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Post-perovskite

MgGeO3

third-order Birch-Murnaghan · Original · 2006

V₀
179.2
ų
Unit cell
K₀
207
GPa
Isothermal
K′
4.400
dimensionless

Volume (V₀)

Value Unit Basis Z
179.2 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
GeO21

Formula: MgGeO3

Conditions & method

Tref
Pref
Structure
post-perovskite (CaIrO3-type, Cmcm)
Method
experiment (XRD / DAC / multianvil compression)
in situ synchrotron x-ray diffraction, laser-heated diamond anvil cell (experiment)
Sample
MgGeO3 pPv synthesized from orthoenstatite + Pt, laser-heated DAC

Source

Paper
Stability and equation of state of the post‐perovskite phase in MgGeO3 to 2 Mbar
Authors
Atsushi Kubo; Boris Kiefer; Guoyin Shen; Vitali B. Prakapenka; R. J. Cava; T. S. Duffy
DOI
10.1029/2006gl025686
Year
2006
Journal
Geophysical Research Letters
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

By this method, we constrained equation of state parameters of MgGeO3 pPv phase as K0 = 207 ± 5 GPa, V0 = 179.2 ± 0.7 Å3 with fixed K'0 of 4.4 (solid line in Figure 3). Table 2: MgGeO3 179.2(7) 207(5) 4.4 EXP, 1 (This study).

Additional notes

constraint
K0 and V0 constrained using semi-empirical elasticity systematics (K·V = const.) with MgSiO3 pPv reference values
pressure scale
Pt (Holmes et al. 1989), 111 reflection only
data range
data below 47 GPa excluded from EOS fit