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Conductivity of melts in the system CaO-FeO-Fe2O3-SiO2

V. Daněk, T. Ličko, and Z. Pánek

Institute of Inorganic Chemistry, Centre for Chemical Research, Slovak Academy of Sciences, CS-842 36 Bratislava

 

Abstract: Conductivity of the CaO—FeO—Fe203—Si02 melts in the temperature range 1530 К to 1920 К and in the atmosphere of air increases with the increasing temperature and with the increasing concentration of the iron oxides. The presence of iron in two oxidation states, Fe(II) and Fe(III), results in a partial electronic conductance which is due to the jumping electron. The dependence of logarithm of the conductivity value on the reciprocal tempera­ture was described by the third order polynomial. The dependence of conduc­tivity on the composition was described by the equation x=  ∑ ziFui(ci - ci,o) From the above equation mobilities and diffusion coefficients for Ca2+, Fe2+, and Fe3+ cations and for electrons at 1723 К and 1823 К were calculated by the multiple linear regression. The concentration of the electrons in the melt is proportionate to 2x(Fe203) • x(FeO). Both mobility and diffusion coefficient of the present conductive particles increase in the order u (Fe3+)<u(Fe2+)<u(Ca2+)<u(е-)

Full paper in Portable Document Format: 402a215.pdf

 

Chemical Papers 40 (2) 215–223 (1986)

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