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首页> 外文期刊>Mineralogical Magazine >Uranium and technetium interactions with wustite [Fe1-xO] and portlandite [Ca(OH)(2)] surfaces under geological disposal facility conditions
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Uranium and technetium interactions with wustite [Fe1-xO] and portlandite [Ca(OH)(2)] surfaces under geological disposal facility conditions

机译:地质处置设施条件下铀与net与辉铁矿[Fe1-xO]和硅酸盐[Ca(OH)(2)]表面的相互作用

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Iron oxides resulting from the corrosion of large quantities of steel that are planned to be installed throughout a deep geological disposal facility (GDF) are expected to be one of the key surfaces of interest for controlling radionuclide behaviour under disposal conditions. Over the lengthy timescales associated with a GDF, the system is expected to become anoxic so that reduced Fe(II) phases will dominate. Batch experiments have therefore been completed in order to investigate how a model reduced Fe-oxide surface (wustite, Fe1-xO) alters as a function of exposure to aqueous solutions with compositions representative of conditions expected within a GDF. Additional experiments were performed to constrain the effect that highly alkaline solutions (up to pH 13) have on the adsorption behaviour of the uranyl (UO22+) ion onto the surfaces of both wustite and portlandite [Ca(OH)(2); representative of the expected cementitious phases]. Surface co-ordination chemistry and speciation were determined by ex situ X-ray absorption spectroscopy measurements (both X-ray absorption near-edge structure analysis (XANES) and extended X-ray absorption fine structure analysis (EXAFS)). Diffraction, elemental analysis and XANES showed that the bulk solid composition and Fe oxidation state remained relatively unaltered over the time frame of these experiments (120 h), although under alkaline conditions possible surface hydroxylation is observed, due presumably to the formation of surface hydroxyl complexes. The surface morphology, however, is altered significantly with a large degree of roughening and an observed decrease in the average particle size. Reduction of U(VI) to U(IV) occurs during adsorption in almost all cases and this is interpreted to indicate that wustite may be an effective reductant of U during surface adsorption. This work also shows that increasing the carbonate concentration in reactant solutions dramatically decreases the adsorption coefficients for U on both wustite and portlandite, consistent with U speciation and surface reactivity determined in other studies. Finally, the EXAFS results include new details about exactly how U bonds to this metal oxide surface.
机译:计划在整个深部地质处置设施(GDF)中安装的大量钢的腐蚀产生的氧化铁,有望成为控制处置条件下放射性核素行为的主要关注表面之一。在与GDF相关的漫长时间范围内,预计该系统将变得缺氧,因此还原的Fe(II)相将占主导地位。因此,已经完成了批量实验,以研究模型还原的Fe氧化物表面(铁矾,Fe1-xO)如何随着暴露于水溶液而变化,其组成代表GDF内预期的条件。为了限制高碱性溶液(pH值高达13)对铀酰(UO22 +)离子在钙铁矿和钙铁矿[Ca(OH)(2)的表面上的吸附行为的影响,还进行了其他实验。预期的胶结阶段的代表]。通过异位X射线吸收光谱测量(X射线吸收近边缘结构分析(XANES)和扩展X射线吸收精细结构分析(EXAFS))确定表面配位化学和形态。衍射,元素分析和XANES表明,在这些实验的时间范围内(120小时),固相组成和铁的氧化态保持相对不变,尽管在碱性条件下可能观察到表面羟基化,可能是由于表面羟基络合物的形成。但是,表面形态会随着粗糙化程度的增加而显着改变,并且观察到平均粒径的减小。在几乎所有情况下,U(VI)还原为U(IV)的过程均被解释为表明,在表面吸附过程中,钙长石可能是U的有效还原剂。这项工作还表明,增加反应物溶液中的碳酸盐浓度会极大地降低U在钙铁矿和硅酸盐上的吸附系数,这与其他研究中确定的U形态和表面反应性一致。最后,EXAFS结果包括有关U如何与该金属氧化物表面精确结合的新细节。

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