The electric grid has been expanding both in size and the technologies used. As of the 2020s, the United States power grid consists of more than 9,200 electric generating units with more than 1 million megawatts of generating capacity connected to more than 300,000 miles of transmission lines. The United States electricity grid has rapidly expanded in recent decades, and the majority (over 70\%) of its infrastructure has exceeded 25 years of age. Due to its size and age, several challenges have emerged. Widespread power outages have been increasing across the United States. Between 2018 and 2020, more than 231,000 power outages occurred in the United States that lasted more than one hour, out of which 17,484 lasted at least eight hours. In the same period, the power outages resulted in an annual loss of 520 million customer hours across 2,447 U.S. counties. Moreover, and with the rapidly changing climate, between 2000 and 2021, approximately 83\% of significant power outages impacting a minimum of 50,000 customers in the United States were attributed to severe weather conditions. Lastly, the increasing use of renewables and other non-traditional generation methods forces the power system towards a more decentralized model, with many integrated systems constantly added to the grid. This decentralization adds additional burdens on controlling systems and grid operators. The rapid growth of technology and data storage allowed the deployment of sensing devices across the electric grid. Such technologies present a golden opportunity to tackle many of the electric grid's challenges. Despite that, such technologies presented many challenges simultaneously. With the large amounts of data, it became humanly impossible to comprehend, analyze, and use all collected data manually. While machine learning can be used to analyze smart grid data, this can be challenged by the nature of its data. Smart grid produces high-dimensional spatiotemporal data, and many applications require multi-modal data. Moreover, power systems' data quality challenges add complexities to model development. The data is noisy, contains missing segments, and usually has incomplete and inaccurate labels. In addition, interpreting machine learning models in the context of smart grids poses unique challenges. To address these challenges, different models for multiple smart-grid applications were introduced in this research, where each model focused on producing practical solutions for the challenges facing current-day smart grids. Using spatiotemporal data, a solar generation prediction model was proposed. The solution combined spatial and temporal data, then utilized machine learning embeddings to build datasets to train downstream models. This resulted in accurate prediction of solar generation across several settings. In addition to solar generation prediction, several models were introduced to detect, predict and explain power grid faults. A neural model is introduced to detect power faults from Phasor Measurement Unit (PMU) data. A novel method is introduced to preprocesses, de-noise, and combine high dimensional data, then this data is used to train novel neural methods that detect faults in multiple settings. This model addressed issues of high dimensionality and data quality. After that, several models studying power fault prediction and precursor discovery were introduced. A model that jointly predicts outages 6 hours ahead and produces explainable event precursors from multi-modal data is introduced. Where such precursors can assist power grid operators to take action to mitigate widespread power outages. Finally, a novel methodology is introduced that expands to previous work by predicting and extracting event precursors spatiotemporally 12 hours in advance. Where event precursors can be predicted on multiple spatial locations simultaneously, extracted spatiotemporal event precursors can help grid operators narrow down mitigation plans and help reduce the risk of widespread power outages. / Computer and Information Science

Les chondres, sphérules infra-millimétriques composées de minéraux silicatés de haute température, sont les constituants majeurs des météorites primitives. Ils présentent d'importantes variabilités texturales et chimiques révélatrices d'une histoire complexe. Cette thèse s'est intéressée à la chronologie de formation des chondres et de leurs précurseurs à deux échelles de temps distinctes aux moyens de deux approches complémentaires : la géochimie isotopique via le chronomètre isotopique à courte période ²⁶lAl-²⁶Mg et la pétrologie expérimentale. Le développement au cours de cette thèse d'un protocole analytique innovant de mesure in situ de haute précision par sonde ionique des compositions isotopiques du Mg et Al, a permis de démontrer l'homogénéité de la distribution de l'²⁶Al dans le disque d'accrétion, ce qui présente d'importantes implications sur la chronologie relative et les processus de formation des chondres, mais aussi sur l'origine de l'²⁶Al dans le Système Solaire. L'application de ce protocole analytique aux olivines reliques des chondres permet de préciser leur origine, ainsi que leur chronologie et leur processus de formation. Les expérimentations permettent de montrer qu'il est aisé de former des analogues de chondres de type II PO à partir de chondres de type I PO. Un tel processus de formation des chondres implique l'application de régimes thermiques isothermes suivis d'une trempe rapide, incompatibles avec les mécanismes classiques d'ondes de choc. D'autre part, nous montrons que les compositions chimiques en éléments majeurs et traces des différents types de chondres porphyriques peuvent être reproduites par le mélange de trois phases réfractaires solides héritées des précurseurs des chondres (olivine réfractaire, liquide réfractaire et métal) et d'une phase gazeuse riche en éléments volatils et modérément volatils. Ces résultats nous ont conduit à proposer un modèle de filiation entre les chondres / Chondrules are the major constituent of primitive meteorites. The large variability of textures and chemical compositions within chondrules is indicative of a complex history. This work is focused on the chronology of formation of chondrules and of their precursors by using two complementary tools: the short-lived radio-isotopes ²⁶Al-²⁶Mg and the experimental petrology.The development of a high precision analytical methodology for in situ measurements of the Mg and Al isotopic compositions by ion probe allows to demonstrate that the distribution of ²⁶Al was homogeneous within the accretion disk. This result has important implications for the chronology and process of chondrule formation and also for the origin of ²⁶Al in the Solar System. By using the same methodology with relict olivines in chondrules, we were able to constrain their origin and their formation process.From experimental petrology studies, we show that it was easy to form type II PO chondrules analogues from type I PO analogues. Such a process for chondrules formation implies an isothermal heating followed by a quick quench which is incompatible with the classical shock-waves model. Moreover, we show that the chemical compositions for major and trace elements of the different types of porphyritic chondrules can be easily reproduced by a mixing model composed of three refractory phases inherited from chondrules precursors (refractory olivine, refractory liquid and iron metal) and a gas phase enriched in volatile and moderately volatile elements. Finally, we propose a model of genetic linkage between the different types of porphyritic chondrules

Per- and polyfluoroalkyl substances (PFASs) are a group of artificial chemicals which have been used in a wide area of applications such as surface protection agents in cloths and different industrial applications. It has been found that PFASs are potentially toxic and are frequently found in the environment due to their persistent and mobile properties. Effluents from wastewater treatment plants (WWTPs) have been identified as an important point source of PFASs. Bark, by-product from the paper and wood industry, is a low-cost adsorbent and has the potential to be used as a filter material for PFASs in WWTPs. In this study, the removal of PFASs in wastewater has been investigated using granulated active carbon (GAC) (n = 2) and bark (n = 2) in a pilot scale experiment at Kungsängsverket, Uppsala over a period of five weeks. The specific objects included: i) investigate the influence of flow-rate (10, 30 40 and 60 Ld-1 ) on the removal efficiency of PFASs in the GAC and bark filters, ii) investigate the influence of particle size of bark on the removal efficiency of PFASs and iii) establish what circumstances that potentially promotes removal of PFASs in GAC and bark filters. The results showed that GAC was the most effective method compared to bark, with a reduction of 73-93%, with increasing efficiency under low flow (10-30 L d-1 ) conditions. The removal efficiency of bark was 45% with a particle size of 2-5 mm and under low flow conditions (10-30 L d-1 ), while under high flow conditions (60 L d-1 ) with the same particle size the removal of PFASs was not efficient, instead the total PFAS concentration increased with 40%. In contrast, bark with a particle size of 5-7 mm proved to be not efficient in removing PFASs (removal efficiency = 0%). In general, the removal efficiency increased with smaller particle size of the adsorbent and lower flow rate. The results indicate that bark may be a low-cost alternative in reducing PFASs from wastewater, under certain conditions. / Per- och polyfluroalkyla ämnen (PFAS) är en familj av artificiella fluorerade organiska föreningar som har använts sedan 1950-talet i en rad olika applikationer, såsom impregnering i kläder. Studier har visat att PFAS är potentiellt toxiska och att de förekommer globalt på grund av deras persistenta och mobila egenskaper. Spillvatten från avloppsreningsverk etablerats som en betydande källa för PFAS. Bark, vilket är en biprodukt från pappers- och träindustrin, är ett poröst material vilket möjligen kan användas som adsorbent av PFAS. Denna studie har jämfört effektiviteten hos granulerat aktivt kol (GAC) och bark för att minska PFAS i avloppsvatten. Experimentet var utformat som ett småskaligt kolonn-experiment vid Kungsängsängsverket, Uppsala, och pågick under en fem veckors period. Frågeställningen var att i) studera vilka effekter flödes-hastigheten (10, 30, 40 och 60 L d-1 ) har på reduktionen av PFAS hos GAC och barkfiltren, ii) studera vilka effekter partikelstorleken hos bark har på reduktion av PFAS och iii) redogöra vilka förhållanden som potentiellt gynnar reduktionen av PFAS i GAC och bark filtren. Resultaten visade att GAC var det mest effektiva av de två materialen, med en total reduktion på 73- 93% av PFAS, med ökande effektivitet under låga flödesförhållanden (10-30 L d-1 ). Bark minskade den totala mängden av PFAS med 45% då partikelstorleken var 2-5 mm och under låga flödesförhållanden (10-30 L d-1 ) medan bark med samma partikelstorlek under ökade flödesförhållanden (60 L d-1 ) visade en ökning på 40% av PFAS i det utgående vattnet. Bark med en partikelstorlek på 5-7 mm visade ingen reduktion av PFAS. Generellt visade resultaten att reduktionen av PFAS ökar under låga flödesförhållanden och minskad partikelstorlek. Resultaten visade att bark kan vara ett alternativt material för att minska PFAS i avloppsvatten förutsatt att gynnsamma förhållanden upprätthålls.

Résumé La Ribonucléase P (RNase P) est une enzyme principalement reconnue pour sa participation à la maturation en 5’des ARN de transfert (ARNt). Cependant, d’autres substrats sont reconnus par l’enzyme. En général, la RNase P est composée d’une sous-unité ARN (le P-ARN, codé par le gène rnpB) qui porte le centre actif de l’enzyme et d’une ou de plusieurs sous-unités protéiques (la P-protéine). Les P-ARN chez toutes les bactéries, la majorité des archéobactéries et dans le génome nucléaire de la plupart des eucaryotes, possèdent généralement une structure secondaire très conservée qui inclut le noyau (P1-P4); l’hélice P4 constitue le site catalytique de l’enzyme et l’hélice P1 apparie les extrémités du P-ARN en stabilisant sa structure globale. Les P-ARN mitochondriaux sont souvent moins conservés et difficiles à découvrir. Dans certains cas, les seules régions de structure primaire qui restent conservées sont celles qui définissent le P4 et le P1. Pour la détection des gènes rnpB, un outil de recherche bioinformatique, basé sur la séquence et le profil de structure secondaire, a été développé dans le laboratoire. Cet outil permet le dépistage de toutes les séquences eucaryotes (nucléaires et mitochondriales) du gène avec une très grande confiance (basée sur une valeur statistique, E-value). Chez les champignons, plusieurs ascomycètes encodent un gène rnpB dans leur génome mitochondrial y compris tous les membres du genre d’Aspergillus. Cependant, chez les espèces voisines, Neurospora crassa, Podospora anserina et Sordaria macrospora, une version mitochondriale de ce gène n’existe pas. Au lieu de cela, elles contiennent deux copies nucléaires du gène, légèrement différentes en taille et en contenu nucléotidique. Mon projet a été établi dans le but d’éclaircir l’évolution de la RNase P mitochondriale (mtRNase P) chez ces trois espèces voisines d’Aspergillus. En ce qui concerne les résultats, des modèles de structures secondaires pour les transcrits de ces gènes ont été construits en se basant sur la structure consensus universelle de la sous-unité ARN de la RNase P. Pour les trois espèces, par la comparaison de ces modèles, nous avons établi que les deux copies nucléaires du gène rnpB sont assez distinctes en séquence et en structure pour pouvoir y penser à une spécialisation de fonction de la RNase P. Chez N. crassa, les deux P-ARN sont modifiés probablement par une coiffe et les extrémités 5’, 3’ sont conformes à nos modèles, ayant un P1 allongé. Encore chez N. crassa, nous avons constaté que les deux copies sont transcrites au même niveau dans le cytoplasme et que la plus petite et la plus stable d’entre elles (Nc1) se retrouve dans l’extrait matriciel mitochondrial. Lors du suivi du P-ARN dans diverses sous-fractions provenant de la matrice mitochondriale soluble, Nc1 est associée avec l’activité de la RNase P. La caractérisation du complexe protéique, isolé à partir de la fraction active sur un gel non dénaturant, révèle qu’il contient au moins 87 protéines, 73 d’entre elles ayant déjà une localisation mitochondriale connue. Comme chez la levure, les protéines de ce complexe sont impliquées dans plusieurs fonctions cellulaires comme le processing de l’ADN/ARN, le métabolisme, dans la traduction et d’autres (par exemple : la protéolyse et le repliement des protéines, ainsi que la maintenance du génome mitochondrial). Pour trois protéines, leur fonction est non déterminée. / Abstract Ribonuclease P (RNase P) is an endonuclease that cleaves 5’- leader sequences from tRNA precursors and a few other small RNAs. In most cases, the enzyme is a ribonucleo-protein complex (ribozyme), containing an RNA subunit (P-RNA; encoded by the rnpB gene) that carries the active centre of the enzyme, plus one or more protein subunits. P-RNAs in Bacteria, Eukarya and Archaea have a highly conserved secondary structure including the core P1 and P4 helices. P4 forms the catalytic site of the ribozyme, and P1 pairs the RNA termini, stabilizing overall structure and protecting from nuclease degradation. For processing of mitochondrial (mt) tRNAs, certain eukaryotic species (e.g., Saccharomyces cerevisiae, Aspergillus nidulans) have separate mtDNA-encoded P-RNAs (of bacterial origin). Mt P-RNAs are often less conserved, and difficult to discover. To identify rnpB genes, we have developed a search tool based on sequence plus secondary structure profiles. It predicts all known eukaryotic (nuclear and organellar) rnpB genes with high confidence (based on E-values). In fungi, many ascomycetes encode a mitochondrial rnpB gene, including all members of Aspergillus. Yet, the closely related Neurospora crassa, Podospora anserina and Sordaria macrospora lack an mtDNA-encoded gene version. Instead, they contain two nuclear gene copies with slightly different sequences. My project aims to elucidate the evolution of mitochondrial RNase P in these three closely related species. We have established secondary structure models based on comparisons with the universal minimum consensus secondary structure for all nuclear gene mtP-RNAs copies in all three species. By comparison of these secondary structure models, we have established that the two nuclear copies of rnpB gene are quite distinct in sequence and structure, suggesting a specialization of function. In N. crassa, both P-RNAs are modified most likely by capping, and 5’- 3’ termini perfectly conform to P-RNA structure models that have an elongated P1 helical pairing. Furthermore, we find that the two nuclear copies of rnpB gene are present at about the same level in the cytoplasm, and that the shorter form of P-RNA (Nc1) translocates into the (soluble) mitochondrial matrix. When tracing P-RNA in different mitochondrial sub-fractions of a native gel, the presence of Nc1 and mitochondrial RNase P activity are associated. A proteomics characterization of a P-RNA complex isolated by native gel electrophoresis reveals that it contains at least 87 proteins, 73 of which are of known mitochondrial localization. Like in yeast, the complex contains proteins potentially involved in other DNA/RNA processing activities, but also in translation, in metabolism, and in protein folding. Only three proteins are of unknown function.

L'étude des signes précurseurs d'un effondrement brutal au-dessus de cavités souterraines, dont le recouvrement est caractérisé par la présence d'un banc massif et raide, est un problème majeur pour la sécurité publique. Aussi, pour progresser dans la compréhension et l'évolution des mécanismes mis en jeu, une cavité saline, située dans le NE de la France, a été suivie en temps réel, entre 2004 et 2009, jusqu'à son effondrement. Celle-ci a été exploitée par dissolution, jusqu'à atteindre une dimension critique (de l'ordre de 180 m) sous un recouvrement de 180 m, armé d'un banc raide de Dolomie situé à 120 m de profondeur.Un système de mesures multi-paramètres haute résolution visait à caractériser les signes précurseurs ainsi qu'à suivre l'effondrement lui-même. Il comprenait des dispositifs à la fois géotechniques et géophysiques, dont des mesures de nivellement de surface et un réseau permanent d'écoute microsismique. Ce dernier, dont les données font l'objet principal de cette thèse, était constitué de neuf sondes équipées de géophones 40 Hz (5 unidirectionnels et 4 tridirectionnels), réparties autour et à l'aplomb de la cavité, dont une dans le banc raide.L'évolution de la cavité a été marquée par deux épisodes majeurs d'activité microsismique :- au printemps 2008, la reprise de la dissolution dans la cavité a engendré l'apparition de crises répétées avec plusieurs milliers d'événements en quelques jours, traduisant un changement de régime microsismique, marqueur de l'instabilité de la cavité ;- en février 2009, suite à ces observations, l'exploitant a décidé de provoquer l'effondrement, par le rabattement intensif de saumure dans la cavité. Pendant les trois jours d'opération, plus de 30000 événements ont été enregistrés (sur 60000 depuis 2004).L'étude de la signature des événements apporte des renseignements essentiels pour la surveillance opérationnelle et la discrimination de ces deux périodes. En particulier, alors que les valeurs maximales atteintes en amplitude, énergie au capteur et fréquence fondamentale apparente, sont assez stables au cours des crises, les sauts marqués durant l'effondrement, permettent de présumer de son imminence. L'évolution de la distribution des microséismes en termes d'énergie libérée et d'occurrence, calculée de manière similaire à la loi de Gutenberg-Richter, bien que souvent difficile à interpréter, a pu être associée à des hausses du niveau piézométrique, ainsi qu'à de petites accélérations de l'affaissement mesuré en surface. Pendant la période d'effondrement, le nombre d'événements microsismiques augmente en suivant une loi en puissance.La localisation des microséismes a nécessité la mise en place d'une stratégie adaptée pour garantir la qualité et l'homogénéité des résultats (sélection des enregistrements, calibrage, étude paramétrique).Cependant, l'utilisation d'un modèle de vitesse constant sur toute la période s'est révélé impossible, compte tenu de l'évolution rapide et permanente du milieu. Il a donc été entrepris d'établir des modèles de vitesse différents en fonction des périodes d'évolution de la cavité.Les distributions spatio-temporelles des foyers ainsi localisés montrent l'existence de structures préférentielles de rupture et souligne le rôle majeur du banc raide.Croisées avec les autres mesures acquises sur le site, ces résultats ont permis d'établir un scénario probable d'évolution de la cavité et de proposer quelques recommandations pour la surveillance opérationnelle / The study of the precursory signs of a brutal collapse above underground caverns, with an overburden characterized by the presence of a massive and stiff bench, is a major problem for public safety. Thus, to progress in the comprehension and the evolution of the concerned mechanisms, a salt cavern, located in the NE France, was monitored in real-time, since 2004 to 2009, until its collapse. This cavern was mined by solution, until reaching its critical dimension (about 180 m) under a covering of 180 m thick, armed with a stiff Dolomite bench located at 120 m of depth.A multi-parameter high resolution monitoring system aimed at characterizing the precursory signs and following collapse itself. It included both geotechnical and geophysical devices as surface leveling measurements and a permanent microseismic network. This one, which data are the principal subject of this thesis, consisted in nine probes equipped with 40 Hz geophones (5 1D and 4 3D), distributed around and directly below the cavern, including one located in the stiff bench.The evolution of the cavern was marked by two major episodes of microseismic activity:- at the beginning of spring 2008, the dissolution restart in the cavern which caused repeated crisis with several thousand events in a few days, this represent a change in the microseismic regime and marked the cavern instability;- in February 2009, following these observations, the owner decided to trigger the collapse by intensive brine pumping in the cavern. During the three days of the operation, more than 30,000 events were recorded (against 60,000 since 2004).The study of the event signature provides essential information for operational monitoring and the discrimination of these two periods. Particularly, while maximal values reached in amplitude, energy and apparent fundamental frequency are quite stable during the 2008 episodes, the rises of this values are important during the collapse period (prior to the peak of activity), allowed us to suppose its imminence. The evolution of the microseism distribution in terms of energy released and occurrence, calculated similarly to the Gutenberg-Richter law, although often difficult to interpret, has been associated with piezometric level rises, and with small accelerations of surface subsidence. During the collapse, the microseismic activity acceleration follows a power law.Microseisms location required the establishment of an appropriate strategy to ensure the quality and the consistency of the results (record selection, calibration, parametric analysis). However, the use of a constant velocity model over all the period was impossible due to the fast and permanent evolution of the environment. Thus, several models were used, according to the a priori known cavern evolution.The event spatiotemporal distributions, thus located, revealed the existence of preferential failure structures and highlight the role of the stiff bench, located at 120 m depth

Cette thèse porte sur l’étude de l’évolution de la qualité de l’air en Europe et en France dans les prochaines décennies à l’aide de simulations numériques. Dans les études des impacts de l’évolution du climat sur la qualité de l’air, les modèles de chimie atmosphérique utilisent des sorties de modèles climatiques globaux ou régionaux qui fournissent les « forçages », c’est-à-dire les conditions météorologiques simulées pour les périodes futures. Contrairement aux analyses météorologiques, qui représentent la variabilité jour à jour du temps, les sorties des modèles de climat doivent nécessairement être interprétées de manière statistique : elles ne représentent la météorologie que dans un sens climatologique. Afin de pouvoir commenter utilement les simulations futures de qualité de l’air, il est nécessaire d’évaluer au préalable et pour le climat présent, la qualité des simulations calculées avec des forçages climatiques par rapport aux références que constituent les simulations calculées avec des forçages analysés et, bien entendu, les observations. Trois simulations pluri-annuelles (6 ans) ont été lancées pour la période actuelle (2000-2010) et ont été comparées ; elles différent par l’utilisation d’analyses météorologiques ou de forçages de modèle de climat (pour les paramètres atmosphériques seuls et par ailleurs, pour les paramètres atmosphériques et le calcul des échanges en surface) en entrée du modèle de chimie-transport tridimensionnel de Météo-France, MOCAGE. Nous avons évalué ces différentes simulations par comparaison aux observations de la base de données européenne AirBase. Nous avons ensuite comparé les performances de ces simulations pour un grand nombre de scores quantitatifs, en analysant d’une part les effets liés aux champs météorologiques (température, vent, humidité, etc.) et d’autre part, ceux liés aux échanges en surface (comme les vitesses de dépôts, les émissions biogéniques) qui dépendent également de la météorologie. Nous avons ainsi évalué comment ces changements affectent les distributions horizontales et verticales des polluants. In fine, nous avons caractérisé la fiabilité des simulations de qualité de l’air reposant sur des forçages issus de modèles climatiques pour le climat présent : des indicateurs (biais moyens, biais moyens normalisés, RMSE, déviations standards) et des index de qualité de l’air (comme le dépassement de seuils) se distinguent et peuvent donc servir de base fiable pour l’interprétation des résultats pour les simulations du futur. Enfin dans une troisième partie, ces indicateurs considérés comme pertinents ont été utilisés pour étudier des simulations de qualité de l’air aux horizons 2030 et 2050 (5 ans). Comme attendu, l’évolution des paramètres météorologiques (température, précipitation, vent) modifie les quantités et la dispersion des polluants dans l’atmosphère, mais l’évolution des émissions en Europe et dans le reste du monde joue aussi un rôle important. Ainsi, face à l’évolution du climat et la hausse des émissions dans certains pays du monde, en Asie notamment, les effets des politiques Européennes pour réduire les émissions anthropiques sont mitigés selon les régions et les polluants, dépendant de l’influence relative des phénomènes locaux et du transport de polluant à longue distance. / This thesis aims at predicting how European and French air quality could evolve over the next decades using numerical modeling. In order to study the impacts of climate change up on regional air quality, atmospheric chemistry models rely on global or regional climate models to produce “forcings”, i.e. meteorological conditions for future periods. Unlike meteorological analyses, which can represent specifically each date and hour thanks to the assimilation of observations, climate model outputs need to be averaged and can only be interpreted in a climatological sense. And so are air quality hindcasts relying on them for their forcings. In order to properly interpret air quality simulations in a future climate, it is a pre-requisite to assess how realistic air quality hindcasts are when driven by forcings from climate models for the current period in comparison to the references, which are simulations with the same set-up but relying on meteorological analyses and observations. Three six-year simulations for the current climate (2000-2010) have been run with the three-dimensional chemistry transport model of Météo-France, MOCAGE. These simulations only differ by the meteorological forcings used, either operational meteorological analyses or outputs from climate simulations (for atmospheric parameters only ; for atmospheric parameters as well as surface exchanges, which depend also on the weather). We compared the three simulations and evaluated them against the European air quality database of the European Environment Agency, AirBase. Further, we investigated how statistical skill indicators compare in the different simulations, assessing the effects of meteorology on atmospheric fields (temperature, wind, humidity,...) and on the dependent emissions and deposition processes (such as deposition velocities, volatile organic compound emissions, ...) that depend upon meteorology. We have in particular studied how these factors affect the horizontal and vertical distributions of species. In the end, we have estimated how reliable are skill indicators for the simulations run with “climate” forcings : some indicators (mean bias, mean normalized bias, RMSE, deviation standards, number of exceedance days) are sufficiently close to the ones obtained with the reference configuration (relying on analysed meteorological forcings) to be considered reliable. They can thus be used to interpret simulations for future periods. We have run simulations of European air quality in the 2030s and 2050s (5 years for each period). They are discussed using the indicators previously indentified. As expected, the changes in meteorological parameters (temperature, precipitation, wind, ...) affect the quantities and distributions of pollutants in the atmosphere, but the future evolutions in European and global emissions also play a significant role. Faced with climate change and increased emissions in some countries in the world, as in Asia, the impacts of European policies for reducing anthropogenic emissions are mitigated, depending on the regions and the pollutants due to the respective influence of local emission and of long-range transport of pollutants.

Je présente ici mes travaux de thèseque j’ai réalisé ces trois dernières années au seindu Laboratoire ATMosphères et Observations Spa-tiales (LATMOS) de l’Université de Versailles St-Quentin-en-Yvelines (UVSQ) et du Jet PropulsionLaboratory (JPL), California Institute of Technol-ogy. Pendant ces 3 ans je me suis intéressé à la réac-tivité chimique des composés organiques en phasegaz et solide, en utilisant des expériences de labo-ratoire simulant les conditions de l’ionosphère et dela basse atmosphère de Titan, le plus gros satellitede Saturne. Titan est la seule lune du Système So-laire qui possède sa propre atmosphère. Cette atmo-sphère est principalement composée d’azote molécu-laire (N2). Le méthane (CH4) forme le gaz sec-ondaire. D’une part, j’ai analysé les composés neu-tres et les composés chargés (ions) présents dansdes mélanges gazeux simulant la haute atmosphèrede Titan. Ces composés sont considérés commeprécurseurs chimique à la brume organique observéeentourant Titan. C’est-à-dire qu’ils forment les pre-mières étapes d’une succession de réactions chim-iques de plus en plus élaborées formant plus bas dansl’atmosphère des particules solides complexes. Lanature de ces particules dans l’atmosphère de Titanreste encore à élucider complètement. Mon travailpendant cette thèse a été d’utiliser des expériencesde laboratoire pour investiguer la réactivité chim-ique en phase gaz (Chapitres 3 & 4), précurseurs àla formation d’aérosols, ainsi que le vieillissement deces composés plus bas dans l’atmosphère lorsqu’ilsforment les premiers condensats de nucléation à laformation de nuages (Chapitre 5). / Titan is the only moon in the SolarSystem to possess its own dense and gravitationallybound atmosphere, and is even larger than planetMercury. Its rocky diameter is a mere 117 km shy ofGanymede’s. If we were to scoop up a 1 cm3 sam-ple from Titan’s upper atmosphere, we would findtwo dominant molecules: molecular nitrogen N2 andmethane CH4. Should we look a bit more carefully,we would find many neutral molecules and positiveand negative ion compounds. These chemical speciesare the outcome of processes resulting from ener-getic radiation reaching Titan’s upper atmosphere,breaking apart the initial N2 and CH4. A cascadeof subsequent reactions will trigger the formationof new gas phase products more and more com-plex. Eventually, these products mainly contain-ing hydrogen, carbon and nitrogen will form largefractal aggregates composing the opaque haze en-shrouding the surface of Titan. This haze is whatgives Titan such a unique brownish hue. Most ofthe photochemically-produced volatiles will eventu-ally condense in the lower atmosphere, where theymay aggregate to form micrometer-sized icy parti-cles and clouds. During my PhD, I have focusedmy studies on (i) the gas phase reactivity of aerosolprecursors in experimental conditions analogous toTitan’s upper atmosphere (Chapters 3 & 4), and (ii)the end of life of some of the products as they con-dense in the lower and colder atmosphere (Chapter5). I used two experiments to address these respec-tive issues: the PAMPRE plasma reactor, located atLATMOS, UVSQ, Guyancourt, France, and the Ac-quabella chamber at the Jet Propulsion Laboratory,California Institute of Technology, Pasadena, USA.In this manuscript, I present my work on the neutraland positive ion reactivity in the PAMPRE plasmadischarge, as well as ice photochemistry results usinglaser irradiation in near-UV wavelengths.

Fossils fuels are highly demanded in everyday life domestically or industrially. Fossil fuels are finite resources and they are rapidly depleting, as such alternative renewable feedstocks are sought to replace fossil fuels. Tall oil from paper processing and cashew nut shell liquid from the cashew nut industry are the two major renewable sources we studied, they are both waste byproducts, and have the potential to be converted into value-added materials. Tall oil from the paper industry mainly contained tall oil fatty acid, and under isomerising methoxycarbonylation with palladium catalyst, dimethyl 1,19-dimethyl nonadecanedioate can be obtained. This difunctional ester, dimethyl 1,19-dimethyl nonadecanedioate, is converted to diols, secondary and primary diamines by a hydrogenation reaction with ruthenium complexes of 1,1,1-tris(diphenylphosphinometyl)ethane (triphos) as catalysts in the presence of water, amine or aqueous ammonia respectively. In the case of aqueous ammonia it is necessary to use a two step reaction via diol to obtain 1,19-diaminononadecane. Diesters, diols and diamines are useful precursors for the synthesis of polyesters and polyamides. Difunctional substrates with 8-19 carbon chains are all tolerated under the reaction conditions and are successfully converted to the corresponding diols and diamines in high yields. Under similar hydrogenation conditions with the same ruthenium catalyst, cyclic products were predominantly produced with decreased chain length. N-heterocycles, which are important building blocks for the synthesis of drug molecules, were formed from the hydrogenation of diesters with 4-7 carbon chains in the presence of an amine. Another polymer precursor, ε-caprolactam, which is the precursor for Nylon 6, is obtained in a reasonable yield from both adipic acid and adipate esters together with aqueous ammonia in the presence of ruthenium catalyst. Cashew nut shell liquid was also converted into useful medical drugs, such as norfenefrine, rac-phenylephrine, etilefrine and fenoprofene in reasonable yields. Most of these drug molecules have been formed from 3-vinylphenol by catalytic hydroxyamination followed by methylation or ethylation. 3-Vinylphenol was synthesised from cardanol by ethenolysis to 3-non-8-enylphenol followed by isomerising ethenolysis, whilst the N-alkylation reactions used methyl or ethyl triflate to avoid dialkylation. Fenoprofene was formed by firstly O-phenylating cardanol then ethenolysis followed by isomerising ethenolysis to form 1-phenoxy-3-vinylbenzene. Methoxycarbonyation followed by hydrolysis formed the final product in good yield. Our methods start from renewable waste materials and avoid unpleasant reagents in the original stoichiometric synthesis of those drugs, for example, cyanide is no longer essential for the synthesis of fenoprofene.

Made available in DSpace on 2014-12-17T15:42:21Z (GMT). No. of bitstreams: 1 JoseEMS_TESE.pdf: 5374821 bytes, checksum: 56fe60cd3bbf0a42f7512c62fe5b976e (MD5) Previous issue date: 2013-03-08 / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior / Were synthesized spinel-type ferrites with general formula Ni0,8Mg0.2-xMxFe2O4, where M represents the doping Mn, Co or Mn + Co simultaneously, x ranges for the values 0.02, 0.05 and 0.1. The value of x was divided by 2 in cases where M equals Mn and Co conjugates. We used the citrate precursor method and heat treatment to obtain the phases at 1100?C. The materials were characterized by XRD, TGA/ DTGA, SEM, MAV and reflectivity measurements by the method of waveguide. Powders to 350?C/3.5 h were crystalline and nanosized. According to the results this temperature all powders have a percentage of ferrite phase over 90%. The composition had the addition of Mn and Co simultaneously showed a higher percentage of secondary phase NiO, 5.8%. The TGA/DTGA curves indicate that this sample reached phase (s) crystalline (s) at lowest temperatures. The X-ray diffractograms of the samples calcined at 350?C and 1100?C were treated with the Rietveld refinament technique. The powders calcined at 1100 ?C/3h in air show to be 100% except spinel phase composition with 0.02 doping. The micrographs show clusters of particles with sizes smaller than 1 μm in calcination temperature of 1100?C which agreed with the result of Rietveld refinement. In the compositions doped with Mn were higher values of magnetization (45.90 and 53.20 Am2/kg), which did not cause high microwave absorption. The theoretical calculation of magnetization (MT) was consistent with the results, considering that there was agreement between the increase of magnetization experimental and theoretical. It was observed that there was the interrelation of the final effect of absorption with the thickness of MARE, the composition of ferrimagnetic materials and in particular the specific values of frequency. The analysis shows that the reflectivity increases in the concentration of cobalt increased the frequency range and also for absorption 10.17 GHz and 84%, respectively. The best result of chemical homogeneity and the value of 2.96 x 10-2 tesla coercive field were crucial for high performance ferrite absorber with 0.1 cobalt. The Cobalt has high magnetocrystalline anisotropy, it is associated with an increased coercive field, Hc. Therefore, this property improves the results of reflectivity of spinel ferrites / Foram sintetizadas ferritas do tipo espin?lio com f?rmula geral Ni0,8Mg0,2-xMxFe2O4, onde M representa os dopantes Mn, Co ou Mn + Co simultaneamente, x varia para os valores 0,02; 0,05 e 0,1. O valor de x foi dividido por 2 nos casos em que M equivale a Mn com Co conjugados. Foi utilizado o m?todo dos citratos precursores e tratamento t?rmico na obten??o das fases a 1100?C. Os materiais foram caracterizados por DRX, TGA/DTGA, MEV, MAV e medidas de refletividade pelo m?todo de guia de ondas. Os p?s a 350?C/3,5h foram cristalinos e nanom?tricos. De acordo com os resultados nesta temperatura todos os p?s apresentam um percentual de fase ferrita superior a 90%. A composi??o que teve a adi??o de Mn e Co simultaneamente apresentou maior percentual de fase secund?ria NiO, 5,8%. As curvas TGA/DTGA indicam que essa amostra alcan?ou fase(s) cristalina(s) em temperaturas mais baixas. Os difratogramas de raios X das amostras calcinadas a 350?C e 1100?C foram tratados pela t?cnica de refinamento Rietveld. Os p?s calcinados a 1100?C/3h em atmosfera ambiente mostram ser 100% de fase espin?lio exceto a composi??o com 0,02 de dopantes. As micrografias apresentam aglomerados de part?culas com tamanhos menores que 1 μm na temperatura de calcina??o de 1100?C, o que concordou com o resultado de refinamento Rietveld. Nas composi??es dopadas com Mn ocorreram os maiores valores de magnetiza??o (45,90 e 53,20 Am2/kg), o que n?o acarretou alta absor??o de microondas. O c?lculo te?rico da magnetiza??o (MT) foi coerente com os resultados, considerando-se que houve concord?ncia entre o aumento das magnetiza??es experimental e te?rica. Observa-se que houve interrela??o do efeito final de absor??o com a espessura do MARE, a composi??o do material ferrimagn?tico em particular e os valores espec?ficos de freq??ncia. A an?lise de refletividade indica que o aumento na concentra??o de cobalto aumentou a faixa de freq??ncia e a absor??o para 10,17 GHz e 84%, respectivamente. O resultado indica que a melhor homogeneidade qu?mica e o valor 2,96 x 10-2 tesla de campo coercitivo foram determinantes para o alto desempenho absorvedor da ferrita com 0,1 de cobalto. O Cobalto tem alta anisotropia magnetocristalina, isto est? associado ao aumento do campo coercitivo, Hc. Portanto, essa propriedade melhora os resultados de refletividade das ferritas espin?lio

<p>U ovom radu, sintetisani su poli(uretan-izocijanuratni) elastomeri sa kovalentnim<br />čvorovima, katalitičkom ciklotrimerizacijom teleheličnih diizocijanata kao prekursora mreže<br />na osnovu 2,4-toluen-diizocijanata, &alpha;,&omega;-dihidroksipoli(oksipropilen)diola i monoola<br />dietilenglikolmonometiletra. Dobijeni su i termoplastični segmentirani poliuretani, sa<br />čvorovima fizičkog umreženja, jednostepenim postupkom i metodom prepolimerizacije,<br />reakcijom dve vrste alifatskog polikarbonatnog diola, koji se razlikuju u strukturi lanca,<br />heksametilen-diizocijanata i produživača lanca (1,4-butandiola). Sintetisana je i serija<br />poliuretanskih hibridnih materijala, dodatkom 1% <em>m/m</em> nanočestica organski modifikovanih<br />glina (montmorilonita i bentonita). Prioritet rada je bio da se utvrdi uticaj udela elastično<br />aktivnih i visećih lanaca na dinamičko-mehanička svojstva, toplotnu stabilnost i svojstva<br />prigu&scaron;enja poliuretanskih mreža sa izocijanurat (heksahidro-1,3,5-triazin-2,4,6-trion)<br />prstenovima, kao čvorovima. Takođe, cilj istraživanja je bio da se ispita uticaj odnosa<br />reaktivnih grupa diizocijanata, polikarbonatne komponente i produživača lanca, kao i dodatka nanočestica na svojstva povr&scaron;ine, morfologiju, dinamičko-mehanička i toplotna svojstva segmentiranih neojačanih i ojačanih elastomera. Toplotna degradacija poli(uretanizocijanuratnih) mreža i segmentiranih termoplastičnih poliuretana praćena je neizotermskim ispitivanjima, koristeći istovremenu termogravimetrijsku i masenu analizu (TG-MS), kao i istovremenu termogravimetriju i diferencijalno skenirajuću kalorimetriju (TG-DSC). Viskoelastična svojstva i svojstva prigu&scaron;enja dobijenih poliuretanskih elastomera su ispitivana pomoću dinamičko-mehaničke analize (DMA). Toplotno pona&scaron;anje segmentiranih poliuretana i nanokompozita, dobijenih jednostepenim postupkom sinteze, je proučavano modulovanom diferencijalno skenirajućom kalorimetrijom (MDSC). Temperatura prelaska u staklasto stanje i termoplastična svojstva neojačanih i ojačanih poliuretanskih materijala, dobijenih postupkom prepolimerizacije, određeni su primenom diferencijalno skenirajuće kalorimetrije (DSC). Hemijska struktura i formiranje vodoničnih veza dobijenih elastomera proučavane su koristeći Furijeovu transmisionu infracrvenu spektroskopiju (FTIR). Uticaj udela tvrdih segmenata na morfologiju i svojstva povr&scaron;ine segmentiranih poliuretana, ispitivan je pomoću mikroskopije atomskih sila (AFM). Stepen kristalnosti uzoraka i dispergovanje nanočestica u dobijenim hibridnim materijalima su odre&ntilde;eni primenom metode rasipanja X-zraka pod &scaron;irokim uglom (WAXS).</p> / <p> In this work, poly(urethane-isocyanurate) elastomers, with covalent junction points,<br /> were synthesized by catalytic cyclotrimerization of telechelic diisocyanates as network<br /> presursors based on 2.4-tolylenediisocyanate, a,w,dihydroxypoly(oxypropylene) and monool<br /> component 2-(2-metoxyetoxy)ethanol. Thermoplastic polyurethanes, with physical<br /> crosslinking, were obtained by one-step technique and pre-polimerization method, using two<br /> aliphatic polycarbonate diols (differening in chain constitution), hexamethylene-diisocyanate<br /> and chain extender (1,4-butane diol) as reactive components. One serie of polyurethane<br /> hybrid materials was prepared by addition of 1 wt. % of organically modified clay<br /> nanoparticles (bentonite and montmorillonite). The goal of this work was to investigate the<br /> influence of elastically active and dangling chains content on thermal stability, dynamic<br /> mechanical and damping properties of polyurethane networks with heat-resistant<br /> isocyanurate-(hexahydro-1,3,5-triazin-2,4,6-trion) rings, as crosslinks. The aim was also to<br /> determine the influence of diisocyanate, macrodiol and chain extender reactive groups&rsquo; ratio<br /> and nanoparticles addition on surface properties, morphology, dynamic mechanical and<br /> thermal properties of obtained segmented unfilled and filled elastomers. Thermal degradation<br /> of poly(urethane-isocyanurate) networks and segmented thermoplastic polycarbonate-based<br /> polyurethanes was investigated by nonisothermal analysis, using thermogravimetry coupled<br /> with mass spectroscopy analysis (TG-MS) and thermogravimetry coupled with differential<br /> scanning calorimetry (TG-DSC). Viscoelastic and damping properties of obtained<br /> polyurethane elastomers were estimated by dynamic mechanical measurements (DMA).<br /> Modulated differential calorimetry (MDSC) was used to investigate thermal behavior of<br /> segmented polyurethanes and nanocomposites, synthesized using one-step technique. The<br /> glass transition temperature and thermoplastic properties of unfilled and filled polyurethane<br /> materials, prepared by pre-polimerization procedure were assessed by differential scanning<br /> calorimetry (DSC). Fourier transform infrared spectroscopy (FTIR) was used to investigate<br /> the hydrogen bond formation and chemical structure of prepared segmented elastomers. The<br /> investigation of the influence of hard segment content on morphology and surface topography<br /> of prepared segmented elastomers sheets was done by atomic force microscope (AFM). In<br /> order to determine the degree of cristallinity and to evaluate the dispersion of<br /> montmorillonite and bentonite in the polyurethane matrices, the prepared hybrid materials<br /> were characterized by wide angle X-ray scattering (WAXS).</p>