Post-perovskite
MgSiO3
Birch-Murnaghan (order unspecified) · Original · 2015
V₀
24.2
cm³/mol
Molar
K₀
253.700
GPa
Isothermal
K′
4.030
dimensionless
Volume (V₀)
| Value | Unit | Basis | Z |
|---|---|---|---|
| 24.2 | cm³/mol | Molar | — |
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 |
| SiO2 | 1 |
Formula: MgSiO3
Conditions & method
- Tref
- 298.2 K
- Pref
- 0.000 GPa
- Structure
- post-perovskite (CaIrO3-type, Cmcm)
- Method
- unknownfit to P–V–T measurements (Guignot et al., 2007; Komabayashi et al., 2008; Ono et al., 2006); Prv EOS parameters used as initial approximation due to lack of ambient heat-capacity data
- Sample
- Table 1, Postperovskite column
Source
- Paper
- The equations of state of forsterite, wadsleyite, ringwoodite, akimotoite, MgSi…
- Authors
- Peter I. Dorogokupets; А. M. Dymshits; T. S. Sokolova; B. S. Danilov; Konstantin D. Litasov
- DOI
- 10.1016/j.rgg.2015.01.011
- Year
- 2015
- Journal
- Russian Geology and Geophysics
- Origin
- Original (measured or fitted in the source paper)
Evidence from the paper
Table 1. Postperovskite: V0, cm3/mol = 24.2; K0, GPa = 253.7; K′ = 4.03; k = 5. 'For lack of measurements of the heat capacity of PPrv at ambient pressure, the parameters of the equation of state for Prv were used as the initial approximation. The obtained equation of state for PPrv (Table 1) ensures a good smoothing of the P–V–T measurements from (Guignot et al., 2007; Komabayashi et al., 2008).'
Additional notes
U0 kJ per mol
-1447.9
theta01 K
943
m1
7.5
theta02 K
417
m2
7.5
gamma0
1.67
beta
2.22
gamma inf
0
k
5