首页> 外文期刊>Ambio: A Journal of the Human Environment >PCB Levels in Laminated Coastal Sediments of the Baltic Sea along Gradients of Eutrophication Revealed by Stable Isotopes (#delta#~(15)N, #delta#~ (13)C)
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PCB Levels in Laminated Coastal Sediments of the Baltic Sea along Gradients of Eutrophication Revealed by Stable Isotopes (#delta#~(15)N, #delta#~ (13)C)

机译:稳定同位素揭示的富营养化梯度波罗的海沿岸沉积物中的PCB水平(#delta#〜(15)N,#delta#〜(13)C)

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摘要

A systematic investigation of PCB in coastal sediments of the Baltic Sea was initiated in 1996 by retrieving dated subsurface layers (1992-1994) from 88 sites in 19 sheltered archipelago areas, where laminated sediments were found to be common. PCBs7 (HELCOM's standard sum of 7 congeners, 1/6 of total PCB) was quantified, as well as the abundance and isotopic composition of nutrients (N, C), in order to trace effects of eutrophication and potential influences on the turnover of PCB. In most of the areas, the median of PCBs7/C was within 70 to 120 ng g~(-1) C. This is similar to recent values in regional offshore sediments, and thus consistent with a rapid exchange between coastal and open waters. Elevated PCBs7 levels up to around 1000 ng g~(-1) C were found within 50 km from Stockholm. Here, but not in other areas, PCBs7IC increased linearly with the degree of eutrophication. This was evident from the isotopic composition of sediment N and C, reflecting local eutrophication as well as its link to freshwater input. In contrast, concentrations or ratios of nutrients in sediments were poor indicators of eutrophication. Our results demonstrate that the Stockholm watershed still is a source of both PCB and excess nutrients to the Baltic Sea, but do not support any enrichment or dilution of PCBs7/C ratios caused by eutrophication.
机译:1996年,通过从19个庇护群岛地区的88个地点取回陈旧的地下层(1992-1994年),开始了对波罗的海沿岸沉积物中PCB的系统研究,该地区被发现是常见的叠层沉积物。定量PCBs7(HELCOM标准的7个同类物的总和,占PCB总量的1/6)以及营养物的丰度和同位素组成(N,C),以追踪富营养化的影响以及对PCB周转量的潜在影响。在大多数地区,PCBs7 / C的中值在70至120 ng g(-1)C之内。这与区域性近海沉积物的最新值相似,因此与沿海和开放水域之间的快速交换相一致。在距斯德哥尔摩50公里的范围内发现PCBs7的水平升高,最高可达1000 ng g(-1)C。在这里,但在其他地区却没有,PCBs7IC随富营养化程度线性增加。从沉积物N和C的同位素组成可以明显看出这一点,反映了局部富营养化及其与淡水输入的联系。相反,沉积物中养分的浓度或比例是富营养化的不良指标。我们的结果表明,斯德哥尔摩分水岭仍然是波罗的海多氯联苯和过量养分的来源,但不支持富营养化引起的PCBs7 / C比的任何富集或稀释。

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