• Open Access

Return to isotropy of homogeneous shear-released turbulence

Ping-Fan Yang, Alain Pumir, and Haitao Xu
Phys. Rev. Fluids 6, 044601 – Published 2 April 2021

Abstract

The presence of mean velocity gradients induces anisotropies in turbulent flows, which affect even the smallest scales of motion at finite Reynolds numbers. By performing direct numerical simulations of the Navier-Stokes equations, we study the return to isotropy of a homogeneous turbulent flow initially in a statistically stationary state under a uniform shear, S=U1x2, in the conceptually simple situation where the mean shear is suddenly released. In particular, we characterize the timescales involved in the dynamics. We observe that the Reynolds stress tensor, which measures the large-scale flow anisotropy, relaxes towards an isotropic form over a timescale of the order of the large-eddy turnover time of turbulence, in qualitative agreement with previous studies with different types of initially imposed mean velocity gradient. We also investigate how the correlations of the velocity gradient tensor relax to isotropy with time. In particular, we focus on the properties of the one-point vorticity correlations ωiωj and ωiωjωk. The nonzero off-diagonal term of the second-order correlation tensor, i.e., the correlation between the streamwise and the transverse components of vorticity, ω1ω2, decreases towards 0 over a time of the order of the Kolmogorov timescale. In comparison, the anisotropies in the diagonal components ωi2 (i=1, 2, or 3) relax over a time significantly longer than the Kolmogorov timescale. This difference can be explained by an elementary theoretical analysis of the dynamics of the anisotropy tensor bijωωiωjωkωk13δij at the instant when the shear is released. We also observe that the skewness of the spanwise component of vorticity, Sω3, relaxes slowly towards zero. The relaxation of a small-scale quantity over a time much longer than the Kolmogorov timescale, as surprising as it may seem, is in fact consistent with a known relation between velocity-gradient correlations and the pressure-rate-of-strain correlation, and raises the important question of separation between the timescales characterizing the return to isotropy at large and small scales.

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  • Received 31 August 2020
  • Accepted 17 March 2021

DOI:https://doi.org/10.1103/PhysRevFluids.6.044601

Published by the American Physical Society under the terms of the Creative Commons Attribution 4.0 International license. Further distribution of this work must maintain attribution to the author(s) and the published article's title, journal citation, and DOI. Open access publication funded by the Max Planck Society.

Published by the American Physical Society

Physics Subject Headings (PhySH)

  1. Research Areas
Nonlinear DynamicsFluid Dynamics

Authors & Affiliations

Ping-Fan Yang1, Alain Pumir2,3, and Haitao Xu4

  • 1Center for Combustion Energy and Department of Energy and Power Engineering, Tsinghua University, 100084 Beijing, China
  • 2Université Lyon, ENS de Lyon, Université Claude Bernard, Centre National de la Recherche Scientifique, Laboratoire de Physique, F-69342 Lyon, France
  • 3Max Planck Institute for Dynamics and Self-Organization, 37077 Göttingen, Germany
  • 4Center for Combustion Energy and School of Aerospace Engineering, Tsinghua University, 100084 Beijing, China

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Issue

Vol. 6, Iss. 4 — April 2021

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