CO₂ charged brines changed rock strength and stiffness at Crystal Geyser, Utah: Implications for leaking subsurface CO₂ storage reservoirs

Journal Article · Fri Apr 06 00:00:00 EDT 2018 · International Journal of Greenhouse Gas Control

DOI:https://doi.org/10.1016/j.ijggc.2018.03.017· OSTI ID:1473934

Espinoza, D. Nicolas ^[1]; Jung, Hojung ^[1]; Major, Jonathan R.  ^[2]; Sun, Zhuang ^[1]; Ramos, Matthew J. ^[2]; Eichhubl, Peter  ^[2]; Balhoff, Matthew T. ^[1]; Choens, R. Charles ^[3]; Dewers, Thomas A. ^[3]

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1. Univ. of Texas, Austin, TX (United States). Dept. of Petroleum and Geosystems Engineering
2. Univ. of Texas, Austin, TX (United States). Bureau of Economic Geology. Jackson School of Geosciences
3. Sandia National Lab. (SNL-NM), Albuquerque, NM (United States). Geomechanics Dept.

CO₂ geological storage in saline aquifers results in acidification of resident brine. Chemical reactions between acidified brine and rock minerals lead to dissolution and precipitation of minerals at various time scales. Mineral dissolution and precipitation are often neglected in assessing the mechanical integrity of target storage formations, yet, changes in rock strength and deformational behavior can impact trapping mechanisms. This paper shows the impact of exposure to CO₂-charged brine on shear strength and stiffness of various outcrop rocks evaluated through triaxial testing. The tested rocks were exposed to CO₂-charged brine over geological time at a naturally occurring near-surface seepage along the Little Grand Wash Fault and Salt Wash Grabens, which include the Crystal Geyser site near the town of Green River, Utah. Prior work suggests that this site provides a near-surface structural analog for possible fault-controlled CO₂ leakage over time scales that exceed expected injection time scales (10–100 years). Results show mechanical alteration in various aspects: (1) CO₂-charged brine alteration at near-surface conditions results in mineral dissolution/precipitation and reduction of shear strength and brittleness of Entrada sandstone and Summerville siltstone samples, and (2) carbonate precipitation in fractured Mancos shale leads to matrix stiffening and fracture mineralization resulting in overall stiffer and likely tighter shale. Additional discrete element simulations coupled with a bonded-particle-model confirm the role of cement bond size alteration as one of the main controls for rock chemo-mechanical alteration in sandstones. The chemo-mechanical alteration path that mimics cement dissolution (under stressed subsurface conditions) results in vertical compaction and lateral stress relaxation. Overall, results show that rock exposure to CO₂-charged brine can impart distinct petrophysical and geomechanical changes according to rock lithology and location with respect to major CO₂ conduits. Finally, while mineral dissolution in the storage rock may result in undesired reservoir strains and changes of stresses, mineral precipitation downstream from a leakage path can help seal potentially induced fractures.

• Research Organization: Sandia National Lab. (SNL-NM), Albuquerque, NM (United States); Univ. of Texas, Austin, TX (United States)
• Sponsoring Organization: USDOE Office of Science (SC), Basic Energy Sciences (BES); USDOE National Nuclear Security Administration (NNSA)
• Grant/Contract Number: NA0003525; SC0001114
• OSTI ID: 1473934
• Report Number(s): SAND-2018-9986J; 667805
• Journal Information: International Journal of Greenhouse Gas Control, Vol. 73; ISSN 1750-5836
• Publisher: Elsevier
• Country of Publication: United States
• Language: English

Related Subjects

58 GEOSCIENCES
mechanical and chemical diagenesis
reactive fluid flow
mineral dissolution and precipitation
triaxial testing
DEM
fault reactivation