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一种综合胶体分级方法应用于贫铀污染场地孔隙水铀-腐殖质相互作用的表征。

An integrated colloid fractionation approach applied to the characterisation of porewater uranium-humic interactions at a depleted uranium contaminated site.

作者信息

Graham Margaret C, Oliver Ian W, Mackenzie Angus B, Ellam Robert M, Farmer John G

机构信息

School of GeoSciences, Crew Building, University of Edinburgh, The King's Buildings, West Mains Road, Edinburgh, EH9 3JN, United Kingdom.

出版信息

Sci Total Environ. 2008 Oct 1;404(1):207-17. doi: 10.1016/j.scitotenv.2008.05.042. Epub 2008 Jul 16.

DOI:10.1016/j.scitotenv.2008.05.042
PMID:18635249
Abstract

Methods for the fractionation of aquatic colloids require careful application to ensure efficient, accurate and reproducible separations. This paper describes the novel combination of mild colloidal fractionation and characterisation methods, namely centrifugal ultrafiltration, gel electrophoresis and gel filtration along with spectroscopic (UV-visible) and elemental (Inductively Coupled Plasma-Optical Emission Spectroscopy, Inductively Coupled Plasma-Mass Spectrometry) analysis, an approach which produced highly consistent results, providing improved confidence in these methods. Application to the study of the colloidal and dissolved components of soil porewaters from one soil at a depleted uranium (DU)-contaminated site revealed uranium (U) associations with both large (100 kDa-0.2 microm) and small (3-30 kDa) humic colloids. For a nearby soil with lower organic matter content, however, association with large (100 kDa-0.2 microm) iron (Fe)-aluminium (Al) colloids in addition to an association with small (3-30 kDa) humic colloids was observed. The integrated colloid fractionation approach presented herein can now be applied with confidence to investigate U and indeed other trace metal migration in soil and aquatic systems.

摘要

水胶体分级分离方法需要谨慎应用,以确保实现高效、准确且可重复的分离。本文描述了温和的胶体分级分离与表征方法的新颖组合,即离心超滤、凝胶电泳和凝胶过滤,以及光谱(紫外可见)和元素(电感耦合等离子体发射光谱、电感耦合等离子体质谱)分析,该方法产生了高度一致的结果,增强了对这些方法的信心。将其应用于对一个贫铀(DU)污染场地土壤孔隙水中胶体和溶解成分的研究,结果显示铀(U)与大分子(100 kDa - 0.2微米)和小分子(3 - 30 kDa)腐殖质胶体均有关联。然而,对于附近有机质含量较低的土壤,除了观察到与小分子(3 - 30 kDa)腐殖质胶体有关联外,还发现与大分子(100 kDa - 0.2微米)铁(Fe) - 铝(Al)胶体有关联。本文介绍的综合胶体分级分离方法现在可以放心地用于研究土壤和水生系统中铀以及其他痕量金属的迁移。

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