VLIZ
VLAAMS INSTITUUT VOOR DE ZEE
MARIEN EN KUSTGEBONDEN ONDERZOEK & BELEID IN VLAANDEREN
   
© VLIZ © VLIZ © VLIZ © VLIZ © VLIZ
 
 
  English  Sitemap  Print
U bent hier: VLIZ > datacentrum
menu1 Over het VLIZ menu2 Infoloket menu3 Zeebibliotheek menu4 Cijfers&Beleid menu5 Faciliteiten menu6 Datacentrum
   
Datacentrum
  - IMIS: Integrated Marine Information System -
log in

Personen | Instituten | Publicaties | Projecten | Datasets | Kaarten
meld een fout in dit recordmandje (0): toevoegen | tonen Print-vriendelijke versie

Modelling sand resuspension by waves over a rippled bedPeer reviewed article
Trouw, K.; Williams, J.J.; Rose, C.P. (2000). Modelling sand resuspension by waves over a rippled bed Est., Coast. and Shelf Sci. 50(1): 143-151. dx.doi.org/10.1006/ecss.1999.0542
In: Estuarine, Coastal and Shelf Science. Academic Press/Elsevier: Amsterdam. ISSN 0272-7714, meer

Ook gepubliceerd als
  • Trouw, K.; Williams, J.J.; Rose, C.P. (2000). Modelling sand resuspension by waves over a rippled bed, in: (2000). VLIZ Coll. Rep. 30(2000). VLIZ Collected Reprints: Marine and Coastal Research in Flanders, 30: pp. chapter 42 [Subsequent publication], meer

Trefwoorden
    Beddingvorm; Gesuspendeerd particulair materiaal; Hydraulische modellen; Oceaanbodem; Resuspensie; Heropwoeling; Verticale profielen; Zand; Zandribbels; Marien
Author keywords
    sediment transport; ripples; waves; wave flume; sand concentrations; sediment cloud

Auteurs  Top 

Abstract
    With a two-dimensional Kappa-Epsilon-model and equations to describe sediment entrainment, diffusion, convection and settling, wave-induced flow velocities and sediment concentration fields over rippled beds have been calculated. Results from the simulations are compared with time-averaged vertical suspended sediment concentration profiles, C-profiles, measured in a large wave flume using the autonomous multi-sensor instrument STABLE. The simulations make it possible to examine in detail the mechanisms of sediment entrainment, vortex formation and advection. The resulting animations of model output allow a quasi-3-D visualization of sediment resuspension processes and aid quantification of the resulting vertical suspended sediment concentration field due to regular waves, asymmetric waves and wave groups. The work contributes therefore, to knowledge about wave-sediment interactions and to understanding of sediment transport mechanics.

 Top | Auteurs 
 

 

Vlaams Instituut voor de Zee
InnovOcean site
Wandelaarkaai 7
B-8400 OOSTENDE, België
Tel: +32 [0]59/34 21 30
Fax: +32 [0]59/34 21 31
Email: info@vliz.be
   

 

Vlaamse Gemeenschap Provincie West-Vlaanderen