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Page 4429, results 110701 - 110725

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Not all publications have extents, not all extents are completely accurate
Quantity and quality of storm runoff from three urban catchments in Bellevue, Washington
E. A. Prych, J.C. Ebbert
1986, Water-Resources Investigations Report 86-4000
Data on the quantity and quality of urban runoff were collected, analyzed, and used to evaluate the effects of street sweeping and of stormwater detention on quality of runoff. The data included rainfall, runoff discharge, concentrations of selected constituents in discrete samples of runoff, and chemical characteristics of wet- and...
Verification of regression equations for estimating flood magnitudes for selected frequencies on small natural streams in Georgia
McGlone Price, Glen W. Hess
1986, Water-Resources Investigations Report 86-4337
In 1976 the U.S. Geological Survey, in cooperation with the Georgia Department of Transportation, began a program to monitor small natural streams in Georgia to verify the accuracy of the flood frequency estimating equations for the five flood frequency regions that were published in a previous study. Data collection consisted...
Results of exploratory drilling for water in Waihanau Valley, Molokai, Hawaii
K. J. Takasaki
1986, Water-Resources Investigations Report 85-4332
Three exploratory wells, located in lower Waihanau Valley on Molokai, were drilled and tested for their yields during the period May to October 1983. The first well, 582 ft deep, tapped the main water body in a basaltic aquifer intruded by scattered near-parallel volcanic dikes. Water in this water body...
Traveltime and dispersion in the Shenandoah River and its tributaries, Waynesboro, Virginia, to Harpers Ferry, West Virginia
K.R. Taylor, R.W. James, B.M. Helinsky
1986, Water-Resources Investigations Report 86-4065
Two traveltime and dispersion measurements using rhodamin dye were conducted on a 178-mile reach of the Shenandoah River between Waynesboro, Virginia, and Harpers Ferry, West Virginia. The flows during the two measurements were at approximately the 85% and 45% flow durations. The two sets of data were used to develop...
Simulation of mine drainage for preliminary development of oil shale and associated minerals, Piceance basin, northwestern Colorado
O. James Taylor
1986, Water-Resources Investigations Report 86-4011
The Piceance basin of northwestern Colorado contains large resources of oil shale, nahcolite, and dawsonite. Development of these minerals will require drainage of water from mines. A six-layer hydrologic model of the basin was prepared to simulate mine drainage for mineral development. Streams and major tributaries were simulated as head-dependent...
Selected drill-stem test data for the Upper Colorado River basin
R.W. Teller, D. T. Chafin
1986, Water-Resources Investigations Report 84-4146
Permeability data from aquifers and confining layers may be available from drill-stem tests made during the course of petroleum exploration. During the drill-stem test, the stratigraphic interval of interest is isolated in the hole by the use of packers attached to the drill string. Fluid flows into the drilling pipe...
The relation of ground-water quality to housing density, Cape Cod, Massachusetts
J.H. Persky
1986, Water-Resources Investigations Report 86-4093
Correlation of median nitrate concentration in groundwater with housing density for 18 sample areas on Cape Cod yields a Pearson correlation coefficient of 0.802, which is significant at the 95 % confidence level. In five of nine sample areas where housing density is greater than one unit/acre, nitrate concentrations exceed...
Direction of ground-water flow and ground-water quality near a landfill in Falmouth, Massachusetts
J.H. Persky
1986, Water-Resources Investigations Report 85-4188
A landfill in Falmouth, Massachusetts, is upgradient of a pond used for municipal water supply, but analysis of groundwater flow directions and groundwater quality indicates that leachate from the landfill does not threaten the municipal water supply. A network of water table observation wells was established, and water table altitudes...
Potential for updip movement of salinewater in the Edwards Aquifer, San Antonio, Texas
Roberto Perez
1986, Water-Resources Investigations Report 86-4032
The salinity front, locally known as the "bad-water" line, in the Edwards aquifer separates the freshwater from the salinewater and occurs where the aquifer is confined. The concentration of dissolved solids of the salinewater at the salinity front is 1,000 milligrams per liter. The concentration of dissolved solids in water...
Simulation analysis of water-level changes in the Navajo sandstone due to changes in the altitude of Lake Powell near Wahweap Bay, Utah and Arizona
B. E. Thomas
1986, Water-Resources Investigations Report 85-4207
A two-dimensional, finite difference, digital computer model was used to simulate various concepts of groundwater flow near Wahweap Bay, Lake Powell. The filling of Lake Powell started in March 1963; and by 1983 the lake had risen almost 550 ft. This resulted in a maximum observed water level rise of...
Organic compounds in ground water near a sanitary landfill in the Town of Brookhaven, Long Island, New York
K.A. Pearsall, E. J. Wexler
1986, Water-Resources Investigations Report 85-4218
Landfill leachate and groundwater near the Brookhaven landfill site were analyzed for volatile, acid-extractable, and base/neutral-extractable organic compounds classified by EPA as ' priority pollutants, ' and for dissolved organic carbon (DOC) and inorganic constituents. Thirteen priority pollutants were detected, including benzene, chlorobenzene, ethyl benzene, and naphthalene. The most commonly...
Natural flow and water consumption in the Milk River basin, Montana and Alberta, Canada
R.E. Thompson
1986, Water-Resources Investigations Report 86-4006
A study was conducted to determine the differences between natural and nonnatural Milk River streamflow, to delineate and quantify the types and effects of water consumption on streamflow, and to refine the current computation procedure into one which computes and apportions natural flow. Water consumption consists principally of irrigated agriculture,...
Effects of surface coal mining on suspended-sediment discharge in a small mountain watershed, Fayette County, Pennsylvania
T.M. Mastrilli, D.E. Stump
1986, Water-Resources Investigations Report 85-4093
Data collected in the upper Stony Fork basin from July 1980 to November 1981 indicate that logging operations associated with block-cut surface mining temporarily increased suspended-sediment discharge of Stony Fork. However, the strip-mining operation did not increase the suspended sediment discharges of Stony Fork because of effective sediment-control measures. These...
Temperature of ground water at Philadelphia, Pennsylvania, 1979- 1981
Gary N. Paulachok
1986, Water-Resources Investigations Report 84-4189
Anthropogenic heat production has undoubtedly caused increased ground-water temperatures in many parts of Philadelphia, Pennsylvania, as shown by temperatures of 98 samples and logs of 40 wells measured during 1979-81. Most sample temperatures were higher than 12.6 degrees Celsius (the local mean annual air temperature), and many logs depict cooling...
Retention time and flow patterns in Lake Moultrie, South Carolina
G. G. Patterson, R.M. Harvey
1986, Water-Resources Investigations Report 85-4121
A liquid dye tracer was injected into the inflow to Lake Moultrie, South Carolina, during high-flow conditions and again during low-flow conditions. Tracer concentrations were monitored at a network of fixed sampling stations in the lake to determine dispersion and transport characteristics in and through the lake. Wind-generated currents were...
Simulation of rain floods on Willow Creek, Valley County, Montana
Charles Parrett
1986, Water-Resources Investigations Report 86-4341
The Hydrologic Engineering Center-1 rainfall-runoff simulation model was used to assess the effects of a system of reservoirs and waterspreaders in the 550-sq mi Willow Creek Basin in northeastern Montana. For simulation purposes, the basin was subdivided into 100 subbasins containing 84 reservoirs and 14 waterspreaders. Precipitation input to the...
Suspended sediment in Minnesota streams
L. H. Tornes
1986, Water-Resources Investigations Report 85-4312
Suspended-sediment samples have been collected by the U.S. Geological Survey from 115 sites on Minnesota streams since October 1960. Data from 42 sites were sufficient for characterizing sediment concentrations and yields. Average concentrations ranged from 4.4 milligrams per liter on the Baptism River in northeastern Minnesota to 190 milligrams per...
Estimated monthly percentile discharges at ungaged sites in the upper Yellowstone River Basin in Montana
Charles Parrett, J. A. Hull
1986, Water-Resources Investigations Report 86-4009
Once-monthly streamflow measurements were used to estimate selected percentile discharges on flow-duration curves of monthly mean discharge for 40 ungaged stream sites in the upper Yellowstone River basin in Montana. The estimation technique was a modification of the concurrent-discharge method previously described and used by H.C. Riggs to estimate annual...
Quality of ground water in the Payette River basin, Idaho
D. J. Parliman
1986, Water-Resources Investigations Report 86-4013
As part of a study to obtain groundwater quality data in areas of Idaho were land- and water-resource development is expected to increase, water quality, geologic, and hydrologic data were collected for 74 wells in the Payette River basin, west-central Idaho, from July to October 1982. Historical (pre-1982) data from...
Three-dimensional steady-state simulation of flow in the sand-and-gravel aquifer, southern Escambia County, Florida
Henry Trapp, L.H. Geiger
1986, Water-Resources Investigations Report 85-4278
The sand-and-gravel aquifer is the only freshwater aquifer in southern Escambia County, Florida and is the source of public water supply for the area, including the City of Pensacola. The aquifer was simulated by a two-layer, digital model to provide hydrologic information for water resource planning. The lower layer represents...
Geophysical well-log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada
Frederick L. Paillet, A.E. Hess
1986, Water-Resources Investigations Report 86-4052
Various conventional geophysical borehole measurements were made in conjunction with measurements using a recently designed, low-frequency, acoustic-waveform probe and slow velocity flowmeter for characterization of a fractured mafic intrusion in southern Ontario, Canada. Conventional geophysical measurements included temperature, caliper, gamma, acoustic, single-point resistance, and acoustic televiewer logs. Hole stability problems...