Preferential concentration by mechanically-driven turbulence in the two-fluid formalism
arXiv:2103.08121 · doi:10.1103/PhysRevFluids.6.104303
Abstract
Preferential concentration is thought to play a key role in promoting particle growth, which is crucial to processes such as warm rain formation in clouds, planet formation, and industrial sprays. In this work, we investigate preferential concentration using 3D Direct Numerical Simulations adopting the Eulerian-Eulerian two-fluid approach, where the particles are treated as a continuum field with its own momentum and mass conservation laws. We consider particles with Stokes number in moderately turbulent flows with fluid Reynolds number . In our previous work (Nasab & Garaud, Physical Review Fluids. doi: 10.1103/PhysRevFluids.5.114308, 2020), we established scaling laws to predict maximum and typical particle concentration enhancements in the context of the particle-driven convective instability. Here we verify that the same results apply when turbulence is externally driven, extending the relevance of our model to a wider class of particle-laden flows. We find in particular that (i) the maximum particle concentration enhancement above the mean scales as , where is the rms fluid velocity, is the particle stopping time, and is the assumed particle diffusivity from the two-fluid equations; (ii) the typical particle concentration enhancement over the mean scales as ; and (iii) the probability distribution function of the particle concentration enhancement over the mean has an exponential tail whose slope scales like . We conclude by discussing the caveats of our model and its implications in a relevant cloud application.
arXiv comment28 pages, 12 figures
References in corpus (10)
- Dust Evolution and the Formation of Planetesimals
- Numerically determined transport laws for fingering ("thermohaline") convection in astrophysics
- Dynamics of fingering convection I: Small-scale fluxes and large-scale instabilities
- Dynamics of fingering convection II: The formation of thermohaline staircases
- Bifurcations in a Quasi-Two-Dimensional Kolmogorov-Like Flow
- A New Model for Mixing By Double-Diffusive Convection (Semi-Convection). III. Thermal and Compositional Transport Through Non-Layered ODDC
- The stability of stratified spatially periodic shear flows at low Péclet number
- Turbulent transport in a strongly stratified forced shear layer with thermal diffusion
- Sub critical transition to turbulence in three-dimensional Kolmogorov flow
- Preferential concentration in the particle-induced convective instability