We analyze a one-equation model for the turbulent kinetic energy of an
open channel flow in the presence of suspension sediment. Engelund's
pioneer analysis and his criterion for the threshold conditions for th
e initiation of suspension are revisited, and it is concluded that suc
h criterion does not represent any physical response of the system und
er consideration, but rather appears to be an artifact of the mathemat
ical manipulations of the turbulent energy equation. The present analy
sis indicates that the effect of the suspended sediment on the turbule
nt kinetic energy near the bed is to reduce such energy when the parti
cle size is sufficiently small, and that the reduction increases with
the sediment concentration and the particle settling velocity to flow
shear velocity ratio. On the other hand, suspended particles of larger
size can enhance the turbulence of the flow because of the production
of turbulent kinetic energy through vortex shedding mechanisms. A cri
terion is proposed to estimate the conditions for which turbulent enha
ncement due to the presence of suspended sediment occurs.