Modelling the reaction of uranium with carboxylic groups on surfaces through mono- and multi- dentate surface complexes on the basis of pH and redox potential

Steven McGowan, Claude Degueldre, Farid Aiouache
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Abstract

An analytical expression is proposed to simulate effects of pH and redox potential (E) on the sorption of uranium onto bioorganic model particles in saline or other aquatic environments. The elaborated expression is intended to avoid use of the classical approach of sorption which relies on experimental data and empirical models. The goal is to produce an expression that provides a distribution coefficient (Kd e.g. mL g−1) as function of pH, E and ligand concentration (through complex formation in solution) by applying a surface complexation model on one type of mono-dentate surface sites> (SuOH) as well as utilizing multi-dentate surface sites> (SuOH)c. The formulation of the worked out expression makes use of correlations between the surface complexation and hydrolysis constants for all species and sorption sites. The model was applied to the sorption of uranium onto bioorganic sites with and without carbonates in solution e.g. Log Kd: + 2.75 at pH 8 for 2 sites per nm2. The calculated distribution coefficients were found very sensitive to the presence of carbonates, e.g. Log Kd: − 7.0 at pH 8 for 2 × 10−3 M total carbonate. The potential reduction of uranium U(VI) and its complexes (carbonates) which are the primary stable species in surface waters, to U(IV) during sorption was simulated in association with a decrease in the redox potential and was found generally below the redox stability limits of water. The calculated distribution coefficient values were validated by the values reported in literature for the sorption of uranium onto specific adsorbents. The investigated simulations are also applicable to the sorption of other redox sensitive elements.

在pH值和氧化还原电位的基础上,通过单齿和多齿表面配合物模拟铀与表面羧基的反应
提出了一个分析表达式来模拟pH和氧化还原电位(E)对盐水或其他水生环境中生物有机模型颗粒吸附铀的影响。详细的表述旨在避免使用依赖于实验数据和经验模型的经典吸附方法。目标是通过在一种类型的单齿表面位点上应用表面络合模型来产生提供作为pH、e和配体浓度(通过在溶液中形成络合物)的函数的分布系数(Kd,例如mL g−1)的表达式>;(SuOH)以及利用多齿表面位点>;(SuOH)c。计算出的表达式的公式利用了所有物种和吸附位点的表面络合和水解常数之间的相关性。该模型应用于在溶液中含有和不含有碳酸盐的生物有机位点上吸附铀,例如在pH 8下,对数Kd:+2.75,每nm2吸附2个位点。计算的分布系数对碳酸盐的存在非常敏感,例如,对于2×10−3 M的总碳酸盐,在pH 8时的对数Kd:−7.0。铀U(VI)及其络合物(碳酸盐)是地表水中的主要稳定物种,在吸附过程中被模拟为U(IV)的电势还原与氧化还原电势的降低有关,并且通常低于水的氧化还原稳定性极限。计算的分布系数值通过文献中报道的铀在特定吸附剂上的吸附值进行了验证。所研究的模拟也适用于其他氧化还原敏感元素的吸附。
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