We have used small-angle X-ray scattering (SAXS) and oscillatory shear rheo
metry to study the salt-induced flocculation of a concentrated colloidal si
lica dispersion in water. The SAXS results provided qualitative confirmatio
n of a primary contact coordination shell and barrier as predicted by the D
LVO model. The results are consistent with an irreversible, but volume-cons
erving, growth of a network of interparticle contacts. The activation energ
y for network growth turns out to be substantially greater than the barrier
in the pair potential predicted by the DLVO model, and this difference is
ascribed to the importance of multiparticle interactions. The storage modul
us of the gel (reflecting the long-range structure) continued to evolve lon
g after changes in the local structure could no longer be distinguished, bu
t ultimately it also converged to a quasi-stationary state. Disruption of t
he gel network by shear had no detectable effect on the local structure, bu
t caused a dramatic reduction in the moduli which subsequently recovered fo
llowing different kinetics than in the initial growth process.