Potassium in the Earth's core?

Potassium in the Earth's core?

The partitioning of K and Na between liquid Fe-S-O alloys and silicate melt has been determined over the pressure and temperature range 2.5-24 GPa and 1500-1900°C. In experiments with S-free Fe alloys, the alkali elements show completely lithophile behaviour. When S is added, however, K and Na begin...

Deskribapen osoa

Xehetasun bibliografikoak
Egile Nagusiak:	Gessmann, C, Wood, B
Formatua:	Journal article
Hizkuntza:	English
Argitaratua:	2002

Antzeko izenburuak

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Cooling of the Earth and core formation after the giant impact
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Lead was strongly partitioned into Earth's core and not lost to space
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The lead isotopic age of the Earth can be explained by core formation alone.
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The earth's core/
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The Lithophile Element Budget of Earth's Core
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Evidence for Turbulent Magnetic Diffusion in Earth's Core
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Isotopic evidence for silicon within the Earth's core
nork: Georg, R, et al.
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nork: Wilson, AJ, et al.
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Magnetostrophic MRI in the earth's outer core
nork: Petitdemange, L, et al.
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Understanding the effects of the core on the nutation of the Earth
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HYDROGEN IN THE EARTH’S OUTER CORE, AND ITS ROLE IN THE DEEP EARTH GEODYNAMICS
nork: V. N. Rumyantsev
Argitaratua: (2016-03-01)

New metal-silicate partition coefficients and constraints on core composition and oxygen fugacity during Earth accretion
nork: Corgne, A, et al.
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The effect of the differential rotation of the earth inner core on the free core nutation
nork: Mian Zhang, et al.
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Phase Relations of Earth’s Core-Forming Materials
nork: Tetsuya Komabayashi
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Editorial: Stratification in the Cores of Earth and Other Planets
nork: Hagay Amit, et al.
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Chemical Convection and Stratification in the Earth's Outer Core
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Experimental evidence for hydrogen incorporation into Earth’s core
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High thermal conductivity of the Earth's core and geodynamo
nork: Reshetnyak M. Yu.
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Superrotation of Earth’s Inner Core, Extraterrestrial Impacts, and the Effective Viscosity of Outer Core
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