A Mountain‐Scale Model for Characterizing Unsaturated Flow and Transport in Fractured Tuffs of Yucca Mountain-Reference-Cited by-同舟云学术

A Mountain‐Scale Model for Characterizing Unsaturated Flow and Transport in Fractured Tuffs of Yucca Mountain

Published:2004-08 Issue:3 Volume:3 Page:796-805
ISSN:1539-1663
Container-title:Vadose Zone Journal
language:en
Short-container-title:Vadose zone j.

Author:

Wu Yu‐Shu¹,Lu Guoping¹,Zhang Keni¹,Bodvarsson G. S.¹

Affiliation:

1. Earth Sciences DivisionLawrence Berkeley National LaboratoryBerkeleyCA94720

Funder

U.S. Department of Energy

Publisher

Wiley

Subject

Soil Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.2136/vzj2004.0796

Reference28 articles.

1. Characterization and prediction of subsurface pneumatic response at Yucca Mountain, Nevada

2. Calibrating hydrogeologic parameters for the 3-D site-scale unsaturated zone model of Yucca Mountain, Nevada

3. Development of discrete flow paths in unsaturated fractures at Yucca Mountain

4. Buesch D.C. R.W.Spengler P.H.Nelson D.T.Vaniman S.J.Chipera andD.L.Bish.1995.Geometry of the vitric‐zeolitic transition in tuffs and the relation to fault zones at Yucca Mountain Nevada.International Union of Geodesy and Geophysics XXI General Assembly. 2–14 July 1995. A426.

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