A systematic approach to explore the effects of dynamic interaction of
liquid and solid phases on sediment-laden turbulent open channel flow
s is proposed. The investigation is carried out based on systematic an
alysis of basic momentum and continuity equations. The effect of suspe
nded sediment on the turbulent flow is taken as a perturbation to equi
valent turbulent dear water how of the same water depth. A perturbatio
n analysis is then developed, in an attempt to quantitatively describe
the physical process of the interaction between the turbulent flow an
d the suspended sediment. As a result, a generalized suspended sedimen
t concentration distribution is derived directly from the momentum equ
ation; After conducting an analysis of the generation of the induced R
eynolds stress, the mean velocity profile of the perturbed flow is als
o obtained. The derived concentration and mean velocity distributions
agree well with experimental data. The present analysis improves our u
nderstanding of the coupling mechanism, develops a framework, and offe
rs new analytical results for further study.