← Browse · Ferropericlase

Ferropericlase

(Mg0.490(3)Fe0.483(2)Ti0.027(5))O (Fp48, 48 mol% FeO)

spin-crossover EOS · Original · 2016

Why this differs from similar rows?

High-spin (HS) state fit with K' free (4.12); sibling row is the low-spin (LS) state of the same sample, fitted with K' fixed to 4 since it was unconstrained by the data.

V₀
77.29
ų
Unit cell
K₀
160
GPa
Isothermal
K′
4.120
dimensionless

Volume (V₀)

Value Unit Basis Z
77.29 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
MgO0.49
FeO0.483
TiO20.027

Formula: (Mg0.490Fe0.483Ti0.027)O

Conditions & method

Tref
300 K
Pref
Structure
B1 rocksalt (Fm-3m)
Method
experiment (XRD / DAC / multianvil compression)
X-ray diffraction (DAC, Ne pressure medium, ruby scale)
Sample
Fp48, polycrystalline, 95% 57Fe-enriched, this study; high-spin (HS) state

Source

Paper
Equation of state and spin crossover of (Mg,Fe)O at high pressure, with implica…
Authors
Natalia Solomatova; Jennifer M. Jackson; W. Sturhahn; J. K. Wicks; Jiyong Zhao; T. S. Toellner; Bora Kalkan; William Steinhardt
DOI
10.2138/am-2016-5510
Year
2016
Journal
American Mineralogist
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

The zero-pressure bulk modulus K0T,HS for the HS state is 160(2) GPa with a K'0T,HS of 4.12(14) and a unit-cell V0,HS of 77.29(0) Å3. Table 7: (Mg0.49Fe0.48)O, V0,HS 77.29(0), K0T,HS 160(2), K'0T,HS 4.12(14), This study.

Additional notes

P tr GPa
68.8(2.7)
P tr width GPa
18.4
prior K0T HS
160 (±5) GPa
ambient measured volume
77.29(1) Å3 at 0.0(0) GPa (Table 1)