Arsenate substitution in hydroxylapatite: Structural characterization of the Ca5(PxAs1–xO4)3OH solid solution
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Young J. Lee
, Peter W. Stephens , Yuanzhi Tang , Wei Li , Brian L. Phillips , John B. Parise and Richard J. Reeder
Abstract
Arsenate (As5+) substitution in the hydroxylapatite structure was examined using a combination of crystallographic and spectroscopic techniques. Samples of hydroxylapatite, the As5+-substituted analog (synthetic johnbaumite), and five intermediate compositions were synthesized from solution. Synchrotron X-ray diffraction data show that all samples are single-phase, confirming complete substitution. No evidence is found for lowering of symmetry below P63/m. Rietveld structure refinements show progressive expansion of the unit cell with increasing As substitution, which can be accounted for primarily by an average expansion of the tetrahedral site. Sizes of Ca polyhedra show little variation as a result of As substitution. NMR results show no evidence for local clustering of PO4 tetrahedra. EXAFS confirms that the size of As-centered tetrahedra remains constant across the solid-solution series.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
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- Arsenate substitution in hydroxylapatite: Structural characterization of the Ca5(PxAs1–xO4)3OH solid solution
- The crystal chemical role of Zn in alunite-type minerals: Structure refinements for kintoreite and zincian kintoreite
- Application of precession electron diffraction to the characterization of (021) twinning in pseudo-hexagonal coesite
- Structure, thermodynamic, and transport properties of molten Mg2SiO4: Molecular dynamics simulations and model EOS
- High-pressure behavior of åkermanite and gehlenite and phase stability of the normal structure in melilites
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