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Publications

Browse more than 150,000 publications authored by our scientists over the past 100+ year history of the USGS.  Publications available are: USGS-authored journal articles, series reports, book chapters, other government publications, and more.

Upper Midwest Environmental Sciences Center Publications

Filter Total Items: 3323

Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds

Isobornyl thiocyanoacetate (Thanite) is an insecticide that induces a surfacing response in fish and therefore has been considered to have potential as a fish collection agent. Analyses for residues of Thanite in carp (Cyprinus carpio) and largemouth bass (Micropterus salmoides) exposed to chemical yielded only a trace of the parent compound. A metabolite, isobornyl a-(methylthio)acetate...
Authors
J. L. Allen, J.B. Sills, V. K. Dawson, R.T. Amel

Effect of snowmelt on the quality of Filson Creek and Omaday Lake, northeastern Minnesota Effect of snowmelt on the quality of Filson Creek and Omaday Lake, northeastern Minnesota

Concentrations of major constituents were determined in the surface water, ground water, and precipitation in Filson Creek watershed to evaluate the effects of acid precipitation on surface-water quality during snowmelt. Concentrations of sulfate increased in Filson Creek and Omaday Lake during snowmelt from less than 2 to 12 milligrams per liter in 1977 and from less than 2 to 4...
Authors
Donald I. Siegel, L. E. Anderson, J. A. Rogalla

Water quality of Alimagnet, Farquar, and Long Lakes in Apple Valley, Minnesota Water quality of Alimagnet, Farquar, and Long Lakes in Apple Valley, Minnesota

Alimagnet, Farquar, and Long Lakes, in Apple Valley, Minnesota, were sampled from 1973-79 to determine their physical and chemical characteristics. A storm-sewer inlet to Alimagnet Lake was also sampled during two storms in 1978. The 1976-77 drought caused a more noticeable effect on the quality of the lakes than any other factor. Chloride concentrations were 10 to 15 milligrams per...
Authors
M.R. Have, G. A. Payne, M. A. Ayers

Hydrogeologic setting of the Glacial Lake Agassiz Peatlands, northern Minnesota Hydrogeologic setting of the Glacial Lake Agassiz Peatlands, northern Minnesota

Seven test holes drilled in the Glacial Lake Agassiz Peatlands indicate that the thickness of surficial materials along a north-south traverse parallel to Minnesota Highway 72 ranges from 163 feet near Blackduck, Minnesota to 57 feet about 3 miles south of Upper Red Lake. Lenses of sand and gravel occur immediately above bedrock on the Itasca moraine and are interbedded with lake clay...
Authors
Donald I. Siegel

Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin

Various changes in the management practices for the Winnebago pool have been proposed. The objectives of the proposed changes are protecting wetlands adjacent to the lakes in the pool and assuring adequate flow in the Fox River downstream from Lake Winnebago. Three proposed operation plans for the Winnebago pool were studied to determine the effects on lake stage and discharge. A digital...
Authors
William R. Krug

An assessment of streamflow, water quality, and the effects of constructing an impoundment on Bridge Creek at Augusta, Wisconsin An assessment of streamflow, water quality, and the effects of constructing an impoundment on Bridge Creek at Augusta, Wisconsin

This study documents Streamflow, temperature, and water-quality conditions of Bridge Creek at Augusta, Wisconsin, and evaluates the potential effects of a proposed small impoundment on the creek. The effects are of concern to the Wisconsin Department of Natural Resources because the stream is a Class II trout stream. Average daily Streamflow, from records collected during the 1980 water...
Authors
Leo B. House

Hydraulic characteristics of an underdrained irrigation circle, Muskegon County, wastewater disposal system, Michigan Hydraulic characteristics of an underdrained irrigation circle, Muskegon County, wastewater disposal system, Michigan

Muskegon County, Michigan, disposes of waste water by spray irrigating farmland on its waste-disposal site. Buried drains in the highly permeable unconfined aquifer at the site control the level of the water table. Hydraulic conductivity of the aquifer and drain-leakance, the reciprocal of resistance to flow into the drains, was determined at a representative irrigation circle while...
Authors
M.G. McDonald

Designation of principal water-supply aquifers in Minnesota Designation of principal water-supply aquifers in Minnesota

Fourteen aquifers, ranging from Quaternary to Precambrian in age, have been identified as the principal sources of water to wells in Minnesota. Half the municipal population anc nearly all the rural population depend on water from these aquifers. Buried and surficial sand and gravel aquifers of Quaternary age occur in nearly all areas of the State and are composed of outwash, beach-ridge...
Authors
D. G. Adolphson, J. F. Ruhl, R. J. Wolf

Preliminary evaluation of ground-water contamination by coal-tar derivatives, St. Louis Park area, Minnesota Preliminary evaluation of ground-water contamination by coal-tar derivatives, St. Louis Park area, Minnesota

Operation of a coal-tar distillation and wood preserving plant for 1918-72 in St. Louis Park, Minnesota, resulted in ground-water contamination. This report presents the results of the first year (1979) of an ongoing study. By 1932, water in the Prairie du Chien-Jordan aquifer, the region 's major source of ground water, was contaminated 3,500 feet from the plant. The hydraulic...
Authors
Marc F. Hult, Michael Schoenberg

Geology and hydrology for environmental planning in Washtenaw County, Michigan Geology and hydrology for environmental planning in Washtenaw County, Michigan

Washteaw County is underlain by glacial deposits that range in thickness from about 50 feet to about 450 feet. Underlying the glacial deposits are sedimentary rocks of Mississippian and Devonian age. The youngest of these rocks are the sandstones of the Marshall Formation in the western part of the county; the oldest are the limestones of the Detroit River Group in the southeast corner...
Authors
William B. Fleck
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