Origination of Cellular Secondary Cells in Wide Open-Channel Turbulent Unsteady Flows over Spanwise-Oriented Alternate Rough and Smooth Bed Strips

被引:0
作者
Chattopadhyay T. [1 ]
Kundu S. [1 ]
机构
[1] Department of Mathematics, NIT Jamshedpur, Adityapur, Jharkhand, Jamshedpur
关键词
Longitudinal Bed forms; Open channel turbulent flow; Secondary current (SC); Spectal collocation method; Unsteady flow;
D O I
10.1007/s40996-024-01432-7
中图分类号
学科分类号
摘要
This study presents an analysis of the formation of large-scale turbulent induced cellular secondary flows commonly occurring in straight wide open channel uniform flows with rectangular cross-sections. The study aimed to investigate the plausible scenario of the formation of cellular structures of the secondary currents (SC) occurring in open channels with spanwise-oriented alternate rough and smooth bed strips. Starting with the continuity equation and the Reynolds averaged Navier–Stokes equation, the governing equations for secondary flow velocities are obtained with linear stability analysis of the convective terms. Unlike previous studies, the governing equation results as the balancing between two opposite effects, the generation of SC (consists of normal stresses) and suppression of SC due to viscous force and the Reynolds shear force. Using the spectral collocation method the semi-analytical solutions are derived assuming a sinuous instability along transverse direction due to spanwise-oriented alternate rough and smooth bed strips. The obtained solutions are validated with experimental observations for the stationary state and a good agreement was obtained. Time analysis results show that though the formation of cellular cells originates due to lateral variation in bed conditions, the centers of circulations are generated near the free surface which gradually shifts with time towards the middle of the flow depth. Apart from these, the effects of SC on the settling velocity vector are analyzed. Results demonstrate how the streamlines of the settling velocity vector are distorted due to the formation and generation of cellular secondary flow cells. This study also provides a clear idea of how the retention zones are formed with the existence of secondary flow circulations. © The Author(s), under exclusive licence to Shiraz University 2024.
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页码:3643 / 3660
页数:17
相关论文
共 45 条
[1]  
Amarloo A., Forooghi P., Abkar M., Secondary flows in statistically unstable turbulent boundary layers with spanwise heterogeneous roughness, Theor Appl Mech Lett, 12, pp. 1-7, (2022)
[2]  
Brundrett E., Baines W.D., The production and diffusion of vorticity in duct flow, J Fluid Mech, 19, pp. 375-394, (1964)
[3]  
Camporeale C., Cannamela F., Canuto C., Et al., Stability analysis of open-channel flows with secondary currents, J Fluid Mech, 927, (2021)
[4]  
Castro I.P., Rough-wall boundary layers: mean flow universality, J Fluid Mech, 585, pp. 469-485, (2007)
[5]  
Chattopadhyay T., Kundu S., Modified second log.wake law for mean velocity distributions along vertical and transverse directions in smooth open.channel turbulent flows with application to natural rivers, Iran J Sci Technol Trans Civil Eng, (2023)
[6]  
Coleman J., Brahmaputra river
[7]  
channel process and sedimentation, Sed Geol, 3, pp. 129-239, (1969)
[8]  
Colombini M., Turbulence driven secondary flows and the formation of sand ridges, J Fluid Mech, 254, pp. 701-719, (1993)
[9]  
Demuren A.O., Rodi W., Calculation of turbulence-driven secondary motion in non-circular ducts, J Fluid Mech, 140, pp. 189-222, (1984)
[10]  
Flack K.A., Schutz M.P., Roughness effects on wall-bounded turbulent flows, Phys Fluids, 26, 10, (2014)