Seismic wave attenuation and dispersion resulting from wave-induced flow in porous rocks—A review

TM Müller, B Gurevich, M Lebedev - Geophysics, 2010 - library.seg.org
One major cause of elastic wave attenuation in heterogeneous porous media is wave-
induced flow of the pore fluid between heterogeneities of various scales. It is believed that …

Computational poroelasticity—A review

JM Carcione, C Morency, JE Santos - Geophysics, 2010 - library.seg.org
Computational physics has become an essential research and interpretation tool in many
fields. Particularly in reservoir geophysics, ultrasonic and seismic modeling in porous media …

Wave propagation in infinituple‐porosity media

L Zhang, J Ba, JM Carcione - Journal of Geophysical Research …, 2021 - Wiley Online Library
The fractal texture (or fabric) of porous media, which supports fluid flow at different scales, is
the main cause of wave anelasticity (dispersion and attenuation) on a wide range of …

Physics-informed neural networks for solving nonlinear diffusivity and Biot's equations

T Kadeethum, TM Jørgensen, HM Nick - PloS one, 2020 - journals.plos.org
This paper presents the potential of applying physics-informed neural networks for solving
nonlinear multiphysics problems, which are essential to many fields such as biomedical …

Physical laws meet machine intelligence: current developments and future directions

T Muther, AK Dahaghi, FI Syed, V Van Pham - Artificial Intelligence Review, 2023 - Springer
The advent of technology including big data has allowed machine learning technology to
strengthen its place in solving different science and engineering complex problems …

Quasi‐static finite element modeling of seismic attenuation and dispersion due to wave‐induced fluid flow in poroelastic media

B Quintal, H Steeb, M Frehner… - Journal of Geophysical …, 2011 - Wiley Online Library
The finite element method is used to solve Biot's equations of consolidation in the
displacement‐pressure (u− p) formulation. We compute one‐dimensional (1‐D) and two …

Generalized effective Biot theory and seismic wave propagation in anisotropic, poroviscoelastic media

X Huang, S Greenhalgh, L Han… - Journal of Geophysical …, 2022 - Wiley Online Library
The interior of the Earth is quite complex due to the actual geometrical structure and the
presence of complex rheological materials, including viscoelastic rocks, porous sediments …

A review of domain decomposition methods for simulation of fluid flows: concepts, algorithms, and applications

HS Tang, RD Haynes, G Houzeaux - Archives of Computational Methods …, 2021 - Springer
Abstract Domain decomposition (DD) is a powerful approach to numerically solve partial
differential equations, and it has become popular and indispensable in simulations of fluid …

Modeling of seismic wave scattering in poroelastic media

X Huang, T Sun, S Greenhalgh - Geophysics, 2024 - library.seg.org
Understanding wave scattering in the earth is considered fundamental in describing seismic
wave propagation and providing information on structural features of the earth's interior …

[HTML][HTML] 不分裂卷积完全匹配层与旋转交错网格有限差分在孔隙弹性介质模拟中的应用

张鲁新, 符力耘, 裴正林 - 地球物理学报, 2010 - html.rhhz.net
完全匹配层吸收边界在地震波模拟中已广泛使用, 但常用的场分裂格式完全匹配层吸收边界(
SPML) 和传统的不分裂完全匹配层吸收边界(NPML) 对极低频入射波或大角度入射波的边界 …