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The crystal structure of synthetic zeolite Na-P 1, an isotype of gismondine

Published/Copyright: July 28, 2010
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Abstract

The crystal structure of synthetic zeolite Na-P 1 (or B1) has been solved using x-ray data obtained from a multiply twinned crystal. The structure is shown to be based on a gismondine-type framework with maximum possible symmetry I41/amd. The cell dimensions were found to be a = c = 10.04 Å but the intensity data clearly indicated noncubic symmetry. Weak b reflections with h + k + l = 2n + 1 have also been recorded but were not used in this investigation. Refinement assuming space group I[unk] proceeded to an intensity R value of 0.077. The true symmetry must be lower and the structure appears to be highly pseudosymmetric.

The typical spherulitic aggregates of most Na-P 1 preparations are thought to be submicroscopically twinned. The formation of twins is favoured by the topology and the extraordinary flexibility of the framework. Its flexibility also explains the comparatively large variations in cell dimensions and apparent symmetry of known gismondine isotypes, and could account for the occurrence of various P phases.

Published Online: 2010-07-28
Published in Print: 1972-09
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