TY - JOUR
T1 - Fractional Laplacians viscoacoustic wavefield modeling with k -space-based time-stepping error compensating scheme
AU - Wang, Ning
AU - Zhu, Tieyuan
AU - Zhou, Hui
AU - Chen, Hanming
AU - Zhao, Xuebin
AU - Tian, Yukun
N1 - Funding Information:
We would like to thank the editors and three anonymous reviewers for their valuable comments and helpful suggestions. This work was partly supported by the National Key R&D Program of China (2018YFA0702502), the National Natural Science Foundation of China (41630314, 41874130), the National Science and Technology Program (2016ZX05010001), and the Major Project of the China National Petroleum Corporation (2018A-33). The first author was financially supported by the China Scholarship Council to carry out his research at The Pennsylvania State University.
Publisher Copyright:
© 2020 Society of Exploration Geophysicists.
PY - 2020/1/1
Y1 - 2020/1/1
N2 - The spatial derivatives in decoupled fractional Laplacian (DFL) viscoacoustic and viscoelastic wave equations are the mixed-domain Laplacian operators. Using the approximation of the mixed-domain operators, the spatial derivatives can be calculated by using the Fourier pseudospectral (PS) method with barely spatial numerical dispersions, whereas the time derivative is often computed with the finite-difference (FD) method in second-order accuracy (referred to as the FD-PS scheme). The time-stepping errors caused by the FD discretization inevitably introduce the accumulative temporal dispersion during the wavefield extrapolation, especially for a long-time simulation. To eliminate the time-stepping errors, here, we adopted the k-space concept in the numerical discretization of the DFL viscoacoustic wave equation. Different from existing k-space methods, our k-space method for DFL viscoacoustic wave equation contains two correction terms, which were designed to compensate for the time-stepping errors in the dispersion-dominated operator and loss-dominated operator, respectively. Using theoretical analyses and numerical experiments, we determine that our k-space approach is superior to the traditional FD-PS scheme mainly in three aspects. First, our approach can effectively compensate for the time-stepping errors. Second, the stability condition is more relaxed, which makes the selection of sampling intervals more flexible. Finally, the k-space approach allows us to conduct high-accuracy wavefield extrapolation with larger time steps. These features make our scheme suitable for seismic modeling and imaging problems.
AB - The spatial derivatives in decoupled fractional Laplacian (DFL) viscoacoustic and viscoelastic wave equations are the mixed-domain Laplacian operators. Using the approximation of the mixed-domain operators, the spatial derivatives can be calculated by using the Fourier pseudospectral (PS) method with barely spatial numerical dispersions, whereas the time derivative is often computed with the finite-difference (FD) method in second-order accuracy (referred to as the FD-PS scheme). The time-stepping errors caused by the FD discretization inevitably introduce the accumulative temporal dispersion during the wavefield extrapolation, especially for a long-time simulation. To eliminate the time-stepping errors, here, we adopted the k-space concept in the numerical discretization of the DFL viscoacoustic wave equation. Different from existing k-space methods, our k-space method for DFL viscoacoustic wave equation contains two correction terms, which were designed to compensate for the time-stepping errors in the dispersion-dominated operator and loss-dominated operator, respectively. Using theoretical analyses and numerical experiments, we determine that our k-space approach is superior to the traditional FD-PS scheme mainly in three aspects. First, our approach can effectively compensate for the time-stepping errors. Second, the stability condition is more relaxed, which makes the selection of sampling intervals more flexible. Finally, the k-space approach allows us to conduct high-accuracy wavefield extrapolation with larger time steps. These features make our scheme suitable for seismic modeling and imaging problems.
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U2 - 10.1190/geo2019-0151.1
DO - 10.1190/geo2019-0151.1
M3 - Article
AN - SCOPUS:85084329450
SN - 0016-8033
VL - 85
SP - T1-T13
JO - Geophysics
JF - Geophysics
IS - 1
ER -