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Influence on Uranium(Ⅵ) migration in soil by iron and manganese salts of humic acid: Mechanism and behavior

机译:腐殖酸铁锰盐对土壤中铀(Ⅵ)迁移的影响:机理与行为

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Soil contains large amounts of humic acid (HA), iron ions and manganese ions, all of which affect U(VI) migration in the soil. HA interacts with iron and manganese ions to form HA salts (called HA-Fe and HA-Mn in this paper); however, the effects of HA-Fe and HA-Mn on the migration of U(VI) is not fully understood. In this study, HA-Fe and HA-Mn were compounded by HA interactions with ferric chloride hexahydrate and manganese chloride tetrahydrate, respectively. The influence of HA, HA-Fe and HA-Mn on U(VI) immobilization and migration was investigated by bath adsorption experiments and adsorption-desorption experiments using soil columns. The results showed that the presence of HA, HA-Fe and HA-Mn retarded the migration of U(VI) in soil. Supported by X-ray photoelectron spectroscopy (XPS) and BCR sequential extraction analyses, a plausible explanation for the retardation was that HA-Fe and HA-Mn could reduce hexavalent uranium to stable tetravalent uranium and increase the specific gravity of Fe/Mn oxide-bound uranium and organic/sulfide-bound uranium, which made it difficult for them to longitudinally migrate in soil. Scanning electron microscopy (SEM), Fourier transform infrared (FTIR) spectroscopy, X-ray diffraction (XRD), and surface area and pore size analyses indicated that the complex formed between the hydroxyl, amino and carboxyl groups of HA-Fe and U(VI) increased the crystallinity of HA-Fe. The reaction between U(VI) and the hydroxyl, amino, aldehyde, keto and chlorine-containing groups of HA-Mn had no effect on the crystallinity of HA-Mn. Notably, the column desorption experiment found that the U(VI) immobilized in the soil remigrated under the effect of rain leaching, and acid rain promoted uranium remigration better than neutral rain. The findings provide some guidance for the decommissioning disposal of uranium contaminated site and it's risk assessments. (C) 2019 Elsevier Ltd. All rights reserved.
机译:土壤中含有大量的腐殖酸(HA),铁离子和锰离子,所有这些都会影响U(VI)在土壤中的迁移。 HA与铁和锰离子相互作用形成HA盐(在本文中称为HA-Fe和HA-Mn)。然而,人们尚未完全了解HA-Fe和HA-Mn对U(VI)迁移的影响。在这项研究中,HA-Fe和HA-Mn分别通过HA与六水合氯化铁和四水合氯化锰的相互作用而复合。通过浴吸附实验和土壤柱吸附-解吸实验研究了HA,HA-Fe和HA-Mn对U(VI)固定化和迁移的影响。结果表明,HA,HA-Fe和HA-Mn的存在会阻碍U(VI)在土壤中的迁移。在X射线光电子能谱(XPS)和BCR顺序萃取分析的支持下,延迟的合理解释是HA-Fe和HA-Mn可以将六价铀还原为稳定的四价铀并增加Fe / Mn氧化物的比重,结合铀和有机/硫化物结合铀,这使它们难以在土壤中纵向迁移。扫描电子显微镜(SEM),傅立叶变换红外(FTIR)光谱,X射线衍射(XRD)以及表面积和孔径分析表明,HA-Fe和U()的羟基,氨基和羧基之间形成了络合物VI)增加了HA-Fe的结晶度。 U(VI)与HA-Mn的羟基,氨基,醛,酮和氯基之间的反应对HA-Mn的结晶度没有影响。值得注意的是,柱解吸实验发现,固定在土壤中的U(VI)在雨淋作用下迁移了,而酸雨比中性雨更能促进铀的迁移。研究结果为铀污染场地的退役处置及其风险评估提供了一些指导。 (C)2019 Elsevier Ltd.保留所有权利。

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