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Nb-substitution and Cs+ ion-exchange in the titanosilicate sitinakite
Journal article   Peer reviewed

Nb-substitution and Cs+ ion-exchange in the titanosilicate sitinakite

V Luca, J V Hanna, M E Smith, M James, D R G Mitchell and John R Bartlett
Microporous and Mesoporous Materials, Vol.55(1), pp.1-13
2002
url
https://doi.org/10.1016/S1387-1811(02)00353-0View
Published Version

Abstract

Chemical Sciences Engineering silicotitanate titanosilicate ion-exchange cesium NMR XRD
Cesium-133 MAS NMR and X-ray powder diffraction have been used to investigate Cs+ ion-exchange in synthetic samples of the titanosilicate mineral, sitinakite. The effect of incorporating Nb using Nb(V) ethoxide as the Nb source into the sitinakite framework and its influence on Cs+ ion-exchange was also studied. Refinements of X-ray powder data show that substitution of niobium for titanium in the sitinakite framework occurs to a limited extent using the synthetic method employed. Niobium substitution is also supported by 29Si MAS NMR spectra. Any niobium that was not substituted into the sitinakite structure was present in a distinct Nb-rich oxide/hydroxide phase. NMR studies reveal that in the undoped samples with low Cs loadings, at least four types of Cs+ are present, while at higher levels of Cs+ loadings, an additional two sites are populated. Similar sites appear to be occupied in the Nb-substituted samples but the relative occupancies are strongly modulated relative to the undoped samples. The multiple Cs environments are attributed to Cs+ ions occupying similar structural sites in the titanosilicate channels but experiencing different hydration water coordination environments.

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