957 resultados para matrix-located processing peptidase


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Thermoset phenolic composites reinforced with sisal fibers were prepared to optimize the cure step. In the present study, processing parameters such as pressure, temperature, and time interval were varied to control the vaporization of the water generated as a byproduct during the crosslinking reaction. These molecules can vaporize forming voids, which in turn affect the final material properties. The set of results on impact strength revealed that the application of higher pressure before the gel point of the phenolic matrix produced composites with better properties. The SEM images showed that the cure cycle corresponding to the application of higher values of molding pressure at the gel point of the phenolic resin led to the reduction of voids in the matrix. In addition, the increase in the molding pressure during the cure step increased the resin interdiffusion. Better filling of the fiber channels decreased the possibility of water molecules diffusing through the internal spaces of the fibers. These molecules then diffused mainly through the bulk of the thermoset matrix, which led to a decrease in the water diffusion coefficient (D) at all three temperatures (25, 55 and 70 degrees C) considered in the experiments. (C) 2009 Elsevier Ltd. All rights reserved.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Fiber reinforced epoxy composites are used in a wide variety of applications in the aerospace field. These materials have high specific moduli, high specific strength and their properties can be tailored to application requirements. In order to screening optimum materials behavior, the effects of external environments on the mechanical properties during usage must be clearly understood. The environmental action, such as high moisture concentration, high temperatures, corrosive fluids or ultraviolet radiation (UV), can affect the performance of advanced composites during service. These factors can limit the applications of composites by deteriorating the mechanical properties over a period of time. Properties determination is attributed to the chemical and/or physical damages caused in the polymer matrix, loss of adhesion of fiber/resin interface, and/or reduction of fiber strength and stiffness. The dynamic elastic properties are important characteristics of glass fiber reinforced composites (GRFC). They control the damping behavior of composite structures and are also an ideal tool for monitoring the development of GFRC's mechanical properties during their processing or service. One of the most used tests is the vibration damping. In this work, the measurement consisted of recording the vibration decay of a rectangular plate excited by a controlled mechanism to identify the elastic and damping properties of the material under test. The frequency amplitude were measured by accelerometers and calculated by using a digital method. The present studies have been performed to explore relations between the dynamic mechanical properties, damping test and the influence of high moisture concentration of glass fiber reinforced composites (plain weave). The results show that the E' decreased with the increase in the exposed time for glass fiber/epoxy composites specimens exposed at 80 degrees C and 90% RH. The E' values found were: 26.7, 26.7, 25.4, 24.7 and 24.7 GPa for 0, 15, 30, 45 and 60 days of exposure, respectively. (c) 2005 Springer Science + Business Media, Inc.

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The purpose of this study was to histologically analyze the influence of bioactive glass and/or acellular dermal matrix on bone healing in surgically created defects in the tibiae of 64 rats (Rattus norvegicus, albinus, Wistar). Materials and Methods: A 4-mm X 3-mm unicortical defect was created on the anterolateral surface of the tibia. Animals were divided into 4 groups: C, control; BG, the defect was filled with bioactive glass; ADM, the defect was covered with acellular dermal matrix; and BG/ADM, the defect was filled with bioactive glass and covered with acellular dermal matrix. Animals were sacrificed at 10 or 30 days postoperatively, and the specimens were removed for histologic processing. The formation of new bone in the cortical area of the defect was evaluated histomorphometrically. Results: At 10 and 30 days postoperatively, groups C (39.65% +/- 5.63% / 63.34% +/- 5.22%) and ADM (38.12% +/- 5.53 / 58.96% +/- 7.05%) presented a larger amount of bone formation compared to the other groups (P<.05). In the same periods, groups BG (13.10% +/- 6.29% / 29.5% +/- 5.56%) and BG/ADM (20.72% +/- 8.31% / 24.19% +/- 6.69%) exhibited statistically similar new bone formation. However, unlike the other groups, group BG/ADM did not present a significant increase in bone formation between the 2 time points. Conclusion: Based on these results, it can be concluded that all of the materials used in this study delayed bone healing in non-critical-size defects. INT J ORAL MAXILLOFAC IMPLANTS 2008;23:811-817

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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This paper describes a methodology for solving efficiently the sparse network equations on multiprocessor computers. The methodology is based on the matrix inverse factors (W-matrix) approach to the direct solution phase of A(x) = b systems. A partitioning scheme of W-matrix , based on the leaf-nodes of the factorization path tree, is proposed. The methodology allows the performance of all the updating operations on vector b in parallel, within each partition, using a row-oriented processing. The approach takes advantage of the processing power of the individual processors. Performance results are presented and discussed.

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The use of sewage sludge in agricultural land as a means of sludge disposal and recycling has been shown to be economical and suitable because of the presence of nutrients such as nitrogen and phosphorus. However, municipal sludges often contain high quantities of toxic metals and other compounds that must be removed for its safe use in agricultural soils. The biological leaching of metals from sewage sludges has been shown to be a promising technique for metal detoxifying in such complex matrix. The process efficiency is dependent on several physico-chemical parameters, such as total solids concentration, metal forms, pH-ORP, and temperature. Scale-up of the process has not yet been defined and is still pursuing the correct operational design. Current research involving the bioleaching of metals from sewage sludge and its application to land, which affects soil physical properties, are presented and discussed.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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We present photoluminescence and decay of photo excited conductivity data for sol-gel SnO(2) thin films doped with rare earth ions Eu(3+) and Er(3+), a material with nanoscopic crystallites. Photoluminescence spectra are obtained under excitation with several monochromatic light sources, such as Kr(+) and Ar(+) lasers, Xe lamp plus a selective monochromator with UV grating, and the fourth harmonic of a Nd: YAG laser (4.65eV), which assures band-to-band transition and energy transfer to the ion located at matrix sites, substitutional to Sn(4+). The luminescence structure is rather different depending on the location of the rare-earth doping, at lattice symmetric sites or segregated at grain boundary layer, where it is placed in asymmetric sites. The decay of photo-excited conductivity also shows different trapping rate depending on the rare-earth concentration. For Er-doped films, above the saturation limit, the evaluated capture energy is higher than for films with concentration below the limit, in good agreement with the different behaviour obtained from luminescence data. For Eu-doped films, the difference between capture energy and grain boundary barrier is not so evident, even though the luminescence spectra are rather distinct.

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The sedimentary Curitiba basin is located in the Central-Southern part of the first Parananense plateau, and comprises Curitiba (PR), and part of the neighbour Municipalities (fig.1). It is supposed to be of Plio-Pleistocene age. It has a shallow sedimentary fulfillment, represented by the Guabirotuba formation (BIGARELLA and SALAMUNI, 1962) which is dristributed over a large area of about 3.000km2. The internal geometry, not entirely known yet, is actually object of detailed research, that shows its geological evolution to Cenozoic tectonic movements. For the purpose of this study the definition of the structural contour of the basement and their depo-centers is fundamental. This paper presents the results of the integration of surface and subsurface data, processed by statistical methods, which allowed a more precise definition of the morphostructural framework of the basement. For the analysis of the geological spacial data, specific softwares were used for statistical processing for trend surfaces analysis. The data used in this study are of following types: a) drilling logs for ground water; b) description of surface points of geological maps (CRPM, 1977); c) description of points of geotechnical drillings and down geological survey. The data of 223 drilling logs for ground water were selected out of 770 wells. The description files of 700 outcrops, as well as planialtimetric field data, were used for the localization of the basement outcrop. Thus, a matrix with five columns was set up: utm E-W (x) and utm N-S (y); surface altitude (z); altimetric cote of the contact between sedimentary rocks and the basement (k); isopachs (l). For the study of the basement limits, the analysis of surface trends of 2(nd) and 3(rd) degree polinomial for the altimetric data (figs. 2 and 3) were used. For the residuals the method of the inverse of the square of the distance (fig.4) was used. The adjustments and the explanations of the surfaces were made with the aid of multiple linear regressions. The analysis of 3rd degree polinomial trend surface (fig.3) confirmed that the basement tends to be more exposed towards NNW-SSE explaining better the data trend through an ellipse, which striking NE-SW and dipping SW axis coincides with the trough of the basin observed in the trending surface of the basement. The performed analysis and the respective images offer a good degree of certainty of the geometric model of the Curitiba Basin and of the morphostructure of its basement. The surface trend allows to sketch with a greater degree of confidence the structural contour of the topgraphic surface (figs. 5 and 6) and of the basement (figs. 7 and 8), as well as the delimitation of intermediate structural heights, which were responsible for isolated and assymmetric depocenters. These details are shown in the map of figures 9 and 10. Thus, the Curitiba Basin is made up by a structural trough stretching NE-SW, with maximum preserved depths of about 80m, which are separated by heights and depocenters striking NW-SE (fig. 11). These structural features seems to have been controlled by tectonic reactivation during the Tertiary (HASUI, 1990) and which younger dissection was conditioned by neotectonic processes (SALAMUNI and EBERT, 1994).

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As a chemical medium for preservation of tissues, glycerin has shown good results because it maintains the cellular integrity despite the tissue dehydration it causes. Taking advantage of the osteoinducing properties of the osseous matrix and glycerin as a proper medium for tissue preservation, osseous matrix was implanted in rat tibias. Twenty-four rats were used, each receiving two surgical wounds. In one of the wounds an osseous matrix preserved in 98% glycerin was implanted and the other received a matrix without preservatives. Six animals were sacrificed on days 10, 20, 30 and 60 post-implant. After routine histological processing, the specimens were stained in hematoxylin-eosin and Masson's trichrome. The results showed that the matrixes preserved in glycerin presented faster resorption with replacement by newly formed tissue.

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Objectives: The incretin-based therapy might be effective in patients possessing certain levels of preserved pancreatic beta-cells. However, doubts still exist regarding the efficacy of this atment in the recovery of tissues damaged by type 1 diabetes. Thus, the objective of this study was to evaluate the treatment with MK0431 in salivary glands of spontaneously diabetic mice, focusing mainly on the possible therapeutic and hypoglycaemic effects of this dipeptidyl peptidase IV inhibitor in the recovery of these salivary tissues. Methods and results: Twenty mice were divided into two groups of 10 animals each: group I (NOD diabetic/untreated) and group II (NOD diabetic MK0431/treated). The group II was treated during 4 weeks with MK0431 mixed in the food. The group I was maintained in the same way without receiving, however, any treatment. Glucose levels were monitored during treatment and salivary glands samples were collected at the end of treatment for the histological examination under both transmitted and polarized light microscopy. High glucose levels were observed in untreated animals, while in animals with treatment, reduction of these levels was observed. Tissue restructuring was also observed in animals submitted to therapy with MK0431, mainly in relation to the attempt to extracellular matrix reorganization. Conclusions: According to results, the treatment with this dipeptidyl peptidase IV inhibitor contributed to the general homeostasis of the organism and to the reestablishment of both epithelial and stromal compartments which were damaged by the hyperglycaemic condition, demonstrating that the incretin-based therapy may be an important complementary treatment for the type 1 diabetic condition. © 2012 Elsevier Ltd.

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Pós-graduação em Agronomia (Energia na Agricultura) - FCA

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Os aspectos morfodinâmicos relacionados à erosão ou acresção da linha de costa são alguns dos assuntos analisados na gestão das zonas costeiras que vêem sendo tratada em todo mundo no sentido de monitorar e proteger essas zonas. Esta tese objetiva analisar o comportamento da morfodinâmica costeira de Salinópolis, relacionando-o ao uso da orla oceânica. A área de estudo foi compartimentada em três setores: Oeste (praias da Corvina e do Maçarico), Central (praia do Farol Velho) e Leste (praia do Atalaia). A metodologia consistiu na: (a) aquisição e tratamento de imagens multitemporais (1988-2001-2013) do satélite Landsat 5 TM, 7 ETM e 8 OLI; (b) aplicação de entrevistas/questionários com banhistas, (c) aquisição de dados de campo durante as estações chuvosa (26, 27, 28/04/2013) e menos chuvosa (04, 05, 06/10/2013); e (d) análise laboratorial para o tratamento dos dados adquiridos em campo (topografia das praias estudadas, amostragem de sedimentos superficiais das mesmas e com o uso de armadilhas, e medições oceanográficas de ondas, marés, correntes e turbidez). Foram feitas as representações gráficas dos perfis topográficos das praias, calculados os parâmetros estatísticos granulométricos de Folk & Ward (1957), as taxas do transporte sedimentar nas praias e os parâmetros morfométricos de Short & Hesp (1982), estes últimos foram calculados com o intuito de relacioná-los aos estados morfodinâmicos de praias propostos por Wright & Short (1984) e Masselink & Short (1993). Para a classificação da costa oceânica de Salinópolis em termos de uso e ocupação foi utilizado o decreto nº 5.300 de 7 de dezembro de 2004. A partir das pesquisas sobre a urbanização na costa e das obras situadas nos ambientes costeiros foi utilizada uma matriz proposta por Farinaccio & Tessler (2010) que lista uma série de impactos ambientais, e o quadro de geoindicadores do comportamento da linha de costa proposto por Bush et al. (1999), para a identificação de locais com vulnerabilidade à erosão ou acresção. Para as condições oceanográficas em cada praia e periculosidade ao banho nas mesmas, foram integralizados os dados de ondas, de correntes, de morfodinâmica praial e questionários aplicados com banhistas. Atualmente, a orla oceânica de Salinópolis possui diferentes características quanto à utilização e conservação, abrangendo desde a tipologia de orlas naturais (Classe A) até orlas com urbanização consolidada (Classe C). A primeira ocorre nos extremos da área de estudo e, a segunda, na região da sede municipal. Quatro tipos de praias foram identificados segundo a exposição marítima e o grau das condições oceanográficas: tipo 1 (Maçarico), tipo 2 (Corvina), tipo 3 (Farol Velho) e tipo 4 (Atalaia). O trecho de costa com maiores impactos ambientais e com elevada erosão costeira localiza-se na praia do Farol Velho. O grau de periculosidade ao banho foi de 4 (praia do Maçarico) a 7 (praia do Atalaia) – médio a alto grau de risco. As praias de Salinópolis apresentam declives suaves (< 1,5°), grandes variações na linha de costa entre as estações do ano (9,6 a 88, 4 m) e volume sedimentar variável dependendo do grau de exposição das praias ao oceano aberto. Predominou o estado morfodinâmico dissipativo (Ω>5,5) para estas praias, mas com ocorrência do estado de banco e calha longitudinais (4,7<Ω<5,5) no setor oeste. As macromarés na área de estudo apresentaram altura máxima de 5,3 m (Setor Central, durante a estação menos chuvosa) e mínima de 4 m no mesmo setor, durante a estação chuvosa. As correntes longitudinais foram mais intensas no setor leste (>0,45 m/s) durante as duas estaçoes do ano. As alturas de ondas foram também maiores no setor leste (máximo de 1,05 m durante a maré enchente na estação menos chuvosa) e os períodos de ondas foram mais curtos (<4,5 s) no setor oeste. A média granulométrica obtida dos sedimentos coletados na face praial apresentou escala mais freqüente entre 2,6 a 2,8 phi, indicando a predominância de areia fina. O grau de seleção predominante dos sedimentos foi de 0,2 a 0,5 phi (muito bem selecionados e bem selecionados), e da assimetria foi de positiva (0,10 a 0,30) e de aproximadamente simétrica (-0,10 a 0,10). O grau de curtose variou desde muito platicúrtica (<0,67) a muito leptocúrtica (1,50 a 3,00). Foram observados eventos de acresção sedimentar da estação chuvosa a menos chuvosa. De 22/07/1988 a 28/08/2013 (25 anos) também houve predomínio de acresção, onde o avanço médio linear da linha de costa foi de 190,26 m. O recuo médio linear obtido para toda área de estudo foi de -42,25 m. Áreas com maior erosão são pontuais: divisas das praias da Corvina e Maçarico, e Farol Velho e Atalaia. Os traps portáteis indicaram uma maior quantidade de sedimentos transportados longitudinalmente na estação menos chuvosa (Mín. 280 g/m3: enchente, setor oeste; Máx. 1098 g/m3: vazante, setor leste). Nos traps de espraiamento, o balanço entre a quantidade de sedimentos entrando e saindo nas praias foi menor no setor central (Mín. 80 g/m3: vazante, estação menos chuvosa; Máx. 690 g/m3: enchente, estação menos chuvosa). A circulação costeira sedimentar é proveniente, principalmente, do efeito das marés, com direção governada pela enchente e vazante dos rios que atravessam a costa. Os dados indicam o transporte longitudinal de sedimentos da ilha de Atalaia e rio Sampaio para o setor oeste e as margens das faixas praiais.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)