We have employed amplitude- and phase-resolved second-harmonic
generation spectroscopy to investigate ion-specific effects of monovalent
cations at the fused silica:water interface maintained under acidic,
neutral, and alkaline conditions. We find a negligible dependence
of the total potential (as negative as −400 mV at pH 14), the
second-order nonlinear susceptibility (as large as 1.5 × 10–21 m2 V–1 at pH 14), the
number of Stern layer water molecules (1 × 1015 cm–2 at pH 5.8), and the energy associated with water
alignment upon going from neutral to high pH (ca.
−24 kJ mol–1 to −48 kJ mol–1 at pH 13 and 14, close to the cohesive energy of liquid water but
smaller than that of ice) on chlorides of the alkali series (M+ = Li+, Na+, K+, Rb+, and Cs+). Attempts are presented to provide estimates
for the molecular hyperpolarizability of the cations and anions in
the Stern layer at high pH, which arrive at ca. 20-fold
larger values for α
total ions
(2) = α
M
+
(2) + α
OH
–
(2) + α
Cl
–
(2) when compared to water’s molecular hyperpolarizability
estimate from theory and point to a sizable contribution of deprotonated
silanol groups at high pH. In contrast to the alkali series, a pronounced
dependence of the total potential and the second-order nonlinear susceptibility
on monovalent cationic (cetrimonium bromide, CTAB) and anionic (perfluorooctanoic
and perfluorooctanesulfonic acid, PFOA and PFOS) surfactants
was quantifiable. Our findings are consistent with a low surface coverage
of the alkali cations and a high surface coverage of the surfactants.
Moreover, they underscore the important contribution of Stern layer
water molecules to the total potential and second-order nonlinear
susceptibility. Finally, they demonstrate the applicability of heterodyne-detected
second-harmonic generation spectroscopy for identifying perfluorinated
acids at mineral:water interfaces.