Philosophiae Doctor - PhD / This ethno a h explores the mean in s of personhood and agency in Maneberg a township located on the Cape Flats, in Cape Town South Africa. The township was a site of relocation for people who were classified coloured during the apartheid era and who were forcibly removed from newly declared white areas in the city in the 1960s I argue that despite the old apartheid state's attempts to reify the meaning of colouredness through racial legislation,\the residents of Manenberg created their own meanings of personhood, agency and community within the bureaucratic, social and economic interstices of the apartheid systems Yet at the same time they also reinstated the very structural processes at the heart of their racial and gendered subjugation. I indicate how the cohesiveness of the Rio Street community in Manenberg, the survival of its residents and their validation as respectable mothers, tough men and good daughters hinged on and effloresced from a moral economy that articulated with the structural location of coloured women in the apartheid economy and racial bureaucracy. I draw upon the writings of Fortes (1969), Giddens (1984) and Karp (1995) to elaborate upon the concept personhood in Manenberg. I show how the local understandings of personhood provide residents with agency, whilst connecting the latter to township history and apartheid social structure, thereby illustrating its limits. The concept personhood captures the duality of existence of Manenberg residents and maps out their negotiation and contestation about personhood and agency. I use Hobart (1990) and Kratz (2000) to indicate that lagency in Manenberg is complex and is situationally determined~Finally I utilise the theoretical insights of Donham (1999) to indicate that Manenberg's social, economic and historical location in the South African context allows for several notions of personhood to prevail in the township. These notions are grounded in the multiple, interconnected, hierarchically ordered, competing cultural and economic systems of production at the local, national and global levels. This complex location of Manenberg residents generates multiple constructs of inequality, power and agency that impinge upon each other and that are reflected in the contestations about personhood in diverse township spaces.

Diploma thesis focuses on one of the most important variables of proportional electoral systems - electoral districts. This problematic is researched in the context of municipal elections to the Prague City Assembly. In the Czech municipal electoral system this variable can be changed very flexibly and in Prague we can find three variations of electoral districts. The aim of thesis is to explore these variants of electoral districts from the point of proportionality and efficiency of governance. The topic is researched in three cases of municipal elections in Prague in 2010, 2014 and 2018. In the introduction of diploma thesis two research questions are defined. The first part is theoretical, and it is focused on the municipal electoral system in the Czech Republic, electoral district in the theory of electoral systems, variants of electoral districts in Prague and academic debate about proportionality and efficiency. Results of three researched elections are analysed as well. The analytical part of thesis is focused on models of seats distribution in accordance with electoral districts. In the conclusion results are evaluated and compared. Research questions are answered in this part as well.

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O objetivo do presente estudo é avaliar o uso associado dos proxies ?18O e Mg/Ca obtidos em testas de foraminíferos. Para alcançar tal objetivo foram realizadas análises de ?18O e Elemento/Ca em amostras de foraminíferos planctônicos (G. ruber e G. sacculifer) e bentônicos (Cibicidoides spp., C. corpulentus, Uvigerina spp. e H. elegans) de dois testemunhos do Atlântico Sul. Os resultados demonstraram que apesar dos proxies ?18O e Mg/Ca apresentarem perfis distintos em relação às espécies os mesmos se correlacionam de forma apropriada, sendo possível estimar a temperatura e os sinais de ?18OSW e ?18OLocal a partir dos mesmos. A partir dos dados de temperatura estimados com base em Mg/Ca foi possível identificar uma anomalia negativa das águas superficias entre o LGM e o HL de -1,5 ± 0,2 °C, enquanto que nas águas profundas observou-se uma anomali positiva de 1,7 ± 0,4 °C para o mesmo período. Os dados de ?18OSW estimados com base nos dados de temperatura e ?18O indicaram uma oscilação de 1,0 ± 0,1 ? e 2,0 ± 0,2 ? para as espécies planctônicas e bentônicas durante o LGM e o HL. Segundo o valor esperado para a variação do volume de gelo (~1,2 ?) há uma oscilação muito baixa da salinidade nas águas superficias da região de estudo, em contraste com uma oscilação bem marcada da salinidade nas águas de fundo. As estimativas de ?18OLocal indicaram uma oscilação entre o LGM e o HL muito pequena da salinidade (~0,1 ?) nas águas superficiais, com uma oscilação maior nas águas de fundo (1,0 ± 0,3 ?). O aumento da salinidade das águas de fundo durante o LGM corrobora a anomalia positiva da temperatura observada neste estudo, visto que, para a ocorrência da mesma, é necessário que a densidade das águas de fundo seja suficiente para manter a estratificação da coluna de água. / The goal of this study is to evaluate the associated use of the proxies ?18O and Mg/Ca, both analyzed in foraminifera tests. ?18O and trace metals analyses were performed in order to achieve this purpose on samples of planktonic (G. ruber and G. sacculifer) and benthic (Cibicidoides spp., C. corpulentus, Uvigerina spp. and H. elegans) species of foraminifera from two cores from South Atlantic. Despite of the fact that the proxies used on this study present distinct fits within the species they correlate very well, being possible to estimate the values of temperature, ?18OSW and ?18OLocal. Based on the temperature estimated by Mg/Ca it was possible to identify a negative anomaly of -1,5 ± 0,2 °C between the LGM and HL, meanwhile a positive anomaly of 1,7 ± 0,4 °C was observed in the deep waters for the same period. The ?18OSW data estimated by temperature and ?18O indicate an oscilation of 1,0 ± 0,1 ? and 2,0 ± 0,2 ? for planktonic and benthic species between the LGM and the HL. Based on the literature value for the ice volume signal (~1,2 ?) the superficial waters of the study area indicated a very low salinity oscilation, opposite to the high salinity oscillation in the deep waters. The ?18OLocal estimatives exhibited a very weak salinity oscillation between LGM and HL in the superficial waters (~0,1 ?), providing a much more strong oscilation in the deep waters (1,0 ± 0,3 ?). The salinity increase during the LGM in the deep waters establish the validity of the positive temperature anomaly observed in this study, since the density of the deep water needs to be adequate to maintain the water column stratification.

O objetivo do presente estudo é avaliar o uso associado dos proxies ?18O e Mg/Ca obtidos em testas de foraminíferos. Para alcançar tal objetivo foram realizadas análises de ?18O e Elemento/Ca em amostras de foraminíferos planctônicos (G. ruber e G. sacculifer) e bentônicos (Cibicidoides spp., C. corpulentus, Uvigerina spp. e H. elegans) de dois testemunhos do Atlântico Sul. Os resultados demonstraram que apesar dos proxies ?18O e Mg/Ca apresentarem perfis distintos em relação às espécies os mesmos se correlacionam de forma apropriada, sendo possível estimar a temperatura e os sinais de ?18OSW e ?18OLocal a partir dos mesmos. A partir dos dados de temperatura estimados com base em Mg/Ca foi possível identificar uma anomalia negativa das águas superficias entre o LGM e o HL de -1,5 ± 0,2 °C, enquanto que nas águas profundas observou-se uma anomali positiva de 1,7 ± 0,4 °C para o mesmo período. Os dados de ?18OSW estimados com base nos dados de temperatura e ?18O indicaram uma oscilação de 1,0 ± 0,1 ? e 2,0 ± 0,2 ? para as espécies planctônicas e bentônicas durante o LGM e o HL. Segundo o valor esperado para a variação do volume de gelo (~1,2 ?) há uma oscilação muito baixa da salinidade nas águas superficias da região de estudo, em contraste com uma oscilação bem marcada da salinidade nas águas de fundo. As estimativas de ?18OLocal indicaram uma oscilação entre o LGM e o HL muito pequena da salinidade (~0,1 ?) nas águas superficiais, com uma oscilação maior nas águas de fundo (1,0 ± 0,3 ?). O aumento da salinidade das águas de fundo durante o LGM corrobora a anomalia positiva da temperatura observada neste estudo, visto que, para a ocorrência da mesma, é necessário que a densidade das águas de fundo seja suficiente para manter a estratificação da coluna de água. / The goal of this study is to evaluate the associated use of the proxies ?18O and Mg/Ca, both analyzed in foraminifera tests. ?18O and trace metals analyses were performed in order to achieve this purpose on samples of planktonic (G. ruber and G. sacculifer) and benthic (Cibicidoides spp., C. corpulentus, Uvigerina spp. and H. elegans) species of foraminifera from two cores from South Atlantic. Despite of the fact that the proxies used on this study present distinct fits within the species they correlate very well, being possible to estimate the values of temperature, ?18OSW and ?18OLocal. Based on the temperature estimated by Mg/Ca it was possible to identify a negative anomaly of -1,5 ± 0,2 °C between the LGM and HL, meanwhile a positive anomaly of 1,7 ± 0,4 °C was observed in the deep waters for the same period. The ?18OSW data estimated by temperature and ?18O indicate an oscilation of 1,0 ± 0,1 ? and 2,0 ± 0,2 ? for planktonic and benthic species between the LGM and the HL. Based on the literature value for the ice volume signal (~1,2 ?) the superficial waters of the study area indicated a very low salinity oscilation, opposite to the high salinity oscillation in the deep waters. The ?18OLocal estimatives exhibited a very weak salinity oscillation between LGM and HL in the superficial waters (~0,1 ?), providing a much more strong oscilation in the deep waters (1,0 ± 0,3 ?). The salinity increase during the LGM in the deep waters establish the validity of the positive temperature anomaly observed in this study, since the density of the deep water needs to be adequate to maintain the water column stratification.

Dans le cadre du projet LIU, vise à augmenter la puissance des injecteurs du LHC, le CERN PS Booster (PSB) sera mis à jour avec un système d'injection d'échange de charge H- et son énergie d'injection sera portée de 50 MeV à 160 MeV pour obtenir la luminosité du faisceau nécessaire pour le LHC High-Luminosity Upgrade. Effets de charge d'espace comme pertes de faisceau et incrément d’émittance transversale à l'injection vont être les principales limites vers la réalisation de la haute luminosité souhaitée. Des études sur la dynamique du faisceau en présence de charge d'espace afin d'évaluer les performances du PSB après la mise à niveau ont été effectuées. La première partie du travail consiste de mesures dans la présente machine, pour étudier les effets de charge d'espace et son interaction avec les résonances et d'avoir un ensemble de données pour le code benchmarking. Le code choisi pour le suivi du faisceau en présence de charge d'espace est PTC-Orbit (et PyOrbit). Les études de convergence numériques nécessaires sont présentées conjointement avec les études de la comparaison des simulations avec les mesures dans la machine. Une fois évalué le code et ses limites, les prévisions pour l'injection dans le PSB à 160 MeV avec des poutres de luminosité élevé sont livrés en termes de pertes de faisceau et incrément d’émittance. Ces études comprennent l'optimisation du point de fonctionnement, la compensation des résonances et/ou la correction de chromaticité en tenant compte des erreurs magnétiques attendus dans la machine. / As part of the LHC Injector Upgrade Project, the CERN PS Booster (PSB) will be upgraded with a H- charge exchange injection system and its injection energy will be raised from 50 MeV to 160 MeV to obtain the beam brightness required for the LHC High-Luminosity Upgrade. Space charge effects like beam losses and transverse emittance blow-up at injection are expected to be the main limitations towards the achievement of the required high brightness. Studies of beam dynamics in presence of space charge in order to evaluate the performances of the PSB after the Upgrade have been performed. The first part of the work consists of measurements in the present machine, to study the effects of space charge and its interplay with resonances and to have a good set of data for code benchmarking. The code chosen for the beam tracking in presence of space charge is PTC-Orbit (and PyOrbit). Necessary numerical convergence studies are presented together with a benchmark with the PSB measurements. Once assessed the code and its limitations, predictions for the 160 MeV injection with high- brightness beams are delivered in terms of beam losses and emittance blow-up. These studies include the optimization of the working-point, resonance compensation and/or chromaticity correction taking into account the expected magnetic errors in the machine.

The diploma thesis "Media Coverage of Prague Public Transport Company" intends to describe the media image of the company in selected Czech dailies Metro, MF Dnes, Právo and Pražský deník during the years 2011 and 2012. A total of 680 articles were analyzed both quantitatively and qualitatively systematically describing their content during the period mentioned. The theoretical part introduces the reader to a broader context and serves as a platform anchoring the practical part. At first this part introduces the chosen methodology and then the results and interpretation. The quantitative content analysis explores how often and how much the topic appears in print media, its timing during the given period, and deals with researching of mainly published topics mentioned in press and their relationships in connection to Prague Public Transport Company. The thesis also focuses on the types of articles (hard news and soft news) and also examines which actors appeared in the selected newspapers. The next part deals with the linguistic interpretation of individual statements about Prague Public Transport Company, therefore, in what areas is the subject of analysis evaluated positively or negatively, on the basis of the attributes of language resources and comparison. The obtained data evaluation leads me...

Cette thèse montre comment l'astérosismologie, basée sur l'observation et la modélisation, peut rendre compte de la structure interne d'une étoile naine blanche DAV, notamment comment il est possible de déduire la masse de son enveloppe d'hydrogène résiduel. Nous avons étudié 2 ZZ Ceti: HL Tau 76 (bord rouge de la bande d'instabilité) et G 185-32 (bord bleu). La modélisation indique que ces 2 étoiles possèdent une enveloppe d'hydrogène de masse sensiblement identique: M(H)= 2.0(+/-0.3)x 10e-4 Mstar. Cela suggèrerait une possible constance de la masse de cette enveloppe pour l'ensemble des étoiles DA et par là même d'éventuelles implications pour la cosmochronologie et les mécanismes de l'évolution stellaire. Par ailleurs, cette thèse illustre comment la modélisation permet de révéler certaines caractéristiques physiques comme une rotation de l'étoile non-uniforme, un couplage non-linéaire au sein d'un triplet de modes résonants, une intéraction entre les pulsations et la convection.

Thesis (Ph.D.)--University of Aberdeen, 2005. / Includes bibliographical references. Available in PDF format via the World Wide Web.