Periclase
MgO
none (not an EOS fit) · Cited · 2000
Why this differs from similar rows?
Cites Isaak et al. [1989] (single crystal + sound velocity, 300-1800 K); sibling row cites a different original study (Jackson and Niesler 1982).
V₀
—
Unknown basis
K₀
161.600
GPa
Isothermal
K′
—
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
- unknownsingle crystal + sound velocity
- Sample
- Isaak et al. [1989] single crystal
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: Isaak et al. [1989], single crystal + sound velocity, P 10-4 GPa, T range 300-1800 K, KT 161.6 GPa (no K' reported).
Additional notes
P range GPa
10-4
T range K
300-1800