放顶煤开采上覆巨厚砾岩层变形移动规律研究
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  • 英文篇名:Study on the deformation movement law of hugely-thick conglomerate stratum over longwall top coal caving
  • 作者:翟新献 ; 赵晓凡 ; 涂兴子 ; 李如波 ; 卢德芳
  • 英文作者:ZHAI Xinxian;ZHAO Xiaofan;TU Xingzi;LI Rubo;LU Defang;School of Energy Science and Engineering,Henan Polytechnic University;Tianan Coal Mining Co.,Ltd.,of Pingdignshan;Gengcun Coal Mine,Henan Dayou Energy Co.Ltd.;
  • 关键词:特厚煤层 ; 放顶煤开采 ; 巨厚砾岩层 ; 变形移动 ; 裂隙场 ; 初次来压
  • 英文关键词:extremely-thick coal seam;;longwall top coal caving;;hugely-thick conglomerate stratum;;deformation movement;;fractured field;;first weighting
  • 中文刊名:JGXB
  • 英文刊名:Journal of Henan Polytechnic University(Natural Science)
  • 机构:河南理工大学能源科学与工程学院;平顶山天安煤业股份有限公司开拓处;河南大有能源股份有限公司耿村煤矿;
  • 出版日期:2019-01-14 14:12
  • 出版单位:河南理工大学学报(自然科学版)
  • 年:2019
  • 期:v.38;No.188
  • 基金:国家自然科学基金资助项目(51574110,51674102)
  • 语种:中文;
  • 页:JGXB201903003
  • 页数:8
  • CN:03
  • ISSN:41-1384/N
  • 分类号:23-30
摘要
放顶煤开采时上覆巨厚砾岩层垮落直接影响综放工作面的安全生产,为了研究放顶煤开采上覆巨厚砾岩层变形移动规律,以河南大有能源股份有限公司耿村煤矿综放工作面特厚煤层及其上覆巨厚砾岩层为工程背景,采用相似材料模拟试验,研究了放顶煤开采时上覆巨厚砾岩层变形移动全过程。结果表明:(1)随着煤层开采,依据巨厚砾岩层裂隙场的特征,巨厚砾岩层变形移动和垮落的全过程分为下位和上位垮落过程,其中下位砾岩层初次断裂时垮落体形态为梯形,上位砾岩层断裂控制着地表的变形;(2)当工作面停采后,巨厚砾岩层裂隙演化发展具有较明显的时间效应;(3)下位砾岩层初次垮落步距650. 0 m,周期垮落步距175. 0 m,上位砾岩层初次垮落步距825. 0 m,地表下沉系数0. 267。研究结果可为耿村煤矿巨厚砾岩层下综放开采提供安全技术支撑。
        The collapse of hugely-thick conglomerate stratum (HTCS) over longwall top coal caving (LTCC) affects its safe production. Taking the coal face extremely-thick coal seam and its overlying HTCS in Gengcun coal mine as the engineering background,the whole process of deformation movement of HTCS over the coal face was studied with similar simulation test. The results showed that: (1) With the coal mining,the whole process of deformation movement and collapse of HTCS was divided into ones in the lower and in the upper conglomerate stratum based on the characteristics of the fractured field of HTCS. There was trapezoidal caving body when the lower conglomerate stratum was firstly fractured,while the surface deformation was controlled by the upper conglomerate stratum fractured. (2) When the coal face advancement was stopped,there was obvious time effect on the evolution of the fractures in HTCS. (3) The parameters of deformation movement of HTCS were obtained. The first caving interval of the lower conglomerate stratum was 650. 0 m,the periodic caving interval was 175. 0 m,and the first caving interval of the upper conglomerate stratum was 825. 0 m. The surface subsidence coefficient was 0. 267. The conclusions provided a technical support for LTCC under HTCS in Gengcun coal mine.
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