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Seasonal Dynamics of Gaseous CO2 Concentrations in a Karst Cave Correspond with Aqueous Concentrations in a Stagnant Water Column

Autor: Holger Class, Leon Keim, Larissa Schirmer, Bettina Strauch, Kai Wendel, Martin Zimmer

Publikováno v: Geosciences, Vol 13, Iss 2, p 51 (2023)

Dissolved CO2 in karst water is the key driving force of karstification. Replenishment of CO2 concentrations in karst water occurs by meteoric water that percolates through the vadose zone, where CO2 produced from microbial activity is dissolved. CO2

Externí odkaz: https://doaj.org/article/6ab1c87415cd478697c5102455840959

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Dynamics of seasonal CO2 concentrations above and below the karst-water table are influenced by density-driven transport: monitoring data from a cave in the Swabian Jura and interpretation with numerical simulation models

Autor: Holger Class, Leon Keim, Larissa Schirmer, Bettina Strauch, Kai Wendel, Martin Zimmer

Publikováno v: Abstracts

It is long known that dissolved aqueous CO2 is the key driving force of chemical reactions leading to rock corrosion, which is denoted as karstification. Accordingly, it is evident that meteoric water percolating through the biologically active vados

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9cba14fb55e14a094c9d32f13088f51e
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019488

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