Quadrature-Based Restarted Arnoldi Method for Fast 3-D TEM Forward Modeling of Large-Scale Models

Kailiang Lu;Jianhua Yue;Jianmei Zhou;Ya’Nan Fan;Kerui Fan;He Li;Xiu Li
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Abstract

For large-scale geophysical models, the order of the coefficient matrix in 3-D transient electromagnetics (TEMs) forward modeling can reach millions or even tens of millions. Balancing computational efficiency and memory usage presents a challenge worthy of in-depth exploration. In this letter, we utilize an integral representation of the iterative error in the Arnoldi method to construct an efficient quadrature-based restarted forward algorithm. First, the mimetic finite volume (MFV) method on a staggered hexahedral grid is employed to discretize the time-domain Maxwell’s equations, expressing the TEM response after the step-off waveform shutoff as the product of the matrix exponential function $f({\text {A}})$ and vector b. Then, using Cauchy’s integral formula, the expression of ${f}({\text {A}}){b}$ is transformed into an integral form and approximated using the restarted Arnoldi (RA) algorithm. Our method does not require solving linear systems and can leverage GPU parallel technology and optimize the RA algorithm parameters to enhance computational efficiency. Comparative studies with other numerical methods validate the advantages and accuracy of our approach, which numerical example demonstrates can fully achieve large-scale fast 3-D TEM forward modeling.
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基于正交法的大尺度瞬变电磁法快速三维正演模拟
对于大尺度地球物理模型,三维瞬变电磁法正演中系数矩阵的阶数可达百万级甚至千万级。平衡计算效率和内存使用是一个值得深入探索的挑战。在本文中,我们利用Arnoldi方法中迭代误差的积分表示来构造一个有效的基于正交的重新启动前向算法。首先,采用交错六面体网格模拟有限体积(MFV)方法对时域麦克斯韦方程组进行离散化,将阶跃波形关闭后的TEM响应表示为矩阵指数函数$f({\text {a}})$与向量b的乘积。然后,利用Cauchy积分公式,将${f}({\text {a}}){b}$的表达式转化为积分形式,并使用重新启动的Arnoldi (RA)算法进行近似。我们的方法不需要求解线性系统,并且可以利用GPU并行技术和优化RA算法参数来提高计算效率。通过与其他数值方法的对比研究,验证了该方法的优越性和准确性,算例表明该方法完全可以实现大尺度快速三维瞬变电磁法正演模拟。
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