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Bank full discharge is generally considered to be the dominant steady flow which would generate the same regime channel shape and dimensions as the natural sequences of flows would.This is because investigation on the magnitude and frequency of sediment transport have determined that for stable rivers the flow which in the longer term transports most material has the same frequency of occurrence as bankfull flow.For stable gravel-bed rivers,this is considered to be the 1.5-year flood.
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篇名 Sensitivity Analysis Of Geographical River Boundary Layers
来源期刊 地理研究(英文) 学科 工学
关键词 RIVER BOUNDARY LAYERS Sensitivity analysis REGIME
年,卷(期) 2019,(2) 所属期刊栏目
研究方向 页码范围 25-34
页数 10页 分类号 TV1
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地理研究(英文)
季刊
2630-5070
12 Eu Tong Sen Stree
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57
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