Effect of the sediment discharge on the equilibrium bed morphology of movable bed open-channel confluences

Geomorphology ◽  
2020 ◽  
Vol 367 ◽  
pp. 107329
Author(s):  
G. Bombar ◽  
A.H. Cardoso
2007 ◽  
Vol 51 ◽  
pp. 823-828
Author(s):  
Takashi DEGUCHI ◽  
Ichiro FUJITA ◽  
Ryota TSUBAKI ◽  
Masashi OZONO

2018 ◽  
Vol 40 ◽  
pp. 02017
Author(s):  
Hela Romdhane ◽  
Amel Soualmia ◽  
Ludovic Cassan ◽  
Gilles Belaud

Vegetation is a common feature in natural coastal and riverine waters, interacting with both water flow and sediment transport. However, the physical processes governing these interactions are still poorly understood, which makes it difficult to predict sediment transport and associated morphodynamics in a vegetated environment. In this context, an experimental study was conducted in laboratory with a movable bed trapped in artificial vegetation. The experimental flume is a rectangular open channel 5.75 m long and 0.29 m wide. For flow measurements, the channel is equipped with a fast camera and ADV probe. This work focuses on identifying the vegetation effects on flows and sediment transport. In fact, it was shown that the vegetation presence in a watercourse promotes deposition and sediment accumulation. This is explained by a reduction of the bed shear stress, since the friction occurs mainly by the drag force effect exerted by the vegetation. It was shown too that the vegetation reduced the bedload transport. Thanks to the partitioning of shear stress, it was possible to predict the bedload transport using standard formulas with a reasonable accuracy.


1998 ◽  
Vol 42 ◽  
pp. 1069-1074
Author(s):  
Muneo HIRANO ◽  
Haruyuki HASHIMOTO ◽  
Hiroaki TAGAWA

1987 ◽  
Vol 25 (1) ◽  
pp. 89-102 ◽  
Author(s):  
C. Fouladi Nashta ◽  
R. J. Garde ◽  
P. K. Swa Mee

1994 ◽  
Vol 21 (3) ◽  
pp. 490-498
Author(s):  
A. Sadok ◽  
C. Marche

Several computational methods of sediment discharge in open channel flows are reported in the existing literature. However, sediment transport is a complex procedure that implies several parameters which in some cases are difficult to estimate. Even if direct confrontations of methods used are published, it is difficult to draw significant conclusions that would help determine a model or the models likely to produce the best results for a specific case. To facilitate that choice, the authors have attempted to establish a classification of the various methods commonly used by determining their relative performance, and to improve the performance by proposing a new model which distinguishes the type of sediment transport and the nature of the bed. Key words: sediment discharge, sediment transport, open channel flow, model, performance.[Journal translation]


2003 ◽  
Vol 47 ◽  
pp. 571-576
Author(s):  
Haruyuki HASHIMOTO ◽  
Kichan PARK ◽  
Shinya IKEMATSU ◽  
Nobutada TASAKI

Water ◽  
2021 ◽  
Vol 13 (6) ◽  
pp. 828
Author(s):  
Joana Baltazar ◽  
Elsa Alves ◽  
Gökçen Bombar ◽  
António Heleno Cardoso

This laboratory study focused on the effect of a submerged vane-field on the flow pattern and bed morphology near and inside the entrance reach of a movable bed 90° lateral diversion. The system was modelled under live bed conditions for a water discharge ratio of ≈0.2. Two experiments were run until bed equilibrium was reached: with and without a vane-field installed close to the diversion entrance to control the transfer of sediments into the diversion channel. The equilibrium bed morphology and the associated 3D flow field were measured in great detail. The bed load diverted into the diversion was reduced by approximately one quarter due to the action of the vane-field. The vanes prevented the formation of the diversion vortex in the main channel, upstream of the diversion’s entrance, thus contributing to that decrease. They also created a main channel vortex that started at the most upstream vanes and further decreased the amount of bed load entering the diversion. The flow separation zone inside the diversion was larger with vanes, but conveyance was balanced through a slightly deeper scour trench therein. The flow structures described were confirmed through the measurements of the turbulent kinetic energy.


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