An Assessment
of Carbon Sequestration Options in the Mt. Simon of the Illinois Basin
Leetaru, Hannes1, Scott M.
Frailey1, David G. Morse1, Robert J. Finley1
(1) Illinois State Geological Survey, Champaign, IL
Deep, saline water-bearing reservoirs
offer the greatest potential for sequestration of large volumes of CO2.
In the Midwest, the most significant
saline reservoir is the Mt. Simon Sandstone. The Mt. Simon underlies one of the
largest concentrations of coal fired power plants in the world and this sandstone
may provide one of the most significant carbon storage resources in the United States. An assessment of any
potential Mt. Simon sequestration site must
include knowledge of its depositional history, current structural
configuration, and seal. An understanding of Mt. Simon geology alone is not
adequate for addressing the public concerns for a safe repository for the
permanent sequestration of CO2. For example, although there can be
as much as 2,000 feet of Mt. Simon sandstone present, numerical flow modeling
suggests that CO2 would migrate vertically and be primarily trapped
in the uppermost part of the formation. Therefore, site assessment must also be
concerned with the integrity of the caprock, formation capacity and
injectivity, and vertical heterogeneities that would slow the upward migration
of CO2 and allow greater interactions with CO2, water,
and rock.
Another public concern is whether the
deep native saline waters would discharge into shallower outcrops, subcrops, or
into freshwater regions of the same formation. Preliminary estimates using
pressure transient theory indicates small pressure (1< psi) changes occur 30
– 40 miles away from a single well after 30 years of injecting 1 Mtonne/year.