Laboratory study of bed shear stress in gradually varied flow over a sudden change in bed roughness

被引:0
作者
Jamil, Muhammad Farrukh [1 ]
Ting, Francis C. K. [1 ]
Kafle, Monika [1 ]
机构
[1] South Dakota State Univ, Dept Civil & Environm Engn, Brookings, SD 57007 USA
基金
美国国家科学基金会;
关键词
Open-channel flow; Roughness transition; Logarithmic law; Bed shear stress; Equivalent roughness; Particle image velocimetry; TURBULENT-BOUNDARY-LAYER; OPEN-CHANNEL FLOW; STEP CHANGE; SURFACE-ROUGHNESS; SMOOTH;
D O I
10.1007/s10652-025-10024-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The evolution of bed shear stress in open-channel flow due to a sudden change in bed roughness was investigated experimentally for rough-to-smooth (RTS) and smooth-to-rough (STR) transitions. The velocity field was measured in the longitudinal-vertical plane from upstream to downstream using a Particle Image Velocimetry system. The bed shear stress was determined from the measured velocity profile and water depth using various methods. It was found that the variation of bed shear stress in gradually varied flow through a roughness transition was influenced by both flow depth and bottom roughness. In both RTS and STR transitions, the bed shear stress adjusted to the new bed condition almost immediately even though the velocity profile away from the bed was still evolving, but unlike external and close-conduit flows the bed shear stress in open-channel flows continued to evolve until the flow depth was uniform. It is shown that the evolution of bed shear stress in a STR transition is dependent on the choice of the displacement height on the rough bed, which affects the mixing length used to derive the logarithmic velocity profile and equivalent roughness. Bed shear stress variation consistent with published data was obtained when the ks/d90\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${k}_{s}/{d}_{90}$$\end{document} ratio was determined as a function of the h/d90\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$h/{d}_{90}$$\end{document} ratio, where ks\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${k}_{s}$$\end{document} is the equivalent roughness height, h\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$h$$\end{document} is the flow depth, and d90\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${d}_{90}$$\end{document} is the grain diameter with 90% of finer particles.
引用
收藏
页数:37
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