Recent Advances in 2D Frequency-Domain Marine Controlled-Source EM Inversion Using Adjoint Approximate Sensitivities

IF 6.2 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Gang Li, Yutao Liu, Octavio Castillo-Reyes
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Abstract

Marine controlled-source electromagnetic (CSEM) inversion is a widely used technique for imaging subsurface structures beneath the seafloor and exploring hydrocarbon or mineral resources. Although essential for data interpretation, the inversion process is computationally intensive, particularly due to the high memory demands and time consumption associated with sensitivity calculations, even in 2D cases. This paper presents recent advances in frequency-domain marine CSEM inversion algorithms, including a novel method for approximating sensitivities that significantly accelerates 2D inversion without relying on exact sensitivity matrices. A 2.5D frequency-domain CSEM forward modeling solver is employed as a testbed, where the secondary-field formulation is adopted to mitigate source singularities and enhance numerical accuracy. In the developed 2D inversion routine, the sensitivity matrix is computed via the adjoint-state method, integrating the inner product of the adjoint and forward electric fields over each cell during each iteration. The inversion is performed using the Gauss–Newton optimization scheme. To improve computational efficiency, adjoint fields are evaluated over a simplified layered model rather than the full multidimensional true model. Numerical experiments demonstrate that the proposed sensitivity approximation achieves nearly identical inversion performance to that of the exact sensitivities. Results from both synthetic and experimental datasets confirm that the approximate sensitivities are sufficiently accurate to ensure convergence toward geologically meaningful solutions.

Abstract Image

基于伴随近似灵敏度的二维频域海洋可控源电磁反演研究进展
海洋可控源电磁(CSEM)反演是一种广泛应用于海底地下结构成像和油气矿产资源勘探的技术。虽然对数据解释至关重要,但反演过程的计算量很大,特别是由于高内存需求和与灵敏度计算相关的时间消耗,即使在2D情况下也是如此。本文介绍了频率域海洋CSEM反演算法的最新进展,包括一种新的近似灵敏度方法,该方法可以在不依赖精确灵敏度矩阵的情况下显著加速二维反演。采用2.5维频域CSEM正演求解器作为实验平台,采用二次场公式减轻了源奇异性,提高了数值精度。在所开发的二维反演程序中,通过伴随状态法计算灵敏度矩阵,在每次迭代中对每个单元的伴随电场和正演电场的内积进行积分。采用高斯-牛顿优化方案进行反演。为了提高计算效率,在简化的分层模型上计算伴随场,而不是在全多维真模型上计算伴随场。数值实验表明,所提出的灵敏度近似与精确灵敏度近似获得了几乎相同的反演性能。合成数据集和实验数据集的结果证实,近似灵敏度足够精确,可以确保收敛到有地质意义的解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Surveys in Geophysics
Surveys in Geophysics 地学-地球化学与地球物理
CiteScore
10.00
自引率
10.90%
发文量
64
审稿时长
4.5 months
期刊介绍: Surveys in Geophysics publishes refereed review articles on the physical, chemical and biological processes occurring within the Earth, on its surface, in its atmosphere and in the near-Earth space environment, including relations with other bodies in the solar system. Observations, their interpretation, theory and modelling are covered in papers dealing with any of the Earth and space sciences.
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