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/sup 222/Rn concentrations in deep formation waters and the geohydrology of the Cajon Pass borehole

Journal Article · · Geophys. Res. Lett.; (United States)
Measurements of /sup 222/Rn, /sup 226/Ra, and /sup 238/U in formation waters derived from granitic rocks surrounding the Cajon Pass borehole indicate concentrations of about 700, 1, and 0.01 dpm/1, respectively. The radon profile in the borehole indicates that inputs are localized and several fracture zones must contribute significant amounts of inflow. Radon concentrations in fracture fluids indicate a minimum fracture width of 0.3 ..mu..m, and this width may be combined with the measured permeability to show that fracture porosity does not exceed 1.5 x 10/sup -3/. It is likely that the calculated fracture width is too small because incongruent weathering enriches fracture walls in /sup 238/U and /sup 226/Ra relative to the bulk rock. However, radon concentrations are lower than those in formation waters from other crystalline rocks, suggesting that the wall enrichments here are less pronounced and that fractures have experienced relatively limited fluid flow. copyright American Geophysical Union 1988
Research Organization:
Department of Geological Sciences, University of Southern California, Los Angeles
OSTI ID:
7079025
Journal Information:
Geophys. Res. Lett.; (United States), Journal Name: Geophys. Res. Lett.; (United States) Vol. 15:9; ISSN GPRLA
Country of Publication:
United States
Language:
English