Thesis (Ph. D.)--Ohio State University, 2005. / Title from first page of PDF file. Includes bibliographical references (p. 152-160).

Resumo: Os atributos mineralógicos e físicos possuem dependência espacial e a distribuição espacial destes atributos possui relação com as formas do relevo. O objeto deste trabalho foi avaliar os atributos mineralógicos da fração argila e os atributos físicos de um argissolo em curvaturas do relevo, assim como avaliar a correlação entre esses atributos. Uma malha de dimensão 100 x 100 m foi delimitada em uma área caracterizada pela forma convexa e outra pela fôrma côncava. As malhas possuem espaçamento regular de 10 x 10 m e os pontos de cruzamento deste espaçamento determinaram os pontos de coleta das amostras, num total de 121 pontos amostrais georreferenciados em cada malha. Os atributos físicos foram avaliados nas profundidades 0,0- 0,2 e 0,2-0,4 m e os atributos mineralógicos na profundidade 0,0- 0,2 m. Os atributos físicos analisados foram diâmetro médio ponderado, diâmetro médio geométrico, agregados maiores que 2 mm, agregados entre 2 e 1 mm , agregados menores que 1 mm, microporos, macroporos, volume total de poros, densidade do solo, resistência do solo à penetração e teor de água no solo, já os atributos mineralógicos da fração argila foram largura a meia altura, diâmetro médio do cristal dos óxidos de ferro, da caulinita e gibbsita, substituição isomórfica e área de superfície específica da hematita e goethita. Os teores da goethita e hematita e razão goethita/(goethita+hematita) e razão caulinita/(caulinita+gibbsita) também foram calculados. Os dados foram submetidos às análises estatísticas e geoestatísticas para avaliação da variabilidade espacial e influência das curvaturas nestes atributos. Para avaliação da relação entre os atributos da mineralogia e físicos realizaram-se as análises de correlação simples e espacial. Os atributos físicos e mineralógicos apresentaram-se dependentes das curvaturas do relevo... (Resumo completo, clicar acesso eletrônico abaixo) / Abstract: The mineralogicals and physical attributes have spatial dependence and the distribution of these attributes has relation with the forms of relief. The object of this study was to evaluate the attributes of clay mineralogy and the physical attributes of an argissol in curvatures of relief, as well as assess the correlation between these attributes. A grid size of 100 x 100 meters was defined in an area characterized by the convex shape and another in an area characterized by the concave shape. The grids have regular spacing of 10 x 10 m and the spacing of the points of intersection determine the points of collection of samples, a total of 121 georeferenced sample points in each grid. The physical attributes were evaluated in depth from 0.0 - 0.2 and 0.2 -0.4 m and the mineralogical attributes in depth 0,00-0,20 m. The physical attributes were analyzed: mean weight diameter, mean geometric diameter, aggregates larger than 2 mm, aggregates between 2 and 1 mm, aggregates smaller than 1 mm, microporosity, macroporosity, total porosity, bulk density, penetration resistance and water content in soil. The attributes of minerals were: width at half height, average diameter of crystals of iron oxides and kaolinite and gibbsite and isomorphic substitution and specific surface area of hematite and goethite. The contents of goethite and hematite and ratio goethite / (goethite + hematite) [Gt / (Gt + Hm)] and ratio kaolinite / (kaolinite + gibbsite) [Ct / (Ct + Gb)] were also calculated. Data were subjected to statistical and geostatistical analysis to evaluate the spatial variability and influence of these curvatures on these attributes. To assess the relation between mineralogy and physical attributes simple and spation correlation analysis where made. The physical and mineralogical attributes and depend on the curvature of the relief. There was also the influence of crystallinity of goethite and gibbsite in soil physical. / Orientador: José Marques Júnior / Coorientador: Gener Tadeu Pereira / Banca: Marcílio Vieira Martins Filho / Banca: Zigomar Menezes de Souza / Mestre

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.

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.

Made available in DSpace on 2015-04-09T12:28:14Z (GMT). No. of bitstreams: 0 Previous issue date: 2014-02-24Bitstream added on 2015-04-09T12:47:54Z : No. of bitstreams: 1 000812392.pdf: 1487689 bytes, checksum: e155f277ba7975354c26851aa72d038f (MD5) / Considerando a carência de informações referentes aos diversos ambientes amazônicos, o estudo dos atributos do solo e seu comportamento diante das ações antrópicas sofridas durante o manejo são muito importantes na região sul do Amazonas. Neste sentido, o objetivo deste estudo foi à caracterização de atributos do solo em ambientes na região sul do estado do Amazonas. Neste estudo foram realizadas coletas de solos em seis trincheiras de diferentes locais e manejos em solos de Terra Preta Arqueológica (TPA) onde foi feita a sua caracterização e classificação. Em seguida, foram montadas cinco malhas na região sul do Amazonas sendo elas compostas de floresta, TPA, agrofloresta, mandioca e cana-de-açúcar. Foram feitas medidas da emissão de CO2, temperatura e umidade do solo, onde foram caracterizadas pontualmente e também realizadas análises físicas e químicas do solo. Foram realizados teste de média, análises estatísticas descritivas, geoestatística e análise multivariada nos dados obtidos. Verificou-se nos atributos físicos e químicos comportamento similar nos perfis estudados. Concluiu-se que a hematita e goethita determinados por difração de raio-x e espectroscopia de reflectância difusa além de não apresentarem variações importantes entre os solos estudados, apresenta características similares aos solos não antropizados brasileiros. A cor medida por espectroscopia de reflectância difusa mostrou-se eficiente para indicar variações entre as TPAs estudadas, provando ser uma técnica inovadora, eficiente e promissora para a quantificação indireta dos atributos do solo de forma simples e de baixo custo. A caracterização dos atributos físicos, químicos e biológicos em ambientes antropizados, na região sul do Amazonas, mostrou que os ambientes mandioca e cana-de-açúcar são os que mais se aproximam do ambiente natural Floresta. Assim, os manejos que mais contribuíram para o aumento da ... / Considering the lack of information regarding the different Amazonian environments, the study of soil properties and their behavior in the face of human actions incurred during handling are very important in southern Amazonas. In this sense, the objective of this study is the characterization of soil environments in the southern state of Amazon. In this study soil samples were taken in six different locations of trenches and managements in archaeological black earth soils (ABE) where it has been the characterization and classification. Then were assembled five stitches in southern Amazon them being composed of forest, ABE, agroforestry, cassava and sugar cane. Measurements of CO2, temperature and soil moisture, which were characterized punctually and also performed physical and chemical soil analyzes were made. Mean test, descriptive statistical analyzes, geostatistics and multivariate analyzes were performed on data obtained. It was concluded that hematite and goethite determined by x-ray diffraction and diffuse reflectance spectroscopy in addition to not having significant variations between the soils, shows similar uncontaminated soil anthropogenic Brazilian characteristics. The measured color by diffuse reflectance spectroscopy has been successful to indicate variations between ABE studied, proving to be a novel, effective and promising for indirect quantification of soil properties in a simple and low cost technique. The characterization of physical, chemical and biological attributes in anthropogenic environments in the southern Amazon region, showed that cassava environments and cane sugar are those that come closest to the natural environment Forest. Thus, managements that most contributed to the increased variability of attributes in relation to natural variability of forest and agroforestry were ABE

Made available in DSpace on 2014-06-11T19:28:32Z (GMT). No. of bitstreams: 0 Previous issue date: 2009-02-18Bitstream added on 2014-06-13T20:37:31Z : No. of bitstreams: 1 camargo_la_me_jabo.pdf: 1106150 bytes, checksum: d8d5b3f2596351c9b11f923ae4b5fc44 (MD5) / Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) / Os atributos mineralógicos e físicos possuem dependência espacial e a distribuição espacial destes atributos possui relação com as formas do relevo. O objeto deste trabalho foi avaliar os atributos mineralógicos da fração argila e os atributos físicos de um argissolo em curvaturas do relevo, assim como avaliar a correlação entre esses atributos. Uma malha de dimensão 100 x 100 m foi delimitada em uma área caracterizada pela forma convexa e outra pela fôrma côncava. As malhas possuem espaçamento regular de 10 x 10 m e os pontos de cruzamento deste espaçamento determinaram os pontos de coleta das amostras, num total de 121 pontos amostrais georreferenciados em cada malha. Os atributos físicos foram avaliados nas profundidades 0,0- 0,2 e 0,2-0,4 m e os atributos mineralógicos na profundidade 0,0- 0,2 m. Os atributos físicos analisados foram diâmetro médio ponderado, diâmetro médio geométrico, agregados maiores que 2 mm, agregados entre 2 e 1 mm , agregados menores que 1 mm, microporos, macroporos, volume total de poros, densidade do solo, resistência do solo à penetração e teor de água no solo, já os atributos mineralógicos da fração argila foram largura a meia altura, diâmetro médio do cristal dos óxidos de ferro, da caulinita e gibbsita, substituição isomórfica e área de superfície específica da hematita e goethita. Os teores da goethita e hematita e razão goethita/(goethita+hematita) e razão caulinita/(caulinita+gibbsita) também foram calculados. Os dados foram submetidos às análises estatísticas e geoestatísticas para avaliação da variabilidade espacial e influência das curvaturas nestes atributos. Para avaliação da relação entre os atributos da mineralogia e físicos realizaram-se as análises de correlação simples e espacial. Os atributos físicos e mineralógicos apresentaram-se dependentes das curvaturas do relevo... / The mineralogicals and physical attributes have spatial dependence and the distribution of these attributes has relation with the forms of relief. The object of this study was to evaluate the attributes of clay mineralogy and the physical attributes of an argissol in curvatures of relief, as well as assess the correlation between these attributes. A grid size of 100 x 100 meters was defined in an area characterized by the convex shape and another in an area characterized by the concave shape. The grids have regular spacing of 10 x 10 m and the spacing of the points of intersection determine the points of collection of samples, a total of 121 georeferenced sample points in each grid. The physical attributes were evaluated in depth from 0.0 - 0.2 and 0.2 -0.4 m and the mineralogical attributes in depth 0,00-0,20 m. The physical attributes were analyzed: mean weight diameter, mean geometric diameter, aggregates larger than 2 mm, aggregates between 2 and 1 mm, aggregates smaller than 1 mm, microporosity, macroporosity, total porosity, bulk density, penetration resistance and water content in soil. The attributes of minerals were: width at half height, average diameter of crystals of iron oxides and kaolinite and gibbsite and isomorphic substitution and specific surface area of hematite and goethite. The contents of goethite and hematite and ratio goethite / (goethite + hematite) [Gt / (Gt + Hm)] and ratio kaolinite / (kaolinite + gibbsite) [Ct / (Ct + Gb)] were also calculated. Data were subjected to statistical and geostatistical analysis to evaluate the spatial variability and influence of these curvatures on these attributes. To assess the relation between mineralogy and physical attributes simple and spation correlation analysis where made. The physical and mineralogical attributes and depend on the curvature of the relief. There was also the influence of crystallinity of goethite and gibbsite in soil physical.

Thesis submitted in fulfilment of the requirements for the degree of Masters of Technology: Chemical Engineering in the Faculty of Engineering Cape Peninsula University of Technology, South Africa Supervisor: Prof TV Ojumu Cape Town Campus September 2013 / Jarosite formation is regarded as undesirable in the bioleaching processes as it depletes ferric reagent; a critical reagent for the oxidation of most sulphide minerals, from bioleach solution. It creates kinetic barriers and clogs on mineral surfaces, thereby retarding leach rates of most minerals. However, jarosite has also been shown to serve as support for the attachment of bioleaching microbes, facilitating a high ferric-iron generation rate. In this study, a series of experiments on microbial ferrous-iron oxidation by a mesophilic microbe were carried out in a novel packed-column bioreactor with a view to investigating the potential use of solution pH to manage jarosite accumulation in the bioreactor. The kinetics of the oxidation was also investigated to establish base case data for the novel bioreactor. The bioreactor was packed with glass balls 15 mm in diameter. The experiments were conducted at a constant temperature of 38.6 °C, residence time of 18 hrs, airflow rate of 20 mL.s-1 and at desired solution pHs (1.3, 1.5 and 1.7). The results showed that the amount of jarosite accumulation is proportional to the operating solution pH and also to the duration of operation of the bioreactor. Jarosite precipitate of 4.95, 5.89 and 7.08 g.L-1 were obtained after 10 days of continuous operation at solution pH of 1.3, 1.5 and 1.7 respectively, while after 15 days the precipitate concentration increased to 5.50, 7.90 and 9.98 g.L-1respectively. The results also showed that a 33% and 52% reduction in jarosite accumulation could be achieved by a gradual decrease of the bioreactor solution pH after being continuously operated for 10 days from pH 1.7 to 1.5 and pH 1.7 to 1.3, respectively, for an additional five days of continuous operation. The results of the ferrous-iron biooxidation kinetics investigated at pH 1.3 show a maximum ferrous oxidation rate ( max 2 Fe r ) of 6.85 mmol.L-1.h-1 and apparent affinity kinetics constants (   2 Fe K , 2 Fe K ) of 0.001 mmol Fe2+.L-1 and 0.006 (dimensionless) using Hansford and Monod equations, respectively. Although a direct relationship exists between jarosite formation and solution pH, the results of this study may be relevant in bioleach heaps, or at least in column bioreactors, to manage and control jarosite accumulation, thereby improving leach kinetics of sulphide minerals.

Thesis submitted in fulfilment of the requirements for the degree of Masters of Technology: Chemical Engineering in the Faculty of Engineering Cape Peninsula University of Technology, South Africa, 2013 / Jarosite formation is regarded as undesirable in the bioleaching processes as it depletes ferric reagent; a critical reagent for the oxidation of most sulphide minerals, from bioleach solution. It creates kinetic barriers and clogs on mineral surfaces, thereby retarding leach rates of most minerals. However, jarosite has also been shown to serve as support for the attachment of bioleaching microbes, facilitating a high ferric-iron generation rate. In this study, a series of experiments on microbial ferrous-iron oxidation by a mesophilic microbe were carried out in a novel packed-column bioreactor with a view to investigating the potential use of solution pH to manage jarosite accumulation in the bioreactor. The kinetics of the oxidation was also investigated to establish base case data for the novel bioreactor. The bioreactor was packed with glass balls 15 mm in diameter. The experiments were conducted at a constant temperature of 38.6 °C, residence time of 18 hrs, airflow rate of 20 mL.s-1 and at desired solution pHs (1.3, 1.5 and 1.7). The results showed that the amount of jarosite accumulation is proportional to the operating solution pH and also to the duration of operation of the bioreactor. Jarosite precipitate of 4.95, 5.89 and 7.08 g.L-1 were obtained after 10 days of continuous operation at solution pH of 1.3, 1.5 and 1.7 respectively, while after 15 days the precipitate concentration increased to 5.50, 7.90 and 9.98 g.L-1respectively. The results also showed that a 33% and 52% reduction in jarosite accumulation could be achieved by a gradual decrease of the bioreactor solution pH after being continuously operated for 10 days from pH 1.7 to 1.5 and pH 1.7 to 1.3, respectively, for an additional five days of continuous operation. The results of the ferrous-iron biooxidation kinetics investigated at pH 1.3 show a maximum ferrous oxidation rate ( max 2 Fe r ) of 6.85 mmol.L-1.h-1 and apparent affinity kinetics constants (   2 Fe K , 2 Fe K ) of 0.001 mmol Fe2+.L-1 and 0.006 (dimensionless) using Hansford and Monod equations, respectively. Although a direct relationship exists between jarosite formation and solution pH, the results of this study may be relevant in bioleach heaps, or at least in column bioreactors, to manage and control jarosite accumulation, thereby improving leach kinetics of sulphide minerals.

Orientador: José Marques Junior / Coorientador: Milton Cesar Costa Campos / Banca: Marcílio Vieira Martins Filho / Banca: Rafael Montanari / Resumo: Considerando a carência de informações referentes aos diversos ambientes amazônicos, o estudo dos atributos do solo e seu comportamento diante das ações antrópicas sofridas durante o manejo são muito importantes na região sul do Amazonas. Neste sentido, o objetivo deste estudo foi à caracterização de atributos do solo em ambientes na região sul do estado do Amazonas. Neste estudo foram realizadas coletas de solos em seis trincheiras de diferentes locais e manejos em solos de Terra Preta Arqueológica (TPA) onde foi feita a sua caracterização e classificação. Em seguida, foram montadas cinco malhas na região sul do Amazonas sendo elas compostas de floresta, TPA, agrofloresta, mandioca e cana-de-açúcar. Foram feitas medidas da emissão de CO2, temperatura e umidade do solo, onde foram caracterizadas pontualmente e também realizadas análises físicas e químicas do solo. Foram realizados teste de média, análises estatísticas descritivas, geoestatística e análise multivariada nos dados obtidos. Verificou-se nos atributos físicos e químicos comportamento similar nos perfis estudados. Concluiu-se que a hematita e goethita determinados por difração de raio-x e espectroscopia de reflectância difusa além de não apresentarem variações importantes entre os solos estudados, apresenta características similares aos solos não antropizados brasileiros. A cor medida por espectroscopia de reflectância difusa mostrou-se eficiente para indicar variações entre as TPAs estudadas, provando ser uma técnica inovadora, eficiente e promissora para a quantificação indireta dos atributos do solo de forma simples e de baixo custo. A caracterização dos atributos físicos, químicos e biológicos em ambientes antropizados, na região sul do Amazonas, mostrou que os ambientes mandioca e cana-de-açúcar são os que mais se aproximam do ambiente natural Floresta. Assim, os manejos que mais contribuíram para o aumento da ... / Abstract: Considering the lack of information regarding the different Amazonian environments, the study of soil properties and their behavior in the face of human actions incurred during handling are very important in southern Amazonas. In this sense, the objective of this study is the characterization of soil environments in the southern state of Amazon. In this study soil samples were taken in six different locations of trenches and managements in archaeological black earth soils (ABE) where it has been the characterization and classification. Then were assembled five stitches in southern Amazon them being composed of forest, ABE, agroforestry, cassava and sugar cane. Measurements of CO2, temperature and soil moisture, which were characterized punctually and also performed physical and chemical soil analyzes were made. Mean test, descriptive statistical analyzes, geostatistics and multivariate analyzes were performed on data obtained. It was concluded that hematite and goethite determined by x-ray diffraction and diffuse reflectance spectroscopy in addition to not having significant variations between the soils, shows similar uncontaminated soil anthropogenic Brazilian characteristics. The measured color by diffuse reflectance spectroscopy has been successful to indicate variations between ABE studied, proving to be a novel, effective and promising for indirect quantification of soil properties in a simple and low cost technique. The characterization of physical, chemical and biological attributes in anthropogenic environments in the southern Amazon region, showed that cassava environments and cane sugar are those that come closest to the natural environment Forest. Thus, managements that most contributed to the increased variability of attributes in relation to natural variability of forest and agroforestry were ABE / Mestre

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.