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ELASTIC WAVE-PROPAGATION SIMULATION IN HETEROGENEOUS MEDIA BY THE SPECTRAL MOMENTS METHOD

机译:谱矩法在非均质介质中的弹性波传播模拟

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The second-order elastic wave propagation equations are solved using the spectral moments method. This numerical method, previously developed in condensed matter physics, allows the computation of Green's functions for very large systems, The elastic wave equations are transformed in the Fourier domain for time derivatives, and the partial derivatives in space are computed by second-order finite differencing. The dynamic matrix of the discretized system is built from the medium parameters and the boundary conditions. The Green's function, calculated for a given source-receiver couple, is developed as a continued fraction whose coefficients are related to the moments and calculated from the dynamic matrix. The continued fraction coefficients and the moments are computed using a very simple algorithm, We show that the precise estimation of the waveform for the successive waves arriving at the receiver depends on the number of moments used. For long recording times, more moments are needed for an accurate solution. Efficiency and accuracy of the method is illustrated by modeling wave propagation in 1-D acoustic and 2-D elastic media and by comparing the results obtained by the spectral moments method to analytical solutions and classical finite-difference methods. [References: 43]
机译:使用谱矩法求解二阶弹性波传播方程。这种数值方法是以前在凝聚态物理中发展起来的,它允许对非常大的系统进行格林函数的计算,在傅立叶域中对弹性波方程进行时间导数转换,并通过二阶有限差分计算空间中的偏导数。 。离散化系统的动态矩阵是根据介质参数和边界条件建立的。为给定的源-接收器对计算的格林函数被开发为一个连续的分数,其系数与力矩有关,并从动态矩阵计算得出。连续分数系数和矩是使用非常简单的算法计算的。我们证明,到达接收器的连续波的波形精确估计取决于所用的矩数。对于较长的记录时间,需要更多的时间来提供准确的解决方案。通过对一维声学和二维弹性介质中的波传播进行建模,并将频谱矩量法与解析解和经典有限差分法所获得的结果进行比较,来说明该方法的效率和准确性。 [参考:43]

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