Affiliation:
1. School of Mines China University of Mining & Technology Xuzhou Jiangsu 221116 China cumt.edu.cn
2. Jiangsu Engineering Laboratory of Mine Earthquake Monitoring and Prevention Xuzhou China University of Mining & Technology Xuzhou Jiangsu 221116 China cumt.edu.cn
3. Xuzhou Wushuo Information Co. Ltd Xuzhou Jiangsu 221116 China
4. School of Civil Engineering & Architecture Changzhou Institute of Technology Changzhou Jiangsu 213032 China czu.cn
Abstract
Abstract
With the increase of mining depth, rock burst disasters frequently occur in steeply inclined coal seams. Firstly, this paper analyzes the rock burst of 5521-20 working face in Yaojie No. 3 coal mine and summarizes the characteristics of rock burst in horizontal section mining of steeply inclined extra-thick coal seam (SIETCS). Then, the static load distribution characteristics and the influence of dynamic load in the horizontal section mining of SIETCS are systematically studied by combining theoretical analysis with numerical simulation. On this basis, the mechanism of rock burst in horizontal section mining of SIETCS is put forward, verified by actual measurement. The results show that the SIETCS is “clamped” under the combined action of the same change trend of roof and floor. The maximum principal stress peak values on the roof and floor sides reach 22.0 MPa and 20.5 MPa. The maximum shear stress earned 8.7 MPa and 8.4 MPa, which makes the shear stress concentration in the coal body high and tends to “shear dislocation.” Under this “shear-clamping” action, an approximate “trapezoidal” plastic zone and a “rectangular” stress concentration zone are formed under the section. With the increase of mining depth, the “shear-clamping” action of SIETCS becomes more and more intense. When the roof cantilever reaches the ultimate span and breaks, the intense dynamic load increases the shear stress and failure of coal, which is easy to induce rock burst. The superimposed load greatly affects the area from the roof side to the middle of the working face, and the rock burst is intense. The rock burst is weak on the floor side due to the pressure relief of the surrounding plastic zone. The monitoring results show that the supports pressure and MS events activity on the roof side and near the middle part of the working face is considerable, while the floor side is opposite, which verifies the research results.
Funder
Graduate Research and Practice Innovation Program of Jiangsu Province
Major Science and Technology Innovation Program of Shandong Province
National Natural Science Foundation of China
Cited by
6 articles.
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