Long-term coupled effects of hydrological factors on kinematic responses of a reactivated landslide in the Three Gorges Reservoir

2019 ◽  
Vol 261 ◽  
pp. 105271 ◽  
Author(s):  
Shi-Lin Luo ◽  
Xiao-Guang Jin ◽  
Da Huang
2018 ◽  
Vol 37 (4) ◽  
pp. 1258-1267 ◽  
Author(s):  
Pengcheng Lin ◽  
Xin Gao ◽  
Fei Liu ◽  
Mingzheng Li ◽  
Huanzhang Liu

2012 ◽  
Vol 209-211 ◽  
pp. 786-791
Author(s):  
Jing Li Yang ◽  
Hua Fu ◽  
Yao Chang Ma ◽  
Yun Yun Yang

Jialing River flows into Yangtze River at main city zone of Chongqing Municipality, evolutional mechanism of rivers near the confluence site obviously shows some estuary properties. In September 2008, the Three Gorges Reservoir experimented to fill water at 175m, thus, rivers near the Chongqing Municipality are located in the upper or middle area of fluctuating backwater region and alternatively behave as reservoirs or natural rivers. On the basis of field experimental data of the reservoir impoundment process, the properties of sediment transport of some key harbors were investigated to study the waterway characters. The results show that most of the rivers took place silting. The specific results are that, at the Jiulongpo and the Jinshaqi areas, the sediment deposition grew higher 1-2m and 1-3m, respectively, and at the Zhuerqi zone, there was a few silting. The disadvantages of long-term impoundment process of the Three Gorges Reservoir on water transportation should be further explored in time.


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