995 resultados para Sé de Évora
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“Silêncio no Vácuo” - Experiência (vídeo de 2 min 21 s, Graça Carraça, Departamento de Física, Escola de Ciências e Tecnologia- Universidade de Évora). O trabalho experimental registado neste vídeo faz parte de um conjunto de trabalhos de divulgação, seleccionados de entre os vários que podem ser explorados nas nossas aulas experimentais de Física. Este trabalho foi recentemente apresentado como demonstração experimental a jovens do Campo de Férias SASUE - 2016, sob o tema “Explorando o som”. Apesar de neste caso estarmos perante um público muito jovem, crianças dos 7 aos 12 anos, suscitou a curiosidade e o interesse sobre a explicação dos fenómenos em causa. Com este registo em vídeo pretende-se sobretudo facilitar o trabalho dos alunos e professores que queiram realizar a experiência e fazer pensar na possibilidade de explorar este sistema para além da demostração aqui apresentada.
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A corrosion product rarely reported in the literature has been found on the copper support of three miniature paintings of the 17th and 18th centuries. This product, which has been identified as dicoppertrihydroxyformate (Cu2(OH)3HCOO), is an unusual basic copper formate found on copper artifacts. The identification and characterization of dicoppertrihydroxyformate was carried out directly over the corroded surface of the objects, using a nondestructive approach, which combines the integrated use of various microanalytical techniques. Using this approach, it was possible to obtain a set of new reference data about the natural form of Cu2(OH)3HCOO, that will enable its unambiguous identification in other similar objects. In this work, the probable causes that may have contributed to its formation are also discussed.
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NEW DATA ON THE CHRONOLOGY OF THE VALE DO FORNO SEDIMENTARY SEQUENCE (LOWER TAGUS RIVER TERRACE STAIRCASE) AND ITS RELEVANCE AS FLUVIAL ARCHIVE OF THE MIDDLE PLEISTOCENE IN WESTERN IBERIA Pedro P. Cunha 1, António A. Martins 2, Jan-Pieter Buylaert 3,4, Andrew S. Murray 4, Luis Raposo 5, Paolo Mozzi 6, Martin Stokes 7 1 MARE - Marine and Environmental Sciences Centre, Department of Earth Sciences, University of Coimbra, Portugal: pcunha@dct.uc.pt 2 MARE - Marine and Environmental Sciences Centre, Dep. Geociências, University of Évora, Portugal; aam@uevora.pt 3 Centre for Nuclear Technologies, Technical University of Denmark, Risø Campus, Denmark; jabu@dtu.dk 4 Nordic Laboratory for Luminescence Dating, Aarhus University, Risø DTU, Denmark; anmu@dtu.dk 5 Museu Nacional de Arqueologia, Lisboa, Portugal; 3raposos@sapo.pt 6 Department of Geosciences, University of Padova, Italy; paolo.mozzi@unipd.it 7 School of Geography, Earth and Environmental Sciences, University of Plymouth, UK; m.stokes@plymouth.ac.uk The stratigraphic units that record the evolution of the Tagus River in Portugal (study area between Vila Velha de Ródão and Porto Alto villages; Fig. 1) have different sedimentary characteristics and lithic industries (Cunha et al., 2012): - a culminant sedimentary unit (the ancestral Tagus, before the drainage network entrenchment) – SLD13 (+142 to 262 m above river bed – a.r.b.; with probable age ca. 3,6 to 1,8 Ma), without artefacts; - T1 terrace (+84 to 180 m; ca. 1000? to 900 ka), without artefacts; - T2 terrace (+57 to 150 m; top deposits with a probable age ca. 600 ka), without artefacts; - T3 terrace (+43 to 113 m; ca. 460 to 360? ka), without artefacts; - T4 terrace (+26 to 55 m; ca. 335 a 155 ka), Lower Paleolithic (Acheulian) at basal and middle levels but early Middle Paleolithic at top levels; - T5 terrace (+5 to 34 m; 135 to 73 ka), Middle Paleolithic (Mousterian; Levallois technique); - T6 terrace (+3 to 14 m; 62 to 32 ka), late Middle Paleolithic (late Mousterian); - Carregueira Sands (aeolian sands) and colluvium (+3 a ca. 100 m; 32 to 12 ka), Upper Paleolithic to Epipaleolithic; - alluvial plain (+0 to 8 m; ca. 12 ka to present), Mesolithic and more recent industries. The differences in elevation (a.r.b.) of the several terrace staircases results from differential uplift due to active faults. Longitudinal correlation with the terrace levels indicates that a graded profile ca. 200 km long was achieved during terrace formation periods and a strong control by sea base level was determinant for terrace formation. The Neogene sedimentary units constituted the main source of sediments for the fluvial terraces (Fig. 2). Geomorphological mapping, coupled with lithostratigraphy, sedimentology and luminescence dating (quartz-OSL and K-feldspar post-IRIR290) were used in this study focused on the T4 terrace, which comprises a Lower Gravels (LG) unit and an Upper Sand (US) unit. The thick, coarse and dominantly massive gravels of the LG unit indicate deposition by a coarse bed-load braided river, with strong sediment supply, high gradient and fluvial competence, during conditions of rapidly rising sea level. Luminescence dating only provided minimum ages but it is probable that the LG unit corresponds to the earlier part of the MIS9 (ca. 335 to 325 ka), immediately postdating the incision promoted by the very low sea level (reaching ca. -140 m) during MIS10 (362 to 337 ka), a period of relatively cold climate conditions with weak vegetation cover on slopes and low sea level. Fig. 1. Main Portuguese reaches in which the Tagus River can be divided (Lower Tagus Basin): I – from the Spanish border to Arneiro (a general E–W trend, mainly consisting of polygonal segments); II – from Arneiro to Gavião (NE–SW); III – from Gavião to Arripiado (E–W); IV – from Arripiado to Vila Franca de Xira (NNE-SSW); V – from Vila Franca de Xira to the Atlantic shoreline. The faults considered to be the limit of the referred fluvial sectors are: F1 – Ponsul-Arneiro fault (WSW-ENE); F2 – Gavião fault (NW-SE); F3 – Ortiga fault (NW-SE); F4 – Vila Nova da Barquinha fault (W-E); F5 – Arripiado-Chamusca fault (NNE-SSW). 1 – estuary; 2 – terraces; 3 – faults; 4 – Tagus main channel. The main Iberian drainage basins are also represented (inset). The lower and middle parts of the US unit, comprising an alternation of clayish silts with paleosols and minor sands to the east (flood-plain deposits) and sand deposits to the west (channel belt), have a probable age of ca. 325 to 200 ka. This points to formation during MIS9 to MIS7, under conditions of high to medium sea levels and warm to mild conditions. The upper part of the US unit, dominated by sand facies and with OSL ages of ca. 200 to 154 ka, correlates with the early part of the MIS6. During this period, progradation resulted from climate deterioration and relative depletion of vegetation that promoted enhanced sediment production in the catchment, coupled with initiation of sea-level lowering that increased the longitudinal slope. The Vale do Forno and Vale da Atela archaeological sites (Alpiarça, central Portugal) document the earliest human occupation in the Lower Tagus River, well established in geomorphological and environmental terms, within the Middle Pleistocene. The Lower Palaeolithic sites were found on the T4 terrace (+26 m, a.r.b.). The oldest artefacts previously found in the LG unit, display crude bifacial forms that can be attributed to the Acheulian, with a probable age of ca. 335 to 325 ka. The T4 US unit has archaeological sites stratigraphically documenting successive phases of an evolved Acheulian, that probably date ca. 325 to 300 ka. Notably, these Lower Palaeolithic artisans were able to produce tools with different sophistication levels, simply by applying different strategies: more elaborated reduction sequences in case of bifaces and simple reduction sequences to obtain cleavers. Fig. 2. . Simplified geologic map of the Lower Tagus Cenozoic basin, adapted from the Carta Geológica de Portugal, 1/500000, 1992). The study area (comprising the Vale do Forno and Vale de Atela sites) is located on the more upstream sector of the Lower Tagus River reach IV, between Arripiado and Chamusca villages. 1 – alluvium (Holocene); 2 – terraces (Pleistocene); 3 – sands, silts and gravels (Paleogene to Pliocene); 4 – Sintra Massif (Cretaceous); 5 – limestones, marls, silts and sandstones (Mesozoic); 6 – quartzites (Ordovician); 7 – basement (Proterozoic to Palaeozoic); 8 – main fault. The main Portuguese reaches of the Tagus River are identified (I to V). The VF3 site (Milharós), containing a Final Acheulian industry, with fine and elaborated bifaces) found in a stratigraphic level located between the T4 terrace deposits and a colluvium associated with Late Pleistocene aeolian sands (32 to 12 ka), has an age younger than ca. 154 ka but much older than 32 ka. In the study area, the sedimentary units of the T4 terrace seem to record the river response to sea-level changes and climatically-driven fluctuations in sediment supply. REFERENCES Cunha P. P., Almeida N. A. C., Aubry T., Martins A. A., Murray A. S., Buylaert J.-P., Sohbati R., Raposo L., Rocha L., 2012, Records of human occupation from Pleistocene river terrace and aeolian sediments in the Arneiro depression (Lower Tejo River, central eastern Portugal). Geomorphology, vol. 165-166, pp. 78-90.
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O presente documento de avaliação do projeto Margens de Desenvolvimento (EQUAL-A2-EM-154) assume-se como uma versão definitiva do 2º e último Relatório de Avaliação disponibilizada em 11 de Janeiro de 2005, nas instalações da Rota do Guadiana-ADI, em Serpa, de acordo com o estabelecido no Protocolo de Colaboração e Contrato de Prestação de Serviços, celebrado em 28 de Novembro de 2003, entre a Rota do Guadiana-ADI e a Universidade de Évora.
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O presente trabalho teve como objectivo identificar a influência da variedade e o impacto da fermentação maloláctica, no perfil em compostos fenólicos de baixa massa molecular de vinhos varietais do Alentejo. Para o efeito, foram doseados alguns compostos fenólicos (aldeído protocatéquico e ácidos gálico, protocatéquico, caftárico, vanílico, fertárico, siringico, cafeíco, p-coumárico, ferúlico e coutárico) em 81 vinhos varietais produzidos na Adega Experimental da Universidade de Évora, 48 da casta Trincadeira, e os restantes das castas Aragonez, Cabernet Sauvignon, Alfrocheiro, Castelão e Touriga Nacional. A análise dos dados obtidos, através do método da partição de variância, permitiu identificar a variedade como a variável que mais influência teve no perfil em compostos fenólicos de baixa massa molecular dos vinhos varietais
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Introdução: Entre os jovens, o uso regular ou abusivo do álcool parece aliar-se a fatores individuais, em ambiente social. O consumo de bebidas alcoólicas, nas faixas etárias mais jovens, segundo o World Development Report, vai além dos 60%. Objetivos: Este estudo pretendeu conhecer as influências pessoais, dos familiares, do grupo de pertença e do meio escolar, sobre os hábitos de abstinência e de consumo de bebidas alcoólicas entre os jovens. Métodos: Investigação de carácter qualitativo, com recurso a entrevistas compreensivas semiestruturadas, desenvolvido numa escola do distrito de Évora, Portugal. A amostra é constituída por 10 alunos do 8º ano de escolaridade, cinco não consumidores e cinco consumidores. Principais resultados: A experimentação acontece entre os 12-14 anos de idade em consequência da curiosidade, motivação explícita ou tácita, para “dar estilo”, do ambiente, da diversão e da observação de comportamentos. Entre os efeitos da ingestão indicados como motivadores ao consumo destaca-se o atingir estados de alegria e boa disposição. Os familiares tendem a incentivar a ingestão moderada em ocasiões festivas. Os elementos do grupo de pertença tendem a motivar, de forma explícita, à ingestão, entre os alunos consumidores. Conclusão: A ingestão de bebidas alcoólicas entre os jovens sofre as influências pessoal, familiar e do grupo de pertença. As iniciativas desenvolvidas na escola tendem a não surtir efeito.
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Existirão certamente mais jardins que jardineiros e, definitivamente, mais lugares da Antropologia que Antropólogos. No panorama português, Francisco Martins Ramos é o Antropólogo ao Sul. Docente universitário por mais de 30 anos na Universidade de Évora (Portugal), aí percorreu todas as etapas da carreira académica, de Assistente Estagiário a Professor Catedrático e a ela continua ligado como Professor Emérito, título que lhe foi atribuído em 2010. O Jardineiro do Cacuaco é o nono livro do Autor. Trata-se de uma obra eminentemente académica, orientada para estudantes de Antropologia mas, sobretudo para os seus alunos, antigos e actuais, que certamente gostarão de (re)encontrar em formato de livro textos de cariz antropológico, alguns inéditos, outros já publicados e agora actualizados. Ao todo, e para além das palavras prévias e de um Prefácio docemente intitulado “Os Exercícios de Francisco Ramos ou a Ternura da Memória”, da autoria de Jorge Gaspar, a obra é composta por dezoito textos tematicamente diferenciados e de estrutura, dimensão e estilo narrativo variável, a que se junta um pequeno conto, o qual, aliás, dá o nome ao volume. No livro que agora vem à estampa pelas Edições Colibri, Francisco Martins Ramos reúne alguns dos já clássicos lugares da Antropologia, revê e acrescenta outros e a todos dá profundidade. Da superfície para o fundo, este é um livro de e sobre lugares: geográficos, académicos, simbólicos e, também, afectivos. E em todos esses lugares a Antropologia respira; é não apenas o substantivo mas também o verbo que o autor habilmente conjuga da sociedade vila-velhense ao mundo globalizado, como aliás tinha já insignemente demonstrado em De Monsaraz a Melbourne: Reflexões Antropológicas numa Era Global (Edições Colibri, 2012).
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Greenhouse production is a very important activity in the West region of Portugal, with an area of approximately 800 ha where the regular production consists in two crops per year, one in winter-spring and the other in summer-autumn. Many growers are now prepared to better exploit market opportunities, since they know that the big export window opportunity is from June to September, when the production is difficult in other regions of south due to high temperatures. Grower’s use new and more productive varieties, either in soil or hydroponic systems, mostly in unheated greenhouses, naturally ventilated, and equipped with modern fertigation systems. Greenhouse production causes some environmental impacts due to the high use of inputs. Several improvements in technologies and crop practices may contribute to increase the use efficiency of resources, decreasing the negative environmental impacts. Greenhouse vegetable production in Northern EU countries is based on the supply of heating and differs significantly from the production system in the Southern EU countries. In the Northern countries, direct energy inputs, mostly for heating, are predominant while in the South the indirect energy input is also important, mainly associated with fertilizers, plastic cover materials and other auxiliary materials. The main objective of this work was to characterise the greenhouse production systems in the West region of Portugal, in order to evaluate the energetic consumptions (direct and indirect), the GHH emissions, the production costs and the farmer’s income. With this work the mostly important inputs were identified, allowing proposing alternative measures to improve efficiency and sustainability. All the data was obtained by surveys performed directly with growers, previously selected to be representative of the crop practices and greenhouse type of the region. However, more research should be performed in order to develop and to test technologies capable to improve resources use efficiency in greenhouse production.
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Olive tree sap flow measurements were collected in an intensive orchard near Évora, Portugal, during the irrigation seasons of 2013 and 2014, to calculate daily tree transpiration rates (T_SF). Meteorological variables were also collected to calculate reference evapotranspiration (ETo). Both data were used to assess values of basal crop coefficient (Kcb) for the period of the sap flow observations. The soil water balance model SIMDualKc was calibrated with soil, biophysical ground data and sap flow measurements collected in 2013. Validated in 2014 with collected sap flow observations, the model was used to provide estimates of dual e single crop coefficients for 2014 crop growing season. Good agreement between model simulated daily transpiration rates and those obtained with sapflow measurements was observed for 2014 (R2=0.76, RMSE=0.20 mm d-1), the year of validation, with an estimation average absolute error (AAE) of 0.20 mm d-1. Olive modeled daily actual evapotranspiration resulted in atual ETc values of 0.87, 2.05 and 0.77 mm d-1 for 2014 initial, mid- and end-season, respectively. Actual crop coefficient (Kc act) values of 0.51, 0.43 and 0.67 were also obtained for the same periods, respectively. Higher Kc values during spring (initial stage) and autumn (end-stage) were published in FAO56, varying between 0.65 for Kc ini and 0.70 for Kc end. The lower Kc mid value of 0.43 obtained for the summer (mid-season) is also inconsistent with the FAO56 expected Kc mid value of 0.70 for the period. The modeled Kc results are more consistent with the ones published by Allen & Pereira [1] for olive orchards with effective ground cover of 0.25 to 0.5, which vary between 0.40 and 0.80 for Kc ini, 0.40–0.60 for Kc mid with no active ground cover, and 0.35–0.75 for Kc end, depending on ground cover. The SIMDualKc simulation model proved to be appropriate for obtaining evapotranspiration and crop coefficient values for our intensive olive orchard in southern Portugal.
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Biophysical and meteorological variables as well as radiometric canopy temperatures were collected in an intensive orchard near Évora, Portugal, with 28% ground cover by canopy and combined in a simplified two-source energy balance model (STSEB) to independently calculate the olive tree transpiration (T_STSEB) component of the total evapotranspiration (ETc). Sap flow observations were simultaneously taken in the same orchard allowing also for independent calculations of tree transpiration (T_SF). Model water use results were compared with water use estimates from the sap flow measurements. Good agreement was observed (R2=0.86, RMSE=0.20 mm d-1), with an estimation average absolute error (AAE) of 0.17 mm d-1. From June to August, on average olive water use were 1.92 and 1.89 mm d-1 for sap flow and STSEB model respectively, and 1.38 and 1.58 mm d-1 for the month of September. Results were also used to assess the olive basal crop coefficients (Kcb). Kcb estimates of 0.33 were obtained for sap flow and STSEB model, respectively, for June to August, and of 0.44 and 0.53 for the month of September. Basal crop coefficients were lower than the suggested FAO56 average Kcb values of 0.65 for June to August, the crop mid-season growth stage, and of 0.65 for the month of September, the end-season.
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O livro antigo continua a ter leitores, sobretudo, entre os investigadores na área das humanidades. A sua existência já não se confina às estantes das bibliotecas, dado que se encontra disponível nas bibliotecas digitais de todo o mundo, embora nem sempre seja disponibilizado de forma adequada. As humanidades digitais reforçaram a necessidade de colocar conteúdos em linha, dando enfase à sua utilização e reutilização e permitindo que as obras possam ser lidas, tanto pelo homem, como por algoritmos informáticos. A colocação do livro antigo em linha implica, em primeiro lugar, que se conheça as suas características materiais, em seguida, que se determine quais os requisitos dos investigadores. A partir destes pressupostos, analisamos duas bibliotecas digitais portuguesas, a Biblioteca Nacional Digital (BND) e a Alma Mater da Universidade de Coimbra e, em particular, a coleção de livro antigo disponibilizado na BND.
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Nas bibliotecas municipais portuguesas existe um vasto património bibliográfico que urge conhecer e divulgar. Por conseguinte, neste short paper pretende-se apresentar o projeto “RECOPA: Rede de Coleções Patrimoniais das Bibliotecas do Alentejo”, desenvolvido no âmbito da linha de investigação Literacias e Património Textual (lpt) do Centro Interdisciplinar de História, culturas e Sociedades da Universidade de Évora (CIDEHUSUE/FCT). O projeto tem como finalidade a constituição de uma rede que, com o intuito de revalorizar este património, ligue todas as bibliotecas municipais do Alentejo detentoras de coleções patrimoniais, dando-as a conhecer ao público em geral. Correspondendo aos desafios colocados pelas Humanidades Digitais, pois ultrapassa a digitalização e disponibilização de fontes primárias, o projeto facultará ferramentas para a análise e divulgação dessas fontes, contribuindo para que a aquisição cognitiva seja mais fácil, imediata e intuitiva. O short paper organizar-se-á nos seguintes termos: a) apresentação dos objetivos do projeto; b) apresentação das fases que o constituem, resultados esperados e parcerias; c) conclusões/recomendações.
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En esta investigación pretendemos conocer si las emociones que experimenta el alumnado de Primaria al ser evaluado con rúbrica pueden verse afectadas por la formación y el conocimiento que sobre dicho instrumento se les presupone a sus evaluadores. Por ello, se establece una comparativa entre las emociones que sienten los estudiantes al ser evaluados por profesores (a los que se les reconoce una formación sobre rúbrica) y las que sienten aquellos que son coevaluados por sus iguales o autoevaluados. Un total de 66 alumnos del 2º ciclo de Enseñanza Básica (10 años y 11 años) de Évora (Portugal), que habían tenido experiencia de heteroevaluación, autoevaluación o coevaluación con rúbrica, cumplimentaron un amplio cuestionario. Los resultados muestran que cerca de un 62% de los estudiantes que fueron evaluados por pares o autoevaluados a través de una rúbrica experimentan emociones positivas, frente a un 91 % de aquellos cuyo trabajo fue valorado por profesores utilizando dicho instrumento. En consonancia con este dato, existe mayor probabilidad de experimentar emociones positivas cuando se recibe una evaluación con rúbrica por parte de un maestro que cuando la valoración procede de un igual o de uno mismo. También se ha observado que el porcentaje de estudiantes que experimenta emociones negativas es mayor cuando no son evaluados por el profesor. Además, un 76 % de los alumnos evaluados con rúbrica por los compañeros considera que esta acción puede ayudarles, frente a un 81% de los evaluados por el docente que comparten esta opinión. Por último, cabe destacar la posibilidad de que estos resultados estén mediatizados por la percepción de que una evaluación realizada por un igual no posee la misma calidad que la que lleva a cabo un profesor.
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This article assesses how the last-visit features and the socio-demographic profile of tourists moderate repeat-visit patterns to Portugal, a mature destination where the persistence of loyal visitors has made its mark on tourism development. The methodology used is a survival analysis to assess the tourists’ repeat patterns. To test the model, a database of 4612 observations was employed, which was obtained from a survey of international tourists. Only repeat visitors with more than two visits over the years were considered for the purpose of the research. The study finds that a combination of socio-demographic characteristics, expectation/satisfaction, trip purpose, pull motivations and regional destination has a positive effect on repeat patterns, confirming that tourists’ willingness to repeat visits to Portugal is far from ceasing. Based on those tourists to Portugal who declared when they started to visit the country, and the number of years of their repeat visits, the article contributes to the literature by introducing new methods of assessing tourists’ repeat patterns for destinations.
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The impact of different irrigation scheduling regimes on the water use, yield and water productivity from a high-density olive grove cv. Cobrançosa in southern Portugal was assessed during the irrigation seasons of 2011, 2012, 2013 and 2014. The experiments were conducted in a commercial olive orchard at the Herdade Álamo de Cima, near Évora (38o 29' 49.44'' N, 7o 45' 8.83'' W; alt. 75 m) in southern Alentejo, Portugal. The orchard was established with 10-year old Cobrançosa trees in grids of 8.0 x 4.2 m (300 trees ha-1) in the E-W direction, and experiments conducted on a shallow sandy loam Regosoil Haplic soil. From mid-May to the end of September the orchard was irrigated and three plots were subjected to one of two irrigation treatments: a control treatment A, irrigated to replace 100% ETc, a moderate deficit irrigation treatment B irrigated to 70% of ETc, and a more severe deficit irrigation treatment C that provided for approximately 50% of ETc. Daily tree transpiration rates were obtained by continuously monitoring of sap flow in representative trees per treatment. Among the irrigated treatments, water use efficiency (WUE, ratio of water used to irrigation- water applied) of treatment C was the highest, with a value of 0.89, being treatment B slightly lower, with a WUE of 0.76. Olive harvest for 2012 was an exceptional “on year”. Bearing yields showed contrasting differences within years where an “on year” was followed by an “off year”. In 2011 and 2012 treatment B yields were 41 and 50% higher than treatment C, respectively. In 2013 treatment B yield was 45% higher than yield of the fully irrigated treatment A, and treatment C showed practically the same yield than treatment A. In the “on year” of 2014 treatment B averaged 48% higher yield than treatment C. Treatment B farm irrigation water productivity (WPI-Farm, ratio of yield to water applied) was the highest among all treatments. Treatment A showed the lowest conversion efficiency of all treatments, indicating treatment B as the adequate deficit irrigation treatment for our Cobrançosa orchard