Publications
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Filter Total Items: 669
Evapotranspiration and the water budget of prairie potholes in North Dakota Evapotranspiration and the water budget of prairie potholes in North Dakota
The mass-transfer method was used to study the hydrologic behavior of 10 prairie potholes in central North Dakota during the 5-year period 1960-64. Many of the potholes went dry when precipitation was low. The average evapotranspiration during the May to October period each year was 2.11 feet, and the average seepage was 0.60 foot. These averages remained nearly constant for both wet and...
Authors
J.B. Shjeflo
Estimated use of water in the United States, 1965 Estimated use of water in the United States, 1965
Estimates of water use in the United States for 1965 indicate that an average of about 310 bgd (billion gallons per day) were withdrawn for public-supply, rural domestic and livestock, irrigation, and industrial (including thermoelectric power)uses--that is, about 1,600 gallons per capita per day. This represents an increase of 15 percent over the withdrawal of 270 bgd reported for 1960...
Authors
Charles Richard Murray
A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota
A hydrologic study of the Big Sioux aquifer system was begun July 1, 1966, by the U.S. Geological Survey, in cooperation with the City of Sioux Falls and the East Dakota Conservancy Sub-District. Test drilling being done in the search for a southern outlet to the Big Sioux aquifer has led to the discovery of the outlet and of a deeper aquifer than was previously know to exist in this...
Authors
Kenneth D. Vaughan, Earl A. Ackroyd
Geological Survey research 1968: Chapter C Geological Survey research 1968: Chapter C
No abstract available.
Authors
Water Resources Division U.S. Geological Survey
Design and construction of a dual recharge system at Minot, North Dakota Design and construction of a dual recharge system at Minot, North Dakota
In 1965, a ground-water recharge facility was constructed and placed in operation to forestall an impending water shortage at Minot, North Dakota. The facility is unique in that the rate of recharge to a buried sand and gravel aquifer is augmented by perforating an overlying bed of clay using hydraulic connectors (gravel-filled bored holes) in conjunction with an open-pit excavation. The
Authors
Wayne A. Pettyjohn
Hydrology for urban land planning - A guidebook on the hydrologic effects of urban land use Hydrology for urban land planning - A guidebook on the hydrologic effects of urban land use
This circular attempts to summarize existing knowledge of the effects of urbanization on hydrologic factors. It also attempts to express this knowledge in terms that the planner can use to test alternatives during the planning process. Because the available data used in this report are applied to a portion of the Brandywine Creek basin in Pennsylvania, this can be considered as a report...
Authors
Luna Bergere Leopold
Geological Survey research 1968, Chapter D Geological Survey research 1968, Chapter D
This collection of 48 short papers is the third published chapter of "Geological Survey Research 1968." The papers report on scientific and economic results of current work by members of the Geologic and Water Resources Divisions of the U.S. Geological Survey.
Authors
Water Resources Division U.S. Geological Survey
Geology and ground water resources of Eddy and Foster Counties, North Dakota Geology and ground water resources of Eddy and Foster Counties, North Dakota
Eddy and Foster Counties are in east-central North Dakota, high on the eastern flank of the Williston Basin. They are underlain by 3200 to 4300 feet of Paleozoic and Mesozoic rocks that dip gently to the west. The uppermost formation, the Cretaceous Pierre Shale, lies directly beneath the glacial drift and crops out in the valleys of the James and Sheyenne Rivers. Glacial drift that...
Authors
John P. Bluemle, Henry Trapp
Artificial Recharge at Valley City, North Dakota, 1932 to 1965 Artificial Recharge at Valley City, North Dakota, 1932 to 1965
Valley City, North Dakota, has an average daily water use of 750,000 gallons, which is obtained from wells tapping pattly confined gravel deposits in the Sheyenne River valley. These deposits at Valley City have a maximum thickness of more than 50 feet and an areal extent of approximately 1 square mile. The aquifer has been artificially recharged successfully since 1932 by diversion of...
Authors
T. E. Kelly
Hydrologic applications of lithofacies clastic-ratio maps Hydrologic applications of lithofacies clastic-ratio maps
No abstract available.
Authors
Wayne A. Pettyjohn, Phillip G. Randich