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Experimental and numerical investigation of wave induced forces and motions of partially submerged bodies near a fixed structure in irregular waves

机译:不规则波中波浪对固定结构附近的部分淹没物体的感应力和运动的实验和数值研究

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This paper is the third of a series covering investigations of the wave induced force and motion behavior of ice masses near a fixed structure. The objective of this phase of the study was to determine whether the effects observed in regular waves (Sayeed et al. (2017b, 2018)) still held in irregular seas. In the present case, wave characteristics measured in front of the fixed structure showed that the significant wave heights follow a standing wave pattern generated by the superposition of the incident and reflected peak frequency wave. Thus it may be inferred that the significant surge and heave forces and motions will be increased or decreased at the node and antinode locations in front of the structure as previously observed for regular waves. Force spectra generated from regular wave force data (Sayeed et al. 2017b) and wave measurements from the present study showed that beyond the nodal location at D/lambda(p) = 0.25, the significant surge force goes down and significant heave force goes up as the body gets close to the structure. Direct measurements of irregular wave forces on a fixed berg model at different proximity to the fixed structure demonstrate the change in significant wave forces based on the ratio of separation distance to peak wavelength. When the berg body is positioned closer to the fixed structure, the normalized significant forces in the horizontal direction decrease, and the normalized significant forces in the vertical direction increase. Significant differences were found between the directly measured force spectra and those produced by linear superposition of regular wave force transfer functions. This is attributed to non-linear effects arising from the iceberg profile and low freeboard.
机译:本文是研究固定结构附近冰块的波浪感应力和运动行为的系列文章的第三篇。该研究阶段的目的是确定在规则波浪中观察到的影响(Sayeed等人(2017b,2018))是否仍在不规则海域中发生。在当前情况下,在固定结构前面测量的波特性表明,有效波高遵循由入射和反射峰值频率波的叠加所产生的驻波模式。因此,可以推断出,如先前对于规则波所观察到的,在结构前面的节点和波腹位置处,显着的浪涌和升沉力和运动将增加或减少。根据常规波浪力数据(Sayeed et al.2017b)生成的力谱以及本研究的波浪测量结果表明,在D / lambda(p)= 0.25的节点位置之外,明显的浪涌力下降而显着的升力上升随着身体接近结构。在不固定于固定结构的固定berg模型上对不规则波浪力的直接测量表明,基于分离距离与峰值波长的比率,显着波浪力的变化。当冰山主体位于更靠近固定结构的位置时,水平方向上的归一化显着力减小,而垂直方向上的归一化显着力增加。发现直接测量的力谱与常规波力传递函数的线性叠加产生的力谱之间存在显着差异。这是由于冰山轮廓和低干舷引起的非线性影响。

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