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Kinetics and Mechanism of ~·OH Mediated Degradation of Dimethyl Phthalate in Aqueous Solution: Experimental and Theoretical Studies

机译:〜·OH介导邻苯二甲酸邻苯二甲酸二甲酯降解的动力学及机理:实验和理论研究

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摘要

The hydroxyl radical (~·OH) is one of the main oxidative species in aqueous phase advanced oxidation processes, and its initial reactions with organic pollutants are important to understand the transformation and fate of organics in water environments. Insights into the kinetics and mechanism of ~·OH mediated degradation of the model environmental endocrine disruptor, dimethyl phthalate (DMP), have been obtained using radiolysis experiments and computational methods. The bimolecular rate constant for the ~·OH reaction with DMP was determined to be (3.2 ± 0.1) × 10~9 M~(-1)s~(-1). The possible reaction mechanisms of radical adduct formation (RAF), hydrogen atom transfer (HAT), and single electron transfer (SET) were considered. By comparing the experimental absorption spectra with the computational results, it was concluded that the RAF and HAT were the dominant reaction pathways, and OH-adducts (~·DMPOH_1, ~·DMPOH_2) and methyl type radicals ~·DMP(-H)α were identified as dominated intermediates. Computational results confirmed the identification of transient species with maximum absorption around 260 nm as ~·DMPOH_1 and ~·DMP(-H)α, and these radical intermediates then converted to monohydroxylated dimethyl phthalates and monomethyl phthalates. Experimental and computational analyses which elucidated the mechanism of ~·OH-mediated degradation of DMP are discussed in detail.
机译:羟基自由基(〜·OH)是水相高级氧化过程中的主要氧化物质之一,其与有机污染物的初始反应对于理解水环境中有机物的转化和结局非常重要。使用辐射分解实验和计算方法已经获得了对〜·OH介导的模型环境内分泌干扰物邻苯二甲酸二甲酯(DMP)降解的动力学和机理的见解。与DMP的〜·OH反应的双分子速率常数确定为(3.2±0.1)×10〜9 M〜(-1)s〜(-1)。考虑了自由基加合物形成(RAF),氢原子转移(HAT)和单电子转移(SET)的可能反应机理。通过将实验吸收光谱与计算结果进行比较,可以得出结论,RAF和HAT是主要的反应途径,OH加合物(〜·DMPOH_1,〜·DMPOH_2)和甲基型自由基〜·DMP(-H)α被确定为主要中间体。计算结果证实,在〜260 nm附近具有最大吸收的瞬态物种被识别为〜·DMPOH_1和〜·DMP(-H)α,然后这些自由基中间体转化为邻苯二甲酸单羟基化二邻苯二甲酸酯和邻苯二甲酸单甲酯。详细讨论了实验和计算分析,阐明了〜·OH介导的DMP降解的机理。

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  • 来源
    《Environmental Science & Technology》 |2014年第1期|641-648|共8页
  • 作者单位

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China;

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China,University of Chinese Academy of Sciences, Beijing 100049, People's Republic of China;

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China;

    Radiation Laboratory University of Notre Dame, Notre Dame, Indiana 46556,Department of Chemistry and Biochemistry, University of Notre Dame, Notre Dame, Indiana 46556;

    Department of Chemistry, Indiana University-Northwest, Gary, Indiana 46408, United States;

    Department of Chemistry and Biochemistry, University of Notre Dame, Notre Dame, Indiana 46556;

  • 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);
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  • 正文语种 eng
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