Sediment transport over sills at longitudinal training dams with unaligned main flow

Abstract (2017)
Author(s)

S.M.M. Jammers (HKV Lijn in Water, Deltares, National University of Singapore)

AJ Paarlberg (HKV Lijn in Water)

Wim Uijttewaal (TU Delft - Environmental Fluid Mechanics)

Research Group
Rivers, Ports, Waterways and Dredging Engineering
Copyright
© 2017 S.M.M. Jammers, AJ Paarlberg, E. Mosselman, W.S.J. Uijttewaal
More Info
expand_more
Publication Year
2017
Language
English
Copyright
© 2017 S.M.M. Jammers, AJ Paarlberg, E. Mosselman, W.S.J. Uijttewaal
Research Group
Rivers, Ports, Waterways and Dredging Engineering
Pages (from-to)
86-87
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

Longitudinal
training dams (LTDs) are  constructed in
the River Waal in the  Netherlands. They
are aligned parallel to the  river shore
and divide the river into a main and  side
channel. The existing groynes are  removed
yielding more discharge capacity at  high
flows. The side channel creates possibly a 
sheltered environment for species compared to  the traditional groyne field (Collas, 2014).  Although the lay-out of the LTDs has been  extensively studied using numerical models  (e.g. Huthoff et al., 2011), the
morphodynamic  response is yet unclear and
depends strongly  on the dimensions
(length and height) of the  openings. The
inlet and openings (see Fig. 1)  are
sill-type structures which can be changed 
relatively easy.  These sills are
designed in such a way that  they serve
as a barrier for water and bed load  sediment.
To make long-term morphological  predictions,
it is necessary to understand the  bed
load transport processes over these sills. 
Suspended sediment transport is not 
considered in this study. We developed an  analytical model to predict sediment
transport  paths on a slope, using a
correction on the  well-known critical
Shields parameter. 



Files

License info not available