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极地甚低频电磁波跨冰层传播衰减特性分析

张嘉雨 冯士民 窦高奇 代晨鹏 王臻 王颢

张嘉雨, 冯士民, 窦高奇, 等. 极地甚低频电磁波跨冰层传播衰减特性分析[J]. 水下无人系统学报, 2024, 32(5): 1-9 doi: 10.11993/j.issn.2096-3920.2024-0100
引用本文: 张嘉雨, 冯士民, 窦高奇, 等. 极地甚低频电磁波跨冰层传播衰减特性分析[J]. 水下无人系统学报, 2024, 32(5): 1-9 doi: 10.11993/j.issn.2096-3920.2024-0100
Zhang Jiayu, FENG Shimin, DOU Gaoqi, Dai Chenpeng, WANG Zhen, WANG Hao. Analysis of attenuation characteristics of polar VLF electromagnetic wave propagation across ice[J]. Journal of Unmanned Undersea Systems. doi: 10.11993/j.issn.2096-3920.2024-0100
Citation: Zhang Jiayu, FENG Shimin, DOU Gaoqi, Dai Chenpeng, WANG Zhen, WANG Hao. Analysis of attenuation characteristics of polar VLF electromagnetic wave propagation across ice[J]. Journal of Unmanned Undersea Systems. doi: 10.11993/j.issn.2096-3920.2024-0100

极地甚低频电磁波跨冰层传播衰减特性分析

doi: 10.11993/j.issn.2096-3920.2024-0100
基金项目: 国家自然科学基金项目资助(61871473), 海军工程大学自主研发计划项目(2023503090).
详细信息
    作者简介:

    张嘉雨(2000), 男, 博士研究生, 水下通信、低频通信

  • 中图分类号: TN91, TN92

Analysis of attenuation characteristics of polar VLF electromagnetic wave propagation across ice

  • 摘要: 随着极地科学考察和资源勘探活动的增加, 极地海冰环境中的通信探测设备得到了广泛应用。甚低频(VLF)电磁波由于其能够穿透海水的特性, 成为在极地环境下进行跨介质通信的可靠方法。本文针对极地甚低频电磁波在跨冰层传播中的问题, 建立了基于传输矩阵的多层介质传播模型。通过二端口网络等效电路方法, 研究了甚低频电磁波在空气-冰层-海水中的衰减特性以及入射角度的影响。通过结合仿真模拟和实地实验数据, 首次量化了在冰层中的甚低频电磁波的场强衰减规律, 揭示了每米冰层厚度衰减不足1 dB的重要发现。评估了海冰对极地VLF通信的影响, 结果表明海冰对VLF电磁波的损耗较小, 不是影响VLF通信的主要因素。

     

  • 图  1  电磁波跨空-冰-海3层介质模型结构

    Figure  1.  Electromagnetic wave cross-space-ice-sea-sea four layer medium model structure

    图  2  3 kHz、30 kHz平面电磁波入射海水与海冰的入射角和反射角关系

    Figure  2.  Relation between incidence angle and reflection angle of 3 kHz and 30 kHz planar electromagnetic wave incident seawater and sea ice

    图  3  VLF电磁波入射海水和海冰平均每米衰减情况

    Figure  3.  Average attenuation per meter of VLF electromagnetic wave incident seawater and sea ice e

    图  4  电磁波的“等效电路”形式

    Figure  4.  ‘Equivalent circuit’ form of electromagnetic wave

    图  5  空-冰-海模型结构仿真示意图

    Figure  5.  Schematic diagram of the structural simulation of the air-ice-sea model

    图  6  18.2 kHz电磁波在空-冰-海结构中电磁场随垂直距离变化情况

    Figure  6.  18.2 kHz electromagnetic waves Variation of electromagnetic fields with vertical distance in an air-ice-sea structure

    图  7  主要VLF长波台跨介质归一化电场强度随垂直距离变化情况

    Figure  7.  Variation of the cross-medium normalized electric field intensity of the main VLF long-wave stations with vertical distance

    图  8  主要VLF长波台跨介质归一化磁场强度随垂直距离变化情况

    Figure  8.  Variation of the cross-medium normalized magnetic field intensity of the main VLF long-wave stations with vertical distance

    图  9  海底对海冰和海水磁场强度影响情况

    Figure  9.  Effecf of the seabed on the magnetic field intensity of sea ice and seawater

    图  10  实验原理与实验现场

    Figure  10.  Experimental principle and experimental site

    图  11  数据采集设备

    Figure  11.  Data acquisition equipment

    图  12  (a)设备全局接收图(b)设备局部接收图(c)0 kHz-400 kHz瀑布图数据记录图

    Figure  12.  (a) Device global reception diagram (b) Device local reception diagram (c) 0 kHz-400 kHz waterfall diagram data recording diagram

    图  13  (a)冰层上方数据记录图(b)冰层下方数据记录图(c)海水1.2 m处数据记录图

    Figure  13.  (a) Data record above the ice sheet (b) data record below the ice sheet (c) Data record at 1.2m of seawater

    图  14  实验数据记录

    Figure  14.  Experimental data recording

    图  15  部分实验过程数据记录图

    Figure  15.  Part of experimental process data recording

    图  16  长波发信台信号传播示意图

    Figure  16.  Signal propagation diagram of long wave transmitting station

    图  17  JJI台—北极黄河站信号传播示意图

    Figure  17.  Schematic diagram of signal propagation at JJI—Arctic Yellow River Station

    表  1  仿真参数

    Table  1.   Ssimulation parameters

    介质 $\mu $ $\sigma $/(S/m) $\varepsilon $ 厚度/m
    空气 1 1 1 无限大
    冰层 1 0.03~0.0003 3~9 1~5
    海水 1 2.5~3.33 81 无限大
    下载: 导出CSV
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出版历程
  • 收稿日期:  2024-05-30
  • 修回日期:  2024-08-15
  • 录用日期:  2024-09-09
  • 网络出版日期:  2024-10-16

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