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

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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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Transitional flow in channel junctions

NIHan-gen, +1 more
TL;DR: In this article, a simple one-dimensional formulation was proposed to predict the transitional flow at an open-channel junction, based on energy and continuity equations, and an empilical relation between the junction losses, the junction angle, and the discharge ratio was suggested which agrees well with the experimental results.
Journal ArticleDOI

Impact of confluence on hydrological and morphological characters of the trunk stream: a study on the Manu River of North-east India

TL;DR: In this article, a study was conducted at the point of convergence of the River Deo with the River Manu using simple geospatial technique and field work to justify the hydrological and morphological changes in downstream of the confluence point.
Journal ArticleDOI

Control of sediment inflow into a trapezoidal intake canal using submerged vanes

TL;DR: In this paper, experiments were conducted to control sediment entry into an intake channel using submerged vanes in a physical model with a rectangular mobile-bed main channel and a trapezoidal rigid-bed intake channel diverting at an angle of 45°.
Journal ArticleDOI

Review of Flow Hydrodynamics and Sediment Transport at Open Channel Confluences

TL;DR: A confluence is a place where two flows with different flow and sediment characteristics merge together as discussed by the authors, which is a common occurrence along the natural rivers as well as artificial open channels.
Journal ArticleDOI

Improving the Hydro-Morpho Dynamics of A River Confluence by Using Vanes

TL;DR: In this article, a 2D numerical model is used in simulating hydromorpho dynamics in the rivers confluence to mitigate the erosion and deposition zones by adopting vanes as control structures.
References
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Book

Earth Surface Processes, Landforms and Sediment Deposits

TL;DR: In this article, the authors present an overview of the Earth's surface and its geology, including the basic fluid flow, sediment transport, erosion and deposition of soft sediment, as well as a discussion of long-term, large-scale processes.
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Mixing-layer distortion at the confluence of channels of different depth

TL;DR: In this paper, the mixing layer that forms at their confluence is distorted by interacting with a separation zone which forms in the lee of the mouth of the shallower channel, which imparts a complex three-dimensional flow to the junction, promoting vertical fluid upwelling and significantly enhancing rapid mixing within the flow of the shallow tributary, while retarding the rate of mixing across the deeper channel.
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Sediment movement under unidirectional flows: an assessment of empirical threshold curves

TL;DR: A selection of threshold data sets from previous investigations is used to re-examine, selectively, some of the empirical curves that are most commonly used for the prediction of sediment threshold, implying that the formulae must be treated with caution in applications.
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Longitudinal changes in size and sorting of stream-bed material in four English rivers

TL;DR: In this article, the authors examined the downstream changes in mean grain size and sorting coefficient for four streams flowing in similar physiographic environments, and explained the periodic behavior of the sorting coefficient in terms of sediment inputs from tributary sources being superimposed on the over-all tendency for sorting and abrasion processes acting in the main stream to improve bed material sorting in the direction of transport.
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Dynamics of a river channel confluence with discordant beds: Flow turbulence, bed load sediment transport, and bed morphology

TL;DR: In this article, the authors measured near-bed flow turbulence, bed load transport rates, and changes in bed morphology for eight different flow conditions at a sand bed discordant confluence and found that low mean flow velocities are combined with the highest values of Reynolds shear stresses and that turbulence generation is associated with intense upward movements of flow.
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