O caulim do Rio Capim na Amazônia Oriental se constitui num depósito importante para o Brasil, ocupando lugar de destaque na produção mundial desta matéria prima mineral. Os modelos estabelecem uma origem para a caulinita vinculada ao intemperismo em condições lateríticas (Paleogeno Inferior) a partir de um substrato formado por rochas sedimentares da Formação Ipixuna (Cretáceo Superior). No perfil, destacam-se em ordem de importância entre os compostos de ferro, a hematita e a goethita, minerais pouco estudados no caulim do Rio Capim. A partir dos fácies principais do caulim (fácies caulim macio na base e caulim duro no topo), foram separados e concentrados os minerais de interesse para estudos de detalhe, utilizando a difratometria de raios X (DRX) e a espectrometria de infravermelho por transformada de Fourier (FTIR). Entre os parâmetros determinados, obtiveram-se estimativas da dimensão, forma, área superficial e substituição isomórfica. A interpretação dos resultados evidencia o potencial de aplicação das informações na estimativa do comportamento destes minerais durante o processo de beneficiamento e para a discussão do modelo genético dos perfis de caulim. As goethitas e hematitas de ambos os fácies possuem propriedades muito semelhantes, reforçando o modelo que especula sobre uma origem comum para a fácies caulim macio e caulim duro do perfil. Entre as propriedades, destacam-se a elevada cristalinidade e a baixa participação do alumínio em sua composição, proporcionando a estes minerais um comportamento com resistência moderada a elevada nos processos de lixiviação ácida e a tendência de dissolução preferencial da hematita. O conjunto de características dos óxidos e oxihidróxidos de ferro são compatíveis com uma formação em ambientes hidromórficos, com baixa influência da matéria orgânica a partir de soluções com baixa atividade do ferro, moderadamente redutoras a fracamente ácidas. Dentro do modelo genético da formação do caulim, sua origem não está associada à zona de laterização do perfil, sendo compatível com um ambiente saprolítico e hidromórfico. As propriedades observadas permitem afirmar que os processos naturais que favoreceram a formação da caulinita na base do manto de alteração foram suficientemente longos e intensos para promover a retirada do ferro destas fácies num processo não dissociado no tempo. No modelo, o caulim é uma fácies da base do perfil formado abaixo do nível freático de um espesso perfil laterítico em condições moderadamente redutoras e ácidas com elevada atividade do Si e do Al, porém, com carência de Al disponível para a formação da hematita e da goethita. Neste ambiente, haveria uma lenta mobilização do Fe dentro do perfil sem a necessidade do estabelecimento de um evento excepcional com uma elevada atividade da matéria orgânica, como previsto em alguns modelos. / The Rio Capim Kaolin from the eastern Amazon is recognized as one of the largest deposits of Brazil with a quality and volume that place this area amongst the most important deposits in the world. Despite the importance and the significant amount of studies about kaolin, many questions remain unanswered and the genesis of this occurrence is not well understood. Perhaps, the consensus today is the acceptance of the Rio Capim kaolin origin to be related to a lateritic weathering process during the Early Paleogene, period with favorable geotectonic, duration and climatic conditions to originate a thick cover with the development of a complete weathering profile above a substrate composed by sedimentary rocks of the Ipixuna Formation (Cretaceous). The models consider kaolin to be a bottom facies of a thick lateritic profile, but nowadays the upper lateritic facies was destroyed (probably by erosion periods along the middle to upper Paleogene). The kaolin profile has two facies: the bottom one, which is called soft kaolin, and the upper, differentiated one forming the flint kaolin. Most controversial points are related to the way that the flint kaolin was formed and the mechanism in which the iron was mobilized from the kaolin profile as a whole. This study aims to get some insight about the Rio Capim kaolin development using some properties measured from the iron oxides and oxyhydroxides. The iron and titanium minerals from the kaolin represent the most important contaminants, and a large effort is made by the industry to eliminate their influence but, despite this negative reputation, those minerals also represent a source of valuable information about the environmental conditions of the profile. Among them, hematite is the most widespread in the entire kaolin profile, followed by goethite, whose importance increases in the direction of the flint kaolin facies. Representative samples of kaolin facies were selected from the kaolin profile and submitted to an approach that allowed concentrating the iron minerals and eliminating the influence of kaolinite. Using X-ray diffraction (XRD) and Fourier Transform Infrared (FTIR), a set of properties of the hematite and goethite were determined, including median crystal dimensions, shapes, specific surface area and mineral composition by estimating the isomorphous replacement of iron (Fe) by aluminum (Al). The results show that hematites and goethites do not have enough differences in their properties to support a genesis model with radical changes in their conditions . In terms of behavior to acid leaching, the observed variations were important to predict differences in the rate of mineral dissolution and possibilities of preferential dissolution of hematite in relation to goethite, promoting the increase of the yellow component with the leaching. Both hematite and goethite have high crystallinity and the isomorphous replacement of Fe by Al is low. Comparing the properties observed in synthetic and natural environments, the hematite and goethite from the Rio Capim kaolin profile have characteristics that relate these minerals to a formation environment in hydromorphic conditions where the influence of organic matter was low, with low iron activity, weakly reduced and acidic conditions. These conditions are found in a saprolitic domain in accordance with the bottom facies of a thick laterite profile. Despite agreeing with a laterite model, differences make it difficult to explain iron depletion by organic matter only (Pirabas Event) and the origin of flint kaolin facies by a subsequent and superimposed laterite period. With the hematite and goethite properties found in this study, it is possible to propose that the Rio Capim kaolin is the bottom facies of a laterite profile formed in the zone permanently below the water table. Contrasting with the upper laterite portion of the profile, the bottom zone is in hydromorphic conditions and allowed the fixation of Al and Si to form kaolinite by primary feldspar and mica minerals of the Ipixuna Formation. This environment promotes the slow depletion of iron without the need of an exceptional accumulation of organic matter. The flint kaolin facies was formed in the same period of the soft kaolin facies and the observed differences in the kaolinite morphology are only related to changes caused by the location of this facies in the intermediate zone characterized by the water table fluctuation, but again without the need of subsequent superimposed lateritic processes.

O caulim do Rio Capim na Amazônia Oriental se constitui num depósito importante para o Brasil, ocupando lugar de destaque na produção mundial desta matéria prima mineral. Os modelos estabelecem uma origem para a caulinita vinculada ao intemperismo em condições lateríticas (Paleogeno Inferior) a partir de um substrato formado por rochas sedimentares da Formação Ipixuna (Cretáceo Superior). No perfil, destacam-se em ordem de importância entre os compostos de ferro, a hematita e a goethita, minerais pouco estudados no caulim do Rio Capim. A partir dos fácies principais do caulim (fácies caulim macio na base e caulim duro no topo), foram separados e concentrados os minerais de interesse para estudos de detalhe, utilizando a difratometria de raios X (DRX) e a espectrometria de infravermelho por transformada de Fourier (FTIR). Entre os parâmetros determinados, obtiveram-se estimativas da dimensão, forma, área superficial e substituição isomórfica. A interpretação dos resultados evidencia o potencial de aplicação das informações na estimativa do comportamento destes minerais durante o processo de beneficiamento e para a discussão do modelo genético dos perfis de caulim. As goethitas e hematitas de ambos os fácies possuem propriedades muito semelhantes, reforçando o modelo que especula sobre uma origem comum para a fácies caulim macio e caulim duro do perfil. Entre as propriedades, destacam-se a elevada cristalinidade e a baixa participação do alumínio em sua composição, proporcionando a estes minerais um comportamento com resistência moderada a elevada nos processos de lixiviação ácida e a tendência de dissolução preferencial da hematita. O conjunto de características dos óxidos e oxihidróxidos de ferro são compatíveis com uma formação em ambientes hidromórficos, com baixa influência da matéria orgânica a partir de soluções com baixa atividade do ferro, moderadamente redutoras a fracamente ácidas. Dentro do modelo genético da formação do caulim, sua origem não está associada à zona de laterização do perfil, sendo compatível com um ambiente saprolítico e hidromórfico. As propriedades observadas permitem afirmar que os processos naturais que favoreceram a formação da caulinita na base do manto de alteração foram suficientemente longos e intensos para promover a retirada do ferro destas fácies num processo não dissociado no tempo. No modelo, o caulim é uma fácies da base do perfil formado abaixo do nível freático de um espesso perfil laterítico em condições moderadamente redutoras e ácidas com elevada atividade do Si e do Al, porém, com carência de Al disponível para a formação da hematita e da goethita. Neste ambiente, haveria uma lenta mobilização do Fe dentro do perfil sem a necessidade do estabelecimento de um evento excepcional com uma elevada atividade da matéria orgânica, como previsto em alguns modelos. / The Rio Capim Kaolin from the eastern Amazon is recognized as one of the largest deposits of Brazil with a quality and volume that place this area amongst the most important deposits in the world. Despite the importance and the significant amount of studies about kaolin, many questions remain unanswered and the genesis of this occurrence is not well understood. Perhaps, the consensus today is the acceptance of the Rio Capim kaolin origin to be related to a lateritic weathering process during the Early Paleogene, period with favorable geotectonic, duration and climatic conditions to originate a thick cover with the development of a complete weathering profile above a substrate composed by sedimentary rocks of the Ipixuna Formation (Cretaceous). The models consider kaolin to be a bottom facies of a thick lateritic profile, but nowadays the upper lateritic facies was destroyed (probably by erosion periods along the middle to upper Paleogene). The kaolin profile has two facies: the bottom one, which is called soft kaolin, and the upper, differentiated one forming the flint kaolin. Most controversial points are related to the way that the flint kaolin was formed and the mechanism in which the iron was mobilized from the kaolin profile as a whole. This study aims to get some insight about the Rio Capim kaolin development using some properties measured from the iron oxides and oxyhydroxides. The iron and titanium minerals from the kaolin represent the most important contaminants, and a large effort is made by the industry to eliminate their influence but, despite this negative reputation, those minerals also represent a source of valuable information about the environmental conditions of the profile. Among them, hematite is the most widespread in the entire kaolin profile, followed by goethite, whose importance increases in the direction of the flint kaolin facies. Representative samples of kaolin facies were selected from the kaolin profile and submitted to an approach that allowed concentrating the iron minerals and eliminating the influence of kaolinite. Using X-ray diffraction (XRD) and Fourier Transform Infrared (FTIR), a set of properties of the hematite and goethite were determined, including median crystal dimensions, shapes, specific surface area and mineral composition by estimating the isomorphous replacement of iron (Fe) by aluminum (Al). The results show that hematites and goethites do not have enough differences in their properties to support a genesis model with radical changes in their conditions . In terms of behavior to acid leaching, the observed variations were important to predict differences in the rate of mineral dissolution and possibilities of preferential dissolution of hematite in relation to goethite, promoting the increase of the yellow component with the leaching. Both hematite and goethite have high crystallinity and the isomorphous replacement of Fe by Al is low. Comparing the properties observed in synthetic and natural environments, the hematite and goethite from the Rio Capim kaolin profile have characteristics that relate these minerals to a formation environment in hydromorphic conditions where the influence of organic matter was low, with low iron activity, weakly reduced and acidic conditions. These conditions are found in a saprolitic domain in accordance with the bottom facies of a thick laterite profile. Despite agreeing with a laterite model, differences make it difficult to explain iron depletion by organic matter only (Pirabas Event) and the origin of flint kaolin facies by a subsequent and superimposed laterite period. With the hematite and goethite properties found in this study, it is possible to propose that the Rio Capim kaolin is the bottom facies of a laterite profile formed in the zone permanently below the water table. Contrasting with the upper laterite portion of the profile, the bottom zone is in hydromorphic conditions and allowed the fixation of Al and Si to form kaolinite by primary feldspar and mica minerals of the Ipixuna Formation. This environment promotes the slow depletion of iron without the need of an exceptional accumulation of organic matter. The flint kaolin facies was formed in the same period of the soft kaolin facies and the observed differences in the kaolinite morphology are only related to changes caused by the location of this facies in the intermediate zone characterized by the water table fluctuation, but again without the need of subsequent superimposed lateritic processes.

Orientadores: Marcelo Knobel, Daniela Zanchet / Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Fisica Gleb Wataghin / Made available in DSpace on 2018-08-08T20:01:50Z (GMT). No. of bitstreams: 1 Alves_TatianaMidoriMartinsTelles_M.pdf: 13757564 bytes, checksum: 9fff2bc36efd863f581707b11f77fa22 (MD5) Previous issue date: 2007 / Resumo: Neste trabalho são realizados estudos de propriedades morfológicas, estruturais e magnéticas de nanopartículas de óxidos de ferro sintetizadas por métodos químicos. Procuramos relacionar os parâmetros de síntese às características das partículas produzidas com a finalidade de melhorar sua qualidade em relação às amostras comerciais e avaliar sua aplicabilidade em biomedicina. Foram adotados os métodos de síntese por co-precipitação de sais em solução aquosa e de decomposição térmica de dois diferentes precursores organometálicos: acetilacetonato de ferro III (Fe(acac)3) e ferro pentacarbonil (Fe(CO). Para caracterização desses sistemas, foram utilizadas as técnicas de microscopia eletrônica de transmissão convencional e de alta resolução, microscopia eletrônica de varredura com canhão de emissão de campo, difração de raios-X e medidas de magnetização, além de experimentos de transfecção em células HeLa e posterior detecção por imagens de ressonância magnética. Os estudos mostraram que as partículas sintetizadas por co-precipitação não apresentam muitas vantagens em relação às amostras comerciais, pois possuem larga distribuição de tamanhos. Através da síntese por decomposição térmica de Fe(acac)3, partículas com distribuição mais estreita foram produzidas e resultados positivos de incorporação por células HeLa e detecção por imagens de ressonância magnética foram obtidos. Com as partículas geradas pela decomposição térmica de Fe(CO)5 foram realizados tratamentos térmicos em atmosfera ambiente que proporcionaram aumento do grau de cristalização, aumento do diâmetro médio e estabilização de suas propriedades magnéticas, em detrimento da perda dos contornos esféricos e aumento na dispersão de tamanhos. De uma maneira geral, foi possível demonstrar que a decomposição térmica de compostos organometálicos em solventes orgânicos produz partículas mais homogêneas em relação àquelas produzidas por co-precipitação e às comercialmente disponíveis, e essa qualidade apresenta um grande potencial para aplicações biomédicas mais sofisticadas / Abstract: In this work, morphological, structural and magnetic investigations were performed in iron oxide nanoparticles synthesized by chemical methods. Our goal was to correlate the synthesis parameters to the characteristics of the produced particles to improve their quality when compared to commercial samples and to evaluate their applicability in biomedicine. The synthetic methods were the co-precipitation of metal salts in aqueous solution and the thermal decomposition of two different organometallic precursors: iron (III) acetylacetonate (Fe(acac)3) and iron pentacarbonil (Fe(CO)5). The following techniques were used for the characterization of these systems: transmission electron microscopy, high resolution transmission electron microscopy, field emission gun scanning electron microscopy, X-ray diffraction and magnetic measurements, in addition to incorporation experiments by HeLa cells and their detection by magnetic resonance imaging. The studies showed that nanoparticles synthesized by the co-precipitation method present no advantage over the commercial samples, once they have the same broad size distribution. Through thermal decomposition of Fe(acac)3, particles with narrower size distribution were produced and positive results on their incorporation by HeLa cells and magnetic resonance imaging detection were obtained. Thermal treatments under air atmosphere were performed in the particles generated by thermal decomposition of Fe(CO)5, giving rise to crystallization, an increase of the mean diameter and stabilization of their magnetic properties, with the disadvantages of loss of the spherical shape and increase of the size dispersion. In summary, it was possible to demonstrate that thermal decomposition of organometallic compounds in hot organic solvents produces more homogeneous particles when compared with those produced by co-precipitation and commercially available ones, and this quality presents great potential for more sophisticated biomedical applications / Mestrado / Física da Matéria Condensada / Mestre em Física

The isolation of single layers of van der Waals materials has shown that their properties can be significantly different compared to their bulk counterparts. These observations, illustrates the importance of interface interactions for determining the materials properties even in weakly interacting materials and raise the question if materials properties of single layer van der Waals materials can be controlled by appropriate hetero-interfaces. To study interface effects in monolayer systems, surface science techniques, such as photoemission spectroscopy and scanning probe microscopy/spectroscopy, are ideally suited. However, before these characterization methods can be employed, approaches for the synthesis of hetero-van der Waals systems must be developed, preferably in-situ with the characterization methods, i.e. in ultra-high vacuum. Therefore, in this thesis, we explored novel approaches for creating van der Waals heterostructures and characterized fundamental structural and electronic properties of such systems. Specifically, we developed an approach to decouple graphene from a Ir(111) growth substrate by intercalation growth of a 2D-FeO layer, and we investigate van der Waals epitaxy of MoSe2 on graphite and other transition metal dichalcogenide substrates. For the Ir(111)/2D-FeO/graphene heterostructure system, we first demonstrated the growth of 2D-FeO on Ir(111). The FeO monolayer on Ir(111) exhibits a long range moiré structure indicating the locally varying change of the coordination of the Fe atoms with respect to the substrate Ir atoms. This variation also gives rise to modulations in the Fe2+-O2- separation, and thus in the monolayer dipole. We demonstrated that this structure can be intercalated underneath of graphene grown on Ir(111) by chemical vapor deposition. The modulation of the dipole in the 2D-FeO moiré structure consequently gives rise to a modulated charge doping in the graphene. This effect has been studied by C-1s core level broadening. In general, this study demonstrates that modulated substrates can be used to periodically modify 2D materials. Growth of transition metal dichalcogenides (TMDCs) by molecular beam epitaxy (MBE) is a very versatile approach for growing TMDC heterostructures. However, there may be unforeseen challenges in the synthesis of some of these materials. Here we show that in MBE growth of MoSe2, the formation of twin grain boundaries is very abundant. While this is detrimental in our efforts for characterizing interface properties of TMDC heterostructures, however the twin grain boundaries have exciting properties. Since the twin grain boundaries are aligned in an epitaxial film we were able to characterize their properties by angle resolved photoemission spectroscopy (ARPES), which may be the first time a material’s line defects could be studied by this method. We demonstrate that the line defects are metallic and exhibit a parabolic dispersing band. Because of the 1D nature of the metallic lines, embedded in a semiconducting matrix, the electronic structure follows a Tomonaga Luttinger formalism and our studies showed strong evidence of the predicted so-called spin charge separation in such 1D electron systems. Moreover, a metal-to-insulator Peierls transition has been observed in this system by scanning tunneling microscopy as well as in transport measurements. Finally, we have shown that the defect network that forms at the surface also lends itself for decoration with metal clusters. Although unexpected, the formation of grain boundary networks in MoSe2 marks the discovery of a new material with exciting quantum properties.

The redox cycling of iron is intimately linked to the cycling of C, S, N, P as well as the speciation, mobility, and bioavailability of various toxic contaminants in soils and sediments. Within these environments, the cycling of iron is catalytically driven by iron-oxidizing (FeOB) and iron reducing bacteria (FeRB) which mediate the formation, transformation, and dissolution of various iron-bearing minerals. Under oxic conditions, FeOB promote the formation of iron oxides on or in close proximity of their cell walls and extracellular polymeric substances, and such composite, termed biogenic iron oxides (BIOS), offers highly reactive heterogenous sites that efficiently immobilize trace metals and contaminants alike. However, under reducing conditions, FeRB mediate the reductive dissolution of BIOS and in turn lead to the remobilization of associated contaminants. Conversely, contaminants may become immobilized by secondary iron minerals that form from the metabolic activity of FeRB. Therefore, determining the factors that influence the reactivity of BIOS, as well as the formation of secondary iron minerals is of critical importance to develop a better understanding of the geochemical cycling of iron and in turn the transport of contaminants in the environment. This thesis investigated (1) the impact of simulated diagenesis (ageing for ~5 years at 4ºC) on the mineral stability and reactivity of BIOS towards reduction by Shewanella putrefaciens CN32, (2) the effects of phosphate at an environmentally relevant (10µM) and excess (3.9mM) concentration on the rates and extent of microbial reduction of synthetic 2-line ferrihydrite and BIOS, as well as the formation of secondary iron minerals, and (3) the impact of sterilization by γ-irradiation on the mineral stability and reactivity of BIOS. It was found that simulated diagenesis did not affect the mineralogical composition of BIOS but significantly lowered the reactivity of BIOS towards microbial reduction. The concentration of phosphate was found to have contrasting effects on the rates of reduction of ferrihydrite and BIOS, but in general, excess concentration of phosphate enhanced the extent of Fe(III) reduction. The formation of a specific secondary iron mineral was also found to depend on the concentration of phosphate, as well as, in the case for BIOS, the presence of intermixed cell derived organic matter. γ-irradiation did not alter the mineralogy and reactivity of BIOS towards microbial reduction, and it was concluded to be a suitable technique to sterilize BIOS.

The study of acid rock and mine (ARD and AMD) environments mainly focused on the mineralogical and microbiological conditions and responses of such systems. Most of the research that involved some organic viewpoint was related to the amelioration of the environmental conditions, sometimes with contradictory results. How organic matter (OM) participates and which organic fractions are involved in ARD and AMD processes remain unclear. In this work we have applied organic geochemistry tools combined with mineralogical ad molecular microbiology techniques to study of ARD and AMD environments. The main objectives were to identify and characterise the natural sources of OM occurring both at ARD and AMD sites, and to determine whether the OM sources identified are involved in the generation or amelioration of AMD/ARD. This study shows that multiple OM sources occur naturally in acid drainage environments, included plant derived material and mature, petroleum-derived hydrocarbons, originating from the source rocks, apparently have not directly influence on the processes. This suggests that the generation of ARD and AMD is a completely chemoautotrophic process. Particle size of the iron phases present at ARD sites seems to be involved in the iron bioavailability. The presence of goethite in ARD/AMD systems may have a relationship with the presence of OM. Stimulation of ARD sediments using plant derived OM, abundantly present in and around ARD and AMD ponds systems does not result in the neutralisation of ARD or AMD. This suggests that plant material is not used by Fe(III)-reducing bacteria. However, it fuels fermentation processes and it is likely that fermentation products such as acetate, detected in microcosms and in situ, could limit Fe(III)-reduction. In contrast, the stimulation of ARD sediments using manure (particularly sheep manure) raises the pH up to near neutral conditions. Although it remains unclear which OM fraction from the manure is actively involved in the neutralisation of ARD; these results suggest that manure may make an interesting and non-expensive electron donor in AMD/ARD treatments.

The Nkout (Cameroon) and Putu (Liberia) oxide facies iron ore deposits comprise fresh magnetite banded iron formation (BIF) at depth, which weathers towards the surface, forming high grade martite–goethite ores. This study aimed to improve the mineralogical understanding of these deposits in order to predict their metallurgical responses. It concentrated on developing the QEMSCAN® technique and testing its application to these ore types, but also used a variety of other analysis methods. The QEMSCAN® species identification protocol was developed to include three goethite entries: goethite/limonite, phosphorus-bearing and aluminium-bearing goethite. QEMSCAN® was also used to distinguish between the iron oxides using their backscattered electron signals. To test the correlation between the mineralogy and metallurgical characteristics, magnetic separations were carried out. The samples were divided into 4 main groups based on their whole rock Fe content, determined by XRF analysis, and their degree of weathering: enriched material, weathered magnetite itabirite, transitional magnetite itabirite and magnetite itabirite. Quartz and Al oxide and hydroxide minerals such as gibbsite are the major gangue minerals in the magnetite BIF and martite–goethite ores respectively. From the QEMSCAN® analysis it was concluded that the iron oxides are closely associated and liberation of them individually is poor. Liberation increases when they are grouped together as iron oxide. Chamosite concentrations > 6 wt. % significantly lower liberation of the iron oxides. From the metallurgical testing, it was concluded that iron oxide modal mineralogy gives an indication of iron recovery but other QEMSCAN® data such as mineral association and liberation could be important especially if the iron oxide minerals are not liberated. Grain size and instrument characteristics also affect recovery of iron minerals. There is no evidence to show that there is any structural control on the BIF mineralisation at Nkout because metamorphism has significantly affected the lithological characteristics. The BIF mineralised zones occur as stacks with no particular stratigraphic relationship. Alteration and stratigraphy are the main controls on the martite–goethite ores. These results are applicable to most other BIFs so that as direct shipping ores are exhausted, the approach used here can help to develop the lower grade portions of the deposits.

Há poucos estudos sobre a influência da mineralogia no comportamento do solo em relação aos atributos de resistência física. Neste sentido, o estudo tem como hipótese que independentemente do potencial matricial de água no solo a composição mineralógica da fração argila interfere na pressão de préconsolidação, modificando a capacidade de suporte de carga dos solos. Assim, objetivou-se caracterizar a composição mineralógica de classes de solos representativas no Rio Grande do Sul; Determinar parâmetros físico-mecânicos dos solos; E estabelecer correlações entre parâmetros físico-mecânicos com mineralógicos melhorando o entendimento da capacidade de suporte de carga. Para tal, foram selecionados sete solos de duas classes de solos; três Argissolos e quatro Latossolos. As amostras deformadas e indeformadas foram coletadas sob vegetação natural na camada de 10 a 15 cm de profundidade. Na fração TFSA, foram realizadas análises físicas (granulometria e área superficial específica), químicas (carbono orgânico total, teor de óxidos de ferro pedogênicos e óxidos de baixa cristalinidade) e mineralógicas (difratometria de raio x e refletância difusa). Nas amostras indeformadas foram realizadas as análises de permeabilidade ao ar e o ensaio de compressão uniaxial. Os dados foram analisados por correlações de Pearson. Os solos avaliados possuem a caulinita como principal mineral da fração argila, no entanto diferenças com relação aos óxidos de ferro foram encontradas, os quais correlacionaram com a pressão de pré-consolidação. A hematita influenciou positivamente sobre a pressão de pré-consolidação à 100 kPa, assim, dependendo do potencial matricial de água no solo. / There are few studies on the influence of mineralogy on the ground behavior in relation to physical resilience attributes. The is study has hypothesized that regardless of the matric potential of soil water the mineralogical composition of the clay fraction interferes with the pre-consolidation pressure by modifying the soil bearing capacity. Therefore, this study aimed to characterize the mineralogical composition of representative soil classes in Rio Grande do Sul; determine physical-mechanical parameters of the soil; and establish correlations between physico-mechanical parameters mineralogical improving the understanding of the load-bearing capacity. To this end, it was selected seven soils of two soil classes; three Ultisols and four Oxisols. The disturbed and undisturbed samples were collected under natural vegetation in the layer from 10 to 15 cm deep. In TFSA fraction, physical analyzes were performed (particle size and specific surface area), chemical (total organic carbon content of pedogenic iron oxides and low crystallinity oxides) and mineralogical (x ray diffraction and diffuse reflectance). In undisturbed soil samples were carried out air permeability tests and uniaxial compression test. Data were analyzed by Pearson correlations. The evaluated soils have kaolinite as the main mineral of the clay fraction, however differences with respect to iron oxides were found, which correlated with the pressure of pre-consolidation. The hematite had a positive effect on the pre-consolidation pressure of 100 kPa, thus depending on the matric potential of soil water.

Title: NMR in magnetic systems Author: Petr Křišťan Department: Department of Low Temperature Physics Supervisor: prof. RNDr. Helena Štěpánková, CSc. Abstract: Magnetically ordered iron oxides, namely magnetite, maghemite, hexagonal ferrite M or system Fe-B, with nano or submicron dimensions of particles are the main subject of study of the presented thesis. The materials were investigated mainly by 57 Fe nuclear magnetic resonance (NMR). The results were thoroughly analyzed and compared with the results obtained by other methods (Mössbauer spectroscopy, ZFC/FC magnetic measurement, X-ray diffraction or TEM). In case of the maghemite nanoparticles a regular distribution of vacancies in octahedral positions was verified by the help of NMR in external magnetic fields and at various temperatures. The experi- mental results were also compared with ab-initio calculations. In thin layers of barium M type hexaferrite, effects of reduced particle size on 57 Fe NMR spectra were observed. The NMR methods were also successfully applied to investigation of system FeMoCuB of amorphous and nanocrystalline ribbons, where 57 Fe NMR was able to resolve formation of different phases in depen- dence on the process of preparation. Due to different NMR excitation condi- tions of signal from strontium M type hexaferrite and maghemite,...

No description available.