'A.N.Severtsov Institute of Ecology and Evolution RAS - IEE RAS'
Abstract
Proceedings of the 2001 Georgia Water Resources Conference, April 26 and 27, 2001, Athens, Georgia.The Upper Floridan aquifer (UFA) it the principal source of groundwater for coastal Georgia and South Carolina. A progressive increase in goundwater
use since the late 1800s has resulted in a large (-30-mile
radius) cone of depression on the aquifer's potentiometric
surface that is centered on Savannah, GA. In coastal and
inner shelf areas where the overlying Miocene aquitard is
absent, the UFA is susceptible to seawater recharge. As part of the Sound Science Initiative (SSI), the Georgia Environmental Protection Division (EPD) recently funded
geophysical mapping to identify those locations where the
Miocene aquitard is thin or absent
Geophysical surveys identified ten Areas of Concern (ADCs) where the UFA is susceptible to seawater
intrusion. At each AOC, the aquifer is present at shallow
depth, erosion has removed the aquitard, the overlying
water column is saline, and the area lies within or adjacent to the Savannah cone of depression. Research results are contributing to a database of information being developed
under SSI that will provide input necessary for managing
groundwater resources in southeast Georgia.Sponsored and Organized by: U.S. Geological Survey, Georgia Department of Natural Resources, Natural Resources Conservation Service, The University of Georgia, Georgia State University, Georgia Institute of TechnologyThis book was published by the Institute of Ecology, The University of Georgia, Athens, Georgia 30602-2202. The views and statements advanced in this publication are solely those of the authors and do not represent official views or policies of The University of Georgia, the U.S. Geological Survey, the Georgia Water Research Institute as authorized by the Water Resources Research Act of 1990 (P.L. 101-397) or the other conference sponsors