T246 A Century of Hydrogeologic Investigations and Groundwater Modeling in the Great Basin: What Have We Learned?
Wednesday, 5 November 2003
1:30 PM - 5:30 PM
YUCCA MOUNTAIN OVERSIGHT
Paper number: T246-8
Program: Technical Sessions
Time: 3:25 PM – 3:45 PM
Authors
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Richard R. Parizek Presenting AuthorMember, US Nuclear Waste Technical Review Board, University Park, PA
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David M. DiodatoNuclear Waste Technical Review Board, Arlington, VA
Abstract
The DOE's task of predicting water flow and radionuclide transport at Yucca Mountain for 10,000 years is unprecedented. Hydrogeologic factors that may be significant to that prediction include: precipitation; percolation through the unsaturated zone and seepage into repository tunnels; presence or absence of fractures and faults; thermal perturbation of natural hydrologic processes from emplacement of hot wastes; matrix diffusion; sorption and retardation; colloid-facilitated transport; secondary mineralization; anisotropy of sedimentary and volcanic rocks and faults; and climate change.
Substantial progress has been made in creating regional and local hydrostratigraphic and hydrogeologic models, as well as in analyzing paleoclimate signals at Devil's Hole and in packrat middens. However, a vigorous effort is still required to reduce uncertainty and increase confidence in models and predictions of repository performance and to improve fundamental scientific understanding.