4.6 Article

Reflection and Transmission of Inhomogeneous Plane Waves in Thermoelastic Media

Journal

FRONTIERS IN EARTH SCIENCE
Volume 10, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2022.850331

Keywords

thermoelasticity and elasticity; reflection and transmission coefficients; energy partitions; inhomogeneous plane waves; attenuation angle

Funding

  1. National Natural Science Foundation of China [41821002]
  2. 111 project Deep-Superdeep Oil & Gas Geophysical Exploration [B18055]
  3. Innovation fund project for graduate students of China University of Petroleum (East China) [CXJJ2022-17]

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This study investigates the reflection and transmission coefficients of plane waves incident on an interface between two thermoelastic half spaces and compares them with the elastic case. The results show that the thermoelastic and elastic models predict different energy partitions and energy flux directions.
We study the reflection and transmission coefficients of plane waves incident at an interface between two isotropic thermoelastic half spaces and compare them with those of the elastic case. The models include the classical-Biot (B) and extended Lord-Shulman (LS) theories, and predict reflected and transmitted fast-compressional (P), thermal (T) and shear (S) waves. The coefficients are formulated in terms of incidence and inhomogeneity angles, medium properties and potential functions. We consider different incident wave types and inhomogeneity angles to analyze the magnitude, phase and energy ratio of the plane waves, and perform a comparison with the isothermal (elastic) theory. The thermoelastic and elastic models predict different energy partitions between the P and S modes, satisfying the conservation of energy. The LS model exhibits higher T-wave thermal attenuation with increasing inhomogeneity angle at high frequencies, accordingly predicting more interference energy. The angle affects the energy partitions, particularly at the critical angle and near grazing incidence for an incident P wave, which satisfies the conservation of energy. Beyond the critical angle, the energy flux perpendicular to the interface of the isothermal model vanishes, while it is significant in the thermoelastic case. The T-wave magnitudes increase when the thermal conductivity (relaxation time) increases.

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