Browse EOS records
One row per paper — expand to see every matching EOS record from that study.
205 papers · 1304 EOS records
1996 2 EOS records The search for a universal equation of state correct up to very high pressures 10.1088/0953-8984/8/1/008
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | 123.747 au Unit cell |
157 | 4.370 | Vinet | — | Original | ||||||
| Bridgmanite |
|
— | 40.25 ų Unit cell |
272 | 3.800 | Vinet | — | Cited |
1996 3 EOS records Chemical composition of the lower mantle inferred from the equation of state of MgSiO 3 perovskite 10.1098/rsta.1996.0053
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.46 cm³/mol Molar |
261 | 3.750 | third-order Birch-Murnaghan | — | Original | ||||||
| Bridgmanite |
|
300 K | — | 261 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Ferropericlase |
|
300 K | 11.25 cm³/mol Molar |
157 | 4 | third-order Birch-Murnaghan | — | Cited |
1996 3 EOS records High-pressure X-ray diffraction study and equation of state of MgSiO 3 ilmenite 10.2138/am-1996-1-206
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Akimotoite |
|
— | 262.17 ų Unit cell |
212 | 7.500 | third-order Birch-Murnaghan | ruby fluorescence | Original | ||||||
| Akimotoite |
|
— | 262.17 ų Unit cell |
212 | 5.600 | third-order Birch-Murnaghan | ice VII EOS (Hemley et al. 1987) | Original | ||||||
| Akimotoite |
|
— | — | 212 | — | unknown | — | Cited |
1995 2 EOS records Compressional sound velocity, equation of state, and constitutive response of shock‐compressed magnesium oxide 10.1029/94jb02065
1995 9 EOS records High pressure effects on thermal properties of MgO 10.1029/95gl01086
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | 18.66 ų Unit cell |
160.100 | 4.220 | unknown | — | Cited | ||||
| Why this differs from similar rows: Compiled 'Exp.' column in Table 1 combining Mao and Bell [1979] (V0), Sumino et al. [1983] (K_T), and Chang and Barsch [1969] (K_T'); other columns cite different studies. | ||||||||||||
| Periclase |
|
300 K | 18.7 ų Unit cell |
153.110 | 4.680 | unknown | — | Original | ||||
| Periclase |
|
300 K | 18.66 ų Unit cell |
180.100 | 4.150 | unknown | — | Cited | ||||
| Why this differs from similar rows: Quasi-harmonic PIB model calculation of Isaak et al. [1990] (Table 1, QH PIB column); other columns in this table cite different original studies/methods. | ||||||||||||
| Periclase |
|
300 K | 18.69 ų Unit cell |
177 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Quasi-harmonic VIB model calculation of Wolf and Bukowinski [1988] (Table 1, QH VIB column); other columns cite different original studies/methods. | ||||||||||||
| Periclase |
|
300 K | 18.73 ų Unit cell |
232 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Empirical model (EM) calculation of Reynard and Price [1990] (Table 1, EM column); other columns in this table cite different original studies/methods. | ||||||||||||
| Periclase |
|
300 K | — | 161.300 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Empirical model (EM) calculation of Agnon and Bukowinski [1990] (Table 1, EM column); other columns cite different original studies/methods. | ||||||||||||
| Periclase |
|
940 K | 19.29 ų Unit cell |
132.090 | 5.010 | unknown | — | Original | ||||
| Periclase |
|
1880 K | 20.29 ų Unit cell |
104.150 | 5.440 | unknown | — | Original | ||||
| Periclase |
|
2830 K | 21.38 ų Unit cell |
83.930 | 5.660 | unknown | — | Original | ||||
1995 6 EOS records Calculation models of structures and physical properties of CaSiO3, CaMgSi2O6, and Ca2BaSi3O9 crystals. 10.2465/minerj.17.290
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | 47.34 ų Unit cell |
247 | 5.090 | unknown | — | Original | ||||||
| Why this differs from similar rows: From Table 6 static lattice-energy WMIN calculation (K0=0.247 TPa); sibling row 1287 is from Table 7's separate pressure-dependence WMIN calculation (K0=0.245 TPa). | ||||||||||||||
| Davemaoite |
|
— | 55.74 ų Unit cell |
274 | 3.850 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites the lattice-dynamics calculation of Wolf and Jeanloz (1985); sibling rows cite Hemley et al. (1987) or the Tamai and Yagi (1989) observation. | ||||||||||||||
| Davemaoite |
|
— | 45.81 ų Unit cell |
347 | 5.300 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites the lattice-dynamics calculation of Hemley et al. (1987); sibling rows cite Wolf and Jeanloz (1985) or the Tamai and Yagi (1989) observation. | ||||||||||||||
| Davemaoite |
|
— | 45.58 ų Unit cell |
325 | 4 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites the observation of Tamai and Yagi (1989), whose bulk modulus has large stated uncertainty because V0 was estimated by extrapolating high-pressure data, not measured directly. | ||||||||||||||
| Davemaoite |
|
— | — | 245 | — | unknown | — | Original | ||||||
| Why this differs from similar rows: From Table 7 pressure-dependence WMIN calculation (K0=0.245 TPa), distinct from the Table 6 static lattice-energy calculation (K0=0.247 TPa) in sibling row 1283. | ||||||||||||||
| Bridgmanite |
|
— | — | 261 | — | unknown | — | Cited | ||||||
1994 1 EOS record Thermoelasticity of perovskite: An emerging consensus 10.1029/94eo01093
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin |
|---|---|---|---|---|---|---|---|---|
| Bridgmanite | (Mg,Fe)SiO3 | 300 K | — | 263 | 3.900 | unknown | — | Cited |
1994 1 EOS record Thermal expansion of MgSiO3 perovskite at 20.5 GPa 10.1029/94gl00844
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 263 | 3.900 | Birch-Murnaghan (order unspecified) | — | Unknown |
1994 6 EOS records Thermoelasticity of CaSiO3 perovskite and implications for the lower mantle 10.1029/94gl00976
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
300 K | 45.83 ų Unit cell |
280 | 4 | second-order Birch-Murnaghan | — | Original | ||||||
| Davemaoite |
|
— | — | 288 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Tamai and Yagi (1989) K0=288 GPa as one of three literature comparison values quoted in the text; sibling row instead cites Tarrida and Richet (1989). | ||||||||||||||
| Davemaoite |
|
— | — | 281 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Davemaoite |
|
— | — | 275 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites Tarrida and Richet (1989) K0=275 GPa as one of three literature comparison values quoted in the text; sibling row instead cites Tamai and Yagi (1989). | ||||||||||||||
| Bridgmanite | Mg1-xFexSiO3 | — | 24.46 cm³/mol Molar |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Davemaoite |
|
300 K | 27.59 cm³/mol Molar |
281 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||
1994 4 EOS records Comparison between the lattice dynamics and molecular dynamics methods: Calculation results for MgSiO3 perovs… 10.1029/94gl01370
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
500 K | 24.68 cm³/mol Molar |
237 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Lattice-dynamics (LD) quasi-harmonic simulation result at 500 K/0 GPa; sibling row uses a molecular-dynamics (MD) simulation instead, giving a slightly different K_T. | ||||||||||||||
| Bridgmanite |
|
500 K | 24.7 cm³/mol Molar |
236 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Molecular-dynamics (MD) simulation (with Wigner-Kirkwood quantum corrections) at 500 K/0 GPa; sibling row uses a lattice-dynamics (LD) simulation instead. | ||||||||||||||
| Bridgmanite |
|
1000 K | 25.25 cm³/mol Molar |
200 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Lattice-dynamics (LD) quasi-harmonic simulation result at 1000 K/0 GPa; sibling row uses a molecular-dynamics (MD) simulation instead, giving K_T=208 GPa versus 200 GPa here. | ||||||||||||||
| Bridgmanite |
|
1000 K | 25.19 cm³/mol Molar |
208 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Molecular-dynamics (MD) simulation (with quantum corrections) at 1000 K/0 GPa; sibling row uses a lattice-dynamics (LD) simulation instead. | ||||||||||||||
1994 2 EOS records Static compression of chondrodite: Implications for water in the upper mantle 10.1029/94gl01592
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| chondrodite |
|
— | 110.88 cm³/mol Molar |
136.200 | 3.700 | third-order Birch-Murnaghan | — | Original | ||||||||||||
| chondrodite (mantle density model, iron… |
|
300 K | 109.18 cm³/mol Molar |
136.200 | 3.700 | Birch-Murnaghan (order unspecified) | — | Original |
1994 9 EOS records Ab initiodetermination of the bulk properties of MgO 10.1103/physrevb.49.8574
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | 180 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table I, uncorrelated Hartree-Fock result with basis set [8511/8411]; sibling rows use different basis sets and/or add correlation corrections (CS, P86, P91). | ||||||||||||
| Periclase |
|
— | — | 181 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table I, uncorrelated Hartree-Fock result with basis set [8511*/8411*] including polarization functions, distinct from the other basis/correlation combinations in the table. | ||||||||||||
| Periclase |
|
— | — | 196 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table II, Hartree-Fock plus a posteriori Colle-Salvetti (CS) correlation correction, basis [8511/8411]; sibling rows use different correlation functionals or basis sets. | ||||||||||||
| Periclase |
|
— | — | 212 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table II, Hartree-Fock plus a posteriori Perdew 1986 (P86) correlation correction, basis [8511/8411]; sibling rows use different correlation functionals or basis sets. | ||||||||||||
| Periclase |
|
— | — | 212 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table II, Hartree-Fock plus a posteriori Perdew 1991 (P91) correlation correction, basis [8511/8411]; sibling rows use different correlation functionals or basis sets. | ||||||||||||
| Periclase |
|
— | — | 205 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table III, Hartree-Fock plus CS correlation correction with the polarized basis [8511*/8411*]; sibling rows use different correlation functionals or the unpolarized basis. | ||||||||||||
| Periclase |
|
— | — | 204 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table III, Hartree-Fock plus P86 correlation correction with the polarized basis [8511*/8411*]; sibling rows use different correlation functionals or the unpolarized basis. | ||||||||||||
| Periclase |
|
— | — | 205 | — | none (not an EOS fit) | — | Original | ||||
| Why this differs from similar rows: Table III, Hartree-Fock plus P91 correlation correction with the polarized basis [8511*/8411*]; sibling rows use different correlation functionals or the unpolarized basis. | ||||||||||||
| Periclase |
|
77 K | — | 164.600 | — | unknown | — | Cited | ||||
1993 1 EOS record High pressure and high temperature in situ X‐ray observation of MgSiO3 Perovskite under lower mantle conditio… 10.1029/92gl02960
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 162.75 ų Unit cell |
260 | 4 | unknown | — | Cited |
1993 2 EOS records Refinement of enthalpy measurement of MgSiO3 perovskite and negative pressure‐temperature slopes for Perovski… 10.1029/93gl01265
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298 K | 24.44 cm³/mol Molar |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||
| Periclase |
|
298 K | 11.25 cm³/mol Molar |
160 | 4.100 | Birch-Murnaghan (order unspecified) | — | Cited |
1993 1 EOS record Static compressibility of magnesite to 20 GPa: Implications for MgCO3 in the lower mantle 10.1029/93gl02507
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
— | — | — | 4.200 | Birch-Murnaghan (order unspecified) | — | Cited |
1993 12 EOS records Equation of state and high‐pressure phase transitions of stishovite (SiO2): Ab initio (periodic Hartree‐Fock)… 10.1029/93jb00783
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Stishovite |
|
— | 46.2 ų Unit cell |
328 | 4 | third-order Birch-Murnaghan | — | Original | ||||
| SiO2 modified-fluorite |
|
— | 42.9 ų Unit cell |
387 | 4.400 | third-order Birch-Murnaghan | — | Original | ||||
| Stishovite |
|
— | — | 300 | 4 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Bassett and Barnett [1970], 0-8.5 GPa experimental compression; this is a compilation table (Table 2) where other rows cite different original studies. | ||||||||||||
| Stishovite |
|
— | — | 344 | 2 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Liu et al. [1974], 0-22.3 GPa; text notes nonhydrostatic conditions were present in this experiment, unlike other cited studies in the same compilation table. | ||||||||||||
| Stishovite |
|
— | — | 298 | 0.700 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Sato [1977], 0-11 GPa experimental compression; compilation table (Table 2) where other rows cite different original studies. | ||||||||||||
| Stishovite |
|
— | — | 306 | — | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Weidner et al. [1982] Brillouin scattering (no K' reported), a different method from the compression studies cited in sibling rows of this table. | ||||||||||||
| Stishovite |
|
— | 46.591 ų Unit cell |
313 | 6 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Sugiyama et al. [1987], 0-6 GPa experimental compression; other rows in this compilation table cite different original studies. | ||||||||||||
| Stishovite |
|
— | — | 376 | 4 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Tsuchida and Yagi [1989], 0-80 GPa DAC; text notes hydrostatic conditions were not obtained in their diamond anvil cell, unlike other cited studies. | ||||||||||||
| Stishovite |
|
— | 46.615 ų Unit cell |
313 | 2.800 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Ross et al. [1990], 0-15 GPa experimental compression, with crystallographic parameters also reported; other rows in this table cite different original studies. | ||||||||||||
| Stishovite |
|
— | 47.5 ų Unit cell |
288 | 3.140 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Park et al. [1988] LAPW ab initio result; text notes a discrepancy with Cohen [1991] and this work, possibly from incomplete convergence of Park et al.'s LAPW energies. | ||||||||||||
| Stishovite |
|
— | 46.16 ų Unit cell |
324 | 4.040 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Cohen [1991] LAPW ab initio result; sibling rows in this table cite different original studies (Park et al. [1988], Keskar et al. [1991]). | ||||||||||||
| Stishovite |
|
— | 45.64 ų Unit cell |
292 | 5.860 | unknown | — | Cited | ||||
| Why this differs from similar rows: Cites Keskar et al. [1991] plane-wave pseudopotential (PW-PP) calculation, a different ab initio method from the LAPW results in sibling rows; text notes PW-PP underestimates V0. | ||||||||||||
1993 4 EOS records Equation of state, elastic properties, and stability of CaSiO3 perovskite: First principles (periodic Hartree… 10.1029/93jb02175
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Davemaoite |
|
— | 44.96 ų/f.u. Formula unit |
301 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Uses the more complete extended basis set B (8-31G* Si, 8-51G O) in the periodic Hartree-Fock fit; sibling row uses a smaller basis set described as inadequate. | ||||||||||||||
| Davemaoite |
|
— | 44.87 ų Unit cell |
290 | 5.600 | finite strain (unspecified form) | — | Original | ||||||
| Davemaoite |
|
— | 43.96 ų Unit cell |
412 | — | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Uses smaller basis set A (6-21G), explicitly described by authors as inadequate/unreliable, giving K0 45% too high and V0 about 4% too low vs the basis-B result. | ||||||||||||||
| Davemaoite |
|
— | — | 281 | 4 | third-order Birch-Murnaghan | — | Cited | ||||||
1993 5 EOS records Ab initiomolecular dynamics with variable cell shape: Application toMgSiO3 10.1103/physrevlett.70.3947
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | — | 259 | 3.900 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Ab initio calculation for the Pbnm (orthorhombic) phase (K0=259, K'0=3.9); sibling row is for a distinct hypothetical cubic phase of the same composition (K0=258, K'0=4.0). | ||||||||||||||
| Bridgmanite |
|
— | — | 258 | 4 | third-order Birch-Murnaghan | — | Original | ||||||
| Why this differs from similar rows: Ab initio calculation for a hypothetical cubic phase (K0=258, K'0=4.0); sibling row is for the Pbnm (orthorhombic) phase of the same composition (K0=259, K'0=3.9). | ||||||||||||||
| Bridgmanite |
|
— | — | 279 | 3.400 | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cites a different ab initio study, a full-potential LAPW calculation by Cohen et al. [28], distinct from the two experimental citations in sibling rows. | ||||||||||||||
| Bridgmanite |
|
— | — | 243 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cited as the low end of an interlaboratory range, from Yeganeh-Haeri et al. [27]; sibling rows cite a different experimental study [20] or a theoretical LAPW calculation [28]. | ||||||||||||||
| Bridgmanite |
|
— | — | 266 | — | unknown | — | Cited | ||||||
| Why this differs from similar rows: Cited as the high end of an interlaboratory range, from Knittle and Jeanloz [20]; sibling rows cite a different experimental study [27] or a theoretical LAPW calculation [28]. | ||||||||||||||
1993 5 EOS records Effect of Pressure on the Composition of the Lower Mantle End Member Fe x O 10.1126/science.259.5091.66
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Wüstite |
|
— | — | 169 | 4 | unknown | — | Cited | ||||
| Wüstite |
|
— | — | 152 | — | unknown | — | Cited | ||||
| Wüstite |
|
— | — | 154 | — | unknown | — | Cited | ||||
| Wüstite |
|
— | — | 178 | — | unknown | — | Cited | ||||
| Wüstite | Fe_xO, x = 0.90 to 0.95 | — | — | 150 | — | unknown | — | Cited |
1993 2 EOS records Computer Simulation of the Structural and Physical Properties of Minerals in the Earth's Deep-Interior. 10.5940/jcrsj.35.190
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 24.44 cm³/mol Molar |
247 | — | none (not an EOS fit) | — | Cited | ||||||
| Bridgmanite |
|
— | 24.56 cm³/mol Molar |
250 | — | unknown | — | Original |
1992 3 EOS records Thermoelasticity of Silicate Perovskite and Magnesiowüstite and Stratification of the Earth's Mantle 10.1126/science.257.5073.10…
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
— | 24.56 cm³/mol Molar |
263 | 3.900 | Birch-Murnaghan (order unspecified) | — | Original | ||||||||
| Bridgmanite | (Mg,Fe)SiO3 | — | 24.46 Molar |
— | — | Birch-Murnaghan (order unspecified) | — | Original | ||||||||
| Ferropericlase |
|
— | 11.25 Molar |
157 | 4 | Birch-Murnaghan (order unspecified) | — | Original |
1991 8 EOS records Effect of pressure, temperature, and composition on lattice parameters and density of (Fe,Mg)SiO3‐perovskites… 10.1029/91jb00176
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
298 K | 162.49 ų Unit cell |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||||
| Bridgmanite |
|
298 K | 162.79 ų Unit cell |
261 | 4 | Birch-Murnaghan (order unspecified) | gold (Anderson et al., 1989); ruby R1; ne… | Original | ||||||||
| Bridgmanite |
|
298 K | 163.53 ų Unit cell |
261 | 4 | Birch-Murnaghan (order unspecified) | — | Original | ||||||||
| Bridgmanite |
|
298 K | — | 246 | — | unknown | adiabatic | Cited | ||||||||
| Bridgmanite |
|
298 K | — | 247 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
| Why this differs from similar rows: Cites Kudoh et al. [1987], single-crystal XRD in a methanol-ethanol-water medium to 10 GPa; other rows in this compilation cite different original studies/samples/pressure media. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 254 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
| Why this differs from similar rows: Cites Ross and Hazen [1989], single-crystal XRD in methanol-ethanol and Ne media to 13 GPa; other rows cite different original studies/samples/pressure media. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 258 | 4 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
| Why this differs from similar rows: Cites Yagi et al. [1982], powder XRD in a methanol-ethanol medium to 7 GPa (nonhydrostatic above 7.5-9 GPa, only data below 7.5 GPa used); other rows cite different original studies/samples/pressure media. | ||||||||||||||||
| Bridgmanite |
|
298 K | — | 266 | 3.900 | Birch-Murnaghan (order unspecified) | — | Cited | ||||||||
1991 7 EOS records Modified potential-induced-breathing model of potentials between close-shell ions 10.1103/physrevb.44.2495
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Periclase |
|
300 K | 18.65 ų Unknown basis |
180 | 4.040 | Birch-Murnaghan (order unspecified) | — | Original | ||||
| Periclase |
|
300 K | 18.67 ų Unknown basis |
163 | 4.130 | unknown | — | Cited | ||||
| Periclase |
|
— | — | 139 | — | unknown | — | Cited | ||||
| Periclase |
|
300 K | 18.07 ų Unknown basis |
175 | 4.200 | unknown | — | Original | ||||
| Stishovite |
|
— | 45.54 ų Unit cell |
378 | 6.400 | unknown | — | Original | ||||
| Stishovite |
|
— | 46.54 ų Unit cell |
287 | 1.700 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table VI 'Experiment' column, citing literature refs 30-32; sibling row is a theoretical PIB (potential-induced-breathing) model calculation (Ref. 2). | ||||||||||||
| Stishovite |
|
— | 43.39 ų Unit cell |
411 | 3.730 | unknown | — | Cited | ||||
| Why this differs from similar rows: Table VI 'PIB Model' column, a theoretical potential-induced-breathing electron-gas calculation attributed to Ref. 2 (Cohen 1987); sibling row is experimental data. | ||||||||||||
1991 2 EOS records Phase Transition and Thermal Expansion of MgSiO 3 Perovskite 10.1126/science.251.4992.410
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.725 cm³ Molar |
246.500 | 4 | unknown | — | Original | ||||||
| Bridgmanite |
|
300 K | — | — | — | unknown | — | Original |
1990 6 EOS records Constraints on lower mantle composition and temperature from density and bulk sound velocity profiles 10.1029/gl017i008p01153
| Phase | Composition | Tref | V₀ | K₀ (GPa) | K′ | EOS model | Method note | Origin | ||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bridgmanite |
|
300 K | 24.46 cm³ Molar |
269 | 4 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Bridgmanite |
|
300 K | 25.49 cm³ Molar |
269 | 4 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Periclase |
|
300 K | 11.25 cm³ Molar |
162.700 | 4.100 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Wüstite |
|
300 K | 12.25 cm³ Molar |
179.700 | 3.600 | third-order Birch-Murnaghan | adiabatic | Cited | ||||||
| Bridgmanite |
|
— | — | 273 | — | unknown | adiabatic | Cited | ||||||
| Why this differs from similar rows: Cites K_S0=273 GPa from Mao and Hemley (personal communication, 1989), close to the adopted Knittle and Jeanloz value; sibling row cites a lower literature value (~245 GPa). | ||||||||||||||
| Bridgmanite |
|
— | — | — | — | unknown | adiabatic | Cited | ||||||
| Why this differs from similar rows: Cites lower K_S0~245 GPa from Kudoh et al. and Yeganeh-Haeri et al.; text says results are nearly identical if K_S0' is instead raised to ~4.5 (a proposed adjustment, not fitted). | ||||||||||||||