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Full Waveform Inversion Using Student's t Distribution: a Numerical Study for Elastic Waveform Inversion and Simultaneous-Source Method

机译:使用学生t分布进行全波形反演:弹性波形反演和同时源方法的数值研究

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Seismic full waveform inversion (FWI) has primarily been based on a least-squares optimization problem for data residuals. However, the least-squares objective function can suffer from its weakness and sensitivity to noise. There have been numerous studies to enhance the robustness of FWI by using robust objective functions, such as l (1)-norm-based objective functions. However, the l (1)-norm can suffer from a singularity problem when the residual wavefield is very close to zero. Recently, Student's t distribution has been applied to acoustic FWI to give reasonable results for noisy data. Student's t distribution has an overdispersed density function compared with the normal distribution, and is thus useful for data with outliers. In this study, we investigate the feasibility of Student's t distribution for elastic FWI by comparing its basic properties with those of the l (2)-norm and l (1)-norm objective functions and by applying the three methods to noisy data. Our experiments show that the l (2)-norm is sensitive to noise, whereas the l (1)-norm and Student's t distribution objective functions give relatively stable and reasonable results for noisy data. When noise patterns are complicated, i.e., due to a combination of missing traces, unexpected outliers, and random noise, FWI based on Student's t distribution gives better results than l (1)- and l (2)-norm FWI. We also examine the application of simultaneous-source methods to acoustic FWI based on Student's t distribution. Computing the expectation of the coefficients of gradient and crosstalk noise terms and plotting the signal-to-noise ratio with iteration, we were able to confirm that crosstalk noise is suppressed as the iteration progresses, even when simultaneous-source FWI is combined with Student's t distribution. From our experiments, we conclude that FWI based on Student's t distribution can retrieve subsurface material properties with less distortion from noise than l (1)- and l (2)-norm FWI, and the simultaneous-source method can be adopted to improve the computational efficiency of FWI based on Student's t distribution.
机译:地震全波形反演(FWI)主要基于数据残差的最小二乘优化问题。但是,最小二乘目标函数可能会受其弱点和对噪声的影响。有许多研究通过使用鲁棒的目标函数(例如基于l(1)-范数的目标函数)来增强FWI的鲁棒性。但是,当残差波场非常接近零时,l(1)范数可能会遇到奇点问题。最近,Student's t分布已应用于声学FWI,从而为噪声数据提供合理的结果。与正态分布相比,Student's t分布具有过度分散的密度函数,因此对于具有异常值的数据很有用。在这项研究中,我们通过将弹性FWI的基本特性与l(2)范数和l(1)范数目标函数的基本特性进行比较,并将这三种方法应用于噪声数据,研究了学生t分布用于弹性FWI的可行性。我们的实验表明,l(2)范数对噪声敏感,而l(1)范数和Student的t分布目标函数为嘈杂数据提供了相对稳定和合理的结果。当噪声模式复杂时(即,由于缺少迹线,意外的离群值和随机噪声的组合),基于Student t分布的FWI提供的结果要好于l(1)-和l(2)-范数FWI。我们还研究了基于学生t分布的同时源方法在声学FWI中的应用。通过计算梯度和串扰噪声项的系数期望值并绘制迭代信噪比,即使在同时源FWI与Student's t相结合的情况下,我们也可以确认随着迭代的进行,串扰噪声得到了抑制。分配。从我们的实验中,我们得出结论,基于学生t分布的FWI可以获取比l(1)-和l(2)-范数FWI更少的噪声失真的地下材料属性,并且可以采用同时源方法来改进基于学生t分布的FWI计算效率。

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