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SHEAR STRESS FOR INITIATION OF MOTION OF NON-UNIFORM SEDIMENT MIXTURES

查看全文 作  者:Liton Kumar [1]SARKER;M. Monowar [2]HOSSAIN;M. Anisul [3]HAQUE 高影响力作者 机构地区:[1]Assis. Engg., Bangladesh Water Development Board (BWDB), Lakshmipur, Bangladesh;[2]Prof., Department of Water Resources Engineering, Bangladesh University of Engineering and Technology (BUET), Dhaka-1000, Bangladesh;[3]Prof., Institute of Water and Flood Management (IWFM), Bangladesh University of Engineering and Technology (BUET), Dhaka-1000, Bangladesh高影响力机构 出  处:《International Journal of Sediment Research》索引2007年第22卷第3期,共11页高影响力期刊 摘  要:Experiments on initiation of motion of different fractions of non-uniform sediment mixtures are reported. Four sediment mixes and reference transport method to define the threshold of bed particle movement are used in this analysis. Factors controlling the initiation of motion are analyzed. It is found that relative size of different grains with respect to a median size greatly affects the initiation of movement. The incipient motion of non-uniform sediment is very much dependent on the absolute size for coarser fractions. Considering the factors controlling the initiation of motion the experimental data sets along with the other available data yield a new relationship for the calculation of critical shear stress of non-uniform sediments. A set of equations have found that all the data points fall into a single line for the finer and for coarser fractions. 关 键 词:临界 剪切力 沉淀物 淤泥
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