Thortveitite-type Tm2Si2O7
Single crystals of dithulium disilicate, Tm2Si2O7, were obtained in flux synthesis experiments in the system SiO2–Tm2O3–LiF at ambient pressure. The compound belongs to the group of sorosilicates, i.e. it is based on [Si2O7]-units and crystallizes in the thortveitite (Sc2Si2O7) structure type. The T...
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Series: | Acta Crystallographica Section E |
Online Access: | http://scripts.iucr.org/cgi-bin/paper?S1600536814013142 |
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doaj-ab8e3fc6fd5344b4bf68e91d24f739dd2020-11-25T01:27:09ZengInternational Union of CrystallographyActa Crystallographica Section E1600-53682014-07-01707i34i3510.1107/S1600536814013142wm5029Thortveitite-type Tm2Si2O7Volker Kahlenberg0Paul Aichholzer1University of Innsbruck, Institute of Mineralogy & Petrography, Innrain 52, A-6020 Innsbruck, AustriaUniversity of Innsbruck, Institute of Mineralogy & Petrography, Innrain 52, A-6020 Innsbruck, AustriaSingle crystals of dithulium disilicate, Tm2Si2O7, were obtained in flux synthesis experiments in the system SiO2–Tm2O3–LiF at ambient pressure. The compound belongs to the group of sorosilicates, i.e. it is based on [Si2O7]-units and crystallizes in the thortveitite (Sc2Si2O7) structure type. The Tm3+ cation (site symmetry .2.) occupies a distorted octahedral site, with Tm—O bond lengths in the range 2.217 (4)–2.289 (4) Å. Each of the octahedra shares three of its edges with adjacent [TmO6] groups, resulting in the formation of layers parallel to (001). The individual [SiO4] tetrahedra are more regular, i.e. the differences between the bond lengths between Si and the bridging and non-bridging O atoms are not very pronounced. The layers containing the octahedra and the sheets containing the [Si2O7] groups (point group symmetry 2/m) form an alternating sequence. Linkage is provided by sharing common oxygen vertices.http://scripts.iucr.org/cgi-bin/paper?S1600536814013142 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Volker Kahlenberg Paul Aichholzer |
spellingShingle |
Volker Kahlenberg Paul Aichholzer Thortveitite-type Tm2Si2O7 Acta Crystallographica Section E |
author_facet |
Volker Kahlenberg Paul Aichholzer |
author_sort |
Volker Kahlenberg |
title |
Thortveitite-type Tm2Si2O7 |
title_short |
Thortveitite-type Tm2Si2O7 |
title_full |
Thortveitite-type Tm2Si2O7 |
title_fullStr |
Thortveitite-type Tm2Si2O7 |
title_full_unstemmed |
Thortveitite-type Tm2Si2O7 |
title_sort |
thortveitite-type tm2si2o7 |
publisher |
International Union of Crystallography |
series |
Acta Crystallographica Section E |
issn |
1600-5368 |
publishDate |
2014-07-01 |
description |
Single crystals of dithulium disilicate, Tm2Si2O7, were obtained in flux synthesis experiments in the system SiO2–Tm2O3–LiF at ambient pressure. The compound belongs to the group of sorosilicates, i.e. it is based on [Si2O7]-units and crystallizes in the thortveitite (Sc2Si2O7) structure type. The Tm3+ cation (site symmetry .2.) occupies a distorted octahedral site, with Tm—O bond lengths in the range 2.217 (4)–2.289 (4) Å. Each of the octahedra shares three of its edges with adjacent [TmO6] groups, resulting in the formation of layers parallel to (001). The individual [SiO4] tetrahedra are more regular, i.e. the differences between the bond lengths between Si and the bridging and non-bridging O atoms are not very pronounced. The layers containing the octahedra and the sheets containing the [Si2O7] groups (point group symmetry 2/m) form an alternating sequence. Linkage is provided by sharing common oxygen vertices. |
url |
http://scripts.iucr.org/cgi-bin/paper?S1600536814013142 |
work_keys_str_mv |
AT volkerkahlenberg thortveititetypetm2si2o7 AT paulaichholzer thortveititetypetm2si2o7 |
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