Vibrational spectroscopy is a powerful tool for determining
the
local hydrogen-bonding environment. However, vibrational coupling
present in H2O makes it difficult to relate vibrational
spectra to a molecular description of the system. While numerous bulk
studies have shed light on this phenomenon, the influence of both
intra- and intermolecular vibrational coupling on the resulting electrical
double layer spectra at buried interfaces remains largely unexplored.
By utilizing vibrational sum frequency generation (vSFG), electrokinetic
measurements, and the maximum entropy method on isotopically diluted
water (HOD) at the silica/aqueous interface, we reveal the influence
of vibrational coupling on the Stern and diffuse layer spectra as
the pH is varied. For the Stern layer spectra, we observe differences
in the frequency centers at pH 2 that are less significant at higher
pH, signifying the presence of intermolecular coupling that can be
related to the double-donor hydrogen-bonded structure of water. Furthermore,
the differences in the evolution of the Stern layer of H2O and HOD suggest that the presence of intramolecular coupling in
the former may distort the spectral response. Moreover, we observe
that the evolution of HOD closely matches the pK
a of the out-of-plane silanols predicted by previous molecular
dynamic simulations.