with a population of more than 6,000. The Town is situated just south of the mouth of the Caloosahatchee River and on the southeastern edge of the Caloosahatchee River's greater estuarine area. The Town is known primarily for its natural beauty, including clear blue waters, shell beaches, world-class sport fisheries, and wildlife refuges. Cape Coral is a duly-formed municipality in Lee County and is the largest city between Tampa and Miami, with a population in excess of 150,000. Cape Coral is bordered on the south by the Caloosahatchee River and has over 400 miles of navigable canals and waterways, all of which are within the Caloosahatchee River's greater estuarine area. In addition, Cape Coral has an assigned load reduction allocation under the Basin Management Action Plan (BMAP) for the Caloosahatchee River Estuary (CRE) due to it being designated as impaired for dissolved oxygen and nutrients. Maintaining sufficient flow in the Caloosahatchee River would have a direct impact on Cape Coral's ability to meet its assigned load reduction allocation. In addition to living on or near the water, a substantial number of the residents of Sanibel, Cape Coral, and the Town engage in water-based recreational activities such as swimming, fishing, boating, kayaking, paddle boarding, bird watching, and nature observation in and around the Caloosahatchee River's greater estuarine area. Fort Myers is a duly-formed municipality in Lee County and has a population of approximately 80,000. Fort Myers is bordered by the CRE throughout its entire jurisdictional boundary. Fort Myers owns and maintains a yacht basin (Ft. Myers Yacht Basin), which includes a mooring field and an anchorage field in the Caloosahatchee River. Fort Myers presented testimony that commercial crabbing and recreational fishing have declined and that it has suffered economic harm due to water quality issues. Fort Myers owns the submerged land in the Caloosahatchee River from Marker 39 to Marker 58, and islands in the river. One such island will be used as a park for recreational activities such as canoeing, kayaking, and hiking for visitors to enjoy the Caloosahatchee River. Fort Myers also owns and operates piers and a public boat ramp within the Caloosahatchee River. Fort Myers' dock master has observed declines in seagrasses in the Caloosahatchee River during his 19-year career working at the Ft. Myers Yacht Basin. Fort Myers has adopted a Harbor Management Plan for the management of its mooring and anchorage fields in the Caloosahatchee River. Fort Myers has also been assigned a load reduction allocation under the BMAP for the CRE, and is responsible for a certain amount of pollution reduction over time. Bonita Springs is a municipality of more than 50,000 in Lee County. The borders of Bonita Springs include portions of Estero Bay, which, along with San Carlos Bay and the Caloosahatchee River, is part of the greater Lower Charlotte Harbor Estuary. Bonita Springs includes wildlife refuges, such as the Estero Bay Aquatic Preserve and Lovers Key State Park and Recreation Area. While Bonita Springs' strategic priorities include environmental protection and water quality, it does not have environmental staff or test water quality. Bonita Springs participates in Estero Bay Management and the Charlotte Harbor National Estuary Program (CHNEP). Bonita Springs provides financial assistance to the Caloosahatchee Citizen Sea Grass Gardening Project. Concerns regarding harm to the CRE and tape grasses are shared by a significant number of residents in Bonita Springs and Estero, including injury to the quality of life and recreational uses such as swimming, boating, and kayaking in the waterways. Estero is a municipality of more than 30,000 in Lee County. Estero borders the eastern portion of Estero Bay. Estero includes wildlife refuges, such as Estero Bay Aquatic Preserve and Koreshan State Park. While Estero has environmental policies, it does not have environmental staff or test water quality. Estero makes financial contributions to CHNEP. Estero is concerned that the Proposed Rule will affect its water quality, which could affect its residents' quality of life. Estero believes it could be harmed by poor water quality because its residents are portable retirees who can move away, or tourists who can choose not to visit. Captiva Island is situated at the mouth of the Caloosahatchee River, within the Caloosahatchee's greater estuarine area. CCP is a Florida not-for-profit corporation representing property owners, businesses, and the community of Captiva Island. Captiva Island is part of unincorporated Lee County and is located north of Sanibel. CCP has 200 financial contributors comprised of property owners, businesses, and residents on Captiva Island. CCP's mission includes protection of clean off-shore water, diverse and healthy marine life, and robust native vegetation along with the protection of mangrove fringe and water quality. CCP works with Lee County on provisions of the County's comprehensive plan, which include the quality of adjacent waters. CCP relied on the expertise of James Evans, the director of natural resources for Sanibel, and on the Sanibel- Captiva Conservation Foundation (SCCF). CCP was advised that the Proposed Rule was not sufficient to protect the environment and Vallisneria americana (Vallisneria) or tape grass during the dry season. Caloosahatchee River and Estuary The watershed of the Caloosahatchee River covers approximately 861,058 acres. The watershed consists of four sub-watersheds, three of which are upstream of the S-79 structure. The Tidal Caloosahatchee Basin sub-watershed (estuarine system) is downstream of the S-79 structure. The S-79 structure captures all the upstream discharges of fresh water that go into the estuarine system through the S-79 structure. Major tidal tributaries of the Tidal Caloosahatchee Basin are the Orange River and Telegraph Creek, which drain into the upper estuary downstream of the S-79 structure. Fresh water inflows from these and other tributaries also contribute fresh water into the estuarine system. The Caloosahatchee River was originally a natural watercourse running from its origin at Lake Flirt to San Carlos Bay. It is currently defined as the "surface waters that flow through the S-79 structure, combined with tributary contributions below S-79 that collectively flow southwest to San Carlos Bay." Fla. Admin. Code. R. 40E-8.021(2). Man-made alterations to the Caloosahatchee River began as early as 1884, but major alterations began in the 1930s with the authorization and construction of the C-43 Canal. The C-43 Canal runs 41.6 miles from Lake Okeechobee at Moore Haven, i.e., from the S-77 structure, to Olga, i.e., the S-79 structure. The C-43 Canal serves as a conveyance feature to drain water from the three sub-watersheds located upstream of the S-79 structure and convey regulatory discharges of water from Lake Okeechobee. In 1957, the United States Army Corps of Engineers (USACOE) prepared a report focused on drainage, flood control, and navigation needs of the Caloosahatchee River Basin, and one recommendation was construction of the S-79 structure. The key objectives of the S-79 structure were to eliminate undesirable salinity in the lower Caloosahatchee River, prevent the rapid depletion of water supplies, and raise the prevailing dry weather water table levels. The S-79 structure was constructed in 1965. It is a lock and dam structure that is also known as the Franklin Lock and Dam. The S-79 structure captures all upstream fresh water discharges that go into the CRE. The S-79 structure demarcates the head of the CRE, which extends 26 miles downstream to Shell Point, where it empties into San Carlos Bay in the southern portion of the greater Lower Charlotte Harbor Estuary. Most of this surface water flow takes a southerly route, flowing to the Gulf of Mexico under the Sanibel Causeway that crosses San Carlos Bay. When fresh water inflows are high, tidal action pushes some of this water back up into Matlacha Pass and Pine Island Sound. Additionally, some water exits to the south and flows into Estero Bay through Matanzas Pass. Salinity exhibits a strong gradient in the CRE. Changes in the watershed upstream of the S-79 structure have profoundly influenced the delivery of fresh water to the CRE. Runoff is now more variable with higher wet season flows and lower dry season discharges. Large volumes of fresh water during the wet season can flush salt water from the tidally-influenced sections of the water body, resulting in low salinity conditions throughout most of the CRE. In contrast, fresh water inflow at the S-79 structure can stop entirely during the dry season, especially during significant drought events. This results in saline intrusion that can extend upstream to the S-79 structure. Fluctuations of this magnitude at the head and mouth of the system cause mortality of organisms at both ends of the salinity gradient. Downstream of the S-79 structure, the CRE was significantly altered by multiple dredging activities, including the removal of extensive shoals and oyster bars. Seven automobile bridges, a railroad trestle, and the Sanibel Causeway were built between the 1880s and 1960s. A large canal network was built along the northern shoreline of the CRE in Cape Coral. To provide navigational access from the canal network to deeper water, multiple access channels were dredged within the CRE. Alterations to the delivery of fresh water combined with structural changes to the tidally-influenced sections of the water body have had lasting ecological consequences. These include the loss of extensive shoals and oyster bars, loss of a flourishing bay scallop fishery, and significant decline in seagrass cover in deeper areas. MFLs An MFL is the limit at which further withdrawals would be significantly harmful to the water resources or ecology of the area. The District's rules define significant harm as the "temporary loss of water resource functions, which results from a change in surface or ground water hydrology, that takes more than two years to recover, but which is considered less severe than serious harm." Fla. Admin. Code R. 40E-8.021(31). The rule further specifies that a water body's specific water resource functions addressed by an MFL are defined in the MFL technical support document. Id. MFLs are calculated using the best information available. The regulatory agency is required to consider changes and structural alterations to watersheds, and the constraints such changes or alterations placed on the hydrology of an affected watershed. Certain waterbodies may not serve their historical hydrologic functions and recovery of these waterbodies to historical hydrologic conditions may not be economically or technically feasible. Accordingly, the regulatory agencies may determine that setting an MFL for such a water body based on its historical condition is not appropriate. Caloosahatchee MFL For the CRE, MFL criteria were designed to protect the estuary from significant harm due to insufficient fresh water inflows and were not guidelines for restoration of estuarine functions to conditions that existed in the past. The MFL criteria consider three aspects of the flow in terms of potential significant harm to the estuary: (1) the magnitude of the flow or the volume of fresh water entering the estuary; (2) the duration of time that flows can be below the recommended level before causing significant harm; and (3) the return frequency, or the number of times the MFL can be violated over a number of years before it results in significant harm, recognizing that natural climatic variability will be expected to cause fresh water inflows to fall below recommended levels at some natural frequency. The CRE MFL initially adopted in 2001 was primarily based on the salinity tolerance of one valued ecosystem component (VEC). The VEC was Vallisneria americana or tape grass, a fresh water aquatic plant that tolerates low levels of salinity. A major assumption of this approach was that flow and salinity conditions that protect Vallisneria would also protect other key organisms in the estuary. The 2001 CRE MFL was based on a regression model for estimating the relationship between surface salinity measured at the Ft. Myers monitoring station located in the Ft. Myers Yacht Basin and discharge at the S-79 structure. Although the District monitors surface and bottom salinity at multiple stations in the CRE, the Ft. Myers monitoring station is located centrally in the CRE and at the historical downstream extent of the Vallisneria habitat. The Ft. Myers monitoring station also has the most comprehensive period of record of monitoring data available. The fixed data sondes that monitor surface and bottom salinity are located at 20 percent and 80 percent of total river depth measured at mean low water. The data sondes continuously measure temperature and specific conductivity and, depending on the manufacturer, contains programs that calculate salinity. Those calculations are based on standards recognized and used worldwide by estuarine, marine, and oceanographic scientists.1/ The regression model only implicitly included inflows from the Tidal Caloosahatchee Basin sub-watershed downstream of the S-79 structure. To address this, during the 2003 re-evaluation, a linear reservoir model of Tidal Caloosahatchee Basin inflows was developed. The regression model results showed that a total inflow from S-79 plus the Tidal Caloosahatchee Basin of about 500 cubic feet per second (cfs) was required to produce a salinity of 10 at the Ft. Myers monitoring station. Thus, the 2001 CRE MFL of 300 cfs measured at the S-79 structure would produce a salinity of 10 at the Ft. Myers monitoring station only with additional inflow from the downstream Tidal Caloosahatchee Basin sub- watershed. However, that additional inflow estimate was highly uncertain. The conclusion was that actual flow measurements over a period of time were needed in order to perform more robust calibrations for the new models that were being developed. The Re-evaluation The District's re-evaluation effort began in 2010 after the Conservancy of Southwest Florida filed a petition requesting review of the Caloosahatchee MFL. At the time, the governing board denied the petition but directed staff to undertake additional research and monitoring to ensure a future revision would be supported by the best information available. The first step was to review the September 2000 Final Peer Review Report (PRR) for the initial adoption. The 2000 PRR identified several items the District should consider, including a hydrodynamic salinity model, a numerical population model for Vallisneria, quantification of habitat value for Vallisneria, and documentation of the effects of minimum flows on downstream estuarine biota. The 2000 PRR documented concerns that the current MFL was based solely on the salinity tolerance of Vallisneria and recommended using multiple indicator species. To address those recommendations, the District conducted studies to evaluate multiple ecological indicators, such as zooplankton, aquatic vegetation, oysters, benthic communities, and blue crabs, in the Caloosahatchee from the S-79 structure to beyond Shell Point. In addition, the District collected flow data from the Tidal Caloosahatchee Basin sub-watershed for at least five years to develop watershed, flow, and hydrodynamic models that could properly simulate inflows and salinity responses. When the initial research was complete in 2016, the District published the Draft Science Document containing 11 component studies. In September 2016, the District held a two- day Science Symposium to present the 11 component studies and gather public comment. In response to public comment, the District performed additional evaluations, modeling, and updated the component studies to produce a Draft Technical Document. A Peer Review Panel reviewed the Draft Technical Document, which included the Draft Science Document. The Peer Review Panel has over 150 years of combined relevant scientific experience. The Peer Review Panel toured the CRE by air and water. The District also held a Peer Review Session to engage the public and obtain feedback. The Peer Review Panel's 2017 report (PRP report) stated that the District had "crafted a well-executed and well- documented set of field and laboratory studies and modeling effort" to re-evaluate the CRE MFL. The PRP report supported the 11 component studies, the modeling, the evaluations, and the initial proposed rule language. The Final Technical Document published in January 2018 incorporated five different models and additional science, examining the entire watershed and the criteria itself. The Final Science Document was Appendix A to the Final Technical Document and contained the scientific research and analysis that was done for the 11 component studies, the modeling, and the additional scientific analyses performed in response to public and stakeholder input. The District initiated rule development in December 2017. Rule development workshops were held in February and June 2018 and a stakeholder technical meeting was held in May 2018. The District validated the comments after each workshop and meeting, and revised the proposed rule language. The District published its Notice of Proposed Rule on July 23, 2018.2/ At its September 13, 2018, meeting, the District's governing board held a public hearing on the Proposed Rule. The mayors of Sanibel, Cape Coral, and the Town publicly commented at the hearing. After considering public comments, the governing board adopted the Proposed Rule. The District documented and responded to each public comment, memorializing the information in the Final Technical Document. Later, after the rule workshops and May 2018 technical meeting, the District prepared and presented all of the updated information, including public comment, at the September 2018 adoption hearing. Thus, the District's re-evaluation process was open and transparent. The Re-evaluated Caloosahatchee MFL The science supporting the re-evaluation involved a comprehensive assessment of the effects of diminished dry season fresh water inflows on the CRE. The dry season was chosen for two reasons. First, because it is well-established that the upstream migration of salt combined with reduced fresh water inflow alters the health and productivity of estuarine habitats. Second, because the dry seasons are the times when the current MFL criteria are likely to be exceeded or violated. The 11 component studies targeted specific concerns regarding physical and ecological characteristics. Together they offered a holistic understanding of the negative effects of diminished fresh water inflow on estuarine ecology. The re-evaluated MFL criteria were developed using a resource-based approach. The approach combined the VEC approach and the habitat overlap concept. The habitat overlap approach is based on the idea that estuaries serve a nursery function and salinity determines the distribution of species within an estuary, including distribution during different life stages. The combined approach studied the minimum flow requirements of the various indicator species in terms of magnitude, duration, and return frequency, resulting in the following three aspects of the flow: (1) for magnitude, a 30-day moving average flow of 400 cfs measured at the S-79 structure; for duration, an MFL exceedance occurs during a 365-day period when the 30-day moving average flow at S-79 is below 400 cfs and the 30-day moving average salinity exceeds 10 at the Ft. Myers salinity monitoring station; and (3) for return frequency, an MFL violation occurs when an exceedance occurs more than once in a five-year period. The magnitude component is based on the salinity requirements of Vallisneria, along with results from the 11 studies modeling salinity and considering the salinity requirements of the other VECs. The duration component is based mainly on the estimates of rate of loss of Vallisneria shoots when salinity rises above 10 and the recovery rate of the shoots when salinities fall back below 10. Return frequency was determined based on long-term rainfall records rather than flow measurements from the S-79 structure, which the PRP report felt was well justified. In addition to the component studies, the re-evaluated MFL criteria and existing recovery strategy were evaluated using a suite of hydrologic and ecological models simulating long-term fresh water inflow to the CRE associated with varying management options, the resulting salinity in the CRE, and the ecological response of indicator species that are sensitive to low fresh water inflows. Five models were utilized. Three models simulated fresh water inflows to the CRE: two for S-79 flows; and one for Tidal Caloosahatchee Basin sub-watershed flows. The other two models were a three-dimensional hydrodynamic salinity model and a Vallisneria model. Tidal Caloosahatchee Basin sub-watershed has a number of tributaries that drain fresh water into the CRE. The flow at several of the tributaries was monitored for a five-year period. The measured flow was used to calibrate a watershed model and conduct a long-term simulation. The results showed an average fresh water inflow for all seasons of approximately 430 cfs. The average fresh water inflow during the dry season was 245 cfs while the wet season average fresh water inflow was 613 cfs. Fresh water inflow from the Tidal Caloosahatchee Basin sub- watershed was approximately 20 percent of total fresh water inflow to the CRE while 80 percent was released through the S-79 structure. Petitioners' and Intervenors' Objections 400 cfs Is Too Low Sanibel relied on a memorandum prepared by Dr. David Tomasko (Tomasko report) concerning his company's review of the January 2018 Final Technical Document supporting the Proposed Rule. The Tomasko report, dated October 23, 2018, was in the form of a "technical memorandum" outlining "preliminary findings." The Tomasko report was admitted as a joint exhibit; however, Dr. Tomasko did not testify at the final hearing. The Tomasko report is hearsay that was not used to supplement or explain competent direct evidence. Although hearsay is admissible in this proceeding, it cannot be the sole basis for a finding of fact.3/ See § 120.57(1)(c), Fla. Stat. The District's expert witnesses, who testified at the final hearing, explained that ten of the 11 component studies identified average indicator flows at S-79 ranging from 237 to 545 cfs with standard deviations ranging from plus or minus 57 to plus or minus 774 cfs.4/ The District's experts performed three different evaluations of those flow results. They identified the mean of all the means, calculated the median of the means, and performed a probability density function. The flow results for each of the three evaluations were 381 cfs, 400 cfs, and 365 cfs, with standard deviations that ranged from plus or minus 277 cfs to plus or minus 706 cfs. The District's experts testified that the three flow results are indistinguishable from a statistical point of view. The District chose 400 cfs because it was the highest flow result, and, therefore, the most protective of the three. The Petitioners and Intervenors failed to present evidence that showed any deficiencies in the District's component studies, hydrologic, hydrodynamic, or statistical modeling, or analysis of compliance data. The preponderance of the evidence established that the District used the best available science to calculate the MFL criteria. The District did not act arbitrarily or capriciously when it chose 400 cfs as the magnitude component of the MFL criteria. Inclusion of Salinity in the MFL Criteria The preponderance of the evidence also established that Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE. It supports essential ecological goods and services, is sensitive to salinity fluctuations at the ecosystem scale, and has value to a variety of stakeholders. The location of Vallisneria habitat in the upper CRE and its negative response to increased salinity made it an excellent candidate as an ecological indicator for fresh water inflow. A combination of field monitoring, mesocosm studies, and modeling results allowed the application of Vallisneria responses as a platform to quantify the effects of high salinity duration in the upper CRE. Component Study Eight reviewed the development and initial application of a simulation model for Vallisneria in the CRE. The Vallisneria model was used to evaluate the salinity conditions that led to net annual mortality, or, in other words, the duration of high salinity exposure that led to decreased Vallisneria shoots versus the duration of low salinity conditions required for recovery. Component Study Seven included an analysis of the relationship between the number of consecutive days where salinity at the Ft. Myers monitoring station was greater than 10 and the percentage of initial Vallisneria shoots remaining at the end of each high salinity period. To further evaluate the duration element associated with the MFL criteria, the field monitoring data contained in Component Study Seven was evaluated with the mesocosm and modeling results. All three sources were analyzed similarly to derive a combined curve showing high salinity exposure duration that is significantly harmful to Vallisneria. The model also provided information that was used to quantify the duration of low salinity conditions required for Vallisneria to recover a relative fraction of shoots after high salinity exposure. Merging the exposure and recovery evaluations facilitated a determination of the unfavorable salinity duration that could significantly harm Vallisneria habitat. With significant harm defined as the environmental harm from which two years are required to recover, the determination was that Vallisneria should experience no more than 55 consecutive days of salinity greater than 10. However, stakeholders expressed concerns regarding the percentage loss of Vallisneria habitat after 55 days of high salinity exposure. In response, the District conducted further analysis of modeling results and revised the duration component to accept the stakeholder recommendation, now expressed in the Proposed Rule, of a 30-day moving average salinity greater than 10. The Petitioners and Intervenors argued that by expressing the MFL as a "flow plus salinity component" the Proposed Rule enlarges, modifies, or contravenes the specific provisions of law implemented. However, the duration component is part of compliance and represents the duration of time that flows can be below the recommended level before causing significant harm to the indicator species Vallisneria. The MFL in the Proposed Rule is a 30-day moving average flow of 400 cfs measured at the S-79 structure. Flow is both measured and operationally controlled at the S-79 structure. However, as previously found, there are other sources of fresh water entering the CRE downstream of the S-79 structure. The District does not control and cannot control these downstream sources, which modeling reveals contribute approximately 20 percent of total fresh water inflow to the CRE. By including salinity, the District can account for fresh water inflows coming from the tidal basin when there are low or no flows at S-79 since the significant harm threshold in the CRE is directly related to salinity tolerance of the indicator species Vallisneria. The District's experts also testified that salinity can be used as a flow component because it is not affected by chemical or biological processes and is an indicator of how much fresh water is entering the system.5/ Salinity is included in the duration component of the MFL criteria and is an exceedance criterion because the science established that the salinity gradient is crucial to the overall health of the CRE. Including salinity in the duration component of the MFL criteria achieves the purpose of the statutory mandate to set MFLs that are designed to avoid significant harm to the water resources and ecology of the area. No Unit of Measurement for Salinity The Petitioners and Intervenors argued that the Proposed Rule is vague because the language does not contain any units for salinity. The UNESCO calculation is the standard equation used by the estuarine and marine science community to convert specific conductivity and temperature data to salinity. The District's experts testified that the UNESCO calculation reports salinity as a ratio, which is a dimensionless number and has no units. The District uses the UNESCO calculation and performs the conversion in a spreadsheet that it maintains. In some instances, certain brands of data sondes are programmed to perform the calculation and provide the salinity number. The preponderance of the evidence established that use of the practical salinity unit (PSU) is not technically correct. PSU is a misnomer, a pseudo-unit equivalent to a unitless salinity number. The Petitioners' and Intervenors' expert witness, Dr. Anthony Janicki, conceded there is no difference between reporting salinity as unitless or as PSU. And although technically incorrect, he suggested that placing the word "practical" or putting "PSU" in the Proposed Rule would reduce confusion and vagueness. However, since the preponderance of the evidence established that use of PSU is not technically correct, the use of a pseudo-unit would actually cause confusion instead of reduce confusion. The Petitioners and Intervenors also argued that the Proposed Rule is vague because the language does not state that the method of measuring salinity is specific conductivity, or that the equation used to convert specific conductivity and temperature data to salinity is the standard developed by UNESCO. The Petitioners and Intervenors essentially argued that members of the public and those who may be regulated by the Proposed Rule are left to guess about the method or methods used to measure salinity. Because the Proposed Rule identifies and locates by latitude and longitude coordinates the Ft. Myers salinity monitoring station as the location where salinity would be measured for compliance, the Proposed Rule language is not vague. The Proposed Rule is not vague because it does not describe the data sondes, what parameters are measured by the data sondes, and how those parameters are converted to a salinity number. Salinity Monitoring Location and Mean Low Water The Petitioners and Intervenors argued that the Proposed Rule is vague for failing to define the phrase "20% of the total river depth at mean low water," and is arbitrary or capricious for failing to include more than one salinity monitoring station. Total river depth or the water column depth is a standardized measurement that is made from the surface down to the bottom of the river bed. Mean low water is commonly understood in the oceanographic and coastal sciences community as the average of all low tides over the time period defined as the national tidal datum epic. The District's expert witness, Dr. Cassondra Armstrong, testified that mean low water can be determined by using two documents prepared by the National Oceanographic and Atmospheric Administration (NOAA), i.e., the NOAA tide charts and glossary. The District's expert witnesses testified that "20% of the total river depth at mean low water" is the location of the data sonde at the Ft. Myers monitoring station that measures surface salinity. This is also the depth at which Vallisneria is located in the CRE. Since, the Proposed Rule language simply identifies the location of the existing data sonde at the Ft. Myers salinity monitoring station, the language is not vague. The preponderance of the evidence established that the Ft. Myers salinity monitoring station has two salinity data sondes, the one at 20 percent of the total river depth and the other at 80 percent. The data sonde at 20 percent of the total river depth was identified in the Proposed Rule for the following reasons. First, this is the depth where Vallisneria grows and is representative of the salinity exposure for Vallisneria. Second, it guarantees the data sonde is always submerged and able to record data. Third, it has the most comprehensive period of record of monitoring data available. As previously found, Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE. The location of Vallisneria habitat in the upper CRE and its negative response to increased salinity made it an excellent candidate as an ecological indicator for fresh water inflow. Because the preponderance of the evidence established that Vallisneria continues to be a particularly useful indicator of environmental conditions in the CRE, the choice of the Ft. Myers monitoring station is not arbitrary or capricious. Water Resource Functions vs. Environmental Values The District's MFL rule specifies that a water body's specific water resource functions addressed by an MFL are defined in the MFL technical support document. See Fla. Admin. Code R. 40E-8.021(31). The Final Technical Document identified the relevant water resource functions of the CRE as fish and wildlife habitats, estuarine resources, water supply, recreation, navigation, and flood control. The Petitioners and Intervenors argued that the environmental values listed in Florida Administrative Code Chapter 62-40, also known as the Water Resource Implementation Rule, were not adequately addressed in the Final Technical Document. A proposed rule challenge is not the proper forum to determine whether a proposed rule is consistent with the Water Resource Implementation Rule. Such a determination is within the exclusive jurisdiction of the Department of Environmental Protection under section 373.114(2), Florida Statutes. Consistency of the District's Proposed Rule with the Water Resource Implementation Rule of the Department of Environmental Protection is not a basis in this proceeding for a finding that the Proposed Rule is an invalid exercise of delegated legislative authority. Other Issues The Petitioners and Intervenors raised other issues during the hearing, although not specifically argued in their proposed final order. Since those issues were identified as disputed issues in the Joint Pre-hearing Stipulation, they are addressed below. 1. Elimination of Single-day Exceedance Criterion During the rulemaking process, Sanibel and SCCF sent the District a letter requesting justification for eliminating the single-day exceedance salinity criterion in the current rule. The District staff evaluated the available Caloosahatchee River MFL compliance record, dating back to when the MFL was adopted in September 2001. The District maintains a historical record of MFL monitoring data and reviewed it to determine if the single-day exceedance salinity criterion was exceeded before the 30-day moving average criterion. The compliance record showed five exceedance events of the single-day salinity criterion have occurred. However, the compliance record also showed that the 30- day moving average salinity criterion had already been exceeded before the five events occurred. In other words, the single-day criterion was never exceeded before the 30-day moving average criterion. Based on this evaluation, the District eliminated the single-day exceedance salinity criterion because it did not provide any additional resource protection. The District's decision was not arbitrary or capricious. 2. Not Using the Latest Model Evaluation of recommended MFL criteria and a recovery strategy for the CRE were greatly aided by integration of a suite of hydrologic and ecological models simulating (1) long-term fresh water inflow associated with varying management options, (2) the resulting salinity in the estuary, and (3) ecological response of indicator species that are sensitive to low fresh water inflows. Five models were specifically utilized, including three models for simulations of fresh water inflows to the CRE, a three-dimensional hydrodynamic salinity model, and a Vallisneria model. The three models simulating fresh water inflows included (1) the South Florida Water Management Model (SFWMM) to simulate fresh water discharges at S-79, which includes regional operations of Lake Okeechobee and incorporates Caloosahatchee River irrigation demands; (2) the C-43 Reservoir Model, which uses the SFWMM-simulated daily S-79 flow as input and simulates the management benefit of the C-43 Reservoir; and (3) the Watershed (WaSh) Model to simulate tidal tributary inflow from the Tidal Caloosahatchee Basin sub-watershed. The Caloosahatchee Hydrodynamic/Salinity Model was based on the Curvilinear Hydrodynamic Three-dimensional Model (CH3D) modeling framework with the functionality of simulating the spatial salinity structure across the entire estuary. The Vallisneria Model took the CH3D modeled salinity as input to simulate Vallisneria growth at critical locations in the estuary. The District did review the more recent Environmental Fluid Dynamic Code (EFDC) model developed for the Caloosahatchee Total Maximum Daily Load (TMDL) and being used by the Department of Environmental Protection. The District's expert witness, Dr. Detong Sun, testified that until 2014, the hydrodynamic part of the EFDC model was not working well. He testified that in 2016, the District still had concerns and suggested the use of the District's continuous monitoring data from seven locations across the CRE rather than grab samples for model calibration. Dr. Sun's opinion was that the EFDC model has improved in recent years, but was still behind the CH3D model in terms of performance. The District's expert witness, Dr. Amanda Kahn, testified that the water quality component of the EFDC model was not appropriate for this re-evaluation because the MFL is about water quantity, not water quality. The water quality component of the EFDC model addresses nutrient loadings, not minimum flows. Dr. Kahn also testified that in setting MFL criteria for the CRE, salinity was not a water quality component. Salinity was used as a water quantity component because it does not change with biological processes and can be a measure of how much fresh water is coming into the system. Based on a preponderance of the evidence, the District's decision not to use the EFDC model was not arbitrary or capricious. 3. Seasonality The Petitioners and Intervenors argued that the District is required to set an MFL that varies by season. For the CRE, the District set MFL criteria that protect the system from low flow that would occur in either the wet or dry season. As previously found, the re-evaluation studies focused on the dry season for two reasons: first, because it is well-established that the upstream migration of salt combined with reduced fresh water inflow alters the health and productivity of estuarine habitats; and second, because the dry seasons are the times when the current MFL criteria are likely to be exceeded or violated. The MFL statute states that "when appropriate, [MFLs] may be calculated to reflect seasonal variations." § 373.042(1)(b), Fla. Stat. The preponderance of the evidence showed that for the CRE, it was not necessary to set an MFL that varied by season. Improper Purpose The Petitioners, Sanibel, Cape Coral, and the Town, did not participate in this proceeding primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of litigation. The Petitioners did not participate in this proceeding for an improper purpose. The Intervenors, Fort Myers, Estero, Bonita Springs, and CCP, did not participate in this proceeding primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of litigation. The Intervenors did not participate in this proceeding for an improper purpose.
The Issue The issue to be determined is whether Consumptive Use Permit No. 2-083-91926-3, and Environmental Resource Permit No. IND-083-130588-4 should be issued as proposed in the respective proposed agency actions issued by the St. Johns River Water Management District.
Findings Of Fact The Parties Sierra Club, Inc., is a national organization, the mission of which is to explore, enjoy, and advocate for the environment. A substantial number of Sierra Club’s 28,000 Florida members utilize the Silver River, Silver Springs, the Ocklawaha River, and the St. Johns River for water-based recreational activities, which uses include kayaking, swimming, fishing, boating, canoeing, nature photography, and bird watching. St. Johns Riverkeeper, Inc., is one of 280 members of the worldwide Waterkeepers Alliance. Its mission is to protect, restore, and promote healthy waters of the St. Johns River, its tributaries, springs, and wetlands -- including Silver Springs, the Silver River, and the Ocklawaha River -- through citizen- based advocacy. A substantial number of St. Johns Riverkeeper’s more than 1,000 members use and enjoy the St. Johns River, the Silver River, Silver Springs, and the Ocklawaha River for boating, fishing, wildlife observation, and other water-based recreational activities. Karen Ahlers is a native of Putnam County, Florida, and lives approximately 15 miles from the Applicant’s property on which the permitted uses will be conducted. Ms. Ahlers currently uses the Ocklawaha River for canoeing, kayaking, and swimming, and enjoys birding and nature photography on and around the Silver River. Over the years, Ms. Ahlers has advocated for the restoration and protection of the Ocklawaha River, as an individual and as a past-president of the Putnam County Environmental Council. Jeri Baldwin lives on a parcel of property in the northeast corner of Marion County, approximately one mile from the Applicant’s property on which the permitted uses will be conducted. Ms. Baldwin, who was raised in the area, and whose family and she used the resources extensively in earlier years, currently uses the Ocklawaha River for boating. Florida Defenders of the Environment (FDE) is a Florida corporation, the mission of which is to conserve and protect and restore Florida's natural resources and to conduct environmental education projects. A substantial number of FDE’s 186 members, of which 29 reside in Marion County, Florida, use and enjoy Silver Springs, the Silver River, and the Ocklawaha Aquatic Preserve, and their associated watersheds in their educational and outreach activities, as well as for various recreational activities including boating, fishing, wildlife observation, and other water-based recreational activities. Sleepy Creek Lands, LLC (Sleepy Creek or Applicant), is an entity registered with the Florida Department of State to do business in the state of Florida. Sleepy Creek owns approximately 21,000 acres of land in Marion County, Florida, which includes the East Tract and the North Tract on which the activities authorized by the permits are proposed. St. Johns River Water Management District (SJRWMD or 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. The Consumptive Use Permit The CUP is a modification and consolidation of two existing CUP permits, CUP No. 2-083-3011-7 and CUP No. 2-083- 91926-2, which authorize the withdrawal of 1.46 mgd from wells located on the East Tract. Although the existing CUP permits authorize an allocation of 1.46 mgd, actual use has historically been far less, and rarely exceeded 0.3 mgd. The proposed CUP modification will convert the authorized use of water from irrigation of 1,010 acres of sod grass on the East Tract, to supplemental irrigation of improved pasture for grass and other forage crops (approximately 97 percent of the proposed withdrawals) and cattle watering (approximately three percent of the proposed withdrawals) on the North Tract and the East Tract. An additional very small amount will be used in conjunction with the application of agricultural chemicals. CUP No. 2-083-3011-7 is due to expire in 2021. CUP No. 2-083-91926-2 is due to expire in 2024. In addition to the consolidation of the withdrawals into a single permit, the proposed agency action would extend the term of the consolidated permit to 20 years from issuance, with the submission of a compliance report due 10 years from issuance. Sleepy Creek calculated a water demand of 2.569 mgd for the production of grasses and forage crops necessary to meet the needs for grass-fed beef production, based on the expected demand in a 2-in-10 drought year. That calculation is consistent with that established in CUP Applicant’s Handbook (CUP A.H.) section 12.5.1. The calculated amount exceeds the authorized average allocation of 1.46 mgd. Mr. Jenkins testified as to the District’s understanding that the requested amount would be sufficient, since the proposed use was a “scaleable-type project,” with adjustments to cattle numbers made as necessary to meet the availability of feed. Regardless of demand, the proposed permit establishes the enforceable withdrawal limits applicable to the property. With regard to the East Tract, the proposed agency action reduces the existing 1.46 mgd allocation for that tract to a maximum allocation of 0.464 mgd, and authorizes the irrigation of 611 acres of pasture grass using existing extraction wells and six existing pivots. With regard to the North Tract, the proposed agency action authorizes the irrigation of 1,620 acres of pasture and forage grain crops using 15 center pivot systems. Extraction wells to serve the North Tract pivots will be constructed on the North Tract. The proposed North Tract withdrawal wells are further from Silver Springs than the current withdrawal locations. The proposed CUP allows Sleepy Creek to apply the allocated water as it believes to be appropriate to the management of the cattle operation. Although the East Tract is limited to a maximum of 0.464 mgd, there is no limitation on the North Tract. Thus, Sleepy Creek could choose to apply all of the 1.46 mgd on the North Tract. For that reason, the analysis of impacts from the irrigation of the North Tract has generally been based on the full 1.46 mgd allocation being drawn from and applied to the North Tract. The Environmental Resource Permit As initially proposed, the CUP had no elements that would require issuance of an ERP. However, in order to control the potential for increased runoff and nutrient loading resulting from the irrigation of the pastures, Sleepy Creek proposes to construct a stormwater management system to capture runoff from the irrigated pastures, consisting of a series of vegetated upland buffers, retention berms and redistribution swales between the pastures and downgradient wetland features. Because the retention berm and swale system triggered the permitting thresholds in rule 62-330.020(2)(d) (“a total project area of more than one acre”) and rule 62-330.020(2)(e) (“a capability of impounding more than 40 acre-feet of water”), Sleepy Creek was required to obtain an Environmental Resource Permit for its construction. Regional Geologic Features To the west of the North Tract is a geologic feature known as the Ocala Uplift or Ocala Platform, in which the limestone that comprises the Floridan aquifer system exists at or very near the land surface. Karst features, including subterranean conduits and voids that can manifest at the land surface as sinkholes, are common in the Ocala Uplift due in large part to the lack of consolidated or confining material overlaying the limestone. Water falling on the surface of such areas tends to infiltrate rapidly through the soil into the Floridan aquifer, occasionally through direct connections such as sinkholes. The lack of confinement in the Ocala Uplift results in few if any surface-water features such as wetlands, creeks, and streams. As one moves east from the Ocala Uplift, a geologic feature known as the Cody Escarpment becomes more prominent. In the Cody Escarpment, the limestone becomes increasingly overlain by sands, shell, silt, clays, and other less permeable sediments of the Hawthorn Group. The North Tract and the East Tract lie to the east of the point at which the Cody Escarpment becomes apparent. As a result, water tends to flow overland to wetlands and other surface water features. The Property The North and East Tracts are located in northern Marion County near the community of Fort McCoy. East Tract Topography and Historic Use The East Tract is located in the Daisy Creek Basin, and includes the headwaters of a small creek that drains directly to the Ocklawaha River. The historic use of the East Tract has been as a cleared 1,010-acre sod farm. The production of sod included irrigation, fertilization, and pest control. Little change in the topography, use, and appearance of the property will be apparent as a result of the permits at issue, but for the addition of grazing cattle. The current CUPs that are subject to modification in this proceeding authorize groundwater withdrawals for irrigation of the East Tract at the rate of 1.46 mgd. Since the proposed agency action has the result of reducing the maximum withdrawal from wells on the East Tract to 0.464 mgd, thus proportionately reducing the proposed impacts, there was little evidence offered to counter Sleepy Creek’s prima facie case that reasonable assurance was provided that the proposed East Tract groundwater withdrawal allocation will meet applicable CUP standards. There are no stormwater management structures to be constructed on the East Tract. Therefore, the ERP permit discussed herein is not applicable to the East Tract. North Tract Topography and Historic Use The North Tract has a generally flat topography, with elevations ranging from 45 feet to 75 feet above sea level. The land elevation is highest at the center of the North Tract, with the land sloping towards the Ocklawaha River to the east, and to several large wet prairie systems to the west. Surface water features on the North Tract include isolated, prairie, and slough-type wetlands on approximately 28 percent of the North Tract, and a network of creeks, streams, and ditches, including the headwaters of Mill Creek, a contributing tributary of the Ocklawaha River. A seasonal high groundwater elevation on the North Tract is estimated at 6 to 14 inches below ground surface. The existence of defined creeks and surface water features supports a finding that the North Tract is underlain by a relatively impermeable confining layer that impedes the flow of water from the surface and the shallow surficial aquifer to the upper Floridan and lower Floridan aquifers. If there was no confining unit, water going onto the surface of the property, either in the form of rain or irrigation water, would percolate unimpeded to the lower aquifers. Areas in the Ocala Uplift to the west of the North Tract, where the confining layer is thinner and discontiguous, contain few streams or runoff features. Historically, the North Tract was used for timber production, with limited pasture and crop lands. At the time the 7,207-acre North Tract was purchased by Sleepy Creek, land use consisted of 4,061 acres of planted pine, 1,998 acres of wetlands, 750 acres of improved pasture, 286 acres of crops, 78 acres of non-forested uplands, 20 acres of native forest, 10 acres of open water, and 4 acres of roads and facilities. Prior to the submission of the CUP and ERP applications, much of the planted pine was harvested, and the land converted to improved pasture. Areas converted to improved pasture include those proposed for irrigation, which have been developed in the circular configuration necessary for future use with center irrigation pivots. As a result of the harvesting of planted pine, and the conversion of about 345 acres of cropland and non-forested uplands to pasture and incidental uses, total acreage in pasture on the North Tract increased from 750 acres to 3,938 acres. Other improvements were constructed on the North Tract, including the cattle processing facility. Aerial photographs suggest that the conversion of the North Tract to improved pasture and infrastructure to support a cattle ranch is substantially complete. The act of converting the North Tract from a property dominated by planted pine to one dominated by improved pasture, and the change in use of the East Tract from sod farm to pasture, were agricultural activities that did not require a permit from the District. As such, there is no impropriety in considering the actual, legal use of the property in its current configuration as the existing use for which baseline conditions are to be measured. Petitioners argue that the baseline conditions should be measured against the use of the property as planted pine plantation, and that Sleepy Creek should not be allowed to “cattle-up” before submitting its permit applications, thereby allowing the baseline to be established as a higher impact use. However, the applicable rules and statutes provide no retrospective time-period for establishing the nature of a parcel of property other than that lawfully existing when the application is made. See West Coast Reg’l Water Supply Auth. v. SW Fla. Water Mgmt. Dist., Case No. 95-1520 et seq., ¶ 301 (Fla. DOAH May 29, 1997; SFWMD ) (“The baseline against which projected impacts conditions [sic] are those conditions, including previously permitted adverse impacts, which existed at the time of the filing of the renewal applications.”). The evidence and testimony in this case focused on the effects of the water allocation on the Floridan aquifer, Silver Springs, and the Silver River, and on the effects of the irrigation on water and nutrient transport from the properties. It was not directed at establishing a violation of chapter 373, the rules of the SJRWMD, or the CUP Applicant’s Handbook with regard to the use and management of the agriculturally-exempt unirrigated pastures, nor did it do so. Soil Types Soils are subject to classifications developed by the Soil Conservation Service based on their hydrologic characteristics, and are grouped into Group A, Group B, Group C, or Group D. Factors applied to determine the appropriate hydrologic soil group on a site-specific basis include depth to seasonal high saturation, the permeability rate of the most restrictive layer within a certain depth, and the depth to any impermeable layers. Group A includes the most well-drained soils, and Group D includes the most poorly-drained soils. Group D soils are those with seasonal high saturation within 24 inches of the soil surface and a higher runoff potential. The primary information used to determine the hydrologic soil groups on the North Tract was the depth to seasonal-high saturation, defined as the highest expected annual elevation of saturation in the soil. Depth to seasonal-high saturation was measured through a series of seven hand-dug and augered soil borings completed at various locations proposed for irrigation across the North Tract. In determining depth to seasonal-high saturation, the extracted soils were examined based on depth, color, texture, and other relevant characteristics. In six of the seven locations at which soil borings were conducted, a restrictive layer was identified within 36 inches of the soil surface. At one location at the northeastern corner of the North Tract, the auger hole ended at a depth of 48 inches -- the length of the auger -- at which depth there was an observable increase in clay content but not a full restrictive layer. However, while the soil assessment was ongoing, a back-hoe was in operation approximately one hundred yards north of the boring location. Observations of that excavation revealed a heavy clay layer at a depth of approximately 5 feet. In each of the locations, the depth to seasonal-high saturation was within 14 inches of the soil surface. Based on the consistent observation of seasonal-high saturation at each of the sampled locations, as well as the flat topography of the property with surface water features, the soils throughout the property, with the exception of a small area in the vicinity of Pivot 6, were determined to be in hydrologic soil Group D. Hydrogeologic Features There are generally five hydrogeologic units underlying the North Tract, those units being the surficial aquifer system, the intermediate confining unit, the upper Floridan aquifer, the middle confining unit, and the lower Floridan aquifer. In areas in which a confining layer is present, water falling on the surface of the land flows over the surface of the land or across the top of the confining layer. A surficial aquifer, with a relatively high perched water table, is created by the confinement and separation of surface waters from the upper strata of the Floridan aquifer. Surface waters are also collected in or conveyed by various surface water features, including perched wetlands, creeks, and streams. The preponderance of the evidence adduced at the final hearing demonstrates that the surficial aquifer exists on the property to a depth of up to 20 feet below the land surface (bls). Beneath the surficial aquifer is an intermediate confining unit of dense clay interspersed with beds of sand and calcareous clays that exists to a depth of up to 100 feet bls. The clay material observed on the North Tract is known as massive or structureless. Such clays are restrictive with very low levels of hydraulic conductivity, and are not conducive to development of preferential flow paths to the surficial or lower aquifers. The intermediate confining unit beneath the North Tract restricts the exchange of groundwater from the surficial aquifer to the upper Floridan aquifer. The upper Floridan aquifer begins at a depth of approximately 100 feet bls, and extends to a depth of approximately 340 feet bls. At about 340 feet bls, the upper Floridan aquifer transitions to the middle confining unit, which consists of finely grained, denser material that separates the interchange of water between the upper Floridan aquifer and the lower Floridan aquifer. Karst Features Karst features form as a result of water moving through rock that comprises the aquifer, primarily limestone, dissolving and forming conduits in the rock. Karst areas present a challenging environment to simulate through modeling. Models assume the subsurface to be a relatively uniform “sand box” through which it is easier to simulate groundwater flow. However, if the subsurface contains conduits, it becomes more difficult to simulate the preferential flows and their effect on groundwater flow paths and travel times. The District has designated parts of western Alachua County and western Marion County as a Sensitive Karst Area Basin. A Sensitive Karst Area is a location in which the porous limestone of the Floridan aquifer occurs within 20 feet of the land surface, and in which there is 10 to 20 inches of annual recharge to the Floridan aquifer. The designation of an area as being within the Sensitive Karst Area Basin does not demonstrate that it does, or does not, have subsurface features that are karstic in nature, or that would provide a connection between the surficial aquifer and the Floridan aquifer. The western portion of the North Tract is within the Sensitive Karst Area Basin. The two intensive-use areas on the North Tract that have associated stormwater facilities -- the cattle unloading area and the processing facility -- are outside of the Sensitive Karst Area Basin. The evidence was persuasive that karst features are more prominent to the west of the North Tract. In order to evaluate the presence of karst features on the North Tract, Mr. Andreyev performed a “desktop-type evaluation,” with a minimal field survey. The desktop review included a review of aerial photographs and an investigation of available data, including the Florida Geological Survey database of sinkhole occurrence in the area. The aerial photographs showed circular depressions suggestive of karst activity west and southwest of the North Tract, but no such depressions on the North Tract. Soil borings taken on the North Tract indicated the presence of layers of clayey sand, clays, and silts at a depth of 70 to 80 feet. Well-drilling logs taken during the development of the wells used for an aquifer performance test on the North Tract showed the limestone of the Floridan aquifer starting at a depth below ground surface of 70 to 80 feet. Other boring data generated on the North Tract suggests that there is greater than 100 feet of clay and sandy clay overburden above the Floridan aquifer on and in the vicinity of the North Tract. Regardless of site-specific differences, the observed confining layer separating the surficial aquifer from the Floridan aquifer is substantial, and not indicative of a karst environment. Aquifer performance tests performed on the North Tract were consistent in showing that drawdown in the surficial aquifer from the tests was minimal to non-detectable, which is strong evidence of an intact and low-permeability confining layer. The presence of well-developed drainage features on the North Tract is further evidence of a unit of confinement that is restricting water from going deeper into the subsurface, and forcing it to runoff to low-lying surface water features. Petitioners’ witnesses did not perform any site- specific analysis of karst features on or around the Sleepy Creek property. Their understanding of the nature of the karst systems in the region was described as “hypothetical or [] conceptual.” Dr. Kincaid admitted that he knew of no conduits on or adjacent to the North Tract. As a result of the data collected from the North Tract, Mr. Hearn opined that the potential for karst features on the property that provide an opening to the upper Floridan aquifer “is extremely remote.” Mr. Hearn’s opinion is consistent with the preponderance of the evidence in this case, and is accepted. In the event a surface karst feature were to manifest itself, Sleepy Creek has proposed that the surface feature be filled and plugged to reestablish the integrity of the confining layer. More to the point, the development of a surficial karst feature in an area influenced by irrigation would be sufficient grounds for the SJRWMD to reevaluate and modify the CUP to account for any changed conditions affecting the assumptions and bases for issuance of the CUP. Silver Springs, the Silver River, and the Ocklawaha River The primary, almost exclusive concern of Petitioners was the effect of the modified CUP and the nutrients from the proposed cattle ranch on Silver Springs, the Silver River, and the Ocklawaha River. Silver Springs Silver Springs has long been a well-known attraction in Florida. It is located just to the east of Ocala, Florida. Many of the speakers at the public comment period of this proceeding spoke fondly of having frequented Silver Springs over the years, enjoying its crystal clear waters through famous glass-bottomed boats. For most of its recorded history, Silver Springs was the largest spring by volume in Florida. Beginning in the 1970s, it began to lose its advantage, and by the year 2000, Rainbow Springs, located in southwestern Marion County, surpassed Silver Springs as the state’s largest spring. Silver Springs exists at the top of the potentiometric surface of the Floridan aquifer. Being at the “top of the mountain,” when water levels in the Floridan aquifer decline, groundwater flow favors the lower elevation springs. Thus, surrounding springshed boundaries expand to take more water to maintain their baseflows, at the expense of the Silver Springs springshed, which contracts. Rainbow Springs shares an overlapping springshed with Silver Springs. The analogy used by Dr. Knight was of the aquifer as a bucket with holes at different levels, and with the Silver Springs “hole” near the top of the bucket. When the water level in the bucket is high, water will flow from the top hole. As the water level drops below that hole, it will preferentially flow from the lower holes. Rainbow Springs has a vent or outlet from the aquifer, that is 10 feet lower in elevation than that of Silver Springs. Coastal springs are lower still. Thus, as groundwater levels decline, the lower springs “pirate flow” from the upper springs. Since the first major studies of Silver Springs were conducted in the 1950s, the ecosystem of Silver Springs has undergone changes. The water clarity, though still high as compared to other springs, has been reduced by 10 to 15 percent. Since the 1950s, macrophytic plants, i.e., rooted plants with seeds and flowers, have declined in population, while epiphytic and benthic algae have increased. Those plants are sensitive to increases in nitrogen in the water. Thus, Dr. Knight’s opinion that increases in nitrogen emerging from Silver Springs, calculated to have risen from just over 0.4 mg/l in the 1950s, to 1.1 mg/l in 2004, and to up to 1.5 mg/l at present,1/ have caused the observed vegetative changes is accepted. Silver River Silver Springs forms the headwaters for the Silver River, a spring run 5 1/2 miles in length, at which point it becomes a primary input to the Ocklawaha River. Issues of water clarity and alteration of the vegetative regime that exist at Silver Springs are also evident in the Silver River. In addition, the reduction in flow allows for more tannic water to enter the river, further reducing clarity. Dr. Dunn recognized the vegetative changes in the river, and opined that the “hydraulic roughness” caused by the increase in vegetation is likely creating a spring pool backwater at Silver Springs, thereby suppressing some of the flow from the spring. The Silver River has been designated as an Outstanding Florida Water. There are currently no Minimum Flows and Levels established by the District for the Silver River. Ocklawaha River The Ocklawaha River originates near Leesburg, Florida, at the Harris Chain of Lakes, and runs northward past Silver Springs. The Silver River is a major contributor to the flow of the Ocklawaha River. Due to the contribution of the Silver River and other spring-fed tributaries, the Ocklawaha River can take on the appearance of a spring run during periods of low rainfall. Historically, the Ocklawaha River flowed unimpeded to its confluence with the St. Johns River in the vicinity of Palatka, Florida. In the 1960s, as part of the Cross-Florida Barge Canal project, the Rodman Dam was constructed across the Ocklawaha River north of the Sleepy Creek property, creating a large reservoir known as the Rodman Pool. Dr. Knight testified convincingly that the Rodman Dam and Pool have altered the Ocklawaha River ecosystem, precipitating a decline in migratory fish populations and an increase in filamentous algae. At the point at which the Ocklawaha River flows past the Sleepy Creek property, it retains its free-flowing characteristics. Mill Creek, which has its headwaters on the North Tract, is a tributary of the Ocklawaha River. The Ocklawaha River, from the Eureka Dam south, has been designated as an Outstanding Florida Water. However, the Ocklawaha River at the point at which Mill Creek or other potential surface water discharges from the Sleepy Creek property might enter the river are not included in the Outstanding Florida Water designation. There are currently no Minimum Flows and Levels established by the District for the Ocklawaha River. The Silver Springs Springshed A springshed is that area from which a spring draws water. Unlike a surface watershed boundary, which is fixed based on land features, contours, and elevations, a springshed boundary is flexible, and changes depending on a number of factors, including rainfall. As to Silver Springs, its springshed is largest during periods of more abundant rainfall when the aquifer is replenished, and smaller during drier periods when groundwater levels are down, and water moves preferentially to springs and discharge points that are lower in elevation. The evidence in this case was conflicting as to whether the North Tract is in or out of the Silver Springs springshed boundary. Dr. Kincaid indicated that under some of the springshed delineations, part of the North Tract was out of the springshed, but over the total period of record, it is within the springshed. Thus, it was Dr. Kincaid’s opinion that withdrawals anywhere within the region will preferentially impact Silver Springs, though he admitted that he did not have the ability to quantify his opinion. Dr. Knight testified that the North Tract is within the Silver Springs “maximum extent” springshed at least part of the time, if not all the time. He did not opine as to the period of time in which the Silver Springs springshed was at its maximum extent. Dr. Bottcher testified that the North Tract is not within the Silver Springs springshed because there is a piezometric rise between North Tract and Silver Springs. Thus, in his opinion, withdrawals at the North Tract would not be withdrawing water going to Silver Springs. Dr. Dunn agreed that the North Tract is on the groundwater divide for Silver Springs. In his view, the North Tract is sometimes in, and sometimes out of the springshed depending on the potentiometric surface. In his opinion, the greater probability is that the North Tract is more often outside of the Silver Springs springshed, with seasonal and year—to—year variation. Dr. Dunn’s opinion provides the most credible explanation of the extent to which the North Tract sits atop that portion of the lower Floridan aquifer that feeds to Silver Springs. Thus, it is found that the groundwater divide exists to the south of the North Tract for a majority of the time, and water entering the Floridan aquifer from the North Tract will, more often than not, flow away from Silver Springs. Silver Springs Flow Volume The Silver Springs daily water discharge has been monitored and recorded since 1932. Over the longest part of the period of record, up to the 1960s, flows at Silver Springs averaged about 800 cubic feet per second (cfs). Through 1989, there was a reasonable regression between rainfall and springflow, based on average rainfalls. The long-term average rainfall in Ocala was around 50 inches per year, and long-term springflow was about 800 cfs, with deviations from average generally consistent with one another. Between 1990 and 1999, the relationship between rainfall and springflow declined by about 80 cubic feet per second. Thus, with average rainfall of 50 inches per year, the average springflow was reduced to about 720 cfs. From 2000 to 2009, there was an additional decline, such that the total cumulative decline for the 20-year period through 2009 was 250 cfs. Dr. Dunn agreed with Dr. Knight that after 2000, there was an abrupt and persistent reduction in flow of about 165 cfs. However, Dr. Dunn did not believe the post-2000 flow reduction could be explained by rainfall directly, although average rainfall was less than normal. Likewise, groundwater withdrawals did not offer an adequate explanation. Dr. Dunn described a natural 30-year cycle of wetter and drier periods known as the Atlantic Multidecadal Oscillation (AMO) that has manifested itself over the area for the period of record. From the 1940s up through 1970, the area experienced an AMO wet cycle with generally higher than normal rainfall at the Ocala rain station. For the next 30-year period, from 1970 up to 2000, the Ocala area ranged from a little bit drier to some years in which it was very, very dry. Dr. Dunn attributed the 80 cfs decline in Silver Springs flow recorded in the 1990s to that lower rainfall cycle. After 2000, when the next AMO cycle would be expected to build up, as it did post—1940, it did not happen. Rather, there was a particularly dry period around 2000 that Dr. Dunn believes to have had a dramatic effect on the lack of recovery in the post-2000 flows in the Silver River. According to Mr. Jenkins, that period of deficient rainfall extended through 2010. Around the year 2001, the relationship between rainfall and flow changed such that for a given amount of rainfall, there was less flow in the Silver River, with flow dropping to as low as 535 cfs after 2001. It is that reduction in flow that Dr. Knight has attributed to groundwater withdrawals. It should be noted that the observed flow of Silver Springs that formed the 1995 baseline conditions for the North Central Florida groundwater model that will be discussed herein was approximately 706 cfs. At the time of the final hearing in August 2014, flow at Silver Springs was 675 cfs. The reason offered for the apparent partial recovery was higher levels of rainfall, though the issue was not explored in depth. For the ten-year period centered on the year 2000, local water use within Marion and Alachua County, closer to Silver Springs, changed little -- around one percent per year. From a regional perspective, groundwater use declined at about one percent per year for the period from 1990 to 2010. The figures prepared by Dr. Knight demonstrate that the Sleepy Creek project area is in an area that has a very low density of consumptive use permits as compared to areas adjacent to Silver Springs and more clearly in the Silver Springs springshed. In Dr. Dunn’s opinion, there were no significant changes in groundwater use either locally or regionally that would account for the flow reduction in Silver Springs from 1990 to 2010. In that regard, the environmental report prepared by Dr. Dunn and submitted with the CUP modification application estimated that groundwater withdrawals accounted for a reduction in flow at Silver Springs of approximately 20 cfs as measured against the period of record up to the year 2000, with most of that reduction attributable to population growth in Marion County. In the March 2014, environmental impacts report, Dr. Dunn described reductions in the stream flow of not only the Silver River, but of other tributaries of the lower Ocklawaha River, including the upper Ocklawaha River at Moss Bluff and Orange Creek. However, an evaluation of the Ocklawaha River water balance revealed there to be additional flow of approximately 50 cfs coming into the Ocklawaha River at other stations. Dr. Dunn suggested that changes to the vent characteristics of Silver Springs, and the backwater effects of increased vegetation in the Silver River, have resulted in a redistribution of pressure to other smaller springs that discharge to the Ocklawaha River, accounting for a portion of the diminished flow at Silver Springs. The Proposed Cattle Operation Virtually all beef cattle raised in Florida, upon reaching a weight of approximately 875 pounds, are shipped to Texas or Kansas to be fattened on grain to the final body weight of approximately 1,150 pounds, whereupon they are slaughtered and processed. The United States Department of Agriculture has a certification for grass—fed beef which requires that, after an animal is weaned, it can only be fed on green forage crops, including grasses, and on corn and grains that are cut green and before they set seed. The forage crops may be grazed or put into hay or silage and fed when grass and forage is dormant. The benefit of grass feeding is that a higher quality meat is produced, with a corresponding higher market value. Sleepy Creek plans to develop the property as a grass- fed beef production ranch, with pastures and related loading/unloading and slaughter/processing facilities where calves can be fattened on grass and green grain crops to a standard slaughter weight, and then slaughtered and processed locally. By so doing, Sleepy Creek expects to save the transportation and energy costs of shipping calves to the Midwest, and to generate jobs and revenues by employing local people to manage, finish, and process the cattle. As they currently exist, pastures proposed for irrigation have been cleared and seeded, and have “fairly good grass production.” The purpose of the irrigation is to enhance the production and quality of the grass in order to maintain the quality and reliability of feed necessary for the production of grass-fed beef. East Tract Cattle Operation The East Tract is 1,242 acres in size, substantially all of which was previously cleared, irrigated, and used for sod production. The proposed CUP permit authorizes the irrigation of 611 acres of pasture under six existing center pivots. The remaining 631 acres will be used as improved, but unirrigated, pasture. Under the proposed permit, a maximum of 1,207 cattle would be managed on the East Tract. Of that number, 707 cattle would be grazed on the irrigated paddocks, and 500 cattle would be grazed on the unirrigated improved pastures. If the decision is made to forego irrigation on the East Tract, with the water allocation being used on the North Tract or not at all, the number of cattle grazed on the six center pivot pastures would be decreased from 707 cattle to 484 cattle. The historic use of the East Tract as a sod farm resulted in high phosphorus levels in the soil from fertilization, which has made its way to Daisy Creek. Sleepy Creek has proposed a cattle density substantially below that allowed by application of the formulae in the Nutrient Management Plan in order to “mine” the phosphorus levels in the soil over time. North Tract Cattle Operation The larger North Tract includes most of the “new” ranch activities, having no previous irrigation, and having been put to primarily silvicultural use with limited pasture prior to its acquisition by Sleepy Creek. The ranch’s more intensive uses, i.e., the unloading corrals and the slaughter house, are located on the North Tract. The North Tract is 7,207 acres in size. Of that, 1,656 acres are proposed for irrigation by means of 15 center- pivot irrigation systems. In addition to the proposed irrigated pastures, the North Tract includes 2,382 acres of unirrigated improved pasture, of which approximately 10 percent is wooded. Under the proposed permit, a maximum of 6,371 cattle would be managed on the North Tract. Of that number, 3,497 cattle would be grazed on the irrigated paddocks (roughly 2.2 head of cattle per acre), and 2,374 cattle would graze on the improved pastures (up to 1.1 head of cattle per acre). The higher cattle density in the irrigated pastures can be maintained due to the higher quality grass produced as a result of irrigation. The remaining 500 cattle would be held temporarily in high-concentration corrals, either after offloading or while awaiting slaughter. On average, there will be fewer than 250 head of cattle staged in those high-concentration corrals at any one time. In the absence of irrigation, the improved pasture on the North Tract could sustain about 4,585 cattle. Nutrient Management Plan, Water Conservation Plan, and BMPs The CUP and ERP applications find much of their support in the implementation of the Nutrient Management Plan (NMP), the Water Conservation Plan, and Best Management Practices (BMPs). The NMP sets forth information designed to govern the day to day operations of the ranch. Those elements of the NMP that were the subject of substantive testimony and evidence at the hearing are discussed herein. Those elements not discussed herein are found to have been supported by Sleepy Creek’s prima facie case, without a preponderance of competent and substantial evidence to the contrary. The NMP includes a herd management plan, which describes rotational grazing and the movement of cattle from paddock to paddock, and establishes animal densities designed to maintain a balance of nutrients on the paddocks, and to prevent overgrazing. The NMP establishes fertilization practices, with the application of fertilizer based on crop tissue analysis to determine need and amount. Thus, the application of nitrogen- based fertilizer is restricted to that capable of ready uptake by the grasses and forage crops, limiting the amount of excess nitrogen that might run off of the pastures or infiltrate past the root zone. The NMP establishes operation and maintenance plans that incorporate maintenance and calibration of equipment, and management of high-use areas. The NMP requires that records be kept of, among other things, soil testing, nutrient application, herd rotation, application of irrigation water, and laboratory testing. The irrigation plan describes the manner and schedule for the application of water during each irrigation cycle. Irrigation schedules for grazed and cropped scenarios vary from pivot to pivot based primarily on soil type. The center pivots proposed for use employ high-efficiency drop irrigation heads, resulting in an 85 percent system efficiency factor, meaning that there is an expected evaporative loss of 15 percent of the water before it becomes available as water in the soil. That level of efficiency is greater than the system efficiency factor of 80 percent established in CUP A.H. section 12.5.2. Other features of the irrigation plan include the employment of an irrigation manager, installation of an on-site weather station, and cumulative tracking of rain and evapotranspiration with periodic verification of soil moisture conditions. The purpose of the water conservation practices is to avoid over application of water, limiting over-saturation and runoff from the irrigated pastures. Sleepy Creek has entered into a Notice of Intent to Implement Water Quality BMPs with the Florida Department of Agriculture and Consumer Services which is incorporated in the NMP and which requires the implementation of Best Management Practices.2/ Dr. Bottcher testified that implementation and compliance with the Water Quality Best Management Practices manual creates a presumption of compliance with water quality standards. His testimony in that regard is consistent with Department of Agriculture and Consumer Services rule 5M-11.003 (“implementation, in accordance with adopted rules, of BMPs that have been verified by the Florida Department of Environmental Protection as effective in reducing target pollutants provides a presumption of compliance with state water quality standards.”). Rotational Grazing Rotational grazing is a practice by which cattle are allowed to graze a pasture for a limited period of time, after which they are “rotated” to a different pasture. The 1,656 acres proposed for irrigation on the North Tract are to be divided into 15 center-pivot pastures. Each individual pasture will have 10 fenced paddocks. The 611 acres of irrigated pasture on the East Tract are divided into 6 center-pivot pastures. The outer fence for each irrigated pasture is to be a permanent “hard” fence. Separating the internal paddocks will be electric fences that can be lowered to allow cattle to move from paddock to paddock, and then raised after they have moved to the new paddock. The NMP for the North Tract provides that cattle are to be brought into individual irrigated pastures as a single herd of approximately 190 cattle and placed into one of the ten paddocks. They will be moved every one to three days to a new paddock, based upon growing conditions and the reduction in grass height resulting from grazing. In this way, the cattle are rotated within the irrigated pasture, with each paddock being used for one to three days, and then rested until each of the other paddocks have been used, whereupon it will again be used in the rotation. The East Tract NMP generally provides for rotation based on the height of the pasture grasses, but is designed to provide a uniform average of cattle per acre per year. Due to the desire to “mine” phosphorus deposited during the years of operation of the East Tract as a sod farm, the density of cattle on the irrigated East Tract pastures is about 30 percent less than that proposed for the North Tract. The East Tract NMP calls for a routine pasture rest period of 15 to 30 days. Unlike dairy farm pastures, where dairy cows traverse a fixed path to the milking barn several times a day, there will be minimal “travel lanes” within the pastures or between paddocks. There will be no travel lanes through wetlands. If nitrogen-based fertilizer is needed, based upon tissue analysis of the grass, fertilizer is proposed for application immediately after a paddock is vacated by the herd. By so doing, the grass within each paddock will have a sufficient period to grow and “flush up” without grazing or traffic, which results in a high—quality grass when the cattle come back around to feed. Sleepy Creek proposes that rotational grazing is to be practiced on improved pastures and irrigated pastures alike. The rotational practices on the improved East Tract and North Tract pastures are generally similar to those practiced on the irrigated pastures. The paddocks will have permanent watering troughs, with one trough serving two adjacent paddocks. The troughs will be raised to prevent “boggy areas” from forming around the trough. Since the area around the troughs will be of a higher use, Sleepy Creek proposes to periodically remove accumulated manure, and re-grade if necessary. Other cattle support items, including feed bunkers and shade structures are portable and can be moved as conditions demand. Forage Crop Production The primary forage crop on the irrigated pastures is to be Bermuda grass. Bermuda grass or other grass types tolerant of drier conditions will be used in unirrigated pastures. During the winter, when Bermuda grass stops growing, Sleepy Creek will overseed the North Tract pastures with ryegrass or other winter crops. Due to the limitation on irrigation water, the East Tract NMP calls for no over-seeding for production of winter crops. Crops do not grow uniformly during the course of a year. Rather, there are periods during which there are excess crops, and periods during which the crops are not growing enough to keep up with the needs of the cattle. During periods of excess, Sleepy Creek will cut those crops and store them as haylage to be fed to the cattle during lower growth periods. The North Tract management plan allows Sleepy Creek to dedicate one or more irrigated pastures for the exclusive production of haylage. If that option is used, cattle numbers will be reduced in proportion to the number of pastures dedicated to haylage production. As a result of the limit on irrigation, the East Tract NMP does not recommend growing supplemental feed on dedicated irrigation pivot pastures. Direct Wetland Impacts Approximately 100 acres proposed for irrigation are wetlands or wetland buffer. Those areas are predominantly isolated wetlands, though some have surface water connections to Mill Creek, a water of the state. Trees will be cut in the wetlands to allow the pivot to pass overhead. Tree cutting is an exempt agricultural activity that does not require a permit. There was no persuasive evidence that cutting trees will alter the fundamental benefit of the wetlands or damage water resources of the District. The wetlands and wetland buffer will be subject to the same watering and fertigation regimen as the irrigated pastures. The application of water to wetlands, done concurrently with the application of water to the pastures, will occur during periods in which the pasture soils are dry. The incidental application of water to the wetlands during dry periods will serve to maintain hydration of the wetlands, which is considered to be a benefit. Fertilizers will be applied through the irrigation arms, a process known as fertigation. Petitioners asserted that the application of fertilizer onto the wetlands beneath the pivot arms could result in some adverse effects to the wetlands. However, Petitioners did not quantify to what extent the wetlands might be affected, or otherwise describe the potential effects. Fertigation of the wetlands will promote the growth of wetland plants. Nitrogen applied through fertigation will be taken up by plants, or will be subject to denitrification -- a process discussed in greater detail herein -- in the anaerobic wetland soils. The preponderance of the evidence indicated that enhanced wetland plant growth would not rise to a level of concern. Since most of the affected wetlands are isolated wetlands, there is expected to be little or no discharge of nutrients from the wetlands. Even as to those wetlands that have a surface water connection, most, if not all of the additional nitrogen applied through fertigation will be accounted for by the combined effect of plant uptake and denitrification. Larger wetland areas within an irrigated pasture will be fenced at the buffer line to prevent cattle from entering. The NMP provided a blow-up of the proposed fencing related to a larger wetland on Pivot 8. Although other figures are not to the same scale, it appears that larger wetlands associated with Pivots 1, 2, 3, and 12 will be similarly fenced. Cattle would be allowed to go into the smaller, isolated wetlands. Cattle going into wetlands do not necessarily damage the wetlands. Any damage that may occur is a function of density, duration, and the number of cattle. The only direct evidence of potential damage to wetlands was the statement that “[i]f you have 6,371 [cattle] go into a wetland, there may be impacts.” The NMP provides that pasture use will be limited to herds of approximately 190 cattle, which will be rotated from paddock to paddock every two to three days, and which will allow for “rest” periods of approximately 20 days. There will be no travel lanes through any wetland. Thus, there is no evidence to support a finding that the cattle at the density, duration, and number proposed will cause direct adverse effects to wetlands on the property. High Concentration Areas Cattle brought to the facility are to be unloaded from trucks and temporarily corralled for inspection. For that period, the cattle will be tightly confined. Cattle that have reached their slaughter weight will be temporarily held in corrals associated with the processing plant. The stormwater retention ponds used to capture and store runoff from the offloading corral and the processing plant holding corral are part of a normal and customary agricultural activity, and are not part of the applications and approvals that are at issue in this proceeding. The retention ponds associated with the high-intensity areas do not require permits because they do not exceed one acre in size or impound more than 40 acre-feet of water. Nonetheless, issues related to the retention ponds were addressed by Petitioners and Sleepy Creek, and warrant discussion here. The retention ponds are designed to capture 100 percent of the runoff and entrained nutrients from the high concentration areas for a minimum of a 24—hour/25—year storm event. If rainfall occurs in excess of the designed storm, the design is such that upon reaching capacity, only new surface water coming to the retention pond will be discharged, and not that containing high concentrations of nutrients from the initial flush of stormwater runoff. Unlike the stormwater retention berms for the pastures, which are to be constructed from the first nine inches of permeable topsoil on the property, the corral retention ponds are to be excavated to a depth of six feet which, based on soil borings in the vicinity, will leave a minimum of two to four feet of clay beneath the retention ponds. In short, the excavation will penetrate into the clay layer underlying the pond sites, but will not penetrate through that layer. The excavated clay will be used to form the side slopes of the ponds, lining the permeable surficial layer and generally making the ponds impermeable. Organic materials entering the retention ponds will form an additional seal. An organic seal is important in areas in which retention ponds are constructed in sandy soil conditions. Organic sealing is less important in this case, where clay forms the barrier preventing nutrients from entering the surficial aquifer. Although the organic material is subject to periodic removal, the clay layer will remain to provide the impermeable barrier necessary to prevent leakage from the ponds. Dr. Bottcher testified that if, during excavation of the ponds, it was found that the remaining in-situ clay layer was too thin, Sleepy Creek would implement the standard practice of bringing additional clay to the site to ensure adequate thickness of the liner. Nutrient Balance The goal of the NMP is to create a balance of nutrients being applied to and taken up from the property. Nitrogen and phosphorus are the nutrients of primary concern, and are those for which specific management standards are proposed. Nutrient inputs to the NMP consist generally of deposition of cattle manure (which includes solid manure and urine), recycling of plant material and roots from the previous growing season, and application of supplemental fertilizer. Nutrient outputs to the NMP consist generally of volatization of ammonia to the atmosphere, uptake and utilization of the nutrients by the grass and crops, weight gain of the cattle, and absorption and denitrification of the nutrients in the soil. The NMP, and the various models discussed herein, average the grass and forage crop uptake and the manure deposition to match that of a 1,013 pound animal. That average weight takes into account the fact that cattle on the property will range from calf weight of approximately 850 pounds, to slaughter weight of 1150 pounds. Nutrients that are not accounted for in the balance, e.g., those that become entrained in stormwater or that pass through the plant root zone without being taken up, are subject to runoff to surface waters or discharge to groundwater. Generally, phosphorus not taken up by crops remains immobile in the soil. Unless there is a potential for runoff to surface waters, the nutrient balance is limited by the amount of nitrogen that can be taken up by the crops. Due to the composition of the soils on the property, the high water table, and the relatively shallow confining layer, there is a potential for surface runoff. Thus, the NMP was developed using phosphorus as the limiting nutrient, which results in nutrient application being limited by the “P-index.” A total of 108 pounds of phosphorus per acre/per year can be taken up and used by the irrigated pasture grasses and forage crops. Therefore, the total number of cattle that can be supported on the irrigated pastures is that which, as a herd, will deposit an average of 108 pounds of phosphorus per year over the irrigated acreage. Therefore, Sleepy Creek has proposed a herd size and density based on calculations demonstrating that the total phosphorus contained in the waste excreted by the cattle equals the amount taken up by the crops. A herd producing 108 pounds per acre per year of phosphorus is calculated to produce 147 pounds of nitrogen per acre per year. The Bermuda grass and forage crops proposed for the irrigated fields require 420 pounds of nitrogen per acre per year. As a result of the nitrogen deficiency, additional nitrogen-based fertilizer to make up the shortfall is required to maintain the crops. Since phosphorus needs are accounted for by animal deposition, the fertilizer will have no phosphorus. The NMP requires routine soil and plant tissue tests to determine the amount of nitrogen fertilizer needed. By basing the application of nitrogen on measured rather than calculated needs, variations in inputs, including plant decomposition and atmospheric deposition, and outputs, including those affected by weather, can be accounted for, bringing the full nutrient balance into consideration. The numeric values for crop uptakes, manure deposition, and other estimates upon which the NMP was developed were based upon literature, values, and research performed and published by the University of Florida and the Natural Resource Conservation Service. Dr. Bottcher testified convincingly that the use of such values is a proven and reliable method of developing a balance for the operation of similar agricultural operations. A primary criticism of the NMP was its expressed intent to “reduce” or “minimize” the transport of nutrients to surface waters and groundwater, rather than to “negate” or “prevent” such transport. Petitioners argue that complete prevention of the transport of nutrients from the property is necessary to meet the standards necessary for issuance of the CUP and ERP. Mr. Drummond went into some detail regarding the total mass of nutrients expected to be deposited onto the ground from the cattle, exclusive of fertilizer application. In the course of his testimony, he suggested that the majority of the nutrients deposited on the land surface “are going to make it to the surficial aquifer and then be carried either to the Floridan or laterally with the groundwater flow.” However, Mr. Drummond performed no analysis on the fate of nitrogen through uptake by crops, volatization, or soil treatment, and did not quantify the infiltration of nitrogen to groundwater. Furthermore, he was not able to provide any quantifiable estimate on any effect of nutrients on Mill Creek, the Ocklawaha River, or Silver Springs. In light of the effectiveness of the nutrient balance and other elements of the NMP, along with the retention berm system that will be discussed herein, Mr. Drummond’s assessment of the nutrients that might be expected to impact water resources of the District is contrary to the greater weight of the evidence. Mr. Drummond’s testimony also runs counter to that of Dr. Kincaid, who performed a particle track analysis of the fate of water recharge from the North Tract. In short, Dr. Kincaid calculated that of the water that makes it as recharge from the North Tract to the surficial aquifer, less than one percent is expected to make its way to the upper Floridan aquifer, with that portion originating from the vicinity of Pivot 6. Recharge from the other 14 irrigated pastures was ultimately accounted for by evapotranspiration or emerged at the surface and found its way to Mill Creek. The preponderance of the competent, substantial evidence adduced at the final hearing supports the effectiveness of the NMPs for the North Tract and East Tract at managing the application and use of nutrients on the property, and minimizing the transport of nutrients to surface water and groundwater resources of the District. North Central Florida Model All of the experts involved in this proceeding agreed that the use of groundwater models is necessary to simulate what might occur below the surface of the ground. Models represent complex systems by applying data from known conditions and impacts measured over a period of years to simulate the effects of new conditions. Models are imperfect, but are the best means of predicting the effects of stresses on complex and unseen subsurface systems. The North Central Florida (NCF) model is used to simulate impacts of water withdrawals on local and regional groundwater levels and flows. The NCF model simulates the surficial aquifer, the upper Floridan aquifer, and the lower Floridan aquifer. Those aquifers are separated from one another by relatively impervious confining units. The intermediate confining unit separates the surficial aquifer from the upper Floridan aquifer. The intermediate confining unit is not present in all locations simulated by the NCF model. However, the evidence is persuasive that the intermediate confining unit is continuous at the North Tract, and serves to effectively isolate the surficial aquifer from the upper Floridan aquifer. The NCF model is not a perfect depiction of what exists under the land surface of the North Tract or elsewhere. It was, however, acknowledged by the testifying experts in this case, despite disagreements as to the extent of error inherent in the model, to be the best available tool for calculating the effects of withdrawals of water within the boundary of the model. The NCF model was developed and calibrated over a period of years, is updated routinely as data becomes available, and has undergone peer review. Aquifer Performance Tests In order to gather site-specific data regarding the characteristics of the aquifer beneath the Sleepy Creek property, a series of three aquifer performance tests (APTs) was conducted on the North Tract. The first two tests were performed by Sleepy Creek, and the third by the District. An APT serves to induce stress on the aquifer by pumping from a well at a high rate. By observing changes in groundwater levels in observation wells, which can be at varying distances from the extraction well, one can extrapolate the nature of the subsurface. In addition, well-completion reports for the various withdrawal and observation wells provide actual data regarding the composition of subsurface soils, clays, and features of the property. The APT is particularly useful in evaluating the ability of the aquifer to produce water, and in calculating the transmissivity of the aquifer. Transmissivity is a measure of the rate at which a substance passes through a medium and, as relevant to this case, measures how groundwater flows through an aquifer. The APTs demonstrated that the Floridan aquifer is capable of producing water at the rate requested. The APT drawdown contour measured in the upper Floridan aquifer was greater than that predicted from a simple run of the NCF model, but the lateral extent of the drawdown was less than predicted. The most reasonable conclusion to be drawn from the combination of greater than expected drawdown in the upper Floridan aquifer with less than expected extent is that the transmissivity of the aquifer beneath the North Tract is lower than the NCF model assumptions. The conclusion that the transmissivity of the aquifer at the North Tract is lower than previously estimated means that impacts from groundwater extraction would tend to be more vertical than horizontal, i.e., the drawdown would be greater, but would be more localized. As such, for areas of lower than estimated transmissivity, modeling would over-estimate off-site impacts from the extraction. NCF Modeling Scenarios The initial NCF modeling runs were based on an assumed withdrawal of 2.39 mgd, an earlier -- though withdrawn - - proposal. The evidence suggests that the simulated well placement for the 2.39 mgd model run was entirely on the North Tract. Thus, the results of the model based on that withdrawal have some limited relevance, especially given that the proposed CUP allows for all of the requested 1.46 mgd of water to be withdrawn from North Tract wells at the option of Sleepy Creek, but will over-predict impacts from the permitted rate of withdrawal. A factor that was suggested as causing a further over-prediction of drawdown in the 2.39 mgd model run was the decision, made at the request of the District, to exclude the input of data of additional recharge to the surficial aquifer, wetlands and surface waters from the irrigation, and the resulting diminution in soil storage capacity. Although there is some merit to the suggestion that omitting recharge made the model results “excessively conservative,” the addition of recharge to the model would not substantially alter the predicted impacts. A model run was subsequently performed based on a presumed withdrawal of 1.54 mgd, a rate that remains slightly more than, but still representative of, the requested amount of 1.46 mgd. The 1.54 mgd model run included an input for irrigation recharge. The simulated extraction points were placed on the East Tract and North Tract in the general configuration as requested in the CUP application. The NCF is designed to model the impacts of a withdrawal based upon various scenarios, identified at the hearing as Scenarios A, B, C, and D. Scenario A is the baseline condition for the NCF model, and represents the impacts of all legal users of water at their estimated actual flow rates as they existed in 1995. Scenario B is all existing users, not including the applicant, at end-of-permit allocations. Scenario C is all existing users, including the applicant, at current end-of-permit allocations. Scenario D is all permittees at full allocation, except the applicant which is modeled at the requested (i.e., new or modified) end-of-permit allocation. To simulate the effects of the CUP modification, simulations were performed on scenarios A, C, and D. In order to measure the specific impact of the modification of the CUP, the Scenario C impacts to the surficial, upper Floridan, and lower Floridan aquifers were compared with the Scenario D impacts to those aquifers. In order to measure the cumulative impact of the CUP, the Scenario A actual-use baseline condition was compared to the Scenario D condition which predicts the impacts of all permitted users, including the applicant, pumping at full end-of-permit allocations. The results of the NCF modeling indicate the following: 2.39 mgd - Specific Impact The surficial aquifer drawdown from the simulated 2.39 mgd withdrawal was less than 0.05 feet on-site and off- site, except to the west of the North Tract, at which a drawdown of 0.07 feet was predicted. The upper Floridan aquifer drawdown from the 2.39 mgd withdrawal was predicted at between 0.30 and 0.12 feet on-site, and between 0.30 and 0.01 feet off-site. The higher off-site figures are immediately proximate to the property. The lower Floridan aquifer drawdown from the 2.39 mgd withdrawal was predicted at less than 0.05 feet at all locations, and at or less than 0.02 feet within six miles of the North Tract. 2.39 mgd - Cumulative Impact The cumulative impact to the surficial aquifer from all permitted users, including a 2.39 mgd Sleepy Creek withdrawal, was less than 0.05 feet on-site, and off-site to the north and east, except to the west of the North Tract, at which a drawdown of 0.07 feet was predicted. The cumulative impact to the upper Floridan aquifer from all permitted users, including a 2.39 mgd Sleepy Creek withdrawal, ranged from 0.4 feet to 0.8 feet over all pertinent locations. The cumulative impact to the lower Floridan aquifer from all permitted users, including a 2.39 mgd Sleepy Creek withdrawal, ranged from 1.0 to 1.9 feet over all pertinent locations. The conclusion drawn by Mr. Andreyev that the predicted impacts to the lower Floridan are almost entirely from other end-of-permit user withdrawals is supported by the evidence and accepted. 1.54 mgd - Specific Impact The NCF model runs based on the more representative 1.54 mgd withdrawal predicted a surficial aquifer drawdown of less than 0.01 feet (i.e., no drawdown contour shown) on the North Tract, and a 0.01 to 0.02 foot drawdown at the location of the East Tract. The drawdown of the upper Floridan aquifer from the CUP modification was predicted at up to 0.07 feet on the property, and generally less than 0.05 feet off-site. There were no drawdown contours at the minimum 0.01 foot level that came within 9 miles of Silver Springs. The lower Floridan aquifer drawdown from the CUP modification was predicted at less than 0.01 feet (i.e., no drawdown contour shown) at all locations. 1.54 mgd - Cumulative Impact A comparison of the cumulative drawdown contours for the 2.36 mgd model and 1.54 mgd model show there to be a significant decrease in predicted drawdowns to the surficial and upper Floridan aquifers, with the decrease in the upper Floridan aquifer drawdown being relatively substantial, i.e., from 0.5 to 0.8 feet on-site predicted for the 2.36 mgd withdrawal, to 0.4 to 0.5 feet on-site for the 1.54 mgd model. Given the small predicted individual impact of the CUP on the upper Floridan aquifer, the evidence is persuasive that the cumulative impacts are the result of other end-of-permit user withdrawals. The drawdown contour for the lower Floridan aquifer predicted by the 1.54 mgd model is almost identical to that of the 2.36 mgd model, thus supporting the conclusion that predicted impacts to the lower Floridan are almost entirely from other end-of-permit user withdrawals. Modeled Effect on Silver Springs As a result of the relocation of the extraction wells from the East Tract to the North Tract, the NCF model run at the 1.54 mgd withdrawal rate predicted springflow at Silver Springs to increase by 0.15 cfs. The net cumulative impact in spring flow as measured from 1995 conditions to the scenario in which all legal users, including Sleepy Creek, are pumping at full capacity at their end-of-permit rates for one year3/ is roughly 35.4 cfs, which is approximately 5 percent of Silver Springs’ current flow. However, as a result of the redistribution of the Sleepy Creek withdrawal, which is, in its current iteration, a legal and permitted use, the cumulative effect of the CUP modification at issue is an increase in flow of 0.l5 cfs. Dr. Kincaid agreed that there is more of an impact to Silver Springs when the pumping allowed by the CUP is located on the East Tract than there is on the North Tract, but that the degree of difference is very small. Dr. Knight testified that effect on the flow of Silver Springs from relocating the 1.46 mgd withdrawal from the East Tract to the North Tract would be “zero.” The predicted increase of 0.15 cfs is admittedly miniscule when compared to the current Silver Springs springflow of approximately 675 cfs. However, as small as the modeled increase may be -- perhaps smaller than its “level of certainty” -- it remains the best evidence that the impact of the CUP modification to the flow of Silver Springs will be insignificant at worst, and beneficial at best. Opposition to the NCF Model Petitioners submitted considerable evidence designed to call the results generated by the District’s and Sleepy Creek’s NCF modeling into question. Karst Features A primary criticism of the validity of the NCF model was its purported inability to account for the presence of karst features, including conduits, and their effect on the results. It was Dr. Kincaid’s opinion that the NCF model assigned transmissivity values that were too high, which he attributed to the presence of karst features that are collecting flow and delivering it to springs. He asserted that, instead of assuming the presence of karst features, the model was adjusted to raise the overall capacity of the porous medium to transmit water, and thereby match the observed flows. In his opinion, the transmissivity values of the equivalent porous media were raised so much that the model can no longer be used to predict drawdowns. That alleged deficiency in the model is insufficient for two reasons. First, as previously discussed in greater detail, the preponderance of the evidence in this case supports a finding that there are no karst features in the vicinity of the North Tract that would provide preferential pathways for water flow so as to skew the results of the NCF model. Second, Dr. Kincaid, while acknowledging that the NCF model is the best available tool for predicting impacts from groundwater extraction on the aquifer, suggested that a hybrid porous media and conduit model would be a better means of predicting impacts, the development of which would take two years or more. There is no basis for the establishment of a de facto moratorium on CUP permitting while waiting for the development of a different and, in this case, unnecessary model. For the reasons set forth herein, it is found that the NCF model is sufficient to accurately and adequately predict the effects of the Sleepy Creek groundwater withdrawals on the aquifers underlying the property, and to provide reasonable assurance that the standards for such withdrawals have been met. Recharge to the Aquifer Petitioners argued that the modeling results showing little significant drawdown were dependent on the application of unrealistic values for recharge or return flow from irrigation. In a groundwater model, as in the physical world, some portion of the water extracted from the aquifer is predicted to be returned to the aquifer as recharge. If more water is applied to the land surface than is being accounted for by evaporation, plant uptake and evapotranspiration, surface runoff, and other processes, that excess water may seep down into the aquifer as recharge. Recharge serves to replenish the aquifer and offset the effects of the groundwater withdrawal. Dr. Kincaid opined that the NCF modeling performed for the CUP application assigned too much water from recharge, offsetting the model's prediction of impacts to other features. It is reasonable to assume that there is some recharge associated with both agricultural and public supply uses. However, the evidence suggests that the impact of recharge on the overall NCF model results is insignificant on the predicted impacts to Silver Springs, the issue of primary concern. Mr. Hearn ran a simulation using the NCF model in which all variables were held constant, except for recharge. The difference between the “with recharge” and “without recharge" simulations at Silver Springs was 0.002 cfs. That difference is not significant, and is not suggestive of adverse impacts on Silver Springs from the CUP modification. Dr. Kincaid testified that “the recharge offset on the property is mostly impacting the surficial aquifer,” and that “the addition of recharge in this case didn't have much of an impact on the upper Floridan aquifer system.” As such, the effect of adding recharge to the model would be as to the effect of groundwater withdrawal on wetlands or surface water bodies, and not on springs. As previously detailed, the drawdown of the surficial aquifer simulated for the 2.39 mgd “no recharge” scenario were less than 0.05 feet on-site and off-site, except for a predicted 0.07 foot drawdown to the west of the North Tract. The predicted drawdown of the surficial aquifer for the 1.54 mgd “with recharge” scenario was 0.02 feet or less. The preponderance of the evidence supports a finding that drawdowns of either degree are less than that at which adverse impacts to wetlands or surface waters would occur. Thus, issues related to the recharge or return flows from irrigation are insufficient to support a finding or conclusion that the NCF model failed to provide reasonable assurance that the standards for issuance of the CUP modification were met. External Boundaries The boundaries of the NCF model are not isolated from the rest of the physical world. Rather, groundwater flows into the modeled area from multiple directions, and out of the modeled area in multiple directions. Inflows to the model area are comprised of recharge, which is an assigned value, and includes water infiltrating and recharging the aquifer from surface waters; injection wells; upward and downward leakage from lower aquifers; and flow across the external horizontal boundaries. Outflows from the model area include evapotranspiration; discharge to surface waters, including springs and rivers; extraction from wells; upward and downward leakage from lower aquifers; and flow against the external model boundaries. Dr. Kincaid testified that flow across the external model boundary is an unknown and unverifiable quantity which increases the uncertainty in the model. He asserted that in the calibrated version of the model, there is no way to check those flows against data. His conclusion was that the inability of the NCF model to accurately account for external boundary flow made the margin of error so great as to make the model an unreliable tool with which to assess whether the withdrawal approved by the proposed CUP modification will increase or decrease drawdown at Silver Springs. The District correlates the NCF model boundaries with a much larger model developed by the United States Geological Survey, the Peninsula of Florida Model, more commonly referred to as the Mega Model, which encompasses most of the State of Florida and part of Southeast Georgia. The Mega Model provides a means to acknowledge that there are stresses outside the NCF model, and to adjust boundary conditions to account for those stresses. The NCF is one of several models that are subsets of the Mega Model, with the grids of the two models being “nested” together. The 1995 base year of the NCF model is sufficiently similar to the 1993-1994 base year of the Mega Model as to allow for a comparison of simulated drawdowns calculated by each of the models. By running a Mega Model simulation of future water use, and applying the change in that use from 1993 base year conditions, the District was able to come to a representative prediction of specific boundary conditions for the 1995 NCF base year, which were then used as the baseline for simulations of subsequent conditions. In its review of the CUP modification, the District conducted a model validation simulation to measure the accuracy of the NCF model against observed conditions, with the conditions of interest being the water flow at Silver Springs. The District ran a simulation using the best information available as to water use in the year 2010, the calculated boundary conditions, irrigation, pumping, recharge, climatic conditions, and generally “everything that we think constitutes that year.” The discharge of water at Silver Springs in 2010 was measured at 580 cfs. The discharge simulated by the NCF model was 545 cfs. Thus, the discharge predicted by the NCF model simulation was within six percent of the observed discharge. Such a result is generally considered in the modeling community to be “a home run.” Petitioners’ objections to the calculation of boundary conditions for the NCF model are insufficient to support a finding that the NCF model is not an appropriate and accurate tool for determining that reasonable assurance has been provided that the standards for issuance of the CUP modification were met. Cumulative Impact Error As part of the District’s efforts to continually refine the NCF, and in conjunction with a draft minimum flows and levels report for Silver Springs and the Silver River, the cumulative NCF model results for the period of baseline to 2010 were compared with the simulated results from the Northern District Model (NDF), a larger model that overlapped the NCF. As a result of the comparison, which yielded different results, it was discovered that the modeler had “turned off” not only the withdrawal pumps, but inputs to the aquifer from drainage wells and sinkholes as well. When those inputs were put back into the model run, and effects calculated only from withdrawals between the “pumps-off” condition and 2010 pumping conditions, the cumulative effect of the withdrawals was adjusted from a reduction in the flow at Silver Springs of 29 cfs to a reduction of between 45 and 50 cfs, an effect described as “counterintuitive.” Although that result has not undergone peer review, and remains subject to further review and comparison with the Mega Model, it was accepted by the District representative, Mr. Bartol. Petitioners seized upon the results of the comparison model run as evidence of the inaccuracy and unreliability of the NCF model. However, the error in the NCF model run was not the result of deficiencies in the model, but was a data input error. Despite the error in the estimate of the cumulative effect of all users at 2010 levels, the evidence in this case does not support a finding that the more recent estimates of specific impact from the CUP at issue were in error. NCF Model Conclusion As has been discussed herein, a model is generally the best means by which to calculate conditions and effects that cannot be directly observed. The NCF model is recognized as being the best tool available for determining the subsurface conditions of the model domain, having been calibrated over a period of years and subject to peer review. It should be recognized that the simulations run using the NCF model represent the worst—case scenario, with all permittees simultaneously drawing at their full end-of-permit allocations. There is merit to the description of that occurrence as being “very remote.” Thus, the results of the modeling represent a conservative estimate of potential drawdown and impacts. While the NCF model is subject to uncertainty, as is any method of predicting the effects of conditions that cannot be seen, the model provides reasonable assurance that the conditions simulated are representative of the conditions that will occur as a result of the withdrawals authorized by the CUP modification. Environmental Resource Permit The irrigation proposed by the CUP will result in runoff from the North Tract irrigated pastures in excess of that expected from the improved pastures, due in large measure to the diminished storage capacity of the soil. Irrigation water will be applied when the soils are dry, and capable of absorbing water not subject to evaporation or plant uptake. The irrigation water will fill the storage space that would exist without irrigation. With irrigation water taking up the capacity of the soil to hold water, soils beneath the irrigation pivots will be less capable of retaining additional moisture during storm events. Thus, there is an increased likelihood of runoff from the irrigated pastures over that expected with dry soils. The increase in runoff is expected to be relatively small, since there should be little or no irrigation needed during the normal summer wet season. The additional runoff may have increased nutrient levels due to the increased cattle density made possible by the irrigation of the pastures. The CUP has a no—impact requirement for water quality resulting from the irrigation of the improved pasture. Thus, nutrients leaving the irrigated pastures may not exceed those calculated to be leaving the existing pre-development use as improved pastures. Retention Berms The additional runoff and nutrient load is proposed to be addressed by constructing a system of retention berms, approximately 50,0004/ feet in length, which is intended to intercept, retain, and provide treatment for runoff from the irrigated pasture. The goal of the system is to ensure that post—development nutrient loading from the proposed irrigated pastures will not exceed the pre—development nutrient loading from the existing improved pastures. An ERP permit is required for the construction of the berm system, since the area needed for the construction of the berms is greater than the one acre in size, and since the berms have the capability of impounding more than 40 acre-feet of water. The berms are to be constructed by excavating the top nine inches of sandy, permeable topsoil and using that permeable soil to create the berms, which will be 1 to 2 feet in height. The water storage areas created by the excavation will have flat or horizontal bottoms, and will be very shallow with the capacity to retain approximately a foot of water. The berms will be planted with pasture grasses after construction to provide vegetative cover. The retention berm system is proposed to be built in segments, with the segment designed to capture runoff from a particular center pivot pasture to be constructed prior to the commencement of irrigation from that center pivot. A continuous clay layer underlies the areas in which the berms are to be constructed. The clay layer varies from 18 to 36 inches below the ground surface, with at least one location being as much as five feet below the ground surface. As such, after nine inches of soil is scraped away to create the water retention area and construct the berm, there will remain a layer of permeable sandy material above the clay. The berms are to be constructed at least 25 feet landward of any jurisdictional wetland, creating a “safe upland line.” Thus, the construction, operation, and maintenance of the retention berms and redistribution swales will result in no direct impacts to jurisdictional wetlands or other surface waters. There will be no agricultural activities, e.g., tilling, planting, or mowing, within the 25-foot buffers, and the buffers will be allowed to establish with native vegetation to provide additional protection for downgradient wetlands. As stormwater runoff flows from the irrigated pastures, it may, in places, create concentrated flow ways. Redistribution swales will be built in those areas to spread any remaining overland flow of water and reestablish sheet flow to the retention berm system. At any point at which water may overtop a berm, the berm will be hardened with rip—rap to insure its integrity. The berms are designed to intercept and collect overland flow from the pastures and temporarily store it behind the berms, regaining the soil storage volume lost through irrigation. A portion of the runoff intercepted by the berm system will evaporate. The majority will infiltrate either through the berm, or vertically into the subsurface soils beneath it. When the surficial soils become saturated, further vertical movement will be stopped by the impermeable clay layer underlying the site. The runoff water will then move horizontally until it reemerges into downstream wetland systems. Thus, the berm system is not expected to have a measurable impact on the hydroperiod of the wetlands on the North Tract. Phosphorus Removal Phosphorus tends to get “tied up” in soil as it moves through it. Phosphorus reduction occurs easily in permeable soil systems because it is removed from the water through a chemical absorption process that is not dependent on the environment of the soil. As the soils in the retention areas and berms go through drying cycles, the absorption capacity is regenerated. Thus, the retention system will effectively account for any increase in phosphorus resulting from the increased cattle density allowed by the irrigation such that there is expected to be no increase in phosphorus levels beyond the berm. Nitrogen Removal When manure is deposited on the ground, primarily as high pH urine, the urea is quickly converted to ammonia, which experiences a loss of 40 to 50 percent of the nitrogen to volatization. Soil conditions during dry weather conditions are generally aerobic. Remaining ammonia in the manure is converted by aerobic bacteria in the soil to nitrates and nitrites. Converted nitrates and nitrites from manure, along with nitrogen from fertilizer, is readily available for uptake as food by plants, including grasses and forage crops. Nitrates and nitrites are mobile in water. Therefore, during rain events of sufficient intensity to create runoff, the nitrogen can be transported downstream towards wetlands and other receiving waters, or percolate downward through the soil until blocked by an impervious barrier. During storm events, the soils above the clay confining layer and the lower parts of the pervious berms become saturated. Those saturated soils are drained of oxygen and become anaerobic. When nitrates and nitrites encounter saturated conditions, they provide food for anaerobic bacteria that exist in those conditions. The bacteria convert nitrates and nitrites to elemental nitrogen, which has no adverse impact on surface waters or groundwater. That process, known as denitrification, is enhanced in the presence of organic material. The soils from which the berms are constructed have a considerable organic component. In addition to the denitrification that occurs in the saturated conditions in and underlying the berms, remaining nitrogen compounds that reemerge into the downstream wetlands are likely to encounter organic wetland-type soil conditions. Organic wetland soils are anaerobic in nature, and will result in further, almost immediate denitrification of the nitrates and nitrites in the emerging water. Calculation of Volume - BMPTRAINS Model The calculation of the volume necessary to capture and store excess runoff from the irrigated pastures was performed by Dr. Wanielista using the BMPTRAINS model. BMPTRAINS is a simple, easy to use spreadsheet model. Its ease of use does not suggest that it is less than reliable. The model has been used as a method of calculating storage volumes in many conditions over a period of more than 40 years. The model was used to calculate the storage volumes necessary to provide storage and treatment of runoff from fifteen “basins” that had a control or a Best Management Practice associated with them. All of the basins were calculated as being underlain by soils in poorly-drained hydrologic soil Group D, except for the basin in the vicinity of Pivot 6, which is underlain by the more well-drained soil Group A. The model assumed about percent of the property to have soil Group A soils, an assumption that is supported by the evidence. Soil moisture conditions on the property were calculated by application of data regarding rainfall events and times, the irrigation schedule, and the amount of irrigation water projected for use over a year. The soil moisture condition was used to determine the amount of water that could be stored in the on-site soils, known as the storage coefficient. Once the storage coefficient was determined, that data was used to calculate the amount of water that would be expected to run off of the North Tract, known as the curve number. The curve number is adjusted by the extent to which the storage within a soil column is filled by the application of irrigation water, making it unable to store additional rainfall. As soil storage goes down, the curve number goes up. Thus, a curve number that approaches 100 means that more water is predicted to run off. Conversely, a lower curve number means that less water is predicted to run off. The pre-development curve number for the North Tract was based on the property being an unirrigated, poor grass area. A post-development curve number was assigned to the property that reflected a wet condition representative of the irrigated soils beneath the pivots. In calculating the storage volume necessary to handle runoff from the basins, the wet condition curve number was adjusted based on the fact that there is a mixture of irrigated and unirrigated general pasture within each basin to be served by a segment of the retention berm system, and by the estimated 15 percent of the time that the irrigation areas would be in a drier condition. In addition, the number was adjusted to reflect the 8 to 10 inches of additional evapotranspiration that occurs as a result of irrigation. The BMPTRAINS model was based on average annual nutrient-loading conditions, with water quality data collected at a suitable point within Reach 22, the receiving waterbody. The effects of nutrients from the irrigated pastures on receiving waterbodies is, in terms of the model, best represented by average annual conditions, rather than a single highest-observed nutrient value. Pre-development loading figures were based on the existing use of the property as unirrigated general pasture. The pre-development phosphorus loading figure was calculated at an average event mean concentration (EMC) of 0.421 milligrams per liter (mg/l). The post—condition phosphorus loading figure was calculated at an EMC of 0.621 mg/l. Therefore, in order to achieve pre-development levels of phosphorus, treatment to achieve a reduction in phosphorus of approximately 36 percent was determined to be necessary. The pre-development nitrogen loading figure was calculated at an EMC of 2.6 mg/l. The post—condition nitrogen loading figure was calculated at an EMC of 3.3 mg/l. Therefore, in order to achieve pre-development levels of nitrogen, treatment to achieve a reduction in nitrogen of approximately 25 percent was determined to be necessary. The limiting value for the design of the retention berms is phosphorus. To achieve post-development concentrations that are equal to or less than pre-development concentrations, the treatment volume of the berm system must be sufficient to allow for the removal of 36 percent of the nutrients in water being retained and treated behind the berms, which represents the necessary percentage of phosphorus. In order to achieve the 36 percent reduction required for phosphorus, the retention berm system must be capable of retaining approximately 38 acre—feet of water from the 15 basins. In order to achieve that retention volume, a berm length of approximately 50,000 linear feet was determined to be necessary, with an average depth of retention behind the berms of one foot. The proposed length of the berms is sufficient to retain the requisite volume of water to achieve a reduction in phosphorus of 36 percent. Thus, the post-development/irrigation levels of phosphorus from runoff are expected to be no greater than pre-development/general pasture levels of phosphorus from runoff. By basing the berm length and volume on that necessary for the treatment of phosphorus, there will be storage volume that is greater than required for a 25 percent reduction in nitrogen. Thus, the post-development/irrigation levels of nitrogen from runoff are expected to be less than pre- development/general pasture levels of nitrogen from runoff. Mr. Drummond admitted that the design of the retention berms “shows there is some reduction, potentially, but it's not going to totally clean up the nutrients.” Such a total clean-up is not required. Rather, it is sufficient that there is nutrient removal to pre-development levels, so that there is no additional pollutant loading from the permitted activities. Reasonable assurance that such additional loading is not expected to occur was provided. Despite Mr. Drummond’s criticism of the BMPTRAINS model, he did not quantify nutrient loading on the North Tract, and was unable to determine whether post-development concentrations of nutrients would increase over pre-development levels. As such, there was insufficient evidence to counter the results of the BMPTRAINS modeling. Watershed Assessment Model In order to further assess potential water quantity and water quality impacts to surface water bodies, and to confirm stormwater retention area and volume necessary to meet pre-development conditions, Sleepy Creek utilized the Watershed Assessment Model (WAM). The WAM is a peer-reviewed model that is widely accepted by national, state, and local regulatory entities. The WAM was designed to simulate water balance and nutrient impacts of varying land uses. It was used in this case to simulate and provide a quantitative measure of the anticipated impacts of irrigation on receiving water bodies, including Mill Creek, Daisy Creek, the Ocklawaha River, and Silver Springs. Inputs to the model include land conditions, soil conditions, rain and climate conditions, and water conveyance systems found on the property. In order to calculate the extent to which nutrients applied to the land surface might affect receiving waters, a time series of surface water and groundwater flow is “routed” through the modeled watershed and to the various outlets from the system, all of which have assimilation algorithms that represent the types of nutrient uptakes expected to occur as water goes through the system. Simulations were performed on the North Tract in its condition prior to acquisition by Sleepy Creek, in its current “exempted improved pasture condition,” and in its proposed “post—development” pivot-irrigation condition. The simulations assessed impacts of the site conditions on surface waters at the point at which they leave the property and discharge to Mill Creek, and at the point where Mill Creek merges into the Ocklawaha River. The baseline condition for measuring changes in nutrient concentrations was determined to be that lawfully existing at the time the application was made. Had there been any suggestion of illegality or impropriety in Sleepy Creek’s actions in clearing the timber and creating improved pasture, a different baseline might be warranted. However, no such illegality or impropriety was shown, and the SJRWMD rules create no procedure for “looking back” to previous land uses and conditions that were legally changed. Thus, the “exempted improved pasture condition” nutrient levels are appropriate for comparison with irrigated pasture nutrient levels. The WAM simulations indicated that nitrogen resulting from the irrigation of the North Tract pastures would be reduced at the outflow to Mill Creek at the Reach 22 stream segment from improved pasture levels by 1.7 percent in pounds per year, and by 0.6 percent in milligrams per liter of water. The model simulations predicted a corresponding reduction at the Mill Creek outflow to the Ocklawaha River of 1.3 percent in pounds per year, and 0.5 percent in milligrams per liter of water. These levels are small, but nonetheless support a finding that the berm system is effective in reducing nitrogen from the North Tract. Furthermore, the WAM simulations showed levels of nitrogen from the irrigated pasture after the construction of the retention berms to be reduced from that present in the pre- development condition, a conclusion consistent with that derived from the BMPTRAINS model. The WAM simulations indicated that phosphorus from the irrigated North Tract pastures, measured at the outflow to Mill Creek at the Reach 22 stream segment, would be reduced from improved pasture levels by 3.7 percent in pounds per year, and by 2.6 percent in milligrams per liter of water. The model simulations predicted a corresponding reduction at the Mill Creek outflow to the Ocklawaha River of 2.5 percent in pounds per year, and 1.6 percent in milligrams per liter of water. Those levels are, again, small, but supportive of a finding of no impact from the permitted activities. The WAM simulations showed phosphorus in the Ocklawaha River at the Eureka Station after the construction of the retention berms to be slightly greater than those simulated for the pre-development condition (0.00008 mg/l) -- the only calculated increase. That level is beyond miniscule, with impacts properly characterized as “non- measurable” and “non-detectable.” In any event, total phosphorus remains well below Florida’s nutrient standards. The WAM simulations were conducted based on all of the 15 pivots operating simultaneously at full capacity. That amount is greater than what is allowed under the permit. Thus, according to Dr. Bottcher, the predicted loads are higher than those that would be generated by the permitted allocation, making his estimates “very conservative.” Dr. Bottcher’s testimony is credited. During the course of the final hearing, the accuracy of the model results was questioned based on inaccuracies in rainfall inputs due to the five-mile distance of the property from the nearest rain station. Dr. Bottcher admitted that given the dynamics of summer convection storms, confidence that the rain station rainfall measurements represent specific conditions on the North Tract is limited. However, it remains the best data available. Furthermore, Dr. Bottcher testified that even if specific data points simulated by the model differ from that recorded at the rain station, that same error carries through each of the various scenarios. Thus, for the comparative purpose of the model, the errors get “washed out.” Other testimony regarding purported inaccuracies in the WAM simulations and report were explained as being the result of errors in the parameters used to run alternative simulations or analyze Sleepy Creek’s simulations, including use of soil types that are not representative of the North Tract, and a misunderstanding of dry weight/wet weight loading rates. There was agreement among witnesses that the WAM is regarded, among individuals with expertise in modeling, as an effective tool, and was the appropriate model for use in the ERP application that is the subject of this proceeding. As a result, the undersigned accepts the WAM simulations as being representative of comparative nutrient impacts on receiving surface water bodies resulting from irrigation of the North Tract. The WAM confirmed that the proposed retention berm system will be sufficient to treat additional nutrients that may result from irrigation of the pastures, and supports a finding of reasonable assurance that water quality criteria will be met. With regard to the East Tract, the WAM simulations showed that there would be reductions in nitrogen and phosphorus loading to Daisy Creek from the conversion of the property to irrigated pasture. Those simulations were also conservative because they assumed the maximum number of cattle allowed by the nutrient balance, and did not assume the 30 percent reduction in the number of cattle under the NMP so as to allow existing elevated levels of phosphorus in the soil from the sod farm to be “mined” by vegetation. Pivot 6 The evidence in this case suggests that, unlike the majority of the North Tract, a small area on the western side of the North Tract drains to the west and north. Irrigation Pivot is within that area. Dr. Harper noted that there are some soils in hydrologic soil Group A in the vicinity of Pivot 6 that reflect soils with a deeper water table where rainfall would be expected to infiltrate into the ground. Dr. Kincaid’s particle track analysis suggested that recharge to the surficial aquifer ultimately discharges to Mill Creek, except for recharge at Pivot 11, which is accounted for by evapotranspiration, and recharge at Pivot 6. Dr. Kincaid concluded that approximately 1 percent of the recharge to the surficial aquifer beneath the North Tract found its way into the upper Floridan aquifer. Those particle tracks originated only on the far western side of the property, and implicated only Pivot 6, which is indicative of the flow divide in the Floridan aquifer. Of the 1 percent of particle tracks entering the Floridan aquifer, some ultimately discharged at the St. John’s River, the Ocklawaha River, or Mill Creek. Dr. Kincaid opined, however, that most ultimately found their way to Silver Springs. Given the previous finding that the Floridan aquifer beneath the property is within the Silver Springs springshed for less than a majority of the time, it is found that a correspondingly small fraction of the less than 1 percent of the particle tracks originating on the North Tract, perhaps a few tenths of one percent, can reach Silver Springs. Dr. Bottcher generally agreed that some small percentage of the water from the North Tract may make it to the upper Floridan aquifer, but that amount will be very small. Furthermore, that water reaching the upper Floridan aquifer would have been subject to the protection and treatment afforded by the NMP and the ERP berms. The evidence regarding the somewhat less restrictive confinement of the aquifer around Pivot 6 is not sufficient to rebut the prima facie case that the CUP modification, coupled with the ERP, will meet the District’s permitting standards. Public Interest The primary basis upon which Sleepy Creek relies to demonstrate that the CUP is “consistent with the public interest” is that Florida's economy is highly dependent upon agricultural operations in terms of jobs and economic development, and that there is a necessity of food production. Sleepy Creek could raise cattle on the property using the agriculturally-exempt improved pastures, but the economic return on the investment would be questionable without the increased quality, quantity, and reliability of grass and forage crop production resulting from the proposed irrigation. Sleepy Creek will continue to engage in agricultural activities on its properties if the CUP modification is denied. Although a typical Florida beef operation could be maintained on the property, the investment was based upon having the revenue generation allowed by grass-fed beef production in order to realize a return on its capital investment and to optimize the economic return. If the CUP modification is denied, the existing CUP will continue to allow the extraction of 1.46 mgd for use on the East Tract. The preponderance of the evidence suggests that such a use would have greater impacts on the water levels at Silver Springs, and that the continued use of the East Tract as a less stringently-controlled sod farm would have a greater likelihood of higher nutrient levels, particularly phosphorus levels which are already elevated.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law set forth herein it is RECOMMENDED that the St. Johns River Water Management District enter a final order: approving the issuance of Consumptive Use Permit No. 2-083-91926-3 to Sleepy Creek Lands, LLC on the terms and conditions set forth in the complete Permit Application for Consumptive Uses of Water and the Consumptive Use Technical Staff Report; and approving the issuance of Environmental Resource Permit No. IND-083-130588-4 to Sleepy Creek Lands, LLC on the terms and conditions set forth in the complete Joint Application for Individual and Conceptual Environmental Resource Permit and the Individual Environmental Resource Permit Technical Staff Report. DONE AND ENTERED this 29th day of April, 2015, in Tallahassee, Leon County, Florida. S E. GARY EARLY 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 29th day of April, 2015.
Findings Of Fact THE PARTIES The Respondent is the successor agency to the Florida Department of Environmental Regulation and has permitting authority over the subject project pursuant to Chapter 403, Florida Statutes. The Respondent's file number for this matter is 311765419. Petitioner, Alden Pond, Inc., is a subsidiary of First Union National Bank of Florida and is the successor in interest to Orchid Island Associates. John C. Kurtz is the designated property manager for this project and appeared at the formal hearing as Alden Pond's authorized agent. THE PROPERTY AND THE VICINITY Petitioner has record title to all of Government Lot 9 in Section 15, Township 31 South, Range 39 East, less the Jungle Trail Road right of way, and all of Government Lots 2, 3, 6, and 7, Section 22, Township 31 South, Range 39 East, less the road right of way for State Road 510. Petitioner does not own land below the mean high water line of the Indian River, which forms the western boundary of the property. Much of the property, approximately the northern half, abuts a part of the Indian River that has been leased by the State of Florida to the United States Fish and Wildlife Service as part of the Pelican Island National Wildlife Refuge. The Pelican Island National Wildlife Refuge was the first national wildlife refuge established in the United States and has been declared to be a water of international importance. Upland of the proposed project is a golf course and residential development. The Indian River at the project site is within the Indian River Aquatic Preserve, which is classified as Class II Outstanding Florida Waters. The Indian River in the vicinity of the project is part of the Intercoastal Waterway system, is navigable by large vessels, and is an important travel corridor for manatees. The Indian River in the vicinity of the project is a healthy estuarine system. Minor deviations from Respondent's dissolved oxygen standards have been recorded. These minor deviations are typical and represent natural conditions for this type of system. Water quality sampling from March 1994 yielded no samples in which deviations from Respondent's dissolved oxygen standards were observed. THE ORIGINAL PROJECT On February 21, 1990, Orchid Island Associates submitted to the Respondent an application for a wetland resource permit to construct a boat basin and canal on its property adjacent to the Indian River. The artificial waterway that Petitioner proposes to construct on its property will, for ease of reference, also be referred to as a canal. Petitioner proposes to dredge from the north terminus of the canal to the Intercoastal Waterway a channel, which will be referred to as the hydrological channel. Petitioner proposes to dredge from the south terminus of the canal to the Intercoastal Waterway a channel, which will be referred to as the access channel. The original project involved, among other features, a canal approximately 6,400 feet long, the dredging of the hydrological channel and the access channel, the construction of 44 docks to be located along the eastern side of the canal, and the dredging of an area adjacent to the canal for a 58 slip marina. The width of the canal was to range between 100 and 200 feet. The original project required the filling of 4.72 acres of wetlands and the dredging of 8.81 acres of wetlands for a direct impact on 13.53 acres of wetlands. On January 15, 1991, Respondent issued a preliminary evaluation letter pertaining to the initial application that contained the following conclusion: "the project cannot be recommended for approval." On September 12, 1991, Respondent issued a Notice of Permit Denial dated September 12, 1991, which stated that the application would be denied. This denial letter did not suggest any revisions that would make the project permittable and represented a strong position by the Respondent that the project as originally proposed should be denied. The September 12, 1991, Notice of Denial correctly described the project site and the initial proposal as follows: . . . The proposed project is located north of and adjacent to County Road 510, north and east of Wabasso Bridge and adjacent to the eastern shore of the Indian River. The Indian River at the project site is within the Indian River Aquatic Preserve, which is classified as Class II, Outstanding Florida Waters. The Pelican Island National Wildlife Refuge, also an aquatic preserve and an Outstanding Florida Water, is immediately west of the project site. Historically, the site of the marina and its associated upland development consisted of a wetland adjacent to the Indian River and a large citrus grove. Subsequently, the wetland was surrounded by a dike and impounded for mosquito control purposes. At some point in the past, a borrow pit 1/ was excavated within the landward (eastern) edge of the impounded wetland. Most of the citrus grove has been converted to a residential community associated with a golf course. * * * The proposed project included excavation of a 6,400 linear ft. canal along the upland/wetland edge between the impoundment and the adjacent upland, dredging the existing borrow pit to a depth of -8 ft. NGVD to create a boat basin that will connect it to the excavated canal, construction of 58 boat slips within the excavated boat basin, excavation of two flushing channels through a portion of the impoundment dike and wetlands within the impoundment to connect the excavated channel to the Indian River and a natural lake within the impoundment, excavation of a 700 ft. long access channel to connect the excavated canal to the Intercoastal Waterway through the seagrass beds along the southern boundary of the project site, filling of 4.72 ac. of wetlands at three locations within the impoundment to create uplands, and construction of a boardwalk along the southern edge of the excavated canal through the wetlands in the impoundment to provide access to the marina basin. To mitigate for the loss of wetlands, the applicant proposes to enhance 68 ac. of wetlands within the mosquito impoundment by returning the impoundment berm to grade and implementing a rotary ditching project and open marsh mosquito management to improve the hydrology of the wetlands in the impoundment, planting high marsh species, and donating the enhanced wetlands to the State of Florida for incorporation into the Pelican Island National Wildlife Refuge through a lease to the United States Fish and Wildlife Service. The September 12, 1991, Notice of Denial provided, in pertinent part, the following reasons for the denial of the project: The Department hereby denies the permit for the following reasons: Water quality data for the Indian River adjacent to the project site indicates that the dissolved oxygen (D.O.) standard is not currently being met. The proposed 8 ft. deep canal and marina basin to the Indian River would be expected to result in introduction of additional low D.O. waters into a system which already does not meet the D.O. standard, thereby resulting in further degradation of the water quality in the Indian River. In addition to the D.O. problem, the project would result in water quality degradation due to the pollutant loading of marina related pollutants from the boats docked at the 58 slips that are proposed as part of the project in the marina basin. Additional water quality degradation also may result from boats that are moored at docks that may be constructed at a later date by the owners of the 44 lots adjacent to the canal, pursuant to the exemption in Section 403.813(2)(b), Florida Statutes. This exemption provides that private docks in artificially constructed waters are exempt from dredge and fill permitting and may be constructed without a permit providing they meet the size criteria listed in the statute and provided they do not impede navigation, affect flood control, or cause water quality violations. The boats in the canal system and boat basin would be a chronic source of pollutants for the life of the facility. The proposed water depths and slip sizes will make the basin accessible for use by large boats which can be expected to have on-board sanitation devices. The hydrographic report submitted by the applicant indicates the proposed waters will flush with a 2.6 hr. duration. Although this flushing rate will prevent water quality pollutants from being concentrated in the waters of the basin, it also will have the effect of transporting boat related pollutants to the Indian River, thereby causing degradation of the Outstanding Florida Water. The project site is within Class II Waters, prohibited for shellfish harvesting, but is adjacent to Class II Waters, approved for shellfish harvesting. Discussion with the Department of Natural Resources, Bureau of Regulation and Development, indicates that the pollutant loading from the project would probably cause the adjacent waters to be reclassified as "prohibited for shellfish harvesting." The reclassification of the adjacent waters would lower the existing use of the waterbody. Rules 17-302.300(1), (4), , and (6), Florida Administrative Code, state that: Section 403.021, Florida Statutes, declares that the public policy of the State is to conserve the waters of the State to protect, maintain, and improve the quality thereof for public water supplies, for the propagation of wildlife, fish and other aquatic life, and for domestic, agricultural, industrial, recreational, and other beneficial uses. It also prohibits the discharge of wastes into Florida waters without treatment necessary to protect those beneficial uses of the waters. * * * Existing uses and the level of water quality necessary to protect the existing uses shall be fully maintained and protected. Such uses may be different or more extensive than the designated use. Pollution which causes or contributes to new violations of water quality standards or to continuation of existing violations is harmful to the waters of this State and shall not be allowed. Waters having water quality below the criteria established for them shall be protected and enhanced. However, the Department shall not strive to abate natural conditions. If the Department finds that a new or existing discharge will reduce the quality of the receiving waters below the classification established for them or violate any Department rule or standard, it shall refuse to permit the discharge. As a result of the above cited factors, degradation of water quality is expected. The applicant has not provided reasonable assurance that the immediate and long-term impacts of the project will not result in the degradation of existing water quality in an Outstanding Florida Water and the violation of water quality standards pursuant to Rules 17-312.080(1) and (3), Florida Administrative Code, and Rule 17-4.242(2)(a)2.b, Florida Administrative Code. Specific State Water Quality Standards in Rules 17-302.500, 17-302.510 and 17-302.550, Florida Administrative Code, affected by the completion of the project include the following: Bacteriological Quality - the median coliform MPN (Most Probable Number) of water shall not exceed seventy (70) per hundred (100) milliliters, and not more than ten percent (10 percent) of the samples shall exceed a MPN of two hundred and thirty (230) per one hundred (100) milliliters. The fecal coliform bacterial level shall not exceed a median value of 14 MPN per 100 milliliters with not more than ten percent (10 percent) of the samples exceeding 43 MPN per 100 milliliters. Dissolved Oxygen - the concentration in all waters shall not average less than 5 milligrams per liter in a 24-hour period and shall never be less than 4 milligrams per liter. Normal daily and seasonal fluctuations above these levels shall be maintained. Oils and Greases: Dissolved or emulsified oils and greases shall not exceed 5.0 milligrams per liter. No undissolved oil, or visible oil defined as iridescence, shall be present so as to cause taste or odor, or otherwise interfere with the beneficial use of waters. In addition the applicant has not provided reasonable assurance that ambient water quality in the OFW will not be degraded pursuant to Rule 17-4.242(2)(a)2.b, Florida Administrative Code. In addition, pursuant to Rule 17-312.080(6)(a), Florida Administrative Code, the Department shall deny a permit for dredging or filling in Class II waters which are not approved for shellfish harvesting unless the applicant submits a plan or proposes a procedure to protect those waters and waters in the vicinity. The plan or procedure shall detail the measures to be taken to prevent significant damage to the immediate project areas and to adjacent area and shall provide reasonable assurance that the standards for Class II waters will not be violated. In addition to impacts to water quality, the project is expected to adversely affect biological resources. A portion (estimated at between 0.4 and 0.5 ac.) of the access channel alignment is vegetated by seagrasses, the dominant species being Halodule wrightii (Cuban shoal weed). Seagrass beds provide important habitat and forage for a variety of wildlife species. The loss of seagrass beds will result in a loss of productivity to the entire system that would be difficult to replace. The 4.72 ac. of wetlands proposed to be filled and the excavation required for the proposed channels (approximately 38 ac.) are productive high marsh and mixed mangrove wetlands which are providing wildlife habitat and water quality benefits. These wetlands have been adversely impacted by the freeze of 1989, but they appear to be recovering well. The proposed mitigation would provide some benefits through exotic removal and increased hydrologic connection to the Indian River. However, these benefits would not be adequate to offset the adverse impacts of the proposed wetland losses for this project. The project site and the adjacent Pelican Island National Wildlife Refuge are used for nesting and foraging by a variety of species, including little blue heron (Egretta caerulea) (Species of Special Concern (SSC)--Florida Game and Fresh Water fish Commission (FGFWFC)), reddish egret (E. rufescens) (SSC-FGFWFC), snowy egrets (E. thula) (SSC-FGFWFC), tricolored herons (E. tricolor) (SSC-FGFWFC), brown pelicans (Pelecanus occidentalis) (SSC-FGFWFC), roseate spoonbills (Ajaja ajaja) (SSC-FGFWFC), least tern (Sterna antillarum) (threatened-FGFWFC), and wood storks (endangered-FGFWFC). The construction of the project and the increased boating activity due to the project would result in the disturbance of those species that use the wetlands in the project area. The Indian River adjacent to the project site is used by the West Indian Manatee (endangered-FGFWFC). The increased boat traffic would increase the chance of manatee deaths due to boat impact. In addition, the excavation of the access channel through the seagrass beds would decrease the available forage for manatees in the project area. For the above reasons, this project is also not clearly in the public interest, as required pursuant to Section 403.918(2), Florida Statutes, because it is expected to: adversely affect the conservation of fish and wildlife, including endangered or threatened species, or their habitats; adversely affect the fishing or recreational values or marine productivity in the vicinity of the project; be permanent in nature; diminish the current condition and relative value of functions being performed by areas affected by the proposed activity. The applicant has not provided reasonable assurance that the project is clearly in the public interest. On September 12, 1991, the owner and holder of the mortgage on the Orchid Island development (which includes the real property on which the Petitioner hopes to construct the project at issue in this proceeding) instituted foreclosure proceedings. The circuit judge who presided over the foreclosure proceeding soon thereafter appointed an interim receiver to manage the property until a receiver who would manage the property for the duration of the foreclosure proceeding could be appointed. THE PROJECT MODIFICATIONS AND FACTS AS TO ESTOPPEL On October 31, 1991, representatives of Orchid Island Associates met with Respondent's staff to discuss this application. Trudie Bell, the Environmental Specialist assigned to supervise this application, and Douglas MacLaughlin, an attorney employed by Respondent, attended the meeting. Those attending the meeting on behalf of Orchid Island Associates included the interim trustee, the attorney for Orchid Island Associates, and Darrell McQueen, who at all times pertinent to this proceeding was the project engineer. Mr. McQueen was upset that the project was going to be denied and wanted to know what could be done to make it a permittable project. In response to Mr. McQueen, Ms. Bell, without making any promises, suggested the following modifications to the project that might make it permittable: moving the canal more upland, elimination of the boat basin/marina, reducing the depth of the artificial waterway, and increasing the width of the littoral zone. On November 11, 1991, the representatives of Orchid Island Associates responded to the Respondent's suggested modifications and agreed to make the modifications. In an effort to design a project that would be acceptable to Respondent, Orchid Island Associates proposed to the Respondent to make certain modifications to the design of the project. Petitioner has agreed to those modifications which include the following: Elimination of the boat basin and associated 58 dock marina and clubhouse, but with the addition of 18 relatively narrow residential lots, each of which would have a dock on the south end of the waterway. 2/ Reduction of the depth of the artificial waterway to -7 feet NGVD from the proposed -8 feet NGVD. Realignment of the artificial waterway as depicted on the sealed drawings submitted to Respondent and dated January 28, 1993. Increasing the width of the littoral zone to be created along the length of the artificial waterway to 40 feet on the west side and 10 feet on the east side. On November 12, 1991, John C. Kurtz was appointed the receiver of the Orchid Island Associates property and remained the receiver until the property was conveyed to Petitioner at a foreclosure sale on July 31, 1993. After it acquired the property, Petitioner employed Mr. Kurtz to manage the subject property. Mr. Kurtz has been active in the project since his appointment as the receiver of the property. On November 21, 1991, Petitioner met with Respondent's staff, including Ms. Bell, to discuss the modifications. At that meeting, the Respondent's staff reacted favorably to the modifications agreed to by Petitioner. Ms. Bell described the revisions as "excellent" and "a great idea" and stated that the project was "a nice project" and that it looked like the project was heading in the right direction. Ms. Bell also represented that the Respondent would grant the Petitioner extensions of time to allow for a formal revision if the project was deemed permittable. Ms. Bell kept her superiors informed of the status of her review. On December 11, 1991, Charles Barrowclaugh, an employee of the Respondent, made an inspection of the site and informed representatives of the Petitioner that he had briefed Carol Browner, who was Secretary of the Department of Environmental Regulation, as to the project and the proposed modifications. Mr. Barrowclaugh stated that he believed the project was permittable. Petitioner was encouraged by Mr. Barrowclaugh's comments and by the fact that he would incur the expenses of traveling to the site. Between December 11, 1991, and November 13, 1992, Petitioner provided information to Respondent pertaining to the revised project. This additional information included a description of the revised plan and a revised schematic drawing, but it did not include detailed drawings of the revised project. On November 13, 1992, Ms. Bell wrote to Mr. McQueen a letter that stated, in pertinent part, as follows: The Bureau of Wetland Resource Management has reviewed the revised plan and additional information submitted on September 16. The revised proposal appears to address all of the issues that made the original proposal unpermittable. The detailed 8.5 by 11 inch permitting drawings will have to be revised to reflect the revised proposal and submitted to the Bureau for review. Kelly Custer and Orlando Rivera will be reviewing the project in the future. Petitioner interpreted that letter to mean that the Respondent intended to permit the project. At the time she wrote the letter of November 13, 1992, Ms. Bell thought the revised project would be permitted. Petitioner relied on the oral representations made by Respondent's staff and on the November 13, 1992, letter in continuing pursuit of a permit. Absent these encouraging comments by Respondent's staff, Petitioner would have discontinued pursuit of the permit. Although Petitioner was understandably encouraged by the discussions its representatives had with Respondent's staff, it knew, or should have known, that the favorable comments it was receiving from members of Respondent's staff were preliminary and that additional information would be required and further evaluation of the project would take place. Petitioner's representatives knew that the staff with whom they were having these discussions did not have the authority to approve the application, but that they could only make recommendations to their superiors. In late 1992, Kevin Pope, an Environmental Specialist employed by Respondent, was assigned as the primary reviewer of the revised project. At the time he became the primary reviewer of the project, Mr. Pope did not make an immediate, independent evaluation of the project, and relied on what other staffers who had been involved in the review told him. Until he conducted his own review of the project, Mr. Pope believed that the project was "clearly permissible". Mr. Pope informed a representative of the Petitioner of that belief and told the representative that he was prepared to start drafting the permit once he received final drawings documenting the modifications to the project. Subsequent to that conversation, Mr. Pope received the drawings he requested. After he received and reviewed the final drawings, Mr. Pope determined that all issues raised by the denial letter had not been addressed. Among the concerns he had was the fact that the project would dredge into the Indian River to the Intercoastal Waterway and that part of the dredging activity (at the north end of the project) would be in Class II shellfish approved waters. Mr. Pope again contacted the state and federal agencies that had originally commented on the project, described the proposed modifications to the project, and requested comments. Most of the agencies continued to object to the project. On August 5, 1992, Mr. Pope held a meeting with the commenting agencies and with representatives of the Petitioner to discuss the objections to the project. 3/ The agencies provided additional comments after this meeting and most continued to oppose the project. Mr. Kurtz testified that on June 1, 1993, Stacey Callahan, an attorney employed by Respondent, told him that she was attempting to draft the permit for the project. Ms. Callahan asked for sample wording for a restrictive covenant or for an easement that would limit the number of boats that could use the proposed docks. Subsequent to that inquiry, Petitioner was informed by Mr. Pope that the project would be denied. Petitioner has not made any specific proposal to assure a limitation on the number of boats that will be able to dock in the proposed canal. In June of 1993, a large number of objections to the project were filed with Respondent by members of the public. In early July, 1993, Secretary Wetherell responded to those objectors with a letter stating, in part, that the "Department's letter of November 1992 indicating an intent to issue for the project was imminent appears to have been premature." On September 20, 1993, Mr. Pope informed Petitioner's attorney that the Respondent was not going to change its position that the project, even with the modifications, should be denied. The decision not to permit the modified project was made by Mr. Pope. The only permit application filed by the Petitioner was the application for the initial permit. No formal amended application that incorporates all of the changes that Petitioner discussed with Respondent's staff was filed. A total of $74,735 was spent on behalf of the applicant on this project between December 26, 1991, (the date of the meeting with Mr. Barrowclaugh) and July 31, 1993, (the date the property was conveyed to Petitioner). From July 31, 1993, through April of 1994, Petitioner spent an additional $47,488 on the application for this project. The expenditures after July 31, 1993, included engineering costs that were incurred before that date. These figures do not include the costs of this proceeding. THE REVISED PROJECT The revised project may be summarily described as follows: Petitioner proposes to construct a canal that will be approximately 6,400 feet long, up to 200 feet wide, and -7 NGVD deep as depicted on drawings that have been submitted into evidence. There will be a littoral zone 40 feet wide on the west side of the canal and a littoral zone 10 feet wide on the east side. A hydrological channel, proposed from the north terminus of the canal to the Intercoastal Waterway to enable a proper flow of water through the canal, will be some 200 feet wide, 70 feet in length, and -3 NGVD. Petitioner proposes to construct a barrier at the north terminus of the canal to prevent manatees and boats from entering the canal from the north and has agreed to maintain that barrier. An access channel, proposed from the south terminus to the Intercoastal Waterway to enable boats access to the canal, will be some 200 feet wide, 700 feet in length, and -7 NGVD. A total of 62 docks are proposed. The project includes a mitigation plan that will be discussed below. THE REQUESTED VARIANCE The construction of the hydrological channel would be in Class II conditionally approved shellfish waters. Dredging in Class II conditionally approved shellfish waters is prohibited unless a variance is issued by Respondent that would permit this otherwise prohibited activity. Petitioner's attorney submitted a letter to the Respondent on August 18, 1993, for a variance to construct the channel from the north terminus of the canal to the Intercoastal Waterway. That letter stated, in pertinent part, as follows: DEP Rule 17-312.080(17) states: "Permits for dredging or filling directly in Class II or Class III waters which are approved for shellfish harvesting by the Department of Natural Resources shall not be issued." This provision is applicable to the pending application by Orchid Island Associates. Accordingly, we discussed Orchid Island requesting a variance pursuant to Section 403.201, Florida Statutes, and Rule 17-103.100, Florida Administrative Code, as a means of overcoming this prohibition. Since the dredge and fill application is pending, you indicated it would be appropriate for Orchid Island to ask, during final review of this application, that the Department also consider a request for a variance pursuant to the above mentioned statute and rule. Please consider this letter that request. . . . Petitioner did not submit along with its request the fee required by Respondent to process that request. Respondent did not advise Petitioner that it would not process its request without the requisite application fee until the prehearing stipulation was prepared for this proceeding shortly before the formal hearing. There was no evidence that Petitioner attempted to check on the status of its request for a variance or that it expected Respondent to act on the request for a variance independent of its final review of the overall project. As of the time of the formal hearing, Petitioner had not submitted to Respondent the fee that Respondent asserts is required before the request for the variance will be processed. Respondent asserted that position in the prehearing statement that was filed shortly before the formal hearing. The evidence as to the flow of water through the proposed canal assumed the existence of the hydrological channel from the north terminus of the proposed canal to the Intercoastal Waterway and the existence of the access channel from the south terminus of the proposed canal to the Intercoastal Waterway. CONSTRUCTION OF THE PROJECT The revised version of the artificial waterway will be excavated primarily from uplands, but the excavation will require that 3.6 acres of wetlands be filled and 7.1 acres of wetlands be dredged. The direct impact on wetlands will be at least 10.7 acres. The mitigation plan proposes that the berms around the mosquito impoundment will be leveled, the berm ditches will be filled, and certain rotary ditches will be dredged. The amount of wetlands to be impacted by that proposed activity was not established. The artificial waterway will be constructed utilizing a series of separate construction cells, a rim ditch, and filtration chambers. All excavated material will be disposed of on uplands. The construction system will filter most solids. Turbidity suppression devices will be used to minimize any turbidity associated with the excavation of the access channel at the south terminus and the hydrological channel at the north terminus. Petitioner established that its proposed construction techniques are consistent with best management practices. The small body of water that is referred to as the former borrow pit in the denial letter of September 12, 1991, is known as Boot Lake. Petitioner proposes to dredge the eastern end of Boot Lake, consisting of an area 800 feet by 180 feet (3.3 acres), to create part of the canal. The access channel at the south terminus of the canal will be approximately 700 feet in length and will have to be hydraulically excavated in the Indian River to connect the canal to the Intercoastal Waterway. The hydrological channel at the north terminus of the canal will be hydraulically excavated to connect the canal to the Indian River. The connection will require approximately 70 feet of dredging to -3 NGVD, which is the minimum necessary to maintain the proper flow of water through the canal. HYDROLOGY OF THE CANAL The artificial waterway will function as a flow-through system driven by a difference in the water surface elevation (the head difference) between the north terminus and the south terminus. The flushing of the artificial waterway far exceeds the Respondent's flushing requirement benchmark, which is a flushing time of four days. If a hypothetical pollutant's concentration is reduced to 10 percent of its initial concentration in four days, the flushing is considered to be acceptable. The flushing time for the system is approximately 2.6 hours, which will produce five total volume replacements per tidal cycle. The predicted flushing of the artificial waterway is quite rapid and energetic. The predominate flow of water in the artificial waterway is from north to south. At times, however, the flow will be from the south to the north. At the request of the Respondent, Petitioner conducted a tracer dye study within the Indian River at the proposed south terminus of the artificial waterway. No tracer dye study was requested for the north terminus. Although there was some disagreement as to the import of the tracer dye study, it established that pollutants introduced into the Indian River from the canal would be rapidly dispersed in the Indian River. WATER QUALITY - THE CANAL The artificial waterway will be classified as Class III waters of the State. Water quality within the artificial waterway will reflect the current water quality in the Indian River. Petitioner has provided reasonable assurances that the water quality within the artificial waterway itself will not violate state standards. Two potential sources of pollutants to the artificial waterway have been identified. The first source is stormwater runoff through the stormwater management system associated with the upland development. The second is pollution inherent with the docking and operation of large vessels. Respondent interprets its rules so that discharge of pollutants into the artificial waterway will constitute indirect discharges to the Indian River. Because of the excellent flushing capacity of the canal, pollutants will not tend to accumulate in the canal. A pollutant entering the canal or a spill of pollutants into the canal will mix very little in the canal, probably less than five percent, so the pollutant will discharge from the canal into the Indian River as a plug. There was a conflict in the evidence as to whether pollutants introduced into the canal will enter the Indian River in measurable quantities. Testimony was elicited from Dr. Roessler, one of Petitioner's experts, that water entering the Indian River from the artificial waterway will not contain pollutants that are either measurably or statistically differentiable from the Indian River itself. That result depends, however, on the amount and the source of the pollutant introduced into the canal. Because of the rapid flushing of the canal, small spills or slowly released discharges of pollutants are not expected to result in water quality degradation in the Indian River. Since a pollutant introduced into the canal will exit in a plug essentially in the same concentration as it entered the canal, Petitioner has not provided reasonable assurances that large spills or discharges of pollutants from vessels or from other sources will not be discharged into the Indian River in concentrations that can be measured or that such large spills or discharges will not degrade the quality of the Indian River. Water from the canal will come out of both the north end and the south end of the canal. Some of the plume coming out of the north end may tend to hug the shoreline, with some of the plume reentering the canal when the tides change. Stormwater runoff contains significant amounts of fecal coliform, sometimes more than raw sewage. The stormwater management system associated with the upland development was permitted by the St. Johns Water Management District. The majority of the system is currently in place and functioning to retain stormwater runoff. The stormwater management system is designed to retain all of the first 4.75 inches of rainfall and most of the first 6.2 inches of rainfall. The design of this system exceeds the requirements imposed by the St. Johns Water Management District, which is that the first 1.5 inches of rainfall be retained. Stormwater management regulations are technology-based treatment criteria. If a system meets the retention requirement, it is presumed that no water quality will be violated by discharges through the system. Petitioner established that the stormwater management system was designed and constructed to retain at least three times the amount of rainfall required by the St. Johns Water Management District. Construction of the proposed canal will intercept two stormwater discharge pipes from the upland golf course and residential development. There was no evidence that the St. Johns Water Management System has reviewed this change in the system that has been permitted. The proposed change in where the outflow will be discharged could be significant since the discharge pipes are presently designed to discharge overflows from the system into wetland areas that provided additional natural treatment of the overflow before the overflow reaches the Indian River. With this change the overflow will be discharged during extraordinary storm events into the canal and thereafter into the Indian River without additional natural treatment. Because there will be modifications to the stormwater system the approval of that system by the St. Johns Water Management District should not be relied upon as providing reasonable assurances that no water quality violations will be caused by stormwater discharge. If this project is to be permitted, Petitioner should be required as a condition precedent to the issuance of the permit to have the proposed changes to the system reviewed by the St. Johns Water Management District and it should be required to obtain an amendment to the stormwater management system permit that would authorize the proposed changes. The project contemplates the construction of 62 docks. The size and the docking capacity of each dock has not been established. While Petitioner presented testimony that it is likely that only 50 percent of the docks will likely be used at any one time, that testimony is considered to be speculative. The number and size of boats that can or will be docked in the canal at any one time or on a regular basis is unknown. It is likely that each dock will have docking capacity for at least one vessel up to 60 feet in length and for a smaller vessel. The manner in which these docks will be constructed was not established. Chromatic copper arsenic, which is frequently used to coat docks and anti-fouling paints containing heavy metals used on boats are sources of contamination to shellfishing. Oils and greases from boats contain hydrocarbons which can adversely impact shellfish. These contaminants can have adverse impacts to shellfish at very low concentrations. Petitioner has agreed to prohibit live-aboard vessels and to prohibit the fueling and maintenance of vessels within the artificial waterway. Sewage containing fecal coliform dumped or spilled from boats or from stormwater discharge is a primary source of contamination for shellfishing waters. It is the practice of the Respondent's Shellfish Environmental Assessment Section to close waters to shellfishing in the vicinity of marinas, mainly due to potential contamination from untreated sewage. The Shellfish Environmental Assessment Section does not recommend the immediate closing of shellfishing waters when a project involves single family docks associated with a residence because it assumes people will use bathroom facilities in the house instead of on the boat. The Respondent does not have reasonable assurances that there will be houses associated with each of the 50 foot lots designated at the southern end of the canal. If a proposed facility has boat docks, but does not have houses associated with each dock, the Shellfish Environmental Assessment Section would recommend closure of shellfishing in the vicinity of the facility. The Shellfish Environmental Assessment Section would not recommend immediate closure of the shellfishing waters in the vicinity of this proposed project because it has assumed that each of the proposed docks will be associated with a house. If this project is to be permitted, reasonable assurances should be required that a residence will be constructed before or contemporaneously with the construction of a dock. The modifications made by Petitioner to the project will reduce the danger of pollutants from vessels in the artificial waterway. However, because the number and the size of the vessels that will be using the artificial waterway was not established, the extent of pollutants from vessels is unknown. Consequently, it is concluded that Petitioner did not provide reasonable assurances that measurable pollutants would not indirectly discharge into the Indian River from the canal. IMPACT ON WETLANDS Of the approximately 10.70 acres of wetlands that will be directly impacted by the proposed waterway, 4.10 acres are predominately impacted by invasive exotic (non-native) plants, 4.27 acres are somewhat impacted by exotic plants, and 2.23 acres are not impacted by exotic plants. The exotic plants found at the project site are primarily Australian Pine and Brazilian Pepper. The mitigation plan, which will be discussed below, proposes that the berms constructed around the mosquito impoundment area be removed and the rim ditches that abut the berms be filled. The amount of wetlands to be impacted by that activity was not established. The project contemplates that rotary ditches will be constructed at different places in the mosquito impoundment area after the berms are removed and the berm ditches filled. The areas to be impacted by the construction of the rotary ditches were not identified. The Petitioner proposes to dredge out the entire east end of Boot Lake for use as part of the canal. This area will be approximately 800 feet by 180 feet and will be 3.3 acres. Boot Lake is a fairly healthy biological system, about the same as the Indian River. It was found to contain 22 species of fish and seven species of birds, with brown pelican and the great blue heron dominant. Eleven species of crustacean, six species of mollusks, 24 vermes 4/ and one coelenterate were collected from the lake. Replacement of the eastern portion of Boot Lake with the canal will adversely impact those species. Between the Indian River and the proposed waterway is a mosquito impoundment constructed in the early 1960s. The mosquito impoundment and associated berms total approximately 105 acres. The exact area was not established since there is an unresolved issue as to the exact location of the mean high water line. 5/ The impoundment is breached in several locations and no longer functions efficiently as a mosquito impoundment. IMPACTS ON SEAGRASSES The excavation of the access channel from the south terminus to the Intercoastal Waterway will involve the removal of approximately 2500 square feet of a healthy, productive seagrass bed. Seagrasses are beneficial for wildlife habitat as they provide a substrate for algae and diatoms. Seagrasses are a direct food source for manatees and other species, and provide shelter and protection for fish. Seagrasses observed in this area where grasses will be eliminated are Halodule writtii, Syringodium filiforme, and Halophia johnsonii. Halophia, one of the identified species in this seagrass bed, is designated by the Florida Natural Areas Inventory as a rare and endangered species. Besides the seagrasses actually eliminated where the channel is to be constructed, other nearby seagrasses are also likely to be affected. The sides of the channel are likely to slough to some degree, which would adversely impact the seagrasses abutting the channel. The operation of power boats, even at slow speeds, will cause turbidity that will likely adversely impact seagrasses. Maintenance dredging, which will be required every few years, will cause turbidity that will likely adversely impact seagrasses. There are presently thousands of acres of seagrasses located within the Indian River. There has been a historical decline in seagrass in the Indian River Lagoon. Since 1950, there has been a 30 percent loss of seagrasses and seagrass habitat. IMPACTS ON SHELLFISH The proposed project will have an adverse impact on shellfish and shellfishing. At a minimum, the project will require dredging in a shellfishing area. The hydrological channel that will be dredged to connect the north terminus of the canal with the Intercoastal Waterway will be located in Class II waters that have been conditionally approved for shellfishing. Both commercial and recreational shellfishing occur in the Indian River adjacent to the project site. The predominate flow of water through the canal will be southerly. There will be, however, a predictable northerly flow of waters that will cause waters from the proposed canal and any associated contaminants contained in those waters to flow from the north terminus of the canal into the Class II waters that have been conditionally approved for shellfishing. The proposed project may introduce a significant amount of freshwater into the adjoining shellfishing waters of Indian River, primarily in the vicinity of the north terminus of the canal. Any additional freshwater discharges to shellfishing waters is a concern because fecal coliform bacteria survive longer in freshwater than saltwater. Three likely sources of freshwater that would be added by this project to the Indian River in the conditionally approved shellfishing area were identified by Respondent. First, the proposed canal appears to be intersecting near its north terminus with a sulphur spring or artesian well which produces fresh water with a high sulphur content. Fresh water will likely be introduced into the canal from this source and discharged into the shellfishing waters when the tidal flow becomes northward. Second, freshwater may be introduced into the canal from the overflow pipes from the surface water management system. This source of freshwater would not be significant. Third, additional freshwater may enter the area after the berms around the mosquito impoundment area are removed as contemplated by the mitigation plan. The extent of this source of freshwater was not established. If this project is permitted, the Shellfish Environmental Assessment Section will monitor this area for water quality to determine if the area will have to be closed for shellfishing. This additional monitoring, for which Respondent will pay, will be required because of the potential adverse impacts this project presents to shellfishing. Because of evidence of deteriorating water quality, the Shellfish Environmental Assessment Section is recommending that the shellfishing waters adjacent to the site be reclassified from "conditionally approved" to "conditionally restricted". In "conditionally restricted" waters, shellfish can still be harvested, but the harvested shellfish have to be placed in designated waters or in on-land facilities so the shellfish can cleanse themselves of fecal coliform before going to market. The conditions in the area of the proposed project are not yet bad enough to prohibit shellfishing. IMPACT ON MANATEES There are approximately 2,000 manatees living in Florida waters, with approximately 1,000 living on the east coast and approximately 1,000 living on the west coast. The manatee is an endangered species, and the long-term survival of the species is not secure. The Indian River in the area of the proposed project provides good habitat for manatees and is a major travel corridor for several hundred manatees. Indian River County is one of 13 key counties that has been designated by the Governor and Cabinet to address special manatee concerns. Manatees traveling back and forth in this area usually use the channel of the Intercoastal Waterway because it is deeper and allows manatees an easier travel route. Speed zones for boat traffic are an effective manatee protection mechanism. The artificial waterway will be posted as an idle speed zone. The area where the access channel connecting the south terminus of the canal with the Intercoastal Waterway will be dredged is presently designated as a slow speed zone and the access channel itself will be marked. Petitioner has agreed to implement Respondent's standard manatee conditions. Seagrasses are an important source of food for manatees. The project contemplates that 0.05 acres of seagrass will be dredged, but that Spartina will be planted in parts of the littoral zone. While manatees eat Spartina to some extent, they prefer seagrasses. Since there are thousands of acres of seagrass located in the Indian River, it is concluded that the elimination of 0.05 acres of seagrass associated with this project is negligible and will not adversely affect manatees. A barrier to navigation will be maintained at the north terminus of the waterway to preclude boat access and limit access to the waterway by manatees. Manatees would be unable to enter or leave the artificial waterway via the north terminus. The artificial waterway will not attract manatees and should not, in and of itself, adversely impact manatees. The main adverse impact to manatees from this proposed project is the threat of collisions by boats that leave the canal and enter the waters of the Indian River, including the Intercoastal Waterway. At least ten West Indian manatees have been killed by boats in Indian River County since 1981. Even with the speed limits, the increase in boating in this area will present an increased risk to manatees. IMPACT ON BIRDS No species of wading birds, including those listed as endangered or threatened, nests or roosts within the project site. The project site is not currently heavily utilized by wading birds, but several species of wading birds were observed foraging for food in Boot Lake. It is reasonable to expect that dredging of Boot Lake and the increased boat traffic will have an adverse impact on birds. Diving birds, such as the brown pelican and least tern, will benefit from the increased open waterway created by the canal, which should serve as a feeding habitat. Wading birds congregate and nest in rookeries. The area of the proposed project is within the foraging range of 14 active rookeries, and it is reasonable to expect that those rookeries will be disturbed by the increased boat use or human activity that the project will bring to this area. Officials of Pelican Island National Wildlife Refuge have observed such disturbances and are opposed to this project. The pressure of human and boating activities on bird rookeries in the Pelican Island National Wildlife Refuge, including human intrusion into buffer zones established to protect the birds, has resulted in a continuing decline of the bird population since 1960. When disturbed by boats or by humans, the parent wading bird will often leave the nest, which exposes the eggs or the chicks to attack by predators or to overexposure to sunlight. Boaters will often cause wading birds who are foraging for food to flush, which disturbs their search for food. Certain species of wading birds are flushed more frequently and for longer distances when flushed from narrow tidal creeks in Spartina marshes (a habitat similar to the proposed canal) than in open shoreline habitat. IMPACT ON FISH The existing ditches inside the mosquito impoundment berms presently provide a habitat similar to that of a tidal creek for a variety of fish, including juvenile snook, tarpon, red drum, black drum, lady fish, and mullet. The proposed project will result in the filling of these habitats and impoundments. As a consequence of that activity, these species of fish will be adversely impacted by the project. Although Petitioner proposes to construct certain rotary ditches that it asserts would provide a habitat similar to that provided by the existing ditches, Petitioner has not submitted any plans or drawings or other specific information concerning these rotary ditches and has not provided reasonable assurances that these proposed rotary will replace the habitat that will be eliminated by the filling of the existing ditches. CUMULATIVE IMPACTS Other projects have been permitted on the Indian River north and south of the proposed project that have increased boat traffic on the Indian River in the vicinity of the project. The Respondent has not identified any similar projects which have been permitted in the vicinity within the last five years. The only similar application pending before the Respondent in the vicinity of the project is for two docks north of the project site. Although Respondent established that boat traffic on the Indian River has increased, this project is unique in scope and design, and it is concluded that Petitioner has given reasonable assurances that no negative cumulative impacts will be associated with the project. OTHER PERMITTING CRITERIA The parties stipulated to the following facts that pertain to permitting criteria: The project will not adversely affect navigation or the flow of water. The project will not cause harmful erosion or shoaling. The project will be of a permanent nature. The project will not adversely affect any significant historical or archaeological resources. The project will not adversely affect the property of others. The proposed waterway will be located almost entirely on private property in areas not currently utilized for fishing or other recreational activities. Except for the impacts on shellfishing, birds, and fish discussed above, the project will not adversely affect the fishing or recreational values within the vicinity of the project. THE MITIGATION PLAN Petitioner has taken all reasonable steps to minimize the adverse impacts associated with the type project it is proposing. Because there will be adverse impacts to an Outstanding Florida Water, the project can be permitted only if it is determined that the mitigation plan offsets the adverse impacts and makes the project clearly in the public interest. Petitioner's mitigation plan was contained in the original application and was revised between October 1991 and January 1992. Respondent considered the current mitigation plan in its review of this project. The current mitigation plan consists of the creation of wetlands, the enhancement of wetlands, and the preservation and donation of wetlands owned by Petitioner within the mosquito impoundment. The estimated cost of creation and enhancement of the mitigation plan is $600,000. Petitioner proposes to create approximately 14 acres of wetlands by removing the mosquito impoundment berms and converting other uplands within the impoundment to wetlands. These areas will be revegetated with various wetland plant species including red, black, and white mangroves. In addition, Petitioner proposes to create a forty foot wide intertidal littoral zone along the entire length of the western side of the artificial waterway and a ten foot wide littoral zone along the entire eastern side of the artificial waterway. Approximately three acres of the littoral zone will be created from uplands. The littoral zone will be revegetated with 80 percent cord grass and 20 percent red mangrove. Petitioner proposes to implement an open marsh mosquito control management program consisting of the elimination of natural accumulations of water in low lying areas within the impoundment by rotary ditching small channels to allow these areas to drain and to allow predator fish access to the areas. Petitioner will remove exotic plant species throughout the impoundment and will revegetate with native species such as red, black, and white mangroves. Petitioner proposes to monitor the project area to assure that exotic plant species do not re-colonize. The mosquito impoundment area and the associated berms is estimated as being approximately 105 acres. Because of the difficulty in determining the mean high water line and because of the number of breaches in the berms, the precise acreage within the impoundment area that is not currently sovereign lands was not established. If accurately surveyed, it is possible that the amount of acreage within the impoundment owned by Petitioner may be determined to be up to 10 percent less than is currently estimated. For the purposes of this proceeding, it is found that 105 acres is a reasonable estimate of the area of the impoundment owned by Petitioner. After completion of the enhancement program, Petitioner proposes to donate all the property it owns within the impoundment to the State of Florida. Petitioner asserts that it would have the right to construct single family docks from its property directly into the Indian River if this project is not permitted and that these docks would not be subject to Respondent's permitting jurisdiction. The construction of such docks would have an adverse impact on manatees and seagrasses. As part of its mitigation plan, Petitioner offers to waive its right to construct single family docks from its property directly into the Indian River. EVALUATION OF THE MITIGATION PLAN The wetland in the existing impoundment area is presently a good biological system that contains a good diversity of plants and animals. While Petitioner's proposals will enhance this area, the evaluation of that enhancement should take into consideration the quality of the existing system. There are at least three existing breaches in the berm system. Through these breaches there is some tidal influences and the export of detrital material. Because of the relatively isolated nature of the mosquito impoundment, it currently contributes little to the productivity of the Indian River. The removal of the berm system will result in greater tidal influence in the impoundment area. As a consequence, much of the leaf litter from mangroves within the impoundment that presently accumulates on site would be exported as detrital material to the Indian River, which will add material to the food chain. It is expected that increased tidal influence will also result in an improvement in the dissolved oxygen levels within the impoundment. The reestablishment of tidal influence within the impoundment area will increase habitat for fish, shrimp, and crabs, and therefore benefit the Indian River. Removal of the impoundment berms to reestablish tidal influences within the impoundment area will increase and improve feeding and forage habitat for wading birds. Consequently, wading birds that nest in the vicinity of the project will be benefited. Increased tidal influence will likely result in better growth for mangroves which would create roosting sites for wading birds where none presently exist. Currently, Australian pines are the dominate species in areas within the impoundment area. Other areas of the impoundment are heavily populated by Brazilian pepper. Australian pines and Brazilian peppers do not serve as food sources for any native wildlife and have the potential to crowd out native plant species such as mangroves. If not removed, the potential exists for Brazilian pepper to become the dominate plant species. Removal of exotics and replanting with native species is a benefit to the Indian River system. With an appropriate monitoring plan, the exotic removal should be successful. If the project is permitted, the implementation of an appropriate monitoring plan should be a condition of the permit. Because of widespread mosquito control activities, the high marsh ecosystem is now rare in the Indian River system. The restoration of the impoundment area to an area of high marsh would be of benefit to the Indian River ecosystem. Prior to alteration by man, the mosquito impoundment was a high marsh ecosystem consisting primarily of black and white mangroves over an understory of succulent plants. There was a conflict in the evidence as to whether the Petitioner's proposals would result in the impoundment area returning to a high marsh area. While the impoundment area will be enhanced by the Petitioner's proposals, it is found that whether the area will be returned to a high marsh system is speculative. The mosquito impoundment is breached in various locations and, as a consequence, the impoundment is not functioning to control mosquitoes as it was originally designed. The current primary mechanism for mosquito control within the breached mosquito impoundment is aerial spraying of insecticides. The proposed removal of the existing berms will not adversely affect mosquito control and may positively affect mosquito control due to the increased accessibility of the impoundment by natural predators such as fish. This open marsh management plan is an effective means of controlling mosquitoes. The wetland creation proposed by Petitioner should have a high rate of success. Petitioner has agreed to implement a suitable monitoring plan to further guarantee the success of the proposal. If the project is permitted, the implementation of a suitable monitoring plan should be a condition of the permit. Scraping down the mosquito berms will create more wetlands, but the earth from the berms will be placed in the adjacent ditches, which presently serve as valuable tidal creek type habitat. Therefore, the mitigation itself will have some adverse impact. Petitioner's unspecified proposal to put in some rotary ditches to offset the loss of tidal creek habitat is inadequate in that there has been no specific proposal as to the location, size, shape, configuration, or acreage of the proposed rotary ditches. While planting of the littoral zones on the edges of the canal with Spartina provides some biological value, the growth of Spartina on the ten foot ledge on the east side will be impacted by boats and docks. The littoral zones will likely perform valuable wetland functions if properly planted and monitored and will likely become a productive wetland system that will provide habitat for wading birds. If the project is permitted, the Petitioner should be required to monitor the Spartina planting to ensure its successful growth. Even if the creation of the 13.9 acres of wetlands is successful, it will take years to become a mature biological system similar to the wetlands they are to replace. This time lag should be taken into account when evaluating the mitigation plan. There are adverse impacts from this proposed project that the mitigation plan does not offset. The mitigation plan does not offset the elimination of seagrasses, the loss of the Boot Lake habitat, the potential adverse impacts to shellfish and shellfishing, or the impacts to manatees. It is likely that property owners wishing to construct docks directly into the Indian River would have to get a permit from Respondent to gain access to the parts of the property where these docks could be constructed. Any proposal to extend docks into the Pelican Island National Wildlife Refuge would likely be prevented by the U.S. Fish and Wildlife Service. Whether such docks would, or could, be constructed is speculative, and this portion of the mitigation plan should be accorded little weight. As part of its mitigation plan, Petitioner proposes to donate approximately 105 acres to the State of Florida. This is considered to be a favorable aspect of the mitigation plan. The central issue in this proceeding is whether the mitigation plan offsets the negative impacts of this project so that the project becomes "clearly in the public interest." This issue is resolved by finding that even when the mitigation plan and the conditions that are recommended herein are considered, this project is "not clearly in the public interest."
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Respondent enter a final order that adopts the findings of fact and conclusions of law contained herein and which denies the modified application for the subject project. DONE AND ENTERED this 31st day of August 1994, in Tallahassee, Leon County, Florida. CLAUDE B. ARRINGTON 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 31st day of August, 1994.
Findings Of Fact The Petitioner, Bocilla Waterways, Inc., is a corporate entity formed for the purpose of pursuing the subject project and installing the proposed channel. Randall Craig Noden, secretary- treasurer of that corporation, and a director of it, is a realtor who sells and develops property on Don Pedro Island, in the vicinity of the proposed project. He and other officers and directors of the Petitioner corporation have an interest in property on some, but not all, upland areas adjacent to Bocilla Lagoon, Old Bocilla Pass and Kettle Harbor, the water bodies germane to this proceeding. The Respondent, State of Florida, Department of Environmental Regulation, is a state agency charged with regulating dredge and fill projects in state waters and navigable waters pursuant to Chapters 253 and 403, Florida Statutes, and Rule Chapters 17-3 and 17-4, Florida Administrative Code. The Intervenor, Environmental Confederation of Southwest Florida (ECOSWF), is an incorporated, not-for-profit organization whose membership includes numerous environmentally concerned public interest organizations or associations located throughout southwest Florida. Members of the Intervenor use Old Bocilla Pass, Kettle Harbor, Bocilla Lagoon and Lemon Bay, an adjacent contiguous water body, for boating, swimming, fishing (both recreational and commercial), and collecting shellfish. Some of the membership of the Intervenor live in the immediate area of the proposed project. Project Description The Petitioner submitted a dredge and fill permit application to the Respondent, DER, proposing excavation of an access channel through the uplands of Don Pedro Island and adjacent transitional and submerged lands. The channel would be 100 feet wide, 450 feet long and dredged to a depth of -5.0 feet mean low water, with 2:1 side slopes grading to 3:1 at approximately +0.5 feet NGVD. The channel below mean high water would be 70 feet wide' and 670 feet long to a depth of -5.0 feet mean low water, with 2:1 side slopes. A rip-rap strip five feet wide would be placed in the littoral zone on either side of the channel. As originally proposed, the channel excavation would be performed by dragline and clamshell with spoil placed upon uplands for disposal. The excavation would progress from the west side of the project to the east, with plugs remaining at the eastern terminus of the channel until it stabilizes and the rip- rap is placed along the excavated channel. A turbidity curtain is proposed to be used to maintain water quality above state standards regarding turbidity. The applicant originally proposed to transplant seagrasses, displaced in the excavation process, back into the bottom of the excavated channel. Earthen slopes above mean high water would be vegetated in order to achieve stabilization. Some of these proposals were modified after negotiations with DER staff, such that the seagrass transplanting portion of the project would be accomplished in surrounding areas of the water bottom of Bocilla Lagoon and Kettle Harbor, specifically, bare areas and otherwise degrassed, vegetated flats. The applicant also proposes to install navigation aides in Bocilla Lagoon and Kettle Harbor in order to help maintain boat traffic in the channel, and to facilitate ingress and egress through the proposed channel. Don Pedro Island is a barrier island lying off the coast of Charlotte County, Florida. The only access to the island is by boat or helicopter. Bocilla proposes to excavate the proposed channel in order to, in part, provide better navigational access to Bocilla Lagoon which lies within Don Pedro Island. There is presently a navigational channel in the Bocilla Lagoon through what is called "Old Bocilla Pass," located at the north end of Bocilla Lagoon and communicating with Lemon Bay. Bocilla contends that the channel is somewhat tortuous and subject to shoaling, with concomitant grassbed damage by boat propellers, and that thus, a better navigational access in the form of a shorter, deeper, more direct channel from the southern end of Bocilla Lagoon to Kettle Harbor is required. The project would involve the removal of approximately .18 acres of mangroves (red and black mangroves) and .187 acres of seagrasses. Bocilla has proposed to mitigate the damage involved in the mangrove and seagrass removal by replanting mangroves, on three foot centers, along both sides of the proposed channel, and replanting or transplanting seagrasses in bare areas of Kettle Harbor, near the proposed project. Description of Pertinent State Waters Bocilla Lagoon, Kettle Harbor and Old Bocilla Pass are designated as Class II, navigable waters of the state and are designated for shellfish propagation or harvesting. Shellfish, including clams and oysters, occur in Bocilla Lagoon, Kettle Harbor and Old Bocilla Pass. As demonstrated by Intervenor's witnesses Wade, Cole and Wysocki, shellfish are harvestable and harvested in Bocilla Lagoon and Kettle Harbor at the present time. Bocilla Lagoon, Kettle Harbor and Old Bocilla Pass have also been conditionally approved by DNR for shellfish harvesting. DNR approves or prohibits waters for shellfish harvesting, and as a matter of policy generally prohibits shellfish harvesting in manmade "dead-end" canals. A "conditionally approved" water body, such as those involved herein, is an area approved for shellfish harvesting, but one which is more likely to be affected by pollution events. Thus, they are monitored more closely by DNR. Such events as additional residential development in an area, resulting in more septic tank sewage discharge, on-board toilet discharges from boats or the installation of a water and sewer treatment plant, can result in DNR temporarily or permanently closing a conditionally approved area to shellfish harvesting. Natural phenomenon such as the influx of red tide is also a factor which is considered by DNR in electing to classify a shellfish harvesting area as conditionally approved, and in electing to prohibit shellfish harvesting in an area. It was established through testimony of witnesses Feinstein and Setchfield of DER that long-standing DER policy provides that when DNR conditionally approves waters as being shellfish harvestable, that means they are "approved" for all shellfish harvesting purposes, but simply subjected to closer monitoring and with an increased likelihood of closure due to immediate pollution events. Therefore, the prohibition in Rule 17- 4.28(8)(a), Florida Administrative Code, prohibits issuance of dredge and fill permits in areas approved for shellfish harvesting or "conditionally" approved, since there is no difference in the "shellfish harvestable" nature of the waters until a closure occurs, which may simply occur sooner in conditionally approved waters. Bocilla Lagoon and Kettle Harbor are both naturally- formed water bodies, although some dredging has been allowed to occur in them in the past. They are not manmade, "dead-end" canals. Neither water body has the physical or biological characteristics of a "typical dead-end canal". Both are quite high quality habitats for the natural flora and fauna occurring in the marine environment in that area, and thus the general policy of DNR established by witnesses Cantrell, Fry, Feinstein and Sperling which prohibits shellfish harvesting in manmade, dead-end canals, does not apply to Bocilla Lagoon and Kettle Harbor. The water quality in both bodies of water is good and within DER standards generally. At times however, the water quality in Kettle Harbor suffers from a failure to meet DER dissolved oxygen standards contained in Chapter 17-3, Florida Administrative Code. Indeed, the water quality in Bocilla Lagoon is generally somewhat better than the water quality in Kettle Harbor. Environmental Impacts The project as currently proposed would result in the removal of approximately .18 acres of mangroves and .18 acres of seagrasses. Seagrasses and mangroves are important in providing areas of cover, food, and habitat for various estuarine species. Seagrasses serve to stabilize marine soils resulting in a decrease of suspended solids in contiguous waters with resulting decrease in turbidity in those waters. The loss of seagrasses can result in de- stabilization of the bottom sediment, such that suspended solids or turbidity increases in involved waters, which can result in decreased light penetration to the vegetated bottoms. Decreased light penetration, if of a sufficient degree, can result in the further loss of seagrasses and other bottom flora, causing in turn, increased turbidity and further decreased light penetration, with progressively destructive results to seagrass beds and other marine flora and fauna, with a substantial detrimental effect on the marine biological community in general. Mangroves serve as biological filters, trapping sediments, heavy metals, nutrients and other pollutants, uptaking them through their roots and converting them to usable plant food and thus filtering such harmful elements from state waters and rendering them into environmentally harmless substances. The removal of the mangroves at the proposed channel site will result in a loss of their beneficial effects. These beneficial effects will be absent for a greater period of time than it takes to merely plant replacement mangrove plants, since mature trees will be removed and mangrove seedlings will be replanted in their stead. Maturation of mangroves at this location would take in excess of three years, thus replacement of the beneficial filtering effects of the removed mangroves will take in excess of three years, to which time must be added the time which lapses between the original mangrove removal and the replanting of the seedlings, which would start the maturation period. Bocilla proposes to mitigate the removal of the mangroves by that replanting, as well as to transplant seagrasses removed from the channel site to other nearby areas currently bare of seagrass. Seagrass replanting is not a well-established practice. Compared to mangrove replanting, there is less experience, less information and a lower success ratio historically. Of the hundreds of dredge and fill projects occurring and approved throughout Florida, only three have involved replanting of removed seagrasses. Two of the projects involved the Port of Miami in Dade County and the "New Pass site" in Sarasota County. In both of these cases, seagrass replanting cannot be termed successful. The Port of Miami project resulted in a final survival rate of only twelve per cent of ,the grasses replanted. The New Pass project thus far has resulted in a survival rate of only 39 per cent of the seagrasses replanted, after only nine months. The Petitioner proposes that the replanting be accomplished by Mangrove Systems, Inc. That firm is headed by Robin Lewis, who oversaw the seagrass replanting project at the New Pass area in Sarasota. The location and method of replanting seagrasses at New Pass, as to water depth, type of bottom, type of grass and planting method, was generally similar to that proposed for the Bocilla project. That is, it would be accomplished by "plug planting," of "bald" spots at generally the same latitude and similar water depth. The survival rate at the end of six months at the New Pass project was 73 per cent. The survival rate at the end of nine months was 39 per cent. Mangrove Systems, Inc. and Mr. Lewis acknowledges that it is difficult to attribute the decrease in survival rates and grass shoot densities to any one cause, but that predation and a shift in sediments due to the vagaries of water currents, were probably the chief causes for the decrease in seagrass survival. Mangrove Systems, Inc. and the Petitioner propose a guarantee whereby Mangrove Systems, Inc. would replant more seagrasses, if needed, if a low survival rate occurs, which it defines to mean less than a 70 to 80 per cent survival rate after one or two years. There is no guarantee concerning the survival rate after a second planting, however. It was not established when the survival rate will be measured, in determining whether a 70 to 80 per cent survival is being achieved. In this connection, the central Florida coast where the Bocilla project is proposed, is not as conducive to seagrass growth as other more tropical marine areas, such as in the Florida Keys. In the area of the proposed project, seagrasses do not generally produce a great deal of seed and tend not to grow back very readily, once they are destroyed. Seagrasses in the Florida Keys tend to have, in comparison, much greater seed production and for this and other reasons, tend to reproduce themselves more readily once destroyed. They tend to be more amenable to transplanting in the Florida Keys marine environment. Mangrove Systems, Inc. has conducted a seagrass replanting project in the Florida Keys, however. One-third of the seagrasses planted in that project have not survived after two years. In short, the likelihood of seagrass survival has been insufficiently tested in the geographical area and latitude and in similar soils, water depths and temperatures as those involved in the instant case, such that reasonable assurance of adequate seagrass survival with the replanting project proposed will occur. Hydrographics and Maintenance Dredging The evidence is uncontradicted that the opening of the proposed channel would increase circulation in the southern end of Bocilla Lagoon. Increased circulation tends to have good effects in that it reduces stratification in water bodies. Stratification is a condition which occurs when the deeper waters of a given water body do not interchange with surface waters, but rather stratify or become characterized by layers of differing levels of dissolved oxygen, temperature, pH, etc. Typically, lower levels of a stratified body of water are characterized by low levels of dissolved oxygen. The present water quality of Bocilla Lagoon however, is not characterized by statification in any significant degree. It is very similar in water quality, in terms of dissolved oxygen, temperature, pH and other Chapter 17-3 water criteria, to that water quality of the nearby intra-coastal waterway into which the channel into and through Kettle Harbor would open. The intra-coastal waterway is agreed to be a well- circulated body of water, meeting all current State water quality standards. Accordingly, the opening of the channel and the increased circulation it may cause in the southern end of Bocilla Lagoon would have minimal, positive benefits. The change in circulation and in water current patterns and velocities caused by the opening of the direct, shorter channel from lower Bocilla Lagoon and Kettle Harbor may, negatively affect the present seagrass growth in seagrass beds in Kettle Harbor and Bocilla Lagoon in the vicinity of each end of the proposed channel, due in part to increased current velocities that would result from tidal exchange through the shorter, straight channel which would be opened. The expert witnesses in the area of hydrographics disagreed on the effect of the proposed channel on water circulation in the northern end of Bocilla Lagoon and Old Bocilla Pass, which is the north channel opening into northern Bocilla Lagoon. Witness Sperling for the Department opined that a major reduction in flows through Old Bocilla Pass channel would occur. Witness Tackney for the Petitioner acknowledged there would be some reduction in flow, and witness Olsen opined that a reduction in flow would occur, but there could also be an increase in circulation. Both witnesses Tackney and Olsen, in opining that a flow-through, enhanced circulation and flushing system may result from installing the channel, based that opinion to a significant degree, on their belief on the effects of wind on forcing water through the Pass and Bocilla Lagoon. No wind data or records were adduced however, to show the likely effects of wind on creating the Petitioner's desired "flow-through" system. Witness Sperling disagreed as to the significance of this flow-through effect, but there was no disagreement among the hydrographic experts that reduced flows through Old Bocilla Pass, which all acknowledged can occur to one degree or another, can result in increased sedimentation in Old Bocilla Pass, which can result in turn, in the need for increased maintenance dredging in Bocilla Lagoon and Old Bocilla Pass in the future. Maintenance dredging in Old Bocilla Pass may have to be increased if the proposed channel is constructed. The proposed channel itself will likely have to be periodically maintenance dredged as well. Maintenance dredging can cause environmental problems. Dredging activities result in the loss of marine habitat and the destabilization of marine sediments, with resulting increased turbidity and reduced photic effects, with concomitant detrimental effects on seagrasses and other bottom flora and fauna. Increased turbidity resulting from dredging and destabilization of sediments can directly adversely affect shellfish, including clams and oysters. Dredging impacts and siltation can negatively affect seagrass growth and water quality by increasing turbidity resulting in reduced photosynthesis in seagrass, by smothering the seagrass directly and by silting fauna and vegetation in adjacent productive grassbeds. Persons other than the officers and directors of Bocilla Waterways, Inc. own property and have riparian rights on the Old Bocilla Pass channel. These persons have in the past, and have the right in the future, to use Old Bocilla Pass for navigational purposes and could elect to maintenance dredge Old Bocilla Pass as they have in the past. If the proposed channel is constructed, there is obviously a more direct access and shorter water route between the waters of Bocilla Lagoon and Kettle Harbor. Water quality at times in Kettle Harbor has been worse than that in Bocilla Lagoon, especially in terms of low dissolved oxygen. If poorer water quality exists in Kettle Harbor due to low dissolved oxygen, an influx of red tide or some other cause, the construction of the proposed channel would increase the chance, by the more direct connection and increased flow in the southern end of Bocilla Lagoon, to contaminate the water of Bocilla Lagoon. The Public Interest Public opposition was expressed at the hearing, including that of ECOSWF, the Intervenor, some of whose members include people who live in the area of the proposed channel and use the involved waters. Local fishermen who harvest shellfish and finfish in Bocilla-Lagoon and Kettle Harbor, and use Old Bocilla Pass for navigation between Lemon Bay and Bocilla Lagoon, oppose the project, some of whom are members of the organized Fishermen of Florida, an association of approximately 25,000 members. Residents of Bocilla Lagoon and the immediate area, who habitually navigate Old Bocilla Pass, including local fishermen, have had little trouble navigating Old Bocilla Pass because they are familiar with the channel. Although the Petitioner alleges that the new channel is needed in part for the safety of people living on Bocilla Lagoon to assure quick access to the mainland in case of medical emergencies, the members of the public living on Bocilla Lagoon, (with one exception) and on surrounding areas of the island, do not wish such increased access for medical purposes. The island is presently reached from the mainland by either watercraft or helicopter. Formerly, there was a bridge connecting the island with the mainland which has since been destroyed, and not rebuilt. The residents living on Bocilla Lagoon, either full- time or part-time, buy their homes and choose to live there with knowledge of the present mode of access through Old Bocilla Pass, which is also the means they would achieve access to the mainland in case of medical emergencies or, alternatively, by helicopter transport or by transport over island roads to the ferry landing, with access to the mainland by ferry. The residents, in general, desire to maintain the isolation of life on the island as it presently exists and do not desire enhanced access between the island and the mainland, since part of the charm of having homes and living on the island is its isolation from the more populous mainland. Other than the testimony of Petitioner's witnesses, there was no testimony presented expressing any public need for the proposed channel, as for instance from public officials having knowledge of any medical or public health need for enhanced access to Bocilla Lagoon and the island. The proposed project is contrary to the public interest due to its adverse effects on seagrasses, shellfish, and water quality as delineated above. The adverse effects on seagrasses would result from the dredging itself and the destruction of a portion of the extant seagrass beds, and the resultant likelihood of poor survival rates in the attempted transplanting of seagrass as a replacement for that destroyed by the channel dredging. The proposed project is not in the public interest of those people with riparian rights on Old Bocilla Lagoon and northern Bocilla Lagoon, as there is substantial likelihood the proposed project will reduce flows through Old Bocilla Pass' channel with the resultant increased settling out of sediment and thus increased shoaling of that channel, which would concomitantly increase the need for maintenance dredging in Old Bocilla Lagoon and channel. Additional maintenance dredging and the possible negative effects of such additional dredging on marine, flora and fauna in Bocilla Lagoon and Old Bocilla Pass constitute an additional burden on these riparian owners, the bearing of which is not in their interest. The proposed project is also contrary to the public interest in that the proposed channel is deeper, wider and more direct as an entry into Bocilla Lagoon from Kettle Harbor and Lemon Bay, and would thus allow larger, deeper draft boats to enter Bocilla Lagoon with concomitant increased pollution from oils, greases and possible discharge of onboard sewage, which could have adverse environmental impacts on water quality in Bocilla Lagoon, as well as Kettle Harbor. The use of deeper draft, larger boats with larger propellers and more powerful engines could also result in damage to adjacent grassbeds in the vicinity of either ends of the proposed channel, either through direct propeller contact or through prop wash, when such boats are navigated in areas minimally deep enough to accommodate their draft. Since the installation of the proposed channel would result in a deeper, more readily used access to Bocilla Lagoon by larger boats with the remaining original channel usable also, at least for a time, there is a-substantial likelihood of increased residential development on riparian property around Bocilla Lagoon. This could have the result of reducing water quality in the lagoon, or potentially so, through septic tank leachate, stormwater runoff and other adverse environmental effects, such that the water in the lagoon traditionally approved for shellfish harvesting may be prohibited in the future.
Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence of record, the candor and demeanor of the witnesses and the pleadings and arguments of the parties, it is, therefore RECOMMENDED: That a Final Order be entered by the Department of Environmental Regulation denying both the variance application and the permit application sought by Bocilla Waterways, Inc. DONE and ENTERED this 24th day of January, 1985 in Tallahassee, Florida. P. MICHAEL RUFF Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904)488-9675 FILED with the Clerk of the Division of Administrative Hearings this 24th day of January, 1985. COPIES FURNISHED: Kenneth O. Oertel, Esquire Segundo J. Fernandez, Esquire 646 Lewis State Bank Building Tallahassee, Florida 32301 Douglas H. MacLaughlin, Esquire Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 Thomas W. Reese, Esquire Environmental Confederation of Southwest Florida 123 Eighth Street, North St. Petersburg, Florida 33701 Victoria Tschinkel, Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301
