Structural, spectroscopic and computational studies on the monoclinic polymorph (form I) of potassium hydrogen disilicate (KHSi2O5)

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.

Publisher

Mineralogical Society

Subject

Geochemistry and Petrology

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