Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
85 papers · 347 EOS records
1994 4 EOS records Comparison between the lattice dynamics and molecular dynamics methods: Calculation results for MgSiO3 perovs… 10.1029/94gl01370
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
500 K | 24.68 cm³/mol Molar |
237 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Lattice-dynamics (LD) quasi-harmonic simulation result at 500 K/0 GPa; sibling row uses a molecular-dynamics (MD) simulation instead, giving a slightly different K_T. | ||||||||||||||
| Bridgmanite |
|
500 K | 24.7 cm³/mol Molar |
236 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Molecular-dynamics (MD) simulation (with Wigner-Kirkwood quantum corrections) at 500 K/0 GPa; sibling row uses a lattice-dynamics (LD) simulation instead. | ||||||||||||||
| Bridgmanite |
|
1000 K | 25.25 cm³/mol Molar |
200 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Lattice-dynamics (LD) quasi-harmonic simulation result at 1000 K/0 GPa; sibling row uses a molecular-dynamics (MD) simulation instead, giving K_T=208 GPa versus 200 GPa here. | ||||||||||||||
| Bridgmanite |
|
1000 K | 25.19 cm³/mol Molar |
208 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Molecular-dynamics (MD) simulation (with quantum corrections) at 1000 K/0 GPa; sibling row uses a lattice-dynamics (LD) simulation instead. | ||||||||||||||
1993 1 EOS record High pressure and high temperature in situ X‐ray observation of MgSiO3 Perovskite under lower mantle conditio… 10.1029/92gl02960
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.75 ų Unit cell |
260 | 4 | unknown | — | Cited |
1993 1 EOS record Refinement of enthalpy measurement of MgSiO3 perovskite and negative pressure‐temperature slopes for Perovski… 10.1029/93gl01265
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298 K | 24.44 cm³/mol Molar |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited |
1993 5 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). | ||||||||||||||
| Bridgmanite |
|
— | — | 279 | 3.400 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites a different ab initio study, a full-potential LAPW calculation by Cohen et al. [28], distinct from the two experimental citations in sibling rows. | ||||||||||||||
| Bridgmanite |
|
— | — | 243 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cited as the low end of an interlaboratory range, from Yeganeh-Haeri et al. [27]; sibling rows cite a different experimental study [20] or a theoretical LAPW calculation [28]. | ||||||||||||||
| Bridgmanite |
|
— | — | 266 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cited as the high end of an interlaboratory range, from Knittle and Jeanloz [20]; sibling rows cite a different experimental study [27] or a theoretical LAPW calculation [28]. | ||||||||||||||
1993 2 EOS records Computer Simulation of the Structural and Physical Properties of Minerals in the Earth's Deep-Interior. 10.5940/jcrsj.35.190
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 24.44 cm³/mol Molar |
247 | — | none (not an EOS fit) | — | Cited | ||||||
| Bridgmanite |
|
— | 24.56 cm³/mol Molar |
250 | — | unknown | — | Original |
1992 2 EOS records Thermoelasticity of Silicate Perovskite and Magnesiowüstite and Stratification of the Earth's Mantle 10.1126/science.257.5073.10…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 24.56 cm³/mol Molar |
263 | 3.900 | Birch-Murnaghan (order unspecified) | — | Original | ||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | 24.46 Molar |
— | — | Birch-Murnaghan (order unspecified) | — | Original |
1991 8 EOS records Effect of pressure, temperature, and composition on lattice parameters and density of (Fe,Mg)SiO3‐perovskites… 10.1029/91jb00176
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298 K | 162.49 ų Unit cell |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||||
| Bridgmanite |
|
298 K | 162.79 ų Unit cell |
261 | 4 | Birch-Murnaghan (order unspecified) | gold (Anderson et al., 1989); ruby R1; ne… | Original | ||||||||
| Bridgmanite |
|
298 K | 163.53 ų Unit cell |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||||
| Bridgmanite |
|
298 K | — | 246 | — | unknown | adiabatic | Cited | ||||||||
| Bridgmanite |
|
298 K | — | 247 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
| Why this differs from similar rows: Cites Kudoh et al. [1987], single-crystal XRD in a methanol-ethanol-water medium to 10 GPa; other rows in this compilation cite different original studies/samples/pressure media. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 254 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
| Why this differs from similar rows: Cites Ross and Hazen [1989], single-crystal XRD in methanol-ethanol and Ne media to 13 GPa; other rows cite different original studies/samples/pressure media. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 258 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
| Why this differs from similar rows: Cites Yagi et al. [1982], powder XRD in a methanol-ethanol medium to 7 GPa (nonhydrostatic above 7.5-9 GPa, only data below 7.5 GPa used); other rows cite different original studies/samples/pressure media. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 266 | 3.900 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
1991 2 EOS records Phase Transition and Thermal Expansion of MgSiO 3 Perovskite 10.1126/science.251.4992.410
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.725 cm³ Molar |
246.500 | 4 | unknown | — | Original | ||||||
| Bridgmanite |
|
300 K | — | — | — | unknown | — | Original |
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 | ||||||
| Bridgmanite |
|
— | — | 273 | — | unknown | adiabatic | Cited | ||||||
| Why this differs from similar rows: Cites K_S0=273 GPa from Mao and Hemley (personal communication, 1989), close to the adopted Knittle and Jeanloz value; sibling row cites a lower literature value (~245 GPa). | ||||||||||||||
| Bridgmanite |
|
— | — | — | — | unknown | adiabatic | Cited | ||||||
| Why this differs from similar rows: Cites lower K_S0~245 GPa from Kudoh et al. and Yeganeh-Haeri et al.; text says results are nearly identical if K_S0' is instead raised to ~4.5 (a proposed adjustment, not fitted). | ||||||||||||||
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 |
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