BUOYANCY-INDUCED INCLINED BOUNDARY-LAYER FLOW IN A POROUS-MEDIUM RESULTING FROM COMBINED HEAT AND MASS BUOYANCY EFFECTS

被引：32
|
作者：
JANG, JY
CHANG, WJ
机构：
[1] Natl Cheng-Kung Univ, Tainan, Taiwan, Natl Cheng-Kung Univ, Tainan, Taiwan
来源：
INTERNATIONAL COMMUNICATIONS IN HEAT AND MASS TRANSFER | 1988年 / 15卷 / 01期
关键词：
FLOW OF FLUIDS - Boundary Layer - MASS TRANSFER - Calculations;
D O I：
10.1016/0735-1933(88)90003-6
中图分类号：
O414.1 [热力学];
学科分类号：
摘要：
An implicit finite difference method is used to analyze the natural convection boundary layer flow in a saturated porous medium resulting from combined heat and mass buoyancy effects adjacent to an inclined surface. Both the streamwise and normal components of the buoyancy force are retained in the momentum of inclination ranging from 0 to close to 90 degrees from the horizontal.
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页码：17 / 30
页数：14
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