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Page 4727, results 118151 - 118175

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Ground-water flow and water quality in northeastern Union County, Ohio
K. S. Wilson
1987, Water-Resources Investigations Report 87-4083
A study was done by the U.S. Geological Survey, in cooperation with the Village of Richwood, Ohio, to determine directions of ground-water flow, ground-water-level fluctuations, and water quality in the northeastern part of Union County. The topography of the study area generally is featureless, and the land surfaces slopes gently eastward...
Methods for the determination of organic substances in water and fluvial sediments
R.L. Wershaw, M. J. Fishman, R. R. Grabbe, L. E. Lowe, editor(s)
1987, Techniques of Water-Resources Investigations 05-A3
This manual describes analytical methods used by the U.S. Geological Survey to determine organic substances in water, water-suspended-sediment mixtures, and bottom material. Some of the analytical procedures yield determinations for specific com-pounds, whereas others provide a measure of the quantity of groups of compounds present in the sample. Examples of...
Rainfall and runoff quantity and quality characteristics of four urban land-use catchments in Fresno, California, October 1981 to April 1983
R.N. Oltmann, M.V. Shulters
1987, Open-File Report 84-710
Rainfall and runoff quantity and quality were monitored for industrial, single-dwelling residential, multiple-dwelling residential, and commercial land-use catchments in Fresno, California, during 1981-82 and 1982-83 rain seasons. Storm-composite rainfall and discrete runoff samples were analyzed for physical, inorganic, organic, and biological constituents. Atmospheric dry-deposition- and street-surface particulate samples also were...
Selected water-quality data for the Murtaugh Lake area, south-central Idaho, June 1987
D. J. Parliman, H.W. Young
1987, Open-File Report 87-466
This report presents June 1987 water-quality data, principally dissolved chloride and dissolved nitrite plus nitrate (as nitrogen), for water samples from 45 wells in the Murtaugh Lake area, south-central Idaho. Chloride concentrations ranged from 23 to 320 milligrams per liter; the median concentration was 70 milligrams per liter. Nitrogen concentrations...
Selected water-quality data for the Minidoka Irrigation District, south-central Idaho, June 1987
H.W. Young, D. J. Parliman, I. O'Dell
1987, Open-File Report 87-465
This map report presents June 1987 water-quality data, principally dissolved nitrite plus nitrate (as nitrogen), and depth-to-water measurements for 67 wells in the Minidoka Irrigation District, south-central Idaho. Nitrogen concentrations ranged from 0.2 to 76 milligrams per liter; the median concentrations was 6.6 milligrams per liter. Nitrogen concentrations in 9...
Selected water-quality data for the Burley irrigation district, south-central Idaho, March-April, 1987
H.W. Young, D. J. Parliman, M.L. Jones
1987, Open-File Report 87-240
This map report presents selected March-April 1987, water quality data, principally dissolved nitrite plus nitrate as nitrogen, and depth-to-water measurements for 118 wells in the Burley Irrigation District, south-central Idaho. Nitrogen concentrations ranged from 0.37 to 30 mg/L; the median concentration was 8.0 mg/L. Nitrogen concentrations in 19 wells equaled...
Laboratory data on coarse-sediment transport for bedload-sampler calibrations
David Wellington Hubbell, H.H. Stevens Jr., J. V. Skinner, J.P. Beverage
1987, Water Supply Paper 2299
A unique facility capable of recirculating and continuously measuring the transport rates of sediment particles ranging in size from about 1 to 75 millimeters in diameter was designed and used in an extensive program involving the calibration of bedload samplers. The facility consisted of a 9-footwide by 6-foot-deep by 272-foot-long...
Measuring and computing natural ground-water recharge at sites in south-central Kansas
M.A. Sophocleous, C. A. Perry
1987, Water-Resources Investigations Report 87-4097
To measure the natural groundwater recharge process, two sites in south-central Kansas were instrumented with sensors and data microloggers. The atmospheric-boundary layer and the unsaturated and saturated soil zones were monitored as a single regime. Direct observations also were used to evaluate the measurements. Atmospheric sensors included an anemometer, a...