煤炭工程 ›› 2025, Vol. 57 ›› Issue (4): 145-153.doi: 10. 11799/ ce202504021

• 研究探讨 • 上一篇    下一篇

离散元条件下岩石细观力学特征与声发射定量表征

袁安营,李唐,黄昊,等   

  1. 1. 安徽理工大学
    2. 安徽理工大学深部煤矿采动响应与灾害防控国家重点实验室
  • 收稿日期:2024-06-20 修回日期:2024-08-06 出版日期:2025-04-10 发布日期:2025-05-28
  • 通讯作者: 李唐 E-mail:15156631964@139.com

Quantitative characterization of rock micromechanics and acoustic emission based on discrete element method

  • Received:2024-06-20 Revised:2024-08-06 Online:2025-04-10 Published:2025-05-28

摘要:

为揭示深部岩体破坏的细观力学本质,获取岩石破坏的前兆信息,以力链研究为主线,以非连续介质离散元理论为依据,采用PFC数值模拟方法,开展了岩石细观力学特征与声发射定量表征研究。结果表明:颗粒物质间配位数变化表明了颗粒之间粘结数量的变化,进而表征了微裂纹的发育情况,且颗粒配位数与裂纹发育整体呈负相关;岩石加载过程中,“强力链带”形成于宏观破坏面附近,其延伸方向逐渐向宏观破坏面方向偏转,最终与宏观破坏面方向一致;改进了声发射模拟研究方法,将声发射演化过程划分为5个阶段,探明了声发射空间分布特征,声发射事件主要集中在岩石宏观破坏面附近,定量表征了声发射强度,在岩石峰值前存在声发射短时沉寂期,将该特征定义为岩石破坏的“临界前兆信息”。

关键词:

颗粒物质 , 微裂纹发育 , 力链演化 , 声发射 , 前兆信息

Abstract:

In order to reveal the micromechanical nature of deep rock failure and obtain the precursory information of rock failure, based on the force chain research and the discrete element theory of discontinuous media, the quantitative characterization of rock micromechanical characteristics and acoustic emission were carried out by PFC numerical simulation method. The results show that: the change of coordination number between particles indicates the change of bonding number between particles, which further characterizes the development of microcracks, and the coordination number of particles is negatively correlated with the overall development of cracks; In the process of rock loading, the "strong chain" is formed near the macro failure surface, and its extension direction gradually deflects to the macro failure surface direction, and finally is consistent with the macro failure surface direction; The acoustic emission simulation research method is improved. The acoustic emission evolution process is divided into five stages, and the spatial distribution characteristics of acoustic emission are proved. Acoustic emission events are mainly concentrated near the macro failure surface of rock, which quantitatively characterizes the intensity of acoustic emission. There is a short silence period of acoustic emission before the peak value of rock, and this characteristic is defined as the "critical precursory information" of rock failure.

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