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Page 5130, results 128226 - 128250

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Not all publications have extents, not all extents are completely accurate
Progress report on water resources of the Tulalip Indian Reservation, Washington
B. W. Drost
1979, Water-Resources Investigations Report 78-31
Updated information on the Tulalip Indian Reservation 's resources indicates that the newly developed tribal well field yielded about 100 million gallons of water during August 1975-October 1976. At 16 or 17 streamflow sites, mean annual discharges during the 1976 water year exceeded those of the 1975 water year by...
Water resources of the Swinomish Indian Reservation, Washington
B. W. Drost
1979, Water-Resources Investigations Report 79-12
The Swinomish Indian Reservation occupies 17 mi2on Fidalgo Island, northwestern Washington. Six square miles are underlain by mudflats or low-lying alluvial deposits, and are not part of the study area. An appraisal of the water resources of the reservation was made because the Swinomish Tribal Community expects rapid economic and...
Probable hydrologic effects of a hypothetical failure of Mackay Dam on the Big Lost River Valley from Mackay, Idaho to the Idaho National Engineering Laboratory
Leroy Druffel, Gloria J. Stiltner, Thomas N. Keefer
1979, Water-Resources Investigations Report 79-99
Mackay Dam is an irrigation reservoir on the Big Lost River, Idaho, approximately 7.2 kilometers northwest of Mackay, Idaho. Consequences of possible rupture of the dam have long concerned the residents of the river valley. The presence of reactors and of a management complex for nuclear wastes on the reservation...
Hydrogeologic features of the alluvial deposits in the Greybull River valley, Bighorn Basin, Wyoming
M. E. Cooley, W. J. Head
1979, Water-Resources Investigations Report 79-6
The alluvial aquifer along the Greybull River in Wyoming, consists principally of the Greybull terrace doposits and flood-plain alluvium but also includes Burlington terrace deposits east of Burlington, the McKinnie terrace, and the younger, generally undissected alluvial-fan deposits. Well-log data and 18 surface-resistivity measurements at four localities indicate that the...
Determination of selected anions in water by ion chromatography
Marvin J. Fishman, Grace Pyen
1979, Water-Resources Investigations Report 79-101
Ion chromatography is a rapid, sensitive, precise, and accurate method for the determination of major anions in rain water and surface waters. Simultaneous analyses of a single sample for bromide, chloride, fluoride, nitrate, nitrite, orthophosphate, and sulfate require approximately 20 minutes to obtain a chromatogram.Minimum detection limits range from 0.01...
Ground water in the San Juan Basin, New Mexico and Colorado
Forest P. Lyford
1979, Water-Resources Investigations Report 79-73
Principal aquifers in the San Juan Basin of New Mexico and Colorado are the Entrada Sandstone, Westwater Canyon Member of the Morrison Formation, Gallup Sandstone, several sandstones in the Mesaverde Group above the Gallup (Dalton Sandstone, Point Lookout Sandstone, Menefee Formation, Cliffhouse Sandstone), and sandstones of tertiary.Most ground water flows...
Water resources of the Port Madison Indian Reservation, Washington
W. E. Lum II
1979, Water-Resources Investigations Report 78-112
The study summarized in this report was made to provide Suquamish Tribal leaders with information on the reservation's surface- and ground-water resources. The Tribal leaders need this information to help them manage and protect their water resources against overdevelopment. The quantity of ground water that is estimated to be available...
Estimated drawdowns in the Floridan aquifer due to increased withdrawals, Duval County, Florida
Bernard J. Franks, G. G. Phelps
1979, Water-Resources Investigations Report 79-84
Hydrologic investigations of the Floridan aquifer in Duval County, Florida, have shown that an appropriate simplified model of the aquifer system consists of a series of sub aquifers separated by semipermeable beds. Data from more than 20 aquifer tests were reanalyzed by the Hantush modified method, which takes into account...
Hydrology of major estuaries and sounds of North Carolina
G. L. Giese, Hugh B. Wilder, Garald G. Parker Jr.
1979, Water-Resources Investigations Report 79-46
Hydrology-related problems associated with North Carolina's major estuaries and sounds include contamination of some estuaries with municipal and industrial wastes and drainage from adjacent intensively-farmed areas, and nuisance-level algal blooms. In addition, there is excessive shoaling in some navigation channels, saltwater intrusion into usually fresh estuarine reaches, too-high or too-low...
Ground-water quality in the upper Santa Ana River basin, southern California
Lawrence A. Eccles
1979, Water-Resources Investigations Report 79-113
The principal ground-water quality problems in the Santa Ana River basin, as determined from two samplings (1968-69 and 1977-78), are high concentrations of dissolved solids in general and nitrate-nitrogen in particular. The distribution of dissolved solids exceeding 800 milligrams per liter was smaller in area in 1977-78 than in 1968-69....
Experimental salinity alleviation at Malaga Bend of the Pecos River, Eddy County, New Mexico
John S. Havens, D. W. Wilkins
1979, Water-Resources Investigations Report 80-4
Upward-leaking brine, from a confined aquifer at the base of the Rustler Formation, mixes with fresher water in a shallow aquifer, resulting in discharge to the Pecos River in southern Eddy County, New Mexico, of about 0.5 cubic feet per second of saturated brine. Pumping brine from the aquifer at...
Chemical, physical, and radiological quality of selected public water supplies in Florida, November 1977-February 1978
G. A. Irwin, Robert W. Hull
1979, Water-Resources Investigations Report 79-50
Virtually all treated public water supplies sampled in Florida meet the National Interim Primary and Proposed Secondary Drinking Water Regulations. These findings are based on a water-quality reconnaissance of 129 treated public supplies throughout the State during the period November 1977 through February 1978. While primary drinking water regulation exceedences...
Analytical method for dissolved-organic carbon fractionation
Jerry A. Leenheer, Edward W. D. Huffman Jr.
1979, Water-Resources Investigations Report 79-4
A standard procedure for analytical-scale dissolved organic carbon fractionation is presented, whereby dissolved organic carbon in water is first fractionated by a nonionic macroreticular resin into acid, base, and neutral hydrophobic organic solute fractions, and next fractionated by ion-exchange resins into acid, base, and neutral hydrophilic solute fractions. The hydrophobic...
Coastal flood of February 7, 1978, in Maine, Massachusetts, and New Hampshire
Russell A. Gadoury
1979, Water-Resources Investigations Report 79-61
On February 6-8, 1978, New England was battered by one of the most severe winter storms of record. The storm produced record snowfall in many areas of Rhode Island and Massachusetts. Spring high tides (sun and moon in such alinement as to cause the highest tides of the month), a...
Revision of the documentation for a model for calculating effects of liquid waste disposal in deep saline aquifers
Inc. INTERA Environmental Consultants
1979, Water-Resources Investigations Report 79-96
The model developed under this contract is a modified version of the deep well disposal model developed by INTERCOMP Resource Development and Engineering, Inc., for the U.S. Geological Survey (A model for calculating effects of liquid waste disposal in deep saline aquifers). The model is a finite-difference numerical solution of...
Water-table map of Waukesha County, Wisconsin
J. B. Gonthier
1979, Water-Resources Investigations Report 79-43
A map (scale 1:100,000) was prepared of the water table in Waukesha County in southeastern Wisconsin using water levels from more than 1,700 wells. The work was done as part of a cooperative project between the U.S. Geological Survey, the University of Wisconsin-Extension, Geological and Natural History Survey, and the...
Red Cedar River basin, Wisconsin: Low-flow characteristics
W.A. Gebert
1979, Water-Resources Investigations Report 79-29
Low-flow characteristics in the Red Cedar River basin, Wis., where surplus water may be diverted, and methods to determine low-flow characteristics at additional sites are presented. The low-flow characteristics were determined by various methods at 71 sites. For the three gaging stations in the basin, frequency analysis was used to...
Low-flow characteristics of streams in the Lake Superior Basin, Wisconsin
W.A. Gebert
1979, Water-Resources Investigations Report 79-38
Low-flow characteristics of streams in the Lake Superior basin include estimates of low-flow frequency and flow duration at 9 gaging stations, low-flow frequency at 16 low-flow partial-record stations and 38 miscellaneous sites; and a list of base-flow discharge measurement is available. The equations were determined from multiple-regression analyses that relate...
Water resources of shallow aquifers in the Upper Poplar River basin, northeastern Montana
R.D. Feltis
1979, Water-Resources Investigations Report 79-51
The aquifer system studied in the upper Popular River basin in Montana ranges in age from Late Cretaceous to Holocene. Most wells obtain water from the Paleocene Fort Union Formation or younger rocks. The potentiometric surface of the Fort Union and overlying rocks indicates movement of water from the high...
Connector well experiment to recharge the Floridan Aquifer, East Orange County, Florida
P. W. Bush
1979, Water-Resources Investigations Report 78-73
An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer, and cased through the confining layer between the two aquifers, was drilled in east Orange County, Florida, to obtain information on the nature and function of the shallow aquifer as related to...
Annual peak discharges from small drainage areas in Montana for stations discontinued before 1978
R. J. Omang, J. A. Hull, Charles Parrett
1979, Open-File Report 79-510
Annual peak stage and discharge data have been tabulated for crest-stage gage sites in Montana. The crest-stage program was begun in July 1955 to investigate the magnitude and frequency of floods from samll drainage areas. The program has expanded from 45 crest-stage gaging stations initially to 172 stations maintained in...
One-dimensional steady-state stream water-quality model
Daniel P. Bauer, Marshall E. Jennings, Jeffrey E. Miller
1979, Water-Resources Investigations Report 79-45
A computer program, based on a one-dimensional mathematical model which predicts the stream water-quality response characteristics from waste source inputs, is described and documented. Variables predicted include dissolved oxygen, biochemical oxygen demand, nitrogen forms, total and fecal-coliform bacteria, orthophosphate-phosphorus, and various conservative substances. The model is based primarily on the...
Traveltime, unit-concentration, longitudinal-dispersion, and reaeration characteristics of upstream reaches of the Yampa and Little Snake Rivers, Colorado and Wyoming
Daniel P. Bauer, R. E. Rathbun, H. W. Lowham
1979, Water-Resources Investigations Report 78-122
Measurements were made along a 58-mile reach of the Yampa River in Colorado and a 77-mile reach of the Little Snake River in Colorado and Wyoming to determine traveltime, unit-concentration , and longitudinal-dispersion characteristics. Two traveltime, unit-concentration, and dispersion analyses were made along the Yampa River when its average streamflow...
Selected water resources data, Clarion River and Redbank Creek basins, northwestern Pennsylvania: Part 2
Theodore F. Buckwalter, Clifford H. Dodge, George R. Schiner
1979, Water-Resources Investigations Report 79-19
This report presents selected basic data collected during a study of the water resources of the Clarion River and Redbank Creek basins in northwestern Pennsylvania. Hydrologic information including data on aquifers, water levels, and yields is presented for 1,304 wells. Records for 51 springs are also given. The report contains...