On Homogenization-Based Methods for Large-Eddy Simulation

[+] Author and Article Information
L. Persson

The Swedish Defense Research Agency, FOI, Department of NBC Defense, Environment and Protection, SE-901 82 Umea, Sweden

C. Fureby

The Swedish Defense Research Agency, FOI, Department of Weapons and Protection, Warheads and Propulsion, SE-172 Stockholm, Sweden

N. Svanstedt

Chalmers University of Technology, Department of Mathematics, SE-412 96 Gothenburg, Sweden

J. Fluids Eng 124(4), 892-903 (Dec 04, 2002) (12 pages) doi:10.1115/1.1516577 History: Received March 12, 2002; Revised June 24, 2002; Online December 04, 2002
Copyright © 2002 by ASME
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Grahic Jump Location
A typical sample path of w , according to Eq. (40), in green with a sample path of the Brownian motion (in red) in the one-dimensional case
Grahic Jump Location
Comparison of (a) the energy spectrum E and (b) the PDF of the vorticity magnitude |ω̄| of forced homogeneous isotropic turbulence at ReT=96 at 643 resolution for conventional LES, using the OEEVM, and the homogenisation-based LES model
Grahic Jump Location
Volumetric visualization in terms of iso-surfaces of the vorticity magnitude |ω | and contours of the eddy viscosity νk and |A | of forced homogeneous isotropic turbulence at ReT=96 at 643 resolution from (a) conventional LES using the OEEVM, and from (b) the homogenization based LES model
Grahic Jump Location
Contours of streamwise vorticity ω̄1 projected onto the side and bottom walls together with contours of the streamwise velocity fluctuations v1=v̄1−〈v̄1〉 at y+≈20, and iso-surfaces of the second invariant of the velocity gradient tensor Q for (a) OEEVM and (b) the homogenization-based subgrid model at 603 resolution at Reτ=395
Grahic Jump Location
Time-averaged velocity profiles 〈v̄1〉 (a) in outer scaling and the corresponding rms velocity fluctuations v̄1rms (b) in inner scaling for the fully developed turbulent channel flow case at Reτ=395



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