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Influence of earthquake ground motion modelling on the dynamic responses of offshore wind turbines

机译:地震地面运动模型对海上风力涡轮机动态响应的影响

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Offshore wind turbines (OWTs) are more and more widely used to produce electrical energy nowadays. Besides the constant wind and wave loads, earthquake excitation can be another important vibration source to the OWTs since many OWTs have been/will be constructed in the seismic prone areas. Extensive research works have been carried out to understand the dynamic behaviours of OWTs when they are subjected to multi-hazards (e.g. the simultaneous wind, wave and/or earthquake loadings). However, when seismic excitations are considered, the onshore earthquake records are normally used as inputs in the analyses due to the lack of offshore data and the difficulty in synthesizing the offshore seismic motions. This practice may lead to inaccurate structural response estimations since it is well known that the seawater can significantly suppress the seafloor vertical motions near the P wave resonant frequencies of the seawater layer, which in turn results in the different characteristics of onshore and offshore earthquake recordings. Moreover, the earthquake motions along the pile of OWTs are different from those at the ground surface, i.e. the earthquake motions vary with the soil depth. Recently, a method to stochastically simulate the earthquake ground motions on the offshore site was proposed, in which the influence of seawater layer was considered and the earthquake motions at any soil depth could be obtained. This paper carries out numerical simulations on the dynamic behaviours of OWTs subjected to the combined wind, wave and earthquake loadings, and the depth-varying offshore seismic motions are used as inputs in the analyses. The seismic responses of OWTs obtained from the onshore and offshore earthquake motions are calculated and compared. The influence of depth-varying ground motions on the dynamic responses of OWTs is discussed.
机译:近海风力涡轮机(OWTS)越来越广泛地用于现在产生电能。除了恒定的风和波浪载荷之外,由于已经在地震俯卧面积中建造了许多欠款,因此地震激励可以是欠的另一个重要振动源。已经进行了广泛的研究,以了解欠款时的动态行为(例如,同时风,波和/或地震载荷)。然而,当考虑地震激励时,由于缺乏海上数据以及综合近海地震运动的难度,陆海地震记录通常用作分析中的投入。这种做法可能导致结构反应估计不准确,因为众所周知,海水可以显着抑制海水层的P波谐振频率附近的海底垂直运动,这又导致陆上和海上地震录制的不同特征。此外,沿着浪费的地震运动与地面的地震运动不同,即地震运动随着土壤深度而变化。最近,提出了一种随机模拟近海部位地震地面运动的方法,其中考虑了海水层的影响,可以获得任何土壤深度的地震运动。本文对对云,波浪和地震载荷进行的欠款的动态行为进行了数值模拟,并且深度不同的离岸地震运动用作分析中的输入。计算并比较了从陆上和近海地震动作获得的欠款的地震反应。讨论了深度不同地面动作对欠款动力响应的影响。

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