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Interference effects of aircraft on earth's electromagnetic response at very low frequency and low frequency

机译:飞机在极低频和低频下对地球电磁响应的干扰效应

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摘要

Over the last few decades, very low frequency electromagnetics has been widely and successfully applied in mineral exploration and groundwater exploration. Many radio transmitters with strong signal-to-noise ratios are scattered in the very low frequency band and low frequency band. Based on experiences gained from ground measurements with the radio-magnetotelluric technique operating in the frequency interval 1-250 kHz, broadband magnetometers have been used to cover both very low frequency (3-30 kHz) and low frequency (30-300 kHz) bands to increase the resolution of the near-surface structure. The metallic aircraft as a conductive body will distort the magnetic signal to some extent, and thus it is important to investigate aircraft interference on the electromagnetic signal. We studied noise caused by rotation of an aircraft and the aircraft itself as a metallic conductive body with three methods: 3D wave polarization, determination of transmitter direction and full tipper estimation. Both very low frequency and low frequency bands were investigated. The results show that the magnetic field is independent of the aircraft at low frequencies in the very low frequency band and part of the low frequency band (below 100 kHz). At high frequencies (above 100 kHz), the signals are more greatly influenced by the aircraft, and the wave polarization directions are more scattered, as observed when the aircraft turned. Some aircraft generated noise mixed with radio transmitter signals, detected as 'dummy' signals by the 3D wave polarization method. The estimated scalar magnetic transfer functions are dependent on the aircraft flight directions at high frequencies, because of aircraft interference. The aircraft eigenresponse in the transfer functions (tippers) between vertical and horizontal magnetic field components was compensated for in the real part of the estimated tippers, but some unknown effect was still observed in the imaginary parts.
机译:在过去的几十年中,极低频电磁已广泛成功地应用于矿物勘探和地下水勘探。许多具有高信噪比的无线电发射机分散在非常低的频段和低频段。根据使用频率范围为1-250 kHz的无线电电磁技术进行地面测量获得的经验,宽带磁力计已用于覆盖极低频(3-30 kHz)和低频(30-300 kHz)频段以提高近地表结构的分辨率。金属飞机作为导电体会在某种程度上使磁信号失真,因此研究飞机对电磁信号的干扰非常重要。我们使用三种方法研究了由飞机旋转以及作为金属导电体的飞机本身引起的噪声:3D波极化,确定发射器方向和完全倾翻估计。研究了非常低频和低频频段。结果表明,在非常低的频段和部分低频段(100 kHz以下),低频处的磁场与飞机无关。如飞机转弯时所观察到的,在高频下(100 kHz以上),信号受到飞机的影响更大,并且波极化方向更加分散。一些飞机产生的噪声与无线电发射器信号混合在一起,并通过3D波极化方法检测为“虚拟”信号。由于飞机干扰,估计的标量磁传递函数取决于飞机在高频下的飞行方向。飞机在垂直和水平磁场分量之间传递函数(自卸车)的本征响应在估算的自卸车的实部得到补偿,但在虚部仍观察到一些未知的影响。

著录项

  • 来源
    《Geophysical Prospecting》 |2015年第1期|211-224|共14页
  • 作者

    C. Shan; L.B. Pedersen;

  • 作者单位

    Department of Earth Sciences, Uppsala University, Villavaegen 16, 75236, Uppsala, Sweden;

    Department of Earth Sciences, Uppsala University, Villavaegen 16, 75236, Uppsala, Sweden;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Airborne Electromagnetics; Noise; Signal processing;

    机译:机载电磁;噪声;信号处理;
  • 入库时间 2022-08-18 03:31:21

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