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Detailed Reference Information |
Lin, J., Jacobsen, S.D. and Wentzcovitch, R.M. (2007). Electronic Spin Transition of Iron in the Earth's Deep Mantle. Eos, Transactions American Geophysical Union 88: doi: 10.1029/2007EO020001. issn: 0096-3941. |
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Electronic spin is a quantum property of every electron, associated with its intrinsic angular momentum. Though there are no suitable physical analogies to describe the spin quantum number, there are two possibilities, called spin 'up' and spin 'down.' The electronic structure of iron in minerals is generally such that valence electrons will more abundantly occupy different spatial orbitals and maintain the same spin than occupy the same spatial orbital and assume opposite spin, called 'spin-paired.' |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Mineral Physics, Mineral Physics, High-pressure behavior, Mineralogy and Petrology, Mineral and crystal chemistry |
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Journal
Eos, Transactions American Geophysical Union |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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