1996
DOI: 10.2172/437703
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Status of understanding of the saturated-zone ground-water flow system at Yucca Mountain, Nevada, as of 1995

Abstract: Portions of this document may be illegible in electronic image products. Images are produced from the best available original document.

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Cited by 31 publications
(74 citation statements)
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“…The results also indicate that the Calico Hills Formation (Tac), which is a zeolitized tuff that functions as the Upper Volcanic Confining Unit (Luckey et al 1996, Figure 7), has a higher permeability than the Bullfrog Tuff (Tcb) and the Carbonate Aquifer. This paradoxical result may reflect the fact that, because it is unsaturated in the western half of Yucca Mountain, the Calico Hills Formation could be hydraulically tested only in the highly faulted eastern half of Yucca Mountain, whereas the other units were also tested in less intensely faulted areas to the west.…”
Section: The Imentioning
confidence: 90%
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“…The results also indicate that the Calico Hills Formation (Tac), which is a zeolitized tuff that functions as the Upper Volcanic Confining Unit (Luckey et al 1996, Figure 7), has a higher permeability than the Bullfrog Tuff (Tcb) and the Carbonate Aquifer. This paradoxical result may reflect the fact that, because it is unsaturated in the western half of Yucca Mountain, the Calico Hills Formation could be hydraulically tested only in the highly faulted eastern half of Yucca Mountain, whereas the other units were also tested in less intensely faulted areas to the west.…”
Section: The Imentioning
confidence: 90%
“…For instance, in cases in which the test interval was in the Prow Pass Tuff, with or without some portion of the adjacent bedded tuffs, the test results were grouped with other permeability estimates for the Prow Pass Tuff. If other units within the Middle Volcanic Aquifer (MVA), as defined by Luckey et al (1996, Figure 7), were also present in the test interval along with the Prow Pass Tuff, the test results were considered to represent the MVA. If hydrogeologic units other than those in the MVA were present in the test interval along with the Prow Pass Tuff, the permeability estimate for the test was grouped with the most general category, which is the mixed tuffs.…”
Section: Single-hole Testsmentioning
confidence: 99%
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“…Many previous publications contain comprehensive site descriptions that have evolved during site investigation (DOE, 1995;Luckey et al, 1996;Flint et al, 1996;Scott and Bonk, 1984;Wilson et al, 1994;Winopd and Thordarson, 1975;Younker et al, 1992). The 1988 Site Characterization Plan (SCP) (DOE, 1988b) contains extensive background information for virtually all aspects of the geologic barrier subsystem.…”
Section: Data Sources and Previous Studiesmentioning
confidence: 99%
“…The saturated zone at Yucca Mountain is an unconfined aquifer that is part of the Alkali Flat-Furnace Creek groundwater basin which is part of the larger (47,000 km2) Death Valley groundwater flow system (Luckey et al, 1996). Groundwater flow fromYucca Mountain is generally to the south to southeast, which is why saturated zone modeling is often focused on a path in this direction relative to the repository.…”
Section: -8mentioning
confidence: 99%