首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >A parallel 3-D staggered grid pseudospectral time domain method for ground-penetrating radar wave simulation
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A parallel 3-D staggered grid pseudospectral time domain method for ground-penetrating radar wave simulation

机译:并行3D交错网格伪谱时域方法用于探地雷达波仿真

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We presented a parallel 3-D staggered grid pseudospectral time domain (PSTD) method for simulating ground-penetrating radar (GPR) wave propagation. We took the staggered grid method to weaken the global effect in PSTD and developed a modified fast Fourier transform (FFT) spatial derivative operator to eliminate the wraparound effect due to the implicit periodical boundary condition in FFT operator. After the above improvements, we achieved the parallel PSTD computation based on an overlap domain decomposition method without any absorbing condition for each subdomain, which can significantly reduce the required grids in each overlap subdomain comparing with other proposed algorithms. We test our parallel technique for some numerical models and obtained consistent results with the analytical ones and/or those of the nonparallel PSTD method. The above numerical tests showed that our parallel PSTD algorithm is effective in simulating 3-D GPR wave propagation, with merits of saving computation time, as well as more flexibility in dealing with complicated models without losing the accuracy. The application of our parallel PSTD method in applied geophysics and paleoseismology based on GPR data confirmed the efficiency of our algorithm and its potential applications in various subdisciplines of solid earth geophysics. This study would also provide a useful parallel PSTD approach to the simulation of other geophysical problems on distributed memory PC cluster.
机译:我们提出了一种并行的3-D交错网格伪谱时域(PSTD)方法,用于模拟探地雷达(GPR)波的传播。我们采用交错网格方法来减弱PSTD中的全局效应,并开发了一种改进的快速傅立叶变换(FFT)空间导数算子,以消除由于FFT算子中隐含的周期性边界条件而产生的环绕效应。经过以上改进,我们实现了一种基于重叠域分解方法的并行PSTD计算,每个子域没有任何吸收条件,与其他算法相比,可以显着减少每个重叠子域中所需的网格。我们对某些数值模型测试了并行技术,并与分析和/或非并行PSTD方法获得了一致的结果。上述数值测试表明,我们的并行PSTD算法可以有效地模拟3-D GPR波的传播,具有节省计算时间,在处理复杂模型时更加灵活而又不损失精度的优点。基于GPR数据,我们的并行PSTD方法在应用地球物理学和古地震学中的应用证实了我们的算法的有效性及其在固体地球物理学各个子学科中的潜在应用。这项研究还将为模拟分布式存储PC集群上的其他地球物理问题提供有用的并行PSTD方法。

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