波传播随机分析中的多项式混沌扩展与蒙特卡罗模拟

IF 2.1 3区 物理与天体物理 Q2 ACOUSTICS
Aneta Herbut, Włodzimierz Brząkała
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引用次数: 0

摘要

本文以地震波在地层介质中的传播为例,论述了随机波在弹性介质中的传播。底土参数的识别永远不会精确或完整,这就需要使用随机场模型或随机变量模型作为输入数据;因此,底土的响应也是随机的。在本文中,在随机变量的背景下,重点是敏感性分析,解决输入数据(路基参数)的不确定性如何影响所得结果(位移)的问题。本文介绍了两种不同的随机分析方法--伽勒金投影支持下的侵入多项式混沌法和蒙特卡罗模拟法,并以弹性半平面上的波传播为例进行了比较。两种方法得出的结果一致,但计算效率不同。本文讨论了两种方法的优缺点。上层底土层对随机解方差的影响远大于下层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Polynomial chaos expansion vs. Monte Carlo simulation in a stochastic analysis of wave propagation

The paper deals with the propagation of a stochastic wave in an elastic medium using the example of a seismic wave in a ground medium. Identification of subsoil parameters is never exact or complete which justifies the use of random field models or random variable models for input data; thus, the response of the subsoil is also random. In this paper and in the context of random variables, the focus is on a sensitivity analysis addressing the question of how the uncertainty of the input data (subgrade parameters) influences the obtained results (displacements). Two different methods of stochastic analysis are presented—the intrusive polynomial chaos approach supported by the Galerkin projection and Monte Carlo simulation—and compared by using an example of wave propagation in the elastic half-plane. Consistency in the results of both approaches has been achieved; however, the calculation efficiencies differ. The advantages and disadvantages of both approaches are discussed. The upper subsoil layer influences the variances of the random solutions much more than does the lower layer.

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来源期刊
Wave Motion
Wave Motion 物理-力学
CiteScore
4.10
自引率
8.30%
发文量
118
审稿时长
3 months
期刊介绍: Wave Motion is devoted to the cross fertilization of ideas, and to stimulating interaction between workers in various research areas in which wave propagation phenomena play a dominant role. The description and analysis of wave propagation phenomena provides a unifying thread connecting diverse areas of engineering and the physical sciences such as acoustics, optics, geophysics, seismology, electromagnetic theory, solid and fluid mechanics. The journal publishes papers on analytical, numerical and experimental methods. Papers that address fundamentally new topics in wave phenomena or develop wave propagation methods for solving direct and inverse problems are of interest to the journal.
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