Table 5 Parameters for calculating the Gibbs free energy of the end members of Bdm and Fper
From: Phase relations of bridgmanite, the most abundant mineral in the Earth’s lower mantle
F0 (kJ mol−1) | V0 (cm3mol−1) | K (GPa) | K′ | Θ0 | γ0 | q0 | |
|---|---|---|---|---|---|---|---|
MgSiO3 (Bdm) | −1362.443 | 24.45 | 251 | 4.1 | 880 | 1.54 | 0.84 |
FeSiO3 (Bdm) | −1002.663 | 25.32 | 271 | 4.01 | 746 | 1.54 | 0.84 |
FeFeO3 (Bdm) | −537(5) | 29.55 | 157 | 4 | 444(13) | 1.54 | 0.84 |
AlAlO3 (Bdm) | −1517.729 | 24.94 | 242 | 4.1 | 858 | 1.54 | 0.84 |
FeAlO3 (Bdm) | −1107(3) | 26.90 | 220 | 4.1 | 697(8) | 1.54 | 0.84 |
MgAlO2.5 (Bdm) | −1379(5) | 26.65 | 155 | 4.1 | 799(3) | 1.54 | 0.84 |
MgO (Fper) | −569.527 | 11.25 | 161 | 3.9 | 771 | 1.45 | 1.55 |
Fe2+O (Fper) | −243.652 | 12.26 | 161 | 4 | 454 | 1.45 | 1.55 |
