岩土力学 ›› 2023, Vol. 44 ›› Issue (5): 1385-1394.doi: 10.16285/j.rsm.2022.0779

• 基础理论与实验研究 • 上一篇    下一篇

侧限条件下密实砂土蠕变的颗粒运动特征

高燕1, 2,余骏远3,陈庆1,史天根1   

  1. 1. 中山大学 地球科学与工程学院,广东 珠海 519082;2. 南方海洋科学与工程广东省实验室(珠海),广东 珠海 519082; 3. 浙江大学 海洋学院,浙江 舟山 316021
  • 收稿日期:2022-05-24 接受日期:2022-10-12 出版日期:2023-05-09 发布日期:2023-04-30
  • 作者简介:高燕,女,1984年生,博士,副教授,博士生导师,主要从事土的宏微观特征、蠕变研究方面的工作。
  • 基金资助:
    国家自然科学基金(No. 42072295, No. 41807244),广东省创新创业团队项目(No. 2017ZT07Z066)

Particle motion characteristics of dense sand during creep under lateral confinement

GAO Yan1, 2, YU Jun-yuan3, CHEN Qing1, SHI Tian-gen1   

  1. 1. School of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai, Guangdong 519082, China; 2. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, Guangdong 519082, China; 3. Ocean College, Zhejiang University, Zhoushan, Zhejiang 316021, China
  • Received:2022-05-24 Accepted:2022-10-12 Online:2023-05-09 Published:2023-04-30
  • Supported by:
    The work was supported by National Natural Science Foundation of China (42072295, 41807244) and Guangdong Province Innovation and Entrepreneurship Team Project (2017ZT07Z066).

摘要: 任何构筑物长久安全稳定的重要性使得土的时间效应成为该领域学者最为关心的问题之一。基于3D打印杆件的等效砂土颗粒,通过侧限条件下的蠕变试验,采用近景摄影测量与粒子图像测速(particle image velocimetry,简称PIV)技术,从单颗粒运动与颗粒间接触运动的角度出发,探究密实砂土蠕变的内部颗粒运动特征及其与宏观蠕变变形的关系。试验结果表明,3D打印杆件能够很好地反映密实砂土蠕变的宏观变形特性,侧限条件下蠕变变形随时间的增加而增加,随蠕变应力的增加而减小,蠕变变形呈现出蠕变速率减小并趋于稳定的初始蠕变阶段与稳态蠕变阶段。其原因为蠕变最初阶段颗粒整体向下平动,并发生较大转动,颗粒间孔隙明显减小,蠕变变形主要由颗粒间孔隙的压密提供;而后颗粒间孔隙减小不明显,趋于稳定,颗粒发生不规则方向平动,蠕变变形主要由局部的颗粒位置调整与重排列控制,揭示了宏观的蠕变变形与微观的颗粒平动变化有着密切联系。颗粒间的接触运动随着蠕变时间的增加而明显增大。蠕变过程中,接触滚动和接触滑动同时发生,并逐渐集中在某些易发生移动的接触点上。强运动接触点的平均滑动距离与平均滚动距离存在着良好的线性关系,随着时间的增加,平均滑动距离逐渐大于平均滚动距离,表明颗粒间滑动产生体积收缩,控制宏观蠕变变形。

关键词: 密实砂土, 蠕变, 颗粒运动, 平动, 转动

Abstract: The importance of long-term stability of any structure makes the time effect of soil is one of the most concerned problems in geotechnical engineering. In this study, the creep tests on the equivalent sand particles of three-dimensional (3D) printed rods under lateral confined condition are conducted. In the tests, the internal particle motion characteristics of dense sand during creep and its relationship with macroscale creep deformation are explored from the perspective of single particle motion and contact motion between particles based on the close-range photogrammetry and particle image velocimetry (PIV) technology. The test results show that the 3D printed rod can reflect the macroscale deformation characteristics of dense sand during creep well. Under the lateral confinement, the creep deformation increases with the increase in time and decreases with the increase in creep stress, and the creep rate decreases and tend to be stable at the initial and secondary creep stages. This can be explained by that at the initial stage of creep, the particles move downward and rotate greatly which makes the pores between particles obviously reduced, and the creep deformation is mainly induced by the compression of pores between particles; then, the pores between particles do not decrease obviously and tend to be stable, the particles move in irregular directions, which indicates that the creep deformation is mainly controlled by local particle position adjustment and rearrangement. This also reveals that the macroscale creep deformation is closely related to the microscale translational change of particles. The contact motion between particles increases obviously with increasing time. During creep, contact rolling and contact sliding occur simultaneously, and gradually concentrate on some contacts that are easy to move. There is a good linear relationship between the average contact sliding distance and rolling distance of the strong moving contacts, i.e. with the increase of time, the average contact sliding distance is gradually greater than the average contact rolling distance, indicating that the sliding produces volume contraction and controls the macroscale creep deformation.

Key words: dense sand, creep, particle motion, translation, rotation

中图分类号: TU 411
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