Vorticity and Turbulence in the Wake of a Bridge Pier

Dissipation rates of turbulence kinetic energy (TKE) epsiv and enstrophy zeta 2 are reported in a high Reynolds number turbulent wake. Previous turbulent wake observations have been made in laboratory experiments with relatively low Reynolds number flows O (10 3 ). Results presented here are from a...

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Veröffentlicht in:IEEE journal of oceanic engineering 2009-07, Vol.34 (3), p.307-314
Hauptverfasser: Ren-Chieh Lien, Sanford, T.B.
Format: Artikel
Sprache:eng
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Zusammenfassung:Dissipation rates of turbulence kinetic energy (TKE) epsiv and enstrophy zeta 2 are reported in a high Reynolds number turbulent wake. Previous turbulent wake observations have been made in laboratory experiments with relatively low Reynolds number flows O (10 3 ). Results presented here are from a set of rare field observations of vorticity and turbulence in a turbulent wake with a high Reynolds number O (10 7 ). The turbulent wake was formed by an unsteady strong tidal current interacting with a bridge pier. Measurements were taken mostly in the intermediate wake, i.e., 10 les x / d les 60, where x is the downstream distance and d is the width of the bridge pier. Both epsiv and zeta 2 show a similar downstream decay rate that is faster than that predicted by the self-preservation similarity in the far wake. The theoretical relation epsiv = nuzeta 2 for high Reynolds number flow is confirmed by field observations. The magnitudes of the vertical and horizontal components of enstrophy do not differ significantly. The turbulence internal intermittency is ~ 0.2, estimated from autocorrelation coefficients of enstrophy; this value is close to that reported previously in turbulent wakes and jets.
ISSN:0364-9059
1558-1691
DOI:10.1109/JOE.2009.2019383