Sediment transport modelling in combined sewer

1996 ◽  
Vol 33 (9) ◽  
pp. 61-67 ◽  
Author(s):  
Lin Huseng ◽  
Benoit Le Guennec

The classical solid transport theory has been used to analyse the experimental results obtained from the No. 13 combined sewer trunk of Marseille for more than two years. This study demonstrates that the sediment transport phenomena in a combined sewer trunk are nothing other than the classical ones. A numerical model has been established according to the analyses. Based on a permanent flow regime, this model considers not only the effects of the real channel geometry, non-uniform particles size, but also the coexistence of mineral and organically materials. Some particular sediment transport phenomena such as the armouring of bed have also been taken into account. It also shows that although the influence of the suspension particles is not necessarily considered, the simulation including the variations of particle density with each granular fraction may be improved.

Fluids ◽  
2022 ◽  
Vol 7 (1) ◽  
pp. 23
Author(s):  
Joseph T. Wallwork ◽  
Jaan H. Pu ◽  
Snehasis Kundu ◽  
Prashanth R. Hanmaiahgari ◽  
Manish Pandey ◽  
...  

This paper reviews existing studies relating to the assessment of sediment concentration profiles within various flow conditions due to their importance in representing pollutant propagation. The effects of sediment particle size, flow depth, and velocity were considered, as well as the eddy viscosity and Rouse number influence on the drag of the particle. It is also widely considered that there is a minimum threshold velocity required to increase sediment concentration within a flow above the washload. The bursting effect has also been investigated within this review, in which it presents the mechanism for sediment to be entrained within the flow at low average velocities. A review of the existing state-of-the-art literature has shown there are many variables to consider, i.e., particle density, flow velocity, and turbulence, when assessing the suspended sediment characteristics within flow; this outcome further evidences the complexity of suspended sediment transport modelling.


2011 ◽  
Vol 60 (1) ◽  
pp. 191-213 ◽  
Author(s):  
Alessio Radice ◽  
Elisa Giorgetti ◽  
Davide Brambilla ◽  
Laura Longoni ◽  
Monica Papini

2010 ◽  
Vol 388 (3-4) ◽  
pp. 399-413 ◽  
Author(s):  
Jonathan L. Carrivick ◽  
Vern Manville ◽  
Alison Graettinger ◽  
Shane J. Cronin

2016 ◽  
Vol 154 ◽  
pp. 536-543 ◽  
Author(s):  
Elodie Zavattero ◽  
Mingxuan Du ◽  
Qiang Ma ◽  
Olivier Delestre ◽  
Philippe Gourbesville

2021 ◽  
pp. 103-117
Author(s):  
Davor Kvočka

Sediment transport can have a negative impact on riparian environments, as it can lead to the deterioration of ecological diversity and increase flood risks. Sediment transport modelling is thus a key tool in river basin management and the development of river training structures. In this study, we examined the appropriateness of 1D modelling for total sediment transport loads using the Engelund–Hansen and Ackers–White transport equations for the Lower Danube River. The study evaluated the effect of sediment grading on the accuracy of 1D model results, the appropriateness of 1D sediment transport modelling within technical or engineering projects, and the appropriateness of the Engelund–Hansen and Ackers–White equations for estimating sediment yield in the area of the Lower Danube River. The model results have been compared to field measurements, with the accuracy of the modelling results being evaluated with statistical tests. The obtained results show: (i) the sediment grading does not have a significant impact on the 1D modelling results, (ii) 1D sediment transport modelling gives sufficiently accurate results for practical engineering use (e.g. the estimation of dredging activities), and (iii) the Engelund–Hansen equation is generally better for sediment transport modelling in the Lower Danube River.


2013 ◽  
Vol 47 ◽  
pp. 193-206 ◽  
Author(s):  
Narayan Kumar Shrestha ◽  
Olkeba Tolessa Leta ◽  
Bruno De Fraine ◽  
Ann van Griensven ◽  
Willy Bauwens

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