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比较泥炭和湖泊沉积物记录中的汞和锌分布与加拿大马尼托巴省弗林弗隆金属冶炼厂排放历史变化的关系。

Comparison of mercury and zinc profiles in peat and lake sediment archives with historical changes in emissions from the Flin Flon metal smelter, Manitoba, Canada.

机构信息

Geological Survey of Canada, Natural Resources Canada, 601 Booth St., Ottawa K1A 0E8, Canada.

出版信息

Sci Total Environ. 2011 Jan 1;409(3):548-63. doi: 10.1016/j.scitotenv.2010.10.041. Epub 2010 Nov 20.

Abstract

The copper-zinc smelter at Flin Flon, Manitoba, was historically the largest single Hg point-source in Canada, as well as a major source of Zn. Although emissions were reported by industry to have declined significantly since the late 1980s, these reductions have never been independently verified. Here, the histories of Hg and Zn deposition over the past century or more were determined at five lake sediment and three peat study sites in the surrounding region. At sites spanning the range from heavy to minor pollution, lake sediment Hg and Zn concentration and flux profiles increased significantly in the early 1930s after the smelter opened. Two of the three peat archives were wholly or partially compromised by either physical disturbances or biogeochemical transitions which reduced their effectiveness as atmospheric metal deposition recorders. But the remaining peat records, including a detailed recent 20 yr record at a moderately polluted site, appeared to show that substantive reductions in metal levels had occurred after the late 1980s, coincident with the reported emission reductions. However, the lake sediment results, taken at face value, contradicted the peat results in that no major declines in metal concentrations or fluxes occurred over recent decades. Mercury and Zn fluxes have in fact increased substantially since 1988 in most lakes. We suggest that this discrepancy may be explained by catchment soil saturation by historically deposited metals which are now mobilizing and leaching into lakes, as has been reported from other smelter polluted systems in Canada, whereas the upper sections of the peat cores reflected recent declines in atmospheric deposition. However, further research including instrumented wet and dry deposition measurements and catchment/lake mass balance studies is recommended to test this hypothesis, and to provide definitive data on current atmospheric metal deposition rates in the area.

摘要

曼尼托巴省弗林弗隆的铜锌冶炼厂是加拿大历史上最大的汞排放单一污染源,也是锌的主要来源之一。尽管自 20 世纪 80 年代末以来,工业界报告排放量已大幅下降,但这些降幅从未得到独立验证。在这里,在该地区的五个湖泊沉积物和三个泥炭研究点确定了过去一个多世纪以来汞和锌的沉积史。在从重度污染到轻度污染的各个地点,自冶炼厂开放以来,湖泊沉积物中的汞和锌浓度和通量剖面在 20 世纪 30 年代初期显著增加。三个泥炭档案中有两个全部或部分受到物理干扰或生物地球化学转变的影响,这些干扰或转变降低了它们作为大气金属沉积记录器的有效性。但是,其余的泥炭记录,包括在一个中度污染点的详细最近 20 年记录,似乎表明,自 20 世纪 80 年代末以来,金属水平已经实质性下降,与报告的排放量减少相吻合。然而,就表面价值而言,湖泊沉积物的结果与泥炭结果相矛盾,因为在最近几十年中,金属浓度或通量并没有大幅下降。实际上,自 1988 年以来,大多数湖泊中的汞和锌通量都大幅增加。我们认为,这种差异可以通过历史上沉积的金属使集水区土壤饱和来解释,这些金属现在正在迁移并浸出到湖泊中,这在加拿大其他受冶炼厂污染的系统中已有报道,而泥炭芯的上部则反映了最近大气沉积的下降。但是,建议进行进一步的研究,包括仪器化的干湿沉降测量和集水区/湖泊质量平衡研究,以检验这一假设,并提供该地区当前大气金属沉积率的明确数据。

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