One major cause of elastic wave attenuation in heterogeneous porous media is wave-
induced flow of the pore fluid between heterogeneities of various scales. It is believed that …

Seismic fluid identification works as an effective approach to characterize the fluid feature
and distribution of the reservoir underground with seismic data. Rock physics which builds …

Physiological mechano-acoustic signals, often with frequencies and intensities that are
beyond those associated with the audible range, provide information of great clinical utility …

The fractal texture (or fabric) of porous media, which supports fluid flow at different scales, is
the main cause of wave anelasticity (dispersion and attenuation) on a wide range of …

A major cause of seismic attenuation in fluid-saturated rocks is the flow of the pore fluid
induced by the passing wave. At sonic and ultrasonic frequencies, attenuation appears to be …

The effect of pore fluids on seismic wave attenuation in carbonate rocks is important for
interpreting remote sensing observations of carbonate reservoirs undergoing enhanced oil …

The finite element method is used to solve Biot's equations of consolidation in the
displacement‐pressure (u− p) formulation. We compute one‐dimensional (1‐D) and two …

Different theoretical and laboratory studies on the propagation of elastic waves in real rocks
have shown that the presence of heterogeneities larger than the pore size but smaller than …

Saturation of porous rocks with a mixture of two fluids (known as partial saturation) has a
substantial effect on the seismic waves propagating through these rocks. In particular, partial …

Saturation of porous rocks with a mixture of two fluids has a substantial effect on seismic‐
wave propagation. In particular, partial saturation causes significant attenuation and …