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Bidispersive double diffusive convection

delete2018-11-01
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B
Brian Straughan *
DOI:10.1016/j.ijheatmasstransfer.2018.05.056delete
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摘要

摘要

En 中文
A model is developed for double diffusive convection in a bidisperse porous medium. Double diffusive convection is convective movement of fluid due to temperature and salt gradient effects. A bidisperse porous medium is one where there are pores known as macropores, but the solid skeleton contains cracks or fissures which give rise to a porosity in the skeleton, known as microporosity. We concentrate on the case of a single temperature field and attention is focussed on the situation where the layer is heated from below and simultaneously salted from below. (C) 2018 Elsevier Ltd. All rights reserved.
Keyword:
Bidispersive porous media
Convection in porous media
Bidispersive convection
Double diffusive convection
Linear instability
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期刊

International Journal of Heat and Mass Transfer 封面图
International Journal of Heat and Mass Transfer
IF:
5.8
论文数:
2.6W
被引数:
10.2W

机构

D
Durham University
学者数:
1.3W
论文数: 1.5W
被引数: 2.1W
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