1995
DOI: 10.1007/bf02671244
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Thermodynamic assessment of the CaO-MgO-SiO2 system

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Cited by 69 publications
(52 citation statements)
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“…Two-sublattice Thermo-Calc [21] T m (CaO) = 2900 °C [22] CaO-rich part: [23] Miscibility gap: [24], [25] [26], [27], [28] Modified quasichemical FactSage [1], [29] T m (CaO) = 2572 °C [30] Miscibility gap: [24], [25] [31], [13] Cellular Mtdata [21] T m (CaO) = 2900 °C [32] CaO-rich part: [23] Miscibility gap: [24], [25] [33] Two-sublattice Thermo-Calc [45] Liquidus: [46], [47], [48], [49], [50] Field of mullite: [51], [52], [53], [54] [55]…”
Section: Systemmentioning
confidence: 99%
“…Two-sublattice Thermo-Calc [21] T m (CaO) = 2900 °C [22] CaO-rich part: [23] Miscibility gap: [24], [25] [26], [27], [28] Modified quasichemical FactSage [1], [29] T m (CaO) = 2572 °C [30] Miscibility gap: [24], [25] [31], [13] Cellular Mtdata [21] T m (CaO) = 2900 °C [32] CaO-rich part: [23] Miscibility gap: [24], [25] [33] Two-sublattice Thermo-Calc [45] Liquidus: [46], [47], [48], [49], [50] Field of mullite: [51], [52], [53], [54] [55]…”
Section: Systemmentioning
confidence: 99%
“…Para ello, se utilizará sucesivamente la información suministrada por los sistemas binarios SiO 2 -CaO [23,24] y SiO 2 -MgO [25,24] y del sistema ternario SiO 2 -CaO -Al 2 O 3 [26,24].…”
Section: Refractarios De Síliceunclassified
“…Para encontrar la respuesta hay que recurrir al sistema SiO 2 -MgO [25,24]. En este sistema, la sílice es termodinámicamente Sin embargo, como se puede apreciar, el campo de estabilidad de la tridimita, que por las razones expuestas anteriormente es la fase polimórfica de la sílice que interesa obtener en el material, se extiende hasta la temperatura de 1.470 o C. Estando esta por debajo de la primera formación de fase líquida, la cual tiene lugar a 1.543 o C. Este hecho dificulta seriamente la transformación polimórfica del cuarzo (β) a tridimita, que tendría que tener lugar en estado sólido, evitándola, y justificando que el MgO no pueda usarse como aglomerante de la sílice.…”
Section: Fase Polimórficaunclassified
“…In the Fe-O-Si system, fayalite, with the formula 2FeO⅐SiO 2 , has the same crystal structure and thus, olivine has its end compounds fixed by these two systems. The phase is described with the formula (Ca +2 ,Fe +2 )(Ca +2 ,Fe +2 )(Si +4 )(O Ϫ2 ) 4 . The two sublattices with Ca +2 and Fe +2 , to be denoted by I and II, respectively, are structurally different and Ca +2 prefers one of them, here, denoted by II.…”
Section: Thermodynamic Modelsmentioning
confidence: 99%
“…The Fe-O system was evaluated by Sundman. [1] The CaO-SiO 2 system was evaluated by Hillert et al [2,3] and reassessed by Huang et al [4] The Ca-Fe-O system was assessed by Hillert et al [5] and later modified together with the Fe-O system by Selleby and Sundman. [6] The Fe-O-Si system was evaluated simultaneously with the present work and is presented in a separate article.…”
Section: Introductionmentioning
confidence: 99%