960 resultados para Political regime


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Nesta pesquisa, elegemos Alma Infantil (1912) como fonte e objeto de estudo: obra escrita pela poetisa Francisca Júlia da Silva em parceria com seu irmão, o também poeta Júlio César da Silva. A pesquisa busca evocar o cenário literário escolar do entresséculos (XIX-XX) e do início do século XX, em suas particularidades, coordenando o projeto político e pedagógico que conformava as escolas no período com os temas, autores e textos que circulavam nas salas de aula, sobretudo no estado de São Paulo, onde se verifica, no período, a maior incidência de planos e ações pedagógicas. Temos por finalidade exprimir as relações entre Alma Infantil e alguns projetos de nação propostos pelo governo na Primeira República (1889-1930). Alma Infantil, publicado pela Livraria Editora Magalhães no início do século XX é livro para uso escolar, mais especificamente, livro de leitura suplementar. Este material, assim como muitos outros, estava comprometido com a moral e a ordem cívica dos primeiros anos do novo regime, com a exaltação à natureza, aos animais e às riquezas naturais do país, conforme a análise dos poemas indica. O livro dos irmãos Silva, em seus 48 poemas e quatro hinos, apresenta linguagem acessível e adaptada à leitura da criança, de fácil compreensão, conformados por um conceito de moral notoriamente verificado. Em grande parcela dos poemas, encontramos referências a uma linguagem leve, descompromissada com a rigidez e culto à forma diferentemente da que o exaltava. Outrossim, a presença dos hinos em Alma Infantil demarca ainda mais esta unidade patriótica a que o Brasil se propunha compor no entresséculos. Os temas dos hinos estudo, escola, trabalho, pátria - alinham os ideais republicanos de ordem, trabalho e progresso que vigorava no Brasil naquele momento. Sendo assim, através da pesquisa histórica que resultou neste texto, podemos afirmar por meio de análise textual e documental que Alma Infantil é obra confeccionada para uso escolar, como sua própria capa o diz, e mais, é uma legítima amostra do maquinário político educacional dos primeiros anos do regime republicano neste país.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): Selected hydrometeorological (HM) data for the Pacific Northwest and atmospheric and North Pacific sea-surface temperature (SST) data are examined for three successive periods that are subsets of the historical record to estimate if their characteristics have changed.

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The effects of turbulent Reynolds number on the statistical behaviour of the displacement speed have been studied using three-dimensional Direct Numerical Simulation of statistically planar turbulent premixed flames. The probability of finding negative values of the displacement speed is found to increase with increasing turbulent Reynolds number when the Damkhler number is held constant. It has been shown that the statistical behaviour of the Surface Density Function, and its strain rate and curvature dependence, plays a key role in determining the response of the different components of displacement speed. Increasing the turbulent Reynolds number is shown to reduce the strength of the correlations between tangential strain rate and dilatation rate with curvature, although the qualitative nature of the correlations remains unaffected. The dependence of displacement speed on strain rate and curvature is found to weaken with increasing turbulent Reynolds number when either Damkhler or Karlovitz number is held constant, but the qualitative nature of the correlation remains unaltered. The implications of turbulent Reynolds number effects in the context of Flame Surface Density (FSD) modelling have also been addressed, with emphasis on the influence of displacement speed on the curvature and propagation terms in the FSD balance equation. © 2011 Nilanjan Chakraborty et al.

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Three spatial structure groups of radionuclides in U and Th series, 210Pb-excess and 137Cs, and 40K were found based on analyzing temporal and spatial datum of their content by factor analysis with oblique rotation in Nhatrang bay. U and Th spatial structure with their contours decreased toward the offshore, ran longshore and divided seawater of bay into two parts with strong gradient on both sides. Inside part located from center of Nhatrang bay toward the seashore with three main deposit centers of their contents higher than 23 Bq/kg.dry for 238U and 40 Bq/kg.dry for 232Th, indicated unstability of shoreline. Almost sediments coming from river extended toward the offshore, were stopped and transported toward southeastern. The outside part was less than above mentioned content. The boundary line between two parts superposed with the constantly limit line of turbid plume in the rainy season. Direct influence of the continental runoff was limited by the 9 Bq/kg.dry contour of 238U, 19 Bq/kg.dry contour of 232Th. Longshore current was a predominant process whereas lateral transport as sifting and winnowing process of finer grains in sediments of Nhatrang bay. Areas that had very low content of 137Cs and 210 Pb-excess adjoining shoreline showed areas being eroded. Accumulation of 137Cs and 210 Pbexcess nearby river mouth characterized for fine compositions of sediments controlled by seasonal plumes and sites further toward the south indicated finer materials transported from river and accumulated in lack of hydrodynamic process. Near shore accumulation of 40K revealed the sediments there originated from bed erosion.

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The characteristics of the scalar dissipation rate transport in the corrugated flamelets and the thin reaction zones regimes are studied based on two three-dimensional Direct Numerical Simulation (DNS) databases for freely propagating statistically planar turbulent premixed flames. The turbulent flame parameters are so chosen that the database which represents the corrugated flamelets regime has a global Damköhler number Da>1 whereas the database representing the thin reaction zones regime has Da <1. It is demonstrated that the terms originating from the correlation between fluctuating velocity and scalar gradient T1 shows strong Da dependence. The terms originating from dilatation T2, the scalar inner product of gradients of velocity and scalar fields T3 and the correlation between reaction rate and scalar gradients T4 and the dissipation term D2 remain important for both the flames. However, T3 dissipates scalar dissipation rate in the Da > 1 flame while it produces scalar dissipation rate in the Da < 1 flame. This difference is because of the change in the alignment between scalar and velocity gradients