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Seabed propagation of ULF/ELF electromagnetic fields from harmonic dipole sources located on the seafloor

机译:来自海底谐波偶极子源的ULF / ELF电磁场在海底的传播

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摘要

The amplitudes of the quasi-static electromagnetic fields generated at points on the seafloor by harmonic dipole sources (vertically directed magnetic dipoles, horizontally directed magnetic dipoles, vertically directed electric dipoles, and horizontally directed electric dipoles) also located on the seafloor are computed using a numerical integration technique. The primary purpose of these computations is to obtain field amplitudes that can be used in undersea communication studies. An important secondary purpose is to examine the enhancements of the fields produced at moderate to large distances by the presence of the relatively less conducting seafloor, as compared with the fields produced at the same distances in a sea of infinite extent, for frequencies in the ULF/ELF bands (frequencies less than 3 kHz). These latter enhancements can be surprisingly large, with increases of 4 orders of magnitude or more being typical at distances of 20 seawater skin depths.
机译:谐波偶极子源(垂直方向的磁偶极子,水平方向的磁偶极子,垂直方向的电偶极子和水平方向的电偶极子)也位于海底,在海底的点上生成的准静态电磁场的幅度是使用数值积分技术。这些计算的主要目的是获得可用于海底通信研究的场振幅。一个重要的次要目的是针对ULF中的频率,检查与无限距离海中相同距离处产生的磁场相比,由于传导性相对较小的海底的存在,对中等至较大距离处产生的磁场的增强作用/ ELF频段(频率小于3 kHz)。后面这些增强可能会令人惊讶地大,在20个海水表层深度处,典型地增加4个数量级或更多。

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