Over het archief
Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.
Dit archief wordt uitgebouwd en beheerd volgens de principes van de Open Access Movement, en het daaruit ontstane Open Archives Initiative.
Basisinformatie over ‘Open Access to scholarly information'.
Influence of aquatic plants on the flow resistance and the hydraulic capacity of vegetated rivers
De Doncker, L.; Troch, P.; Verhoeven, R.; Bal, K.; Meire, P. (2006). Influence of aquatic plants on the flow resistance and the hydraulic capacity of vegetated rivers, in: Alves, E.C.T.L. et al. (Ed.) River Flow 2006: Proceedings of the International Conference on Fluvial Hydraulics, Lisbon, Portugal, 6-8 September 2006. pp. 593-602. dx.doi.org/10.1201/9781439833865.ch61
In: Alves, E.C.T.L. et al. (Ed.) (2006). River Flow 2006: Proceedings of the International Conference on Fluvial Hydraulics, Lisbon, Portugal, 6-8 September 2006. Taylor & Francis: Lisbon. ISBN 978-0-415-40815-8. Two Volume Set pp., meer
|
| Beschikbaar in | Auteurs |
|
Documenttype: Congresbijdrage
|
| Abstract |
Vegetation growth drastically influences water levels and flow patterns in lowland rivers. Rise of the water level can have consequences for the surrounding areas and varying velocity patterns can influence the morphology of the river. The universities of Ghent and Antwerp are carrying out research in the river Aa, the Grote Kaliebeek and the Desselse Nete (Antwerp, Belgium) in order to better understand the natural phenomena involved and to come to a more accurate determination of the different parameters. Field measurements are carried out to collect data on discharge, stage and amount and variation of aquatic weed growth. The variation of the friction factor (Manning coefficient), influenced by the varying amount of vegetation, is determined as a function of time and distance. Following a seasonal cycle, flow resistance increases with plant growth in spring, reaches a maximum in early summer and then decreases slowly to the minimum in winter. Knowledge of the variation of the biomass in the time will lead to appropriate use of roughness coefficients in modelling surface flow in rivers. |
IMIS is ontwikkeld en wordt gehost door het VLIZ.
