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Identification Of Uranyl Surface Complexes On Ferrihydrite: Advanced Exafs Data Analysis And Cd-music Modeling

机译:亚铁酸盐上铀酰表面复合物的鉴定:高级exafs数据分析和Cd音乐模型

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Previous spectroscopic research suggested that uranium(Ⅵ) adsorption to iron oxides is dominated by ternary uranyl-carbonate surface complexes across an unexpectedly wide pH range. Formation of such complexes would have a significant impact on the sorption behavior and mobility of uranium in aqueous environments. We therefore reinvestigated the identity and structural coordination of uranyl sorption complexes using a combination of U LⅢ-edge extended X-ray absorption fine structure (EXAFS) spectroscopy and iterative transformation factor analysis, which enhances the resolution in comparison to conventional EXAFS analysis. A range of conditions (pH, C0_2 partial pressure, ionic strength) made it possible to quantify the variations in surface speciation. In the resulting set of spectral data (N= 11) the variance is explained by only two components, which represent two structurally different types of surface complexes: (1) a binary uranyl surface complex with a bidentate coordination to edges of Fe(0,0H)_6 octahedra and (2) a uranyl triscarbonato surface complex where one carbonate ion bridges uranyl to the surface. This ternary type B complex differs from a type A complex where uranyl is directly attached to surface atoms and carbonate is bridged by uranyl to the surface. Both surface complexes agree qualitatively and quantitatively with predictions by a charge distribution (CD) model. According to this model the edge-sharing uranyl complex has equatorial ligands (-OH_2, -OH, or one -C0_3 group) that point away from the surface. The monodentate uranyl triscarbonato surface complex (type B) is relevant only at high pH and elevated PCO_2. At these conditions, however, it is responsible for significant uranyl sorption, whereas standard models would predict only weak sorption. This paper presents the first spectroscopic evidence of this ternary surface complex, which has significant implications for immobilization of uranyl in carbonate-rich aqueous environments.
机译:先前的光谱研究表明,铀(Ⅵ)在氧化铁上的吸附主要是在一个意想不到的宽pH范围内由三重铀酰-碳酸盐表面配合物引起的。这种配合物的形成将对铀在水环境中的吸附行为和迁移率产生重大影响。因此,我们结合使用了ULⅢ边缘扩展X射线吸收精细结构(EXAFS)光谱学和迭代转换因子分析技术,对铀酰吸附复合物的身份和结构配比进行了重新研究,与传统的EXAFS分析相比,该方法提高了分离度。一系列条件(pH,CO 2分压,离子强度)可以量化表面形态的变化。在所得的一组光谱数据(N = 11)中,仅用两个分量来解释方差,这两个分量代表两种结构上不同的表面复合物:(1)具有与Fe(0, 0H)_6八面体和(2)铀酰三碳酸盐表面配合物,其中一个碳酸根离子将铀酰桥接到表面上。这种三元B型络合物与A型络合物不同,在该A型络合物中,铀酰直接附着于表面原子,而碳酸盐则通过铀酰桥接于表面。两种表面复合物在质量和数量上均与电荷分布(CD)模型的预测一致。根据该模型,边缘共享的铀酰复合物具有指向远离表面的赤道配体(-OH_2,-OH或一个-C0_3基团)。单齿铀酰三碳酸盐表面复合物(B型)仅在高pH和升高的PCO_2下才有意义。然而,在这些条件下,它负责显着的铀酰吸附,而标准模型只能预测弱的吸附。本文介绍了这种三元表面复合物的第一个光谱学证据,这对于在富含碳酸盐的水性环境中将铀酰固定化具有重要意义。

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