Related Experiment Video
Updated: May 5, 2026

Sulfate Separation by Selective Crystallization with a Bis-iminoguanidinium Ligand
Published on: September 8, 2016
Salt recovery from a reverse osmosis brine by eutectic freeze crystallization method for waste brine management
Amira Nemmour1, Hongtao Zhang1, Khadije El Kadi1
1Department of Mechanical and Nuclear Engineering, Center for Membranes and Advanced Water Technology, Khalifa University, Abu Dhabi, United Arab Emirates.
None:
Freeze desalination (FD) is a promising method for the treatment of desalination brines due to its ability to recover clean water and solid salts with a low energy compared to traditional techniques. In this work, eutectic freeze crystallization (EFC) for a reverse osmosis brine was conducted to investigate the feasibility of using EFC for the recovery/removal of different salts such as sodium sulfate (Na2SO4), magnesium sulfate (MgSO4), and sodium chloride (NaCl). An indirect freeze crystallization experiment was conducted on the effect of temperature reduction on multi-component ions of the brine. Additionally, thermodynamic modeling of the brine was developed in order to simulate the experimental setup. Subsequently, a comparison with the experiment was performed to assess the developed theoretical model. Thermal analysis revealed the production of ice and salt crystals like mirabilite (NaSO4.10H2O) and hydro-halite (NaCl.10H2O). The FD achieved high water recovery of approximately 88% with recovered solid salts of NaSO4.10H2O and NaCl.10H2O with yields of 16.7g/L and 79.4 g/L, respectively. Ionic analysis compared with theoretical modeling suggests that components such as sodium, magnesium, and chloride might be recovered as solid hydrates from brine with considerable quantities. The study gives an outlook of the step towards achieving zero liquid discharge resulting in high water recovery, effective use of salt resources as well as brine volume reduction.
Related Concept Videos
Freezing Point Depression and Boiling Point Elevation
The boiling point of a liquid is the temperature at which its vapor pressure is equal to ambient atmospheric pressure. Since the vapor pressure of a solution is lowered due to the presence of nonvolatile solutes, it stands to reason that the solution’s boiling point will subsequently be increased. Vapor pressure increases with temperature, and so a solution will require a higher temperature than will pure solvent to achieve any given vapor pressure, including one...
Osmosis and Osmotic Pressure of Solutions
Recrystallization: Solid–Solution Equilibria
Precipitation and Co-precipitation
Freezing Point Depression and Boiling Point Elevation

