基于自适应幅度估计的层析全波形鲁棒反演

A. Almomin
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引用次数: 0

摘要

本文研究了层析全波形反演(TFWI)缓慢收敛的基础,发现其背后的原因是正则化项设计中幅度和相位的不平衡效应。这种不平衡导致运动更新对幅度拟合的强烈依赖,减缓了收敛速度。为了缓解这个问题,我对层析反演提出了两个修改。首先,通过修改正则化项使其更加关注相位信息;其次,同时更新源函数进行建模。调整减少了梯度伪影,并允许对残差的幅度和相位进行显式控制。层析全波形反演(Symes, 2008;Sun and Symes, 2012;Biondi和Almomin, 2012)是一种创新的反演技术,它保留了全波形反演(FWI)的所有优点和优点,同时绕过了其严格的初始模型要求和周期跳变挑战。为了实现这一目标,TFWI通过将经典形式与改进形式的波动方程偏移速度分析(WEMVA)相结合来改变FWI。这种组合表现为通过虚拟轴对速度模型的扩展(Biondi和Almomin, 2013)。无论初始模型的精度如何,建模算子都可以利用扩展轴的运动学信息,不考虑周期跳变的发生,通过将速度模型扩展到适当的轴来匹配观测数据。反演的目的是从虚拟轴中提取所有基本信息,并将其平滑地折叠回模型的原始非扩展形式。成功地反演了数据的运动学和动力学信息,具有出色的鲁棒性和精度。尽管跳过周期不是TFWI的问题,但这种方法也有自己的挑战,即;它的高计算成本和需要的大量迭代(Almomin和Biondi, 2013)。传统的FWI每次迭代只使用一个频率来匹配相位(Pratt, 1999;Shin and Ha, 2008)。不使用振幅降低了解决方案的准确性,因为它阻止了尺度的同时反演。修改梯度计算是另一种用于减少一些“运动学”伪影的方法(Fei和Williamson, 2010;Shen and Symes, 2015)。这些方法适用于图像域速度分析方法,如WEMVA。非线性建模算子和数据空间残差的显式计算使其无法应用于TFWI。提出了对TFWI的两种调整,以减少缓慢的收敛,并允许更多地控制幅度和相位之间的比率。这些调整在TFWI框架中是一致的,并允许对数据空间中的梯度进行精确计算。调整进行了测试,并导致在梯度中的运动学伪影的减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Robust Tomographic Full Waveform Inversion using Adaptive Amplitude Estimation
I examine the basis of slow convergence of tomographic full waveform inversion (TFWI) and discover that the reason behind it is the unbalanced effects of amplitudes and phase in the design of the regularization term. This imbalance results in a strong reliance of the kinematic updates on the amplitude fitting, slowing down the convergence. To mitigate the problem I propose two modifications to the tomographic inversion. First, by modifying the regularization term to focus more on the phase information, and second, simultaneously updating the source function for modeling. The adjustments reduce the gradient artifacts and allow for explicit control over the amplitudes and phases of the residuals. Tomographic full waveform inversion (Symes, 2008; Sun and Symes, 2012; Biondi and Almomin, 2012) is an innovative inversion technique that preserves all the advantages and benefits of full waveform inversion (FWI) while at the same time bypassing its strict initial model requirement and cycle-skipping challenges. To reach this objective, TFWI alters FWI by merging its classical form with a modified form of wave-equation migration-velocity analysis (WEMVA). This combination displays itself as an extension of the velocity model through virtual axes (Biondi and Almomin, 2013). The modeling operator is able to match the observed data by extending the velocity model with the proper axis, no matter what the accuracy of the initial model is, by using kinematic information from the extended axis with disregard to the occurrence of cycle skipping. The inversion is set up to extract all the essential information from the virtual axes and smoothly fold them back into their original, nonextended form of the model. The kinematic and dynamic information of the data were successfully inverted with exceptional robustness and precision. Even though cycle-skipping is not an issue with TFWI, this method creates its own challenges, which are; its high computational cost and the big number of iterations that it needs (Almomin and Biondi, 2013). The conventional FWI uses only a single frequency per iteration to match the phase (Pratt, 1999; Shin and Ha, 2008). Not using amplitudes reduces the accuracy of the solution because it prevents the simultaneous inversion of scales. Modifying the gradient calculation is another method that is used to reduce some "kinematic" artifacts (Fei and Williamson, 2010; Shen and Symes, 2015). These methods are appropriate for image-domain velocity analysis methods, such as WEMVA. The explicit calculations of the nonlinear modeling operator and residuals in the data space prevents it from being applied in TFWI. Two adjustments to TFWI are proposed to reduce the slow convergence and allow for more control of the ratio between amplitude and phase. These adjustments are consistent in the framework of TFWI and allow for an accurate calculation of the gradient in the data space. The adjustments were tested and resulted in a reduction in the kinematic artifacts in the gradient.
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