基础理论与实验研究

压实膨胀土非饱和抗剪强度的湿度与密度效应

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  • 1. 信阳师范学院 建筑与土木工程学院,河南 信阳 464000; 2. 中国科学院武汉岩土力学研究所 岩土力学与工程国家重点实验室,湖北 武汉 430071
周葆春,男,1978年生,博士,教授,主要从事非饱和土与特殊土力学性质与本构模拟方面的研究工作

收稿日期: 2017-04-09

  网络出版日期: 2018-06-05

基金资助

国家自然科学基金项目(No.51009118);河南省高等学校重点科研项目(No.17A560008)。

Effects of moisture and density states on unsaturated shear strength of compacted expansive soil

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  • 1. College of Architecture and Civil Engineering, Xinyang Normal University, Xinyang, Henan 464000, China; 2. State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China

Received date: 2017-04-09

  Online published: 2018-06-05

Supported by

This work was supported by the National Nature Science Foundation of China (51009118) and the Key Research Program of Higher Education of Henan Province (17A560008).

摘要

为获得压实膨胀土在湿度与密度变化范围内的抗剪强度全貌,采用非饱和直剪试验测定38种湿度与密度组合状态下荆门弱膨胀土的抗剪强度,获得了湿度从风干到饱和、密度在孔隙比0.539~1.089范围内的抗剪强度的分布规律。结果表明,(1)剪切过程中试样大多呈应变软化,仅在低密度与高湿度组合下产生应变强化。高密度与低湿度组合下易出现“应力跌落”。相同密度下,随湿度增大,土体塑性变形能力增强。相同湿度下,随密度降低,土体塑性变形能力增强;(2)非饱和抗剪强度与总黏聚力均随湿度增加先增大后减小而呈现出显著的“山峰效应”;(3)非饱和抗剪强度、总黏聚力、总内摩擦角均随密度减小而显著降低,呈现出显著的“密度效应”。

本文引用格式

周葆春,孔令伟,马全国,罗正涛,张彦钧, . 压实膨胀土非饱和抗剪强度的湿度与密度效应[J]. 岩土力学, 2017 , 38(S1) : 240 -246 . DOI: 10.16285/j.rsm.2017.S1.029

Abstract

To investigate unsaturated shear strength of compacted expansive soil within the entire range of moisture and density state, the unsaturated direct shear tests are conducted on Jingmen expansive soil associated with 38 types of moisture and density state combinations. The distribution of shear strength are obtained with respect to moisture state varying from air-dry to saturation and density represented by void ratio ranging from 0.539 to 1.089. Conclusions are as follows: (1) Strain-softening phenomenon is observed in shear for most samples. In contrast, strain-hardening phenomenon is observed in shear only for the lower-density and higher-moisture state combination. Stress plummeting phenomenon is observed in shear for the higher-density and lower-moisture state combination. Plastic deformation capacity of the soil samples is improved by increasing moisture under the same density or improved by decreasing density under the same moisture. (2) With the moisture increasing from air-dry to saturation, the unsaturated shear strength and total cohesion increase and then decrease, which can be called the peak effect. (3) Unsaturated shear strength, total cohesion, and total friction angle all decrease with decreasing density, which can be called the density effect.
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