Flow under standing waves Part 2. Scour and deposition in front of breakwaters
Publication: Research - peer-review › Journal article – Annual report year: 2009
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Flow under standing waves Part 2. Scour and deposition in front of breakwaters. / Gislason, Kjartan; Fredsøe, Jørgen; Sumer, B. Mutlu.
In: Coastal Engineering, Vol. 56, No. 3, 2009, p. 363-370.Publication: Research - peer-review › Journal article – Annual report year: 2009
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TY - JOUR
T1 - Flow under standing waves Part 2. Scour and deposition in front of breakwaters
A1 - Gislason,Kjartan
A1 - Fredsøe,Jørgen
A1 - Sumer,B. Mutlu
AU - Gislason,Kjartan
AU - Fredsøe,Jørgen
AU - Sumer,B. Mutlu
PB - Elsevier BV
PY - 2009
Y1 - 2009
N2 - A 3-D general purpose Navier-Stokes solver was used to calculate the 2-D flow in front of the breakwater. The k-omega, SST (shear-stress transport) model was selected as the turbulence model. The morphologic model of the present code couples the flow solution with a sediment transport description and routines for, updating the computational mesh based on the mass balance of sediment. Laboratory experiments of scour also were conducted in a wave flume to obtain data for model verification. Both in the numerical simulations and in the laboratory experiment, two kinds of breakwaters were used: A vertical-wall breakwater; and a sloping-wall breakwater (Slope: 1:1.5). Numerically obtained scour-deposition profiles were compared with the experiments. The numerical results show that the equilibrium scour depth normalized by the wave height decreases with increasing water-depth-to-wave-length ratio. Although the numerical results obtained for vertical-wall breakwaters are consistent with the existing experimental data (including the present experiment), the numerical results for the sloping-wall case appear to be not very satisfactory.
AB - A 3-D general purpose Navier-Stokes solver was used to calculate the 2-D flow in front of the breakwater. The k-omega, SST (shear-stress transport) model was selected as the turbulence model. The morphologic model of the present code couples the flow solution with a sediment transport description and routines for, updating the computational mesh based on the mass balance of sediment. Laboratory experiments of scour also were conducted in a wave flume to obtain data for model verification. Both in the numerical simulations and in the laboratory experiment, two kinds of breakwaters were used: A vertical-wall breakwater; and a sloping-wall breakwater (Slope: 1:1.5). Numerically obtained scour-deposition profiles were compared with the experiments. The numerical results show that the equilibrium scour depth normalized by the wave height decreases with increasing water-depth-to-wave-length ratio. Although the numerical results obtained for vertical-wall breakwaters are consistent with the existing experimental data (including the present experiment), the numerical results for the sloping-wall case appear to be not very satisfactory.
KW - Breakwaters
KW - Steady streaming
KW - Standing waves
KW - Scour
KW - Deposition
KW - Bed morphology
KW - Waves
KW - Turbulence modelling
U2 - 10.1016/j.coastaleng.2008.11.002
DO - 10.1016/j.coastaleng.2008.11.002
JO - Coastal Engineering
JF - Coastal Engineering
SN - 0378-3839
IS - 3
VL - 56
SP - 363
EP - 370
ER -