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首页> 外文期刊>Bulletin of engineering geology and the environment >Relationship between water content, shear deformation, and elastic wave velocity through unsaturated soil slope
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Relationship between water content, shear deformation, and elastic wave velocity through unsaturated soil slope

机译:水含量,剪切变形和弹性波速度通过不饱和土坡之间的关系

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摘要

This study aims to determine the relationship between water content, shear deformation, and elastic wave velocity of unsaturated soil slope. The individual influence of volumetric water content and tilt angle on the normalized wave velocity through unsaturated soil was investigated through a series of adjustable slope model tests. The relationship function between volumetric water content, tilt angle, and normalized wave velocity was established. To verify the proposed relationship function, fixed slope model tests were carried out. The relationship functions could be used to estimate the behaviors of wave velocity in rainfall-induced slope failure model tests. The applicability of proposed relationship function for wave velocity behaviors is also presented. It is found that the relationship function is highly consistent with the measurements for wave velocity behaviors through unsaturated soil slope. In addition, the effects of rainfall duration/initial water content, density, slope angle, and surface layer thickness seem to be small on the decrease rate of normalized wave velocity with volumetric water content and tilt angle.
机译:本研究旨在确定不饱和土坡的水含量,剪切变形和弹性波速度之间的关系。通过一系列可调的斜坡模型试验研究了体积含水量和倾斜角度对通过不饱和土壤的归一化波速度的各个影响。建立了体积含水量,倾斜角度和归一化波速度之间的关系功能。为了验证所提出的关系功能,执行固定斜率模型测试。关系功能可用于估计降雨引起的斜坡故障模型测试中的波速的行为。还提出了建议的波速行为关系功能的适用性。结果发现,关系功能与通过不饱和土斜率的波速行为的测量高度一致。此外,降雨持续时间/初始水含量,密度,斜坡角度和表面层厚度的影响似乎小于具有体积水含量和倾斜角度的归一化波速度的降低速率。

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