2002
DOI: 10.1016/s0883-2927(02)00029-x
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The geohydrologic setting of Yucca Mountain, Nevada

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Cited by 34 publications
(11 citation statements)
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“…Faults, fractures, and cooling joints in the welded tuffs form a partially connected network of pathways that allow downward movement of fracture water through the rock mass. The geology and hydrology of the site are summarized elsewhere (U.S. Department of Energy, 2000Energy, , 2001Stuckless and Dudley, 2002).…”
Section: Hydrogeologic Backgroundmentioning
confidence: 99%
“…Faults, fractures, and cooling joints in the welded tuffs form a partially connected network of pathways that allow downward movement of fracture water through the rock mass. The geology and hydrology of the site are summarized elsewhere (U.S. Department of Energy, 2000Energy, , 2001Stuckless and Dudley, 2002).…”
Section: Hydrogeologic Backgroundmentioning
confidence: 99%
“…Regionally, the mean annual free-water surface evaporation is 125-250 cm (Stuckless and Dudley, 2002); therefore, the infiltration at Yucca Mountain and subsequent percolation of moisture through the proposed repository horizon are both small. The water table is deep, lying 500-750 m below land surface (Stuckless and Dudley, 2002). Beneath the proposed repository the water table is nearly flat, with the hydraulic gradient ranging from 0.0001 to 0.0003 (Luckey and others, 1996).…”
Section: Introductionmentioning
confidence: 99%
“…Key features in the structural geology of the region include blockbounding faults, occurring every 1-4 km, and intrablock faults (Stuckless and Dudley, 2002). Because the proposed geological repository will include kilometers of horizontal tunnels, it will inevitably be intercepted by near-vertical faults.…”
Section: Introductionmentioning
confidence: 99%