Propagation of the slow Biot wave is investigated within the low-frequency range. For the first time it is proven theoretically that longitudinal wave of the second kind is not propagatory if its wave number is lower than some critical value. This critical wave number is a bifurcation point, above which longitudinal wave of the second kind becomes to be propagatory. Asymptotical formulae for phase velocity and attenuation of P2 wave are derived
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
Existence and propagation of the surface waves at a free interface of a saturated porous medium are ...
Asymptotic behavior of the Biot slow wave is investigated. Formulae for short- and long-wave approxi...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
The paper contains the analysis of the propagation of acoustic waves in two-component poroelastic me...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
Spatial heterogeneity of hydrocarbon reservoirs causes significant attenuation and dispersion of sei...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
We present a derivation of the equations describing wave propagation in porous media based upon an a...
Acoustic wave propagation in porous media is formulated according to the Biot theory. The theory is ...
International audienceThis paper deals with the numerical modeling of wave propagation in porous med...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
Existence and propagation of the surface waves at a free interface of a saturated porous medium are ...
Asymptotic behavior of the Biot slow wave is investigated. Formulae for short- and long-wave approxi...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
The paper contains the analysis of the propagation of acoustic waves in two-component poroelastic me...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
Spatial heterogeneity of hydrocarbon reservoirs causes significant attenuation and dispersion of sei...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
We present a derivation of the equations describing wave propagation in porous media based upon an a...
Acoustic wave propagation in porous media is formulated according to the Biot theory. The theory is ...
International audienceThis paper deals with the numerical modeling of wave propagation in porous med...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...
International audienceAs originally described by Biot in 1956, seismic propagation in fluid-filled p...