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

We establish a generalization of the thermoelasticity wave equation to the porous case,
including the Lord–Shulman (LS) and Green–Lindsay (GL) theories that involve a set of …

We develop a numerical algorithm for simulation of wave propagation in linear
nonisothermal poroelastic media, based on Biot theory and a generalized Fourier law of …

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 …

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

SUMMARY The Lord–Shulman thermoelasticity theory combined with Biot equations of
poroelasticity, describes wave dissipation due to fluid and heat flow. This theory avoids an …

We have developed continuous and discrete-time finite-element (FE) methods to solve an
initial boundary-value problem for the thermo-poroelasticity wave equation based on the …

Thermoelastic attenuation is similar to wave-induced fluid-flow attenuation (mesoscopic
loss) due to conversion of the fast P wave to the slow (Biot) P mode. In the thermoelastic …

Insights into wave propagation in prestressed porous media are important in geophysical
applications, such as monitoring changes in geo-pressure. This can be addressed by poro …

A multi-scale variational-asymptotic homogenization method for periodic microstructured
materials in presence of thermoelasticity with periodic spatially dependent one relaxation …