T234 Assessment and Characterization of Geologic Formations for Long-Term CO2 Storage (Sequestration)
Wednesday, 10 November 2004
1:30 PM - 5:30 PM
BASELINE MEASUREMENTS OF SOIL GAS EXCHANGE WITH THE ATMOSPHERE AT THE TEAPOT DOME SEQUESTRATION TEST SITE, WYOMING
Paper number: T234-13
Program: Technical Sessions
Time: 4:30 PM – 4:45 PM
Authors
Abstract
The average CO2 flux into the atmosphere at Teapot Dome was 227 mg m-2day-1, and for CH4 was 0.137 mg m-2day-1. Both positive (upward) and negative (downward) fluxes for CH4 were observed. Downward CH4 fluxes and sub-atmospheric CH4 concentrations were observed in soil gas due to methanotrophic oxidation below the frost line, with the system in very close balance. Concentrations of CO2 in soil gas averaged 618, 645, and 1010 ppmv at 30-, 60-, and 100-cm depth, respectively, contrasting with an average atmospheric concentration of 379 ppmv during the measurement period at Teapot. Stable carbon isotopic ratios indicated that soil gas CO2 was dominated by biological processes, even in the winter. Methane concentrations averaged 0.94, 0.92, and 0.92 ppmv, respectively, at 30-, 60-, and 100-cm. Ten-meter deep holes have been drilled at selected locations and equipped for nested gas sampling at five different depths.