Key Laboratory of Eco-Geochemistry, Ministry of Natural Resources, National Research Center for Geoanalysis, 26 Baiwanzhuang Street, Beijing, 100037, China; Department of Chemistry, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, K1S 5B6, Canada.
Department of Earth and Environmental Sciences, University of Ottawa, ON K1N 6N5, Canada.
J Hazard Mater. 2020 Feb 15;384:121134. doi: 10.1016/j.jhazmat.2019.121134. Epub 2019 Sep 5.
The uranium speciation in humic acid (HA) and fulvic acid (FA) model solutions was investigated by diffusive gradients in thin films (DGT). A reference solution was used to normalize the DGT data from different samples. This approach was used to assess uranium DGT-available fraction (F), which was calculated from experimental data and reflect both the mobility and lability of uranium species. F decreased with increasing HA or FA concentrations, because more uranium was able to bind the strong binding sites of HA or FA. When copper was spiked, F increased due to the competition between copper and uranium. In HA model solutions, an increase of ionic strength could increase F, and when pH was greater than 7, F increased significantly. The DGT uptake factor (φ), which can be obtained from data fitting, is the ratio of the product of diffusion coefficient and lability degree of the unknown sample to that of the reference solution. In U-HA-NaHCO solutions, UO(CO) had a relatively high φ value and might be the most DGT-available species. This approach allows the comparison of DGT data from different samples, and combining with a data fitting procedure, it can be used to investigate the distribution of metal species.
采用薄膜扩散梯度技术(DGT)研究了腐殖酸(HA)和富里酸(FA)模型溶液中的铀形态。参考溶液用于归一化来自不同样品的 DGT 数据。该方法用于评估铀 DGT 有效分数(F),它是根据实验数据计算得出的,反映了铀物种的迁移性和不稳定性。F 值随着 HA 或 FA 浓度的增加而降低,因为更多的铀能够与 HA 或 FA 的强结合位点结合。当添加铜时,由于铜和铀之间的竞争,F 值增加。在 HA 模型溶液中,离子强度的增加可以增加 F 值,当 pH 值大于 7 时,F 值显著增加。可以从数据拟合中获得的 DGT 吸收因子(φ)是未知样品的扩散系数和不稳定性的乘积与参考溶液的比值。在 U-HA-NaHCO 溶液中,UO(CO)具有相对较高的φ值,可能是最 DGT 有效的物种。该方法允许比较不同样品的 DGT 数据,并结合数据拟合程序,用于研究金属物种的分布。