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• W2055804904 abstract "Fractures are relatively planar discontinuities in rocks induced by the huge internal stresses which are created by the slow but constant motions of the underground masses. Deposition of a single solute in a single fracture is addressed in the limit where the geometrical changes are very slow compared to the average fluid velocity. The deposition fluxes are calculated by means of a finite-difference scheme which is much more efficient than random walks. Examples of deterministic fractures, random but uncorreiated fractures, Gaussian and self-affine fractures are studied for four different values of the Peclet and the Peclet-Damkohler numbers. Some general trends are discussed." @default.
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• W2055804904 date "1996-06-01" @default.
• W2055804904 modified "2023-09-27" @default.
• W2055804904 title "DEPOSITION IN FRACTURES" @default.
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• W2055804904 doi "https://doi.org/10.1080/00986449608936530" @default.
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