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U.S. Department of Energy
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Geochemistry of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama

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OSTI ID:5379764

The chemical quality of the groundwater in the Floridan aquifer system is determined primarily by mineral-water interaction. However, some changes in water quality have been imposed by development, particularly near coastal pumping centers. A total of 601 chemical analyses, all from different wells, most completed in the upper part of the aquifer system, were used to describe the variations in water chemistry and to study the processes responsible for observed changes. The Floridan aquifer system is a vertically continuous sequence of Tertiary carbonate rocks that are of generally high permeability and are hydraulically connected in varying degrees. Dissolved solids concentrations in water from the Upper Floridan aquifer generally range from < 25 mg/L near outcrops to > 25,000 mg/L along the coasts. The dominant cations in the groundwater are Ca(2+), Mg(2+), and Na(+); the dominant anions are HCO3({minus}), Cl({minus}), and SO4(2{minus}). The concentration of Ca(2+) is controlled primarily by calcite saturation. Concentrations of Mg(2+), Na(+), and Cl({minus}) are highest where mixing of freshwater and saltwater occurs. Concentrations of HCO3({minus}) reflect the control of calcite solubility. The concentration of SO4(2{minus}) is highest where gypsiferous rock units are present in the aquifer system. The major geochemical processes that occur in the Upper Floridan aquifer, based on water quality maps and computations using a geochemical model are: (1) dissolution of aquifer minerals toward equilibrium; (2) mixing of groundwater with recharge, leakage, or seawater; (3) sulfate reduction; and (4) cation exchange between water and aquifer minerals.

OSTI ID:
5379764
Country of Publication:
United States
Language:
English