UPSCALING OF CONSTITUTIVE RELATIONS IN UNSATURATED HETEROGENEOUS TUFF MATRIX

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dc.contributor.author Liu H.H.
dc.contributor.author Bodvarsson G.S.
dc.date.accessioned 2022-01-23T03:37:38Z
dc.date.available 2022-01-23T03:37:38Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=1481989
dc.identifier.citation Journal of Hydrology, 2003, 276, 1-4, 198-209
dc.identifier.issn 0022-1694
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/34523
dc.description.abstract When numerical models are used for modeling large-scale flow and transport processes in the subsurface, upscaling is generally needed to determine large-scale hydraulic properties from small-scale measurements. This study is focused on the upscaling of constitutive relations (among relative permeability, capillary pressure, and saturation) for unsaturated tuff matrix (or a porous medium with a large air entry value). Unsaturated flow in tuff matrix is of interest at a number of existing and proposed waste disposal sites, as well as in connection with environmental contamination in arid and semiarid regions. Based on the notion that a large air entry value corresponds to a spatially uniform capillary pressure distribution, even at a relatively large scale for steady-state unsaturated flow, we present an upscaling approach for constitutive relations of tuff matrix. Numerical experiments were used to verify and demonstrate the usefulness of the approach.
dc.subject UNSATURATED FLOW
dc.subject YUCCA MOUNTAIN
dc.subject VADOSE ZONE HYDROLOGY
dc.subject RELATIVE PERMEABILITY
dc.title UPSCALING OF CONSTITUTIVE RELATIONS IN UNSATURATED HETEROGENEOUS TUFF MATRIX
dc.type Статья


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