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EXPLORING CARBON CYCLING IN SELECTED MICRO-ORGANISMS EXPOSED TO TERRESTRIAL CARBON SEQUESTRATION

South Africaâs economy is primarily driven by the utilization of coal to provide electricity, which results in more fossil fuels to be burnt that contributes towards global warming. The average daily temperature is estimated to rise between 1.1 to 6.4ËC by 2100. Carbon sequestration is a technology that can limit CO2 emission into the atmosphere by storing the CO2 away in oceans or the terrestrial subsurface. South Africa is focusing on geological storage at depths of 1 000 m. Limited scientific knowledge is available on the direct impact when large amounts of supercritical CO2 is injected into the subsurface. This includes the diversity of the deep subsurface microbial communities as well as their ecosystems and biogeochemical processes.
The main aim of this project was to use selected deep subsurface micro-organisms (T. scotoductus, Geobacillus sp. GE-7 and Geobacillus sp. A12) and an organism that was known to grow under pressure (E. limosum) and introduce them to CCS conditions using a high pressure syringe incubator system.
The identities of the selected micro-organisms were verified using molecular techniques, the genomes of these micro-organisms were retrieved and information regarding possible CO2 fixation pathways was verified using the Metacyc database collection. The CO2 fixation pathways of interest were the Calvin cycle, the reductive acetyl Co-enzyme A and the reductive citric acid cycles. Surprisingly, T. scotoductus and E. limosum were able to remain viable and metabolically active even at 100 bar and 100% CO2. This has never been previously reported in literature. However Geobacillus sp. GE-7 and Geobacillus sp. A12 could not remain viable when the pressure was increased from 2 bar to 20 bar or higher.
The outcomes of this study indicate that the interactions between supercritical CO2 and the subsurface organisms should be considered as biogeochemical cycling. However, these interactions in the subsurface are still relatively unknown and the availability of interactive metabolic pathways indicate that the subsurface communities could survive and interact with this introduced substrate.

Identiferoai:union.ndltd.org:netd.ac.za/oai:union.ndltd.org:ufs/oai:etd.uovs.ac.za:etd-10272014-163824
Date27 October 2014
CreatorsChen, Jou-an
ContributorsMs M Erasmus, Prof J Albertyn, Prof E van Heerden
PublisherUniversity of the Free State
Source SetsSouth African National ETD Portal
Languageen-uk
Detected LanguageEnglish
Typetext
Formatapplication/pdf
Sourcehttp://etd.uovs.ac.za//theses/available/etd-10272014-163824/restricted/
Rightsunrestricted, I hereby certify that, if appropriate, I have obtained and attached hereto a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dissertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to University Free State or its agents the non-exclusive license to archive and make accessible, under the conditions specified below, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report.

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