Pore scale CO2-brine-mineral interactions in an Ohio sandstone
Alexander M. Swift
The School of Earth Sciences, The Ohio State University
Columbus, Ohio, U.S.A.
[email protected]
The Mount Simon sandstone of western Ohio has been identified as a potential storage reservoir for CO2 derived from power plant point sources. Predicting how the Mount Simon will react to CO2 injection requires the development of kinetic models informed by the mineralogy of rocks accessible to CO2-bearing fluid. Advancing on previous efforts, we develop models of CO2-saturated brine in contact with rock that draw upon pore, rather than bulk, mineralogies. 2D mineral and pore scan raster maps of thin sections are obtained using a field emission gun scanning electron microscope (FEG-SEM) equipped with QEMSCAN software that compares backscattered electron (BSE) and characteristic x-ray signals against a database of standard mineral patterns. These methods permit the analysis of how micron-scale mineralogical heterogeneity varies over distances of tens of vertical meters.
The Geochemist’s Workbench is used to model interactions of CO2-saturated brine and rock at subsurface pressures and temperatures covering the range of natural values (8 – 32 MPa; 25 – 35 degrees C). Kinetic modeling tests the importance of parameters such as heterogeneity in modal mineralogy and pore versus bulk mineralogy on scenarios of CO2-brine-rock system evolution. When pore and bulk mineralogies are compared, it is found that certain relatively reactive minerals comprising minor proportions of the bulk rock, such as illite and chlorite, are sufficiently abundant adjacent to pores to become determining factors in the modeling of Ph-dependent solution chemistry.
AAPG Search and Discovery Article #90157©2012 AAPG Foundation 2012 Grants-in-Aid Projects