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Durham Research Online
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Bidispersive double diffusive convection.

Straughan, B. (2018) 'Bidispersive double diffusive convection.', International journal of heat and mass transfer., 126 . pp. 504-508.

Abstract

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.

Item Type:Article
Full text:(AM) Accepted Manuscript
Available under License - Creative Commons Attribution Non-commercial No Derivatives.
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Status:Peer-reviewed
Publisher Web site:https://doi.org/10.1016/j.ijheatmasstransfer.2018.05.056
Publisher statement:© 2018 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
Date accepted:11 May 2018
Date deposited:05 June 2018
Date of first online publication:29 May 2018
Date first made open access:29 May 2019

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