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首页> 外文期刊>Journal of Electromagnetic Analysis and Applications >Effect of Exponentially Temperature-Dependent Viscosity on the Onset of Penetrative Ferro-Thermal-Convection in a Saturated Porous Layer via Internal Heating
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Effect of Exponentially Temperature-Dependent Viscosity on the Onset of Penetrative Ferro-Thermal-Convection in a Saturated Porous Layer via Internal Heating

机译:指数温度依赖性粘度对内部加热作用下饱和多孔层中穿透性铁热对流发生的影响

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The effect of viscosity depending exponentially on temperature on the onset of penetrative ferro-thermal-convection (FTC) in a saturated horizontal porous layer in the presence of vertical magnetic field is investigated. The bounding surface of the ferrofluid layer is considered to be rigid-rigid and insulated to temperature perturbations. The resulting eigenvalue problem is solved numerically using the Galerkin technique and also analytically by a regular perturbation technique with wave number as a perturbation parameter. The analytical and numerical results are found to be concurrence. The characteristics of stability of the system are strongly dependent on the viscosity parameter B . The effect of B on the onset of ferroconvection in a porous layer is dual in nature depending on the choices of physical parameters and a sublayer starts to form at higher values of B . Whereas, increase in magnetic number M _(1) and the Darcy number Da is to advance the onset of ferroconvection in a porous layer. The nonlinearity of fluid magnetization M _(3?)is found to have no influence on the onset of ferroconvection.
机译:研究了在垂直磁场存在下,饱和温度水平多孔层中渗透率随温度成指数变化对渗透性铁热对流(FTC)的影响。铁磁流体层的边界表面被认为是刚性的并且绝缘于温度扰动。由此产生的特征值问题使用伽勒金(Galerkin)技术进行了数值求解,并且还通过以波数作为扰动参数的常规扰动技术进行了解析。发现分析和数值结果是一致的。系统的稳定性特征在很大程度上取决于粘度参数B。 B对多孔层中铁对流开始的影响本质上是双重的,具体取决于物理参数的选择,并且在较高的B值下开始形成子层。然而,磁数M _(1)和达西数Da的增加是为了促进多孔层中铁对流的开始。发现流体磁化强度的非线性M _(3?)对铁对流的开始没有影响。

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