247 resultados para Afloramento costeiro


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O conteúdo fossilífero do afloramento Posto, localizado na cidade de Dona Francisca (Formação Santa Maria, Bacia do Paraná, Triássico Médio), UTM (22) 0270854/6720302 tem sido estudado e coletado com enfoque a classificação sistemática dos fósseis encontrados. Uma vez que grande parte dos trabalhos relacionados à tafonomia do Rio Grande do Sul englobam a paleoherpetofauna como um todo, este trabalho torna-se importante por deterse em concentrações específicas, sendo raros os estudos tafonômicos enfocando o conteúdo fossilífero de apenas um único afloramento. O material desta área, encontra-se em diferentes estados de articulação e preservação, sendo encontrado restos de cinodontes (crânios), dicinodontes (de crânios a outros elementos pós-cranianos) e arcossauriformes (crânios, vários elementos pós-cranianos, geralmente isolados e um esqueleto articulado, composto por seqüência vertebral, cintura pélvica e membros associados). Este trabalho tem como principal objetivo contar a história tafonômica do material fóssil encontrado na área de estudo, onde estes foram localizados pontualmente em seis perfis detalhados do afloramento, e posteriormente considerar tais elementos fósseis dentro do sistema deposicional nas respectivas fácies.(Continua0 A tafocenose é interpretada como sendo representante de uma paleofauna autóctone preservada em fácies de planície de inundação, e embora sejam encontrados diversos fósseis de diferentes posições ecológicas, com restos de predadores e presas dispersos no sedimento, não ocorreu concentração por predadores e provavelmente sem morte catastrófica. A presença das paleoalterações pedogênicas e freáticas, indicando uma distância relativa ao canal principal bastante grande, sugere um tempo de exposição bastante razoável até o soterramento das carcaças ou dos elementos isolados, permitindo um grau de desarticulação bastante avançado para alguns elementos ósseos. Para os esqueletos ou restos ósseos semiarticulados, é sugerido que o tempo de exposição entre morte e soterramento tenha sido menor, permitindo que grande parte dos seus elementos ósseos tenham sido preservados articulados associados a outros restos dispersos na planície já isolados.

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A tartaruga-verde, Chelonia mydas, possui ampla distribuição geográfica circuntropical, ocorrendo em toda zona costeira brasileira. A espécie está incluída em diversas listas de animais ameaçados de extinção, sendo assim fundamental a elaboração de modelos demográficos que possam vir a subsidiar futuros planos de manejo. Contudo, muitos aspectos referentes à história de vida destes animais ainda são pouco conhecidos, por serem animais marinhos de difícil observação, especialmente durante o período que despendem nas áreas de alimentação e durante as grandes migrações. As tartarugas marinhas apresentam características, em seu ciclo de vida, que dificultam a realização de estudos de marcação e recaptura, para determinação de parâmetros importantes como crescimento e determinação de idade. Por esta razão, muitos estudos envolvendo determinação de idade utilizando linhas cíclicas de crescimento presentes nos tecidos rígidos - esqueletocronologia, vêm sendo acumulados para esta espécie. Muito pouco se sabe sobre quaisquer aspectos relacionados às etapas do ciclo de vida das tartarugas marinhas que habitam o litoral do Rio Grande do Sul, deste modo, este estudo tem como principal objetivo avaliar a técnica histológica utilizada usualmente nas análises de esqueletocronologia em tartarugas marinhas a fim de verificar a ocorrência de crescimento cíclico nos ossos e de se obter estimativas de idade para a população local. As amostras são provenientes de tartarugas-verdes encalhadas no litoral norte do Rio Grande do Sul e coletadas, de forma sistemática entre Torres e Mostardas, de março de 1994 a setembro de 2003. Os 89 exemplares (35%) de tartarugas-verdes registrados indicam que a espécie é a segunda em número de ocorrências, sendo menos freqüente apenas que Caretta caretta (54%). Foi verificada apenas a ocorrência de exemplares juvenis (ccc = 29,0 a 52,0 cm, média = 38,9cm), que estão iniciando o período de desenvolvimento costeiro. A técnica avaliada não apresentou os resultados esperados, necessitando de algumas modificações metodológicas. A partir da observação dos cortes histológicos pôde-se constatar a presença de linhas de crescimento ósseo em apenas onze dos vinte e quatro indivíduos que apresentaram resultados satisfatórios na preparação histológica, indicando que a deposição das linhas pode ser variável e dependente de fatores ambientais. Nos onze indivíduos puderam ser distinguidas de uma a cinco linhas de crescimento, indicando uma idade entre 1 e 5 anos para o término da fase no ambiente pelágico. Com estes resultados obteve-se o primeiro registro da presença de linhas de crescimento ósseo, assim como, a primeira estimativa de idade para a população de Chelonia mydas no início de sua fase de desenvolvimento costeiro no Brasil.

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Dimensão: 1407x2349. Tamanho: 126Kb.

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The present work develops a methodology to establish a 3D digital static models petroleum reservoir analogue using LIDAR and GEORADAR technologies. Therefore, this work introduce The methodolgy as a new paradigm in the outcrop study, to purpose a consistent way to integrate plani-altimetric data, geophysics data, and remote sensing products, allowing 2D interpretation validation in contrast with 3D, complexes depositional geometry visualization, including in environmental immersive virtual reality. For that reason, it exposes the relevant questions of the theory of two technologies, and developed a case study using TerraSIRch SIR System-3000 made for Geophysical Survey Systems, and HDS3000 Leica Geosystems, using the two technologies, integrating them GOCAD software. The studied outcrop is plain to the view, and it s located at southeast Bacia do Parnaíba, in the Parque Nacional da Serra das Confusões. The methodology embraces every steps of the building process shows a 3D digital static models petroleum reservoir analogue, provide depositional geometry data, in several scales for Simulation petroleum reservoir

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On Rio Grande do Norte northern coast the process of sediment transport are intensely controlled by wind and sea (waves and currents) action, causing erosion and shoreline morphological instability. Due to the importance of such coastal zone it was realized the multi-spectral mapping and physical-chemical characterization of mudflats and mangroves aiming to support the mitigating actions related to the containment of the erosive process on the oil fields of Macau and Serra installed at the study area. The multi-spectral bands of 2000 and 2008 LANDSAT 5 TM images were submitted on the several digital processing steps and RGB color compositions integrating spectral bands and Principal Components. Such processing methodology was important to the mapping of different units on surface, together with field works. It was possible to make an analogy of the spectral characteristics of wetlands with vegetations areas (mangrove), showing the possibility to make a restoration of this area, contributing with the environmental monitoring of that ecosystem. The maps of several units were integrated in GIS environment at 1:60,000 scale, including the classification of features according to the presence or absence of vegetation cover. Thus, the strategy of methodology established that there are 10.13 km2 at least of sandy-muddy and of these approximately 0.89 km2 with the possibility to be used in a reforestation of typical flora of mangrove. The physical-chemical characterization showed areas with potential to introduce local species of mangrove and they had a pH above neutral with a mean of 8.4. The characteristic particle size is sand in the fine fractions, the high levels of carbonate, organic matter and major and trace element in general are concentrated where the sediment had the less particles size, showing the high correlation that those elements have with smaller particles of sediment. The application of that methodological strategy is relevant to the better understanding of features behavior and physical-chemical data of sediment samples collected on field allow the analysis of efficiency/capability of sandy-muddy to reforestation with local mangrove species for mitigation of the erosive action and coastal processes on the areas occupied by the oil industry

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Among the various effects caused by the climate change and human intervention, the mangrove ecosystem changes through of the years has been worth mentioning, which hasn t known which are the pros and cons for the adjacent coastal and estuarine environments yet. It happens due to the present dynamism in these areas, besides of the difficult understanding of the processes associated with evolution. This study aimed to environmentally evaluate adjacent mangroves from the Macau and Serra oil fields, located on Rio Grande do Norte northern coast, to support the mitigating actions related to the containment of the erosive process, as well as, according to the principles of the Clean Development Mechanism (CDM), to assess the amount of atmospheric carbon sequestered by the studied ecosystem. An inventory was conducted through mangrouve mapping which has supplied this research, especially regarding to the structural characterization of mangrove areas. To understand the local mangrove behavior in a greater level detail, techniques of remote sensing, GIS and GPS were used to make an analogy between the current and past states of the mangrove studied, allowing to make anticipated projections for the future impacts or changes in that region. This study combined data from multispectral LANDSAT 5 TM, Landsat 7 ETM+ with radar microwave data from SAR RADARSAT-1, which increased the interpretation capacity of the data from optical sensor systems. The interpretations have been supported by the data field, representing a better and innovative methodology for the environmental and taxonomic characterization of mangrove forests considered. The results reveal that mangroves of the Ponta do Tubarão Sustainable Development Reserve are biologically representative areas and providing a variety of benefits, especially for local communities, constituting the priority sites for actions development aimed at conservation. They also have been showing the necessity to make mitigating measures in order to recover degraded areas through reforestation or creating new areas of mangrove, as currently 7.1% of the mangrove forests studied are dead or in an advanced state of decomposition. The amount of atmospheric carbon sequestered proved very significant when analyzed for the whole area, which is able to sequester atmospheric 4,294,458 Ton CO2 per year

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Oil spills in marine environments represent immediate environmental impacts of large magnitude. For that reason the Environmental Sensitivity to Oil Maps constitute a major instrument for planning actions of containment and cleanup. For both the Environmental Sensitivity Maps always need to be updated, to have an appropriate scale and to represent accurately the coastal areas. In this context, this thesis presents a methodology for collecting and processing remote sensing data for the purpose of updating the territorial basis of thematic maps of Environmental Sensitivity to Oil. To ensure greater applicability of the methodology, sensors with complementary characteristics, which provide their data at a low financial cost, were selected and tested. To test the methodology, an area located on the northern coast of the Northeast of Brazil was chosen. The results showed that the products of ASTER data and image hybrid sensor PALSAR + CCD and HRC + CCD, have a great potential to be used as a source of cartographic information on projects that seek to update the Environmental Sensitivity Maps of Oil

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The objective of this Doctoral Thesis was monitoring, in trimestral scale, the coastal morphology of the Northeastern coast sections of Rio Grande do Norte State, in Brazil, which is an area of Potiguar Basin influenced by the oil industry activities. The studied sections compose coastal areas with intense sedimentary erosion and high environmental sensitivity to the oil spill. In order to achieve the general objective of this study, the work has been systematized in four steps. The first one refers to the evaluation of the geomorphological data acquisition methodologies used on Digital Elevation Model (DEM) of sandy beaches. The data has been obtained from Soledade beach, located on the Northeastern coast of Rio Grande Norte. The second step has been centered on the increasing of the reference geodetic infrastructure to accomplish the geodetic survey of the studied area by implanting a station in Corta Cachorro Barrier Island and by conducting monitoring geodetic surveys to understand the beach system based on the Coastline (CL) and on DEM multitemporal analysis. The third phase has been related to the usage of the methodology developed by Santos; Amaro (2011) and Santos et al. (2012) for the surveying, processing, representation, integration and analysis of Coastlines from sandy coast, which have been obtained through geodetic techniques of positioning, morphological change analysis and sediment transport. The fourth stage represents the innovation of surveys in coastal environment by using the Terrestrial Laser Scanning (TLS), based on Light Detection and Ranging (LiDAR), to evaluate a highly eroded section on Soledade beach where the oil industry structures are located. The evaluation has been achieved through high-precision DEM and accuracy during the modeling of the coast morphology changes. The result analysis of the integrated study about the spatial and temporal interrelations of the intense coastal processes in areas of building cycles and destruction of beaches has allowed identifying the causes and consequences of the intense coastal erosion in exposed beach sections and in barrier islands

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O objetivo deste trabalho foi avaliar cenários de níveis freáticos extremos, em bacia hidrográfica, por meio de métodos de análise espacial de dados geográficos. Avaliou-se a dinâmica espaço‑temporal dos recursos hídricos subterrâneos em área de afloramento do Sistema Aquífero Guarani. As alturas do lençol freático foram estimadas por meio do monitoramento de níveis em 23 piezômetros e da modelagem das séries temporais disponíveis de abril de 2004 a abril de 2011. Para a geração de cenários espaciais, foram utilizadas técnicas geoestatísticas que incorporaram informações auxiliares relativas a padrões geomorfológicos da bacia, por meio de modelo digital de terreno. Esse procedimento melhorou as estimativas, em razão da alta correlação entre altura do lençol e elevação, e agregou sentido físico às predições. Os cenários apresentaram diferenças quanto aos níveis considerados extremos - muito profundos ou muito superficiais - e podem subsidiar o planejamento, o uso eficiente da água e a gestão sustentável dos recursos hídricos na bacia.

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El objetivo de este estudio consistió en capturar y reconstituir el modo por el cual profesoras y profesores vinculados a la educación infantil y a la fase inicial de la enseñanza fundamental producen su identidad docente, en el contexto de una tardía profesionalización. El campo de esa pesquisa envolvió tres instituciones públicas de enseñanza superior, dos en Natal (RN) y una en João Pessoa (PB), que desenvulven programas especiales de formación de docentes vinculados a las respectivas redes locales de enseñanza. Para el atendimiento del objetivo arriba propuesto, fue utilizada la teoría de las representaciones sociales para la captura de los elementos constitutivos de las representaciones sociales del profesorado conforme la formulación de Serge Moscovici y colaboradores, considerándose, aqui, especialmente, la contribución de Abric en su complementar teoría de nucleo central de las representaciones. Teniendo en vista la necesidad de identificación de los elementos estructuradores de las representaciones, y definidores de las identidades en cuestión, se privilegió en la pesquisa la producción discursiva docente y sus condiciones de producción. La utilización de sus evocaciones, bien como de las fuentes escritas por los propios sujetos envolvidos, oportunizó el afloramiento de las diferentes faces constitutivas del ser profesor/a . El corpus decorriente de ese estudio fue entonces somentido a una serie de diferentes métodos / técnicas condensadas en programas informatizados y otros manuales en um esfuerzo para conferir un mayor rigor al análisis de los resultados apuntados. Se utilizó, aún, un referencial de análisis del discurso para viabilizar la emergencia de diferentes ângulos de la configuracion de la identidad en foco. Los resultados apuntam para un significativo deslocamiento de las representaciones docentes, bien como permitem afirmar la hipótesis, inicialmente puesta, de que la profesionalización docente ocurre no apenas de manera tardía, como también viene provocando una resignificación de los referentes de identidad de esos profesionales

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Through out the course of a steady increase in search and recovery of space in the coastal zone, there is also an expanding concern about the erosion processes of this area. The main problem in coastal areas is that urbanization occurs in a disorderly fashion and unsustainable, further aggravating the problems of coastal dynamics. The study area of this work is located on the southern coast of Pirangi do Norte beach to about 20km south of Natal, capital of Rio Grande do Norte in the Parnamirim City. This area has the length of approximately 1km, divided into three sections (Western, Central and Eastern) with a morphology consisting of a tableland at the top, sea cliffs in the West and Central parts and sand dunes in the Eastern section, both vegetated, and a coastal plain on the inferior part associated with the presence of beach rocks. This study aimed to analyze the erosion processes operating in the excerpt of Pirangi do Norte beach and assess the feasibility of their monitoring making use of DGPS (Global Positioning System Differential mode). During the work it was carried out a physical description of the area through photo-interpretation and site survey after measurement of the shoreline in the period between November 2004 and November 2009 and beach profiles between August 2005 and July 2006. The analysis of the results of the annual surveys showed the occurrence of variations of the shoreline along the stretch traveled. Sites are identified in advancement coast from the sea and it was verified in loco the presence of erosion with deposition of materials on the lower part of the coastal bluff, the former position of the shoreline, showing a false notion of advancing it. This leads to the conclusion that the data collected in a survey of the shoreline should always be accompanied by photographic records of the local area and with the highest rate of erosion, thus avoiding the mistake of treating the deposit materials as evidence of progress coast. At the end of the study, after a review of various works to mitigate the erosion in the coastal zone, it is recommended to the area of study the adoption of an artificial feeding of the beach, aiming the minimization of the erosive effects of the tides. Moreover, it is suggested that even the continuity of monitoring, maintenance of existing vegetation and control of the occupation on the edge of sea cliffs

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Digital Elevation Models (DEM) are numerical representations of a portion of the earth surface. Among several factors which affect the quality of a DEM, it should be emphasized the attention on the input data and the choice of the interpolating algorithm. On the other hand, several numerical models are used nowadays to characterize nearshore hydrodynamics and morphological changes in coastal areas, whose validation is based on field data collection. Independent on the complexity of the physical processes which are modeled, little attention has been given to the intrinsic bathymetric interpolation built within the numerical models of the specific application. Therefore, this study aims to investigate and to quantify the influence of the bathymetry, as obtained by a DEM, on the hydrodynamic circulation model at a coastal stretch, off the coast of the State of Rio Grande do Norte, Northeast Brazil. This coastal region is characterized by strong hydrodynamic and littoral processes, resulting in a very dynamic morphology with shallow coastal bathymetry. Important economic activities, such as oil exploitation and production, fisheries, salt ponds, shrimp farms and tourism, also bring impacts upon the local ecosystems and influence themselves the local hydrodynamics. This fact makes the region one of the most important for the development of the State, but also enhances the possibility of serious environmental accidents. As a hydrodynamic model, SisBaHiA® - Environmental Hydrodynamics System ( Sistema Básico de Hidrodinâmica Ambiental ) was chosen, for it has been successfully employed at several locations along the Brazilian coast. This model was developed at the Coastal and Oceanographical Engineering Group of the Ocean Engineering Program at the Federal University of Rio de Janeiro. Several interpolating methods were tested for the construction of the DEM, namely Natural Neighbor, Kriging, Triangulation with Linear Interpolation, Inverse Distance to a Power, Nearest Neighbor, and Minimum Curvature, all implemented within the software Surfer®. The bathymetry which was used as reference for the DEM was obtained from nautical charts provided by the Brazilian Hydrographic Service of the Brazilian Navy and from a field survey conducted in 2005. Changes in flow velocity and free surface elevation were evaluated under three aspects: a spatial vision along three profiles perpendicular to the coast and one profile longitudinal to the coast as shown; a temporal vision from three central nodes of the grid during 30 days; a hodograph analysis of components of speed in U and V, by different tidal cycles. Small, but negligible, variations in sea surface elevation were identified. However, the differences in flow and direction of velocities were significant, depending on the DEM

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The activities developed in the coastal zone always arise the researchers interest, mainly when it is developed in fragile ecological areas, not observing the sustenable development laws. In this context, the analysis presented developed around the estuary of Curimatau river, located in the Eastern coast of Rio Grande do Norte state, integrates information provided by high resolution images of orbital remote sensing (IKONOS II, dated of July of 2003) and images of not-orbital remote sensing (Air photographs of DPU, dated of March of 1997) in a multitemporary perspective, diagnosising patterns of use and occupation, evaluating the main area´s impacts, together with the estuarian region fisiograph of Curimatau river. The use of high resolution images consequently allowed generates a precision cartography, facilitating the quantification of the evolution of the landscape and supporting decisions. Was possible yet, the definition of use areas, conservation areas and preservation areas; that were inserted in the concept of Potentialities: a fundamental element to management of vulnerable areas of the natural point of view. The information provided during the research had been stored in an Enviromental Georreferenced Data Base, constructed under the optics of Geographical Information Systems (GIS), that they facilitate the environment management Through fast access to information. The results were satisfactory, because permits the quantification of evolution of the landscape and the mapping. Beyond the geoenviromental diagnosis, was possible develop maps and matrixes that support the Rio Grande do Norte state costal Management.

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The mangrove is a coastal ecosystem of the big ecological importance, showing high fragility front by natural process and the human interventions in the coastal zone. This research has objective to analyses the relation between mangrove species distribution and geochemical parameters variation of the water and soil in Apodi/Mossoro estuary, located in the Rio Grande do Norte state north coastline. The results were obtained from floristic and structural analysis of the vegetation and Quick Bird satellite images interpretation (collected in 2006 year), manipulated with ENVI 4.3 and ArcGIS 9.2 software s. This estuary was characterized by to presents a gradient of the salinity around 40 kilometers extension, finding amount between 50 and 90 g/l-1. Will be identified the formation of the mix vegetation formation in the estuary mount, where the water salinity no show express wide variation on seawater (36 g/l-1), finding species: Rhizophora mangle L., Laguncularia racemosa (L.) C. F. Gaertn, Avicennia schaueriana Stap. & Leechman e Avicennia germinans L. Along of the estuary, have a streak formation of the vegetation composed by Avicennia spp. and L. racemosa. In high estuary, where the salinities value stay above 60 g/l-1, only A. germinans predominate in dwarf form. In this sense, the salinity is as a limiting factor of stress on the mangrove vegetation as it enters the estuary, this parameter should be taken into account when drawing up management plans and environmental restoration in the estuary in question