Sedimentation of overbank floods in the confined complex channel-floodplain system of the Lower Yellow River, China
文献类型:期刊论文
作者 | Zhang, Min2,3,4; Huang, He Qing2,3; Carling, Paul A.1; Zhang, Mingwu4 |
刊名 | HYDROLOGICAL PROCESSES
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出版日期 | 2017-09-30 |
卷号 | 31期号:20页码:3472-3488 |
关键词 | channel-floodplain interaction erosion Lower Yellow River overbank floods sedimentation |
ISSN号 | 0885-6087 |
DOI | 10.1002/hyp.11260 |
通讯作者 | Huang, He Qing(huanghq@igsnrr.ac.cn) |
英文摘要 | The channel boundary conditions along the Lower Yellow River (LYR) have been altered significantly since the 1950s with the continual reinforcement and construction of both main and secondary dykes and river training works. To evaluate how the confined complex channel-floodplain system of the LYR responds to floods, this study presents a detailed investigation of the relationship between the tempo-spatial distribution of sedimentation/erosion and overbank floods occurred in the LYR. For large overbank floods, we found that when the sediment transport coefficient (ratio of sediment concentration of flow to flow discharge) is less than 0.034, the bankfull channel is subject to significant erosion, whereas the main and secondary floodplains both accumulate sediment. The amount of sediment deposited on the main and secondary floodplains is closely related to the ratio of peak discharge to bankfull discharge, volume of water flowing over the floodplains, and sediment concentration of overbank flow, whereas the degree of erosion in the bankfull channel is related to the amount of sediment deposited on the main and secondary floodplains, water volume, and sediment load in flood season. The significant increase in erosion in the bankfull channel is due to the construction of the main and secondary dykes and river training works, which are largely in a wide and narrow alternated pattern along the LYR such that the water flowing over wider floodplains returns to the channel downstream after it drops sediment. For small overbank floods, the bankfull channel is subject to erosion when the sediment transport coefficient is less than 0.028, whereas the amount of sediment deposited on the secondary floodplain is associated closely with the sediment concentration of flow. Over the entire length of the LYR, the situation of erosion in the bankfull channel and sediment deposition on the main and secondary floodplains occurred mainly in the upper reach of the LYR, in which a channel wandering in planform has been well developed. |
WOS关键词 | UPPER MISSISSIPPI RIVER ; AMAZON RIVER ; EXTREME FLOOD ; HUANGHE RIVER ; RATES ; DEPOSITION ; PLAIN ; PATTERNS ; BASIN ; STORAGE |
资助项目 | National Natural Science Foundation of China[41330751] ; National Natural Science Foundation of China[51509101] ; National Key R&D Program of China[2016YFC0402502] ; Central Government for Non-profit Research Institutes[HKY-JBYW-2017-05] |
WOS研究方向 | Water Resources |
语种 | 英语 |
WOS记录号 | WOS:000410745000002 |
出版者 | WILEY |
资助机构 | National Natural Science Foundation of China ; National Key R&D Program of China ; Central Government for Non-profit Research Institutes |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/61902] ![]() |
专题 | 中国科学院地理科学与资源研究所 |
通讯作者 | Huang, He Qing |
作者单位 | 1.Univ Southampton, Geog & Environm, Univ Rd, Southampton SO17 1BJ, Hants, England 2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China 3.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China 4.Yellow River Water Conservancy Commiss, Inst Hydraul Res, Minist Water Resources, Key Lab Yellow River Sediment, Zhengzhou 450003, Henan, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang, Min,Huang, He Qing,Carling, Paul A.,et al. Sedimentation of overbank floods in the confined complex channel-floodplain system of the Lower Yellow River, China[J]. HYDROLOGICAL PROCESSES,2017,31(20):3472-3488. |
APA | Zhang, Min,Huang, He Qing,Carling, Paul A.,&Zhang, Mingwu.(2017).Sedimentation of overbank floods in the confined complex channel-floodplain system of the Lower Yellow River, China.HYDROLOGICAL PROCESSES,31(20),3472-3488. |
MLA | Zhang, Min,et al."Sedimentation of overbank floods in the confined complex channel-floodplain system of the Lower Yellow River, China".HYDROLOGICAL PROCESSES 31.20(2017):3472-3488. |
入库方式: OAI收割
来源:地理科学与资源研究所
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