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淮河干流吴家渡至小柳巷河段泥沙冲淤分析
引用本文:虞邦义,郁玉锁,倪晋.淮河干流吴家渡至小柳巷河段泥沙冲淤分析[J].泥沙研究,2009(4).
作者姓名:虞邦义  郁玉锁  倪晋
作者单位:1. 安徽省·水利部淮委水利科学研究院,安徽省水利水资源重点实验室,安徽,蚌埠,233000
2. 河海大学,江苏,南京,210098
基金项目:水利部现代水利科技创新项目“淮河干流河相关系和整治方向研究”(XDS2007-1);;安徽省人才开发基金资助(2008Z046)
摘    要:采用输沙量法对淮河干流吴家渡至小柳巷段实测水文资料完整的20年进行年际变化分析,河段总体表现为冲刷。枯水年份河段输沙基本平衡或微淤;中水年份冲刷年多于淤积年;丰水年份总体表现为冲刷。丰水年和中水年的总体冲淤趋势取决于汛期,枯水年非汛期对全年冲淤影响较大。系统分析了河段冲淤与吴家渡站来流量以及年均来沙系数的关系。

关 键 词:输沙量法  造床流量  排沙比  来沙系数  

Analysis on erosion and deposition in Wujiadu-Xiaoliuxiang reach of the main stem Huaihe River
YU Bang-yi,YU Yu-suo,NI Jin.Analysis on erosion and deposition in Wujiadu-Xiaoliuxiang reach of the main stem Huaihe River[J].Journal of Sediment Research,2009(4).
Authors:YU Bang-yi  YU Yu-suo  NI Jin
Affiliation:2;1.Huaihe River Water Resources Research Institute;Bengbu Anhui 233000;2.Hohai University;Nanjing Jiangsu 210098
Abstract:Based on 20-year observed data,the interannual variation of deposition/erosion in Wujiadu-Xiaoliuxiang reach of Huaihe River is analyzed using sediment balance method.It is shown that this channel is generally under erosion state.In low flow years,the channel shows equilibrium or slight deposition.The erosion amout is more than deposition during medium flow years,and the channel exhibits erosion almost in all high flow years.The deposition or erosion in the reach during high flow years and normal years is m...
Keywords:sediment balance method  bed-forming discharge  sediment discharge ratio  incoming sediment coefficient  
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