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

被引:12
作者
Suntoyo [1 ]
Tanaka, Hitoshi [2 ]
机构
[1] Inst Teknol Sepuluh Nopember ITS, Fac Marine Technol, Dept Ocean Engn, Surabaya 60111, Indonesia
[2] Tohoku Univ, Dept Civil Engn, Sendai, Miyagi 9808579, Japan
基金
日本学术振兴会;
关键词
Turbulent boundary layers; Shallow water; Asymmetric wave; Bed-load transport; OSCILLATORY FLOW; SHEAR-STRESS; SHEET FLOW; PREDICTION; EQUATION;
D O I
10.1016/j.coastaleng.2009.06.005
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
This paper presents an investigation of the roughness effects in the turbulent boundary layer for asymmetric waves by using the baseline (BSL) k-omega 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. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:960 / 969
页数:10
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