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首页> 外文期刊>Journal of Heat Transfer >Temperature Gradient in the Unfrozen Liquid Layer for Multiphase Energy Balance With Incoming Droplets
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Temperature Gradient in the Unfrozen Liquid Layer for Multiphase Energy Balance With Incoming Droplets

机译:未冻结液体层中的温度梯度,用于引入液滴的多相能量平衡

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摘要

Phase change heat transfer with impinging supercooled droplets on an ice surface is examined. Partial solidification of incoming droplets leads to an unfrozen water layer above the ice. The significance of temperature variations within the water layer is considered. The multiphase energy balance is shown to approach the measured rate of ice growth when the surface heat input is lowered sufficiently. This asymptotic behavior is essential for establishing the proper role of heat conduction in the solid and liquid (unfrozen water) layers. Predicted results are successfully validated by comparisons with experimental data involving ice buildup on heated circular conductors.
机译:研究了相变传热,其中过冷液滴撞击在冰面上。进入的液滴的部分固化导致冰上未冻结的水层。考虑了水层内温度变化的重要性。当表面热量输入充分降低时,多相能量平衡显示接近冰的测得速率。这种渐近行为对于在固体和液体(未冻结的水)层中建立热传导的适当作用至关重要。通过与涉及在加热的圆形导体上结冰的实验数据进行比较,成功地验证了预测结果。

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