在西南极洲的火核中稳定同位素比 (δ18O和δD)
Manoela B P Portella1,2, Jefferson C Simões1,2,3, Ronaldo T Bernardo2
1Universidade Federal do Rio Grande do Sul, Programa de Pós-graduação em Geociências, Av. Bento Gonçalves, 9500, 91540-000 Porto Alegre, RS, Brazil.
Anais da Academia Brasileira de Ciencias
|December 21, 2023
概括
西南极洲冰芯分析显示了13年的气候记录 (1990-2003). 高度的积累率和同位素数据表明强烈的海洋蒸发和湿度受影响的水分来源.
科学领域:
- * 古气候学 古代气候学
- * * 冰川学 冰川学
- * 同位素地质化学
背景情况:
- *冰芯BR-IC-4从西南极冰盖中提取出来.
- *22.48米的核心是在2004-2005年澳洲夏季收集的.
- * 这项研究为国际跨南极探险计划做出了贡献.
研究的目的:
- *使用冰芯数据建立一个13年的古气候记录.
- *分析南极冰的同位素组成 (δD和δ18O).
- * 调查过去的水分来源和大气条件.
主要方法:
- *气体源质谱和空腔环降光谱用于同位素分析.
- *主要离子 (MS-,Na+,nssSO42-) 和微量元素 (Na,S,Sr) 的分析.
- * 基于同位素比和化学度的相对约会.
主要成果:
- *分析的冰芯部分跨越了1990年至2003年的时间.
- *平均积累率为每年0.48±0.09米水当量.
- *确定了稳定的同位素值 (δD: -314.42 ± 19.01‰, δ18O: -39.95 ± 2.05‰) 和多的过量 (3.70 ± 1.54‰).
结论:
- *高积累率可能受到雪地漂移的影响.
- * 的过量值表明有时会发生强烈的海洋蒸发.
- * 根据同位素数据,水源的相对湿度很高.
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