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International Journal of Fluid Mechanics Research

Erscheint 6 Ausgaben pro Jahr

ISSN Druckformat: 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

Effect of Gravity Modulation on the Onset of Thermal Convection in Rotating Viscoelastic Fluid and Porous Layer

Volumen 39, Ausgabe 6, 2012, pp. 535-557
DOI: 10.1615/InterJFluidMechRes.v39.i6.50
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ABSTRAKT

The combined effect of gravity modulation and rotation on the onset of thermal convection in a viscoelastic horizontal fluid layer and a fluid-saturated porous layer is studied analytically using linear stability theory. The regular perturbation method based on small amplitude of modulation is employed to compute the critical value of Rayleigh number and wavenumber. The correction critical Rayleigh number is calculated as a function of Deborah number, Taylor number, Prandtl number, Darcy number, frequency of the modulation and normalized porosity. It is shown that in general the gravity modulation produces a stabilizing effect in case of viscous fluid and Darcy porous layer and both destabilizing and stabilizing effects in case of Brinkman porous layer. It is shown that the onset of convection can be advanced or delayed by proper tuning of various governing parameters.

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

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