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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
271

Sol traités aux liants : performances hydro-mécaniques et hygro-thermiques : application en BTP / Soils treated with binders‎ : hydro-mechanical and hygro-thermal performances : applications in building and civil engineering works

Hibouche, Akli 25 October 2013 (has links)
ALa terre crue est l’un des principaux matériaux de construction utilisés depuis les temps les plus reculés. C’est un matériau abondant, qui nécessite très peu d'énergie pour sa fabrication et qui ne génère pas de déchets. Construire aujourd’hui avec des matériaux à base de terre crue nécessite de ces derniers des performances mécaniques remarquables. Pour atteindre ces performances, le traitement des sols aux liants est l’une des techniques utilisées pour améliorer la résistance mécanique et la durabilité de ces matériaux. On s’intéresse dans cette thèse à l’étude de la terre crue traitée aux liants pour deux applications différentes : un remblai expérimental pour une application en travaux publics (conception innovante de digue par l’utilisation de matériaux obtenus via un traitement à la chaux) et un béton de terre dénommé « Cématerre » pour une application en bâtiment (éléments structuraux et cloisons présentant de bonnes performances hygro-thermiques). Dans les deux cas, le but est de caractériser, et éventuellement d’améliorer, la résistance mécanique, la rigidité, les caractéristiques hydriques et hydrauliques, ainsi que les propriétés hygro-thermiques. Concernant le béton de terre « Cématerre », les études préliminaires menées selon un protocole expérimental établi conformément au cahier des charges du CSTB, ont permis sa qualification, matérialisée par l’obtention d’une ATEx A. La phase suivante a consisté à améliorer sa formulation avec comme objectif l’amélioration de la résistance mécanique du matériau. Les plans d’expériences utilisés ont permis d’établir des modèles de formulations ciblant les résistances mécaniques recherchées. L’étude du comportement hygro-thermique du béton de terre est abordé en analysant les transferts couplés de chaleur et d’humidité. Pour cela un certain nombre de paramètres hygro-thermiques du matériau Cématerre ont été déterminés au laboratoire. La mesure de ces paramètres a permis la réalisation de simulations hygro-thermiques dynamiques qui ont mis en évidence l’intérêt de ce matériau par rapport au béton « classique ». Concernant le limon traité à la chaux et compacté, les résultats ont montré que le module en petites déformations E augmente avec la contrainte de confinement et l’âge du matériau et décroit légèrement avec le niveau de déformation dans le domaine des contraintes testées. Une loi de type E = ßo1m décrit la variation du module, β et m étant des paramètres fonctions de l’âge et du niveau du déviateur. Par ailleurs, les coefficients de perméabilité saturée et non saturée n’évoluent pas avec le temps de cure. Le fluage volumique ne semble pas non plus être influencé par le temps de cure, autrement dit, l’augmentation de la rigidité du matériau liée au développement des réactions pouzollaniques n’a pas empêché le matériau de fluer autant à 28 jours qu’après un an de temps de cure. / AEarthen construction is one of the most common construction technique used since the earliest times. The raw material is abundant, requires very little energy to manufacture, and does not generate waste. Building today with raw materials made from the earth requires outstanding mechanical performance from such non-fired materials. To achieve this performance, the treatment of the soil with binders is one of the techniques used to improve the strength and durability of these materials. The aim of the present PhD dissertation is to study the treated soils with binders for two different applications: an experimental compacted embankment for application in public works ( a dam innovative design, through the use of materials obtained by treatment with lime ) and earthen concrete called " Cematerre " for application in building ( walls and structural elements with good hygrothermal performance). In both cases, the goal is to characterize and possibly improve the mechanical strength, stiffness, hydric and hydraulic characteristics and the hygrothermal properties. For the earthen concrete " Cematerre ", the preliminary studies according to an experimental protocol under CSTB specifications have led to the so-called “ATEx A” official qualification. The next phase was to improve the formulation with the aim of improving the mechanical strength of the material. The design of experiments has been used to establish models formulations targeting the sought strength. The study of hygrothermal behavior of earthen concrete is addressed by analyzing the coupled transfer phenomenon of heat and moisture. Hygrothermal parameters were determined in the laboratory. The measurement of these parameters has allowed the realization of dynamic thermal simulations that have highlighted the benefit of this material when compared with standard concrete. For silt treated with lime and compacted, the results showed that the small strain modulus E increases with the confining stress and the curing time and decreases slightly with the strain level in the range of stress tested. A power law E = ßo1m describes the variation of the modulus, β and m are functions of the curing time and the strain level. Moreover, the coefficients of saturated and unsaturated permeability do not change with the curing time. The volumetric creep does not appear to be influenced by the curing time, i.e. , the increase in stiffness due to the development of pozzolanic reactions did not prevent the material from creeping as much after 28 days as after a year of curing time.
272

Modelo de sazonalização da energia assegurada de usinas hidrelétricas utilizando algoritmos genéticos. / Model to alocate the assured energy of hydro power plants using genetic algorithms.

Sokei, Cristiane Toma 05 September 2008 (has links)
A receita operacional de uma empresa de geração predominantemente hidrelétrica é composta de duas parcelas: a comercialização de seus contratos de energia e a liquidação na Câmara de Comercialização de Energia (CCEE). A parcela de receita de contratos é previsível, mas a receita proveniente da liquidação da CCEE é de difícil mensuração porque depende das alocações do Mecanismo de Realocação de Energia (MRE) e do Preço de Liquidação das Diferenças (PLD). O trabalho apresenta os conceitos gerais dos componentes que influenciam a receita do mercado de curto prazo e um modelo para sazonalização da energia assegurada que é um dos fatores determinantes para a alocação de MRE e para a liquidação das diferenças. O modelo foi detalhado e implementado em uma ferramenta computacional utilizando Algorítmos Genéticos para a minimização da perda esperada e do risco com a sazonalização. / The operating revenue of power generation companies has two different components: revenues arising from power purchase agreements and from spot market, managed by the Câmara de Comercialização de Energia - CCEE The income of contracts is predictable, but there are a lot of difficulties to do prognosis with the spot market revenue component, because it depends on both the Energy Reallocation Mechanism (MRE) and the spot price (PLD). This text presents the influences of some components in spot market incomes and a model to alocate the assured energy along the year since this is the main factor influencing the MRE and the spot market revenues. The model was formulated and implemented in a computational tool using Genetic Algorithms (AG) to minimize the expected losses and the sazonal risk.
273

Organosiloxane-Boron Based Liquid Electrolytes for Application in Lithium-Air Batteries

Alzharani, Ahmed A 14 December 2018 (has links)
The synthesis of 2,4,6,8-Tetramethylcyclotetrasiloxane (D4H), and Poly(methylhydrosiloxane) (PMHS) average molecular weight 1700-3200 g/mol, were functionalized with different repeat units of methoxy polyethylene glycol (PEG) (n = 8,12,17). These compounds act as polymer electrolytes with a backbone of siloxane and they were prepared via hydro-silylation reaction to be functionalized with different molecular weights of Ally-PEG. The compounds were confirmed by FT-IR, 1H-NMR and 13C NMR spectroscopy. A hydro-silylation reaction between the functionalized AllyPEG of different molecular weights produced four compounds with a low glass transition temperature that could improve comb like polymer electrolytes conductivity by reducing crystalline phase of PEO. Another way to increase the percentage of the amorphous phase of PEO is to blend it with other polymers. The blending method is considered to be an important method to improve the ionic conductivities and dimensional stability of polymer electrolytes. The main advantages of the blend systems are the simplicity of preparation and the ease to control the physical properties. A high molecular weight of poly 2- vinyl pyridine (Mw=200,000) was added to improve the dimensional stability. Differential scanning calorimetry (DSC) thermal analysis shows that all the blend systems will exhibit an increase in the glass transition temperature by increasing the salt content. The other novel synthesis of polymer electrolytes are triglyme borane and borosilicate. They were synthesized via hydro-boration. These compounds were characterized and confirmed by FT-IR, 1H-NMR 13C NMR spectroscopy. The ionic conductivity of both systems, pure and blend, of different compositions were determined at four temperatures i.e. 25°C, 40°C, 55°C and 70°C. A maximum ionic conductivity value of the siloxane blend is 9.1x10-4 S cm-1 and the pure triglyme borane is 2.14x10-3 S cm-1 at ambient temperature. The ratios of ethylene oxide to lithium salt of siloxane blend and pure triglyme borane were 10:1 and 35:1 respectively. These ratios were the highest conductivity obtained in all the electrolyte systems. The ionic conductivity increases with increasing temperature and salt content to reach optimum concentration. This behavior results in ionic transport, which is supported by the segmental motion of the polymer matrix host.
274

Análise de juntas soldadas por fricção utilizando pinos consumíveis com adição de níquel em chapas de aço com manganês

Buzzatti, Jonas Trento January 2017 (has links)
Os processos de união por soldagem entre peças e componentes metálicos são indispensáveis para nossa realidade tecnológica. O processo de soldagem por fricção com pino consumível conhecido como FHPP (Friction Hydro Pillar Processing) é um processo desenvolvido recentemente que ocorre no estado sólido através da fricção entre dois materiais e, com isso, reúne algumas vantagens sobre os processos convencionais de soldagem por fusão. Esta técnica apresenta grande potencial de aplicação na indústria de óleo e gás visando reparos de trincas e descontinuidades em equipamentos e estruturas de aços em geral. Apesar do grande potencial desta técnica, o estudo sobre a sua aplicação para produzir juntas com materiais dissimilares ainda é escasso se comparado com outras técnicas de soldagem. Desta forma, este trabalho tem como objetivo o desenvolvimento e a análise de juntas soldadas utilizando pinos com adição de níquel em chapas de aço com manganês, visando determinar a combinação entre material de pino e parâmetros de soldagem que forneça a junta com melhores características mecânicas e metalúrgicas. Os parâmetros de soldagem que variaram foram: velocidade de rotação e a força axial. Os materiais utilizados nos conjuntos soldados foram chapas de aço ao manganês, classificadas comercialmente como ASTM A516 grau 70, e barras de aço baixo carbono com adição de 3, 6 e 9% de níquel. A análise realizada sobre as juntas abrangeu a caracterização da microestrutura e das propriedades de dureza das regiões específicas da solda além dos ensaios mecânicos de dobramento, tração com micro-amostras e de tenacidade à fratura através do parâmetro CTOD. Todas as soldas tiveram bom preenchimento, porém alguns materiais de pino não proporcionaram boa ductilidade durante o dobramento. As falhas ocorridas durante o dobramento juntamente com os estudos da tenacidade à fratura na zona de ligação mostraram que o acúmulo de inclusões nesta região representa degradação das propriedades mecânicas localmente. Os ensaios de tração com micro-amostras indicam aumento da resistência mecânica na região do material depositado do pino e os valores de CTOD no material termomecânicamente afetado são significativamente maiores do que na zona de ligação, porém não alcançam os valores obtidos nos materiais como não processados. / The processes of union by welding between parts and metallic components are indispensable for our technological reality. The Friction Hydro Pillar Processing (FHPP) process is a newly developed process that occurs in the solid state through friction between two materials and thus has some advantages over conventional fusion welding processes. This technique presents great potential of application in the oil and gas industry aiming repairs of cracks and discontinuities in equipment and steel structures in general. Despite the great potential of this technique, the study of its application to produce joints with dissimilar materials is still scarce compared to other welding techniques. The aim of this work is the development and analysis of welded joints using rod with nickel addition in steel sheets with manganese, in order to determine the combination of rod material and welding parameters that provides the joint with better mechanical and metallurgical characteristics. The welding parameters that varied were: speed of rotation and axial force. The materials used in the welded assemblies were manganese steel plates, commercially classified as ASTM A516 grade 70, and low carbon steel with addition of 3, 6 and 9% nickel. The analysis of the joints included the characterization of the microstructure and the hardness properties of the specific regions of the weld in addition to the bend test, micro-tensile test and fracture toughness through the parameter CTOD. All welds were well filled, however, some rod materials did not provide good ductility during bend test. The failures during folding together with the fracture toughness studies in the bonding zone showed that the accumulation of inclusions in this region represents degradation of the mechanical properties locally. The micro-tensile test indicate increased mechanical strength in the region of the deposited material of the rod and the values of CTOD in the thermomechanically affected material are significantly higher than in the bonding zone, but do not reach the values obtained in the unprocessed material.
275

Avaliação das propriedades mecânicas e metalúrgicas de juntas soldadas pelo processo de fricção com pino consumível, em aço estrutural de alta resistência classificado como grau R4 pela norma IAC W22

Magalhães, Márcio Medeiros de January 2017 (has links)
Este estudo tem por objetivo avaliar a possibilidade de confeccionar juntas soldadas pelo processo de soldagem por fricção com pino consumível (Friction Hydro Pillar Processing), em aço classificado como grau R4 de acordo com a norma IAC W22. As juntas soldadas foram produzidas com três diferentes forças axiais: 30 kN, 45 kN e 60 kN, e após a soldagem, submetidos a três diferentes tempos de tratamento térmico de revenimento: uma hora, duas horas e quatro horas, na temperatura de 650 C. A microestrutura predominantemente martensítica resultante destes processos, foi caracterizada através de microscopia óptica, e de um mapeamento de microdureza Vickers. As soldas tiveram suas zonas afetadas pelo processo mensuradas através do software de análise de imagens ImageJ, sendo observadas maiores zonas para menores forças axiais empregadas. Caracterizou-se ainda, o nível de tensões residuais oriundos do processo de soldagem através do método de difração de nêutrons, para uma solda produzida com força axial de 45 kN, em duas diferentes condições, no estado de como soldado e com revenimento de quatro horas após a soldagem. Com os resultados obtidos neste trabalho pode-se concluir que as juntas soldadas com a força de 60 kN apresentaram a melhor combinação de propriedades avaliadas, que são, um menor tamanho de zonas afetadas pelo processo, e manteve um bom nível de dureza mesmo após o revenimento. Todas as juntas soldadas apresentaram uma ótima união metalúrgica, e os diferentes tempos de tratamento térmico empregados promoveram alterações microestruturais e nas propriedades do material já esperadas para o tratamento térmico de revenimento. / The aim of this study is to evaluate the possibility of making joints welded by Friction Hydro Pillar Processing, in steel grade R4 according to IAC W22. The repairs were produced with three different axial forces: 30 kN, 45 kN and 60 kN, and after welding, subjected to three different tempering heat treatment times: one hour, two hours and four hours, at a temperature of 650 C. The predominantly martensitic microstructure resulting from these processes was characterized by optical microscopy and a Vickers microhardness mapping. The welds had their zones affected by the process measured through the ImageJ image analysis software, with larger zones being observed for smaller axial forces employed. It was also characterized the level of residual stresses from the welding process, through the neutron diffraction method, for a weld produced with axial force of 45 kN, in two different conditions, as welded and annealing for four hours after welding. With the results obtained in this work it can be concluded that the welded joints with the force of 60 kN presented the best combination of evaluated properties, which are, a smaller size of zones affected by the process, and maintained a good level of hardness even after the annealing. All the welded joints presented an excellent metallurgical bonding, and the different times of thermal treatment employed promoted microstructural changes and in the properties of the material already expected for the heat treatment of annealing.
276

Comportement hydromécanique différé des barrières ouvragées argileuses gonflantes / Hydro-mechanical behaviour of bentonite-sand mixture used as sealing materials in radioactive waste disposal galleries

Saba, Simona 09 December 2013 (has links)
Dans le but de vérifier l'efficacité des dispositifs de scellement ou des barrières ouvragées dans le stockage géologique des déchets radioactifs, l'Institut de Radioprotection et de Sûreté Nucléaire (IRSN) a mis en œuvre le projet expérimental SEALEX (SEALing performance EXperiments) auquel ce travail est étroitement lié. Dans le cadre de ce projet, des essais in-situ sont effectués à l'échelle représentative et dans des conditions naturelles sur un mélange compacté de bentonite et de sable. Ce matériau de mélange a été choisi pour sa faible perméabilité et surtout pour sa capacité de gonflement qui permet de colmater les vides existant dans le système, notamment le vide technologique correspondant au vide radial entre le noyau de scellement et la roche hôte et qui est inévitable au cours de l'installation du noyau dans le forage. Une fois les vides scellés, le gonflement à volume constant engendre une pression de gonflement aussi bien sur la roche hôte (radiale) que sur les structures de confinement en béton (axiale). Le comportement de ce matériau dans ces conditions de couplages hydromécaniques est alors étudié dans ce travail. La microstructure du matériau à son état initial a été premièrement examinée par micro-tomographie rayons-X. Ceci a permis de voir la distribution des grains de bentonite et de sable ainsi que le réseau de pores dans l'échantillon. Des macro-pores se sont retrouvés concentrés à la périphérie de l'échantillon ainsi qu'entre les grains de sable, ce qui pourra affecter à court terme la perméabilité. L'hydratation du même matériau en condition de gonflement limité a été ensuite observée par une photographie 2D et par la micro-tomographie aux rayons-X. Le mécanisme de gonflement par production de gel de bentonite, la cinétique de gonflement, la diminution de densité et l'homogénéisation du matériau final on été analysés. L'hydratation en conditions de gonflement empêché a été aussi étudiée par des essais où la pression de gonflement a été mesurée dans deux directions : radialement et axialement. La différence retrouvée entre les pressions de gonflement axiales et radiales a évoqué la présence d'une anisotropie de microstructure qui a été analysée en fonction de la masse volumique sèche de bentonite dans le mélange. Des essais en modèle réduit reproduisant à une échelle 1/10ème les essais in situ (SEALEX) ont été également effectués afin d'étudier le comportement du noyau compacté après la reprise des vides au cas d'un accident détruisant les éléments de confinement. Des mesures locales de pression de gonflement le long des échantillons ont permis de mettre en évidence l'évolution du gradient de densité durant le gonflement axial. Finalement une comparaison entre les résultats obtenus dans ce travail et ceux d'un essai in situ (SEALEX) a été faite. Une bonne correspondance entre les valeurs d'humidités relatives a été retrouvée pour les mêmes longueurs d'hydratation tout en prenant en compte la saturation par le vide technologique radial. Par contre, la comparaison des évolutions et des valeurs de pressions de gonflement était plus compliquée vu les différences de configurations des essais / In order to verify the effectiveness of the geological high-level radioactive waste disposal, the French Institution of Radiation protection and Nuclear Safety (IRSN) has implemented the SEALEX project to control the long-term performance of swelling clay-based sealing systems, and to which this work is closely related. Within this project, In-situ tests are carried out on compacted bentonite-sand mixture in natural conditions and in a representative scale. This material is one of the most appropriate sealing materials because of its low permeability and good swelling capacity. Once installed, this material will be hydrated by water from the host-rock and start swelling to close all gaps in the system, in particular the internal pores, rock fractures and technological voids. Afterwards, swelling pressure will develop. In the present work, laboratory experiments were performed to investigate the sealing properties under this complex hydro-mechanical conditions taking into consideration the effect of technological voids. The microstructure of the material in its initial state was first examined by microfocus X-ray computed tomography (µCT). This allowed identification of the distribution of grains of sand and bentonite as well as the pores in the sample. Macro-pores are found concentrated at the periphery of the sample and between the grains of sand, which could affect in the short term the permeability. The hydration of the same material in limited swelling conditions was then observed by 2D photography and 3D µCT. The swelling mechanism with bentonite gel production, the swelling kinetics, the density decrease and the homogenisation of the material were analyzed. The hydration in the conditions of prevented swelling was also studied by swelling pressure tests with radial and axial measurements of swelling pressure. The difference found between the axial and radial swelling pressures suggested the presence of an anisotropic microstructure. Mock-up tests at a 1/10 scale of the in situ SEALEX tests were carried out for the study of the recovery capacity of the mixture in case of an accident causing the failure of the confining structures. Local measurements of swelling pressures along the sample allowed analysis of the density gradient evolution during axial swelling. Finally, a comparison between the laboratory results and those from an in-situ test was done, showing a good fitting in the relative humidity curves for the same infiltration length while considering the saturation effect from the technological void. The swelling pressure comparison was more complex because of the different configurations of the tests (existence of technological void in-situ that could affect the kinetics)
277

Análise da dinâmica hídrica nas unidades geológico-geomorfológicas quaternárias (UQ) da Bacia do Rio Guaratuba, Bertioga (SP) / Analysis of the dynamics of Quaternary Geomorphological-Geological units (UQs) in Guaratuba River Basin, Bertioga (SP)

Daniel dos Santos Pereira 19 January 2012 (has links)
Bertioga possui todos os tipos de Unidades Geológicas-Geomorfológicas Quaternárias (UQs) que podem ser encontradas no restante do litoral paulista, encaixados em uma planície costeira de pequenas dimensões. Tendo em vista a escassez de trabalhos que integrem os atributos hidrológicos da paisagem, o objetivo desta pesquisa foi analisar a dinâmica hídrica atmosférica, subterrânea e superficial da Bacia do Rio Guaratuba, tendo como viés a distribuição espacial das UQs, a partir de uma série de monitoramento de 24 meses, entre julho/2009 e agosto/2011. Para tanto foram analisados os seguintes componentes hídricos: (a) atmosféricos - por meio da análise das distribuições de pluviosidade, temperatura e umidade relativa do ar, para a caracterização do balanço hídrico climático (BHC) da bacia; (b) subterrâneos, a partir da variabilidade do nível do lençol freático; (c) superficial por meio da análise morfométrica das UQs. Os resultados foram tratados à luz de análises sinóticas dos sistemas atuantes no período de monitoramento e das séries históricas (décadas de 1960 a 1990) de pluviosidade e temperatura. Foi identificada uma tendência positiva na distribuição das chuvas, da praia para a baixa encosta da Serra do Mar, caracterizando assim o efeito orográfico. Chamou a atenção à ocorrência de invernos bastante úmidos em 2009 e 2010, ao contrário de 2011 e das tendências da série histórica. Neste sentido, não se pode descartar a possibilidade de influência de fenômenos de mesoescala, como o ENOS (El Niño e Oscilação Sul). Entre 2009 e meados de 2010 atuou o El Niño, sucedido pela La Niña, desde junho/2010 até o presente momento (início do decaimento em maio/2011, segundo dados do INPE). Os índices registrados se assemelham aos do ano de 1990, quando também ocorreu elevado volume de chuva durante o inverno e atuava um El Niño de forte intensidade. A temperatura e a umidade relativa do ar variaram de modo mais marcante entre áreas naturais e antropizadas, embora tenham se apresentado relativamente elevadas durante todo o período de monitoramento, quando comparadas às médias para a região. O BHC normal (série histórica) apresentou déficit hídrico apenas em agosto, com todos os outros meses caracterizando excedentes hídricos. Já o BHC sequencial (período de monitoramento) alternou-se entre excedentes hídricos elevados e meses de déficit hídrico, como ocorreu em abril e maio/2010 e maio e junho/2011. Portanto, entre essas duas séries parece ter havido uma migração do período seco, de agosto para abril/junho. Na planície costeira os níveis de lençol freático (NA) mais profundos ocorrem nas UQs mais antigas e de topografia mais elevada (terraços marinhos e fluviais pleistocênicos), localizados salvo quando há interferência local do horizonte B espódico, que regula a profundidade do (NA) e pode torná-lo temporariamente mais elevado ou mesmo suspenso. Os mais rasos (aflorantes e subaflorantes) estão nas paleodepressões estuarinas-lagunares holocênicas a atuais, localizadas na porção central da bacia. A oscilação vertical do NA ao longo do tempo apresentou correlação positiva com a variação mensal do BHC sequencial, mostrando que o sistema está em relativo equilíbrio. / Bertioga has all kinds of Quaternary Geomorphological-Geological units (UQs) that can be found in the rest of the coast paulista, embedded in a small coastal plain. Given the paucity of studies that incorporate the attributes of the hydrological landscape, the aim of this study was to analyze the dynamics of atmospheric water, groundwater and surfacewater of the Guaratuba River Basin, with the bias of the spatial distribution UQs from a series of 24 month-monitoring between July/2009 and August/2011. Therefore, were analyzed the following hydrological components: (a) atmospheric - by analyzing the distribution of rainfall, temperature and relative humidity, to characterize the climatic water balance (BHC) basin, (b) underground, from variability of groundwater level, (c) surface by means of morphometric analysis of UQs. The results were treated in the light of analysis of the synoptic systems operating in the rainfall and temperature monitoring period and the time series (the 1960s to 1990s). It was identified a positive trend in the rainfall distribution, from the beach to the low slope of Serra do Mar, characterizing the orographic effect. Attention has been drawn to the occurrence of very wet winters in 2009 and 2010, unlike 2011 and the historical series trends. In this sense, one cannot rule out the influence of mesoscale phenomena such as ENSO (El Niño and Southern Oscillation). Between 2009 and mid-2010 El Niño has happened, followed by La Niña, from June/2010 to the current date (beginning of the decay in May/2011, according to data from INPE). The rates are similar to those from the year 1990, when high rainfall also occurred during the winter and El Niño happened. The temperature and relative humidity ranged from a more marked way between natural and disturbed areas, although they have been performing relatively high throughout the monitoring period, compared to the averages for the region. The BHC normal (series) had only water deficit in August, with every other month featuring over water. Since the BHC sequential (monitoring period) alternated between high water surpluses and months of drought, as occurred in April and May/2010 and May and June/2011. Therefore a migration of the dry period from August to April/ June seems to have happened between these two series. The deeper coastal plain groundwater levels (NA) occur in oldest and with highest topography (Pleistocene marine terraces and river) UQs, located except when there is local spodic B horizon interference, which regulates the depth of the (NA) and can make it higher or temporarily suspended. The shallowest ones (outcrop and under outcrop) are in the lagoon-estuarine paleodepressions the current Holocene, located in the central portion of the basin. The vertical oscillation of the NA over time was positively correlated with the monthly variation of BHC sequence, showing that the system is in relative balance.
278

Modelo de sazonalização da energia assegurada de usinas hidrelétricas utilizando algoritmos genéticos. / Model to alocate the assured energy of hydro power plants using genetic algorithms.

Cristiane Toma Sokei 05 September 2008 (has links)
A receita operacional de uma empresa de geração predominantemente hidrelétrica é composta de duas parcelas: a comercialização de seus contratos de energia e a liquidação na Câmara de Comercialização de Energia (CCEE). A parcela de receita de contratos é previsível, mas a receita proveniente da liquidação da CCEE é de difícil mensuração porque depende das alocações do Mecanismo de Realocação de Energia (MRE) e do Preço de Liquidação das Diferenças (PLD). O trabalho apresenta os conceitos gerais dos componentes que influenciam a receita do mercado de curto prazo e um modelo para sazonalização da energia assegurada que é um dos fatores determinantes para a alocação de MRE e para a liquidação das diferenças. O modelo foi detalhado e implementado em uma ferramenta computacional utilizando Algorítmos Genéticos para a minimização da perda esperada e do risco com a sazonalização. / The operating revenue of power generation companies has two different components: revenues arising from power purchase agreements and from spot market, managed by the Câmara de Comercialização de Energia - CCEE The income of contracts is predictable, but there are a lot of difficulties to do prognosis with the spot market revenue component, because it depends on both the Energy Reallocation Mechanism (MRE) and the spot price (PLD). This text presents the influences of some components in spot market incomes and a model to alocate the assured energy along the year since this is the main factor influencing the MRE and the spot market revenues. The model was formulated and implemented in a computational tool using Genetic Algorithms (AG) to minimize the expected losses and the sazonal risk.
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Análise da dinâmica hídrica nas unidades geológico-geomorfológicas quaternárias (UQ) da Bacia do Rio Guaratuba, Bertioga (SP) / Analysis of the dynamics of Quaternary Geomorphological-Geological units (UQs) in Guaratuba River Basin, Bertioga (SP)

Pereira, Daniel dos Santos 19 January 2012 (has links)
Bertioga possui todos os tipos de Unidades Geológicas-Geomorfológicas Quaternárias (UQs) que podem ser encontradas no restante do litoral paulista, encaixados em uma planície costeira de pequenas dimensões. Tendo em vista a escassez de trabalhos que integrem os atributos hidrológicos da paisagem, o objetivo desta pesquisa foi analisar a dinâmica hídrica atmosférica, subterrânea e superficial da Bacia do Rio Guaratuba, tendo como viés a distribuição espacial das UQs, a partir de uma série de monitoramento de 24 meses, entre julho/2009 e agosto/2011. Para tanto foram analisados os seguintes componentes hídricos: (a) atmosféricos - por meio da análise das distribuições de pluviosidade, temperatura e umidade relativa do ar, para a caracterização do balanço hídrico climático (BHC) da bacia; (b) subterrâneos, a partir da variabilidade do nível do lençol freático; (c) superficial por meio da análise morfométrica das UQs. Os resultados foram tratados à luz de análises sinóticas dos sistemas atuantes no período de monitoramento e das séries históricas (décadas de 1960 a 1990) de pluviosidade e temperatura. Foi identificada uma tendência positiva na distribuição das chuvas, da praia para a baixa encosta da Serra do Mar, caracterizando assim o efeito orográfico. Chamou a atenção à ocorrência de invernos bastante úmidos em 2009 e 2010, ao contrário de 2011 e das tendências da série histórica. Neste sentido, não se pode descartar a possibilidade de influência de fenômenos de mesoescala, como o ENOS (El Niño e Oscilação Sul). Entre 2009 e meados de 2010 atuou o El Niño, sucedido pela La Niña, desde junho/2010 até o presente momento (início do decaimento em maio/2011, segundo dados do INPE). Os índices registrados se assemelham aos do ano de 1990, quando também ocorreu elevado volume de chuva durante o inverno e atuava um El Niño de forte intensidade. A temperatura e a umidade relativa do ar variaram de modo mais marcante entre áreas naturais e antropizadas, embora tenham se apresentado relativamente elevadas durante todo o período de monitoramento, quando comparadas às médias para a região. O BHC normal (série histórica) apresentou déficit hídrico apenas em agosto, com todos os outros meses caracterizando excedentes hídricos. Já o BHC sequencial (período de monitoramento) alternou-se entre excedentes hídricos elevados e meses de déficit hídrico, como ocorreu em abril e maio/2010 e maio e junho/2011. Portanto, entre essas duas séries parece ter havido uma migração do período seco, de agosto para abril/junho. Na planície costeira os níveis de lençol freático (NA) mais profundos ocorrem nas UQs mais antigas e de topografia mais elevada (terraços marinhos e fluviais pleistocênicos), localizados salvo quando há interferência local do horizonte B espódico, que regula a profundidade do (NA) e pode torná-lo temporariamente mais elevado ou mesmo suspenso. Os mais rasos (aflorantes e subaflorantes) estão nas paleodepressões estuarinas-lagunares holocênicas a atuais, localizadas na porção central da bacia. A oscilação vertical do NA ao longo do tempo apresentou correlação positiva com a variação mensal do BHC sequencial, mostrando que o sistema está em relativo equilíbrio. / Bertioga has all kinds of Quaternary Geomorphological-Geological units (UQs) that can be found in the rest of the coast paulista, embedded in a small coastal plain. Given the paucity of studies that incorporate the attributes of the hydrological landscape, the aim of this study was to analyze the dynamics of atmospheric water, groundwater and surfacewater of the Guaratuba River Basin, with the bias of the spatial distribution UQs from a series of 24 month-monitoring between July/2009 and August/2011. Therefore, were analyzed the following hydrological components: (a) atmospheric - by analyzing the distribution of rainfall, temperature and relative humidity, to characterize the climatic water balance (BHC) basin, (b) underground, from variability of groundwater level, (c) surface by means of morphometric analysis of UQs. The results were treated in the light of analysis of the synoptic systems operating in the rainfall and temperature monitoring period and the time series (the 1960s to 1990s). It was identified a positive trend in the rainfall distribution, from the beach to the low slope of Serra do Mar, characterizing the orographic effect. Attention has been drawn to the occurrence of very wet winters in 2009 and 2010, unlike 2011 and the historical series trends. In this sense, one cannot rule out the influence of mesoscale phenomena such as ENSO (El Niño and Southern Oscillation). Between 2009 and mid-2010 El Niño has happened, followed by La Niña, from June/2010 to the current date (beginning of the decay in May/2011, according to data from INPE). The rates are similar to those from the year 1990, when high rainfall also occurred during the winter and El Niño happened. The temperature and relative humidity ranged from a more marked way between natural and disturbed areas, although they have been performing relatively high throughout the monitoring period, compared to the averages for the region. The BHC normal (series) had only water deficit in August, with every other month featuring over water. Since the BHC sequential (monitoring period) alternated between high water surpluses and months of drought, as occurred in April and May/2010 and May and June/2011. Therefore a migration of the dry period from August to April/ June seems to have happened between these two series. The deeper coastal plain groundwater levels (NA) occur in oldest and with highest topography (Pleistocene marine terraces and river) UQs, located except when there is local spodic B horizon interference, which regulates the depth of the (NA) and can make it higher or temporarily suspended. The shallowest ones (outcrop and under outcrop) are in the lagoon-estuarine paleodepressions the current Holocene, located in the central portion of the basin. The vertical oscillation of the NA over time was positively correlated with the monthly variation of BHC sequence, showing that the system is in relative balance.
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Totara Valley micro-hydro development : a thesis presented in partial fulfillment of the requirements for the degree of Master of Applied Science in Renewable Energy Engineering, Massey University, Palmerston North, New Zealand

Donnelly, David Ronald Unknown Date (has links)
This study focuses on the design, construction and operation of a distributed generation system based on micro-hydro technology. The project is sited in the Totara Valley, a small rural community approximately 70km from the Massey University, Turitea campus, Palmerston North. The Massey University Centre for Energy Research (MUCER) has a long history of renewable energy research within the Totara Valley community. This project complements these existing schemes and provides a foundation for future research into distributed generation technologies. The project encompasses the following objectives: - to gain practical experience in the design, engineering and implementation of a distributed generation system in rural New Zealand; - to evaluate contemporary micro-hydro technology and compare the performance of this equipment in a theoretical and practical context; - to identify barriers that hinder the widespread adoption of micro-hydro systems in rural New Zealand; - to develop a spreadsheet based life cycle costing tool. The results from this study demonstrate that economic considerations are the fundamental aspect to be considered when assessing the long-term viability of these projects. The viability of micro-hydro projects are primarily determined by four factors: - the volume and head (height) of water available above the turbine site; - the length and therefore the cost of the pipeline required for transporting water to the turbine; - the legal and administrative costs involved in obtaining a resource consent to maintain access to the water resources; - the prices received and paid for electricity. Considerable charges were payable to the local authority to secure and maintain the right to harness the water resources at this site. This cost contributed considerable risk to the project and creates a significant barrier to establishing similar systems at other sites. The reduction of resource consent charges to levels that fairly reflect the negligible environmental impacts of these projects would encourage the adoption of this technology and deliver benefits to rural New Zealand communities.

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