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Garnet-type Mn(3)Cr(2)(GeO(4))(3)

Single crystals of garnet-type trimanganese(II) dichrom­i­um(III) tris­[orthogermanate(IV)], Mn(II) (3)Cr(III) (2)(GeO(4))(3), were obtained by utilizing a chemical transport reaction. Corres­ponding to the mineral garnet with the general formula A (II) (3) B (III) (2)(SiO(4))(3), each of the four e...

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Autores principales: Lipp, Christian, Strobel, Sabine, Lissner, Falk, Niewa, Rainer
Formato: Online Artículo Texto
Lenguaje:English
Publicado: International Union of Crystallography 2012
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3344288/
https://www.ncbi.nlm.nih.gov/pubmed/22590054
http://dx.doi.org/10.1107/S1600536812016832
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author Lipp, Christian
Strobel, Sabine
Lissner, Falk
Niewa, Rainer
author_facet Lipp, Christian
Strobel, Sabine
Lissner, Falk
Niewa, Rainer
author_sort Lipp, Christian
collection PubMed
description Single crystals of garnet-type trimanganese(II) dichrom­i­um(III) tris­[orthogermanate(IV)], Mn(II) (3)Cr(III) (2)(GeO(4))(3), were obtained by utilizing a chemical transport reaction. Corres­ponding to the mineral garnet with the general formula A (II) (3) B (III) (2)(SiO(4))(3), each of the four elements occupies only one crystallographically distinct position. Mn(2+) occupies the respective A position (Wyckoff site 24c, site symmetry 2.22), being surrounded by eight O atoms that form a distorted cube [d(Mn—O) = 2.291 (2) and 2.422 (2) Å, 4× each], while Cr(3+) on the B position (Wyckoff site 16a, site symmetry .-3.) is situated in a slightly distorted octa­hedron of six O(2−) anions [d(Cr—O) = 1.972 (2) Å, 6×]. In addition, the O atoms on general site 96h form isolated [GeO(4)](4−) tetra­hedra with Ge(4+) on site 24d [site symmetry -4..; d(Ge—O) = 1.744 (2) Å, 4×].
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spelling pubmed-33442882012-05-15 Garnet-type Mn(3)Cr(2)(GeO(4))(3) Lipp, Christian Strobel, Sabine Lissner, Falk Niewa, Rainer Acta Crystallogr Sect E Struct Rep Online Inorganic Papers Single crystals of garnet-type trimanganese(II) dichrom­i­um(III) tris­[orthogermanate(IV)], Mn(II) (3)Cr(III) (2)(GeO(4))(3), were obtained by utilizing a chemical transport reaction. Corres­ponding to the mineral garnet with the general formula A (II) (3) B (III) (2)(SiO(4))(3), each of the four elements occupies only one crystallographically distinct position. Mn(2+) occupies the respective A position (Wyckoff site 24c, site symmetry 2.22), being surrounded by eight O atoms that form a distorted cube [d(Mn—O) = 2.291 (2) and 2.422 (2) Å, 4× each], while Cr(3+) on the B position (Wyckoff site 16a, site symmetry .-3.) is situated in a slightly distorted octa­hedron of six O(2−) anions [d(Cr—O) = 1.972 (2) Å, 6×]. In addition, the O atoms on general site 96h form isolated [GeO(4)](4−) tetra­hedra with Ge(4+) on site 24d [site symmetry -4..; d(Ge—O) = 1.744 (2) Å, 4×]. International Union of Crystallography 2012-04-21 /pmc/articles/PMC3344288/ /pubmed/22590054 http://dx.doi.org/10.1107/S1600536812016832 Text en © Lipp et al. 2012 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
Lipp, Christian
Strobel, Sabine
Lissner, Falk
Niewa, Rainer
Garnet-type Mn(3)Cr(2)(GeO(4))(3)
title Garnet-type Mn(3)Cr(2)(GeO(4))(3)
title_full Garnet-type Mn(3)Cr(2)(GeO(4))(3)
title_fullStr Garnet-type Mn(3)Cr(2)(GeO(4))(3)
title_full_unstemmed Garnet-type Mn(3)Cr(2)(GeO(4))(3)
title_short Garnet-type Mn(3)Cr(2)(GeO(4))(3)
title_sort garnet-type mn(3)cr(2)(geo(4))(3)
topic Inorganic Papers
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3344288/
https://www.ncbi.nlm.nih.gov/pubmed/22590054
http://dx.doi.org/10.1107/S1600536812016832
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