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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Conference among others, and will be discussed in the coming ICCE <strong>2000</strong> Sydney Conference,<br />
and in an end-users conference “Presentation of Research Results in Coastal Engineering,<br />
Scour Around Marine Structures, and Morphodynamics Around Coastal Structures” in Paris 3-<br />
4. October, <strong>2000</strong> (e-mail to hildur@isva.dtu.dk for information on this latter conference).<br />
The project is organized in two main tasks: Task 1. Flow and scour processes, and Task 2.<br />
Sediment behaviour close to the structure and scour.<br />
FLOW AND SCOUR PROCESSES (TASK 1)<br />
The work in Task 1, led by HR, concentrates on the interaction between the water flow and the<br />
sediment at the toe of the structure. The work is sub-divi<strong>de</strong>d into four topics:<br />
TOPIC 1.1. FLOW AND SCOUR PROCESSES AROUND VERTICAL CYLINDERS.<br />
The data on scour around vertical cylin<strong>de</strong>rs - slen<strong>de</strong>r piles, pile groups and large diameter<br />
cylin<strong>de</strong>rs - has been obtained in wave flumes and wave basins. Test conditions have covered<br />
the cases for waves alone, including non-linear shallow water waves and breaking waves, as<br />
well as waves and currents. The work on scour around pile groups has been published Sumer<br />
and Fredsøe (1998) and Mory et al (1999). Additional test results were obtained for the scour<br />
and settlement of a single pile into the sand bed. A 3D numerical mo<strong>de</strong>l for bed scour around a<br />
slen<strong>de</strong>r pile has been <strong>de</strong>vised (Roulund et al, 1998).<br />
TOPIC 1.2. SCOUR AT RUBBLE MOUND BREAKWATER. Experimental results for<br />
the scour <strong>de</strong>velopment at the toe of a rubble mound breakwater (RMB) have been published<br />
(Sumer et al, <strong>2000</strong>). This work investigated the scour <strong>de</strong>velopment at the trunk section of a<br />
breakwater and the efficiency of scour protection measures. The results have been exten<strong>de</strong>d to<br />
the 3D case through test data for scour <strong>de</strong>velopment around a shore-parallel RMB. The data<br />
was collected in a large 3D wave basin. A total of 5 tests investigated the time <strong>de</strong>velopment of<br />
scour and the equilibrium morphology around the breakwater for normal and oblique inci<strong>de</strong>nce<br />
waves and with a tidal current. Scour protection measures were tested and the influence of<br />
storm (breaking) waves was simulated. The first results have been published (Sutherland et al,<br />
1999a) and a data report written (Sutherland et al, 1999b). Measurements of the pore pressure<br />
field in the bed at a number of locations during the 3D tests will enhance the link with Task 2<br />
of the project.<br />
TOPIC 1.3. SCOUR AROUND SUBMERGED BREAKWATERS. The large-scale 2D<br />
wave flume experiments on scour <strong>de</strong>velopment at the toe of submerged breakwaters is<br />
un<strong>de</strong>rway. The tests show the extent of scour <strong>de</strong>velopment un<strong>de</strong>r different wave conditions<br />
and varying levels of freeboard. Scour protection measures will be tested. In parallel,<br />
mathematical mo<strong>de</strong>lling of the wave hydrodynamics and morphodynamics around the<br />
submerged breakwater has been completed. These results are used in conjunction with some<br />
earlier test results to <strong>de</strong>termine both the hydraulic performance of the structure and the seabed<br />
scour. Early results have already been published (Gironella and Sanchez-Arcilla, 1999).<br />
TOPIC 1.4. THE EFFECT OF TURBULENCE ON SEDIMENT TRANSPORT. The<br />
turbulence levels in the vicinity of coastal structures can be high and the flow field non-steady<br />
and non-uniform. The influence of an external (grid) turbulence field on the bed shear stress<br />
and sediment transport has been measured in steady flow flume experiments. The sediment<br />
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