986 resultados para Rio Pericumã (MA)


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Este trabalho refere-se ao levantamento dos solos do Estado do Rio de Janeiro, que abrange uma área de 43.797,5 km2. Consiste no reconhecimento e caracterização dos solos em sua ambiência, visando contribuir para o planejamento do uso e ocupação das terras de forma racional e sustentável. Foi realizado em nível de reconhecimento de baixa intensidade, com mapa final em escala 1:250.000, de acordo com os procedimentos metodológicos preconizados pela Embrapa. Como material cartográfico básico foram utilizadas fotografias aéreas 1:60.000 (USAF), com apoio adicional de imagens de satélite Landsat (escala 1:100.000 e 1:250.000) e bases planialtimétricas 1:50.000 (IBGE). A distribuição espacial dos solos no estado é representada em cartas topográficas 1:250.000 através de 161 unidades de mapeamento, que compõem uma legenda de identificação de solos, individualizados até o quarto nível categórico, conforme o atual Sistema Brasileiro de Classificação de Solos (SiBCS), seguido de textura, tipo de horizonte A, fases de vegetação, relevo, e, para o caso específico dos Cambissolos desenvolvidos de sedimentos aluvionares recentes, substrato geológico. As principais classes de solos identificadas foram: Argissolos (Amarelos, Vermelhos e Vermelho-Amarelos), Latossolos (Amarelos, Vermelhos e Vermelho- -Amarelos), Cambissolos (Húmicos e Háplicos), Neossolos (Litólicos e Regolíticos), Luvissolos (Crômicos e Hipocrômicos), Chernossolos (Rêndzicos e Argilúvicos) e Nitossolos (Vermelhos e Háplicos), que predominam nas áreas de drenagem livre, enquanto nas partes mais baixas da paisagem ocorrem Gleissolos (Tiomórfi cos, Sálicos, Melânicos e Háplicos), Neossolos (Flúvicos e Quartzarênicos), Espodossolos (Cárbicos e Ferrocárbicos), Planossolos (Nátricos, Hidromórfi cos e Háplicos) e Organossolos (Tiomórficos, Mésicos e Háplicos). Foram identificados quatro grandes ambientes na área do estado, com padrões de distribuição de solos característicos, cujas principais relações com os outros elementos do meio natural são descritas.

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Wykorzystanie seksualne dziecka jest związane z przestępstwami z art. 200 i z kilku artykułów pokrewnych polskiego Kodeksu karnego. Czynniki społeczno-kulturowe oddziaływają na to zjawisko poprzez dwa rodzaje socjalizacji. Socjalizacja wtórna zachodzi w populacji polskiej w sposób jednolity dla wszystkich sprawców, natomiast różnicuje ich socjalizacja pierwotna, w związku z czym to ona winna być przedmiotem badań. Najlepsze wyjaśnienia zjawiska oferują ujęcia zintegrowane, akcentujące, między innymi, rolę czynników rodzinnych w jego powstawaniu. W niniejszym artykule, jako teoretyczną podstawę badań, wykorzystano zintegrowaną teorię etiologii przestępstw seksualnych, która uznaje rodzinne doświadczenia sprawcy za główną przyczynę późniejszego seksualnego wykorzystywania dzieci. Zaproponowano cztery ścieżki rozwoju patologii wskazujące, w jaki sposób wczesne uwarunkowania psychologiczne (typ opieki i postawy rodziców) przyczyniają się do zostania sprawcą wykorzystania seksualnego dziecka w przyszłości, oraz zweryfikowano je w badaniach własnych. Wyniki przeprowadzonych badań częściowo potwierdzają zaprezentowany model teoretyczny i pozwalają wyznaczyć kierunki dalszych poszukiwań.

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Wydział Nauk Społecznych: Instytut Kulturoznawstwa

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In the article I present the structure of rural marriage in Poland of the 80-ies. I analyse basic factors of marriage mating, especially the reasons for getting married. Among the most important reasons are: love, material reasons, friendship, prestige, social position, sex. The article includes also the results of the research on marriage durability (stability), and also on factors influencing the marriage success or failure.

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This thesis presents a framework for aggregated congestion management for TCP flows and shows how to integrate such an approach in an existing TCP protocol stack. The thesis presents an initial implementation of this congestion management scheme in Linux, with performance evaluation in ns as well.

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This research asks the question: “What are the relational dynamics in Masters (MA) supervision?” It does so by focusing upon the supervisory relationship itself. It does this through dialoguing with the voices of both MA supervisors and supervisees in the Humanities using a Cultural Historical Activity Theory (CHAT) framework. In so doing, this research argues for a re-evaluation of how MA supervision is conceptualised and proposes a new theoretical framework for conceptualising MA supervision as a relational phenomenon. The research design was derived from an Activity Theory-influenced methodology. Data collection procedures included the administration of Activity Theory Logs, individual semi-structured interviews with both supervisors and supervisees and the completion of reflective journals. Grounded Theory was used to analyse the data. The sample for the study consists of three supervisor-supervisee dyads from three disciplines in the Humanities. Data was collected over the course of one academic year, 2010-2011. This research found that both individual and shared relational dynamics play an important role in MA supervision. Individual dynamics, such as supervisors’ iterative negotiation of ambiguity/clarity and supervisees’ boundary work, revealed that both parties attempt to negotiate a separation between their professional-academic identities and personal identities. However, an inherent paradox emerged when the shared relational dynamics of MA supervision were investigated. It was found that the shared space created by the supervisory relationship did not only exist in a physical setting, but was also psychoactive in nature and held strong emotional resonances for both parties involved. This served to undermine the separation between professional-academic and personal identities. As a result, this research argues that the interaction between the individual and shared relational dynamics in MA supervision enables, for both supervisors and supervisees, a disciplined improvisation of academic identity.

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Paris

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Extensive contour scaling of a 200 year old granite church is associated with the breaching of an apparently iron-rich crust and the widespread deposition of atmospheric dust within the canyon-like streetscape of Rio de Janeiro. Contemporary dust, accumulated dust from within the a depression on the building surface, the surface crust and the underlying granite are examined by a combination of total element analysis and sequential extraction, X-ray diffraction and energy dispersive X-ray fluorescence. Results indicate an increase in total organic carbon and a marked decrease in pH within the accumulated dust, and a rapid mobilization of anions and cations from the water-soluble and carbonate phases. It is considered that the latter is linked to salt accumulation within and eventual salt weathering of the granite. Post-depositional alteration of the dust is also linked with the de-silicification of clay minerals (Illite to kaolinite) and the loss of silica from the amorphous Fe/Mn phase of the accumulated dust under the initially saline and progressively more acidic conditions experienced at the stone - atmosphere interface. This mobilization of silica is associated with the formation of what is, in effect, a thin silica-rich surface crust or glaze. Within the glaze, assessory amounts of extractable iron are concentrated within the amorphous and crystalline Fe/Mn phases at levels that are significantly elevated with respect to the underlying granite, but much lower than the equivalent phases of the accumulated dust from which it is principally assumed to derive. The protection afforded to the stone work by the crust is not, however, permanent and within the last 15 years it has been possible to observe a rapid increase in the surface delamination of the church close to street level.