Study on the sediment discharge regulation of the Xiaolangdi reservoir during flood season

Author(s):  
W. Ting ◽  
W. Yuanjian ◽  
Q. Shaojun ◽  
L. Xiaoping ◽  
D. Shentang
2012 ◽  
Vol 204-208 ◽  
pp. 2318-2323
Author(s):  
Ting Wang ◽  
Jun Hua Zhang ◽  
Shu Kui Chen ◽  
Huai Bao Ma ◽  
Kun Peng Li

Zhenshui is the biggest tributary of Xiaolangdi Reservoir and its original storage capacity is 1.767 billion m3. By October 2010, the amount of sediment in Zhenshui reached 0.1691 billion m3, and the sand bar at Zhenshui estuary was 7m in height. Influenced by operational mode of reservoir and terrain, the formation of sand bar has certain inevitabilities. The sand bar can prevent water and sediment exchange between mainstream and tributary, and the internal storage capacity of tributary is not effectively used. The experimental result shows that during the later sediment retaining period, some small reservoirs can be built at the end of Zhenshui. By restoring water during the high water level in non-flood season in these small reservoirs and discharging flow during the low water level in flood season to scour sand bar, the tributary and main channel in Xiaolangdi Reservoir can be linked up in long term, service efficiency and life of tributary storage can be increased.


2014 ◽  
Vol 501-504 ◽  
pp. 1907-1911
Author(s):  
Jun Jie Chen

Suction jet scheme has brought forward sediment suspension transport work parameter in the scheme of water and sediment transporting and sediment adding in discharge water before the flood season of Xiaolangdi Reservoir. Suction jet system starts suspended sediments as per 1 natural bottom slope of Xiaolangdi Reservoir while jet pump eject muddy water, which forms into density current and transport forward, and makes longitudinal deposition in the process of sediment transport. Transport distance shall be 1,264~1,903m while 50% longitudinal attenuation of sediments as effective transport distance. Bottom slope of sediment deposition is reduced to 6.7 with obscure longitudinal attenuation of sediments and can transport to longer distance.


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