Microbial influence on the kinetics of karstification
The traditional model of karst and cave formation is that of carbonic acid limestone dissolution, where biologically-produced CO₂ in meteoric water reacts with and dissolves limestone. However, an alternative model has been proposed for several karst sysems where sulfide is abundant, known as sulfur...
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| Format: | Thesis |
| Language: | English |
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2008
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| Online Access: | https://hdl.handle.net/2152/115489 https://doi.org/10.26153/tsw/42388 |