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3D numerical simulation for the transient electromagnetic field excited by the central loop based on the vector finite-element method

机译:基于矢量有限元方法的中心回路激发的瞬变电磁场的3D数值模拟

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摘要

Based on the principle of abnormal field algorithms, Helmholtz equations for electromagnetic field have been deduced. We made the electric field Helmholtz equation the governing equation, and derived the corresponding system of vector finite element method equations using the Galerkin method. For solving the governing equation using the vector finite element method, we divided the computing domain into homogenous brick elements, and used Whitney-type vector basis functions. After obtaining the electric field's anomaly field in the Laplace domain using the vector finite element method, we used the Gaver-Stehfest algorithm to transform the electric field's anomaly field to the time domain, and obtained the impulse response of magnetic field's anomaly field through the Faraday law of electromagnetic induction. By comparing 1D analytic solutions of quasi-H-type geoelectric models, the accuracy of the vector finite element method is tested. For the low resistivity brick geoelectric model, the plot shape of electromotive force computed using the vector finite element method coincides with that of the integral equation method and finite difference in time domain solutions.
机译:根据异常场算法的原理,推导了电磁场的亥姆霍兹方程。我们将电场亥姆霍兹方程作为控制方程,并使用Galerkin方法推导了相应的矢量有限元方法方程组。为了使用矢量有限元方法求解控制方程,我们将计算域划分为均匀的砖块元素,并使用了Whitney型矢量基函数。在使用向量有限元方法获得拉普拉斯域中的电场异常场之后,我们使用了Gaver-Stehfest算法将电场的异常场转换为时域,并通过法拉第获得了磁场异常场的脉冲响应。电磁感应定律。通过比较准H型地电模型的一维解析解,测试了矢量有限元方法的准确性。对于低电阻砖地电模型,使用矢量有限元法计算的电动势的曲线形状与积分方程法和时域解的有限差分一致。

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