SOLUTE TRANSPORT IN A SINGLE FRACTURE WITH NEGLIGIBLE MATRIX PERMEABILITY: 2. MATHEMATICAL FORMALISM

dc.contributor.author	Bodin J.
dc.contributor.author	Delay F.
dc.contributor.author	de Marsily G.
dc.date.accessioned	2022-02-03T04:39:26Z
dc.date.available	2022-02-03T04:39:26Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=13774830
dc.identifier.citation	Hydrogeology Journal, 2003, 11, 4, 434-454
dc.identifier.issn	1431-2174
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34891
dc.description.abstract	This report provides an overview of the mathematical expressions for modeling fundamental solute transport mechanisms at the fracture scale. It focuses on low-permeability rocks where advection in the matrix is negligible as compared to that in fractures. The following processes are considered: (1) advective transport in fractures, (2) hydrodynamic dispersion along the fracture axis, (3) molecular diffusion from the fracture to the porous matrix, (4) sorption reactions on the fracture walls and within the matrix, and (5) decay reactions. The aim of this review is to gather in a single article the transport equations and their analytical solutions, using a homogeneous notation to facilitate comparison and exploitation.
dc.subject	Fractured rocks
dc.subject	Mathematical formalism
dc.subject	Solute transport
dc.subject	Topical review
dc.title	SOLUTE TRANSPORT IN A SINGLE FRACTURE WITH NEGLIGIBLE MATRIX PERMEABILITY: 2. MATHEMATICAL FORMALISM
dc.type	Статья

Files in this item

Name: Bodi_03.pdf

Size: 354.3Kb

Format: PDF