The Issue The issue to be determined is whether Consumptive Use Permit No. 2-083-91926-3, and Environmental Resource Permit No. IND-083-130588-4 should be issued as proposed in the respective proposed agency actions issued by the St. Johns River Water Management District.
Findings Of Fact The Parties Sierra Club, Inc., is a national organization, the mission of which is to explore, enjoy, and advocate for the environment. A substantial number of Sierra Club’s 28,000 Florida members utilize the Silver River, Silver Springs, the Ocklawaha River, and the St. Johns River for water-based recreational activities, which uses include kayaking, swimming, fishing, boating, canoeing, nature photography, and bird watching. St. Johns Riverkeeper, Inc., is one of 280 members of the worldwide Waterkeepers Alliance. Its mission is to protect, restore, and promote healthy waters of the St. Johns River, its tributaries, springs, and wetlands -- including Silver Springs, the Silver River, and the Ocklawaha River -- through citizen- based advocacy. A substantial number of St. Johns Riverkeeper’s more than 1,000 members use and enjoy the St. Johns River, the Silver River, Silver Springs, and the Ocklawaha River for boating, fishing, wildlife observation, and other water-based recreational activities. Karen Ahlers is a native of Putnam County, Florida, and lives approximately 15 miles from the Applicant’s property on which the permitted uses will be conducted. Ms. Ahlers currently uses the Ocklawaha River for canoeing, kayaking, and swimming, and enjoys birding and nature photography on and around the Silver River. Over the years, Ms. Ahlers has advocated for the restoration and protection of the Ocklawaha River, as an individual and as a past-president of the Putnam County Environmental Council. Jeri Baldwin lives on a parcel of property in the northeast corner of Marion County, approximately one mile from the Applicant’s property on which the permitted uses will be conducted. Ms. Baldwin, who was raised in the area, and whose family and she used the resources extensively in earlier years, currently uses the Ocklawaha River for boating. Florida Defenders of the Environment (FDE) is a Florida corporation, the mission of which is to conserve and protect and restore Florida's natural resources and to conduct environmental education projects. A substantial number of FDE’s 186 members, of which 29 reside in Marion County, Florida, use and enjoy Silver Springs, the Silver River, and the Ocklawaha Aquatic Preserve, and their associated watersheds in their educational and outreach activities, as well as for various recreational activities including boating, fishing, wildlife observation, and other water-based recreational activities. Sleepy Creek Lands, LLC (Sleepy Creek or Applicant), is an entity registered with the Florida Department of State to do business in the state of Florida. Sleepy Creek owns approximately 21,000 acres of land in Marion County, Florida, which includes the East Tract and the North Tract on which the activities authorized by the permits are proposed. St. Johns River Water Management District (SJRWMD or District) is a water-management district created by section 373.069(1). It has the responsibility to conserve, protect, manage, and control the water resources within its geographic boundaries. See § 373.069(2)(a), Fla. Stat. The Consumptive Use Permit The CUP is a modification and consolidation of two existing CUP permits, CUP No. 2-083-3011-7 and CUP No. 2-083- 91926-2, which authorize the withdrawal of 1.46 mgd from wells located on the East Tract. Although the existing CUP permits authorize an allocation of 1.46 mgd, actual use has historically been far less, and rarely exceeded 0.3 mgd. The proposed CUP modification will convert the authorized use of water from irrigation of 1,010 acres of sod grass on the East Tract, to supplemental irrigation of improved pasture for grass and other forage crops (approximately 97 percent of the proposed withdrawals) and cattle watering (approximately three percent of the proposed withdrawals) on the North Tract and the East Tract. An additional very small amount will be used in conjunction with the application of agricultural chemicals. CUP No. 2-083-3011-7 is due to expire in 2021. CUP No. 2-083-91926-2 is due to expire in 2024. In addition to the consolidation of the withdrawals into a single permit, the proposed agency action would extend the term of the consolidated permit to 20 years from issuance, with the submission of a compliance report due 10 years from issuance. Sleepy Creek calculated a water demand of 2.569 mgd for the production of grasses and forage crops necessary to meet the needs for grass-fed beef production, based on the expected demand in a 2-in-10 drought year. That calculation is consistent with that established in CUP Applicant’s Handbook (CUP A.H.) section 12.5.1. The calculated amount exceeds the authorized average allocation of 1.46 mgd. Mr. Jenkins testified as to the District’s understanding that the requested amount would be sufficient, since the proposed use was a “scaleable-type project,” with adjustments to cattle numbers made as necessary to meet the availability of feed. Regardless of demand, the proposed permit establishes the enforceable withdrawal limits applicable to the property. With regard to the East Tract, the proposed agency action reduces the existing 1.46 mgd allocation for that tract to a maximum allocation of 0.464 mgd, and authorizes the irrigation of 611 acres of pasture grass using existing extraction wells and six existing pivots. With regard to the North Tract, the proposed agency action authorizes the irrigation of 1,620 acres of pasture and forage grain crops using 15 center pivot systems. Extraction wells to serve the North Tract pivots will be constructed on the North Tract. The proposed North Tract withdrawal wells are further from Silver Springs than the current withdrawal locations. The proposed CUP allows Sleepy Creek to apply the allocated water as it believes to be appropriate to the management of the cattle operation. Although the East Tract is limited to a maximum of 0.464 mgd, there is no limitation on the North Tract. Thus, Sleepy Creek could choose to apply all of the 1.46 mgd on the North Tract. For that reason, the analysis of impacts from the irrigation of the North Tract has generally been based on the full 1.46 mgd allocation being drawn from and applied to the North Tract. The Environmental Resource Permit As initially proposed, the CUP had no elements that would require issuance of an ERP. However, in order to control the potential for increased runoff and nutrient loading resulting from the irrigation of the pastures, Sleepy Creek proposes to construct a stormwater management system to capture runoff from the irrigated pastures, consisting of a series of vegetated upland buffers, retention berms and redistribution swales between the pastures and downgradient wetland features. Because the retention berm and swale system triggered the permitting thresholds in rule 62-330.020(2)(d) (“a total project area of more than one acre”) and rule 62-330.020(2)(e) (“a capability of impounding more than 40 acre-feet of water”), Sleepy Creek was required to obtain an Environmental Resource Permit for its construction. Regional Geologic Features To the west of the North Tract is a geologic feature known as the Ocala Uplift or Ocala Platform, in which the limestone that comprises the Floridan aquifer system exists at or very near the land surface. Karst features, including subterranean conduits and voids that can manifest at the land surface as sinkholes, are common in the Ocala Uplift due in large part to the lack of consolidated or confining material overlaying the limestone. Water falling on the surface of such areas tends to infiltrate rapidly through the soil into the Floridan aquifer, occasionally through direct connections such as sinkholes. The lack of confinement in the Ocala Uplift results in few if any surface-water features such as wetlands, creeks, and streams. As one moves east from the Ocala Uplift, a geologic feature known as the Cody Escarpment becomes more prominent. In the Cody Escarpment, the limestone becomes increasingly overlain by sands, shell, silt, clays, and other less permeable sediments of the Hawthorn Group. The North Tract and the East Tract lie to the east of the point at which the Cody Escarpment becomes apparent. As a result, water tends to flow overland to wetlands and other surface water features. The Property The North and East Tracts are located in northern Marion County near the community of Fort McCoy. East Tract Topography and Historic Use The East Tract is located in the Daisy Creek Basin, and includes the headwaters of a small creek that drains directly to the Ocklawaha River. The historic use of the East Tract has been as a cleared 1,010-acre sod farm. The production of sod included irrigation, fertilization, and pest control. Little change in the topography, use, and appearance of the property will be apparent as a result of the permits at issue, but for the addition of grazing cattle. The current CUPs that are subject to modification in this proceeding authorize groundwater withdrawals for irrigation of the East Tract at the rate of 1.46 mgd. Since the proposed agency action has the result of reducing the maximum withdrawal from wells on the East Tract to 0.464 mgd, thus proportionately reducing the proposed impacts, there was little evidence offered to counter Sleepy Creek’s prima facie case that reasonable assurance was provided that the proposed East Tract groundwater withdrawal allocation will meet applicable CUP standards. There are no stormwater management structures to be constructed on the East Tract. Therefore, the ERP permit discussed herein is not applicable to the East Tract. North Tract Topography and Historic Use The North Tract has a generally flat topography, with elevations ranging from 45 feet to 75 feet above sea level. The land elevation is highest at the center of the North Tract, with the land sloping towards the Ocklawaha River to the east, and to several large wet prairie systems to the west. Surface water features on the North Tract include isolated, prairie, and slough-type wetlands on approximately 28 percent of the North Tract, and a network of creeks, streams, and ditches, including the headwaters of Mill Creek, a contributing tributary of the Ocklawaha River. A seasonal high groundwater elevation on the North Tract is estimated at 6 to 14 inches below ground surface. The existence of defined creeks and surface water features supports a finding that the North Tract is underlain by a relatively impermeable confining layer that impedes the flow of water from the surface and the shallow surficial aquifer to the upper Floridan and lower Floridan aquifers. If there was no confining unit, water going onto the surface of the property, either in the form of rain or irrigation water, would percolate unimpeded to the lower aquifers. Areas in the Ocala Uplift to the west of the North Tract, where the confining layer is thinner and discontiguous, contain few streams or runoff features. Historically, the North Tract was used for timber production, with limited pasture and crop lands. At the time the 7,207-acre North Tract was purchased by Sleepy Creek, land use consisted of 4,061 acres of planted pine, 1,998 acres of wetlands, 750 acres of improved pasture, 286 acres of crops, 78 acres of non-forested uplands, 20 acres of native forest, 10 acres of open water, and 4 acres of roads and facilities. Prior to the submission of the CUP and ERP applications, much of the planted pine was harvested, and the land converted to improved pasture. Areas converted to improved pasture include those proposed for irrigation, which have been developed in the circular configuration necessary for future use with center irrigation pivots. As a result of the harvesting of planted pine, and the conversion of about 345 acres of cropland and non-forested uplands to pasture and incidental uses, total acreage in pasture on the North Tract increased from 750 acres to 3,938 acres. Other improvements were constructed on the North Tract, including the cattle processing facility. Aerial photographs suggest that the conversion of the North Tract to improved pasture and infrastructure to support a cattle ranch is substantially complete. The act of converting the North Tract from a property dominated by planted pine to one dominated by improved pasture, and the change in use of the East Tract from sod farm to pasture, were agricultural activities that did not require a permit from the District. As such, there is no impropriety in considering the actual, legal use of the property in its current configuration as the existing use for which baseline conditions are to be measured. Petitioners argue that the baseline conditions should be measured against the use of the property as planted pine plantation, and that Sleepy Creek should not be allowed to “cattle-up” before submitting its permit applications, thereby allowing the baseline to be established as a higher impact use. However, the applicable rules and statutes provide no retrospective time-period for establishing the nature of a parcel of property other than that lawfully existing when the application is made. See West Coast Reg’l Water Supply Auth. v. SW Fla. Water Mgmt. Dist., Case No. 95-1520 et seq., ¶ 301 (Fla. DOAH May 29, 1997; SFWMD ) (“The baseline against which projected impacts conditions [sic] are those conditions, including previously permitted adverse impacts, which existed at the time of the filing of the renewal applications.”). The evidence and testimony in this case focused on the effects of the water allocation on the Floridan aquifer, Silver Springs, and the Silver River, and on the effects of the irrigation on water and nutrient transport from the properties. It was not directed at establishing a violation of chapter 373, the rules of the SJRWMD, or the CUP Applicant’s Handbook with regard to the use and management of the agriculturally-exempt unirrigated pastures, nor did it do so. Soil Types Soils are subject to classifications developed by the Soil Conservation Service based on their hydrologic characteristics, and are grouped into Group A, Group B, Group C, or Group D. Factors applied to determine the appropriate hydrologic soil group on a site-specific basis include depth to seasonal high saturation, the permeability rate of the most restrictive layer within a certain depth, and the depth to any impermeable layers. Group A includes the most well-drained soils, and Group D includes the most poorly-drained soils. Group D soils are those with seasonal high saturation within 24 inches of the soil surface and a higher runoff potential. The primary information used to determine the hydrologic soil groups on the North Tract was the depth to seasonal-high saturation, defined as the highest expected annual elevation of saturation in the soil. Depth to seasonal-high saturation was measured through a series of seven hand-dug and augered soil borings completed at various locations proposed for irrigation across the North Tract. In determining depth to seasonal-high saturation, the extracted soils were examined based on depth, color, texture, and other relevant characteristics. In six of the seven locations at which soil borings were conducted, a restrictive layer was identified within 36 inches of the soil surface. At one location at the northeastern corner of the North Tract, the auger hole ended at a depth of 48 inches -- the length of the auger -- at which depth there was an observable increase in clay content but not a full restrictive layer. However, while the soil assessment was ongoing, a back-hoe was in operation approximately one hundred yards north of the boring location. Observations of that excavation revealed a heavy clay layer at a depth of approximately 5 feet. In each of the locations, the depth to seasonal-high saturation was within 14 inches of the soil surface. Based on the consistent observation of seasonal-high saturation at each of the sampled locations, as well as the flat topography of the property with surface water features, the soils throughout the property, with the exception of a small area in the vicinity of Pivot 6, were determined to be in hydrologic soil Group D. Hydrogeologic Features There are generally five hydrogeologic units underlying the North Tract, those units being the surficial aquifer system, the intermediate confining unit, the upper Floridan aquifer, the middle confining unit, and the lower Floridan aquifer. In areas in which a confining layer is present, water falling on the surface of the land flows over the surface of the land or across the top of the confining layer. A surficial aquifer, with a relatively high perched water table, is created by the confinement and separation of surface waters from the upper strata of the Floridan aquifer. Surface waters are also collected in or conveyed by various surface water features, including perched wetlands, creeks, and streams. The preponderance of the evidence adduced at the final hearing demonstrates that the surficial aquifer exists on the property to a depth of up to 20 feet below the land surface (bls). Beneath the surficial aquifer is an intermediate confining unit of dense clay interspersed with beds of sand and calcareous clays that exists to a depth of up to 100 feet bls. The clay material observed on the North Tract is known as massive or structureless. Such clays are restrictive with very low levels of hydraulic conductivity, and are not conducive to development of preferential flow paths to the surficial or lower aquifers. The intermediate confining unit beneath the North Tract restricts the exchange of groundwater from the surficial aquifer to the upper Floridan aquifer. The upper Floridan aquifer begins at a depth of approximately 100 feet bls, and extends to a depth of approximately 340 feet bls. At about 340 feet bls, the upper Floridan aquifer transitions to the middle confining unit, which consists of finely grained, denser material that separates the interchange of water between the upper Floridan aquifer and the lower Floridan aquifer. Karst Features Karst features form as a result of water moving through rock that comprises the aquifer, primarily limestone, dissolving and forming conduits in the rock. Karst areas present a challenging environment to simulate through modeling. Models assume the subsurface to be a relatively uniform “sand box” through which it is easier to simulate groundwater flow. However, if the subsurface contains conduits, it becomes more difficult to simulate the preferential flows and their effect on groundwater flow paths and travel times. The District has designated parts of western Alachua County and western Marion County as a Sensitive Karst Area Basin. A Sensitive Karst Area is a location in which the porous limestone of the Floridan aquifer occurs within 20 feet of the land surface, and in which there is 10 to 20 inches of annual recharge to the Floridan aquifer. The designation of an area as being within the Sensitive Karst Area Basin does not demonstrate that it does, or does not, have subsurface features that are karstic in nature, or that would provide a connection between the surficial aquifer and the Floridan aquifer. The western portion of the North Tract is within the Sensitive Karst Area Basin. The two intensive-use areas on the North Tract that have associated stormwater facilities -- the cattle unloading area and the processing facility -- are outside of the Sensitive Karst Area Basin. The evidence was persuasive that karst features are more prominent to the west of the North Tract. In order to evaluate the presence of karst features on the North Tract, Mr. Andreyev performed a “desktop-type evaluation,” with a minimal field survey. The desktop review included a review of aerial photographs and an investigation of available data, including the Florida Geological Survey database of sinkhole occurrence in the area. The aerial photographs showed circular depressions suggestive of karst activity west and southwest of the North Tract, but no such depressions on the North Tract. Soil borings taken on the North Tract indicated the presence of layers of clayey sand, clays, and silts at a depth of 70 to 80 feet. Well-drilling logs taken during the development of the wells used for an aquifer performance test on the North Tract showed the limestone of the Floridan aquifer starting at a depth below ground surface of 70 to 80 feet. Other boring data generated on the North Tract suggests that there is greater than 100 feet of clay and sandy clay overburden above the Floridan aquifer on and in the vicinity of the North Tract. Regardless of site-specific differences, the observed confining layer separating the surficial aquifer from the Floridan aquifer is substantial, and not indicative of a karst environment. Aquifer performance tests performed on the North Tract were consistent in showing that drawdown in the surficial aquifer from the tests was minimal to non-detectable, which is strong evidence of an intact and low-permeability confining layer. The presence of well-developed drainage features on the North Tract is further evidence of a unit of confinement that is restricting water from going deeper into the subsurface, and forcing it to runoff to low-lying surface water features. Petitioners’ witnesses did not perform any site- specific analysis of karst features on or around the Sleepy Creek property. Their understanding of the nature of the karst systems in the region was described as “hypothetical or [] conceptual.” Dr. Kincaid admitted that he knew of no conduits on or adjacent to the North Tract. As a result of the data collected from the North Tract, Mr. Hearn opined that the potential for karst features on the property that provide an opening to the upper Floridan aquifer “is extremely remote.” Mr. Hearn’s opinion is consistent with the preponderance of the evidence in this case, and is accepted. In the event a surface karst feature were to manifest itself, Sleepy Creek has proposed that the surface feature be filled and plugged to reestablish the integrity of the confining layer. More to the point, the development of a surficial karst feature in an area influenced by irrigation would be sufficient grounds for the SJRWMD to reevaluate and modify the CUP to account for any changed conditions affecting the assumptions and bases for issuance of the CUP. Silver Springs, the Silver River, and the Ocklawaha River The primary, almost exclusive concern of Petitioners was the effect of the modified CUP and the nutrients from the proposed cattle ranch on Silver Springs, the Silver River, and the Ocklawaha River. Silver Springs Silver Springs has long been a well-known attraction in Florida. It is located just to the east of Ocala, Florida. Many of the speakers at the public comment period of this proceeding spoke fondly of having frequented Silver Springs over the years, enjoying its crystal clear waters through famous glass-bottomed boats. For most of its recorded history, Silver Springs was the largest spring by volume in Florida. Beginning in the 1970s, it began to lose its advantage, and by the year 2000, Rainbow Springs, located in southwestern Marion County, surpassed Silver Springs as the state’s largest spring. Silver Springs exists at the top of the potentiometric surface of the Floridan aquifer. Being at the “top of the mountain,” when water levels in the Floridan aquifer decline, groundwater flow favors the lower elevation springs. Thus, surrounding springshed boundaries expand to take more water to maintain their baseflows, at the expense of the Silver Springs springshed, which contracts. Rainbow Springs shares an overlapping springshed with Silver Springs. The analogy used by Dr. Knight was of the aquifer as a bucket with holes at different levels, and with the Silver Springs “hole” near the top of the bucket. When the water level in the bucket is high, water will flow from the top hole. As the water level drops below that hole, it will preferentially flow from the lower holes. Rainbow Springs has a vent or outlet from the aquifer, that is 10 feet lower in elevation than that of Silver Springs. Coastal springs are lower still. Thus, as groundwater levels decline, the lower springs “pirate flow” from the upper springs. Since the first major studies of Silver Springs were conducted in the 1950s, the ecosystem of Silver Springs has undergone changes. The water clarity, though still high as compared to other springs, has been reduced by 10 to 15 percent. Since the 1950s, macrophytic plants, i.e., rooted plants with seeds and flowers, have declined in population, while epiphytic and benthic algae have increased. Those plants are sensitive to increases in nitrogen in the water. Thus, Dr. Knight’s opinion that increases in nitrogen emerging from Silver Springs, calculated to have risen from just over 0.4 mg/l in the 1950s, to 1.1 mg/l in 2004, and to up to 1.5 mg/l at present,1/ have caused the observed vegetative changes is accepted. Silver River Silver Springs forms the headwaters for the Silver River, a spring run 5 1/2 miles in length, at which point it becomes a primary input to the Ocklawaha River. Issues of water clarity and alteration of the vegetative regime that exist at Silver Springs are also evident in the Silver River. In addition, the reduction in flow allows for more tannic water to enter the river, further reducing clarity. Dr. Dunn recognized the vegetative changes in the river, and opined that the “hydraulic roughness” caused by the increase in vegetation is likely creating a spring pool backwater at Silver Springs, thereby suppressing some of the flow from the spring. The Silver River has been designated as an Outstanding Florida Water. There are currently no Minimum Flows and Levels established by the District for the Silver River. Ocklawaha River The Ocklawaha River originates near Leesburg, Florida, at the Harris Chain of Lakes, and runs northward past Silver Springs. The Silver River is a major contributor to the flow of the Ocklawaha River. Due to the contribution of the Silver River and other spring-fed tributaries, the Ocklawaha River can take on the appearance of a spring run during periods of low rainfall. Historically, the Ocklawaha River flowed unimpeded to its confluence with the St. Johns River in the vicinity of Palatka, Florida. In the 1960s, as part of the Cross-Florida Barge Canal project, the Rodman Dam was constructed across the Ocklawaha River north of the Sleepy Creek property, creating a large reservoir known as the Rodman Pool. Dr. Knight testified convincingly that the Rodman Dam and Pool have altered the Ocklawaha River ecosystem, precipitating a decline in migratory fish populations and an increase in filamentous algae. At the point at which the Ocklawaha River flows past the Sleepy Creek property, it retains its free-flowing characteristics. Mill Creek, which has its headwaters on the North Tract, is a tributary of the Ocklawaha River. The Ocklawaha River, from the Eureka Dam south, has been designated as an Outstanding Florida Water. However, the Ocklawaha River at the point at which Mill Creek or other potential surface water discharges from the Sleepy Creek property might enter the river are not included in the Outstanding Florida Water designation. There are currently no Minimum Flows and Levels established by the District for the Ocklawaha River. The Silver Springs Springshed A springshed is that area from which a spring draws water. Unlike a surface watershed boundary, which is fixed based on land features, contours, and elevations, a springshed boundary is flexible, and changes depending on a number of factors, including rainfall. As to Silver Springs, its springshed is largest during periods of more abundant rainfall when the aquifer is replenished, and smaller during drier periods when groundwater levels are down, and water moves preferentially to springs and discharge points that are lower in elevation. The evidence in this case was conflicting as to whether the North Tract is in or out of the Silver Springs springshed boundary. Dr. Kincaid indicated that under some of the springshed delineations, part of the North Tract was out of the springshed, but over the total period of record, it is within the springshed. Thus, it was Dr. Kincaid’s opinion that withdrawals anywhere within the region will preferentially impact Silver Springs, though he admitted that he did not have the ability to quantify his opinion. Dr. Knight testified that the North Tract is within the Silver Springs “maximum extent” springshed at least part of the time, if not all the time. He did not opine as to the period of time in which the Silver Springs springshed was at its maximum extent. Dr. Bottcher testified that the North Tract is not within the Silver Springs springshed because there is a piezometric rise between North Tract and Silver Springs. Thus, in his opinion, withdrawals at the North Tract would not be withdrawing water going to Silver Springs. Dr. Dunn agreed that the North Tract is on the groundwater divide for Silver Springs. In his view, the North Tract is sometimes in, and sometimes out of the springshed depending on the potentiometric surface. In his opinion, the greater probability is that the North Tract is more often outside of the Silver Springs springshed, with seasonal and year—to—year variation. Dr. Dunn’s opinion provides the most credible explanation of the extent to which the North Tract sits atop that portion of the lower Floridan aquifer that feeds to Silver Springs. Thus, it is found that the groundwater divide exists to the south of the North Tract for a majority of the time, and water entering the Floridan aquifer from the North Tract will, more often than not, flow away from Silver Springs. Silver Springs Flow Volume The Silver Springs daily water discharge has been monitored and recorded since 1932. Over the longest part of the period of record, up to the 1960s, flows at Silver Springs averaged about 800 cubic feet per second (cfs). Through 1989, there was a reasonable regression between rainfall and springflow, based on average rainfalls. The long-term average rainfall in Ocala was around 50 inches per year, and long-term springflow was about 800 cfs, with deviations from average generally consistent with one another. Between 1990 and 1999, the relationship between rainfall and springflow declined by about 80 cubic feet per second. Thus, with average rainfall of 50 inches per year, the average springflow was reduced to about 720 cfs. From 2000 to 2009, there was an additional decline, such that the total cumulative decline for the 20-year period through 2009 was 250 cfs. Dr. Dunn agreed with Dr. Knight that after 2000, there was an abrupt and persistent reduction in flow of about 165 cfs. However, Dr. Dunn did not believe the post-2000 flow reduction could be explained by rainfall directly, although average rainfall was less than normal. Likewise, groundwater withdrawals did not offer an adequate explanation. Dr. Dunn described a natural 30-year cycle of wetter and drier periods known as the Atlantic Multidecadal Oscillation (AMO) that has manifested itself over the area for the period of record. From the 1940s up through 1970, the area experienced an AMO wet cycle with generally higher than normal rainfall at the Ocala rain station. For the next 30-year period, from 1970 up to 2000, the Ocala area ranged from a little bit drier to some years in which it was very, very dry. Dr. Dunn attributed the 80 cfs decline in Silver Springs flow recorded in the 1990s to that lower rainfall cycle. After 2000, when the next AMO cycle would be expected to build up, as it did post—1940, it did not happen. Rather, there was a particularly dry period around 2000 that Dr. Dunn believes to have had a dramatic effect on the lack of recovery in the post-2000 flows in the Silver River. According to Mr. Jenkins, that period of deficient rainfall extended through 2010. Around the year 2001, the relationship between rainfall and flow changed such that for a given amount of rainfall, there was less flow in the Silver River, with flow dropping to as low as 535 cfs after 2001. It is that reduction in flow that Dr. Knight has attributed to groundwater withdrawals. It should be noted that the observed flow of Silver Springs that formed the 1995 baseline conditions for the North Central Florida groundwater model that will be discussed herein was approximately 706 cfs. At the time of the final hearing in August 2014, flow at Silver Springs was 675 cfs. The reason offered for the apparent partial recovery was higher levels of rainfall, though the issue was not explored in depth. For the ten-year period centered on the year 2000, local water use within Marion and Alachua County, closer to Silver Springs, changed little -- around one percent per year. From a regional perspective, groundwater use declined at about one percent per year for the period from 1990 to 2010. The figures prepared by Dr. Knight demonstrate that the Sleepy Creek project area is in an area that has a very low density of consumptive use permits as compared to areas adjacent to Silver Springs and more clearly in the Silver Springs springshed. In Dr. Dunn’s opinion, there were no significant changes in groundwater use either locally or regionally that would account for the flow reduction in Silver Springs from 1990 to 2010. In that regard, the environmental report prepared by Dr. Dunn and submitted with the CUP modification application estimated that groundwater withdrawals accounted for a reduction in flow at Silver Springs of approximately 20 cfs as measured against the period of record up to the year 2000, with most of that reduction attributable to population growth in Marion County. In the March 2014, environmental impacts report, Dr. Dunn described reductions in the stream flow of not only the Silver River, but of other tributaries of the lower Ocklawaha River, including the upper Ocklawaha River at Moss Bluff and Orange Creek. However, an evaluation of the Ocklawaha River water balance revealed there to be additional flow of approximately 50 cfs coming into the Ocklawaha River at other stations. Dr. Dunn suggested that changes to the vent characteristics of Silver Springs, and the backwater effects of increased vegetation in the Silver River, have resulted in a redistribution of pressure to other smaller springs that discharge to the Ocklawaha River, accounting for a portion of the diminished flow at Silver Springs. The Proposed Cattle Operation Virtually all beef cattle raised in Florida, upon reaching a weight of approximately 875 pounds, are shipped to Texas or Kansas to be fattened on grain to the final body weight of approximately 1,150 pounds, whereupon they are slaughtered and processed. The United States Department of Agriculture has a certification for grass—fed beef which requires that, after an animal is weaned, it can only be fed on green forage crops, including grasses, and on corn and grains that are cut green and before they set seed. The forage crops may be grazed or put into hay or silage and fed when grass and forage is dormant. The benefit of grass feeding is that a higher quality meat is produced, with a corresponding higher market value. Sleepy Creek plans to develop the property as a grass- fed beef production ranch, with pastures and related loading/unloading and slaughter/processing facilities where calves can be fattened on grass and green grain crops to a standard slaughter weight, and then slaughtered and processed locally. By so doing, Sleepy Creek expects to save the transportation and energy costs of shipping calves to the Midwest, and to generate jobs and revenues by employing local people to manage, finish, and process the cattle. As they currently exist, pastures proposed for irrigation have been cleared and seeded, and have “fairly good grass production.” The purpose of the irrigation is to enhance the production and quality of the grass in order to maintain the quality and reliability of feed necessary for the production of grass-fed beef. East Tract Cattle Operation The East Tract is 1,242 acres in size, substantially all of which was previously cleared, irrigated, and used for sod production. The proposed CUP permit authorizes the irrigation of 611 acres of pasture under six existing center pivots. The remaining 631 acres will be used as improved, but unirrigated, pasture. Under the proposed permit, a maximum of 1,207 cattle would be managed on the East Tract. Of that number, 707 cattle would be grazed on the irrigated paddocks, and 500 cattle would be grazed on the unirrigated improved pastures. If the decision is made to forego irrigation on the East Tract, with the water allocation being used on the North Tract or not at all, the number of cattle grazed on the six center pivot pastures would be decreased from 707 cattle to 484 cattle. The historic use of the East Tract as a sod farm resulted in high phosphorus levels in the soil from fertilization, which has made its way to Daisy Creek. Sleepy Creek has proposed a cattle density substantially below that allowed by application of the formulae in the Nutrient Management Plan in order to “mine” the phosphorus levels in the soil over time. North Tract Cattle Operation The larger North Tract includes most of the “new” ranch activities, having no previous irrigation, and having been put to primarily silvicultural use with limited pasture prior to its acquisition by Sleepy Creek. The ranch’s more intensive uses, i.e., the unloading corrals and the slaughter house, are located on the North Tract. The North Tract is 7,207 acres in size. Of that, 1,656 acres are proposed for irrigation by means of 15 center- pivot irrigation systems. In addition to the proposed irrigated pastures, the North Tract includes 2,382 acres of unirrigated improved pasture, of which approximately 10 percent is wooded. Under the proposed permit, a maximum of 6,371 cattle would be managed on the North Tract. Of that number, 3,497 cattle would be grazed on the irrigated paddocks (roughly 2.2 head of cattle per acre), and 2,374 cattle would graze on the improved pastures (up to 1.1 head of cattle per acre). The higher cattle density in the irrigated pastures can be maintained due to the higher quality grass produced as a result of irrigation. The remaining 500 cattle would be held temporarily in high-concentration corrals, either after offloading or while awaiting slaughter. On average, there will be fewer than 250 head of cattle staged in those high-concentration corrals at any one time. In the absence of irrigation, the improved pasture on the North Tract could sustain about 4,585 cattle. Nutrient Management Plan, Water Conservation Plan, and BMPs The CUP and ERP applications find much of their support in the implementation of the Nutrient Management Plan (NMP), the Water Conservation Plan, and Best Management Practices (BMPs). The NMP sets forth information designed to govern the day to day operations of the ranch. Those elements of the NMP that were the subject of substantive testimony and evidence at the hearing are discussed herein. Those elements not discussed herein are found to have been supported by Sleepy Creek’s prima facie case, without a preponderance of competent and substantial evidence to the contrary. The NMP includes a herd management plan, which describes rotational grazing and the movement of cattle from paddock to paddock, and establishes animal densities designed to maintain a balance of nutrients on the paddocks, and to prevent overgrazing. The NMP establishes fertilization practices, with the application of fertilizer based on crop tissue analysis to determine need and amount. Thus, the application of nitrogen- based fertilizer is restricted to that capable of ready uptake by the grasses and forage crops, limiting the amount of excess nitrogen that might run off of the pastures or infiltrate past the root zone. The NMP establishes operation and maintenance plans that incorporate maintenance and calibration of equipment, and management of high-use areas. The NMP requires that records be kept of, among other things, soil testing, nutrient application, herd rotation, application of irrigation water, and laboratory testing. The irrigation plan describes the manner and schedule for the application of water during each irrigation cycle. Irrigation schedules for grazed and cropped scenarios vary from pivot to pivot based primarily on soil type. The center pivots proposed for use employ high-efficiency drop irrigation heads, resulting in an 85 percent system efficiency factor, meaning that there is an expected evaporative loss of 15 percent of the water before it becomes available as water in the soil. That level of efficiency is greater than the system efficiency factor of 80 percent established in CUP A.H. section 12.5.2. Other features of the irrigation plan include the employment of an irrigation manager, installation of an on-site weather station, and cumulative tracking of rain and evapotranspiration with periodic verification of soil moisture conditions. The purpose of the water conservation practices is to avoid over application of water, limiting over-saturation and runoff from the irrigated pastures. Sleepy Creek has entered into a Notice of Intent to Implement Water Quality BMPs with the Florida Department of Agriculture and Consumer Services which is incorporated in the NMP and which requires the implementation of Best Management Practices.2/ Dr. Bottcher testified that implementation and compliance with the Water Quality Best Management Practices manual creates a presumption of compliance with water quality standards. His testimony in that regard is consistent with Department of Agriculture and Consumer Services rule 5M-11.003 (“implementation, in accordance with adopted rules, of BMPs that have been verified by the Florida Department of Environmental Protection as effective in reducing target pollutants provides a presumption of compliance with state water quality standards.”). Rotational Grazing Rotational grazing is a practice by which cattle are allowed to graze a pasture for a limited period of time, after which they are “rotated” to a different pasture. The 1,656 acres proposed for irrigation on the North Tract are to be divided into 15 center-pivot pastures. Each individual pasture will have 10 fenced paddocks. The 611 acres of irrigated pasture on the East Tract are divided into 6 center-pivot pastures. The outer fence for each irrigated pasture is to be a permanent “hard” fence. Separating the internal paddocks will be electric fences that can be lowered to allow cattle to move from paddock to paddock, and then raised after they have moved to the new paddock. The NMP for the North Tract provides that cattle are to be brought into individual irrigated pastures as a single herd of approximately 190 cattle and placed into one of the ten paddocks. They will be moved every one to three days to a new paddock, based upon growing conditions and the reduction in grass height resulting from grazing. In this way, the cattle are rotated within the irrigated pasture, with each paddock being used for one to three days, and then rested until each of the other paddocks have been used, whereupon it will again be used in the rotation. The East Tract NMP generally provides for rotation based on the height of the pasture grasses, but is designed to provide a uniform average of cattle per acre per year. Due to the desire to “mine” phosphorus deposited during the years of operation of the East Tract as a sod farm, the density of cattle on the irrigated East Tract pastures is about 30 percent less than that proposed for the North Tract. The East Tract NMP calls for a routine pasture rest period of 15 to 30 days. Unlike dairy farm pastures, where dairy cows traverse a fixed path to the milking barn several times a day, there will be minimal “travel lanes” within the pastures or between paddocks. There will be no travel lanes through wetlands. If nitrogen-based fertilizer is needed, based upon tissue analysis of the grass, fertilizer is proposed for application immediately after a paddock is vacated by the herd. By so doing, the grass within each paddock will have a sufficient period to grow and “flush up” without grazing or traffic, which results in a high—quality grass when the cattle come back around to feed. Sleepy Creek proposes that rotational grazing is to be practiced on improved pastures and irrigated pastures alike. The rotational practices on the improved East Tract and North Tract pastures are generally similar to those practiced on the irrigated pastures. The paddocks will have permanent watering troughs, with one trough serving two adjacent paddocks. The troughs will be raised to prevent “boggy areas” from forming around the trough. Since the area around the troughs will be of a higher use, Sleepy Creek proposes to periodically remove accumulated manure, and re-grade if necessary. Other cattle support items, including feed bunkers and shade structures are portable and can be moved as conditions demand. Forage Crop Production The primary forage crop on the irrigated pastures is to be Bermuda grass. Bermuda grass or other grass types tolerant of drier conditions will be used in unirrigated pastures. During the winter, when Bermuda grass stops growing, Sleepy Creek will overseed the North Tract pastures with ryegrass or other winter crops. Due to the limitation on irrigation water, the East Tract NMP calls for no over-seeding for production of winter crops. Crops do not grow uniformly during the course of a year. Rather, there are periods during which there are excess crops, and periods during which the crops are not growing enough to keep up with the needs of the cattle. During periods of excess, Sleepy Creek will cut those crops and store them as haylage to be fed to the cattle during lower growth periods. The North Tract management plan allows Sleepy Creek to dedicate one or more irrigated pastures for the exclusive production of haylage. If that option is used, cattle numbers will be reduced in proportion to the number of pastures dedicated to haylage production. As a result of the limit on irrigation, the East Tract NMP does not recommend growing supplemental feed on dedicated irrigation pivot pastures. Direct Wetland Impacts Approximately 100 acres proposed for irrigation are wetlands or wetland buffer. Those areas are predominantly isolated wetlands, though some have surface water connections to Mill Creek, a water of the state. Trees will be cut in the wetlands to allow the pivot to pass overhead. Tree cutting is an exempt agricultural activity that does not require a permit. There was no persuasive evidence that cutting trees will alter the fundamental benefit of the wetlands or damage water resources of the District. The wetlands and wetland buffer will be subject to the same watering and fertigation regimen as the irrigated pastures. The application of water to wetlands, done concurrently with the application of water to the pastures, will occur during periods in which the pasture soils are dry. The incidental application of water to the wetlands during dry periods will serve to maintain hydration of the wetlands, which is considered to be a benefit. Fertilizers will be applied through the irrigation arms, a process known as fertigation. Petitioners asserted that the application of fertilizer onto the wetlands beneath the pivot arms could result in some adverse effects to the wetlands. However, Petitioners did not quantify to what extent the wetlands might be affected, or otherwise describe the potential effects. Fertigation of the wetlands will promote the growth of wetland plants. Nitrogen applied through fertigation will be taken up by plants, or will be subject to denitrification -- a process discussed in greater detail herein -- in the anaerobic wetland soils. The preponderance of the evidence indicated that enhanced wetland plant growth would not rise to a level of concern. Since most of the affected wetlands are isolated wetlands, there is expected to be little or no discharge of nutrients from the wetlands. Even as to those wetlands that have a surface water connection, most, if not all of the additional nitrogen applied through fertigation will be accounted for by the combined effect of plant uptake and denitrification. Larger wetland areas within an irrigated pasture will be fenced at the buffer line to prevent cattle from entering. The NMP provided a blow-up of the proposed fencing related to a larger wetland on Pivot 8. Although other figures are not to the same scale, it appears that larger wetlands associated with Pivots 1, 2, 3, and 12 will be similarly fenced. Cattle would be allowed to go into the smaller, isolated wetlands. Cattle going into wetlands do not necessarily damage the wetlands. Any damage that may occur is a function of density, duration, and the number of cattle. The only direct evidence of potential damage to wetlands was the statement that “[i]f you have 6,371 [cattle] go into a wetland, there may be impacts.” The NMP provides that pasture use will be limited to herds of approximately 190 cattle, which will be rotated from paddock to paddock every two to three days, and which will allow for “rest” periods of approximately 20 days. There will be no travel lanes through any wetland. Thus, there is no evidence to support a finding that the cattle at the density, duration, and number proposed will cause direct adverse effects to wetlands on the property. High Concentration Areas Cattle brought to the facility are to be unloaded from trucks and temporarily corralled for inspection. For that period, the cattle will be tightly confined. Cattle that have reached their slaughter weight will be temporarily held in corrals associated with the processing plant. The stormwater retention ponds used to capture and store runoff from the offloading corral and the processing plant holding corral are part of a normal and customary agricultural activity, and are not part of the applications and approvals that are at issue in this proceeding. The retention ponds associated with the high-intensity areas do not require permits because they do not exceed one acre in size or impound more than 40 acre-feet of water. Nonetheless, issues related to the retention ponds were addressed by Petitioners and Sleepy Creek, and warrant discussion here. The retention ponds are designed to capture 100 percent of the runoff and entrained nutrients from the high concentration areas for a minimum of a 24—hour/25—year storm event. If rainfall occurs in excess of the designed storm, the design is such that upon reaching capacity, only new surface water coming to the retention pond will be discharged, and not that containing high concentrations of nutrients from the initial flush of stormwater runoff. Unlike the stormwater retention berms for the pastures, which are to be constructed from the first nine inches of permeable topsoil on the property, the corral retention ponds are to be excavated to a depth of six feet which, based on soil borings in the vicinity, will leave a minimum of two to four feet of clay beneath the retention ponds. In short, the excavation will penetrate into the clay layer underlying the pond sites, but will not penetrate through that layer. The excavated clay will be used to form the side slopes of the ponds, lining the permeable surficial layer and generally making the ponds impermeable. Organic materials entering the retention ponds will form an additional seal. An organic seal is important in areas in which retention ponds are constructed in sandy soil conditions. Organic sealing is less important in this case, where clay forms the barrier preventing nutrients from entering the surficial aquifer. Although the organic material is subject to periodic removal, the clay layer will remain to provide the impermeable barrier necessary to prevent leakage from the ponds. Dr. Bottcher testified that if, during excavation of the ponds, it was found that the remaining in-situ clay layer was too thin, Sleepy Creek would implement the standard practice of bringing additional clay to the site to ensure adequate thickness of the liner. Nutrient Balance The goal of the NMP is to create a balance of nutrients being applied to and taken up from the property. Nitrogen and phosphorus are the nutrients of primary concern, and are those for which specific management standards are proposed. Nutrient inputs to the NMP consist generally of deposition of cattle manure (which includes solid manure and urine), recycling of plant material and roots from the previous growing season, and application of supplemental fertilizer. Nutrient outputs to the NMP consist generally of volatization of ammonia to the atmosphere, uptake and utilization of the nutrients by the grass and crops, weight gain of the cattle, and absorption and denitrification of the nutrients in the soil. The NMP, and the various models discussed herein, average the grass and forage crop uptake and the manure deposition to match that of a 1,013 pound animal. That average weight takes into account the fact that cattle on the property will range from calf weight of approximately 850 pounds, to slaughter weight of 1150 pounds. Nutrients that are not accounted for in the balance, e.g., those that become entrained in stormwater or that pass through the plant root zone without being taken up, are subject to runoff to surface waters or discharge to groundwater. Generally, phosphorus not taken up by crops remains immobile in the soil. Unless there is a potential for runoff to surface waters, the nutrient balance is limited by the amount of nitrogen that can be taken up by the crops. Due to the composition of the soils on the property, the high water table, and the relatively shallow confining layer, there is a potential for surface runoff. Thus, the NMP was developed using phosphorus as the limiting nutrient, which results in nutrient application being limited by the “P-index.” A total of 108 pounds of phosphorus per acre/per year can be taken up and used by the irrigated pasture grasses and forage crops. Therefore, the total number of cattle that can be supported on the irrigated pastures is that which, as a herd, will deposit an average of 108 pounds of phosphorus per year over the irrigated acreage. Therefore, Sleepy Creek has proposed a herd size and density based on calculations demonstrating that the total phosphorus contained in the waste excreted by the cattle equals the amount taken up by the crops. A herd producing 108 pounds per acre per year of phosphorus is calculated to produce 147 pounds of nitrogen per acre per year. The Bermuda grass and forage crops proposed for the irrigated fields require 420 pounds of nitrogen per acre per year. As a result of the nitrogen deficiency, additional nitrogen-based fertilizer to make up the shortfall is required to maintain the crops. Since phosphorus needs are accounted for by animal deposition, the fertilizer will have no phosphorus. The NMP requires routine soil and plant tissue tests to determine the amount of nitrogen fertilizer needed. By basing the application of nitrogen on measured rather than calculated needs, variations in inputs, including plant decomposition and atmospheric deposition, and outputs, including those affected by weather, can be accounted for, bringing the full nutrient balance into consideration. The numeric values for crop uptakes, manure deposition, and other estimates upon which the NMP was developed were based upon literature, values, and research performed and published by the University of Florida and the Natural Resource Conservation Service. Dr. Bottcher testified convincingly that the use of such values is a proven and reliable method of developing a balance for the operation of similar agricultural operations. A primary criticism of the NMP was its expressed intent to “reduce” or “minimize” the transport of nutrients to surface waters and groundwater, rather than to “negate” or “prevent” such transport. Petitioners argue that complete prevention of the transport of nutrients from the property is necessary to meet the standards necessary for issuance of the CUP and ERP. Mr. Drummond went into some detail regarding the total mass of nutrients expected to be deposited onto the ground from the cattle, exclusive of fertilizer application. In the course of his testimony, he suggested that the majority of the nutrients deposited on the land surface “are going to make it to the surficial aquifer and then be carried either to the Floridan or laterally with the groundwater flow.” However, Mr. Drummond performed no analysis on the fate of nitrogen through uptake by crops, volatization, or soil treatment, and did not quantify the infiltration of nitrogen to groundwater. Furthermore, he was not able to provide any quantifiable estimate on any effect of nutrients on Mill Creek, the Ocklawaha River, or Silver Springs. In light of the effectiveness of the nutrient balance and other elements of the NMP, along with the retention berm system that will be discussed herein, Mr. Drummond’s assessment of the nutrients that might be expected to impact water resources of the District is contrary to the greater weight of the evidence. Mr. Drummond’s testimony also runs counter to that of Dr. Kincaid, who performed a particle track analysis of the fate of water recharge from the North Tract. In short, Dr. Kincaid calculated that of the water that makes it as recharge from the North Tract to the surficial aquifer, less than one percent is expected to make its way to the upper Floridan aquifer, with that portion originating from the vicinity of Pivot 6. Recharge from the other 14 irrigated pastures was ultimately accounted for by evapotranspiration or emerged at the surface and found its way to Mill Creek. The preponderance of the competent, substantial evidence adduced at the final hearing supports the effectiveness of the NMPs for the North Tract and East Tract at managing the application and use of nutrients on the property, and minimizing the transport of nutrients to surface water and groundwater resources of the District. North Central Florida Model All of the experts involved in this proceeding agreed that the use of groundwater models is necessary to simulate what might occur below the surface of the ground. Models represent complex systems by applying data from known conditions and impacts measured over a period of years to simulate the effects of new conditions. Models are imperfect, but are the best means of predicting the effects of stresses on complex and unseen subsurface systems. The North Central Florida (NCF) model is used to simulate impacts of water withdrawals on local and regional groundwater levels and flows. The NCF model simulates the surficial aquifer, the upper Floridan aquifer, and the lower Floridan aquifer. Those aquifers are separated from one another by relatively impervious confining units. The intermediate confining unit separates the surficial aquifer from the upper Floridan aquifer. The intermediate confining unit is not present in all locations simulated by the NCF model. However, the evidence is persuasive that the intermediate confining unit is continuous at the North Tract, and serves to effectively isolate the surficial aquifer from the upper Floridan aquifer. The NCF model is not a perfect depiction of what exists under the land surface of the North Tract or elsewhere. It was, however, acknowledged by the testifying experts in this case, despite disagreements as to the extent of error inherent in the model, to be the best available tool for calculating the effects of withdrawals of water within the boundary of the model. The NCF model was developed and calibrated over a period of years, is updated routinely as data becomes available, and has undergone peer review. Aquifer Performance Tests In order to gather site-specific data regarding the characteristics of the aquifer beneath the Sleepy Creek property, a series of three aquifer performance tests (APTs) was conducted on the North Tract. The first two tests were performed by Sleepy Creek, and the third by the District. An APT serves to induce stress on the aquifer by pumping from a well at a high rate. By observing changes in groundwater levels in observation wells, which can be at varying distances from the extraction well, one can extrapolate the nature of the subsurface. In addition, well-completion reports for the various withdrawal and observation wells provide actual data regarding the composition of subsurface soils, clays, and features of the property. The APT is particularly useful in evaluating the ability of the aquifer to produce water, and in calculating the transmissivity of the aquifer. Transmissivity is a measure of the rate at which a substance passes through a medium and, as relevant to this case, measures how groundwater flows through an aquifer. The APTs demonstrated that the Floridan aquifer is capable of producing water at the rate requested. The APT drawdown contour measured in the upper Floridan aquifer was greater than that predicted from a simple run of the NCF model, but the lateral extent of the drawdown was less than predicted. The most reasonable conclusion to be drawn from the combination of greater than expected drawdown in the upper Floridan aquifer with less than expected extent is that the transmissivity of the aquifer beneath the North Tract is lower than the NCF model assumptions. The conclusion that the transmissivity of the aquifer at the North Tract is lower than previously estimated means that impacts from groundwater extraction would tend to be more vertical than horizontal, i.e., the drawdown would be greater, but would be more localized. As such, for areas of lower than estimated transmissivity, modeling would over-estimate off-site impacts from the extraction. NCF Modeling Scenarios The initial NCF modeling runs were based on an assumed withdrawal of 2.39 mgd, an earlier -- though withdrawn - - proposal. The evidence suggests that the simulated well placement for the 2.39 mgd model run was entirely on the North Tract. Thus, the results of the model based on that withdrawal have some limited relevance, especially given that the proposed CUP allows for all of the requested 1.46 mgd of water to be withdrawn from North Tract wells at the option of Sleepy Creek, but will over-predict impacts from the permitted rate of withdrawal. A factor that was suggested as causing a further over-prediction of drawdown in the 2.39 mgd model run was the decision, made at the request of the District, to exclude the input of data of additional recharge to the surficial aquifer, wetlands and surface waters from the irrigation, and the resulting diminution in soil storage capacity. Although there is some merit to the suggestion that omitting recharge made the model results “excessively conservative,” the addition of recharge to the model would not substantially alter the predicted impacts. A model run was subsequently performed based on a presumed withdrawal of 1.54 mgd, a rate that remains slightly more than, but still representative of, the requested amount of 1.46 mgd. The 1.54 mgd model run included an input for irrigation recharge. The simulated extraction points were placed on the East Tract and North Tract in the general configuration as requested in the CUP application. The NCF is designed to model the impacts of a withdrawal based upon various scenarios, identified at the hearing as Scenarios A, B, C, and D. Scenario A is the baseline condition for the NCF model, and represents the impacts of all legal users of water at their estimated actual flow rates as they existed in 1995. Scenario B is all existing users, not including the applicant, at end-of-permit allocations. Scenario C is all existing users, including the applicant, at current end-of-permit allocations. Scenario D is all permittees at full allocation, except the applicant which is modeled at the requested (i.e., new or modified) end-of-permit allocation. To simulate the effects of the CUP modification, simulations were performed on scenarios A, C, and D. In order to measure the specific impact of the modification of the CUP, the Scenario C impacts to the surficial, upper Floridan, and lower Floridan aquifers were compared with the Scenario D impacts to those aquifers. In order to measure the cumulative impact of the CUP, the Scenario A actual-use baseline condition was compared to the Scenario D condition which predicts the impacts of all permitted users, including the applicant, pumping at full end-of-permit allocations. The results of the NCF modeling indicate the following: 2.39 mgd - Specific Impact The surficial aquifer drawdown from the simulated 2.39 mgd withdrawal was less than 0.05 feet on-site and off- site, except to the west of the North Tract, at which a drawdown of 0.07 feet was predicted. The upper Floridan aquifer drawdown from the 2.39 mgd withdrawal was predicted at between 0.30 and 0.12 feet on-site, and between 0.30 and 0.01 feet off-site. The higher off-site figures are immediately proximate to the property. The lower Floridan aquifer drawdown from the 2.39 mgd withdrawal was predicted at less than 0.05 feet at all locations, and at or less than 0.02 feet within six miles of the North Tract. 2.39 mgd - Cumulative Impact The cumulative impact to the surficial aquifer from all permitted users, including a 2.39 mgd Sleepy Creek withdrawal, was less than 0.05 feet on-site, and off-site to the north and east, except to the west of the North Tract, at which a drawdown of 0.07 feet was predicted. The cumulative impact to the upper Floridan aquifer from all permitted users, including a 2.39 mgd Sleepy Creek withdrawal, ranged from 0.4 feet to 0.8 feet over all pertinent locations. The cumulative impact to the lower Floridan aquifer from all permitted users, including a 2.39 mgd Sleepy Creek withdrawal, ranged from 1.0 to 1.9 feet over all pertinent locations. The conclusion drawn by Mr. Andreyev that the predicted impacts to the lower Floridan are almost entirely from other end-of-permit user withdrawals is supported by the evidence and accepted. 1.54 mgd - Specific Impact The NCF model runs based on the more representative 1.54 mgd withdrawal predicted a surficial aquifer drawdown of less than 0.01 feet (i.e., no drawdown contour shown) on the North Tract, and a 0.01 to 0.02 foot drawdown at the location of the East Tract. The drawdown of the upper Floridan aquifer from the CUP modification was predicted at up to 0.07 feet on the property, and generally less than 0.05 feet off-site. There were no drawdown contours at the minimum 0.01 foot level that came within 9 miles of Silver Springs. The lower Floridan aquifer drawdown from the CUP modification was predicted at less than 0.01 feet (i.e., no drawdown contour shown) at all locations. 1.54 mgd - Cumulative Impact A comparison of the cumulative drawdown contours for the 2.36 mgd model and 1.54 mgd model show there to be a significant decrease in predicted drawdowns to the surficial and upper Floridan aquifers, with the decrease in the upper Floridan aquifer drawdown being relatively substantial, i.e., from 0.5 to 0.8 feet on-site predicted for the 2.36 mgd withdrawal, to 0.4 to 0.5 feet on-site for the 1.54 mgd model. Given the small predicted individual impact of the CUP on the upper Floridan aquifer, the evidence is persuasive that the cumulative impacts are the result of other end-of-permit user withdrawals. The drawdown contour for the lower Floridan aquifer predicted by the 1.54 mgd model is almost identical to that of the 2.36 mgd model, thus supporting the conclusion that predicted impacts to the lower Floridan are almost entirely from other end-of-permit user withdrawals. Modeled Effect on Silver Springs As a result of the relocation of the extraction wells from the East Tract to the North Tract, the NCF model run at the 1.54 mgd withdrawal rate predicted springflow at Silver Springs to increase by 0.15 cfs. The net cumulative impact in spring flow as measured from 1995 conditions to the scenario in which all legal users, including Sleepy Creek, are pumping at full capacity at their end-of-permit rates for one year3/ is roughly 35.4 cfs, which is approximately 5 percent of Silver Springs’ current flow. However, as a result of the redistribution of the Sleepy Creek withdrawal, which is, in its current iteration, a legal and permitted use, the cumulative effect of the CUP modification at issue is an increase in flow of 0.l5 cfs. Dr. Kincaid agreed that there is more of an impact to Silver Springs when the pumping allowed by the CUP is located on the East Tract than there is on the North Tract, but that the degree of difference is very small. Dr. Knight testified that effect on the flow of Silver Springs from relocating the 1.46 mgd withdrawal from the East Tract to the North Tract would be “zero.” The predicted increase of 0.15 cfs is admittedly miniscule when compared to the current Silver Springs springflow of approximately 675 cfs. However, as small as the modeled increase may be -- perhaps smaller than its “level of certainty” -- it remains the best evidence that the impact of the CUP modification to the flow of Silver Springs will be insignificant at worst, and beneficial at best. Opposition to the NCF Model Petitioners submitted considerable evidence designed to call the results generated by the District’s and Sleepy Creek’s NCF modeling into question. Karst Features A primary criticism of the validity of the NCF model was its purported inability to account for the presence of karst features, including conduits, and their effect on the results. It was Dr. Kincaid’s opinion that the NCF model assigned transmissivity values that were too high, which he attributed to the presence of karst features that are collecting flow and delivering it to springs. He asserted that, instead of assuming the presence of karst features, the model was adjusted to raise the overall capacity of the porous medium to transmit water, and thereby match the observed flows. In his opinion, the transmissivity values of the equivalent porous media were raised so much that the model can no longer be used to predict drawdowns. That alleged deficiency in the model is insufficient for two reasons. First, as previously discussed in greater detail, the preponderance of the evidence in this case supports a finding that there are no karst features in the vicinity of the North Tract that would provide preferential pathways for water flow so as to skew the results of the NCF model. Second, Dr. Kincaid, while acknowledging that the NCF model is the best available tool for predicting impacts from groundwater extraction on the aquifer, suggested that a hybrid porous media and conduit model would be a better means of predicting impacts, the development of which would take two years or more. There is no basis for the establishment of a de facto moratorium on CUP permitting while waiting for the development of a different and, in this case, unnecessary model. For the reasons set forth herein, it is found that the NCF model is sufficient to accurately and adequately predict the effects of the Sleepy Creek groundwater withdrawals on the aquifers underlying the property, and to provide reasonable assurance that the standards for such withdrawals have been met. Recharge to the Aquifer Petitioners argued that the modeling results showing little significant drawdown were dependent on the application of unrealistic values for recharge or return flow from irrigation. In a groundwater model, as in the physical world, some portion of the water extracted from the aquifer is predicted to be returned to the aquifer as recharge. If more water is applied to the land surface than is being accounted for by evaporation, plant uptake and evapotranspiration, surface runoff, and other processes, that excess water may seep down into the aquifer as recharge. Recharge serves to replenish the aquifer and offset the effects of the groundwater withdrawal. Dr. Kincaid opined that the NCF modeling performed for the CUP application assigned too much water from recharge, offsetting the model's prediction of impacts to other features. It is reasonable to assume that there is some recharge associated with both agricultural and public supply uses. However, the evidence suggests that the impact of recharge on the overall NCF model results is insignificant on the predicted impacts to Silver Springs, the issue of primary concern. Mr. Hearn ran a simulation using the NCF model in which all variables were held constant, except for recharge. The difference between the “with recharge” and “without recharge" simulations at Silver Springs was 0.002 cfs. That difference is not significant, and is not suggestive of adverse impacts on Silver Springs from the CUP modification. Dr. Kincaid testified that “the recharge offset on the property is mostly impacting the surficial aquifer,” and that “the addition of recharge in this case didn't have much of an impact on the upper Floridan aquifer system.” As such, the effect of adding recharge to the model would be as to the effect of groundwater withdrawal on wetlands or surface water bodies, and not on springs. As previously detailed, the drawdown of the surficial aquifer simulated for the 2.39 mgd “no recharge” scenario were less than 0.05 feet on-site and off-site, except for a predicted 0.07 foot drawdown to the west of the North Tract. The predicted drawdown of the surficial aquifer for the 1.54 mgd “with recharge” scenario was 0.02 feet or less. The preponderance of the evidence supports a finding that drawdowns of either degree are less than that at which adverse impacts to wetlands or surface waters would occur. Thus, issues related to the recharge or return flows from irrigation are insufficient to support a finding or conclusion that the NCF model failed to provide reasonable assurance that the standards for issuance of the CUP modification were met. External Boundaries The boundaries of the NCF model are not isolated from the rest of the physical world. Rather, groundwater flows into the modeled area from multiple directions, and out of the modeled area in multiple directions. Inflows to the model area are comprised of recharge, which is an assigned value, and includes water infiltrating and recharging the aquifer from surface waters; injection wells; upward and downward leakage from lower aquifers; and flow across the external horizontal boundaries. Outflows from the model area include evapotranspiration; discharge to surface waters, including springs and rivers; extraction from wells; upward and downward leakage from lower aquifers; and flow against the external model boundaries. Dr. Kincaid testified that flow across the external model boundary is an unknown and unverifiable quantity which increases the uncertainty in the model. He asserted that in the calibrated version of the model, there is no way to check those flows against data. His conclusion was that the inability of the NCF model to accurately account for external boundary flow made the margin of error so great as to make the model an unreliable tool with which to assess whether the withdrawal approved by the proposed CUP modification will increase or decrease drawdown at Silver Springs. The District correlates the NCF model boundaries with a much larger model developed by the United States Geological Survey, the Peninsula of Florida Model, more commonly referred to as the Mega Model, which encompasses most of the State of Florida and part of Southeast Georgia. The Mega Model provides a means to acknowledge that there are stresses outside the NCF model, and to adjust boundary conditions to account for those stresses. The NCF is one of several models that are subsets of the Mega Model, with the grids of the two models being “nested” together. The 1995 base year of the NCF model is sufficiently similar to the 1993-1994 base year of the Mega Model as to allow for a comparison of simulated drawdowns calculated by each of the models. By running a Mega Model simulation of future water use, and applying the change in that use from 1993 base year conditions, the District was able to come to a representative prediction of specific boundary conditions for the 1995 NCF base year, which were then used as the baseline for simulations of subsequent conditions. In its review of the CUP modification, the District conducted a model validation simulation to measure the accuracy of the NCF model against observed conditions, with the conditions of interest being the water flow at Silver Springs. The District ran a simulation using the best information available as to water use in the year 2010, the calculated boundary conditions, irrigation, pumping, recharge, climatic conditions, and generally “everything that we think constitutes that year.” The discharge of water at Silver Springs in 2010 was measured at 580 cfs. The discharge simulated by the NCF model was 545 cfs. Thus, the discharge predicted by the NCF model simulation was within six percent of the observed discharge. Such a result is generally considered in the modeling community to be “a home run.” Petitioners’ objections to the calculation of boundary conditions for the NCF model are insufficient to support a finding that the NCF model is not an appropriate and accurate tool for determining that reasonable assurance has been provided that the standards for issuance of the CUP modification were met. Cumulative Impact Error As part of the District’s efforts to continually refine the NCF, and in conjunction with a draft minimum flows and levels report for Silver Springs and the Silver River, the cumulative NCF model results for the period of baseline to 2010 were compared with the simulated results from the Northern District Model (NDF), a larger model that overlapped the NCF. As a result of the comparison, which yielded different results, it was discovered that the modeler had “turned off” not only the withdrawal pumps, but inputs to the aquifer from drainage wells and sinkholes as well. When those inputs were put back into the model run, and effects calculated only from withdrawals between the “pumps-off” condition and 2010 pumping conditions, the cumulative effect of the withdrawals was adjusted from a reduction in the flow at Silver Springs of 29 cfs to a reduction of between 45 and 50 cfs, an effect described as “counterintuitive.” Although that result has not undergone peer review, and remains subject to further review and comparison with the Mega Model, it was accepted by the District representative, Mr. Bartol. Petitioners seized upon the results of the comparison model run as evidence of the inaccuracy and unreliability of the NCF model. However, the error in the NCF model run was not the result of deficiencies in the model, but was a data input error. Despite the error in the estimate of the cumulative effect of all users at 2010 levels, the evidence in this case does not support a finding that the more recent estimates of specific impact from the CUP at issue were in error. NCF Model Conclusion As has been discussed herein, a model is generally the best means by which to calculate conditions and effects that cannot be directly observed. The NCF model is recognized as being the best tool available for determining the subsurface conditions of the model domain, having been calibrated over a period of years and subject to peer review. It should be recognized that the simulations run using the NCF model represent the worst—case scenario, with all permittees simultaneously drawing at their full end-of-permit allocations. There is merit to the description of that occurrence as being “very remote.” Thus, the results of the modeling represent a conservative estimate of potential drawdown and impacts. While the NCF model is subject to uncertainty, as is any method of predicting the effects of conditions that cannot be seen, the model provides reasonable assurance that the conditions simulated are representative of the conditions that will occur as a result of the withdrawals authorized by the CUP modification. Environmental Resource Permit The irrigation proposed by the CUP will result in runoff from the North Tract irrigated pastures in excess of that expected from the improved pastures, due in large measure to the diminished storage capacity of the soil. Irrigation water will be applied when the soils are dry, and capable of absorbing water not subject to evaporation or plant uptake. The irrigation water will fill the storage space that would exist without irrigation. With irrigation water taking up the capacity of the soil to hold water, soils beneath the irrigation pivots will be less capable of retaining additional moisture during storm events. Thus, there is an increased likelihood of runoff from the irrigated pastures over that expected with dry soils. The increase in runoff is expected to be relatively small, since there should be little or no irrigation needed during the normal summer wet season. The additional runoff may have increased nutrient levels due to the increased cattle density made possible by the irrigation of the pastures. The CUP has a no—impact requirement for water quality resulting from the irrigation of the improved pasture. Thus, nutrients leaving the irrigated pastures may not exceed those calculated to be leaving the existing pre-development use as improved pastures. Retention Berms The additional runoff and nutrient load is proposed to be addressed by constructing a system of retention berms, approximately 50,0004/ feet in length, which is intended to intercept, retain, and provide treatment for runoff from the irrigated pasture. The goal of the system is to ensure that post—development nutrient loading from the proposed irrigated pastures will not exceed the pre—development nutrient loading from the existing improved pastures. An ERP permit is required for the construction of the berm system, since the area needed for the construction of the berms is greater than the one acre in size, and since the berms have the capability of impounding more than 40 acre-feet of water. The berms are to be constructed by excavating the top nine inches of sandy, permeable topsoil and using that permeable soil to create the berms, which will be 1 to 2 feet in height. The water storage areas created by the excavation will have flat or horizontal bottoms, and will be very shallow with the capacity to retain approximately a foot of water. The berms will be planted with pasture grasses after construction to provide vegetative cover. The retention berm system is proposed to be built in segments, with the segment designed to capture runoff from a particular center pivot pasture to be constructed prior to the commencement of irrigation from that center pivot. A continuous clay layer underlies the areas in which the berms are to be constructed. The clay layer varies from 18 to 36 inches below the ground surface, with at least one location being as much as five feet below the ground surface. As such, after nine inches of soil is scraped away to create the water retention area and construct the berm, there will remain a layer of permeable sandy material above the clay. The berms are to be constructed at least 25 feet landward of any jurisdictional wetland, creating a “safe upland line.” Thus, the construction, operation, and maintenance of the retention berms and redistribution swales will result in no direct impacts to jurisdictional wetlands or other surface waters. There will be no agricultural activities, e.g., tilling, planting, or mowing, within the 25-foot buffers, and the buffers will be allowed to establish with native vegetation to provide additional protection for downgradient wetlands. As stormwater runoff flows from the irrigated pastures, it may, in places, create concentrated flow ways. Redistribution swales will be built in those areas to spread any remaining overland flow of water and reestablish sheet flow to the retention berm system. At any point at which water may overtop a berm, the berm will be hardened with rip—rap to insure its integrity. The berms are designed to intercept and collect overland flow from the pastures and temporarily store it behind the berms, regaining the soil storage volume lost through irrigation. A portion of the runoff intercepted by the berm system will evaporate. The majority will infiltrate either through the berm, or vertically into the subsurface soils beneath it. When the surficial soils become saturated, further vertical movement will be stopped by the impermeable clay layer underlying the site. The runoff water will then move horizontally until it reemerges into downstream wetland systems. Thus, the berm system is not expected to have a measurable impact on the hydroperiod of the wetlands on the North Tract. Phosphorus Removal Phosphorus tends to get “tied up” in soil as it moves through it. Phosphorus reduction occurs easily in permeable soil systems because it is removed from the water through a chemical absorption process that is not dependent on the environment of the soil. As the soils in the retention areas and berms go through drying cycles, the absorption capacity is regenerated. Thus, the retention system will effectively account for any increase in phosphorus resulting from the increased cattle density allowed by the irrigation such that there is expected to be no increase in phosphorus levels beyond the berm. Nitrogen Removal When manure is deposited on the ground, primarily as high pH urine, the urea is quickly converted to ammonia, which experiences a loss of 40 to 50 percent of the nitrogen to volatization. Soil conditions during dry weather conditions are generally aerobic. Remaining ammonia in the manure is converted by aerobic bacteria in the soil to nitrates and nitrites. Converted nitrates and nitrites from manure, along with nitrogen from fertilizer, is readily available for uptake as food by plants, including grasses and forage crops. Nitrates and nitrites are mobile in water. Therefore, during rain events of sufficient intensity to create runoff, the nitrogen can be transported downstream towards wetlands and other receiving waters, or percolate downward through the soil until blocked by an impervious barrier. During storm events, the soils above the clay confining layer and the lower parts of the pervious berms become saturated. Those saturated soils are drained of oxygen and become anaerobic. When nitrates and nitrites encounter saturated conditions, they provide food for anaerobic bacteria that exist in those conditions. The bacteria convert nitrates and nitrites to elemental nitrogen, which has no adverse impact on surface waters or groundwater. That process, known as denitrification, is enhanced in the presence of organic material. The soils from which the berms are constructed have a considerable organic component. In addition to the denitrification that occurs in the saturated conditions in and underlying the berms, remaining nitrogen compounds that reemerge into the downstream wetlands are likely to encounter organic wetland-type soil conditions. Organic wetland soils are anaerobic in nature, and will result in further, almost immediate denitrification of the nitrates and nitrites in the emerging water. Calculation of Volume - BMPTRAINS Model The calculation of the volume necessary to capture and store excess runoff from the irrigated pastures was performed by Dr. Wanielista using the BMPTRAINS model. BMPTRAINS is a simple, easy to use spreadsheet model. Its ease of use does not suggest that it is less than reliable. The model has been used as a method of calculating storage volumes in many conditions over a period of more than 40 years. The model was used to calculate the storage volumes necessary to provide storage and treatment of runoff from fifteen “basins” that had a control or a Best Management Practice associated with them. All of the basins were calculated as being underlain by soils in poorly-drained hydrologic soil Group D, except for the basin in the vicinity of Pivot 6, which is underlain by the more well-drained soil Group A. The model assumed about percent of the property to have soil Group A soils, an assumption that is supported by the evidence. Soil moisture conditions on the property were calculated by application of data regarding rainfall events and times, the irrigation schedule, and the amount of irrigation water projected for use over a year. The soil moisture condition was used to determine the amount of water that could be stored in the on-site soils, known as the storage coefficient. Once the storage coefficient was determined, that data was used to calculate the amount of water that would be expected to run off of the North Tract, known as the curve number. The curve number is adjusted by the extent to which the storage within a soil column is filled by the application of irrigation water, making it unable to store additional rainfall. As soil storage goes down, the curve number goes up. Thus, a curve number that approaches 100 means that more water is predicted to run off. Conversely, a lower curve number means that less water is predicted to run off. The pre-development curve number for the North Tract was based on the property being an unirrigated, poor grass area. A post-development curve number was assigned to the property that reflected a wet condition representative of the irrigated soils beneath the pivots. In calculating the storage volume necessary to handle runoff from the basins, the wet condition curve number was adjusted based on the fact that there is a mixture of irrigated and unirrigated general pasture within each basin to be served by a segment of the retention berm system, and by the estimated 15 percent of the time that the irrigation areas would be in a drier condition. In addition, the number was adjusted to reflect the 8 to 10 inches of additional evapotranspiration that occurs as a result of irrigation. The BMPTRAINS model was based on average annual nutrient-loading conditions, with water quality data collected at a suitable point within Reach 22, the receiving waterbody. The effects of nutrients from the irrigated pastures on receiving waterbodies is, in terms of the model, best represented by average annual conditions, rather than a single highest-observed nutrient value. Pre-development loading figures were based on the existing use of the property as unirrigated general pasture. The pre-development phosphorus loading figure was calculated at an average event mean concentration (EMC) of 0.421 milligrams per liter (mg/l). The post—condition phosphorus loading figure was calculated at an EMC of 0.621 mg/l. Therefore, in order to achieve pre-development levels of phosphorus, treatment to achieve a reduction in phosphorus of approximately 36 percent was determined to be necessary. The pre-development nitrogen loading figure was calculated at an EMC of 2.6 mg/l. The post—condition nitrogen loading figure was calculated at an EMC of 3.3 mg/l. Therefore, in order to achieve pre-development levels of nitrogen, treatment to achieve a reduction in nitrogen of approximately 25 percent was determined to be necessary. The limiting value for the design of the retention berms is phosphorus. To achieve post-development concentrations that are equal to or less than pre-development concentrations, the treatment volume of the berm system must be sufficient to allow for the removal of 36 percent of the nutrients in water being retained and treated behind the berms, which represents the necessary percentage of phosphorus. In order to achieve the 36 percent reduction required for phosphorus, the retention berm system must be capable of retaining approximately 38 acre—feet of water from the 15 basins. In order to achieve that retention volume, a berm length of approximately 50,000 linear feet was determined to be necessary, with an average depth of retention behind the berms of one foot. The proposed length of the berms is sufficient to retain the requisite volume of water to achieve a reduction in phosphorus of 36 percent. Thus, the post-development/irrigation levels of phosphorus from runoff are expected to be no greater than pre-development/general pasture levels of phosphorus from runoff. By basing the berm length and volume on that necessary for the treatment of phosphorus, there will be storage volume that is greater than required for a 25 percent reduction in nitrogen. Thus, the post-development/irrigation levels of nitrogen from runoff are expected to be less than pre- development/general pasture levels of nitrogen from runoff. Mr. Drummond admitted that the design of the retention berms “shows there is some reduction, potentially, but it's not going to totally clean up the nutrients.” Such a total clean-up is not required. Rather, it is sufficient that there is nutrient removal to pre-development levels, so that there is no additional pollutant loading from the permitted activities. Reasonable assurance that such additional loading is not expected to occur was provided. Despite Mr. Drummond’s criticism of the BMPTRAINS model, he did not quantify nutrient loading on the North Tract, and was unable to determine whether post-development concentrations of nutrients would increase over pre-development levels. As such, there was insufficient evidence to counter the results of the BMPTRAINS modeling. Watershed Assessment Model In order to further assess potential water quantity and water quality impacts to surface water bodies, and to confirm stormwater retention area and volume necessary to meet pre-development conditions, Sleepy Creek utilized the Watershed Assessment Model (WAM). The WAM is a peer-reviewed model that is widely accepted by national, state, and local regulatory entities. The WAM was designed to simulate water balance and nutrient impacts of varying land uses. It was used in this case to simulate and provide a quantitative measure of the anticipated impacts of irrigation on receiving water bodies, including Mill Creek, Daisy Creek, the Ocklawaha River, and Silver Springs. Inputs to the model include land conditions, soil conditions, rain and climate conditions, and water conveyance systems found on the property. In order to calculate the extent to which nutrients applied to the land surface might affect receiving waters, a time series of surface water and groundwater flow is “routed” through the modeled watershed and to the various outlets from the system, all of which have assimilation algorithms that represent the types of nutrient uptakes expected to occur as water goes through the system. Simulations were performed on the North Tract in its condition prior to acquisition by Sleepy Creek, in its current “exempted improved pasture condition,” and in its proposed “post—development” pivot-irrigation condition. The simulations assessed impacts of the site conditions on surface waters at the point at which they leave the property and discharge to Mill Creek, and at the point where Mill Creek merges into the Ocklawaha River. The baseline condition for measuring changes in nutrient concentrations was determined to be that lawfully existing at the time the application was made. Had there been any suggestion of illegality or impropriety in Sleepy Creek’s actions in clearing the timber and creating improved pasture, a different baseline might be warranted. However, no such illegality or impropriety was shown, and the SJRWMD rules create no procedure for “looking back” to previous land uses and conditions that were legally changed. Thus, the “exempted improved pasture condition” nutrient levels are appropriate for comparison with irrigated pasture nutrient levels. The WAM simulations indicated that nitrogen resulting from the irrigation of the North Tract pastures would be reduced at the outflow to Mill Creek at the Reach 22 stream segment from improved pasture levels by 1.7 percent in pounds per year, and by 0.6 percent in milligrams per liter of water. The model simulations predicted a corresponding reduction at the Mill Creek outflow to the Ocklawaha River of 1.3 percent in pounds per year, and 0.5 percent in milligrams per liter of water. These levels are small, but nonetheless support a finding that the berm system is effective in reducing nitrogen from the North Tract. Furthermore, the WAM simulations showed levels of nitrogen from the irrigated pasture after the construction of the retention berms to be reduced from that present in the pre- development condition, a conclusion consistent with that derived from the BMPTRAINS model. The WAM simulations indicated that phosphorus from the irrigated North Tract pastures, measured at the outflow to Mill Creek at the Reach 22 stream segment, would be reduced from improved pasture levels by 3.7 percent in pounds per year, and by 2.6 percent in milligrams per liter of water. The model simulations predicted a corresponding reduction at the Mill Creek outflow to the Ocklawaha River of 2.5 percent in pounds per year, and 1.6 percent in milligrams per liter of water. Those levels are, again, small, but supportive of a finding of no impact from the permitted activities. The WAM simulations showed phosphorus in the Ocklawaha River at the Eureka Station after the construction of the retention berms to be slightly greater than those simulated for the pre-development condition (0.00008 mg/l) -- the only calculated increase. That level is beyond miniscule, with impacts properly characterized as “non- measurable” and “non-detectable.” In any event, total phosphorus remains well below Florida’s nutrient standards. The WAM simulations were conducted based on all of the 15 pivots operating simultaneously at full capacity. That amount is greater than what is allowed under the permit. Thus, according to Dr. Bottcher, the predicted loads are higher than those that would be generated by the permitted allocation, making his estimates “very conservative.” Dr. Bottcher’s testimony is credited. During the course of the final hearing, the accuracy of the model results was questioned based on inaccuracies in rainfall inputs due to the five-mile distance of the property from the nearest rain station. Dr. Bottcher admitted that given the dynamics of summer convection storms, confidence that the rain station rainfall measurements represent specific conditions on the North Tract is limited. However, it remains the best data available. Furthermore, Dr. Bottcher testified that even if specific data points simulated by the model differ from that recorded at the rain station, that same error carries through each of the various scenarios. Thus, for the comparative purpose of the model, the errors get “washed out.” Other testimony regarding purported inaccuracies in the WAM simulations and report were explained as being the result of errors in the parameters used to run alternative simulations or analyze Sleepy Creek’s simulations, including use of soil types that are not representative of the North Tract, and a misunderstanding of dry weight/wet weight loading rates. There was agreement among witnesses that the WAM is regarded, among individuals with expertise in modeling, as an effective tool, and was the appropriate model for use in the ERP application that is the subject of this proceeding. As a result, the undersigned accepts the WAM simulations as being representative of comparative nutrient impacts on receiving surface water bodies resulting from irrigation of the North Tract. The WAM confirmed that the proposed retention berm system will be sufficient to treat additional nutrients that may result from irrigation of the pastures, and supports a finding of reasonable assurance that water quality criteria will be met. With regard to the East Tract, the WAM simulations showed that there would be reductions in nitrogen and phosphorus loading to Daisy Creek from the conversion of the property to irrigated pasture. Those simulations were also conservative because they assumed the maximum number of cattle allowed by the nutrient balance, and did not assume the 30 percent reduction in the number of cattle under the NMP so as to allow existing elevated levels of phosphorus in the soil from the sod farm to be “mined” by vegetation. Pivot 6 The evidence in this case suggests that, unlike the majority of the North Tract, a small area on the western side of the North Tract drains to the west and north. Irrigation Pivot is within that area. Dr. Harper noted that there are some soils in hydrologic soil Group A in the vicinity of Pivot 6 that reflect soils with a deeper water table where rainfall would be expected to infiltrate into the ground. Dr. Kincaid’s particle track analysis suggested that recharge to the surficial aquifer ultimately discharges to Mill Creek, except for recharge at Pivot 11, which is accounted for by evapotranspiration, and recharge at Pivot 6. Dr. Kincaid concluded that approximately 1 percent of the recharge to the surficial aquifer beneath the North Tract found its way into the upper Floridan aquifer. Those particle tracks originated only on the far western side of the property, and implicated only Pivot 6, which is indicative of the flow divide in the Floridan aquifer. Of the 1 percent of particle tracks entering the Floridan aquifer, some ultimately discharged at the St. John’s River, the Ocklawaha River, or Mill Creek. Dr. Kincaid opined, however, that most ultimately found their way to Silver Springs. Given the previous finding that the Floridan aquifer beneath the property is within the Silver Springs springshed for less than a majority of the time, it is found that a correspondingly small fraction of the less than 1 percent of the particle tracks originating on the North Tract, perhaps a few tenths of one percent, can reach Silver Springs. Dr. Bottcher generally agreed that some small percentage of the water from the North Tract may make it to the upper Floridan aquifer, but that amount will be very small. Furthermore, that water reaching the upper Floridan aquifer would have been subject to the protection and treatment afforded by the NMP and the ERP berms. The evidence regarding the somewhat less restrictive confinement of the aquifer around Pivot 6 is not sufficient to rebut the prima facie case that the CUP modification, coupled with the ERP, will meet the District’s permitting standards. Public Interest The primary basis upon which Sleepy Creek relies to demonstrate that the CUP is “consistent with the public interest” is that Florida's economy is highly dependent upon agricultural operations in terms of jobs and economic development, and that there is a necessity of food production. Sleepy Creek could raise cattle on the property using the agriculturally-exempt improved pastures, but the economic return on the investment would be questionable without the increased quality, quantity, and reliability of grass and forage crop production resulting from the proposed irrigation. Sleepy Creek will continue to engage in agricultural activities on its properties if the CUP modification is denied. Although a typical Florida beef operation could be maintained on the property, the investment was based upon having the revenue generation allowed by grass-fed beef production in order to realize a return on its capital investment and to optimize the economic return. If the CUP modification is denied, the existing CUP will continue to allow the extraction of 1.46 mgd for use on the East Tract. The preponderance of the evidence suggests that such a use would have greater impacts on the water levels at Silver Springs, and that the continued use of the East Tract as a less stringently-controlled sod farm would have a greater likelihood of higher nutrient levels, particularly phosphorus levels which are already elevated.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law set forth herein it is RECOMMENDED that the St. Johns River Water Management District enter a final order: approving the issuance of Consumptive Use Permit No. 2-083-91926-3 to Sleepy Creek Lands, LLC on the terms and conditions set forth in the complete Permit Application for Consumptive Uses of Water and the Consumptive Use Technical Staff Report; and approving the issuance of Environmental Resource Permit No. IND-083-130588-4 to Sleepy Creek Lands, LLC on the terms and conditions set forth in the complete Joint Application for Individual and Conceptual Environmental Resource Permit and the Individual Environmental Resource Permit Technical Staff Report. DONE AND ENTERED this 29th day of April, 2015, in Tallahassee, Leon County, Florida. S E. GARY EARLY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 29th day of April, 2015.
The Issue The issue is whether Respondent, Krista Howard,2/ is entitled to issuance of the Consolidated Environmental Resource Permit and Recommended Intent to Grant Sovereignty Submerged Lands Authorization, Permit No. 53-0351424-001-EI, as announced by Respondent, Department of Environmental Protection, in the Consolidated Notice of Intent to Issue Environmental Resource Permit and Lease to Use Sovereignty Submerged Lands issued on July 28, 2017, and subsequently amended on January 11, 2018.3/
Findings Of Fact The Parties Petitioner Defenders is a Florida non-profit corporation that has been in existence since the mid-1980s or earlier. Defenders' primary purpose is to protect and preserve Crooked Lake so that it may remain an Outstanding Florida Water ("OFW") for all members of the public to use and enjoy. Defenders has more than 25 members who reside in Polk County, Florida. Its membership consists of approximately 100 family memberships, mostly comprised of persons who live on or near Crooked Lake. Petitioners Gerards are riparian landowners on Crooked Lake, whose property is located immediately adjacent to, and slightly to the northwest of, Respondent Howard's property. The Gerards' home address is 1055 Scenic Highway North, Babson Park, Florida 33827. Respondent Howard is the applicant for the Consolidated Authorization for the Dock. Howard's property, which is riparian to Crooked Lake, is located at 1045 Scenic Highway North, Babson Park, Florida 33827. Respondent DEP is the administrative agency of the State of Florida statutorily charged with, among other things, protecting Florida's water resources. As part of DEP's performance of these duties, it administers and enforces the provisions of chapter 373, part IV, Florida Statutes, and the rules adopted pursuant to that statute. Pursuant to that authority, DEP determines whether to issue or deny applications for ERPs. Pursuant to section 253.002, Florida Statutes, DEP also serves as staff to the Board of Trustees of the Internal Improvement Trust Fund ("Board of Trustees") and, in that capacity, reviews and determines whether to issue or deny, applications for approval to use sovereignty submerged lands.5/ DEP Review of the Application The Dock is proposed to be located on sovereignty submerged lands and in surface waters subject to State of Florida regulatory jurisdiction. Therefore, an environmental resource permit and a sovereignty submerged lands lease are required. On or about February 14, 2017, Todd Rickman, Howard's professional contractor who designed the Dock, filed an Application for a Sovereignty Submerged Lands Lease for Existing Structures and Activities6/ ("Application") with DEP's Southwest District Office, seeking approval to construct and operate the Dock. On or about March 15, 2017, DEP requested additional information regarding the project. Howard submitted the requested items, and the Application was determined complete on May 30, 2017. Notice of DEP's receipt of the Lease portion of the Application was provided as required by section 253.115. The comment period commenced on June 15, 2017, and ended on July 6, 2017. As previously noted, on July 28, 2017, DEP issued the Consolidated Notice of Intent, proposing to issue the Consolidated Authorization to construct and operate the Dock. On January 11, 2018, DEP amended the Consolidated Notice of Intent to accurately reflect the "clearly in the public interest" permitting standard for the ERP portion of the Consolidated Authorization, which is applicable to projects proposed in OFWs. Background Crooked Lake Crooked Lake (also, "Lake") is an approximately 4,247-acre freshwater lake in Polk County, Florida. It is an irregularly shaped karst lake roughly resembling an inverted "L," with the longer axis running north to south. It is located on the Lake Wales Ridge. Crooked Lake is designated an OFW by Florida Administrative Code Rule 62-302.700(9)(i)9.7/ The Lake is classified as a Class III waterbody pursuant to Florida Administrative Code Rule 62-302.400(15).8/ The elevations and bottom contours in Crooked Lake vary substantially throughout the Lake. Thus, water depths may, and generally do, vary substantially from one location to another throughout the Lake. The water levels in Crooked Lake fluctuate frequently and, at times, dramatically, depending on rainfall frequency and amounts. A graph prepared by Petitioners' Witness James Tully, using Southwest Florida Water Management District ("SWFWMD") historical water level data for Crooked Lake measured in National Geodetic Vertical Datum of 1929 ("NGVD") shows water levels historically fluctuating from as low as approximately 106 feet in or around 1991, to as high as 123 feet NGVD in or around 1951, 1961, and 2004. Rickman generated a water level graph using the Polk County Water Atlas ("Atlas") website. This graph, which covers the period of 2008 through mid-2017, shows that the water levels in Crooked Lake, for this most recent ten-year period, fluctuated approximately five feet, with the lowest levels falling slightly below 114 feet NGVD for relatively short periods in 2012 and 2013, and the highest level rising to approximately 119 feet NGVD in mid-2017. The competent, credible evidence shows that although water levels in Crooked Lake may occasionally rise to levels at or around 123 feet NGVD, those conditions have been associated with extreme weather events such as hurricanes, are atypical, and are relatively short-lived. The maximum water level in Crooked Lake is subject to control by a weir located south of the Lake. Discharge from the weir occurs at a control elevation of 120 feet NGVD. As such, the water level in parts of Crooked Lake may, at times, temporarily exceed 120 feet NGVD, but will eventually decrease to 120 feet NGVD as the water flows south and is discharged through the weir. To the extent rainfall does not recharge the Lake, water levels may fall below 120 feet NGVD. The ordinary high water line ("OHWL"), which constitutes the boundary between privately-owned uplands and sovereignty submerged lands, has been established at 120.0 feet NGVD for Crooked Lake. Crooked Lake is used for recreational activities such as fishing, swimming, boating, and jet ski use, and there are public and private boat ramps at various points on the lake that provide access to the Lake. There is no marina having a fueling station on the Lake. The credible evidence shows that the northeast portion of the Lake, where the Dock is proposed to be located, experiences a substantial amount of boat and jet ski traffic. This portion of the Lake also is used for swimming, water- skiing, wakeboarding, the use of "towables" such as inner tubes, and for other in-water recreational uses. The Proposed Dock Howard holds fee title by warranty deed to parcel no. 333028-000000-033140 located at 1045 Scenic Highway, Babson Park, Florida.9/ This parcel has approximately 110 linear feet of riparian shoreline on Crooked Lake. The Dock is proposed to be constructed and operated on sovereignty submerged lands adjacent to this riparian upland parcel, which is located on the eastern shore of the northeastern portion of Crooked Lake. The Dock, as proposed, is a private single-family residential dock that will be used by Howard for water-dependent recreational purposes, such as specifically, boating, fishing, swimming, and sunbathing. The Dock is not proposed to be constructed or used by, or to otherwise serve, commercial or multifamily residential development. The Dock is configured as a "T," supported by pilings and consisting of a 4-foot-wide by 152-foot-long access walkway, and an approximately 1,983-square-foot terminal platform comprised of a lower-level platform having four vessel slips and a flat platform roof. Two sets of stairs lead from the lower level of the terminal platform to the platform roof, which will be elevated eight feet above the lower-level platform and will have a railed perimeter. The platform roof will function as a roof for the boat storage area below and a sundeck. The four slips on the Dock's lower-level platform will be used for permanent mooring for up to six watercraft: a 23-foot-long ski boat,10/ a 20-foot-long fishing boat, and four jet skis. As proposed, the Dock will occupy a total area of approximately 2,591 square feet. The lower platform of the Dock is proposed to be constructed at an elevation of 121 feet NGVD. The roof/upper platform will be constructed eight feet above that, at an elevation of 129 feet NGVD. The pilings supporting the Dock will be wrapped in an impervious material to prevent leaching of metals and other pollutants into the water. Pursuant to the Specific Purpose Field Survey ("Survey") for the Lease submitted as part of the Application, the Lease will preempt approximately 2,591 square feet, and closely corresponds to the footprint of the Dock. The submerged lands surrounding the Dock that are not occupied by the footprint of the Dock, including the area between terminal platform and the shoreline, are not included in the preempted area of the Lease.11/ The Survey shows "approximate riparian lines" which delineate Howard's riparian area oriented to the center of the waterbody and to the primary navigation channel in the northeast portion of Crooked Lake. As shown on the version of the Survey initially filed as part of the Application, the Dock was proposed to be located approximately 4.7 feet, at its closest point, from the southern riparian line. However, in response to DEP's request for additional information, the Survey was modified in April 2017, to shift the Dock northward within Howard's riparian area. The Dock is now proposed to be located 25.1 feet, at its closest point, from the southern riparian line, and 29.4 feet, at its closest point, from the northern riparian line. The walkway of the Dock will commence at an approximate elevation of 120 feet NGVD, which corresponds to the OHWL established for Crooked Lake. As previously noted above, the walkway will extend waterward approximately 152 feet, where it will intersect with the terminal platform. The terminal platform will extend another 52 feet waterward. In total, the Dock is proposed to extend waterward approximately 204 feet from the OHWL. Although the Dock would be one of the longest and largest docks on Crooked Lake, the credible evidence establishes that there are several other docks of similar size and/or length on the Lake. Rickman testified that he obtained approvals for, or was otherwise aware of, several docks over 2,000 square feet on the Lake. Additionally, the evidence showed that eight other docks on the Lake are longer than the proposed Dock.12/ Rickman testified that most of the larger docks on Crooked Lake have roofs, and that most of these roofs are pitched, rather than flat.13/ As noted above, the water level in Crooked Lake frequently and, at times, extensively fluctuates. As a result, there are periods during which water depths in parts of the Lake are extremely shallow. Rickman testified that the Dock was designed to extend far enough out into Crooked Lake to reach sufficient water depth to enable Howard to maximize the use of the Dock for boating throughout the year. The Dock is designed to extend out to the point at which the bottom elevation of the Lake is approximately 109.9 feet NGVD. Based on the Atlas' ten-year water level graph for Crooked Lake referenced above, Rickman projected that at this point, the water depth typically would be sufficient to allow Howard to operate her largest vessel, the 23-foot ski boat. The ski boat has a 25-inch draft.14/ The boat will be stored out of the water on a boat lift on the Dock, attached by cables to a sub-roof immediately beneath the platform roof. When being lowered into or hoisted from the water, the boat will be placed in a boat cradle consisting of two containment railings approximately 18 inches high each on either side, and a "V" shaped aluminum bottom with bunks on which the boat is cradled. The aluminum bottom of the cradle was estimated to be two to three inches thick. Although the boat cradle is approximately 18 to 21 inches in "total height,"15/ the cradle does not have to be completely lowered its entire 18- to 21-inch height into the water when used. Steven Howard explained, credibly, that the cradle needs to be lowered into the water only a few inches lower than the ski boat's 25-inch draft to enable the boat to float into or out of the cradle. To that point, Rickman testified that taking into account the 25-inch draft of the ski boat and the "total height" of the boat cradle, between 40 and 44 inches of water depth would be required when the cradle is used in order to avoid coming into contact with the Lake bottom. Based on the Atlas graph showing the lowest water levels for the previous ten-year period at approximately 114 feet NGVD, Rickman designed the Dock to extend out to the 109.9-foot NGVD bottom elevation point. At this point, the projected water depth would be slightly more than four feet during periods of the lowest projected water levels for Crooked Lake. For the Dock to be able to wharf out to 109.9 feet NGVD bottom elevation, it must extend a total of approximately 204 feet waterward into the Lake. The credible evidence establishes that while Howard's ski boat is one of the largest, it is not the largest boat operated on Crooked Lake. Impacts Assessment for Environmental Resource Permit Water Quality Impacts As noted above, Crooked Lake is a Class III waterbody. Accordingly, the surface water quality standards and criteria applicable to Class III waters in Florida codified in rule 62-302.300 apply to Crooked Lake. The Dock, as proposed to be constructed and operated, is not anticipated to adversely affect or degrade water quality in Crooked Lake. Specifically, as required by the Consolidated Authorization, a floating turbidity curtain will be installed around the boundary of the construction area before construction commences, and it must be left in place until construction is complete and turbidity levels in the work area have returned to background levels. Additionally, as noted, the pilings supporting the Dock must be wrapped in an impervious material to prevent leaching of metals and other pollutants into the water over the life of the structure. The Consolidated Authorization also prohibits the installation and use of fueling equipment at the Dock; prohibits the discharge of sewage or other waste into the water; prohibits liveaboards; prohibits fish cleaning or the installation of fish cleaning stations unless sufficient measures such as sink screens and waste receptacles are in place; and prohibits repair and maintenance activities involving scraping, sanding, painting, stripping, recoating, and other activities that may degrade water quality or release pollutants into the water. Although the Consolidated Authorization imposes a specific condition requiring, for all vessels using the Dock, a minimum 12-inch clearance between the deepest draft of the vessel (with motor in the down position) and the top of submerged resources, it does not specifically address circumstances where the use of the boat cradle, rather than the vessel itself, may come into contact with the Lake bottom. DEP's witness acknowledged that if the boat cradle were to come into contact with the Lake bottom, water quality standards may be violated. Given the information presented at the final hearing regarding the operation of the boat lift and the need for sufficient clearance between the bottom of the boat cradle and the lake bottom, the undersigned recommends that a specific condition be included in the Consolidated Authorization prohibiting contact of the Lake bottom by the boat cradle. This recommended condition is set forth in paragraph 73.A., below. Upon consideration of the conditions imposed by the Consolidated Authorization discussed above, including imposing a specific condition that prohibits contact of the boat cradle with the Lake bottom, the undersigned finds that the Dock will not adversely affect or degrade the water quality of Crooked Lake. Water Quantity Impacts The Dock, as proposed, is a piling-supported structure that will not impound, store, or impede the flow of surface waters. As such, the Dock will not cause adverse flooding to on-site or offsite property, will not result in adverse impacts to surface water storage and conveyance capabilities, and will not result in adverse impacts to the maintenance of surface or ground water levels. Impacts to Fish, Wildlife, and Listed Species and Habitat The Application states, in section 5, question 6, that there is no vegetation on Howard's riparian shoreline. However, the Survey depicts an area of emergent grasses approximately 60 feet wide and extending diagonally approximately 70 feet waterward into the Lake. The Survey depicts this grassed area as straddling the riparian line between Howard's property and the adjacent parcel to the south. The Survey shows the Dock as being located a significant distance waterward of the grassed area, such that no portion of the Dock will be located on or near this grassed area. Additionally, an aerial photograph of Howard's property and the Lake waterward of Howard's property shows a smaller patch of what appears to be emergent grasses further offshore. This grassed area is not shown on the Survey, and it cannot definitively be determined, by examining the Survey and the aerial photograph, whether this grassed area is growing in an area that will be impacted by the Dock. Steven Howard acknowledged that this smaller grassed area may be located at or near the jet ski slip on the southeastern side of the Dock. An environmental assessment of this smaller grassed area was not performed or submitted as part of the Application. Thus, any value that this area may have as fish and wildlife habitat was not assessed as part of DEP's determination that the Dock will not adversely impact the value of functions provided to fish, wildlife, and to listed species and their habitat. In order to provide reasonable assurance that the Dock will not adversely impact the value of functions provided to fish, wildlife, and to listed species and their habitat, the undersigned recommends including a specific condition in the Consolidated Authorization requiring this smaller grassed area to be completely avoided during construction and operation of the Dock, or, if avoidance is not feasible, that an environmental assessment be performed prior to construction so that the value of this grassed area, if any, to fish, wildlife, and listed species can be evaluated to determine whether minimization and compensatory mitigation should be required. This recommended condition is set forth in paragraph 73.B., below. As previously noted, the Consolidated Authorization contains a specific condition requiring a minimum 12-inch clearance between the deepest draft of the vessel (with the motor in the down position) and the top of submerged resources for all vessels that will use the docking facility. Compliance with this condition will help ensure that the value of functions provided to fish and wildlife and to listed species and their habitat of any such submerged resources is not adversely impacted by vessels using the Dock. The Consolidated Authorization also contains a specific condition requiring handrails to be installed on the Dock to prevent mooring access to portions of the Dock other than the wetslips. This will help protect submerged resources in shallower areas in the vicinity of the Dock. Fish populations in the immediate area of the Dock site may temporarily be affected during construction of the Dock; however, those impacts are not anticipated to be permanent. Additionally, as previously discussed, the Dock pilings must be wrapped with an impervious material to prevent leaching of pollutants into the water, and once installed, the pilings may provide habitat for fish and a substrate for benthic organisms. Provided that the conditions set forth in the draft Consolidated Authorization, as well as the recommendation regarding the smaller grassed area, are included in the final version of the Consolidated Authorization, it is determined that the construction and operation of the Dock will not adversely impact the value of functions provided to fish, wildlife, or to listed species or their habitat.16/ Impact on Navigation Petitioners assert that the Dock will constitute a hazard to navigation in the northeast portion of Crooked Lake. Specifically, they assert that because the Dock will extend out approximately 204 feet into the Lake, it necessarily will create a navigational hazard to boaters in the vicinity. As support, Petitioners presented evidence consisting of Steven Howard's testimony that an inner tube on which his nephew was riding, that was being pulled behind a motor boat, collided with the Gerards' 84-foot-long floating dock adjacent to Howard's riparian area. Petitioners argue that if an 84-foot-long dock creates a navigational hazard, a 204-foot-long dock would create an even greater navigational hazard. The undersigned does not find this argument persuasive. The portion of Crooked Lake on which the Dock is proposed to be located is approximately a mile and a half to two miles long and one-half to three-quarters of a mile wide. Although this portion of Crooked Lake experiences substantial boat traffic, the evidence shows that the Lake is sufficiently large in this area, even with the Dock in place, to allow safe navigation. To this point, it is noted that there are two other longer docks in the northeastern portion of Crooked Lake, extending 220 and 244 feet into the Lake from the shoreline. There was no evidence presented showing that either of these docks constitutes a navigational hazard.17/ Petitioners also assert that during periods of high water in this portion of Crooked Lake, the Dock will be underwater and thus will present a navigational hazard. In support, they presented photographs taken on October 30, 2017—— approximately six weeks after Hurricane Irma struck central Florida——showing ten docks, out of the 109 docks on Crooked Lake, that were partially or completely submerged.18/ When the photographs were taken, the approximate water elevation was 119.2 feet NGVD. All or a portion of the submerged docks had been constructed at or below the 119.2-foot NGVD elevation. The docks without roofs were mostly or completely invisible under the water. However, for the roofed docks, the roofs remained visible above the water even when their docking platforms were submerged. Here, although the walkway and lower platform of Howard's Dock is proposed to be constructed at an elevation of 121 feet NGVD, the roof will be constructed at an elevation of 129 feet NGVD. Thus, even during the relatively infrequent periods19/ during which the water level in Crooked Lake may exceed 121 feet NGVD, the platform roof will still be visible to vessels navigating in this portion of the Lake. Additionally, the Consolidated Authorization contains a specific condition requiring the waterward end of the Dock to be marked with a sufficient number of reflectors to be visible from the water at night by reflected light. This condition provides additional assurance that the Dock will not present a navigational hazard. For these reasons, it is determined that the Dock will not adversely affect navigation. Other ERP-Related Issues The evidence did not show that the Dock is proposed to be located in or proximate to a "work of the District," as defined in section 373.019(28). The only "work of the District" about which evidence was presented is the weir located south of Crooked Lake. This structure is many thousands of feet south of the Dock. There was no evidence presented showing that the Dock would have any impact on this weir. The Dock, as proposed, was designed by an experienced professional contractor who has designed and installed many docks on Crooked Lake, and, as such, is anticipated to function as proposed. The Dock must be built according to engineering diagrams to the Consolidated Authorization, and as-built drawings must be submitted when Dock construction is complete so that DEP can confirm that the Dock is constructed in accordance with the approved design. The evidence establishes that Howard, as the applicant, and Rickman, as the professional contractor in charge of construction, are financially, legally, and administratively capable of ensuring that the activity will be undertaken in accordance with the terms and conditions of the Consolidated Authorization. No evidence to the contrary was presented. The Dock will be located in the waters of Crooked Lake and will be affixed to the submerged bottom. The Department of State, Division of Historical Resources ("DHR"), did not provide any comments indicating that historical or archaeological resources are anticipated to be impacted by the project. Additionally, the Consolidated Authorization contains a general condition requiring subsurface activity associated with construction of the Dock to immediately cease, and DHR to be contacted, if any prehistoric or historic artifacts, such as pottery or ceramics, stone tools or implements, dugout canoes, or other physical remains that could be associated with Native American cultures or early colonial or American settlements are encountered at any time within the project site area. Additional Recommended Conditions Based on the foregoing, the undersigned recommends that the following specific conditions be included in the Consolidated Authorization, Permit No. 53-0351424-001-EI: A minimum six-inch clearance shall be maintained between the top of all submerged resources and the deepest draft of the cradle of the boat lift while in use. For purposes of this condition, submerged resources consist of the bottom sediment and/or any submerged grasses or other aquatic organisms. Any emergent grasses in the permittee's riparian area shall be avoided during the construction and operation of the Dock. If it is not feasible to avoid these grasses, an environmental assessment of the grassed area shall be performed and submitted to the Department prior to commencing construction, so that the value of this grassed area, if any, to fish, wildlife, and listed species can be evaluated and the extent to which minimization and/or compensatory mitigation is appropriate can be determined. Clearly in the Public Interest Florida Administrative Code Rule 62-4.070, Standards for Issuing or Denying Permits, states in pertinent part: A permit shall be issued to the applicant upon such conditions as the Department may direct, only if the applicant affirmatively provides the Department with reasonable assurance based on plans, test results, installation of pollution control equipment, or other information, that the construction, expansion, modification, operation, or activity of the installation will not discharge, emit, or cause pollution in contravention of Department standards or rules. In addition to the foregoing permitting requirements, because the Dock is proposed to be located in an OFW, Howard also must provide reasonable assurance that the Dock meets the "clearly in the public interest" standard. The "clearly in the public interest" standard does not require the applicant to demonstrate need for the project or a net public benefit from the project. Rather, this standard requires the applicant to provide greater assurances, under the circumstances specific to the project, that the project will comply with the applicable permitting requirements.20/ For the reasons discussed above, and with the inclusion of the additional recommended conditions in paragraphs 73.A. and 73.B., it is determined that the proposed Dock meets the applicable permitting requirements and the "clearly in the public interest" standard for issuance of the ERP. Impacts Assessment for Sovereignty Submerged Lands Lease Water-Dependency of the Proposed Dock A water-dependent activity is one which can only be conducted in, on, over, or adjacent to water areas because the activity requires direct access to the water body or sovereignty submerged lands for specified activities, including recreation, and where the use of water or sovereignty submerged lands is an integral part of the activity. See Fla. Admin. Code R. 18-21.003(71). Petitioners argue that the Dock will not constitute a water-dependent activity because the depth of water in the slips may, at times, be insufficient to allow operation of Howard's vessels while complying with the requirement that a minimum 12- inch clearance be maintained between the lowest draft of the vessel and submerged resources. The undersigned finds this argument unpersuasive. The Dock is being constructed specifically for the purpose of enabling Howard to use her vessels for boating——a recreational activity for which use of the water indisputably is an integral part. The Dock's primary purpose is to moor vessels that will be used for the water-dependent recreational activities of boating and fishing, and other water-dependent recreational uses of the Dock include fishing, swimming and sunbathing. Case law interpreting the Florida Administrative Code Chapter 18-21 makes clear that because docks are used for mooring vessels or conducting other in-water recreational uses, they are "water-dependent" activities for purposes of the rules.21/ Thus, even if water depths in the Dock's slips are at times insufficient for vessel mooring or launching,22/ this does not render the Dock not a "water-dependent activity." Resource Management Requirements The preempted area of the Lease is proposed to be used for a Dock that will be used for boating, fishing, and swimming. These traditional in-water recreational uses are consistent with the management purposes of sovereignty submerged lands as described in rule 18-21.004(2)(a). With the inclusion of the conditions currently proposed in the draft Consolidated Approval, as well as the recommended conditions in paragraphs 73.A. and 73.B., the undersigned determines that the Dock will not result in adverse impacts to sovereignty submerged lands and associated resources. With the inclusion of the conditions currently proposed in the draft Consolidated Approval, as well as the recommended conditions in paragraphs 73.A. and 73.B., the undersigned determines that the Dock is designed to minimize or eliminate impacts to fish and wildlife habitat and submerged resources. With the inclusion of the currently proposed conditions in the draft Consolidated Authorization, as well as the recommended conditions set forth in paragraphs 73.A. and 73.B., it is determined that the Dock, as designed and constructed, will minimize or eliminate cutting, removal, or destruction of wetland vegetation. Additionally, as discussed above, the proposed Consolidated Approval requires the avoidance of adverse impacts to historic and cultural resources. Riparian Rights Consistent with rule 18-21.004(3)(d), the Dock is proposed to be constructed in Howard's riparian area and will be set back more than 25 feet from the northerly and southerly riparian lines shown on the Survey. Rule 18-21.004(3)(a) prohibits activities authorized under chapter 18-21 from being implemented in a manner that would unreasonably infringe on traditional common law riparian rights, as defined in section 253.141, of upland owners adjacent to sovereignty submerged lands. Similarly, rule 18-21.004(3)(c) requires all structures and activities to be designed and conducted in a manner that will not unreasonably restrict or infringe upon the riparian rights of adjacent riparian owners. Collectively, these provisions prohibit an activity that will occur on sovereignty submerged lands from unreasonably infringing on or unreasonably restricting the riparian rights of upland riparian owners. Riparian rights are rights appurtenant to, and inseparable from, riparian land that borders on navigable waters. § 253.141, Fla. Stat.; Broward v. Mabry, 50 So. 830 (Fla. 1909). At common law, riparian rights include the rights of navigation, fishing, boating, and commerce. Hayes v. Bowman, 91 So. 2d 795 (Fla. 1957). The right of navigation necessarily includes the right to construct and operate a dock to access navigable waters. Belvedere Dev. Corp. v. Dep't of Transp., 476 So. 2d 649 (Fla. 1985); Shore Vill. Prop. Owners' Ass'n v. Dep't of Envtl. Prot., 824 So. 2d 208, 211 (Fla. 4th DCA 2002). Common law riparian rights also include the right to an obstructed view. Lee Cnty v. Kiesel, 705 So. 2d 1013 (Fla. 2d DCA 1998). Many of these common law riparian rights have been statutorily codified in section 253.141. Statutory riparian rights include the "rights of ingress, egress, boating, bathing, and fishing and such others as may be or have been defined by law." § 253.141(1), Fla. Stat. At issue in this case are the competing riparian rights of next-door neighbors——i.e., Howard's right to wharf out to navigable waters for purposes of boating and other water- dependent recreational activities, and the Gerards' right to an unobstructed view. The question is whether Howard's proposed construction and operation of a dock of sufficient length to enable her to use her boats would unreasonably infringe on or unreasonably restrict the Gerards' right to an unobstructed view of the Lake. By virtue of the riparian rights appurtenant to Howard's riparian property, she is entitled to wharf out to water deep enough to enable her to navigate. She owns two boats, one of which pulls a draft of 25 inches, and the other, a draft of 20 inches, which she uses to navigate the Lake. Thus, an essential aspect of Howard's riparian right of navigation is her ability to construct and operate a dock long enough to enable her to reach water depths sufficient to use these boats. However, as noted above, this right is not unfettered. Howard's exercise of her riparian navigation right cannot unreasonably infringe on Gerard's right to an unobstructed view. Florida case law holds that the right to an "unobstructed" view does not entail a view free of any infringement or restriction whatsoever by neighboring structures or activities. In Hayes, the court defined the right as "a direct, unobstructed view of the [c]hannel and as well a direct, unobstructed means of ingress and egress . . . to the [c]hannel." Id. at 801 (emphasis added). The court then prescribed the rule that "in any given case, the riparian rights of an upland owner must be preserved over an area 'as near as practicable' in the direction of the [c]hannel so as to distribute equitably the submerged lands between the upland and the [c]hannel." Id. (emphasis added). To the extent there is no channel in this portion of the Lake, Hayes dictates that riparian rights must be apportioned equitably, so that a riparian owner's right to an unobstructed view can extend only from the owner's property in the direction of the center of the Lake. Kling v. Dep't of Envtl. Reg., Case No. 77-1224 (Fla. DOAH Oct. 6, 1977; Fla. DER Nov. 18, 1977) at ¶¶ 11-12 (emphasis added). Here, no evidence was presented showing that the Dock——which will be located immediately south and east of the Gerards' riparian property and attendant riparian area——will present an obstruction to the Gerards' view of the Lake channel. Additionally, the evidence did not establish that Howard's Dock would obstruct the Gerards' view of the center of the northeast portion of Crooked Lake, which is located west and slightly south of their property.23/ Administrative precedent in Florida provides additional support for the determination that the Dock will not unreasonably infringe on the Gerards' right to an unobstructed view. In O'Donnell v. Atlantic Dry Dock Corporation, Case No. 04-2240 (Fla. DOAH May 23, 2005; Fla. DEP Sept. 6, 2005), riparian owners challenged the proposed approval of expansions of sovereignty submerged lands leases authorizing Atlantic Dry Dock, a neighboring commercial shipyard, to expand its shipyard facilities and install new docking facilities. The administrative law judge noted that although the expanded shipyard would further encroach on the riparian owners' already somewhat-restricted view from their property, it would not substantially and materially obstruct the Petitioners' view to the channel. He commented: "it [their view] may be further obstructed to the west in the direction of the Atlantic Marine yard, but not in the direction of the channel." To that point, he found that although "any lateral encroachment on the Petitioners' line-of-sight to the channel by the large eastern dry dock proposed will be an annoyance, . . . [it] will not rise to the level of a substantial and material interference or obstruction of the Petitioners' view to the channel." Id. at ¶ 119. He found that "there is no 'special riparian right' to a view of the sunset, just as there was no right to a particular object of view . . . by the riparian owners complaining in the Hayes case." Id. at ¶ 120. Castoro v. Palmer, Case Nos. 96-0736, 96-5879 (Fla. DOAH Sept. 1, 1998; Fla. DEP Oct. 19, 1998), also is instructive. In Castoro, neighboring riparian owners challenged the proposed issuance of an environmental approval and sovereignty submerged lands lease for a 227-foot-long dock having a terminal platform with boat lift. The owners contended that due to the dock's length, it would impermissibly obstruct their views of the water. The administrative law judge rejected that contention, distinguishing the circumstances from those in Lee County v. Kiesel, 705 So. 2d 1013 (Fla. 2d DCA 1998), in which the construction of a bridge that blocked 80 percent of the riparian owners' view of the channel was held to constitute a "substantial and material" obstruction to the riparian right of view. The ALJ noted that although the dock would have "some impact on the neighbors' views" and their use of the waterbody, it did not unreasonably impact their riparian rights to an unobstructed view or to use of the waterbody. Id. at ¶¶ 73-74. In Trump Plaza of the Palm Beaches Condominium v. Palm Beach County, Case No. 08-4752 (Fla. DOAH Sept. 24, 2009; Fla. DEP Oct. 8, 2009), a condominium association challenged the proposed issuance of a sovereignty submerged lands use approval to fill in a dredged area and create mangrove islands in the Lake Worth Lagoon, alleging, among other things, that the creation of the mangrove islands would unreasonably infringe on their riparian right to an unobstructed view. In rejecting this position and recommending issuance of the submerged lands use approval, the ALJ noted that the area obstructed by the mangrove islands would be negligible compared to the remaining expanse of the view, and further noted that the owners' real concern was directed at the aesthetics of the project——specifically, they did not want to view mangrove islands. The ALJ stated: "[t]he evidence supports a finding that while the project will undoubtedly alter the view of the water from [the riparian owners' property], the impact on view is not so significant as to constitute an unreasonable infringement of their riparian rights." Id. at ¶ 86. Applying these case law principles, it is determined that the Dock will not unreasonably infringe on or unreasonably restrict the Gerards' riparian right to an unobstructed view. To that point, the cases make clear that the right to an "unobstructed" view is not an unfettered right to a view of the water completely free of any lateral encroachment, but, instead is the right of a view toward the channel or the center of a lake without unreasonable infringement or restriction. Here, although the Dock will laterally encroach on the Gerards' full panoramic view of the Lake——and, as such, may even constitute an annoyance, the evidence did not show that the Dock will obstruct or otherwise restrict their view to the channel or the center of the Lake. Moreover, to the extent the Gerards have expressed concern about the Dock interfering with their view of the south shore of the Lake, O'Donnell makes clear the desire to have a particular object of view——here, the south shore of the Lake——is not a legally protected riparian right. It is also found that the Dock will not unreasonably interfere with the Gerards' riparian rights of ingress, egress, boating, or navigation. As previously noted, the Dock will be located at least 25 feet inside the riparian lines established for Howard's upland property, and, it will not be constructed in a location or operated in a manner that will obstruct, interfere with, or restrict the Gerards' access to the Lake or to sufficient water depths to enable navigation.24/ The evidence also did not establish that the Dock will restrict or otherwise interfere with the Gerards' use of their riparian area for ingress and egress, boating, fishing, bathing, or other riparian uses. In sum, it is concluded that the Dock will not unreasonably infringe on or restrict the riparian rights of adjacent upland riparian owners. Accordingly, it is determined that the Dock will meet the requirements and standards in rule 18-21.004(3) regarding riparian rights. Navigational Hazard For the reasons discussed in paragraphs 63 through 67, it is determined that the Dock will not constitute a navigational hazard in violation of rule 18-21.004(7)(g). Not Contrary to the Public Interest Rule 18-21.004(1)(a) requires an applicant to demonstrate that an activity proposed to be conducted on sovereignty submerged lands will not be contrary to the public interest. To meet this standard, it is not necessary that the applicant show that the activity is affirmatively in the "public interest," as that term is defined in rule 18-21.003(51). Rather, it is sufficient that the applicant show that there are few, if any, "demonstrable environmental, social, and economic costs" of the proposed activity. Castoro, at ¶ 69. For the reasons discussed above, and with the inclusion of the additional recommended conditions in paragraphs 73.A. and 73.B., it is determined that the proposed Dock meets the "not contrary to the public interest" standard required for issuance of the Lease. Demonstration of Entitlement to ERP Howard met her burden under section 120.569(2)(p) to present a prima facie case of entitlement to the ERP by entering into evidence the Application, the Notice of Intent, and supporting information regarding the proposed Dock. She also presented credible, competent, and substantial evidence beyond that required to meet her burden under section 120.569(2)(p) to demonstrate prima facie entitlement to the ERP. The burden then shifted to Petitioners to demonstrate, by a preponderance of the competent substantial evidence, that the Dock does not comply with section 373.414 and applicable ERP rules. For the reasons discussed above, it is determined that Petitioners did not meet their burden of persuasion under section 120.569(2)(p) in this proceeding. Accordingly, for the reasons addressed above, it is determined that Howard is entitled to issuance of the ERP for the Dock. Demonstration of Entitlement to Lease As previously discussed, Howard bore the burden of proof in this proceeding to demonstrate, by a preponderance of the evidence, that the Dock meets all applicable statutory and rule requirements for issuance of the Lease for the Dock. For the reasons discussed above, it is determined that Howard met this burden, and, therefore, is entitled to issuance of the sovereignty submerged lands lease for the Dock. Petitioners' Standing Defenders' Standing As stipulated by the parties and noted above, Defenders is an incorporated non-profit entity created for the primary purpose of protecting and preserving Crooked Lake so that it may remain an OFW for all members of the public to enjoy. Defenders has been in existence since at least the mid- 1980s. Robert Luther, the president of Defenders, testified that the organization's purpose also entails providing education and promoting public awareness in order to preserve the natural beauty, water quality, ecological value, and quality of life around Crooked Lake. As stipulated by the parties and noted above, Defenders has more than 25 members. Luther testified that Defenders has approximately 100 family members, most of whom live on or around Crooked Lake. He noted that many of Defenders' members own boats, which they park at a local boat landing on the Lake. Based on this testimony, it is inferred that these members operate their boats on Crooked Lake. After receiving the public notice of the project, Defenders' board of directors voted to oppose issuance of the Consolidated Authorization for the Dock. Luther testified that the board's decision was based on the determination that "it was clearly within the public interest" to oppose the Dock. Gerards' Standing The Gerards reside at 1055 Scenic Highway, Babson Park, Florida. Their riparian property is immediately adjacent to, and northwest of, Howard's property. The Gerards own a floating dock that is located within their riparian area.25/ The dock consists of two 4-foot- wide by 30-foot-long ramps attached to a 24-foot-long by 8-foot- wide pontoon boat. Priscilla Gerard testified that she enjoys spending time sitting and reading books on the beach in front of her property, and that having that area to sit and read is a significant aspect of her enjoyment of her lakefront property. Ms. Gerard observed that extensive boating activities in the northeast portion of the Lake on weekends is disruptive, and interferes with her use of her beach for relaxing and reading. She particularly noted that boats operating very close to the shore cause waves to splash up on her beach, interfering with her ability to sit and read close to the shore. She did not contend that Howard's use of the Dock for boating would contribute to the disruptive nature of existing boat traffic in the vicinity. Ms. Gerard has viewed the plans for the proposed Dock and is very concerned that due to its size, her view of the south side of the Lake will be completely blocked. She acknowledged, and other competent, credible evidence showed, that there are other docks on the Lake in the vicinity of her riparian property. The evidence shows that existing docks having lengths of 145 feet and 170 feet are located in the vicinity of, and are visible from, the Gerards' property. She testified that an existing dock and tiki hut block her view of the Lake to the north. She acknowledged that although Howard's Dock, if constructed as proposed, may somewhat obstruct her view to the left (south) of her property, it would not block her view straight out into the Lake. Phillip Gerard testified that he has boated extensively on Crooked Lake in a variety of vessel types. He further testified that he has observed a range of boating practices on Crooked Lake, including seeing water skiers and persons being towed behind motorized vessels on inner tubes and other types of "towables." He testified that, based on his personal observations, persons being towed do not have independent control of the speed or direction of the "towable"; thus, depending on the direction in which the towing vessel turns, the towable may be slung to the left or the right. Gerard commented that such lack of control could result in a person riding on a towable colliding with a dock, and he noted that Howard's nephew, who was riding on an inner tube being towed by a boat, was involved in such a collection with his (Mr. Gerard's) own dock. Mr. Gerard did not testify that the Dock would present a navigational hazard to, or otherwise interfere with, the Gerards' riparian right of ingress and egress. Neither of the Gerards testified that the Dock would impact their ability to access navigable waters in the Lake. Mr. Gerard acknowledged that if Howard's Dock were constructed, boats that currently travel very close to the shoreline of his property would be forced to swing further out in the Lake, away from his riparian shoreline, in order to avoid the Dock.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Environmental Protection enter a final order approving the issuance of Consolidated Environmental Resource Permit and Recommended Intent to Grant Sovereignty Submerged Lands Authorization, Permit No. 53-0351424-001-EI, on the terms and conditions set forth in the Consolidated Notice of Intent and attached draft of Permit No. 53-0351424-001-EI, as modified to include the Additional Recommended Conditions set forth in paragraphs 73.A. and 73B. DONE AND ENTERED this 5th day of July, 2018, in Tallahassee, Leon County, Florida. S CATHY M. SELLERS Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 5th day of July, 2018.
The Issue This case involves a challenge to St. Johns River Water Management District’s (District or SJRWMD) intended issuance of an Environmental Resource Permit (ERP) granting the City's Application No. 4-127-97380-1, for the construction and operation of a surface water management system for a retrofit flood-relief project known as Drysdale Drive/Chapel Drive Drainage Improvements consisting of: excavation of the Drysdale Drive pond (Pond 1); improvement to the outfall at Sterling Lake; and the interconnection of Pond 1 and four existing drainage retention areas through a combination of pump stations and gravity outfalls (project or system). The issue is whether the applicant, the City of Deltona (City or Deltona), has provided reasonable assurance the system complies with the water quantity, environmental, and water quality criteria of the District’s ERP regulations set forth in Chapter 40C-4, Florida Administrative Code,1 and the Applicant’s Handbook: Management and Storage of Surface Waters (2005) (A.H.).2
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the St. Johns River Water Management District enter a final order issuing to the City of Deltona an ERP granting the City's Application No. 4-127-97380-1, subject to the conditions set forth in the Technical Staff Report. DONE AND ENTERED this 17th day of March, 2006, in Tallahassee, Leon County, Florida. S J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 17th day of March, 2006.
The Issue The issue is whether the applicant for an Environmental Resource Permit ("ERP"), the City of Deltona ("City" or "Applicant"), has provided reasonable assurance that the system proposed complies with the water quantity, environmental, and water quality criteria of the St. Johns River Water Management District's ("District") ERP regulations set forth in Florida Administrative Code Chapter 40C-4, and the Applicant's Handbook: Management and Storage of Surface Waters (2005).
Findings Of Fact The District is a special taxing district created by Chapter 373, Florida Statutes, charged with the duty to prevent harm to the water resources of the District, and to administer and enforce Chapter 373, Florida Statutes, and the rules promulgated thereunder. The City of Deltona is a municipal government established under the provisions of Chapter 165, Florida Statutes. The Lake Theresa Basin is comprised primarily of a system of interconnected lakes extending from Lake Macy in the City of Lake Helen to the Butler Chain of Lakes (Lake Butler and Lake Doyle). The Lake Theresa Basin is land-locked and does not have a natural outfall to Lake Monroe and the St. Johns River. In 2003, after an extended period of above-normal rainfall in the Deltona area, the lakes within the land-locked Lake Theresa Basin staged to extremely high elevations that resulted in standing water in residential yards, and rendered some septic systems inoperable. Lake levels within the Lake Theresa Basin continued to rise and were in danger of rising above the finished floor elevations of some residences within the basin. On March 25, 2003, the District issued an Emergency Order (F.O.R. No. 2003-38) authorizing the construction and short-term operation of the Lake Doyle and Lake Bethel Emergency Overflow Interconnection. Since wetland and surface water impacts would occur, the Emergency Order required the City of Deltona to obtain an ERP for the system. The project area is 4.1 acres, and the system consists of a variable water structure on the west shore of Lake Doyle connected to a series of pipes, swales, water control structures, and wetland systems which outfall to a finger canal of Lake Bethel, with ultimate discharge to Lake Monroe and the St. Johns River. The first segment of the system extends downstream from the weir structure on the west shore of Lake Doyle via a pipe entrenched in the upland berm of the Sheryl Drive right-of-way. The pipe passes under Doyle Road and through xeric pine-oak uplands to the northeast shore of a large (approximately 15 acres) deepwater marsh. Water flows south through the deepwater marsh where it outfalls through four pipes at Ledford Drive. Two of the four pipes are overflow structures, controlled by canal gates. The pipes at Ledford Drive discharge into a ditch and into a large (greater than 20 acres) shallow bay swamp. The south end of the bay swamp is defined (and somewhat impounded) by a 19th Century railroad grade. Water flows through the bay swamp where it outfalls through five pipes at the railroad grade. Three of the five pipes are overflow structures, controlled by channel boards. The pipes at the railroad grade discharge to a 1500-foot long finger canal that was dug some time during the period 1940-1972 from the north central shore of Lake Bethel. The overflow interconnection system has three locations whereby the system can be shut down: 1) Lake Doyle--a control weir, controlled by three sluice gates; 2) Ledford Drive--two thirty-inch reinforced concrete pipes, controlled by canal gates; and 3) railroad grade--three thirty-inch reinforced concrete pipes, controlled by channel boards (collectively referred to as "Overflow Structures"). The Overflow Structures are designed to carry the discharge of water from Lake Doyle to Lake Bethel. With the Overflow Structures closed the system returns to pre-construction characteristics, meaning there will be no increase or decrease in the quantity or quality of water throughout the path of the system as a result of the project. An unequivocal condition of the permit is that the system would operate with all of the Overflow Structures closed. As an added assurance, the City proposes to place a brick and mortar plug in the Lake Doyle weir structure outfall pipe to prevent any discharge from the weir. The City has submitted to the District preliminary plans for a future phase in which the system would be modified for the purpose of alleviating high water levels within the Lake Theresa Basin when the water level in Lake Doyle rises above an elevation of 24.5 feet. The District shall require a separate permit application to be submitted for such future plans. Petitioner, Barbara Ash, has lived on Lake Theresa for 19 years. Ms. Ash lives upstream from the area of the weir that will be plugged in accordance with the ERP. She does not trust either the City of Deltona to comply with or the District to enforce the conditions of the ERP applied for by the City. Petitioner, Barbara Ash, also served as the qualified representative for Petitioners, Francell Frei, Bernard J. and Virginia Patterson, and Ted and Carol Sullivan. Ms. Ash represented that Ms. Frei has lived on Lake Theresa for 12 years, and both the Pattersons and the Sullivans live on Lake Louise, which is within the area of concern in this proceeding. Petitioner, Diana Bauer, has lived on Lake Theresa since February 2004. She fears that the lake will become too dry if the system is allowed to flow. She also believes the wildlife will be adversely affected if the water levels are too low since many species need a swampy or wet environment to thrive. She fears her property value will decrease as a result of the approval of the ERP. She also does not trust either the City to comply with or the District to enforce the conditions of the ERP. Petitioner, Howard Ehmer, lives two to three hundred yards down Lake Theresa from Ms. Bauer. He is concerned about the lake bed being too dry and attracting people on all terrain vehicles who enjoy driving around the lake bottom. He is concerned about his property value decreasing if the lake bed is dry. Further, when the lake level is too low, people cannot enjoy water skiing, boating, and fishing on Lake Theresa. Petitioner, Phillip Lott, a Florida native, has also owned and lived on property abutting Lake Theresa since 1995. Mr. Lott has a Ph.D. in plant ecology, and M.P.A. in coastal zone studies, an M.B.A. in international business, and a B.S. in environmental resource management and planning. Mr. Lott has been well acquainted with the water levels on Lake Theresa for many years. Based upon his personal observations of the lake systems in the Deltona area over the years, Mr. Lott has seen levels fluctuate greatly based upon periods of heavy and light rainfall. Mr. Lott is concerned that the District will permit the City to open the weir to let water flow through the system and cause flooding in some areas and low water levels in other areas. He fears that the District will allow the water to flow and upset the environmental balance, but he admits that this ERP application is for a closed system that will not allow the water to flow as he fears. Mr. Lott similarly does not trust the City to comply with and the District to enforce the conditions of the ERP. Petitioners, James E. and Alicia M. Peake, who were represented by Steven L. Spratt at hearing as their qualified representative, live on Lake Louise, which is interconnected with the Lake Theresa basin. The Peakes are concerned that if the level of Lake Louise drops below 21 feet, nine inches, they will not be able to use the boat launch ramps on the lake. Petitioner, Steven L. Spratt, also lives on Lake Louise, and is concerned about the water levels becoming so low that he cannot use the boat launch on the lake. He has lived on the lake since 2000, and remembers when the water level was extremely low. He fears that approval of the ERP in this case will result in low levels of water once again. Petitioner, Gloria Benoit, has live on Lake Theresa for two years. She also enjoys watching recreational activities on the lake, and feels that approval of the ERP will devalue her lakefront property. Ms. Benoit appeared at the first day of the hearing, but offered no testimony on her behalf. J. Christy Wilson, Esquire, appeared prior to the final hearing as counsel of record for Petitioners, Steven E. Larimer, Kathleen Larimer, and Helen Rose Farrow. Neither Ms. Wilson nor any of the three Petitioners she represented appeared at any time during the hearing, filed any pleadings seeking to excuse themselves from appearing at the final hearing, or offered any evidence, testimony, pre- or post- hearing submittals. Petitioner, Gary Jensen, did not appear at hearing, did not file any pleadings or papers seeking to be excused from appearing at the final hearing, and did not offer any evidence, testimony, pre- or post-hearing submittals. Both the City and the District recognize that areas downstream from the project site, such as Stone Island and Sanford, have experienced flooding in the past in time of high amounts of rainfall. The system proposed by the City for this ERP will operate with the overflow structures closed and a brick and mortar plug in the outfall pipe to prevent water flow from Lake Doyle to Lake Bethel. So long as the overflow structures are closed, the system will mimic pre-construction flow patterns, with no increase in volume flowing downstream. The District has considered the environment in its proposed approval of the ERP. The area abutting the project is little urbanized and provides good aquatic and emergent marsh habitat. With the exception of the western shore area of the deepwater marsh ("west marsh area"), the bay swamp and remaining deepwater marsh area have good ecological value. In the 1940's, the west marsh area was incorporated into the drainage system of a poultry farm that occupied the site. This area apparently suffered increased nutrient influxes and sedimentation that contributed to a proliferation of floating mats of aquatic plants and organic debris. These tussocks reduced the deepwater marsh's open water and diminished the historical marsh habitat. Water under the tussocks is typically anoxic owing to total shading by tussocks and reduced water circulation. Thick, soft, anaerobic muck has accumulated under the matted vegetation. Exotic shrubs (primrose willow Ludwigia peruvania) and other plants (cattails Typha spp.) dominate the tussocks. The construction of the project, from the 2003 Emergency Order, resulted in adverse impacts to 1.3 acres of wetlands having moderately high- to high ecological value and 0.2 acres of other surface waters. The 0.2 acre impact to other surface waters was to the lake bottom and the shoreline of Lake Doyle where the weir structure was installed. The 0.3 acres of wetland impacts occurred at the upper end of the deepwater marsh where the pipe was installed. The largest wetland impact (1.0 acre) was to the bay swamp. The bay swamp is a shallow body dominated by low hummocks and pools connected inefficiently by shallow braided channels and one acre is filled with a 1-2 foot layer of sediment following swamp channelization. Disturbance plants (e.g., primrose willow, Ludwigia peruvania, and elderberry Sambucus Canadensis) now colonize the sediment plume. Pursuant to the District's elimination and reduction criteria, the applicant must implement practicable design modifications, which would reduce or eliminate adverse impacts to wetlands and other surface waters. A proposed modification, which is not technically capable of being done, is not economically viable, or which adversely affects public safety through endangerment of lives or property is not considered "practicable." The City reduced and/or eliminated the impacts to the lake bottom and shoreline of Lake Doyle and deepwater marsh, to the extent practicable. The impacts were the minimum necessary to install the weir structure and pipe for the system; the weir structure and pipe were carefully installed on the edges of the wetland and surface water systems, resulting in a minimum amount of grading and disturbance. To compensate for the loss of 1.3 acres of wetlands and 0.2 acres of other surface waters, the City proposes to preserve a total of 27.5 acres of wetlands, bay swamp, marsh, and contiguous uplands. Included in this 27.5 acres are 6.4 acres of the west marsh, which are to be restored. The parties stipulated that the mitigation plan would adequately compensate for losses of ecological function (e.g. wildlife habitat and biodiversity, etc.) resulting from the project. Water quality is a concern for the District. Lake Monroe is included on the Florida Department of Environmental Protection's verified list of impaired water bodies for nitrogen, phosphorous, and dissolved oxygen. Water quality data for Lake Monroe indicate the lake has experienced high levels of nitrogen and phosphorous and low levels of dissolved oxygen. Prior to construction of the project, there was no natural outfall from the Lake Theresa Basin to Lake Monroe and therefore no contribution from this basin to nitrogen and phosphorous loadings to Lake Monroe. Lake Colby, Three Island Lakes (a/k/a Lake Sixma), and the Savannah are surface waters within the Lake Theresa Basin for which minimum levels have been adopted pursuant to Florida Administrative Code Chapter 40C-8. The system will operate with the overflow structures closed and a brick and mortar plug in the outfall pipe to prevent water flow from Lake Doyle to Lake Bethel, resulting in no outfall from the Theresa Basin to Lake Monroe. Minimum flows established for surface waters within the Lake Theresa Basin will not be adversely impacted. Under the first part of the secondary impact test, the City must provide reasonable assurance that the secondary impacts from construction, alteration, and intended or reasonable expected use of the project will not adversely affect the functions of adjacent wetlands or surface waters. The system is designed as a low intensity project. As proposed, little activity and maintenance are expected in the project site area. The reasonably expected use of the system will not cause adverse impacts to the functions of the wetlands and other surface waters. None of the wetland areas adjacent to uplands are used by listed species for nesting or denning. In its pre-construction state, the project area did not cause or contribute to state water quality violations. Under the second part of the secondary impact test, the City must provide reasonable assurance that the construction, alteration, and intended or reasonably expected uses of the system will not adversely affect the ecological value of the uplands to aquatic or wetland dependent species for enabling existing nesting or denning by these species. There are no listed threatened or endangered species within the project site area. Under the third part of the secondary impact test, and as part of the public interest test, the District must consider any other relevant activities that are closely linked and causally related to any proposed dredging or filling which will cause impacts to significant historical and archaeological resources. When making this determination, the District is required, by rule, to consult with the Division of Historical Resources. The Division of Historical Resources indicated that no historical or archaeological resources are likely present on the site. No impacts to significant historical and archaeological resources are expected. Under the fourth part of the secondary impact test, the City must demonstrate that certain additional activities and future phases of a project will not result in adverse impacts to the functions of wetlands or water quality violations. The City has submitted to the District preliminary plans for a future phase in which the system would be modified for the purpose of alleviating high water levels within the Lake Theresa Basin when the level in Lake Doyle rises above an elevation of 24.5 feet. Based upon the plans and calculations submitted, the proposed future phase, without additional measures, could result in minor increases in the loadings of nitrogen and phosphorous to Lake Monroe. Lake Monroe is included on the Florida Department of Environmental Protection's verified list of impaired water bodies due to water quality data indicating the lake has experienced high levels of nitrogen and phosphorous, and low levels of dissolved oxygen. Under this potential future phase, there would be an outfall from the Lake Theresa Basin to Lake Monroe. To address the impact on water quality of this potential future phase, the City has submitted a loading reduction plan for nitrogen, phosphorous, and dissolved oxygen. The plan includes compensating treatment to fully offset the potential increased nutrient loadings to Lake Monroe. Specifically, the loading reduction plan includes: Construction and operation of compensating treatment systems to fully offset anticipated increased nutrient loadings to Lake Monroe. Weekly water quality monitoring of the discharge from Lake Doyle for total phosphorous and total nitrogen. A requirement that the overflow structure be closed if the total phosphorous level reaches 0.18 mg/l or higher or the total nitrogen level reaches 1.2 mg/l or higher in any given week and will remain closed until levels fall below those limits. The implementation of these water quality mitigation measures will result in a net improvement of the water quality in Lake Monroe for nitrogen, phosphorous, or dissolved oxygen. The future phase was conceptually evaluated by the District for impacts to wetland functions. The future phase as proposed could result in adverse impacts to wetland functions. Operation of the system with the overflow structures open could impact the bay swamp and deepwater marsh. The City has demonstrated that any adverse impacts could be offset through mitigation. Based upon the information provided by the City and general engineering principles, the system is capable of functioning as proposed. The City of Deltona will be responsible for the operation, maintenance, and repair of the surface waster management system. A local government is an acceptable operation and maintenance entity under District rules. The public interest test has seven criteria. The public interest test requires the District to evaluate only those parts of the project actually located in, on, or over surface waters or wetlands, to determine whether a factor is positive, neutral, or negative, and then to balance these factors against each other. The seven factors are as follows: the public health, safety, or welfare of others; conservation of fish and wildlife and their habitats; fishing, recreational value, and marine productivity; temporary or permanent nature; 5) navigation, water flow, erosion, and shoaling; 6) the current condition and relative value of functions; and 7) historical and archaeological resources. There are no identified environmental hazards or improvements to public health and safety. The District does not consider impacts to property values. To offset any adverse impacts to fish and wildlife and their habitats, the City has proposed mitigation. The areas of the project in, on, or over wetlands do not provide recreational opportunities. Construction and operation of the project located in, on, or over wetlands will be permanent in nature. Construction and operation of the project located in, on, or over wetlands will not cause shoaling, and does not provide navigational opportunities. The mitigation will offset the relative value of functions performed by areas affected by the proposed project. No historical or archaeological resources are likely on the site of the project. The mitigation of the project is located within the same drainage basin as the project and offsets the adverse impacts. The project is not expected to cause unacceptable cumulative impacts.
Recommendation Based upon the Findings of Fact and Conclusions of Law, it is RECOMMENDED that a Final Order be entered granting the City of Deltona's application for an environmental resource permit with the conditions set forth in the Technical Staff Report, and dismissing the Petitions for Formal Administrative Hearing filed by Gary Jensen in Case No. 04-2405, and by Steven E. Larimer, Kathleen Larimer, and Helen Rose Farrow in Case No. 04-3048. DONE AND ENTERED this 27th day of May, 2005, in Tallahassee, Leon County, Florida. S ROBERT S. COHEN Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 27th day of May, 2005. COPIES FURNISHED: George Trovato, Esquire City of Deltona 2345 Providence Boulevard Deltona, Florida 32725 Diana E. Bauer 1324 Tartan Avenue Deltona, Florida 32738 Barbara Ash, Qualified Representative 943 South Dean Circle Deltona, Florida 32738-6801 Phillip Lott 948 North Watt Circle Deltona, Florida Howard Ehmer Nina Ehmer 32738-7919 1081 Anza Court Deltona, Florida 32738 Francell Frei 1080 Peak Circle Deltona, Florida 32738 Bernard T. Patterson Virginia T. Patterson 2518 Sheffield Drive Deltona, Florida 32738 Kealey A. West, Esquire St. Johns River Water Management District 4049 Reid Street Palatka, Florida 32177 J. Christy Wilson, Esquire Wilson, Garber & Small, P.A. 437 North Magnolia Avenue Orlando, Florida 32801 Gloria Benoit 1300 Tartan Avenue Deltona, Florida 32738 Gary Jensen 1298 Tartan Avenue Deltona, Florida 32738 James E. Peake Alicia M. Peake 2442 Weatherford Drive Deltona, Florida 32738 Steven L. Spratt 2492 Weatherford Drive Deltona, Florida 32738 Ted Sullivan 1489 Timbercrest Drive Deltona, Florida 32738 Kirby Green, Executive Director St. Johns River Water Management District 4049 Reid Street Palatka, Florida 32177
The Issue Whether the activities conducted on respondent's property required a dredge/fill permit and whether respondent violated the conditions of the permit issued on February 15, 1985.
Findings Of Fact Respondent is the record holder of a parcel of land located within Section 35, Township 45, South, Range 21 East, in Lee County, Florida. Respondent's property is contiguous to Pine Island Sound, a Class II, Outstanding Florida Water. Maureen Powers, an Environmental Specialist with the Department initially inspected respondent's property on May 23, 1984, after the Department received an anonymous complaint that someone was clearing away mangroves on the property. Ms. Powers-discovered that an earthen-fill road had been constructed on the property, and a portion of the road, 24' x 43'; was located within the landward extent of the state's waters. The determination that the portion of the road was within the Department's jurisdiction was based on the dominance of black and white mangroves. There had been recent mangrove cutting in the area, and a pile of vegetative debris, the result of the cutting, had been placed in the jurisdictional wetlands contiguous to Pine Island Sound. On June 1, 1984, Ms. Powers met with respondent in Langley Adair's office to discuss the violations observed on May 23, 1984, and to discuss the resolution of these violations. Respondent agreed to remove all of the earthen fill and vegetative debris that he had deposited within the jurisdictional wetlands. He agreed to refrain from any further work within the jurisdictional area prior to receiving a permit from the department. He also agreed to open up a flow channel in the berm along Pine Island Sound to restore circulation to the area. On July 11, 1984, Ms. Powers conducted an on-site inspection and discovered that the vegetative debris and the fill material had not been removed. Further, it was apparent that respondent's proposed home site, outlined by string and stakes, was submerged and directly connected by water to Pine Island Sound. The water standing on the property covered a portion of the fill area. On August 8, 1984, another inspection was performed, and it was discovered that respondent still had not removed the fill materials. The condition of the property was essentially the same as it had been on July 11, 1984. By letter dated August 20, 1984, respondent was again notified of the violations and reminded that he had agreed on June 1, 1984, to remove the vegetative and earthen fill. Respondent was informed that he needed to remove the fill materials within 30 days of receipt of the letter in order to avoid further enforcement action. On September 5, 1984, Ms. Powers again inspected the property and found that the proposed homesite and a portion of the fill were still submerged, that the water connected directly with Pine Island Sound and the fill materials had not been removed. Also apparent was a flume of milky white water which originated at the toe of the fill and continued into Pine Island Sound. Water samples were taken which revealed that the erosion of the unauthorized fill was resulting in a violation of state surface water quality criteria, specifically, turbidity1 greater than 29 Nephelometric Turbidity Units above natural background. The background sample, taken upstream from the site of the discharge, had a value of 5.2 turbidity units. The water sample taken two feet from the toe of the fill had a value of 69 turbidity units, and the sample from Pine Island Sound waterward of the mangrove fringe had a value of 46 turbidity units. On October 9, 1984, a letter was sent to respondent which pointed out that the earthen and vegetative fill had not been removed and notifying respondent that erosion of the earthen fill into the waters of Pine Island Sound had resulted in violation of surface water quality criteria. Respondent was requested to immediately cease and desist from all unauthorized. activity under the Department's jurisdiction. To clarify the situation, original photos of the site were sent with the letter which showed the earthen fill, the vegetative debris, and the turbid water leaving the site. A diagram of the site was also included to show the location fill materials that were to have been removed. On October 25, 1984, Ms. Powers met with Mr. Decker at the site. Ms. Powers showed respondent the earthen fill and vegetative debris that should have been removed. Ms. Powers noted that the waterward 23' x 24' section of the earthen fill had become heavily colonized by black mangrove seedings and, therefore, excepted that portion of the fill from the removal requirement so that the seedlings would not be disturbed. Mr. Decker stated that he would remove the unauthorized fill within two weeks. Meanwhile, apparently in September, respondent had submitted a permit application. Mr. Beaver was the field inspector assigned by DER to evaluate the application and make a recommendation on the feasibility of the project to the dredge and fill supervisor. On October 8, 1984, Mr. Beaver performed the field inspection at the site, and on October 23, 1984, issued his permit application appraisal recommending that the application be denied. Mr. Beaver recommended that the project be reconsidered for a permit if, among other things, the house site were removed from the landward extent of the state waters and located in the uplands, the septic tank were removed from the low lying portions of the site, and previously cut areas were allowed to regrow in native vegetation. On November 15, 1984, Mr. Beaver met with Mr. Decker and Mr. Cantrell, the district supervisor of dredge and fill, to discuss the project. Mr. Cantrell asked how the project could be modified so that Mr. Decker could have his house in the location where he wanted it. Mr. Beaver suggested a stilt, elevated house with a small fill pad that would allow access to the entrance of the house. The house would have to be elevated -enough so that revegetation of wetland plants could occur underneath the house structure and water flow could be maintained. On November 19, 1984, Ms. Powers and Mr. Beaver met Mr. Decker at the property. Ms. Powers and Mr. Beaver staked the DER jurisdiction line and marked the proposed location of Mr. Decker's boardwalk. Mr. Decker asked about placing wood chip mulch on the wetlands on his property in order to beautify the area. Mr. Decker was informed that wood chip mulch was considered vegetative fill and would require modification of his permit application. Subsequent to the meeting of November 15 and the on- site inspection of November 19, Mr. Decker modified his project. However, wood chip mulch was not mentioned. On December 7, 1984, Mr. Beaver recommended that the application be approved subject to specified conditions, which were ultimately incorporated into the permit. On December 11, 1984, Ms. Powers inspected the site and discovered that a large pile of wood chips had been placed on the northeast end of the fill road waterward of the jurisdiction line. The vegetative debris and earthen fill that had previously been on the project had not been removed. Respondent was notified of the violations by a Cease and Desist letter dated January 4, 1985. The letter pointed out that respondent had been told specifically that wood chip mulch was considered vegetative fill and that dredge/fill permit would be required prior to the placement of any fill material. On February 5, 1984, respondent met with DER, officials to discuss the violations. Mr. Decker stated that the fill had been removed as requested. The Department informed Mr. Decker that an inspection would be performed and, if the fill had not been removed, the Department would pursue formal enforcement action. On February 7, 1985, the site was inspected none of the fill material had been removed. A subsequent inspection on February 20, 1985, revealed that the wood chips had been spread throughout the jurisdictional wetlands. On February 15, 1985, respondent received a permit to fill and to construct a dock and boardwalk. The specific conditions of the permit include the following: 2. A 20' x 16' - 4" fill pad shall be the only fill placed waterward of the jurisdictional line. This fill pad will be composed of clean sand and have the banks stabilized by a riprap revetment with a slope not greater than 2H:1V. * * * The house and all associated structures shall be built upon stilts with concrete footings and/or wooden pilings. On-site turbidity control devices shall be installed and properly maintained to localize turbidity impacts to the construction area. * * * All vegetative debris, trash and spoil material resulting from concrete footing placement shall be removed from the landward extent of State Waters as defined by the jurisdiction line staked by the DER. Upon completion of construction, non- filled areas beneath the stilt house and associated structures shall be returned to original grade if they were altered by construction. Wetland vegetation shall be planted in the previously cleared area and mangroves removed by construction activities shall be replaced on a 2 for 1 basis with 80% survival over a three year period. * * * 11. The project shall comply with applicable State Water Quality Standards, namely: 17-3.051 - Minimum Criteria for All Waters at All Times and All Places. 17-3.061 - Surface Waters: General Criteria 17-3.111 - Criteria - Class II Waters Shellfish Propagation or Harvesting, Surface Waters General Conditions 2 and 5 of the permit provide: 2. This permit is valid only for the specific processes and operation applied for and indicated in the approved drawings or exhibits. Any unauthorized deviation from the approved drawings, exhibits, specifications, or conditions of this permit may constitute grounds for 81' filled area was located within the landward extent of the state waters. 19. Respondent has violated several conditions of the permit issued February 15, 1985. Specific Condition #2 provided that the 20' x 16' fill pad would be "the only fill placed waterward of the jurisdictional line." Instead, respondent filled an area approximately 78' x 81' to an average height of about 2\', totaling approximately 585 cubic yards of fill. The fill was non-native fill brought onto the site. The permit did not authorize fill for a septic tank in the revocation and enforcement action by the department. 5. This permit does not relieve the permittee from liability for harm or injury to human health or welfare, animal, plant or aquatic life or property and penalties therefor caused by the construction or operation of this permitted source, nor does it allow the permittee to cause pollution in contravention of Florida Statutes and department rules, unless specifically authorized by an order from the department. On March 19, 1985, an inspection of the property revealed that Mr. Decker had totally ignored the conditions of his permit. Rather than a fill pad of 20' x 16', respondent had filled an area approximately 78' x 81'.2 The fill was unstabilized, and no turbidity control devices were in place. Fill material had been used to construct a earthen berm across a natural flow channel, blocking the flow of water onto the property. Further, the vegetative debris resulting from the construction of the boardwalk had been deposited in the mangrove wetlands. On March 22, 1985, a Notice of Violation and. Orders for Corrective Action was sent to the respondent. Respondent received the notice on or about March 26, 1985. The landward extent of the state waters on respondent's property, the area in which a DER permit is required for dredging and filing, was determined by the presence of red mangroves (Rhizophora mangle), black mangroves (Avicennia germinans), and saltwort (Basis maritime) as the dominant species. The jurisdiction line was originally staked on November 19, 1984, and was reestablished on April 23, 1985, from remaining landmarks, due to the original markers being removed. The 78' x81' filled area was located within the landward extent of the state waters. Respondent has violated several conditions of the permit issued February 15, 1985. Specific Condition #2 provided that the 20' x 16' fill pad would be "the only fill placed waterward of the jurisdictional line." Instead, respondent filled an area approximately 78' x 81' to an average height of about 21/2', totaling approximately 585 cubic yards of fill. The fill was non-native fill brought onto the site. The permit did not authorize fill for a septic tank in the jurisdictional wetlands, but respondent placed a septic tank and drainfield in that area.3 By filling an area several times the size of the area authorized, respondent has seriously violated the conditions of the permit. A fill area of the size that now exists eliminates the habitat and water quality functions that the area historically performed. Respondent has violated Specific Condition #4, which required that the house and associated structures be built on stilts. The purpose of such a requirement is to preserve undisturbed the existing substrate, which constitutes the base of the food chain, and to allow for a free flow of water across the site, which is essential to the health of the mangrove system. Respondent not only filled an area larger than his proposed house, he poured a solid, continuous, concrete foundation on top of the fill, which would prevent the flow of water should the water rise high enough to come onto the filled area.4 By filling the area, destroying the substrate, and preventing the flow of water into the area, respondent has violated Specific Condition #4 of the permit. Respondent violated Specific Condition #5 of his permit in that respondent failed to install any turbidity control devices. Turbidity control devices of some sort are necessary in a fill area such as the one in this case. Turbidity screens or staked hay bales could have been used. Respondent also violated Specific Condition #8. Construction debris and vegetative debris were located throughout the area. Although respondent technically has not violated Specific Condition #9, in that it requires acts to be performed "upon completion of construction", respondent has made compliance with that provision an impossibility because he has filled the "non- filled areas beneath the stilt house" and therefore there are no "non-filled areas" to return to original grade. Respondent has never requested that his permit conditions and requirements be modified. By his actions, respondent has repeatedly shown a complete disregard for the requirements of the law, and he has totally ignored the conditions set forth in the permit. Mr. Decker was not qualified as an expert and I did not find him to be a credible witness. The reasonable costs and expenses incurred by the Department in relation to the enforcement aspects of this action are $866.17. These costs and expenses were incurred by the Department in its effort to control and abate pollutants and to restore the waters and property of the state to their former condition.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the respondent's permit, number 360902245, be revoked that the respondent be ordered to make payment to the Department in the amount of $866.17 for costs and expenses incurred by the state and that the following corrective action be ordered: Respondent shall within thirty (30) days, remove all unauthorized fill material placed within the area of Department jurisdiction. Prior to initiating the fill removal respondent shall arrange for Department personnel to stake the area to be restored. All areas shall be restored to the elevation and soil conditions which existed prior to the placement of fill material. Respondent shall take all necessary precautions to ensure that state water quality standards are not violated during the restoration work. Respondent shall not disturb adjacent areas within the jurisdiction of the Department unless approved by the Department in writing. DONE and ENTERED this a 24th day of January, 1986, in Tallahassee, Leon County, Florida. DIANE A. GRUBBS Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 FILED with the Clerk of the Division of Administrative Hearings this 24th day of January, 1986.
The Issue Whether Petitioner's application for a dredge and fill permit under Chapter 403, F.S. and PL 92-500, to conduct rock mining activities in Dade County, Florida should be approved. At the commencement of the hearing, the parties orally stipulated that the only matters in issue were those relating to biological integrity, lead, oil and grease, and dissolved oxygen, as affecting water quality pursuant to Chapter 17- 3, Florida Administrative Code, and the cumulative impact of this and other like projects in the general area in question. Additionally, Petitioner had amended his petition prior to hearing to allege that Respondent lacked jurisdiction over the proposed excavation activities because the project site is not located in the waters of the State. The jurisdictional question will he determined hereinafter in Conclusions of Law. At the hearing, Petitioner presented the testimony of five witnesses and submitted ten exhibits. Respondent called four witnesses and submitted six Rodney Dehan were received in evidence at the request of Petitioner as reflected in the hearing transcript. considered, and those portions thereof not adopted herein are deemed to be either unnecessary, irrelevant, or unsupported in fact or law. Petitioner Florida Mining and Materials Corporation, Tampa, Florida, a wholly owned subsidiary of Moore-McCormick Corporation, conducts rock mining 566 acres of land in Section 14, Township 55 South, Range 38 East, Dade County, Florida, for rock mining purposes. The tract of land is located about one mile Highway 41). The property is bounded on the east by Levee L31-N and a drainage canal. There are no public or private roads at the present time providing By application, dated May 19, 1980, which was filed with Respondent Department of Environmental Regulation (DER) on June 16, 1980, Petitioner (Testimony of Coleman, Petitioner's Exhibit 1) Respondent asked for additional information concerning the proposed To Deny the application on July 21, 1981. The stated grounds for the intended denial were that the proposed project would destroy approximately 566 acres of quality by the assimilation and transformation of nutrients, and that the project would destroy productive biological habitat which depends on and notice further stated that pollutants could be expected to enter waters of the State through the pits which would provide direct openings to the Biscayne create water bodies unable to meet State water quality standards. Finally, the notice stated that the cumulative impact of existing and proposed similar Everglades and the ground waters of the Biscayne aquifer, and that therefore Petitioner had not provided reasonable assurance pursuant to Rule 17-4.07 and not result in violations of water quality standards for surface waters. At the hearing, by stipulation of the parties, Respondent abandoned its concerns as to Respondent's Exhibit 1) Petitioner plans to dredge approximately 70 percent of the land area by dragline will total approximately 25,427,000 cubic yards. Approximately 353,000 cubic yards of the dredged material will be used as fill for roads, be transported to an on-site processing plant where it will be crushed, sized, washed, and then conveyed to storage piles of various size aggregate. Water and containing "face powder" size limestone residue will then be piped back into the lake. Material from the storage piles will be conveyed to a final wash station and sent to storage bins for loading on trucks, or by conveyer belt to an adjacent railroad spur for loading. No chemicals or additives are used in processing the material. Motor vehicles and heavy equipment used in the operation will use diesel fuel or unleaded gas. No oil or grease is introduced in the manufacturing cycle, although such materials will necessarily be used in connection with the operation of vehicles and equipment. A perimeter buffer zone of 85 feet will separate the pit excavations from adjacent property lines on the north, south and west sides of the site. On the east side, a rail siding will be set back 200 feet and the lakes 400 feet from the Levee L31-N right-of-way. A perimeter berm of undetermined size will encircle the entire site. A 25 foot wide road from the north of the site to the Tamiami Trail will be constructed on an 80-acre "alley" to permit access to and from the mining area. Maintenance roads will be constructed around the perimeters of the four lakes. An 18 foot wide drainage ditch will be constructed immediately behind the perimeter berm to receive runoff from the adjacent maintenance roads. Earth berms will encircle all excavated areas to eliminate surface water inflow. Lake excavation areas will comprise approximately 70 percent, or 394 acres, of the 566 acre site. The remaining land area will be 172 acres. Petitioner will be able to mine approximately 70 percent of the estimated twenty-four million tons of existing rock which underlies the land area. It is estimated that mining operations will take place for approximately fifteen to twenty years to remove the available rock material. There is a 2 foot layer of topsoil overlying the lime rock which will be stored to return non-excavated areas to their original level when the project is completed. The areas will be revegetated at that time. (Testimony of Coleman, Petitioner's Exhibits 1, 5,6,8) Although the project area has groundwater levels within one foot of tide land surface for most of an average year, surface water is on the site during a maximum of 36 days a year. Vegetation is present on approximately 55 percent of the property. The dominant species is sawgrass, although several other wetland species such as beakrush, marsh fleabane, spike rush, and maiden cane, are present to a lesser extent. Periphyton algal mats are found throughout the project area. Such mats provide habitat and protection for a variety of organisms and their egg masses. Sawgrass is one of the species listed in Rule 17-4.02(17), Florida Administrative Code which, under Rule 17- 4.28, Florida Administrative Code, is used as a guide in the establishment of the border of certain water bodies listed therein. (Testimony of Lotspeich, Molnar, Gatewood, Kraft, Respondent's Exhibits 4-6) The following findings address the stipulated issues as to whether Petitioner has given Respondent reasonable assurance that the proposed project will not result in water quality violations with respect to concentrations of lead, oil and grease, dissolved oxygen, and impacts on biological integrity in Class III waters: Lead--Petitioner will not use materials containing lead in the conduct of its rock mining operations, and therefore no water quality violation active rock mining pits in the general area revealed only negligible amounts of lead. (Testimony of Sullivan, Baljet, Petitioner's Exhibit 10) heavy equipment which require oil and grease incident to its excavation and mining operations. DER Rule 17-3.061(1)(j), Florida Administrative Code (as dissolved or emulsified oils and greases shall not exceed 5.0mg. per liter, nor shall visible oil be present to cause taste, odor, or interfere with the general area show that State standards are being met. It would take over 24,000 pounds of oil and grease to result in a violation of the quality standard on equipment and inspection should prevent other than insignificant discharges of oil and grease. Although oil sheens have been observed on water surfaces of situation would exist as a result of Petitioner's proposed operations. (Testimony of Sullivan, Baljet, Lotspeich, Kraft) waters provides that the concentration of dissolved oxygen shall not be less than 5 mg. per liter. Petitioner's proposed operation will not discharge oxygen dissolved oxygen. Excavation of the proposed lakes will permit interchange from the pits and surrounding groundwater. As groundwater rises to the surface, aeration. Tests of several water filled rock pits in the surrounding area meet state standards as to dissolved oxygen. The storage of excavated muck soil in which could lower the dissolved oxygen concentration, but the perimeter berms surrounding the lakes should prevent other than a minimal amount of such organic powder" size lime rock residue could present a suspended solids and BOD problem over a long term as it eventually forms a layer on the bottom of the lake. Such penetration and re-suspend easily. Although the waters of the rock pits probably will not meet the State standards of 5.0 mg. per liter at various of the groundwater in the area. Deep water bodies provide less water circulation and consequent lowered dissolved oxygen levels than do shallow (Deposition), Petitioner's Exhibit 10) d. Biological Integrity--Rule 17-3.121(7), F.A.C. provides that the reduced to less than 75 percent of established background levels. Sampling equipment to perform this test requires a minimum of seven inches of water for a October, 1981 after a hurricane at which time there was approximately 14 to 16 inches of surface water on the site. The test showed a moderate to slightly low levels and survive during the normally dry periods in pockets of water. They have a high degree of adaptability. Disruption to the regimes will be caused to the pit excavations which will divert sheet flow around the site. However, actual effects of the project cannot be determined until tests can be made after construction. However, the ability to perform valid testing on a sawgrass prairie where surface water is present only after rainfall over a total of 36 days a year is remote. Such tests are designed for lakes and streams. In the opinion of DER's chief biologist as to the use of a sampler, ". . .it is rather ridiculous to put it on a sawgrass prairie". (Testimony of Sullivan, Pruitt, Ross (Deposition)) DER asserted jurisdiction over Petitioner's proposed activities based on the fact that there is continuous sawgrass vegetation from the site southwest to the Shark River which begins at Florida Bay some 60 miles away. The Shark River is located in the southwestern portion of the State and sloughs from thee river proceed in undefined patterns to the northwest. Sheet flow from the sawgrass prairie area travels slowly in a southwesterly direction where it is drained by the Shark River system. However, only approximately 10 percent of surface water flow over Petitioner's site would reach the defined river which ends approximately 15 to 20 miles from the coast. No exchange of water from the Shark River takes place at Petitioner's site, nor does any tidal flow from Florida Bay reach that area. The sawgrass and other wetland species survive due to the high groundwater level in the area which generally results in damp soils. DER does not seek to assert jurisdiction arising from the project's proximity to the L31-N canal due to the existence of the adjacent dike which would prevent any discharge from Petitioner's site. However, it does consider that the Petitioner's land is within the landward extent of waters of the State in that it is a part of the water body either of the Shark River or of Florida Bay. (Testimony of Lotspeich, Molner, Gatewood, Kraft, Respondent's Exhibit 1) Although some 33 applications to conduct rock mining activities in Dade County have been received by DER over the years, the agency did not assert jurisdiction over those located east of the L31-N canal due to the fact that the canal altered the natural hydrological pattern of the area, and wetland species of vegetation no longer were dominant in the area. There is no other pending application for rock mining activities other than that of Petitioner to the west of the canal at the present time. (Testimony of Lotspeich, Kraft, Respondent's Exhibits 2-3) An additional ground stated by DER for proposed denial of the project is that approval of Petitioner's permit would set a precedent for future similar operations and that the cumulative impact of such projects would result in a decline of water quality of the surface waters of the Everglades. However, no applications for similar permits in the area near Petitioner's site are pending, nor have any been granted west of the L31-N canal to date. (Testimony of Lotspeich, Kraft, Respondent's Exhibit 2) It would therefore be speculative to base such a finding upon concerns about future possible applications which might be filed due to the presence of limestone rock in sufficient quantities for profitable operations. In 1976, Petitioner's request for a variance from Dade County zoning ordinances to permit mining on its site was denied by the county commission. Petitioner appealed the denial to the Dade County Circuit Court, which found that the county had acted in an arbitrary manner by permitting essentially identical mining activities on nearby tracts of land, and ordered the county to grant necessary permits for mining activities upon proper application by Petitioner. This decision was appealed to the Third District Court of Appeal which affirmed the lower court in Case No. 77-1223 on October 17, 1978. Thereafter, by resolution, dated July 19, 1979, the Dade County Board of County These conditions require adequate turbidity controls during construction, a temporary perimeter berm to permit silt runoff, stockpiling of excavated topsoil of the property to pre-excavation condition after completion of operations, construction of adequate culverts to maintain overland sheet flow, and other the conditions require the posting of a surety bond to ensure compliance with county requirements, and further purport to limit transfer of title to the the conclusion of mining operations, utilize the property for passive recreational purposes, or as a wildlife refuge. (Testimony of Coleman,
Recommendation That this proceeding be dismissed for lack of jurisdiction by Respondent Department of Environmental Regulation under Chapter 403, Florida Statutes. DONE and ENTERED this 12 day of April, 1982, in Tallahassee, Florida. THOMAS C. OLDHAM 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 12 day of April, 1982. COPIES FURNISHED: Ray H. Pearson, Esquire and Bruce A. Christensen, Esquire FLOYD, PEARSON, STEWART, RICHMAN GREER & WEIL, P.A. One Biscayne Tower - 25th floor Miami, Florida 33131 Paul R. Ezatoff, Jr., Esquire Assistant General Counsel Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 Honorable Victoria Tschinkel Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301
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.
The Issue The ultimate issue to be addressed in this proceeding is whether the Applicants should be granted a dredge and fill permit. Petitioner contends that the Applicants have failed to provide reasonable assurances that the short-term and long-term effects of their proposed activities will not result in violations of the Department's water quality standards for both surface water and groundwater. The Applicants and the Department contend that reasonable assurances have been provided.
Findings Of Fact The Applicants are the owners of a 1,248-acre parcel of land located at the intersection of State Road 710 and State Road 711 in northern Palm Beach County, Florida. The Applicants are proposing to develop an industrial park known as "Palm Beach Park of Commerce" (PBPC). PBPC will provide sites for tenants to carry on various commercial and industrial activities. In order to prepare the site for development, the Applicants have designed a surface water management system. In order to develop the system, the Applicants must conduct dredging and filling activities in areas where the Department of Environmental Regulation has permitting jurisdiction. The Petitioner is an association of home owners within a single family residential development known as "Caloosa." The development is located to the southeast of the proposed PBPC. Surface and ground water flows from the PBPC site are toward Caloosa. Residents of Caloosa and members of the Petitioner are entirely dependent on private individual wells for their drinking water. The surficial aquifer is the only viable source of drinking water. The proposed PBPC surface water management system would allow water to drain from the site into an excavated canal which would essentially follow the perimeter of the site. The canal would discharge at the southeast corner of the site into the Caloosa Canal, which runs through the Caloosa residential development. The Caloosa Canal is designated as a Class III water body. The Caloosa Canal drains into the "C-18 Canal," which is maintained by the South Florida Water Management District. The point at which the Caloosa Canal discharges into the C-18 Canal is approximately 2.4 miles from the PBPC site. The C-18 Canal is designated as a Class I water body. The C-18 Canal ultimately discharges into the Loxahatchee River Basin, a Class II water body, which is located approximately 12.9 miles from the PBPC site. It is possible that during some periods of the year, water from the PBPC site would ultimately find its way to the Jonathan Dickinson park, where water has been designated as "outstanding Florida waters." It is approximately 13.2 miles from the PBPC site to the Jonathan Dickinson Park. The PBPC site is a high, marginal, stressed Everglades system. It is a prairie or pine flatwood area. During periods of heavy rainfall, water covers most of the site. During dry periods, there is standing water only in depressions. Approximately 200 acres of the site are inundated with water during a sufficient portion of the year to support predominantly wetland vegetation. Approximately 24 acres of the wetlands on the site are directly connected to drainage ditches that presently rim the site. The ditches are connected to the Caloosa Canal so that these 24 acres are ultimately connected through canal systems to the Loxahatchee River. These wetland areas, which will be hereafter referenced as "jurisdictional wetlands," are the only wetland areas other than the existing drainage ditches over which the Department of Environmental Regulation asserts jurisdiction under its Rule 17-4.28, Florida Administrative Code. As a part of its surface water management system, the Applicants propose to maintain 133.7 acres of the wetlands on the site in their natural condition. These wetland areas would be incorporated into the surface water management system so that surface water would flow into the wetlands, then through culverts or drainage ditches into the perimeter canal. The remaining wetlands on the site, including all of the "jurisdictional wetlands," would be filled. The wetlands on the PBPC site perform a significant water quality function. The wetlands serve as a filtration system. Wetland vegetation removes nutrients and turbidity from surface water before it is discharged into the canals and ultimately into the Loxahatchee River. The wetlands that the Applicants propose to preserve on the site would continue to perform that beneficial function. In order to mitigate the loss of the wetlands that would be filled, the Applicants propose to create approximately 85 acres of new wetland areas and to vegetate these areas. These artificially created wetlands, if properly constructed, vegetated and maintained, would perform the same beneficial functions as the natural wetland communities. The Applicants have proposed to introduce several safeguards into their water management system to assure that the quality of surface and ground water in the area will not be adversely impacted. The preservation of 133 acres of natural wetland areas and the creation of approximately 85 acres of artificial wetland areas is one of these safeguards. In addition, the surface water management system includes the creation of swales around water bodies so that the first one inch of stormwater runoff on the site will not drain directly into surface water bodies. By retaining the first one inch of runoff, pollutants contained in stormwater runoff will be retained on the site and will not enter surface or ground waters. Each commercial or industrial site at PBPC will be required to retain an additional one inch of stormwater runoff on the individual site. This will serve to filter pollutants out of stormwater runoff even before the runoff reaches the overall surface water management system in which one inch of runoff will also be retained on site. The Applicants have also agreed to establish a surface water quality management program to prohibit the discharge of any industrial waste into the surface water management system and to have the surface water management system maintained by the Northern Palm Beach Water Control District. There are further safeguards proposed by the Applicants. The Applicants have agreed to prohibit the most potentially hazardous industrial activities from being undertaken on the site. Applicants have also agreed to require each individual site plan to be reviewed by local government, the South Florida Water Management District, and the Department of Environmental Regulation so that potential water quality problems connected with site-specific uses can be identified and, if necessary, prohibited. The Applicants have agreed to establish an environmental liaison officer whose function will be to monitor all development on the site and report routinely to local government, the South Florida Water Management District, and the Department of Environmental Regulation regarding environmental issues. In order that any potential groundwater pollution can be detected and, if necessary, steps taken to remove pollutants from the groundwater, the Applicants have agreed to establish well- monitoring systems for the project as a whole and for individual sites. Individual site plans have not yet been formulated. It is not practical or possible to design water monitoring programs for the individual sites at this time. Once the nature of activities at a site are known, monitoring programs can be effectively set up and maintained. In the event that surface or ground water contamination occurs, it can be detected through monitoring programs, and the contaminants can be removed. The Applicants have provided reasonable assurance that the short-term and long-term effects of the construction of the PBPC water management system will not result in violations of the Department's water quality standards for surface or ground water. By use of turbidity screens during construction, short-term impacts will be negligible. Absent any construction on the site beyond the creation of the surface water management system, it is likely that the quality of water leaving the PBPC site will be as good or better than at present. Since the Applicants have not yet located tenants or made individual site plans for commercial and industrial activities within PBPC, it is not possible to determine if some specific activity in the future could operate to cause violations of the Department's water quality standards. In order that there be such assurances, the Applicants have agreed to subject individual site plans to review by local government, the South Florida Water Management District, and the Department of Environmental Regulation. In the event that a future tenant is not able to provide required assurances, the use can and should be prohibited, and can be prohibited by regulatory agencies as a condition of permits issued to the Applicants. Water quality violations presently occur in the Caloosa Canal and the C-18 Canal. The safeguards proposed by Applicants reasonably assure that the implementation of the proposed water management system will not exacerbate or cotribute to these violations. There is approximately an 11-square-mile area which drains into the Caloosa Canal through the outfall at the southeast corner of the PBPC site. The PBPC site constitutes approximately two square miles of this area. The remaining nine square miles are located to the north and west of the PBPC site. These off-site areas are undeveloped and have an ecology very similar to the presently undeveloped PBPC site. The evidence would not establish a finding that development of these off-site parcels together with development of the PBPC site would cumulatively result in water quality violations of surface or ground waters. The Applicants will be required to obtain permits to construct a wastewater treatment facility on the PBPC site. Whether any proposed wastewater treatment system will meet the standards of regulatory agencies would appropriately be considered in later proceedings. Similarly, individual tenants will, in some cases, be required to operate wastewater treatment systems that pretreat industrial waste before it is introduced into the system-wide wastewater treatment system or before it is otherwise removed from the site. These systems would also be subject to future permitting proceedings. Some of the potential activities that could be carried on by tenants at the PBPC involve the use of volatile organic compounds and other hazardous toxic substances. If proper techniques are not followed for the handling of such substances, or if some accident occurs, the substances could be introduced into the surface and ground waters. Review of each individual site plan and the establishing of systems for properly handling toxic substances can reduce the possibility of incidents occurring. Human frailties existing as they do, however, it is not unlikely that such an incident will occur. If such an incident occurs, it is vitally important that the contamination of surface or ground water be quickly detected and that steps be taken to remove the contaminant. The establishing of proper monitoring systems can reasonably assure that the contamination is identified. Techniques do exist for removing contaminants from surface and ground waters. Since individual tenants and site plans have not yet been established, it is not possible to make any finding as to whether any individual tenant or site plan might operate in such a manner as to cause violations of the Department's water quality standards. It is therefore appropriate that individual tenants and site plans be subjected to further review by appropriate regulatory agencies before they are permitted to operate on the PBPC site. The Applicants have agreed to such a review process. Since surface water flows into the Caloosa Canal can be controlled through the outfall structure at the southeast corner of the PBPC site, it appears practical to isolate any contaminant that might enter the surface water and to remove it. Groundwater flows in the aquifer lying below the PBPC site are very slow--less than one-tenth of one foot per day. Given such flow rates, it is likely that any contaminants that enter the groundwater can be detected and effectively removed. Even given the implementation of the best procedures for handling toxic substances, the best monitoring program for detecting accidental releases of the substances, and the best systems for removing the substances from surface and ground waters, there is some possibility that an accident could occur, that a contaminant would not be detected, and that violations of the Department's water quality standards could occur as a result in the Caloosa Canal or in the groundwater which underlies the Caloosa development and provides drinking water to residents there. The result of such an incident could have very serious impacts. The introduction of toxic substances into the surface waters could cause a substantial damage as far downstream as the Loxahatchee River Basin. Contamination of the groundwater could result in a loss of water supply to residents or in serious public health consequences. While such possibilities exist, they appear unlikely given the safeguards that have been proposed for PBPC. The Applicants do not propose to undertake any dredging or filling activities in any navigable waters.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED: That the Department of Environmental Regulation enter a final order issuing a permit to Caleffe Investment, Ltd., Worthington Enterprises, Inc., to conduct the dredging and filling activities proposed by the Applicants. To ensure that state water quality standards will not be violated, the conditions cited in the Department's Intent to Issue notice dated October 22, 1982, should be made a part of the permit. In addition, the following conditions should be made a part of the permit: All individual site plans within PBPC should be subject to the Department's permitting processes in accordance with Rule 17-4.28, Florida Administrative Code, and other provisions of Chapter 17, Florida Administrative Code, and Chapter 403, Florida Statutes, as may apply. The Applicants should be required to post bond in a sufficient amount to assure proper implementation and operation of monitoring systems for individual sites and to assure that adequate funds are available to remove and properly treat contaminants that might enter surface or ground waters as a result of accidents. RECOMMENDED this 19th day of May, 1983, in Tallahassee, Florida. G. STEVEN PFEIFFER Assistant Director 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 19th day of May, 1983. COPIES FURNISHED: Randall E. Denker, Esquire Lehrman & Denker Post Office Box 1736 Tallahassee, Florida 32302 Dennis R. Erdley, Esquire Alfred J. Malefatto, Esquire Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 Robert M. Rhodes, Esquire Terry E. Lewis, Esquire James Hauser, Esquire Messer, Rhodes & Vickers Post Office Box 1876 Tallahassee, Florida 32302 Alan J. Ciklin, Esquire Boose & Ciklin 8th Floor - The Concourse 2000 Palm Beach Lakes Boulevard West Palm Beach, Florida 33409 Tracy Sharpe, Esquire Farish, Farish & Romani 316 First Street West Palm Beach, Florida 33402 Ms. Victoria Tschinkel Secretary Department of Environmental Regulation 2600 Blair Stone Road Tallahassee, Florida 32301 Ms. Liz Cloud, Chief Administrative Code Bureau Department of State The Capitol, Suite 1802 Tallahassee, Florida 32301 Carroll Webb, Esquire Executive Director Administrative Procedures Committee Room 120, Holland Building Tallahassee, Florida 32301
