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Light-Mediated Reactive Oxygen Species Generation and iron Redox Transformations in the Presence of Exudate from the Cyanobacterium Microcystis aeruginosa

机译:铜绿微囊藻渗出液中光介导的活性氧的产生和铁的氧化还原转化

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摘要

The photochemical properties of the organic exudate secreted by a toxic strain of Microcystis aeruginosa were studied by measuring reactive oxygen species (ROS) generation and redox transformations of iron in the presence of the organic exudate under acidic (pH 4) and alkaline (pH 8) conditions. Our results show that the organic exudate generates nanomolar concentrations of superoxide and hydrogen peroxide on irradiation with simulated sunlight in a manner consistent with that reported for terrigenous natural organic matter. The photo-generated superoxide plays an important role in Fe(m) reduction under alkaline conditions with nearly 45% of the observed Fe(n) generation on Fe(m) reduction occurring via Fe(lH) reduction by superoxide while the rest of the Fe(lll) reduction occurs via a ligand-to-metal charge transfer (LMCT) pathway. In contrast, under acidic conditions, 100% of the observed photochemical Fe(Il) generation on Fe(ffl) reduction occurs via a LMCT pathway. These results suggest that steady-state dissolved Fe concentrations and hence Fe availability in natural waters will significantly increase in the presence of these algal exudates. Furthermore, significant diel variation in Fe(n) concentration is to be expected, even in acidic waters, since time scales of light-mediated Fe(lH) reduction and thermal Fe(lll) reduction differ markedly. A kinetic model is developed that adequately describes both the "generation of ROS and the photochemical redox transformations of iron in the presence of M. aeruginosa exudate.
机译:通过测量在酸性(pH 4)和碱性(pH 8)下有机渗出液中铁的活性氧(ROS)的生成和铁的氧化还原转化,研究了铜绿微囊藻毒性菌株分泌的有机渗出液的光化学性质。条件。我们的结果表明,有机渗出液在模拟阳光照射下会产生纳摩尔浓度的超氧化物和过氧化氢,其方式与报道的陆源天然有机物一致。光生的超氧化物在碱性条件下的Fe(m)还原中起重要作用,在观察到的Fe(n)还原中,将近45%的Fe(n)生成是通过超氧化物的Fe(1H)还原而其余的Fe(III)还原通过配体到金属的电荷转移(LMCT)途径发生。相反,在酸性条件下,通过LMCT途径发生的Fe(ffl)还原过程中观察到的光化学Fe(II)生成的100%。这些结果表明,在存在这些藻类渗出物的情况下,稳态溶解的Fe浓度以及天然水中的Fe利用率将显着增加。此外,由于光介导的Fe(IH)还原和热Fe(III)还原的时间尺度显着不同,因此即使在酸性水中,Fe(n)浓度也会发生明显的狄尔变化。建立了一个动力学模型,该模型充分描述了“铜绿假单胞菌渗出液存在下ROS的产生和铁的光化学氧化还原转化。

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  • 来源
    《Environmental Science & Technology》 |2017年第15期|8384-8395|共12页
  • 作者单位

    School of Civil and Environmental Engineering, The University of New South Wales, Sydney, NSW 2052, Australia;

    School of Civil and Environmental Engineering, The University of New South Wales, Sydney, NSW 2052, Australia;

    School of Civil and Environmental Engineering, The University of New South Wales, Sydney, NSW 2052, Australia;

  • 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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