单桩子结构上的极端波浪荷载:与压力冲击冲击荷载模型耦合的预计算运动学

F. Pierella, A. Ghadirian, H. Bredmose
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引用次数: 4

摘要

单桩是目前在浅至中水深的海底固定式海上风力涡轮机的首选子结构类型。在这些地方,造成极端载荷的大波是强烈非线性的。因此,它们不容易通过海上工业中常用的简单工程模型来复制。在当前的方法中,我们开发了一个设计模式来改进这个标准方法。为了保持力计算中的非线性,我们通过潜在的全非线性代码(OceanWave3D)预先计算了许多波浪实现,用于大范围的无量纲水深和显著的波高。然后,设计人员可以从预先计算的集合中提取波浪运动学时间序列,根据弗劳德定律对其进行缩放,并将其与合适的力模型耦合以计算载荷。为了完成这幅图,撞击载荷是通过DTU最近开发的所谓压力冲击模型来计算的。该模型不是计算撞击载荷的时间序列,而是使用几个参数来计算压力脉冲,除了一个参数可以从入射波中确定之外。首先与在DeRisk项目框架下获得的实验结果进行比较,结果很有希望。模拟得到的波浪力和波浪高程统计值与实验结果吻合较好。由于不完美的缩放和物理和数值领域的差异,存在一些差异。当将波浪速度提取为地表高程的时间梯度与x向空间梯度之比时,撞击模型计算得到的载荷与实验结果吻合较好。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Extreme Wave Loads on Monopile Substructures: Precomputed Kinematics Coupled With the Pressure Impulse Slamming Load Model
Monopiles are nowadays the preferred substructure type for bottom-fixed offshore wind turbines at shallow to intermediate water depths. At these locations, the large waves that contribute to extreme loads are strongly nonlinear. Therefore they are not easily reproduced via the simple engineering models who are commonly used in the offshore industry. In the current approach, we develop a design pattern which improves this standard methodology. To retain nonlinearity in the force computations, we have precomputed a number of wave realizations by means of a potential fully-nonlinear code (OceanWave3D), for a wide span of nondimensional water depths and significant wave heights. The designer can then extract a wave kinematics time series from the precomputed set, scale it by the Froude law, and couple it with a suitable force model to compute loads. To complete the picture, slamming loads are calculated by means of the so-called pressure impulse model, recently developed at DTU. Rather than computing the time series of the slamming load, the model uses a few parameters, all except one determinable from the incident wave to calculate the pressure impulse. First comparisons with experimental results, obtained in the framework of the DeRisk project, are promising. The force and the wave elevation statistics from the precomputed simulations are in good agreement with the experiments. Some discrepancies are present, due to an imperfect scaling and to the differences in the physical and numerical domains. The computed loads from the slamming model match the experimental ones quite closely, when the wave celerity is extracted as the ratio between the time gradient and the x-wise space gradient of the surface elevation.
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