义煤矿区冲击地压微震信号频谱特征分析

    Spectrum Characteristic Analysis of Rock Burst Microseismic Signal in Yimei Mining Area

    • 摘要: 利用微震监测系统,搜集了义煤矿区跃进矿、千秋矿和常村矿发生冲击地压时微震信号,对其进行快速傅里叶(FFT)变换,分析微震信号的时域波形及频谱特征。得出如下结论:冲击地压发生时,主震振幅较大,其中跃进矿高振幅持续时间短,波形持续时间(大于0.2 s);千秋矿高振幅持续时间长(大于0.3 s),波形持续时间长(大于0.4 s);常村矿高振幅持续时间长(0.5~1.0 s),尾波持续时间(大于0.2 s)。低频所占比例较大,频带较宽,其中跃进矿主频集中在0~80 Hz,大能量波形主频集中在0~40 Hz之间;千秋矿主频集中在0~240 Hz,大能量波形主频集中在0~100 Hz;常村矿主频集中在0~100 Hz,大能量波形主频集中在0~40 Hz。

       

      Abstract: Through the seismic monitoring system, abundant microseismic signals are collected during the period of rock burst in Yuejin Coal Mine, Qianqiu Coal Mine and Changcun Coal Mine of Yimei mining area. The time-domain waveform and spectrum characteristics of microseismic signals are analyzed by the fast fourier transformation (FFT).The results show that when the rock burst occurs, the main seismic amplitude is large, and the duration of high amplitude is short in Yuejin Coal Mine, the waveform duration is greater than 0.2 s; the duration of high amplitude is greater than 0.3 s in Qianqiu Coal Mine, the waveform duration is greater than 0.2 s; the duration of high amplitude is from 0.5 s to 1.0 s in Changcun Coal Mine, the coda wave duration is greater than 0.2 s. The low-frequency proportion is big, the frequency band is wide. The frequency of Yuejin Coal Mine mainly concentrates in the range from 0 Hz to 80 Hz, the high energy waveform frequency is from 0 Hz to 40 Hz; the frequency of Qianqiu Coal Mine concentrates from 0 Hz to 240 Hz, the high energy waveform frequency is from 0 Hz to 80 Hz; the frequency of Changcun Coal Mine mainly concentrates from 0 Hz to 100 Hz, the high energy wave frequency is from 0 Hz to 40 Hz.

       

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