Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2

The crystal chemistries of synthetic mimetite, Pb10(As5+O4)6(Cl2-xOx/2), a neutral apatite, and finnemanite, Pb10(As3+O3)6Cl2, a reduced apatite, were characterized using a combination of X-ray powder diffraction, neutron diffraction, transmission electron microscopy and X-ray photoelectron spe...

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Main Authors: Baikie, Tom, Ferraris, Cristiano, Pring, Allan, Klooster, Wim T., Madhavi, S., Pramana, Stevin S., Schmidt, G., White, Timothy John
Other Authors: School of Materials Science & Engineering
Format: Article
Language:English
Published: 2014
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Online Access:https://hdl.handle.net/10356/79513
http://hdl.handle.net/10220/18841
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-795132023-07-14T15:57:13Z Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2 Baikie, Tom Ferraris, Cristiano Pring, Allan Klooster, Wim T. Madhavi, S. Pramana, Stevin S. Schmidt, G. White, Timothy John School of Materials Science & Engineering DRNTU::Engineering::Materials The crystal chemistries of synthetic mimetite, Pb10(As5+O4)6(Cl2-xOx/2), a neutral apatite, and finnemanite, Pb10(As3+O3)6Cl2, a reduced apatite, were characterized using a combination of X-ray powder diffraction, neutron diffraction, transmission electron microscopy and X-ray photoelectron spectroscopy. Both phases conform to hexagonal P63/m symmetry; however, the temperature-driven transformation of clinomimetite to mimetite described earlier was not confirmed. The average mimetite structure is best described through the introduction of partially occupied oxygen sites. A better understanding of the mixed arsenic speciation in apatites can guide the formulation of waste form ceramics and improve models of long-term durability after landfill disposal. Published version 2014-02-19T04:34:11Z 2019-12-06T13:27:10Z 2014-02-19T04:34:11Z 2019-12-06T13:27:10Z 2008 2008 Journal Article Baikie, T., Ferraris, C., Klooster, W. T., Madhavi, S., Pramana, S. S., Pring, A., et al. (2008). Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2. Acta crystallographica section B structural science, B64, 34-41. https://hdl.handle.net/10356/79513 http://hdl.handle.net/10220/18841 10.1107/S0108768107066402 en Acta crystallographica section B structural science © 2008 International Union of Crystallography. This paper was published in Acta Crystallographica Section B Structural Science and is made available as an electronic reprint (preprint) with permission of International Union of Crystallography. The paper can be found at: [DOI: http://dx.doi.org/10.1107/S0108768107066402]. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law. application/pdf
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic DRNTU::Engineering::Materials
spellingShingle DRNTU::Engineering::Materials
Baikie, Tom
Ferraris, Cristiano
Pring, Allan
Klooster, Wim T.
Madhavi, S.
Pramana, Stevin S.
Schmidt, G.
White, Timothy John
Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2
description The crystal chemistries of synthetic mimetite, Pb10(As5+O4)6(Cl2-xOx/2), a neutral apatite, and finnemanite, Pb10(As3+O3)6Cl2, a reduced apatite, were characterized using a combination of X-ray powder diffraction, neutron diffraction, transmission electron microscopy and X-ray photoelectron spectroscopy. Both phases conform to hexagonal P63/m symmetry; however, the temperature-driven transformation of clinomimetite to mimetite described earlier was not confirmed. The average mimetite structure is best described through the introduction of partially occupied oxygen sites. A better understanding of the mixed arsenic speciation in apatites can guide the formulation of waste form ceramics and improve models of long-term durability after landfill disposal.
author2 School of Materials Science & Engineering
author_facet School of Materials Science & Engineering
Baikie, Tom
Ferraris, Cristiano
Pring, Allan
Klooster, Wim T.
Madhavi, S.
Pramana, Stevin S.
Schmidt, G.
White, Timothy John
format Article
author Baikie, Tom
Ferraris, Cristiano
Pring, Allan
Klooster, Wim T.
Madhavi, S.
Pramana, Stevin S.
Schmidt, G.
White, Timothy John
author_sort Baikie, Tom
title Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2
title_short Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2
title_full Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2
title_fullStr Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2
title_full_unstemmed Crystal chemistry of mimetite, Pb10(AsO4)6Cl1.48O0.26, and finnemanite, Pb10(AsO3)6Cl2
title_sort crystal chemistry of mimetite, pb10(aso4)6cl1.48o0.26, and finnemanite, pb10(aso3)6cl2
publishDate 2014
url https://hdl.handle.net/10356/79513
http://hdl.handle.net/10220/18841
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