The porous boundary of alluvial channels allows water to interact with the surrounding
groundwater. With reduction in groundwater level, transfer of water from the main channel to …

This research aims to investigate the near-bed turbulent flow characteristics in a meandering
channel with both mobile bed and immobile bed conditions. Experiments were performed in …

Sinuous channel flows are the most natural form of alluvial streams. The complex flow in the
channel bends has been the main focus of the study. This paper examines the flow velocity …

The study estimates the turbulence anisotropy for flow in a sinuous channel under the
influence of downward seepage. Anisotropy provides the deviation from the isotropic …