Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
205 papers · 1304 EOS records
2016 3 EOS records Two‐stage spin transition of iron in FeAl‐bearing phase D at lower mantle 10.1002/2016jb013209
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Phase D |
|
— | 85.711 ų Unit cell |
— | — | Birch-Murnaghan (order unspecified) | high-spin Fe2+ and Fe3+… | Original | ||||||||||||
| Phase D |
|
— | 85.201 ų Unit cell |
— | — | Birch-Murnaghan (order unspecified) | — | Original | ||||||||||||
| Phase D |
|
— | — | 253 | — | unknown | low-spin Fe3+ (LS-Fe3+… | Cited |
2016 17 EOS records Experimental and theoretical thermal equations of state of MgSiO3 post-perovskite at multi-megabar pressures 10.1038/srep22652
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Post-perovskite |
|
— | 162.86 ų/f.u. Formula unit |
231.930 | 4.430 | Vinet | — | Cited | ||||||
| Why this differs from similar rows: Oganov and Ono ab initio result using the LDA functional (Table 1); sibling row uses the GGA functional instead, giving different V0/K0/K'. | ||||||||||||||
| Post-perovskite |
|
— | 167.64 ų/f.u. Formula unit |
199.960 | 4.541 | Vinet | — | Cited | ||||||
| Why this differs from similar rows: Oganov and Ono ab initio result using the GGA functional (Table 1); sibling row uses the LDA functional instead. | ||||||||||||||
| Post-perovskite |
|
— | 163.81 ų/f.u. Formula unit |
222 | 4.200 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Tsuchiya et al. ab initio LDA result (Table 1); other rows cite different original studies/methods (GGA theory, shock experiment). | ||||||||||||||
| Post-perovskite |
|
— | 167.67 ų/f.u. Formula unit |
— | — | unknown | — | Cited | ||||||
| Post-perovskite |
|
300 K | 162.86 ų/f.u. Formula unit |
237 | 4 | third-order Birch-Murnaghan | A-Au: Equation of state of Au by Anderson… | Cited | ||||||
| Post-perovskite |
|
300 K | 162.86 ų/f.u. Formula unit |
248 | 4 | third-order Birch-Murnaghan | Dw-Au: Equation of state of Au by Dewaele… | Cited | ||||||
| Post-perovskite |
|
300 K | 162.2 ų/f.u. Formula unit |
231.200 | 4 | third-order Birch-Murnaghan | S/K-MgO: Speziale et al. MgO scale (room… | Cited | ||||||
| Post-perovskite |
|
— | 163.4 ų/f.u. Formula unit |
200 | 4.230 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Caracas and Cohen ab initio GGA result (Table 1); other rows cite different original studies/methods. | ||||||||||||||
| Post-perovskite |
|
— | 162.2 ų/f.u. Formula unit |
225 | 4.210 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Mosenfelder et al. shock-compression experiment, using Guignot et al.'s P-V-T data and V0 (Table 1); other rows cite different original studies/methods. | ||||||||||||||
| Post-perovskite |
|
300 K | 158 ų/f.u. Formula unit |
292 | 3.740 | third-order Birch-Murnaghan | T-MgO: Tange et al. MgO scale (3BM) | Original | ||||||
| Post-perovskite |
|
300 K | 156.5 ų/f.u. Formula unit |
324 | 3.300 | Vinet | T-MgO: Tange et al. MgO scale (Vinet) | Original | ||||||
| Post-perovskite |
|
300 K | 155.9 ų/f.u. Formula unit |
336 | 3.130 | AP2 | T-MgO(AP2): Tange et al. MgO scale | Original | ||||||
| Why this differs from similar rows: 'fit3': This study + Guignot et al. data with V0 free; sibling row 'fit4' instead fixes V0 to the g-G-plot value (163.45 A3), changing the fitted K0/K'. | ||||||||||||||
| Post-perovskite |
|
300 K | 163.45 ų/f.u. Formula unit |
228 | 4.180 | AP2 | T-MgO(AP2): Tange et al. MgO scale | Original | ||||||
| Why this differs from similar rows: 'fit4': This study + Guignot et al. data with V0 fixed to 163.45 A3 from the g-G plot; sibling row 'fit3' instead lets V0 float freely. | ||||||||||||||
| Post-perovskite |
|
300 K | 157.16 ų/f.u. Formula unit |
310 | 3.470 | Keane | T-MgO(Keane): Tange et al. MgO scale | Original | ||||||
| Why this differs from similar rows: 'fit5': This study + Guignot et al. data (Keane EOS) with all parameters free; sibling fits fix V0/K-infinity' to these values (fit6/fit7) or use ab initio data instead (fit8). | ||||||||||||||
| Post-perovskite |
|
300 K | 157.16 ų/f.u. Formula unit |
310 | 3.470 | Keane | T-MgO(Keane): Tange et al. MgO scale | Original | ||||||
| Why this differs from similar rows: 'fit6': same dataset as fit5 but with V0 and K-infinity' fixed to the fit5 values (157.16, 2.19) while other parameters are refit; V0/K0/K' match fit5 but theta0/beta differ. | ||||||||||||||
| Post-perovskite |
|
300 K | 164.26 ų/f.u. Formula unit |
203 | 5.350 | Keane | T-MgO(Keane): Tange et al. MgO scale | Original | ||||||
| Why this differs from similar rows: 'fit7' (preferred experimental EOS): V0 fixed to 164.26 A3 from the g-G plot, unlike the free V0 of fit5/fit6; text notes K-infinity' may be slightly misestimated in this fit. | ||||||||||||||
| Post-perovskite |
|
300 K | 164.22 ų/f.u. Formula unit |
205.400 | 5.069 | Keane | — | Original | ||||||
| Why this differs from similar rows: 'fit8': ab initio DFT-LDA theoretical data (not experimental XRD like sibling fits), all parameters free; V0 determined without extrapolation. | ||||||||||||||
2016 1 EOS record Solid-liquid density and spin crossovers in (Mg, Fe)O system at deep mantle conditions 10.1038/srep37269
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| MgO liquid (periclase melt, reference f… |
|
3000 K | 30 ų Unknown basis |
16.600 | 6.140 | third-order Birch-Murnaghan | EOS (Equation 2) descri… | Original |
2016 31 EOS records Thermodynamic estimation the compressibility of ferropericlase under high pressure 10.1063/1.4967779
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 164 | 4.200 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Li et al. (ref. 43) as the specific reference the authors selected as MgO reference data; sibling row instead reports a broader literature range spanning refs. 6,10,43-45. | ||||||||||||||
| Wüstite |
|
— | — | — | 3.600 | unknown | — | Cited | ||||||
| Periclase |
|
— | — | 159 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I entry gives an experimental range (159-164 GPa) from multiple refs. (6,10,43-45) rather than one specific study; sibling row instead cites Li et al. specifically. | ||||||||||||||
| Ferropericlase |
|
— | — | 163.800 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 163 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 153 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 159 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 166 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I entry for x=0.15 citing ref. 50 as the specific literature source; sibling row cites a different reference (ref. 51) instead. | ||||||||||||||
| Ferropericlase |
|
— | — | 168 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I entry for x=0.15 citing ref. 51; sibling row cites a different reference (ref. 50) instead. | ||||||||||||||
| Ferropericlase |
|
— | — | 160 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I entry for x=0.17 citing ref. 11; sibling row cites a different reference (ref. 3) instead. | ||||||||||||||
| Ferropericlase |
|
— | — | 166 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I entry for x=0.17 citing ref. 3; sibling row cites a different reference (ref. 11) instead. | ||||||||||||||
| Ferropericlase |
|
— | — | 158 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 160 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 158.400 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 162 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 156 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I entry for x=0.39 citing ref. 12; sibling row cites a different reference (ref. 53) instead. | ||||||||||||||
| Ferropericlase |
|
— | — | 166 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I entry for x=0.39 citing ref. 53; sibling row cites a different reference (ref. 12) instead. | ||||||||||||||
| Ferropericlase |
|
— | — | 157 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I is a compilation citing different original sources for x=0.4; this row cites ref. 2, the sibling row cites ref. 54. | ||||||||||||||
| Ferropericlase |
|
— | — | 158 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I is a compilation citing different original sources for x=0.4; this row cites ref. 54, the sibling row cites ref. 2. | ||||||||||||||
| Ferropericlase |
|
— | — | 160 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 155.800 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 153 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 149 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I compilation for x=0.6 cites ref. 46 for this row; the sibling row instead cites ref. 51. | ||||||||||||||
| Ferropericlase |
|
— | — | 171 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I compilation for x=0.6 cites ref. 51 for this row; the sibling row instead cites ref. 46. | ||||||||||||||
| Ferropericlase |
|
— | — | 148 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I compilation for x=0.75 cites ref. 55 for this row; the sibling row instead cites ref. 50. | ||||||||||||||
| Ferropericlase |
|
— | — | 151.300 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Table I compilation for x=0.75 cites ref. 50 for this row; the sibling row instead cites ref. 55. | ||||||||||||||
| Ferropericlase |
|
— | — | 152 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 166 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 148 | — | unknown | — | Cited | ||||||
| Ferropericlase |
|
— | — | 197.400 | — | unknown | — | Cited | ||||||
| Wüstite |
|
— | — | 146 | — | unknown | — | Cited | ||||||
2016 1 EOS record Stability of Fe,Al-bearing bridgmanite in the lower mantle and synthesis of pure Fe-bridgmanite 10.1126/sciadv.1600427
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 178.98 ų Unit cell |
190 | 4 | Birch-Murnaghan (order unspecified) | — | Original |
2016 16 EOS records Equation of state and spin crossover of (Mg,Fe)O at high pressure, with implications for explaining topograph… 10.2138/am-2016-5510
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
300 K | 77.29 ų Unit cell |
160 | 4.120 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin (HS) state fit with K' free (4.12); sibling row is the low-spin (LS) state of the same sample, fitted with K' fixed to 4 since it was unconstrained by the data. | ||||||||||||||||
| Ferropericlase |
|
300 K | 73.64 ų Unit cell |
173 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin (LS) state fit with K' fixed to 4 (not constrained by data); sibling row is the high-spin (HS) state of the same sample, fitted with K' free. | ||||||||||||||||
| Ferropericlase |
|
300 K | 75.55 ų Unit cell |
159 | 3.960 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin state refit of Marquardt et al. (2009b) data, K' free (3.96); sibling row is the low-spin state of the same dataset, refit with K' fixed to 4. | ||||||||||||||||
| Ferropericlase |
|
300 K | 74.59 ų Unit cell |
159 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin state refit of Marquardt et al. (2009b) data with K' fixed to 4; sibling row is the high-spin state of the same dataset, fitted with K' free. | ||||||||||||||||
| Ferropericlase |
|
300 K | 75.94 ų Unit cell |
160 | 4.040 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin state refit of Lin et al. (2005) data, K' free (4.04); sibling row is the low-spin state of the same dataset, refit with K' fixed to 4. | ||||||||||||||||
| Ferropericlase |
|
300 K | 72.29 ų Unit cell |
190 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin state refit of Lin et al. (2005) data with K' fixed to 4; sibling row is the high-spin state of the same dataset, fitted with K' free. | ||||||||||||||||
| Ferropericlase |
|
300 K | 76.34 ų Unit cell |
160 | 4.280 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin state refit of Mao et al. (2011) data, K' free (4.28); sibling row is the low-spin state of the same dataset, refit with K' fixed to 4. | ||||||||||||||||
| Ferropericlase |
|
300 K | 73.74 ų Unit cell |
174 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin state refit of Mao et al. (2011) data with K' fixed to 4; sibling row is the high-spin state of the same dataset, fitted with K' free. | ||||||||||||||||
| Ferropericlase |
|
300 K | 77.1 ų Unit cell |
162 | 3.990 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin state refit of Chen et al. (2012) data, K' free (3.99); sibling row is the low-spin state of the same dataset, refit with K' fixed to 4. | ||||||||||||||||
| Ferropericlase |
|
300 K | 73.77 ų Unit cell |
171 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin state refit of Chen et al. (2012) data with K' fixed to 4; sibling row is the high-spin state of the same dataset, fitted with K' free. | ||||||||||||||||
| Ferropericlase |
|
300 K | 77.49 ų Unit cell |
161 | 4.250 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin state refit of Fei et al. (2007) data, K' free (4.25); other rows are the LS state of this dataset or HS/LS states of a different dataset (Zhuravlev et al. 2010). | ||||||||||||||||
| Ferropericlase |
|
300 K | 74.83 ų Unit cell |
162 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin state refit of Fei et al. (2007) data, K' fixed to 4; other rows are the HS state of this dataset or a different dataset (Zhuravlev et al. 2010). | ||||||||||||||||
| Ferropericlase |
|
300 K | 77.41 ų Unit cell |
160 | 4.070 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin state refit of Zhuravlev et al. (2010) data, K' free (4.07); other rows are the LS state of this dataset or a different dataset (Fei et al. 2007). | ||||||||||||||||
| Ferropericlase |
|
300 K | 73.56 ų Unit cell |
170 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin state refit of Zhuravlev et al. (2010) data, K' fixed to 4; other rows are the HS state of this dataset or a different dataset (Fei et al. 2007). | ||||||||||||||||
| Ferropericlase |
|
300 K | 77.9 ų Unit cell |
159 | 3.820 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: High-spin state refit of Lin et al. (2005) (Mg0.40Fe0.60)O data, K' free (3.82); sibling row is the low-spin state of the same dataset, refit with K' fixed to 4. | ||||||||||||||||
| Ferropericlase |
|
300 K | 73.83 ų Unit cell |
169 | 4 | spin-crossover EOS | — | Original | ||||||||
| Why this differs from similar rows: Low-spin state refit of Lin et al. (2005) (Mg0.40Fe0.60)O data with K' fixed to 4; sibling row is the high-spin state of the same dataset, fitted with K' free. | ||||||||||||||||
2015 1 EOS record Small shear modulus of cubic CaSiO3 perovskite 10.1002/2015gl063446
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | 27.8 cm³/mol Molar |
206.600 | 4.410 | finite strain (unspecified form) | — | Cited |
2015 1 EOS record Effects of the Fe3+ spin transition on the equation of state of bridgmanite 10.1002/2015gl064400
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 162.6 ų Unit cell |
284 | 4 | third-order Birch-Murnaghan | Pt scale of Fei et al. [2007a] | Original |
2015 8 EOS records The thermal equation of state of (Mg, Fe)SiO3bridgmanite (perovskite) and implications for lower mantle struc… 10.1002/2015jb012108
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 163.16 ų Unit cell |
243.800 | 4.160 | Vinet | — | Original | ||||||||
| Bridgmanite |
|
300 K | 162.12 ų Unit cell |
262.300 | 4.044 | Vinet | — | Original | ||||||||
| Why this differs from similar rows: V0 fitted freely (Bayesian prior) from reanalyzed Tange et al. (2012) data, giving V0=162.12, K0=262.3; differs from sibling's fixed-V0 conditional fit. | ||||||||||||||||
| Bridgmanite |
|
300 K | 162.5 ų Unit cell |
253.200 | — | Vinet | — | Original | ||||||||
| Why this differs from similar rows: Conditional fit with V0 fixed to 162.5 (typical measured value) rather than fitted freely, yielding a different K0=253.2; sibling row fits V0 freely. | ||||||||||||||||
| Bridgmanite |
|
300 K | — | 252 | — | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 253 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cites Fiquet et al. [2000] (253-259 GPa depending on whether heated data included); V0 fixed to a measured volume; sibling row cites a different original study (Mao et al. 2011). | ||||||||||||||||
| Bridgmanite |
|
— | — | 259.600 | — | unknown | — | Cited | ||||||||
| Why this differs from similar rows: Cites Mao et al. [2011] (259.6 GPa); V0 fixed to a measured volume per that study; sibling row cites a different original study (Fiquet et al. 2000). | ||||||||||||||||
| Bridgmanite |
|
— | 162.373 ų Unit cell |
— | — | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 253 | — | none (not an EOS fit) | adiabatic | Cited | ||||||||
2015 4 EOS records The equations of state of forsterite, wadsleyite, ringwoodite, akimotoite, MgSiO3-perovskite, and postperovsk… 10.1016/j.rgg.2015.01.011
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298.2 K | 24.45 cm³/mol Molar |
252 | 4.380 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Post-perovskite |
|
298.2 K | 24.2 cm³/mol Molar |
253.700 | 4.030 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Akimotoite |
|
298.2 K | 26.35 cm³/mol Molar |
215.300 | 4.910 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Periclase |
|
298.2 K | 11.248 cm³/mol Molar |
160.300 | 4.250 | Birch-Murnaghan (order unspecified) | — | Cited |
2015 1 EOS record Crystal structure, equation of state and elasticity of phase H (MgSiO4H2) at Earth’s lower mantle pressures 10.1038/srep15534
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Phase H |
|
— | 58.9 ų Unit cell |
147.500 | 4.900 | Birch-Murnaghan (order unspecified) | — | Original |
2015 2 EOS records Elasticity of Ferropericlase across the Spin Crossover in the Earth’s Lower Mantle 10.1038/srep17188
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
— | — | — | 4.100 | unknown | high-spin (HS) | Original | ||||||
| Ferropericlase |
|
— | — | — | 4 | unknown | low-spin (LS) | Original |
2015 2 EOS records Spin crossover and Mott—Hubbard transition under high pressure and high temperature in the low mantle of the … 10.1088/1742-6596/653/1/012…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
— | — | 210 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Value is for the high-spin (HS) state (B_HS = 210 GPa, B' fixed to 4, from ref [21]); the sibling row is the low-spin (LS) state of the same composition. | ||||||||||||||
| Ferropericlase |
|
— | — | 161 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Why this differs from similar rows: Value is for the low-spin (LS) state (B_LS = 161 GPa, B' fixed to 4, from ref [21]); the sibling row is the high-spin (HS) state of the same composition. | ||||||||||||||
2015 7 EOS records Equation of state and elasticity of the 3.65 Å phase: Implications for the X-discontinuity 10.2138/am-2015-5312
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 3.65 Å phase |
|
— | 194.52 ų Unit cell |
83 | 4.900 | third-order Birch-Murnaghan | — | Original | ||||||||
| 3.65 Å phase |
|
— | 194.52 ų Unit cell |
77 | — | fourth-order Birch-Murnaghan | — | Original | ||||||||
| 3.65 Å phase |
|
— | 202.02 ų Unit cell |
80 | 3.400 | fourth-order Birch-Murnaghan | — | Original | ||||||||
| Periclase |
|
— | — | 160.200 | — | unknown | — | Cited | ||||||||
| Stishovite |
|
— | — | 294 | — | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 256.700 | — | unknown | — | Cited | ||||||||
| Phase D |
|
— | — | 166 | — | unknown | — | Cited |
2014 10 EOS records P‐V‐T equation of state of cubic CaSiO3 perovskite from first‐principles computation 10.1002/2013jb010905
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
1000 K | 46.17 ų/f.u. Formula unit |
203.500 | 4.760 | Vinet | — | Original | ||||||
| Davemaoite |
|
1000 K | 46.21 ų Unit cell |
206.600 | 4.410 | third-order Birch-Murnaghan | — | Original | ||||||
| Davemaoite |
|
2000 K | 48.65 ų Unit cell |
170.900 | 4.760 | third-order Birch-Murnaghan | — | Cited | ||||||
| Davemaoite |
|
— | 44.537 ų Unit cell |
249 | 4.090 | third-order Birch-Murnaghan | — | Cited | ||||||
| Davemaoite |
|
— | 44.581 ų Unit cell |
244 | 4.440 | unknown | — | Cited | ||||||
| Davemaoite |
|
300 K | 45.58 ų Unit cell |
242 | 4.180 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Zhang et al. (2006) molecular dynamics EOS; other rows in this Table 2 compilation cite different original studies (Wang 1996, Shim 2000, Ricolleau 2010). | ||||||||||||||
| Davemaoite |
|
300 K | 45.58 ų Unit cell |
232 | 4.800 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Wang et al. (1996) experimental P-V-T data fit to BM3; sibling rows in this compilation table cite different original studies. | ||||||||||||||
| Davemaoite |
|
300 K | 45.58 ų Unit cell |
236 | 3.900 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Shim et al. (2000) EDXRD experiment (18-96 GPa, 1238-2419 K, BM3 fit); sibling rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
300 K | 45.6 ų Unit cell |
244 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Ricolleau et al. (2010), explicitly noted in text as based on a multicomponent, multiphase system; K' fixed to 4, unlike some sibling rows. | ||||||||||||||
| Davemaoite |
|
700 K | 45.8 ų Unit cell |
238 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
2014 3 EOS records Prediction of a potential high-pressure structure ofFeSiO3 10.1103/physrevb.90.140102
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 44.31 ų/f.u. Formula unit |
225 | 4.420 | Vinet | — | Original | ||||||
| Post-perovskite |
|
— | 44.9 ų/f.u. Formula unit |
189 | 4.730 | Vinet | — | Original | ||||||
| Why this differs from similar rows: Table III value for the PPv (base post-perovskite) structure; sibling row is for a distinct newly predicted phase, PPv-II (Cmmm), at the same nominal composition. | ||||||||||||||
| Post-perovskite |
|
— | 45.45 ų/f.u. Formula unit |
195 | 4.670 | Vinet | — | Original | ||||||
| Why this differs from similar rows: Table III value for PPv-II, a newly predicted Cmmm structure distinct from the base post-perovskite (PPv) phase in the sibling row. | ||||||||||||||
2014 8 EOS records Analysis of Equation of States for the Suitability at High Pressure: MgO as an Example 10.1155/2014/289353
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 160 | 4.150 | unknown | — | Cited | ||||
| Why this differs from similar rows: Literature-compilation value cited from ref [13]; other rows in the same table cite different original references ([14],[15],[28]-[31]) with their own B0/B0'. | ||||||||||||
| Periclase |
|
— | — | 161 | 3.940 | unknown | — | Cited | ||||
| Why this differs from similar rows: Literature-compilation value cited from ref [14], distinct from the other cited references ([13],[15],[28]-[31]) in the same table. | ||||||||||||
| Periclase |
|
— | — | 160.200 | 3.990 | unknown | — | Cited | ||||
| Why this differs from similar rows: Literature-compilation value cited from ref [15], distinct from the other cited references in the same table. | ||||||||||||
| Periclase |
|
— | — | 161.400 | 4.290 | unknown | — | Cited | ||||
| Why this differs from similar rows: Literature-compilation value cited from ref [28], distinct from the other cited references in the same table. | ||||||||||||
| Periclase |
|
— | — | 160.200 | 4.150 | unknown | — | Cited | ||||
| Why this differs from similar rows: Literature-compilation value cited from ref [29], distinct from the other cited references in the same table. | ||||||||||||
| Periclase |
|
— | — | 153 | 4.100 | unknown | — | Cited | ||||
| Why this differs from similar rows: Literature-compilation value cited from ref [30], distinct from the other cited references in the same table. | ||||||||||||
| Periclase |
|
— | — | 160.200 | 4.030 | unknown | — | Cited | ||||
| Why this differs from similar rows: Literature-compilation value cited from ref [31], distinct from the other cited references in the same table. | ||||||||||||
| Periclase |
|
— | — | 161.300 | 4.240 | third-order Birch-Murnaghan | — | Cited | ||||
2013 8 EOS records New Thermodynamic Models and Calculated Phase Equilibria in NCFMAS for Basic and Ultrabasic Compositions thro… 10.1093/petrology/egt035
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298 K | 2.445 kJ kbar-1 Molar |
251 | 4.140 | modified Tait | — | Original | ||||||||
| Bridgmanite |
|
298 K | 2.534 kJ kbar-1 Molar |
281 | 4.140 | modified Tait | — | Original | ||||||||
| Bridgmanite |
|
298 K | 2.54 kJ kbar-1 Molar |
203 | 4 | modified Tait | — | Original | ||||||||
| Bridgmanite |
|
298 K | 2.334 kJ kbar-1 Molar |
203 | 4 | modified Tait | — | Original | ||||||||
| Davemaoite |
|
298 K | 2.745 kJ kbar-1 Molar |
236 | 3.900 | modified Tait | — | Original | ||||||||
| Periclase |
|
298 K | 1.125 kJ kbar-1 Molar |
161.600 | 3.950 | modified Tait | — | Original | ||||||||
| Wüstite |
|
298 K | 1.206 kJ kbar-1 Molar |
152 | 4.900 | modified Tait | — | Original | ||||||||
| Stishovite |
|
298 K | 1.401 kJ kbar-1 Molar |
309 | 4.600 | modified Tait | — | Original |
2013 5 EOS records Cubic perovskite polymorph of strontium metasilicate at high pressures 10.2138/am.2013.4470
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| cubic perovskite (SrSiO3) |
|
— | 49.18 ų Unit cell |
211 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| cubic perovskite (SrSiO3), theoretical |
|
— | 49.97 ų Unit cell |
207.700 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| 6H-type hexagonal perovskite (SrSiO3), … |
|
— | 311.23 ų Unit cell |
183.800 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Bridgmanite |
|
— | 40.575 ų Unknown basis |
260 | — | unknown | — | Cited | ||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
232 | — | unknown | — | Cited |
2013 1 EOS record Elastic Properties of CaSiO3 Perovskite from ab initio Molecular Dynamics 10.3390/e15104300
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
300 K | 45.58 ų Unit cell |
236 | 3.900 | third-order Birch-Murnaghan | — | Cited |
2013 4 EOS records Effect of substitution Fe2+ on physical properties of MgSiO3 perovskite at high temperature and high pressure 10.7498/aps.62.049101
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.378 ų Unit cell |
244 | 4 | third-order Birch-Murnaghan | — | Original | ||||||||
| Bridgmanite |
|
— | 164.977 ų Unit cell |
248 | 4.030 | third-order Birch-Murnaghan | — | Original | ||||||||
| Bridgmanite |
|
300 K | 162.345 ų Unit cell |
264 | — | unknown | — | Cited | ||||||||
| Bridgmanite |
|
— | — | 246 | 3.900 | unknown | — | Cited |
2012 6 EOS records P‐V‐T equation of state of MgSiO3 perovskite based on the MgO pressure scale: A comprehensive reference for m… 10.1029/2011jb008988
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 162.373 ų Unit cell |
258.400 | 4.100 | Vinet | — | Original | ||||||
| Why this differs from similar rows: Table 2 preferred Vinet-form fit, KT0/K'T0 free, V0 fixed to Tange et al. [2009b]; sibling row is an alternative fit additionally constrained by external KS0 = 253 GPa. | ||||||||||||||
| Bridgmanite |
|
300 K | 162.373 ų Unit cell |
256.700 | 4.090 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Table 2 third-order Birch-Murnaghan fit with KT0/K'T0 free, V0 fixed to Tange et al. [2009b]; sibling row is an alternative fit constrained by an external KS0 = 253 GPa. | ||||||||||||||
| Periclase |
|
300 K | 74.698 ų Unit cell |
160.630 | 4.367 | Vinet | — | Cited | ||||||
| Periclase |
|
300 K | 74.698 ų Unit cell |
160.640 | 4.221 | third-order Birch-Murnaghan | — | Cited | ||||||
| Bridgmanite |
|
300 K | 162.373 ų Unit cell |
250.600 | 4.420 | Vinet | — | Original | ||||||
| Why this differs from similar rows: Alternative fit constraining KS0 to 253 GPa from Brillouin/ultrasonic literature; authors note it deviates systematically from the volume data vs. the unconstrained fit (sibling row). | ||||||||||||||
| Bridgmanite |
|
300 K | 162.373 ų Unit cell |
250.600 | 4.458 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Alternative BM3-form fit constrained by external KS0 = 253 GPa (same constraint type as the Vinet-form alternative fit elsewhere in this paper); sibling row is the unconstrained fit. | ||||||||||||||
2012 2 EOS records P‐V‐T equation of state of stishovite up to mid‐lower mantle conditions 10.1029/2011jb009100
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Stishovite |
|
300 K | 46.55 ų Unit cell |
292 | 5.010 | Vinet | — | Original | ||||
| Stishovite |
|
300 K | 46.55 ų Unit cell |
294 | 4.850 | third-order Birch-Murnaghan | — | Original |
2012 21 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 | ||||||||||
| Periclase |
|
300 K | 11.24 cm³/mol Molar |
161 | 3.900 | third-order Birch-Murnaghan | — | Cited | ||||||||||
| Wüstite |
|
300 K | 12.26 cm³/mol Molar |
179 | 4.900 | third-order Birch-Murnaghan | — | Cited | ||||||||||
| Davemaoite |
|
300 K | 27.45 cm³/mol Molar |
236 | 3.900 | third-order Birch-Murnaghan | — | Cited | ||||||||||
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 | ||||||||||