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为什么在磷酸盐缓冲溶液中芬顿反应的活性氧物种会从氧代铁(IV)物种转变为羟基自由基?一个计算原理。

Why the Reactive Oxygen Species of the Fenton Reaction Switches from Oxoiron(IV) Species to Hydroxyl Radical in Phosphate Buffer Solutions? A Computational Rationale.

作者信息

Chen Hsing-Yin

机构信息

Department of Medicinal and Applied Chemistry, Kaohsiung Medical University, Kaohsiung 80708, Taiwan.

出版信息

ACS Omega. 2019 Aug 13;4(9):14105-14113. doi: 10.1021/acsomega.9b02023. eCollection 2019 Aug 27.

DOI:10.1021/acsomega.9b02023
PMID:31497730
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6714542/
Abstract

It has been shown that the major reactive oxygen species (ROS) generated by the aqueous reaction of Fe(II) and HO (i.e., the Fenton reaction) are high-valent oxoiron(IV) species, whereas the hydroxyl radical plays a role only in very acidic conditions. Nevertheless, when the Fenton reaction is conducted in phosphate buffer solutions, the resulting ROS turns into hydroxyl radical even in neutral pH conditions. The present density functional theory (DFT) study discloses the underlying principle for this phenomenon. Static and dynamic DFT calculations indicate that in phosphate buffer solutions, the iron ion is highly coordinated by phosphoric acid anions. Such a coordination environment substantially raises the p of coordinated water on Fe(III). As a consequence, the Fe(III)-OH intermediate, resulting from the reductive decomposition of HO by ferrous ion is relatively unstable and will be readily protonated by phosphoric acid ligand or by free proton in solution. These proton-transfer reactions, which become energetically favorable when the number of phosphate coordination goes up to three, prevent the Fe(III)-OH from hydrogen abstraction by nascent OH to form Fe(IV)=O species. On the basis of this finding, a ligand design strategy toward controlling the nature of ROS produced in the Fenton reaction is put forth. In addition, it is found that while phosphate buffers facilitate OH radical generation in the Fenton reaction, phosphoric acid anions can act as OH radical scavengers through hydrogen atom transfer reactions.

摘要

研究表明,铁(II)与羟基(即芬顿反应)的水相反应产生的主要活性氧物种(ROS)是高价氧合铁(IV)物种,而羟基自由基仅在非常酸性的条件下起作用。然而,当在磷酸盐缓冲溶液中进行芬顿反应时,即使在中性pH条件下,产生的ROS也会转化为羟基自由基。目前的密度泛函理论(DFT)研究揭示了这一现象的潜在原理。静态和动态DFT计算表明,在磷酸盐缓冲溶液中,铁离子与磷酸阴离子高度配位。这样的配位环境大大提高了铁(III)上配位水的pKa。因此,亚铁离子对羟基的还原分解产生的铁(III)-OH中间体相对不稳定,并且会很容易被磷酸配体或溶液中的游离质子质子化。当磷酸盐配位数增加到三个时,这些质子转移反应在能量上变得有利,从而阻止铁(III)-OH被新生的羟基夺取氢以形成铁(IV)=O物种。基于这一发现,提出了一种控制芬顿反应中产生的ROS性质的配体设计策略。此外,还发现虽然磷酸盐缓冲液促进了芬顿反应中羟基自由基的产生,但磷酸阴离子可以通过氢原子转移反应作为羟基自由基清除剂。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0950/6714542/03149660f6b5/ao9b02023_0007.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0950/6714542/36a3995e9f92/ao9b02023_0003.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0950/6714542/03149660f6b5/ao9b02023_0007.jpg

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