A study of the CaO-SiO2-MgO-CaF2 system was undertaken to determine th
e effect of the various precipitated mineral species on slag theology.
Slags prepared included both basic and acid variations. Three mineral
ogical species were found in the basic slags; merwinite, monticellite
and rankinite. Solidification behaviour was influenced by the concentr
ation of each component, with the more basic slags containing more mer
winite and monticellite; this resulted in higher solidification temper
atures for these melts. The acidic slags examined contained several va
riations of impure pseudowollastonite as well as impure calcium fluori
de. In selected slag mixtures, the fluorspar component was replaced wi
th an alkali-aluminosilicate tailings material to assess its suitabili
ty as a fluorspar substitute. The new slag system was slightly more vi
scous than comparable slags containing fluorspar; however, the shape o
f the temperature-viscosity profile was more favourable with respect t
o an industrial environment. Mineralogical phases encountered here wer
e merwinite, monticellite and akermanite, precipitated from a complex
calcia-msgnesia-alumino-silicate melt. (C) 1997 Published by Elsevier
Science Ltd.