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Nonlinear convection in an elasticoviscous fluid-saturated anisotropic porous layer using a local thermal nonequilibrium model

机译:使用局部热非预测模型在弹性流体饱和各向异性多孔层中的非线性对流

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摘要

By adopting a perturbation method and a local thermal nonequilibrium model, nonlinear thermal convection in an anisotropic porous layer saturated by an elasticoviscous fluid is investigated. An elasticoviscous fluid is modeled by a modified Darcy-Oldroyd-B model, and the fluid and solid phase temperatures are represented using a two-field model for the heat transport equation. Anisotropy in permeability and fluid and solid thermal conductivities are considered. A cubic Landau equation is derived separately to study the stability of bifurcating solution of both stationary and oscillatory convection, and the results of linear instability theory are delineated. The boundary between stationary and oscillatory convection is demarcated by identifying codimension-two points in the viscoelastic parameters plane. It is found that the subcritical instability is not possible, and the linear instability analysis itself completely captures the behavior of the onset of convection. Heat transfer is obtained in terms of Nusselt number, and the effect of governing parameters on the same is discussed. The results of the Maxwell fluid are obtained as a particular case from the present study.
机译:通过采用扰动方法和局部热非纤维模型,研究了通过弹性体流体饱和的各向异性多孔层中的非线性热对流。弹性液体由改进的达西族 - 博伊奥德-B型号建模,并且使用用于热传输方程的双场模型来表示流体和固相温度。考虑了渗透性和流体的各向异性和固体导热性。分别推导出立方体地区等式,以研究静止和振荡对流的分叉解决方案的稳定性,以及线性不稳定理论的结果划定。通过识别粘弹性参数平面中的分型两点来划分静止和振荡对流之间的边界。发现不可能的亚临界不稳定性,并且线性不稳定分析本身完全捕捉到对流开始的行为。讨论了在篮区的数量方面获得了传热,并且讨论了控制参数的影响。从本研究中获得麦克斯韦流体的结果。

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