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Effect of Suspended Particles on Couple-Stress Fluid Heated and Soluted from Below in Porous Medium

卷 7, 册 1, 2004, 10 pages
DOI: 10.1615/JPorMedia.v7.i1.20
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摘要

A layer of a couple-stress fluid permeated with suspended particles, heated and soluted from below in a porous medium, is considered. For the case of stationary convection, the stable solute gradient and couple-stress have stabilizing effects on the onset of convection, whereas the suspended particles and medium permeability have destabilizing effects on the couple-stress fluid permeated with suspended particles, heated and soluted from below in a porous medium. Graphs have been plotted by giving numerical values to the parameters, to depict the stability characteristics. The stable solute gradient is found to introduce oscillatory modes in the system, which were nonexistent in its absence. A sufficient condition for the nonexistence of overstability is obtained.

对本文的引用
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  2. Sunil , Sharma Anupama, Kumar Pardeep, Gupta Urvashi, The effect of magnetic-field-dependent viscosity and rotation on ferrothermohaline convection saturating a porous medium in the presence of dust particles, Journal of Geophysics and Engineering, 2, 3, 2005. Crossref

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  9. Sunil , Chand Prakash, Mahajan Amit, EFFECT OF SUSPENDED PARTICLES ON MARGINAL STABILITY OF A DOUBLE-DIFFUSIVE MAGNETIZED FERROFLUID WITH INTERNAL ANGULAR MOMENTUM, Chemical Engineering Communications, 197, 12, 2010. Crossref

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