The Issue The issue is whether the 100 foot separation of respondents/applicants sewage treatment plant from the surface water management system is adequate.
Findings Of Fact Based upon all of the evidence, the following supplemental findings of fact are determined: Background Respondents/applicant, John D. Remington and Bolton S. Drackett (applicants), are the owners of record of approximately two thirds, or around 2,700 acres, of Keewaydin Island (Key Island), which lies just south of the mainland portion of the City of Naples, Florida. In conjunction with a planned luxury development of forty-two homes on Key Island, applicants have filed an application with respondent, South Florida Water Management District (District), seeking the issuance of a permit authorizing the construction and operation of a surface water management system (system) through which stormwater runoff from the project will be directed and controlled. Petitioner, Florida Audubon Society (FAS), has initiated this proceeding to contest the issuance of a permit. In an earlier and separate proceeding (DOAH Case No. 90-2415), applicants applied for a permit from the Department of Environmental Regulation (DER) to construct a wastewater treatment plant (plant) to serve the planned development. The permit was issued on January 2, 1990, and because all appeals by FAS in Case No. 90-2415 have been concluded, that proceeding is now final. Although the wastewater treatment plant has not yet been constructed, the parties agree that it will be situated more than one hundred feet from the surface water management system. This distance (100 feet) is the minimum amount of space allowed by District rule between the plant and system. Even so, the purpose of the remand proceeding is to determine whether that amount of separation is adequate. Thus, the factual issue here is whether the treated wastewater from the plant and filter fields will enter the surface water management system and cause a violation of applicable water quality standards and other relevant District criteria. In support of their respective positions on this issue, the parties have presented the testimony of a number of experts. In resolving the conflict in their testimony, the undersigned has accepted the more credible and persuasive testimony which is embodied in the findings below. A Brief Description of the Development and System The proposed development and surface water management system were described in detail in the prior recommended order entered in this case. For purposes of this Supplemental Recommended Order, it need only be noted that Key Island now has a lodge, guest quarters and recreation facilities, all presently served by septic tanks. Access to the island is provided by motor launch from an existing shore station. Subaqueous utility crossings from the mainland provide electric power and potable water to the island. The planned development includes the construction of forty-two large luxury homes and an expansion of the lodge facilities to accommodate the needs of the new residents. The homes will be built in phases with approximately ten to be built in the first year. The entire project may take as long as seven or eight years to complete. The proposed surface water management system was designed to handle a seventy-five residential unit development. However, by virtue of a reduction in size imposed by the City of Naples, the project has been reduced to forty-two homes. Even so, the capacity of the system has not been downsized. Therefore, the system as designed will more than accommodate all proposed development on the island. The development area has been divided into seven surface water management basins based upon seven existing natural water sheds on the upland portion of the project. Each basin will have a system of inlets, culverts and swales which will direct runoff to control structures. The dry swales are approximately one foot deep and five to ten feet wide and run parallel on both sides of the cart paths that link the various portions of the project. The cart paths, which will be at an elevation of 5.5 feet above mean sea level (NGVD), will have culverts running underneath to aid in maintaining the natural flow of water and limit impounding of water. The swale bottoms are designed to be one foot below the cart path elevation, or at 4.5 feet NGVD, and will be dry, except during significant rain events, because they are designed so that the bottom of the swale is at least one foot above the average wet season water table. Both the cart paths and swale system utilize a design system that is common to residential developments. Once the water reaches a specified height, it goes over the control structure and is discharged downstream into spreader swales from which the water is dispersed into either interior, low wetland areas or into two artificial lakes (7.3 and 1.0 acres in size) created for wet detention. Basins one, two, three, four and seven are designed to treat water quality by the dry detention method, that is, by the unlined swales that parallel cart paths, while water quality is accomplished in basins five and six by best management practices and wet retention, that is, the two artificial lakes. The Wastewater Treatment Plant The DER permit was issued on January 2, 1990, and carries an expiration date of January 2, 1995. It authorizes applicants to: construct a 0.035 MGD extended aeration process wastewater treatment plant with reclaimed water to dual absorption fields located at the project site as depicted on Wilson, Miller, Barton, Soll & Peek, Inc. design drawings, project number 6270, sheets 1 thru 5 of 5, dated March 20, 1989, revised October 16, 1989 and received October 19, 1989. The design drawings were submitted in support of construction application, engineering report, hydrologeolic characteristics and hydraulic modeling for effluent disposal report and related documents, dated March 20, 1989. The hydraulic capacity of the plant is limited to 0.030 MGD based on the reclaimed water disposal system. The collection system shall not exceed the 0.030 MGD hydraulic capacity as well. The wastewater treatment plant is designed to meet all DER water quality, health and safety standards. For example, the plant must achieve 90% removal of biological oxygen demand (BOD) and 90% removal of total suspended solids from the raw wastewater, or effluent levels below 20 parts per million for BOD and 10 parts per million suspended solids, whichever is more stringent. The plant must also have twenty-four hour detention in the aeration chamber and four hours detention in the clarifer. Further, a chlorine chamber contact time of fifteen minutes is required. In addition, DER has issued the permit with certain specific conditions. Among others, these include standards as to effluent chlorine residuals, the requirement that a professional engineer inspect the construction, operation requirements, sampling schedules, defined perameter levels, and the establishment of a hydraulic plant load (permitted maximum daily flow) at 30,000 gallons per day. By issuing the permit, DER has concluded that up to 30,000 gallons per day of sewage effluent can be treated and disposed of by the plant filter fields without violation of applicable DER water quality, health and safety standards. The wastewater treatment plant will be located on a centralized utility site within basin seven of the system. There are also gravity sand filters and a drainfield effluent disposal system located in basin six, which is the northeastern corner of the project. The plant will provide a high degree of treatment and disinfection for the effluent before it is discharged to the filter field. The filtered (treated) effluent will flow by gravity main to the filter fields located in an adjacent basin. Two filter fields will be used in disposing of the treated wastewater effluent. Constructed as sand mounds at a grade level of two or three feet above the existing island elevation, each filter will have dimensions of twenty feet wide and four hundred feet long. The filter fields will be constructed as a bed of gravel wrapped in filter cloth and placed within a mound of soil. A perforated four-inch pipe will be installed within the gravel bed at 5.5 feet NGVD to distribute the effluent through the filter beds. The effluent will then percolate downward and laterally away from the bed and into the groundwater table. At that point, the effluent will become indistinguishable from the groundwater Because the total daily flow will be pumped alternately into one part of the two sections of the drainfield, this allows one filter field to "rest" for a seven-day period during the use of the other filter field, thereby avoiding saturation. Therefore, the average theoretical maximum input into a filter field over a one year period at the plant's maximum capacity is 15,000 gallons per day. The plant was designed and permitted for maximum daily flows at all times of the year. However, the actual operating conditions will reflect significantly less flows due to the seasonality of the population and occupancy levels. More specifically, the plant was designed and permitted for seventy- five dwelling units and ancillary uses with an estimated maximum design flow of 28,450 gallons per day. The approved planned development will contain only forty-two dwelling units and ancillary uses with a maximum design flow of 21,200 gallons per day. Therefore, the permitted plant will treat the wastewater to a higher level due to the reserve capacity, and the plant will rarely be used at over fifty percent of its available capacity. Revised projected wastewater flows will range from daily loads of 2,325 gallons per day during the months of August and September to a high of 15,137 gallons per day during the month of February. This projected usage is consistent with historical occupancy and usage trends in the Naples area which show that occupancy of homes is at its peak during the dry season (the cooler winter months) and substantially lower during the wet season (the hot summer months). Applicants' projected wastewater flows are found to be reasonable and are hereby accepted. In making this finding, the undersigned has rejected the contention by FAS that the daily wastewater flows will be higher than that projected by the applicants and the plant will operate at maximum capacity for sustained periods of time. The system plans reflect that there will be swales within basin six located between one hundred ten and one hundred twenty feet to the west of the filter fields. These swales run parallel along a cart path and flow to the north discharging into an artificial lake at the north end of the project. The swales in this basin have a bottom elevation of 4.5 feet NGVD and decrease to an elevation of 3.5 feet NGVD at the point of discharge into the artificial lake. Adequacy of Separation Between Plant and System Rule 40E-4.091, Florida Administrative Code, adopts and incorporates by reference a document known as the "Basis for Review for Surface Water Management Permit Applications within the South Florida Water Management District - September 1989" (Basis for Review). Section 3.2.2.8 of the Basis for Review reads as follows: Sewage treatment percolation ponds. Above ground pond dikes shall not be within 200 feet of water bodies or 100 feet of dry detention/ detention areas. Additional calculations by the applicant may be necessary in unusual cases requiring deviations from these dimensions. The purpose of the above section is to provide adequate separation between above-ground percolation ponds and surface water management systems in case the percolation pond dike fails. For example, above grade percolation ponds contain large volumes of sewage treatment plant effluent. If a pond dike should fail, a large portion of effluent would be quickly released into the adjacent ground. The minimum 100-foot separation is designed to provide adequate distance for percolation into the ground prior to infiltrating the surface water management system. However, filter fields contain lesser volumes of effluent than do percolation ponds, and should a filter field fail, the effluent will trickle out the side of the field with a much lower rate of effluent release than from a failed pond dike. In accordance with the District rule, applicants have proposed to locate the surface water management system more than one hundred feet from the wastewater treatment plant and filtration beds. Even though the rule standards have been met, the purpose of this remand proceeding is to determine whether that amount of separation is adequate to prevent adverse impacts to the water quantity and water quality functions of the system from the operation and location of the filter fields. The Computer Models As a part of their application filed with DER in 1989, applicants' witness Missimer prepared and submitted a report known as "Hydrogeologic Characteristics and Hydraulic Modeling for Effluent Disposal at Keewaydin Club". The report was based on a computer model known as "Modflow" and was designed to show the increase in elevation of the water table for a loading rate of 30,000 gallons per day alternating between the two filtration beds. The purpose of the modeling analysis filed with DER was to investigate whether the plant would continue to discharge effluent to the drainfields under the most extreme conditions. The model demonstrated that the effluent discharge would not be impaired even under conditions that are beyond any reasonable or probable operating conditions. After reviewing the model, DER accepted those results and issued a permit. Utilizing in large part the underlying assumptions and parameters of the Missimer model, and without performing any independent field evaluation on the site, FAS witness Chin ran the model to investigate the impact of the operation of the plant on the system. Because the model used by Dr. Chin was not constructed for the design of a surface water management system, but rather was constructed for the purpose of designing an adsorption field, without modification it provided a more than worst case scenario of impacts associated with the operation of a plant. In this case, Dr. Chin utilized the ultra- conservative assumptions used in designing the adsorption field and made no revisions to the model. Thus, it is found that the model as used by Dr. Chin, and any conclusions drawn from the model alone, are not a sufficient or reasonable basis for evaluating the impact of the plant on the system. The model used by Dr. Chin is not representative of the natural occurring conditions on the island or the reasonably expected plant flow rates. Moreover, in developing the worst case scenario, as opposed to reasonable expectations, both the Chin and Missimer models incorporated the simultaneous occurrence of certain conservative assumptions including an impermeable flow boundary, a year round wet season water table elevation, a conservative rate of transmissivity, and a constant rate of evapotranspiration. The use of these assumptions caused the model output to grossly overstate the effects of the plant on the system in the following manner. First, by assuming a flow barrier on the island, the model had the effect of overestimating the height of the groundwater mound from operation of the plant than would occur if no boundary were used. Second, the assumption of a year-round wet season groundwater level is unrealistic since groundwater levels fluctuate seasonally, receding to near zero NGVD on the island during the dry season. Thus, the model overestimated the height of the groundwater level. Further, by using only the upper ten feet of the water table aquifer in calculating the rate of transmissivity, the model incorporated a much lower rate than would be attained had the entire thickness (74 feet) of the aquifer been used. This also resulted in an over-estimation in the height of the mound from the operation of the plant. Finally, by assuming a constant rate of evapotranspiration, the model "grossly exaggerated" the impact to the groundwater level from operation of the plant. In reality, as the water table increases, the loss of water from evapotranspiration increases significantly and constitutes a major output of a water budget. Besides the foregoing assumptions, the Chin model also assumed a continuous loading rate of 30,000 gallons per day for a period of up to one year. While the District should properly consider the permitted flow rate of the plant in evaluating a worst case of potential impact, there was no evidence substantiating any likelihood of the plant actually producing 30,000 gallons per day for 365 consecutive days in conjunction with all other conservative assumptions discussed above. The more reasonable and accepted method of analyzing the impact of plant flows is to examine the peak month's average day flow over a six-month period. As noted earlier, for the proposed forty-two units, the peak day flow is estimated to be approximately 21,200 gallons per day. Therefore, it is highly probable that actual flow rates will be much lower than the maximum plant capacity of 30,000 gallons per day. By failing to use the more reasonable and realistic reduced flow rates, the Chin model overestimated the elevation of the groundwater level from the operation of the plant. In contrast, the Missimer analysis demonstrates that it is extremely unlikely that the plant output will ever elevate groundwater to the extent that it would reach the system swales by either surface water or groundwater flow. The foregoing modeling assessments, including the criticisms of the Chin model, were concurred in by the District expert. Water Quantity Impacts There is no credible evidence to support a finding that the operation of the plant will adversely impact the ability of the system to provide adequate flood protection and drainage. Indeed, the more credible evidence shows that an alteration of existing drainage patterns will not occur by virtue of the operation of the plant, and the post-development discharge rates will not exceed the pre-development discharge rates. Therefore, the undersigned's previous finding that applicants have provided reasonable assurance that the the system provides adequate protection and drainage is not altered after considering the operation and location of the plant. There is insufficient credible evidence to support a finding that the plant's operation will adversely impact the system functions in such a way as to cause adverse water quantity impacts on receiving waters and adjacent lands. Indeed, the post-development discharge rate approximates the pre-development discharge rate on receiving waters, the ultimate receiving water body (the Gulf of Mexico) has an infinite capacity to receive water, and there are no adjacent lands subject to flooding from discharge of the system regardless of whether there is any impact of the plant on the system. There is no credible evidence to support a finding that the plant will cause the system to have an adverse impact on surface and groundwater levels and flows. Rather, the more persuasive evidence shows that the plant's operation will not result in groundwater elevation in the area of the system that would cause the impoundment of water or prevent the percolation of water into the soil. In addition, the overflow levels for control structures will operate as designed to insure against over-drainage or flooding. Finally, the operation of the filter fields will not cause adverse impacts on surface and groundwater levels and flows. Water Quality Impacts The operation of the plant will not impair the water quality functions of the system. This is because the swales will continue to detain the first flush of run-off allowing the majority of the suspended solids and other pollutants to settle out regardless of the operation of the plant. Further, in the unlikely event the treated wastewater effluent reached the system, it would be indistinguishable from the stormwater or rainfall due to the high level of treatment from the plant, the filter fields and dilution from groundwater and rainfall. The operation of the plant will not cause adverse water quality impacts on the receiving waters. In making this finding, the undersigned notes initially that the plant is permitted by DER, and therefore it is assumed to comply with all DER water quality standards. Second, there is no evidence that the system will impact the operation of the plant. In the event the groundwater mixed with treated effluent resurfaces, there would be no adverse impact to the surface water quality. This is because the treated effluent from the plant exceeds state water quality standards. Once the treated effluent becomes a part of the groundwater, it is unlikely that it will resurface again in the areas of the swales, which are more than one hundred ten feet away. Indeed, in order for the groundwater with effluent to travel that distance, it would have been in the groundwater system for at least one hundred days. This period of time is more than sufficient for the denitrification and adsorption processes to remove all nutrients. Even if the worst case scenario became a reality and the groundwater reached the swale bottoms, it would only result in a wetting of the ground and would not be of sufficient quantity to create a flow of water in the swale to travel off-site impacting a receiving water. In any event, at that point, any groundwater resurfacing that distance away would no longer be effluent. Finally, during abnormal conditions, such as a hurricane or large storm event, the groundwater may rise to the surface and mix with the surface water and enter the system. However, any effluent already significantly diluted under normal circumstances would be indistinguishable from the stormwater or rainfall. Adverse Environmental Impacts There is no credible evidence that the operation of the plant filter fields will adversely impact the system in such a manner as to cause an adverse environmental impact. In so finding, the undersigned rejects the contention that the system will act as a conduit for treated effluent to travel off-site to the ponds, marsh, mangrove areas or receiving waters. The evidence shows that the design of the filter fields and high permeability of the island soils will prevent the surface flow of effluent to the system swales. The elevation of the swales above the groundwater table level will prevent the introduction of effluent into the swale system. In the unlikely event the groundwater reaches the bottom elevation of the swale, there would be no significant environmental impact because the quality of effluent would be indistinguishable from the groundwater due to the high level of treatment and dilution, and such water would still be further treated by the system before discharge to receiving bodies. The location of the plant and system will not have an adverse impact on the gopher tortoise population on the island. Rather, the system should enhance the gopher tortoise population by providing mananged land with vegetation suitable for gopher consumption. Further, the general development on the island will reduce the number of raccoons which prey on gopher eggs and young gophers. Miscellaneous During the remand hearing, FAS presented evidence concerning the impact of tides and mean sea level rise and saline lakes on the island. This evidence was essentially the same as that presented in the prior hearing and was rejected in favor of the more credible evidence presented by the applicants on this issue. Nothing was presented during the remand hearing which would alter these prior findings. During the hearing, and in response to a question by District counsel, witness Missimer agreed it would not be unreasonable to install a few monitoring wells to insure that the system is operating properly. Because this requirement is not unreasonable, will serve a valuable purpose, and has been utilized by the District as a special condition on numerous prior occasions, it should be incorporated into the permit conditions. Even though the evidence clearly shows that seasonal tidal fluctuations would not have an adverse impact on the functioning of the system, if such a tidal incursion were to occur, the placement of a check valve device on the water control structures would prevent sea water from flowing back into the system. Such a device would be a minor addition to the system, would not otherwise affect its design, and if deemed necessary by the District, should be incorporated into the permit conditions. Prior to hearing, the District retained the services of an outside consultant to assist it in preparation for trial. The consultant did not testify at final hearing and prepared no reports. He did make several computer runs, none of which are a part of this record. Among other things, District witness Rogers relied upon the computer runs in formulating his opinion on the issue presented on remand.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that a final order be entered granting the requested permit in accordance with the agency's proposed agency action dated March 28, 1990. DONE and ENTERED this 22 day of March, 1991, in Tallahassee, Florida. DONALD R. ALEXANDER Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 22 day of March, 1991.
The Issue On June 7, 1991 the Department of Environmental Regulation (DER) released its intent to issue Permit No. DC05-194008, authorizing Florida Cities Water Company (FCWC) to construct a 300-acre restricted public access spray irrigation system for the land application of treated domestic wastewater (Sprayfield Permit). And, on August 6, 1991 DER released its intent to issue Permit No. MS05-194894, relating to stormwater management and management and storage of surface waters (MSSW Permit) for the sprayfield site. Petitioners Brevard Groves, Inc. and H & S Groves, Inc. (Groves), Parrish Properties, Inc., Parrish Management, Inc. (Parrishes), Atico Financial Corp. (Atico) and David and Eleanor Shreve (Shreve), each requested a formal administrative hearing challenging the issuance of the sprayfield permit. Groves requested a hearing challenging the issuance of the MSSW Permit. The ultimate issue is whether FCWC is entitled to these permits.
Findings Of Fact FCWC is a private utility company, with headquarters at 4837 Swift Road, Suite 100, Sarasota, Florida, 34231. FCWC's Barefoot Bay Wastewater Treatment Plant (the WWTP) provides water and wastewater service to the Barefoot Bay development in southern Brevard County, Florida. DER, 2600 Blair Stone Road, Tallahassee, Florida 32399-2900, is an agency of the State of Florida which regulates domestic wastewater treatment and disposal facilities and permits their construction and operation. For domestic wastewater projects, DER is also charged with reviewing applications for stormwater management and management and storage of surface water pursuant to an operating agreement between DER and St. Johns River Water Management District. David and Eleanor Shreve are beekeepers who live approximately a quarter-mile from the proposed sprayfield. They maintain beehives in the groves and woods surrounding the proposed site. The remaining Petitioners own citrus groves that are adjacent to, or in the immediate vicinity of the proposed site. These groves are producing and are actively maintained. The WWTP has a treatment capacity of 0.9 million gallons per day (MGD). As of July, 1990, the WTTP was treating and disposing of effluent from approximately 4,200 residences in the Barefoot Bay development. At buildout, within the five-year life of the Sprayfield Permit, the WWTP will serve 5,000 residents, and will generate approximately 0.6 MGD of wastewater. Disposal of treated effluent is presently achieved by a 40-acre sprayfield, storage ponds and direct discharge of pond overflow to the San Sebastian Drainage District Canal (Canal). In 1986, DER issued FCWC a warning notice to the WWTP regarding an unlawful discharge to the Canal. FCWC met with DER to discuss options to correct the discharge. In 1988, FCWC entered a Consent Order that would allow FCWC to discharge treated effluent into the Canal until a deep injection well could be built for alternative disposal. FCWC also discussed other alternatives with DER, such as golf course irrigation. The Consent Order was amended in 1991 to provide for land application in lieu of deep injection. In accordance with the amended Consent Order, FCWC has submitted monthly monitoring reports to DER, for the WWTP and for the storage (percolation) ponds. DER has never issued a notice of violation to FCWC for failure to comply with monitoring in the Consent Order. The Site The proposed sprayfield site is divided into two large tracts, the "northern parcel" and the "southern parcel." The site is primarily citrus groves. Although some citrus trees were damaged by a freeze in recent years, most are still viable. Most of the areas between the trees and limited areas without trees are covered with dense grasses and weeds. The site, and the surrounding groves, have been significantly altered to provide sufficient drainage for citrus trees, which require well-drained conditions. The area is covered by shallow ditches (swales), between mounded rows of earth comprising beds for the trees. These citrus mounds, created by soil cast up during excavation of the swales, occur on 60-foot centers and rise 2 1/2-3 feet above the bottom of the swales. The swales have pipes at each end, which discharge into an agricultural collection ditch or the Canal. Each block of citrus is surrounded by a collection ditch some 8-10 feet deep. All collection ditches ultimately discharge into the Canal, which borders the site on the north and is approximately 20 feet deep and 100 feet wide. The collection ditches and Canal prevent the entrance of offsite surface water run- off into the site and receive surface water run-off and groundwater seepage from the site. The Sprayfield Project The project is proposed in two phases. Phase I meets total annual effluent disposal needs of 0.55 MGD, using both the proposed sprayfield and the existing 40-acre sprayfield, which will continue in operation for both phases of the project. Phase II meets the total annual effluent disposal needs of 0.6 MGD at build-out. This results in an average annual application rate of 0.54 inch/week or approximately 28 inches per year on the proposed sprayfield. The project is designed to eliminate the current discharge to the Canal. The effluent will be given secondary treatment with basic disinfection. The treated effluent will be pumped from the WWTP to storage ponds and then to the proposed sprayfield. The existing ponds will be retrofitted as storage ponds for Phase I. An additional storage pond will be constructed at the proposed sprayfield for Phase II. The spray irrigation system will operate primarily with four traveling gun sprinklers. Two sets of fixed-head sprinklers will also be used for the two small triangular portions of the site. The traveling sprinklers will be operated for approximately 5.9 hours/day during Phase I and 6.5 hours during Phase II. The four traveling sprinklers will run simultaneously on four of the thirty-three travel lanes (tracks) located between the swales covering the site. Ordinarily each track will be sprayed every eighth day. To make up for days when irrigation is not possible, additional disposal capacity can be obtained by operating the sprinklers for extra shifts on tracks not previously irrigated that day. The site will be mowed regularly, and any accumulated grasses or debris will be removed. Any areas presently in weeds, or the areas not covered by vegetation are reasonably expected to fill in with dense grasses when irrigation commences. Maintaining the grass cover in the swales will prevent erosion of soil and debris into the swales and reduce the need for maintenance of clogged swale outlet pipes. The system is designed and will be operated to avoid ponding or direct surface run-off of sprayed treated effluent. However, there may be some very limited potential for droplets of treated effluent clinging to vegetation being washed into the swales by a heavy storm event immediately following an application. Therefore, the sprinklers will not be operated when the water table is closer than four inches from the bottom of the swales. Operators will know when to spray by reading automatic groundwater elevation monitoring gauges installed in several places throughout each block of citrus, including the middle. In addition, an automatic device will shut off sprinklers during a rainfall, so that no significant amount of treated effluent will leave the site mixed with stormwater. The site is bordered on three sides by groves and on one side by undeveloped vacant land. The width of the proposed buffer zone from the sprayfield wetted area to the site property line is at least 100 feet, as required in Rule 17-610.421(2), F.A.C., and is substantially wider for extensive lengths of the project border. The buffer is approximately 130 ft. wide on the eastern boundary of the northern parcel, approximately 250 to 235 ft. wide on the western boundary of the northern parcel, and approximately 225 to 160 ft. on the western border of the southern parcel. The distance between the wetted area and adjacent property owners' boundaries is much greater than 100 ft. for other portions of the sprayfield borders due to linear features that provide additional buffering. It is over 200 ft. from the wetted area to the nearest property owner on the northern border of the northern parcel because of the San Sebastian Canal, and 160 ft. on the southern border of the northern parcel and the southern and eastern borders of the southern parcel because of the 60-foot wide Micco Road right-of-way. Aerosal Drift and Other Off-Site Impacts While Petitioners allege that their groves would be contaminated by aerosol drift from the site, they presented no expert or other competent, substantial evidence on the extent or volume of such drift. FCWC air modelling expert, Dr. Robert Sholtes, used the EPA Industrial Source Complex Model (ISC), the most commonly used predictive model in the air pollution community, to evaluate the project's aerosol drift. While the sprinklers are planned to be operated a maximum 6.5-hour shift, a conservative 7.0-hour shift was used. Other data inputs to the ISC Model were hourly windspeeds at the Daytona Beach weather station for five years; sprinkler nozzle size and pressure; and droplet size, distribution and settling rates obtained from the American Society of Agricultural Engineers. The model yielded the annual average deposition of sprayed effluent in grams per square meter (gm/m2) outside the wetted area for one sprinkler as it moves along its track. The accumulated deposition off the site property line, considering operation of all tracks, can be predicted using these results. Because heavy deposition of droplets settles out fairly rapidly, the aerosol from tracks farther into the site does not significantly affect the maximum impact shown for one track. Due to the prevailing east and west coastal winds, heaviest deposition will occur off the eastern and western property line of the site. The volume of treated effluent that will be blown offsite is not substantial. The greatest volume is approximately 1000 millimeters/square meter/year (ml/m2/yr) off the eastern property line out to approximately 50-75 feet, and 500 ml/m2/yr off the western property line out to approximately 75 feet. A maximum of 100 ml/m2/yr is predicted and a maximum of 50 ml/m2/yr is predicted off the southern and northern lines, respectively. In practice, volumes of aerosol drift off-site will be below the predicted levels in areas where trees occur in the buffers. Most significantly, there are existing rows of citrus trees along the eastern border of the northern parcel within the buffer area, which is the area of heaviest predicted drift. In addition, aerosol drift will be minimized by operating procedures. Wind speed and direction will be monitored at the site. If the wind is over 20 miles per hour, there will be no spraying. For winds of lesser speeds, the spray tracks on the edges of the sprayfield will not be used during a strong directional wind, e.g., for a wind blowing east, the track on the eastern border will not be utilized. The tracks are on approximately 240-foot centers. Therefore, elimination of spraying for the track on the edge of the site will have the effect of withdrawing the aerosol drift deposition pattern 240 feet further into the sprayfield. Considering that the farthest extent of the maximum 1000 ml/m2/yr levels of drift is 75 feet, such a program will be very effective in minimizing drift. Because no motors will be required to operate the site, significant noise is not expected. The treated effluent will not contain significant amounts of odor-causing constituents, and odors are not expected. Finally, lighting is not planned on the proposed sprayfield, so this is not expected to be a source of offsite impact. Assurances for Proposed Application Rate A determination of the site's ability to accept treated effluent at the maximum proposed application rate of 0.54 inch/week without adverse effects was based on (1) the hydraulic loading capacity of the site to receive the applied water, considering soil permeability and other physical site conditions, and (2) the allowable nitrogen loading rate, considering the ability of the vegetation to uptake the nitrogen contained in the treated effluent. The U.S. Environmental Protection Agency (EPA) publishes a general manual for technical assistance in designing land application systems across the United States. This manual, "Land Treatment of Municipal Wastewater - Process Design Manual" (EPA Manual), is cited as a general technical guidance source in DER Rule 17- 610.300(4), F.A.C. The EPA Manual contains formulae for the calculation of both the hydraulic loading capacity and the allowable nitrogen loading rate. The EPA Manual recommends use of the more restrictive of the hydraulic loading capacity or the allowable nitrogen loading rate as the hydraulic loading rate for the project. Hydraulic Loading Capacity. A hydraulic loading capacity of 0.63 inch/week for the proposed sprayfield was determined based on field exploration, laboratory testing, hydrogeological conditions and engineering evaluation, summarized in a report included in the application. This 0.63 inch/week hydraulic loading capacity is above the maximum proposed application rate of 0.54 inch/week and substantially below the maximum rate of 2 inches/week allowed by DER Rule 17-610.423(4), F.A.C. EPA Equation 4-3 for hydraulic loading capacity balances the volume of water that enters the site with the volume of water that leaves the site. Values in Equation 4-3 are evapotranspiration, which is the water released to the atmosphere from soil surfaces and by vegetation (ET); precipitation rate (rainfall); and Pw, which is water removed by vertical percolation downward through the soils. Due to the high vertical permeabilities of the sandy soils at this site, unrefined use of EPA Equation 4-3 would give a very high hydraulic loading capacity for this project, on the order of 10 times that proposed by FCWC. Therefore, a more detailed input/output water balance formula was used to determine annual hydraulic loading capacity (applied effluent in the formula) of 0.63 inch/week: rainfall + applied effluent + groundwater inflow = evapotranspiration, + groundwater outflow + surface run-off + evaporation + irrigation losses. The average annual rainfall, based on data from the U.S. NOAA weather station at Melbourne, is 48.17 inches. Due to the isolating effect of the deep ditches surrounding the site, groundwater inflow is considered to be so negligible that it was not assigned a value for the equation. ET, based on standard scientific references, is 45 inches/year for citrus trees. An additional 20 inches/year loss is attributable to grasses covering soil surfaces. In lieu of vertical percolation, groundwater outflow laterally through the surficial aquifer was projected to be 1.8 inches per year, based on hydraulic conductivity and soil permeabilities for the site. Surface run-off of stormwater was estimated to be 10 inches per year. Irrigation losses were estimated at 15% of the amount of applied effluent. Pond Storage Capacity. The proposed application rates for the two phases of the project are annual averages. The volume of storage needed for occasions when conditions preclude application must be determined. DER requires the calculation of storage by analytical means for the 10-year rainfall recurrence interval, using 20 years of rainfall data, and accounting for all water inputs on a monthly basis, using site-specific data. A minimum storage volume equal to three days application is required. Rule 17-610.414 (2), F.A.C. Calculations presented in the application met these requirements and showed storage needs of 8.08 million gallons (MG), or approximately 15 application days' volume, for Phase I; and 15 MG, or 25 application days for Phase II. Additional storage calculations, reflecting the monthly variations of wastewater inflow due to the seasonal population, were prepared for Phase I. These calculations reflected the same storage requirements. Petitioners' Allegations Regarding Application Rate and Storage Although they had prepared no analyses, performed no calculations, conducted no laboratory tests and undertaken only one field test (test hole for groundwater level), Petitioners' witnesses asserted that site conditions precluded successful operation of the sprayfield at the maximum proposed application rate of 0.54 inch/week. They asserted that swale pipes would plug and a clay "hardpan" at the bottom of the swales would prohibit percolation of stormwater. Thus, the swales would be full of water for long periods and further application would be precluded. They also asserted that significant volumes of treated effluent would leave the site as run-off. They alleged treated effluent would enter the swales directly from accumulation of spray and indirectly from seepage from the sides of the citrus mounds. Finally, Petitioners asserted 15 days of storage was inadequate because the site would be too wet for application for at least a month. FCWC presented testimony and evidence based on site reviews, numerous field and laboratory tests, computer modelling, and calculations that successfully refuted these allegations. Petitioners' expert in grove management and local soil conditions, Mr. Burnette, stated that extremely wet conditions required pumping of swales for weeks at a time in nearby groves. FCWC's experts asserted that the proposed sprayfield site currently has, and will continue to have, under proper maintenance, much better drainage than Mr. Burnette's groves, where regular grading of swale inverts and herbicide applications denude soil and cause erosion which plugs pipes and backs up water in the swales. In addition, unlike the situation described in Burnette's groves, the proposed site contains no swales that are lower in elevation than the collection ditches, thereby facilitating stormwater run-off. The top layer of soil comprising the citrus mounds and the swales is relatively clean sand. Petitioners' so-called "hardpan" is a slightly clayey to clayey fine sand layer which separates the upper sand from a thick layer of very clean, beach-type sand. FCWC geotechnical experts determined the clayey sand layer was 18 to 24 inches below the bottom of the swales. Without any field testing, Petitioners' expert hydrogeologist, Mr. Oros, asserted that the clayey sand layer was at the bottom of the swales. In contrast, Mr. Burnette stated that the clayey sand layer occurs four to eight inches below the bottom of the swales on the adjoining groves, where the graded swales are 10 to 14 inches deeper than the shallow swales on the proposed sprayfield site. Thus, Mr. Burnette's testimony supports the FCWC conclusion that this layer is found up to 2 feet below the swales on the proposed site. Moreover, contrary to Petitioners' assertions that the layer acts as a "hardpan", water can pass relatively freely through it and the water table will not "perch" above it. The U.S. Department of Agriculture Soil Conservation Service (SCS) reports a permeability value for this soil type of one to 12 feet per day. Dr. John Garlanger, FCWC expert in subsurface investigation and soil mechanics, conducted a field inspection of the soil and reviewed grain size distribution analyses. He determined that the permeability of the clayey sand layer is about one foot of water per day. Petitioners' expert hydrogeologist concurred that the layer could have this permeability rate. Soil is at the "wilting point" when its water content is too low for plants to transpire additional water. Soil is at "field capacity" when added water "fills up" the soil and it becomes saturated. The "water table" is the level at which the soil is totally saturated. Petitioners erroneously assert that 90% of the 0.54 inch of treated effluent will travel straight down to the water table. Instead, due to capillary action, the first foot of the sandy soil at the site can store about 0.6 inch of water between the wilting point and field capacity. If there is no rain between applications, 100% of the 0.54 inch will be transpired by vegetation out of the first foot of soil. This "resets" the soil moisture content to the wilting point in preparation for another application. If heavy rains cause the soil to remain at field capacity rather than returning to the wilting point through ET, the soil can still absorb up to 2.25 inches of water per foot, or three-fourths to one inch of water per four inches of soil, before it reaches saturation. Therefore, even if the soil is saturated up to 4 inches below the swales, the top 4 inches of soil will still absorb the 0.54 inch of treated effluent without reaching total saturation or causing any run-off. If subsequent heavy rains saturate the remaining soil and raise the water table to the bottom of the swales, the excess rainwater which falls on the saturated surface will run off as stormwater, and most of the treated effluent will remain stored within the soil. Furthermore, because the water table is proposed to be measured at centers of the blocks where, due to distance from the drainage ditches, the water table is closest to the surface, soil storage capacity across the site will exceed these projected levels. Petitioners' experts also asserted that if it rains after the 0.54 inch application, the groundwater will "mound" up below the citrus mounds, creating a hydraulic gradient or head differential (between the water table under the citrus mounds and the water table below the swales) sufficiently great to cause the treated effluent in the mound to flow toward the swales and seep into them from the sides of the citrus mounds. Mr. Golding admitted that such seepage would not occur when the groundwater table is below the bottom of the swales. Nevertheless, he opined that seepage of treated effluent would be considerable because he believed, based on opinion and experience alone, that the water table would be at the bottom of the swales or higher for at least 30 days straight in a "wet year." FCWC's experts successfully refuted these assertions. A significant portion of the treated effluent falling onto the citrus mounds will be stored in the soil as described above. The treated effluent (only applied when water level is 4 inches below the swales) that actually reaches the water table will cause only a very slight "water mound" (only 2 inches in 30 feet) which will not produce any appreciable "head" or lateral flow to the swales. On only three occasions (a total of 8 days) during the wettest year in ten did the "water mound" rise above the bottom of the swales resulting in any groundwater seepage from the citrus mounds into the swales. Thus, during the entire wettest year in ten, less than one-half of 1% (0.12 inch of the approximately 28 inches) of annual applied treated effluent, very diluted with groundwater, might seep from the mounds into the swale. Contrary to Petitioners' expert's assertion that the seasonal high water level (SHWL) was not provided by FCWC, this information was supplied in the application and was reaffirmed by calculations of Dr. Garlanger at rebuttal. The importance attached to the SHWL for this project was not adequately explained by Petitioners. FCWC experts explained that the SHWL is the average (NOT maximum) height of the groundwater during the two to six wettest months of the year. Because the water table varies throughout the year, it is the calculation of the position of the water table from month to month that is significant and is required by DER. This monthly changing water table was the basis of storage water balance calculations contained in the application. Even though the monthly storage calculation in the application meets the DER/EPA requirements, Petitioners' witnesses asserted that the application did not indicate how many days the water table would rise to four inches below the swales and thus how many days spraying was precluded and storage was required. Dr. Garlanger analytically calculated the water table beneath the site, using Darcy's Law, and known parameters at the site, such as the depths of the ditches, the geometry and relative distances, and the thickness and permeability of the soil layers. Thus, although never required for any of the 100 land application projects he has evaluated, Dr. Garlanger performed computer modelling and calculations to predict the daily level of the water table beneath the swales for both Phase I and II during the wettest year in ten. Water inputs in his model included treated effluent and daily rainfall from an actual year (1969) when rainfall reached the levels of the statistically wettest year in ten. Water losses were soil storage, ET, distribution losses, deep percolation and run-off. Treated effluent was not applied when the model predicted that the water table would be higher than four inches below the bottom of the swales and when there was significant rainfall (more than one-hundredth of an inch). This modelling predicted that 6.1 MG/11-day storage was needed for Phase I. Thus, the project as proposed has substantially more storage than needed, with a proposed 8.1 MG/15-day storage. The model produced similar results for Phase II, showing a total 10.1 MG/18-day storage need compared with the proposed 15 MG/25-day storage. Petitioners also challenged various "irrigation efficiency" figures used by FCWC experts. All water leaving a water source, in this case the WWTP, does not reach the roots of the crops for which it is intended. "Irrigation efficiency" expresses this fact as the percentage of water pumped that is used by the vegetation. In the monthly storage water balance calculations the applicant used an "irrigation efficiency" of 70% of the total applied treated effluent, which is recommended in IFAS Bulletin 247 and in the USDA, SCS, "Florida Irrigation Guide"; 15% of the applied treated effluent was attributed to "irrigation losses" in the calculations in the application to determine the hydraulic loading capacity; and Dr. Sholtes stated that data he used indicated that 94% of "the water that came out of the nozzle reached the ground" within the wetted area of the site and the remaining 6% was aerosol drift and evaporation. Petitioners' expert questioned whether an irrigation efficiency of 70%, 85% or 94% should have been used and suggested that the calculations should be redone. The expert misunderstood the terms, comparing the proverbial apples and oranges. With a 70% irrigation efficiency, 30% treated effluent is lost to the plants. Only a small portion of this 30% loss is attributable to aerosol drift and evaporation in the air. Most of the 30% treated effluent hits the ground but is still lost to the plants through evaporation of treated effluent intercepted on plant leaves, losses from the distribution system, e.g., leaky fittings at the WTTP, and percolation of water below the reach of plant roots. The "irrigation losses" (15%) in the application include all of those types of losses, except the treated effluent losses through percolation. This approximately 15% of the total treated effluent appeared as a separate value from "irrigation efficiency." Water Quality Assurances Nitrogen Loading Rate. Because nitrogen is generally the constituent of most concern for sprayfields, EPA Equation 4-4, which is intended to produce a conservative result, projects nitrogen loading possible without exceeding the groundwater standard for nitrate. Two FCWC experts calculated the allowable nitrogen loading rate. James Christopher, project engineer and expert in water quality and chemistry, adjusted the EPA equation to reflect stormwater leaving the site, which is a more technically correct refinement of the equation and has the effect of lowering the allowable rate. A "U value" (the variable for rate of nitrogen uptake by crop)of 100 kilograms/hectare/year (kg/ha/yr) was used by James Christopher. Dr. Harvey Harper, another FCWC water quality expert, an environmental engineer, who has taught numerous university courses in wastewater treatment and has been involved in scientific studies of pollution removal, also calculated the nitrogen loading rate for the annual average rainfall and the wettest year in ten. He did not adjust EPA Equation 4-4 for stormwater run-off, because Petitioners had questioned any deviations from the formula. He used a U value of 150 kg/ha/yr, because he considered a value of 100 too low to be realistic. He used the highest nitrogen value in data from the WWTP. Other values he used in the equation were nearly identical to those of Mr. Christopher. The results were an allowable nitrogen loading rate of 0.75 inch/week for a year of average rainfall and 0.93 inch/week for the wettest year in ten. These rates are substantially higher than the proposed gross hydraulic loading rate of 0.54 inch/week. Petitioners' expert, Dr. J. P. Subramani, asserted that a U value of 0 kg/ha/yr should have been used, although he admitted that a site with a U value of 0 kg/ha/yr would be bare sand devoid of vegetation. The U values of 100 and 150 kg/ha/yr used by FCWC were extremely conservative. The EPA Manual provides U value ranges for forage grasses, at a low of 130-225 kg/ha/yr for bromegrass, to a high of 400-675 kg/hayr for coastal bermuda grass. Ignoring the testimony of FCWC witnesses that the grass would be mowed and removed from the site, Dr. Subramani supported his opinion only with the unfounded contrary assertion that the vegetation on site will not be harvested and removed as a crop. Petitioners alleged that discharges from the site would contaminate surface and ground waters and otherwise adversely affect water quality; inadequate renovation of pollutants would take place in the soil; and the receiving waters were already below standards. Petitioners' experts did no studies or analyses, nor did they predict expected concentrations for any parameters for sprayed treated effluent leaving the site as surface waters or groundwaters. Petitioners' exhibits regarding water quality issues consisted of two single-day monitoring reports for the existing WWTP discharge and the Canal and a set of 1990-91 water quality report sheets for the WWTP. FCWC's expert, Dr. Harper, analyzed the project's impacts on groundwater and on surface waters (the Canal) if the treated effluent were to leave the site as surface run-off in the swales, as groundwater seepage into the collection ditches, or as aerosol drift. Based on 1990-91 water quality monitoring of the WWTP's existing treated effluent, Dr. Harper projected the concentrations of parameters of concern for the treated effluent to be sprayed at the site. Although monitoring of heavy metals is not required at the WWTP, he also projected levels for these parameters based on EPA figures and existing data from two larger domestic wastewater treatment plants. Because those two plants have contributions from industrial and commercial components not found at the WWTP, the projections substantially over-estimated heavy metals expected for the WWTP. Groundwater Impacts. Dr. Harper estimated the pollution removal efficiencies for treated effluent traveling through approximately one foot of soil by reference to the EPA Manual and a study he had performed. He then applied these efficiencies to the projected concentrations for the sprayed treated effluent. Even at maximum projected concentrations, the results showed that projected constituents would be at or better than groundwater quality standards after renovation in the soil. Thus, due to low levels of constituents of concern, including those for which no numerical standard is provided in the rules, the project will not cause groundwater water quality violations and will have no adverse effect on the biological functions in the groundwaters directly underlying the site. Contrary to Petitioners' assertions, DER witnesses stated that DER does not interpret provisions of Rules 17-600.530(4) and 17-610.310(3)(c)4, F.A.C., as requiring background groundwater samples in the application. Because research has shown that groundwater quality results for sprayfields are generally very good, DER routinely defers such sampling until after permit issuance. Thus, the groundwater monitoring plan in the application and in the draft sprayfield permit provides that all monitoring wells will be sampled to establish background water quality and results submitted to DER prior to spray irrigation. DER's expert witness in environmental engineering and wastewater land application design, Christianne Ferraro, as well as John Armstrong, DER's environmental specialist in site contamination clean-up, stated that they had reviewed groundwater monitoring currently provided by FCWC for the WWTP. They found no nitrogen violations. Surface Water Impacts. The preponderant evidence showed that treated effluent will not flow directly into the swales. Therefore, FCWC proved it will not leave site as surface run-off. However, in order to project the worst-case water quality evaluation for droplets greatly diluted by rainwater or groundwater which may enter the swales, it was assumed that all treated effluent landing within swales "made of glass" would run off directly into the Canal. In addition, uptake, removal or dilution likely to occur in the collection ditches was ignored. Pollution removal efficiencies for grassed swales (based on a year-long study) were applied to the projected concentrations for the treated effluent. After renovation in the swales, any treated effluent leaving the site would contain concentrations for parameters of concern at or better than surface water quality standards. Therefore, water quality in the receiving surface waters will not be violated. Due to removal efficiencies for soils, the treated effluent leaving the site as groundwater seepage into the collection ditches is expected to meet surface water quality standards. In addition, the trace quantity of effluent (0.12 inch for wettest year in ten) which may seep into the swales will reach the San Sabastian Canal only after being greatly diluted within the groundwater and filtered and purified in the soil in the citrus mounds and grassed swales. Even projecting ten times the amount of aerosol drift predicted for the project, the water quality impact of any sprayed treated effluent entering the Canal as drift is so small as to be insignificant. Ambient Water Quality. The existing discharge is having minimal effect on the water quality of the Canal. Furthermore, by eliminating the direct discharge, the project will reduce the present impacts on the Canal by 92-99%. Nonetheless, Petitioners suggest that the project may further degrade ambient waters which they allege are already below standards. Dr. Harper assessed the ambient water quality characteristics of the Canal, which is Class III fresh surface water and the ultimate receiving water for the site. Even including water quality data for the Canal put in evidence by Groves, the Canal is not currently at or below any state water quality standards for Class III waters, except for occasional Dissolved Oxygen (DO) levels. Levels of DO in sprayed treated effluent are expected to be very high. Even if groundwater seepage into the collection ditches and the Canal from the proposed sprayfield contains low levels of DO due its travel underground, it will not lower levels of DO in the ambient waters because the groundwater will also be low in BOD, which depresses DO. Thus, groundwater seepage is expected to have a neutral effect on ambient DO or to increase DO levels due to its diluting effect on BOD. Groundwater inflow to the site is negligible but outflow occurs at a significant measured rate. The only significant inputs are sprayed treated effluent and rainfall. Therefore, the groundwater under the site will eventually reach a stable condition where its constituent levels are the average of the constituent levels in rainwater and the treated effluent. The treated effluent to be applied on this site is at or above state groundwater standards. Necessarily, regardless of the condition of the existing groundwater it cannot possibly be degraded by the treated effluent to below state standards and may well be improved by it. Thus, FCWC has provided reasonable assurances that Rule 17- 600.530(4), F.A.C., has been met, without monitoring of ambient groundwaters in the application. The deposition of treated effluent will not violate the standard that all waters of the state shall be free from components which, alone or in combination with other substances, are present in concentrations that are carcinogenic or teratogenic to humans, animals or aquatic species or that pose a serious threat to public health, safety or welfare. Human Health Risk and Contamination. Petitioners allege that the sprayfield poses a hazard for contamination of their properties. They produced no witness or evidence of contamination other than experts in grove management, citrus production and management, and Petitioners themselves, who expressed scientifically unsubstantiated fears of the impact of the sprayfield on human health or the marketing of their fruit and honey. FCWC expert Dr. Christopher Teaf, who teaches biology, toxicology and risk assessment at Florida State University and is also president and principal toxicologist with a firm doing hazardous substance and waste management research, determined that the project poses no off-site contamination hazard. Pathogens. Fecal coliform is a standard measure for the health hazards of treated effluent based on an indicator group of microbiological organisms, present in the intestinal tracts of all warm-blooded animals as well as a number of insects and cold-blooded species. These organisms do not themselves ordinarily cause human disease, but may indicate the presence of other pathogenic organisms. Coliform bacteria are common in water bodies in general, and the state limit for these bacteria is 200/100 ml. Rule 17- 302.560(6), F.A.C. The World Health Organization has concluded that levels as high as 1,000/100 ml constitute an adequate standard and will not be associated with human disease. Only extremely limited numbers of bacteria can survive the hazardous journey from the WTTP to the Petitioners' property. First, required chlorination at the WWTP will reduce the coliforms to no more than 200/100 ml. At that level, pathogenic bacteria are negligible, if present at all. Pressures during ejection from the spray heads will cause a 70-90% mortality rate. Once airborne, bacteria will be killed because of temperature, ultraviolet radiation and desiccation. As water drops evaporate, constituents become more concentrated and the drops become toxic environments for bacteria. Bacteria falling to earth are filtered in the first few inches of surface soils. Any organisms borne off site will find that, due to the antibacterial qualities of citrus peel and fruit and the plethora of chemical agents routinely applied, the adjacent groves are an extremely inhospitable environment. Too few bacteria will survive at FCWC's proposed application levels, or at 10 times those levels, to constitute an infective dose and contribute to the incidence of human disease. Thus, treated effluent in the form of aerosol drift will have no adverse effect on the health of humans or otherwise cause contamination of areas adjacent to the proposed sprayfield. Consumption of Fruit. Bacteria are not taken up by the plant roots and the aerosol drift will not have any effect on the actual health of the citrus trees themselves. The minimal deposition from spray will be removed through washing required by governmental standards to remove dirt, grime and other contamination, such as fungicides, herbicides and pesticides applied as a normal practice in the citrus industry. Based on fifteen years of scientific literature, including the EPA Manual, crops irrigated with treated effluent do not contribute to human health problems in populations that consume those crops. With application of treated effluent with bacterial concentrations, even 10,000 to 100,000 times higher than the standard, there has been no incidence of human disease related to the consumption of such crops. Part II of Rule 17-610, F.A.C., "Reuse: Slow rate land application systems; restricted public access;" governs the type of sprayfield proposed by FCWC. Petitioners alleged that, due to the proximity of their groves and beekeeping activities, higher levels of treatment than those in Part II should be required. They argued that "advanced wastewater treatment" (AWT), defined in Section 403.086(4), F.S., would be more appropriate. This statute gives DER the discretion to require AWT when it deems necessary. Section 403.086(1)(a), F.S. However, AWT would not meet the requirements of Part III of Rule 17-610, which governs irrigation ("direct contact") of edible food crops and requires Class I reliability for treatment which is not required for AWT. Section 403.086(4), F.S.; Rule 17-610.460 and 17-610.475, F.A.C. Adjacent land uses were a part of the permit review for this project required in Part II. Buffer restrictions provide protection from the sprayfield so that levels of deposition are negligible compared to those when spray irrigation is applied directly at the food crop site. Thus, by its decision to issue this permit, DER recognized that minimal aerosol drift is not the "direct contact" envisioned in Part III and that because the project did not pose a hazard to adjoining groves higher levels of treatment are not necessary. Aerosol drift from treated effluent will have no effect on human health due to contamination of honey or adverse effects on the Shreve's bees located near the proposed sprayfield. Natural enzymes in unpasteurized honey are hostile to bacteria. The Shreves have never experienced a problem with the existing forty acre sprayfield even though it is accessible to their bees and has been in the area as long as the bees have. Petitioners allege that the sprayfield will attract birds, creating an aviation hazard to airplanes using the grass airstrip owned by Petitioner, Parrish Properties. Mr. Parrish, who is a licensed pilot, asserted that water ponding on the site and the mowing operation will attract birds. Both the proposed sprayfield and the surrounding groves will be mowed and irrigated and thus will provide the same type of mixed grass and citrus tree habitat as presently found in the groves. Therefore, Petitioners are currently attracting the same type and number of birds to their groves as FCWC's proposed sprayfield will attract. FCWC's expert in botany and ornithology, Mr. Noel Wamer, observed no large birds at the site, the existing 40-acre sprayfield or the surrounding citrus groves. He did observe small birds such as northern cardinals, towhees, and warblers, typical of citrus grove habitats. Cattle egrets might also be expected in the groves and the proposed sprayfield, particularly during mowing operations. Wading birds would only be attracted if water remained on the site for approximately one week or more to allow development of aquatic organisms as a food source. Birds present on the proposed sprayfield are very unlikely to fly up and collide with planes. The grass airstrip is used infrequently, with only 12 landings in the past year. For a number of years Mr. Wamer has observed bird behavior at the Tallahassee sewage treatment plant sprayfields near the Tallahassee Airport. The one-half mile distance between the runway and sprayfields in Tallahassee is nearly the same as the distance between the Petitioners' grass airstrip and the site. Planes landing at the Tallahassee airport are at an altitude of between 500 and 600 feet over the sprayfields, the same height as predicted over the site. Regardless of the size of planes, the birds, primarily cattle egrets, do not react, but continue feeding or resting. Stormwater and Surface Water Management Activities. On April 3, 1991, FCWC submitted an application with DER to modify and operate the existing stormwater and surface water management system on the sprayfield site (MSSW system). The Notice of Intent to Issue the MSSW Permit was published in the Florida Today newspaper on July 27, 1991. Minor activities are proposed to improve the existing system: (1) culverts at the ends of swales will be cleaned to restore full flow capacity; (2) obstructions and excess vegetation will be removed from the collection ditches to restore their original flow lines; and (3) any depressions in the swales will be filled and regraded to attain a minimum swale bottom elevation of 20.2 feet above mean sea level. As asserted by DER's expert in surface water management, the stormwater discharges will not be a combination of stormwater and domestic waste sufficient to trigger review of stormwater under DER rules as required by Rule 40C-42.061(3), F.A.C. Considering all proof adduced, particularly that stormwater will be treated to applicable standards in the grassed swales, water quality will not be violated, and the post- development peak discharge will not exceed the pre-development peak discharge from the site, FCWC provided reasonable assurances that the proposed MSSW system would not be harmful to the water resources in the area and would not be inconsistent with the overall objectives of the district. Summary of Findings and Permit Conditions FCWC has established that the sprayfield, as proposed, will meet the applicable regulatory requirements for the sprayfield and MSSW permits. Included in the specific conditions attached to the notice of intent to issue the sprayfield construction permit is the requirement that the site be operated to preclude saturated ground conditions or ponding. (FCWC Exhibit #3, paragraph 13, specific conditions). Witnesses for the applicant described certain proposals to assure this condition is met, and those proposals should be incorporated into the condition. Those proposals include the cessation of spraying during a rain event and the installation of devices to automatically turn off the sprinklers when rain occurs, the cessation of spraying whenever the groundwater level is within four inches of the bottom of the swales, and the installation of ground water gauges to determine when this level is reached. In order to minimize aerosol drift, the applicant proposes to establish wind gauges indicating the direction and speed of wind at the site. It was suggested that spraying would cease when the wind reaches 20 miles an hour, and sprinklers should be positioned to avoid spraying the downwind perimeter of the site when drift is likely to occur. This condition should also be incorporated in the permit. If the operational adjustments cannot be made automatically it will be necessary to require that the plant be staffed at all times that the spray system is turned on, notwithstanding the minimum six hours, five days a week required in Rule 17-602.370, F.A.C. and referenced in the intent to issue. Engineering computations in the application rely on the assumption that the vegetation onsite will be harvested (mowed and removed). Since spray irrigation treatment of wastewater depends on renovation or removal of effluent by the soil vegetation system, periodic mowing and removal of the vegetation should also be included as a permit condition.
Recommendation Based on the foregoing, it is hereby, RECOMMENDED: That a final order be entered issuing permits number DC05-194008 and MS05- 194894, with the additional conditions addressed in Finding of Fact paragraphs 60 and 61, above. DONE and RECOMMENDED this 27th day of May, 1992, in Tallahassee, Leon County, Florida. MARY CLARK Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 27th day of May, 1992. APPENDIX TO RECOMMENDED ORDER The following constitute specific rulings on the findings of fact proposed by Petitioners, Groves and Shreve: Rejected as unsupported by competent evidence (as to the allegation of irresponsible plant operation). 2.-4. Rejected as irrelevant. 5.-7. Addressed in Conclusions of Law. Rejected as irrelevant. Adopted in paragraph 9. 10.-11. Rejected as contrary to the weight of evidence as to "irrigation efficiency". 12.-13. Rejected as contrary to the weight of evidence. Rejected as contrary to the weight of evidence and mischaracterization of the witness' testimony. Rejected as unnecessary. Rejected as statement of testimony, not finding of fact, which testimony is outweighed by other evidence. 17.-18. Adopted in paragraph 3. 19. Adopted in paragraph 28. 20.-21. Adopted in paragraph 8. 22.-23. Adopted in substance in paragraph 22. Rejected as contrary to the weight of evidence. Average annual application rate of .54 inches/week yields 28 inches a year. Rejected as unnecessary. Addressed in Conclusions of Law. 26.-29. Rejected as contrary to the weight of evidence. 30.-31. Rejected as unnecessary. Rejected as contrary to the weight of evidence. Adopted in paragraph 19. Adopted in paragraph 20. Adopted in paragraph 11. Adopted in paragraph 19. Addressed in paragraph 36; adopted in substance. 38.-39. Rejected as unnecessary. 40. Adopted in paragraph 31. 41.-47. Rejected as unnecessary, or contrary to the weight of evidence as to "irrigation efficiency". 48.-49. Rejected as cumulative and unnecessary. 50. Adopted in paragraph 34. 51.-52. Rejected as contrary to the weight of evidence. The grass will be mowed and removed. The "U" value was based on the grasses, not the citrus. 53. Rejected as contrary to the evidence, as to "unknown density and type". 54.-57. Rejected as unnecessary. Rejected as contrary to the evidence. Adopted in paragraph 7. Rejected as unnecessary. Rejected as contrary to the weight of evidence. Rejected as unnecessary. 63.-64. Rejected as contrary to the weight of evidence. 65. Rejected as confusing, as to the term "unsuitable conditions". 66.-69. Rejected as contrary to the evidence. 70. Rejected as confusing. 71.-72. Rejected as unnecessary. 73.-74. Rejected as a mischaracterization of the witnesses' testimony. 75.-82. Rejected as unnecessary. Rejected as contrary to the weight of evidence. 84.-85. Rejected as unnecessary. 86.-87. Rejected as contrary to the evidence. 88.-89. Rejected as unnecessary. 90.-94. Rejected as contrary to the evidence. 95.-97. Rejected as unnecessary. 98.-99. Addressed in Conclusions of Law. 100.-103. Rejected as contrary to the weight of evidence. 104.-109. Rejected as a mischaracterization of the testimony or misunderstanding of the term "irrigation efficiency". 110.-112. Rejected as cumulative and unnecessary. 113.-114. Addressed in Conclusions of Law. Rejected as unnecessary. Addressed in Conclusions of Law. 117.-118. Rejected as irrelevant. Rejected as contrary to the law and evidence. Rejected as unnecessary. Adopted in paragraph 16 by implication. Rejected as unnecessary and misunderstanding of the testimony. Addressed in Conclusions of Law. 124.-126. Rejected as unnecessary. Rejected as contrary to the weight of evidence. Adopted by implication in paragraph 21. 129.-130. Rejected as unnecessary. 131. Rejected as contrary to the evidence. 132.-134. Rejected as unnecessary. 135.-138. Rejected as contrary to the evidence. 139.-141. Rejected as unnecessary. COPIES FURNISHED: Kenneth G. Oertel, Esquire M. Christopher Bryant, Esquire OERTEL, HOFFMAN, FERNANDEZ & COLE, P.A. P. O. Box 6507 Tallahassee, FL 32314-6507 Harry A. Jones, Esquire EVANS, JONES & ABBOTT P.O. Box 2907 Titusville, FL 32781-2907 Kathleen Blizzard, Esquire Richard W. Moore, Esquire P.O. Box 6526 Tallahassee, FL 32314 Douglas MacLaughlin Asst. General Counsel Dept. of Environmental Regulation 2600 Blairstone Rd. Tallahassee, FL 32399 Daniel H. Thompson, General Counsel Dept. of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, FL 32399-2400
The Issue The issue is whether the applicant for an Environmental Resource Permit ("ERP"), the City of Deltona ("City" or "Applicant"), has provided reasonable assurance that the system proposed complies with the water quantity, environmental, and water quality criteria of the St. Johns River Water Management District's ("District") ERP regulations set forth in Florida Administrative Code Chapter 40C-4, and the Applicant's Handbook: Management and Storage of Surface Waters (2005).
Findings Of Fact The District is a special taxing district created by Chapter 373, Florida Statutes, charged with the duty to prevent harm to the water resources of the District, and to administer and enforce Chapter 373, Florida Statutes, and the rules promulgated thereunder. The City of Deltona is a municipal government established under the provisions of Chapter 165, Florida Statutes. The Lake Theresa Basin is comprised primarily of a system of interconnected lakes extending from Lake Macy in the City of Lake Helen to the Butler Chain of Lakes (Lake Butler and Lake Doyle). The Lake Theresa Basin is land-locked and does not have a natural outfall to Lake Monroe and the St. Johns River. In 2003, after an extended period of above-normal rainfall in the Deltona area, the lakes within the land-locked Lake Theresa Basin staged to extremely high elevations that resulted in standing water in residential yards, and rendered some septic systems inoperable. Lake levels within the Lake Theresa Basin continued to rise and were in danger of rising above the finished floor elevations of some residences within the basin. On March 25, 2003, the District issued an Emergency Order (F.O.R. No. 2003-38) authorizing the construction and short-term operation of the Lake Doyle and Lake Bethel Emergency Overflow Interconnection. Since wetland and surface water impacts would occur, the Emergency Order required the City of Deltona to obtain an ERP for the system. The project area is 4.1 acres, and the system consists of a variable water structure on the west shore of Lake Doyle connected to a series of pipes, swales, water control structures, and wetland systems which outfall to a finger canal of Lake Bethel, with ultimate discharge to Lake Monroe and the St. Johns River. The first segment of the system extends downstream from the weir structure on the west shore of Lake Doyle via a pipe entrenched in the upland berm of the Sheryl Drive right-of-way. The pipe passes under Doyle Road and through xeric pine-oak uplands to the northeast shore of a large (approximately 15 acres) deepwater marsh. Water flows south through the deepwater marsh where it outfalls through four pipes at Ledford Drive. Two of the four pipes are overflow structures, controlled by canal gates. The pipes at Ledford Drive discharge into a ditch and into a large (greater than 20 acres) shallow bay swamp. The south end of the bay swamp is defined (and somewhat impounded) by a 19th Century railroad grade. Water flows through the bay swamp where it outfalls through five pipes at the railroad grade. Three of the five pipes are overflow structures, controlled by channel boards. The pipes at the railroad grade discharge to a 1500-foot long finger canal that was dug some time during the period 1940-1972 from the north central shore of Lake Bethel. The overflow interconnection system has three locations whereby the system can be shut down: 1) Lake Doyle--a control weir, controlled by three sluice gates; 2) Ledford Drive--two thirty-inch reinforced concrete pipes, controlled by canal gates; and 3) railroad grade--three thirty-inch reinforced concrete pipes, controlled by channel boards (collectively referred to as "Overflow Structures"). The Overflow Structures are designed to carry the discharge of water from Lake Doyle to Lake Bethel. With the Overflow Structures closed the system returns to pre-construction characteristics, meaning there will be no increase or decrease in the quantity or quality of water throughout the path of the system as a result of the project. An unequivocal condition of the permit is that the system would operate with all of the Overflow Structures closed. As an added assurance, the City proposes to place a brick and mortar plug in the Lake Doyle weir structure outfall pipe to prevent any discharge from the weir. The City has submitted to the District preliminary plans for a future phase in which the system would be modified for the purpose of alleviating high water levels within the Lake Theresa Basin when the water level in Lake Doyle rises above an elevation of 24.5 feet. The District shall require a separate permit application to be submitted for such future plans. Petitioner, Barbara Ash, has lived on Lake Theresa for 19 years. Ms. Ash lives upstream from the area of the weir that will be plugged in accordance with the ERP. She does not trust either the City of Deltona to comply with or the District to enforce the conditions of the ERP applied for by the City. Petitioner, Barbara Ash, also served as the qualified representative for Petitioners, Francell Frei, Bernard J. and Virginia Patterson, and Ted and Carol Sullivan. Ms. Ash represented that Ms. Frei has lived on Lake Theresa for 12 years, and both the Pattersons and the Sullivans live on Lake Louise, which is within the area of concern in this proceeding. Petitioner, Diana Bauer, has lived on Lake Theresa since February 2004. She fears that the lake will become too dry if the system is allowed to flow. She also believes the wildlife will be adversely affected if the water levels are too low since many species need a swampy or wet environment to thrive. She fears her property value will decrease as a result of the approval of the ERP. She also does not trust either the City to comply with or the District to enforce the conditions of the ERP. Petitioner, Howard Ehmer, lives two to three hundred yards down Lake Theresa from Ms. Bauer. He is concerned about the lake bed being too dry and attracting people on all terrain vehicles who enjoy driving around the lake bottom. He is concerned about his property value decreasing if the lake bed is dry. Further, when the lake level is too low, people cannot enjoy water skiing, boating, and fishing on Lake Theresa. Petitioner, Phillip Lott, a Florida native, has also owned and lived on property abutting Lake Theresa since 1995. Mr. Lott has a Ph.D. in plant ecology, and M.P.A. in coastal zone studies, an M.B.A. in international business, and a B.S. in environmental resource management and planning. Mr. Lott has been well acquainted with the water levels on Lake Theresa for many years. Based upon his personal observations of the lake systems in the Deltona area over the years, Mr. Lott has seen levels fluctuate greatly based upon periods of heavy and light rainfall. Mr. Lott is concerned that the District will permit the City to open the weir to let water flow through the system and cause flooding in some areas and low water levels in other areas. He fears that the District will allow the water to flow and upset the environmental balance, but he admits that this ERP application is for a closed system that will not allow the water to flow as he fears. Mr. Lott similarly does not trust the City to comply with and the District to enforce the conditions of the ERP. Petitioners, James E. and Alicia M. Peake, who were represented by Steven L. Spratt at hearing as their qualified representative, live on Lake Louise, which is interconnected with the Lake Theresa basin. The Peakes are concerned that if the level of Lake Louise drops below 21 feet, nine inches, they will not be able to use the boat launch ramps on the lake. Petitioner, Steven L. Spratt, also lives on Lake Louise, and is concerned about the water levels becoming so low that he cannot use the boat launch on the lake. He has lived on the lake since 2000, and remembers when the water level was extremely low. He fears that approval of the ERP in this case will result in low levels of water once again. Petitioner, Gloria Benoit, has live on Lake Theresa for two years. She also enjoys watching recreational activities on the lake, and feels that approval of the ERP will devalue her lakefront property. Ms. Benoit appeared at the first day of the hearing, but offered no testimony on her behalf. J. Christy Wilson, Esquire, appeared prior to the final hearing as counsel of record for Petitioners, Steven E. Larimer, Kathleen Larimer, and Helen Rose Farrow. Neither Ms. Wilson nor any of the three Petitioners she represented appeared at any time during the hearing, filed any pleadings seeking to excuse themselves from appearing at the final hearing, or offered any evidence, testimony, pre- or post- hearing submittals. Petitioner, Gary Jensen, did not appear at hearing, did not file any pleadings or papers seeking to be excused from appearing at the final hearing, and did not offer any evidence, testimony, pre- or post-hearing submittals. Both the City and the District recognize that areas downstream from the project site, such as Stone Island and Sanford, have experienced flooding in the past in time of high amounts of rainfall. The system proposed by the City for this ERP will operate with the overflow structures closed and a brick and mortar plug in the outfall pipe to prevent water flow from Lake Doyle to Lake Bethel. So long as the overflow structures are closed, the system will mimic pre-construction flow patterns, with no increase in volume flowing downstream. The District has considered the environment in its proposed approval of the ERP. The area abutting the project is little urbanized and provides good aquatic and emergent marsh habitat. With the exception of the western shore area of the deepwater marsh ("west marsh area"), the bay swamp and remaining deepwater marsh area have good ecological value. In the 1940's, the west marsh area was incorporated into the drainage system of a poultry farm that occupied the site. This area apparently suffered increased nutrient influxes and sedimentation that contributed to a proliferation of floating mats of aquatic plants and organic debris. These tussocks reduced the deepwater marsh's open water and diminished the historical marsh habitat. Water under the tussocks is typically anoxic owing to total shading by tussocks and reduced water circulation. Thick, soft, anaerobic muck has accumulated under the matted vegetation. Exotic shrubs (primrose willow Ludwigia peruvania) and other plants (cattails Typha spp.) dominate the tussocks. The construction of the project, from the 2003 Emergency Order, resulted in adverse impacts to 1.3 acres of wetlands having moderately high- to high ecological value and 0.2 acres of other surface waters. The 0.2 acre impact to other surface waters was to the lake bottom and the shoreline of Lake Doyle where the weir structure was installed. The 0.3 acres of wetland impacts occurred at the upper end of the deepwater marsh where the pipe was installed. The largest wetland impact (1.0 acre) was to the bay swamp. The bay swamp is a shallow body dominated by low hummocks and pools connected inefficiently by shallow braided channels and one acre is filled with a 1-2 foot layer of sediment following swamp channelization. Disturbance plants (e.g., primrose willow, Ludwigia peruvania, and elderberry Sambucus Canadensis) now colonize the sediment plume. Pursuant to the District's elimination and reduction criteria, the applicant must implement practicable design modifications, which would reduce or eliminate adverse impacts to wetlands and other surface waters. A proposed modification, which is not technically capable of being done, is not economically viable, or which adversely affects public safety through endangerment of lives or property is not considered "practicable." The City reduced and/or eliminated the impacts to the lake bottom and shoreline of Lake Doyle and deepwater marsh, to the extent practicable. The impacts were the minimum necessary to install the weir structure and pipe for the system; the weir structure and pipe were carefully installed on the edges of the wetland and surface water systems, resulting in a minimum amount of grading and disturbance. To compensate for the loss of 1.3 acres of wetlands and 0.2 acres of other surface waters, the City proposes to preserve a total of 27.5 acres of wetlands, bay swamp, marsh, and contiguous uplands. Included in this 27.5 acres are 6.4 acres of the west marsh, which are to be restored. The parties stipulated that the mitigation plan would adequately compensate for losses of ecological function (e.g. wildlife habitat and biodiversity, etc.) resulting from the project. Water quality is a concern for the District. Lake Monroe is included on the Florida Department of Environmental Protection's verified list of impaired water bodies for nitrogen, phosphorous, and dissolved oxygen. Water quality data for Lake Monroe indicate the lake has experienced high levels of nitrogen and phosphorous and low levels of dissolved oxygen. Prior to construction of the project, there was no natural outfall from the Lake Theresa Basin to Lake Monroe and therefore no contribution from this basin to nitrogen and phosphorous loadings to Lake Monroe. Lake Colby, Three Island Lakes (a/k/a Lake Sixma), and the Savannah are surface waters within the Lake Theresa Basin for which minimum levels have been adopted pursuant to Florida Administrative Code Chapter 40C-8. The system will operate with the overflow structures closed and a brick and mortar plug in the outfall pipe to prevent water flow from Lake Doyle to Lake Bethel, resulting in no outfall from the Theresa Basin to Lake Monroe. Minimum flows established for surface waters within the Lake Theresa Basin will not be adversely impacted. Under the first part of the secondary impact test, the City must provide reasonable assurance that the secondary impacts from construction, alteration, and intended or reasonable expected use of the project will not adversely affect the functions of adjacent wetlands or surface waters. The system is designed as a low intensity project. As proposed, little activity and maintenance are expected in the project site area. The reasonably expected use of the system will not cause adverse impacts to the functions of the wetlands and other surface waters. None of the wetland areas adjacent to uplands are used by listed species for nesting or denning. In its pre-construction state, the project area did not cause or contribute to state water quality violations. Under the second part of the secondary impact test, the City must provide reasonable assurance that the construction, alteration, and intended or reasonably expected uses of the system will not adversely affect the ecological value of the uplands to aquatic or wetland dependent species for enabling existing nesting or denning by these species. There are no listed threatened or endangered species within the project site area. Under the third part of the secondary impact test, and as part of the public interest test, the District must consider any other relevant activities that are closely linked and causally related to any proposed dredging or filling which will cause impacts to significant historical and archaeological resources. When making this determination, the District is required, by rule, to consult with the Division of Historical Resources. The Division of Historical Resources indicated that no historical or archaeological resources are likely present on the site. No impacts to significant historical and archaeological resources are expected. Under the fourth part of the secondary impact test, the City must demonstrate that certain additional activities and future phases of a project will not result in adverse impacts to the functions of wetlands or water quality violations. The City has submitted to the District preliminary plans for a future phase in which the system would be modified for the purpose of alleviating high water levels within the Lake Theresa Basin when the level in Lake Doyle rises above an elevation of 24.5 feet. Based upon the plans and calculations submitted, the proposed future phase, without additional measures, could result in minor increases in the loadings of nitrogen and phosphorous to Lake Monroe. Lake Monroe is included on the Florida Department of Environmental Protection's verified list of impaired water bodies due to water quality data indicating the lake has experienced high levels of nitrogen and phosphorous, and low levels of dissolved oxygen. Under this potential future phase, there would be an outfall from the Lake Theresa Basin to Lake Monroe. To address the impact on water quality of this potential future phase, the City has submitted a loading reduction plan for nitrogen, phosphorous, and dissolved oxygen. The plan includes compensating treatment to fully offset the potential increased nutrient loadings to Lake Monroe. Specifically, the loading reduction plan includes: Construction and operation of compensating treatment systems to fully offset anticipated increased nutrient loadings to Lake Monroe. Weekly water quality monitoring of the discharge from Lake Doyle for total phosphorous and total nitrogen. A requirement that the overflow structure be closed if the total phosphorous level reaches 0.18 mg/l or higher or the total nitrogen level reaches 1.2 mg/l or higher in any given week and will remain closed until levels fall below those limits. The implementation of these water quality mitigation measures will result in a net improvement of the water quality in Lake Monroe for nitrogen, phosphorous, or dissolved oxygen. The future phase was conceptually evaluated by the District for impacts to wetland functions. The future phase as proposed could result in adverse impacts to wetland functions. Operation of the system with the overflow structures open could impact the bay swamp and deepwater marsh. The City has demonstrated that any adverse impacts could be offset through mitigation. Based upon the information provided by the City and general engineering principles, the system is capable of functioning as proposed. The City of Deltona will be responsible for the operation, maintenance, and repair of the surface waster management system. A local government is an acceptable operation and maintenance entity under District rules. The public interest test has seven criteria. The public interest test requires the District to evaluate only those parts of the project actually located in, on, or over surface waters or wetlands, to determine whether a factor is positive, neutral, or negative, and then to balance these factors against each other. The seven factors are as follows: the public health, safety, or welfare of others; conservation of fish and wildlife and their habitats; fishing, recreational value, and marine productivity; temporary or permanent nature; 5) navigation, water flow, erosion, and shoaling; 6) the current condition and relative value of functions; and 7) historical and archaeological resources. There are no identified environmental hazards or improvements to public health and safety. The District does not consider impacts to property values. To offset any adverse impacts to fish and wildlife and their habitats, the City has proposed mitigation. The areas of the project in, on, or over wetlands do not provide recreational opportunities. Construction and operation of the project located in, on, or over wetlands will be permanent in nature. Construction and operation of the project located in, on, or over wetlands will not cause shoaling, and does not provide navigational opportunities. The mitigation will offset the relative value of functions performed by areas affected by the proposed project. No historical or archaeological resources are likely on the site of the project. The mitigation of the project is located within the same drainage basin as the project and offsets the adverse impacts. The project is not expected to cause unacceptable cumulative impacts.
Recommendation Based upon the Findings of Fact and Conclusions of Law, it is RECOMMENDED that a Final Order be entered granting the City of Deltona's application for an environmental resource permit with the conditions set forth in the Technical Staff Report, and dismissing the Petitions for Formal Administrative Hearing filed by Gary Jensen in Case No. 04-2405, and by Steven E. Larimer, Kathleen Larimer, and Helen Rose Farrow in Case No. 04-3048. DONE AND ENTERED this 27th day of May, 2005, in Tallahassee, Leon County, Florida. S ROBERT S. COHEN 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 27th day of May, 2005. COPIES FURNISHED: George Trovato, Esquire City of Deltona 2345 Providence Boulevard Deltona, Florida 32725 Diana E. Bauer 1324 Tartan Avenue Deltona, Florida 32738 Barbara Ash, Qualified Representative 943 South Dean Circle Deltona, Florida 32738-6801 Phillip Lott 948 North Watt Circle Deltona, Florida Howard Ehmer Nina Ehmer 32738-7919 1081 Anza Court Deltona, Florida 32738 Francell Frei 1080 Peak Circle Deltona, Florida 32738 Bernard T. Patterson Virginia T. Patterson 2518 Sheffield Drive Deltona, Florida 32738 Kealey A. West, Esquire St. Johns River Water Management District 4049 Reid Street Palatka, Florida 32177 J. Christy Wilson, Esquire Wilson, Garber & Small, P.A. 437 North Magnolia Avenue Orlando, Florida 32801 Gloria Benoit 1300 Tartan Avenue Deltona, Florida 32738 Gary Jensen 1298 Tartan Avenue Deltona, Florida 32738 James E. Peake Alicia M. Peake 2442 Weatherford Drive Deltona, Florida 32738 Steven L. Spratt 2492 Weatherford Drive Deltona, Florida 32738 Ted Sullivan 1489 Timbercrest Drive Deltona, Florida 32738 Kirby Green, Executive Director St. Johns River Water Management District 4049 Reid Street Palatka, Florida 32177
The Issue The ultimate issue is whether Celebrity Resorts, Inc., (Celebrity) is entitled to a Management and Storage of Surface Waters (MSSW) permit for a surface management system to serve its proposed development in Marion County, Florida.
Findings Of Fact PROPOSED PROJECT Celebrity is seeking a District MSSW permit to construct a surface water management system to serve a proposed recreation vehicle (RV) park. The facility is to be located in northern Marion County on the southern border of Orange Lake, an Outstanding Florida Water. The entire site is within the geographic boundaries of the District. The RV park is to be located on 75 acres of land, and is to contain 372 RV and "park model" sites, four bath houses, a clubhouse, and an expanded boathouse. There is a "break" in the watersheds of the Celebrity property caused by a ridge across the approximate center of the project site. The effect of this "break" is that approximately one-half of the property drains toward the lake while the approximate southerly half of the property drains into an independent depression creating a watershed separate from the lake. Parts of Marion County and Alachua county have been designated as Sensitive Karst Area Basin by the District. The project site is located in the designated area. The existing land use is open pasture. The property was previously used for citrus groves. STANDING Concerned Citizens of Orange Lake Area is an unincorporated group of approximately 76 individuals who want to prevent pollution of Orange Lake. Of the 76 members, three members were present and testified at the hearing. The members attending the hearing were an artist (Riley), a photographer (Suto), and a bass guide (Solomon). Ms. Suto testified that she lives about 1 to 1 1/2 miles from the site. Ms. Riley testified that she lives next door to Ms. Suto and determined that to be over two miles away from the site. Mr. Solomon testified that he lives on the southeast side of Orange Lake approximately 1 to 1 1/2 miles from the project site. No witness testified that any member has a property interest in the subject property. Of the members who testified, none use the subject property. There was no testimony that other members use the property. Twenty-six members wrote letters of concern to the District. Ms. Suto testified to the existence of high levels of lead in her well water. WATER QUANTITY The existing land use, pasture, was used to determine the pre- development peak rate and volume of discharge. The existing surface drainage of the 75-acre project site is divided into two basins. On the north side of the property, the surface water flows toward Orange Lake. This basin is designated on the plans, sheet 3 of 16, by a "2." The south portion of the property is contained within the landlocked drainage basin which is designated on the plans, sheet 3 of 16, by a "1." The post-development flow of surface water will be in the same direction as the pre-development flow. There are no proposed development plans or encroachments into the 100- year floodplain. Therefore, there is no increase in potential for damages to off-site property or persons caused by floodplain development or encroachment, retardance, acceleration, displacement, or diversion of surface waters. There is no reduction in natural storage areas and, in fact, the proposed project increases the natural storage on site. Drainage Basin 2 The District's criterion for systems discharging to basins with an outlet is that the post-development peak rate of discharge for the 25-year, 24- hour storm event shall not exceed the pre-development peak rate of discharge for the 25-year, 24-hour storm event. The District's criteria also require that the post-development volume of discharge not exceed the pre-development volume of discharge. The retention system which ultimately discharges to Orange Lake is designed to retain the entire 25-year, 24-hour storm event through the series of basins on site. The pre-development peak rate of discharge for the drainage basin which flows to the lake is 55 cubic feet per second (cfs) during the 25-year, 24-hour storm event. The post-development peak rate of discharge from drainage basin 2 is 4 cfs. The post-development peak rate of discharge is less than the pre- development peak rate of discharge. Runoff from each RV site will be collected in an individual, ten-inch- deep retention basin. Runoff from the road will be collected in roadside swales. Runoff from the clubhouse, country store, and associated parking lots will be conveyed to drainage retention area (DRA) No. 8. The individual retention basins have the capacity to retain the 25- year, 24-hour storm event without discharging. Any surface water discharges from the individual retention basins in Basins 2A, 2B, and 2C as designated on sheet 3 of 16 will flow to DRA Nos. 4, 5, and 7, respectively. In Basin 2D, runoff from the road and RV park model sites will flow to DRA No. 6. The discharge from DRA No. 6 in the 25-year, 24-hour storm will be zero (0) cfs. In larger storms, any discharge from DRA No. 6 will flow to DRA No. 7. In the event DRA No. 7 overflows, the runoff will flow to DRA No. 5. Basins 2G and 2F are located around two existing sinkholes which currently collect stormwater runoff. In the proposed project, Basins 2G and 2F continue to drain the same area as pre-development. However, additional impervious surfaces will be placed in the drainage area. For this reason, an additional three to five feet of clean fill will be placed in the bottom of each sinkhole for filtration purposes. Basins 2H and 2I are less than one acre and currently drain off site. Berms are proposed around the property line at the basin to keep the stormwater on site. Basins 2H and 2I retain 3/4 inch of runoff over the individual basin. The runoff from Basins 2E1 and 2E flows to DRA No. 8 via a drainage swale. DRA No. 8 will retain 3/4 inch of runoff from the drainage area and is an off-line retention basin. The DRA No. 8 is equipped with a diversion box which allows the 3/4 inch of runoff to enter the DRA and then diverts the runoff from larger storms around the DRA so that the treatment volume of runoff (3/4 inch) continues to be treated in DRA No. 8 and does not mix with and discharge from DRA No. 8 during larger storms. Drainage Basin 1 Drainage Basin 1 as designated on plan sheet 3 of 16 is a landlocked basin which does not discharge to Orange Lake. In Drainage Basin 1, as in Basin 2, the runoff from the RV sites flows to the individual retention basins which retain the 25-year, 96-hour storm event. The runoff from the road flows to swales. Overflow from the basins and swales flow to the DRAs. Drainage Basin 1 does not discharge during the 100- year, 24-hour or the 25-year, 24-hour storm event, pre-development or post- development Drainage Basin 1 is designed to retain the 100-year, 24-hour storm, which is an 11 inch storm event. Drainage Basin 1 is also designed to retain the 25-year, 96-hour storm event. The 25-year, 96-hour storm event is 143% of the 25-year, 24-hour storm event. WATER QUALITY Design Criteria The District's design criteria for water quality are set out in Section 40C-42.025, Florida Administrative Code. The District's retention criteria require that a proposed system have a treatment/pollution abatement volume of 1/2 inch of runoff from the site. For discharges to an OFW, the pollution abatement volume is increased by fifty percent. Therefore, the system must have the volume to retain 3/4 inch of runoff from the site. Each retention basin retains a minimum of 3/4 inch of runoff from the site. The District's criteria regarding quantity of water discharged require a larger volume of runoff to be retained than the District's criteria regarding quality. Therefore, the retention system exceeds the District's criteria regarding quality in order to meet the criteria regarding quantity. The District's retention criteria require that the basin recover the treatment volume within 72 hours. Most of the retention basins retain more than the required treatment volume of 3/4 inch, and most will also recover, or become dry, within 72 hours. The retention basins are capable of being effectively maintained in that the side slopes and bottom of the basins can easily accommodate mowing equipment. For erosion control, staked hay bales and silt screens will be utilized on site during construction to prevent the off-site transport of soil material. Following construction, the retention basins will be vegetated with sod to prevent erosion. The District's criteria require that facilities which receive stormwater runoff from areas with greater than fifty percent of impervious surface shall include a baffle or other device for preventing oil and grease from leaving the system. DRA Nos. 1, 4, 5, and 8 are equipped with an oil and grease removal device called a baffle. The baffle is an acceptable engineering design for the removal of oil and grease from stormwater in a retention basin. The facility operation is uncomplicated. If the individual basins did fill due to a storm event greater than the 25-year, 24-hour or the 25-year, 96- hour in the landlocked basin, they would simply overflow into a DRA. No structures are involved to prevent flooding in large storm events. Water Quality Impacts The individual retention basin at each RV site is considered off-line because it does not discharge in the 25-year, 24-hour storm event. DRA Nos. 1, 2, 3, 4, 5, 6, and 7 are considered off-line because they do not discharge during the design storm. DRA No. 8 is considered off-line because of the diversion box which provides for the retention of the treatment volume and diversion of the larger storms. Off-line retention systems generally show greater pollutant treatment efficiencies than other types of stormwater treatment. The first 1/2 inch of runoff or the "first flush" of rainfall contains ninety percent of the pollutants from the site. SURFACE WATER Utilizing information and methodologies generally accepted by experts in the field of water quality, the District analyzed and projected the average surface water and groundwater quality of the discharge from the surface water management system for the proposed project. No data on runoff concentrations currently exists for RV parks. This analysis was based on a review of existing data on untreated runoff concentrations from three multifamily developments and one highway study. Because data from studies of multifamily residential and highway projects was used, the District's estimates of the untreated runoff concentrations for this project are conservative in that the actual concentrations are probably less than estimated. The District's analysis of the average quality of the discharge from the proposed system was also based on projecting the treatment efficiencies associated with the system. This analysis was done by reviewing data from documented studies previously conducted to ascertain the treatment efficiency of retention methods of stormwater treatment. Generally, retention of the first 1/2 inch of runoff removes eighty percent of the pollutants. On this project, a treatment efficiency of ninety-five percent was assumed based on the fact that the system is off-line treatment and a minimum of 3/4 inch of runoff from the site will be retained in the basins prior to discharge. The expected average untreated runoff concentrations were then educed by the expected treatment efficiencies to project post-treatment water quality of the discharge from the proposed system. These numbers were then compared to Chapter 17-302, Florida Administrative Code, water quality standards for Class III water bodies, and ambient water quality in Orange Lake. Orange Lake is classified as an OFW. Therefore, the proposed project cannot be permitted if it will cause degradation of that water body. The background data or ambient water quality data for phosphorous and nitrogen was taken from the Orange Lake Biological Report by the Florida Game and Freshwater Fish Commission in 1986. The ambient water quality for the other parameters in Table 2 of District Exhibit 2 was computed using eight years of data from a District monitoring station on Orange Lake. The projected average concentration for each constituent in the discharge from the system is less than the ambient water quality of Orange Lake. Therefore, the proposed surface water discharge will not violate state water quality standards in waters of the state. The post-development pollutant loading rates should be equal to or better than the pollutant loading rates from the use of the property as citrus or pastureland because the runoff is being retained on site and treated before being discharged. GROUNDWATER Groundwater discharges were reviewed by assessing the type of soil below the retention basin and the distance to the water table. The soil on the site contains some organic matter which is beneficial for treatment purposes. Based on the borings submitted by Celebrity, the water table, if any, is five feet or more below the bottom of any proposed retention basin. Runoff in the basin will percolate through the soil. Nutrients such as nitrogen and phosphorus will be taken up by the vegetation in the bottom of the basins. Metals will bind to the soil material below the basin. Oils and greases will be broken down through microbial degradation into nontoxic material. Groundwater discharges from the proposed system will not violate any applicable state groundwater quality standards. These standards will be met within the first three feet below the treatment basins. The standards will also be met by the time the groundwater discharge moves to the edge of the zone of discharge which is at the property boundary. The discharge from the proposed Celebrity project will not cause or contribute to a violation of state water quality standards in the receiving waters. SINKHOLES Sinkholes may form on the site. Sinkholes that form will probably be "cover subsidence" sinkholes. Cover subsidence sinkholes are those in which a void below the surface fills with the soil from above, causing a depression in the ground surface. There are four relict sinkholes on site. They are cover subsidence sinkholes. The sinkhole nearest the lake has water in the bottom. Stormwater runoff is directed away from the sinkhole. Any water which enters the sinkhole from the land surface or above will enter from the sky. The District has proposed criteria for stormwater systems in designated Sensitive Karst Area Basins. Those criteria are that 1) the water in the basins shall be no deeper than ten feet deep; 2) there should be at least three feet of unconsolidated material between the bottom of the basin and the top of the water table; and 3) the basins should be fully vegetated. The District currently applies these criteria as policy. In this project, the basins are shallow, ranging from ten inches deep at the RV sites to 2 1/2 feet in the DRAs. The basins have at least three feet of unconsolidated material between the bottom of the basin and the top of the water table. In the soil borings performed by Celebrity, the water table was shown to exist between five and fifty feet below land surface. The proposed project design meets or exceeds the proposed criteria for Sensitive Karst Area Basins. The basins will be fully vegetated or sodded with grass. Lineations or lineaments are solution features which may indicate a fracture of the underlying limestone. There may be a lineament on the site. There are other sinkholes in the area. If a cover subsidence sinkhole develops in an individual retention basin or DRA, stormwater, if any, will seep or percolate through the several feet of soil prior to reaching an aquifer. Most of the pollutants in the retention basin will meet groundwater quality standards prior to percolation and further treatment in the soil. OPERATION AND MAINTENANCE Special conditions Nos. 13, 14, and 15 on the permit will require Celebrity to inspect the system monthly for sinkhole development. If a sinkhole develops, Celebrity must notify the District within 48 hours of its discovery. Celebrity must submit a detailed repair plan within 30 days for written approval by the District. Celebrity proposes to repair any sinkholes that develop by a District- approved method. Celebrity Resorts, Inc., is a legally established corporation registered in Delaware and owns the subject property. Celebrity does not intend to subdivide the property but to sell memberships to use the property on a time-share basis. Celebrity will administratively operate the site by employing a park manager who will remain on the property 24 hours a day. If any problems occur with the basins, either he or his designee will be on site to respond quickly to the situation. The park manager will have a full-time maintenance staff which will operate the park. Celebrity will financially operate and maintain the proposed system using funds currently raised and in the future by membership fees. Celebrity is a publicly held corporation. Funds raised from the sale of stock, approximately $3,500,000, have paid for legal and administrative fees as well as the land purchase. Approximately $400,000 has been reserved to operate the facility. It will cost approximately $15,000 per month to run the park. Memberships will be sold for $300 per year. Part of the membership fees will go toward the general maintenance of the site. Maintenance of the proposed system will include regular mowing and monthly inspection for sinkholes and repair if necessary. WETLANDS IMPACTS OF THE PROJECT The property contains waters of the state wetlands and isolated wetlands. The waters of the state wetlands are those along the shore of Orange Lake. One isolated wetland exists on site in the sinkhole which is closest to the lake. The sinkhole has standing water in which lemna, or duckweed, is growing. Duckweed is a listed plant species in Section 16.1.1(2) of the Handbook. No construction is proposed in either the waters of the state wetlands or the isolated wetland. The District criteria require the review of impacts to off-site aquatic and wetland dependent species relative to the functions currently provided by the wetlands to these types of fish and wildlife. Since there will be no construction in the wetlands, there will be no impacts to the habitat, abundance and diversity, or food sources of off-site aquatic and wetland dependent species from this proposed project. No threatened or endangered aquatic and wetland dependent species were observed on site. The proposed permit application will not adversely affect natural resources, fish, or wildlife in a manner which is inconsistent with the District criteria. The proposed permit application will not adversely affect hydrologically-related environmental functions in a manner which is inconsistent with the District criteria.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the petition filed by Concerned Citizens of Orange Lake Area be dismissed for lack of standing and that Celebrity Resorts, Inc., be issued a MSSW permit for its system as designed and proposed. DONE and ENTERED this 19th day of July, 1991, in Tallahassee, Florida. DIANE K. KIESLING Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 19th day of July, 1991. APPENDIX TO THE RECOMMENDED ORDER The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on the proposed findings of fact submitted by the parties in this case. Specific Rulings on Proposed Findings of Fact Submitted by Petitioner, Concerned Citizens of Orange Lake Area 1. Proposed findings of fact 1-6 are subordinate to the facts actually found in this Recommended Order. Specific Rulings on Proposed Findings of Fact Submitted by Respondent, Celebrity Resorts, Inc. 1. Proposed findings of fact 1-38 are subordinate to the facts actually found in this Recommended Order. Specific Rulings on Proposed Findings of Fact Submitted by Respondent, St. Johns River Water Management District 1. Each of the following proposed findings of fact is adopted in substance as modified in the Recommended Order. The number in parentheses is the Finding of Fact which so adopts the proposed finding of fact: 1&2(1); 3-7(4-7); 8-20(8- 20); 21(2); 22-31(21-30); 32(16); and 33-107(31-105). COPIES FURNISHED: Crawford Solomon Qualified Representative Concerned Citizens of Orange Lake Post Office Box 481 Citra, FL 32681 William L. Townsend, Jr. Attorney at Law Post Office Box 250 Palatka, FL 32178-0250 Nancy B. Barnard Attorney at Law St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429 Henry Dean, Executive Director St. Johns River Water Management District Post Office Box 1429 Palatka, FL 32178-1429
The Issue 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.
Findings Of Fact Respondent, International Paper Realty Corporation, ("IPR" hereafter) is the developer of a proposed residential development located In Panama City. As part of this development, IPR proposed to do some dredge and fill work on its property requiring a permit from the Department of Environmental Regulation ("DER hereafter). On November 5, 1976, IPR submitted an application for approval of a construction, dredge and fill permit to DER. On December 7, 1976 DER requested further information regarding (a) cross-sectional areas and volumes to be dredged; (b) details of Proposed drainage structures; and (c) data regarding the retention of runoff. On January 4, 1977 IPR submitted to DER the information requested by Its letter of December 7, 1976. On January 7, 1977 DER requested further information from IPR pertaining to the overall topography of the area and information pertaining to the dominant vegetation. On January 20th and January 24th, 1977 IPR submitted the information requested by DER on January 7, 1977. On February 9, 1977 DER requested from IPR further information regarding clarification of the computation of 1.6 inches of rainfall volume and a request regarding pollutional loads that could be discharged to the state waters of Robison Bayou or North Bay. On February 17, 1977 and on March 8, 1977 conferences were held by DER with IPR, and representatives from other affected state and local regulatory agencies to review the concern of DER relative to the original permit application. On April 29, 1977 IPR submitted to DER the first modification of its original application of November 1976 which incorporated all of the recommended changes suggested by the regulatory agencies at the conference meetings. Included with this submission were charts, figures and diagrams indicating the proposed work and a hydrological design report dealing with the overall project. On May 16, 1977 IPR met with DER to discuss In detail the permit application as modified on April 29, 1977. On May 18, 1977 DER requested further information from IPR regarding water quality background, a monitoring program, computation of the anticipated dredge material and clarification of slide slopes of the proposed lakes and pond construction. On May 23, 1977 IPR submitted to DER its response to the requested information of May 18, 1977. This response dealt with the anticipated volumes of excavation; anticipated water pollutant load; and the clarification regarding slide slopes of the ponds and lakes. On June 8, 1977 IPR received from DER a request for further information regarding the slide slopes, a recommended monitoring program and specific information regarding background water quality data. On July 5, 1977 IPR responded to DER's request of June 8, 1977 and submitted with that response the water quality data taken from locations in Robison Bayou and North Bay. On August 5 and August 31, 1977 conferences were held by DER with IPR, as well as other involved state and regulatory agencies, and as a result of this meeting it was determined that the permit application should be further modified. On September 14, 1977 IPR submitted to DER a second modification to the original application; and the application as modified, provided for dredging approximately 43,500 cubic yards in an area adjacent to North Hay and Robison Bayou, in order to create an approximately 6 acre residential lake connected via culverts to Robison Bayou and to deepen an existing lake and pond connecting to North Bay. All dredging would be to -3 feet mean sea level. Approximately 40 cubic yards would be dredged in North Bay to increase water circulation into the existing lake. Approximately 1000 cubic yards would be removed to deepen the existing 2 acre pond, with the remaining material removed from the two lakes. Drainage has been designed to maximize detention and thereby discourage direct discharge of stormwater runoff into these lakes. The existing lake will provide both freshwater and saltwater systems by means of a berm across the middle of the lake, with only the North portion open to North Bay via the existing pond. The project area, approximately 90 acres in size, will accommodate proposed construction of up to 534 dwellings, including streets, recreational facilities, and electrical, water and sewer systems. On September 20, 1977 DER requested that IPR publish the required public notice in the local newspaper in that the application was now deemed complete by DER. The application, as modified, was filed herein as Joint Exhibit 1. The testimony concerning the various requests for information from IPR by DER and the response by IPR to DER were submitted by DER's witness Jean Tolman and the exhibits of DER accepted into evidence in this proceeding. Chapter 403, Florida Statutes, and Chapter 17-4, Florida Administrative Code, promulgated thereunder, set forth the procedural requirements and standards applicable to a construction, dredge and fill permit. DER is charged with the responsibility of determining whether the applicant has provided reasonable assurance that the activity to be permitted will not violate the provisions of Chapter 403 or the rules promulgated thereunder. Upon making this determination DER issues the applicant a permit and, if applicable, issues a certification to the Corp. of Engineers pursuant to Public Law 92-500. As outlined above, extensive proceedings were held by DER which ultimately resulted in DER determining that IPR's application met the applicable environmental standards and a permit should issue. (DER's memorandum of January 30, 1978 filed herein and the testimony of Jean Tolman) . However, prior to the actual issuance of the permit, Petitioner, Joe Tannenhill, and petitioners Mark E. Jones and Charles E. Whitehead filed petitions to intervene herein. DER requested that a hearing officer from the Division of Administrative Hearings be assigned to conduct the necessary proceedings involving both petitions and a hearing officer was so assigned pursuant to Chapter 120.57(1), Florida Statutes. Petitioner Joe Tannenhill's petition alleged that the proposed DER action of issuing a permit to IPR would affect his personal property rights. Petitioners Mark E. Jones and Charles E. Whitehead filed petitions which alleged that IPR's application failed to comply with the requirements of Chapter 380 and Chapter 403, Florida Statutes, and certain noted provisions of Chapter 17-4 Florida Administrative Code. During a prehearing conference on February 10, 1978, IPR and DER moved to dismiss Tannenhill from the proceedings. Grounds offered in support of the motion were that his allegation that the permitted activity would affect his personal property rights did not involve an issue over which DER has jurisdiction and therefore if true would not be material to the issue of whether the permit should be issued to IPR by DER. These grounds were accepted and by oral order of February 10, 1978 Tannenhill was dismissed from the proceeding. Also during the same prehearing conference IPR and DER moved to strike all allegations in the petition filed by Mark E. Jones and Charles A. Whitehead pertaining to Chapter 380 of the Florida Statutes. Grounds offered in support of the motion were that the provisions of Chapter 380, Florida Statutes, had no application to and in no way pertained to a construction, dredge and fill permit filed with DER. These grounds were accepted and by oral order entered on February 10, 1978 the provisions of Chapter 380 were deemed immaterial to this proceeding and all allegations pertaining thereto were stricken from the pleading filed. Petitioners Mark E. Jones and Charles A. Whitehead presented their cases jointly at the final hearing. They called the following witnesses: James Walters (T16-36); Charles A. Whitehead (T37-43); Mark E. Jones (43-52); Miss Carol Daugherty (T52-74) Dr. John Taylor (T75-135); and Ed McKay (T135-140). Respondent DER called as its only witness Jean Tolman (T140-281). Respondent IPR did not present any witnesses. Mr. Walters presented a series of slides (Exhibits 1-12) of the subject property, adjacent property and adjoining water bodies. Mr. Whitehead testified that he owns his home adjoining Robison Bayou and that it was in his best interests to keep the quality of the water therein good. He specifically stated, however, that he had no knowledge as to how IPR's proposed project would affect the water quality of Robison Bayou. (P 41) Mr. Jones testified that he owns a home near Robison Bayou and that it was in his best interest to prevent the water therein from getting polluted. He did not testify that IPR's project would affect Robison Bayou but only if it did that it would affect his financial interest in his property. The testimony of Mr. Walters, Mr. Whitehead, and Mr. Jones did not relate in any probative way to the issue in this proceeding. Miss Carol Daugherty was qualified as an expert to make chemical analysis of water. She testified that Dr. Jack Taylor brought some water samples to her and she performed a chemical analysis of same. The results of her test (Exhibit 13) indicated that the water contained a high count of fecal coliform bacteria which indicated to her that improperly treated sewage was in the water. (T 67) She did not testify that IPR was responsible for the bacteria found in the water she analyzed or that the permit which is the subject of this proceeding would authorize an activity which would increase the bacteria in the waters involved. Simply put, Miss Daugherty's testimony proved, if anything, that on the day the samples were taken, improperly treated sewage had been discharged into the waters involved. As to the issue in this proceeding - whether DER has been reasonably assured the the activity to be permitted will not violate water quality standards - the testimony of Miss Daugherty has no probative value. Dr. Taylor was qualified as an expert in marine ecology. He testified that he obtained water samples at high and low tides from five locations In Robison Bayou on February 16. (P 84-85) To determine its water quality for that day he delivered the samples to Miss Daugherty (P 88). As a result of the testing done by Miss Daugherty, Dr. Taylor testified that he was concerned with the level of total nitrogen and phosphorus in the samples but admitted that DER has no prescribed limit for either. (T 89) He further stated that he was concerned with the fecal strep levels found in the samples tested by Miss Daugherty but admitted "there is no standard as yet established for fecal strep" (T 98). Based solely on samples taken on one day, Dr. Taylor testified that he believes that Robison Bayou is overautrified and contaminated with harmful bacteria. (P 99) It was his opinion that this condition of Robison Bayou was caused by improperly treated sewage being discharged therein from a trailer park and drainage from a hospital and an industrial park nearby. (T 114-115) He did not testify that IPR was in any way responsible for the condition of Robison Bayou as he found it on February 16, 1978. Although Dr. Taylor expressed concern respecting the runoff from IPR's proposed development, he admitted that any analysis of drainage from the development "would be a matter of conjecture." (T 101) He further admitted that IPR's method for treating stormwater runoff "probably addressed it in as good a way as you can." (P117) His only exception to this admission was that he would have planned the project to have all runoff going into North Bay rather than Robison Bayou. It is obvious from this statement that Dr. Taylor is not concerned with the quality of the waters that might runoff the proposed project into waters of the state but is really only concerned with the existing quality of the body of water to receive the runoff, Robison Bayou. The testimony of Dr. Taylor might have some value in an enforcement proceeding involving parties who are in fact degrading Robison Bayou. Here, however, the issue is whether DER has been provided reasonable assurance that the activity to be permitted will not violate water quality standards. As to this Issue, Dr. Taylor's testimony has no probative value. DER is charged with the responsibility of evaluating the impact of a proposed construction, dredge and fill permit on waters of the State. Section 403.021(2), Florida Statutes. The major considerations in this evaluation are whether the quality of water will be degraded by (1) the destruction of resources which maintain water quality, and (2) the discharging of harmful materials into the environment. No testimony was offered by Petitioners that the activity of IPR proposed to be permitted by DER would destroy resources which maintain water quality or that the runoff from the project will discharge harmful materials into the waters of the State. Petitioners appeared to support its position in this proceeding solely on the basis of the water quality of Robison Bayou. However, the standards to be applied to IPR's permit do not concern themselves with the water quality of Robison Bayou but apply only to the quality of the water to be discharged to Robison Bayou. The testimony of DER's witness, Jean Tolman, was uncontradicted that IPR's application, as modified, affirmatively provided reasonable assurance to DER that the short-term and long-term effects of the permitted activity will not violate water quality standards of the State. Ms. Tolman is presently head of DER's program on water resource restoration and preservation. Prior to that, however, she was head of the standard permitting section involving dredge and fill permitting for DER and testified that she personally reviewed the application in question in that capacity. Ms. Tolman was accepted as an expert qualified to answer the questions and express the opinions which were propounded to her and expressed by her. She testified in great detail concerning the original application on November 5, 1976; the many requests by DER for additional information and the submission of same by IPR; the many meetings with the applicant, DER and other affected state and federal agencies; and the modifications to the original application submitted on April 29, 1977, and September 14, 1977. Her uncontradicted testimony was that the application, subsequent submittals and subsequent modifications were adequate and complete to form the basis for a determination by DER. Based on all of this information, and the expertise of DER, Ms. Tolman testified that the application as revised would in fact meet the water quality standards pertaining thereto. She did state that DER would require as a condition to issuance of the permit that IPR submit a detailed drainage plan prior to actual construction.
Conclusions IPR's application for a construction, dredge and fill permit originally submitted to DER on November 5, 1976, and subsequently modified on April 29, 1977, and September 4, 1977, was an adequate and complete application sufficient to form the basis for a determination by DER on whether or not the permit should issue. Testimony presented at the hearing by the witnesses for Petitioners related primarily to the water quality of Robison Bayou on February 16, 1978. Admittedly on the day in question the level of fecal coliform bacteria found in the waters of Robison Bayou exceeded that established by DFR for Class II waters. However, no testimony presented at the hearing indicated that Respondent IPR was responsible for this fact nor did any testimony presented at this hearing Indicate that the activity to be permitted will increase the focal coliform bacteria level in Robison Bayou. There was no testimony presented at the hearing to indicate that the dredge and fill activity proposed would in fact violate the water quality standards established by Chapter 403, Florida Statutes, or the rules promulgated by DER thereunder. Although is is clear that there will be some stormwater runoff from IPR's proposed residential development once constructed, there was no testimony offered to indicate that this stormwater runoff would violate the water quality standards of Chapter 403 or the rules promulgated by DER thereunder. There was testimony offered by Ms. Tolman that it was her personal opinion and the determination by DER that in fact the stormwater runoff would not violate the water quality standards.
The Issue The issues presented in this matter concern the request by the Petitioner to be granted a management and storage of surface waters permit by Respondent. Respondent proposes to deny the permit based upon the perception that the activities contemplated by Petitioner: (1) are not consistent with the public interest as envisioned by Section 373.016, Florida Statutes, and 40C- 4.301(1)(b), Florida Administrative Code, (2) are not a reasonable and beneficial activity, per Section 40C-4.301(1)(a), Florida Administrative Code, alter the peak discharge rate of runoff from the proposed activity or the downstream peak stage or duration for the 1 in 10 year design storm, per Section 40C-4.301(3)(a), Florida Administrative Code, (4) cause an increase in velocity or flood stage on lands other than those owned, leased, or otherwise controlled by the applicant for the design storm, per Section 40C-4.301(3)(b), Florida Administrative Code, (5) cause an increase in flow or stage such that it would adversely affect lands other than those owned, leased, or otherwise controlled by the applicant, per Section 40C-4.301(3)(c), Florida Administrative Code. 1/
Findings Of Fact A predecessor applicant had requested permission to construct and operate the water management system which is the subject of this controversy. The approximate acreage involved was 197 acres in Lake County, Florida. This acreage and requested activity was subject to the regulatory requirements of St. Johns River Water Management District. Clay Island Farms, Inc., hereinafter referred to as CIF, was substituted for the initial applicant and this matter has been litigated before the Division of Administrative Hearings on the continuing application of the Petitioner. The permit application number is 4- 8089. This application was considered with application number 4-8088, pertaining to property owned by A. Duda and Sons, Inc. Subsequently, the latter application shall be referred to as the Duda request for permit. Certain additional information was sought by Respondent from the applicants, CIF and Duda, in the permit review, by correspondence dated October 2, 1981. A copy of that correspondence may be found as Petitioner's Exhibit No. 16 admitted into evidence. In particular, CIF was requested to prepare pre and post-development runoff rates in the 1 in 10, 1 in 25,and 1 in 100-year storms, to include stage-storage and stage-discharge rates for any and all retention facilities within the project design. Petitioner's Composite Exhibit No. 1 admitted into evidence contains a copy of the engineering report by CIF which are CIF's responses to the request for information. The date of the engineering report is July 12, 1982. The CIF application, as originally envisioned, called for the construction of exterior and interior ditches to be placed around a dike of 71 feet MSL elevation. The dike would enclose a proposed farm operation of approximately 197 acres, should the permit be granted. Within that 197 acre plot, would be found numerous drainage ditches to include major ditches and minor arterial ditches. The purpose of those ditches found in the 197 acres would be to serve as a conveyance for rainfall runoff. The system of conveyance would be connected to an existing conveyance system already in place and related to farm operations of A. Duda and Sons. The runoff would be eventually placed in a retention pond and at times discharged from that retention pond or basin into Lake Apopka by means of gravity flow. The particulars of the development of the 197 acre plot and its service dike, canals, and ditches are more completely described in Petitioner's Exhibit No. 1, which is the engineering report for the surface water management permit application. The CIF application was reviewed by the staff of the Respondent. Recommendation was made to deny the permit. Details of that denial may be found in Respondent's Exhibit No. 1. In the face of the denial, CIF requested an administrative hearing. This request was made on August 27, 1982, by petition for formal Subsection 120.57(1), Florida Statutes, hearing to determine Petitioner's entitlement to the requested permit. St. Johns River Water Management District, in the person of its governing board, determined to refer this matter to the Division of Administrative Hearings to conduct the formal proceeding and the request for the assignment of a hearing officer was received by the Division on September 13, 1982, leading to the final hearing in this cause. During the course of the final hearing, the CIF permit application was modified in a fashion which reduced the amount of acreage sought for cultivation. Now, approximately 122 acres would be farmed per the amended proposal. A general depiction of the design of the project in its amended form may be found in the engineer's sheet, which is Petitioner's Exhibit No. 20 admitted into evidence. When contrasted with the engineering drawings set out in Petitioner's Composite Exhibit No. 1, the new design is essentially the same as contemplated in the original permit application, on a lesser scale. Other than dimensions, the basic concepts of the CIF operation would remain the same under the amended proposal. At present, Petitioner proposes to remove the vegetation which covers the subject 122 acre plot and to conduct a muck farming operation. That vegetation is mostly mixed hardwood with the primary species being red maple. The soil in this area is constituted of monteverde muck, which is conducive to the production of corn and carrots, the crops which Petitioner would plant, to prepare the land for the operation, the system of ditches dikes and canals described would be installed following the cleaning, draining, and leveling of the 122 acres. Petitioner's Exhibit No. 10 admitted into evidence depicts land which has been cultivated and the subject 122 acres in its undisturbed state. Petitioner's Exhibit No. 4 admitted into evidence shows the overall CIF area is outlined in red, except for its southerly extent, which carries a red and yellow line on the exhibit. This exhibit depicts Wolfshead Lake which is a small interior lake in the southeastern corner of the overall CIF property. The yellow line in the middle of the CIF property represents, the location of a former north-south canal. The westernmost north-south reach, which is shown with a red line, depicts a canal which runs north from Wolfshead Lake into the existing Duda system of canals and ditches. The Duda operation has attempted to plug that north-south canal on the western fringe to stop the flow from the area of Wolfshead Lake, but has been unsuccessful and the water still enters the Duda farm ditches and canals. In the 1940's and early 1950's, the CIF property had been partially developed for a cattle operation and truck farming. Those canals, as described before, were installed, together with the diagonal yellow line on Petitioner's Exhibit 4, which represents a canal that was built with an axis running northeast and southwest. In addition, there was a centrally placed east-west canal and a slough running from Wolfshead Lake in a southeasterly direction. The slough is still there, although water that might be diverted from the Wolfshead Lake area into the slough is flowing north in the westerly north-south canal at present. If the project were allowed, most of the water flowing in and around the Wolfshead Lake would be introduced into the slough and from there exit to Lake Apopka. The center north-south canal and the interior east-west canal, together with the diagonal canal, are not in operation at present. The center north-south-canal would become the approximate eastern boundary of the 122 acres with the western north-south canal representing the approximate western boundary of the 122 acre plot. The northern boundary of the CIF property is constituted of an east-west canal which is part of the present Duda system. This is the only one of the canals associated with the former farming operation on the CIF property which is part of any maintained system of conveyances presently in existence. Approximately 1,000 acres are being farmed by Duda and Sons in property north of the proposed project. The Duda permit application, 4-8088 as granted, is described in Petitioner's Exhibit No. 13 which is a copy of the permit. This acreage is generally found to the northwest of the CIF plot, and would allow an additional 300 acres to be farmed in that muck area, on land which has been cleared for the most part and/or which has an elevation predominantly above 68.5 feet MSL. Eighty acres of the proposed Duda permit application was denied based upon the fact that it had not been cleared prior to the Duda permit application and in consideration of the amount of the 80 acre segment which lies below 68.5 feet MSL. The elevation 68.5 feet MSL represents the flood plain for the 1 in 10 year rainfall event for Lake Apopka. The area of the Duda permit is depicted on Petitioner's Exhibit No. 4 and outlined on that exhibit with lines of green and yellow at the southern end, green and yellow and red and yellow on its western flanks, red at the north end and by red on the east side, together with a Duda drainage ditch, which runs north from the terminus of the north-south drainage ditch coming from Wolfshead Lake and the east-west drainage ditch at the northern extent of the CIF property. Exhibit No. 4 was made prior to clearing operations depicted in Petitioner's Exhibit No. 10 and that letter exhibit is a more correct indication of the appearance of the new Duda permit property today. A green diagonal line running northwest and southeast intersecting with a line running east-west and a line running north-south depicts the approximate part of the 80 acres, which lies below 68.5 feet MSL, as shown in Petitioner's Exhibit No. 4. Farm operations, in keeping with the authority of Permit No. 4-8088, have not commenced. If the CIF permit application is successful, the original 1,000 acres, approximately 300 acre area of the Duda permit and the 122 acres of CIF, would be tied in by a system of conveyance ditches or canals allowing the interchange and transport of water through and around the three farm areas. The existing retention pond would be expanded to accommodate the additional farm acreage. The Petitioner is willing to increase the present retention pond to a design capacity which would equal one acre of basin for each ten acres of farm land, at the place in time when all three elements of the muck farm operation were under way. This again pertains to the existing 1,000 acres, the approximately 300 acre recent Duda permit, and the 122 acres related to the CIF application. With the addition of the CIF acreage, when water in the ditches reached 67.1 feet MSL, this would cause the engagement of a 40,000 GPM pump allowing the ditch water influent into the retention pond. The pump automatically would shut off at any time the water level in the access ditches to the pond dropped below 61 feet MSL. The primary purpose of the retention pond is to make water available for irrigation of crops, in its present state, and as contemplated with the addition of the CIF project. The pond does and would detain farm water for a period of about a day allowing the settling out of certain nutrients which are in particulate form. The existing pond and in its expanded form does not and would not filter nutrients which have been dissolved and have become a part of the water column. At times of high incidence of rainfall, when the crops are inundated with water for a 48-hour period of time, the retention pond is now designed and as contemplated by the addition of the CIF farm land, would allow for the discharge of effluent into Lake Apopka through two discharge culverts. The discharge is by means of gravity through an adjustable riser system. The retention pond as presently designed and as contemplated in its expansion has established the height at which water would be released from the retention pond into Lake Apopka through the riser at 68 feet MSL. The occasion of high incidence of rainfall occurs during the normal rainy season in a given year. Discharge could also be expected in the 1 in 10 year, 24hour storm event. During that storm event or design, Lake Apopka would rise to a level of 68.54 feet MSL, a level which would correspond to the 10year flood plain. Whether in the pre or post-development phase of the 122 acres, waters from that acreage would be discharged during the course of the storm through culverts leading from the retention pond into Lake Apopka. This process would continue until the gravity flow stopped at the moment where the water level in the pond and the water level in Lake Apopka adjacent to the discharge culverts achieved equilibrium of elevation. At that point in time, the gravity flow or discharge from the retention basin would cease, there no longer being a positive gradient from the detention pond to Lake Apopka. There will be some amount of discharge in the 24-hour storm event through the culverts at the retention pond either in the pre or post-development phases of the project, because, at present, the western most north-south ditch, which is found at the western boundary of the CIF property, allows water to flow north into the present Duda ditch system, water which has fallen on the 122 acres in question. From the ditch system, that water finds its way into the retention pond and thus into the lake. The contemplated system to be installed with the 122 acres at build-out would also allow water from the 122 acres to go through a system of conveyances and to the retention pond and from there into Lake Apopka. Although considerable testimony was presented by both parties on the subject of comparing pre-development and post-development peak discharge rates of runoff from the proposed activity, in the 1 in 10 year, 24-hour storm design or event, neither party has satisfactorily proven the dimensions of the pre-development and post-development peak discharge rates of runoff from the proposed activity. This determination is made having reviewed the testimony and the exhibits in support of that testimony. Notwithstanding a lack of proof of this differential with exactitude, it has been shown by the testimony and exhibits that the post- development peak discharge rate of runoff in the 1 in 10 year, 24-hour design storm or event can be expected to exceed that of the pre-development rate. On the associated topic of the ability of the post-development design to accommodate the differential in peak discharge rate of runoff between pre- development and post-development, Petitioner has failed to establish this proof. The modeling that was done by the Petitioner, in an effort to depict the differential as 10 acre feet with an available capacity of attenuation approximating 26 acre feet within the system of ditches, is not convincing. Nor has petitioner shown that there is sufficient storage in the retention pond, in the course of the storm event. The data offered in support of Petitioner's position does not sufficiently address accommodation of the drainage from areas surrounding the 122 acres in question, which are not part of the Duda system; the amounts of water already found in the system of ditches and canals at the onset of the storm event; the amount of water located on the crops at the onset of the storm event, which would have to be removed; and the amount of water already found in the retention pond at the time of the storm event. During the 1 in 10 year 24-hour storm, the CIF 122 acres will be protected by the 71-foot MSL dike, in that the expected elevation of Lake Apopka would not exceed 68.54 feet MSL. The dike would also protect the 122 acres in the 25, 50, and 100-year, 24-hour storm events whose elevations are anticipated to be 68.98, 69.28, and 69.56 feet MSL, respectively. As a consequence, an increase in flood stage would occur on lands other than those controlled by CIF. The amount of increase in flood stage would be approximately .046 inches during the 1 in 10 year storm, and an increasingly greater amount for the larger storms. It was not established where the amount of water which could not be staged on the 122 acres would be brought to bear through the surface flow on the 31,000 acres of water which constitute Lake Apopka. Nonetheless, that water could be expected to increase the flood stage on lands other than those of the Applicant. Possibly the dikes protecting the muck farms on the northern side of Lake Apopka could be influenced by the .046 inches in elevation due to the forces associated with the 1 in 10 year storm event, such as winds and movement of the water in the lake. This is true, notwithstanding the fact that the design goal of the dikes in the area is 71 feet MSL. The dikes are constituted of muck and are susceptible to overtopping, erosion, or blowout. By history, there have bean dike failures in the northern end of Lake Apopka, and associated increases in stage or flood stage. This incremental increase in water level in the 1 in 10 year storm event, due to the CIF development, when considered in the context with the other influences of that storm event, could possibly be the determining incident leading to dike failure in the northern perimeter of Lake Apopka. However, given the history of dike failures, prior to this potential loss of the storage area on the applicant's property, it has not been shown that the proximate cause of dike failure in the 1 in 10 year storm could be expected to be the contribution of an additional .046 inches of water on the lake surface. Those failures existed prior to the potential for the addition of water and were the result of inadequate maintenance of a structure which demanded a better quality of attention. Nonetheless, the additional amount of water could be expected to exacerbate the extent of a dike breach in any 1 in 10 year storm event that occurred subsequent to the development of the CIF 122 acres. In summary, the likelihood that the increase in elevation of water caused by the loss of storage on the subject property will be the critical event that causes a dike failure is not accepted. A dike could breach because of the influence of the storm even itself, without regard for the incremental increases in water elevation due to loss of water storage on the CIF property. The poor condition of some dikes due to less than adequate design or maintenance, would promote that dike failure and be exacerbated to the extent of more water being introduced on that property through the incremental amount of increase due to loss of storage on the CIF property. The dike failure circumstance in and of itself would not be sufficient to deny the permit application; however, the applicant had the burden of addressing the possible problem of increases in stage or flood stage on other properties, not its own, which are not protected by dikes. This showing was not made by the applicant, notwithstanding the fact that an increase in stage or flood stage could be expected to occur on property fronting Lake Apopka, which property is not protected by any form of artificial barrier. The installation of the protective dike aground the 122 areas of the CIF property in the 1 in 10 year design storm and potentially at times of lesser rainfall events, could be expected to increase the stage or flood stage on lands unprotected by dikes and thereby adversely affect lands other than those controlled by the applicant. Most of the 122 acres and the property to the east of that development and a portion of the undeveloped 80 acres in the recent Duda permit would be inundated in the 1 in 10 year storm event, prior to development. This is true because the elevation of much of that property is approximately 67.5 foot MSL. During the 1 in 10 year storm event, it would store approximately one foot of water, as presently constituted. It could also be expected to be inundated on an average of approximately once in two years. Lake Apopka is a part of a controlled system of lakes known as the Oklawaha River chain of lakes. Respondent regulates the water level in that chain of lakes by operation of a lock on the Apopka-Beauclair canal. The maximum desirable elevation of 67.5 feet MSL for Lake Apopka is a part of the regulation schedule found in Respondent's Exhibit No. 2 admitted into evidence. In the 1 in 10 year or better storm event, the Apopka-Beauclair system could not draw down the surface water at a rate faster than 27 days per foot, even assuming the lock was fully open to flow. Consequently, those properties that were suffering an, increase in flood stage on their surface could not expect to gain prompt relief through the regulation of waters in the Oklawaha River chain of lakes. Lake Apopka is an hyper-eutrophic lake. Although it is classified as Class III water body (ambient water quality) within the meaning of Section 17- 3.161, Florida Administrative Code, it fails to match that classification in terms of its actual water quality. This is as a consequence of its highly eutrophic state, brought about by the age of the lake and the contributions of man. Some of the contributors to the eutrophication have been removed from the lake area and water quality has improved. Those facilities removed were sewage treatment and citrus processing plants around the Lake Apopka rim. The muck farms remain and the quality of the water in the retention basins or ponds when compared to the receiving waters of Lake Apopka is similar in nature. Consequently, the receiving waters are not enhanced in their water quality when the retention ponds discharge water into Lake Apopka. As stated before, the retention ponds do not have as their primary purpose the treatment of water. Any water quality improvement is a secondary function of the retention pond. The retention ponds do improve the water somewhat, as described, and are adequately sized to fulfill that partial cleansing. Whether the water quality in Lake Apopka would ever improve sufficiently to allow Lake Apopka to become a more diversified habitat for fish and wildlife is not certain, even if all contributing discharges of pollutants were curtailed, to include the discharge of water from the muck farms with its high nutrient loads. Nonetheless, Lake Apopka cannot accomplish the recovery if the effluent from the muck farms continues to be introduced into the lake with the present constituents found in the water. Out of concern for the water quality in Lake Apopka, officials of the University of Florida have conducted experiments on nutrient removal which they hoped would approximate the quality of removal accomplished by transitional vegetation and swamp. (The 122 acres at issue and the western and eastern adjoining property are constituted of these water treatment zones.) This experiment of nutrient removal through use of retention ponds calls for the retention of the muck farm water for a period of six days allowing settlement of particulates and for the vegetation within those experimental retention basins to uptake dissolved nutrients. Several types of vegetation are used to gain a better quality of nutrient uptake add the vegetation is harvested every six to eight weeks to improve that performance. The experiment has shown that the quality of water discharged from the ponds utilized by the University of Florida was comparable in its quality to the natural wetlands system water discharge. The natural wetlands discharge is of a better quality than the receiving waters. Unlike the university experiment, the pond contemplated by CIF primarily emphasizes detention for a shorter period of time than was used in the experiment and allows highly eutrophic water to be mixed with that quality of water already found in Lake Apopka. The only exception to that comment is that water flowing from Wolfshead Lake, which is south of the proposed 122 acres, is a high quality of water, and through the project as contemplated, this water would be directly introduced into Lake Apopka through a flow over a natural wetlands system. This is in opposition to the present situation where the water from Wolfshead Lake flows primarily to the north through an existing canal and is mixed with water from the muck farm and is, therefore, of the eutrophic character as opposed to the high quality character. The Duda permit, which was issued, would allow the introduction of water which is similar in character to the water of Lake Apopka, through the system of ditch conveyances, placement in the retention pond, and at times, flow to the lake. In its effect, the nutrient loading which occurs by introduction of waters from that new farm, would be similar to that proposed in the CIF project. The fact of this similarity does not prohibit the district from evaluating water quality matters on the occasion of the CIF permit decision. Should the 122 acres be converted from natural vegetation to a muck farm, wildlife and fish habitat would be adversely impacted. The habitat provided by the plot is in scarce supply and is essential to the maintenance of a diversified fish population. The hardwood swamp, which is part of and adjacent to the 122 acres of the CIF application, supports benthic invertebrates, which are a food source for game fish. The type of vegetation found in the lake, due to its eutrophic state, is plankton and one of the by- products of the reproduction of that plant through the process and respiration is the destruction of the fish population. This occurs in the summer months. The plankton has replaced the emergent and submergent vegetation which once covered as much as two-thirds of Lake Apopka and now represents .05 percent of the lake. As a consequence, game fish have diminished over a period of years with plankton feeding fish predominating. Consequently, the fish population is less diverse and the removal of the vegetation becomes a significant contributor to the imbalance in fish population.
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.
The Issue The issues in this case are set out in the Petition to Determine Invalidity of Agency Rules and Agency Statement filed by A. Duda and Sons, Inc. (Duda): Count I, whether the St. Johns River Water Management District (SJRWMD) has an invalid and unadopted strategy to use various means to negate the agricultural exemption set out in Section 373.406(2), Florida Statutes; Count II, whether Section 3.4.1(b) of SJRWMD's Applicant's Handbook: Management and Storage of Surface Waters (the Handbook), which is incorporated by reference in Florida Administrative Code Rule 40C-4.091, is invalid essentially because it conflicts with the agricultural exemption set out in Section 373.406(2), Florida Statutes, and is vague; Count III, whether Rule 40C-4.041 is invalid essentially because it conflicts with the agricultural exemption set out in Section 373.406(2), Florida Statutes, and is vague; Count IV, whether certain documents--namely, all or part of The Manual of Reference Management Practices for Agricultural Activity (November 1978) (the Manual), excerpts from the Journals of the Florida House of Representatives and Senate (1984), and parts of the Model Water Code Commentary (Univ. of Florida 1972)(the Code Commentary), all of which are referred to in Section 3.4.1 of the Handbook but not filed with the Secretary of State--are invalid because they were not properly incorporated by reference under Rule 1S-1.005(2), because they conflict with the agricultural exemption set out in Section 373.406(2), Florida Statutes, and because they are vague; and Count V, whether Rule 40C-44.041 is invalid because it conflicts with the agricultural exemption set out in Section 373.406(2), Florida Statutes, and is vague.
Findings Of Fact Duda clearly has standing since it is challenging the validity of SJRWMD rules and alleged rules that pertain to an enforcement action SJRWMD is bringing against Duda. As reflected in the Statement of the Issues, Section 373.406(2), Florida Statutes, is at the heart of most of the issues in this case. It states: Nothing herein, or in any rule, regulation, or order adopted pursuant hereto, shall be construed to affect the right of any person engaged in the occupation of agriculture, silviculture, floriculture, or horticulture to alter the topography of any tract of land for purposes consistent with the practice of such occupation. However, such alteration may not be for the sole or predominant purpose of impounding or obstructing surface waters. Section 3.4.1(b) of SJRWMD's Handbook states, in pertinent part, how SJRWMD interprets the exemption set out in Section 373.406(2), Florida Statutes: In determining whether an exemption is available to a person engaged in the occupation of agriculture, silviculture, floriculture or horticulture, the following questions much be addressed: Is the proposed topographic alteration consistent with the practice of agriculture, silviculture, floriculture, or horticulture? Is the proposed topographic alteration for the sole or predominant purpose of impounding or obstructing surface waters? If the first question is answered affirmatively and the second is answered negatively, an exemption under subsection 373.406(2), F.S., is available. The exemption is construed as set forth in the Conference Committee Report on CS/CS/HB 1187, Journal of the House of Representatives, May 29, 1984, page 734 and Journal of the Senate, May 28, 1984, page 475. The District presumes that the following activities are consistent with the practice of silviculture when they are undertaken to place property into silvicultural use or to perpetuate the maintenance of property in silvicultural use. The following activities are also presumed not to be for the sole or predominant purpose of impounding or obstructing surface waters: normal site preparation for planting of the tree crop; planting; and harvesting. If any activity is undertaken to place the property into a use other than silviculture (for example: harvesting which is designed to clear property in preparation for commercial, industrial or residential development rather than regeneration) the activity is not considered to be consistent with the practice of silviculture and will be subject to the permitting jurisdiction of the District. Examples of activities which are considered to be for the sole or predominant purpose of impounding or obstructing surface waters because they have the effect of more than incidentally trapping, obstructing or diverting surface water are activities which create canals, ditches, culverts, impoundments or fill roads. In determining consistency with the practice of agriculture occupations, the District will refer to the following publication: "A Manual of Reference Management Practices for Agricultural Activities (November, 1978)[.]" The following practices described in the manual are considered as having impoundment or obstruction of surface waters as a primary purpose: Diversion, when such practice would cause diverted water to flow directly onto the property of another landowner Floodwater Retarding Structure Irrigation Pit or Regulating Reservoir Pond Structure for Water Control Regulating Water in Drainage Systems Pumping Plant for Water Control, when used for controlling water levels on land Other practices which are described in the manual and which are constructed and operated in compliance with Soil Conservation Service standards and approved by the local Soil and Water Conservation District are presumed to be consistent with agricultural activities. Practices which are not described in the manual are presumed to be inconsistent with the practice of agriculture and a permit is required for the construction, alteration, operation, maintenance, removal, or abandonment of a system, subject to the thresholds. See Appendix H for a complete listing of agricultural practices described in the manual. A copy of the manual may be obtained by contacting the District headquarters. Appendix H to the Handbook sets out brief descriptions of listed soil conservation practices for agriculture and states that those practices are described in detail in the Soil Conservation Service's Field Office Technical Guides; it also sets out several other recognized Best Management Practices (BMPs) for agriculture. Appendix H of the Handbook is a verbatim reproduction of the part of the Manual from which it is taken. While Section 3.4.1(b) of the Handbook advises that a copy of the entire Manual may be obtained from SJRWMD, it only incorporates the parts set out verbatim in it and Appendix H. The conference committee reports referred to in Section 3.4.1(b) of the Handbook recommended enactment of the Warren S. Henderson Wetlands Protection Act of 1984 (the Henderson Act), were voted on, and were approved by the House of Representatives and the Senate. Both reports stated in pertinent part: The language contained in s. 403.913, relating to agricultural activities, shall be construed in conjunction with s. 373.406(2) to exempt from permitting only those activities defined as "agricultural activities" pursuant to this act in accordance with the Commentary to s. 4.02.(2) of the Model Water Code. Section 403.913[now 403.927](4)(a), Florida Statutes, stated: "Agricultural activities" includes all necessary farming and forestry operations which are normal and customary for the area, such as site preparation, clearing, fencing, contouring to prevent soil erosion, soil preparation, plowing, planting, harvesting, construction of access roads, and placement of bridges and culverts, provided such operations do not impede or divert the flow of surface waters. The Commentary to Section 4.02.(2) states in pertinent part: The intent of this subsection is to allow persons engaged in agricultural, floricultural, and horticultural operations to engage in ordinary farming and gardening without obtaining a construction permit under §4.04. Theoretically, such operations may incidentally trap or divert some surface water. For example, by plowing a pasture a farmer is trapping and diverting surface water that would have constituted part of the runoff and eventually would have become part of the surface water of the state. Without this exemption the farmer would have theoretically been required to obtain a permit under §4.04. In addition, it would appear that all changes of topography which would alter natural runoff, such as contour plowing, would also require a construction permit under §4.04. The quantity of the water being diverted and trapped is so small that it would serve no practical purpose to require a permit for such work. In addition, the administrative burden of regulating such operations would be enormous. Rule 40C-4.041 provides in pertinent part: Unless expressly exempt, an individual or general environmental resource permit must be obtained from the District under Chapter 40C-4, 40C-40, 40C-42, 40C-44 or 40C-400, F.A.C., prior to the construction, alteration, operation, maintenance, abandonment or removal of any stormwater management system, dam, impoundment, reservoir, appurtenant work or works, including dredging or filling, and for the maintenance and operation of existing agricultural surface water management systems or the construction of new agricultural surface water management systems. Rule 40C-44.041 provides in pertinent part: Unless expressly exempt by Section 373.406, F.S., or Rule 40C-4.051 or 40C- 44.051, F.A.C., a permit is required under this chapter for the maintenance and operation of existing agricultural surface water management systems which serve an agricultural operation as described in paragraph (a) or (b) below. Other than the argument that certain agency statements are unadopted statements defined as rules, Duda's primary argument is that Section 373.406(2), Florida Statutes, is unambiguous and that SJRWMD's interpretation of it, as reflected in its rules and statements, is contrary to the plain meaning of the unambiguous statutory language. Specifically, Duda focuses on SJRWMD's interpretation of the language "for purposes consistent with the practice of such occupation" and "not for the sole or predominant purpose of . . . obstructing surface waters." But it is concluded that SJRWMD's interpretation of the statutory language is as or more reasonable than Duda's. Section 3.4.1(b) of SJRWMD's Handbook describes seven activities that are not "consistent with the practice of [the listed occupations]," including just one that may be disputed by Duda--namely: "Diversion, when such practice would cause diverted water to flow directly onto the property of another landowner." Since Duda's activities that are subject to SJRWMD's enforcement actions do not "cause diverted water to flow directly onto the property of another landowner," Duda's challenge did not focus on that part of Section 3.4.1(b) of the Handbook but rather on diversions of water that do not "cause diverted water to flow directly onto the property of another landowner." But to the extent that Duda was attacking this part of SJRWMD's interpretation, the evidence presented by Duda did not prove that diversion of water to flow directly on the property of another landowner is consistent with the practice of the listed occupations. The Handbook also describes, through Appendix H, activities "presumed to be consistent with agricultural activities." Duda has no dispute with activities described in Appendix but disputes the Handbook's statement that all other activities are "presumed to be inconsistent with the practice of agriculture." But the presumption is rebuttable, and the impact of the statements in the Handbook is to simply require proof of entitlement to the agricultural exemption for activities not listed in Appendix H in proceedings under Sections 120.569 and 120.57, Florida Statutes. Duda also argues that, by its plain meaning, the word "purpose" as used in Section 373.406(2), Florida Statutes, means the actor's subjective intent, not the action's objective effect --in this case, namely, the more-than-incidental trapping or diversion of water to create canals, ditches, culverts, or fill roads. To the contrary, one of the several accepted meanings of the word "purpose" is: "1a : . . . an object or end to be attained : INTENTION b : RESOLUTION, DETERMINATION 2 : a subject under discussion or an action in course of execution." See Merriam Webster's Collegiate Dictionary 1011 (11th ed. 2005). That dictionary also identifies intention as a synonym of the first sense given for purpose and lists design and end among the additional synonyms in the synonymy paragraph after the entry for intention. See id. at 651. For a list of synonyms of the second main meaning of purpose listed in the dictionary ("an action in the course of execution"), one may turn to the second entry for purpose in the companion thesaurus likewise published by Merriam- Webster. That entry lists use in its fourth sense ("a particular service or end") and function as additional synonyms of purpose. See Merriam Webster's Collegiate Thesaurus 591 (1988). Likewise, the dictionary lists purpose as a synonym of function in its sense as "the action for which a person or thing is specially fitted or used or for which a thing exists." See Merriam Webster's Collegiate Dictionary 507 ("function implies a definite end or purpose that the one in question serves or a particular kind of work it is intended to perform"). Broadly, these potential meanings of purpose describe an action, operation, or effect (or a function, use, or result) of a thing done, which can be observed objectively. Duda also argues that, by its plain meaning, the word "obstructing surface waters" as used in Section 373.406(2), Florida Statutes, cannot mean just more-than-incidentally trapping or diverting surface waters to create canals, ditches, and culverts because those works speed or increase water flow rather than obstruct it. To the contrary, Merriam-Webster defines obstruct as "1 :to block or close up by an obstacle 2 :to hinder from passage, action, or operation : IMPEDE 3 :to cut off from sight." Treating impede as a synonym for hinder and obstruct and listing further synonyms at hinder. See Merriam Webster's Collegiate Dictionary 857. The synonymy paragraph at hinder states that the core meaning shared by obstruct and its synonyms is "to interfere with the activity or progress [of something]." Id. at 588 (emphasis added); accord, The American Heritage Dictionary 960 (defiing obstruct as "1. To block or fill a passage with obstacles or an obstacle. . . . 2. To impede, retard, or interfere with; hinder"). One of these possible meanings of obstruct describes interfering with or hindering something, including its passage, action, or operation. In interpreting the word "purpose" in Section 373.406(2), Florida Statutes, it is reasonable for SJRWMD to choose the alternative meaning of an action, operation, or effect (or a function, use, or result) of a thing done, which can be observed objectively. To choose the other alternative meaning of the word would place the regulator at the mercy of the subjective intent of the person regulated and could lead to absurd results. Also, in interpreting the word "obstructing" in Section 373.406(2), Florida Statutes, it is reasonable for SJRWMD to choose the alternative meaning of interfering with or hindering something, including its passage, action, or operation. First, if the word meant only blocking, obstructing would mean the same thing as impounding and would be redundant. Second, if SJRWMD chose "blocking" as the meaning the latter meaning of the word "obstructing," it would countenance draining wetlands to use the drained land for agricultural purposes. Such a result would be in direct conflict with the intent of Chapter 373 to manage and protect water resources. See Conclusion of Law 23, infra. The extrinsic evidence of legislative intent supports SJRWMD's interpretation of Section 373.406(2), Florida Statutes. For that reason, SJRWMD's interpretation of the statute--as reflected in the Handbook--does not conflict with, exceed, modify, or contravene the statute; does not exceed statutory authority; is not standard-less or vague (so as to give SJRWMD unbridled discretion); is not arbitrary or capricious; and is not unsupported by competent, substantial evidence. It also was not proven that SJRWMD has an invalid and unadopted strategy to use various means to negate the agricultural exemption set out in Section 373.406(2), Florida Statutes. To the contrary, the evidence proved that SJRWMD interprets the statute validly and in accordance with the extrinsic evidence of the legislative intent. Finally, in the nearly 25 years that SJRWMD has interpreted Section 373.406(2), Florida Statutes, essentially as reflected in the Handbook, the Joint Administrative Procedure Committee (JAPC) has never objected to SJRWMD's interpretation as being invalid.
The Issue The issue is whether Respondent, Krista Howard,2/ is entitled to issuance of the Consolidated Environmental Resource Permit and Recommended Intent to Grant Sovereignty Submerged Lands Authorization, Permit No. 53-0351424-001-EI, as announced by Respondent, Department of Environmental Protection, in the Consolidated Notice of Intent to Issue Environmental Resource Permit and Lease to Use Sovereignty Submerged Lands issued on July 28, 2017, and subsequently amended on January 11, 2018.3/
Findings Of Fact The Parties Petitioner Defenders is a Florida non-profit corporation that has been in existence since the mid-1980s or earlier. Defenders' primary purpose is to protect and preserve Crooked Lake so that it may remain an Outstanding Florida Water ("OFW") for all members of the public to use and enjoy. Defenders has more than 25 members who reside in Polk County, Florida. Its membership consists of approximately 100 family memberships, mostly comprised of persons who live on or near Crooked Lake. Petitioners Gerards are riparian landowners on Crooked Lake, whose property is located immediately adjacent to, and slightly to the northwest of, Respondent Howard's property. The Gerards' home address is 1055 Scenic Highway North, Babson Park, Florida 33827. Respondent Howard is the applicant for the Consolidated Authorization for the Dock. Howard's property, which is riparian to Crooked Lake, is located at 1045 Scenic Highway North, Babson Park, Florida 33827. Respondent DEP is the administrative agency of the State of Florida statutorily charged with, among other things, protecting Florida's water resources. As part of DEP's performance of these duties, it administers and enforces the provisions of chapter 373, part IV, Florida Statutes, and the rules adopted pursuant to that statute. Pursuant to that authority, DEP determines whether to issue or deny applications for ERPs. Pursuant to section 253.002, Florida Statutes, DEP also serves as staff to the Board of Trustees of the Internal Improvement Trust Fund ("Board of Trustees") and, in that capacity, reviews and determines whether to issue or deny, applications for approval to use sovereignty submerged lands.5/ DEP Review of the Application The Dock is proposed to be located on sovereignty submerged lands and in surface waters subject to State of Florida regulatory jurisdiction. Therefore, an environmental resource permit and a sovereignty submerged lands lease are required. On or about February 14, 2017, Todd Rickman, Howard's professional contractor who designed the Dock, filed an Application for a Sovereignty Submerged Lands Lease for Existing Structures and Activities6/ ("Application") with DEP's Southwest District Office, seeking approval to construct and operate the Dock. On or about March 15, 2017, DEP requested additional information regarding the project. Howard submitted the requested items, and the Application was determined complete on May 30, 2017. Notice of DEP's receipt of the Lease portion of the Application was provided as required by section 253.115. The comment period commenced on June 15, 2017, and ended on July 6, 2017. As previously noted, on July 28, 2017, DEP issued the Consolidated Notice of Intent, proposing to issue the Consolidated Authorization to construct and operate the Dock. On January 11, 2018, DEP amended the Consolidated Notice of Intent to accurately reflect the "clearly in the public interest" permitting standard for the ERP portion of the Consolidated Authorization, which is applicable to projects proposed in OFWs. Background Crooked Lake Crooked Lake (also, "Lake") is an approximately 4,247-acre freshwater lake in Polk County, Florida. It is an irregularly shaped karst lake roughly resembling an inverted "L," with the longer axis running north to south. It is located on the Lake Wales Ridge. Crooked Lake is designated an OFW by Florida Administrative Code Rule 62-302.700(9)(i)9.7/ The Lake is classified as a Class III waterbody pursuant to Florida Administrative Code Rule 62-302.400(15).8/ The elevations and bottom contours in Crooked Lake vary substantially throughout the Lake. Thus, water depths may, and generally do, vary substantially from one location to another throughout the Lake. The water levels in Crooked Lake fluctuate frequently and, at times, dramatically, depending on rainfall frequency and amounts. A graph prepared by Petitioners' Witness James Tully, using Southwest Florida Water Management District ("SWFWMD") historical water level data for Crooked Lake measured in National Geodetic Vertical Datum of 1929 ("NGVD") shows water levels historically fluctuating from as low as approximately 106 feet in or around 1991, to as high as 123 feet NGVD in or around 1951, 1961, and 2004. Rickman generated a water level graph using the Polk County Water Atlas ("Atlas") website. This graph, which covers the period of 2008 through mid-2017, shows that the water levels in Crooked Lake, for this most recent ten-year period, fluctuated approximately five feet, with the lowest levels falling slightly below 114 feet NGVD for relatively short periods in 2012 and 2013, and the highest level rising to approximately 119 feet NGVD in mid-2017. The competent, credible evidence shows that although water levels in Crooked Lake may occasionally rise to levels at or around 123 feet NGVD, those conditions have been associated with extreme weather events such as hurricanes, are atypical, and are relatively short-lived. The maximum water level in Crooked Lake is subject to control by a weir located south of the Lake. Discharge from the weir occurs at a control elevation of 120 feet NGVD. As such, the water level in parts of Crooked Lake may, at times, temporarily exceed 120 feet NGVD, but will eventually decrease to 120 feet NGVD as the water flows south and is discharged through the weir. To the extent rainfall does not recharge the Lake, water levels may fall below 120 feet NGVD. The ordinary high water line ("OHWL"), which constitutes the boundary between privately-owned uplands and sovereignty submerged lands, has been established at 120.0 feet NGVD for Crooked Lake. Crooked Lake is used for recreational activities such as fishing, swimming, boating, and jet ski use, and there are public and private boat ramps at various points on the lake that provide access to the Lake. There is no marina having a fueling station on the Lake. The credible evidence shows that the northeast portion of the Lake, where the Dock is proposed to be located, experiences a substantial amount of boat and jet ski traffic. This portion of the Lake also is used for swimming, water- skiing, wakeboarding, the use of "towables" such as inner tubes, and for other in-water recreational uses. The Proposed Dock Howard holds fee title by warranty deed to parcel no. 333028-000000-033140 located at 1045 Scenic Highway, Babson Park, Florida.9/ This parcel has approximately 110 linear feet of riparian shoreline on Crooked Lake. The Dock is proposed to be constructed and operated on sovereignty submerged lands adjacent to this riparian upland parcel, which is located on the eastern shore of the northeastern portion of Crooked Lake. The Dock, as proposed, is a private single-family residential dock that will be used by Howard for water-dependent recreational purposes, such as specifically, boating, fishing, swimming, and sunbathing. The Dock is not proposed to be constructed or used by, or to otherwise serve, commercial or multifamily residential development. The Dock is configured as a "T," supported by pilings and consisting of a 4-foot-wide by 152-foot-long access walkway, and an approximately 1,983-square-foot terminal platform comprised of a lower-level platform having four vessel slips and a flat platform roof. Two sets of stairs lead from the lower level of the terminal platform to the platform roof, which will be elevated eight feet above the lower-level platform and will have a railed perimeter. The platform roof will function as a roof for the boat storage area below and a sundeck. The four slips on the Dock's lower-level platform will be used for permanent mooring for up to six watercraft: a 23-foot-long ski boat,10/ a 20-foot-long fishing boat, and four jet skis. As proposed, the Dock will occupy a total area of approximately 2,591 square feet. The lower platform of the Dock is proposed to be constructed at an elevation of 121 feet NGVD. The roof/upper platform will be constructed eight feet above that, at an elevation of 129 feet NGVD. The pilings supporting the Dock will be wrapped in an impervious material to prevent leaching of metals and other pollutants into the water. Pursuant to the Specific Purpose Field Survey ("Survey") for the Lease submitted as part of the Application, the Lease will preempt approximately 2,591 square feet, and closely corresponds to the footprint of the Dock. The submerged lands surrounding the Dock that are not occupied by the footprint of the Dock, including the area between terminal platform and the shoreline, are not included in the preempted area of the Lease.11/ The Survey shows "approximate riparian lines" which delineate Howard's riparian area oriented to the center of the waterbody and to the primary navigation channel in the northeast portion of Crooked Lake. As shown on the version of the Survey initially filed as part of the Application, the Dock was proposed to be located approximately 4.7 feet, at its closest point, from the southern riparian line. However, in response to DEP's request for additional information, the Survey was modified in April 2017, to shift the Dock northward within Howard's riparian area. The Dock is now proposed to be located 25.1 feet, at its closest point, from the southern riparian line, and 29.4 feet, at its closest point, from the northern riparian line. The walkway of the Dock will commence at an approximate elevation of 120 feet NGVD, which corresponds to the OHWL established for Crooked Lake. As previously noted above, the walkway will extend waterward approximately 152 feet, where it will intersect with the terminal platform. The terminal platform will extend another 52 feet waterward. In total, the Dock is proposed to extend waterward approximately 204 feet from the OHWL. Although the Dock would be one of the longest and largest docks on Crooked Lake, the credible evidence establishes that there are several other docks of similar size and/or length on the Lake. Rickman testified that he obtained approvals for, or was otherwise aware of, several docks over 2,000 square feet on the Lake. Additionally, the evidence showed that eight other docks on the Lake are longer than the proposed Dock.12/ Rickman testified that most of the larger docks on Crooked Lake have roofs, and that most of these roofs are pitched, rather than flat.13/ As noted above, the water level in Crooked Lake frequently and, at times, extensively fluctuates. As a result, there are periods during which water depths in parts of the Lake are extremely shallow. Rickman testified that the Dock was designed to extend far enough out into Crooked Lake to reach sufficient water depth to enable Howard to maximize the use of the Dock for boating throughout the year. The Dock is designed to extend out to the point at which the bottom elevation of the Lake is approximately 109.9 feet NGVD. Based on the Atlas' ten-year water level graph for Crooked Lake referenced above, Rickman projected that at this point, the water depth typically would be sufficient to allow Howard to operate her largest vessel, the 23-foot ski boat. The ski boat has a 25-inch draft.14/ The boat will be stored out of the water on a boat lift on the Dock, attached by cables to a sub-roof immediately beneath the platform roof. When being lowered into or hoisted from the water, the boat will be placed in a boat cradle consisting of two containment railings approximately 18 inches high each on either side, and a "V" shaped aluminum bottom with bunks on which the boat is cradled. The aluminum bottom of the cradle was estimated to be two to three inches thick. Although the boat cradle is approximately 18 to 21 inches in "total height,"15/ the cradle does not have to be completely lowered its entire 18- to 21-inch height into the water when used. Steven Howard explained, credibly, that the cradle needs to be lowered into the water only a few inches lower than the ski boat's 25-inch draft to enable the boat to float into or out of the cradle. To that point, Rickman testified that taking into account the 25-inch draft of the ski boat and the "total height" of the boat cradle, between 40 and 44 inches of water depth would be required when the cradle is used in order to avoid coming into contact with the Lake bottom. Based on the Atlas graph showing the lowest water levels for the previous ten-year period at approximately 114 feet NGVD, Rickman designed the Dock to extend out to the 109.9-foot NGVD bottom elevation point. At this point, the projected water depth would be slightly more than four feet during periods of the lowest projected water levels for Crooked Lake. For the Dock to be able to wharf out to 109.9 feet NGVD bottom elevation, it must extend a total of approximately 204 feet waterward into the Lake. The credible evidence establishes that while Howard's ski boat is one of the largest, it is not the largest boat operated on Crooked Lake. Impacts Assessment for Environmental Resource Permit Water Quality Impacts As noted above, Crooked Lake is a Class III waterbody. Accordingly, the surface water quality standards and criteria applicable to Class III waters in Florida codified in rule 62-302.300 apply to Crooked Lake. The Dock, as proposed to be constructed and operated, is not anticipated to adversely affect or degrade water quality in Crooked Lake. Specifically, as required by the Consolidated Authorization, a floating turbidity curtain will be installed around the boundary of the construction area before construction commences, and it must be left in place until construction is complete and turbidity levels in the work area have returned to background levels. Additionally, as noted, the pilings supporting the Dock must be wrapped in an impervious material to prevent leaching of metals and other pollutants into the water over the life of the structure. The Consolidated Authorization also prohibits the installation and use of fueling equipment at the Dock; prohibits the discharge of sewage or other waste into the water; prohibits liveaboards; prohibits fish cleaning or the installation of fish cleaning stations unless sufficient measures such as sink screens and waste receptacles are in place; and prohibits repair and maintenance activities involving scraping, sanding, painting, stripping, recoating, and other activities that may degrade water quality or release pollutants into the water. Although the Consolidated Authorization imposes a specific condition requiring, for all vessels using the Dock, a minimum 12-inch clearance between the deepest draft of the vessel (with motor in the down position) and the top of submerged resources, it does not specifically address circumstances where the use of the boat cradle, rather than the vessel itself, may come into contact with the Lake bottom. DEP's witness acknowledged that if the boat cradle were to come into contact with the Lake bottom, water quality standards may be violated. Given the information presented at the final hearing regarding the operation of the boat lift and the need for sufficient clearance between the bottom of the boat cradle and the lake bottom, the undersigned recommends that a specific condition be included in the Consolidated Authorization prohibiting contact of the Lake bottom by the boat cradle. This recommended condition is set forth in paragraph 73.A., below. Upon consideration of the conditions imposed by the Consolidated Authorization discussed above, including imposing a specific condition that prohibits contact of the boat cradle with the Lake bottom, the undersigned finds that the Dock will not adversely affect or degrade the water quality of Crooked Lake. Water Quantity Impacts The Dock, as proposed, is a piling-supported structure that will not impound, store, or impede the flow of surface waters. As such, the Dock will not cause adverse flooding to on-site or offsite property, will not result in adverse impacts to surface water storage and conveyance capabilities, and will not result in adverse impacts to the maintenance of surface or ground water levels. Impacts to Fish, Wildlife, and Listed Species and Habitat The Application states, in section 5, question 6, that there is no vegetation on Howard's riparian shoreline. However, the Survey depicts an area of emergent grasses approximately 60 feet wide and extending diagonally approximately 70 feet waterward into the Lake. The Survey depicts this grassed area as straddling the riparian line between Howard's property and the adjacent parcel to the south. The Survey shows the Dock as being located a significant distance waterward of the grassed area, such that no portion of the Dock will be located on or near this grassed area. Additionally, an aerial photograph of Howard's property and the Lake waterward of Howard's property shows a smaller patch of what appears to be emergent grasses further offshore. This grassed area is not shown on the Survey, and it cannot definitively be determined, by examining the Survey and the aerial photograph, whether this grassed area is growing in an area that will be impacted by the Dock. Steven Howard acknowledged that this smaller grassed area may be located at or near the jet ski slip on the southeastern side of the Dock. An environmental assessment of this smaller grassed area was not performed or submitted as part of the Application. Thus, any value that this area may have as fish and wildlife habitat was not assessed as part of DEP's determination that the Dock will not adversely impact the value of functions provided to fish, wildlife, and to listed species and their habitat. In order to provide reasonable assurance that the Dock will not adversely impact the value of functions provided to fish, wildlife, and to listed species and their habitat, the undersigned recommends including a specific condition in the Consolidated Authorization requiring this smaller grassed area to be completely avoided during construction and operation of the Dock, or, if avoidance is not feasible, that an environmental assessment be performed prior to construction so that the value of this grassed area, if any, to fish, wildlife, and listed species can be evaluated to determine whether minimization and compensatory mitigation should be required. This recommended condition is set forth in paragraph 73.B., below. As previously noted, the Consolidated Authorization contains a specific condition requiring a minimum 12-inch clearance between the deepest draft of the vessel (with the motor in the down position) and the top of submerged resources for all vessels that will use the docking facility. Compliance with this condition will help ensure that the value of functions provided to fish and wildlife and to listed species and their habitat of any such submerged resources is not adversely impacted by vessels using the Dock. The Consolidated Authorization also contains a specific condition requiring handrails to be installed on the Dock to prevent mooring access to portions of the Dock other than the wetslips. This will help protect submerged resources in shallower areas in the vicinity of the Dock. Fish populations in the immediate area of the Dock site may temporarily be affected during construction of the Dock; however, those impacts are not anticipated to be permanent. Additionally, as previously discussed, the Dock pilings must be wrapped with an impervious material to prevent leaching of pollutants into the water, and once installed, the pilings may provide habitat for fish and a substrate for benthic organisms. Provided that the conditions set forth in the draft Consolidated Authorization, as well as the recommendation regarding the smaller grassed area, are included in the final version of the Consolidated Authorization, it is determined that the construction and operation of the Dock will not adversely impact the value of functions provided to fish, wildlife, or to listed species or their habitat.16/ Impact on Navigation Petitioners assert that the Dock will constitute a hazard to navigation in the northeast portion of Crooked Lake. Specifically, they assert that because the Dock will extend out approximately 204 feet into the Lake, it necessarily will create a navigational hazard to boaters in the vicinity. As support, Petitioners presented evidence consisting of Steven Howard's testimony that an inner tube on which his nephew was riding, that was being pulled behind a motor boat, collided with the Gerards' 84-foot-long floating dock adjacent to Howard's riparian area. Petitioners argue that if an 84-foot-long dock creates a navigational hazard, a 204-foot-long dock would create an even greater navigational hazard. The undersigned does not find this argument persuasive. The portion of Crooked Lake on which the Dock is proposed to be located is approximately a mile and a half to two miles long and one-half to three-quarters of a mile wide. Although this portion of Crooked Lake experiences substantial boat traffic, the evidence shows that the Lake is sufficiently large in this area, even with the Dock in place, to allow safe navigation. To this point, it is noted that there are two other longer docks in the northeastern portion of Crooked Lake, extending 220 and 244 feet into the Lake from the shoreline. There was no evidence presented showing that either of these docks constitutes a navigational hazard.17/ Petitioners also assert that during periods of high water in this portion of Crooked Lake, the Dock will be underwater and thus will present a navigational hazard. In support, they presented photographs taken on October 30, 2017—— approximately six weeks after Hurricane Irma struck central Florida——showing ten docks, out of the 109 docks on Crooked Lake, that were partially or completely submerged.18/ When the photographs were taken, the approximate water elevation was 119.2 feet NGVD. All or a portion of the submerged docks had been constructed at or below the 119.2-foot NGVD elevation. The docks without roofs were mostly or completely invisible under the water. However, for the roofed docks, the roofs remained visible above the water even when their docking platforms were submerged. Here, although the walkway and lower platform of Howard's Dock is proposed to be constructed at an elevation of 121 feet NGVD, the roof will be constructed at an elevation of 129 feet NGVD. Thus, even during the relatively infrequent periods19/ during which the water level in Crooked Lake may exceed 121 feet NGVD, the platform roof will still be visible to vessels navigating in this portion of the Lake. Additionally, the Consolidated Authorization contains a specific condition requiring the waterward end of the Dock to be marked with a sufficient number of reflectors to be visible from the water at night by reflected light. This condition provides additional assurance that the Dock will not present a navigational hazard. For these reasons, it is determined that the Dock will not adversely affect navigation. Other ERP-Related Issues The evidence did not show that the Dock is proposed to be located in or proximate to a "work of the District," as defined in section 373.019(28). The only "work of the District" about which evidence was presented is the weir located south of Crooked Lake. This structure is many thousands of feet south of the Dock. There was no evidence presented showing that the Dock would have any impact on this weir. The Dock, as proposed, was designed by an experienced professional contractor who has designed and installed many docks on Crooked Lake, and, as such, is anticipated to function as proposed. The Dock must be built according to engineering diagrams to the Consolidated Authorization, and as-built drawings must be submitted when Dock construction is complete so that DEP can confirm that the Dock is constructed in accordance with the approved design. The evidence establishes that Howard, as the applicant, and Rickman, as the professional contractor in charge of construction, are financially, legally, and administratively capable of ensuring that the activity will be undertaken in accordance with the terms and conditions of the Consolidated Authorization. No evidence to the contrary was presented. The Dock will be located in the waters of Crooked Lake and will be affixed to the submerged bottom. The Department of State, Division of Historical Resources ("DHR"), did not provide any comments indicating that historical or archaeological resources are anticipated to be impacted by the project. Additionally, the Consolidated Authorization contains a general condition requiring subsurface activity associated with construction of the Dock to immediately cease, and DHR to be contacted, if any prehistoric or historic artifacts, such as pottery or ceramics, stone tools or implements, dugout canoes, or other physical remains that could be associated with Native American cultures or early colonial or American settlements are encountered at any time within the project site area. Additional Recommended Conditions Based on the foregoing, the undersigned recommends that the following specific conditions be included in the Consolidated Authorization, Permit No. 53-0351424-001-EI: A minimum six-inch clearance shall be maintained between the top of all submerged resources and the deepest draft of the cradle of the boat lift while in use. For purposes of this condition, submerged resources consist of the bottom sediment and/or any submerged grasses or other aquatic organisms. Any emergent grasses in the permittee's riparian area shall be avoided during the construction and operation of the Dock. If it is not feasible to avoid these grasses, an environmental assessment of the grassed area shall be performed and submitted to the Department prior to commencing construction, so that the value of this grassed area, if any, to fish, wildlife, and listed species can be evaluated and the extent to which minimization and/or compensatory mitigation is appropriate can be determined. Clearly in the Public Interest Florida Administrative Code Rule 62-4.070, Standards for Issuing or Denying Permits, states in pertinent part: A permit shall be issued to the applicant upon such conditions as the Department may direct, only if the applicant affirmatively provides the Department with reasonable assurance based on plans, test results, installation of pollution control equipment, or other information, that the construction, expansion, modification, operation, or activity of the installation will not discharge, emit, or cause pollution in contravention of Department standards or rules. In addition to the foregoing permitting requirements, because the Dock is proposed to be located in an OFW, Howard also must provide reasonable assurance that the Dock meets the "clearly in the public interest" standard. The "clearly in the public interest" standard does not require the applicant to demonstrate need for the project or a net public benefit from the project. Rather, this standard requires the applicant to provide greater assurances, under the circumstances specific to the project, that the project will comply with the applicable permitting requirements.20/ For the reasons discussed above, and with the inclusion of the additional recommended conditions in paragraphs 73.A. and 73.B., it is determined that the proposed Dock meets the applicable permitting requirements and the "clearly in the public interest" standard for issuance of the ERP. Impacts Assessment for Sovereignty Submerged Lands Lease Water-Dependency of the Proposed Dock A water-dependent activity is one which can only be conducted in, on, over, or adjacent to water areas because the activity requires direct access to the water body or sovereignty submerged lands for specified activities, including recreation, and where the use of water or sovereignty submerged lands is an integral part of the activity. See Fla. Admin. Code R. 18-21.003(71). Petitioners argue that the Dock will not constitute a water-dependent activity because the depth of water in the slips may, at times, be insufficient to allow operation of Howard's vessels while complying with the requirement that a minimum 12- inch clearance be maintained between the lowest draft of the vessel and submerged resources. The undersigned finds this argument unpersuasive. The Dock is being constructed specifically for the purpose of enabling Howard to use her vessels for boating——a recreational activity for which use of the water indisputably is an integral part. The Dock's primary purpose is to moor vessels that will be used for the water-dependent recreational activities of boating and fishing, and other water-dependent recreational uses of the Dock include fishing, swimming and sunbathing. Case law interpreting the Florida Administrative Code Chapter 18-21 makes clear that because docks are used for mooring vessels or conducting other in-water recreational uses, they are "water-dependent" activities for purposes of the rules.21/ Thus, even if water depths in the Dock's slips are at times insufficient for vessel mooring or launching,22/ this does not render the Dock not a "water-dependent activity." Resource Management Requirements The preempted area of the Lease is proposed to be used for a Dock that will be used for boating, fishing, and swimming. These traditional in-water recreational uses are consistent with the management purposes of sovereignty submerged lands as described in rule 18-21.004(2)(a). With the inclusion of the conditions currently proposed in the draft Consolidated Approval, as well as the recommended conditions in paragraphs 73.A. and 73.B., the undersigned determines that the Dock will not result in adverse impacts to sovereignty submerged lands and associated resources. With the inclusion of the conditions currently proposed in the draft Consolidated Approval, as well as the recommended conditions in paragraphs 73.A. and 73.B., the undersigned determines that the Dock is designed to minimize or eliminate impacts to fish and wildlife habitat and submerged resources. With the inclusion of the currently proposed conditions in the draft Consolidated Authorization, as well as the recommended conditions set forth in paragraphs 73.A. and 73.B., it is determined that the Dock, as designed and constructed, will minimize or eliminate cutting, removal, or destruction of wetland vegetation. Additionally, as discussed above, the proposed Consolidated Approval requires the avoidance of adverse impacts to historic and cultural resources. Riparian Rights Consistent with rule 18-21.004(3)(d), the Dock is proposed to be constructed in Howard's riparian area and will be set back more than 25 feet from the northerly and southerly riparian lines shown on the Survey. Rule 18-21.004(3)(a) prohibits activities authorized under chapter 18-21 from being implemented in a manner that would unreasonably infringe on traditional common law riparian rights, as defined in section 253.141, of upland owners adjacent to sovereignty submerged lands. Similarly, rule 18-21.004(3)(c) requires all structures and activities to be designed and conducted in a manner that will not unreasonably restrict or infringe upon the riparian rights of adjacent riparian owners. Collectively, these provisions prohibit an activity that will occur on sovereignty submerged lands from unreasonably infringing on or unreasonably restricting the riparian rights of upland riparian owners. Riparian rights are rights appurtenant to, and inseparable from, riparian land that borders on navigable waters. § 253.141, Fla. Stat.; Broward v. Mabry, 50 So. 830 (Fla. 1909). At common law, riparian rights include the rights of navigation, fishing, boating, and commerce. Hayes v. Bowman, 91 So. 2d 795 (Fla. 1957). The right of navigation necessarily includes the right to construct and operate a dock to access navigable waters. Belvedere Dev. Corp. v. Dep't of Transp., 476 So. 2d 649 (Fla. 1985); Shore Vill. Prop. Owners' Ass'n v. Dep't of Envtl. Prot., 824 So. 2d 208, 211 (Fla. 4th DCA 2002). Common law riparian rights also include the right to an obstructed view. Lee Cnty v. Kiesel, 705 So. 2d 1013 (Fla. 2d DCA 1998). Many of these common law riparian rights have been statutorily codified in section 253.141. Statutory riparian rights include the "rights of ingress, egress, boating, bathing, and fishing and such others as may be or have been defined by law." § 253.141(1), Fla. Stat. At issue in this case are the competing riparian rights of next-door neighbors——i.e., Howard's right to wharf out to navigable waters for purposes of boating and other water- dependent recreational activities, and the Gerards' right to an unobstructed view. The question is whether Howard's proposed construction and operation of a dock of sufficient length to enable her to use her boats would unreasonably infringe on or unreasonably restrict the Gerards' right to an unobstructed view of the Lake. By virtue of the riparian rights appurtenant to Howard's riparian property, she is entitled to wharf out to water deep enough to enable her to navigate. She owns two boats, one of which pulls a draft of 25 inches, and the other, a draft of 20 inches, which she uses to navigate the Lake. Thus, an essential aspect of Howard's riparian right of navigation is her ability to construct and operate a dock long enough to enable her to reach water depths sufficient to use these boats. However, as noted above, this right is not unfettered. Howard's exercise of her riparian navigation right cannot unreasonably infringe on Gerard's right to an unobstructed view. Florida case law holds that the right to an "unobstructed" view does not entail a view free of any infringement or restriction whatsoever by neighboring structures or activities. In Hayes, the court defined the right as "a direct, unobstructed view of the [c]hannel and as well a direct, unobstructed means of ingress and egress . . . to the [c]hannel." Id. at 801 (emphasis added). The court then prescribed the rule that "in any given case, the riparian rights of an upland owner must be preserved over an area 'as near as practicable' in the direction of the [c]hannel so as to distribute equitably the submerged lands between the upland and the [c]hannel." Id. (emphasis added). To the extent there is no channel in this portion of the Lake, Hayes dictates that riparian rights must be apportioned equitably, so that a riparian owner's right to an unobstructed view can extend only from the owner's property in the direction of the center of the Lake. Kling v. Dep't of Envtl. Reg., Case No. 77-1224 (Fla. DOAH Oct. 6, 1977; Fla. DER Nov. 18, 1977) at ¶¶ 11-12 (emphasis added). Here, no evidence was presented showing that the Dock——which will be located immediately south and east of the Gerards' riparian property and attendant riparian area——will present an obstruction to the Gerards' view of the Lake channel. Additionally, the evidence did not establish that Howard's Dock would obstruct the Gerards' view of the center of the northeast portion of Crooked Lake, which is located west and slightly south of their property.23/ Administrative precedent in Florida provides additional support for the determination that the Dock will not unreasonably infringe on the Gerards' right to an unobstructed view. In O'Donnell v. Atlantic Dry Dock Corporation, Case No. 04-2240 (Fla. DOAH May 23, 2005; Fla. DEP Sept. 6, 2005), riparian owners challenged the proposed approval of expansions of sovereignty submerged lands leases authorizing Atlantic Dry Dock, a neighboring commercial shipyard, to expand its shipyard facilities and install new docking facilities. The administrative law judge noted that although the expanded shipyard would further encroach on the riparian owners' already somewhat-restricted view from their property, it would not substantially and materially obstruct the Petitioners' view to the channel. He commented: "it [their view] may be further obstructed to the west in the direction of the Atlantic Marine yard, but not in the direction of the channel." To that point, he found that although "any lateral encroachment on the Petitioners' line-of-sight to the channel by the large eastern dry dock proposed will be an annoyance, . . . [it] will not rise to the level of a substantial and material interference or obstruction of the Petitioners' view to the channel." Id. at ¶ 119. He found that "there is no 'special riparian right' to a view of the sunset, just as there was no right to a particular object of view . . . by the riparian owners complaining in the Hayes case." Id. at ¶ 120. Castoro v. Palmer, Case Nos. 96-0736, 96-5879 (Fla. DOAH Sept. 1, 1998; Fla. DEP Oct. 19, 1998), also is instructive. In Castoro, neighboring riparian owners challenged the proposed issuance of an environmental approval and sovereignty submerged lands lease for a 227-foot-long dock having a terminal platform with boat lift. The owners contended that due to the dock's length, it would impermissibly obstruct their views of the water. The administrative law judge rejected that contention, distinguishing the circumstances from those in Lee County v. Kiesel, 705 So. 2d 1013 (Fla. 2d DCA 1998), in which the construction of a bridge that blocked 80 percent of the riparian owners' view of the channel was held to constitute a "substantial and material" obstruction to the riparian right of view. The ALJ noted that although the dock would have "some impact on the neighbors' views" and their use of the waterbody, it did not unreasonably impact their riparian rights to an unobstructed view or to use of the waterbody. Id. at ¶¶ 73-74. In Trump Plaza of the Palm Beaches Condominium v. Palm Beach County, Case No. 08-4752 (Fla. DOAH Sept. 24, 2009; Fla. DEP Oct. 8, 2009), a condominium association challenged the proposed issuance of a sovereignty submerged lands use approval to fill in a dredged area and create mangrove islands in the Lake Worth Lagoon, alleging, among other things, that the creation of the mangrove islands would unreasonably infringe on their riparian right to an unobstructed view. In rejecting this position and recommending issuance of the submerged lands use approval, the ALJ noted that the area obstructed by the mangrove islands would be negligible compared to the remaining expanse of the view, and further noted that the owners' real concern was directed at the aesthetics of the project——specifically, they did not want to view mangrove islands. The ALJ stated: "[t]he evidence supports a finding that while the project will undoubtedly alter the view of the water from [the riparian owners' property], the impact on view is not so significant as to constitute an unreasonable infringement of their riparian rights." Id. at ¶ 86. Applying these case law principles, it is determined that the Dock will not unreasonably infringe on or unreasonably restrict the Gerards' riparian right to an unobstructed view. To that point, the cases make clear that the right to an "unobstructed" view is not an unfettered right to a view of the water completely free of any lateral encroachment, but, instead is the right of a view toward the channel or the center of a lake without unreasonable infringement or restriction. Here, although the Dock will laterally encroach on the Gerards' full panoramic view of the Lake——and, as such, may even constitute an annoyance, the evidence did not show that the Dock will obstruct or otherwise restrict their view to the channel or the center of the Lake. Moreover, to the extent the Gerards have expressed concern about the Dock interfering with their view of the south shore of the Lake, O'Donnell makes clear the desire to have a particular object of view——here, the south shore of the Lake——is not a legally protected riparian right. It is also found that the Dock will not unreasonably interfere with the Gerards' riparian rights of ingress, egress, boating, or navigation. As previously noted, the Dock will be located at least 25 feet inside the riparian lines established for Howard's upland property, and, it will not be constructed in a location or operated in a manner that will obstruct, interfere with, or restrict the Gerards' access to the Lake or to sufficient water depths to enable navigation.24/ The evidence also did not establish that the Dock will restrict or otherwise interfere with the Gerards' use of their riparian area for ingress and egress, boating, fishing, bathing, or other riparian uses. In sum, it is concluded that the Dock will not unreasonably infringe on or restrict the riparian rights of adjacent upland riparian owners. Accordingly, it is determined that the Dock will meet the requirements and standards in rule 18-21.004(3) regarding riparian rights. Navigational Hazard For the reasons discussed in paragraphs 63 through 67, it is determined that the Dock will not constitute a navigational hazard in violation of rule 18-21.004(7)(g). Not Contrary to the Public Interest Rule 18-21.004(1)(a) requires an applicant to demonstrate that an activity proposed to be conducted on sovereignty submerged lands will not be contrary to the public interest. To meet this standard, it is not necessary that the applicant show that the activity is affirmatively in the "public interest," as that term is defined in rule 18-21.003(51). Rather, it is sufficient that the applicant show that there are few, if any, "demonstrable environmental, social, and economic costs" of the proposed activity. Castoro, at ¶ 69. For the reasons discussed above, and with the inclusion of the additional recommended conditions in paragraphs 73.A. and 73.B., it is determined that the proposed Dock meets the "not contrary to the public interest" standard required for issuance of the Lease. Demonstration of Entitlement to ERP Howard met her burden under section 120.569(2)(p) to present a prima facie case of entitlement to the ERP by entering into evidence the Application, the Notice of Intent, and supporting information regarding the proposed Dock. She also presented credible, competent, and substantial evidence beyond that required to meet her burden under section 120.569(2)(p) to demonstrate prima facie entitlement to the ERP. The burden then shifted to Petitioners to demonstrate, by a preponderance of the competent substantial evidence, that the Dock does not comply with section 373.414 and applicable ERP rules. For the reasons discussed above, it is determined that Petitioners did not meet their burden of persuasion under section 120.569(2)(p) in this proceeding. Accordingly, for the reasons addressed above, it is determined that Howard is entitled to issuance of the ERP for the Dock. Demonstration of Entitlement to Lease As previously discussed, Howard bore the burden of proof in this proceeding to demonstrate, by a preponderance of the evidence, that the Dock meets all applicable statutory and rule requirements for issuance of the Lease for the Dock. For the reasons discussed above, it is determined that Howard met this burden, and, therefore, is entitled to issuance of the sovereignty submerged lands lease for the Dock. Petitioners' Standing Defenders' Standing As stipulated by the parties and noted above, Defenders is an incorporated non-profit entity created for the primary purpose of protecting and preserving Crooked Lake so that it may remain an OFW for all members of the public to enjoy. Defenders has been in existence since at least the mid- 1980s. Robert Luther, the president of Defenders, testified that the organization's purpose also entails providing education and promoting public awareness in order to preserve the natural beauty, water quality, ecological value, and quality of life around Crooked Lake. As stipulated by the parties and noted above, Defenders has more than 25 members. Luther testified that Defenders has approximately 100 family members, most of whom live on or around Crooked Lake. He noted that many of Defenders' members own boats, which they park at a local boat landing on the Lake. Based on this testimony, it is inferred that these members operate their boats on Crooked Lake. After receiving the public notice of the project, Defenders' board of directors voted to oppose issuance of the Consolidated Authorization for the Dock. Luther testified that the board's decision was based on the determination that "it was clearly within the public interest" to oppose the Dock. Gerards' Standing The Gerards reside at 1055 Scenic Highway, Babson Park, Florida. Their riparian property is immediately adjacent to, and northwest of, Howard's property. The Gerards own a floating dock that is located within their riparian area.25/ The dock consists of two 4-foot- wide by 30-foot-long ramps attached to a 24-foot-long by 8-foot- wide pontoon boat. Priscilla Gerard testified that she enjoys spending time sitting and reading books on the beach in front of her property, and that having that area to sit and read is a significant aspect of her enjoyment of her lakefront property. Ms. Gerard observed that extensive boating activities in the northeast portion of the Lake on weekends is disruptive, and interferes with her use of her beach for relaxing and reading. She particularly noted that boats operating very close to the shore cause waves to splash up on her beach, interfering with her ability to sit and read close to the shore. She did not contend that Howard's use of the Dock for boating would contribute to the disruptive nature of existing boat traffic in the vicinity. Ms. Gerard has viewed the plans for the proposed Dock and is very concerned that due to its size, her view of the south side of the Lake will be completely blocked. She acknowledged, and other competent, credible evidence showed, that there are other docks on the Lake in the vicinity of her riparian property. The evidence shows that existing docks having lengths of 145 feet and 170 feet are located in the vicinity of, and are visible from, the Gerards' property. She testified that an existing dock and tiki hut block her view of the Lake to the north. She acknowledged that although Howard's Dock, if constructed as proposed, may somewhat obstruct her view to the left (south) of her property, it would not block her view straight out into the Lake. Phillip Gerard testified that he has boated extensively on Crooked Lake in a variety of vessel types. He further testified that he has observed a range of boating practices on Crooked Lake, including seeing water skiers and persons being towed behind motorized vessels on inner tubes and other types of "towables." He testified that, based on his personal observations, persons being towed do not have independent control of the speed or direction of the "towable"; thus, depending on the direction in which the towing vessel turns, the towable may be slung to the left or the right. Gerard commented that such lack of control could result in a person riding on a towable colliding with a dock, and he noted that Howard's nephew, who was riding on an inner tube being towed by a boat, was involved in such a collection with his (Mr. Gerard's) own dock. Mr. Gerard did not testify that the Dock would present a navigational hazard to, or otherwise interfere with, the Gerards' riparian right of ingress and egress. Neither of the Gerards testified that the Dock would impact their ability to access navigable waters in the Lake. Mr. Gerard acknowledged that if Howard's Dock were constructed, boats that currently travel very close to the shoreline of his property would be forced to swing further out in the Lake, away from his riparian shoreline, in order to avoid the Dock.
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 approving the issuance of Consolidated Environmental Resource Permit and Recommended Intent to Grant Sovereignty Submerged Lands Authorization, Permit No. 53-0351424-001-EI, on the terms and conditions set forth in the Consolidated Notice of Intent and attached draft of Permit No. 53-0351424-001-EI, as modified to include the Additional Recommended Conditions set forth in paragraphs 73.A. and 73B. DONE AND ENTERED this 5th day of July, 2018, in Tallahassee, Leon County, Florida. S CATHY M. SELLERS 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 5th day of July, 2018.
