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dc.contributor.authorMemon, Shoaib
dc.contributor.authorFeng, Runhua
dc.contributor.authorAli, Muhammad
dc.contributor.authorBhatti, Masood Ahmed
dc.contributor.authorGiwelli, Ausama
dc.contributor.authorKeshavarz, Alireza
dc.contributor.authorXie, Quan
dc.contributor.authorSarmadivaleh, Mohammad
dc.date.accessioned2021-12-21T12:42:38Z
dc.date.available2021-12-21T12:42:38Z
dc.date.issued2021-11
dc.identifier.citationMemon, S., Feng, R., Ali, M., Bhatti, M. A., Giwelli, A., Keshavarz, A., … Sarmadivaleh, M. (2021). Supercritical CO2-Shale interaction induced natural fracture closure: Implications for scCO2 hydraulic fracturing in shales. Fuel, 122682. doi:10.1016/j.fuel.2021.122682
dc.identifier.issn0016-2361
dc.identifier.doi10.1016/j.fuel.2021.122682
dc.identifier.urihttp://hdl.handle.net/10754/674135
dc.description.abstractMulti-stage hydraulic fracturing has been identified as a must to develop shale gas reservoirs by increasing the stimulated reservoir volume (SRV). Supercritical CO2 (scCO2) has been studied as an alternating fracturing fluid due to its tendency to solve numerous problems associated with conventional aqueous based hydraulic fracturing such as formation damage, clay swelling, water scarcity and ground water contamination. However, its consequences to the host rock are not well understood. It has been recognized that scCO2-shale interaction alters the petrophysical properties during the long-term exposure of shale into scCO2, far little attention has been paid to understand the impact of this process for the short term. Thus, laboratory fracturing experiments using scCO2 on cubic shale samples (50 × 50 × 50 mm) in true triaxial stress cell (TTSC) were conducted. X-ray computed tomography (CT) imaging and low-pressure N2 adsorption were also performed to gain a deeper understanding of the fluid-rock interactions on the studied shales at a short-time process. Post-fracturing x-ray CT scans revealed a significant reduction, in the range of 14% to 46%, in the aperture of the natural fractures, indicating towards a possible scCO2 induced swelling. Mechanical compression test on the sample results in around 12% reduction in the fracture aperture, ruling out the possibility of confining stress being the key factor behind the fracture closure observed during fracturing. scCO2 soaking and N2 adsorption experiments showed the narrowing down of the macropores after scCO2 treatment implying the adsorption swelling as one of the controlling factors for the reduction of fracture aperture. Taken together, our results suggest that scCO2-shale interactions during the short term process of hydraulic fracturing can contribute to decreasing the conductivity of pathways between matrix and hydraulic fractures and hence adversely affecting the post-fracturing productivity of the rock.
dc.description.sponsorshipThe author acknowledges the support provided by the Australian Government and Curtin University for providing the funding under their Research Training Program Scholarship and provision of the required support, facilities, and equipment for this research. The author is thankful to Edith Cowan University and Commonwealth Scientific and Industrial Research Organisation (CSIRO), specially Mr. Shane Kager, Dr. Joel Sarout, Dr. Jeremie Dautriat, Dr. Lionel Estebin, Mr. Michael Verall, Mr. David Nguyen and Mr. Hamed Akhondzadeh, for providing support and access to their laboratory equipment. The author is also grateful to the National Geosequestration Laboratory (NGL) of Australia for providing funding to build the stress cell. Funding for this facility was provided by the Australian Federal Government. In addition, the author would like to appreciate the support provided by Pawsey Supercomputing Centre with funding from the Australian Government and the Government of Western Australia in providing access to their data analysis and visualisation resources. In the end, the author is thankful to Dr. Jamiu Ekundayo and Mr. Faaiz Al-shajalee for their special assistance during revision of this manuscript.
dc.publisherElsevier BV
dc.relation.urlhttps://linkinghub.elsevier.com/retrieve/pii/S0016236121025485
dc.rightsNOTICE: this is the author’s version of a work that was accepted for publication in Fuel. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Fuel, [, , (2021-11)] DOI: 10.1016/j.fuel.2021.122682 . © 2021. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectSupercritical Carbon dioxide
dc.subjectFracturing
dc.subjectscCO2-shale interactions
dc.subjectAdsorption swelling
dc.subjectNatural fractures
dc.subjectShale
dc.titleSupercritical CO2-Shale interaction induced natural fracture closure: Implications for scCO2 hydraulic fracturing in shales
dc.typeArticle
dc.contributor.departmentPhysical Science and Engineering (PSE) Division
dc.identifier.journalFuel
dc.rights.embargodate2023-11-01
dc.eprint.versionPost-print
dc.contributor.institutionWestern Australia School of Mines: Minerals, Energy and Chemical Engineering, Curtin University, 26 Dick Perry Avenue, Kensington, WA 6151, Australia
dc.contributor.institutionPremier Oilfield Solutions PVT LTD, Sector I-11/2 Islamabad, Pakistan
dc.contributor.institutionCSIRO Energy, Australian Resources Research Centre (ARRC), 26 Dick Perry Avenue, Kensington, WA 6151, Australia
dc.contributor.institutionSchool of Engineering, Edith Cowan University, 270 Joondalup Drive, Joondalup, WA 6027, Australia
dc.identifier.pages122682
kaust.personAli, Muhammad
dc.identifier.eid2-s2.0-85120937942


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