The return to isotropy of homogeneous turbulence

Author:

Lumley John L.,Newman Gary R.

Abstract

The return to isotropy of homogeneous turbulence without mean velocity gradients is attacked by considering changes to be slow relative to turbulence time scales. This single assumption permits the problem to be cast as one of finding the form of three invariant functions. Examination of limiting behaviour for large Reynolds number and small anisotropy, as well as small Reynolds number and arbitrary anisotropy, places restrictions on the form of the functions. Realizability conditions (requiring that energies be non-negative) reduce the problem to two functions subject to further restrictions. A convenient interpolation form is found for the functions, satisfying all the restrictions, and it is shown that predictions based on this are in excellent agreement with all available data.

Publisher

Cambridge University Press (CUP)

Subject

Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics

Reference23 articles.

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4. Comte-Bellot, G. & Corrsin, S. 1966 The use of a contraction to improve the isotropy of grid-generated turbulence.J. Fluid Mech. 25,657–682.

5. Lumley, J. L. 1975 Prediction methods for turbulent flows, introduction. Lecture notes for series Prediction Methods for Turbulent Flows .Von Kármân Inst., Rhode-St-Genese, Belgium.

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