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Periclase

MgO

third-order Birch-Murnaghan · Original · 2001

Why this differs from similar rows?

Fit with K0T fixed to 160.2 GPa from high-precision sound-velocity measurements, giving V0=74.71 and K'=3.99; marked preferred fit. Sibling row fits K0T freely.

V₀
74.71
ų
Unit cell
K₀
160.200
GPa
Isothermal
K′
3.990
dimensionless

Volume (V₀)

Value Unit Basis Z
74.71 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
MgO1

Formula: MgO

Conditions & method

Tref
300 K
Pref
Structure
B1 rocksalt (Fm-3m)
Method
experiment (XRD / DAC / multianvil compression)
energy dispersive synchrotron X-ray diffraction in diamond anvil cell, quasi-hydrostatic, 300 K; K0T fixed from sound velocity measurements
Sample
pure MgO powder, DAC with methanol-ethanol (to 10 GPa) or helium (to 52 GPa) medium

Source

Paper
Quasi‐hydrostatic compression of magnesium oxide to 52 GPa: Implications for th…
Authors
S. Speziale; Chang‐Sheng Zha; T. S. Duffy; Russell J. Hemley; Ho‐kwang Mao
DOI
10.1029/2000jb900318
Year
2001
Journal
Journal of Geophysical Research Atmospheres
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

By fixing K0T = 160.2 ± 0.2 GPa from high-precision sound velocity measurements (Table 2) we can obtain: K0T' = 3.99 ± 0.01 and V0 = 74.71 ± 0.01. Abstract: Fixing the bulk modulus K0T = 160.2 GPa, a fit of the data to the third-order Birch-Murnaghan equation of state yields: V0 = 74.71 ± 0.01 ų, (∂K0T/∂P)T = 3.99 ± 0.01.

Additional notes

preferred fit
True
thermal EOS parameters
Birch-Murnaghan-Debye: γ0 = 1.524 ± 0.025, q0 = 1.65 ± 0.4 (thermodynamic constraint), θ0 = 773 K; model with q decreasing from 1.65 at 0.1 MPa to 0.01 at 200 GPa