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Cidadãos mostram sua insatisfação com o salário mínimo. O Deputado Vilson de Souza (PMDB-SC) declara que a Constituição pode melhorar a vida das pessoas garantindo um piso salarial mínimo e que as políticas econômicas adotadas nos últimos anos têm arrochado brutalmente a massa salarial. O Deputado Jesus Tajra (PFL-PI) acredita que o salário deve ser estabelecido na livre negociação entre sindicatos de trabalhadores e sindicatos patronais. O Deputado Vitor Buaiz (PT-ES) informa que é preciso que o salário minimo seja reformulado, de tal forma que se torne suficiente para satisfazer também as necessidades das famílias em relação a educação, saúde e lazer. Sessão da Comissão de Sistematização da Assembleia Nacional Constituinte (ANC) discute a qualidade da alimentação dos brasileiros. O Deputado Manuel Viana (PMDB-CE) defende a implantação do Sistema Único de Saúde como forma de fiscalizar a qualidade dos remédios e dos alimentos. Parlamentaristas chegam a um acordo sobre o sistema de governo e o novo texto do substitutivo. O texto apresentado ao substitutivo é uma fusão das teses dos Senadores Afonso Arinos (PFL-RJ), Nelson Carneiro (PMDB-RJ) e Carlos Chiarelli (PDS-RS). O Relator Adjunto, Senador José Ignácio Ferreira (PMDB-ES) anuncia como ficará no substitutivo a questão da jornada de trabalho, da aposentadoria e do tráfico de drogas. O tempo de implantação do sistema parlamentarista e a imissão de posse ainda ficaram pendentes e serão decididos no Plenário pelo voto.

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60MeV/u18O离子与232Th反应产生放射性Ba同位素。通过3次BaCl2沉淀,将Ba从大量的Th和其他反应产物混合物中分离出来。使用离线!谱学方法完成Ba样品!活性的测量。根据各个Ba同位素的特征!射线峰的活度和其他相关数据,得到Ba同位素的产生截面。

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Documento de 76 fotografías, setenta y una a color.

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This latest edition of J. S. Bach’s B-minor Mass, by Ulrich Leisinger, described by the publisher as a ‘hybrid edition’, aptly addresses the needs of present-day performers and at the same time fulfils the scholarly expectations of new critical editions to conform to the current study environment

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New data show that island arc rocks have (Pb-210/Ra-226)(o) ratios which range from as low as 0.24 up to 2.88. In contrast, (Ra-22S/Th-232) appears always within error of I suggesting that the large Ra-226-excesses observed in arc rocks were generated more than 30 years ago. This places a maximum estimate on melt ascent velocities of around 4000 m/year and provides further confidence that the Ra-226 excesses reflect deep (source) processes rather than shallow level alteration or seawater contamination. Conversely, partial melting must have occurred more than 30 years prior to eruption. The Pb-210 deficits are most readily explained by protracted magma degassing. Using published numerical models, the data suggest that degassing occurred continuously for periods up to several decades just prior to eruption but no link with eruption periodicity was found. Longer periods are required if degassing is discontinuous, less than 100% efficient or if magma is recharged or stored after degassing. The long durations suggest much of this degassing occurs at depth with implications for the formation of hydrothermal and copper-porphyry systems. A suite of lavas erupted in 1985-1986 from Sangeang Api volcano in the Sunda arc are characterised by deficits of Pb-210 relative to Ra-226 from which 6-8 years of continuous Rn-222 degassing would be inferred from recent numerical models. These data also form a linear (Pb-210)/Pb-(Ra-226)/Pb array which might be interpreted as a 71-year isochron. However, the array passes through the origin suggesting displacement downwards from the equiline in response to degassing and so the slope of the array is inferred not to have any age significance. Simple modelling shows that the range of (Ra-226)/Pb ratios requires thousands of years to develop consistent with differentiation occurring in response to cooling at the base of the crust. Thus, degassing post-dated, and was not responsible for magma differentiation. The formation, migration and extraction of gas bubbles must be extremely efficient in mafic magma whereas the higher viscosity of more siliceous magmas retards the process and can lead to Pb-210 excesses. A possible negative correlation between (Pb-210/Ra-226)(o) and SO2 emission rate requires further testing but may have implications for future eruptions. (C) 2004 Elsevier B.V. All rights reserved.

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New data show that island arc rocks have (Pb-210/Ra-226)(o) ratios which range from as low as 0.24 up to 2.88. In contrast, (Ra-22S/Th-232) appears always within error of I suggesting that the large Ra-226-excesses observed in arc rocks were generated more than 30 years ago. This places a maximum estimate on melt ascent velocities of around 4000 m/year and provides further confidence that the Ra-226 excesses reflect deep (source) processes rather than shallow level alteration or seawater contamination. Conversely, partial melting must have occurred more than 30 years prior to eruption. The Pb-210 deficits are most readily explained by protracted magma degassing. Using published numerical models, the data suggest that degassing occurred continuously for periods up to several decades just prior to eruption but no link with eruption periodicity was found. Longer periods are required if degassing is discontinuous, less than 100% efficient or if magma is recharged or stored after degassing. The long durations suggest much of this degassing occurs at depth with implications for the formation of hydrothermal and copper-porphyry systems. A suite of lavas erupted in 1985-1986 from Sangeang Api volcano in the Sunda arc are characterised by deficits of Pb-210 relative to Ra-226 from which 6-8 years of continuous Rn-222 degassing would be inferred from recent numerical models. These data also form a linear (Pb-210)/Pb-(Ra-226)/Pb array which might be interpreted as a 71-year isochron. However, the array passes through the origin suggesting displacement downwards from the equiline in response to degassing and so the slope of the array is inferred not to have any age significance. Simple modelling shows that the range of (Ra-226)/Pb ratios requires thousands of years to develop consistent with differentiation occurring in response to cooling at the base of the crust. Thus, degassing post-dated, and was not responsible for magma differentiation. The formation, migration and extraction of gas bubbles must be extremely efficient in mafic magma whereas the higher viscosity of more siliceous magmas retards the process and can lead to Pb-210 excesses. A possible negative correlation between (Pb-210/Ra-226)(o) and SO2 emission rate requires further testing but may have implications for future eruptions. (C) 2004 Elsevier B.V. All rights reserved.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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