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首页> 外文期刊>Bulletin of the Seismological Society of America >Localized Boundary Integral Equation-Discrete Wavenumber Method for Simulating Wave Propagation in Irregular Multiple Layers, Part I: Theory
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Localized Boundary Integral Equation-Discrete Wavenumber Method for Simulating Wave Propagation in Irregular Multiple Layers, Part I: Theory

机译:模拟不规则多层中波传播的局部边界积分方程-离散波数方法,第一部分:理论

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摘要

We present a new method of synthesizing seismograms for irregular multilayered problems. It is an extension of the local (lo) boundary integral equation (BIE) discrete wavenumber method (DWM) topography problem. Following similar procedures as those developed in solving the P-SV waves of topography problems, we first provide the formulation of Bouchon and Campillo's BIE-DWM (Bouchon, 1985; Campillo and Bouchon, 1985) for the multilayered problem. By orthogonally decomposing the forces on irregular and flat parts of each interface and applying a discrete Fourier transform (DFT) we derive their relation. Finally, considering the continuity of displacement and traction on each interface, we get a linear equation only involving the unknown forces on irregular parts of interfaces and discuss its solution. In this algorithm the dimension of the lineal equation is decided by the sampling number on irregular parts of interfaces. Therefore, its computation efficiency increases dramatically, particularly for the problem in which the corrugated part of the layer is highly localized.
机译:我们提出了一种合成不规则多层问题地震图的新方法。它是局部(lo)边界积分方程(BIE)离散波数方法(DWM)地形问题的扩展。遵循与解决P-SV地形问题的方法类似的程序,我们首先为多层问题提供Bouchon和Campillo的BIE-DWM(Bouchon,1985; Campillo和Bouchon,1985)的公式。通过正交分解每个界面的不规则部分和平坦部分上的力并应用离散傅里叶变换(DFT),我们可以得出它们的关系。最后,考虑到每个界面上位移和牵引力的连续性,我们得到了仅包含未知力作用于界面不规则部分上的线性方程,并讨论了其解决方案。在该算法中,线性方程的维数由界面不规则部分上的采样数决定。因此,其计算效率显着提高,特别是对于层的波纹部分高度局部化的问题。

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