67 resultados para multimodal reflection

em Repositório Científico do Instituto Politécnico de Lisboa - Portugal


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The effects of the Miocene through Present compression in the Tagus Abyssal Plain are mapped using the most up to date available to scientific community multi-channel seismic reflection and refraction data. Correlation of the rift basin fault pattern with the deep crustal structure is presented along seismic line IAM-5. Four structural domains were recognized. In the oceanic realm mild deformation concentrates in Domain I adjacent to the Tore-Madeira Rise. Domain 2 is characterized by the absence of shortening structures, except near the ocean-continent transition (OCT), implying that Miocene deformation did not propagate into the Abyssal Plain, In Domain 3 we distinguish three sub-domains: Sub-domain 3A which coincides with the OCT, Sub-domain 3B which is a highly deformed adjacent continental segment, and Sub-domain 3C. The Miocene tectonic inversion is mainly accommodated in Domain 3 by oceanwards directed thrusting at the ocean-continent transition and continentwards on the continental slope. Domain 4 corresponds to the non-rifted continental margin where only minor extensional and shortening deformation structures are observed. Finite element numerical models address the response of the various domains to the Miocene compression, emphasizing the long-wavelength differential vertical movements and the role of possible rheologic contrasts. The concentration of the Miocene deformation in the transitional zone (TC), which is the addition of Sub-domain 3A and part of 3B, is a result of two main factors: (1) focusing of compression in an already stressed region due to plate curvature and sediment loading; and (2) theological weakening. We estimate that the frictional strength in the TC is reduced in 30% relative to the surrounding regions. A model of compressive deformation propagation by means of horizontal impingement of the middle continental crust rift wedge and horizontal shearing on serpentinized mantle in the oceanic realm is presented. This model is consistent with both the geological interpretation of seismic data and the results of numerical modelling.

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Optical fiber microwires (OFMs) are nonlinear optical waveguides that support several spatial modes. The multimodal generalized nonlinear Schrodinger equation (MM-GNLSE) is deduced taking into account the linear and nonlinear modal coupling. A detailed theoretical description of four-wave mixing (FWM) considering the modal coupling is developed. Both, the intramode and the intermode phase-matching conditions is calculated for an optical microwire in a strong guiding regime. Finally, the FWM dynamics is studied and the amplitude evolution of the pump beams, the signal and the idler are analyzed.

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Chronic liver disease (CLD) is most of the time an asymptomatic, progressive, and ultimately potentially fatal disease. In this study, an automatic hierarchical procedure to stage CLD using ultrasound images, laboratory tests, and clinical records are described. The first stage of the proposed method, called clinical based classifier (CBC), discriminates healthy from pathologic conditions. When nonhealthy conditions are detected, the method refines the results in three exclusive pathologies in a hierarchical basis: 1) chronic hepatitis; 2) compensated cirrhosis; and 3) decompensated cirrhosis. The features used as well as the classifiers (Bayes, Parzen, support vector machine, and k-nearest neighbor) are optimally selected for each stage. A large multimodal feature database was specifically built for this study containing 30 chronic hepatitis cases, 34 compensated cirrhosis cases, and 36 decompensated cirrhosis cases, all validated after histopathologic analysis by liver biopsy. The CBC classification scheme outperformed the nonhierachical one against all scheme, achieving an overall accuracy of 98.67% for the normal detector, 87.45% for the chronic hepatitis detector, and 95.71% for the cirrhosis detector.

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In research on Silent Speech Interfaces (SSI), different sources of information (modalities) have been combined, aiming at obtaining better performance than the individual modalities. However, when combining these modalities, the dimensionality of the feature space rapidly increases, yielding the well-known "curse of dimensionality". As a consequence, in order to extract useful information from this data, one has to resort to feature selection (FS) techniques to lower the dimensionality of the learning space. In this paper, we assess the impact of FS techniques for silent speech data, in a dataset with 4 non-invasive and promising modalities, namely: video, depth, ultrasonic Doppler sensing, and surface electromyography. We consider two supervised (mutual information and Fisher's ratio) and two unsupervised (meanmedian and arithmetic mean geometric mean) FS filters. The evaluation was made by assessing the classification accuracy (word recognition error) of three well-known classifiers (knearest neighbors, support vector machines, and dynamic time warping). The key results of this study show that both unsupervised and supervised FS techniques improve on the classification accuracy on both individual and combined modalities. For instance, on the video component, we attain relative performance gains of 36.2% in error rates. FS is also useful as pre-processing for feature fusion. Copyright © 2014 ISCA.

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The conjugate margins system of the Gulf of Lion and West Sardinia (GLWS) represents a unique natural laboratory for addressing fundamental questions about rifting due to its landlocked situation, its youth, its thick sedimentary layers, including prominent palaeo-marker such as the MSC event, and the amount of available data and multidisciplinary studies. The main goals of the SARDINIA experiment, were to (i) investigate the deep structure of the entire system within the two conjugate margins: the Gulf of Lion and West Sardinia, (ii) characterize the nature of the crust, and (iii) define the geometry of the basin and provide important constrains on its genesis. This paper presents the results of P-wave velocity modelling on three coincident near-vertical reflection multi-channel seismic (MCS) and wide-angle seismic profiles acquired in the Gulf of Lion, to a depth of 35 km. A companion paper [part II Afilhado et al., 2015] addresses the results of two other SARDINIA profiles located on the oriental conjugate West Sardinian margin. Forward wide-angle modelling of both data sets confirms that the margin is characterised by three distinct domains following the onshore unthinned, 33 km-thick continental crust domain: Domain I is bounded by two necking zones, where the crust thins respectively from 30 to 20 and from 20 to 7 km over a width of about 170 km; the outermost necking is imprinted by the well-known T-reflector at its crustal base; Domain II is characterised by a 7 km-thick crust with anomalous velocities ranging from 6 to 7.5 km/s; it represents the transition between the thinned continental crust (Domain I) and a very thin (only 4-5 km) "atypical" oceanic crust (Domain III). In Domain II, the hypothesis of the presence of exhumed mantle is falsified by our results: this domain may likely consist of a thin exhumed lower continental crust overlying a heterogeneous, intruded lower layer. Moreover, despite the difference in their magnetic signatures, Domains II and III present the very similar seismic velocities profiles, and we discuss the possibility of a connection between these two different domains.

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Geophysical data acquired on the conjugate margins system of the Gulf of Lion and West Sardinia (GLWS) is unique in its ability to address fundamental questions about rifting (i.e. crustal thinning, the nature of the continent-ocean transition zone, the style of rifting and subsequent evolution, and the connection between deep and surface processes). While the Gulf of Lion (GoL) was the site of several deep seismic experiments, which occurred before the SARDINIA Experiment (ESP and ECORS Experiments in 1981 and 1988 respectively), the crustal structure of the West Sardinia margin remains unknown. This paper describes the first modeling of wide-angle and near-vertical reflection multi-channel seismic (MCS) profiles crossing the West Sardinia margin, in the Mediterranean Sea. The profiles were acquired, together with the exact conjugate of the profiles crossing the GoL, during the SARDINIA experiment in December 2006 with the French R/V L'Atalante. Forward wide-angle modeling of both data sets (wide-angle and multi-channel seismic) confirms that the margin is characterized by three distinct domains following the onshore unthinned, 26 km-thick continental crust : Domain V, where the crust thins from 26 to 6 km in a width of about 75 km; Domain IV where the basement is characterized by high velocity gradients and lower crustal seismic velocities from 6.8 to 7.25 km/s, which are atypical for either crustal or upper mantle material, and Domain III composed of "atypical" oceanic crust.The structure observed on the West Sardinian margin presents a distribution of seismic velocities that is symmetrical with those observed on the Gulf of Lion's side, except for the dimension of each domain and with respect to the initiation of seafloor spreading. This result does not support the hypothesis of simple shear mechanism operating along a lithospheric detachment during the formation of the Liguro-Provencal basin.

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Relatório Final de Projecto Pedagógico apresentado à Escola Superior de Dança, com vista à obtenção do grau de Mestre em Metodologias do Ensino da Dança

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Dissertação apresentada à Escola Superior de Comunicação Social como parte dos requisitos para obtenção de grau de mestre em Audiovisual e Multimédia.

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The use of iris recognition for human authentication has been spreading in the past years. Daugman has proposed a method for iris recognition, composed by four stages: segmentation, normalization, feature extraction, and matching. In this paper we propose some modifications and extensions to Daugman's method to cope with noisy images. These modifications are proposed after a study of images of CASIA and UBIRIS databases. The major modification is on the computationally demanding segmentation stage, for which we propose a faster and equally accurate template matching approach. The extensions on the algorithm address the important issue of pre-processing that depends on the image database, being mandatory when we have a non infra-red camera, like a typical WebCam. For this scenario, we propose methods for reflection removal and pupil enhancement and isolation. The tests, carried out by our C# application on grayscale CASIA and UBIRIS images show that the template matching segmentation method is more accurate and faster than the previous one, for noisy images. The proposed algorithms are found to be efficient and necessary when we deal with non infra-red images and non uniform illumination.

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Dissertação apresentada para obtenção do grau de Mestre em Educação Matemática na Educação Pré-Escolar e no 1.º e 2.º Ciclos do Ensino Básico

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The crustal and lithospheric mantle structure at the south segment of the west Iberian margin was investigated along a 370 km long seismic transect. The transect goes from unthinned continental crust onshore to oceanic crust, crossing the ocean-continent transition (OCT) zone. The wide-angle data set includes recordings from 6 OBSs and 2 inland seismic stations. Kinematic and dynamic modeling provided a 2D velocity model that proved to be consistent with the modeled free-air anomaly data. The interpretation of coincident multi-channel near-vertical and wide-angle reflection data sets allowed the identification of four main crustal domains: (i) continental (east of 9.4 degrees W); (ii) continental thinning (9.4 degrees W-9.7 degrees W): (iii) transitional (9.7 degrees W-similar to 10.5 degrees W); and (iv) oceanic (west of similar to 10.5 degrees W). In the continental domain the complete crustal section of slightly thinned continental crust is present. The upper (UCC, 5.1-6.0 km/s) and the lower continental crust (LCC, 6.9-7.2 km/s) are seismically reflective and have intermediate to low P-wave velocity gradients. The middle continental crust (MCC, 6.35-6.45 km/s) is generally unreflective with low velocity gradient. The main thinning of the continental crust occurs in the thinning domain by attenuation of the UCC and the LCC. Major thinning of the MCC starts to the west of the LCC pinchout point, where it rests directly upon the mantle. In the thinning domain the Moho slope is at least 13 degrees and the continental crust thickness decreases seaward from 22 to 11 km over a similar to 35 km distance, stretched by a factor of 1.5 to 3. In the oceanic domain a two-layer high-gradient igneous crust (5.3-6.0 km/s; 6.5-7.4 km/s) was modeled. The intra-crustal interface correlates with prominent mid-basement, 10-15 km long reflections in the multi-channel seismic profile. Strong secondary reflected PmP phases require a first order discontinuity at the Moho. The sedimentary cover can be as thick as 5 km and the igneous crustal thickness varies from 4 to 11 km in the west, where the profile reaches the Madeira-Tore Rise. In the transitional domain the crust has a complex structure that varies both horizontally and vertically. Beneath the continental slope it includes exhumed continental crust (6.15-6.45 km/s). Strong diffractions were modeled to originate at the lower interface of this layer. The western segment of this transitional domain is highly reflective at all levels, probably due to dykes and sills, according to the high apparent susceptibility and density modeled at this location. Sub-Moho mantle velocity is found to be 8.0 km/s, but velocities smaller than 8.0 km/s confined to short segments are not excluded by the data. Strong P-wave wide-angle reflections are modeled to originate at depth of 20 km within the lithospheric mantle, under the eastern segment of the oceanic domain, or even deeper at the transitional domain, suggesting a layered structure for the lithospheric mantle. Both interface depths and velocities of the continental section are in good agreement to the conjugate Newfoundland margin. A similar to 40 km wide OCT having a geophysical signature distinct from the OCT to the north favors a two pulse continental breakup.

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Projeto de intervênção apresentado à Escola Superior de Educação para a obtenção do grau de mestre em Didática da Língua Portuguesa em 1º e 2º Ciclos do Ensino Básico

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A responsabilidade da construção de uma escola para todos deve ser o grande objectivo de todo e qualquer professor, criando espaços de reflexão conjunta no sentido de serem traçados projectos curriculares diferenciados que dêem resposta a todos os alunos na sua diversidade plural. Assim, a concepção e construção da escola inclusiva implicam mudanças, quer nas atitudes e práticas dos agentes educativos, quer nas estruturas do sistema de ensino ao nível organizacional e da gestão curricular. Neste âmbito, a adequação do currículo às necessidades educativas especiais (NEE) dos alunos torna-se essencial na (re)construção e operacionalização dos diferentes processos curriculares. O trabalho que agora se apresenta foi desenvolvido através de um estudo de caso. Constitui uma tentativa de compreensão das percepções dos professores e das práticas pedagógicas que desenvolvem para efectuar adequações curriculares para alunos com NEE. Centrámo-nos nos professores de um conselho de turma do sétimo ano do terceiro ciclo do ensino básico (3º CEB) que inclui uma aluna com NEE, procurando saber o que pensam sobre o processo de adequação curricular, como o concebem e como o implementam. Como metodologia de recolha dos dados utilizamos as técnicas da entrevista, da análise documental e da observação naturalista. Concluímos que, apesar das dificuldades que expressam e demonstram, os professores assumem a necessidade de implementar adequações curriculares face às NEE dos alunos, como resposta às diferenças e particularidades de cada um, tendo em vista o desenvolvimento de competências essenciais e a conclusão da escolaridade obrigatória. As Adequações Curriculares são percepcionadas como muito vantajosas do ponto de vista da promoção do sucesso educativo para todos os alunos e em particular para os alunos com NEE, proporcionando a estes, acompanhar o currículo mais próximo do que é normal, sentirem-se como “iguais” aos seus colegas, melhorar a sua auto-estima, auto-confiança e motivação ABSTRACT The responsibility of building a school for all must be the ultimate goal of any teacher, creating spaces for joint reflection in order to draw differentiated curricular projects which respond to all students in their plural diversity. Thus, the design and construction of the inclusive school involve changes both in attitudes and practices of the educational agents, and in the structures of the education system regarding the organization and the curriculum management. In this context, the adequacy of the curriculum to students’ special educational needs (SEN) becomes essential in the (re) construction and operationalization of the different curriculum processes. The work now presented was developed through a case study. It attempts to understand the perceptions of teachers and the pedagogical practices they develop to make curricular adjustments for students with SEN. We focused on the teachers of a seventh year class of the third cycle of basic education (3rd CBE) which includes a pupil, a girl, with SEN, trying to find out what they think about the process of adapting the curriculum, how they conceive and implement it. As a methodology of data collection we used different techniques: the interview, the documentary analysis and the naturalistic observation. We concluded that, despite the difficulties that teachers express and demonstrate they assume the need to implement curricular adjustments in relation to pupils with SEN in response to the differences and particularities of each one in order to develop core competencies and to complete compulsory schooling. The Curriculum Adequacies are perceived as very advantageous from the standpoint of promoting educational success for all students and particularly for pupils with SEN, providing the latter the possibility of following the curriculum closer than usual, feeling as "equal" to their schoolmates, improving their self-esteem, self- confidence and motivation.

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Enquadramento – A reforma dos Cuidados de Saúde Primários (CSP) é um facto irreversível. Uma “onda” de reforma percorre igualmente grande parte dos países ocidentais exigindo uma reflexão sobre o processo. Objetivo – Descrever a reforma em curso nos CSP e identificar os potenciais factores de sucesso e insucesso dos serviços públicos de cuidados de saúde primários. Metodologia – Análise crítica da literatura. Resultados e conclusões – A eficiência, eficácia e equidade de acesso aos cuidados de saúde são insuficientes. Mudanças organizacionais estão a ser operadas alterando as relações e a cooperação inter‑profissional e inter‑organizacional. É evidente a tensão que existe entre as partes envolvidas. Novas formas organizacionais estão a ser criadas para garantir a viabilidade das reformas e equilíbrio dos sistemas. O novo modelo organizacional, se pretender garantir a sustentabilidade e a viabilidade dos cuidados primários, deverá assentar num equilíbrio de gestão de recursos e numa estratégia de saúde para todos que não significa saúde para tudo. ABSTRACT: Background – Primary Health Care (PHC) reform is a fact in several countries and is happening also in Portugal demanding a reflection on the process. Aim – To describe the PHC reform and to identify the factors of success or potential failure in PHC public services. Methods – Critical appraisal of the literature. Results and Conclusions – The efficiency, efficacy and access to health care are insufficient. Organizational changes are taking place altering inter‑professional and inter‑organizational cooperation and relationship. Tension among the parts involved is evident. New organizational models are being created to secure the sustainability of the reforms and the systems. The new models should provide a balanced management of the available resources, in a strategy of health for all that doesn’t mean health for everything.

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No centro desta reflexão teórica situa-se a conjuntura sociopolítica que fez (re)emergir o 1.º ciclo do ensino básico como “problema” de política educativa, ou seja, como terreno prioritário para o Estado, através do Governo, formular e executar um “modelo” de operacionalização da política de “Escola a Tempo Inteiro” (ETI). Analisamos esta política reportando-a a referenciais de representação de um “novo modelo educativo” (dimensão educativa), de um “novo paradigma de escola pública” (dimensão política) e de uma “nova conceção de administração da educação” (dimensão administrativa). O recurso ao quadro heurístico da “análise das políticas públicas” permite pôr em evidência as representações e a ação governativas. At the centre of this theoretical reflection is the socio-political conjuncture that (re)emerged the 1st. cycle of basic education as an education policy “problem”, that is to say, a priority ground to the State, through the Government, create and implement an operational “model” for “full-time school” policy. We analyse this policy by referring to the referential representation of a “new educational model” (educational dimension), a “new paradigm of public school” (political dimension) and a “new conception of educational administration” (administrative dimension). The use of the heuristic framework of “public policy analysis” allows us to highlight the representations and governmental action.