Caustic formation in a non-Gaussian model for turbulent aerosols
J. Meibohm, L. Sundberg, B. Mehlig, K. Gustavsson
TL;DR
This work addresses how caustics form for inertial particles in turbulence when the fluid-velocity gradients have non-Gaussian tails. By constructing a non-Gaussian statistical model with $M$ superposed velocity fields and applying large-deviation/optimal-fluctuation theory, it shows that the caustic formation rate $\mathscr{J}$ at small $\text{St}$ is governed by the tails of the gradient distribution, while the optimal fluctuation leading to caustics remains robust and mirrors the Gaussian case, aligning with the Vieillefosse line in the $Q$-$R$ plane. The authors derive a scaling function $\mathcal{F}(a)$ with $a=[\tfrac14+\delta\lambda_{th}]/(\sqrt{M}\sigma_S\text{St})$ that collapses data across parameters, predicting $-\ln(\mathscr{J}\tau_K) \sim \text{St}^{-2}$ for $\sqrt{M}\text{St}\gg1$ and $\sim \text{St}^{-1}$ for $\sqrt{M}\text{St}\ll1$, with finite-$\text{St}$ corrections $\delta\lambda_{th}\sim \text{St}^{2/3}$. DNS results qualitatively agree on the optimal fluctuation's shape but reveal non-universal scaling due to turbulence-driven tail statistics. Overall, the paper explains why Gaussian theories mispredict DNS rates and highlights the crucial role of gradient-tail statistics in turbulent caustics, with implications for interpreting particle collisions in 3D turbulence.
Abstract
Caustics in the dynamics of heavy particles in turbulence accelerate particle collisions. The rate $\mathscr{J}$ at which these singularities form depends sensitively on the Stokes number St, the non-dimensional inertia parameter. Exact results for this sensitive dependence have been obtained using Gaussian statistical models for turbulent aerosols. However, direct numerical simulations of heavy particles in turbulence yield much larger caustic-formation rates than predicted by the Gaussian theory. In order to understand possible mechanisms explaining this difference, we analyse a non-Gaussian statistical model for caustic formation in the limit of small St. We show that at small St, $\mathscr{J}$ depends sensitively on the tails of the distribution of Lagrangian fluid-velocity gradients. This explains why different authors obtained different St-dependencies of $\mathscr{J}$ in numerical-simulation studies. The most-likely gradient fluctuation that induces caustics at small St, by contrast, is the same in the non-Gaussian and Gaussian models. Direct-numerical simulation results for particles in turbulence show that the optimal fluctuation is similar, but not identical, to that obtained by the model calculations.
