Abstract:
The hydration products of hydrothermally cured OPC-quartz blends incorporating clay-brick waste were characterised using simultaneous
DTA-TG, XRD and SEM. The exotherm above 800°C on the DTA curve, due to the formation of -wollastonite ( -CS) was related
to the compressive strength. The area and/or height of the exotherm increased with compressive strength and was due primarily to
the presence of calcium silicate hydrate phases including 1.1 nm tobermorite. Supporting evidence is provided by XRD and SEM.