首页> 外文会议>Fourth International Conference on Advanced Computational Methods in Heat Transfer held in Udine, Italy, in July 1996 >Double diffusive natural convectionin binary gase with horizontal thermal and solutal gradients resulting in opposing buoyancy forces
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Double diffusive natural convectionin binary gase with horizontal thermal and solutal gradients resulting in opposing buoyancy forces

机译:具有水平热梯度和溶解梯度的二元气体中的双扩散自然对流,导致相反的浮力

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The natural convection of air in a square cavity wit horizontal temperature and concentration gradients which give opposing buoyancy forces near the vertical walls was studied numerically. The basic equations sloved are the continuity equation, the Navier-Stokes equations, the energy equation and the concentration equation. Computations were carried ot for Prandtl number Pr=0.71, aspect ratio A=1, Rayleigh number Ra=10~8, buoyanc ratio(-solutal buoyancy/thermal buoyancy) N=2 and various Lewis numbers Le. For Le=0.5 a strong main flow was formed near the walls and then a stratified layer in both the temperature and the concentration fields was formed between two convection layers. Secondary samall rol cells in each cnvection layer migrated periodically. For Le=1 and 2 the flow gradually became steady. For Le=5 a complicated pattern of small roll cells appeared near the walls.
机译:数值研究了方形腔内空气的自然对流,其水平温度和浓度梯度在垂直壁附近产生相反的浮力。推广的基本方程是连续性方程,Navier-Stokes方程,能量方程和浓度方程。计算为普朗特数Pr = 0.71,长径比A = 1,瑞利数Ra = 10〜8,布安克比(溶质浮力/热浮力)N = 2和各种路易斯数Le。对于Le = 0.5,在壁附近形成强的主流,然后在两个对流层之间形成温度和浓度场的分层层。每个保护层中的次要SAMOL rol细胞定期迁移。对于Le = 1和2,流量逐渐稳定。对于Le = 5,在壁附近出现小卷状电池的复杂图案。

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