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Numerical Simulations of the Ice Load of a Ship Navigating in Level Ice Using Peridynamics

机译:斜度冰冰冰荷载的数值模拟

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摘要

In this study, a numerical method was developed based on peridynamics to determine the ice loads for a ship navigating in level ice. Convergence analysis of three-dimensional ice specimen with tensile and compression loading are carried out first. The effects of ice thickness, sailing speed, and ice properties on the mean ice loads were also investigated. It is observed that the ice fragments resulting from the icebreaking process will interact with one another as well as with the water and ship hull. The ice fragments may rotate, collide, or slide along the ship hull, and these ice fragments will eventually drift away from the ship. The key characteristics of the icebreaking process can be obtained using the peridynamic model such as the dynamic generation of cracks in the ice sheet, propagation and accumulation of ice fragments, as well as collision, rotation, and sliding of the ice fragments along the ship hull. The simulation results obtained for the ice loads and icebreaking process were validated against those determined from the Lindqvist empirical formula and there is good agreement between the results.
机译:在该研究中,基于白颌动态开发了一种数值方法,以确定在冰冰中导航的船舶的冰负荷。首先进行具有拉伸和压缩负荷的三维冰标本的收敛性分析。还研究了冰厚度,帆船速度和冰性质对平均冰负荷的影响。观察到由破冰过程产生的冰片段将彼此相互作用,以及水和船体。冰片碎片可以沿着船船体旋转,碰撞或滑动,这些冰块最终将远离船舶偏离。可以使用智能动力学模型获得破冰过程的关键特征,例如冰片中的裂缝的动态产生,冰片段的传播和积累,以及沿着船船体的冰片段的碰撞,旋转和滑动。对冰负荷和破冰过程获得的模拟结果验证了来自Lindqvist经验公式确定的那些,结果与结果之间存在良好的一致性。

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