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CO2 Sequestration through Deep Saline Injection and ...

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[56], <strong>and</strong> is accessible from most locations in the basin, it also has potential for <strong>CO2</strong> leakage<br />

along the many wells that have been drilled into or <strong>through</strong> the formation. The wells are<br />

distributed over most of the 468,000 km 2 area, giving an overall average well density of 1 well<br />

every 2 km 2 . Over half of all wells that penetrate the Viking aquifer are classified as ab<strong>and</strong>oned<br />

wells [54]. This concern will be addressed in detail below.<br />

5.2. TRAPPING MECHANISMS AND SEQUESTRATION CAPACITY<br />

Upon injection into saline aquifers, <strong>CO2</strong> may be stored by one or more of three processes,<br />

hydrodynamic trapping, solubility trapping, or mineral trapping [7]. The most critical concern of<br />

hydrodynamic trapping is the potential for <strong>CO2</strong> leakage <strong>through</strong> imperfect confinement.<br />

Solubility trapping is not subject to buoyancy <strong>and</strong> is therefore less likely to leak. In mineral<br />

trapping, <strong>CO2</strong> is stored for very long periods by conversion into carbonate. Solubility <strong>and</strong><br />

mineral trapping are the most important long term solutions to <strong>CO2</strong> sequestration in geologic<br />

media [29], while hydrodynamic trapping represents the crucial short term step in the trapping<br />

process, as <strong>CO2</strong> must remain hydrodynamically trapped for sufficient time to allow the other<br />

processes to take hold.<br />

Figure 35<br />

Alberta Basin Stratigraphy [57]<br />

5.2.1. Hydrodynamic Trapping<br />

Crucial to all mechanisms of <strong>CO2</strong> capture in a reservoir system is the ability of the reservoir to<br />

maintain the injected volume of <strong>CO2</strong> for a sufficient residence time for other mechanisms to<br />

succeed (hydrodynamic trapping). Hydrodynamic trapping may occur via the existence of a<br />

slow transport gradient over a long distance or via structural traps which may serve to coral the<br />

<strong>CO2</strong> <strong>and</strong> prevent migration. In either case, caprock integrity is of primary interest to prevent<br />

leakage over an extended period of time. Accurate prediction of the hydrodynamic behavior of<br />

<strong>CO2</strong> is a complex venture into many critical parameters, <strong>and</strong> numerical modeling is often<br />

required. A detailed numerical modeling analysis has been conducted for this purpose, <strong>and</strong> is<br />

presented later in this report.<br />

46

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