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International Journal of Fluid Mechanics Research

Publicado 6 números por año

ISSN Imprimir: 2152-5102

ISSN En Línea: 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

Velocity Characteristics of Turbulent Natural Convection in Convergent-Plates Vertical Channels

Volumen 29, Edición 2, 2002, 21 pages
DOI: 10.1615/InterJFluidMechRes.v29.i2.30
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SINOPSIS

Velocity measurements of natural convection in symmetrically and asymmetrically heated convergent-plates vertical channels are presented. In the first case, symmetrical flow, the two channel plates were both kept at a constant temperature higher than the ambient. In the second case, asymmetrical flow, one plate was kept at a temperature higher than ambient temperature while the other plate was kept at a temperature lower than the ambient temperature. The velocity measurements were performed using a Laser Doppler Anemometer. In the case of symmetrical flow, the results indicate a zero velocity region located at the center of the channel close to its exit. In the case of asymmetrical flow, the results show that the flow accelerates by the hot side and decelerates by the cold plate. The results also indicate that cooling one of the two plates below ambient influences the flow pattern significantly and results in the formation of a large vortex at the center of the channel.

CITADO POR
  1. Ayinde Taofeek F., Said Syed A. M., Habib Mohammed A., Turbulent natural convection flow in a vertical channel with anti-symmetric heating, Heat and Mass Transfer, 44, 10, 2008. Crossref

  2. Ayinde T.F., Experimental investigation of turbulent natural convection flow in a converging channel, Experimental Thermal and Fluid Science, 32, 6, 2008. Crossref

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