420,000 year assessment of fault leakage rates shows geological carbon storage is secure
Carbon capture and storage (CCS) technology is routinely cited as a cost effective tool for climate change mitigation. CCS can directly reduce industrial CO 2 emissions and is essential for the retention of CO 2 extracted from the atmosphere. To be effective as a climate change mitigation tool, CO 2...
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Published in | Scientific reports Vol. 9; no. 1; p. 769 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
London
Nature Publishing Group UK
25.01.2019
Nature Publishing Group |
Subjects | |
Online Access | Get full text |
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Summary: | Carbon capture and storage (CCS) technology is routinely cited as a cost effective tool for climate change mitigation. CCS can directly reduce industrial CO
2
emissions and is essential for the retention of CO
2
extracted from the atmosphere. To be effective as a climate change mitigation tool, CO
2
must be securely retained for 10,000 years (10 ka) with a leakage rate of below 0.01% per year of the total amount of CO
2
injected. Migration of CO
2
back to the atmosphere via leakage through geological faults is a potential high impact risk to CO
2
storage integrity. Here, we calculate for the first time natural leakage rates from a 420 ka paleo-record of CO
2
leakage above a naturally occurring, faulted, CO
2
reservoir in Arizona, USA. Surface travertine (CaCO
3
) deposits provide evidence of vertical CO
2
leakage linked to known faults. U-Th dating of travertine deposits shows leakage varies along a single fault and that individual seeps have lifespans of up to 200 ka. Whilst the total volumes of CO
2
required to form the travertine deposits are high, time-averaged leakage equates to a linear rate of less than 0.01%/yr. Hence, even this natural geological storage site, which would be deemed to be of too high risk to be selected for engineered geologic storage, is adequate to store CO
2
for climate mitigation purposes. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 2045-2322 2045-2322 |
DOI: | 10.1038/s41598-018-36974-0 |