Simulation of a resonant inverter

Mostly developed since the Industrial Revolution, the automation of systems and equipment around us is responsible for a technological progress and economic growth without precedents, but also by a relentless energy dependence. Currently, fossil fuels still tend to come as the main energy source, even in developed countries, due to the ease in its extraction and the mastery of the technology needed for its use. However, the perception of its ending availability, as well as the environmental impact of this practice has led to a growing energy production originated from renewable sources. Easy maintenance, coupled with the fact that they are virtually inexhaustible, makes the solar and wind energy very promising solutions. In this context, this work proposes to facilitate energy production from these sources. To this end, in this work the power inverter is studied, which is an equipment responsible for converting DC power available by solar or wind power in traditional AC power. Then it is discussed and designed a new architecture which, in addition to achieve a high energy e - ciency, has also the ability to adapt to the type of conversion desired by the user, namely if he wants to sell electricity to the power grid, be independent of it or bet on a self consumption system. In order to achieve the promised energy e ciency, the projected inverter uses a resonant DC-DC converter, whose architecture signi cantly decreases the energy dissipated in the conversion, allowing a higher power density. The adaptability of the equipment is provided by an adaptive control algorithm, responsible for assessing its behavior on every iteration and making the necessary changes to achieve maximum stability throughout the process. To evaluate the functioning of the proposed architecture, a simulation is presented using the PLECS simulation software.

Estratégia de desenvolvimento sustentável do turismo na Ria de Aveiro

O turismo costeiro é a atividade turística mais relevante em Portugal. Este facto deve-se essencialmente à extensa e diversificada linha de costa e à crescente procura destas áreas pelas suas características paisagísticas, que levou a um forte desenvolvimento da atividade turísticas ao longo das últimas décadas. No entanto, o turismo que se tem vindo a praticar nas áreas costeiras portuguesas não responde às questões da sustentabilidade que cada vez mais estão na base da competitividade dos destinos turísticos. A garantia de sustentabilidade e a atração pelo novo e pelo diferente são fatores essenciais à capacidade de atração e competitividade de um determinado território. O sector turístico não foge à regra. Como tal é necessário inverter o modelo massificado que caracteriza o turismo costeiro e inovar nos métodos e nos modelos de desenvolvimento deste turismo A região da Ria de Aveiro, composta por 11 municípios, é uma região com fortes potencialidades turísticas, mas que se encontram subaproveitadas ou incorretamente geridas. Esta região apresenta um forte potencial para a prática de um turismo sustentável, valorizando os recursos naturais e culturais que possui. É uma região que tem como ponto de conexão a “Ria de Aveiro”, sendo uma das principais zonas húmidas do território português. Além da Ria, possui variadíssimos recursos turísticos tais como praias marítimas e fluviais, frentes ribeirinhas, marinhas de sal, florestas, áreas de interesse conservacionista, aldeias serranas, património arquitetónico, nomeadamente religioso, casas de interesse (arte nova, palheiros), museus, azulejaria, estações arqueológicas, entre outros. A proximidade entre o mar e a serra cria condições para a diversificação da paisagem, surgindo áreas tipicamente serranas que contrastam com a planície costeira e lagunar. Esta variedade de recursos constitui uma excelente oportunidade para os municípios que compõem a região, porque podem ajudar a definir e a sustentar estratégias de desenvolvimento turístico mais competitivas e associadas ao quadro de recursos naturais disponíveis. É necessário, assim, uma aposta nas singularidades e especificidades da região, oferecendo o que outros destinos não conseguem oferecer, através da exploração sustentável dos recursos endógenos. No entanto, é fundamental existir vontade política para que se possam promover e aplicar estratégias de turismo sustentável neste território. Pretende-se com este trabalho apresentar um modelo estratégico para o sector do turismo da região da Ria de Aveiro, através de uma abordagem diferenciadora, que promova e potencie, de forma integrada o quadro de recursos existentes. Esta abordagem baseia-se em quatro premissas que pretendem estruturar e orientar o modelo estratégico apresentado, sendo elas a identidade da região, a sustentabilidade e competitividade, a construção de redes e a coesão sociocultural.

Modelling the Minho river plume intrusion into the rias baixas

The Minho River, situated 30 km south of the Rias Baixas is the most important freshwater source flowing into the Western Galician Coast (NW of the Iberian Peninsula). This discharge is important to determine the hydrological patterns adjacent to its mouth, particularly close to the Galician coastal region. The buoyancy generated by the Minho plume can flood the Rias Baixas for long periods, reversing the normal estuarine density gradients. Thus, it becomes important to analyse its dynamics as well as the thermohaline patterns of the areas affected by the freshwater spreading. Thus, the main aim of this work was to study the propagation of the Minho estuarine plume to the Rias Baixas, establishing the conditions in which this plume affects the circulation and hydrographic features of these coastal systems, through the development and application of the numerical model MOHID. For this purpose, the hydrographic features of the Rias Baixas mouths were studied. It was observed that at the northern mouths, due to their shallowness, the heat fluxes between the atmosphere and ocean are the major forcing, influencing the water temperature, while at the southern mouths the influence of the upwelling events and the Minho River discharge were more frequent. The salinity increases from south to north, revealing that the observed low values may be caused by the Minho River freshwater discharge. An assessment of wind data along the Galician coast was carried out, in order to evaluate the applicability of the study to the dispersal of the Minho estuarine plume. Firstly, a comparative analysis between winds obtained from land meteorological stations and offshore QuikSCAT satellite were performed. This comparison revealed that satellite data constitute a good approach to study wind induced coastal phenomena. However, since the numerical model MOHID requires wind data with high spatial and temporal resolution close to the coast, results of the forecasted model WRF were added to the previous study. The analyses revealed that the WRF model data is a consistent tool to obtain representative wind data near the coast, showing good results when comparing with in situ wind observations from oceanographic buoys. To study the influence of the Minho buoyant discharge influence on the Rias Baixas, a set of three one-way nested models was developed and implemented, using the numerical model MOHID. The first model domain is a barotropic model and includes the whole Iberian Peninsula coast. The second and third domains are baroclinic models, where the second domain is a coarse representation of the Rias Baixas and adjacent coastal area, while the third includes the same area with a higher resolution. A bi-dimensional model was also implemented in the Minho estuary, in order to quantify the flow (and its properties) that the estuary injects into the ocean. The chosen period for the Minho estuarine plume propagation validation was the spring of 1998, since a high Minho River discharge was reported, as well as favourable wind patterns to advect the estuarine plume towards the Rias Baixas, and there was field data available to compare with the model predictions. The obtained results show that the adopted nesting methodology was successful implemented. Model predictions reproduce accurately the hydrodynamics and thermohaline patterns on the Minho estuary and Rias Baixas. The importance of the Minho river discharge and the wind forcing in the event of May 1998 was also studied. The model results showed that a continuous moderate Minho River discharge combined with southerly winds is enough to reverse the Rias Baixas circulation pattern, reducing the importance of the occurrence of specific events of high runoff values. The conditions in which the estuarine plume Minho affects circulation and hydrography of the Rias Baixas were evaluated. The numerical results revealed that the Minho estuarine plume responds rapidly to wind variations and is also influenced by the bathymetry and morphology of the coastline. Without wind forcing, the plume expands offshore, creating a bulge in front of the river mouth. When the wind blows southwards, the main feature is the offshore extension of the plume. Otherwise, northward wind spreads the river plume towards the Rias Baixas. The plume is confined close to the coast, reaching the Rias Baixas after 1.5 days. However, for Minho River discharges higher than 800 m3 s-1, the Minho estuarine plume reverses the circulation patterns in the Rias Baixas. It was also observed that the wind stress and Minho River discharge are the most important factors influencing the size and shape of the Minho estuarine plume. Under the same conditions, the water exchange between Rias Baixas was analysed following the trajectories particles released close to the Minho River mouth. Over 5 days, under Minho River discharges higher than 2100 m3 s-1 combined with southerly winds of 6 m s-1, an intense water exchange between Rias was observed. However, only 20% of the particles found in Ria de Pontevedra come directly from the Minho River. In summary, the model application developed in this study contributed to the characterization and understanding of the influence of the Minho River on the Rias Baixas circulation and hydrography, highlighting that this methodology can be replicated to other coastal systems.

Numerical and combinatorial applications of generalized Appell polynomials

This thesis studies properties and applications of different generalized Appell polynomials in the framework of Clifford analysis. As an example of 3D-quasi-conformal mappings realized by generalized Appell polynomials, an analogue of the complex Joukowski transformation of order two is introduced. The consideration of a Pascal n-simplex with hypercomplex entries allows stressing the combinatorial relevance of hypercomplex Appell polynomials. The concept of totally regular variables and its relation to generalized Appell polynomials leads to the construction of new bases for the space of homogeneous holomorphic polynomials whose elements are all isomorphic to the integer powers of the complex variable. For this reason, such polynomials are called pseudo-complex powers (PCP). Different variants of them are subject of a detailed investigation. Special attention is paid to the numerical aspects of PCP. An efficient algorithm based on complex arithmetic is proposed for their implementation. In this context a brief survey on numerical methods for inverting Vandermonde matrices is presented and a modified algorithm is proposed which illustrates advantages of a special type of PCP. Finally, combinatorial applications of generalized Appell polynomials are emphasized. The explicit expression of the coefficients of a particular type of Appell polynomials and their relation to a Pascal simplex with hypercomplex entries are derived. The comparison of two types of 3D Appell polynomials leads to the detection of new trigonometric summation formulas and combinatorial identities of Riordan-Sofo type characterized by their expression in terms of central binomial coefficients.

Plano de ação para a sustentabilidade energética do Município de Vale de Cambra

O crescimento exponencial da população mundial que assentou essencialmente na utilização de combustíveis fósseis e o facto de aproximadamente ¾ da população mundial viver em cidades, criou uma situação insustentável de emissões de CO2 para a atmosfera. No sentido de minimizar e tentar reverter este comportamento a União Europeia criou o programa Pacto dos Autarcas, que visa o comprometimento de um território em reduzir as suas emissões de CO2 em, pelo menos, 20% até 2020, através do chamado Plano de Ação. O presente trabalho pretende desenvolver um possível Plano de Ação para a Sustentabilidade Energética para o município de Vale de Cambra. Da realização da matriz energética para este município foi inventariado o consumo de 47.154 tep e respectivas emissões de CO2 associada de 108.084 toneladas, para o ano de referência 2012. Face ao estudo compreendido entre 2002 e 2012 são previstos consumos e emissões na ordem de 54.327 tep e 123.059 toneladas de CO2 respetivamente até 2020 caso não sejam tomadas medidas para inverter essa tendência. Baseado na interpretação da matriz energética criada, propõe-se um conjunto de ações nas áreas da indústria, mobilidade, edifícios, energias renováveis, eficiência energética, governabilização e ainda sensibilização/formação para obter uma redução de 20% das emissões e consumo em 2020, passando para 98.447 toneladas de CO2 emitidas e 43.462 tep respetivamente. Conclui-se que o planeamento energético de um território é de elevada importância porque permite articular vários aspectos, conseguindo aumentar a protecção do ambiente (com a redução de emissões de gases efeito de estufa) e aumentando a eficiência energética do território, aumenta a sua competitividade económica e consequentemente maior oportunidade de investimentos externos, criando mais oportunidades de emprego e bem-estar social.