管翅式换热器平直翅片表面结霜特性数值模拟

Numerical Simulation of Frost Formation Characteristics on the Plain Fin Surface of a Fin-and-Tube Heat Exchanger

  • 摘要: 基于欧拉多相流模型,采用数值模拟方法研究了湿空气入口温度、冷面温度、相对湿度及入口流速等关键工况参数对平直翅片管换热器翅片表面结霜特性的影响。结果表明,各参数对换热器表面结霜的空间分布、积累速率均具有显著且耦合的影响。总体而言,入口湿空气温度和相对湿度的升高,以及冷面温度和入口流速的降低,均加速了翅片表面霜层厚度的积累。其中,冷面温度是影响霜层厚度增长的主导因素:当冷面温度由−5 ℃降至−20 ℃时,霜层厚度增加了32.04%;入口流速对霜层厚度的影响最小,流速由2 m/s降至0.5 m/s时,厚度仅提高12.55%。在霜层密度方面,湿空气入口温度的提升作用最为显著,温度由−5 ℃升高至5 ℃时,霜层密度增长了41.32%。研究结果为管翅式换热器在实际工况下的防霜与除霜优化设计提供了一定的理论参考与数据支撑。

     

    Abstract: Based on the Eulerian multiphase flow model, this paper uses numerical simulation to study the effects of key operating parameters such as wet air inlet temperature, cold surface temperature, relative humidity and inlet flow rate on the surface frosting characteristics of the fins of a flat and straight finned tube heat exchanger. The results show that each parameter has a significant and coupled effect on the spatial distribution and accumulation rate of heat exchanger surface frost. Overall, the increase of inlet wet air temperature and relative humidity, as well as the decrease of cold surface temperature and inlet flow rate accelerated the accumulation of frost thickness on the fin surface. Among them, the cold surface temperature was the dominant factor influencing the increase of frost layer thickness: when the cold surface temperature was decreased from −5 ℃ to −20 ℃, the frost layer thickness increased by 32.04%; the inlet flow velocity had the least influence on the frost layer thickness, and the thickness only increased by 12.55% when the flow velocity was decreased from 2 m/s to 0.5 m/s. In terms of frost layer density, the enhancement of wet air inlet temperature was the most significant, and the frost layer density increased by 41.32% when the temperature was increased from −5 ℃ to 5 ℃. The results of the study can provide some theoretical references and data support for the optimal design of frost prevention and defrosting of tube and fin heat exchangers under actual working conditions.

     

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