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Journal ArticleDOI

Methods to control bed erosion at 90° river confluence: an experimental study

TLDR
In this article, vanes and circular piles are proposed as scour mitigation measures in a distorted mobile bed model with 90° confluence angle and three discharge ratios (Qr = 0.33, 0.50 and 0.75) are used.
Abstract
Confluence is a common occurrence in rivers. The convergence of flows often leads to erosion of the river bed and formation of a deep scour-hole at the confluence. In the present experimental study, vanes and circular piles are proposed as scour mitigation measures. Experiments are performed in a distorted mobile bed model (d50 = 0.28 mm) with 90° confluence angle. Three different discharge ratios (Qr = ratio of lateral to main flow discharge) of 0.33, 0.50 and 0.75 are used. Vanes (1.5 cm width and 1 mm thick) or piles (ɸ = 8 mm and 12 mm) are arranged in a row perpendicular to the lateral flow at a spacing of 5, 10 or 15 cm. Three vane angles of 15°, 30° and 60° with respect to the main flow are used. The experimental results show that scour depth (Sd) increases with an increase of Qr. Sd reduces by 33%, 50% and 47% with vanes for Qr = 0.33, 0.50 and 0.75, respectively. Sd reduces by 43%, 55% and 55% with 12 mm piles and by 70%, 60% and 59% with 8 mm piles, for the corresponding discharge ratios...

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Citations
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Journal ArticleDOI

Assessment of Vanes Effectiveness in Controlling Erosion and Deposition Zones at a River Confluence using a 2D model

TL;DR: In this paper, a two-dimensional (2D) numerical model was used to simulate the confluence between Kurau and Ara rivers, Perak, Malaysia, to investigate the effectiveness of different shapes and sizes of 30o obstacles/vanes in controlling erosion and deposition zones.
Journal ArticleDOI

Effect of side slope of main channels on formation and penetration of scour hole in confluences

TL;DR: In this paper, the effect of channel geometry on the flow dynamics at the confluence of the main and tributary channels was investigated under clear-water condition for the main channel, and the mean penetration rate of scour hole to all directions for different side slope angles was obtained.
Journal ArticleDOI

Experimental investigation of flow pattern over a fully developed bed at a 60° river confluence in large floods

TL;DR: In this article , the authors measured the 3D velocity at specific points at the confluence to understand the flow pattern corresponding to the river bed behavior in the case of large floods.
Journal ArticleDOI

Scour depth in confluences considering tributary flow, bank slope, and post-confluence conditions

TL;DR: In this paper, the effects of bank slope angle (θ) of the main channel, discharge ratio (Qr) of tributary channel and densimetric Froude number (Frg3) of post-confluence channel were experimentally studied.
References
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Journal ArticleDOI

Sediment transport; Part I, Bed load transport

TL;DR: In this article, a method is presented which enables the computation of the bed-load transport as the product of the saltation height, the particle velocity and the bed load concentration.
Journal ArticleDOI

Bed material transport and the morphology of alluvial river channels

TL;DR: In this article, the authors studied the relationship between sediment transport and river morphology by defining sediment transport regimes on the basis of the Shields number, a non-dimensional measure of the capacity of the channel to move sediment of a given caliber.
Journal ArticleDOI

Design method for local scour at bridge piers

TL;DR: In this paper, a design method for the estimation of equilibrium depths of local scour at bridge piers is presented, based upon envelope curves drawn to experimental data derived mostly from laboratory experiments.
Journal ArticleDOI

Sediment transport and bed morphology at river channel confluences

TL;DR: In this paper, the authors present results of a quantitative investigation of sediment transport at channel confluences accomplished through both scaled laboratory flume simulation and complementary monitoring of a natural channel confluence, showing that sediment contributions from the confluent channels are progressively segregated in their paths through the junction, with sediment being transported around rather than through the centre of the confluence.
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