煤炭工程 ›› 2016, Vol. 48 ›› Issue (4): 89-92.doi: 10.11799/ce201604027

• 研究探讨 • 上一篇    下一篇

煤层重复采动关键层失稳与地表移动规律研究

宋利杰   

  1. 华北理工大学
  • 收稿日期:2015-11-02 修回日期:2015-12-28 出版日期:2016-04-10 发布日期:2016-04-18
  • 通讯作者: 宋利杰 E-mail:slj_hblg@126.com

The study between the destabilization of key strata influenced on repeating seam mining and the regularity of surface movement

  • Received:2015-11-02 Revised:2015-12-28 Online:2016-04-10 Published:2016-04-18

摘要: 基于滕南地区两个煤矿的岩移数据、导水裂缝带高度观测数据和工作面钻孔资料,分析两煤矿3上、3下工作面重复采动下地表移动规律与关键层的关系,对比研究重复开采时关键层有无失稳两种情况下地表的移动规律,并通过导水裂缝带高度观测进行验证,总结了近距离煤层重复开采关键层的变化对地表移动规律的影响。结果表明:重复开采不破坏关键层时,地表移动不会产生明显变化|对关键层造成破坏时,地表移动会加剧。

关键词: 重复采动, 地表移动, 关键层, 导水裂缝带

Abstract: Based on the rock movement data of two coal mines in the TengNan area, height observation data of water flowing fractured zone and borehole data of the working face, the paper analyses the relationship between the surface movement rule and the key strata under upper and lower No.3 coal seams situation. According to the analysis of key strata and the comparative study on the regularity rule of surface movement depend on the key strata buckling or not under repeating mining condition, adding verification of overburden rock damage by observing water flowing fractured zone height under different repeated mining conditions , the paper put forward that the change of repeating mining at short range will impact the regularity of surface movement. The results showed that surface movement won’t have significant change when repeating mining doesn’t destroy the key strata. 0therwise, surface movement will get intensified.

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