2016
DOI: 10.1016/j.advwatres.2016.07.019
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A general gridding, discretization, and coarsening methodology for modeling flow in porous formations with discrete geological features

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Cited by 129 publications
(59 citation statements)
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“…One important component of our approach is a local fine grid simulation, which is typical in many multiscale and numerical upscaling techniques. In general, a fine grid simulation involving flow and transport in heterogenous fracture media can be decomposed into two parts (we refer [24] for an overview). First of all, an unstructured fine mesh is needed to model the geometries of the fractures and background heterogeneities.…”
Section: Introductionmentioning
confidence: 99%
“…One important component of our approach is a local fine grid simulation, which is typical in many multiscale and numerical upscaling techniques. In general, a fine grid simulation involving flow and transport in heterogenous fracture media can be decomposed into two parts (we refer [24] for an overview). First of all, an unstructured fine mesh is needed to model the geometries of the fractures and background heterogeneities.…”
Section: Introductionmentioning
confidence: 99%
“…with | f | the face area, and x f a collocation point on f that allows for enforcing point-wise pressure continuity across the face in case of incompressible single-phase flow. In our implementation x f is selected as the intersection of the face and the line connecting the cell centroids x K and x L [94] as shown in Fig. A.1.…”
Section: Appendix a Tpfa Transmissibility Computationmentioning
confidence: 99%
“…We consider a case of two-continua at the (7)) c ∂ξ ∂t − div(κ∇ξ) = 0 in the RVE and impose ξ = 1 at the fracture nodes. One can also use a source term in the fracture or the local eigenvalue problems see [21]. It is assumed that zero Neumann boundary conditions are imposed on the rest of the boundaries.…”
Section: Rve-based Multi-continuum Computationsmentioning
confidence: 99%