Research on Characteristics of Sediment in Yichang-Wuhan Reach after Impoundment of the Three Gorges

Article Preview

Abstract:

Reservoir regulation make conditions of sediment under the dam change greatly after impoundment of the Three Gorges Project. This paper analyzes change trend and abrupt change situation of incoming sediment and studies characteristics of new sediment of Yichang and Hankou Stations after impoundment of the Three Gorges with Mann-Kendall nonparametric rank test method. The result indicates that after operation of the Three Gorges Reservoir, annual sediment runoff changed suddenly and sediment runoff reduced sharply in Yichang and Hankou Stations; sediment entering the Yichang-Wuhan reach decreases substantially and it almost can be regarded as clean water discharge. Research shows unsaturated degree of the clear water released from reservoirs decreased after obtaining sediment along the river, so the sediment discharge would be partly recovered.

You might also be interested in these eBooks

Info:

Periodical:

Pages:

2250-2253

Citation:

Online since:

September 2013

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2013 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

[1] Jiang L, Yi Y T, Sun Z H, Channel evolution of Jingjiang reach and its influences on waterway after impoundment of the Three Gorges project, Journal of Basic Science and Engneeing. 18(2010) 1-10.

Google Scholar

[2] Zhang C Y, Chen L, Zhang J Y, et al, Lateral erosion in downstream of the reservoir, Advances in Water Science, 16(2005) 356-360.

Google Scholar

[3] Li G Z, Huang L W, Guo Z X, Study on the riverbed adjustment principle caused by clear water scouring at the downstream of reservoir, Journal of Schuan University, 42(2010) 36-42.

Google Scholar

[4] Xu J X, Response of channel sediment budget to flow and sediment inputs: an example of the Yichang—Wuhan Reach, Yangtze River, Acta Geographica Sinica, 60(2005) 337-348.

DOI: 10.1201/9781439833865.ch241

Google Scholar

[5] Ying M, Li J F, Wan X N, etal, Study on time series of sediment discharge at Datong Station in the Yangtze River, Resources and Environment in the Yangtze Basin, 14(2005) 83-87.

Google Scholar

[6] Qin N X, Jiang T, Xu C Y, Trends and abruption analysis on the discharge in the Yangtze basin, Resources and Environment in the Yangtze Basin, 14(2005) 589-594.

Google Scholar