Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that application number 07256-F be APPROVED subject to the special conditions set forth above. DONE AND ORDERED this 15th day of July 1987, in Tallahassee, Leon County, Florida. DONALD R. ALEXANDER Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 904/488-9675 Filed with the Clerk of the Division of Administrative Hearings this 15th day of July 1987.
Findings Of Fact Mr. Mills owns a 105 acre tract of land on which he raises cattle. This land is directly east of South Bull Pond in Putnam County, Florida. The land which he proposes to fill lies within the landward extent of South Bull Pond. The pond is a natural lake of approximately 350 acres which does not become dry each year. The lake has a maximum average depth of greater than 2 feet throughout the year. Its shoreline is owned by more than one person. South Bull Pond is a Class III water of the State of Florida. Petitioner's proposed project involves the excavation of approximately 5,000 cubic yards of sand and muck from the lake bottom. He plans to place the fill in an area adjacent to the dredge site but within the landward extent of the lake. The area to be excavated is 200 feet long and 50 feet wide. The area to be filled with spoil material is the same size immediately to the east of the dredge area. The excavation will be approximately three feet deep into the lake bottom. Mr. Mills' application indicates that the purpose of the proposed work is to keep his cows out of the bog and also to increase the value of his property. The proposed dredging and filling will result in the permanent elimination of approximately one-half acre of natural vegetation along the lake. This area consists of a natural berm formed by alluvial deposits and a wet bog landward of the berm. There is an opening through the berm which allows the free exchange of waters between the main body of the lake and the bog area. The top elevation of the berm is such that the berm area is submerged for long periods of time. Ordinary high water inundates the berm and passes over it into the bog which is at a lower elevation than the berm. The field appraisal of the proposed site was conducted by Mr. John Hendrix, a Department biologist, on May 5, 1981. The site consists of three areas: the lakeshore, the berm, and the bog. The dominate species along the lakeshore are Saw grass (Cladium jamaicensis), Water Lily (Nymphaea spp.), Pickerelweed (Pontederia lanceolata), and Spatter dock (Nuphar spp.). The dominant fresh water species on the berm are: Saw grass (Cladium jamaicensis), and Arrowhead (Sagittaria spp.). Two transitional fresh water species also grow on the berm: St. John's wort (Hypericum fasciculatum) and Button bush (Cephalanthus occidentalis). The dominant species of the bog, which is landward of the berm, are Water Lily (nymphaea spp.), Water shield (Brasenia schreberi), Royal fern (Osmunda regalis), and Arrowhead (Sagittaria spp.). The lake is presently mesotrophic. It has a large productive vegetative structure primarily along the shoreline. The nutrients are "tied up" or stored in the marshes and peaty sediments of this shoreline and are not freely circulating in the main water body. The shoreline vegetation provides filtration for the main water body. The plants physically entrap sediments and biochemically assimilate them. They also store nutrients which otherwise degrade the water in the lake. The proposed dredging and filling will degrade water quality in two ways: 1) The equipment used for dredging will disrupt the sediments. They will then discharge freely into the water column of the lake and release their stored nutrients. 2) The berm and bog areas will be destroyed so that they can no longer stabilize the shoreline or provide the filtration function. Adverse water quality impacts from the project will be both short and long term. The short terms impacts include expected violations of the following water quality criteria found in Chapter 17-3, Florida Administrative Code: BOD; dissolved oxygen; transparency; biological integrity; turbidity; pH; nuisance species; and both nutrients criteria. The long term impacts will include stimulation of shifting of the natural balance of the lake towards a more eutrophic state and violation of the water quality criteria for nutrients, dissolved oxygen, BOD and transparency. Petitioner wants to fill the bog to prevent injury to his cows. A workable alternative to filling the bog is to erect a fence across the property to exclude the cows from that area. The drawings submitted by Petitioner as part of his application show that the operation of the dredging machinery would be from the berm. During the hearing Petitioner indicated that such machinery would be operating from the lakeshore. This modification would create fewer short term violations of water quality criteria. However, the following criteria would still be violated: BOD, turbidity, nuisance species, biological integrity, dissolved oxygen, transparency and nutrients.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Department of Environmental Regulation enter a final order denying Petitioner's permit application. DONE AND ENTERED this 14th day of October 1981 in Tallahassee, Florida. MICHAEL PEARCE DODSON Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 14th day of October 1981. COPIES FURNISHED: Jimmie L. Mills Route 2, Box 244 Hawthorne, Florida 32640 Silvia Morell Alderman, Esquire Cynthia K. Christen, Esquire Assistant General Counsel Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301
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 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
Findings Of Fact The petitioner is a private landowner of a tract of land adjacent to the Suwannee River in Dixie County, Florida. The Respondent, State of Florida, Department of Environmental Regulation, is an agency of the State of Florida charged with carrying out the mandates of Chapter 403, Florida Statutes, and the rules contained in the Florida Administrative Code promulgated thereunder. The Petitioner's proposed project entails the construction of a twelve- foot wide filled road across approximately 270 feet of swampy area in which the dominant plant species is bald cypress (taxodium distichum), a species listed in Rule 17-4.02(17), Florida Administrative Code. The property to be so developed by the petitioner lies within the landward extent of the Suwannee River in Dixie County. The Suwannee River, in this project area, constitutes waters of the state over which the Department has dredge and fill permitting jurisdiction pursuant to Rule 17-4.28(a), Florida Administrative Code. The project areas within "outstanding Florida waters" as defined in Rule 17-3.04(1)(3)g, Florida Administrative Code. The "upland berm" or river terrace on the property immediately adjacent to the navigable portion of the river is caused by the natural alluvial deposition of the river and the landward extent of the state waters here involved crosses the property in approximately the center of the parcel. The proposed filing for the road crossing the swamp would result in the permanent elimination of at least 3,240 square feet of area within the landward extent of the Suwannee River. Specifically, the project would consist of a road some 12 feet wide at the bottom and 8 feet wide at the top, extending approximately 270 feet across the swampy area in question from the portion of the property which fronts on a public road, to the river terrace or "berm" area along the navigable portion of the Suwannee River. The road will be constructed with approximately 450 cubic yards of clean fill material with culverts 12 feet in length and 3 feet in diameter placed under the road at 25 foot intervals. The parties have stipulated that the Department has jurisdiction pursuant to Chapter 403, Florida Statutes, and Public Law 92-500, to require a permit and water quality certification or the construction of a stationary installation within the waters of the state which this project has been stipulated to be. The area to be filled is primarily vegetated by bald cypress, ash, blackgum, planer trees and other swamp species falling within the definitional portion of the above rule. The swamp contributes to the maintenance of water quality in the river itself by the filtering of sediment and particulates, assimilating and transforming nutrients and other pollutants through the uptake action of the plant species growing therein. The proposed project would destroy by removal, and by the filling, a substantial number of these species on the site which perform this function. The swamp area also serves as a habitat, food source and breeding ground for various forms of fish and wildlife including a species of state concern, the yellow-crowned night heron, which has been observed on this site and which requires such habitat for breeding and for its food source (see the testimony of Kautz). The area in question provides flood protection by storing flood waters and releasing them in a gradual fashion to the river system, especially during dry periods when the river level is lower than that of the swamp which serves to augment stream flow in such periods. As established by witness Kautz, as well as witnesses Rector and Tyler, the filling proposed by the Petitioner would cause degradation of local water quality within the immediate area where the fill would be placed and, the attendant construction activity adjacent to either side of the filled area would disturb trees, animals and other local biota. The period during and immediately after the construction on the site would be characterized by excessive turbidity and resultant degradation of the water quality within the area and downstream of it. The long-term impact of the project would include continued turbidity adjacent to and downstream from the filled road due to sloughing off of the sides of the road caused by an excessively steep slope and to the necessary maintenance operations required to re-establish the road after washouts caused by each rain or rainy period. An additional long-term detrimental effect will be excessive nutrient enrichment expected in the area due to the removal of the filtrative functions caused by removal of the trees and other plant life across the entire width of the swamp and the resultant inability of the adjacent areas to take up the nutrient load formerly assimilated by the plant life on the project area. The project will thus permanently eradicate the subject area's filtrative and assimilative capacity for nutrients, heavy metals and other pollutants. The effect of this project, as well as the cumulative effect of many such already existent fill roads in this vicinity along the Suwannee River, and the effect of proliferation of such filling, will cause significant degradation of local water quality in violation of state standards. The effect of even this single filled road across the subject swamp is especially severe in terms of its "damming" effect (even with culverts). The resultant retention of water standing in the swamp for excessive periods of time will grossly alter the "hydro period" of the area or the length of time the area is alternately inundated with floodwaters or drained of them. This will cause a severe detrimental effect on various forms of plant and animal life and biological processes necessary to maintenance of adequate water quality in the swamp and in its discharge to the river itself. The excessive retention of floodwaters caused by this damming effect will ultimately result in the death of many of the tree species necessary for the uptake of nutrients and other pollutants which can only tolerate the naturally intermittent and brief flood periods. This permit is not necessary in order for the Petitioner to have access to his property as his parcel fronts on a public access road. The purpose of the proposed road is merely to provide access to the river terrace or "upland berm" area on the portion of the property immediately adjacent to the navigable waters of the Suwannee River. The Department advocated through its various witnesses that a viable and acceptable alternative would be the construction of a walkway or a bridge on pilings across the jurisdictional area in question connecting the two upland portions of Petitioner's property. Such a walkway would also require a permit, but the Department took the position that it would not object to the permitting of an elevated wooden walkway or bridge for vehicles. The petitioner, near the close of the hearing, ultimately agreed that construction of such a walkway or bridge would comport with his wishes and intentions for access to the river berm portion of his property and generally indicated that that approach would be acceptable to him. It should also be pointed out that access is readily available to the waterward portion of the property from the navigable waters of the river by boat. The Petitioner did not refute the evidence propounded by the Department's expert witnesses, but testified that he desired the fill-road alternative because he believed it to be somewhat less expensive than construction of an elevated wooden bridge or walkway and that he had been of the belief that the use of treated pilings for such a walkway or bridge would result in chemical pollution of the state waters in question. The expert testimony propounded by the Respondent, however, establishes that any leaching action of the chemical in treated pilings would have a negligible effect on any life forms in the subject state waters at any measurable distance from the pilings. In summary, the petitioner, although he did not stipulate to amend his petition to allow for construction of the bridge as opposed to the fill road, did not disagree with it as a viable solution and indicated willingness to effect establishment of access to the riverfront portion of his property by that alternative should it be permitted.
Recommendation Based upon the findings of fact and conclusions of law recited above, it is recommended that petitioner's application for a permit to connect his canal to the Caloosahatchee River be DENIED. Respectfully submitted and entered this 22nd day of December, 1976, in Tallahassee, Florida. DIANE D. TREMOR Hearing Officer Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 22nd day of December, 1976.
The Issue The issues to be determined in these consolidated cases are whether All Aboard Florida – Operations, LLC (“the Applicant”), and Florida East Coast Railway, LLC (“FECR”), are entitled to an Environmental Resource Permit Modification authorizing the construction of a stormwater management system and related activities to serve railway facilities, and a verification of exemption for work to be done at 23 roadway crossings (collectively referred to as “the project”).
Findings Of Fact The Parties Petitioners Martin County and St. Lucie County are political subdivisions of the State of Florida. Petitioners have substantial interests that could be affected by the District’s proposed authorizations. Intervenor Town of St. Lucie Village is a political subdivision of the State of Florida. Intervenor has substantial interests that could be affected by the District’s proposed authorizations. The Applicant, All Aboard Florida – Operations, LLC, is a Delaware limited liability company based in Miami. All Aboard Florida is part of a group of corporate entities formed for the principal purpose of developing and operating express passenger train service in Florida. Co-applicant Florida East Coast Railway, LLC, is a Florida limited liability company based in Jacksonville. FECR owns the existing railway corridor the passenger train service will use between Miami and Cocoa. South Florida Water Management District is a regional agency granted powers and assigned duties under chapter 373, part IV, Florida Statutes, including powers and duties related to the regulation of construction activities in wetlands. The proposed activities are within the boundaries of the District. Background The objective of the All Aboard Florida Project is to establish express passenger train service connecting four large urban areas: Miami, Fort Lauderdale, West Palm Beach, and Orlando. Most of the passenger service route, including the portion which will pass through Martin County and St. Lucie County, will use an existing railroad right-of-way used since the late 1800s. The FECR rail corridor runs along Florida’s east coast from Miami to Jacksonville. It supported passenger and freight operations on shared double mainline tracks from 1895 to 1968. The passenger service was terminated in 1968 and portions of the double track and certain bridge structures were removed. The freight service continued and remains in operation today. The passenger service will use the FECR right-of-way from Miami to Cocoa and then turn west on a new segment to be constructed from Cocoa to Orlando. The railway corridor will be operated as a joint facility, with passenger and freight trains sharing the double mainline tracks. The Applicant is upgrading the portion of the corridor between Miami and Cocoa by, among other things, replacing existing railroad ties and tracks, reinstalling double mainline tracks, and improving grade crossings. The Applicant is also installing Positive Train Control systems which provide integrated command and control of passenger and freight train movements and allow the trains to be directed and stopped remotely or automatically in the event of operator error or disability, or an obstruction on the track. The All Aboard Florida Project is being developed in two phases, Phase I extends from Miami to West Palm Beach, and Phase II from West Palm Beach to Orlando. This proceeding involves a segment within Phase II, known as Segment D09, which runs from just north of West Palm Beach to the northern boundary of St. Lucie County. The railway corridor in Segment D09 passes through Jonathan Dickinson State Park in Martin County and the Savannas Preserve State Park, parts of which are in both Martin County and St. Lucie County. Surface waters within these state parks are Outstanding Florida Waters (“OFWs”). The railway in Segment D09 also passes over the St. Lucie River using a bridge that can be opened to allow boats to pass. The Applicant plans to run 16 round trips per day between Miami and Orlando, which is about one train an hour in each direction, starting early in the morning and continuing to mid-evening. In 2013, the District issued the Applicant an exemption under section 373.406(6), which exempts activities having only minimal or insignificant adverse impacts on water resources. The 2013 exemption covers proposed work in approximately 48 of the 65 miles which make up Segment D09, and includes replacement of existing tracks and re-establishment of a second set of mainline tracks where they were historically located. The 2013 exemption covers all but 24 of the roadway crossings within Segment D09 where work is to be done in connection with the All Aboard Florida Project. In 2015, the District issued the Applicant a general permit under rule 62-330.401, which authorizes activities that are expected to cause minimal adverse impacts to water resources, for the installation of fiber optic cable along the rail bed within Segment D09. The 2013 exemption and 2015 general permit were not challenged and became final agency action. The Proposed Agency Actions The ERP Modification covers work to be done in approximately 17 of the 65 miles which make up Segment D09. The work will consist primarily of replacing existing tracks, installing new tracks, making curve modifications in some locations to accommodate faster trains, culvert modifications, and work on some fixed bridge crossings over non-navigable waters. The 2017 Exemption at issue in this proceeding covers improvements to 23 of the 24 roadway crossings that were not covered by the 2013 exemption. Proposed improvements at Southeast Florida Street in Stuart will be permitted separately. The improvements covered by the 2017 Exemption include upgrading existing safety gates and signals; installing curbs, guardrails, and sidewalks; resurfacing some existing paved surfaces; and adding some new paving. Petitioners argue that, because the District’s staff report for the ERP Modification states that the ERP does not cover work at roadway crossings, track work at roadway crossings has not been authorized. However, the staff report was referring to the roadway improvements that are described in the 2017 Exemption. The proposed track work at the roadway crossings was described in the ERP application and was reviewed and authorized by the District in the ERP Modification. “Segmentation” Petitioners claim it was improper for the District to separately review and authorize the proposed activities covered by the 2013 exemption, the 2015 general permit, the ERP Modification, and the 2017 Exemption. Petitioners contend that, as a consequence of this “segmentation” of the project, the District approved “roads to nowhere,” by which Petitioners mean that these activities do not have independent functionality. Petitioners’ argument is based on section 1.5.2 of the Applicant’s Handbook, Volume 1,1/ which states that applications to construct phases of a project can only be considered when each phase can be constructed, operated, and maintained totally independent of future phases. However, the activities authorized by the four agency actions are not phases of a project. They are all parts of Phase II of the All Aboard Florida Project, which is the passenger railway from West Palm Beach to Orlando. Section 1.5.2 is not interpreted or applied by the District as a prohibition against separate review and approval of related activities when they qualify under the District’s rules for exemptions, general permits, and ERPs. Much of Phase II is outside the District’s geographic boundaries and, therefore, beyond its regulatory jurisdiction. The District can only review and regulate a portion of Phase II. The District is unable to review this portion as a stand-alone railway project that can function independently from other project parts. The Proposed Stormwater Management System Where the Applicant is replacing existing tracks or re- establishing a second set of tracks, it will be laying new ties, ballast, and rail on previously-compacted earth. In those areas, no stormwater management modifications were required by the District. The Applicant’s new proposed stormwater management system will be located in a five-mile area of the corridor where an existing siding will be shifted outward and used as a third track. In this area, swales with hardened weir discharge structures and skimmers will be installed to provide stormwater treatment beyond what currently exists. The weir discharge structures will serve to prevent erosion at discharge points. The skimmers will serve to capture any floating oils or refuse. Because the FECR right-of-way is not wide enough in some three-track areas to also accommodate swales, the proposed stormwater management system was oversized in other locations to provide compensating volume. The District determined that this solution was an accepted engineering practice for linear systems such as railroads. Petitioners argue that the Applicant’s proposed stormwater management system is deficient because some of the proposed swales do not meet the definition of “swale” in section 403.803(14) as having side slopes equal to or greater than three feet horizontal to one foot vertical (3:1). The statute first defines a swale to include a manmade trench which has “a top width-to-depth ratio of the cross-section equal to or greater than 6:1.” The swales used in the proposed stormwater management system meet this description. Petitioners showed that the plans for one of the 46 proposed swales included some construction outside the FECR right-of-way. In response, the Applicant submitted revised plan sheets to remove the swale at issue. The Emergency Access Way The ERP application includes proposed modifications to portions of an existing unpaved emergency access way which runs along the tracks in some areas. The access way is a private dirt road for railroad-related vehicles and is sometimes used for maintenance activities. At the final hearing, Petitioners identified an inconsistency between an application document which summarizes the extent of proposed new access way construction and the individual plan sheets that depict the construction. The Applicant resolved the inconsistency by correcting the construction summary document. Petitioners also identified an individual plan sheet showing proposed access way modifications to occur outside of the FECR right-of-way. This second issue was resolved by eliminating any proposed work outside the right-of-way. Petitioners believe the proposed work on the access way was not fully described and reviewed because Petitioners believe the access way will be made continuous. However, the access way is not continuous currently and the Applicant is not proposing to make it continuous. No District rule requires the access way segments to be connected as a condition for approval of the ERP. Water Quantity Impacts An applicant for an ERP must provide reasonable assurance that the construction, operation, and maintenance of a proposed project will not cause adverse water quantity impacts to receiving waters and adjacent lands, adverse flooding to on-site or off-site property, or adverse impacts to existing surface water storage and conveyance capabilities. The District’s design criterion to meet this requirement for water quantity management is a demonstration that the proposed stormwater system will capture the additional runoff caused during a 25-year/3-day storm event. The Applicant’s proposed stormwater system meets or exceeds this requirement. Petitioners argue that the Applicant failed to provide reasonable assurance because the ERP application materials did not include a calculation of the discharge rates and velocities for water discharging from the swales during the design storm. The ERP application contains the information required to calculate the discharge rates and velocities and the Applicant’s stormwater expert, Bruce McArthur, performed the calculations and testified at the final hearing that in the areas where there will be discharges, the discharge rates and velocities would be “minor” and would not cause adverse impacts. The District’s stormwater expert, Jesse Markle, shared this opinion. Petitioners argue that this information should have been provided to the District in the permit application, but this is a de novo proceeding where new evidence to establish reasonable assurances can be presented. Petitioners did not show that Mr. McArthur is wrong. Petitioners failed to prove that the proposed project will cause adverse water quantity impacts, flooding, or adverse impacts to surface water storage and conveyance capabilities. Water Quality Impacts To obtain an ERP, an applicant must provide reasonable assurance that the construction, operation, and maintenance of a regulated project will not adversely affect the quality of receiving waters, such that state water quality standards would be violated. The District’s design criteria for water quality required the Applicant to show that its proposed stormwater system will capture at least 0.5 inches of runoff over the developed area. To be conservative, the Applicant designed its proposed system to capture 1.0 inch of runoff in most areas. Under District rules, if a stormwater system will directly discharge to impaired waters or OFWs, an additional 50 percent of water quality treatment volume is required. The proposed stormwater system will not directly discharge to either impaired waters or OFWs. In some locations, there is the potential for stormwater discharged from the proposed stormwater system to reach OFWs by overland flow, after the stormwater has been treated for water quality purposes. The Applicant designed its proposed stormwater system to provide at least an additional 50 percent of water quality treatment volume in areas where this potential exists. To ensure that the proposed construction activities do not degrade adjacent wetlands, other surface waters, or off-site areas due to erosion and sedimentation, the Applicant prepared an Erosion and Sediment Control Plan. Temporary silt fences and turbidity barriers will be installed and maintained around the limits of the construction. The District’s design criteria for water quality do not require an analysis of individual contaminants that can be contained in stormwater, except in circumstances that do not apply to this project. Compliance with the design criteria creates a presumption that water quality standards for all potential contaminants are met. See Applicant’s Handbook, V. II, § 4.1.1. Although not required, the Applicant provided a loading analysis for the proposed swales which could potentially discharge overland to impaired waters or OFWs. The analysis compared pre- and post-development conditions and showed there would be a net reduction in pollutant loading. Petitioners believe the pollutant loading analysis was inadequate because it did not specifically test for arsenic and petroleum hydrocarbons. However, the analysis was not required and adequate treatment is presumed. Petitioners did not conduct their own analysis to show that water quality standards would be violated. Petitioners’ expert, Patrick Dayan, believes the compaction of previously undisturbed soils in the emergency access way would increase stormwater runoff. However, he did not calculate the difference between pre- and post-construction infiltration rates at any particular location. His opinion on this point was not persuasive. Petitioners failed to prove that the proposed project will generate stormwater that will adversely affect the quality of receiving waters such that state water quality standards would be violated. The preponderance of the evidence shows the project complies with District design criteria and will not cause water quality violations. Soil and Sediment Contamination Petitioners argue that the ERP Modification does not account for the disturbance of existing contaminants in soils and sediments that could be carried outside of the right-of-way and into OFWs. Petitioners’ argument is based on investigations by their geologist, Janet Peterson, who collected soil, sediment, and surface water samples at 13 sites along the FECR rail corridor in the vicinity of OFWs, or surface waters that eventually flow into OFWs. During her sampling visits, Ms. Peterson saw no visual evidence of an oil spill, fluid leak, or other release of hazardous materials. Ms. Peterson compared her soil sample results to the Residential Direct Exposure Soil Cleanup Target Levels (“SCTLs”) established in rule 62-777. The SCTLs are the levels at which toxicity becomes a human health concern and the residential SCTLs assume soil ingestion of 200 mg/day for children, and 100 mg/day for adults, 350 days a year, for 30 years. Some of the soil sampling results showed exceedances of SCTLs, but the SCTLs are not applicable here because none of the sample sites are locations where children or adults would be expected to ingest soil at such levels for such lengths of time. Petitioners did not show that the contaminants are likely to migrate to locations where such exposure would occur. Ms. Peterson compared her soil sample results to the Marine Surface Water Leachability SCTLs, but she did not develop site-specific leachability-based SCTLs using DEP’s approved methodology. Nor did she show that the proposed project will cause the soils to leach the contaminants. Ms. Peterson collected sediment samples from shorelines, but not where construction activities are proposed. She compared her sediment sample results to the Florida Department of Environmental Protection’s (“DEP”) Sediment Quality Assessment Guidelines (“SQAGs”). These guidelines are not water quality standards. Any exceedance of these guidelines requires further analysis to determine potential water quality impacts. Ms. Peterson did not conduct the analysis. Ms. Peterson acknowledged that there are numerous sources for these pollutants at or near her sample sites, such as high-traffic roads, vehicular bridges, commercial and industrial facilities, boatyards, and golf courses. She did not establish baselines or controls. Ms. Peterson collected surface water samples at seven sites, some of which were located outside the FECR right-of-way. The results showed levels of phosphorous and nitrogen above the criteria for nutrients at some locations. Phosphorous, nitrogen, and the other nutrients are prevalent in the waters of Martin County and St. Lucie County and come from many sources. Petitioners’ evidence focused on existing conditions and not expected impacts of the proposed project. The evidence was insufficient to prove the proposed project will cause or contribute to water quality violations. Functions Provided by Wetlands and Other Surface Waters An applicant for an ERP must provide reasonable assurance that a proposed project will not adversely impact the value of functions provided to fish and wildlife and listed species by wetlands and other surface waters. Petitioners claim the Applicant and District should not have relied on Florida Land Use Cover and Forms Classification System (“FLUCCS”) maps to identify and characterize wetlands and other habitat areas because the maps are too general and inaccurate. However, the FLUCCS maps were not used by the Applicant or District to evaluate impacts to wetlands or other habitats. The Applicant began its evaluation of impacts to wetlands and other habitat areas by field-flagging and surveying the wetland and surface water boundaries in the project area using a GPS device with sub-meter accuracy. It then digitized the GPS delineations and overlaid them with the limits of construction to evaluate anticipated direct impacts to wetlands and other surface waters. The District then verified the delineations and assessments in the field. The Applicant and District determined that there are a total of 4.71 acres of wetlands within the FECR right-of-way, including tidal mangroves, freshwater marsh, and wet prairie. They also determined the proposed project will directly impact 0.35 acres of wetlands, consisting of 0.09 acres of freshwater marsh and 0.26 acres of mangroves. Petitioners contend that the Applicant failed to account for all of the project’s wetland impacts, based on the wetland delineations made by their wetland expert, Andrew Woodruff. Most of the impacts that Mr. Woodruff believes were not accounted for are small, between 0.01 and 0.05 acres. The largest one is acres. The Applicant’s delineations are more reliable than Mr. Woodruff’s because the methodology employed by the Applicant had greater precision. It is more likely to be accurate. Petitioners argue that the 2013 exemption and the 2015 general permit did not authorize work in wetlands and, therefore, the impacts they cause must be evaluated in this ERP Modification. However, Petitioners did not prove that there are unaccounted-for wetland impacts associated with those authorizations. Any impacts associated with best management practices for erosion control, such as the installation of silt fences, would be temporary. The District does not include such temporary minor impacts in its direct, secondary, or cumulative impacts analyses. Most of the wetlands that would be directly impacted by the ERP Modification are degraded due to past hydrologic alterations and soil disturbances from the original construction and historical use of the FECR railway corridor, and infestation by exotic plant species. Most of these wetlands are also adjacent to disturbed uplands within or near the rail corridor. The functional values of most of the wetlands that would be affected have been reduced by these disturbances. The Applicant provided reasonable assurance that the project will not adversely impact the value of functions provided to fish and wildlife and listed species by wetlands and other surface waters. Secondary Impacts Section 10.2.7 of the Applicant’s Handbook requires an applicant to provide reasonable assurance that the secondary impacts from construction, alteration, and intended or reasonably expected uses of a proposed activity (a) will not cause or contribute to violations of water quality standards or adverse impacts to the functions of wetlands or other surface waters; (b) will not adversely impact the ecological value of uplands for bald eagles, and aquatic or wetland-dependent listed animal species for nesting or denning by these species; (c) will not cause impacts to significant historical or archaeological resources; and (d) additional phases for which plans have been submitted, and closely linked projects regulated under chapter 373, part IV, will not cause water quality violations or adverse impacts to the functions of wetlands or other surface waters. The proposed work will be entirely within the limits of the existing railway corridor where secondary impacts to wetlands and other surface waters caused by noise, vibration, fragmentation of habitats, and barriers to wildlife have existed for decades. The preponderance of the evidence shows that any increase in these kinds of impacts would be insignificant and would not reduce the current functions being provided. Because the affected wetlands are not preferred habitat for wetland-dependent, endangered, or threatened wildlife species, or species of special concern, and no such species were observed in the area, no adverse impacts to these species are expected to occur. Petitioners contend that adverse impacts will occur to the gopher tortoise, scrub jay, and prickly apple cactus. These are not aquatic or wetland-dependent species. However, the preponderance of the evidence shows any increase in impacts to these species would be insignificant. When the train bridges are closed, boats with masts or other components that make them too tall to pass under the train bridges must wait for the bridge to open before continuing. Petitioners contend that the current “stacking” of boats waiting for the bridges to open would worsen and would adversely impact seagrass beds and the West Indian Manatee. However, it was not shown that seagrass beds are in the areas where the boats are stacking. The available manatee mortality data does not show a link between boat stacking and boat collisions with manatees. Mr. Woodruff’s opinion about increased injuries to manatees caused by increased boat stacking was speculative and unpersuasive. The preponderance of the evidence shows that the adverse effects on both listed and non-listed wildlife species, caused by faster and more numerous trains would be insignificant. The activities associated with the 2013 exemption and the 2015 general permit for fiber optic cable were based on determinations that the activities would have minimal or insignificant adverse impacts on water resources. These determinations are not subject to challenge in this proceeding. The Applicant provided reasonable assurance that the secondary impacts of the project will not cause or contribute to violations of water quality standards, adversely impact the functions of wetlands or other surface waters, adversely impact the ecological value of uplands for use by listed animal species, or cause impacts to significant historical or archaeological resources. Elimination and Reduction of Impacts Under section 10.2.1.1 of the Applicant’s Handbook, if a proposed activity will result in adverse impacts to wetlands and other surface waters, the applicant for an ERP must implement practicable design modifications to eliminate or reduce the impacts, subject to certain exceptions that will be discussed below. Petitioners argue that this rule requires the Applicant and District to evaluate the practicability of alternative routes through the region, routes other than the existing railway corridor in Segment D09. As explained in the Conclusions of Law, that argument is rejected. The evaluation of project modifications to avoid impacts was appropriately confined to the railway corridor in Segment D09. The Applicant implemented practicable design modifications in the project area to reduce or eliminate impacts to wetlands and other surface waters. Those modifications included the shifting of track alignments, the elimination of certain third-track segments, and the elimination of some proposed access way modifications. However, the project qualified under both “opt out” criteria in section 10.2.1.2 of the Applicant’s Handbook so that design modifications to reduce or eliminate impacts were not required: (1) The ecological value of the functions provided by the area of wetland or surface water to be adversely affected is low, and the proposed mitigation will provide greater long-term ecological value; and (2) the applicant proposes mitigation that implements all or part of a plan that provides regional ecological value and provides greater long-term ecological value. Mitigation The Applicant proposes to mitigate for impacts to wetlands by purchasing mitigation credits from four District- approved mitigation banks: the Bluefield Ranch, Bear Point, Loxahatchee, and F.P.L. Everglades Mitigation Banks. Each is a regional off-site mitigation area which implements a detailed management plan and provides regional long-term ecological value. The number of mitigation credits needed to offset loss of function from impacts to wetlands was calculated using the Modified Wetland Rapid Assessment Procedure (“MWRAP”) or Wetland Assessment Technique for Environmental Review (“WATER”), as prescribed in the state permit for each mitigation bank. Applying these methods, the Applicant is required to purchase mitigation credits. The Applicant proposed to mitigate the adverse impacts to freshwater marsh wetlands by purchasing 0.01 freshwater herbaceous credits from the Bluefield Ranch Mitigation Bank, and 0.06 freshwater herbaceous credits from the Loxahatchee Mitigation Bank. The adverse impacts to tidal mangrove wetlands would be mitigated by purchasing 0.12 saltwater credits from the Bear Point Mitigation Bank, and 0.02 saltwater credits from the F.P.L. Everglades Mitigation Bank. The Applicant committed to purchase an additional 0.29 freshwater herbaceous credits from the Bluefield Ranch Mitigation Bank, for a total of 0.50 mitigation credits. The proposed mitigation implements a plan that will provide greater long-term ecological value than is provided by the wetlands that will be impacted. The Applicant proved by a preponderance of the evidence that the project complies with the District’s mitigation requirements. Cumulative Impacts To obtain an ERP, an applicant must provide reasonable assurance that a regulated activity will not result in unacceptable cumulative impacts to water resources. This assurance can be provided by proposing to fully mitigate the impacts within the same basin. However, when an applicant proposes mitigation in another drainage basin, the applicant must demonstrate that the regulated activity will not cause unacceptable cumulative impacts. The proposed project will adversely impact 0.02 acres of freshwater marsh wetlands and 0.21 acres of tidal mangrove wetlands in the St. Lucie River basin. The impacts to the freshwater marshes must be mitigated out-of-basin because there are no mitigation banks in the basin which offer freshwater herbaceous mitigation credits. The proposed project will adversely impact 0.07 acres of the freshwater marshes and 0.05 acres of the mangrove wetlands in the Loxahatchee River basin. Those impacts must also be mitigated out-of-basin because there are no mitigation banks in the Loxahatchee River basin. Because some of the Applicant’s proposed mitigation must be provided out-of-basin, the ERP application included a cumulative impact analysis. The analysis evaluated whether the proposed project, when considered in conjunction with other possible development within the St. Lucie River and Loxahatchee River drainage basins, would result in unacceptable cumulative impacts considering each basin as a whole. There are approximately 10,068 acres of freshwater marshes within the St. Lucie basin, of which an estimated 4,929 acres are not preserved and would be at risk of potential future development. The proposed project will adversely impact 0.02 of those acres, which is only 0.0004 percent of the total at-risk acreage. There are about 34,000 acres of freshwater marshes within the Loxahatchee River basin, of which an estimated 7,463 acres are at risk of future development, and approximately 564 acres of tidal mangrove wetlands, of which an estimated 75 acres are at risk of future development. The project will adversely impact 0.07 acres of the freshwater marshes (0.0009 percent), and 0.05 acres of the tidal mangrove wetlands (0.0667 percent). Petitioners contend the Applicant’s analysis did not account for impacts from proposed activities authorized in the 2013 and 2015 general permit. However, Petitioners failed to prove there are unaccounted-for wetland impacts. The preponderance of the evidence supports the District’s determination that the proposed project will not cause unacceptable cumulative impacts to wetlands and other surface waters. Public Interest When an applicant seeks authorization for a regulated activity in, on, or over wetlands or surface waters, it must provide reasonable assurance that the activity will not be contrary to the public interest, or if the activity is within or significantly degrades an OFW, is clearly in the public interest, as determined by balancing the following criteria set forth in section 373.414(1)(a): Whether the activities will adversely affect the public health, safety, or welfare or the property of others; Whether the activities will adversely affect the conservation of fish and wildlife, including endangered or threatened species, or their habitats; Whether the activities will adversely affect navigation or the flow of water or cause harmful erosion or shoaling; Whether the activities will adversely affect the fishing or recreational values or marine productivity in the vicinity of the activity; Whether the activities will be of a temporary or permanent nature; Whether the activities will adversely affect or will enhance significant historical and archaeological resources; and The current condition and relative value of functions being performed by areas affected by the proposed activities. The proposed work is not within an OFW, but entirely within the FECR corridor. The potential for overland flow and indirect impacts to OFWs is addressed by additional treatment of the stormwater prior to discharge. The proposed project would not significantly degrade an OFW. Therefore, the applicable inquiry is whether the project is contrary to the public interest. Factor 1: Public Safety, Safety, and Welfare Petitioners contend that the proposed project will adversely affect public health, safety, and welfare by impacting water quantity, water quality, and certain non-environmental matters such as emergency response times, traffic congestion, and potential train collisions with pedestrians and vehicles. Potential environmental impacts have been addressed above and, by a preponderance of the evidence, the District and the Applicant showed that such impacts would be insignificant or would be mitigated. As to the potential for non-environmental impacts associated with train operations, it is explained in the Conclusions of Law that the public interest test does not include consideration of non-environmental factors other than those expressly articulated in the statute, such as navigation and preservation of historical or archaeological resources. However, because evidence of non-environmental impacts was admitted at the final hearing, the issues raised by Petitioners will be briefly addressed below. The regulatory agency with specific responsibility for railroad safety is the Federal Railroad Administration (“FRA”). The FRA reviewed the safety features associated with the proposed passenger train operations, and approved them. Public safety will be enhanced at roadway crossings because of the proposed improvements and the use of modern technology in monitoring and managing the movement of trains. Petitioners contend that the addition of the passenger rail service will impede emergency response times in Martin County and St. Lucie County due to more frequent roadway closures. However, freight trains currently impede emergency response times due to their length and slow speed. The passenger trains will be much shorter in length and faster so that roadway crossing closures for passing passenger trains will be much shorter than for freight trains. The ERP Modification and 2017 Exemption do not affect freight train operations. The preponderance of the evidence shows that passenger rail service is unlikely to cause a material increase in the occurrence of circumstances where an emergency responder is impeded by a train. The current problem must be addressed through changes in freight train operations. Petitioners also contend that the passenger rail service will interfere with hurricane evacuation. The persuasive evidence does not support that contention. Train service would cease when a hurricane is approaching. Petitioners contend the trains will have to be “staged” on either side of the two moveable bridges while other trains cross, thereby blocking road intersections. However, this was a matter of speculation. The Applicant does not propose or want to stage trains at the bridges. Petitioners contend that the project will cause hazards to boaters on the St. Lucie River because there will be more times when the train bridge will be closed to allow the passage of passenger trains. Although there were many statistics presented about the number of boats affected, the evidence was largely anecdotal with respect to the current hazard associated with boaters waiting for the passage of freight trains and speculative as to the expected increase in the hazard if shorter and faster passenger trains are added. Factor 2: Conservation of Fish and Wildlife As previously found, the proposed activities will not adversely affect the conservation of fish and wildlife, including threatened or endangered species. The preponderance of the evidence shows the project will have only insignificant adverse impacts on water resources and wildlife. Factor 3: Navigation of the Flow of Water Petitioners claim the project will hinder navigation on the St. Lucie and Loxahatchee Rivers because of the increase in bridge closures if passenger trains are added. The U.S. Coast Guard is the agency with clear authority to regulate the opening and closing of moveable train bridges over navigable waters in the interests of navigation. Petitioners’ insistence that the District address the bridge openings is novel. No instance was identified by the parties where this District, any other water management district, or DEP has attempted through an ERP to dictate how frequently a railroad bridge must open to accommodate boat traffic. The Coast Guard is currently reviewing the project’s potential impacts on navigation and will make a determination about the operation of the moveable bridges. It has already made such a determination for the moveable bridge which crosses the New River in Ft. Lauderdale. Petitioners point to section 10.2.3.3 of the Applicant’s Handbook, which states that the District can consider an applicant’s Coast Guard permit, and suggest that this shows the District is not limited to what the Coast Guard has required. However, Section 10.2.3.3 explains the navigation criterion in terms of preventing encroachments into channels and improving channel markings, neither of which encompasses the regulation of train bridges. The preponderance of the evidence shows the project would not cause harmful erosion or shoaling or adversely affect the flow of water. Factor 4: Fishing, Recreational Values, and Marine Productivity The preponderance of the evidence shows that there would be no adverse impacts or only insignificant impacts to fishing or recreational values and marine productivity. Factor 5: Permanent Impact The proposed project will have both temporary and permanent impacts. The temporary impacts include the installation of silt fences and turbidity barriers designed to reduce water quality impacts and impacts to functions provided by wetlands and surface waters. The impacts due to track installation, construction and rehabilitation of the non-moveable bridges, at-grade crossing improvements, and stormwater system improvements are permanent in nature. The permanent impacts have been minimized and mitigated. Factor 6: Historical or Archaeological Resources Petitioners do not contend that the project will adversely affect significant historical or archaeological resources. Factor 7: Wetland Functions in Areas Affected Because the proposed work is within the limits of an existing railway corridor where impacts have been occurring for decades, and the majority of the wetlands to be affected are of a low to moderate quality, there would be only a small loss of functional values and that loss would be fully mitigated. Public Interest Summary When the seven public interest factors are considered and balanced, the proposed project is not contrary to the public interest. Even if Petitioners’ non-environmental issues are included, the project is not contrary to the public interest. Compliance With Other Permit Conditions The project is capable, based on accepted engineering and scientific principles, of performing and functioning as proposed. The Applicant demonstrated sufficient real property interests over the lands upon which project activities will be conducted. It obtained the required consent for proposed activities relating to bridge crossings over state-owned submerged lands. The Applicant provided reasonable assurance of compliance with all other applicable permit criteria. Exemption Verification for Roadway Crossings The Applicant’s ERP application included a mixture of activities which required an individual permit, as well as activities in roadway crossings which the Applicant claimed were exempt from permitting. Pursuant to section 5.5.3.4 of the Applicant’s Handbook, the Applicant requested a verification of exemption as to certain work to be done within 23 of those 24 roadway crossings. The District determined that the improvements for which an exemption was sought were exempt from permitting under rule 62-330.051(4)(c) for minor roadway safety construction, rule 62-330.051(4)(d) resurfacing of paved roads, and rule 62-330.051(10) for “construction, alteration, maintenance, removal or abandonment of recreational paths for pedestrians, bicycles, and golf carts.” The preponderance of the evidence shows the proposed work qualifies for exemption under these rules.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the South Florida Water Management District enter a final order that: approves Environmental Resource Permit Modification No. 13-05321-P on the terms and conditions set forth in the District’s Corrected Proposed Amended Staff Report of May 11, 2017; and approves the Verification of Exemption dated March 31, 2017. DONE AND ENTERED this 29th day of September, 2017, in Tallahassee, Leon County, Florida. S BRAM D. E. CANTER Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 29th day of September, 2017.
Findings Of Fact On December 12, 1991, Petitioner applied to the Respondent for a permit/water quality certification to grade and level, in stages, approximately 20,000 square feet or 0.45 acres of lake front to remove and prevent the formation of berms and depressions in the exposed lake bottom adjacent to his property. The project site is located at 3955 Placid View Drive which lies along the shoreline of Lake Placid, a natural waterbody in Highlands County, Section 24, Township 37 South, Range 29 East. Lake Placid is not an aquatic preserve, and is not an outstanding Florida water. It has been designated as a Class III waterbody. Petitioner's unsubdivided lot lies at the western end of Lake Placid. The shoreline measures approximately 203 feet. The western lot line also measures 203 feet, and fronts on Placid View Drive. The water level of Lake Placid has receded in recent years which allows large expanses of what was historically lake bottom to become beaches, lawns, and areas of habaceous marsh. The specific project which the Petitioner proposes calls for the leveling of the berms and depressions which form on the exposed lake bottom from collected water, which stagnates and permits various noxious creatures, including mosquitoes, to breed in them. The berms and depressions are approximately six inches high or deep and between one and three feet wide, and generally extend the length of the shoreline. The proposed area affected is approximately 20,000 square feet or 0.45 acres of lake front, although Petitioner proposes to actually level a much smaller area in stages of approximately 2,000 square feet on an "as needed" basis. No material other than sod in the beach area is proposed to be brought from or removed to off-site locations. Petitioner is highly sensitive to mosquito bites. The area proposed for leveling was previously cleared of vegetation without authorization. Very little revegetation of the shoreline has occurred since the area was cleared. Vegetation colonizing the beach, at present, includes pennyworts (Centella asiatica and Hydrocotyle umbellata) and water- hyssops (Bacopa sp.) Blue green algae was observed in the depressions which have formed along the shore since the clearing. Fauna observed on-site included gulls (Larus sp.), small fish in the adjacent lake shallows, and water-boatmen (Order Hemiptera) in the depressions. An area landward of the wetlands considered here was also cleared previously and is proposed to be seeded. An adjacent, uncleared shoreline was vegetated with primrose willow (Ludwigia sp.), cattail (Typha sp.), flat sedge (Cyperus odorata), and other wetland species for an almost 100% plant coverage. The Petitioner proposes to use a small tractor in leveling of the shore which will cause turbidity in the lake water. No turbidity controls were proposed by the Petitioner. Petitioner failed to provide reasonable assurances that the turbidity caused by the earthmoving equipment in areas presently above water would not cause degradation of water quality in Lake Placid; would not contribute to the long-term degradation of water quality in the lake caused by upland runoff that would flow into the lake without benefit of retention or filtration by shoreland vegetation (freshwater herbaceous habitat) which would be permanently removed under Petitioner's proposal. Nutrients such a nitrogen and phosphorus and pollutants such as pesticides, herbicides and other chemicals commonly used in lawn and garden care would be included in the runoff, and would have an adverse impact on fishing and marine productivity in the lake. The project would have a minor adverse impact on erosion and soil stabilization in the area surrounding the lake. Petitioner has failed to provide reasonable assurance that the proposed project is not contrary to the public interest. Petitioner can mitigate the project by eliminating the use of heavy equipment and substitute hand equipment to smooth out ruts, berms and depressions in jurisdictional areas.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Petitioner's application for Wetland Resource Regulation permit be DENIED. DONE and ENTERED this 8th day of March, 1993, in Tallahassee, Florida. DANIEL M. KILBRIDE Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings ths 8th day of March, 1993. COPIES FURNISHED: Francine M. Ffolkes, Esquire Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32399-2400 Mr. Vincent J. Woeppel 3955 Placid View Drive Lake Placid, Florida 33852 Daniel H. Thompson Department of Environmental Regulation Acting General Counsel Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32399-2400 Virginia B. Wetherell Secretary Department of Environmental Regulation Twin Towers Office Building 2600 Blair Stone Road Tallahassee, Florida 32399-2400
The Issue At issue in this proceeding is whether certain development orders issued by Monroe County to Homeowners, Ocean Reef Club and Key Largo Foundation (Applicants) for a project that would ultimately result in the construction of a flushing canal in the Ocean Reef Club development on north Key Largo are consistent with the Monroe County comprehensive plan and land development regulations.
Findings Of Fact The parties Petitioner, Department of Community Affairs (Department), is the state land planning agency charged with the responsibility of administering and enforcing the provisions of Chapter 380, Florida Statutes, and all rules promulgated thereunder. Section 380.031(18) and 380.032(1), Florida Statues. Respondent, Monroe County, is a local government within the Florida Keys area of Critical State Concern designated by Section 380.0552, Florida Statutes, and is responsible for the implementation of, and the issuance of development orders that are consistent with, the Monroe County comprehensive plan and land development regulations, as approved and adopted in Chapters 9J-14 and 28-20, Florida Administrative Code. Respondents, Homeowners, Ocean Reef Club and Key Largo Foundation (Applicants), are the owners of real property in the Ocean Reef and Harbour Course subdivisions, Key Largo, Monroe County, Florida; properties that are located within that part of Monroe County designated as an area of Critical State Concern. The Applicants have sought the development orders (permits) at issue in this proceeding incident to their 8-year quest to achieve regulatory approval to initiate a project that would restore the water quality of Dispatch Creek to Class III water standards. Background The site of the proposed project, the present terminus of Dispatch Creek, is located within the Ocean Reef Club development on north Key Largo. That development is bordered on the east by the Atlantic Ocean and John Pennekamp Coral Reef State Park, on the north by Biscayne National Park, and on the west by the Biscayne Bay/Card Sound Aquatic Preserve. Currently, the development at the Ocean Reef Club includes a number of canals and boat basins, an airstrip; three 18-hole golf courses, a 174-slip marina capable of docking vessels in excess of 100 feet, and extensive residential and-commercial uses. In the mid-1970's, Dispatch Creek was a natural, albeit shallow, waterbody that was able to maintain, through natural tidal actions, water quality standards. However, in 1977 Ocean Reef Club, under permits issued by the Department of Environmental Regulation (DER) in the mid-1970's excavated the creek to new depths to create a navigable channel and extended its length beyond its natural contours. When completed, the creek was converted from a natural waterbody, that could maintain water quality standards through natural tidal action, into a dead-end system, that could not maintain such standards through natural processes along the course of its extended terminus. 1/ Over time, the water quality of Dispatch Creek from its approximate midpoint to its dead-end terminus has steadily declined. The cause of this decline is reasonably attributable to the biochemical oxygen demand placed on the creek by the continuous input of detritus from mangroves, which boarder the creek on the east and to a lesser extent on the west, and the length of the channel, coupled with the dead-end basin surrounding an island, which has assured the continued decline of water quality due to poor water circulation. As a consequence, the creek, as a habitat, has been altered from an oxygen rich system supportive of aerobic life to an oxygen poor system supportive of anaerobic life. This has evidenced itself through algae blooms, the intermittent emission of hydrogen sulfide gas, and a change in water clarity to that of a "coffee au lait" color. Currently, a significant portion of Dispatch Creek is devoid of aerobic life, and unless its condition is reversed it could not support aerobic marine organisms in the future. /2 Today, conditions in portions of Dispatch Creek fail to meet DER standards. DER regulations establish the dissolved oxygen (DO) standard to be not less than five milligrams per liter in a 24-hour period, and never less that four milligrams per liter. The DO Standard is currently violated in Dispatch Creek beginning at the mid point of the creek to its terminus. At its terminus, DO levels are chronically below one milligram per liter. Additionally, DER nutrient standards prohibit the alteration of nutrient concentrations of a body of water so as to cause an imbalance in natural populations of aquatic flora or fauna. Here, the high nutrient levels of Dispatch Creek resulting from the mangrove detritus and lack of circulation has, as heretofore noted, caused the natural aquatic flora and fauna to be replaced by anaerobic life. As a consequence of the changes in water quality that had occurred in Dispatch Creeks the Applicants have, over the course of the past eight years, sought approval from various regulatory authorities, including DER and Monroe County, of a plan to improve the water quality in Dispatch Creek. Such approval has been garnered from DER, and Monroe County's approval is at issue in this proceeding. The DER permit On February 7, 1986, the Applicants received approval from DER for a permit to construct a flushing canal from the terminus of Dispatch Creek to the Atlantic Ocean. That permit authorized the Applicants: To construct a "flushing canal" between the dead end of Dispatch Creek Waterway and the Atlantic Ocean by: excavating approximately 13,000 cubic yards to create a canal approximately 3000 ft. long by 20 ft. wide with a bottom elevation of 6 ft. Mean Low Water; placing three 6 ft. by 6 ft. by 380 ft. box culverts in the canal alignment at the basin end; placing tidal actuated flap gates on the basin end of the culverts in a manner which will allow the basin to intake water from the flushing canal on incoming tides while preventing discharge into the flushing canal on outgoing tides; placing 5 pilings across the canal at it's juncture with the Atlantic Ocean to prevent navigation in the canal; and creating a 12,900 sq. ft. mangrove mitigation area by excavating approximately 1,450 cu. yds. from a spoil area to create an area with an elevation of +1.4 Ft. NGVD which will be planted with red mangroves. DER was, in evaluating the application pending before it, charged with the duty to apply, enter alia, the criteria of the 1984 Warren Henderson Wetlands Act, Section 403.918(2), Florida Statutes, as well as Chapters 17-3 and 17-4, Florida Administrative Code. Based on DER's decision to issue its permit, it is reasonable to conclude that DER, within its permitting jurisdiction, concluded that construction of the proposed circulation channel would not lower ambient water quality, and would not significantly degrade Outstanding Florida Waters (OFW), including those of John Pennekamp Coral Reef State Park. As heretofore noted, the Department does not contend that the subject project will violate any specific criteria within DER's Chapter 403, Florida Statutes, permitting jurisdiction. The Monroe County permits On July 19, 1989, Monroe County issued to the Applicants the building permit, excavation permit, and land clearing permit (development orders), each numbered 8930001680, at issue in these proceedings. As permitted, the project proposed by the Applicants is designed to improve the water quality of Dispatch Creek, particularly in the vicinity of its dead-end terminus, and consists of two phases. Phase I contemplates the installation and operation of an aeration system for at least one year, which will extend from the dead-end terminus of Dispatch Creek toward its midpoint, as well as a water quality monitoring program, until such time as the water quality of the entire creek comports with that of adjacent Class III waters. Should the Applicants be successful in Phase I, they would then be authorized to proceed with Phase II, which would allow the construction of the flushing canal contemplated by the DER permit. As approved by Monroe County, Phase I would consist of the installation of an aeration system around the island, located at the terminus of Dispatch Creek, and in the canal, as well as the suction dredging of loose sediments in the upper reaches of Dispatch Creek. The system would consist of fifteen microporus diffuser/aerators producing approximately 5 CFM per unit, and would be anchored near the bottom to maximize the introduction of dissolved oxygen into the anaerobic water and to optimize water movement. Operation of such system, coupled with the introduction of aerobic bacteria, will shortly reduce the concentration of hydrogen sulfide dissolved in the water, reduce the concentration of ionized sulfides in solution, retard the growth and propagation of anaerobics in the benthic layer, and activate the growth and propagation of aerobics in all strata. As a consequence, over time, water clarity will improve, which will allow the penetration of sunlight into the benthos. This illumination will spawn the growth of photosynthetic bacteria, as well as phytoplankton, which will aid in the continued aerobic cleansing of the water and bottom sediments. In all, installation and operation of the aeration system, which has proven successful at other locations, should, over time, restore the waters of Dispatch Creek to Class III standards, without any adverse impacts to adjacent waters or the park. While operation of the aeration system will, over time, restore the waters of Dispatch Creek to Class III standards, the perpetual maintenance of such system would be energy intensive and expensive. for this reason, the Applicants have proposed the Phase II canal, which would maintain, through natural tidal processes, water quality standards within the creek. The canal permitted by Monroe County under Phase II is consistent in all respects with the DER permit except the Monroe County permits require that the canal be sited 20 feet landward of the alignment permitted-by DER into previously scarified uplands. So aligned, the canal would begin at the landward terminus of Dispatch Creeks run easterly within the rear lot lines of at least 15 lots within Harbour Course South subdivision, a platted subdivision, pass through a fringe of red and black mangroves fronting the ocean, and terminate approximately 100 feet seaward of the mean high water line (MHWL) within the boundaries of John Pennekamp State Park. At the point where the canal would join with Dispatch Creek, three 6 foot by 6 foot by 380 foot box culverts would!! be installed with one-way tidal activated flap gates, which would permit waters from the Atlantic to enter Dispatch Creek on a rising tide, but would preclude an exchange of waters from Dispatch Creek on a falling tide. Through such design, sufficient mix and force will be exerted within the waters of Dispatch Creek to maintain Class III water quality standards by natural circulation, and to return the habitat offered by the creek to an oxygen rich system capable of supporting aerobic life. While construction of the canal would be beneficial, by restoring the waters: of Dispatch Creek to Class III standards, it is not without cost to the environment. As aligned, the canal, although predominately within previously cleared or scarified uplands, will require excavation through several types of habitat that are either undisturbed or reestablished, including undisturbed buttonwood association, salt marsh, hardwood hammock, transitional habitat, mangroves and submerged lands, and will require the removal of approximately one-tenth of an acre of red and black mangroves, a species of special concern, as well as a number of mahogany trees, twisted air plants, prickly pear cactus and barpar cactus, which are threatened species. Its construction would likewise sever the uplands from the adjacent transitional and wetland areas that traditionally buffer, insulate and protect nearshore waters from runoff from upland areas. Construction of the canal should not, however, adversely impact any threatened or endangered animal species since the proposed alignment is currently a poor habitat for threatened or endangered species, such as the Key Largo woodrat, that may reside in the area, and there is currently no threatened or endangered animal species inhabiting the site. This is not, however, to suggest that the site would not support such species in the future, provided that existing habitat is permitted to continue its progress towards reestablishment. To mitigate the loss of habitat types, the Monroe County permit provides: The agreed mitigation for the loss of all rare and/or endangered habitat types located within the area impacted by the dredging shall be carried out prior to initiation of the dredge project. This shall be based on existing vegetation surveys and an assessment of species currently located within the confines of the project area. Prior to initiation of any dredge activity, a formal inventory of the project site shall be made and a one-to-one replacement program (baked on species rarity or level of endangerment) shall be established and agreed upon. Such an agreement will include defining an appropriate site and the number and type of trees, as well as a maintenance plan for the agreed upon area. Additionally, the DER permit addresses the loss of mangroves, by requiring the establishment of a 12,900 square foot mangrove mitigation area. Under the facts of this case, the mitigation proposed would, assuming the propriety of such development under the Monroe County comprehensive plan and land development regulations, address the loss of habitat types occasioned by development of the proposed canal. To assure that water quality within Dispatch Creek comports with Class III standards before the canal is dug, and that the creek maintains such standards following construction, the Monroe County permits establish a water quality monitoring program. During the first year, samples will be taken and tests performed on a weekly basis for pH, DO, turbidity, Secchi Disc, temperature, and sulfite; on a biweekly basis for total bacterial count and composition; on a monthly basis for total nitrogen and phosphate; on a quarterly basis for: macro-invertebrates and macrophytes; and on a semiannual basis for heavy metals and pesticides. During the second yearn biweekly testing will be done for DO, temperature, hydrogen sulfide, turbidity and Secchi Disc; quarterly testing for total nitrogen and phosphate, macro- invertebrates, and macrophytes; and, annual testing for heavy metals and pesticides. After the second year, monthly tests will be done for DO, temperature, hydrogen sulfide, turbidity, and Secci Disc; quarterly tests for total nitrogen and phosphate, as well as macro- invertebrates; and annual tests for heavy metals and pesticides. Should the water quality of the creek fail to maintain Class III standards following construction of the canal, the Monroe County permit contains the following special condition: The water quality monitoring program shall be maintained to assess the quality of water in Dispatch Creek subsequent to the dredge project completion. If at any time the water quality fails to meet the standards established by this permit, the one way flushing valve shall be closed by the applicant, and in applicant's failure to do so, by the County. The applicant assumes all costs of closing said valve, whether closed by applicant or the County. Aeration, aid/or other means at the discretion of the applicant, shall be utilized to reestablish quality. The valve shall not be reopened until the water quality standard is met. The purpose of the foregoing condition, as well as the requirement that the waters of Dispatch Creek meet Class III standards before the canal can be dug, is to assure that operation of the canal will not lower ambient water quality within the Outstanding Florida Waters of John Pennekamp Coral Reef State Park, and thereby protect the park from any adverse impacts associated with the improved circulation of the creek. John Pennekamp Coral Reef State Park is a unique and world-renowned resource, attracting millions of visitors each year. At least fifty percent of the activities engaged in by visitors to the park are water-related, including fishing, observational diving and boating. Any degradation of the ambient quality of those waters would be contrary to DER's rules promulgated under Chapter 403, Florida Statutes, and could adversely impact the natural biota of the park, with a corresponding reduction in the number of visitors to the park and revenues contributed by those visitors to the local economy. Here, the proof demonstrates, consistent with DER's prior permitting, that the subject project, built as proposed, would not lower the ambient water quality of adjacent waters through the discharge of pollutants, and therefore would not adversely affect the park. If anything, the Monroe County permits, with one exception to be discussed infra, offer stronger assurances than the DER permit that adverse impacts will not occur. Notably, under such permits the Applicants must first bring the water quality of the Creek up to Class III standards before the canal can be dug. If the Applicants are ssuccessful at that phase of the project, there will not be excessive nutrient loading within the creek, and the detritus that may thereafter be removed from the creek by improved circulation would not adversely affect water quality or the park. Currently, there are no heavy metals in the sediments or water column of the creek which are at levels above those found naturally, and no pesticides or toxic organics. In sum, there is no basis to conclude, based on the record, that-there is any substance within the waters or sediments of Dispatch Creek that would, upon the waters achieving Class III standards, lower the amient quality of adjacent waters or adversely impact the park. /4 Ostensibly, as an added measure of protection to adjacent waters, the Monroe County permits contain a condition, with which the Applicants concur, that should the waters of Dispatch Creek fail to maintain Class III standards following construction of the canal, the one-way tidal actuated flap gates will be closed. That condition, a noted supra, provides: If at any time the water quality [of the creek] fails to meet the standards established by this permit, the one way flushing valve shall be closed by the applicant, and in the applicant's failure to do so, by the County. The applicant assumes all costs of closing by applicant or the County. Aeration, and/or other means at the discretion of the applicant, shall be utilized to reestablish quality. The valve shall not be reopened until the water quality standards is met. The foregoing condition presumes to address the possibility that should the proposed project fail to function as expected by the experts, as did the current Dispatch Creek fail to function as expected, that such failure will no result in an adverse impact to adjacent waters or the park. In this regard, it is worthy of note that DER's approval of the extension of Dispatch Creek to create a 7,200 foot dead-end canal in the mid-flush the pollutants from the canal into the park. The Applicants presented persuasive testimony, however, through their 1970's was, based on current knowledge, an error, and that today no dead-end system would be approved in excess of soon feet. Monroe County's condition, while preventing the discharge of degraded waters from Dispatch Creek to the park upon closure of the one way flushing valves, fails to address, however, the adverse impacts that could result from its closure. By closure of the valves, the flushing canal would be instantly converted into a 3,000-foot dead-end canal, and would suffer the same water quality problems as similar systems, with probable adverse effects to adjacent waters and the park. Accordingly, so as not to compound the existing error occasion by the extension of Dispatch Creek in the mid-1970's, prudence would dictate a proviso that, if the valves are shut, appropriate monitoring will occur within the waters of the flushing canal to detect any significant degradation of water quality, and that should such degradation pose a threat to adjacent waters or the park, that the Applicants be required, at their expense, to restore promptly the water quality within the flushing canal to Class III standards or restore the area to its present condition. Consistency of the proposed project with the Monroe County comprehensive plan and land development regulations Lack of plat approval As heretofore noted, the proposed canal would begin at the landward terminus of Dispatch Creek and run easterly within the rear lot lines of at least 15 lots in Harbour Course South subdivision, a platted subdivision, before it passed through fringing mangroves and terminated in the Atlantic Ocean. Currently, the final recorded plats of Harbour Course South subdivision do not reflect the proposed canal, as mandated by Section 177.091(15), Florida Statutes, and the Applicants have not sought to amend the plat to include the proposed canal. Pertinent to this case, the Monroe County Code (MCC), the land development regulations, /5 provides: Sec. 9.5-1. Purpose. It is the purpose of this chapter, the Land Development Regulations, to establish the standards, regulations, and procedures for review and approval of all proposed development of property in unincorporated Monroe County, and to provide a development review process what will be comprehensive, consistent and efficient in the implementation of the goals, policies and standards of the comprehensive plan . . . Sec. 9.5-2. Applicability. General Applicability: The provisions of this chapter shall apply to all land in unincorporated Monroe County. All development of whatever type and character, whether permitted as of right or as a conditional use, shall comply with the development standards and the environmental design criteria set forth in article VII hereof. No development shall be undertaken without prior approval and issuance of a development permit under the provisions of this chapter and other applicable laws and regulations. Sec. 9.5-81. Plat approval and recording required. * * * No building permit, 6/ except for single family detached dwellings and accessory uses thereto, shall be issued for the construction of any building, structure or improvement unless a final plat has been approved in accordance with the provisions of this division and recorded for the lot on which the construction is proposed. * * * (e) If a plat has been previously approved and recorded, technical or minor changes to the plat may be approved by the director of planning. All other changes shall be considered in accordance with the provisions of this Division. Sec. 9.5-94. Amendment of a recorded final plat. An amendment of a recorded final plat or portion thereof shall be accomplished in the same manner as for approval of the plat. Here, the subject permits were issued contrary to the foregoing provisions of the MCC because there was no final plat of record approving the canal as to each affected lot. While the Applicants offered proof, if credited, that the existing plat could be amended to include the canal as a "minor change" upon approval of the Director of Planning, it is noteworthy that no such approval has been obtained. More importantly, it is found that a change in the existing plat to include the canal would not constitute a "technical or minor change," and that formal amendment of the plat would be required. 7/ The provision of the MCC dealing with plat approval, provide a comprehensive scheme to assure, among other things, than the proposed plat is consistent with the purposes, goals and objectives of the comprehensive plan, the development regulations, and state laws, as well as affording an opportunity for public input. Of import here, the MCCs provide: Sec. 9.5-82. General Standards for Plat Approval. No preliminary or final plat shall be approved unless the plat is consistant with the purposes, goals and objectives of this plan, this chapter, applicable provisions of state law, the provisions governing the development of land set forth in article VII, and the procedures set forth in this article. Sec. 9.5-83. Preliminary Plat Approval. Generally. All applicants for approval of a plat involving five (5) or more lots shall submit a preliminary plat for approval in accordance with the provisions of this section. Application. An application for preliminary approval shall be submitted to the development review coordinator in accordance with the provisions of this section, accompanied by a nonrefundable fee as established from time to time by the board of county commissioners. The application shall contain the information required on a form provided by the director of planning. Staff Review. After a determination that the application for preliminary plat approval is complete under the provisions of section 9.5-44, the development review coordinator shall submit the application to the development review committee, which shall prepare a recommendation and report for the commission. Public Hearing and Action by the Planning Commission. The planning commission shall conduct a public hearing on an application for preliminary plat approval of a subdivision involving five (5) or more lots, in accordance with the requirements of sections 9.5-46 and 9.5-47. The commission shall review such applications, the recommendation of the development review committee, and the testimony at the public hearing, and shall recommend granting preliminary plat approval, granting approval subject to specified conditions, or denying the application at its next meeting following submittal of the report and recommendation of the development review committee. Effect of Approval of Preliminary Plat. Approval of a preliminary plat shall not constitute approval of a final plat or permission to proceed with development. Such approval shall constitute only authorization to proceed with the preparation of such documents as are required by the director of planning for a final plat. Sec. 9.5-84. Final Plat Approval. Generally. All applicants for approval of a plat shall submit a final plat for approval in accordance With the provisions of this section. Application. It shall be the responsibility of the developer to complete, have in final form, and submit to the development review coordinator for final processing the final plat, along with all final construction plans, required documents, exhibits, legal instruments to guarantee performance, certificates properly executed by all required agencies and parties as required in this article, and the recording fee, and any other documents or information as are required by the director of planning. After receipt of a complete application for final plat approval, as determined in accordance with section 9.5-44, development review coordinator shall submit the application and accompanying documents to the development review committee. Review and action by Development Review Committee. The development review committee shall review all applications for final plat approval. b. For a final plat for subdivision involving five (5) or more lots, if the plat conforms to the approved preliminary plate and the substantive and procedural requirements of this chapter, at its next regular meeting or as soon as practical after receipt of a complete application, the development reviews committee shall recommend to the planning commission approval of the final plat or approval with conditions. If the committee finds that the plant does not substantially conform to the approved preliminary plat or the substantive and procedural requirements of these regulations, the committee shall recommend denial, specifying the area(s) of nonconformity. Review and Action by the Planning Commission. The planning commission shall review all applications far final plat approval involving five (5) or more lots and the recommendation of the development review committee. If the commission finds that the final plat conforms to the approved preliminary plat and the substantive and procedural requirements of this chapter, the commission shall recommend to the board of county commissioners approval of the final plat, or approval with specified conditions, and shall submit a report and written findings in accordance with section 9.5-47. Public Hearing by the Board of Country Commissioners. The board off county commissioners shall conduct a public hearing on all applications for final plat approval involving five (5) or more lots in accordance with the procedures of section 9.5-46C. Action by the Board of County Commissioners. For proposed subdivisions involving five (5) or more lots the board of county commissioners shall review the application, the recommendations of the development review committee and the planning commission, and the testimony at the public hearing, and shall grant final plat approval, grant approval subject to specified conditions, or deny the application, in accordance with the provisions of section 9.5-47. Sec. 9.5-90.Maintenance of Private Improvements. If any plat of subdivision contains streets, easements, or other improvements to be retained for private use, the final plat for recordation shall indicate to the satisfaction of the director of planning and the county attorney the method or entity by which maintenance of the private improvements shall be performed. As a consequence of Monroe County's failure to comply with the provisions of its regulations which require final plat approval before a building permit may be issued, there has been no review by the Development Review Committee, no public hearing conducted by the Planning Commission, no recommendation of the Planning Commission, and no public hearing before the County Commissioners on the propriety of amending the subject plat to permit the proposed construction, or a resolution, through the plat approval process, as to whether the proposed canal is consistent with, inter alia, the purposes, goals, and objectives of the Monroe County comprehensive plan, as mandated by section 9.5-82(a), MCC. As importantly, where, as here, the proposed canal is to be retained for private use, there is no indication on the recorded plat, 4s required by MCC 9.5-90, of the method or entity by which maintenance of the canal shall be performed. Notably, the property through which the canal will be constructed is not owned by any of the Applicants but, rather, by Driscoll Properties , with whom the Applicants state they have an agreement to permit construction. 8/ Open space requirements and environmental design criteria Pertinent to this case, the MCC further provides: Sec. 9.5-3. Rules of construction. In the construction of the language of this chapter, the rules set out in this section shall be observed unless such construction would be inconsistent with the manifest intent of the board of commissioners as expressed in the Monroe County Comprehensive Plan or an element or portion thereof, adopted pursuant to chapters 163 and 380, Florida Statutes (1985). The rules of construction and definitions set out herein shall not be applied to any section of these regulations which shall contain any express provisions excluding such construction, or where the subject matter or context of such section is repugnant thereto. (a) Generally: All provisions, term , phrases and expressions contained in this chapter shall be liberally construed in order that the true intent and meaning of the board of county commissioners may be fully carried out. Terms used in this chapter, unless otherwise specially provided, shall have the meanings prescribed by the statutes of this state for the same terms. In the interpretation and application of any provision of this chapter, it shall be held to be the minimum requirement adopted for the promotion of the public health, safety, comfort, convenience and general welfare. Where any provision of this chapter imposes greater restrictions upon the subject matter than a general provision imposed by the Monroe County Code or another provision of this chapter, the provision imposing the greater restriction or regulation shall be deemed to be controlling . . (Emphasis added) Sec. 9-804 (MCLDR) Open space requirements. No land shall be developed, used or occupied such that the amount of open space on the parcel proposed for development is less than the following ratios, nor shall open space be cleared or otherwise disturbed including ground cover, understory, mid-story, and canopy vegetation. All such required areas shall be maintained in their natural condition. The amount of open space required on any parcel for development shall be determined according to each land type and no development activity within any individual land type shall exceed the open space ratio for that land type. Land Type on Existing Open Space Conditions Map Ratio Open Waters 1.00 Mangrove and Freshwater 1.00 Wetlands Salt Marsh and Buttonwood .80 Associations .85 High Hammock (High Quality) .80 High Hammock (Moderate Quality) .60 High Hammock (Low Quality) . 4 Low Hammock (High Quality) .80 Low Hammock (Moderate Quality) .60 Low Hammock (Low Quality) . 4 Palm Hammock .90 Cactus Hammock .90 Pinelands (High Quality) .80 Pinelands (Low Quality) .60 Beach Berm .90 Disturbed . 2 Disturbed with Hammock . 2 Disturbed with Salt Marsh and Buttonwood . 2 Disturbed Beach/Berm . 2 Disturbed with Exotics . 2 Disturbed with Slash Pines . 2 Offshore Islands . 9 (Emphasis added) Sec. 9.5-345. Environmental design criteria. No land, as designated on the existing conditions map and analyzed in accordance with the standards in sections 9.5-339 and 9.5-340, shall be developed, used ~re occupied except in accordance with the following criteria unless the county biologist recommends an authorized deviation from the following criteria in order to better serve the purpose and objectives of the plan and the director of planning or planning commission approves the recommendation as a minor or major conditional use. No recommendation for an authorized deviation from these environmental design criteria shall be made unless the county biologist makes written findings of fact and conclusions of biological opinion which substantiate the need and/or benefits to be derived from the authorized deviation. (m) Mangroves and Submerged Lands: Except as provided in subsection (3), only piers, docks, utility pilings and walkways shall be permitted on submerged lands and mangroves; All structures on any submerged lands and mangroves shall be designed, located and constructed such that: All structures shall be constructed on pilings or other supports; Bulkheads and seawall shall be permitted only to stabilize disturbed shorelines or to replace deteriorated existing bulkheads and seawalls; No structure shall be located on submerged land which is vegetated with sea grasses except as is necessary to reach waters at least four (4) feet below mean low level for docking facilities. (Emphasis added) From the foregoing regulations it is apparent that Monroe County has accorded mangroves the highest of protections. The regulations mandate a 100 percent open space ratio in such areas, and preclude any clearing or other disturbance of such areas. The only exception provided by the regulators, absent approval of an application for a minor or major conditional use, is for the construction of piers, docks, utility pilings and walkways, and then only when such structures are constructed on pilings or other supports to minimize their impact. Here, the proposed development, "permitted as of right" and not as a minor or major conditional use, fails to comply with the Monroe County land development regulations because it will result in the elimination of an existing mangrove community. In addition to the environmental design criteria established for mangroves by section 9.5-345, discussed supra, that section likewise establishes-specific performance standards for the development of any parcel (lot) depending on the habitat type, and where mixed habitat is encountered, requires that development occur on the least sensitive portions of the parcel. Here, while the Applicants did address the habitat types encountered along the canal alignment, the record fails to address the habitat types encountered on each of the platted lots through which the canal will run. Consequently, the Applicants failed to demonstrate that development of those lots, by construction of a canal within their rear boundary, would be consistent with the open space ratios mandated by section 9-804, MCLDR, or the environmental design criteria mandated by section 9.5-345, MCC. C. The Monroe County land development regulations further and implement the Monroe County comprehensive plan. The foregoing land development regulations were adopted by Monroe County, as well as approved by the Department and adopted by the Administrations Commission, to further and implement the standards, objectives and policies of the Monroe County comprehensive plan. That plan evidences a strong commitment to the protection, maintenance, and improvement of the Florida Keys environment. In this regard, the comprehensive plan provides: Sec. 2-104. Nearshore Waters The Florida Keys are dependent nearshore water quality for their environmental and economic integrity. The heart of the Florida Keys economy, the means by which Monroe County exists as a civil and social institution, is based on its unique, oceanic character. If nearshore water quality is not maintained, then the quality of life and the economy of Monroe County will be directly and immediately impacted. OBJECTIVES 1. To protect, maintain and, where appropriate, improve the quality of nearshore waters in Monroe County. POLICIES 1. To prohibit land uses that directly or indirectly degrade nearshore water quality. To prohibit the development of water dependent facilities, including marinas, at locations that would involve significant of the biological character of submerged lands. To limit the location of water- dependent facilities at locations that will not have a significant adverse impact on offshore resources of particular importance. For the purposes of this policy, offshore resources of particular importance shall mean hard coral bottoms, habitats of state or federal threatened and endangered species, shallow water areas with natural marine communities with depths at mean low tide of legs than four (4) feet, and all designated Aquatic Preserves under Ch. 258.39 et seq. the Florida Statutes. To limit the location of docking facilities to areas which have adequate circulation and tidal flushing. To protect wetland and transitional areas that serve to buffer, insulate and protect nearshore waters from run- off from upland areas. To prohibit the discharge of any pollutant directly or indirectly into nearshore waters. For the purposes of this policy, indirect discharge into nearshore waters shall include surface runoff, surface spreading or well injection of any effluent that does not meet state or federal standards for point and non-point discharges. To monitor nearshore water quality to ensure that growth and envelopment is not degrading nearshore water quality. To encourage the rehabilitation of canals and other water bodies where water quality has deteriorated. Sec. 2-105. Wetlands and Associated Systems Wetlands are an essential element of the Florida Keys and they play several vital roles. Wetlands serve as principal habitats for a wide variety of plants and animals, including juvenile forms of several commercially-exploited species of seafood. In addition, wetland plants play an important role in pollution control through nutrient uptake, and in primary production control through nutrient uptake, and in primary production for food webs. Wetland plants also serve as important natural buffers to the onslaught of storm-driven winds and water. OBJECTIVE To protect and maintain the functional integrity of wetlands and associated transitional areas within the Florida Keys. POLICIES To prohibit the destruction, disturbance or modification of any wetland or associated transition area, except where it can be demonstrated that the functional integrity of a wetland or associated transitional area will not be significantly adversely affected by such disturbance or modification. Marine Resources The great value attributed to Monroe County's marine resources is due to their crucial role in the local economy, and in providing a wide range of natural amenities and services. Health and integrity of the marine system is a fundamental prerequisite if these resources are to continue to provide social, economic, and environmental benefits that we have at times taken for granted. Mangroves, seagrasses, and coral reefs, all of which are susceptible to pollution and dredging, are extremely important in providing food and shelter for myriad forms of marine life, providing storm protection, and maintaining water quality. If uses and activities such as dredge and fill, destruction of natural vegetation, use of pesticides and fertilizers, improper sewage and solid waste disposal continue indiscriminately and uncontrolled; the ability of the marine system to function effectively will deteriorate, thereby resulting in the loss of many natural services and socioeconomic benefits to society. Therefore, it is imperative that such uses and activities be carefully regulated so as to insure conservation and protection of resources and long-term maintenance of their productivity. Marine Resources Management Policies Recognizing the crucial role that the marine environment plays in the economy, the protection, conservation, and management of marine resources will be viewed as an issue requiring the County's utmost attention. In an effort to protect and conserve marine resources, emphasis will be placed on protecting the entire marine ecosystem. To this end, maintenance of water quality; protection of marine flora and fauna, including shoreline vegetation; and preservation of coral reefs will be regarded as being absolutely essential to maintaining the integrity of the marine system. * * * Land and water activities which are incompatible with the preservation of marine resources because of their potential adverse effects will be prohibited, restricted, or carefully regulated depending upon the nature of activity and the extent of potential impact. * * * 3.2. Dredging and/or filling associated with maintenance or necessary water- dependent public projects shall be minimized and carefully managed to prevent unnecessary adverse environmental impact. The County will develop and enforce stringent development regulations to minimize water pollution from point and non-point sources in an effort to: improve and maintain quality of coastal waters. . Marine grass beds, mangrove communities, and associated shoreline vegetation will be preserved to the fullest extent possible. Removal of vegetation or modification of natural patters of tidal flow and nutrient input, cycling and export should be considered only in the case of overriding public interest. The County will encourage creation and restoration of marine grass beds, and mangrove communities in areas which could support such growth and could potentially enhance the environmental quality. As far as possible, natural patterns of gradual and dispersed runoff will be maintained. Land and water activity in the vicinity of stress areas (coral, grass bed, and inshore water quality) as identified and illustrated in the Florida Keys Coastal Zone Management Study and as may be discovered during any future study will be carefully controlled and regulated in an effort to arrest further deterioration. Research and study directed toward alleviating the stresses and restoring their condition to natural healthy state will be encouraged arid supported. Marine Resources Areas of Particular Concern Site-specific Designations Lignumvitae Key Aquatic Preserve. * * * Management Policies: B. Development activity on Upper and Lower Matecumbe Keys, including dredging and filling will be prohibited so as not to degrade the waters of the Preserve. * * * 3. John Pennekamp Coral Reef State Park and Key Largo Coral Reef Marine Sanctuary. Management Policies: * * * B. Development activity on Key Largo, including dredging and filling, urban runoff water, and the use of septic tanks will be controlled and regulated in order to minimize stresses which result in cater quality deterioration. Generic Designations All marine grass beds in waters off the Florida Keys. All patch reef coral and other reef formations found in the surrounding waters off the Keys. All shore-fringing mangrove and associated vegetation extending up to 50 feet laterally upland from the landward limit of the shoreline mangrove. Management Policies A. These biotic communities will be preserved to the fullest extent possible. Natural Vegetative Resources The diverse and often unique plant associations of the Florida Keys are a vital element of Monroe County's natural system and economic structure. The natural functions performed by these plant communities with1 regard to marine resources, unique and endangered wildlife, shoreline stabilization, filtering of urban runoff and scenic value make them vital elements in maintainance of the urban structure and attractions for the tourist base of Monroe County's economy. Natural Vegetation Management Policies In recognizing the need to preserve as much natural vegetation as possible, the County will direct its land use and development regulations; to minimize destruction of natural vegetation and modification of landscape. Guidelines and performance standards designed to protect natural vegetation from development will be developed and enforced. Clearing of native vegetation for development will be controlled. 3. Regulations controlling development in areas characterized primarily by wetland vegetative species such as mangrove and associated vegetation will emphasize preservation of natural vegetation to the maximum degree possible. 8. The existing County ordinances designed to protect and conserve natural vegetation will be strictly interpreted, rigidly enforced, and/or amended when necessary. Consistent with the Monroe County comprehensive plan, the Monroe County land development regulations further the standards, policies and objectives of the plan to protect, maintain and improve the Florida Keys environment. In this regard, the provisions of the regulations requiring final plat approval before a development order may issued provide assurance that the proposed activity will be -consistent with the comprehensive plan, the land development regulations, and applicable provisions of state law. Likewise, pertinent to this case, the provisions of section 9-864, MCLDR, regarding open space requirements, and section 9.5-345, regarding environmental design criteria, further the plan's policy to minimize the destruction of natural vegetation and modification of landscape, and to preserve to the maximum degree possible areas characterized primarily by wetland vegetation, such as mangroves and associated vegetation, and to permit such removal only in cases of overriding public interest. Here, while it cannot be concluded, as advocated by the Department, that the Monroe County comprehensive plan and land development regulations prohibit, under any circumstances, construction of the subject canal, it must be concluded, at this stage, that construction of the canal has not been demonstrated to be consistent with the plan and regulations. To be consistent, the Applicants would have to secure final plat approval for the canal, through the plat amendment process; a minor or major conditional use approval, as appropriate, as mandated by, inter alia, section 9 .5-345, MCC, for destruction of the mangrove community; and demonstrate that excavation of the canal on each of the platted lots would be consistent with the open space ratios of section 9- 804, MCLDR, and the environmental design criteria of section 9.5-34, MCC, or secure a conditional use as required by section 9.5-34-5, MCC. Amendment to the application post hearing In their proposed recommended order, submitted post hearing, the Applicants propose that the hearing officer recommend that, as a condition, the proposed canal terminate at the line of mean high water instead of extending approximately 100 feet into the boundaries of John Pennekamp State Park. The ostensible reason for the Applicants' request is their desire to eliminate the need for seeking approval from the Department of Natural Resources for intrusion into the boundaries of the park, and thereby shorten the time needed to secure all governmental approvals. While the Applicants did elicit testimony at hearing, albeit on rebuttal, that termination of the canal at the mean high water line would not significantly affect its performance as a flushing canal due to the extreme porosity of the caprock, the proof is not persuasive that the subject permits should be so limited or conditioned. Notably, the opinion that was offered in this regard was that of an expert hydrographic engineer who directed his remarks solely from a hydrographic viewpoint. The Applicants offered no testimony or other proof that would address the potential impacts, in any, that might occur to, inter alia, water quality or the biota, should the canal be terminated or closed in such a fashion. Under the circumstances, the Applicants failed to persuasively demonstrate that such amendment or condition is appropriate. This finding is not, however, preclusive of their applying for such modification to Monroe County.
Recommendation Based on the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Florida Land and Water Adjudicatory Commission enter a final order sustaining Monroe County's issuance of the subject permits in so far as they relate to Phase I of the proposed project, and reversing Monroe County's decision to issue the subject permits in so far as they relate to Phase II of the proposed project. It is further recommended that such final order specify those items set forth in paragraph 4, Conclusions of Law, as the changes necessary that would make the Applicants' proposal eligible to receive the requested permits for Phase II of their proposal. DONE AND ENTERED in Tallahassee, Leon County, Florida, this 19th day of October 1990. WILLIAM J. KENDRICK 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 19th day of October 1990.
Findings Of Fact Joyce K. Anderson and Thomas Barnett have filed an application for issuance of a permit to dredge and fill a small area in the littoral, or "near shore," zone of Gillis Pond, a "sandhill lake" lying in what is known as the "sandhill region" of Central Florida, generally northeast of Gainesville. The dredging and filling as now proposed would be on and waterward of two lakefront lots jointly owed by the permit applicants. They seek by their application, authorization to dredge and fill at only one site on the waterward margin of the two lots with that modified project area reduced in size to a dimension of 12 feet by 25 feet. Fifteen feet of the project would be waterward of the shoreline. The Respondent, the Department of Environmental Regulation, is an agency of the State of Florida charged with the duty of enforcing, as pertinent hereto, the provisions of Chapter 403, Florida Statutes, and Chapter 17-3 and 4, Florida Administrative Code, enforcing the water quality standards contained therein as they relate to dredge and fill projects of this sort, with concomitant permitting jurisdiction over such projects. The permit applicants desire this dredge and fill permit in order to make a safe, comfortable swimming area for Mrs. Anderson's family and friends. Mrs. Anderson desires to remove the tree stumps, roots and vegetation existing in the littoral zone area of the above dimensions in order to make access directly from the shore more comfortable and pleasant, especially for small children who are unable to swim in the deep water off the waterward end of the existing dock. Mrs. Anderson already has a 56 foot dock extending from her property into the lake. The water is 7 feet deep at the waterward end of the dock and the littoral zone containing aquatic vegetation extends beyond the length of the dock in a waterward direction. The project area would extend waterward of the shoreline, a distance of 15 feet, and would parallel the shoreline approximately a distance of 12 feet. The littoral zone vegetation at the site, however, extends waterward from the shoreline 50 to 60 feet. The proposed area to be dredged is quite small in size in relation to the total linear shoreline of the subject lake of approximately 4,000 feet. The dredged material would be excavated to a depth of approximately 6 inches over that 12 by 15 foot area and replaced with clean sand fill. The dredged material removed from the site would be secured on an upland site such that nutrient pollutants from that dredged material could not be leached or carried back into the lake through storm water runoff. Approximately one-third of the shoreline of the lake is bordered by a marsh or wet prairie which is approximately as large in area as the lake itself. The dominant vegetative species in the project area and surrounding the lake, including the marsh, are submerged freshwater species listed in Rule 17- 4.02(17), Florida Administrative Code, including maidencane, sawgrass and a rare aquatic plant, websteria confervodies. Gillis Pond is a Class III water of the state, although its water quality parameters, or some of them, clearly exceed in quality, the minimum standards for Class III waters. Gillis Pond is what is termed an "ultra- oligotrophic lake, which means that its waters are characterized by a high level of transparency and very low nutrient content, that is to say that they are essentially pristine in nature. An oligotrophic lake such as this is very sensitive to any addition of nutrient pollutants. Even a small addition of nutrients to such water can cause an imbalance in the fauna and flora which have evolved to become dependent upon a low nutrient aquatic environment. Specifically, the rare aquatic plant named above is very sensitive to any enhanced nutrient levels and thus serves as a barometer of the water quality in this body of water. The addition of any nutrient pollutants to the lake, even in small amounts, might alter the chemical balance of the water in a derogatory manner so that the websteria confervodies might be eliminated. The elimination of this species from the littoral zone vegetation band surrounding the lake would likely result in other forms of vegetation supplanting it, altering the balance and makeup of the community of fauna and flora native to the lake and possibly hastening the progress of the lake toward eutrophication and degradation. The present water quality in the lake is such that dissolved oxygen and other criteria are better than the Class III water quality standards. The vegetation in the littoral zone of the lake and extending out as much as 50 to 60 feet waterward performs a significant function in uptaking and fixing nutrient pollutants that wash into the lake from storm water runoff from the surrounding uplands. Inasmuch as 30 to 40 feet of this belt of littoral zone vegetation would remain waterward of the dredged and filled area if the permit is granted, the nutrient uptake function of the vegetation in the littoral zone would not be significantly degraded. There are two locations where littoral zone vegetation has been removed in a similar fashion and water quality and flora and fauna communities characteristic of an oligotrophic lake are still present and healthy. Further, there is an extremely low nutrient level in the lake at the present time, and no significant amount of nutrient pollutants are leached or washed into the lake through septic tanks, storm water runoff or other sources. There is no question that the project as proposed would result in some slight, transitory degradation of water quality in the form of increased turbidity and reduced transparency. Turbidity will be caused during and shortly after the dredging and filling operation itself, caused by stirring up of bottom peat or sediments and by removal of a 12 by 15 foot area of aquatic vegetation in the littoral zone of the lake. Turbidity curtains in still waters such as involved here, can substantially reduce the spread of turbidity caused by the stirring up of bottom material and can substantially reduce the period of its suspension in the water by containing it at the dredged site. The vast majority of the littoral zone vegetation surrounding and waterward of the area to be dredged will remain such that the nutrient uptake function will be essentially undisturbed, thus any adverse impact on water quality will be insignificant. In terms of cumulative effect of allowing a multiplicity of such projects, not even a 10 percent loss of the littoral zone band of vegetation in the lake, which would be the maximum possible loss if all riparian land owners were allowed a similar size dredged and filled area on the front of their lots, would cause a violation of Department water quality standards. Parenthetically, it should be pointed out that such riparian owners cannot be prevented by any water quality criteria in Chapter 403 or Chapter 17, Florida Administrative Code, from having access to the lake in front of their lots. Such human traffic will have the gradual affect of destroying a significant amount of the littoral zone vegetation on and waterward of those lots (which is a cause and result the Department is powerless to regulate). By confining the destruction of littoral zone vegetation to such a small area as that involved in the application at bar and thus guaranteeing adequate, comfortable access for the riparian owner, the survivability of the remaining critical littoral zone vegetation will be significantly enhanced.
Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence in the record and the candor and demeanor of the witnesses, it is, therefore RECOMMENDED: That the application of Joyce K. Anderson and Thomas Barnett for a dredge and fill permit as described in the modified and amended application be GRANTED; provided, however, that turbidity curtains are used during all dredging and filling activity and for a reasonable time thereafter until turbidity caused by the project has settled out of the water column. DONE and ENTERED this 26th day of September, 1983, in Tallahassee, Florida. P. MICHAEL RUFF, Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 26th day of September, 1983. COPIES FURNISHED: Tim Keyser, Esquire Post Office Box 92 Interlachen, Florida 32048 Dennis R. Erdley, Esquire Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 Joyce K. Anderson and Thomas Barnett 6216-B, Southwest 11th Place Gainesville, Florida 32601 Victoria Tschinkel, Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301
