plane Rayleigh waves 平面Rayleigh波
cylindrical rayleigh waves 圆柱瑞利波
generalized Rayleigh waves 广义瑞利波
phase velocity of rayleigh waves 瑞利波相速度
earthquake of approximate Rayleigh waves 近似Rayleigh地震波
rayleigh-type waves 瑞利型波
rayleigh surface waves rayleigh表面波
In section two, the theory of Rayleigh waves is discussed and a matrix method for elastic wave problem - Knopoff Method is introduced.
第二部分讨论了瑞雷波勘探原理，同时介绍了瑞雷波的一种矩阵计算方法—Knopoff快速计算法。
参考来源 - 工程场地地基土体参数的瑞雷波勘探研究The attenuation for the two Rayleigh waves, the displacement and the pore pressure, the pore pressure and the displacement of the P or SV wave field are discussed.3.
分析了饱和土中两种瑞利波的衰减特性、位移和孔压，讨论了饱和土参数对P、SV波的位移、孔压的影响。
参考来源 - 饱和土中桩基础在弹性波作用下的动力响应·2,447,543篇论文数据，部分数据来源于NoteExpress
The propagation depth of Rayleigh waves was about 2.0 times of wavelengths.
瑞利波随深度衰减快，其传播深度约为波长的2.0倍。
The conventional interpretation theory has been based on propagation of free-surface Rayleigh waves.
传统的解释理论以自由表面瑞利面波的传播为基础。
There are two basic methods of Rayleigh wave exploration: transient Rayleigh waves and standing Rayleigh waves.
瑞雷波勘探的方法主要有两种，即瞬态法和稳态法。
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