970 resultados para formation processes
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This volume focuses on word formation processes in smaller and so far underrepresented indigenous languages of South America. The data for the analyses have been mainly collected in the field by the authors. The several language families described here, among them Arawakan, Takanan, and Guaycuruan, as well as language isolates, such as Yurakaré and Cholón, reflect the linguistic diversity of South America. Equally diverse are the topics addressed, relating to word formation processes like reduplication, nominal and verbal compounding, clitic compounding, and incorporation. The traditional notions of the processes are discussed critically with respect to their implementation in minor indigenous languages. The book is therefore not only of interest to readers with an Amerindian background but also to typologists and historical linguists, and it is a supplement to more theory-driven approaches to language and linguistics.
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Recent findings of elevated PCDDs from an unknown source in the coastal marine environment of Queensland, Australia has instigated further investigations into the distribution of, and environments associated with the PCDD contamination. This study presents data for OCDD concentrations in the coastal, mountainous and inland environment of Queensland. Additionally, full 2,3,7,8-substituted polychlorinated dibenzo-p-dioxins and dibenzofuran (PCDD/F) profiles from different land-use types and environments in the coastal region were analysed. Distinct east-west gradients were detected in topsoil collected from various bushland regions with elevated OCDD concentrations confined to the coastal region. However, PCDD/F results from topsoil and river sediments collected in the Queensland coastal region suggest that elevated OCDD concentrations cannot be attributed to any of the environments, land-use or industry types investigated. PCDD/F congener profiles from select samples were remarkably similar to those previously described in marine sediments collected along the entire Queensland coastline. In addition, kaolinite clay samples from Queensland exhibited elevated OCDD concentrations, and PCDD/F profiles in these samples were similar to those detected in kaolinite clays elsewhere. Natural formation processes have been hypothesised as the source of elevated PCDDs in Queensland and other locations, where similar PCDD/F profiles and the general lack of anthropogenic sources are evident. This study presents additional data supporting this hypothesis and provides further information that may assist in the identification of the processes involved in the natural formation of PCDDs. (C) 2002 Elsevier Science Ltd. All rights reserved.
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Este artigo tem como objetivo relatar a experiência de um curso de formação da Política Nacional de Humanização voltado para gestores e trabalhadores da atenção básica de um município no estado do Rio de Janeiro. O curso visou a formação de apoiadores institucionais capazes de fomentar rede no Sistema Único de Saúde (SUS), promover mudanças e consolidação nos modos de atenção e de gestão dos serviços. Como referencial metodológico, buscou-se um modo de "formação-intervenção" que fosse baseado em práticas concretas de intervenção dos trabalhadores nos processos de trabalho em saúde. O curso envolveu quarenta participantes, gestores e trabalhadores de nível médio e superior, ligados à atenção básica, oriundos da Estratégia de Saúde da Família e de Unidades de Saúde. Como resultados destacam-se ações de co-gestão no formato de reuniões com os usuários para o compartilhamento de decisões relativas ao serviço; implementação de acolhimento, com intervenções que garantam o acesso do usuário ao serviço; e de clínica ampliada, com discussões em equipe dos casos clínicos; e ações no campo da saúde do trabalhador, como efeito das discussões dos processos de trabalho nas equipes multiprofissionais.
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A pesquisa tem como sujeito a criança pequena em uma instituição de educação infantil e investiga processos de formação mediados pela experiência sensível com as artes visuais. A educação infantil é lugar das interações, das brincadeiras e da educação estética, sensível. Problematiza o espaço da alfabetização na escola, restrito à apropriação da linguagem verbal, escrita. Por meio de intervenção, propõe um elo entre a criança, sua cultura e seu meio, sugerindo um contato mais próximo com as múltiplas linguagens e com a educação estética. Investiga a educação infantil como o lugar da experiência, da brincadeira e da formação do ser humano em sua totalidade, que não se limita à alfabetização pautada na linguagem verbal e na fragmentação do saber. Este trabalho foi realizado em uma Creche-Escola do município de Vitória/ES, situada no bairro Jardim da Penha. Tem como público crianças de seis meses a cinco anos, divididas em grupos conforme a faixa etária. A participação ativa da pesquisadora na rotina da instituição pesquisada direcionou a um diálogo com a pesquisa-ação, um tipo de pesquisa de natureza qualitativa que se revela na ação e no discurso, segundo Barbier (2007). Busca analisar os possíveis efeitos dessa experiência estética no cotidiano das crianças, observando como afetam e geram interlocuções com a comunidade escolar e com a família. Fundamenta-se nos conceitos de experiência, sentidos como uma experiência estética e a linguagem visual como uma forma de comunicação nas discussões de Vigotski (2010), Duarte Júnior (2001) e Bakhtin (2010). Procura reconhecer a criança como sujeito ativo, em consonância com as contribuições da Sociologia da Infância, expressa no pensamento de Sarmento (2008). Focaliza a criança como ser social, lúdico, pleno de direitos, apto a viver e ressignificar experiências individuais e sociais. O estudo dialoga com o pensamento de Benjamin (1987) que, em seus escritos filosóficos, revela o conceito de uma infância universal, e de Giorgio Agamben (2005) sobre infância e experiência. Com Angel Pino (2005) analisa a constituição do ser humano como um ser cultural. Apoia-se também em autores que realizam uma reflexão sobre a criança e a infância, como Ribes (2012). Apresenta a Arte como área de conhecimento capaz de formar e inserir a criança em seu meio cultural, proporcionando um conhecimento mais amplo do mundo e da sociedade em que está inserida. Acompanhou quatro momentos que promoveram a aproximação das crianças às expressões artísticas, por meio de visitas a espaços expositivos com a presença da artista plástica, ceramista, a professora Drª. Regina Rodrigues, no espaço educacional. Analisa os processos de interação e a expressão das crianças em face à experiência com a Arte. A chegada ao museu e a interação lúdica das crianças com os espaços, com as obras, com os diversos ambientes e com os mediadores despontou como material potente de conhecimento. A pesquisa mostrou a importância de a instituição de ensino estar aberta à cidade, provocando nas crianças a percepção do pertencimento aos espaços de cultura, lazer e demais lugares que a compõem.
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Mestrado (PES II), Educação Pré-Escolar e Ensino do 1.º Ciclo do Ensino Básico, 24 de Junho de 2015, Universidade dos Açores.
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Mestrado, Ensino de História e Geografia no 3.º ciclo do Ensino Básico e no Ensino Secundário, 9 de Março de 2016, Universidade dos Açores (Relatório de Estágio).
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Cabatuquila conglomerate ferricrete (Malanje Province, located North Central Angola) corresponds to a thick (1O-15m) and hardcornice at the top of "Baixa de Cassanje" escarpment. "Baixa de Cassanje" is a large graben part of South Congo basin. Cabatuquila conglomerate ferricrete seems to correspond to a Plio-Pleistocene morphology which has already disappeared. Laterization dynamics and ferricrete formation processes took place on the Tertiary surface, before being tilted to the Congo Basin. Materials submitted to these processes are mainly alluvial deposits from a pre-Cuanza drainage system. This drainage system flowed to the North before being captured to the Atlantic, as a consequence of the movement which deformed the Tertiary surface during the Pleistocene. The erosion dynamics, which created the Cassanje depression, has occurred after the late Tertiary surface deformation. That dynamics might be related to the Cuango drainage system, which was reorganized after that deformation.
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Knowledge of the soil physical properties, including the clay content, is of utmost importance for agriculture. The behavior of apparently similar soils can differ in intrinsic characteristics determined by different formation processes and nature of the parent material. The purpose of this study was to assess the efficacy of separate or combined pre-treatments, dispersion methods and chemical dispersant agents to determine clay in some soil classes, selected according to their mineralogy. Two Brazilian Oxisols, two Alfisols and one Mollisol with contrasting mineralogy were selected. Different treatments were applied: chemical substances as dispersants (lithium hydroxide, sodium hydroxide, and hexametaphosphate); pre-treatment with dithionite, ammonium oxalate, and hydrogen peroxide to eliminate organic matter; and coarse sand as abrasive and ultrasound, to test their mechanical action. The conclusion was drawn that different treatments must be applied to determine clay, in view of the soil mineralogy. Lithium hydroxide was not efficient to disperse low-CEC electropositive soils and very efficient in dispersing high-CEC electronegative soils. The use of coarse sand as an abrasive increased the clay content of all soils and in all treatments in which dispersion occurred, with or without the use of chemical dispersants. The efficiency of coarse sand is not the same for all soil classes.
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Crystallisation of hydrous mafic magmas at high pressure is a subject of numerous petrologic and experimental studies since the last century and is mainly related to the process of continental crust formation and the possible link between mantle derived melts and low pressure granitoids. Albeit the sequence of crystallization is well constrained by experimental studies, the origin of exposed lower crustal rocks exposed on the earth surface is controversial. Ones line of argument is favouring high pressure crystallization of dry or wet mafic magmas, whereas others invoke partial melting of pre-existing crust. Therefore studies involving field, textural and chemical observations of exposed lower crust such as in Kohistan (Pakistan) or Talkeetna (Alaska) are crucial to understand the continental crust formation processes via arc magmatism. Epidote-bearing gabbros are very sparse and always associated with the deep part of continental crust (>30 km) as in the Kohistan Arc Complex (Pakistan) or in the Chelan Complex (western U.S.). Magmatic epidote is restricted to a small temperature interval above the water-saturated solidus of MORB and represent the last crystallizing liquids in lower crustal regions. However, epidote and melt stability at lower crustal pressures are not clearly established.¦The Chelan complex (western U.S.) at the base of the Cascadian Arc is composed mainly by peraluminous tonalité associated with gabbroic and ultramafic rocks and was traditionally interpreted as a migmatitic terrain. However field, chemical and mineralogical observations rather suggest a magmatic origin and point to a protracted crystallization at intermediate to high pressure ~ 1.0 GPa dominated by amphibole fractionation and followed by isobaric cooling down to 650°C. Crystal fractionation modelling using whole rock composition and field constraints is able to generate peraluminous tonalité. The modelled crystallisation sequence and the volume proportions are in agreement with experimental studies performed at these pressures. The Chelan complex was thus not formed during a partial melting event, but represent the sequence of crystallisation occurring at the base of the crust. Massive fractionation of hornblende is able to generate peraluminous tonalité without significant assimilation of crustal rock.¦Similarly to the Chelan complex, the base of the Kohistan arc is composed of cumulates derived by high pressure crystallization of hydrous magma. In garnet gabbros, epidote occurs as magmatic phase, crystallising from hydrous interstitial melt trapped between grain boundaries at lower crustal pressures (Ρ ~ 1.2 GPa) for temperature of (650-700 °C). Trace and REE signature in epidote indicate that epidote was formed through peritectic reaction involving garnet, clinopyroxene and plagioclase. At the beginning of the crystallisation epidote signature is dominated by REE content in the melt, whereas at the end the signature is dominated by reacting phases. Melt in equilibrium with epidote inferred from the partition coefficients available is similar to intrusive tonalité up the section indicating that hydrous melt was extracted from the garnet gabbros. In some gabbros epidote shows single homogeneous compositions, while in others coexisting epidote have different compositions indicating the presence of solvi along the Al-Fe3+ join. The overgowths are only observed in presence of paragonite in the assemblage, suggesting high water content. At high water content, the hydrous solidus is shift to lower temperature and probably intersects the solvi observed along the Al-Fe3+ join. Therefore, several compositions of epidote is stable at high water content.¦-¦La composition chimique de la croûte continentale est considérée comme similaire à celle du magmatisme calco-alcalin de marge continentale active (enrichissement en éléments mobiles dans les fluides, anomalies négatives en Nb, Ta et éléments à haut potentiel électronique, etc...). Cependant la nature andésitique de la croûte continentale (Si02 > 60 wt%), résultant des nombreuses intrusions de granitoïdes dans la croûte supérieure, est sujette à polémique et le lien entre les magmas dérivés du manteau et les roches évoluées de faible profondeur n'est pas clairement établi (fusion partielle de croûte basaltique, cristallisation fractionnée à haute pression, etc...).¦Les affleurements de croûte profonde sont rares mais précieux, car ils permettent d'observer les phénomènes se passant à grande profondeur. Le complexe de Chelan (Washington Cascades) en est un exemple. Formé à environ 30 km de profondeur, il est composé de roches gabbroïques et ultramafiques, ainsi que de tonalités, qui furent souvent interprétés comme le produit de la fusion partielle de la croûte. Cependant, les relations de terrain, la chimie des éléments majeurs et des éléments traces sont cohérentes avec l'évolution d'un complexe magmatique mafique dans la croûte profonde ou moyenne ( 1.0 GPa), dominée par le fractionnement de l'amphibole. Après son emplacement, le complexe a subi un refroidissement isobare jusqu'à des températures de l'ordre de 650 °C, déduit de la composition chimique des minéraux. Un bilan de masse contraint pax les observations de terrain permet de calculer la séquence et les volumes de fractionnement. Les faciès évolués légèrement hyperalumineux observés sur le terrain peuvent être générés par la cristallisation de 3 % de websterite à olivine, 12 % d'hornblendite à pyroxène 33 % d'hornblendite, 19 % de gabbros, 15 % de diorite et 2 % de tonalité. Nous montrons ainsi qu'une série de fractionnement contrôlée par l'amphibole permet de générer des tonalités sans assimilation de matériel crustal et l'exemple de Chelan illustre la viabilité de ce processus dans la formation de croûte continentale.¦Les réactions proches du solidus saturé en H20 dans les systèmes basaltiques à des pressions élevées restent énigmatiques. Diverses expériences tendent à montrer que l'épidote est stable dans ces conditions, mais rarement observée (décrite ?) comme phase primaire dans les systèmes naturels. Les épidotes trouvées dans les gabbros de Jijal (nord-Pakistan) montrent des textures de type .magmatique telles qu'observées dans les roches évoluées. Le contenu en terres rares de ces épidotes est très variable allant de signatures enrichies en terres rares légères impliquant la présence de liquide interstitiel à des signatures complètement déprimées en ces mêmes éléments, évoquant une cristallisation en coexistence avec du grenat. Ces diverses signatures reflètent un chemin de cristallisation en présence de liquide interstitiel et enregistrent des réactions péritectiques impliquant grenat, clinopyroxene et plagioclase à des pressions de ~ 1.2 GPa pour des températures de 650-700 °C. Cependant dans quelques échantillons deux ou trois compositions d'épidotes coexistent démontrant la présence de lacunes d'immiscibilité le long de la solution solide épidote-clinozoïsite. La forte teneur en H20 du liquide magmatique est certainement à l'origine de la coexistence de deux compositions distinctes.
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This work starts with a historical perspective of the social and scientific progress related to the understanding of the atmospheric aerosol. Its origin, physical, chemical and optical characteristics, as well as its environmental behaviour are described, retracing the evolution of the concepts related to this subject over the last centuries. The main sources that contribute to atmospheric particulate matter and the modern understanding of its formation processes and constitution, focusing on the chemical pathways leading to it and on its organic components are presented. This discussion is complemented with recent evaluations of the quantities emitted by primary, secondary, biogenic and anthropogenic sources and the effects due to accumulation or dispersion of aerosols, justifying the chemical and environmental interest they engender.
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Diplomityön tavoitteena on parantaa Mikkelin seudun teknologiayritysten kilpailukykyä verkostoitumisen avulla. Lisäksi tavoitteena on toteuttaa konkreettinen verkostoitumisprosessi ja luoda malli verkostoitumishankkeen toteuttamiseksi. Työ koostuu verkostoitumiseen liittyvästä kirjallisuuskatsauksesta ja työn ohessa toteutetuista käytännön toimenpiteistä. Kohderyhmäksi valittuihin puutuoteteollisuuden kone- ja laitevalmistajiin on perehdytty haastattelujen ja arvojärjestelmäanalyysin perusteella. Yrityksiltä on lisäksi haastattelujen yhteydessä kerätty verkostoitumisaloitteita, joiden perusteella on tehty tarvittavia jatkotoimenpiteitä. Työn tuloksena on luotu kuvaus kohdeyritysten arvojärjestelmästä Mikkelin seudulla ja edesautettu kolmen verkostoitumisprosessien käynnistymistä. Lisäksi kokemusten ja havaintojen perusteella on luotu verkostoitumismalli alueellisen kehittäjäorganisaation käyttöön.
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Tässä Pro gradu –tutkielmassa tavoiteltiin kokonaiskuvaa teemapuistoalan asiakastyytyväisyyden muodostumisesta kognitiivisesta, affektiivisesta ja kognitiivis-affektiivisesta näkökulmasta. Lisäksi tarkasteltiin kunkin näkökulman teoriapohjaa; miten asiakas muodostaa arvionsa tyytyväisyydestään sekä tyytyväisyyteen vaikuttavia tekijöitä kussakin näkökulmassa. Tutkimus toteutettiin kvalitatiivisena tutkimuksena, ryhmähaastatteluna. Tutkimustulosten perusteella todettiin asiakastyytyväisyyden muodostuvan kognitioiden ja affektien yhteisvaikutuksesta, tulosten tukien kognitiivis-affektiivista näkökulmaa. Lisäksi tuloksissa saatiin viitteitä sosiaalisesta näkökulmasta asiakastyytyväisyyden muodostumisessa, affektiivisesta diskonfirmaatiosta sekä asiakastyytyväisyyden dynaamisesta luonteesta. Myös asiakastyytyväisyyden ja –tyytymättömyyden prosessien havaittiin eroavan ainakin jossain määrin. Uudet, viitekehyksen ulkopuoliset havainnot tukivat uusimman kirjallisuuden käsitystä asiakastyytyväisyydestä monitasoisena ja –ulotteisena käsitteenä.
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Internationally, Finland has been among the most respected countries during several decades in terms of public health. WHO has had the most significant influence on Finnish health policy and the relationship has traditionally been warm. However, the situation has slightly changed in the last 10-20 years. The objectives of Finnish national health policy have been to secure the best possible health for the population and to minimize disparities in health between different population groups. Nevertheless, although the state of public health and welfare has steadily improved, the socioeconomic disparities in health have increased. This qualitative case study will demonstrate why health is political and why health matters. It will also present some recommendations for research topics and administrative reforms. It will be argued that lack of political interest in health policy leads to absence of health policy visions and political commitment, which can be disastrous for public health. This study will investigate how Finnish health policy is defined and organised, and it will also shed light on Finnish health policy formation processes and actors. Health policy is understood as a broader societal construct covering the domains of different ministries, not just Ministry of Social Affairs and Health (MSAH). The influences of economic recession of the 1990s, state subsidy reform in 1993, globalisation and the European Union will be addressed, as well. There is not much earlier Finnish research done on health policy from political science viewpoint. Therefore, this study is interdisciplinary and combines political science with administrative science, contemporary history and health policy research with a hint of epidemiology. As a method, literature review, semi-structured interviews and policy analysi will be utilised. Institutionalism, policy transfer, and corporatism are understood as the theoretical framework. According to the study, there are two health policies in Finland: the official health policy and health policy generated by industry, media and various interest organisations. The complex relationships between the Government and municipalities, and on the other hand, the MSAH and National Institute for Health and Welfare (THL) seemed significant in terms of Finnish health policy coordination. The study also showed that the Investigated case, Health 2015, does not fulfil all necessary criteria for a successful public health programme. There were also several features both in Health 2015 and Finnish health policy, which can be interpreted in NPM framework and seen having NPM influences.
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Kirjallisuusarvostelu
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El presente trabajo de investigación busca responder cuestiones relativas a los procesos de formación de identidades bajo la lógica de un modelo transnacional de las migraciones. De manera más específica, es un intento por analizar el desarrollo de los sucesos que provocaron en enero de este año el revocamiento del mandato de Zine El Abidine Ben Alí, quien se mantuvo en el poder desde 1987, a la luz de conceptos como la identidad nacional, la migración transnacional y la formación de identidades. ¿Cuál es el proyecto nacional que se está planteando la sociedad tunecina actual y sobre cuáles han sido los factores sociales, políticos, económicos y culturales que han determinado las actuaciones de los tunecinos luego de su independencia de Francia. ¿Han sido estas protestas el reflejo de un cambio en la manera en la cual los tunecinos se identifican unos con otros?, o, en otras palabras, ¿el proyecto político emprendido por la sociedad tunecina actual responde a un cambio en la construcción de identidad de la nación, y cuáles han sido los factores que han determinado ese proceso?