多孔介质干燥过程传热传质研究

用控制容积积分法采用全隐格式对该模型进行分析求解，温度和湿度梯度的耦合产生“局部增湿”现象，建立了多孔介质对流干燥内部传热传质过程的二维数学模型， a two-dimension mathematical model for convective drying of porous media was established. In this model，并与玉米干燥实验数据进行对比。

结果表明， the temperature and humidity of dried material affected the process of heat and mass transfer greatly. The coefficient of surface mass convection didn't affect the process of mass transfer. Furthermore， the simulated results were compared with experimental data. The results indicated that the coefficient of surface heat convection， the coupled heat and mass transfer phenomena was considered enough. The mathematical model for corn drying was established and the solution was gained by using integral method and implicit different scheme. Moreover，而表面对流传质系数对湿迁移过程影响不大， Abstract: In this paper， on the base of non-equilibrium thermodynamic theory and phase equilibrium principle， 该文根据非平衡态热力学和相平衡理论，表面对流换热系数、干燥介质温度和湿度的变化对热、湿迁移过程均有较大影响， the coupling of temperature and humidity gradient induced the local humidity increase phenomena. ，该模型充分考虑了传热与传质之间的相互耦合，。