土工基础 ›› 2026, Vol. 40 ›› Issue (2): 232-237.

• 专题论述 • 上一篇    下一篇

地下多煤层采动作用下山区矿山形变演化过程研究

周雷1,李黔辉2,3,朱涛2,3,陶通伟3,4   

  1. (1.中国电建集团贵州电力设计研究院有限公司,贵阳 550025;2.贵州大学资源与环境工程学院,贵阳 550025;3.贵州大学贵州省山地地质灾害防治工程技术研究中心,贵阳 5500252;4.贵州大学 喀斯特地质资源与环境教育部重点实验室,贵阳 550025)
  • 收稿日期:2024-01-25 修回日期:2024-02-08 出版日期:2026-04-30 发布日期:2026-04-22
  • 作者简介:周雷(1997-),男,硕士,研究方向为矿山地质灾害。
  • 基金资助:
    贵阳市科技计划项目(筑科合同[2023]13-10号)

Deformation Evolution of Mountain Mines under the Action of Underground Multi Seam Mining

ZHOU Lei1, LI Qianhui2,3, ZHU Tao2,3, TAO Tongwei3,4   

  1. (1.Guizhou Electricity Design and Research Institute Co. Ltd., Power China, Guiyang 550025;
    2.College of Resource and Environmental Engineering, Guizhou University, Guiyang 550025;
    3.Mountain Geohazard Prevention and Mitigation Engineering Research Center, Guizhou University, Guiyang  550025;
    4.Key Laboratory of Karst Georesources and Environment, Ministry of Education, Guizhou University, Guiyang 550025)
  • Received:2024-01-25 Revised:2024-02-08 Online:2026-04-30 Published:2026-04-22

摘要: 我国西南地区广泛分布着高陡斜坡且地质环境条件复杂,采煤活动频繁形成大面积采空区,多煤层开采的斜坡经常发生崩滑灾害。以贵州省发耳煤矿为例,采用离散元颗粒数值模拟方法研究多煤层采动作用下矿山坡体形变演化。研究结果表明:煤层采动后,采空区的顶板开始冒落下沉,逐渐被压密;采空区边界最先产生采动裂隙,而后向上覆岩体扩展,随着开采层数的增多,形变不断加剧,裂隙向坡体临空面方向发育,形成潜在滑动面;矿山斜坡逐渐发育成不稳定斜坡进而引发灾难性地质灾害。单煤层开采对矿山斜坡扰动程度较小,多煤层开采层数越多对矿山斜坡扰动程度较大。多煤层开采为矿山地质灾害的发生提供相应孕育条件。多煤层采动作用下矿山形变演化可以分为:表生改造、冒落沉陷、裂缝扩展和临界崩滑四个阶段。 

关键词: 多煤层采动, 采动裂隙, 矿山滑坡, 形变演化, 数值模拟

Abstract: The southwestern region of China is mainly characterized by mountainous landforms, widely distributed with high and steep slopes, and complex geological environmental conditions. In addition, with abundant mineral resources and frequent coal mining activities, large areas of goaf are formed, and slopes with multiple coal seams often suffer from collapse and sliding disasters; As a result, it causes huge loss of life and property. The article presents the Fa’er Coal Mine in Guizhou Province as case history and uses the discrete element particle numerical simulation method to study the deformation and evolution of mining slopes under the action of multiple coal seam mining. The research results indicate that after coal seam mining, the roof of the goaf begins to collapse and sink, gradually being compacted; The boundary of the goaf first generates mining induced fractures, which then expand towards the overlying rock mass. As the number of mining layers increases, the deformation intensifies, and the fractures develop towards the goaf direction of the slope, forming a potential sliding surface; The slope of the mine gradually develops into an unstable slope, leading to catastrophic geological disasters. Single coal seam mining causes less disturbance to mining slopes, while multi coal seam mining with more layers causes greater disturbance to mining slopes. Multi seam mining provides corresponding breeding conditions for the occurrence of geological disasters in mines. The deformation evolution of mines under the action of multi coal seam mining can be divided into four stages: surface transformation, collapse and subsidence, crack propagation, and critical collapse and sliding.

Key words: Multi Coal Seam Mining, Mining Induced Fractures, Mine Landslides, Deformation Evolution, Numerical Simulation

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