Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
85 papers · 347 EOS records
2004 1 EOS record Equation of State, Phase Stability of (Mg0.92, Fe0.08)SiO3 Perovskite from Shock Wave Study and Its Geophysic… 10.1063/1.1780510
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 260.090 | 4.170 | third-order Birch-Murnaghan | adiabatic | Original |
2002 9 EOS records Elasticity of (Mg,Fe)SiO3‐perovskite at high pressures 10.1029/2002gl014683
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 159.6 ų Unit cell |
264.300 | 3.940 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: EOS-derived value from a volumetric fit (V0=159.6, K0=264.3, K'=3.94) for x=0; sibling row instead reports elastic-constant-derived (VRH-averaged) moduli from Eulerian strain fits. | ||||||||||||||||
| Bridgmanite |
|
— | 160.5 ų Unit cell |
270 | 3.960 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: EOS-derived volumetric fit for x=0.25, spin-polarized with Fe on the large 4c site (V0=160.5, K0=270, K'=3.96); sibling row instead reports VRH-averaged elastic-constant moduli. | ||||||||||||||||
| Bridgmanite |
|
— | — | 263 | 4.060 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Table 1 value from third-order Eulerian strain fits to elastic constants, VRH-averaged (K=263, K'=4.06); sibling row instead reports the volumetric EOS fit (K0=264.3, K'=3.94). | ||||||||||||||||
| Bridgmanite |
|
— | — | 268 | 4.100 | third-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Table 1 value from Eulerian strain fits to elastic constants, VRH-averaged, x=0.25 (K=268, K'=4.10); sibling row instead reports the volumetric EOS fit (K0=270, K'=3.96). | ||||||||||||||||
| Bridgmanite |
|
— | — | 259 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cites Wentzcovitch et al. [1998] first-principles calculation; sibling rows cite different original studies (Karki et al. 1997; Oganov et al. 2001b). | ||||||||||||||||
| Bridgmanite |
|
— | — | 258 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cites Karki et al. [1997] first-principles calculation; sibling rows cite different original studies (Wentzcovitch et al. 1998; Oganov et al. 2001b). | ||||||||||||||||
| Bridgmanite |
|
— | — | 231 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cites Oganov et al. [2001b] GGA calculation; text explicitly attributes its substantially lower value to the GGA functional, vs LDA used by sibling rows. | ||||||||||||||||
| Bridgmanite |
|
— | — | 264 | — | unknown | adiabatic | Cited | ||||||||
| Bridgmanite |
|
— | 24.46 cm³/mol Molar |
— | — | unknown | — | Cited | ||||||||
2002 3 EOS records Molecular dynamics simulation of MgSiO3-Al2O3 perovskite. 10.2465/jmps.97.13
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298 K | — | 182 | — | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Model 1 (random coupled Al-Fe substitution) MD simulation result; sibling row is Model 2 (adjacent-pair coupled substitution) for the same composition. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 179 | — | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Why this differs from similar rows: Model 2 (adjacent-pair coupled substitution, local charge balance) MD result; sibling row is Model 1 (random coupled substitution) for the same composition. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 247.500 | — | fourth-order Birch-Murnaghan | — | Original | ||||||||
2001 6 EOS records First principles thermoelasticity of MgSiO3‐perovskite: Consequences for the inferred properties of the lower… 10.1029/2001gl012910
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 164.1 ų Unit cell |
247 | 3.970 | unknown | — | Original | ||||||||
| Bridgmanite |
|
— | 162 ų Unit cell |
259 | 4.010 | unknown | — | Original | ||||||||
| Bridgmanite |
|
300 K | 162.3 ų Unit cell |
253 | 3.900 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Table 1 experimental column cites a single source, Fiquet et al. [2000] (K0=253, K'=3.9); sibling row instead reports a value derived by combining several data sets. | ||||||||||||||||
| Bridgmanite | (Mg,Fe)SiO3 | 300 K | 162.5 ų Unit cell |
261 | 4 | unknown | — | Cited | ||||||||
| Bridgmanite |
|
300 K | — | 256 | 3.900 | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Text-stated combined value (K0=256, K'=3.9) derived from several data sets [Mao 1991; Wang 1994; Funamori 1996; Fiquet 2000], distinct from the single-source Table 1 value. | ||||||||||||||||
| Bridgmanite |
|
— | — | — | — | unknown | — | Cited | ||||||||
2001 1 EOS record Compositional constraints on the equation of state and thermal properties of the lower mantle 10.1046/j.1365-246x.2001.00…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin |
|---|---|---|---|---|---|---|---|---|
| Bridgmanite | (Mg,Fe)SiO3 with small Al2O3 admixture; atomic ratio Fe/(Fe+Mg) = f | 290 K | — | 264 | 3.800 | unknown | adiabatic | Cited |
2000 7 EOS records Thermoelastic properties and crystal structure of MgSiO3 perovskite at lower mantle pressure and temperature … 10.1029/1999gl008397
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.27 ų Unit cell |
253 | 3.900 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 162.3 ų Unit cell |
259 | 3.700 | Mie-Grüneisen-Debye / thermal EOS | — | Original | ||||||
| Bridgmanite |
|
— | 162.3 ų Unit cell |
259.500 | 3.690 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Table 3 fit (1): this study's data plus Fiquet et al. [1998], 63 data points, V0 fixed to 162.3; sibling fit (2) uses a different combined literature data set (213 points). | ||||||||||||||
| Bridgmanite |
|
— | 162.3 ų Unit cell |
267.600 | 3.780 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Table 3 fit (2): optimized from Wang et al. [1994], Funamori et al. [1996] and Saxena et al. [1999]; sibling fit (1) uses this study's data plus Fiquet et al. [1998]. | ||||||||||||||
| Bridgmanite |
|
— | — | 254 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Ross and Hazen [1990] single-crystal XRD, K'0 fixed to 4; sibling rows cite different original studies (Fiquet et al. 1998; Mao et al. 1991). | ||||||||||||||
| Bridgmanite |
|
— | — | 256 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites the authors' own previous study, Fiquet et al. [1998] (laser-heated DAC synchrotron XRD); sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 261 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Mao et al. [1991] XRD to 30 GPa, K'0=4; sibling rows cite different original studies (Ross and Hazen 1990; Fiquet et al. 1998). | ||||||||||||||
2000 2 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 | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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. | ||||||||||||||
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 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 |
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 2 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 |
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 2 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 |
1998 7 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. | ||||||||||||||||
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. | ||||||||
1996 1 EOS record Thermal equation of state of CaSiO3 perovskite 10.1029/95jb03254
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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 1 EOS record The search for a universal equation of state correct up to very high pressures 10.1088/0953-8984/8/1/008
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 40.25 ų Unit cell |
272 | 3.800 | Vinet | — | Cited |
1996 2 EOS records Chemical composition of the lower mantle inferred from the equation of state of MgSiO 3 perovskite 10.1098/rsta.1996.0053
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.46 cm³/mol Molar |
261 | 3.750 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | third-order Birch-Murnaghan | — | Original |
1995 1 EOS record Calculation models of structures and physical properties of CaSiO3, CaMgSi2O6, and Ca2BaSi3O9 crystals. 10.2465/minerj.17.290
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 261 | — | unknown | — | Cited |
1994 1 EOS record Thermoelasticity of perovskite: An emerging consensus 10.1029/94eo01093
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin |
|---|---|---|---|---|---|---|---|---|
| Bridgmanite | (Mg,Fe)SiO3 | 300 K | — | 263 | 3.900 | unknown | — | Cited |
1994 1 EOS record Thermal expansion of MgSiO3 perovskite at 20.5 GPa 10.1029/94gl00844
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 263 | 3.900 | Birch-Murnaghan (order unspecified) | — | Unknown |
1994 1 EOS record Thermoelasticity of CaSiO3 perovskite and implications for the lower mantle 10.1029/94gl00976
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin |
|---|---|---|---|---|---|---|---|---|
| Bridgmanite | Mg1-xFexSiO3 | — | 24.46 cm³/mol Molar |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited |