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黄河郑州段河道冲淤变化及影响因素研究
引用本文:郭恒亮,赫晓慧,石姗.黄河郑州段河道冲淤变化及影响因素研究[J].人民黄河,2012(3):4-5.
作者姓名:郭恒亮  赫晓慧  石姗
作者单位:郑州大学水利与环境学院
基金项目:河南省教育厅自然科学研究计划项目(2010B170012)
摘    要:以黄河下游郑州段多时段的遥感影像及水文资料为主要数据源,对黄河郑州段河道的淤积与演变及其与水沙的关系进行了研究。结果表明:黄河郑州段河道岸线、河道宽度、曲流位置和角度都有变化,且年际变化大;小浪底水库的投入运用,控制了下游的来水来沙条件,造成河道的摆动幅度减小,但弯曲长度增加,横河、斜河呈发展趋势;河道冲淤变化的主要影响因素为流量变化。

关 键 词:遥感  来水来沙  河道冲淤  郑州河段  黄河

Siltation and Erosion in Zhengzhou Section of the Yellow River Channel and Its Influencing Factors
GUO Heng-liang,HE Xiao-hui,SHI Shan.Siltation and Erosion in Zhengzhou Section of the Yellow River Channel and Its Influencing Factors[J].Yellow River,2012(3):4-5.
Authors:GUO Heng-liang  HE Xiao-hui  SHI Shan
Affiliation:(School of Water Conservancy and Environment,Zhengzhou University,Zhengzhou 450001,China)
Abstract:Taking the multi remote sensing images dated and hydrological data as the main data sources,the changes in siltation and erosion of the Yellow River in Zhengzhou section were studied.The results show that the river shoreline,channel width,meandering position and angle have changed,and inter-annual change is big.With the application of Xiaolangdi Reservoir,the coming water and sediment conditions of the downstream have been controlled.The swing range of the river channel becomes smaller,but the bending length becomes longer.The transverse current and oblique flows are developing.The main factor of channel siltation and erosion is the flow change.
Keywords:RS  incoming flow and sediment  siltation and erosion of river channel  Zhengzhou section  Yellow River
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