Ceramics-Silikáty 36, (4) 199 - 204 (1992) |
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INTERACTION AT THE PERICLASE - SLAG MELT PHASE BOUNDARY
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Vadász Pavol, Molnár Ludovít
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lnstitute of Metallurgy and Material, Faculty of Metallurgy, Technical University Košice, Park Komenského 3, 049 85 Košice, Czechoslovakia
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Corrosion of periclase monocrystal by the ferrite-calcium, silicate and composite slag melts is for the most part caused by diffusion of iron. In silicate and composite slag, periclase dissolved while at the same time forming magnesium silicate. Diffusion of calcium and silicon into periclase could not be proved by the method employed. |
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