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Ferropericlase

(Mg0.73Fe0.27)O

third-order Birch-Murnaghan · Original · 2005

V₀
77.3
ų
Unit cell
K₀
154
GPa
Isothermal
K′
4
dimensionless

Volume (V₀)

Value Unit Basis Z
77.3 ų Unit cell

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
MgO0.73
FeO0.27

Formula: (Mg0.73Fe0.27)O

Conditions & method

Tref
300 K
Pref
0.000 GPa
Structure
B1 rocksalt (Fm-3m)
Method
experiment (XRD / DAC / multianvil compression)
single-crystal synchrotron X-ray diffraction, diamond-anvil cell, helium pressure medium, ruby fluorescence pressure scale
Sample
sample Fe27, single crystal synthesized by interdiffusion, a0 = 4.2599 (3) Å

Source

Paper
Single-crystal synchrotron X-ray diffraction study of wüstite and magnesiowüsti…
Authors
Steven D. Jacobsen; Jung‐Fu Lin; R. J. Angel; Guoyin Shen; Vitali B. Prakapenka; Przemysław Dera; Ho-kwang Mao; Russell J. Hemley
DOI
10.1107/s0909049505022326
Year
2005
Journal
Journal of Synchrotron Radiation
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

The fitted equation-of-state parameters for this composition are V0 = 77.30 (±0.09) Å3, K0 = 154 (±3) GPa and K' = 4.0 (±0.1). Table 2: (Mg0.73Fe0.27)O, P range 0–51, V0 77.30 (±0.09), K0 154 (±3), K' 4.0 (±0.1), This study.

Additional notes

P range GPa
0-51
rho0 g cm3
4.195 (±0.005)
F f plot V0
V0 = 77.30 ± 0.02 Å3 determined experimentally per Fig. 7 caption
note
No rhombohedral distortion observed to 51 GPa; composition stated as relevant to Earth's lower mantle