Geologic carbon storage (GCS) is a rapidly evolving technology
with the potential to reduce the environmental impact of fossil fuel
usage. Saline aquifers, which comprise a sandstone matrix with brine
contained in the pores, make up much of the pore space available for
CO2 storage in the United States. When CO2 is
injected in saline aquifers, however, capillary fingering occurs,
and only a small percentage of the pore space is filled with CO2. This fingering effect is due to the low viscosity of CO2, which is roughly ten times less viscous than brine. To address
this problem, we tested the ability of inexpensive, commercially available
nonionic surfactants to be dissolved in injected CO2 and
increase the apparent viscosity of CO2 by generating CO2-in-water foams in situ. We focused our study on nonionic
tridecyl ethoxylate surfactants with the number of ethoxylate groups
ranging from 11 to 18 (TDA-11, TDA-13, TDA-15, TDA-18). These surfactants
exhibited sufficient CO2-solubility and were shown to reduce
the CO2-brine interfacial tension (IFT), stabilize bulk
CO2-in-brine foams, and reduce the mobility of CO2 during core floods of CO2 in brine-saturated Berea sandstone.
The surfactants did not alter the wettability of the Berea sandstone.
Modeling results showed that in a reservoir field injection scenario,
the presence of TDA-11 (0.1 wt %) increased both the CO2 storage resource and storage efficiency by 17%. Simulations also
showed that the lateral extension area of the plume was reduced by
23% and that CO2 saturation within the plume increased
by 26%.