Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/17060
Title: Mixed Convective Mmagnetohydrodynamics Micropolar Boundary Layer Flow Past a Stretching Sheet with Heat Generation 1Yusuf, A., 1 Ishaq, M. A., 1Salihu, N. O., 2Salisu, A. and 1Bolarin, G. 1Department of Mathematics, Federal University of Technology, Minna, Niger State, Nigeria 2Department of Computer Science, Niger State Polytechnic, Zungeru, Niger State, Nigeria ABSTRACT The problem of mixed convective magnetohydrodynamics micropolar boundary layer past a stretching sheet with heat generation was presented in rectangular form. The partial differential equations formulated are transformed into nonlinear ordinary differential equations using the stream functions and appropriate similarity variables. The solution to the nonlinear coupled ordinary differential equations is presented via decomposition method. The results are validated with the literatures and there is an agreement. The effects of dimensionless physical parameters which occur in the presented results are graphically studied in the absence of microstructural slip. The micro rotation is found to be a reducing agent of thermal and mass Grashof numbers while the fluid is an increasing agent due to the increase in the temperature which resulted in reduction of the viscousity.
Authors: YUSUF, A.
ISHAQ, M. A.
SALIHU, NASIRU OMEIZA
SALISU, A.
BOLARIN, G.
Keywords: Micropolar
Heat generation
Magnetohydrodynamics
Decomposition method
Boundary layer
Issue Date: 2022
Publisher: Savanna Journal of Basic and Applied Science (June, 2022), 4(1): pp 83-91
Abstract: The problem of mixed convective magnetohydrodynamics micropolar boundary layer past a stretching sheet with heat generation was presented in rectangular form. The partial differential equations formulated are transformed into nonlinear ordinary differential equations using the stream functions and appropriate similarity variables. The solution to the nonlinear coupled ordinary differential equations is presented via decomposition method. The results are validated with the literatures and there is an agreement. The effects of dimensionless physical parameters which occur in the presented results are graphically studied in the absence of microstructural slip. The micro rotation is found to be a reducing agent of thermal and mass Grashof numbers while the fluid is an increasing agent due to the increase in the temperature which resulted in reduction of the viscousity.
URI: http://www.sjbas.com.ng/
http://repository.futminna.edu.ng:8080/jspui/handle/123456789/17060
Appears in Collections:Mathematics

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