Diário da Constituinte [gravação de vídeo] : [programa n. 680 2ª ed.]

Os constituintes já garantiram vários aspectos dos direitos individuais e coletivos. Já aprovaram 27 incisos, mas faltam 57. Os direitos já foram garantidos: habeas data, defesa do consumidor, racismo como crime inafiançável, mandado de segurança e injunção. Os constituintes pedem maior rigor aos faltantes. O presidente Ulysses solicita a presença em plenário para a votação do 2º turno da Assembléia Constituinte, que deverá votar 708 destaques.

Medida Provisória nº 680, de 2015

A MP 680/2015 institui o Programa de Proteção ao Emprego – PPE, que permite que a empresa, mediante acordo coletivo, reduza a jornada e o salário de seus empregados em até trinta por cento, sendo garantida uma compensação pecuniária equivalente a cinquenta por cento do valor da redução salarial

Diário da Constituinte [gravação de vídeo] : [programa n. 680 2ª ed.]

Ulysses Guimarães faz apelo para a votação do segundo turno, que deve terminar o Capítulo das Liberdades Individuais e Coletivas, ainda faltam 56 incisos para votação neste capítulo. Já foram aprovados 27 incisos e são dados como certo de aprovação: o habeas data, a defesa do consumidor, racismo, o mandado de injunção e coletivo. Os direitos individuais recebem o apoio de todos os setores. Ulysses Guimarães apela para que os constituintes compareçam para a votação do 2º turno para apreciar 708 destaques.

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 680 - Mitteilung über die Bankgeschäfte mit dem Bankhaus Muhl

u.a.: Vorschläge Johanna Schopenhauers über die Aufteilung der Erbschaft;

Na 1 Nachlass Max Horkheimer, 680 - "Antisemitism among American Labor" Band III (p. IX 146.1 Bd III)

"Antisemitism among American Labor. Report on a Research Project conducted by the Institute of Social Research in 1944-1945". Typoskript, in 4 Bänden gebunden, 1450 Blatt;

Contents, partition, and isotopic composition of sulphur in sediments from ODP Sites 680 and 686

We have determined (1) the abundance and isotopic composition of pyrite, monosulphide, elemental sulphur, organically bound sulphur, and dissolved sulphide; (2) the partition of ferric and ferrous iron; (3) the organic carbon contents of sediments recovered at two sites drilled on the Peru Margin during Leg 112 of the Ocean Drilling Program. Sediments at both sites are characterised by high levels of organically bound sulphur (OBS). OBS comprises up to 50% of total sedimentary sulphur and up to 1% of bulk sediment. The weight ratio of S to C in organic matter varies from 0.03 to 0.15 (mean = 0.10). Such ratios are like those measured in lithologically similar, but more deeply buried petroleum source rocks of the Monterey and Sisquoc formations in California. The sulphur content of organic matter is not limited by the availability of porewater sulphide. Isotopic data suggest that sulphur is incorporated into organic matter within a metre of the sediment surface, at least partly by reaction with polysulphides. Most inorganic Sulphur occurs as pyrite. Pyrite formation occurred within surface sediments and was limited by the availability of reactive iron. But despite highly reducing sulphidic conditions, only 35-65% of the total iron was converted to sulphide; 10-30% of the total iron still occurs as Fe(III). In surface sediments, the isotopic composition of pyrite is similar to that of both iron monosulphide and dissolved sulphide. Either pyrite, like monosulphide, formed by direct reaction between dissolved sulphide and detrital iron, and/or the sulphur species responsible for converting FeS to FeS2 is isotopically similar to dissolved sulphide. Likely stoichiometries for the reaction between ferric iron and excess sulphide imply a maximum resulting FeS2:FeS ratio of 1:1. Where pyrite dominates the pool of iron sulphides, at least some pyrite must have formed by reaction between monosulphide and elemental sulphur and/or polysulphide. Elemental sulphur (S°) is most abundant in surface sediments and probably formed by oxidation of sulphide diffusing across the sediment-water interface. In surface sediments, S° is isotopically heavier than dissolved sulphide, FeS and FeS2 and is unlikely to have been involved in the conversion of FeS to FeS2. Polysulphides are thus implicated as the link between FeS and FeS2.