Infrared spectroscopic study of the formation of reactive silica by pyrolysis in vacuo of a trimethylsiloxylated sample

Citation
A. Burneau et al., Infrared spectroscopic study of the formation of reactive silica by pyrolysis in vacuo of a trimethylsiloxylated sample, J PHYS CH B, 104(5), 2000, pp. 990-996
Citations number
36
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF PHYSICAL CHEMISTRY B
ISSN journal
15206106 → ACNP
Volume
104
Issue
5
Year of publication
2000
Pages
990 - 996
Database
ISI
SICI code
1520-6106(20000210)104:5<990:ISSOTF>2.0.ZU;2-K
Abstract
The pyrolysis of a trimethylsiloxylated silica (TMS-silica) in vacuo up to 750 degrees C gives a "reactive silica" with surface species and properties similar to those previously reported by degassing a methoxylated silica ab ove 600 degrees C. Both surface silanes absorbing around 2290 cm(-1) and ve ry stable Si-C drop CH groups appear. A dissociative chemisorption of water on the reactive silica at 25 degrees C, leading to both SiH and SiOH group s, involves silylene centers (SiO)(2)Si: with a bicoordinated silicon atom. A concentration of about 0.13 sorption centers nm(-2) is estimated, which is a value higher than on pyrolyzed ex-methoxylated silica. The SiH stretch ing range in the infrared spectra of TMS-silica displays a larger variety o f intermediate SiH sites, at increasing temperatures, than for a methoxylat ed silica. In addition, the pyrolysis of TMS-silica creates intermediate al iphatic species absorbing at 2975 and 2986 cm(-1), correlated to the intens ity decrease of the v(a)CH(3) band of the TMS group at 2964 cm(-1). Similar intermediate components, assigned to Si(CH3)(2) and SiCH3 groups, were obs erved by oxidation of TMS-silica in air, although at much lower temperature s than in vacuo. A SiCH3 bond is thus attributed to the previously unidenti fied species which absorbs at 2983 cm(-1) during the last stages of the pyr olysis of a methoxylated silica.