Caustics in turbulent aerosols form along the Vieillefosse line at weak particle inertia

TL;DR

This paper analyzes how caustics form in turbulent aerosols at weak particle inertia, revealing that they occur along the Vieillefosse line due to large fluid-velocity gradient excursions, with implications for collision rates.

Contribution

It introduces a statistical model predicting that caustics form along the Vieillefosse line via an optimal fluctuation, advancing understanding of particle clustering in turbulence.

Findings

Caustics form along the Vieillefosse line in the invariant plane.

Large strain-dominated excursions induce caustics at weak inertia.

Optimal fluctuations dominate caustic formation even at moderate inertia.

Abstract

Caustic singularities of the spatial distribution of particles in turbulent aerosols enhance collision rates and accelerate coagulation. Here we investigate how and where caustics form at weak particle inertia, by analysing a three-dimensional Gaussian statistical model for turbulent aerosols in the persistent limit, where the flow varies slowly compared with the particle relaxation time. In this case, correlations between particle- and fluid-velocity gradients are strong, and caustics are induced by large, strain-dominated excursions of the fluid-velocity gradients. These excursions must cross a characteristic threshold in the plane spanned by the invariants $Q$ and $R$ of the fluid-velocity gradients. Our method predicts that the most likely way to reach this threshold is by a unique ``optimal fluctuation'' that propagates along the Vieillefosse line, $27R^2/4 +Q^3=0$. We determine the shape of the optimal fluctuation as a function of time and show that it is dominant in numerical statistical-model simulations even for moderate particle inertia.