797 resultados para 901


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In April 1998, the RBI, the Indian central bank, formally announced a shift in its policy framework from monetary targeting to a multiple indicator approach, and since then, under this framework, the bank has considered a range of economic and financial variables as policy indicators for drawing policy perspectives. This paper aims to examine the effectiveness of this current policy framework in India by analyzing the causal relationships of each indicator variable on the objective variables. The results reveal that, except for bank credit, all indicator variables considered in this study have a causal relationship with at least either output or price level, suggesting that most preannounced economic and financial variables have served as useful policy indicators under the multiple indicator approach.

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This work evaluates a spline-based smoothing method applied to the output of a glucose predictor. Methods:Our on-line prediction algorithm is based on a neural network model (NNM). We trained/validated the NNM with a prediction horizon of 30 minutes using 39/54 profiles of patients monitored with the Guardian® Real-Time continuous glucose monitoring system The NNM output is smoothed by fitting a causal cubic spline. The assessment parameters are the error (RMSE), mean delay (MD) and the high-frequency noise (HFCrms). The HFCrms is the root-mean-square values of the high-frequency components isolated with a zero-delay non-causal filter. HFCrms is 2.90±1.37 (mg/dl) for the original profiles.

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Inclui bibliografia

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Introdução: Estudos têm demonstrado que doenças crônicas e alterações metabólicas podem atuar como fator de aceleração na degeneração do sistema auditivo decorrente da idade. Todavia, os estudos sobre a associação entre a perda auditiva com o diabetes mellitus (DM) e com a hipertensão arterial (HA) em idosos mostraram conclusões controversas. Sendo assim, novos estudos sobre este assunto são necessários, a fim de esclarecer o efeito destas doenças crônicas sobre o sistema auditivo. Objetivos: Comparar uma audiometria inicial (A1) com uma audiometria sequencial (A2) realizada com um intervalo de 3 a 4 anos em uma população de idosos portadores de DM e/ou HA; realizar um estudo comparativo entre quatro grupos de idosos: grupo controle (GC), formado por idosos sem alterações crônicas, grupo de idosos portadores de DM; grupo de idosos portadores de HA, grupo de idosos portadores de DM e HA. Métodos: Foi realizado um levantamento em 901 prontuários do Estudo Longitudinal de Saúde Auditiva do Adulto (ELSAA), de indivíduos atendidos no Hospital Universitário (HU) da Universidade de São Paulo, no período de 2009 a 2015. De acordo com os critérios de inclusão, foram selecionados 100 indivíduos para participarem da presente pesquisa. A avaliação inicial (A1), constando de anamnese, audiometria tonal e imitânciometria foram utilizadas e foi feita uma nova avaliação audiológica (A2) após o período de 3 a 4 anos. Os participantes foram distribuídos em quatro grupos: 20 indivíduos portadores de DM (grupo DM), 20 indivíduos portadores de HA (grupo HA), 20 indivíduos portadores de DM e HA (grupo DMHA) e 40 indivíduos não portadores de DM nem de HA (GC). Para cada grupo estudo (HA, DM e DMHA), foram selecionados indivíduos (entre os 40 do GC) de forma a parear as características referentes a idade e sexo. Foram utilizados os testes estatísticos ANOVA, teste exato de Fisher e Kruskal-Wallis, com nível de significância de 0,05. Foi também calculada a odds ratio, com intervalo de confiança de 95%. Resultados: Não houve diferença estatisticamente significante entre as orelhas para nenhum dos grupos; sendo assim, as orelhas direita e esquerda foram agrupadas para as outras comparações. Na comparação da média de aumento anual dos limiares auditivos da primeira avaliação A1 com a segunda avaliação A2 entre os grupos, pode-se observar que para o grupo DM, não houve diferença estatisticamente significante para nenhuma das frequências avaliadas, quando comparado ao seu respectivo controle; para o grupo HA foram observadas diferenças significantes a partir de 4kHz, bem como tendência à diferença estatisticamente significante em 3 kHz, quando comparado a seu respectivo controle. Já para o grupo DMHA, quando comparado a seu grupo controle, foram observadas diferenças significantes nas frequências de 500, 2k, 3k e 8kHz, além de tendência à diferença estatisticamente significante em 4k e 6kHz. Considerando-se os casos novos de perda auditiva, pode-se observar que houve diferença estatisticamente significante apenas para o grupo HA, para as frequências altas. Verificou-se também que, para as frequências altas (3k a 8kHz), os números de casos novos de perda auditiva foram sempre maiores nos grupos estudo quando comparados aos seus respectivos controles. Na comparação das médias dos limiares auditivos, tanto na avaliação A1 quanto na avaliação A2, observou-se que os grupos estudo (DM, HA e DMHA) apresentaram limiares auditivos mais prejudicados, quando comparados a seus respectivos grupos controle. Na comparação entre os grupos apenas para a avaliação A2, pode-se observar que para as frequências altas, houve associação estatisticamente significante entre apresentar as condições clínicas (DM, HA e DMHA) e a presença de perda auditiva. A OR para DM foi de 5,57 (2,9-14,65), para HA foi de 4,2 (1,35-13,06) e para DMHA foi de 5,72 (1,85-17,64). Conclusão: Verificou-se que os idosos portadores de DM, HA ou ambos apresentaram limiares auditivos mais rebaixados quando comparados a seus respectivos grupos controle, principalmente nas altas frequências, o que sugere que estas patologias podem ter um efeito deletério sobre a audição. Além disso, nota-se que o grupo HA apresentou limiares auditivos piores para a maioria das frequências e foi o que apresentou maior queda dos limiares auditivos no segmento de 3 a 4 anos, quando comparado aos outros dois grupos estudo (DMHA e DM), sugerindo que dentre as três condições estudadas, a hipertensão parece ser a que teve maior influência sobre a audição

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Visual symptoms are relatively common in Parkinson's disease (PD) and optical coherence tomography has indicated possible retinal thinning. Accumulation of aggregated α-synuclein is thought to be a central pathogenic event in the PD brain but there have not as yet been reports of retinal synucleinopathy. Retinal wholemounts were prepared from subjects with a primary clinicopathological diagnosis of PD (N = 9), dementia with Lewy bodies (DLB; N = 3), Alzheimer's disease (N = 3), progressive supranuclear palsy (N = 2) as well as elderly normal control subjects (N = 4). These were immunohistochemically stained with an antibody against α-synuclein phosphorylated at serine 129, which is a specific molecular marker of synucleinopathy. Phosphorylated α-synuclein-immunoreactive (p-syn IR) nerve fibers were present in 7/9 PD subjects and in 1/3 DLB subjects; these were sparsely distributed and superficially located near or at the inner retinal surface. The fibers were either long and straight or branching, often with multiple en-passant varicosities along their length. The straight fibers most often had an orientation that was radial with respect to the optic disk. Together, these features are suggestive of either retinopetal/centrifugal fibers or of ganglion cell axons. In one PD subject there were sparse p-syn IR neuronal cell bodies with dendritic morphology suggestive of G19 retinal ganglion cells or intrinsically photosensitive ganglion cells. There were no stained nerve fibers or other specific staining in any of the non-PD or non-DLB subjects. It is possible that at least some of the observed visual function impairments in PD subjects might be due to α-synucleinopathy.

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The voltammetric profile of preferentially shaped platinum nanoparticles has been used to analyze the different sites present on the surface. For the first time, this analysis has been made in NaOH solutions and revisited in sulfuric and perchloric acid media. The comparison with the voltammetric profiles of the model surfaces, that is, single-crystal electrodes, allows assigning the different signals appearing in the voltammograms of the nanoparticle to specific sites on the surface. A good correlation between the shape of the nanoparticle determined by TEM and the voltammetric profile is obtained. For the nanoparticles characterized in alkaline media, the adsorbed species on the surface have been characterized, and three major regions can be identified. Below 0.2 V, the major contribution is due to hydrogen adsorption, whereas above 0.6 V, adsorbed OH is the main species on the surface. Between those values, the signals are due to the competitive adsorption/desorption process of OH/H. New criteria for determining the active area in NaOH solutions has been proposed. In this medium, the total charge density measured between 0.06 and 0.90 V stands for 390 μC cm–2. The areas measured are in perfect agreement with those measured in acid media. Once the nanoparticles have been characterized, the behavior of the nanoparticles toward CO oxidation is analyzed and compared with that observed for single-crystal electrodes.

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Pollen analyses and 14C-datings were carried out on two late glacial profiles from Ruegen Island, Mecklenburg-Vorpommern at the southwestern Baltic coast. The palaeoclimatic and palaeoecologic interpretations were supported by carpological investigations. The organogenic deposits of the 'Hoelle' outcrop near Dwasieden Park were chosen because of their unique stratigraphic position, which according to PANZIG (1989), lay under a m3m-Glacial Till of the Mecklenburg Advance (W3). The results indicated that the initial phase of the late glacial sedimentation in a relatively small and asymmetrical lake basin (in comparison with the larger Nieder- and Credner lake to the southwest), probably had its origin in the older Alleroed (II a) after FIRBAS (1949). The basal clastic sediments were rapidly followed by peat deposits and later, due to a rising water table, by muds rich in organic matter. The area was covered with sparse Betula-(Pinus) forests having heliophilous late-glacial elements typical of the surrounding areas during the younger Alleroed (II b). With the climatic change to colder and drier conditions at the beginning of the Younger Dryas (III), the vegetation decreased and enhanced erosional processes led to the fill up of the depression with fine clastic sediments. The intense relief differences of the surroundings coupled with high water saturation in the sediments led to solifluction in the m3m-Glacial Till and its placement discordantly over the organogenic sequence.

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The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.