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首页> 外文期刊>Computers & geosciences >Ace-a Fortran Subroutine For Analytical Computation Of Effective Grid Parameters For Finite-difference Seismic Waveform Modeling With Standard Earth Models
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Ace-a Fortran Subroutine For Analytical Computation Of Effective Grid Parameters For Finite-difference Seismic Waveform Modeling With Standard Earth Models

机译:Ace-a Fortran子例程,用于使用标准地球模型对有限差分地震波形建模的有效网格参数进行解析计算

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Despite the broad use of the heterogeneous finite-difference (FD) method for seismic waveform modeling, accurate treatment of material discontinuities inside the grid cells has been a serious problem for many years. One possible way to solve this problem is to introduce effective grid elastic moduli and densities (effective parameters) calculated by the volume harmonic averaging of elastic moduli and volume arithmetic averaging of densities in grid cells. This scheme enables us to place a material discontinuity in an arbitrary position in the spatial grids.rnStandard Earth models have made a significant contribution to synthetic seismo-gram calculations with a variety of numerical procedures such as the FD method. For the FD computation of seismic waveform with these models, we must first ensure accurate treatment of material discontinuities in the radius (or depth). The present paper introduces a FORTRAN subroutine ace which calculates effective parameters analytically for an arbitrary spatial region in either the radius or depth direction for four major standard Earth models, namely, the PREM, IASP91, SP6, and AK135. This program is intended for all FD users who are concerned with seismic wave simulation for these models.
机译:尽管在地震波形建模中广泛使用了非均质有限差分(FD)方法,但是多年以来,精确处理网格单元内部材料不连续性一直是一个严重的问题。解决此问题的一种可能方法是引入有效的网格弹性模量和密度(有效参数),该弹性模量和密度(有效参数)是通过网格单元中的弹性模量的体积谐波平均和密度的体积算术平均来计算的。这种方案使我们能够将材料间断点放置在空间网格中的任意位置。标准地球模型通过多种数值程序(例如FD方法)为合成地震图计算做出了重要贡献。对于使用这些模型进行地震波形的FD计算,我们必须首先确保准确处理半径(或深度)上的材料不连续性。本文介绍了FORTRAN子例程ace,该子例程通过解析计算四个主要标准地球模型(即PREM,IASP91,SP6和AK135)在半径或深度方向上任意空间区域的有效参数。该程序适用于与这些模型的地震波仿真有关的所有FD用户。

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