Based on an analysis of hydrodynamic inter-particle interactions, a mo
del describing particle clusters in two-phase, turbulent, gas-solid fl
ow through vertical pipes is presented. The initial stage in the evolu
tion of a cluster is the formation of a hydrodynamical aggregate of a
small number of particles. This aggregate will then grow due to sedime
ntation aggregation. The growth law of clusters, i.e. the cluster size
and velocity as functions of its age, is found using a 'mean field th
eory' approach. It is shown that clusters have large relative Reynolds
numbers which leads to the formation of turbulent wakes behind them.
Due to the complex turbulent flow structures, partially induced by the
wakes of all clusters, the horizontal motion of a specific cluster ca
n be considered to be a random walk. This horizontal motion eventually
drives the cluster to the wall. The final stage is the destruction of
the cluster due to a collision with the wall or with a high speed par
ticle. It is shown that the former dominates the latter. Using this th
eory the cluster size distribution function and the mean cluster size
are calculated. Theoretical predictions are compared to available expe
rimental data and good agreement is found. Furthermore an expression i
s derived for the effective radial solid flux in terms of the intensit
y with which small hydrodynamical aggregates are formed. This then pro
vides an explicit microscopic mechanism for the formation of a core-an
nulus structure in gas-solid flow through vertical pipes.