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首页> 外文期刊>Journal of geophysics and engineering >Onset of Darcy-Brinkman double-diffusive convection in a magnetized ferrofluid layer using a thermal non-equilibrium model: A nonlinear stability analysis
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Onset of Darcy-Brinkman double-diffusive convection in a magnetized ferrofluid layer using a thermal non-equilibrium model: A nonlinear stability analysis

机译:使用热非平衡模型在磁化铁磁流体层中达西-布林克曼双扩散对流的爆发:非线性稳定性分析

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This paper presents a nonlinear stability analysis of a double-diffusive convection in a magnetized ferrofluid layer confined between stress-free boundaries using a thermal non-equilibrium model by the energy method. A Darcy-Brinkman model is used for the momentum equation and a two-field model is used for the energy equation, each representing the solid and fluid phases separately. The mathematical emphasis is on how to control the nonlinear terms caused by magnetic body and inertia forces. The effects of the interface heat transfer coefficient (H), magnetic parameter (M_3), Darcy-Brinkman number (D?a) and porosity-modified conductivity ratio (γ') on the onset of ferroconvection in the presence of solute (S') have been analysed. For all the cases studied, it is found that solute gradient enhances the stability of the system. A comparison with linear instability theory shows that there is a difference between the critical Rayleigh numbers and thus indicates the possibility of the existence of a subcritical instability region for ferrofluids. However, for non-ferrofluids stability and instability boundaries coincide.
机译:本文利用能量方法通过热非平衡模型,对无应力边界之内的磁化铁磁流体层中的双扩散对流进行了非线性稳定性分析。动量方程式使用Darcy-Brinkman模型,能量方程式使用两场模型,每个模型分别表示固相和液相。数学上的重点是如何控制由磁体和惯性力引起的非线性项。在溶质存在的情况下,界面传热系数(H),磁参数(M_3),达西-布林克曼数(DΔa)和孔隙率修正的电导率(γ')对铁对流开始的影响)进行了分析。对于所有研究的情况,发现溶质梯度增强了系统的稳定性。与线性不稳定性理论的比较表明,临界瑞利数之间存在差异,因此表明存在铁磁流体亚临界不稳定性区域的可能性。但是,对于非铁磁流体,稳定性和不稳定边界是重合的。

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