16 resultados para tip-timing

em Repositório Científico do Instituto Politécnico de Lisboa - Portugal


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El acompañante musical de danza (AMD) traduce a sonido secuencias de movimiento, basando su práctica en la observación de las acciones motoras del bailarín. ¿Cómo es que el AMD llega a comprender las calidades motoras en términos musicales? ¿Qué es lo que el AMD identifica a partir de su observación? ¿Cuáles son las diferencias y semejanzas de timing de las representaciones motoras en el planeamiento de una acción cuando se trabaja con estímulos auditivos y visuales en simultáneo? Con el objeto de comenzar a responder algunas de esos interrogantes se diseñó un estudio en el que se indagan diferentes aspectos de la habilidad para sincronizar con la imagen y el sonido de una secuencia de danza de las personas habitualmente involucradas en la realización de este tipo de secuencias (Profesores, Estudiantes Bailarines y AMD).

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Este trabalho tem como objectivo apresentar as ferramentas do Lean Thinking e realizar um estudo de caso numa organização em que este sistema é utilizado. Numa primeira fase do trabalho será feito uma análise bibliográfica sobre o ―Lean Thinking”, que consiste num sistema de negócios, uma forma de especificar valor e delinear a melhor sequência de acções que criam valor. Em seguida, será realizado um estudo de caso numa Empresa – Divisão de Motores – no ramo da aeronáutica com uma longa e conceituada tradição com o objectivo de reduzir o TAT (turnaround time – tempo de resposta), ou seja, o tempo desde a entrada de um motor na divisão até à entrega ao cliente. Primeiramente, analisando as falhas existentes em todo o processo do motor, isto é, a análise de tempos de reparação de peças à desmontagem do motor que têm que estar disponíveis à montagem do mesmo, peças que são requisitadas a outros departamentos da Empresa e as mesmas não estão disponíveis quando são precisas passando pelo layout da divisão. Por fim, fazer uma análise dos resultados até então alcançados na divisão de Motores e aplicar as ferramentas do ―Lean Thinking‖ com o objectivo da implementação. É importante referir que a implementação bem-sucedida requer, em primeiro lugar e acima de tudo, um firme compromisso da administração com uma completa adesão à cultura da procura e eliminação de desperdício. Para concluir o trabalho, destaca-se a importância deste sistema e quais são as melhorias que se podem conseguir com a sua implantação.

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We present a palaeomagnetic study on 38 lava flows and 20 dykes encompassing the past 1.3 Myr on S. Jorge Island (Azores ArchipelagoNorth Atlantic Ocean). The sections sampled in the southeastern and central/western parts of the island record reversed and normal polarities, respectively. They indicate a mean palaeomagnetic pole (81.3 degrees N, 160.7 degrees E, K= 33 and A95= 3.4 degrees) with a latitude shallower than that expected from Geocentric Axial Dipole assumption, suggesting an effect of non-dipolar components of the Earth magnetic field. Virtual Geomagnetic Poles of eight flows and two dykes closely follow the contemporaneous records of the Cobb Mountain Subchron (ODP/DSDP programs) and constrain the age transition from reversed to normal polarity at ca. 1.207 +/- 0.017 Ma. Volcano flank instabilities, probably related to dyke emplacement along an NNWSSE direction, led to southwestward tilting of the lava pile towards the sea. Two spatially and temporally distinct dyke systems have been recognized on the island. The eastern is dominated by NNWSSE trending dykes emplaced before the end of the Matuyama Chron, whereas in the central/western parts the eruptive fissures oriented WNWESE controlled the westward growth of the S. Jorge Island during the Brunhes Chron. Both directions are consistent with the present-day regional stress conditions deduced from plate kinematics and tectonomorphology and suggest the emplacement of dykes along pre-existing fractures. The distinct timing and location of each dyke system likely results from a slight shift of the magmatic source.

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Introdução – A doença oncológica tem sido assunto de abordagem historiográfica particularmente abundante no contexto internacional. No caso português só recentemente começaram a surgir os primeiros trabalhos em redor desta ampla temática. Objetivos – Revolvendo em torno da emergência e estruturação da luta anticancerosa no âmbito internacional, pretende-se apresentar uma breve síntese sobre a evolução deste fenómeno em Portugal na primeira metade do século XX. Metodologia – Análise documental. Qualitativa e heurística. Resultados/Discussão/Considerações finais – A luta contra a doença oncológica em Portugal não destoou do contexto médico-científico e do movimento internacional anticanceroso da primeira metade do século XX. No entanto, a emergência e a institucionalização do projeto anticanceroso nacional apresentou algumas particularidades. Inserido entre uma especialidade médica em processo de afirmação e as necessidades assistenciais dos cancerosos, resultou da conjugação de uma série de fatores que ultrapassam a mera assimilação de novas tecnologias médicas ou da criação de um espaço próprio para a prática da oncologia. Tornou-se também num meio para realizar um trabalho intenso de educação para a saúde, num instrumento de ponta na formação médica especializada e numa referência de modernidade científica no contexto do Estado Novo.

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Dissertação apresentada à Escola Superior de Educação de Lisboa para obtenção de grau de mestre em Ciências da Educação - Especialidade Educação Especial

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Dissertação para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Vias de Comunicação e Transportes

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Dissertação apresentada à Escola Superior de Educação de Lisboa para a obtenção de grau de mestre em Ciências da Educação, Especialização em Intervenção Precoce

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Relatório Final de Estágio apresentado à Escola Superior de Dança com vista à obtenção do Grau de Mestre em Ensino de Dança.

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Micro-generation is the small scale production of heat and/or electricity from a low carbon source and can be a powerful driver for carbon reduction, behavior change, security of supply and economic value. The energy conversion technologies can include photovoltaic panels, micro combined heat and power, micro wind, heat pumps, solar thermal systems, fuel cells and micro hydro schemes. In this paper, a small research of the availability of the conversion apparatus and the prices for the micro wind turbines and photovoltaic systems is made and a comparison between these two technologies is performed in terms of the availability of the resource and costs. An analysis of the new legal framework published in Portugal is done to realize if the incentives to individualspsila investment in sustainable and local energy production is worth for their point of view. An economic evaluation for these alternatives, accounting with the governmentpsilas incentives should lead, in most cases, into attractive return rates for the investment. Apart from the attractiveness of the investment there are though other aspects that should be taken into account and those are the benefits that these choices have to us all. The idea is that micro-generation will not only make a significant direct contribution to carbon reduction targets, it will also trigger a multiplier effect in behavior change by engaging hearts and minds, and providing more efficient use of energy by householders. The diversified profile of power generation by micro-generators, both in terms of location and timing, should reduce the impact of intermittency or plant failures with significant gains for security of supply.

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A detailed analysis of fabrics of the chilled margin of a thick dolerite dyke (Foum Zguid dyke, Southern Morocco) was performed in order to better understand the development of sub-fabrics during dyke emplacement and cooling. AMS data were complemented with measurements of paramagnetic and ferrimagnetic fabrics (measured with high field torque magnetometer), neutron texture and microstructural analyses. The ferrimagnetic and AMS fabrics are similar, indicating that the ferrimagnetic minerals dominate the AMS signal. The paramagnetic fabric is different from the previous ones. Based on the crystallization timing of the different mineralogical phases, the paramagnetic fabric appears related to the upward flow, while the ferrimagnetic fabric rather reflects the late-stage of dyke emplacement and cooling stresses. (C) 2014 Elsevier B.V. All rights reserved.

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We present a palaeomagnetic study on 38 lava flows and 20 dykes encompassing the past 1.3 Myr on S. Jorge Island (Azores ArchipelagoNorth Atlantic Ocean). The sections sampled in the southeastern and central/western parts of the island record reversed and normal polarities, respectively. They indicate a mean palaeomagnetic pole (81.3 degrees N, 160.7 degrees E, K= 33 and A95= 3.4 degrees) with a latitude shallower than that expected from Geocentric Axial Dipole assumption, suggesting an effect of non-dipolar components of the Earth magnetic field. Virtual Geomagnetic Poles of eight flows and two dykes closely follow the contemporaneous records of the Cobb Mountain Subchron (ODP/DSDP programs) and constrain the age transition from reversed to normal polarity at ca. 1.207 +/- 0.017 Ma. Volcano flank instabilities, probably related to dyke emplacement along an NNWSSE direction, led to southwestward tilting of the lava pile towards the sea. Two spatially and temporally distinct dyke systems have been recognized on the island. The eastern is dominated by NNWSSE trending dykes emplaced before the end of the Matuyama Chron, whereas in the central/western parts the eruptive fissures oriented WNWESE controlled the westward growth of the S. Jorge Island during the Brunhes Chron. Both directions are consistent with the present-day regional stress conditions deduced from plate kinematics and tectonomorphology and suggest the emplacement of dykes along pre-existing fractures. The distinct timing and location of each dyke system likely results from a slight shift of the magmatic source.

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Seismic ambient noise tomography is applied to central and southern Mozambique, located in the tip of the East African Rift (EAR). The deployment of MOZART seismic network, with a total of 30 broad-band stations continuously recording for 26 months, allowed us to carry out the first tomographic study of the crust under this region, which until now remained largely unexplored at this scale. From cross-correlations extracted from coherent noise we obtained Rayleigh wave group velocity dispersion curves for the period range 5–40 s. These dispersion relations were inverted to produce group velocity maps, and 1-D shear wave velocity profiles at selected points. High group velocities are observed at all periods on the eastern edge of the Kaapvaal and Zimbabwe cratons, in agreement with the findings of previous studies. Further east, a pronounced slow anomaly is observed in central and southern Mozambique, where the rifting between southern Africa and Antarctica created a passive margin in the Mesozoic, and further rifting is currently happening as a result of the southward propagation of the EAR. In this study, we also addressed the question concerning the nature of the crust (continental versus oceanic) in the Mozambique Coastal Plains (MCP), still in debate. Our data do not support previous suggestions that the MCP are floored by oceanic crust since a shallow Moho could not be detected, and we discuss an alternative explanation for its ocean-like magnetic signature. Our velocity maps suggest that the crystalline basement of the Zimbabwe craton may extend further east well into Mozambique underneath the sediment cover, contrary to what is usually assumed, while further south the Kaapval craton passes into slow rifted crust at the Lebombo monocline as expected. The sharp passage from fast crust to slow crust on the northern part of the study area coincides with the seismically active NNE-SSW Urema rift, while further south the Mazenga graben adopts an N-S direction parallel to the eastern limit of the Kaapvaal craton. We conclude that these two extensional structures herald the southward continuation of the EAR, and infer a structural control of the transition between the two types of crust on the ongoing deformation.

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Trabalho final de Mestrado para obtenção do grau de Mestre em Engenharia de Electrónica e Telecomunicações