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Radioactive K may be a heat source in Earth's core

机译:放射性钾可能是地球核心的热源

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Radioactive potassium appears also to be a substantial source of heat in the Earth's core, according to recent experiments by University of California, Berkeley, geophysicists. Radioactive potassium, uranium, and thorium are thought to be the three main sources of heat in the Earth's interior, aside from that generated by the formation of the planet. Together, the heat keeps the mantle actively churning and the core generating a protective magnetic field. But geophysicists have found much less potassium in the Earth's crust and mantle than would be expected based on the composition of rocky meteors that supposedly formed the Earth. If, as some have proposed, the missing potassium resides in the Earth's iron core, how did an element as light as potassium get there, especially since iron and potassium don't mix?
机译:根据加州大学伯克利分校地球物理学家的最新实验,放射性钾似乎也是地球核心的主要热源。除了行星形成所产生的热量外,放射性钾,铀和th被认为是地球内部的三个主要热源。热量一起使地幔活跃地搅动,并且芯层产生保护磁场。但是地球物理学家发现,地壳和地幔中的钾含量要比根据推测形成地球的岩石流星的成分所预期的少得多。如果像某些人建议的那样,缺少的钾存在于地球的铁芯中,那么像钾这样轻的元素如何到达那里,尤其是由于铁和钾不会混合?

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    《Nuclear news》 |2004年第2期|p.53-54|共2页
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