par Pontès, José;Christov, Christo Ivanov 
;Velarde, Manuel G.
Référence International journal of bifurcation and chaos in applied sciences and engineering, 6, 10, page (1883-1890)
Publication Publié, 1996-10
;Velarde, Manuel G. Référence International journal of bifurcation and chaos in applied sciences and engineering, 6, 10, page (1883-1890)
Publication Publié, 1996-10
Article révisé par les pairs
| Résumé : | Pattern formation in a finite layer of fluid induced either by buoyancy or by a surface-tension gradient is considered. The fluid is confined between poor conducting horizontal boundaries, leading to patterns with a characteristic horizontal scale much larger than the fluid depth. The evolution of the system is studied by numerical integration of the (1+2)D equation introduced by Knobloch [1990]: ∂u/∂t = αu - μ▽2u - ▽4u + κ▽ · ( |
