Comment on "Convection in a horizontal fluid layer under an inclined temperature gradient" [Phys. Fluids 23, 084107 (2011)]
Albert Sharifulin

TL;DR
This paper comments on a previous study of convection in a fluid layer under an inclined temperature gradient, highlighting that the equations used are well-established and have been extensively studied both theoretically and experimentally for over fifty years.
Contribution
The paper clarifies that the equations analyzed in the referenced study are not new, as they are well-known and have been thoroughly investigated historically.
Findings
The equations of flow are classical and well-studied.
Previous work has provided exact solutions over fifty years ago.
The study emphasizes the importance of recognizing established theoretical foundations.
Abstract
Ortiz-P\'erez and D\'avalos investigated the stability of parallel convective flow. From the article it seems that this equations of flow obtained by the authors. Meanwhile, it is well studied theoretically and experimentally(exact solution obtained more than half a century ago.
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Taxonomy
TopicsFluid Dynamics and Turbulent Flows · Nanofluid Flow and Heat Transfer · Rheology and Fluid Dynamics Studies
