523 resultados para Argila organofílica
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Neste trabalho são apresentados os resultados de caracterização das principais argilas usadas pela indústria cerâmica vermelha regional e, também, de alguns resíduos sólidos produzidos na região de Presidente Prudente - SP. Os resultados da incorporação destes resíduos em massas cerâmicas são avaliados através do estudo de suas propriedades tecnológicas. Para a caracterização dos materiais foram utilizadas as seguintes técnicas: análise textural (concentração das frações areia, silte e argila), difratometria de raios X e análise térmica. As propriedades tecnológicas de corpos de prova cerâmicos foram avaliadas através dos seguintes parâmetros: retração linear (RL), perda de massa ao fogo (PF), massa específica aparente (MEA), porosidade aparente (PA), absorção de água (AA) e resistência mecânica à flexão (RMF). Corpos de prova, com diferentes concentrações de resíduos, foram prensados (prensa uniaxial manual) e queimados em temperaturas que variaram de 800 a 1200 oC, usando um forno tipo mufla com controle de temperatura. As argilas sedimentares foram coletadas nas margens do rio Paraná e em áreas de várzea, próximas as cerâmicas. As amostras estudadas, coletadas nos depósitos das cerâmicas, são usadas para produção de tijolos maciços, blocos furados e telhas. Quatro tipos diferentes de resíduos foram estudados: (1) lodo de estação de tratamento de água ETA, (2) torta de filtro de indústria de re-refino de óleo lubrificante, (3) pó de vidro (soda-cal) de garrafa tipo long neck descartável, e (4) cinza de bagaço de cana. Estes resíduos foram incorporados em massas cerâmicas coletadas nas indústrias... (Resumo completo, clicar acesso eletrônico abaixo)
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The main goal in this research is a tectono-estructural characterization of the Cherne, Albacora and Namorado Fields, located at Campos Basin, in order to investigate the relationship between the geologic evolution and the rock´s physical properties of the reservoir, and how they affect the hydrocarbon accumulation in those fields. Well correlations show that the inferior turbidites have a regional lateral continuity. Basic petrophysics analysis, calculated here, shows that the three fields present porosity values that range from 15 to 20%, shale volume range from 26 to 30% and formation water saturation range from 23 to 45%, based on formation water resistivity dada from Albacora Field. Petrophysics maps feature a trend in Albacora Field that increase the porosity values to SE, and in Cherne and Namorado Field the trend increase towards N. Seismic horizons where interpreted between the first appearance of the Namorado Sandstone and the top of Quissamã Formation. This interval presents normal listric faulting, in Cherne and Namorado Field with NWSE and NE-SW direction, and sedimentation trend to NW-SE, in Albacora Field the faulting presents a NNE-SSW and N-S direction, with a sedimentation trend to NE-SW. Seismic attribute maps present amplitude anomalies close to the producing wells, and on Namorado Field, it indicates a potential hydrocarbon accumulation in the NE region. For each field is indicated laboratory tests for a better characterization of the petrophysical properties, since that they don’t form the same reservoir level, therefore, not influencing the water saturation calculation
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This study aimed the geological characterization at scale 1:50.000 of an area belonging to the southern sector of the Brasilia Belt, located in the western portion of the Passos Nappe, near the town of Cássia, MG. In this region, outcrops rock types belonging to Araxá Group, composed of metasediments associated with metavolcanics which form a tectonometamorphic terrain of great importance for understanding the geological evolution of southeast and midwest regions of Brazil. With the development of work was possible to group the rocks in 10 lithostratigraphic units and had been identified 3 different zones of metamorphism generated during the peak metamorphism. The structural pattern of the area shows that the main foliation has average dip 30 ° NW and mineral lineation parallel to the stretching direction with 290 °. Still, we can conf irm that this inverse gradient metamorphic rocks of the Passos Nappe, described by several authors. Also, were seen lithotypes of economic interest, some already in exploitation, such as clay and sand, and other mineral commodities, which are occurring and can be used: quartz, quartzite, garnet, kyanite, rutile and zircon.
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This work presents a proposal to create a Polo Ceramic Craft in the town of Indiana - SP, through the potter’s organization in a cooperative that will coordinate activities to add value to ceramic pieces. To achieve this, two things are essential: improving the ceramic body and improve the properties of the ceramic material. For the first action it’s necessary to create a Central Mass Production of Ceramics, to provide raw materials and homogeneous composition that results in differentiated ceramic after burning process (sintering). To this end, we propose the incorporation of additives (which act as fluxes) to the clay material. These additives can be mineral such as feldspar and nefelinas or leavings, such as glass powder obtained from disposable containers. For the second action is necessary to acquire an oven, electric or gas, it reaches higher temperatures (around 1200 ° C). The presence of the additive and burning at higher temperatures will enable better production of sintered ceramic material with less porosity and water absorption and higher mechanical strength, and pieces vitrified and glazed, allowing them to assign a higher value. For the production of these materials (thinner walls) requires a smaller volume of clayey raw materials. Besides benefiting the ceramic pieces, the proposed changes reduce the environmental impact caused by burning wood, since it will be replaced by natural gas (or electricity), and even will reduce the disposal of glass containers in the environment by recycling and incorporating this material in the clay. From a social standpoint, the cooperative is crucial to the viability of the proposed project, to coordinate activities and commercial production, which will result in better wages and profits for companies and consequently for the city and its population
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Of the four lacustrine deltaic models, which were found in the Pendência formation, two are represented in the Serraria field. Respectively the deltaic models 1 and 3 shows the reservoir zones A and B. The Zone A is divided into six sub-areas. Each is representing a smaller cycle of development of sigmoidal lobes of deltaic front. Zone B produces in reservoirs of Model 3, or so called Full delta. The Zone B is formed by overlapping the deltaic plain system over the deltaic/prodeltaic front (model 1). This work uses the method of zooming with the aim to contextualize the geometric aspects of the sand bodies, highlighting the analysis of facies and diagenesis with help of pictures and testimonies of thin sections. The sigmoidal lobes of Zone A are fine to very fine sandstones, well sorted, with a arcosian composition.;practically with a weak compaction and cementation of a kind of film of clay (if very fine) and overgrowth feldspar (fine texture). This silicate phases are succeeded by cementation of poiquilotópica calcite, and after this a stage of dissolution, containing only regular permoporosity for this reservoir. Zone B has a combination of two types of deltaic plain reservoir. One is the rarest of distributary channel and the other the most common of lobes of crevasse. In the channel coarse to medium-grained and poor to moderate sorted sandstones are formed (tuning up), and with a lytic arcosiana nature. Rarely there are cements, including growth of feldspar and rhombohedral dolomite, which prevent a high permoporosity of the reservoir. In the crevasse lobes, the sandstones are laminated, fine and well sorted, arkosic, rarely with overgrowth feldspar and calcite poiquilotópica, and with a good intergranular permoporosity
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In the present study it was investigated, in plant and population scale, the relationship between the amount of resource and body size, species diversity and abundance and biomass of bruchids and their parasitoids. Possible effects of resource quality (soil quality and concentration of tannins in seeds) in response to the variables mentioned above were also analyzed. Mimosa bimucronata fruits were collected in two areas during the occurrence of bruchids during the years 2009 and 2010. Only the species of bruchid Acanthoscelides schrankiae was found infesting the fruits of M. bimucronata. The parasitoids belong to families Braconidae, Encyrtidae, Eulophidae, Eupelmidae, Eurytomidae and Pteromalidae. Most local-level analysis showed no significant results for both years of collection and study areas. There was only significant result for the relationship between the biomass of parasitoids and the concentration of tannins considering the year 2009 (negative trend). The soil from Lageado showed higher percentages of silt and clay. With respect to chemical analysis, pH, cation exchange capacity, and concentrations of organic matter, potassium, calcium and magnesium were all significantly higher in soil from Lageado. Therefore, it was found that the plants from Lageado are growing in more fertile soils. However, it was found that the amount of fruits and seeds was significantly higher in Rubião. Comparisons of the abundance of bruchids and parasitoids diversity among the areas that showed the highest values were observed in Rubião. In this study it was found that the abundance of bruchids and parasitoids, as well as the diversity of parasitoids was greatest in the area that had higher amounts of fruits and seeds, suggesting a significant relationship between the amount of resources and the abundance and diversity. However, it is possible that ...(Complete abstract click electronic access below)
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Os Isoptera são insetos sociais cujas colônias apresentam diversas castas, as quais têm um rígido sistema de divisão de trabalho que visa otimizar a eficiência da colônia. Estas castas apresentam morfologia específica, que capacita estes indivíduos a desenvolverem determinadas tarefas com eficiência. Os cupins apresentam aparelho bucal mastigador, constituído pelas seguintes peças bucais: labro, mandíbulas, maxilas, lábio, epifaringe e hipofaringe. Sua dieta alimentar é celulósica e bastante variada, sendo que estes insetos podem se alimentar de madeira (em vários estágios de decomposição), gramíneas, plantas herbáceas, serapilheira, fungos, líquens, partes de artrópodes e húmus. O estudo desse tipo de dieta é muito difícil, uma vez que o material já se encontra bastante decomposto antes de ser ingerido pelo animal. Cornitermes cumulans é uma espécie de cupim nativa do Cerrado brasileiro, pertencente à família Termitidae, subfamília Syntermitinae, que constrói ninhos em montículos, ricos em argila, que podem atingir até 4 metros de altura. Na parte interna dos ninhos, pode-se observar galerias grandes e de aspecto arredondado e um centro celulósico de coloração escura, de textura lisa e pouco resistente, onde os cupins armazenam um alimento, que parece ser previamente mastigado e depois regurgitado. Mesmo com a grande ocorrência desta espécie de cupim nas áreas de pastagens, seus verdadeiros hábitos alimentares são ainda pouco conhecidos. As informações disponíveis são contraditórias, uma vez que não está esclarecido a qual grupo funcional C. cumulans pertence e se existe realmente uma alimentação “in situ” desta espécie no campo. Em vista do exposto, este estudo teve como objetivo geral esclarecer o hábito alimentar de C. cumulans e a natureza química do alimento armazenado no ninho para compará-lo com o alimento coletado pelos... (resumo completo, clicar acesso eletrônico abaixo)
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The environmental diagnosis of any area affected for mining activities contributes in a positive form for the analysis of the characteristics of the environment, biological and social, thus being able to establish control parameters. The clay extration for red ceramics promotes the environment degradation as any another one cultivates of mineral goods, but in lesser scale, which had to the dimensions of potteries. Being thus, some decurrent environment characteristics of the clay extration had been inquired clearly used for potteries located in the city of Rio Claro, SP. For this, the followed method was the cadastre of these areas and potteries in created tables, searching, with this, the contribution for the involved people in the extract activity of related potteries and the facilitation in the visualization of the main problems, necessities and proposals for each one. It could be perceived that the environmental diagnosis of the areas had in common presented referring points to the places where if they find the activities. The same ones are located in the region the northwest of Rio Claro and well next one to the others. Moreover, they have in common, referring characteristics to the process of manufacture of bricks. In common, all the responsibility for the administration and course of the activities competes to the proper families, since the administrative part, even though to the process of manufacture of the bricks. Moreover, from the comment of the areas through field work, the prominent use of diverse areas in the region for the clay extration is noticed, making with that the region has great importance in the regional scene.
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A importância da agroecologia se dá no sentido de fornecer e ser, base e estrutura de conhecimentos mesclados, incorporando saberes tradicionais aos saberes técnicos científicos atuais, sem excluir ou rejeitar, mas usando ambos a favor da transição para uma pratica agrícola mais sustentável e coerente com os fluxos e com a complexidade natural de um ecossistema, o que não se percebe nas práticas agrícolas modernas e convencionais. Inúmeros estudos constataram que para uma boa efetividade de sistemas agroecológicos é necessário recuperar e manter o equilíbrio biológico do solo, pois isso influenciará em suas características físicas e químicas. O objetivo desse trabalho foi de caracterizar o solo sob Sistema Agroflorestal (SAF) e uma Pastagem, no município de Rio Claro (SP), para a obtenção de atributos do solo, morfológicos, físicos e químicos e também descrever a diversidade do extrato arbóreo presente na área, incluindo as espécies agrícolas, e levantar o histórico de implantação do sistema, de modo a criar e dar início a formação de um banco de dados científicos para o Grupo de Extensão Gira-Sol. Foram escolhidos dois perfis nas seguintes situações: sistema agroflorestal e uma Pastagem para descrição morfológica do solo. Em cada área foi efetuada a coleta de amostras deformadas e indeformadas e caracterizados os atributos granulometria, analises química, densidade do solo, porosidade do solo e resistência à penetração. Para a descrição morfológica dos perfis foi utilizado os procedimentos descritos por Lemos e Santos (2002), para os atributos químicos e de fertilidade do solo, Camargo et al. (1986) e EMBRAPA (1997), para granulometria, densidade e porosidade do solo e argila dispersa em água. A descrição da vegetação foi feita com auxilio de guias de identificação e por meio de parcelas, onde as espécies foram tabeladas e plotadas em um mapa da área para localização das mesmas, e.
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Pós-graduação em Agronomia (Ciência do Solo) - FCAV
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Pós-graduação em Agronomia (Ciência do Solo) - FCAV
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Pós-graduação em Agronomia (Ciência do Solo) - FCAV
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Pós-graduação em Química - IBILCE
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Pós-graduação em Ciência dos Materiais - FEIS
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)