Enhanced bed load sediment transport by unsteady flows in a degrading channel

被引:0
|
作者
Zhijing Li [1 ,2 ]
Honglu Qian [1 ]
Zhixian Cao [1 ]
Huaihan Liu [3 ]
Gareth Pender [4 ]
Penghui Hu [1 ]
机构
[1] State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University
[2] Changjiang River Scientific Research Institute
[3] Yangtze River Waterway Bureau
[4] School of Energy, Geoscience, Infrastructure and Society, Heriot-Watt University
基金
中国国家自然科学基金;
关键词
Bed load; Gravel; Sand; Unsteady flow; Enhancement effect;
D O I
暂无
中图分类号
TV147 [河道演变];
学科分类号
081502 ;
摘要
Laboratory flume experiments were done to investigate bed load sediment transport by both steady and unsteady flows in a degrading channel. The bed, respectively composed of uniform sand, uniform gravel,or sand-gravel mixtures, always undergoes bulk degradation. It is found that both uniform and nonuniform bed load transport is enhanced greatly by unsteady flows as compared to their volumeequivalent steady flows. This enhancement effect is evaluated by means of an enhancement factor, which is shown to be larger with a coarser bed and lower discharges. Also, the fractional transport rates of gravel and sand in non-uniform sand-gravel mixtures are compared with their uniform counterparts under both steady and unsteady flows. The sand is found to be able to greatly promote the transport of gravel, whilst the gravel considerably hinders the transport of sand. Particularly, the promoting and hindering impacts are more pronounced at lower discharges and tend to be weakened by flow unsteadiness.
引用
收藏
页码:327 / 339
页数:13
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