Reactive transport of uranium(VI) and phosphate in a goethite-coated sand column: An experimental study

• Published in: Chemosphere (Oxford) 2007-07, Vol.68 (7), p.1218-1223
• Main Authors: Cheng, Tao, Barnett, Mark O., Roden, Eric E., Zhuang, Jinling
• Format: Article
• Language: English
• Subjects: Adsorption/desorption on goethite; Batch and column experiments; Kinetics; Phosphate; Solute transport; Uranium(VI)
• ISSN: 0045-6535; 1879-1298
• DOI: 10.1016/j.chemosphere.2007.01.063

The migration of uranium(VI) in subsurface environments is strongly influenced by its adsorption/desorption reactions at the solid/solution interface. Phosphate is often present in subsurface systems and was shown to significantly affect U(VI) adsorption in previous batch experiments. In this study, column experiments were conducted to investigate the effects of phosphate on U(VI) adsorption and transport under flow conditions. The adsorption of U(VI) and phosphate was very low on pure quartz sand with negligible effects on U(VI) and phosphate transport. However, U(VI) and phosphate transport was retarded in a column packed with goethite-coated sand. The presence of phosphate, either as a co-solute with U(VI) or pre-adsorbed, greatly increased U(VI) adsorption and retardation. U(VI) and phosphate adsorption in our column experiments were rate-limited, and the adsorption of U(VI) and phosphate was not reversible, with kinetic limitations more pronounced for desorption than for adsorption. This study demonstrated the importance of phosphate in controlling U(VI) mobility in subsurface environments and helped illustrate some phenomena potentially applicable to U(VI) adsorption and transport in natural systems, especially where U(VI) adsorption is rate-limited.