2017
DOI: 10.1002/nag.2673
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The intrinsic permeability of microcracks in porous solids: Analytical models and Lattice Boltzmann simulations

Abstract: The paper presents a synthesis of analytical modeling and computational simulations of the intrinsic permeability of microcracks, embedded in porous materials taking into account the interaction of the fluid flow in the microcrack with the surrounding porous material. In the first part of the paper, using the DARCY, STOKES, BRINKMAN, and the BEAVERS-JOSEPH approximations, we derive the intrinsic permeability of a plain non-rough microcrack in terms of the microcrack geometry and the permeability of the porous … Show more

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Cited by 9 publications
(5 citation statements)
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“…The hydromechanical coupling takes place at the midpoint of a common edge of two adjacent Voronoi polygons (point C in Figure 2A), at which both mechanical and transport responses are available. The discrete formulation of a 1D lattice element is in the sense of 1D classical FEM, which is different from other lattice formulations, for instance, the lattice spring model 49 and lattice discrete particle model 50 …”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The hydromechanical coupling takes place at the midpoint of a common edge of two adjacent Voronoi polygons (point C in Figure 2A), at which both mechanical and transport responses are available. The discrete formulation of a 1D lattice element is in the sense of 1D classical FEM, which is different from other lattice formulations, for instance, the lattice spring model 49 and lattice discrete particle model 50 …”
Section: Methodsmentioning
confidence: 99%
“…The discrete formulation of a 1D lattice element is in the sense of 1D classical FEM, which is different from other lattice formulations, for instance, the lattice spring model 49 and lattice discrete particle model. 50…”
Section: Hydromechanical Lattice Modelmentioning
confidence: 99%
“…Proceeding with the same deformed granular assemblies (3D images extracted from the DEM RVE) as used for retention curve database generation in Section 3.2, LB single‐phase flow simulation is applied to generate the database of the pore‐fluid flow 89–97 . This database will then be used for the ANN‐based intrinsic permeability tensor estimation.…”
Section: Retention Behavior and Anisotropic Darcy Flow Representation In MLmentioning
confidence: 99%
“…Numerous studies have been conducted to link theories and soil experiments to gain further knowledge on the Forchheimer formula for non-Darcy flows [8,22,[34][35][36]42]. However, the nature of geomaterials has prevented ideal conditioning and observation and has hindered the systematic construction of relationships between material properties and permeability.…”
Section: Introductionmentioning
confidence: 99%