[pt] Um dos maiores problemas encontrados na indústria mineral é a perda de material ultrafino em processos convencionais de separação. A operação de floculação seletiva vem sendo estudada para a recuperação destes materiais. Por outro lado, o uso de biossurfactantes no processamento mineral, extraídos de microrganismos, vem apresentando bons resultados para a recuperação deste tipo de material, além de serem biodegradáveis e possuírem baixa toxicidade. Nesta pesquisa, tem-se como objetivo o estudo da floculação seletiva de partículas ultrafinas de hematita contidas em rejeito de minério de ferro usando o biossurfactante extraído da levedura Cândida stellata. Foi realizado um estudo de caracterização envolvendo análise granulométrica, análise química e difração raio-X (DRX). Para avaliar a interação do biossurfactante na superfície dos minerais de hematita e quartzo, foram desenvolvidos estudos de espectroscopia de infravermelho com transformada de Fourier (FTIR), potencial Zeta, microscopia eletrônica de varredura (MEV) e tensão superficial. Para os testes de floculação, realizados por jar test – teste de proveta, avaliou-se a influência do pH, concentração de sólidos e concentração de biossurfactante. A energia de interação foi avaliada através das teorias DLVO e DLVO Estendida (X-DLVO). As análises de espectroscopia no infravermelho (FTIR) e potencial zeta indicaram uma forte adsorção do biossurfactante na superfície da hematita, sendo que o ponto isoelétrico da hematita foi alterado de 5,35 para 3,25. No estudo de tensão superficial do biossurfactante indicou uma concentração micelar crítica (CMC) de 150 mg/L em pH 3, alcançando um valor próximo de 30 mN/m. Durante os ensaios de floculação foi alcançada uma recuperação de 99 por cento de hematita em pH 3, usando 75 mg/L de biossurfactante e uma concentração de sólidos de 0,50 por cento (1,25 g/500 mL). Pelo estudo da energia de interação entre as partículas, devido ao sinal negativo das interações de ácido-base de Lewis, as partículas de hematita flocularam após o contato com o biossurfactante, indicando que houve uma forte interação hidrofóbica entre elas. Os resultados obtidos neste trabalho indicam que o biossurfactante extraído da levedura Cândida stellata possui uma boa seletividade para a aglomeração das partículas ultrafinas de hematita. / [en] One of the biggest problems encountered in the mineral industry is the loss of ultrafine material in conventional separation processes. The selective flocculation operation has been studied to recover these materials. On the other hand, the use of biosurfactants in mineral processing, extracted from microorganisms, has been showing good results for the recovery of this type of material, in addition to being biodegradable and having low toxicity. In this research, the objective is to study the selective flocculation of ultrafine hematite particles contained in iron ore tailings using the biosurfactant extracted from the yeast Candida stellata. A characterization study was carried out involving particle size analysis, chemical analysis and X-ray diffraction (XRD). In order to evaluate the interaction of the biosurfactant on the surface of hematite and quartz minerals, studies of Fourier transform infrared spectroscopy (FTIR), Zeta potential, scanning electron microscopy (SEM) and surface tension were developed. For the flocculation tests, performed by jar test, the influence of pH, solids concentration and biosurfactant concentration was evaluated. The interaction energy was evaluated using the DLVO and DLVO Extended (X-DLVO) theories. The infrared spectroscopy (FTIR) and zeta potential analyzes indicated a strong adsorption of the biosurfactant on the hematite surface, with the hematite isoelectric point being changed from 5,35 to 3,25. In the surface tension study of the biosurfactant, it indicated a critical micellar concentration (CMC) of 150 mg/L at pH 3, reaching a value close to 30 mN/m. During the flocculation tests, a recovery of 99 percent of hematite at pH 3 was achieved, using 75 mg/L of biosurfactant and a solids concentration of 0,50 percent (1,25 g). By studying the interaction energy between the particles, due to the negative sign of the Lewis acid-base interactions, the hematite particles flocculated after contact with the biosurfactant, indicating that there was a strong hydrophobic interaction between them. The results obtained in this work indicate that the biosurfactant extracted from the yeast Candida stellata has a good selectivity for the agglomeration of ultrafine hematite particles.

We are facing an important challenge, to reduce the greenhouse gas emissions to make sure that we limit global warming to 2 °C, preferably 1.5 °C. Drastic changes and developing new methods may be our only chance to keep global warming under 1.5 °C. The steel production in Sweden today accounts for 10% of the CO2 emission. The joint venture HYBRIT (Hydrogen Breakthrough Ironmaking Technology), between SSAB, LKAB and Vattenfall, aims to reduce the CO2 emission by developing a method that reduces iron ore pellets with hydrogen gas, leaving only water as off-gas. From simple thermodynamic calculations, it is evident that the reduction of iron ore using hydrogen gas is an endothermic reaction, requiring heat. Based on the calculated energy requirement, the temperature at the center of the pellet should not be the same as the temperature at the surface of the pellet but instead, decrease as the reduction reaction takes place. This report presents the temperature profile at the surface and in the center of a hematite pellet during hydrogen reduction at temperatures of 600 °C, 700 °C, 800 °C and 900 °C. Ideally, the results can be implemented in a model to better simulate the reduction reaction taking place inside a hematite pellet. The experiment consists of three sub-experiments, the first measures the temperature profile of the unreduced iron ore pellet in an argon gas atmosphere, secondly, the temperature profile and mass loss are measured during reduction, lastly, the temperature profile is measured for the reduced pellet in a hydrogen atmosphere. The mass loss measured during hydrogen reduction is used to calculate the degree of reduction. The results show that the reaction rate increases with increasing temperature and concentration of H2. Additionally, a higher reduction temperature gives the largest temperature decrease inside the pellet during reduction. At 900 °C, the temperature decrease is equal to 39 °C and at 600 °C, it is equal to 3 °C. The results prove that after a certain initial stage, gas diffusion and heat conduction through the product layers play important roles in controlling the reaction rate. There is even a period where a plateau of the reduction is observed, the reaction is mostly controlled by heat transfer. / Idag står vi inför en viktig utmaning, att minska utsläppen av växthusgaser och se till så att vi inte överskrider 2 °C uppvärmning, helst inte 1.5 °C. För att klara detta krävs drastiska förändringar och utvecklingar av nya metoder kan vara vår enda chans att uppnå 1.5-gradersmålet. Ståltillverkningen i Sverige idag står för 10% av CO2 utsläppen och för att bidra till att minska utsläppen av CO2 har företaget HYBRIT, vilket står för Hydrogen Brakethrough Ironmaking Technology, skapats. HYBRIT är en joint venture mellan SSAB, LKAB och Vattenfall som tillsammans vill skapa stål på ett mer miljövänligt sätt. Processen går ut på att reducera järnmalmspellets med hjälp av vätgas för att producera järnsvamp och ge ifrån sig vatten som avgas. Från enkla termodynamiska beräkningar är det lätt att inse att reduktionen med hjälp av vätgas är en endoterm process, som kräver energi. Det är genom denna kunskap som en kan föreställa sig att reduktionen av järnmalmspellets med hjälp av vätgas kommer bidra till en temperaturminskning. I denna rapport har temperaturprofilen inne i och på ytan av en hematitpellet mätts under tiden som den blivit reducerad med vätgas. Idealt kan resultaten implementeras i en modell för att bättre simulera reduktionsreaktionen som äger rum i en hematitpellets. Fyra olika reduktionstemperaturer har undersökts: 600 °C, 700 °C, 800 °C och 900 °C. Experimenten består av tre del-experiment, först mäts temperaturprofilen av den oreducerad hematitpelletsen i en argonatmosfär, sedan mäts viktminskningen och temperaturprofilen av pelleten medan den reduceras i en vätgasatmosfär, slutligen mäts temperaturprofilen av den reducerade pelleten i en argonatmosfär. Viktminskningen under reduktionen används för att beräkna reduktionsgraden under reduktionsförloppet. Resultaten visade att reduktionshastigheten ökade med ökande temperatur och koncentration av H2. Ökad temperatur gav även den största temperaturminskningen inne i pelleten då den reducerats med vätgas. Vid 900 °C uppmätes en temperaturminskning på 39 °C, varav reduktion vid 600 °C gav en temperaturminskning på 3 °C. Resultaten visar att efter en viss tids reduktion, spelar gasdiffusionen och värmeledningen genom produktlagret en viktig roll och är det som begränsar reduktions-hastigheten. Fortsatt, då hematitpelleten reducerades uppstod en platå där temperaturen var konstant och reaktionen till största delen var begränsad av värmeledningen genom produktlagret.

[pt] A literatura recente tem revelado o potencial de uso de estirpes microbianas na biotecnologia mineral. Pela afinidade com diferentes sistemas minerais, tais estirpes microbianas podem modificar as propriedades de superfície, e, dessa forma, mudar as características de uma superfície mineral. A bioflotação de minerais utiliza microrganismos como reagentes de flotação. No presente trabalho foi estudado o comportamento eletrocinético das partículas de quartzo e hematita, antes e após a interação com duas cepas da bactéria Bacillus subtilis. Os experimentos mostraram um deslocamento do ponto isoelétrico (PIE) da hematita que passou de 4 para 2,5 após interação com a cepa B. subtilis BAM, sugerindo um mecanismo de adsorção química. Já, a interação entre hematita e B. subtilis GLI, apresentou-se bem mais acentuada na faixa mais alcalina de pH. As medidas experimentais de ângulo de contato (método da gota séssil) foram realizadas para as superfícies das partículas minerais (hematita igual 27,4 graus; quartzo igual 13,0 graus) e das cepas B. Subtilis BAM (32,0 graus) e B. subtilis GLI (41,0 graus). A estirpe B. subtilis GLI foi capaz de modificar a superfície da hematita (46,0 graus) e, em menor proporção, a do quartzo (23,3 graus). Os valores de ângulo de contato foram utilizados para calcular as componentes de energia livre interfacial do quartzo, da hematita e das cepas. Os ensaios de microflotação realizados em tubo Hallimond modificado evidenciaram a aplicação da B. subtilis GLI como biorreagente. A melhor flotabilidade isolada de quartzo e hematita, conduzida por uma solução de B. subtilis GLI (600 mg.L(-1)), foi obtida em pH 6, com uma recuperação de 40 e 80 por cento, respectivamente. A seguir, o desempenho da flotação de uma mistura sintética, quartzo e hematita (na proporção 1:1), na presença de 600 mg.L(-1) da cepa B. subtilis GLI e em pH 6, foi avaliado, obtendose um concentrado contendo um teor de 74 por cento de Fe2O3.As teorias DLVO e XDLVO foram aplicadas para avaliar as energias de interação entre as cepas e os minerais em função da distância. A teoria X-DLVO foi capaz de prever a interação entre B. subtilis GLI e hematita justificando os resultados dos ensaios de flotação. Os resultados deste trabalho evidenciaram que a cepa B. subtilis GLI é promissora como biorreagente na flotação seletiva da hematita em relação ao quartzo. / [en] The recent literature has unveiled the potential use of microbial strains in mineral bioprocessing. Because of their affinity for different mineral systems, such microbial strains may modify the surface properties and in this way change the characteristics of a mineral surface. Mineral bioflotation uses microorganisms as flotation reagents. In the present work, the electrokinetic behavior of particles of quartz and hematite, before and after interaction with two strains of Bacillus subtilis, was studied. The experiments revealed a shift of the isoelectric point (IEP) which of hematite that changed from 4 to 2.5 after interaction with the strain B. subtilis BAM, suggesting a chemical adsorption mechanism, while the interaction between hematite and B. subtilis GLI presented itself much more pronounced in the alkaline pH range. The experimental measurements of the contact angle (sessile drop method) were taken for the surfaces of the mineral particles (hematite equal 27.4 degrees, 13.0 degrees equal quartz) and for the B. subtilis BAM (32.0 degrees) and B. subtilis GLI (41.0 degrees) strains. The B. subtilis GLI strain was capable of modifying the surface of the hematite (46.0 degrees), and to a lesser extent, the quartz (23.3 degrees). The contact angle values were used to calculate the interface free energy components of quartz, hematite and the bacterial strains. The microflotation tests on a modified Hallimond tube evidenced the application of B. subtilis GLI as bioreagent. The best isolated flotability of quartz and hematite conducted by a solution of B. subtilis GLI (600 mg.L(-1)) was obtained at pH 6, with a recovery of 40 and 80 percent, respectively. Subsequently, the flotation performance of a synthetic mixture, quartz and hematite (in ratio 1:1) in the presence of 600 mg.L(-1) of the strain B. subtilis GLI at pH 6, was evaluated and showed a concentrate with a content of 74 percent Fe2O3. The DLVO and X-DLVO theories were applied to assess the energies of interaction between strains and minerals depending on the distance. The X-DLVO theory was able to preview the interaction between B. subtilis GLI and hematite, justifying the results of the flotation tests. The results of this study indicated that the strain B. subtilis GLI is promising as a bioreagent in the selective flotation of hematite relative to quartz.

<p> The "B" horizon at Tilt Cove occurs in subaqueous mafic volcanics near the base of the Silurian Cape St. John Group. It is 3 metres below a well-banded oxide iron formation ("A" horizon). </p> <p> Mineralization in the "B" horizon is analogous to that of the East Mine in that it is volcanogenic and has resulted in extensive chloritization of the footwall rocks, and in the deposition of banded sulphides or the replacement of the existing mafic volcanics by sulphides. There are differences in the geochemistry mineral textures and mineral types. The East Mine host volcanics are alkali depleted basaltic komatiites to magnesium theleiites. The horizon host volcanics are spillitized magnesium tholeiites. Samples of ore from the East Mine show well-developed colloform and framboidal textures. Pyrite, magnetite, hematite and chalcopyrite are the dominant minerals with minor sphalerite and accessory covellite. Samples from the horizon show relict colloform textures and framboids with less internal structure due to overgrowths. Atoll textures indicating extensive replacement are common. Pyrite is the dominant sulphide followed by sphalerite, chalcopyrite, accessory covellite and gold. The chalcopyrite occurs both as replacement of pyrite and exsolution in sphalerite. The most significant difference between samples from the East Mine and "B" horizon is the greater abundance of gold in the "B" horizon and its correlation with sphalerite. </p> / Thesis / Bachelor of Science (BSc)

No description available.

No description available.

M.Tech. (Department of Chemistry, Faculty of Applied Sciences), Vaal University of Technology / Many oxidic iron compounds—iron oxides; oxy-hydroxides and hydroxides—not only play an important role in a variety of disciplines but also serve as a model system of reduction and catalytic reactions. There are more than 16 identifiable oxidic iron compounds. The reduction of these compounds has been investigated for centuries. Despite this, the reduction behavior of the oxides is not fully understood as yet. To date the reduction mechanism is still plagued with uncertainties and conflicting theories, partly due to the complex nature of these oxides and intermediates formed during the reduction. Thermodynamically, the reduction of iron oxide occurs in steps. For example, during the reduction of hematite (a-Fe2O3) magnetite (Fe3O4) is first formed followed by non-stoichiometric wüstite (Fe1-yO) and lastly metallic iron (a-Fe). The rate of transformation depends on the reduction conditions. Further, this reduction is accompanied by changes in the crystal structure. The reduction behavior of iron oxides using graphite under ball-milling conditions was investigated using Planetary mono mill (Fritsch Pulverisette 6), Mössbauer Spectroscopy (MS), X-ray Diffraction (XRD), Scanning electron microscopy (SEM) and Transmission Electron Microscopy (TEM). It was found that hematite transformed into magnetite, Wüstite and or cementite depending on the milling conditions. The study shows that by increasing the milling time, the rotational speed and / or the ball to powder ratio, the extent of the conversion of hematite to its reduction products increased. Further investigations are required for the elucidation of the reduction mechanism. The reaction og magnetite and graphite at different milling conditions lead to the formation of Fe2+ and Fe3+ species, the former increasing at the expense of Fe3O4. Fe3O4 completely disappeared after a BPR of 50:1 and beyond. The Fe2+ species was confirmed to be due to FeO using XRD analysis. HRSEM images Fe2O3 using scanning electron microscopy prior to and after milling at different times showed significant changes while the milling period was increased, HRSEM images showed that the once well defined hematite particles took ill-defined shapes and also became smaller in size, which was a results of the milling action that induced reaction between the two powders to form magnetite. EDX spectra at different milling times also confirmed formation of magnetite. EDX elemental analysis and quantification confirmed the elemental composition of starting material consisting mainly of iron. Similarly, HRSEM images of Fe3O4 using Scanning electron microscopy (SEM) prior to and after milling at different BPR showed significant changes when the milling period was increased. EDX spectra at different milling times also confirmed formation of partial FeO and EDX elemental analysis and quantification confirmed the elemental composition of starting material consisting mainly of iron than Fe2O3. TEM images of both Fe2O3 and Fe3O4 particles at different milling conditions displayed observable particle damages as a function of milling period.The once well - defined particles (Fe2O3 and Fe3O4 ) successively took ill – defined shapes, possibly accompanied by crystallite size reduction. MAS showed that the reactive milling of α- Fe2O3 and C resulted in reduction to Fe3O4 , FeO and or cementite depending on the milling conditions etc Time, milling speed and BPR variation which influenced the reduction. The study shows that by increasing the milling time, the rotational speed and / or the ball to powder ratio, the extent of the conversion of hematite to its reduction products increased. XRD study investigations even though were unable to detect spm species (Fe2+ and Fe3+ ) which has smaller crystallites below detection limits ,the variation in time showed an increment in the magnetite peaks accompanied by recession of hematite and graphite peaks as the milling time was increased which relates to the MAS observation.XRD also corroborated the data obtained from MAS that showed that the main constituent was magnetite and further evidence in support of the reduction of hematite to magnetite under reactive milling was obtained using XRD . Overall, the work demonstrated selective reduction of Fe2O3 to Fe3O4 and Fe3O4 to FeO by fine tuning the milling conditions. It is envisaged that the reduction of FeO to Fe and possible carburization to FexC could also be achieved.

Les instabilités paramétriques non linéaires (NL) ont été observées sur les ondes magnéto-élastiques dans le cas d’un couplage de trois quasi-phonons sous pompage électromagnétique. La théorie en prédit une dynamique supercritique explosive, mais limitée expérimentalement par le décalage de fréquence dû aux fortes nonlinéarités. La dynamique supercritique des instabilités paramétriques NL est étudiée dans deux matériaux antiferromagnétiques "plan facile" (AFEP): l’hématite α-Fe2O3 et le borate de fer FeBO3. Ces matériaux possèdent une très grande NL acoustique effective en raison du couplage magnéto-élastique élevé. Les mécanismes de limitation de la dynamique explosive ont été analysés à l'aide de l'approximation anharmonique. La compensation du décalage fréquentiel NL par une modulation de phase singulière du pompage a été proposée et théoriquement vérifiée, puis utilisée pour l’observation expérimentale de la dynamique supercritique explosive des excitations de trois quasi-phonons dans les résonateurs magnéto-élastiques. Les études sur FeBO3 ont été réalisées dans la gamme de température 77 K - 293 K où les paramètres magnéto-élastiques du cristal varient de façon significative. Un modèle fortement non linéaire des excitations de trois quasi-phonons dans les AFEPs a été développé. Les simulations numériques sont en accord avec les résultats expérimentaux. Les études théoriques de couplage de trois ondes magnéto-élastiques progressives ont été effectuées sur la base de modèles théoriques prenant en compte la non-linéarité cubique des cristaux AFEP réels. Les simulations numériques prévoient un comportement explosif et une localisation spatiale des triades générées / Recently discovered nonlinear parametric instabilities occur when nonlinear parameter of a system is modulated. These instabilities were reported on magnetoelastic waves as three quasi-phonon coupling under electromagnetic pumping. Theoretical studies predicted supercritical explosive dynamics of these instabilities. Experimentally such singular behavior is limited by strong nonlinear frequency shift.Presented work studies supercritical dynamics of nonlinear parametric instabilities in two easy plane antiferromagnets (AFEP): hematite α-Fe2O3 and iron borate FeBO3. These materials possess unprecedented effective acoustic nonlinearity due to high magneto-elastic coupling. Limiting mechanisms of explosive dynamics were analyzed with the help of anharmonic approximation. Nonlinear frequency shift compensation via singular pumping field phase modulation was suggested and theoretically approbated. This technique was successfully used for experimental observation and investigation of supercritical explosive dynamics of three quasi-phonon excitations in magnetoelastic resonators. Iron borate studies were performed in the temperature range 77 K – 293 K where magnetoelastic parameters of the crystal vary essentially. Strongly nonlinear model of three quasi-phonon excitations in AFEPs was developed. Numerical simulations of the model showed good agreement with experimental results.Theoretical studies of three travelling magnetoelastic waves coupling are performed on the basis of suggested theoretical models that take into account cubic nonlinearity of real AFEP crystals. Numerical simulations of the models suggest explosive behavior and spatial localization of generated triads

Im Mittelpunkt der in dieser Arbeit durchgeführten Untersuchungen steht die Aufklärung der Strukturen der Komplexe von Uran mit aliphatischen (Hydroxy-)Carbonsäuren als Liganden sowie die Strukturen, die bei Sorption von Uran an dem Eisenmineral Hämatit in An- und Abwesenheit organischer Säuren gebildet werden. Das ternäre System aus Hämatit, Uran(VI) und organischem Ligand ist sehr komplex. Daher ist es notwendig eine Aufspaltung in einfachere binäre Systeme vorzunehmen und die Ergebnisse dieser Teilsysteme heranzuziehen, um das komplexere ternäre System zu verstehen. Anhand der umfangreichen durchgeführten Arbeiten zu den wässrigen Uran(VI)-Komplexen können nun Rückschlüsse von der Struktur einer Carbonsäure auf die Struktur der gebildeten Uran(VI)-Komplexe in Abhängigkeit vom pH getroffen werden. Zuerst sollte festgehalten werden, dass Uran(VI) üblicherweise pentagonal-bipyramidale Komplexe ergibt. Das Pentaaquauranylion zeigt beispielsweise zwei axiale Sauerstoffatome (Oax) bei einem Abstand von 1,76 Å und fünf äquatoriale Sauerstoffatome (Oeq) bei einem Abstand von 2,40 Å, die von koordinierten Wassermolekülen stammen. Im Zuge der Komplexierung mit organischen Liganden werden die Wassermoleküle durch organische Liganden ersetzt, was zu messbaren Veränderungen der Bindungsabstände führt. Monocarbonsäuren bilden mit Ausnahme der Ameisensäure nacheinander mit steigendem pH 1:1-, 1:2- und 1:3-Komplexe. Die teilweise in der Literatur postulierten 1:4-Komplexe beschränken sich wahrscheinlich auf extrem hohe Ligandkonzentration (>>1 M) oder nicht-wässrige Lösungen (z. B. 1:4-U-ac-Komplex [Ryan 1967]). Anhand der Verringerung der spektralen Aufspaltung Δν der symmetrischen und antisymmetrischen Valenzschwingung der Carboxygruppe konnte für diese Komplexe eine bidentate Koordination nachgewiesen werden. Mittels EXAFS konnte die bidentate Struktur anhand einer Verlängerung des Oeq-Abstandes auf 2,47 Å im Falle der 1:3-Komplexe in den Systemen U-ac und U-prop bestätigt werden. Die Ameisensäure hingegen bildet monodentate Komplexe. Dies konnte durch eine Erhöhung von Δν und eine Verkürzung des Oeq-Abstandes gezeigt werden. Ursache für dieses Verhalten ist der fehlende +I-Effekt durch den organischen Rest, der unter anderem eine deutliche Erhöhung der Säurestärke im Falle der Ameisensäure nach sich zieht. Bei Bi- und Tricarbonsäuren bestimmt der Abstand der Carboxygruppen zueinander, welche Art der Koordinierung auftritt. Werden die Carboxygruppen durch maximal ein Kohlenstoffatom voneinander getrennt (Oxal- und Malonsäure) oder wird durch eine cis-Doppelbindung eine cis-Konfiguration der Carboxygruppen zueinander erzwungen (Maleinsäure), treten 1:1- und 1:2 , sowie für Oxalsäure auch 1:3-Komplexe mit chelatartiger Koordinierung auf. Dies wird durch eine Erhöhung von Δν und eine Verringerung von r(U-Oeq) auf 2,36 Å (1:2-Komplexe) untermauert. Liegen mindestens zwei Kohlenstoffatome zwischen den Carboxygruppen (Bernsteinsäure, Tricarballylsäure), so bilden sich überwiegend bidentate Komplexe aus. Der 1:3-Komplex im System U-suc ist allerdings gemischt bidentat/monodentat und erreicht deshalb auch einen gegenüber dem 1:3 U-ac Komplex etwas verkürzten Oeq-Abstand von 2,45 Å. Eine weitere wichtige Gruppe von Liganden sind die α- und β-Hydroxycarbonsäuren. Die α-Hydroxycarbonsäuren bilden 1:1-, 1:2-, 2:2- und 3:3-Komplexe aus. Der Ligand koordiniert dabei als 5-Ring-Chelat an Uran(VI). Die Bildung polynuklearer Spezies wird belegt mit einem stufenweisen und sehr starken Ansteigen der Absorption im UV/VIS-Bereich, der durch eine Deformation der linearen O=U=O-Bindung hervorgerufen wird. Außerdem zeigt die EXAFS-Spektroskopie, dass bei pH ~ 2–4 eine U-U-Wechselwirkung bei r(U-U) ~ 3,92 Å auftritt, wodurch die Bildung eines µ2-O verbrückten Dimers nachgewiesen ist. Im nahneutralen pH-Bereich (pH 6–7) ist eine sehr starke U-U-Wechselwirkung bei r(U-U) ~ 3,83 Å er-kennbar. Diese kann durch Ausbildung einer µ3-O verbrückten dreikernigen Struktur erklärt werden. Zwischen den α-Hydroxymonocarbonsäuren und den α-Hydroxydi- und -tricarbon-säuren, die als substituierte Äpfelsäure aufgefasst werden können, besteht der wesentliche Unterschied, dass die Homologen der Äpfelsäure das Dimer im oben genannten pH-Bereich als dominierende Spezies aufweisen, während es bei den Monocarbonsäuren erst bei höheren pH-Werten (pH ~ 4–5) und lediglich zu ~50 % (lac) auftritt. Die β-Hydroxycarbonsäuren bilden hingegen bidentat koordinierende 1:1-, 1:2- und 1:3-Komplexe. Die 1:3-Komplexe sind isostrukturell zum 1:3-U-ac-Komplex. Die Hydroxygruppe in β-Position beteiligt sich folglich nicht an der Komplexierung. Bei der Sorption von Uran(VI) an Hämatit in An- und Abwesenheit organischer Liganden ergibt sich ein breit gefächertes Spektrum an Möglichkeiten. Allgemein lässt sich feststellen, dass die Sorption etwa bei pH 3–4 einsetzt und im nahneutralen pH-Bereich (pH 6–7) maximal wird. Die Anwesenheit organischer Liganden bewirkt im Allgemeinen eine Verschiebung der Sorptionskante zu höheren pH-Werten, wobei folgende Reihenfolge der pH-Werte bei 50 %iger Sorption zu beobachten war: ohne Ligand ~ Protocatechusäure < Essigsäure < Bernsteinsäure < Weinsäure. Weiterhin kann festgestellt werden, dass die Sorptionskomplexe in der Nähe der Sorptionskante monomer sind und in oligomere Urankomplexe im nahneutralen pH-Bereich übergehen. Ohne Zugabe eines Liganden bildet sich mit steigendem pH zuerst ein über Kante verknüpfter, monomerer Sorptionskomplex (ES-Monomer) aus, der sich durch einen Fe-Abstand von ~3,45 Å und einen Oeq-Abstand von ~2,40 Å auszeichnet. Im neutralen pH-Bereich sorbiert Uran als oligomerer (wahrscheinlich dreikerniger) Sorptionskomplex (ES-Trimer) mit r(U-U) = 3,82–3,88 Å und r(U-Oeq) = 2,33–2,37 Å. Im Übergangsbereich kann sich zu geringen Teilen ein einfach oder doppelt über Ecke verknüpfter Sorptionskomplex (SCS- oder DCS-Monomer), wobei das SCS-Monomer einen Fe-Abstand von ~3,70–3,75 Å und einen Oeq-Abstand von ~2,40 Å aufweist, bilden. In Gegenwart von Essigsäure ändern sich lediglich die Strukturparameter minimal. In Gegenwart von Bernstein- und Weinsäure bilden sich im Gegensatz dazu über den Liganden verknüpfte Sorptionskomplexe aus, die also keine U-Fe-Wechselwirkung zeigen und sich besonders durch ihren sehr niedrigen DW(Oeq) von den anderen Sorptionskomplexen unter-scheiden. Im neutralen pH-Bereich liegen wiederum dreikernige Sorptionskomplexe vor, wo-bei es im Falle der Weinsäure auch möglich wäre, dass das aus dem aquatischen System be-kannte Trimer über die Weinsäure an die Oberfläche bindet. Im Unterschied dazu sorbiert Uran(VI) in Gegenwart der Protocatechusäure nahe der Sorptionskante als Gemisch eines monomeren ES- und DCS-Komplexes. Bei weiterer Erhöhung des pH dominiert der DCS-Komplex, der eine starke U-Fe-Wechselwirkung bei r(U-Fe) = 4,19 Å zeigt. Eine Oligomerisierung bleibt in diesem Falle aus. Die im Rahmen dieser Arbeit gewonnenen Ergebnisse tragen zu einem besseren Verständnis der Wechselwirkung von Uran(VI) mit organischen Säuren, sowie von Uran(VI) mit Hämatit in Gegenwart organischer Säuren, bei und liefern die Strukturen für die gebildeten wässrigen Komplexe und die Sorptionskomplexe. Damit unterstützen sie den Aufklärungsprozess des Transports radioaktiver Stoffe und können somit zuverlässigere Risikobewertungen für Endlager nuklearer Abfälle und für Rückstände des Uranerzbergbaus ermöglichen. / This study is focussed on throwing light on the structures of uranium(VI) complexes with aliphatic (hydroxy-) carboxylic acids and on the structures of the sorption complexes on the iron mineral hematite in presence and absence of organic acids. The ternary system of hematite, uranium(VI), and organic ligand is very complicated, thus it is necessary to decompose it in binary systems. The results within these binary systems are used to better understand the complicated ternary system. Based on the comprehensive investigations on the aqueous uranium(VI) complexes, it is now possible to draw inferences from the structure of the carboxylic acid about the structure of the formed uranium(VI) complex in dependence of the pH. At first it has to be mentioned that uranium(VI) commonly gives pentagonal bipyramidal complexes. The pentaaquauranylion is formed by two axial oxygen atoms (Oax) at a distance of 1.76 Å and five equatorial oxygen atoms (Oeq) at 2.40 Å stemming from coordinated water molecules. Due to complexation with organic ligands water is replaced by the ligand, thus the interatomic distances change. Monocarboxylic acids, except for formic acid, form with rising pH 1:1, 1:2, and 1:3 complex-es, successively. 1:4-complexes that were sometimes postulated in literature are probably restricted to very high ligand concentrations (>>1 M) or to non-aqueous solutions. On the basis of the decrease of the spectral splitting Δν of the symmetric and antisymmetric vibration mode of the carboxylic group bidentate coordination is verified. By using EXAFS spectros-copy the structure of the 1:3 complexes with acetic and propionic acid shows an elongation of the U-Oeq distance (r(U-Oeq)) to 2.47 Å and a six fold coordination in the equatorial plane. This distance is characteristic for bidentate coordination of the carboxylic group. In contrast, formic acid gives monodentate complexes. This is proved by an increase of Δν and a shortening of r(U-Oeq). The reason for this behaviour is the missing +I effect from the organic chain that accounts for a dramatically stronger acidity of formic acid. Among the bi- and tricarboxylic acids, the distance between the carboxylic groups is decisive for the prevailing mode of coordination. If the carboxylic groups are only separated by no more than one carbon atom (oxalic and malonic acid) or if the cis-configuration of the carboxylic groups is enforced by a cis-configuration of the ligand (maleic acid), 1:1 and 1:2 complexes with chelating coordination will be formed. This is evidenced by an increase of Δν and a decrease of r(U-Oeq) to 2.36 Å (1:2-complexes). If at least two carbon atoms separate the carboxylic groups from each other (succinic acid), the coordination will be mainly bidentate. However, the 1:3 complex in the U-suc system gives a mixed bidentate/monodentate coordination, thus r(U-Oeq) is only increased to 2.45 Å. Another important group of ligands are the α- and β-Hydroxy acids. α-Hydroxy acids form 1:1, 1:2, 2:2, and 3:3 complexes with rising pH. In all cases the ligand gives 5-membered ring chelates. The formation of polynuclear species is evidenced by a stepwise and very strong increase of the absorption in the UV-Vis range that is caused by a deformation of the linear O=U=O moiety. Moreover, EXAFS spectroscopy shows a uranium-uranium interaction at r(U-U) ~ 3.92 Å in the pH range of 2–4. This distance gives evidence for the formation of a µ2-O bridged dimer. In the near neutral pH range (pH 6–7) a very strong U-U interaction is visible at r(U-U) ~ 3,83 Å. This feature can be explained by the formation of a µ3-O bridged trimeric structure. The main difference between the α-Hydroxy diacids that can be understood as homologues of malic acid and the α-Hydroxy monoacids (glycolic acid, lactic acid, etc.) is the strength of the dimeric complex. Among the homologues of malic acid the complex sta-bility constant of the dimer is so high that the formation of a 1:2 complex is suppressed and the relative concentration of the dimer is at least 90 % in the pH range of 2–4. Among the α-Hydroxy monoacids the occurrence of the dimer is shifted to higher pH values and the relative concentration is limited (e.g. ~50 % in the U-lac system). On the contrary, β-Hydroxy acids form bidentate coordinated 1:1, 1:2, and 1:3 complexes. The 1:3 complexes are isostructural to the 1:3 complex in the U-ac system. Hence, the β-Hydoxy group does not participate in the coordination. For the sorption of uranium(VI) on hematite in absence and presence of organic ligands a widespread array of opportunities exists. In general, sorption starts at pH 3–4 and reaches its maximum in the near neutral pH range (pH 6–7). The presence of organic ligands leads to a shift of the sorption edge to higher pH. The following sequence of the pH where 50 % sorp-tion is reached were found: without ligand ~ protocatechuic acid < acetic acid < succinic acid < tartaric acid. Moreover, it can be stated that the complexes near to the sorption edge are monomeric and merge into oligomeric uranium(VI) complexes in the near neutral pH range. In the absence of organic ligands a monomeric edge-sharing complex (ES monomer) is formed at low pH which is characterized by an U-Fe distance of ~3.45 Å and an Oeq distance of ~2.40 Å. In the near neutral pH range an oligomeric edge-sharing complex (ES trimer) is formed with r(U-U) = 3.82–3.88 Å and r(U-Oeq) = 2.33–2.37 Å. It is possible that in the intermediate pH range a small fraction of single or double corner-sharing (SCS or DCS) complexes occur. The SCS monomer is characterized by r(U-Fe) ~3,70–3,75 Å and r(U-Oeq) ~2,40 Å. The presence of acetic acid has only small effects on the structural parameters. In presence of succinic and tartaric acid and at low pH the sorption complexes are of the type hematite-ligand-uranium, thus no uranium-iron interaction can be found and the DW(Oeq) is very small in contrast to all the other investigated sorption complexes. In the neutral pH range trimeric sorption complexes are formed again. In case of tartaric acid it is conceivable that the trimeric complex known from the aqueous U-tar system is sorbed to the hematite surface. In contrast, the presence of protocatechuic acid results in the formation of a mixture of ES and DCS monomeric complexes at low pH. With ongoing increase of pH the fraction of the DCS monomer rises. This DCS complex shows a strong uranium-iron interaction at r(U-Fe) = 4,19 Å. A formation of oligomeric complexes at neutral pH does not appear. The results gained during all these investigations can help to better understand the interaction of uranium(VI) and carboxylic acids, and beyond that the sorption of uranium(VI) on hematite in the presence of carboxylic acids. Structures of the aqueous and sorption complexes are proposed. All these findings support the ongoing research on the transport behaviour of radioactive matter and may lead to more reliable risk assessment in connection with the permanent disposal of nuclear waste and the residues of uranium mining.

The chemistry and corrosion mechanisms associated with reduced sulfur compounds such as calcium sulfide, present in ground granulated blast-furnace slag (GGBFS), have been studied in high-density concrete, mortar and simulated pore-water environments. The high-density concrete and mortar samples were produced to replicate the high-density GGBFS concrete, in the dry storage containers (DSCs), used for radiation shielding from used nuclear fuel. Electrochemical measurements on embedded steel electrodes in high-density GGBFS concrete and mortar samples, showed that sulfide is capable of consuming oxygen to create a stable, reducing environment, though not in all cases, and the high-frequency electrolyte resistance increases with hydration time. Ion chromatography on simulated pore-water environments determined that thiosulfate is quite kinetically stable as a sulfide oxidation product and magnetite is capable of oxidizing sulfide. Microscopy has also been used to provide visual evidence of GGBFS hydration and elemental quantification of the hydrating microstructure in different environments.