Cette thèse porte sur l'étude de la caractérisation et le traitement de saumures alcalines. La carbonatation directe de saumures résiduaires (SR), par introduction d'une partie du CO2 issu de fumées industrielles, est réalisée dans un souhait de réduction des émissions de CO2 et en vue d'une valorisation potentielle des produits obtenus. Cette recherche se concentre sur l'étude des composés carbonatés, l'objectif général est d'établir le lien entre la réactivité des carbonates et leur valorisation (ici, désulfuration de fumées acides). Les SR sont complexes, l'étude de leur composition chimique et minéralogique a été réalisée en partie par spectroscopie Raman afin de mettre en évidence les interactions OH-Cl dans les échantillons humides. Les différents hydroxydes sont consommés au cours de la carbonatation pour précipiter des carbonates de calcium (calcite, aragonite). La composition chimique détermine les réactions de carbonatation alors que les paramètres physiques influencent la vitesse des réactions ainsi que la morphologie et la pureté des carbonates. L'évolution des phases au cours de la carbonatation des SR a été suivie par spectroscopie et un premier modèle statistique de prédiction des concentrations en carbonates a été développé. La deuxième partie de ce travail porte sur la caractérisation des carbonates obtenus et des paramètres, tel que l'hydratation, pouvant influencer leur valorisation. L'importance de l'hydratation dans la réactivité des produits DECALCO a été observée de l'échelle microscopique au pilote semi-industriel. Les essais de désulfuration de fumées acides ont été menés avec des taux de conversion du SO2 atteignant 65 à 70 % / This study is a contribution to the characterization and the treatment of alkaline industrial wastes. The direct carbonation of residual brines (RB) by CO2 bubbling results in a gas emission reduction and a potentially valorization of resulting products. This research was focused on carbonate products. The main objective is to link reactivity and valorization (here, desulfurization of industrial fumes). The RB are complex, their chemical and mineralogical composition was studied in particular by Raman spectroscopy to monitor OH-Cl interaction in humid samples. The different hydroxides phases are consumed during carbonation to precipitate calcium carbonates (calcite and aragonite). The chemical composition of RB determines the main part of the reaction of carbonation whereas physical parameters influence the reaction kinetics, the by-products morphology and purity. The feasibility of on-line monitoring of the phases evolution during carbonation using spectroscopy has been validated and a first statistical model for the prediction of carbonate concentration has been developed. The second part of this works concerns the characterization of precipitated carbonates and some parameters as hydration which can influence their valorization. The importance of hydration on the carbonates reactivity was observed in microscopy and at pilot scale. Desulfurization tests of industrial fumes in semi-humid way provided a conversion rate of SO2 ranging between 65 and 70%

Les Cendres Volantes d’Electrofiltres (CVE) d’incinération d’ordures ménagères sont considérées comme des déchets dangereux et mises en décharges après une phase de stabilisation et de solidification par un liant hydraulique. Leur utilisation dans des matériaux cimentaires permet l’élimination d’un déchet en diminuant la demande de matériaux de construction. Cependant, avant leur incorporation dans des matériaux cimentaires, les CVE doivent subir plusieurs traitements. Premièrement, un lavage à l’eau permet de diminuer fortement la concentration en chlorures. Dans un deuxième temps, une séparation granulométrique des CVE est appliquée afin de ne sélectionner que la fraction la moins contaminée en métaux lourds, notamment en plomb et en zinc, ces métaux lourds étant connus comme retardateurs de prise. Enfin, une troisième étape consiste à oxyder l’aluminium métallique présent dans les CVE à l’aide d’un lavage basique à l’hydroxyde de sodium. S’il n’est pas oxydé durant la phase de traitement, l’aluminium métallique se transforme en aluminates dans la matrice cimentaire tout en produisant de l’hydrogène, responsable de l’apparition de vides et de fissures endommageant ainsi le matériau. Une fois traitées, les CVE peuvent alors être utilisées en substitution partielle du ciment pour une étude de leur réactivité potentielle. Les résultats de cette étude ont montré que l’activité des CVE traitées à l’hydroxyde de sodium est principalement d’origine physique (granulométrique et surface développée). Les CVE ne présentent pas de nature pouzzolanique. Les essais de lixiviation ont montré une durabilité équivalente et une très bonne stabilisation du chrome, du plomb et du zinc, qui permet de respecter les normes environnementales européennes./Municipal Solid Waste Incineration (MSWI) Electrofilter Fly Ash (EFA) is considered as hazardous waste and landfilled after stabilisation and solidification with a hydraulic binder. Its use in cementitious materials allows the elimination of a waste and a decrease of construction materials use. However, before its incorporation in cementitious materials, EFA has to be treated. Firstly, a water washing allows an important decrease in chloride concentration. In a second time, size-based separation is used to select the less heavy metals contaminated fraction, especially in lead and zinc. Indeed, these heavy metals are knows as setting retarders. Finally, a third step involves oxidizing of metallic aluminium contained in EFA during a basic washing with sodium hydroxide. Indeed, if it is not oxidize during the treatment, metallic aluminium converts in aluminates in the cementitious material, and produces hydrogen, generating cracking and voids, and damaging the cementitious material. After the treatment step, a study of the potential reactivity of EFA used in partial replacement of cement is carried out. Results show the activity of EFA treated with sodium hydroxide is mainly physical (grading and developed surface). EFA presents not pozzolanic effect. Leachability tests show an equivalent durability and a very efficient stabilisation of chrome, lead and zinc, allowing the respect of the European environmental standard. / Doctorat en Sciences de l'ingénieur / info:eu-repo/semantics/nonPublished

Le ciment est la principale source des impacts sur l’environnement de l’utilisation du matériau béton. Afin d’optimiser ce dernier d’un point de vue environnemental, il est nécessaire de réduire son dosage en ciment. Cela peut être entrepris en remplaçant une partie du ciment par des additions minérales lors de sa fabrication.Ces travaux de thèse visent à étudier les phénomènes physico-chimiques ayant lieu lors du processus de carbonatation de bétons à forts taux de remplacement du ciment par des additions minérales ainsi que leur résistance à ce type d’attaque.Une campagne expérimentale a été menée sur des bétons de référence préparés à base de ciments courants et sur des Écobétons préparés en substituant une partie du ciment par des cendres volantes ou du laitier de haut-fourneau. Les différentes études menées portent sur la durabilité des Écobétons vis-à-vis de la carbonatation, sur l’équivalence de performances des Écobétons avec celles des bétons de référence, et sur les paramètres de composition et de microstructure contrôlant la cinétique de carbonatation. La carbonatation a été étudiée en conditions accélérées et naturelles. Les résultats montrent que les Écobétons à forts taux de substitution du ciment par des cendres (50 %) ou du laitier (75 %) pourraient remplacer, dans certains cas, les bétons conformes à la norme en vigueur.En complément à l’étude expérimentale, des simulations numériques du couplage hydratation/séchage ont été menées en vue de déterminer l’effet du séchage sur les propriétés contrôlant la cinétique de carbonatation accélérée des bétons étudiés (la porosité, la quantité de Portlandite et le degré de saturation en eau liquide). Les résultats montrent que la cinétique de séchage augmente avec le taux de substitution du ciment par des additions. Ils remettent aussi en cause la pertinence du préconditionnement des échantillons lors de l’essai de carbonatation accélérée mené selon la norme française XP P 18-458 actuellement en vigueur. / Cement is the main source of environmental impacts of concrete use. It is thus recognized that the most pragmatic solution for minimizing environmental impacts of concrete is the reduction of the cement content. This could be achieved by replacing a part of cement by mineral additions such as fly ash or blast-furnace slag during concrete mixing.The present work aims at studying the physico-chemical phenomena occurring during the process of carbonation of concrete mixtures with high substitution rates of cement by mineral additions and their resistance against this type of attack.An experimental campaign was conducted on reference concrete mixtures prepared with common cements and on other concrete mixtures, called “Écobétons” (Green concretes), prepared by replacing a part of cement by fly ash or blast-furnace slag. The study focused on the Écobétons durability, especially their resistance against carbonation, on the equivalence of Écobétons performances with the reference mixtures performances and on the composition and microstructure parameters controlling the kinetics of carbonation. Carbonation has been studied in natural and accelerated conditions. The results show that Écobétons mixtures with high substitution rates of cement by fly ash (50 %) and blast-furnace slag (75 %) could replace, in some cases, concretes that are in accordance with the current standard.In addition to the experimental study, numerical simulations of the coupling between hydration and drying were conducted in order to determine the effect of drying on the properties controlling the accelerated carbonation kinetics of the studied concrete mixtures (porosity, Portlandite content and water saturation degree). The results show that the kinetics of drying increases with the degree of substitution of cement by mineral additions. They also question the relevance of the preconditioning of the samples during accelerated carbonation test conducted according to the French standard XP P 18-458.

Triple oxygen and hydrogen isotope analysis of the structurally-bound water in gypsum can provide a direct measure of past hydrologic variability. This thesis presents the development of the water extraction and isotopic measurement procedures, the calculation of the gypsum-water isotope fractionation factors, and the application of the method to constrain the palaeohydrologic conditions in two temporally and geographically disparate sites. Measurement of the isotopic composition of gypsum hydration water is used to examine the hydrological changes that occurred during the Terminal Classic Drought of the Maya lowlands (~800-1000 CE), coincident with the period when the Classic Maya Civilization of Mesoamerica collapsed. The data provide a complete and direct archive of hydrological conditions that have previously been limited to ice core records. Mean annual rainfall is shown to have decreased by between 41% and 54%, with intervals of up to 70%, compared to present-day conditions. This study has also shown for the first time that relative humidity was 2%-7% lower during the Terminal Classic Drought compared to today. The methodology is also applied to the massive gypsum deposits in the marginal and deep basins of the Mediterranean to interpret the chemical evolution of parent water bodies during the Messinian Salinity Crisis (5.97-5.3 Ma). By combining the measurement of gypsum hydration water with other traditional (e.g. strontium) and novel (e.g. calcium and barium) isotope tracers, the hydrological changes during the deposition of Primary Lower Gypsum units of the Sorbas Basin in southeastern Spain, the Upper Gypsum units of Sicily, and deep basin deposits have been constrained. The results indicate that all deposits experienced a significant freshwater contribution to the mother fluids from which they formed. It is proposed that obliquity-controlled sea level and eccentricity-modulated precession, superimposed on longer-term tectonic restriction of the Mediterranean-Atlantic exchange, together controlled the varying depositional environments during the formation of the Messinian Salt Giant. This thesis demonstrates that the analysis of gypsum hydration water is a powerful tool for palaeoclimate reconstruction. The methodology can be applied to gypsum (and other hydrated minerals) in a wide range of settings across geological space and time, providing a rich source of information about the environmental conditions under which they formed.

Les aquaporines (AQPs) sont des petites protéines formant des canaux hydriques àtravers les membranes cellulaires. Les AQPs 0, 1, 2 ,4 ,5 ,6 et 8 assurent le transport sélectif de l’eautandis que les AQPs 3, 7, 9 et 10 permettent également le passage du glycérol. Nous avons étudié leurexpression dans l’épiderme, la couche supérieure de notre peau supposée imperméable. Dans lesmélanocytes, des cellules dendritiques responsables de la pigmentation, seule l’AQP1 est exprimée.Nous avons montré que les kératinocytes, les cellules majoritaires de l’épiderme, expriment enprolifération les AQPs 3 et 10, alors que les kératinocytes différenciés expriment les AQPs 3 et 9. Lalocalisation de l'AQP3 a été précédemment rapportée à la membrane plasmique des kératinocytes, de lacouche basales à la couche épineuse. Nous avons localisé l'AQP9 dans les kératinocytes différenciés dela couche granuleuse au contenu riche en glycérol et réduit en eau. De fait nous pensons que l'AQP9 ysert de transporteur de glycérol. Enfin contrairement à d'autres auteurs, nous n’avons pu mettre enévidence de lien entre prolifération tumorale et expression des aquaporines. / Aquaporins (AQPS) are a family of small proteins forming water channels across cell membranes.AQPs 0, 1, 2, 4, 5, 6 and 8 are strictly water channel whereas AQPs 3, 7, 9 and 10 allow transport ofwater and glycerol. We have studied their expression in the epidermis, the outer-most water-impermeablelayer of the skin. In melanocytes, dendritic cells responsible for pigmentation, only AQP1 is expressed, invitro and ex vivo. We have shown that keratinocytes, principal cells of the epidermis, express AQPs 3 and10 in proliferation, whereas differentiated keratinocytes express AQPs 3 and 9. The localisation of AQP3to plasma membrane of keratinocytes was previously reported from the basal layer to the spinous layer ofthe skin. We localised AQP9 in the fully differentiated keratinocytes of the granular layer, where there is ahigh glycerol and low water content. So we think that AQP9 likely functions as a glycerol transporter.Unlike other authors, we were unable to identify a link between tumorous proliferation and the expressionof aquaporins.

Les chapes autonivelantes sont souvent composées de ciment alumineux et de sulfate de calcium pour assurer une prise rapide. Le ciment alumineux est généralement à base de monocalcium aluminate (CA). Récemment, un nouveau ciment alumineux riche en mayénite (C12A7) a été conçu pour optimiser l’application des chapes par l’augmentation de la quantité d’ettringite formée. Le développement de l’hydratation au jeune âge (pendant les premières 24 heures) de ce type de produit est pourtant très peu connu. L’objectif principal de cette étude est d’évaluer l’interaction entre l’hydratation au jeune âge et le séchage naturel à travers un modèle de couplage. Ce modèle est appliqué à l’étude d’une pâte pure ettringitique composée de ciment riche en C12A7 et de plâtre alpha. Tout d’abord, un modèle cinétique d’hydratation, initialement développé en système dilué, a été proposé pour étudier l’hydratation d’une pâte pure ettringitique en condition endogène. Il permet de décrire l’évolution en fonction du temps de la porosité, de la teneur en eau, des quantités de phases (réactifs et hydrates). Un modèle de distribution de rayon de pores a été aussi proposé. Ce modèle permet d’obtenir la courbe de pression capillaire au jeune âge nécessaire pour la modélisation des transferts hydriques. Ensuite, une modélisation complète des transferts hydriques a été présentée. Elle a montré que l’hypothèse d’une pression de gaz constante conduit à une surestimation de perte de masse pour des matériaux à faible perméabilité. Pourtant, pour le cas des ciments alumineux, cette hypothèse peut être retenue pour simplifier le couplage avec le modèle cinétique d’hydratation. Enfin, une modélisation des couplages entre l’hydratation et la dessiccation a été développée. L’originalité de ce modèle porte sur l’intégration de la courbe isotherme issue du modèle de distribution poreuse dans la modélisation des transferts hydriques via une fonction Matlab. Le modèle a été capable de reproduire la cinétique de perte de masse d’un échantillon de pâte pure ettringite réactive soumis au séchage précoce. La nécessité de la prise en compte de l’évolution de température a été mise en évidence. De plus, le modèle a prévu un arrêt précoce de l’hydratation à la surface séchante après 10 heures d’hydratation. L’effet de la dessiccation atteint une profondeur de 5 mm sur un échantillon de 3 cm d’épaisseur. / Self-leveling flooring compounds (SLC) are often composed of calcium aluminate cements (CAC) and calcium sulfate to ensure rapid setting. The mineral composition of calcium aluminate cements is usually designed around monocalcium aluminate (CA). Recently, a new cement with the main compound of mayenite (C12A7) has been designed to optimize the application of SLC by increasing the amount of ettringite in the hydration product. However, there is a lack of knowledge related to early-age hydration (during the first 24 hours) of this type of product. The main objective of this study is to evaluate the interaction between early-age hydration and natural drying through a coupling model. This model is applied to the study of an ettringite binder composed of cement rich in C12A7 and plaster First, a kinetic model of hydration, initially developed in a diluted system, has been proposed to study the hydration of an ettringite paste under endogenous conditions. It allows to describe the evolution as a function of time of the porosity, the water content, and the quantities of phases (reactants and hydrates). A model of pore size distribution has also been proposed. This model allows us to obtain the capillary pressure curve at early-age, which is necessary for the modeling of moisture transport. Then, a complete modeling of water transfers was presented. It has shown that the assumption of constant gas pressure leads to an overestimation of mass loss for weakly permeable materials. However, for the case of CAC, this hypothesis can be retained to simplify the coupling with the kinetic model of hydration. Finally, a modeling of the coupling between hydration and desiccation has been developed. The originality of this model concerns the integration of the isothermal curve resulting from the pore size distribution model in the modeling of water transfers via a Matlab function. The model was able to reproduce the kinetics of mass loss of a sample of ettringite binder subjected to early drying. The role of temperature was also elucidated. In addition, the model predicted an early stop of hydration on the drying surface after 10 hours of hydration. The effect of desiccation reaches a depth of 5 mm on a sample with a thickness of 3 cm.

Les molécules d’intérêt biologique ont pour caractéristique principale de participer aux processus biologiques, que ce soit au sein d’un organisme du monde du vivant, ou bien dans l’espace (exobiologie). Dans ces deux cas, l’eau joue un rôle prépondérant sur les propriétés des systèmes considérés. Les simulations numériques constituant désormais un élément incontournable pour l’interprétation des expériences, l’objectif de cette thèse sera de tenter de reproduire par des méthodes de chimie quantique les spectres IR expérimentaux relatifs à deux systèmes hydratés : les aérosols de nitrate, présents dans l’atmosphère, ainsi que les bases d’acides nucléiques microhydratées. Ce travail présente une même démarche afin d’obtenir la meilleure adéquation possible entre théorie et expérience. Tout d’abord, le modèle géométrique permettant de représenter au mieux nos systèmes a été recherché à partir de l’utilisation du code GSAM développé au laboratoire. Puis, nous nous sommes attachés à déterminer la méthode théorique la plus adaptée à l’étude de chacun des systèmes. Pour ce faire, différentes méthodes de calcul de structure électronique (dont B3LYP et ses analogues prenant en compte les interactions à moyenne et longue portée B3LYP-D et CAMB3LYP), de traitement vibrationnel (VPT2, VCI-P ou bien DM) ont été testées. L’évolution expérimentale observée pour les nombres d’onde associés aux cinq modes de vibration de l’ion nitrate en fonction du nombre de molécules d’eau au sein de l’aérosol est ainsi reproductible en utilisant un modèle d’agrégats d’agrégats du type (NaNO3,nH2O)3 au niveau calculatoire B3LYP/6-311+G(d,p) à 15cm-1 près. En ce qui concerne les bases d’acides nucléiques (X=C, T, U, A et G) microhydratées, la meilleure représentation d’un environnement aqueux est constitué d’un modèle explicite du type X,nH2O avec n=1 à 5 -déterminé à partir de l’application du code GSAM-, associé à un modèle implicite tel que PCM. La comparaison des nombres d’onde dans la zone de signature vibrationnelle 1000-1800cm-1 pour chaque base et à deux niveaux calculatoires différents B3LYP et B3LYP-D a conduit globalement à favoriser la première. En revanche, les méthodes de traitement vibrationnel dépendantes et indépendantes du temps donnent des résultats voisins dans cette zone, avec un coût calculatoire moins important pour la méthode VPT2. / Molecules with biological interest participate to biological processes in living organisms or in space (exobiology). Water plays a predominant part on properties of considered systems.Since computations take an important part in interpretation of experiments, the aim of this phD will be to try to reproduct IR experimental spectra with methods of quantum chemistry for two different hydrated systems : nitrate aerosols and microhydrated nucleic acid bases. This work presents a same approach to obtain the best agreement between experience and theory. First, the geometrical model for representation of hydration was investigated with the GSAM code developed at the laboratory. Then, the most adapted theoretical method was determined for studies of each system. Different methods of determination of electronic structure, especially B3LYP and their analogs considering medium and long range interactions B3LYP-D and CAMB3LYP, and vibrational treatments (VPT2, VCI-P and MD) were tested. The experimental evolution observed for wavenumbers associated to the five vibrational modes of the nitrate ion depending on the number of water molecules within the aerosol is reproducible using a model of aggregates of molecular clusters labeled (NaNO3,nH2O)3 at the B3LYP/6-311+G(d,p) level of theory : the average discrepancy between theory and experience reaches 15cm-1. Concerning microhydrated nucleic acid bases (X=C, T, U, A et G), the best representation of aqueous environment is made of an explicit model labeled X,nH2O with n=1 to 5 -determined from the application of the GSAM code-, with an implicit one like the PCM model. The comparison of wavenumbers calculated at the B3LYP and B3LYP-D levels of theory in the 1000-1800cm-1 spectral region which represents the vibrational signature for each base favoured the first method. But time-dependent and time-independent methods of vibrational treatment provide comparable results in this region, with a computational cost less important for the VPT2 approach.

Depuis le milieu des années 90, la minéralisation in situ du CO2 est envisagée comme une solution durable et efficace pour limiter ses émissions anthropiques vers l'atmosphère. Il s'agit de récupérer le CO2 émis par certaines industries pour le piéger en profondeur sous forme minérale (carbonates) dans les aquifères mafiques et ultramafiques naturels (de type basaltes et péridotites). La carbonatation du CO2 a été largement décrite dans les systèmes naturels où elle apparait à travers une série de réactions chimiques couplées au transport des espèces réactives dans le fluide. Plusieurs expériences en réacteurs fermés ont été menées depuis une quinzaine d'années afin de mieux comprendre les paramètres physico-chimiques contrôlant ces réactions. Mais très peu d'études n'ont encore caractérisé les processus de transport-réactif au cours de l'injection et de la minéralisation in situ du CO2 dans ces roches.Ces travaux visent à répondre à 3 principaux objectifs : (i) caractériser l'évolution des chemins réactifs lors de l'injection de CO2 dans des roches (ultra-)mafiques, (ii) mesurer les effets en retour des réactions sur les propriétés hydrodynamiques du milieu et (iii) quantifier le rendement et la pérennité des processus sur le long terme. Ils s'appuient sur le développement de protocoles expérimentaux pour (i) reproduire l'injection de CO2 dans les roches (ultra-)mafiques et (ii) caractériser les réactions à l'aide d'une série d'outils géochimiques et analytiques de l'échelle atomique à centimétrique. Trois séries d'expériences de percolation réactive ont été réalisé sur des agrégats (ultra-)mafiques relativement simples (olivines de San Carlos et d'Hawaii) et plus complexes (basaltes de Stapafell) dans des conditions de P-T-confinement in situ (Ptot=10-25 MPa ; T=180-185°C;Pconf=15-28 MPa).Les résultats obtenus ont permis de différencier plusieurs chemins réactifs dans ces systèmes en fonction du transport du fluide, de la porosité du milieu, des hétérogénéités locales de la roche, de la minéralogie et/ou des variations locales de la composition chimique du fluide. Les calculs du bilan de masse ont révélé une minéralisation efficace du CO2 contrôlée par les propriétés chimiques et hydrodynamiques du milieu. Mais certaines réactions associées à l'altération des roches (ultra-)mafiques (hydratation) ont des effets en retour négatifs sur les propriétés réservoirs de la roche (porosité, perméabilité) pouvant compromettre la pérennité du stockage du CO2 dans les aquifères naturels sur le long terme.Ces nouvelles données permettront aux modèles numériques de mieux simuler la carbonatation des roches (ultra-)mafiques en connaissant les propriétés hydrodynamiques du milieu et les hétérogénéités structurales du réservoir. Elles suggèrent aussi qu'un meilleur contrôle de certains paramètres d'injection, comme le débit ou la composition du fluide injecté (ex: pCO2), permettrait d'améliorer le taux et le rendement de la carbonatation. / Since the mid-90s, in situ mineralization of CO2 has been considered as a safe and efficient solution to mitigate its anthropogenic emissions to the atmosphere. It is to recover the CO2 emitted by some industries and trap it in the mineral form (carbonates) in mafic and ultramafic aquifers (e.g. basalts and peridotites). The carbonation of CO2 has been widely described in natural systems where it occurs through a series of complex chemical reactions coupled to the transport of reactive species in the fluid. Numerous experiments have been conducted in batch reactors over the past fifteen years to better understand the physico-chemical parameters controlling the carbonation of (ultra-)mafic rocks. But few studies have further characterized the coupling reactive-transport processes during the injection and in situ mineralization of CO2 in these rocks.This work aims to meet 3 main objectives: (i) characterize changes in reaction paths during the injection of CO2 in (ultra-)mafic systems, (ii) measure the feedbacks effects of chemical reactions on the hydrodynamic rock properties and (iii) quantify the efficiency and sustainability of such processes over long time periods. It is based on the development of experimental protocols to (i) reproduce the injection of CO2 into (ultra-)mafic rocks and (ii) characterize the reactions using a series of geochemical and analytical tools from the atomic to the centimetric scale. Three series of reactive percolation experiments have been performed on (ultra-)mafic aggregates from relatively simple (olivines from San Carlos and Hawaii) to more complex samples (basalts from Stapafell) under in situ P-T-containment conditions (Ptot=10-25 MPa; T=180-185°C; Pcont=15-28 MPa).The results allowed us to differentiate several reactions paths in these systems depending on the fluid transport, rock porosity, local hydrodynamic properties, mineralogy and/or local changes in the fluid composition. Mass balance calculations have revealed an efficient mineralization of CO2 in the samples. It is controlled by the chemical and the hydrodynamic properties of the rock at the pore scale. But some reactions associated with the alteration of (ultra-)mafic rocks (e.g. hydration) have negative feedbacks effects on the reservoir rock properties (porosity and permeability) that may compromise the sustainability of CO2 storage in natural aquifers in the long term.These new supporting data will allow numerical models to better simulate the carbonation of (ultra-)mafic rocks knowing the hydrodynamic properties and the structural heterogeneities of the reservoir. They also suggest that a better control of some injection parameters, such as the flow injection rate and the injected fluid composition (e.g. pCO2), would improve the rate and yield of CO2 mineralization in these systems.

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No. of bitstreams: 2 Dissertação - Junaine Vasques da Silva - 2002.pdf: 3727327 bytes, checksum: 4cb8c1db4d3fb95798779f39aae78673 (MD5) license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) Previous issue date: 2002-12-19 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES / The main function of the most superficial layer of the epidermis, the Stratum Corneum (SC), is to provide a physical barrier that controls the transepidermal water loss as well as the permeation of another substances in both directions across the skin. The SC is formed by anabolically dead cells, the terminally differentiated corneocyte, and its function is essentially accomplished by forming a highly insoluble protein structure on the surface of the corneocytes, termed the cornified cell envelope, and by impeding water diffusion across the SC by mortaring the corneocytes together by layers of skin-specific lipids, essentially ceramide, cholesterol and fatty acid. In this work the cell envelope of the SC was spin labeled with a sulfhydryl-specific nitroxide reagent to investigate the water content effects upon the protein dynamics directly in the intact tissue. A two-state model for the nitroxide side chain described the coexistence of two spectral components in the electron paramagnetic resonance (EPR) spectra. The so-called strongly immobilized component, S, is associated with the EPR signal of a motionally restricted nitroxide fraction having its N-O group hydrogen bonded to protein (rigid structure) while the weakly immobilized component, W, corresponds to the signal provided by the spin labels with higher mobility (~10 times greater) exposed to the aqueous environment. The relative populations between these two mobility states, S and W, are in thermodynamic equilibrium. The standard Gibbs free energy, enthalpy and entropy changes for transferring the nitroxide side chain from the state contacting the solvent, W, to the one contacting protein, S, indicated that the reduction of the SC water content to below ~h 0.69, g H2O per g dry SC, stabilizes the protein interacting state, S. Upon decreasing the SC hydration level below ~h 0.69 the segmental motion of the polypeptide chains and the rotational motion of the spin-labeled side chain were also constrained. To test our methodology in a pure and very well known protein, we also studied the effects of two types of detergents on the bovine serum albumin (BSA). Both detergents, the anionic sodium dodecyl sulfate (SDS) and the zwitterionic N-hexadecyl-N,N-dimethyl-3-ammonium-1-propanesulfonate (HPS) increase the mobility of the protein backbone and of the nitroxide side chain. The thermodynamic parameters indicated that these detergents destabilize the protein favoring less compact conformations. This work can also be useful to improve the spectral analysis of site-directed spin labeling, especially for a more quantitative description in terms of thermodynamic parameters. / A camada mais superficial da epiderme, o Estrato Córneo (EC), tem como função principal a formação de uma barreira física que controla a perda de água do corpo bem como a permeação de outras substâncias em ambas as direções da pele. O EC é formado por células anabolicamente mortas, os corneócitos, os quais sofreram diferenciação celular terminal, e sua função é realizada formando uma estrutura de proteínas altamente insolúveis na superfície do corneócito, chamada de envelope celular, e também uma matriz lipídica, essencialmente ceramídios, colesterol e ácidos graxos, que dificultam a difusão da água. Neste trabalho, o EC foi marcado com marcadores de spin específicos para reagir com os grupos sulfidrilas das proteínas, para investigar os efeitos do conteúdo de água na dinâmica de proteínas diretamente no tecido intacto. Um modelo de dois estados para a cadeia lateral do nitróxido descreveu a coexistência de duas componentes espectrais de ressonância paramagnética eletrônica (RPE). A componente denominada fortemente imobilizada (S), surge de uma fração de marcadores com o átomo de oxigênio do nitróxido ligado à proteína (estrutura rígida) enquanto a componente fracamente imobilizada é gerada pelos marcadores com mobilidade mais alta (~10 vezes maior) e expostos ao ambiente aquoso. As populações relativas entre estes dois estados de mobilidade, S e W, estão em equilíbrio termodinâmico. Os parâmetros da termodinâmica: energia livre padrão de Gibbs, entalpia e entropia, envolvidos na transferência da cadeia lateral do nitróxido do estado W, contatando ao solvente, para o estado S, contatando a proteína, indicaram que a redução do conteúdo de água para abaixo de ~0.69g de H2O por g de EC seco, estabiliza o estado S (cadeia lateral do nitróxido dobrada sobre a cadeia principal da proteína). Ao diminuir o nível de hidratação para abaixo de ~ h 0.69 (g H2o/g EC seco) o movimento local da cadeia polipeptídica e o movimento rotacional da cadeia lateral do marcador de spin foram ambos reduzidos. Para testar nossa metodologia em uma proteína pura e bem conhecida, estudamos os efeitos de dois tipos de detergentes sobre a albumina do soro bovino (BSA). Ambos os detergentes, o aniônico dodecil sulfato de sódio (SDS) e o ziteriônico N-hexadecil-N,N-dimetil-3-amônio-1-propanosulfonato (HPS) aumentaram a mobilidade da cadeia principal da proteína e da cadeia lateral do nitróxido. Os parâmetros termodinâmicos indicaram que estes detergentes desestabilizam a proteína favorecendo conformações menos compactas. Os resultados do presente trabalho também podem contribuir para aprimorar a

Submitted by Silvana Teresinha Dornelles Studzinski (sstudzinski) on 2016-12-22T12:03:13Z No. of bitstreams: 1 Josué Claudio Metz_.pdf: 3580473 bytes, checksum: 4bb7f81d4d0a95ef4e39a7d4dffb0599 (MD5) / Made available in DSpace on 2016-12-22T12:03:13Z (GMT). No. of bitstreams: 1 Josué Claudio Metz_.pdf: 3580473 bytes, checksum: 4bb7f81d4d0a95ef4e39a7d4dffb0599 (MD5) Previous issue date: 2016-09-19 / Nenhuma / A concepção de desenvolvimento sustentável tem resultado no aumento de pressões ambientais para a melhoria da eficiência na utilização de recursos, e para a redução das emissões e da geração de resíduos. No processo de fabricação de aço, nas siderúrgicas com fornos elétricos a arco (FEA), ocorre a geração do resíduo sólido denominado pó de aciaria elétrica (PAE). O PAE é constituído por diferentes óxidos metálicos. Contém os elementos químicos cromo (Cr), chumbo (Pb) e cádmio (Cd) e, por isso, é classificado como resíduo classe I – Perigoso pela NBR 10004. Gerado em grandes quantidades diariamente em todo o país, o PAE ainda tem como principal destinação final o aterro industrial. A indústria de papel e celulose, outra atividade de destaque na indústria nacional, gera uma grande quantidade de resíduos em diferentes etapas do processo, entre os quais está o resíduo do forno de cal (RFC), cuja geração está associada a interrupções no funcionamento do forno de cal. A indústria da construção civil, devido a quantidade de matérias-primas consumida e variedade de materiais empregados – cimento, concreto, agregados, cerâmica, entre outros – apresenta-se como alternativa para a reciclagem de resíduos gerados em outros setores da economia. A incorporação do PAE no cimento e concreto produz retardo no tempo de pega em razão da presença de zinco (Zn) no resíduo. Estudos sugerem que em quantidades próximas a 1%, a incorporação de PAE não afeta de forma significativa as propriedades do cimento. O objetivo deste trabalho foi avaliar a influência do uso combinado de PAE e RFC no processo de endurecimento e evolução da hidratação de pastas de cimento. Para tanto, foi realizada a caracterização dos resíduos através dos ensaios de distribuição granulométrica, perda ao fogo, massa específica, área superficial específica, análise química elementar, difração de raios X com refinamento por Rietveld e microscopia eletrônica de varredura. A influência dos resíduos nas pastas de cimento foi avaliada através do ensaio de tempo de pega de acordo com a NBR NM 65 (ABNT, 2003b) e evolução da temperatura semi-adiabática das pastas em estado fresco, além de DRX, com refinamento por Rietveld, e microscopia eletrônica de varredura nas pastas de cimento com diferentes teores de substituição de resíduos (REF, 1%, 2%, 3%, 5% e 10%) em diferentes idades (1, 4 e 7 dias). Os resultados de tempo de pega e evolução da temperatura semi-adiabática indicaram a influência do PAE na hidratação das pastas de cimento. Nas pastas de cimento com substituição de 1% de PAE combinado ou não com RFC, não foram verificados retardos significativos no tempo de pega, demonstrando o potencial do uso de PAE e do RFC na produção de artefatos de cimento. / The sustainable development conception has resulted in increased environmental pressures to improve the efficient use of resources and reduction of emissions and waste generation. In the steelmaking process through electric arc furnaces (EAF), dust generation occurs which is called electric arc furnace dust (EAFD). EAFD is composed by different metal oxides. Some common elements those constitute this dust is chromium, lead and cadmium, and therefore, waste is classified as class I – hazardous by NBR 10004. EAFD has been generated in large quantities every day across the country and it still has mainly landfilled. The pulp and paper industry, another important activity in the domestic industry, generates a lot of waste in different stages of the process, among which is the lime kiln waste (LKW), whose generation is associated with disruptions in the lime oven. Due to expressive amount of raw materials consumed in civil construction industry and also the variety of products available - cement, concrete, aggregates, ceramics, among others - this seems to be an alternative for waste recycling generated in other sectors. The incorporation of EAFD in the cement and concrete produces delayed setting time due to the presence of zinc (Zn) in the waste. Studies suggest that in amounts up to 1%, EAFD incorporation does not affect significantly cement properties. The aim of this work was to evaluate the influence of the combined use of EAFD and LKW in the process of hardening and evolution of the cement pastes hydration. Therefore, were evaluated the characterization of the waste performed through the grain size distribution, loss on ignition, specific gravity, specific surface area, elemental chemical analysis, pH, X ray powder diffraction with refinement by Rietveld and scanning electron microscopy.. The influence of the waste on the cement pastes was evaluated through the setting time tests in accordance with the NBR NM 65 (ABNT, 2003b) and evolution of semi-adiabatic temperature in fresh conditions, XRD with refinement by Rietveld, and SEM in cement pastes with different levels of waste substitution (REF, 1%, 2%, 3%, 5% e 10%) at different ages (1, 4 and 7 days). The setting time results and evolution of semi-adiabatic temperature indicated an increase in the setting time with the increase of the EAFD in cement pastes. In cement pastes with replacement of 1% EAFD combined or not with LKW, significant delays were not verified in the setting time, demonstrating the potential use of EAFD in the production of cement artifacts.