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Investigation of ULF magnetic anomaly before moderate earthquakes

机译:中地震前超低频磁场异常的研究

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Electromagnetic anomalies covering a wide range of frequencies from ultra low frequency (ULF), very low frequency (VLF) up to very high frequency (VHF) have been observed before earthquakes. However, the ULF range emissions provide a greater source of information regarding the earthquake precursor. One of the main techniques of investigating such a precursor is by using a magnetic sensor. In this paper, we have carried out a study of spectral density (magnetic field intensity) and polarization ratio methods to extract earthquake precursory signatures of the ULF data for moderate earthquakes (magnitude M_b = 3.7—4.8), using a three-component induction coil magnetometer installed at Shivaji University, Kolhapur (16.40°N, 74.15°E), India. We have applied a Fast Fourier Transform (FFT) procedure to calculate the spectral density of the ULF time series. We have found enhancement in ULF magnetic field intensity 3 to 5 days before the main shock and this specific enhancement appeared ±3 h around the main shock time in the 1 -5 Hz frequency range. We have examined ULF variations with polarization values and K_p index data. Magnetic field intensity of ULF data can give important information about earthquake preparation processes and it can be involved in the development of earthquake prediction methodology.
机译:在地震发生之前,已经观察到电磁异常涵盖了从超低频(ULF),极低频(VLF)到极高频(VHF)的广泛频率范围。但是,ULF范围发射提供了有关地震前兆的更多信息源。研究这种前体的主要技术之一是使用磁传感器。在本文中,我们进行了频谱密度(磁场强度)和极化率方法的研究,以使用三分量感应线圈提取中度地震(震级M_b = 3.7-4.8)的ULF数据的地震前兆特征。磁力计安装在印度Kolhapur的Shivaji大学(16.40°N,74.15°E)。我们已经应用了快速傅立叶变换(FFT)程序来计算ULF时间序列的频谱密度。我们发现在主震前3至5天ULF磁场强度得到了增强,并且这种特定的增强在1 -5 Hz频率范围内的主震时间附近出现了±3 h。我们已经检查了极化强度和K_p指数数据的ULF变化。 ULF数据的磁场强度可以提供有关地震准备过程的重要信息,并且可以参与地震预测方法的开发。

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