Reflection and transmission of shear wave at interface between soil layers with different saturation degrees
|更新时间:2026-06-25
|
Reflection and transmission of shear wave at interface between soil layers with different saturation degrees
Vol. 34, Issue 3, (2013)
作者机构:
1. 浙江大学 软弱土与环境土工教育部重点实验室,杭州,310058
2. 浙江大学 岩土工程研究所,杭州,310058
作者简介:
基金信息:
DOI:
CLC:TU459
Online First:20 March 2013,
Published:2013
稿件说明:
移动端阅览
CHEN Wei-yun, XIA Tang-dai, WANG Ning, et al. Reflection and transmission of shear wave at interface between soil layers with different saturation degrees[J]. 2013, 34(3).
DOI:
CHEN Wei-yun, XIA Tang-dai, WANG Ning, et al. Reflection and transmission of shear wave at interface between soil layers with different saturation degrees[J]. 2013, 34(3).DOI:
Reflection and transmission of shear wave at interface between soil layers with different saturation degrees
the propagation equations for the various elastic waves in unsaturated soils are derived. According to the boundary conditions at the interface
the relationships between different wave amplitudes of various potential functions are established; and then the reflection and transmission problems of incident shear wave at the interface between unsaturated soil layers with different saturation degrees are discussed. Three compressional waves and one shear wave exist in the infinite unsaturated soils
therefore four reflected waves and four transmitted waves are generated when the shear wave propagates at the interface between different unsaturated soil layers. The theoretical expressions for the amplitude ratios and energy ratios for the various waves are derived; and the numerical analysis is then performed. In the numerical examples
the influences of incident frequency
incident angle and saturation degrees of the upper and lower soil layers on the proportionality coefficients of the reflected wave energy and transmitted wave energy (namely energy reflection ratios and energy transmission ratios) are discussed respectively. It is shown that the energy reflection ratios and energy transmission ratios are affected by both the incident angle and the incident frequency. Additionally
the influence of the saturation degrees of the upper and lower soil layers on the reflected and transmitted waves should not be ignored.