Periclase
MgO
Birch-Murnaghan (order unspecified) · Cited · 2000
Why this differs from similar rows?
Cites Utsumi et al. [1998] (multianvil+XRD, 0-10 GPa, 300-1700 K); text notes this study's parameters differed from the authors' own (K0=153, K'=4).
V₀
—
Unknown basis
K₀
153
GPa
Isothermal
K′
4
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
| Oxide | Molar |
|---|---|
| MgO | 1 |
Formula: MgO
Conditions & method
- Tref
- 300 K
- Pref
- —
- Structure
- B1 rocksalt (Fm-3m)
- Method
- experiment (XRD / DAC / multianvil compression)multianvils + X-ray diffraction
- Sample
- Utsumi et al. [1998]
Source
- Paper
- P‐V‐T equation of state of periclase from synchrotron radiation measurements
- Authors
- Agnès Dewaele; G. Fiquet; D. Andrault; Daniel M. Häusermann
- DOI
- 10.1029/1999jb900364
- Year
- 2000
- Journal
- Journal of Geophysical Research Atmospheres
- Origin
- Cited (quoted from earlier work)
Evidence from the paper
Table 1: Utsumi et al. [1998], multianvils + X-ray diffraction, P range 0-10 GPa, T range 300-1700 K, KT 153(3) GPa, K' 4.0. Text: 'the T0 elastic parameters from the study of Utsumi et al. differed from ours (K0 = 153 GPa, K'0 = 4)'.
Additional notes
P range GPa
0-10
T range K
300-1700