| North-Central Section–40th Annual Meeting (20–21 April 2006) | |
| Paper No. 9-1 | |
| Presentation Time: 8:40 AM-9:00 AM | ||
A NEW DIGITAL GEOLOGIC MODEL FOR CARBON SEQUESTRATION PLANNING IN THE APPALACHIAN AND MICHIGAN BASINS | ||
|
VENTERIS, Erik R.1, MCDONALD, James1, CARTER, Kristin M.2, WELLS, Joseph G.1, SLUCHER, Ernie R.1, BARNES, David A.3, RADHAKRISHNAN, Premkrishnan4, SOLIS, Michael P.5, and LUCKHARDT, Catherine M.6, (1) Ohio Division of Geological Survey, 2045 Morse Rd, Bldg. C-1, Columbus, OH 43229-6693, Erik.Venteris@dnr.state.oh.us, (2) Bureau of Topographic and Geological Survey, 500 Waterfront Dr, Pittsburgh, PA 15222, (3) Geosciences, Western Michigan University, 1903 West Michigan Ave, Kalamazoo, MI 49008, (4) Indiana Geological Survey, Indiana Univ, 611 North Walnut Grove, Bloomington, IN 47405-2208, (5) Kentucky Geological Survey, 228 Mining and Mineral Resources Building, Lexington, KY 40506-0107, (6) Center for GIS, Towson University, Towson, MD 21252 Injecting carbon dioxide (CO2) into geologic reservoirs is a promising method to mitigate anthropogenic greenhouse gases. To facilitate planning, a regional-scale, digital geological model was created. This work was conducted for a seven-state area as part of U.S. DOE-funded projects including the Midwest Regional Carbon Sequestration Partnership –(MRCSP) and the NATional CARBon Geographic Information System (GIS) project (NATCARB). The study sought to determine areas where the geology was promising for CO2 injection, and to estimate storage capacity of various geologic units. A regional stratigraphic correlation chart was developed to identify major target horizons for injection and potential seal layers. Key geologic siting criteria were high porosity and permeability, presence of a confining layer (trap), and overburden greater than 2,500 feet (to maintain CO2 in a dense, supercritical state). Structure and isopach maps were constructed using geostatistical methods based on elevations derived from ~85,000 individual oil and gas well records. A regional digital map of oil and gas fields was produced to show locations of natural geologic reservoirs and to support future enhanced oil-recovery operations. Various GIS techniques were used to assemble these data sets into planning maps and tools. Structure and isopach maps, coupled with estimates of porosity, permeability, salinity and geothermal gradient were used to estimate the CO2 capacities for various units in the region. To provide conservative estimates, it was assumed that only 10 percent of the reservoir pore volume was available for injection. Capacities for both volumetric displacement and solution were calculated. For example, the Mt. Simon Sandstone was estimated to have 217 gigatonnes of capacity volumetrically, and 8.3 gigatonnes of solution capacity. CO2 emissions in the region from fixed point sources (power plants, steel mills, etc.) are about 750 million tonnes/ year, thus the Mt Simon alone could provide 100 to 200 years of storage capacity. | ||
|
North-Central Section–40th Annual Meeting (20–21 April 2006)
General Information for this Meeting | ||
| Session No. 9 Carbon Dioxide Sequestration: From the Atmosphere to Subsurface and All Points in between: Terrestrial, Geologic, and Applications Student Center, University of Akron: Room 316 8:40 AM-10:00 AM, Thursday, 20 April 2006 Geological Society of America Abstracts with Programs, Vol. 38, No. 4, p. 14 | ||
© Copyright 2006 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||