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Within the 500 to 700 meter thickness of unsaturated zone at Yucca Mountain, site of the : proposed high-level nuclear waste repository, subsurface hydrologic processes occur in an arid environment within highly heterogeneous layers of anisotropic, fractured ash flow and air fall tuffs. Characterization of fluid flow and heat transfer through such a system has been a challenge due to the large-scale heterogeneity inherent in the mountain. Quantitative evaluation of water, gas, and heat flow is essential for design of the potential repository; although numerical modeling has played a crucial role this effort, accuracy and reliability of such model predictions are critically dependent on model parameters.

A FIELD-SCALE MODELING STUDY AND CHARACTERIZING HYDRAULIC PROPERTIES FOR WATER, AIR AND HEAT FLOW IN THE UNSATURATED ZONE OF YUCCA MOUNTAIN, NEVADA