979 resultados para Pré-sal
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
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O histórico de prospecção de hidrocarbonetos da Bacia Paleozoica do Parnaíba, situada no norte-nordeste do Brasil, sempre foi considerado desfavorável quando comparado aos super-reservatórios estimados do Pré-Sal das bacias da Margem Atlântica e até mesmo interiores, como a Bacia do Solimões. No entanto, a descoberta de gás natural em depósitos da superseqüência mesodevoniana-eocarbonífera do Grupo Canindé, que incluem as formações Pimenteiras, Cabeças e Longá, impulsionou novas pesquisas no intuito de refinar a caracterização paleoambiental, paleogeográfica, bem como, entender o sistema petrolífero, os possíveis plays e a potencialidade do reservatório Cabeças. A avaliação faciológica e estratigráfica com ênfase no registro da tectônica glacial, em combinação com a geocronologia de zircão detrítico permitiu interpretar o paleoambiente e a proveniência do reservatório Cabeças. Seis associações de fácies agrupadas em sucessões aflorantes, com espessura máxima de até 60m registram a evolução de um sistema deltaico Devoniano influenciado por processos glaciais principalmente no topo da unidade. 1) frente deltaica distal, composta por argilito maciço, conglomerado maciço, arenito com acamamento maciço, laminação plana e estratificação cruzada sigmoidal 2) frente deltaica proximal, representada pelas fácies arenito maciço, arenito com laminação plana, arenito com estratificação cruzada sigmoidal e conglomerado maciço; 3) planície deltaica, representada pelas fácies argilito laminado, arenito maciço, arenito com estratificação cruzada acanalada e conglomerado maciço; 4) shoreface glacial, composta pelas fácies arenito com marcas onduladas e arenito com estratificação cruzada hummocky; 5) depósitos subglaciais, que englobam as fácies diamictito maciço, diamictito com pods de arenito e brecha intraformacional; e 6) frente deltaica de degelo, constituída pelas fácies arenito maciço, arenito deformado, arenito com laminação plana, arenito com laminação cruzada cavalgante e arenito com estratificação cruzada sigmoidal. Durante o Fammeniano (374-359 Ma) uma frente deltaica dominada por processos fluviais progradava para NW (borda leste) e para NE (borda oeste) sobre uma plataforma influenciada por ondas de tempestade (Formação Pimenteiras). Na borda leste da bacia, o padrão de paleocorrente e o espectro de idades U-Pb em zircão detrítico indicam que o delta Cabeças foi alimentado por áreas fonte situadas a sudeste da Bacia do Parnaíba, provavelmente da Província Borborema. Grãos de zircão com idade mesoproterozóica (~ 1.039 – 1.009 Ma) e neoproterozóica (~ 654 Ma) são os mais populosos ao contrário dos grãos com idade arqueana (~ 2.508 – 2.678 Ma) e paleoproterozóica (~ 2.054 – 1.992 Ma). O grão de zircão concordante mais novo forneceu idade 206Pb/238U de 501,20 ± 6,35 Ma (95% concordante) indicando idades de áreas-fonte cambrianas. As principais fontes de sedimentos do delta Cabeças na borda leste são produto de rochas do Domínio Zona Transversal e de plútons Brasilianos encontrados no embasamento a sudeste da Bacia do Parnaíba, com pequena contribuição de sedimentos oriundos de rochas do Domínio Ceará Central e da porção ocidental do Domínio Rio Grande do Norte. No Famenniano, a movimentação do supercontinente Gondwana para o polo sul culminou na implantação de condições glaciais concomitantemente com o rebaixamento do nível do mar e exposição da região costeira. O avanço das geleiras sobre o embasamento e depósitos deltaicos gerou erosão, deposição de diamictons com clastos exóticos e facetados, além de estruturas glaciotectônicas tais como plano de descolamento, foliação, boudins, dobras, duplex, falhas e fraturas que refletem um cisalhamento tangencial em regime rúptil-dúctil. O substrato apresentava-se inconsolidado e saturados em água com temperatura levemente abaixo do ponto de fusão do gelo (permafrost quente). Corpos podiformes de arenito imersos em corpos lenticulares de diamicton foram formados pela ruptura de camadas pelo cisalhamento subglacial. Lentes de conglomerados esporádicas (dump structures) nos depósitos de shoreface sugere queda de detritos ligados a icebergs em fases de recuo da geleira. A elevação da temperatura no final do Famenniano reflete a rotação destral do Gondwana e migração do polo sul da porção ocidental da América do Sul e para o oeste da África. Esta nova configuração paleogeográfica posicionou a Bacia do Parnaíba em regiões subtropicais iniciando o recuo de geleiras e a influência do rebound isostático. O alívio de pressão é indicado pela geração de sills e diques clásticos, estruturas ball-and-pillow, rompimento de camadas e brechas. Falhas de cavalgamento associadas à diamictitos com foliação na borda oeste da bacia sugerem que as geleiras migravam para NNE. O contínuo aumento do nível do mar relativo propiciou a instalação de sedimentação deltaica durante o degelo e posteriormente a implantação de uma plataforma transgressiva (Formação Longá). Diamictitos interdigitados com depósitos de frente deltaica na porção superior da Formação Cabeças correspondem a intervalos com baixo volume de poros e podem representar trapas estratigráficas secundárias no reservatório. As anisotropias primárias subglaciais do topo da sucessão Cabeças, em ambas as bordas da Bacia do Parnaíba, estende a influência glacial e abre uma nova perspectiva sobre a potencialidade efetiva do reservatório Cabeças do sistema petrolífero Mesodevoniano-Eocarbonífero da referida bacia.
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On the grounds of the great advances achieved over recent years, the process HF/ERW (High-Frequency/Electric Resistance Welding)welded pipe have played an active role in the oil and gas industry for deep water applications, at high and extremely low temperatures, under high pressure and in highly corrosive environments, gradually replacing manufactured pipes by other processes. However, studies have shown that defects in the welded joints are a the leading causes of pipelines failures, which has required the determination of toughness values in this region, in compliance with the strict recommendations of the codes and standards with manufacturers and construction companies, on the oil and gas sector. As part of the validation process required toughness values, this research project focuses on a microstructural analysis in HF / ERW tubes microalloyed, steel grade API 5CT P110, designed to explore oil and gas in deep waters, the subject of strategic relevance to the country because of the recent discoveries in the Santos mega fields: Tupi and Libra (pre-salt). In this scientific work will be presented and discussed the results of mechanical tensile and Charpy, a few CTOD tests curves (showing the trend of toughness values to be obtained), and the microstructures of the base material obtained by optical microscopy, with special emphasis on the formation of nonmetallic inclusions in the welded joint
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The oil market is not a common market, and its complexity increases dramatically when considering the strategic and geopolitical involved, thus resulting in large uncertainties and concerns. The attempt to control prices has always been a challenge for the major world powers, since the increase in oil prices benefits the exporting countries, but harms importers, especially those regarded as less developed. Understand and try to predict some strategies adopted up the oil crises is one of the main points of the research, in order to demonstrate how economics can be used as an instrument of power and domination between nations, and how plans and strategies and rearrangements of supply and demand favor the growth of this economy, especially in the current period, with the new Brazilian oil era, beginning with the discovery of pre-salt, amid a context of growing need for the use of oil and its derivatives
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Acoustic communication is essential in mammals and has three main functions: acquisition of information about the environment, intraspecific communication and detection of predators and prey. Studies indicate that the introduction of sounds produced by anthropogenic activities such as military exercises, use of sonar and activities related to the extraction of oil and natural gas can cause interference in cetacean communication. Recently, the discovery of pre-salt tends to increase these activities. After a decade since the launch date of IBAMA`s licensing and before the imminent increase in exploration activities in Brazil, it is essential to conduct studies to monitor closely the impact of this type of activity on the marine ecosystem. Thus, this study aims to identify potential impacts that the process of oil and natural gas exploration and production might have on the communication of baleen whales. Data from literature on bioacoustics and ecology of these animals were linked with technical-scientific data regarding this type of activity. 310 documents related to the topic were analyzed. Among them only 81 documents are of academic origin, and the others mostly action plans and reports from government agencies. 80% of the documents do not have any species as a focus, and in the remaining 20%, 17% were focused on the Greenland Whale (Balaena mysticetus) and 22% on the gray whale (Eschrichtius robustus). The main impacts identified in this study were the increased frequency and amplitude of vocalization, reduction or cessation of more elaborate songs and masking problems
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Since it was proposed, the Ibsen Pinheiro amendment has given rise to a huge debate in Brazilian society. This amendment proposes to share the revenue generated by royalties and special participations from offshore oil drilling between all municipalities and states, using for this the states and municipalities participation funds. This new distribution is a great rupture with the current model, which mandates that these resources should only be distributed to producing municipalities and states. Since the new proposal affects all offshore operations, and not only those in the new pre-salt areas, the producing municipalities and states would face an immediate loss of revenue in the scale of billions of reais. This study's objective is to analyze the validity of the criteria of redistribution of the government participations proposed by the Ibsen amendment. In this sense, we present the current Brazilian government participation model, focusing on the overfinancing of subnational spheres generated by this model, and compare it to a distribution simulation using the Ibsen amendment criteria. This comparison shows that the current beneficiaries would face a significant loss of revenue, and a distribution that favors the poorest regions of the country, consequence of the states and municipalities participation funds use. The study's last part discusses the various arguments in favor and against the amendment, especially those of constitutional character, most of which are contrary to the Ibsen amendment
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Given the intense expansion of the industries in Brazil and the discovery of hydrocarbons in the pre-salt layer of the Santos and Campos Basin, there is a need to expand the distribution of oil and gas network in the country. The present work aims to present the development of susceptibility map by two distinct methods of two events (debris flows and full wave), applied to the establishment of pipelines on Ribeirão da Prata Basin. The research area covers two municipalities: São João da Boa Vista and Águas da Prata, in total 145 km2. In the paper was used the methodology proposed by Zaine (2011) for the physiographic subdivision method, which uses geological maps, geomorphological maps, digital terrain models and aerial photographs, used to extract the main elements of the physical environment, as rivers, lines, ridges, tops forms and valley forms and historical processes. Thus, the basin was divided into 11 physiographic zones, considering the following elements: thickness of soil, rock type, geomorphology, amplitude, ridges orientation, erosion occurences and mass movements. Were subsequently performed location maps of dams, that had as main purpose to localize major dams in the study area along with their area and perimeter of the reservoir, and land use map that subdivided the area in woody vegetation, permanent culture, temporary culture and urban area. Along with the preparation of the auxiliar maps was conducted a field campaign with three days and approximately 2 points per km2, which aimed to better understand the physical environment and check the main peculiarities of the study area. Criteria have been established for susceptibility maps physiographic subdivision and land use, and a survey of criteria weights used in each map for both processes under study. For the preparation of susceptibility maps were adopted two different methods, which treat the weighted average and the multiplicand. The weighted average method it is...
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The analysis of the extraction process in oil wells is presented exploring the challenges to the effectiveness of the procedure is shown step by step in the process. There is an analysis of the major tools and equipment needed in the drilling process, promoting the understanding of the challenges in the pre-salt layers, compared to conventional processes. The work is reinforced through studies of the influence of the corrosive compared not corrosive environment in drill strings
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The objective of the research is to map and analyze the investment, strategies of develop and prospects of green chemical industry in Brazil and show the fundamental importance of basic research and applied research in the development of this industry in recent years. The complementary objectives are: (i) to evaluate the role of the Brazilian government as a catalyst, encouraging the development of green chemistry industry through incentives, subsidies and ease in credit lines; ii) mapping of relationships between companies universities and public research institutes in the field of green chemistry; iii) verification of the strategies in the world stage green chemistry, the course of time; iv) the theoretical issues and national plans, and your practicable; v) continued investment in the area, with the worry of them being affected by any matter cyclical such as the discovery of a large deposit of shale gas in the United States and a technological development of oil extraction in Brazil and vi) the pace of R&D for basic and applied in the country with the passage of time
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This paper presents a study based on literature and examples found on literature of the potential of petroleum gas to be used as a primary source to generate electricity. The steady increase electricity demand in Brazil makes desirable an effective use of all available primary sources, combined with this need the momentum of the country with the discovery of the presalt reserves becomes interesting the use of this gas, often wasted, for generating electricity. The electricity generation in this work is illustrated by the cogeneration in oil refining plants that have the combined cycle thermal operation. The ultimate goal is to provide a text to identify the advantages, disadvantages and trends of this type of generation
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On the grounds of the great advances achieved over recent years, the process HF/ERW (High-Frequency/Electric Resistance Welding)welded pipe have played an active role in the oil and gas industry for deep water applications, at high and extremely low temperatures, under high pressure and in highly corrosive environments, gradually replacing manufactured pipes by other processes. However, studies have shown that defects in the welded joints are a the leading causes of pipelines failures, which has required the determination of toughness values in this region, in compliance with the strict recommendations of the codes and standards with manufacturers and construction companies, on the oil and gas sector. As part of the validation process required toughness values, this research project focuses on a microstructural analysis in HF / ERW tubes microalloyed, steel grade API 5CT N80, designed to explore oil and gas in deep waters, the subject of strategic relevance to the country because of the recent discoveries in the Santos mega fields: Tupi and Libra (pre-salt). In this scientific work will be presented and discussed the results of mechanical tensile and Charpy, a few CTOD tests curves (showing the trend of toughness values to be obtained), and the microstructures of the base material obtained by optical microscopy, with special emphasis on the formation of non-metallic inclusions in the welded joint
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Pós-graduação em Geologia Regional - IGCE
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Pós-graduação em Economia - FCLAR
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The Areado Group of the Sanfranciscana Basin is a Lower Cretaceous continental sedimentary system that is correlated to the Brazilian Pre-Salt beds. The Aerado Group is composed of Abaeté, Quiricó and Três Barras formations. Paleocurrent data for the Areado Group were previously presented, although not systematically which prevented significative interpretations on the basin paleogeography. This work attempts to systematically evaluate paleocurrent data, aiming to recognize depositional environment and paleogeographic reconstruction, based on the sedimentary facies and paleocurrents measurements along vertical profiles. Fluvial paleocurrents of the Abaeté Formation indicate paleoflows towards NW whereas aeolian palecurrents of the Três Barras Formation show paleowinds towards SW. The depositional systems interpreted for the Areado Group were: braided river, alluvial fan, lacustrine, playa lake, fluvial-deltaic and aeolian. The combined analyses of facies and paleocurrents allowed a reliable paleogeographic reconstruction of the basin, with paleodip towards northwest, paleowinds towards south-southwest and source-area located at southeast. These results indicate that paleowinds were orthogonal to paleostream, but parallel to depositional strike of the basin. The interpreted depositional systems characterize a desert environment during the Abaeté sub-basin times. The association of dunes and wet interdunes followed by large scale dunes and dry interdunes suggests a decrease in humidity towards the top of the Três Barras Formation, with a dry aeolian system onlapping the basement. The observed decrease of humidity in Sanfranciscana Basin may reflect local or regional paleoclimatic changes during the opening of the South Atlantic, but this assumption is only tentative