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Factors influencing the oxidation, reduction, methylation and demethylation of mercury species in coastal waters

机译:影响沿海水域汞物种的氧化,还原,甲基化和去甲基化的因素

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摘要

The objective of this study was to examine the redox reactions and other transformations of mercury (Hg) species in surface waters, and the factors determining the rates of these reactions. For the redox studies completed at the Chesapeake Biological Laboratory (CBL), two isotopes (~(199)Hg~(11) and ~(202)Hg~0) were added into different types of filtered water (fresh to seawater) to examine the oxidation and reduction reactions. Further studies of both the redox reactions and methylation/demethylation reactions of Hg were conducted with unfiltered water on board research vessels during cruises in May and July 2005 on the Chesapeake Bay and shelf. While CH_3~(199)Hg~(11) was added to allow the examination of demethylation, ~(201)Hg~(11) was used to examine both reduction and methylation, and ~(202)Hg~0 was used to examine oxidation. Overall, the results showed that both Hg oxidation and reduction were simultaneously occurring and were photochemically mediated in the waters investigated. In contrast to the previously assumed "unreactive" nature of Hg~0, the studies found that the magnitude of the rate constant for Hg~0 oxidation was greater than that for reduction, indicating its importance in estuarine and coastal waters. In addition, both experiments at CBL and on board ship showed that Hg" reduction was similar in magnitude, suggesting that biotic processes were relatively unimportant. While no measurable methylation occurred during the incubation period during the on board studies, concentration of CH_3~(199)Hg~(11) decreased over the time during the experiments. It appeared that the demethylation processes were not dominantly photochemically driven, but could be microbially mediated. Further studies are needed in order to help better understand Hg redox and transformations in natural water systems.
机译:这项研究的目的是检查地表水中汞的还原反应和其他转化形式,以及决定这些反应速率的因素。对于切萨皮克生物实验室(CBL)完成的氧化还原研究,将两种同位素(〜(199)Hg〜(11)和〜(202)Hg〜0)添加到不同类型的过滤水中(从新鲜到海水),以检查氧化还原反应。在2005年5月和7月于切萨皮克湾和陆架上航行期间,在研究船上用未经过滤的水对汞的氧化还原反应和甲基化/脱甲基反应进行了进一步研究。在添加CH_3〜(199)Hg〜(11)进行脱甲基的同时,使用〜(201)Hg〜(11)进行还原和甲基化的检测,〜(202)Hg〜0进行检测氧化。总的来说,结果表明汞的氧化和还原同时发生,并且在所研究的水中是光化学介导的。与先前假定的Hg-0的“无反应性”性质相反,研究发现Hg-0氧化速率常数的幅度大于还原速率,表明其在河口和沿海水域的重要性。此外,在CBL和船上的两个实验均表明,Hg“的减少幅度相似,这表明生物过程相对不重要。尽管在船上研究的潜伏期中没有可测量的甲基化,但CH_3〜(199 )Hg〜(11)在实验过程中随着时间的推移而降低,似乎脱甲基过程不是主要由光化学驱动的,而是可以通过微生物介导的,还需要进一步研究以帮助更好地了解天然水系统中的Hg氧化还原和转化。

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