Please use this identifier to cite or link to this item: http://gukir.inflibnet.ac.in:8080/jspui/handle/123456789/4360
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dc.contributor.authorGaikwad S.N
dc.contributor.authorDhanraj M.
dc.date.accessioned2020-06-12T15:03:40Z-
dc.date.available2020-06-12T15:03:40Z-
dc.date.issued2013
dc.identifier.citationSpecial Topics and Reviews in Porous Media , Vol. 4 , 4 , p. 359 - 374en_US
dc.identifier.uri10.1615/SpecialTopicsRevPorousMedia.v4.i4.70
dc.identifier.urihttp://gukir.inflibnet.ac.in:8080/jspui/handle/123456789/4360-
dc.description.abstractThe onset of double diffusive convection in a Maxwell fluid saturated anisotropic porous layer with internal heat source is studied using both linear and weak nonlinear stability analyses. The linear theory is being related to the normal mode method. The modified Darcy-Maxwell model is used for the momentum equation. The effects of various parameters on the stationary, oscillatory, and finite amplitude convection is shown graphically. It is found that the effects of the internal Rayleigh number, mechanical anisotropy parameter, and relaxation parameter have a destabilizing effect, while the thermal anisotropy parameter has a stabilizing effect on the stationary, oscillatory, and finite amplitude convection. A weak nonlinear stability analysis is based on truncated representation of Fourier series method and is employed to find the Nusselt number and Sherwood number. Further, the transient behavior of the Nusselt and Sherwood numbers is obtained by solving the finite amplitude equations using a numerical method. © 2013 by Begell House, Inc.en_US
dc.subjectAnisotropy
dc.subjectDouble diffusive convection
dc.subjectHeat mass transfer
dc.subjectInternal Rayleigh number
dc.subjectMaxwell fluid
dc.subjectPorous layer
dc.titleOnset of double diffusive convection in a maxwell fluid saturated anisotropic porous layer with internal heat sourceen_US
dc.typeArticle
Appears in Collections:1. Journal Articles

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