基于运行模态分析的TetraSpar浮子两种构型阻尼辨识

A. Pegalajar-Jurado, Freddy J. Madsen, H. Bredmose
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引用次数: 5

摘要

二阶流体动力载荷可以在浮动风力涡轮机的固有频率下引起运动。这些共振响应高度依赖于流体动力阻尼,而流体动力阻尼主要是由粘性效应引入的。在数值上,这些粘性效应通常由具有相对速度的莫里森阻力项表示,其中引入了强迫、与海况相关的线性阻尼和与幅值相关的二次阻尼。最近的文献表明,校正莫里森阻力系数的衰减试验是不够的,以达到准确的响应在数值模型。此外,仅校正阻力系数就会改变力和阻尼。因此,按照通常的做法,需要额外的阻尼项,这需要根据操作条件进行校准。在这项研究中,我们将操作模态分析(OMA)应用于Stiesdal Offshore Technologies公司的TetraSpar浮子的波盆结果。该浮子以1:60的比例与DTU 10MW参考风力涡轮机进行了测试,包括半桅杆和桅杆构型。我们确定了不同环境条件下浪涌和俯仰的线性化阻尼比,并研究了其与海况和运动幅值的关系。初步结果表明,随着波高和运动幅值的显著增加,俯仰模态的阻尼呈增加趋势,而浪涌模态的阻尼呈不太明显的趋势。这与较大的阻尼水平、较小的固有频率和较大的浪涌OMA不确定性有关。本文最后讨论了OMA估计对数据量及其处理的依赖性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Damping Identification of the TetraSpar Floater in Two Configurations With Operational Modal Analysis
Second-order hydrodynamic loads can induce motions at the natural frequencies of a floating wind turbine. These resonant responses are highly dependent on the hydrodynamic damping, which is mostly introduced by viscous effects. Numerically, these viscous effects are often represented by a Morison drag term with relative velocity, which introduces forcing, sea state-dependent linear damping and amplitude-dependent quadratic damping. Recent literature shows that calibration of the Morison drag coefficients to decay tests is not sufficient to achieve an accurate response in the numerical models. In addition, calibration of the drag coefficient alone changes both forcing and damping. Hence, following common practice, additional damping terms are needed, which require calibration against operating conditions. In this study, we apply Operational Modal Analysis (OMA) to wave basin results for the TetraSpar floater of Stiesdal Offshore Technologies. The floater was tested at scale 1:60 with the DTU 10MW reference wind turbine, both in the semi and spar configurations. We identify the linearized damping ratio in surge and pitch for different environmental conditions and investigate its dependency on the sea state and the motion amplitude. Our preliminary results show that the damping of the pitch mode follows increasing trends with significant wave height and motion amplitude, whereas the damping in surge presents a less clear tendency. This is linked to the larger damping level, smaller natural frequency and larger OMA uncertainty for surge. The paper concludes with a discussion of the dependency of OMA estimates on the amount of data and its processing.
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