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Variation of the Carbon Isotope Composition in Some Natural Processes

dc.contributor.advisorThode, H. G.
dc.contributor.authorTaylor, Edwin William
dc.contributor.departmentChemistryen_US
dc.date.accessioned2019-03-24T20:48:40Z
dc.date.available2019-03-24T20:48:40Z
dc.date.issued1955-10
dc.description.abstractThe variation in the carbon isotope composition of the cap rock of Texas and Louisiana sulphur wells was investigated by means of a simultaneous collection mass spectrometer. These rocks showed anomalously large depletions in C-13. The isotope depletion in the decarboxylation of pyruvic acid, both by chemical means and by bacteria, was measured and the isotope composition of the carbon dioxide released was found to be similar to that of the cap rock. The hypothesis is advanced that the carbonate of the cap rock may have originated by the precipitation of carbon dioxide released in the bacterial decarboxylation of an organic substrate.en_US
dc.description.degreeMaster of Science (MSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/24144
dc.language.isoenen_US
dc.subjectisotopeen_US
dc.subjectcarbonen_US
dc.subjectTexasen_US
dc.subjectcap rocken_US
dc.subjectsulphur wellsen_US
dc.subjectLouisianaen_US
dc.subjectmass spectrometeren_US
dc.subjectdecarboxylationen_US
dc.titleVariation of the Carbon Isotope Composition in Some Natural Processesen_US
dc.typeThesisen_US

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