土工基础 ›› 2026, Vol. 40 ›› Issue (2): 273-278.

• 专题论述 • 上一篇    下一篇

软弱夹层黏土矿物成分与抗剪强度相关性分析

刘柄材1,江兴元1,2   

  1. (1.贵州大学资源与环境工程学院,贵阳 550025;2.贵州大学喀斯特地质资源与环境教育部重点实验室,贵阳 550025)
  • 收稿日期:2024-03-20 修回日期:2024-04-13 出版日期:2026-04-30 发布日期:2026-04-23
  • 通讯作者: 江兴元(1986-),男,副教授,博士,研究方向为地质工程、岩土工程。
  • 作者简介:刘柄材(1996-),男,硕士研究生,研究方向为地质灾害防治。
  • 基金资助:
    国家自然科学基金项目(42007271);贵州省科技支撑计划项目(黔科合支撑[2023]一般119)

Correlation Analysis of Clay Mineral Composition and Shear Strength of Weak Interlayer

LIU Bingcai1, JIANG Xingyuan1,2   

  1. (1.College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025;
    2.Key Laboratory of Karst Georesources and Environment, Ministry of Education, Guizhou University, Guiyang 550025)
  • Received:2024-03-20 Revised:2024-04-13 Online:2026-04-30 Published:2026-04-23

摘要: 以贵州六种不同软弱夹层为研究对象,进行不同含水率的软弱夹层直剪试验,分析不同含水率的软弱夹层黏聚力和内摩擦角变化趋势和黏土对软弱夹层变化趋势的控制作用。结果显示:蒙脱石、伊利石和绿泥石对软弱夹层抗剪强度参数变化趋势起控制作用。①随含水率升高,软弱夹层黏聚力和内摩擦角整体呈下降趋势,但是不同软弱夹层变化趋势各不相同。②当软弱夹层中伊利石含量占黏土矿物含量的53%以上时,黏聚力变化趋势与伊利石相似;而当蒙脱石含量超过黏土矿物含量22%,且伊利石占比不达53%时,则与蒙脱石相似。③当蒙脱石含量占黏土矿物含量38%以上,且无绿泥石时,内摩擦角变化趋势与蒙脱石相似;而当伊利石占比超45%时,且无绿泥石,则与伊利石相似;有绿泥石时,且绿泥石占比达26%以上,则与绿泥石相似。④在相同含水率变化区间,蒙脱石的黏聚力降幅大于伊利石,蒙脱石的内摩擦角降幅最大,伊利石次之,绿泥石最小。


关键词: 软弱夹层, 含水率, 黏土矿物, 控制作用

Abstract: To study the mechanism of clay minerals that control the softening of soft interlayers under different water contents, six types of soft interlayers in Guizhou province are collected as research objects. Direct shear tests of soft interlayers with different water content are carried out to analyze the change trend of cohesion and internal friction angle of soft interlayers with different water contents and the control effect of clay on the change trend of soft interlayers. The results show that: Montmorillonite, Illite and Chlorite contents control the variation trend of shear strength parameters of weak interlayers. (1) With the increase of water content, the cohesion and internal friction angle of the weak interlayers show a downward trend, but the change trend of different weak interlayers is different. (2) When the content of Illite in the weak interlayer accounts for more than 53% of the clay mineral content, the change trend of cohesion is similar to that of Illite; When the content of Montmorillonite exceeds the content of clay minerals by 22% and the proportion of Illite is less than 53%, it is similar to Montmorillonite. (3) When the content of Montmorillonite is more than 38% of the clay mineral content, and there is no chlorite, the change trend of internal friction angle is similar to that of Montmorillonite; When the proportion of Illite exceeds 45%, and there is no chlorite, it is similar to Illite; When Chlorite exists, and chlorite accounts for more than 26%, it is similar to chlorite. (4) In the same moisture content range, the cohesion of Montmorillonite is greater than that of Illite, and the internal friction angle of Montmorillonite is the largest, followed by Illite, and chlorite is the smallest.

Key words: Weak Interlayer, Water Content, Clay Minerals, Control Function

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