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Effects of strong network modifiers on Fe3+/Fe2+ in silicate melts: an experimental study
Authors:Alexander?Borisov  author-information"  >  author-information__contact u-icon-before"  >  mailto:aborisov@igem.ru"   title="  aborisov@igem.ru"   itemprop="  email"   data-track="  click"   data-track-action="  Email author"   data-track-label="  "  >Email author  author-information__orcid u-icon-before icon--orcid u-icon-no-repeat"  >  http://orcid.org/---"   itemprop="  url"   title="  View OrcID profile"   target="  _blank"   rel="  noopener"   data-track="  click"   data-track-action="  OrcID"   data-track-label="  "  >View author&#  s OrcID profile,Harald?Behrens,Francois?Holtz
Affiliation:1.Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry,Russian Academy of Sciences,Moscow,Russia;2.Vernadsky Institute of Geochemistry and Analytical Chemistry,Russian Academy of Sciences,Moscow,Russia;3.Institut für Mineralogie,Leibniz Universit?t Hannover,Hanover,Germany
Abstract:The effect of CaO, Na2O, and K2O on ferric/ferrous ratio in model multicomponent silicate melts was investigated in the temperature range 1450–1550?°C at 1-atm total pressure in air. It is demonstrated that the addition of these network modifier cations results in an increase of Fe3+/Fe2+ ratio. The influence of network modifier cations on the ferric/ferrous ratio increases in the order Ca?3+/Fe2+ ratio in simple model liquids are critically evaluated. An empirical equation is proposed to predict the ferric/ferrous ratio in SiO2–TiO2–Al2O3–FeO–Fe2O3–MgO–CaO–Na2O–K2O–P2O5 melts at air conditions.
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