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Mineralogy, Structure, and Green Processing of Clay Minerals

Mineralogy, Structure, and Green Processing of Clay Minerals [Pg.11]

Plastic natural ceramic raw materials, consisting predominately of kaolinite, illite and/or montmorUlonite, are accompanied by residual quartz, feldspar, mica, and calcite as well as organic residues. In particular, the hmestone content has been used to distinguish between clay ( 4 mass% hme), marly day (4—10 mass% lime), clayey marl (10-40 mass% hme), marl (40-75 mass% hme), calcareous marl (75-90 mass% lime), marly hmestone (90-96 mass% hne), and hmestone ( 96 mass% hme). Kaolinitic raw materials formed in situ (autochthoneous) are called kadine, while kaolinitic raw materials found in secondary deposits (aUochthone-ous) are called clays. Marl and marly hmestones are important raw materials for Portland cement production (see Section 5.2.1). [Pg.11]

Classic and Advanced Ceramics From Fundamentals to Applications, Robert B. Heimann 2010 WILEY-VCH Verlag GmbH Co. KGaA, Weinheim ISBN 978-3-527-32517-7 [Pg.11]


I 2 Mineralogy, Structure, and Green Processing of Clay Minerals Table Z1 Origin, formation, and transformation relations of clay minerals (Heimann and Franklin, 1979). [Pg.14]




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Clay minerals

Clay minerals structures

Clays process

Green clays

Green processing

Mineral processing

Mineral structure

Mineralization structure

Mineralogical

Mineralogy minerals)

Process Greenness

Process structure

Structural clay

Structure of clay minerals

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