Third‐Order Padé Thermoelastic Constants of Solid Rocks

Classical third‐order thermoelastic constants are generally derived from the theory of small‐amplitude acoustic waves in isotropic materials during heat treatments. Investigating higher‐order thermoelastic constants for higher temperatures is challenging owing to the involvement of the number of unk...

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Veröffentlicht in:	Journal of geophysical research. Solid earth 2022-09, Vol.127 (9), p.n/a
Hauptverfasser:	Yang, Jian, Fu, Li‐Yun, Fu, Bo‐Ye, Deng, Wubing, Han, Tongcheng
Format:	Artikel
Sprache:	eng
Schlagworte:	Accuracy Acoustic waves Approximation Coefficients Constants Crystals Deformation Elastic waves Free energy Geophysics Heat treatment Heat treatments High temperature Isotropic material Isotropic materials Lithology Low temperature Mathematical models Microcracks Modelling Olivine Pade approximation Parameters Physics Polycrystals Predictions Rational functions Rocks Sandstone Sedimentary rocks Shale Sound waves Taylor series Temperature Temperature dependence Thermal expansion Thermal strain Thermoelasticity Ultrasonic methods Velocity
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