Incipient motion and bed load transport of non-uniform sediment

被引:0
|
作者
Huang Tingjie [1 ,2 ]
Lu Yongjun [1 ]
Lu Yan [1 ]
机构
[1] Nanjing Hydraul Res Inst, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210029, Jiangsu, Peoples R China
[2] Coll Water Conservancy & Hydropower Engn, Nanjing 210098, Jiangsu, Peoples R China
关键词
shear stress; incipient motion; bed-load transport rate; non-uniform sediment; EAST FORK RIVER; BEDLOAD MEASUREMENTS; MIXTURES; MODEL;
D O I
暂无
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
This study explores characteristics of incipient motion and transport of non-uniform sediments analytically and experimentally. A review of published studies on non-uniform sediment transport is first submitted for better understand the state-of-the-art in this area of research. A new formula to calculate the critical shear stress and another to predict frictional bed load transport rate of non-uniform bed materials has been proposed with the aid of experiments. A modification of Wu et al.'s formula to calculate the critical shear stress of incipient motion of non-uniform was proposed. After that, a new formula to calculate the critical shear stress of individual fractions of non-uniform sediment was established, considering factors of grain size and gradation of bed materials and the different threshold of incipient motion for uniform sediment with various diameters. A new fractional non-uniform sediment bed load transport formula based on energy balance theory was proposed. A wide range of laboratory and field data agree well with this theoretical equation. Good agreement is achieved with the newly proposed formula for uniform sediment.
引用
收藏
页码:1931 / 1944
页数:14
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