Previous studies characterising horseshoe vortices upstream of circular cylinders in open channels have focused on changes in the Reynolds number. This study investigates the effect of the Froude number and other flow and geometrical parameters on the nature of the horseshoe vortex system that develops in front of a circular cylinder. The results show horseshoe vortex dynamics dominated by cylinder diameter, Froude number and flow depth. Instantaneous vorticity fields were classified into either two or three groups of vortex formations based on their turbulence stress magnitudes with a high dependence shown upon the Froude number and cylinder diameter. The peak stress properties of theudhorseshoe vortex system was found to be controlled within a certain threshold of Froude numbers (Fr ≤ 0.3 and Fr ≥ 1.7). It was also found that a single point under the horseshoe vortex can represent the vortices better than the whole field that encompasses the wholeudsystem. The characteristics of the horseshoe vortex formed upstream of a wall-mounted circular cylinder in an open channel were studied using two dimensional Particle Image Velocimetry. Experiments were conducted for different flow conditions and focused on Froude numbers, cylinder diameters, flow depths and bulk flow velocities. Two groups of experiments were conducted. The rest consisted of twenty five experiments with audwide range of Froude numbers, including sub-critical, critical and super-critical flow conditions.udThis group was analysed as a whole and then the lower sub-critical experiments followed by the upper sub-critical to super-critical experiments. Another set of nine sub-critical experiments were conducted focusing on the experimental design to segregate flow and geometrical parameters. Quadrant analysis was used to analyse the contribution of near-bed turbulent stresses in the region upstream of the cylinder. Applying multivariateudstatistical techniques, the relationship between geometrical parameters, flow conditions and the changes in the location and magnitude of the turbulent stresses under the horseshoe vortex were examined.udThis study, introduces the Froude number as a new governing parameter of the horseshoe vortex system, which can be important for fluvial systems with change of hydraulics regimes as mountainous rivers.
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