238U and 232Th series nuclides in groundwater from the J-13 well at the Nevada Test Site: implications for ion retardation

Copenhaver, Sally A. ; Krishnaswami, S. ; Turekian, Karl K. ; Shaw, Henry (1992) 238U and 232Th series nuclides in groundwater from the J-13 well at the Nevada Test Site: implications for ion retardation Geophysical Research Letters, 19 (13). pp. 1383-1386. ISSN 0094-8276

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Official URL: http://www.agu.org/pubs/crossref/1992/92GL01437.sh...

Related URL: http://dx.doi.org/10.1029/92GL01437

Abstract

The activities of members of the 238U and 232Th decay chains have been determined in water from well J-13 at the Nevada Test Site near Yucca Mountain. Using 222Rn as a measure of recoil flux, adsorption (k1) and desorption (k2) rate constants for Ra and Pb have been determined. The ratio (k1/k2), defined as the dimensionless distribution coefficient, K, is 1.3 × 104 for Ra and 2.7 × 104 for Pb and is estimated to be about 104 for Th.

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