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The crystal structure of aklimaite, Ca4[Si2O5(OH)2](OH)4 · 5 H2O

  • Natalia V. Zubkova , Igor V. Pekov , Dmitry Yu. Pushcharovsky , Aleksandr. E. Zadov and Nikita V. Chukanov
Published/Copyright: December 21, 2011
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Zeitschrift für Kristallographie - Crystalline Materials
From the journal Volume 227 Issue 7

Abstract

Aklimaite, Ca4[Si2O5(OH)2](OH)4 · 5 H2O, is monoclinic, space group C2/m, a = 16.907(5), b = 3.6528(8), c = 13.068(4) Å, β = 117.25(4)°, V = 717.5(4) Å3, Z = 2. The crystal structure was solved by direct methods and refined to R(F) = 0.1100 for 1196 unique reflections with I > 2σ(I). Aklimaite is a sorosilicate of a new structure type. The structure is based on corrugated layers of Ca-centered polyhedra formed by alternating columns of edge-sharing Ca octahedra and seven-coordinated polyhedra, extending along [010] which are connected with Ca seven-coordinated polyhedra of another type via common edges. Si-centered tetrahedra form isolated Si2O5(OH)2 groups which are combined in a motif like interrupted chains (“dotted lines”) sharing O—O edges with Ca polyhedra of the layers.


* Correspondence address: Moscow State University, Geology Department, 119991 Moscow, Russische Föderation,

Published Online: 2011-12-21
Published in Print: 2012-07

© by Oldenbourg Wissenschaftsverlag, München, Germany

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