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Synthesis of gold nanoparticles in sol–gel glass porogens containing [bmim][BF4] ionic liquid

The [bmim][BF 4 ] ionic liquid effect on gold nanoparticles formation in silica sol–gel materials is studied in order to produce gel-derived glasses with optical properties. The characteristic red color from gold nanoparticles is observed for transparent glass monoliths obtained sintering, between 3...

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Bibliographic Details
Published in:Journal of sol-gel science and technology 2013-11, Vol.68 (2), p.234-244
Main Authors: Ruivo, A., Ventura, M. G., Gomes da Silva, M. D. R., Laia, C. A. T.
Format: Article
Language:English
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Summary:The [bmim][BF 4 ] ionic liquid effect on gold nanoparticles formation in silica sol–gel materials is studied in order to produce gel-derived glasses with optical properties. The characteristic red color from gold nanoparticles is observed for transparent glass monoliths obtained sintering, between 365 and 425 °C, a silica sol–gel precursor containing HAuCl 4 ·3H 2 O and [bmim][BF 4 ], under normal atmospheric conditions. The effect of sintering the ionogel at different temperatures (T sint ) or times (t sint ) on the optical properties, shape, size, and distribution of gold nanoparticles is discussed. Presence of the gold particles is observed using transmission electron microscopy images followed by energy dispersive X-ray spectroscopy analysis. The thermal decomposition of [bmim][BF 4 ] in the ionogel is investigate using calorimetric and spectroscopic techniques, and by analysis of volatile compounds released by the sol–gel material during sintering. With these results a mechanism for the formation of the gold nanoparticles is proposed, where a first ionic liquid degradation step provides the reductive environment that enables the gold nanoparticles production at the range of temperatures between 350 and 425 °C. Upon sintering the synthesized materials the ionic liquid acts as a sacrificial additive and the ionic liquid thermal decomposition products enables the formation of gold nanoparticles in the sol–gel matrix.
ISSN:0928-0707
1573-4846
DOI:10.1007/s10971-013-3159-6