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首页> 外文期刊>Environmental Science & Technology >Investigation of the Iron-Peroxo Complex in the Fenton Reaction: Kinetic Indication, Decay Kinetics, and Hydroxyl Radical Yields
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Investigation of the Iron-Peroxo Complex in the Fenton Reaction: Kinetic Indication, Decay Kinetics, and Hydroxyl Radical Yields

机译:Fenton反应中的铁-过氧配合物的研究:动力学指示,衰变动力学和羟基自由基产率。

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摘要

The Fenton reaction describes the reaction of Fe(II) with hydrogen peroxide. Several researchers proposed the formation of an intermediate iron-peroxo complex but experimental evidence for its existence is still missing. The present study investigates formation and lifetime of this intermediate at various conditions such as different Fe(II)-concentrations, absence vs presence of a hydroxyl radical scavenger (dimethyl sulfoxide, DMSO), and different pH values. Obtained results indicate that the iron-peroxo complex is formed under all experimental conditions. Based on these data, stability of the iron-peroxo complex could be examined. At pH 3 regardless of [Fe(II)](0) decay rates, for the iron-peroxo complex of about SO s(-1) were determined in absence and presence of DMSO. Without DMSO and [Fe(II)](0) = 300 mu M variation of pH yielded decay rates of about 70 s(-1) for pH 1 and 2 and of about 50 s(-1) at pH 3 and 4. Hence, the iron-peroxo complex becomes more stable with increasing pH. Furthermore, pH-dependent hydroxyl radical yields were determined to investigate whether the increasing stability of the intermediate complex may indicate a different reaction of the iron-peroxo complex which might yield Fe(IV) instead of hydroxyl radical formation as suggested in literature. However, it was found that hydroxyl radicals were produced proportionally to the Fe (II)-concentration.
机译:Fenton反应描述了Fe(II)与过氧化氢的反应。几位研究人员提出了中间铁-过氧配合物的形成,但仍缺乏其存在的实验证据。本研究调查了该中间体在各种条件下的形成和寿命,例如不同的Fe(II)浓度,是否存在羟基自由基清除剂(二甲基亚砜,DMSO)以及不同的pH值。所得结果表明在所有实验条件下均形成了铁-过氧配合物。基于这些数据,可以检查铁-过氧配合物的稳定性。在pH 3下,无论[Fe(II)](0)的衰减速率如何,在不存在和存在DMSO的情况下,测定的铁-过氧络合物约为SO s(-1)。在没有DMSO和[Fe(II)](0)= 300μM的情况下,pH值的变化对于pH 1和2产生大约70 s(-1)的衰减速率,在pH 3和4产生大约50 s(-1)的衰减速率。因此,铁-过氧配合物随着pH的增加变得更稳定。此外,测定pH依赖性羟基自由基的收率,以调查中间配合物稳定性的提高是否表明铁-过氧配合物有不同的反应,从而可能生成Fe(IV)而不是文献中所建议的形成羟基自由基。然而,发现羟基自由基与Fe(II)浓度成比例地产生。

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  • 来源
    《Environmental Science & Technology》 |2017年第24期|14321-14329|共9页
  • 作者单位

    Univ Duisburg Essen, Instrumental Analyt Chem, Univ Str 5, D-45141 Essen, Germany;

    Univ Duisburg Essen, Instrumental Analyt Chem, Univ Str 5, D-45141 Essen, Germany;

    Univ Duisburg Essen, Instrumental Analyt Chem, Univ Str 5, D-45141 Essen, Germany;

    Univ Duisburg Essen, Instrumental Analyt Chem, Univ Str 5, D-45141 Essen, Germany;

    Univ Duisburg Essen, Instrumental Analyt Chem, Univ Str 5, D-45141 Essen, Germany;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
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