在平流层颗粒中检测到4He,为外星起源提供了证据
R S Rajan1, D E Brownlee, D Tomandl
1Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, D.C. 98195, USA.
Nature
|May 12, 1977
概括
科学家在平流层粒子中检测到高度的-4 (4He),证实它们是真正的微石. 这一发现表明外星人起源,并且在进入过程中大气的升温最小.
科学领域:
- 宇宙尘埃研究 宇宙尘埃研究
- 行星科学 行星科学
- 大气化学 大气化学
背景情况:
- 微流星是小行星间的粒子,预计可以在进入大气层时幸存下来.
- 最近的平流层粒子收集表明外星起源,因为元素组成与原始石相匹配.
研究的目的:
- 调查平流层粒子的组成,以确认它们的微流星状况.
- 在收集的颗粒中识别太阳风暴露和最小大气加热的证据.
主要方法:
- 在两年内收集了微米大小的平流层粒子.
- 要素组成分析,与原始石进行比较.
- 在粒子中检测到-4 (4He) 度.
主要成果:
- 在几个平流层粒子中检测到大量的-4 (4He).
- 4He的存在表明暴露于太阳风.
- 的保留表明粒子在进入大气层时没有受到显著的摩擦加热.
结论:
- 检测到的-4证实了平流层粒子是真正的微石.
- 这些粒子提供了外星物质的证据,这些物质与地球大气层的相互作用最小.
- 这些发现支持惠普尔关于微型石生存的预测.
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