高亚军,李国斌,陆永军. 刘家峡水库变动回水区河床质泥沙粒径分布[J]. 水利水运工程学报, 2006, (1): 14-18.
引用本文: 高亚军,李国斌,陆永军. 刘家峡水库变动回水区河床质泥沙粒径分布[J]. 水利水运工程学报, 2006, (1): 14-18.
shu
GAO Ya-jun,LI Guo-bin,LU Yong-jun. Distribution of sediment diameter of bed load at the fluctuating backwater reach of Liujiaxia Reservoir[J]. Hydro-Science and Engineering, 2006, (1): 14-18.
Citation: GAO Ya-jun,LI Guo-bin,LU Yong-jun. Distribution of sediment diameter of bed load at the fluctuating backwater reach of Liujiaxia Reservoir[J]. Hydro-Science and Engineering, 2006, (1): 14-18.
shu

刘家峡水库变动回水区河床质泥沙粒径分布

Distribution of sediment diameter of bed load at the fluctuating backwater reach of Liujiaxia Reservoir

    摘要
  • 摘要: 根据刘家峡水库变动回水区的河段地形特征和历年河床质泥沙粒径级配资料,分析了变动回水区河段淤积和冲刷时,河床质泥沙中值粒径的沿程变化和历年河床质泥沙中值粒径变化过程,并指出粒径分布由粗变细的转折点在变动回水区寺沟峡峡口处.

     

    Abstract: Based on the topographic features and data of sediment particle size of bed load at the fluctuating backwater reach of Liujiaxia Reservoir,the streamwise variation and variation process of median diameter of bed load during silting and scouring periods of the fluctuating backwater reach are analyzed,and it can be seen that the turning point for the sediment diameter variation from coarse to fine is located at the outlet of Shigou Gorge of the fluctuating backwater reach.

     

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