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从快速旋转的地球形成月球:一场巨大的撞击,随后发生了共振反转
1Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA. cuk@eps.harvard.edu
概括
巨大的撞击在快速旋转的原地球上可以解释月球与地球类似的组成. 一个更快的早期地球-月球系统,然后抛弃角动量,以达到其当前状态.
科学领域:
- 行星科学 行星科学
- 地质化学 地质化学
- 天体物理学 天体物理学
背景情况:
- 地球和月球相同的同位素组成表明它们有共同的起源.
- 主流的巨大撞击假设努力解释月球的同位素相似性,因为模拟表明大多数材料应该来自撞击器.
- 之前的模型假定撞击后的角度动量比预期的要低,因为地球质量行星的积累.
研究的目的:
- 为了调查一个快速旋转的早期地球是否可以解决月球形成模型中的同位素差异.
- 探索早期地球-月球系统中角动量演变的机制.
主要方法:
- 在快速旋转的原地球上发生巨大撞击的计算机模拟.
- 模拟早期地球-月球系统中角动量演变的模型.
主要成果:
- 模拟显示,对快速旋转的原地球的冲击会产生一个主要来自地球地幔的月球形成盘.
- 较高的初始角动量使得早期的地球-月球系统可以失去多余的角动量.
- 与太阳的轨道共振被确定为角动量损失的合理机制.
结论:
- 快速旋转的早期地球是形成具有类似地球同位素特征的月球的关键.
- 早期的地球-月球系统可能具有更高的角动量,随后通过自然过程减少,以匹配当今的状态.
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