Bidispersive double diffusive convection

Straughan, B.

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.

Citation

Straughan, B. (2018). Bidispersive double diffusive convection. International Journal of Heat and Mass Transfer, 126, 504-508. https://doi.org/10.1016/j.ijheatmasstransfer.2018.05.056

• Journal Article Type: Article
• Acceptance Date: May 11, 2018
• Online Publication Date: May 29, 2018
• Publication Date: Nov 30, 2018
• Deposit Date: Jun 5, 2018
• Publicly Available Date: May 29, 2019
• Journal: International Journal of Heat and Mass Transfer
• Print ISSN: 0017-9310
• Electronic ISSN: 1879-2189
• Publisher: Elsevier
• Peer Reviewed: Peer Reviewed
• Volume: 126
• Pages: 504-508
• DOI: https://doi.org/10.1016/j.ijheatmasstransfer.2018.05.056
• Public URL: https://durham-repository.worktribe.com/output/1329504