A caracterização de rochas de reservatórios por microtomografia de raios X (MRX) consiste em uma técnica de análise digital para estudar tridimensionalmente microestruturas e formações geológicas. Para materiais geológicos porosos, a distinção do corpo mineral e dos vazios é facilmente realizada devido à diferença de atenuação dos raios X irradiados, fornecendo modelos tridimensionais de tamanho de grão, porosidade e estrutura de poros. Os métodos tradicionais de petrologia, como a microscopia óptica ou a microscopia eletrônica de varredura (MEV), apresentam menor significância estatística para a área analisada e são limitados à análise bidimensional; assim o MRX apresenta um avanço para as técnicas de caracterização por aquisição e análise digital de imagens. Paralelamente, são conhecidas outras técnicas experimentais para caracterização de porosidade de materiais geológicos por intrusão de fluidos ou envelopamento de partículas. Destas, destaca-se a porosimetria com intrusão de mercúrio que atua no intervalo de poros micro a nanométricos, e possibilita também a determinação da distribuição de tamanho de poros. Este trabalho tem por objetivo determinar a porosidade e densidade de análogos de rocha reservatório pela conjugação de procedimentos de MRX bi e tridimensionais, porosimetria por intrusão de mercúrio e picnometria com gás Hélio. As condições operacionais foram previamente avaliadas até se estabelecer parâmetros capazes de gerar resultados reprodutíveis e com elevada repetitividade. Os resultados demonstram que as melhores correlações foram estabelecidas entre os resultados da porosimetria com mercúrio e microtomografia tridimensional, considerando-se a mesma resolução de tamanho de poro. Apesar dos princípios serem distintos e das comparações serem entre medidas indiretas e análise de imagens digitais, ambas são medidas volumétricas. Na avaliação de continuidade de poros, a correlação entre as determinações bi e tridimensionais revela presença de heterogeneidades. As determinações de densidade por porosimetria com mercúrio e picnometria com gás hélio são congruentes, desde que a quantidade de poros fechados não seja significativa em relação à porosidade total. A microscopia de raios X contribui significativamente para análise digital de rochas reservatório com possibilidade de determinação de porosidade, distribuição de tamanho, morfologia e conectividade de poros. Com a proibição iminente do uso de mercúrio por restrições ambientais, a MRX se torna uma suplente possível para estudos de materiais com porosidades micrométricas, com limitações na detecção poros nanométricos. / Reservoir rock characterization by X-ray microtomography (XRM) consists of a digital analysis to study microstructures and geological formations. The distinction of matrix and voids within the rock sample can be easily carried out due to the attenuation difference of irradiated X-rays, providing three-dimensional models of grain size, porosity and pore structure. Traditional petrology methods, such as optical microscopy or scanning electron microscopy (SEM) presents lower statistical significance for the characterized area and are limited to two-dimensional analysis; therefore, XRM presents an advance for characterization techniques by acquisition and digital image analysis. At the same time, experimental techniques are known for porosity characterization of geological materials by fluid intrusion or particle envelopment. It can be emphasized the mercury intrusion porosimetry acts in the range of micro and nanopores and also allows the analysis of pore size distribution. This study aims to determine porosity and density of reservoir rock analogous by the combination of two and three dimensional XRM procedures, mercury intrusion porosimetry and helium gas pycnometry. Operating parameters were prior evaluated to establish conditions for obtaining reproducible results with high repeatability. The results were assessed individually with subsequent correlations under the same resolution. The results demonstrate that the best correlations were established between mercury porosimetry and three-dimensional microtomography data, considering the same pore size resolution. Although the principles are completely different, and the comparisons refers to indirect measurements and digital image analysis, both considers volumetric measurements. In the evaluation of pore continuity, the correlation between two and three-dimensional determinations reveals the presence of heterogeneities. The density determinations by mercury intrusion porosimetry and pycnometry with helium gas are congruent, as long as the number of closed pores is not significant in relation to the total porosity. X-ray microscopy contributes significantly to reservoir rock digital analysis with the possibility of determining porosity, pore size distribution, morphology and pore connectivity. With the mercury use prohibition by environmental constraints, MRX becomes a possible substitute to characterize materials with micrometric porosities, with limitations in the detection of nanometric pores.

Cette thèse présente un ensemble de résultats expérimentaux sur une argile remaniée non saturée proche de la saturation, dont le degré de saturation est généralement supérieur à 70%.Après une série d’essais de caractérisation physique et mécanique du matériau, plusieurs méthodes expérimentales ont été utilisées pour étudier le comportement et certaines pathologies du sol compacté telles que l’orniérage et le matelassage.Une étude systématique du comportement du sol compacté sur chemins de drainage-humidification dans différents états initiaux a été effectuée, complétée par des mesures de succion par papier filtre et psychromètre. Les essais de porosimétrie par intrusion de mercure ont apporté un éclairage sur la microstructure du sol.La thèse a également permis d’étudier les variations de pression interstitielle du sol compacté sur chemin triaxial non drainé en utilisant la technique de translation d’axes, où quelques améliorations et modifications du montage ont été proposées. / This thesis present an experimental study of an unsaturated clayey soil close to saturation, whose degree of saturation is generally above 70%.After characterizing the physical and mechanical properties of the material, several experimental methods were used to study the behaviour and some pathologies of the compacted soil, such as rutting and quilting.A systematic study of the behaviour of the compacted soil on drying-wetting paths starting from different initial states was carried out, completed by suction measurements using filter-paper and psychrometer. Mercury intrusion porosimetry tests gave an insight of the soil microstructure.The thesis also addressed the question of the pore pressure variations of the compacted soil on undrained triaxial path using the axis-translation technique, where some improvements and modifications of the testing device were proposed.

A caracterização de rochas de reservatórios por microtomografia de raios X (MRX) consiste em uma técnica de análise digital para estudar tridimensionalmente microestruturas e formações geológicas. Para materiais geológicos porosos, a distinção do corpo mineral e dos vazios é facilmente realizada devido à diferença de atenuação dos raios X irradiados, fornecendo modelos tridimensionais de tamanho de grão, porosidade e estrutura de poros. Os métodos tradicionais de petrologia, como a microscopia óptica ou a microscopia eletrônica de varredura (MEV), apresentam menor significância estatística para a área analisada e são limitados à análise bidimensional; assim o MRX apresenta um avanço para as técnicas de caracterização por aquisição e análise digital de imagens. Paralelamente, são conhecidas outras técnicas experimentais para caracterização de porosidade de materiais geológicos por intrusão de fluidos ou envelopamento de partículas. Destas, destaca-se a porosimetria com intrusão de mercúrio que atua no intervalo de poros micro a nanométricos, e possibilita também a determinação da distribuição de tamanho de poros. Este trabalho tem por objetivo determinar a porosidade e densidade de análogos de rocha reservatório pela conjugação de procedimentos de MRX bi e tridimensionais, porosimetria por intrusão de mercúrio e picnometria com gás Hélio. As condições operacionais foram previamente avaliadas até se estabelecer parâmetros capazes de gerar resultados reprodutíveis e com elevada repetitividade. Os resultados demonstram que as melhores correlações foram estabelecidas entre os resultados da porosimetria com mercúrio e microtomografia tridimensional, considerando-se a mesma resolução de tamanho de poro. Apesar dos princípios serem distintos e das comparações serem entre medidas indiretas e análise de imagens digitais, ambas são medidas volumétricas. Na avaliação de continuidade de poros, a correlação entre as determinações bi e tridimensionais revela presença de heterogeneidades. As determinações de densidade por porosimetria com mercúrio e picnometria com gás hélio são congruentes, desde que a quantidade de poros fechados não seja significativa em relação à porosidade total. A microscopia de raios X contribui significativamente para análise digital de rochas reservatório com possibilidade de determinação de porosidade, distribuição de tamanho, morfologia e conectividade de poros. Com a proibição iminente do uso de mercúrio por restrições ambientais, a MRX se torna uma suplente possível para estudos de materiais com porosidades micrométricas, com limitações na detecção poros nanométricos. / Reservoir rock characterization by X-ray microtomography (XRM) consists of a digital analysis to study microstructures and geological formations. The distinction of matrix and voids within the rock sample can be easily carried out due to the attenuation difference of irradiated X-rays, providing three-dimensional models of grain size, porosity and pore structure. Traditional petrology methods, such as optical microscopy or scanning electron microscopy (SEM) presents lower statistical significance for the characterized area and are limited to two-dimensional analysis; therefore, XRM presents an advance for characterization techniques by acquisition and digital image analysis. At the same time, experimental techniques are known for porosity characterization of geological materials by fluid intrusion or particle envelopment. It can be emphasized the mercury intrusion porosimetry acts in the range of micro and nanopores and also allows the analysis of pore size distribution. This study aims to determine porosity and density of reservoir rock analogous by the combination of two and three dimensional XRM procedures, mercury intrusion porosimetry and helium gas pycnometry. Operating parameters were prior evaluated to establish conditions for obtaining reproducible results with high repeatability. The results were assessed individually with subsequent correlations under the same resolution. The results demonstrate that the best correlations were established between mercury porosimetry and three-dimensional microtomography data, considering the same pore size resolution. Although the principles are completely different, and the comparisons refers to indirect measurements and digital image analysis, both considers volumetric measurements. In the evaluation of pore continuity, the correlation between two and three-dimensional determinations reveals the presence of heterogeneities. The density determinations by mercury intrusion porosimetry and pycnometry with helium gas are congruent, as long as the number of closed pores is not significant in relation to the total porosity. X-ray microscopy contributes significantly to reservoir rock digital analysis with the possibility of determining porosity, pore size distribution, morphology and pore connectivity. With the mercury use prohibition by environmental constraints, MRX becomes a possible substitute to characterize materials with micrometric porosities, with limitations in the detection of nanometric pores.

Natural and other aggregated or structured soils present peculiar mechanical behaviour which differs, in some parts, from the behaviour of soils reconstituted in laboratory. This difference can be explained by a specific structure which gathers the particles arrangement and bonding. However, numerous constitutive models were originally based on the behaviour of reconstituted soils. Therefore, classical models should be extended in order to reproduce more complex features of behaviour linked to the soil structure. This work provides a general framework to describe and predict the behaviour of aggregated and reconstituted soils. A multi-scale study was performed to understand the effect of the structure and its evolution upon loading. From an experimental point of view, a preliminary review of literature has been completed by an experimental program carried out on a silty soil in which different structures have been generated by various compaction conditions. At the macro-scale, conventional mechanical tests evidence the overconsolidation effect induced by structure and the important compressibility during its degradation. At the micro-scale, the fabric evolution during the destructuration process (induced by saturation and loading) has been mainly quantified by the evolution of the pore size distribution. This characterisation has been done by Mercury Intrusion Porosimetry. The samples compacted on the dry side of optimum exhibit a double porosity characterized by a bimodal pore size distribution, by opposition to the samples compacted on wet side of optimum that show a single class of pores. The deformation induced by mechanical loading is related to the closure of the biggest pores and the pore size distribution of aggregated soils tends towards unimodal shape upon the destructuration process. A constitutive critical state model (ACMEG) has been extended, based on experimental observations, in order to reproduce the behaviours of aggregated and reconstituted soils. In this purpose, a structure variable has been introduced in the yield function and its evolution has been integrated in the hardening law. Explicit and implicit methods of integration have been discussed and implemented to reproduce stress-strain responses on geomechanical tests (oedometric, isotropic and triaxial compression tests). Finally, the model has been validated by comparison of model predictions with the experimental results. / Doctorat en Sciences de l'ingénieur et technologie / info:eu-repo/semantics/nonPublished

The content of this diploma thesis was testing the applicability of available structural analysis techniques on a appropriate model hydrogel system. The main aim was to evaluate the advantages and disadvantages of selected structural analysis techniques and the influence of the composition change of the hydrogel system on its internal structure. Semi-interpenetrated hydrogels based on agarose of different concentration were chosen as model system, this type of material was chosen for simple and repeatable preparation and also for its application potential. Electron microscopy (SEM, cryoSEM), mercury porosimetry and turbidimetry were chosen as structural analysis techniques. Experimental results could be used to improve knowledge about the influence of hydrogel composition on its structure and the comparison of chosen techniques will be used for the choice of appropriate structural analysis in the future, which will be applicable to other hydrogel systems as well.

The aim of this study was to determine the effect of quicklime (1 - 8% CaO) and maturation time (1 - 540 days) on the structure of clayey soil compacted at optimum moisture content by Proctor standard energy and whether expected change in structure affects the long - term permeability. The change of pore space of compacted loess with 1-8% lime (CaO) was studied by mercury porosimetry (MIP) for a long period of maturation (from 1 to 540 days). Development of pozzolanic reactions were monitored by measuring the pH. The development of new mineral phases (calcium silicate hydrates, calcium aluminate hydrates and calcium aluminate carbonate hydrate) in the treated soil was investigated by using X-Ray diffraction. The MIP indicated that 2% of CaO were sufficient for long term pozzolanic reaction. The threshold value is below the initial consumption of lime determined from the pH measurements (Eades and Grim, 1966). The alteration of the voids of the lime treated soil is noticeable, but the pH value can not drop below 11.7. At 4% of CaO, at 8% of CaO respectively, the macroporosity kept decreasing due to increasing mesoporosity for 360 curing days, for 540 curing days respectively, due to the new mineral phases. At 2% of CaO, the decrease of the macroporosity stops after 120 days. Below 2% of lime, the...

Alterations of fluid phase transitions in porous materials are conventionally employed for the characterization of mesoporous solids. In the first approximation, this may be based on the application of the Kelvin equation for gas–liquid and the Gibbs–Thomson equation for solid–liquid phase equilibria for obtaining pore size distributions. Herein, we provide a comparative analysis of different phase coexistences measured in mesoporous silica solids with different pore sizes and morphology. Instead of comparing the resulting pore size distributions, we rather compare the transitions directly by using a common coordinate for varying the experiment’s thermodynamic parameters based on the two equations mentioned. Both phase transitions in these coordinates produce comparable results for mesoporous solids of relatively large pore sizes. In contrast, marked differences are found for materials with smaller pore sizes. This illuminates the fact that, with reducing confinement sizes, thermodynamic fluctuations become increasingly important and different for different equilibria considered. In addition, we show that in the coordinate used for analysis, mercury intrusion matches perfectly with desorption and freezing transitions.

Background: Separation science is heavily reliant on materials to fulfill ever more complicated demands raised by other areas of science, notably the rapidly expanding molecular biosciences and environmental monitoring. The key to successful separations lies in a combination of physical properties and surface chemistry of stationary phases used in liquid chromatographic separation, and this thesis address both aspects of novel separation materials. Methods: The thesis accounts for several approaches taken during the course of my graduate studies, and the main approaches have been i) to test a wild-grown variety of published methods for surface treatment of fused silica capillaries, to ascertain firm attachment of polymeric monoliths to the wall of microcolumns prepared in silica conduits; ii) developing a novel porogen scheme for organic monoliths including polymeric porogens and macromonomers; iii) evaluating a mesoporous styrenic monolith for characterization of telomers intended for use in surface modification schemes and; iv) to critically assess the validity of a common shortcut used for estimating the porosity of monoliths prepared in microconduits; and finally v) employing plasma chemistry for activating and subsequently modifying the surface of rigid, monodisperse particles prepared from divinylbenzene. Results: The efforts accounted for above have resulted in i) better knowledge of the etching and functionalization parameters that determine attachment of organic monoliths prepared by radical polymerization to the surface of silica; ii) polar methacrylic monoliths with a designed macroporosity that approaches the desired "connected rod" macropore morphology; iii) estab¬lishing the usefulness of monoliths prepared via nitroxide mediated polymerization in gradient polymer elution chromatography; iv) proving that scanning electron microscopy images are of limited value for assessing the macroporous properties of organic monoliths, and that pore measurements on externally polymerized monolith cocktails do not represent the porous properties of the same cocktail polymerized in narrow confinements; and v) showing that plasma bromination can be used as an activation step for rigid divinylbenzene particles to act as grafting handles for epoxy-containing telomers, that can be attached in a sufficiently dense layer and converted into carboxylate cation exchange layer that allows protein separations in fully aqueous eluents.

No description available.

Colloidal assemblies of surfactants and polymers in aqueous solutions have been used by human mankind for hundreds of years and they are of great importance in many of our technological processes, such as fabrication of soap and papermaking. Less than two decades ago the idea of using colloidal assemblies as templates of inorganic materials was borne. A new population of materials, referred to as surfactant templated materials, took form. These materials showed extraordinary properties such as monodisperse pore size distribution, large surface areas and pore volumes.   The main focus of this thesis has been on synthesis and functionalisation of spherical mesostructured silica particulate materials. In the first part of the work, mesostructured materials with expanded pores have been produced using a well established aerosol-based method as well as the newly developed emulsion and solvent evaporation (ESE) method. Increase in pore size was realized through using Pluronic block copolymer F127 together with a swelling agent poly(propylene glycol) as template. The influence of the swelling agent on pore size expansion was shown to have a roughly linear relationship. Furthermore, the impact of synthesis parameters on internal and exterior morphology has been investigated. Accessibility of the internal pore space, as well as the external surface roughness were shown to be highly dependent on synthesis temperature. Additionally, a very interesting well ordered 3D closed packed (P63/mmc) material was produced using the ionic surfactant C16TAB as template in the ESE method.   In the second part of the thesis work, mesoporous spheres with large pore size, having either hydrophilic or hydrophobic surface properties, were used as carriers of an enzyme, lipase. The enzymatic activity of lipase was increased onto the hydrophobic surface, compared to lipase immobilized into the hydrophilic support as well as for lipase free in solution. This effect was probably due to a combination of enhanced hydrophobic interactions preventing denaturation of the enzyme and interfacial activation of the enzyme.  This study generated an inorganic carrier material that is a promising candidate for biocatalysis applications. Additionally, mesoporous spheres were used as carriers of a model drug, Ibuprofen, to study the effect of polyelectrolyte multilayers on release properties. However, these layers were shown impermeable independent on pH and the substance was only released from uncoated particles. / <p>QC 20100811</p>