18 resultados para Ragin, Charles C.: Fuzzy-set social science


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Video games in a learning environ-ment and their application to the educational world has become a common study between researchers because the use of videogames in the classroom is coherent with a compe-tence-based education theory. A social science approach to video-games allows an exhaustive under-standing of the video games and of the game experience in the classroom. When a video game gives to the user a high level of immersion, all his interest and energy is focused in the game, this fact together with the motivation in the video game is the basis of interest for educators and researchers in the potentiality of the video games as learning environ-ments. In this presentation, we will show and analyze the importance of the video games in an educational context, using a case study: the video game "Monturiol el joc". In the paper, we describe the video game structure, the instructional function, the practice application and the future work. Also, we discuss the impor-tance of the video games as a learning immersive environment, and we conclude our report with a brief analysis of the importance of the study of video games.

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L’estiu de 1990 moria a Amsterdam un dels sociòlegs més preeminents del segle XX, l’alemany Norbert Elias. La seva vida i la seva obra, profundament imbricades, són un reflex de la complexitat, de les llums i les ombres del segle passat. Amb aquesta proposta de retrat intel·lectual pretenem per una banda commemorar l’efemèride dels 20 anys de la mort d’un sociòleg poc reconegut i poc emprat. I d’altra banda, oferir una introducció a un personatge i una obra que, per la seva magnitud i originalitat, mereixen estar entre les més rellevants de la sociologia. Com a fil conductor de l’article proposem una combinació de llocs físics i simbòlics que van marcar la seva trajectòria.

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A new dynamic model of dolomitization predicts a multitude of textural, paragenetic, geochemical and other properties of burial dolomites. The model is based on two postulates, (1) that the dolomitizing brine is Mg-rich but under saturated with both calcite and dolomite, and (2) that the dolomite-for-calcite replacement happens not by dissolution-precipitation as usually assumed, but by dolomite-growth-driven pressure solution of the calcite host. Crucially, the dolomite-for-calcite replacement turns out to be self-accelerating via Ca2 : the Ca2 released by each replacement increment accelerates the rate of the next, and so on. As a result, both pore-fluid Ca2 and replacement rate grow exponentially.