It
is generally assumed that the hydrothermal stability of organically
modified silica networks is promoted by high monomer connectivity,
network flexibility, and the presence of hydrophobic groups in the
network. In this study a range of organosilica compositions is synthesized
to explore the extent to which these factors play a role in the hydrothermal
dissolution of these materials. Compositions were synthesized from
hexafunctional organically bridged silsesquioxanes (OR1)3Si–R–Si(OR1)3 (R
= −CH2–, –C2H4–, –C6H12–, –C8H16–, –p-C6H4–; R1 = −CH3, –C2H5), tetrafunctional (OEt)2Si(CH3)–C2H4–Si(CH3)(OEt)2 and Si(OEt)4, trifunctional silsesquioxanes
R′-Si(OMe)3 (R′=CH3, n-C3H7, cyclo-C6H11, phenyl),
and bifunctional Si(i-C3H7)2(OMe)2. The bond strain, connectivity and hydroxyl
concentration of all networks were estimated using 29Si
cross-polarized magic angle spinning nuclear magnetic resonance and
Fourier-transform infrared spectroscopy. The hydrophilicity was characterized
by monitoring the water uptake of the materials in moisture treatments
with thermogravimetric analysis, differential scanning calorimetry,
and Fourier-transform infrared spectroscopy. The resistance of each
network against hydrothermal dissolution in a water/1,5-pentanediol
mixture at 80 °C and pH 1, 7, and 13 was analyzed with inductively
coupled plasma optical emission spectroscopy and X-ray fluorescence.
Bond strain appears to significantly increase the tendency to dissolve
under hydrothermal conditions. The stabilizing influences of increased
connectivity and hydrophobicity were found to be weak.