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Title: Distribution of /sup 226/Ra in the lower paleozoic aquifers of southeast Kansas and adjacent areas

Conference · · Trace Subst. Environ. Health; (United States)
OSTI ID:6240893

Prior routine monitoring of public water supplies by health agencies in the Tri-State Region of Kansas, Oklahoma and Missouri revealed several areas where water samples from wells finished in the Cambro-Ordovician exceeded the maximum contaminant levels set by USEPA for radium /sup 226/Ra. The purpose of this study was to determine the region-wide distribution pattern and geochemistry of this radionuclide. /sup 226/Ra activities were found to vary from 0.5 to 11 pCi/l (1 pCi = 10/sup -12/ g) and were highest along the eastern margin of the transition from fresh to saline water; /sup 226/Ra activities are highly correlated with specific conductance and the presence of hydrogen sulfide (H/sub 2/S). Along 2 traverses through the region uranium (U) concentration decreases by an order of magnitude while the /sup 226/Ra//sup 234/U activity ratio (AR) increases by an order of magnitude or more where H/sub 2/S is present. The /sup 234/U//sup 238/U AR is uniformly high along both traverses. /sup 226/Ra is likely generated by the decay of /sup 238/U precipitated from westward flowing groundwaters from the recharge area and is mixed with radium-bearing, low-sulfate connate waters west of the transition zone.

Research Organization:
Kansas Geological Survey, Lawrence
OSTI ID:
6240893
Report Number(s):
CONF-8106251-
Journal Information:
Trace Subst. Environ. Health; (United States), Vol. 15; Conference: 15. annual conference on trace substances in environmental health, Columbia, MO, USA, 1 Jun 1981
Country of Publication:
United States
Language:
English