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Filter Total Items: 670

Geochemistry of artificial-recharge tests in the Oakes aquifer near Oakes, southeastern North Dakota Geochemistry of artificial-recharge tests in the Oakes aquifer near Oakes, southeastern North Dakota

As part of an artificial-recharge feasibility study, water from the James River was introduced into the Oakes aquifer of southeastern North Dakota by infiltration through a recharge basin. Chemical composition of water in the recharge basin and ground water from two separate flow paths beneath the basin was determined from samples taken during two artificial-recharge tests. Changes...
Authors
G. F. Huff, J. D. Wald

Water-quality data for selected wells and drains in the Oakes study area, south-central North Dakota, December 1986 through September 1987 Water-quality data for selected wells and drains in the Oakes study area, south-central North Dakota, December 1986 through September 1987

Operation of the Garrison Diversion Unit in North Dakota will divert water from the Missouri River near Lake Audubon into the upper James River basin (fig. 1). The diverted water will augment flows in the James River sufficiently to permit expanded irrigation and to provide additional water supplies for municipal and industrial use. The proposed Garrison Diversion Unit development and...
Authors
James D. Wald, C.S. Helgesen, M.C. Pokladnik

Water resources data, North Dakota, water year 1988 Water resources data, North Dakota, water year 1988

No abstract available.
Authors
R.E. Harkness, N.D. Haffield, G.L. Ryan, E. A. Wesolowski

Streamflow at selected gaging stations on the James River in North Dakota and South Dakota, 1953-82, with a section on climatology Streamflow at selected gaging stations on the James River in North Dakota and South Dakota, 1953-82, with a section on climatology

Historic stream flow data were compiled and record extension techniques were used, when necessary, to develop a monthly stream flow record for 1953-82 at streamflow-gaging stations on the James River in North Dakota and South Dakota. The record extension techniques included both Maintenance of Variance Extension Type 1 and Ordinary Least Squares. In addition to the historic stream flow...
Authors
Gregg J. Wiche, Rick D. Benson, Douglas G. Emerson

Dissolved-solids data for the James River salinity model, North Dakota and South Dakota Dissolved-solids data for the James River salinity model, North Dakota and South Dakota

Operation of the Garrison Diversion Unit in North Dakota will divert water from the Missouri River into the James River basin and thereby augment flows in the James River sufficiently to permit expanded irrigation and to provide new water supplies for municipal and industrial use. Salinity of water in the James River currently is marginal for irrigation use f and expanded irrigation may...
Authors
L. I. Briel

The design and use of a hydraulic potentiomanometer for direct measurement of differences in hydraulic head between groundwater and surface water The design and use of a hydraulic potentiomanometer for direct measurement of differences in hydraulic head between groundwater and surface water

The hydraulic potentiomanometer described herein consists of a potentiometer connected to a manometer by a flexible tube. The device is used to directly measure the direction of seepage as well as the hydraulic-head difference between groundwater and surface water. The device works most effectively in sandy materials. For accurate measurements the device must be free of air leaks.
Authors
Thomas C. Winter, James W. LaBaugh, Donald O. Rosenberry

National water summary 1986: Hydrologic events and ground-water quality National water summary 1986: Hydrologic events and ground-water quality

Ground water is one of the most important natural resources of the United States and degradation of its quality could have a major effect on the welfare of the Nation. Currently (1985), ground water is the source of drinking water for 53 percent of the Nation's population and for more than 97 percent of its rural population. It is the source of about 40 percent of the Nation's public...

Capacity of McKenzie Slough near McKenzie, North Dakota Capacity of McKenzie Slough near McKenzie, North Dakota

A topographic survey of McKenzie Slough, N. Dak., was conducted from August 1984 through August 1986 by the U.S. Geological Survey in cooperation with the Burleigh County Water Resources District. McKenzie Slough is located near the town of McKenzie, N. Dak. McKenzie is about 18 miles east of the city of Bismarck and 1 mile south of U.S. Interstate Highway 94. The slough is in the Apple...
Authors
Robert W. Gauger

Review of mechanisms, methods, and theory for determining recharge to shallow aquifers in North Dakota Review of mechanisms, methods, and theory for determining recharge to shallow aquifers in North Dakota

Effective management of ground-water resources requires knowledge of all components of the water budget for the aquifer of interest. Efforts to simulate ground-water flow prior to development and the effects of proposed pumping in several of North Dakota's shallow glacial aquifers have been hindered by the lack of reliable estimates of ground-water recharge. This study was done to (1)...
Authors
W.F. Horak

Surface-water hydrology of Hay Creek watershed, Montana, and West Branch Antelope Creek watershed, North Dakota Surface-water hydrology of Hay Creek watershed, Montana, and West Branch Antelope Creek watershed, North Dakota

Hydrologric data were used to determine the premining surface-water conditions in two small basins in the Fort Union coal region of Montana and North Dakota. The two streams. Hay Creek and West Branch Antelope Creek, are ephemeral. Most of the volume and peak discharges are due to snowmelt runoff. Little rainfall runoff occurs, and volume and peak discharges for this runoff are...
Authors
Douglas G. Emerson
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