Abstract
The use of the set of quasi-hydrodynamic equations for mathematical simulation of flows of a viscous heat-conducting compressible fluid in digital samples of rocks is considered. On the basis of a computation experiment, the permeability coefficient is determined.
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References
S. Succi, The Lattice Boltzmann Equation for Fluid Dynamics and Beyond (Clarendon Press, Oxford, 2001).
B. N. Chetverushkin, Kinetic Schemes and Quasi-GasDynamic Set of Equations (MAKS Press, Moscow, 2004) [in Russian].
T. G. Elizarova, Quasi-Gas-Dynamic Equations and Methods of Calculation of Viscous Flows (Nauchnyi mir, Moscow, 2007) [in Russian].
Yu. V. Sheretov, Dynamics of Continuums at Space–Time Averaging (Moscow, Izhevsk, 2009) [in Russian].
H. Dong and M. Blunt, Phys. Rev. E 80 (3), 036307–1 (2009).
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Original Russian Text © V.A. Balashov, E.B. Savenkov, 2016, published in Doklady Akademii Nauk, 2016, Vol. 467, No. 5, pp. 534–536.
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Balashov, V.A., Savenkov, E.B. Direct pore-scale flow simulation using quasi-hydrodynamic equations. Dokl. Phys. 61, 192–194 (2016). https://doi.org/10.1134/S1028335816040066
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DOI: https://doi.org/10.1134/S1028335816040066