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Multiple slip and variable transport property effects on magnetohydromagnetic dissipative thermo-solutal convection in porous media

机译:多孔介质中磁氢磁耗散热固对流的多重滑动和可变输运性质影响

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摘要

A mathematical study is presented to investigate the influence of variable transport properties and momentum, thermal and mass slip on magnetohydrodynamic (MHD)\udmomentum, heat and mass transfer in a porous media. Slip effects are simulated via careful imposition of boundary conditions at the wall. Joule heating and viscous\uddissipation are also studied. The governing partial differential boundary layer equations are analyzed using Lie group theory and rendered with appropriate transformations into a system of nonlinear, coupled ordinary differential equations. The multi-physical boundary value problem is dictated by twelve thermophysical parameters- concentration diffusivity\udparameter (Dc), Hartmann magnetic number (M), permeability parameter (omaga), Eckert number (Ec), momentum slip (a), thermal slip (b), mass (species) slip (d), Prandtl number (Pr), Schmidt number (Sc), power law index for non-isothermal and non-iso-solutal\udeffects (m), viscosity variation parameter (A) and thermal conductivity variation parameter (S). A numerical solution is obtained for the effects of selected parameters on transport characteristics using the robust Runge-Kutta-Fehlberg fourth-fifth order numerical quadrature method in Maple16. Excellent correlation is achieved between the present computational results and for the constant transport properties (A=S=Dc=0), nonporous (omega=0), non-thermal slip (b=0), non-solutal slip (d = 0) and non-dissipative solutions without Joule heating (Ec= 0) of Yazdi et al. [35]. Increasing momentum slip enhances temperatures whereas increasing thermal slip reduces them. An increase in thermal conductivity boosts temperatures whereas greater viscosity reduces temperatures. Increasing magnetic parameter suppresses velocity and increasing permeability parameter\udelevates temperatures. Species concentration is enhanced with increasing concentration diffusivity and permeability parameter but depressed with increasing viscosity. Furthermore concentration is enhanced with momentum slip but reduced with mass slip parameter. Moreover increasing magnetic field is observed to aid species diffusion in the regime. The present study finds applications in trickle-bed reactor hydromagnetics,\udmagnetic polymeric materials processing and MHD energy generator slip flows.
机译:进行了数学研究,以研究可变传输特性和动量,热和质量滑动对多孔介质中磁流体动力学(MHD)\动量,传热和传质的影响。滑移效果是通过在墙处仔细施加边界条件来模拟的。还研究了焦耳加热和粘性\扩散。使用李群理论分析支配的偏微分边界层方程,并将其适当转换为非线性耦合的常微分方程系统。多物理边界值问题由12个热物理参数决定-浓度扩散率\超参数(Dc),哈特曼磁数(M),磁导率参数(omaga),埃克特数(Ec),动量滑移(a),热滑移( b),质量(种类)滑移(d),普朗特数(Pr),施密特数(Sc),非等温和非等溶\屈服力的幂律指数(m),粘度变化参数(A)和导热系数变化参数(S)。使用Maple16中鲁棒的Runge-Kutta-Fehlberg四阶五阶数值正交方法,获得了针对所选参数对传输特性影响的数值解。在当前的计算结果与恒定的传输特性(A = S = Dc = 0),无孔(ω= 0),非热滑移(b = 0),非绝对滑移(d = 0)之间实现了极好的相关性)和Yazdi等人的无焦耳加热(Ec = 0)的非耗散溶液。 [35]。动量滑动增加会提高温度,而热滑动增加会降低温度。导热系数的增加会提高温度,而更大的粘度会降低温度。磁参数的增加会抑制速度,磁导率参数的增加会降低温度。物种浓度随着浓度扩散系数和渗透率参数的增加而增强,但随着粘度的增加而降低。此外,动量滑移会提高集中度,而质量滑移参数会降低集中度。此外,观察到增加的磁场有助于该状态下的物质扩散。本研究发现在滴流床反应堆的水磁学,\ udmagnetic聚合材料处理和MHD能量发生器滑流中的应用。

著录项

  • 作者

    Uddin, MJ; Beg, A; Uddin, MN;

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  • 年度 2016
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  • 正文语种 en
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