A study on the law of overlying strata migration and separation space evolution under hard and thick strata in underground coal mining by similar simulation

被引:29
作者
Wu, Quansen [1 ]
Jiang, Lishuai [2 ,3 ]
Wu, Quanlin [4 ]
Xue, Yanchao [1 ]
Gong, Bin [1 ,5 ]
机构
[1] Shandong Univ Sci & Technol, Sch Min & Safety Engag, Qianwangang Rd 579, Qingdao 266590, Peoples R China
[2] Shandong Univ Sci & Technol, State Key Lab Min Disaster Prevent & Control Cofo, Qianwangang Rd 579, Qingdao 266590, Peoples R China
[3] Shandong Univ Sci & Technol, Minist Sci & Technol, Qianwangang Rd 579, Qingdao 266590, Peoples R China
[4] Jining Univ, Dept Chem & Chem Engn, Xingtan Rd 1, Qufu 273100, Peoples R China
[5] Nagasaki Univ, Grad Sch Engn, Nagasaki 8528521, Japan
来源
DYNA | 2018年 / 93卷 / 02期
基金
中国国家自然科学基金;
关键词
hard and thick key strata; similar simulation; overlying strata movement; separated stratum; dynamic disasters; ROCKBURST; ROCK; MINES; ZONES;
D O I
10.6036/8678
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Fracture of the hard and thick key layer can easily cause dynamic disasters, such as the rock burst and mine seismicity, which seriously threatens the safety of underground coal mining. To analyze the characteristics of overlying strata fracture and law of evolution of separation fissures under hard and thick strata in underground coal mining, and further reveal the process of the occurrence of dynamic disasters, the fracture characteristics of overlying strata during underground coal mining were analyzed via similar simulation in this study. The characteristics of surface movement and deformation before and after the fracture of hard and thick strata were then discussed based on the law of overlying rock displacement. Finally, the development law of separation fissures under the hard and thick strata was revealed. Results show that the key stages of overlying strata movement during underground coal mining are immediate roof fracture, main roof fracture; main roof cycle fracture, and hard and thick rock fracture, respectively. Before the hard and thick strata are fractured, as the key layer, bearing the weight of the overlying strata and the overburden strata subsidence is small. The developmental height of the separated stratum stops at the bottom of the hard and thick strata, and the separated stratum stays in an unclosed state for a long time, which provides the incubation space for the accumulation of gas and water in the strata. After the hard and thick strata are fractured, the subsidence of the overlying strata increases dramatically, and the separated stratum is closed rapidly, inducing gas outburst, water inrush, dramatically surface subsidence, and other disasters in the working face. The research results of this study are of considerable significance to the safe mining of working face under similar geological conditions.
引用
收藏
页码:175 / 181
页数:7
相关论文
共 33 条