β-Ca11B2Si4O22: six-fold twinning, crystal structure and thermal expansion

Author:

Volkov Sergey N.1,Yukhno Valentina A.1,Bubnova Rimma S.12,Shilovskikh Vladimir V.3

Affiliation:

1. Grebenshchikov Institute of the Silicate Chemistry of the Russian Academy of Sciences , Makarov Emb. 2 , 199034 St. Petersburg , Russia

2. Department of Crystallography , St. Petersburg State University , University Emb 7/9 , 199034 St. Petersburg , Russia

3. Geomodel Centre , St. Petersburg State University, Uliyanovskaya St. 1 , 198504 St. Petersburg , Russia

Abstract

Abstract The low-temperature polymorph β-Ca11B2Si4O22 crystallizes as a monoclinic structure [space group is P21/c, a=14.059(9), b=6.834(5), c=10.597(7) Å, β=100.735(8)°]. The crystal investigated by single-crystal X-ray diffraction was a twin composed of six individuals. The crystal structure is similar to that of mineral spurrite, Ca5(SiO4)2CO3, and can be described as a framework of [CaO5] and [CaO6] polyhedra, the cavities of which are filled with [SiO4] and [BO3] groups. The orientation relationship of twin domains was investigated by electron backscatter diffraction (EBSD). Thermal expansion was studied by high-temperature X-ray powder diffraction. It is slightly anisotropic: α 11=10, α 22=16, α 33=12×10−6°C−1 at 200°C.

Publisher

Walter de Gruyter GmbH

Subject

Inorganic Chemistry,Condensed Matter Physics,General Materials Science

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