Data for: On the role of density-driven dissolution of CO2 in phreatic karst 
systems

Class, H.; Bürkle, P.; Trötschler, O.; Strauch [Beeskow-Strauch], B.; Zimmer, Martin

doi:10.18419/darus-2040

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Data for: On the role of density-driven dissolution of CO2 in phreatic karst systems

Urheber*innen

Class, H.
External Organizations;

Bürkle, P.
External Organizations;

Trötschler, O.
External Organizations;

/persons/resource/betti

Strauch [Beeskow-Strauch], B.
3.1 Inorganic and Isotope Geochemistry, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/weihei

Zimmer, Martin
3.1 Inorganic and Isotope Geochemistry, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Externe Ressourcen

https://doi.org/10.1002/essoar.10507661.1
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Zitation

Class, H., Bürkle, P., Trötschler, O., Strauch [Beeskow-Strauch], B., Zimmer, M. (2021): Data for: On the role of density-driven dissolution of CO2 in phreatic karst systems.
https://doi.org/10.18419/darus-2040

Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5009088

Zusammenfassung

Data of the "density-driven dissolution of CO2 in karst water" column experiment. A laboratory column was filled with tapwater (water level 5,55 m) and exposed it to an elevated gaseous CO2-concentration, roughly 50 times the current atmospheric concentration (20000 +/- 5000 ppm). After stripping the water with ambient air, it was initially in equilibrium with atmospheric conditions. Then, the concentration of dissolved CO2 was measured over a time period of 60 days in two different depths in the column. Measuring points are in the column air, 1 m below water level and 0,15 m above ground. CO2-air concentration was provided using an air-membrane pump (KNF N86 KTE) and a 100 l TEDLAR bag (for more detailed information look into the related publication Class 2021 et al.)