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Reverse-time Migration in Tilted Transversely Isotropic Media with Decoupled Equations

机译:具有解耦方程的横观各向同性倾斜介质中的逆时偏移

摘要

Conventional modeling and migration for tilted transversely isotropic (TTI) media may suffer from numerical instabilities and shear wave artifacts due to the coupling of the P-wave and SV-wave modes in the TTI coupled equations. Starting with the separated P- and SV-phase velocity expressions for vertical transversely isotropic (VTI) media, I extend these decoupled equations for modeling and reverse-time migration (RTM) in acoustic TTI media. Compared with the TTI coupled equations published in the geophysical literature, the new TTI decoupled equations provide a more stable solution due to the complete separation of the P-wave and SV-wave modes. The pseudospectral (PS) method is the most convenient method to implement these equations due to the form of wavenumber expressions and has the added benefit of being highly accurate and thus avoiding numerical dispersion. The rapid expansion method (REM) in time is employed to produce a broad band numerically stable time evolution of the wavefields. Synthetic results validate the proposed TTI decoupled equations and show that modeling and RTM in TTI media with the decoupled P-wave equation remain numerically stable even for models with strong anisotropy and sharp contrasts.The most desirable feature of the TTI decoupled P-wave equation is that it is absolutely free of shear-wave artifacts and the consequent alleviation of numerical instabilities generally suffered by some systems of coupled equations. However, due to several forward-backward Fourier transforms in wavefield extrapolation at each time step, the computational cost is also high, and thereby hampers its prevalence. I hereby propose to use a hybrid pseudospectral and finite-difference (FD) scheme to solve the TTI decoupled P-wave equation. In the hybrid solution, most of the cost-consuming wavenumber terms in the equation are replaced by inexpensive FD operators, which in turn accelerates the computation and reduces the computational cost. To demonstrate the benefit in cost saving of the new scheme, 2D and 3D RTM examples using the hybrid solution to the decoupled P-wave equation are carried out, and respective runtimes are listed and compared. Computation examples show that the hybrid strategy demands less computation time and is faster than using the pseudospectral method alone. Furthermore, this new hybrid TTI RTM algorithm is less computationally expensive than the FD solution to the conventional TTI coupled equations but more stable.
机译:倾斜横观各向同性(TTI)介质的常规建模和迁移可能会由于TTI耦合方程中P波和SV波模式的耦合而遭受数值不稳定性和剪切波伪影的困扰。从垂直横向各向同性(VTI)介质的分离的P相和SV相速度表达式开始,我扩展了这些解耦方程,用于声学TTI介质中的建模和逆时偏移(RTM)。与地球物理文献中发表的TTI耦合方程相比,由于P波和SV波模式完全分离,新的TTI解耦方程提供了更稳定的解决方案。由于波数表达式的形式,伪谱(PS)方法是最便捷的方法来实现这些方程式,并且具有高精度,避免数值分散的优点。时间上的快速扩展方法(REM)用于产生波场的宽带数值稳定的时间演化。综合结果验证了所提出的TTI解耦方程,并表明,即使对于具有强各向异性和强烈反差的模型,具有解耦P波方程的TTI介质中的建模和RTM仍保持数值稳定。它完全没有剪切波伪像,因此消除了某些耦合方程组通常所遭受的数值不稳定性。但是,由于在每个时间步的波场外推中都进行了一些前向-后向傅里叶变换,因此计算量也很高,从而妨碍了它的普及。我在此提出使用混合伪谱和有限差分(FD)方案来求解TTI解耦的P波方程。在混合解决方案中,方程式中的大多数成本高昂的波数项均由便宜的FD运算符代替,从而加快了计算速度,并降低了计算成本。为了证明该新方案节省成本的好处,我们使用了对解耦P波方程的混合解决方案的2D和3D RTM示例,并列出并比较了各自的运行时间。计算示例表明,混合策略比单独使用伪光谱方法需要更少的计算时间并且更快。此外,这种新的混合TTI RTM算法在计算上比常规TTI耦合方程的FD解决方案便宜,但更稳定。

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    Zhan Ge;

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  • 年度 2012
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  • 原文格式 PDF
  • 正文语种 en
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