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首页> 外文期刊>Chemosphere >Mercury in the unconfined aquifer of the Isonzo/Soca River alluvial plain downstream from the Idrija mining area
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Mercury in the unconfined aquifer of the Isonzo/Soca River alluvial plain downstream from the Idrija mining area

机译:Idrija矿区下游的Isonzo / Soca河冲积平原的无限制含水层中的汞

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摘要

AbstractThis work aims at evaluating mercury (Hg) occurrence, spatial distribution and speciation in groundwater of the Isonzo/Soča River upper alluvial plain downstream from the Idrija Hg mine (Western Slovenia). Several wells and piezometers were sampled both in static and dynamic mode. Total (THg) and filtered (FHg) concentrations were generally higher in static (THg, 1.87–855 ng L−1; FHg, 0.20–13.61 ng L−1) than in dynamic mode (THg, 0.08–78.77 ng L−1; FHg, 0.28–6.65 ng L−1). The estimated background value accounts for 2–3 ng L−1.On the basis of hydrochemistry and isotopic composition, the main sources of groundwater were established. Hg concentrations in the Slovenian sector, supplied by local rainfall, are comparable to values measured close to the Isonzo River. Possible further Hg local sources have been suggested. Stability field analysis for the aqueous Hg species revealed that in the presence of chloride Hg solubility may be increased by the formation of chlorocomplexes. Mercury that rarely enters reduced surrounding conditions can be bound to sulphur to form polysulphide species depending on the pH of water.Since Hg-contaminated alluvial sediments of the Isonzo River may act as a secondary Hg source in groundwater, a borehole was dug down to the water table. Mercury content and speciation revealed thatcinnabar(HgS) is the prevalent form followed by the matrix-bound Hg (Hgbound). Variations of the physico-chemical boundary conditions, as well as the raising/lowering of the water table, may be locally responsible for the slight variability of Hg concentrations in the aquifer.Graphical abstractDisplay OmittedHighlightsHg spatial distribution and speciation in the groundwater of the Isonzo River alluvial plain were investigated.Two sampling methods (static and dynamic) were compared to study Hg mobility.Hg content in the groundwater was not affected by the enriched alluvial deposits.Hg speciation showed that Clhas a key role in the formation of soluble species.Hg ascinnabar(HgS) was found to be the dominant form in alluvial sediments.
机译: 摘要 此工作旨在评估Isonzo /Soča河上游冲积平原下游地下水中汞(Hg)的发生,空间分布和形态。 Idrija Hg矿(斯洛文尼亚西部)。在静态和动态模式下都采样了几口井和压计。静态总浓度(THg)和过滤后浓度(FHg)通常较高(THg,1.87–855 ng L -1 ; FHg,0.20–13.61 ng L < ce:sup loc =“ post”> − 1 )比动态模式下(THg,0.08–78.77 ng L -1 ; FHg ,0.28–6.65 ng L − 1 )。估计的背景值占2–3 ng L − 1 在水化学和同位素组成的基础上,建立了地下水的主要来源。由当地降雨提供的斯洛文尼亚地区的汞浓度与在伊松佐河附近测得的值相当。建议进一步的汞本地来源。对Hg水溶液的稳定性场分析表明,在存在氯化物的情况下,Hg的溶解度可能会因形成氯配合物而增加。汞很少进入降低的环境条件,取决于水的pH值,其可以与硫结合形成多硫化物。 由于汞艾森佐河(Isonzo River)污染的冲积沉积物可能是地下水中的汞的次要来源,一个钻孔被挖到了地下水位。汞含量和形态表明,朱砂(HgS)是普遍存在的形式,其后是与基质结合的Hg(Hg 结合)。物理化学边界条件的变化以及地下水位的升高/降低可能是造成含水层中汞浓度略有变化的局部原因。 图形摘要 省略显示 突出显示 比较了两种采样方法(静态和动态)来研究汞迁移率。 < / ce:list-item> 汞含量地下水不受富集冲积层的影响。 汞的形成表明Cl -在可溶性物质的形成中起关键作用。 Hg由于朱砂(HgS)是冲积沉积物中的主要形式。

著录项

  • 来源
    《Chemosphere》 |2018年第3期|749-761|共13页
  • 作者单位

    Department of Mathematics and Geosciences, University of Trieste;

    Department of Mathematics and Geosciences, University of Trieste;

    Department of Mathematics and Geosciences, University of Trieste;

    Department of Mathematics and Geosciences, University of Trieste,Department of Chemical and Pharmaceutical Sciences, University of Trieste;

    Department of Mathematics and Geosciences, University of Trieste;

    Laboratory for Environmental and Life Sciences, University of Nova Gorica,Aerosol d.o.o.;

    Geological Survey of Slovenia;

    Department of Mathematics and Geosciences, University of Trieste;

    Department of Mathematics and Geosciences, University of Trieste;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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