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A revisit of the equilibrium assumption for predicting near-wall turbulence

Published online by Cambridge University Press:  07 November 2014

Farid Karimpour
Affiliation:
Department of Civil and Environmental Engineering, Colorado State University, Fort Collins, CO 80523-1372, USA
Subhas K. Venayagamoorthy*
Affiliation:
Department of Civil and Environmental Engineering, Colorado State University, Fort Collins, CO 80523-1372, USA
*
†Email address for correspondence: vskaran@colostate.edu
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Abstract

In this study, we revisit the consequence of assuming equilibrium between the rates of production ( $P$ ) and dissipation  $({\it\epsilon})$ of the turbulent kinetic energy  $(k)$ in the highly anisotropic and inhomogeneous near-wall region. Analytical and dimensional arguments are made to determine the relevant scales inherent in the turbulent viscosity ( ${\it\nu}_{t}$ ) formulation of the standard $k{-}{\it\epsilon}$ model, which is one of the most widely used turbulence closure schemes. This turbulent viscosity formulation is developed by assuming equilibrium and use of the turbulent kinetic energy $(k)$ to infer the relevant velocity scale. We show that such turbulent viscosity formulations are not suitable for modelling near-wall turbulence. Furthermore, we use the turbulent viscosity $({\it\nu}_{t})$ formulation suggested by Durbin (Theor. Comput. Fluid Dyn., vol. 3, 1991, pp. 1–13) to highlight the appropriate scales that correctly capture the characteristic scales and behaviour of $P/{\it\epsilon}$ in the near-wall region. We also show that the anisotropic Reynolds stress ( $\overline{u^{\prime }v^{\prime }}$ ) is correlated with the wall-normal, isotropic Reynolds stress ( $\overline{v^{\prime 2}}$ ) as $-\overline{u^{\prime }v^{\prime }}=c_{{\it\mu}}^{\prime }(ST_{L})(\overline{v^{\prime 2}})$ , where $S$ is the mean shear rate, $T_{L}=k/{\it\epsilon}$ is the turbulence (decay) time scale and $c_{{\it\mu}}^{\prime }$ is a universal constant. ‘A priori’ tests are performed to assess the validity of the propositions using the direct numerical simulation (DNS) data of unstratified channel flow of Hoyas & Jiménez (Phys. Fluids, vol. 18, 2006, 011702). The comparisons with the data are excellent and confirm our findings.

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© 2014 Cambridge University Press 
Figure 0

Figure 1. Comparison of (a) $U_{k{-}{\it\epsilon}}$ with $U_{TVH}$; (b) $L_{k{-}{\it\epsilon}}$ with $L_{TVH}$ and (c) $T_{k{-}{\it\epsilon}}$ with $T_{TVH}$; in a turbulent channel flow, computed from the DNS data of Hoyas & Jiménez (2006) for $\mathit{Re}_{{\it\tau}}=2003$.

Figure 1

Figure 2. Comparison of $c^{2}=-\overline{u^{\prime }v^{\prime }}/k$ for different Reynolds numbers, using (a) DNS data of turbulent channel flows for $\mathit{Re}_{{\it\tau}}=2003,934,590,395$ and 180; and (b) experimental data of boundary layer flow of Marusic & Perry (1995).

Figure 2

Figure 3. Comparison of Reynolds stresses and the turbulent kinetic energy ($k$) computed from (a) DNS data of Hoyas & Jiménez (2006) for $\mathit{Re}_{{\it\tau}}=2003$; and (b) experimental boundary layer data of Marusic & Perry (1995) for $\mathit{Re}_{{\it\theta}}=19\,133$.

Figure 3

Figure 4. Comparison of Durbin’s model $P/{\it\epsilon}$ and the exact value computed from DNS data of Hoyas & Jiménez (2006) for $\mathit{Re}_{{\it\tau}}=2003$.

Figure 4

Figure 5. Comparison of (a) $U_{k{-}{\it\epsilon}{-}v^{2}}$ and $(\overline{v^{\prime 2}})^{1/2}$ with $U_{TVH}$; and (b) $L_{k{-}{\it\epsilon}{-}v^{2}}$ with $L_{TVH}$ computed from DNS data of Hoyas & Jiménez (2006) for $\mathit{Re}_{{\it\tau}}=2003$.