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Phase and chemical transformations in the SiO2-Fe2O3(Fe3O4) system at various oxygen partial pressures
Institute of Silicate Chemistry of Russian Academy of Sciences.
Grebenshchikov Institute of Silicate Chemistry, Russian Academy of Sciences.
Institute of Silicate Chemistry of Russian Academy of Sciences.
b Grebenshchikov Institute of Silicate Chemistry, Russian Academy of Sciences, St. Petersburg, Russia.
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2006 (English)In: Russian Journal of Inorganic Chemistry, ISSN 0036-0236, E-ISSN 1531-8613, Vol. 51, no 1, 118-125 p.Article in journal (Refereed) Published
Abstract [en]

The SiO2-Fe2O3(F3O4) system has been studied in air, oxygen, and an inert atmosphere. The dissociation temperatures for iron oxides, the onset and full melting temperatures for coexisting phases, and the melt demixing temperatures have been determined as a function of the oxygen partial pressure. A scenario of the phase and chemical transformations in the title systems has been developed.

Place, publisher, year, edition, pages
2006. Vol. 51, no 1, 118-125 p.
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Energy Engineering
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URN: urn:nbn:se:kth:diva-53498DOI: 10.1134/S0036023606010190ISI: 000246410800019OAI: oai:DiVA.org:kth-53498DiVA: diva2:470176
Note
QC 20111228Available from: 2011-12-28 Created: 2011-12-28 Last updated: 2017-12-08Bibliographically approved

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Bechta, Sevostian

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