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Convolutional and Non-convolutional PMLs for High-order Schemes Optimized at Grazing Incidence for the Seismic Wave Equation

机译:用于地震波动方程的放牧发生率优化的高阶方案的卷积和非卷积PMLS

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The perfectly matched layer (PML) absorbing boundary condition has proven to be very efficient from anumerical point of view for the elastic wave equation to absorb both body waves with nongrazingincidence and surface waves.However, at grazing incidence the classical discrete PML method suffers from large spurious reflectionsthat make it less efficient for instance in the case of very thin mesh slices, in the case of sources locatedclose to the edge of the mesh, and/or in the case of receivers located at very large offset.The PML can be improved at grazing incidence for the seismic wave equation based on unsplitconvolution (CPML) or non convolution techniques (ADE-PML/Auxiliary Differential Equations PML).Unsplit CPMLs for the velocity and stress formulation of the seismic wave equation are classicallycomputed based on a second-order finite-difference time scheme.To increase the accuracy of thealgorithm, particularly for long time periods, we implemented an unsplit non-convolutional high-ordertime-stepping version of ADE-PML. ADE-PML and CPML are equivalent at the second-order in time.Applications to purely elastic, anisotropic, poroelastic and viscoelastic thin slices in 2D/3D configurationsare shown.
机译:从弹性波动方程的体积视角被证明是完美匹配的层(PML)的层(PML)吸收边界条件是从弹性波形方程吸收与非折叠和表面波的体波。然而,在放牧发生率时,古典离散的PML方法遭受大量假杂散的反射液使得例如在非常薄的网状切片的情况下效率较低,在源位于网状物的边缘的源,和/或在非常大的偏移的接收器的情况下。可以改善PML掠入射基于unsplitconvolution(CPML)或非卷积技术(ADE-PML /辅助微分方程PML).Unsplit CPMLs为地震波方程的速度和应力制剂中的地震波方程classicallycomputed基于第二阶有限-difference时间方案。要提高脚的准确性,特别是对于长时间的时间,我们实施了一个未卷积的非卷积嗨GH-ORDERTIME-STAPPING版本的ADE-PML。 ADE-PML和CPML是在time.Applications到纯弹性,各向异性的,在2D / 3D多孔弹性和粘弹性薄片二阶等效configurationsare所示。

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