We establish a generalization of the thermoelasticity wave equation to the porous case, including the Lord–Shulman (LS) and Green–Lindsay (GL) theories that involve a set of relaxation times (τi,i=1,…,4). The dynamical equations predict four propagation modes, namely, a fast P wave, a Biot slow wave, a thermal wave, and a shear wave. The plane-wave analysis shows that the GL theory predicts a higher attenuation of the fast P wave, and consequently a higher velocity dispersion than the LS theory if τ1= τ2> τ3, whereas both models predict the same anelasticity for τ1= τ2= τ3. We also propose a generalization of the LS theory by applying two different Maxwell–Vernotte–Cattaneo relaxation times related to the temperature increment (τ3) and solid/fluid strain components (τ4), respectively. The generalization predicts positive quality factors when τ4≥ τ3, and increasing τ4 further enhances the attenuation. The wavefields are computed with a direct meshing algorithm using the Fourier pseudosp...

Generalized Thermo-poroelasticity Equations and Wave Simulation

Carcione J. M.;
2021-01-01

Abstract

We establish a generalization of the thermoelasticity wave equation to the porous case, including the Lord–Shulman (LS) and Green–Lindsay (GL) theories that involve a set of relaxation times (τi,i=1,…,4). The dynamical equations predict four propagation modes, namely, a fast P wave, a Biot slow wave, a thermal wave, and a shear wave. The plane-wave analysis shows that the GL theory predicts a higher attenuation of the fast P wave, and consequently a higher velocity dispersion than the LS theory if τ1= τ2> τ3, whereas both models predict the same anelasticity for τ1= τ2= τ3. We also propose a generalization of the LS theory by applying two different Maxwell–Vernotte–Cattaneo relaxation times related to the temperature increment (τ3) and solid/fluid strain components (τ4), respectively. The generalization predicts positive quality factors when τ4≥ τ3, and increasing τ4 further enhances the attenuation. The wavefields are computed with a direct meshing algorithm using the Fourier pseudosp...
2021
Fourier pseudospectral method; Poroelasticity; Simulation; Thermoelasticity; Waves;
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14083/42527
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