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Bridgmanite

MgSiO3

Vinet · Original · 1998

Why this differs from similar rows?

Static-lattice parameters adopted directly from Stixrude and Cohen [1993] LAPW calculation; sibling row instead adjusts only V0 to better match specific experimental runs.

V₀
160.74
ų
Unit cell
K₀
266
GPa
Unknown
K′
4.200
dimensionless

Volume (V₀)

Value Unit Basis Z
160.74 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

OxideMolar
MgO1
SiO21

Formula: MgSiO3

Conditions & method

Tref
Pref
Structure
other / unspecified
Method
first-principles DFT / ab initio
four-parameter thermodynamic model; static parameters adopted from Stixrude and Cohen [1993] LAPW calculation
Sample
Table 2, static lattice parameters adopted in the present model

Source

Paper
Equation of state of MgSiO3 perovskite and its thermoelastic properties under l…
Authors
Juichiro Hama; Kaichi Suito
DOI
10.1029/97jb03672
Year
1998
Journal
Journal of Geophysical Research Atmospheres
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

Table 2. Static Lattice Parameters for MgSiO3 and (Mg0.9, Fe0.1)SiO3 Perovskites Used in the Present: MgSiO3 V0=160.74 Å3, K0=266.0 GPa, K0'=4.20, Θ0=994 K. 'Thus we adopt the values by Stixrude and Cohen for V0, K0, and K0' in the present paper.'

Additional notes

Theta 0
994 K (static lattice Debye temperature, determined to reproduce experimental Θ_D = 980 K at ambient conditions from Akaogi and Ito [1993])
calculated ambient volume
162.54 Å3, within experimental range 162.1-162.80 Å3 [Ross and Hazen, 1989]
derived K T0
256.4 GPa at ambient conditions (Table 3)
derived K T0 prime
4.23 at ambient conditions (Table 3)
gamma 0
1.279 (Table 3)
delta T0
5.21 (Table 3)
alpha T0
1.57e-5 K^-1
dKT dT P
-2.09e-2 GPa K^-1 (Table 3)