Answers are grounded in this paper and cite their sources.
In the current study, a dynamic layer freeze desalination system is simulated numerically. The computational domain is a two-dimensional rectangular channel which contains inlet and outlet flows, and the simulation is performed using computational fluid dynamics. A pre-concentrated mixture is considered as the feed solution with an initial temperature and concentration of 257 K and 0.2 kg/kg, respectively. In this work, since the simulation parameters such as temperature and species mass fraction have high importance across the entire domain, the k–ω shear stress transport turbulence model was selected. A parametric study on the effect of the heat flux of the cold wall on the ice salinity and desalination rate is performed using three cases with heat fluxes of −1000, −1500, and −3000 Wm−2. It is observed that the ice generation speed in the case with a heat flux of −3000 Wm−2 is 3.28 times greater compared to the case with −1000 Wm−2 and its desalination rate is only 2.59% lower. The effect of the inlet velocity on the mentioned parameters is also investigated. It is observed that the cases with turbulent flow have approximately 19% and 23% lower ice salinity compared to the case with laminar flow.
No takes yet. Share an insight, caveat, or question.
Moradian et al. (2024) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: