基于小波分析的场地波速测量方法  

Wave-velocity logging based on wavelet analysis

作　　者：陈旭庚[1] 田家勇[1] 王恩福[1] 张国宏[1] 赵国存[1] 谢周敏[1] 

机构地区：[1]中国地震局地壳应力研究所,北京100085

出　　处：《地震工程与工程振动》2007年第1期159-163,共5页Earthquake Engineering and Engineering Dynamics

基　　金：国家自然科学基金项目(10602053);中国地震局"十五"重点项目

摘　　要：在场地波速测量中,由于噪声等因素的影响很难准确识别P、S波的初至时刻,致使波速结果存在很大的误差。本文给出了一种基于小波变换的波速测量的新方法。该方法利用波动信号的小波变换与弹性波群速度的关系准确识别弹性波初至时刻。弹性波小波变换的峰值时刻代表着以群速度传播的弹性波的初至时刻,使P波、S波的初至时刻的确定具有明确的物理意义,波速的结果准确、可靠、稳定。此外,波动信号的小波多尺度分析还可以确定地层中传播的弹性波的频散特性。最后,该方法在场地波速测量的实测信号的应用表明该方法可准确确定P、S波速。It is difficult to identify the arrival times of P and S waves in wave velocity logging, which yields great error of P and S wave velocities. We present a new method for the calculation of wave velocities based on wavelet analysis. Peak values of wavelet-transformed signal represent the arrival of elastic waves with the group velocities, which makes the calculation of wave velocities accurate and reliable. Furthermore, the dispersive characteristic of waves is also shown by wavelet method. An illustrative example shows that this method can determine the accurate P and S wave velocities.

关 键 词：场地波速 初至 小波变换 峰值 

分 类 号：P315.3[天文地球—地震学] TN911.7[天文地球—固体地球物理学]