岩土力学 ›› 2020, Vol. 41 ›› Issue (11): 3591-3603.doi: 10.16285/j.rsm.2020.0144

• 基础理论与实验研究 • 上一篇    下一篇

基于3D-DIC技术的砂岩变形局部化 荷载速率效应试验研究

彭守建1, 2,冉晓梦1, 2,许江1, 2,陈灿灿1, 2,宋肖徵1, 2,闫发志1, 2   

  1. 1. 重庆大学 煤矿灾害动力学与控制国家重点实验室,重庆 400044; 2. 重庆大学 复杂煤气层瓦斯抽采国家地方联合工程实验室,重庆 400044
  • 收稿日期:2020-01-09 修回日期:2020-04-13 出版日期:2020-11-11 发布日期:2020-12-24
  • 作者简介:彭守建,男,1983年生,博士,副教授,主要从事矿山岩石力学、煤与瓦斯突出灾害动力学与控制等方面的研究工作。
  • 基金资助:
    国家自然科学基金项目(No. 51874055,No. 51974041);重庆市基础与前沿研究计划项目(No. cstc2018jcyjAX0626)。

Experimental study on loading rate effects of sandstone deformation localization based on 3D-DIC technology

PENG Shou-jian1, 2, RAN Xiao-meng1, 2, XU Jiang1, 2, CHEN Can-can1, 2, SONG Xiao-zheng1, 2, YAN Fa-zhi1, 2   

  1. 1. State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400044, China; 2. State and Local Joint Engineering Laboratory of Methane Drainage in Complex Coal Gas Seam, Chongqing University, Chongqing 400044, China
  • Received:2020-01-09 Revised:2020-04-13 Online:2020-11-11 Published:2020-12-24
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51874055, 51974041) and the Basic and Frontier Research Projects of Chongqing (cstc2018jcyjAX0626)

摘要: 利用可视化三轴压缩伺服控制试验系统研究了不同加载速率条件下砂岩的变形局部化特征。通过3D-DIC测试系统,获得了砂岩在三轴应力条件下的轴向及径向应变场云图,分析了加载速率对砂岩变形局部化的影响规律。研究表明:在峰值强度前,砂岩表面变形较为均匀;在峰值强度时出现应变集中现象,且在峰后阶段迅速扩展,最终形成贯穿试样表面的变形局部化带;随着荷载速率增加,砂岩的峰值强度、弹性模量、泊松比、峰值点轴向应变和峰值点径向应变均增大;当荷载速率从1×10–6 s–1增大到1×10–3 s–1时,变形局部化启动应力随之增大,且轴向及径向变形局部化启动应力水平即比值 和 分别从峰后的92.00%、93.75%变至峰前的97.17%、96.00%,表明砂岩变形局部化具有较为明显的荷载速率效应。

关键词: 砂岩, 3D-DIC, 应变场云图, 变形局部化, 速率效应

Abstract: The characteristics of sandstone localized deformation have been studied by visual triaxial compression servo control test system under different loading rates. By the use of the 3D-DIC (3 dimensional digital image correlation) test system, we obtain the axial and radial strain field nephogram, as well as the crack evolution process of sandstone under triaxial stress. The influence of loading rate on the localized deformation of sandstone has been analyzed. The results show that: before the peak strength, the surface deformation of sandstone is relatively uniform. The strain concentration phenomenon occurs at the peak strength, and it expands rapidly in the post-peak stage, and finally forms a deformation localized zone that penetrates the sample surface. As the load rate increases, the peak strength, elastic modulus, Poisson's ratio, peak axial strain and peak radial strain of sandstone all increase. When the loading rate increases from 1×10–6 s–1 to 1×10–3 s–1, the starting stress of localization of deformation also increases. Besides, the ratios and , which describe the levels of the starting stress of axial and radial deformation localization, have changed from 92.00% and 93.75% after the peak to 97.17% and 96.00% before the peak, respectively, indicating that the deformation localization of sandstone has relatively obvious loading rate effects.

Key words: sandstone, 3D-DIC, strain field nephogram, deformation localization, rate effect

中图分类号: TU 451
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