Regularized Seismic Full Waveform Inversion Using Inverse Scattering Approach and Preconditioned L-BFGS Optimization

IF 8.6 1区 地球科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC IEEE Transactions on Geoscience and Remote Sensing Pub Date : 2025-02-14 DOI:10.1109/TGRS.2025.3542019
Wenrui Ye;Xingguo Huang;Li Han;Cong Wang;Xiaodong Luo;Naijian Wang;Yunshan Lei;Yinpo Xu
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Abstract

Although full waveform inversion (FWI) is widely recognized as one of the state-of-the-art techniques in geophysical exploration, there remain several aspects of FWI that require further improvements, specifically in resolution and modeling efficiency. To address this, we introduce an inverse scattering approach to frequency-domain seismic FWI by utilizing a regularized objective function. Different from traditional adjoint methods, the scattering theory allows us to derive the sensitivity kernel explicitly through two Greens’ functions and transforms the nonlinear inverse scattering problem into a series of linear inverse scattering problems, thereby facilitating the calculation of the gradient and Hessian. To mitigate the computational cost when calculating the background and actual wavefields, the fast Fourier transform (FFT) combined with the Krylov subspace method is used to solve the Lippmann-Schwinger (L-S) integral equation (IE) iteratively. Additionally, we incorporate minimum support (MS) stabilizing functional as an extra model misfit term alongside the traditional data misfit function, for a better recovery of the shape structure within the model. Furthermore, the inversion framework is enhanced by integrating an improved limited memory Broyden-Fletcher–Goldfarb-Shanno algorithm, with the regularized Hessian serving as a preconditioner. To demonstrate the efficacy of our method, numerical tests on Marmousi and BP models are presented to validate the performance and robustness of the proposed approach.
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基于反散射法的正则化地震全波形反演及预处理L-BFGS优化
尽管全波形反演(FWI)被广泛认为是地球物理勘探领域最先进的技术之一,但FWI仍有几个方面需要进一步改进,特别是在分辨率和建模效率方面。为了解决这个问题,我们引入了一种利用正则化目标函数对频域地震FWI进行逆散射的方法。与传统的伴随方法不同,散射理论允许我们通过两个格林函数显式地推导灵敏度核,并将非线性逆散射问题转化为一系列线性逆散射问题,从而便于梯度和Hessian的计算。为了减少背景波场和实际波场计算时的计算量,采用快速傅里叶变换(FFT)和Krylov子空间法对Lippmann-Schwinger (L-S)积分方程(IE)进行迭代求解。此外,为了更好地恢复模型内的形状结构,我们将最小支持(MS)稳定函数作为传统数据不拟合函数的额外模型不拟合项。此外,通过集成改进的有限内存Broyden-Fletcher-Goldfarb-Shanno算法,以正则化Hessian作为前置条件,增强了反演框架。为了证明该方法的有效性,在Marmousi模型和BP模型上进行了数值试验,以验证该方法的性能和鲁棒性。
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来源期刊
IEEE Transactions on Geoscience and Remote Sensing
IEEE Transactions on Geoscience and Remote Sensing 工程技术-地球化学与地球物理
CiteScore
11.50
自引率
28.00%
发文量
1912
审稿时长
4.0 months
期刊介绍: IEEE Transactions on Geoscience and Remote Sensing (TGRS) is a monthly publication that focuses on the theory, concepts, and techniques of science and engineering as applied to sensing the land, oceans, atmosphere, and space; and the processing, interpretation, and dissemination of this information.
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