上层煤极限平衡区的边界空间形态的演变和入效应在急剧入的煤层中
Xiaobo Wu1,2, Xiaolou Chi3, Ding Lang4,5
1College of Energy and Mining Engineering, Xi'an University of Science and Technology, Xi'an, 710054, China. xust_wxb@126.com.
Scientific reports
|March 5, 2026
概括
预测顶层煤炭断裂边界形态对于急剧入煤层的稳定性至关重要. 这项研究揭示了它的不对称进化和连续阶段,有助于矿山安全.
科学领域:
- 采矿工程 采矿工程 采矿工程
- 地质技术工程 地质技术工程
- 岩石机械学 岩石机械学
背景情况:
- 顶层煤炭的稳定性对于"支周围岩石"系统在的煤层中至关重要.
- 准确预测顶煤故障边界形态对于系统稳定性控制至关重要.
研究的目的:
- 量化分析顶煤极限平衡区边界空间形态的演变及其入效应.
- 揭示"支周围岩石"系统在的煤层中的不稳定机制.
主要方法:
- 工程背景来自Changshanzi煤矿的一个完全机械化的洞穴面.
- 边界空间形态演变和入效应的定量分析.
- 确定了三个进化阶段:初始的,不对称的弧形带状曲面形成,以及稳定的.
主要成果:
- 顶层煤炭断层边界演变表现出不对称性和沿入和冲击方向的顺序进展.
- 随着工作面的推进,不对称性会加剧.
- 随着俯冲角的增加,进化加速,导致故障深度的增加和更明显的不对称性.
结论:
- 这项研究提供了详细的了解顶层煤失效边界进化在的沉浸煤层.
- 这些发现为指导类似采矿业务的安全和高效生产提供了理论支持.
- 识别的阶段和不对称性是管理系统稳定的关键.
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