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赤铁矿电极上由H₂O衍生的Fe(IV)=O的电化学形成作为选择性烃氧化反应的活性催化位点

Electrochemical Formation of Fe(IV)=O Derived from H O on a Hematite Electrode as an Active Catalytic Site for Selective Hydrocarbon Oxidation Reactions.

作者信息

Kamiya Kazuhide, Kuwabara Akito, Harada Takashi, Nakanishi Shuji

机构信息

Department of Chemical Science and Engineering Graduate School of Engineering Science, Osaka University 1-3 Machikaneyama, Toyonaka, Osaka, 560-8531, Japan.

Research Center for Solar Energy Chemistry, Osaka University 1-3 Machikaneyama, Toyonaka, Osaka, 560-8531, Japan.

出版信息

Chemphyschem. 2019 Mar 4;20(5):648-650. doi: 10.1002/cphc.201801207. Epub 2019 Feb 6.

DOI:10.1002/cphc.201801207
PMID:30659730
Abstract

The high-valence iron species (Fe(IV)=O) in the cytochrome P450 enzyme superfamily is generated via the activation of O , and serves as the active center of selective hydrocarbon oxidation reactions. Furthermore, P450 can employ an alternate route to produce Fe(IV)=O, even from H O without O activation. Meanwhile, Fe(IV)=O has recently been revealed to be the reactive intermediate during H O oxidation to O on hematite electrodes. Herein, we demonstrated the generation of Fe(IV)=O on hematite electrodes during the electrochemical oxidative decomposition of H O using in situ UV-visible absorption spectra. The generation of Fe(IV)=O on hematite electrodes from H O exhibited 100 mV lower overpotential than that from H O. This is because H O serves not only as the oxygen source of Fe(IV)=O, but also as the additional oxidant. Finally, we confirmed that the Fe(IV)=O generated on hematite electrodes can serve as the catalytic site for styrene epoxidation reactions.

摘要

细胞色素P450酶超家族中的高价铁物种(Fe(IV)=O)是通过O的活化产生的,并作为选择性烃氧化反应的活性中心。此外,P450甚至可以采用另一种途径,在不进行O活化的情况下从H O生成Fe(IV)=O。同时,最近发现Fe(IV)=O是赤铁矿电极上H O氧化为O过程中的反应中间体。在此,我们利用原位紫外-可见吸收光谱证明了在H O的电化学氧化分解过程中赤铁矿电极上生成了Fe(IV)=O。从H O在赤铁矿电极上生成Fe(IV)=O的过电位比从H O生成时低100 mV。这是因为H O不仅作为Fe(IV)=O的氧源,还作为额外的氧化剂。最后,我们证实了在赤铁矿电极上生成的Fe(IV)=O可以作为苯乙烯环氧化反应的催化位点。

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