Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
105 papers · 412 EOS records
1993 2 EOS records Ab initiomolecular dynamics with variable cell shape: Application toMgSiO3 10.1103/physrevlett.70.3947
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 259 | 3.900 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Ab initio calculation for the Pbnm (orthorhombic) phase (K0=259, K'0=3.9); sibling row is for a distinct hypothetical cubic phase of the same composition (K0=258, K'0=4.0). | ||||||||||||||
| Bridgmanite |
|
— | — | 258 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Ab initio calculation for a hypothetical cubic phase (K0=258, K'0=4.0); sibling row is for the Pbnm (orthorhombic) phase of the same composition (K0=259, K'0=3.9). | ||||||||||||||
1990 4 EOS records Constraints on lower mantle composition and temperature from density and bulk sound velocity profiles 10.1029/gl017i008p01153
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.46 cm³ Molar |
269 | 4 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Bridgmanite |
|
300 K | 25.49 cm³ Molar |
269 | 4 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Periclase |
|
300 K | 11.25 cm³ Molar |
162.700 | 4.100 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Wüstite |
|
300 K | 12.25 cm³ Molar |
179.700 | 3.600 | third-order Birch-Murnaghan | adiabatic | Cited |
1990 1 EOS record Calculated elastic and thermal properties of MGO at high pressures and temperatures 10.1029/jb095ib05p07055
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | — | 183.100 | 3.950 | third-order Birch-Murnaghan | — | Original |
1990 1 EOS record Fundamental thermodynamic relations and silicate melting with implications for the constitution of D″ 10.1029/jb095ib12p19311
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.46 cm³/mol Molar |
266 | 3.900 | third-order Birch-Murnaghan | — | Cited |
1990 3 EOS records Elasticity, shear‐mode softening and high‐pressure polymorphism of wüstite (Fe1‐xO) 10.1029/jb095ib13p21671
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Wüstite |
|
— | — | 154.900 | 4.900 | third-order Birch-Murnaghan | adiabatic | Original | ||||
| Why this differs from similar rows: Reports isothermal pressure derivative (dKS/dP)_T=4.90 from ultrasonic Cij(P) data, used with Birch-Murnaghan extrapolation; sibling row reports isentropic derivative instead. | ||||||||||||
| Wüstite |
|
— | — | 152.300 | 4.920 | third-order Birch-Murnaghan | — | Original | ||||
| Wüstite |
|
— | — | 154.900 | 4.840 | third-order Birch-Murnaghan | adiabatic | Original | ||||
| Why this differs from similar rows: Reports the isentropic pressure derivative (dKS/dP)_S = 4.84, derived from the isothermal value (4.90, sibling row) via a thermodynamic identity, used to construct the Hugoniot. | ||||||||||||
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