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OBSERVED SUSPENDED SEDIMENT PROFILES UNDER THE EFFECT OF SINGLE AND DOUBLE PEAKED WAVE SPECTRA

机译:在单一和双峰值波谱的效果下观察到悬浮沉积物曲线

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A series of experiments have been carried out in the DHI Shallow Water Basin in order to identify possible effects of a double peaked wave spectrum on sediment transport related processes. Wave conditions for different tests were chosen on the basis of a constant total amount of energy but with different distribution of this energy in the two peaks. Results show an increase in time averaged concentrations when a small swell component is added to a wind sea dominated spectrum. Similarly, a reduction takes place when a small wind sea component is added to a spectrum accounting for swell conditions. The analysis of the vertical distribution of turbulence and bed roughness features provides indicators of the origin of these variations in suspended sediment concentrations.
机译:在DHI浅水盆地中进行了一系列实验,以确定双峰值波谱对沉积物传输相关过程的可能影响。基于恒定总能量,但在两个峰值中具有不同的能量分布,选择了不同测试的波条件。结果表明,当将小膨胀组分添加到风水海导光谱中时,显示时间平均浓度的增加。类似地,当将小风海组分添加到频谱算法中时,发生了减少,以进行膨胀条件。湍流粗糙度粗糙度特征的垂直分布的分析提供了这些悬浮沉积物浓度的这些变化的起源指标。

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