CONDENSATION BY HETEROGENEOUS NUCLEATION IN A THERMAL-BOUNDARY-LAYER

被引:2
作者
CHEN, MS
JONES, BW
机构
[1] Industrial and Engineering Technology, Central Michigan University, Mt. Pleasant, MI
[2] Institute for Environment Research, Kansas State University, Manhattan, KS
关键词
CONDENSATION; HETEROGENEOUS NUCLEATION; BOUNDARY LAYER;
D O I
10.1016/0142-727X(90)90052-D
中图分类号
O414.1 [热力学];
学科分类号
摘要
Condensation can occur by the nucleation and growth of water droplets on particles in the air. This mode of mass transport can readily occur in a thermal boundary layer. The primary condition required for droplet nucleation is the existence of supersaturation in the boundary layer. Equations are developed to describe droplet nucleation and transport for the boundary layer on a horizontal, upward facing surface. These equations allow diffusion and nucleation mass fluxes and droplet concentration at a point in the boundary layer to be calculated. Experimental data were collected and compared to the theoretical calculations. Accurately predicting droplet concentration is difficult, but the presence of nucleation condensation can be readily predicted.
引用
收藏
页码:290 / 297
页数:8
相关论文
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