Fe2+/Fe3+ substitution in hydroxyapatite: Theory and experiment

Ming Jiang, J. Terra, A. M. Rossi, M. A. Morales, E. M. Baggio Saitovitch, and D. E. Ellis
Phys. Rev. B 66, 224107 – Published 11 December 2002
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Abstract

Electron paramagnetic resonance, Mössbauer spectroscopy, and electronic structure calculations were combined in order to study the local geometry of Fe2+/Fe3+ in Fe-doped hydroxyapatite. Atomistic simulations were carried out to obtain estimates of local geometry and lattice strain associated with fourfold, fivefold, and sixfold Fe sites. First-principles embedded cluster density functional calculations were performed to investigate the electronic structure associated with the substitution of calcium by Fe2+/Fe3+. Mössbauer isomer shift, quadrupole splitting, and the hyperfine magnetic field were calculated for each site and local coordination, for comparison to an experimental fit to a five-line model consisting of two bulk sites each for Fe2+ and Fe3+ and a surface hematitelike Fe3+ species.

  • Received 3 May 2002

DOI:https://doi.org/10.1103/PhysRevB.66.224107

©2002 American Physical Society

Authors & Affiliations

Ming Jiang1,2, J. Terra3, A. M. Rossi3, M. A. Morales3, E. M. Baggio Saitovitch3, and D. E. Ellis1

  • 1Department of Physics and Astronomy and Materials Research Center, Northwestern University, Evanston, Illinois 60208
  • 2Department of Physics, Yantai University, Yantai, People’s Republic of China, 264005
  • 3Centro Brasileiro de Pesquisas Fisicas, Rio de Janeiro, Brazil, 22290

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Vol. 66, Iss. 22 — 1 December 2002

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