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  • Ocean Drilling Program; ODP  (1)
  • Stokes' law radii  (1)
  • Wechselwirkung  (1)
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  • 1
    Keywords: Water-rock interaction ; Geochemistry ; Hydrogeology ; Konferenzschrift ; Aufsatzsammlung ; Wasser ; Gestein ; Wechselwirkung ; Hydrochemie ; Fluid-Fels-System ; Thermodynamik
    Type of Medium: Book
    Pages: XVII, 569 S , Ill., graph. Darst.
    ISBN: 9780939950843
    Series Statement: Reviews in mineralogy and geochemistry 70
    Language: English
    Note: Hier auch später erschienene, unveränderte Nachdrucke
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  • 2
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    PANGAEA
    In:  Supplement to: Mavromatis, Vasileios; Meister, Patrick; Oelkers, Eric H (2014): Using stable Mg isotopes to distinguish dolomite formation mechanisms: A case study from the Peru Margin. Chemical Geology, 385, 84-91, https://doi.org/10.1016/j.chemgeo.2014.07.019
    Publication Date: 2024-01-09
    Description: The magnesium isotope composition of diagenetic dolomites and their adjacent pore fluids were studied in a 250 m thick sedimentary section drilled into the Peru Margin during Ocean Drilling Program (ODP) Leg 201 (Site 1230) and Leg 112 (Site 685). Previous studies revealed the presence of two types of dolomite: type I dolomite forms at ~ 6 m below seafloor (mbsf) due to an increase in alkalinity associated with anaerobic methane oxidation, and type II dolomite forms at focused sites below ~ 230 mbsf due to episodic inflow of deep-sourced fluids into an intense methanogenesis zone. The pore fluid delta 26Mg composition becomes progressively enriched in 26Mg with depth from values similar to seawater (i.e. -0.8 per mil, relative to DSM3 Mg reference material) in the top few meters below seafloor (mbsf) to 0.8 ± 0.2 per mil within the sediments located below 100 mbsf. Type I dolomites have a delta 26Mg of -3.5 per mil, and exhibit apparent dolomite-pore fluid fractionation factors of about -2.6 per mil consistent with previous studies of dolomite precipitation from seawater. In contrast, type II dolomites have delta 26Mg values ranging from -2.5 to -3.0 per mil and are up to -3.6 per mil lighter than the modern pore fluid Mg isotope composition. The enrichment of pore fluids in 26Mg and depletion in total Mg concentration below ~ 200 mbsf is likely the result of Mg isotope fractionation during dolomite formation, The 26Mg enrichment of pore fluids in the upper ~ 200 mbsf of the sediment sequence can be attributed to desorption of Mg from clay mineral surfaces. The obtained results indicate that Mg isotopes recorded in the diagenetic carbonate record can distinguish near surface versus deep formed dolomite demonstrating their usefulness as a paleo-diagenetic proxy.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Journal of solution chemistry 18 (1989), S. 601-640 
    ISSN: 1572-8927
    Keywords: Limiting equivalent conductances ; Stokes' law radii ; apparent solvation numbers ; Walden product ; residual friction coefficient ; supercritical aqueous electrolytes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract The limiting equivalent conductances at temperatures from 0° to 1000°C and pressures from 1 to 5000 bars of a large number of aqueous ions have been calculated from limiting equivalent conductances of electrolytes reported in the literature. The limiting equivalent conductances of individual ions typically increase by a factor of about 15 with increasing temperatures from 0° to 1000°C and decrease about 30 percent with increasing pressure from 1 to 5 kb. The equivalent conductance of H2O approximated by the sum of the limiting equivalent conductances of H+ and OH− is essentially independent of pressure, but increases from about 350 to a maximum of approximately 1800 S-cm2-equiv−1 in response to an increase in temperature from 0° to 500°C at 1kb. Stokes' law radii and Walden products generated from the computed limiting equivalent conductances of ions exhibit changes over the temperature and pressure range of interest by as much as 100 percent for all of the ions except H+ and OH−, which vary by an order of magnitude. Apparent solvation numbers calculated as a function of pressure and temperature from the Stokes' law radii using the volume and dielectric constant of H2O and Born coefficients of the individual ions approach infinity at the critical point of H2O. Residual friction coefficients as a general rule approach zero as temperatures increases to 1000°C. The excess limiting equivalent conductances of the hydrogen and hydroxyl ions computed from the differences between the limiting equivalent conductances of HCl and KCl, and NaOH and NaCl, respectively, increases with increasing pressure, and maximize at 250°C.
    Type of Medium: Electronic Resource
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