Location of type B carbonate ion in type A-B carbonate apatite synthesized at high pressure

被引:126
作者
Fleet, ME [1 ]
Liu, XY [1 ]
机构
[1] Univ Western Ontario, Dept Earth Sci, London, ON N6A 5B7, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
carbonate apatite; CAp; type B (phosphate) carbonate ion; bone; enamel; high-pressure phosphates;
D O I
10.1016/j.jssc.2004.04.002
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
The structure of a complex, disordered type A-B carbonate apatite (CAp) of approximate composition Ca-10(PO4)(6-y)(CO3)(x+(3/2)y)(OH)(2-2x), x-0.7, y-0.6, synthesized at 3GPa, 1400degreesC has been determined using single-crystal X-ray diffraction and FTIR spectroscopy at room temperature and pressure. Crystal data are: hexagonal, space group P6(3)/M, Z = 1; a = 9.5143(3), c = 6.8821(2) Angstrom, V = 539.5 Angstrom(3), and R = 0.025. There are three structural locations for the carbonate ion. The channel carbonate is mainly in the closed vertical configuration of the M structure, with two of its oxygen atoms close to the c-axis (A1 carbonate; IR bands at 1541 and 1449cm(-1)), but subordinate amounts are also located in an open vertical configuration (A2 carbonate; IR bands at 1563 and 1506cm(-1)). The type B carbonate ion is located close to the sloping faces of the PO4 tetrahedron (IR bands at 1474 and 1406cm(-1)), confirming earlier inferences from polarized IR spectra. (C) 2004 Elsevier Inc. All rights reserved.
引用
收藏
页码:3174 / 3182
页数:9
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