AAPG ANNUAL CONFERENCE AND EXHIBITION
Making the Next Giant Leap in Geosciences
April 10-13, 2011, Houston, Texas, USA
The Effect of Natural
CO2
Occurrence on CO2 Storage in Geological Formations
(1) ExxonMobil Upstream Research Company, Houston, TX.
Natural
CO2
occurrence can have significant impact on
CO2
injection performance and capacity estimation. The primary control on naturally occurring
CO2
in the Earth’s crust results from its origin. The generated
CO2
is further controlled by the migration processes, trapping mechanisms, and eventually, mineral-gas-fluid buffering interactions. We investigated the controls on natural occurring
CO2
, including its concentration as a function of temperature, mineralogy, and fluid chemistry. We coupled
CO2
thermodynamic modeling with field data to describe the geological controls on
CO2
occurrence, and refined a theoretical correlation for estimating
CO2
concentrations in geological formations. The primary observation used for estimating
CO2
volumetrics is that the partial pressure of
CO2
(pCO2) covaries with temperature, while the reservoir mineralogy plays a significant role in determining the pCO2 - T correlation. This trend can be related to pH buffering associated with minerals and pore water interactions based on fundamental thermodynamic principles. The theoretical correlation matches the field data reasonably well, and should apply to a wide range of
CO2
concentrations for reservoirs with constrained access to
CO2
rich fluids.
We applied
CO2
injection reactive transport modeling (RTM) to investigate how natural occurring
CO2
affect
CO2
storage. Our RTM simulates large-scale
CO2
injection into subsurface reservoirs, with the ability to capture the complex interplay of multiphase flow, capillary trapping, diffusion, convection, and chemical reactions. The simulation results suggest that reservoirs with initial
CO2
concentration below the buffering capacity tend to favor
CO2
storage with higher solubility trapping, resulting in smaller
CO2
plumes that can be better contained by structural trapping. The under saturation conditions also help to avoid potential mineral precipitation and formation damage near the injection well and therefore, is a better choice for
CO2
storage over reservoirs with initial
CO2
exceeding the buffering capacity. We also investigated
CO2
injections in different types of siliciclastic and carbonate reservoirs. This study expanded our fundamental understanding of
CO2
occurrence, buffering and
sequestration
processes at multiple spatial and temporal scales in nature. The results can help us make better judgments of
CO2
storage capacity and site selection from appraisal to development to monitoring.