Nearly perfectly matched layer boundary conditions for operator upscaling of the acoustic wave equation

被引:0
作者
Chen Lai
Susan E. Minkoff
机构
[1] The University of Maryland,Department of Mathematics and Statistics
[2] Baltimore County,Department of Mathematical Sciences
[3] The University of Texas at Dallas,undefined
来源
Computational Geosciences | 2017年 / 21卷
关键词
Nearly perfectly matched layers; Absorbing boundary conditions; Acoustic wave propagation; Upscaling; MSC 86–08; MSC 35L05; MSC 65M60; MSC 65M06;
D O I
暂无
中图分类号
学科分类号
摘要
Acoustic imaging and sensor modeling are processes that require repeated solution of the acoustic wave equation. Solution of the wave equation can be computationally expensive and memory intensive for large simulation domains. One scheme for speeding up solution of the wave equation is the operator-based upscaling method. The algorithm proceeds in two steps. First, the wave equation is solved for fine grid unknowns internal to coarse blocks assuming the coarse blocks do not need to communicate with neighboring blocks in parallel. Second, these fine grid solutions are used to form a new problem which is solved on the coarse grid. Accurate and efficient wave propagation schemes also must avoid artificial reflections off of the computational domain edges. One popular method for preventing artificial reflections is the nearly perfectly matched layer (NPML) method. In this paper, we discuss applying NPML to operator upscaling for the wave equation. We show that although we only apply NPML to the first step of this two step algorithm (directly affecting the fine grid unknowns only), we still see a significant reduction of reflections back into the domain. We describe three numerical experiments (one homogeneous medium experiment and two heterogeneous media examples) in which we validate that the solution of the wave equation exponentially decays in the NPML regions. Numerical experiments of acoustic wave propagation in two dimensions with a reasonable absorbing layer thickness resulted in a maximum pressure reflection of 3–8%. While the coarse grid acceleration is not explicitly damped in our algorithm, the tight coupling between the two steps of the algorithm results in only 0.1–1% of acceleration reflecting back into the computational domain.
引用
收藏
页码:359 / 372
页数:13
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