Affiliations: Department of Civil & Global Environment
Engineering, Kyoto University, Yoshidahonmachi, Sakyo-ku, Kyoto 606- 8501,
Japan.
Abstract: PIV measurements in side-cavity open-channel flows that simulate
"Wando" in rivers, were conducted in a laboratory flume. Five types of side
cavities were built by using a transparent plate at the wando flow. The pattern
of the instantaneous flow fields was quite different from that of time-averaged
ones. It was found that a vortex, which is located in the side cavity, is
stable when the junction mouth between the side-cavity and main channel is
narrow. In contrast, large-scale unstable vortices are generated
semi-periodically when the junction mouth is wide. The free-surface
fluctuations in and outside the wando were also measured by three sets of
supersonic wave gauges. The amplitude of the water-surface fluctuations is
large when the junction mouth is wide as compared with when its mouth is
narrow. When the elevation of the free surface in the side-cavity is rising,
its elevation in the main channel is falling, and vice versa when the junction
mouth is wide.