Bridgmanite
MgSiO3
Birch-Murnaghan (order unspecified) · Original · 2015
V₀
24.45
cm³/mol
Molar
K₀
252
GPa
Isothermal
K′
4.380
dimensionless
Volume (V₀)
| Value | Unit | Basis | Z |
|---|---|---|---|
| 24.45 | 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
- perovskite (unspecified)
- Method
- unknownsimultaneous optimization of heat capacity, thermal expansion, adiabatic bulk modulus, and P–V–T measurements
- Sample
- Table 1, Perovskite 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. Parameters of equations of state... Perovskite: V0, cm3/mol = 24.45; K0, GPa = 252.0; K′ = 4.38; k = 5. 'An equation of state for perovskite was set up with the use of the P–V–T measurements from (Katsura et al., 2009c; Tange et al., 2012)... as well as measurements of volume at ambient pressure (Knittle et al., 1986; Ross and Hazen, 1989) and heat capacity from (Akaogi et al., 2008).'
Additional notes
U0 kJ per mol
-1472.5
theta01 K
943
m1
7.5
theta02 K
417
m2
7.5
gamma0
1.7
beta
3.0
gamma inf
0
k
5
note
Text states 'The V0 values are usually taken from reference data, and the bulk modulus under standard conditions (K0) is determined from ultrasonic measurements, i.e., recalculated from the adiabatic bulk modulus'; Table 1 caption describes all as fitted parameters obtained by simultaneous optimization.