Bed-Load Transport Flume Experiments on Steep Slopes

2008 ◽  
Vol 134 (9) ◽  
pp. 1302-1310 ◽  
Author(s):  
A. Recking ◽  
P. Frey ◽  
A. Paquier ◽  
P. Belleudy ◽  
J. Y. Champagne
2009 ◽  
Vol 36 (11) ◽  
pp. 1755-1763 ◽  
Author(s):  
Burkhard Rosier ◽  
Jean-Louis Boillat ◽  
Anton J. Schleiss

Side weirs are free overflow regulation and diversion structures commonly encountered in flood protection engineering. The lateral loss of water reduces the bed-load transport capacity in the main channel, leading to local sediment deposition near the side overflow. As a consequence, the design overflow is increased in an uncontrolled way. Since this flow–sediment interaction in such a channel has not been studied so far, systematic flume experiments have been performed. Based on these experiments, a two-dimensional empirical model to describe the longitudinal evolution of the aggraded channel reach near the weir has been developed. In addition, a simple and straightforward approach for direct estimation of the side overflow in presence of bed-load transport has been established. To be generally applicable in engineering practice, all input variables are expressed in terms of dimensionless parameters. Finally, the application of the models is demonstrated in a case study on the Rhone River in Switzerland.


Author(s):  
Virginie Hergault ◽  
Philippe Frey ◽  
Francois Métivier ◽  
Christophe Ducottet ◽  
Tobias Böhm ◽  
...  

2017 ◽  
Vol 55 (4) ◽  
pp. 455-469 ◽  
Author(s):  
Carmelo Juez ◽  
Sandra Soares-Frazao ◽  
Javier Murillo ◽  
Pilar García-Navarro

2021 ◽  
Author(s):  
Eric Deal ◽  
Jeremy Venditti ◽  
Santiago Benavides ◽  
Ryan Bradley ◽  
Qiong Zhang ◽  
...  

Bed load sediment transport, in which wind or water flowing over a bed of sediment causes grains to roll or hop along the bed, is a critically important mechanism in contexts ranging from river restoration to planetary exploration. Despite its widespread occurrence, predictions of bed load sediment flux are notoriously imprecise. Many studies have focused on grain size variability as a source of uncertainty, but few have investigated the role of grain shape, even though shape has long been suspected to influence transport rates. Here we show that grain shape can modify bed load transport rates by an amount comparable to the scatter in many sediment transport data sets. We develop a theory that accounts for grain shape effects on fluid drag and granular friction and predicts that the onset and efficiency of bed load transport depend on the mean drag coefficient and bulk friction coefficient of the transported grains. Laboratory flume experiments using a variety of grain shapes confirm these predictions. We propose a shape-independent sediment transport law that collapses our experimental measurements onto a single trend, allowing for more accurate predictions of sediment transport and helping reconcile theory developed for spherical particle transport with the behavior of natural sediment grains.


2010 ◽  
Vol 13 (3) ◽  
pp. 78-87
Author(s):  
Hoai Cong Huynh

The numerical model is developed consisting of a 1D flow model and the morphological model to simulate the erosion due to the water overtopping. The step method is applied to solve the water surface on the slope and the finite difference method of the modified Lax Scheme is applied for bed change equation. The Meyer-Peter and Muller formulae is used to determine the bed load transport rate. The model is calibrated and verified based on the data in experiment. It is found that the computed results and experiment data are good agreement.


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