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Natural Convection Heat Transfer from a Plane Wall to Thermally Stratified Porous Media

by Ihsan Y. Hussain, Basim K. Raheem
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International Journal of Computer Applications
Foundation of Computer Science (FCS), NY, USA
Volume 65 - Number 1
Year of Publication: 2013
Authors: Ihsan Y. Hussain, Basim K. Raheem
10.5120/10891-5792

Ihsan Y. Hussain, Basim K. Raheem . Natural Convection Heat Transfer from a Plane Wall to Thermally Stratified Porous Media. International Journal of Computer Applications. 65, 1 ( March 2013), 33-41. DOI=10.5120/10891-5792

@article{ 10.5120/10891-5792,
author = { Ihsan Y. Hussain, Basim K. Raheem },
title = { Natural Convection Heat Transfer from a Plane Wall to Thermally Stratified Porous Media },
journal = { International Journal of Computer Applications },
issue_date = { March 2013 },
volume = { 65 },
number = { 1 },
month = { March },
year = { 2013 },
issn = { 0975-8887 },
pages = { 33-41 },
numpages = {9},
url = { https://ijcaonline.org/archives/volume65/number1/10891-5792/ },
doi = { 10.5120/10891-5792 },
publisher = {Foundation of Computer Science (FCS), NY, USA},
address = {New York, USA}
}
%0 Journal Article
%1 2024-02-06T21:17:33.452327+05:30
%A Ihsan Y. Hussain
%A Basim K. Raheem
%T Natural Convection Heat Transfer from a Plane Wall to Thermally Stratified Porous Media
%J International Journal of Computer Applications
%@ 0975-8887
%V 65
%N 1
%P 33-41
%D 2013
%I Foundation of Computer Science (FCS), NY, USA
Abstract

The thermal and fluid transport phenomena adjacent to a plane wall in a stable, thermally stratified saturated porous medium is investigated numerically and experimentally in the present work. Glass bead is taken as porous material with diameter (12mm). The temperature distribution and Nusselt number are discussed numerically (Fluent Program) and experimentally for different values of heat flux (150, 250, 500, 750, 1000, 1250 W/m2), thermal stratification (0,-0. 6,-0. 8,-1. 6,-2,-5,-10) and inclination angles (0,-15, 15, 30, 45deg). It is observed that the temperature distribution is affected strongly by thermal stratification where it increases when thermal stratification decreases and it is unaffected strongly by the inclination angles. Also the results show that the Nusselt number varies linearly with downstream coordinate (X) and increases with decreasing stratification parameter.

References
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Index Terms

Computer Science
Information Sciences

Keywords

Natural convection Thermal Stratification Porous Media Experimental and Numerical Study

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