U(VI) mitigation via forward osmosis: Elucidation of retention mechanisms and co-ion effects

Uranium (U) is a chemical and radioactive toxic contaminant affecting many groundwater systems. The focus of this study was to evaluate the suitability of forward osmosis (FO) for uranium rejection from contaminated groundwater under field-relevant conditions. Laboratory experiments with aqueous solution containing uranium were performed with FO membrane to understand the uranium rejection mechanism under varied pH, draw solution concentration, and presence of co-ions. Further, experiments were performed with U-contaminated field groundwater. Results of the hydrogeochemcial modelling using PHREEQC indicated that the rejection mechanism of uranium was highly dependent on aqueous speciation. Uranium rejection was maximum at alkaline pH with ca. 99% rejection due to charge-based interactions between membrane and dominant uranyl complexes. The results of the co-ion study indicated that nitrate and phosphate ions decrease uranium rejection. Whereas, bicarbonates, calcium, and magnesium ions concentrated uranium in feed solution. Further, the uranium adsorption onto the membrane surface primarily depended on pH of the aqueous solution with maximum adsorption at pH 5.5. Our results show that the World Health Organization's drinking water guideline value of 30 μgL−1 for U could be achieved via FO process in field groundwater containing low dissolved solids. [Display omitted] •Uranium mitigation in field relevant (Na+ - HCO3-) low TDS (< 500 mgL−1) groundwater.•Uranium rejection was maximum at alkaline pH (i.e. 99.2% for pH 10.0).•Co-ions viz. nitrate and phosphate reduce uranium rejection.•Bicarbonates, calcium, and magnesium lead to concentrating uranium in feed solution.•WHO's drinking water guidelines were achieved in contaminated groundwater using FO.