GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Keywords
Language
  • 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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-01-09
    Keywords: 112-685A; 201-1230A; Comment; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Latitude of event; Leg112; Leg201; Longitude of event; Main Lithology; MC-ICP-MS Thermo-Finnigan Neptune; Ocean Drilling Program; ODP; Replicates; Sample code/label; South Pacific Ocean; Traces; δ25Mg; δ25Mg, standard deviation; δ26Mg; δ26Mg, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2024-01-09
    Keywords: 201-1230A; 201-1230B; 201-1230D; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg201; Magnesium; MC-ICP-MS Thermo-Finnigan Neptune; Ocean Drilling Program; ODP; Replicates; Sample code/label; Sample ID; South Pacific Ocean; δ25Mg; δ25Mg, standard deviation; δ26Mg; δ26Mg, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 142 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2024-01-09
    Keywords: 112-685; 112-685A; 201-1230A; Calcite; Carbon, inorganic, total; Clay minerals; Comment; COMPCORE; Composite Core; DEPTH, sediment/rock; Description; Dolomite; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Feldspar; Joides Resolution; Leg112; Leg201; Magnesium-Calcite; Ocean Drilling Program; ODP; Quartz; Sample code/label; Sample type; South Pacific Ocean; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 386 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2019-09-23
    Description: Magnesium calcites were synthesized from aqueous solutions supersaturated with respect to calcite at 25, 40, 60, and 80 °C in gas tight batch reactors for up to 35 days. Any amorphous material still present in the precipitates was removed using a partial dissolution treatment. Resulting purified Mg-calcite had Mg contents ranging from 6 to 32 mol% MgCO3. An isotopic steady-state was attained between the fluid and the precipitated solids within two weeks at 25 °C. δ18O values derived from the experiments at steady-state, depend on both temperature and the Mg content of the calcite in accord with: 1000lnαMg-calcite–H2O=18,030/T−32.42+(6×108/T3–5.47×106/T2+16,780/T−17.21)×CMg where αMg-calcite–H2O represents the calcite–water oxygen isotope fractionation factor, T refers to the temperature in °K and CMg denotes the mole percent of MgCO3 in the calcite. These results indicate that the addition of 5 mol% MgCO3 into the calcite increases 1000lnαMg-calcite–H2O by 0.88 as compared to that of pure calcite at 25 °C. This difference could lead to a 4.2 °C decrease in estimated formation temperature estimates. These results demonstrate that the accurate interpretation of oxygen isotope fractionation in magnesium calcites requires explicit provision for the effect of magnesium on oxygen isotope fractionation factors. Highlights ► The effect of Mg on calcite–aqueous fluid oxygen isotope fractionation was investigated. ► Mg incorporation is increasing the calcite–aqueous fluid oxygen isotope fractionation. ► This effect is reduced at higher temperatures. ► Obtained results are important for paleo-temperature estimation. Gadget timed out while loading
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2023-02-08
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2023-02-08
    Description: Fluid-rock interactions in hydrothermal systems at or near mid-oceanic ridges (MOR) play a major role in determining the composition of the oceanic crust and seawater. To quantify the processes that govern cation exchange in these environments we have experimentally studied the isotopic evolution of δ26/24Mg in the fluid phase during seawater-basalt interaction at 250 and 290 °C. Mass balance constraints indicate that isotopically heavy Mg was preferentially incorporated into non-exchangeable (octahedral) sites in secondary clay minerals such as saponite (Mg-rich smectite), leaving residual fluids enriched in light Mg isotopes. The magnitude of fractionation observed during smectite precipitation in our experiments () ranged from ‰ to ‰. This observation, which contrasts with the preferential uptake of light Mg isotopes into biogenic and inorganic marine carbonates, highlights the potential utility of Mg isotopes as tracers of the precipitation dynamics of authigenic Mg-silicate and Mg-carbonate phases. Furthermore, although Mg isotopic fractionation is often masked by the almost complete removal of Mg in high temperature marine hydrothermal systems, our experiments demonstrate that it does become significant at lower temperatures where Mg removal by clay formation is incomplete. Under such conditions, this fractionation will create isotopically light fluids due to smectite precipitation, thus potentially represents an important component of the marine Mg isotope inventory.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...