2016
DOI: 10.48550/arxiv.1612.06594
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A Finite-Volume Discretization for Deformation of Fractured Media

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Cited by 3 publications
(5 citation statements)
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“…We use a recently developed cell-centered finite volume method, Multi-Point Stress Approximation (MPSA) [Keilegavlen and Nordbotten, 2017;Nordbotten, 2014], to approximate the solution of the linear momentum balance equation because it enables the use of the same data structure applied in the fluid flow discretization. MPSA enables the efficient inclusion of fractures by modeling them as internal boundary conditions, including fracture deformations in both the normal direction (change in the mechanical aperture) and the shear direction (caused by excess shear stress) [Ucar et al, 2016].…”
Section: Multi-physics Couplingmentioning
confidence: 99%
“…We use a recently developed cell-centered finite volume method, Multi-Point Stress Approximation (MPSA) [Keilegavlen and Nordbotten, 2017;Nordbotten, 2014], to approximate the solution of the linear momentum balance equation because it enables the use of the same data structure applied in the fluid flow discretization. MPSA enables the efficient inclusion of fractures by modeling them as internal boundary conditions, including fracture deformations in both the normal direction (change in the mechanical aperture) and the shear direction (caused by excess shear stress) [Ucar et al, 2016].…”
Section: Multi-physics Couplingmentioning
confidence: 99%
“…Future models might also include fracture roughness and solve the full equilibrium equations to estimate aperture changes that influence permeability. Recently, progress in this direction has been made using boundary element methods, multi-point stress approximations (MPSA) and the novel extended finite volume method (XFVM) (Norbeck et al, 2016;Ucar et al, 2016;Deb and Jenny, 2016). However, these models are not yet as computationally efficient as to allow an adaption for THERMAID.…”
Section: Discussionmentioning
confidence: 99%
“…In line with previous studies (Aagaard et al, 2013;Crouch & Starfield, 1982), the two surfaces of fracture are modeled as face pairs that have positive and negative sides. The face pairs are integrated as internal boundary conditions to the momentum balance equations, which are introduced in Section 2.3, by using the method developed by Ucar et al (2016). The discontinuity relations due to the fracture deformation (equation ( 2), (5), and ( 6)) are defined as 𝒖 + − 𝒖 − = ∆𝒖 𝑓 on 𝛤 where ∆𝒖 𝑓 = 𝒏 + (𝛥𝐸 𝑛,𝑟𝑒𝑣 + 𝛥𝐸 𝑛,𝑖𝑟𝑟𝑒𝑣 ) + 𝜻 + 𝛥𝑑 𝑠 .…”
Section: Mechanics Of Fracturesmentioning
confidence: 99%
“…Here, the primary variable, displacement, is defined at the face centers of the fracture faces as illustrated in Figure 2b. The details about the grid structure can be found in Ucar et al (2016). For illustration purposes, we show a gap between two red dots, but there is no gap between the duplicated faces and the face centers in the computational mesh.…”
Section: Grid Structurementioning
confidence: 99%
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