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Finite-difference method Stokes solver (FDMSS) for 3D pore geometries: Software development, validation and case studies

delete2018-05-01
delete63
PRE
AI
K
Kirill M. Gerke *
R
Roman Vasilyev
K
Khirevich, Siarhei
D
Daniel Collins
M
Marina V. Karsanina
T
Timofey O. Sizonenko
Д
Д. В. Корост
S
Sébastien Lamontagne
D
Dirk Mallants
DOI:10.1016/j.cageo.2018.01.005delete
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Abstract

Abstract

En 中文
Permeability is one of the fundamental properties of porous media and is required for large-scale Darcian fluid flow and mass transport models. Whilst permeability can be measured directly at a range of scales, there are increasing opportunities to evaluate permeability from pore-scale fluid flow simulations. We introduce the free software Finite-Difference Method Stokes Solver (FDMSS) that solves Stokes equation using a finite-difference method (FDM) directly on voxelized 3D pore geometries (i.e. without meshing). Based on explicit convergence studies, validation on sphere packings with analytically known permeabilities, and comparison against lattice Boltzmann and other published FDM studies, we conclude that FDMSS provides a computationally efficient and accurate basis for single-phase pore-scale flow simulations. By implementing an efficient parallelization and code optimization scheme, permeability inferences can now be made from 3D images of up to 10(9) voxels using modem desktop computers. Case studies demonstrate the broad applicability of the FDMSS software for both natural and artificial porous media.
Keywords:
Pore-scale modelling
Stokes flow solver
X-ray micro-tomography (XMT)
Velocity field
Pressure field
REV analysis
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Journal

C
Computers and Geosciences
IF:
4.4
Papers:
5.0K
Citations:
1.5W

Organization

K
king abdullah university of science & technology
Scholars:
1.3W
Papers: 1.3W
Citations: 32
L
lomonosov moscow state university
Scholars:
2.1W
Papers: 1.5W
Citations: 19
R
russian academy of sciences
Scholars:
9.1W
Papers: 6.0W
Citations: 60
D
Dokuchaev Soil Science Institute
Scholars:
239
Papers: 131
Citations: 0
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