Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis
[AI]4[AII]6(BO4)6X2 apatites can flexibly accommodate numerous cationic, metalloid and anionic substitutions. Using a combination of new refinements and published structures, this paper reviews correlations between substituent type and framework adaptation through adjustment of the AIO6 metaprism tw...
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sg-ntu-dr.10356-856082023-07-14T15:51:06Z Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis Lim, S. C. Baikie, Tom Pramana, Stevin S. Smith, Ron White, Timothy John School of Materials Science & Engineering Metaprism twist angle Apatite crystal chemistry [AI]4[AII]6(BO4)6X2 apatites can flexibly accommodate numerous cationic, metalloid and anionic substitutions. Using a combination of new refinements and published structures, this paper reviews correlations between substituent type and framework adaptation through adjustment of the AIO6 metaprism twist angle, φ. These systematics are illustrated through powder neutron diffraction refinement of the crystal chemistry of A10(PO4)6F2 (A=Ca, Sr) fluorapatites. Variations in φ reflect changes in the relative size of the AI4(BO4)6 framework and AII6X2 tunnel content and can be used to quantitatively assess the reliability of AI/AII cation partitioning coefficients determined by Rietveld analysis. In the simplest cases of bi-ionic substitution, the metaprism twist systematics conform to three principle trends: (i) For A-type divalent substitution, the larger A2+ species preferentially enters the channel before partitioning to the framework. This leads to parabolic modification in φ across the compositional series; (ii) For B-type pentavalent compounds, the φ variation will be linear in accord with the relative B5+ ionic size; and (iii) For X-type substitution of halide anions, φ will be reduced as the average size increases. Departures from these trends may indicate polymorphism, compositional anomalies, AI/AII order disequilibrium, or poor structure refinement, and may be extended to chemically complex apatites with simultaneous substitutions over the A, B and X sites. Accepted version 2017-09-15T07:00:15Z 2019-12-06T16:07:03Z 2017-09-15T07:00:15Z 2019-12-06T16:07:03Z 2011 Journal Article Lim, S. C., Baikie, T., Pramana, S. S., Smith, R., & White, T. J. (2011). Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis. Journal of Solid State Chemistry, 184(11), 2978-2986. 0022-4596 https://hdl.handle.net/10356/85608 http://hdl.handle.net/10220/43742 10.1016/j.jssc.2011.08.031 en Journal of Solid State Chemistry © 2011 Elsevier. This is the author created version of a work that has been peer reviewed and accepted for publication by Journal of Solid State Chemistry, Elsevier. It incorporates referee’s comments but changes resulting from the publishing process, such as copyediting, structural formatting, may not be reflected in this document. The published version is available at: [http://dx.doi.org/10.1016/j.jssc.2011.08.031]. 38 p. application/pdf |
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Metaprism twist angle Apatite crystal chemistry Lim, S. C. Baikie, Tom Pramana, Stevin S. Smith, Ron White, Timothy John Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis |
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[AI]4[AII]6(BO4)6X2 apatites can flexibly accommodate numerous cationic, metalloid and anionic substitutions. Using a combination of new refinements and published structures, this paper reviews correlations between substituent type and framework adaptation through adjustment of the AIO6 metaprism twist angle, φ. These systematics are illustrated through powder neutron diffraction refinement of the crystal chemistry of A10(PO4)6F2 (A=Ca, Sr) fluorapatites. Variations in φ reflect changes in the relative size of the AI4(BO4)6 framework and AII6X2 tunnel content and can be used to quantitatively assess the reliability of AI/AII cation partitioning coefficients determined by Rietveld analysis. In the simplest cases of bi-ionic substitution, the metaprism twist systematics conform to three principle trends:
(i) For A-type divalent substitution, the larger A2+ species preferentially enters the channel before partitioning to the framework. This leads to parabolic modification in φ across the compositional series;
(ii) For B-type pentavalent compounds, the φ variation will be linear in accord with the relative B5+ ionic size; and
(iii) For X-type substitution of halide anions, φ will be reduced as the average size increases.
Departures from these trends may indicate polymorphism, compositional anomalies, AI/AII order disequilibrium, or poor structure refinement, and may be extended to chemically complex apatites with simultaneous substitutions over the A, B and X sites. |
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School of Materials Science & Engineering |
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School of Materials Science & Engineering Lim, S. C. Baikie, Tom Pramana, Stevin S. Smith, Ron White, Timothy John |
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Article |
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Lim, S. C. Baikie, Tom Pramana, Stevin S. Smith, Ron White, Timothy John |
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Lim, S. C. |
title |
Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis |
title_short |
Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis |
title_full |
Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis |
title_fullStr |
Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis |
title_full_unstemmed |
Apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis |
title_sort |
apatite metaprism twist angle (φ) as a tool for crystallochemical diagnosis |
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2017 |
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https://hdl.handle.net/10356/85608 http://hdl.handle.net/10220/43742 |
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1772828546572484608 |