前进速度下确定性重复耐波性试验中遇到波浪的变异性

Sanne van Essen
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引用次数: 4

摘要

船舶在波浪中前进速度的数值耐波性代码通常是基于实验验证或调整的,这使得了解实验变异性至关重要。在最先进的耐波性运动期间,通过重复测试评估了这种变异性。研究了纵向盆地轴上的陡波条件(波ea)和不太陡的斜波条件(波eb)。由于船舶对波浪时间序列中每个点的响应不是同样敏感,因此讨论了总体相似性以及个别波峰高度、陡度和时间变异性。对于波a,测得的入射波峰及其时序随距离波源的远近而增加。波浪b的波峰高度变异性较低,在盆地长度上更恒定(因为在斜波中到模型的传播距离是恒定的,波浪破碎的可能性较小)。结果表明,只有一小部分变化是由“输入”不确定性引起的,如波发生器襟翼运动的精度、测量载体的位置、它们的同步性和测量精度。其余的变化是由波浪和盆地效应引起的,例如波浪破碎不稳定性和以前测试中残留的小波感应电流。后者取决于先前的波浪条件,这需要进一步研究。关于波浪变率对船舶运动变率、沿船相对波高和船舶前进速度时甲板上的冲击载荷的影响的进一步研究将在下一期出版物中发表。
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Variability in Encountered Waves During Deterministically Repeated Seakeeping Tests at Forward Speed
Numerical seakeeping codes for ships at forward speed in waves are often validated or tuned based on experiments, which makes knowledge about the experimental variability essential. This variability was evaluated using repeat tests during a state-of-the-art seakeeping campaign. A steep wave condition over the longitudinal basin axis (waveA) and a less steep oblique wave condition (waveB) were studied. Overall similarity as well as individual crest height, steepnesses and timing variability are discussed, because ship response is not equally sensitive for every point in the wave time series. The variability of the measured incoming wave crests and their timing increases with distance from the wave generator for waveA. The crest height variability for waveB is lower and more constant over the basin length (because the propagation distance to the model is constant in oblique waves and wave breaking is less likely). It was shown that only a small part of the variability close to the wave generator is caused by ‘input’ uncertainties such as the accuracy of the wave generator flap motions, measurement carriage position, their synchronisation and measurement accuracy. The rest of the variability is caused by wave and basin effects, such as wave breaking instabilities and small residual wave-induced currents from previous tests. The latter depend on previous wave conditions, which requires further study. Further work on the influence of the wave variability on the variability of ship motions, relative wave elevation along a ship and impact loads on deck of a ship at forward speed will be presented in a next publication.
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