Abstract
The cooling DSC technique was employed to measure the heat of freezing H of water present in the vicinity of the surface of ceramic powder particles. The powders used were α-Al2O3, ultrafine SiO2, kaolin-clay and ZrO2 being partially stabilized with Y2O3 (Y-PSZ). The thermodynamic stability of the vicinal water was in the order of ultrafine SiO2>>kaolin clay>α-Al2O3≥Y-PSZ. The differences were also clearly seen in the relationship of H to Tr (freezing onset temperature) and to t (thickness of the water molecule layer on the surface)