Outer-core compositional stratification from observed core wave speed profiles
書誌事項
- 公開日
- 2010-12
- 権利情報
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- http://www.springer.com/tdm
- DOI
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- 10.1038/nature09636
- 公開者
- Springer Science and Business Media LLC
この論文をさがす
説明
Light elements must be present in the nearly pure iron core of the Earth to match the remotely observed properties of the outer and inner cores. Crystallization of the inner core excludes light elements from the solid, concentrating them in liquid near the inner-core boundary that potentially rises and collects at the top of the core, and this may have a seismically observable signal. Here we present array-based observations of seismic waves sensitive to this part of the core whose wave speeds require there to be radial compositional variation in the topmost 300 km of the outer core. The velocity profile significantly departs from that of compression of a homogeneous liquid. Total light-element enrichment is up to five weight per cent at the top of the core if modelled in the Fe-O-S system. The stratification suggests the existence of a subadiabatic temperature gradient at the top of the outer core.
収録刊行物
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- Nature
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Nature 468 (7325), 807-810, 2010-12
Springer Science and Business Media LLC
