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A hybrid solver based on the integral equation method and vector finite-element method for 3D controlled-source electromagnetic method modeling

机译:一种基于整体方程方法的混合求解器和3D控制源电磁法建模的有限元方法

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摘要

The integral equation method (IEM) and differential equation methods have been widely applied to provide numerical solutions of the electromagnetic (EM) fields caused by inhomogeneity for the controlled-source EM method. IEM has a bounded computational domain and has been well-known for its efficiency, whereas differential equation methods are commonly used for complex geologic models. To use the advantages of the two types of approaches, a hybrid method is developed based on the combination of IEM and the edge-based finite-element method (vector FEM). In the hybrid scheme, Maxwell's differential equations of the secondary electric fields in the frequency domain are derived for a volume with boundary placed slightly away from the inhomogeneity. The vector FEM is applied to solve Maxwell's differential equations, and a system of linear equations for the secondary electric fields can be derived by the minimum theorem. The secondary electric fields on the boundary are represented by IEM in terms of the secondary electric fields inside the inhomogeneity. The linear equations from substituting the boundary values into the vector FEM linear equations then can be solved to obtain the secondary electric fields inside the inhomogeneity. The secondary electric fields at receivers are calculated by IEM based on the secondary electric field solutions inside the inhomogeneity. The hybrid algorithm is verified by comparison of simulated results with earlier works on canonical 3D disc models with a high accuracy. Numerical comparisons with two conventional IEMs demonstrate that the hybrid method is more accurate and efficient for highconductivity contrast media.
机译:积分方程方法(IEM)和微分方程方法已被广泛应用于提供由受控源EM方法的不均匀性引起的电磁(EM)场的数值解。 IEM具有有限的计算领域,并且众所周知,效率,而微分方程方法通常用于复杂地质模型。为了利用两种类型的方法的优点,基于IEM和基于边缘的有限元方法(Vector FEM)的组合来开发混合方法。在混合方案中,频域中的次级电场的麦克斯韦尔的微分方程被导出,其中边界略微远离不均匀性。载体FEM被应用于解决Maxwell的微分方程,并且可以通过最小定理导出次级电场的线性方程系统。边界上的二次电场由IEM在不均匀性内的二次电场方面表示。然后可以解决从将边界值代入矢量比线性方程中的线性方程以获得不均匀性内的二次电场。接收器处的二次电场通过IEM基于在不均匀性内的次级电场溶液的基础上计算。通过对先前工作的模拟结果进行仿真结果,验证了混合算法,以高精度的规范3D光盘模型。具有两个常规IEM的数值比较表明,混合方法对高导造影介质更准确且有效。

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    Cent S Univ Sch Geosci &

    Infophys Human Key Lab Nonferrous Resources &

    Geol Hazards Changsha 410083 Hunan Peoples R China;

    Cent S Univ Sch Geosci &

    Infophys Human Key Lab Nonferrous Resources &

    Geol Hazards Changsha 410083 Hunan Peoples R China;

    Cent S Univ Sch Geosci &

    Infophys Human Key Lab Nonferrous Resources &

    Geol Hazards Changsha 410083 Hunan Peoples R China;

    Cent S Univ Sch Geosci &

    Infophys Human Key Lab Nonferrous Resources &

    Geol Hazards Changsha 410083 Hunan Peoples R China;

    Cent S Univ Sch Geosci &

    Infophys Human Key Lab Nonferrous Resources &

    Geol Hazards Changsha 410083 Hunan Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

  • 入库时间 2022-08-20 03:13:49

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