Multi-Phase Simulation of Droplet Trajectories of Wave-Impact Sea Spray Over a Vessel

S. Mintu, D. Molyneux, B. Colbourne
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引用次数: 3

Abstract

Sea spray, generated by ship-wave collisions, is the main source of marine icing. In certain, but not all, circumstances a cloud of spray forms after a wave impacts a ship. The spray cloud comprises numerous water droplets of various sizes. These droplets are dispersed and transported over the vessel deck by the surrounding wind and fall onto the deck or into the ocean under the effect of gravity. The motion of these droplets is important since they determine the extent of the spray cloud and its duration over the deck, which consequently affects the distribution of icing accumulation on a ship in freezing weather. In this paper, a multi-phase air-water simulation of droplet trajectory is used to predict the cloud motion of various size droplets. A smooth particle hydrodynamics (SPH) computational fluid dynamics (CFD) model is implemented and the simulation is accelerated using GPU computing. The field observation data is used to simulate the trajectory. The results of the simulations are compared with an available theoretical model and reasonable agreement is found. The inverse dependence of size and velocity for droplets after the breakup process is examined. The simulation results are consistent with the theoretical model in that neither the largest nor the smallest droplets reach the maximum height of the spray cloud, but the mid-size droplets do. The spray cloud spreads faster and crosses the front of the vessel quicker than predicted by the theoretical model. It is also found that the trajectory of a single droplet is significantly affected by surrounding droplets in a multi-droplet trajectory model. A mono-droplet theoretical trajectory model, therefore, is not as accurate as the multi-droplet CFD model.
船舶上海浪冲击海沫液滴轨迹的多相模拟
船浪碰撞产生的浪花是海洋结冰的主要来源。在某些情况下,但不是所有情况下,波浪撞击船只后会形成一团水雾。喷雾云由许多大小不一的水滴组成。这些水滴被周围的风分散并在甲板上传播,在重力的作用下落在甲板上或进入海洋。这些液滴的运动很重要,因为它们决定了喷雾云的范围及其在甲板上的持续时间,从而影响了寒冷天气下船上结冰的分布。本文采用液滴轨迹的多相空气-水模拟来预测不同大小液滴的云运动。建立了光滑粒子流体力学(SPH)计算流体力学(CFD)模型,并利用GPU计算加速了仿真。利用野外观测资料对弹道进行了模拟。将仿真结果与已有的理论模型进行了比较,得到了合理的吻合。研究了破碎过程后液滴大小和速度的反比关系。模拟结果与理论模型一致,最大和最小的液滴都没有达到喷雾云的最大高度,而中等大小的液滴达到了最大高度。喷雾云的扩散速度比理论模型预测的更快,并且穿过容器的前部。在多液滴轨迹模型中,单个液滴的轨迹受到周围液滴的显著影响。因此,单液滴的理论轨迹模型不如多液滴的CFD模型精确。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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