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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
41

\" Atividades do 226 Ra águas subterrâneas extraídas de dois poços localizados no plúton meridional, granitóides de Morungaba, SP\" / Radium content in ground waters from two wells drilled in the Morungaba Batholith, Saõ Paulo, Brazil.

Fabio de Oliveira Lucas 18 May 2004 (has links)
Atividades específicas do 226Ra dissolvido foram medidas e atividades de 226Ra associado ao material em suspensão foram estimadas em águas subterrâneas extraídas de dois poços perfurados em granitos do Plúton Meridional, Granitóides de Morungaba, no leste do Estado de São Paulo. / Specifc activities of dissolved 226Ra isotope were measured and 226Ra isotope activities associated to suspended solids were estimated in ground waters drawn from two wells drilled in a fracturated granitic aquifer of the Meridional Pluton, Morungaba Granitoids, eastern São Paulo State.
42

Jesus the Samaritan : ethnic labeling in the Gospel of John

Penwell, Stewart K. January 2016 (has links)
This thesis will answer, “How do ethnic labels function in the Gospel of John?” In order to answer this question properly, this thesis draws on social-scientific theories on ethnic groups, deviancy, and labeling. The primary examples of ethnic labeling for this thesis are John 4:9 and 8:48. In each instance, members from “the Jews” (ʼΙουδαῖοι) and “Samaritans” label Jesus as a member of each other’s group. The Gospel of John’s dual ethnic labeling of Jesus participates in a history of discourse between “the Jews” and “Samaritans.” Both people groups adhere to an “us” versus “them” mentality because they both identify themselves as Israelites while rejecting the other group’s claim to that identity. The parameters of the discourse are determined by not only how each ethnic group identifies themselves but particularly how they construct the category for the other’s group. Once the parameters of discourse are in place, then we can address the function of ethnic labels in the Gospel of John. On both occasions Jesus is labeled because he deviates from what are deemed to be acceptable practices as a member of “the Jews.” The function of Jesus’s dual ethnic labeling in the Gospel of John is to establish a new pattern of practices and categories for the “children of God” who are a trans-ethnic group united as a fictive-kinship and who are embedded within the Judean ethnic group’s culture and traditions. The Johannine Jesus is portrayed as “the Jews’” Messiah (1:45; 20:31), who brings “salvation from the Jews” (4:22), and who is “the savior of the world” (4:42). The Gospel of John presents Jesus as broadening the more restrictive boundaries within “his own people” (1:11) in order to “draw all people to myself” (12:32).
43

Determinacao de sup226Ra e sup228Ra em aguas minerais da regiao de Aguas da Prata

OLIVEIRA, JOSELENE de 09 October 2014 (has links)
Made available in DSpace on 2014-10-09T12:37:30Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:03:31Z (GMT). No. of bitstreams: 1 05171.pdf: 1226633 bytes, checksum: a8a8ac2deed7ddd884b8a9228185c81d (MD5) / Dissertacao (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN/CNEN-SP
44

Determinacao de sup226Ra e sup228Ra em aguas minerais da regiao de Aguas da Prata

OLIVEIRA, JOSELENE de 09 October 2014 (has links)
Made available in DSpace on 2014-10-09T12:37:30Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:03:31Z (GMT). No. of bitstreams: 1 05171.pdf: 1226633 bytes, checksum: a8a8ac2deed7ddd884b8a9228185c81d (MD5) / Dissertacao (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN/CNEN-SP
45

Avaliação da concentração de atividade de Ra-226, Ra-228 e Pb-210 em sedimentos provenientes da Antártica na região da Baía do Almirantado / Evaluation of the activity concentration of 226Ra, 228Ra and 210Pb in sediments from Antarctica in the admiralty bay region

Mora, Tamires de Araujo 08 December 2015 (has links)
Os radionuclídeos naturais das séries radioativas do 238U, 235U e 232Th são frequentemente utilizados como traçadores em estudos ambientais para a compreensão da dinâmica que ocorre no ambiente marinho e terrestre, como por exemplo, em pesquisas de processos oceânicos e gerenciamento da região costeira. No ambiente marinho, estes radionuclídeos podem ser empregados para estimar fluxos biogeoquímicos de partículas e de nutrientes que ocorrem tanto na coluna dágua, quanto nos sedimentos. Várias pesquisas aplicam a distribuição e o respectivo desequilíbrio dos radionuclídeos naturais no meio ambiente, inclusive em modelos geocronológicos para se obter informações históricas em testemunhos sedimentares. Nesse estudo, realizou-se a caracterização radioquímica das distribuições de 226Ra, 228Ra e 210Pb de uma coluna sedimentar denominada 1B (248 cm de comprimento), coletada na Baía do Almirantado, Antártica. A metodologia utilizada incluiu a lixiviação ácida de amostras de sedimentos, seguida de separação radioquímica sequencial de 226Ra e de 228Ra pela co-precipitação com Ba(Ra)SO4 e de 210Pb pela co-precipitação com PbCrO4. Todas as medidas foram realizadas pela contagem alfa e beta total dos precipitados obtidos, em um detector proporcional de fluxo gasoso de baixa radiação de fundo. As concentrações de atividade de 226Ra e 210Pb foram empregadas para se estimar a atividade de 210Pbnão-suportado presentes no perfil sedimentar 1B. Considerando-se as concentrações de atividade de 210Pbnão-suportado obtidas e a aplicação do modelo CIC(Constant Initial Concentration), foi possível determinar a taxa de sedimentação de 0,59±0,05 cm/ ano. / The natural radionuclides from radioactive series of 238U, 235U and 232Th have been applied as tracers in environmental studies for understanding the dynamics that occur in both marine and terrestrial environment, as for example, in research of oceanic processes and management of the coastal region. In the marine environment, these radionuclides can be used to estimate biogeochemical fluxes of marine particles and nutrients that occur in the water column as well as in the sediment. Several research works applied the distribution and the respective disequilibrium degree of natural radionuclides in the environment, including geochronological models for obtaining historical information on samples of certain sediment profile. In this study we performed a radiochemical characterization of the distribution of 226Ra, 228Ra and 210Pb from a sedimentary column called 1B (248 cm long) collected in the Admiralty Bay, Antarctic Peninsula region. The methodology used included the acid leaching of sediment samples followed by the radiochemical sequential separation of 226Ra and 228Ra by co-precipitation with Ba(Ra)SO4 and 210Pb by co-precipitation with PbCrO4. All measurements were carried out by counting of gross alpha and gross beta measures in a low background gas flow proportional detector. The activity concentrations of 226Ra and 210Pb were used to estimate the unsupported 210Pb activities present in sediment profile 1 B. Based on unsupported 210Pb data and the application of the CIC model (Constant Initial Concentration), it was possible to determine the sedimentation rate of 0.59 ± 0.05 cm /year.
46

Avaliação da concentração de atividade de Ra-226, Ra-228 e Pb-210 em sedimentos provenientes da Antártica na região da Baía do Almirantado / Evaluation of the activity concentration of 226Ra, 228Ra and 210Pb in sediments from Antarctica in the admiralty bay region

Tamires de Araujo Mora 08 December 2015 (has links)
Os radionuclídeos naturais das séries radioativas do 238U, 235U e 232Th são frequentemente utilizados como traçadores em estudos ambientais para a compreensão da dinâmica que ocorre no ambiente marinho e terrestre, como por exemplo, em pesquisas de processos oceânicos e gerenciamento da região costeira. No ambiente marinho, estes radionuclídeos podem ser empregados para estimar fluxos biogeoquímicos de partículas e de nutrientes que ocorrem tanto na coluna dágua, quanto nos sedimentos. Várias pesquisas aplicam a distribuição e o respectivo desequilíbrio dos radionuclídeos naturais no meio ambiente, inclusive em modelos geocronológicos para se obter informações históricas em testemunhos sedimentares. Nesse estudo, realizou-se a caracterização radioquímica das distribuições de 226Ra, 228Ra e 210Pb de uma coluna sedimentar denominada 1B (248 cm de comprimento), coletada na Baía do Almirantado, Antártica. A metodologia utilizada incluiu a lixiviação ácida de amostras de sedimentos, seguida de separação radioquímica sequencial de 226Ra e de 228Ra pela co-precipitação com Ba(Ra)SO4 e de 210Pb pela co-precipitação com PbCrO4. Todas as medidas foram realizadas pela contagem alfa e beta total dos precipitados obtidos, em um detector proporcional de fluxo gasoso de baixa radiação de fundo. As concentrações de atividade de 226Ra e 210Pb foram empregadas para se estimar a atividade de 210Pbnão-suportado presentes no perfil sedimentar 1B. Considerando-se as concentrações de atividade de 210Pbnão-suportado obtidas e a aplicação do modelo CIC(Constant Initial Concentration), foi possível determinar a taxa de sedimentação de 0,59±0,05 cm/ ano. / The natural radionuclides from radioactive series of 238U, 235U and 232Th have been applied as tracers in environmental studies for understanding the dynamics that occur in both marine and terrestrial environment, as for example, in research of oceanic processes and management of the coastal region. In the marine environment, these radionuclides can be used to estimate biogeochemical fluxes of marine particles and nutrients that occur in the water column as well as in the sediment. Several research works applied the distribution and the respective disequilibrium degree of natural radionuclides in the environment, including geochronological models for obtaining historical information on samples of certain sediment profile. In this study we performed a radiochemical characterization of the distribution of 226Ra, 228Ra and 210Pb from a sedimentary column called 1B (248 cm long) collected in the Admiralty Bay, Antarctic Peninsula region. The methodology used included the acid leaching of sediment samples followed by the radiochemical sequential separation of 226Ra and 228Ra by co-precipitation with Ba(Ra)SO4 and 210Pb by co-precipitation with PbCrO4. All measurements were carried out by counting of gross alpha and gross beta measures in a low background gas flow proportional detector. The activity concentrations of 226Ra and 210Pb were used to estimate the unsupported 210Pb activities present in sediment profile 1 B. Based on unsupported 210Pb data and the application of the CIC model (Constant Initial Concentration), it was possible to determine the sedimentation rate of 0.59 ± 0.05 cm /year.
47

Estudo dos radionuclídeos naturais - Ra-226, Ra-228 e Pb-210 - em alguns registros sedimentares do Atlântico Sudoeste ao longo do Holoceno / Study of natural radionuclides - 226Ra, 228Ra and 210Pb - in marine sediment cores from Southwest Atlantic during the Holocene

Costa, Alice Miranda Ribeiro 19 August 2016 (has links)
Os radionuclídeos naturais das séries radioativas do 238U e do 232Th têm sido aplicados com sucesso como traçadores de processos ambientais atuais e mudanças climáticas. O 210Pb (meia-vida de 22,2 anos) é empregado na técnica de datação geocronológica de testemunhos sedimentares dos últimos 100-150 anos e na determinação de taxa de sedimentação. As concentrações dos isótopos 226Ra e 228Ra (meia-vida de 1.600 anos e 5,75 anos, respectivamente) auxiliam no cálculo das atividades de 210Pb em excesso no sedimento e auxiliam na identificação de processos marinhos importantes, como, por exemplo, a intrusão de água subterrânea. Neste trabalho foram quantificadas as concentrações de atividade de 226Ra, 228Ra e 210Pb em quatro testemunhos marinhos curtos coletados desde a plataforma continental até o talude superior do Atlântico Sudoeste. A partir dos resultados obtidos, as taxas de sedimentação em cada local e as idades de cada fatia de sedimento foram determinadas pelo método de datação geocronológica com 210Pb. As amostras sedimentares sofreram digestão total ácida em microondas. A separação radioquímica sequencial de 226Ra, 228Ra e 210Pb foi realizada com a obtenção dos precipitados de Ba(Ra)SO4 e PbCrO4. As medidas α total do 226Ra e β total do 228Ra e do 210Pb a partir dos precipitados foram feitas em um detector proporcional de fluxo gasoso de baixa radiação de fundo. Com relação aos testemunhos analisados, as concentrações de atividade dos radionuclídeos variaram de 14 Bq.kg-1 a 154 Bq.kg-1 para o 226Ra; de 17 Bq.kg-1 a 45 Bq.kg-1 para o 228Ra; de 20 Bq.kg-1 a 2.073 Bq.kg-1 para o 210Pb. Valores altos de 210Pb foram encontrados no topo de todos os perfis sedimentares, proveniente principalmente da deposição atmosférica. Os dados coletados neste trabalho estão na mesma faixa de grandeza de outros relacionados a medições de 226Ra, 228Ra, 210Pb em áreas não contaminadas do Oceano Atlântico Sudoeste. As taxas de sedimentação diminuíram com o aumento da profundidade de coluna dágua, cujos valores variaram de 0,049 cm.ano-1 a 0,40 cm.ano-1. / Natural radionuclides from 238U and 232Th series have been successfully applied as tracers of environmental process and climate changes. The 210Pb (half-life of 22.2 years) is used in the geochronological dating technique of sediment cores of the last 100-150 years, and its respective sedimentation rate determination. The study of 226Ra and 228Ra concentrations (half-lives of 1,600 years and 5.75 years, respectively) helps calculate the activity of 210Pb in excess in the environment, besides being important tracers of marine processes, as ground water discharge. In this work it was determined the activity concentrations of 226Ra, 228Ra and 210Pb in four short marine cores collected since the continental platform to upper slope of Southwest Atlantic Ocean. Taking into account the results obtained, sedimentation rates and the ages of each sediment layer were determined using the geochronological dating method with 210Pb. All sediment samples were total acid digested in microwave. The sequential radiochemical separation of 226Ra, 228Ra, 210Pb were performed, obtaining in the end the precipitation of Ba(Ra)SO4 and PbCrO4. The gross α measurements of 226Ra and gross β measurements of 228Ra and 210Pb from the precipitates were carried out in a gas-flow low background proportional counter. Concerning all cores analyzed, the activities concentrations of 226Ra ranged from 14 Bq.kg-1 to 154 Bq.kg-1; the concentrations of 228Ra ranged from 17 Bq.kg-1 to 45 Bq.kg-1; and the concentrations of 210Pb ranged from 20 Bq.kg-1 to 2,073 Bq.kg-1. High values of 210Pb were observed on the top of all the cores studied, mainly related to atmospheric deposition. The results obtained in this work were of the same order of magnitude of those reported in the literature available on non contaminated areas of Southeast Brazilian Coast. Sedimentation rates fall with the increase of water column depth and ranged from 0,049 cm.ano-1 to 0.40 cm.y-1.
48

Estudo dos radionuclídeos naturais - Ra-226, Ra-228 e Pb-210 - em alguns registros sedimentares do Atlântico Sudoeste ao longo do Holoceno / Study of natural radionuclides - 226Ra, 228Ra and 210Pb - in marine sediment cores from Southwest Atlantic during the Holocene

Alice Miranda Ribeiro Costa 19 August 2016 (has links)
Os radionuclídeos naturais das séries radioativas do 238U e do 232Th têm sido aplicados com sucesso como traçadores de processos ambientais atuais e mudanças climáticas. O 210Pb (meia-vida de 22,2 anos) é empregado na técnica de datação geocronológica de testemunhos sedimentares dos últimos 100-150 anos e na determinação de taxa de sedimentação. As concentrações dos isótopos 226Ra e 228Ra (meia-vida de 1.600 anos e 5,75 anos, respectivamente) auxiliam no cálculo das atividades de 210Pb em excesso no sedimento e auxiliam na identificação de processos marinhos importantes, como, por exemplo, a intrusão de água subterrânea. Neste trabalho foram quantificadas as concentrações de atividade de 226Ra, 228Ra e 210Pb em quatro testemunhos marinhos curtos coletados desde a plataforma continental até o talude superior do Atlântico Sudoeste. A partir dos resultados obtidos, as taxas de sedimentação em cada local e as idades de cada fatia de sedimento foram determinadas pelo método de datação geocronológica com 210Pb. As amostras sedimentares sofreram digestão total ácida em microondas. A separação radioquímica sequencial de 226Ra, 228Ra e 210Pb foi realizada com a obtenção dos precipitados de Ba(Ra)SO4 e PbCrO4. As medidas α total do 226Ra e β total do 228Ra e do 210Pb a partir dos precipitados foram feitas em um detector proporcional de fluxo gasoso de baixa radiação de fundo. Com relação aos testemunhos analisados, as concentrações de atividade dos radionuclídeos variaram de 14 Bq.kg-1 a 154 Bq.kg-1 para o 226Ra; de 17 Bq.kg-1 a 45 Bq.kg-1 para o 228Ra; de 20 Bq.kg-1 a 2.073 Bq.kg-1 para o 210Pb. Valores altos de 210Pb foram encontrados no topo de todos os perfis sedimentares, proveniente principalmente da deposição atmosférica. Os dados coletados neste trabalho estão na mesma faixa de grandeza de outros relacionados a medições de 226Ra, 228Ra, 210Pb em áreas não contaminadas do Oceano Atlântico Sudoeste. As taxas de sedimentação diminuíram com o aumento da profundidade de coluna dágua, cujos valores variaram de 0,049 cm.ano-1 a 0,40 cm.ano-1. / Natural radionuclides from 238U and 232Th series have been successfully applied as tracers of environmental process and climate changes. The 210Pb (half-life of 22.2 years) is used in the geochronological dating technique of sediment cores of the last 100-150 years, and its respective sedimentation rate determination. The study of 226Ra and 228Ra concentrations (half-lives of 1,600 years and 5.75 years, respectively) helps calculate the activity of 210Pb in excess in the environment, besides being important tracers of marine processes, as ground water discharge. In this work it was determined the activity concentrations of 226Ra, 228Ra and 210Pb in four short marine cores collected since the continental platform to upper slope of Southwest Atlantic Ocean. Taking into account the results obtained, sedimentation rates and the ages of each sediment layer were determined using the geochronological dating method with 210Pb. All sediment samples were total acid digested in microwave. The sequential radiochemical separation of 226Ra, 228Ra, 210Pb were performed, obtaining in the end the precipitation of Ba(Ra)SO4 and PbCrO4. The gross α measurements of 226Ra and gross β measurements of 228Ra and 210Pb from the precipitates were carried out in a gas-flow low background proportional counter. Concerning all cores analyzed, the activities concentrations of 226Ra ranged from 14 Bq.kg-1 to 154 Bq.kg-1; the concentrations of 228Ra ranged from 17 Bq.kg-1 to 45 Bq.kg-1; and the concentrations of 210Pb ranged from 20 Bq.kg-1 to 2,073 Bq.kg-1. High values of 210Pb were observed on the top of all the cores studied, mainly related to atmospheric deposition. The results obtained in this work were of the same order of magnitude of those reported in the literature available on non contaminated areas of Southeast Brazilian Coast. Sedimentation rates fall with the increase of water column depth and ranged from 0,049 cm.ano-1 to 0.40 cm.y-1.
49

Genre of Acts and collected biography

Adams, Sean A. January 2011 (has links)
This thesis argues that the best genre parallel for the Acts of the Apostles is collected biography. This conclusion is reached through an application of ancient and modern genre theory and a detailed comparison of Acts and collected biographies. Chapter 1 offers prolegomena to this study and further delineates the contours of the thesis. Chapter 2 provides an extensive history of research, not only to provide the context and rationale for the present work, but also to indicate some of the shortcomings of previous investigations and the need for this present study. Chapter 3 presents the methodological perspective for this exploration. Making use of ancient and modern genre theory, I propose that scholars need to understand genre as a dynamic and flexible system that is culturally influenced and highly adaptable. In Chapter 4 I trace the diachronic development of ancient biographies, describe different sub-divisions, and note the strong, enduring relationship between biography and history. In evaluating the development of biography as a whole, there appears to be a distinct preference by ancient biographers for collected biographies. Chapters 5 to 7 interpret Acts in light of its possible relationship with collected biographies. Chapter 5 provides a detailed comparison of the structural and content features of history, novels, collected biographies, and Acts. Overall, this chapter argues that the structural and content features of Acts are most strongly related to the genre of biography and, secondarily, to history. Chapters six and seven evaluate Acts as a modified collected biography, identifying notable similarities in content features, structure, and endings. Chapter 8 summarizes and concludes the thesis, along with a brief mention of avenues for future research. Related literary investigations, such as a list of literary topoi references in biographies, biographies referenced by Diogenes Laertius, and a full discussion of biography’s adaptability in the first century (modelled by Plutarch and Philo), are treated in appendices.
50

Language and identity in ancient narratives : the relationship between speech patterns and social context in the Acts of the Apostles, Acts of John, and Acts of Philip

Snyder, Julia Ann January 2013 (has links)
Drawing on insights from sociolinguistics, the thesis investigates the relationship between speech patterns and social context in three ancient Greek narratives: the Acts of the Apostles, Acts of John, and Acts of Philip. The thesis explores how characters’ speech patterns correlate with their Christian status, and with the Christian status of their addressees. The relationship between speech patterns and gentile/Jewish identity is also assessed. Linguistic variables include plural forms of address and third-person references to Jesus and the Christian god. The thesis shows that Christian characters are portrayed as speaking differently amongst themselves than when addressing non-Christian characters. It also demonstrates that parameters of sociolinguistic variation in each text point to differing understandings of Christian identity. It is argued that attention to sociolinguistic relationships highlights the importance of ascetic practices and baptism in the Acts of Philip, the gradual nature of Christian conversion in the Acts of John, and the close relationship between Jewish and Christian identity in the Acts of the Apostles. The thesis also examines characterization and implied audience, and argues that attention to social context is necessary to appreciate the full significance of an author’s choice of words.

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