TY - JOUR
T1 - Application of perturbation theory to a P-wave eikonal equation in orthorhombic media
AU - Stovas, Alexey
AU - Masmoudi, Nabil
AU - Alkhalifah, Tariq Ali
N1 - KAUST Repository Item: Exported on 2020-10-01
Acknowledgements: A. Stovas would like to acknowledge the ROSE Project for financial support. N. Masmoudi and T. Alkhalifah would like to thank KAUST for financial support.
PY - 2016/10/12
Y1 - 2016/10/12
N2 - The P-wave eikonal equation for orthorhombic (ORT) anisotropic media is a highly nonlinear partial differential equation requiring the solution of a sixth-order polynomial to obtain traveltimes, resulting in complex and time-consuming numerical solutions. To alleviate this complexity, we approximate the solution of this equation by applying a multiparametric perturbation approach. We also investigated the sensitivity of traveltime surfaces inORT mediawith respect to three anelliptic parameters. As a result, a simple and accurate P-wave traveltime approximation valid for ORT media was derived. Two different possible anelliptic parameterizations were compared. One of the parameterizations includes anelliptic parameters defined at zero offset: η1, η2, and ηxy. Another parameterization includes anelliptic parameters defined for all symmetry planes: η1, η2, and η3. The azimuthal behavior of sensitivity coefficients with different parameterizations was used to analyze the crosstalk between anelliptic parameters. © 2016 Society of Exploration Geophysicists.
AB - The P-wave eikonal equation for orthorhombic (ORT) anisotropic media is a highly nonlinear partial differential equation requiring the solution of a sixth-order polynomial to obtain traveltimes, resulting in complex and time-consuming numerical solutions. To alleviate this complexity, we approximate the solution of this equation by applying a multiparametric perturbation approach. We also investigated the sensitivity of traveltime surfaces inORT mediawith respect to three anelliptic parameters. As a result, a simple and accurate P-wave traveltime approximation valid for ORT media was derived. Two different possible anelliptic parameterizations were compared. One of the parameterizations includes anelliptic parameters defined at zero offset: η1, η2, and ηxy. Another parameterization includes anelliptic parameters defined for all symmetry planes: η1, η2, and η3. The azimuthal behavior of sensitivity coefficients with different parameterizations was used to analyze the crosstalk between anelliptic parameters. © 2016 Society of Exploration Geophysicists.
UR - http://hdl.handle.net/10754/621907
UR - http://library.seg.org/doi/10.1190/geo2016-0097.1
UR - http://www.scopus.com/inward/record.url?scp=84991229769&partnerID=8YFLogxK
U2 - 10.1190/GEO2016-0097.1
DO - 10.1190/GEO2016-0097.1
M3 - Article
SN - 0016-8033
VL - 81
SP - C309-C317
JO - GEOPHYSICS
JF - GEOPHYSICS
IS - 6
ER -