Understanding particle transport and deposition in wall-bounded turbulent flows is critical for numerous industrial and environmental applications. In this study, we investigate the dispersion and deposition dynamics of small aerosol and hydrosol particles in a turbulent channel flow at a friction Reynolds number of using point-particle direct numerical simulations (PP–DNS). By decomposing the particle acceleration into drag, lift, pressure gradient, virtual mass, and Basset history components, we assess the relative influence of each acceleration across a range of particle sizes and density ratios (aerosol and hydrosol) in an upward flow motion, i.e. opposite direction of gravity. Our results show that while drag dominates the particle dynamics particularly for aerosols, lift becomes increasingly important with rising particle size. The Basset history, pressure gradient and virtual mass accelerations have only a negligible contribution to the total acceleration. Regarding hydrosol, pressure gradient has a constant contribution to particle acceleration, largely independent of particle size, where the effect of virtual mass decreases with the increase of particle size. On the other hand, Basset history acceleration, shows size-dependent behavior. For small particles, the Basset history acceleration contributes to the particle acceleration with a magnitude comparable to the pressure gradient. As the particle size increases, this contribution decreases, and its dynamics changes once the hydrosol particle size approaches the Kolmogorov scale. Additionally, both pressure gradient and Basset history have significant input on deposition for hydrosol particles comparable to Kolmogorov length scale.
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