极地研究

极地研究 ›› 2001, Vol. 12 ›› Issue (1-English): 48-52.

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Preliminary research on the transmission path of nssSO42- and NO3- in Antarctic ice sheet

 Zhang Mingjun1, Li Zhongqin2, Qin Dahe2, Xiao Cunde2, Yang Huian2, Kang Jiancheng3 and Li Jun4   

  1. 1 State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    2 Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    3 Polar Research Institute of China, Shanghai 200129, China;
    4 Antarctic CRC and Australian Antarctic Division, Hobart 7001, Australia      
  • 出版日期:1951-03-30 发布日期:1951-03-30
  • 通讯作者: Zhang Mingjun

Preliminary research on the transmission path of nssSO42- and NO3- in Antarctic ice sheet

 Zhang Mingjun1, Li Zhongqin2, Qin Dahe2, Xiao Cunde2, Yang Huian2, Kang Jiancheng3 and Li Jun4   

  1. 1 State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    2 Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    3 Polar Research Institute of China, Shanghai 200129, China;
    4 Antarctic CRC and Australian Antarctic Division, Hobart 7001, Australia
  • Online:1951-03-30 Published:1951-03-30
  • Contact: Zhang Mingjun

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摘要：

The main sources of nssSO42-  and NO3- were summarized in this paper. By analyzing the spatial distribution features of major ions in Antarctic ice sheet and studying on the different time of the same volcanic event recorded by different ice cores from different regions in Antarctica, this paper intends to study the transmission path of nssSO42- and NO3-. Results show thatnssSO42- and NO3- are transmitted to the ice sheet through long distance and high altitude. The procedure of the transmission is that nssSO42- and NO3- are transmitted to the level between the top of troposphere and the bottom of stratosphere, then subsided to the ice sheet surface and spread to other regions.

关键词: Antarctic ice sheet, nssSO42-, NO3-, transmission path

Abstract:

The main sources of nssSO42-  and NO3- were summarized in this paper. By analyzing the spatial distribution features of major ions in Antarctic ice sheet and studying on the different time of the same volcanic event recorded by different ice cores from different regions in Antarctica, this paper intends to study the transmission path of nssSO42- and NO3-. Results show thatnssSO42- and NO3- are transmitted to the ice sheet through long distance and high altitude. The procedure of the transmission is that nssSO42- and NO3- are transmitted to the level between the top of troposphere and the bottom of stratosphere, then subsided to the ice sheet surface and spread to other regions.

Key words: Antarctic ice sheet, nssSO42-, NO3-, transmission path