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水位涨落对库岸滑坡孔隙水压力影响的非饱和渗流分析
Unsaturated seepage analysis of the influence of water level fluctuation on pore water pressure of landslide in reservoir area
【Author】 LIU Qun-yi~1 ZHU Zi-qiang~1 HE Xian-qi~1 LU Guang-yin~1 TANG Jun-feng~(2,3) (1. School of Info-physics and Geomatics Engineering, Central South University, Changsha 410083, China; 2. School of Resources & Safety Engineering, Central South University, Changsha, 410083, China; 3. Central South Design and Research Institute, CHECC Changsha 410014, China)
【机构】 中南大学信息物理工程学院; 中南大学资源与安全工程学院; 中国水电工程顾问集团公司中南勘测设计研究院;
【摘要】 以某水库库岸滑坡为工程背景,根据饱和-非饱和渗流控制方程,针对不同滑坡体渗透性和库水位升降速率,研究库水位变化条件下滑坡体内孔隙水压力的动态响应,得到:(1)水位升降时,在相同的入渗条件下,饱和渗透系数对初始地下水位有明显的影响;增大饱和渗透系数能降低地下水位,使地下水位线变得平缓,滑坡体的动、静水压力减小,有利于稳定;(2)增加库水位升降速率,地下水位响应滞后变得显著,地下水位线形态整体变陡,滑坡体的动水压力增大,不利于边坡稳定性。
【Abstract】 Iandslide in a certain reservoir area is chosen as the engineering background.According to the saturated-unsaturated seepage equation,the dynamic response of pore water pressure in the landslide influenced by the fluctuation of water level is studied when considering the infiltration characteristics and the fluctuation velocity of water level.The analysis results show that(1)when the water level fluctuates,the saturated permeability coefficient has great impact on the initial water level under the same infiltration condition;with the increase of the saturated permeability coefficient,the water level becomes lower,and the water level line becomes more smooth,which has smaller impact on the dynamic and static pore water pressure,and is good to the slope stability;(2) with the increase of fluctuation velocity of water level,the response of water level lags behind,the water level line becomes steeper, which causes greater dynamic pore water pressure to the slope,and is worse to the slope stability.
【Key words】 water level fluctuation; slope at reservoir area; pore water pressure; unsaturated seepage;
- 【会议录名称】 第二届中国水利水电岩土力学与工程学术讨论会论文集(一)
- 【会议名称】第二届中国水利水电岩土力学与工程学术讨论会
- 【会议时间】2008-11
- 【会议地点】中国湖北武汉
- 【分类号】TV223.4
- 【主办单位】中国水利学会岩土力学专业委员会