弹性波传播模拟中ESyS-Particle的尺度基准

D. Weatherley, V. Boros, W. Hancock, S. Abe
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引用次数: 17

摘要

离散元法(DEM)是一种流行的基于粒子的数值方法,用于模拟地震、岩石破碎和颗粒流动等地球物理过程。通常,由数千个粒子组成的模拟不足以再现许多地球物理过程的微观力学,在某些情况下需要数百万个粒子。DEM的高计算费用阻碍了在台式pc上执行这种规模的问题。ESyS-Particle是DEM的并行实现,设计用于在集群超级计算机上执行。利用MPI实现了三维空间域分解,实现了进程间通信。我们给出了每个工作人员的问题大小保持不变的可伸缩性基准测试的结果。当工人的数量从27个增加到1000个时,执行时间几乎保持不变,允许模拟8.7万个粒子的实时时间与模拟240K个粒子的实时时间大致相同。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Scaling Benchmark of ESyS-Particle for Elastic Wave Propagation Simulations
The Discrete Element Method (DEM) is a popular particle-based numerical method for simulating geophysical processes including earthquakes, rock breakage and granular flow. Often simulations consisting of thousands of particles have insufficient resolution to reproduce the micromechanics of many geophysical processes, requiring millions of particles in some instances. The high computational expense of the DEM precludes execution of such problem sizes on desktop PCs. ESyS-Particle is a parallel implementation of the DEM, designed for execution on cluster supercomputers. Three-dimensional spatial domain decomposition is implemented using the MPI for interprocess communications. We present results of scaling benchmarks in which problem size per worker remains constant. As the number of workers increases from 27 to 1000, execution time remains near-constant, permitting simulations of 8.7M particles in approximately the same real time as simulations comprising 240K particles.
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