Dissecting inertial clustering and sling dynamics in high-Reynolds number particle-laden turbulence
In this work, we aim to deepen the understanding of inertial clustering and the role of sling events in high-Reynolds number ($Re$) particle-laden turbulence. To this end, we perform one-way coupled particle tracking in flow fields obtained from direct numerical simulations (DNS) of forced homogeneo...
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Zusammenfassung: | In this work, we aim to deepen the understanding of inertial clustering and
the role of sling events in high-Reynolds number ($Re$) particle-laden
turbulence. To this end, we perform one-way coupled particle tracking in flow
fields obtained from direct numerical simulations (DNS) of forced homogeneous
isotropic turbulence. Additionally, we examine the impact of filtering utilized
in large eddy simulations (LES) by applying a sharp spectral filter to the DNS
fields. Our analysis reveals that while instantaneous clustering through the
centrifuge mechanism explains clustering at early times, the path history
effect--the sampling of fluid flow along particle trajectories--becomes
important later on. The filtered fields expose small-scale fractal clustering
that cannot be predicted by the instantaneous flow field. We show that there
exists a filter-effective Stokes number that governs the degree of fractal
clustering and preferential sampling, revealing scale-similarity in the spatial
distributions and fractal dimensions. Sling events are prevalent throughout our
simulations and impose prominent patterns on the particle fields. In pursuit of
investigating the sling dynamics, we compute the relative velocity,
ensemble-averaged over proximal neighboring particles, to identify particles
undergoing caustics. As postulated in recent theories, we find that in fully
resolved, high-$Re$ turbulence, sling events occur in thin sheets of high
strain, situated between turbulent vortices. This behavior is driven by rare,
extreme events of compressive straining, manifested by fluctuations of the flow
velocity gradients that propagate back and forth the positive branch of the
Vieillefosse line. |
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DOI: | 10.48550/arxiv.2410.14549 |