Hostname: page-component-586b7cd67f-r5fsc Total loading time: 0 Render date: 2024-11-25T17:42:04.444Z Has data issue: false hasContentIssue false

Chlorine-36 Investigations of Groundwater Infiltration in the Exploratory Studies Facility at Yucca Mountain, Nevada

Published online by Cambridge University Press:  03 September 2012

Schön S. Levy
Affiliation:
Los Alamos National Laboratory, Los Alamos, New Mexico 87545
June T. Fabryka-Martin
Affiliation:
Los Alamos National Laboratory, Los Alamos, New Mexico 87545
Paul R. Dixon
Affiliation:
Los Alamos National Laboratory, Los Alamos, New Mexico 87545
Beiling Liu
Affiliation:
Los Alamos National Laboratory, Los Alamos, New Mexico 87545
H. J. Turin
Affiliation:
Los Alamos National Laboratory, Los Alamos, New Mexico 87545
Andrew V. Wolfsberg
Affiliation:
Los Alamos National Laboratory, Los Alamos, New Mexico 87545
Get access

Abstract

Chlorine-36, including the natural cosmogenic component and the component produced during atmospheric nuclear testing in the 1950's and 1960's (bomb pulse), is being used as an isotopie tracer for groundwater infiltration studies at Yucca Mountain, a potential nuclear waste repository. Rock samples have been collected systematically in the Exploratory Studies Facility (ESF), and samples were also collected from fractures, faults, and breccia zones. Isotopie ratios indicative of bomb-pulse components in the water (36Cl/Cl values > 1250 × 10-15), signifying less than 40-yr travel times from the surface, have been detected at a few locations within the Topopah Spring Tuff, the candidate host rock for the repository. The specific features associated with the high 36Cl/Cl values are predominantly cooling joints and syngenetic breccias, but most of the sites are in the general vicinity of faults. The non-bomb pulse samples have 36Cl/Cl values interpreted to indicate groundwater travel times of at least a few thousand to possibly several hundred thousand years. Preliminary numerical solute-travel experiments using the FEHM (Finite Element Heat and Mass transfer) code demonstrate consistency between these interpreted ages and the observed 36Cl/Cl values but do not validate the interpretations.

Type
Research Article
Copyright
Copyright © Materials Research Society 1997

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

1. Bentley, H.W., Phillips, F.M., and Davis, S.N. in Handbook of Environmental Isotope Geochemistry, Vol. 11B, edited by Fontes, J.C. and Fritz, P., Elsevier, Amsterdam, 1986, 427480.Google Scholar
2. Fabryka-Martin, J.T., Turin, H.R., Brenner, D., Dixon, P.R., Liu, B., Musgrave, J., and Wolfsberg, A.V., Summary Report of Chlorine-36 Studies, Los Alamos National Laboratory YMP Milestone Report 3782M (in press).Google Scholar
3. Glasstone, S. (ed.), The Effects of Nuclear Weapons, Revised Edition, U.S. Atomic Energy Commission, Washington D.C., 1962, 730 pp.Google Scholar
4. Fabryka-Martin, J., Wolfsberg, A.V., Dixon, P.R., Levy, S., Musgrave, J., and Turin, H.J., Summary Report of Chlorine-36 Studies: Systematic Sampling for Chlorine-36 in the Exploratory Studies Facility, Los Alamos National Laboratory, YMP Level 3 Milestone Report 3783M (in press).Google Scholar
5. Paces, J.B., Neymark, L.A., Marshall, B.D., Whelan, J.F., and Peterman, Z.E., Ages and Origins of Subsurface Secondary Minerals in the Exploratory Studies Facility (ESF), U.S. Geological Survey - Yucca Mountain Project Branch 1996 Milestone Report 3GQH450M (in press).Google Scholar
6. Zyvoloski, G.A., Dash, Z.V., and Kelkar, S., FEHMN 1.0: Finite Element Heat and Mass Transfer Code, Los Alamos National Laboratory Report LA-12062-MS, Rev. 1 (1992).Google Scholar
7. Flint, A.L., Hevesi, J.A., and Flint, L.E., Conceptual and Numerical Model of Infiltration for the Yucca Mountain Area, Nevada, U.S. Geological Survey Water Resources Investigation Report (in press).Google Scholar
8. Vaniman, D.T., Chipera, S.J., and Bish, D.L., Los Alamos National Laboratory Report LA-13096-MS (1995).Google Scholar