EarthRef.org Reference Database (ERR)
Development and Maintenance by the EarthRef.org Database Team

Detailed Reference Information
Lin et al. 2007
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.

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.'

BACKGROUND DATA FILES

Abstract

Keywords
Mineral Physics, Mineral Physics, High-pressure behavior, Mineralogy and Petrology, Mineral and crystal chemistry
Journal
Eos, Transactions American Geophysical Union
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
Click to clear formClick to return to previous pageClick to submit