Structural controls on the location and distribution of CO 2 emission at a natural CO 2 spring in Daylesford, Australia

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Secure storage of CO 2 is imperative for carbon capture and storage technology, and relies on a thorough understanding of the mechanisms of CO 2 retention and leakage. Observations at CO 2 seeps around the world find that geological structures at a local and regional scale control the location, distribution and style of CO 2 emission. Bedrock-hosted natural CO 2 seepage is found in the Daylesford region in Victoria, Australia, where many natural springs contain high concentrations of dissolved CO 2 . Within a few meters of the natural Tipperary Mineral Spring, small CO 2 bubble streams are emitted from bedrock into an ephemeral creek. We examine the relationship between structures in the exposed adjacent outcropping rocks and characteristics of CO 2 gas leakage in the stream, including CO 2 flux and the distribution of gas emissions. We find that degassing is clustered within ˜1 m of a shale-sandstone geological contact. CO 2 emission points are localised along bedding and fracture planes, and concentrated where these features intersect. The bubble streams were intermittent, which posed difficulties in quantifying total emitted CO 2 . Counterintuitively, the number of bubble streams and CO 2 flux was greatest from shale dominated rather than the sandstone dominated features, which forms the regional aquifer. Shallow processes must be increasing the shale permeability, thus influencing the CO 2 flow pathway and emission locations. CO 2 seepage is not limited to the pool; leakage was detected in subaerial rock exposures, at the intersection of bedding and orthogonal fractures. These insights show the range of spatial scales of the geological features that control CO 2 flow. Microscale features and near surface processes can have significant effect on the style and location and rates of CO 2 leakage. The intermittency of the bubble streams highlights challenges around characterising and monitoring CO 2 stores where seepage is spatially and temporally variable. CCS monitoring programmes must therefore be informed by understanding of shallow crustal processes and not simply the processes and pathways governing CO 2 fluid flow at depth. Understanding how the CO 2 fluids leaked by deep pathways might be affected by shallow processes will inform the design of appropriate monitoring tools and monitoring locations.




Roberts, J. J., Leplastrier, A., Feitz, A. J., Shipton, Z. K., Bell, A. F., & Karolytė, R. (2019). Structural controls on the location and distribution of CO 2 emission at a natural CO 2 spring in Daylesford, Australia. International Journal of Greenhouse Gas Control, 36–46.

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