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白令海峡水团来源的镭同位素示踪

陈敏 李艳平 邱雨生 杨俊鸿

陈敏, 李艳平, 邱雨生, 杨俊鸿. 白令海峡水团来源的镭同位素示踪[J]. 海洋学报, 2011, 33(2): 69-76.
引用本文: 陈敏, 李艳平, 邱雨生, 杨俊鸿. 白令海峡水团来源的镭同位素示踪[J]. 海洋学报, 2011, 33(2): 69-76.
CHEN Min, LI Yan-ping, QIU Yu-sheng, YANG Jun-hong. Water masses in the Bering Strait revealed by radium isotopes[J]. Haiyang Xuebao, 2011, 33(2): 69-76.
Citation: CHEN Min, LI Yan-ping, QIU Yu-sheng, YANG Jun-hong. Water masses in the Bering Strait revealed by radium isotopes[J]. Haiyang Xuebao, 2011, 33(2): 69-76.

白令海峡水团来源的镭同位素示踪

基金项目: 国际极地年中国行动计划项目;中国第3次北极科学考察资助项目;福建省自然科学基金杰出青年基金项目(2009J06026)。

Water masses in the Bering Strait revealed by radium isotopes

  • 摘要: 对白令海峡64.3°N纬向断面镭同位素的研究表明,水体中226Ra比活度、228Ra比活度和228Ra/226Ra)A.R.存在明显的纬向变化,反映出太平洋与北冰洋水体交换的多种路径。根据温度、盐度和镭同位素的水平与垂直分布,太平洋水进入北冰洋的路径可能主要有3支,分别为白令海峡西侧的阿拉德水、白令海峡东侧的阿拉斯加沿岸水和中部的白令海陆架水。2003年7月和9月对该断面西侧站位进行的复测显示,水体中的226Ra比活度、228Ra比活度和228Ra/226Ra)A.R.发生了明显变化,9月份测值均高于7月份测值,说明白令海峡西部水体在9月份可能受到西伯利亚沿岸流南向混合的影响。
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  • 收稿日期:  2010-08-12

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