2006
DOI: 10.1016/j.jpcs.2006.03.012
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Phase diagram and thermodynamics of the La2O3–Ga2O3 system revisited

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Cited by 28 publications
(16 citation statements)
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“…The considerable error might be explained by experimental difficulties to reach equilibrium at the low investigation temperatures, and/ or by significant deviations between the thermodynamic standard data used for the calculation of the enthalpy of formation from the elements [29] and assessed values. [8][9][10] Anyway the model parameters were fitted to the experimental data, [30] whereas the calculated standard enthalpy of formation from the elements [29] was rejected, bearing in mind the high degree of uncertainty of the resulting description. The perovskite phase: the calculated heat capacities of LaCrO 3 are compared with experiments from the literature in Fig.…”
Section: Lanthanum Chromatesmentioning
confidence: 99%
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“…The considerable error might be explained by experimental difficulties to reach equilibrium at the low investigation temperatures, and/ or by significant deviations between the thermodynamic standard data used for the calculation of the enthalpy of formation from the elements [29] and assessed values. [8][9][10] Anyway the model parameters were fitted to the experimental data, [30] whereas the calculated standard enthalpy of formation from the elements [29] was rejected, bearing in mind the high degree of uncertainty of the resulting description. The perovskite phase: the calculated heat capacities of LaCrO 3 are compared with experiments from the literature in Fig.…”
Section: Lanthanum Chromatesmentioning
confidence: 99%
“…The assessment of the La-Cr-O system using the Calphad approach is based on the recently reassessed La-O [8] and Cr-O subsystems. [9] The lattice stabilities of elements are adopted from Dinsdale.…”
Section: Introductionmentioning
confidence: 99%
“…No quaternary phases or solid solutions were found in the Sr-Mn-Cr-O oxide system. 16 Previous assessments of the La-O, Cr-O, La-Cr-O, and Cr-Mn-O oxide databases are adopted from Povoden et al, [17][18][19][20][21] with some modifications denoted in the supplement file to this paper, LSCM_v1.0.tcm (ThermoCalc macrofile), and the La-Sr-Mn-O oxide database is taken from Grundy et al, [22][23][24][25][26][27] also with the following slight modification: Grundy et al 23,24 allowed Mn 31 on the A-site of LSM to reproduce experimental oxygen nonstoichiometries under low oxygen partial pressures. Due to large differences between the ionic radii of La 31 and Mn 31 and possible coordination numbers (1.5 Å for 12-fold coordinated La 31 , 0.785 Å for at maximum 6-fold coordinated Mn 31 ), 28 we omit Mn 31 on the A-site.…”
Section: Assessment Of Oxide Subsystemsmentioning
confidence: 99%
“…The assessment of the La-Fe-O system is based on the recently reassessed La-O [41] and the Fe-O subsystems. [42] The two-sublattice ionic liquid model (Fe 2+ ,Fe 3+ ) p (O 2À ,Va qÀ ) q is adopted from Taylor and Dinsdale [43] for the liquid description in the Fe-O system.…”
Section: Thermodynamic Modeling and Optimizationmentioning
confidence: 99%
“…Higher oxidation states are unlikely to exist in the liquid at normal oxygen partial pressures. Two different models for the Fe-O liquid have been presented: (Fe 2+ ,Fe 3+ ) p (O 2À ,Va qÀ ) q was used by Taylor and Dinsdale, [43] whereas Selleby and Sundman [42] proposed the description (Fe 2+ ) p (FeO 3 [41] Dinsdale, [44] Selleby and Sundman, [42] and Taylor and Dinsdale. [43] G liq Fe 3þ :Va qÀ is obtained by the reciprocal reaction:…”
Section: Perovskite Phasementioning
confidence: 99%