Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
205 papers · 1304 EOS records
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 Shock‐induced melting of MgSiO3 perovskite and implications for melts in Earth's lowermost mantle 10.1029/2004gl020237
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| MgSiO3 melt (H.P.P. melt) |
|
— | — | 125 | 4 | third-order Birch-Murnaghan | adiabatic | Original |
2004 2 EOS records Elasticity of post‐perovskite MgSiO3 10.1029/2004gl020278
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Post-perovskite |
|
— | — | 231 | 4.300 | unknown | — | Original | ||||||
| Bridgmanite |
|
— | — | 257 | — | unknown | — | Cited |
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 |
2004 1 EOS record Performance of an ab initio equation of state for magnesium oxide 10.1088/0953-8984/16/30/006
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | — | 160.300 | 4.130 | third-order Birch-Murnaghan | — | Cited |
2004 1 EOS record Pressure-Induced Magnetization in FeO: Evidence from Elasticity and Mössbauer Spectroscopy 10.1103/physrevlett.93.2155…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Wüstite |
|
— | — | 154.800 | 5.060 | Birch-Murnaghan (order unspecified) | — | Cited |
2003 12 EOS records All-electron and pseudopotential study of MgO: Equation of state, anharmonicity, and stability 10.1103/physrevb.67.224110
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | 77.629 ų Unit cell |
151.707 | 4.212 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Table I, static GGA calculation using an effective core pseudopotential with large-core Mg; sibling rows use small-core Mg, PAW potentials, or a pressure-corrected fit. | ||||||||||||
| Periclase |
|
— | 76.595 ų Unit cell |
150.839 | 4.052 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Table I, static GGA calculation using an ultrasoft effective core pseudopotential with small-core Mg; sibling rows use large-core Mg, PAW potentials, or a pressure-corrected fit. | ||||||||||||
| Periclase |
|
— | 76.049 ų Unit cell |
154.183 | 4.141 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Table I, static GGA calculation using a projector augmented-wave (PAW) potential with large-core Mg; sibling rows use ECP potentials, small-core Mg, or a pressure-corrected fit. | ||||||||||||
| Periclase |
|
— | 76.947 ų Unit cell |
150.597 | 4.103 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Table I, static GGA calculation using a projector augmented-wave (PAW) potential with small-core Mg; sibling rows use ECP potentials, large-core Mg, or a pressure-corrected fit. | ||||||||||||
| Periclase |
|
298 K | 74.712 ų Unit cell |
159.940 | 4.112 | third-order Birch-Murnaghan | — | Cited | ||||
| Periclase |
|
— | 73.425 ų Unit cell |
181.240 | 3.997 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Table V, pressure-corrected static PAW-GGA EOS with a constant -7.736 GPa shift to match the experimental ambient volume; distinct from uncorrected Table I rows. | ||||||||||||
| Periclase |
|
— | 74.439 ų Unit cell |
173.480 | 4.014 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
298 K | 74.67 ų Unit cell |
170.530 | 4.036 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
1000 K | 76.549 ų Unit cell |
152.595 | 4.130 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
2000 K | 79.915 ų Unit cell |
127.719 | 4.244 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
3000 K | 83.772 ų Unit cell |
106.110 | 4.331 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
4000 K | 88.006 ų Unit cell |
88.473 | 4.385 | third-order Birch-Murnaghan | — | Original | ||||
2003 7 EOS records Equation of state of stishovite to lower mantle pressures 10.2138/am-2003-2-307
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Stishovite |
|
— | 46.5126 ų Unit cell |
309.900 | 4.590 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Full unit-cell third-order BM EoS fit to combined single-crystal + powder XRD data; sibling row instead reports a linearized axial (a3) modulus, not the full-volume EoS. | ||||||||||||
| Stishovite |
|
— | — | 291 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Stishovite |
|
— | — | 302 | — | unknown | — | Cited | ||||
| Stishovite |
|
— | — | 258 | 4 | second-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Axial modulus for the a3 lattice parameter (second-order BM, K' fixed to 4); sibling row is the corresponding c3 axial modulus (496 GPa), a different crystallographic axis. | ||||||||||||
| Stishovite |
|
— | — | 496 | 4 | second-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Axial modulus for the c3 lattice parameter (second-order BM, K' fixed to 4); sibling row is the corresponding a3 axial modulus (258 GPa), a different crystallographic axis. | ||||||||||||
| Stishovite |
|
— | — | 250.900 | 5.480 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Axial (linearized a3) modulus from a separate fit to model the a lattice parameter alone, not the full unit-cell EoS reported in the sibling row. | ||||||||||||
| Post-stishovite (CaCl₂-type) |
|
— | 46.31 ų Unit cell |
334 | 4 | second-order Birch-Murnaghan | — | Original | ||||
2002 19 EOS records On the structure and compressibility of CaSiO3 perovskite 10.1029/2001gl013523
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Stishovite |
|
300 K | 46.53 ų Unit cell |
313.200 | 4.400 | third-order Birch-Murnaghan | — | Original | ||||||
| Stishovite |
|
— | 46.51 ų Unit cell |
313.400 | — | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Weidner et al. [1981]; sibling row in this compilation table cites a different original study (Panero et al. 2001). | ||||||||||||||
| Stishovite |
|
— | 46.54 ų Unit cell |
312.900 | 4.800 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Panero et al. [2001], with V0 taken from Ross et al. [1990]; sibling row cites a different original study (Weidner et al. 1981). | ||||||||||||||
| Davemaoite |
|
300 K | 45.9 ų Unit cell |
228 | 4.300 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: VIBC calculation for the Pnma structural model; sibling rows use a different space group (Pm3m) or the VIB method without covalent correction. | ||||||||||||||
| Davemaoite |
|
300 K | 45.92 ų Unit cell |
229 | 4.300 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: VIBC calculation for the Pm3m structural model; sibling rows use a different space group (Pnma) or the VIB method without covalent correction. | ||||||||||||||
| Davemaoite |
|
300 K | 44.75 ų Unit cell |
305 | 3.500 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: VIB calculation (no covalent correction) for the Pm3m structural model; sibling rows use the covalent-corrected VIBC method instead. | ||||||||||||||
| Davemaoite |
|
300 K | 45.82 ų Unit cell |
235 | 4.150 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Karki & Crain [1998] first-principles calculation; compilation Table 2 (Theoretical) cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
300 K | 45.62 ų Unit cell |
227 | 4.290 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Chizmeshya et al. [1996] first-principles calculation; compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
300 K | 46.66 ų Unit cell |
246.500 | 4.400 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Wentzcovitch et al. [1995] first-principles calculation; compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
300 K | 45.34 ų Unit cell |
295 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Sherman [1993] theoretical calculation, K'=4.0 assumed (footnote *); compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
300 K | 45.81 ų Unit cell |
347 | 5.300 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Hemley et al. [1987] theoretical calculation; compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
300 K | 55.74 ų Unit cell |
263 | 4.130 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Wolf & Bukowinski [1987] theoretical calculation; compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
300 K | 56.13 ų Unit cell |
269.500 | 3.860 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Wolf & Jeanloz [1985] theoretical calculation; compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
236 | 3.900 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Shim et al. [2000] experimental (approximately hydrostatic), V0 assumed (footnote *); compilation Table 2 (Experimental) cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
— | 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 (quasi-hydrostatic); compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
— | 45.37 ų Unit cell |
281 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Mao et al. [1989], K' assumed=4.0 (footnote *); compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
325 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Tamai & Yagi [1989], K' assumed=4.0 (footnote *); compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
288 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Yagi et al. [1989], K' assumed=4.0 (footnote *); compilation table cites a different original study per row. | ||||||||||||||
| Davemaoite |
|
— | 45.6 ų Unit cell |
275 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
| Why this differs from similar rows: Cites Tarrida & Richet [1989], K' assumed=4.0 (footnote *); compilation table cites a different original study per row. | ||||||||||||||
2002 10 EOS records Equation of state of the hydrous phase δ‐AlOOH at room temperature up to 22.5 GPa 10.1029/2001gl014224
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| delta-AlOOH |
|
— | 56.54 ų Unit cell |
252 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Fit with K'0T fixed to 4, giving K0T=252 GPa; sibling row instead fits both parameters freely, yielding a different K0T=228 and K'=7. | ||||||||||||||
| delta-AlOOH |
|
— | 56.54 ų Unit cell |
228 | 7 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Why this differs from similar rows: Least-squares fit with two free variable parameters (K0T and K'0T both free), giving K0T=228, K'0T=7; sibling row instead fixes K'0T=4 (K0T=252). | ||||||||||||||
| Stishovite |
|
— | — | 291 | 4.790 | unknown | — | Cited | ||||||
| hydrous ringwoodite | hydrous ringwoodite, water content 2.8 ± 0.2 wt % | — | — | 148 | 5 | unknown | — | Cited | ||||||
| hydrous ringwoodite | hydrous ringwoodite (footnote b: water content of hydrous wadsleyite was 2.5 ± 0.3 wt %) | — | — | 155 | 4.300 | unknown | — | Cited | ||||||
| phase A | — | — | — | 145 | 4 | unknown | — | Cited | ||||||
| Superhydrous phase B | — | — | — | 142.600 | 5.800 | unknown | — | Cited | ||||||
| phase E | — | — | — | 112 | — | unknown | — | Cited | ||||||
| phase G | — | — | — | 200 | 4 | unknown | — | Cited | ||||||
| diaspore |
|
— | — | 167.500 | 4 | unknown | — | Cited | ||||||
2002 6 EOS records Structure and elasticity of single‐crystal (Mg,Fe)O and a new method of generating shear waves for gigahertz … 10.1029/2001jb000490
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ferropericlase |
|
— | 76.336 ų Unit cell |
158.400 | 5.490 | third-order Birch-Murnaghan | — | Original | ||||||
| Ferropericlase |
|
— | 77.453 ų Unit cell |
155.800 | 5.530 | third-order Birch-Murnaghan | — | Original | ||||||
| Ferropericlase |
|
— | 78.082 ų Unit cell |
151.300 | 5.550 | third-order Birch-Murnaghan | — | Original | ||||||
| Wüstite |
|
— | — | 142 | — | unknown | — | Cited | ||||||
| Wüstite |
|
— | — | 175 | — | unknown | — | Cited | ||||||
| Periclase |
|
— | — | — | — | unknown | — | Cited |
2002 5 EOS records First‐principles lattice dynamics and thermoelasticity of MgSiO3 ilmenite at high pressure 10.1029/2001jb000702
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Akimotoite |
|
— | 43.61 ų Unknown basis |
210 | 4.570 | fourth-order Birch-Murnaghan | — | Original | ||||||
| Akimotoite |
|
300 K | 44.2 ų Unknown basis |
201 | 4.640 | fourth-order Birch-Murnaghan | — | Original | ||||||
| Akimotoite |
|
1000 K | 45.03 ų Unknown basis |
182 | 4.860 | fourth-order Birch-Murnaghan | — | Original | ||||||
| Akimotoite |
|
2000 K | 48.59 ų Unknown basis |
153 | 5.200 | fourth-order Birch-Murnaghan | — | Original | ||||||
| Akimotoite |
|
300 K | 43.76 ų Unknown basis |
212 | 5.700 | unknown | — | Cited |
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 Tetragonal structure of CaSiO3 perovskite above 20 GPa 10.1029/2002gl016148
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | 45.58 ų Unit cell |
255 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
| Davemaoite |
|
— | — | 281 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Text cites a range (281-325 GPa) from several older studies, cubic-cell analysis (Tamai/Yagi, Mao, Yagi, Tarrida/Richet 1989); sibling row cites more recent, lower studies. | ||||||||||||||
| Davemaoite |
|
— | — | 232 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Text cites a range (232-236 GPa) from more recent studies (Wang et al. 1996; Shim et al. 2000a), also cubic-cell analysis; sibling row cites older, higher-value studies. | ||||||||||||||
2002 2 EOS records Thermodynamic Representations for Solid/Melt Systems at High Pressure and Temperature 10.1063/1.1483512
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
800 K | — | 3147 | 3.900 | Vinet | — | Cited | ||||
| periclase (melt) |
|
3105 K | — | 37.500 | 3.900 | Vinet | — | Original |
2002 1 EOS record Pressure-volume equation of state of the high-pressureB2phase of NaCl 10.1103/physrevb.65.104114
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 160.200 | 3.990 | Birch-Murnaghan (order unspecified) | — | Cited |
2002 5 EOS records Strength and Elasticity ofSiO2across the Stishovite–CaCl2-type Structural Phase Boundary 10.1103/physrevlett.89.2555…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Stishovite |
|
— | — | 304 | — | Birch-Murnaghan (order unspecified) | — | Original | ||||
| Stishovite |
|
— | — | — | 3.980 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites K'0 = 3.98 from static compression using a He pressure medium [1] (Hemley, Prewitt, and Kingma 1994); sibling rows cite different original studies/methods. | ||||||||||||
| Stishovite |
|
— | — | — | 5.100 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites K'0 = 5.1 from ultrasonic elasticity measurements [25] (Li and Liebermann 2001); sibling rows cite different original studies/methods. | ||||||||||||
| Stishovite |
|
— | — | — | 5 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites K'0 = 5.0 from direct shock (dynamic) compression [27] (Luo et al. 2002), noted as not a static measurement; sibling rows cite different, static methods. | ||||||||||||
| Stishovite |
|
— | — | — | 4.800 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites K'0 = 4.8 from static compression of quenched laser-heated samples [26] (Panero, Benedetti, and Jeanloz); sibling rows cite different original studies/methods. | ||||||||||||
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 18 EOS records Quasi‐hydrostatic compression of magnesium oxide to 52 GPa: Implications for the pressure‐volume‐temperature … 10.1029/2000jb900318
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | 74.53 ų Unit cell |
170 | 3.590 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Fit with V0, K0T, and K' all free, yielding V0=74.53, K0T=170, K'=3.59; sibling row instead fixes K0T from independent sound-velocity data. | ||||||||||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
160.200 | 3.990 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Fit with K0T fixed to 160.2 GPa from high-precision sound-velocity measurements, giving V0=74.71 and K'=3.99; marked preferred fit. Sibling row fits K0T freely. | ||||||||||||
| Periclase |
|
300 K | — | 160.200 | 4.120 | Vinet | — | Original | ||||
| Periclase |
|
300 K | — | 160.200 | 4.210 | other named EOS | — | Original | ||||
| Periclase |
|
300 K | 9.338 ų Unknown basis |
— | — | other named EOS | — | Original | ||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
159.800 | 4.520 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Anderson and Andreatch [1966] acoustic/ultrasonic data converted to isothermal conditions; large Table 2 compilation cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
160.500 | 3.890 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Spetzler [1970] ultrasonic data converted to isothermal conditions; compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | 74.74 ų Unit cell |
161.400 | 4.290 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Vassiliou and Ahrens [1981] shock-wave experiment; compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | 74.7 ų Unit cell |
160.200 | 4.150 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Jackson and Niesler [1982] ultrasonic interferometry converted to isothermal conditions; compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | 74.61 ų Unit cell |
161 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Sumino et al. [1983] acoustic measurements; compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | 74.7 ų Unit cell |
161.600 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Isaak et al. [1989] acoustic resonance measurements; compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | — | 160.400 | 4.150 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Yoneda [1990] ultrasonic data converted to isothermal conditions; compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
153 | 4.100 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Utsumi et al. [1998] static compression; text explicitly flags this as giving 'an anomalously low bulk modulus' compared with other cited studies. | ||||||||||||
| Periclase |
|
300 K | 74.78 ų Unit cell |
160 | 4.150 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Fei [1999] static compression, K' fixed (footnote a); compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | — | 160.900 | 4.020 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Sinogeikin and Bass [1999] Brillouin scattering converted to isothermal conditions; compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
161 | 3.940 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Dewaele et al. [2000] static compression, K0 fixed (footnote a); compilation table cites a different original study per row. | ||||||||||||
| Periclase |
|
— | — | — | 4.520 | other named EOS | — | Cited | ||||
| Why this differs from similar rows: Cites Hama and Suito [1999/2000] wide-range P-V-T model (K'=4.52); text says this value is inconsistent with the most recent experimental results in this study. | ||||||||||||
| Periclase |
|
— | — | — | 4.769 | other named EOS | — | Cited | ||||
| Why this differs from similar rows: Cites Jacobs and Oonk [2000] wide-range P-V-T model (K'=4.769); text applies the same inconsistency comment as for the Hama and Suito model. | ||||||||||||
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 17 EOS records 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 | ||||||
| Ferropericlase | (Mg,Fe)O; atomic ratio Fe/(Fe+Mg) = 2f | 290 K | — | 162.500 | 4.130 | unknown | adiabatic | Cited | ||||||
| Davemaoite |
|
290 K | — | 220 | 4 | unknown | adiabatic | Cited | ||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
325 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Tamai & Yagi (1989) in the Table 6 compilation (K' fixed to 4.0); other rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
288 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Yagi et al. (1989) in the Table 6 compilation (K' fixed to 4.0); other rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | 45.6 ų Unit cell |
275 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Tarrida & Richet (1989) in the Table 6 compilation (K' fixed to 4.0); other rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | 45.37 ų Unit cell |
281 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Mao et al. (1989) in the Table 6 compilation (K' fixed to 4.0); other rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | 45.83 ų Unit cell |
280 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Wang & Weidner (1994) in the Table 6 compilation (K' fixed to 4.0); other rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
232 | 4.800 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Wang et al. (1996) in Table 6, the only row where K' is fitted freely (4.8) rather than fixed to 4.0; other rows cite different studies with K' fixed. | ||||||||||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
212 | — | unknown | adiabatic | Cited | ||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
236 | 3.900 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Shim et al. (2000a,b) in the Table 6 compilation with V0 fixed and K' fitted freely (3.9); other rows cite different original studies. | ||||||||||||||
| Davemaoite |
|
— | 45.06 ų Unit cell |
256 | 4.720 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Hama & Suito (1998), 'analysis of experiment', in Table 6; sibling row instead cites a theoretical calculation (Chizmeshya et al.). | ||||||||||||||
| Davemaoite |
|
— | 44.96 ų Unit cell |
301 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Sherman (1993) athermal (0 K, static-lattice) theory in Table 6; other rows cite different original theoretical studies. | ||||||||||||||
| Davemaoite |
|
— | 46.15 ų Unit cell |
254 | 4.400 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Wentzcovitch et al. (1995) athermal static-lattice theory in Table 6; other rows cite different original theoretical studies. | ||||||||||||||
| Davemaoite |
|
— | 45.04 ų Unit cell |
238 | 4.180 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Chizmeshya et al. (1996) athermal static-lattice theory in Table 6; other rows cite different original theoretical studies. | ||||||||||||||
| Davemaoite |
|
— | 45.62 ų Unit cell |
227 | 4.290 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Chizmeshya et al. (1996) theory with thermal correction applied from 0 K to room temperature (Table 6); sibling row instead cites an experimental analysis (Hama & Suito). | ||||||||||||||
| Davemaoite |
|
— | 45.35 ų Unit cell |
241 | 4.140 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Karki & Crain (1998) athermal static-lattice theory in Table 6; other rows cite different original theoretical studies. | ||||||||||||||
2001 6 EOS records Systematics of elasticity: Ab initio study in B1-type alkaline earth oxides 10.1063/1.1371498
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 160 | 4.010 | third-order Birch-Murnaghan | — | Original | ||||
| Periclase |
|
— | — | 172 | 4.090 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites LAPW LDA calculation (Ref. 22) for MgO in Table I; other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | 171 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites LMTO-ASA LDA calculation (Ref. 23) for MgO in Table I (no B' reported); other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | 160 | 4.260 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites pseudopotential plane-wave (PWPP) LDA calculation (Ref. 8) for MgO in Table I; other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | 159 | 4.300 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites density functional perturbation theory (DFPT)+PWPP LDA calculation (Ref. 11) for MgO in Table I; other rows cite different original studies/methods. | ||||||||||||
| Periclase |
|
— | — | 160 | 4.150 | unknown | — | 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 12 EOS records P‐V‐T equation of state of periclase from synchrotron radiation measurements 10.1029/1999jb900364
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | 74.71 ų Unit cell |
159 | 4 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Fit with K' fixed to 4.0, giving K0=159 GPa; sibling row instead fixes K0 to 161 GPa (acoustic value) and fits K' freely (=3.94). | ||||||||||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
161 | 3.940 | third-order Birch-Murnaghan | — | Original | ||||
| Why this differs from similar rows: Fit with K0 fixed to 161 GPa (from acoustic/sound-velocity measurements), K' fitted freely to 3.94; sibling row instead fixes K'=4 and fits K0 freely (=159). | ||||||||||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
161 | 3.750 | Murnaghan | — | Original | ||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
161 | 4.010 | Vinet | — | Original | ||||
| Periclase |
|
300 K | 74.71 ų Unit cell |
161 | 4.080 | other named EOS | — | Original | ||||
| Periclase |
|
300 K | — | 160.300 | 4.150 | none (not an EOS fit) | — | Cited | ||||
| Why this differs from similar rows: Cites Jackson and Niesler [1982] (single crystal + sound velocity, 0-3 GPa); sibling row in this compilation table cites a different original study (Isaak et al. 1989). | ||||||||||||
| Periclase |
|
300 K | — | 161.600 | — | none (not an EOS fit) | — | Cited | ||||
| Why this differs from similar rows: Cites Isaak et al. [1989] (single crystal + sound velocity, 300-1800 K); sibling row cites a different original study (Jackson and Niesler 1982). | ||||||||||||
| Periclase |
|
300 K | — | 160 | 4.700 | unknown | — | Cited | ||||
| Periclase |
|
300 K | — | 177 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Why this differs from similar rows: Cites Duffy et al. [1995] (DAC+XRD, 0-227 GPa); table compiles several original studies, each with a different pressure range and cited source. | ||||||||||||
| Periclase |
|
300 K | — | 162 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Why this differs from similar rows: Cites Fiquet et al. [1996] (DAC+XRD, 0-18 GPa); table compiles several original studies with differing pressure ranges and sources. | ||||||||||||
| Periclase |
|
300 K | — | 153 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Why this differs from similar rows: Cites Utsumi et al. [1998] (multianvil+XRD, 0-10 GPa, 300-1700 K); text notes this study's parameters differed from the authors' own (K0=153, K'=4). | ||||||||||||
| Periclase |
|
300 K | — | 160 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||
| Why this differs from similar rows: Cites Fei [1999] (DAC+XRD, 0-65 GPa, 300-1100 K); table compiles several original studies with differing pressure ranges and sources. | ||||||||||||