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Hydrogeologic and geochemical studies of selected natural radioisotopes and barium in groundwater in Illinois. Research report No. 180 (final)

Technical Report ·
OSTI ID:5328267

Dissolved concentration of the natural radioisotopes /sup 222/Rn, /sup 226/Ra, /sup 228/Ra, /sup 230/Th, /sup 232/Th, /sup 234/U, and /sup 238/U and the element Ba (/sup 2 +/) were investigated in a study of high concentrations of /sup 226/Ra, /sup 228/Ra, and Ba (/sup 2 +/) in groundwater from the Cambrian and Ordovician bedrock of northern Illinois. The high radium and barium concentrations are present in the major aquifers - the sandstone bedrock. Therefore, remedial well construction measures will not lower the concentrations. The combined concentrations of /sup 226/Ra and /sup 228/Ra range from 2.3 to 50.2 pCi/L; the majority of analyses exceed the drinking water reulations of 50.0 pCi/L. The high Ba (/sup 2 +/) concentrations occur in groundwater that is depleted in dissolved SO/sub 4//sup 2 -/ by anaerobic microbial reactions. A map presents the distribution of Ba /sup 2 +/ in groundwater from the Cambrian and Ordovician bedrock in northeastern Illinois.

Research Organization:
Illinois Univ., Urbana (USA). Water Resources Center
OSTI ID:
5328267
Report Number(s):
PB-83-258426
Country of Publication:
United States
Language:
English

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