Fundamental study for morphodynamic modelling: Sand mounds in oscillatory flows

• Published in: Coastal engineering (Amsterdam) 2009-04, Vol.56 (4), p.408-418
• Main Authors: Stansby, P.K., Huang, J., Apsley, D.D., García-Hermosa, M.I., Borthwick, A.G.L., Taylor, P.H., Soulsby, R.L.
• Format: Article
• Language: English
• Subjects: Bed load; Bed slope; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Engineering geology; Exact sciences and technology; Geomorphology, landform evolution; Marine and continental quaternary; Modelling; Sand mound; Sediment transport; Surficial geology
• ISSN: 0378-3839; 1872-7379
• DOI: 10.1016/j.coastaleng.2008.09.011

Experiments on sand mounds in oscillatory flow, undertaken in controlled, large-scale laboratory conditions, have produced well-defined data sets for model comparison. Three bathymetries with different levels of submergence, including a surface-piercing case, were tested. The maximum slope was about 1:5.5. Sediment transport is due to bed load with ripple formation. The principal time-dependent bulk parameters are the vertical distance of the centre of gravity above the base and the volume of the mound. A semi-implicit finite-volume depth-averaged hydrodynamic model is used to drive morphodynamics, using van Rijn's sediment flux model generalized to take account of bed slope, and some justification is given for depth-averaged modeling in these conditions. Starting the model runs with the conditions at the end of the first cycle avoided initial atypical physical behaviour. In general good predictions were obtained with an angle of repose reduced from the standard value of about 30° for stationary beds to 15°. For these situations, morphodynamics was largely unaffected by a hydrodynamic roughness height in the range 2.5 D 50 to 51 D 50, with larger values accounting for ripple roughness. The reduced angle of repose may be physically expected with mobile beds but this specific value is only expected to be suited to this form of bed motion. In one case an exaggerated ripple formed near the top of the mound reducing agreement with experiment. For the submerged case with normal ripple structure excellent predictions were obtained. For the initially surface-piercing mound, the time of submergence was better predicted with a 30° angle of repose, presumably due to the prominent influence of the near stationary bed near the wet/dry interface, although long term predictions were better predicted with 15°. The occurrence of vortex shedding in the first cycle modeled was in agreement with experimental observation.