摘要
对瑞利波勘探中“之”字形频散曲线形成的物理机理进行了理论分析,研究了诸波模的传播特性及相互关系.指出在地表下存在具有水平界面的软弱夹层和地层裂缝时,瑞利波频散曲线中的“之”字形结构是低速夹层或地层裂缝中出现多模现象的结果.利用阻尼最小二乘法和遗传算法对瑞利波频散曲线反演介质参数进行了研究和分析,发现最小二乘法不适合瑞利波“之”字形反演问题研究,而用遗传算法得到了较好的结果.
The mechanism of zigzag dispersion curves in the Rayleigh wave exploration is theoretically analyzed. The propagation characteristics and interrelation of the guided waves are studied thoroughly. It is presented that the zigzag stature of Rayleigh wave dispersion curves is the result of many modes generated by the low-velocity layers or fractures in multilayered. The inverse problems are also investigated on the formation structure with the dispersion curves of the Rayleigh wave by the damping method of least squares and the genetic algorithm. It is found that the damping method of least squares is not suitable to the inversion of zigzag dispersion problem of Rayleigh wave, while the genetic algorithm is a good method for this problem.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2000年第4期557-567,共11页
Chinese Journal of Geophysics
基金
国家自然科学基金项目!(19804019)
关键词
瑞利波
层状半空间
“之”形频散曲线
地震勘探
Rayleigh wave, Stratified half-space, Guided wave, Low-velocity layer and fractures.