Reseach on Controlling of Rock Mass Structure on Water Inrush From Coal Seam Floor in Huaibei Mining Area
Huaibei Mining Area is located in the south of the North China Coal-bearing Region. Its hydrogeological condit(i)on has basic features of the North China Coalfield. The hydrogeological condition is complex. The mining in the coal seam of Shanxi Formation where water inrush from coal seam floor happened mang times is generally seriously, threatened by the limestone water from floor. The paper systematically analyzes typical cases about water inrush from coal seam floor in the researched area, and uncovered the different features of water inrush caused by different geological structure condition and water-inrush passage, which is of typical meaning to study controlling of rock mass structure on water inrush from coal seam floor.
water inrush from floor water inrush mechanism rock mass structure Huaibei mining area
WU Jiwen JIANG Zhenquan ZHAI Xiaorong
Anhui University of Science and Technology, Huainan 232001, China China University of Mining and Technology, Xuzhou 221008, China
国际会议
The First International Symposium on Mine Safety Science and Engineering (首届矿山安全科学与工程学术会议)
北京
英文
358-365
2011-10-27(万方平台首次上网日期,不代表论文的发表时间)