Visual experimental study on suffusion in double-layered soil under different retention ratios

被引:0
|
作者
Luo Y. [1 ]
Li A. [1 ]
Zhang H. [1 ]
Zhang X. [1 ]
You C. [2 ]
Yuan X. [3 ]
Sheng J. [1 ]
Wang H. [1 ]
机构
[1] College of Water Conservancy and Hydropower Engineering, Hohai University, Jiangsu, Nanjing
[2] School of Civil and Architecture Engineering, Hunan Institute of Technology, Hunan, Hengyang
[3] Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Qinghai, Xining
关键词
deep alluvium foundation; double-layered soil; filter criterion; retention ratio; soil mechanics; suffusion; visualization;
D O I
10.13722/j.cnki.jrme.2022.1202
中图分类号
学科分类号
摘要
Geological structure significantly influences the evolution of suffusion in alluvium foundations,and then may affects the safety of dams. However,the present studies mainly focus on the internal instability and hydraulic conditions initiating suffusion of the internally unstable soils,and the influence of geological structure is neglected. A series of transparent suffusion tests on double-layered foundation were carried out by a new suffusion visualization apparatus based on planar laser induced fluorescence technology. In the double-layered foundation,the upper and lower soil layers serve as filter and base soil,respectively. The influence of retention ratio of double-layered soil on the evolution of suffusion was investigated. The results indicate that the upper soil layer has a remarkable influence on the critical hydraulic gradients at the initiation of suffusion and at blowout. The critical hydraulic gradients decrease with the increase of the retention ratio. The retention ratio significantly influences the fine particle migration and failure modes. If the retention ratio is less than or equal to 5,the eroded fine particles from the lower soil layer were clogged at the interface,and eventually induces tensile failure;if the retention ratio is larger than 5,the upper soil layer can′t effectively protect the lower soil layer,the fine particles from the lower soil layer were eroded into the upper soil layer,and then pass through the layer,and eventually induce suffusion failure. A new filter criterion for the internally unstable base soils was proposed,and then it was validated by the experimental results presented in reference. © 2024 Academia Sinica. All rights reserved.
引用
收藏
页码:226 / 235
页数:9
相关论文
共 31 条
  • [1] Internal erosion of existing dams,levees and dikes,and their foundations-Volume 1:Internal erosion processes and engineering assessment[M], pp. 59-65, (2013)
  • [2] LUO Yulong, SU Baoyu, SHENG Jinchang, Et al., New understandings on piping mechanism[J], Chinese Journal of Geotechnical Engineering, 33, 12, pp. 1895-1902, (2011)
  • [3] WU Mengxi, YU Ting, ZHANG Qi, Finite element simulation of influence of deep overburden suffusion on dam stress and deformation[J], Rock and Soil Mechanics, 38, 7, pp. 2087-2095, (2017)
  • [4] ULHAQ I., Tarbela dam:resolution of seepage[J], Proceedings of the Institution of Civil Engineers-Geotechnical Engineering, 119, 1, pp. 49-56, (1996)
  • [5] FOSTER M, FELL R, SPANNAGLE M., A method for assessing the relative likelihood of failure of embankment dams by piping[J], Canadian Geotechnical Journal, 37, 5, pp. 1025-1061, (2000)
  • [6] KENNEY T C, LAU D., Internal stability of granular filters[J], Canadian Geotechnical Journal, 22, 2, pp. 215-225, (1985)
  • [7] SKEMPTON A W, BROGAN J M., Experiments on piping in sandy gravels[J], Geotechnique, 44, 3, pp. 449-460, (1994)
  • [8] YAO Zhixiong, ZHOU Jian, ZHANG Gang, Et al., Experimental study of particle grading impact on piping mechanism[J], Chinese Journal of Hydraulic Engineering, 47, 2, pp. 200-208, (2016)
  • [9] MOFFAT R, FANNIN R J, GARNER S J., Spatial and temporal progression of internal erosion in cohesionless soil[J], Canadian Geotechnical Journal, 48, 3, pp. 399-412, (2011)
  • [10] MARTINEZ-MORENO F J, Et al., Identification of leakage and potential areas for internal erosion combining ERT and IP techniques at the Negratín Dam left abutment(Granada,southern Spain)[J], Engineering Geology, 240, 5, pp. 74-80, (2018)