Dans cette thèse on s'est intéressé à l'étude de problèmes concernant la théorie des écoulements compressibles. Dans une première partie on a traité le problème de transport instationnaire avec un champ de vitesse peu régulier, on a établi un résultat d'existence en passant à la limite sur des schémas numériques volumes finis avec un choix décentré amont qui garantie la positivité de la masse volumique. Pour le problème de Stokes, le résultat est démontré par deux approches : une approche par schéma numérique et une approche par régularité visqueuse.Dans la première méthode on propose une discrétisation qui combine la méthode des éléments finis et la méthode des volumes finis qui repose sur les espaces Crouzeix-Raviart. Une première difficulté de ce travail est de démontrer les estimations sur la solution discrète, en particulier à cause de la présence de la gravité dans le terme source de l'équation de quantité de mouvement. Le fait de considérer une loi d'état très générale conduit des difficultés supplémentaires en particulier dans le passage à la limite sur cette équation.Dans la deuxième méthode, le résultat d'existence est démontré en utilisant une approximation par viscosité. Ceci consiste essentiellement en deux parties : l'étude du problème de convection diffusion (qui apparait dans le problème régularisé) où on démontre l'existence et l'unicité de solution et en deuxième partie le passage à la limite sur le problème régularisé. / This thesis is concerned with the study of problems relating in the theory of compressible flows . We prove the existence of the considered problems in a first part by passing to the limit on the numerical schemes proposed for the discretisation of these problems. In the second part, the existence result is obtained by passing to the limit on the approximate solutions given by a corresponding regularized problem.The main result is to prove the existence of a solution of the stationnary compressible Stokes problem with a general equation of state.We first prove this result by passing to the limit on the numerical scheme as the mesh size tends to zero. The fact to consider a general E.O.S induces some additional difficulties in particular to get estimates on the discrete solution (which comes also from the presence of the gravity in the momentum equation) and in the passage to the limit on the E.O.S.We also prove the existence result by passing to the limit on a regularized problem. We first treat the convection-diffusion problem (which appears in the regularized problem), we give an existence and uniqueness result, and we then prove estimates on the approwimate solutions and pass to the limit on the regularized problem.

We study a random homogenization problem concerning the flow of a viscous fluid through a permeable membrane with a highly oscillatory geometry and nonlinear boundary condition on it. Along an interface we consider a periodic distribution of small permeable obstacles with a random geometry. Leak boundary conditions of threshold type are considered on the obstacle part of the membrane: the normal velocity of the fluid is zero until the jump of the normal component of the stress acting on it reaches a certain limit, and then the fluid may pass freely. The problem is studied first in the deterministic case, and then in the random case, for which assumptions on the randomness of the solid obstacles are needed in order to obtain a limiting behaviour. The description of the obstacles is given in terms of a random set-valued variable defined on a probability space and a dynamical system acting on it. Effective boundary conditions for the fluid are derived, and these depend on the relative size of the obstacles. We establish two major cases, in one of them we obtain an effective permeability across the membrane and in the critical case a slip boundary condition of Navier type. If the dynamical system is assumed to be ergodic, the limiting behaviour of the fluid is deterministic. The approach is based on the Mosco convergence, which also allows us to pass from the stationary case to the time dependent case via the convergence of the associated semigroups.

Les équations fondamentales décrivant la dynamique de l'océan sont en théorie les équations de Navier-Stokes sur une sphère en rotation, auxquelles il faut a jouter une équation d'état pour la densité, et des équations de transport-diffusion pour les traceurs. Toutefois, un certain nombre de considérations physiques et de limitations pratiques ont nécessité le développement de modèles plus simples. En effet, un certain nombre d'hypothèses simplificatrices sont pleinement justifiées du point de vue de la physique des mouvements océaniques, dont les principales sont les approximations de couche mince et de Boussinesq. D'autre part, étant donné les dimensions des bassins océaniques (plusieurs centaines à plusieurs milliers de kilomètres), les coûts de calculs sont un facteur pratique extrêmement limitant. On est, à l'heure actuelle, capable de simuler l'océan mondial avec une résolution de l'ordre de dix kilomètres, en utilisant des modèles dits aux équations primitives, dont le coût de calcul est bien inférieur à celui des équations de Navier-Stokes. On est donc bien loin d'une modélisation complète des phénomènes décrits par ces équations, qui nécessiterait en théorie de considérer des échelles de l'ordre du millimètre. Les équations primitives sont issues des équations complètes de la mécanique des fluides en effectuant l'approximation hydrostatique, justifiée par la faible profondeur des domaines considérés au regard de leur dimension horizontale. Dans cette thèse, nous considérerons les équations de Navier-Stokes (NS) qui sont le coeur du modèle complet évoqué ci-dessus, sans prendre en compte les équations de la densité et des traceurs (salinité, température, etc.). Nous utiliserons l'approximation hydrostatique dans le chapitre 10, et le modèle sera naturellement appelé Navier-Stokes hydrostatique (NSH). Il correspond aux équations primitives dans lesquelles on ne prendrait pas en compte la densité et les traceurs. C'est dans ce cadre que se situe le travail présenté dans cette thèse, avec l'objectif à moyen terme de pouvoir coupler de façon rigoureuse et efficace les équations de Navier-Stokes avec les équations primitives. Dans une première partie, on présentera quelques rappels sur les équations de Navier-Stokes, leur discrétisation, ainsi que le cas-test de la cavité entraînée qui sera utilisé dans tout ce document. Dans une deuxième partie, on met en œuvre les méthodes de Schwarz sur les équations de Stokes et Navier-Stokes, en dérivant notamment des conditions absorbantes exactes et approchées pour ces systèmes. Enfin, dans une troisième partie, on proposera des pistes vers le couplage Navier-Stokes/Navier-Stokes hydrostatique décrit ci-dessus. / Fundamental equations describing the ocean dynamic are theoretically Navier-Stokes equations over a rotating sphere, whom need to add a state equation for the fluid density, and advection-diffusion equations for tracers. However, some physical considerations and practical limitations required to developped more simple models. Indeed, some simplifying hypotheses are well justified from a ocean dynamic point of view, whose principal ones are thin layer and Boussinesq approximations. On the other hand, considering the dimensions of oceans (from serveral hundreds to serveral thousands kilometers), computations costs are a very practical limitating factor. We are, by now, able to simulate the global ocean with about ten kilometers large grid mesh. This is very far from a complete modelisation of all phenomenes decribed by the Navier-Stokes equations, which require to consider scales of milimeters order. Primitives equations derive from complete equations describing fluid mecanics, by doing the hydrostatic approximations, which is justified by the low deepness of considered domains with regard to their horizontal dimension. In this thesis, we are considering Navier-Stokes equations (NS) which are the heart of the complete modele mentionned previously, without holding in account density and tracers equations. We will use the hydrostatic approximations, and the resulting equations will be named as hydrostatic Navier-Stokes equations (NSH).The mid term objective is to couple carefully Navier-Stokes equations with primitive equation. In a first part, we will remind few results for Navier-Stokes equations, their discretization, and the lid-driven cavity which wil be used as a test-case. In a second part, we will use Schwarz method with Stokes and Navier-Stokes equations, deriving in particular exact and approched absorbing interface conditions for these systems. Finally, in a third part, we shall propose first results towards coupling Navier-Stokes and hydrostatic Navier-Stokes equations.

Next, we consider that the fluids are isentropic and the domain is also bounded, smooth, simply connected in R2 . We show that the estimates are uniform in all time if the smallness assumption on the initial data is prescribed. It follows that the solutions of compressible Navier-Stokes equations converge to the incompressible ones uniformly in both spatial and temporal variables as the Mach number vanishes. / This thesis deals with the low Mach number limit of the compressible Navier-Stokes equations. It is to verify that the compressible fluids become incompressible as Mach number tends to zero. In another words, the pressure due to compression can be neglected. This is a singular limit. / We will show that, as the Mach number tends to zero, the local smooth solutions of compressible Navier-Stokes equations with zero thermal conductivity coefficient converge strongly to the solutions of incompressible Navier-Stokes equations, provided that the initial data satisfy the "bounded derivative conditions". The key point, which is one of our main contributions, is the uniform high norm estimates in Mach number. We will study two cases. The first case is that, the domain is a finite interval and the boundary condition for the velocity is no-slip. In the second case, the domain is bounded, smooth, and simply connected in R2 . The boundary condition for the velocity is replaced by the slip-type's, thus the vorticity and the divergence of velocity can be estimated separately. / Ou, Yaobin. / Adviser: Zhouping Xin. / Source: Dissertation Abstracts International, Volume: 70-06, Section: B, page: 3546. / Thesis (Ph.D.)--Chinese University of Hong Kong, 2008. / Includes bibliographical references (leaves 107-111). / Electronic reproduction. Hong Kong : Chinese University of Hong Kong, [2012] System requirements: Adobe Acrobat Reader. Available via World Wide Web. / Electronic reproduction. [Ann Arbor, MI] : ProQuest Information and Learning, [200-] System requirements: Adobe Acrobat Reader. Available via World Wide Web. / Abstracts in English and Chinese. / School code: 1307.

Yu, Rongfeng. / Thesis (M.Phil.)--Chinese University of Hong Kong, 2011. / Includes bibliographical references (p. 57-63). / Abstracts in English and Chinese. / Introduction --- p.3 / Chapter 1 --- Preliminaries --- p.11 / Chapter 1.1 --- Notations and function spaces --- p.11 / Chapter 1.2 --- Some useful inequalities --- p.12 / Chapter 1.3 --- Fundamental lemmas --- p.15 / Chapter 2 --- Compressible Navier-Stokes Equations for Quantum Fluids --- p.16 / Chapter 2.1 --- Background --- p.17 / Chapter 2.2 --- Derivation of model --- p.17 / Chapter 3 --- Global Weak Solutions to Barotropic Navier-Stokes Equations for Quantum Fluids --- p.22 / Chapter 3.1 --- Reformulation and main results --- p.23 / Chapter 3.2 --- Construction of approximate solutions --- p.27 / Chapter 3.3 --- A priori estimates --- p.39 / Chapter 3.4 --- Proof of Theorem 3.1.6 --- p.40 / Chapter 4 --- Global Existence and Large Time Behavior of Weak Solutions to Quantum Navier-Stokes-Poisson Equa-tions --- p.46 / Chapter 4.1 --- Global existence of weak solutions --- p.47 / Chapter 4.2 --- Large time behavior --- p.50 / Chapter 5 --- Discussions and Future Work --- p.55 / Bibliography --- p.56

Submitted by SABRINA SUELEN AMARAL null (sabrinasuelen_5@hotmail.com) on 2017-02-26T00:34:42Z No. of bitstreams: 1 Dissertação definitiva Sabrina S Amaral - Copia.pdf: 862726 bytes, checksum: ef97a1fa8d86f69f3436915d6d9a433d (MD5) / Approved for entry into archive by Juliano Benedito Ferreira (julianoferreira@reitoria.unesp.br) on 2017-03-07T13:47:33Z (GMT) No. of bitstreams: 1 amaral_ss_me_sjrp.pdf: 862726 bytes, checksum: ef97a1fa8d86f69f3436915d6d9a433d (MD5) / Made available in DSpace on 2017-03-07T13:47:33Z (GMT). No. of bitstreams: 1 amaral_ss_me_sjrp.pdf: 862726 bytes, checksum: ef97a1fa8d86f69f3436915d6d9a433d (MD5) Previous issue date: 2017-02-22 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) / Neste trabalho analisamos as equações de Navier-Stokes em R^n, (n≤3) e mostramos boa colocação global, quando a velocidade inicial pertence ao espaço de Morrey e tem norma suficientemente pequena. Mostramos, também, que se o dado inicial é uma função homogênea de grau -1 então as soluções mild são autossimilares. Além disso, apresentamos um resultado de estabilidade assintótica das soluções mild. / In this work we will analyze the Navier-Stokes equations in R^n, (n≤3) and we will show global well-posedness, when the initial velocity belongs to the Morrey space and with a sufficiently small norm. We will also show that if the initial data is a homogeneous function of degree -1, then the mild solutions are self-similar. Moreover, we will present an asymptotic stability result of the mild solutions.

Orientador: Messias Meneguette Júnior / Banca: Heloisa Helena Marino Silva / Banca: Marcos Tadeu de Oliveira Pimenta. / Resumo: Neste trabalho é estudada a estabilidade para a equação de Stokes com diferentes condições de contorno em um esquema implícito. São consideradas análise pelo modonormal (método de Fourier) e pela computação numérica do fator de amplificação / Abstract: In this work we studied the stability for the Stokes equation with different boundary conditions in an implicit scheme. The normal-mode analysis (Fourier method) and numerical computation of the amplification factor are considered / Mestre

We present an immersed interface algorithm for the incompressible Navier Stokes equations. The interface is represented by cubic splines which are interpolated through a set of Lagrangian control points. The position of the control points is implicitly updated using the fluid velocity. The forces that the interface exerts on the fluid are computed from the constitutive relation of the interface and are applied to the fluid through jumps in the pressure and jumps in the derivatives of pressure and velocity. A projection method is used to time advance the Navier-Stokes equations on a uniform cartesian mesh. The Poisson-like equations required for the implicit solution of the diffusive and pressure terms are solved using a fast Fourier transform algorithm. The position of the interface is updated implicitly using a quasi-Newton method (BFGS) within each timestep. Several examples are presented to illustrate the flexibility of the presented approach. / Singapore-MIT Alliance (SMA)

The current thesis studies a model of two dimensional convection of an ideal gas in a rectangular domain having walls of finite thickness. The temperature outside of walls is considered constant. Heat exchange between walls and outside/inside air is computed using Newton's law of cooling. Heat transfer inside walls is modelled with the heat equation. The mathematical model inside enclosure involves Navier-Stokes equations coupled with equation of state for gas. The model is numerically studied using the method of large particles. One of the main goals of the current thesis was to develop a software in C# language for numerical solution of the above-described model. Physically meaningful results, including stream lines and distribution of parameters of gas and temperature inside solid walls were obtained.

The current thesis studies a model of two dimensional convection of an ideal gas in a rectangular domain having walls of finite thickness. The temperature outside of walls is considered constant. Heat exchange between walls and outside/inside air is computed using Newton's law of cooling. Heat transfer inside walls is modelled with the heat equation. The mathematical model inside enclosure involves Navier-Stokes equations coupled with equation of state for gas. The model is numerically studied using the method of large particles. One of the main goals of the current thesis was to develop a software in C# language for numerical solution of the above-described model. Physically meaningful results, including stream lines and distribution of parameters of gas and temperature inside solid walls were obtained.