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南极阿德雷岛湖泊沉积210Pb、137Cs定年及其环境意义

孙立广 谢周清 赵俊琳 项亮

湖泊科学2001,Vol.13Issue(1):93-99,7.
湖泊科学2001,Vol.13Issue(1):93-99,7.

南极阿德雷岛湖泊沉积210Pb、137Cs定年及其环境意义

210pb, 137Cs Dating of Lake Sediments from Ardley Island(Maritime Antarctic) and Their Environmental Implications

孙立广 1谢周清 1赵俊琳 2项亮3

作者信息

  • 1. 中国科学技术大学极地研究室,合肥230026
  • 2. 北京师范大学环境科学研究所,北京100875
  • 3. 中国科学院南京地理与湖泊研究所,南京210008
  • 折叠

摘要

Abstract

The activity of 210Pb and 137Cs of lake sediments, namely Y2 and G, respectively from Ardley Island,Antarctica have been measured. According to the profiles of 210Pb and 137Cs activity, we used CRS model to date the G lake, which spans about 134 ± 43 years. Base on the dating, we estimate the velocity of deposition. The increased sedimentation rates and the inventories of 210Pb and 137Cs as well as their flux being higher than the atmospheric deposition could be reasonably attributed to the supply of a great amount of ice-melt water.

关键词

南极湖泊沉积物210Pb137Cs定年

分类

天文与地球科学

引用本文复制引用

孙立广,谢周清,赵俊琳,项亮..南极阿德雷岛湖泊沉积210Pb、137Cs定年及其环境意义[J].湖泊科学,2001,13(1):93-99,7.

基金项目

国家自然科学基金(40076032)和中国科学院创新项目(KZCX2-303)联合资助 (40076032)

湖泊科学

OACSCD

1003-5427

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