The Sorption Processes of U(VI) onto SiO 2 in the Presence of Phosphate: from Binary Surface Species to Precipitation

The ternary system containing aqueous U(VI), aqueous phosphate and solid SiO was comprehensively investigated using a batch sorption technique, in situ attenuated total reflection Fourier-transform infrared (ATR FT-IR) spectroscopy, time-resolved luminescence spectroscopy (TRLS), and surface complex...

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Published inEnvironmental science & technology Vol. 50; no. 21; pp. 11610 - 11618
Main Authors Comarmond, M Josick, Steudtner, Robin, Stockmann, Madlen, Heim, Karsten, Müller, Katharina, Brendler, Vinzenz, Payne, Timothy E, Foerstendorf, Harald
Format Journal Article
LanguageEnglish
Published United States 01.11.2016
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Summary:The ternary system containing aqueous U(VI), aqueous phosphate and solid SiO was comprehensively investigated using a batch sorption technique, in situ attenuated total reflection Fourier-transform infrared (ATR FT-IR) spectroscopy, time-resolved luminescence spectroscopy (TRLS), and surface complexation modeling (SCM). The batch sorption studies on silica gel (10 g/L) in the pH range 2.5 to 5 showed no significant increase in U(VI) uptake in the presence of phosphate at equimolar concentration of 20 μM, but significant increase in U(VI) uptake was observed for higher phosphate concentrations. In situ infrared and luminescence spectroscopic studies evidence the formation of two binary U(VI) surface species in the absence of phosphate, whereas after prolonged sorption in the presence of phosphate, the formation of a surface precipitate, most likely an autunite-like phase, is strongly suggested. From SCM, excellent fitting results were obtained exclusively considering two binary uranyl surface species and the formation of a solid uranyl phosphate phase. Ternary surface complexes were not needed to explain the data. The results of this study indicate that the sorption of U(VI) on SiO in the presence of inorganic phosphate initially involves binary surface-sorption species and evolves toward surface precipitation.
ISSN:0013-936X
1520-5851
DOI:10.1021/acs.est.6b02075