Occurrence of strontium in the surface and ground waters of Champaign county, Ohio

Economic Geology
By:  and 

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Abstract

Naturally occurring strontium was found in both surface and ground waters during an investigation of the water resources of Champaign CountyOhio. The strontium is related to the presence of celestite (strontium sulfate) in rocks associated with evaporite deposition. The principal source of celestite in Ohio is in rocks of Late Silurian age. Celestite is present also in the glacial deposits of western Ohio, which contain rock material of Late Silurian age. Total time in contact with the rock material seems to have a large effect upon concentrations of strontium in ground water. Streamflow, during low-flow periods, is made up largely of ground-water seepage and contains detectable strontiumStrontium has been found in ground water in other counties in western Ohio and in the brines of eastern Ohio.

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Publication type Article
Publication Subtype Journal Article
Title Occurrence of strontium in the surface and ground waters of Champaign county, Ohio
Series title Economic Geology
DOI 10.2113/gsecongeo.55.1.176
Volume 55
Issue 1
Year Published 1960
Language English
Publisher location Society of Economic Geologist
Description 11 p.
First page 176
Last page 186
Country United States
State Ohio
County Champaign County
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