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首页> 外文期刊>Geoscience and Remote Sensing Letters, IEEE >Application of Optimal Transport to Exact Zoeppritz Equation AVA Inversion
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Application of Optimal Transport to Exact Zoeppritz Equation AVA Inversion

机译:最优输运在精确Zoeppritz方程AVA反演中的应用

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摘要

Since most information on S-wave velocity and density exists in the middle to large angle range of seismic data, traditional inversion methods based on the Zoeppritz approximation have difficulty in obtaining satisfactory results. Therefore, as a high-accuracy amplitude varied with angle (AVA) inversion, exact Zoeppritz (EZ) equation inversion has aroused a lot of attention in recent years. As for any other nonlinear inversion, iterative convergence and error are the important problems. In this letter, based on a Bayesian framework, we introduce optimal transport into EZ equation AVA inversion. Then, the limited-memory Broyden–Fletcher–Goldfarb–Shanno method is adopted to solve the regularization-constrained least-square argument function to obtain the inversion results, including P-wave velocity, S-wave velocity, and density. We compare this method with a conventional method, which is based on an Ln2nnorm or weighted Ln2nnorm as a residual method in the model test. The results show that the proposed method not only reduces the error of the results to be smaller than Ln2nnorm, but it also improves the convergence rate.
机译:由于有关S波速度和密度的大多数信息都存在于地震数据的中到大角度范围内,因此基于Zoeppritz近似的传统反演方法很难获得令人满意的结果。因此,随着高精度振幅随角度(AVA)反演而变化,精确的Zoeppritz(EZ)方程反演引起了近年来的广泛关注。对于任何其他非线性反演,迭代收敛和误差是重要的问题。在这封信中,基于贝叶斯框架,我们将最佳输运量引入EZ方程AVA反演。然后,采用有限内存的Broyden–Fletcher–Goldfarb–Shanno方法求解正则化约束的最小二乘自变量函数,以获得反演结果,包括P波速度,S波速度和密度。我们将此方法与基于Ln 2 nnorm或加权Ln 2 nnorm作为模型测试中的残差方法。结果表明,所提出的方法不仅将结果的误差减小到小于Ln 2nnorm,但这也提高了收敛速度。

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