利用瓦瑟斯坦距离与贝叶斯优化法进行多模式瑞利波频散谱反演

GEOPHYSICS Pub Date : 2024-01-26 DOI:10.1190/geo2023-0223.1
Yanlong Niu, Gang Fang, Yunyue Elita Li, S. C. Chian, E. Nilot
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引用次数: 0

摘要

我们提出了一种新的无损多通道面波分析(MASW)自动框架,该框架结合了多模式频散谱匹配和基于有限元法(FEM)的反演,以提高现场调查活动中地下剖面测量的准确性。该框架无需人工识别瑞利波能量分量和多模式分配,减少了对操作人员经验和判断的依赖。频散谱通过有限元模型生成,该模型模拟二维地震波的传播,并考虑到实际采集布局和地下的横向变化。我们引入了瓦瑟斯坦距离(WD)来评估观测频谱和模拟频谱之间的差异,并结合贝叶斯优化技术来有效反演剪切波速度剖面。通过合成数据实例证明了所提框架的有效性,并通过与传统的基于均方误差(MSE)的目标函数进行比较,说明了基于 WD 的目标函数的优越性。随后,我们在一个填埋场进行了实地测试,以验证所提出的框架。该测试证实了该框架检索多模式瑞利波的能力,并证明了其在提供浅表次表层高分辨率剪切波剖面方面的有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multi-Mode Rayleigh Wave Dispersion Spectrum Inversion Using Wasserstein Distance Coupled with Bayesian Optimization
We propose a new automatic framework for non-destructive multi-channel analysis of surface waves (MASW) that combines multi-mode dispersion spectrum matching and the finite element method (FEM)-based inversion to enhance the accuracy of subsurface profiling in site investigation activities. This framework eliminates the need for manual identification of the Rayleigh wave energy component and multi-mode assignment, reducing the dependence on operator experience and judgment. The dispersion spectrum is generated through a FEM model that simulates 2D seismic wave propagation, taking into account the actual acquisition layout and lateral variations in the subsurface. We introduce the Wasserstein distance (WD) for evaluating the difference between observed and simulated spectra, and incorporate Bayesian optimization for efficiently inverting shear wave velocity profiles. The effectiveness of the proposed framework is demonstrated through synthetic data examples, and the superiority of the WD-based objective function is illustrated by comparing it with the conventional mean square error (MSE)-based objective function. Subsequently, we conduct a field test on a reclaimed landfill to validate the proposed framework. This test confirms the ability of framework to retrieve multi-mode Rayleigh waves and demonstrates its effectiveness in providing high-resolution shear wave profiles of the shallow subsurface.
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