Author:
Schmidmair D.,Kahlenberg V.,Perfler L.,Többens D. M.
Abstract
AbstractHydrothermal treatment of quartz with 2 M K2CO3solutions at 623 K and 1 kbar resulted in the formation of single crystals of the monoclinic polymorph of potassium hydrogen disilicate (KHSi2O5or KSi2O4(OH)). Basic crystallographic data of this so-called phase I at room conditions are as follows: space groupC2/m,a= 14.5895(10) Å,b= 8.2992(3) Å,c= 9.6866(7) Å, β = 122.756(10)°,V= 986.36(10) Å3,Z= 8. The structure was determined by direct methods and refined to a residual of R(|F|) = 0.0224 for 892 independent observed reflections withI> 2σ(I). The compound belongs to the group of chain silicates. It is based on crankshaft-likeviererdouble-chains running parallel to [010]. The H atoms are associated with silanol groups. Hydrogen bonding between neighbouring double-chains results in the formation of ∼5 Å wide slabs. The three crystallographically independent K cations with six to eight O ligands provide linkage (1) between the chains of a single slab or (2) between adjacent slabs. Structural investigations have been supplemented by micro-Raman spectroscopy. The interpretation of the spectroscopic data including the allocation of the bands to certain vibrational species has been aided by DFT calculations.
Subject
Geochemistry and Petrology
Cited by
5 articles.
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