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A secondary field based hp-Finite Element Method for the simulation of magnetotelluric measurements

机译:基于次级场的hp有限元方法,用于模拟大地电磁测量

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In some geophysical problems, it is sometimes possible to divide the subsurface resistivity distribution as a one dimensional (1D) contribution plus some two dimensional (2D) inhomogeneities. Assuming this scenario, we split the electromagnetic fields into their primary and secondary components, the former corresponding to the 1D contribution, and the latter to the 20 inhomogeneities. While the primary field is solved via an analytical solution, for the secondary field we employ a multi-goal oriented self-adaptive hp-Finite Element Method (FEM). To truncate the computational domain, we design a Perfectly Matched Layer (PML) that automatically adapts to high-contrast materials that appear in the subsurface and in the air-ground interface. Numerical results illustrate the robustness of the proposed PML and the gains of the secondary field approach, where we obtain results with comparable accuracy than with a full field based formulation but with a much lower computational cost. (C) 2015 Elsevier B.V. All rights reserved.
机译:在某些地球物理问题中,有时可以将地下电阻率分布划分为一维(1D)贡献加上一些二维(2D)不均匀性。假设发生这种情况,我们将电磁场分为它们的主要和次要成分,前者对应于一维贡献,而后者对应于20种不均匀性。通过解析解决方案解决主场时,对于次场,我们采用面向多目标的自适应hp有限元方法(FEM)。为了截断计算域,我们设计了一个完美匹配层(PML),该层可以自动适应出现在地下和空中地面接口中的高对比度材料。数值结果说明了所提出的PML的鲁棒性和二次场方法的收益,与基于全场的公式相比,我们获得的结果具有可比的准确性,但计算成本却低得多。 (C)2015 Elsevier B.V.保留所有权利。

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