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1993
DOI: 10.2172/139248
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Processes, mechanisms, parameters, and modeling approaches for partially saturated flow in soil and rock media; Yucca Mountain Site Characterization Project

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Cited by 6 publications
(7 citation statements)
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References 61 publications
(91 reference statements)
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“…Detailed analyses of the distributions and the correlations of soil and tuff parameters are in the report by Wang and Narasimhan (1989). In this review, we focus on two parameters: the saturated permeability and the unsaturated air entry scaling factor.…”
Section: Parameter Distributions: Difference Between Tight Tuffmatrixmentioning
confidence: 99%
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“…Detailed analyses of the distributions and the correlations of soil and tuff parameters are in the report by Wang and Narasimhan (1989). In this review, we focus on two parameters: the saturated permeability and the unsaturated air entry scaling factor.…”
Section: Parameter Distributions: Difference Between Tight Tuffmatrixmentioning
confidence: 99%
“…6, Wang et aI., 1988;Wang and Narasimhan, 1989) will be needed to characterize the fractured, tuff fonnations and to scale the hydrological parameters. As site characterization activities at Yucca Mountain (DOE, 1989) proceed, the uncertainties about the ambient conditions will be better quantified and models for performance assessment will be better calibrated and validated.…”
Section: Review and Summarymentioning
confidence: 99%
“…Knowledge of K, Rf, and d, as a function of .the volumetric water content, referred to as the characteristic behaviors of a porous medium, is particularly important in the near-field transition zone around high-level waste packages where changes in temperature, water content, compaction of backfill, infiltration of fines, and secondary mineralization will alter transport characteristics. An excellent discussion of transport parameters, processes, and mechanisms in partially saturated media can be found in Wang and Narasimhan, 1993. However, transport parameters have generally been difficult to obtain as a function of the volumetric water content. Traditional methods of investigating unsaturated systems require very long times to attain homogeneous distributions of water because normal gravity does not provide.…”
Section: Introductionmentioning
confidence: 99%
“…Knowledge of K, Rf, and D, as a function of the volumetric water content, referred to as the characteristic behaviors of a porous medium, is particularly important in the near-field transition zone around high-level waste packages where changes in temperature, water content, compaction of backfill, infiltration of fines, and secondary mineralization will alter transport characteristics. An excellent discussion of transport parameters, processes, and mechanisms in partially saturated media can be found in Wang and Narasimhan, 1993. However, transport parameters have generally been difficult to obtain as a function of the volumetric water content. Traditional methods of investigating unsaturated systems require very long times to attain homogeneous distributions of water because normal gravity does not provide a large enough driving force relative to the low hydraulic conductivities that characterize unsaturated conditions.…”
Section: Introductionmentioning
confidence: 99%