A few remarks on Biot's model and linear acoustics of poroelastic saturated materials
K Wilmanski - Soil Dynamics and Earthquake Engineering, 2006 - Elsevier
This review article consists of two parts. The first part concerns the admissibility of four
contributions characteristic for Biot's model of poroelastic materials: coupling of partial …
contributions characteristic for Biot's model of poroelastic materials: coupling of partial …
Analysis of the propagation of sound waves in partially saturated soils by means of a macroscopic linear poroelastic model
B Albers - Transport in porous media, 2009 - Springer
In this paper, the propagation of sound waves in partially saturated soils is investigated. A
macroscopic linear model that is based on the two-component model of Biot and on the …
macroscopic linear model that is based on the two-component model of Biot and on the …
Nonlocal scale effect on Rayleigh wave propagation in porous fluid-saturated materials
In this paper, a Rayleigh wave model in fluid saturated porous materials based on a
nonlocal Biot theory is proposed. The general characteristic equations expressed in terms of …
nonlocal Biot theory is proposed. The general characteristic equations expressed in terms of …
Analysis of dispersion and attenuation of surface waves in poroelastic media in the exploration-seismic frequency band
We analyse dispersion and attenuation of surface waves at free surfaces of possible
vacuum/poroelastic media: permeable-'open pore', impermeable-'closed pore'and partially …
vacuum/poroelastic media: permeable-'open pore', impermeable-'closed pore'and partially …
Wave fields and spectra of Rayleigh waves in poroelastic media in the exploration seismic frequency band
A better understanding of the influences of different surface fluid drainage conditions on the
propagation and attenuation of surface waves as the stipulated frequency is varied is a key …
propagation and attenuation of surface waves as the stipulated frequency is varied is a key …
Low-frequency Stoneley wave propagation at the interface of two porous half-spaces
MG Markov - Geophysical Journal International, 2009 - academic.oup.com
Summary The Frenkel-Biot theory is used to study a propagation of Stoneley elastic wave at
the boundary of two fluid-saturated porous media. The velocity and attenuation of the …
the boundary of two fluid-saturated porous media. The velocity and attenuation of the …
[HTML][HTML] 含流体孔隙介质中面波的传播特性及应用
张煜, 徐义贤, 夏江海, 张双喜, 平萍 - 地球物理学报, 2015 - dzkx.org
基于单相介质中地震波理论的高频面波法已广泛应用于求取浅地表S 波的速度.
然而水文地质条件表明, 普遍的浅地表地球介质富含孔隙. 孔隙中充填的流体会显著地影响面波 …
然而水文地质条件表明, 普遍的浅地表地球介质富含孔隙. 孔隙中充填的流体会显著地影响面波 …
The diffraction of Rayleigh waves by a fluid-saturated alluvial valley in a poroelastic half-space modeled by MFS
Two dimensional diffraction of Rayleigh waves by a fluid-saturated poroelastic alluvial valley
of arbitrary shape in a poroelastic half-space is investigated using the method of …
of arbitrary shape in a poroelastic half-space is investigated using the method of …
Time harmonic point load and dynamic contact problem of contacting fluid and poroelastic half-spaces
R He, L Wang, HY Yu - Soil Dynamics and Earthquake Engineering, 2012 - Elsevier
The dynamic response of contacting fluid and fluid-saturated poroelastic half-spaces to a
time-harmonic vertical point force or a point pore pressure is investigated. The solutions are …
time-harmonic vertical point force or a point pore pressure is investigated. The solutions are …
Influence of coupling through porosity changes on the propagation of acoustic waves in linear poroelastic materials
B Albers, K Wilmański - Archives of Mechanics, 2006 - am.ippt.gov.pl
In earlier works it has been shown that linearization of thermodynamical models of
poroelastic materials yields a contribution to stresses in the form βΔ n, Δ n:= nn E, where n is …
poroelastic materials yields a contribution to stresses in the form βΔ n, Δ n:= nn E, where n is …