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国际流体力学研究期刊

每年出版 6 

ISSN 打印: 2152-5102

ISSN 在线: 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

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Numerical Modelling of Darcy - Brinkman - Forchheimer Magnetohydrodynamic Mixed Convection Flow in a Porous Medium with Transpiration and Viscous Heating

卷 29, 册 1, 2002, 26 pages
DOI: 10.1615/InterJFluidMechRes.v29.i1.10
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摘要

A mathematical model is presented to investigate the combined effects of buoyancy, porous inertial drag, boundary vorticity diffusion (Brinkman friction), transverse magnetic field, viscous dissipation, wall transpiration, thermal conductivity and various other thermofluid parameters on the convection boundary layer flow of an electrically-conducting fluid past a vertical permeable semi-infinite plate in a saturated porous medium. The transformed boundary layer equations are solved numerically on a x-h domain using the robust Keller-box finite difference method and a powerful double-shooting Runge-Kutta method (DSRK). Results are presented graphically for the local skin-friction function (surface shear stress parameter) and the local Nusselt number function (local heat transfer parameter) for a wide range of the pertinent physical parameters. For the special case of x = 0 (at the leading edge), plots are given to compare the computations by both numerical methods and found to be in excellent agreement.

对本文的引用
  1. Bég O. A., Zueco J., Bég T. A., Takhar H. S., Kahya E., NSM analysis of time-dependent nonlinear buoyancy-driven double-diffusive radiative convection flow in non-Darcy geological porous media, Acta Mechanica, 202, 1-4, 2009. Crossref

  2. Khademi Ramin, Razminia Abolhassan, Shiryaev Vladimir I., Conjugate-mixed convection of nanofluid flow over an inclined flat plate in porous media, Applied Mathematics and Computation, 366, 2020. Crossref

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