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A High-Order Time and Space Formulation of the Unsplit Perfectly Matched Layer for the Seismic Wave Equation Using Auxiliary Differential Equations (ADE-PML)

机译:使用辅助微分方程(ADE-PML)的地震波方程的未分裂完美匹配层的高阶时空公式

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摘要

Unsplit convolutional perfectly matched layers (CPML) for the velocity and stress formulation of the seismic wave equation are classically computed based on a second-order finite-difference time scheme. However it is often of interest to increase the order of the time-stepping scheme in order to increase the accuracy of the algorithm. This is important for instance in the case of very long simulations. We study how to define and implement a new unsplit non-convolutional PML called the Auxiliary Differential Equation PML (ADE-PML), based on a high-order Runge-Kutta time-stepping scheme and optimized at grazing incidence. We demonstrate that when a second-order time-stepping scheme is used the convolutional PML can be derived from that more general non-convolutional ADE-PML formulation, but that this new approach can be generalized to high-order schemes in time, which implies that it can be made more accurate. We also show that the ADE-PML formulation is numerically stable up to 100,000 time steps.
机译:经典地基于二阶有限差分时间方案来计算地震波方程的速度和应力公式的未分裂卷积完全匹配层(CPML)。然而,经常感兴趣的是增加时间步进方案的顺序以增加算法的准确性。例如,对于非常长的仿真,这很重要。我们研究如何基于高阶Runge-Kutta时间步长方案并在掠入射时进行优化,来定义和实现一种新的非分裂非卷积PML,称为辅助微分方程PML(ADE-PML)。我们证明了,当使用二阶时间步长方案时,卷积PML可以从更通用的非卷积ADE-PML公式中得出,但是这种新方法可以及时推广到高阶方案,这意味着可以使其更加准确。我们还表明,ADE-PML公式在数值上稳定到100,000个时间步长。

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