2003
DOI: 10.1098/rspa.2002.1036
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On the existence and uniqueness of the stationary solution to equations of natural convection with boundary data in L 2

Abstract: By M. S a n t o s d a R o c h a 1 , M a r k o A. R o j a s-M e d a r 1 a n d M. D r i n a R o j a s-M e d a r 2

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Cited by 13 publications
(5 citation statements)
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“…Most of these theoretical studies have been directed to the case in which the driving force is a volume force (as implicit in the problem statement per se). For the case of buoyancy flow, as an example, the interested reader may consider [61][62][63][64][65][66][67][68][69][70][71][72][73][74][75][76][77][78][79]. Surprisingly, however, no results specific for the case of Marangoni flow have been obtained or presented so far.…”
Section: Discussionmentioning
confidence: 99%
“…Most of these theoretical studies have been directed to the case in which the driving force is a volume force (as implicit in the problem statement per se). For the case of buoyancy flow, as an example, the interested reader may consider [61][62][63][64][65][66][67][68][69][70][71][72][73][74][75][76][77][78][79]. Surprisingly, however, no results specific for the case of Marangoni flow have been obtained or presented so far.…”
Section: Discussionmentioning
confidence: 99%
“…has the Carathéodory property (see [ By [8,Theorem 12.10] we deduce that the Němytskiȋ operator N is a continuous operator from L r (Ω) into L r (Ω) (recall (8)). Since we assume θ n → θ in W 2−ε,r (Ω) and W 2−ε,r (Ω) ֒→ L r (Ω), we get (25).…”
Section: Preliminariesmentioning
confidence: 99%
“…Coefficient α 1 reflects the dissipation effect, which is omitted frequently in many mathematical models [19,24,25,26]. Otherwise, taking into account the dissipative term α 1 νe(u) : e(u) with quadratic growth of the gradient, the equations ( 1)-( 7) represent the elliptic system with strong nonlinearities without appropriate general existence and regularity theory.…”
Section: Introductionmentioning
confidence: 99%
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“…No sistema linearizado, ele aplicou os resultados obtidos por Conca [21], [22] e definiu uma contração que permite aplicar o Teorema do ponto fixo de Banach. A extensão para as equações de Boussinesq foram dadas por Santos et al [114] os quais analisaram o sistema (2.1), mas com condições de fronteira do tipo Dirichlet não somente para a velocidade u mas também para a temperatura θ. Em outros modelos da Hydrodinâmica, Guillén-González et al [ 5 1 ]e s t udaram o conceito de solução ultra fraca para o sistema de Stokes hidrostático com condições de Neumann não suaves sobre a superfície rígida e condições do tipo Dirichlet sobre o resto da fronteira. Em [115], são consideradas as equações estacionárias de Navier-Stokes com dados de fronteira em algum espaço W 1− 1 q ,q (Γ).…”
Section: Novalisunclassified