The rheological behavior of concentrated nearly monodisperse, nearly spheri
cal silica, and narrow particle size distribution alumina suspensions was m
easured in Couette geometry. Attractive forces between the particles (suspe
nsions flocculated at or near the isoelectric point) produce high viscositi
es. Repulsive forces between the particles produce dispersed suspensions an
d decrease the viscosity at low and intermediate shear rates. The viscosity
of the dispersed suspensions shear thickens (abruptly increases and approa
ches that of the flocculated suspensions) at a critical shear rate land the
refore stress) provided the volume fraction of solids of the suspension is
sufficiently high. As the pH is adjusted farther from the isoelectric point
the critical shear rate land stress) increase. At pH away from the isoelec
tric point the addition of salt decreases the critical shear rate land stre
ss). Thus shear thickening is not only dependent upon hydrodynamic interact
ions but also depends on surface forces, in particular repulsive interparti
cle forces. Increasing the magnitude and range of the repulsive forces incr
eases the shear stress land rate) at which shear thickening starts. Reducin
g the magnitude of the repulsive force allows the particles to be more easi
ly forced into clusters resulting in shear thickening. (C) 2000 The Society
of Rheology. [S0148-6055(00)01604-7].