Contribuição ao beneficiamento de finos de fosfatos

Foram estudadas as características de floculação da hidro-xiapatita, calcita e quartzo com poliacrilamidas aniônicas. Tanto as suspensões de hidroxiapatita como a calcita foram completamente floculadas enquanto que o quartzo foi refratário a floculação com esses polimeros. Entretanto, observou-se que a floculação da calcita foi impedida com a utilização de um poliacrilato de sódio, enquanto que a hidroxiapatita continuou a ser floculada pela poliacrilamida num intervalo de concentração de O a 1000 g/ton de poliacrilato. Estes resultados permitiram estabelecer condições para a floculação seletiva de hidroxiapatita em misturas sintéticas com quartzo e calcita. Nestes sistemas foram estudados diversos parâmetros operacionais, tais como tipo de separação, efeito do teor da alimentação, e influência da moagem. Onde a separação estagiada apresentou melhor resultado, uma moagem adicional no sistema não favoreceu a seletividade. Por outro lado, o teor de P205 no concentrado é proporcional ao teor presente na alimentação. A hidroxiapatita, em estudo, de alta pureza (de acordo com técnicas de análise química, espectrofotometria de infravermelho e difração de raios X) apresentou um parto de carga zero em pH 6,77 na presença de diversos eletrólitos. A aplicação do sistema de floculação seletiva a fraçoes ultrafinas industriais foi estudada em detalhe e comparada com processos de flotação e floco-flatação. 0s resultados obtidos mostraram que a floculação seletiva somente foi eficiente nos sistemas sintéticos. A flotação, embora o minério apresente uma granulometria muito fina, foi mais eficiente que a floculação seletiva e a floco-flotação nos sistemas reais, em termos de taxa de enriquecimento e percentual de rejeição de massa. Entretanto com a floco-flotação foi possivel obter altas recuperações(-90%) para os minérios de Araxá e Itataia. Para o minério de Tapira, um aumento do teor de P2O5 foi obtido com a flotação da fração seletivamente floculada. As taxas de enriquecimento obtidas foram baixas (entre 1,35 e 2,101 em função das associações entre a apatita do minério com óxido de ferro e argila, o que revelou a caracterização mineralógica. Conclue-se que a concentração de minerios fosfatados de baixo teor é uma operação onerosa, onde o fator predominante é a absorção seletiva de reagentes e atransferência não específica de material de ganga nos respectivos concentrados.

A língua estrangeira e sua inclusão no currículo da educação do povo: necessária ou supérflua ?

Este trabalho propõe-se a pesquisa~ os critérios que impelem os legi~ ladores a determinar a adoção ou a supressão da língua estrangeira nos currículos escolare~; identificar as ideologias que servem de suporte a estes critérios; analisar os objetivos da educação formal e determinar o grau de importância do aprendizado da língua estrangeira na consecuçao destes objetivos. Considerando-se os valores que definiram ,os tipos de educação privil~ giados pela sociedade brasileira nas diferentes fases da sua evolução, le vantou-se a seguinte hipótese: o ensino da língua estrangeira tem sido vinculado ao modelo político-econõmico em vigor. Sua adoção ou supressão articula-se com as ideologias que legitimam e sustentam a hegemonia das classes dominantes. Para comprovar esta hipótese, fez-se um levantamento histórico da edu cação no Brasil Çolonial, Imperial e Republicano e sua divisão em perío - dos. Procedeu~se' a uma caracterização político~econômica e sócio-cultural de cada período, identificando-se as ideologias dominantes e suas articulações com a educação. Definiram-se os saberes dominantes superiores e i!!, feri ores , os critérios estabelecidos pelas classes hegemônicas para a transmissão dos mesmos e suas vinculações com o aprendizado da língua estrangeira. Tratou-se da omissão de educação, a partir da impostura do discurso dos detentores do poder decisório, proclamando valores que nao correspondiam ao seu pensamento e sua ação reais; e do caminho percorrido do "humanismo" à "tecnologia", no ensino das línguas estrangeiras, do seu papel de divulgadoras de idéias à transmissão de ideologias. Procurou-se estabelecer de que modo a herança histórica plasmou nosso presente, no d~ IDÍnio da educação, desde o colonialismo até à construção da identidade n~ cional. Identificaram-se razões que recomendam a diversidade de oferta e aprendizado de varias línguas estrangeiras, como componentes, entre outras disciplinas consideradas "supérfluas", da formação do patrimônio intelectual e cultural de cada indivíduo e da corrn.midade como um todo. Conclui-se denunciando os mecanismos adotados pelas classes hegeIDÔnicas para impedir o crescimento educacional do povo, a fim de que este não se torne uma ameaça a esta hegemonia. Como propostas de solução,serão publicadas duas pesquisas j á realizadas: problema quantidade de efetivos 2Lqualidade de ensino da língua estrangeira e o domínio da língua materna x a organização do pensamento x as possibilidades de produção na língua estrangeira.

Um estudo do traço de ansiedade numa população de professores universitários

Esta pesquisa surge do ~nteresse pela ~mportanc~a do estu- do_ do comportamento humêno, face ~s distintas situaçÕes de desem- penha, manifestado por atitudes que revelam o compromisso no meio eoucacional. Trata-se de verificar se h~ alguma rElação significativa entre o traço de ansiedade (na vis;o te~rica de Spielberger) de uma popul8ção amo,stral de profesf;ores universit~rios e seus dados . , ' institucionais: estado, civil, sexo, ~daae, numero de filhos,renda ~ ., - mensal, formaçao academica, area de concentrêçao, de estudos, cate goria profissional e tempo de ensino. t' , No primeiro cap~tulo poder-se-a apreciar uma aborcagem teg, ric8, na expectativa de conciliar os diferentes enfoques dados ao estudo da ansiedade pelas escolas e seus autores. , t O problema pesquisado esta delimitado no segundo cap~tulo 6It# , •• _ na forma de uma reflexao da pratJ.ca educncJ.onal, uma reflexao so- bre o professor universit~rio e un pequeno aspecto do seu mundo pessoal e profissional. t Verifica-se com alguns detalhes, no terceiro cap~tulo,qual o procedimento, metodol~gico utilizado neste estudo, seguindo-se a descrição dos instrumentos, bem como, o tratamento, , . analJ.se e conclusões.

Influência do teor de calcário no comportamento físico, mecânico e microestrutural de cerâmicas estruturais

There are ores of clay in Piauí State that are used for red structural ceramics, which are naturally contaminated with calcareous vein. This is one thing that impedes its exploration in an adequate way, especially for tile production. The present work aims at verifying the influence of the calcareous contents in the technological structural ceramics area, seeking to determine a maximum permissible calcareous proportion/contents in the ceramic mass using the patterns of the local industry production. For the consecution of this paper, it was characterized the clay and calcareous material by FRX, DRX, TGA and DTA. It was also configurated by extrusion and burnt in the temperatures of 850°C, 900°C, 950°C and 1000°C pieces of the corpus with 0, 5, 10, 15 e 20% of calcareous proportion. After that, it was carried out technological samples of linear retraction, water absortion, apparent porosity, specific apparent mass and mechanic resistance. The results showed the possibility of using calcareous in the ceramic mass and in some cases the technological properties got better

Obtenção de pós de tântalo metálico a partir da redução aluminotérmica com ignição a plasma

Metallic tantalum has a high commercial value due to intrinsic properties like excellent ductility, corrosion resistance, high melt and boiling points and good electrical and thermal conductivities. Nowadays, it is mostly used in the manufacture of capacitors, due to excellent dielectric properties of its oxides. In the nature, tantalum occurs in the form of oxide and it is extracted mainly from tantalite-columbite ores. The tantalum is usually produced by the reduction of its oxide, using reductants like carbon, silicon, calcium, magnesium and aluminum. Among these techniques, the aluminothermic reduction has been used as the industrial method to produce niobium, tantalum and their alloys, due to the easy removal of the Al and Al2O3 of the system, easing further refining. In conventional aluminothermic reduction an electrical resistance is used to trigger the reaction. This reaction self-propagates for all the volume of material. In this work, we have developed a novel technique of aluminothermic reduction that uses the hydrogen plasma to trigger the reaction. The results obtained by XRD, SEM and EDS show that is possible to obtain a compound rich in tantalum through this technique of aluminothermic reduction in the plasma reactor

Incorporação do resíduo oriundo do beneficiamento de caulim em concreto asfáltico

The municipal district of Equador-RN is located in an area of great amounts of ores, being your main economical activity the extraction and the kaolin improvement. The main originating from environmental problem that activity is the amount of generated residue, about 70% of the extracted kaolin. The residues are simply piled up in lands of the improvement companies, occupying like this a large area and causing impact in the existent flora. When dry, the residues transform powdered and for the action of the wind, they disperse, polluting the air. Being like this, the present work has as objective evaluates the incorporation of the great residue, originating from of the kaolin improvement, in partial substitution of all the employed aggregates in a conventional mixture of asphalt concrete, which was used in the paving of BR101/RN061 - passage between Ponta Negra and Ares. That evaluation was accomplished in three stages. The first refers to the evaluation of the physical, thermal and mineralogical characteristics of the residue with the intention of to classify it and to define your application as aggregate (small and great). The second refers to the physical characterization of the aggregates and of the asphalt material used in the conventional mixture. And the third, to the evaluation of the mixtures containing residue, which were elaborated starting from the conventional mixture with the gradual incorporation of the residue, from 5 to 40%, in substitution to the part of the conventional aggregates, in way to obtain similar particle size curves the one of the conventional mixture. That evaluation was accomplished through the comparison between the volumetric composition, the mechanical behavior and the susceptibility to the humidity of the mixtures containing residue with the one of the conventional mixture, and with the one of the DNIT specifications. The results show that the great residue originating from of the kaolin improvement has grains of the most varied size, being like this, it can substitute part of all the conventional aggregates and of the filler in an asphalt mixture. Besides, your mineralogical composition presented the same present minerals in the composition of conventional aggregates used in paving. The results evaluation of the volumetric composition of the mixtures containing residue indicates that it can use up to 30% of residue in substitution to the conventional aggregates. The evaluation of the mechanical behavior of those mixtures indicates that the residue increment in the studied mixtures caused an increase of the stability and a reduction of the resistance to the traction. The values obtained in the resistance to the traction meet below the minimum value specified by DNIT, but close to the value obtained in the conventional mixture. When taking in consideration the susceptibility of the same ones to the humidity, the results indicate that she can use up to 25% of residue

Fission-track dating of Macusanite glasses with plateau and size correction methods

Two Macusanite pebbles (MB1 and MB2) were dated with the fission-track method. Six irradiations were carried out in different nuclear reactors: Pavia (Italy), IPEN-CNEN (Brazil) and IPEN-Lima (Peru). Measurements of the thorium and uranium induced-fission per target nucleus using natural thorium thin films and natural U-doped glasses calibrated against natural uranium thin films, together with lambda(F) of 8.46 x 10(-17) a(-1) were used to determine the ages. The apparent ages were corrected using the plateau and size correction methods. Track measurements were performed by different analysts, using different counting criteria. In addition, tracks were measured on samples which had been submitted to thermal treatment as well as on samples which had not been heated. Thermal treatments were carried out to erase the fossil tracks before neutron irradiation. No significant differences have been found in individual results, using the two Macusanite pebbles and the different nuclear reactors, age correction techniques, analysts, track-counting criteria, and thermal treatments before neutron irradiation. The great majority of the results (14/17) is compatible with the Ar-Ar ages of 5.12 +/- 0.11 and 5.10 +/- 0.11 Ma, Macusanite MB1 and MB2, respectively. However, the fission-track ages are systematically less (similar to8%) than the Ar-Ar ages of the two Macusanite samples studied. (C) 2003 Published by Elsevier Ltd.

Group analysis method for fission track thermochronology

A methodology to obtain ages and thermal histories of sets of apatite samples from localities with geologically compatible characteristics is described. A methodology exploring the fact that samples with similar geological characteristics should present the same thermal history is proposed. This approach can contribute for the obtainment of more conclusive results by analysing fewer samples than it is necessary when the samples are individually analysed. In order to determine the ages, we use the absolute neutron dosimetry through thin films of natural uranium along with lambda(f) = 8.46 x 10(-17) a(-1). As an example of application of the proposed methodology, we analyse samples collected in a Brazilian region, Sao Francisco Craton, which experienced low tectonic activity. (C) 2008 Elsevier Ltd. All rights reserved.

The upgraded DO detector

The DO experiment enjoyed a very successful data-collection run at the Fermilab Tevatron collider between 1992 and 1996. Since then, the detector has been upgraded to take advantage of improvements to the Tevatron and to enhance its physics capabilities. We describe the new elements of the detector, including the silicon microstrip tracker, central fiber tracker, solenoidal magnet, preshower detectors, forward muon detector, and forward proton detector. The uranium/liquid -argon calorimeters and central muon detector, remaining from Run 1, are discussed briefly. We also present the associated electronics, triggering, and data acquisition systems, along with the design and implementation of software specific to DO. (c) 2006 Elsevier B.V. All rights reserved.

Radioactivity distribution in some Permian sediments from the Irati and Corumbatal formations of the Parana basin, southeastern Brazil

in the city of Limeira, southeastern Brazil, an important exposure of Permian sediments of the Parana basin was revealed by an open pit mine that exploits limestone for production of soil correction compounds and raw materials for the ceramic industry. The radioactivity of these sediments was investigated in some detail and the results provided a general view of the vertical distributions of uranium, thorium and potassium concentrations and of the element ratios U/K, U/Th and Th/K. In general, the concentrations of the main natural radioactive elements are low, with uranium being enriched in some limestone and shale levels. In addition the results showed that the U-238 series is in radioactive disequilibrium in many of the analyzed samples. Although the origin of the observed disequilibrium has not been investigated, the results suggest that it is due to weathering processes and water interaction with the rock matrix. (C) 2003 Elsevier Ltd. All rights reserved.

Nitrification processes in groundwaters evidenced by modification on the U contents and U-234/U-238 activity ratios

Groundwaters from the Botucatu-Piramboia aquifer system located at the Parana sedimentary basin in Brazil and sampled at Ribeirao Preto city, São Paulo State, were chemically and isotopically analysed, with the aim of evaluating how uranium isotopes U-234 and U-238 can be utilized to monitor the progress of nitrate, the main indicator of agrichemical pollution into an aquifer. Based on the isotope dilution analysis, the U-234/U-238 activity ratio and U content data in the groundwaters were utilized to deduce their proportions in a mixture, suggesting that the water not affected significantly by nitrification still dominates the exploitation system involving the studied wells.

A laboratory study of the transfer of U-234 and U-238 during water-rock interactions in the Carnmenellis granite (Cornwall, England) and implications for the interpretation of field data

Laboratory time-scale experiments were conducted on gravels from the Carnmenellis granite, Cornwall, England, with the purpose of evaluating the release of natural uranium isotopes to the water phase. The implications of these results for the production of enhanced U-234/U-238 activity ratios in Cornish groundwaters are discussed. It is suggested that the U-234/U-238 lab data can be used to interpret activity ratios from Cornwall, even when the observed inverse relationship between dissolved U and U-234/U-238 in leachates/etchates is taken into account. (C) 2001 Elsevier B.V. Ltd. All rights reserved.

Hydro(radio)chemical relationships in the giant Guarani aquifer, Brazil

This investigation was carried out within the Parana sedimentary basin and involved the sampling of 78 pumped tubular wells for evaluating the hydrochemistry and radioactivity due to the nuclides (238)U, (234)U, (222)Ra, (226)Ra, and (228)Ra in the Brazilian part of Guarani aquifer. Several significant correlations were found involving the geostatic pressure, for instance, specific flow rate, CO(3)(2-), SO(4)(2-) temperature, dissolved O(2), free CO(2), pH, redox potential Eh, conductivity, Na, HCO(3)-, CO(3)(2-) , SI(calcite), Cl(-), F(-), SO(4)(2-), and B. Carbonates precipitation was evidenced by inverse correlation between CO(3)(2-) and Ca, Mg, Sr, and Ba, whereas Na exhibited an opposite trend, dissolving rather than precipitating with increasing CO(3)(2-) concentration. An inverse correlation between 3 and K was found, possibly related to the increasing tendency of K to recombine with the thickness of the clayey layers. HCO(3)-played an important role on Na, Ca, Mg, and Sr dissolution. The dissolved U content and (234)U/(238)U activity ratio data were plotted on a two-dimensional diagram that was successfully utilized on identifying an unreported zone of U accumulation, though not necessarily of economic size and grade. The variability in chemical and radionuclides data indicated an important influence of the underlying Paleozoic sediments in the composition of waters from Guarani aquifer. The available data allowed estimate the groundwater residence time by two U-isotopes disequilibrium methods. Values of 45-61 ka were initially calculated, depending on the adopted porosity (15-20%), but a longer residence time (- 640 ka) was also estimated, which is more compatible with the hydraulic conductivity data in Guarani aquifer and groundwater flow velocity occurring at Milk River aquifer, Alberta, Canada. Such time range agrees with previously reported (14)C ages exceeding 30 ka BP at the more central parts of the Parana sedimentary basin. (c) 2005 Elsevier B.V. All rights reserved.

Implications of groundwater weathered profile interactions to the mobilization of radionuclides

This study reports the nature and extent of open-system interaction between groundwater and a weathered profile developed in the high grade thorium and REE ore body in Morro do Ferro, Pocos de Caldas plateau. The radioelement mobility in the shallow oxidizing environment was considered by using chemical data in conjunction with U-234/U-238, Ra-226/Th-230, Th-230/U-234, Th-228/Th-232, Ra-228/Th-232 and Th-230/Ra-228 activity ratios (AR's) for borehole spoil and groundwater samples.Recharging groundwater from the studied borehole has low salinity values, with total dissolved solids content of 14.7 mg/l and total ionic strength of 0.00018. The ratio of the weight of dissolved radioelement per unit volume of solution to the weight of radioelement in solid phase per unit weight of solid phase showed that the radioelement solubility in the studied waters varied according to the following order: radium> uranium >thorium.U-234/U-238 AR's less than 1 were measured in solid phase and can justify the enhancement of U-234 in solution. Ra-226/Th-230 AR's greater than 1 and Th-230/U-234 AR'S less than 1 were evaluated between 20 and 27 m in depth, where a 2.1-m thick magnetite dike was intersected. These ratios could be justified by deposition of U and Ra associated with Fe-Mn oxides and kaolinite, where mineral saturation indices evaluated from the available data confirm this possibility. Covariations among disequilibria involving Th-228/(228) Ra and Ra-228/Th-232 AR's showed the preferential removal of Ra-228 relative to Tn isotopes, Th-228 and Th-232. The recent deposition of radium within the timescale of at least the last 35 years also is suggested. (C) 1998 Elsevier B.V. Ltd. All rights reserved.

U-ages in soils and groundwater evidencing wet periods 400-600 kyr ago in southeast Brazil

U-238 and its radiogenic daughter U-234 have been utilized for dating soil formation and groundwater residence time during the last 1.5 million years, in this case based on the U-clissolution/precipitation occurring during modifications of the oxidation-reduction conditions. In this paper, we report a 400-600 kyr proxy of wet periods from sediments occurring in a soil profile developed over rocks outcropping at the Parana sedimentary basin in Brazil, and from groundwater exploited of Guarani aquifer at the same basin. The approaches indicated successful use of the U-modeled ages for suggesting wet periods exceeding the past 116-210 kyr from previous studies. (C) 2007 Elsevier Ltd. All rights reserved.