首页> 外文会议>American Chemical Society National Meeting >PROBING OXIDE SURFACE REACTIVITY WITH ORGANIC CONTAMINANTS: FROM KINETIC AND PRODUCT STUDIES TO STABLE ISOTOPE FRACTIONATION
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PROBING OXIDE SURFACE REACTIVITY WITH ORGANIC CONTAMINANTS: FROM KINETIC AND PRODUCT STUDIES TO STABLE ISOTOPE FRACTIONATION

机译:探测氧化物表面反应性与有机污染物:从动力学和产品研究中稳定同位素分馏

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In recent years, exciting new findings have furthered our understanding of surface-bound ferrous iron and its role in the reductive transformation of contaminants. Iron oxide surfaces have been demonstrated to be dynamic systems in which adsorbed Fe(II) quickly transfers its electron into the underlying mineral and even crystal restructuring may be catalyzed by the presence of aqueous Fe(II). Organic contaminants were used as probe compounds and found to react only at certain mineral faces, while reaction rates with different pollutants showed surprising, substance-specific differences between seemingly similar iron oxides. Parallel to such kinetic studies, the product distribution in reductive dehalogenation of halogenated methanes revealed pronounced dependencies on the type of iron oxide crystal, pH-value and even the presence of organic buffers.
机译:近年来,令人兴奋的新发现进一步了解我们对污染物的还原转化中的表面结合的亚铁铁及其作用。已经证明了氧化铁表面是动态系统,其中吸附的Fe(II)迅速将其电子转移到下面的矿物中,甚至可以通过含水Fe(II)的存在催化晶体重构。有机污染物被用作探针化合物,发现仅在某些矿物面上反应,而具有不同污染物的反应速率令人惊讶,看似相似的铁氧化物之间的特异性特异性差异。与此类动力学研究平行,卤化甲烷的还原脱卤的产物分布揭示了氧化铁晶体,pH值甚至有机缓冲液的存在的明显依赖性。

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