TY - GEN
T1 - Acoustic anisotropic wavefields through perturbation theory
AU - Alkhalifah, T.
PY - 2012
Y1 - 2012
N2 - Solving the anisotropic acoustic wave equation in a conventional manner (i.e. finite difference implementation) introduces a number of problems, and sets media restrictions, and it rarely contributes to our ability to resolve the anisotropic parameters. Utilizing perturbation theory in developing the solution of the anisotropic acoustic wave equation allows us direct access to the desired limitations-free solutions, that is solutions perturbed from the elliptical anisotropic background medium. It also provides a platform for parameter estimation as we can isolate the wavefield dependency on the perturbed anisotropic parameters. As a result, I derive approximate phase operators for a spectral domain wavefield extrapolation in transversely isotropic media based on perturbations in the anisotropic parameters. The solutions of the perturbation equations represent the coefficients of a Taylor's series type expansion of the wavefield as a function of the perturbed parameter, which is in this case the anellipticity parameter and the symmetry axis. The accuracy is relatively high in even inhomogeneous media.
AB - Solving the anisotropic acoustic wave equation in a conventional manner (i.e. finite difference implementation) introduces a number of problems, and sets media restrictions, and it rarely contributes to our ability to resolve the anisotropic parameters. Utilizing perturbation theory in developing the solution of the anisotropic acoustic wave equation allows us direct access to the desired limitations-free solutions, that is solutions perturbed from the elliptical anisotropic background medium. It also provides a platform for parameter estimation as we can isolate the wavefield dependency on the perturbed anisotropic parameters. As a result, I derive approximate phase operators for a spectral domain wavefield extrapolation in transversely isotropic media based on perturbations in the anisotropic parameters. The solutions of the perturbation equations represent the coefficients of a Taylor's series type expansion of the wavefield as a function of the perturbed parameter, which is in this case the anellipticity parameter and the symmetry axis. The accuracy is relatively high in even inhomogeneous media.
UR - http://www.scopus.com/inward/record.url?scp=84928139284&partnerID=8YFLogxK
U2 - 10.3997/2214-4609.20148102
DO - 10.3997/2214-4609.20148102
M3 - Conference contribution
AN - SCOPUS:84928139284
T3 - 74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012: Responsibly Securing Natural Resources
SP - 830
EP - 834
BT - 74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012
PB - European Association of Geoscientists and Engineers, EAGE
T2 - 74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012: Responsibly Securing Natural Resources
Y2 - 4 June 2012 through 7 June 2012
ER -