期刊
PHYSICS
卷 5, 期 1, 页码 298-309出版社
MDPI
DOI: 10.3390/physics5010022
关键词
thermal convection; buoyancy force; variable density; porous media
The Oberbeck-Boussinesq approximation is commonly used for studying natural or mixed convection flows. However, misunderstandings of this approximation can lead to paradoxes or incorrect conclusions. This paper briefly reviews the basic features of the Oberbeck-Boussinesq approximation and provides three simple examples where it can be misused. These misuses result in erroneous conclusions and violations of mass conservation. The paper also discusses the Oberbeck-Boussinesq approximation as an asymptotic theory obtained by letting the product of the thermal expansion coefficient and the reference temperature difference tend to zero.
The Oberbeck-Boussinesq approximation is the most commonly employed theoretical scheme for the study of natural or mixed convection flows. However, the misunderstanding of this approximated framework is a possibility that may cause the emergence of paradoxes or, at least, incorrect conclusions. In this paper, the basic features of the Oberbeck-Boussinesq approximation are briefly recalled and three simple examples where this theoretical scheme may be misused are provided. Such misuses of the approximation lead to erroneous conclusions that, in the examples presented in this note, entail violations of the principle of mass conservation. A discussion about the Oberbeck-Boussinesq approximation as an asymptotic theory obtained by letting the product of the thermal expansion coefficient and the reference temperature difference tend to zero is also presented.
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