来自Kilauea火山的空气颗粒中的丰富:1983年1月
概括
基拉韦亚火山的火山排放含有高水平的,这是此前在此类喷发中未见过的元素. 这表明基拉韦亚是基拉韦亚.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 大气科学 大气科学
背景情况:
- 在Mauna Loa天文台采集空气中的颗粒物样本,监测全球颗粒物循环.
- 1983年1月 Kilauea火山爆发提供了一个分析火山排放的机会.
研究的目的:
- 为了分析来自 Kilauea 喷发的空气中的颗粒物的元素组成.
- 调查火山排放中不寻常的元素丰富,特别是.
主要方法:
- 在Mauna Loa天文台的空气过器上收集空气中的颗粒物.
- 收集过器样本的元素分析,以确定各种元素的度.
主要成果:
- 样本显示预期的高度的,,,黄金和硫.
- 检测到异常高度的,与的比率是夏威夷玄武岩的17000倍.
- 丰富与火山气体中高含量相关.
结论:
- 基拉韦亚火山喷发的丰富表明,一个不寻常的火山系统可能被地幔岩所滋养.
- 这些发现表明,可以作为一种挥发性化合物释放出来,例如与相关的六化 (IrF6).
- 这项研究强调了在火山排放中发现新兴地质化学过程的潜力.
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