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411.
Glacial ice features in the northern and central Barents Sea may threaten ships and offshore structures. Particularly, small glacial ice features, which are difficult to detect and manage by concurrent technologies, are of concern. Additionally, small glacial ice features are more susceptible to wave-driven oscillatory motions, which increases their pre-impact kinetic energy and may damage ships and offshore structures. This paper is part of three related papers. An initial paper (Monteban et al., 2020) studied glacial ice features’ drift, size distribution and encounter frequencies with an offshore structure in the Barents Sea. The following two papers (Paper I and Paper II) further performed glacial ice impact studies, including impact motion analysis (Paper I) and structural damage assessment (Paper II). This paper (Paper I) studies the wave-driven motion of small glacial ice features and their subsequent impact with a given offshore structure. The aim here is to develop a numerical model that is capable of efficiently calculating the relative motion between the ice feature and structure and to sample a sufficient amount of impact events from which statistical information can be obtained. The statistical information entails the distributions of the impact location and associated impact velocities. Given the distributions of the impact velocities at different locations, we can quantify the kinetic energy for related impact scenarios for a further structural damage assessment in Paper II (Yu et al., 2020).In Paper I, a numerical model that separately calculates the wave-driven oscillatory motion and the mean drift motion of small glacial ice features is proposed, implemented and validated. Practical and fit-for-purpose hydrodynamic simplifications are made to simulate and sample sufficient impact events. The numerical model has been favourably validated against existing numerical results and experimental data. A case study is presented where a 10 m wide glacial ice feature is drifting under the influence of surface waves towards an offshore structure. The case study shows that if an impact happens, the overall impact location and impact velocity can be best fitted by the Normal and Weibull distributions, respectively. Additionally, the impact velocity increases with impact height. Moreover, the impact velocity increases and the impact range is more dispersed in a higher sea state. It is also important to notice that the approaches and methods proposed in this paper adhere to and reflect the general requirements stated in ISO19906 (2019) and NORSOK N-003 (2017) for estimating the design kinetic energy for glacial ice impacts. 相似文献
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为了能够准确、高效地计算深水桥梁的墩-水耦合作用,以墩高及入水深度均为60m的圆形实心墩为研究对象,在对目前常用的3种动水压力计算方法(Morison公式、辐射波浪法和流体声单元法)进行理论研究、对流体声单元法流体域边界条件进行改进的基础上,建立了相应的墩-水耦合计算模型,对常用深水桥墩动力特性和动力响应进行对比分析,得到3种方法在计算效率、计算精度方面的差异及适用范围。结果表明:辐射波浪法、Morison公式计算效率高于流体声单元法;辐射波浪法计算精度高于Morison公式、流体声单元法;流体声单元法适用范围比Morison公式、辐射波浪法广。 相似文献
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某型救生船的流体动力性能和动力定位能力评估 总被引:1,自引:0,他引:1
简要介绍了某救生船的流体动力性能试验和多推力器推力分配方法,并对某救生船在稳定的风、浪、流作用下保持固定位置和艏向的能力予以评估. 相似文献
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