中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hydraulic geometry change of a large river: a case study of the upper Yellow River

文献类型:SCI/SSCI论文

作者Ran L. S. ; Wang S. J. ; Lu X. X.
发表日期2012
关键词Hydraulic geometry Channel pattern Bedrock channel Alluvial channel Upper Yellow River channel geometry bedrock channels mountain streams sediment load new-zealand reach china variability yangtze
英文摘要Study on hydraulic geometry can reveal the response of river systems to basin attributes, and the trends in channel change. Based on 35 years of data collected at 10 hydrological stations (cross-sections), the hydraulic geometry relations between cross-sectional variables and discharge were established, and the derived parameters were analyzed. The channel behavior of the mountainous bedrock reach (from riverhead to Xunhua cross-section) and the alluvial reach (from Xunhua to Toudaoguai cross-sections) differed significantly over the past decades in response to dramatic water and sediment changes. The hydraulic geometry quasi-equilibrium was achieved through equally adjusting water depth and flow velocity in the mountainous bedrock reach; while primarily through flow velocity in the alluvial reach. The change rate of river width with varying discharge was relatively small in the whole upper Yellow River. Compared with the lower Yellow River and other rivers in the world, both similarity and differences existed, indicating the general adjustment direction of hydraulic quasi-equilibrium and also the importance of considering other influencing factors in hydraulic geometry studies. In addition, dams played an important role in affecting the changes of hydraulic geometry exponents.
出处Environmental Earth Sciences
66
4
1247-1257
收录类别SCI
语种英语
ISSN号1866-6280
源URL[http://ir.igsnrr.ac.cn/handle/311030/26811]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Ran L. S.,Wang S. J.,Lu X. X.. Hydraulic geometry change of a large river: a case study of the upper Yellow River. 2012.

入库方式: OAI收割

来源:地理科学与资源研究所

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