943 resultados para Cutting


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RESUMO: Objectivo: Face à exiguidade de estudos em Portugal nesta temática, o objectivo do estudo foi a análise entre a aptidão cardiorrespiratória (ACR), e a prevalência da pré-obesidade e obesidade em crianças do 4º ano do 1º ciclo. Método: Foi efectuada uma revisão sistemática da literatura (RSL), evocando-se estudos tranversais e de RCT, cruzando-se com resultados do estudo observacional, do Agrupamento de Escolas Professor Armando Lucena, do concelho de Mafra, distrito de Lisboa. Do estudo de RSL, e estudo observacional, fez-se a análise da verificação da associação inversa, entre a “aptidão cardiorespiratória, a pré-obesidade e obesidade”. O estudo observacional, foi transversal, incidindo sobre 143 crianças, (73 raparigas) dos 9-12 anos de idade do concelho de Mafra. Foram utilizados os pontos de corte da International Obesity Task Force (IOTF), para definir a pré-obesidade e obesidade. Registou-se o IMC e a % Massa Gorda por bioimpedância. A avaliação da ACR foi efectuada através do teste Vaivém 20 metros Fitnessgram, utilizando-se equação de Fernhall et al., (1998). Os alunos foram avaliados por questionário sobre actividade física (AF) extra-curricular (QAD, Telama et al., 1997); os pais sobre os níveis AF (IPAQ, Bauman et al., 2009) e estatuto sócio-económico (ESE). Resultados: Os resultados do estudo observacional, corroboram os de outros estudos RSL. Não houve diferenças entre géneros na prevalência de pré-obesidade e obesidade: rapazes (20.55% e 8.21%) e raparigas (34.28% e 5.71%) (p<0.176). As crianças com maior ACR têm menor IMC (p<0.01) e MG (p<0.001) e a idade não esteve associada à ACR. Os pré-obesos são na sua maioria insuficientemente activos, e os normoponderais são insuficientemente activos (p=0.033). Não houve associação entre o ESE e AF dos pais e o IMC, ACR ou QAD dos alunos. Com base nos resultados encontrados na revisão, procurou-se situar diferentes abordagens teóricas sobre a actividade física, dando ênfase principal à importância “ da promoção (acesso) da actividade física através da educação física orientada pedagogicamente em todos os ciclos de ensino. Conclusão: As crianças que tiveram maior ACR registaram menor IMC e MG, independente da idade e do sexo. Verificou-se ainda que as variáveis de ESE e AF dos pais, não está associada aos resultados da ACR, IMC e MG das crianças. ABSTRACT: Objective: Given the paucity of studies in Portugal on this theme, the goal of the study was to analyse the of cardiorespiratory fitness (CRF), and the prevalence of overweight and obesity in children attending the fourth year of primary school. Method: A systematic literature review was conducted, in which cross-cutting studies and RCT were covered and, intersected with observational results obtained, from the group of Schools Professor Armando Lucena, located in, the municipality of Mafra, Lisbon district. From the systematic review of literature (SRL), plus the observational study, the verification analysis of the inverse association between 'cardiorespiratory fitness, pre-obesity and obesity' was performed.The observational study was cross-sectional, focusing on 143 children (73 girls) of 9-12 years old. To define overweight and obesity the IOTF cutoffs were used. BMI and percentage of fat mass were recorded by means of bioelectrical impedance. The assessment was made through the CRF test shuttle Fitnessgram 20 meters, using the equation proposed by Fernhall et al., (1998). Students were assessed by questionnaire on physical activity (PA), extra-curricular PA (PAF Telama et al., 1997); parents were questioned regarding their PA levels (IPAQ, Bauman et al., 2009) and socio-economic status (SES). Results: The results of the observational study, corroborate, other SRL studies. There were no gender differences in the prevalence of overweight and obesity: men (20. 55% and 8.21%) and girls (34.28% and 5.71%) (p <0.176). Children with higher BMI have a lower CRF (p <0.01) and MG (p <0.001). Age was not observed to be associated with CRF. The pre-obese are mostly insufficiently active, and the normalweight are insufficiently active (p = 0.033). There was no association between the PA, the ESS, the parents, and the BMI, the CRF or the PAF of the students. Based on the results found in the review, different theoretical approaches regarding physical activity were. Emphasis was given to the importance of promoting the access to physical activity through pedagogically oriented physical education in all cycles of education. Conclusion: Children who had higher ACR showed lower FAT and BMI, regardless of age and sex. Furthermore, it was found that parents’ SES and PA variables are, not associated to children’s CRF, BMI and FAT.

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Nesse trabalho investigamos de que maneira a escola vem desenvolvendo as questões referentes à educação ambiental enquanto tema transversal e interdisciplinar. Levantamos informações sobre como a Educação Ambiental vem sendo desenvolvida na prática pedagógica de uma escola da rede pública estadual da cidade de Mossoró/RN - Brasil. Onde foi identificada a percepção dos atores envolvidos no processo de educação ambiental, a saber: o nível de consciência ecológica, manifestada pelos alunos, suas práticas em relação aos problemas ambientais vivenciados; a abordagem do docente, frente à temática; bem como a percepção dos representantes do poder, como o professor, a diretoria da escola, a secretária de educação do estado e gerente de meio ambiente do município de Mossoró – RN. Contando com um apanhado bibliográfico com autores como Saviani (2008), Dias (2004), Gadotti (2008), Paulo Freire (1991), Sato (2012), Loureiro (2004), Leff (2010), entre outros. Para essa investigação utilizamos uma abordagem qualitativa e quantitativa, sendo desenvolvido 4 entrevistas com os representantes do poder e um questionário que foi aplicado com os alunos da escola, depois de respondidos esses dados foram tabulados em planilhas do Excel a fim de serem lançados para análises estatísticas, logo em seguida foram tratados através da construção de um banco de dados na planilha eletrônica Microsoft Excel. Após a digitação da base de dados, o banco foi exportado para o software SPSS versão 13.0 no qual foi realizada a análise. Para análise dos dados foram calculadas as frequências observadas e percentuais das percepções dos alunos acerca do julgamento, procedimentos utilizados pela escola, itens associados, problemas e temas relacionados ao meio ambiente. Além das frequências calculadas foram construídos os gráficos para cada distribuição. Já a análise qualitativa de conteúdo possui como estratégia de análise a interpretação qualitativa de emparelhamento de dados. Percebemos que nossos sujeitos acreditam que a educação ambiental vem como instrumento para modificação de comportamentos humanos, é através da educação que modificamos atitudes e conscientizamos a nossa população aos cuidados para com o nosso planeta. Nesta investigação identificamos que 83,1% dos alunos disseram estar bastante consciente da problemática ambiental, e ainda, 71,8% dos discentes disseram que estão bastante motivados para desenvolver projetos de educação ambiental na sua escola. Todavia não foi constatado isso pelos representantes do poder os quais afirma que esses não possuem o nível de consciência ecológica identificada pelos alunos, podendo perceber uma visão crítica por parte dos representantes do poder a respeito da temática, diferente dos discentes que dizem ter consciência, contudo suas práticas não condizem com a realidade. Acreditamos que se a Educação Ambiental fosse introduzida como componente curricular obrigatória essa poderia ser trabalhada de maneira mais direta e contundente a fim de formamos cidadãos verdadeiramente consciente da questão ambiental, uma vez que essa deve ir além dos muros da escola, a questão ambiental é uma questão também social, necessitamos de intervenções a nível global afim de todos contribuírem de maneira significativa para sustentabilidade.

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‘Escola, Família e Educação da Sexualidade’ fundamenta historicamente o processo de desenvolvimento da sexualidade na sociedade humana em Freud, Foucault e outros, como suporte teórico para abordar a necessidade de buscar a formação da criança na parceria escola e família, amparados pela lei nº 9.394/96, das Diretrizes e Bases da Educação Brasileira e Parâmetros Curriculares Nacionais em seus Temas Transversais. Visa compreender a complexidade da temática em uma unidade escolar por meio da pesquisa ação, na identificação, descrição e análise da prática educativa reflexiva. Utiliza a abordagem qualitativa e visão dialética, o que pressupõe o processo histórico da sociedade e dos sujeitos. Indaga os professores do Ensino Fundamental I do município de Cotia - SP sobre a relação escola e família, constituída em parceria, de forma a favorecer a orientação educativa da sexualidade. Destacam no contexto do Projeto Político Pedagógico escolar, os desafios e perspectivas dessa relação, a concepção dos docentes sobre essa questão e o desenvolvimento integral do aluno. Conclui que escola e família revelam dificuldades em abordar o tema com as crianças e reconhecem a necessidade da parceria entre elas. As análises contribuem para o Projeto Político Pedagógico da escola, possibilitam a caracterização da relação escola e família e indicam a necessidade de revisão de posturas e valores, reforçados na proposta de orientação educativa da sexualidade, produto deste estudo de caso e desenvolvida pela pesquisadora em horário de trabalho pedagógico coletivo, durante a pesquisa ação. Este estudo motivou a construção do conhecimento indicando novas pesquisas e aprofundamento.

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Two stark reminders of the difficulties that people on the move encounter in the Mediterranean have been grabbing headlines recently: the so-called ‘left-to-die’ boat report and the ground-breaking Hirsi judgment. These two instances present the worst of both worlds: the first concerns a migrant boat that was ignored altogether, resulting in many deaths, whereas the second concerns a migrant boat being intercepted but subsequently dealt with in a way that contradicts Europe’s human rights standards. These two cases are neither isolated nor incidental. Instead they are of wider concern to the EU and reminders of structural deficiencies in Europe’s approach to people on the move in the Mediterranean. This paper identifies those cross-cutting deficiencies and proposes recommendations to correct them.

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The boreal forest of western Canada is being dissected by seismic lines used for oil and gas exploration. The vast amount of edge being created is leading to concerns that core habitat will be reduced for forest interior species for extended periods of time. The Ovenbird (Seiurus aurocapilla) is a boreal songbird known to be sensitive to newly created seismic lines because it does not include newly cut lines within its territory. We examined multiple hypotheses to explain potential mechanisms causing this behavior by mapping Ovenbird territories near lines with varying states of vegetation regeneration. The best model to explain line exclusion behavior included the number of neighboring conspecifics, the amount of bare ground, leaf-litter depth, and canopy closure. Ovenbirds exclude recently cut seismic lines from their territories because of lack of protective cover (lower tree and shrub cover) and because of reduced food resources due to large areas of bare ground. Food reduction and perceived predation risk effects seem to be mitigated once leaf litter (depth and extent of cover) and woody vegetation cover are restored to forest interior levels. However, as conspecific density increases, lines are more likely to be used as landmarks to demarcate territorial boundaries, even when woody vegetation cover and leaf litter are restored. This behavior can reduce territory density near seismic lines by changing the spatial distribution of territories. Landmark effects are longer lasting than the effects from reduced food or perceived predation risk because canopy height and tree density take >40 years to recover to forest interior levels. Mitigation of seismic line impacts on Ovenbirds should focus on restoring forest cover as quickly as possible after line cutting.

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This edited collection brings together international experts from the vibrant and growing field of geographies of children, youth and families. The book provides an overview of current conceptual and theoretical debates, and gives a wide range of examples of cutting-edge research from a variety of national contexts across the globe. The theme of 'disentangling the socio-spatial contexts of young people and/or their families' advances debates in geographies and social studies of young people and families by emphasising the context of young people's social agency. The book is designed to provide an introduction to the topic of geographies of children, youth and families and is an invaluable course text for undergraduate and postgraduate students of geography and the social sciences. This interdisciplinary text is also of likely interest to students and practitioners of education, youth work, social policy and social work.

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Young people's bodies have been at the centre of much policy and media discourse of late, forming the focal point of moral panics about obesity, substance abuse, and anti-social behaviour, to name just a few. Political responses to these issues are often focused on finding 'pragmatic' solutions based on a normative understanding of child development. This book, instead, demonstrates the contested and differentiated nature of childhood and youth embodiment. It combines the critical analysis of imagined and disciplined youthful bodies with a focus on young people's lived and performed, embodied subjectivities. Contested Bodies of Childhood and Youth points towards ways of addressing the issues that affect young people's wellbeing without criminalising and stigmatising them. It presents cutting edge interdisciplinary research in an accessible style that seeks to bridge the divide between theory and practice in research.

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The purpose of Research Theme 4 (RT4) was to advance understanding of the basic science issues at the heart of the ENSEMBLES project, focusing on the key processes that govern climate variability and change, and that determine the predictability of climate. Particular attention was given to understanding linear and non-linear feedbacks that may lead to climate surprises,and to understanding the factors that govern the probability of extreme events. Improved understanding of these issues will contribute significantly to the quantification and reduction of uncertainty in seasonal to decadal predictions and projections of climate change. RT4 exploited the ENSEMBLES integrations (stream 1) performed in RT2A as well as undertaking its own experimentation to explore key processes within the climate system. It was working at the cutting edge of problems related to climate feedbacks, the interaction between climate variability and climate change � especially how climate change pertains to extreme events, and the predictability of the climate system on a range of time-scales. The statisticalmethodologies developed for extreme event analysis are new and state-of-the-art. The RT4-coordinated experiments, which have been conducted with six different atmospheric GCMs forced by common timeinvariant sea surface temperature (SST) and sea-ice fields (removing some sources of inter-model variability), are designed to help to understand model uncertainty (rather than scenario or initial condition uncertainty) in predictions of the response to greenhouse-gas-induced warming. RT4 links strongly with RT5 on the evaluation of the ENSEMBLES prediction system and feeds back its results to RT1 to guide improvements in the Earth system models and, through its research on predictability, to steer the development of methods for initialising the ensembles

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A set of lysimeter based experiments was carried out during 2000/01 to evaluate the impact of soil type and grassland management on potassium (K) leaching. The effects of (1) four soil textures (sand, loam, loam over chalk and clay), (2) grazing and cutting (with farmyard manure application), and (3) K applied as inorganic fertilizer, dairy slurry or a mixture of both sources were tested. Total K losses in the clay soil were more than twice those in the sand soil (13 and 6 kg K ha(-1), respectively) because of the development of preferential flow in the clay soil. They were also greater in the cut treatment than in the grazed treatment (82 and 51 kg K ha(-1), respectively; P less than or equal to0.01), associated with a 63% increase of K concentration in the leachates from the former (6.7 +/- 0.28 and 4.1 +/- 0.22 mg K L-1 for cut and grazed, respectively; P less than or equal to0.01) because of the K input from the farmyard manure. The source of fertilizer did not affect total K losses or the average K concentration in the leachates (P >0.05), but it changed the pattern of these over time.

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We have integrated information on topography, geology and geomorphology with the results of targeted fieldwork in order to develop a chronology for the development of Lake Megafazzan, a giant lake that has periodically existed in the Fazzan Basin since the late Miocene. The development of the basin can be best understood by considering the main geological and geomorphological events that occurred thought Libya during this period and thus an overview of the palaeohydrology of all Libya is also presented. The origin of the Fazzan Basin appears to lie in the Late Miocene. At this time Libya was dominated by two large rivers systems that flowed into the Mediterranean Sea, the Sahabi River draining central and eastern Libya and the Wadi Nashu River draining much of western Libya. As the Miocene progressed the region become increasingly affected by volcanic activity on its northern and eastern margin that appears to have blocked the River Nashu in Late Miocene or early Messinian times forming a sizeable closed basin in the Fazzan within which proto-Lake Megafazzan would have developed during humid periods. The fall in base level associated with the Messinian desiccation of the Mediterranean Sea promoted down-cutting and extension of river systems throughout much of Libya. To the south of the proto Fazzan Basin the Sahabi River tributary know as Wadi Barjuj appears to have expanded its headwaters westwards. The channel now terminates at Al Haruj al Aswad. We interpret this as a suggestion that Wadi Barjuj was blocked by the progressive development of Al Haruj al Aswad. K/Ar dating of lava flows suggests that this occurred between 4 and 2 Ma. This event would have increased the size of the closed basin in the Fazzan by about half, producing a catchment close to its current size (-350,000 km(2)). The Fazzan Basin contains a wealth of Pleistocene to recent palaeolake sediment outcrops and shorelines. Dating of these features demonstrates evidence of lacustrine conditions during numerous interglacials spanning a period greater than 420 ka. The middle to late Pleistocene interglacials were humid enough to produce a giant lake of about 135,000 km(2) that we have called Lake Megafazzan. Later lake phases were smaller, the interglacials less humid, developing lakes of a few thousand square kilometres. In parallel with these palaeohydrological developments in the Fazzan Basin, change was occurring in other parts of Libya. The Lower Pliocene sea level rise caused sediments to infill much of the Messinian channel system. As this was occurring, subsidence in the Al Kufrah Basin caused expansion of the Al Kufrah River system at the expense of the River Sahabi. By the Pleistocene, the Al Kufrah River dominated the palaeohydrology of eastern Libya and had developed a very large inland delta in its northern reaches that exhibited a complex distributary channel network which at times fed substantial lakes in the Sirt Basin. At this time Libya was a veritable lake district during humid periods with about 10% of the country underwater. (C) 2008 Elsevier B.V. All rights reserved.

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Rapidly-flowing sectors of an ice sheet (ice streams) can play ail important role in abrupt climate change through tile delivery of icebergs and meltwater and tile Subsequent disruption of ocean thermohaline circulation (e.g., the North Atlantic's Heinrich events). Recently, several cores have been raised from the Arctic Ocean which document the existence of massive ice export events during tile Late Pleistocene and whose provenance has been linked to Source regions in the Canadian Arctic Archipelago. In this paper, satellite imagery is used to map glacial geomorphology in the vicinity of Victoria Island, Banks Island and Prince of Wales Island (Canadian Arctic) in order to reconstruct ice flow patterns in the highly complex glacial landscape. A total of 88 discrete flow-sets are mapped and of these, 13 exhibit the characteristic geomorphology of palaeo-ice streams (i.e., parallel patterns of large, highly elongated mega-scale glacial lineations forming a convergent flow pattern with abrupt lateral margins). Previous studies by other workers and cross-cutting relationships indicate that the majority of these ice streams are relatively young and operated during or immediately prior to deglaciation. Our new mapping, however, documents a large (> 700 km long; 110 km wide) and relatively old ice stream imprint centred in M'Clintock Channel and converging into Viscount Melville Sound. A trough mouth fan located on the continental shelf Suggests that it extended along M'Clure Strait and was grounded at tile shelf edge. The location of the M'Clure Strait Ice Stream exactly matches the Source area of 4 (possibly 5) major ice export events recorded in core PS 1230 raised from Fram Strait, the major ice exit for the Arctic Ocean. These ice export events occur at similar to 12.9, similar to 15.6, similar to 22 and 29.8 ka (C-14 yr BP) and we argue that they record vigorous episodes of activity of the M'Clure Strait Ice Stream. The timing of these events is remarkably similar to the North Atlantic's Heinrich events and we take this as evidence that the M'Clure Strait Ice Stream was also activated around the same time. This may hold important implications for tile cause of the North Atlantic's Heinrich events and hints at tile possibility of a pall-ice sheet response. (c) 2005 Elsevier B.V. All rights reserved.

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Ascertaining the location of palaeo-ice streams is crucial in order to produce accurate reconstructions of palaeo-ice sheets and examine interactions with the ocean-climate system. This paper reports evidence for a major ice stream in Amundsen Gulf, Canadian Arctic Archipelago. Mapping from satellite imagery (Landsat ETM+) and digital elevation models, including bathymetric data, is used to reconstruct flow-patterns on southwestern Victoria Island and the adjacent mainland (Nunavut and Northwest Territories). Several flow-sets indicative of ice streaming are found feeding into the marine trough and cross-cutting relationships between these flow-sets (and utilising previously published radiocarbon dates) reveal several phases of ice stream activity centred in Amundsen Gulf and Dolphin and Union Strait. A large erosional footprint on the continental shelf indicates that the ice stream (ca. 1000 km long and ca. 150 km wide) filled Amundsen Gulf, probably at the Last Glacial Maximum. Subsequent to this, the ice stream reorganised as the margin retreated back along the marine trough, eventually splitting into two separate low-gradient lobes in Prince Albert Sound and Dolphin and Union Strait. The location of this major ice stream holds important implications for ice sheet-ocean interactions and specifically, the development of Arctic Ocean ice shelves and the delivery of icebergs into the western Arctic Ocean during the late Pleistocene. Copyright (C) 2006 John Wiley & Sons, Ltd.

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Edited volume, containing a huge variety of cutting-edge contributions on the Roman verse inscriptions of the Republican period.