Skip to main content

Research Repository

Advanced Search

Double-diffusive penetrative convection simulated via internal heating in an anisotropic porous layer with throughflow

Capone, F.; Gentile, M.; Hill, Antony A.

Authors

F. Capone

M. Gentile

Profile image of Antony Hill

Antony Hill Antony.Hill@uwe.ac.uk
College Dean of Learning and Teaching



Abstract

A model for double-diffusive convection in an anisotropic porous layer with a constant throughflow is explored, with penetrative convection being simulated via an internal heat source. Both linear instability and nonlinear stability analyses are performed to assess the suitability of linear theory to predict the destabilisation of the throughflow. It is shown that due to oscillatory instability modes, there are three distinct regions, where increasing the ascending throughflow from rest actually has a stabilising effect, before following the standard destabilisation and stabilisation pattern. This is a previously unobserved phenomenon. The agreement between the linear and nonlinear thresholds is substantial when a small descending throughflow is introduced, although this does deteriorate for ascending throughflow. © 2010 Elsevier Ltd. All rights reserved.

Journal Article Type Article
Publication Date Mar 1, 2011
Deposit Date Oct 24, 2012
Journal International Journal of Heat and Mass Transfer
Print ISSN 0017-9310
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 54
Issue 7-8
Pages 1622-1626
DOI https://doi.org/10.1016/j.ijheatmasstransfer.2010.11.020
Keywords throughflow, energy method, internal heat source, anisotropic porous media
Public URL https://uwe-repository.worktribe.com/output/967477
Publisher URL http://dx.doi.org/10.1016/j.ijheatmasstransfer.2010.11.020
Contract Date Nov 15, 2016