长江科学院院报 ›› 2016, Vol. 33 ›› Issue (9): 83-86.DOI: 10.11988/ckyyb.20150607

• 岩土工程 • 上一篇    下一篇

蒙脱石含量对黏土表面干缩裂隙影响试验研究

夏冬生a,刘清秉b,项伟a,b,王菁莪b,艾密b   

  1. 中国地质大学武汉 a.工程学院;b.教育部长江三峡库区地质灾害研究中心,武汉 430074
  • 收稿日期:2015-07-20 修回日期:2015-09-05 出版日期:2016-09-25 发布日期:2016-09-22
  • 通讯作者: 刘清秉(1984-),男,安徽芜湖人,副教授,博士,从事岩土工程稳定性评价、地质灾害防治方面的教学与科研工作,(电话)13419681857(电子信箱)liuqingbing_1357@163.com。
  • 作者简介:夏冬生(1989-),男,湖北宜昌人,硕士研究生,主要从事岩土体工程力学性质方面的研究,(电话)15271862621(电子信箱)523953672@qq.com。
  • 基金资助:
    国家自然科学基金(41202199,41572286);湖北省自然科学基金(2015FB247);中国博士后科学基金(2013M542098)

Impact of Montmorillonite Content on Desiccation Cracks on Clay Surface

XIA Dong-sheng1, LIU Qing-bing2, XIANG Wei1,2, WANG Jing-e2, AI Mi2   

  1. 1. Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;
    2. Three Gorges Research Center for Geo-hazard under Ministry of Education, China University of Geosciences, Wuhan 430074, China
  • Received:2015-07-20 Revised:2015-09-05 Online:2016-09-25 Published:2016-09-22

摘要: 蒙脱石作为膨胀土中主要的黏土矿物成分,对膨胀土胀缩性质及裂隙性具有重要的影响。为研究蒙脱石含量对裂隙发育的影响同时规避其他成分的影响,对13组不同蒙脱土含量的蒙脱土-石英砂饱和泥浆样进行了干燥试验,试验控制温度为40 ℃。

关键词: 蒙脱土, 干燥曲线, 裂隙, 临界含水率, 定量化分析

Abstract: As a major clay mineral in swelling soil, montmorillonite has important influence on swelling-shrinkage properties and developing fissures of swelling soil. Desiccation tests were conducted under 40 ℃ on initially saturated montmorillonite-silica sand mixture slurry to investigate the effects of montmorillonite content on shrinkage and cracking characteristics. Water loss and surface crack evolution were monitored during the whole drying period while the critical moisture content and surface crack ratio δS were obtained with computer software. The results showed that during drying period, the process of water loss showed three obvious phases: the evaporation phase at constant speed, the decline phase and the residual phase. And cracks on the surface of samples mostly developed in the first phase. The final surface crack ratio δSF and the initial moisture content wI at which the cracks start were significantly influenced by the content of montmorillonite showing trend of increasing with the growth of the content of montmorillonite. But the final moisture content wF at which the cracks end were different, yet, the difference Δw between wI and wF is positively related to the content of montmorillonite.

Key words: montmorillonite, drying curve, crack, critical moisture content, quantitative analysis

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