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Dimensionally adaptive hp-finite element simulation and inversion of 2D magnetotelluric measurements

机译:尺寸自适应hp有限元模拟和二维大地电磁测量反演

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摘要

Magnetotelluric (MT) problems often contain different subdomains where the conductivity of the media depends upon one, two, or three spatial variables. Traditionally, when a MT problem incorporates a three-dimensional (3D) subdomain, the numerical method employed for simulation and inversion was 3D over then entire domain. In here, we propose to take advantage of the possibly lower dimensionality of certain subdomains during the inversion process. By doing so, we obtain significant computational savings (up to 75% in some scenarios) and increased accuracy on the results. We numerically illustrate this method by employing two dimensional (2D) computations based on a multi-goal oriented hp-adaptive Finite Element Method (FEM) that exhibits superior convergence properties. Additionally, we provide a formulation for implementing an efficient adjoint based method for the computation of the derivatives of the impedance, and we show the importance of the (a) proper selection of the inversion variable, and (b) the advantages of using both the Transverse Electric (TE) and Transverse Magnetic (TM) measurements for the proper inversion of MT data. (C) 2016 Elsevier B.V. All rights reserved.
机译:大地电磁(MT)问题通常包含不同的子域,其中介质的电导率取决于一个,两个或三个空间变量。传统上,当MT问题包含三维(3D)子域时,用于模拟和反演的数值方法是整个域上的3D。在这里,我们建议在反演过程中利用某些子域的可能较低的维数。这样,我们可以节省大量计算量(在某些情况下,最高可达75%),并提高了结果的准确性。我们通过使用二维(2D)计算来数字化地说明此方法,该计算基于多目标定向的hp自适应有限元方法(FEM),它显示出优异的收敛性。此外,我们提供了一种公式,用于实现基于有效的基于伴随的方法来计算阻抗的导数,并且我们展示了(a)正确选择反演变量,以及(b)同时使用两个变量的优点的重要性。横向电学(TE)和横向磁学(TM)测量,用于正确反转MT数据。 (C)2016 Elsevier B.V.保留所有权利。

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