三峡库区康家嘴滑坡破坏过程及演绎研究

三峡库区康家嘴滑坡是在其老滑坡泥石流的前缘堆积扇体中形成的新滑动变形体。滑体表面为第四纪风化土层,滑带为灰绿色粉质粘土或粘土,在降雨与库区蓄水的周期性浸泡作用下,饱和后蠕滑变形,处于欠稳定-极限稳定状态,亟需整治。本文针对其破坏过程及形态加以详细描述,并对滑坡的阶段性演绎过程加以追溯。在查清滑坡地质条件与发展趋势的基础上,通过经济对比分析,对康家嘴滑坡不同变形阶段提出了具有针对性的防治方案:在新滑坡体(强变形区)采用抗滑桩+排水沟+局部回填压脚、后部变形体采用抗滑桩+排水沟。经对滑体计算,该滑坡体处于稳定状态,达到了防灾减灾的目的。     

DAMAGE MODEL OF CONTROL FISSURE IN PERILOUS ROCK

Hitherto, perilous rock is the weakest topic in disasters studies. Specially, damage of control fissure under loads is one key technique in study of develop mechanism of perilous rock. Damage division of end area of control fissure was defined by authors, then calculation methods of timed-Poisson's ratio and timed-Young's modulus were established in damage mechanics theory. Further, the authors set up damage constitutive equation of control fissure, which founds important basis to numerical simulation for control fissure to develop.     

危岩主控结构面损伤模型研究

危岩是迄今研究程度极其薄弱的地质灾害类型,而主控结构面受荷损伤是危岩发育机理研究的核心技术．通过定义主控结构面裂端损伤区,运用损伤力学方法建立了裂端损伤区的即时泊松比和即时弹性模量的计算方法,并据此构建了主控结构面裂端损伤本构方程,为主控结构面断裂演化数值模拟奠定了理论基础．