1997
DOI: 10.1007/s11663-997-0029-z
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An assessment of the Fe-O-Si system

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Cited by 25 publications
(25 citation statements)
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“…The composition of the FeO-rich slag reported by Greig [8] at the miscibility gap is not in agreement with the crystobalite liquidus measured by Bowen and Schairer [2] and Turkdogan and Bills, [10] and cannot be reproduced by the present and previous models. [35][36][37] The composition reported by Greig [8] is not the true slag liquidus composition at the monotectic temperature since FeO-rich liquid and small amount of SiO 2 -rich liquid were observed in the sample. The cristobalite liquidus compositions reported by Turkdogan and Bills [10] are lower in SiO 2 compared to the calculated liquidus compositions.…”
Section: Resultsmentioning
confidence: 97%
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“…The composition of the FeO-rich slag reported by Greig [8] at the miscibility gap is not in agreement with the crystobalite liquidus measured by Bowen and Schairer [2] and Turkdogan and Bills, [10] and cannot be reproduced by the present and previous models. [35][36][37] The composition reported by Greig [8] is not the true slag liquidus composition at the monotectic temperature since FeO-rich liquid and small amount of SiO 2 -rich liquid were observed in the sample. The cristobalite liquidus compositions reported by Turkdogan and Bills [10] are lower in SiO 2 compared to the calculated liquidus compositions.…”
Section: Resultsmentioning
confidence: 97%
“…5) compared to previous assessment by Selleby. [35] Figure 6 shows that Wu et al [34] and Jak et al [37] do not reproduce the enthalpy of data by Ban-Ya et al [30] ; these previous assessments appear to give more preference to phase equilibria data. The relationships between oxygen partial pressures versus SiO 2 /[SiO 2 ?…”
Section: Slag-metal Equilibriummentioning
confidence: 83%
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