Hostname: page-component-7b7567c8c-tnzcf Total loading time: 0 Render date: 2026-11-14T18:31:49.882Z Has data issue: false hasContentIssue false

Turbulent pair dispersion as a ballistic cascade phenomenology

Published online by Cambridge University Press:  08 May 2015

Mickaël Bourgoin*
Affiliation:
Laboratoire des Écoulements Géophysiques et Industriels, CNRS/UJF/G-INP, UMR 5519, Université de Grenoble, BP53, 38041, Grenoble, France
*
†Email address for correspondence: mickael.bourgoin@hmg.inpg.fr

Abstract

Since the pioneering work of Richardson in 1926, later refined by Batchelor and Obukhov in 1950, it is predicted that the rate of separation of pairs of fluid elements in turbulent flows with initial separation at inertial scales, grows ballistically first (Batchelor regime), before undergoing a transition towards a super-diffusive regime where the mean-square separation grows as $t^{3}$ (Richardson regime). Richardson empirically interpreted this super-diffusive regime in terms of a non-Fickian process with a scale-dependent diffusion coefficient (the celebrated Richardson’s ‘ $4/3$ rd’ law). However, the actual physical mechanism at the origin of such a scale dependent diffusion coefficient remains unclear. The present article proposes a simple physical phenomenology for the time evolution of the mean-square relative separation in turbulent flows, based on a scale-dependent ballistic scenario rather than a scale-dependent diffusive. It is shown that this phenomenology accurately retrieves most of the known features of relative dispersion for particles mean-square separation, among others: (i) it is quantitatively consistent with most recent numerical simulations and experiments for mean-square separation between particles (both for the short-term Batchelor regime and the long-term Richardson regime, and for all initial separations at inertial scales); (ii) it gives a simple physical explanation of the origin of the super-diffusive $t^{3}$ Richardson regime which naturally builds itself as an iterative process of elementary short-term scale-dependent ballistic steps; (iii) it shows that the Richardson constant is directly related to the Kolmogorov constant (and eventually to a ballistic persistence parameter); and (iv) in a further extension of the phenomenology, taking into account third-order corrections, it robustly describes the temporal asymmetry between forward and backward dispersion, with an explicit connection to the cascade of energy flux across scales. An important aspect of this phenomenology is that it simply and robustly connects long-term super-diffusive features to elementary short-term mechanisms, and at the same time it connects basic Lagrangian features of turbulent relative dispersion (both at short and long times) to basic Eulerian features of the turbulent field: second-order Eulerian statistics control the growth of separation (both at short and long times) while third-order Eulerian statistics control the temporal asymmetry of the dispersion process, which can then be directly identified as the signature of the energy cascade and associated to well-known exact results as the Karman–Howarth–Monin relation.

Information

Type
Papers
Copyright
© 2015 Cambridge University Press 
Figure 0

Figure 1.Qualitative illustration of the non-normal dispersion of a dense cluster of particles as proposed in Richardson’s original 1926 article (Richardson 1926), from which the figure is reproduced.

Figure 1

Figure 2.Illustration of the iterative ballistic cascade for the relative separation of two particles initially separated by a distance $D_{0}$: at each iteration step $k$, the mean-square separation between particles grows ballistically from $D_{k}^{2}$ to $D_{k+1}^{2}$ with a growth rate $S_{2}(D_{k})$, during a time lag $t_{k}$. Depending on the physical process at the origin of the local ballistic behaviour, both $S_{2}$ and $t_{k}$ may eventually depend on the local scale $D_{k}$. The overall time required to reach the mean-square separation $D_{k}^{2}$ at the iteration number $k$ is $T_{k}=\sum _{j=0}^{k-1}t_{j}(D_{j})$.

Figure 2

Figure 3.(a) Dependency of the Richardson constant $g$ on the Kolmogorov constant $C$ in the ballistic mode when the persistence parameter is fixed to ${\it\alpha}=1$. (b) Prediction of the Richardson constant $g$ on the persistence parameter ${\it\alpha}$, when the Kolmogorov constant is fixed to $C=C^{3D}=7.7$.

Figure 3

Figure 4.Growth of the mean-square separation between particles predicted as the iterative scale dependent ballistic process (defined by (2.4)) propagates starting from several initial separations $D_{0}$ in the inertial range of turbulence. The mean-square separation $\langle D^{2}\rangle$ is normalized by the square of the dissipative scale ${\it\eta}^{2}$ and time is normalized by the dissipative time scale ${\it\tau}_{{\it\eta}}$. Turbulent energy dissipation rate and dissipative scales have been chosen to match experiments in Bourgoin et al. (2006), although as shown in figure 5, the results are independent of this particular choice when the data is properly normalized. It can be seen in this plot that at long times, a dispersive regime ‘à la Richardson’, cubic in time and independent of initial separation, is naturally built by the iterative scale-dependent ballistic process.

Figure 4

Figure 5.Growth of the mean-square separation (with the initial separation subtracted) normalized by $t_{0}S_{2}(D_{0})$ as a function of time normalized by $t_{0}$. The solid black line correspond to the exact same data as in figure 4 from the ballistic model (with $C=7.7$ and ${\it\alpha}=0.12$), which with the present normalization collapses onto a single curve, according to relation (3.1). The mid-grey line corresponds to the prediction of the ballistic model with $C=7.7$ and ${\it\alpha}=1$. Coloured circles correspond to experimental results for the mean-square pair separation in Bourgoin et al. (2006) for different initial separations. Other symbols correspond to the mean-square separation for different initial separations from the DNS by Bitane et al. (2012). Finally the light grey line shows the prediction from Grossmann and Procaccia’s model (Grossmann & Procaccia 1984; Grossmann 1990). Two important aspects to be noted are: (i) the limited temporal range of experimental data, which does not allow to probe the transition between the initial ballistic regime and the late Richardson cubic regime; and (ii) the remarkable agreement between the ballistic model and the numerical simulations.

Figure 5

Table 1.Values to be used for the asymmetry parameter $C_{au}$ for the different cases.

Figure 6

Figure 6.Dependency of the Richardson constant predicted by the ballistic cascade model (with third-order term correction (4.3)) for the forward and backward dispersion problem in direct cascade 3D turbulence, as a function of the persistence parameter. The plot shows the forward Richardson constant $g_{fwd}^{3D}$ (full line, blue online), the backward Richardson constant $g_{bwd}^{3D}$ (dot–dashed line, red online) and the ratio $g_{bwd}^{3D}/g_{fwd}^{3D}$ (dashed line, yellow online). The vertical dot line emphasizes the optimal value for the persistence parameter, determined as the smallest value of this parameter for which the forward Richardson constant predicted by the model matches the values in the literature ($g_{fwd}^{3D}\simeq 0.55$). The horizontal lines emphasize the corresponding values for the forward and backward Richardson constants, as well as for the ratio $g_{bwd}^{3D}/g_{fwd}^{3D}$ (these values are reported on the right-hand side of the plots).

Figure 7

Figure 7.Same as figure 6, but for the case of 2D inverse cascade. The optimal value for the persistence parameter, is here determined as the smallest value for which the forward Richardson constant predicted by the model matches the value in Faber & Vassilicos (2009) ($g_{fwd}^{2D}\simeq 6.9$).