Rock Burst Mechanism under Coupling Action of Working Face Square and Regional Tectonic Stress

被引:8
作者
Zhu, Sitao [1 ]
Ge, Decheng [1 ]
Jiang, Fuxing [1 ]
Wang, Cunwen [2 ]
Li, Dong [3 ]
Shang, Xiaoguang [1 ]
Zhang, Baoliang [4 ]
Wang, Zhaoyi [5 ]
机构
[1] Univ Sci & Technol Beijing, Sch Civil & Resource Engn, Beijing 100083, Peoples R China
[2] Shandong Energy Grp Co LTD, Res Ctr Rock Burst Control, Jinan 250014, Shandong, Peoples R China
[3] North China Inst Sci & Technol, Safety Engn Coll, Beijing 101601, Peoples R China
[4] Liaocheng Univ, Sch Architecture & Civil Engn, Liaocheng 252059, Shandong, Peoples R China
[5] Shandong Energy Feicheng Min Grp Co LTD, Liangbaosi Coal Mine, Jining 272400, Shandong, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
IN-SITU; ROCKBURST;
D O I
10.1155/2021/5538179
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
With the development of faults in many coalfields, many large faults will form a relatively independent area, forming regional tectonic stress concentration. Under the influence of mining, it is easy to induce fault activation, produce mine tremor, and then induce rock burst. Through field investigation, theoretical analysis, numerical simulation, and engineering verification, the overburden movement model of No. 3504 working face square and fault activation in Liangbaosi Coal Mine was established. The stress variation and energy release law of working face advance and fault area were analyzed, and the mechanism of rock burst under the coupling action of working face square and regional tectonic stress was revealed. The results show that the regional stress adjustment and fault activation are caused by the large-scale overall movement of overburden during the working face square, and there is a peak value of elastic energy release during the fault activation, which is easy to produce large energy mine earthquake. The energy level of the daily maximum energy event is higher than that of the initial mining stage in the square period, and the location of on-site large energy microseismic event is basically consistent with the predicted fault strike. The study provides a theoretical basis for the prevention and control of rock burst during the working face square under the condition of regional tectonic stress.
引用
收藏
页数:11
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