同位素的证据表明太阳系内部的晚期层的起源
Mario Fischer-Gödde1, Thorsten Kleine1
1Institut für Planetologie, University of Münster, Wilhelm-Klemm-Strasse 10, 48149 Münster, Germany.
Nature
|January 28, 2017
概括
地球的地幔中含有"晚期层"的石物质. 鲁同位素分析显示,这种层并非源自太阳系外的碳化,反驳了它们作为地球水和挥发物的主要来源的作用.
科学领域:
- 地质化学
- 宇宙化学
- 星球科学
背景情况:
- 地球的地幔中含有大量的 siderophile 元素,这归因于核心形成后添加的流星物质的"晚期层".
- 这个晚期层的起源 (内部与外部太阳系) 对于了解地球挥发物和水的来源至关重要.
研究的目的:
- 通过分析 (Ru) 同位素来研究地球晚期层的起源.
- 为了确定碳状石是否是地球挥发物质的潜在来源,
主要方法:
- 分析各种混凝土 (包括碳化混凝土) 中的 (Ru) 同位素组成.
- 与已知地球地幔的Ru同位素组成进行对比.
主要成果:
- 所有分析的混凝土,包括碳化混凝土,都表现出与地球地幔不同的Ru同位素组成.
- 观察到Ru同位素异常的明显趋势,从静态到普通到碳酸.
- 这种趋势表明,在更大的日中心距离形成的物质具有更大的Ru同位素异常.
结论:
- 这项研究驳斥了太阳系外层的起源.
- 晚期层可能不是地球上的挥发物和水的主要来源,这挑战了之前的假设.
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