Quartz crystal microbalance
with dissipation (QCM-D) monitoring
is used to investigate the adsorption processes at liquid–solid
interfaces and applied increasingly to characterize viscoelastic properties
of complex liquids. Here, we contribute new insights into the latter
field by using QCM-D to investigate the structure near the interface
and the high-frequency viscoelastic properties of charge-stabilized
polystyrene particles (radius 37 nm) dispersed in water. The study
reveals changes with increasing ionic strength and particle concentration.
Replacing water with a dispersion is usually expected to give rise
to a decrease in frequency, f. Increases in both f and dissipation, D, were observed on
exchanging pure water for particle dispersions at a low ionic strength.
The QCM-D data are well-represented by a viscoelastic model, with
viscosity increasing from 1.0 to 1.3 mPa s as the particle volume
fraction changes from 0.005 to 0.07. This increase, higher than that
predicted for noninteracting dispersions, can be explained by the
charge repulsion between the particles giving rise to a higher effective
volume fraction. It is concluded that the polystyrene particles did
not adhere to the solid surface but rather were separated by a layer
of pure dispersion medium. The QCM-D response was successfully represented
using a viscoelastic Kelvin–Voigt model, from which it was
concluded that the thickness of the dispersion medium layer was of
the order of the particle–particle bulk separation, in the
range of 50–250 nm, and observed to decrease with both particle
concentration and addition of salt. Similar anomalous frequency and
dissipation responses have been seen previously for systems containing
weakly adherent colloidal particles and bacteria and understood in
terms of coupled resonators. We demonstrate that surface attachment
is not required for such phenomena to occur, but that a viscoelastic
liquid separated from the oscillating surface by a thin Newtonian
layer gives rise to similar responses.