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On the Homogenization of Geological Fissured Systems With Curved non-periodic Cracks

Abstract

We analyze the steady fluid flow in a porous medium containing a network of thin fissures i.e. width O(ϵ)\mathcal{O}(\epsilon), where all the cracks are generated by the rigid translation of a continuous piecewise C1C^{1} functions in a fixed direction. The phenomenon is modeled in mixed variational formulation, using the stationary Darcy's law and setting coefficients of low resistance O(ϵ)\mathcal{O}(\epsilon) on the network. The singularities are removed performing asymptotic analysis as ϵ0\epsilon \rightarrow 0 which yields an analogous system hosting only tangential flow in the fissures. Finally the fissures are collapsed into two dimensional manifolds.Comment: 24 pages, 4 figure

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