A new structural model of shear-thickening ''dilatancy'' is proposed f
or (strongly) stabilized disperse systems. This model is based on the
effective volume fraction (EVF) concept, developed in Part I of this s
eries and previously used for the rheological modeling of complex flui
ds. In such a description, the latter are considered as concentrated d
ispersions of basic structural units (SUs) - either small? compact clu
sters or primary particles -, forming large structures at low shear. A
s shear rate increases, rupturing of these large structures leads to t
he shear thinning observed prior to dilatancy. The novelty of this mod
el lies in assuming that, beyond the onset of dilatancy, hydrodynamic
forces promote, at the expense of basic-SUs; the formation of hydrodyn
amic clusters as both rheo-optical experiments and numerical simulatio
ns recently demonstrated, in contradiction with the (classical) theory
based on a shear induced disruption of particle layering. Dilatancy d
irectly results from the increase of the EVF of the dispersion, closel
y related to the increasing volume of continuous phase imprisoned insi
de hydroclusters whose size grows as the shear rate: increases. Predic
tions of the model are discussed in comparison with the main features
observed in a large number of dilatant dispersions: especially the vol
ume fraction dependences of viscosity and critical shear rates (onset
of dilatancy, maximum and discontinuity in viscosity) also the effects
of particle size, polydispersity and suspending fluid viscosity.