在沃斯托克湖水热过程和水交换的限制来自同位素
P Jean-Baptiste1, J R Petit, V Y Lipenkov
1Laboratoire des Sciences du Climat et de l'Environnement, CEA/CNRS, Centre d'études de Saclay, 91191 Gif sur Yvette, France. pjb@lsce.saclay.cea.fr
Nature
|May 25, 2001
概括
在南极洲沃斯托克湖的同位素分析.
科学领域:
- 地质化学 地质化学
- 冰川学的冰川学
- 同位素分析分析 同位素分析
背景情况:
- 沃斯托克湖是南极洲最大的冰下湖,埋在3,7504,100米的冰下.
- 从重新结的湖水中形成的积累冰提供了对冰下环境的洞察力.
- 冰中的同位素为冰下湖泊过程提供了独特的标志物.
研究的目的:
- 为了调查伏斯托克湖积累的冰中的起源.
- 评估湖内水热或地幔驱动的能源潜力.
- 为了估计湖泊的水更新时间.
主要方法:
- 在来自沃斯托克站钻孔的冰芯样本中分析同位素 (3He/4He比率).
- 检查代表冰川冰和积累的湖冰之间的边界的冰块.
- 模拟流量和预算以确定湖泊更新时间.
主要成果:
- 积累的冰表现出的丰富,具有大陆地特征的放射性同位素签名.
- 测量的3He/4He比率与来自高能地幔或热水过程的显著输入不一致.
- 估计的气预算表明,湖水更新时间约为5000年.
结论:
- 沃斯托克湖的源源自周围的古老大陆地.
- 显著的热水或地幔驱动的热源不太可能影响湖泊.
- 沃斯托克湖具有相对较长的水更新时间表,大约为数千年.
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