An experimental study was carried out to investigate the resuspension
(fluidization) of a loosely held monodispersed particle bed by a momen
tum jet, discharging from below. The work was motivated by its applica
tions to limnological situations where the bottom sediments are suspen
ded by a series of jets fed by a ground-water karstic system. Two diff
erent flow regimes were identified, and the conditions under which the
y occur were mapped on a regime diagram between the two important nond
imensional variables, h(o)/d(p) and h(o)/ (M(o)(1/2)/w(s)), where h(o)
is the height of the particle layer; w(s) is the particle-settling ve
locity; and M(o) is the momentum flux of the jet. The maximum height o
f rise of particles within the jet was also determined as a function o
f these nondimensional variables. Comparisons of laboratory and field
observational results were also made.