工作面导水裂隙带高度观测分析
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  • 英文篇名:Height observation and analysis of water conducting fissure zone in working face
  • 作者:张陆
  • 英文作者:ZHANG Lu;Xishan coal and electricity Ma Lan coal mine;
  • 关键词:回采工作面 ; 导水裂隙带 ; 观测分析
  • 英文关键词:Coal face;;Water conducting fissure zone;;Observation and analysis
  • 中文刊名:MKXD
  • 英文刊名:Coal Mine Modernization
  • 机构:西山煤电马兰矿;
  • 出版日期:2019-04-01
  • 出版单位:煤矿现代化
  • 年:2019
  • 期:No.150
  • 语种:中文;
  • 页:MKXD201903021
  • 页数:3
  • CN:03
  • ISSN:37-1205/TD
  • 分类号:65-67
摘要
工作面回采后上覆岩层遭到破坏,下沉形成导水裂隙,导水裂隙带高度的确定对于顶板水害的防治具有重要的意义。文中首先对导水裂隙带高度观测系统工作原理及系统构成进行了阐述,其次对回采工作面垮落带和弯曲下沉带理论计算分析,最后将导水裂隙带高度观测系统运用到回采工作面导水裂隙观测实践。研究结果表明导水裂隙带高度观测系统可以有效的确定工作面上覆导水裂隙带高度,实测结果对指导该矿防治顶板突水具有重要的参考意义。
        The overlying strata are destroyed after the working face, and the subsidence is formed to form the water guide fissure, and the determination of the height of the water guide fissure zone is of great significance to the prevention and control of the water damage of the roof. In this paper, the working principle and system composition of the height observation system of water conducting fracture zone are first described.Secondly, the theoretical calculation and analysis of the caving zone and the bending and sinking zone of the mining face are analyzed. Finally,the water guide fracture zone height observation system is applied to the observation practice of water guide fissure in the mining face. The results show that the height of the water fissure zone on the surface of the working face can be determined effectively by the height observation system of the water conducting fracture zone. The measured results have important reference significance for guiding the prevention and control of the roof water inrush of the mine.
引文
[1]李超峰,刘英锋,李抗抗.导水裂隙带高度井下仰孔探测装置改进及应用[J].煤炭科学技术,2018,46(05):166-172.
    [2]李超.煤炭开采中导水裂隙带发育高度预测的研究[J].内蒙古煤炭经济,2016(17):88-89.
    [3]高保彬,刘云鹏,潘家宇,袁恬.水体下采煤中导水裂隙带高度的探测与分析[J].岩石力学与工程学报,2014,33(S1):3384-3390.
    [4]郝天轮,王东成,李玉梅.薄煤层开采覆岩导水裂隙带高度的确定[J].山东煤炭科技,2013(03):96-97.
    [5]刘德清.综放开采冒落带发育规律及应用研究[D].山东科技大学,2011.

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