32 resultados para message passing


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Tese de Mestrado em Engenharia Electrotécnica e de Computadores

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IEEE International Symposium on Circuits and Systems, pp. 724 – 727, Seattle, EUA

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Thesis presented in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of Electrical and Computer Engineering

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Dissertação apresentada para a obtenção do Grau de Doutor em Informática pela Universidade Nova de Lisboa, Faculdade de Ciências e Tecnologia

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A Work Project, presented as part of the requirements for the Award of a Masters Degree in Management from the NOVA – School of Business and Economics

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(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-EfE-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing oeean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

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Les rapports complexes entre les différentes façons de faire circuler les idées et les informations ne datent pas de nos jours. A toutes les époques, les messages qui circulent emploient toutes sortes de véhicules et de langages, très souvent complémentaires. Ces véhicules et ces langages n'ont peut-être rien d'extraordinaire. Ils appartiennent au monde des gestes de tous les jours, des gestes qui se répètent et dont la répétition est elle-même importante pour la construction du sens de chaque message. Ces gestes qui sont répétés, qui sont attendus et qui sont reconnus incluent des sons, des images, des comportements, des mots, ou des citations. Il y a donc un rapport qui s'y établit entre répétition et nouveauté, rapport dans lequel la répétition fournit chaque fois une nouvelle information, même si elle est déjà attendue, tandis que leur absence peut représenter l'anxiété, ou même le scandale.

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Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para obtenção do grau de Mestre em Engenharia Informática

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Trabalho apresentado no âmbito do Mestrado em Engenharia Informática, como requisito parcial para obtenção do grau de Mestre em Engenharia Informática

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(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-E/E-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing ocean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

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A synthesis about the Neogene and Quaternary of Algarve (Southern Portugal) is presented. New isotopic 87Sr/86Sr ages as well as biostratigraphic data about the Miocene deposits allow to present a new stratigraphic frame for the previously characterized units. The Lagos-Portimão Formation corresponds to deposits of temperate carbonate platform sedimentological type, developed during a long time span (Lower Burdigalian to Upper Serravallian). A major change in sedimentation conditions (carbonate to siliciclastic environments) occurred in the Lower Tortonian with the deposition of yellowish sands. Spongoliths rich in microfossils are represented in Algarve inland. Their age is not well established; calcareous nannofossils indicate the CN5a zone (Upper Serravallian) while foraminifera point out at least Nl6 zone (Lower Tortonian). In the Upper Tortonian, the sedimentation is widespread in Eastern Algarve, related with the Guadalquivir Basin infill. The deposits begin with detrital limestones, locally very rich in Heterostegina, passing to fossiliferous conglomerates and siltstones (Cacela Formation). Coarse-grained conglomerates at Galvana (Faro) pose some age problems. K/Ar age on glauconite indicates 6.72±0.17 Ma. However, glauconites may be reworked from older deposits (Cacela Formation). The Galvana Conglomerate could be related to Pliocene deposits are not well characterized. Olhos de Água sands, with a thin marine intercalation rich in marine vertebrates (fishes, a crocodile, cetaceans, sirenians), may be Upper Pliocene; however, the vertebrates point out to a Serravallian to Tortonian age. 87Sr/86Sr ages on oysters from above the level with vertebrates point out to 3.0(+2.5-1.0) Ma. Similar sand deposits occur at Morgadinho (Luz de Tavira). These sands are overlain by marls, lignite clays, lacustrine limestones and a silty calcareous crust. A small mammals association indicate an age span between Upper Pliocene and Lower Middle Pleistocene (MN17-MN20). A Biharian mammal fauna (Lower Pleistocene) was collected at Algoz in similar deposits. In the present state of knowledge, Morgadinho and Algoz deposits may be correlative.

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The Peniche section has revealed moderately-to-well preserved calcareous nannofossil assemblages across the Pliensbachian/Toarcian boundary. This good record has allowed the proposition of a refined biostratigraphic scheme. The stage boundary, as defined by ammonites, is comprised within the NJ5b C. impontus (NW Europe; BOWN & COOPER, 1998) or the NJT5b L. sigillatus (Mediterranean Tethys; MATTIOLI & ERBA, 1999) nannofossil subzones. Since in the Lusitanian Basin a mixing of N- and S-Tethyan taxa is observed, both biozonation schemes can be applied. Some nannofossil events (mainly first occurrences) are observed earlier in Portugal than in other Tethyan settings. It is still unclear if these events are real first occurrences. A diversification phase occurred across the Pliensbachian/Toarcian boundary. This phase is well recorded at Peniche, where a change is observed passing from the Pliensbachian, when assemblages are dominated by muroliths, to the Toarcian showing assemblages where placoliths are abundant. A quantification of nannofossils per gram of rock shows that absolute abundances are the highest across the Pliensbachian/Toarcian boundary. Indeed, Peniche exhibits nannofossil abundances very high with respect to correlative levels in other Tethyan settings. The pelagic carbonate fraction (produced by nannofossils) is important in the marly hemi-couplets of Peniche. In some levels, nannofossils account for more than 50% of the total carbonate fraction.

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A investigação científica que se seguiu à descoberta da infecção pelo vírus da imunodeficiência humana (VIH) representou um marco histórico importante, permitindo a instituição de terapêutica e alterando a história natural da infecção, melhorando as expectativas dos indivíduos infectados.Se, por um lado, a terapêutica antirretroviral de alta eficácia (do inglês, Highly Active Antiretroviral Theraphy: HAART), nos países desenvolvidos, teve um enorme impacto na melhoria da qualidade de vida e esperança média de vida dos indivíduos infectados, permitindo-lhes encarar a infecção como uma doença crónica, por outro lado, introduziu-se uma nova dinâmica epidemiológica na transmissão de VIH e um novo desafio para a sua prevenção.Os comportamentos sexuais são o factor-alvo através do qual se pode, de uma forma mais eficaz, prevenir a possibilidade de infectar um qualquer indivíduo na comunidade. Parece, pois, importante haver necessidade de um olhar atento da Saúde Pública sobre a vida sexual dos indivíduos infectados, não só na tentativa de, promover a sua qualidade de vida, como também, de prevenir a disseminação da doença, e, ainda mais importante, prevenir a disseminação do vírus nas suas formas resistentes.O objectivo deste estudo foi analisar a consistência do uso de preservativo/práticas de sexo seguro, em indivíduos infectados por VIH, seguidos em Consulta de Imunodepressão, do Serviço de Doenças Infecciosas, do Hospital de Santa Maria. Pretende-se avaliar, no âmbito da “Educação para a Saúde”, a necessidade de aconselhamento aos indivíduos infectados, relativamente aos seus comportamentos sexuais.Para o efeito, realizou-se um estudo descritivo e transversal. A população envolvida compreendeu todos os indivíduos infectados seguidos na Consulta de Imunodepressão. A amostra foi seleccionada através de aleatorização simples e constituída por 98 elementos. A colheita de dados foi efectuada através do método de entrevista, a qual só teve início após a assinatura do consentimento informado. O estudo decorreu entre 14 de Março e 27 de Junho de 2008.Foram analisados os dados relativamente às variáveis: sócio-demográficas, estado serológico da infecção, história sexual, consumo de substâncias, comportamento sexual e percepção de risco da transmissão da infecção por VIH.Os comportamentos de sexo não seguro foram associados ao número de parceiros sexuais/ano (p=0,007), ter parceiro sexual habitual (p=0,010), ter múltiplos parceiros sexuais ocasionais (p=0,000) e à prática de sexo oral (sexo oral receptivo, p=0,001; sexo oral activo, p=0,006).Os resultados demonstraram a importância da prevenção secundária nos indivíduos infectados por VIH. A necessidade dos centros de atendimento estarem providos de mensagem de prevenção, ensinos e aconselhamento a todas as pessoas infectadas e, também, aos seus parceiros sexuais, aumentando-lhes a qualidade de vida e reduzindo o risco de transmissão da infecção por HIV. ABSTRACT: The scientific research that followed the finding of human immunodeficiency virus (HIV) infection represented an important historical mark, allowing therapeutic institution and changing the natural history of the infection, thus improving the expectations of infected individuals. If by one side the Highly Active Antiretroviral Therapy (HAART) had an enormous impact on the improvement of life quality and life expectancy of the infected individuals on the developed countries, allowing them to face the infection as a chronic disease, on the other side it was introduced a epidemiologic dynamic on the HIV transmission and a new challenge for its prevention. Sexual behaviour is the main factor through which is possible to prevent more efficiently the possibility of infection of a community’s individual. Thus it appears important the need of Public Health to have a careful look into the sexual life of infected individuals, not only to try to promote their life quality but as well to prevent the dissemination of the disease and more importantly prevent the dissemination of the virus in its resistant forms. The objective of this study was to analyse the consistency of the use of condoms/safe sex by individuals infected by HIV that are followed by the Infectious Disease Service of the Santa Maria Hospital through Immune-depression Appointments. The goal was to evaluate the need of advisement to the infected individuals relatively to their sexual behaviours. For that it was done a descriptive and transversal study. The involved population included all infected individuals followed in the Immune-depression Appointments. The sample was selected by simple randomisation and was composed by 98 elements. The data was obtained by interview method, which was initiated after signing the informed consent. The study was took place between 14 March and 27 June 2008. It was analysed the data relative to the variables: socio-demographics, serologic state of the infection, sexual history, substances consumption, sexual behaviour and risk perception on the transmission of HIV infection. The unsafe sexual behaviours were associated to the number of sexual partners/year (p=0,007), having steady partner (p= 0,010), having occasional sexual partners (p=0,000) and oral sex practice (receptive oral sex, p=0,001; active oral sex, p= 0,006).The results demonstrated the importance of the secondary prevention on individuals infected by HIV. It also demonstrated the need of providing the attendance centres with a prevention message, teachings and advises to all infected persons as well as to their sexual partners, increasing their life quality and reducing the transmission risk of HIV infection.

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Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para obtenção do grau de Mestre em Engenharia Informática

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RESUMO - A flexibilidade dos contratos de trabalho é cada vez mais uma realidade. Em 2009, cerca de 18% da população activa em Portugal tinha um vínculo instável. Na instituição onde se realizou o estudo, 38,8% dos profissionais de saúde têm este tipo de vínculo. Este estudo foi realizado num hospital distrital com a participação de 103 prestadores de cuidados directos – assistentes operacionais, enfermeiros, médicos e técnicos de diagnóstico e terapêutica - aos quais foi dado um questionário de auto-resposta. Através deste, fez-se a comparação dos níveis de satisfação dos profissionais com diferentes tipos de vínculo. Concluiu-se que as dimensões mais valorizadas são as relacionais e condições de trabalho e saúde. A dimensão da Segurança no Emprego surge no meio da tabela. Ao contrário do que dizem os estudos, a autonomia e poder foi das menos valorizadas. Os profissionais com vínculo laboral instável dão maior importância à segurança. As dimensões relacionais são as que apresentam maiores níveis de satisfação. As que apresentam menores níveis são a Remuneração, Condições de Trabalho e Saúde e Segurança no Emprego, sendo que nesta ultima se registam diferenças significativas entre profissionais com diferentes tipos de vínculo. Verifica-se com 95% de confiança que existem diferenças significativas na dimensão da Segurança no Emprego, onde os profissionais com vínculo instável apresentam menores níveis de satisfação. Os profissionais com vínculo instável demonstram que este facto lhes trouxe consequências negativas ao nível pessoal e social. Não existe significância na diferença entre os níveis da satisfação dos profissionais de saúde com diferentes vínculos. -----------------------------------ABSTRACT - Employment contract flexibility is becoming a reality with each passing day. In 2009, around 18% of the active population in Portugal had an unstable bond. In the institution where this study was conducted, 38.8% of the health professionals have this kind of arrangement. This study was conducted in a district hospital with the participation of 103 direct care providers - operating assistants, nurses, doctors and technical diagnostic and therapeutic - that were given a self-response questionnaire. Through this questionnaire, the levels of satisfaction of the professionals with different types of employment bond were compared. It was concluded that the most valued dimensions are relational and work and health conditions. Work security appears in the middle of the table. Contrary to what studies say, autonomy and power were less valued. Professionals with an unstable bond give greater importance to safety. The relational dimensions are those with higher levels of satisfaction. Those with lower levels are the wages, working conditions and health and safety in employment, where in health and safety in employment show significant differences between professionals with different types of employment bond. We can verify with a 95% confidence interval that there are significant differences in the work safety dimension, where professionals with unstable employment bonds present lower levels of satisfaction. Professionals with an unstable employment bond show that this fact brought them negative consequences at the personal and social level. There is no significant difference between the levels of satisfaction of health professionals with different types of employment bond.