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

被引:26
|
作者
Li, J. H. [1 ]
Zhu, Z. Q. [1 ]
Liu, S. C. [2 ]
Zeng, S. H. [3 ]
机构
[1] Cent S Univ, Sch Earth Sci & Infophys, Changsha 410083, Hunan, Peoples R China
[2] China Univ Min & Technol, Sch Resource & Geosci, Xuzhou 221116, Peoples R China
[3] China Univ Geosci, Inst Geophys & Geomet, Wuhan 430074, Peoples R China
关键词
transient electromagnetic method; central loop; vector finite element method; numerical simulation; 3-DIMENSIONAL BODY; 2-D;
D O I
10.1088/1742-2132/8/4/008
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
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.
引用
收藏
页码:560 / 567
页数:8
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