879 resultados para Depósitos continentales


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Six Paleogene-Aquitanian successions have been reconstructed in the Alicante area (eastern External Betic Zone). The lithofacies association evidences “catastrophic” syn-sedimentary tectonic processes consisting of slumps, mega-olisthostromes, “pillow-beds” and turbiditic deposits. This kind of sedimentation is related to unconformity surfaces delimiting sequence and para-sequence cycles in the stratigraphic record. The data compiled have enabled the reconstruction of the Paleogene-Aquitanian paleogeographic and geodynamic evolution of this sector of the External Betics. During the Eocene the sedimentary basin is interpreted as a narrow trough affected by (growth) folding related to blind thrust faulting with a source area from the north-western margin, while the southeastern margin remained inactive. During the Oligocene-Aquitanian, the sourcing margin becames the southeastern margin of the basin affected by a catastrophic tectonic. The activity of the margins is identified from specific sediment source areas for the platform-slope-trough system and from tectofacies analysis. The southeastern South Iberian Margin is thought to be closer to the Internal Betic Zone, which was tectonically pushing towards the South Iberian Margin. This pushing could generate a lateral progressive elimination of subbetic paleogeographic domains in the eastern Betics. This geodynamic frame could explain the development of such “catastrophic” tectono-sedimentary processes during the Late Oligocene-Early Miocene.

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En la actualidad, los arrecifes de coral, ecosistemas productivos de gran vulnerabilidad, se encuentran en un estado de degradación continua por factores tanto de carácter antropogénico como natural. Consecuentemente se han desarrollado diversas metodologías de conservación y restauración de las cuales destaca el uso de técnicas electroquímicas. Dicha técnica consiste en el depósito electroasistido de carbonatos de calcio sobre soportes de acero inoxidable (u otro material conductor) que sumergido en el agua de mar y por la aplicación de una corriente de reducción genera un depósito mineral sobre el soporte metálico. En primer lugar, se han estudiado diversos sustratos conductores, tanto metálicos como carbonosos mediante técnicas voltamperométricas en las que se ha podido apreciar la efectividad de cada uno de ellos para la precipitación de minerales. Si se aplica una intensidad de corriente en la electrolisis de agua de mar se produce una reacción de reducción electroquímica en el electrodo sumergido que actúa como cátodo que induce un cambio de los parámetros químicos del agua: el pH, alcalinidad, concentración de calcio y magnesio, etc. A la vez, en la superficie del cátodo se promueve la formación y crecimiento de un depósito mineral. Este se ha analizado mediante diversas técnicas de microscopía, microanálisis y difracción de rayos X y los resultados muestran como la aplicación de distintas densidades de corriente durante las electrólisis tienen la capacidad de modular, las características morfológicas, atómicas y cristalográficas de los depósitos. La composición mineralógica del compuesto agregado en el electrodo consta de Mg(OH)2 y CaCO3. Las estructuras cristalinas de tales especies corresponden a la forma brucita, con una textura lisa e homogénea y aragonito con hábito botroidal. Densidades de corriente aplicadas por encima de 1 mA/cm2 generan depósitos con más de un 93% de presencia de brucita además de presentar una cristalografía más amorfa y un progresivo descenso de la eficiencia del proceso con un elevado gasto energético. En cambio, se ha comprobado que es posible modular las características del depósito a obtener con densidades de corriente comprendidas entre 0.01 y 1 mA/cm2, obteniendo una composición del depósito con cantidades de aragonito, textura y morfología óptimas para una futura aplicación con corales.

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As paisagens dunares são sistemas de elevado dinamismo, devido à proximidade do mar e à extrema mobilidade do substrato arenoso e prevê-se que venham a ser severamente afetadas pelas alterações ambientais globais. As dunas são depósitos de areia criados por processos eólicos e apresentam uma vegetação muito característica. Estes depósitos de areia em conjunto com a vegetação formam uma barreira essencial ao avanço do mar durante as marés altas de águas vivas e tempestades. Em Portugal, a degradação dos ecossistemas costeiros é muito preocupante. O problema das espécies exóticas invasoras agravou-se, aumentando a pressão sobre as plantas nativas. Embora este problema não seja o único motivo da degradação dos ecossistemas costeiros, este trabalho pretende divulgar as plantas dunares da zona costeira de Matosinhos, sensibilizar para a proteção e conservação das dunas e alertar para o facto de diversas plantas invasoras rapidamente colonizarem espaços abertos, pondo em causa e estabilidade dos ecossistemas costeiros. O conhecimento detalhado destes ecossistemas permitirá a aplicação de processos de vigilância e monitorização bem como o restauro ecológico de áreas dunares degradadas.

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Tese de doutoramento, Farmácia (Tecnologia Farmacêutica), Universidade de Lisboa, Faculdade de Farmácia, 2016

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Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

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Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

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Para a conclusão do Mestrado em Gestão Financeira, obtei pela realização de um estágio curricular, o qual foi concretizado na Caixa Geral de Depósitos, S.A. (CGD), na agência de Odivelas, durante o período de seis meses, entre 3 de setembro de 2012 e 1 de março de 2013. O título deste relatório pretende informar acerca do objeto do estágio, que me pôs em contato com os produtos, serviços e operações realizadas pelas instituições bancárias. As instituições financeiras, às quais os bancos fazem parte, têm como principal função a canalização da poupança para o investimento nos mercados financeiros. Além disso, são consideradas de intermediário entre os agentes económicos, ou seja entre aqueles que pretendem realizar poupanças e aqueles que pretendem efetuar investimentos. Nesse sentido, as instituições financeiras apresentam um leque bastante diversificado de produtos e serviços, permitindo ao cliente fazer a gestão dos seus rendimentos e forma de acesso de acordo com as suas necessidades. Este estágio permitiu-me a aquisição de novas competências, tanto a nível profissional como a nível pessoal. A nível profissional é de salientar o desenvolvimento de capacidades de trabalho autónomo e de pesquisa e a capacidade de lidar com um conjunto de situações que resultam da dinâmica do atendimento ao público. Por outro lado, a nível pessoal permitiu-me desenvolver capacidades comunicacionais e de argumentação no relacionamento interpessoal.

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"Cronica y bibliografia" included in each number.

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En port.: Ouvrage qui fait suite à celui de M. Toullier, mais dans lequel on a adopté la forme plus commode du commentaire.

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Esta publicación es producto de la selección y edición de los mejores trabajos presentados durante las II Jornadas de Planificación organizadas por ILPES en Santiago de Chile, del 24 al 25 de septiembre de 2014, con el apoyo de la República de Corea. Estas II Jornadas se desarrollaron en paralelo con el Seminario Internacional “Latinoamérica y el Caribe al 2030: visiones del mundo, miradas continentales”.

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The drilling of wells for petroleum extraction generates rocks and soils fragments, among other residues. These fragments are denominated petroleum drilling gravel or simply petroleum drilling residue. On the sites of onshore exploration are formed big deposits of drilling gravel, an expensive final destination material. This work aims at evaluating the addition of drilling residue to a lateritic soil, as composite material, for construction of compacted fills for earth work projects. Soil and residue were evaluated by X-ray diffraction (XRD) and X-ray fluorescence (XRF) and by laboratory tests traditionally used in soil mechanics, as particle-size analysis of soils, determination of liquid and plasticity indexes and compaction test. After soil and residue characterization, soil-residue mixtures were studied, using dosages of 2,5%, 5%, 10%, and 15% of residue in relation to the dry soil mass. These mixtures were submitted to compaction test, CBR, direct shear test and consolidation test. The test results were compared to the current legislation of DNIT for compacted fill construction. The results showed that the mixtures presented the minimal necessary parameters, allowing, from the point of view of geotechnical analysis, the use of these mixtures for construction of compacted fills

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The Cacimbinha and Madeiro beaches are located in the eastern coast of Rio Grande do Norte state, in the municipality of Tibau do Sul. Given the indicative of erosion in the coast of this district and the coastal processes acting on the beaches, the global aim of this project is comprehend the evolution of depositional environment on the Cacimbinha beach, moreover, the project seeks to characterize deposits from the Cacimbinha and Madeiro beaches, according to the geomorphologic compartments identified on these beaches; distinguish the coastal features which possibly interact with the Cacimbinha beach; identify the potential relationship between the sediments from the coastal features and the deposits from Cacimbinha beach; understand which depositional processes that prevail at each facies deposited on the beach; and identify the probable sedimentary environments and its energy of deposition through of the materials recorded on the Cacimbinha beach. This study was based on previous bibliographic and field research, both guided by academic works, laws, concepts and theories concerning the physical geography, geomorphology of the quaternary, sedimentary geology and stratigraphy. Thus, the methodology was divided in three steps: Prefield step: office work was performed; Field step: Sampling of facies of sedimentation; PosField step: analysis and integration of data obtained during the research period. Thus, the results showed deposicional facies with distinguished energy in the relief compartments, beach and terrace. After the sedimentary analysis and its interpretation linked to the architecture of the mounted sections based on drilling, it became possible to trace the evolutionary history of this stretch of beach. Therefore, it can be stated that studies performed on coastal areas are of great importance, as long as, around the world, the most part of urban zones are seated on deposits of quaternary age and, then this work improve the knowledge regarding the sedimentary dynamics of this beach, becoming scientific support for management and planning of this area which focus on, mainly, the foreign tourism

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In the coastal region of Ceará, between the municipalities of Acaraú and Itapipoca, thirteen sites were identified containing indicators of relative sea level, six of these being dated by optically stimulated luminescence (OSL) and radiocarbon. Ages obtained supports that were formed prograding beaches in the study area. In the eastern portion, beaches in coastal plain deposits occur while a system lagoon/barrier paleomangrove occurs in the western portion of the study area. In both cases the coastal deposits prograde from east to west. Higher sea levels were identified between the current: (a) 3.110-2.830 cal. yr. BP; (b) 1.830 yr. BP (OSL) - 1.490 cal. yr. BP; (c) between 1.240-1.060 cal. yr. BP; (d) 845-715 yr. BP (OSL). Since then the sea level suffered by lowering the current level. Variations in sea level are interpreted as responses to changes in the pattern of marine circulation and do not exclude possible tectonic disturbances in the basin of the continental margin. The indicators of relative sea level west coast of Ceará present differently from other curves constructed in the coastal northeast, suggesting that local factors mentioned above contributed to sea level fluctuations.

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Systems of incised valleys have been studied in different continental shelves, including the Brazilian continental margin. The interest to characterize this feature is given by the information that it can provide variations on sea level, as well as the ability to host economically significant quantities of hydrocarbons in reservoirs located in deposits filling of the incised valleys. This thesis has the overall objective to characterize the morphology and sedimentary cover of the incised valley Apodi-Mossoró, located in the Northern Continental shelf of Rio Grande do Norte state, adjacent to Areia Branca city. The methodology included the integration of satellite imagery, bathymetric data, sedimentological data, shallow seismic, and the identification of foraminifera. The results indicate that the ApodiMossró incised valley is currently formed by two channels, shallow channel and deep channel, which have distinct morphological and sedimentological characteristics. The deep channel has connection with one of the heads of the Apodi Canyon, located in the slope area. The acquisition, processing and interpretation of shallow seismic data allowed the recognition of the depositional surface, erosional surface, discordance, and sismofaceis. The erosional surface mapped from shallow seismic sections is possibly a indicative of an ancient surface of valley incision, where it would probably be associated with the limit Pleistocene/Holocene. Different sismofaceis were identified and reflect the rise in sea level with standards sometimes agradacional, sometimes progradational. The thickness of sediments on this surface was estimated at a maximum of 22m thick in the central portion of the incised valley. Statistically, there are differences between the adjacent continental shelf and channels, and between these channels, for the content of calcium carbonate, organic matter, sand and mud perceptual, except for the gravel grain size. The analysis of living and dead foraminifera showed the presence of fifty species distributed in regards to morphology, depth and type of sediment. Four type of seismic echocharacteres were identified and mapped, as well as their bedforms, indicating different sedimentary processes along the incised valley. The integration of results suggests an activation of the Apodi-Mossoró incised valley in the Late Pleistocene.

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Through participant observation, held in the administrative region east of Natal / RN, this research aimed to understand about the daily life of men and women living on the streets in the city. How they relate to the space where they live? In this relationship, which uses and survival strategies triggered by this social segment? These were some of the questions that guided this research, in order to highlight the specificities of this way of life and the possible consequences that such a situation could reverberate. In this sense, there was an effort to keep up with people on the streets, their itineraries and seize their narratives. Along the search path - which took place intermittently between the years 2011-2015 - attended spaces of occupation and traffic of this population group in the street, as well as insert me and got involved in events, forums, seminars, meetings and subject of joints on the streets as a political movement (MNPR / RN). They are considered in this study as people on the street to those who occupy the street as their main space of survival and ordering of daily life: in the streets sleep, feed themselves, meet the physiological and hygienic needs, and is where draw sustenance. The street is taken in this research in its broadest sense, including all possible places relatively protected from the cold, rain and exposure to violence, thus includes both open and public spaces: as squares and parks; but also closed and private places: hostels, abandoned warehouses, prisons, etc. It was observed that in none of these spaces guys on the street are established in a fixed manner, in contrast, they experience the roaming, which in part is due to urban systems - which tends to stigmatize them and delete them places - and the very need to survive, because while living in the street differentiated practices are triggered, and these differ from the dominant mode of sedentary life.