Volatiles are a fundamental component of the Magmatic-Hydrothermal model of platinum group element (PGE) ore deposition for PGE deposits in layered mafic intrusions such as Bushveld and Stillwater. Volatiles have the potential to complex with PGEs in silicate melts and hydrothermal fluids, increasing PGE solubility; in order to assess the models of PGE ore deposition reliable estimates on the solubilities in the various magmatic phases must be known. However, experimental studies on the solubility and partitioning behaviour of PGEs in mafic magmatic-hydrothermal systems under relevant conditions are sparse, and the data that do exist produce conflicting results and new or adapted experimental methods must be applied to investigate these systems. Experimental results are presented here, investigating the effect of volatiles (i.e. H2O, Cl and CO2) on Pt and Ir solubility in a haplobasaltic melt and fluid-melt partitioning of Pt between an aqueous fluid and a haplobasaltic melt under magmatic conditions using a sealed-capsule technique. Also included are the details of the development of a novel experimental technique to observe fluid-melt partitioning in mafic systems and application of the method to the fluid-melt partition of Pt. Solubility experiments were conducted to assess the effect of volatiles on Pt and Ir solubility in a haplobasaltic melt of dry diopside-anorthite eutectic composition at 1523K and 0.2GPa. Synthetic glass powder of an anhydrous, 1-atm eutectic, diopside-anorthite (An42-Di58) haplobasalt composition was sealed in a platinum or platinum-iridium alloy capsule and was allowed to equilibrate with the noble metal capsule and a source of volatiles (i.e. H2O, H2O-Cl or H2O-CO2) at experimental conditions. All experiments were run in an internally-heated pressure vessel equipped with a rapid quench device, with oxygen fugacity controlled by the water activity and intrinsic hydrogen fugacity of the autoclave (MnO-Mn3O4). The resultant crystal- and bubble-free run product glasses were analyzed using a combination of laser ablation ICP-MS and bulk solution isotope-dilution ICP-MS to determine equilibrium solubilities of Pt and Ir and investigate the formation and contribution of micronuggets to overall bulk determined concentrations. In water-bearing experiments, it was determined that water content did not have an intrinsic effect on Pt or Ir solubility for water contents between 0.9 wt. % and 4.4 wt. % (saturation). Water content controlled the oxygen fugacity of the experiment and the resulting variations in oxygen fugacity, and the corresponding solubilities of Pt and Ir, indicate that over geologically relevant conditions both Pt and Ir are dissolved primarily in the 2+ valence state. Pt data suggest minor influence of Pt4+ at higher oxygen fugacities; however, there is no evidence of higher valence states for Ir. The ability of the sealed capsule technique to produce micronugget-free run product glasses in water-only experiments, allowed the solubility of Pt to be determined in hydrous haplobasalt at lower oxygen fugacities (and concentrations) then was previously observed. Pt and Ir solubility can be represented as a function of oxygen fugacity (bars) by the following equations: [Pt](ppb)= 1389(fO-sub-2)+7531(fO-sub-2)^(1/2) [Ir](ppb)=17140(fO-sub-2)^(1/2) In Cl-bearing experiments, experimental products from short run duration (<96hrs) experiments contained numerous micronuggets, preventing accurate determination of platinum and iridium solubility. Longer run duration experiments showed decreasing amounts of micronuggets, allowing accurate determination of solubility; results indicate that under the conditions studied chlorine has no discernable effect on Pt solubility in the silicate melt from 0.6 to 2.75 wt. % Cl (saturation). Over the same conditions, a systematic increase in Ir solubility is found with increasing Cl content; however, the observed increase is within the analytical variation/error and is therefore not conclusive. If there is an effect of Cl on PGE solubility the effect is minor resulting in increased Ir solubilities of 60% at chlorine saturation. However, the abundance of micronuggets in short run duration experiments, which decreases in abundance with time and increases with Cl-content, offers compelling evidence that Cl-bearing fluids have the capacity to transport significant amounts of Pt and Ir under magmatic conditions. It is suggested that platinum and iridium dissolved within the Cl-bearing fluid are left behind as the fluid dissolves into the melt during the heating stages of the experiment, leaving small amounts of Pt and Ir along the former particle boundaries. With increasing run duration, the metal migrates back to the capsule walls decreasing the amount of micronuggets contained within the glass. Estimates based on this model, using mass-balance calculations on the excess amount of Pt and Ir in the run product glasses (i.e. above equilibrium solubility) in short duration experiments, indicate estimated Pt and Ir concentrations in the Cl-bearing fluid ranging from tens to a few hundred ppm, versus ppb levels in the melt. Respective apparent (equilibrium has not been established) partition coefficients (D,fluid-melt) of 1x10^3 to 4x10^3 and 300-1100 were determined for Pt and Ir in Cl-bearing fluids; suggesting that Cl-bearing fluids can be highly efficient at enriching and transporting PGE in mafic magmatic-hydrothermal ore-forming systems. Platinum solubility was also determined as a function of CO2 content in a hydrous haplobasalt at controlled oxygen fugacity. Using the same sealed capsule techniques and melt composition as for H2O and Cl, a hydrous haplobasaltic melt was allowed to equilibrate with the platinum capsule and a CO2-source (CaCO3 or silver oxalate) at 1523 K and 0.2 GPa. Experiments were conducted with a water content of approximately 1 wt. %, fixing the log oxygen fugacity (bars) between -5.3 and -6.1 (log NNO = -6.95 @ 1573 K and 0.2 GPa). Carbon dioxide contents in the run product glasses ranged from 800-2500 ppm; and over these conditions, CO2 was found to have a negligible effect on Pt solubility in the silicate melt. Analogous to the Cl-bearing experiments, bulk concentrations of Pt in CO2-bearing experiments increased with increasing CO2 content due to micronugget formation. Apparent Pt concentrations in the H2O-CO2 fluid phase, prior to fluid dissolution, were calculated to be 1.6 to 42 ppm, resulting in apparent partition coefficients(D,fluid-melt) of 1.5 x 10^2 to 4.2 x 10^3, increasing with increasing mol CO2:H2O up to approximately 0.15, after which increasing CO2 content does not further increase partitioning. As well, a novel technique was developed and applied to assess the partitioning of Pt between an aqueous fluid and a hydrous diopside-anorthite melt under magmatic conditions. Building upon the sealed-capsule technique utilized for solubility studies, a method was developed by adding a seed crystal to the capsule along with a silicate melt and fluid. By generating conditions favourable to crystal growth, and growing the crystal from the fluid, it is possible to entrap fluid inclusions in the growing crystal, allowing direct sampling of the fluid phase at the conditions of the experiment. Using a diopside seed crystal with the diopside-anorthite eutectic melt, it was possible to control diopside crystallization by controlling the temperature, thus allowing control of the crystallization and fluid inclusion entrapment conditions. Subsequent laser ablation ICP-MS analysis of the fluid inclusions allowed fluid–melt partition coefficients of Pt to be determined. Synthetic glass powder of an anhydrous, 1-atm eutectic, diopside-anorthite (An42¬Di58) haplobasalt composition (with ppm levels of Ba, Cs, Sr and Rb added as internal standards), water and a diopside seed crystal were sealed in a platinum capsule and were allowed to equilibrate at experimental conditions. Water was added in amounts to maintain a free fluid phase throughout the experiment, and the diopside crystal was separated from the melt. All experiments were run in an internally heated pressure vessel equipped with a rapid-quench device, with oxygen fugacity controlled by the water activity and intrinsic hydrogen fugacity of the autoclave (MnO-Mn3O4). Experiments were allowed to equilibrate (6-48 hrs) at experimental conditions (i.e. 1498K, 0.2 GPa, fluid+melt+diopside stable) before temperature was dropped (i.e. to 1483K) to induce crystallization. Crystals were allowed to grow for a period of 18-61 hours, prior to rapid isobaric quenching to 293K at the conclusion of the experiment. Experimental run products were a crystal- and bubble-free glass and the diopside seed crystal with a fluid-inclusion-bearing overgrowth. Analysis of fluid inclusions provides initial solubility estimates of Pt in a H2O fluid phase at 1488 K and 0.2 GPa at or near ppm levels and fluid melt partition coefficients ranging from 2 – 48. This indicates substantial metal enrichment in the fluid phase in the absence of major ligands such as carbonate or chlorine. The results of this study indicate that the volatiles studied (i.e. H2O, CO2, and Cl) do not have a significant effect on Pt and Ir solubility in a haplobasaltic melt at magmatic conditions. These results suggest that complexing of Pt and Ir by OH, Cl, and carbonate species in a haplobasaltic melt is insignificant and the presence of these volatiles will not result in significantly increased PGE contents over their dry counterparts, as has been suggested. Preliminary evidence of minor Cl-complexing of Ir is presented; however, resulting in only a slight increase (<100%) in Ir solubility at Cl-saturation. Significant partitioning of Pt and Ir into a fluid phase at magmatic conditions has been demonstrated; with estimates of fluid-haplobasaltic melt partition coefficients increasing from 1x10^1 for pure water to up to an apparent 4x10^3 with the addition of Cl or CO2 to the system. This result indicates complexing of Pt and Ir with OH< HxCOy≤ Cl. Using these estimates, Cl- or CO2-bearing magmatic fluids can be highly efficient at enriching and transporting platinum group elements (PGEs) in mafic magmatic-hydrothermal ore-forming systems.

Asymmetric hydrogenation has emerged as a versatile methodology to obtain a wide range of chiral precursors. This thesis focused on the synthesis of new chiral ligands and the expansion of the substrate scope of asymmetric hydrogenations. Paper I described the synthesis and evaluation of N,P-ligands for the Ir-catalyzed hydrogenations of unfunctionalized olefins. The substrate scope of Ir-catalyzed asymmetric hydrogenations is limited to a narrow range of “test” olefins. The foremost focus of this thesis was to expand the substrate scope of Ir-catalyzed asymmetric hydrogenations. Papers II and III disclosed the potential of the N,P-ligated Ir complexes in hydrogenation of the enol phosphinates. This substrate class is attractive because the hydrogenated products are chiral alkylphosphinates that can be transformed into chiral alcohols and chiral phosphines without sacrificing enantiopurity. A wide range of enol phosphinates were hydrogenated to excellent conversions and enatioselectivities. The hydrogenation of purely alkyl-substituted enol phosphinates in very high conversions and ee values was emphasized in these studies. Paper IV described the investigation of unfunctionalized enamines as substrates in Ir-catalyzed hydrogenation studies. The hydrogenation results and structural limitations of the substrates are presented. Paper V described the asymmetric hydrogenation of diphenylvinylphosphine oxides, di- and trisubstituted vinyl phosphonates. The hydrogenation of diphenylvinylphosphine oxides gives direct access to protected chiral phosphines. The hydrogenated products of vinylphosphonates are highly synthetically useful in pharmaceutical and material chemistry. Hydrogenation of E/Z mixtures of carboxyethyl vinylphosphonates with perfect enantioselectivities was striking in these studies. In paper VI, we have reported the development of a new, highly enantioselective synthetic route to building blocks with CF3 at the chiral center. Several functionalized and unfunctionalized CF3-substituted olefins were hydrogenated with varied degree of success. This methedilogy is useful in the formation of chiral fluorine-containing molecules for a wide range of applications. Paper VII described the hydrogenation of imines using the phosphine-free Cp*Ru/diamine complexes. Chiral version of this reaction was also examined. Despite the modest results, this is the first study to use phosphine-free Cp*Ru/diamine complexes as catalysts for the reduction of C=N double bonds.

No description available.

No description available.

La physique mésoscopique est actuellement dominée par des mesures de transport permettant d'extraire les propriétés électroniques globales des systèmes étudiés. La spectroscopie tunnel permet d'avoir un accès direct à la densité d'états locale (LDOS). Nous pouvons donc sonder les évolutions spatiale des propriétés électroniques notamment à l'interface entre 2 matériaux possédant des propriétés différentes. Au cours de cette thèse, nous avons développé un microscope à sonde locale qui combine microscopie à force atomique (AFM) et microscopie à effet tunnel (STM) et qui fonctionne à 100mK. L'AFM permet de localiser un nanocircuit unique sur un substrat isolant grâce à un Length Extension Resonator (LER). Nous pouvons ensuite mesurer la spectroscopie tunnel locale du nanocircuit conducteur. La résolution énergétique obtenue avec ce système est de 70µeV. Nous avons montré la faisabilité expérimentale d'une telle étude en mesurant l'effet de proximité sur un îlot de cuivre (métal normal) connecté par deux électrodes supraconductrices en aluminium à l'équilibre, hors-équilibre et sous champ magnétique. Nous avons également mesuré la LDOS du graphène sur Ir(111) qui présente des propriétés proches du graphène intrinsèque avec un dopage de type p de l'ordre de 0.34eV. Nous avons observé que ce dopage fluctue spatialement avec la présence de poches de charges avec une taille typique de l'ordre de 9nm. Ces observations sont similaires à des résultats déjà reportés sur des systèmes graphène sur SiO2. Cependant, le profil des poches que nous avons mesuré montre une forte corrélation avec la topographie due à une modulation du potentiel électrostatique induit par le métal sous le graphène. Une analyse plus fine a permis également de réveler la présence d'interférences de quasiparticules se traduisant par une inhomogénéité de la DOS. La taille typique des structures est de l'ordre de la longueur d'onde de Fermi avec une dépendance linéaire avec l'énergie selon E=ħvFk avec vF = 8.3±0.7x10^5m/s proche de la vitesse de Fermi théorique de 1x10^6m/s. Cela met évidence la présence de diffusion intravallée et prouve le caractère de fermions de Dirac sans masse des particules du graphène sur Ir(111).

Cette thèse vise à maitriser la synthèse MPCVD de films hétéroépitaxiés de diamant de haute qualité cristalline sur substrat d'iridium pour la réalisation de dosimètres en radiothérapie. Cet objectif nous a conduits à élaborer la couche d'iridium épitaxiée sur des substrats SrtiO3 (001). Un bâti sous vide équipé d'un canon à électrons a donc été développé et calibré. Les couches obtenues ont été caractérisées par DRX et présentent une qualité structurale équivalente à l'état de l'art. Le procédé de nucléation (BEN) - MPCVD induit sur la surface de l'iridium des " domaines " spécifiques à la nucléation du diamant sur iridium. Un travail important a été mené sur l'optimisation du (BEN) - MPCVD de façon à obtenir un procédé fiable et reproductible pour obtenir des " domaines " homogènes sur une surface de 5x5mm2 d'Ir/SrtiO3. Des études de caractérisation de surface (MEB, XPS, AES) des " domaines " nous ont permis de dresser leur carte d'identité chimique et morphologique. Nous démontrons ainsi qu'ils contiennent des nuclei de diamant. De plus, la propagation de ces " domaines " semble suivre des directions préférentielles [110] induites par l'épitaxie de l'iridium au cours du temps durant l'étape de (BEN)-MPCVD. A partir de ces résultats, des films de diamant hétéroépitaxiés autosupportés de 100&#956-m ont été élaborés. La corrélation entre la qualité cristalline du diamant hétéroépitaxié et sa réponse en détection a été menée avec l'équipe dosimétrie du LCD. Des inhomogénéités de la structure cristalline due à la présence de défauts structuraux ont été mises en évidence. Afin d'étudier localement ces échantillons, une campagne de mesure par microfaisceau X a été réalisée sur la ligne Diffabs du Synchrotron Soleil. L'assemblage des différentes connaissances acquises lors de cette thèse a permis de fabriquer et de caractériser un premier détecteur à base de diamant hétéroépitaxié au LCD

Nos últimos anos, complexos de irídio tem sido sugeridos para uso em materiais luminescentes, tais como diodos orgânicos emissores de luz (OLED\'s) e células eletroquímicas emissoras de luz (LEEC\'s). Suas potenciais utilidades como dispositivo é devido as suas características físico-químicas e fotofísicas, as quais são caracterizadas por tempos de vida curtos para o tripleto, estabilidade térmica, além da possibilidade de modificar a emissão sobre uma vasta gama de cores do espectro. Atualmente, muitas pesquisas tentam encontrar complexos de irídio com emissão de luz azul. No entanto, embora emissores de luz azul já tenham sido desenvolvidos, existe o problema relacionado a agregação destes complexos. Para resolver este o problema da agregação é necessário modificar a estrutura padrão do complexo com cadeias carbônicas saturadas para evitar empilhamento &pi;-&pi;. Experimentalmente esta é uma tarefa um tanto difícil. Dessa forma, métodos computacionais têm sido viáveis como uma abordagem para entender a estrutura e propriedades eletrônicas dos sistemas estudados. Aqui, é apresentado um estudo teórico baseado na teoria do funcional da densidade (DFT) para investigar a agregação de complexos de irídio, além de predizer como esta pode ser controlada com o uso de grupos substituintes adequados. Os cálculos foram realizados usando funcional PBE0 e conjunto de base 6-31G*, o qual provou ser adequada na descrição das propriedades do complexo. Portanto, cálculos subsequentes mostraram bons resultados, onde os estados excitados foram previstos ser de natureza predominantemente MLCT (transferência de carga do metal para o ligante) para o complexo 1 e LC (carga centrada no ligante) para o complexo 2. Alterações no ambiente químico provou ter grande influência sobre os estados excitados, onde a inclusão do solvente favoreceu a estabilidade, mantendo os estados excitados tripletos com energia entre 3.01 eV e 3.03 eV. Além disso, o uso dos grupos substituintes provou ser de grande importância para prevenir a agregação, especialmente no complexo 2, em que a partir do dímero matriz (sem substituintes) para o complexo substituído 2-1 (com metil) houve uma desestabilização da energia de interação entre os monômeros no dímero por ~ 19.78 kcal/mol, sendo que a energia do primeiro foi estimada ser -39.78 kcal/mol, enquanto o segundo foi -20 kcal/mol. Nossos resultados sugerem que a modificação do complexo torna-se bastante promissora, fazendo uso de pequenos grupos substituintes e cadeias carbônicas alifáticas, evitando assim, a agregação por empilhamento &pi;-&pi;. / In the last few years, iridium complexes have been suggested for use in luminescent materials such as organic light-emitting diodes (OLEDs) and light emitting electrochemical cells (LEECs)1-3. Their potential utility as luminescent devices is due to the physicochemical and photophysical properties, which are featured by short triplet emitting lifetimes (microseconds time scale), thermal stability, besides of possibility to tune the emission over desired spectral range. Actually, many researches try to find iridium complexes with efficient deep-blue emission, in order to use in these devices. Although many deep-blue emitters have been developed, there is still a big problem related to aggregation. So far, little has been reported about iridium complexes in solid environments, such as inorganic matrix of OLEDs and LEECs devices. To solve this issue is needed tune the structure of the complex in order to prevent the aggregation (steric hindrance), by means of drawing saturated carbon chains on the ligands to avoid the &pi;-&pi; stacking. Experimentally, this is a rather challenging and expensive task. In this aspect, computational methods have been performed as approaches to gain deeper insights about the structure and electronic properties of the studied systems. Here, we present a theoretical study based on density functional theory to investigate the aggregation iridium complexes, in addition to predict how this can be controlled with the use of suitable substituent groups. Calculations were performed using functional PBE0 and 6-31G* basis functions, which proved adequate in describing the properties of the complex. Therefore, subsequent calculations showed good results, where the excited state of the complex are provided, these being predominantly MLCT (metal to ligand charge transfer) nature for the complex 1 and LC (ligand centered) nature to complex 2. Changes in the chemical environment proved to have great influence on the excited states, where the inclusion of the solvent favored its stability, keeping the triplet excited states with energy between 3.01 and 3.03 eV. Furthermore, the use of substituent groups proved to be of great importance to prevent aggregation, especially in complex 2, wherein from the matrix dimer (no substituted) to complex with methyl groups there was a destabilization of the interaction energy between the monomers in the dimer by ~ 19.78 kcal / mol, being that the energy of the first was -39.78 kcal / mol, while the second was to -20 kcal / mol. Our results suggest that the modification of the complex becomes quite promising, making use of small groups and aliphatic carbon chains, thus avoiding aggregation by stacking.

Made available in DSpace on 2014-10-09T12:51:57Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:07:25Z (GMT). No. of bitstreams: 0 / Tese (Doutoramento) / IPEN/T / Instituto de Pesquisas Energeticas e Nucleares - IPEN-CNEN/SP

Made available in DSpace on 2014-10-09T12:51:57Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:07:25Z (GMT). No. of bitstreams: 0 / Neste trabalho foram estudados os níveis excitados do 193Ir produzidos a partir do decaimento &beta; do 193Os (T1/2 ~ 30h). Para a obtenção das amostras radioativas, ~ 5mg de Ósmio metálico (99% enriquecido em 192Os) foram irradiados no reator IEA-R1, sob um fluxo de nêutrons da ordem de 1012cm2 s1 e depois analisadas, empregando-se a técnica de espectroscopia &gamma; simples (unidimensional) com espectrômetro &gamma; de alta resolução, bem como as técnicas de espectroscopia de coincidência &gamma;&gamma; e de correlação angular direcional &gamma;&gamma; (&theta;) usando um sistema de aquisição multiparamétrica composto por 4 detectores HPGe. A partir destes dados, foi possível adicionar 28 transições a este esquema de decaimento, 11 das quais já eram conhecidas de outros estudos envolvendo reações nucleares, além de 17 observadas pela primeira vez. Também foram acrescentados 8 níveis excitados ao esquema de decaimento, sendo 3 conhecidos por outras reações e 5 completamente novos. Além disso, foi possível confirmar a suspeita encontrada na literatura de que os níveis a 848,93keV e 849,093keV são o mesmo, além de confirmar a existência de um nível excitado a 806,9keV. A análise de correlação angular direcional permitiu a definição do spin de do nível excitado a 874kev (5/2+), além de propor uma probabilidade de 79% do nível a 1078keV ter spin 5/2, e de restringir as possibilidades de spin para o nível novo a 960keV para duas (1/2 ou 3/2). Também foi possível determinar a razão de mistura multipolar (&delta;Ln+1/Ln) para 43 transições, sendo 19 pela primeira vez e praticamente todas as restantes com precisão melhor que a encontrada na literatura. Finalmente, foi feita uma tentativa de compreender o núcleo através de um modelo teórico, o qual reproduziu muito bem o estado fundamental e os dois primeiros estados excitados do 193Ir. / Tese (Doutoramento) / IPEN/T / Instituto de Pesquisas Energeticas e Nucleares - IPEN-CNEN/SP

A extratibilidade de sais de fosfônio foi aproveitada para elaborar método de separação Ir-Rh, mediante a extração do sal de trifenil n-propil fosfônio do cloro-complexo de Ir(IV,) em clorofórmio. O coeficiente de extração de 99,2%, permite retirar o irídio do meio aquoso com grande eficiência. O irídio assim separado é determinado diretamente, por via espectrofotométrica, em 494 m&#181;, em faixa de concentração de 5,0 a 50,0 &#181;g/ml. Pd(II), Pt(IV) e Os(IV) interferem e são eliminados previamente, assim como Au(III). Os ânions interferentes, I-, Br- e SCN- são também eliminados previamente. Muitos íons podem estar presentes, tais como Co(II),Cu(II), Mn(II), Fe(III), Ni(II), As(V), Sb(V), NO3-, ClO4- e SO4--. Após a separação do Ir (IV), o Rh(III) que permanece, na solução é complexado com íons azoteto e extraído em clorofórmio depois de precipitado com íons trifenil n-propil fosfônio, sendo o coeficiente de extração de 98,3%. A determinação ê também feita no próprio solvente, mediante medida espectrofotométrica em 404-408 m&#181;, para um intervalo de concentração de . 10,0 a 70,0 &#181;g/ml. Uma separação envolvendo Os(IV), Pd(II)e Pt(IV) foi elaborada, eliminando-se Pd(II) e Pt(IV) por extração de ambos em metil n-butil cetona a partir de uma solução contendo SCN-. O Os(IV) é determinado na solução aquosa na forma de OsC16-- por medida espectrofotométrica em 370 m&#181;, válida para a faixa de concentração de 2,0 a 20,0 &#181;g/m1. / Abstract not available.