Vandenborre Johan, Drot Romuald, Simoni Eric
Institut de Physique Nucléaire, IPNO UMR 7808 CNRS-Université Paris-Sud-Orsay, 15 rue Georges Clémenceau, 91406 Orsay, France.
Inorg Chem. 2007 Feb 19;46(4):1291-6. doi: 10.1021/ic061783d.
This paper is devoted to the study of the mechanisms of interaction between uranyl ion and rutile TiO2. Among the radionuclides of interest, U(VI) can be considered as a model of the radionuclides oxo-cations. The substrate under study here is the rutile titanium dioxide (TiO2) which is an interesting candidate as a methodological solid since it can be easily found as powder and as manufactured single crystals. This material presents also a wide domain of stability as a function of pH. Then, it allows the study of the retention processes on well-defined crystallographic planes, which can lead to a better understanding of the surface reaction mechanisms. Moreover, it is well-established that the (110) crystallographic orientation is dominating the surface chemistry of the rutile powder. Therefore, the spectroscopic results obtained for the U(VI)/rutile (110) system and other relevant crystallographic orientations were used to have some insight on the nature of the uranium surface complexes formed on rutile powder. This goal was achieved by using time-resolved laser-induced fluorescence spectroscopy (TRLFS) which allows the investigation, at a molecular scale, of the nature of the reactive surface sites as well as the surface species. For rutile surfaces, oxygen atoms can be 3-fold, 2-fold (bridging oxygens), or single-fold (top oxygens) coordinated to titanium atoms. However, among these three types of surface oxygen atoms, the 3-fold coordinated ones are not reactive toward water molecules or aqueous metallic cations. This study led to conclude on the presence of two uranium(VI) surface complexes: the first one corresponds to the sorption of aquo UO22+ ion sorbed on two bridging oxygen atoms, while the second one, which is favored at higher surface coverages, corresponds to the retention of UO22+ by one bridging and one top oxygen atom. Thus, the approach presented in this paper allows the establishment of experimental constraints that have to be taken into account in the modeling of the sorption mechanisms.
本文致力于研究铀酰离子与金红石型TiO₂之间的相互作用机制。在感兴趣的放射性核素中,U(VI)可被视为放射性核素含氧阳离子的一个模型。此处所研究的底物是金红石型二氧化钛(TiO₂),它作为一种方法学上的固体是一个有趣的候选物,因为它既可以很容易地以粉末形式获得,也可以是制成的单晶。这种材料作为pH的函数还呈现出广泛的稳定性范围。然后,它允许对明确的晶面上的保留过程进行研究,这有助于更好地理解表面反应机制。此外,众所周知,(110)晶向主导着金红石粉末的表面化学。因此,针对U(VI)/金红石(110)体系以及其他相关晶向所获得的光谱结果被用于深入了解在金红石粉末上形成的铀表面配合物的性质。通过使用时间分辨激光诱导荧光光谱(TRLFS)实现了这一目标,该技术能够在分子尺度上研究反应性表面位点以及表面物种的性质。对于金红石表面,氧原子可以与钛原子形成三配位、双配位(桥连氧)或单配位(顶氧)。然而,在这三种类型的表面氧原子中,三配位的那些对水分子或水基金属阳离子没有反应性。这项研究得出结论,存在两种铀(VI)表面配合物:第一种对应于水合UO₂²⁺离子吸附在两个桥连氧原子上,而第二种在较高表面覆盖率时更有利,对应于UO₂²⁺被一个桥连氧原子和一个顶氧原子保留。因此,本文所提出的方法允许建立在吸附机制建模中必须考虑的实验约束条件。