Temporal damping effect of the Yucca Mountain fractured unsaturated rock on transient infiltration pulses

Author:

Zhang Keni,Wu Yu-Shu,Pan Lehua

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference31 articles.

1. BSC (Bechtel SAIC Company) 2004a. UZ Flow Models and Submodels, MDL-NBS-HS-000006, REV02, Las Vegas, Nevada: Bechtel SAIC Company. ACC: DOC. 20041101.0004; DOC. 20050629.0003.

2. BSC (Bechtel SAIC Company) 2004b. Simulation of Net Infiltration for present-Day and Potential Future Climates. MDL-NBS-HS-000023 REV 00, Las Vegas, Nevada: Bechtel SAIC Company. ACC: DOC, 20041109.0004.

3. Fabryka-Martin, J.T., 2000. Analysis of geochemical data for the unsaturated zone, Report ANL-NBS-GS-00004, Los Alamos National Laboratory, CRWMS M&O.

4. On the physics of unstable infiltration, seepage, and gravity drainage in partially saturated tuffs;Faybishenko;J. Contam. Hydrol.,2003

5. Flint, A.L., Hevesi, J.A., Flint, L.E., 1996. Conceptual and numerical model of infiltration for the Yucca Mountain area, Milestone 3GU1623M, Water Resources Investigation Report, U.S. Geological Survey, Denver CO.

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