程潮铁矿西区采空区地表塌陷机制与变形规律初探
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  • 英文篇名:Study on the mechanism of surface collapse and ground deformation in western mined area of of Chengchao iron mine
  • 作者:宋许根 ; 刘秀敏 ; 陈从新 ; 郑先伟 ; 夏开宗 ; 杨括宇 ; 陈山
  • 英文作者:SONG Xugen;LIU Xiumin;CHEN Congxin;ZHENG Xianwei;XIA Kaizong;YANG Kuoyu;CHEN Shan;State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences;University of Chinese Academy of Science;WISCO Resources Group Chengchao Mining Co.,Ltd.;
  • 关键词:采矿工程 ; 地下采矿 ; 塌陷机制 ; 矿山监测 ; 地表变形规律
  • 英文关键词:mining engineering;;underground mining;;mechanism of ground collapse;;mine monitoring;;surface deformation
  • 中文刊名:YSLX
  • 英文刊名:Chinese Journal of Rock Mechanics and Engineering
  • 机构:中国科学院武汉岩土力学研究所岩土力学与工程国家重点实验室;中国科学院大学;武钢资源集团程潮矿业有限公司;
  • 出版日期:2018-10-15
  • 出版单位:岩石力学与工程学报
  • 年:2018
  • 期:v.37;No.347
  • 基金:国家自然科学基金资助项目(41602325);; 国家重点研发计划专项(2017YFC0805307);; 中国科学院青年创新促进会资助项目(2015271)~~
  • 语种:中文;
  • 页:YSLX2018S2048
  • 页数:12
  • CN:S2
  • ISSN:42-1397/O3
  • 分类号:465-476
摘要
以程潮铁矿西区为例,依据地质调查分析与地表水平位移和垂直位移监测成果,结合采空区顶板崩落钻孔监测和崩落区高密度电法勘探等手段,分析程潮铁矿西区顶板崩落特征和在2006年采矿初期地表塌陷机制,探讨地面塌陷以后地表变形规律。研究结果表明:采空区顶板崩落呈间断的、不连续的特点,当顶板崩落传递到石膏岩时,石膏岩呈整体向下垮落的特点;石膏岩作为岩溶地下水隔水层的存在,对采矿初期地表塌陷起重要作用;电法探测的结果表明,采矿初期阶段地表塌陷不是由于顶板崩落传递到地表引起,塌陷的根本原因,是由于岩溶中的地下水迅速排泄引起的岩溶塌陷;这种塌陷机制作用下地表塌陷的位置有可能是在采空区正上方,也可能在采空区边缘;塌陷发生以后,地表变形呈漏斗状不断向外扩展,测点加速时间与地下采矿推进有很好的对应关系,表明地下采矿引起的岩层扰动已经传递到地表,地表变形受地下采矿的控制。
        Taking west area of Chengchao iron mine as background engineering. According to the analysis of geological survey and the monitoring results from horizontal displacement and subsidence displacement in the west area of Chengchao Iron mine,and combining with approaches of drill-hole monitoring in goaf roof and high-density electrical prospecting in cave region,then the roof collapse characteristics and the ground collapse mechanism are analyzed,besides the law of surface deformation after ground collapse. The research results indicate that the process of goaf roof collapse is intermittent,and whole sinking occurs when the goaf roof collapse spreads upwards to gypsum stratum. Large amounts of groundwater are deposited in rock fractures and karst caves due to the aquiclude of gypsum,which has great influence on surface subsidence in preliminary stage of mining. High-density electrical prospecting results prove that the essential reason to the surface collapse is the rapid increased negative pressure generated by fast dewatering after gypsum stratum collapsed. Under the action of this mechanism,the location of surface collapse may be either right above the mined-out or near the mined-out boundary. Surface deformation extends outward with funnel-shaped tendency,and the displacements increasing timing of measuring points corresponds to the proceeding of underground mining well,showing that rock disturbance caused by underground mining has already extended to surface and ground collapse is controlled by the underground mining.
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