Abstract
Using density functional theory+Hubbard U (DFT+U) calculations, we investigate the spin states and nuclear hyperfine interactions of iron incorporated in magnesium silicate (MgSiO 3) post-perovskite (Ppv), a major mineral phase in the Earth's D" layer, where the pressure ranges from ~120 to 135GPa. In this pressure range, ferrous iron (Fe 2+) substituting for magnesium at the dodecahedral (A) site remains in the high-spin (HS) state; intermediate-spin (IS) and low-spin (LS) states are highly unfavorable. As to ferric iron (Fe 3+), which substitutes magnesium at the A site and silicon at the octahedral (B) site to form (Mg,Fe)(Si,Fe)O 3 Ppv, we find the combination of HS Fe 3+ at the A site and LS Fe 3+ at the B site the most favorable. Neither A-site nor B-site Fe 3+ undergoes a spin-state crossover in the D" pressure range. The computed iron quadrupole splittings are consistent with those observed in Mössbauer spectra. The effects of Fe 2+ and Fe 3+ on the equation of state of Ppv are found nearly identical, expanding the unit cell volume while barely affecting the bulk modulus.
Original language | English (US) |
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Pages (from-to) | 1-7 |
Number of pages | 7 |
Journal | Earth and Planetary Science Letters |
Volume | 331-332 |
DOIs | |
State | Published - May 15 2012 |
Bibliographical note
Funding Information:This work is supported by the NSF grants EAR-0810272 , EAR-1047629 , and partially by the MRSEC Program of NSF grants DMR-0212302 and DMR-0819885 . We thank Peter Blaha for valuable discussions on the calculations of EFG via the WIEN2k code. All calculations were performed at the Minnesota Supercomputing Institute (MSI).
Copyright:
Copyright 2012 Elsevier B.V., All rights reserved.
Keywords
- D" layer
- Equation of state
- Fe-bearing post-perovskite (MgSiO )
- Ferrous and ferric iron (Fe and Fe )
- LDA+U
- Lower mantle
- Quadrupole splittings
- Spin state crossover