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MHD Double-Diffusive and Viscous Dissipative Boundary Layer Flow over a Vertical Plate with Heat Source, Reacting Species, and Thermal and Mass Transfer Gradients

Received: 19 February 2023    Accepted: 15 March 2023    Published: 15 June 2023
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Abstract

Fluid flow problems with convective boundary conditions have applications in the science and engineering worlds. Specifically, they are relevant in the heating and cooling processes observed in glass fiber production, and aerodynamic extrusion. This paper investigates the problem of steady MHD double-diffusive, viscous dissipative boundary layer flow over a vertical plate with heat source, reacting species, and thermal and mass transfer gradients effects. Usually, the problem of flow through porous media is examined using the Boussinesq’s approximations. The governing nonlinear partial differential equations are coupled and complex. Making them tractable, they are linearized into a set of ordinary differential equations using the similarity transform. The evolving set of ordinary differential equations is solved numerically using the fifth-order Runge-Kutta Fehlberg Method and Maple 21 mathematical computational software. The results obtained for the concentration, temperature, and velocity are presented graphically. The analysis of results shows, amongst others, that an increase in the magnetic field parameter increases the temperature and concentration, but decreases the velocity of the fluid; an increase in the Biot number increases the temperature, concentration, and velocity of the fluid; an increases in the concentration difference parameter increases the temperature, but decreases the concentration and velocity of the fluid; an increase in the Eckert number increases the concentration, but decreases the temperature and velocity of the fluid.

Published in International Journal of Fluid Mechanics & Thermal Sciences (Volume 9, Issue 1)
DOI 10.11648/j.ijfmts.20230901.11
Page(s) 1-11
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Double-Diffusion, Heat Source, MHD, Reacting Species, Thermal/Mass Transfer Gradients, Viscous Dissipation

References
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[13] Imoro R., Arthur F. M., Seini Y. I., 2014. Heat and mass transfer over a vertical surface with convective boundary conditions in the presence of viscous dissipation and nth-order chemical reaction. Int. J. Comput. and Appl. Math. 9 (2), 101-118.
[14] Shateyi S., 2017. Heat and mass transfer for natural convection MHD flow over a permeable moving vertical plate with convective boundary condition in the presence of viscous dissipation. AIP Conf. Proc., 1863, 560075, https://doi.org/10.5098/hmt.9.7.
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[23] Narayana P. V., Kesavaiah D. Ch., Venkataramana S., 2011. Viscous dissipation and thermal radiation effects on unsteady MHD convection flow past a semi-infinite vertical permeable moving porous plate. Int. J. Math. Archives 2 (4), 76.
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  • APA Style

    Okuyade Ighoroje Wilson Ata, Mebine Promise. (2023). MHD Double-Diffusive and Viscous Dissipative Boundary Layer Flow over a Vertical Plate with Heat Source, Reacting Species, and Thermal and Mass Transfer Gradients. International Journal of Fluid Mechanics & Thermal Sciences, 9(1), 1-11. https://doi.org/10.11648/j.ijfmts.20230901.11

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    ACS Style

    Okuyade Ighoroje Wilson Ata; Mebine Promise. MHD Double-Diffusive and Viscous Dissipative Boundary Layer Flow over a Vertical Plate with Heat Source, Reacting Species, and Thermal and Mass Transfer Gradients. Int. J. Fluid Mech. Therm. Sci. 2023, 9(1), 1-11. doi: 10.11648/j.ijfmts.20230901.11

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    AMA Style

    Okuyade Ighoroje Wilson Ata, Mebine Promise. MHD Double-Diffusive and Viscous Dissipative Boundary Layer Flow over a Vertical Plate with Heat Source, Reacting Species, and Thermal and Mass Transfer Gradients. Int J Fluid Mech Therm Sci. 2023;9(1):1-11. doi: 10.11648/j.ijfmts.20230901.11

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  • @article{10.11648/j.ijfmts.20230901.11,
      author = {Okuyade Ighoroje Wilson Ata and Mebine Promise},
      title = {MHD Double-Diffusive and Viscous Dissipative Boundary Layer Flow over a Vertical Plate with Heat Source, Reacting Species, and Thermal and Mass Transfer Gradients},
      journal = {International Journal of Fluid Mechanics & Thermal Sciences},
      volume = {9},
      number = {1},
      pages = {1-11},
      doi = {10.11648/j.ijfmts.20230901.11},
      url = {https://doi.org/10.11648/j.ijfmts.20230901.11},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijfmts.20230901.11},
      abstract = {Fluid flow problems with convective boundary conditions have applications in the science and engineering worlds. Specifically, they are relevant in the heating and cooling processes observed in glass fiber production, and aerodynamic extrusion. This paper investigates the problem of steady MHD double-diffusive, viscous dissipative boundary layer flow over a vertical plate with heat source, reacting species, and thermal and mass transfer gradients effects. Usually, the problem of flow through porous media is examined using the Boussinesq’s approximations. The governing nonlinear partial differential equations are coupled and complex. Making them tractable, they are linearized into a set of ordinary differential equations using the similarity transform. The evolving set of ordinary differential equations is solved numerically using the fifth-order Runge-Kutta Fehlberg Method and Maple 21 mathematical computational software. The results obtained for the concentration, temperature, and velocity are presented graphically. The analysis of results shows, amongst others, that an increase in the magnetic field parameter increases the temperature and concentration, but decreases the velocity of the fluid; an increase in the Biot number increases the temperature, concentration, and velocity of the fluid; an increases in the concentration difference parameter increases the temperature, but decreases the concentration and velocity of the fluid; an increase in the Eckert number increases the concentration, but decreases the temperature and velocity of the fluid.},
     year = {2023}
    }
    

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  • TY  - JOUR
    T1  - MHD Double-Diffusive and Viscous Dissipative Boundary Layer Flow over a Vertical Plate with Heat Source, Reacting Species, and Thermal and Mass Transfer Gradients
    AU  - Okuyade Ighoroje Wilson Ata
    AU  - Mebine Promise
    Y1  - 2023/06/15
    PY  - 2023
    N1  - https://doi.org/10.11648/j.ijfmts.20230901.11
    DO  - 10.11648/j.ijfmts.20230901.11
    T2  - International Journal of Fluid Mechanics & Thermal Sciences
    JF  - International Journal of Fluid Mechanics & Thermal Sciences
    JO  - International Journal of Fluid Mechanics & Thermal Sciences
    SP  - 1
    EP  - 11
    PB  - Science Publishing Group
    SN  - 2469-8113
    UR  - https://doi.org/10.11648/j.ijfmts.20230901.11
    AB  - Fluid flow problems with convective boundary conditions have applications in the science and engineering worlds. Specifically, they are relevant in the heating and cooling processes observed in glass fiber production, and aerodynamic extrusion. This paper investigates the problem of steady MHD double-diffusive, viscous dissipative boundary layer flow over a vertical plate with heat source, reacting species, and thermal and mass transfer gradients effects. Usually, the problem of flow through porous media is examined using the Boussinesq’s approximations. The governing nonlinear partial differential equations are coupled and complex. Making them tractable, they are linearized into a set of ordinary differential equations using the similarity transform. The evolving set of ordinary differential equations is solved numerically using the fifth-order Runge-Kutta Fehlberg Method and Maple 21 mathematical computational software. The results obtained for the concentration, temperature, and velocity are presented graphically. The analysis of results shows, amongst others, that an increase in the magnetic field parameter increases the temperature and concentration, but decreases the velocity of the fluid; an increase in the Biot number increases the temperature, concentration, and velocity of the fluid; an increases in the concentration difference parameter increases the temperature, but decreases the concentration and velocity of the fluid; an increase in the Eckert number increases the concentration, but decreases the temperature and velocity of the fluid.
    VL  - 9
    IS  - 1
    ER  - 

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Author Information
  • Department of Mathematics/Statistics, Federal Polytechnic of Oil and Gas, Bonny Island, Nigeria

  • Department of Mathematics/Computer Science, Niger Delta University, Wilberforce Island, Nigeria

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