原行星盘的同位素演化以及地球和月球的构建块
Martin Schiller1, Martin Bizzarro1, Vera Assis Fernandes2,3
1Centre for Star and Planet Formation and Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5-7, DK-1350, Denmark.
Nature
|March 23, 2018
概括
太阳系内部的同位素变化不是由于空间差异,而是原行星盘内的同位素的快速变化. 这种与早期太阳质量积累相关的快速变化影响了我们对行星形成和地球月球系统的理解.
科学领域:
- 星球科学
- 宇宙化学
- 同位素地化学
背景情况:
- 太阳系物体中的核合成同位素变异性告诉石和行星的遗传关系.
- 之前的研究表明原行星盘的空间异质性,使地球和月球的构建块不受限制.
研究的目的:
- 研究太阳系内部核合成同位素变化的主要驱动因素.
- 用同位素重新评估陆地行星和地球月球系统的积累历史.
主要方法:
- 在石 (石,石),维斯塔,火星和地球中测量质量独立的48Ca/44Ca比率.
- 同位素组成与母体/行星质量的相关性分析 (积累时间表).
- 来自普通石的同位素分析.
主要成果:
- 内太阳系的同位素变化主要是由原行星盘固体的快速变化驱动的,而不是空间异质性.
- 在质量独立的48Ca/44Ca比率和积累时间尺度之间存在正相关性.
- 圆柱体揭示出同位素变异的全部范围,表明了早期原行星盘的快速组成变化.
结论:
- 在地球行星形成区域的同位素组成的世俗演变被推断出来.
- 建议在早期太阳质量积累过程中将外太阳系物质混合到内部盘中.
- 该模型预测地球和月球的同位素组成相同,如果月球形成的撞击涉及到晚期积聚的物体.
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