摘要
节理产状应力波反演时,关键问题在根据测试振动信号判断出节理面反射纵波初至时刻。借助H ilbert变换可实现信号的复信号分析,人工合成振动信号的复信号分析说明了瞬时振幅、瞬时频率二者在反射波识别方面均有很好的效果,用节理岩体模拟实验测得的信号分析表明,即使面波干扰严重,瞬时频率还是能有效判断节理反射纵波初至时刻。
When stress wave is used to inverse joint's attitude, the key problem is judge the initial arriving moment of reflected P-wave from the tested vibration signal. Through Hilbert transform we can implement a signal's complex signal analysis. A synthesized vibration signal's complex signal analysis demonstrates that both instantaneous amplitude and instantaneous frequency are efficient in identifying the reflected wave. A simulating jointed rock masses has been made and the complex signal analysis has been used to analyze the vibration signal on the testing spot. Despite the Rayleigh wave's serious interference, the initial arriving moment of reflected wave still can be judged from instantaneous frequency efficiently.
出处
《重庆大学学报(自然科学版)》
EI
CAS
CSCD
北大核心
2008年第2期220-223,共4页
Journal of Chongqing University
基金
教育部重点科技项目(03113)
关键词
复信号分析
反射波
初至时刻
HILBERT变换
节理产状
应力波反演
complex signal analysis
reflected wave
initial arriving moment
Hilbert transform
joint attitude
stress wave inverse