“…While the aforementioned studies focused on the scalar fields in a continuous phase, physicochemical hydrodynamics following turbulent mixing can also lead to precipitation of a dissolved component into a dispersed phase, which undergoes oversaturation, droplet nucleation, droplet growth, and sometimes also shrinkage due to evaporation (Marié et al, 2014;Li et al, 2023) in the turbulent flow. Such precipitation processes include aerosol formation through condensation (Lesniewski and Friedlander, 1998;Zhou et al, 2014;Ng et al, 2021;Li et al, 2023), soot formation in turbulent combustion (Bisetti et al, 2012;Attili et al, 2014a), particle formation by chemical reaction (Schikarski et al, 2022;Tang et al, 2022), and droplet formation upon solvent exchange (Lee et al, 2022). Lesniewski and Friedlander (1998) experimentally studied dibutyl-phthalate (DBP) aerosol formation in a turbulent jet flow, indicating that with high DBP vapor concentration, the droplets nucleate both within the initial shear layer and in the downstream turbulent region.…”