| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699275 | Chemical Geology | 2012 | 9 Pages |
The retardation of contaminants in aquifers is mainly determined by chemical reactions occurring at the solid/liquid interface. For a more detailed understanding of the molecular reactions of uranium(VI) at Al-hydroxide surfaces, the surface speciation of the radionuclide on gibbsite was studied in aqueous medium by a combined spectroscopic approach using time-resolved Attenuated Total Reflection Fourier-Transform Infrared (ATR FT-IR) and Extended X-ray Absorption Fine Structure (EXAFS) spectroscopy. For the first time, the impact of the surface morphology and of atmospherically derived carbonate on the uranyl surface speciation was systematically investigated under environmentally relevant conditions, namely in the near neutral pH range, at maximum initial U(VI) concentrations of 20 μM, and at different surface loadings. Concordantly, the formation of a monomeric binary inner-sphere surface complex is derived from vibrational and EXAFS spectroscopic data irrespective of the prevailing atmospheric condition and surface loading. In addition, from infrared spectra it was found that U(VI) surface precipitation occurs at a micromolar concentration level after a relatively short contact time in an inert gas atmosphere. However, this is circumvented by lowering the initial U(VI) concentration or in the presence of atmospheric CO2 due to the formation of ternary uranyl carbonato surface complexes. The ternary complex was identified as a dimeric inner-sphere uranyl surface species containing a bidentately coordinated carbonate ligand. The results of this work might be of relevance for a comprehensive description of the dissemination of uranium in groundwater systems.
► U(VI) surface speciation on gibbsite probed by online monitoring. ► U(VI) surface precipitation on gibbsite–water interface ► Identification of inner-sphere surface species ► Formation of ternary dimeric surface species due to presence of atmospheric CO2
