La qualité d'impression est une notion difficile à maîtriser. L'œil est souvent utilisé en industrie comme outil permettant de juger la qualité d'un film polymère imprimé. Afin d'atteindre un niveau supérieur de qualité, il est nécessaire de trouver un moyen pour quantifier la qualité d'impression, et ainsi permettre d'atteindre soit une qualité dite « point par point », soit une qualité dite « all-over ». Plusieurs éléments sont nécessaires à cette quantification : une image en microscopie optique de l'échantillon, ainsi qu'une valeur d'intensité moyenne et d'homogénéité de couleur, que l'on obtient grâce à un rugosimètre confocal. Ainsi nous avons pu définir, pour un support mis en forme par calandrage et un support mis en forme par enduction, les paramètres majeurs agissant sur la qualité d'impression. En termes de procédé, il apparaît que la vitesse d'impression et la pression du cylindre presseur influencent grandement l'imprimabilité. Au niveau des matériaux utilisés, la viscosité et la tension de surface de l'encre ont un effet important alors qu'en termes de support, un film calandré sera plus sensible aux variations des différents paramètres qu'un film enduit. / Printing quality idea is hard to control. In industry, eye is often used to judge the quality of a printed polymer film. In order to get a new level in terms of printing quality and get “point by point” or “all-over” quality, it is necessary to find a way to quantify printing quality. Some elements are important concerning the quantification of the printing quality: an optical microscopic image, a value of the average intensity and a value on the homogeneity of the color. We can define, for a calendered and a coated substrate, the main parameters acting on the printing quality. Printing speed and pressure of the rubber roll are the two main process parameters to act, viscosity and surface tension of the ink are the two main ink properties to act, while the calendered substrate is more sensitive to the variation of the parameters than the coated one.

Submitted by Fabio Sobreira Campos da Costa (fabio.sobreira@ufpe.br) on 2017-07-28T13:17:05Z No. of bitstreams: 2 license_rdf: 811 bytes, checksum: e39d27027a6cc9cb039ad269a5db8e34 (MD5) DISSERTAÇÃO.pdf: 1904426 bytes, checksum: 881aba48363b69adb462f39f38edbbe8 (MD5) / Made available in DSpace on 2017-07-28T13:17:05Z (GMT). No. of bitstreams: 2 license_rdf: 811 bytes, checksum: e39d27027a6cc9cb039ad269a5db8e34 (MD5) DISSERTAÇÃO.pdf: 1904426 bytes, checksum: 881aba48363b69adb462f39f38edbbe8 (MD5) Previous issue date: 2016-02-23 / As proteases são enzimas com a capacidade de hidrolisar proteínas em peptídeos menores ou aminoácidos livres, sendo essenciais para animais, plantas e micro-organismos devido à sua atuação na regulação metabólica. As proteases são utilizadas com diversas finalidades, no processo industrial da fabricação de detergentes, na indústria farmacêutica e de alimentos, além de ser utilizada na recuperação e aproveitamento de resíduos e subprodutos. Em virtude da grande importância das proteases este trabalho teve como objetivo comparar a produção de proteases produzidas por Mucor subtilissimus UCP 1262 em fermentação em estado sólido (FES) e submersa (FS), bem como extrair em Sistema de duas fases aquosas (SDFA) PEG/Fosfato, as colagenases oriundas de ambas as fermentações. O meio de produção da FES e FS no qual o micro-organismo foi cultivado era constituído principalmente de farelo de soja e farinha de soja. As determinações enzimáticas e dosagem proteica foram realizadas após 72h de fermentação. Para montagem do SDFA foram realizados dois planejamentos fatoriais 23, o primeiro planejamento foi realizado com amostras da FES e o segundo com amostras da FS. Neste sistema foi analisada a influência de três variáveis no processo de extração: massa molar do PEG (200, 550 e 1000 g/mol), concentração do PEG (17,5; 20 e 22,5%) e concentração do sal fosfato de sódio (15; 17,5 e 20%). A maior produção de proteases (362,66 U/ml) ocorreu na FES, enquanto que na FS obteve-se apenas 26,33 U/ml. Dentre as atividades proteásicas específicas: colagenolítica, fibrinolítica e queratinolítica, os melhores resultados foram obtidos para a atividade colagenolítica, sendo esta de: 179,81 U/ml, em FES. A colagenase presente no extrato bruto obtida nos processos fermentativos foram particionadas para fase rica em PEG do SDFA. O maior valor para a variável resposta Fator de purificação (FP=3,49) foi obtido no sistema que utilizou o extrato obtido por FES. Com base nas condições estudadas, os dois sistemas mostraram-se viáveis para a extração de colagenase, pois além de ser um processo que pode ser utilizado em larga escala é constituído por componentes de baixo custo e as condições utilizadas no SDFA favoreceram a extração desta enzima. Todavia, a extração da colagenase oriunda da FES foi mais promissora em virtude da maior concentração da enzima de interesse encontrada nesse tipo de fermentação. / Proteases are enzymes with the ability to hydrolyze proteins into smaller peptides and free amino acids. They are vital for animals, plants and micro-organisms due to their role in metabolic regulation. Proteases have been used in various purposes, in the industrial process of detergents, pharmaceutical and food industry, as well as being used in the recovery and utilization of waste and by-products. Due to their economic feasibility and great medical and farmaceutical importance this study aimed to compare the production of proteases produced by Mucor subtilissimus UCP 1262 in solid state fermentation (SSF) and submerged fermentation (SF) as well as extract collagenolytic proteases using Aqueous two-phase system (ATPS) -PEG/Phosphate from both fermentations. The medium composition for the fungal fermentation in SSF and SF was based in soybean flour. Enzymatic determinations and protein levels were performed after 72 hours of fermentation. To mount the ATPS were two 23 factorial design, the first planning was carried out with samples of SSF and the second with samples of SF. In this system was analyzed the influence of three variables in the extraction process: PEG molar mass (200, 550 and 1000), the PEG concentration (17,5; 22,5 and 20%) and sodium phosphate salt concentration (15; 17,5 and 20%). The higher proteolytic activity (362,66 U/ml) was produced using SSF, while in the FS was obtained 26,33 U/ml. Among the specific proteolytic activities: collagenolytic, fibrinolytic and keratinolytic, the best results were obtained for the collagenolytic activity, this being: 179,81 U / ml in the SSF. The Collagenase present in the crude extract obtained in the fermentative processes partitioned preferencially to the PEG-rich phase. The highest value for the variable response Purification Factor (PF = 3,49) was obtained in the system that used SSF crude extract. According with the showed results, both extraction systems seemed to be feasible for collagenase extraction, as well as being a process that can be used in large scale, constituted by low cost components and conditions used in this ATPS favored the enzyme extraction. Furthermore, the collagenase extraction from the SSF was more promising because of the higher interest enzyme concentration found in this type of fermentation.

Orientador: Mário Noboru Tamashiro / Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Física Gleb Wataghin / Made available in DSpace on 2018-08-26T19:25:53Z (GMT). No. of bitstreams: 1 Braga_FilipeLeoncio_D.pdf: 3256250 bytes, checksum: 73d43bfd44605cb6f23213feb8aeedf9 (MD5) Previous issue date: 2015 / Resumo: Modelos termo-estatísticos que tentam reproduzir o comportamento de soluções aquosas de polímeros foram amplamente estudados ao longo dos anos. Entretanto, o número de trabalhos relacionados a sistemas aquosos contendo polímeros e sais adicionados ainda é bem restrito. Na tese desenvolvida, abordamos através de uma modelagem de Flory-Huggins a formação de sistemas aquosos bifásicos contendo cadeias poliméricas longas de polietileno-glicol em misturas contendo sais inorgânicos monovalentes. Dentro da modelagem, a competição entre a formação de ligações de hidrogênio por parte das moléculas de água e os monômeros da cadeia polimérica, além das interações íon-dipolo entre água e os íons dos sais dissociados, desempenham papel fundamental na formação das configurações de equilíbrio. Através de ajustes numéricos de dados experimentais, para cada tipo de sal introduzido na mistura, com previsões do modelo para as menores temperaturas para a formação das duas fases, as chamadas Cloud Point Temperatures (CPT), encontramos um conjunto de quatro parâmetros de interação que possibilitam a reprodução adequada do comportamento contínuo das CPT's em função das concentrações dos solutos / Abstract: Thermal-statistical models that try to reproduce the behavior of aqueous polymer solutions have been extensively studied over the years. However, the number of articles related to aqueous systems containing polymers and added salts is still very restricted. Across the developed thesis, we work with a Flory-Huggins theory to model the formation of aqueous two-phase systems containing long-polymer chains of polyethylene-glycol in mixtures containing monovalent inorganic salts. Within the model, the competition between the hydrogen-bond formation between water molecules and the monomers of the polymer chain, in addition to the ion-dipole interactions between water and the dissociated salt ions play a key role in shaping equilibrium configurations. Through numerical fits of experimental data for each type of salt introduced into the mixture with model predictions for the lowest temperatures for the formation of two phases, so-called Cloud Point Temperature (CPT), we find a set of four parameters of interaction that enable proper representation of the continuous behavior of CPT's as a function of the solutes concentration / Doutorado / Física / Doutor em Ciências

As biotécnicas da reprodução animal, amplamente difundidas no Brasil, tem possibilitado maior controle em relação à transmissão de agentes patogênicos, porém, a transmissão de doenças continua a ser uma preocupação justificável para a busca de melhores meios de controle. O objetivo do trabalho foi o de avaliar a diminuição da replicação viral (BoHV-1 Colorado) em embriões murinos após tratamentos com Produtos Naturais (PN). Trabalhamos com 3 grupos de PN, totalizando 18 tratamentos: Oléos Essenciais (OE) de Chamomilla recutita, Allium sativum, Zingiber officinale, Syzygium aromaticum, Illicium verum Hook f., Punica granatum e Melissa officinalis; Extratos Etanólicos (EE) das mesmas plantas anteriores com acréscimo de Pterodon emarginatus (casca e semente) e Extrato Aquoso (EA) de Própolis e Agaricus blazei. Inicialmente encontramos concentrações não tóxicas em células MDBK (Madin Darby Bovine Kidney) relacionada a cada PN (ampla sintonia) para posteriormente verificarmos as concentrações não tóxicas para os zigotos/embriões murinos (sintonia fina). Após encontrarmos as concentrações não tóxicas, os zigotos foram divididos em quatro grupos: G1 (Controle), G2 (expostos aos vírus BoHV-1 Colorado à 108 TCID50/mL), G3 (expostos aos PN) e G4 (expostos aos vírus e PN). Os grupos foram mantidos a 37,5 ºC em meio TCM199 (100 μL) com 10% de soro fetal bovino em estufa a 5% de CO2 e 95% de umidade. Após 24h, analisamos a taxa de clivagem (Teste Exato de Fisher_p<0,05), a morfologia (por microscopia óptica), a n-PCR e a titulação dos embriões em co-cultura com células MDBK após mais 72h do tratamento com os PN (Teste de Mann Whitney_ p<0,05). Dentre as 18 análises, os embriões murinos tratados com EA de Própolis, EE de Punica granatum e de Pteron emarginatus (Casca) apresentaram resultados satisfatórios: sem alterações morfológicas, taxa de clivagem semelhante aos controles e apesar da constatação da partícula viral junto aos embriões pela n-PCR, houve diminuição da concentração viral após tratamentos com estes extratos, o que sugere interferência destes tratamentos no ciclo viral do BoHV-1 Colorado. / The biotech Animal reproduction widespread in Brazil, has allowed greater control over the transmission of pathogens, however, the disease transmission remains a justifiable concern for the pursuit of the best means of control. The aim of this study was to evaluate the reduction of viral replicarion (Colorado BoHV-1) in murine embryos after treatments with natural products (NP). We work with groups \'3 \'PN, totaling 18 treatments: essential oils (EO) of Chamomilla recutita, Allium sativum, Zingiber officinale, Syzygium aromaticum, Illicium verum Hook f., Melissa officinalis and Punica granatum; ethanol extracts (EE) of the same plants prior to adding Pterodon emarginatus (skin and seed) and Aqueous Extract (EA) Propolis and Agaricus blazei. Initially we find non-toxic concentrations in MDBK (Madin Darby Bovine Kidney) related to each PN (broad line) then we check for the non-toxic concentrations for zygotes / embryos murine (fine tuning). After finding the non-toxic concentrations, zygotes were divided into four groups: G1 (control), G2 (exposed to viruses BoHV-1 at 108 Colorado TCID50/mL), G3 (exposed to PN) and G4 (exposed to viruses and PN .) The groups were maintained at 37.5 °C in TCM199 (100 mL) with 10% fetal bovine serum in an incubator at 5% CO2 and 95% humidity. After 24h, we analyzed the cleavage rate (Exact Test Fisher_p <0.05), morphology (light microscopy), the n-PCR and titration of embryos in co-culture with MDBK cells after 72 h of treatment with more NPs (Mann Whitney_ p <0.05). Among the 18 analyzes, murine embryos treated with EA Propolis, EE Punica granatum and Pteron emarginatus (bark) showed satisfactory results: no morphological changes, cleavage rate similar to controls, and despite the finding of the viral particle with the embryos by n-PCR, decreased the viral concentration after treatment with these extracts, suggesting interference of these treatments in the viral cycle of BoHV-1 Colorado.

Cette thèse s’est déroulée dans le cadre du projet FONGEOSEC, qui vise à développer la filière de la géothermie profonde en France avec la conception d’un démonstrateur d’une centrale de production d’énergie géothermique dans le bassin Rhénan. Ce projet est piloté par Fonroche Géothermie, qui gère un consortium de plus de dix acteurs du milieu académique et industriel. Le financement du projet est réalisé avec participation de l’Agence de l’Environnement et de la Maîtrise de l’Énergie (ADEME). Ainsi, les travaux exposés dans ce document se sont intéressés à la caractérisation thermodynamique des fluides géothermaux (saumures chaudes contenant des gaz dissous) de la région ciblée par le projet. Il est nécessaire de déterminer la solubilité de chacun des gaz dissous dans ces saumures aux conditions de pression, température et salinité de l’exploitation géothermique. Des modèles thermodynamiques de prévision des équilibres entre phases liquide et vapeur peuvent être utilisés pour estimer ces solubilités. Néanmoins, en absence des mesures expérimentales dans les conditions de pression, température et salinité d’intérêt, pour effectuer la régression de paramètres de ces modèles, il sera difficile d’obtenir avec précision ces solubilités à partir de simulations. Ainsi, cette thèse est centrée sur l’étude expérimentale des solubilités des gaz dans des saumures représentatives des fluides du bassin Rhénan. La gamme de pression de FONGEOSEC va de 6.0 MPa à 40.0 MPa pour des températures de 333.15 K et 453.15 K. Le dispositif expérimental utilisé dans cette thèse fonctionne dans ces conditions. Les gaz dissous dans les saumures visées par le projet sont constitués essentiellement de dioxyde de carbone (CO2), puis d’azote (N2) et enfin de méthane (CH4) en plus faibles quantités. Les sels dissous dans ces fluides sont surtout du chlorure de sodium et du chlorure de calcium, à molalité de 1.2 mol NaCl-0.2 mol CaCl2.Kg H2O-1. Dans cette thèse, nous avons effectué la détermination expérimentale de la solubilité du dioxyde de carbone dans des saumures typiques du bassin Rhénan aux conditions de pression et de température du projet FONGEOSEC. Des réflexions sont proposées quant à une méthodologie d’analyse de solubilité du méthane et de l’azote dans des phases aqueuses. Nous observons aussi que dans les conditions de pression et température de fond du puits, la solubilité du dioxyde de carbone dans les saumures typiques du bassin Rhénan est la plus élevée parmi toutes les conditions caractérisées. Une étude du sating-out effect dans ces saumures est également proposée dans cette thèse. Enfin, il est remarqué que le modèle de Pitzer (Pitzer.dat sur PhreeqC) semble prédire de façon correcte nos mesures expérimentales à 333.15 K, mais il perd son efficacité à 453.15 K. Dans cette condition, le modèle E-NRTL (Simulis®) semblerait être plus approprié. / This thesis was part of the FONGEOSEC project, which aims to develop the deep geothermal energy sector in France through the the design of a geothermal power pilot plant on the Upper Rhine Graben. This project is controled by Fonroche Géothermie, which manages a consortitium of more than ten academic and industrial partners. The French Environment & Energy Management Agency (ADEME) participates at the fundings of the project.Therefore, the work exposed in this document concerns the thermodynamic characterisation of geothermal fluids (hot brines containing dissolved gases) from the target region of this project. It is thus necessary to determine the solubility of each gas dissolved in these brines at the pressure, temperature and salinity conditions of geothermal energy exploitation.Thermodynamic models that predict liquid-vapour phase equilibrium can be used to estimate these solubilities. However, if there is a lack of experimental measures on the pressure, temperature and salinity conditions of interest, it will not be possible to regress these models interaction parameters and, therefore, it will be difficult to have precise solubility results from these thermodynamic simulations. Thus, this thesis has focused on the experimental study of gas solubilities in brines representing the Upper Rhine Graben fluids. The pressure range of the FONGEOSEC project goes from 6.0 MPa to 40.0 MPa for temperatures of 333.15 K and 453.15 K. The experimental setup used on this thesis can operate at these conditions. Dissolved gases in the brines concerned by this project are mainly composed by carbon dioxyde (CO2), and then by nitrgen (N2) and methane (CH4) at lower quantitites. Dissolved salts in these fluids are basically chloride sodium and chloride calcium, at molalities of 1.2 mol NaCl-0.2 mol CaCl2.Kg H2O-1.On the scope of this thesis, we have performed the experimental determination of carbon dioxyde solubility in Upper Rhine Graben-type brines at the pressure and temperature conditions of the FONGEOSEC project. We propose a discussion about an analysis methodology for measuring nitrogen and methane solubility in aqueous phases. We also observed that at the pressure and temperature conditions found at the bottom of the production well, carbon dioxyde solubility in the Upper Rhine Graben-type brines reaches its highest value among all the conditions studied in this thesis. A salting-out effect study in these brines is also proposed in this document. Finally, it is noticed that the Pitzer model (Pitzer.dat at PhreeqC) seems to predict properly our experimental data at 333.15 K, but it is less efficient at 453.15 K. In this condition, the E-NRTL model (Simulis®) seems to be more appropriate.

La planète Mars a connu une période où l'eau liquide était durablement stable. Outre les vestiges morphologiques d'une activité hydrologique en surface, l'interaction chimique de l'eau avec la croûte basaltique s'est traduite par la formation d'argiles et de sels hydratés en surface et en profondeur. Ces minéraux hydratés ont été détectés à la surface de Mars en 2004 grâce à l'instrument OMEGA, l'imageur hyperspectral infrarouge proche embarqué sur la sonde européenne Mars Express. Leur étude permet de reconstruire l'histoire de l'activité aqueuse sur Mars et de caractériser une période ancienne où l'environnement a pu être favorable à l'apparition d'une chimie pré-biotique. Ce travail de thèse s'intéresse aux environnements aqueux de Mars en couplant les données minéralogiques des imageurs hyperspectraux embarqués OMEGA/Mars Express et CRISM/Mars Reconnaissance Orbiter avec la morphologie. De nouveaux outils de traitement et d'analyse des données sont développés et ont permis la détection et la caractérisation spectrale de plus d'un millier de dépôts de minéraux hydratés sur Mars, fournissant une vue d'ensemble de l'altération. Celle-ci a eu lieu principalement dans la première partie du Noachien et a surtout formé des phyllosilicates ferro-magnésiens de la famille des vermiculites et smectites. Une importante diversité minérale est par ailleurs constatée avec une dizaine de familles minérales différentes, traçants des conditions géo-chimiques variées. Placés dans leur contexte géologique, certaines détections permettent de proposer l'existence passée d'un système hydrologique sur l'ensemble de la planète qui a donné naissance à un cycle des argiles similaire au cycle terrestre. Il apparait par ailleurs que les cratères d'impact sont le contexte privilégié des minéraux hydratés, mais le lien entre ces derniers et les processus d'impact demeure ambigu. La découverte d'un cycle des argiles est compatible avec l'hypothèse d'une planète potentiellement habitable au Noachien mais qui devra être vérifiée par l'exploration in-situ. / The planet Mars has experienced an era during which water was stable in its liquid state. In addition to morphological evidence for aqueous activity, the chemical interaction of water with the basaltic crust has led to the formation of hydrated clays and salts both on the surface and at depth. These hydrated minerals were first detected on the surface of Mars in 2004 with the OMEGA near infrared imaging spectrometer, onboard European probe Mars Express. Their study allows us to piece together the aqueous activity on Mars and to better understand an early era when the environment may have been conducive to prebiotic chemistry. This work focuses on the aqueous environments on Mars by coupling mineralogy data from the spaceborne imaging spectrometers OMEGA/Mars Express and CRISM/Mars Reconnaissance Orbiter to the surface morphology. The development of new data processing and analysis tools have led to the detection and spectral inquiry of over a thousand hydrated mineral exposures on Mars, thus providing a broad view of the aqueous alteration. The latter mostly took place during the Noachian era and formed primarily iron-magnesium bearing phyllosilicates of the vermiculite and smectite groups. In addition, great mineral diversity is found, implying varied geo-chemical formation conditions. Placed in their geological context, these detections show the likely existence of a past hydrological cycle on Mars which sustained a clay cycle similar to Earth's. It was also found that impact craters are the most common morphological context for these minerals, although the link between them remains unclear. The discovery of a clay cycle on Mars bodes well for the past habitability potential on Mars, but will need to be verified through in-situ exploration.

Des recherches sur de nouvelles sources énergétiques ont été initiées pour faire face à la hausse de la demande mondiale. Dans le domaine nucléaire, la filière Th-U est envisagée pour compléter ou remplacer la filière U-Pu. Toutefois, des améliorations technologiques sont nécessaires avant l’aboutissement industriel de ce projet, notamment sur l’adaptation du procédé de retraitement du combustible U-Pu à celui du cycle Th-U, qui consiste à dissoudre le combustible en milieu acide nitrique, suivi d’une extraction liquide-liquide. Or, contrairement à l’uranium, l’oxyde de thorium n’est pas soluble dans HNO₃ concentré. Un ajout de petites quantités de fluorures est nécessaire à l’obtention d’une dissolution totale. Cependant, la dissolution reste lente et le milieu HNO₃-HF est très corrosif. L’objectif de cette étude est de comprendre les réactions mises en jeu afin d’optimiser la composition de la solution pour diminuer la corrosion et améliorer la cinétique de dissolution. La poudre d’oxyde de thorium synthétisée en laboratoire est solubilisée dans des conditions expérimentales et selon un protocole prédéfinis. L’effet des caractéristiques du solide, de la méthode de dissolution et du milieu de dissolution ont été étudiés. La morphologie de l’oxyde a une forte influence sur la vitesse de dissolution. L’impact majeur des ultrasons de puissance est l’augmentation de la température, qui améliore considérablement la vitesse de dissolution. Le remplacement des fluorures par d’autres complexants du thorium n’a pas permis d’atteindre une dissolution quantitative de l’oxyde. L’augmentation des concentrations de HF et de HNO₃ accélère la dissolution, mais une concentration trop importante de fluorure mène à la formation d’un précipité blanc qui passive la surface. Sur la base de cette étude, un mécanisme réactionnel a été proposé. L’étape limitante est la formation d’un complexe activé. L’écriture et la résolution des équations cinétiques et des équilibres thermodynamiques a permis d’établir une relation analytique exprimant le taux de dissolution de ThO₂ en fonction des paramètres expérimentaux. La simulation des résultats expérimentaux à l’aide de cette relation a ensuite permis de déterminer les constantes thermodynamiques et cinétiques rendant compte de tous les phénomènes observés, validant ainsi le mécanisme proposé. / Studies of new energy sources are necessary to meet the rising global demand. In the nuclear area, Th-U cycle has been reinvestigated to supplement or replace the currently used U-Pu cycle. This project though needs further improvement to be operated in an industrial plant, especially on the reprocessing process, which consists in fuel dissolution in nitric acid medium, followed by liquid-liquid extraction. Still, unlike uranium, thorium oxide does not dissolve in concentrated nitric acid. Small amounts of fluoride are required to achieve the dissolution. The dissolution is rather slow and HNO₃-HF mixture is very corrosive. The aim of this project is thus to find an efficient dissolution method which both decreases corrosion and improves dissolution rate. The synthetized thorium oxide powder has been dissolved in chosen conditions. Effects of solid parameters, dissolution method and dissolution medium have been studied. Results show a strong dependence on oxide crystallinity. No improvement on dissolution rate was observed with power ultrasounds, except for the temperature increase, which greatly enhances dissolution rate. No other complexing agents than fluoride allows total dissolution. Rising HNO₃ and HF concentrations increases dissolution rate until the amount of fluorides is so high that a precipitate forms at the surface. This study led to the proposal of a dissolution mechanism whose limiting step is the formation of an activated complex. Based on kinetics and equilibrium equations, initial dissolution rate was then written as a function of the different studied parameters. Experimental results were finally fitted by this relation to find kinetics and thermodynamics constants, proving the accuracy of the proposed mechanism.

Ice-templating, znm tak© jako freeze-casting, je relativnÄ jednoduchou, levnou a velmi univerzln­ technikou pro vrobu por©zn­ch keramickch struktur s ­zenou mikrostrukturou. Takto pipraven© keramick© struktury jsou pouity pro vrobu hybridn­ch keramickch kompozit, nebo jako biokeramick© scaffoldy. Hybridn­ keramick© kompozitn­ materily jsou zaloeny na napodobovn­ p­rodn­ch/ biologickch materil. Hlavn­m c­lem je napodobit v p­rodÄ se vyskytuj­c­ zhouevnauj­c­ mechanismy t­m, e por©zn­ keramick© struktury jsou po slinut­ naputÄny polymern­mi materily. Hlavn­m probl©mem pi vrobÄ por©zn­ch keramickch vzork s velkmi rozmÄry, pomoc­ metody ice-templating, je dosaen­ ­zen©ho rstu ledovch krystal v cel©m objemu vzorku. Aby tedy bylo mon© z­skat velk© keramick© vzorky s dobe definovanou lamelrn­ strukturou je teba proces ice-templatingu velmi pesnÄ kontrolovat. Biologick aktivita biokeramickch materil zvis­ na kombinaci fyzikln­ch a chemickch charakteristik, kter© silnÄ souvisej­ s jejich mikrostrukturou. Porozita scaffold mus­ bt vzjemnÄ propojen a velikost­ pr dostateÄnÄ velk pro spÄn rst kostn­ tknÄ v cel©m objemu implanttu. Prezentovan disertaÄn­ prce je zamÄena na problematiku zvÄtovn­ rozmÄr keramickch vzork pipravench pomoc­ metody ice-templating, vytvoen­ v­cerovov© porozity uvnit vzork a vrobu hybridn­ch keramickch kompozit pro balistickou ochranu. Keramick© suspenze pro ice-templating byly spÄnÄ pipraveny z rznch prk (zejm©na hydroxyapatitu a oxidu hlinit©ho s rznm plnÄn­m keramick©ho prku od 7,5 obj.% do 45 obj.%. Byl tak© studovn vliv aditiv na utven­ lamelrn­ drsnosti a mezilamelrn­ch pemostÄn­. V souÄasnosti je zkoumn dopad tÄchto strukturn­ch prvk na vsledn© mechanick© vlastnosti. Hybridn­ kompozity oxid hlinit/polymer byly spÄnÄ navreny a pipraveny z destiÄek z oxidu hlinit©ho pipravench metodou ice-templating s d©lkou lamel a 70 mm a rznch polymern­ch pryskyic. Byla testovny mechanick© vlastnosti hybridn­ch kompozit oxid hlinit/polymer a vsledky ukzaly, e ice-templating je robustn­ metodou pro vrobu hybridn­ch kompozit keramika-polymer s dobrm pomÄrem pevnost/hustota. Avak balistick© testy hybridn­ch kompozit oxid hlinit/polymer odhalily, e vÄtina kompozit vytvoench v rmci t©to prce nebyla schopna ÄinnÄ zastavit stely s prbojnm jdrem. Ukzalo se, e kombinace procesu ice-templating a nep­m©ho 3D tisku umouje vrobu biokeramickch scaffold pro kostn­ nhrady z hydroxyapatitu s v­cerovovou porozitou, co by se mohlo ukzat jako prospÄn© pro vvoj bioaktivn­ch vysoce por©zn­ch scaffold se zvenou biologickou aktivitou. Ice-templating tak© vznamnÄ ovlivnil zmÄnu fzov©ho sloen­ bÄhem slinovn­ hydroxyapatitovch vzork.

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Die chemische Zusammensetzung und die physikalischen Eigenschaften von troposphärischen Gasen, Partikeln und Wolken hängen aufgrund zahlreicher Prozesse stark voneinander ab. Insbesondere chemische Multiphasenprozesse in Wolken können die physiko-chemischen Eigenschaften der Luft und troposphärischer Partikel klein- und großräumig verändern. Diese chemische Prozessierung des troposphärischen Aerosols innerhalb von Wolken beeinflusst die chemischen Umwandlungen in der Atmosphäre, die Bildung von Wolken, deren Ausdehnung und Lebensdauer, sowie die Transmissivität von einfallender und ausgehender Strahlung durch die Atmosphäre. Damit sind wolken-chemische Prozesse relevant für das Klima auf der Erde und für verschiedene Umweltaspekte. Daher ist ein umfassendes Verständnis dieser Prozesse wichtig. Die explizite Behandlung chemischer Reaktionen in der Flüssigphase stellt allerdings eine Herausforderung für atmosphärische Computermodelle dar. Detaillierte Beschreibungen der Flüssigphasenchemie werden deshalb häufig nur für Boxmodelle verwendet. Regionale Chemie-Transport-Modelle und Klimamodelle berücksichtigen diese Prozesse meist nur mit vereinfachten chemischen Mechanismen oder Parametrisierungen. Die vorliegende Arbeit hat zum Ziel, den Einfluss der chemischer Mehrphasenprozesse innerhalb von Wolken auf den Verbleib relevanter Spurengase und Partikelbestandteile mit Hilfe des state‑of‑the‑art 3D-Chemie-Transport-Modells COSMO-MUSCAT zu untersuchen. Zu diesem Zweck wurde das Model um eine detaillierte Beschreibung chemischer Prozesse in der Flüssigphase erweitert. Zusätzlich wurde das bestehende Depositionsschema verbessert, um auch die Deposition von Nebeltropfen zu berücksichtigen. Die durchgeführten Modellerweiterungen ermöglichen eine bessere Beschreibung des troposphärischen Multiphasensystems. Das erweiterte Modellsystem wurde sowohl für künstliche 2D-Bergüberströmungsszenarien als auch für reale 3D-Simulationen angewendet. Mittels Prozess- und Sensitivitätsstudien wurde der Einfluss (i) des Detailgrades der verwendeten Mechanismen zur Beschreibung der Flüssigphasenchemie, (ii) der Größenauflösung des Tropfenspektrums und (iii) der Tropfenanzahl auf die chemischen Modellergebnisse untersucht. Die Studien belegen, dass die Auswirkungen der Wolkenchemie aufgrund ihres signifikanten Einflusses auf die Oxidationskapazität in der Gas- und Flüssigphase, die Bildung von organischer und anorganischer Partikelmasse sowie die Azidität der Wolkentropfen und Partikel in regionalen Chemie-Transport-Modellen berücksichtigt werden sollten. Im Vergleich zu einer vereinfachten Beschreibung der Wolkenchemie führt die Verwendung des detaillierten chemischen Flüssigphasenmechanismus C3.0RED zu verringerten Konzentrationen wichtiger Oxidantien in der Gasphase, einer höheren Nitratmasse in der Nacht, geringeren nächtlichen pH-Werten und einer veränderten Sulfatbildung. Darüber hinaus ermöglicht eine detaillierte Wolkenchemie erst Untersuchungen zur Bildung sekundärer organischer Partikelmasse in der Flüssigphase. Die größenaufgelöste Behandlung der Flüssigphasenchemie hatte nur geringen Einfluss auf die chemischen Modellergebnisse. Schließlich wurde das erweiterte Modell für Fallstudien zur Feldmesskampagne HCCT‑2010 genutzt. Zum ersten Mal wurde dabei ein chemischer Mechanismus mit der Komplexität von C3.0RED verwendet. Die räumlichen Effekte realer Wolken z. B. auf troposphärische Oxidantien oder die Bildung anorganischer Masse wurden untersucht. Der Vergleich der Modellergebnisse mit verfügbaren Messungen hat viele Übereinstimmungen aber auch interessante Unterschiede aufgezeigt, die weiter untersucht werden müssen. / In the troposphere, a vast number of interactions between gases, particles, and clouds affect their physico-chemical properties, which, therefore, highly depend on each other. Particularly, multiphase chemical processes within clouds can alter the physico-chemical properties of the gas and the particle phase from the local to the global scale. This cloud processing of the tropospheric aerosol may, therefore, affect chemical conversions in the atmosphere, the formation, extent, and lifetime of clouds, as well as the interaction of particles and clouds with incoming and outgoing radiation. Considering the relevance of these processes for Earth\''s climate and many environmental issues, a detailed understanding of the chemical processes within clouds is important. However, the treatment of aqueous phase chemical reactions in numerical models in a comprehensive and explicit manner is challenging. Therefore, detailed descriptions of aqueous chemistry are only available in box models, whereas regional chemistry transport and climate models usually treat cloud chemical processes by means of rather simplified chemical mechanisms or parameterizations. The present work aims at characterizing the influence of chemical cloud processing of the tropospheric aerosol on the fate of relevant gaseous and particulate aerosol constituents using the state-of-the-art 3‑D chemistry transport model (CTM) COSMO‑MUSCAT. For this purpose, the model was enhanced by a detailed description of aqueous phase chemical processes. In addition, the deposition schemes were improved in order to account for the deposition of cloud droplets of ground layer clouds and fogs. The conducted model enhancements provide a better insight in the tropospheric multiphase system. The extended model system was applied for an artificial mountain streaming scenario as well as for real 3‑D case studies. Process and sensitivity studies were conducted investigating the influence of (i) the detail of the used aqueous phase chemical representation, (ii) the size-resolution of the cloud droplets, and (iii) the total droplet number on the chemical model output. The studies indicated the requirement to consider chemical cloud effects in regional CTMs because of their key impacts on e.g., oxidation capacity in the gas and aqueous phase, formation of organic and inorganic particulate mass, and droplet acidity. In comparison to rather simplified aqueous phase chemical mechanisms focusing on sulfate formation, the use of the detailed aqueous phase chemistry mechanism C3.0RED leads to decreased gas phase oxidant concentrations, increased nighttime nitrate mass, decreased nighttime pH, and differences in sulfate mass. Moreover, the treatment of detailed aqueous phase chemistry enables the investigation of the formation of aqueous secondary organic aerosol mass. The consideration of size-resolved aqueous phase chemistry shows only slight effects on the chemical model output. Finally, the enhanced model was applied for case studies connected to the field experiment HCCT-2010. For the first time, an aqueous phase mechanism with the complexity of C3.0RED was applied in 3‑D chemistry transport simulations. Interesting spatial effects of real clouds on e.g., tropospheric oxidants and inorganic mass have been studied. The comparison of the model output with available measurements revealed many agreements and also interesting disagreements, which need further investigations.