岩石变形破坏次声异常的能量特征研究
Energy characteristics of infrasound abnormality during rock deformation and failure of rock
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摘要: 采用室内试验方法,对8组砂岩试件进行了压缩破坏试验,同步记录岩石变形破坏过程中的次声信号,采用小波分析方法对异常信号的能量特征进行了分析研究。结果表明:岩石变形破坏次声异常信号能量主要集中在3.91~7.81 Hz的中频段和7.81~15.62 Hz的高频段两个频率范围内,其中中频段能量大于高频段能量,同时在低频段0~3.19 Hz内也存在一定的能量分布,通过不同频段能量分布对比,可对信号进行识别;随着岩石变形破坏程度的增加,次声异常信号的中低频段能量在相对减少,而高频段能量相对增加,在岩石临近破坏前,次声信号的中低频段能量与高频段能量的比值接近1。以上几个方面特征的发现,为岩石变形破坏的次声异常信号识别及破坏前兆预警提供了重要的依据。Abstract: Eight groups of axial compression tests on sandstone are conducted in laboratory. The infrasound signals of each test process are recorded synchronously, and then the energy characteristics of each specimen are analyzed using the wavelet decomposition method. The results show that the infrasound energy of rock failure is mainly concentrated in two frequency bands. One is the medium frequency band with frequency range of 3.91~7.81 Hz, and the other is the high frequency band with frequency range of 7.81~15.62 Hz. The energy of the former is higher than that of the latter. At the same time there still exists a certain amount of energy with frequency range of 0~3.91 Hz in the signal. By comparing the energy distribution in different frequency bands, the infrasound of rock deformation and failure can be recognized. With the increasing degree of rock deformation, the energy with medium and low frequency bands decreases, and the energy with high frequency band increases relatively. When rock failure is coming, the ratio of the energy in medium and low frequency bands to that in high frequency band is near 1. The discovery of the above characteristics of infrasound during deformation and failure of rock may provide an important basis for recognizing infrasound signals and failure warning of rock.