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. Download PDF (116Kb) |
| 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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