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Methylation index as means of quantification of the compliance of sedimentary mercury to be methylated

机译:甲基化指数作为量化要被甲基化的沉积汞的顺应性的手段

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Methylmercury (MeHg) is the most bioavailable and toxic mercury species in the marine environment. MeHg concentration levels, methylation rates leading to MeHg formation, and methylation index (MI) are all used to assess the compliance of mercury to be methylated in the marine sedimentary environment. This paper reports on the works conducted on the MI upgrade. This paper proposes a new formula for calculating MI. Apart from labile mercury(II) and organic matter, it includes redox potential and abundance of sulfur-reducing bacteria (SRB), both essential factors for MeHg generation. The obtained MI is validated against actual sedimentary MeHg concentrations proving the potential usefulness of MI as a factor characterizing status of sedimentary environment regarding possible occurrence of MeHg. Moreover, values of the methylation index in particular regions show that MI values correspond well to environmental conditions in those areas. The values calculated correlate well with MeHg concentrations; however, the correlation coefficients vary between different regions. This has been attributed to the lack of empirical coefficients. Thus, MI could be used as a characteristic of the sedimentary environment indicating the potential presence of MeHg. It could also be used in methylation rate modeling, provided that empirical constants are applied to improve model performance.
机译:甲基汞(MeHg)是海洋环境中生物利用度最高,毒性最大的汞种类。 MeHg浓度水平,导致MeHg形成的甲基化速率和甲基化指数(MI)均用于评估海洋沉积环境中要甲基化的汞的顺应性。本文报告了有关MI升级的工作。本文提出了一种计算MI的新公式。除了不稳定的汞(II)和有机物外,它还包括氧化还原电势和大量还原硫细菌(SRB),这都是产生MeHg的重要因素。相对于实际的沉积MeHg浓度对获得的MI进行了验证,证明了MI的潜在有用性,作为表征MeHg可能发生的沉积环境状况的一个因素。此外,特定区域的甲基化指数值表明MI值与这些区域的环境条件非常吻合。计算得出的值与MeHg浓度密切相关;但是,相关系数在不同区域之间有所不同。这归因于缺乏经验系数。因此,MI可以用作沉积环境的特征,表明可能存在MeHg。如果将经验常数应用于改善模型性能,它也可以用于甲基化速率建模。

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