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Natural convection in a cavity filled with porous medium under the effect of a partial magnetic field

机译:腔内的自然对流填充有多孔介质的部分磁场的效果

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Natural convection flow in presence of partially applied magnetic field in a porous medium is investigated in this study. Partial magnetic field is applied horizontally in the direction of positive x-axis, and vertical walls of unit square cavity are differentially heated. Fluid flow in the porous medium is modelled by Brinkman-Forchheimer-extended Darcy equation of motion. Pseudo spectral method based on polyharmonic spline radial basis function f = r(7) is numerically performed for discretization of space derivatives and backward Euler method is carried out for time derivatives in governing dimensionless equations. The variation of the length of the partial magnetic field, Hartmann number, Rayleigh number, Darcy number and the location of the center of the partial magnetic field is presented in terms of streamlines, isotherms and vorticity contours. Central vortex in streamlines is pushed as the length of partial magnetic field increases in case of a top centered applied partial magnetic field. Convective heat transfer is suppressed if middle centered magnetic field is applied partially. Partial magnetic field may control fluid flow and heat transfer at required parts of the cavity.
机译:在该研究中研究了多孔介质中部分施加的磁场存在的自然对流流。部分磁场在正x轴的方向上水平施加,并且单位方形腔的垂直壁被差别加热。多孔介质中的流体流动由Brinkman-Forchheimer - 延伸的达西运动方程建模。基于多球样条型径向基函数F = R(7)的伪光谱法在数值上进行了空间衍生物的离散化,并对控制无量纲方程的时间衍生物进行后向欧拉方法。在流线,等温线和涡旋轮廓方面,提出了部分磁场,Hartmann号,瑞利数,达西数和部分磁场中心的位置的变化。随着在顶部占用的施加部分磁场的情况下,部分磁场的长度随着部分磁场的长度而增加,在流动线上被推为推动中央涡流。如果部分地施加了中央磁场,则抑制了对流传热。部分磁场可以控制腔的所需部件的流体流动和热传递。

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