Side weirs, also known as lateral weirs, and
overflow dams are free overflow regulation and diversion devices commonly
encountered in hydraulic engineering. The lateral loss of water is reducing the
sediment transport capacity in the main-channel and the formation of a local
sediment deposit in the downstream of weir. The head over the side weir rises
and the side overflow discharge as well. The design discharge to be diverted
over the weir is increased by this flow-sediment transport interaction. Although
there were no studies that scrutinized the scouring depth and geometry that
occurs around the labyrinth side weirs in channels with movable bed, there are
limited number of studies that examined the scouring geometry around the
classical side weir. In the present study, local scour depths formed in the
periphery of triangular labyrinth side weir mounted in a live-bed rectangular
cross-section straight channel were experimentally investigated under steady
state flow and free overflow from the side weir conditions. To provide for
live-bed conditions, the sediment was added to bed material in the experiments.
A series of experiments were conducted for live-bed scouring conditions (for
flow intensity greater than one) to determine the maximum scour depths that occur
around the triangular labyrinth side weir with different flow depths, different
main channel discharges, different volumetric amounts of sediment feed,
different crest heights, different Froude numbers, different flow intensities
and using uniform bed material. In the experiments, the dimensions of the
scours and sediment deposits that occur upstream and downstream of the weir
exhibited a periodic change (increase and decrease). The maximum depth of scour
occurred at the downstream end of the triangular labyrinth side weir
frequently.
Triangular labyrinth side weir Flow intensity Local scour Live-bed scour Sediment transport
Primary Language | English |
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Subjects | Engineering |
Journal Section | TJST |
Authors | |
Publication Date | March 1, 2018 |
Submission Date | January 27, 2017 |
Published in Issue | Year 2018 Volume: 13 Issue: 1 |