近水平煤层开采上覆岩层运动与沉陷规律相关研究  

Study on the relation between stratum movement and subsidence of flat seam mining

作　　者：王崇革[1] 宋振骐[2] 石永奎[2] 郑文华[2] 

机构地区：[1]山东科技大学力学教研室,山东泰安271019 [2]山东科技大学资源与环境工程学院,山东泰安271019

出　　处：《岩土力学》2004年第8期1343-1346,共4页Rock and Soil Mechanics

基　　金：国家自然科学基金资助项目(No.50028403)。

摘　　要：将近水平煤层开采的上覆岩层运动与地表沉陷作为一个整体系统进行研究,论述了采场上覆岩层的运动规律和裂隙拱的形成及发展变化过程。并结合地表沉陷的GPS观测,确定了针对具体地质条件的地表移动变形边界角、移动角,找到了井下工作面推进位置与地表下沉速度之间的关系。We can look the stratum movement and subsidence as a whole system to study. The common nature of stratum movement and the development procedure of crack arch are described. Meanwhile, based on the ground observation by the global positioning system (GPS), the boundary angle and the motion angle, which aim at special geologic conditions, are determined. The relation between the position of underground working face and ground subsidence velocity are found.

关 键 词：矿山压力 岩层运动 地表沉陷 沉陷规律 

分 类 号：TD327[矿业工程—矿井建设]