Silica gel containing diyne units have been obtained from molecular organosilicon precursors and the properties associated to the very reactive unsaturated organic moieties have been explored. The sol−gel polymerization of 1,4-bis(trimethoxysilyl)-1,3-butadiyne ((MeO) 3 SiC⋮CC⋮CSi(OMe) 3 ) quantitatively led to a silsesquioxane network, [O 1.5 SiC⋮CC⋮CSiO 1.5 ] n, consisting of siloxanes chains with bridging diyne units. The derived xerogels were characterized by IR and 13 C and 29 Si CP MAS NMR spectroscopies. The major environment of the Si atom corresponded to a T 2 C Si (OR)(OSi) 2 substructure, and only minor Si−C bond cleavage occurred during the sol−gel condensation. The chemical reactivity of the hybrid organic−inorganic gel was studied and used as a tool for the study of the organization of the solid induced by the organic moieties. Upon heating, in the solid state, the diyne fragments undergo a polyaddition to give an ene−yne structure. The polymerization, observed in the solid state, suggests favorable arrangements of the organic fragments within the amorphous solid. The resulting composite material consists in a network made of interpenetrating ene−yne and siloxane polymers. On the other hand, the organic diyne fragments in the hybrid gel have been removed, leaving silica behind, in two ways: (i) The thermal oxidation in air led to microporous silicas with N 2 BET surface areas in the range 300−350 m 2 g -1 . (ii) Interestingly, the smooth Si−C bond cleavage by MeOH catalyzed by NH 4 F gave highly porous silica with N 2 BET surface areas up to 950 m 2 g -1 . The latter elimination of the organic moiety under mild reaction conditions is of particular interest since it gives rise to silica with a surface area significantly higher than that produced upon thermal oxidation and higher than that of the originating hybrid precursor.
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Corriu et al. (1996) studied this question.
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