ADVANCES IN POLAR SCIENCE ›› 1997, Vol. 8 ›› Issue (1-English): 33-36.

• Contents • Previous Articles     Next Articles

210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica

 Zhao Ye1 and Xu Cuihua2   

  1. 1Institute fo Resources and Environmental Sciences, Beijing Normal University, Beijing 100875, China 2Laboratory of Industrial Hygiene, Ministry of Public Health, Beijing 100088, China
  • Online:1947-03-30 Published:1947-03-30
  • Contact: Zhao Ye
  • Supported by:

    This project was supported by National Natural Science Foundation (49501008) and the State Antarctic Committee of China.

Abstract:

The results of 210Pb measurements in the lake sediment core from Antarctica are reported: the relative specific activities of 210Pb in the lake sediment were found to decrease exponentially with the depth in the study area; the sedimentation rate of the lake is about 0.072 cm/a. This paper shows that 210Pb method is applicable to Antarctic lake sediment ,and during the 1960's the atmospheric nuclear tests have an effect on the rate of 210Pb deposition in Antarctica.

Key words: Antarctica, Great Wall Station, lake sediment core, 210Pb method