Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
205 papers · 1304 EOS records
2000 6 EOS records The stability and P–V–T equation of state of CaSiO3 perovskite in the Earth's lower mantle 10.1029/2000jb900183
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
300 K | 27.45 cm³/mol Molar |
236 | 3.900 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: This study's own EDXRD LHDAC fit (18-96 GPa) with V0, K0, K' fixed from Shim et al. [2000] static-compression results; only gamma0 and q fitted here. | ||||||||||||||
| Davemaoite |
|
300 K | 27.45 cm³/mol Molar |
232 | 4.800 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Bridgmanite |
|
300 K | 24.43 cm³/mol Molar |
262 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Cites literature parameter set of Jackson and Rigden [1996] (K'=4 assumed per footnote); sibling row cites a different original study (Fiquet et al. 2000). | ||||||||||||||
| Bridgmanite |
|
300 K | 24.43 cm³/mol Molar |
259.500 | 3.690 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Cites Fiquet et al. [2000] LHDAC XRD result; sibling row instead cites Jackson and Rigden [1996]'s literature parameter set. | ||||||||||||||
| Davemaoite |
|
300 K | — | 280 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Fit of earlier 300 K DAC data to 130 GPa (Tamai/Yagi, Yagi, Tarrida/Richet, Mao 1989) with K' assumed=4; authors argue this K0 is biased high by nonhydrostatic stress. | ||||||||||||||
| Davemaoite |
|
— | — | 301.400 | — | unknown | — | Cited | ||||||
2000 7 EOS records A new equation of state based on Grover, Getting and Kennedy's empirical relation between volume and bulk mod… 10.1039/a910247g
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
298.2 K | 11.25 m³/mol Molar |
161.500 | 4.769 | other named EOS | — | Original | ||||
| Periclase |
|
— | — | — | 5.400 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Mao and Bell static (nonhydrostatic/quasi-hydrostatic) compression value (Table 2); other rows in this compilation cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | — | 4.850 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Richet et al. static (quasi-hydrostatic) compression value (Table 2); other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | — | 4.680 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Inbar and Cohen molecular-dynamics value (Table 2); other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | — | 4.540 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Carter et al. shock-wave value (Table 2); other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | — | 4.290 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Chang and Barsch ultrasonic pulse superposition value (Table 2); other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | 162.500 | 4.130 | unknown | — | Cited | ||||
2000 5 EOS records Effect of defect clustering on the high-pressure behaviour of wüstite. High-pressure X-ray diffraction and la… 10.1039/b006026g
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Wüstite |
|
— | — | 150 | 4 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: K0 derived using the (200) reflection alone for volume, preferred by authors due to anisotropic broadening under slightly non-hydrostatic conditions; sibling row uses 3 reflections. | ||||||||||||
| Wüstite |
|
— | — | 167 | 4 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: K0 derived using (111)+(200)+(220) reflections combined for volume; differs from sibling row's (200)-only approach due to anisotropic broadening from non-hydrostatic conditions. | ||||||||||||
| Wüstite |
|
— | — | 161 | — | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Fit to Fe0.99O data using all points P<14 GPa; sibling row instead excludes data above 6 GPa, giving a lower K0 (150 vs 161 GPa here). | ||||||||||||
| Wüstite |
|
— | — | 150 | — | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Fit to Fe0.99O data excluding points above 6 GPa; sibling row uses the full P<14 GPa dataset instead, giving a higher K0 (161 GPa). | ||||||||||||
| Wüstite |
|
— | — | 175 | — | unknown | — | Cited | ||||
2000 6 EOS records Elasticity of MgO and a primary pressure scale to 55 GPa 10.1073/pnas.240466697
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | — | 162.500 | 3.990 | fourth-order Birch-Murnaghan | adiabatic | Original | ||||
| Periclase |
|
300 K | — | 160.200 | 4.030 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
— | — | 163.200 | 4 | fourth-order Birch-Murnaghan | adiabatic | Cited | ||||
| Why this differs from similar rows: Table 2 cites Ref. 25 (Sinogeikin & Bass), single-crystal Brillouin scattering to 18.6 GPa; sibling row cites Ref. 37, a first-principles theoretical result. | ||||||||||||
| Periclase |
|
— | — | 162.500 | 4.130 | none (not an EOS fit) | adiabatic | Cited | ||||
| Why this differs from similar rows: Table 2 cites Ref. 8 (Jackson & Niesler), ultrasonic measurements to only 3 GPa; sibling row cites a different study (Ref. 14) measured to 37 GPa. | ||||||||||||
| Periclase |
|
— | — | 162 | 4.080 | none (not an EOS fit) | adiabatic | Cited | ||||
| Why this differs from similar rows: Table 2 cites Ref. 14 (Chopelas), fluorescence side-band spectroscopy to 37 GPa; sibling row cites a different study (Ref. 8) measured only to 3 GPa. | ||||||||||||
| Periclase |
|
— | — | 159.700 | 4.260 | fourth-order Birch-Murnaghan | adiabatic | Cited | ||||
| Why this differs from similar rows: Table 2 cites Ref. 37 (Karki et al.), a first-principles theoretical calculation; sibling row cites Ref. 25, an experimental Brillouin scattering study. | ||||||||||||
2000 1 EOS record Temperature Coefficient of Sound Velocity of Perovskite-Enstatite and Lateral Thermal Heterogeneity in Earth'… 10.1088/0256-307x/17/3/022
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 263 | — | unknown | — | Cited |
2000 1 EOS record Thermal pressure in MgO and MgSiO 3 perovskite at lower mantle conditions 10.2138/am-2000-1013
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | 18.69 ų Unit cell |
160 | 4.150 | third-order Birch-Murnaghan | — | Cited |
2000 5 EOS records The MD simulation of the equation of state of MgO: Application as a pressure calibration standard at high tem… 10.2138/am-2000-2-308
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | 11.2382 cm³/mol Molar |
160.500 | 4.100 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
300 K | — | 161 | 4.100 | fourth-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
300 K | — | 160 | 4.150 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Periclase |
|
300 K | — | 157 | 4.300 | third-order Birch-Murnaghan | — | Cited | ||||
| Periclase |
|
300 K | — | 162 | 3.900 | none (not an EOS fit) | — | Cited |
2000 4 EOS records Ab initio structure of MgSiO 3 ilmenite at high pressure 10.2138/am-2000-2-309
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Akimotoite |
|
— | 252.75 ų Unit cell |
224 | 4.180 | third-order Birch-Murnaghan | — | Original | ||||||
| Akimotoite |
|
— | 262.54 ų Unit cell |
212 | — | unknown | adiabatic | Cited | ||||||
| Akimotoite |
|
— | — | 212 | 5.600 | unknown | ice VII equation of state | Cited | ||||||
| Akimotoite |
|
— | — | 212 | 7.500 | unknown | ruby fluorescence scale | Cited |
2000 3 EOS records Thermoelasticity of silicate perovskites and magnesiowustite and its implications for the Earth’s lower mantle 10.2138/am-2000-2-310
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 40.185 ų Unknown basis |
266 | 4.200 | Vinet | — | Original | ||||||
| Davemaoite |
|
— | 45.064 ų Unknown basis |
255.600 | 4.724 | Vinet | — | Original | ||||||
| Ferropericlase |
|
— | 18.682 ų Unknown basis |
160.200 | 4.521 | Vinet | — | Original |
2000 19 EOS records Compressibility of Mg<sub>0.9</sub>Al<sub>0.2</sub>Si<sub>0.9</sub>O<s… 10.2183/pjab.76.103
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 163.6 ų Unit cell |
215.400 | 7.200 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Fits K_T0' freely from all volume data (7.2, poorly constrained since compression is under 4%); sibling row fixes K_T0' to 4 instead. | ||||||||||||||||
| Bridgmanite |
|
— | 163.6 ų Unit cell |
225.500 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: K_T0' fixed to 4 (consistent with the MgSiO3 perovskite value) rather than fit freely; sibling row fits K' freely to 7.2 on the same run's data. | ||||||||||||||||
| Bridgmanite |
|
— | — | 260 | 4 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 1: DAC, polycrystalline, methanol-ethanol medium, Pmax 7 GPa; other rows in this compilation cite different original references/methods. | ||||||||||||||||
| Bridgmanite |
|
— | — | 266 | 3.900 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 2: DAC, polycrystalline, no pressure medium, Pmax 112 GPa; other rows in this compilation cite different original references/methods. | ||||||||||||||||
| Bridgmanite |
|
— | — | 247 | 4 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 3: DAC, single-crystal, methanol-ethanol-water medium, Pmax 10 GPa; other rows in this compilation cite different original references. | ||||||||||||||||
| Bridgmanite |
|
— | — | 246 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Refs. 4, 5: Brillouin scattering, single-crystal; other rows in this compilation cite different original references/methods. | ||||||||||||||||
| Bridgmanite |
|
— | — | 254 | 4 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 6: DAC, single-crystal, methanol-ethanol/Ne media, Pmax 13 GPa; other rows in this compilation cite different original references. | ||||||||||||||||
| Bridgmanite | (Mg1-xFex)SiO3 | — | — | 261 | 4 | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 264 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 8: Brillouin scattering, single-crystal; other rows in this compilation cite different original references/methods. | ||||||||||||||||
| Bridgmanite |
|
— | — | 265 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 9: infrared spectroscopy, polycrystalline and single-crystal; other rows in this compilation use Brillouin scattering instead. | ||||||||||||||||
| Bridgmanite |
|
— | — | 256 | 4 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 10: DAC, polycrystalline, argon medium, Pmax 60 GPa; other rows in this compilation cite different original references/methods. | ||||||||||||||||
| Bridgmanite |
|
— | — | 253 | 3.900 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 11: DAC, polycrystalline, argon/no medium, Pmax 94 GPa; other rows in this compilation cite different original references/methods. | ||||||||||||||||
| Bridgmanite |
|
— | — | 248 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 12 (Akamatsu et al.): molecular dynamics calculation, not an experiment, Pmax 60 GPa; other rows in this compilation are DAC experiments. | ||||||||||||||||
| Bridgmanite |
|
— | — | 216 | 4 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 21 (Yusa et al.): DAC XRD experiment, methanol-ethanol-water medium, Pmax 15 GPa; sibling row is a molecular-dynamics calculation instead. | ||||||||||||||||
| Bridgmanite |
|
— | — | 198 | — | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 234 | — | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 232 | — | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 236 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 23 (Weidner): reports Pmax 10 GPa, vs Pmax 9 GPa in the other two Weidner rows in this table; paper does not further explain the three separate values. | ||||||||||||||||
| Bridgmanite |
|
— | — | 182 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table II Ref. 12 (Akamatsu et al.): molecular dynamics calculation, Pmax 60 GPa; sibling row is a DAC XRD experiment (Yusa et al.) instead. | ||||||||||||||||
2000 2 EOS records Molecular Dynamics(MD) simulation of the elasticity of MgSiO3 perovskite and the temperature anomaly in the l… 10.2465/jmps.95.236
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 271 | 4.400 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | — | 261 | 4 | third-order Birch-Murnaghan | — | Cited |
1999 10 EOS records Seismic velocities of major silicate and oxide phases of the lower mantle 10.1029/1999jb900069
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 260 | 4.020 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | — | 264 | 4 | unknown | — | Cited | ||||||
| Davemaoite |
|
— | — | 236 | 4.420 | third-order Birch-Murnaghan | — | Original | ||||||
| Davemaoite |
|
— | — | 232 | 4.800 | unknown | — | Cited | ||||||
| Periclase |
|
— | — | 157 | 4.270 | third-order Birch-Murnaghan | — | Original | ||||||
| Periclase |
|
— | — | 162 | 4.130 | unknown | — | Cited | ||||||
| CaO (lime) |
|
— | — | 115 | 4.480 | third-order Birch-Murnaghan | — | Original | ||||||
| CaO (lime) |
|
— | — | 114 | 4.050 | unknown | — | Cited | ||||||
| Stishovite |
|
— | — | 310 | 4.240 | third-order Birch-Murnaghan | — | Original | ||||||
| Stishovite |
|
— | — | 312 | 4.300 | unknown | — | Cited |
1999 3 EOS records Single-crystal elasticity of MgO at high pressure 10.1103/physrevb.59.r14141
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 163.200 | 4 | fourth-order Birch-Murnaghan | adiabatic | Original | ||||
| Periclase |
|
— | — | 162.500 | 4.130 | finite strain (unspecified form) | adiabatic | Cited | ||||
| Why this differs from similar rows: Table I cites Ref. 9 (Jackson & Niesler), ultrasonic measurements only to 3 GPa; sibling row cites a different study (Ref. 10) measured to 7.8 GPa under nonhydrostatic conditions. | ||||||||||||
| Periclase |
|
— | — | 162.700 | 4.130 | finite strain (unspecified form) | adiabatic | Cited | ||||
| Why this differs from similar rows: Table I cites Ref. 10 (Yoneda), ultrasonic to 7.8 GPa under nonhydrostatic conditions (may bias K'); sibling row cites Ref. 9 to only 3 GPa. | ||||||||||||
1999 8 EOS records Thermal Equation of State of Aluminum-Enriched Silicate Perovskite 10.1126/science.284.5415.782
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 163.051 ų Unit cell |
234 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Table 3, Run 1 of the in situ P-V-T XRD experiment; ambient V0 fixed to the measured Run 1 unit-cell volume (163.051 A3), distinct from Runs 2 and 3. | ||||||||||||||
| Bridgmanite |
|
300 K | 163.184 ų Unit cell |
232 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Table 3, Run 2 of the in situ P-V-T XRD experiment; ambient V0 fixed to the measured Run 2 unit-cell volume (163.184 A3), distinct from Runs 1 and 3. | ||||||||||||||
| Bridgmanite |
|
300 K | 163.22 ų Unit cell |
236 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Table 3, Run 3 of the in situ P-V-T XRD experiment; ambient V0 fixed to the measured Run 3 unit-cell volume (163.220 A3), distinct from Runs 1 and 2. | ||||||||||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
1999 4 EOS records Equation of state of MgSiO 3 with the perovskite structure based on experimental measurement 10.2138/am-1999-0303
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.45 cm³/mol Molar |
261 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Model 1 fit: thermal expansivity fitted to Anderson's (1998) data (Eq. 14); sibling row (Model 2) uses a different dataset (Funamori et al. 1996, Eq. 20), giving a different K0. | ||||||||||||||
| Bridgmanite |
|
300 K | 24.45 cm³/mol Molar |
260.510 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Model 2 fit: thermal expansivity fitted to Funamori et al. (1996) data (Eq. 20), unlike sibling row (Model 1) which uses Anderson's (1998) data (Eq. 14). | ||||||||||||||
| Bridgmanite |
|
— | — | 261 | — | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Bridgmanite |
|
— | — | 264.400 | — | Mie-Grüneisen-Debye / thermal EOS | — | Cited | ||||||
1999 4 EOS records Compression of CaTiO 3 and CaGeO 3 perovskites 10.2138/am-1999-0309
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 223.764 ų Unit cell |
170.900 | 6.600 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 206.49 ų Unit cell |
194 | 6.100 | third-order Birch-Murnaghan | — | Original | ||||||
| Davemaoite |
|
— | — | 232 | — | unknown | — | Cited | ||||||
| Davemaoite |
|
— | — | 212 | — | unknown | — | Cited |
1998 8 EOS records Equation of state of MgSiO3 perovskite and its thermoelastic properties under lower mantle conditions 10.1029/97jb03672
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 160.74 ų Unit cell |
266 | 4.200 | Vinet | — | Cited | ||||||||
| Bridgmanite |
|
— | 157.5 ų Unit cell |
259 | 3.900 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cites Wentzcovitch et al. [1995] ab initio MD result (Table 1); text notes this gives volumes ~2% smaller than experiment; sibling row cites Hemley et al. [1987] PIB model instead. | ||||||||||||||||
| Bridgmanite |
|
— | 163.37 ų Unit cell |
256 | 4 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cites Hemley et al. [1987] potential-induced breathing (PIB) model result (Table 1); sibling row cites Wentzcovitch et al. [1995] ab initio MD instead. | ||||||||||||||||
| Bridgmanite |
|
— | 160.74 ų Unit cell |
266 | 4.200 | Vinet | — | Original | ||||||||
| Why this differs from similar rows: Static-lattice parameters adopted directly from Stixrude and Cohen [1993] LAPW calculation; sibling row instead adjusts only V0 to better match specific experimental runs. | ||||||||||||||||
| Bridgmanite |
|
— | 160.452 ų Unit cell |
266 | 4.200 | Vinet | — | Original | ||||||||
| Why this differs from similar rows: V0 adjusted to 160.452 A3 to match isobars of runs 3A, 3B, and 8 of Wang et al. [1994]; K0 and K0' held identical to sibling row 546's adopted values. | ||||||||||||||||
| Bridgmanite |
|
— | 161.16 ų Unit cell |
263.900 | 4.180 | Vinet | — | Original | ||||||||
| Why this differs from similar rows: Least-squares fit combining Knittle and Jeanloz [1987] P-V data with Wang et al. [1994] zero-pressure data; sibling row is an alternative V0-only adjustment of this fit. | ||||||||||||||||
| Bridgmanite |
|
— | 162.06 ų Unit cell |
263.900 | 4.180 | Vinet | — | Original | ||||||||
| Why this differs from similar rows: Alternative V0=162.06 A3 (dotted lines, Figure 14) with K0 and K0' held identical to the fitted values in sibling row 548; only V0 differs. | ||||||||||||||||
| Periclase |
|
— | — | 160.300 | 4.150 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
1998 6 EOS records First‐principles determination of elastic properties of CaSiO3 perovskite at lower mantle pressures 10.1029/98gl51952
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | 45.34 ų Unit cell |
241 | 4.140 | third-order Birch-Murnaghan | — | Original | ||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
232 | 4.800 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Wang et al. [1996] quasi-hydrostatic XRD compression result (Table 1); other rows in this comparison table cite different original studies/methods (theory vs. experiment). | ||||||||||||||
| Davemaoite |
|
— | — | 238 | 4.180 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Chizmeshya et al. [1996] all-electron LAPW calculation (Table 1); other rows cite different original studies/methods. | ||||||||||||||
| Davemaoite |
|
— | — | 254 | 4.400 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Wentzcovitch et al. [1995] plane-wave pseudopotential calculation (Table 1); other rows cite different original studies/methods. | ||||||||||||||
| Davemaoite |
|
— | — | 290 | 4.370 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Sherman [1993] periodic Hartree-Fock calculation (Table 1), noted as giving a much larger bulk modulus than other methods; other rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | — | 281 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Mao et al. [1989] diamond-anvil XRD (no pressure medium, up to 134 GPa, non-hydrostatic; Table 1); other rows cite different original studies/methods. | ||||||||||||||
1998 3 EOS records High‐pressure transformations in MgAl2O4 10.1029/98jb01575
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| CaFe2O4-type MgAl2O4 |
|
— | 240.3 ų Unit cell |
211 | 4 | second-order Birch-Murnaghan | — | Original | ||||||
| CaTi2O4-type MgAl2O4 |
|
— | 240.3 ų Unit cell |
206 | 4 | second-order Birch-Murnaghan | — | Original | ||||||
| CaFe2O4-type MgAl2O4 |
|
— | — | 241 | 4 | Birch-Murnaghan (order unspecified) | — | Cited |
1997 5 EOS records Finding the isentropic density of perovskite: Implications for iron concentration in the lower mantle 10.1029/96gl03951
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin |
|---|---|---|---|---|---|---|---|---|
| Bridgmanite | (Mg,Fe)SiO3 | — | — | — | 3.900 | unknown | — | Cited |
| Why this differs from similar rows: Cites Stixrude et al. [1992] in a compilation table (Table 1) of thermoelastic parameters; other rows in this table cite different original studies. | ||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | — | — | 4 | unknown | — | Cited |
| Why this differs from similar rows: Cites Wang et al. [1994] in the same compilation table (Table 1); other rows cite different original studies. | ||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | — | — | 3.900 | unknown | — | Cited |
| Why this differs from similar rows: Cites Anderson & Masuda [1994] in the same compilation table (Table 1); other rows cite different original studies. | ||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | — | — | 4 | unknown | — | Cited |
| Why this differs from similar rows: Cites Utsumi et al. [1995] in the same compilation table (Table 1); other rows cite different original studies. | ||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | — | — | 4 | unknown | — | Cited |
| Why this differs from similar rows: Cites Funamori et al. [1996] in the same compilation table (Table 1); other rows cite different original studies. | ||||||||
1997 11 EOS records Structure and elasticity of MgO at high pressure 10.2138/am-1997-1-207
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 159.700 | 4.260 | fourth-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
— | — | 159.400 | 4.280 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
— | — | 146 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Theory) row citing Chang and Cohen (1984) pseudopotential calculation; other rows cite different original theoretical/experimental studies. | ||||||||||||
| Periclase |
|
— | — | 155 | 4.160 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Theory) row citing Bukowinski (1985); a different original theoretical study than sibling rows in the same table. | ||||||||||||
| Periclase |
|
— | — | 172 | 4.090 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Theory) row citing Mehl and Cohen (1988) LAPW calculation; a different original study/method than sibling rows. | ||||||||||||
| Periclase |
|
— | — | 181.900 | 4.120 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Theory) row citing Isaak et al. (1990) ab initio PIB model; a different original study/method than sibling rows. | ||||||||||||
| Periclase |
|
— | — | 160.030 | 4.200 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Fei (unpublished), with a0 from Wyckoff (1963); a different original source than sibling rows. | ||||||||||||
| Periclase |
|
— | — | 157 | 4.300 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Carter et al. (1971); a different original experimental study than sibling rows. | ||||||||||||
| Periclase |
|
— | — | 162.500 | 4.130 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Jackson and Niesler (1982) ultrasonic measurement; a different original study/method than sibling rows. | ||||||||||||
| Periclase |
|
— | — | 162.500 | 4.090 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Duffy and Ahrens (1995); a different original experimental study than sibling rows. | ||||||||||||
| Periclase |
|
— | — | 162 | 4.080 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table 1 (Experiment) row citing Chopelas (1996); a different original experimental study than sibling rows. | ||||||||||||
1996 12 EOS records Thermal equation of state of CaSiO3 perovskite 10.1029/95jb03254
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | 45.58 ų Unit cell |
232 | 4.800 | third-order Birch-Murnaghan | — | Original | ||||||
| Davemaoite |
|
— | 45.71 ų Unit cell |
244 | 4.800 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Refit of Mao et al. [1989] DAC data weighting remaining points equally, low-pressure amorphized data excluded; sibling rows use different weighting/exclusion schemes on same data. | ||||||||||||||
| Davemaoite |
|
— | 45.3 ų Unit cell |
282 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Refit of Mao et al. [1989] DAC data using the entire data set weighted by pressure uncertainties; sibling rows instead exclude certain low-pressure points or weight equally. | ||||||||||||||
| Davemaoite |
|
— | 45.47 ų Unit cell |
268 | 4.300 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Refit of Mao et al. [1989] data excluding points below 1 GPa (likely amorphization), same weighting as row 508; other sibling row weights all points equally instead. | ||||||||||||||
| Davemaoite |
|
— | 45.37 ų Unit cell |
281 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Davemaoite |
|
— | — | 275 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Tarrida and Richet [1989] K0=275 GPa (DAC, no medium), one of three literature comparison values quoted; sibling row instead cites Tamai and Yagi [1989]. | ||||||||||||||
| Davemaoite |
|
— | — | 325 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Tamai and Yagi [1989] K0=325 GPa (DAC, no medium), one of three literature comparison values quoted; sibling row instead cites Tarrida and Richet [1989]. | ||||||||||||||
| Davemaoite |
|
300 K | 45.6 ų Unit cell |
233 | 4.800 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Table 2 'Weighted' fit using all four measurement runs; sibling fits instead use only run 13 alone or an unweighted scheme on the same data. | ||||||||||||||
| Davemaoite |
|
300 K | 45.61 ų Unit cell |
229 | 4.800 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Table 2 'Weighted, 2' fit using run 13 alone; sibling fits instead use all four runs (weighted) or an unweighted scheme. | ||||||||||||||
| Davemaoite |
|
300 K | 45.58 ų Unit cell |
233 | 4.800 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Table 2 'Unweighted' fit using all data without pressure-uncertainty weighting; sibling fits instead apply weighting to all four runs or to run 13 alone. | ||||||||||||||
| Davemaoite |
|
— | 27.45 cm³/mol Molar |
232 | 4.800 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: New in situ synchrotron XRD (SAM-85 cubic-anvil) measurement (Table 4), a different dataset from the Mao et al. [1989] DAC-data refits reported in sibling rows. | ||||||||||||||
| Bridgmanite |
|
— | 24.46 cm³/mol Molar |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
1996 4 EOS records Thermoelastic properties of MgSiO3 perovskite determined by in situ X ray observations up to 30 GPa and 2000 K 10.1029/95jb03732
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 162.32 ų Unit cell |
261 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: From run 1 (enstatite single crystals, flux method); V0 fitted per run while K0/K' fixed to Mao et al. [1991] values, so only V0 differs from sibling run 2. | ||||||||||||||||
| Bridgmanite |
|
300 K | 162.19 ų Unit cell |
261 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: From run 2 (enstatite single crystals, flux method); V0 was fitted per run while K0 and K' were fixed to Mao et al. [1991] values, so only V0 differs from sibling run 1. | ||||||||||||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | unknown | — | Cited | ||||||||
| Bridgmanite |
|
300 K | — | 260 | 4 | unknown | — | Cited | ||||||||
1996 10 EOS records First‐principles calculation of the equation‐of‐state, stability, and polar optic modes of CaSiO3 perovskite 10.1029/96gl02624
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | 45.04 ų Unit cell |
241.800 | 4.150 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Static-lattice LAPW calculation with RKmax=7 basis-set cutoff (Table 1); sibling rows use RKmax=8 or RKmax=9, giving slightly different converged EOS values. | ||||||||||||||
| Davemaoite |
|
— | 45.02 ų Unit cell |
241 | 4.160 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Static-lattice LAPW calculation with RKmax=8 basis-set cutoff (Table 1); sibling rows use RKmax=7 or RKmax=9 instead. | ||||||||||||||
| Davemaoite |
|
— | 45.06 ų Unit cell |
238.200 | 4.180 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Static-lattice LAPW calculation with RKmax=9 basis-set cutoff, the value the authors adopt for subsequent analysis (Table 1); sibling rows use RKmax=7 or 8. | ||||||||||||||
| Davemaoite |
|
— | 44.99 ų Unit cell |
289.900 | 4.370 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Davemaoite |
|
300 K | 45.55 ų Unit cell |
237.900 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Thermally-corrected LAPW(9) fit with K0' fixed to 4 (constrained fit, denoted by asterisk in Table 2); sibling row fits the same data with K0' free (4.29). | ||||||||||||||
| Davemaoite |
|
300 K | 45.62 ų Unit cell |
227 | 4.290 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Thermally-corrected LAPW(9) fit with K0' free (unconstrained, =4.29, per the abstract and Table 2); sibling row instead fixes K0' to 4 on the same underlying data. | ||||||||||||||
| Davemaoite |
|
300 K | 45.43 ų Unit cell |
290.500 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: PHF (Sherman, 1993) thermally-corrected fit with K0' fixed to 4 (constrained fit, denoted by asterisk); sibling row uses the same PHF data but fits K0' freely (4.45). | ||||||||||||||
| Davemaoite |
|
300 K | 45.45 ų Unit cell |
278.300 | 4.450 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: PHF (Sherman, 1993) thermally-corrected fit with K0' free (=4.45); sibling row fixes K0' to 4 on the same underlying PHF data. | ||||||||||||||
| Davemaoite |
|
300 K | 45.59 ų Unit cell |
233 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Refit of Wang et al. [1996] (WWG) XRD data with K0' fixed to 4.0; a different original dataset from the Mao et al. [1989] refit in sibling row 531. | ||||||||||||||
| Davemaoite |
|
300 K | 45.37 ų Unit cell |
281 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Refit of Mao et al. [1989] DAC data (to 134 GPa, no pressure medium) with K0' fixed to 4.0; a different original dataset from the Wang et al. [1996] refit in sibling row 530. | ||||||||||||||
1996 6 EOS records The stability and equation of state of majoritic garnet synthesized from natural basalt at mantle conditions 10.1029/96gl03027
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| majoritic garnet |
|
300 K | — | 226.200 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||||||||
| Why this differs from similar rows: Fit to the static-compression data converging to K0=226.2 GPa with K' fixed to 4.0; paper notes an equally acceptable alternative fit (sibling row) fixing K0 to 180 GPa instead. | ||||||||||||||||||||||
| majoritic garnet |
|
300 K | — | 180 | 7 | third-order Birch-Murnaghan | — | Original | ||||||||||||||
| Why this differs from similar rows: Alternative equally-acceptable fit with K0 constrained to 180 GPa (matching ambient elasticity of related garnets), giving K'=7; sibling row instead floats K0 to 226.2 GPa. | ||||||||||||||||||||||
| majoritic garnet | natural meteoritic majorite (iron-rich) | — | — | 221 | 4.400 | unknown | — | Cited | ||||||||||||||
| Stishovite |
|
— | — | 342 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||||||||
| Davemaoite |
|
— | — | 281 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||||||||
| majoritic garnet | basaltic garnet component of crustal density models | — | — | 226 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||||||||||