2017
DOI: 10.1063/1.5008689
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Thermosolutal instability of Rivlin-Ericksen fluid under the effect of suspended particles and compressibility in porous medium

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Cited by 3 publications
(6 citation statements)
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“…When the instability sets in as stationary convection, the marginal state will be characterized by . Putting , the dispersion relation (26) where ̅ and denote respectively the critical Rayleigh numbers in the presence and absence of compressibility.…”
Section: The Stationary Convectionmentioning
confidence: 99%
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“…When the instability sets in as stationary convection, the marginal state will be characterized by . Putting , the dispersion relation (26) where ̅ and denote respectively the critical Rayleigh numbers in the presence and absence of compressibility.…”
Section: The Stationary Convectionmentioning
confidence: 99%
“…Proof: For overstability, we wish to determine the critical Rayleigh number for the onset of instability via a state of pure oscillations, it is suffice to find conditions for which equation (26) will admit of solutions with real.…”
Section: Theoremmentioning
confidence: 99%
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“…In a different piece of research, Kumar et al (2005) investigated the MHD instability of rotating superposed Rivlin-Ericksen viscoelastic fluids that were traveling over porous surfaces. In the research that Aggarwal & Dixit (2017), they investigated the thermosolutal instability of a layer of elasticoviscous fluid in a porous media that included suspended particles. This instability was caused by the effect of compressibility.…”
Section: Introductionmentioning
confidence: 99%
“…The convection problem when the fluid layer is heated and soluted from below is studied by Veronis [2] and Nield [3]. The instability of non-Newtonian fluids has been studied by several authors [4][5][6][7][8][9][10][11][12][13][14][15] and [16,17,18,19,20,21]. There are so many problems in engineering, oceanography and limnology which can be studied by double diffusive convection.…”
Section: Introductionmentioning
confidence: 99%