Reservoir-induced landslides and risk control in Three Gorges Project on Yangtze River,China

被引:75
作者
Yueping Yin [1 ]
Bolin Huang [2 ]
Wenpei Wang [1 ]
Yunjie Wei [1 ]
Xiaohan Ma [3 ]
Fei Ma [4 ]
Changjun Zhao [5 ]
机构
[1] China Institute of Geo-Environment Monitoring China Geological Survey
[2] Wuhan Center of China Geological Survey
[3] Department of Land and Resources of Hubei Province
[4] Department of Land and Resources of Chongqing
[5] Changjiang Institute of Survey,Planning,Design and Research Co,Ltd
关键词
Three Gorges Reservoir(TGR); Reservoir-induced landslide; Reactivation mechanism; Impulsive wave generated by landslide; Water level variation; Risk control;
D O I
暂无
中图分类号
TV697.2 [水库观测]; P642.22 [滑坡];
学科分类号
081504 ; 0837 ;
摘要
The Three Gorges region in China was basically a geohazard-prone area prior to construction of the Three Gorges Reservoir(TGR).After construction of the TGR,the water level was raised from 70 m to 175 m above sea level(ASL).and annual reservoir regulation has caused a 30-m water level difference after impoundment of the TGR since September 2008.This paper first presents the spatiotemporal distribution of landslides in six periods of 175 m ASL trial impoundments from 2008 to 2014.The results show that the number of landslides sharply decreased from 273 at the initial stage to less than ten at the second stage of impoundment.Based on this,the reservoir-induced landslides in the TGR region can be roughly classified into five failure patterns,i.e.accumulation landslide,dip-slope landslide,reversed bedding landslide,rockfall,and karst breccia landslide.The accumulation landslides and dip-slope landslides account for more than 90%.Taking the Shuping accumulation landslide(a sliding mass volume of 20.7 × 10~6 m3) in Zigui County and the Outang dip-slope landslide(a sliding mass volume of about 90 × 10~6 m3) in Fengjie County as two typical cases,the mechanisms of reactivation of the two landslides are analyzed.The monitoring data and factor of safety(FOS) calculation show that the accumulation landslide is dominated by water level variation in the reservoir as most part of the mass body is under 175 m ASL,and the dip-slope landslide is controlled by the coupling effect of reservoir water level variation and precipitation as an extensive recharge area of rainfall from the rear and the front mass is below 175 m ASL.The characteristics of landslide-induced impulsive wave hazards after and before reservoir impoundment are studied,and the probability of occurrence of a landslide-induced impulsive wave hazard has increased in the reservoir region.Simulation results of the Ganjingzi landslide in Wushan County indicate the strong relationship between landslide-induced surge and water variation with high potential risk to shipping and residential areas.Regarding reservoir regulation in TGR when using a single index,i.e.1-d water level variation,water resources are not well utilized,and there is also potential risk of disasters since 2008.In addition,various indices such as 1-d.5-d,and 10-d water level variations are proposed for reservoir regulation.Finally,taking reservoir-induced landslides in June2015 for example,the feasibility of the optimizing indices of water level variations is verified.
引用
收藏
页码:577 / 595
页数:19
相关论文
共 37 条
[21]   大型基岩顺层滑坡滑带形成演化过程与模式 [J].
李守定 ;
李晓 ;
吴疆 ;
刘艳辉 .
岩石力学与工程学报, 2007, (12) :2473-2480
[22]   香溪河流域白家堡滑坡变形失稳机制分析 [J].
黄波林 ;
陈小婷 .
岩土工程学报, 2007, (06) :938-942
[23]   湖北省香溪河流域白家堡滑坡稳定性分析与评价 [J].
陈小婷 ;
黄润秋 .
中国地质灾害与防治学报, 2006, (04) :29-33
[24]   三峡库区边坡结构及失稳模式研究 [J].
殷跃平 .
工程地质学报, 2005, (02) :145-154
[25]   1994-04-30四川省武隆县鸡冠岭滑坡→崩塌→碎屑流→堵江灾害链 [J].
陈自生,张晓刚 .
山地研究, 1994, (04) :225-229
[26]   长江三峡工程重大地质与地震问题研究主要成果综述 [J].
刘广润 ;
楚占昌 ;
郭希哲 ;
柳源 .
中国地质灾害与防治学报, 1992, (01) :9-16
[27]  
Modelling of fast catastrophic landslides and impulse waves induced by them in fjords, lakes and reservoirs[J] . M. Pastor,I. Herreros,J.A. Fernández Merodo,P. Mira,B. Haddad,M. Quecedo,E. González,C. Alvarez-Cedrón,V. Drempetic.Engineering Geology . 2008 (1)
[28]  
Mechanism for the rapid motion of the Qianjiangping landslide during reactivation by the first impoundment of the Three Gorges Dam reservoir, China[J] . Fawu Wang,Yeming Zhang,Zhitao Huo,Xuanming Peng,Shimei Wang,Shintaro Yamasaki.Landslides . 2008 (4)
[29]  
Movement of the Shuping landslide in the first four years after the initial impoundment of the Three Gorges Dam Reservoir, China[J] . Fawu Wang,Yeming Zhang,Zhitao Huo,Xuanming Peng,Kiminori Araiba,Gonghui Wang.Landslides . 2008 (3)
[30]  
The Papua New Guinea tsunami of 17 July 1998: anatomy of a catastrophic event[J] . Tappin D. R.,Watts P.,Grilli S. T..Natural Hazards and Earth System Science . 2008 (75)