Periclase
MgO
unknown · Cited · 1995
Why this differs from similar rows?
Quasi-harmonic VIB model calculation of Wolf and Bukowinski [1988] (Table 1, QH VIB column); other columns cite different original studies/methods.
V₀
18.69
ų
Unit cell
K₀
177
GPa
Isothermal
K′
—
dimensionless
Volume (V₀)
| Value | Unit | Basis | Z |
|---|---|---|---|
| 18.69 | 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
| Oxide | Molar |
|---|---|
| MgO | 1 |
Formula: MgO
Conditions & method
- Tref
- 300 K
- Pref
- —
- Structure
- B1 rocksalt (Fm-3m)
- Method
- molecular dynamicsquasi-harmonic VIB model calculation
- Sample
- Table 1, QH VIB column (Wolf and Bukowinski 1988), 300 K
Source
- Paper
- High pressure effects on thermal properties of MgO
- Authors
- Iris Inbar; R. E. Cohen
- DOI
- 10.1029/95gl01086
- Year
- 1995
- Journal
- Geophysical Research Letters
- Origin
- Cited (quoted from earlier work)
Evidence from the paper
Table 1: QH VIBb column: V [A3] 18.69; K_T [GPa] 177. b) Wolf and Bukowinski [1988]