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Spatial variations of Pb, As, and Cu in surface snow along the transect from the Zhongshan Station to Dome A, East Antarctica

机译:南极东部中山站-A穹顶面雪中Pb,As和Cu的空间变化

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摘要

The spatial distributions of lead, arsenic, and copper (Pb, As, and Cu, respectively) in surface snow along the transect from the Zhongshan Station to Dome A, East Antarctica, are presented. The mean concentrations of Pb, As, and Cu are 1.04±1.56 pg/g, 0.39±0.08 pg/g, and 11.2±14.4 pg/g, respectively. It is estimated that anthropogenic contributions are dom-inant for Pb, As, and Cu. Spatially, Pb concentrations show an exponentially decreasing trend from the coast inland, while a moderate decreasing trend is observed for Cu concentrations in the coastal area (below 2,000 m above sea level (a.s.l.)). In the intermediate area (2,000–3,000 m a.s.l.), the concentrations and enrichment factors of all these elements show high variability due to the complicated characteristics of climate and environment. On the inland plateau (above 3,000 m a.s.l.), the high concentrations of As and Pb are induced by high deposition efficiency, the existence of polar stratospheric precip-itation, and the different fraction deposition to East Antarctica. The extremely high concentrations with maximum values of 9.59 pg/g and 69.9 pg/g for Pb and Cu, respectively, are suggested to result mainly from local human activities at the sta-tion. Our results suggest that source, transport pathway, and deposition pattern, rather than distance from the coast or alti-tude, lead to the spatial distributions of Pb, As, and Cu; and it is further confirmed by spatial variations of the three metals deposited over the whole continent of Antarctica.
机译:给出了从中山站到南极东部穹顶A的样地表雪中铅,砷和铜(分别为Pb,As和Cu)的空间分布。 Pb,As和Cu的平均浓度分别为1.04±1.56 pg / g,0.39±0.08 pg / g和11.2±14.4 pg / g。据估计,人为贡献主要是Pb,As和Cu。在空间上,铅的浓度从沿海内陆开始呈指数下降趋势,而在沿海地区(海拔2,000 m以下(a.s.l.))观察到铜浓度呈中等下降趋势。在中部地区(2,000-3,000 m a.s.l.),由于气候和环境的复杂特征,所有这些元素的浓度和富集因子显示出高度的可变性。在内陆高原(3,000 m a.s.l.以上),高浓度的沉积效率,极地平流层降水的存在以及南极东部的不同馏分沉积引起了高浓度的砷和铅。铅和铜的最高浓度分别为9.59 pg / g和69.9 pg / g的极高浓度,主要是由于该站的当地人类活动造成的。我们的研究结果表明,源,输运途径和沉积方式,而不是距海岸或高原的距离,导致了Pb,As和Cu的空间分布。沉积在整个南极大陆上的三种金属的空间变化进一步证实了这一点。

著录项

  • 来源
    《寒旱区科学(英文版)》 |2018年第3期|219-231|共13页
  • 作者单位

    Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210023, China;

    Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210023, China;

    Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210023, China;

    Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210023, China;

    Polar Research Institute of China, Shanghai 200136, China;

    Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210023, China;

    Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210023, China;

    Climate Change Institute, University of Maine, Orono, Maine 04469, USA;

    School of Earth and Climate Sciences, University of Maine, Orono, Maine 04469, USA;

    Climate Change Institute, University of Maine, Orono, Maine 04469, USA;

    Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210023, China;

    Polar Research Institute of China, Shanghai 200136, China;

    Climate Change Institute, University of Maine, Orono, Maine 04469, USA;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-19 03:41:28
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