21 resultados para Filósofos - Portugal - séc. 20

em Repositório Científico da Universidade de Évora - Portugal


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This chapter explores the relationship between environmental conflicts and technical progress, trying to understand, in the case of large mines of the Iberian Pyrite Belt, in Alentejo, how emerging environmental problems conditioned the performance or led to the search for alternative technical solutions, taking as chronological limit for this observation the beginning of World War II. In the absence of the archives of the companies, the research was based on existing administrative documents in the state archives (mining engineers reports, the licensing of mining activities), on reports and documents published in specialized mining press, in particular, the Bulletin of the Ministry of Public Works, Trade and Industry, the Journal of Public Works, Trade and Industry (both in Portuguese), and finally in the local press. Despite that limitation, the information available shows that in global competition markets, the success of the British enterprise in Santo Domingo had the active search for new technical solutions for the creation and adaptation of existing knowledge to local problems in order to maximize the mineral resources available. The early development of the hydrometallurgical processes for the treatment of poor ores, named ‘natural cementation’, can be explained as the way these companies tried to solve problems of competitiveness, boosting economies of scale. Thus, they transferred the environmental costs previously limited to agriculture to more fragile social groups, the poor fishermen of Guadiana River and of Vila Real de Santo António. Therefore, the hydrometallurgy of pyrites was developed locally, pioneered in Santo Domingo that allowed the survival and expansion of the British company from the late 1870s, that is, at a time when most small mines shut since they were not able to compete globally. Through different consented and regulated processes (judicial), through conflict or parliamentary mediation, the State imposed exceptionally additional costs to companies, either for compensation, the imposing the application of remediation measures to reduce the environmental damage in some cases, thus contributing to derail some projects. These cases suggest that the interaction between local conflicts, corporate behavior and technological progress proves to be complex. This article aims to contribute to the debate on economic and social history between the environment and technological progress, arguing that the fixed costs and economic imponderable social risks were factors that encouraged the companies to search for new solutions and to introduce innovations since that would allow the expansion of their activity. In this process the companies sometimes faced environmental dilemmas and unforeseen costs with consequences on the economy of firms. The nature of the knowledge needed to address the environmental problems they created, however, is of a very different nature from that knowledge needed to face the environmental burdens that were inherent to the development of its activity.

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Above ground biomass is frequently estimated with forest inventory data and an extrapolation method for the per unit area evaluations. This procedure is labour demanding and costly. In this study above ground biomass functions, whose independent variable is crown horizontal projection, were developed. Multi-resolution segmentation method and object-oriented classification, based on very high spatial resolution satellite images, were used to obtain the area of tree crown horizontal projection for umbrella pine (Pinus pinea L.). A set of inventory plots were measured and with existing allometric functions for this species above ground biomass per tree and per plot were calculated. The two data sets were used to fit linear functions both for individual plot and their cumulative values. The results show a good performance of the models. Errors smaller than 10% are obtained for stand areas greater than 1.4 ha. These functions have the advantages of estimating above ground biomass for all the area under study or surveillance, not requiring forest inventory; allow monitoring in short time periods; and are easily implemented in a geographical information system environment.

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This abstract tries to make known one of the first attempts to recuperate the buildings heritage at the end of the 19th century in Spain: It’s called Atarazanas Market’s squares in Málaga, a marvellous Joaquín Rucoba’s architect work. It is one of the first examples in iron architecture in Spain which opted preservation building heritage from the respect of the place memory even in his last restoration.

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O tronco unificador da árvore educativa em Portugal sintetiza-se num conjunto de normativos que regulam o processo de ensino/aprendizagem, do pré-escolar ao ensino universitário, passando pelas diversas vertentes e modalidades que assume a escolaridade portuguesa. O primeiro documento, a partir do qual se postula toda a legislação em vigor é a Constituição Portuguesa de 1976, sendo a Lei n.o 46/86 de 14 de Outubro, a Lei de Bases do Sistema Educativo, o documento base estruturador do sistema educativo português. De 1986 a 2010, têm-se sucedido reformas, alterações curriculares, diferentes perspectivas de se encarar a educação e os seus actores. Com o presente estudo, que se enquadra no âmbito de uma investigação mais ampla, pretende-se apresentar e debater as principais linhas do pensamento educativo, com base na interpretação dos principais normativos em vigor, procurando responder à questão de qual será o modus operandi mais adequado para dar resposta aos desafios do século XXI, em Portugal. Paradoxalmente, elementos da pedagogia crítica coexistem com elementos de um pensamento neoconservador, no quadro normativo português: ideias como a “igualdade de oportunidades” e “inclusão” surgem ao mesmo tempo em que cada vez mais se incrementam “Quadros de Valor e Excelência”, “Prémios de Mérito” para docentes e discentes, numa procura de excelência mais próxima de uma política neoconservadora.

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This paper aims to look at the teaching situation of the nursing undergraduate degree’s courses about eldercare in Portugal. A documentary research on the teaching programs in 39 nursing schools, 26 schools presented syllabus units related to the topic ‘eldercare’ and in eight of these schools the contents of the units were identified. Using textual analysis and from the categories we concluded that the teaching regarding eldercare for the nurse training in Portugal is focused on hospital care; it is directed to the adult/elderly/family; it explores the definitions related to the aging process; it explores community issues, legislation and research. People responsible for the design/monitoring of teaching programs should include teaching regarding eldercare in the nurse training, considering that the elder population is increasing in Portugal.

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O turismo, na sua complexidade e multiplicidade, afecta as pessoas, os locais e a cultura de uma sociedade. A visão antropológica é insuficiente para compreender a riqueza e a diversidade do fenómeno turístico. No entanto, ela tem dado e continua a dar um contributo fundamental para a análise das práticas turísticas culturais em diferentes sociedades. O presente artigo pretende analisar a importância que a Antropologia assume nos planos curriculares dos Cursos Superiores de Turismo em Portugal.

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Na sequência de trabalhos anteriores, analisam-se aqui algumas das reflexões de natureza fonético-fonológica presentes na obra de Francisco José Freire, Reflexões sobre a língua portuguesa, avaliando a sua contribuição para o conhecimento da língua portuguesa no séc. XVIII.

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The Santa Eulalia plutonic complex (SEPC) is a late-Variscan granitic body placed in the Ossa-Morena Zone. The host rocks of the complex belong to metamorphic formations from Proterozoic to Lower Paleozoic. The SEPC is a ring massif (ca. 400 km2 area) composed by two main granitic facies with different colours and textures. From the rim to the core, there is (i) a peripheral pink medium- to coarse-grained granite (G0 group) involving large elongated masses of mafic and intermediate rocks, from gabbros to granodiorites (M group), and (ii) a central gray medium-grained granite (G1 group). The mafic to intermediate rocks (M group) are metaluminous and show wide compositions: 3.34–13.51 wt% MgO; 0.70–7.20 ppm Th; 0.84–1.06 (Eu/Eu*)N (Eu* calculated between Sm and Tb); 0.23–0.97 (Nb/Nb*)N (Nb* calculated between Th and La). Although involving the M-type bodies and forming the outer ring, the G0 granites are the most differentiated magmatic rocks of the SEPC, with a transitional character between metaluminous and peraluminous: 0.00–0.62 wt% MgO; 15.00–56.00 ppm Th; and 0.19–0.42 (Eu/Eu*)N ; 0.08–0.19 (Nb/Nb*)N [1][2]. The G1 group is composed by monzonitic granites with a dominant peraluminous character and represents the most homogeneous compositional group of the SEPC: 0.65–1.02 wt% MgO; 13.00–16.95 ppm Th; 0.57–0.70 (Eu/Eu*)N ; 0.14–0.16 (Nb/Nb*)N . According to the SiO2 vs. (Na2O+K2O–CaO) relationships, the M and G1 groups predominantly fall in the calc-alkaline field, while the G0 group is essencially alkali-calcic; on the basis of the SiO2 vs. FeOt/(FeOt+MgO) correlation, SEPC should be considered as a magnesian plutonic association [3]. New geochronological data (U-Pb on zircons) slightly correct the age of the SEPC, previously obtained by other methods (290 Ma, [4]). They provide ages of 306  2 Ma for the M group, 305  6 Ma for the G1 group, and 301  4 Ma for the G0 group, which confirm the late-Variscan character of the SEPC, indicating however a faintly older emplacement, during the Upper Carboniferous. Recent whole-rock isotopic data show that the Rb-Sr system suffered significant post-magmatic disturbance, but reveal a consistent set of Sm-Nd results valuable in the approach to the magmatic sources of this massif: M group (2.9 < Ndi < +1.8); G1 group (5.8 < Ndi < 4.6); G0 group (2.2 < Ndi < 0.8). These geochemical data suggest a petrogenetic model for the SEPC explained by a magmatic event developed in two stages. Initially, magmas derived from long-term depleted mantle sources (Ndi < +1.8 in M group) were extracted to the crust promoting its partial melting and extensive mixing and/or AFC magmatic evolution, thereby generating the G1 granites (Ndi < 4.6). Subsequently, a later extraction of similar primary magmas in the same place or nearby, could have caused partial melting of some intermediate facies (e.g. diorites) of the M group, followed by magmatic differentiation processes, mainly fractional crystallization, able to produce residual liquids compositionally close to the G0 granites (Ndi < 0.8). The kinetic energy associated with the structurally controlled (cauldron subsidence type?) motion of the G0 liquids to the periphery, would have been strong enough to drag up M group blocks as those occurring inside the G0 granitic ring.

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Este estudo propõe-se fazer uma análise comparativa de dois manuais de leitura do ensino primário, um em Língua Portuguesa e o outro em Língua Alemã. A pesquisa aponta afinidades e temas comuns na forma como em ambos os livros são abordados elementos representativos da identidade nacional e da memória colectiva. O nosso trabalho procura evidenciar, através dos manuais analisados e de uma fundamentação teórica, a manipulação destes conceitos durante o período do Estado Novo e do Terceiro Reich, época a que se reportam os manuais escolares. A nossa dissertação de mestrado insere-se no âmbito da Literatura Comparada, apoiando-se no que diz respeito à sua fundamentação teórica em estudos e autores trabalhados no contexto das disciplinas de Literatura e Cultura de Massas e de Literatura Infanta-Juvenil, investigações essenciais para estabelecer uma análise comparativa entre os dois manuais de leitura do ensino básico. ABSTRACT: This study aims at a comparative analysis of two primary textbooks, one in Portuguese and the other in German language. The research points out common topics, affinities as well as a similar approach to representative elements of the National Identity and the Collective Memory in Portugal and in Germany. Based on the analysis of the schoolbooks mentioned and supported by a theoretical ground basis, our work tries to show the manipulation of these concepts during the years of the Estado Novo and the Third Reich, the period of time in which both schoolbooks were published and taught. Our dissertation applies to the study field of Compared Literature, having its theoretical ground basis on studies and authors referred to in the scope of the disciplines of Literature and Culture of the Masses as well as Children’s and Youth Literature which provided us essential knowledge for a comparative analysis of these two primary schoolbooks.

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Portugal regista atualmente um dos mais baixos níveis de fecundidade da Europa e do mundo, resultado da redução do número de filhos e do adiamento dos nascimentos para idades mais tardias. As características individuais e a idade ao nascimento do primeiro filho são determinantes cruciais para o número de filhos que se tem e que se espera ter, variando em função do grau de instrução. Apesar das alterações comportamentais ao longo das últimas décadas, os contextos familiares e a conjugalidade continuam a ser centrais na vida dos portugueses, pois aqueles que não vivem com cônjuge ou companheiro apresentam fecundidades mais baixas. A dimensão familiar ideal é outro determinante crítico, dado que ideais mais baixos potenciam que se tenha menos filhos, dificultando a recuperação da fecundidade. O ideal parece corresponder ao número de filhos que permite manter um determinado nível de vida para a família e ainda garantir aos filhos mais oportunidades, mesmo que para tal se tenha apenas um filho. Daí também a atual relevância das questões económicas nas decisões de fecundidade. A alteração de mentalidades parece ter gerado um novo modelo social marcado por uma crescente valorização dos filhos.

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This study examines the long profiles of tributaries of the Tejo (Tagus) and Zêzere rivers in central eastern Portugal (West Iberia) in order to provide new insights into the patterns, timing and controls on drainage development during the Pleistocene to Holocene incision stage. The long profiles were extracted from lower order tributary streams associated with the trunk drainage of the Tejo River and one main tributary, the Zêzere River (Fig. 1). These streams flow through a landscape strongly influenced by variations in bedrock lithology (mainly granites and metasediments), fault structures delimiting crustal blocks with distinct uplift rates, and a base-level lowering history (tectonic uplift / eustatic). The long profiles of the tributaries of the Tejo and Zêzere rivers record a series of transient and permanent knickpoints. The permanent knickpoints have direct correlation with the bedrock strength, corresponding to the outcropping of very hard quartzites or to the transition from softer (slates/metagreywaques) to harder (granite) basement. The analyzed streams/rivers record also an older transient knickpoint/knickzone separating: a) an upstream relict graded profile, with lower steepness and higher concavity, that reflects a long period of quasi-equilibrium conditions reached after the beginning of the incision stage; and b) a downstream reach displaying a rejuvenated long profile, with steeper gradient and lower concavity, particularly for the final segment, which is often convex (Fig. 2). The rejuvenated reaches testify the upstream propagation of several incision waves that are the response of each stream to continuous or increasing crustal uplift and dominant periods of base-level lowering by the trunk drainages, coeval of low sea level conditions. The long profiles and their morphological configurations enabled spatial and relative temporal patterns of incision to be quantified for each individual tributary stream. The incision values of streams flowing in uplifted blocks of the Portuguese Central Range (PCR) (ca.380-280 m) indicate differential uplift and are higher than the incision values of streams flowing on the adjacent South Portugal planation surface – the Meseta (ca. 200 m). The normalized steepness index, calculated using the method of Wobus et al. (2006), proved to be sensitive to active tectonics, as lower ksn values were found in relict graded profiles of streams located in less uplifted blocks, (e.g. Sertã stream in the PCR), or in those flowing through tectonic depressions. Fig. 1 – Geological map of the study area. 1 – fluvial terraces (Pleistocene); 2 – sedimentary cover (Paleogene and Neogene); 3 – slates and metasandstones (Devonian); 4 – slates and quartzites (Silurian); 5 – quartzites (Ordovician); 6 – slates and metagreywackes (Precambrian to Cambrian); 7 – slates, metagreywackes and limestones (Precambrian); 8 – granites and ortogneisses; 9 – diorites and gabros; 10 - fault. SFf – Sobreira Formosa fault; Sf – Sertã fault; Pf – Ponsul fault; Gf – Grade fault. The differential uplift indicated by the distribution of the ksn values and by the fluvial incision was likely accumulated on a few major faults, as the Sobreira Formosa fault (SFf), thus corroborating the tectonic activity of these faults. Due to the fact that the relict graded profiles can be correlated with other geomorphic references documented in the study area, namely the T1 terrace of the Tagus River (with an age of ca. 1 Myr), the following incision rates can be estimated: a) for the studied streams located in uplifted blocks of the PCR, 0.38 m/kyr to 0.28 m/kyr; b) for the streams flowing on the South Portugal planation surface, 0.20 m/kyr. The differential uplift inferred between crustal blocks in the study area corroborates the neotectonic activity of the bordering faults, which has been proposed in previous studies based upon less robust data. Fig. 2 – Longitudinal profile of the Nisa stream a tributary of the Tejo River. Note the equilibrium relict profile upstream the older transient knickpoint (hatched line) and the downstream rejuvenated profile (continuous line). Legend: tKP – transient knickpoint; rKp – resistant knickpoint; Mt – schist and phyllite; Gr – granite; Hf – hornfels; Og – orthogneisse. In the inset Distance – Slope plots, fill circles correspond to the relict graded profile, crosses correspond to the rejuvenated profile located downstream the older transient knickpoint (tKP).

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A qualidade em educação constitui uma das grandes preocupações de governantes, políticos, académicos e investigadores e tem sido uma questão amplamente debatida em encontros científicos e estudada em diversos programas de investigação educacional nos mais diversos países do mundo ocidental. A avaliação das escolas (interna e externa) são processos fundamentais para o desiderato da qualidade e da melhoria das escolas. Nesta comunicação apresentamos alguns dos resultados do projeto de investigação “Impacto e Efeitos da Avaliação Externa nas Escolas do Ensino não Superior”, financiado pela FCT (Projeto PTDC/CPE-CED/116674/2010), no sentido de responder ao problema de investigação – Que impacto e efeitos produz a AEE no primeiro e segundo ciclos do modelo, tendo em referência a melhoria da escola, a participação da comunidade e a implementação de políticas de accountability? Os dados empíricos recolhidos e analisados, permitem afirmar que a AEE tem produzido impacto e efeitos nas dimensões organizacionais e funcionais das escolas, os quais são visíveis: a) na melhoria da escola, mais a nível organizacional do que a nível curricular e dos modos de trabalho pedagógico, sendo o impacto nesta última dimensão reconhecido como reduzido ou inexistente; b) na aceitação e apropriação pela escola dos referentes utilizados no processo de avaliação externa e consequente consolidação da avaliação institucional; c) na participação da comunidade na vida social da escola, reforçando as parcerias existentes e dando voz aos diversos atores sociais que intervêm diretamente na escola; d) na institucionalização de planos de melhoria focados nas fragilidades identificas nos relatórios da avaliação externa das escolas; e) na monitorização de resultados académicos, embora sem efeitos visíveis; f) na apropriação do discurso da qualidade, da eficácia, da eficiência e da accountability nas escolas.

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The present work describes the measurement effort for direct normal irradiance (DNI) evaluation in the sunny south of Portugal, with a network of eight radiation measurement stations in several locations (including Évora) providing a good coverage of the region. This new initiative for DNI measurement will still need many years (typically 10 or more) to produce a time series which can claim having long term statistical value. This problem can, however, be temporarily mitigated by measuring DNI at the same time as GHI and DHI, in a place where long term series dating back, already exist for those two. It so happens that a long term series (20 years) of global and diffuse solar irradiation exists for the location Évora. So the expectation is to establish correlations with the goal of attributing at least some long term statistical significance to the short and recent DNI series. The paper describes the setup of the measuring stations and presents the preliminary measurements obtained. It further presents the first correlations of monthly averages between normal beam (DNI), global and diffuse radiation. It then uses these correlations, admittedly without acceptable statistical significance (short series of less than one year of measured data), to exemplify how to get a prediction of long term DNI for Évora. This preliminary obtained value is compared to that predicted by the commercial data from Meteonorm.

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Seminário “Qualificação dos Adultos: Realidades e Desafios no Sul de Portugal”, integrado no projecto de investigação “As Novas Núpcias da Qualificação no Alentejo”, no Colégio do Espírito Santo da Universidade de Évora, a 20 de Junho de 2011.

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During its history, several significant earthquakes have shaken the Lower Tagus Valley (Portugal). These earthquakes were destructive; some strong earthquakes were produced by large ruptures in offshore structures located southwest of the Portuguese coastline, and other moderate earthquakes were produced by local faults. In recent years, several studies have successfully obtained strong-ground motion syntheses for the Lower Tagus Valley using the finite difference method. To confirm the velocity model of this sedimentary basin obtained from geophysical and geological data, we analysed the ambient seismic noise measurements by applying the horizontal to vertical spectral ratio (HVSR) method. This study reveals the dependence of the frequency and amplitude of the low-frequency (HVSR) peaks (0.2–2 Hz) on the sediment thickness. We have obtained the depth of the Cenozoic basement along a profile transversal to the basin by the inversion of these ratios, imposing constraints from seismic reflection, boreholes, seismic sounding and gravimetric and magnetic potentials. This technique enables us to improve the existing three-dimensional model of the Lower Tagus Valley structure. The improved model will be decisive for the improvement of strong motion predictions in the earthquake hazard analysis of this highly populated basin. The methodology discussed can be applied to any other sedimentary basin.