Abstract

A scalar emanating from a point source in a turbulent boundary layer does not mix homogeneously, but is organized in large regions with little variation of the concentration: uniform concentration zones. We measure scalar concentration using laser-induced fluorescence and, simultaneously, the three-dimensional velocity field using tomographic particle image velocimetry in a water tunnel boundary layer. We identify uniform concentration zones using both a simple histogram technique, and more advanced cluster analysis. From the complete information on the turbulent velocity field, we compute two candidate velocity structures that may form the boundaries between two uniform concentration zones. One of these structures is related to the rate of point separation along Lagrangian trajectories and the other one involves the magnitude of strong shear in snapshots of the velocity field. Therefore, the first method allows for the history of the flow field to be monitored, while the second method only looks at a snapshot. The separation of fluid parcels in time was measured in two ways: the exponential growth of the separation as time progresses (related to finite-time Lyapunov exponents and unstable manifolds in the theory of dynamical systems), and the exponential growth as time moves backward (stable manifolds). Of these two, a correlation with the edges of uniform concentration zones was found for the past Lyapunov field but not with the time-forward future field. The magnitude of the correlation is comparable to that of the regions of strong shear in the instantaneous velocity field.

Highlights

  • A plume of pollutant that emanates from a point source in a turbulent flow spreads mainly through turbulent diffusion

  • We call these regions ‘uniform concentration zones’ (UCZs). These regions are reminiscent of the regions of uniform momentum in turbulent boundary layers (Meinhart & Adrian 1995; Hutchins et al 2012; Eisma et al 2015)

  • This has inspired our nomenclature, but we will highlight the connection with ramp–cliff structures below

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Summary

Introduction

A plume of pollutant that emanates from a point source in a turbulent flow spreads mainly through turbulent diffusion. In time-dependent two-dimensional flows, LCS form transient barriers of transport, while they are advected almost passively These objects offer the tantalizing prospect of predicting the spread of contaminants from knowledge of large-scale coherent structures only. LCS may be a useful concept in fully developed 3-D turbulence When they organize as sheets, LCS structures may hinder scalar mixing and may be associated with boundaries of UCZs. In this paper, we will explore this concept in an experiment of a turbulent boundary layer that provides the full 3-D velocity field. We will explore this concept in an experiment of a turbulent boundary layer that provides the full 3-D velocity field Using this information, we measure the finite-time Lyapunov field in a plane perpendicular to the boundary.

Experiment
Uniform concentration zones
Finite-time Lyapunov exponents
Shear vorticity ωsh
Results
Conditional averages
Conclusion
Full Text
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