Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
205 papers · 1304 EOS records
1990 8 EOS records 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 |
|
— | 18.4 ų Unit cell |
189.400 | 4.070 | fourth-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
— | 18.59 ų Unit cell |
184.600 | 4.090 | fourth-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
300 K | 18.66 ų Unit cell |
180.100 | 4.150 | fourth-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
300 K | — | 183.100 | 3.950 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
300 K | 18.66 ų Unit cell |
160.500 | 4.220 | unknown | — | Cited | ||||
| Periclase |
|
1300 K | 19.33 ų Unit cell |
150.400 | 4.460 | fourth-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
1300 K | — | 131.200 | — | unknown | — | Cited | ||||
| Periclase |
|
2000 K | 19.97 ų Unit cell |
127.600 | 4.740 | fourth-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 8 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. | ||||||||||||
| Wüstite |
|
— | — | 151.900 | 2.100 | unknown | — | Cited | ||||
| Wüstite |
|
— | — | 153.100 | 2.100 | unknown | — | Cited | ||||
| Wüstite |
|
— | — | 154 | 2.100 | unknown | — | Cited | ||||
| Wüstite |
|
— | — | 150 | 3.800 | unknown | — | Cited | ||||
| Wüstite |
|
— | — | 185 | 3.200 | Birch-Murnaghan (order unspecified) | adiabatic | Cited | ||||
1990 2 EOS records Thermodynamic Functions and Properties of MgO at High Compression and High Temperature 10.1063/1.555873
1990 2 EOS records An equation of state applied to 50 solids. II 10.1088/0953-8984/2/39/003
← Prev
Page 9 / 9