Numerical simulation of the seismic wave propagation and fluid pressure in complex porous media at the mesoscopic scale
DOI10.1080/17455030.2019.1577584OpenAlexW2917895614WikidataQ128340161 ScholiaQ128340161MaRDI QIDQ5885261
Unnamed Author, Tingting Liu, Liguo Han
Publication date: 3 April 2023
Published in: Waves in Random and Complex Media (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1080/17455030.2019.1577584
Fourier transformfinite element methodphase velocityDarcy lawBiot theorycracked mediumhigh-order staggered-grid finite difference methodinverse attenuation factor
Bulk waves in solid mechanics (74J10) Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Finite element methods applied to problems in solid mechanics (74S05) Flows in porous media; filtration; seepage (76S05) Seismology (including tsunami modeling), earthquakes (86A15) Finite difference methods applied to problems in solid mechanics (74S20) Geophysical solid mechanics (74L05)
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Cites Work
- Coupled method of finite and dynamic infinite elements for simulating wave propagation in elastic solids involving infinite domains
- Inversely-mapped analytical solutions for flow patterns around and within inclined elliptic inclusions in fluid-saturated rocks
- Convective and advective heat transfer in geological systems
- Dynamic and transient infinite elements. Theory and geophysical, geotechnical and geoenvironmental applications
- Mapped transient infinite elements for heat transfer problems in infinite media
- Numerical simulation of double-diffusion driven convective flow and rock alteration in three-dimensional fluid-saturated geological fault zones
- Analytical solutions for pore-fluid flow focusing within inclined elliptic inclusions in pore-fluid-saturated porous rocks: Solutions derived in an elliptical coordinate system
- Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below
- Fundamentals of computational geoscience. Numerical methods and algorithms
- Theoretical analyses of nonaqueous phase liquid dissolution-induced instability in two-dimensional fluid-saturated porous media
- Theoretical and numerical analyses of chemical-dissolution front instability in fluid-saturated porous rocks
- Computational simulation of chemical dissolution-front instability in fluid-saturated porous media under non-isothermal conditions
- Mechanics of Deformation and Acoustic Propagation in Porous Media
- Overall properties of a cracked solid
- A numerical model for wave scattering problems in infinite media due to p- and sv-wave incidences
- Incident P and SV wave scattering effects under different canyon topographic and geological conditions
- A dynamic infinite element for three‐dimensional infinite‐domain wave problems
- Transient infinite elements for seepage problems in infinite media
- Transient infinite elements for contaminant transport problems
- Numerical modelling of transient contaminant migration problems in infinite porous fractured media using finite/infinite element technique. Part I: Theory
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