Polarization of plane wave propagating inside elastic hexagonal system solids

Based on the reported physical parameters for hexagonal system solids, we have calculated the effects of anisotropy on polarization of plane P-wave propagation. Herein we report the results of calculations and the newly observed physical phenomena. It is found that, for a given propagation, if the polarization is parallel to the wave vector, so also to the Poynting vector. In such a case, the phase velocity is identical to the energy velocity; the quasi P-wave degenerates to a pure P-wave along the propagation. It is also noted that if the polarization is parallel to the Poynting vector but not to the wave vector, the propagating wave cannot be a pure P-wave. Furthermore, the polarization in a quasi P-wave may deviate from the wave vector for more than 45°, but the deviation from the Poynting vector is always less than 45°. The energy velocity of a quasi SV-wave can be larger than that of the quasi P-wave in some propagation directions, even though the phase velocity of a quasi SV-wave may never be larger than either the phase velocity or energy velocity of the quasi P-wave. Finally, in case of parameters ɛ=0 and δ*≠0, the polarization of a quasi P-wave has an observed symmetry at a 45° phase angle. The anisotropy of a hexagonal system solid determines if a pure P-wave can be created and what the propagation direction is for a plane wave propagating inside such a hexagonal system solid.

[1]  J. Etgen,et al.  Seismic migration problems and solutions , 2001 .

[2]  Bernard Hosten REFLECTION AND TRANSMISSION OF ACOUSTIC PLANE WAVES ON AN IMMERSED ORTHOTROPIC AND VISCOELASTIC SOLID LAYER , 1991 .

[3]  P. Lorrain,et al.  Electromagnetic fields and waves , 1970 .

[4]  Kees Wapenaar,et al.  Modal expansion of one‐way operators in laterally varying media , 1998 .

[5]  G. Backus Long-Wave Elastic Anisotropy Produced by Horizontal Layering , 1962 .

[6]  David Kessler,et al.  Accurate depth migration by a generalized phase-shift method , 1987 .

[7]  Jenö Gazdag,et al.  Modeling of the acoustic wave equation with transform methods , 1981 .

[8]  J. Gazdag,et al.  Wave Equation Migration with the Accurate Space Derivative METHOD , 1980 .

[9]  Piero Sguazzero,et al.  Migration of seismic data by phase-shift plus interpolation: Geophysics , 1984 .

[10]  Andreas Rüger,et al.  P-wave reflection coefficients for transversely isotropic models with vertical and horizontal axis of symmetry , 1997 .

[11]  I. Tsvankin,et al.  Synthesis of body wave seismograms from point sources in anisotropic media , 1990 .

[12]  Edip Baysal,et al.  Migration with the full acoustic wave equation , 1983 .

[13]  V. Červený,et al.  Seismic Ray Theory , 2001, Encyclopedia of Solid Earth Geophysics.

[14]  Jenö Gazdag,et al.  Wave equation migration with the phase-shift method , 1978 .

[15]  J. Castagna,et al.  Effects of anisotropy on time-depth relation in transversely isotropic medium with a vertical axis of symmetry , 2010 .

[16]  J. Carcione,et al.  Seismic modelingSeismic modeling , 2002 .

[17]  MIGRATION IN TERMS OF SPATIAL DECONVOLUTION , 1979 .

[18]  John Etgen,et al.  Computational methods for large-scale 3D acoustic finite-difference modeling: A tutorial , 2007 .

[19]  R. M. Alford,et al.  ACCURACY OF FINITE‐DIFFERENCE MODELING OF THE ACOUSTIC WAVE EQUATION , 1974 .

[20]  Sameera K. Abeykoon,et al.  New full-wave phase-shift approach to solve the Helmholtz acoustic wave equation for modeling , 2012 .

[21]  B. Auld,et al.  Acoustic fields and waves in solids , 1973 .

[22]  F. Hron,et al.  Reflection and transmission coefficients for seismic waves in ellipsoidally anisotropic media , 1979 .

[23]  L. Thomsen Weak elastic anisotropy , 1986 .

[24]  Edip Baysal,et al.  Forward modeling by a Fourier method , 1982 .

[25]  R. Kosloff,et al.  Absorbing boundaries for wave propagation problems , 1986 .

[26]  Lin Fa,et al.  Effects of electric-acoustic and acoustic-electric conversions of transducers on acoustic logging signal , 2012 .

[27]  R. Stolt MIGRATION BY FOURIER TRANSFORM , 1978 .

[28]  J. Castagna,et al.  An accurately fast algorithm of calculating reflection/transmission coefficients , 2008 .

[29]  Jack K. Cohen,et al.  Mathematics of Multidimensional Seismic Imaging, Migration, and Inversion , 2001 .

[30]  John P. Castagna,et al.  Offset-dependent reflectivity : theory and practice of AVO analysis , 1993 .

[31]  S. Crampin,et al.  The polarization of P-waves in anisotropic media , 1982 .

[32]  José M. Carcione,et al.  Wave Fields in Real Media: Wave Propagation in Anisotropic, Anelastic and Porous Media , 2011 .

[33]  N. Bleistein On the imaging of reflectors in the earth , 1987 .

[34]  C. Wapenaar Representation of seismic sources in the one‐way wave equations , 1990 .

[35]  Evgeni M. Chesnokov,et al.  Upscaling of elastic properties of anisotropic sedimentary rocks , 2008 .

[36]  Moshe Reshef,et al.  Practical implementation of three-dimensional poststack depth migration , 1989 .

[37]  Seismic Signal and Data Analysis of Rock Media with Vertical Anisotropy , 2013 .

[38]  J. Claerbout Toward a unified theory of reflector mapping , 1971 .

[39]  Ilya Tsvankin,et al.  Seismic Signatures and Analysis of Reflection Data in Anisotropic Media , 2001 .

[40]  P. Lanceleur,et al.  The use of inhomogeneous waves in the reflection–transmission problem at a plane interface between two anisotropic media , 1993 .

[41]  M. Schoenberg,et al.  Anomalous polarization of elastic waves in transversely isotropic media , 1985 .

[42]  Zhijing Wang Seismic anisotropy in sedimentary rocks, part 2: Laboratory data , 2002 .

[43]  A. Nur,et al.  Ultrasonic velocity and anisotropy of hydrocarbon source rocks , 1992 .

[44]  Chuan Wang,et al.  DOUBLING THE CAPACITY OF QUANTUM KEY DISTRIBUTION BY USING BOTH POLARIZATION AND DIFFERENTIAL PHASE SHIFT , 2009 .

[45]  Anomalous postcritical refraction behavior for certain transversely isotropic media. , 2006, The Journal of the Acoustical Society of America.