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Droplet size and velocity distributions of wave-impact sea spray over a marine vessel

机译:冲击波海浪在船舶上的液滴大小和速度分布

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The spatial distribution of droplets in a spray cloud created by wave-impact sea spray and the distribution of their sizes and velocities over a vessel deck are investigated. Existing mono-size and mono-velocity models of sea spray are not accurate enough for modelling marine icing phenomena. Wave-impact sea spray Creates numerous droplets in front of and around a vessel. Droplets are the result of sheet and droplet breakup of sea water. The velocity-size dependence of the resultant droplets causes the creation of various sizes and velocities of droplets. A droplet trajectory method employs the velocity-size dependence of the droplets to find their spatial distributions in the cloud of spray over the vessel deck. Drag and body forces overcome the initial velocities of the droplets, and consequently, they follow the wind and gravitational directions. The motion of the droplets affects the shape and extent of the spray cloud over the vessel. A numerical scheme is used to find the distribution of sizes and velocities of the droplets over a vessel. Results show that neither the smallest nor the largest droplets reach the maximum height. The medium-sized droplets can reach the maximum height of the spray cloud. As the spray cloud travels over the deck, the droplet velocities become almost the same. Comparing the numerical results with field observations shows that the predicted results are consistent and have reasonable agreerhent with the field measurements. (C) 2016 Elsevier B.V. All. rights reserved.
机译:研究了波浪冲击海浪在喷雾云中液滴的空间分布及其在船甲板上的大小和速度分布。现有的海浪单尺度和单速度模型对于模拟海洋结冰现象还不够准确。冲击波的海浪在船只的前面和周围产生大量的水滴。水滴是海水表层和水滴破裂的结果。所得液滴的速度-尺寸依赖性导致产生各种尺寸和速度的液滴。液滴轨迹方法利用液滴的速度-大小相关性在容器甲板上方的喷雾云中找到其空间分布。阻力和体力克服了液滴的初始速度,因此,它们遵循风向和重力方向。液滴的运动会影响容器上方喷雾云的形状和范围。使用数值方案来找到液滴在容器上的大小和速度的分布。结果显示最小或最大的液滴均未达到最大高度。中型液滴可以达到喷雾云的最大高度。当喷雾云在甲板上移动时,液滴的速度几乎相同。将数值结果与现场观测结果进行比较表明,预测结果是一致的,与现场测量结果具有合理的一致性。 (C)2016 Elsevier B.V. All。版权所有。

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