煤炭工程 ›› 2023, Vol. 55 ›› Issue (8): 108-113.doi: 10. 11799/ ce202308020

• 研究探讨 • 上一篇    下一篇

浅埋薄基岩采场覆岩破断特征及其导水裂隙带发育规律研究#br#

刘国建,杨富强,高学丰,姜宁   

  1. 1. 鄂尔多斯昊华精煤有限责任公司高家梁煤矿, 内蒙古 鄂尔多斯 017000
    2. 山东科技大学 能源与矿业工程学院, 山东 青岛 266590

  • 收稿日期:2022-09-30 修回日期:2023-04-03 出版日期:2023-08-20 发布日期:2025-04-08
  • 通讯作者: 刘国建 E-mail:1015640776@qq.com

Research on the fracture characteristics of the overlying rock and the development law of the water-conducting fracture zone in the shallow-buried thin bedrock stope

  • Received:2022-09-30 Revised:2023-04-03 Online:2023-08-20 Published:2025-04-08

摘要:

以高家梁煤矿20107工作面为工程背景, 借助物理相似材料试验及UDEC数值模拟对浅埋薄基岩开采条件下工作面覆岩破断规律进行系统研究。结果表明: 工作面推进至48m处直接顶开始产生离层并垮入采空区, 推进至72m处时, 基本顶在自重及上覆载荷作用下发生周期性破断, 覆岩经历了弯曲下沉、触矸压实、最终稳定等一系列过程, 最大破坏高度达152m; 数值模拟同样再现了工作推进过程中顶板破坏演化特征, 工作面推进至150m时顶板破断运动至稳定状态,覆岩最终破坏高度达100m左右; 最后通过井下仰孔分段注水观测法对顶板导水裂隙带发育高度进行现场实测, 实测覆岩破坏高度约为采高的25倍, 与物理模拟、数值模拟结果基本吻合, 表明20107工作面回采对上覆含水层影响有限, 可为类似矿井工作面安全开采提供参考依据。

关键词: 浅埋煤层, 覆岩破坏, UDEC, 岩层移动, 导水裂隙带, 数值模拟

Abstract:

n this paper, taking the 20107 working face of Gaojialiang Coal Mine as the engineering background, with the help of the physical similar material test system and the UDEC numerical simulation program, the breaking law of the overlying rock under the mining conditions of the shallow coal seam is studied. Numerical simulation and physical test results are verified. The research results show that: with the continuous advancement of the mining face, the roof collapses directly after the layer is separated to a certain extent, and the collapsed gangue fills part of the goaf, and then the roof basically bends under the action of its own weight and overlying load. A series of processes such as subsidence, periodic breaking, gangue compaction, and final stabilization; after the mining of the working face, the "three-zone" structure of the overlying rock is basically formed; the observation results of staged water injection in the downhole vertical hole show that the overlying rock failure height is about 100m , the fracture zone is highly developed into the fine-grained sandstone layer, and the simulation results of similar materials and numerical simulations are in good agreement with the actual situation in the field.

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