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首页> 外文期刊>Magnetohydrodynamics >THERMAL CONVECTIVE INSTABILITY IN A MICROPOLAR FERROMAGNETIC FLUID SATURATED POROUS LAYER HEATED FROM BELOW
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THERMAL CONVECTIVE INSTABILITY IN A MICROPOLAR FERROMAGNETIC FLUID SATURATED POROUS LAYER HEATED FROM BELOW

机译:从下面加热的微极铁磁流体饱和多孔层中的热对流不稳定性

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The onset of ferromagnetic convection in a micropolar ferromagnetic fluid saturated porous layer heated from below in the presence of a uniform applied vertical magnetic field has been investigated. The rigid-isothermal boundaries of the fluid layer are considered to be ferromagnetic and the eigenvalue problem is solved numerically using the Galerkin method. It is noted that the paramagnetic boundaries with large magnetic susceptibility χ mainly delay the onset of ferromagnetic convection if compared to a very low magnetic susceptibility as well as to ferromagnetic boundaries. The increase in value of the magnetic parameter M_1 and spin diffusion (couple stress) parameter N_3 is to hasten, while the increase in value of the coupling parameter N_1 and micropolar heat conduction parameter N_5 is to delay the onset of ferromagnetic convection.
机译:已经研究了在均匀施加垂直磁场的情况下从下方加热的微极性铁磁流体饱和多孔层中铁磁对流的发生。流体层的刚性-等温边界被认为是铁磁性的,并且使用Galerkin方法以数值方式解决了特征值问题。注意,与非常低的磁化率以及铁磁边界相比,具有大磁化率χ的顺磁边界主要延迟了铁磁对流的发生。磁性参数M_1和自旋扩散(耦合应力)参数N_3的值的增加将被加快,而耦合参数N_1和微极性导热参数N_5的值的增加将延迟铁磁对流的开始。

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