White's model for wave propagation in partially saturated rocks: Comparison with poroelastic numerical experiments

By José M. Carcione, H. B. Helle, N. H. Pham. 2003

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Quasi-static finite element modeling of seismic attenuation and dispersion due to wave-induced fluid flow in poroelastic media (2011, methodology): “However, calculating seismic attenuation due to wave‐induced fluid flow with numerical algorithms for wave propagation in poroelastic media is computationally inefficient because wave propagation, fluid flow, and the diffusive fluid pressure response occur on significantly different time scales [e.g”
Biot-Rayleigh theory of wave propagation in double-porosity media (2011, methodology): “The generalization of these differential equations to the variable porosity case is given by Carcione et al. [2003] , by using the analogy with the two‐phase case and the complementary energy theorem.”