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Page 1293, results 32301 - 32325

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Laboratory and quality assurance protocols for the analysis of herbicides in ground water from the Management Systems Evaluation Area, Princeton, Minnesota
S.J. Larson, P. D. Capel, A.G. VanderLoop
1996, Water-Resources Investigations Report 95-4178
Laboratory and quality assurance procedures for the analysis of ground-water samples for herbicides at the Management Systems Evaluation Area near Princeton, Minnesota are described. The target herbicides include atrazine, de-ethylatrazine, de-isopropylatrazine, metribuzin, alachlor, 2,6-diethylaniline, and metolachlor. The analytical techniques used are solid-phase extraction, and analysis by gas chromatography with mass-selective...
Mass balance, meteorological, ice motion, surface altitude, and runoff data at Gulkana Glacier, Alaska, 1992 balance year
R.S. March, D.C. Trabant
1996, Water-Resources Investigations Report 95-4277
The 1992 measured winter snow, maximum winter snow, net, and annual balances in the Gulkana Glacier basin were evaluated on the basis of meteorological, hydrological, and glaciological data measured in the basin and are reported herein. Averaged over the glacier, the measured winter snow balance was 0.97 meters on March...
Technique for estimating magnitude and frequency of peak flows in Maryland
Jonathan J.A. Dillow
1996, Water-Resources Investigations Report 95-4154
Methods are presented for estimating peak-flow magnitudes of selected frequencies for drainage basins in Maryland. The methods were developed by generalized least-squares regression techniques using data from 219 streamflow-gaging stations in and near Maryland, and apply to peak flows with recurrence intervals of 2, 5, 10, 25, 50, 100, and...
Technique for estimating magnitude and frequency of peak flows in Delaware
J.J. Dillow
1996, Water-Resources Investigations Report 95-4153
Methods are presented for estimating peak-flow magnitudes of selected frequencies for drainage basins in Delaware. The methods were developed by generalized least-squares regression techniques using data from 74 streamflow-gaging stations in and near Delaware, and apply to peak flows with recurrence intervals of 2, 5, 10, 25, 50, 100, and...
Simulation of water available for runoff in clearcut forest openings during rain-on-snow events in the western Cascade Range of Oregon and Washington
Marijke van Heeswijk, J.S. Kimball, Danny Marks
1996, Water-Resources Investigations Report 95-4219
Rain-on-snow events are common on mountain slopes within the transient-snow zone of the Pacific Northwest. These events make more water available for runoff than does precipitation alone by melting the snowpack and by adding a small amount of condensate to the snowpack. In forest openings (such as those resulting from...
Infiltration of wastewater effluent in the Santa Cruz River Channel, Pima County, Arizona
Ken Galyean
1996, Water-Resources Investigations Report 96-4021
Infiltration of effluent into the Santa Cruz River channel from water-treatment plants near Tucson, Arizona was studied from March 23, 1990, to September 30, 1993. The study reach extended along a 23-mile stream reach from the water-treatment plants, about 5 miles northwest of central Tucson, downstream to Trico Road, about...
Sediment transport, particle size, and loads in North Fish Creek in Bayfield County, Wisconsin, water years 1990-91
W. J. Rose, D.J. Graczyk
1996, Water-Resources Investigations Report 95-4222
North Fish Creek is underused as a trout and salmon hatchery despite its excellent water quality. The shifting-sand streambed in the lower 9 miles of the stream inhibits successful spawning and is a poor habitat for macroinvertebrates, the primary food for juvenile trout and salmon. To provide data necessary for...
Age of ground water in basalt aquifers near Spring Creek National Fish Hatchery, Skamania County, Washington
Stephen R. Hinkle
1996, Water-Resources Investigations Report 95-4272
Water samples from four springs and five wells in basalt aquifers near Spring Creek National Fish Hatchery in Skamania County, Washington, were collected and analyzed for selected inorganic ions and stable isotopes. Eight samples were analyzed for carbon-14 (14C), carbon-13 ([3C), and either chlorofluorocarbons (CFCs) or tritium. This work was...
Geochemical and isotopic composition of ground water with emphasis on sources of sulfate in the upper Floridan Aquifer in parts of Marion, Sumter, and Citrus counties, Florida
Laura A. Sacks
1996, Water-Resources Investigations Report 95-4251
In inland areas of northwest central Florida, sulfate concentrations in the Upper Floridan aquifer are extremely variable and sometimes exceed drinking water standards (250 milligrams per liter). This is unusual because the aquifer is unconfined and near the surface, allowing for active recharge. The sources of sulfate and geochemical processes...
Physical and chemical characteristics of Lake Powell at the forebay and outflows of Glen Canyon Dam, northeastern Arizona, 1990-91
R. J. Hart, K.M. Sherman
1996, Water-Resources Investigations Report 96-4016
The physical and chemical characteristics of Lake Powell have a direct effect on the quality of water below Glen Canyon Dam. Understanding the physical and chemical characteristics of the lake and outflows from the dam is essential in order to effectively manage the operation of the dam. During August 1990...
Simulation of subsurface storage and recovery of treated effluent injected in a saline aquifer, St. Petersburg, Florida
D. K. Yobbi
1996, Water-Resources Investigations Report 95-4271
The potential for subsurface storage and recovery of treated effluent into the uppermost producing zone (zone A) of the Upper Floridan aquifer in St. Petersburg, Florida, is being studied by the U.S. Geological Survey, in cooperation with the city of St. Petersburg and the Southwest Florida Water Management District. A...
Hydrogeology and simulation of ground-water flow at the South Well Field, Columbus, Ohio
W. L. Cunningham, E. Scott Bair, W.P. Yost
1996, Water-Resources Investigations Report 95-4279
The City of Columbus, Ohio, operates four radial collector wells in southern Franklin County. The 'South Well Field' is completed in permeable outwash and ice-contact deposits, upon which flow the Scioto River and Big Walnut Creek. The wells are designed to yield approximately 42 million gallons per day; part of...
Calculated hydrographs for unsteady research flows at selected sites along the Colorado River downstream from Glen Canyon Dam, Arizona, 1990 and 1991
Eleanor R. Griffin, Stephen M. Wiele
1996, Water-Resources Investigations Report 95-4266
A one-dimensional model of unsteady discharge waves was applied to research flowr that were released from Glen Canyon Dam in support of the Glen Canyon Environmental Studies. These research flows extended over periods of 11 days during which the discharge followed specific, regular patterns repeated on a daily cycle that...
Relation between selected water-quality variables and lake level in Upper Klamath and Agency Lakes, Oregon
Tamara M. Wood, Gregory J. Fuhrer, Jennifer L. Morace
1996, Water-Resources Investigations Report 96-4079
Upper Klamath Lake is a large (140 square-mile), shallow (mean depth about 8 ft) lake in south-central Oregon that the historical record indicates has been eutrophic since its discovery by non-Native Americans. In recent decades, however, the lake has had annual occurrences of near- monoculture blooms of the blue-green alga...
Effects of increased urbanization from 1970's to 1990's on storm-runoff characteristics in Perris Valley, California
J. R. Guay
1996, Water-Resources Investigations Report 95-4273
Urban areas in Perris Valley, California, have more than tripled during the last 20 years. To quantify the effects of increased urbanization on storm runoff volumes and peak discharges, rainfall-runoff models of the basin were developed to simulate runoff for 1970-75 and 1990-93 conditions. Hourly rainfall data for 1949-93 were...
Synthesis of natural flows at selected sites in the upper Missouri River basin, Montana, 1928-89
L. E. Cary, Charles Parrett
1996, Water-Resources Investigations Report 95-4261
Natural monthly streamflows were synthesized for the years 1928-89 for 43 sites in the upper Missouri River Basin upstream from Fort Peck Lake in Montana. The sites are represented as nodes in a streamflow accounting model being developed by the Bureau of Reclamation. Recorded and historical flows at most sites...
Discharge, water-quality characteristics, and nutrient loads from McKay Bay, Delaney Creek, and East Bay, Tampa, Florida, 1991-1993
Y.E. Stoker, V.A. Levesque, E.M. Fritz
1996, Water-Resources Investigations Report 95-4167
Nutrient enrichment in Tampa Bay has caused a decline in water quality in the estuary. Efforts to reduce the nutrient loading to Tampa Bay have resulted in improvement in water quality from 1981 to 1991. However, Tampa Bay still is onsidered enriched with nutrients. Water quality in East Bay (located...
Hydrogeology of the Quitobaquito Springs and La Abra Plain area, Organ Pipe Cactus National Monument, Arizona, and Sonora, Mexico
R. L. Carruth
1996, Water-Resources Investigations Report 95-4295
Quitobaquito Springs, in Organ Pipe Cactus National Monument near the south end of the northwestward-trending Quitobaquito Hills, are less than 0.25 mile north of the international boundary between the United States and Mexico. The National Park Service is concerned that the natural flow from Quitobaquito Springs might be reduced by...
The effect of discharge and water quality of the Alafia River, Hillsborough River, and the Tampa Bypass Canal on nutrient loading to Hillsborough Bay, Florida
Y.E. Stoker, V.A. Levesque, W. M. Woodham
1996, Water-Resources Investigations Report 95-4107
Techniques to measure discharge and nutrient loads in the tidally affected portions of two major rivers tributary to Tampa Bay, the Alafia River and the Hillsborough River, were developed and tested. Discharge, water quality, and total phosphorus and total nitrogen loads for the period April 1, 1991, through March 31,...
Evaluation of selected information on splitting devices for water samples
P. D. Capel, S.J. Larson
1996, Water-Resources Investigations Report 95-4141
Four devices for splitting water samples into representative aliquots are used by the U.S. Geological Survey's Water Resources Division. A thorough evaluation of these devices (14-liter churn, 8-liter churn, plastic cone, and Teflon cone) encompasses a wide variety of concerns, based on both chemical and physical considerations. This report surveys...
Trend analysis of selected water-quality data associated with salinity-control projects in the Grand Valley, in the lower Gunnison River basin, and at Meeker Dome, western Colorado
D. L. Butler
1996, Water-Resources Investigations Report 95-4274
To decrease salt loading to the Colorado River from irrigated agriculture, salinity-control projects have been under construction since 1979 by the Bureau of Reclamation and the U.S. Department of Agriculture in the Grand Valley and since 1988 in the lower Gunnison River Basin of western Colorado. In 1980, a salinity-control...
Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Selected metals, arsenic, and phosphorus in streambed sediments of first- and second-order streams, 1987
D. Q. Tanner, J. L. Ryder
1996, Water-Resources Investigations Report 94-4196
The occurrence and geographic distribution of major metals and trace elements was assessed in the lower Kansas River Basin of Kansas and Nebraska by studying the concentrations of metals and nonmetallic elements in the less-than 63-micrometer-sized fraction of streambedsediment samples from 422 sites on first- and second-order streams. Median concentrations...
Hydrogeology and simulation of ground-water flow in the alluvial aquifer at Louisville, Kentucky
M. A. Lyverse, J.J. Starn, M.D. Unthank
1996, Water-Resources Investigations Report 91-4035
The alluvial aquifer at Louisville, Ky., lies in a valley eroded by glacial meltwater that was later partly filled with outwash sand and gravel deposits. The aquifer is primarily unconfined, and the direction of flow is from the adjacent limestone and shale valley wall toward the Ohio River and major...
Trends in chloride, dissolved-solids, and nitrate concentrations in ground water, Carson Valley and Topaz Lake Areas, Douglas County, Nevada, 1959-88
C. E. Thodal
1996, Water-Resources Investigations Report 95-4254
Rapid population growth in Douglas County, an area of approximately 750 square miles in west-central Nevada, has led to concern about the present and future effects of development on ground water. This report describes the results of two nonparametric statistical procedures applied to detect trends in concentrations of chloride, dissolved...