ESCOLA PÚBLICA DE TEMPO INTEGRAL: UM ESTUDO DE CASO DAS REPRESENTAÇÕES SOCIAIS DOS PROFESSORES SOBRE OS PROCESSOS FORMATIVOS

O presente trabalho analisa as origens do modelo de Escola Pública de Tempo Integral, a partir de uma abordagem histórica que compara dois modelos: o da Escola-parque e a proposta implantada em 2006, no Estado de São Paulo. Investiga a questão com base na Teoria das Representações Sociais de Moscovici com o intuito de desvelar as representações sociais de professores, para aprofundar a reflexão sobre a sua inserção e preparação para a atuação neste modelo de escola. Prioriza, também, uma discussão sobre uma divisão que se percebe no contexto da Escola Pública de Tempo Integral, que se refere a uma distinção entre a proposta de atividades desenvolvidas sobre as atividades do currículo normal (consideradas mais importantes) e as atividades de extensão do currículo oficinas (consideradas menos importantes), cujas diferenças são geradas pela ausência de preparação destes profissionais nos processos formativos do projeto.(AU)

Because I Say So…

Catalog of an exhibition from the collection of Debra and Dennis Scholl, held at the Patricia & Phillip Frost Art Museum.

The (Un)Folding of Multidomain Proteins Through the Lens of Single-molecule Force-spectroscopy and Computer Simulation

Proteins are specialized molecules that catalyze most of the reactions that can sustain life, and they become functional by folding into a specific 3D structure. Despite their importance, the question, "how do proteins fold?" - first pondered in in the 1930's - is still listed as one of the top unanswered scientific questions as of 2005, according to the journal Science. Answering this question would provide a foundation for understanding protein function and would enable improved drug targeting, efficient biofuel production, and stronger biomaterials. Much of what we currently know about protein folding comes from studies on small, single-domain proteins, which may be quite different from the folding of large, multidomain proteins that predominate the proteomes of all organisms.

In this thesis I will discuss my work to fill this gap in understanding by studying the unfolding and refolding of large, multidomain proteins using the powerful combination of single-molecule force-spectroscopy experiments and molecular dynamic simulations.

The three model proteins studied - Luciferase, Protein S, and Streptavidin - lend insight into the inter-domain dependence for unfolding and the subdomain stabilization of binding ligands, and ultimately provide new insight into atomistic details of the intermediate states along the folding pathway.

(Table T1) Density, porosity, void ratio, diffusivity and permeability of ODP Site 185-1149 sediments

The subduction of oceanic plates regulates crustal growth, influences arc volcanism, and refertilizes the mantle. Continental growth occurs by subduction of crustal material (seawater components, marine sediments, and basaltic crust). The geochemical and physical evolution of the Earth's crust depends, in large part, on the fate of subducted material at convergent margins (Armstrong, 1968, doi:10.1029/RG006i002p00175; Karig and Kay, 1981, 10.1098/rsta.1981.0108). The crustal material on the downgoing plate is recycled to various levels in the subduction zone. The recycling process that takes place in the "Subduction Factory" is difficult to observe directly but is clearly illuminated using chemical tracers. Von Huene and Scholl (1991, doi:10.1029/91RG00969) and Plank and Langmuir (1993, doi:10.1038/362739a0) preliminarily calculated a large flux of subducted materials. By mass balancing the chemical tracers and measuring the fractionations that occur between them, the Subduction Factory work and the effect on the Earth's evolution can be estimated. In order to elucidate this mass balance, Ocean Drilling Program Leg 185 drilled two deepwater shales into the oceanic crust situated in the Mariana-Izu Trenches and recovered core samples of incoming oceanic crust. The calculations of mass circulation in the subduction zone, however, did not take into account the mass transfer properties within subducted oceanic crust, although the dewatering fluid and diffused ions may play an important role in various activities such as seismogeneity, serpentine diapiring, and arc volcanism. Thus, this paper focuses on the quantitative measurements of the physical and mass transfer properties of subducted oceanic crust.