Using vertical vibrations, we have induced convection in a granular system
completely immersed in fluid inside a cylindrical container. Convection is
established in a single convection roll, which carries the material upward
in the center and downward along the side walls of the container. We measur
e the rise times of tracer particles embedded in the medium at various dept
hs along the central axis of the system. By fitting this data to an appropr
iate functional form, we obtain information on the depth dependence of conv
ection velocity. Significant differences are found in the frequency and acc
eleration amplitude dependence of convection between wet and otherwise iden
tical dry systems. In addition, we find that a power-law form provides a be
tter fit to our data than the logarithmic form used in dry systems.