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K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3)

During an attempt to crystallize potassium manganese diiron phosphate KMnFe(2)(PO(4))(3) by the flux method, a new phase, potassium dimanganese iron triphosphate, K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3), was isolated. This phase, whose composition was confirmed by ICP analysis, is isotypic with the alluau...

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Autores principales: Hidouri, Mourad, Ben Amara, Mongi
Formato: Texto
Lenguaje:English
Publicado: International Union of Crystallography 2010
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3050314/
https://www.ncbi.nlm.nih.gov/pubmed/21522509
http://dx.doi.org/10.1107/S1600536810051238
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author Hidouri, Mourad
Ben Amara, Mongi
author_facet Hidouri, Mourad
Ben Amara, Mongi
author_sort Hidouri, Mourad
collection PubMed
description During an attempt to crystallize potassium manganese diiron phosphate KMnFe(2)(PO(4))(3) by the flux method, a new phase, potassium dimanganese iron triphosphate, K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3), was isolated. This phase, whose composition was confirmed by ICP analysis, is isotypic with the alluaudite-like phosphates, thus it exhibits the (A2)(A′2)(A1)(A′1)(A′′1)(M1)(M2)(2)(PO(4))(3) general formula. The site occupancies led to the following cation distribution: 0.53 K on A′2 (site symmetry 2), 0.31 Mn on A′′1, 1.0 Mn on M1 (site symmetry 2) and (0.62 Fe + 0.38 Mn) on M2. The structure is built up from infinite chains of edge-sharing M1O(6) and M2O(6) octa­hedra. These chains run along [10[Image: see text]] and are connected by two different PO(4) tetrahedra, one of which exhibits 2 symmetry. The resulting three-dimensional framework delimits large tunnels parallel to [001], which are partially occupied by the K(+) and Mn(2+) cations.
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spelling pubmed-30503142011-04-26 K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3) Hidouri, Mourad Ben Amara, Mongi Acta Crystallogr Sect E Struct Rep Online Inorganic Papers During an attempt to crystallize potassium manganese diiron phosphate KMnFe(2)(PO(4))(3) by the flux method, a new phase, potassium dimanganese iron triphosphate, K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3), was isolated. This phase, whose composition was confirmed by ICP analysis, is isotypic with the alluaudite-like phosphates, thus it exhibits the (A2)(A′2)(A1)(A′1)(A′′1)(M1)(M2)(2)(PO(4))(3) general formula. The site occupancies led to the following cation distribution: 0.53 K on A′2 (site symmetry 2), 0.31 Mn on A′′1, 1.0 Mn on M1 (site symmetry 2) and (0.62 Fe + 0.38 Mn) on M2. The structure is built up from infinite chains of edge-sharing M1O(6) and M2O(6) octa­hedra. These chains run along [10[Image: see text]] and are connected by two different PO(4) tetrahedra, one of which exhibits 2 symmetry. The resulting three-dimensional framework delimits large tunnels parallel to [001], which are partially occupied by the K(+) and Mn(2+) cations. International Union of Crystallography 2010-12-11 /pmc/articles/PMC3050314/ /pubmed/21522509 http://dx.doi.org/10.1107/S1600536810051238 Text en © Hidouri and Ben Amara 2011 http://creativecommons.org/licenses/by/2.0/uk/ This is an open-access article distributed under the terms of the Creative Commons Attribution Licence, which permits unrestricted use, distribution, and reproduction in any medium, provided the original authors and source are cited.
spellingShingle Inorganic Papers
Hidouri, Mourad
Ben Amara, Mongi
K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3)
title K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3)
title_full K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3)
title_fullStr K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3)
title_full_unstemmed K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3)
title_short K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3)
title_sort k(0.53)mn(2.37)fe(1.24)(po(4))(3)
topic Inorganic Papers
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3050314/
https://www.ncbi.nlm.nih.gov/pubmed/21522509
http://dx.doi.org/10.1107/S1600536810051238
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