煤炭工程 ›› 2026, Vol. 58 ›› Issue (5): 184-192.doi: 10.11799/ce202605023

• 研究探讨 • 上一篇    下一篇

不同因素影响下无锚煤岩组合体分时破裂演化规律研究

赵 爽,高 林,唐仕贤,高昌思,莫飞龙,李 胜,翟浩然   

  1. 1. 贵州大学 矿业学院,贵州 贵阳 550025

    2. 煤炭行业巷道支护与灾害防治工程研究中心,北京 100083

    3. 贵州大学 喀斯特地区优势矿产资源高效利用国家地方联合工程实验室,贵州 贵阳 550025

  • 收稿日期:2025-12-08 修回日期:2026-01-12 出版日期:2026-05-15 发布日期:2026-05-27
  • 通讯作者: 高林 E-mail:113395965@qq.com

Study on time-dependent fracture evolution law of unanchored coal-rock combination under the influence of different factors

  • Received:2025-12-08 Revised:2026-01-12 Online:2026-05-15 Published:2026-05-27

摘要:

为解决贵州矿区广泛分布的半煤岩巷道在采动应力下易发生非对称大变形的问题,以盘江矿区典型半煤岩巷道为工程背景,基于数字图像相关技术(DIC),开展不同煤岩分界面倾角、高度比及强度比条件下无锚煤岩组合体的单轴压缩试验,同步获取宏观力学响应与全场变形数据。结果表明:DIC应变场演化清晰呈现“煤体应变集中→煤体主破裂→应力转移→岩体滞后破坏”的分时破裂全过程;分界面倾角增大通过增强界面剪切滑移分量,促使破裂模式由煤体压溃主导逐渐转向界面滑移主导;煤岩高度比通过调控煤体在结构中的主导性与岩体约束效应,影响分时破裂的时序特征与破坏剧烈程度,其中1∶1高度比是分时破裂序列最为典型的临界构型;煤岩强度比是驱动分时破裂的本质因素,其差异越大,分时破裂序列越显著、时间差越明显。

Abstract:

In order to solve the problem of asymmetric large deformation control of coal and rock roadways widely distributed in Guizhou mining area, based on digital image correlation technology ( DIC ), the macroscopic mechanical response and deformation data of the whole process were collected synchronously. Through the digital image full-field strain analysis and macroscopic stress-strain response comprehensive characterization, the uniaxial compression test of unanchored coal-rock combination specimens under different coal-rock interface dip angles, height ratios and strength ratios was carried out. The results show that the evolution of DIC strain field clearly presents the whole process of time-sharing fracture of ' coal strain concentration → coal main fracture → stress transfer → rock mass lag failure '. The increase of the dip angle of the interface enhances the shear slip component of the interface, which makes the fracture mode gradually shift from coal crushing to interface slip. The coal-rock height ratio affects the timing characteristics and damage severity of time-sharing fracture by regulating the dominance of coal in the structure and the constraint effect of rock mass. The strength ratio of coal rock is the essential factor driving time-sharing fracture. The larger the difference is, the more significant the time-sharing fracture sequence is, and the more obvious the time difference is. The above research results further reveal the time-sharing fracture evolution law and formation mechanism of unanchored coal-rock combination under uniaxial compression load, and provide a theoretical basis for the control of surrounding rock of coal-rock roadway.

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