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Title: Helium 4 and radon 222 concentrations in groundwater and soil as indicators of zones of fracture concentration in unexposed rock

Journal Article · · J. Geophys. Res.; (United States)

The presence of zones of fracture concentration in unexposed rock may be partially assessed by measuring the concentrations of /sup 4/He and /sup 222/Rn in groundwater and soil gas. Helium 4 in groundwater and soil gas and /sup 222/Rn in groundwater were measured in the vicinity of two intersecting linements in Lehigh County, Pennsylvania. The limeaments are thought to mark deep fracture systems which provide conduits for the migration of /sup 4/He and /sup 222/Rn. High groundwater /sup 4/He concentrations revealed the presence of the two lineaments. Low groundwater /sup 222/Rn activities are found near the lineaments and qualitatively support a numerical model which relates low /sup 222/Rn activity to high fracture transmissivity. Radon 222 activity correlates most strongly with the presence of H/sub 2/S in groundwater, implying that geochemical controls or groundwater circulation patterns strongly influence radon concentration. Soil gas concentrations of /sup 4/He barely exceeded background levels and did not reliably indicate the lineament zones. The data show that groundwater /sup 4/He concentrations may be used to identify fracture zones in unexposed bedrock. copyright American Geophysical Union 1988

Research Organization:
GAI Consultants, Incorporated, Monroeville, Pennsylvania
OSTI ID:
5426230
Journal Information:
J. Geophys. Res.; (United States), Vol. 93:B1
Country of Publication:
United States
Language:
English