Abstract The seismic reflection and transmission characteristics of a single layer sandwiched between two dissimilar poroelastic solids saturated with two immiscible viscous fluids are investigated. The sandwiched layer is modeled as a porous solid with finite thickness. The propagation of waves is represented with potential functions. The displacements of particles in different phases of the aggregate are defined in terms of these potential functions. Due to the presence of viscosity in pore fluids, the reflected and transmitted waves are inhomogeneous in nature, i.e., with different directions of propagation and attenuation. The closed-form analytical expressions for reflection and transmission coefficients are derived theoretically for a...
International audienceWave propagation in macroscopically inhomogeneous porous materials has receive...
AbstractWave propagation in a porous elastic medium saturated by two immiscible fluids is investigat...
The characteristics of the seismic P-wave reflection coefficient can depend on the properties of the...
Wave propagation in poroelastic media is a subject that finds applications in many fields of researc...
The deformation of poroelastic saturated media due to passing seismic waves results in coupled solid...
Wave propagation in saturated porous media involves complicated couplings between the solid skeleton...
Abstract The phenomenon of reflection and refraction is studied at the welded interface between two ...
The reflection and refraction of inhomogeneous waves at the boundary between two linear viscoelastic...
The underground rock is composed of rock skeleton and pore fluids. When seismic waves propagate in u...
© The Author(s) 2010. This article is published with open access at Springerlink.com Abstract Analys...
Analysis of compression wave propagation in a poroelastic medium predicts a peak of reflection from ...
Analysis of compression wave propagation in a poroelastic medium predicts a peak of reflection from ...
Using Biot’s poroelasticity theory, we derive expressions for the reflection and transmission coeffi...
Analysis of compression wave propagation through a high-permeability layer in a homogeneous poroelas...
Using Biot’s poroelasticity theory, we derive expressions for the reflection and transmission coeffi...
International audienceWave propagation in macroscopically inhomogeneous porous materials has receive...
AbstractWave propagation in a porous elastic medium saturated by two immiscible fluids is investigat...
The characteristics of the seismic P-wave reflection coefficient can depend on the properties of the...
Wave propagation in poroelastic media is a subject that finds applications in many fields of researc...
The deformation of poroelastic saturated media due to passing seismic waves results in coupled solid...
Wave propagation in saturated porous media involves complicated couplings between the solid skeleton...
Abstract The phenomenon of reflection and refraction is studied at the welded interface between two ...
The reflection and refraction of inhomogeneous waves at the boundary between two linear viscoelastic...
The underground rock is composed of rock skeleton and pore fluids. When seismic waves propagate in u...
© The Author(s) 2010. This article is published with open access at Springerlink.com Abstract Analys...
Analysis of compression wave propagation in a poroelastic medium predicts a peak of reflection from ...
Analysis of compression wave propagation in a poroelastic medium predicts a peak of reflection from ...
Using Biot’s poroelasticity theory, we derive expressions for the reflection and transmission coeffi...
Analysis of compression wave propagation through a high-permeability layer in a homogeneous poroelas...
Using Biot’s poroelasticity theory, we derive expressions for the reflection and transmission coeffi...
International audienceWave propagation in macroscopically inhomogeneous porous materials has receive...
AbstractWave propagation in a porous elastic medium saturated by two immiscible fluids is investigat...
The characteristics of the seismic P-wave reflection coefficient can depend on the properties of the...