Summary of the hydrology of the Southeastern Coastal Plain aquifer system in Mississippi, Alabama, Georgia, and South Carolina
USGS professional paper1992
Citations Over Time
Abstract
tion of the ground water. From outcrop areas downgradient, the fades are calcium bicarbonate, sodium bicarbonate, and sodium chloride. Geochemical modeling was used to demonstrate the likely chemical processes that have produced the observed water chemistry. Groundwater flow rates for the Pearl River, Chattahoochee River, and Black Warrior River aquifers derived by geochemical methods are 18,13, and 3 feet per year, respectively. These rates are compatible with rates of 14.8, 9.9, and 0.9 feet per year, respectively, independently derived from digital simulations of the flow system.
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