Brian Straughan
Thermosolutal Convection with a Navier–Stokes–Voigt Fluid
Straughan, Brian
Authors
Abstract
We present a model for convection in a Navier–Stokes–Voigt fluid when the layer is heated from below and simultaneously salted from below, the thermosolutal convection problem. Instability thresholds are calculated for thermal convection with a dissolved salt field in a complex viscoelastic fluid of Navier–Stokes–Voigt type. The Kelvin–Voigt parameter is seen to play a very important role in acting as a stabilizing agent when the convection is of oscillatory type. The quantitative size of this effect is displayed. Nonlinear stability is also discussed, and it is briefly indicated how the global nonlinear stability limit may be increased, although there still remains a region of potential sub-critical instability, especially when the Kelvin–Voigt parameter increases.
Citation
Straughan, B. (2021). Thermosolutal Convection with a Navier–Stokes–Voigt Fluid. Applied Mathematics and Optimization, 84(3), 2587-2599. https://doi.org/10.1007/s00245-020-09719-7
Journal Article Type | Article |
---|---|
Online Publication Date | Sep 20, 2020 |
Publication Date | 2021-12 |
Deposit Date | Oct 7, 2020 |
Publicly Available Date | Oct 7, 2020 |
Journal | Applied Mathematics and Optimization |
Print ISSN | 0095-4616 |
Electronic ISSN | 1432-0606 |
Publisher | Springer |
Peer Reviewed | Peer Reviewed |
Volume | 84 |
Issue | 3 |
Pages | 2587-2599 |
DOI | https://doi.org/10.1007/s00245-020-09719-7 |
Public URL | https://durham-repository.worktribe.com/output/1260278 |
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Advance onlne version This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
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