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Basic Research Needs for Geosciences - Energetics Meetings and ...

Basic Research Needs for Geosciences - Energetics Meetings and ...

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APPENDIX 1: TECHNICAL PERSPECTIVES RESOURCE DOCUMENTFigure 6. Conceptual risk profile of a geological carbon sequestration site. Vertical axis isleakage risk. Overall, risk decreases dramatically post-injection <strong>and</strong> then more gradually.Courtesy of S. Benson 2006.manifestation. In addition, rapid mineral dissolution <strong>and</strong> release of metals <strong>and</strong> volatile organiccompounds may result from such leakage (e.g., Kharaka et al. 2006). Cement carbonation aroundwellbores can change physical <strong>and</strong> rheological properties (e.g., Carey et al. 2006). Aging,corrosion, <strong>and</strong> shifting of completion materials can cause leaks (IEA GHG 2006), <strong>and</strong>mechanical well failure by shear on bedding <strong>and</strong> fault planes presents a real hazard to long-termoperations <strong>and</strong> storage effectiveness (Bruno 2001).Wells in CO 2 -enhanced oil recovery areas do not appear to have high failure rates, <strong>and</strong> manytechnologies exist to plug <strong>and</strong> mitigate leakage even from major well failures (e.g., Lynch et al.1985). However, “sweet” corrosion (no sulfur) <strong>and</strong> an increased incidence of blowouts in CO 2 -enhanced oil recovery areas have grown as concerns over the last 10 years (Skinner 2003),although there are proactive operational measures to prevent <strong>and</strong> mitigate CO 2 blowouts. Ingeneral, the reported events generally have not received scientific study, <strong>and</strong> it is possible thatprocesses with long time-scale effects (e.g., well-bore corrosion) have not yet reached keythresholds. Major issues that will need to be considered are location <strong>and</strong> construction of existingwells, methods used to seal old wells, availability of methods to seal surface leaks, <strong>and</strong> theatmospheric risk associated with releases as a function of location <strong>and</strong> weather conditions (e.g.,Bogen et al. 2006).Substantial uncertainty remains around the nature of the long-term wellbore environment atdepth, the presence <strong>and</strong> stability of fractures within <strong>for</strong>mations near wells, the condition <strong>and</strong>distribution of cement around well casings, <strong>and</strong> the static <strong>and</strong> dynamic relationships betweenrock, casing, cement, <strong>and</strong> plugs (IEA GHG 2006). Key processes remain poorly parameterized,such as the degree <strong>and</strong> nature of <strong>for</strong>mation damage in the wellbore environment, the bondingprocess, <strong>and</strong> permeability dynamics in CO 2 -rock-brine-casing-cement systems.Appendix 1 • 20<strong>Basic</strong> <strong>Research</strong> <strong>Needs</strong> <strong>for</strong> <strong>Geosciences</strong>: Facilitating 21 st Century Energy Systems

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