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Turbulent dispersion with broken reflectional symmetry

Published online by Cambridge University Press:  10 February 1997

Michael Borgas
Affiliation:
CSIRO Division of Atmospheric Research, Aspendale, Victoria 3195, Australia
Thomas K. Flesch
Affiliation:
University of Alberta, Edmonton, Canada
Brian L. Sawford
Affiliation:
CSIRO Division of Atmospheric Research, Aspendale, Victoria 3195, Australia

Extract

We consider dispersion in axisymmetric turbulence which lacks reflectional symmetry. A stochastic equation for the Lagrangian evolution of the velocity of a fluid particle, which is appropriate for infinite Reynolds number turbulence, is used to model the dispersion. Such equations are now common as Lagrangian dispersion models for atmospheric transport problems, but are only strictly well founded for isotropic homogeneous turbulence. It is the minimalist variation from this state of affairs that is considered here. Axisymmetry is the most highly symmetric turbulence that can be suitably analysed by these techniques, spherical symmetry being equivalent to full isotropy in the class of models considered. This simple relaxation of full symmetry leads to oscillations of the Lagrangian velocity autocorrelation, oscillatory growth of the dispersion, significant reduction of dispersion for fixed turbulence kinetic energy and dissipation rate, spiralling fluid-particle trajectories, and tracer fluxes orthogonal to gradients (skew diffusion). The mean fluid-particle angular momentum is an important parameter.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1997

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References

Anand, M. S. & Pope, S. B. 1985 Diffusion behind a line source in grid turbulence. In Turbulent Shear Flows (ed. Bradbury, L. J. S., Durst, F., Launder, B. E., Schmidt, F. W. & Whitelaw, J. H.), vol. 4. Springer.Google Scholar
Angell, J. K., Pack, D. H. & Dickson, C. R. 1967 A Lagrangian study of helical circulations in the planetary boundary layer. J. Atmos. Sci. 25, 707717.Google Scholar
Batchelor, G. K. 1953 The Theory of Homogeneous Turbulence. Cambridge University Press.Google Scholar
Borgas, M. S. & Sawford, B. L. 1991 The small-scale structure of acceleration correlations and its role in the statistical theory of turbulent dispersion. J. Fluid Mech. 228, 295320.Google Scholar
Borgas, M. S. & Sawford, B. L. 1994a Stochastic equations with multifractal increments for modelling turbulent dispersion. Phys. Fluids A 6, 618633.CrossRefGoogle Scholar
Borgas, M. S. & Sawford, B. L. 19946 A family of models for two-particle dispersion in isotropic homogeneous stationary turbulence. J. Fluid Mech. 279, 6999.Google Scholar
Borgas, M. S. & Sawford, B. L. 1996 Molecular diffusion and viscous effects on concentration statistics in grid turbulence. J. Fluid Mech. 324, 2554.Google Scholar
Chatwin, P. C. & Sullivan, P. J. 1989 The intermittency factor of scalars in turbulence. Phys. Fluids A 1, 761763.Google Scholar
Cieszelski, R. 1994 Diffusion of pollutants by helical vortices with subgrid turbulence. In Air Pollution II Vol. I: Computer Simulations (ed. Baldasano, J. M., Brebbia, C. A., Power, H. & Zannetti, P.), pp. 175182. Computational Mechanics Publications, Southampton Boston.Google Scholar
Corrsin, S. 1951 The decay of isotropic temperature fluctuations in an isotropic turbulence. J. Aeronaut. Sci. 18.Google Scholar
Drummond, I. T., Duane, S. & Horgan, R. R. 1984 Scalar diffusion in simulated helical turbulence with molecular diffusivity. J. Fluid Mech. 138, 7591.Google Scholar
Etling, D. 1985 Some aspects of helicity in atmospheric flows. Beitr. Phys. Atmos. 58, 88100.Google Scholar
Flesch, T. K. & Wilson, J. D. 1992 A two-dimensional trajectory-simulation model for non- Gaussian, inhomogeneous turbulence within plant canopies. Boundary-Layer Met. 61, 349374.Google Scholar
Gardiner, C. W. 1983 Handbook of Stochastic Methods. Springer.Google Scholar
Inoue, E. 1952 On the Lagrangian correlation coefficient for turbulent diffusion and application to atmospheric diffusion phenomena. Geophys. Res. Paper No. 19, 397412.Google Scholar
Jayesh & Warhaft, Z. 1992 Probability distribution, conditional dissipation, and transport of passive temperature fluctuations in grid-generated turbulence. Phys. Fluids A 4, 22922307.Google Scholar
Kholmyansky, M., Kit, E., Teitel, M. & Tsinober, A. 1991 Some experimental results on velocity and vorticity measurements in turbulent grid flows with controlled sign of mean helicity. Fluid Dyn. Res. 7, 6575.Google Scholar
Kraichnan, R. H. 1977 Lagrangian velocity covariance in helical turbulence. J. Fluid Mech. 81, 385398.Google Scholar
Moffatt, H. K. 1983 Transport effects associated with turbulence, with particular attention to the influence of helicity. Rep. Prog. Phys. 46, 621664.Google Scholar
Moffatt, H. K. & Tsinober, A. 1992 Helicity in laminar and turbulent flow. Ann. Rev. Fluid Mech. 24, 281312.Google Scholar
Obukhov, A. M. 1959 Description of turbulence in terms of Lagrangian variables. Adv. Geophvs. 6, 113115.Google Scholar
Pope, S. B. 1994 Lagrangian PDF methods for turbulent flows. Ann. Rev. Fluid Mech. 26, 2363.Google Scholar
Sawford, B. L. 1991 Reynolds number effects in Lagrangian stochastic models of dispersion. Phys. Fluids A 3, 15771586.Google Scholar
Sawford, B. L. & Borgas, M. S. 1994 On the continuity of stochastic models for the Lagrangian velocity in turbulence. Physica D 76, 297311.Google Scholar
Taylor, G. I. 1921 Diffusion by continuous movements. Proc. Lond. Math. Soc. 20, 196211.Google Scholar
Thomson, D. J. 1987 Criteria for the selection of stochastic models of particle trajectories in turbulent flows. J. Fluid Mech. 180, 529556.CrossRefGoogle Scholar
Zeman, O. 1994 A note on the spectra and decay of rotating homogeneous turbulence. Phys. Fluids A 6, 32213223.Google Scholar