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首页> 外文期刊>Biogeochemistry >MMHg production and export from intertidal sediments to the water column of a tidal lagoon (Arcachon Bay, France)
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MMHg production and export from intertidal sediments to the water column of a tidal lagoon (Arcachon Bay, France)

机译:MMHg的生产以及从潮间带沉积物到潮汐泻湖水柱的出口(法国阿卡雄湾)

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摘要

Hg cycling in biologically productive coastal areas is of special importance given the potential for bioaccumulation of monomethylmercury (MMHg) into aquatic organisms. Field experiments were performed during three different seasons in Arcachon Bay, a mesotidal lagoon (SW France), to assess the variability of the water column concentrations, sediment-water exchanges and potential formation and degradation of MMHg. The objectives were to evaluate the contribution of intertidal mudflats to MMHg production and the various pathways of Hg species export. Dissolved and bulk concentrations of Hg species in the water column downstream of tidal flats were measured throughout several tidal cycles. The Hg benthic fluxes at the sediment-water interface were determined by means of benthic chambers for three different stations. Hg methylation and demethylation potentials were determined in surficial sediments and the water column using isotopic tracers. The tidal surveys demonstrated that benthic remobilization of Hg occurs primarily in association with sediment erosion and advection during ebb tide. However, elevated dissolved Hg concentrations observed at low tide were found to be caused by a combination of pore-waters seeping, benthic fluxes and methylation in the water column. Benthic fluxes were more intense during late winter conditions (median MMHg and inorganic Hg (IHg) fluxes: 64 and 179 pmol m(-2) h(-1), respectively) and subsequently decreased in spring (median 0.7 and -5 pmol m(-2) h(-1), respectively) and fall (median -0.4 and -1.3 pmol m(-2) h(-1), respectively). The trends in methylation and demethylation potentials were at the opposite of the fluxes, two times lower during winter than for spring or fall conditions. In this tidal environment, MMHg production in surface sediments and its subsequent release is estimated to be the major source of MMHg to the water column during winter and spring time. However, during the more productive summer period, the Hg methylation extent in the water column may be very significant and equivalent to the sediment contribution.
机译:考虑到单甲基汞(MMHg)可能向水生生物体内蓄积,在具有生物生产能力的沿海地区进行汞循环特别重要。在中生环礁泻湖阿尔卡雄湾(法国西南部)的三个不同季节进行了野外试验,以评估水柱浓度,沉积物-水交换以及MMHg的潜在形成和降解的变化。目的是评估潮间带滩涂对MMHg产生的贡献以及汞物种出口的各种途径。在整个潮汐周期中,测量潮汐滩下游水柱中Hg物种的溶解和总体浓度。沉积物-水界面处的Hg底栖通量是通过三个不同站的底栖室确定的。使用同位素示踪剂测定表层沉积物和水柱中的汞甲基化和脱甲基化潜力。潮汐调查显示,汞的底栖迁移主要与退潮期间的沉积物侵蚀和对流有关。但是,发现在退潮时观察到的溶解汞浓度升高是由孔隙水渗漏,底流和水柱中的甲基化共同引起的。在冬季后期,底栖通量更加强烈(中值MMHg和无机汞(IHg)通量分别为64和179 pmol m(-2)h(-1)),随后在春季下降(中值0.7和-5 pmol m (-2)h(-1))和下降(中位数分别为-0.4和-1.3 pmol m(-2)h(-1))。甲基化和脱甲基化趋势与通量相反,冬季比春季或秋季低两倍。在这种潮汐环境中,估计在冬季和春季,表层沉积物中MMHg的产生及其随后的释放是MMHg进入水柱的主要来源。但是,在夏季多产的时期,水柱中的汞甲基化程度可能非常显着,相当于沉积物的贡献。

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