EurOCEAN 2000 - Vlaams Instituut voor de Zee
EurOCEAN 2000 - Vlaams Instituut voor de Zee
EurOCEAN 2000 - Vlaams Instituut voor de Zee
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Mo<strong>de</strong>lling results for rippled bed regime<br />
Innovative research mo<strong>de</strong>lling work on rippled beds has been started in Year 1. Research<br />
mo<strong>de</strong>ls of differing complexity have been un<strong>de</strong>r <strong>de</strong>velopment in Task Group 2. Research<br />
mo<strong>de</strong>ls have been <strong>de</strong>veloped by four institutes (DTU, SINTEF, UGe and UCNW). In addition,<br />
IMAR’s mo<strong>de</strong>l can be used for rippled as well as plane beds, and DHI’s STP mo<strong>de</strong>l can also be<br />
used for ripples (though it was <strong>de</strong>veloped primarily for plane beds). In Year 1, DTU has<br />
completed mo<strong>de</strong>lling work on roughness and friction above vortex ripples using a k-ω<br />
turbulence mo<strong>de</strong>l, and has ma<strong>de</strong> systematic comparisons of the (mean) drag coefficient for<br />
wave+current flows and for currents alone. This mo<strong>de</strong>l has been used also to make<br />
morphological calculations to predict the profiles of fully <strong>de</strong>veloped vortex ripples. At<br />
SINTEF a mo<strong>de</strong>l has been <strong>de</strong>veloped of (mainly) steady flow above undulating beds, based on<br />
the Reynolds equations and standard closures for the turbulence and sediments. This mo<strong>de</strong>l<br />
also performs morphological calculations. A feature of importance suggested by the solution is<br />
the possible role of suspen<strong>de</strong>d sediments in suppressing flow separation above the lee slopes of<br />
bedforms. At UGe in Year 1, computer co<strong>de</strong> to perform a 3D direct numerical simulation of<br />
the oscillatory flow over fixed ripples has been <strong>de</strong>veloped and validated. This mo<strong>de</strong>l will be<br />
used to study sediment dynamics using a Lagrangian approach. Also at UGe a study of the<br />
ripple formation process has been completed using a linear stability analysis, with emphasis on<br />
the role of near-bed drift currents, and the resulting migration of ripples. These latter results<br />
have been compared successfully with preliminary experimental data from the University of<br />
Catania. Finally, at UCNW, a new mo<strong>de</strong>l for wave+current flows above rippled beds has been<br />
<strong>de</strong>veloped. Unlike the mo<strong>de</strong>ls above, this is a simplified 1DV mo<strong>de</strong>l in which vortex shedding<br />
is represented in the near-bed layer by an analytical eddy viscosity formulation. The near-bed<br />
solution is coupled with a standard turbulence mo<strong>de</strong>l in the outer layer. This mo<strong>de</strong>l will be<br />
further validated in Year 2.<br />
As in the case of the flat-bed research mo<strong>de</strong>ls, it is still un<strong>de</strong>r discussion how best to use the<br />
rippled-bed mo<strong>de</strong>ls in practical applications, and how the results should be systematised for<br />
this purpose.<br />
Engineering mo<strong>de</strong>l results<br />
As a good starting point, an intercomparison exercise with field data proposed by HR has been<br />
carried out in or<strong>de</strong>r to assess the reliability of existing engineering mo<strong>de</strong>ls and methods. The<br />
results showed an unexpectedly large discrepancy between the different mo<strong>de</strong>l predictions and<br />
the data applied. The intercomparison exercise was joined by DUT, DH, IMAR, UCNW and<br />
LNH.<br />
Existing mo<strong>de</strong>ls and methods need to be improved in or<strong>de</strong>r to achieve the overall objective of<br />
the project which is to make sediment transport rate predictions within a factor 2. This has been<br />
started for example by DH, which has exten<strong>de</strong>d its engineering mo<strong>de</strong>l (TRANSPOR) based on<br />
existing field data sets and large scale experiments, in or<strong>de</strong>r to inclu<strong>de</strong> the effect of the waverelated<br />
suspen<strong>de</strong>d transport. The work by IMAR can also be mentioned, which has exten<strong>de</strong>d<br />
the Dibajnia and Watanabe formula, in or<strong>de</strong>r to improve sediment transport rate predictions for<br />
finer sand.<br />
A framework for a new engineering formula has been proposed jointly by HR and UCNW<br />
based on the parameterization of their own mo<strong>de</strong>l results. It was <strong>de</strong>ci<strong>de</strong>d at the first stage to run<br />
improved mo<strong>de</strong>ls for a given set of input parameters and to produce graphs which could be<br />
used later on to fit the different coefficients of the proposed framework.<br />
An exploitation plan for the results of the project has been completed by EDF. A web page and<br />
leaflets has been prepared by DUT. A questionnaire has been sent out by DHI to target/user<br />
groups: national and regional coastal and sea authorities, harbour/port authorities, consulting<br />
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