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- W1966592244 abstract "The established codes for modelling the re-saturation of compacted bentonite are based on the assumption that the hydraulic processes can be described as a two-phase flow of liquid water and air. Some models additionally take vapour flow into account. Recent investigations suggest, though, that compacted bentonite in contact with liquid water does not re-saturate via the liquid water phase but exclusively by evaporation in the pore space and subsequent vapour diffusion. The present paper adds further evidence to support this hypothesis. Under certain conditions a balance equation for the water vapour in the bentonite can be transformed into the well-known Fickian approach that has been empirically derived from observations of uptake experiments with liquid water. This transformed balance equation allows to interpret the so-called “diffusion coefficient” as a product of several simple physical parameters. An exemplary set of parameters for compacted MX-80 bentonite yields a value that lies within the narrow band of empirically determined “diffusion coefficients”." @default.
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- W1966592244 date "2005-12-01" @default.
- W1966592244 modified "2023-09-27" @default.
- W1966592244 title "New evidence for the dominance of vapour diffusion during the re-saturation of compacted bentonite" @default.
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- W1966592244 doi "https://doi.org/10.1016/j.enggeo.2005.09.015" @default.
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