Entropy Regularized Nonlinear Joint PP-PS AVO Inversion Using Zoeppritz Equations

被引:1
|
作者
Xue, Yaru [1 ,2 ]
Su, Junli [1 ,2 ]
Geng, Weiheng [3 ]
Chen, Xiaohong [1 ]
Feng, Luyu [1 ,2 ]
Liang, Qi [1 ,2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, CNPC Key Lab Geophys Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Coll Informat Sci & Engn, Beijing 102249, Peoples R China
[3] Tsinghua Univ, Dept Automat, Beijing 100084, Peoples R China
关键词
Entropy; Mathematical models; Stability analysis; Uncertainty; Reservoirs; Reflection; Petroleum; Amplitude entropy regularization; joint inversion; quantum annealing (QA) algorithm; Zoeppritz equation; AMPLITUDE VARIATION; BAYESIAN-INFERENCE;
D O I
10.1109/TGRS.2024.3388579
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Based on the Bayesian framework, pre-stack inversion aims to find the solution with the maximum posterior probability under the prior constraint. The prior constraint is usually a mathematical expression of the inverted parameters and guides the updating of the inversion results. To obtain a stable, high-resolution, and high-fidelity inversion result, we introduce a new prior constraint named "amplitude entropy" to help perform the pre-stack inversion. The amplitude entropy can make the chaos of the parameters to be inverted close to those of the known well-logging data. Compared with the traditional $L_{2}$ prior constraint, amplitude entropy can improve the resolution of the inversion results, and compared with the conventional $L_{1}$ prior constraint, it can obtain a solution that is more consistent with the geological characteristics. In addition, multicomponent seismic data contain richer lithology and fluid information than single-component data. Therefore, in this article, we directly develop the pre-stack inversion method based on the multicomponent seismic data. Furthermore, due to the high nonlinearity of the objective function under the amplitude entropy constraint, the quantum annealing (QA) algorithm is employed to solve the objective function of the joint inversion and find the final solution. Synthetic and field data examples demonstrate that the pre-stack inversion method with the amplitude entropy constraint is effective and stable, especially for processing seismic data with a low signal-to-noise ratio.
引用
收藏
页码:1 / 12
页数:12
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