Characteristics and influencing factors of sediment deposition-scour in the Sanhuhekou-Toudaoguai Reach of the upper Yellow River, China | |
Yao B(姚波); Liu QQ(刘青泉)![]() | |
Source Publication | INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH
![]() |
2018-09-01 | |
Volume | 33Issue:3Pages:303-312 |
ISSN | 1001-6279 |
Abstract | The annual changes of sediment deposition-scour on the riverbed in the Sanhuhekou-Toudaoguai Reach of the upper Yellow River during the years 1952-2010 were investigated based on runoff and sediment transport observations from the Sanhuhekou and Toudaoguai hydrological stations. Multiple influencing factors such as reservoir operations, tributary inflows, as well as runoff and sediment loads from the Shidakongdui area were analyzed. The results show that even though the sediment loads from the major sources, the Shidakongdui area as well as the upstream tributaries such as the Qingshui River and the Zuli River have reduced especially since the 2000s as a result of enhanced water-soil conservation measures and improvement of vegetation cover, the study reach was still generally in a status of cumulative aggradation. This is mainly due to the joint operations of the Liujiaxia Reservoir and the Longyangxia Reservoir, which significantly reduced the annual runoff and sediment loads at the Sanhuhekou Crosssection. The reservoirs also remarkably altered the summer flood characteristics of the study reach, inducing the shape of the annual flow curve changing from a 'single-peak' into a 'double-peak'. These alternations sharply decreased the sediment transport capacity of flooding in the summer flood season which yields more than 90% of the sediment loads, leading to an unbalanced relation between the water and sediment. In addition, the estimated incoming sediment coefficient of the Sanhuhekou Crosssection ranged from 0.003 to 0.014 kg s/m(6), of which 0.004 kg s/m(6) was suggested as a rough critical value to determine the scour or deposition status of the study reach. (C) 2018 International Research and Training Centre on Erosion and Sedimentation/the World Association for Sedimentation and Erosion Research. Published by Elsevier B.V. All rights reserved. |
Keyword | Upper Yellow River Sanhuhekou-Toudaoguai Reach Sediment deposition Incoming sediment coefficient Runoff Sediment loads |
DOI | 10.1016/j.ijsrc.2018.03.003 |
URL | 查看原文 |
Indexed By | SCI ; EI |
Language | 英语 |
WOS ID | WOS:000443198500009 |
WOS Keyword | SUSPENDED SEDIMENT ; LOESS PLATEAU ; EROSION ; IMPACTS ; RUNOFF ; TREND ; LOAD ; CONSERVATION ; DOWNSTREAM ; RESERVOIRS |
WOS Research Area | Environmental Sciences ; Water Resources |
WOS Subject | Environmental Sciences & Ecology ; Water Resources |
Funding Organization | National Natural Science Foundation of China [11432015, 11202217] |
Classification | Q3 |
Ranking | 1 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://dspace.imech.ac.cn/handle/311007/77948 |
Collection | 流固耦合系统力学重点实验室 |
Affiliation | 1.Chinese Acad Sci, Inst Mech, Key Lab Mech Fluid Solid Coupling Syst, Beijing 100190, Peoples R China 2.Beijing Inst Technol, Sch Aerosp Engn, Dept Mech, Beijing 100081, Peoples R China |
Recommended Citation GB/T 7714 | Yao B,Liu QQ. Characteristics and influencing factors of sediment deposition-scour in the Sanhuhekou-Toudaoguai Reach of the upper Yellow River, China[J]. INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH,2018,33,3,:303-312. |
APA | 姚波,&刘青泉.(2018).Characteristics and influencing factors of sediment deposition-scour in the Sanhuhekou-Toudaoguai Reach of the upper Yellow River, China.INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH,33(3),303-312. |
MLA | 姚波,et al."Characteristics and influencing factors of sediment deposition-scour in the Sanhuhekou-Toudaoguai Reach of the upper Yellow River, China".INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH 33.3(2018):303-312. |
Files in This Item: | Download All | |||||
File Name/Size | DocType | Version | Access | License | ||
IrJ2018337.pdf(1870KB) | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | View Download |
Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.
Edit Comment