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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The University of Texas at Austin
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ftdatacite:10.26153/tsw/42388 2024-03-31T07:52:15+00:00 Microbial influence on the kinetics of karstification ... Steinhauer, Elspeth Susan 2008 electronic https://dx.doi.org/10.26153/tsw/42388 https://repositories.lib.utexas.edu/handle/2152/115489 en eng The University of Texas at Austin Restricted Copyright © is held by the author. Presentation of this material on the Libraries' web site by University Libraries, The University of Texas at Austin was made possible under a limited license grant from the author who has retained all copyrights in the works. Karst formation Cave formation Karstification Limestone Bacteria Lower Kane Cave Wyoming Text article-journal Thesis ScholarlyArticle 2008 ftdatacite https://doi.org/10.26153/tsw/42388 2024-03-04T14:05:02Z 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 sulfuric acid speleogenesis (SAS). Here, acid produced by chemoautotrophic sulfur-oxidizing bacteria (SOB) corrodes limestone while producing dissolved calcium and sulfate. Little is known about the rate of limestone dissolution due to SOB activity, or the nature of the microbe-limestone attachment and interaction. The field site for this study is Lower Kane Cave, WY, an active SAS-formed cave where rapid steam H₂S oxidation is associated with sulfur-oxidizing microbial mats. In this study, the rate of limestone dissolution due to microbial oxidation of reduced sulfur compounds was investigated using laboratory and field microcosms. Laboratory chemostat chamber experiments were designed to mimic the cave environment ... Thesis Carbonic acid DataCite Metadata Store (German National Library of Science and Technology) Kane ENVELOPE(-63.038,-63.038,-73.952,-73.952) Sob’ ENVELOPE(66.156,66.156,66.322,66.322) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Karst formation Cave formation Karstification Limestone Bacteria Lower Kane Cave Wyoming |
spellingShingle |
Karst formation Cave formation Karstification Limestone Bacteria Lower Kane Cave Wyoming Steinhauer, Elspeth Susan Microbial influence on the kinetics of karstification ... |
topic_facet |
Karst formation Cave formation Karstification Limestone Bacteria Lower Kane Cave Wyoming |
description |
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 sulfuric acid speleogenesis (SAS). Here, acid produced by chemoautotrophic sulfur-oxidizing bacteria (SOB) corrodes limestone while producing dissolved calcium and sulfate. Little is known about the rate of limestone dissolution due to SOB activity, or the nature of the microbe-limestone attachment and interaction. The field site for this study is Lower Kane Cave, WY, an active SAS-formed cave where rapid steam H₂S oxidation is associated with sulfur-oxidizing microbial mats. In this study, the rate of limestone dissolution due to microbial oxidation of reduced sulfur compounds was investigated using laboratory and field microcosms. Laboratory chemostat chamber experiments were designed to mimic the cave environment ... |
format |
Thesis |
author |
Steinhauer, Elspeth Susan |
author_facet |
Steinhauer, Elspeth Susan |
author_sort |
Steinhauer, Elspeth Susan |
title |
Microbial influence on the kinetics of karstification ... |
title_short |
Microbial influence on the kinetics of karstification ... |
title_full |
Microbial influence on the kinetics of karstification ... |
title_fullStr |
Microbial influence on the kinetics of karstification ... |
title_full_unstemmed |
Microbial influence on the kinetics of karstification ... |
title_sort |
microbial influence on the kinetics of karstification ... |
publisher |
The University of Texas at Austin |
publishDate |
2008 |
url |
https://dx.doi.org/10.26153/tsw/42388 https://repositories.lib.utexas.edu/handle/2152/115489 |
long_lat |
ENVELOPE(-63.038,-63.038,-73.952,-73.952) ENVELOPE(66.156,66.156,66.322,66.322) |
geographic |
Kane Sob’ |
geographic_facet |
Kane Sob’ |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_rights |
Restricted Copyright © is held by the author. Presentation of this material on the Libraries' web site by University Libraries, The University of Texas at Austin was made possible under a limited license grant from the author who has retained all copyrights in the works. |
op_doi |
https://doi.org/10.26153/tsw/42388 |
_version_ |
1795031279053307904 |