2001
DOI: 10.1071/aj00041
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The Search for Sites for Geological Sequestration of Co2 in Australia: A Progress Report on Geodisc

Abstract: The APCRC GEODISC research program has encountered many challenges looking for geological sequestration sites for CO2, but has also found some solutions. Challenges already faced have been in effectively searching databases, developing uniform terminology and evaluation methodology, establishing comparative quality assessment of Australia’s sequestration sites against each other and against those from overseas, improving our understanding of the injection and trapping properties of CO2 and predicting its effec… Show more

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Cited by 31 publications
(18 citation statements)
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“…However, high injection pressure generates new fractures or reactivates existing faults in the rock mass, causing seismic activities. Supercritical CO 2 then leaks out along the new fractures and the reservoir seal is reduced, as shown by earlier studies (Rigg et al 2001;Sminchak et al 2002). Possible damage to the cap rocks caused by excessive CO 2 injection pressure could also lead to leakage.…”
Section: Introductionmentioning
confidence: 49%
“…However, high injection pressure generates new fractures or reactivates existing faults in the rock mass, causing seismic activities. Supercritical CO 2 then leaks out along the new fractures and the reservoir seal is reduced, as shown by earlier studies (Rigg et al 2001;Sminchak et al 2002). Possible damage to the cap rocks caused by excessive CO 2 injection pressure could also lead to leakage.…”
Section: Introductionmentioning
confidence: 49%
“…Are there viable natural resources at the site that may be compromised, e.g. proven petroleum system, groundwater, coal or other natural resource Bradshaw et al, 2002;Rigg et al, 2001)?…”
Section: Carbon Capture and Storage (Ccs)mentioning
confidence: 99%
“…Research studies on the action of rock mechanics with pore fluid are gradually becoming problems of interest in the field of geotechnical engineering. The injection of artificial fluid into deep strata changes the pore pressure and fluid components and may lead to surface uplift, caprock rupture, and fault activation and induce earthquakes . For example, In Salah CO 2 geological sequestration project, the surface bulged upward at an average rate of 5 mm per year, causing the project to be halted temporarily .…”
Section: Introductionmentioning
confidence: 99%