The crystal structure of synthetic penkvilksite-2O, disodium titanium tetrasilicate dihydrate, Na2TiSi4O112H2O, a microporous titanosilicate, confirms the major features of a previous model that had been obtained by order–disorder (OD) theory from the known structure of penkvilksite-1M. An important difference from the previous model involves the hydrogen bonding of the water molecule which, on the basis of a Raman spectrum and the finding of only one of the two H atoms, is proposed to be disordered about a fixed O–H direction. The structure of penkvilksite-2O is based on (100) silicate layers linked by isolated TiO6 octahedra to form a heteropolyhedral framework. The layer is strongly corrugated, based on interlaced spiral chains, and is crossed by two different channels that have an effective channel width of about 3 A

Penkvilksite-2O: Na2TiSi4O11.2H2O

FERRARIS, Giovanni
2008-01-01

Abstract

The crystal structure of synthetic penkvilksite-2O, disodium titanium tetrasilicate dihydrate, Na2TiSi4O112H2O, a microporous titanosilicate, confirms the major features of a previous model that had been obtained by order–disorder (OD) theory from the known structure of penkvilksite-1M. An important difference from the previous model involves the hydrogen bonding of the water molecule which, on the basis of a Raman spectrum and the finding of only one of the two H atoms, is proposed to be disordered about a fixed O–H direction. The structure of penkvilksite-2O is based on (100) silicate layers linked by isolated TiO6 octahedra to form a heteropolyhedral framework. The layer is strongly corrugated, based on interlaced spiral chains, and is crossed by two different channels that have an effective channel width of about 3 A
2008
C64
i87
i90
Penkvilksite; OD theory; polytype; crystal structure; crystallography; mineralogy
Cadoni M.; Ferraris G.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2318/55518
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