The flow structure and geomorphology of rivers are significantly affected by vegetation patterns. In the present study, the effect of vegetation in the form of discontinuous and vertically double layered patches particularly on the resulting flow turbulence was examined computationally in an open channel. Ak-ε model was implemented in this research work which was developed using 3-D numerical code FLUENT (ANSYS). After the validation process of numerical model, the impact of discontinuous layered vegetation patches on the flow turbulence was investigated against varying vegetation density and patch length. The mean stream-wise velocities at specified positions showed larger spatial fluctuations directly upstream and downstream of vegetation elements, whereas sharp inflections in the profiles were witnessed at the top of smaller submerged elements i.e.,z/hs=1 (wherez is the flow depth,hs is the smaller vegetation height). The reduction in flow velocity due to tall vegetation structure was more as compared with that of short vegetation. The mean velocity in the patch regions was visibly higher than that in the gap regions. The profiles of turbulent flow properties showed more rise and fall within the patches with a high vegetation density i.e.,Ss/d=4,St/d=8 (where Ss/d and St/d are the smaller and taller vegetation spacing, whiled is the vegetation diameter) as compared with low vegetation density i.e., Ss/d=8,St/d=16. The turbulent flow structure in the large patch and gap regions was found to be more stable than that in the small patches and gaps; whereas, due to the variation in distribution form of the patch, turbulence is relatively unaffected, and the flow structure variation is low. Turbulence was observed to be large, followed by a saw-tooth distribution within the patches; whereas, low turbulence is observed in the non-vegetation regions. The turbulent intensity acquired maximum of 13％ turbulence for dense vegetation arrangement as compared with that of sparse arrangement having maximum of 9％ turbulent intensity. A noteworthy rise in turbulent kinetic energy and turbulent intensity was witnessed as the flow passed through the vegetated regions. Hence, a non-uniform flow was observed through discontinuous and double layered vegetation patches.