996 resultados para Incarcal (Crespià, Catalonia : Archaeological site)


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El poblat iberic de Montbarbat (Lloret de Mar-Ma~anet de la Selva, La Selva) té excavada l'area sud-oest, on es !roben diverses vivendes adossades al parament intem de la muralla. La datació deis sois d'habitació, que ve donada per la ceramica d'importació, correspon al segle IV i a inicis del segle III a.E. En aquest artiele s' estudien les llars i els elements relacionats amb elles, així com també un fom de coure aliments que hi ha en el mateix barrio.

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Presentem una figura d'animal fragmentada, realitzada amb fang, trobada al poblat iberic de Montbarbat (LLoret de Mar -Maçanet de la Selva, La Selva). 1 estudiem també diverses figures d'animals --exemptes o formant part de vasos-que provenen d'altres jaciments de Catalunya.

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El jaciment és situat dins del terme municipal de Santa Margalida, a la part meridional de la badia d' AIcúdia, damunt d'un petit illot de forma vagament el·lipsoidal, d'uns 70 m per 45 m, situat a uns 50 m de la línia de costa i a uns 500 m a l' oest de la gran necropoli de Son Real (o Punta deIs Fenicis) (Tarradell, 1964), amb la que guarda una relació evident (Uim. 1). La hipotesi que en epoca antiga hagués pogut estar unida aterra ferma (Tarradell, 1964,23) és, segons sembla, versemblant, pero de moment no ha estat verificada. Les restes arqueologiques es concentren a la meitat meridional, ja que la resta de l'illot a penes s'aixeca per damunt del nivell del mar i és batuda per les onades; no sembla probable que mai hi hagi hagut en aquesta zona cap tipus d'ocupació humana.

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Pese a que ya en algunos trabajos de fines del siglo XIX se cita la existencia de materiales arqueológicos en el Puig de Sant Andreu (Ullastret), y al hecho de que a instancia del Institut d'Estudis Catalans el enclave fuese incluido en el Registre del Patrimoni Historie, Artístie i Arqueologie de Catalunya l'any 1936 (DOGC de 08/07/1936), no fue hasta 1947 en que Miquel Oliva, animado por el Dr. Lluís Pericot, Comisario Provincial de Excavaciones en Gerona, inició las intervenciones sistemáticas en el yacimiento, realizando una labor ininterrumpida hasta su fallecimiento en 1974.

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A Embrapa Monitoramento por Satélite, há mais de uma década, utiliza a Internet como meio de difusão de resultados de pesquisa e de interação com clientes, parceiros e usuários. Com intuito de avaliar o uso do web site por esse público e o desempenho do sistema de comunicação eletrônica envolvido, tem-se utilizado o programa Webalizer, que monitora e elabora estatísticas de entradas e saídas do sistema, com base na análise de arquivos de log. Com os indicadores contabilizados pelo programa foi possível avaliar aspectos sobre a origem dos acessos, as ações executadas pelos usuários e sobre aspectos do desempenho do sistema em termos de respostas enviadas às solicitações dos usuários. Os resultados podem possibilitar a remodelagem do web site, de modo a melhorar a dinâmica de interação instituição-usuário e promover o desenvolvimento de uma abordagem própria de análise de logs.

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A partir da adaptação de um conjunto de critérios de avaliação de sites web centrados no usuário, foram identificados fatores motivadores de uso de site de governo eletrônico. O site web selecionado para análise foi o Comprasnet. O objetivo geral da pesquisa foi identificar os critérios determinantes na tomada de decisão pela opção de uso do Comprasnet. Para tanto, foram realizadas entrevistas por telefone, em âmbito nacional, com os usuários do Comprasnet. Concluiu-se com a apresentação e discussão dos fatores motivadores de uso do Comprasnet, e foram apresentadas as limitações e recomendações para estudos posteriores.

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This case study deals with a rock face monitoring in urban areas using a Terrestrial Laser Scanner. The pilot study area is an almost vertical, fifty meter high cliff, on top of which the village of Castellfollit de la Roca is located. Rockfall activity is currently causing a retreat of the rock face, which may endanger the houses located at its edge. TLS datasets consist of high density 3-D point clouds acquired from five stations, nine times in a time span of 22 months (from March 2006 to January 2008). The change detection, i.e. rockfalls, was performed through a sequential comparison of datasets. Two types of mass movement were detected in the monitoring period: (a) detachment of single basaltic columns, with magnitudes below 1.5 m3 and (b) detachment of groups of columns, with magnitudes of 1.5 to 150 m3. Furthermore, the historical record revealed (c) the occurrence of slab failures with magnitudes higher than 150 m3. Displacements of a likely slab failure were measured, suggesting an apparent stationary stage. Even failures are clearly episodic, our results, together with the study of the historical record, enabled us to estimate a mean detachment of material from 46 to 91.5 m3 year¿1. The application of TLS considerably improved our understanding of rockfall phenomena in the study area.

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After a rockfall event, a usual post event survey includes qualitative volume estimation, trajectory mapping and determination of departing zones. However, quantitative measurements are not usually made. Additional relevant quantitative information could be useful in determining the spatial occurrence of rockfall events and help us in quantifying their size. Seismic measurements could be suitable for detection purposes since they are non invasive methods and are relatively inexpensive. Moreover, seismic techniques could provide important information on rockfall size and location of impacts. On 14 February 2007 the Avalanche Group of the University of Barcelona obtained the seismic data generated by an artificially triggered rockfall event at the Montserrat massif (near Barcelona, Spain) carried out in order to purge a slope. Two 3 component seismic stations were deployed in the area about 200 m from the explosion point that triggered the rockfall. Seismic signals and video images were simultaneously obtained. The initial volume of the rockfall was estimated to be 75 m3 by laser scanner data analysis. After the explosion, dozens of boulders ranging from 10¿4 to 5 m3 in volume impacted on the ground at different locations. The blocks fell down onto a terrace, 120 m below the release zone. The impact generated a small continuous mass movement composed of a mixture of rocks, sand and dust that ran down the slope and impacted on the road 60 m below. Time, time-frequency evolution and particle motion analysis of the seismic records and seismic energy estimation were performed. The results are as follows: 1 ¿ A rockfall event generates seismic signals with specific characteristics in the time domain; 2 ¿ the seismic signals generated by the mass movement show a time-frequency evolution different from that of other seismogenic sources (e.g. earthquakes, explosions or a single rock impact). This feature could be used for detection purposes; 3 ¿ particle motion plot analysis shows that the procedure to locate the rock impact using two stations is feasible; 4 ¿ The feasibility and validity of seismic methods for the detection of rockfall events, their localization and size determination are comfirmed.

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B-cell-activating factor of the TNF family (BAFF)/BLyS contributes to B-cell homeostasis and function in the periphery. BAFF is expressed as a membrane-bound protein or released by proteolytic cleavage, but the functional importance of this processing event is poorly understood. Mice expressing BAFF with a mutated furin consensus cleavage site, i.e. furin-mutant BAFF (fmBAFF), were not different from BAFF-deficient mice with regard to their B-cell populations and responses to immunization. It is however noteworthy that an alternative processing event releases some soluble BAFF in fmBAFF mice. Mild overexpression (∼ 5-fold) of fmBAFF alone generated intermediate levels of B cells without improving humoral responses to immunization. Processed BAFF was however important for B-cell homeostasis, as peripheral B-cell populations and antibody responses were readily restored by administration of soluble BAFF trimers in BAFF-deficient mice. However, the rescue of CD23 expression in B cells of BAFF-deficient mice required both soluble BAFF trimers and fmBAFF, or a polymeric form of soluble BAFF (BAFF 60-mer). These results point to a predominant role of processed BAFF for B-cell homeostasis and function, and indicate possible accessory roles for membrane-bound BAFF.

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The correlation between the species composition of pasture communities and soil properties in Plana de Vic has been studied using two multivariate methods, Correspondence Analysis (CA) for the vegetation data and Principal Component Analysis (PCA) for the soil data. To analyse the pastures, we took 144 vegetation relevés (comprising 201 species) that have been classified into 10 phytocoenological communities elsewhere. Most of these communities are almost entirely built up by perennials, ranging from xerophilous, clearly Mediterranean, to mesophilous, related to medium-European pastures, but a few occurring in shallow soils are dominated by therophytes. As for the soil properties, we analysed texture, pH, depth, bulk density, organic matter, C/N ratio and the carbonates content of 25 samples, correspondingto representative relevés of the communities studied.

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On the basis of two parallel data sets refering to phenological events in open scrubs and pastures at two sites (Balaguer and Vic), the authors present a comprehensive report of the phenology of these Mediterranean communities. Four main phenophases (vegetative growth, flowering, fruiting and resting) were recorded monthly in 11 communities over 15 months. The results allow comparisons to be drawn between localities and communities, both at community and species levels, and to consider the effects of contemporary climatic data. This yielded useful information on general trends and on the particular responses of each community type to their corresponding constraints.

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The first part of a general survey of the vegetation of Catalonia andAndorra, this paper reports all the phytocoenological associations and subassociations recorded in this area. For each community, we provide the correct name and usual synonyms, its typification (where appropriate), all the references including relevés, and the most outstanding features of its structure, species composition, ecology, distribution and diversity. Moreover, associations and subassociations are ordered appropriately in a syntaxonomic scheme. Syntaxonomic ranks are considered in a fairly broad, conservative sense. This classification established 101 associations, which correspond to the classes Lemnetea, Zosteretea, Potametea, Littorelletea, Montio-Cardaminetea, Phragmiti-Magnocaricetea, Scheuchzerio-Caricetea, Isoeto-Nanojuncetea and Molinio-Arrhenatheretea.