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Page 62, results 1526 - 1550

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Hydrologic environments and water-quality characteristics at four landfills in Mecklenburg County, North Carolina, 1980-86
A.P. Cardinell, C.R. Barnes, W.H. Eddins, R. W. Coble
1989, Water-Resources Investigations Report 89-4035
A water-quality study was conducted during 1980-86 at four landfills in Mecklenburg County, North Carolina. Each landfill has a three-layered hydrogeologic system typical of the Piedmont, consisting of (1) the regolith; (2) a transition zone; and (3) unweathered, fractured crystalline bedrock. As much as 7.6 inches per year of rainfall...
Appraisal of ground-water quality in the Bunker Hill Basin of San Bernardino Valley, California
L. F. Duell Jr., R. A. Schroeder
1989, Water-Resources Investigations Report 88-4203
Water samples were collected from 47 wells and analyzed for concentration of major inorganic ions, nitrogen species, and volatile (purgeable) organic priority pollutants to assess groundwater quality in the Bunker Hill basin, California. Data were supplemented with additional analysis of nitrate, tetrachloroethylene, and trichloroethylene made by other agencies. The organic...
Relation between land use and ground-water quality in the upper glacial aquifer in Nassau and Suffolk Counties, Long Island, New York
D. A. Eckhardt, W.J. Flipse Jr., E. T. Oaksford
1989, Water-Resources Investigations Report 86-4142
The chemical quality of groundwater in the upper glacial (water-table) aquifer beneath the 10 types of land-use areas of Nassau and Suffolk Counties, NY was examined to evaluate the effect of human activities on groundwater. The highest median chloride and total dissolved-solids concentrations were found in wells in high-density residential...
Biannual water-resources review, White Sands Missile Range, New Mexico, 1986 and 1987
Robert G. Myers, Steven C. Sharp
1989, Open-File Report 89-49
Hydrologic data were collected at White Sands Missile Range, New Mexico in 1986 and 1987. The total groundwater withdrawal in 1986 was 565,462,500 gal and in 1987 it was 620,492,000 gal. The total groundwater withdrawal was 110,971,300 gal less in 1986 than in 1985, but 55,029,500 gal more in 1987...
Hydrogeologic and chemical data for the O-Field area, Aberdeen Proving Ground, Maryland
P.R. Nemoff, D.A. Vroblesky
1989, Open-File Report 89-238
O-Field, located at the Edgewood area of Aberdeen Proving Ground , Maryland, was periodically used for disposal of munitions, waste chemicals, and chemical-warfare agents from World War II through the 1950' s. This report includes various physical, geologic, chemical, and hydrologic data obtained from well-core, groundwater, surface water, and bottom-sediment...
Compilation of geohydrologic data collected as part of the areal appraisal of ground-water resources near Branson, Missouri
J. L. Imes
1989, Open-File Report 89-401
A rapidly developing retirement community and tourist industry in the Branson, Missouri area has created an increased demand for potable water, especially in the summer months. The rapid pace of residential and business expansion has created concerns regarding the future groundwater availability and quality. Water levels measured in the Ozark...
Quality of water from public-supply wells in principal aquifers of Illinois, 1984-87
David C. Voelker
1989, Water-Resources Investigations Report 88-4111
The quality of water from public-supply wells that tap the principal aquifers in Illinois are summarized. Water quality data collected during the study included inorganic and volatile organic constituents in 2,756 samples and soluble organic constituents in 330 samples from 2,080 public supply wells. Water quality differs among the aquifers...
Ground-water flow and quality near the Upper Great Lakes connecting channels, Michigan
J.L. Gillespie, D.H. Dumouchelle
1989, Water-Resources Investigations Report 88-4232
The Upper Great Lakes connecting channels are the St. Marys, St. Clair and Detroit Rivers, and Lake St. Clair. The effect of ground water on the connecting channels is largely unknown, and the controls on its movement and quality are undefined. Geologic, hydrologic, and environmental conditions near the channels have...
Relation of ground-water quality to land use in the Philadelphia, Pennsylvania-Camden, New Jersey area
Ray S. Blickwedel, C. R. Wood
1989, Water-Resources Investigations Report 88-4211
The distributions of common dissolved constituents, trace metals, and volatile organic compounds in ground water near Philadelphia, Pennsylvania, and Camden, New Jersey, are influenced by local geology and land use. Many common dissolved constituents are more concentrated in ground water beneath urban and industrial areas than in water beneath suburban...
Inorganic and organic ground-water chemistry in the Canal Creek area of Aberdeen Proving Ground, Maryland
M.M. Lorah, D.A. Vroblesky
1989, Water-Resources Investigations Report 89-4022
Groundwater chemical data were collected from November 1986 through April 1987 in the first phase of a 5-year study to assess the possibility of groundwater contamination in the Canal Creek area of Aberdeen Proving Ground, Maryland. Water samples were collected from 87 observation wells screened in Coastal Plain sediments; 59...
Water quality in Reedy Fork and Buffalo Creek basins in the Greensboro area, North Carolina, 1986-87
M.S. Davenport
1989, Water-Resources Investigations Report 88-4210
Water and bottom-sediment samples were collected from April 1986 through September 1987 at 19 sites in Guilford County and the City of Greensboro, North Carolina. Sampling locations included 13 stream sites, two lakes that supply the City of Greensboro with drinking water, two City of Greensboro finished drinking-water filtration plants,...
Screening of ground water samples for volatile organic compounds using a portable gas chromatograph
Robert C. Buchmiller
1989, Ground Water Monitoring Review (9) 126-130
A portable gas chromatograph was used to screen 32 ground water samples for volatile organic compounds. Seven screened samples were positive; four of the seven samples had volatile organic substances identified by second-column confirmation. Four of the seven positive, screened samples also tested positive in laboratory analyses of duplicate samples....
Origin and age of the Lake Nyos maar, Cameroon
J. P. Lockwood, M. Rubin
1989, Journal of Volcanology and Geothermal Research (39) 117-124
Lake Nyos occupies a young maar crater in the Precambrian granitic terrane of northwest Cameroon. The lake is partly surrounded by poorly consolidated, ultramafic nodule-bearing pyroclastic surge deposits that were explosively ejected from the Nyos crater at the time of its formation. Radiocarbon dates show that the maar probably formed...
Ground-water contamination at an inactive coal and oil gasification plant site, Gas Works Park, Seattle, Washington
G. L. Turney, D.F. Goerlitz
1989, Water-Resources Investigations Report 88-4224
Gas Works Park, in Seattle, Washington, is located on the site of a coal and oil gasification plant that ceased operation in 1956. During operation, many types of wastes, including coal, tar, and oil, accumulated on site. The park soil is presently (1986) contaminated with compounds such as polynuclear aromatic...
Preservation of samples for dissolved mercury
S. N. Hamlin
1989, Water Resources Bulletin (25) 255-262
Water samples for dissolved mercury requires special treatment because of the high chemical mobility and volatility of this element. Widespread use of mercury and its compounds has provided many avenues for contamination of water. Two laboratory tests were done to determine the relative permeabilities of glass and plastic sample bottles...
Distribution and bioaccumulation of selenium in aquatic microcosms
John M. Besser, James N. Huckins, Edward E. Little, Thomas W. La Point
1989, Environmental Pollution (62) 1-12
Closed-system microcosms were used to study factors affecting the fate of selenium (Se) in aquatic systems. Distribution and bioaccumulation of Se varied among sediment types and Se species. A mixture of dissolved 75Se species (selenate, selenite and selenomethionine) was sorbed more rapidly to fine-textured, highly organic pond sediments than to...
Selected ground-water data, Chester County, Pennsylvania
Ronald A. Sloto
1989, Open-File Report 87-217
Hydrologic data for Chester County, Pennsylvania are given for 3,010 wells and 32 springs. Water levels are given for 48 observation wells measured monthly during 1936-86. Chemical analyses of ground water are given for major ions, physical properties, nutrients, metals and other trace constituents, volatile organic compounds, acid organic compounds,...
Origin and transport of chloride in superheated geothermal steam
A.H. Truesdell, J.R. Haizlip, H. Armannsson, F. D’Amore
1989, Geothermics (18) 295-304
Hydrogen chloride (HCl) is a known component of some volcanic gases and volcanic-related hydrothermal systems. It has recently been discovered in superheated steam in exploited geothermal systems, usually as a result of HCl-induced corrosion of well casing and steam gathering systems....
Chemistry and origin of minor and trace elements in vitrinite concentrates from a rank series from the eastern United States, England, and Australia
P.C. Lyons, C.A. Palmer, N. H. Bostick, J.D. Fletcher, F.T. Dulong, F. W. Brown, Z. A. Brown, M.R. Krasnow, L.A. Romankiw
1989, International Journal of Coal Geology (13) 481-527
A rank series consisting of twelve vitrinite concentrates and companion whole-coal samples from mined coal beds in the eastern United States, England, and Australia were analyzed for C, H, N, O, ash, and 47 trace and minor elements by standard elemental,...
Preliminary evaluations of regional ground-water quality in relation to land use
D. Cain, D.R. Helsel, S.E. Ragone
1989, Ground Water (27) 230-244
Preliminary results from New York, New Jersey, Connecticut, Florida, Nebraska, and Colorado indicate that regional ground-water quality has been affected by human activities. The frequencies of detection of volatile organic compounds and some trace elements were larger in ground water underlying urban or industrial areas in comparison to undeveloped areas....