3D airborne electromagnetic data inversion basing on the block coordinate descent method

GEOPHYSICS Pub Date : 2024-05-22 DOI:10.1190/geo2023-0673.1
Zhang Bo, Kelin Qu, C. Yin, Yunhe Liu, X. Ren, Yang Su, V. Baranwal
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Abstract

Airborne electromagnetic (AEM) surveys usually covers a large area and create a large amount of data. This has limited the application of three-dimensional (3D) AEM inversions. To make 3D AEM data inversion at a large scale possible, the local mesh method has been proposed to avoid solving large matrix equations in 3D AEM modeling. However, the local mesh only saves the computational cost and memory during forward modeling and Jacobian calculations. When the survey area is very large, the cost for storing and solving the inversion equations can be very high. This brings big challenges to practical 3D AEM inversions. To solve this problem, we develop a 3D scheme based on the block coordinate descent (BCD) method for inversions of large-scale AEM data. The BCD method divides the inversion for large models into series of small-local inversions, so that we can avoid solving the large matrix equations. Numerical experiments demonstrate that the BCD method can get very similar results to those from the existing inversion methods but saves huge amounts of memory.
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基于块坐标下降法的三维机载电磁数据反演
机载电磁(AEM)勘测通常覆盖面积大,产生的数据量大。这限制了三维(3D)AEM 反演的应用。为了实现大规模的三维 AEM 数据反演,人们提出了局部网格法,以避免在三维 AEM 建模中求解大型矩阵方程。然而,局部网格法只能在正演建模和雅各布计算时节省计算成本和内存。当勘测区域非常大时,存储和求解反演方程的成本会非常高。这给实际的三维 AEM 反演带来了巨大挑战。为了解决这个问题,我们开发了一种基于块坐标下降(BCD)方法的三维方案,用于大规模 AEM 数据的反演。BCD 方法将大型模型的反演分为一系列小局部反演,从而避免了求解大型矩阵方程。数值实验证明,BCD 方法能得到与现有反演方法非常相似的结果,但能节省大量内存。
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