4.5 Article

Determination of the free-ion concentration of rare earth elements by an ion-exchange technique: implementation, evaluation and limits

期刊

ENVIRONMENTAL CHEMISTRY
卷 13, 期 3, 页码 478-488

出版社

CSIRO PUBLISHING
DOI: 10.1071/EN15136

关键词

free metal ions; humic acid; lanthanides; speciation

资金

  1. Environment Canada
  2. Natural Sciences and Engineering Research Council of Canada
  3. Fonds de recherche du Quebec - Nature et technologies
  4. Canada Research Chair Programme

向作者/读者索取更多资源

Environmental context The lanthanides are a group of heavy elements (from lanthanum to lutetium) increasingly used in many electronic consumer products and little is known about their environmental mobility and toxicity. In natural systems, these elements will bind to natural organic matter but metal toxicity is usually defined by the free metal ion concentration. Here, we propose a method based on sample equilibration with an ion-exchange resin to measure the free lanthanide ion concentration in the presence of natural organic matter. Abstract An ion-exchange technique that employs a polystyrene sulphonate ion-exchange resin was developed for determining environmentally relevant free-ion concentrations of Ce, Eu, La and Nd. Owing to the high affinity of rare earth elements (REE) for the selected resin, this method requires the addition of an inert salt to increase the concentration of the counter-ions (i.e. cations that are exchanged with REE bound to the resin). The use of a batch equilibration approach to calibrate the resin allowed the implementation of the ion-exchange technique at reasonably low ionic strength (I = 0.1M). Several ligands were used to test the selectivity of the method, which proved to be highly selective for the free metal ion in presence of the tested cationic and anionic complexes (REE-nitrate, REE-malic acid and REE-nitrilotriacetic acid systems) and operational for very low proportions of REE3+, owing to the strong REE-resin interactions. The ion-exchange technique was also implemented to determine [Eu](inorg) in the presence of natural humic matter (Suwannee River Humic Acid) and the results were compared with those obtained using equilibrium dialysis and those calculated with chemical equilibrium models. At pH 4.00, the measured [Eu](inorg) values were in fairly good agreement with those predicted with the Windermere Humic Aqueous Model and Stockholm Humic Model, whereas the Non-Ideal Competitive Absorption model appeared to underestimate the [Eu](inorg). However, the inorganic europium concentrations were strongly underestimated (4 < [Eu](inorg, IET)/[Eu](inorg, calc) < 18) with the three prediction models at higher pH (5.3 and 6.2).

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