computational software program mathematica 10 (Wolfram Research)
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computational software program mathematica 10
Computational Software Program Mathematica 10, supplied by Wolfram Research, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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Average 90 stars, based on 1 article reviews
Computational Software Program Mathematica 10, supplied by Wolfram Research, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/computational+software+program+mathematica+10/computational+software+program+mathematica+10/10__1063_slash_1__4939287-90-13-18
Average 90 stars, based on 1 article reviews
computational software program mathematica 10 - by Bioz Stars,
2026-09
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Software:Article Title: Instability of stationary two-dimensional mixed convection across a vertical porous layer Article Snippet: Instability of stationary two-dimensional mixed convection across a vertical porous layer Antonio Barletta Citation: Physics of Fluids 28, 014101 (2016); doi: 10.1063/1.4939287 View online: http://dx.doi.org/10.1063/1.4939287 View Table of Contents: http://aip.scitation.org/toc/phf/28/1 Published by the American Institute of Physics Instability of stationary two-dimensional mixed convection across a vertical porous layer Antonio Barlettaa) Department of Industrial Engineering, Alma Mater Studiorum Università di Bologna, Viale Risorgimento 2, 40136 Bologna, Italy (Received 17 August 2015; accepted 17 December 2015; published online 8 January 2016) The two-dimensional and stationary mixed convection in a vertical porous layer is studied.. This mixed convection flow is caused by the pressure and temperature difference between the parallel boundaries of the porous layer.. In the limiting case where the boundary pressure difference is zero, the two-dimensional flow actually becomes the one-dimensional conduction regime of natural convection. |