Volumetrics of CO{sub 2} Storage in Deep Saline Formations
Concern about the role of greenhouse gases in global climate change has generated interest in sequestering CO{sub 2} from fossil-fuel combustion in deep saline formations. Pore space in these formations is initially filled with brine, and space to accommodate injected CO{sub 2} must be generated by displacing brine, and to a lesser extent by compression of brine and rock. The formation volume required to store a given mass of CO{sub 2} depends on the storage mechanism. We compare the equilibrium volumetric requirements of three end-member processes: CO{sub 2} stored as a supercritical fluid (structural or stratigraphic trapping); CO{sub 2} dissolved in pre-existing brine (solubility trapping); and CO{sub 2} solubility enhanced by dissolution of calcite. For typical storage conditions, storing CO{sub 2} by solubility trapping reduces the volume required to store the same amount of CO{sub 2} by structural or stratigraphic trapping by about 50%. Accessibility of CO{sub 2} to brine determines which storage mechanism (structural/stratigraphic versus solubility) dominates at a given time, which is a critical factor in evaluating CO{sub 2} volumetric requirements and long-term storage security.
- Research Organization:
- National Energy Technology Lab. (NETL), Pittsburgh, PA, and Morgantown, WV (United States). In-house Research; National Energy Technology Laboratory (NETL), Pittsburgh, PA, Morgantown, WV (United States)
- Sponsoring Organization:
- USDOE Office of Fossil Energy (FE)
- DOE Contract Number:
- DE-FE0004000
- OSTI ID:
- 1129773
- Report Number(s):
- A-UNIV-PUB-036
- Journal Information:
- ENVIRONMENTAL SCIENCE & TECHNOLOGY, Vol. 47, Issue 1
- Country of Publication:
- United States
- Language:
- English
Similar Records
Predictive modeling of CO2 sequestration in deep saline sandstone reservoirs: Impacts of geochemical kinetics
Center for Frontiers of Subsurface Energy Security. Final Report