Abstract Adsorption of uranium (U) from real mine contaminated water (U 1.652 mg/L) by phosphate rock apatite (PRA) was investigated in the batch experiment and flow column test system. In batch… Click to show full abstract
Abstract Adsorption of uranium (U) from real mine contaminated water (U 1.652 mg/L) by phosphate rock apatite (PRA) was investigated in the batch experiment and flow column test system. In batch experiment, the equilibrium adsorption amount is 0.1133 mg/g with the highest uranium removal efficiency of 76.89% under the ratio of solid to liquid (1:100) in 15 h. And the pH of wastewater became neutral (pH 7.51) from acidic (pH 3.88) after adsorption equilibrium. The saturated adsorption amount (0.2021 mg/g) in batch experiment is higher than the maximum accumulative adsorption amount (0.0684 mg/g) in column experiment. Langmuir model and pseudo-second order kinetic model are fitted well and, indicating that PRA is a favorable adsorbent with monolayer coverage and a chemisorption for uranium. Moreover, the surface morphology of the adsorbent by SEM confirmed the surface changes after uranium adsorption. XRD spectra showed that two new mineral phase of Metaankoleite [K(UO 2 )(PO 4 )·3H 2 O], Chernikovite [H 2 (UO 2 ) 2 (PO 4 ) 2 ·8H 2 O] have been generated on PRA after uranium adsorption, but which were trace for relatively low uranium concentration in tested polluted water. In addition, the FT-IR spectra results confirmed the uranium in contaminated water was adsorbed onto the PRA in the form of (O = U = O) 2+ with the participation of the PO 4 3– in binding of it.
               
Click one of the above tabs to view related content.