Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium

The present work emphasizes the MHD mixed convective stagnation point flow over a shrinking/stretching surface saturated in a porous medium. The double stratification with heat source effects are also considered while the magnetic field is imposed normal to the sheet. The governing model (partial di...

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Main Authors: Khashi'ie, Najiyah Safwa, Md Arifin, Norihan, Rashidi, Mohammad Mehdi, Hafidzuddin, Ezad Hafidz, Wahi, Nadihah
Format: Article
Language:English
Published: Springer 2020
Online Access:http://psasir.upm.edu.my/id/eprint/86616/
http://psasir.upm.edu.my/id/eprint/86616/1/Magnetohydrodynamics%20%28MHD%29%20stagnation%20point%20flow%20past%20.pdf
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author Khashi'ie, Najiyah Safwa
Md Arifin, Norihan
Rashidi, Mohammad Mehdi
Hafidzuddin, Ezad Hafidz
Wahi, Nadihah
author_facet Khashi'ie, Najiyah Safwa
Md Arifin, Norihan
Rashidi, Mohammad Mehdi
Hafidzuddin, Ezad Hafidz
Wahi, Nadihah
author_sort Khashi'ie, Najiyah Safwa
building UPM Institutional Repository
collection Online Access
description The present work emphasizes the MHD mixed convective stagnation point flow over a shrinking/stretching surface saturated in a porous medium. The double stratification with heat source effects are also considered while the magnetic field is imposed normal to the sheet. The governing model (partial differential equations) is converted into a system of ordinary (similarity) differential equations using similarity transformations. The boundary value problem solver (bvp4c) in the MATLAB software is utilized for the numerical computations. Numerical results are graphically illustrated in the form of velocity, temperature and concentration profiles for several values of buoyancy, magnetic, thermal and solutal stratification parameters. The graphs of skin friction coefficient, local Nusselt and Sherwood numbers portray that the dual solutions are achievable within a certain range of the buoyancy and velocity ratio parameters. Both assisting and opposing flow cases can generate two solutions, whereas the forced convective flow only produces a unique solution. The execution of stability analysis affirms the reliability of the first solution. Both heat and mass transfer rates intensify with the increment of the velocity ratio parameter for all type of convective flows. The fluid temperature and concentration decrease with the increment of the thermal and solutal stratification parameters, respectively, whereas the magnetic and buoyancy parameters reduce both temperature and concentration profiles.
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institution Universiti Putra Malaysia
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language English
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spelling upm-866162021-10-13T07:55:14Z http://psasir.upm.edu.my/id/eprint/86616/ Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium Khashi'ie, Najiyah Safwa Md Arifin, Norihan Rashidi, Mohammad Mehdi Hafidzuddin, Ezad Hafidz Wahi, Nadihah The present work emphasizes the MHD mixed convective stagnation point flow over a shrinking/stretching surface saturated in a porous medium. The double stratification with heat source effects are also considered while the magnetic field is imposed normal to the sheet. The governing model (partial differential equations) is converted into a system of ordinary (similarity) differential equations using similarity transformations. The boundary value problem solver (bvp4c) in the MATLAB software is utilized for the numerical computations. Numerical results are graphically illustrated in the form of velocity, temperature and concentration profiles for several values of buoyancy, magnetic, thermal and solutal stratification parameters. The graphs of skin friction coefficient, local Nusselt and Sherwood numbers portray that the dual solutions are achievable within a certain range of the buoyancy and velocity ratio parameters. Both assisting and opposing flow cases can generate two solutions, whereas the forced convective flow only produces a unique solution. The execution of stability analysis affirms the reliability of the first solution. Both heat and mass transfer rates intensify with the increment of the velocity ratio parameter for all type of convective flows. The fluid temperature and concentration decrease with the increment of the thermal and solutal stratification parameters, respectively, whereas the magnetic and buoyancy parameters reduce both temperature and concentration profiles. Springer 2020-08 Article PeerReviewed text en http://psasir.upm.edu.my/id/eprint/86616/1/Magnetohydrodynamics%20%28MHD%29%20stagnation%20point%20flow%20past%20.pdf Khashi'ie, Najiyah Safwa and Md Arifin, Norihan and Rashidi, Mohammad Mehdi and Hafidzuddin, Ezad Hafidz and Wahi, Nadihah (2020) Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium. Journal of Thermal Analysis and Calorimetry, 139 (1). 3635 - 3648. ISSN 1388-6150; ESSN: 1572-8943 https://link.springer.com/article/10.1007/s10973-019-08713-8 10.1007/s10973-019-08713-8
spellingShingle Khashi'ie, Najiyah Safwa
Md Arifin, Norihan
Rashidi, Mohammad Mehdi
Hafidzuddin, Ezad Hafidz
Wahi, Nadihah
Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium
title Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium
title_full Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium
title_fullStr Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium
title_full_unstemmed Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium
title_short Magnetohydrodynamics (MHD) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium
title_sort magnetohydrodynamics (mhd) stagnation point flow past a shrinking/ stretching surface with double stratification effect in a porous medium
url http://psasir.upm.edu.my/id/eprint/86616/
http://psasir.upm.edu.my/id/eprint/86616/
http://psasir.upm.edu.my/id/eprint/86616/
http://psasir.upm.edu.my/id/eprint/86616/1/Magnetohydrodynamics%20%28MHD%29%20stagnation%20point%20flow%20past%20.pdf