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International Journal of Fluid Mechanics Research

Published 6 issues per year

ISSN Print: 2152-5102

ISSN Online: 2152-5110

The Impact Factor measures the average number of citations received in a particular year by papers published in the journal during the two preceding years. 2017 Journal Citation Reports (Clarivate Analytics, 2018) IF: 1.1 To calculate the five year Impact Factor, citations are counted in 2017 to the previous five years and divided by the source items published in the previous five years. 2017 Journal Citation Reports (Clarivate Analytics, 2018) 5-Year IF: 1.3 The Eigenfactor score, developed by Jevin West and Carl Bergstrom at the University of Washington, is a rating of the total importance of a scientific journal. Journals are rated according to the number of incoming citations, with citations from highly ranked journals weighted to make a larger contribution to the eigenfactor than those from poorly ranked journals. Eigenfactor: 0.0002 The Journal Citation Indicator (JCI) is a single measurement of the field-normalized citation impact of journals in the Web of Science Core Collection across disciplines. The key words here are that the metric is normalized and cross-disciplinary. JCI: 0.33 SJR: 0.256 SNIP: 0.49 CiteScore™:: 2.4 H-Index: 23

Indexed in

Marangoni Convection in a Composite Porous Layer and a Fluid Layer with a Deformable Free Surface

Volume 34, Issue 4, 2007, pp. 352-373
DOI: 10.1615/InterJFluidMechRes.v34.i4.40
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ABSTRACT

The linear stability analysis of Marangoni convection in a composite system comprised of an incompressible fluid-saturated porous layer underlying a layer of the same fluid is considered. The upper fluid surface, free to the atmosphere, is considered to be deformable and subjected to temperature-dependent surface tension. The fluid flow in the porous layer is governed by the Forchheimer-extended-Darcy equation, and both Beavers-Joseph and Jones conditions are employed at the interface between the two layers. The resulting eigenvalue problem is solved exactly and also by the regular perturbation technique when the boundaries of the system are insulated to temperature perturbations. The effect of the crispation number, Bond number, and the other physical parameters involved therein are analyzed for the stability of the system. It is found that a decrease in the crispation number and an increase in the Bond number delay the onset of convection. Also, the effect of the ratio of the fluid to the porous layer thickness along with the other physical parameters on the control (suppress or augment) of convection is analyzed in detail.

CITED BY
  1. Shivakumara I.S., Lee Jinho, Chavaraddi Krishna B., Onset of surface tension driven convection in a fluid layer overlying a layer of an anisotropic porous medium, International Journal of Heat and Mass Transfer, 54, 4, 2011. Crossref

  2. Suma S. P., Gangadharaiah Y. H., Indira R., Shivakumara I. S., Throughflow Effects on Penetrative Convection in Superposed Fluid and Porous Layers, Transport in Porous Media, 95, 1, 2012. Crossref

  3. Shivakumara I. S., Suma S. P., Indira R., Gangadharaiah Y. H., Effect of Internal Heat Generation on the Onset of Marangoni Convection in a Fluid Layer Overlying a Layer of an Anisotropic Porous Medium, Transport in Porous Media, 92, 3, 2012. Crossref

  4. Nield Donald A., Bejan Adrian, Internal Natural Convection: Heating from Below, in Convection in Porous Media, 2017. Crossref

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