Abstract
This study considers the propagation of harmonic plane waves in general anisotropic dissipative media. This propagation is governed by a complex slowness vector, which is resolved into a propagation vector and an attenuation vector. The attenuation part is decomposed into homogeneous attenuation and evanescent attenuation. This makes a generalised specification of slowness vector to represent (in)homogeneous propagation in (an)isotropic (an)elastic media. This specification applies to incident waves, scattered waves as well as surface/interface waves at the plane boundary of the medium. With the choice of involved parameters, this specification can represent the corresponding wave-fields in the absence of anisotropy and/or dissipation. This specification has been used to formulate a corrected procedure for the reflection of plane waves in a transversely isotropic piezothermoelastic medium.
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Appendices
Appendix A: Phase velocities
Consider a general anisotropic medium represented by elastic tensor \(c_{ijkl}\), and density \(\rho\). The Christoffel equations (3) govern the harmonic propagation of bulk waves, for \({\textbf{p}}={\textbf{N}}/V,~{\textbf{N}}\cdot {\textbf{N}}=1.\) The resulting characteristic equation (\(\det \{c_{ijkl}N_jN_l-\rho V^2\delta _{ik}\}=0\)) is solved into a cubic equation, given by
Roots of this cubic equation define the velocities (\(V_k,~k=1,2,3)\) of three bulk waves (say, qP, qS1, qS2) in general anisotropic media. Various unknowns in equation (10) are defined as follows.
for unit tensor \(\textbf{N}\) as row matrix \({\textbf{N}}=(N_1,N_2,N_3)\) and \({\textbf{N}}^{T}\) being its transpose. The \(3\times 3\) matrices, \(\textbf{A,B,C,D,E}\) and \(\textbf{F}\), are given by
The elements \(a_{IJ}=c_{IJ}/\rho ,~(I,J=1,2,...,6)\) make a \(6\times 6\) matrix of density-normalized elastic coefficients, where \(c_{IJ}\) are two-suffix notations for fourth-order elastic tensor (\(c_{ijkl}\)). As a convenient alternative, a symbol function in MATLAB can be used to resolve the determinant \(\det \{c_{ijkl}N_jN_l-\rho V^2\delta _{ik}\}\) into a cubic polynomial in \(V^2\).
Appendix B: Vertical slownesses
For known horizontal slowness \((p_1,p_2)\), the determinantal equation \(\det \{c_{ijkl}p_jp_l-\rho \delta _{ik}\}=0\) is solved into a sixth-degree algebraic equation in vertical slowness \(p_3\), given by
The coefficients \(d_n\) are calculated as:
where the symbol |XYZ| denotes the determinant of a matrix obtained by selecting first row from matrix \(\textbf{X}\), second row from matrix \(\textbf{Y}\) and third row from matrix \(\textbf{Z}\). The \(3\times 3\) matrices \(\mathbf{X,~Y,~Z}\) are defined as:
where \(c_{IJ}~(I,J=1,2,...,6)\) are two-suffix notations for elastic tensor \(c_{ijkl}\). A symbol function in MATLAB can be used to resolve the determinant \(\det \{c_{ijkl}p_jp_l-\rho \delta _{ik}\}\) into a polynomial of degree six.
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Sharma, M.D. Complex slowness vector for generalised propagation of harmonic plane waves at the boundaries of real materials. J Earth Syst Sci 133, 32 (2024). https://doi.org/10.1007/s12040-023-02234-7
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DOI: https://doi.org/10.1007/s12040-023-02234-7