通过组稀疏性与拉顿算子实现稳健的多维重建

GEOPHYSICS Pub Date : 2024-01-17 DOI:10.1190/geo2023-0465.1
Ji Li, Dawei Liu
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引用次数: 0

摘要

地震数据处理,特别是去噪和插值等任务,往往取决于线性系统的稀疏解。组稀疏性通过增强稀疏反演在这方面发挥着重要作用。它引入了更精细的约束条件,保留了地震数据中的固有关系。为此,我们提出了一种稳健的正交匹配追寻算法,结合频率-慢度 f- p 域中的拉顿算子,来解决强组稀疏性问题。这种方法对于同时插值地震数据和衰减不稳定噪声至关重要。我们的算法利用了组稀疏性的优势,在每次迭代中选择主要的慢度组,并通过交替方向乘法(ADMM)求解器以稳健的 ℓ1-ℓ1 准则拟合 Radon 系数。它能够抵御不稳定噪声,在同步源去耦和高噪声陆上数据集重建等应用中表现出色,突出了组稀疏性的重要性。合成和实际对比分析进一步证明,强组稀疏性反演始终优于没有组稀疏性约束的相应传统方法。这些比较强调了在这些应用中整合群稀疏性的必要性,从而显示了群稀疏性在优化地震数据处理中不可或缺的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Robust multi-dimensional reconstruction via Group Sparsity with Radon operators
Seismic data processing, specifically tasks like denoising and interpolation, often hinges on sparse solutions of linear systems. Group sparsity plays an essential role in this context by enhancing sparse inversion. It introduces more refined constraints, which preserve the inherent relationships within seismic data. To this end, we propose a robust Orthogonal Matching Pursuit algorithm, combined with Radon operators in the frequency-slowness f- p domain, to tackle the strong group-sparsity problem. This approach is vital for interpolating seismic data and attenuating erratic noise simultaneously. Our algorithm takes advantage of group sparsity by selecting the dominant slowness group in each iteration and fitting Radon coefficients with a robust ℓ1-ℓ1 norm by the alternating direction method of multipliers (ADMM) solver. Its ability to resist erratic noise, along with its superior performance in applications such as simultaneous source deblending and reconstruction of noisy onshore datasets, underscores the importance of group sparsity. Both synthetic and real comparative analyses further demonstrate that strong group sparsity inversion consistently outperforms corresponding traditional methods without the group sparsity constraint. These comparisons emphasize the necessity of integrating group sparsity in these applications, thereby showing its indispensable role in optimizing seismic data processing.
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