Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
85 papers · 347 EOS records
2012 18 EOS records Acoustic velocities of pure and iron‐bearing magnesium silicate perovskite measured to 25 GPa and 1200 K 10.1029/2012gl053075
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 4.11 g·cm-3 Unknown basis |
257 | 4 | second-order Birch-Murnaghan | — | Original | ||||||||||
| Bridgmanite |
|
300 K | 4.161 g·cm-3 Unknown basis |
246 | 4 | second-order Birch-Murnaghan | — | Original | ||||||||||
| Bridgmanite |
|
300 K | — | 247 | 4.500 | third-order Birch-Murnaghan | adiabatic | Original | ||||||||||
| Why this differs from similar rows: Fit uses this study's velocity and volume data alone; sibling row instead fits a combined dataset with Li and Zhang [2005] data added for better constraints. | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 252 | 4.100 | third-order Birch-Murnaghan | adiabatic | Original | ||||||||||
| Why this differs from similar rows: Fit combines this study's data with Li and Zhang [2005] data for better constraints; sibling row uses only this study's data alone. | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 253 | 4.400 | finite strain (unspecified form) | adiabatic | Cited | ||||||||||
| Bridgmanite |
|
300 K | — | 253 | — | unknown | adiabatic | Cited | ||||||||||
| Bridgmanite |
|
300 K | — | 251 | 4.110 | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Table cites Boffa Ballaran et al. [2012]; K_T = 251 GPa regardless of 10 or 75 GPa fit range. Other rows cite different original studies (Ross and Hazen 1990; Fiquet 2000; Vanpeteghem 2006). | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 254 | — | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Table cites Ross and Hazen [1990]; other rows in this compilation cite different original studies (Boffa Ballaran et al. 2012; Fiquet et al. 2000; Vanpeteghem et al. 2006). | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 259.500 | — | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Table cites Fiquet et al. [2000]; other rows in this compilation cite different original studies (Boffa Ballaran et al. 2012; Ross and Hazen 1990; Vanpeteghem et al. 2006). | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 253 | 4 | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Table cites Vanpeteghem et al. [2006], K' fixed to 4; other rows cite different original studies (Boffa Ballaran 2012; Ross and Hazen 1990; Fiquet 2000). | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 236 | 4.700 | third-order Birch-Murnaghan | adiabatic | Original | ||||||||||
| Bridgmanite |
|
300 K | — | 253 | 3.990 | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Cites Boffa Ballaran et al. [2012], fit over 0-75 GPa; sibling rows cite same study fit over narrower ranges (0-40, 0-25 GPa), which changes derived K_T/K'. | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 245 | 4.400 | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Cites Boffa Ballaran et al. [2012], fit over 0-40 GPa; sibling rows cite the same study fit over 0-75 GPa or 0-25 GPa instead, which changes the derived K_T/K'. | ||||||||||||||||||
| Bridgmanite |
|
300 K | — | 236 | 5.600 | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Cites Boffa Ballaran et al. [2012]; fitting the data only to 25 GPa gives K_T = 236 GPa, vs. wider-range fits of same study in sibling rows (0-40, 0-75 GPa). | ||||||||||||||||||
| Bridgmanite | (Mg,Fe)SiO3 | 300 K | — | 255.400 | 4 | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Table cites Andrault et al. [2001] with K' fixed to 4; sibling row cites a different original study (Mao et al. 1991, also K' fixed to 4). | ||||||||||||||||||
| Bridgmanite | (Mg,Fe)SiO3 | 300 K | — | 261 | 4 | unknown | — | Cited | ||||||||||
| Why this differs from similar rows: Table cites Mao et al. [1991] with K' fixed to 4; sibling row cites a different original study (Andrault et al. 2001, also K' fixed to 4). | ||||||||||||||||||
| Bridgmanite |
|
300 K | 24.42 cm³/mol Molar |
252 | 4.100 | third-order Birch-Murnaghan | — | Original | ||||||||||
| Bridgmanite |
|
300 K | 25.5 cm³/mol Molar |
236 | 4.700 | third-order Birch-Murnaghan | — | Original | ||||||||||
2012 11 EOS records Thermodynamic properties of (Mg,Fe2+)SiO3 perovskite at the lower-mantle pressures and temperatures: an inter… 10.1111/j.1365-246x.2012.05…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 24.3325 cm³/mol Molar |
259.341 | 3.940 | third-order Birch-Murnaghan | high-spin (HS) | Original | ||||||||||
| Why this differs from similar rows: Table 1(a) Model 1, high-spin Fe with a 2x2x1 supercell (Fe-Fe distance 6.8794 A); sibling rows use different Fe-Fe distances/supercells (Models 2, 3) or the low-spin state. | ||||||||||||||||||
| Bridgmanite |
|
— | 24.3326 cm³/mol Molar |
259.292 | 3.940 | third-order Birch-Murnaghan | high-spin (HS) | Original | ||||||||||
| Why this differs from similar rows: Table 1(a) Model 2, high-spin Fe with a 2x1x2 supercell (Fe-Fe distance 4.9246 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 3) or the low-spin state. | ||||||||||||||||||
| Bridgmanite |
|
— | 24.3317 cm³/mol Molar |
259.461 | 3.940 | third-order Birch-Murnaghan | high-spin (HS) | Original | ||||||||||
| Why this differs from similar rows: Table 1(a) Model 3, high-spin Fe with a 1x2x2 supercell (Fe-Fe distance 4.7723 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 2) or the low-spin state. | ||||||||||||||||||
| Bridgmanite |
|
— | 24.2583 cm³/mol Molar |
260.799 | 3.940 | third-order Birch-Murnaghan | low-spin (LS) | Original | ||||||||||
| Why this differs from similar rows: Table 1(b) Model 1, low-spin Fe with a 2x2x1 supercell (Fe-Fe distance 6.8752 A); sibling rows use different Fe-Fe distances/supercells (Models 2, 3) or the high-spin state. | ||||||||||||||||||
| Bridgmanite |
|
— | 24.2605 cm³/mol Molar |
260.798 | 3.940 | third-order Birch-Murnaghan | low-spin (LS) | Original | ||||||||||
| Why this differs from similar rows: Table 1(b) Model 2, low-spin Fe with a 2x1x2 supercell (Fe-Fe distance 4.9197 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 3) or the high-spin state. | ||||||||||||||||||
| Bridgmanite |
|
— | 24.2596 cm³/mol Molar |
260.744 | 3.940 | third-order Birch-Murnaghan | low-spin (LS) | Original | ||||||||||
| Why this differs from similar rows: Table 1(b) Model 3, low-spin Fe with a 1x2x2 supercell (Fe-Fe distance 4.7644 A); sibling rows use different Fe-Fe distances/supercells (Models 1, 2) or the high-spin state. | ||||||||||||||||||
| Bridgmanite |
|
— | 24.2717 cm³/mol Molar |
258.786 | 3.940 | third-order Birch-Murnaghan | — | Original | ||||||||||
| Bridgmanite |
|
— | — | 253 | 3.900 | unknown | — | Cited | ||||||||||
| Bridgmanite |
|
300 K | — | 247 | 3.970 | unknown | — | Cited | ||||||||||
| Bridgmanite |
|
— | — | — | — | unknown | — | Cited | ||||||||||
| Bridgmanite |
|
— | — | — | — | unknown | — | Cited | ||||||||||
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 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 | ||||||||
2009 2 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 |
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 1 EOS record 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 |
2009 4 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). | ||||||||||||||
| Bridgmanite |
|
— | — | 253 | — | unknown | adiabatic | Cited | ||||||
| Bridgmanite |
|
— | — | — | 3.700 | unknown | — | Cited | ||||||
2009 5 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 |
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). | ||||||||||||||||
2007 1 EOS record Effects of Fe spin transition on the elasticity of (Mg, Fe)O magnesiowüstites and implications for the seismo… 10.1029/2006jb004730
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 163.9 ų Unit cell |
260 | 4.030 | third-order Birch-Murnaghan | — | Cited |
2007 3 EOS records Indoor seismology by probing the Earth's interior by using sound velocity measurements at high pressures and … 10.1073/pnas.0608609104
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 253 | 4.400 | finite strain (unspecified form) | adiabatic | Cited | ||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | — | 253 | 4.400 | unknown | adiabatic | Cited | ||||||
| Bridgmanite |
|
— | — | — | 3.700 | unknown | — | Cited |
2007 1 EOS record Influence of New Interaction Potential on MD Simulation of MgSiO3 Perovskite Thermodynamic Properties 10.1088/1674-0068/20/05/547…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 25.071 cm³/mol Molar |
— | — | unknown | — | Original |
2006 8 EOS records Crystal structure and equation of state of MgSiO3 perovskite 10.1029/2005gl024955
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.51 ų Unit cell |
253 | 4 | second-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | — | 251 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: KT calculated from KS reported by Li and Zhang [2005] (ultrasonic interferometry + XRD); sibling rows in this table cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 251 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: KT calculated from KS reported by Sinogeikin et al. [2004] (Brillouin spectroscopy); sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 253 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Fiquet et al. [2000] X-ray diffraction; sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 262 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: KT calculated from KS reported by Yeganeh-Haeri [1994] (Brillouin spectroscopy); sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 254 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Ross and Hazen [1990] X-ray diffraction; sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 257 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: KT calculated from KS reported by Wentzcovitch et al. [1998] (theoretical calculation); sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 256 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: KT calculated from KS reported by Karki et al. [1997] (theoretical calculation); sibling rows cite different original studies. | ||||||||||||||
2006 4 EOS records Equation of state of the postperovskite phase synthesized from a natural (Mg,Fe)SiO 3 orthopyroxene 10.1073/pnas.0506811103
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 163.3 ų Unit cell |
255 | 3.700 | second-order Birch-Murnaghan | — | Original | ||||||||||||
| Bridgmanite |
|
— | 162.3 ų Unit cell |
259 | 3.700 | unknown | — | Cited | ||||||||||||
| Why this differs from similar rows: Table 1 cites Ref. 17 (Fiquet et al. 2000) experimental result; sibling row cites a different original study, Ref. 19 (Sinogeikin et al. 2004). | ||||||||||||||||||||
| Bridgmanite |
|
— | 162.7 ų Unit cell |
255.400 | 4 | unknown | — | Cited | ||||||||||||
| Bridgmanite |
|
— | — | 253 | — | unknown | — | Cited | ||||||||||||
| Why this differs from similar rows: Table 1 cites Ref. 19 (Sinogeikin et al. 2004) experimental result; sibling row cites a different original study, Ref. 17 (Fiquet et al. 2000). | ||||||||||||||||||||
2006 7 EOS records First-Principles Study of Orthorhombic Perovskites MgSiO 3 up to 120 GPa and Its Geophysical Implications 10.1088/0256-307x/23/8/101
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.253 ų Unit cell |
264 | 3.830 | fourth-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 161.658 ų Unit cell |
255 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 162.486 ų Unit cell |
— | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 Experiment column cites ref [1]; sibling rows in this table cite different original studies, refs [9] and [3] (Fiquet). | ||||||||||||||
| Bridgmanite |
|
— | 162.398 ų Unit cell |
— | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 Experiment column cites ref [9]; sibling rows in this table cite different original studies, refs [1] and [3] (Fiquet). | ||||||||||||||
| Bridgmanite |
|
— | 162.3 ų Unit cell |
— | 3.900 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 Experiment column cites ref [3] (Fiquet), described as room-temperature compression; sibling rows cite different studies, refs [1] and [9]. | ||||||||||||||
| Bridgmanite |
|
— | — | 261 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 Experiment column cites ref [22]; sibling row instead cites a different original study, ref [23]. | ||||||||||||||
| Bridgmanite |
|
— | — | 263 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 Experiment column cites ref [23]; sibling row instead cites a different original study, ref [22]. | ||||||||||||||
2006 2 EOS records Simulation of Melting Behavior of the MgSiO3 Perovskite Under Lower Mantle Conditions 10.1360/cjcp2006.19(4).311.4
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.414 cm³/mol Molar |
— | — | unknown | — | Original | ||||||
| Bridgmanite |
|
— | — | — | 4.920 | unknown | — | Cited |
2006 2 EOS records Equation of state of CaIrO3-type MgSiO3 up to 144 GPa 10.2138/am.2006.2118
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 162.49 ų Unit cell |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Cites Mao et al. (1991) literature value with Au pressure standard; sibling row cites Fiquet et al. (2000) with a Pt standard instead. | ||||||||||||||
| Bridgmanite |
|
300 K | 162.27 ų Unit cell |
253 | 3.900 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Cites Fiquet et al. (2000) literature value with Pt pressure standard; sibling row cites Mao et al. (1991) with an Au standard instead. | ||||||||||||||
2005 7 EOS records Effect of chemistry on the stability and elasticity of the perovskite and post‐perovskite phases in the MgSiO… 10.1029/2005gl023164
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 40.78 ų/f.u. Formula unit |
232 | 3.860 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 38.53 ų/f.u. Formula unit |
271 | 3.740 | third-order Birch-Murnaghan | GGA | Original | ||||||||
| Bridgmanite |
|
— | 42.67 ų/f.u. Formula unit |
231 | 4.030 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 44.12 ų/f.u. Formula unit |
237 | 4.160 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 41.08 ų/f.u. Formula unit |
269 | 4.170 | third-order Birch-Murnaghan | GGA | Original | ||||||||
| Bridgmanite |
|
— | 43.22 ų/f.u. Formula unit |
202 | 3.950 | third-order Birch-Murnaghan | LDA | Original | ||||||||
| Bridgmanite |
|
— | 39.93 ų/f.u. Formula unit |
223 | 4.220 | third-order Birch-Murnaghan | GGA | Original |
2005 5 EOS records Effect of Al on the sharpness of the MgSiO3 perovskite to post‐perovskite phase transition 10.1029/2005gl023192
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 41.75 ų Unit cell |
235 | 3.840 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Al-free (0 mol% Al2O3) end-member perovskite; sibling rows are Al-bearing perovskite with different substitution mechanisms (CCM, OVM, AlHM), same normalized MgSiO3 formula. | ||||||||||||||
| Bridgmanite |
|
— | 41.86 ų Unit cell |
232 | 3.860 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: 6.25 mol% Al2O3 via the charge-coupled mechanism (CCM: MgSi->AlAl); sibling rows use different Al content/substitution mechanisms (none, OVM, AlHM). | ||||||||||||||
| Bridgmanite |
|
— | 42.83 ų Unit cell |
205 | 4.030 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 42.36 ų Unit cell |
214 | 3.960 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: 6.25 mol% Al2O3 via the oxygen-vacancy-forming mechanism (OVM: SiSiO->AlAl+vacancy); sibling rows use different Al content/substitution mechanisms. | ||||||||||||||
| Bridgmanite |
|
— | 42.2 ų Unit cell |
228 | 3.850 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: 3.125 mol% Al2O3 via the hydrous Al substitution mechanism (AlHM: Si->AlH); sibling rows use different Al content/substitution mechanisms. | ||||||||||||||
2004 5 EOS records Temperature derivatives of elastic moduli of MgSiO3 perovskite 10.1029/2003gl018762
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 249 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 row b cites Andrault et al. [2001] (static compression in DAC), K' fixed to 4.0; sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 253 | 3.900 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 row c cites Fiquet et al. [2000] (static compression in DAC), K' free (=3.9); sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 261 | 4 | unknown | — | Cited | ||||||
| Bridgmanite |
|
— | — | 261 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 row e cites Wang et al. [1994] (static compression in DAC), K' fixed to 4.0; sibling rows cite different original studies. | ||||||||||||||
| Bridgmanite |
|
— | — | 261 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table 1 row f cites Funamori et al. [1996] (static compression in a Kawai-type multianvil apparatus, not DAC), K' fixed to 4.0; sibling rows use DAC data from different studies. | ||||||||||||||
2004 1 EOS record Equation of state and phase stability of mantle perovskite up to 140 GPa shock pressure and its geophysical i… 10.1029/2003gl019132
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 260.100 | 4.180 | third-order Birch-Murnaghan | adiabatic | Original |
2004 4 EOS records Elasticity of single crystal and polycrystalline MgSiO3 perovskite by Brillouin spectroscopy 10.1029/2004gl019559
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.4 ų Unit cell |
253 | — | none (not an EOS fit) | adiabatic | Original | ||||||
| Bridgmanite |
|
— | 162.4 ų Unit cell |
253 | — | none (not an EOS fit) | adiabatic | Original | ||||||
| Bridgmanite |
|
— | — | 264 | — | none (not an EOS fit) | adiabatic | Cited | ||||||
| Bridgmanite |
|
— | — | — | — | unknown | — | Cited |
2004 6 EOS records Effect of aluminium on the compressibility of silicate perovskite 10.1029/2004gl020213
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 163.23 ų Unit cell |
251.500 | 4 | second-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | 163.23 ų Unit cell |
251.500 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
— | — | 259 | — | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Bridgmanite |
|
— | — | 253 | 4 | second-order Birch-Murnaghan | — | Cited | ||||||
| Bridgmanite |
|
— | — | 259 | 3.700 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Bridgmanite |
|
— | 163.26 ų Unit cell |
— | — | none (not an EOS fit) | — | Cited |
2004 1 EOS record Elasticity of post‐perovskite MgSiO3 10.1029/2004gl020278
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 257 | — | unknown | — | Cited |