地震地质

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人工源极低频电磁波场空间分布的计算

杨静1,陈小斌2,3,赵国泽3   

  1. 1. 山西省地震局临汾中心地震台
    2. 应急管理部国家自然灾害防治研究院
    3. 中国地震局地质研究所
  • 收稿日期:2020-10-12 修回日期:2021-04-02 发布日期:2021-09-26
  • 通讯作者: 陈小斌
  • 基金资助:
    中国地震局星火计划项目;国家发展改革委项目;极低频探地工程地震预测分系统;国家自然科学基金项目

Calculation of Spatial Distribution of CSELF Electromagnetic Field

Yang Jing1,XIao-Bin CHEN2,3, 1   

  1. 1.
    2. Institute 哦发Geology,CEA
    3. National Institute of Natural Hazards,MEMC
  • Received:2020-10-12 Revised:2021-04-02 Published:2021-09-26
  • Contact: XIao-Bin CHEN

摘要: 本文对人工源极低频(CSELF)电磁波空间传播特征进行了较为细致的研究。CSELF电磁波的空间传播区域可划分为近区、远区和波导区。在近区和远区,CSELF电磁波的传播理论与CSAMT相似,本文整理、验证了已有文献中的场强计算公式;在波导区,借鉴无线电通信技术成果,本文给出了地球-大气层-电离层球形谐振腔模型的CSELF电磁波的近似计算公式;在此基础上,设计了可视化软件,实现了三种坐标系下CSELF电磁波场的计算;最后依据计算结果分析了CSELF在近区、远区、波导区的空间传播特征。本文研究表明:CSELF的近区场和远区场衰减很快,而波导区场衰减较慢;电场比磁场更早进入波导区;在地球模型下,场源对极点附近出现了波导区场强增大现象,显示了与水平地层模型完全不同的电磁波传播特征。此外,还认识到,基于水平电偶极子源的频率域电磁测深中,远区测深主要依赖于磁场而非电场。本文的研究为CSELF的应用提供了理论和计算方面的支持。

关键词: CSELF, 感应场, 辐射场, 波场分布, 电磁测深

Abstract: This paper has carried out a more detailed study on the spatial propagation characteristics of the electromagnetic (EM) of controlled-source extremely low frequency (CSELF). The CSELF EM waves cover almost all sections of space which can be divided into near, far and waveguide zones. The propagation theory of CSELF EM wave is similar to CSAMT in the near and far Zones, and we collated and verified the field strength calculation formulas in the existing literature. While in the waveguide zone, learned the achievements of communication technology, this paper presents the approximate calculation formula of CSELF EM wave of the earth-air-ionosphere spherical cavity model. Based on the above, this paper has complied a piece of visualized software for calculation of the CSELF EM field in three coordinate systems (Cartesian, cylindrical and spherical coordinates). Finally, according to the calculation results, the spatial propagation characteristics of CSELF in the near area, far area and waveguide area are analyzed.The results show that the decay of CSELF EM field intensity is rapid in the near and far zone, but slightly slow in the far zone, and the electric field enters the waveguide zone earlier than the magnetic field. Under the earth model, there is an increase in the field strength in the waveguide area near the antipole of the dipole source which shows completely different EM waves propagation characteristics in horizontal formation model. In addition, it is also recognized that in the frequency domain EM sounding based on the horizontal electric dipole source, the far-field sounding mainly depends on the magnetic field rather than the electric field. The research in this paper provides theoretical and computational support for the application of CSELF.

Key words: CSELF, Induction field, Radiation field, Wave field distribution, Electromagnetic sounding