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Physicochemical methods for studying the mineral composition and pore structure for the argillaceous part zircon-ilmenite ore gravitation tailings

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Refractories and Industrial Ceramics Aims and scope

It is established that the argillaceous part zircon-ilmenite ore gravitation tailings (ZIG) is a refractory clay, but it has a complex mineral composition, including in contrast to traditional refractory clays more than ten minerals and an increased amount of Fe2O3 (>5%). The main clay mineral of ZIG is kaolinite, which is poorly crystallized. An increase in ZIG ceramic specimen firing temperature to 1300°C promotes pore size uniformity.

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Authors and Affiliations

  1. S. P. Korolev Samara State Aerospace University, Samara, Russia

    E. S. Abdrakhimova

  2. Samara State Architectural Building University, Samara, Russia

    V. Z. Abdrakhimov

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  1. E. S. Abdrakhimova
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  2. V. Z. Abdrakhimov
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Translated from Novye Ogneupory, No. 1, pp. 10 – 16, January 2011.

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Abdrakhimova, E.S., Abdrakhimov, V.Z. Physicochemical methods for studying the mineral composition and pore structure for the argillaceous part zircon-ilmenite ore gravitation tailings. Refract Ind Ceram 52, 1–5 (2011). https://doi.org/10.1007/s11148-011-9352-7

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  • DOI: https://doi.org/10.1007/s11148-011-9352-7

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