ISSN:
1432-0827
Keywords:
Key words: Fluoride — Octacalcium phosphate — Apatite — Fluoridation — Enamel mineralization
Source:
Springer Online Journal Archives 1860-2000
Topics:
Biology
,
Medicine
,
Physics
Notes:
Abstract. To study the roles of F− ions in the formation of apatite crystals embedding octacalcium phosphate (OCP) lamella in the center of apatite (Ap), a range of the Ap/OCP/Ap lamellar-mixed crystals were synthesized under various concentrations of fluoride ion (F−) from 0.1–1.0 ppm at pH 6.5 and 37°C. The products were analyzed for the F− incorporation, F− distribution, and the amount of OCP and Ap by chemical analysis, X-ray diffraction (XRD), electron probe microanalysis (EPMA), and nuclear magnetic resonance (NMR) techniques. The F− content and the amount of apatite in the crystalline product increased with an increase in the F− concentration in solution, whereas the amount of OCP and the yield of total product decreased. EPMA indicated that F− ions are distributed in the crystals almost homogeneously. The combined analysis suggested that a low-substituted fluoridated hydroxyapatite (FHAp) grew on a small amount of F−-containing OCP or on a surface-reaction layer of OCP, which has accumulated a small amount of F−. The roles of F− ions were hypothesized as the reduction of the growth rate and/or the critical thickness in the a*-axis direction of OCP, the enhancement of hydrolysis of OCP, and the activation of the growth of FHAp, resulting in thinner OCP lamella and thicker apatite lamella in the a*-axis direction with an increase in F− concentration.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/s002239900143
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