Transport and deposition of dilute microparticles in turbulent thermal convection

TL;DR

This study investigates how dilute microparticles behave in turbulent thermal convection, revealing their distribution, clustering, sedimentation, and deposition patterns through detailed numerical simulations.

Contribution

It provides new insights into particle transport, clustering, and deposition mechanisms in turbulent Rayleigh-Bénard convection, including phase diagrams of deposition states.

Findings

Particles with low Stokes number are homogeneously distributed.

Particles with intermediate Stokes number tend to cluster into bands.

Larger particles sediment quickly and preferentially deposit on vertical walls.

Abstract

We analyze the transport and deposition behavior of dilute microparticles in turbulent Rayleigh-B\'enard convection. Two-dimensional direct numerical simulations were carried out for the Rayleigh number ($Ra$) of $10^{8}$ and the Prandtl number ($Pr$) of 0.71 (corresponding to the working fluids of air). The Lagrangian point particle model was used to describe the motion of microparticles in the turbulence. Our results show that the suspended particles are homogeneously distributed in the turbulence for the Stokes number ($St$) less than $10^{-3}$, and they tend to cluster into bands for $10^{-3} \lesssim St \lesssim 10^{-2}$. At even larger $St$, the microparticles will quickly sediment in the convection. We also calculate the mean-square displacement (MSD) of the particle's trajectories. At short time intervals, the MSD exhibits a ballistic regime, and it is isotropic in vertical and lateral directions; at longer time intervals, the MSD reflects a confined motion for the particles, and it is anisotropic in different directions. We further obtained a phase diagram of the particle deposition positions on the wall, and we identified three deposition states depending on the particle's density and diameter. An interesting finding is that the dispersed particles preferred to deposit on the vertical wall where the hot plumes arise, which is verified by tilting the cell and altering the rotation direction of the large-scale circulation.