Simulation of Reclaimed-Water Injection and Pumping Scenarios and Particle-Tracking Analysis near Mount Pleasant, South Carolina
Matthew D. Petkewich, Bruce G. Campbell
2009, Scientific Investigations Report 2009-5185
The effect of injecting reclaimed water into the Middendorf aquifer beneath Mount Pleasant, South Carolina, was simulated using a groundwater-flow model of the Coastal Plain Physiographic Province of South Carolina and parts of Georgia and North Carolina. Reclaimed water, also known as recycled water, is wastewater or stormwater that has...
Simulated Effects of Seasonal Ground-Water Pumpage for Irrigation on Hydrologic Conditions in the Lower Apalachicola-Chattahoochee-Flint River Basin, Southwestern Georgia and Parts of Alabama and Florida, 1999-2002
L. Elliott Jones, Lynn J. Torak
2006, Scientific Investigations Report 2006-5234
To determine the effects of seasonal ground-water pumpage for irrigation, a finite-element ground-water flow model was developed for the Upper Floridan aquifer in the lower Flint River Basin area, including adjacent parts of the Chattahoochee and Apalachicola River Basins. The model simulates withdrawal from the aquifer at 3,280 irrigation, municipal,...
Simulation of selected ground-water pumping scenarios at Fort Stewart and Hunter Army Airfield, Georgia
Gregory S. Cherry
2006, Open-File Report 2006-1148
A regional MODFLOW ground-water flow model of parts of coastal Georgia, Florida, and South Carolina was used to evaluate the effects of current and hypothetical groundwater withdrawal, and the relative effects of pumping in specific areas on ground-water flow in the Upper Floridan aquifer near Fort Stewart and Hunter Army...
Pond-aquifer flow and water availability in the vicinity of two coastal area seepage ponds, Glynn and Bulloch Counties, Georgia
John S. Clarke, Malek Abu Rumman
2005, Scientific Investigations Report 2004-5260
Pond-aquifer flow and water availability at excavated seepage pond sites in Glynn County and in southern Bulloch County, Georgia, were evaluated to determine their potential as sources of water supply for irrigation. Excavated seepage ponds derive water primarily from ground water seeping into the pond, in a manner similar to...
Quantifying contributions to storm runoff through end-member mixing analysis and hydrologic measurements at the Panola Mountain research watershed (Georgia, USA)
Douglas A. Burns, Jeffery J. McDonnell, R. P. Hooper, N.E. Peters, J.E. Freer, C. Kendall, K. Beven
2001, Hydrological Processes (15) 1903-1924
The geographic sources and hydrologic flow paths of stormflow in small catchments are not well understood because of limitations in sampling methods and insufficient resolution of potential end members. To address these limitations, an extensive hydrologic dataset was collected at a 10 ha catchment at Panola Mountain research watershed near...
Selecting remediation goals by assessing the natural attenuation capacity of groundwater systems
Francis H. Chapelle, Paul M. Bradley
1998, Bioremediation Journal (2) 227-238
Remediation goals for the source areas of a chlorinated ethene‐contaminated groundwater plume were identified by assessing the natural attenuation capacity of the aquifer system. The redox chemistry of the site indicates that sulfate‐reducing (H2 ∼ 2 nanomoles [nM]) per liter conditions near the contaminant source grade to Fe(III)‐reducing conditions (H2...
Ground-water resources of the lower-middle Chattahoochee River basin in Georgia and Alabama, and middle Flint River basin in Georgia - Subarea 3 of the Apalachicola-Chattahoochee-Flint and Alabama-Coosa-Tallapoosa River basins
Gregory C. Mayer
1997, Open-File Report 96-483
Drought conditions in the 1980's focused attention on the multiple uses of the surface- and ground-water resources in the Apalachicola-Chattahoochee-Flint (ACF) and Alabama-Coosa-Tallapoosa (ACT) River basins in Georgia, Alabama, and Florida. State and Federal agencies also have proposed projects that would require additional water resources and revise operating practices within...
Hydrogeology of the interstream area between Ty Ty Creek and Ty Ty Creek tributary near Plains, Georgia
Lisa M. Stewart, David W. Hicks
1996, Water-Resources Investigations Report 96-4052
This report is part of an interdisciplinary effort to identify and describe processes that control movement and fate of selected fertilizers and pesticides in the surface and subsurface environments in the Fall Line Hills district of the Georgia Coastal Plain physiographic province. This report describes the hydrogeology of the interstream...
Predicting watershed acidification under alternate rainfall conditions
Thomas G. Huntington
1996, Water, Air, & Soil Pollution (90) 429-450
The effect of alternate rainfall scenarios on acidification of a forested watershed subjected to chronic acidic deposition was assessed using the model of acidification of groundwater in catchments (MAGIC). The model was calibrated at the Panola Mountain Research Watershed, near Atlanta, Georgia, U.S.A. using measured soil properties, wet and dry...
User's guide to revised method-of-characteristics solute-transport model (MOC--version 31)
Leonard F. Konikow, G.E. Granato, G.Z. Hornberger
1994, Water-Resources Investigations Report 94-4115
The U.S. Geological Survey computer model to simulate two-dimensional solute transport and dispersion in ground water (Konikow and Bredehoeft, 1978; Goode and Konikow, 1989) has been modified to improve management of input and output data and to provide progressive run-time information. All opening and closing of files are now done...
Some observations of landslides triggered by the 29 April 1991 Racha earthquake, Republic of Georgia
R.W. Jibson, C.S. Prentice, B.A. Borissoff, E.A. Rogozhin, C.J. Langer
1994, Bulletin of the Seismological Society of America (84) 963-973
On 29 April 1991 an Ms 7.0 earthquake occurred in the Racha region of the Great Caucasus Mountains in north-central Republic of Georgia. The earthquake occurred on a thrust fault striking roughly east-west and dipping about 20° to 45° northward; focal depth was 17 ± 2 km. We observed no...
Geohydrology and evaluation of water-resource potential of the upper Floridan Aquifer in the Albany area, southwestern Georgia
L.J. Torak, G. S. Davis, G.A. Strain, J.G. Herndon
1993, Water Supply Paper 2391
In the Albany area of southwestern Georgia, the Upper Floridan aquifer lies entirely within the Dougherty Plain district of the Coastal Plain physiographic province, and consists of the Ocala Limestone of late Eocene age. The aquifer is divided throughout most of the study area into an upper and a lower...
Geohydrology and evaluation of water-resource potential of the Upper Floridan aquifer in the Albany area, southwestern Georgia
Lynn J. Torak, G. S. Davis, George A. Strain, Jennifer G. Herndon
1991, Open-File Report 91-52
In the Albany area of southwestern Georgia, the Upper Floridan aquifer lies entirely within the Dougherty Plain district of the Coastal Plain physiographic province, and consists of the Ocala Limestone of late Eocene age. The aquifer is divided throughout most of the study area into an upper and a lower...
Ground-water hydraulics, regional flow, and ground-water development of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama
Peter W. Bush, Richard H. Johnston
1988, Professional Paper 1403-C
The Floridan aquifer system is one of the major sources of groundwater supplies in the United States. This productive aquifer system underlies all of Florida, southeast Georgia, and small parts of adjoining Alabama and South Carolina, for a total area of about 100,000 square miles. About 3 billion gallons of...
Preliminary observations of streamflow generation during storms in a forested Piedmont watershed using temperature as a tracer
J. B. Shanley, N.E. Peters
1988, Journal of Contaminant Hydrology (3) 349-365
Variations in streamwater temperature at the outlet of a 41-ha forested watershed at Panola Mountain in the Georgia Piedmont indicate that the initial rapid hydrologic response is caused by a combination of groundwater discharge and channel interception of rainwater. A storm in May 1986 caused a rapid increase in discharge...
Regional ground-water discharge to large streams in the upper coastal plain of South Carolina and parts of North Carolina and Georgia
W. R. Aucott, R.S. Meadows, G. G. Patterson
1987, Water-Resources Investigations Report 86-4332
Base flow was computed to estimate discharge from regional aquifers for six large streams in the upper Coastal Plain of South Carolina and parts of North Carolina and Georgia. Aquifers that sustain the base flow of both large and small streams are stratified into shallow and deep flow systems. Base-flow...
Relations of fresh and salty ground water along the southeastern U. S. Atlantic Coast
R. L. Wait, J.T. Callahan
1965, Groundwater (3) 3-17
Studies of the hydrogeologic environments and the dynamic and equilibrium relations of fresh and salt water in aquifers have been intensified at several places along the southeastern Atlantic Coast. Some salt-water problems involve the coastal water-table aquifer, and others involve parts of the artesian system.On the sandy coastal islands of...
Salt-water encroachment, geology, and ground-water resources of Savannah area, Georgia and South Carolina
H. B. Counts, Ellis Donsky
1963, Water Supply Paper 1611
The Savannah area consists of about 2,300 square miles of the Coastal Plain along the coast of eastern Georgia and southeastern South Carolina. Savannah is near the center of the area. Most of the large ground-water developments are in or near Savannah. About 98 percent of the approximately 60 mgd...