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Article Dans Une Revue Geothermics Année : 2006

Flow channeling in a single fracture induced by shear displacement

Résumé

The effect on the transport properties of fractures of a relative shear displacement $\vec u$ of rough walls with complementary self-affine surfaces has been studied experimentally and numerically. The shear displacement $\vec u$ induces an anisotropy of the aperture field with a correlation length scaling as $u$ and significantly larger in the direction perpendicular to $\vec u$. This reflects the appearance of long range channels perpendicular to $\vec u$ resulting in a higher effective permeability for flow in the direction perpendicular to the shear. Miscible displacements fronts in such fractures are observed experimentally to display a self affine geometry of characteristic exponent directly related to that of the rough wall surfaces. A simple model based on the channelization of the aperture field allows to reproduces the front geometry when the mean flow is parallel to the channels created by the shear displacement.
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Dates et versions

hal-00020184 , version 1 (08-03-2006)
hal-00020184 , version 2 (28-08-2006)

Identifiants

Citer

Harold Auradou, German Drazer, Alejandro Boschan, Jean-Pierre Hulin, Joel Koplik. Flow channeling in a single fracture induced by shear displacement. Geothermics, 2006, 35, pp.576--588. ⟨10.1016/j.geothermics.2006.11.004⟩. ⟨hal-00020184v2⟩
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