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2012 FDOT Mitigation Plan - Southwest Florida Water Management ...

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(Figure C), eradicate pasture grasses, conduct extensive planting, and perpetual herbicide maintenance<br />

activities.<br />

B. Brief description of pre-construction condition: Historically, surface water from Banana Lake<br />

maintained a sheet flow hydrology connectivity east through forested and marsh wetland habitat and flowing<br />

into Lake Hancock. During the 1940’s, the construction of the Banana Creek Canal between the two lakes,<br />

along with connecting tributary ditches, substantially drained the wetlands to convert into improved pasture.<br />

In addition, a large levee was constructed along the western property boundary (Figure C). This impounded<br />

water in the forested wetland west of the project area, diverted the ground and surface water away from the<br />

wetlands in the Reserve, and forced water to flow directly into the canal. Spoil material rimmed each side of<br />

the canal, so water in contributing conveyance ditches were also pumped over the berms into the canal to<br />

flow directly into Lake Hancock. The several decades of extensive drainage and dewatering converted the<br />

majority of the historic wetland acreage to improved pastures for intensive cattle grazing (refer to site<br />

photos). This resulted in inadequate hydrology to support appropriate wetland habitat benefits and functions<br />

to benefit wildlife. Prior to restoration construction in 2005-2006, the majority of the remnant wetlands were<br />

associated with a few forested wetlands bordering the pastures and scattered small ephemeral marsh<br />

pockets within the improved pastures. Historically there were additional forested wetlands that were lost as a<br />

result of the altered drainage and subsequent muck oxidation resulting in tree fall. In a complete reversal of<br />

the impounded surface waters in wetlands west of boundary levee, the remnant forested wetlands in the<br />

Reserve no longer had surface water. As a result, the forested areas were used for shade by cattle, with<br />

additional trees routinely falling due to the soil subsidence. Additional information is provided in the<br />

attachments.<br />

C. Brief description of conducted work: After the cattle lease was discontinued in 2001, the dewatering<br />

pump system was removed and with the rains from El Nino conditions in 2003 and Hurricanes Charley and<br />

Frances that crossed near the property in 2004, all drainage was not allowed to be conveyed into the canal in<br />

order to commence partial hydrologic restoration necessary to achieve the desired bahiagrass mortality and<br />

regeneration of hydrophytic vegetation. Construction activities commenced in the fall, 2005. Two pre-existing<br />

north-south berms (Figures B, C –Eastern and Central Roads) were substantially regraded to provide<br />

necessary structural stability and culverts installed at appropriate locations and elevations to convey and<br />

restore the natural sheet-flow wetland hydrology & appropriate hydroperiods. The length of the Central Road<br />

is approximately 3000 ft. and 2300 ft. for the Eastern Road. Fill material for the road berm reconstruction<br />

was obtained from widening the existing borrow pit within the north side of the property and creating the 2-<br />

acre “Gator Pond” marsh within an adjacent upland area. The western access road is a wet crossing<br />

constructed with crushed concrete to match adjacent surface grade elevations. After the two access road<br />

berms and culverts were constructed, the spoil rim material was used to backfill the Banana Creek Canal<br />

segment west of the Center Road and the western boundary levee was removed to restore hydrologic sheet<br />

flow patterns throughout the wetland floodplain. Approximately half of the historic western forested wetland<br />

213

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