Orientador: João Frederico da Costa Azevedo Meyer / Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Matemática, Estatística e Computação Científica / Made available in DSpace on 2018-08-18T17:19:29Z (GMT). No. of bitstreams: 1 Krindges_Andre_D.pdf: 12331441 bytes, checksum: ca3fa7d1c704c02f04ba59043413e0f7 (MD5) Previous issue date: 2011 / Resumo: Um dos problemas enfrentados pelo grupo de Ecologia Matemática do IMECC da UNICAMP é o de trabalhar com difusão de uma pluma poluente com 3 variáveis espaciais, além da temporal. Esta tese não só aborda esta questão, propondo, inclusive um algoritmo computacional para esta situação, mas fá-lo resolvendo aproximadamente a Equação de Navier-Stokes num domínio irregular. A primeira parte consiste na formulação do modelo matemático para o estudo de um sistema que inclui o campo de velocidades e o comportamento evolutivo de um material poluente. Na segunda parte, é feita a formulação variacional, são constituídas aproximações via o método de Galerkin para Elementos Finitos no espaço e Crank-Nicolson no tempo para a equação de difusão-advecção, e o método da projeção para a equação de Navier-Stokes. Em seguida, faz-se a descrição do algoritmo, indicando dificuldades operacionais do ponto de vista de computação científica e apontando soluções. O domínio utilizado para o estudo de caso é o da represa do rio Manso, que, discretizada em três dimensões, foi tratado com o software livre GMSH. Finalmente, um código numérico em plataforma MATLAB foi executado e resultados são apresentados no texto. O programa e diversas considerações técnicas essenciais fazem parte dos anexos / Abstract: One of the challenges faced by the Mathematical Ecology group at the Mathematics Institute at Campinas State University is that of working with the diffusion of a pollutant plume in three spatial variables, besides time. This work not only addresses this issue by proposing an approximation strategy as well as a computer algorithm for this situation, but it also includes a three-dimensional numerical approximation for the Navier-Stokes equation in an irregular domain. The first part consists in formulating the mathematical model for the study of a system that includes the velocity field and the evolutionary behavior of a polluting material. The second part begins with the variational formulation of the Navier-Stiokes system, and approximations are undertaken via the Galerkin method for finite elements in space and Crank-Nicolson in time for both the advection-diffusion equation and the method of projection for the Navier-Stokes equations. The algorithm is described, indicating operational difficulties in terms of scientific computing as well as the way in which these aforementioned difficulties are solved. The domain used for the case study is the Manso River reservoir, which, discretized in three dimensions, was treated with the free software GMSH. Finally, a numeric code in MATLAB environment was completed and results are presented in the text. The program and various essential technical considerations are part of the annexes / Doutorado / Matematica Aplicada / Doutor em Matemática Aplicada

Orientador: Donato Giorgio Torrieri / Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Física Gleb Wataghin / Made available in DSpace on 2018-08-31T06:57:06Z (GMT). No. of bitstreams: 1 Coelho_DavidMontenegro_M.pdf: 2238497 bytes, checksum: 78f745f9d544a31d97a2d7a80b7dc505 (MD5) Previous issue date: 2016 / Resumo: O interesse científico cresceu após confirmado por testes experimentais o comportamento do Plasma de Quark-Glúon como um fluido quase perfeito no LHC e RHIC. O objetivo desse trabalho é fornecer as bases teóricas da Effective Field Theory (EFT) na abordagem da Hidrodinâmica, pois vários recursos não-triviais na dinâmica relativística dos fluidos são claramente explicados por esse formalismo. Problemas teóricos na EFT sugerem a inclusão de uma nova formulação do Princípio de Hamilton compatível com o princípio da causalidade, através do Closed-Time-Path. Após resolvido esse problema, alcançamos o requisito necessário para derivar a hidrodinâmica dissipativa em altas ordens por meio da ação. Assim, conseguimos caracterizar a Lagrangeana de Navier-Stokes ao introduzir a quebra de simetria na preservação do difeomorfismo pelo volume por meio do termo $B^{-1}_{IJ}$. No entanto, uma análise pelo método de Ostrogradski levou à supressão dessa equação, através da inclusão da Lagrangeana de Israel-Stewart na expansão que é justificada por meios de argumentos de estabilidade e causalidade. Por fim, propomos uma variável $X_{IJ}$ na Lagrangeana de Israel-Stewart, simétrica, anisotrópica e dependente das condições iniciais que juntamente com os já estabelecidos graus de liberdade de campo, formam a base para a derivação bottom-up em altas ordens da EFT e propicia medidas para estudar turbulência e instabilidade no vácuo e outras situações que chegam da relação entre graus de liberdade macroscópico e microscópico / Abstract: Scientific interest grew after the behavior of the quark-gluon Plasma as a nearly perfect fluid in the LHC and RHIC. The objective of this dissertation is offer support to use the Effective Field Theory (EFT) approach to study hydrodynamics because many non-trivial features in relativistic fluid dynamics are clearly explained by this Lagrangian formalism. Theoretical problems in EFT considering by including a new formulation of the Hamiltonian principle that is compatible with the principle of causality for non-conservative field through the Closed-Time-Path formalism. After solving this problem, we reached requirement to derive the dissipative hydrodynamics in higher orders of action. We were able to characterize Navier-Stokes' Lagrangian by introducing the symmetry breaking of preserving diffeomorphism through the volume with the term $B^{-1}_{IJ} $ to the Lagrangian of Navier-Stokes. An analyse of Ostrogradski's method led to the removal of equation by including the Israel-Stewart term in the Lagrangian expansion that provides an extra justification by means of symmetry and causality arguments. Finally, we propose a variable $ X_ {IJ} $, Israel-Stewart's Lagrangian, symmetric, anisotropic and dependent on initial conditions together with an established degree of freedom of the field, which form the basis for the derivation of higher orders of the bottom up and promote steps to the study of turbulence by instability in the vacuum, and other situations arising from the relationship between macroscopic and microscopic degrees of freedom / Mestrado / Física / Mestre em Física / 147435/2014-5 / CNPQ

Cílem této diplomové práce je vytvořit 3D model horních dýchacích cest podle originálního modelu segmentovaného z CT dat, aplikovat různé podmínky na průtok vzduchu v modelu, a poté hodnotit změnu charakteristik rychlosti a tlaku. Model horních dýchacích cest byl vytvořen v prostředí softwaru ANSYS, který využívá výpočetní dynamiku tekutin, a byly použity Navier-Stokesovy rovnice pro modelování průtoku vzduchu v modelu. Nejprve byl vytvořen jednoduchý 2D model za účelem seznámení se s prostředím ANSYS. Dále byl zkonstruován 3D model horních dýchacích cest a byly modelovány charakteristiky rychlosti a tlaku za různých podmínek. Tyto podmínky zahrnují různé umístění a množství míst pro odběr vzorků v modelu a výběr různých kombinací vstupů. Nakonec byly prezentovány a hodnoceny výsledky spolu s ilustracemi modelů modelovaných za různých podmínek. 3D model lze považovat ze kompromis mezi výpočetní náročností a složitostí modelu a lze jej použít jako základ pro další výzkum.

This thesis focuses on fluid simulation, particularly on coupling between particle based simulation and grid based simulation and thus modeling evaporation. Mentioned coupling is based on the article Evaporation and Condensation of SPH-based Fluids of authors Hendrik Hochstetter a Andreas Kolb. The goal of this thesis is not purely implementing ideas of the mentioned article, but also study of different methods used for fluid simulation.

Im Rahmen des Modellierungsseminars wurde die Kopplung einer Strömung mit der Ausbreitung einer reaktiven Substanz im Strömungsgebiet untersucht. Die Strömung wurde dabei durch die inkompressiblen Navier-Stokes-Gleichungen beschrieben. Zusätzlich wurde ein mathematisches Modell für die Ausbreitung der Substanz durch eine Diffusions-Konvektions-Gleichung bestimmt. Beide wurden durch die FEM- Sofware NAVIER berechnet und simuliert.:0 Notation 3 1 Aufgabenstellung 4 1.1 Projekt 4 1.2 Navier-Stokes-Strömung gekoppelt mit (passivem) Transport einiger (reaktiver) Substanzen 4 2 Einleitung 6 2.1 Strömungslehre 6 2.2 Regelungstheorie 7 3 Mathematische Modellierung 8 3.1 Strömungsmodellierung 8 3.2 Modell zur Ausbreitung des gelösten Stoffes 8 3.3 Gekoppeltes Modell und Randbedingungen 12 3.4 Grenzschichten 13 3.5 Feedback-Steuerung 15 4 Numerische Simulation 19 4.1 Umsetzung des Modells in NAVIER 19 4.1.1 Mathematische Grundlagen für NAVIER 20 4.1.2 Problemimplementation 21 4.2 Beispielsimulation 24 4.2.1 Gebietstriangulation 24 4.2.2 Konfigurationsdaten sowie Anfangs- und Randbedingungen 25 4.2.3 Ergebnisauswertung 28 4.3 Zusatzfunktionen für die Regelung 34 4.3.1 outflow-Funktion 34 4.3.2 Systemmatrizen 34 4.3.3 Feedback-Funktion 34 5 Zusammenfassung/Ausblick 35 5.1 Zusammenfassung 35 5.2 Ausblick 36 6 Schlusswort 37 7 Quellenverzeichnis 38 8 Verzeichnisse 39

The aim of this work is to provide new results of global existence for dif- ferent evolution equations of fluid mechanics. We are in general interested in finding weak solutions without restrictions on the size of initial data. The proofs of existence are based on several different approaches including en- ergy methods, convergence analysis of finite numerical methods and convex integration. All these techniques significantly exploit results of mathematical analysis and other branches of mathematics. 1

We prove a global-in-time and large-data existence of a suitable weak solution to a system of partial differential equations describing an unsteady flow of homogeneous incom- pressible viscoelastic rate-type fluid. The material parameters are continuous functions of temperature and, in particular, the dependence of the shear modulus is assumed to be linear. It is shown that studied models obey the fundamental laws of thermodynamics. The key step towards the existence proof is derivation of the balance of entropy. This in- equality is paramount in the analysis and as its consequence, we obtain sufficient a priori estimates, positivity of temperature and also regularity of the elastic deformation. The second part of the thesis deals with the existence analysis for the isothermal case, however using a completely different method, which is of independent interest. 1

Numerical solutions of the Navier-Stokes Equations became more popular in recent decades with increasingly accessible and powerful computational resources. Simulations in reconstructed or artificial pore geometries are often performed to gain insight into microscopic fluid flow structures or are used for upscaling quantities of interest, like hydraulic conductivity. A physically adequate representation of pore-scale flow fields requires analysis of large domains. We solve the incompressible NSE in artificial ordered and random pore-space structures. A simple cubic and face-centred packings of spheres placed in a square duct are analysed. For the fluid flow simulations of random media, packings of spheres, icosahedra, and cubes forming unconsolidated sediments are generated using a rigid body simulation software. The Direct Numerical Simulation method is used for the solution of the NSE implemented in the open-source computational fluid dynamics software OpenFOAM. The influence of the number of spheres in ordered packings, the mesh type, and the mesh resolution is investigated for fluid flow up to Reynolds numbers of 100 based on the spheres' diameter. The random media mesh generation method relies on approximate surface reconstruction. The resulting tetrahedral meshes are then used for steady-state simulations and refined based on an a-posteriori error estimator. The fluid flow simulation results can further be used twofold: 1) They provide homogenized hydro-mechanical properties of the analysed medium for the larger meso and macro groundwater flow simulations. A concept of one-way binding for large-scale simulations is presented. 2) Visualisation: A post-processing image rendering technique was employed in interactive and still image visualisation environments allowing better overview over local fluid flow structures. The ogs FEM code for the solution of large-scale groundwater processes was inspected for computational efficiency. The conclusions drawn from this analysis formed the~basis for the implementation of the~new version of the code---ogs6. The improvements include comparison of linear algebra software realisations and an implementation of optimized memory access patterns in FEM-local assembler part.

In this report the regular finite differences method (FDM) and a least-squares radial basis function-generated finite differences method (RBF-FD-LS) is used to solve the two-dimensional incompressible Navier-Stokes equations for the lid driven cavity problem. The Navier-Stokes equations is solved using stream function-vorticity formulation. The purpose of the report is to compare FDM and RBF-FD-LS with respect to accuracy and computational cost. Both methods were implemented in MATLAB and the problem was solved for Reynolds numbers equal to 100, 400 and 1000. In the report we present the solutions obtained as well as the results from the comparison. The results are discussed and conclusions are drawn. We came to the conclusion that RBF-FD-LS is more accurate when the stepsize of the grids used is held constant, while RBF-FD-LS costs more than FDM for similar accuracy.

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第19677号 / 工博第4132号 / 新制||工||1638(附属図書館) / 32713 / 京都大学大学院工学研究科都市社会工学専攻 / (主査)教授 五十嵐 晃, 准教授 米山 望, 准教授 森 信人 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM