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Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri
Wayne R. Berkas
1982, Water-Resources Investigations Report 82-26
A network of water-quality-monitoring stations was established upstream and downstream from the Southwest Wastewater-Treatment Plant on Wilsons Creek to monitor the effects of sewage effluent on water quality. Data indicate that 82 percent of the time the flow in Wilsons Creek upstream from the wastewater-treatment plant is less than the...
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 1982
John B. Townshend, J.E. Papp, E.A. Sauter, L.Y. Torrence, T.K. Cunningham
1982, Open-File Report 82-300-I
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory;...
Water-level maps of the alluvial aquifer, northwestern Mississippi, September 1981
Daphne Darden
1982, Open-File Report 82-574
The study area, locally known as "the Delta", covers the Mississippi River Alluvial Plain in northwestern Mississippi. The Delta is a nearly flat southward sloping surface characterized by oxbow lakes, abandoned stram channels, natural levees, backswamp areas, and bayous.The accompanying maps were prepared to show the effects of ground-water withdrawal...
Chemical and isotopic composition of water from thermal springs and mineral springs of Washington
Robert H. Mariner, T. S. Presser, William C. Evans
1982, Open-File Report 82-98
Water from thermal springs of Washington range in chemical composition from dilute NaHC03, to moderately saline C02-charged NaHC03-Cl waters. St. Martin 's Hot Spring which discharges a slightly saline NaCl water, is the notable exception. Mineral springs generally discharge a moderately saline C02-charged NaHC03-Cl water. The dilute Na-HC03 waters are...
Laboratory investigations of the physics of steam flow in a porous medium
W.N. Herkelrath, A.F. Moench
1982, Open-File Report 82-95
Experiments were carried out in the laboratory to test a theory of transient flow of pure steam in a uniform porous medium. This theory is used extensively in modeling pressure-transient behavior in vapor-dominated geothermal systems. Transient, superheated steam-flow experiments were run by bringing a cylinder of porous material to a...
Geohydrology of the valley-fill aquifer in the Jamestown area, Chautauqua County, New York
H. R. Anderson, W. G. Stelz, J. L. Belli, R. V. Allen
1982, Open-File Report 82-113
This report is the sixth in a series of 11 map sets depicting geohydrologic conditions in selected aquifers in upstate New York. Geohydrologic data are compiled on six maps at 1:24,000 scale. Together, the maps provide a comprehensive overview of a major valley-fill aquifer in southeastern Chautauqua County. The maps...
Palaeocopid and podocopid Ostracoda from the Lexington Limestone and Clays Ferry Formation (Middle and Upper Ordovician) of central Kentucky
S.M. Warshauer, J.M. Berdan
1982, Professional Paper 1066-H
The Middle through lower Upper Ordovician Lexington Limestone and lower part of the Clays Ferry Formation contain an abundant and diversified ostracode fauna. More than 10,000 specimens belonging to 39 genera and 53 species have been found in 73 collections made by members of the U.S. Geological Survey in cooperation...
Appraisal of ground-water quality near wastewater-treatment facilities, Glacier National Park, Montana
Joe A. Moreland, Wayne A. Wood
1982, Water-Resources Investigations Report 82-4
Water-level and water-quality data were collected from monitoring wells at wastewater-treatment facilities in Glacier National Park. Five additional shallow observation wells were installed at the Glacier Park Headquarters facility to monitor water quality in the shallow ground-water system.Water-level, water-quality, and geologic information indicate that some of the initial monitoring wells...
A three-dimensional ground-water-flow model modified to reduce computer-memory requirements and better simulate confining-bed and aquifer pinchouts
P.P. Leahy
1982, Water-Resources Investigations Report 82-4023
The Trescott computer program for modeling groundwater flow in three dimensions has been modified to (1) treat aquifer and confining bed pinchouts more realistically and (2) reduce the computer memory requirements needed for the input data. Using the original program, simulation of aquifer systems with nonrectangular external boundaries may result...
Analysis of three tests of the unconfined aquifer in southern Nassau County, Long Island, New York
J.B. Lindner, T. E. Reilly
1982, Water-Resources Investigations Report 82-4021
Drawdown and recovery data from three 2-day aquifer tests (OF) the unconfined (water-table) aquifer in southern Nassau County, N.Y., during the fall of 1979, were analyzed. Several simple analytical solutions, a typecurve-matching procedure, and a Galerkin finite-element radial-flow model were used to determine hydraulic conductivity, ratio of horizontal to vertical...
Algal conditions in the Caloosahatchee River (1975-79), Lake Okeechobee to Franklin Lock, Florida
Benjamin F. McPherson, Henry R. La Rose
1982, Water-Resources Investigations Report 81-81
Maximum numbers of suspended algae occurred in late spring and early summer, in each of the years 1975-79, in the Caloosahatchee River. Numbers exceeded 100,000 cells per milliliter at all stations sometime during the study. Concentrations decreased during late summer and autumn and were low during winter, except in January...