Abstract
Quartz (SiO2) is the main silicon source for production of metallurgical grade silicon in submerged arc furnaces. During heating in the furnace, quartz will first transform to other SiO2 polymorphs, then soften and melt. Volume changes during heating and melting are expected to affect for the rate of reactions with SiO2 and gas flow. Industrial quartz sources are investigated here with heating rates relevant for industrial furnaces. A method to study softening and melting of quartz at conditions relevant for Si-production was developed. Both volume expansion and melting properties vary considerably between quartz sources. Theoretical volume expansion is 22 % and melting temperature 1726 °C. Volume increase up to 40 %, softening temperatures in the range 1675 °C to 1800 °C, and melting temperatures in the range 1790 °C to 1900 °C were recorded.
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Ringdalen, E., Tangstad, M. (2016). Softening and Melting of SiO2, an Important Parameter for Reactions with Quartz in Si Production. In: Reddy, R.G., Chaubal, P., Pistorius, P.C., Pal, U. (eds) Advances in Molten Slags, Fluxes, and Salts: Proceedings of the 10th International Conference on Molten Slags, Fluxes and Salts 2016. Springer, Cham. https://doi.org/10.1007/978-3-319-48769-4_4
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DOI: https://doi.org/10.1007/978-3-319-48769-4_4
Publisher Name: Springer, Cham
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