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 …

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 …

利用高阶交错网格有限差分法模拟地震波在非均匀孔隙介质中的传播

王秀明 - 地球物理学报, 2003 - dzkx.org
烃类储集层是一种复合多相介质, 在固体颗粒的空隙中含有气体或液体. 研究弹性波在该类地层
中的传播规律对于油气勘探开发, 特别对于全波列声波测井有重要意义. 为了提高孔隙弹性介质 …

Discontinuous Galerkin methods for wave propagation in poroelastic media

J De La Puente, M Dumbser, M Käser, H Igel - Geophysics, 2008 - library.seg.org
We have developed a new numerical method to solve the heterogeneous poroelastic wave
equations in bounded three-dimensional domains. This method is a discontinuous Galerkin …

Some aspects of the physics and numerical modeling of Biot compressional waves

JM Carcione, G Quiroga-Goode - Journal of Computational …, 1995 - World Scientific
We investigate the problem of wave propagation in a porous medium, in the framework of
Biot's theory, computing the numerical solution of the differential equations by a grid method …

Finite difference modeling of Biot's poroelastic equations at seismic frequencies

YJ Masson, SR Pride, KT Nihei - Journal of Geophysical …, 2006 - Wiley Online Library
Across the seismic band of frequencies (loosely defined as< 10 kHz), a seismic wave
propagating through a porous material will create flow in the pore space that is laminar; that …

Finite-difference modeling of Biot's poroelastic equations across all frequencies

YJ Masson, SR Pride - Geophysics, 2010 - library.seg.org
An explicit time-stepping finite-difference scheme is presented for solving Biot's equations of
poroelasticity across the entire band of frequencies. In the general case for which viscous …

完全匹配层吸收边界在孔隙介质弹性波模拟中的应用

赵海波, 王秀明, 王东, 陈浩 - 地球物理学报, 2007 - dzkx.org
模拟弹性波在孔隙介质中传播, 需要稳定有效的吸收边界来消除或尽可能的减小由人工边界引起
的虚假反射. 本文在前人工作基础上, 首次建立了弹性孔隙介质情况下完全匹配层吸收边界的高 …

Stress Relaxing Simulation on Digital Rock: Characterize Attenuation Due To Wave‐Induced Fluid Flow and Scattering

W Zhu, L Zhao, Z Yang, H Cao, Y Wang… - Journal of …, 2023 - Wiley Online Library
Digital rock physics (DRP) is essential to understand the wave elastic and attenuation
characteristics of complex porous rocks, offering insights into interpreting seismic and sonic …