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Three-dimensional Ice Accretion Using Revised Myers Model

机译:使用修订后的迈星模型的三维冰增冰

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Ice accretion and water film flow on an arbitrary three-dimensional surface are the essential factors that influence the precision of ice simulation. The Myers icing model in which the water film flow equations are coupled with ice growth equations is revised and used to perform the simulation successfully. The revision mainly includes the determination of the transition from rime ice to glaze ice. The transition is determined by both its ice thickness and water flux in the revised model which can remove unreasonable ice horn and improve ice calculation result. Also, an effective numerical scheme for water film is presented. Glaze ice calculation results of a two-dimensional NACA0012 airfoil and three-dimensional GLC-305 swept wing are presented and compared with experimental ice shape to validate its accuracy. The calculation results show major characteristics of glaze ice and agree well with the experimental results. Compared with the LEWICE results, the current method is more suitable for calculating runback ice accretion, but it has disadvantages while predicting ice horn growth.
机译:随意的三维表面上的冰渐流和水膜流动是影响冰仿真精度的基本因素。修订中,其中水膜流动方程与冰增长方程耦合的孤立糖果模型并用来成功执行模拟。修订主要包括确定从霜冰釉冰的过渡。转变由其修订模型中的冰厚度和水通量决定,可以去除不合理的冰角并改善冰计算结果。而且,提出了一种用于水膜的有效数值方案。釉料冰计算结果的二维NaCA0012翼型和三维GLC-305扫过的扫翼,与实验冰形状进行比较,以验证其精度。计算结果表明了釉冰的主要特征,并与实验结果很好。与lewice结果相比,目前的方法更适合于计算回归冰增冰,但是在预测冰喇叭生长的同时存在缺点。

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