Backfilling of a scour hole around a pile in waves and current

被引:0
作者
机构
[1] Technical Univ. of Denmark, DTU Mekanik, Section for Fluid Mechanics, Coastal and Maritime Engineering
[2] Dept. of Civil and Environmental Engineering, Univ. of Catania
来源
Sumer, B.M. (bms@mek.dtu.dk) | 1600年 / American Society of Civil Engineers (ASCE), United States卷 / 139期
关键词
Backfilling; Current; Offshore wind turbine; Offshore windfarm; Pile; Scour; Time scale; Waves;
D O I
10.1061/(ASCE)ww.1943-5460.0000161
中图分类号
学科分类号
摘要
This paper presents the results of an experimental investigation of the backfilling of scour holes around circular piles. Scour holes around a pile are generated either by a current or a wave. Subsequently, the flow climate is changed from current to wave, combined waves and current, or wave to a smaller wave, leading to the backfilling of the scour hole. The investigation has shed light onto the mechanism behind the backfilling process. The results showthat the scour depth corresponding to the equilibriumstate of backfilling is the same as that corresponding to the equilibrium state of scour around the pile for the same wave (or combined waves and current) climate. The time scale of backfilling has been determined as a function of three parameters, namely, (1) the Keulegan-Carpenter number of the initialwave or current (which generates the initial scour hole); (2)that of the subsequent wave, which backfills the scour hole; and (3) the Shields parameter associatedwith the latter wave, for livebed conditions. In the case of thecombined waves and current, thecurrent-to-wave-velocity ratio is also involved. The time scale of the backfilling process is completely different from that of scour. The time scale of backfilling is much larger than that of scour when the Keulegan-Carpenter number associatedwith the backfilling is KCf<O(10) (typical wind farmapplication),while the time scale of backfilling can be smaller than that of scour when KCf≫≫O(10). © 2013 American Society of Civil Engineers.
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页码:9 / 23
页数:14
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