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Hydromagnetic Stability of Metallic Nanofluids (Cu-Water and Ag-Water) Using Darcy-Brinkman Model

机译:达西 - Brinkman模型中金属纳米流体(Cu水和Ag水)的水质稳定性

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摘要

Thermal convection of a nanofluid layer in the presence of imposed vertical magnetic field saturated by a porous medium is investigated for both-free, rigid-free, and both-rigid boundaries using Darcy-Brinkman model. The effects of Brownian motion and thermophoretic forces due to the presence of nanoparticles and Lorentz’s force term due to the presence of magnetic field have been considered in the momentum equations along with Maxwell’s equations. Keeping in mind applications of flow through porous medium in geophysics, especially in the study of Earth’s core, and the presence of nanoparticles therein, the hydromagnetic stability of a nanofluid layer in porous medium is considered in the present formulation. An analytical investigation is made by applying normal mode technique and Galerkin type weighted residuals method and the stability of Cu-water and Ag-water nanofluids is compared. Mode of heat transfer is through stationary convection without the occurrence of oscillatory motions. Stability of the system gets improved appreciably by raising the Chandrasekhar number as well as Darcy number whereas increase in porosity hastens the onset of instability. Further, stability of the system gets enhanced as we proceed from both-free boundaries to rigid-free and to both-rigid boundaries.
机译:使用Darcy-Brinkman模型研究无阳性介质饱和的施加垂直磁场存在的纳米流体层的热对流。在Maxwell等式中,在动量方程中考虑了由于纳米颗粒的存在和Lorentz的力期由于纳米颗粒和Lorentz的力项的影响。通过在地球物理中的多孔培养基中,尤其是在地球核的研究中,以及其中纳米颗粒的存在,在本发明的制剂中考虑了多孔介质中纳米颗粒的含氢稳定性。通过应用正常模式技术和Galerkin型加权残留方法进行分析研究,比较Cu水和Ag水纳米流体的稳定性。传热模式通过静止对流而不会发生振荡运动。通过提高Chandrasekhar数以及达西数,系统的稳定性得到了显着改善,而磁性数量升高,则升压不稳定性。此外,当我们从无双界和无刚性边界进行刚性和刚性边界时,系统的稳定性得到增强。

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