Transactions of Nonferrous Metals Society of China The Chinese Journal of Nonferrous Metals

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中国有色金属学报

ZHONGGUO YOUSEJINSHU XUEBAO

第10卷    第3期    总第36期    2000年6月

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文章编号:1004-0609(2000)03-0451-04
边坡残余构造应力引起的宏观破坏特征及机制
杜炜平1, 古德生1, 颜荣贵2

(1. 中南工业大学资源环境与建筑工程学院, 长沙410083; 2. 长沙矿冶研究院, 长沙410012)

摘 要: 针对某采场软岩边坡大型滑坡破坏体罕见的宏观破坏特征, 研究了边坡开挖时残余构造应力释放对岩体的作用机制和泥化夹层水膜化效应的力学原理。研究结果表明, 该矿软岩边坡的破坏特征受控于残余构造应力释放及泥化夹层水膜化效应。

 

关键字:  软岩边坡; 残余构造应力; 歪斜滑移; 泥化夹层; 水膜效应

Mechanism and macrocharacters of landslide caused by relief of residual tectonic stress
DU Wei-ping1, GU De-sheng1, YAN Rong-gui2

1. College of Resource, Environment and Civil Engineering, Central South University of Technology, Changsha 410083, P.R.China;
2. Changsha Research Institute of Mining and Metallurgy, Changsha 410012,P.R.China

Abstract:As for rare macrocharacters of landslide of soft rock slope in a mine, the mechanism that the residual tectonic stress impacted the slope and the mechanics of waterfilm of intercalated clay layer were studied. The result verifies that the macrocharacter of the slope slide is controlled by the relief of residual tectonics stress and waterfilm of the weak layer.

 

Key words: soft rock slope; residual stress; slope sliding; intercalated clay layer; effect of water film

ISSN 1004-0609
CN 43-1238/TG
CODEN: ZYJXFK

ISSN 1003-6326
CN 43-1239/TG
CODEN: TNMCEW

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