膨胀土微结构对膨胀行为的影响
DOI:
作者:
作者单位:

1.长沙理工大学 交通运输工程学院;2.中国铁路南宁局集团有限公司

作者简介:

通讯作者:

中图分类号:

U416.1

基金项目:

国家自然科学基金(51978085)、中国国家铁路集团有限公司科技研究开发计划课题(K2020G036, K2019G045)资助.


INFLUENCE OF MICROSTRUCTURE OF EXPANSIVE SOIL ON SWELLING BEHAVIOR
Author:
Affiliation:

1.School of Traffic and Transport Engineering,Changsha University of Science and Technology;2.China Railway Nanning Group Co,Ltd

Fund Project:

National Natural Science Foundation of China (No. 51978085); Research and Development Project of China National Railway Group Co., Ltd (Grant No. K2020G036, K2019G045)

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    评估膨胀土的膨胀行为对于膨胀土地区的结构设计十分重要。因降雨入渗,膨胀土在垂直方向和水平方向均产生膨胀变形,当膨胀变形受抑制时将产生膨胀压力,影响其周围结构的稳定性。为揭示膨胀土在增湿膨胀过程中出现的各向异性的原因,本文从微观角度出发,通过电镜扫描(SEM)对百色中膨胀土和枝江弱膨胀土的微观结构进行了观察,并通过图像处理技术统计分析了膨胀土内黏土矿物颗粒的层状排列。同时,通过研发的二维膨胀仪和改进的试件制备方法,从宏观角度测得了侧限条件下的两向膨胀规律。研究结果表明,膨胀土的微观结构呈片状且面-面相叠;当膨胀土处于天然松散状态时,其内部的黏土矿物颗粒随机定向排列且集聚;压实后,因受各向不均等应力作用,黏土矿物颗粒开始趋向于水平层状排列。干密度越大,土样越密实,其水平层状排列越显著。侧限条件下,两向的膨胀规律表现出显著的差异,干密度越大,膨胀性越强,这种差异就越明显。然而对黏土矿物颗粒来说,其膨胀的方向垂直于其长轴,故高度的水平定向是造成膨胀土在宏观上表现出膨胀各向异性的原因。这种两向的膨胀差异受到干密度和膨胀性的影响,难以做出预测,因此建议在工程实践中实测两向的膨胀规律。

    Abstract:

    Evaluation of swelling behavior is significantly important for designing structures in expansive soils areas. Due to infiltration, the expansive soil produces swelling deformation in both vertical and horizontal directions, the swelling pressure occurs if the swelling deformation was restrained that influences the stability of surrounding structures. In order to reveal the causes of anisotropy behavior of expansive soil in the process of wetting and swelling, from the microscopic point of view, this paper observed the microstructure of expansive soil from Baise with medium swelling potential and expansive soil from Zhijiang with weak swelling potential, and statistically analyzed the orientated distribution of clay mineral particles in expansive soil by image processing technology. At the same time, from the macroscopic point of view, the two-dimensional variations of swelling strain with swelling pressure were measured under lateral confined condition via the developed two-dimensional dilatometer and the modified specimen preparation method. The results show that the microstructure of expansive soil is flaky and stacked layer by layer; When the expansive soil is in a natural loose state, the clay mineral particles are randomly oriented and aggregated; After compaction, clay mineral particles tend to be horizontally oriented due to the anisotropic stress. The higher the dry density, the denser the soil sample, and the more obvious its horizontal orientation. Under lateral confined condition, significantly swelling differences are observed between the vertical direction and horizontal direction. The greater the dry density, the stronger the swelling ability, and the more obvious the difference. However, for clay mineral particles, the swelling direction is perpendicular to their long axis, so the highly horizontal orientation is the reason why expansive soil shows swelling anisotropy behavior in macroscopic view. The swelling anisotropy is influenced by dry density and swelling ability, which is hard to estimate, so it is suggested to measure the swelling principle in two directions in engineering practice.

    参考文献
    相似文献
    引证文献
引用本文
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2021-08-24
  • 最后修改日期:2021-11-27
  • 录用日期:2021-12-18
  • 在线发布日期:
  • 出版日期: