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Title: Availability and quality of water from the Dakota aquifer, northwest Iowa

Technical Report ·
OSTI ID:5191599

The Dakota aquifer in northwest Iowa consists of sandstones in the Dakota Formation. It underlies most of the study area and is the most extensive source of ground water in the area. Individual sandstone beds are from less than 10 to more than 150 feet thick. The cumulative thickness of sandstone is more than 200 feet throughout much of the area. Water flows through the aquifer from the northcental part of the study area to the east, south and southwest. Recharge is dominantly by infiltration from the land surface through the confining materials. Discharge is to underlying Paleozoic aquifers and to the alluvium and glacial outwash deposits along the Missouri and Big Sioux Rivers in the southwest part of the area. Pumping tests conducted in the study area indicate a narrow range of hydraulic conductivities of the Dakota aquifer, from 37 to 50 feet per day. Yields of more than 250 gallons per minute can be expected throughout much of the study area and more than 1000 gallons per minute could be produced in some areas. The quality of water from the Dakota is a calcium, magnesium, sulfate type. The concentration of a radium-226 and other radionuclides exceeds recommended limits at several sites. The quality of water pumped from the aquifer my be altered by induced leakage from the underlying aquifers in Paleozoic age rocks if withdrawals reverse the pattern of natural flow from the Dakota into the Paleozoic aquifers. Evidence for such a reversal exists in the area around the city of LeMars. 10 refs., 4 figs., 5 tabs.

Research Organization:
Geological Survey, Denver, CO (USA)
OSTI ID:
5191599
Report Number(s):
USGS-WSP-2215; ON: TI85902208
Country of Publication:
United States
Language:
English