With the progress of high alloy steelmaking processes, it is essential to minimize the loss of valuable metals, like chromium and vanadium during the decarburization process, from both economic as well as environmental view points. One unique technique to realize this aim, used in the present work, is the decarburization of high alloy steel grades using oxygen with CO2 in order to reduce the partial pressure of oxygen. In the present work, the investigation on the oxidation of iron-chromium and iron-vanadium molten alloys under CO2-O2 mixtures was carried out and presented in this dissertation. For oxidation study on Fe-Cr molten alloy with CO2-O2 mixtures, on the basis of thermodynamic analysis, energy balance calculation and modeling results, experimental validation in laboratory was carried out, and later on, the oxidation kinetics of Fe-Cr and Fe-Cr-C melts under controlled partial pressure of oxygen was investigated. Thermodynamics calculation and energy balance estimation demonstrated that, it is possible to use CO2 or CO2-O2 mixtures as decarburizers during EAF process and high initial carbon contents in the steel can be adopted at the beginning in order to reduce the cost. A generic model has been developed to describe the overall process kinetics prevailing in metallurgical reactors containing liquid metal and gas bubbles. This model is general and can be extended further to consider any gas liquid reactions in any chemical engineering reactor, and especially the metallurgical ones, like AOD. In the present dissertation, the model is applied in predicting the evolution of Cr and C contents in a Fe-C-Cr melt during injection of different O2-CO2 mixtures. The related simulation results illustrated that CO2 is efficient in Cr retention. In order to verify the modeling results, 1kg induction furnace experiments were carried out in the present laboratory. The results indicated that the predictions of the model are in good agreement with the experimental results. Meanwhile, the experimental results indicated that the Cr-losses can be significantly lowered by replacing the oxygen with CO2 in the injected gas, specifically for Fe-Cr-C melts with carbon levels higher than about 0.8 mass%. Subsequently, the oxidation kinetics of Fe-Cr and Fe-Cr-C melts was investigated under different CO2-O2 mixtures. It is indicated that, the oxidation rate is controlled by the chemical reaction at the initial stage and the reaction rate can be expressed as  at the Cr range of 11-21 mass% in the Fe-Cr melt. For oxidation study on Fe-V liquid alloy, the investigation of the oxidation kinetics was carried out under CO2-O2 mixtures, which is followed by the study on thermodynamic properties of vanadium containing slags. During oxidation of Fe-V melt, in the case of alloys with vanadium contents exceeding 10 mass%, there exists an incubation period before the chemical reactions prevail the process. In addition, the ‘incubation time’ increased with the increase of temperature and the vanadium content, whereas it decreased with the increase of oxygen partial pressure in the oxidant gas. High-temperature mass spectrometric method was used to determine the activity of the vanadium oxide in CaO-MgO-Al2O3-SiO2-V2O3 slags, whereas, the oxidation states of vanadium in the CaO-MgO-Al2O3-SiO2-VOxslag system was studied by XANES method. The results indicated that, higher basicities stabilize higher vanadium oxidation state, whereas, higher temperature stabilizes lower vanadium oxidation state. The present work, which was carried out within the ECO-STEELMAKING project funded by MISTRA via Jernkontoret is expected to lead to implementation of some modifications in high alloy steel production based on fundamental concepts towards more environment-friendly steel processing. / <p>QC20100628</p>

Cette étude s’inscrit dans le cadre du stockage de l’hydrogène pour des applications mobiles de faibles puissances électriques. Elle a été réalisée dans le cadre du projet FUI HyCAN. L’objectif était la formulation et la fonctionnalisation d’un alliage métallique de structure cubique corps centrée. Ces solutions solides désordonnées sont à base de vanadium qui présente initialement une bonne réactivité vis-à-vis de l’hydrogène.Cependant la thermodynamique du système V-H ne permet pas une utilisation pour des températures inférieures à 40°C, son coût est prohibitif et sa mise en oeuvre en milieu industriel nécessite quelques précautions. Nous avons travaillé sur trois grandes familles d’alliages à base de vanadium. Les alliages de Ti-V-Cr ont été étudiés au rayonnement synchrotron par diffraction X in operando dans le but de comprendre les transformations structurales observables lors de l’hydruration et de les relier à la thermodynamique des composés. Dans unsecond temps, le cahier des charges du projet nous a orienté vers des composites à base de vanadium dans lesquels nous développons une structure intergranulaire permettant une meilleure activation et une déstabilisation contrôlée de l’hydrure pour atteindre des températures de fonctionnement proche de 0°C.L’utilisation du ferro-vanadium en tant que précurseur a motivé l’étude des alliages de type Ti-V-Fe et Ti-V-Fe-Cr. La viabilité des solutions de stockage sur la base de ces matériaux est discutée. Tout au long de ces travaux la relation microstructure/propriété de sorption de l’hydrogène est systématiquement discutée et des modèles empiriques décrivant l’équilibre de l’hydrure sont systématiquement confrontés à la base bibliographique.Enfin, une partie de l’étude est consacrée à l’étude et à la modélisation des réservoirs en condition de fonctionnement, d’un point de vue de la thermique, du respect des normes de sécurité et des contraintes mécaniques générées par le lit de poudre réactif. / This study has been carried out in the framework of solid state hydrogen storage for mobile applications withlow electrical power. It was conducted under the FUI project HyCAN. The objective was to develop andfunctionalize a bcc alloy. Such disordered solid solutions are based on vanadium, which initially has a goodreactivity in relation to hydrogen. However, the thermodynamics of V-H system does not allow applicationsbelow 40 ° C, the cost is prohibitive and its implementation in industrial environments is not straightforward.We worked on three major families of vanadium alloys. Alloys Ti-V-Cr have been studied by in operandosynchrotron radiation X-ray diffraction in order to understand the observable structural transformations that takeplace during hydrogenation and then to link them to the thermodynamics of compounds. In a second step, thespecifications of the project directed us towards vanadium composites in which we develop an intergranularstructure for a better controlled activation and destabilization of the hydride so as to reach operatingtemperatures near 0 ° C. The use of ferro-vanadium as a precursor prompted the study of alloys in the Ti-V-Feand Ti-V-Cr-Fe systems. The viability of storage solutions on the basis of these materials is discussed.Throughout the course of this work the relationship between microstructure and hydrogen sorption properties issystematically discussed and empirical models describing the hydride equilibrium are routinely faced with thebibliographic database.Finally, part of the study is devoted to the study and modeling of reservoirs in operating condition, from thepoint of view of heat exchange, compliance with safety standards and mechanical stresses generated by the bedreactive powder.

Physical systems having dimensions smaller than, or of the same order of magnitude as, the characteristic length scale relevant to a physical property are referred to as mesoscopic physical systems. Due to the dimensions of the system, several physical properties get affected and this could reveal interesting physics which would other-wise have not been apparent. In the recent times, a lot interesting applications have resulted from such studies. The fundamental length scale in ferromagnetic systems is the exchange length. It is related to the magnetic anisotropy and exchange constants. Other length scales such as the size of a magnetic domain or a domain wall depends on the minimisation of energy associated with this length scale along with other factors such as zeeman energy, magnetostatic, magnetoelastic and anisotropy energies. Ultrathin magnetic films have thickness smaller than the exchange length. In this thickness regime, the surface of the film plays an important role. The magnetic anisotropy energy would get a significant contribution from the surface of the film and if it dominates over the volume contribution, would eventually lead to magnetisation pointing out of the plane of the film as opposed to imposition of demagnetising fields. Examples for such cases are FePt(L10 phase) films and Co(0001) films. Such films are important in memory applications where perpendicularly magnetised recording media are desired. When the lateral dimensions of thin films are reduced, demagnetising fields become even more important. Depending on the anisotropy in the system, certain domain patterns get stabilised in the final structure. This has led to important applications in the field of magnonics. The use of angular momentum transfer from spin polarised electrons to change the configuration of magnetisation of structured magnetic films has led to interesting memory and oscillator applications. The underlying physical parameter that needs to be controlled and carefully studied in all these cases is the magnetic anisotropy. It is favourable to have uniaxial magnetic anisotropy for memory and oscillators. This thesis chiefly deals with Fe/GaAs(001) systems. The choice of the physical system follows interest in spintronics where spin injection is desired into a semiconductor from a ferromagnet. The thesis is organized into chapters as follows. Chapter 1 attempts to introduce the reader to some of the basic concepts of mag-netism and some magnetic phenomena. The characteristic nature of a ferro-magnetic material is its spontaneous magnetisation due to long range ordering below the Curie temperature. But the moment is coupled, through some in-teractions, to spatial co-ordinates which leads to spatial variation of magnetic properties. Such interactions are also responsible for the formation of magnetic domains. The spatial variation of magnetic properties within a ferromagnet is called magnetic anisotropy. A major part of the thesis deals with the study of magnetic anisotropy of Fe thin films grown on GaAs(001) substrates. For a better understanding, the structure of the semiconductor is introduced first before discussing the influence of the structure of GaAs on the growth of Fe. A short description of the uniaxial magnetic anisotropy in Fe films is given before starting on an exploration of some possible reasons for it. Concepts of ferromagnetic resonance, spin torque effect and micromagnetic simulations are given. Chapter 2 gives a brief description of some of the experimental apparatus that was setup during the course of the research along with an overview of the differ-ent sample preparation and characterisation techniques used. The chapter is organised according to the general functionality of the techniques. Some con-cepts such as the use of low energy electrons, nanostructuring etc are introduced along with the corresponding techniques since it is best understood along with the instrumentation. Chapter 3 reports some surprising findings about the in-plane magnetic anisotropy in Fe films grown on an MgO underlayer. Until now, it has been understood that such films should exhibit only a four-fold magnetic anisotropy within the plane of the film. But the Fe/MgO/GaAs(001) films studied here exhibited an in-plane uniaxial magnetic anisotropy(IPUMA). IPUMA is dominant upto about 25 ML of Fe in case of Fe/MgO/GaAs(001) films whereas, in Fe/GaAs(001) films it is dominant only upto about 15 ML. Thus, the presence of the MgO film even appeared to enhance the uniaxial anisotropy as compared to the Fe/GaAs(001) films. In the ferromagnetic resonance (FMR) spectra, as many as three peaks were observed in Fe/GaAs(001) films of thickness 50 ML close to the hard axis of magnetisation. This means that three could be three energy minima possibly due to a competition between the anisotropies involved. Chapter 4 elaborates the investigations of the effect of orientation and doping con-centration of the GaAs substrate on the magnetic anisotropy of Fe/GaAs(001) films. It is found that doping the substrate (n type) reduces the strength of the IPUMA in Fe/GaAs films. In the wake of the long-standing debate of electronic structure v/s stress as the origin of the IPUMA in Ferromagnet/Semiconductor films, this result is important because it implies that the electronic structure of the Fe/GaAs interface influences the magnetic anisotropy. But stress, as a cause of IPUMA cannot be ruled out. The influence of deposition techniques on magnetic anisotropy is also investigated. Chapter 5 presents a way of manipulating magnetic anisotropy, and hence mag-netisation dynamics, by nanostructuring of epitaxial Fe films. It is based on the property that magnetic anisotropy of Fe films is thickness dependent. It is demonstrated that using techniques of nanostructuring, a 2 dimensional mag-netic system with controllable variation of local magnetic anisotropy is created. Such a system could be a potential magnonic crystal. chapter 6 demonstrates the proof of concept of a new memory device where memory is stored in the magnetic domain configuration of a ring in relation to that of a nano-wire. Switching between the memory states is acheived through spin trasfer torque of an electric current passing through the device, whereas read-out of the memory state is through the measurement of resistance of the device. Devices are made using NiFe and Co; it is seen that the behaviour of the devices can be explained taking into account the anisotropic magnetoresistance of the material used. Finally, the various results are summarised and a broad outlook is given. Some possible future research related to the topics dealt within this thesis is discussed.

No description available.

Oxyborate minerals can represent the most important sink for boron in silica-undersaturated mineralised systems such as those of the Långban-type. Yet, their distribution, characteristics and parageneses are still not completely known. In order to test the hypothesis that the chemical compositions of oxyborates are essentially reflecting their local environments, the present study was set up. Additional observations regarding their assemblages, textures and structure would allow for a broader understanding of their formation and paragenetic interrelationships. A representative selection of Mg-(Fe-Mn) oxyborates and associated minerals have been characterised using optical microscopy, field emission electron probe microanalysis (FE-EPMA) with wavelength dispersive spectroscopy (WDS), and Raman spectroscopy. The studied samples are from a suite of carbonate-hosted Fe-Mn oxide deposits in the western part of the Palaeoproterozoic Bergslagen ore province, in south central Sweden and include the minerals blatterite [(Mn2+,Mg)35(Mn3+,Fe3+)9Sb5+3(BO3)16O32], fredrikssonite [Mg2(Mn3+,Fe3+)BO5], chemically variable ludwigites [c. (Mg,Fe2+)2Fe3+BO5], orthopinakiolite [(Mg,Mn2+)2Mn3+BO5] and pinakiolite [(Mg,Mn2+)2(Mn3+,Sb5+)BO5]. The results show a correlation between the cation distribution in the oxyborates fredrikssonite, ludwigite, orthopinakiolite as well as pinakiolite, and their associated metal oxides consisting of hausmannite and spinel group minerals. This combined with the textural relationships of the phases suggests that the bulk contents of magnesium, manganese and iron in the oxyborates were sequestered from these pre-existing metal oxides. The chemically broad range of hausmannite and spinel group minerals associated with specifically fredrikssonite and ludwigite agrees with their more frequent general occurrence, compared to orthopinakiolite and pinakiolite. Raman spectroscopy verified the structural character of the studied oxyborates and indicates a potential connection between the presence of manganese and whether local BO33- ions are allowed to be positioned in symmetry sites which result in a split E´ mode. The results from this study contribute to the understanding of this family of minerals and their potential diversity in mineralised systems, and form a fundamental prerequisite for their potential application for boron isotope studies. / Mineral är kemiska föreningar eller rena grundämnen som har en väldefinierad kemisk sammansättning, ordnad kristallstruktur och är bildade av geologiska processer. Oxyborater är en typ av sådana föreningar vilka innehåller grundämnena bor och syre samt olika kombinationer av metalliska grundämnen. Oxyboratmineral kan bland annat bildas i och omkring malmfyndigheter där grundämnet kisel är ovanligt eller icke förekommande, och kan utgöra de viktigaste borföreningarna i vissa sådana miljöer. Genom att bättre förstå denna typ av mineral och de kemiska och bildningsmässiga samband som finns mellan dem och andra föreningar kan vi få en större kunskap om hur de bildas, samt hur olika grundämnen kan omfördelas i sådana geologiska system. I denna studie har ett representativt urval av oxyborater undersökts med hjälp av mikroskopi och mikrokemiska samt spektroskopiska metoder för att testa huruvida deras kemiska sammansättning är direkt kopplad till den lokala miljön. De studerade proven kommer från karbonatbundna mineraliseringar i den västra delen av malmprovinsen Bergslagen i södra Mellansverige. De mineral som undersökts närmre är oxyboraterna blatterit, fredrikssonit, ludwigit, ortopinakiolit och pinakiolit. Resultaten visar på direkta kemiska samband mellan uppträdandet av fredrikssonit, ludwigit, ortopinakiolit samt pinakiolit, och de lokalt bergartsbildande mineral som de samexisterar med. Den breda kemiska fördelningen hos de metall- och syreföreningar som finns i samma omgivning som fredrikssonit och ludwigit förklarar också varför dessa två oxyborater generellt är mera vanligt förekommande än ortopinakiolit och pinakiolit. De spektroskopiska analyserna verifierar den tidigare klassificeringen av de studerade oxyboraterna samt visar på ett möjligt samband mellan innehållet av metallen mangan, samt hur grundämnet bor förekommer i deras kristallstruktur. Resultaten från denna studie bidrar med en kombination av nya kemiska, paragenetiska och spektroskopiska data samt ökar förståelsen av dessa värdmineral för grundämnet bor i malmfyndigheter med låg eller ingen kiselhalt. Resultaten ger även en insikt i hur den kemiska sammansättningen potentiellt kan påverka kristallstrukturen hos dessa oxyborater.

Theoretische Berechnungen sagen für tetragonal gedehntes Fe-Co eine hohe magnetokristalline Anisotropie voraus, wie sie für seltenerdfreie Dauermagnetwerkstoffe vorteilhaft wäre. In dieser experimentellen Arbeit werden epitaktische Fe-Co-Schichten strukturell und magnetisch charakterisiert. Zur Untersuchung der Dehnung in diesen Schichten eignen sich AuxCu100-x-Pufferschichten besonders, da über die Stöchiometrie (x) deren lateraler Gitterparameter eingestellt werden kann. Wird Fe-Co auf einer solchen Pufferschicht abgeschieden, erfolgt aufgrund dessen hoher elastischer Energie schon in den ersten Monolagen eine vollständige Relaxation der pufferinduzierten Dehnung. In ternären Fe-Co-X-Schichten, in denen kleine X-Atome (X = B, C oder N) Oktaederlücken besetzen, wird jedoch eine spontane tetragonale Dehnung c/a bis zu 1,05 beobachtet. Entlang der gedehnten c-Achse tritt eine uniaxiale magnetokristalline Anisotropie auf, die für B- oder C-Zulegierungen von 2 at% eine maximale Anisotropiekonstante von 0,4 MJ/m³ zeigt. Wird der X-Gehalt weiter erhöht, nehmen die Kristallinität der Schichten und die magnetische Anisotropie ab. Neben der magnetokristallinen Anisotropie des Schichtvolumens wird an den Fe-Co(-X)-Schichten eine hohe Grenzflächenanisotropie beobachtet. Der Beitrag der freien Oberfläche übersteigt den der Au-Cu-Grenzfläche dabei deutlich. / Theoretical calculations predict a high magnetocrystalline anisotropy for tetragonally strained Fe-Co, which would be beneficial for rare-earth free permanent magnet materials. In this experimental work, epitaxial Fe-Co films are investigated structurally and magnetically. AuxCu100-x buffer layers are very suitable to study the strain in these films since their in-plane lattice parameter can be tailored via the applied stoichiometry (x). However, when Fe-Co is deposited on such a buffer layer, the induced strain of the Fe-Co lattice relaxes completely within the first monolayers, due to its high elastic energy. In ternary Fe-Co-X films, where small atoms X like B, C or N occupy octahedral interstitial sites, a spontaneous strain c/a up to 1.05 is observed. A uniaxial magnetocrystalline anisotropy along the strained c axis appears. Their maximum anisotropy constant is 0.4 MJ/m³ for B or C contents of 2 at%. If the X content is further increased, the crystallinity and thus, the magnetic anisotropy of the films degrade. Together with the magnetocrystalline anisotropy of the films’ volumes, a high interface anisotropy is observed for the Fe-Co(-X) films. The contribution of the free surface clearly exceeds the contribution of the Au-Cu interface.

No description available.

ELEMENTAL AND ISOTOPIC STUDY OF DIFFERENTIATED METEORITES AND IMPLICATIONS FOR THE ORIGIN AND EVOLUTION OF THEIR PARENT BODIES Iron meteorites are differentiated meteorites composed largely of Fe-Ni alloys. The metallic phase of many iron meteorites shows a texture called the Widmanstätten pattern, which develops as a two-phase intergrowth of kamacite (α-bcc, ferrite) and taenite (γ-fcc, austenite), and forms by nucleation and growth of kamacite from taenite during slow cooling of the parent body. Selected iron meteorites - octahedrites of different structural and chemical groups (Canyon Diablo, Toluca, Bohumilitz, Horh Uul, Alt Biela, Nelson County, Gibeon and Joe Wright Mountain) were studied with intention to evaluate the scale and extent of Fe isotopic heterogeneities in iron meteorites and to find the possible link between the isotopic variations and thermal histories of the respective meteorite parent bodies. The Fe isotopic compositions of kamacite and taenite in the studied meteorites, obtained by three independent analytical techniques with different spatial resolution capabilities (laser ablation and solution MC ICP-MS and SIMS) show significant variations of up to ~4.5‰ in δ56 Fe. The taenite is isotopically heavier compared to kamacite in all studied meteorites. There is no correlation...

L’obtention de nanoparticules d’or nécessite le contrôle de nombreux paramètres et la compréhension du mode d’interaction entre l’or et le support. Pour cela, le choix du support est très important. Le premier volet de la thèse concerne la préparation contrôlée des catalyseurs à base d’or supporté sur les oxydes mésoporeux réductibles TiO₂, CeO₂ et Fe₂O₃ synthétisés via deux stratégies Soft et hard template en utilisant respectivement comme agents structurants le tribloc copolymère (Pluronic 123) et la silice mésoporeuse SBA-15. Les différentes techniques de caractérisation mettent bien en évidence que le taux de dépôt de l’or dépend de la concentration initiale de HAuCl₄, de la méthode de préparation (DPU, DP NaOH), de la teneur en or visée et de la nature du support ; Ces résultats sont à relier à la spéciation des espèces or en solution en fonction du pH final de la solution. Les taux de dépôt de l’or sont plus importants sur CeO₂ et ceci quelle que soit la teneur en or visée dans ce travail. Une dispersion très élevée est obtenue (la taille moyenne des particules d’or est de 2nm) sur les catalyseurs à 1% et 2%Au/CeO₂ préparés par la méthode DPU et calcinés à 400°C. Le deuxième volet de cette étude concerne l’oxydation en phase gaz d’une molécule organique modèle le toluène et l’oxydation en phase liquide d’une molécule organique modèle le phénol par des réactions de type Fenton et photo Fenton. Dans l’oxydation du toluène en phase gazeuse, les catalyseurs à base d’or supportés sur oxydes mésoporeux sont totalement sélectifs en CO₂ et H₂O. Les performances catalytiques dépendent des conditions de synthèse des catalyseurs et de la nature de l’oxyde utilisé ; le catalyseur 1%Au/CeO₂ est très actif et très stable au cours de quatre cycles successifs et au cours du temps. L’oxydation en phase liquide d’une molécule organique modèle le phénol par des réactions de type Fenton et photo Fenton a été effectuée sur les catalyseurs FeSBA-15 synthétisés via différentes stratégies : introduction du fer par voie postsynthétique et par voie hydrothermale en milieu faiblement et fortement acide respectivement à pH=6 et pH=3. Les performances catalytiques dépendent du rapport Si/Fe et de la taille des particules des espèces de fer, la taille des particules étant directement liée à la stratégie de synthèse des catalyseurs. Le catalyseur FeSBA-15(Si/Fe=60) synthétisé à pH=6 est un candidat potentiel dans la dégradation de polluants organiques par procédé Fenton et photo-Fenton en milieu neutre. / Well dispersed gold nanoparticles are the key to obtain an active gold catalyst. Obtaining gold nanoparticles requires control of many parameters and understanding of the interaction mode between gold and the support. For this reason the choice of the support is very important. The first part of this thesis concerns the controlled preparation of gold catalysts supported on reducible mesoporous oxides TiO₂, CeO₂ and Fe₂O₃ synthesized via two strategies Soft and Hard template using respectively. triblock copolymer (Pluronic 123) and mesoporous silica SBA-15 as template. This study clearly shows that the gold loading depends on the initial concentration of HAuCl₄, the method of preparation (DPU DP NaOH), theoretical gold content and the nature of the support. These results are to relate to the gold speciation which is a function of pH of the solution. The gold loading is higher on CeO₂ than on TiO₂ and Fe₂O₃ whatever the theoretical gold content. Very high gold dispersion is obtained (the gold particle size is 2 nm) on 1wt% and 2wt% Au/CeO₂ prepared by DPU and calcined at 400°C. The second part of this study concerns the toluene oxidation in the gas phase on Au/mesoporous oxide catalysts and the Fenton and photo-Fenton degradation of phenolic aqueous solutions by H₂O₂ on FeSBA-15 catalysts prepared following different synthesis routes, direct synthesis by adjusting pH at 3 and 6 and with post synthesis procedure. In the toluene oxidation in the gas phase Au/mesoporous oxide catalysts are totally selective for CO₂ and H₂O. The catalytic performances depend on the synthesis conditions of catalysts and the support; the 1wt% Au/CeO₂ catalyst is very active and exhibits a long-term stability. In the Fenton and photo-Fenton degradation of phenolic aqueous solutions the catalytic performances depend on the Si/Fe ratio and the particle size of the iron species, the particle size being directly related to the synthesis strategy of the catalysts. The catalyst FeSBA-15 (Si/Fe = 60) synthesized at pH = 6 is a potential candidate in the degradation of organic pollutants by Fenton and photo-Fenton process in neutral medium. / م لخصمسقني لمعلا يف هذه ةحورطألا ىلإ نيئزج:OiT 2ب وا سطة OeC 2و , Fe2O ي خ تص الاول ال ق سم ب تح ض يرمح فزات من ال ذهبن وع من م يزوب ري ة ب مواد مدعم 3ان واع مخ ت لف ال تح ض ير. ت شخ يص ف ي ال م س ت عم لة ال ت ق ن يات مخ ت لفت ب ين ال مح ضرة ل مح فزات انال دعم ط ب ي عة ك ذا و ال مح فز ت ح ض ير وطري قة HAuCl ت ر سب معدل ي ت ع لق ل ذه با ت رك يز ع لى 4ي ع ضو جزيء و سطغازي enèuloT أك سدة ف ي ال مواد هذه ب تط ب يق ي ت ع لق ال ثان ي ال ق سم ف يال مح فز ت ح ض ير Ò طرق ك ذا و ل ت فاعل هذا ع لى ال مؤث رة ل عوامل ب درا سة ق م نا سال فا ال مذك ورة ل لمح فزات ال ف عال ية ع لان واع مخ ت لف ب وا سطة FeSBA- ي ع ضو جزيء lonehP ت فاعل ب وا سطة notneF سائ ل و سط ف ي وعمن 51 ن مح فزات ع لىوHp ال و سط Si/Fe قلعتي ةبسنب FeSBA- ريضحتلا.ادأء 1515FeSBA-15, Fenton, Phenol, Toluène, TiO و 2 CeO2, Fe2O3, SBA- ال ك لمات ال م ف تاح ية ׃م يزوب وري ة ,

Esse trabalho teve como objetivo verificar o efeito da adição do ácido oléico na moagem de alta velocidade/energia na obtenção de pós magnéticos em escala nanométricas da liga Pr12Fe65,9Co16B6Nb0,1. A primeira etapa deste trabalho, envolveu a obtenção de pós magnéticos por meio do processo de hidrogenação, desproporção, dessorção e recombinação (HDDR), utilizando a pressão de H2 de 930 mbar (hidrogenação e desproporção) e temperatura de dessorção e recombinação de 840 ºC. Inicialmente, os pós HDDR foram submetidos à moagem de alta velocidade/energia a 900 rpm, com variação do volume do meio de moagem (ciclohexano) sem adição de ácido oleico. Em seguida, os pós HDDR foram submetidos à moagem com adição de ácido oleico, variando o tempo de moagem. Após a moagem, foi realizado tratamento térmico dos pós a 700 ºC ou 800 ºC durante 30 min., com a finalidade de cristalização do pó. Foi verificado que, a utilização de 6,6 ml de ciclohexano como meio de moagem e com adição de ácido oleico há uma melhora na eficiência da moagem dos pós. Para adições de surfactante, de 0,02 a 0,05 ml e tempos de moagem até 360 minutos, não ocorre a aglomeração dos pós magnéticos no pote de moagem, obtendo acima de 90% de eficiência na moagem. A segunda etapa deste trabalho envolveu a caracterização dos pós magnéticos: utilizando magnetômetro de amostra vibrante, microscopia eletrônica de Varredura, microscopia eletrônica de transmissão e difração de raios-X. Os resultados obtidos mostraram que a adição de ácido oléico na moagem de alta velocidade/energia proporciona uma melhora nas propriedades magnéticas. Com a variação do tempo de moagem a fase Fe-&alpha; presente no pó HDDR apresenta diminuição no tamanho do cristalito (de 35 para ~ 10 nm) enquanto que, na fase Pr2Fe14B verifica-se menor grau de cristalinidade. / This work verified the effect caused by adding the surfactant in the high speed/energy milling in order to obtain Pr12Fe65.9Co16B6Nb0.1 magnetic nanopowders. The first part of this work involved the magnetic powder obtainment through the process of hydrogenation, disproportionation, desorption and recombination (HDDR). The pressure of H2 during the hydrogenation and disproportion steps was 930 mbar and the temperature of desorption and recombination was 840 ºC. Initially, the HDDR powders were subjected a highspeed milling process at 900 rpm, with quantity variations of the milling medium (cyclohexane) and without the addition of oleic acid. Then, the HDDR powders were subjected to the milling process with the addition of oleic acid and with milling time variations. After the milling process, heat treatments of the powder were carried out at 700 °C or 800 °C for 30 minutes in order to obtain the crystallization of the powder. By performing the procedures, it was verified that the milling efficiency improved with the addition of 6.6 ml of cyclohexane as the milling medium and with the addition of oleic acid. It was determined that for the surfactant additions of 0.02 ml to 0.05 ml, with a milling time of up to 360 minutes, powder agglomeration does not occur in the milling pot and the milling efficiency is higher than 90%. The second stage of this work involved the magnetic powders characterization obtained by using vibrating sample magnetometer, scanning electron microscopy, transmission electron microscopy and X-ray diffraction. Through the characterizations it was found that the powders magnetic properties improved when the addition of oleic acid in a high-speed /energy milling occurred. It was also verified that the &alpha;-Fe phase, present in the powder, shows a crystallite size decrease (from 35 nm to ~ 10 nm) when the time milling variation occurred; meanwhile, the crystallinity degree was lower in the Pr2Fe14B phase when the time milling variations was carried out.