Canonical analytical solutions of wave-induced thermoelastic attenuation

Author:

Carcione José M12,Gei Davide1,Santos Juan E234,Fu Li-Yun5,Ba Jing2

Affiliation:

1. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42c, Sgonico 34010, Trieste, Italy

2. School of Earth Sciences and Engineering, Hohai University, Nanjing 210023, China

3. Facultad de Ingenieria, Instituto del Gas y del Petróleo, Universidad de Buenos Aires, Av. Las Heras 2214, Piso 3, Buenos Aires C1127AAR, Argentina

4. Department of Mathematics, Purdue University, 150 N. University Street, West Lafayette, IN 47907-2067, USA

5. School of Geosciences, China University of Petroleum (East China), Qingdao 266580, China

Abstract

SUMMARY Thermoelastic attenuation is similar to wave-induced fluid-flow attenuation (mesoscopic loss) due to conversion of the fast P wave to the slow (Biot) P mode. In the thermoelastic case, the P- and S-wave energies are lost because of thermal diffusion. The thermal mode is diffusive at low frequencies and wave-like at high frequencies, in the same manner as the Biot slow mode. Therefore, at low frequencies, that is, neglecting the inertial terms, a mathematical analogy can be established between the diffusion equations in poroelasticity and thermoelasticity. We study thermoelastic dissipation for spherical and cylindrical cavities (or pores) in 2-D and 3-D, respectively, and a finely layered system, where, in the latter case, only the Grüneisen ratio is allowed to vary. The results show typical quality-factor relaxation curves similar to Zener peaks. There is no dissipation when the radius of the pores tends to zero and the layers have the same properties. Although idealized, these canonical solutions are useful to study the physics of thermoelasticity and test numerical algorithm codes that simulate thermoelastic dissipation.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference31 articles.

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