ISSN 0862-5468 (Print), ISSN 1804-5847 (online) 

Ceramics-Silikáty 55, (1) 54 - 58 (2011)


IRON REDOX EQUILIBRIUM AND DIFFUSIVITY IN MIXED ALKALI-ALKALINE EARTH-SILICA GLASS MELTS
 
Kim Ki-Dong
 
Department of Materials Science and Engineering, Kunsan National University, Kunsan 573-701, Korea

Keywords: Iron, Redox, Voltammetry, Diffusivity, Mixed alkali oxide
 

Dependence of redox behavior and diffusivity of iron on temperature and composition was studied in mixed alkali-alkaline earth-silica glass melts by means of square wave voltammetry (SWV). The voltammograms showed that irrespective of K₂O/(Na₂O+K₂O) the peak potential due to Fe³⁺/Fe²⁺ moved toward negative direction with temperature decrease and the peak current showed a strong dependence on frequency at constant temperature. Iron diffusion coefficient versus melt viscosity showed a good linearity. The compositional dependence showed that the peak potential shifted to the positive direction with increase of K₂O but a typical mixed alkali effect occurred in iron diffusion either at constant temperature or at constant viscosity.


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