Long-time self-diffusion and sedimentation of tracer spheres in dispersions
of rigid colloidal host rods has been measured in situ as a function of ro
d volume fraction for various sphere and rod dimensions. The sphere frictio
n factor, which was always the same for diffusion and sedimentation, is det
ermined only by the macroscopic rod viscosity when the rods are relatively
mobile (dilute regime). However, when the host-rod dynamics is slow (Semi-d
ilute regime) the tracer friction is much smaller than expected from the ho
st viscosity, and markedly dependent on the sphere/rod size ratio. These ex
periments on well defined rod-sphere mixtures, supported by low-shear rheol
ogy and birefringence measurements,confirm that current models for hindered
tracer dynamics do not (adequately) incorporate host mobility.