21 resultados para Alchornea Sw.

em Consorci de Serveis Universitaris de Catalunya (CSUC), Spain


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El projecte que es presenta a continuació, té com a objectiu implementar un sistema HW/SW encastat en una FPGA, capaç d’executar funcions de control remot per infraroig en plataformes de televisió flexibles de Sony Corp. El disseny obtingut, s’incorporarà a un sistema més ampli de verificació i test de circuits impresos, dins del marc de producció SMD. La finalitat d’aquest projecte, és la realització d’un sistema flexible per a la implementació de comandaments de comunicació per infraroig amb circuits impresos. Prèviament, s’ha estudiat els conceptes bàsics referents a la implementació de sistemes amb FPGAs, la seva metodologia de desenvolupament i les principals característiques de la seva arquitectura. Com a especificacions, s’ha utilitzat l’estàndard de control remot per infraroig de Sony Corp SIRCS (Sony Infrared remote control system).

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The distribution patterns of benthic algal assemblages in the Tinto, Odiel and Piedras rivers were analyzed during the winter of 2005 in 18 sampling stations. The main objective was to assess and compare the algal communities and parameters affecting them both in the zones affected by acid mine drainage (AMD) and in naturally alkaline waters. A total of 108 benthic diatom taxa and 31 non-diatom taxa were identi ed. Results showed large differences between algal communities in the two environments: Pinnularia acoricola, P. subcapitata and Eunotia exigua were the most frequent diatom taxa in regions affected by acid mine drainage, along with algae like Klebsormidium and Euglena mutabilis were the most relevant non-diatom taxa. In alkaline waters the dominant diatom taxa were Planothidium frequentissimum, Gomphonema angustum, Fragilaria capucina, and some species of Navicula (N. viridula, N. veneta or N. radiosa), accompanied by Oscillatoria and Anabaena as well as by streptophytes of the group of zygnemataceae and desmidiaceae

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Els sediments del fons marí són molt importants en els ecosistemes aquàtics. Aquests sediments són considerats absorbents naturals, ja que s’hi acumulen moltes substàncies nocives, com ara metalls pesants i contaminants orgànics persistents (COPs). En aquest estudi s’han analitzat mostres de sediments del mar Mediterrani amb la finalitat d’examinar els COPs i la possible procedència d’hidrocarburs derivats del petroli. Les mostres han estat extretes davant de la desembocadura del riu Besòs (se n’ha fet una extracció a 8 km i una altra a 54 km de distància respecte la costa) i davant del municipi català anomenat Vilanova i la Geltrú (se n’ha fet, també, una extracció a 8-10 km i una altra a 30-40 km de distància respecte la costa). D’aquestes mostres, obtingudes per perforació, se n’han analitzat el primer i segon centímetres. S’han quantificat els hidrocarburs aromàtics policíclics (PAHs), els bifenils policlorats (PCBs) i els compostos organoclorats (OCPs) utilitzats antigament com a pesticides. S’ha posat de manifest que en les zones més properes a la costa, les concertacions COPs són més elevades a la regió més meridional, tot i estar davant de la desembocadura del riu Besòs. Segurament això és degut a la influència de la deriva litoral (corrent costaner marí en direcció NE-SW). Finalment, l’índex Phytane/Pristane, l’índex de preferència de carboni o, en anglès Carbon Preference Index (CPI) i la barreja complexa sense resoldre o, en anglès, Unresolved Complex Mixture (UCM) apunten a la conclusió que l’origen dels hidrocarburs analitzats (n-alcans) podria ser petrogènic.

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Se ha desarrollado en la empresa UNIT 4 de acuerdo con un convenio que tienen con la Escola d’Enginyeria de la UAB. Esta empresa se dedica al desarrollo de SW para pequeñas y grandes empresas y disponen de un ERP (ekon) que incluye una sección (ekon finanzas) destinada a la gestión de finanzas. En este caso el proyecto estará dentro del apartado de gestión de facturas. La tecnología con la que se realizara el proyecto es con Eclipse y el lenguaje de programación será Java además de las aplicación karat para crear los formularios y SQL server para la base de datos.

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We report here a new empirical density functional that is constructed based on the performance of OPBE and PBE for spin states and SN 2 reaction barriers and how these are affected by different regions of the reduced gradient expansion. In a previous study [Swart, Sol̀, and Bickelhaupt, J. Comput. Methods Sci. Eng. 9, 69 (2009)] we already reported how, by switching between OPBE and PBE, one could obtain both the good performance of OPBE for spin states and reaction barriers and that of PBE for weak interactions within one and the same (SSB-sw) functional. Here we fine tuned this functional and include a portion of the KT functional and Grimme's dispersion correction to account for π- π stacking. Our new SSB-D functional is found to be a clear improvement and functions very well for biological applications (hydrogen bonding, π -π stacking, spin-state splittings, accuracy of geometries, reaction barriers)

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The Guilleries are a small and mountainous area located in the north-westem part of the Catalonian Coastal Ranges where metamorphic and igneous Paleozoic rocks are exposed. After the main hercynian folding this area was affected by a brittle deformation that is mainly manifested by the intrusion of a very large number of dykes of granodiorite and the development of a complex joint system. Trends of dykes indicate that their intrusion was related to a SE-NW extension, whose estimated value is 40% on an average. This extension seems to stand, although without any associated igneous event, with the development of NE-SW directed joints which make the main set. Five families more were developed later, onegently-dipping and fou upright; the latter trending roughly SE-NW, ENE-WSW, ESE-WNW and N-S. AU the joint sets appear in the metasedimentary Paleozoic rocks and in the hercynian intrusive bodies. Concerning the ages, joints that belong to the NE-SW and SE-NW directed sets and also those slightly dipping have been attributed to the late-hercynian times and all the other are considered to be later

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This paper, fundamentally stratigraphic, is based on the vertical distribution of fauna in sediments which constitute the Montgri Massif. The stratigraphic series is composed of two units: one allochtonous (Mesozoic) and a second one autochtonous (Paleogene). The latter crops out in front of the thrust belt and presents the typical facies described by PALLI (1972). The allochtonous part is formed by the following units (from bottom to top): variegated gypsiferous shales of Keuper age; marls, limestones and dolomites from the Lias (Domerian); gray breccia ted dolomites: supraliassic; and Cretaceous limestones with rare interbeds of calcareous marls and nodular shaly marls. In this unit the Neocomian, Barremian (?), Aptian, Albian, Cenomanian, Turonian (?) and Santonian haven been recognized. Structurally, the Montgri Massif is part of a thrust belt which has been divided into three parts of different development ang age. Both parts are affected by ample synclinal folds of NE-SW directions and fractures of NW-SE orientation. The fractures condition the torrential streams as well as the karstic phenomena present in the Massif. These and the eolian actions are the main causes of the present geomorphology of the Montgri

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Las características geoquímicas (elementos mayores y trazas) de las rocas analizadas son similares a las del arco volcánico de Ke rmadec en Pa c í fico SW. Por último, los bajos contenidos en REE, el patrón de REE con morfología plana, así como los bajos contenidos en elementos incompatibles (K, Rb, Zr, Th) son similares a los de las series tipo IAT presentes en el arco volcánico del Caribe. Estos nuevos datos sobre el volcanismo del Paleógeno de la Sierra Maestra sugieren que los modelos de placas tectónicas que han sido propuestos para explicar el origen del arco volcánico de Sierra Maestra deben ser revisados.

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Las mineralizaciones filonianas del area de L'Argentera estan encajadas indistintamente en la srie sedimentaria pre-carbonfera y carbonfera y en las granodioritas tardihercinicas. NE-SW y presentan dos asociaciones minerales geograficamente bien discriminadas: de Ba-(F) y de cuarzo + galena + arseniuros de Ni-Co. La serie detrtica roja discordante del Triasico inferior (Buntsandstein) muestra asimismo cemento de baritina (fluorita) o cuarzo, en neta correspondencia con las asociaciones minerales de los filones infrayacentes encajados en el zcalo hercnico. Gran parte del contenido filoniano se deposit a partir de soluciones altarnente salinas (20% NaCl peso eq.) y de bajas temperaturas (90 a 120C). Las observaciones realizadas son compatibles con un modelo deposicional basado en una mezcla de aguas termales ascendentes en fracturas permeables y soluciones sulfatadas percolantes a partir de un ambiente de tipo sabkha instalado en el Buntsandstein superior.

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En el presente trabajo se describen las principales características estratigráficas y sedimentológicas del relleno de la fosa de la Cerdanya. A partir de éstas se han diferenciado dos unidades: la Unidad Neógena Inferior y la Unidad Neógena Superior que reflejan dos situaciones tectónicas diferentes. La Unidad Inferior corresponde al período de formación y posterior evolución de la fosa bajo el movimiento direccional de la falla NE-SW de la Tet, mientras que la Unidad Superior refleja una situación extensional generalizada. La revisión de los numerosos yacimientos de Mamíferos fósiles de la Unidad Neógena Inferior, expuesta en esta nota, permiten concluir que esta se sedimentó en el Vallesiense. Por contra, el hallazgo del nuevo yacimiento de Can Vilella, indican que la sedimentación de la Unidad Superior se inició en el Turoliense superior (MN 13)

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En este trabajo se presentan los resultados derivados de la interpretacón de 320 estaciones gravimétricas realizadas sobre el diapiro de Cardona con el objetivo de obtener información sobre su geometría tridimensional. Para obtener una distribución tridimensional de la masa salina que explique las anomalías observadas se ha aplicado un método iterativo de ajustes sucesivos basado en un algoritmo de inversión automática. Esta metodología ha mostrado ser muy rápida, fácil de usar y con suficiente poder de resolución para perfilar no sólo la geometría del cuerpo salino, sino también la de estructuras similares. El diapiro salino de Cardona presenta un mínimo gravimétrico relacionado con el anticlinal de Pins-Cardona que se prolonga hacia el SW. El análisis cualitativo de la anomalía residual permite apreciar que el diapiro muestra una cierta vergencia hacia sur con un flanco sureste subvertical y un flanco noroeste con pendientes más suaves.

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Background: Interventions designed to increase workplace physical activity may not automatically reduce high volumes of sitting, a behaviour independently linked to chronic diseases such as obesity and type II diabetes. This study compared the impact two different walking strategies had on step counts and reported sitting times. Methods: Participants were white-collar university employees (n = 179; age 41.3 ± 10.1 years; 141 women), who volunteered and undertook a standardised ten-week intervention at three sites. Preintervention step counts (Yamax SW-200) and self-reported sitting times were measured over five consecutive workdays. Using pre-intervention step counts, employees at each site were randomly allocated to a control group (n = 60; maintain normal behaviour), a route-based walking group (n = 60; at least 10 minutes sustained walking each workday) or an incidental walking group (n = 59; walking in workday tasks). Workday step counts and reported sitting times were re-assessed at the beginning, mid- and endpoint of intervention and group mean± SD steps/day and reported sitting times for pre-intervention and intervention measurement points compared using a mixed factorial ANOVA; paired sample-t-tests were used for follow-up, simple effect analyses. Results: A significant interactive effect (F = 3.5; p < 0.003) was found between group and step counts. Daily steps for controls decreased over the intervention period (-391 steps/day) and increased for route (968 steps/day; t = 3.9, p < 0.000) and incidental (699 steps/day; t = 2.5, p < 0.014) groups. There were no significant changes for reported sitting times, but average values did decrease relative to the control (routes group = 7 minutes/day; incidental group = 15 minutes/day). Reductions were most evident for the incidental group in the first week of intervention, where reported sitting decreased by an average of 21 minutes/day (t = 1.9; p < 0.057). Conclusion: Compared to controls, both route and incidental walking increased physical activity in white-collar employees. Our data suggests that workplace walking, particularly through incidental movement, also has the potential to decrease employee sitting times, but there is a need for on-going research using concurrent and objective measures of sitting, standing and walking.

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From 6 to 8 November 1982 one of the most catastrophic flash-flood events was recorded in the Eastern Pyrenees affecting Andorra and also France and Spain with rainfall accumulations exceeding 400 mm in 24 h, 44 fatalities and widespread damage. This paper aims to exhaustively document this heavy precipitation event and examines mesoscale simulations performed by the French Meso-NH non-hydrostatic atmospheric model. Large-scale simulations show the slow-evolving synoptic environment favourable for the development of a deep Atlantic cyclone which induced a strong southerly flow over the Eastern Pyrenees. From the evolution of the synoptic pattern four distinct phases have been identified during the event. The mesoscale analysis presents the second and the third phase as the most intense in terms of rainfall accumulations and highlights the interaction of the moist and conditionally unstable flows with the mountains. The presence of a SW low level jet (30 m s-1) around 1500 m also had a crucial role on focusing the precipitation over the exposed south slopes of the Eastern Pyrenees. Backward trajectories based on Eulerian on-line passive tracers indicate that the orographic uplift was the main forcing mechanism which triggered and maintained the precipitating systems more than 30 h over the Pyrenees. The moisture of the feeding flow mainly came from the Atlantic Ocean (7-9 g kg-1) and the role of the Mediterranean as a local moisture source was very limited (2-3 g kg-1) due to the high initial water vapour content of the parcels and the rapid passage over the basin along the Spanish Mediterranean coast (less than 12 h).

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Genetic and environmental trends in 2 lines of rabbit (B and R) selected on individual weight gain (WG) from weaning (4 wk) to slaughter (11 wk) were estimated using mixed model methodology. Line B was derived from the California breed and line R was a synthetic of stock of different origin. The data were collected from a single herd and comprised 7 718 individuals in line B and 9 391 in line R, the lines having 12 and 9 generations of selection respectively. Realized responses in the 2 lines were 2.7% and 2.2% of the initial mean per year respectively and showed that selection on WG was effective but was less than expected. Selection on slaughter weight (SW) and effects of selection on other economic traits are discussed. It is concluded that selection on either WG or SW is a simple method for improving growth rate in rabbit sire line stocks.

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In recent years, Semantic Web (SW) research has resulted in significant outcomes. Various industries have adopted SW technologies, while the ‘deep web’ is still pursuing the critical transformation point, in which the majority of data found on the deep web will be exploited through SW value layers. In this article we analyse the SW applications from a ‘market’ perspective. We are setting the key requirements for real-world information systems that are SW-enabled and we discuss the major difficulties for the SW uptake that has been delayed. This article contributes to the literature of SW and knowledge management providing a context for discourse towards best practices on SW-based information systems.