Approximate velocity formula over mobile sediment bed induced by velocity-skewed waves and current

被引:1
|
作者
Chen, Xin [1 ]
Chen, Minghong [1 ]
Wu, Jingkai [2 ,3 ]
Liu, Haifei [4 ]
Yang, Chen [5 ]
机构
[1] China Agr Univ, Beijing Engn Res Ctr Safety & Energy Saving Techn, Beijing 100083, Peoples R China
[2] Tsinghua Univ, Dept Hydraul Engn, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[3] China Huadian Corp, Beijing 100031, Peoples R China
[4] Beijing Normal Univ, Sch Environm, Beijing 100875, Peoples R China
[5] North China Univ Water Resources & Elect Power, Sch Water Conservancy, Zhengzhou 450045, Peoples R China
基金
中国国家自然科学基金;
关键词
Analytical approximate velocity; Mobile sediment bed; Sediment transport; Velocity asymmetry; Wave and current; OSCILLATORY SHEET-FLOW; BOUNDARY-LAYER; SAND TRANSPORT; MODEL;
D O I
10.1016/j.ijsrc.2021.11.001
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A velocity formula is proposed for flow over a mobile sediment bed induced by velocity-skewed waves and current. The formula is obtained by a separation of waves and current velocities and requires seven free variables related to free stream velocity and sediment characteristics. The formula includes two parts: (1) a wave part consisting of the free stream velocity and defect function, which considers phase lead, wave boundary layer thickness, and mobile bed level, and (2) a current part, which changes the wave part through the boundary layer thickness and mobile bed level, influenced by wave eddy viscosity. The wave part is superior to the current part such that the boundary layer characteristics are mainly determined by the waves. The wave process is divided into four quarter stages to model the asymmetries of parameters in velocity and acceleration. Under velocity-skewed waves and current conditions, velocity asymmetry and residual velocity are accounted for in the formula, especially the offshore residual velocity with a large phase lag and mobile bed effect with a small phase lag. Phase lead is shown to be nonconstant in velocity-skewed oscillatory sheet flow and corresponds to an extra offshore residual velocity. (c) 2021 International Research and Training Centre on Erosion and Sedimentation/the World Association for Sedimentation and Erosion Research. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:317 / 327
页数:11
相关论文
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    Minghong Chen
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