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Apportioning atmospheric pollution to Canadian and American sources in Kejimkujik National Park, Nova Scotia, using Pb isotopes in precipitation

机译:使用降水中的Pb同位素将大气污染分配给新斯科舍省Kejimkujik国家公园的加拿大和美国资源

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Precipitation samples were collected from July 2001 through June 2002 to determine sources of anthropogenic heavy metal pollutants to Kejimkujik National Park, Nova Scotia using Pb isotope ratios. Generally, Mean annual Pb concentrations (0.116μgl~(-1)) and depositional fluxes (151 μgm~(-2)) are lower than other reported mid-Atlantic coastal regions. Pb isotope compositions may be explained by binary mixing of anthropogenic emissions from US and Canadian sources, indicating long-range atmospheric transport of pollutants from populated and industrial regions of northeastern US and southeastern Canada. The ~(206)Pb/~(207)Pb ratios in precipitation ranged from 1.165 to 1.201, with an annual weighted mean ~(206)Pb/~(207)Pb ratio of 1.181, indicating that on an annual basis, US and Canadian sources contribute 61% and 39%, respectively, of the anthropogenic Pb (and likely other similarly behaved metal pollutants) reaching Kejimkujik Park. These results differ from those estimated by using epiphytic lichens due to one or a combination of the following possibilities: (1) some of the Pb in the lichens reflects more radiogenic local bedrock sources; (2) there has been an overall increase in the proportion of Canadian inputs since the early 1990s; (3) there was an unusually higher proportion of Pb inputs from Canadian sources during the study period; or (4) possible shifts in the isotopic composition of the Canadian and US sources that may have occurred due to increased international trade in lead and a lesser dependency on national production. As well, seasonal variations in the sources were observed, with summer and fall months having a lower mean ~(206)Pb/~(207)Pb ratio of 1.178 (more Canadian) than the winter and spring months with ~(206)Pb/~(207)Pb of 1.185 (more American).
机译:从2001年7月至2002年6月收集了降水样品,以铅同位素比率确定了新斯科舍省Kejimkujik国家公园的人为重金属污染物的来源。通常,年平均铅浓度(0.116μgl〜(-1))和沉积通量(151μgm〜(-2))低于其他报告的大西洋中部沿海地区。铅同位素的组成可以通过美国和加拿大的人为排放物的二元混合来解释,这表明来自美国东北部和加拿大东南部人口密集地区和工业区的污染物在大气中的远距离迁移。降水中〜(206)Pb /〜(207)Pb的比率在1.165至1.201之间,年加权〜(206)Pb /〜(207)Pb的比率为1.181,表明美国和美国来自加拿大的碳源分别达到到达Kejimkujik公园的人为铅(和可能的其他类似行为的金属污染物)的61%和39%。由于以下一种或多种可能性,这些结果与使用附生地衣估计的结果不同:(1)地衣中的某些Pb反映了更多的放射源性当地基岩源; (2)自1990年代初以来,加拿大投入的比例总体上增加了; (3)在研究期间,来自加拿大的铅输入比例异常高; (4)由于铅的国际贸易增加和对国内生产的依赖程度降低,加拿大和美国来源的同位素组成可能发生了变化。同样,观察到源头的季节变化,夏季和秋季月份的〜(206)Pb /〜(207)Pb平均值比〜和(206)Pb的冬季和春季月份低,平均为(178)1.178(加拿大) /〜(207)Pb为1.185(更多美国人)。

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