Phase and chemical transformations in the SiO2-Fe2O3(Fe3O4) system at various oxygen partial pressures
2006 (English)In: Russian Journal of Inorganic Chemistry, ISSN 0036-0236, Vol. 51, no 1, 118-125 p.Article in journal (Refereed) Published
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.
IdentifiersURN: urn:nbn:se:kth:diva-53498DOI: 10.1134/S0036023606010190ISI: 000246410800019OAI: oai:DiVA.org:kth-53498DiVA: diva2:470176
QC 201112282011-12-282011-12-282012-01-21Bibliographically approved