Spatially uniform disperse system where the processes of coagulation, fragm
entation, and sedimentation of fractal aggregates occur simultaneously, was
discussed. Kinetics of the passage of such system from the initial state,
where the dispersed phase was already separated into fine and coarse fracti
ons, to a new equilibrium state was studied. The enlargement of aggregates
takes place both due to the capture of the particles of fine fraction and t
heir adherence during collisions. Disintegration of aggregates occurs by th
e detachment of fragments from the aggregate surface under the action of hy
drodynamic stresses arising during aggregate sedimentation. The solution of
the coagulation-fragmentation equations indicates that, at the intermediat
e stage of a process, the aggregate mass distribution density is characteri
zed by polymodal structure, which is degenerated into bimodal by the end of
the passage.