Homogeneous turbophoresis of heavy inertial particles in turbulent flow
J\'er\'emie Bec, Robin Vall\'ee

TL;DR
This paper demonstrates that turbophoresis significantly influences inertial particle distributions even in statistically homogeneous turbulent flows, through a detailed analysis of particle dynamics and scale-dependent effects.
Contribution
It introduces a novel framework linking turbulence fluctuations to particle inhomogeneities via a scale-dependent Péclet number and multifractal energy dissipation statistics.
Findings
Turbophoresis affects particle distribution in homogeneous turbulence.
The scale-dependent Péclet number scales as $l^ ext{delta}/\tau_{\rm p}$ with $\delta\approx 0.84$.
Void sizes follow a power-law distribution with exponent approaching 2 as $Pe_l\to 0$.
Abstract
Heavy particles suspended in turbulent flow possess inertia and are ejected from violent vortical structures by centrifugal forces. Once piled up along particle paths, this small-scale mechanism leads to an effective large-scale drift. This phenomenon, known as turbophoresis, causes particles to leave highly turbulent regions and migrate towards calmer regions, explaining why particles transported by non-homogeneous flows tend to concentrate near the minima of turbulent kinetic energy. It is demonstrated here that turbophoretic effects are just as crucial in statistically homogeneous flows. Although the average turbulent activity is uniform, instantaneous spatial fluctuations are responsible for inertial-range inhomogeneities in the particle distribution. Direct numerical simulations are used to probe particle accelerations, specifically how they correlate to local turbulent activity,…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsParticle Dynamics in Fluid Flows · Aeolian processes and effects · Granular flow and fluidized beds
