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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >The ferrozine method revisited: Fe(II)/Fe(III) determination in natural waters
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The ferrozine method revisited: Fe(II)/Fe(III) determination in natural waters

机译:再谈铁锌方法:天然水中的Fe(II)/ Fe(III)测定

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摘要

The original ferrozine method has been modified to sequentially determine the Fe(II)/Fe(III) speciation in small volumes of fresh and marine water samples, at the submicromolar level. Spectrophotometric analyses of the Fe(II)ferrozine complex are performed on a single aliquot before and after a reduction step with hydroxylamine. The procedure is calibrated using Fe(III) standards stable under normal conditions of analysis. It is shown also that the presence of high concentrations of dissolved NOM (natural organic matter) do not create any significant artifacts. The method was used to measure Fe(II) and Fe(III) depth distribution in salt marsh pore waters and in a stratified marine basin. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 23]
机译:最初的铁锌方法已经过修改,可以在亚微摩尔水平上依次测定少量淡水和海水样品中的Fe(II)/ Fe(III)形态。 Fe(II)亚铁嗪络合物的分光光度分析是在用羟胺还原的步骤之前和之后对单个等分试样进行的。该过程使用在正常分析条件下稳定的Fe(III)标准品进行校准。还表明存在高浓度的溶解的NOM(天然有机物)不会产生任何明显的伪影。该方法用于测量盐沼孔隙水和分层海洋盆地中Fe(II)和Fe(III)的深度分布。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:23]

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