5 CO2 Sequestration
Monday, 23 April 2012
8:40 AM - 12:00 PM
Room 202
CO2-BRINE-PORE MINERAL INTERACTIONS IN THE MOUNT SIMON, OHIO
Paper number: 5-7
Program: Theme Sessions
Time: 10:40 AM – 11:00 AM
Authors
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David R. ColeThe Ohio State University, Columbus, OH
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Michael V. MurphyThe Ohio State University, Columbus, OH
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Julia M. SheetsThe Ohio State University, Columbus, OH
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Susan A. WelchThe Ohio State University, Columbus, OH
Abstract
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.
Work is performed by the Subsurface Energy Materials Characterization and Analysis Lab at The Ohio State University, and is sponsored by the Dept. of Energy “Nanoscale Control of Geologic CO2” Energy Frontier Research Center. Core is provided by the Ohio Department of Natural Resources.