Yes / Several contributions in answering granulation challenges including the use of computer simulation and well thought out experimental analyses are being researched. Using a twin screw granulator (TSG) by design of experiments (DoE), comparisons on 1) equipment similarities i.e., continuous and 2) shear forces, are made to previous literature on continuous equipment and a Cyclomix. This study proposes that equipment specific DoE, better explains the contribution of parameters than investigating an identified parameter from the experimental findings from a specific equipment. Granule strength and structure are presented together with the contribution of process parameters, speed, temperature, and binder content. Seeded structures are present in all but the Extrudomix. Longer residence times within the Cyclomix facilitates seeded structures. Granule crushing strengths are higher in TSG than all other continuous equipment. Optimum condition for the formation of stronger granules with least variation is around 65.4 °C. / The authors would like to acknowledge the support from the CCIP grant (Collaboration, Capacity and IP Development) fund from the University of Bradford for ordering cunsumables and equipment.

No description available.

Silicate melt inclusions (MI) are small samples of melt that are trapped during crystal growth at magmatic pressures and temperatures. The MI represent a sample of the melt that was isolated from the magma during host crystal growth. Thus, MI provide a valuable tool for constraining the magmatic history of igneous systems because they provide an unambiguous method to directly determine compositions of melts from which the host crystal grew. As such, coupled petrographic examination and geochemical analyses of MI and host crystals can reveal information about crystal/melt processes in igneous systems that are difficult (or impossible) to assess through conventional methods. Many studies have used MI to monitor large scale petrogenetic processes such as partial melting and fractional crystallization. The research presented below focuses on using MI to constrain processes that operate at the crystal/melt interface because MI are samples of melt that resided adjacent to the host crystal prior to entrapment as an inclusion. Chapter one addresses challenges associated with preparing small crystals containing MI for geochemical analysis. In chapter two trace element analyses of MI and the immediately adjacent host zircon crystals are used to determine zircon/melt partition coefficients. In chapter 3 the significance of boundary layer development adjacent to growing crystals is evaluated by comparing the trace element compositions of MI host crystals that have significantly different trace element mineral/melt partitioning behavior. / Ph. D.

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>

The reliance on freshwater released by mountain glaciers and ice caps demands that the effects of climate change on these thermally-sensitive systems are evaluated thoroughly. Coupling climate variability to processes of mass and energy exchange at the glacier scale is challenged, however, by a lack of climate data at an appropriately fine spatial resolution. The thesis addresses this challenge through attempting to reconcile this scale mismatch: glacier boundary-layer observations of meteorology and ablation at Vestari Hagafellsjökull, Iceland, and Storglaciären, Sweden, are related to synoptic-scale meteorological variability recorded in gridded, reanalysis data. Specific attention is directed toward synoptic controls on: i) near-surface air temperature lapse rates; ii) stationarity of temperature-index melt model parameters; and iii) glacier-surface ablation. A synoptic weather-typing procedure, which groups days of similar reanalysis meteorology into weather categories , forms the basis of the analytical approach adopted to achieve these aims. Lapse rates at Vestari Hagafellsjökull were found to be shallowest during weather categories characterised by warm, cloud-free weather that encouraged katabatic drainage; steep lapse rates were encountered in weather categories associated with strong synoptic winds. Quantitatively, 26% to 38% of the daily lapse-rate variability could be explained by weather-category and regression-based models utilizing the reanalysis data: a level of skill sufficient to effect appreciable improvements in the accuracy of air temperatures extrapolated vertically over Vestari Hagafellsjökull. Weather categories also highlighted the dynamic nature of the temperature-ablation relationship. Notably, the sensitivity of ablation to changes in air temperature was observed to be non-stationary between weather categories, highlighting vulnerabilities of temperature-index models. An innovative solution to this limitation is suggested: the relationship between temperature and ablation can be varied as a function of weather-category membership. This flexibility leads to an overall improvement in the simulation of daily ablation compared to traditional temperature-index formulations (up to a 14% improvement in the amount of variance explained), without the need for additional meteorological data recorded in-situ. It is concluded that weather categories are highly appropriate for evaluating synoptic controls on glacier meteorology and surface energetics; significant improvements in the parameterization of boundary-layer meteorology and ablation rates are realised through their application.

Décrypter les mécanismes et cinétiques de croissance et dissolution des minéraux dans les liquides silicatés est indispensable à la compréhension des processus magmatiques fondamentaux. La migration transcristalline des inclusions magmatiques sous l'effet d'un gradient thermique permet de quantifier une loi cinétique de croissance et dissolution du minéral hôte dans des conditions proches de celles qui prévalent le plus souvent dans la nature. L'objectif principal de ce travail de thèse était : i) d'étudier l'effet de la composition du liquide piégé sur le processus de migration dans l'olivine et ii) d'exploiter systématiquement le processus de migration afin de quantifier les lois cinétiques pour d'autres couples minéral-liquide. Lorsqu'elles sont soumises à un gradient thermique, les inclusions siliceuses (SiO2 ≥ 60pds%) piégées dans les olivines mantelliques et les inclusions basaltiques piégées dans les clinopyroxènes volcaniques migrent à travers leur hôte en direction du point chaud de la zone de travail. La migration s'effectue à une vitesse constante et, dans les olivines, sans modification de la composition du liquide piégé ; les inclusions des clinopyroxènes subissent en revanche une rééquilibration chimique transitoire en début de migration. Les cavités, subsphériques avant la migration, évoluent vers la forme en cristal-négatif du minéral hôte en cours d'expérience. L'achèvement de l'évolution morphologique nécessite un temps caractéristique gouverné par la diffusion chimique dans le liquide. La bulle de gaz exsolvé dans les inclusions n'est pas entraînée dans la migration. Elle se sépare du liquide magmatique et donne naissance à une inclusion fluide isolée au sein du cristal hôte. Les résultats expérimentaux indiquent que la migration procède par dissolution du minéral hôte à l'avant et recristallisation à l'arrière de l'inclusion. La vitesse de migration est limitée par les mécanismes à l'interface cristal-liquide, non par la diffusion chimique. Les taux de croissance et dissolution de l'olivine et du clinopyroxène que nous obtenons sont respectivement trente et quinze fois inférieurs à ceux déterminés dans une étude antérieure à partir d'expériences de migration d'inclusions basaltiques dans des olivines volcaniques. Ils obéissent cependant à la même forme de loi cinétique, qui peut être aisément transposée à des environnements de cristallisation ou de fusion naturels, similaires ou de plus faible déséquilibre. Le taux de croissance et dissolution de l'olivine lors des migrations n'a pas de lien simple avec la composition du liquide piégé ; il est peut-être aussi en grande partie contrôlé par la densité de dislocations du cristal hôte. Le phénomène de migration n'a pas été observé dans le quartz et le plagioclase pour les durées d'expériences réalisées. Il est néanmoins probable que l'absence de migration lors des expériences ne soit qu'apparente. Notamment, la prédominance de liaisons de forte énergie dans la structure du quartz et du plagioclase est susceptible de rendre les processus interfaciaux, et donc aussi la dissolution, particulièrement lente. Au cours de ce travail de thèse, l'opportunité s'est présentée d'étudier les inclusions magmatiques piégées dans les cristaux d'olivine de la pallasite Brahin. En particulier, deux familles d'inclusions ont été identifiées. La première consiste en des plans d'inclusions secondaires contenant de nombreuses chromites et des assemblages à métal-sulfure et olivine phosphorée ; la seconde correspond à des inclusions isolées renfermant pour la plupart de la stanfieldite, une bulle de gaz et de l'olivine phosphorée. Les inclusions secondaires se seraient formées suite à un choc ayant eu lieu alors que l'assemblage minéralogique actuel de Brahin était déjà formé, ou en cours de formation. En revanche, les inclusions de stanfieldite témoigneraient d'un choc prépallasitique. / Deciphering the mechanisms and kinetics of crystal growth and dissolution in silicate melts is essential for understanding the fundamental magmatic processes. When remelted and subjected to an imposed thermal gradient, melt inclusions migrate through their host, which provides a direct access to the host crystal growth / dissolution kinetics and allows to quantify the kinetic laws at very low undercoolings or overheatings, i.e. in conditions appropriate to many natural systems. The main goal of the present study was: i) to study the effect of the trapped melt composition on the migration process in olivine and ii) to extend the transcrystalline melt migration approach to quantify the kinetic law for other mineral-melt pairs. When subjected to a thermal gradient, Si-rich melt inclusions (SiO2 ≥ 60 wt%) in mantle olivines and basaltic melt inclusions in volcanic clinopyroxenes migrate through their host toward the host spot of the working zone. Migration proceeds at a constant rate and in olivine, without modification of the trapped melt composition ; melt inclusions in clinopyroxene, however, undergo a transient chemical reequilibration while they begin to migrate. While moving, the melt inclusions gradually change from subspherical to a faceted, negative-crystal shape. Completion ofthe morphological evolution requires a characteristic time that is governed by chemical diffusion. When a gas bubble is initially present, it responds to elastic forces by quickly shifting toward the cold end of the inclusion, where it soon becomes engulfed as an isolated fluid inclusion in the reprecipitated crystal. The experimental results indicate that the migration operates by progressive dissolution and recrystallistion of the host, governed by interface kinetics with no interference of chemical diffusion.The growth / dissolution rates we obtained for olivine and clinopyroxene are respectively thirty and fifteen times lower than those determined in a previous study from melt migration experiments on basaltic inclusions in volcanic olivines. Nevertheless, they obey the same form of kinetic law, which can be transposed to equally or more sluggish melting or crystallisation events in nature. Dependence of the growth / dissolution rate of olivine on trapped melt composition is not straightforward ; rates may be largely controlled by the density of dislocations in the host crystal. The melt migration phenomenon was not observed in quartz and plagioclase for the investigated experiment durations. Nonetheless, the lack of migration during experiments may only be apparent. Notably, the dominance of high-strength bonds in the quartz and plagioclase structure may render interfacial reactions, and so dissolution, particularly slow. During this research work, we had the opportunity to study the melt inclusions trapped in olivine crystals from the Brahin pallasite. In particular, two contrasted sets of melt inclusions were evidenced. The first set consists of plans of secondary inclusions containing abundant chromite and assemblies of metal, sulfide, and phosphoran olivine ; the second set corresponds to isolated inclusions consisting for the most part of stanfieldite, a gas bubble, and phosphoran olivine. Secondary inclusions may have formed during a shock event that took place while the current stony-iron assembly of the Brahin pallasite was already formed, or was created by this shock. However, stanfieldite inclusions may originate from a pre-pallasitic shock event.

Les alliages conducteurs à haute tenue mécanique sont utilisés dans de nombreux domaines tels que le transport, l’énergie et l’industrie électronique. La demande en ces matériaux est croissante. Les alliages Cu-Be constituent à l’heure actuelle les matériaux conducteurs les plus résistants mais posent un problème de toxicité et de coût. Pour proposer une alternative à ces derniers, nous avons étudié des alliages Cu-Mg hypo-eutectiques. Deux voies de synthèse ont été utilisées afin d’obtenir des composites endogènes possédant une combinaison originale de propriétés structurelles et fonctionnelles : le refroidissement conventionnel et la solidification rapide par melt-spinning. Les microstructures obtenues ont en commun la présence d’agrégats eutectiques et diffèrent principalement par la dimension des paramètres métallurgiques tels que la taille de grains et la distance interlamellaire. Les systèmes présentent des forces motrices de transformation de phases importantes conduisant à une précipitation au cours d’un maintien thermique. L’investigation des propriétés mécaniques et électriques des alliages Cu-Mg montre que ces dernières égalent celles des alliages Cu-Be. En complément de l’approche expérimentale, nous avons adapté deux modèles : un modèle thermocinétique pour décrire l’évolution temporelle de la microstructure qui a lieu à haute température et un modèle mécanique permettant de rationaliser l'influence des paramètres microstructuraux sur les propriétés mécaniques et électriques. / Copper-based high strength conductive alloys are used in a myriad of applications such as transport, energy and electronic industries. The demand for these materials is booming. The strongest conductive alloy is based on the Cu-Be system which has the disadvantage of toxicity and cost. In an attempt to find an alternative to these, we have developed hypoeutectic Cu-Mg alloys. Two synthesis routes were applied to produce endogenous compounds with a unique combination of structural and functional properties: the conventional cooling and the rapid solidification by melt-spinning. The obtained microstructures share the presence of eutectic aggregates and differ mainly by the size of the metallurgical parameters such as grain size and interlamellar distance. The two systems provide high driving forces for phase transformations leading to precipitation during aging. The investigation of the mechanical and electrical properties of Cu-Mg alloys shows that they are equal to those of the Cu-Be alloys. In addition to experimental approach, we have adapted two models: a thermo-kinetic one to describe time evolution of the microstructure which takes place at high temperature and a mechanical one to rationalize the influence of microstructural parameters on mechanical and electrical properties.

Předmětem této diplomové práce je vytvoření databáze známých sekvenčních a melt typů patogenních bakterií a nástroje pro správu databáze. Metoda popisovaná v této práci je poměrně nová technika typizace patogenních bakterií založena na překladu sekvenčních typů na příslušející melt typ a využívá k tomu převodní klíč, který byl vytvořen ve spolupráci s Centrem molekulární biologie a genové terapie Interní hematologické a onkologické kliniky Fakultní nemocnice Brno. Obsahem práce je vytvoření prostoru na databázovém serveru, načtení potřebných dat, aplikace převodního klíče, vytvoření GUI, vytvoření dalších vhodných ošetření a rozšíření, testování a následná analýza výsledků. V první kapitole jsou diskutovány nejznámější metody bakteriální typizace, další kapitola je pak věnována server-client aplikacím a databázovým nástrojům. Třetí kapitola popisuje implementaci databáze na server a čtvrtá kapitola stručně shrnuje všechny funkce programu. V poslední kapitole je pak popsána analýza vylepšení převodního klíče, které získalo pracovní název půlené alely.

Melting and melt segregation are key processes in the geochemical evolution of the Earth. However, mechanism and time scale of melt transport from the source to the surface are still not well understood and are dependent on the grain-scale distribution of melt. A related question is the retention of melt in partially molten regions of the Earths upper mantle. Seismic observations from mid-ocean ridges (MOR) and subduction zones are interpreted to show in-situ melt contents up to 3%, while geochemical observations from MOR basalts are inferred to indicate very efficient extraction of melt (porosities of order 0.1%). Earlier theoretical models of the melt distribution were based on the balance of surface tension between melt and uniform crystalline grains, predicting a simple net- work of melt along three-grain edges. Analyses of experimentally produced samples of olivine and basaltic melt show that the melt geometry is much more complex, and includes wetted two-grain boundaries. I reconstructed the melt geometry of two experimentally produced samples by serial sectioning and 3-D rendering of the pore geometry which demonstrates for the first time that melt exists in thin layers on two-grain boundaries. This confirms the inferences from previous 2-D observations and has significant implications for physical properties of partially molten regions, for example seismic velocities and attenuation. The wetted two-grain boundaries are inferred to be a consequence of continuous grain growth. Due to the complexity of the 3-D melt geometry the perme- ability of partially molten rocks can not be predicted from simple models. I therefore investigated the permeability as a function of porosity for both synthetic and ex- perimentally determined pore geometries using a lattice-Boltzmann method. The calculated permeability is not a simple function of porosity, but increases rapidly at a critical fraction of wetted two-grain boundaries. In order to extrapolate the experimentally based findings to grain sizes expected in natural rocks I examined the geometry of secondary phases inferred to represent relict melt in mantle peridotites from the Krivaja massif in Bosnia. These findings corroborate the experimental observations of wetted two-grain boundaries.

High shear melt granulation (HSMG) is an established technology for a production of densified granules. In this project, it was used as a novel solvent-free method for the preparation of cocrystals. Cocrystals produced by HSMG were compared to those prepared by Hot Melt Extrusion (HME) to investigate the influence of variable parameters and conditions on the process of cocrystal conversion. The potential for the active control of cocrystals polymorphism utilising the intrinsic properties of lipids was also investigated in this project. Different cocrystal pairs were prepared by both cocrystallisation methods using glycol derivative polymers. Thermal analysis, powder X-ray diffraction and Raman spectroscopy were used as analytical techniques to determine the cocrystal yield and purity. The results obtained from HSMG suggest that sufficient binder concentrations (above 12.5% w/w) in a molten state and continuous shearing force are necessary to achieve a complete cocrystals conversion. Further increase in binder concentration (15% w/w) was found to provide more regular shape and smooth surface to the prepared spherical granules. Cocrystals preparation by HME was achievable after introducing a mixing zone to the extruder configuration (Conf B and Conf C) providing densified extrudates containing pure cocrystals. In conclusion, HSMG was found as a versatile technique for the preparation of pure pharmaceutical cocrystals embedded in polymer matrix within a spherical shape granule of smooth surfaces, providing additional desirable characteristics. Intensive surface interaction, enhanced by sufficient mixing under optimal parameters, was found as a key influencing factor in cocrystallisation. Cocrystals polymorphism was actively controlled by employing the intrinsic properties of polymers and lipids.