Inversion of Rayleigh Wave Dispersion Curves via BP Neural Network and PSO

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Yijian Luo
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Abstract

Rayleigh wave analysis serves as a critical tool for subsurface characterization in geotechnical engineering and geophysical exploration, while reconstructing stratigraphic velocity profiles from dispersion curves remains challenging due to inherent nonlinearity and solution multiplicity. This study proposes a hybrid inversion framework integrating a backpropagation (BP) neural network with particle swarm optimization (PSO). A statistically representative training database encompassing realistic stratigraphic configurations is systematically established through random perturbation of shear-wave velocity profiles. Then, a BP neural network is employed to establish the nonlinear correspondence between dispersion curves and stratum-specific shear-wave velocity profiles. The trained BP neural network demonstrates computational efficacy in generating geophysically plausible velocity estimates, albeit with limited spatial resolution. These network-derived models serve as physics-informed initial inputs for the subsequent PSO inversion framework, forming a dual-phase inversion framework. This synergistic methodology specifically targets two persistent challenges in geophysical parameter estimation: (i) the non-iterative nature of standard BP architectures that restricts progressive model improvement, and (ii) the suboptimal search efficiency of standalone PSO implementations when initialized without physically meaningful constraints. Benchmark synthetic experiments confirm the enhanced robustness of the dual-phase inversion framework, exhibiting a significant reduction in mean relative error compared to BP neural network and PSO under controlled noise conditions. Furthermore, field implementation at the Baotou–Yinchuan railway site successfully identified weak interlayers, as confirmed by the borehole data.

Abstract Image

Abstract Image

基于BP神经网络和粒子群算法的瑞利波频散曲线反演
瑞利波分析是岩土工程和地球物理勘探中地下表征的重要工具,但由于其固有的非线性和解的多重性,利用频散曲线重建地层速度剖面仍然具有挑战性。提出了一种结合反向传播(BP)神经网络和粒子群优化(PSO)的混合反演框架。通过对横波速度剖面的随机扰动,系统地建立了一个具有统计代表性的包含真实地层配置的训练数据库。然后,利用BP神经网络建立色散曲线与层间横波速度曲线的非线性对应关系。经过训练的BP神经网络在产生地球物理上合理的速度估计方面显示出计算效率,尽管空间分辨率有限。这些网络衍生模型作为后续PSO反演框架的物理信息初始输入,形成双相位反演框架。这种协同方法专门针对地球物理参数估计中两个持续存在的挑战:(i)标准BP架构的非迭代性质限制了渐进模型的改进,以及(ii)在没有物理上有意义的约束的情况下初始化独立PSO实现的次优搜索效率。基准合成实验证实了双相位反演框架的鲁棒性增强,在可控噪声条件下,与BP神经网络和粒子群算法相比,平均相对误差显著降低。此外,在包银川铁路现场实施,成功识别出弱夹层,并得到钻孔资料的证实。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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