中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
River Channel Forms in Relation to Bank Steepness: A Theoretical Investigation Using a Variational Analytical Method

文献类型:期刊论文

作者Fan, Jinsheng1,2; Huang, Heqing1,2; Yu, Guoan1; Su, Teng1
刊名WATER
出版日期2020-05-01
卷号12期号:5页码:18
关键词alluvial rivers riverbank anti-scourability variational method equilibrium river channel forms
DOI10.3390/w12051250
通讯作者Huang, Heqing(huanghq@igsnrr.ac.cn)
英文摘要Riverbanks vary considerably in anti-scourability and consequently take various profiles. By using an isosceles trapezoid as the generalized form of river channel cross-sections and then incorporating the effects of bank angle into the variational analytical approach developed by Huang and Nanson (2000), this study presents a detailed theoretical investigation of the self-adjustment of alluvial channel forms. It is demonstrated that when alluvial channel flow achieves stable equilibrium, a significant decrease in riverbank steepness leads to a slight decrease in maximum sediment (bedload) discharge, and yet results in a significant increase in optimal channel width and a considerable decrease in optimal channel depth. The hydraulic geometry relations, theoretically derived for bank steepness to vary across a wide range, show that among the multivariant controls, the roles of bed sediment size, channel roughness, flow discharge and sediment (bedload) discharge are independent of bank steepness. While the effects of bank steepness illustrated in the theoretically derived hydraulic geometry relations are highly consistent with the results of threshold theory and previous empirical studies, limitations on using bank angle to reflect the anti-scourability of natural riverbanks are also highlighted.
WOS关键词UNIT STREAM POWER ; GRAVEL-BED RIVERS ; MAXIMUM FLOW EFFICIENCY ; HYDRAULIC GEOMETRY ; EXTREMAL HYPOTHESES ; EQUILIBRIUM BANKS ; STRAIGHT RIVERS ; STABLE WIDTH ; MINIMUM RATE ; MOBILE BED
资助项目National Key Research and Development Program of China[2016YFC0402502] ; National Natural Science Foundation of China[41561144012] ; National Natural Science Foundation of China[41661144030] ; National Natural Science Foundation of China[41971010]
WOS研究方向Water Resources
语种英语
WOS记录号WOS:000555915200029
出版者MDPI
资助机构National Key Research and Development Program of China ; National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/158146]  
专题中国科学院地理科学与资源研究所
通讯作者Huang, Heqing
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
2.Univ Chinese Acad Sci, Coll Resources & Enviroment, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Fan, Jinsheng,Huang, Heqing,Yu, Guoan,et al. River Channel Forms in Relation to Bank Steepness: A Theoretical Investigation Using a Variational Analytical Method[J]. WATER,2020,12(5):18.
APA Fan, Jinsheng,Huang, Heqing,Yu, Guoan,&Su, Teng.(2020).River Channel Forms in Relation to Bank Steepness: A Theoretical Investigation Using a Variational Analytical Method.WATER,12(5),18.
MLA Fan, Jinsheng,et al."River Channel Forms in Relation to Bank Steepness: A Theoretical Investigation Using a Variational Analytical Method".WATER 12.5(2020):18.

入库方式: OAI收割

来源:地理科学与资源研究所

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