Numerical study of magneto-convective heat and mass transfer from inclined surface with Soret diffusion and heat generation effects: A model for ocean magnetic energy generator fluid dynamics

被引:32
作者
Beg, O. Anwar [1 ]
Beg, T. A. [2 ]
Karim, I [3 ]
Khan, M. S. [3 ]
Alam, M. M. [3 ]
Ferdows, M. [4 ]
Shamshuddin, Md [5 ]
机构
[1] Univ Salford, Mech & Aeronaut Engn, Manchester M5 4WT, Lancs, England
[2] Computat Mech & Renewable Energy Res, Dickenson Rd, Manchester M13, Lancs, England
[3] Khulna Univ, Math Discipline Sci Engn & Technol, Khulna 9208, Bangladesh
[4] Louisiana Tech Univ, Coll Engn & Sci, Ruston, LA 71270 USA
[5] Vaagdevi Coll Engn, Dept Math, Warangal, Telangana, India
关键词
Salinity; Soret number; MHD energy; Nakamura difference scheme; HAM; BOUNDARY-LAYER-FLOW; NATURAL-CONVECTION; MIXED CONVECTION; POROUS-MEDIUM; MHD FLOW; NANOFLUID; SEAWATER; PLATE; FIELD; ABSORPTION;
D O I
10.1016/j.cjph.2019.05.002
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
A mathematical model is developed for steady state magnetohydrodynamic (MHD) heat and mass transfer flow along an inclined surface in an ocean MHD energy generator device with heat generation and thermo-diffusive (Soret) effects. The governing equations are transformed into nonlinear ordinary differential equations with appropriate similarity variables. The emerging two-point boundary value problem is shown to depend on six dimensionless thermophysical parameters - magnetic parameter, Grashof number, Prandtl number, modified Prandtl number, heat source parameter and Sorer number in addition to plate inclination. Numerical solutions are obtained for the nonlinear coupled ordinary differential equations for momentum, energy and salinity (species) conservation, numerically, using the Nachtsheim-Swigert shooting iteration technique in conjunction with the Runge-Kutta sixth order iteration scheme. Validation is achieved with Nakamura's implicit finite difference method. Further verification is obtained via the semi-numerical Homotopy analysis method (HAM). With an increase in magnetic parameter, skin friction is depressed whereas it generally increases with heat source parameter. Salinity magnitudes are significantly reduced with increasing heat source parameter. Temperature gradient is decreased with Prandtl number and salinity gradient (mass transfer rate) is also reduced with modified Prandtl number. Furthermore, the flow is decelerated with increasing plate inclinations and temperature also depressed with increasing thermal Grashof number.
引用
收藏
页码:167 / 179
页数:13
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