Startseite Naturwissenschaften Electron paramagnetic resonance spectroscopic study of synthetic fluorapatite: Part II. Gd3+ at the Ca1 site, with a neighboring Ca2 vacancy
Artikel
Lizenziert
Nicht lizenziert Erfordert eine Authentifizierung

Electron paramagnetic resonance spectroscopic study of synthetic fluorapatite: Part II. Gd3+ at the Ca1 site, with a neighboring Ca2 vacancy

  • Ning Chen , Yuanming Pan EMAIL logo , John A. Weil und Mark J. Nilges
Veröffentlicht/Copyright: 28. März 2015
Veröffentlichen auch Sie bei De Gruyter Brill

Abstract

A W-band (94 GHz) electron paramagnetic resonance (EPR) study of synthetic fluorapatite with 57 ± 4 ppm Gd has been made on single crystals at ~287 K. The spectra disclosed the presence of a previously unreported type of Gd3+ center denoted by “b” herein (S = 7/2), in addition to the Gd3+ center “a” assigned to the Ca2 site using the results of a previous X-band (9.5 GHz) EPR study (Chen et al. 2002). In particular, the single-crystal W-band EPR spectra from three orthogonal-rota­tion planes allowed determination of an appropriate spin-Hamiltonian for center “b,” including the spin terms of type BS (matrix g) and S2 (matrix D) and the parameters associated with the high-spin terms of type S4and S6 as well as BS3 and BS5. Agreement between the observed and simulated single-crystal spectra confirmed the validity of the spin-Hamiltonian analysis.β

The principal values of the matrices g and D [e.g.. D/geβe = 1069.2( 1) G and E/geβe = 52.4(3) G] suggest a considerably distorted rhombic local environment for the Gd3+ ions in center “b.” The principal directions of D suggest that “b” corresponds to Gd3+ at the Ca 1 site. This site assignment is supported by a pseudo-symmetry analysis of the term S4, i.e., approximate matching of the direc­tions of the calculated pseudo-symmetry axes to the bond directions and face normals of the coordi­nation polyhedron of the ideal Cal site. The data suggest that the incorporation of Gd3+ into the Cal site is achieved by a coupled substitution (2Gd3+ + □ ↔ 3Ca2+) involving a Ca2+ vacancy □ and that the vacancy is located at a next-nearest-neighbor Ca2 site, resulting in a Gd3+- - □ - Gd3+ arrange­ment, with the cations well separated.

Received: 2000-12-15
Accepted: 2001-8-10
Published Online: 2015-3-28
Published in Print: 2002-1-1

© 2015 by Walter de Gruyter Berlin/Boston

Artikel in diesem Heft

  1. Study on adsorption of submicrometer gold on kaolinite by quantum chemistry calculations
  2. Image distortion in scanning probe microscopy
  3. Multiple length scale growth spirals on metamorphic graphite {001} surfaces studied by atomic force microscopy
  4. 29Si MAS NMR study of diopside–Ca-Tschermak clinopyroxenes: Detecting both tetrahedral and octahedral Al substitution
  5. Electron paramagnetic resonance spectroscopic study of synthetic fluorapatite: Part I. Local structural environment and substitution mechanism of Gd3+ at the Ca2 site
  6. Electron paramagnetic resonance spectroscopic study of synthetic fluorapatite: Part II. Gd3+ at the Ca1 site, with a neighboring Ca2 vacancy
  7. Determination of the H3BO3 concentration in fluid and melt inclusions in granite pegmatites by laser Raman microprobe spectroscopy
  8. Analysis of natural H2O + CO2 + NaCl fluid inclusions in the hydrothermal diamond anvil cell
  9. Thermodynamics of the amphiboles: Ca-Mg-Fe2+ quadrilateral
  10. Phase boundary between rutile-type and CaCl2-type germanium dioxide determined by in situ X-ray observations
  11. The nature, formation, and stability of end-member illite: A hypothesis
  12. Determination of melanterite-rozenite and chalcanthite-bonattite equilibria by humidity measurements at 0.1 MPa
  13. Pressure-temperature paths from garnet-zoning: Evidence for multiple episodes of thrust burial in the hinterland of the Sevier orogenic belt
  14. Mineralogical and Mössbauer spectroscopic study of a diopside occurring in the marbles of Andranondambo, southern Madagascar
  15. Correlations of octahedral cations with OH, O2–, Cl, and F in biotite from volcanic rocks and xenoliths
  16. H positions in leucophoenicite, Mn7Si3O12(OH)2: A close relative of the hydrous B phases
  17. Ominelite, (Fe,Mg)Al3BSiO9 (Fe2+ analogue of grandidierite), a new mineral from porphyritic granite in Japan
  18. Closure in crystal size distributions (CSD), verification of CSD calculations, and the significance of CSD fans
  19. Icosahedral domain structure of framboidal pyrite
Heruntergeladen am 5.2.2026 von https://www.degruyterbrill.com/document/doi/10.2138/am-2002-0106/pdf
Button zum nach oben scrollen