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Akimotoite

MgSiO3

fourth-order Birch-Murnaghan · Original · 2002

V₀
43.61
ų
Unknown basis
K₀
210
GPa
Isothermal
K′
4.570
dimensionless

Volume (V₀)

Value Unit Basis Z
43.61 ų 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
MgO1
SiO21

Formula: MgSiO3

Conditions & method

Tref
Pref
Structure
ilmenite (akimotoite)
Method
first-principles DFT / ab initio
first-principles density functional perturbation theory (LDA) with quasi-harmonic approximation
Sample
first-principles static lattice (Table 3, Static column)

Source

Paper
First‐principles lattice dynamics and thermoelasticity of MgSiO3 ilmenite at hi…
Authors
Bijaya B. Karki; Renata M. Wentzcovitch
DOI
10.1029/2001jb000702
Year
2002
Journal
Journal of Geophysical Research Atmospheres
Origin
Original (measured or fitted in the source paper)

Evidence from the paper

Table 3. Calculated Thermodynamic and Elastic Parameters at Zero Pressure: Static column: V, Å3 43.61; K_T, GPa 210; ∂K_T/∂P 4.57; ∂2K_T/∂P2, GPa−1 −0.041. 'A series of thermal equations of state (EOS) isotherms obtained by fitting the fourth-order finite strain equation to the calculated free energy versus volume results at each temperature'.

Additional notes

d2KT dP2 GPa-1
-0.041
T condition
static (athermal, no zero-point motion)
volume basis note
volume appears to be per formula unit (footnote a: 'Volume per unit formula [Horiuchi et al., 1982]')
phase scope note
MgSiO3 ilmenite framed as important in transition zone and uppermost part of the lower mantle