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Effect of bed roughness on turbulent boundary layer and net sediment transport under asymmetric waves

Authors :
Suntoyo
Tanaka, Hitoshi
Source :
Coastal Engineering. Sep2009, Vol. 56 Issue 9, p960-969. 10p.
Publication Year :
2009

Abstract

Abstract: This paper presents an investigation of the roughness effects in the turbulent boundary layer for asymmetric waves by using the baseline (BSL) k–ω model. This model is validated by a set of the experimental data with different wave non-linearity index, N i (namely, N i =0.67, N i =0.60 and N i =0.58). It is further used to simulate asymmetric wave velocity flows with several values of the roughness parameter (a m /k s ) which increase gradually, namely from a m /k s =35 to a m /k s =963. The effect of the roughness tends to increase the turbulent kinetic energy and to decrease the mean velocity distribution in the inner boundary layer, whereas in the outer boundary layer, the roughness alters the turbulent kinetic energy and the mean velocity distribution is relatively unaffected. A new simple calculation method of bottom shear stress based on incorporating velocity and acceleration terms is proposed and applied into the calculation of the rate of bed-load transport induced by asymmetric waves. And further, the effect of bed roughness on the bottom shear stress and bed-load sediment transport under asymmetric waves is examined with the turbulent model, the newly proposed method, and the existing calculation method. It is found that the higher roughness elements increase the magnitude of bottom shear stress along a wave cycle and consequently, the potential net sediment transport rate. Moreover, the wave non-linearity also shows a big impact on the bottom shear stress and the net sediment transport. [Copyright &y& Elsevier]

Details

Language :
English
ISSN :
03783839
Volume :
56
Issue :
9
Database :
Academic Search Index
Journal :
Coastal Engineering
Publication Type :
Academic Journal
Accession number :
43527086
Full Text :
https://doi.org/10.1016/j.coastaleng.2009.06.005