suppose the fireclay is kaolin. the formation of metakaolin at about 600 C- can it be reverted? Progressive temperature rise causes spinel-like 2Al2O3.3SiO2 at about 950 C and mullite formation at about 1050 C, every time giving away SiO2 Upon progressive disassociation. After firing to 1600 c and cooling, the structure is mainly various polymorph of silica plus mullite. (or other aluminosilicates?). acn the fired product be chemically reverted back to kaolin? if yes , How? if no, why not?

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