Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
205 papers · 1304 EOS records
2012 2 EOS records ANALYSIS OF THERMAL EXPANSIVITY OF SOLIDS UNDER HIGH PRESSURES 10.1142/s0217984912501461
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 162 | 4.150 | Stacey reciprocal K-primed | — | Cited | ||||||
| lower mantle aggregate (silicate perovs… |
|
— | — | 206 | 4.200 | Stacey reciprocal K-primed | adiabatic | Cited |
2012 4 EOS records Phase stability and elastic properties of the NAL and CF phases in the NaMg2Al5SiO12 system from first princi… 10.2138/am.2012.3915
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| CF |
|
— | 35.2 cm³/mol Molar |
213.200 | 4.120 | third-order Birch-Murnaghan | — | Original | ||||||||||
| CF |
|
— | 35.3 cm³/mol Molar |
196.500 | 4.500 | third-order Birch-Murnaghan | — | Cited | ||||||||||
| CF | CF (exp) | — | 36.3 cm³/mol Molar |
200 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||||||
| Why this differs from similar rows: Cites experimental data of Guignot and Andrault (2004); sibling row cites a different original study, Yutani et al. (1997), for the CF phase. | ||||||||||||||||||
| CF | CF (exp) | — | 36.1 cm³/mol Molar |
241 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||||||
| Why this differs from similar rows: Cites experimental data of Yutani et al. (1997); sibling row cites a different original study, Guignot and Andrault (2004), for the CF phase. | ||||||||||||||||||
2012 7 EOS records Static compression of (Mg0.83,Fe0.17)O and (Mg0.75,Fe0.25)O ferropericlase up to 58 GPa at 300, 700, and 1100… 10.2138/am.2012.3937
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
300 K | 75.849 ų Unit cell |
160 | 4.080 | third-order Birch-Murnaghan | — | Original | ||||||
| Ferropericlase |
|
300 K | 76.372 ų Unit cell |
160 | 4.220 | third-order Birch-Murnaghan | — | Original | ||||||
| Ferropericlase |
|
300 K | 77.369 ų Unit cell |
159 | 3.800 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Ferropericlase |
|
300 K | 77.369 ų Unit cell |
160 | 4.350 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Periclase |
|
300 K | — | 162.500 | — | none (not an EOS fit) | adiabatic | Cited | ||||||
| Periclase |
|
300 K | — | 159.700 | — | none (not an EOS fit) | — | Cited | ||||||
| Wüstite |
|
300 K | — | — | — | none (not an EOS fit) | adiabatic | Cited |
2011 3 EOS records Dolomite III: A new candidate lower mantle carbonate 10.1029/2011gl049519
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Fe-dolomite |
|
300 K | 321.77 ų Unit cell |
94.100 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||||||
| Fe-dolomite-III (low spin) |
|
300 K | 231.8 ų Unit cell |
184 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||||||
| Fe-dolomite-III (high spin) |
|
300 K | 239.2 ų Unit cell |
164 | 4 | third-order Birch-Murnaghan | — | Original |
2011 2 EOS records Thermal equation of state of lower-mantle ferropericlase across the spin crossover 10.1029/2011gl049915
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
300 K | 76.34 ų Unit cell |
162 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: V0/K_T0 correspond to the high-spin (HS) ferropericlase state, with V0 fixed in the fit; sibling row is the low-spin (LS) state with a different V0/K_T0 (V0 not fixed there). | ||||||||||||||
| Ferropericlase |
|
300 K | 74.4 ų Unit cell |
166 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: V0/K_T0 correspond to the low-spin (LS) ferropericlase state; sibling row is the high-spin (HS) state with a different, fixed V0/K_T0. | ||||||||||||||
2011 7 EOS records Elastic Tensor and Thermodynamic Property of Magnesium Silicate Perovskite from First-principles Calculations 10.1088/1674-0068/24/06/703…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.88 ų Unit cell |
241 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 162.12 ų Unit cell |
— | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I cites Hartree-Fock calculation ref [25] (D'Arco et al. 1994); sibling rows in this table cite different methods/sources (LDA, GGA, or experiment). | ||||||||||||||
| Bridgmanite |
|
— | 157.5 ų Unit cell |
— | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I cites first-principles LDA calculation ref [26] (Wentzcovitch et al. 1995); sibling rows cite different methods/sources (HF, other LDA studies, GGA, or experiment). | ||||||||||||||
| Bridgmanite |
|
— | 162.47 ų Unit cell |
— | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I cites first-principles LDA calculation ref [8] (Karki et al. 1997); sibling rows cite different methods/sources (HF, other LDA studies, GGA, or experiment). | ||||||||||||||
| Bridgmanite |
|
— | 164.1 ų Unit cell |
— | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I cites first-principles LDA calculation ref [11] (Wentzcovitch et al. 2004); sibling rows cite different methods/sources (HF, other LDA studies, GGA, or experiment). | ||||||||||||||
| Bridgmanite |
|
— | 168.04 ų Unit cell |
— | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I cites a first-principles GGA calculation (labeled ref [75] in the table); sibling rows cite different methods/sources (HF, LDA studies, or experiment). | ||||||||||||||
| Bridgmanite |
|
— | 162.45 ų Unit cell |
— | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I cites experimental Brillouin scattering ref [5] (Yeganeh-Haeri), the only ambient-condition experiment; sibling rows are theoretical calculations. | ||||||||||||||
2011 5 EOS records Analysis of a new two-parameter equation of state for MgO 10.1139/p11-040
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | — | 180 | 4.150 | other named EOS | — | Cited | ||||
| Periclase |
|
500 K | — | 175 | 4.210 | other named EOS | — | Cited | ||||
| Periclase |
|
1000 K | — | 160 | 4.360 | other named EOS | — | Cited | ||||
| Periclase |
|
1500 K | — | 144 | 4.530 | other named EOS | — | Cited | ||||
| Periclase |
|
2000 K | — | 128 | 4.740 | other named EOS | — | Cited |
2011 4 EOS records High Pressure Generation in a Kawai-Type Apparatus Equipped with Sintered Diamond Anvils 10.4131/jshpreview.21.272
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | — | 268 | 3.800 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Fit uses the full P-V dataset from run M868 up to >90 GPa; sibling row restricts the fit to data below 70 GPa, giving a different KT0/K'. | ||||||||||||||||
| Bridgmanite |
|
300 K | — | 257 | 4.300 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Fit restricted to the P<70 GPa subset of run M868's data; sibling row uses the full dataset to >90 GPa. Deviation above 70 GPa is noted as possibly linked to an Fe spin transition. | ||||||||||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | — | 256 | 3.800 | unknown | — | Cited | ||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | — | 253 | 4.100 | unknown | — | Cited | ||||||||
2010 4 EOS records Quantum Monte Carlo computations of phase stability, equations of state, and elasticity of high-pressure sili… 10.1073/pnas.0912130107
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Stishovite |
|
300 K | 23.56136905 ų Molar |
— | 3.700 | Vinet | — | Original | ||||
| Stishovite |
|
300 K | 23.30945504 ų Molar |
— | 4.290 | unknown | — | Cited | ||||
| alpha-PbO2-type SiO2 |
|
300 K | 22.93899326 ų Molar |
— | 4.100 | Vinet | — | Original | ||||
| alpha-PbO2-type SiO2 |
|
300 K | 23.38206555 ų Molar |
— | 3.430 | unknown | — | Cited |
2010 5 EOS records HIGHER ORDER THERMOELASTIC PROPERTIES OF THE EARTH LOWER MANTLE AND CORE 10.1142/s0217979210055238
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin |
|---|---|---|---|---|---|---|---|---|
| lower mantle (bulk Earth lower mantle, … | aggregate lower mantle (not a single mineral phase) | — | — | 206.090 | 4.060 | unknown | adiabatic | Original |
| Why this differs from similar rows: Table 1 column (a): parameters from a modified Rydberg EOS fit to seismic data; sibling row uses column (e), a different EOS formulation (Kushwah EOS), giving a different K'. | ||||||||
| lower mantle (bulk Earth lower mantle, … | aggregate lower mantle (not a single mineral phase) | — | — | 206.090 | 4.060 | other named EOS | adiabatic | Original |
| lower mantle (bulk Earth lower mantle, … | aggregate lower mantle (not a single mineral phase) | — | — | 206.090 | 4.060 | other named EOS | adiabatic | Original |
| lower mantle (bulk Earth lower mantle, … | aggregate lower mantle (not a single mineral phase) | — | — | 206.090 | 4.200 | Stacey reciprocal K-primed | adiabatic | Original |
| lower mantle (bulk Earth lower mantle, … | aggregate lower mantle (not a single mineral phase) | — | — | 206.090 | 4.200 | unknown | adiabatic | Original |
| Why this differs from similar rows: Table 1 column (e): parameters from the Kushwah EOS fit to seismic data; sibling row uses column (a), a different EOS formulation (modified Rydberg), giving a different K'. | ||||||||
2010 7 EOS records THERMODYNAMIC PROPERTIES OF MgSiO3 POST-PEROVSKITE 10.1142/s0217984910022391
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Post-perovskite |
|
— | 163.3 ų Unit cell |
219.300 | 4.400 | third-order Birch-Murnaghan | — | Original | ||||||
| Post-perovskite |
|
— | 162.9 ų Unit cell |
231.900 | 4.400 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Table 1 compilation row citing Oganov and Ono's LDA first-principles result (ref 7); other rows cite different original studies/methods (GGA, Tsuchiya, experiments). | ||||||||||||||
| Post-perovskite |
|
— | 167.6 ų Unit cell |
200 | 4.500 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Table 1 compilation row citing Oganov and Ono's GGA first-principles result (ref 7), distinct from their own LDA row and other cited studies in the same table. | ||||||||||||||
| Post-perovskite |
|
— | 163.8 ų Unit cell |
215.900 | 4.400 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Table 1 compilation row citing the first-principles result of Tsuchiya et al. (ref 31), a different original study than the other rows in this table. | ||||||||||||||
| Post-perovskite |
|
— | 162.2 ų Unit cell |
231.200 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Guignot et al. (ref 30), with V0 and K' fixed values (marked with asterisk); a different original study/fit than sibling rows. | ||||||||||||||
| Post-perovskite |
|
— | 162.9 ų Unit cell |
237 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Ono et al. (ref 29), with V0 and K' fixed values (marked with asterisk); a different original study/fit than sibling rows. | ||||||||||||||
| Post-perovskite |
|
— | 164.9 ų Unit cell |
219 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Shieh et al. (ref 28), with only K' fixed (V0, K0 reported with uncertainties); a different original study/fit than sibling rows. | ||||||||||||||
2010 1 EOS record Thermo-chemical and thermo-physical properties of the high-pressure phase anhydrous B (Mg14Si5O24): An ab-ini… 10.2138/am.2010.3368
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
298.2 K | 11.25 cm³/mol Molar |
160.900 | 4.120 | unknown | — | Cited |
2009 3 EOS records Characteristics of lateral heterogeneities with thermal and chemical origins in the pyrolitic lower mantle 10.1016/j.pnsc.2009.09.002
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 253 | 4.300 | third-order Birch-Murnaghan | adiabatic | Original | ||||||||
| Bridgmanite |
|
— | — | 253 | 4.400 | Birch-Murnaghan (order unspecified) | adiabatic | Cited | ||||||||
| Ferropericlase | (Mg1-yFey)O | — | — | 162.500 | 4.100 | third-order Birch-Murnaghan | adiabatic | Cited |
2009 5 EOS records P‐V‐T relations of MgSiO3 perovskite determined by in situ X‐ray diffraction using a large‐volume high‐pressu… 10.1029/2008gl035658
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | — | 256 | 3.800 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Primary free fit to P-V-T XRD data (19-53 GPa, 300-2300 K) yielding both K_T0 and K'_T0; sibling row instead fixes K_T0 to 253 GPa and refits only K'_T0. | ||||||||||||||
| Bridgmanite |
|
300 K | — | 253 | 4.100 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Alternative fit where K_T0 is assumed/fixed at 253 GPa and only K'_T0 is refit from the dataset; sibling row instead lets both K_T0 and K'_T0 vary freely. | ||||||||||||||
| Bridgmanite |
|
— | — | 253 | 3.900 | third-order Birch-Murnaghan | — | Cited | ||||||
| Bridgmanite |
|
— | — | 253 | — | unknown | adiabatic | Cited | ||||||
| Bridgmanite |
|
— | — | — | 3.700 | unknown | — | Cited | ||||||
2009 4 EOS records Density profile of pyrolite under the lower mantle conditions 10.1029/2008gl036759
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite | Al- and Fe-bearing Mg-perovskite in natural KLB-1 peridotite | — | 164 ų Unit cell |
245 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Davemaoite |
|
— | 45.6 ų Unit cell |
244 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Ferropericlase |
|
— | 76.44 ų Unit cell |
158 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: High-spin (HS) ferropericlase state, K0 fixed to 158 GPa from Fei et al. [2007b] (K' fixed to 4); sibling row is the low-spin (LS) state with a different fixed K0. | ||||||||||||||
| Ferropericlase |
|
— | 74.04 ų Unit cell |
170 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Low-spin (LS) ferropericlase state, K0 fixed to 170 GPa from Fei et al. [2007b] (K' fixed to 4); sibling row is the high-spin (HS) state with a different fixed K0. | ||||||||||||||
2009 6 EOS records The MgSiO3system at high pressure: Thermodynamic properties of perovskite, postperovskite, and melt from glob… 10.1029/2008jb005900
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.35 ų Unit cell |
254.700 | 4.260 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Why this differs from similar rows: Model BM3S: global inversion includes Saxena et al. [1999] static data, excludes Fiquet et al. [2000]; sibling row (BM3F) uses opposite data selection. | ||||||||||||||
| Bridgmanite |
|
— | 162.35 ų Unit cell |
257 | 3.880 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Why this differs from similar rows: Model BM3F: global inversion includes Fiquet et al. [2000] static data, excludes Saxena et al. [1999]; text notes BM3F gives higher K0S, lower K'0S than BM3S (sibling row). | ||||||||||||||
| Post-perovskite |
|
— | 162.2 ų Unit cell |
225 | 4.210 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Bridgmanite |
|
— | — | 253 | — | unknown | adiabatic | Cited | ||||||
| Bridgmanite |
|
— | — | — | 3.700 | unknown | — | Cited | ||||||
| Post-perovskite |
|
— | 162.2 ų Unit cell |
231 | 4 | second-order Birch-Murnaghan | adiabatic | Cited | ||||||
2009 10 EOS records FIRST-PRINCIPLES STUDY OF THE STRUCTURAL, ELECTRONIC AND OPTICAL PROPERTIES OF MgSiO3 AT HIGH PRESSURE 10.1142/s0129183109014242
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 168.12 Unit cell |
234.800 | 4.199 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 162.3 Unit cell |
259.500 | 3.690 | third-order Birch-Murnaghan | — | Cited | ||||||
| Bridgmanite |
|
— | 168.08 Unit cell |
235.700 | 4.294 | Vinet | — | Original | ||||||
| Bridgmanite |
|
— | 167.42 Unit cell |
230.050 | 4.142 | Vinet | — | Cited | ||||||
| Bridgmanite |
|
— | 168.04 Unit cell |
237 | 4.384 | other named EOS | — | Original | ||||||
| Post-perovskite |
|
— | 168.29 Unit cell |
223.730 | 4.152 | third-order Birch-Murnaghan | — | Original | ||||||
| Post-perovskite |
|
— | 167.64 Unit cell |
199.960 | 4.541 | third-order Birch-Murnaghan | — | Cited | ||||||
| Post-perovskite |
|
— | 168.05 Unit cell |
224.200 | 4.406 | Vinet | — | Original | ||||||
| Post-perovskite |
|
— | 168.26 Unit cell |
223.700 | 4.152 | Vinet | — | Cited | ||||||
| Post-perovskite |
|
— | 167.75 Unit cell |
226.700 | 4.684 | other named EOS | — | Original |
2009 11 EOS records PRESSURE-RELATED PHASE STABILITY OF MgSiO3and(Mg0.75, Fe0.25)SiO3 AT LOWER MANTLE CONDITION 10.1142/s0217979209053047
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.38 ų Unit cell |
262.370 | 3.870 | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Reports the Pbnm (orthorhombic) MgSiO3 polymorph from Table 1; other rows are different computed space-group polymorphs (P4mbm, Pm-3m), not repeat fits of one phase. | ||||||||||||||||
| Bridgmanite |
|
— | 164.99 ų Unit cell |
258.390 | 4.040 | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Reports the P4mbm (tetragonal) MgSiO3 polymorph from Table 1, a different computed space-group structure than the Pbnm and Pm-3m rows in the same table. | ||||||||||||||||
| Bridgmanite |
|
— | 168.33 ų Unit cell |
258.340 | 4.070 | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Reports the Pm-3m hypothetical cubic MgSiO3 polymorph from Table 1, a different computed space-group structure than the Pbnm and P4mbm rows. | ||||||||||||||||
| Bridgmanite |
|
— | 165.49 ų Unit cell |
241.630 | 4.160 | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Reports the Pm space-group Fe-bearing bridgmanite structure from Table 1; other rows are different computed polymorphs (Pmmm, P4mmm) of the same composition. | ||||||||||||||||
| Bridgmanite |
|
— | 167.57 ų Unit cell |
235.720 | 4.310 | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Reports the Pmmm space-group polymorph from Table 1, distinct from the Pm and P4mmm rows for the same composition. | ||||||||||||||||
| Bridgmanite |
|
— | 172.13 ų Unit cell |
227.670 | 4.350 | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Reports the P4mmm space-group polymorph from Table 1, distinct from the Pm and Pmmm rows for the same composition. | ||||||||||||||||
| Bridgmanite |
|
— | 162.3 ų Unit cell |
— | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cited experimental literature value (ref. 21, V0=162.300 A3) quoted for comparison with the DFT result; sibling row cites a different reference (22) with a different V0. | ||||||||||||||||
| Bridgmanite |
|
— | 162.486 ų Unit cell |
— | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cited experimental literature value (ref. 22, V0=162.486 A3) quoted for comparison; sibling row cites a different reference (21) with a different V0. | ||||||||||||||||
| Bridgmanite |
|
— | — | 259.800 | 4.060 | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | 164.03 ų Unit cell |
— | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: V0 taken from the linear V0-x relation of Hemley and Cohen; sibling row instead cites the Katsura and Ito relation (different original source and units, cm3/mol). | ||||||||||||||||
| Bridgmanite |
|
— | 24.718 cm³/mol Molar |
— | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: V0 (24.718 cm3/mol) taken from the linear V0-x relation of Katsura and Ito; sibling row instead cites the Hemley and Cohen relation (in A3). | ||||||||||||||||
2009 1 EOS record Pressure Dependence of Interatomic Separation and Thermal Expansivity for Alkali Halides and Periclase (MgO) 10.12693/aphyspola.115.709
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 17.300 | — | unknown | — | Cited |
2009 11 EOS records Dislocation modeling in calcium silicate perovskite based on the Peierls-Nabarro model 10.2138/am.2009.3003
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | — | 220 | 3.690 | unknown | — | Original | ||||||
| Davemaoite |
|
— | — | 236.600 | 3.990 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Li et al. (2006) GGA-AIMD calculation; other rows in this compilation table (Table 2) cite different original studies/methods. | ||||||||||||||
| Davemaoite |
|
— | — | 305 | 3.500 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Akber-Knutson et al. (2002) variationally-induced-breathing (VIB) calculation; other rows in this table cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | — | 241 | 4.140 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Karki and Crain (1998) first-principles LDA calculation; other rows in this table cite different original studies/methods. | ||||||||||||||
| Davemaoite |
|
— | — | 238 | 4.180 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Chizmeshya et al. (1996) first-principles LDA calculation; other rows in this table cite different original studies/methods. | ||||||||||||||
| Davemaoite |
|
— | — | 254 | 4.400 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Wentzcovitch et al. (1995) ab initio LDA calculation; other rows in this table cite different original studies/methods. | ||||||||||||||
| Davemaoite |
|
— | — | 290 | 4.370 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Sherman (1993) periodic Hartree-Fock calculation; other rows in this table cite different original studies/methods. | ||||||||||||||
| Davemaoite |
|
— | — | 246 | 4.500 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Shieh et al. (2004) experiment; other rows in this table cite different original studies/methods (both experimental and theoretical). | ||||||||||||||
| Davemaoite |
|
— | — | 236 | 3.900 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Shim et al. (2000) experiment; other rows in this table cite different original studies/methods (both experimental and theoretical). | ||||||||||||||
| Davemaoite |
|
— | — | 232 | 4.800 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Wang et al. (1996) experiment; other rows in this table cite different original studies/methods (both experimental and theoretical). | ||||||||||||||
| Davemaoite |
|
— | — | 281 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Mao et al. (1989) experiment; other rows in this table cite different original studies/methods (both experimental and theoretical). | ||||||||||||||
2008 2 EOS records Pressure correction in density-functional calculations 10.1103/physrevb.78.224103
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | 3782.3 a.u.³ Unknown basis |
177.486 | 4.026 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Car-Parrinello MD fit using LDA exchange-correlation functional; sibling row uses the GGA functional instead, giving a different V0/K0/K'. | ||||||||||||
| Periclase |
|
— | 4046.43 a.u.³ Unknown basis |
149.320 | 4.080 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Car-Parrinello MD fit using GGA exchange-correlation functional; sibling row uses the LDA functional instead, giving a different V0/K0/K'. | ||||||||||||
2008 1 EOS record EXTREME COMPRESSION BEHAVIOUR OF SOLIDS BASED ON THE ROY-ROY INVERTED EQUATION OF STATE 10.1142/s0217979208038910
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | — | 4.370 | Murnaghan | — | Cited |
2008 2 EOS records Bulk Modulus and Equation of State Under the Effect of Highv Temperature and High Pressure for MgO 10.1515/zna-2008-1-209
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
300 K | — | 180.100 | — | unknown | — | Original | ||||
| Ferropericlase |
|
300 K | — | 180.100 | — | unknown | — | Cited |
2008 10 EOS records Single-crystal elastic properties of (Mg0.987, Fe0.013)O to 9 GPa 10.2138/am.2008.2717
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
— | — | 161.100 | 4.200 | third-order Birch-Murnaghan | adiabatic | Original | ||||||
| Periclase |
|
— | — | 163.200 | 3.830 | unknown | adiabatic | Cited | ||||||
| Why this differs from similar rows: Cites Sinogeikin and Bass (2000) Brillouin-spectroscopy result; other rows in this table cite different original studies/methods for MgO. | ||||||||||||||
| Periclase |
|
— | — | 162.500 | 4.130 | unknown | adiabatic | Cited | ||||||
| Why this differs from similar rows: Cites Jackson and Niesler (1982) ultrasonic-interferometry result; other rows in this table cite different original studies/methods for MgO. | ||||||||||||||
| Periclase |
|
— | — | 162.800 | 3.850 | unknown | adiabatic | Cited | ||||||
| Why this differs from similar rows: Cites Spetzler (1970) ultrasonic-interferometry result; other rows in this table cite different original studies/methods for MgO. | ||||||||||||||
| Ferropericlase |
|
— | — | 163 | 3.900 | unknown | adiabatic | Cited | ||||||
| Ferropericlase |
|
— | — | 165.500 | 4.170 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Wüstite | Fe1-xO | — | — | 154.400 | 5.060 | unknown | adiabatic | Cited | ||||||
| Ferropericlase |
|
— | — | — | 5.490 | unknown | — | Cited | ||||||
| Why this differs from similar rows: MW sample with 27 mol% FeO (Jacobsen et al. 2002); sibling rows report 56 and 78 mol% FeO samples from the same study, with different K'. | ||||||||||||||
| Ferropericlase |
|
— | — | — | 5.530 | unknown | — | Cited | ||||||
| Why this differs from similar rows: MW sample with 56 mol% FeO (Jacobsen et al. 2002); sibling rows report 27 and 78 mol% FeO samples from the same study, with different K'. | ||||||||||||||
| Ferropericlase |
|
— | — | — | 5.550 | unknown | — | Cited | ||||||
| Why this differs from similar rows: MW sample with 78 mol% FeO (Jacobsen et al. 2002); sibling rows report 27 and 56 mol% FeO samples from the same study, with different K'. | ||||||||||||||
2008 11 EOS records Compression of single-crystal magnesium oxide to 118 GPa and a ruby pressure gauge for helium pressure media 10.2138/am.2008.2988
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | 74.698 ų Unit cell |
164.100 | 4.050 | third-order Birch-Murnaghan | non-hydrostatic ruby gauge of Mao et al.… | Original | ||||
| Why this differs from similar rows: Non-hydrostatic KCl-medium fit including the V0 data point, using the Mao et al. (1978) ruby scale; sibling rows use different data subsets or the He medium. | ||||||||||||
| Periclase |
|
— | 74.73 ų Unit cell |
163 | 4.080 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Same non-hydrostatic KCl-medium data as sibling row but with the V0 point excluded from the fit, giving a different V0/K0/K'. | ||||||||||||
| Periclase |
|
— | 74.69 ų Unit cell |
164.600 | 4.030 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Same KCl-medium data as sibling rows but with K' fixed to 4.03 following Zha et al. (2000), instead of fitting K' freely. | ||||||||||||
| Periclase |
|
— | 74.687 ų Unit cell |
159.600 | 3.740 | third-order Birch-Murnaghan | quasi-hydrostatic ruby gauge of Mao et al… | Original | ||||
| Why this differs from similar rows: Three-parameter fit to all He-medium data from all three runs (Mao et al. 1986 ruby scale plus diamond-Raman for six highest points); differs from the KCl-medium fits. | ||||||||||||
| Periclase |
|
— | 74.697 ų Unit cell |
159.500 | 3.740 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Same He-medium data as sibling row but excluding the six highest-pressure points (diamond-Raman-derived pressures), using ruby pressures only. | ||||||||||||
| Periclase |
|
— | 74.695 ų Unit cell |
160.200 | 3.709 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: He-medium fit with KT0 fixed to 160.2 GPa for direct comparison with Speziale et al. (2001), instead of fitting KT0 freely as in sibling He-medium rows. | ||||||||||||
| Periclase |
|
— | — | 165 | 3.740 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Re-analysis of the published He-only P-V data of Speziale et al. (2001), not this study's own KCl/He run data, with a 3rd-order BM EOS. | ||||||||||||
| Periclase |
|
— | — | 160.200 | 3.990 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Why this differs from similar rows: Cites Speziale et al. (2001) polycrystalline He-medium result (KT0 fixed 160.2 GPa, K'=3.99); sibling row instead cites the Zha et al. (2000) primary MgO scale. | ||||||||||||
| Periclase |
|
— | 74.53 ų Unit cell |
170 | 3.590 | third-order Birch-Murnaghan | — | Cited | ||||
| Periclase |
|
— | — | 160.200 | 4.030 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Why this differs from similar rows: Cites the Zha et al. (2000) primary MgO pressure scale (KT0=160.2 GPa, K'=4.03); sibling row instead cites Speziale et al. (2001), which has a different K'. | ||||||||||||
| Periclase |
|
— | 74.698 ų Unit cell |
— | — | none (not an EOS fit) | — | Cited | ||||