4.7 Article

Coherent structures in the inner part of a rough-wall channel flow resolved using holographic PIV

Journal

JOURNAL OF FLUID MECHANICS
Volume 711, Issue -, Pages 161-170

Publisher

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2012.382

Keywords

boundary layer structure; turbulent boundary layers

Funding

  1. Office of Naval Research [000140-91-10-0-7]
  2. National Science Foundation [0932941]
  3. Directorate For Engineering
  4. Div Of Chem, Bioeng, Env, & Transp Sys [0932941] Funding Source: National Science Foundation

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Microscopic holographic PIV performed in an optically index-matched facility resolves the three-dimensional flow in the inner part of a turbulent channel flow over a rough wall at Reynolds number Re-tau = 3520. The roughness consists of uniformly distributed pyramids with normalized height of k(s)(+) = 1.5k(+) = 97. Distributions of mean flow and Reynolds stresses agree with two-dimensional PIV data except very close to the wall (<0.7k) owing to the higher resolution of holography. Instantaneous realizations reveal that the roughness sublayer is flooded by low-lying spanwise and groove-parallel vortical structures, as well as quasi-streamwise vortices, some quite powerful, that rise at sharp angles. Conditional sampling and linear stochastic estimation (LSE) reveal that the prevalent flow phenomenon in the roughness sublayer consists of interacting U-shaped vortices, conjectured in Hong et al. (J. Fluid M e c h., 2012, doi:10.1017/jfm.2012.403). Their low-lying base with primarily spanwise vorticity is located above the pyramid ridgeline, and their inclined quasi-streamwise legs extend between ridgelines. These structures form as spanwise vorticity rolls up in a low-speed region above the pyramid's forward face, and is stretched axially by the higher-speed flow between ridgelines. Ejection induced by interactions among legs of vortices generated by neighbouring pyramids appears to be the mechanism that lifts the quasi-streamwise vortex legs and aligns them preferentially at angles of 54 degrees-63 degrees to the streamwise direction.

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