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Influence of bank vegetation and gravel bed on velocity and Reynolds stress distributions

查看全文 作  者:Hossein [1]AFZALIMEHR;Subhasish [2]DEY 高影响力作者 机构地区:[1]Department of Water Engineering,Isfahan University of Technology;[2]Department of Civil Engineering,Indian Institute of Technology高影响力机构 出  处:《International Journal of Sediment Research》索引2009年第24卷第2期,共11页高影响力期刊 摘  要:This paper presents the results of a laboratory flume experimental study on the interaction of bank vegetation and gravel bed on the flow velocity(primarily on the location of the maximum velocity,Umax) and the Reynolds stress distributions. The results reveal that the dip of the maximum velocity below the water surface is up to 35% of flow depth and the difference between Umax and the velocity at the water surface is considerable in the presence of vegetation on the walls. The zone of the log-law varies from y/h=2 up to 15 percent of flow depth and it does not depend on distance from the wall. Deviation of the velocity profile in the outer layer over a gravel bed with vegetation cover on the walls is much larger than the case of flow over a gravel bed without vegetation cover on the walls. The presence of vegetation on the walls changes uniform flow to non-uniform flow. This fact can be explained by considering the nonlinear Reynolds stress distribution and location of maximum velocity in each profile at different distances across the flume. The Reynolds stress distributions at the distance 0.02 m from the wall have negative values and away from the wall,they change the sign taking positive values with specific convex form with apex in higher location. Average of von Karman constant κ for this study is equal to 0.16. Based on κ=0.16,the methods of Clauser and the Reynolds stress are compatible for determination of shear velocity. 关 键 词:植被覆盖 应力分布 血流速度 砾石 银行 最大速度 水槽实验 非均匀流
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