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From Time to Space and Back: Convection and Wave Velocities in Turbulent Shear Flows

  • B. Ganapathisubramani
  • R. de Kat
Conference paper
Part of the Springer Proceedings in Physics book series (SPPHY, volume 165)

Abstract

To obtain spatial spectra, experimentalists map temporal spectra using Taylor’s hypothesis [18]. This transfer function relates wavenumber to frequency using a convection velocity, a velocity that proves difficult to define and use. Adding to this difficulty, convection and wave velocities have been treated the same, despite the obvious difference between them. Convection velocities are velocities at which a specific structure moves—group velocity—and wave velocities are velocities at which a single wave moves—phase velocity. The ideal mapping function to go between wavenumber and frequency is the wavenumber-frequency spectrum that shows a range of wave velocities can contribute to a single wavenumber or a single frequency, and this range can differ significantly between them. To try to capture the influence of this range, experimentalists have applied various peak or average wave velocities with varying success. However, none account for the spread in wave velocities directly. In this paper we propose a two-point cross-spectral approach that uses a distribution of wave velocities to reconstruct the wavenumber-frequency plane. This plane can then be integrated to obtain the spatial spectrum. We verify the technique on particle image velocimetry data set of a turbulent boundary layer, and we obtain a transfer function from this data set. The transfer function is applied to hot-wire data at a comparable Reynolds, and comparison of the newly proposed technique with the classic Taylor’s hypothesis approach shows that Taylor’s hypothesis hold for larger frequencies and wavenumbers the smaller frequencies and wavenumbers (long temporal and spatial scales) there are significant differences.

Keywords

Wave Velocity Particle Image Velocimetry Turbulent Boundary Layer Velocity Fluctuation Streamwise Velocity 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

We gratefully acknowledge the support from UK Engineering and Physical Sciences Research Council (EPSRC) through Grant EP/I004785/1. The research leading to these results has also received funding from the European Research Council under the European Union’s Seventh Framework Programme (FP7/2007–2013)/ERC Grant agreement no 277472-WBT.

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Copyright information

© Springer International Publishing Switzerland 2016

Authors and Affiliations

  1. 1.Faculty of Engineering and the EnvironmentUniversity of SouthamptonSouthamptonUK

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