Variability of wave-induced ripple migration in wave-flume experiments and its implications for sediment transport

被引:6
作者
Yamaguchi, Naofumi [1 ]
Sekiguchi, Hideo [2 ]
机构
[1] AIST, Geol Survey Japan, Tsukuba, Ibaraki 3058567, Japan
[2] Osaka City Univ, Grad Sch Sci, Sumiyoshi Ku, Osaka 5588585, Japan
关键词
Wave ripple migration; Sediment transport; Phase-lag effect; Oscillatory flow; Wave-flume experiment; FULL-SCALE RIPPLES; OSCILLATORY FLOWS; BEDFORM MIGRATION; SHEET FLOW; NEARSHORE;
D O I
10.1016/j.coastaleng.2011.03.001
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
A thorough discussion of results from laboratory experiments with regular waves sheds light on the gap that lies between the sediment transport associated with ripple migration and the performance of a standard bedload transport formula in terms of bed shear concept. It is found that the extent of deviations of the bedload transport formula by Ribberink (1998) from the measured rate of sediment transport associated with ripple migration becomes systematically apparent under conditions of increasing settling time factor Omega(s) (=eta/w(0)T); eta is the ripple height, w(0) the settling velocity and T the wave period). Re-examination of previous two field studies demonstrates a further reinforcement for phase-lag argument addressed in this paper. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:671 / 677
页数:7
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