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承压水底板关键层失稳的尖点突变模型
引用本文:白晨光,黎良杰.承压水底板关键层失稳的尖点突变模型[J].煤炭学报,1997,22(2):149-154.
作者姓名:白晨光  黎良杰
作者单位:[1]北京科技大学 [2]北京大学
摘    要:根据煤矿长壁工作面的布置以及底板突水的可能性分析,提出了底板关键层的力学模型;在此基础上,应用突变理论的方法,对底板关键层的力学模型进行分析,推导出了关键层系统的总势能函数表达式,建立了底板关键层的尖角(CUSP)型突变模型。根据这一模型分析了承压水底板关键层失稳的力学机制,得到的结论符合实际情况,为研究煤矿底板突水机制引入了一种新的理论分析方法。

关 键 词:突变理论  尖角型模型  底板突水  关键层

CUSP CATASTROPHE MODEL FOR INSTABILITY OF KEYSTRATUM IN FLOOR WITH WATER INRUSH
Bai Chenguang.CUSP CATASTROPHE MODEL FOR INSTABILITY OF KEYSTRATUM IN FLOOR WITH WATER INRUSH[J].Journal of China Coal Society,1997,22(2):149-154.
Authors:Bai Chenguang
Affiliation:Bai Chenguang(University of Science and Technology Beijing) Li Liangjie(Peking University) Yu Xuefu(University of Science and Technology Beijing)
Abstract:Based on layout of a longwall face and possibility of water inrush from the floor,a mechanical model of a key stratum is proposed,with the help of catastrophic theory,the mechanical model of a key stratum is analyzed,and an expression of total potential energy function is derived.A cusp catastrophe model of a key layer of floor is established.The mechanical mechanism of instability of a unstable key layer in the floor with confined water is studied.The conclusions from the investigation conform with the practical situation.It is a new theoretical approach for studying the mechanism of water inrush from the floor.
Keywords:catastrophic theory  cusp model  water inrush from the floor  key stratum
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