The thermal oxidative decomposition in air of 0-1.5 wt% of pyrite adde
d to two traditional powdered clays was investigated by non-isothermal
DTA. It emerged that the first step of the exothermic oxidation of py
rite, in the 350-500 degrees C range, partly overlapped the endothermi
c dehydroxylation of clay minerals, centred at 590 degrees C, and the
result was dependent on the pyrite contents. Based on the values of th
e area of the oxidative peak and of the corresponding oxidation heat,
it is possible to calculate quantitatively the amount of pyrite presen
t in the industrial clay bodies and therefore to inform the technician
s of the factories so they can avoid the negative effects of reducing
reactions that could occur during firing of ceramic raw materials.