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Abstract
Forty-eight core samples of ash-flow tuffs from Yucca Mountain, NV, were selected for comparative analysis by uranium-based methods to estimate past interaction with oxidizing water. Results aid in the selection of hydrologically isolated host rocks for radioactive waste disposal. U abundances were consistently more variable than thorium in whole rocks, suggesting some selective redistribution of U. Dissolved U correlates most strongly with dissolved manganese, indicating a predominant association of U with manganese oxides.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Rock-water interaction in ash-flow tuffs (Yucca Mountain, Nevada, USA)- The record from uranium studies |
| Series title | Uranium |
| Volume | 2 |
| Issue | 4 |
| Year Published | 1986 |
| Language | English |
| Publisher | Elsevier |
| Contributing office(s) | Central Energy Resources Science Center, Geosciences and Environmental Change Science Center |
| Description | 26 p. |
| First page | 361 |
| Last page | 386 |
| Country | United States |
| State | Nevada |
| Other Geospatial | Yucca Mountains |
| Google Analytic Metrics | Metrics page |