Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia
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Abstract
Long-term pumping from the Upper Floridan aquifer in the Savannah, Georgia, area has lowered ground-water levels, resulting in increased salinity of ground water by seawater encroachment at Hilton Head Island, S.C., and by saltwater intrusion at Brunswick, Ga. Increased pumpage could cause further salinization of the ground-water resources.
The Savannah and Ogeechee Rivers can be considered potential water-supply sources for the Savannah, Ga., area, on the basis of historic stream flow records and water-quality constituents and properties examined. Analyses of stream-discharge data indicate that the minimum average discharges for 7 consecutive days for a 10-year recurrence interval (7010), was 5,460 cubic feet per second (ft3/s) at Savannah River near Clyo, Ga., and 192 ft3/s at Ogeechee River near Eden, Ga. For example, 90 percent of the time, flows in excess of the 7010 discharges are about 900 and 200 ft3/s, respectively. However, Georgia Department of Natural Resources, Environmental Protection Division, imposes a non-depletable flow criterion; thus, the actual quantity of water available for withdrawal probably would be less than flows in excess of minimum flow criteria, such as the 7Q10.
Study Area
Publication type | Report |
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Publication Subtype | USGS Numbered Series |
Title | Water-supply potential of major streams and the upper Floridan Aquifer in the vicinity of Savannah, Georgia |
Series title | Open-File Report |
Series number | 92-629 |
DOI | 10.3133/ofr92629 |
Year Published | 1992 |
Language | English |
Publisher | U.S. Geological Survey |
Publisher location | Reston, VA |
Contributing office(s) | South Atlantic Water Science Center |
Description | Report: viii, 49 p.; 19 Plates: 17.34 x 19.64 inches or smaller |
Country | United States |
State | Georgia |
City | Savannah |
Other Geospatial | Floridan Aquifer |