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 …

We study the anelastic properties (attenuation and velocity dispersion) of surface waves at
an interface between a finite water layer and a porous medium described by Biot theory …

Understanding wave scattering in the earth is considered fundamental in describing seismic
wave propagation and providing information on structural features of the earth's interior …

The exploration and exploitation of shale oil is an important aspect in the oil industry.
Seismic properties and well‐log data are essential to establish wave‐propagation models …

Energy loss in porous media containing fluids is typically caused by a variety of dynamic
mechanisms. In the Biot theory, energy loss only includes the frictional dissipation between …

The wave-induced fluid flow (WIFF) is considered to be the main cause of dispersion and
attenuation of seismic waves in fluid-saturated porous media. Among numerous theories …

This study investigates the dynamic response of fractional poroviscoelastic layered media
subjected to a moving harmonic load. The material viscosity includes two parts: the flow …

Determining subsurface properties is of fundamental importance in exploration seismic
imaging. Poroelasticity theory provides an opportunity to extract quantitative fluid-and …

Considering the flow‐independent viscosity of soil skeleton and the lateral inertia effect of
pipe pile, the vertical dynamic behavior of a pipe pile embedded in unsaturated soil is …

The reflection and transmission problems of elastic waves through a partially saturated
porous interlayer sandwiched between two elastic solid half-spaces are investigated. The …