放射性加热维持了长期存在的火山活动和超级地球上的磁力发电机
Haiyang Luo1, Joseph G O'Rourke2, Jie Deng1
1Department of Geosciences, Princeton University, Princeton, NJ, USA.
Science advances
|September 13, 2024
概括
,和等放射性元素在超级地球核心形成条件下成为 siderophile. 这改变了地幔的对流驱动器,增加了核心-地幔边界的热流,并可能为火山活动和磁力发动机提供燃料.
科学领域:
- 行星科学 行星科学
- 地质物理学 地质物理学
- 天体化学是天体化学.
背景情况:
- 从,和中产生放射性热量对于行星能源预算至关重要.
- 传统上,这些元素被认为是光电类元素,它们集中在行星地幔中.
研究的目的:
- 研究在超级地球核心形成条件下放射性元素的行为.
- 了解超级地球上地幔对流和内部热传输的影响.
主要方法:
- 对元素分区的热力学建模.
- 在高压,高温条件下模拟地幔对流.
主要成果:
- ,和在超级地球核心形成压力和温度下表现出 siderophile 行为.
- 放射性元素优先分离到核心,而不是地幔.
- 这种分隔显著提高了核心-地幔边界温度和热流.
结论:
- 超级地球上的地幔对流主要是由核心加热驱动的.
- 超级地球可能拥有持续的火山活动和强大的磁力发电机,由于核心热量流量增加.
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