← Browse · Wüstite

Wüstite

Fe0.93O

third-order Birch-Murnaghan · Original · 2005

Why this differs from similar rows?

Rhombohedral-phase parameters back-calculated to zero pressure from a fit referenced to 28 GPa, a different approach than the direct ambient-pressure fits in sibling rows.

V₀
59.85
ų
Unit cell
K₀
132
GPa
Isothermal
K′
4.200
dimensionless

Volume (V₀)

Value Unit Basis Z
59.85 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
FeO0.93

Formula: Fe0.93O

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
same single crystal as cubic Fe0.93O, high-pressure phase above 23 GPa

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 rhombohedral phase equation-of-state parameters obtained by directly fitting the high-pressure data with a reference pressure of 28 GPa correspond to V0 = 59.85, K0 = 132 GPa and K' = 4.2.

Additional notes

derivation
back-calculated zero-pressure parameters from 28 GPa reference-pressure fit