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contributor authorDavid A. Woolhiser
contributor authorStuart A. Stothoff
contributor authorGordon W. Wittmeyer
date accessioned2017-05-08T21:23:21Z
date available2017-05-08T21:23:21Z
date copyrightJuly 2000
date issued2000
identifier other%28asce%291084-0699%282000%295%3A3%28240%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/49525
description abstractIt has been hypothesized that the Solitario Canyon watershed, just west of Yucca Mountain, Nev., could provide a zone of focused ground-water recharge through its ephemeral-stream channels that might be an important factor in the performance of the potential repository for high-level radioactive waste. To examine this possibility, the KINEROS2 rainfall-runoff model was used to estimate the infiltration from surface runoff in each of 79 channel elements using a 100-year simulated rainfall sequence and two sets of saturated hydraulic conductivity
publisherAmerican Society of Civil Engineers
titleChannel Infiltration in Solitario Canyon, Yucca Mountain, Nevada
typeJournal Paper
journal volume5
journal issue3
journal titleJournal of Hydrologic Engineering
identifier doi10.1061/(ASCE)1084-0699(2000)5:3(240)
treeJournal of Hydrologic Engineering:;2000:;Volume ( 005 ):;issue: 003
contenttypeFulltext


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