Clay as a raw material – geological code determines its firing behaviour (part 1)
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»1 Pico de Teide/Spain: typical primary rock for...
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»2 Rock lifecycle (with additions from Rothe, P;...
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»3 Diagenesis of clay (with additions from Rothe,...
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»4 Metamorphosis of clay (with additions from...
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»5 Fired specimen 6302 “Bavaria Crème”
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»6 Cottbus/Brandenburg clay district: clay for...
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»7 Grading curves according to DIN 18123
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»8 STA diagram “Big Brandenburg”
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»9 Fired specimen 6273 “Big Brandenburg”
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»10 STA diagram “Aida Rosso”
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»11 Fired specimen 6165 “Aida Rosso”
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»12 Kamsdorf Mine/Thuringia: vertical sea bed
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»13 Carboniferous period: Germany on the Equator...
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»14 STA diagram “Pangäa Maroon”
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»15 Fired specimen 6003 “Pangäa Maroon”
Clays constitute some of the most complex naturally found blends of minerals. They are composed of varying fractions of different clay minerals, but also contain other mineral groups such as tectosilicates, carbonates, oxides and hydroxides. It is the infinite variety of geological processes that make this raw material so complicated and it is mineral structures on micro- and nanoscale that make this raw material so sensitive. Cracking the geological code is therefore crucially important for understanding the behaviour of clays in the firing process.
1 Introduction
2 Geo-coding of clays
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