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Photochemical behavior of ferrihydrite-oxalate system: Interfacial reaction mechanism and charge transfer process

机译:水合草酸盐体系的光化学行为:界面反应机理和电荷转移过程

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摘要

Heterogeneous photochemical reactions associated with natural iron (hydr)oxides and oxalic acid have attracted a great deal of scientific attention in the application of organic pollutants degradation. However, the reaction mechanism is still unclear due to the complicated iron cycles and reactive oxygen species (ROS) generation. In this study, the in situ attenuated total reflectance-Fourier transform infrared spectroscopy was implemented to investigate the adsorption process and photochemical behavior of oxalic acid on the surface of ferrihydrite. A comprehensive reaction mechanism from the perspective of charge transfer process, including homogeneous-heterogeneous iron cycling and ROS generation, was illustrated in detail. We found that oxalic acid was first adsorbed on the surface of ferrihydrite with a mononuclear bidentate binding geometry. Interestingly, this mononuclear bidentate complex on the surface of ferrihydrite was stable under visible light irradiation. Subsequently, the whole complex departed from ferrihydrite surface through non-reduction dissolution with the form of Fe(C2O4)(+). In the solution, the Fe(C2O4)(+) complexes would quickly convert to Fe(C2O4)(2)(-) complexes. Under visible light irradiation, the electrons generated from the photolysis of Fe(C2O4)(2)(-) complex reacted with O-2 to form O-2(center dot-)/center dot OOH. Meanwhile, Fe(III) was reduced to Fe(II). Finally, the produced O-2(center dot-)/center dot OOH could react with Fe(II) through a one-step way to generate center dot OH, which possessed higher center dot OH formation efficiency than that through the two-step way of H2O2 as the intermediates. This study helps us with understanding of in-situ photochemical reaction mechanism of ferrihydrite-oxalic acid system, and also provides guidance to effectively utilize widespread iron (hydr)oxides and organic acids in natural environment to develop engineered systems for water treatment. (C) 2019 Elsevier Ltd. All rights reserved.
机译:与天然(氢氧化)铁和草酸有关的多相光化学反应在有机污染物降解的应用中引起了很多科学关注。然而,由于复杂的铁循环和活性氧(ROS)的产生,反应机理仍不清楚。本研究采用原位衰减全反射-傅立叶变换红外光谱技术研究草酸在水铁矿表面的吸附过程和光化学行为。从电荷转移过程的角度详细阐述了一种全面的反应机理,包括均相-非均相铁循环和ROS生成。我们发现草酸首先被吸附在具有单核双齿结合几何形状的水铁矿表面上。有趣的是,亚铁酸盐表面上的这种单核双齿络合物在可见光照射下是稳定的。随后,整个复合物通过非还原溶解以Fe(C2O4)(+)形式从亚铁酸盐表面离开。在解决方案中,Fe(C2O4)(+)络合物将迅速转变为Fe(C2O4)(2)(-)络合物。在可见光照射下,Fe(C2O4)(2)(-)配合物光解产生的电子与O-2反应形成O-2(中心点-)/中心点OOH。同时,Fe(III)还原为Fe(II)。最后,生成的O-2(中心点)/中心点OHH可以通过一步反应与Fe(II)反应生成中心点OH,中心点OH的生成效率高于两步。以过氧化氢为中间体。这项研究有助于我们了解三水铝酸盐-草酸体系的原位光化学反应机理,并为有效利用自然环境中广泛的氧化铁和有机酸开发工程化的水处理系统提供指导。 (C)2019 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Water Research》 |2019年第1期|10-19|共10页
  • 作者单位

    Cent China Normal Univ, Key Lab Pesticide & Chem Biol, Inst Environm & Appl Chem, Minist Educ,Coll Chem, Wuhan 430079, Hubei, Peoples R China;

    Chinese Acad Sci, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, 511 Kehua St, Guangzhou 510640, Guangdong, Peoples R China;

    Cent China Normal Univ, Key Lab Pesticide & Chem Biol, Inst Environm & Appl Chem, Minist Educ,Coll Chem, Wuhan 430079, Hubei, Peoples R China;

    Cent China Normal Univ, Key Lab Pesticide & Chem Biol, Inst Environm & Appl Chem, Minist Educ,Coll Chem, Wuhan 430079, Hubei, Peoples R China;

    Cent China Normal Univ, Key Lab Pesticide & Chem Biol, Inst Environm & Appl Chem, Minist Educ,Coll Chem, Wuhan 430079, Hubei, Peoples R China;

    Cent China Normal Univ, Key Lab Pesticide & Chem Biol, Inst Environm & Appl Chem, Minist Educ,Coll Chem, Wuhan 430079, Hubei, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Oxalic acid; Ferrihydrite; In-situ ATR-FTIR; Fe(III)-Ox complex; Reactive oxygen species;

    机译:草酸;水铁矿;原位ATR-FTIR;Fe(III)-Ox络合物;活性氧;

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