Les spéléothèmes (concrétions carbonatées se formant dans les zones karstiques) sont des archives paleo-climatiques reconnues, dont l’intérêt majeur est de pouvoir être datées précisément par la méthode Uranium-Thorium. En revanche, les traceurs traditionnellement utilisés pour reconstruire les climats passés à partir de ces objets géologiques ne sont pas directement quantifiables en termes de paramètres climatiques comme la température moyenne, ou la quantité de précipitation. Les variations des concentrations en éléments traces contenus dans les spéléothèmes ont pu être relié dans certains sites aux changements climatiques passés, mais des doutes existent sur la robustesse de leur signal au sein d’une même grotte et entre différents sites.Nous nous sommes appliqués à déterminer les variations au cours des 50 000 dernières années de plusieurs catégories d’éléments (alcalino-terreux, uranium, et terres rares) dans des stalagmites de deux grottes situées dans le sud de la France (les grottes de Villars en Dordogne et de Chauvet en Ardèche), par spectrométrie ICP-MS. Les spéléothèmes sélectionnés ont déjà été datés et ont enregistré les variations paleo-environnementales à travers les isotopes stables de la calcite. Trois périodes d’étude caractérisées par des changements particuliers sont étudiées: le stade isotopique 3 de la dernière période glaciaire (~50-30 ka), la dernière déglaciation (~20-10 ka) et la fin de l’Holocène (~2-0 ka).Le signal des variations des alcalino-terreux à Villars pendant le stade isotopique 3 est significatif et robuste. La variabilité du strontium notamment, qui provient de processus hydrologiques intra-karst, suit les événements climatiques rapides enregistrés dans l’hémisphère Nord. D’autre part, le comportement de nombreux éléments traces pendant la déglaciation est similaire entre les grottes de Villars et de Chauvet. Enfin, des changements du couvert végétal sont probablement à l’origine des changements synchrones enregistrés par les éléments traces et les isotopes stables de la calcite au cours des deux derniers millénaires à Villars.Par ailleurs, l’étude des coefficients de partition des alcalino-terreux, de l’uranium et des terres rares dans des conditions variées montre l’importante de la variabilité inter-site de leur partitionnement. / Calcareous deposits forming within caves, also known as speleothems, have become acknowledged paleoclimatic archives. One of their main interests is that they can be absolutely dated by Uranium-Thorium methods. However, traditionally used speleothem climatic proxies cannot be directly translated into environmental variables such as the mean annual temperature or the amount of annual rainfall. In some contexts, the variations of trace element concentrations in speleothem calcite could be linked to past climatic changes, but the robustness of trace element signals between speleothems of the same or nearby caves is still questionable.We determined by ICP-MS the concentrations of several families of chemical elements (alkaline-earth metals, uranium, rare-earth elements) in stalagmites from two caves located in Southern France (Villars cave in Dordogne and Chauvet Cave in Ardèche) spanning the last 50,000 years. The selected speleothems had already been dated and their stable isotope profiles had proven to record paleoenvironmental fluctuations occurring during three separate periods: the Marine Isotopic Stage 3 or MIS 3 (~50-30 ka), the Last Deglaciation (~20-10 ka), and the end of the Holocene (~2-0 ka).Variations of alkaline-earth metals recorded in two stalagmites from Villars Cave during MIS 3 are significant and robust. Notably, Sr concentrations follow the rapid climatic changes recorded in the Northern Hemisphere. Furthermore, several trace elements behave similarly during the Last Deglaciation in the Villars and the Chauvet Cave. Finally, changes of the vegetation cover above the cave are likely to have caused the synchronous fluctuations of the trace element and stable isotope contents that happened during the last two thousand years in Villars speleothems.Lastly, the partition coefficients of alkaline-earth metals, uranium and rare-earth elements were measured in different sites and conditions and proved to be very site-dependent.

[pt] O crescimento populacional vem acarretando um incremento no consumo de combustíveis fósseis e na queima de biomassa e, como conseqüência, um aumento na fonte de partículas de carbono negro (ou black carbon - BC) em ambientes costeiros e estuarinos. Este material orgânico refratário vem sendo estudado nos últimos 30 anos e é considerado um importante reservatório geoquímico. Todavia, sua função no ciclo do carbono ainda não é totalmente caracterizada. O BC desempenha um papel de causador de problemas ambientais (como aquecimento global) e também de atenuador dos riscos representados pelos contaminantes orgânicos devido ao seu efetivo poder sorvente. Este trabalho apresenta de forma inédita a distribuição de BC em sedimentos e sua relação com compostos HPAs de uma região estuarina do Estado do Rio de Janeiro - Baía de Guanabara (ambiente conhecidamente afetado por poluição crônica de diversos compostos). Para realização da pesquisa, foi realizado primeiramente uma validação e escolha metodológica entre 2 protocolos de determinação de BC encontrados na literatura: oxidação química com dicromato/ácido sulfúrico e oxidação térmica a 375 oC, em que este último apresentou maiores vantagens e foi selecionado para determinar BC nas amostras de sedimento. Os teores de BC foram determinados por um analisador elementar Carlo Erba EA1110. Os teores de BC nos sedimentos superficiais (0-2 cm) de 25 estações da região interna da baía foram de 0,19 %p.s. . +- 0,07 %p.s. ., variando entre 0,03 %p.s. . e 0,31 %p.s. . A distribuição na baía de Guanabara sugere a presença de um gradiente decrescente de partículas pirogênicas da região de fundo da baía em direção à zona costeira. Determinações de carbono orgânico total (TOC), razões molares C/N e distribuições BC:TOC (5,35 % +- 2,45 %, n = 25) foram dados adicionais avaliados. Testemunhos de sedimento de 90 cm de comprimento de 3 manguezais da região norte foram estudados: Suruí, Nova Orleans e Piedade, que exibiram teores de BC de 0,11 %p.s. . +- 0,08 %p.s. . e BC:TOC de 1,99 % +- 1,59 % (n = 62). A relação entre o material BC e HPAs (determinados em estudo anterior) nas camadas sedimentares pôde ser analisada através de correlações e da análise de componentes principais e revelaram uma tendência de sorção destes compostos contaminantes com BC nos bosques de Nova Orleans e Suruí. Em Piedade, as razões de compostos HPAs alquilados (1,7-dimetilfenantreno e 2,6- dimetilfenantreno) apontaram para um domínio de produtos de combustão de madeira, que não pode ser isolado pela metodologia aplicada. Adicionalmente, a sorção de HPAs no material BC foi confirmada pela realização de um experimento de fortificação de pireno (concentrações monitoradas por análise de fluorescência - espectrofluorímetro de luminescência Perkin Elmer LS55B). Os resultados discutidos aumentaram o conhecimento sobre as diferentes frações da matéria orgânica nos sedimentos da Baía de Guanabara e apontam para a importância da fração carbono negro (ainda pobremente pesquisada no Brasil) no carbono orgânico total e na regulação da liberação de contaminantes hidrofóbicos para o ambiente e biota. / [en] Black carbon (BC) is a term used to represent the continuum of charred materials produced during incomplete combustion of fossil fuel and biomass. Since the emission rates of BC are increasing in the last decades due to energy requirements from modern human population, there is great interest in the distribution of BC in the environment (atmosphere, water and sediment) because their role in the biogeochemical cycle of carbon is not fully understood and, also, because the high adsorption capacity of BC particles may decrease the bioavailability of organic contaminants (PAH, for example). In the present work it was determined the distribution, for the first time ever, of BC in superficial sediments from Guanabara Bay and it was evaluated the relation between BC (quantified in the present work) and known concentration of polycyclic aromatic hydrocarbons (PAHs) in sediment cores from 3 mangrove regions in the bay (Suruí, Nova Orleans and Piedade). Two analytical protocols for BC quantification were compared (chemical oxidation with dichromate/sulphuric acid and thermal oxidation at 375 ºC), and the second one was chosen for routine analysis. After treatment, the BC content was measured by a dry-oxidation method in a Carlo Erba EA110 elemental analyser. Total organic carbon (TOC) was also measured using the same instrument. In the superficial sediments (0-2 cm) from Guanabara Bay, the mean BC carbon content (n = 25) was 0.19 +- 0.07 % (dry-weight mass), ranging from 0.03 % to 0.31 %. The percentage of BC to TOC was 5,35 +- 2,45 (n = 25). The sediments in the northern sector of the bay had higher contents of BC, what is related to the input of pyrolitc materials from river and urban runoff and local restricted water circulation. In the mangrove sediments, the BC content was 0.11 +- 0.08 % (dry- weight mass) and the BC:TOC fraction was 1.99 +- 1.59 % (n = 62). Linear regression and principal components analysis revealed that the distribution of PAH is closed related to the BC contents in the sediment from Suruí and Nova Orleans, but not for Piedade sediments, probably due to uncertainties in the origin of PAHs in these sediments. An experiment with fortification of sediment with pyrene confirmed the importance of adsorption of PAH to the BC particles. In conclusion, the data obtained in the present work permitted a better understanding of the different fractions of organic matter in the sediments from Guanabara Bay and showed the importance of BC in the fate and possible effects of PAH in this coastal contaminated system.

O Sistema de Nappes Carrancas compõe um sistema de nappes que circunda ao sul o Cráton do São Francisco e é formado pela Unidade Biotita Xisto e pelas formações Campestre e São Tomé das Letras do Grupo Carrancas. A Unidade Biotita Xisto contém veios de quartzo e xistosidade anastomosada e é formada por quartzo, biotita, muscovita, clorita e, localmente plagioclásio, carbonato e granada. A Formação Campestre é formada por quartzitos intercalados a filitos/xistos que variam de cloritóide filitos grafitosos, com muscovita, quartzo e turmalina e, localmente, granada a xistos com granada, estaurolita e cianita. A investigação da Unidade Biotita Xisto como autóctone em relação ao Cráton do São Francisco, seu potencial agrupamento com o Grupo Carrancas em uma megassequência deposicional, bem como sua comparação com a unidadealóctone Xisto Santo Antônio (Nappe Andrelândia) constituem parte dos objetivos deste estudo. Para tal, foram feitas análises químicas e isotópicas (Sr e Nd) em rocha total e geocronologia U-Pb em cristais de zircão detríticos, tanto na Unidade Biotita Xisto como na Formação Campestre, com intuito de elucidar a relação entre as mesmas e compará-las com dados da literatura disponíveis para o Xisto Santo Antônio. A Unidade Biotita Xisto apresenta características químicas compatíveis com sedimentos que sofreram intemperismo químico de intensidade e período de tempo moderados, depositados em ambientes de colisão continental, com área-fontecomposta essencialmente por rochas félsicas. Assinaturas de elementos traço e isotópicas de Sr ( \'ANTPOT.87 Sr\'/\'ANTPOT. 86 Sr\' entre 0,713 e 0,715) e Nd (\'\'épsilon\' IND.Nd\' entre -6 e -5) indicam contribuição de arco magmático e crosta continental e diferem, portanto, daquelas esperadas em ambientes de margempassiva. A mesma contribuição é observada para o Xisto Santo Antônio, cuja área fonte registra importante assinatura de material juvenil. As idades U-Pb LA-MC-ICP MS obtidas em cristais de zircão mostram contribuição principal de rochas do final do Criogeniano e contribuição secundária do Riaciano. A classe modal ao redor de 665 Ma é comparável com a idade cristais de zircão detrítico do Xisto Santo Antônio, o que aponta parauma mesma área-fonte principal para ambas unidades. A deposição dos sedimentos precursores da Unidade Biotita Xisto ocorreu entre 630-611 Ma, sendo as fontes principais os granulitos cálcio-alcalinos e rochas vulcânicas co-genéticas, além de granitos sin-colisionais da Nappe Socorro-Guaxupé. A pouca representatividade de idades paleoproterozóicas e a ausência de assinaturas químicas de margem passiva, inviabilizam as rochas do Cráton doSão Francisco como parte da área-fonte. Desta forma, a Unidade Biotita Xisto não é autóctone em relação ao Cráton do São Francisco, sendo, potencialmente, a unidade que compõe a frente da Nappe Andrelândia. Por outro lado, a Formação Campestre possui assinatura geoquímica de sedimentos que sofreram uma intensa reciclagem e alteração da composição do sedimento original. As assinaturas químicas de elementos traço e isotópicas Sr e Nd indicam contribuição de crosta continental superior, com componente de crosta antiga e sem afinidade com sedimentos depositados em margem passiva (\'ANTPOT.87 Sr\'/\'ANTPOT. 86 Sr\' entre 0,74 e 0,76; \'\'épsilon IND.Nd\' entre -18 e -15). Os zircões detríticos analisados forneceram idades U-Pb LA-MC-ICP-MS variadas, do Toniano ao Mesoarqueano, correlacionáveis com rochas vulcânicas e plutônicas do Cráton do São Francisco, com as faixas marginais do Cráton de Angola e/ou faixas orogênicas do Cráton Amazônico e com rochas dos arcos Mara Rosa e Goiás.A abrangência das idades U-Pb da Formação Campestre e das formações Chapada dos Pilões e Paracatu, permite a correlação, no Orógeno Brasília, entre os Grupos Carrancas e Canastra. A paleogeografia mais provável é a de um ambiente de rifte, antecessor à deriva e aoestabelecimento de uma margem continental passiva. / The Carrancas Nappe System composes a system of nappes that surround the southern margin of the São Francisco Craton and is formed by the Biotite Schist Unit and by the Campestre and São Tomé das Letras formations of the CarrancasGroup. The Biotite Schist Unit encompass quartz veins and anastomosed schistosity and is formed by quartz, biotite, muscovite, chlorite and, locally plagioclase, carbonate and garnet. The Campestre Formation is composed by interleaved quartzites and phyllite/schist that varies from graphite-chloritoid phyllites, with muscovite, quartz, tourmaline and garnet, and locally garnet schists and schists with garnet, staurolite and kyanite. The investigation of the Biotite Schist Unit as authochtonous in relation to the São Francisco Craton, it´s potencial grouping with the Carrancas Group in a deposicional megassequence, as well as it´s comparison with the allochthonous Santo Antônio Schist (Andrelândia Nappe) is part of the goals of this study. For this purpose, chemical and isotopic (Sr and Nd) whole rock analysis were obtained, along with U-Pb detrital zircon data, in the Biotite Schist Unit and also in the Campestre Formation, in order to elucidate the relationship between these units and compare them with literature data available for theSanto Antônio Schist. The Biotite Schist Unit show chemical characteristics compatible with sediments that underwent chemical weathering of moderate intensityand time, deposited in continental collision setting, with source region composed essentially by felsic rocks. Trace elements and Sr isotopic signatures ( \'ANTPOT.87 Sr\'/\'ANTPOT. 86 Sr\' between 0,713 and 0,715) and Nd (\'\'épsilon IND.Nd\' between -6 and -5) points to contribution from magmatic arc and continental crust, and are different from the expected for passive margin settings. The same contribution is observed in the Santo Antônio Schist, which source area registers an important juvenile material signature. The U-Pb LA-MC-ICP MS zircon data show major contribution from rocks of the later Cryogenian and minor contribution from the Ryacian. The modal class around 655 Ma is comparable with the U-Pb detrital zircon data from the Santo Antônio Schist, pointing to the same source area for both units. The deposition of the precursors sediment of the Biotite Schist Unit occurred between 630 - 611 Ma, and the main sources were the calk-alcaline granulites and co-genetic volcanic rocks, besides the Socorro-Guaxupé Nappe sin-collisional granites. The low representation of Paleoproterozoic ages and the absence of passive margin chemical signatures preclude the rocks of the São Francisco Craton as part of the source area. Thus, Biotite Schist Unit is not an autochthonous unit in relation to the São Francisco Craton, and is, potentially, the unit that composes the Andrelândia Nappe front. On the other hand, the Campestre Formation has geochemical signatures of sediments that underwent intense recycling and alteration of the original sediment. The trace element and Sr and Nd isotopic signatures indicates upper continental crust contribution, with older crust component and no affinity with passive margin sediments ( \'ANTPOT.87 Sr\'/\'ANTPOT. 86 Sr\' between 0,74 and 0,76; \'épsilon\' IND.Nd\' between -18 and -15). The U-Pb LA-MC-ICP MS detrital zircon data provide varied ages, from the Tonian to the Mesoarchean, correlated withvolcanic and plutonic rocks of the São Francisco Craton, with the marginal belts of the Angola Craton, and/or orogenic belts of the Amazonian Craton and with the Mara Rosa and Goiás magmatic arcs. The range of the U-Pb ages of the Campestre Formation and the Chapada dosPilões and Paracatu formations, allows the correlation, in the Brasília Orogen, of the Campestre and Canastra groups. The most likely paleogeography is that of a rift setting, before the continental drift and the establishment of a passive continental margin.

Materiais de Referência (MR) de substâncias químicas têm ampla aplicação, sobretudo na área analítica, servindo de referência para validação de métodos, calibração de instrumentos e controle de qualidade, estabelecendo a comparabilidade de resultados analíticos em escala global e permitindo a transferência da exatidão entre métodos, laboratórios e padrões. Norteado por essas necessidades, o trabalho apresenta uma proposta para certificação de MR baseada nas orientações preconizadas por diretrizes e normas internacionais, principalmente as que seguem o ISO Guia 34, para estabelecer as propriedades certificadas através de técnicas analíticas de Espectrometria de Massas de Alta Resolução, Ressonância Magnética Nuclear, de ¹H e de ¹³C, e de Análise Elementar CHN. A certificação contemplou as caracterizações qualitativa e quantitativa, ensaio de estabilidade e o cálculo da estimativa da incerteza da medição. Como resultado, foi produzido e certificado um lote piloto de MR de β-N-metilamino-alanina (BMAA), uma toxina obtida in-house através de síntese química e purificação, cujos valores de propriedades certificadas foram rastreáveis ao SI e acompanhadas da estimativa da incerteza da medição. / Reference Materials (RM) of chemicals have wide application, particularly in the analyses, providing a reference for validation of methods, instrument calibration and quality control, establishing the comparability of analytical results on a global scale and enabling the transfer of accuracy between methods, laboratories and standards. Guided by these requirements, the paper presents a proposal for certification of MR based on the guidelines recommended by international guidelines and standards, especially those which follow the ISO Guide 34, to establish the certified properties through analytical techniques of mass spectrometry High resolution Nuclear Magnetic Resonance, ¹H and ¹³C, and CHN elemental analysis. The certification included qualitative and quantitative characterization, stability test and the calculation of the estimate of measurement uncertainty. As a result, was produced and certified a pilot batch of RM β-N-methylamino-alanine (BMAA), a toxin obtained in-house via chemical synthesis and purification, whose property values are certified and traceable to the SI accompanied by an estimative of the uncertainty of measurement.

Die oxidative Transformation der Thiol-Gruppe des Cysteins in verschiedene andere funktionelle Gruppen wird als sehr wichtige posttranslationale Modifikation (PTM) angesehen. Cysteinsulfensäure (SA) ist eine Zwischenstufe der Thiol-Oxidation: Sie kann entweder mit freien Thiolen reagieren, um Disulfide zu bilden oder durch reaktive Sauerstoffspezies (reactiveoxygenspecies, ROS) weiter oxidiert werden. Jede Störung des zellulären Redox-Haushalts wird mit altersbedingten Erkrankungen , daher stellt die Überwachung des SA-Spiegels einen vielversprechenden Wegdar, den Status dieses Redox-Haushalts festzustellen. Da bereits kleinste Änderungen der Proteinmengen und PTMs tiefe Einblicke in den Zustand des biologischen Systems liefern können, ist eine quantitative Bestimmung von großer Bedeutung.Technologische Fortschritte im Bereich der Trennungsmethoden und Massenspektrometrie (MS) erlaubten die Entwicklung umfassender Möglichkeiten in der Protein-Analytik. In dieser Arbeit wurde eine neue, hochsensitive und selektive Methode zur Detektion von SA entwickelt. Dafür wurde ein Alkin-β-Ketoester (KE) an einen Lanthanid-haltigen (Ln) Chelatkomplex. Zum Nachweis des Funktionsprinzips wurden, mittels H2O2, Sulfensäuren in verschiedenen Peptidsequenzen erzeugt, um die in biologischen Systemen durch ROS hervorgerufenen Oxidationen nachzustellen. Diese Sulfensäuren wurden anschließend durch den Ln-DOTA-KE-Komplex gebunden. Die Bildung dieser SA-Ln-DOTA-KE-Einheit wurde mittels (Elektronenspray-Ionisation/ ESI-MS) und (induktiv gekoppeltem Plasma/ICP-MS) nachverfolgt. Die entwickelte Methode wurde weiterhin auf die Bestimmung von SA-Bildung in humanem Serum angewandt, humanes Serumalbumin wurde angereichert via Affinitätschromatographie. ICP-MS diente der Bestimmung der SA-Ln-DOTA-KE-Einheit, durch Kombination mit einer Isotopenverdünnungsanalyse (IDA) wurde eine absolute Quantifizierung durchgeführt. Die Ergebnisse zeigen oxidative Schäden bis zu 40 % des vorhandenen Albumins. / Oxidative transformation of cysteine thiol group into different functional groups is considered a significant posttranslational modification (PTM) of great importance. Cysteine sulfenic acid (SA) is the transient state for thiol group oxidation; it can react with free thiols to form disulfide bonds or can be further oxidized with reactive oxygen species (ROS) to form sulfinic and sulfonic acids. As any disturbance in the cellular reduction-oxidation (redox) balance is correlated to age-related diseases, the detection of SA transient state formed a sensor for such redox-mediated events. Whereas only any small change in the quantity of proteins, as well as the formed PTMs, can provide deeper insights into the status of the biological system, quantitative analysis should be carried out to reveal the status of the system. On the other hand, the technological advances, in particular the separation techniques and mass spectrometry (MS), allowed the development of several approaches for the comprehensive assessment of proteome analysis. Herein, we provide a new strategy for the highly sensitive and specific detection of SA using alkyne β-ketoester (KE) previously linked to a lanthanide (Ln)-containing chelator (Ln-DOTA. SA was generated by hydrogen peroxide (H2O2) in different peptide sequences by ROS and was detected by the prepared compound Ln-DOTA-KE. Molecular mass spectrometry (electrospray/ ESI-MS) and (Inductively coupled plasma mass spectrometry /ICP-MS) have been used to monitor the formation of SA linked to Ln-DOTA-KE. The developed strategy has been further applied to the determination of SA-induced formation in human serum by using affinity chromatography for purification of albumin followed by ICP-MS to monitor the formed SA linked to Ln-DOTA-KE in combination with isotope dilution analysis (IDA) for the absolute quantification. Quantitative results showed levels of oxidative damage regarding SA formation in human serum up to 40% of the albumin present.

Das Thema der vorliegenden Dissertation ist die Theorie und Terminologie der Mischung nach Galen. Im ersten Teil, der sich aus den ersten zwei Hauptkapiteln zusammensetzt, werden die historischen und theoretischen Quellen für Galens Modell zur Mischung der Primärelemente (das Warme, das Kalte, das Trockene und das Feuchte) und sein System der neun Mischungen (acht schlechte Mischungen und eine gute Mischung, in der keine Qualität überwiegt). Im ersten Hauptkapitel illustriere ich im Gegensatz zu den bisherigen konträren wissenschaftlichen Meinungen, dass Galens Modell zur Mischung der Primärelemente eine klare innere Logik aufweist und von der peripatetischen Naturphilosophie des 2. Jahrhunderts unserer Zeitrechnung beeinflusst wird. Dabei entbehrt es keinesfalls des „archaischen“ hippokratischen Ansatzes. Im zweiten Hauptkapitel der Dissertation analysiere ich die historischen und theoretischen Quellen von Galens Theorie der neun Mischungen. Genauer gesagt zeige ich in diesem Kapitel auf, dass Galens Theorie im Gegensatz zu bisherigen Gelehrtenmeinungen nicht vollständig von dem System der neun Mischungen abhängt, das die Pneumatiker entwickelt haben. In der Tat beruht Galens Modell auf einer anderen – peripatetischen – Elementartheorie. Im Gegensatz zur pneumatischen Medizin ist dieses Modell der neun Mischungen in seinem allgemeinen Weltbild fest verankert. Im zweiten Teil dieser Dissertation, der dem dritten Hauptkapitel entspricht, setze ich mich mit Galens Terminologie der Mischung und genauer gesagt mit seiner Verwendung der Begriffe krasis und mixis auseinander. Im Gegensatz zu vorherigen wissenschaftlichen Arbeiten, die besagen, dass der Unterschied von den Bestandteilen abhänge (krasis wäre eine Mischung von Qualitäten, während mixis eine Mischung von Substanzen wäre), zeige ich, dass der Unterschied zwischen krasis und mixis in der Phase des Prozesses und in dem Grad der Wiedererkennbarkeit der Bestandteile liegt. / The present dissertation aimed at studying the theory and the terminology of mixture in Galen. The first part, which is composed of the first two main chapters, intended to examine the historical and theoretical sources of Galen’s model of mixture of primary elements (the hot, the cold, the dry and the wet) and of its system of nine mixtures (eight bad mixtures and one good mixture, where no quality predominates). In the first main chapter, I illustrated that, differently from the conflicting views expressed so far by the previous scholarship, Galen’s model of mixture of primary elements shows a clear internal logic and comes under the sway of the Peripatetic natural philosophy of the 2nd century CE, while in no way renouncing, on the other hand, the “archaic” Hippocratic background. In the second main chapter of the dissertation I analysed the historical and theoretical sources of Galen’s scheme of nine mixtures. More precisely, in this chapter we pointed out that, differently from what has been said by previous scholarship, although the Pneumatists developed a system of nine mixtures, Galen’s is not entirely dependent on it insofar as Galen’s relies on a different – Peripatetic – elemental theory and, differently from Pneumatic medicine, this scheme of nine mixtures is embedded in Galen’s general world view. In the second part of the thesis, which corresponds to the third main chapter, I have dealt with Galen’s terminology of mixture and, more precisely, with his usage of the terms krasis and mixis. Differently from the previous scholarship according to which the difference would depend on the constituents (krasis would be a mixture of qualities whereas mixis a mixture of substances), I have showed that the difference between krasis and mixis lies in the stage of the process and in the degree of recognisability of the constituents.

A aplicação de fertilizantes aos solos é frequente devido à atual demanda mundial pela produção de alimentos e às projeções feitas para o futuro. Fertilizantes orgânicos têm sido uma opção amplamente explorada devido ao seu preço, possibilidade de reuso de resíduos agriculturais e urbanos, além do caráter sustentável. Podem ser provenientes de diversas origens como lodo de esgoto, estercos e restos de animais e vegetais submetidos a processos de compostagem. Neste trabalho, foi desenvolvido método para determinação elementar total em fertilizantes orgânicos, substratos e condicionadores de solo, e realizados estudos de fracionamento e análise de especiação em fertilizante orgânico. Assim, foi realizada a caracterização geral das amostras com fracionamento por tamanho de partícula, análises dos teores de C e N, difração de Raios-X e determinação elementar total. Para este último, foi desenvolvido método de digestão assistida por radiação micro-ondas, com análise por ICP OES. O procedimento foi otimizado para diferentes misturas ácidas, as quais foram avaliadas quanto aos erros relativos para diversos elementos em CRM de lodo de esgoto, utilizando PCA como ferramenta estatística. A mistura escolhida, constituída por 3 mL HNO3 + 1 mL HBF4 + 2 mL H2O, foi utilizada para digestão das amostras. Apenas a concentração total não traz informações a respeito da mobilidade e disponibilidade dos elementos, então estudos de fracionamento elementar também foram realizados. Na primeira abordagem foi executado fracionamento por tamanho de partícula, no qual foi observado que quanto menor o tamanho de partícula menor o teor de C e maior o teor de N, e maior a concentração de micronutrientes e contaminantes (Cr, Cu, Fe, Mn, Pb e Zn), indicando que estes elementos podem estar mais associados a frações com mais características inorgânicas e maior teor de humificação (dado pela razão C/N). A segunda abordagem refere-se à associação dos elementos com diferentes componentes da matriz seguindo o procedimento de extração sequencial do BCR e extrações em etapa única para avaliar a mobilidade, sendo os extratos analisados por ICP-MS. O elemento Cr mostrou baixa mobilidade e bioacessibilidade. Cu está associado, principalmente, à fração orgânica da matriz, porém também pouco móvel. Fe e Pb também apresentaram baixa mobilidade e associados, principalmente, a óxidos da amostra. Mn e Zn mostraram alta mobilidade, sendo também associados a matéria orgânica e aos óxidos. A análise de especiação dos extratos obtidos foi realizada por SEC-ICP-MS, de modo a investigar a associação dos elementos extraídos com ácidos húmicos e fúlvicos. Nenhum sinal de Cr estava relacionado com a matéria orgânica, enquanto que os elementos Cu, Fe e Pb mostraram associação com ácidos húmicos. Mn apresentou espécies associadas a ácidos fúlvicos, enquanto que o Zn, não está associado a espécies orgânicas. / Fertilizers are frequently applied to soils due to actual global food demand and its future projections. Organic fertilizers have been extensively employed due to its price, as a reuse possibility to agricultural and urban wastes, and its sustainable character. They can be prepared from various sources, such as sewage sludge, manure and plants and animal scraps, submitted to composting process. In this work, it was developed a total elements determination method, as well as fractionating studies and speciation analysis of organic fertilizer. Thus, organic fertilizer samples were generally characterized using particle size fractionating, C and N content analysis, X-Ray diffraction and total elements determination. To the last, it was developed a sample preparation method by microwave-assisted digestion and ICP OES analysis. Digestion procedure was optimized using various acid mixtures, which were evaluated due to its relative errors related to sewage sludge CRM values, using PCA as a statistical tool. The chosen acid mixture constituted of 3 mL HNO3 + 1 mL HBF4 + 2 mL H2O was applied to samples digestion and their total elements determination. As total concentration is not enough to predict elements mobility and bioavailability, fractionation studies were conducted. The first approach was the particle size fractionation, were it was observed that the smaller the particle size the higher the micronutrients and contaminants concentration (Cr, Cu, Fe, Mn and Zn), along with lower C contents and higher N contents, indicating that these elements are associated with inorganic fractions, or with highly humified compounds (due to the lower C/N ratio). A second approach refers to elements association with various matrix components, using BCR and single-step extraction procedures to investigate elements mobility and bioavailability, with ICP-MS analysis of extracts. Cr was poorly mobile and bioavailable. Cu was bound to organic fraction, but also poorly mobile and bioavailable. Fe and Pb were also weakly mobile, and were mostly associated with oxides on matrix. Mn and Zn were greatly mobile and bioavailable, and were also mainly associated with oxides on matrix. Speciation analysis of extract was performed by SEC-ICP-MS, investigating elements association with humic and fulvic acids on previous extracts. Cr could not be associated with any humic substance, as expected with previous extractions results. Cu, Fe and Pb had identifiable species associated with humic acids, while Mn was associated with fulvic acids. Zn, even though high mobile, was not associated with any organic species.

A aplicação de fertilizantes aos solos é frequente devido à atual demanda mundial pela produção de alimentos e às projeções feitas para o futuro. Fertilizantes orgânicos têm sido uma opção amplamente explorada devido ao seu preço, possibilidade de reuso de resíduos agriculturais e urbanos, além do caráter sustentável. Podem ser provenientes de diversas origens como lodo de esgoto, estercos e restos de animais e vegetais submetidos a processos de compostagem. Neste trabalho, foi desenvolvido método para determinação elementar total em fertilizantes orgânicos, substratos e condicionadores de solo, e realizados estudos de fracionamento e análise de especiação em fertilizante orgânico. Assim, foi realizada a caracterização geral das amostras com fracionamento por tamanho de partícula, análises dos teores de C e N, difração de Raios-X e determinação elementar total. Para este último, foi desenvolvido método de digestão assistida por radiação micro-ondas, com análise por ICP OES. O procedimento foi otimizado para diferentes misturas ácidas, as quais foram avaliadas quanto aos erros relativos para diversos elementos em CRM de lodo de esgoto, utilizando PCA como ferramenta estatística. A mistura escolhida, constituída por 3 mL HNO3 + 1 mL HBF4 + 2 mL H2O, foi utilizada para digestão das amostras. Apenas a concentração total não traz informações a respeito da mobilidade e disponibilidade dos elementos, então estudos de fracionamento elementar também foram realizados. Na primeira abordagem foi executado fracionamento por tamanho de partícula, no qual foi observado que quanto menor o tamanho de partícula menor o teor de C e maior o teor de N, e maior a concentração de micronutrientes e contaminantes (Cr, Cu, Fe, Mn, Pb e Zn), indicando que estes elementos podem estar mais associados a frações com mais características inorgânicas e maior teor de humificação (dado pela razão C/N). A segunda abordagem refere-se à associação dos elementos com diferentes componentes da matriz seguindo o procedimento de extração sequencial do BCR e extrações em etapa única para avaliar a mobilidade, sendo os extratos analisados por ICP-MS. O elemento Cr mostrou baixa mobilidade e bioacessibilidade. Cu está associado, principalmente, à fração orgânica da matriz, porém também pouco móvel. Fe e Pb também apresentaram baixa mobilidade e associados, principalmente, a óxidos da amostra. Mn e Zn mostraram alta mobilidade, sendo também associados a matéria orgânica e aos óxidos. A análise de especiação dos extratos obtidos foi realizada por SEC-ICP-MS, de modo a investigar a associação dos elementos extraídos com ácidos húmicos e fúlvicos. Nenhum sinal de Cr estava relacionado com a matéria orgânica, enquanto que os elementos Cu, Fe e Pb mostraram associação com ácidos húmicos. Mn apresentou espécies associadas a ácidos fúlvicos, enquanto que o Zn, não está associado a espécies orgânicas. / Fertilizers are frequently applied to soils due to actual global food demand and its future projections. Organic fertilizers have been extensively employed due to its price, as a reuse possibility to agricultural and urban wastes, and its sustainable character. They can be prepared from various sources, such as sewage sludge, manure and plants and animal scraps, submitted to composting process. In this work, it was developed a total elements determination method, as well as fractionating studies and speciation analysis of organic fertilizer. Thus, organic fertilizer samples were generally characterized using particle size fractionating, C and N content analysis, X-Ray diffraction and total elements determination. To the last, it was developed a sample preparation method by microwave-assisted digestion and ICP OES analysis. Digestion procedure was optimized using various acid mixtures, which were evaluated due to its relative errors related to sewage sludge CRM values, using PCA as a statistical tool. The chosen acid mixture constituted of 3 mL HNO3 + 1 mL HBF4 + 2 mL H2O was applied to samples digestion and their total elements determination. As total concentration is not enough to predict elements mobility and bioavailability, fractionation studies were conducted. The first approach was the particle size fractionation, were it was observed that the smaller the particle size the higher the micronutrients and contaminants concentration (Cr, Cu, Fe, Mn and Zn), along with lower C contents and higher N contents, indicating that these elements are associated with inorganic fractions, or with highly humified compounds (due to the lower C/N ratio). A second approach refers to elements association with various matrix components, using BCR and single-step extraction procedures to investigate elements mobility and bioavailability, with ICP-MS analysis of extracts. Cr was poorly mobile and bioavailable. Cu was bound to organic fraction, but also poorly mobile and bioavailable. Fe and Pb were also weakly mobile, and were mostly associated with oxides on matrix. Mn and Zn were greatly mobile and bioavailable, and were also mainly associated with oxides on matrix. Speciation analysis of extract was performed by SEC-ICP-MS, investigating elements association with humic and fulvic acids on previous extracts. Cr could not be associated with any humic substance, as expected with previous extractions results. Cu, Fe and Pb had identifiable species associated with humic acids, while Mn was associated with fulvic acids. Zn, even though high mobile, was not associated with any organic species.

Military aircraft that require high maneuverability, durability, ballistic protection, reparability, and energy efficiency require structural alloys with low density, high toughness, and high strength. Also, repairs to these aircraft demand a production process that has the flexibility to be relatively in-situ with the same high-performance output. Materials produced by the cold spray process, a thermo-mechanical powder consolidation technique, meet many of the requirements. In accordance with President Obama’s 2011 Materials Genome Initiative, the focus of this effort is to design customized aluminum alloy powders which exploit the unique behavior and properties of the materials created by the cold spray process. Analytical and computational models are used to customize microchemistry, thermal conditioning, and solidification behavior of the powders by predicting equilibrium and non-equilibrium microstructure and resulting materials properties and performance. Thermodynamic, kinetic, and solidification models are used, including commercial software packages Thermo-Calc, Pandat™, and JMatPro®, and TC-PRISMA. Predicted powder properties can be used as input into a cold spray process impact model to determine the consolidated materials’ properties. Mechanical properties of powder particles are predicted as a function of powder particle diameter and are compared to experimental results.

In this thesis complexes of acylchalcogoureas with cadmium (II), lead (II) and nickel (II) have been synthesised and investigated as single source precursors for the formation of metal chalcogenide thin films viaaerosol assisted chemical vapour deposition (AACVD). Routes to binary thin films have been explored using homoleptic complexes of the general structure bis(N,N-diethyl-N'-naphthoylchalcogoureato)metal(II). Analysis of the thin films produced showed the successful deposition of the binary materials from the synthesised complexes when characterised by powder XRD, ICP-OES, SEM and EDX. Routes to ternary thin films with the general structure MExE'1-x, where M represents a metal (Cd, Ni and Pb); and E chalcogen (S or Se) have been investigated using heteroleptic metal complexes of cadmium, nickel or lead including different chalcogen containing N,N-diethyl-N'-naphthoylchalcogoureato ligands and diethyldithiocarbamate. The precursors were fully characterised and novel compounds had their crystal structures determined. The heteroleptic complexes were thermolysed by AACVD forming the MExE'1-x thin films. In the cases of lead, nickel and cadmium the thin films produced showed that the composition of the film tended heavily towards the metal selenide. Ternary films of type MS1-xSex was prepared by mixing their binary precursors of type bis(N,N-diethyl-N'-naphthoylselenoureato)metal(II) and bis(N,N-diethyl-N'-naphthoylthioureato)metal(II) [metal = Cd, Ni and Pb]. In the case of lead and cadmium chalcogenide films variation of the ratio of sulphur and selenium containing precursors allowed for the full transition in composition between metal sulphide and metal selenide. In the case of CdS1-xSexthe band gap of the films was determined from UV-visible spectroscopy to vary from 2.4 eV (CdS) to 1.7 eV(CdSe). In the case of NiS1-xSex the movement from sulphide to selenide was less simple with multiple phases of nickel chalcogenides produced.