Modelação de atributos hidrogeológicos do maciço envolvente à antiga área mineira da Quinta do Bispo

Dissertação para obtenção do Grau de Doutor em Engenharia Geológica

D. João III e D. Miguel da Silva, bispo de Viseu: novas razões para um ódio velho

No Verão de 1540, D. Miguel da Silva (c. 1480-1556), escrivão da puridade de D. João III e bispo de Viseu, abandonou a cidade de Viseu, fugindo para Itália, de onde nunca regressou e onde veio a morrer em 1556. A versão fixada pela cronística e veiculada, quase ne varietur, pela historiografia, é de que a causa do ódio que D. João III veio a conceber por D. Miguel da Silva, a fuga deste para Itália e a perseguição que o monarca lhe moveu até à sua morte em Roma teria sido, em exclusivo e numa relação causal, a ascensão ao cardinalato, em 1539, à revelia da autoridade régia. Em nosso entender, este acontecimento deverá, antes, ser visto no âmbito de um conjunto complexo de razões em que o cardinalato tem, é certo, um papel de destaque, mas não exclusivo. Revisitar-se-á, pois, esta excepcional figura para avaliar e compreender, a uma nova luz, um dos mais perturbadores momentos do reinado de D. João III, que teve como protagonista D. Miguel da Silva, bispo de Viseu.

D. João III e D. Miguel da Silva, bispo de Viseu: novas razões para um ódio velho

No Verão de 1540, D. Miguel da Silva (c. 1480-1556), escrivão da puridade de D. João III e bispo de Viseu, abandonou a cidade de Viseu, fugindo para Itália, de onde nunca regressou e onde veio a morrer em 1556. A versão fixada pela cronística e veiculada, quase ne varietur, pela historiografia, é de que a causa do ódio que D. João III veio a conceber por D. Miguel da Silva, a fuga deste para Itália e a perseguição que o monarca lhe moveu até à sua morte em Roma teria sido, em exclusivo e numa relação causal, a ascensão ao cardinalato, em 1539, à revelia da autoridade régia. Em nosso entender, este acontecimento deverá, antes, ser visto no âmbito de um conjunto complexo de razões em que o cardinalato tem, é certo, um papel de destaque, mas não exclusivo. Revisitar-se-á, pois, esta excepcional figura para avaliar e compreender, a uma nova luz, um dos mais perturbadores momentos do reinado de D. João III, que teve como protagonista D. Miguel da Silva, bispo de Viseu.

A sacristia e a encomenda episcopal portuguesa no período da reforma católica. O caso da Sé de Coimbra e o patrocínio do bispo D. Afonso de Castelo Branco

Tese de Doutoramento em História de Arte Moderna

Estudo Estratigráfico e Paleontológico do Jurássico do Algarve Ocidental

Algarve Province, Southern Portugal, corresponds in part to a meso-cenozoic basin running along the coast from Cabo S. Vicente to beyond Spanish border. Structurally it is a big monocline plunging southwards much deformed mainly by two East-West longitudinal flexures. Lithostratigraphical and chronostratigraphical studies dealt specially with Jurassic formations. This and the geological mapping of the post-Hercynian sedimentary formations allow us to define the following units: Triassic-Lower Liassic Arenitos de Silves (Silves sandstones sensu P. Choffat, pro parte) - At their base the Silves sandstones (0-150m) are represented mainly by cross-bedded red sandstones. This unit is Upper Triassic (Keuper) in age, on the evidence of some Brachiopoda. Complexo margo-carbonatado de Silves (Silves marl-limestone complex=Silves sandstones sensu P. Choffat, pro parte) (80-200m) overlies the preceding, it may be reported to the Upper Triassic-Hettangian. It consists of a thick pelite-marl-dolomite-limestone series with many intercalations of greenstones. Since no fossils were found it is not possible to conclude whether it is still Hettangian or if it does correspond, in the whole or in part, already to the Sinemurian. Liassic Dolomitos e calcários dolomíticos de Espiche (Espiche dolomite-rocks and dolomitic-limestones) - The usually massive and finely crystalline or saccharoidal dolomites and dolomitic-limestones are the toughest strata of the Algarve margin giving rise to several hills. Its thickness attains in certain points 60 metres at least. Based on geometry and on lithological similarities with the carbonated complex of the northern basin of Tagus river (Peniche, São Pedro de Muel, Quiaios), this formation can be accepted as Sinemurian in age. As it happens with the carbonated complex, here also the first dolomite beds are non-isochronal throughout the region; upper time-limit of the dolomitic facies is either Lower Carixian, Lower Toarcian or even Lower Dogger. The dolomitization is secondary but not much later than sedimentation. However, between Cabo S. Vicente-Vila do Bispo there is evidence of an even later secondary dolomitization related to the regional fault complex. Calcário dolomítico com nódulos de silex da praia de Belixe (Belixe beach dolomitic-limestone with silex nodules) (50-55m) - Ascribed to Lower or Middle Carixian on the basis of Platypleuroceras sp., Metaderoceras sp. nov. and M. gr. Venarense. Calcário cristalino compacto com Protogrammoceras, Fuciniceras e ? Argutarpites de Belixe (Belixe compact crystalline limestone with Protogrammoceras, Fuciniceras and ? Argutarpites) (30m) - Ascribed to Lower Domerian. Middle and Upper Domerian are indicated but by a single specimen of ? Argutarpites. Calcários margosos e margas com Dactylioceras semicelatum e Harpoceratídeos de Armação Nova (Armação Nova marly limestones and marls with D. semicelatum and Harpoceratidae) (25m) -Ascribed to Lower Toarcian. Middle and Upper Toarcian formations are not known in the Algarve. Dogger Calcários oolíticos, c. corálicos, c. pisolíticos, c. calciclásticos, c. dolomíticos e dolomitos de Almadena (Almadena oolitic-limestones, coral-reef-limestones, pisolite-limestones, limeclastic-limestones, dolomitic-limestones and dolomite-rocks) (more than 50 metres), with lagoonal facies. Ascribed to Aalenian-Bathonian-? Callovian. Margas acinzentadas e calcários detríticos com Zoophycos da praia de Mareta (Mareta beach greyish marls and detritical limestones with Zoophycos) (40m) - Pelagic transreef facies with Upper Bajocian and Bathonian ammonites. Calcários margosos e margas da praia de Mareta (Mareta beach pelagic marly-limestones and marls) (110m) - Ascribed to the Callovian on its ammonites. Malm Near Cabo S. Vicente and Sagres the first Upper Jurassic level consists of a yellowish-brown nodular, compact, locally phosphated and ferruginous, sometimes conglomeratic, marly limestone (0,35-1,50m) containing a rich macrofauna, which includes: 1) Callovian forms unknown at Lower Oxfordian; 2) Upper Callovian forms that still survived in Lower and Middle Oxfordian; 3) Lower Oxfordian forms (Mariae and Cordatum Zones); 4) Lower and Middle Oxfordian forms (Mariae to Plicatilis Zone); 5) Middle Oxfordian forms (plicatilis Zone), and some ones appearing in Middle Oxfordian. This condensed deposit is therefore dated from Middle Oxfordian (Plicatilis Zone). The other Upper Jurassic lithostratigraphical units were also mapped but their detailed study is not presented in this work. Correlations between lithostratigraphical and chronostratigraphical scales from P. Choffat, J. Pratsch, C. Palain and from the author are stated. Further correlations are attempted between zonc scales of Carixian-Lower Toarcian and Upper Bajocian-Middle Oxfordian of France, Spain (Asturias, Iberian and Betic Chains), Argel (Orania) and Portugal (northern Tagus basin and Algarve). The study of pyritous fossil assemblages common in Upper Bathonian-Lower Callovian marly levels of the praia da Mareta seems to suggest that these sediments were deposited in a bay or in an almost closed coastal re-entrance virtually without deep water circulation. Although such conditions may occur at any depth one may suppose that these ones actually correspond to an infralittoral neritic environment. The thaphocoenosis collected there are almost entirely composed of nektonic (ammonites, Belemnites) and planktonic (Bositra) faunas. The sedentary (crinoids, brachiopods) or free (sea-urchins, gastropods) epibenthonic forms are very scarce; endobenthonic forms are not known. The palaeontological study of all Nautiloids and Ammonoids of the Liassic and Dogger is presented (except Kosmoceratidae and Perisphinctaceae). Among the thirty one taxa dealt with, one is new (Metaderoceras sp. nov.) and the great majority of the others has been identified for the first time in Algarve. Some others have never been reported before in Portuguese formations. The evolution, during Jurassic times, of the sedimentary basins of the Portuguese plate margin is described. The absence of Cephalopods in the very extensive marly and dolomitic limestones, partly marine, suggests that, during Lower Liassic, palaeogeography underwent no great changes. Dolomitic-limestone with silex nodules from Cabo S. Vicente contain the first ammonites recorded at the base of the Middle Liassic. This facies, although very common in Tethys, is unknown north of the Tagus. The faunal assemblage has a mediterranean to submediterranean character. Comparisons between faunal assemblage" from Algarve with the ones known north of the Tagus show that communications between Boreal Europe and Tethys, virtually non-existent during Lower and Middle Carixian, became very easy during Lower Domerian. In earlier Pliensbachian times two distinct seas were adjacent to the Iberian plate. One, an epicontinental sea with a tethyan fauna, extended southwards from the Meseta margin. Another, was a boreal sea; during its transgressive episodes boreal faunas attained into the basin north of the Tagus. During Middle Carixian and Lower Domerian, owing to simultaneous transgressions, these two seas joined together allowing faunal exchanges along the epicontinental areas which limited the emerging hercynian chains belts. During Liassic, the Algarve belonged undoubtedly to the tethyan submediterranean province. The area north of the Tagus, on the contrary, was a complex realm where subboreal and tethyan affinities alternatively prevailed. In the Algarve the first Middle Jurassic deposits do frequently show lateral thickness reductions as well as unconformities contemporaneous with other generalized disturbances on the sedimentation processes in other parts of Europe. By this time, near Sagres, a barrier reef developed separating lagoonal or ante-reef facies from the transreef pelagic zone. The presence of tethyan fauna, the abundance of Phylloceratidae and the absence of boreal forms allow us to consider the Algarve basin as a submediterranean province. The presence of Callovian pelagic fossiliferous formations in the Loulé area shows that during Middle Jurassic the marl-limestone transreef sedimentation was not confined to the western Algarve. They would extend eastwards where they only can be seen in the core of some anticlines. This is due to the progressive sinking of the meso-cenozoic formations as we proceed towards the South of the Sagres-Algoz-Querença flexure. In the whole of the Peninsule, and as for the Middle Callovian, an important regression can be clearly recognized on the evidence of an erosion surface which strikes obliquely the Middle and Upper Callovian strata. The geographic boundaries of the different faunal provinces are not changed by the presence of many Kosmoceratidae in the phosphate nodules since they are but a minority in comparison with the tethyan forms. An abstract model can be constructed showing that in Western Europe the Kosmoceratidae may have migrated South and westwards through a channel of the sea that linked Paris basin to Poitou and Aquitaine. By migrating between the Iberian meseta and the Armorican massif this fauna reached northern Tagus basin at the beginning of Upper Callovian (Athleta Zone); this south and southwest bound migration would have proceeded, allowing such forms to reach Algarve basin only in latest Callovian times (Lamberti Zone). This migration means that during Middle Jurassic a widely spread North Atlantic sea would exist, flooding the western part of Portugal up to the Poitou.

Analysis of glycosylation heterogeneity in antibody production by Pichia pastoris

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

Os topónimos algarvios na Paleontologia portuguesa

Since the XIX century, Portuguese and foreign geologists have defined 47 new invertebrate taxa (foraminifera, ostracods, coelenterates, brachiopods, gastropods, ammonoids, echinoids), 2 new fossil plant taxa (charophyte and pteridophyte) and 1 ichnofossil, using toponymy from the Algarve; these taxa refer to 1 genera, 47 species and 2 varieties. Besides the Algarve toponym, the most used as specific name, twenty others have been used, mostly from western Algarve; these toponyms are associated to: – Miocene units, particularly from Ribeira de Cacela and Ferragudo; – Cretaceous units between Zavial and Marim; – Upper Jurassic units from Sagres, Carrapateira and Loulé and Middle Jurassic units from Sagres and Guilhim; – Triassic units from Vila do Bispo to Tavira; – Carboniferous units, particularly from the Aljezur-Bordeira-Carrapateira region. The earliest of these designations were attributed to seven gastropods from the Upper Miocene of Cacela (COSTA, 1866-1867). The majority of the named species are typical of the Algarve, but some have been collected, as well, in the Lusitanian Basin. Although extensively cited in the geological literature, some of these taxa either do not fulfill the ICZN rules, or fall into synonymy with previously established taxa, or should be formally considered as non valid names (nomem nudum and nomen oblitum). Only widespread bibliographical review, associated with the palaeontological revision of some of these groups and the correct interpretation of the ICZN articles, will allow confirming, or not, the doubts that have now arisen.

Heidegger leitor de Agostinho: A memoria como fenómeno existencial

Dissertação apresentada para cumprimento dos requisitos necessários à obtenção do grau de Mestre em Filosofia Geral

Entre Constâncio II e Juliano: a linguagem de potâmio de Lisboa e o conhecimento da lusitânia do Séc. IV

Com um nome de ressonâncias gregas, que nos transporta para o conceito de rio, em gr. Potamós, Potamius surge-nos na História como o primeiro bispo conhecido de Lisboa, cuja acmê ou, melhor dizendo, cujo floruit se baliza entre os anos de 343 e 360. Esteve presente no Sínodo anomeano de Sirmium, na Panónia, reunido no ano de 357, cuja fórmula ariana assinou e, possivelmente, participou também no Concilio de Rimini de 359'. Teria passado do catolicismo ao arianismo nos anos 355-356 e falecido por volta de 360, a caminho de uma Villa que lhe teria sido oferecida pelo Imperador Constâncio II, que reinou entre 337 e 361. Como, porém, a notícia da sua morte só nos vem de um texto escrito em 383 ou 3842, Q^^Q bispo poderá ter vivido até aos anos oitenta do séc. FV, ou seja, até ao tempo do Imperador Teodósio.

Levantamento e Caracterização de Projectos Musicais Implementados em Estabelecimentos Prisionais Femininos Portugueses (2005 a 2010)

Tese apresentada para cumprimento dos requisitos necessários à obtenção do grau de Doutor em Ciências Musicais na especialidade de Ensino e Psicologia da Música

Análise de estratégias para participação ativa de consumidores na contratação bilateral de eletricidade em mercados liberalizados

Pode-se constatar que a energia elétrica, desde o início do século XX, assumiu um papel fundamental na nossa sociedade, tornando-se nos dias de hoje uma necessidade de primeira ordem. Infelizmente, cerca de 1,2 mil milhões de pessoas ainda vivem sem eletricidade e a quota das energias renováveis no consumo global apenas aumentou ligeiramente em 20 anos, como revela um relatório coliderado pelo Banco Mundial e pela Agência Internacional da Energia. Nos últimos anos, com o objetivo de alcançar um modelo de Mercado de Energia Elétrica (MEE) que seja livre, competitivo, o setor elétrico de diversos países sofreu inúmeras alterações. Em particular, ocorreu a reestruturação da organização de várias empresas monopolistas, sendo que estas, sendo verticalmente integradas não tinham qualquer concorrência, gerindo desde a produção até à venda da eletricidade, produzindo, transportando e distribuindo a energia elétrica. O modelo de mercado tem também como objetivo permitir melhores condições para os consumidores finais de energia, mais precisamente preços mais baixos. Atualmente, a estrutura do mercado retalhista apoia-se na coexistência de duas formas de contratação de fornecimento de energia elétrica (ERSE, 2009):  contratação em mercado regulado, a partir de contratos bilaterais, ou no mercado organizado, através de aplicação de tarifas integrais reguladas;  contratação em mercado liberalizado, em que as condições de negociação de energia, que serão definidas entre as partes e a componente de acesso às redes, são aplicadas através de preços regulados. Os principais objetivos desta dissertação são os seguintes: (i) estudar a contratação bilateral de energia em mercados liberalizados, com principal ênfase para o desenvolvimento de estratégias que possibilitem uma participação ativa dos consumidores, (ii) testar novas estratégias de negociação através do desenvolvimento de um caso de estudo sobre a participação efetiva de consumidores na contratação bilateral, baseado em dados dos mercados sobre preços e volumes de energia, e (iii) adotar um modelo de negociação bilateral, previamente desenvolvido, e estendê-lo por forma a representar as preferências dos negociadores, nomeadamente com o modelo multiplicativo. Em termos sucintos, os resultados obtidos com as estratégias de negociação permitem concluir que os intervenientes no mercado apresentam um comportamento esperado na gestão de preços e volumes de energia. Pode-se também afirmar que as estratégias constituem um auxiliar efetivo na tomada de decisão inerente à negociação bilateral em mercados de energia.

Integrated data model and DSL modifications

Companies are increasingly more and more dependent on distributed web-based software systems to support their businesses. This increases the need to maintain and extend software systems with up-to-date new features. Thus, the development process to introduce new features usually needs to be swift and agile, and the supporting software evolution process needs to be safe, fast, and efficient. However, this is usually a difficult and challenging task for a developer due to the lack of support offered by programming environments, frameworks, and database management systems. Changes needed at the code level, database model, and the actual data contained in the database must be planned and developed together and executed in a synchronized way. Even under a careful development discipline, the impact of changing an application data model is hard to predict. The lifetime of an application comprises changes and updates designed and tested using data, which is usually far from the real, production, data. So, coding DDL and DML SQL scripts to update database schema and data, is the usual (and hard) approach taken by developers. Such manual approach is error prone and disconnected from the real data in production, because developers may not know the exact impact of their changes. This work aims to improve the maintenance process in the context of Agile Platform by Outsystems. Our goal is to design and implement new data-model evolution features that ensure a safe support for change and a sound migration process. Our solution includes impact analysis mechanisms targeting the data model and the data itself. This provides, to developers, a safe, simple, and guided evolution process.

We are all on fire [...]’: os primórdios da canonização da literatura medieval inglesa

Tomando como ponto de partida a célebre confissão do Bispo Hurd em Letters on Chivalry and Romance (1762), o nosso texto procurará reflectir, enquadrando-os culturalmente, sobre os processos de (re)descoberta, reavaliação e revalorização setecentistas da literatura medieval, mercê das histórias literárias pioneiras de Hugh Blair (1718-1800), Thomas Warton (1728-1790) e do próprio Richard Hurd (1720-1808).

Using an LED as a sensor and visible light communication device in a smart illumination system

The need for more efficient illumination systems has led to the proliferation of Solid-State Lighting (SSL) systems, which offer optimized power consumption. SSL systems are comprised of LED devices which are intrinsically fast devices and permit very fast light modulation. This, along with the congestion of the radio frequency spectrum has paved the path for the emergence of Visible Light Communication (VLC) systems. VLC uses free space to convey information by using light modulation. Notwithstanding, as VLC systems proliferate and cost competitiveness ensues, there are two important aspects to be considered. State-of-the-art VLC implementations use power demanding PAs, and thus it is important to investigate if regular, existent Switched-Mode Power Supply (SMPS) circuits can be adapted for VLC use. A 28 W buck regulator was implemented using a off-the-shelf LED Driver integrated circuit, using both series and parallel dimming techniques. Results show that optical clock frequencies up to 500 kHz are achievable without any major modification besides adequate component sizing. The use of an LED as a sensor was investigated, in a short-range, low-data-rate perspective. Results show successful communication in an LED-to-LED configuration, with enhanced range when using LED strings as sensors. Besides, LEDs present spectral selective sensitivity, which makes them good contenders for a multi-colour LED-to-LED system, such as in the use of RGB displays and lamps. Ultimately, the present work shows evidence that LEDs can be used as a dual-purpose device, enabling not only illumination, but also bi-directional data communication.