Different forms of fluctuations of the terrestrial gravity field are observed by gravity
experiments. For example, atmospheric pressure fluctuations generate a gravity-noise …

A new indirect boundary integral equation method (IBIEM) is developed to solve the seismic
wave scattering problem in a three-dimensional fluid-saturated layered half-space. Based …

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 …

Multiple scattering effects due to a random distribution of identical spheres are investigated
in the general case of elastic or poroelastic host media, where both longitudinal and …

We studied seismic attenuation of P-and S-waves caused by the physical mechanism of
wave-induced fluid flow at the mesoscopic scale. Stress relaxation experiments were …

A method is suggested to express the effective bulk modulus of the solid frame of a
poroelastic material as a function of the saturated bulk modulus. This method enables …

The indirect boundary element method (IBEM) is extended to solve the scattering of elastic
waves by three-dimensional (3-D) subsurface irregularities in a fluid-saturated poroelastic …

Many media (such as geological formations or osseous tissues) are composites made up of
at least two basic materials which can themselves obey complex constitutive laws. Such …

A mathematical formulation is presented for the dynamic stress intensity factor (mode I) of a
permeable penny-shaped crack subjected to a time-harmonic propagating longitudinal …

Elastic wave propagation in porous media containing a movable fluid is frequently
accompanied by electromagnetic field generation. Such field can be produced, for instance …