首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Superoxide-mediated reduction of organically complexed iron(III): Impact of pH and competing cations (Ca2+)
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Superoxide-mediated reduction of organically complexed iron(III): Impact of pH and competing cations (Ca2+)

机译:超氧化物介导的有机络合铁的还原(III):pH和竞争性阳离子(Ca2 +)的影响

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The mechanism and kinetics of superoxide-mediated reduction of a variety of organic iron(III) complexes has been investigated over the pH range 7-9. Our experimental results show that the rate of iron(II) formation is a function of pH, ligand type and H.-and concentration with the measured rate varying between 0.44 +/- 0.07 and 39.25 +/- 1.77 pM s(-1) in the systems investigated. Additionally, our results show that the presence of competing cations such as Ca2+ have a significant impact on iron(II) formation if the organic ligand is strongly complexed by Ca2+. Formation of iron(II) occurs by either (or, in some instances. both) reaction of superoxide with inorganic iron(III) after its dissociation from the complex (dissociative reduction) or by direct reaction of superoxide with the complex (non-dissociative reduction). In the presence of weak ligands, dissociative reduction (DR) dominates; however non-dissociative reduction (NDR) becomes important in the presence of either strongly binding ligands or high concentrations of weakly binding ligands. The major factors contributing to the pH dependence of the iron(II) formation rate are the complexation kinetics of inorganic iron(III) (which controls the DR contribution) and the reduction kinetics of the iron(III) complex (which controls the NDR contribution). The relative NDR contribution increases with increasing superoxide and ligand concentration and decreasing pH for all ligands examined. Since iron(II) formation occurring via NDR results in a significantly larger increase in the proportion of iron in free aquated form than does DR, this non-dissociative pathway of superoxide-mediated iron(III) reduction is particularly effective in increasing the]ability of iron in aquatic systems. (C) 2007 Elsevier Ltd. All rights reserved.
机译:在7-9的pH范围内,研究了超氧化物介导的多种有机铁(III)配合物还原的机理和动力学。我们的实验结果表明,铁(II)的形成速率是pH,配体类型和H.以及浓度的函数,所测得的速率在0.44 +/- 0.07和39.25 +/- 1.77 pM s(-1)之间变化在调查的系统中。此外,我们的结果表明,如果有机配体被Ca2 +强烈络合,则竞争性阳离子(如Ca2 +)的存在对铁(II)的形成会产生重大影响。铁(II)的形成是通过(或在某些情况下)超氧化物与无机铁(III)从络合物中解离(解离还原)或超氧化物与络合物的直接反应(非解离)发生的减少)。在弱配体存在下,解离还原(DR)占主导。然而,在存在强结合配体或高浓度弱结合配体的情况下,非离解还原(NDR)变得很重要。影响铁(II)形成速率的pH依赖性的主要因素是无机铁(III)的络合动力学(控制DR的贡献)和铁(III)络合物的还原动力学(控制NDR的贡献) )。对于所有检测的配体,NDR的相对贡献都随着超氧化物和配体浓度的增加以及pH值的降低而增加。由于通过NDR形成的铁(II)导致游离水合形式的铁比例比DR显着增加,因此这种超氧化物介导的铁(III)还原的非解离途径特别有效地提高了水系统中的铁(C)2007 Elsevier Ltd.保留所有权利。

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