Mechanical model and numerical simulation of the formation of karst collapse columns in the Huainan coalfield of Northern China

被引:2
|
作者
Zhang, Haitao [1 ,4 ]
Xu, Guangquan [1 ]
Zhang, Yanxi [2 ]
Tang, Ming [3 ]
Zhang, Gang [2 ]
Liu, Xiaoguo [3 ]
机构
[1] Anhui Univ Sci & Technol, Sch Earth & Environm, Huainan, Peoples R China
[2] Huainan Min Grp Co Ltd, Dept Geol & Hydrogeol, Xieqiao Coal Mine, Huainan, Peoples R China
[3] Huainan Min Grp Co Ltd, Dept Geol & Hydrogeol, Zhangji Coal Mine, Huainan, Peoples R China
[4] Anhui Univ Sci & Technol, Sch Earth & Environm, Huainan 232001, Peoples R China
基金
中国国家自然科学基金;
关键词
Karst collapse columns (KCCs); roof collapse; formation mechanism; cave; 3DEC; INRUSH;
D O I
10.1177/01445987231168715
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Karst collapse columns (KCCs) are channels where groundwater and gas gather, and they pose a great threat to mining safety. In this study, a mechanical model and criterion for the roof collapse of KCCs were established, and simulations were performed to analyze the formation mechanism of KCCs in the Huainan coalfield of Northern China. The results showed that the roof collapse and upward development of KCCs were facilitated by increasing the cave radius of the KCC basement and decreasing the groundwater pressure, single-layer thickness of the roof strata, lateral pressure coefficient of the rock mass, and cohesion and internal friction angle between fractures. The KCC formation process in the Huainan coalfield could be divided into four stages: (I) early collapse, (II) middle-early rapid collapse, (III) middle-late slow collapse, and (IV) late filling compaction. The simulation results were generally consistent with actual KCCs observed in the Huainan coalfield, which verified the theoretical analysis. The results of this study provide an important reference for the formation mechanism and evolution of KCCs in Northern China.
引用
收藏
页码:1356 / 1373
页数:18
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