Publications
Publications from USGS science centers throughout the Southeast Region.
Filter Total Items: 10364
National water summary 1983: Hydrologic events and issues National water summary 1983: Hydrologic events and issues
The United States as a Nation possesses abundant water resources and has developed and used those resources extensively. The national renewable supply of water is about 1,400 billion gallons per day (for the conterminous 48 States). Approximately 380 billion gallons per day of freshwater is withdrawn for use by the Nation's homes, farms, and industries, and about 280 billion gallons per...
Authors
Water Resources Division U.S. Geological Survey
Ground-water data for Georgia, 1983 Ground-water data for Georgia, 1983
Continuous water-level records from 134 wells and more than 700 water-level measurements made in Georgia during 1983 provide the basic data for this report. Selected wells illustrate the effects that changes in recharge and pumping have had on the various ground-water resources in the State. Daily mean water levels are shown in hydrographs for 1983. Monthly means are shown for the 10...
Authors
J.S. Clarke, M.F. Peck, S.A. Longsworth, K.W. McFadden
Adaptive variation in offspring size in the terrestrial isopod, Armadillidium vulgare Adaptive variation in offspring size in the terrestrial isopod, Armadillidium vulgare
Variation in the birth size of offspring of the terrestrial isopod, Armadillidium vulgare, was observed in laboratory experiments and in field populations. In the laboratory, larger offspring were produced when the mother's food supply was reduced. In field populations, larger offspring were produced during the summer, a period of reduced food availability. Smaller offspring are produced...
Authors
M.S. Brody, L.R. Lawlor
Geohydrology of the Edwards Aquifer in the Austin area, Texas Geohydrology of the Edwards Aquifer in the Austin area, Texas
No abstract available.
Authors
E. T. Baker, R.M. Slade, M.E. Dorsey, L.M. Ruiz, G.L. Duffin
Water resources data for Texas, water year 1983, volume 3. Colorado River, Lavaca River, Guadalupe River, Nueces River, Rio Grande basins, and intervening coastal basins Water resources data for Texas, water year 1983, volume 3. Colorado River, Lavaca River, Guadalupe River, Nueces River, Rio Grande basins, and intervening coastal basins
No abstract available.
Authors
Water Resources Division U.S. Geological Survey
Quality of water recovered from a municipal effluent injection well in the Floridan aquifer system, Pompano Beach, Florida Quality of water recovered from a municipal effluent injection well in the Floridan aquifer system, Pompano Beach, Florida
Approximately 69 million gallons of backflow from an injection well used for the disposal of secondary treated municipal effluent in the Floridan aquifer system near Pompano Beach, Florida, was periodically sampled for inorganic quality from March 1975 through March 1977. Analyses of the backflow effluent showed a concomitant increase in dissolved solids and a change in ionic composition...
Authors
D.J. McKenzie, G. A. Irwin
Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-84 and 1983-84, and measured compaction, 1973-84, in the Houston-Galveston region, Texas Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-84 and 1983-84, and measured compaction, 1973-84, in the Houston-Galveston region, Texas
This report, which was prepared in cooperation with the City of Houston and Harris-Galveston Coastal Subsidence District, presents data on water-level changes during 1977-84 and 1983-84 in the Chicot and Evangeline aquifers (figs. 1-4) and data on measured compaction 1973-84 (fig. 5). Water levels in about 550 wells were used to construct the maps showing water-level changes. Compaction...
Authors
Jeffrey L. Strause
Preliminary study of the aquifers of the lower Mesilla Valley in Texas and New Mexico by model simulation Preliminary study of the aquifers of the lower Mesilla Valley in Texas and New Mexico by model simulation
The aquifers in the lower Mesilla Valley of Texas and New Mexico provide water for irrigation, industrial use, and municipal supply. At present (1984), the shallow aquifer is used principally for irrigation. The medium-depth aquifer (the top of which is about 160 to 260 feet below land surface) and deep aquifer (about 460 to 680 feet below land surface) are used almost exclusively by the...
Authors
J. S. Gates, D. E. White, E. R. Leggat
Mapping of forested wetland: Use of seasat radar images to complement conventional sources Mapping of forested wetland: Use of seasat radar images to complement conventional sources
Distinguishing forested wetland from dry forest using aerial photographs has been handicapped because photographs often do not reveal the presence of water below the tree canopies. Images obtained during the summer months of 1978 by the Seasat satellite's L-band (23-cm) radar reveal forested wetland as patterns of high radar reflection in the Atlantic coastal plain between Maryland and...
Authors
John L. Place
Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Texas Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Texas
This report on ground-water levels, springs, and depth to ground water in the Basin and Range province of Texas (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger...
Authors
B. T. Brady, M. S. Bedinger, D. A. Mulvihill, John Mikels, W. H. Langer
General description of the hydrology and burial trenches at the low-level radioactive waste burial facility near Barnwell, South Carolina General description of the hydrology and burial trenches at the low-level radioactive waste burial facility near Barnwell, South Carolina
The Barnwell low-level radioactive solid waste burial site is located in Barnwell County, South Carolina, 5 miles west of the city of Barnwell. Approximately 1,050 feet of stratified gravel, sand, silt, clay, and limestone, ranging in age from Late Cretaceous to Holocene, underlie the burial site. Ground water within the study area occurs under water table, semi-confined, and artesian...
Authors
B.B. McDonald
Water-Level Measurements for the Coastal Plain Aquifers of South Carolina Prior to Development Water-Level Measurements for the Coastal Plain Aquifers of South Carolina Prior to Development
Tabulations of water-level measurements for the Coastal Plain aquifers of South Carolina representing water levels prior to man-made development are presented. Included with the tabulations are local well number, location, land-surface altitude, well depth, screened interval, depth to water, water- level altitude, and date measured. These water-level measurements were used in compiling
Authors
Walter R. Aucott, Gary K. Speiran