SPE Reservoir Evaluation & Engineering
Volume 13,
Number 5,
October 2010,
pp. 791-804
Summary
The solubility of carbon dioxide (CO2) in underground saline
formations is considered to offer significant long-term storage capability to
effectively sequester large amounts of anthropogenic CO2. Unlike
enhanced oil recovery (EOR), geosequestration relies on longer time scales and
involves significantly greater volumes of CO2. Many geosequestration
studies assume that the initial brine state is one containing no dissolved
hydrocarbons and, therefore, apply simplistic two-component solubility models
starting from a zero dissolved-gas state. Many brine formations near
hydrocarbons, however, tend to be close to saturation by methane
(CH4). The introduction of excess CO2 in such systems
results in an extraction of the CH4 into the CO2-rich
phase, which, in turn, has implications for monitoring of any sequestration
project and offers the possibly additional CH4 mobilization and
recovery.
© 2010. Society of Petroleum Engineers
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History
- Original manuscript received:
7 July 2009
- Meeting paper published:
5 October 2009
- Revised manuscript received:
18 February 2010
- Manuscript approved:
11 May 2010
- Published online:
11 October 2010
- Version of record:
27 October 2010