999 resultados para Conselho Geral
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In this work, we studied the strong consistency for a class of estimates for a transition density of a Markov chain with general state space E ⊂ Rd. The strong ergodicity of the estimates for the density transition is obtained from the strong consistency of the kernel estimates for both the marginal density p(:) of the chain and the joint density q(., .). In this work the Markov chain is supposed to be homogeneous, uniformly ergodic and possessing a stationary density p(.,.)
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The North Paraíba River Estuary, located in the eastern portion of the Paraíba State, Northeast Brazil, on coordinates 34º50 00 -34º57 30 S and 6º55 00 -7º7 30 W, constitutes a fluvio-marine plain formed by the North Paraíba River and its tributaries Sanhauá, Paroeira, Mandacaru, Tiriri, Tambiá, Ribeira and Guia. This estuary comprises an area of about 260 km2. Increasing human demands on the estuary area and inadequate environment managing have generated conflicts. The present work main purpose is to evaluate the geodynamic evolution of the North Paraíba River Estuary in the period from 1969 to 2001, using digital image processing techniques, thematic digital cartography and multitemporal data integration, combined to geological-geophysical field surveys. The SUDENE cartographic database, converted to digital format were, used to obtain occupation and topographic maps from 1969 and to generate a Digital Elevation Model (DEM). Digital Landsat 7 ETM+ and Spot HRVIR-PAN satellite images interpretation allowed the environmental characterization of the estuary. The most important digital processing results were achieved color composites RGB 5-4-3, 5-3-1, 5-2-NDWI and band ratio 7/4-5/3-4/2, 5/7-3/1-5/4). In addition the fusion image technique RGBI was used by the inclusion of the Spot HRVRI and Landsat 7 ETM+ panchromatic band on I layer with RGB triplets 5-4-3, 5-3-1 and 5/7-3/1-5/4. The DEM and digital images integration allowed the identification of seven geomorphological units: coastal tableland, flowing tray, tide plain, fluvial terrace, submerged dune, beach plain and beach). Both Side Scan Sonar and Echosound were used to analyse underwater surface and bedforms of the estuarine channel, sand predominance (fine to very fine) and 2D dune features 5 m wide and 0.5 m height. This investigation characterized the estuary as an environment dominated by regimen of average flow. The channel depth varies between 1 m and 11 m, being this last quota reached in the area of Porto de Cabedelo. The chanel estuary is relatively shallow, with erosion evidences mainly on its superior portion, attested by sand banks exposed during the low tide. Multitemporal digital maps from 1969 and 2001 integration were obtained through geoprocessing techniques, resulting the geodynamic evolution of the estuary based on landuse, DEM geomorphology and bathymetric maps
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It is presently assumed that the Borborema Province resulted from a complex collisional process associated with the convergent movement of plates, possibly involving amalgamation and accretion of microplates. This process was consolidated at the end of the Brasiliano event. It is investigated the possible limits for the tectonostratigraphic terranes in the northern portion of the province based on an integrated study of geological and gravity data. The study area comprises the portion of the Borborema Province located north of the Patos Lineament, limited by longitudes 33º00 W and 43º29 44"W and latitudes 1º36 S and 8º00 S. A revision of the regional geology allowed to identify areas presenting contrasting geological attributes, possibly representing different terranes whose limits are always shear zones of Brasiliano-age. The Sobral-Pedro II shear zone is the only one undoubtedly presenting geological attributes of sutures zones. The other shear zones are very likely associated with a geodinymic context of accretion, involving oblique collisions (docking), transcurrent and/or transforming sutures, and deep intracrustal shear zones. The gravity data contributed as a tool to identify strong lateral contrasts of density inside the upper crust possibly associated with crustal blocks tectonically juxtaposed. The dominant long wavelength anomaly in the Bouguer anomaly map is an expressive gradient, grossly parallel to the continental margin, caused by density variation across the crust-mantle interface in the transition from the continental crust to the oceanic crust originated by the separation between South America and Africa. Medium to small wavelength anomalies are due to intracrustal heterogeneities such as different Precambrian crustal blocks, Brasiliano-age granites and Mesozoic sedimentary basins. A regional-residual separation of the Bouguer anomaly map was performed in order to enhance in the residual map the effect due to intracrustal heterogeneities. The methodology used for this separation was a robust polinomial fitting. The inversion of residual gravity field resulted in a density contrast map (Δρ), in an equivalent layer that provided more accurated anomalies contours and consolidated the model which the sources of residual anomalies are located in the upper part of the present crust. Based on the coincidence of gravity lineaments in the residual map and Brasiliano shear zones, and using additional geological information, the following shear zones are proposed as limits between terranes: Patos shear zone, Sobral-Pedro II shear zone, Picuí-João Câmara shear zone, Remígio-Pocinhos shear zone, Senador Pompeu shear zone, Tauá shear zone, and Portalegre shear zone. Based on the geological/geophysical information it is attributed a higher level of confidence to the first three proposed limits(Patos, Sobral Pedro II, and Picuí-João Câmara shear zones). From west to east, these shear zones individualize the following terranes: Northwest of Ceará terrane, Central Ceará terrane, Tauá terrane, Orós-Jaguaribe terrane, Seridó terrane, and São José de Campestre terrane. In our study, the Rio Piranhas and Patos terranes are questioned because their previously proposed limits do not present good geological and gravimetric evidences. On the other hand, the previously proposed Cearense terrane is now subdivided into Central Ceará and Tauá terranes. Two residual gravity profiles located in the Seridó belt were interpreted using 2 ½ D direct gravity modeling. The main result of the modeling process is that all anomalies, with the exception of one, can be explained by outcroppring bodies, therefore restricted to the upper part of the present crust
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This dissertation deals with sedimentological and structural framework of the siliciclastic rock of the Serra do Martins Formation (FSM) in the Portalegre, Martins and Santana plateau, located to the south of Potiguar Basin, in the southwest and central Rio Grande do Norte state. This formation, regarded as of Oligo-Miocene age based on intrusive relations of the Miocene Macau volcanics, has a still disputable age due to the lack of appropriate bio and/or chronostratigraphic markers. The FSSM deposits crop out along 650 to 750 m high plateau, as a remanescent sedimentary cover directly overlying topographically uplifted pre-cambrian crystalline rocks. During the last decades, these deposits were interpreted according to a Tertiary paleoclimatic evolutionary model, associated to pedogenetic processes. The sedimentological characterization of the FSM was done through a detailed study of its facies, petrography and diagenetic features. The facies study was based on description of field relations, textures and structures, the piling up of the strata and their lateral variations. The FSM was deposited by an anastomosing to coarse-meandering fluvial system, including deposits of lag, cannel-fill, ouver-bank and flood plain. The petrographic composition of the sediments, coupled to their facies and paleocurrent directions, suggest a rather distal sourcearea, to the south of the present plateau. The diagenetic study identified an incipient grain mechanical compaction, pronounced dissolution of the framework, matrix and/or cement components, intense precipitation of kaolinite, silic and, eventually, iron oxides, besides mechanical infiltration of the clays. Most of these events, regarded in the literature as associated to near-surface conditions (eo or telodiagenesis), indicate the FSM sediments were never deeply buried. Topographic relations along longitudinal and transversal sections reaching the Potiguar Basin to the north identified regional dips that allow to discuss stratigraphic correlations between the FSM and the basin formations. The sedimentological features of the different units and the intrusive relations of the Macau volcanics were also considered in these correlations,which support the Oligo-Miocene age previously accepted for the FSM. Concerning the tectonic framework of the FSM, this work investigated the pre-cambrian to cretaceous heritage and the cenozoic deformation, allowing the recognition of pre-, sin and post-FSM structures. The crystalline basement, belonging to the Seridó Belt, displays NE and WNW foliation trends related to the Brasiliano-age ductile shear zones. In this terrain, brittle-ductile and brittle NE- and NW-trending structures, associated with extensional joints filled with pegmatites and quartz veins, are related to an E-W compression by the end of Brasiliano Cycle. The E-W joints and NE-trending fractures were reactivated by N-S to N-S to NW extension during late Jurassic to Cretaceous times, controlling the emplacement of the Rio Ceará-Mirim basic dyke swarm and the opening of the Potiguar rift basin
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The history match procedure in an oil reservoir is of paramount importance in order to obtain a characterization of the reservoir parameters (statics and dynamics) that implicates in a predict production more perfected. Throughout this process one can find reservoir model parameters which are able to reproduce the behaviour of a real reservoir.Thus, this reservoir model may be used to predict production and can aid the oil file management. During the history match procedure the reservoir model parameters are modified and for every new set of reservoir model parameters found, a fluid flow simulation is performed so that it is possible to evaluate weather or not this new set of parameters reproduces the observations in the actual reservoir. The reservoir is said to be matched when the discrepancies between the model predictions and the observations of the real reservoir are below a certain tolerance. The determination of the model parameters via history matching requires the minimisation of an objective function (difference between the observed and simulated productions according to a chosen norm) in a parameter space populated by many local minima. In other words, more than one set of reservoir model parameters fits the observation. With respect to the non-uniqueness of the solution, the inverse problem associated to history match is ill-posed. In order to reduce this ambiguity, it is necessary to incorporate a priori information and constraints in the model reservoir parameters to be determined. In this dissertation, the regularization of the inverse problem associated to the history match was performed via the introduction of a smoothness constraint in the following parameter: permeability and porosity. This constraint has geological bias of asserting that these two properties smoothly vary in space. In this sense, it is necessary to find the right relative weight of this constrain in the objective function that stabilizes the inversion and yet, introduces minimum bias. A sequential search method called COMPLEX was used to find the reservoir model parameters that best reproduce the observations of a semi-synthetic model. This method does not require the usage of derivatives when searching for the minimum of the objective function. Here, it is shown that the judicious introduction of the smoothness constraint in the objective function formulation reduces the associated ambiguity and introduces minimum bias in the estimates of permeability and porosity of the semi-synthetic reservoir model
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This work presents a study on the environmental vulnerability of the coastal region of Pititinga, Rio do Fogo/RN. The coastal erosion of Pititinga beach was analyzed and considerated as one more process that produces environmental vulnerability in the area of study, taking into account its human and natural environment and establishing the relation between them, to understand the arrangement that produced its spatial configuration. The natural environment was expressed by thematics maps with geology, geomorphology, vegetation and soil themes, while the human environment was expressed by the use and occupation of the soil map. The coastal erosion was put in an erosion vulnerability map. The methodological procedure to generate the thematics maps, vulnerability maps and of the erosion coastal involved the bibliographic research, field visits with check-list form fill, collect and analysis of sediment sample, photo-interpretation techniques, integration of the information in a database, data store and spatial analysis in a Geographic Information System (GIS) ambient. The natural vulnerability map shows a predominancy of environments with low (29,6%) or medium (42,4%) vulnerability, pointed the frontal and mobile dune as the areas with the highest vulnerability. The environmental vulnerability map, presents a predominancy of environments with low vulnerability (53,8%), with the high vulnerability concentrated on Pititinga community. The coastal erosion vulnerability presented distinct behaviors on three sections among the coastal line according each one characteristics. Where there are frontal and transgressive dunes, vulnerability are, generally, medium or low, respectively, and in the absence of them, as what occurs in Pititinga community, the vulnerability is predominately very high
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The current paper aims to check the environmental population perception of the two east side districts of Natal / RN (Rocas and Petrópolis) on its afforestation. The issues related to the environmental perception and afforestation of cities are gaining prominence in the many different areas of knowledge. However, the approaches and methodologies that are following an analytical perspective that by the rule aimed an policy of spatial planning not always responds to the aspirations and needs of the urban population. The research has been consisted of a preliminary survey, collecting data through the representative population of the neighborhoods in Petrópolis and Rocas, which were applied 210 forms (with the households), 130 in the neighborhood of Rocas and 80 in Petrópolis, which corresponds to 5% of the total households of the two districts, using as indicators, among many others, the income, the level of education and the environmental characteristics of the neighborhood. Through analysis sample was possible to verify that Petrópolis neighborhood that, 68% of interviewee believes their lives in the neighborhood where good and only 2% consider bad, in Rocas neighborhood, 57% considered life in his neighborhood good and only 5% consider bad. When asked about the main characteristics that remind the neighborhood Petrópolis, 90% of residents mentioned that one of its main advantages are the means of transport available, followed by 82% who quoted the ventilation as one of the main benefits of the neighborhood. In Rocas neighborhood, items mentioned by residents, were the ventilation with 47% of all interviewee and 32% said that peace is one of the most positive point of the neighborhood. From the description of some of the environmental needs of the neighborhoods Petrópolis and Rocas, it is possible to infer that environmental issues in general, and afforestation are always present in the speech of the residents, even indirect way, it shows that regardless of the education degree or the income, environmental quality is present as one of the basic needs of urban areas with implications both in the personal and social life as of its inhabitants.
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The development has been a phenomenon in constant discussion today, whose fundamental importance should be to promote the welfare of humanity. Thus, the development becomes an element that adds political, economic, social and environmental values . In Mozambique the development model adopted by the State prioritizes the economic dimension, in this case favoring the growth of capitalist structure production. Thus , the basic conditions for human survival still leaves much to be desired and the Mozambican population in general and the district of Chibuto , in particular , continue to face several difficulties to have access to such conditions, and the lack of potable water is a that most of the problems afflicting this population . The water was always a factor related to the socio-economic development of the population, where great civilizations and major economic marks were always influenced by water availability, and today this feature is present in all sectors of production. In Mozambique, much effort has been made by the government, national and international organizations to enhance and guarantee the supply of potable and drinking water, and despite all this effort, most of the population does not have access to this precious resource. In this sense, this work presents an analysis of the effects of the National Water Policy in the study area, analyzes the shortage of potable water in the district of Chibuto, discusses the design and development contained in the official discourse of the state and, opposes the idea of human development. For such issues that help to understand the phenomenon under study, such as territory, public policy and criticism of hegemonic conception of development are addressed. To make the desired approach, we performed a characterization of the District of Chibuto, addressing the issue of poverty, with a brief discussion of this concept, from different approaches, and analyze the impact of the PARPA (Action Plan for the Reduction of Absolute Poverty) in fighting poverty in Mozambique, and became a description of the scenario of poverty and vulnerability in Chibuto district with the construction of Territorial Human Development Index. Research also brings up a discussion about territory and technicization which describes the senary of the water supply system in the District and territorial dynamics of Chibuto, from the analysis and description of existing structures and other technical objects that structure the territory under study. Thus, it was found that the development should be summarized in the satisfaction of human needs, and should be the cornerstone of the new type of development that is intended for the purpose of triggering urgently actions to overcome or combat bleak misery suffered by the majority of inhabitants of the District of Chibuto
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OBJETIVO: Avaliar as causas de baixa visão e cegueira em indivíduos facectomizados, de amostra da população de cidades da região centrooeste do estado de São Paulo. Métodos: Estudo transversal, observacional, feito em cinco cidades da região centro-oeste do estado de São Paulo, em amostra domiciliar e baseada nos dados do último Censo Demográfico (IBGE, 1995), com escolha sistemática dos domicílios. Foi considerada para o presente estudo uma subamostra de indivíduos facectomizados, dos quais foram obtidos dados de identificação e exame oftalmológico completo. Os dados foram avaliados por estatísticas descritivas, análise de freqüência de ocorrência e proporção de concordância, com intervalo de confiança de 95%. RESULTADOS: Dos indivíduos amostrados, 2,37% haviam sido submetidos à facectomia. Dos 201 olhos operados, 26,9% apresentavam acuidade visual compatível com cegueira ou deficiência visual. Com a melhor correção óptica, a acuidade visual permaneceu <0,3 em 19,0%. O exame refracional proporcionou melhora da acuidade visual para 27,9% dos indivíduos facectomizados. As causas de baixa visão foram os erros refrativos não corrigidos, opacidade de cápsula posterior (19,4%), ceratopatia bolhosa (8,3%) coriorretinite cicatricial (8,3%), afacia (8,3%), degeneração macular relacionada a idade (5,5%), leucoma (5,5%), glaucoma (5,5%), atrofia de papila (5,5,%), descolamento de retina (2,8%), atrofia de epitelio pigmentado da retina (2,8%) e alta miopia (2,8%). CONCLUSÃO: Apesar da catarata ser causa de cegueira que pode ser evitável, mesmo após a correção cirúrgica porcentagem expressiva de indivíduos permanece com baixa visão, em geral, em decorrência de fatores relacionados ao seguimento pós-operatório negligenciado.
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OBJETIVO: Avaliar o perfil dos portadores de cavidade anoftálmica e a evolução dos pacientes com os tratamentos empregados. MÉTODOS: Estudo retrospectivo, realizado na Faculdade de Medicina de Botucatu, avaliando-se o perfil e a evolução dos portadores de cavidade anoftálmica, tratados no serviço. Os dados foram estudados segundo frequência de ocorrência e análise de associação. RESULTADOS: Os portadores de cavidade anoftálmica eram mais frequentemente em homens, trabalhadores em atividades exercidas com as mãos, jovens. O trauma e a phthisis bulbi foram as causas mais encontradas, havendo diferenças de acordo com a faixa etária e sexo. O índice complicações foi alto (57,1% dos casos), a maioria ocorrendo tardiamente. CONCLUSÕES: O trauma continua sendo causa importante de perda do olho. As complicações que ocorrem durante o acompanhamento do portador de cavidade anoftálmica são frequentes e ocorrem, em geral, tardiamente, o que reforça a necessidade de acompanhamento periódico e prolongado destes pacientes.
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Os autores apresentam um caso de coristoma ósseo episcleral (COE), cujo diagnóstico foi dado pelo exame histopatológico. O coristoma ósseo episcleral é tipo raro de coristoma, em geral localizado no quadrante temporal superior, sendo formado por tecido ósseo maduro.
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OBJETIVO: Avaliar a segurança e a efetividade do uso do 5-fluoruracila (5-FU) como tratamento adjuvante do pterígio, aplicado sob a forma de infiltração subconjuntival, no período intraoperatório. MÉTODOS: Foram avaliados prospectivamente 125 indivíduos (125 olhos) portadores de pterígio. Os indivíduos foram operados segundo a técnica de retalho de deslizamento e receberam, ao final do procedimento, injeção subconjuntival de 0,2 mL de 5-FU (25 mg/mL). Foram anotados os dados do paciente como idade, sexo, profissão, características da lesão (primário ou recidivado, tamanho, carnoso ou involutivo) e feito seguimento pós-operatório, aos 7, 21, 60 e 180 dias. Os dados foram submetidos à avaliação estatística. RESULTADOS: Não foram observados casos de complicação decorrente do uso do 5-FU em injeção no intraoperatório do pterígio. A taxa de recidiva geral observada aos 180 dias de pós-operatório foi de 35,8%, sendo de 35,7% para os pterígios primários e de 36,4% para os recidivados. CONCLUSÃO: A aplicação do 5-FU no período intraoperatório sob a forma de infiltração subconjuntival é segura. Entretanto, ainda resulta em altas taxas de recidiva e novos estudos devem ser realizados a fim de conhecer a concentração/dose ideal que permitirá menores chances de recidiva da lesão.
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OBJETIVO: O objetivo geral foi detectar fatores ambliopigênicos em uma população de pré-escolares, utilizando exames refratométricos e o PhotoScreenerTM (PS) e o objetivo específico foi verificar se a avaliação feita com o PS é útil como método de triagem em campanhas de prevenção de ambliopia em crianças. MÉTODOS: Foi realizado um estudo observacional, prospectivo, de janeiro a dezembro de 2007, avaliando-se 227 crianças pré-escolares, com o intuito de detectar, através da aplicação de um questionário, exames refratométricos e fotografias utilizando o PS, a presença de fatores causadores de ambliopia na população de estudo. Todas as crianças foram avaliadas pelo PS. em seguida, todas as crianças foram submetidas à cicloplegia , sendo avaliadas usando refrator automático Shin Nippon®. As crianças detectadas como portadoras de problemas oculares receberam prescrição óptica, segundo os critérios: hipermetropia maior que +1,50 D, miopia maior que -1,00 D e astigmatismo maior que 1,00 D. Analisaram-se os dados através do teste de concordância de Goodman, estatística descritiva e estudo da especificidade e sensibilidade ao emprego do PS, comparando os resultados com ele obtidos, com os resultados dos outros métodos de avaliação oftalmológica. RESULTADOS: A distribuição entre os sexos foi semelhante, sendo que a maioria das crianças apresentava quatro ou cinco anos de idade. A sensibilidade (S) do PS, comparando-se o resultado obtido neste aparelho com o autorrefrator sob cicloplegia, foi de 50,9%. Já a especificidade foi de 78,9%; valor preditivo positivo 70%; valor preditivo negativo 62,5% e acurácia 65,1%. CONCLUSÕES: Das 101 crianças cujas fotografias tiradas através do PS puderam ser analisadas satisfatoriamente, trinta e seis apresentavam erro refrativo que necessitou de correção. O PS, quando comparado com equivalente esférico do autorrefrator sob cicloplegia, é um método razoável de triagem, embora a sensibilidade não seja boa. Um ponto positivo a ser ressaltado é o considerável valor de especificidade.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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A anestesia obstétrica possibilita um procedimento mais seguro para a mãe e para os fetos. em medicina veterinária, no entanto, a literatura científica a respeito do assunto é deficiente. Este trabalho teve como objetivo avaliar o grau de depressão neurológica, hemodinâmica e respiratória fetais provocado pelo agente anestésico, em que as mães foram submetidas ao parto normal ou à cesariana, utilizando-se sevofluorano como agente de manutenção anestésica, comparando-o com o parto normal. Foram realizados seis partos normais (GN) e seis cesarianas (GC), avaliando-se um total de 36 filhotes. As cesarianas foram realizadas utilizando-se acepromazina, propofol e sevofluorano (GC) e os neonatos foram avaliados clinicamente ao primeiro, quinto e décimo minuto de nascimento, nos dois grupos. Observou-se maior depressão respiratória nos filhotes nascidos de cesariana. Contudo, apesar dessa depressão, o protocolo anestésico empregado não comprometeu de maneira importante a viabilidade e a saúde das mães e dos filhotes, demonstrando ser seguro em cadelas gestantes.