In this paper, investigate a two dimensional unsteady Magneto hydro dynamics (MHD) free convection flow of viscous incompressible and electrically conducting fluid flow past an vertical plate in the presence of Grashof Number, Modified Grashof Number, Prandtl Number, Schamidt Number as well as Dufour effects. The governing equations of the problem contain a system of non-linear partial differential equations; have been transformed into a set of coupled non-linear ordinary differential equations which is solved numerically by applying well known explicit finite difference method. The Finite-difference method is an enormously used technique to investigate of the general non linear partial differential equation. Partial differential equations occur in many branches of applied mathematics for example, in hydrodynamics, elasticity, quantum mechanics. Hence, the proposed study is to investigate the numerical results which are performed for various physical parameters such as velocity profiles, temperature distribution and concentration profiles within the boundary layer are separately discussed in graphically.
Published in | International Journal of Applied Mathematics and Theoretical Physics (Volume 4, Issue 1) |
DOI | 10.11648/j.ijamtp.20180401.13 |
Page(s) | 15-26 |
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), 2018. Published by Science Publishing Group |
MHD, Non-Linear PDE, Rotating System, Mass and Heat Transfer, Explicit Finite Difference Method
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APA Style
Ronju Khatun, Mohammad Roknujjaman, Mohammad Abdul Al Mohit. (2018). Numerical Investigation on Magnetohydrodynamics (MHD) Free Convection Fluid Flow over a Vertical Porous Plate with induced Magnetic Field. International Journal of Applied Mathematics and Theoretical Physics, 4(1), 15-26. https://doi.org/10.11648/j.ijamtp.20180401.13
ACS Style
Ronju Khatun; Mohammad Roknujjaman; Mohammad Abdul Al Mohit. Numerical Investigation on Magnetohydrodynamics (MHD) Free Convection Fluid Flow over a Vertical Porous Plate with induced Magnetic Field. Int. J. Appl. Math. Theor. Phys. 2018, 4(1), 15-26. doi: 10.11648/j.ijamtp.20180401.13
AMA Style
Ronju Khatun, Mohammad Roknujjaman, Mohammad Abdul Al Mohit. Numerical Investigation on Magnetohydrodynamics (MHD) Free Convection Fluid Flow over a Vertical Porous Plate with induced Magnetic Field. Int J Appl Math Theor Phys. 2018;4(1):15-26. doi: 10.11648/j.ijamtp.20180401.13
@article{10.11648/j.ijamtp.20180401.13, author = {Ronju Khatun and Mohammad Roknujjaman and Mohammad Abdul Al Mohit}, title = {Numerical Investigation on Magnetohydrodynamics (MHD) Free Convection Fluid Flow over a Vertical Porous Plate with induced Magnetic Field}, journal = {International Journal of Applied Mathematics and Theoretical Physics}, volume = {4}, number = {1}, pages = {15-26}, doi = {10.11648/j.ijamtp.20180401.13}, url = {https://doi.org/10.11648/j.ijamtp.20180401.13}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijamtp.20180401.13}, abstract = {In this paper, investigate a two dimensional unsteady Magneto hydro dynamics (MHD) free convection flow of viscous incompressible and electrically conducting fluid flow past an vertical plate in the presence of Grashof Number, Modified Grashof Number, Prandtl Number, Schamidt Number as well as Dufour effects. The governing equations of the problem contain a system of non-linear partial differential equations; have been transformed into a set of coupled non-linear ordinary differential equations which is solved numerically by applying well known explicit finite difference method. The Finite-difference method is an enormously used technique to investigate of the general non linear partial differential equation. Partial differential equations occur in many branches of applied mathematics for example, in hydrodynamics, elasticity, quantum mechanics. Hence, the proposed study is to investigate the numerical results which are performed for various physical parameters such as velocity profiles, temperature distribution and concentration profiles within the boundary layer are separately discussed in graphically.}, year = {2018} }
TY - JOUR T1 - Numerical Investigation on Magnetohydrodynamics (MHD) Free Convection Fluid Flow over a Vertical Porous Plate with induced Magnetic Field AU - Ronju Khatun AU - Mohammad Roknujjaman AU - Mohammad Abdul Al Mohit Y1 - 2018/05/10 PY - 2018 N1 - https://doi.org/10.11648/j.ijamtp.20180401.13 DO - 10.11648/j.ijamtp.20180401.13 T2 - International Journal of Applied Mathematics and Theoretical Physics JF - International Journal of Applied Mathematics and Theoretical Physics JO - International Journal of Applied Mathematics and Theoretical Physics SP - 15 EP - 26 PB - Science Publishing Group SN - 2575-5927 UR - https://doi.org/10.11648/j.ijamtp.20180401.13 AB - In this paper, investigate a two dimensional unsteady Magneto hydro dynamics (MHD) free convection flow of viscous incompressible and electrically conducting fluid flow past an vertical plate in the presence of Grashof Number, Modified Grashof Number, Prandtl Number, Schamidt Number as well as Dufour effects. The governing equations of the problem contain a system of non-linear partial differential equations; have been transformed into a set of coupled non-linear ordinary differential equations which is solved numerically by applying well known explicit finite difference method. The Finite-difference method is an enormously used technique to investigate of the general non linear partial differential equation. Partial differential equations occur in many branches of applied mathematics for example, in hydrodynamics, elasticity, quantum mechanics. Hence, the proposed study is to investigate the numerical results which are performed for various physical parameters such as velocity profiles, temperature distribution and concentration profiles within the boundary layer are separately discussed in graphically. VL - 4 IS - 1 ER -