Crystal structure refinement of synthetic osumilite-type phases BaMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub>, SrMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub> and Mg<sub>2</sub>Al<sub>4</sub>Si<sub>11</sub>O<sub>30</sub>BaMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub>, SrMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub> and Mg<sub>2</sub>Al<sub>4</sub>Si<sub>11</sub> O<sub>30</sub> BaMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub>, SrMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub> and Mg<sub>2</sub>Al<sub>4</sub>Si<sub>11</sub> O<sub>30</sub>BaMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub>, SrMg<sub>2</sub>Al<sub>6</sub>Si<sub>9</sub>O<sub>30</sub> and Mg<sub>2</sub>Al<sub>4</sub>Si<sub>11</sub> O<sub>30</sub>
- Autor(en)
- W. Winter, T. Armbruster, Christian Leopold Lengauer
- Abstrakt
Three synthetic osumilite-type double-ring silicates of technical interest as crystalline bases of glass-ceramic materials, with compositions BaMg2Al6Si9O30, SrMg2Al6Si9O30 and Mg2Al4Si11O30 (MAS), were synthesized by crystallization of glasses; their crystal structures were subsequently refined.
The structure of BaMg2AI6Si9O30 (P6/mcc, a = 10.129(2), c = 14.340(2) Å) was refined to Rw = 2.46 % for 1020 single-crystal reflections with MoKα X-radiation. The structures of SrMg2AI6Si9O30 (a = 10.1273(5),
c = 14.2274(8) Å) and Mg2AI4Si11O30 (a = 10.058(2),c = 14.336(3) Å) were refined in space group P6/mcc from CuKα X-ray powder data using multiphase Rietveld methods.
The C site between consecutive double-ring units is occupied by Ba2+ and Sr2+ in BaMg2AI6Si9O30 and SrMg2Al6Si9O30,respectively,while it is empty in MAS osumilite. This leads to increased C-O2 distances in MAS osumilite (3.18(1) Å) compared to 3.041(1) and 3.025(9) Å for the Ba- and Sr-bearing compounds, respectively. The longer C-O2 distance is compensated by a stronger distortion of the neighbouring Tl double-rings and T2 tetrahedra. In BaMg2AI6Si9O30 and SrMg2Al6Si9O30,Mg is constrained to the octahedral A site whereas in MAS
osumilite the A octahedron and the T2 tetrahedron have a mixed Mg, AI occupation.Osumilite-type compounds with partial A1 in the six-membered double-rings show a different T1-O-T1 angular distortion compared to double-ring silicates with pure Si12O30 units. The reason for this difference is not primarily the A1 concentration on T1 but the higher ionic valences on A and T2 which become necessary for charge balance. -from Authors
- Organisation(en)
- Institut für Mineralogie und Kristallographie
- Externe Organisation(en)
- TH Darmstadt, Universität Bern
- Journal
- European Journal of Mineralogy
- Band
- 7
- Seiten
- 277-286
- Anzahl der Seiten
- 10
- ISSN
- 0935-1221
- Publikationsdatum
- 1995
- Peer-reviewed
- Ja
- ÖFOS 2012
- 105116 Mineralogie, 105113 Kristallographie
- ASJC Scopus Sachgebiete
- Geochemistry and Petrology
- Link zum Portal
- https://ucrisportal.univie.ac.at/de/publications/crystal-structure-refinement-of-synthetic-osumilitetype-phases-bamg2al6si9o30-srmg2al6si9o30-and-mg2al4si11o30bamg2al6si9o30-srmg2al6si9o30-and-mg2al4si11-o30-bamg2al6si9o30-srmg2al6si9o30-and-mg2al4si11-o30bamg2al6si9o30-srmg2al6si9o30-and-mg2al4si11-o30(310396c8-01a8-4cb7-9768-fa8a53ba3ce8).html