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A dissipative random velocity field for fully developed fluid turbulence

Published online by Cambridge University Press:  04 April 2016

Rodrigo M. Pereira*
Affiliation:
Univ Lyon, Ens de Lyon, Univ Claude Bernard, CNRS, Laboratoire de Physique, 46 allée d’Italie F-69342 Lyon, France CAPES Foundation, Ministry of Education of Brazil, Brasília/DF 70040-020, Brazil
Christophe Garban
Affiliation:
Université de Lyon, Institut Camille Jordan, 43 blvd. du 11 novembre 1918, F-69622 Villeurbanne CEDEX, France
Laurent Chevillard
Affiliation:
Univ Lyon, Ens de Lyon, Univ Claude Bernard, CNRS, Laboratoire de Physique, 46 allée d’Italie F-69342 Lyon, France
*
†Email address for correspondence: rodrigo.pereira@ens-lyon.fr

Abstract

We investigate the statistical properties, based on numerical simulations and analytical calculations, of a recently proposed stochastic model for the velocity field (Chevillard et al., Europhys. Lett., vol. 89, 2010, 54002) of an incompressible, homogeneous, isotropic and fully developed turbulent flow. A key step in the construction of this model is the introduction of some aspects of the vorticity stretching mechanism that governs the dynamics of fluid particles along their trajectories. An additional further phenomenological step aimed at including the long range correlated nature of turbulence makes this model dependent on a single free parameter, ${\it\gamma}$ , that can be estimated from experimental measurements. We confirm the realism of the model regarding the geometry of the velocity gradient tensor, the power-law behaviour of the moments of velocity increments (i.e. the structure functions) including the intermittent corrections and the existence of energy transfer across scales. We quantify the dependence of these basic properties of turbulent flows on the free parameter ${\it\gamma}$ and derive analytically the spectrum of exponents of the structure functions in a simplified non-dissipative case. A perturbative expansion in power of ${\it\gamma}$ shows that energy transfer, at leading order, indeed take place, justifying the dissipative nature of this random field.

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© 2016 Cambridge University Press 
Figure 0

Figure 1. Logarithmic representation of the joint probability density $\mathscr{P}(Q^{\ast },R^{\ast })$ of $R^{\ast }=R/\langle \unicode[STIX]{x1D61A}_{ij}\unicode[STIX]{x1D61A}_{ij}\rangle ^{3/2}$ and $Q^{\ast }=Q/\langle \unicode[STIX]{x1D61A}_{ij}\unicode[STIX]{x1D61A}_{ij}\rangle$ calculated from the simulation of the field $\boldsymbol{u}^{{\it\epsilon}}$ using $L={\rm\pi}/2$, $N=2048$ and ${\it\epsilon}=3\,(\text{d}x)^{1/3}$. (a) ${\it\gamma}^{2}=0$ (Gaussian case), (b) ${\it\gamma}^{2}=0.033$, (c) ${\it\gamma}^{2}=0.067$ and (d) ${\it\gamma}^{2}=0.133$. Contour lines are the same in all cases, logarithmically spaced by a factor of 10, and start at 1 near the origin. The thick line represents the zero discriminant (or Vieillefosse) line: $(27/4)R^{2}+Q^{3}=0$.

Figure 1

Figure 2. Probability densities of $\cos ({\it\theta})$, where ${\it\theta}$ is the angle between vorticity and the eigenvectors of the rate-of-strain tensor, estimated from the same numerical simulation as in figure 1. We represent alignments with the eigenvectors associated to the most negative (a), intermediate (b) and most positive (c) eigenvalues, for the Gaussian case ${\it\gamma}=0$ (solid lines), ${\it\gamma}^{2}=0.033$ (dashed), ${\it\gamma}^{2}=0.067$ (dot-dashed) and ${\it\gamma}^{2}=0.133$ (dotted).

Figure 2

Figure 3. Logarithmic representation of the flatness of longitudinal (a,b) and transverse (c,d) velocity increments (5.1) as a function of scales: (a,c) dependent case; (b,d) independent case. The parameters of the simulation are $N=2048$, $L={\rm\pi}/2$ and ${\it\epsilon}=(\text{d}x)^{1/3}\approx 0.00307$ (see discussion in § 3). We use several values for the parameter ${\it\gamma}^{2}=0,0.01,0.02,0.04,0.067,0.08,0.10,0.12$, that give in all cases and any scale $\ell$ an increasing value of the flatness. In (a) (respectively (c)) we represent the flatnesses of the longitudinal (transverse) increments corresponding to the vector field $\boldsymbol{u}^{{\it\epsilon}}$ (1.8). We represent in a similar way in (b) and (d) the flatnesses but for the velocity field $\boldsymbol{u}^{ind,{\it\epsilon}}$ (5.3). The power laws observed at moderate scales are superimposed on the same plots.

Figure 3

Figure 4. Estimation of the power-law exponents ${\it\beta}^{\Vert ,\bot }({\it\gamma})$ defined in (5.2) from the fits performed in figure 3 as a function of ${\it\gamma}^{2}$. We represent in (a) the results in the dependent case (corresponding to the fits of figure 3a,c), using the symbols $\times$ for longitudinal, and $\circ$ for the transverse velocity increments. In (b), similar study for the independent case corresponding to the fits of figure 3(b,d). We superimpose in (b) the result of our theoretical predictions: (dashed line) the asymptotic prediction ${\it\beta}^{\Vert ,\bot }({\it\gamma})=-4{\it\gamma}^{2}$ considering that the exponents ${\it\beta}^{\Vert ,\bot }({\it\gamma})$ have been measured at vanishing scales $\ell \rightarrow 0$, and (solid line) a prediction that takes into account corrections implied by the finiteness of the scale $\ell$ (see § 5.2.5).

Figure 4

Figure 5. (a) Skewness of longitudinal velocity increments $\mathscr{S}(\ell )$ (6.27) as a function of the scale $\ell$, estimated from the same type of numerical simulations as the ones used in figure 3, for ${\it\gamma}^{2}=0.0001,0.0009,0.0025,0.005,0.01,0.02,0.067$. (b) Value of the skewness at the origin $\mathscr{S}(0)$ as a function of ${\it\gamma}$. We superimpose a straight line to show the linear behaviour of $\mathscr{S}(0)$ at small ${\it\gamma}$, as predicted by (6.28).