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Mercury dynamics in a changing coastal area over industrial and postindustrial phases: Lessons from the Venice Lagoon

机译:在工业和后工业阶段改变沿海地区的汞动态:威尼斯泻湖的课程

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During the industrial period, significant amounts of mercury (Hg) were discharged into the Venice Lagoon. Here, a spatially explicit model was implemented to reconstruct the temporal evolution of the total mercury (HgT) and methylmercury (MeHgT) concentrations in lagoon water and sediments over two centuries (1900-2100), from preindustrial to postindustrial phases. The model simulates the transport and transformations of particulate and dissolved Hg species. It is forced with time-variable Hg inputs and environmental conditions, including scenarios of future atmospheric deposition, reconstructed according to local and global socioeconomic scenarios. Since 1900, -36 Mg of Hg_r and -380 kg of MeHg_r were delivered to the lagoon, and stored in the sediments. The deposition of Hg from the water to the seafloor increased during a period of eutrophication (1980s): however, the reverse fluxes increased during a period of high sediment resuspension caused by the unregulated fishing of Manila clams (1990s). In the current postindustrial phase, the lagoon sediments have acted as a secondary source to the lagoon waters, delivering Hg (-38 kg y~(-1_)) and MeHg (-0.07 kgy~(-1_). The MeHg inputs from the watershed (~0.28 kg y~(-1)) appear to be higher than the secondary fluxes from the sediments. The estimated Hg_r export to the Adriatic Sea is ~56 kg y~(-1). Since Hg_r and MeHg_r outputs slightly exceed inputs, the concentrations are slowly decreasing. While the decreasing trend is maintained in all scenarios, the future level of atmospheric deposition will affect Hg concentrations and sediment recovery times. Though limited by inherent simplifications, this work results show that the reconstruction of historical dynamics using a holistic approach, supported by data, can improve our understanding of the pollutants distribution and the quantification of local emissions. Downscaling from trends predicted at the global scale taking into account for regional differences seems useful to investigate the pollutants fate.
机译:在工业期间,大量的汞(Hg)排入威尼斯泻湖。这里,实施了空间显式模型,以重建总汞(HGT)和甲基汞(MEHGT)浓度在两世纪(1900-2100)中的泻湖水和沉积物中的汞和甲基汞(MeHGT)浓度的时间演变,从预生产到后期阶段。该模型模拟了颗粒和溶解的Hg物种的运输和转化。它被强制使用时间变量的HG输入和环境条件,包括未来大气沉积的情景,根据当地和全球社会经济情景重建。自1900年以来,-36mg HG_R和-380千克MEHG_R送到泻湖,并储存在沉积物中。在富营养化的时期(2080年)期间,从水中沉积来自水到海底增加:然而,在由Manila Clams(1990年代)的未调节捕鱼引起的高沉沉积期间,反向助熔剂增加。在当前的后期阶段,泻湖沉积物充当泻康龙水的次级源,递送hg(-38kg y〜(-1_))和mehg(-0.07 kgy〜(-1_)。来自的emhg输入流域(约0.28kg y〜(-1))似乎高于沉积物的二次助焊剂。估计的hg_r导出到亚得里亚海是〜56 kg y〜(-1)。由于HG_R和MEHG_R输出略微超过输入,浓度慢慢降低。虽然在所有情况下维持下降的趋势,但是大气沉积的未来水平将影响Hg浓度和沉积物恢复时间。虽然受到固有的简化的限制,但这种工作结果表明使用历史动态的重建通过数据支持的整体方法可以改善我们对污染物分布和当地排放量化的理解。从全球范围内预测的趋势考虑到区域差异令人抵消似乎有用似乎有用污染物命运。

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  • 来源
    《The Science of the Total Environment》 |2020年第15期|140586.1-140586.15|共15页
  • 作者单位

    National Institute of Oceanography and Applied Geophysics - OGS Trieste Italy;

    National Institute of Oceanography and Applied Geophysics - OGS Trieste Italy;

    National Institute of Oceanography and Applied Geophysics - OGS Trieste Italy;

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