H. Benmoussa et al., Synthesis and physicochemical study of new rare-earth-containing vanadocalcic oxyapatites, MATER RES B, 34(9), 1999, pp. 1429-1434
In vanadocalcic oxyapatite Ca-10(VO4)(6)O , the pair (Ca2+, ) can be substi
tuted by the pair (Ln(3+), 1/2O(2-)) (Ln(3+) is a rare-earth ion). In theor
y, this substitution allows for introducing up to two rare-earth ions into
the apatitic lattice. However, a limitation of this substitution depending
on the nature of rare-earth was observed. Thus, this substitution is maximu
m in the case of La3+ and Pr3+ ions and leads to lanthanum or praseodym dio
xyapatites Ca(8)Ln(2)(VO4)(6)O-2 (Ln = La, Pr). With regards to rare earths
such as neodym, samarium, europium, gadolinum, and terbium, the Ln(3+) con
tent limit varies from one rare earth to another. It decreases when the rar
e-earth ionic radius declines. (C) 1999 Elsevier Science Ltd.