Abstract
Summary: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.)Raw Data:Raw data provided by GMP252 CO2 sensor probes, data accessed from ADL-MX Advanced Datalogger via ADL-C softwareSensor positions:CO2_10: column airCO2_20: 1 m below water surfaceCO2_40: 0.15 m above ground/5.40 m below water surfaceProcessed Data:Processed Data calculated after formula in the related publication Class 2021 et al.MC: manufacturer correctionOC: own correctionSherwood:Calculations for Sherwood number. The density was calculated by an approach of Garcia 2001For further information look into the related publication Class 2021 et al.Buerkle2021a:The dumux-pub module used to simulate the different scenarios in the related publication Class 2021 et al.
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