Abstract
A diffuse-interface method for simulating wave fields in saturated elastic porous media is addressed. Wave processes are described by a hyperbolic system of first-order differential equations derived from the theory of thermodynamically consistent systems of conservation laws of continuum mechanics. This unified system of governing equations provides a universal way for the simulation of wave fields in rock samples with sharp interfaces between layers with different elastic/poroelastic petrophysical properties. A good qualitative agreement of numerical calculations with the classical theory of elasticity and Biot’s model is shown.
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Funding
The numerical experiment was supported by the Russian Foundation for Basic Research (project no. 19-01-00347 A), and the development of the theoretical model was supported by the Russian Science Foundation (project no. 19-77-20004).
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Translated by B. Shubik
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Reshetova, G.V., Romensky, E.I. Diffuse-Interface Simulation of Wave Fields in Porous Media. Dokl. Earth Sc. 497, 319–322 (2021). https://doi.org/10.1134/S1028334X21040139
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DOI: https://doi.org/10.1134/S1028334X21040139