← Browse · Wüstite

Wüstite

Fe0.99O

third-order Birch-Murnaghan · Original · 2000

Why this differs from similar rows?

Fit to Fe0.99O data excluding points above 6 GPa; sibling row uses the full P<14 GPa dataset instead, giving a higher K0 (161 GPa).

V₀
Unknown basis
K₀
150
GPa
Unknown
K′
dimensionless

Volume (V₀)

Value Unit Basis Z
Unknown basis

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
FeO0.99

Formula: Fe0.99O

Conditions & method

Tref
Pref
Structure
B1 rocksalt (Fm-3m)
Method
experiment (XRD / DAC / multianvil compression)
high-pressure synchrotron powder X-ray diffraction in diamond anvil cell (N2 pressure medium)
Sample
two-phase sample of nearly stoichiometric wüstite (Fe0.99O) and metastable iron-rich magnetite; volumes from (200) reflection; data points P > 6 GPa excluded

Source

Paper
Effect of defect clustering on the high-pressure behaviour of wüstite. High-pre…
Authors
Camilla Haavik; Svein Stølen; Michael Hanfland; C. Richard A. Catlow
DOI
10.1039/b006026g
Year
2000
Journal
Physical Chemistry Chemical Physics
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

The bulk modulus of Fe0.99O is 161 ± 10 GPa when using all data for P < 14 GPa, while it is 150 ± 10 GPa when the data points for P > 6 GPa are not included in the analysis. The bulk modulus values for the two compositions are equal within the experimental uncertainty.

Additional notes

ambient lattice parameter
432.6 ± 0.2 pm at ambient conditions
Kp note
K0' fixed to 4 was stated explicitly for the Fe0.925O analysis; same BM3 treatment implied for Fe0.99O but not explicitly restated