煤炭工程 ›› 2013, Vol. 45 ›› Issue (6): 90-92.doi:

• 研究探讨 • 上一篇    下一篇

张村矿断层突水特征分析研究

黄存捍   

  1. 河南理工大学
  • 收稿日期:2012-09-06 修回日期:2013-01-20 出版日期:2013-06-10 发布日期:2013-06-10
  • 通讯作者: 黄存捍 E-mail:huangcunhan@163.com

Characteristic Analysis of Fault Water Inrush in Zhangcun mine

  • Received:2012-09-06 Revised:2013-01-20 Online:2013-06-10 Published:2013-06-10

摘要: 针对张村矿断层突水问题,分析了矿区断层分布规律。基于距离判别法对张村矿主要影响断层突水等级进行了判别分析,结果表明:因煤层与太原组石灰岩之间的隔水层太薄,小于底板采动破坏深度,太原组石灰岩水比寒武系石灰岩水更容易发生突水;断层落差越大,在高水压作用下突水或涌水量会增大,因为断层的落差大小决定了其切割深度,其富水性会越强。分析结果与矿区实际情况和瞬变电磁探测结果是吻合的。根据研究结果提出矿区断层突水防治措施,对于矿井安全生产具有一定的指导意义。

关键词: 断层突水, 寒武系石灰岩含水层, 距离判别法, 瞬变电磁探测

Abstract: According to the fault water inrush of Zhangcun mine, the distribution of faults in the mine is analyzed. Based on the distance discriminant analysis method, the water inrush grades of the main effect faults in Zhangcun mine are discriminated. The results show that the taiyuan formation limestone aquifer causes fault water inrush more easily than the Cambrian limestone aquifer does because the thickness of aquifuge between the coal seam and the taiyuan formation limestone aquifer is less than the mining failure thickness of floor. In addition, the larger the fault displacement is, the bigger the water inrush quantity will be in high water pressure. Because the large displacement fault will cut to the Cambrian limestone aquifer, and its water abundance is more stronger than others. The analysis results also consistent to the real condition and the transient electromagnetic exploration results in Zhangcun mine. According to the research results, the prevention measures of fault water inrush are proposed, which have some guiding significance to ensure the safe production of the mine.

Key words: Fault water inrush, the Cambrian limestone aquifer, the distance discriminant analysis method, the transient electromagnetic exploration

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