On the structure of shear stress and turbulent kinetic energy flux across the roughness layer of a gravel-bed channel flow
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Publication:3550407
DOI10.1017/S0022112009990772zbMath1183.76033MaRDI QIDQ3550407
E. Barthelemy, Emmanuel Mignot, D. Hurther
Publication date: 31 March 2010
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Experimental work for problems pertaining to fluid mechanics (76-05) Shear flows and turbulence (76F10)
Related Items (3)
Influence of permeable beds on hydraulically macro-rough flow ⋮ Turbulence modifications induced by the bed mobility in intense sediment-laden flows ⋮ Direct numerical simulation of turbulence over anisotropic porous media
Cites Work
- Turbulent transport in the outer region of rough-wall open-channel flows: the contribution of large coherent shear stress structures (LC3S)
- Double-averaging analysis and local flow characterization of near-bed turbulence in gravel-bed channel flows
- Conditional statistics of Reynolds stress in rough-wall and smooth-wall turbulent boundary layers
- Prediction of the contributions to the Reynolds stress from bursting events in open-channel flows
- Characteristics of vortex packets in turbulent boundary layers
- Turbulence in Plant Canopies
- Vortex organization in the outer region of the turbulent boundary layer
- Secondary flow in sharp open-channel bends
- Rough-wall boundary layers: mean flow universality
- Turbulence structure in sharp open-channel bends
- T<scp>URBULENT</scp> F<scp>LOWS OVER</scp> R<scp>OUGH</scp> W<scp>ALLS</scp>
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