Uranium-series disequilibrium in tuffs from Yucca Mountain, Nevada, as evidence of pore-fluid flow over the last million years

Author:

Gascoyne M.,Miller N.H.,Neymark L.A.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference30 articles.

1. Calibrating hydrogeologic parameters for the 3-D site-scale unsaturated zone model of Yucca Mountain, Nevada;Bandurraga;J. Contam. Hydrol.,1999

2. Overview of scientific investigations at Yucca Mountain—the potential repository for high-level nuclear waste;Bodvarsson;J. Contam. Hydrol,1999

3. Bush, C.A., Bunker, C.M. and Spengler, R.W. 1983. Radioelement distribution in drill-hole USW-G1, Yucca Mountain, Nye County, Nevada. US Geological Survey Open-file Report 83-847.

4. Fabryka-Martin, J.T., Wightman, S.J., Murphy, W.J, Wickham, M.P., Caffee, M.W., Nimz, G.J., Southon, J.R. and Sharma, P., 1993. Distribution of chlorine-36 in the unsaturated zone at Yucca Mountain: an indicator of fast transport paths. Proc. FOCUS ’93: Site Characterization and Model validation, 26–29 Sept. 1993, Las Vegas, Nevada, American Nuclear Society, La Grange Park, IL, pp. 58–68.

5. Gascoyne, M., 1985. Uranium-series disequilibrium studies of Shield rocks and groundwater, Atomic Energy of Canada Limited Report, TR-299, 634–641.11Internal report, available from SDDO, AECL, Chalk River Laboratories, Chalk River, Ontario, Canada K0J 1J0.

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