Variability of Pb, Mn, Al and Na Concentrations is Snow Deposited from Winter to Early Summer 1998 in Livingston lsland, Antarctic Peninsula

  • Sungmin Hong (Polar Sciences Laboratory, Korea Ocean Research and Development Institute) ;
  • Lee, Gangwoong (Department of Environmental Sciences, Hankuk University of Foreign Studies) ;
  • Velde, Katja-Van de (Laboratoire de Glaciologie et Geophysique de l Environnement du CNRS, 54, rue Moliere, Domaine Universitaire) ;
  • Claude F. Boutron (Observatoire des Seciences de lUnivers, Universite, Joseph Fourier de Grenoble)
  • Published : 2000.05.01

Abstract

The concentrations of Pb, Mn, Al and Na were measured from a total of 26 snow samples collected from a 1.5-m deep snow pit in Livingston Island, South Shetland Islands, at the northern tip of the Antarctic Peninsula. Ore sampling location is great concern, because of its proximity to the southern extremity of south America, a candidate for the source regions of pollutant aerosols entering Antarctica. The mean concentrations of Pb and Mn were found to be 4.97 pg g(sup)-1 and 20.6 pgg(sup)-1, respectively. These concentrations levels are similar to those reported for recent snow at other Antarctic sites with pronounced spring maxima for both metals. Contributions form natural sources are estimated to be minor (∼16%) for Pb. For Mn, on the other hand, contribution from rock and soil dusts is found to be very important. Excess Pb over Pb from natural sources is likely to be anthropogenic, especially from South Americal. Our results show that yearly Pb fallout flux is much greater in Antarctic coastal areas than at other Antarctic locations far from the coast , indicating that the transport and deposition patterns of pollutant aerosols are not simple is Antarctica. It is also suggested that the recycling of anthropogenic Pb in seawater to the atmosphere could significantly contribute to the Pb fallout flux in the Antarctic coastal regions.

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