THERMAL-HYDRAULIC ANALYSIS OF TRANSIENT CONJUGATE HEATING BETWEEN HEMI-SPHERICAL BODY AND AIR

被引:7
作者
Rashid, Farhan Lafta [1 ]
Khalaf, Abbas Fadhil [1 ]
Hussein, Ahmed Kadhim [2 ]
Ben Hamida, Mohamed Bechir [3 ,4 ,5 ,6 ]
Ali, Bagh [7 ]
Younis, Obai [8 ]
机构
[1] Univ Kerbala, Coll Engn, Karbala, Iraq
[2] Univ Babylon, Coll Engn, Mech Engn Dept, Babylon City, Iraq
[3] Imam Mohammad Ibn Saud Islamic Univ IMSIU, Coll Engn, Dept Mech Engn, Riyadh, Saudi Arabia
[4] Univ Monastir, Res Lab Ionized Backgrounds, Monastir, Tunisia
[5] Univ Monastir, Preparatory Inst Engn Studies Monastir IPEIM, Reagents Studies EMIR, Monastir, Tunisia
[6] Univ Sousse, Higher Sch Sci & Technol Hammam Sousse ESSTHS, Dept Phys, Sousse, Tunisia
[7] Super Univ, Fac Comp Sci & Informat Technol, Lahore 54000, Pakistan
[8] Prince Sattam Bin Abdulaziz Univ, Coll Engn WadiAddwasir, Mech Engn Dept, Alkharj 11492, Saudi Arabia
来源
FRONTIERS IN HEAT AND MASS TRANSFER | 2022年 / 19卷
关键词
Unsteady conjugate heat transfer; CFD; forced convection; FVM; hemisphere; MIXED CONVECTION; HEAT/MASS TRANSFER; SOLID SPHERE; FLOW; SYSTEMS;
D O I
10.5098/hmt.19.21
中图分类号
O414.1 [热力学];
学科分类号
摘要
Convection and conduction in a fluid flow and a rigid body in contact with each other often occur in engineering situations, resulting in unsteady conjugate heat transfer (CHT). Although the analytical solutions to the separate conduction and convection issues are surprisingly straightforward, the combined conjugate heat transfer problem is substantially more complex to solve. This study investigates the CHT of a fluid (air) passing through an unbounded hemisphere. The hemisphere produces heat at a predictable and regular pace. The governing equations are solved using a finite volume system (FVS) using ANSYS Fluent V.16.0, with axisymmetric, no normal convection, and stable physical characteristics assumed. The findings showed The rise in air temperature will result in a more even dispersion of temperature.The temperature distribution will be narrowed as airflow velocity increases. Heat flow increases in the sphere, resulting in a greater temperature gradient over the object's surface.As airflow increases, so does the dispersion of flow rates. Increasing the pace of airflow will lead to an increase in air pressure distribution.
引用
收藏
页数:6
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