在早期太阳系的外部部分反复出现的小行星形成
Wladimir Neumann1,2,3, Ning Ma4, Audrey Bouvier5
1Institute of Geodesy and Geoinformation Science, Technische Universität Berlin, Kaiserin-Augusta-Allee 104-106, 10553, Berlin, Germany. wladimir.neumann@dlr.de.
Scientific reports
|July 1, 2024
概括
太阳系外层的小行星形成发生了数百万年,其中一些形成较晚,以保存地球可居住性所必需的水. 这项研究揭示了碳状石的多样化积累时间线.
科学领域:
- 行星科学 行星科学
- 太空化学 太空化学
- 天体物理学 天体物理学
背景情况:
- 星球形成涉及到原行星盘中行星的积累.
- 石的组成反映了形成位置,有碳化 (C) 和非碳化 (NC) 组与外部和内部磁盘区域相连.
- 同位素约会提供矿物质冷却年龄,而不是直接形成年龄,需要热进化模型.
研究的目的:
- 为了限制行星小行星的形成时间,特别是在外太阳系的C石中.
- 测试原行星盘中积聚过程及其时间的场景.
- 了解积累时间在行星体中保存诸如水之类的挥发性物质中的作用.
主要方法:
- 应用最先进的热进化模型到石冷却年龄.
- 分析同位素年龄约会数据以推断母体形成时间.
- 积时间与石的变化,变形和分化的相关性.
主要成果:
- 推断太阳系形成后,从Ma到Ma的母体的临时分布积累.
- 证明C储库中的积累早在NC储库开始时就开始,并且在原行星盘的整个生命周期中发生.
- 确定了积累时间与石变化/分化程度之间的反向相关性.
结论:
- 个别的行星体迅速形成 (Ma),但不同的行星体在磁盘的整个生命周期中反复形成.
- 雪线之外的C行星体的晚期积聚 (Ma) 保存了挥发物,包括水.
- 延迟形成富含水的行星体对于地球获得足够的水来说至关重要,从而使其可居住.
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