High temperature thermal treatment to clay mineral often leads to the development of new micro-cracks or extension/widening of pre-existing micro-cracks, which naturally would result in the variation of physical properties. Experiments aiming to understand the evolution of physical properties of clay have been carried out from 20 to 800 Ā°C in a heating furnace, and the results were summarized as follows: two temperature ranges (20ā200 Ā°C and 300ā500 Ā°C) corresponding to the vaporization of moisture (i.e. adhered water or bound water) and oxidation/decomposition reactions of organic matters are obviously evident; clay specimens seem to exhibit the most pronounced physical property changes within the temperature range of 300ā500 Ā°C, which presumably is attributed to the transition of structural water, organic carbon and kaolin of clay. Moreover, within the temperature range of 400ā600 Ā°C, especially between 500 and 600 Ā°C, kaolin structure of clay appears to undergo pronounced chemical changes, ultimately affording increased material porosity accompanied by altered wave velocity.
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