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USGS · fs15896

Hydrogeology of the surficial aquifer system in Southwest Florida

Abstract

Restoration and management of the south Florida ecosystem will be guided by hydrologic models that simulate water flowing through the wetlands and shallow subsurface aquifers beneath them. The restoration of the ecosystem is, essentially, the restoration of the natural hydrologic system. As surface water is re-diverted from manmade canals to its more natural state as overland flow, several changes are predicted to occur. First, because water flowing over land moves more slowly than in canals, overland flow should remain in the wetland ecosystem for a longer period each year. Second, as the flowing water spreads out over the wetlands, recharge to the shallow aquifers should increase as more of that water infiltrates into the ground. The U.S. Corps of Engineers and the South Florida Water Management District (SFWMD) will use hydrologic models to anticipate the consequences of these proposed restoration plans. This research program is designed to provide essential subsurface data to improve hydrologic models for land and water managers in southwest Florida where subsurface information is lacking. Obtaining hydrogeological data requires core drilling, corehole testing, and rock and sediment analysis.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 24.358839683418125° to 26.94633387241865° latitude; -81.87874513277362° to -80.00367070894046° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Members of the Engineering Geology and Ground Water Branches, U.S. Geological Survey. 1996-10-01. Hydrogeology of the surficial aquifer system in Southwest Florida. https://doi.org/10.3133/fs15896

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