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Bridgmanite

MgSiO3

third-order Birch-Murnaghan · Cited · 1990

V₀
24.46
cm³/mol
Molar
K₀
266
GPa
Unknown
K′
3.900
dimensionless

Volume (V₀)

Value Unit Basis Z
24.46 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

OxideMolar
MgO1
SiO21

Formula: MgSiO3

Conditions & method

Tref
300 K
Pref
Structure
perovskite (unspecified)
Method
experiment (XRD / DAC / multianvil compression)
single-crystal X-ray (V0); high-pressure X-ray volume measurements (K0, K0')
Sample
Table 2, Perovskite row

Source

Paper
Fundamental thermodynamic relations and silicate melting with implications for …
Authors
Lars Stixrude; M. S. T. Bukowinski
DOI
10.1029/jb095ib12p19311
Year
1990
Journal
Journal of Geophysical Research Atmospheres
Origin
Cited (quoted from earlier work)

Evidence from the paper

TABLE 2. Parameters of the Fundamental Thermodynamic Relation: Crystals — Perovskite: T0 = 300 K, V0 = 24.46 (1) cm3/mol [Ross and Hazen, 1989], K0 = 266 (6) GPa [Knittle and Jeanloz, 1987], K0' = 3.9 (4) [Knittle and Jeanloz, 1987]. Text: 'V0 is taken from single-crystal X ray measurements for all the minerals. ... that for perovskite was taken from the high-pressure volume measurements of Knittle and Jeanloz [1987]. Compression studies also provided K'0 for diopside and perovskite.'

Additional notes

F0 kJ per mol
102.24 (1) [Ito and Takahashi, 1989]
theta0 K
1012 (6) [Ito and Takahashi, 1989; Knittle et al., 1986]
gamma0
1.73 (14) [Ito and Takahashi, 1989; Knittle et al., 1986]
q
1 (1) assumed for all materials
V0 source
Ross and Hazen [1989]
K0 source
Knittle and Jeanloz [1987]
Kp source
Knittle and Jeanloz [1987]
notes
Thermal parameters gamma0 and theta0 for perovskite constrained by thermal expansion data combined with the measured slope of the ilmenite-perovskite transition boundary; K0 and K0' cited from Knittle and Jeanloz [1987] high-pressure compression measurements.