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Page 4613, results 115301 - 115325

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Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington
W. E. Lum II, Gary L. Turney
1984, Open-File Report 82-508
This study provides basic data on ground-water quality throughout the State. It is intended for uses in planning and management by agencies and individuals who have responsibility for or interest in, public health and welfare. It also provides a basis for directing future studies of ground-water quality toward areas where...
Flood-profile analysis, Big Darby Creek at State Route 762, Orient, Ohio
W.P. Bartlett, J. M. Sherwood
1984, Water-Resources Investigations Report 84-4276
The U.S. Geological Survey, in cooperation with the Ohio Department of Transportation, made a hydraulic analysis of the 25- and 100-year floods on Big Darby Creek where State Route 762 crosses the stream at Orient, Ohio. Two proposed bridge plans were analyzed to determine the effects on flood profiles subsequent...
Cost effectiveness of the stream-gaging program in northeastern California
S.H. Hoffard, V.F. Pearce, Gary D. Tasker, W.H. Doyle
1984, Water-Resources Investigations Report 84-4127
Results are documented of a study of the cost effectiveness of the stream-gaging program in northeastern California. Data uses and funding sources were identified for the 127 continuous stream gages currently being operated in the study area. One stream gage was found to have insufficient data use to warrant cooperative...
Geohydrology, aqueous geochemistry, and thermal regime of the Soda Lakes and Upsal Hogback geothermal systems, Churchill County, Nevada
F. H. Olmsted, A. H. Welch, A. S. Van Denburgh, S. E. Ingebritsen
1984, Water-Resources Investigations Report 84-4054
A flow-routing model of the upper Schoharie Creek basin, New York, was developed and used to simulate high flows at the inlet of the Blenheim-Gilboa Reservoir. The flows from Schoharie Creek at Prattsville, the primary source of flow data in the basin, and tributary flows from the six minor basins...
A digital model for streamflow routing by convolution methods
W.H. Doyle Jr., H.O. Shearman, G.J. Stiltner, W.O. Krug
1984, Water-Resources Investigations Report 83-4160
U.S. Geological Survey computer model, CONROUT, for routing streamflow by unit-response convolution flow-routing techniques from an upstream channel location to a downstream channel location has been developed and documented. Calibration and verification of the flow-routing model and subsequent use of the model for simulation is also documented. Three hypothetical examples...
Drought-related impacts on municipal and major self-supplied industrial water withdrawals in Tennessee -- Part A
Frank M. Alexander, Lee A. Keck, Lewis G. Conn, Stanley J. Wentz
1984, Water-Resources Investigations Report 84-4074
A state-wide water use survey was conducted of all public water suppliers and large, self-supplied industries in Tennessee. This report contains a summation of the data received from 463 public-water suppliers and 129 self-supplied water users. Analysis of the study results and findings indicate that many communities in Tennessee do...
Effects of relocating State Route 151 on the flood profiles of Conotton Creek and its tributaries between Bowerston and Scio, Ohio
W.P. Bartlett, B. E. Krejmas, R.I. Mayo, S. W. Wandle
1984, Water-Resources Investigations Report 83-4130
The Ohio Department of Transportation proposes to relocate an 8-mile segment of State Route 151 between Bowerston and Scio, Harrison County, Ohio. About 3.1 miles of this relocated highway will be within the flood plain of Conotton Creek or its tributaries. Water-surface profiles of the 100-year flood along Conotton Creek...
Effects of storm-water runoff on water quality of the Edwards Aquifer near Austin, Texas
Freeman L. Andrews, Terry L. Schertz, Raymond M. Slade Jr., Jack Rawson
1984, Water-Resources Investigations Report 84-4124
Analyses of samples collected from Barton Springs at approximately weekly Intervals and from Barton Creek and five wells in the Austin area during selected storm-runoff periods generally show that recharge during storm runoff resulted in significant temporal and area! variations in the quality of ground water in the recharge zone...