The hydrodynamic response of turbulent flow in a compound wide rectang
ular open channel with a vegetated domain at the channel bank, in a ch
annel corner and in a floodplain, to the vegetation density and diamet
er is discussed. To this end a phenomenological model was imbedded in
an algebraic stress model with the vegetation modeled as an internal r
esistance that exerts drag force, produces energy of turbulence, and i
nterferes with its anisotropy and length scale. Simple suggestions for
some modeling problems associated with the presence of wide vegetated
domains are used to yield the three-dimensional flow. Vorticity sourc
es relaxation was implemented to smooth periodic behavior, and dissipa
tion correction was introduced as a coordinate-invariant damping. With
these, the results represent fully developed flow.