摘要
斜坡岩体由小变形到大变形乃至滑坡的发生，实质上是由组成斜坡的各子系统协同作用的结果。本文在作者已建立的斜坡失稳时间的协同预测模型的基础上，进一步深入地探讨了斜坡体系在演化过程中的非线性行为。
From slight deformation to large deformation even to sliding, the evolution cause of slope is generally resulted by synergetic interactions of all sub systems which consist in slope. On the basis of synergetic prediction model of slope instability which is presented by authors, nonlinear features which slopes show in the course of development are discussed in this paper, meanwhile, trigger effect of external factors is studied.
出处
《中国地质灾害与防治学报》
CSCD
1997年第1期7-11,共5页
The Chinese Journal of Geological Hazard and Control
基金
国家杰出青年科学基金
霍英东基金
关键词
斜坡
演化规律
自组织
滑坡
slope, evolutional rule, self organization, lyapunov exponent, bifurcation, chaos, catastrophe theory, trigger effect
