Radiação por fenda em guia de ondas

Dissertação para obtenção do Grau de Mestre em Engenharia Electrotécnica e de Computadores

O provérbio: um género marginal(izado)?!

Enquanto o provérbio, numa cultura de tradição oral, representa tipicamente o tesouro do conhecimento e a colecção das regras sociais ou jurídicas, na transição para a cultura escrita e na formulação científica dos saberes, esse género da Literatura Tradicional perde a sua autoridade nos círculos dominantes da sociedade. Ressalve-se, porém, o facto de, ao longo desse processo, haver ciclos.

Managing marginal capital requirements in solvency II: Analysis of a real insurance portfolio

This thesis provides a complete analysis of the Standard Capital Requirements given by Solvency II for a real insurance portfolio. We analyze the investment portfolio of BPI Vida e Pensões, an insurance company affiliated with a Portuguese bank BPI, both at security, sub-portfolio and asset class levels. By using the Standard Formula from EIOPA, Total SCR amounts to 239M€. This value is mostly explained by Market and Default Risk whereas the former is driven by Spread and Concentration Risks. Following the methodology of Leblanc (2011), we examine the Marginal Contribution of an asset to the SCR which allows for the evaluation of the risks of each security given its characteristics and interactions in the portfolio. The top contributors to the SCR are Corporate Bonds and Term Deposits. By exploring further the composition of the portfolio, our results show that slight changes in allocation of Term and Cash Deposits have severe impacts on the total Concentration and Default Risks, respectively. Also, diversification effects are very relevant by representing savings of 122M€. Finally, Solvency II represents an opportunity for the portfolio optimization. By constructing efficient frontiers, we find that as the target expected return increases, a shift from Term Deposits/ Commercial Papers to Eurozone/Peripheral and finally Equities occurs.

A reconnaissance study of Upper Jurassic sediments of the Lusitanian Basin

The Upper Jurassic evolution of the Lusitanian Basin is shown to be linked to the rifting phase which preceded the separation of Iberia and the Grand Banks. Structural controls on sedimentation include both NNE-SSW trending faults in the Hercynian basement, and contemporaneous movement of salt diapirs. At the beginning of Upper Oxfordian times, the entire basin had been levelled to within a few metres of sea level, so that the freshwater algal marsh and marginal marine facies of the Cabaços and Vale Verde Beds rest on Triassic to Callovian strata. In the latter part of the Upper Oxfordian. carbonate sedimentation continued, with fluctuating salinity lagoons in the north (Pholodomya protei Beds) separated from shallow open marine carbonates in the south (Montejunto Beds) by the Caldas da Rainha diapir-barrier island complex. The commencement of rifting is recorded in the Kimmeridgian by the sudden influx of terrigenous clastics (developed in both fluviatile and deltaic/submarine fan environments) and accelerated depositional rates in excess of 10cm/10 k.yrs in association with contemporaneous faulting along the SE margin of the Arruda sub-basin. The Caldas-Santa Cruz chain of diapiric structures continued to influence the distribution of carbonate and clastic sediments. In the Portlandian, a simpler facies pattern occurs, with fluviatile clastics interfingering to the south with shallow low energy carbonates.

The Farrell and Shapiro condition revisited

The purpose of this paper is to study the consequences of using the Farrell and Shapiro (1990) sufficient condition for merger approval to sectors in which a downstream horizontal merger may also affect upstream firms. As will be shown below, in some circumstances the sign of the relevant external effect can no longer be established by considering the merger as a sequence of in finitesimal mergers, each corresponding to a marginal change in output.

Synthesis of the Piacenzian onshore record between the Aveiro and Setubal parallels (Western portuguese margin)

Onshore, the Piacenzianof the Mondego and Lower Tagus Tertiary basins comprises siliciclastic sediments deposited in shallow marine to continental environments. The outcrops of the deposits are relatively widespread in the Aveiro and Seuibal region. A lithostratigraphic synthesis based on the correlation of geological sections, is presented for the two basins. In general, the Piacenzian sediments display a regressive sucession. The Late Tortonian-Zanclean (?) confined drainage pattern changed at the beginning of Piazencian, to fluvial systems draining to the Atlantic, and capturing the drainage of the inner parts of the Hesperic Meseta. The Piacenzian sedimentary sequence post-dates one of the uprising phases during Neogene compression, recorded by a strong regional unconformity. Some local active faulting - as in Lousa, Rio Maior and Senibal- Pinhal Novo - allowed the local thickening of the sedimentary record. Later compressive tectonism continues to generate reverse faulting and diapiric reactivation, affecting those sediments. Currently, the Piacenzian deposits culminates the marginal piedmonts, widely eroded by the Quaternary fluvial dissection.

Children, space, and the urban street: an ethnomathematics posture

Dissertation presented for the PhD Degree in Education Science – Curricular Theory and Science Teaching, by Universidade Nova de Lisboa, Faculdade de Ciências e Tecnologia

Synthesis of the Piacenzian onshore record between the Aveiro and Setúbal parallels (Western portuguese margin)

Onshore, the Piacenzian of the Mondego and Lower Tagus Tertiary basins comprises siliciclastic sediments deposited in shallow marine to continental environments. The outcrops of the deposits are relatively widespread in the Aveiro and Setúbal region. A lithostratigraphic synthesis based on the correlation of geological sections, is presented for the two basins. In general, the Piacenzian sediments display a regressive sucession. The Late Tortonian-Zanclean (?) confined drainage pattern changed at the beginning of Piazencian, to fluvial systems draining to the Atlantic, and capturing the drainage of the inner parts of the Hesperic Meseta. The Piacenzian sedimentary sequence post-dates one of the uprising phases during Neogene compression, recorded by a strong regional unconformity. Some local active faulting - as in Lousa, Rio Maior and Senibal- Pinhal Novo - allowed the local thickening of the sedimentary record. Later compressive tectonism continues to generate reverse faulting and diapiric reactivation, affecting those sediments. Currently, the Piacenzian deposits culminates the marginal piedmonts, widely eroded by the Quaternary fluvial dissection.

Depósitos continentais e marinhos na plataforma litoral da região do Porto. Importância da tectónica na sua organização espacial

One of the most common characteristics of Portuguese littoral is the existence of a planed surface (the so-called "littoral platform"), situated at different altitudes and bordered from the inland by a straight relief, strongly contrasting with that planed surface. This one is generally covered with several outcrops of the so-called Plio-Pleistocene deposits. Till the eighties this platform has been interpreted as stable staircase of old marine levels, registering in a passive way the eustatic variations. The rigid step bordering it easterly should be a fossil cliff. However, our study has proved that many of these deposits have a continental origin. These continental deposits have fluvial or alluvial fan facies and they are lying above 40 meters. Marine deposits seem to be quite rare and they only occupy a small western area, beneath the altitude of 40 meters and developing into three different marine levels. There is a rigid step between the two kinds of deposits. We think that the clear geometric separation between these deposits together with this rigid step, indicates a tectonic origin. It seems that the sea must have touched only the western part of this surface, when neotectonic movements lowered it down. There are more evidences for neotectonic movements: a) there are faults (mainly inverse faults) affecting the higher deposits of this littoral platform; b) the same marine level seems to appear at different altitudes, developing an irregular pattern with a general trend dipping from the North to the South.

Gestão dos custos dos acidentes de trabalho em meio hospitalar

RESUMO - No contexto económico actual, os custos pelos acidentes devem ser tidos em conta por todos os gestores das organizações, com especial destaque ao sector da saúde. Assim a análise económica deste estudo visa alertar para o impacto económico dos acidentes de trabalho em contexto hospitalar e sensibilizar os gestores para a análise do custo-beneficio da prevenção. Existem custos facilmente constatáveis, tais como, o tempo perdido no dia do acidente, quer pelo sinistrado quer pelos colegas de trabalho que o assistem, as despesas de uma ida ao serviço de urgência, a paragem da produção, a formação de mão-de-obra alternativa, a substituição dos trabalhadores, o pagamento de horas extras, o restabelecimento dos trabalhadores, os salários pagos aos trabalhadores sinistrados, as despesas administrativas e o aumento do prémio do seguro, entre outros. Existem outros custos que não são tão evidentes e por conseguinte, dificilmente quantificáveis, como é o caso da deterioração da imagem da empresa e o impacto sentimental que estes provocam nos colegas de trabalho que se traduz em quebras de produtividade. A análise económica foi realizada tendo em conta a definição de várias variáveis, de várias rubricas de custos pertencentes ao mesmo domínio. Neste projecto pretende-se analisar o custo global da sinistralidade segundo três ópticas distintas. A óptica da variabilidade, da imputabilidade e da responsabilidade, de forma a ser possível obter o custo marginal devido à ocorrência de um novo acidente, o montante de custos assumidos pelas empresas e os custos unitários segundo a natureza e a localização da lesão. ---------- ABSTRACT - In the current economic context, the costs originated by labour accidents must be taken in account by all the managers of the organisations, in this case, especially by the health sector. Thus, the economic analysis of this study case aims, to alert for the economic impact of the industrial accidents and motivate the managers for the analysis of the cost-benefit for prevention. There are kinds of costs easily quantified such as, the lost time in the day of the accident, expenses in the urgencies service, production interruption, workforce formation, workers’ substitution, extra work payment, employers’ healing, wages paid to injured workers’, administrative expenses and a biggest insurers’’ prime, among other things. The economic analysis of the labour injuries, was developed taking in account the definition of some variables, of some cost categories which belong to same domain. In this project we pretend to analyse the global cost labour injuries according to three distinct optics: variability, imputability and responsibility. Thus, it became possible to get the cost due to an occurrence of a new accident, the unitary sum of costs assumed by the companies and costs according to nature and the localisation of the injury.

Estudo clínico da oncocercose na Guiné-Bissau

Em África e no Sul da Arábia, a oncocercose está essencialmente associada ao complexo Simulium damnosum (Ovazza, 1967). A propagação da doença resulta essencialmente do tipo de actividade humana, e das alterações do ambiente, especìalmente a desflorestação maciça, transformando o habitat florestal em habitat de savana (Hocking, 1953, Dadzie, 1980, Amazigo, 1991, Amazigo, 2002 a, WHO, 1995 b). 2- Morfologia 2.1 - O ovo O ovo, têm uma forma triangular, com os vértices arredondados, medindo de 0,1 a 0,5 mm de comprimento. A casca é lisa, não apresentando qualquer adaptação especial e o revestimento é viscoso. São de cor branca aquando da oviposição, escurecendo com a embriogénese, aparecendo então com cores rosadas, amareladas e acinzentadas. 2.2 - A larva A larva dos simulídeos, apresenta um formato mais ou menos cilíndrico, com duas dilatações, uma no tórax, ligeira e outra mais acentuada na parte terminal do abdómen. Pode atingir o comprimento de um centímetro, e uma coloração muito variada, dependendo do tipo de alimentos ingeridos, e apresentar-se de coloração totalmente escura, a esbranquiçada. O corpo da larva é formado por três partes distintas – a cabeça, o tórax e o abdómen. A cabeça: A cabeça de uma larva de simulídeo, à observação dorsal, apresenta-se pigmentada, podendo com essa pigmentação expressar-se de duas formas, ou com manchas escuras em fundo claro (modelo positivo), ou manchas claras em fundo escuro (modelo negativo), e um par de finas antenas. Á observação ventral destacam-se dois caracteres de grande valor sistemático – a fenda pósgenal e o hipostoma.

Estudo numérico do galgamento de estruturas de protecção costeira

Dissertação para obtenção do Grau de Mestre em Engenharia Civil - Perfil de Estruturas

Caracterização do betão reforçado com fibras de aço

Dissertação para obtenção do Grau de Mestre em Engenharia Civil-Perfil de Estruturas

A utilização de actos complementares de diagnóstico: uma análise económica

Dissertação submetida para obtenção do grau de Doutor em Saúde Pública Especialidade de Economia da Saúde

Impact of health conditions on absenteeism from work

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