The effect of stress on wave propagation in fluid-saturated porous thermoelastic media is
poorly understood. To fill this gap, we propose the dynamical equations for stressed fluid …

We study the reflection and transmission (R/T) characteristics of inhomogeneous plane
waves at the interface between two dissimilar fluid-saturated thermoporoelastic media at …

Classical third‐order thermoelastic constants are generally derived from the theory of small‐
amplitude acoustic waves in isotropic materials during heat treatments. Investigating higher …

Seismic AVO has a significant potential for fluid identification in time-lapse monitoring of the
cyclic recovery of geothermal reservoirs. With this goal, we develop an AVO method based …

The stress field and thermal field are usually coupled in the Earth's subsurface. The
mechanism of the joint effects of stress and thermal fields on wave propagation in rocks is …

The fluid-saturated porous layered (FSPL) media widely exist in the Earth's subsurface and
their overall mechanical properties, microscopic pore structure and wave propagation …

SUMMARY A mixture theory is employed to analyse the reflection behaviour of a
homogeneous plane-P 1-wave at the boundary of an unsaturated porothermoelastic …

Understanding the mechanisms of wave-induced fluid flow in the pore space combined with
attenuation and dispersion measurements may be used to estimate rock hydraulic …

We present and analyze a high-order discontinuous Galerkin method for the space
discretization of the wave propagation model in thermo-poroelastic media. The proposed …

Thermoelasticity extends the classical elastic theory by coupling the fields of particle
displacement and temperature. The classical theory of thermoelasticity, based on a …