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

Physicochemical methods for studying the mineral composition and pore structure for the... 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. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Refractories and Industrial Ceramics Springer Journals

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

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Publisher
Springer US
Copyright
Copyright © 2011 by Springer Science+Business Media, Inc.
Subject
Materials Science; Characterization and Evaluation of Materials; Materials Science, general; Ceramics, Glass, Composites, Natural Materials
ISSN
1083-4877
eISSN
1573-9139
D.O.I.
10.1007/s11148-011-9352-7
Publisher site
See Article on Publisher Site

Abstract

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.

Journal

Refractories and Industrial CeramicsSpringer Journals

Published: Jun 3, 2011

References

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