高级检索

断层倾角对声发射信号传播规律影响的试验研究

Experimental study on the influence of fault dip angle on acoustic emission sinal propagation

  • 摘要: 因存在断层和岩层间层理面等不连续界面,天然岩体并非均匀连续介质,声发射信号经过断层和层理面时传播规律必然会发生改变,因此研究断层中声发射信号的传播规律成为岩石力学的重点课题之一。基于惠更斯原理对含断层的非均匀介质条件下的波面方程进行推导,并通过室内相似模拟模型试验制作45°、60°、75°以及其他类型断层试件,结合超声波测速仪和DS5-16B全信息声发射信号分析仪对跨断层的声发射信号进行监测和记录,采用非线性拟合和Matlab软件数值计算的方式,研究不同倾角的断层、层理面数量对声发射信号传播速度以及信号特征的影响。研究结果表明:声发射信号的传播速度随着断层倾角的增大逐渐增加,传播速度与断层倾角呈正相关,断层倾角越大信号传播速度越快,信号穿过断层后传播速度会发生衰减,断层倾角越大速度衰减比例越小,层理面会使传播速度发生衰减,单个层理面对速度的影响较小,2个层理面对速度的影响较大;断层会使信号的最大幅值减小,主频率降低,频率区间向低频方向移动,断层倾角越大,最大幅值、主频率、频率区间越大。1个层理面对信号的影响较小,与无层理面的信号时频特征基本相同,2个层理面对信号的影响较大,会使信号的最大幅值、主频、频率区间有较大幅度的减小;断层的存在会导致声发射信号的瞬时能量发生巨大衰减,倾角越小衰减越为严重。研究成果可为射线理论下波速模型的建立提供理论依据。

     

    Abstract: Natural rock mass is not a uniform continuum due to discontinuous interfaces such as faults and bedding planes between rock layers, and the propagation law of acoustic emission signals will inevitably change when they pass through faults and bedding planes. Therefore, studying the propagation law of acoustic emission signals in faults has become one of the key topics in rock mechanics. Based on the Huygens principle, the wave front equation under the condition of heterogeneous media containing faults was derived, and 45°, 60°, 75° and other types of fault specimens were made through laboratory similar simulation model tests. The acoustic emission signals across faults were monitored and recorded by combining ultrasonic tachymeter and DS5-16B full-information acoustic emission signal analyzer. Nonlinear fitting and numerical calculation of Matlab software are used to study the influence of faults and the number of bedding planes of different inclination angles on the propagation speed and signal characteristics of acoustic emission signals. The results show that the propagation speed of acoustic emission signals increases gradually with the increase of fault dip Angle, and the propagation speed is positively correlated with fault dip Angle. The larger the fault dip Angle is, the faster the signal propagation speed will be, and the propagation speed will attenuate after the signal passes through the fault, and the larger the fault dip Angle is, the smaller the proportion of velocity attenuation will be. The propagation velocity is attenuated by the bedding plane, and the single bedding plane has little influence on the velocity, while the two bedding planes have great influence on the velocity. The fault will make the maximum value of the signal decrease, the main frequency decrease, and the frequency interval move to the low frequency direction. The larger the fault inclination, the larger the maximum value, the main frequency and the frequency interval. One layer has little influence on the signal, which is basically the same as the time-frequency characteristics of the signal without stratification, while the two layers have a greater influence on the signal, which will greatly reduce the maximum value, main frequency and frequency interval of the signal. The existence of fault will cause the instantaneous energy of acoustic emission signal to decrease greatly, and the smaller the inclination Angle, the more serious the attenuation is. The research results can provide theoretical basis for the establishment of wave velocity model under the ray theory.

     

/

返回文章
返回