岩土力学 ›› 2020, Vol. 41 ›› Issue (11): 3663-3670.doi: 10.16285/j.rsm.2020.0253

• 基础理论与实验研究 • 上一篇    下一篇

间断级配砂砾石土的渗透变形试验研究

田大浪1,谢强1, 2,宁越3,傅翔4, 5,张建华1   

  1. 1. 重庆大学 土木工程学院,重庆 400045;2. 重庆大学 山地城镇建设与新技术教育部重点实验室,重庆 400045; 3. 渝北区住房和城乡建设委员会,重庆 401120;4. 重庆交通大学 河海学院,重庆 400047;5. 长江水利委员会 长江科学院,湖北 武汉 430010
  • 收稿日期:2020-03-08 修回日期:2020-04-13 出版日期:2020-11-11 发布日期:2020-12-25
  • 通讯作者: 谢强,男,1975年生,博士,教授,博导,主要从事与岩土工程相关的科研和教学工作。E-mail: xieqiang2000@163.com E-mail: tiandalang135@163.com
  • 作者简介:田大浪,男,1993年生,博士研究生,主要从事岩土工程领域的研究工作。
  • 基金资助:
    重庆市教育委员会科学技术研究计划青年项目资助项目(No. KJQN201804303)

Experimental investigation on seepage deformation of gap-graded sand-gravel soils

TIAN Da-lang1, XIE Qiang1, 2, NING Yue3, FU Xiang4, 5, ZHANG Jian-hua1   

  1. 1. School of Civil Engineering, Chongqing University, Chongqing 400045, China; 2. Key Laboratory of New Technology for Construction of Cities in Mountain Area Ministry of Education, Chongqing University, Chongqing 400045, China; 3. Yubei District Housing and Urban Rural Development Committee, Chongqing, 401120, China; 4. Hehai College, Chongqing Jiaotong University, Chongqing 400047, China; 5. Changjiang River Scientific Research Institute of Changjiang Water Resources Commission, Wuhan, Hubei 430010, China
  • Received:2020-03-08 Revised:2020-04-13 Online:2020-11-11 Published:2020-12-25
  • Supported by:
    This work is supported by the Youth Project of Science and Technology Research Program of Chongqing Education Commission (KJQN201804303).

摘要: 渗透变形是颗粒材料中细颗粒在渗流作用下发生重分布且导致土体的内部结构、水力及力学特性发生变化的现象,是导致砂砾石土地基及堤防结构破坏的主要原因之一。利用自主研发的刚性壁渗透仪对不同级配及细颗粒含量的间断级配砂砾石土在恒定水头渗流作用下进行渗透变形全过程试验,监测了渗流过程中的局部水力梯度空间分布以及竖向位移变化,分析了渗透试验结束后土体的颗粒级配空间分布变化。研究结果表明:土粒中细颗粒所处的欠填、满填及过填3种堆积状态决定了粗、细颗粒间不同的接触方式,影响其渗透性。渗透试验结束后细颗粒流失量沿试样高度的空间分布可以划分为3个区域,即顶部流失区、中部均匀区及底部流失区。局部水力梯度的快速下降伴随着竖向位移的突变,意味着渗透变形的开始;渗透变形启动时的局部水力梯度大于全局水力梯度,证实了采用大尺寸试验执行渗透试验的必要性。细颗粒处于过填状态的试样依然会发生渗透变形且导致强烈的沉降变形,值得进一步的研究。

关键词: 渗透变形, 砂砾石土, 局部水力梯度, 竖向位移, 细颗粒含量

Abstract: Seepage deformation is a phenomenon in which fine particles within the soil skeleton in granular materials are redistributed under the action of seepage, leading to the change in the internal fabric, hydraulic properties, and mechanical properties of soils. Seepage deformation has become one of the leading causes for the failure of sand-gravel foundation and embankment dams. The newly self-developed rigid wall permeameter was adopted to conduct the seepage test under the action of constant water head on gap-graded sand-gravel soils with different gradation and fines content. The spatial distribution of local hydraulic gradient along the specimen and the variation of vertical displacement were monitored during the seepage tests. The spatial distribution of soil particle size distribution was analyzed after the seepage test. The test results reveal that there appeared to be three kinds of packing state of fine particles, i.e., under-filled, filled, and over-filled state, and these packing state determined the different contact modes between the coarse particles and the fine particles then affecting the permeability. At the end of the penetration test, the spatial distribution of fine particle loss along the sample height can be divided into three areas, namely the top loss area, the middle uniform loss area and the bottom loss area. The rapid decrease in local hydraulic gradient, accompanied by an abrupt increase in vertical displacement, implied the onset of seepage deformation. The local hydraulic gradient at the start of seepage deformation was more substantial than the global hydraulic gradient, which proves the necessity of carrying out the seepage test on large scale specimens. Specimens with fine particles in the over-filled state are still susceptible to seepage deformation, leading to significant settlement deformation, which is worthy of further investigation.

Key words: seepage deformation, sand-gravel soils, local hydraulic gradient, vertical displacement, fines content

中图分类号: TU 443
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