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Experimental study of frost growth on a horizontal cold surface under forced convection

机译:强制对流条件下水平寒冷表面霜冻生长的实验研究

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Frost formation on a horizontal copper surface under low air temperature and forced convection conditions is investigated experimentally. Both the frost crystals pattern and the frost layer thickness formed on the cold plate are compared under different experimental conditions. The environmental variables considered in this study include the ambient temperature (T_∞), air relative humidity (φ), and velocity (v), as well as the cold surface temperature (T_w). The tested ranges are -5≤T_∞≤5℃, 50%≤φ≤80%, 2.2≤v≤8.0 m/s, -16.8≤T_w≤-25.5℃. The experimental results show the cold surface temperature and the air relative humidity have obvious effects on the frost growth: the frost layer thickness increases strongly with the decreasing cold surface temperature and increasing air relative humidity. The air temperature and air velocity or Reynolds number are also important factors affecting the frost crystals' growth and thickness. With the increase of the air temperature and velocity, the frost crystals become denser, and the frost layer thickness become thicker, but this trend becomes weaker under higher air temperature and velocity.
机译:实验研究了低空气温度和强制对流条件下水平铜表面上的霜冻形成。比较了在不同实验条件下在冷板上形成的霜晶图案和霜层厚度。本研究中考虑的环境变量包括环境温度(T_∞),空气相对湿度(φ)和速度(v)以及冷表面温度(T_w)。测试范围为-5≤T_∞≤5℃,50%≤φ≤80%,2.2≤v≤8.0m / s,-16.8≤T_w≤-25.5℃。实验结果表明,冷表面温度和空气相对湿度对霜冻的生长有明显的影响:随着冷表面温度的降低和空气相对湿度的增加,霜层的厚度大大增加。气温和风速或雷诺数也是影响霜晶体生长和厚度的重要因素。随着空气温度和速度的增加,霜晶体变得更致密,霜层厚度变厚,但是在较高的温度和速度下这种趋势变得更弱。

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