Abstract
This paper reports a numerical investigation with a horizontal layer of dielectric liquid subjected to the simultaneous effects of external thermal and electric fields. The flow is driven by the buoyancy force and the Coulomb force, which depend on the Rayleigh number (Ra) and the electric Rayleigh number (T), respectively. We consider a strong unipolar injection from the lower electrode and a destabilizing thermal gradient. The two driving forces cooperate with each other in destabilizing the system. The neutral stability curve in the Ra-T plane is successfully reproduced from the direct numerical results, and it is shown to be independent on the Prandtl number (Pr) and the dimensionless mobility number (M). On the other hand, both the bifurcation types of the linear instability (subcritical or supercritical) and the finite amplitude stability criterion depend strongly on the combination of Pr and M. © 2015 Elsevier B.V. All rights reserved.
| Original language | English |
|---|---|
| Pages (from-to) | 45-57 |
| Journal | Physica D: Nonlinear Phenomena |
| Volume | 311-312 |
| DOIs | |
| Publication status | Published - 1 Sept 2015 |
| Externally published | Yes |
Bibliographical note
Publication details (e.g. title, author(s), publication statuses and dates) are captured on an “AS IS” and “AS AVAILABLE” basis at the time of record harvesting from the data source. Suggestions for further amendments or supplementary information can be sent to [email protected].Funding
This work was funded by the French Government program “Investissements d’Avenir” ( LABEX INTERACTIFS , reference ANR-11-LABX-0017-01 ) (to Jian Wu), a grant from the French district Poitou–Charentes (to P. Traoré) and financial support from the Spanish Ministerio de Cienciay Tecnología (MCYT) under Research Project No. FIS2011-25161 and Junta de Andalucía under research projects P10-FQM-5735 and P09-FQM-4584 (to A.T. Pérez).
Research Keywords
- Charge injection
- Dielectric liquid
- Electro-thermo-convection
- Electrohydrodynamics
- Numerical analysis
- Rayleigh-Bénard convection
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