Results from recent experimental investigations into the fluidization, size
-segregation and stress-transmission behaviour of model granular materials
are described. Digital high-speed photography and particle-tracking softwar
e are used to study the vibro-fluidization of a two-dimensional powder. The
dependence of granular temperature on vibration frequency, amplitude and n
umber of grains is compared with simulations and a simple analytical model.
Particle tracking at low base accelerations has also shown that a single l
arge intruder in a two-dimensional bed of monodisperse particles moves upwa
rds at the same speed as the smaller grains over a wide range of accelerati
ons, suggesting that convection is the key to size segregation under these
conditions. Force profiles have been measured under conical sandpiles by us
ing a simple elasto-optical technique, which provides a spatial resolution
comparable to the grain diameter. The results confirm the existence of coun
ter-intuitive pressure dips at the centre of the pile. Simple two-dimension
al models for force transmission in granular materials are reviewed; these
are extended to three dimensions and to lattices with perturbations induced
by deformation of the grains or by polydispersity.