(1.成都理工學(xué)院工程地質(zhì)研究所, 成都 610059;
2.東北大學(xué), 沈陽(yáng) 110006)
摘 要: 含有不連續(xù)面的巖石力學(xué)系統(tǒng)，在沿不連續(xù)面的滑動(dòng)過(guò)程中，其響應(yīng)結(jié)果與滑動(dòng)的位移、滑動(dòng)的速度密切相關(guān)。該文對(duì)此現(xiàn)象進(jìn)行了理論分析，指出在一定的滑動(dòng)速度范圍內(nèi)，滑體隨著滑動(dòng)位移的積累，滑動(dòng)速度發(fā)生突變。
關(guān)鍵字: 不連續(xù)面 巖石試件 突變 負(fù)阻尼
（1.Engineering Geology Institute of Chengdu Institute of Technology, Chengdu 610059
2.Northeastern University, Shenyang 110006）
Abstract:The responding result of a rock machanics system, which contains discontinuous faces, is related closely to the displacement and velocity of sliding. This phenomenon has been analysed in the paper and a viewpoint is put forward, that is, in a certain range of relative slipping velocity, the catastrophe of slipping velocity occurs with the accumlating of slipping displacement.
Key words: discontinuous face rock sample catastrophe negative damping
