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Effects of ultraviolet radiation on mercury isotope fractionation during photo-reduction for inorganic and organic mercury species

机译:紫外线对无机和有机汞物种光还原过程中汞同位素分馏的影响

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摘要

Photo-reduction of mercury (Hg) is an important mechanism for removal of both Hg2+ species and monomethylmercury (MMHg) from surface waters. Large mass independent fractionation (MIF) signatures of Hg isotopes preserved in natural samples are thought to reflect MIF produced during aqueous photo-reduction by the magnetic isotope effect (MIE). Recently, Hg MIF signatures in natural samples are being used to quantify photochemical reduction in aquatic systems. However, the fractionation factors used are from laboratory experiments that did not investigate many of the environmental parameters that may affect MIF during photoreduction. In this study, the effects of different regions of the solar spectrum on the expression of MIF caused by the MIE during Hg2+ and MMHg photo-reduction were investigated to assess how the type of radiation affects the extent and signature of MIF. Photo-reduction in the presence of DOM was carried out through exposure to the full natural solar spectrum unfiltered, with the ultraviolet B (UVB; 290-320 nm) portion removed and with both the UVB and the ultraviolet A (UVA; 320-400 nm) removed. There is a clear relationship between the expression and magnitude of MIF and the energy of incident radiation for both Hg2+ and MMHg photo-reduction. The experiments indicate that MIF produced during photo-reduction of Hg2+ is significantly influenced by both UVB and UVA radiation. For MMHg photodemethylation, however, UVB radiation is mostly responsible for the MIF with minor contributions from UVA. Overall, there is a lack of correlation between the observed MIF and total photo-reduction in the experiments conducted in this study, which indicates that indirect and other non-MIF producing pathways of photo-reduction are the dominant pathways by which Hg species are being photo-reduced. Extrapolating these experimental results to natural systems is difficult as the experiments were not performed at realistic Hg/DOM ratios and the distribution of ligands that Hg is bound to in the experiments likely differs from natural systems. However, the strong relationship between MIF and energy of incident radiation in this study supports Hg MIF signatures as promising tools for helping to quantify photochemical cycling of mercury, but this study also highlights the need to understand the link between MIF and total photo-reduction before this tool can be fully utilized. (C) 2015 Elsevier B.V. All rights reserved.
机译:汞(Hg)的光还原是从地表水中去除Hg2 +物种和一甲基汞(MMHg)的重要机制。天然样品中保存的汞同位素的大型非质量分数分离(MIF)标记被认为反映了通过磁性同位素效应(MIE)在水光还原过程中产生的MIF。最近,天然样品中的汞MIF签名被用于量化水生系统中的光化学还原。但是,使用的分馏因子来自实验室实验,该实验没有研究可能在光还原过程中影响MIF的许多环境参数。在这项研究中,研究了在Hg2 +和MMHg光还原过程中,太阳光谱的不同区域对MIE引起的MIF表达的影响,以评估辐射类型如何影响MIF的程度和特征。通过暴露于未经过滤的完整自然太阳光谱,去除紫外线B(UVB; 290-320 nm)部分以及同时去除UVB和紫外线A(UVA; 320-400),在DOM存在下进行光还原。 nm)移除。对于Hg2 +和MMHg光还原,MIF的表达和大小与入射辐射的能量之间存在明显的关系。实验表明,Hb2 +的光还原过程中产生的MIF受UVB和UVA辐射的影响很大。但是,对于MMHg光脱甲基化,UVB辐射主要是MIF的原因,而UVA的贡献很小。总体而言,在这项研究中进行的实验中,观察到的MIF与总的光还原之间缺乏相关性,这表明间接的和其他非MIF产生光还原的途径是汞物种产生的主要途径。减少照片。将这些实验结果推论到自然系统是困难的,因为该实验不是在实际的Hg / DOM比下进行的,并且在实验中与Hg结合的配体的分布可能与自然系统不同。但是,本研究中MIF与入射辐射能量之间的密切关系支持Hg MIF签名作为帮助量化汞的光化学循环的有前途的工具,但这项研究还强调了在使用前需要了解MIF与总光还原之间的联系的必要性。该工具可以得到充分利用。 (C)2015 Elsevier B.V.保留所有权利。

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