How polyelectrolyte adsorption depends on history: A combined Fourier transform infrared spectroscopy in attenuated total reflection and surface forces study
Sa. Sukhishvili et al., How polyelectrolyte adsorption depends on history: A combined Fourier transform infrared spectroscopy in attenuated total reflection and surface forces study, LANGMUIR, 15(24), 1999, pp. 8474-8482
We present a systematic study of how adsorption history affects the thickne
ss, surface forces, and interfacial rheology of a model cationic polymer. T
he polymer was quaternized poly-4-vinylpyridine, QPVP (weight-average degre
e of polymerization n(w) = 325 and 98% quaternized with ethyl bromide). The
main comparisons concerned one-step adsorption from solution at a variable
salt concentration up to 0.5 M NaCl, versus two-step adsorption (initial a
dsorption from buffer solution without added salt, then NaCl added later).
The aqueous solutions were buffered at pH = 9.2 such that the surfaces (mic
a in the case of surfaces forces (SFA) experiments, oxidized silicon in the
case of in situ infrared (FTIR-ATR) experiments) in each case carried a la
rge negative charge. The SFA and FTIR-ATR experiments gave consistent estim
ates of the amount of polymer adsorbed, confirming the expectation that ads
orption should be driven by electrostatic attraction to the surface of larg
e opposite charge. The adsorbed amount showed little dependence on path, va
lidating the common assumption of equilibration in this respect. However th
e layer thickness measured by surface forces, the shear nanorheology respon
se at a given surface force, and the dichroism of pendant side groups of th
e polymer all showed a pronounced dependence on the path to reach the adsor
bed state. We interpret the measurements to suggest that two-step adsorptio
n produces an inhomogeneous layer comprised of a dense layer of segments cl
osest to the solid surface and a sparse outer layer. In particular, two-ste
p adsorption produced thicker layers and a greater tendency to decouple she
ar forces from those that resist compression in the normal direction, there
by lessening the shear forces at a given level of normal force.