A network for continuous monitoring of water quality in the Sabine River basin, Texas and Louisiana
J.F. Blakey, P.W. Skinner
1973, Open-File Report 73-25
The proposed water-quality network for the Sabine River Basin of Texas and Louisiana consists of nine monitoring stations, a central control station, a slave-central station, and a leased-line telecommunications system. This monitoring network would provide continuous transmission of water-quality data to the office of the water manager. Level I operations at...
Fluvial sediment in Double Creek subwatershed No. 5, Washington County, Oklahoma
Gene A. Bednar, Thomas E. Waldrep
1973, Open-File Report 73-22
Double Creek subwatershed No. 5 in Washington County, Oklahoma, is one of six detention structures within the Double Creek watershed and includes 1,530 acres (2.39 square miles). The subwatershed receives runoff from approximately 5 percent of the total area of the watershed. Most precipitation falling on subwatershed No. 5 does not...
Electrical-analog model study of a hydrologic system in Southeast Florida
Charles A. Appel
1973, Open-File Report 73-9
Roughness coefficients for stream channels in Arizona
B. N. Aldridge, J.M. Garrett
1973, Open-File Report 73-3
When water flows in an open channel, energy is lost through friction along the banks and bed of the channel and through turbulence within the channel. The amount of energy lost is governed by channel roughness, which is expressed in terms of a roughness coefficient. An evaluation of the roughness...
Fluvial sediment characteristics of the Kansas River at Wamego, Kansas, 1957-70
C.D. Albert
1973, Open-File Report 73-2
Fluvial-sediment samples have been collected from the Kansas River at Wamego from 1957-70 by the U.S. Geological Survey in cooperation with the Kansas Water Resources Board. During this period. the stream-runoff pattern of the basin has been altered by constructions of Tuttle Creek and Milford Reservoirs. An analysis of data shows...
Part of the Chryse region, Viking Mars 1975 landing site 3, M 250 k, rectified and scaled photographs
Water Resources Division, U.S. Geological Survey
1973, Open-File Report 73-349
Part of the Aquae Apolinares region, Viking Mars 1975 landing site 10, M 250 k, rectified and scaled photographs
Water Resources Division, U.S. Geological Survey
1973, Open-File Report 73-348
Ground water in Santa Barbara and southern San Luis Obispo counties, California, spring 1969 to spring 1970
J. W. Warner
1973, Open-File Report 72-442
Availability of ground water for public-water supply in central and southern Escambia County, Florida
Henry Trapp Jr.
1973, Open-File Report 72-380
Dewatering of the Clayton Formation during construction of the Walter F. George Lock and Dam, Fort Gaines, Clay County, Georgia
J. W. Stewart
1973, Open-File Report 72-361
Airborne chemical elements in Spanish moss
H.T. Shacklette, J. J. Connor
1973, Professional Paper 574-E
Low-flow characteristics of streams in the Puget Sound region, Washington
F.T. Hidaka
1973, Open-File Report 72-163
Periods of low streamflow are usually the most critical factor in relation to most water uses. The purpose of this report is to present data on low-flow characteristics of streams in the Puget Sound region, Washington, and to briefly explain some of the factors that influence low flow in the...
Floods in Harvard NW Quadrangle, northeastern Illinois
R.S. Grant, M.D. Duerk
1973, Open-File Report 72-136
Ground-water conditions in the lower Withlacoochee River-Cross-Florida Barge Canal complex area
Glen L. Faulkner
1973, Open-File Report 72-115
Susquehanna River at Unadilla, New York, floodflow characteristics at proposed bridge site
Bernard Dunn
1973, Open-File Report 72-96
Salt-water movement in the lower Withlacoochee River-Cross-Florida Barge Canal complex
Peter W. Bush
1973, Open-File Report 72-59
Streamflow, sediment, and turbidity in the Mad River basin, Humboldt and Trinity Counties, California
William M. Brown III
1973, Water-Resources Investigations Report 73-36
The Mad River discharged an average suspended-sediment load of 2,710,000 tons per year during a 13-year period beginning October 1957. Preliminary analysis of data collected during the 1971 water year indicated that about 66 percent of the suspended sediment was derived from sources upstream from a proposed reservoir site on...
Geochemical anomalies of a claypit area, Callaway County, Missouri, and related metabolic imbalance in beef cattle
Richard John Ebens, J. A. Erdman, G. L. Feder, A.A. Case, L.A. Selby
1973, Professional Paper 807
Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California
J. W. Warner, J. A. Moreland
1973, Open-File Report 73-358
This is a study of the feasibility of recharging, in the Waterman Canyon-East Twin Creek area, imported water from northern California by way of the State Water Project beginning in 1972. The feasibility of recharging 30,000 acre-feet of water a year in the Waterman Canyon-East Twin Creek area will depend...
Base of fresh ground water approximately 3,000 micromhos in the Sacramento Valley and Sacramento-San Joaquin Delta, California
Charles F. Berkstresser Jr.
1973, Water-Resources Investigations Report 73-40
The study area consists of about 6,600 square miles; about 5,500 square miles of the floor of the Sacramento Valley, and about 1,100 square miles of the Sacramento-San Joaquin Delta. The Sacramento Valley, as defined by Bryan (1923, p. 8), extends from Red Bluff 145 miles southward to Suisun Bay. ...
Recognition of natural brine by electrical soundings near the Salt Fork of the Brazos River, Kent and Stonewall counties, Texas
Adel A. R. Zohdy, Dallas B. Jackson
1973, Professional Paper 809-A
Salt-water movement in the lower Withlacoochee River-Cross Florida Barge Canal Complex
Peter W. Bush
1973, Water-Resources Investigations Report 5-72
Construction of the west end of the Cross Florida Barge Canal changed the regimen of the lower Withlacoochee River. The investigation was made to determine how salt water from the Gulf of Mexico moves in the river-canal complex, and how the factors that control salt-water movement--tides and discharge--have changed since...
Hydrology of the dunes area north of Coos Bay, Oregon
J. H. Robison
1973, Open-File Report 73-241
Hydrology of a 20-square-mile area of dunes along the central Oregon coast was studied. The area is underlain by 80 to 150 feet of Quaternary dune and marine sand which overlies Tertiary marine clay and shale. Ground water for industrial and municipal use is being withdrawn at a rate of...
Iterative digital model for aquifer evaluation
P.C. Trescott
1973, Open-File Report 73-282
Artificial recharge in the Whitewater River area, Palm Springs, California
S.J. Tyley
1973, Open-File Report 73-289
