长江科学院院报 ›› 2024, Vol. 41 ›› Issue (4): 95-103.DOI: 10.11988/ckyyb.20230793

• 岩土工程 • 上一篇    下一篇

节理岩体单轴瞬态卸荷动态响应机理

李新平1, 王良军1, 宋凯文1, 王梓1, 黄俊红2, 刘婷婷1   

  1. 1.武汉理工大学 土木工程与建筑学院,武汉 430070;
    2.武汉理工大学 资源与环境工程学院,武汉 430070
  • 收稿日期:2023-07-19 修回日期:2023-09-18 出版日期:2024-04-01 发布日期:2024-04-11
  • 通讯作者: 宋凯文(1993-),男,湖北武汉人,博士,主要从事岩土工程、地下工程等领域的研究工作。E-mail:kniffy428@gmail.com
  • 作者简介:李新平(1963-),男,湖北天门人,教授,博士,主要从事岩土工程、地下工程等领域的教学与科研工作。E-mail:xinpingli@whut.edu.cn
  • 基金资助:
    国家自然科学基金项目(52109165)

Dynamic Response Mechanism of Uniaxial Transient Unloading in Jointed Rock Mass

LI Xin-ping1, WANG Liang-jun1, SONG Kai-wen1, WANG Shen1, HUANG Jun-hong2, LIU Ting-ting1   

  1. 1. School of Civil Engineering and Architecture, Wuhan University of Technology, Wuhan 430070, China;
    2. School of Resources and Environmental Engineering, Wuhan University of Technology, Wuhan 430070, China
  • Received:2023-07-19 Revised:2023-09-18 Online:2024-04-01 Published:2024-04-11

摘要: 为了研究深部节理岩体开挖瞬态卸荷力学响应及变形损伤规律,通过理论分析、室内试验、数值分析等技术手段,深入研究了深部节理岩体开挖中的瞬态卸荷力学机理及动力响应,探讨了瞬态卸荷和节理的相互作用机制,建立了可描述现场原位试验的数值模型。结果表明:在单轴瞬态卸荷的第1阶段中,岩体内不会产生拉应力,而在第2阶段中,反射拉伸应力波将动能完全转化为弹性势能,导致岩体内产生拉应力;当有节理存在时,卸载波会在节理处产生透反射现象,导致节理张开量与节理刚度呈负相关;在节理岩体的单轴瞬态卸荷第2阶段中,反射拉伸应力波传递至节理时,会导致节理大幅度张开,诱发岩体的位移突变现象。研究结果对于深入了解单轴瞬态卸荷作用下岩体的力学响应机制具有重要意义,为开展深部岩体瞬态卸荷研究提供了重要的参考依据。

关键词: 深部岩体, 节理岩体, 瞬态卸荷, 损伤力学, 数值分析

Abstract: This study aims to examine the mechanical responses and deformation damage mechanisms of deep jointed rock masses during transient unloading. We investigated the mechanical behavior and dynamic responses of these rock masses during transient unloading through theoretical analyses, laboratory experiments, numerical simulations, and other methods. Our research identifies several key factors influencing the dynamic response to transient unloading in jointed rock formations. We develop a numerical model that describes in-situ field conditions closely. Initial findings reveal that in the first stage of uniaxial transient unloading, the rock mass experiences no tensile stress. However, in the subsequent second stage, the reflection of tensile stress waves transforms all kinetic energy into elastic potential, creating tensile stresses within the rock mass. Additionally, the unloading process generates transreflectance at rock joints, leading to an inverse relationship between joint opening and stiffness in the presence of joints. In the second stage of uniaxial transient unloading, significant joint opening occurs, causing a sudden displacement in the rock mass as the reflected tensile stress wave reaches the joint. This research enhances our understanding of the mechanical behavior of rock masses under uniaxial transient unloading, providing valuable insights for addressing transient unloading challenges in deep rock mass excavations.

Key words: deep rock mass, jointed rock mass, transient unloading, damage mechanics, numerical analysis

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