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Bridgmanite

(Mg0.92, Fe0.08)SiO3

third-order Birch-Murnaghan · Original · 2004

V₀
Unknown basis
K₀
260.090
GPa
Adiabatic
K′
4.170
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

OxideMolar
MgO0.92
FeO0.08
SiO21

Formula: (Mg0.92Fe0.08)SiO3

Conditions & method

Tref
Pref
Structure
orthorhombic perovskite (Pbnm/Pnma)
Method
experiment (shock wave)
shock compression (Hugoniot, two-stage light gas gun) reduced via finite-strain F-f analysis
Sample
hot-pressed natural enstatite powder (Damaping Mine, Hebei, China), >98% enstatite, initial density 3.06 g/cm3 (crystal density 3.27 g/cm3)

Source

Paper
Equation of State, Phase Stability of (Mg0.92, Fe0.08)SiO3 Perovskite from Shoc…
Authors
Zizheng Gong
DOI
10.1063/1.1780510
Year
2004
Journal
AIP conference proceedings
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

A linear least squares fit of data in Fig.3 gives K0s=260.09GPa and pressure derivative K0s'=4.17, given our new value of γ, with ρ0=4.19g/cm3. ... By using the third-order Birch-Murnaghan finite strain equation of state (EOS), Our shock experimental data yield a zero-pressure bulk modulus.

Additional notes

rho0 zero pressure high pressure phase
4.19 g/cm3
Gruneisen gamma0
1.84
Gruneisen q
1.69
Gruneisen relation
gamma = gamma0 (rho0/rho)^q
Hugoniot D u relation
D = 3.76 + 1.48u (km/s), up to 140 GPa; conclusion section quotes D = 4.13 + 1.39u (km/s)
initial sample density
3.06 g/cm3 (abstract) / 3.08 g/cm3 (experiments section)
shock temperature range
about 1500-5000 K in experimental pressure range
note on Etr
Energy of transition to high-pressure phase E_tr unknown but has very small influence on K0s
no V0 reported
zero-pressure volume of high-pressure phase given only as density rho0 = 4.19 g/cm3, not as a unit-cell or molar volume