992 resultados para Vialart, Charles, d. 1644.


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We have measured the concentrations of (1) pore-water sulfide and (2) solid-phase pyrite, iron monosulfide (=acid volatile sulfide), elemental sulfur, and extractable and nonextractable organic ("kerogen") sulfur in sediments from Ocean Drilling Program (ODP) Sites 680 and 686. Pore-water sulfide defines classic "bell-shaped" profiles. Maximum concentrations of 6 to 12 mM occur where sulfate is exhausted, or is most depleted, at depths between 15 and 50 mbsf. Sulfide resulting from bacterial sulfate reduction reacts in three ways: (1) some is reoxidized to elemental sulfur in surface sediments; (2) some reacts with detrital iron minerals to form iron monosulfide and pyrite, primarily in the top meter or two of the sediment; and (3) some reacts with, and is incorporated into, kerogen. Incorporation of reduced sulfur into kerogen occurs over the top 15 m of the sediment at both Sites 680 and 686, after the main phase of pyrite formation. Up to 45% of the total sedimentary sulfur is organically bound, and concentrations of 12 wt% sulfur are reached in the kerogen. These values are like those measured in lithologically similar, but more deeply buried, sediments from the Monterey Formation.

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"Contract no. 53-319R-9-90."

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At head of title: Trois chansons.

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Mode of access: Internet.

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Bibliography: p. 71-72.

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Contents: v. 1. Early Period, from the Ascencion of Our Lord to the Conversion of Constantine -- v. 2. Early Middle Period, from the Edict of Milan to the establishments of the new Western Empire under the Carlovingians, the temporal power of the Popes, and the coming into being of the States of the Church (1931) -- v. 3. To the s-called Reformation -- v. 4. Reformation to the triumph of the Papcy in the restoration of the temporal power in 1929 under Pope Pius XI.

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Las 23 p. contienen: "Extrait des registres de l'Academie Royale des Sciences du 23 Août 1752, discussion de la dispute de M. Winslow & de M. Ferrein"