The investigation of the motion of finite size particles with density diffe
rent from that of the fluid is relevant to the study of transport in geophy
sical flows. A two-dimensional model of an incompressible periodic flow is
used in order to assess the role of the different forces acting on the impu
rity. The classic results (stability of the vortex centre for impurities li
ghter than the fluid; unstable motion for denser impurities) are reviewed.
In the former case a typical convergence time scale towards the vortex cent
re is defined and studied as a function of the Stokes number St and the den
sity ratio gamma. In the range of parameters under consideration it is obse
rved that the Basset force acts as a (further) drag term modifying the conv
ergence time without altering the qualitative features of the particle traj
ectory. (C) 2001 Elsevier Science Ltd. All rights reserved.