A fundamental theoretical and experimental study on calcium sulphate scale formation in hydrometallurgical solutions containing various minerals was conducted. A new database for the Mixed Solvent Electrolyte (MSE) model of the OLI Systems® software was developed through fitting of existing literature data such as mean activity, heat capacity and solubility data in simple binary and ternary systems. Moreover, a number of experiments were conducted to investigate the chemistry of calcium sulphate hydrates in laterite pressure acid leach (PAL) solutions, containing Al2(SO4)3, MgSO4, NiSO4, H2SO4, and NaCl at 25–250ºC. The database developed, utilized by the MSE model, was shown to accurately predict the solubilities of all calcium sulphate hydrates (and hence, predict scaling potential) in various multicomponent hydrometallurgical solutions including neutralized zinc sulphate leach solutions, nickel sulphate–chloride solutions of the Voisey’s Bay plant, and laterite PAL solutions over a wide temperature range (25–250°C). The stability regions of CaSO4 hydrates (gypsum, hemihydrate and anhydrite) depend on solution conditions, i.e., temperature, pH and concentration of ions present. The transformation between CaSO4 hydrates is one of the common causes of scale formation. A systematic study was carried out to investigate the effect of various parameters including temperature, acidity, seeding, and presence of sulphate/chloride salts on the transformation kinetics. Based on the results obtained, a mechanism for the gypsum–anhydrite transformation below 100°C was proposed. A number of solutions for mitigating calcium sulphate scaling problems throughout the processing circuits were recommended: (1) operating autoclaves under slightly more acidic conditions (~0.3–0.5 M acid); (2) mixing recycled process solutions with seawater; and (3) mixing the recycling stream with carbonate compounds to reject calcium as calcium carbonate. Furthermore, aging process solutions, saturated with gypsum, with anhydrite seeds at moderate temperatures (~80°C) would decrease the calcium content, provided that the solution is slightly acidic.

A fundamental theoretical and experimental study on calcium sulphate scale formation in hydrometallurgical solutions containing various minerals was conducted. A new database for the Mixed Solvent Electrolyte (MSE) model of the OLI Systems® software was developed through fitting of existing literature data such as mean activity, heat capacity and solubility data in simple binary and ternary systems. Moreover, a number of experiments were conducted to investigate the chemistry of calcium sulphate hydrates in laterite pressure acid leach (PAL) solutions, containing Al2(SO4)3, MgSO4, NiSO4, H2SO4, and NaCl at 25–250ºC. The database developed, utilized by the MSE model, was shown to accurately predict the solubilities of all calcium sulphate hydrates (and hence, predict scaling potential) in various multicomponent hydrometallurgical solutions including neutralized zinc sulphate leach solutions, nickel sulphate–chloride solutions of the Voisey’s Bay plant, and laterite PAL solutions over a wide temperature range (25–250°C). The stability regions of CaSO4 hydrates (gypsum, hemihydrate and anhydrite) depend on solution conditions, i.e., temperature, pH and concentration of ions present. The transformation between CaSO4 hydrates is one of the common causes of scale formation. A systematic study was carried out to investigate the effect of various parameters including temperature, acidity, seeding, and presence of sulphate/chloride salts on the transformation kinetics. Based on the results obtained, a mechanism for the gypsum–anhydrite transformation below 100°C was proposed. A number of solutions for mitigating calcium sulphate scaling problems throughout the processing circuits were recommended: (1) operating autoclaves under slightly more acidic conditions (~0.3–0.5 M acid); (2) mixing recycled process solutions with seawater; and (3) mixing the recycling stream with carbonate compounds to reject calcium as calcium carbonate. Furthermore, aging process solutions, saturated with gypsum, with anhydrite seeds at moderate temperatures (~80°C) would decrease the calcium content, provided that the solution is slightly acidic.

Les sismologues ont révélé l'existence d'une anisotropie sismique complexe dans la graine terrestre. Cette thèse, en deux parties, présente deux approches différentes pour, d'une part, expliquer l'existence de cette anisotropie avec des modèles de graine numérique et, d'autre part, étudier l'effet des transformations de phase sur cette anisotropie.Dans un premier temps, nous avons construit un outil de simulation de la propagation des rais sismiques à travers une graine numérique, afin d'étudier la possibilité de reproduire numériquement les données sismologiques et de contraindre la dynamique et la minéralogie de la graine. Nous concluons qu'aucune structure du fer cubique ne permet de développer une anisotropie sismique significative. Seule la structure hexagonale compacte permet de le faire. Parmi les modèles géodynamiques quadripolaires étudiés, la croissance équatoriale préférentielle est le processus dynamique qui présente le meilleur accord avec les observations de dépendance à la profondeur et d'anisotropie polaire. L'ajout d'une stratification chimique permet d'amplifier d'environ 40% l'anisotropie globale mais augmente la dispersion des résidus sismiques, ce qui n'est pas conforme aux observations de dépendance à la profondeur. Enfin, une croissance dendritique (texture de solidification) est peu compatible avec une anisotropie principale Nord-Sud. Il apparaît clairement qu'aucun de ces modèles géodynamiques ne permet d'obtenir une amplitude d'anisotropie suffisante en utilisant les propriétés élastiques publiées pour le fer dans la graine. A l'issue de ce travail, de nombreux autres processus dynamiques restent encore à étudier, tels que les forces de Lorentz et la translation-convection thermique, processus bipolaire qui présente un fort intérêt pour la caractérisation de la composante hémisphérique de l'anisotropie sismique.Dans un deuxième temps, nous avons procédé à des expériences de transition de phase α-ε (fer cubique centré vers fer hexagonal compact) dans le fer pur. Nous avons simulé les textures résultantes à l'aide du mécanisme de Burgers. Nous avons confronté nos simulations aux résultats expérimentaux. Nous avons pu confirmer la validité du mécanisme de transformation de Burgers. Nous avons trouvé une forte sélection de variant sous l'effet de la contrainte non-hydrostatique dans le sens direct α→ε, produisant de fortes textures. Dans le sens inverse ε→α, on observe des textures finales très faibles, voire aléatoires. Appliqués avec prudence au cas de la graine terrestre, nos résultats indiquent que la transformation de phase du fer hexagonal à cubique ne peut pas expliquer la forte anisotropie observée. Nous avons aussi noté une mémoire de texture partielle, déjà documentée pour d'autres métaux de transition. Enfin, nous avons procédé à des tests préliminaires en cellule diamant en rotation. Les résultats de ces expériences de cisaillement ont également montré un très bon accord avec les simulations fondées sur le mécanisme de Burgers. En revanche, nous avons pu constater de grands écarts entre nos résultats expérimentaux et les simulations en cisaillement présentées dans la littérature [Levitas et al., 2010], notamment en termes de gradient de contraintes. / Seismologists revealed the existence of a complex seismic anisotropy in the Earth's inner core. In this thesis we took two different approaches in order to characterize the anisotropy: in a first part, we tried to explain this anisotropy using formation models of inner core and, in a second part, we considered the impact of eventual phase transitions on anisotropy.Firstly, we simulate the propagation of seismic rays through a numerically grown inner core, in order to measure the seismic anisotropy to compare with actual observations and to constrain the dynamics and mineralogy of the inner core. We conclude that no cubic structure of iron may produce a significant global anisotropy. Only the hexagonal compact phase of iron may produce a measurable signal. Considering a panel of quadripolar geodynamical models, we observe that simple preferential equatorial growth is the most consistent with seismological observations of a polar anisotropy and depth dependence of seismic residuals. Chemical stratification amplifies the global anisotropy by about 40%, but at the same time increases the scatter of residuals in a way that is poorly compatible with the observed depth dependence. Finally the addition of dendritic growth (solidification texture) prohibits the emergence of a first order North-South anisotropy. Independently of the geodynamical model it appears clearly that none of these geodynamical models the development of an anisotropy consistent with observations when using the published elastic properties of iron at inner core conditions. Following this work, several geodynamical models remain to be studied such as magnetic forcing (Lorentz forces). Models involving translation-thermal convection are of great interest as they may account for the hemispherical component of the seismic anisotropy.Secondly, we performed experiments on the α-ε (cubic centered to hexagonal compact iron) phase transition in pure iron. We compare our experimental texture results with our simulations of the transformation considering Burgers mechanism. We confirm here the Burgers atomic path as the mechanism activated during the α-ε transformation in iron. We find direct evidence of a strong variant selection controlled by non-hydrostatic stresses in the diamond anvil cell during the forward α→ε transformation, producing strong textures. The opposite will occur with the reverse ε→α phase transition where an almost complete randomization is to be expected. Our observations can be applied with some caution to the Earth's inner core and show that the strong seismic anisotropy in the inner core may not be explained by the occurrence of a hexagonal to cubic phase transition in the inner core. A limited texture memory effect was brought into light, already documented for other transition metals. At last, we performed a preliminary study on the effect of shear on the α-ε phase transition in pure iron using a rotational cell. Again the α-ε phase transformation in iron can be modelized by the Burgers mechanism. We find that simulations in the literature [Levitas et al., 2010] fail to reproduce our experimental results, particularly in terms of stress field.

Within the collaborative research center SFB 920 “Multifunctional Filters for Metal Melt Filtration”, the thermally induced formation of metastable aluminum oxides and related microstructural changes were investigated. It was confirmed that the γ-Al₂O₃ phase possesses a defective spinel structure containing Al vacancies that preserve the stoichiometry of this phase. The presence of vacancies fragments apparently the γ-Al₂O₃ crystallites into nanocrystalline domains, which are separated by non-conservative antiphase boundaries (APBs) of the type {100} ¼<110>. These APBs form a 3D network that is randomly distributed over all crystallographically equivalent lattice planes. This phenomenon causes a starlike (and hkl-dependent) broadening of the reciprocal lattice points that correspond to the aluminum sublattice. It was shown that the extent of the broadening of the reciprocal lattice points can be predicted by employing the phase shift factors. With increasing degree of the APBs ordering, the initial streaks representing the broadened reflections start to split, forming superstructure reflections. This superstructure of γ-Al₂O₃ is commonly known as δ-Al₂O₃. Between the ordered APBs, the crystal structure of δ-Al₂O₃ is closely related to the crystal structure of monoclinic θ-Al₂O₃. The phase transition of γ-Al₂O₃/δ-Al₂O₃ to θ-Al₂O₃ proceeds via migration of just three Al³⁺ cations to the neighboring tetrahedral and octahedral sites in the cubic close packed (ccp) oxygen sublattice. The general migration vector is ⅛<111> (γ-Al₂O₃). Diffraction effects associated with different intermediate states can be explained by an improper long-range ordering of equivalent APBs or certain Al³⁺ cations and the local formation of θ-Al₂O₃ within the δ-Al₂O₃ superstructure. The formation of θ-Al₂O₃ is accompanied by an increase of the occupancy of the tetrahedral sites in the oxygen sublattice by the Al³⁺ cations. In surrounding local γ-Al₂O₃ domains, however, some cations migrate from the tetrahedral to the octahedral sites. Thus, the local formation of θ-Al₂O₃ is nearly invisible for the ²⁷Al 1D magic angle spinning nuclear magnetic resonance (MAS NMR) spectroscopy. Still, it was recognized by the 2D multiple quantum (MQ) MAS NMR spectroscopy. A continuous formation of the θ-Al₂O₃ domains was confirmed by the Raman spectroscopy, X-ray diffraction (XRD) and selected area electron diffraction (SAED). The proposed microstructure and transformation models helped to explain the thermal stabilization of the metastable alumina phases by Si-doping. For investigation of the thermally induced phase transitions in metastable alumina phases, boehmite (γ-AlO(OH)) was chosen as the starting compound. However, the metastable alumina phases were also observed in endogenous inclusions present in solidified steel melts. For identification of these phases, a procedure for reconstruction of spherical Kikuchi maps from recorded EBSD patterns was developed.