Rapid granular flow is diffusive in character. This diffusive nature i
s important in the generation of constitutive properties such as effec
tive shear and bulk viscosities, effective conductivity of particle fl
uctuation energy, and self-diffusion coefficients. Experiments were pe
rformed in a large air-table apparatus that can sustain up to a few th
ousand small, light disks just above a horizontal porous plane. Experi
ments on 2D diffusion processes were performed using this apparatus. M
easurements of self-diffusion coefficients and granular temperature in
systems having different areal concentrations are in good agreement w
ith predictions based on the kinetic theory and on numerical simulatio
ns.