Contributions of different scales of turbulent motions to the mean wall-shear stress in open channel flows at low-to-moderate Reynolds numbers

被引:27
|
作者
Duan, Yanchong [1 ]
Zhong, Qiang [2 ,3 ]
Wang, Guiquan [4 ,5 ,6 ]
Zhang, Peng [7 ]
Li, Danxun [1 ]
机构
[1] Tsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[2] China Agr Univ, Coll Water Resources & Civil Engn, Beijing 100083, Peoples R China
[3] China Agr Univ, Beijing Engn Res Ctr Safety & Energy Saving Techn, Beijing 100083, Peoples R China
[4] Univ Twente, Phys Fluids Grp, POB 217, NL-7500 AE Enschede, Netherlands
[5] Univ Twente, Twente Max Planck Ctr, Dept Sci & Technol, Mesa Inst, POB 217, NL-7500 AE Enschede, Netherlands
[6] Univ Twente, JM Burgers Ctr Fluid Dynam, POB 217, NL-7500 AE Enschede, Netherlands
[7] Chongqing Jiaotong Univ, Natl Engn Res Ctr Inland Waterway Regulat, Chongqing 400074, Peoples R China
基金
中国国家自然科学基金;
关键词
turbulent boundary layers; channel flow; DIRECT NUMERICAL-SIMULATION; SKIN-FRICTION; BOUNDARY-LAYERS; ATTACHED EDDIES; DRAG; DECOMPOSITION; ROUGH; PIPE;
D O I
10.1017/jfm.2021.236
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Smooth-walled open channel flow datasets, covering both the direct numerical simulation and experimental measurements with a friction Reynolds number Re-tau at a low-to-moderate level of 550 similar to 2400, are adopted to investigate the contributions of different scale motions to the mean wall-shear stress in open channel flows (OCFs). The FIK identity decomposition method by Fukagata et al. (Phys. Fluids, vol. 14, 2002, L73) combined with a scale decomposition is chosen for this research. To see whether/how the contributions in OCFs differ with those in closed channel flows (CCFs), comparisons between the two flows are also made. The scale-decomposed 'turbulent' contribution results of present OCFs exhibit two dominant contribution modes (i.e. large-scale motions (LSMs) and very-large-scale motions (VLSMs)) at a streamwise wavelength lambda(x) = 1 similar to 2h and O(10h), where h is the water depth. The large scales with lambda(x) > 3h and lambda(x) > 10h are demonstrated to contribute to over 40% and 20% of the mean wall-shear stress, respectively. Compared with CCFs, slightly higher and lower contributions in the lambda(x) > O(10h) and lambda(x) < O(10h) wavelength ranges are observed in OCFs, revealing the important free-surface effects in OCFs. Possible mechanisms are discussed to lend support for the observed differences between the two flows.
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页数:28
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