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Ferropericlase

(Fe0.875,Mg0.125)O (Mg x = 0.125)

third-order Birch-Murnaghan · Original · 2017

Why this differs from similar rows?

Table I, high-spin (HS) phase value for Mg x = 0.125 (K0,T=139 GPa); sibling row is the low-spin (LS) phase of the same composition, K' fixed to 4.1 for both.

V₀
143.1
a.u.³/f.u.
Formula unit
K₀
139
GPa
Isothermal
K′
4.100
dimensionless

Volume (V₀)

Value Unit Basis Z
143.1 a.u.³/f.u. Formula unit
21.2052 ų canonical (converted)

Reported value and unit are preserved as extracted. Z (formula units per cell) is not stored yet, so molar ↔ ų/f.u. conversion is not applied automatically.

Composition

OxideMolar
MgO0.125
FeO0.875

Formula: (Mg0.125Fe0.875)O

Conditions & method

Tref
1160 K
Pref
Structure
B1 rocksalt (Fm-3m)
Method
DFT+U / DFT+DMFT
DFT+DMFT total-energy calculations
Sample
Table I row Mg_x = 0.125, HS phase

Source

Paper
Pressure-induced spin-state transition of iron in magnesiowüstite (Fe,Mg)O
Authors
I. Leonov; Alena V. Ponomareva; Roman Nazarov; Igor A. Abrikosov
DOI
10.1103/physrevb.96.075136
Year
2017
Journal
Physical review. B./Physical review. B
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

TABLE I row Mg_x=0.125: V0=143.1 a.u.^3/f.u., K_{0,T}^{HS}=139 GPa; 'K' ≡ dK/dP is fixed to 4.1 for all Mg compositions'; fit of DFT+DMFT total-energy results to third-order Birch-Murnaghan EOS at T = 1160 K.

Additional notes

P tr GPa
82
delta V abs au3 per fu
8.3
delta V over V percent
8