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Ferropericlase

(Mg0.22Fe0.78)O

third-order Birch-Murnaghan · Original · 2017

Why this differs from similar rows?

This study's cubic fit to single-crystal data in helium medium, 1.8-55.5 GPa; other rows use neon medium, a different pressure range/structure, or Zhuravlev et al. (2010) data.

V₀
78.87
ų
Unit cell
K₀
148
GPa
Isothermal
K′
4.090
dimensionless

Volume (V₀)

Value Unit Basis Z
78.87 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
MgO0.22
FeO0.78

Formula: (Mg0.22Fe0.78)O

Conditions & method

Tref
300 K
Pref
Structure
B1 rocksalt (Fm-3m)
Method
experiment (XRD / DAC / multianvil compression)
single-crystal X-ray diffraction (SXRD), diamond-anvil cell, He pressure medium
Sample
Mw78 single crystal in helium medium

Source

Paper
Single-crystal equations of state of magnesiowüstite at high pressures
Authors
Gregory J. Finkelstein; Jennifer M. Jackson; W. Sturhahn; Dongzhou Zhang; E. Ercan; T. S. Toellner
DOI
10.2138/am-2017-5966
Year
2017
Journal
American Mineralogist
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

The best fit-parameters for a crystal with cubic structure in helium are K0T = 148(3) GPa, K'0T = 4.09(12), and V0 = 78.87(6) Å3. Table 3: This Study (cubic), (Mg0.22Fe0.78)O, Helium, SXRD, 1.8-55.5 GPa.

Additional notes

P range GPa
1.8-55.5
V0 prior
Prior of V0 = 78.94 ± 0.1 Å3 (measured ambient unit-cell volume from ALS 11.3.1) used during equation of state fit
fitting software
MINUTI (ver.2.0)