Preparation and characterisation of monoclinic hydroxyapatite and its precipitated carbonate apatite intermediate

Abstract

Five 100 g batches of a carbonate apatite (the intermediate) were produced by heating an aqueous slurry of CaCO 3 and CaHPO 4 with an overall Ca/P mole ratio of 5/3 with vigorous stirring. Each intermediate produced by boiling off water was heated in vacuum at 1100°C to remove carbonate, then steamed at 900°C to ensure complete hydroxylation. Comparison of calculated and observed X-ray diffraction patterns showed final products containing 50–100 wt% monoclinic hydroxyapatite (remainder hexagonal). Rietveld refinements in P6 3/m gave structures similar to several hydroxyapatite standards, including NIST SRM 2910, although there was no evidence from X-ray diffraction that the latter was in the monoclinic form. Refinements from standards and final products were slightly different from published single crystal data for Holly Springs hydroxyapatite. This is attributed to known impurities in mineral hydroxyapatite and indicates that parameters from the Rietveld refinements are closer to the true values for pure hydroxyapatite. Rietveld refinements for intermediates showed small, but significant differences from the final product, the largest being in O1 x, O2 x and O(H) z. All P–O bond lengths were shorter than in the final product, resulting in a 3.2% lower PO 4 tetrahedron volume. The occupancies of P and Ca(2) were reduced. These differences are attributed to partial replacement of PO 4 3− by CO 3 2− ions.