张小艳,赵星,熊峰,等. 内蒙古地倾斜观测主要干扰信号的功率谱密度特征[J]. 华北地震科学,2022, 40(3):62-68. doi:10.3969/j.issn.1003−1375.2022.03.010.
引用本文: 张小艳,赵星,熊峰,等. 内蒙古地倾斜观测主要干扰信号的功率谱密度特征[J]. 华北地震科学,2022, 40(3):62-68. doi:10.3969/j.issn.1003−1375.2022.03.010.
ZHANG Xiaoyan,ZHAO Xing,XIONG Feng,et al. Power Spectral Density Characteristics of Main Interference Signals of Tilt Observation in Inner Mongolia[J]. North China Earthquake Sciences,2022, 40(3):62-68. doi:10.3969/j.issn.1003−1375.2022.03.010.
Citation: ZHANG Xiaoyan,ZHAO Xing,XIONG Feng,et al. Power Spectral Density Characteristics of Main Interference Signals of Tilt Observation in Inner Mongolia[J]. North China Earthquake Sciences,2022, 40(3):62-68. doi:10.3969/j.issn.1003−1375.2022.03.010.

内蒙古地倾斜观测主要干扰信号的功率谱密度特征

Power Spectral Density Characteristics of Main Interference Signals of Tilt Observation in Inner Mongolia

  • 摘要: 选取内蒙古地区地倾斜观测资料的正常背景和受大风、降雨、气压干扰及地震波影响的典型数据,采用功率谱密度(PSD)分析方法,对其正常背景和4种主要干扰信号的功率谱密度特征进行分析。结果表明,在正常背景下,每日PSD结果基本一致,秒采样较分采样数据可多获得8.3 mHz~0.5 Hz频段的高频信息;大风干扰对大于10−3 Hz频段产生影响,并对秒采样数据会造成第二类地脉动噪声信号能量显著增加;降雨干扰主要影响低于10−4 Hz频段,对秒采样数据的0.01~0.10 Hz频段还会产生一定影响;气压干扰影响的是10−4~10−3 Hz和0.01~0.10 Hz频段,对秒采样数据可能会引起第二类地脉动噪声信号能量的明显增加;地震波影响的频段范围、噪声变幅与观测仪器记录到的地震波最大振幅、持续时间呈正比。这4种干扰信号均表现为影响频段内背景噪声明显高于平静日。

     

    Abstract: Based on the Power Spectral Density (PSD) analysis method, the power spectral density characteristics of typical tilt observation data in Inner Mongolia, which on normal time or affected by gale, rainfall, barometric pressure and seismic wave is analyzed. The results show that: under the normal background, the daily PSD results are basically the same, and the second sampling data can obtain 8.3 mHz ~ 0.5 Hz high frequency information more than the minute sampling data; the gale interference affects frequency bands greater than 10−3 Hz, and causes significant increase in the energy of the second kind of ground pulsation noise signal to the second sampling data; the rainfall interference mainly affects the frequency band lower than 10−4 Hz, and also affects the 0.01 ~ 0.10 Hz frequency band of second sampling data; the barometric interference affects the 10−4 ~ 10−3 Hz and 0.01 ~ 0.10 Hz frequency band, and also may cause significant increase in the energy of the second kind of ground pulsation noise signal to the second sampling data; the frequency range and noise amplitude affected by seismic wave are directly proportional to the maximum amplitude and duration of seismic waves recorded by observation instruments. Moreover, in the affected frequency band, the background noise of the four kinds of interference signals is significantly higher than that in the quiet day.

     

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