How pressure buildup and CO[subscript 2] migration can both constrain storage capacity in deep saline aquifers
Name
Szulczewski-2011-How pressure buildup.pdf
Size
281.12 KB
Format
Adobe PDF
Checksum (MD5)
24ce3de9cbfd8b80e0d644ac77f147bf
Author(s) • •
MacMinn, Christopher W.
Szulczewski, Michael L.
Juanes, Ruben
Date Issued
April 2011
Journal
Energy Procedia
Publisher
Elsevier
Citation
Szulczewski, M.L., C.W. MacMinn, and R. Juanes. “How Pressure Buildup and CO[subscript 2] Migration Can Both Constrain Storage Capacity in Deep Saline Aquifers.” Energy Procedia 4 (2011): 4889–4896.
Version
Final published version
Abstract
A promising way to mitigate global warming is to sequester CO[subscript 2] in deep saline aquifers. In order to determine which aquifers are the best for sequestration, it is helpful to estimate how much CO[subscript 2] they can store. Currently, this is difficult because both the pressure buildup from injection and the volume of available pore space have been identified as constraints, but have not been compared to determine which is more important. In this study, we evaluate their relative importance using simple, but dynamic models of how pressure rises during injection and how CO[subscript 2] becomes trapped in the pore space. Our results show that the more important constraint depends on the properties of the aquifer and how the CO[subscript 2] is injected.
MIT Department
Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
Terms of Use
Creative Commons Attribution
Persistent DSpace Link
DOI of Published Version
https://doi.org/10.1016/j.egypro.2011.02.457