摘要
工程勘探中稳态瑞利波法的实测曲线与介质性质有着密切的对应关系.传统的解释理论以自由表面瑞利面波的传播为基础.然而源检距很小时,漏能型面波(或多次复合反射波)的形成能更合理地解释记录曲线上的特征点.解释理论的正确性将有利于扩展该方法的实际应用.
Practical recorded curves of steady-state Raylcigh waves in engineering exploration closely correspond to properties of the media. The conventional interpretation theory has been based on propagation of free-surface Rayleigh waves. In the case of extremely small source-receiver distances, however, the generation of leaking-mode surface waves (or multiple composite reflections) may more reasonably account for characteristic points on recorded curves. Correctness of interpretation theory would be favorable for more extensive applications of this method.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
1993年第1期96-105,共10页
Chinese Journal of Geophysics
关键词
稳态瑞利面波
层状介质
漏能型面波
Steady-state Rayleigh wav ,Dispersion, Layered media, Leaking-mode surface wave,