Methane (CH4) and carbon dioxide (CO2) are two important greenhouse gases. Recent studies have shown that lakes, although they cover a small area of the globe, can be very important natural sources of atmospheric CH4 and CO2. It is therefore important to monitor the fluxes of these gases between lakes and the atmosphere in order to understand the processes that govern the exchange. By using the eddy covariance method for lake flux studies, the resolution in time and in space of the fluxes is increased, which gives more information on the governing processes. Eddy covariance measurements at a Swedish lake revealed a diel cycle in the fluxes of both CH4 and CO2, with higher fluxes during nighttime than daytime. The high nighttime CO2 fluxes could to a large extent be explained with enhanced transfer velocities due to waterside convection. For the diel cycle of CH4 flux it was suggested that waterside convection could enhance the transfer velocity, transport CH4 rich water to the surface, as well as trigger ebullition. Simultaneous flux measurements of CH4 and CO2 have been presented using both the eddy covariance method and the floating chambers method of which the latter is the traditional measuring method for lake fluxes. For CO2 the two methods agreed well during some periods but differed considerably during others. Disagreement between the methods might be due to horizontal heterogeneity in partial pressure of CO2 in the lake. The methods agreed better for the CH4 flux measurements. However, it is clear that due to the discontinuous nature of the floating chambers, this method will likely miss important high flux events. The main conclusions of this thesis are: 1) the two gas flux methods are not directly comparable and should be seen as supplementary to each other 2) waterside convection enhances the fluxes of both CH4 and CO2 over the water-air surface. If gas flux measurements are not conducted during nighttime, potential high flux periods might be missed and estimates of the total amount of gas released from lakes to the atmosphere may be biased.

Tout au long de son histoire, le réseau des chambres de commerce et d’industrie s’est révélé être un acteur majeur du soutien aux entreprises et du développement économique de leur territoire. Conscient des profondes mutations de l’environnement des entreprises, il s’est engagé depuis plusieurs années dans un important mouvement de réformes qui a abouti à la loi du 23 juillet 2010 relative aux réseaux consulaires, au commerce, à l’artisanat et aux services. Censée rationaliser le fonctionnement du réseau des chambres de commerce et d’industrie, cette loi est le fruit d’un difficile compromis. La réforme reste « au milieu du gué », avec son lot de difficultés et d’incohérences. A l’heure de la modernisation de l’action publique, il semble que le réseau des chambres de commerce et d’industrie n’a pas souhaité s’attacher davantage à poursuivre plus en avant les concepts de mutualisation ou de fusion. Or, nombre de nos voisins européens ont déjà opté pour une stratégie de regroupement rationnel de ces structures consulaires - chambres de commerce et d’industrie, chambre de métiers et de l’artisanat, chambres d’agriculture - en une seule et unique structure. Par conséquent, la présente thèse s’interroge légitimement sur la pertinence d’une telle réforme en demi-teinte. / Throughout its history, the network of the Chambers of commerce and industry has demonstrated its capacity to support the enterprises and the economic development of territories. Aware of the profound changes of their environment, the Chambers of commerce have been part of an important reforming process for years, completed with the passage of the Act of July 23, 2010 regarding Chambers of Commerce and Industry, Trade, Crafts and Services. Anyhow, the Act of July 23, 2010, expected to be rationalizing the functioning of the Chambers of commerce and industry network, is a compromise borne out of difficult and complex negotiations. The reform remains incomplete, with its share of difficulties and inconsistencies. At the time of the streamlining of global public policies, the fact that the consular network has been unwilling to pay greater attention to the concepts of mutualizing or merger could appear to be detrimental. Indeed, many of our European neighbors have already adopted a rational consolidation strategy of these consular structures - the Chambers of Commerce & Industry, the Chambers of Trades and Crafts and the Chambers of Agriculture - in a single structure. Therefore, it seems fair to question the relevancy of such an unachieved reform.

Les grandes éruptions caldériques sont parmi les phénomènes les plus destructeurs de la Terre, mais les processus à l’origine des grands réservoirs de magma siliceux et pauvre en cristaux qui alimentent ces éruptions ne sont pas bien compris. Le temps de stockage de ces réservoirs dans la croûte supérieure a un intérêt particulier. De longs temps de stockage—jusqu’à 105 ans—ont été estimés en utilisant les temps de repos entre les éruptions et les âges radiométriques des cristaux qui se trouvent dans les produits éruptifs. Par contre, des travaux récents sur la diffusion dans des cristaux suggèrent que les réservoirs qui alimentent même les plus grandes éruptions peuvent se mettre en place pendant une période beaucoup plus courte—101–102 ans. Afin de répondre à cette question, j’ai étudié l’éruption dacitique de Cape Riva de Santorin, Grèce (>10km3, 22 ka). Pendant les 18.000 ans précédant cette éruption, une série de dômes et de coulées dacitiques a été émise, alternant avec des dépôts de ponce dacitique (le complexe de dômes de Therasia). Ces dacites ont des compositions similaires à celle qui a été émise pendant l’éruption de Cape Riva, et ont été décrites précédemment comme des « fuites » provenant du réservoir de Cape Riva pendant sa croissance. Cependant, le magma de Cape Riva est appauvri en éléments incompatibles (tels que K, Zr, La, Ce) par rapport au magma de Therasia, une différence qui apparaît également dans les cristaux de plagioclase. Cette différence ne peut pas être expliquée par des processus peu profonds, tels que la cristallisation fractionnée ou l’assimilation de la croûte, ce qui suggère que les magmas de Cape Riva et Therasia ont des origines différentes. En outre, il existe des arguments tendant à montrer que les dacites de Therasia n’ont pas été alimentées par un réservoir majoritairement liquide ayant eu une longue durée de vie. Il y a des variations non systématiques dans la composition du magma, les compostions des bords ainsi que les caractéristiques des cristaux de plagioclase tout au long de la séquence. De plus, les temps de résidence à haute température des cristaux de plagioclase et d’orthopyroxène estimés par des modèles de diffusion sont 101–102 ans. Ces temps sont courts par rapport au temps moyen entre éruptions (1.500 ans), ce qui suggère que les cristaux observés dans chaque coulée ne se sont formés que peu de temps avant l’éruption. Les différentes teneurs en éléments incompatibles indiquent qu’un nouveau magma s’est mis en place dans le système volcanique superficiel peu de temps avant l’éruption de Cape Riva. Cet apport de magma a eu lieu après la dernière éruption de Therasia, qui s’est produite <2.800±1.400 ans avant l’éruption de Cape Riva selon les âges 40Ar/39Ar. Les périphéries des cristaux de plagioclase présents dans la dacite de Cape Riva sont en équilibre avec une rhyodacite, avec une composition similaire à celui du verre de l’éruption. Cependant, les zonations dans les éléments majeurs et traces enregistrent des changements dans la composition du liquide magmatique pendant la croissance des cristaux. La composition du centre de la plupart des cristaux de plagioclase est la même que celle des bords ; toutefois ces cristaux sont souvent partiellement résorbés, et la croissance a repris avec du plagioclase plus calcique. Ces cycles se répètent jusqu’à trois fois. La relation étroite entre la teneur en anorthite, Sr et Ti des différentes zones suggère que la composition des plagioclases est corrélé avec la composition du liquide, allant de liquides dacitiques à rhyodacitiques. Des cristaux d’orthopyroxène révèlent une séquence similaire. Les motifs de zonation sont interprétés comme un témoin de la formation du réservoir de Cape Riva dans la croûte supérieure par le mélange de plusieurs magmas ayant des compositions diverses. Des modèles de diffusion de Mg dans le plagioclase et de Fe–Mg dans l’orthopyroxène suggèrent que ce mélange a eu lieu 101–102 ans avant l’éruption. / Large, explosive, caldera-forming eruptions are amongst the most destructive phenomena on the planet, but the processes that allow the large bodies of crystal-poor silicic magma that feed them to assemble in the shallow crust are still poorly understood. Of particular interest is the timescales over which these reservoirs exist prior to eruption. Long storage times—up to 105 y—have previously been estimated using the repose times between eruptions and radiometric dating of crystals found within the eruptive products. However, more recent work modelling diffusion within single crystals has been used to argue that the reservoirs that feed even the largest eruptions are assembled over much shorter periods—101–102 y. In order to address this question, I studied the >10km3, 22-ka, dacitic Cape Riva eruption of Santorini, Greece. Over the 18 ky preceding the Cape Riva eruption a series of dacitic lava dome and coulées were erupted, and these lavas are interspersed with occasional dacitic pumice fall deposits (the Therasia dome complex). These dacites have similar major element contents to the dacite that was erupted during the Cape Riva eruption, and have previously been described as “precursory leaks” from the growing Cape Riva magma reservoir. However, the Cape Riva magma is depleted in incompatible elements (such as K, Zr, La, Ce) relative to the Therasia magma, as are the plagioclase crystals in the respective magmas. This difference cannot be explained using shallow processes such as fractional crystallisation or crustal assimilation, which suggests that the Cape Riva and Therasia magmas are separate batches. Furthermore, there is evidence that the Therasia dacites were not fed from a long-lived, melt-dominated reservoir. There are non-systematic variations in melt composition, plagioclase rim compositions, and plagioclase textures throughout the sequence. In addition, high-temperature residence times of plagioclase and orthopyroxene crystals from the Therasia dacites estimated using diffusion chronometry are 101–102 y. This is short compared to the average time between eruptions (1,500 y), which suggests the crystals in each lava grew only shortly before eruption. The different incompatible element contents of the Cape Riva and Therasia magmas and plagioclase crystals suggest that a new batch of incompatible-depleted silicic magma arrived in the shallow volcanic plumbing system shortly before the Cape Riva eruption. This influx must have taken place after the last Therasia eruption, which 40Ar/39Ar dates show occurred less than 2,800±1,400 years before the Cape Riva eruption. The rims of the plagioclase crystals found in the Cape Riva dacite are in equilibrium with a rhyodacite, with a similar composition to the Cape Riva glass. However, the major and trace element zoning patterns of the crystals record variations in the melt composition during their growth. The compositions at the centre of most crystals are the same as the rims; however, these crystals are often partially resorbed and overgrown by more calcic plagioclase. The plagioclase then grades normally back to rim compositions. This cycle is repeated up to three times. The tight relationships between the anorthite, Sr and Ti contents of the different zones suggests that the composition of the plagioclase crystals correlates with the composition of the melt from which theygrew. The different plagioclase compositions correspond to dacitic and rhyodacitic melt compositions. The orthopyroxene crystals reveal a similar sequence, although they only record one cycle. These zoning patterns are interpreted to document the assembly of the Cape Riva reservoir in the shallow crust through the amalgamation of multiple batches of compositionally diverse magma. Models of magnesium diffusion in plagioclase and Fe–Mg interdiffusion in orthopyroxene suggest that this amalgamation took place within 101–102 y of the Cape Riva eruption.

O objetivo deste trabalho foi estabelecer uma metodologia de calibração em termos de dose absorvida na água para câmaras de ionização de placas paralelas a serem utilizadas em feixes de radiação X de energia baixa (10 kV a 100 kV) para fins terapêuticos. Atualmente, no Brasil nenhum laboratório de calibração está oferecendo este tipo de serviço. Para o estabelecimento desta metodologia de calibração foram utilizadas duas câmaras de ionização PTW modelos 23344. Ambas as câmaras foram caracterizadas e testadas qualitativamente segundo recomendações de normas internacionais. Os testes de caracterização realizados foram: a medição da taxa de dose mínima efetiva, a curva de saturação, a eficiência da coleção de íons, a resposta quanto ao efeito da polaridade e a linearidade da câmara com a resposta. Os testes de controle de qualidade aplicados foram: estabilidade em curto e longo prazos, fuga de corrente sem irradiação, fuga de corrente após-irradiação e tempo de estabilização. Para a implantação da metodologia, foram estabelecidas as qualidades de radiação de T-10 a T-100, seguindo as recomendações do código de prática da AIEA. Desta forma, foi possível determinar a grandeza de referência, dose absorvida na água, utilizando-se as duas câmaras de ionizações e em todas as qualidades estabelecidas. / The objective of this study was to establish a calibration methodology in terms of absorbed dose to water for parallel plate ionization chambers to be used in low energy X rays beams (10kV to 100kV) for therapy purposes. Currently, in Brazil no calibration laboratory is offering this type of service. In order to establish this calibration methodology was used two ionization chambers PTW models 23344. Both chambers were characterized and tested qualitatively according to recommendations of international standards. The characterization tests performed were: measuring the effective minimum dose rate, the saturation curve, the efficiency of ions collection, polarity effect and the linearity of the ionization chamber with the response. The quality control tests applied were: stability in the short and long term, leakage current without irradiation, leakage current after irradiation and settling time. For the implementation of the methodology, the radiation qualities the T- 10 to T-100 were established, following the recommendations of the IAEA code of practice. Thus, it was possible to determine the magnitude of reference absorbed dose in water, using the two ionization chambers in the all established qualities.

O uso de Tomografia Computadorizada (CT) para procedimentos de imagiologia vem crescendo cada vez mais devido aos avanços da tecnologia dos equipamentos de CT, que permitem a obtenção de imagens com melhor resolução do que por outras técnicas, sendo consequentemente responsável pelo aumento da dose de radiação no paciente durante o procedimento. Isso acarretou uma maior preocupação com as doses recebidas pelos pacientes que se submetem a esse tipo de exame. Para a realização da dosimetria de feixes de CT, o instrumento mais utilizado é a câmara de ionização do tipo lápis, pois este dosímetro apresenta uma resposta uniforme ao feixe de radiação incidente em todos os ângulos. A câmara convencional que se encontra disponível no mercado apresenta um comprimento de volume sensível de 10 cm; entretanto, alguns estudos têm mostrado que esse dosímetro tem subestimado os valores de dose. Portanto, neste trabalho optou-se por desenvolver no Laboratório de Calibração de Instrumentos do Instituto de Pesquisas Energéticas e Nucleares (LCI-IPEN/CNEN) duas câmaras de ionização, fazendo uso de materiais nacionais de baixo custo, com comprimentos de volume sensível de 10 cm e 30 cm. A caracterização destas câmaras foi realizada e os resultados se apresentaram dentro dos limites recomendáveis internacionais. Como uma aplicação, as câmaras desenvolvidas, juntamente com uma câmara comercial, foram testadas em um tomógrafo clínico. As câmaras de ionização desenvolvidas foram analisadas de maneira completa, para os seus possíveis usos. / The use of computed tomography (CT) for imaging procedures is growing due to advances in the CT equipment technology, because they allow the obtention of images with better resolution than through other techniques. Therefore, they are responsible for increasing the dose radiation of patients during the procedure. This fact led to a greater concern about the doses received by patients who undergo this type of examination. To perform the dosimetry in CT beams, the most widely used instrument is the pencil type ionization chamber, because this dosimeter has a uniform response to the incident radiation beam for all angles. The conventional ionization chamber, which is available on the market, has a sensitive volume length of 10 cm; however, some studies have shown that this dosimeter has underestimated the dose values. Therefore, in this study two ionization chambers with sensitive volume lengths of 10 cm and 30 cm, making use of low cost national materials, were developed at the Calibration Laboratory of Instruments (LCI-IPEN/CNEN). The characterization of these chambers was performed, and the results were obtained within the international recommended limits. As an application, the developed ionization chambers and a commercial chamber were tested in a clinical tomographer. The developed ionization chambers were analyzed in a complete way for their possible uses.

Os equipamentos de radiação X, por estarem ligados à rede elétrica, podem apresentar flutuações na intensidade de seus feixes de radiação. Essas variações na intensidade, podem, por sua vez, modificar a taxa de kerma no ar produzida por este feixe de radiação. Em um laboratório de calibração de instrumentos, onde são realizadas calibrações de diversos equipamentos detectores de radiação, utilizados principalmente em clínicas ou hospitais, essa possível variação na intensidade do feixe de radiação pode causar um erro na determinação da dose absorvida. As câmaras de ionização monitoras são utilizadas para verificar a constância da intensidade de feixes de radiação, e fornecer uma correção para possíveis oscilações. Neste trabalho foram projetadas, construídas e caracterizadas câmaras de ionização monitoras para feixes de radiação X. As câmaras de ionização desenvolvidas possuem formato inovador, anelar, com eletrodos de alumínio ou de grafite. Essas câmaras de ionização anelares apresentam a vantagem de não interferirem no feixe direto de radiação. Foi ainda construída uma câmara de ionização com volume duplo e eletrodos de grafite, similar à câmara de ionização monitora comercial utilizada no Laboratório de Calibração de Instrumentos do Instituto de Pesquisas Energéticas e Nucleares. Essas câmaras de ionização foram testadas em diversos feixes de radiação padronizados e seus desempenhos foram comparados aos de câmaras de ionização comerciais. Os resultados obtidos mostram que duas dentre as quatro câmaras de ionização desenvolvidas apresentaram desempenho comparável ao das câmaras de ionização comerciais testadas. Além de apresentarem bons resultados, as câmaras de ionização desenvolvidas foram feitas artesanalmente e utilizando materiais de baixo custo, que são facilmente encontrados no mercado. / X radiation equipment may show fluctuations in the radiation beam intensity, as they are connected to the power net. These intensity variations can, in turn, modify the air kerma rate produced by this radiation beam. In a calibration laboratory, where radiation detectors (from clinics and hospital services) are calibrated, variations in the radiation beam intensity may cause an error in the absorbed dose determination. The monitor ionization chambers are used to verify the radiation beam intensity constancy, and to provide a correction for possible fluctuations. In this work, monitor ionization chambers for X radiation beams were designed, assembled and characterized. The developed ionization chambers have an innovative design, ring-shaped, with aluminium or graphite electrodes. These ring-shaped ionization chambers have the advantage of not interfering in the direct radiation beams. A double-volume ionization chamber with graphite electrodes was also developed. This ionization chamber is similar to the commercial monitor ionization chamber used in the Calibration Laboratory of the Instituto de Pesquisas Energéticas e Nucleares. All developed ionization chambers were tested in several standardized radiation beams and their performances were compared with those of commercial ionization chambers. The results show that two of the four ionization chambers developed showed performance comparable to that of the commercial ionization chambers tested. Besides presenting good results, the ionization chambers were designed and manufactured using low cost materials, which are easily found on the Brazilian market.

The aim of this thesis was to understand and illuminate how readingpromotion projects can be carried out, what sort of activities they mightcontain and what sort of lasting impressions they might make. We choseto examine reading promotion projects because we consider thepromotion of reading and literacy a vital and important part of thelibraries work. The study took place at the city library of Uddevalla andthe projects included in the study were all directed towards children andyouth.The theory used in the thesis was Aidan Chambers’s model of theReading Circle which consists of the four themes of selection,‘reading’, response and the enabling adult. Methods used were semistructuredinterview, document studies and observation.The results show that reading promotion projects benefit from cooperationbetween the adults involved and that education of the adultsin order to indirectly target the children is an effective way of spreadingthe love of reading. Involving children and youth in the work anddecision making process proved to be prosperous.The conclusions are that reading promotion projects give the librarieseconomic and creative resources to try out new ways of working andcooperating. With these tools and the aim to spread the love of readingthe librarians have an increased possibility to reach out and providesupport and inspiration to all becoming readers. / Program: Bibliotekarie

As câmaras de extrapolação são câmaras de ionização com volume variável e são utilizadas principalmente como detectores de radiação beta. Neste trabalho foram caracterizadas duas câmaras de extrapolação, uma comercial da marca PTW, e uma outra desenvolvida no Laboratório de Calibração do IPEN, para aplicação como sistemas de referência em feixes de mamografia, radiodiagnóstico convencional e radioterapia. Os resultados obtidos nos testes de caracterização da resposta das câmaras de extrapolação: corrente de fuga, estabilidade de curto e médio prazos, determinação das correntes de saturação e das eficiências de coleção de íons, dependência angular e energética, mostram que estas câmaras de extrapolação podem ser utilizadas em dosimetria de feixes de radiação X de energias baixas. Os fatores de transmissão no tecido e os fatores de calibração foram também determinados para todas as qualidades de radiação citadas. Finalmente, foi estabelecido um procedimento de calibração de detectores de radiação em feixes padronizados de radiação X, utilizando as câmaras de extrapolação. / The extrapolation chambers are ionization chambers with variable volume, and they are mainly utilized as beta radiation detectors. In this work two extrapolation chambers were characterized, a commercial PTW extrapolation chamber and another extrapolation chamber developed at the Calibration Laboratory of IPEN, for application as reference systems in mammography, conventional diagnostic radiology and radiotherapy beams. The results obtained from the characterization tests of the chamber response: leakage current, short- and medium terms stability, determination of the saturation currents and the ion collection efficiencies, angular and energy dependence, show that these extrapolation chambers may be utilized for low-energy X radiation beam dosimetry. The transmission factors in tissue and the calibration factors were also determined for all cited radiation qualities. Finally, a procedure was established for calibration of radiation detectors in standard X radiation beams, using the extrapolation chambers.

This study considers the relationship between landscape and the Arcadian funereal imagination in the context of eighteenth century Britain, arguing that the Arcadian landscapes imagined by the British elite were instruments of rituals facilitating the reformation and transformation of socioeconomic, political, and moral structures of the British empire. Drawing upon texts and landscape practices, three case studies are examined: Alexander Pope’s (1688-1744) Twickenham grotto and his descriptive letter to Edward Blount; Sir William Chambers’ (1723-1796) Dissertation on oriental gardening and his design for Kew gardens, Sir John Soane’s (1753-1837) manuscript Crude hints towards an history of my house in LIF and his house-museum in Lincoln’s Inn Fields in London. The landscape itinerary of Pope’s Twickenham villa, in relation to his letter to Blount, suggests that it was structured analogous to the initiatory route of the Eleusinian mysteries as accounted in Pope’s translation of the Odyssey. Noting Pope’s engagement with Freemasonry, associated with the Opposition party, I suggest this implied Odyssean journey not only metaphorically anticipates the restitution of the Stuart dynasty and the reassertion of a political order founded upon aristocratic land ownership, but is also a means by which the ‘initiates’ contest the Enlightenment ideal of a mind of autonomy. In relation to the Burkean sublime, Chambers’ Dissertation, an imaginary travel narrative, is read as a city landscaping theory which aims to shape the morals of British citizens exposed to the erosion of commercial society. Whilst the scenes of luxury in the Chinese gardens imply a double effect of commercial society, the funereal imagery of ‘the surprising,’ built upon the Burkean sublime-effect, is intended as a cure of moral corruption associated with luxury. Stimulated by geological notions (e.g. stratigraphy and catastrophism), Soane’s ruinous text of Crude hints, a mirror of the house-museum as well as the earth, illustrates a parallel between the ‘first principles’ of the movement of the earth and that of the mind, i.e. imagination and signification. The funereal imagination in the text, which itself represents simultaneous creation and destruction, is revealed to be the architect’s construction of an ideal language that can express the being of the nation and the self. This thesis ends with a theoretical discussion of the role of the funereal imagination in eighteenth century landscape and architecture, i.e. how British imperial identity was forged, transmitted, negotiated, and reconstructed constantly within the temporally and spatially extended discursive realm of Arcadian mythology.

No description available.