The
temperature dependence of the structure of water confined in
hydrophilic mesostructured porous silica (MCM-41) and hydrophobic
benzene-bridged periodic mesoporous organosilicas (PMOs) is studied
by Raman vibrational spectroscopy. For capillary filled pores (75%
relative humidity, RH), the OH stretching region is dominated by the
contribution from liquid water situated in the core part of the pore.
It adopts a bulklike structure that is modestly disrupted by confinement
and surface hydrophobicity. For partially filled pores (33% RH), the
structure of the nonfreezable adsorbed film radically differs from
that found in capillary filled pores. A first remarkable feature is
the absence of the Raman spectral fingerprint of low-density amorphous
ice, even at a low temperature (−120 °C). Second, additional
bands reveal water hydroxyl groups pointing toward the different water/solid
and water/vapor interfaces. For MCM-41, they correspond to water molecules
acting as weak H-bond donors with silica and dangling hydroxyl groups
oriented toward the empty center of the pore. For benzene-bridged
PMO, we found an additional type of dangling hydroxyl groups, which
we attribute to water at the hydrophobic solid interface.