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A Study of Solidification During Ice Slurry Generation in an Inclined Rectangular Cavity

机译:倾斜矩形腔中冰浆期生成过程中的凝固研究

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The solidification process involved in ice slurry generation is accompanied by multiphase convection of liquid and solid phases. In this article, ice slurry generation in an inclined rectangular cavity has been investigated numerically and experimentally. The ice slurry is generated by freezing a hypereutectic aqueous ammonium chloride (H~(2)O?+?NH~(4)Cl) solution from one side of the cavity. In the numerical study, a validated macroscopic model, that consider solidification, multiphase convective flow, interfacial drag and particle sedimentation, is used to analyse the transport phenomena during ice slurry generation. The model predicts flow field, temperature, species and solid fraction distributions. In the experimental study, particle image velocimetry has been used for in situ study of the flow and the solidified and mushy zone thickness during solidification. The thermal history in the cavity at selected strategic locations is recorded by T-type thermocouples. The validation of the model and experimental and numerical results of evolution of solid fraction, temperature profile, multiphase velocity field and mass of ice slurry produced have been discussed.
机译:冰浆产生的凝固过程伴随着液相和固相的多相对流。在本文中,在数值和实验上研究了倾斜矩形腔中的冰浆。通过从腔的一侧冷冻过过化氯化铵水溶液(H〜(2)O→NH〜(4)CL)溶液来产生冰浆。在数值研究中,考虑凝固,多相对流流动,界面阻力和颗粒沉降的验证宏观模型用于分析冰浆生成过程中的运输现象。该模型预测流场,温度,物种和固体分量分布。在实验研究中,粒子图像VENOCIMETRY已用于原位研究在凝固过程中的流动和固化和糊状区厚度。所选战略位置处的腔中的热历史记录由T型热电偶记录。已经讨论了固体级分,温度曲线,多相速度场和产生的冰浆料展现的模型和实验性和数值结果的验证。

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