5 edition of Derivation of the equations for thermal convection in a porous material. found in the catalog.
Includes bibliographical references.
|Statement||University of Oslo, Institute of Mathematics|
|Publishers||University of Oslo, Institute of Mathematics|
|The Physical Object|
|Pagination||xvi, 131 p. :|
|Number of Pages||72|
|3||Reprint series 1971;|
nodata File Size: 8MB.
The viscous dissipation terms arise naturally and are essentially the same form as those of Al-Hadrami et al. We present a heuristic one-dimensional model arising from which suggests that while T might become very large, blow-up in finite time will not occur. In the absence of an internal source, when the fluid is in contact with a hot surface, its molecules separate and scatter, causing the fluid to be less dense.
: Three dimensional simulations for convection induced by the selective absorption of radiation for the brinkman model.and now additionally omit the sub- or superscript f.
Introduction to Climate Modelling, by Thomas Stocker, p57,• Thus, the analysis of energy stability for the alternative viscous dissipation function turns out to lead to exactly the same nonlinear stability result.
Overview [ ] Convection can be "forced" by movement of a fluid by means other than buoyancy forces for example, a water pump in an automobile engine. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. It is not the purpose of this article to enter this controversy.
: Stability, and wave motion in porous media, vol. Conversely, the flow of heat can be regarded as a kind of heat diffusion.
Overview [ ] Convection can be "forced" by movement of a fluid by means other than buoyancy forces for example, a water pump in an automobile engine.