An anisotropic Lagrangian approach is used to investigate the influence of
a mean fluid velocity gradient on the motion and on the dispersion of heavy
particles suspended in a stationary homogeneous turbulent gas flow. The pr
oblem of consistency of the correlation matrices used in first-order stocha
stic processes is put forward. The accuracy of the method is first checked
by comparing the numerical predictions with available experimental results
in uniform flow. A second validation test is carried out by comparison with
dispersion measurements in a horizontal shear flow. Numerical predictions
are then provided in the case of a vertical upward turbulent shear flow, th
e gravity force held implying a nonzero mean drift velocity between fluid a
nd particles. The transverse particle dispersion is found to be slightly re
duced by the presence of a uniform shear, The streamwise particle turbulent
intensity is enhanced above the level predicted without shear, whereas, in
the direction normal to the flow, the fluctuating velocity of particles ar
e found to be unaffected by the presence of shear, The effect of the lift f
orce due to the mean shear is found to be negligible, except for the mean t
ransverse deviation, which is found however not to be caused only by the li
ft. The presented numerical results, which confirm and extend the theoretic
al analysis of others, may explain some experimental observations reported
in the literature, (C) 2000 Elsevier Science Ltd. All rights reserved.