Fractional-order velocity-dilatation-rotation viscoelastic wave equation and numerical solution based on a constant-Q model

Author:

Han Guanghui1ORCID,He Bingshou2ORCID,Zhang Huixing1ORCID,Wang Enjiang1ORCID

Affiliation:

1. Ocean University of China, Ministry of Education, Key Laboratory of Submarine Geosciences and Prospecting Techniques, Evaluation and Detection Technology Laboratory of Marine Mineral Resources, Laoshan National Laboratory of Marine Science and Technology, Qingdao, China.

2. Ocean University of China, Ministry of Education, Key Laboratory of Submarine Geosciences and Prospecting Techniques, Evaluation and Detection Technology Laboratory of Marine Mineral Resources, Laoshan National Laboratory of Marine Science and Technology, Qingdao, China. (corresponding author)

Abstract

Viscoelastic wave equations based on the constant- Q (CQ) model can accurately describe the amplitude dissipation and phase distortion of waves in anelastic media. However, only three velocity or displacement components can be obtained directly by solving such equations. Starting from the time-domain second-order displacement viscoelastic wave equation, we derived the decoupled P- and S-wave displacement vector viscoelastic wave equation by using the polarization difference of P- and S-wave propagation in isotropic media. The equation can be transformed into the velocity-dilatation-rotation viscoelastic wave equation containing the first-order temporal derivative and fractional Laplacian operators, which can be solved directly by using the staggered-grid finite-difference and pseudospectral methods. We use the low-rank decomposition method to approximate the derived mixed space-wavenumber domain fractional Laplacian operators for modeling wave propagation in heterogeneous attenuating media. We also demonstrated the precision of our equation by comparing the numerical solutions with the analytical solutions. Furthermore, compared with the conventional velocity-stress viscoelastic wave equation, experimental results demonstrate that our equation can separate the pure P and S waves from the mixed wavefield during wavefield continuation. In addition, it can be separated into an equation containing predominantly an amplitude attenuation or a phase distortion term.

Funder

National Natural Science Foundation of China

Publisher

Society of Exploration Geophysicists

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