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Modular implementation of magnetotelluric 2D forward modeling with general anisotropy

机译:具有一般各向异性的大地电磁二维正演建模的模块化实现

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摘要

We present a general framework for two-dimensional finite difference modeling of magnetotelluric data in the presence of general anisotropy. Our approach is modular, allowing differential operators for a range of formulations of the governing equations, defined on several possible discrete grids, to be constructed from a basic set of first difference and averaging operators. We specifically consider two formulations of the two-dimensional anisotropic problem, one with Maxwell's equations reduced to a second order system in terms of three coupled electric components, and one in terms of coupled electric and magnetic x-components. Both formulations are discretized on a staggered grid; the second (coupled electric and magnetic) system is also implemented on a grid with fixed nodes (i.e., not staggered). The three implementations are validated and compared using a range of test models, including a half-space with general anisotropy, an infinite fault with axial anisotropy and a simple dyke model. Comparisons to analytic results (for half-space and fault models), and to results from other anisotropic codes, combined with grid-refinement convergence tests, demonstrate that our algorithms are accurate and capable of routine modeling of two-dimensional general anisotropy. These finite difference codes, demonstrating the flexibility of our numerical discretization approach, can be readily applied to other problems.
机译:我们提出了在存在大体各向异性的情况下对大地电磁数据进行二维有限差分建模的一般框架。我们的方法是模块化的,允许从一组基本的一阶差分和求平均值算子构造微分算子,用于在多个可能的离散网格上定义的一系列控制方程式。我们专门考虑了二维各向异性问题的两种表达方式,一种是将麦克斯韦方程式简化为二阶系统,其中包含三个耦合的电子分量,一个则包含了耦合的电磁x分量。两种公式都在交错的网格上离散化;第二个(电气和磁耦合)系统也实现在具有固定节点(即不交错)的网格上。使用一系列测试模型对这三种实现方式进行了验证和比较,包括具有一般各向异性的半空间,具有轴向各向异性的无限断层和简单的堤坝模型。与分析结果(半空间模型和断层模型)以及其他各向异性代码的结果进行比较,并结合网格细化收敛测试,证明我们的算法准确且能够对二维一般各向异性进行常规建模。这些有限差分代码证明了我们的数字离散化方法的灵活性,可以很容易地应用于其他问题。

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