Spectral approach to non-isotropic turbulence subjected to rotation

Author:

Cambon C.,Jacquin L.

Abstract

The non-isotropic effects of solid-body rotation on homogeneous turbulence are investigated in this paper. A spectral formalism using eigenmodes introduces the spectral Coriolis effects more easily and leads to simpler expressions for the integral quadratic terms which come mostly from classical two-point closures. The analysis is then applied to a specific eddy damped quasi-normal Markovian model, which includes the inertial waves regime in the evaluation of triple correlations. This procedure allows for a departure from isotropy by external rotation effects. When started with rigorously isotropic initial data, the various trends observed on the Reynolds stresses and the integral lengthscales remain in accordance with the results from direct simulations; moreover they reflect a very specific spectral angular distribution. Such an angular dependence allows a drain of spectral energy from the parallel to the normal wave vectors (with respect to the rotation axis), and thus appears consistent with a trend toward two-dimensionality.

Publisher

Cambridge University Press (CUP)

Subject

Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics

Reference25 articles.

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2. Cambon, C. :1982 Etude spectrale d'un champ turbulent incompressible soumis à des-effets couples de déformation et de rotation imposés extérieurement. Thèse d'Etat,Université Lyon I.

3. Comte-Bellot, G. & Corrsin, S. 1971 Simple Eulerian time correlation of full and narrow-band velocity signals in grid-generated, ‘isotropic’ turbulence.J. Fluid Mech. 48,273–337.

4. Dang, K. & Roy, Ph. ,1985a Numerical simulation of homogeneous turbulence. In Proc. Workshop on Macroscopic Modelling of Turbulent Flows and Fluid Mixtures .Springer.

5. Bertoglio, J. P. , Cambon, C. , Jeandel, D. & Mathieu, J. ,1979 Comparaison directe entre une modélisation directionnelle du tenseur spectral des corrélations doubles et une solution analytique dans le cas d'une turbulence homogène anisotrope.C. R. Acad. Sci. Paris 288B,473–475.

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