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Ultra-low-frequency electromagnetic waves in the Earth's crust and magnetosphere

机译:地壳和磁层中的超低频电磁波

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摘要

Research on natural intra- and extraterrestrially produced electromagnetic waves with periods ranging from 0.2 to 600 s is reviewed. The way in which the energy of rock movements transforms into the energy of an alternating magnetic field is analyzed. Methods for detecting seismomagnetic signals against a strong background are described. In discussing the physics of ultra-low-frequency waves in the magnetosphere, the 11-year activity modulation of 1-Hz waves and ponderomotive forces affecting plasma distribution are emphasized.
机译:本文综述了周期为0.2至600 s的自然的内外地电磁波的研究。分析了岩石运动的能量转化为交变磁场的能量的方式。描述了在强背景下检测地震磁信号的方法。在讨论磁层中的超低频波的物理过程时,强调了11年的1-Hz波活动调制和影响等离子体分布的质动力。

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