Legal regulation of international trade in military material and civilian weapons The thesis focuses on the comparison of regulations governing international trade with weapons of military and non-military character. The area under consideration is, given the character of the commodity traded, a specific area of international trade in which there are a number of legal norms regulating this area. The analysis and comparison of the legal standards in question is based on international, European and national legislation, with an emphasis on internal interconnection of individual legal norms in order to better understanding and relevance to the international arms trade. The thesis consists of several chapters that are thematically related. The first chapter deals with the theoretical definition of international arms trade with a focus on private international law. Particular attention is paid to the international purchase agreement and international transport agreements that will be applied in the course of the implementation of the arms trade. The second chapter focuses on defining the term "weapon" and its definition in the most important international conventions dealing with weapons. Attention is focused on distinguishing military weapons and weapons for civilian purposes. The next, third to fifth chapters...

The aim of the thesis is to evaluate customer relationship management in a selected organization through a questionnaire survey. At first was identified company marketing through 4P, making it possible to outline how the company does with the product, distribution, pricing and marketing communications. Subsequently, a survey was conducted on a total of 100 respondents. The questionnaire had 20 questions, in which customers expressed their satisfaction with the company's employees, offered goods, services and also compared the individual areas of business to competitors. After evaluation questionnaire was also conducted guided interview with the director of questions regarding the results of the survey. On the basis of all the facts were subsequently proposed changes that the company should take to improve customer relationship management.

The aim of the thesis was "To assess the current state of awareness of the personnel of the social services providers in the field of extraordinary events, to assess the effectiveness of the implemented training program". Based on the stated objective, then, to verify 2 established hypotheses. Hypothesis No. 1, ´Awareness of social service provider staff on the recommended behaviour manners during extraordinary events does not reach 80% of correct response success´ , and Hypothesis No. 2, ´Social service provider staff education leads to an improvement in the current situation of behaviour manners during extraordinary events´. To fulfill this aim, a research survey was created, which I personally carried out in 4 social service providers, fulfilling the following criteria: the social service provider had to provide a ´stay´ form, handicapped individuals had to stay there´, and the place had to be located in the region of South Bohemia. The results were being evaluated via graphics processed in Microsoft Excel Word 2007 programme. To evaluate Hypothesis No. 2 I created an educative material in an e-learning form, containing 5 thematic areas: protection of population, fire, floods, chemical substances, and radio-active substances. I introduced this educative material to the social service provider staff, and subsequently I carried out a second round of interview survey. In the results of this work I was comparing the staff´s responses before the implemented educative programme, and after. The results of my research work have proven that the less staff takes part in education on protection of population, the less individuals are introduced to the recommended manners of behaviour during extraordinary events. The educative programme has brought valuable information for the social service provider staff. An improvement was missing in certain responses, but in my opinion, this is due to an extremely expert or thematic area of questions. The educative programme has brought valuable information for the social service provider staff. A significant improvement was noticed in the second round of questionnaire survey after implementing the educative programme. An improvement was missing in certain responses, but in my opinion, this is due to an extremely expert or thematic area of questions.

This diploma thesis deals with the collection of information on work safety and movement of animals in cattle breeding. Their subsequent evaluation and processing, the identification of risks for breeders and reared cattle. The information is supplemented by measuring the time needed to handle the cattle.

The dissertation addresses the issue of death education. It represents the concept of this education as it was created and is realized in the United States (Levinton, 1977; Wass, 2003; Doka 2015). The aim of qualitative research is to map the experiences of teachers with the theme of school death. It follows experiences of interventions in cases of death in the closest family of pupils or the death of a member of the school community, experience with topics related to death in teaching, as well as conditions for education related to death. The data were obtained through semi-structured interviews with ten teachers. Part of the work on based on teacher intervention in 11 cases, six of which were concerned with deaths in the pupil's family, in three a pupil died. In two cases, deaths were related to teachers. In the interviews, teachers paid much attention to the situation regarding the classroom reporting, usually choosing a factual announcement after which the pupils were recommended how to behave to the mournful classmate. In this recommendation, there was an emphasis on empathy or on the preservation of common behavior. If the event was communicated by a pupil or the teacher perceived their interest, a discussion in which the pupils communicated their reflections, experiences followed. No teacher noticed a strong emotional response from pupils. To the grieving pupil, teachers usually expressed their participation outside the classroom. In their further negotiations with him, they either sought to maintain the order or considered different options. These included both the demands on the pupil and the choice of topics in the classroom respecting the sensitivity to family issues or devoting attention to death issues (often through reading). Part of the work on the subject of death in teaching presents school subjects where teachers can deal with death related topics. It is the Czech language, Elementary studies, Natural sciences, History or Ethical and Dramatic Education. Although the themes of death in the curriculum appear, only some teachers are giving them attention. Most often it is then the case for a wide range of discussions or essay writing of pupils, which usually follows common reading. Teachers perceive pupils' interest in these topics. In some cases, teachers have sought to counterbalance the numbing impact of contemporary death mediation by making pupils feel through reading or film watching. The theme of death has sometimes been raised by the pupils themselves. Teachers perceived support from their personal experience (for five their parents died in childhood or adolescence). In their professional training, they perceived courses such as Critical Thinking or Philosophy for Children superior providing them with tools for work with demanding themes. Many teachers apply a personal approach to their pupils which naturally forms an appropriate framework for interventions as well as teaching on the theme of death.

The present study has as its general goal to analyze possibilities for the physical education of the human body from 1st to 4th year of elementary school. The specific objectives are: toreflect about: the culture of movement and children; how do the functions of movement gain meaning to the children; the dialogue between child/movement and the world; the academical matters and teacher formation to work in the initial years of school teachers and specialists in physical education. The study develops itself from a methodological basis of theoretical and bibliographic research. Through readings of classical literary work and different authors involved in the topic, to discuss and reflect about the reality and suggest the development of a thought that might serve as a basis in the development of alternatives for the reality of Physical Education classes in the initial years of school. Thus we intend that the final report of this study may be useful so that new ways of developing Physical Education classes in the initial years of school may be thought and created. As well as try to sustain a different teacher performance focused on the didacticalpedagogical transformation and a concern with the formal teacher formation such as in a category of a continuous formation. In addition to the Introduction and the Justification this research is complemented with chapters that seek for an approach with the proposed goals: Education, Pedagogy and Physical Education; The child and the Childhood A History; The Movement and To-Move; The Physical Education Developer Current; Psychomotor Education; Biomechanics and Physical Education; Human Movement and the To-Move A Philosophical Path; and completing the research with the chapter: The To-Move in the Process of Education Children in the Physical Education Classes Educational Possibilities. / O presente estudo tem como objetivo geral analisar possibilidades para a Educação Física do movimento humano do 1º ao 4º anos do ensino fundamental. Os objetivos específicos são: refletir sobre a cultura do movimento e crianças; como as funções de movimento ganham significado para as crianças; o diálogo entre criança/movimento e mundo; as questões docentes e a formação de professores para atuar nos anos iniciais unidocentes e especialistas em Educação Física. O estudo se desenvolve a partir de uma base metodológica das pesquisas teórica e bibliográfica. Por meio de leituras de obras clássicas e diferentes autores envolvidos no tema, discutir e refletir sobre a realidade e propor a construção de um pensamento que possa servir de base na construção de alternativas para a realidade das aulas de Educação Física nos anos iniciais. Dessa forma, pretendemos que o relatório final deste estudo possa ser útil para que novas formas de desenvolver as aulas de Educação Física nos anos iniciais possam ser pensadas e criadas, bem como sustentar uma atuação docente voltada para a transformação didático-pedagógica e uma preocupação com a formação de professores, quer de maneira formal, quer em uma categoria de formação continuada. Além da Introdução e da Justificativa, esta pesquisa é complementada com capítulos que procuram aproximação com os objetivos propostos: Educação, Pedagogia e Educação Física; A criança e a Infância Uma História; O Movimento e Se-Movimentar; A Corrente Desenvolvimentista da Educação Física; Educação Psicomotora; Biomecânica e Educação Física; Movimento Humano e o Se-Movimentar Um Caminho Filosófico; e concluímos a pesquisa com o capitulo: O Se-Movimentar no Processo da Educação Criança nas Aulas de Educação Física - Possibilidades Educacionais.

Made available in DSpace on 2015-03-13T17:08:12Z (GMT). No. of bitstreams: 1 KatianeSS_capa_ate_secao3.pdf: 4061338 bytes, checksum: 28febddb7031b2403525b3cbefed2d05 (MD5) Previous issue date: 2007-03-30 / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior / Baixo Vermelho area, situated on the northern portion of Umbuzeiro Graben (onshore Potiguar Basin), represents a typical example of a rift basin, characterized, in subsurface, by the sedimentary rift sequence, correlated to Pend?ncia Formation (Valanginian-Barremian), and by the Carnaubais fault system. In this context, two main goals, the stratigraphic and the structural analysis, had guided the research. For this purpose, it was used the 3D seismic volume and eight wells located in the study area and adjacencies. The stratigraphic analysis of the Valanginian-Barremian interval was carried through in two distinct phases, 1D and 2D, in which the basic concepts of the sequence stratigraphy had been adapted. In these phases, the individual analysis of each well and the correlation between them, allowed to recognize the main lithofacies, to interpret the effective depositional systems and to identify the genetic units and key-surfaces of chronostratigraphic character. The analyzed lithofacies are represented predominantly by conglomerates, sandstones, siltites and shales, with carbonate rocks and marls occurring subordinately. According to these lithofacies associations, it is possible to interpret the following depositional systems: alluvial fan, fluvio-deltaic and lacustrine depositional systems. The alluvial fan system is mainly composed by conglomerates deposits, which had developed, preferentially in the south portion of the area, being directly associated to Carnaubais fault system. The fluvial-deltaic system, in turn, was mainly developed in the northwest portion of the area, at the flexural edge, being characterized by coarse sandstones with shales and siltites intercalated. On the other hand, the lacustrine system, the most dominant one in the study area, is formed mainly by shales that could occur intercalated with thin layers of fine to very fine sandstones, interpreted as turbidite deposits. The recognized sequence stratigraphy units in the wells are represented by parasequence sets, systems tracts and depositional sequences. The parasequence sets, which are progradational or retrogradational, had been grouped and related to the systems tracts. The predominance of the progradation parasequence sets (general trend with coarsening-upward) characterizes the Regressive Systems Tract, while the occurrence, more frequently, of the retrogradation parasequence sets (general trend with finning-upward) represents the Transgressive System Tract. In the seismic stratigraphic analysis, the lithofacies described in the wells had been related to chaotic, progradational and parallel/subparallel seismic facies, which are associated, frequently, to the alluvial fans, fluvial-deltaic and lacustrine depositional systems, respectively. In this analysis, it was possible to recognize fifteen seismic horizons that correspond to sequence boundaries and to maximum flooding surfaces, which separates Transgressive to Regressive systems tracts. The recognition of transgressive-regressive cycles allowed to identify nine, possibly, 3a order deposicional sequences, related to the tectonic-sedimentary cycles. The structural analysis, in turn, was done at Baixo Vermelho seismic volume, which shows, clearly, the structural complexity printed in the area, mainly related to Carnaubais fault system, acting as an important fault system of the rift edge. This fault system is characterized by a main arrangement of normal faults with trend NE-SO, where Carnaubais Fault represents the maximum expression of these lineations. Carnaubais Fault corresponds to a fault with typically listric geometry, with general trend N70?E, dipping to northwest. It is observed, throughout all the seismic volume, with variations in its surface, which had conditioned, in its evolutive stages, the formation of innumerable structural features that normally are identified in Pendencia Formation. In this unit, part of these features is related to the formation of longitudinal foldings (rollover structures and distentional folding associated), originated by the displacement of the main fault plan, propitiating variations in geometry and thickness of the adjacent layers, which had been deposited at the same time. Other structural features are related to the secondary faultings, which could be synthetic or antithetic to Carnaubais Fault. In a general way, these faults have limited lateral continuity, with listric planar format and, apparently, they play the role of the accomodation of the distentional deformation printed in the area. Thus, the interaction between the stratigraphic and structural analysis, based on an excellent quality of the used data, allowed to get one better agreement on the tectonicsedimentary evolution of the Valanginian-Barremian interval (Pend?ncia Formation) in the studied area / A ?rea de Baixo Vermelho, localizada na por??o norte do Graben de Umbuzeiro (Bacia Potiguar emersa), representa um exemplo t?pico de uma bacia do tipo rifte, caracterizada, em subsuperf?cie, pela seq??ncia sedimentar rifte, correlata ? Forma??o Pend?ncia (Valanginiano-Barremiano), e pelo Sistema de Falhas de Carnaubais. Dentro deste contexto, duas abordagens principais nortearam o estudo, a estratigr?fica e a estrutural, em que se lan?ou m?o da interpreta??o do volume s?smico 3D de Baixo Vermelho e de oito po?os explorat?rios da ?rea e adjac?ncias. A an?lise estratigr?fica do intervalo do Valanginiano ao Barremiano foi realizada em duas fases distintas, 1D e 2D, nas quais foram adaptados os conceitos b?sicos da estratigrafia de seq??ncias. Nestas fases, a an?lise individual de cada po?o e a correla??o entre os mesmos permitiu reconhecer as principais litof?cies presentes, interpretar os sistemas deposicionais vigentes e identificar as unidades gen?ticas e as superf?cies-chave de car?ter cronoestratigr?fico. As litof?cies analisadas constituem, predominantemente, conglomerados, arenitos, siltitos e folhelhos, ocorrendo, ainda, de forma subordinada, rochas carbon?ticas e margas. Com base nas associa??es destas litof?cies foram interpretados os sistemas deposicionais de leque aluvial, fl?vio-deltaico e lacustre. O sistema de leque aluvial ? composto, principalmente, por dep?sitos conglomer?ticos, os quais se desenvolveram, principalmente, na por??o sul da ?rea, estando diretamente associados ao Sistema de Falhas de Carnaubais. O sistema fl?viodeltaico, por sua vez, foi desencadeado, preferencialmente, na por??o noroeste da ?rea, na margem flexural, sendo caracterizado por arenitos grossos a finos intercalados a folhelhos e siltitos. Em contrapartida, o sistema lacustre, o mais dominante na ?rea investigada, ? formado principalmente por folhelhos que ocorrem, por vezes, intercalados a delgadas camadas de arenitos finos a muito finos, interpretados como dep?sitos turbid?ticos. As unidades da estratigrafia de seq??ncias reconhecidas nos po?os est?o representadas pelos conjuntos de parasseq??ncias, tratos de sistemas e seq??ncias deposicionais. Os conjuntos de parasseq??ncias, ora progradacionais, ora retrogradacionais, foram agrupados e relacionados aos tratos de sistemas. A predomin?ncia dos conjuntos de parassequ?ncias progradacionais (trend geral com engrossamento textural para o topo) caracteriza o Trato de Sistemas Regressivo, ao passo que a ocorr?ncia, com maior freq??ncia, dos conjuntos de parassequ?ncias retrogradacionais (trend geral com afinamento textural para o topo) representam o Trato de Sistemas Transgressivo. Na an?lise sismoestratigr?fica, as litof?cies descritas nos po?os foram relacionadas ?s sismof?cies ca?tica, progradacional e paralela/subparalela, as quais se associam, freq?entemente, aos sistemas de leques aluviais, fl?vio-deltaico e lacustre, respectivamente. Nesta an?lise foram mapeados quinze horizontes s?smicos que correspondem aos limites de seq??ncias deposicionais e ?s superf?cies de inunda??o m?xima, que separam o trato de sistemas transgressivo do regressivo. O reconhecimento de ciclos transgressivo-regressivo permitiu identificar nove seq??ncias deposicionais, possivelmente de 3a ordem, relacionadas a ciclos tectono-sedimentares. A an?lise estrutural, por sua vez, foi realizada no volume s?smico de Baixo Vermelho, que mostra, com clareza, a complexidade estrutural impressa na ?rea, relacionada, principalmente, ao Sistema de Falhas de Carnaubais, que atua como um importante sistema de falhas de borda de rifte. Este sistema de falhas ? caracterizado por um arranjo principal de falhas normais NE-SO, em que a Falha de Carnaubais representa a express?o m?xima destes lineamentos. A Falha de Carnaubais corresponde a uma falha com geometria tipicamente l?strica, direcionada segundo o trend geral N70?E, mergulhando para noroeste. Apresenta-se, ao longo de todo o volume s?smico, com varia??es em sua superf?cie, as quais condicionaram, em seus est?gios evolutivos, a forma??o de in?meras fei??es estruturais, que s?o comumente identificadas na Forma??o Pend?ncia. Nesta unidade, parte das fei??es est? relacionada ? forma??o de dobramentos longitudinais (estrutura do tipo rollover e dobramentos distensionais associados), decorrentes do deslocamento do plano da falha principal, propiciando varia??es na geometria e espessura dos estratos adjacentes, os quais foram depositados sincronicamente. Outras fei??es estruturais est?o relacionadas a falhamentos secund?rios, tanto sint?ticos quanto antit?ticos ? Falha de Carnaubais. De uma maneira geral, estas falhas t?m continuidade lateral limitada, com formato planar a l?strico e, aparentemente, desempenham o papel de acomoda??o da deforma??o distensional imposta na ?rea. Assim, a intera??o entre as an?lises estratigr?fica e estrutural, alicer?ados pela excelente qualidade dos dados utilizados, permitiu obter um melhor entendimento sobre a evolu??o tectono-sedimentar do intervalo Valanginiano ao Barremiano (Forma??o Pend?ncia) na ?rea de estudo

Made available in DSpace on 2015-03-13T17:08:27Z (GMT). No. of bitstreams: 1 FatimaMCC_DISSERT_1-50.pdf: 5372710 bytes, checksum: 8e3306f0f537e25a61d067b9d1bf86a8 (MD5) Previous issue date: 2010-02-22 / The Palestina Graben is one of the NE-trending asymmetric grabens of the Araripe Basin. This basin rests on the precambrian terrains of the Transversal Zone, Borborema Province, immediately to the south of the Patos Lineament. It is part of the Interior Basins province of Northeastern Brazil, being related to the fragmentation of the Gondwana supercontinent and the opening of the South Atlantic ocean. The Palestina Graben trends NE-SW and presents an asymmetric geometry, controled by the NW extensional eocretaceous strain. The graben borders display distinct geometries. The SE border is a flexural margin, characterized by the non conformity of the eopaleozoic Mauriti Formation (the oldest unit of the basin) overlying the crystalline basement, but also affected by normal faults with small displacements. On the opposite, the NW border is continuous and rectilinear, being marked by normal faults with major displacements, that control the general tilting of the layers to the NW. In this sense, the Mauriti Formation is overlain by the Brejo Santo, Miss?o Velha (which also occurs in the Brejo Santo-Mauriti horst, to the NW of the fault border) and Abaiara formations, the latter restricted to the graben. The interpretation of available gravity data and a seismic line indicates that the main fault has a variable dip slip component, defining two deeper portions within the graben, in which the sedimentary column can reach thicknesses of up to 2 km. Regarding to the stratigraphy of Araripe Basin in the study area, the sedimentary package includes three distinct tectonosequences. The Paleozoic Syneclisis Tectonosequence is composed by the Mauriti Formation, deposited by a braided fluvial system. The Jurassic Tectonosequence, whose tectonic setting is still debatable (initial stage of the Neocomian rift, or a pre-rift syneclisis ?), is represented by the Brejo Santo Formation, originated in a distal floodplain related to ephemeral drainages. The Rift Tectonosequence, of neocomian age, includes the Miss?o Velha Formation, whose lower section is related to a braided to meandering fluvial system, outlining the Rift Initiation Tectonic Systems Tract. The upper section of the Miss?o Velha Formation is separated from the latter by a major unconformity. This interval was originated by a braided fluvial system, overlain by the Abaiara Formation, a deltaic system fed by a meandering fluvial system. Both sections correspond to the Rift Climax Tectonic Systems Tract. In the area, NE-trending normal to oblique faults are associated with NW transfer faults, while ENE to E-W faults display dominant strike slip kinematics. Both NE and E-W fault sets exhibit clear heritage from the basement structures (in particular, shear zones), which must have been reactivated during the eocretaceous rifting. Faults with EW trends display a dominant sinistral shear sense, commonly found along reactivated segments of the Patos Lineament and satellyte structures. Usually subordinate, dextral directional movements, occur in faults striking NNW to NE. Within this framework bearing to the Palestina Graben, classical models with orthogonal extension or pull-apart style deserve some caution in their application. The Palestina Graben is not limited, in its extremeties, by E-W transcurrent zones (as it should be in the case of the pull-apart geometry), suggesting a model close to the classic style of orthogonal opening. At the same time, others, adjacent depocenters (like the Abaiara-Jenipapeiro semi-graben) display a transtensional style. The control by the basement structures explains such differences / O Graben de Palestina comp?e o conjunto de depocentros com orienta??o NESW a ENE, da Bacia do Araripe. Esta bacia foi implantada nos terrenos pr?-cambrianos da Zona Transversal, da Prov?ncia Borborema, imediatamente a sul do Lineamento Patos. A mesma faz parte da prov?ncia das Bacias Interiores do Nordeste, relacionadas ? fragmenta??o do supercontinente Gondwana e abertura do Atl?ntico Sul. O Graben de Palestina apresenta orienta??o NE-SW e uma geometria assim?trica, condicionada pela orienta??o NW dos esfor?os de estiramento crustal eocret?ceo. As suas bordas apresentam comportamento distinto. A borda SE constitui uma margem flexural, caracterizada pelo contato em n?o conformidade da Forma??o Mauriti (de idade eopaleoz?ica, unidade basal da bacia) com o embasamento cristalino, sendo todavia afetado por falhas de rejeito moderado. J? a borda NW ? continua e retil?nea, marcada por falhas com rejeito significativo, que controlam o basculamento das camadas para NW. Nesse sentido, a Forma??o Mauriti ? capeada pelas forma??es Brejo Santo, Miss?o Velha (que tamb?m ocorrem no Horst de Brejo Santo-Mauriti, a NW da borda falhada) e Abaiara, esta ?ltima restrita ao graben. A interpreta??o dos dados gravim?tricos e de uma linha s?smica indicam que a falha principal tem rejeito vari?vel, definindo duas por??es mais profundas no graben, nas quais a coluna sedimentar pode atingir espessuras de at? 2 km. Em rela??o ? estratigrafia na Bacia do Araripe, na ?rea de estudo, o pacote sedimentar agrupa tr?s tectonossequ?ncias distintas. A Tectonossequ?ncia da Sin?clise Paleoz?ica ? composta pela Forma??o Mauriti, depositada por um sistema fluvial entrela?ado. Segue-se a Tectonossequ?ncia Jur?ssica, cujo contexto tect?nico ainda discut?vel (in?cio do rifte neocomiano ou sin?clise pr?-rifte ?), sendo representada pela Forma??o Brejo Santo, originada numa plan?cie de inunda??o distal de canais fluviais ef?meros. A Tectonossequ?ncia Rifte, de idade neocomiana, inclui a Forma??o Miss?o Velha, cuja se??o inferior representa um sistema fluvial entrela?ado a meandrante grosso, sendo interpretada como o Trato de Sistemas Tect?nico de In?cio do Rifte. A se??o superior da Forma??o Miss?o Velha ? separada da precedente por uma importante discord?ncia. Este intervalo inferior foi originado por um sistema fluvial entrela?ado, sendo capeado pela Forma??o Abaiara, originada por um sistema deltaico alimentado por um sistema fluvial meandrante. Ambos correspondem ao Trato de Sistemas Tect?nico de Cl?max do Rifte. Na ?rea s?o distinguidas falhas NE normais a obl?quas, associadas a falhas NW que constituem estruturas de transfer?ncia, e falhas com dire??es variando de ENE a EW, estas com predom?nio de rejeitos direcionais. Os sets NE e E-W exibem evidente paralelismo com estruturas do embasamento (em especial, zonas de cisalhamento), que devem ter sido reativadas quando do rifteamento eocret?ceo. As falhas com orienta??o pr?xima de E-W apresentam componente direcional dominante, sinistral, caracteristicamente presente nos segmentos reativados do Lineamento Patos e estruturas sat?lite. Componentes direcionais dextrais, em geral subordinados mas localmente tamb?m expressivos, ocorrem nas falhas cujas dire??es variam entre NNW a NE. No contexto descrito para o Graben de Palestina, os modelos cl?ssicos em distens?o ortogonal ou pull-apart merecem ressalvas quando de sua aplica??o. O Graben de Palestina n?o est? limitado, nas suas extremidades, por zonas transcorrentes E-W (como deveria ser o caso no modelo pull-apart), o que sugere para o mesmo um modelo pr?ximo ao estilo cl?ssico de abertura ortogonal, ao passo que outros depocentros vizinhos, de mesma idade (como o Semi-graben de Abaiara-Jenipapeiro), exibem um estilo transtracional. Tais diferen?as s?o controladas pela trama estrutural subjacente, do embasamento

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior / A presente dissertação de mestrado pretende abordar as vicissitudes do discurso do capitalista sobre o sujeito. Para tanto, toma como ponto de partida a afirmação de Lacan, em suas palestras em Saint-Anne sobre O saber do psicanalista, de que o que caracteriza o discurso do capitalista é a foraclusão da castração. A partir dessa colocação representada no matema do discurso do capitalista pelo desaparecimento da disjunção entre produto e verdade, bem como pela ausência de um vetor entre agente e Outro, o que demonstra que esse discurso não promove laço social , percorre-se algumas questões que reverberam sobre o sujeito, dentre as quais se destaca: se o sujeito não existe fora do laço social, que sorte de efeitos a ele resulta por freqüentar um discurso que se apresenta como dominante na contemporaneidade em que a castração está foracluída e, portanto, também o liame social? Tendo em vista que a Verwerfung é o que opera no discurso do capitalista, lança-se a hipótese de que a esquizofrenização no nível do discurso resulte na propagação do que Helene Deutsch convencionou chamar de como se. Esse fenômeno surgiria como uma suplência imaginária a que recorreria o sujeito como estabilização face aos efeitos decorrentes da foraclusão da castração no discurso do capitalista. Trata-se de um discurso psicotizante que, ao contrário dos quatro discursos apresentados por Lacan no seminário O avesso da psicanálise, não promove laço social. Se discurso é o que faz laço social e Freud, em 1930, anunciara que a principal fonte de sofrimento de que padece o homem é a relação com os demais, o mal-estar na civilização é o mal-estar dos laços sociais. Logo, os quatro discursos participam do mal-estar na civilização. Ao contrário destes, o discurso do capitalista, na tentativa de eliminar o mal-estar, foraclui o laço social. Por promover o gozo ao invés da renúncia à pulsão, o discurso do capitalista acaba por instigá-la. E, como toda pulsão é pulsão de morte, não é outra coisa senão o empuxo mortífero ao gozo que o discurso do capitalismo produz. A potência que o discurso do capitalista adquiriu na contemporaneidade é analisada a partir de sua íntima relação com o discurso da ciência. A partir de algumas colocações de Hannah Arendt acerca da banalidade do mal presente em um sistema totalitário como o nazista, cogita-se a hipótese de que a aliança entre os discursos do capitalista e da ciência resulte no surgimento de uma nova forma de totalitarismo: o totalitarismo de consumo. / This dissertation aims to address the vicissitudes of the discourse of the capitalist on the subject. For this purpose, it takes as a starting point Lacan statement in his lectures at Saint-Anne on The psychoanalysts knowledge, that what characterizes the discourse of the capitalist is the foreclosure of castration. From this statement - represented in the matheme of the discourse of the capitalist by the disappearance of the disjunction between product and truth, and by the absence of a vector between the agent and the Other, which shows that this discourse does not promote social bond - it traverses some issues that reverberate on the subject, among which stands out: if the subject does not exist apart from the social bond, what sort of effects does he suffer by following a discourse - which appears to be dominant in contemporary society - in which castration is foreclosed and, therefore, also the social bond? Since the Verwerfung is what functions in the discourse of the capitalist, there is the hypothesis that schizophrenizing at the level of the discourse could spread what Helene Deutsch conventionally called as if (als ob). This phenomenon emerges as an imaginary supplementation used by the subject to reach stabilization in view of the effects of castration foreclosure in the discourse of the capitalist. This is a psychosis-inducing discourse that, unlike the four discourses introduced by Lacan at the seminar Psychoanalysis Upside-Down, promotes no social bonding. If the discourse is what promotes social bond and Freud in 1930, announced that the main reason why men suffer is due to the relationship with others, the malaise in civilization is the malaise of social bonds. Thus, the four discourses participate in the malaise of civilization. Unlike these, the discourse of the capitalist, in an attempt to eliminate the malaise, forecloses the social bond. As it promotes enjoyment rather than the renunciation of drive, the discourse of the capitalist eventually instigate it. And, as every drive is a death drive, the discourse of the capitalist produces nothing but the deadly thrust to enjoyment. The power the discourse of the capitalist acquired in contemporary society is analyzed from its close relationship with the discourse of science. From some statements of Hannah Arendt on the banality of evil present in a totalitarian system, such as the Nazi, there is the hypothesis that the alliance between the discourses of the capitalist, and science results in the emergence of a new form of totalitarianism: the totalitarianism of consumption.

Made available in DSpace on 2015-05-15T11:46:23Z (GMT). No. of bitstreams: 1 arquivototal.pdf: 1404779 bytes, checksum: fa23dbf1324f104548ef91fcbbf20fba (MD5) Previous issue date: 2014-09-05 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES / In this work we study questions related to the existence of positive solutions for some classes of quasilinear Schrödinger equations, with hypotheses on the potential that permit this potential to vanish at infinity. In order to use variational methods to obtain our results, we make some changes of variables to obtain some semilinear equations, whose associated functionals are well defined in a classical Sobolev spaces. We also work with these equations on an Orlicz type space whose energy functional satisfy the geometric properties of the Mountain Pass Theorem. We still use the penalty technique due to Del Pino and Felmer and the Moser iteration method to obtain estimates in L1 norm, which are fundamental to our study. / Neste trabalho, estudamos questões relacionadas à existência de soluções positivas para algumas classes de equações de Schrödinger quasilineares, com hipóteses sobre o potencial que o possibilita se anular no infinito. Afim de usarmos métodos variacionais na obtenção de nossos resultados, aplicamos mudança de variáveis para reduzirmos as equações quasilineares a equações semilineares. Os funcionais associados a essas novas equações estão bem definidos em espaços de Sobolev clássicos e em espaços tipo Orlicz e satisfazem as propriedades geométricas do Teorema do Passo da Montanha. Ainda utilizamos a técnica de penalização de Del Pino e Felmer e o método de iteração de Moser para obtenção de estimativas, fundamentais para o nosso estudo, na norma L1.