Experiments on characteristics of infrasonic wave generated by full-regime rock failure under uniaxial loading are carried out with a stiffness material test machine

and the stiffness materials involve granite

limestone

red sandstone

sandstone

phyllite

mudstone. In this study

an advanced digital infrasound emission detecting system to study the characteristics of the infrasonic signals is independently developed. The collected infrasonic signals are processed and analyzed through the wavelet-based denoising method

short-time Fourier transform time-frequency analysis and accumulative ring-down count (ARDC). The results show that: ① The infrasonic wave emission phenomena can apparently appear during the process of uniaxial loading of rocks before rocks fracture. ② The characteristic frequency of prominent infrasonic wave generated by rocks’ fracture typically range 2.0-6.0 Hz. ③ The ARDC of hard rocks

e.g. granite and limestone

are much more than those of soft rocks

e.g. mudstone

in the case of complete structure. Compared with other acoustic signals

infrasound is low-attenuate

cannot be absorbed easily by water and air

and can propagate avoiding huge obstacles due to its long wavelength. Combined with other methods

the further study of the characteristics of infrasonic wave generated by rocks’ microfracture can provide a significant innovate approach and techniques for rock stability monitoring.