435 resultados para lar


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Dissertação apresentada para a obtenção do grau de mestre na área de Educação Social e Intervenção Comunitária

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A violência doméstica tornou-se um fenómeno social de grande complexidade, que não pode ser tratado de forma superficial, seja por parte daqueles que intervêm tecnicamente, seja por parte das vítimas e agressores, pois trata-se da vida real de muitos indivíduos ou sujeitos. Deste modo, tornou-se necessário analisar a violência doméstica, procurando perceber o papel dos agentes, em especial dos técnicos, que acompanham as vítimas de violência doméstica na construção do seu projecto de vida. Para a realização deste estudo, fiz uma abordagem dos diferentes conceitos de violência doméstica, fundamental neste trabalho, em virtude da complexidade e controvérsia que a sua definição implica para diferentes autores e abordagens teóricas. Naturalmente que, se o tema da violência doméstica atravessa todo o trabalho, era indispensável ouvir as vítimas desta problemática quanto ao seu sofrimento, coragem e resiliência, ou abandono do lar e acompanhamento recebido. Assim sendo, e porque pretendi fazer uma análise à forma como é realizado o acompanhamento e intervenção por parte dos técnicos, este trabalho apresenta ainda uma investigação empírica realizada através da aplicação de inquéritos por questionário vítimas e não vítimas de violência doméstica, bem como a caracterização dos dados sociodemográficos do distrito de Portalegre. O tratamento e análise dos dados permitiram confirmar, em larga medida, a fundamentação teórica apresentada na primeira parte do estudo onde se verificou haver a divergência no conceito de violência doméstica, as vítimas serem predominantemente do sexo feminino e os agressores do sexo masculino, os vários motivos que levam as vítimas a permanecer na relação e a importância do papel dos técnicos de acompanhamento na definição de projectos de vida alternativos.

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Viver um maior número de anos não significa necessariamente que se viva com qualidade. Devido às alterações demográficas verificadas nos últimos anos e face ao envelhecimento progressivo da população mundial e consequente aumento da esperança média de vida, ao acréscimo das doenças crónicas e à dependência a elas associada, surgem dificuldades que os doentes e os seus cuidadores enfrentam no seu quotidiano de internamento. Assim, surgiu a necessidade de equacionar a problemática da Qualidade de Vida e a Vulnerabilidade ao Stress dos Cuidadores Formais, que diariamente trabalham numa Unidade de Cuidados Continuados Integrados do Alentejo. Este trabalho foi desenvolvido numa Unidade de Cuidados Continuados Integrados com duas valências de internamento, a Média e a Longa Duração, com os Cuidadores Formais que nele aceitaram participar. Entre eles, encontram-se as mais diversas profissões, desde Auxiliares de Lar, Enfermeiros, Fisioterapeutas, Psicólogos, Animadores Socioculturais, Técnicos de Psicomotricidade, Terapeutas da Fala e Assistentes Sociais. Todos eles representam um papel muito importante no cuidado aos seus clientes, cada um na sua área. Ao delinear este estudo, o Problema prático identificado foi se existia uma relação entre a Qualidade de Vida e a Vulnerabilidade ao Stress dos Cuidadores Formais de uma Unidade de Cuidados Continuados Integrados do Alentejo. Este estudo foi desenvolvido com uma população de 63 elementos, todos Cuidadores Formais a desempenhar funções no local de estudo já referenciado. Foi utilizada a abordagem quantitativa, que é uma metodologia de investigação de vertente epistemológica positivista. Neste estudo, foram utilizados dois instrumentos para aplicar e recolher os dados: um destinado a medir a vulnerabilidade ao stress (23 QVS) dos cuidadores formais; outro para avaliar a qualidade de vida (WHOQOL-Bref), gentilmente cedidos pelos seus autores. Os dados recolhidos, após analisados apontaram no sentido de que à medida que a qualidade de vida aumentava nos diferentes domínios, diminuía a vulnerabilidade ao stress.

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O relatório que aqui se apresenta resulta de um estágio curricular realizado no Lar de Infância e Juventude – Instituto Madre Matilde, situado na Póvoa de Varzim. No âmbito deste estágio desenvolvemos um projeto que passa essencialmente por comprovar a importância das sessões de conversa significativa com jovens institucionalizadas. O projeto foi aplicado tendo como população-alvo jovens institucionalizadas que vivenciaram diversas experiências negativas ao longo da sua infância. O facto de muitas destas adolescentes terem vivido o seu processo de socialização primária em ambientes desestruturados, sem a imposição de regras e por vezes a observar situações de violência física ou verbal, pode efetivamente condicionar o seu futuro. Ao longo deste relatório são levantadas diversas questões, tais como: Quais as consequências que um histórico de violência pode acarretar para o futuro destas jovens? De que forma um grupo onde seja possível conversar livremente e exprimir as suas ideias/opiniões pode ser vantajoso para jovens institucionalizadas, não só como caracter interventivo mas também preventivo? Com esta pesquisa pretendemos partir para uma discussão teórica acerca da importância da conversa significativa e da intervenção social, onde levamos em consideração um conjunto de condições estruturais e conjunturais de vulnerabilidade que as remetem à exclusão social. Conclui-se neste relatório que as instituições respondem frequentemente à garantia das necessidades básicas das jovens que acolhem, mas nem sempre estão preparadas para desenvolver um trabalho de (re) construção das suas vidas por via da palavra, trabalho este que precisa acontecer de forma profunda e contínua onde a conversação contribua efetivamente para o (re) equacionamento do seu projeto de vida e de quem querem ser enquanto pessoas.

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We present a study on the dependence of electric breakdown discharge properties on electrode geometry and the breakdown field in liquid argon near its boiling point. The measurements were performed with a spherical cathode and a planar anode at distances ranging from 0.1 mm to 10.0 mm. A detailed study of the time evolution of the breakdown volt-ampere characteristics was performed for the first time. It revealed a slow streamer development phase in the discharge. The results of a spectroscopic study of the visible light emission of the breakdowns complement the measurements. The light emission from the initial phase of the discharge is attributed to electro-luminescence of liquid argon following a current of drifting electrons. These results contribute to set benchmarks for breakdown-safe design of ionization detectors, such as Liquid Argon Time Projection Chambers (LAr TPC).

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Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000-25,000 14C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia, Poaceae, Asteraceae, and herb tundralike communities with dwarf Betula and Salix dominated during the Sartan (Late Weichselian) Stade, ca. 24,000-10,300 14C yr B.P. The statistical information method used for climate reconstruction shows that the coldest climate was ca. 20,000-17,000 14C yr B.P. A warming (Allerød Interstade?) with mean July temperature ca. 1.5°C warmer than today occurred ca. 12,000 14C yr B.P. The following cooling with temperatures about 3°-4°C cooler than present and precipitation about 100 mm lower corresponds well with the Younger Dryas Stade. Tundra-steppe vegetation changed to Betula nana-Alnus fruticosa shrub tundra ca. 10,000 14C yr B.P. Larch appeared in the area ca. 9400 14C yr B.P. and disappeared after 2900 14C yr B.P. Cooling events ca. 10,500, 9600, and 8200 14C yr B.P. characterized the first half of the Holocene. A significant warming occurred ca. 8500 14C yr B.P., but the Holocene temperature maximum was at about 6000-4500 14C yr B.P. The vegetation cover approximated modern conditions ca. 2800 14C yr B.P. Late Holocene warming events occurred at ca. 3500, 2000, and 1000 14C yr B.P. A cooling (Little Ice Age?) took place between 500 and 200 14C yr ago.

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A pollen profile from the highest known peatbog in the Alps is presented. The peatbog started to grow about 8000 years ago and over the last 5000 years. The influence of man on the vegetation is documented. Before the beginning of the bronze age pasturing started.

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Reliable information of past vegetation changes are important to project future changes, especially for areas undergoing rapid transitioning such as the boreal treeline. The application of detailed sedDNA records has the potential to enhance our understanding of vegetation changes gained mainly from pollen studies of lake sediments. This study investigates sedDNA and pollen records from 31 lakes along a gradient of increasing larch forest cover in northern Siberia (Taymyr Peninsula) and compares them with vegetation field surveys within the lake's catchment. With respect to vegetation richness, sedDNA recorded 114 taxa, about half of them to species level, while pollen analyses identified 43 pollen taxa. Both approaches exceed the 31 taxa revealed by vegetation field surveys of 400 m**2 plots. From north to south, Larix percentages increase, as is consistently recorded by all three methods. Furthermore, tundra sites are separated from forested sites in the plots of the principal component analyses. Comparison of ordination results by Procrustes and Protest analyses yields a significant fit among all compared pairs of records. Despite the overall comparability of sedDNA and pollen analyses certain idiosyncrasies in the compositional signal are observed, such as high percentages of Alnus and Betula in all pollen spectra and high percentages of Salix in all sedDNA spectra. In conclusion, our results from the treeline show that sedDNA analyses perform better than pollen in recording site-specific richness (i.e. presence/absence of certain vegetation taxa in the direct vicinity of the lake) and perform as good as pollen in tracing regional vegetation composition.

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We investigated the sedimentary record of Lake Hancza (northeastern Poland) using a multi-proxy approach, focusing on early to mid-Holocene climatic and environmental changes. AMS 14C dating of terrestrial macrofossils and sedimentation rate estimates from occasional varve thickness measurements were used to establish a chronology. The onset of the Holocene at c. 11600 cal. a BP is marked by the decline of Lateglacial shrub vegetation and a shift from clastic-detrital deposition to an autochthonous sedimentation dominated by biochemical calcite precipitation. Between 10000 and 9000 cal. a BP, a further environmental and climatic improvement is indicated by the spread of deciduous forests, an increase in lake organic matter and a 1.7% rise in the oxygen isotope ratios of both endogenic calcite and ostracod valves. Rising d18O values were probably caused by a combination of hydrological and climatic factors. The persistence of relatively cold and dry climate conditions in northeastern Poland during the first one and a half millennia of the Holocene could be related to a regional eastern European atmospheric circulation pattern. Prevailing anticyclonic circulation linked to a high-pressure cell above the retreating Scandinavian Ice Sheet might have blocked the influence of warm and moist Westerlies and attenuated the early Holocene climatic amelioration in the Lake Hancza region until the final decay of the ice sheet.

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Non-glaciated Arctic lowlands in north-east Siberia were subjected to extensive landscape and environmental changes during the Late Quaternary. Coastal cliffs along the Arctic shelf seas expose terrestrial archives containing numerous palaeoenvironmental indicators (e.g., pollen, plant macro-fossils and mammal fossils) preserved in the permafrost. The presented sedimentological (grain size, magnetic susceptibility and biogeochemical parameters), cryolithological, geochronological (radiocarbon, accelerator mass spectrometry and infrared-stimulated luminescence), heavy mineral and palaeoecological records from Cape Mamontov Klyk record the environmental dynamics of an Arctic shelf lowland east of the Taymyr Peninsula, and thus, near the eastern edge of the Eurasian ice sheet, over the last 60 Ky. This region is also considered to be the westernmost part of Beringia, the non-glaciated landmass that lay between the Eurasian and the Laurentian ice caps during the Late Pleistocene. Several units and subunits of sand deposits, peat-sand alternations, ice-rich palaeocryosol sequences (Ice Complex) and peaty fillings of thermokarst depressions and valleys were presented. The recorded proxy data sets reflect cold stadial climate conditions between 60 and 50 Kya, moderate inderstadial conditions between 50 and 25 Kya and cold stadial conditions from 25 to 15 Kya. The Late Pleistocene to Holocene transition, including the Allerød warm period, the early to middle Holocene thermal optimum and the late Holocene cooling, are also recorded. Three phases of landscape dynamic (fluvial/alluvial, irregular slope run-off and thermokarst) were presented in a schematic model, and were subsequently correlated with the supraregional environmental history between the Early Weichselian and the Holocene.

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Pollen floras were obtained from Miocene sediments recovered at four sites drilled during Ocean Drilling Program Leg 127. The local pollen floras of each site were correlated to the standard pollen zones of northeast Japan by using the concept of the essential members for each pollen zone. At Site 797, the complete floral range was obtained for recognition of the NP2 zone and the pollen components of the NP1 zone were also clarified continuously. The ages of the boundaries between pollen zones NP4/NP3, NP3/NP2, and NP2/NP1 are estimated to be about 7 Ma, 13 Ma, and 17-18.5 Ma, respectively. Even in the same pollen zone, the ratios of major pollen taxa vary with the location. This variation is expressed on maps representing two different times during the Miocene.

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This initial survey of pollen from 192 samples from Hole 794A, supplemented by 189 samples from Hole 795 and 797B, suggests that marine pollen assemblages from the southwestern Sea of Japan provide a consistent Neogene pollen stratigraphy and a solid basis for regional paleoenvironmental reconstructions. Late Miocene vegetation inferred from these pollen data, a mix of conifer and broad-leaf elements with now-extinct Tertiary types well represented, appears similar to Aniai-type floras of Japan. During the late Miocene through early Pliocene, as Tertiary types declined, conifers (including the Sequoia/Cryptomeria group) became more prominent than broad-leaf elements, and herbs played an increasing role in the vegetation. Middle Pliocene pollen assemblages imply significant changes in forest composition. In a 500,000-yr interval centered at ~4 m.y., Tertiary and warm-temperate deciduous types re-expanded and were comparable to or greater than middle-late Miocene levels. Temperate and cold-temperate conifers {Picea, Abies, Tsuga) were minimal. Subsequently, Tertiary and deciduous forest components (including Quercus) decreased, Picea, Tsuga, and Abies were again prominent, and herbs formed an increasingly larger part of the vegetation. Between ~3 m.y. and -2.5 m.y., conifers, except for Cryptomeria types, were prominent, Quercus continued to decline, and other broad-leaf trees were minor. Over the last 2 Ma, the very large and frequent changes in forest composition inferred from pollen in the Sea of Japan correspond to forest dynamics inferred from changes in pollen and floral assemblages throughout Japan. Given present vegetation/climate relationships, broad trends in Neogene climate inferred from these preliminary pollen data include decreasing temperatures, increasing seasonality in temperatures and precipitation, and increasing amplitude and frequency of climatic change. Two significant events, centered at ~9 m.y. and ~4 m.y., punctuate the gradual deterioration of the equable warm, humid subtropical/warm temperate late Miocene and early Pliocene climates. The first indication of cold-temperate conditions comparable to those of Pleistocene glacial intervals occurs ~3 m.y. Subsequently, regional climates oscillated rapidly between temperate and cold-temperate regimes that supported conifer and mixed broad-leaf forests; however, climatic extremes were apparently never great enough to displace warm-temperate and temperate forests from Honshu nor to produce arctic climates on the west coast of Japan.

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Exquisite album of calligraphy (muraqqaʻ / murakkaa) employing ḥadīth of the Prophet executed by the celebrated Ottoman calligrapher Mahmud Celâleddin Efendi (d.1829) in imitation of a model executed by the master calligrapher Hafız Osman Efendi (d.1698).