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Core Theory

机译:核心理论

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摘要

Radioactive potassium, common enough on Earth to make potassium-rich bananas one of "hottest" foods around, appears also to be a substantial source of heat in the Earth's core, according to recent experiments by University of California, Berkeley (UCB) 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 the UC Berkeley 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:加州大学伯克利分校(UCB)地球物理学家最近进行的实验表明,放射性钾在地球上已经很普遍,足以使富含钾的香蕉成为周围“最热”的食物之一,但它似乎也是地球核心的重要热量来源。除了行星形成所产生的热量外,放射性钾,铀和or被认为是地球内部的三种主要热源。热量一起使地幔活跃地搅动,并且芯层产生保护磁场。但是,加州大学伯克利分校的地​​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。正如有人提出的那样,缺失的钾存在于地球的铁芯中,像钾这样的轻元素如何到达那里,尤其是由于铁和钾不会混合?

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