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Onset of convection in a couple-stress fluid-saturated porous medium: effects of non-uniform temperature gradients

机译:偶应力流体饱和多孔介质中对流的开始:温度梯度不均匀的影响

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摘要

Onset of convection in a layer of couple-stress fluid-saturated porous medium is investigated for different types of basic temperature gradients. The boundaries are considered to be adiabatically insulated to temperature perturbations. The eigenvalue equations of the perturbed state obtained from the normal mode analysis are solved analytically using a regular perturbation technique with wave number as a perturbation parameter and also numerically using the Galerkin technique. The critical stability parameters obtained from these two techniques are in excellent agreement and an increase in the value of couple-stress parameter is found to delay the onset of convection. The results also indicate that the piecewise linear temperature profile hastens the onset of convection when compared to linear, parabolic, and inverted parabolic temperature profiles. In addition, the influence of thermal depth on the critical conditions is assessed in the case of piecewise linear temperature profiles, and it is observed that the critical thermal depth decreases marginally with an increase in the couple-stress parameter.
机译:针对不同类型的基本温度梯度,研究了耦合应力流体饱和多孔介质层中对流的开始。该边界被认为是绝热地与温度扰动隔离的。从正常模式分析中获得的摄动状态的特征值方程式,是使用常规的摄动技术(以波数作为摄动参数)解析地求解的,还使用了Galerkin技术进行了数值求解。从这两种技术获得的临界稳定性参数非常一致,并且发现耦合应力参数值的增加会延迟对流的发生。结果还表明,与线性,抛物线和倒抛物线温度曲线相比,分段线性温度曲线会加快对流的发生。另外,在分段线性温度曲线的情况下,评估了热深度对临界条件的影响,并且观察到,随着耦合应力参数的增加,临界热深度略有下降。

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