Made available in DSpace on 2014-12-17T15:03:34Z (GMT). No. of bitstreams: 1 JurandirRMJ_DISSERT.pdf: 1054152 bytes, checksum: 95f074a057b6d2e03d6f4a8700465d95 (MD5) Previous issue date: 2014-03-31 / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior / The aquatic ecosystems can play a role as carbon-dioxide-source or carbon-dioxide-sink systems due to the high predominance of heterotrophic or autotrophic metabolism. The primary production can strongly affect the carbon balance (CO2) through the consumption of carbon dioxide in the photosynthesis, especially in eutrophic environment, acting as a carbon sink. The present study tested the hypothesis that the eutrophic reservoirs in tropical semi-arid region are carbon dioxide-sink systems due to the high primary productivity presented in these systems. Five Brazilian reservoirs from the semi-arid in the northeast region were monitored monthly during four years (2010 to 2013) with a prolonged drought event identified during the study. The results showed an increasing level of eutrophication over the period of prolonged drought, with the predominance of autotrophy. Significant negative correlations were observed between the partial pressure of CO2 (pCO2) (p<0,001) and chlorophyll-a in the Boqueir?o, Passagem das Tra?ras, Dourado and Gargalheiras reservoirs, showing a pattern of the carbon dioxide-sink systems. However, this pattern was not found in Cruzeta reservoir. In summary, in the tropical semi-arid region, hydrological and morphometric variables can lead to different behaviors of the water-supply reservoirs on the carbon metabolism. The eutrophic reservoirs evaluated showed a negative relationship between pCO2 and Chl-a, which suggests that these water bodies show an autotrophic metabolism and behave as carbon dioxide- sink systems / Os ecossistemas aqu?ticos podem atuar como emissores ou sequestradores de carbono em fun??o da predomin?ncia do metabolismo heterotr?fico ou autotr?fico. A produ??o prim?ria pode afetar fortemente o balan?o de carbono (CO2) atrav?s do consumo de di?xido de carbono na fotoss?ntese, especialmente em ambiente eutr?ficos, atuando como sumidouros. O presente estudo testou a hip?tese de que reservat?rios eutrofizados da regi?o tropical semi?rida s?o sequestradores de CO2 em fun??o da alta produtividade evidenciada nesses sistemas. Cinco reservat?rios da regi?o semi?rida do nordeste do Brasil foram monitorados mensalmente durante o per?odo de 2010 ? 2013, com um evento de seca prolongada identificado durante o estudo. Os resultados mostraram um crescente n?vel de eutrofiza??o ao longo do per?odo de seca prolongada com predomin?ncia de autotrofia. Foram observadas correla??es negativas significativas entre a press?o parcial de CO2 (pCO2) (p<0,001) e clorofila-a nos reservat?rios Boqueir?o, Passagem das Tra?ras, Dourado e Gargalheiras, evidenciando um padr?o de sequestro de CO2 desses sistemas. Por?m, este padr?o n?o foi encontrado no reservat?rio Cruzeta. Em s?ntese, na regi?o semi?rida tropical, as vari?veis hidrol?gicas e morfom?tricas podem direcionar diferentes comportamentos dos reservat?rios de abastecimento no metabolismo do carbono. Os reservat?rios eutrofizados avaliados apresentaram uma rela??o negativa entre pCO2 e Chl-a o que sugere que estes corpos h?dricos evidenciam um metabolismo autotr?fico e se comportam como sequestradores de CO2

VILLELA, FRANCO N. J. Análise decadal do fluxo de CO2 entre o oceano e a atmosfera na passagem de Drake, Oceano Austral. 2011. 148 f. Dissertação (mestrado) Programa de Pós-Graduação em Ciência Ambiental (PROCAM), Universidade de São Paulo, São Paulo, 2011. Para a área delimitada pelos paralelos 60ºS e 62,5ºS e pelos meridianos 60ºW e 65ºW, localizada no sul da Passagem de Drake, no Oceano Austral, próximo à Península Antártica, foram calculadas as distribuições médias de 2000 a 2009, sazonais e anual, do fluxo de CO2 na interface oceano-atmosfera e de suas variáveis associadas: a pressão parcial de CO2 na superfície marinha (PCO2sw), a pressão parcial de CO2 na atmosfera (PCO2ar), a diferença da pressão parcial de CO2 entre o oceano e a atmosfera (PCO2) e a taxa de transferência gasosa (TR), que é produto do coeficiente solubilidade do CO2 na água do mar pela velocidade de transferência gasosa. A parametrização utilizada no cálculo dos fluxos foi a de Takahashi et al. (2009) com TR dependente da velocidade do vento ao quadrado multiplicada por um fator de escala 0,26. A área de estudo tem cerca de 75 mil km2 e foi dividida em uma grade espacial de 0,5º x 0,5º, resultando em 50 quadrículas. Foram utilizados mais de 46 mil medições de PCO2sw, que na média espacial variou de 362,7 ±11,2 a 371,9 ±17,5 µatm, no verão e primavera respectivamente. A PCO2 variou de -0,4 a 5,7 µatm no outono e primavera, respectivamente. A TR variou de 0,065 ±0,04 a 0,088 ±0,002 gC.mês-1.m-2.µatm-1, no verão e inverno, respectivamente. O fluxo líquido, se tomando a concentração de gelo como negligenciável, variou de -0,039 ±0,865 a 0,456 ±1,221 gC.m-2.mês-1, no outono e inverno, respectivamente. O fluxo total anual de carbono, estimado através da média espacial por quadrícula, foi de 95 GgC.ano-1. Dessa maneira, na estimativa anual, a superfície do mar se comporta como fonte de CO2 para a atmosfera, principalmente devido à região da plataforma continental com PCO2sw consideravelmente maior que o da atmosfera. Sazonalmente sugere-se que no verão a maior disponibilidade de radiação solar, a temperatura da superfície do mar (TSM) mais elevada e os ventos mais fracos favorecem a produção de biomassa fitoplanctônica, fazendo com que a bomba biológica seja o processo dominante na diminuição da PCO2sw e na absorção de CO2 atmosférico pela superfície marinha. Já no inverno, os ventos se intensificam e, associados com o forte resfriamento da TSM, promovem a mistura com águas profundas ricas em carbono inorgânico dissolvido, levando a superfície marinha a um estado de supersaturação de CO2 em relação à atmosfera. Ventos circumpolares de oeste mais intensos e deslocados para sul tem sido apontados como a causa do aumento da PCO2sw em igual ou maior taxa do que ocorre na atmosfera. Na área de estudo foi levantada uma tendência média da intensidade do vento de 0,23 ±0,03 m.s-1.década-1 e um aumento na freqüência da componente zonal de oeste (positiva) de 1,47 ± 1,13 % .década-1. Sugere-se que estas tendências estejam relacionadas com o Modo Anular Austral (SAM). Entretanto, a tendência decadal estimada para a PCO2sw foi menor que para a atmosfera, apesar de ambas indicarem tendência de aumento. Acredita-se que a grande variabilidade e distribuição esparsa de dados tenham mascarado a magnitude da estimativa da tendência de PCO2sw. / VILLELA, FRANCO N. J. Decadal analysis of the CO2 sea-air flux in the Drake Passage, Southern Ocean 2011. 148 f. Dissertação (mestrado) Programa de Pós-Graduação em Ciência Ambiental (PROCAM), Universidade de São Paulo, São Paulo, 2011. For the area bounded by parallels 60°S and 62.5°S and meridians 60°W and 65°W, located in the southern Drake Passage in the Southern Ocean, near the Antarctic Peninsula, mean seasonal and annual distributions of CO2 flux at the ocean-atmosphere interface, from 2000 to 2009, have been computed, as well as their associated variables: the CO2 partial pressure at sea surface (PCO2sw), the CO2 partial pressure in atmosphere (PCO2ar), the CO2 pressure difference between ocean and atmosphere (PCO2), and the gas transfer rate (TR), which is the product of the CO2 solubility coefficient in sea water by the gas transfer velocity. The parameterization used to calculate fluxes was that of Takahashi et al. (2009) with TR depending on the squared wind speed multiplied by a scale factor 0.26. The study area has about 75,000 km2 and was divided into a grid of 0.5° x 0.5°, resulting in 50 area boxes. Over 46,000 PCO2sw measurements were used, which in the spatial mean varied from 362.7±11.2 to 371.9±17.5 µatm, in summer and spring, respectively. The PCO2 varied from 0.4 to 5.7 µatm in autumn and spring, respectively. TR varied from 0.065±0.04 to 0,088±0.002 gC.month-1.m-2.µatm-1, in summer and winter, respectively. The net flux, taking ice concentration as negligible, varied from 0.039±0.865 to 0.456±1.221 gC.month-1.m-2, in autumn and winter, respectively. The total annual carbon flux, estimated through the spatial mean per square, was 95 GgC.y-1. Thus, in the annual estimate the region acts as a source to the atmosphere, mainly due to the continental shelf having PCO2sw considerably greater than that of the atmosphere. Seasonally, it is suggested that in summer the greater availability of solar radiation, warmer sea surface temperature (SST), and weaker winds favor the production of phytoplanktonic mass, making the biological pump the dominating process in lowering the PCO2sw and the absorption of atmospheric CO2 by the sea surface. On the other hand, in winter winds intensify and, in association with the strong cooling of the SST, promote mixing with deep waters rich in dissolved inorganic carbon, leading the sea surface to a state of supersaturation in CO2 relative to the atmosphere. Stronger circumpolar west winds and displaced to the south have been pointed as the cause for the increase of PCO2sw at a rate equal to or greater than that occurring in the atmosphere. In the study area it has been detected a mean trend of wind intensity 0.23±0.03 m.s-1.decade-1 and an increase in the western zonal component of 1.47±1.3%.decade-1. It is suggested that these trends are related to the Southern Annular Mode (SAM). However, the decadal trend estimated for the PCO2sw was smaller than for the atmosphere, in spite of both indicating increasing tendencies. It is believed that the great variability and scatter distribution of the data have masked the magnitude of the PCO2SW trend estimate.

Bakgrund: Hjärnskakning är en vanlig diagnos och vissa patienter upplever att fysisk ansträngning utlöser symtom lång tid efter hjärnskakningen. En förändring i reglering av cerebralt blodflöde (CBF) har visats vara en potentiell orsak bakom detta. Konditionsträning under tröskeln för symtomexacerbation kan förkorta återhämtningstiden för patienterna. På Neurorehab vid Norrlands universitetsjukhus i Umeå identifieras tröskeln med ett stegrat arbetsprov på ergometercykel. Det finns inte någon studie där transkraniell doppler (TCD) använts för att mäta förändringar i cerebralt blodflöde (CBF) under detta arbetsprov. Syfte: Att undersöka genomförbarhet och klinisk relevans av att använda TCD för mätning av blodflödeshastighet i arteria cerebri media (ACMh), hos friska män, under stegrat arbetsprov. Metod: Sex friska och regelbundet aktiva män genomförde ett stegrat arbetsprov på ergometercykel under samtidig mätning av hjärtfrekvens, blodtryck, partialtryck end-tidal CO2 (PetCO2) och blodflödeshastighet i arteria cerebri media (ACMh, mätt med TCD). Smärta från TCD-utrustning och upplevd ansträngning skattades. Tidsåtgången för TCD-tillägget samt eventuell signalförlust noterades. Resultat: Fem studiedeltagare rapporterade ökad smärta (huvudvärk), skattad med Borg CR10 skala, från TCD-utrustningen. Total tidsåtgång för TCD-tillägget var 7 minuter och 40 sekunder i median (IQR, 5 minuter och 32 sekunder). Signalförlust uppstod för en studiedeltagare på vänster sida. PetCO2 och ACMh följdes åt under arbetsprovet bortsett från avvikelser vid två tillfällen. Slutsatser: Studien visar att mätning av ACMh med TCD är genomförbart och ger relevant information om hur CBF ter sig under genomförandet av stegrat arbetsprov. TCD-utrustningen orsakade smärta vilket kan vara problematiskt vid genomförande för personer med postkontusionellt syndrom.

In this thesis, the focus is on studying BaZrO3-BaCeO3 based proton conductors due to that they represent very promising proton conductors to be used for Intermediate Temperature Solid Oxide Fuel Cells (ITSOFCs). Here, dense BaZr0.5Ce0.3Y0.2O3-δ (BZCY532) ceramics were selected as the major studied materials. These ceramics were prepared by different sintering methods and doping strategies. Based on achieved results, the thesis work can simply be divided into the following parts: 1) An improved synthesis method, which included a water-based milling procedure followed by a freeze-drying post-processing, was presented. A lowered calcination and sintering temperature for a Hf0.7Y0.3O2-δ (YSH) compound was achieved. The value of the relative density in this work was higher than previously reported data. It is also concluded that this improved method can be used for mass-production of ceramics. 2) As the solid-state reactive sintering (SSRS) represent a cost-effective sintering method, the sintering behaviors of proton conductors BaZrxCe0.8-xLn0.2O3-δ (x = 0.8, 0.5, 0.1; Ln = Y, Sm, Gd, Dy) during the SSRS process were investigated. According to the obtained results, it was found that the sintering temperature will decrease, when the Ce content increases from 0 (BZCLn802) to 0.3 (BZCLn532) and 0.7 (BZCLn172). Moreover, the radii of the dopant ions similar to the radii of Zr4+ or Ce4+ ions show a better sinterability. This means that it is possible to obtain dense ceramics at a lower temperature. Moreover, the conductivities of dense BZCLn532 ceramics were determined. The conductivity data indicate that dense BZCY532 ceramics are good candidates as either oxygen ion conductors or proton conductors used for ITSOFCs. 3) The effect of NiO on the sintering behaviors, morphologies and conductivities of BZCY532 based electrolytes were systematically investigated. According to the achieved results, it can be concluded that the dense BZCY532B ceramics (NiO was added during ball-milling before a powder mixture calcination) show an enhanced oxygen and proton conductivity. Also, that BZCY532A (NiO was added after a powder mixture calcination) and BZCY532N (No NiO was added in the whole preparation procedures) showed lower values. In addition, dense BZCY532B and BZCY532N ceramics showed only small electronic conductivities, when the testing temperature was lower than 800 ℃. However, the BZCY532A ceramics revealed an obvious electronic conduction, when they were tested in the range of 600 ℃ to 800 ℃. Therefore, it is preferable to add the NiO powder during the BZCY532 powder preparation, which can lower the sintering temperature and also increase the conductivity. 4) Dense BZCY532 ceramics were successfully prepared by using the Spark Plasma Sintering (SPS) method at a temperature of 1350 ℃ with a holding time of 5 min. It was found that a lower sintering temperature (&lt; 1400 ℃) and a very fast cooling rate (&gt; 200 ℃/min) are two key parameters to prepare dense BZCY532 ceramics. These results confirm that the SPS technique represents a feasible and cost-effective sintering method to prepare dense Ce-containing BaZrO3-BaCeO3 based proton conductors. 5) Finally, a preliminary study for preparation of Ce0.8Sm0.2O2-δ (SDC) and BZCY532 basedcomposite electrolytes was carried out. The novel SDC-BZCY532 based composite electrolytes were prepared by using the powder mixing and co-sintering method. The sintering behaviors, morphologies and ionic conductivities of the composite electrolytes were investigated. The obtained results show that the composite electrolyte with a composition of 60SDC-40BZCY532 has the highest conductivity. In contrast, the composite electrolyte with a composition of 40SDC-60BZCY532 shows the lowest conductivity. In summary, the results show that BaZrO3-BaCeO3 based proton-conducting ceramic materials represent very promising materials for future ITSOFCs electrolyte applications. / <p>QC 20150423</p>

Carbonate minerals play a very important role in nature, they represent some of the most diverse and common mineral species on the Planet. They are directly involved in the carbon dioxide (CO2) cycle acting as relatively stable long term chemical storage reservoirs, moderating both global warming trends and oceanaquatic chemistry through carbonate buffering systems. A range of synthetic metal carbonates have been synthesised for analysis under multiple experimental conditions, in order to study the variation in physical and chemical properties such as phase specificity, metal substitution, hydration/hydroxy carbonate formation under varying partial pressures of CO2 and thermal stability. Synthetic samples were characterised by a variety of instrumental analysis techniques in order to investigate chemical purity and phase specificity. Some of the techniques included, vibrational spectroscopy (IR/Raman), thermal analysis (TGA-MS) (thermal Raman), X-Ray diffraction (XRD) and electron microscopy (SEM-EDX). From the instrumental characterisation techniques, it was found that single phase smithsonite, hydrozincite, calcite and nesquehonite could successfully be synthesised under the conditions used. Minor impurities of other minerals and / or phases were found to form under specific chemical or physical conditions such as in the case of hydrozincite / simonkolleite if zinc chloride was used during hydrothermal synthesis.

This diploma thesis solves the problems of hydrothermal processes in walls of wooden houses and associated issues. A chosen were two apartment buildings, where they underwent exmerimental measurement of indor air, in order to determine the boundary conditions commonly boundary building evelope. Was followed by hygrothermal analysis of four commonly used constructions of wooden buildings in the Czech Republic, using various numerical methods. The quantity of information obtained from various numerical methods were analyzed individually. The final part of the thesis is devoted to experimental measurements of diffusion properties of materials. Namely foil vapor barrier, in terms of its influence on the perforation vapor diffusion resistance factor. Information obtained from the experiments were applied to re numerical analysis for walls with a foil vapor barrier. Followed by comparing both cases, in terms of changes hygrothermal behavior of structures with influence of perforation of the vapor barrier.