S. Suzuki et al., CATION-EXCHANGE CHARACTERISTICS OF SINTERED HYDROXYAPATITE IN THE STRONGLY ACIDIC REGION, Journal of the American Ceramic Society, 76(6), 1993, pp. 1638-1640
The ion-exchange behavior of hydroxyapatite (Ca10(PO4)6-(OH)2) (HAp),
fired at high temperatures, has been investigated in the strongly acid
ic region (pH 2 and 3). According to the present study, HAp fired abov
e 1000-degrees-C can exchange ions from Ca2+ to Pb2+, even at pH 2, wi
thout dissolution. The molar ratios of Pb2+/Ca2+ after ion exchange ar
e approximately unity in all cases. Ion exchange occurs in a thin laye
r near the surface of HAp particles fired at 1300-degrees-C. After ion
exchange, Pb-Cl-apatite crystals are created in the strongly acidic r
egion (pH 2).