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Frequency-Domain Finite-Difference Elastic Wave Modeling in the Presence of Surface Topography

机译:表面形貌存在下频域有限差差弹性波造型

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Seismic numerical modeling in the presence of surface topography has become a valuable tool to characterize seismic wave propagation in basin or mountain areas. Regarding advantages of frequency-domain seismic wavefield simulations (e.g., easy implementation of multiple sources and straightforward extension of adding attenuation factors), we propose a frequency-domain finite-difference seismic wavefield simulation in 2D elastic media with an irregular free surface. In the frequency domain, we first transform second-order elastic wave equations and first-order free surface boundary conditions from the Cartesian coordinate system to the curvilinear coordinate system. Then we apply complex frequency-shifted perfectly matched layer (CFS-PML) absorbing boundary condition to second-order elastic wave equations in the curvilinear coordinate. To better couple free surface boundary conditions and CFS-PML absorbing boundary condition, we also apply the complex coordinate stretching method used in CFS-PML to free surface boundary conditions in the curvilinear coordinate. In the first numerical test, the comparison of the seismograms calculated by our algorithm with an analytical solution indicates that our algorithm can accurately simulate seismic wavefield in the frequency domain. Finally, we choose three more elastic models with different types of surface topographies to further characterize seismic wave propagation.
机译:表面形貌存在下的地震数值模型已成为在盆地或山区地震波传播中表征地震波传播的宝贵工具。关于频域地震波场模拟的优点(例如,轻松实现多种来源和添加衰减因子的简单扩展),我们提出了一种具有不规则自由表面的2D弹性介质中的频域有限差异地震波场模拟。在频域中,我们首先将二阶弹性波方程和从笛卡尔坐标系转换到曲线坐标系的第一阶的自由表面边界条件。然后,我们将复频移位完全匹配的层(CFS-PML)吸收边界条件应用于曲线坐标中的二阶弹性波方程。为了更好地对外的自由表面边界条件和CFS-PML吸收边界条件,我们还将CFS-PML中使用的复杂坐标拉伸方法应用于曲线坐标中的自由表面边界条件。在第一数值测试中,通过算法与分析解决方案计算的地震图的比较表明我们的算法可以准确地模拟频域中的地震波场。最后,我们选择三种具有不同类型的表面拓扑的弹性模型,以进一步表征地震波传播。

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