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Mercury behaviour in estuarine and coastal environment

机译:河口和沿海环境中的汞行为

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General facts about the global mercury cycle with particular emphasis on the coastal and ocean environment are summarized. In the coastal environment the largest source of mercuryis river-born particulate bound species. This portion of mercury is unreactive and is quickly buried in nearshore sediments. Only a small fraction of reactive mercury (ionic mercury in solution that is immediately available for reaction) originates from river inputs. The most important source of reactive mercury in the coastal and oceanic environment is through atmospheric input and via upwelling. Biologically-mediated processes, mainly connected to primary production, are responsible for active redistribution of reactive mercury. In this process a large part of reactive Hg is reduced to elemental mercury which is returned to the atmosphere by evasion, while the rest is scavenged by particles and transported to deeper oceanic waters. Because of the active atmospheric mercury cycle oceans acts as a source and a sink of atmospheric mercury and the global oceanic evasion is balanced by the deposition. Current studies show that methylated species are primarily formed in the deeper ocean and the main source of monomethylmercury (MMHg) compounds in coastal areas is through upwelling of oceanic waters and from in-situ methylation in coastal waters. All these environemntal processes occur at extremely low concentration levels of mercury species; however MMHg in marine organisms accounts for a high proportion of this toxic compounds owing to its proprty for bioaccumulation and biomagnification. Coastal areas on the local scale may account for geochemical differences that significantly influence the conversion between various Hg species. In order to assess the impact of mercury in contaminated and non-contaminated coastal areas on man and his environment, it is of the greatest importance to understand these processes. The paper also identifies uncertainties and gaps in current knowledge of mercuy cycling.
机译:总结了有关全球汞循环的一般事实,特别是沿海和海洋环境。在沿海环境中,汞的最大来源是河流中的微粒结合物种。这部分汞是无活性的,并很快被埋在近岸沉积物中。仅一小部分活性汞(溶液中的离子汞可立即用于反应)来自河流输入。沿海和海洋环境中活性汞的最重要来源是大气输入和上升流。主要与初级生产有关的生物介导过程负责活性汞的主动再分配。在此过程中,大部分反应性汞被还原为元素汞,该汞通过逃逸返回大气,而其余的则被颗粒清除并输送到更深的海洋水域。由于活跃的大气汞循环,海洋成为大气汞的来源和汇聚区,全球海洋逃逸受到沉积的影响。当前的研究表明,甲基化物种主要形成于更深的海洋中,沿海地区的单甲基汞(MMHg)化合物的主要来源是通过海洋水的上升流和沿海水域的原位甲基化。所有这些环境过程都是在极低浓度的汞物种中发生的。然而,由于其对生物蓄积和生物放大作用的特性,海洋生物中的MMHg在这种有毒化合物中占很高的比例。当地规模的沿海地区可能解释了地球化学差异,这些差异显着影响了各种汞物种之间的转化。为了评估受污染和未受污染的沿海地区汞对人类及其环境的影响,了解这些过程至关重要。本文还确定了当前关于汞循环的知识的不确定性和差距。

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