考虑孔隙水微观赋存形态的非饱和粉土有效应力方程及其验证

曾立峰, 邵龙潭, 牛庚, 郭晓霞. 考虑孔隙水微观赋存形态的非饱和粉土有效应力方程及其验证[J]. 水文地质工程地质, 2022, 49(4): 37-46. doi: 10.16030/j.cnki.issn.1000-3665.202110023
引用本文: 曾立峰, 邵龙潭, 牛庚, 郭晓霞. 考虑孔隙水微观赋存形态的非饱和粉土有效应力方程及其验证[J]. 水文地质工程地质, 2022, 49(4): 37-46. doi: 10.16030/j.cnki.issn.1000-3665.202110023
ZENG Lifeng, SHAO Longtan, NIU Geng, GUO Xiaoxia. An effective stress equation for unsaturated silt considering the microstructure of pore water and its verification[J]. Hydrogeology & Engineering Geology, 2022, 49(4): 37-46. doi: 10.16030/j.cnki.issn.1000-3665.202110023
Citation: ZENG Lifeng, SHAO Longtan, NIU Geng, GUO Xiaoxia. An effective stress equation for unsaturated silt considering the microstructure of pore water and its verification[J]. Hydrogeology & Engineering Geology, 2022, 49(4): 37-46. doi: 10.16030/j.cnki.issn.1000-3665.202110023

考虑孔隙水微观赋存形态的非饱和粉土有效应力方程及其验证

  • 基金项目: 国家自然科学基金面上项目(52079018;51479023)
详细信息
    作者简介: 曾立峰(1986-),男,博士,主要从事非饱和土力学方面的研究工作。E-mail: zenglifeng34@163.com
    通讯作者: 邵龙潭(1963-),男,博士研究生,教授,博士生导师,主要从事土和孔隙介质力学基本理论研究、土工结构稳定分析、土工试验测试技术与仪器研发等方面的教学和科研。E-mail: shaolt@dlut.edu.cn
  • 中图分类号: P642.11+6

An effective stress equation for unsaturated silt considering the microstructure of pore water and its verification

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  • 有效应力参数的合理确定是非饱和土有效应力研究的重要内容。然而,现有的有效应力参数未能较好地考虑孔隙水的微观赋存形态对有效应力的影响。为此,分析了孔隙水的微观赋存形态,明确了孔隙水可分为收缩膜、吸附水和毛细水,建立了非饱和粉土的扩展三相孔隙介质模型,即孔隙气、毛细水和广义土骨架。基于该模型,采用分相平衡分析法,推导了非饱和粉土的有效应力方程,该方程通过采用毛细水有效饱和度合理地考虑了毛细水对有效应力的影响。依据推导的有效应力方程,提出了非饱和粉土的抗剪强度公式。采用5种不同围压下重塑非饱和粉质黏土试验数据验证了提出的公式。结果表明:与现有的抗剪强度公式相比,本次提出的公式更好地预测了重塑非饱和粉质黏土的抗剪强度随基质吸力的变化规律。因此,运用提出的抗剪强度公式评价非饱和土边坡稳定性、地基承载力和挡土墙稳定性将会取得更好的效果。

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  • 图 1  非饱和粉土RVE中孔隙水的微观赋存形态

    Figure 1. 

    图 2  非饱和粉土的扩展三相孔隙介质模型

    Figure 2. 

    图 3  非饱和粉土的扩展三相孔隙介质模型的体积—饱和度关系

    Figure 3. 

    图 4  非饱和土整体及各分相的微元体的受力示意

    Figure 4. 

    图 5  两种SWRC模型的拟合结果

    Figure 5. 

    图 6  不同净围压下重塑非饱和粉质黏土的3种抗剪强度公式的预测结果

    Figure 6. 

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出版历程
收稿日期:  2021-10-13
修回日期:  2021-11-20
刊出日期:  2022-07-25

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