Turbulent deformations: Dynamics and statistics of velocity gradients in the inertial range of turbulence.

Charles Meneveau

Department of Mechanical Engineering
The Johns Hopkins University

Abstract-
What is the `canonical structure' of turbulent flows remains an important and multifaceted fundamental question in turbulence research. One facet relates to typical local deformations of fluid elements in the neighborhood of Lagrangian tracers. These deformations are described by the velocity gradient tensor. Its properties determine, for instance, if the deformation produces vorticity stretching along a particular direction (possibly yielding tubular vortex structures), or to produce structures that are flattened out in one direction while expanding in the other two (possibly yielding pancake-like objects).
On the basis of recent three-dimensional measurements in turbulent duct flow using holographic PIV techniques (Tao, Katz & Meneveau, J. Fluid Mech. 2002 in press), we consider the dynamics of the velocity gradient tensor filtered at inertial-range scales. In addition to self-interactions and the filtered pressure Hessian, the evolution of the filtered velocity gradient tensor is determined by the subgrid-scale stress tensor. As in so-called Restricted Euler dynamics, the evolution equations can be simplified by considering two invariants R and Q. The effects of the subgrid-scale stress tensor on them can be quantified unambiguously by evaluating conditional averages that appear in the evolution equation for the joint PDF of the invariants. The HPIV measurements show that the SGS stresses have significant effects, e.g. along the so-called Vieillefosse tail they oppose the formation of a finite-time singularity that occurs in Restricted Euler dynamics. Motivated by practical modeling needs in the context of large eddy simulations, we examine the behavior of various closures for the subgrid stresses. Analysis of the Smagorinsky, nonlinear, and mixed models show that all reproduce the real SGS stress effect along the Vieillefosse tail, but that they fail in several other regions. An attempt is made to optimize the mixed model by letting the two model coefficients be functions of the two invariants R and Q.


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